Glacial dispersal train of Paleozoic erratics, central Baffin Island, N.W.T., Canada

A glacial dispersal train of erratics derived from Paleozoic bedrock has been delineated stretching east-northeast–west-southwest across central Baffin Island. The lithologies of these erratics suggest a derivation from strata of member B of the Ordovician Ship Point Formation to the west, which are...

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Bibliographic Details
Published in:Canadian Journal of Earth Sciences
Main Author: Tippett, Clinton R.
Format: Article in Journal/Newspaper
Language:English
Published: Canadian Science Publishing 1985
Subjects:
Online Access:http://dx.doi.org/10.1139/e85-193
http://www.nrcresearchpress.com/doi/pdf/10.1139/e85-193