Adapting Duckbills to Entry Driving at Greenhill Mine

Canadian Institute of Mining, Metallurgy and Petroleum
H. H. Gardner
Organization:
Canadian Institute of Mining, Metallurgy and Petroleum
Pages:
9
File Size:
3669 KB
Publication Date:
Jan 1, 1947

Abstract

Introduction The Greenhill mine of West Canadian Collieries, Limited, is on the Alberta side of the Crowsnest pass, twelve miles from the Alberta British Columbia boundary-line. Here, five coal seams of Lower Cretaceous age are found in the Kootenay formation. They outcrop on the north and south slopes of the valley, with strike approximately N.30°W., paralleling the main range of the Rocky mountains, and dip about 40 deg. westward. Of the five seams, only two, designated No. 1 and No. 2, have been worked to date. On the West Canadian Collieries property, No. 1 seam ranges in thickness from thirty feet to nil. Generally, it has a hard, strong conglomerate roof. No. 2 seam is separated from No. 1 by forty-five feet of shales and sandstones. It has a thickness of eight to thirty feet.
Citation

APA: H. H. Gardner  (1947)  Adapting Duckbills to Entry Driving at Greenhill Mine

MLA: H. H. Gardner Adapting Duckbills to Entry Driving at Greenhill Mine. Canadian Institute of Mining, Metallurgy and Petroleum, 1947.

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