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Alberta clays and shales : summary of ceramic properties

Ceramic test data for more than 200 deposits of clays and shales in Alberta resulted largely from early investigations of the Federal Department of Mines (1912-15, 1932) supplemented by more recent work of Alberta Research ... Show Abstract

Hamilton, W.N.  Babet, P.H.  1975-03-01


Alberta Bentonites

Low yields, high grit content, or thick overburden reduce the desirability of other deposits.The paucity of glass shards and the mineralogy of the sand and silt fractions suggest rhyodacite as the composition of the parent volcanic ash for each ... Show Abstract

Scafe, D.W.  1975-01-01

BUL 036

Multiple Glaciations in the Foothills, Rocky Mountain House area, Alberta

The purpose of the program is to publish hydrogeological maps-graphic portrayals of the groundwater onditions and their controlling factors-for each of 47 different areas in the province. The main items on a typical map sheet are a central main ... Show Abstract

Boydell, A.N.  1978-01-01

BUL 020

Cretaceous Foraminifera of the Rocky Mountain Foothills, Alberta

In ascending stratigraphic order these are: 1.Miliammina manitobensis; 2.Verneuilinoides kansasensis; 3.lower pelagic and 4.Pseudoclavulina sp. from the Blackstone Formation; 5.Trochammina sp. 1; 6.Brachycythere-Bullopora; 7.Anomalinoides henbesti; ... Show Abstract

Wall, J.H.  1967-01-01

BUL 021

Stratigraphy and Petrology of the Lower Cretaceous Blairmore and Mannville Groups, Alberta Foothills and Plains

The upper unit consists of lensing, grey, siliceous sandstone, siltstone, and varicoloured shale, grading up in the southernmost Foothills into a thick succession of bedded pyroclastic detritus (Crowsnest Member ).These beds grade laterally in the ... Show Abstract

Mellon, G.B.  1967-01-01

BUL 033

Hydrogeology of the Tri-Creek Basin, Alberta

Groundwater flow in the Tri-creek basin, a 23-square mile (60 square km) area of the Rocky Mountain Foothills in western Alberta, is controlled by the surficial and bedrock geology. Response to changes in recipitation is generally rapid, although ... Show Abstract

Currie, D.V.  1976-01-01

ESR 2001-19

Regional Evaluation of the Coal-Bed Methane Potential of the Foothills/Mountains of Alberta

Regional Evaluation of the Coal-Bed Methane Potential of the Foothills/Mountains of Alberta For coal-bed methane (CBM) evaluation purposes, they can be divided into shallow (200 to 2500 m depth) and deep (over 2500 m depth) coal zones. [...]the ... Show Abstract

Beaton, A.P.  Berhane, H.  Langenberg, C.W.  2002-01-30

DIG 2012-0017

Modelled Sandiness of the Paskapoo Formation, Alberta (Tabular data, tab-delimited format)

Sand-abundance values were determined from log analysis of water-well lithologs and petroleum exploration downhole-geophysical logs, specifically gamma-ray logs. Values of modelled sandiness range from 0 (absence of sand) to 1 (100% sand) and are ... Show Abstract

Andriashek, L.D.  Lyster, S.  2012-09-12

OFR 1971-03

The Environmental Impact of Surface Mining in Alberta

The Environmental Impact of Surface Mining in Alberta Coal Deposits of late Jurassic to early Tertiary ages underlie much of the Alberta Plains and Foothills at depths ranging from 0 (i.e. at the surface) to 10,000 feet. Place Keywords 72e 72l 72m ... Show Abstract

Mellon, G.B.  1972-12-17

OFR 1970-03

Alberta Foothills Coal, Extracts from Published Reports of Research Council of Alberta, with Annotations

Recent months have seen an explosive growth of interest in Alberta Foothills coals, chiefly those coals suitable for the manufacture of metallurgical coke. A considerable amount of geological data on coal-bearing strata in the area has emanated ... Show Abstract

Campbell, J.D.  1970-05-01