Sessional papers of the Dominion of Canada 1905 . ver is approached, appears as a monocline dipping to the west, abutting or going under the rocks upheaved to form the Vermilion range. The coal bearing rocks, which in the shallow basin appear only on the summits of the hills, here again form a narrow strip along the west side, in very much the same manner as along the face of the Cascade mountain. The division line between the two types of structure is marked by aheavy fold running from the fault line, at the height-of-land between 1:2 GEOLOGICAL SURVEY DEPARTMENT 4-5 EDWARD VII., A. 1905 the
Sessional papers of the Dominion of Canada 1905 . ver is approached, appears as a monocline dipping to the west, abutting or going under the rocks upheaved to form the Vermilion range. The coal bearing rocks, which in the shallow basin appear only on the summits of the hills, here again form a narrow strip along the west side, in very much the same manner as along the face of the Cascade mountain. The division line between the two types of structure is marked by aheavy fold running from the fault line, at the height-of-land between 1:2 GEOLOGICAL SURVEY DEPARTMENT 4-5 EDWARD VII., A. 1905 the Red Deer and the Panther rivers, south-eastward to the centre ofthe valley near the Panther river, and is probably continued fartherdown the valley. Remnants of this or similar folds are seen on thehills to the south. The sketch introduced here is outlined from a photograph of thesouth end of a hill just north of the Panther river. This is aboutmidway bet%veen the ranges, but from this point the fold bears to theleft, or in a W. N. W.
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