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Excerpt from Transcontinental Excursion C2: Toronto to Victoria and Return Via Canadian Pacific, Grand Trunk Pacific and National Transcontinental Railways From Dunmore to a point a little east of Lethbridge the country is underlain by the Belly River formation arched in the form of a flat anticline, the centre of which is probably near Bow island. The formation consists of shales and sandstones of brackish water deposition referred to Upper Cretaceous. Succeeding the Belly River are the marine Pierre shales, the latest purely marine sediments of the plains. The beds have a slight dip to the west, which increases south wards, and are faulted with small displacements showing that the effect of the Laramide revolution extended as far east as Lethbridge. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works.

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