The Lower Palæozoic Rocks of Austwick and Horton-in-Ribblesdale, Yorkshire

Abstract
The following paper is an attempt to examine how far a theory which during the last few years has obtained more or less support from many very eminent geologists, can be applied to one of the most remarkable features in several mountain-valleys. Although “cirques” are more commonly associated with the Pyrenees, they are by no means infrequent or on a small scale in the Alps; and as I know the former mountain-chain only at second handy I shall confine myself to the latter, and to those instances which I have personally examined.

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