The Arctic World : $b Its plants, animals, and natural phenomena. With a historical sketch of Arctic discovery, down to the British polar expedition: 1875-76.Anonymous
Science
The Arctic World : $b Its plants, animals, and natural phenomena. With a historical sketch of Arctic discovery, down to the British polar expedition: 1875-76.
Anonymous
Arctic regions; Arctic regions -- Discovery and exploration -- British
Here then was, in reality, the counterpart of the river-systems of
other lands. From behind the granite hills the congealed drainings of
the interior water-sheds, the atmospheric precipitations of ages, were
moving in a mass, which, though solid, was plastic, moving down through
every gap in the mountains, swallowing up the rocks, filling the
valleys, submerging the hills: an onward, irresistible, crystal tide,
swelling to the ocean. The surface was intersected by numerous vertical
crevasses, some of considerable depth, which had drained off the melted
snow.
It was midnight when the explorers approached this colossal reservoir.
The sun was several degrees beneath the horizon, and afforded a faint
twilight-gleam. Stars of the second magnitude were dimly perceptible in
the cold, steel-blue Arctic heavens. When they were within about half
a mile of the icy wall, a brilliant meteor fell before them, and, by
its reflection upon the glassy surface beneath, greatly increased the
magical effect of the scene; while loud reports, like distant thunder
or the roll of artillery, broke at intervals from the depths of the
frozen sea.
On closer inspection it was found that the face of the glacier ascended
at an angle of from 30° to 35°. At its base lay a high bank of snow,
and the wanderers clambered up it about sixty feet; but beyond this
their efforts were defied by the exceeding smoothness of the ice.
The mountains, which stood on either hand like giant-warders, were
overlapped, and to some extent submerged, by the glacier. From the
face of the huge ice-river innumerable little rivulets ran down the
channels their action had gradually excavated, or gurgled from beneath
the ice; forming, on the level lands below, a sort of marsh, not twenty
yards from the icy wall. Here, in strange contrast, bloomed beds of
verdurous moss; and in these, tufts of dwarf-willows were wreathing
their tiny arms and rootlets about the feebler flower-growths; and
there, clustered together, crouching among the grass, and sheltered
by the leaves, and feeding on the bed of lichens, flourished a tiny,
white-blossomed draba and a white chickweed. Dotting the few feet of
green around might be seen the yellow flowers of the more hardy poppy,
the purple potentilla, and saxifrages yellow, purple, and white.
* * * * *
The great glacier of Sermiatsialik is one of the arms, or outlets, of
this immense reservoir of ice. It occupies the bed of a valley, varying
from three and a half to five miles in width, and attaining at certain
points a depth of upwards of three hundred and seventy feet. This
valley opens upon the fiord of Sermiatsialik, which is separated from
that of Julianshaab by the range of mountains culminating in the peak
of Redkammen.
Public-domain text, read in full here on John Shaqi.
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