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CHAPTER IX THE CONQUEST OF MOUNT EREBUS There was one
journey possible, a
somewhat difficult undertaking certainly, yet gaining an interest and,
excitement from that very reason, and this was an attempt to reach the
summit
of Mount Erebus. For many reasons the accomplishment of this work
seemed to be
desirable. In the first place the observations of temperature and wind
currents
at the summit of this great mountain would have an important bearing on
the
movements of the upper air, a meteorological problem as yet but
imperfectly
understood. From a geological point of view the mountain ought to
reveal some
interesting facts, and apart from scientific considerations, the ascent
of a
mountain over 13,000 ft. in height, situated so far south, would be a
matter of
pleasurable excitement both to those who were selected as climbers and
to the
rest of us who wished for our companions' success. After consideration
I
decided that Professor David, Mawson, and Mackay should constitute the
party
that was to try to reach the summit, and they were to be provisioned
for ten
days. A supporting-party, consisting of Adams, Marshall, and
Brocklehurst, was
to assist the main-party as far as feasible. The whole expedition was
to be
under Adams' charge until he decided that it was time for his party to
return,
and the Professor was then to be in charge of the advance party. In my
written
instructions to Adams, he was given the option of going on to the
summit if he
thought it feasible for his party to push on; and, he actually did so,
though
the supporting-party was not so well equipped for the mountain work as
the
advance-party, and was provisioned for six days only. Instructions were
given
that the supporting-party was not to hamper the main-party, especially
as
regarded the division of provisions, but, as a matter of fact, instead
of
hampering, the three men became of great assistance to the advance
division,
and lived entirely on their own stores and equipment during the whole
trip. No
sooner was it decided to make the ascent, which was arranged for,
finally, on
March 4, than the winter quarters became busy with the bustle of
preparation.
There were crampons to be made, food-bags to be prepared and filled,
sleeping-bags to be overhauled, ice-axes to be got out and a hundred
and one
things to be seen to; yet such was the energy thrown into this work
that the
men were ready for the road and made a start at 8.30 A.M. on the 5th. In a previous
chapter I have
described the nature and extent of equipment necessary for a sledging
trip, so
that it is not necessary now to go into details regarding the
preparations for
this particular journey, the only variation from the usual standard
arrangement
being in the matter of quantity of food. In the ascent of a mountain
such as
Erebus it was obvious that a limit would soon be reached beyond which
it would
be impossible to use a sledge. To meet these circumstances the
advance-party
had made an arrangement of straps by which their single sleeping-bags
could be
slung in the form of a knapsack upon their backs, and inside the bags
the
remainder of their equipment could be packed. The men of the
supporting-party,
in case they should journey beyond ice over which they could drag the
sledge,
had made the same preparations for transferring their load to their
shoulders.
When they started I must confess that I saw but little prospect of the
whole
party reaching the top, yet when, from the hut, on the third day out,
we saw
through Armytage's powerful telescope six tiny black spots slowly
crawling up
the immense deep snow-field to the base of the rugged rocky spurs that
descended to the edge of the field, and when I saw next day out on the
sky-line
the same small figures, I realised that the supporting-party were going
the
whole way. On the return of this expedition Adams and the Professor
made a full
report, with the help of which I will follow the progress of the party,
the
members of which were winning their spurs not only on their first
Antarctic
campaign, but in their first attempt at serious mountaineering. Mount Erebus bears a name that has loomed large in the history of polar exploration both north and south. Sir James Clark Ross, on January 28, 1841, named the great volcano at whose base our winter quarters were placed after the leading ship of his expedition. The final fate of that ship is linked with the fate of Sir John Franklin and one of the most tragic stories of Arctic exploration, but though both the Erebus and Terror have sunk far from the scenes of their first exploration, that brilliant period of Antarctic discovery will ever be remembered by the mountains which took their names from those stout ships. Standing as a sentinel at the gate of the Great Ice Barrier, Erebus forms a magnificent picture. The great mountain rises from sea-level to an altitude of over 13,000 ft., looking out across the Barrier, with its enormous snow-clad bulk towering above the white slopes that run up from the coast. At the top of the mountain an immense depression marks the site of the old crater, and from the side of this rises the active cone, generally marked by steam or smoke. The ascent of such a mountain would be a matter of difficulty in any part of the world, hardly to be attempted without experienced guides, but the difficulties were accentuated by the latitude of Erebus, and the party started off with the full expectation of encountering very low temperatures. The men all recognised, however, the scientific value of the achievement at which they were aiming, and they were determined to do their utmost to reach the crater itself. How they fared and what they found will be told best by extracts from the report which was made to me. THE FIRST SLOPES OF EREBUS Pulling the
sledge proved fairly
heavy work in places; at one spot, on the steep slope of a small
glacier, the
party had a hard struggle, mostly on their hands and knees, in their
efforts to
drag the sledge up the surface of smooth blue ice thinly coated with
loose
snow. This difficulty surmounted, they encountered some sastrugi, which
impeded
their progress somewhat. " Sastrugi " means wind furrow, and is the
name given to those annoying obstacles to sledging, due to the action
of the
wind on the snow. A blizzard has the effect of scooping out hollows in
the
snow, and this is especially the case when local currents are set up
owing to
some rock or point of land intercepting the free run of the wind. These
sastrugi vary in depth from two or three inches to three or four feet,
according to the position of any rock masses that may be near and to
the force
of the wind forming them. The raised masses of snow between the hollows
are
difficult to negotiate with a sledge, especially when they run more or
less
parallel to the course of the traveller. Though they have many
disadvantages,
still there are times when their presence is welcome; especially is
this the
case when the sky is overcast and the low stratus cloud obliterates all
landmarks.
At these times a dull grey light is over everything, and it is
impossible to
see the way to steer unless one takes the line of sastrugi and notes
the angle
it makes with the compass course, the compass for the moment being
placed on
the snow to obtain the direction. In this way one can steer a fairly
accurate
course, occasionally verifying it by calling a halt and laying off the
course
again with the compass, a precaution that is very necessary, for at
times the
sastrugf alter in direction. The sledgers,
at this particular
juncture, had much trouble in keeping their feet, and the usual
equanimity of
some of the men was disturbed, their remarks upon the subject of
sastrugi being
audible above the soft pad of the finnesko, the scrunch of the
ski-boots, and
the gentle sawing sound of the sledge-runners on the soft snow. About 6
P.M.
the party camped at a small nunatak of black rock, about 2750 ft. above
sea-level and a distance of seven miles from winter quarters. After a
good hot
dinner they turned into their sleeping-bags in the tents and were soon
sound
asleep. The following morning, when the men got up for breakfast, the
temperature was 10° below zero Fahr., whilst at our winter quarters at
the same
time it was zero. They found, on starting, that the gradient was
becoming much
steeper, being 1 in 5, and sastrugi, running obliquely to their course,
caused
the sledge to capsize frequently. The temperature was 8° below zero
Fahr., but
the pulling was heavy work and kept the travellers warm. They camped
that
night, March 6, at an altitude of 5630 ft., having travelled only three
miles
during the whole day, but they had ascended over 2800 ft. above their
previous
camp. The temperature that night was 28° below zero Fahr. The second
camp was
in a line with the oldest crater of Erebus, and from the nature of the
volcanic
fragments lying around, the Professor was of the opinion that Erebus
had been
producing a little lava within its crater quite recently. On the
following morning Adams
decided that the supporting-party should make the attempt with the
forward-party to reach the summit. I had left the decision in this
matter to
his discretion, but I myself had not considered there would be much
shance of
the three men of the supporting-party gaining the summit, and had not
arranged
their equipment with that object in view. They were thus handicapped by
having
a three-man sleeping-bag, which bulky article one man had to carry;
they also
were not so well equipped for carrying packs, bits of rope having to
act as
substitutes for the broad straps provided for the original advance
party. The
supporting-party had no crampons, and so found it more difficult, in
places, to
get a grip with their feet on the slippery surface of the snow slopes.
However,
the Professor, who had put bars of leather on his ski-boots, found that
these
answered as well as crampons, and lent the latter to Marshall. Both
Adams and
the Professor wore ski-booth during the whole of the ascent. Ski could
not be
used for such rough climbing, and had not been taken. All the men were
equipped
with both finnesko and ski-boots and with the necessaries for camping,
and
individual tastes had been given some latitude in the matter of the
clothing
worn and carried. The six men
made a depot of the
sledge, some of the provisions and part of the cooking-utensils at the
second
camp, and then resumed the climb again. They started off with
tent-poles
amongst other equipment, but after going for half a mile they realised
it would
be impossible to climb the mountain with these articles, which were
taken back
to the depot. Each man carried a weight of about 40 lb., the party's
gear
consisting chiefly of sleeping-bags, two tents, cooking apparatus, and
provisions for three days. The snow slopes became steeper, and at one
time Mackay,
who was cutting steps on the hard snow with his ice-axe, slipped and
glissaded
with his load for about a hundred feet, but his further downward career
was
checked by a projecting ledge of snow, and he was soon up again. On the
third
evening, March 7, the party camped about 8750 ft. above sea-level, the
temperature at that time being 20* below zero Fahr. Between 9 and
10 P.M. that night a
strong wind sprang up, and when the men awoke the following morning
they found
a fierce blizzard blowing from the south-east. It increased in fury as
the day
wore on, and swept with terrific force down the rocky ravine where they
were
camped. The whirling snow was so dense and the roaring wind so loud
that,
although the two sections were only about ten yards apart, they could
neither
see nor hear each other. Being without tent-poles, the tents were just
doubled
over the top ends of the sleeping-bags so as to protect the openings
from the
drifting snow, but, in spite of this precaution, a great deal of snow
found its
way into the bags. In the afternoon Brocklehurst emerged from the
three-man
sleeping-bag, and instantly a fierce gust whirled away one of his
wolfskin mite;
he dashed after it, and the force of the wind swept him some way down
the
ravine. Adams, who had left the bag at the same time as Brocklehurst,
saw the
latter vanish suddenly, and in endeavouring to return to the bag to
fetch
Marshall to assist in finding Brocklehurst he also was blown down by
the wind.
Meanwhile, Marshall, the only remaining occupant of the bag, had much
ado to
keep himself from being blown, sleeping-bag and all, down the ravine.
Adams had
just succeeded in reaching the sleeping-bag on his hands and knees when
Brocklehurst appeared, also on his hands and knees, having, by
desperate efforts,
pulled himself back over the rocks. It was a close call, for he was all
but
completely gone, so biting was the cold, before he reached the haven of
the
sleeping-bag. He and Adams crawled in, and then, as the bag had been
much
twisted up and drifted with snow while Marshall had been holding it
down, Adams
and Marshall got out to try and straighten it out. The attempt was not
very
successful, as they were numb with cold and the bag, with only one
person
inside, blew about, so they got into it again. Shortly afterwards Adams
made
another attempt, and whilst he was working at it the wind got inside
the bag,
blowing it open right way up. Adams promptly got in again, and the
adventure
thus ended satisfactorily. The men could do nothing now but lie low
whilst the
blizzard lasted. At times they munched a plasmon biscuit or some
chocolate.
They had nothing to drink all that day, March 8, and during the
following
night, as it would have been impossible to have wept a lamp alight to
thaw out
the snow. They got some sleep during the night in spite of the storm.
On
awaking at 4 A.M. the following day, the travellers found that the
blizzard was
over, so, after breakfast, they started away again at about 5.30 A.M. The angle of
ascent was now
steeper.than ever, being thirty-four degrees, that is, a rise of 1 in
1i. As
the hard snow slopes were much too steep to climb without cutting steps
with an
ice-axe, they kept as much as possible to the bare rocks. Occasionally
the
artte would terminate upwards in a large snow slope, and when this was
the case
they cut steps across the slope to any other bare rocks which seemed to
persist
for some distance in an upward direction. Brocklehurst, who was wearing
ski-boots, began to feel the cold attacking his feet, but did not think
it was
serious enough to change into finnesko. At noon they found a fair
camping-ground, and made some tea. They were, at this time, some 800
ft. below
the rim of the old crater and were feeling the effects of the high
altitude and
the extreme cold. Below them was a magnificent panorama of clouds,
coast and
Barrier snow, but they could not afford to spend much time admiring it.
After a
hasty meal they tackled the ascent again. When they were a little
distance from
the top of the rim of the main crater, Mackay elected to work his way
alone
with his ice-axe up a long and very steep nova slope instead of
following the
less difficult and safer route by the rocks where the rest of the party
were
proceeding. He pasbed out of sight, and then the others heard him call
out that
he was getting weak and did not think he could carry oa much longer...
They
made haste to the top of the ridge, and Marshall and the Professor
dropped to
the point where he was likely to be found. Happily, they met him coming
towards
them, and Marshall took his load, for he looked much done up. It
appeared that
Mackay had found the work of cutting steps with his heavy load more
difficult
than he had anticipated, and he only just managed to reach safety when
he fell
and fainted. No doubt this was due, in part, to mountain sickness,
which, under
the severe conditions and at the high altitude the party had attained,
also
affected Brocklehurst. t Having found
a camping-place, they
dropped their loads, and the members of the party were at leisure to
observe
the nature of their surroundings. They had imagined an even plain of
neve or
glacier ice filling the extinct crater to the brim and sloping up
gradually to
the active cone at its southern end, but instead of this they found
themselves
on the very brink of a precipice of black rock, forming the inner edge
of the
old crater. This wall of dark lava was mostly vertical, while, in some
places,
it overhung, and was from eighty to a hundred feet in height. The base
of the
cliff was separated from the snow plain beyond by a deep ditch like a
huge dry
moat, which was evidently due to the action of blizzards. These winds,
striking
fiercely from the south-east against the great inner wall of the old
crater,
had given rise to a powerful back eddy at the edge of the cliff, and it
was
this eddy which had scooped out the deep trench in the hard snow. The
trench
was from thirty to forty feet deep, and was bounded by more or less
vertical
sides. Around our winter quarters any isolated rock or cliff face that
faced
the south-east blizzard-wind exhibited a similar phenomenon, though, of
course,
on a much smaller scale. Beyond the wall and trench was an extensive
snow-field
with the active cone and crater at its southern end, the latter
emitting great
volumes of steam, but what shrprised the travellers most were the
extraordinary
structures which rose here snd there above the surface of the
snow-field. They
were in the form of mounds and pinnacles of the most varied and
fantastic
appearance. Some resembled beehives, others were like huge ventilating
cowls,
others like isolated turrets, and others again resembled various
animals in
shape. The men were unable at first sight to understand the origin of
these
remarkable structures, and as it was time for food, they left the
closer investigation
for later in the day. As they walked
along the rampart of
the old crater.wall to find a camping-ground, their figures were thrown
up
against the sky-line, and down at our winter quarters they were seen by
us,
having been sighted by Armytage with his telescope. He had followed the
party
for the first two days with the glasses, but they were lost to view
when they
began to work through the rocky ground, and it was just on the crater
edge that
they were picked up again by the telescope. ONE THOUSAND FEET BELOW THE ACTIVE CONE The camp chosen
for the meal was in
a little rocky gully on the north-west slope of the main cone, and
about fifty
feet below the rim of the old crater. Whilst some cooked the meal,
Marshall
examined Brocklehurst's feet, as the latter stated that for some time
past he
had lost all feeling in them. When his ski-boots and socks had been
taken off,
it was found that both his big toes were black, and that four more
toes, though
less severely affected were also frost-bitten. From their appearance it
was
evident that some hours must have elapsed since this had occurred.
Marshall and
Mackay set at work at once to restore circulation in the feet by
warming and
chafing them. Their efforts were, under the circumstances, fairly
successful,
but it was clear that ultimate recovery from so severe a frost-bite
would be
both slow and tedious. Brocklehurst's feet, having been thoroughly
warmed were
put into dry socks and finnesko stuffed with sennegrass, and then all
hands
went to lunch at 3.30 P.M. It must have required great pluck and
determination
on his part to have climbed almost continuously for nine hours up the
steep and
difficult track they had followed with his feet so badly frost-bitten.
After
lunch Brockiehurst was left safely tucked up in the three-man
sleeping-bag, and
the remaining five members of the party started off to explore the
floor of the
old crater. Ascending to the crater rim, they climbed along it until
they came
to a spot where there was a practicable breach in the crater wall and
where a
narrow tongue of snow bridged the neve trench at its base. They all roped
up directly they
arrived on the hard snow in the crater and advanced cautiously over the
snow-plain, keeping a sharp look-out for crevasses. They steered for
some of
the remarkable mounds already mentioned, and when the nearest was
reached and
examined, they noticed some curious hollows, like partly roofed-in
drains,
running towards the mound. Pushing on slowly, they reached eventually a
small
parasitic cone, about 1000 ft. above the level of their camp, and over
a mile
distant from it. Sticking out from under the snow were lumps of lava,
large
felspar crystals, from one to three inches in length, and fragments of
pumice; both
felspar and pumice were in many cases coated with sulphur. Having made
as
complete an examination as time permitted, they started to return to
camp, no
longer roped together, as they had not met any definite crevasses on
their way
Aut. They directed their steps towards one of the ice mounds, which
bore a
whimsical resemblance to a lion couch-ant, and from which smoke
appeared to be
issuing. To the Professor the origin of these peculiar structures was
now no
longer a mystery, for he recognised that they were the outward and
visible
signs of fumaroles. In ordinary climates, a fumarole, or volcanic
vapour-well,
may be detected by the thin cloud of steam above it, and usually one
can at
once feel the warmth by passing one's hand into the vapour column, but
in the
rigour of the Antarctic climate the fumaroles of Erebus have their
vapour
turned into ice as soon as it reaches the surface of the snow-plain.
Thus ice
mounds, somewhat similar in shape to the sinter mounds formed by the
geysers of
New Zealand, of Iceland and of Yellowstone Park, are built up round the
orifices of the fumaroles of Erebus. Whilst exploring one of these
fumaroles,
Mackay fell suddenly up to his thighs into one of its concealed
conduits, and
only saved himself from falling in deeper still by means of his
ice-axe.
Marshall had a similar experience at about the same time. The party
arrived at camp shortly
after 6 P.M., and found Brocklehurst progressing as well as could be
expected.
They sat on the rocks after tea admiring the glorious view to the west.
Below
them was a vast rolling sea of cumulus cloud, and far away the western
mountains glowed in the setting sun. Next morning, when they got up at
4 A.M.,
they had a splendid view of the shadow of Erebus projected on the field
of
cumulus cloud below them by the rising sun. Every detail of the profile
of the
mountain as outlined on the clouds could readily be recognised. After
breakfast, while Marshall was attending to Brocklehurst's feet, the
hypsometer,
which had become frozen on the way up, was thawed out and a
determination of
the boiling-point made. This, when reduced and combined with the mean
of the
aneroid levels, glade the altitude of the old crater rim, just above
the vamp,
11,400 ft. At 6 A.M. the party left the camp and made all speed to
reach the
summit of the present crater. On their way across the old crater,
Mawson
photographed the fumarole that resembled the lion and also took a view
of the
active crater about one and a half miles distant, though there was
considerable
difficulty in taking photographs owing to the focal plane shutter
having become
jammed by frost. Near the furthest point reached by the travellers on
the
preceding afternoon they observed several patches of yellow ice and
found on
examination that the colour was due to sulphur. They next ascended
several
rather steep slopes formed of alternating beds of hard snow and vast
quantities
of large and perfect felspar crystals, mixed with pumice. A little
farther on
they reached the base of the volcano's active cone. Their progress was
now
painfully slow, as the altitude and cold combined to make respiration
difficult. The cone of Erebus is built up chiefly of blocks of pumice,
from a
few inches to a few feet in diameter. Externally these were grey or
often
yellow owing to incrustations of sulphur, but when broken they were of
a
resinous brown colour. At last, a little after 10 A.M., on March 10,
the edge
of the active crater was reached, and the little party stood on the
summit of
Erebus, the first men to conquer perhaps the most remarkable summit in
the
world. They had travelled about two and a half miles from the last
camp, and
had ascended just 2000 ft., and this journey had taken them over four
hours.
The report describes most vividly the magnificent and awe-inspiring
scene
before them. "We stood on
the verge of a
vast abyss, and at first could see neither to the bottom nor across it
on
account of the huge mass of steam filling the crater and soaring aloft
in a
column 500 to 1000 ft. high. After a continuous loud hissing sound,
lasting for
some minutes, there would come from below a big dull boom, and
immediately
great globular masses of steam would rush upwards to swell the volume
of the
snow-white cloud which ever sways over the crater. This phenomenon
recurred at
intervals during the whole of our stay at the crater. Meanwhile, the
air around
us was extremely redolent of burning sulphur. Presently a pleasant
northerly
breeze fanned away the steam cloud, and ab once the whole crater stood
revealed
to us in all its vast extent and depth. Mawson's angular measurement
made the
depth 900 ft. and the greatest width about half a mile. There were ab
least
three well-defined openings at the bottom of the cauldron, and it was
from
these that the steam explosions proceeded. Near the south-west portion
of the
crater there was an immense rift in the rim, perhaps 300 to 400 ft.
deep. The
crater wall opposite the one at the top of which we were standing
presented
features of special interest. Beds of dark pumiceous lava or pumice
alternated
with white zones of snow. There was no direct evidence that the snow
was bedded
with the lava, though it was possible that such may have been the case.
From
the top of one of the thickest of the lava or pumice beds, just where
it
touched the belt of snow, there rose scores of small steam jets all in
a row.
They were too numerous and too close together to have been each an
independent
fumarole; the appearance was rather suggestive of the snow being
converted into
steam by the heat of the layer of rock immediately below it." While at the
crater's edge the party
made a boiling-point determination by the hypsometer, but the result
was not so
satisfactory as that made earlier in the morning at the camp. As the
result of
averaging aneroid levels, together with the hypsometer determination at
the top
of the old crater, Erebus may be calculated to rise to a height of
13,370 ft.
above sea-level. As soon as the measurements had been made and some
photographs
had been taken by Mawson, the party returned to the camp, as it had
been
decided to descend to the base of the main cone that day, a drop of
8000 ft. On the way back
a traverse was made
of the main crater and levels taken for constructing a geological
section.
Numerous specimens of the unique felspar crystals and of the pumice and
sulphur
were collected. On arriving in camp the travellers made a hasty meal,
packed
up, shouldered their burdens once more and started down the steep
mountain
slope. Brocklehursb insisted on carrying his own heavy load in spite of
his
frost-bitten feet. They followed a course a little to the west of the
one they
took when ascending. The rock was rubbly and kept slipping under their
feet, so
that falls were frequent. After descending a few hundred feet they
found that
the rubbly spur of rock down which they were floundering ended abruptly
in a
long and steep neve) slope. Three courses were now open to them: they
could
retrace their steps to the point above them where the rocky spur had
deviated
from the main arete; cut steps across the nevi) slope; or glissade down
some five
or six hundred feet to a rocky ledge below. In their tired state
preference was
given to the path of least resistance, which was offered by the
glissade, and
they therefore rearranged their loads so that they would roll down
easily. They
were now very thirsty, but they found that if they gathered a little
snow,
squeezed it into a ball and placed it on the surface of a piece of
rock, it
melted at once almost on account of the heat of the sun and thus they
obtained
a makeshift drink They
launched their loads
down the slope and
watched them as they bumped and bounded over the wavy ridges of neve.
Brocklehurst's load, which contained the cooking-utensils, made the
noisiest
descent, and the aluminium cookers were much battered when they finally
fetched
up against the rocks below. Then the members of the party, grasping
their
ice-axes firmly, followed their gear. As they gathered speed on the
downward
course and the chisel-edge of the ice-axe bit deeper into the hard
neve, their
necks and faces were sprayed with a shower of ice. All reached the
bottom of
the slope safely, and they repeated this glissade down each succeeding
snow
slope towards the foot of the main cone. Here and there they bumped
heavily on
hard sastrugi and both clothes and equipment suffered in the rapid
descent; unfortunately
also, one of the aneroids was lost and one of the hypsome ter
thermometers
broken. At last the slope flattened out to the gently inclined terrace
where
the depot lay, and they reached it by walking. Altogether they had
dropped down
5000 ft. between three in the afternoon and seven in the evening. Adams and
Marshall were the first to
reach the depot, the rest of the party, with the exception of
Brocklehurst,
having made a detour to the left in consequence of having to pursue
some lost
luggage in that direction. At the depot they found that the blizzard of
the 8th
had played havoc with their gear, for the sledge had been overturned
and some
of the load scattered to a distance and partly covered with drift-snow.
After
dumping their packs, Adams and Marshall went to meet Brocklehurst, for
they
noticed that a slight blizzard was springing up. Fortunately, the wind
soon
died down, the weather cleared, and the three were able to regain the
camp. Tea
was got ready, and the remainder of the party arrived about 10 P.M.
They camped
that night at the depot and at 3 A.M. next day got up to breakfast.
After
breakfast a hunt was made for some articles that were still missing,
and then
the sledge was packed and the march homewards commenced at 5.30 A.M.
They now
found that the sastrugi caused by the late blizzard were very
troublesome, as
the ridges were from four to five feet above the hollows and lay at an
oblique
angle to the course. Rope brakes were put on the sledge-runners, and
two men
went in front to pull when necessary, while two steadied the sledge,
and two
were stationed behind to pull back when required. It was more than
trying to
carry on at this juncture, for the sledge either refused to move or
suddenly it
took charge and overran those who were dragging it, and capsizes
occurred every
few minutes. Owing to the slippery nature of the ground some members of
the
party who had not crampons or barred ski-boots were badly shaken up,
for they
sustained numerous sudden falls. One has to experience a surface like
this to
realise how severe a jar a fall entails. The only civilised experience
that is
akin to it is when one steps unknowingly on a slide which some small
street boy
has made on the pavement. Marshall devised the best means of assisting
the
progress of the sledge. When it took charge he jumped on behind and
steered it
with his legs as it bumped and jolted over the sastrugi, but he found
sometimes
that his thirteen-stone weight did not prevent him from being bucked
right over
the sledge and flung on the nevi on the other side. THE "LION" OF EREBUS Meanwhile, at
winter quarters, we
had been very busy opening cases and getting things ship-shape outside,
with
the result that the cubicles of the absentees were more or less filled
with a
general accumulation of stores. When Armytage reported that he saw the
party on
their way down the day before they arrived at the hut, we decided to
make the
cubicles tidy for the travellers. We had just begun on the Professor's
cubicle
when, about 11 A.M. I left the hut for a moment and was astonished to
see
within thirty yards of me, coming over the brow of the ridge by the
hut, six
slowly moving figures. I ran towards them shouting: "Did you get to the
top?" There was no answer, and I asked again. Adams pointed with his
hand
upwards, but this did not satisfy me, so I repeated my question. Then
Adams
said: "Yes," and I ran back to the hut and shouted to the others, who
all came streaming out to cheer the successful venturers. We shook
hands all
round and opened some champagne, which tasted like nectar to the
way-worn
people. Marshall prescribed a dose to us stay-at-home ones, so that we
might be
able to listen quietly to the tale the party had to tell. Except to
Joyce, Wild, and myself,
who had seen similar things on the former expedition, the eating and
drinking
capacity of the returned party was a matter of astonishment. In a few
minutes
Roberts had produced a great saucepan of Quaker oats and milk, the
contents of
which disappeared in a moment, to be fallowed by the greater part of a
fresh-cut ham and home-made bread, with New Zealand fresh butter. The
six had
evidently found on the slopes of Erebus six fully developed, polar
sledging
appetites. The meal at last ended, came more talk, smokes and then bed
for the
weary travellers. After some
days' delay on account of
unfavourable weather, a party consisting of Adams, the Professor,
Armytage,
Joyce, Wild and Marshall, equipped with a seven-foot sledge, tent, and
provisions, as a precaution against possible bad weather, started out
to fetch
in the eleven-foot sledge with the explorers' equipment. After a heavy
pull
over the soft, new-fallen snow, in cloudy weather, with the temperature
at
mid-day 20* below zero Fahr., and with a stiff wind blowing from the
south-east, they sighted the nunatak, recovered the abandoned sledge
and
placing the smaller one on top, pulled them both back as far as Blue
Lake. I
went out to meet the party, and we left the sledge at Blue Lake until
the
following day, when two of the Manchurian ponies were harnessed to the
sledges
and the gear was brought into winter quarters. Professor David
gave me a short
summary of the scientific results of the ascent, from which I have made
the
following extracts: "Among the
scientific results
may be mentioned the calculation of the height of the mountain. Sir
Jas. C.
Ross in 1841 estimated the height to be 12,367 ft. The National
Antarctic
Expedition, 1901, determined its height at first to be 13,120 ft., but
this was
subsequently altered to 12,922 ft., the height now given on the
Admiralty Chart
of this region. Our observations for altitude were made partly with
aneroids
and partly with a hypsometer. All the aneroid levels and hypsometer
observations have been calculated by means of simultaneous readings of
the
barometer taken at our winter quarters, Cape Royds. These observations
show that
the rim of the second or main crater of Erebus is about 11,350 ft.
above
sea-level and that the summit of the active crater is about 13,350 ft.
above
sea-level. The fact may be emphasised that in both the methods adopted
by us
for estimating the altitude of the mountain, atmospheric pressure was
the sole
factor on which we relied. The determination arrived at by the Discovery was based on measurements made
with a theodolite from sea-level. It is, of course, quite possible that
Ross'
original estimate may have been correct, as this native volcano may
have
increased in height by about a thousand feet during the sixty-seven
years which
have elapsed since his expedition." "As regards the
geological
structure of Erebus, there is evidence of the existence of four
superimposed
craters. The oldest and lowest and at the same time, the largest of
these
attained an altitude of between 6000 and 7000 ft. above sea-level, and
was
fully six miles in diameter: the second rises to 11,350 ft. and has a
diameter
of over two miles: the third crater rises to a height of fully 12,200
ft.; and
its former outline has now been almost obliterated by the material of
the
modern active cone and crater. The latter, which rises about 800 ft.
above the
former, is composed chiefly of fragments of pumice. These vary in size
from an
inch or so to a yard in diameter. Quantities of felspar crystals are
interspersed with them, and both are incrusted with sulphur. "The active
crater measures
about half a mile by one-third of a mile in diameter, and is about 900
ft. in
depth. The active crater of Erebus is about three times as deep as that
of
Vesuvius. The fresh volcanic bombs picked up by us at spots four miles
distant
from the crater and lying on the surface of comparatively new snow are
evidences
that Erebus has recently been projecting lava to great heights. "Two features
in the geology of
Erebus which are specially distinctive are: the vast quantities of
large and
perfect felspar crystals, and the ice fumaroles. The crystals are from
two to three
inches in length; many of them have had their angles and edges slightly
rounded
by attrition, but numbers of them are beautifully perfect. "Its remarkable
crystals, rare
lavas and unique fumaroles are some of its most interesting geological
features:
it served as a gigantic tide-gauge to record the flood level of the
greatest
recent glaciation of Antarctica, when the whole of Ross Island was but
a
nunatak in a gigantic field of ice. "Its situation
between the belt
of polar calms and the South Pole; its isolation from the disturbing
influence
of large land masses; its great height, which enables it to penetrate
the whole
system of atmospheric circulation, and the constant steam cloud at its
summit,
swinging to and fro like a huge wind vane, combine to make Erebus one
of the
most interesting places on earth to the meteorologist." THE CRATER OF EREBUS, 900 FEET DEEP AND HALF A MILE WIDE. STEAM IS SEEN RISING ON THE LEFT. T HE PHOTOGRAPH WAS TAKEN FROM THE LOWER PART OF THE CRATER EDGE |