Summary

Edward Nicholas Kendall Journal of the Royal Geographical Society of London (1833)

In the course of the following afternoon, a partial clearing of the fog showed us more land extending along the S.E. horizon. Like Smith's Island it was only distinguishable from the numerous icebergs by which it was surrounded, by the towering height of its mountains, and by the black fringe of rocks that skirted the water-line.
Source: Wikisource

Edward Nicholas Kendall Journal of the Royal Geographical Society of London (1833)

On reaching the cape the surf was found so violent that we could only effect our purpose by entering one of the numerous inlets that presented themselves, and even then it was a task by no means easy,—the land being composed of a collection of needle-like pinnacles of sienite, covered with snow, and only accessible by watching an opportunity of jumping from the boat during the recession of a wave.
Source: Wikisource

Edward Nicholas Kendall Journal of the Royal Geographical Society of London (1833)

The principal part of the island is composed of alternate layers of ashes and ice, as if the snow of each winter during a series of years, had been prevented from melting in the following summer by the ejection of cinders and ashes from some part where volcanic action is still in progress; and that such is the case appears probable from the fact of there being at least one hundred and fifty holes, from which steam was issuing with a loud hissing noise, and which were visible from the top of one of the hills immediately above the small cove where the Chanticleer was secured.
Source: Wikisource

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