Page:Scott's Last Expedition, Volume 1.djvu/157

From Wikisource
Jump to navigation Jump to search
This page has been proofread, but needs to be validated.
1911]
CLIFFS OF CAPE CROZIER
83

young one shedding its down. (The down had come off the head and flippers and commenced to come off the breast in a vertical line similar to the ordinary moult.) This is an age and stage of development of the Emperor chick of which we have no knowledge, and it would have been a triumph to have secured the chick, but, alas! there was no way to get at it. Another most curious sight was the feet and tails of two chicks and the flipper of an adult bird projecting from the ice on the under side of the jammed floe; they had evidently been frozen in above and were being washed out under the floe.

Finding it impossible to land owing to the swell, we pulled along the cliffs for a short way. These Crozier cliffs are remarkably interesting. The rock, mainly volcanic tuff, includes thick strata of columnar basalt, and one could see beautiful designs of jammed and twisted columns as well as caves with whole and half pillars very much like a miniature Giant's Causeway. Bands of bright yellow occurred in the rich brown of the cliffs, caused, the geologists think, by the action of salts on the brown rock. In places the cliffs overhung. In places, the sea had eaten long low caves deep under them, and continued to break into them over a shelving beach. Icicles hung pendent everywhere, and from one fringe a continuous trickle of thaw water had swollen to a miniature waterfall. It was like a big hose playing over the cliff edge. We noticed a very clear echo as we passed close to a perpendicular rock face. Later we returned to the ship, which had been trying to turn in the bay—she is not very satisfactory in this respect owing to the difficulty of starting the engines either ahead