CHAPTER II.

PENDULUM ISLAND. STATE OF THE ICE NORTHWARDS.

LANDING ON SHANNON ISLAND.

Accident to Dr. Pansch.--Boat voyage to the

mainland.--Scientific operations.--Attempt of the Germania to

advance northwards.--Musk-oxen.

The group of islands known under the name of Pendulum Islands were

first discovered and appropriated by Clavering in the year 1823. He

anchored his ship, the Griper, on the south side of the largest island,

between it and the mainland. On this side of the island is good anchor

ground; several glacier streams debouche here, bringing with them soil

and mud, and the roads are protected from heavy ice by a small island

lying in front, which, from the number of walrus seen there, we called

Walrus Island.

According to our instructions, the position of Sabine’s Observatory

was to be sought for and newly marked, after which we were to advance

northward; this, of course, caused a stay of some days. The astronomers

brought out their instruments to determine our exact position, and

settling the magnetic constants on land, especially towards the tongue

of land eastward from our harbour (Cairn Point), where we conjectured

Sabine’s Observatory to have been, but of which, with all our seeking,

we could find not the slightest trace, nor of anything else which

might show that Europeans had ever visited the spot. First Lieutenant

Payer made preparations for surveying the island; and Dr. Pansch roamed

through it as explorer and naturalist, inspecting the remains of the

Esquimaux huts found by Sabine on the tongue of land to the west of our

stand-point.

In the afternoon the weather, which on our arrival had been unfriendly

and snowy, became fine and clear, with a perfect calm and a temperature

of 41° Fahr. From the plateau of the neighbouring mountains, the

barometrical height of which was 1040 feet, we had an extensive view

over the sea from the north-east round to the south, as well as over

the surrounding land, and along the coast to the north.

The condition of the ice was here first distinctly seen. The straits

between Sabine Island and the mainland, and also between the two

largest islands, were completely blocked with apparently old land ice.

Farther north, between Shannon Island and the mainland, as far as the

eye could reach, the ice was firm, and, from its whole position, we

might well conclude that there would be no breaking up that year. Along

the coast, therefore, we could not advance further north; the only

possible way remaining was by the eastern side of Shannon Island. This

island was distinctly seen, and seemed to be quite surrounded with ice;

though to the south side, and also to the east side of Pendulum Island,

there was open water, only covered with drift-ice. The pack-ice to the

east was very broad, stretching at least twelve nautical miles from

the coast, but farther southward it made a considerable curve inward

towards the land, and lay so dense that in 74°, and even more south

than that, we should with difficulty have been able to penetrate it.

Along the coast to the south there was also much open water, and

Gael Hamkes Bay appeared to be free from ice. For the next few days

scientific work kept us fully employed. In the evening Dr. Pansch

unfortunately shot himself in the arm while following a reindeer, and

had to be brought on board; we found, however, that the ball had only

gone through the muscles, and that no bone had been injured; but it

healed very slowly, and through the whole of the autumn, Dr. Pansch

could take but a small share in all our scientific explorations.

On the 6th it was slightly foggy, with a south wind; but the sun seemed

bright and clear, and the work suffered no interruption. Lieutenant

Payer roamed all over the island, topographically interested as well as

bent upon hunting.

We found many traces of reindeer, and saw a few without being fortunate

enough to kill one, though we killed several walrus which stopped in

our neighbourhood. The fat of these creatures was mostly thrown into

the coal bunk for fuel, in case the Hansa did not join us again.

On the 7th we made a boat excursion to the mainland, and took the

opportunity of sounding the straits. In the middle, at eighty-one

fathoms, it was muddy; towards Sabine Island and Cape Wynn the bottom

was analogous to the character of the land. Indeed the soundings

along the coast, as far as the Germania sailed, were uniform, and the

character of the depths mostly indicated by the land. Shallows in any

way dangerous did not exist along the coast that we sailed by.

On our boat excursion we had a combat with a large walrus and her young

one; the young one was killed easily, but the other escaped severely

wounded. We found it in the afternoon dead upon a floe, and brought it

on board.

We climbed Cape Wynn, which was rather steep but not very high, and

found on the top a plateau of several miles in circumference, quite

free from snow, but scantily covered with vegetation. Farther inland we

came to a valley watered by a glacier stream, and showing moss, grass,

and many green spots. Behind this valley the mountains rose to a height

of more than 1850 feet, but, even here, the summits were perfectly free

from snow, which was only collected in the rifts. The snow-beds and the

falls of snow in East Greenland are much smaller than we expected to

find, and even less than in Spitzbergen, which lies so near.

During our whole stay on this coast we only once, and that in June

1870, saw the land with an entire covering of snow.

The view to the north was bright and clear; in 75½° N. Lat. we could

distinctly see the land edged with firm ice. Over the sea lay a thick

fog, which spread over all by degrees. We went hunting for a reindeer,

but missed it, and had to content ourselves with a white hare. We

returned on board in the evening. In the night ice formed in the bay,

which is also the case in summer during a calm with a clear sky, though

about the beginning of August it disappears in the daytime. The heavy

ice in the straits had these last few days drifted out to sea, and the

land ice was more broken up.

Thanks to the continued fine weather, work was finished by the 10th

of August; the instruments brought on board, and all made ready to

sail, which we did after piling a heap of stones on the eastern point

of land, and, about 100 to 104 feet to the north of it, depositing a

document containing the chief dates of our voyage.

At six on the following morning we weighed anchor, and steered out of

the harbour, with a light southerly breeze, northwards. We passed the

low cliff at eight, and steamed along the firm ice, which at first

stretched to the north and afterwards to the north-east.

The land ice bordered the whole south side of Shannon Island, and also

Cape Philip Broke, which was its most south-easterly point. We doubled

it at noon, and found to the east of the island along the land ice,

which has here an average breadth of from three to four nautical miles

from the coast, a channel of from two to three miles broad, though in

some places so blocked with ice that only by the help of both steam and

sail could we make way through. The border of the land ice was pretty

high; in many places the blocks lay piled up from forty to fifty feet

high.

At three p.m. we broke through a chain of brashes, on the other side of

which was again open water. Here the pack-ice had retreated quite four

nautical miles. As the wind was still south, steam was let off, and we

set all sail to save our coals.

At six p.m. we sighted more ice to the north, which seemed very thick.

The wind shifted to the west and a dense fog came up, hiding everything

from our sight; we therefore halted until the morning.

We were now upon the most northerly point reached by Captain Clavering,

but still Shannon Island stretched further to the north--much further

than is given on the old charts. At first we thought there must be

some mistake in the log’s reckoning, so, as a calm had fallen we

lay-to. Our observations gave 75° 17′ Lat., and 17° 22′ W. Long. from

Greenwich by our chronometer, the stand-point of which was on Sabine

Island. Later on we ascertained that the position of the north-east

cape of the island was 75° 26′ N. Lat., and 18° 0′ W. Long.

The correctness of our reckoning we proved beyond a doubt, and we were

therefore obliged to conclude that it was impossible for Clavering to

have reached the spot indicated by Dr. Petermann on the chart at 75°

14′ N.W. of the frozen bay, and that most likely the whole boat journey

rested upon some misunderstanding; and later, upon going through

Sabine’s and Clavering’s original reports, we found that this supposed

journey had never actually taken place.

We stayed by the ice all that day (12th August), partly to take more

observations, and partly because there was so much ice in the north

which could only be penetrated by a favourable wind or steam.

In the afternoon the current set the ice strong to the south, at a

speed of one and a quarter nautical miles an hour in a perfect calm;

but from four to ten p.m. it stopped completely, when it began to drift

again. It seemed, therefore, as if there was ebb and flood, but that

the current to the south decidedly prevailed.[42] And with all our late

observations we could not prove a decided ebb and flood, although the

tidal wave could regularly be seen along the coast.

In an ice-covered sea it is especially difficult to arrive at any right

conclusion with regard to the currents. Those on the coast of East

Greenland we most carefully noticed. Putting the experience of both

ships together, and that of the floe on which the crew of the Hansa

passed the winter, the following remarks are probably correct.

Along the outer border of the ice, and among the drift-ice even as far

as the fields themselves, which extend a long way within the barrier,

there exists between the latitudes 76° and 72° a south-westerly

current, the average speed of which is from eight to ten nautical miles

in twenty-four hours. The direction taken by this current greatly

depends upon the prevailing winds, and therefore often turns the

foremost portion of the drift considerably to the east or west.

Immediately under the coast, according to our observations, a southerly

motion of both ice and water is not to be denied, but it is far

weaker than that on the outer border; and in summer, when south winds

prevail, it stops altogether, so that at times the ice fields are

stationary, or only move up and down. In winter the drifting is much

more considerable, owing to the prevailing north winds and storms.

Regular ebb and tidal currents the Germania did not meet with in the

latitudes through which she passed, but only a rising and falling

of the water. In the autumn it seems certain that there is always

a setting of the heavy pack-ice to the coast, and what is termed

land-water disappears more and more; indeed, the question as regards

the continuation of this land-water along the coast the whole of the

summer cannot be entertained for a moment; its appearance depends more

upon the formation of the coast, the prevailing winds, and other local

influences, than on the running off of melted water.

The ice in its drift southwards had turned somewhat to the east, thus

leaving more and more open water behind it to the north.

We therefore set sail on the 13th of August, and steered, with a light

south wind, along the border of the firm land ice without meeting with

any great difficulties. A fog bank rose in the south, which soon spread

over Shannon, and the channel which we were following northward was

becoming narrower and narrower; to the east lay boundless fields thick

together, and to the north we soon saw more firm ice, so as the evening

drew on, we lay-to.

On the morning of the 14th the atmosphere was quite clear, and we saw

with dismay that our further advance northward had come to a sudden

halt.

Some nautical miles ahead of us lay a monster ice field, stretching

eastward as far as the eye could see, and apparently joining the land

ice in the west. Far, far to the north-east behind the fields there

seemed to be, judging from a small dark spot in the heavens, more

water; further advance, however, was not possible until the field was

set in motion and separated from the land ice.

The weather was fine and clear; we therefore took some observations,

which gave the latitude 75° 30′ 5″ and 17° 30′ W. Long.; the

declination of the compass, taking the mean of several azimuths, 45°

24′ W.

At night there was mostly a calm, with bright weather. To the north

and north-west there was a very strong refraction, which showed us

that unless a steady wind set the sluggish masses in motion, further

advance to the north would be amongst the impossibilities.

We were all of opinion that in order to avoid the dangerous pressure of

the ice fields, we should withdraw at once to the south side of Shannon

Island, investigate it scientifically, and from the hills watch for a

favourable opportunity of advancing.

As a light breeze from the north-west sprang up on the morning of the

15th, we set sail to carry out our plan; but in order to be sure that

there was no opening to the north, we sailed along the northern border

of the ice as far as the closely-packed end in the east, but without

finding a way through.[43]

At about ten p.m. we were once more to the east of the island, and

the mean height of the firm ice above the water was from two to five

feet, and large blocks of from thirty to forty feet were piled upon the

shore in all directions--proof of the enormous force of the pressure

of the fields in their revolving motion to the south. Our strait was

very narrow in many places, and we sailed round Cape Philip Broke

at half-past eleven a.m. on the 16th of August, and anchored on the

south side in six fathoms of water, between some stranded blocks of

ice. Everything was at once prepared for the land expedition, and the

captain and Lieutenant Payer started first to reconnoitre.

We found the remains of some Esquimaux summer-huts on the shore, with

a great deal of moss and weeds. We climbed a height of about 230 feet,

and were busy fixing a point for observation and building a cairn,

when in the distance we saw a remarkable-looking animal which could be

neither bear nor reindeer. Of musk-oxen we never thought for a moment,

and, when at length we discovered that such was the creature before us,

we were indeed surprised. It was hunted down, however, and killed by

Peter Iversen.

We afterwards found that the whole of the coast up to 77° was

frequented by these ruminating creatures, but that to the south their

numbers decreased. With the reindeer the opposite seemed to prevail;

north of 75½° we did not see a single one.

In the evening calm. Ice formed everywhere, but disappeared again upon

the rising of a southerly breeze.

The following day, on the 17th of August, the land expedition started.

First-Lieutenant Payer received as helpmates--Mr. Sengstacke, Peter

Iversen, and Peter Ellinger; and the two astronomers took Theodor

Klentzer. They were provided with six days’ provisions, and ordered to

return without delay when they saw the flag wave from the Cape.

The German Arctic expedition of 1869-70, and narrative of the wreck of the "Hansa" in the ice · 第 2 / 18 章