Adapting Duckbills to Entry Driving at Greenhill Mine

- 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:
(1947) Adapting Duckbills to Entry Driving at Greenhill MineMLA: Adapting Duckbills to Entry Driving at Greenhill Mine. Canadian Institute of Mining, Metallurgy and Petroleum, 1947.