4 edition of Report on the clay resources of southern Saskatchewan found in the catalog.
Report on the clay resources of southern Saskatchewan
|Statement||by N.B. Davis.|
|Series||CIHM/ICMH Microfiche series = CIHM/ICMH collection de microfiches -- no. 82346|
|Contributions||Canada. Mines Branch.|
|The Physical Object|
|Pagination||2 microfiches (77 fr.)|
|Number of Pages||77|
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Report on the clay resources of southern Saskatchewan. Ottawa, Government Printing Bureau, (OCoLC) Material Type: Government publication, National government publication: Document Type: Book: All Authors / Contributors: Norman B Davis; Canada.
Mines Branch. The Whitemud Formation is a geologic formation of Late Cretaceous (Maastrichtian) age in the Western Canada Sedimentary Basin.
it is present through the plains of southern Saskatchewan, southeastern Alberta and south-central Alberta. Named by N.B. Davis inthe formation is characterized by white kaolinitic clay and is a source of high-quality refractory y: Canada.
1 “Development of Saskatchewan Resources for Saskatchewan,” Public Service Monthly, Junepp.2 N.B. Davis, Report on the Clay Resources of Southern Saskatchewan (Ottawa: Government Printing Bureau, ).
3 University of Saskatchewan Archives, Minute book of Board of Governors, University of Saskatchewan, meeting of Ma 4 W.G. Worcester, “Canada’s First. Report on the building and ornamental stones of Canada by W. A Parks (Book); Description of the laboratories of the Mines branch of the Department of mines, Ottawa by Canada (Book); Catalogue of publications of the Mines branch () by Canada (Book).
Lithology. The Ravenscrag Formation is an eastward-thickening wedge of sediments. It is composed primarily of buff, grey and white silty claystone, with mudstone, siltstone, sandstone, and it includes several significant coal seams.
These sediments were deposited in floodplain, overbank and swamp environments. Age. The Ravenscrag Formation is of early Paleocene age and the base of the Country: Canada. Report on the clay resources of southern Saskatchewan [electronic resource] / (Ottawa: Govt.
Print. Bureau, ), by N. Davis and Canada. Mines Branch (page images at HathiTrust; US access only) Burning clay wares. (Indianapolis, Randall, [c]), by Ellis Lovejoy (page images at HathiTrust).
Canada. Mines Branch: Annual report of the mineral production of Canada. (Ottawa [etc.]), also by Canada. Dominion Bureau of Statistics and Geological Survey of Canada (page images at HathiTrust; US access only) Canada. Mines Branch: Annual report on the mineral production of Canada.
Saskatchewan is part of the Prairie region and is the only province with entirely artificial boundaries. It is bordered by the US to the south, the Northwest Territories to the north, and Manitoba and Alberta to the east and west respectively. It was created from the Northwest Territories inat the same time as Alberta, and shares with that province the distinction of having no coast on.
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The Alberta-Saskatchewan saline lake region is largely underlain by Cretaceous bedrock, composed mainly of shales, silts and sandstones (Hammer. Mallards are abundant and have a wide distribution across the continent and are quite a common duck.
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University of Missouri - Columbia, United.On the Saskatchewan River Delta, pussy willow occurs in low- and tall-shrub community types with shallow peat ( feet ( m)) over silty clay. These soils have a pH of to 7 [ 20 ].
In the willow-alder tall shrub vegetation on rarely flooded levees of the Peace-Athabasca Delta, soils average pH, 18% organic matter, and 82% mineral.