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THE NEW ZEALAND ALPS

Printed by
Spottiswoode and Co., New-Street Square
London


[Illustration:

[Wheeler & Son, Photo.

G. E. Mannering      Mr. J. Dixon      P. H. Johnson
CLIMBING PARTY ON THE TASMAN GLACIER]


WITH AXE AND ROPE
IN
THE NEW ZEALAND ALPS

by

GEORGE EDWARD MANNERING

Member of the New Zealand Alpine Club
Member of the Royal Geographical Society of Australasia
Member of the Philosophical Institute Of Canterbury, N.Z.

With Illustrations






London
Longmans, Green, and Co.
And New York: 15 East 16^{th} Street

1891

All rights reserved




  THIS BOOK IS DEDICATED
  TO ALL LOVERS OF NATURE




PREFACE


This short work contains the story of five seasons’ climbing and
exploring in the New Zealand Alps. Most of the material embodied in it
has already appeared from time to time, in rather a different form, in
the Christchurch (N.Z.) ‘Weekly Press.’

The author trusts that the publication of the same in book form,
together with a map of the locality and a few photographic
reproductions, will supply a want in the shape of a guide-book to the
Alpine mountain district which is already beginning to be felt by
tourists in New Zealand; and he hopes that the contents may not prove
uninteresting to the general public, more especially to Swiss and
Caucasian climbers, few of whom are perhaps aware of the extent and
nature of the New Zealand Alpine chain.

The map is compiled by the New Zealand Government Survey Office from
the work of Mr. T. N. Brodrick, Government Surveyor, and that of Dr.
R. von Lendenfeld. The illustrations are from photographs by Messrs.
Wheeler and Son. Their operator has in several mountain expeditions
accompanied the author, who takes this opportunity of expressing his
thanks to the New Zealand Government Survey Department, and to Messrs.
Wheeler, for their kind assistance.

It will doubtless be said that the summit of Aorangi has not yet been
attained: quite true. Like Mr. Green, the author and his friend were
‘wise in time.’ Yet it is only a quibble to dispute the ascent of the
mountain, for being on the ice-cap of Aorangi is like being on the
topmost rung of a ladder, and yet not upon the projections above that
step.

  CHRISTCHURCH, NEW ZEALAND:
  _April 13, 1891_.




CONTENTS


    CHAPTER I

    INTRODUCTORY

           PAGE

    The New Zealand Alps and their glaciers      1


    CHAPTER II

    THE ROUTE TO THE MOUNT COOK DISTRICT

    A short description of the route to the Mount Cook district, and of
    the topographical features of the Mueller, Hooker, and Tasman
    Valleys                                                        5


    CHAPTER III

    FIRST ATTEMPT TO CLIMB AORANGI

    First impressions—Swagging—The Hochstetter Glacier—Defeat—The
    perils of river crossing                                      14


    CHAPTER IV

    SECOND ATTEMPT TO CLIMB AORANGI

    A flooded camp in the Tasman Valley—Hard struggles—We reach
    Green’s bivouac                                               32


    CHAPTER V

    THIRD ATTEMPT TO CLIMB AORANGI

    Photography on the Tasman Glacier—Attempt to scale Mount De la
    Bêche                                                         42


    CHAPTER VI

    ASCENT OF THE HOCHSTETTER DOME

    Camp under De la Bêche—Twelve hours on snow and ice—The
    pangs of hunger                                               58


    CHAPTER VII

    FOURTH ATTEMPT TO CLIMB AORANGI

    We reach the Great Plateau at last—Defeat again—The crossing of
    the Ball Pass                                                 65


    CHAPTER VIII

    FIRST EXPLORATION OF THE MURCHISON GLACIER

    Hard swagging—Erroneous maps—The struggle for Starvation
    Saddle—Exhaustion and hunger—Return                           76


    CHAPTER IX

    FIFTH ATTEMPT TO CLIMB AORANGI

    Avalanches—The bivouac again—First attempt repulsed—Second
    attempt—The Great Plateau—The Linda Glacier—Hard work
    step-cutting—The terrible _couloirs_—Victory at last—Descent
    by lantern-light—Back to civilisation                         90


    CHAPTER X

    ON SOME OF THE PHENOMENA OF GLACIERS

    The cause of glaciers—Formation and structure—Motion—Moraines:
    Lateral, medial, and terminal—‘Surface’
    moraines—Crevasses—Moulins—Glacier tables—Glacier cones—Surface
    torrents—Avalanches—Cornices                                 109


    CHAPTER XI

    CANOEING ON THE NEW ZEALAND RIVERS

    The Waimakariri—The enormous rainfall—Descent of the Waitaki
    River—The Tasman branch—Lake Pukaki—Leaky canoes—The
    Pukaki Rapids—The Waitaki Gorge—Out on the plains again—Sixty
    miles paddle to catch the train—Home once more               119


    L’ENVOI                                                      131

    APPENDIX                                                     133

    A SHORT GLOSSARY OF TECHNICAL ALPINE TERMS                   139




LIST OF ILLUSTRATIONS

  CLIMBING PARTY ON THE TASMAN GLACIER                   _Frontispiece_

  HOOKER VALLEY AND MOUNT SEFTON FROM GOVERNOR’S CAMP  _To face page_ 8

  AORANGI: MOUNT COOK AND THE HOOKER GLACIER                 ”       10

  MOUNT TASMAN (11,475 FEET) AND HOCHSTETTER ICE-FALL        ”       28

  MOUNT COOK AND THE HERMITAGE                               ”       46

  CROSSING THE HOOKER RIVER                                  ”       48

  AORANGI FROM THE BALL GLACIER                              ”       50

  ICE CAVE, TASMAN GLACIER                                   ”       52

  MOUNT DE LA BÊCHE (10,021 FEET) FROM THE TASMAN GLACIER    ”       54

  PEAKS ON MALTE BRUN                                        ”       58

  THE TASMAN GLACIER                                         ”       66

  MOUNTAIN LILIES (_Ranunculus Lyallii_)                     ”       86

  LOOKING ACROSS THE MURCHISON GLACIER                       ”       90

  AORANGI FROM THE TASMAN GLACIER                            ”       90

  THE MURCHISON GLACIER                                      ”       92

  AORANGI: THE HIGHEST PEAK                                  ”      100

  IN THE ICE-FALL OF THE ONSLOW GLACIER                      ”      120

  THE SURFACE OF A GLACIER                                   ”      128

  MAP                                                          _At end_




CHAPTER I

INTRODUCTORY

_The New Zealand Alps and their glaciers_


It is unnecessary for me in these days of universal education and
enlightenment to describe the geographical position of New Zealand, the
‘Britain of the South,’ and the future playground of Australasia.

Everyone knows that New Zealand consists of three islands, situate
between the 34th and 47th degrees of south latitude, off the south-east
coast of Australia. Reference to almost any handbook of the colony will
furnish every information regarding settlement, population, government,
climate, and so on, and I do not propose to dwell longer than is
necessary on any general matters of this nature.

It is advisable, however, to describe in as brief and concise a manner
as possible the general physical features of a country containing such
varieties of scenery and climate, more especially those of the South
Island (or Middle Island as it is sometimes called), where the High
Alps and their wonderful glaciers are situated.

Speaking generally, the highest mountains of New Zealand may be said to
run in a north-easterly direction from the southernmost point of the
South Island through the whole country, like a vast backbone, to the
north-eastern point of the North Island.

The main formation of the mountains dates back to Jurassic times, so
that the geological structure may be said to be one of great antiquity.

Volcanic action has long since ceased throughout the South Island;
but there are many active volcanoes in the North, where a perfect
wonderland of hot-springs, solfataras, and silica terraces exists.

As a whole, the country is heavily timbered—more thickly on the
western parts, where the greater rainfall occurs. This is notably the
case in the South Island, where the hot and moisture laden winds from
tropical regions are deprived by the Alpine chain of their aqueous
vapour.

The Southern Alps proper may be said to extend over a distance of about
one hundred miles of the middle part of the South Island, the chain
being situated closer to the western than the eastern ocean. The slopes
on the western side are the more precipitous, and are clothed with
heavy timber and intersected by innumerable mountain torrents, fed in
most cases by glaciers, some of which descend to within 600 feet of
sea-level.

Ranges of outlying foot-hills occur on the eastern side, snow-covered
in winter, amongst which many large glacier-fed rivers have cut their
way, and meander over the plains (probably of entirely fluviatile
formation) which slope gradually from the outer bases of the foot-hills
to the eastern ocean.

The peaks of the Alps range in height from 7,000 to 12,350 feet above
sea-level, the majority of those over 10,000 feet being contiguous to
the culminating point in altitude—Aorangi—more popularly known as
Mount Cook. Here also are found the largest glaciers.

The snow-line is a low one when compared with that of Alpine countries
in the northern hemisphere and in relative latitudes. It would be
difficult to compute its average altitude, but in parts where large
glaciers and snow-fields exist it is even as low as 5,000 feet above
sea-level.

By comparison with Switzerland, for instance, it may safely be said
that the snow-line in New Zealand is from 2,000 to 3,000 feet lower;
consequently we have the same Alpine conditions at a much lower level.
Owing to this interesting fact, we find that the New Zealand glaciers
attain far greater dimensions than those of Switzerland, although the
peaks do not rise to such a height above sea-level.

In themselves, I believe the mountains compare favourably as to size
or actual height above the valleys below them; Aorangi, for instance,
rising for nearly 10,000 feet from the Hooker Glacier, and Mount Sefton
8,500 feet from the Mueller Glacier, whilst the western precipices of
Mount Tasman (11,475 feet) are stupendous.

The enormous length attained in remote times by the New Zealand
glaciers is evident on all hands at the lower parts of the valleys,
the heads of which they now occupy; whilst the formation of nearly all
the lakes in the South Island can be traced to the action of ice and
the deposition of terminal moraines, prior to a period of retreat of
the ice.

There is an interesting feature in the glaciers of this country
peculiar to them; I refer to the deposition of singularly extensive
moraines. The lower parts of the large glaciers on the eastern slopes
are, in nearly every instance, completely covered with accumulated
_débris_ derived from the moraines. This is variously accounted for by
the antiquity of the mountain chain, the slow rate of motion in the
ice, and great denudation from rocks which are much jointed and offer
but little resistance to the splitting powers of freezing infiltrated
water.

The western glaciers I am not personally acquainted with, but I
understand that they do not carry anything like the amount of moraine,
and I imagine the cause of the disparity will be found in a faster
motion of the ice, and (a yet more potent factor) in the dip of the
strata of the rocks, which is from east to west, the broken faces being
eastward and the slab-like faces westward.




CHAPTER II

THE ROUTE TO THE MOUNT COOK DISTRICT

 _A short description of the route to the Mount Cook district, and of
 the topographical features of the Mueller, Hooker, and Tasman Valleys_


From Timaru on the east coast the traveller may comfortably reach the
glaciers of Aorangi in a two days’ journey.

Leaving Timaru by an evening train, Fairlie Creek (the present terminus
of the railway line) is reached, where the night is spent. Two days’
coaching then are required to cross over Burke’s Pass into the great
Mackenzie plains, across this great ancient glacier bed, past Lakes
Tekapo and Pukaki, over the rivers of the same names, and up the valley
of the Tasman River to a comfortable hostelry called ‘The Hermitage,’
nestling right under the shadow of that wonderful pile of ice-clad
mountain glory, Mount Sefton.

Lakes Tekapo and Pukaki may both be aptly compared in one way to the
Lake of Geneva, in that they are of glacier origin, and purify the
rivers which now flow from the present glaciers, parting with their
waters again through channels cut in the ancient terminal moraines
which dam their respective southern shores.

They are both beautiful, each in its own way—Tekapo sunny, peaceful,
and calm; Pukaki awe-inspiring and grand—but they lack the charm of
chalet and pine tree, of vine and meadow, which so adorn the shores of
the Swiss lakes.

The immediate vicinity of the road is uninteresting, except from a
geological point of view, for it winds about amongst old moraines,
whose vegetation consists almost entirely of the brown tussock grass so
general in the South Island.

Yet the geologist or student of glacier phenomena can read on the
surface the history of the formation; _roches moutonnées_ abound,
and, in places, old moraines are spread over the bed rock for miles
together, whilst erratic blocks are dotted about in various directions,
evidencing how extensive has been the action of the ice in ages gone by.

Though the scenes contiguous to the road may fail to charm the eye, the
distant panoramas of the glorious Southern Alps cannot fail to draw
forth expressions of wonder from the most callous observer. As the
Hermitage is approached, and the great peaks and glaciers draw closer
and closer, the marvellous grandeur of the chain is gradually realised.

The sight of the reflection of Aorangi in Lake Tekapo, on a calm
morning, is something to remember for a lifetime. The subject has long
been a favourite one for brush and pen, but no one yet has done it
justice.

A substantial bridge spans the exit of the Tekapo River, but only a
ferry stage exists at the Pukaki River where it leaves the lake. A wire
rope, 450 feet long, is thrown across the stream, to which the ferry
stage floating on two punts is attached by runners. The coach and four
is driven bodily on to the stage, and by the aid of a rudder the punts
are slued so as to point across the stream diagonally. The force of the
water rushing obliquely on to the sides of the punts drives the whole
affair across in a space of about three or four minutes. This ingenious
plan is commonly adopted in the New Zealand rivers.

During the months of winter it is possible to reach the Hermitage
direct from Tekapo, and thus avoid striking south to go round Lake
Pukaki, by crossing the Tasman River. During summer, however, as a
rule, this river is impassable, for it rises so fast during warm and
nor’-west weather from rain and melting snow that sometimes the whole
bed of the river—two miles wide—is a network of rushing yellow
torrents quite unfordable by man or beast.

Readers of the Rev. W. S. Green’s ‘High Alps of New Zealand’ will
recollect that his conveyance found a last resting-place in the
quicksands of the Tasman. Von Lendenfeld also, the year after Mr.
Green, experienced an unhappy week’s delay on the eastern bank of the
river. I have myself narrowly escaped drowning at the same point, and
in years gone by the Tasman River has been accountable for more than
one life.

The river in full flood is a sight to see; the water in places runs
fifteen knots an hour, or even more. In the rapids it is piled up in
the middle from sudden contraction of the banks, and forms crested
billows four or five feet in height, whilst now and then a block of ice
from the glacier may be seen bowling along.

The ancient glacier-formed terraces of the Tasman Valley are
instructive and interesting. The highest of them are distinctly marked
all down the valley for a distance of forty miles from Sebastopol—a
large face of ice-worn rock near the Hermitage—on the eastern slopes
of the Ben Ohau Range. The story of the ancient glacier can be read as
the eye follows these strange terraces from their starting point 2,000
feet above the valley bed, down a gentle declination to the terminus of
the Ben Ohau Range.

Before going into the narrative of my five seasons’ climbing amongst
the peaks and glaciers around Aorangi, it would be as well for me to
describe, as concisely as possible, the general topography of the
Mueller, Hooker, and Tasman Glaciers.

We will suppose ourselves in the main Tasman Valley, into which all
these glaciers drain, close to the point where the valley first
branches. As we look northward, Aorangi and the range running southward
for twelve miles from the main body of the mountain bound the view,
and divide the valley into two branches. Let us take the one to the
north-west first. Proceeding up this valley of the Hooker for a few
miles, we arrive at a branch valley from the left or west—the Mueller
Valley—completely occupied by the glacier of the same name. Close to
the Mueller Glacier is situated the Hermitage, presided over by Mr. F.
F. C. Huddleston, a true haven of refuge and comfort for the wearied
tourist or mountaineer.

[Illustration: HOOKER VALLEY AND MOUNT SEFTON FROM GOVERNOR’S CAMP

[_Wheeler & Son, Photo._]

We step on to the Mueller Glacier, here completely covered by moraine,
and, turning westwards, strike up its course. On our right, 8,500
feet above us, clad in ice and snow and glittering in the sunlight,
rises the glorious mass of Mount Sefton, showering down avalanches
upon the glacier. On our left the shingle slips from the rotten and
crumbling crags of the Sealy Range. It is possible for tourists who are
good walkers to reach the head of this glacier, which is seven and a
half miles long and about one mile broad, in one day. The moraine gives
way to the clear ice some three miles or so from the terminal face. Now
we return and make a fresh start up the Hooker Valley due northwards
from the Hermitage.

Crossing the Mueller Glacier we walk through a perfect garden of
lilies (_ranunculus Lyallii_), celmisias, ‘Spaniards,’ and an endless
variety of sub-alpine plants, for a distance of about one mile from
the northern side of the Mueller Glacier, when we come to the terminal
moraine-covered face of the Hooker Glacier.

On our right rises up the bold and verdure clad snow-topped Mount Cook
Range, Mount Wakefield (6,561 feet), Mount Mabel (6,868 feet), Mount
Rosa (6,987 feet), and a nameless peak (7,540 feet) being the principal
points of interest. On our left is the northern continuation of the
ridge of Mount Sefton, known as the Moorhouse Range, part of the main
chain of the Southern Alps. Several secondary glaciers descend from the
slopes, but do not reach the bed of the valley below, which is filled
from side to side with the Hooker Glacier.

Proceeding up the surface of the glacier we get on to the clear ice,
and now on either bank the mountains rise to a great height. On the
right Aorangi suddenly rears itself, from a point known as the Ball
Saddle (7,500 feet), to 12,349 feet in one stupendous rocky ridge,
upon which the ice hangs wherever it can get any hold. This ridge is
known to climbers as the Great Southern _arête_, and has been found,
first by Mr. Green and secondly by myself, to be inaccessible. Right
ahead of us pour down from the highest crags the Mona, Noeline, and
Empress Glaciers, to join the Hooker, alternating with very precipitous
rocky ridges which present every appearance of being quite unscalable.

Several attempts have been made by surveyors and others to reach the
saddle at the head of the Hooker, but it was only in December 1890 that
the efforts of two climbers (Mr. A. P. Harper and Mr. R. Blakiston)
were rewarded. The expedition can only be attempted with any chance of
success in the early part of the season, when the numberless crevasses
are yet covered with the winter snow.

From the Hooker Glacier we turn our faces downwards to the south again,
and pay a visit to the north-eastern branch of the main Tasman Valley.

Crossing the Hooker River at the terminal point of the Mount Cook
Range, where a cage swung on a wire rope over the river now facilitates
the traveller’s passage, we strike north-eastwards up the valley.

For a distance of four miles our way leads over the shingle and boulder
flats of the Tasman river-bed, here some two miles wide. Patches of
good sheep-feed consisting of tussock and cocksfoot grass (the latter
sown by an early settler) occur on the western side of the valley, but
the river as a rule washes the opposite slopes.

[Illustration: AORANGI: MOUNT COOK AND THE HOOKER GLACIER.

[_Wheeler & Son, Photo._]

Arriving at the terminal face of the glacier we strike up a small
valley between the western lateral slopes of the moraine of the
glacier and the Mount Cook Range on our left, and for a distance of
about seven or eight miles force our way through dense scrub and loose
boulders from the moraine and mountain slopes, to the junction of the
Ball Glacier with the Tasman. This Ball Glacier comes from the Great
Southern _arête_ of Aorangi, and is fed almost entirely by avalanches,
there being no snow-fields—or _névés_ as they are called in Alpine
parlance—of any great extent at its head.

From this point upwards we strike out on to the ice on our right,
and another seven miles or so brings us to a further division of
the valley, Mount de la Bêche being the dividing peak. The glacier
of the left-hand or northern branch is known as the Rudolf Glacier,
whilst the main body of the Tasman stretches some six miles further
north-eastwards to the Hochstetter Dome, where it again divides. The
saddle at the head of the left-hand branch, again, has been reached
by Dr. von Lendenfeld and by myself in our respective ascents of the
Hochstetter Dome, and commands a superb view of the Whymper Glacier and
valley, and of the Wataroa River on the west coast. The head of the
branch to the right of the Hochstetter Dome has not yet been reached by
man.

Taking a retrospective glance again at the peaks on either hand, and
commencing at the lower end of the glacier, we have first on our right
the Liebig Range till opposite the Ball Glacier, when the _embouchure_
of the Murchison Valley occurs, followed by the Malte Brun Range, with
the main peak—the Matterhorn of New Zealand—opposite to Mount de la
Bêche, then the Darwin Glacier followed by the mountain of the same
name, and then the saddle between Mount Darwin and the Hochstetter Dome.

Now, again, on the left or western side of the great glacier we have
the Mount Cook Range for ten miles, the Ball Glacier, Aorangi, the
Hochstetter Glacier, Mounts Tasman, Haast, Haidinger, Glacier Peak,
Mounts Spencer, Kant, Rudolf (at the head of the Rudolf Glacier), De la
Bêche, Green, and Elie de Beaumont, the last followed by the Lendenfeld
Saddle, to which I have already referred.

From Mount Tasman northwards to this saddle all these mountains are
situated in the main chain. Aorangi itself, though popularly believed
to belong to the main divide, is in reality separated from it by a
rocky ridge and a saddle of about 10,500 feet, which leads to the
Hooker Glacier on the one hand and the Linda on the other, both being
east of the main divide. Aorangi itself, therefore, consists of a
divergent ridge, the whole of whose drainage goes eastward.

Though for some years I have believed this to be the case, it is only
quite recently that I have been able to substantiate the belief by
ocular demonstration, when the ascent of the mountain was accomplished
by Mr. Dixon and myself. To this expedition I shall refer later on.

The reader must picture to himself the great Tasman Glacier, nearly two
miles in width and eighteen to twenty in length, occupying the whole
of the bed of the valley, and fed on both sides by numerous tributary
ice streams from the mountains.

Of the Murchison Valley it is not necessary for me to speak just now,
as the topographical features will be described when I come to tell the
story of its exploration. Neither is it needful to refer in further
detail to the Tasman for the same reason.




CHAPTER III

FIRST ATTEMPT TO CLIMB AORANGI

_First impressions—Swagging—The Hochstetter Glacier—Defeat—The
perils of river crossing_

‘To climb steep hills requires slow pace at first.’


It was on March 24, 1886, that I left Christchurch, in company with my
cousin, Mr. C. D. Fox, on my first visit to the great Tasman Glacier
and Mount Cook, or Aorangi.[1]

[Footnote 1: The Maori name of Mount Cook is ‘Aorangi,’ or, more
properly, ‘Ao-Rangi.’ The commonly accepted meaning of the term is
‘Sky-piercer’ but as the Maori language admits of many varieties of
translation, each version hovering about the region of true meaning,
it is only natural that authorities should differ as to the correct
construing of the word.

One good Maori scholar, whose reputation as such is almost pre-eminent,
gives the poetical translation of ‘Light of Day’—a singularly
beautiful one, for it is the first peak to catch the morning light and
the last to show the glow of evening.

Another very well-known Maori scholar, the Rev. J. W. Stack, assures
me that the most reasonable interpretation that can be put upon the
word ‘Ao-Rangi’ is ‘Scud Peak’; and this is a singularly apt one,
for the prevailing nor’-west winds always cause condensation and the
gathering of cloud-banners about the higher parts of the mountain.
‘Heaven-piercer’ and ‘Cloud-piercer’ are also often used, but are to a
certain extent fancy names.]

I often look back now with feelings of amusement at the audacity with
which we determined to make our first attempt to scale the great
monarch of the Southern Alps, and wonder how we could have been so
self-satisfied with our own powers and confident of our ability in
undertaking such a gigantic task. I can only suppose that it was
ignorance of what lay before us, and a clear case of ‘fools rush in
where angels fear to tread’; for when my thoughts run back over the
toils, hardships, and bitter lessons of experience undergone during
the past six years, and when I think of the position of two completely
inexperienced men (as far as _true_ Alpine work is concerned) launching
straight out into such an undertaking, my heart seems to quail at the
idea. It is true that we both had heard and read of much Alpine work,
and had been for some time in touch with climbing-men, also we were
both practised in hill-walking and accustomed to such work as mustering
sheep, pig-hunting, and shooting over what in England would be termed
rough mountains, so that as cragsmen we could scarcely be classed as
novices. As to any knowledge other than theoretical of the conditions
of snow and ice, however, we might be termed tyros, though Fox had
done a little scrambling on the Swiss glaciers. Nevertheless, we had
sufficient ‘cheek’ to consider ourselves wise and strong enough to go
straight into a really difficult piece of Alpine work, and, laughing at
all discouragement, we set off for the mountains.

I have already described the customary route to the glaciers of Mount
Cook, so will not weary my readers with a long narrative of the journey.

At Timaru (four hours by rail from Christchurch) we completed our stock
of provisions, consisting of biscuits, tinned meats, &c., and took the
evening train on to Fairlie Creek (forty miles further inland), where
on arrival we hired a horse and buggy and drove to Ashwick Station,
seven miles distant on the road to the mountains.

The next day’s journey took us over Burke’s Pass and into the Mackenzie
country, past the beautiful Lake Tekapo, and on to the ferry situate at
the southern end of Lake Pukaki.

The road itself winds through bleak tussock plains, interesting only
from a geological point of view; but all monotony of the immediate
surroundings is completely lost when one looks further afield and gazes
on the marvellous beauty of such scenes as the Southern Alps from Lake
Tekapo, or the Ben Ohau Range from the plains. Even the most fastidious
globe-trotter could not fail to be deeply impressed with such a picture
as Aorangi from Lake Pukaki.

To look at Aorangi from this approach is enough to damp the spirit of
the stoutest Alpine climber that ever breathed, and is quite sufficient
to account for the disbelief and incredulity cherished in the mind of
many a shepherd in the Mackenzie country regarding the possibility of
ascending the peak.

History repeats itself, and just as we hear of the native mountaineers
of the Himalayas, Andes, and Caucasus discrediting ascents of glacier
peaks around whose very bases they and their ancestors have lived and
died, so we find that our own countrymen, whose calling needs their
constant presence amongst their flocks on the lower ranges, refuse to
believe that mountains presenting such an appearance as Aorangi are in
any manner of way to be scaled.

The following day brought us to the Hermitage. A low mist had hidden
the higher peaks throughout the day, and led to a surprise on the
following morning which I little dreamt of.

I wonder if all Alpine climbers, in first ‘tasting the sweets of
climbing,’ are similarly impressed with their initial Alpine view!

No words of mine can describe the ecstasy which seemed to pervade my
whole being as on the early, cloudless morning the wonderful picture
of Mount Sefton reared itself in indescribable sunlit grandeur above
the old bush-clad moraine close by the Hermitage. Here, indeed, was a
new and a fairy-like world to live in. As we sat in the verandah of the
Hermitage the ice-seamed crags appeared to rise up and up until they
culminated in a long serrated and corniced ridge, seeming almost to
overhang the very spot where we rested.

A scene of mountain glory never to be forgotten, a memory to last a
lifetime!

More than 8,000 feet above us were built up those ice-clad precipices,
their glaciers glinting in the bright morning light, their avalanches
tearing down the mountain sides and waking the echoes of a hundred
ravines and valleys with their thunder.

Where is the man who can describe these

          palaces of Nature, whose vast walls
  Have pinnacled in clouds their snowy scalps?

Where is the mountaineer—not the mere gymnast, but the Nature-loving
mountaineer—who can tell the feelings of such a first impression?

And yet even this scene seems to fade in the memory and suffer by
contrast with those of other pictures in the New Zealand Alps, for up
the Tasman Valley, where later on in the day we wended our way, fresh
vistas of Alpine glory were unfolded to view.

Aorangi from the Hermitage is also a grand sight. The mountain seems
to possess a startling individuality and a majestic grandeur somewhat
different in character from its worthy neighbour Mount Sefton. The view
is more distant, but the bold outline of the peak stands out in relief
against the blue of the heavens, and rears a face of glacier-clad
precipices to a height of 10,000 feet above the Hooker Valley at the
mountain foot. Light clouds float about the peak and lend an ethereal
air to its beauty, imparting a fairy-like, floating appearance to the
peak itself. At other times the outlines are apparently clear cut
against the sky, giving an air of lasting and monumental dignity, and
conveying the idea of stability from past ages to ages to come.

After an early lunch, and accompanied by Mr. Huddleston (the landlord
of the Hermitage), and one of his men, we started off for the Tasman
Glacier. The first part of the way leads down over stony flats to the
termination of the Mount Cook Range, and at this point the Hooker River
is crossed.

On this occasion we double-banked over on horse-back without much
difficulty; but very often the Hooker River is quite impassable with
horses, the torrent being confined in a narrow boulder bed of about 200
feet in width, which in flood time, during the warmer months of spring
and summer, is quite filled with a roaring torrent, often bearing down
with it blocks of ice from the Mueller and Hooker Glaciers above.

Turning in a north-easterly direction round the end of the range we
shaped our course up the Tasman Valley, and in two hours’ time from
the Hermitage arrived at the terminal face of the great glacier, which
fills the whole of the valley from side to side, a width of about two
miles. Here, then, the hard work was about to begin, for the horses
could not proceed further, and it was necessary to carry everything
from this point on our own backs.

Ah! good reader, have you ever carried a swag, a _real_ swag—not a
Swiss knapsack—but a real, torturing, colonial swag? When you take it
up and sling it on your back in the orthodox fashion you remark: ‘Yes;
I think it _does_ weigh fifty pounds.’ In ten minutes your estimate of
its weight has doubled. In an hour you begin to wonder why Nature has
been so foolish as to make men who will carry swags; bad language seems
to slip out ‘quite in a casual way,’ and you begin to bend forward and
do the ‘lift.’ But the ‘lift’ does not seem to fulfil quite all that
is said in its praise, for soon the torturing burden settles down again
and drags on to your shoulders more heavily than ever. After a bit
of nice balancing over loose moraine the swag triumphs. Down you go,
and the wretched thing worries you, whilst you bark your fingers and
swear horribly, bruising your knees and shins, and cursing the day on
which you saw the light of a hard and feelingless world. You recover
and repeat the performance as before, and by the time your day’s work
is done you find out to your own demonstrated satisfaction that the
burden _weighs at least five hundred-weight_. You sling it off and give
it a malicious kick, with the result that you break a thermometer or
some such delicate instrument. Then you try to walk, but stagger about
like a drunken man; there is no small to your back, your back tendons
are puffy and tired like those of an old horse, your head swims, and
your eye is dim. Patience and rest, however, gradually bring you round,
and soon you regain strength and spirits in feeling that at least you
have conquered a day’s difficulties and have brought your board and
lodging so far with you.

Ah! think of it, you knapsack mountaineers, you feather-bed Swiss
mountaineers, with your tracks, your hotels, your guides, your porters,
and your huts. No; this New Zealand work is not like yours.

But then, you see, we are enjoying what you cannot get. Exploring
and opening out virgin fields, learning to be our own guides—and
porters—from that best of masters—hard experience.

We struck up the little valley which here exists between the lateral
moraine on our right and the hill on our left, and toiled on amidst
dense scrub so gnarled and matted that we could at times walk on it
as on a spring bed, though now and then going through, of course. The
scrub alternated with slopes of loose strips of moraine. By evening
we reached a little blue lake which feeds the creek issuing from the
valley’s mouth, and here we pitched our tent for the night.

The sub-Alpine vegetation here is interesting and varied. Wild Irishman
(_te matakuru_ of the natives or _matagowrie_ of the shepherds),
Spaniards, with leaves like carving-knives and points like needles,
having stalks sometimes eight or ten feet high; stunted totara, many
varieties of veronica, celmisias with large marguerite daisy-like
flowers, the beautiful white ranunculus, and a hundred bushes and
creepers all mixed up in the most glorious confusion amid rocks
sometimes covered with slippery moss, over and amongst which it is
anything but pleasant to force one’s way. The mountain sides are
clothed almost up to the snow-line with beech, totara, ribbon-wood,
veronica, and other trees, the rich foliage being beautifully
varied; but not having sufficient time to cut bedding, we spent an
uncomfortable night. The first evening is always the worst in camp.
In the morning we continued our rough journey up the valley and our
struggle with the ‘worrying’ swag.

Soon we discovered traces of fires and old camps, and we knew we were
on the tracks of Green’s and Von Lendenfeld’s parties. An hour for
dinner under a splendid waterfall, and more toiling onwards, till at
last we were over the last boulder-face from the mountain on our left,
with the Ball Glacier in full view. Fox, bending down, picked up a
portion of an old veil, shortly after I found a goggle box, then came a
tomahawk lying on a rock, then the historical tent poles of Mr. Green,
and we knew we had reached ‘Green’s fifth camp.’

Off came the swags, and right glad we were to be done with them. If a
man were only built on the same lines as a Mount Cook grasshopper he
might ‘stand some show’ in those parts, for these insects are the most
accomplished rock acrobats, jumping twenty or thirty times their own
length at a spring, landing on their heads or anyhow with a bang, and
squaring up for the next jump as coolly as cucumbers.

We found many relics of Green’s and of Von Lendenfeld’s parties,
amongst them a surveyor’s chain, which, with Green’s tent poles, we
have for the last five seasons used to pitch our tents.

Scarcely were we made snug for the night when down came a terrific
nor’-wester, blowing with fearful violence, making the tent boom
and shake till we expected it to blow to ribbons. Rain poured down,
thunder, lightning, and avalanches all lent their aid, and the elements
seemed to be having a generally rowdy time of it. All this, of course,
meant snow on the higher peaks; our spirits fell to zero very quickly,
and we gave up all hope of tackling Aorangi for at least a day or two.

The nor’-wester is the _Föhn_ wind of New Zealand, similar in character
to the _Föhn_ winds of Switzerland or the _Pampiero_ of the Andes. Warm
air laden with moisture travels from the equatorial and Australian
waters, till, striking the range of the Southern Alps, precipitation
ensues, the wind descending on to the eastern plains dry and hot.

Having studied Von Lendenfeld’s map of the Tasman Glacier and its
surrounding peaks made in 1883 we knew our whereabouts; but as yet we
had not seen the peak of Mount Cook, having been toiling up close under
the eastern flank of the range, which continues from the peak proper
for a distance of ten or twelve miles in a south-easterly direction.

The morning broke beautifully clear, and we were early aroused by some
inquisitive keas, or mountain parrots, which perched on the tent and
set up an unearthly screeching. These birds are ridiculously amusing
and tame, and we frequently replenished our larder with them by the aid
of a shanghai, or common schoolboy’s catapult, with which instrument of
warfare I have the rather questionable credit of being somewhat of an
adept. When I think of the savoury fries and stews which the shanghai
has brought to our camp table—the table being usually a rock or a
large lily leaf—I begin to be reconciled to the haunting regrets for
apple-destroying and window-smashing which so often beguiled the tedium
of a scholastic career.

We determined not to attempt any climbing so soon after the storm, but
set out to reconnoitre the route taken by Mr. Green.

Mounting the steep lateral moraine of the Ball Glacier we were soon
across it and on to the clear ice of the Hochstetter stream beyond, and
felt the joyful crunching of our well-nailed boots as we tramped along
over the uneven surface.

There is something exhilarating in this setting foot on the clear
ice after days of clambering over cruel rocks, something that seems
to thrill one as the nails go ‘crunch, crunch’ and give such grand
foothold, a cheerful ring in the clink of the ice-axes, a peculiar
charm in the tinkle of the little surface streams, a sense of peace
and loveliness in all around, an inspiration of awe and grandeur
in the glorious masses of mountains which rear their hoary heads
for thousands of feet above, whilst over all there seems to hang an
invisible and imperious over-ruling and omnipotent Power directing the
marvellous workings of Nature. Here man may feel his littleness and
his unworthiness, and yet with Byron he feels what is so beautifully
expressed in ‘Childe Harold’—

  I live not in myself, but I become
  Portion of that around me; and to me
  High mountains are a feeling.

The Hochstetter Glacier is one of the most impressive and beautiful
sights in the Southern Alps. Its supplies come even from the very
summits of Aorangi and Mount Tasman, the two noblest mountains in
Australasia. Avalanches from the eastern and northern slopes of Aorangi
descend to a large ice plateau situate at an altitude of 8,000 feet.
From between the great north-eastern spur of Aorangi and the southern
slopes of Mount Tasman the Linda Glacier issues also into this plateau;
it was discovered and named by Mr. Green. From the eastern slopes of
Mount Tasman and the southern flanks of Mount Haast avalanches also
descend to the plateau, which must be some ten or twelve square miles
in area. This plateau has but one outlet—the fall of the Hochstetter
Glacier. Viewed from below, the frozen cascade tumbles in the wildest
confusion over a precipice of 4,000 feet to join the Tasman Glacier
at an altitude of 4,000 feet (roughly speaking), and presents a most
wonderful appearance. The fall at the top is probably about a mile and
a half in width, narrowing to one mile at its foot, and the ice is
broken up into _séracs_, cubes, pinnacles, and towers of all shapes and
sizes, intersected by crevasses of the divinest bluish-green colour,
and each pinnacle crested with a white cap of unconsolidated snow.
One enormous rock protrudes through the ice in its southern and lower
portion, crowned with toppling _séracs_ 200 or 300 feet in height,
which at regular intervals fall over the face of the rock and descend
in magnificent avalanches. First comes a report like a pistol shot,
then follows an almighty crash accompanied by clouds of snow and ice
dust, succeeded by a low rumbling thunder as the blocks expend their
impetus on the gentler slope below, and finally settle down again into
solid ice, to continue their journey of centuries towards the terminal
face of the glacier nine miles down the valley. Above the fall stand
out, in bold relief against the clear sky, the giant forms of Aorangi
and Tasman.

To stand before this wonderful piece of Nature’s work and gaze on the
weird and fascinating forms of the attendant peaks is an experience not
to be forgotten.

The awful and solemn silence of the mountains, broken only now and
again by the crash and thunder of an ice avalanche or the screech of a
solitary kea, the complete desolation, the loneliness and remoteness
from the haunts of men, all tend to inspire one with deep thoughts and
feelings. One line in Walter C. Smith’s ‘Hilda’ expresses more than
pages of mine would do—

  The silence of the mountains spoke unutterable things.

In two hours’ time we were across the glacier and on the point of the
ridge descending from Mount Haast, which bounds the northern side of
the ice-fall. We began the ascent of the ridge amongst snow-grass and
lilies, but soon the vegetation gave way to rockwork, and when a
height of about 5,000 feet was attained we made sure that this was our
correct route, and, mist coming on, we descended again, and reached our
Ball Glacier camp in the evening.

We resolved to make our attempt on the peak early the following
morning, and accordingly, at 5 A.M. packed our swags, containing
‘tucker’ for three days, spirit lamp, blanket, opossum rug,
mackintoshes, instruments, a change of warm clothing, &c., intending
that night to find a bivouac at 8,000 feet if possible.

Starting at 5.20 A.M. we crossed the Ball Glacier in the very dim
light of a waning moon, and were on the Hochstetter ice at peep of day,
and making good time across, reached the point of the Haast spur in an
hour and three-quarters. A thick mist hung over us, and we waited for
an hour for it to lift, amusing ourselves by smoking and botanising,
and watching the antics of some queer little wrens. These birds are
absurd-looking little creatures with long legs and longer toes, plump
buff-coloured breasts, no tails, staring little eyes, and look for
all the world like boiled potatoes with their jackets on, set up on
hairpins and let loose on the rocks.

As the mist cleared we tackled the ascent, and found it pretty stiff
work, although we had snow-grass to assist us for some way up; but the
rocks above this began to show signs of rottenness, and much care was
required to avoid dislodging them. We made good progress to about 5,000
feet, when we were quite baffled for a time, and were forced to leave
the main _arête_ and look for a more promising route on our right.
Here we proceeded cautiously, crawling through a narrow niche in some
overhanging rocks with a precipice of some hundreds of feet below.
Then the climbing improved till our view upwards was bounded by an
indefinite saddle in the rocks, which might have led to anywhere, but
which did lead, as we subsequently found out, to the easy snow slopes
above.

As the day advanced small falls of stone occurred, which caused some
annoyance and danger, but we managed to avoid being struck by any. Then
followed another stretch of rotten rock which Fox absolutely declined
to tackle, and as it could not be turned by a détour we were brought up
on this route.

Fox suggested descending again to cross a large glacier coming down
from the ridge on our right, and trying the rocks on its opposite side.
This plan we eventually carried out, but it was a fatal mistake as far
as climbing Aorangi was concerned. Descending for about 1,000 feet we
stepped on to the ice of what we then thought was the lower part of the
Linda Glacier—owing to a strange error in Von Lendenfeld’s map—but
which in reality was the Freshfield Glacier. We put on the rope and our
goggles, both indispensable in crossing such a snow-covered ice stream.

On taking to the rocks on the other side we soon gained the lowest ice
slopes, covered with six or eight inches of snow in splendid order,
and adhering well to the ice; now and then we took to the rocks, but
climbed mostly by the snow slopes till we reached the crest of the
ridge and looked over a precipice to Mount Haidinger and the Haast
Glacier below.

It was now 11 A.M., and after a short rest, upon my suggesting a
move upwards, Fox said that he did not fancy the rocks above—which
certainly did look bad—and counselled a retreat. Of course I was
disappointed, and reluctant to give up the attempt so soon, yet there
did seem to be no end to the difficulties above, and experience has
since taught me that Fox was wise in his counsel, for it was indeed
simple madness for two greenhorns to tackle such work.

I soon forgot my troubles in gazing on the scene which burst upon us
as we gained the ridge. Below lay the major part of the Haast Glacier,
descending in a similar manner to the Hochstetter ice-fall from the
corniced _arête_ of Mount Haidinger, a marvellous mass of _sérac_ ice.
A long rest here, and a resolve to revisit the locality during the next
season with a stronger party, and we began the descent.

My first experience of glissading on the snow slopes below was
decidedly amusing; but the art is easily acquired, and after the
inevitable spill or two one soon gets into the way of putting one’s axe
directly behind and not at the side, as is the first impulse. Many and
many a good slide have I enjoyed during the last six years, and I know
no more exhilarating sensation.

[Illustration: MOUNT TASMAN (11,475 FEET) AND THE HOCHSTETTER ICE-FALL

[_Wheeler & Son, Photo._]

In winter time, on the front ranges, we have sometimes made glissades
of 2,000 to 3,000 feet without a stop, and on one occasion, in crossing
the Mount Cook Range, Mr. Arthur Harper and I glissaded close on to
4,000 feet with only occasional stoppages for crevasses.

Reaching the bottom of the slopes we made an examination of the Haast
Glacier at its junction with the Tasman, which disclosed a terribly
crevassed stream, the ice appearing like the leaves of a half-opened
book, the alternating crevasses occupying by far the greater space.
There ensued an aggravating scramble over the moraine, followed by a
weary trudge across the ice of the Hochstetter, and we reached our camp
at the Ball Glacier by nightfall.

Sleep visited our wearied eyelids that night and had never seemed so
sweet, but the morning broke raining and stormy, and as it was from the
nor’-west and looked like continuing, we determined to make homewards
for the Hermitage at once.

Then ensued the awful scramble down between the moraine and the
mountain side with those terrible swags, but, being by this time in
good trim, we arrived at the terminal face of the glacier in four hours
and a quarter, a distance which occupied Mr. Green with Emil Boss and
Ulrich Kaufmann thirteen hours in coming down in their final retreat.

On reaching the Hooker, we found the river running strongly and rising
fast with the nor’-west rain, but after some looking about discovered
a possible ford where the river anastomosed into four branches, and
steadying ourselves with our ice-axes, waded through the torrent. Cold!
Cold was no word for it, and the force of the current was terrible as
it rushed over an uneven and treacherous bed of boulders.

But we got through safely, and soon the Hermitage, our haven of refuge,
was in sight, and we struck up the shingle flats at a merry pace,
reaching our destination in seven hours and a quarter from the Ball
Glacier camp.

On returning from the Hermitage we thought, by crossing the Tasman
River and driving down the opposite bank, to avoid driving round Lake
Pukaki, and so to save thirty miles of travelling. As a rule the river
is not crossable in the summer months, but on this occasion we were
assured of the practicability of getting over; and leaving the track
at Birch Hill Station, we drove out into the great expanse of shingle
which forms the river-bed.

We had crossed all the streams but the last, and were within a few
yards of the further bank of that, when our horse, poor old Nipper,
sank in a quicksand, and as soon as the current caught his body we saw
it was all up. The horse and buggy got broadside on to the current, and
quick as thought we jumped for it, just as the conveyance was turning
over for the first time, Fox down-stream and I up.

The first thing I knew was that I was being washed into the bottom
parts of the buggy, then sideways up, but struggling out and gaining a
footing, the first impulse was to whip out my pocket-knife and cut the
horse free, and, in my haste, both blades were broken before a stitch
of the harness was cut. Fox, in the meanwhile, recovered his feet,
and was holding Nipper’s head above water as we all moved gradually
down-stream with the force of the current, the horse and buggy rolling
over and over. With Fox’s knife I was more successful, and cut the
horse free. Fortunately we were being washed into shallower water
on a spit of shingle, and we were able to wade out with the horse,
after which we returned to extricate the buggy, which had come to
a standstill on its side, and was fast being silted up with moving
shingle. It required all our strength to free it, and in doing so one
of the wheels ‘buckled.’

I have no doubt that we presented an amusing and half-drowned
appearance as we stood on the bank and called the roll. All that was
missing was my mackintosh, a mat, and whip.

Then we jumped on our buckled wheel till it sprang back into its normal
shape, and splicing up the harness, wended our way back across the
minor streams to the track at Birch Hill, wetter, sadder, and wiser men.

We reached Pukaki Ferry an hour after dark and Fairlie Creek the next
evening, where we found the township in a state of jollification over
the annual race-meeting. Most of the New Zealand country townships
boast of their annual race-meeting, the racing lasting one day, and the
whisky part of the proceedings generally running into three.

Then we took the train for Christchurch.




CHAPTER IV

SECOND ATTEMPT TO CLIMB AORANGI

 _A Flooded Camp in the Tasman Valley—Hard Struggles with Bad
 Fortune—We reach Green’s Bivouac_

  If at first you don’t succeed,
  Try, try, try again.—_Nursery Rhyme._


During the winter following my first essay at Alpine climbing I was not
idle, but made several pig-hunting excursions amongst the foot-hills in
North Canterbury, in addition to which, with a companion in the shape
of an old friend and schoolfellow, Mr. M. J. Dixon, I made the ascent
of Mounts Torlesse (6,434 feet) and Puketeraki (5,780 feet) at a time
when these mountains were snow-covered to within 2,000 feet of their
respective bases.

The former ascent was accomplished in the face of a nor’-west gale, and
well I remember how we had sometimes to lie down on the snow and hold
on to our sticks to avoid being blown clean away. We have twice since
climbed this peak under similar conditions, and I never remember the
wind blowing with such force as it does on Mount Torlesse.

It was on February 1, 1887, that Messrs. M. J. Dixon, C. H. Inglis, and
myself left Christchurch for a second try at Aorangi.

We were now well equipped for the attack, having obtained 160 feet of
Alpine rope, three good ice-axes from M. Fritz Boss of Grindelwald,
and suitable nails for our boots. Inglis had his camera and two dozen
plates.

On arriving at the Hermitage we found that the Hooker River was up and
quite impassable for horses, consequently we were forced to cross the
Mueller Glacier by the Hermitage, walk up the Hooker Valley, and cross
the terminal face of that glacier on to the western slopes of the Mount
Cook Range, after which we worked our way down the river till opposite
the Hermitage again, where a length of fencing wire was thrown across
the torrent by which we were able to take our swags over.

The roar of the torrent was deafening, and oral communication across
was quite impossible. The wire on our side was made fast eight or
ten feet above the water, and on the other about twenty feet. Three
cheers were given us by the party of tourists on the other bank, to
which we replied, and then we were cut off from the haunts of men for
a week, and thrown quite on our own resources for clothing, food, and
shelter—board and lodging, in fact.

Then came the arranging of swags, adjustment of carriers, &c., and we
soon discovered that we had all we could carry—over 50 lbs. each. Then
followed the toiling down the steep bank of the river to reach the end
of the range, in the piping heat and glaring sun, now and then having
to ascend the slopes to avoid the river, which rushed along close to
the rocks.

At one place in particular we experienced some difficulty, having
to resort to the use of the rope to climb a ditch or _couloir_ in
the rock-face where the river boiled past at a terrific pace. Here
the camera was accidentally dropped, and falling down fifty feet or
so, lodged on a ledge which overhung the water. Strange to say, when
recovered it was found to be quite uninjured!

By dint of continued exertion and considerable expenditure of adipose
tissue we at last turned the end of the range, and upon reaching the
first water as we struck up the Tasman Valley, boiled the ‘billy’ and
made a good lunch.

The wind now began to rise from the nor’-west, and clouds of dust were
sweeping down the valley, so we lost no time in pressing on to a patch
of Irishman scrub a mile or so below the terminal face of the glacier.
We hurriedly cut some bedding and pitched the tent before the rain came
on, in rather close proximity to an old creek-bed, which had apparently
been dry for some time.

That creek made up for lost time during the night, and soon the rain
came down in bucketsful as we lay our wearied limbs to rest in our
oiled calico blanket-bags. The thunder crashed and the lightning
flashed, and the Tasman River began to roar, and by one o’clock such
a quantity of rain had fallen as to convert the dry creek-bed into a
roaring torrent, whose waters threw up a bank of shingle, and, turning
its course (horror of all horrors!), came right into our tent. In less
than a minute from the time that we felt the first trickle there was a
foot of water in the tent, and all our impedimenta of every description
were sopping or floating about in the dark, and in imminent danger of
being washed away.

Hurriedly we collected all we could into our blanket-bags, got into our
boots somehow, and made for higher ground. We could not see a rise in
the ground, but after wading about found a small portion out of water,
and, with much strong language and trouble, succeeded in repitching the
tent—after a fashion.

Ah! well do we remember the miseries and discomforts of the scene. Wind
blowing in fitful gusts, rain coming down in sheets, while thunder and
lightning and the incessant roar of the Tasman all tended to make the
scene one of terror and discomfort. Matches nearly all destroyed; bread
reduced to a state of pulp; blankets and clothes wet; instruments,
boots, ropes, ice-axes muddled up anywhere, some in the tent, some
being silted up or washed away from the spot where the tent was first
pitched; the floor of the tent now hard, wet stones, in lieu of
comfortable, dry tussock. Oh, the misery of it!

We lay in our wet clothes the rest of that night, all the following
day, and the next night. Inglis and I scarcely stirred but to eat some
disgusting, soppy mixture or to light our pipes; but Dixon pluckily
rigged up a break-wind with an old tent left by the Birch Hill
shepherds, and after three hours’ persistent labour kindled a fire,
improvising a chimney out of a pair of white flannel trousers and
sundry other garments!

We were quite hemmed in by water, and were in a constant state of
anxiety lest the river should make depredations in our direction, as
it was quite close to us, whilst in the creek on the other side we
could hear the rocks being rolled down by the force of water.

Nine inches of rain had fallen during the forty-eight hours, but on
the Sunday it cleared, and once again the warm sun shone out, the
clouds drifted away from the mountains, the birds began to sing, and
the waters subsided as quickly as they had risen, and our spirits rose
again as we spread out our wet belongings on the scrub and donned a
shirt, hat, and a pair of boots apiece, and set out for a visit to
the scene of devastation at the face of the glacier whence the river
issues. The costume was airy but convenient, as we had to cross several
streams before reaching our destination.

We were well rewarded for our walk, for a wonderful sight was presented
where the river flows out from the glacier. For a distance of half a
mile from the face the banks of the main stream were strewn with blocks
of ice of all sizes up to twelve or fifteen feet in thickness. At one
spot the river rushed in mad violence from a great cavern of ice; in
another it rose as from a geyser from under the ice, sending up a large
column of water to a height of six or eight feet.

It was quite a new sensation to be dry again, but that night rheumatism
screwed my joints, and some venomous insect bit my shoulder, causing
intense pain for a short time.

While the rain continued we had all thought of falling back on the
Hermitage as soon as we were able, but a bright sunny morning caused
us to change our plans and forge ahead for the Ball Glacier camp,
weakened though we were in strength and supplies.

Already we felt that our chance of ascending Aorangi was gone, for
the snow lay thick on the upper peaks and avalanches were of common
occurrence; yet we doggedly pushed on, determined not to turn without a
struggle.

Leaping from rock to rock, avoiding the scrub and Spaniards by
sticking to the moraine slopes, and scrambling over great _tali_ of
boulders which came from the mountain sides, by evening we reached our
destination (the Ball Glacier), and finding the surveyor’s chain, tent
poles, and hatchet—left by Fox and myself the previous season—in
good order, we quickly had a comfortable camp pitched. A small army
of mountain parrots or keas soon assembled, and the unerring shanghai
procured grilled kea for supper.

Next morning broke gloriously fine, and by 7 A.M. we were away with
blanket-bags, three days’ ‘tucker,’ and a change of warm clothing,
intending to reach Green’s bivouac on the Haast Ridge that evening, and
to make a final dash at Aorangi on the day following.

Once again we plunged into all those pleasures and joys of
mountaineering. Again we felt the clear ice of the beautiful
Hochstetter Glacier crunch under our iron-shod feet. Now we were
away from all the hum-drum cares of life, from the misery of flooded
camps, in the free mountain air, with the stupendous ice-falls and the
majestic peaks all around. We seemed to breathe a heavenly atmosphere,
to live a new life in another and a better world. Where is the man who
can come into contact with these surroundings and not be better in
body and soul?

We reached the foot of the Haast Ridge by 9.30, and here we debated
as to whether we should tackle Aorangi after all, or try De la
Bêche, further up the glacier (which peak would be an easier ascent
and command a magnificent view of both eastern and western glacier
systems). Aorangi it was, however, we had come to tackle, and so, again
shouldering our swags, we went at the ridge.

We kept to the crest of the spur and found the climbing very simple,
for a thousand feet amongst lilies and snow-grass; but after that the
real business amongst rotten and precipitous rock ridges and faces
commenced, and we had to put on the rope. At this time none of us were
very proficient in the use of the rope, but we soon began to value the
assistance it affords and to appreciate the assurance it inspires.

It was not until 5 P.M. that we reached the top of the ridge, where we
soon discovered Green’s bivouac, not far from which spot we determined
to spend the night.

All the way up we had been climbing with the Hochstetter ice-fall on
our left, and had been favoured with the grandest views of Aorangi,
which looked absolutely impregnable; but as our view of the Linda
Glacier and the Great Plateau was shut off by the upper part of the
Haast Ridge, we could not see the route which we were bent on following.

Here I may remark that the route by which Mr. Green, and subsequently
Dixon and myself climbed the mountain cannot be seen from any distant
point. I refer, of course, to the upper part of the route above the
Haast Ridge. Even the plateau is so shut in as to be invisible from any
distant point, except from the peaks of the Malte Brun Range on the
opposite side of the valley.

Scraping away all the larger stones from under an overhanging rock
and building a semicircular break-wind, we dug holes for our hips
(one gets very sore in hard beds of this nature if such a precaution
be neglected), wriggled into our blanket-bags, boiled a pannikin of
Liebig, and slept like tops till the morning.

The rosy fingers of the morn had just opened the gates of day as our
heads emerged from the apertures of our bags, and showed one of the
most magnificent panoramas of Alpine wonder which it has been my lot to
view.

Three thousand feet below us lay the Tasman Glacier with its marvellous
stream of pure ice, on our right the Hochstetter ice-fall, on which
we could look down and view with wonder its chaos of _séracs_ and
crevasses, the ice-clad precipices of Aorangi rising heavenwards
from it in bold ruggedness. Down the valley to the south-west the
grey moraine, with the meandering river still further afield. Across
the valley the rocky peaks of the Liebig and Malte Brun Ranges with
their hanging glaciers, and right opposite to us Malte Brun himself,
a pyramid of red rock, flanked by ice and snow slopes, standing out
clearly against the morning sky like a great grim castle, and looking
quite safe from any assault of man—on this side at all events.
Following round the panorama to the northwards, Mount Darwin sends
its one great glacier sweeping down into the main stream; then the
Hochstetter Dome stands at the head of the Tasman Glacier itself, and
westward rise the noble summits of Mounts Elie de Beaumont, Green, and
De la Bêche—the last a most beautiful triple peak, queen of the whole
group, and over 10,000 feet in height. Still following round, the eye
falls on the Rudolf Glacier descending from the peak of the same name,
then Mounts Jervois, Spencer, Glacier Peak, and lastly Mount Haidinger,
a fine flat-topped mountain clothed from base to summit in broken ice.

Behind us lay Mount Tasman (11,475 feet), invisible over the higher
parts of the spur on which we were now situated. From our coign of
vantage we counted twenty-five tributary glaciers of the Tasman, some
with ice-falls, others joining with graceful curve.

We congratulated ourselves that all our weary toil and hard swagging
had not been fruitless, and felt quite compensated for the miseries
we had gone through at the lower camp, though the main object of our
visit, we feared, was about to be defeated in a very short time. We
pulled ourselves together, put on the rope, and resolved to make some
pretence of a fight for it.

After an hour’s work we reached the highest rocks, then there came a
dip on to a snow saddle, beyond which, again, snow slopes lead on to
the final summit of the spur which hid the Great Plateau.

But it was not to be; for whenever we went on to snow we sank
waist-deep, and struggled in vain to make any headway. Here, then, we
were beaten, and planting our Christ’s College flag in the highest
rocks, gave it three cheers for the old school days, and depositing a
bottle with the record of our ascent, turned our backs on the grim
giant Aorangi, and began to go down.

We struck a better route down by going into some _couloirs_ north of
the _arête_ of the spur, and reached the Ball Glacier camp again, going
down the following day to the Hermitage, after crossing the Hooker by
the kind assistance of a shepherd from Birch Hill. The Hooker River had
risen to such an extent during the rain storm as to carry away the wire
on which we had slung our swags across. The camera was warped with the
wet at the lower camp, whilst the plates were anything but ‘dry’ after
the storm, so photography was altogether a failure in this excursion.

In the winter time we amused ourselves with another ascent of Mount
Torlesse.




CHAPTER V

THIRD ATTEMPT TO CLIMB AORANGI

_Photography on the Tasman Glacier—Attempt to scale Mount De la Bêche_

  Where rose the mountains, there to him were friends.—_Childe Harold._


It is a thousand pities that the ennobling pursuit of mountaineering is
so neglected in this wonderland of peaks and glaciers. Such advantages
as we enjoy surely cannot exist much longer without calling out the
spirit which lies dormant in hundreds of the lovers of adventure and
worshippers of the beautiful in Nature, who live on in our midst from
day to day in a conventional and monotonous round.

There are pleasures in the pursuit of adventure amongst the great
snow-fields and glaciers which only those who are initiated can
thoroughly enjoy.

Ask the man who goes climbing what these pleasures are, and he cannot
tell you, he cannot define them—yet he feels them, and they are ever
luring him on. They are indefinite, inexpressible; but there is a sort
of ‘mountain fever’ which comes when one has once ‘lost one’s heart
to the great mountains.’ In the work all a man’s best physical, and
many of his mental, powers are brought out and strengthened. There is
the energy, perseverance, and patience to last through a long day’s
swagging, the pluck to face all sorts of dangers amongst the snow,
ice, and rocks, combined with the prudence to know when, for the safety
of oneself and the party, to give in and restrain enthusiasm. There are
the qualities of organisation and system, for which plenty of exercise
is found; indeed, one cannot overrate the benefits which accrue.

Let any who have indulged in different branches of athletics put their
swags on their backs and go for a mountain climb, and I venture to say
that there are greater opportunities for bringing their frames into
good going order and testing their muscular abilities than can be met
with in any school of athletics.

I have known men in England who have revelled in all our great national
games, but who invariably put mountaineering at the head of the list
after once having tasted the sweets of climbing and been captivated by
the charms of the world above the snow-line.

To the artistic what do not the mountains offer? To the botanist, the
geologist, the naturalist, the athlete, and even to the invalid? The
strange new world one enters in sub-Alpine regions, the ‘foretaste of
heaven’ one seems to get above the snow-line.

In out-of-the-way New Zealand we have all these benefits at hand, and
yet we leave the opening out and exploration of our great glacier
systems to foreigners and to visitors from distant lands.

But this is digressive, and I must tell the story of our third visit to
the Tasman Glacier.

On the evening of March 23, 1889, the visitors at the Hermitage
were suddenly moved to compassion, mingled with no small amount of
amusement, in beholding through the fast-falling snow-flakes the
arrival of a dog-cart and tandem.

The leader of the team, a big chestnut draught-mare, seemed to be doing
all the work, and pulling along wheeler, cart and all. The travel-worn
and weary occupants of the vehicle were Mr. M. J. Dixon and myself, and
we had taken French leave for Mr. Huddleston’s chestnut at Birch Hill,
six miles down the road from the Hermitage, our leader having almost
given in after a 250-mile journey from Christchurch.

Another bold, would-be mountaineer, Mr. P. H. Johnson, accompanied
us with the knocked-up leader, and following in the coach was Mr.
F. Cooper, a photographic operator from Messrs. Wheeler and Son of
Christchurch, who was to join our party for a week’s work amongst the
scenes of the Tasman Glacier.

The morning of the 24th revealed the flats around the Hermitage all
snow-covered, and the day was devoted to completing preparations for a
fortnight’s camp on the glacier.

On the 25th, the weather improving, our party left the Hermitage, being
joined by James Annan and William Low, the former a boundary keeper on
the rabbit fence, the latter engaged to help us with the swagging. Two
better men over rough ground never put swag on back, and both entered
into the spirit of the expedition and worked like Trojans to make it a
success.

We drove our dog-cart down to the Hooker River at the usual
crossing-place—the point of the Mount Cook Range—over two or three
miles of boulders which tested the merits of the coachbuilder’s art to
the utmost, as also the driver’s ability to stay in the cart. Here we
found that a wire rope, some 200 feet in length, had been thrown across
the river to facilitate the work of the rabbiters, who were engaged
in keeping back the hordes of ‘silver-greys’ which were making their
way northwards and ruining run-holders right and left. On this wire
rope is slung, on runners, a rude box, travellers entering the same
pull themselves across, and almost invariably take the skin off their
knuckles with the runners. Crossing by this rope we piled our swags on
to Annan’s packhorse and walked three miles up the valley to a patch
of Wild Irishman scrub, where since our last visit a small galvanised
iron hut had been built. A day’s delay here with bad weather, and then
we shouldered our swags, and on the evening of the 27th reached our
well-known Ball Glacier camp.

Our plans were as follows: To do a few days’ work with the
photographer, so as to settle his business first, and then be free
to tackle Aorangi during the following week. We wished to give the
photographer every assistance in our power, as such scenery does not
often come within reach of the photographic artist, however energetic
he may be, and can only be approached by a properly equipped Alpine
party, strong enough to carry a good supply of provisions and all the
necessaries for preserving life in such out-of-the-way parts.

Our first excursion, then, was to cross the Tasman Glacier and make
for the point of the Malte Brun Range at the turn in the glacier just
opposite the point of De la Bêche. Here it was that Dr. von Lendenfeld
had made his bivouac for his remarkable ascent of the Hochstetter
Dome in 1883, when he was accompanied by his wife and one porter—an
ascent that took twenty-seven hours of constant ice and snow work. This
excursion would effect the double purpose of giving us some practice in
ice work, and of securing a fine set of views.

The day was gloriously fine, and we felt our spirits rise as we
scrambled over the massive lateral moraine of the Ball Glacier, across
the glacier itself—which, by-the-by, shows very dirty ice at this
point, being laden with rocks brought down many years since in the
avalanches from the great ice-seamed crags of Aorangi, which towered in
lofty grandeur above us—then over the medial moraine between the Ball
and Hochstetter Glaciers, where a halt was made, and views of Aorangi
and the Hochstetter ice-fall were secured.

Once more we stood before this marvellous piece of Nature’s handiwork,
again we heard the thunder of the avalanches, again we saw the
glinting, bristling _séracs_, and gazed in silence and admiration on
the ice-fall of the Hochstetter.

Crossing the Hochstetter we struck up the medial moraine between that
and the Tasman, straight for the point of De la Bêche.

[Illustration: MOUNT COOK AND THE HERMITAGE

[_Wheeler & Son, Photo._]

The best walking on the New Zealand glaciers is almost invariably found
upon the margin of the medial moraine close to where it joins the clear
ice, so that one is travelling over a mixture of ice and rocks. The
clear ice is too hummocky and entails much undulating progression,
if I may use such an expression, and the moraine itself—well,
the walking on the moraine itself cannot be fitly described in
parliamentary language.

We secured many good views as we proceeded with a 10 × 8 camera. Mount
Haidinger on our left was particularly fine, its eastern face being
almost entirely clothed with the Haast Glacier, which struck us as
being one of the finest cascades of ice we had yet seen, larger in
extent than the ice-fall of the Hochstetter, though not so picturesque.

Time was fast going, and we found that to get off the glacier before
dark it would be requisite to strike away to our right, over a mile of
much crevassed ice, to the gully next in the Malte Brun Range, which we
had originally set out to reach. Jumping crevasses and cutting a few
occasional steps, we at last arrived at the eastern side, finding a
very suitable place to pitch our Whymper tent, and discovering to our
joy a small supply of firewood.

The gully in which we camped had its origin far away up in the
red-sandstone precipices of Malte Brun, and in its bed rushed down a
foaming mountain torrent fed everlastingly by the many small hanging
glaciers above. This stream rushed headlong into a large tunnel of ice
in the side of the Tasman Glacier, over which was formed a tremendous
cave, above which, again, were sheer walls of ice capped with morainic
accumulations, the height from tunnel mouth to moraine summits being
about 500 feet.

A view of this cave was secured by the photographer.

Friday the 29th was a morning to be remembered. Thick mists covered
the peaks and seemed to hang over us like a pall. Here and there a
shaft of sunlight penetrated to the ice-field at our feet. Only now and
then would the rude screech of a kea remind us that we were not really
dreaming in some enchanted land.

We had often talked of attempting the ascent of Mount De la Bêche when
we should have polished off Aorangi; but as Aorangi seemed to require
so much ‘polishing off,’ and we were now camped so close to De la
Bêche, we thought we might as well try our hand at the mountain and see
what we could do in a one-day’s trip from this point, while we left the
artist to his own devices for the time being.

De la Bêche, then, it was to be. So off we started after a breakfast
of sheep’s tongues and Liebig, putting our oilskins on our backs and
taking our axes, and striking due north for the foot of the long
_arête_ which descends from the mountain and separates the Rudolf
from the Tasman Glacier. Halfway to our ridge we had to put on the
rope, for legs began to go through the now snow-covered crevasses in a
promiscuous and unpleasant fashion.

It was indeed like an enchanted land, for the atmospheric effects were
extraordinary. High up, shadowed in the mist, were reproduced the
forms of the highest peaks of Mounts Malte Brun and Darwin. There was
no mistaking their familiar outline, which was thrown out in the mist
thousands of feet above, like the spectre on the Brocken.

[Illustration: CROSSING THE HOOKER RIVER

[_Wheeler & Son, Photo._]

Then the atmospheric effect of the mist hanging over the Rudolf Glacier
was most wonderful. Looking up the glacier, we seemed to gaze into
an enormous blue grotto, the sides being the slopes of the main chain
with all its broken glaciers, and the western slopes of De la Bêche,
whilst the overhanging mist furnished the roof or ceiling. A soft,
warm, blue colour pervaded the whole, beautiful beyond expression.

Arriving at the foot of our mountain we commenced the ascent, finding
the snow of the ice slopes in a loose and powdery condition, and having
to exercise much judgment to avoid precipitating avalanches in the
steeper pinches.

We climbed without the rope, rapidly, and alternately in snow and
rocks, finding the latter very good—mostly of a red sandstone on which
the nails of our boots took good hold. Looking now and then at the
aneroid, we began to feel confident of making the ascent and returning
to our camp by nightfall. But it was not to be, for, at an altitude of
8,100 feet, we were brought up by a very bad _bergschrund_ and ridge of
rocks succeeding it.

To the unlearned in Alpine parlance perhaps an explanation of the
nature of a _bergschrund_ is necessary. At the upper termination of
nearly all highly situated ice slopes there almost invariably occurs
between the rocks above, or between the ice slope and the permanent
clinging ice above, a large gap or crevasse, partially filled or
bridged with new snow during the winter months, but more open as the
warmth of spring and summer causes the snow to melt and the ice to
shrink away.

This crevasse or gap is called a _bergschrund_, and occasionally one
may find in it places where the ice nearly or quite touches the
rocks or ice of the upper side, or sometimes a sound snow bridge may
be discovered. These bridges afford the only means of crossing wide
_bergschrunds_. At the place in question a sharp ridge of ice, the
lower lip of the _bergschrund_, led on to a frail snow bridge with a
dip of some six feet or so in the centre, over a bottomless abyss some
fifteen feet wide.

Dixon cut steps along the ice ridge, having first to remove a foot of
fresh snow from the surface, and then we walked this novel tight rope,
the _bergschrund_ on our left and steep ice slopes on our right, and
crossed the bridge in safety to a small ledge of ice where there was
only just room for three to stand. Could we proceed? The rocks above
were very bad and ice-coated. I went at them, clearing the inch or so
of ice to get my fingers into chinks in the rock, and ‘squirming’ up
on my stomach, clinging with toes and fingers, and feeling disposed to
hang on by my teeth or even by the proverbial eyelids, reached, fifty
feet above, the crest of the ridge.

I had been in some queer places in the mountains, but, pardon the use
of a colonial expression, this one decidedly ‘took the cake,’ and I
shall never forget the start I received when I found myself looking
over a sheer upright face of rock on to an unnamed tributary glacier of
the Rudolf, 1,000, perhaps 2,000, feet below. I dared not stand up and
could scarcely crawl, but lay full length on the steep eastern slope
looking over the sharp ridge down the western precipice. On the right,
the razor-like _arête_ of rock continued upwards, and seemed almost, if
not quite, inaccessible.

[Illustration: AORANGI FROM THE BALL GLACIER

[_Wheeler & Son, Photo._]

Then there was a long-range discussion between Dixon and Johnson
on the ledge below and myself on the ridge, ending in a decision to
descend.

I never to this day can imagine how I came down that fifty feet of
rocks without slipping into the crevasse below, but, by the aid of
Dixon’s directions, I managed to find chinks in the rock-face for the
toes of my boots, and reached the ledge to breathe the air of relief
once more.

Here we held a council of war. We might, by a traverse of the ice
ridge below, gain the rocks again above this bad place; but the summit
was yet 2,000 feet above us, the cold so intense that the steel of
one’s axe would adhere to the hand, the time was fast going, and
the photographer and our men would be much concerned if we stayed
out another night, besides which we were short of provisions, our
original intention having been to stay out but one night. We decided to
acknowledge ourselves beaten for the time being and to return to camp.

It goes against the grain with Dixon and me to turn back beaten from
a peak. Indeed De la Bêche and Aorangi are the only ones to which we
have lowered the colours of our grand old school—Christ’s College
Grammar School, of Christchurch, New Zealand—and the latter we have
since revenged ourselves upon. The former will not run away, and we are
nursing a vindictive feeling against this noble triple-topped summit.

Descending very rapidly, glissading now and then in safe places, we
reached the foot and struck over the Tasman Glacier again for our camp
on the Malte Brun.

Well for us that we had turned from De la Bêche, for an hour from
camp, Dixon, who had been complaining of not feeling up to the mark for
some days and had been lagging—an unusual thing for him—was suddenly
seized with violent cramp in the stomach and thighs. We thought at the
time it was only temporary, consequent upon great physical exertion and
drinking too much snow-water; but unfortunately he did not seem able to
shake it off, and we had some difficulty in reaching camp over the maze
of crevasses which occur in the glacier just where our Malte Brun Creek
enters.

Here was a nice state of affairs. One of our best men gone wrong. How
about Aorangi next week?

Saturday morning found us ‘tuckerless’ and hungry, and Dixon worse
rather than better.

At 9 A.M. we struck camp and started for the Ball Glacier—really
only four hours distant. Whilst taking some views an hour from camp
we suddenly heard shouts down the glacier, and found that it was our
trusty men, Annan and Low, who, being concerned about our lengthened
absence from the lower camp, had come out to look for us.

Johnson, Low, and Annan took the bulk of the swags and started
independently for the Ball Glacier, whilst I stayed to follow at a more
leisurely pace with Dixon and the photographer. Dixon could only walk
for a few minutes at a time and required to rest very frequently, so I
sent Cooper on alone, not dreaming for a moment that he could go wrong
in such simple ground, where no crevasses to speak of occurred.

[Illustration: ICE CAVE, TASMAN GLACIER

[_Wheeler & Son, Photo._]

It was 5 P.M. ere we arrived at the head-quarters after a gallant
struggle on Dixon’s part. These are the times which test a man’s
capabilities, these are the trials of endurance to which the
unfortunate who chances to be taken ill in these Alpine regions is
subjected, and it was a great relief to all to see the afflicted one
struggle bravely into camp.

But a new trouble arose. There was no photographer, and he ought to
have turned up long ago. Johnson set out to look for him, and after
an absence of an hour I was just putting up a swag of mackintoshes,
provisions, &c., prepared to spend the night photographer-hunting on
the glacier, when Johnson’s figure appeared against the sky on the
crest of the lateral moraine, shortly followed by that of the missing
man, who had wandered down past the camp instead of turning off at the
right place. Low and Annan had gone down the valley, and were to come
up next day with more provisions.

The next day being Sunday, we decided to have a day’s well-earned rest.
Messrs. Brodrick and Sladden, of the Survey Department, came up with
Annan and Low to dinner, bearing with them medical comforts for the use
of our invalid.

As there were still some dry plates left unexposed, Cooper and I went
out about 10 A.M. and climbed to a height of 1,000 feet above the camp,
on the Ball Glacier spur, from whence we secured a panoramic view on
four plates of the glacier and the mountains opposite.

From this point, seeing Aorangi looking so grand, we pushed on up the
ridge, intending to secure an exposure from a high altitude. Upwards
we climbed, and the further we went the more I was lured on towards
the main southern ridge of the mountain. I even conceived the idea of
making a pass over to the Hermitage _viâ_ the Hooker Glacier. But the
work became more difficult, and we got into patches of snow and were
unfortunately without our ice-axes. This made our progress more slow
and cautious. Still we pushed forward, the scene becoming grander at
every step.

At length the light began to fade, and I saw that to get an exposure
of the peak from the main ridge was hopeless, so Cooper unlimbered his
instrument and I pushed on alone, determined to reach the saddle, at
least, and see over to the other side. Reaching the final snow—that
covering the actual head of the Ball Glacier, which had been below us
on our right all the day—I sped across it as fast as I could go, and
keeping a sharp look out for indentations indicating covered crevasses,
reached the rocks of a peak situate a little south of the saddle of the
Ball Glacier. Crawling over a snow bridge spanning the _bergschrund_,
which crumbled uncomfortably under me as I laid hold of the rocks on
the upper side, after a short scramble I attained the summit.

How shall I tell of the view southwards which met my astonished gaze?
How describe the glorious sunset effects? Life is not long enough to
attempt it.

I was on the nameless peak south of the Ball Glacier saddle at an
altitude of 7,540 feet—the highest peak south of the great majestic
mass of Aorangi himself, who towered up for another 5,000 feet above me.

[Illustration: MOUNT DE LA BÊCHE (10,021 FEET) FROM THE TASMAN GLACIER

[_Wheeler & Son, Photo._]

I quote from Mr. Green to give some idea of what he thought of our
mountains from this point:—

‘Deep down below us lay the Hooker Glacier, reminding us of the
downward view from the _arête_ of the Finsteraarhorn, while beyond, the
glacier-seamed crags of Mount Sefton towered skywards.

‘Further off lay the _mer de glace_ of the Mueller Glacier, a splendid
field of white ice, its lower moraine-covered termination lost in the
blue depths of the valley at our feet. The high ridge connecting Mount
Sefton with Mount Stokes alone prevented us from seeing the western
sea. It was a glorious day, scarcely a breath of air stirring; no
cloud visible in the whole vault of blue; ranges upon ranges of peaks
in all directions and of every form, from the iced-capped dome to the
splintered _aiguille_. It was a wonderful sight, those lovely peaks
standing up out of the purple haze; and then to think that not one had
been climbed! Here was work, not for a short holiday ramble merely, not
to be accomplished even in a lifetime, but work for a whole company
of climbers, which would occupy them for half a century of summers,
and still there would remain many a new route to be tried. Here, then,
we stood upon the shoulder of the monarch of the whole mountain world
around us, within less than 5,000 feet of his icy crown, but a long,
jagged, ice-seamed ridge lay in our path. Was it accessible? Let us
see!’

It was not accessible, as anyone who has read Mr. Green’s interesting
book will know, and I could see from my standpoint very plainly that
Mr. Green, with Emil Boss and Ulrich Kaufmann—two of the finest
mountaineers in the world—could not do otherwise than accept a defeat.

Just such a scene as Mr. Green describes I saw, only that its mystic
beauty was intensified by the soft glow of evening as the sun sank
lower and lower, at last dipping behind a bank of crimson clouds
hanging over a saddle to the westward.

I seemed spellbound and almost riveted to the spot, and could only tear
myself away when I realised the awkward position of the photographer
and myself, trapped, as it were, by the fast-closing darkness, 4,000
feet above our camp, with all sorts of climbing difficulties below.
Clambering down the rocks and jumping the _bergschrund_, away I sped
over the névé slopes, and reaching Cooper after an hour’s absence,
found him just packing up his camera.

It is too long a story to tell of all our troubles and adventures in
getting down the mountain in the dark; letting ourselves down on to
the rocks, scraping our hands on sharp edges, plunging knee-deep in
soft snow, following false ridges terminating in precipices down to
the Ball Glacier below, retracing our erring steps, and at last coming
to vegetation again; then going down off the ridge towards the Tasman,
trying to hit the head of a long shingle slip I was acquainted with,
hearing 2,000 feet above the camp the first ‘cooee’ from our anxious
mates below, and getting down eventually at half-past ten, ravenous,
and almost torn to pieces by the sharp rocks, Spaniards, and scrub.

Johnson—always self-denying and considerate for others—was out
photographer-hunting again, having gone on to the Ball Glacier and
shouted himself hoarse; he arrived back in camp at 1 A.M. (having been
guided home by a fire which I had kept going on the moraine since
our return), after having experienced a fruitless hunt of eight hours
over rough rocks and ice. This finished the photography, and on the
following day Cooper and Low went down to the Hermitage. A finer week
for securing negatives could not have been wished for, and the thirty
exposures resulted in the best set of mountain views yet obtained in
New Zealand.

Now ensued a few days’ rest, Dixon, Johnson, and I being left in camp
with a week’s provisions and designs on Aorangi, when Dixon should have
recovered his strength.

Only one short excursion did Johnson and I make, to see if it were
possible to reach the Great Plateau from the eastern buttress of the
mountain, and so save crossing the Hochstetter Glacier and climbing
the Haast Ridge beyond. Our endeavours were fruitless, for at a height
of some 6,300 feet we were brought up by a high wall of rock. I still
think, nevertheless, that the plateau could be reached in this manner
when a good deal of snow fills the rocky _couloirs_ or ditches which
in places descend in this wall of rock. Should this be so, it will
no doubt prove to be the route of the future for reaching the Linda
Glacier and Aorangi.

The rock-climbing here, however, is very dangerous, as the frost has
split the rocks up in all directions. One small stone thrown down from
above sufficed to start many tons of loose matter in the _couloirs_,
which rattled down to the glacier below, sending up clouds of dust in
its descent.




CHAPTER VI

THE ASCENT OF THE HOCHSTETTER DOME

_Camp under De la Bêche—Twelve Hours on Snow and Ice—The Pangs of
Hunger_


Thursday, April 4, was a memorable day, for Annan coming up from the
Hermitage with a further supply of the ever-welcome ‘tucker,’ we
started on one of the finest mountain expeditions I have seen in our
New Zealand mountains.

It was not part of our original plan to ascend the Dome; we merely
intended to reach the Lendenfeld Saddle and get a glimpse of the
opposite coast and the western ocean, and it was with this object in
view that Johnson, Annan, and I shouldered our swags and tramped off to
the foot of De la Bêche, which was made in three hours’ hard walking.

Here we camped in a snug hollow between the lateral moraines of the
Tasman and Rudolf Glaciers. Small shingle composed our bed, and a snow
patch close by provided us with water, which we boiled in our ‘Aurora’
stove, as no firewood was to be found so far up the glacier.

[Illustration: PEAKS ON MALTE BRUN

[_Wheeler & Son, Photo._]

A fine Friday morning found us at a quarter to seven on the rope, and
making hard work of it amongst the crevasses of the Tasman Glacier.

I remember well how we resorted to all sorts of dodges to get over
the difficulties, taking the snow slopes of the mountain sides here,
cutting a few steps there, even going to the length of climbing down
into crevasses and crawling under ice blocks. But eventually we passed
the worst of the crevasses, and made good time over the smooth,
snow-covered surface of the glacier.

The distance from our De la Bêche camp to the saddle must be about six
or seven miles, but in the soft and treacherous snow it seemed more
like sixty or seventy.

The glare was something dreadful, and soon our faces and hands were
of the peculiar chocolate colour which invariably comes under such
circumstances. We could not bear the goggles off for an instant.
Gradually we rose as we plodded away, now and then stepping over an
open crevasse or making a détour to find snow bridges. There are but
few crevasses, however, for several miles, only when in the proximity
of the saddle where the gradient increases they once more begin to
occur.

On either hand fresh beauties opened out; De la Bêche on our left
presenting the most wonderful face of _sérac_ ice, streaked here and
there with avalanche slopes, whilst on the right Mount Malte Brun—the
Matterhorn of New Zealand—reared his great red precipices heavenwards,
and further on the Darwin Glacier and Mount Darwin showed in a glorious
light their magic splendour.

Now on our left we passed Mount Green, a fine precipitous cone of rocks
and ice, and then we rose faster and faster as we edged on to the
slopes of the great Hochstetter Dome on our right, whilst opposite,
Mount Elie de Beaumont showered down his ice streams to join the Tasman.

Taking turns at leading, at last we came to what looked like the final
rise. An exclamation broke from Johnson as he espied the new moon
appear over the saddle ahead. It was a small matter, but it seemed
to revive our failing energy and to call us on to victory to see
the silver crescent apparently awaiting us on the snow ridge. Then
a distant peak appeared—a wild cheer broke from us; another peak,
and yet one more, followed by groups of twos and threes, dozens,
hundreds—glaciers! forest! a river! the sea! the boundless ocean!
‘Hurrah!’ we shouted, ‘our tramp has not been in vain.’

Here we were in the heart of Nature’s solitudes, where only once before
the foot of man had trodden the eternal snows.

We spent forty-five minutes refreshing the inner man and drinking in
the glorious view, consulting maps, and reading the aneroid. The saddle
was 8,600 feet high; the Dome was but 9,315 feet. Should we try it?
Yes, we would.

At it we went, cutting many steps and crossing several awkward
_bergschrunds_, until we reached a level plateau. Crossing this field
we attacked the final slopes. It was terrific work, and the last pinch
required 280 steps, all cut with the spike of the axe and deeply
graven, as a slip in such a place would probably have meant the loss of
the entire party in one of the crevasses in the slope below.

My hands were blistered with the axe work, but at 3 P.M. we were able
to walk on the fast rounding-off slopes without steps, and soon we
were on the summit, happy and flushed with victory. The mountain has a
double top and we were on the western and slightly lower one.

What shall I say of the view from the Hochstetter Dome? It is
comprehensive and wonderful. The whole country lay like a map before
us. Westwards Elie de Beaumont and the western ocean, at our feet the
Whymper Glacier, from which flowed the Wataroa River, threading its
way through forest-and glacier-clad mountains to the sea, twenty miles
away. Northwards and eastwards extended in glorious and shining array
the magnificent chain of the Alps; glacier upon glacier, peak upon
peak, range upon range of splendid mountains. Eastwards a fine rocky
peak without a name and Mount Darwin, and looking south-westwards
down the Tasman Glacier, from whence we had toiled our laborious way,
the eye could follow the course of the great ice stream for twelve or
thirteen miles, flanked by the grand mountains which sent down their
tributary ice streams to join the mass in the valley below.

We gave three hearty cheers for her Majesty, and three for our proud
little colony, and commenced the descent, going down backwards in the
steps, and taking firm hold with our axes at every movement.

Time was precious, and on leaving the steps we ran down most of the
less crevassed slopes, and soon found ourselves at the foot of the
conquered mountain. Away we plodded down the glacier again—a hard,
monotonous grind—till we arrived in the failing light at the system
of crevasses on the outside of the turn of the glacier, close to our
camp of the previous night.

This time we kept further out from the edge; but it was six of one and
half a dozen of the other, for soon we were completely entrapped in a
perfect maze of transverse and longitudinal crevasses, over which the
only mode of progression was continued jumping.

This work in the dusk was anything but pleasant, yet had to be
accomplished, and thanks to the aid of the rope, after leaping hundreds
of them, we at length found our way off the side of the glacier to our
tent.

How we watched the slowly warming ‘billy’ with eager eyes, and drank in
fancy over and over again the pannikin of hot Liebig. How we shut the
wind out and nursed the stinking kerosene stove! Alas for our hopes and
our hungry stomachs, the lamp went wrong somehow, and the oil flowing
over, the tent was on the verge of catching fire when Annan gave the
whole concern a kick which sent flaming lamp, ‘billy’ and all outside.
I hope the strong language and expressions of disgust have long since
been forgiven us; but I really think they were justified.

Twelve hours’ hard going did the Dome require. Von Lendenfeld took
twenty-seven from the point of Malte Brun just opposite this camp.

Three hours’ walking the next morning saw us back at our head-quarters,
the Ball Glacier camp, where we found Dixon in active preparation for
an assault on Aorangi, though not so strong as we could have wished.

Now a great council of war was held, the main point of discussion being
as to whether we should attempt our long deferred ascent of Aorangi,
which was, as usual, the chief object of our visit to the glaciers.

Here we were, with provisions for four or five days longer, the
mountain apparently in good order, the weather perfection, and we were
not pushed for time. The mountain had been inspected by various members
of the party from different coigns of vantage. We had seen from a
distance the _névé_ fields leading on to the Linda Glacier.

Against this we had first to consider the state of Dixon’s health. He
was quite prepared, and anxious to try the ascent. We thought that it
would be too much for him. Then there was the accident to the lamp,
which was now useless, there was no firewood at the bivouac, 7,400 feet
up, and no sure means of procuring water. Annan, too, had to leave to
attend to his work down country, and I think, if the truth were told,
that Johnson and I felt as if we had had enough of mountaineering for a
time.

Yet we were very loth to turn our faces away again from the grim giant
who had defied us so long, and it was only with much reluctance that we
decided to abandon the project. So for the third time I retired from
the ramparts of Aorangi unsuccessful, on this occasion without even so
much as an attempt.

We came down to the Hermitage once more, and after a day or two’s quiet
rest yoked Dixon’s celebrated tandem up, crossed the Tasman River, thus
cutting off thirty miles of our homeward journey, and reached Fairlie
Creek in two days. Here I took the train, whilst Dixon and Johnson
drove home. The drive down and back—500 miles—was accomplished in
twelve days’ travelling with the same team of horses.




CHAPTER VII

FOURTH ATTEMPT TO CLIMB AORANGI

_We reach the Great Plateau at last—Defeat again—The Crossing of the
Ball Pass_

‘Perge et perage.’


Once again, on January 4, 1890, in company with Mr. Arthur Harper, a
gentleman who had then done two seasons’ climbing in Switzerland, I
left Christchurch to try conclusions afresh with the monarch of the
Southern Alps.

On this occasion we reached the Hermitage in two days from
Christchurch, riding from Fairlie Creek, and crossing the Tasman River
opposite Burnett’s Mount Cook sheep station. Here we were joined by
Annan, who had already conveyed the bulk of our impedimenta to the Ball
Glacier camp.

On arrival at this point I at once remarked that the ice of the
Ball Glacier had risen above its customary level, and seemed to be
encroaching in a lateral direction—a circumstance which undoubtedly
points to a cycle of advance in the great body of the ice, to be
registered at the terminal face in years to come.

It will not be out of place here to give a description of our usual
Alpine outfit, which may enable others to glean some idea of what is
requisite and convenient for Alpine work in New Zealand.

The most necessary gear for ice and rock work is suitable boots,
broad-soled and flat-heeled, shod well but not too thickly with heavy
hobs, wrought nails being preferable to cast. An ice-axe for each
man—not the light tourist’s axe, but a guide’s axe. Alpine rope
is quite indispensable, and Buckingham’s is the favourite make; we
usually take two or three 50-feet lengths. Two tents, 6 feet by 8
feet and 6 feet by 7 feet, the former for use at the head camp, the
latter a tent built after the ‘Whymper’ pattern with the floor sewn
in, but capable of being pitched on inverted ice-axes lengthened by
two 18-inch supplementary poles (an ingenious contrivance of Dixon’s).
Sleeping bags, 7 feet by 3 feet, made of blanketing, and covered
with an outside bag of oiled calico, impervious to water. Aneroid,
thermometer, prismatic compass, pocket compass. Goggles (neutral tint)
are invaluable, and save the eyes from the awful glare which is always
experienced on new snow and from the blinding sleet which drives in a
storm. Folding lanterns (Austrian pattern) often enable one to find the
way to camp when benighted or to make very early starts. A sheath-knife
comes in very handy in camp, and a supply of fresh nails for our boots
is never omitted, whilst a small ‘Aurora’ lamp stove is invaluable
above the line of vegetation, and a shanghai, or common schoolboy’s
window-breaker, is often useful in procuring birds for the _cuisine_.

[Illustration: THE TASMAN GLACIER FROM NEAR THE DE LA BÊCHE CAMP

[_From a Photograph by A. P. Harper_]

For clothing, woollen shirts and knickerbockers of warm tweed material
are the best, and great comfort is to be found in a loose-fitting
boating ‘sweater’ worn over the waistcoat.

For provisions we generally rely on fresh mutton, to be fried in the
pan or boiled in the ‘billy,’ bread, biscuits, rice, oatmeal, Liebig’s
Extract, chocolate, tea, and so on. A pound or two of fresh butter is
always a boon, and a few tins of marmalade, whilst to some men onions
supply the oft-felt want of a vegetable diet.

There is another indispensable, which here, as in the Caucasus, is very
necessary. I refer to the late Mr. Donkin’s naïve requisite at the end
of his Caucasus list—‘infinite patience’; and to this may be added
fixedness of purpose, determination, and perseverance.

       *       *       *       *       *

Mount Cook, or Aorangi, from a climber’s point of view, is a very
difficult peak to climb, even to a height of 9,000 feet, which our
party attained on this occasion, chiefly on account of the length
and tiresomeness of its approach. It is simply part of a great ridge
which branches off in a southerly direction from the main divide of
the Southern Alps. From its three peaks, all situated on this ridge,
diverge four main spurs (or _arêtes_, as Alpine men call them). From
the lowest and southernmost peak (11,787 feet) descends to the Ball
Pass the southern _arête_; from the middle peak (12,173 feet) the
eastern _arête_, descending on to an enormous buttress which separates
the Ball and Hochstetter Glaciers; from the northernmost and highest
peak (12,349 feet) two _arêtes_ diverge, the north-eastern, separating
the Hochstetter and Linda Glaciers and terminating in the ice of the
Great Plateau; and, lastly, the northern ridge, connecting with the
main divide between Mount Tasman and St. David’s Dome. A comparatively
low rock saddle in this ridge occurs between the highest peak of
Aorangi and the junction with the main divide, leading on one hand into
the Linda Glacier, and on the other to the head of the Hooker Glacier.
Aorangi is thus quite cut off from the west coast, and has, in fact, no
‘western flanks,’ as is generally supposed.

It was an intensely hot day, and scarcely a breath stirred as Harper,
Annan, and I struck out on the now well-known route across the Ball and
Hochstetter Glaciers for the Haast Ridge, but the clear mountain air
seemed to rush into our lungs, putting health and strength into every
fibre.

The mountains were glorious in the noonday glare, and the foliage on
their lower slopes was in its gayest height of blossom. Now and then an
avalanche would thunder down in the ice-fall or from the higher slopes
above, or the whistle of a kaka down the valley could be detected.
These and the merry tinkling of the surface streams were the only
sounds to break the spell of silence and benignant peace which seemed
to reign over all. These are the scenes which go straight to the heart
of the true nature-loving mountaineer.

To reach the foot of the _couloir_ by which three years previously
Dixon, Inglis, and I had descended involved the usual amount of hot
scrambling up _tali_ or fans of detritus from the rocks above. Once
in the _couloir_ (which was snow-filled in places) we were not long
in reaching our old bivouac, where we deposited our first batch of
provisions, &c., our plan being to descend again that day and bring up
more supplies on the morrow.

Coming down, Harper had an almost miraculous escape from swift and
certain destruction. We were glissading on a snow slope when a mass
of rocks broke suddenly away from above and whizzed down the slope at
a terrific rate, passing within a few inches of Harper, who did not
observe them coming, though both Annan and myself had seen the rocks
start a hundred feet or so above him, and had shouted to warn him of
their descent.

This was a warning to us to be careful how we trusted snow _couloirs_
during the afternoon, after the sun’s rays had done their daily
work on the crust of the snow. It is by such lessons that we in New
Zealand have learnt without the aid of Swiss guides to understand, to
appreciate, and circumvent those dangers to which the Alpine climber is
always more or less exposed.

Another fine morning saw us off again with sleeping-bags, tent, &c.,
and by noon we were up at the bivouac with three days’ supplies. Only
resting for an hour or two we pushed on upwards, intending to cross the
Great Plateau—that ice-field of which we knew, but which we seemed
fated never to reach—and find some sheltering rocks under Aorangi’s
uppermost slopes where we might spend the night.

In a few minutes we reached Mr. Green’s sleeping-place, across which
now lay a rock weighing some tons (another warning), illustrating
forcibly the rotten state of the rocks.

We now roped and took to the snow, which led first on to a small dip
or saddle in the ridge (sloping off on the right to the Freshfield
Glacier and on the left to the Hochstetter ice-fall), and then on to
steep snow slopes leading up to the crest of the ridge overlooking the
plateau, now about 1,000 feet above us.

We proceeded cautiously over many half-covered crevasses, and crossing
the small dip or saddle took to the slopes beyond, now and then
taking to the rocks on our left. The climbing was somewhat dangerous,
mainly owing to the bad state of the snow, which would start away in
avalanches, or give way on the edge of a crevasse just at the moment
one put one’s weight on to spring.

At length we gained the highest rocks, which proved very bad going and
seemed likely to bring us to a stand; but the leading man going up the
last fifty feet alone, sent down a spare rope, making one end fast
above, by whose assistance the second man followed in safety, the last
man making the swags fast to the rope below to be hauled up. In the
act of hoisting them, however, one broke away, and commenced a furious
flight down the slopes up which we had so laboriously toiled. To the
swag was attached a pannikin and the tin cistern of our lamp stove, and
at every bound we could hear the rattling of the tin as we watched the
truant bundle leaping down, and we thought of what might be our fate,
were it not for our trusty rope and axes, should we start unexpectedly
down the steep slopes.

Still down went the swag, turning over on its ends and bounding over
crevasses in a manner which made us quite envious. At last it hovered
on a saddle. In breathless anxiety we wondered if it would stop, or
whether it would take the slope to the Hochstetter ice-fall on the
one hand, or the Freshfield on the other. One little effort more it
appeared to make, and then away it went, careering down again towards
the Freshfield ice-fall below.

Our hopes were shattered, and we were fast giving vent to expressions
of despair when the career of the swag was suddenly cut short in a
partially filled _bergschrund_, where it was brought up in some soft
snow.

We dared not risk staying out for the night where we were without
the lost swag, for no rocks affording any shelter were available, so
determined, after making a little further progress to get a view of the
plateau, to return to our bivouac at 7,400 feet—about 1,200 or 1,400
feet below our present altitude—and make a fresh attempt on the next
day, weather permitting. The last man came up the rope, and we made our
way up the final slopes of snow on to that great dome of glacier which
we had so often gazed on from below.

Ah, what a sight burst upon our astonished eyes as we gained its summit!

It seemed the very acme of mountain glory in all the glories around us.
A few hundred feet below lay that _terra incognita_, the Great Plateau,
rounding off southwards to the Hochstetter ice-fall, bounded on the
west by the giant form of Aorangi, on the north by Mount Tasman, and
on the east by Mount Haast and the ridge of that mountain on which we
now stood. The Linda Glacier could just be observed coming round the
north-eastern _arête_ of Aorangi, and on either side of it towered up
to the heavens the two grandest mountains in New Zealand—Aorangi and
Mount Tasman; the former a lowering fortress of black rock and hanging
glaciers, avalanche-streaked throughout, the latter an ice-clad mass
with three summits, covered thickly with hanging glaciers overlapping
one another as do shingles on a housetop, looking utterly unclimbable.
Only two masses of rock are visible, over which avalanches constantly
swept.

The sight is certainly the grandest of its kind I have seen in the
Southern Alps, and Harper tried in vain to recall its equal in
Switzerland.

After working our way upwards along the ridge to the nearest rocks we
deposited a note of our visit in a pannikin, and building a small cairn
over it, beat a retreat.

We experienced some difficulty in getting down the top rocks, but
eventually gained our footsteps in the snow, and following down the
route of the truant swag, recovered it from its snowy bed some 600 feet
below the point where it commenced its downward journey.

We arrived at the bivouac just before dark, and had scarcely finished
brewing a warm drink when down came a nor’-wester upon us.

Pitching the tent was out of the question, so piling stones upon it we
spent a miserably cold night, and by the time morning came all thoughts
of tackling Aorangi had flown, and soon we were speeding down to our
refuge at the Ball Glacier camp again.

Thus ignominiously ended my fourth attempt to climb Mount Cook.

In the afternoon Annan went down the valley with directions to join
us two days afterwards at the Hermitage, Harper and myself being
determined to cross the southern spur of Aorangi at the head of the
Ball Glacier, and work our way down the Hooker Glacier to the Hermitage.


THE FIRST CROSSING OF THE BALL PASS

Starting on a misty morning, we climbed what we call the Ball Glacier
spur—a ridge which diverges from the main ridge of the Mount Cook
Range at a point immediately south of the Ball Pass. It was by this
ridge that Mr. Green’s first and unsuccessful attempt was made, and up
this same route I had climbed the previous season with the photographer.

The major part of the climb is easy, good foothold being obtained on
the red sandstone rocks. In the upper part snow-fields alternate with
the rocks. The Ball Glacier lies couched in the valley on the right,
vast precipices going sheer down to it from the crest of the ridge,
whilst the slopes on the left descend to the Tasman Valley.

After four hours of climbing we reached the main southern _arête_,
and paused on the snow saddle for lunch and rest, and to admire the
splendid prospect of the eastern faces of the mountain, and the
ever-fresh, marvellous panorama of the Tasman Glacier.

Erecting a cairn on the rocks close by, and christening the saddle
after that father of mountaineering—John Ball—we commenced the
descent on a good snow slope towards the Hooker Glacier. All the
mountains on the western side were enveloped in mist, which, however,
fortunately hung high enough to enable us to discern the whole extent
of the Mueller Glacier and most of that of the Hooker.

Bearing away southwards to avoid the crevassed parts of the slope
below, we were soon enjoying a merry glissade—sometimes sitting,
sometimes standing, whizzing down in a cloud of snow which curled up
from our feet and showered down upon us.

Ah, the exhilaration of a good glissade! How you seem to fly through
the air and cleave the fast-speeding surface! How the snow hisses and
the axe grinds! How the excitement thrills you as you look out for
danger ahead, or rushing avalanches behind! There is nothing to touch
it—switchback railway, going downhill on a bicycle, skating—all are
far behind.

In a quarter of an hour we entered a rocky gorge, and still down we
sped on the snow, winding about in and out between magnificent rock
precipices, until before another fifteen minutes had elapsed we emerged
into the Hooker Valley, having come down 4,000 feet under half an hour.

Turning down the valley we kept to the old lateral moraine of the
Hooker Glacier (which stands 235 feet above the present level of the
glacier), and found it good walking.

Once more, however, fortune forsook us, and an enemy in the shape of
a south-west gale, accompanied with heavy rain, met us, against which
at times we could scarcely make any headway. But struggling on we
crossed the Hooker River on the ice of the Mueller Glacier, which at
that time spanned it, and reached the Hermitage drenched to the skin at
4.30—eight hours from the Ball Glacier.

This was the first, and up to the time of writing is the only crossing
of the Ball Pass, an excursion which ere long must become a favourite
one, for a track is just completed to the Ball Glacier, where a
two-roomed hut has been erected by the Government for the use of
tourists and mountaineers.

A finer point of observation than the Ball Pass would be hard to find,
as it commands the most comprehensive views of the Tasman, Hooker, and
Mueller Glacier systems.




CHAPTER VIII

THE FIRST EXPLORATION OF THE MURCHISON GLACIER

_Hard Swagging—Erroneous Maps—The Struggle for Starvation
Saddle—Exhaustion and Hunger—Return_

‘Fresh fields and pastures new.’


I had often cast a longing eye in the direction of the Murchison
Valley, and desired to explore those unvisited scenes which were as
yet unknown and unseen by man. We had frequently during this visit to
the district spoken of making an excursion in that direction should
Mount Cook prove too heavy metal for us. Now was our chance, and we
determined to take it.

Leaving the Hermitage with an addition to our party in the shape of
Messrs. Wells, Timson, and Hamilton—the former two only intending to
visit the Tasman Glacier, and the latter anxious to accompany us on the
Murchison trip—we made the Ball Glacier camp, after the usual hard,
hot grind over the moraine, by evening.

The next morning breaking fine, Wells and Timson went for an hour’s
excursion on to the glacier opposite, returning enchanted with
the grand view of the Hochstetter ice-fall and the surrounding
peaks, whilst the rest of us—viz. Harper, Hamilton, Annan, and
myself—prepared swags for a two days’ excursion up the Murchison
Valley, whose mouth could be discerned some two miles distant across
the Tasman Glacier.

It is a fact worthy of notice that with the exception of mountaineering
parties equipped for climbing—and the numbers of these could be
counted on the fingers of both hands—Messrs. Wells and Timson were
the first two tourists to venture so far up the Tasman as our camp,
and since that time only one other has succeeded in reaching the same
point, that gentleman being his Excellency the Earl of Onslow, Governor
of the colony, whose practical penetration regarding all matters
connected with New Zealand entitles him to the respect and gratitude of
those subjects over whom he exercises vice-regal control.

Since the visit of Lord Onslow a track which had then been formed
within two or three miles of the Ball Glacier has been completed,
making the task of reaching the spot one of comparative ease and
pleasure. Further conveniences for tourists and mountaineers in the
shape of tracks and huts are now in course of construction by a
far-seeing Government, who recognise the fact that New Zealand is fast
becoming the playground of Australasia and the Switzerland of the South.

From careful inquiries made at the Survey Office, from Mr. Sealy—a
gentleman whose early work of exploration amongst the New Zealand
glaciers is too readily forgotten—and from the run-holders and
station hands in the district, we had every reason to believe that the
valley had only once been entered (by Mr. Burnett of Mount Cook sheep
station), and that the face of the glacier had never been reached; only
in one case could we hear of the clear ice having been seen—viz., by
a shepherd of Mr. Burnett’s from a peak of the Liebig range.

There was therefore little or no doubt that we had a virgin field
before us, and it was with feelings of intense eagerness that we
pressed forward across the moraine-covered part of the Tasman Glacier,
and up the shingle flats of the river-bed beyond, towards that massive,
moraine-covered terminal face which fills the valley from side to side,
five miles from the eastern lateral face of the Tasman Glacier.

The valley appeared to be a little over one mile in width. On either
hand rose up most beautifully grassed slopes thickly covered with every
variety of sub-Alpine foliage decked in the gayest height of blossom.

What a place for an artist’s holiday! Flowers innumerable dotted
amongst the richest shades of green—lilies, celmisias in great
variety, Spaniards of many kinds with their golden and spiky heads of
various shapes and sizes, from the orange-coloured dwarf to the great
blue Spaniard with stalks occasionally ten feet in height; snow-grass
with its graceful seed-stalks gently waving in the morning zephyr,
which seemed to fan all Nature into a soft and dreamy repose—such
wealth of colour, such variety of form, such grandeur of outline in the
looming peaks above!

Yes; here the artist might fairly lose himself in delight amongst the
subjects for his brush whilst drinking in the pure sympathy with Nature
which seems to float in the very air.

It is no dream, this lovely valley, though it seems as one. But its
flowers go with the warm geniality of summer, and when the cold winter
comes round it dons its white garment of snow, hiding its beauties
until the hand of gentle spring once more wakens them to burst forth
anew in all their resplendent glory.

Proceeding up the valley between these magnificent mountains we kept
moving onward in a north-easterly direction under the flanks of the
Malte Brun Range, on to whose slopes we were now and then forced by
encroaching streams from the meandering river, and we arrived early in
the afternoon at a large boulder-fan issuing from a rocky gorge above,
whence a magnificent waterfall descended. Here we boiled the ‘billy’
and lunched, making an inspection of the scene, which is one of the
grandest beauty.

Far up in the heavens stands out a noble peak of the Malte Brun Range,
rising out of a glacier which nestles in a basin of rock and bristles
with _séracs_ and pinnacles of blue ice pouring into the gorge below,
from whence issues an imposing waterfall of seventy or eighty feet,
sending up clouds of spray and drenching all within its immediate
vicinity. From long action of the water an almost semicircular cylinder
about ten feet in circumference has been worn into the solid rock, and
the force of water descending this strange funnel seems to drive out in
one direction a current of air which carries the spray with it.

All around this fall the vegetation is most luxuriant, and the rocks
are covered with flowering plants in great profusion, and, in parts
where the spray falls, plants, rare elsewhere, notably the myosotis,
flourish in the abundant moisture.

Taking a more northerly direction we came to the terminal face of the
glacier, which by aneroid measurement we made 3,640 feet—much the
same altitude as our Ball Glacier camp. The survey of the glacier has,
however, since been effected, and this point determined as 3,305 feet.

The moraine is composed of unusually large polyhedral masses of rock,
and is 200 feet in height at the main exit of the river, which is
situated about the middle of the terminal face.

A backward view down the valley revealed but one distant peak—Mount
Sealy—the northernmost of the Ben Ohau Range. This peak was evidently
the only one from which the clear ice of the Murchison can be seen, if
we except those of the Liebig and Malte Brun Ranges, and as none of
these peaks have been ascended, this fact probably accounts for the
Murchison Glacier, which is the second largest in New Zealand, having
lain so long unexplored.

Proceeding up on the western side of the moraine, a new branch glacier
descending from the Malte Brun Range opened out on our left, its lower
ice forming a fine frozen cascade, whilst a waterfall of some 200 feet
descends over a rocky face from its southern and hanging portion. To
this glacier and fall we have given the name of ‘Onslow,’ in honour of
his Excellency the Earl of Onslow.

As it was now getting dark we decided to bivouac for the night, and
selecting a bed of small gravel amongst the larger stones of the
moraine, we dined scantily on cold mutton and tea, and wriggling into
our waterproof blanket-bags were soon ready for sleep. At first all our
attempts at slumber were rendered futile by a congregation of keas, who
hopped around within a few feet of us, jabbering and swearing in their
own peculiar language at such a party of intruders on their domain.

The night was spent in comparative comfort, for we were beginning to
feel the effects of our desperate swagging, and could go to sleep
almost anywhere. It is simply astonishing what a man can put up with,
when he has to; I have slept soundly in all sorts of queer positions,
even upon a mixture of ice and sharp stones, without a tent and with
only one thickness of blanket, when the thermometer has been several
degrees below freezing point.

We were early aroused in the morning by the persistent attentions of
the keas; they even went the length of pecking at our sleeping-bags,
so tame and unaccustomed to man are they in these parts. We all
wanted more rest, but it was not to be thought of if we adhered to
our original plan of crossing a supposed saddle at the head of the
Murchison to the Tasman Glacier by Mount Darwin, and returning to our
head-quarters after accomplishing the circuit of the Malte Brun Range.

We were soon off, and toiled up the small valley formed by the lateral
moraine of the glacier and the slopes of the Malte Brun Range. About
a mile or so up we observed another glacier lying in a comparatively
low saddle above us on our left, beyond this a rocky spur, and then
another and larger branch glacier which for a time we took to be the
main body of the Murchison, as indicated by the maps. We made for it
and climbed its enormous face of ice, and then we discovered our error,
for there, a mile away across the moraine, lay the clear ice of the
Murchison, and far, far away northwards, the valley extended completely
filled with a magnificent _mer de glace_ of pure white ice. We stood
transfixed, for none of us had imagined that such a grand glacier lay
beyond.

Now we saw what was before us, and for a long time debated as to our
ability to face the work ahead.

Hamilton was shockingly out of condition, and a sinew in my leg was
becoming painful, Nature at last rebelling against the strain to which
she was being subjected. We had a very scanty supply of provisions, and
evidently it meant spending another night out if we proceeded.

The temptation was too much for us. We could not let this prize slip
through our fingers, so we decided to go on and put ourselves on
starvation rations rather than turn. Away we struck over the moraine,
and in an hour’s time reached the clear ice, here much crevassed.
Crossing with some difficulty we lunched on the eastern side. Casting
our eyes backward we could see splendidly all the fine peaks we had
been passing under, and could observe the continuation of the range
north-eastwards with five or six more branch glaciers, the final one
northward leading to a snow-field with a saddle at its head. This,
then, must be our saddle, we thought. But it seemed hopeless to cross
it in our tired condition and with our heavy swags.

We set our teeth, however, and went doggedly forward, striking out on
to the clear ice again and making a north-easterly course, at each step
realising more and more the grandeur of the immense ice-field now
gradually opening out and unfolding the wealth of mountain glory which
encloses it.

We tried in vain to identify Mount Darwin or the most northerly peaks
of the Malte Brun Range, which we knew were amongst those on our
left, and, according to our reckoning by the maps—framed from Von
Haast’s—which seems to have been compiled from guesswork as far as
this locality is concerned—we should at this time have been on the
Classen Glacier, which lies at the southern head of the Godley River,
and, in reality, was some miles north over the Liebig Range.

Passing several branch glaciers on our left, and observing that those
on our right were assuming larger proportions, we sidled obliquely
across and made for the snow-field leading to the saddle which we had
every reason to believe led into the Tasman. Altering our course to
due north, and crossing the lower and sloppy part of the snow-field,
which was flat and quite undrained by crevasses, we were soon on snow
in miserable order, and putting on the rope we wound our way gently
upwards amongst the crevasses now beginning to appear.

We had just six hours of daylight, and considered we could reach the
saddle in four if all went well, which would leave us two hours to find
a bivouac on the other side, provided the descent were feasible.

We found it necessary to change leaders again and again to distribute
the arduous task of breaking steps in treacherous snow, just in the
condition to let us through knee-deep as we put our weight on it, and
we had to observe the greatest caution in crossing the crevasses,
which were very deep and almost invariably half covered, or had edges
fringed with cornices of soft snow, which at times had to be removed or
trodden down to enable us to obtain a sound footing on the hard edges
concealed beneath it.

The grade steepened, and we all felt the hard work, more especially
Hamilton, who was sadly out of form, but stuck to his work like a
Trojan, despite the cruel punishing his swags were giving him.

Now we had to make our way across a slope where an avalanche had
recently come, and, worse than all, a thick mist accompanied by a keen
wind began to come over our saddle.

Still we pushed slowly upwards, resting every few minutes. Thoughts of
turning began to arise in our doubting minds. But this would not do
with the col so nearly within our grasp, and the cry was almost one
of ‘Death or victory!’ as we plodded laboriously upwards. Sometimes
we could not see fifty feet ahead, and were compelled to steer by the
compass, taking bearings of crevasses and ice blocks as we proceeded.
Now and then the mist would lift for a moment and we could catch a
glimpse of the longed-for saddle, and at last, when within a couple of
hundred feet, Annan and I cast off on a separate rope, made a rush—as
much of a rush as we could muster up—for the goal, hoping at least to
get a glimpse of the other side ere the mist became too dense.

Hurrah! the saddle was conquered! But what lay beneath? Mist! Mist!
Nothing but a thick impenetrable mist.

The other men arrived, and simultaneously, as if by some providential
magic, the fog began to dissipate.

As it cleared we looked in vain for the familiar points at the head
of the Tasman, which Annan and I knew full well. ‘Where’s Darwin?
Where’s Elie de Beaumont? Where’s the Dome?’ No point in sight could be
associated with the prominent features of the Tasman. As the low-lying
portions of the mist disappeared, we observed that the glacier below
flowed to the right! The Tasman should have flowed in the opposite
direction.

The truth flashed upon us, and a great cry of surprise went up, ‘The
Murchison! The Murchison!’ The very glacier whose middle parts we had
left three hours previously.

Then, leaving Hamilton exhausted on the saddle, the rest of us struck
up to some rocks 300 feet higher on the right, and once more a great
shout arose as Annan and I saw coming into view the unmistakable double
top of the great Hochstetter Dome, whose proud summit we had trodden
the previous season.

From these rocks we observed that the course of the glacier commenced
under a peak on our left (which must be Mount Darwin itself), and
running in a northerly direction for some four or five miles, turning
round the end of the spur upon which our saddle was situated, assumed a
south-westerly course.

The true saddle between the Murchison and Tasman lay across the glacier
below, north-west. Straight ahead of us, north by west, visible over
a rocky and unnamed peak on the opposite side of the valley, lay the
Dome, then to the north another snow saddle, evidently leading into
the Whymper Glacier, and so on to the Wataroa River of the west coast.
Following round the range to the right a very fine mountain stands
boldly up; to the right of this, again, is situated yet another snow
saddle, which we concluded must lead into the Classen Glacier.

The result of the Government survey of the Murchison Glacier, just
completed (1891), confirms our surmises regarding the topography of
this interesting district.

We were astonished at the great length which the Liebig Range assumes,
for it bounds the glacier throughout the whole of its eastern side,
diverging from the main chain of the Southern Alps some distance north
of the Hochstetter Dome.

Any attempt at a description of the panorama from our saddle would be
useless to convey an adequate idea of the view. Harper classed it as
similar in character to the views obtained at high altitudes in the
Bernese Oberland. An aneroid reading gave our height as about 7,900
feet, but this was much out, as by the recent survey the height of
the saddle has been trigonometrically determined as 7,194 feet. Our
estimate of the length of the glacier at the time was twelve miles, and
the survey has now fixed it at eleven and a half, whilst the average
width is as nearly as possible one mile.

[Illustration: MOUNTAIN LILIES (_Ranunculus Lyallii_)

[_Wheeler & Son, Photo._]

Reaching the saddle into the Tasman was now quite out of the question,
for it would involve a descent to the valley below, the crossing of the
upper parts of the glacier, and the scaling of more snow slopes, which
appeared to us to be impracticable owing to the numerous crevasses.
In addition to this, one man was lying _hors de combat_ on the snow
suffering from exhaustion and vomiting. Evidently the only course we
could pursue was to retrace our upward route, and that as quickly as
possible, for there were but three hours of daylight left to reach a
bivouac in the rocks lower down.

After erecting a small cairn, depositing a record of our ascent, and
giving three cheers for nobody quite knew what, we roped up and began
the descent.

It is astonishing how one’s spirits revive when a fresh set of muscles
is brought into action, aided by the force of gravitation, and though
we had been defeated in our attempt to reach the Tasman, what did that
matter? Though we were half-dead with starvation—‘Starvation Saddle’
is now the name of our _col_—and though a real weariness of the flesh
had taken hold of us, what matter? We had explored (I might almost say
discovered) the great glacier we had come out to see, and would be able
to settle all sorts of topographical errors in the maps, and could
speak with authority about many square miles of Alpine country hitherto
entirely unknown.

Our spirits rose as we descended, despite our hungry and tired state,
and we once more wound our way down among the crevasses, and reaching
the glacier again made for the lowest point we could before night
closed in. But we had an hour’s cruel moraine work in the dark ere we
found a sleeping-place on a bed of lilies, where we boiled our last
drop of Liebig and divided our remaining crust of bread.

It rained a little during the night, but we did not care for that with
our oilskin bags, and sleep visited our weary eyelids as it had never
done before.

Hamilton’s condition had improved, but his feet were sore and he was
very weak when at 4.30 A.M. we once more set off for our home on the
glaciers—the Ball Glacier camp. The prospect of boiled rice and fresh
chops lured us on as we made our way down the valley, and putting forth
our last remaining energy we made the ever-welcome refuge in eight
hours, Harper, who had most left in him, going on ahead and preparing a
substantial feed for the stragglers behind.

Oh, that tin plate of rice, _and_ those chops, _and_ that tea!

How came an exhibition of pluck rarely seen. After two hours’ rest
Hamilton said he must reach the Hermitage that night; despite our
dissuasions he determined to go on, and Annan generously volunteered
to accompany him. These two men actually reached the Hermitage that
evening at 8.30. It was the pluckiest day’s work I have ever seen done
in the mountains.

Harper and I came down next day in a snow storm, with fifty-pound swags.

Many people seem to think that a visit to the Alpine regions
necessarily entails contact with very cold weather, even in the summer
time. This is quite an erroneous idea, for on this occasion the
thermometer readings at the lower camp varied from 42° Fahr. in the
morning to 72° in the evening, and I should think that even during
the coldest night the instrument did not register much lower than the
first-named figure. We frequently went about in shirt and knickers
only, and the usual complaint is of the heat, not of the cold. Some
men suffer a good deal of discomfort from sunburn. I myself am a victim
in this respect. It is the upper and freshly fallen snow which is so
ruinous to the epidermis, the reflection from the new and unmelted
crystals being so great as to cause the skin to assume a dark chocolate
colour even during one-day’s work amongst it.

Sometimes blisters form, after which the skin puckers up and eventually
peels off in patches. The noses of persons possessed of aquiline
features are usually a study in themselves after a day or two’s
exposure on new snow.




CHAPTER IX

FIFTH ATTEMPT TO CLIMB AORANGI

 _Avalanches_—_The bivouac again_—_First attempt repulsed_—_Second
 attempt_—_The Great Plateau_—_The Linda Glacier_—_Hard work
 step-cutting_—_The terrible couloirs_—_Victory at last_—_Descent by
 lantern-light_—_Back to civilisation_

  Are not the mountains, waves, and skies a part
  Of me and of my soul, as I of them?
  Is not the love of these deep in my heart
  With a pure passion?


Whymper was eight seasons climbing the Matterhorn. Dent made
innumerable attempts ere he conquered the Aiguille du Dru—why should
we despair about Aorangi?

We certainly were at a great disadvantage as compared with Swiss
mountaineers; we had to begin at the very bottom rung of the ladder,
having no trained guides. But I am confident that if we had been as
many years climbing with guides as we have been without them we should
be far less proficient mountaineers.

[Illustration: LOOKING ACROSS THE MURCHISON GLACIER

[_Wheeler & Son, Photo._]

Probably our case is a unique one, and I doubt if there exists another
instance where two or three novices—at any rate at ice work—have
banded themselves together and gone systematically into heavy Alpine
work ‘right away’ (as the Americans say), doing all their own
porterage and guide work from the start. We learned fast from that best
of masters—‘hard experience.’

[Illustration: AORANGI FROM THE TASMAN GLACIER

[_Wheeler & Son, Photo._]

Had we been consistently following in the footsteps of trained guides
we should not have concerned ourselves about this, that, and the other,
but would have left everything to the men of experience, simply being
towed about in their wake; whereas we have been obliged to train and
exercise all those qualities which a guide possesses, perforce.

Naturally, too, a colonial life is more calculated to teach
self-reliance and independence, and from our earliest schoolboy days we
have been accustomed to rough work on the hills, pig-hunting, &c., and
in camp life on all sorts of hare-brained expeditions. I have, indeed,
been in many an awkward place amongst rocks when out on the foot-hills,
and must have—perhaps unconsciously—acquired many of those qualities
which denote the cragsman.

Want of fixedness of purpose had often lured us away from the peak, and
temptations in glacier expeditions had thwarted our determination. I
felt confident, however, if Dixon and I got together again we should
make a good fight of it with the mountain, for we had learnt to place
confidence in each other in many rough trips, and Dixon was a man after
my own heart for determination.

On December 1, 1890, then, for the last time Dixon and I found
ourselves on the way to the Mount Cook district; we reached Burke’s
Pass that evening in an express waggon which contained besides
ourselves two small Rob Roy canoes, it being our intention to navigate
the Waitaki River from Aorangi to the sea—should we not previously
leave our lifeless bodies at the foot of some precipice or frozen in a
crevasse, as many of our friends prophesied.

December 2 saw us crossing the Tasman River in our canoes ten miles
below its exit from the glacier, and as it was in flood and running
full ten knots, with waves four or five feet high in the rapids, we
had an exciting time of it, yet managed to reach the Hermitage side in
safety, but not without shipping a good deal of water. This was the
first case of a boat of any kind being on these rushing waters, and our
good friends in all directions prophesied dire disaster to what they
were pleased to term our ‘rash venture.’ We are getting quite used to
these consolations of our friends, who seem quite disappointed that we
do not afford them some sensational obituary matter in the daily papers.

Again the faithful Annan was at hand, and greeted us at the Hooker wire
rope with the pleasing intelligence that our camp at the Ball Glacier
was fixed and our swags conveyed there. The Government surveyor (Mr.
Brodrick) and his party were at hand too, and working their way to the
Murchison Glacier to make a survey in continuation of their work on the
Tasman; we spent the following night in comfort at their lower camp,
one mile above the terminal face of the Tasman Glacier, to which point
a horse track had already been formed through the scrub.

[Illustration: THE MURCHISON GLACIER

[_Wheeler & Son, Photo._]

Again we carried our swags up that cruel piece of walking to the
Ball Glacier camp, stopping half-way for lunch at our customary
resting-place—‘The Cove’—a snug little nook in a rock-face where a
rill from the mountain side offers cool refreshment to the weary
swagger.

Friday morning, December 5, found us early astir, and making up swags
of blanket-bags, tent, tinned meats, biscuits, chocolate, raisins,
prunes, rice, oatmeal, Liebig’s Extract, and all such necessaries
as might ensure sustenance and a certain degree of comfort at a
high bivouac. Seeing that our boots were well nailed, our ice-axes
and snow-goggles in good order, we struck out across the Ball and
Hochstetter Glaciers and reached the foot of our climb—the southern
termination of the ridge of Mount Haast. Here we deposited a small
supply of provisions as a standby, in case we should be driven back by
bad weather or by some unforeseen cause.

The day was very warm, and as we toiled slowly up under the weight of
our heavy swags (we were carrying enough provisions to last us for some
days) the perspiration streamed from every pore, and the sun’s rays
seemed to penetrate with singular fierceness.

Soon we came to the lower termination of the new and unmelted winter
snow in the _couloirs_ or ditches between the rock ridges, and as
the day advanced the hissing avalanches came down these slopes with
increasing frequency, and falling stones and rocks now and again passed
close by us. The snow being in such a loose and slushy condition it was
imperative that we should avoid it as much as possible, but climb as we
would we could not help occasionally crossing a snow-filled _couloir_,
and this had to be accomplished with much celerity and caution.

Annan was particularly anxious concerning the ‘shocking state of
repair’ of these lower slopes, and seemed to lose his nerve entirely,
though he is accustomed to work on the higher beats in mustering, &c.,
and he declared his intention of going no farther than the bivouac at
7,400 feet, which we reached in the afternoon. We at once saw that it
would be useless and dangerous to persuade him to join us in the final
assault, for if his self-reliance failed on these lower slopes, what
would the state of his nerve be on the upper ice work where so much
step-cutting would be necessary? Dixon and I knew that we ought not
to try to ascend the peak alone, that such work as we—two guideless
amateurs—were about to attempt, would not be looked upon with favour
by such a body as the English Alpine Club; but we were so tired of
knuckling under to Aorangi that we were becoming desperate, and we
decided to try conclusions without a third man.

Two hours of excavation work removed two feet of snow and eighteen
inches of ice from our bivouac, revealing the faithful ‘Aurora’ stove
and sundry potted meats left twelve months before by Harper and myself,
and soon we had the tent pitched and were snug for the night.

At three o’clock on the Saturday morning Dixon and I crawled out of our
sleeping-bags, and by 4 A.M. we were on the snow slopes, determined to
make a vigorous attack upon the peak which had so long defied us.

Two hours on fairly good snow slopes and a scramble over a nasty
slab-like face of rock, and once again the plateau, and that glorious
scene of Aorangi and Tasman, were before us.

But the wind had risen quickly and was blowing a gale from the
south-west—the cold quarter. To face such a wind for any length of
time, or to attempt to climb Aorangi against it, would be simple
madness, so we turned and ignominiously fled to the refuge of our
bivouac, 1,200 feet below, which we reached at seven o’clock, having
been but three hours absent.

We then sent Annan down, as we were keeping him from his work in the
lower country, telling him to leave word with the survey party that if
we did not arrive back at the Ball Glacier by Monday night something
would probably have gone amiss with us.

During the day the gale blew itself out, and next morning at 3.45 we
were in our steps of the day before, reaching the plateau in an hour
and a half. The morning sun lit up the peaks with a rosy glow, soon
his piercing beams forced us to put on the goggles, while the crust of
the snow began to soften under the great power of penetration which
the rays possess in the rarefied air. This forced us to plod onward in
slushy snow as we headed right for the Linda Glacier, which we could
see rounding the point of the north-eastern _arête_ of our mountain.

On our right rose Mount Tasman clothed in ice, from which during
the night an immense avalanche had descended. We walked close to
its furthest point of motion as it lay stretched out on the level
snow-field like a gigantic breakwater, and found it to be 300 paces in
width; Dixon estimated that it covered from forty to fifty acres.

We now put on the rope, as crevasses began to appear in the gently
rising slopes to the Linda Glacier. On our left we thought that the
north-eastern ridge looked practicable, but deemed it better to rely on
a route chosen by so able a mountaineer as Ulrich Kaufmann, and kept on
our course for the Linda Glacier, taking ten-minute spells at leading
and breaking steps in the soft and slushy snow, and winding our way
amongst ever-increasing crevasses in search of snow bridges over which
we would cautiously crawl.

Now we would have a stretch of gently rising snow, then a crevasse or
perhaps a _bergschrund_, followed by a steep ascent for 100 or 200
feet, then a divergence to one side or the other to avoid a chaos of
_séracs_ or blocks of tumbled and broken ice; and so on, hour after
hour. About noon we had gained a considerable elevation above the
plateau and were well round the corner on the Linda Glacier. Into this
elevated valley the sun poured down through a rarefied atmosphere on
to slopes on either hand which reflected all the light and heat. The
glare was something dreadful, and before midday our faces and hands
had assumed the customary chocolate colour, and the skin was literally
broiled off me; Dixon did not suffer to such an extent. The heat was
most intense, though not of the enervating kind which one feels at
lower altitudes.

Viewed from this quarter Aorangi presents a totally different form than
from any other, and we began to be sanguine about accomplishing our
task. I was in possession of notes and sketches of the route kindly
sent me by Mr. Green, and these were of material assistance to us.

Before us lay the final peak with its capping of ice. From the summit,
now in full view, descended in a north-westerly direction to the right
a steep rocky _arête_ connecting with the ridge leading on to Mount
Tasman. From the lower parts of these rocks steep ice slopes streaked
with marks from falling rocks descend to the upper portions of the
Linda Glacier, bounded all along their lower termination by an immense
_bergschrund_ which severs them from immediate contact with the glacier
itself.

On the left of the summit slopes the north-eastern _arête_, consisting
of a ridge of alternate knife-edges of ice and _gensdarmes_ or towers
of rock. The northern side or face of this ridge descending to the
Linda Glacier is composed of very steep slopes of ice set with three
immense masses of red sandstone rocks, with two ice-filled _couloirs_
or ditches between them. Up these two _couloirs_ lay our route. We
thought, however, that by leaving the glacier and taking to the crest
of the ridge we could improve on the route, but soon found that the
change was a mistake, and so struck back on to our old course up the
middle of the glacier, the final slopes of which were very steep and
exposed to the chance of avalanches from either hand.

It seemed a hopeless task this plunging through soft snow hour after
hour, and it was nearly one o’clock ere we gained the edge of the
big _bergschrund_ and with difficulty discovered a sound enough snow
bridge. Shortly before this an incident occurred in crossing one of
these snow bridges which brought forcibly before our minds the serious
nature of the work in which we were engaged. I—the lighter man by two
stone—had crawled over in safety, and planting myself well in the soft
snow above, was taking in the slack of the rope as Dixon followed,
when suddenly he went through up to his armpits and was dangling in
space, held up by a thin crust of snow and by the rope from above.
I pulled with the strength of despair, and Dixon struggled till he
secured a hold somehow on the other lip of the crevasse and got out.

That sort of thing is all very well to look back upon and talk over
afterwards, but I am not likely to forget for many a long day the
sensation of holding up a thirteen-stone man under such circumstances,
and I must say that I should have been much easier in my mind if we had
had such a man as Emil Boss or Ulrich Kaufmann on one end of the rope.

Immediately after crossing the big _bergschrund_ step-cutting
commenced; and from this point upwards every step, other than those on
rocks, had to be cut in hard ice.

It is no easy task after climbing steadily for nine hours in soft snow
to set to work and cut steps, especially when one knows that a slip
must on no account be made, for with two men only on the rope it would
mean a sudden descent to the crevasses or precipices (as the case may
be) below, and our certain destruction.

An hour’s steady work and we gained the foot of the lowest rocks,
which were found to be quite unscalable. We then sidled round the base
of these rocks to the left and commenced cutting steps up the first
_couloir_, keeping close into the rocks on our right, on which we
could get an occasional hand-grip. Ice blocks were continually coming
down from the broken masses overhanging the top of the _couloir_, but
luckily none struck us. The descent of an ice block in such steep
ice slopes is something to remember. First a rattle above, and then
‘swish, swish’ as the first leaps begin, followed by a ‘whir-r-r-r’
and a ‘hum-m-m-m’ as, like a flash of light, a spinning and
ricochetting object goes by and is lost to sight over the brink of
the precipice below, or perchance is detected spending its momentum
on the soft snow slopes 1,000 feet down.

These falls of ice on the upper slopes are not like the hissing
avalanches, which sometimes even _crawl_ down the lower snow slopes,
but come down with the speed of light, and are calculated to strike
terror into the heart of the stoutest-nerved climber.

We crossed the _couloir_ near its head, partly on ice and partly on
rocks, amid the gravest peril from showers of ice, and took to the
rocks on our left, which were both dangerous and difficult, mainly
owing to their being here and there coated with ice. Soon they became
quite inaccessible, and we were again forced towards our left on to
the ice slopes in the second _couloir_, and here we found the ice even
harder, and we could only make an impression on it with the spike end
of our axes. To add to the difficulty, the angle of ascent became
steeper, inclining in places to about 60° from the horizontal.

We negotiated this _couloir_ in a similar manner to that below, but
water trickling from the overhanging rocks formed awkward hummocks of
ice on the slope close to the rocks, over which we thought it almost
impossible to climb, and to go out into the middle of the _couloir_ was
impossible, owing to falling ice.

Time was quickly passing, and we had a terrible fight to reach the
head of the _couloir_. The rocks now shaded us from the sun’s rays,
and soon our hats, coats, and the rope were frozen as stiff as boards,
while the cold was so intense as to cause the skin of our hands to
adhere to the steel of the ice-axes.

It seemed now more than ever a hopeless task to reach the final
ice-cap, which we knew could not be far above us; but we silently and
doggedly cut away, and at length were rewarded by finding the rocks
on our right practicable; taking to them we were soon on their crest,
and the ice-cap of the mountain lay straight before us. An easy bit of
rock-climbing led up to the slopes, which we found to be covered with a
peculiar form of lumpy and frozen drifted snow. At the top of the rocks
we looked around in vain for Mr. Green’s cairn, with his handkerchief
and Kaufmann’s matchbox, left on the occasion of their ascent in March
1882. Doubtless they have either been long since swept away by falling
ice or were buried in the terminal of the ice slope, which in December
would encroach farther down upon the rocks than in March.

Dixon now counselled a retreat, arguing that we had virtually overcome
all the difficulties and had only the final and easy slope to cut up;
but I persuaded him to stay a little longer and make a push for it, or
at least as much of a push as we were capable of making.

[Illustration: AORANGI: THE HIGHEST PEAK

[_From a Water-colour Sketch_]

It was half-past five. Four hours and a half we had been toiling from
the head of the Linda Glacier, thirteen hours and a half from our
bivouac, without any halt to speak of. A wind began to blow from the
north-west, adding fresh cause for anxiety about the descent. One thing
was certain—if we wanted to get down alive we should have to reach
the Linda Glacier again before dark.

We worked as hard as we were able at step-cutting for another fifteen
minutes, but only made slow progress; yet there was the cornice, just
away to the right, the crest of the ridge to the left, and the top
scarcely a stone’s throw above, with no difficulty in the way. What
would we not have given for another hour of daylight? How could we turn
away when so near to a complete victory over our old foe?

Dixon again suggested turning, and I could not do otherwise than
defer to his advice, for already we were caught in a trap, and
should bad weather come upon us—and the wind and cold were fast
increasing—before we reached the Linda Glacier again the probabilities
were that we never should have returned from the giddy heights of the
great Aorangi, the ‘Sky-piercer.’

The height of the mountain is 12,349 feet; our aneroid read at our
turning-point 12,300, and we reckoned the summit to be 140 feet
above us. The slight error in the reading of the instrument would be
accounted for by the impending change of weather.

The view is magnificently comprehensive. Looking northwards we could
see clear over the top of our giant neighbour, Mount Tasman (11,475
feet). On the western side, the ocean, but twenty miles distant, was
covered by a mantle of low-lying clouds creeping into the bays and
inlets of the coast, studded here and there with islanded hill-tops,
and stretching away to what seemed a limitless horizon on the west. A
streak of blue ocean showed through the cloud mantle near Hokitika,
seventy miles northwards.

North-eastwards the glorious array of the Southern Alps extended,
presenting a panorama of such magnificence and comprehensiveness
that it defies any attempt at description. It is one of those vast
pictures which are indelibly impressed upon the memory—one of those
overpowering examples of Nature’s sublimity which seem to move a man’s
very soul and call him to a sense of his own littleness.

Close under us lay the scenes of all our joys and sorrows of the past
five years: the Tasman Glacier, encircled by those splendid peaks
and snow-fields whose forms we had learned to know and love so well;
further afield lay the Liebig Range, and, showing over this, Mount
Jukes and his attendant satellites of rocky peaks. Beyond this again,
far, far away in the blue and indefinite east, we could distinguish the
hills of Banks Peninsula, close to our homes near Christchurch, whilst
we could imagine that the blue haze distinguishable there was indeed
the eastern ocean, 120 miles distant.

It will, of course, be said that we did not make the complete ascent
of the mountain. Be that so; neither does Mr. Green claim that honour,
though for all practical purposes to be on the ice-cap of Aorangi means
the same thing as being on the top. Mr. Green’s highest point must,
according to his sketches, have been as nearly as possible 100 feet
above ours.

But we could not spare time to moralise and rest as we should like to
have done, for it was imperative that the terrible ice slopes should be
descended before the light failed, and at a few minutes to six we began
to go down backwards in our steps, taking a firm hold with our axes at
every step.

This going down is a fearful strain on the nerves, and requires the
greatest steadiness and caution. In hurrying down the easy rocks we
missed a mark on a snow patch which Dixon had made to denote the right
route, and this mistake at the outset caused us nearly half an hour’s
delay before we found the right spot from which to leave the crest of
the rocks. Dixon led down the rocks and I followed, every now and then
taking a turn round any prominent projection with the rope and easing
him down, whilst he in turn secured a good hold and took in the slack
as I came down.

Bad as it had been coming up the top _couloir_, it was infinitely worse
going down, for what was trickling water on the upward journey was now
solid ice, and many of the steps were filled with re-frozen chips of
ice from the steps we had cut above, and these had to be cleaned out
before we could get a secure foothold.

Cutting steps _up_ is one thing, and cutting them _down_ another, for
on a steep slope one cannot turn round face downwards to get at one’s
work, which in the case of going up-hill lies convenient to the hand.

How we did get down without the fatal slip which I was momentarily
expecting would be made by one or the other of us I never could quite
understand.

The rocks below the topmost _couloir_ were negotiated and the lower
_couloir_ reached. This was not so difficult to descend, and the effect
of the frost was such as to prevent such a continual shower of ice
blocks from above, thus minimising one prominent danger.

The lower parts of the _couloir_ were reached, and here are situated
the rocks which form the ledge upon which with Boss and Kaufmann Mr.
Green stood out for the night. There are several ledges accessible,
but Mr. Green’s party must have been upon one of the higher, for on
some of the lower ledges there is room for a dozen men to stand or
even lie down, though scarcely space enough for a circus or Wild West
show, as Dixon humorously suggested. The light was now fast failing,
and we strained every nerve to reach the big _bergschrund_ below before
darkness was upon us.

We were just in time and that was all, and the frail snow bridge was
passed by our sliding over on our backs; I, the lighter man, led, and
Dixon followed as steady as a rock—not a Mount Cook Rock, but the
proverbial one.

We had now been seventeen hours with every nerve and muscle constantly
in action, and yet, as the darkness set in and the awful glare of
the sun had left us, we began to freshen up, and lighting one of our
Austrian climbing-lanterns we retraced our footsteps of the morning,
being most careful never to deviate from them. Soon it became very
dark, for there was no moon, and we could but dimly distinguish the
ghostly forms of the white-robed peaks which shut us in on all hands.

Hour after hour we plodded on. On one occasion we were brought up by
the crevasse into which Dixon had nearly fallen in the morning; it had
opened wider during the day, and only after walking along its line of
fracture in both directions for half an hour did we discover a bridge
which seemed sufficiently strong. We crossed in our usual way, sliding
over at full length, and putting some weight on to our axe-handles
laid lengthways on the snow to distribute the weight as much as
possible.

As the night wore on, the crust of the snow became harder, and after
passing through that most unpleasant crusted stage when it will bear
until all the weight is put on one foot, became quite pleasant to walk
upon, and over the lower part of the Linda Glacier and across the
plateau we made a fair pace. As we reached the rise off the plateau on
to the Haast Ridge the wind increased in violence, and we had great
difficulty in keeping our lanterns (two of which we now kept going)
alight.

The crest of the ridge was gained, and the descent of the dangerous
snow slopes to the bivouac, 1,200 or 1,400 feet below, commenced. We
were soon in trouble again amongst _bergschrunds_ and crevasses, and on
two occasions, in going down and feeling for the next step behind, I
found on showing a light that my _hind_ leg was dangling in a crevasse!

I must not weary you, dear reader, with further monotonous descriptions
of crossing these deadly enemies of the mountaineer, suffice it to say
that after an exasperating hunt on the steep slopes and in the dark for
our bivouac—the candles being just finished—we finally discovered it
at 2.45 A.M., an hour before daylight, having been twenty-three hours
constantly hard at work without any halt worthy the name.

Sleeping soundly till 9 A.M. we made up our swags, and by 11 A.M. were
on the downward route again for the Ball Glacier camp.

It was quite a wrench to leave our friendly rock, which had become
a haven of rest and refuge to us on this upper beat. Five nights
have I spent under its protection at different times, and as often
have I arisen with the early morn to gaze upon those vast and sublime
solitudes of Nature so grandly unfolded to view. From this little
home—out of which if one stepped one had to be careful not to lose
one’s footing and make a rapid descent to the Hochstetter Glacier on
one hand or to the Freshfield on the other—I have seen the rosy tints
of the newly-born day creep downwards from the hoary snow-caps of the
mountains, and when evening drew on have watched the afterglow envelop
all in its warm embrace, even black rocks turning to a deep crimson
which seemed to pervade the higher peaks ere the black and cold night
once again grasps them in his icy hold.

Here had tired limbs been laid to rest whilst wearied minds dreamed
dreams of success and hope, gaining renewed vigour with the morning
light to go forth afresh into new struggles and enjoyments. Here
in the heart of great Nature’s solitudes the thoughts flew back to
homes of comfort and of love. What wonder that we should have formed
associations with such a spot?

The Ball Glacier camp was reached at 4.30 P.M., where we found Mr.
Sladden of the Survey party anxiously awaiting our arrival, with that
forethought which shows the kindly feeling and consideration for others
that characterises men of worth in these outlandish parts.

That evening Dixon went across with Sladden to the Survey camp in
the Murchison Valley, leaving me to wait for an expected friend from
Christchurch.

Here I was quite alone amongst the mountains, with plenty of time
to muse over the events of the past few days and to let my wandering
thoughts fly back even further, to the struggles of the past five years
whilst attempting to conquer Aorangi.

What is the climber’s reward for all his trouble? Why does he climb?
Who can tell?

Is it renown he struggles for? No; I am convinced that is a very
infinitesimal motive. For mercenary ends? No; there is no financial
harvest to reap.

I have often tried to think why men undergo such labour and hardship,
but cannot come to any definite conclusion. To overcome set tasks
(‘pure cussedness’ the Americans would say) is one reason (after
once putting one’s hand to the plough). To gain physical and mental
strength, to raise and purify the mind in Nature’s great school, are
both potent reasons. But, above all, there is some mysterious influence
pervading all true mountaineers—a mountain fever, a close kinship with
Nature (call it what you will), a hidden impulse that grows on a man
who has once felt what it is to taste the sweets of climbing and to
enjoy the fascinations of the world above the snow-line.

My friend did not arrive, so I made my way over to Mr. Brodrick’s
Survey camp on the Murchison, walking through a thick mist, and
steering across the Tasman by the aid of a compass—a distance of seven
miles, or three hours’ walking from camp to camp.

Here I found Cooper—Messrs. Wheeler & Son’s photographic operator—who
was down securing views of the district for a lecture which I was to
deliver before the Australasian Association for the Advancement of
Science.

It was our intention to make a two days’ excursion up the Murchison
Glacier with Cooper, but showery weather put a veto on our plans,
and we were fain to be content with a short excursion to the Onslow
Glacier, where some exposures were effected.

Leaving Mr. Brodrick’s hospitable quarters on December 10, by the 12th
we were again at the Hermitage.




CHAPTER X

ON SOME OF THE PHENOMENA OF GLACIERS, WITH SPECIAL REGARD TO THOSE OF
NEW ZEALAND

 _The cause of glaciers_—_Formation and
 structure_—_Motion_—_Moraines_: _Lateral_, _medial_, _and
 terminal_—_‘Surface’ moraines_—_Crevasses_—_Moulins_—_Glacier
 cones_—_Glacier tables_—_Surface torrents_—_Avalanches_—_Cornices_


In a work of this nature it may not be out of place to briefly describe
some of those interesting features and phenomena which accompany the
world above the snow-line.

Here is a quotation from a recent review of Professor Heim’s work[2] by
a prominent member of the English Alpine Club:—

‘Some thirty years ago a systematic _résumé_ of all that was known up
to that date about existing glaciers appeared in the work of Professor
Albert Mousson, “Die Gletscher der Jetztzeit,” since which, with
perhaps the exception of Major Hüber’s “Les Glaciers,” no attempt
has been made to collect into a focus the light which numerous able
observers and theorists have subsequently thrown upon the question. The
intricacy of the problem has, indeed, increased almost in proportion to
our enlarged knowledge of its conditions; and in spite of the labours
of a large and very distinguished body of investigators, not only do
many important points remain matters of dispute, but the very materials
for a complete solution are still wanting.’

[Footnote 2: _Handbuch der Gletscherkunde_, von Dr. Albert Heim, Zürich
(Stuttgart: Verlag von J. Engelhorn, 1885, 18 francs.)]


CAUSE OF GLACIERS

The joint cause of glaciers is precipitation and cold. A low
temperature alone can do nothing without moisture, and this fact
quickly disposes of the popular notion that glaciers invariably exist
in cold countries. Thibet, for instance, and also some parts of Arctic
North America are destitute of ice streams, though eternal cold may be
said to reign supreme in these parts.

Imagine for a moment the higher mountains clear of snow and ice, and
then watch for the formation of a glacier. Snow falls and fills up all
the valleys and gullies, avalanches descend from the higher parts, and
a great accumulation gathers in all hollows. By constant repetition
of snow-falls (always provided a greater quantity is deposited than
can be melted by the sun’s rays and by the natural warmth of the
earth’s crust) great pressure is put upon the lower portions by the
superincumbent accumulation, and aided by the infiltration of water and
refreezing (or ‘regelation’ as the correct term is), a large body of
ice is formed which at once begins to move down the valleys containing
it.


GLACIER ICE

Glacier ice is not like the solid blue ice on the surface of water,
but consists of granules joined together by an intricate network of
capillary water-filled fissures.

In exposed sections and upon the surface of the ice can be observed
a ‘veined’ or ‘banded’ structure—veins of a denser blue colour
alternating with those of a lighter shade containing air bubbles.

The cause of this peculiar structure has been the subject of much
theorising amongst investigators, but hitherto I believe the greatest
authorities consider that the explanation of the phenomenon is yet
wanting.


GLACIER MOTION

The motion of glaciers is yet another bone of contention, but it
is generally admitted that the cause of it is to be found mainly
in gravitation, and is also partially accounted for by the strange
property of ‘viscosity’ in what appears to the casual observer to be
nothing more or less than a rigid solid.

Recently observations for ascertaining the rate of progress of the
Tasman, Murchison, Hooker, and Mueller Glaciers have been made by the
New Zealand Government Survey Department. Some of the results were
embodied in a paper by Mr. J. H. Baker, the Chief Surveyor of the
Provincial District of Canterbury, and will appear in the ‘Transactions
of the Australasian Association for the Advancement of Science’ for
1891. At the late meeting of that body a committee was appointed to
further these investigations, and a sum of 25_l._ voted for the aid of
the same.

Before long, therefore, there will be put before the scientific public
reliable measurements of the motion of several of the largest and
least-known glaciers in temperate regions.


MORAINES

There is a remarkable feature of the glaciers of this country which
stamps them as unique in one respect—I refer to the very extensive
moraines. I write feelingly of this, for my acquaintance with them has
been a very close one, and they have impressed me very deeply—in more
ways than one.

The large glaciers of which I have written in this work are completely
moraine-covered over their lower parts.


‘SURFACE’ MORAINES

Moraines may be divided into four sections: ‘Lateral’ moraines,
fringing the sides of the glaciers, their outlying portions often being
‘dead’—that is, at present unmoved by the action of the ice, and
forming banks, as it were, for the ice stream to flow between; ‘medial’
moraines, which begin at the junction of two streams of ice and often
continue for many miles to the terminal face; ‘terminal’ moraines,
formed by the depositing of detritus at the melting point or end of the
glacier; and, lastly, ‘surface’ moraines (so called by Professor Hutton
of Christchurch, N.Z.), which are the combined accumulations of the
first two divisions in the lower parts of the glacier.

It is these ‘surface’ moraines that are such a characteristic feature
of the glaciers situate on the eastern side of the chain in New
Zealand. Of those on the western side I am not able to speak with
authority, never having visited them myself; but I understand that
they do not carry such a large quantity of detritus as those of the
eastern slopes.

This disparity remains to be accounted for and awaits an explanation.
I have a theory of my own upon the subject, which, however, as yet I
would not like to put too strongly forward.

On both sides of Mount Cook, on Mount De la Bêche (ten miles further
along the chain), and on a peak just north of the Hochstetter Dome (ten
miles still further north) I have observed enormous exposed sections of
the rock strata, which in each case dip at a steep angle _from east to
west_, presenting slab faces, not easily disturbed by the action of the
frost, to the westward, but broken and fast denuding faces (‘basset’
faces, as they are geologically termed) to the eastward. I am hoping at
some future time to further investigate this interesting subject.

As the western glaciers, however, must descend steeper valleys than the
eastern, I make no doubt that their rate of progress will be eventually
ascertained to be greater than that of the latter, and this would
militate largely against an accumulation of moraine _upon the ice_.


THE SURFACE OF A GLACIER

All sorts of queer notions as to what the surface of a glacier is like
exist. Indeed I have often heard people inquire if it would be possible
_to skate upon it_!

Let us for a moment imagine ourselves at the head of the great Tasman
Glacier, 8,600 feet above sea-level. All around us is snow, either
freshly fallen or merging into _névé_. We begin to walk down, and
at first, upon the steeper slopes, cross a few large crevasses and
_bergschrunds_ by means of snow bridges; then, as the incline becomes
less steep, we walk for six miles or so upon a smooth surface of
_névé_, or perchance knee-deep in fresh snow, and scarcely a crevasse
exists. At the beginning of the great turn we gradually leave the
_névé_ and find ourselves upon hard, white ice, and soon transverse
crevasses appear; these are a little further on cut by longitudinal
crevasses forming the surface into huge squares, not flat on the top,
but hummocky. A perfect network of crevasses cuts up the whole of the
surface, but those parts on the outside of the curve are infinitely
more disturbed than those on the inside, owing to the tension put upon
them by the faster rate at which they have to move. After rounding the
turn the glacier again consolidates and few crevasses appear, only the
surface is covered with old wounds—if I may coin such a term—from the
rents which have occurred at the turn, and presents a very undulating
appearance. The little gullies are formed into watercourses and
intersect the glacier in all directions. On our right, now, is the
medial moraine formed by detritus from Mount De la Bêche, brought down
partly by the Tasman and partly by the Rudolf Glaciers, and it stands
up 100 feet or so above the surface of the clear ice on either side of
it, owing to the protection from the sun’s rays afforded by it to the
ice beneath, so preventing ‘ablation’ or waste going on so quickly. We
follow down for another four or five miles, and then cross this moraine
(which has in the meantime joined that on the northern side of the
Hochstetter Glacier) on to the Hochstetter on our right.


SURFACE TORRENTS AND MOULINS

We are now immediately below the great ice-fall, and the surface
of the glacier presents an appearance not unlike the back of some
enormous caterpillar wrinkled transversely by crevasses, which close
up as we proceed downwards, and furrowed longitudinally by two large
or main watercourses whose icy banks are in places 100 feet above
their respective torrents. These two small rivers are fed from
every direction by minor watercourses, and a mile or two further
down discharge all their contents into crevasses and _moulins_, or
water-shafts in the ice.


GLACIER TABLES AND CONES—THE ACTION OF WARMTH

The locality of the glacier on which we now are is very interesting,
for Nature’s mills are here seen at work day by day. Glacier
tables—blocks of rock perched upon pedestals of ice formed by the
protection from the action of the sun’s warmth—are of frequent
occurrence. Glacier cones—heaps of sand and small fragments of rock
raised by a similar agency (after having been washed to one spot by
water)—are in places all around us. Then, strange and contradictory
as it may seem, we see thousands of holes, each with a stone at the
bottom and filled with the bluest of blue water, formed also in the
first place by the rays of the sun warming the stone and causing it to
sink in the ice. It is well-known in physics that water at 39° Fahr.
is at its heaviest, and as soon as the warm stone—the dark colour of
the stone having absorbed more heat than the surrounding ice—begins
to sink the warmer water follows it, whilst that in the neighbouring
temperature of 32° Fahr. rises to the surface and becomes in its turn
re-warmed, and so on. This peculiar current often bores the holes in
the ice to a depth of many feet, and is only checked by a preponderance
of cold. It is the larger stones, therefore, which rise upon the ice,
and the smaller ones which sink.


‘SURFACE’ AND ‘TERMINAL’ MORAINES

We walk on down the ice stream, and soon the moraines on either hand
close in upon us and we find ourselves on a mere wedge of ice, at the
point of which we step on to the ‘surface’ moraine. Here the swearing
begins, and it lasts right on to the terminal face four or five miles
below, for it is one continual repetition of walking on loose and
tumbling rocks, up one hillock, along a ridge, jumping from

  Rock to rock with many a shock,

down another hillock, now and then starting a whole avalanche of
many-sided and sharp-edged stones down a treacherous slope of ice,
which we take for a surface deeply covered and sound of footing.

Skate on the surface of a glacier?

‘Not much!’ (as the Colonials say).


AVALANCHES

Very strange notions also exist amongst the uninitiated as to the
nature of avalanches. The popular idea of an avalanche is derived from
heartrending accounts of great sweepings away and annihilation of whole
villages, and few of the general run of people seem to realise that in
Alpine work almost any little descending mass of rock, snow, or ice is
dignified by the name of avalanche. Snow avalanches are most frequent
after fresh falls of snow followed immediately by warm weather, and
after a little experience amongst the mountains one soon learns to
detect their customary tracks. Ice avalanches are mainly caused
through the overhanging portion of ice at the terminals of secondary
glaciers—that is, glaciers which break off before descending to the
valley or to the parent glacier below. The tracks of ice avalanches
are almost invariably unmistakable and are swept night and day without
cessation, and very frequently at regular intervals.

Rock avalanches are more treacherous, and one never knows when to
expect them from above; generally in the early morning the frost
holds the stones above in an icy grip, but as the sun melts the ice
in the chinks the hold is released and a stone will descend into the
_couloirs_ or ditches which scarp the mountain side. If one happens
to be below then it is a case of _sauve qui peut_ and a rush for the
nearest protection, for there is no saying how many tons, or indeed how
many hundreds of tons, of loose rocks or stone may start in a wild and
dusty rattle down the hillside.

But some snow avalanches almost crawl down the _couloirs_, and make a
strange and ever-continued hissing as they move. These are composed of
heavy and sodden snow, and begin after the sun has been up for some
hours, continuing until nightfall. These are not so dangerous on a
gentle slope, and one can often waddle or half glissade down in the
midst of one with perfect safety, though they make one uncomfortably
wet.


CORNICES

Cornices are a frequent source of danger to the mountaineer. They are
formed by the snow drifting over one edge of a ridge and forming a
hanging mass. It is needless to say that one soon learns to walk some
feet away from the outer edge of a cornice, for after poking one’s
axe-handle through three feet of snow, and peeping through a blue hole
down a precipice of perhaps 1,000 feet or so, it is not difficult to
fancy what the result would be should the cornice break.




CHAPTER XI

CANOEING ON THE NEW ZEALAND RIVERS

 _The Waimakariri_—_The enormous rainfall_—_Descent of the Waitaki
 River_—_The Tasman branch_—_Lake Pukaki_—_Leaky canoes_—_The
 Pukaki Rapids_—_The Waitaki Gorge_—_Out on the plains again_—_Sixty
 miles’ paddle to catch the train_—_Home once more_


Canoeing on the New Zealand rivers is desperately exciting work.
On the west coast of the South Island there is a canoe club, whose
members build boats in watertight compartments specially suited for
the rough journeys which they undertake. Some of these men are adepts
at canoe-sailing, and think little of going out to sea in their
cockle-shells and even making long coastal journeys. The brothers Park
have established quite a reputation by their adventurous journeyings.
On one occasion they crossed the South Island with their canoes,
towing up the Teramakau River, crossing a saddle of 1,700 feet at its
head, descending the Hurunui and then coasting fifty miles down to
Christchurch. On another occasion the crossing of Cook Straits was
effected by them.

On the eastern side of the island not much canoeing has been done,
with the exception of the navigation of two of the largest rivers (the
Waimakariri and Waitaki) from their sources to the sea by Mr. Dixon and
myself.

I well remember how universal was the outcry against our attempting to
descend the Waimakariri in 1889, upon which occasion we conveyed the
canoes up to the head waters in the Southern Alps, and came down ninety
miles of rapids at a tremendous rate, going through the celebrated
gorge fourteen miles in length. Dixon reached Christchurch in one
day—a wonderful feat—but I was not able to accomplish more than half
the distance, and took two days over it. This involved a descent of
2,550 feet in altitude from the starting point.

In the following year the Waimakariri was again navigated by myself
and three other kindred adventurous spirits, when a number of line
photographic views of the scenery in the gorge were secured.

The descent of the Waitaki River, however, promised some exciting work,
in addition to giving a grand insight into the story of the ancient
glacier formation—a subject of great geological interest.

The rainfall in the New Zealand mountain districts is enormously
heavy, as much or more than 150 inches per annum being registered in
some parts. The rivers consequently carry a phenomenal amount of water
for their length, and the calculations as to their discharge give
wonderful results. The Clutha River in Otago—the largest river of the
South Island—discharges as much water per annum as the Nile! It seems
a strange statement to make; but such is the fact, the calculations
having been made by competent men.

[Illustration: IN THE ICE-FALL OF THE ONSLOW GLACIER

[_Wheeler & Son, Photo._]

The day following our return from Aorangi we left the Hermitage at 9
A.M., and by 1 P.M. had begun our exciting journey of 140 miles to the
sea.

The Tasman River takes its rise from the Tasman and Murchison Glaciers,
and is soon joined by the Hooker, which drains the Hooker and Mueller
Glaciers. Its course from Mount Cook to its delta at the head of Lake
Pukaki is thirty miles in length, and the fall is considerable, the
terminal face of the Tasman Glacier being 2,456 feet above sea-level,
whilst the altitude of Lake Pukaki is 1,717 feet. The first mile or two
of the journey was marked by several strong rapids, and we could not
avoid shipping much water; and, added to this, we soon found that some
old cracks in the canoes had opened out through exposure to the sun,
although they had been carefully covered over with sacking during our
absence in the mountains. This gave us some cause for anxiety, and the
discomfort of paddling in boats which were half full of water soon made
itself painfully apparent. Indeed, there is nothing more calculated
to put a man out of temper with all the world and his surroundings,
to goad him to strong language, and to give him an uncomfortable and
miserable time generally, than to have to sit for hours in a boat that
floats like an unmanageable log, to say nothing of the increase of
danger to which he is consequently exposed in some parts of a river
such as the Tasman, running, as it does, something approaching ten
knots in many places.

I don’t think Dixon and myself are likely to forget the tortures of
the four hours which we passed through on reaching the lake. Here the
cracks in my boat, which was decidedly the worse of the two, had to
be jammed up with handkerchiefs, &c., before we dared to venture on a
journey of eight or nine miles to the ferry at the other end of the
lake, where is situated the exit of the Pukaki River.

As we scraped over the sandy shallows and pushed off into deep-green
water, my heart sank within me at the idea of having to cross the lake
in its present rough state (for a strong nor’-wester was blowing) in
our frail canoes, which were not built in watertight compartments, and
were quite unsuited for the work. Every ten minutes or so I would have
to stop paddling and bale for dear life with the lid of the ‘billy,’
and the craft would immediately swing round broadside on to the seas,
which seemed to do their best to upset her.

At first we kept edging away for the southern shore, and about half-way
down the lake succeeded in getting within reasonable swimming distance,
which, to a certain extent, we retained for a short time.

In the distance we could make out the island close to the ferry, with
some trees on it, and from our direction there appeared to be but
three. My thoughts at once flew back to the island on the Lake of
Geneva, which Byron has immortalised in his ‘Prisoner of Chillon,’
and on which poor Bonnivard would gaze with sadness and yearning for
freedom and life.

  And then there was a little isle,
  Which in my very face did smile,
      The only one in view.
  A small green isle, it seemed no more,
  Scarce broader than my dungeon floor;
  But in it there were three tall trees,
  And o’er it blew the mountain breeze.
  And by it there were waters flowing,
  And on it there were young flowers growing
      Of gentle breath and hue.

I made sure my hair would be grey, like poor Bonnivard’s, before this
lake was crossed; but soon the wind dropped, and we paddled ashore at 9
P.M. close to the hotel and called for brandy and water hot, and seldom
was the indulgence more justified.

At Pukaki Ferry we enjoyed a well-earned night’s rest, and on Sunday
morning we effected repairs to the leaky canoes, in which operation
we received much valuable advice and assistance from Mr. John Gibb,
artist, who was spending a few days in sketching at this point. By 1
P.M. we were on board again and looking forward to reaching Rugged
Ridges—Mr. W. G. Rutherfurd’s station on the southern bank of the
Waitaki—before nightfall. But we little knew what was ahead of us.

A survey of the river from an eminence of the old moraine through which
it has formed a channel, revealed, as far as the bends of the stream
could be followed, a rushing, seething mass of foam-covered water, with
numberless blocks of rock barring the clear passage of the current, and
though we shot the first two rapids below the exit from the lake it
took us until seven o’clock in the evening to navigate six miles of the
river’s course.

It is not easy to describe the wild course of the river in its descent
through the enormous ancient moraine deposits, some of which might
almost be classed as mountains, and must rear their tops to a height
of 1,000 feet above the level of the river. Such an immense body of
rushing water, receiving, as it does, the whole of the drainage of the
Southern Alps, from the head of the Mueller Glacier to that of the
Murchison, necessarily creates great havoc amongst the glacial and
fluviatile deposits through which it descends, and, as a matter of
course, all the smaller stones are hurried and rolled along to form
shingle on the river-beds further down, leaving the larger ones, which
alone can stand against the force of the flood. The natural consequence
is a stream of the most broken and impetuous character, a stream whose
rushing, roaring, and foaming drowns all sounds contiguous to it;
rapid after rapid of seemingly tempest-tossed and crested billows,
of whirlpools and eddies, of back-waters and heavings into surface
currents, and never a still pool to be found anywhere.

Imagine, then, the troubles of two canoeists in navigating this stretch
of water. No canoe or boat in the world would have the slightest chance
of going through, out in the current, without being smashed into
match-wood and its occupants infallibly drowned, for swimming would
avail a man nothing in such a place.

All we could do, then, was to keep close to the bank and let our frail
boats down by the tow-lines amongst the rocks in the comparatively
shallow water. Now shoving them off into a fair stretch and hauling
them up short in time to avoid contact with some ugly rock in front,
then scrambling along ourselves and coiling our lines as we advanced,
clambering over water-worn and slippery rocks, tearing our way
through the Wild Irishman scrub, or wading a few steps middle-deep in
the turbid water to the points where we had brought our respective
canoes up. Then repeating the same performance over again and again,
bruising our legs against rocks, slipping down amid the slimy stones,
scratching the skin off and receiving numerous thorns from the
scrub, wishing we had never been born, lamenting the hardships of our
lot, anathematising canoes, ropes, paddles, river, rocks, scrub, and
everything in creation.

No, that seven miles journey was _not_ all that could be desired; but
having put our hands to the plough, we both made up our minds that we
would go through with the undertaking, even if we had to repeat the
same performance down to the sea every day for a week, and the worse
the river got the more pig-headed we became. We had beaten Mount Cook,
and we meant also to gain a victory over the Pukaki and Waitaki, if it
cost us our life-blood. At some places where a number of large rocks
were congregated close to the river’s bank we would be compelled to
take the boats out, and shouldering them, climb round the rocks on
shore, and launch them afresh in better water below.

At one time, Dixon, who was leading, accidentally dropped his paddle,
which was whisked away by the current in a trice. He made a great
effort to recover it, and plunged in up to his armpits in the turbulent
water, but failed to reach the truant paddle. Seeing his difficulty I
pushed my boat out to him, and he seized my paddle and, jumping into
the canoe, gave chase to the one he had lost. I ran along the bank,
but could not keep near him; and in fear and trembling I watched him
nearing a horrible fall amongst some sharp teeth-like rocks. I thought
his last moment had come, but just before reaching the danger he
overtook the lost paddle, which he grasped with one hand, and, jumping
out of my canoe, held the tow-rope and brought the boat up within a few
feet of the fall. The whole affair was the work of a few moments, and
was a wonderful exhibition of smartness and presence of mind.

By 7 o’clock we began to think that we had had about enough for the
day, and, putting the boats ashore, we walked back, over the old
moraine and along the rabbit fence (which, by the way, I hear is doing
its work splendidly), to the Pukaki Ferry for the night.

By 7 A.M. next morning we were again with the canoes, and once more
performing gymnastic feats along the rocky bank. But our reward was now
near at hand, for after an hour or so we got on board and sneaked down
the quieter sides of one or two pools. The moraine deposits gave way to
those of fluviatile origin, and the size of the stones in the river-bed
decreased rapidly; consequently we soon began shooting the rapids again
and were making grand headway. The country on either hand opened out;
from our left came in the Tekapo River, and soon after, as we sped on
under Ben More, on our right the Ohau. Now we were in the Waitaki,
which is formed by the junction of these three rivers. ‘Waitaki,’ or
‘Waitangi,’ means ‘Crying water.’

The hydrographic area of the Waitaki Basin is 4,914 square miles, more
than three times as great as that of the Rakaia or Waimakariri, and it
drains most of the principal eastern slopes of the Southern Alps.

The eastern source of the river drains the Godley and Classen Glaciers
with their numerous tributaries, forms the Godley River, and flows
into Lake Tekapo (some fifteen miles in length); it issues from the
southern end of the Lake and curves a channel for itself through the
ancient moraine, when it becomes known by the name of the Tekapo River,
which, flowing for a distance of about twenty-five miles, joins the
Pukaki; all these, with the addition of the Ohau, the junction of which
is a few miles further down, form the Waitaki River. The Hopkins and
Dobson Rivers drain that part of the Alps immediately south-west of
Mount Sefton, and flow into Lake Ohau. The stream issuing from thence,
under the name of the Ohau River, runs for a course of thirteen miles,
and joins the Pukaki and Tekapo as before mentioned.

After the union of these three systems of drainage the course of the
river runs through a wider bed for about five or six miles before
entering a gorge some ten miles in length. Down this fine stretch of
water we now enjoyed a delightful paddle, and soon we sighted Black
Forest sheep station, with its rows of green willow trees, on our left.

Here various kinds of river birds lent an aspect of life and gaiety to
the scene—gulls, terns, paradise and grey duck, teal, dotterel, stilt,
and red-bill soared over us, or rose in startled dismay as we shot by.

We had left the snows behind us and were fast being closed in by the
foot-hills. We neared the gorge at 11 A.M. and paddled ashore on the
Otago side and boiled the ‘billy’ for lunch.

It seemed a delightfully quiet hour after all we had been through; we
sat and smoked in happiness and watching the rabbits skipping about
amongst the bracken. We were certain, if only by that, that we were in
Otago, where rabbits are the monarchs of all they survey.

The Mackenzie country hands had told us that we should find the gorge
_a little rough_, so we knew we were in for it presently; yet for a
couple of miles we found the river good going, though some ominous
spurs of bed rock now and then entering the current—the first bed rock
we had met with since leaving Mount Cook—foretold what we were coming
to.

After going round a few ugly corners the white water became more
frequent, until suddenly we were brought up by an awkward rapid into
which we dared not venture.

[Illustration: THE SURFACE OF A GLACIER

[_Wheeler & Son, Photo._]

A survey from the cliffs, sixty feet above the stream, disclosed a
tongue or groyn of rocks running out into the stream in an oblique
direction from the Otago side, and shooting the main body of the
current on to the rocks opposite. A long stretch of straight water
followed, but the whole stream was confined in rocky banks so close
together that one might throw a biscuit across, and the pace of the
current was something terrific. For half an hour we considered the
situation, finally determining to shoot the rapid. There was really
only about eight or ten feet of safe water close to the point of
the groyn of rocks, and this was right in the body of the current.
On either hand were eddies and whirlpools of the most formidable
character, which, in the event of our making a bad shot, might swirl us
among the rocks on one side or the other, and had such been the case
we trembled to think what would have been our fate. However, at it we
went, Dixon as usual leading, with a head as cool as a cucumber,
and I following, like a spaniel after his master. One wild rush, a
few strokes of the paddle, a mad tossing about in a sheet of crested
foam, half-a-dozen bucketfuls of water on board, and we were through,
breathing again as we tore down the hurrying, but straight and safe,
current below.

Though we met with no greater obstacles to canoeing than this rapid in
the gorge, such performances were several times repeated, and we had to
land now and again to survey the course ahead.

To describe the mad plunging of the river through the gorge is not an
easy matter. Here and there, perhaps, a long even stretch is met with,
but for the most part the river makes a succession of bends bounded
by rocky cliffs on either hand, now and then masses of rock crop up
through the water, against which the stream is banked up by the force
of its mad career to a height of ten or twelve feet; immediately under
the sides of the rock there are vicious-looking heavings, eddies, and
whirlpools, which, if one chances to get into them, twist the boat
about like a feather when blown upon the water’s surface. A black swan
and three cygnets kept ahead of us for the last six miles of the gorge,
but as we entered with relieved feelings upon the more open country,
they eluded our further pursuit in a backwater. Another few miles
and we reached our destination for the night—Mr. W. G. Rutherfurd’s
station, Rugged Ridges—where a warm and hospitable welcome made us
feel that once more we were in the regions of civilisation.

Leaving next morning at 4.30, we gave ourselves eleven hours to
catch the train for Christchurch, at Waitaki, a distance by water
of sixty miles. Four hours saw us in Duntroon (thirty miles), where
we astonished the natives in disgracefully tattered boating attire,
and indulged in that from which we had long been estranged—‘a long
shandy’—and by 9.15 we were off again at eight miles an hour, shooting
down the most beautifully safe and rippling rapids, scaring ducks,
plover, gull, stilt, swan, and all manner of wild fowl; now and then
startling a mob of horses or cattle from their peaceful browsing,
or astonishing some slow-going shepherd or cowboy as they stared
open-mouthed at such an uncommon sight as two madmen in cockle-shells
of canoes rushing down their boatless river, until we put the final
touch to the whole enterprise by carrying our boats up to the station
at Waitaki South (to the amazement of four railway navvies), at 1 P.M.,
having averaged eight miles an hour for sixty miles, allowing for one
hour stoppages.

The distances by water, allowing for sinuosities in the course of
the rivers from Aorangi to the sea, may be roughly summarised as
follows:—From the end of the Mount Cook Range to Pukaki Ferry,
thirty-four miles; from the Ferry to Rugged Ridges, thirty-eight miles;
and from thence to the railway bridge near the sea at Waitaki, sixty
miles; a total distance of 132 miles.

If it were not for the Pukaki Rapids the trip might be comfortably
accomplished in three days, and at a stretch could be done in two;
but the way to enjoy it would be to travel in a good staunch canoe,
with watertight compartments and such accessories as the west coast
canoeists are in the habit of using, and spend a week over the journey.




L’ENVOI


This little book has but told the story of the ramblings and adventures
of a lover of Nature. I fear that I have signally failed to do
justice to her features, or to convey any adequate idea of her mystic
influence. Would that I could impart that which I can feel.

Should it fall into the hands of Swiss climbers it may serve to show
that the brotherhood of the mountains extends even to out-of-the-way
New Zealand, and that in that country, as well as in the Old World, the
ineffable glories of the mountains have power to charm and to captivate
the hearts of men.




APPENDIX


It has been suggested to me that this work would be more complete if
it contained at least a short record of Alpine expeditions undertaken
by parties (other than those organised by the writer) to the glacier
regions which have been under notice. The suggestion is one which the
writer accepts with much pleasure.

The first recorded expedition to the Mount Cook district, as far as I
am able to gather, is that of the late Sir Julius von Haast (then Dr.
von Haast), the narrative of which may be found in his interesting and
learned work ‘The Geology of Canterbury and Westland,’ published by the
‘Times’ office of Christchurch, now unfortunately out of print, and
difficult of access to the majority.

His work was necessarily more that of exploration than of climbing,
and although later surveys have corrected and modified many of his
estimates of the sizes of glaciers and heights of mountains, it must
be remembered that in the days when he visited the locality (in 1862
and 1870) the difficulties of travelling and of securing supplies were
much greater than at the present time, and the work of exploration
consequently much more difficult.

Of Alpine work (carried on in the sense of the word as understood by
Alpine climbers) he did not effect much, his energies being chiefly
confined to geological, botanical, and zoological observations whilst
he was engaged in a geological survey of the province of Canterbury.

His excursions on the glaciers appear to have been confined to a short
trip up the Tasman, probably to some six miles or so from the terminal
face, and a short exploration of the lower portions of the Mueller and
Hooker Glaciers.

His literary contributions are of greater value to science than to
the domain of Alpine record; but naturally they are of the deepest
interest to the latter class of literature, inasmuch as they tell the
tale of the opening out of fresh Alpine fields which are destined
to become—indeed they are now fast becoming—areas of great
mountaineering importance.

Though Von Haast was perhaps the first man of science or literature to
visit these great glaciers, yet their existence was well known to a few
run-holders and early settlers who had penetrated even thus far into
the mountains in the ‘early days’ of New Zealand.

It is to Mr. Edward Percy Sealy of Timaru, however, that we owe the
first close acquaintance of the Mueller, Hooker, and Tasman Glaciers.
Mr. Sealy was a surveyor by profession and a photographer of no mean
ability, and to his energy and perseverance we are indebted for results
which furnished Dr. von Haast with material for constructing his map of
this part of our Alps.

Upon visiting the glaciers at the present time, and being impressed
with the difficulties of transit, one cannot but be filled with
admiration for the man who achieved such splendid results in
photography, burdened as he was with all the necessary and cumbersome
paraphernalia pertaining to the old wet-plate system then in vogue.

Mr. Sealy traversed nearly the whole length of the Mueller Glacier in
1867, and in 1869 pushed his way up the Hooker as far as the tributary
Empress Glacier, and up the Tasman as far as the great turn at Mount De
la Bêche.

To Mrs. Leonard Harper, of Ilam, belongs the honour of being the first
lady to cross to the Aorangi side of the Tasman River.

On this occasion (in March 1873) the party consisted of Mr. and Mrs.
Leonard Harper, of Christchurch, Messrs. G. Dennistoun, G. Parker,
Melville Gray, Wright, C. Smith, and Flint. They camped at Governor’s
Bush, close to where the Hermitage now stands, and went on to the
Mueller Glacier and to the terminal face of the Tasman. Mr. and Mrs.
Harper returned across the Tasman River, leaving the rest of the
party to attempt the passage to the west coast by the Hooker Saddle,
at the head of the glacier of the same name. In this, as may be easily
conceived—considering that the members of the party were inexperienced
and not properly equipped for such an expedition—the party was
unsuccessful, only reaching a point just above where the clear ice
merges into the moraine, and where the crevasses began to appear
formidable.

For many years after this the glaciers were not traversed to any extent
save by camping-out parties, who contented themselves with short
excursions about the terminal faces, until, in 1882, a fresh interest
was awakened in their existence by the visit of the Rev. W. S. Green
with Herr Emil Boss, of Grindelwald, and Ulrich Kaufmann as guide.
His advent was indeed an awakening, and the apathy of the Colonials
regarding the scenic marvels of their own country was somewhat aroused.
The sensation caused by his memorable ascent of Aorangi, after repeated
struggles with flooded rivers and all those hindrances which seem to
fall inevitably to the lot of men who first open out a new district,
has become quite an event of history in the annals of the colony.

Full particulars of Mr. Green’s doings will be found in his admirable
book, ‘The High Alps of New Zealand,’ published by Macmillan & Co.

To Mr. Green undoubtedly belongs the honour of having first introduced
into New Zealand the proper system of Alpine climbing, and he will ever
be looked back to as the father of the noble sport in the colony.

Then, in 1883, followed the visit of Dr. R. von Lendenfeld, a
mountaineer and scientific man of great attainments. He was accompanied
by his plucky wife, and, aided by porters procured in the colony,
during a stay of nineteen days on the Tasman Glacier completed a survey
of the same, and finished up his work by ascending the Hochstetter
Dome, whose higher and easternmost summit he attained in an expedition
extending over a period of twenty-seven hours from his last camp under
the Malte Brun range, accompanied by his wife and one porter.

Full particulars of his work were made public in Petermann’s
‘Mitteilungen,’[3] and a short English notice of the same may be found
in the ‘Alpine Journal,’ vol. xii. page 163.

[Footnote 3: _Ergänzungsheft_, No. 75. Dr. R. von Lendenfeld, _Der
Tasman-Gletscher und seine Umgebung_.]

Shortly after this the Hermitage Company, Limited, was formed, and
the Hermitage Hotel erected near the terminal face of the Mueller
Glacier. This first Alpine hotel of New Zealand was not built without
many serious difficulties, and the ultimate success of the undertaking
speaks volumes for the perseverance of the enthusiastic manager, Mr.
F. F. C. Huddleston. This gentleman has made various excursions on
the Mueller and Hooker Glaciers since the building of the Hermitage,
and possesses an intimate knowledge of the Alpine district around the
hotel. He has, with a party of two others, penetrated, I understand, as
far as the junction of the Empress Glacier on the Hooker, and has since
effected the passage of the Ball Pass from the Tasman to the Hooker
Glaciers.

In 1886 the author began his visits to the districts with properly
equipped Alpine parties, the results of which expeditions have been
given in the foregoing pages.

In 1889 the Government surveys were extended to the Mueller and
Hooker Glaciers, under Mr. Brodrick, a gentleman whose capability and
never-failing pluck in carrying out his work in such rough country is
only equalled by his modesty concerning his Alpine achievements, which
are necessarily incidental to his profession in the district.

Those of my readers who are acquainted with survey and topographical
work amongst the Alps will appreciate the results of but two seasons’
work in the map of the four great glaciers appended to this book.
Climbers will be interested to know that amongst difficult points
attained by Mr. Brodrick are the saddles at the head of the Mueller
Glacier, that connecting the Murchison and Classen Glaciers, the lower
summit of the Hochstetter Dome, and a peak of 8,015 feet on the Liebig
Range.

In 1890, Mr. Malcolm Ross, of Dunedin, a gentleman who has done much
travelling and some exploring in the Southern Lakes district, and
had tried his ’prentice hand upon Mount Earnslaw, visited the Tasman
Glacier in company with his wife. Bad weather frustrated his attempts
at mountaineering, with the exception of an ascent of a peak of about
7,000 feet on the Mount Cook Range, and a partial ascent of Mount
Sealy. He traversed the Tasman Glacier to a point some miles beyond the
junction of the Hochstetter Glacier.

In December 1890 Messrs. A. P. Harper, R. Blakiston, and Beadel made an
excursion to the Tasman Glacier, but bad weather kept them prisoners at
camp nearly all the time of their stay. Messrs. Harper and Blakiston,
after retreating from the Tasman, succeeded in reaching for the first
time the saddle at the head of the Hooker Glacier (8,580 feet), after
a trying expedition. This had been attempted several times before, but
owing to numberless crevasses was found to be unattainable. Being early
in the season and after a considerable snow-fall, however, the party
in question found the crevasses mostly covered, and they were aided,
moreover, by Mr. Harper’s skill and knowledge of Alpine work.

Again, in January 1891, Messrs. Harper and Johnson visited the Tasman
Glacier, and besides attaining a high saddle (about 7,500 feet) in the
Malte Brun Range and making a nearly complete ascent of Mount Sealy,
secured a fine collection of photographs.

       *       *       *       *       *

Such, in brief, is a history of what Alpine work has been accomplished
amongst the Southern Alps of New Zealand. Other glacier excursions, it
is true, there have been, but they are few, and with the exception of
the expeditions of Mr. Sealy and the Government Survey to the Godley
and Classen Glaciers farther north, and of a few attempts to climb
Mount Earnslaw in the Southern Lake district, are not worthy of much
note as Alpine expeditions, undertaken in the orthodox manner with axe
and rope.

As these lines are being penned the New Zealand Alpine Club is in
process of formation, and the writer hears with pleasure of the
probabilities of success which are likely to attend the efforts of the
promoters of the club.

Letters of advice and encouragement from prominent members of the
English Alpine Club have at various times come to hand, and the
friendly interest of mountain explorers of the early days of the
colony gives promise of an auspicious birth to one of those bodies of
enthusiasts whose aims may not be mercenary and self-seeking, but whose
operations may contribute their little unit to the art, literature, and
scientific observation of the times.

Who can say what the future may bring forth in the matter of Alpine
climbing in New Zealand? There is an immense field—magnificent
glaciers and noble peaks without number, as yet practically untouched.

One can already see visions of parties of enthusiasts threading their
way amongst intricate ice-falls, cutting steps up hard ice slopes,
conquering by persistent effort splendid rock peaks, drinking in the
glories of a new and fascinating world. Not climbing from a gymnast’s
point of view, but climbing because—why? They cannot tell you why; but
because they feel and know the physical and spiritual benefits of a
closer contact with Nature, with an Omnipotent and Ever-guiding Hand,
which rules all things and creates a heaven even upon earth.




_A SHORT GLOSSARY OF TECHNICAL ALPINE TERMS._


_Arête._—A ridge either of rock, ice, or snow, or combinations of all
three.

_Bergschrund._—The crevasse or deep moat almost invariably found
between the sides and upper portions of a glacier or ice slope and the
rocks above, or the permanent clinging ice above, as the case may be.
Of late the meaning of the term has become extended, and almost any
crevasse in the upper parts of a glacier with one lip higher than the
other comes under the designation.

_Col._—Saddle, or dip in a ridge.

_Cornice._—The overhanging edge of an _arête_ caused by drifting snow.

_Couloir._—A ditch or deep gully in the mountain side; in the upper
regions being usually floored with ice and swept by avalanches.

_Crevasse._—The rent caused by fracture of the ice under tension.

_Gendarme_, or _rock tower_.—A mass of rock on the crest of an _arête_.

_Moraine._—The accumulation of detritus which has fallen from the
mountains on to the ice and is carried down upon it.

_Névé_, or _firn_.—Snow in a transition stage between snow and ice.
The large fields of this feeding a glacier are spoken of as the _névés_
of the glacier.

_Séracs._—Blocks of ice broken into polyhedral masses (mostly cubic)
by the body of the ice being crevassed in various lines of fracture. So
called from the resemblance the blocks bear to a certain kind of cheese.

_Shale slips_ and _shingle and boulder fans_ are of very common
occurrence in the New Zealand mountains and are caused by the discharge
of detritus down _couloirs_, from which when emerging it spreads out
into fan-shaped slopes.


                PRINTED BY
  SPOTTISWOODE AND CO., NEW-STREET SQUARE
                  LONDON


[Illustration: _Longmans, Green & Co., London & New York._

_F. S. Weiler._]




      *      *      *      *      *      *




Transcriber’s note:

Footnote numbers have been changed to 1, 2 and 3, to avoid confusion.

The spelling of Ranunculus lyalii in the Table of Illustrations and
on Page 86 have been corrected to lyallii. (The species was discovered
by David Lyall, a noted Scottish botanist and doctor.)
Ranunculus lyallii is spelt correctly on Page 9.

Obvious punctuation errors were corrected.

The changes are as follows:

    In the CONTENTS, Chapter III—river-crossing changed to river crossing.
    Page 10—northeastern changed to north-eastern.
    Page 12—ice-streams changed to ice streams.
    Page 30—river bed changed to river-bed.
    Page 30—downstream changed to down-stream.
    Page 35—breakwind changed to break-wind.
    Page 54—look-out changed to look out.
    Page 55—life-time changed to lifetime.
    Page 66—shangai changed to shanghai.
    Page 84—ice-blocks changed to ice blocks.
    Page 89—one day changed to one-day.
    Page 93 and Page 139—mountain-side changed to mountain side.
    Page 97—red-sandstone changed to red sandstone.
    Page 101—step cutting changed to step-cutting.
    Page 103—foot-hold changed to foothold.
    Page 114—water-courses changed to watercourses.
    Page 119—cockleshells changed to cockle-shells.
    Page 120—starting-point changed to starting point.
    Page 126—rabbit-fence changed to rabbit fence.

*** END OF THE PROJECT GUTENBERG EBOOK 60919 ***