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The Proceedings and Transactions of the Nova Scotian Institute of Science, 1923, Vol. 15
Excerpt from The Proceedings and Transactions of the Nova Scotian Institute of Science, 1923
Bed-rock (triassic) sandstone outcrops in this brook, but throughout the valley the stream has never deepened its bed to any great extent. The drift lies, scattered everywhere and a number of boulders are well ice  scratched.
Bed-rock (triassic) sandstone outcrops in this brook, but throughout the valley the stream has never deepened its bed to any great extent. The drift lies, scattered everywhere and a number of boulders are well ice  scratched.
524 pages, Paperback
First published September 27, 2015
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