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A. P. Low Allsmoke anticline average outcrop sample Bearpaw Bearpaw shales Benton shales Bow river Bragg creek branch of Fish branch of Sheep Brown sandstones Canon creek Cardium sandstones chiefly Claggett shales Coal creek coal measures coal seams comb conglomerate considerable covered Coxcomb mountain Cretaceous dark shales distance district eastern Edmonton Elbow river escarpment fault Fernie shales Fish creek Fisher branch Fixed carbon flat fold Font Foothills Forgetmenot ridge G. M. Dawson Geological gray Heer Hoffmann Judith River beds Judith River formation Jumpingpound creek Kootanie coal measures Kootanie formation Kootanie rocks L. W. Bailey lignite limestone Lower Camp Moose Mountain Moose Mountain ridge mouth of Coal muskegs Niobrara-Benton Palaeozoic Pierre places poplar portion quartzites R. G. McConnell rugged sandstone bed sandstone series sandstones and shales seen Sheep river Sibbald creek side south branch summits synclinal timber trail valley wagon road Ware creek wide
Page 68 - Mica, its occurrence, exploitation and uses. Fritz Cirkel. 1905. (Only a few copies available.) Asbestus, its occurrence, exploitation and uses. Fritz Cirkel . 1905. Report of the Commission appointed to investigate the Zinc Resources of British Columbia and the conditions affecting their exploitation. WR Ingalls. 1905. Report on the present and prospective output of the Mines of the Silver-Cobalt ore
Page 38 - ... the mouth of the river and cause the greater part of the falls. These sandstone beds dip to the west at about 20° and the water falls over their hard projecting edges. The lowest bed is a very hard sandstone weathering to a reddish colour, and is fairly well bedded. The sandstone next above is grey in colour on a freshly fractured surface, is very massive, thick, hard, and even quartzitic. There is a conglomerate bed about one foot thick on top of each of these two lower sandstones. The upper...
Page 65 - YUKON AND MACKENZIE. 260. Yukon district, by GM Dawson. 1887. (30c.) 295. Yukon and Mackenzie Basins, by RG McConnell. 1889. (25c.) 687. Klondike gold fields (preliminary), by RG McConnell. 1900.
Page 51 - Immediately on top of the limestones are some very hard, fine-grained, almost white quartzites, from 200 to 300 feet thick, and varying in colour from pure white to a light grey. The shales and sandstones which overlie these are much thicker than to the east around the Moose mountains, although they are otherwise very similar. The conglomerate which overlies the coal measures to the east was not...
Page 65 - BY THE MINES DEPARTMENT OF CANADA (A.— Published by the Geological Survey.) MINERAL RESOURCES BULLETINS 818. Platinum. 859. Salt. 877. Graphite. 851. Coal. 860. Zinc. 880.
Page 65 - McConnell. 1886. (20o.). 263. Cariboo mining district, by A. Bowman. 1887. (25c.). 272. Mineral Wealth, by GM Dawson. 294. West Kootenay district, by GM Dawson. 1888-89. (35c.). 573. Kamloops district, by GM Dawson. 1894. (35c.) 574. Finlay and Omineca Rivers, by RG McConnell.
Page 52 - The conglomerate which overlies the coal measures to the east was not seenhere in place, but considerable of the float was found on the hillsides, so that it very probably outcrops on some of the higher points or ridges ; but as our work was done late in the autumn, with considerable snow on the ground, we did not find it. The formation here consists chiefly of sandstones, characteristically brown in appearance. In fact from the river up to the tops of the high rugged Cretaceous ridge here, the whole...
Page 30 - Coulee, as described on page -We and as figured" in an earlier report, resemble the Eagle sandstone much more closely than any part of the Judith River or any other horizon in the general region. This same sandstone horizon was recognized in Rocky Spring Ridge and on the west flank of West Butte (Sweetgrass Hills) resting on dark shales which at the last-named locality have an estimated thickness of 800 feet.
Page 8 - Kootanie coals are found as anthracitic coals, semi-anthracites, or bituminous coals, according to the amount of local pressure. At one place on the south branch of Sheep river one of these seams, in a tight fold, has been altered to an impure graphite. The Edmonton coals are all lignites or lignitic coals. A few samples collected give evidence by analyses of being the latter. COALS.