The Romance of Polar Exploration: Interesting Descriptions of Arctic and Antarctic Adventure from the Earliest Time to the Voyage of the "Discovery"Scott, G. Firth
History
The Romance of Polar Exploration: Interesting Descriptions of Arctic and Antarctic Adventure from the Earliest Time to the Voyage of the "Discovery"
Scott, G. Firth
Antarctica; Arctic regions
The range was named Admiralty Mountains, and the various peaks after the
different Lords of the Admiralty. With patriotic pride the leader
recorded that "the discovery of this land restored to Great Britain the
honour of having discovered the southernmost known land, which had been
so nobly won by the intrepid Bellinghausen, and for more than twenty
years retained by Russia."
The amount of ice along, and off, the shore prevented a landing being
made, but it was found to be possible to get ashore on an island not far
away from the mainland. The island was named Possession Island, in
commemoration of the fact that on its shores the ceremony of taking
possession of the newly discovered lands in the name of Great Britain
was duly celebrated. Situated in lat. 71° 56' S. and long. 171° 7' E.,
the island was found to be of igneous formation and accessible only on
its western shore. There were no signs of vegetation on the bare
volcanic rocks, "but myriads of penguins completely and densely covered
the whole surface of the island, along the ledges of the precipices, and
even to the summits of the hills, attacking us vigorously as we waded
through their ranks, and pecking at us with their sharp beaks, disputing
possession; which, with their loud, coarse notes and the insuperable
stench from the deep bed of guano, which had been forming for ages, and
which may, at some time, be valuable to the agriculturists of our
Australian colonies, made us glad to get away again, after having loaded
our boats with geological specimens and penguins."
As the voyage continued, the height of the mountains lying further to
the south of Admiralty Mountains was observed to be from 12,000 to
14,000 feet, the majority being obviously of volcanic origin. While
noting these characteristics, a phenomenon was witnessed which, for the
moment, suggested that they were in the presence of a mighty volcanic
upheaval. An angle was being measured, when, in the line of sight, an
island, about one hundred feet high, suddenly seemed to rise from the
ocean. All eyes were turned upon it, the dark colour of the new arrival
standing out in such pronounced contrast with the whiteness of the ice
around it. Then one, more observant than the rest, drew attention to the
fact that a large berg previously observed at the place where the island
had risen, had completely disappeared. At once the riddle was solved.
The berg had turned over, and, as the lower portion was composed of
earth-stained ice, it stood out in such strong relief against the other
ice that the mistake was easily accounted for.
Public-domain text, read in full here on John Shaqi.
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