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CHAP. XIV - RESULTING FORMS:—FIRST, AIGUILLES

Published online by Cambridge University Press:  07 September 2011

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Summary

§ 1. I have endeavoured in the preceding chapters always to keep the glance of the reader on the broad aspect of things, and to separate for him the mountain masses into the most distinctly comprehensible forms. We must now consent to take more pains and observe more closely.

§ 2. I begin with the Aiguilles. In Fig. 24, p. 212, at a, it was assumed that the mass was raised highest merely where the elevating force was greatest, being of one substance with the bank or cliff below. But it hardly ever is of the same substance. Almost always it is of compact crystallines, and the bank of slaty crystallines; or if it be of slaty crystallines the bank is of slaty coherents. The bank is almost always the softer of the two.

Is not this very marvellous? Is it not exactly as if the substance had been prepared soft or hard with a sculpturesque view to what had to be done with it; soft, for the glacier to mould and the torrent to divide; hard, to stand for ever, central in mountain majesty?

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Publisher: Cambridge University Press
Print publication year: 2010
First published in: 1904

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