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ECO 2

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

ECO 7

The ceramic potential of Alberta clays and shales

Many geographical areas and geological formations were missed when the ceramic suitability of materials was studied early this century. Geological formations that are useful for the production of structural clay products or pottery are Pleistocene ... Show Abstract

Scafe, D.W.  1982-01-01

BUL 047

Aggregate resources of the Edmonton/Lloydminster region

The commercial sector produces 75 per cent of the aggregate, most of it directed into road construction (52 per cent), concrete production (18 per cent) or asphalt production (11 per cent). A compilation of geological data indicates that 1100 ... Show Abstract

Edwards, W.A.D.  Hudson, R.N.  Scafe, D.W.  1985-01-01

ESN 1980-A

Potential industrial clays of Alberta : a preliminary assessment, Part II

From the same area, samples of Kaskapau Formation dry well, firing range is moderate to long, and the milk chocolate brown colour could be acceptable in "earth colour" pottery or structural clay products. A sample from the Bearpaw Formation in the ... Show Abstract

Scafe, D.W.  1980-01-01

ESN 1977-A

Stoneware and low duty refractory clays associated with the Athabasca Oil Sands

Abstract: Open-pit mining of the Athabasca Oil Sands in the Fort McMurray area removes most of the overburden from basal McMurray Formation clays which have potential for use as stoneware and low heat duty refractories. These clays, interbedded with sands, form the lowest unit in the stratigraphic interval between the base of the mined zone and the underlying Devonian limestone. The clays have good plasticity and working properties, dry reasonably well, have a total drying and firing shrinkage averaging 10 percent, and have absorptions averaging 2.4 percent at the maximum recommended firing temperature. Pyrometric cone equivalent (P.C.E.) varies from 10 to 23 with 16 as the average from 70 samples. Chemical and mineralogical data suggest that a high content of potassium associated with abundant illite may be a significant factor in control of sample refractoriness. Fired colours are shades of yellow, brown, and grey. Thorough evaluation of these basal clays, to outline the most refractory portions of a deposit, would be necessary prior to extraction for stoneware and low duty refractory uses.Clays from within the mined zone have characteristics similar to those of the basal clays and similar uses can be suggested for them. However, the clay material rejected as "oversize" from the feed material for the oil extraction plant because it remains in large cohesive chunks after mining generally contains enough oil sand, in variable amounts, to preclude the use of the clay for ceramic purposes. The intraformational clays that are subjected to the primary extraction process must be concentrated from the waste stream and they remain contaminated with a small amount of oil. Firing shrinkage is high and bars curl at high temperatures, but the P.C.E. of 23 and the easily accessible unlimited supply of this material suggests that further research to evaluate these clays might be worthwhile. Place Keywords 74d 74e alberta athabasca oil sands area canada clearwater fort mcmurray Theme Keywords clay geology oil sands refractory sand stoneware

Scafe, D.W.  1977-01-01

ESN 1978-A

Potential industrial clays of Alberta : a preliminary assessment, Part I

Potential industrial clays of Alberta : a preliminary assessment, Part I Clays from the Luscar Formation show the most potential as they work well, extrude well, and dry well in addition to firing to an appealing dark chocolate colour at the end of ... Show Abstract

Scafe, D.W.  1978-01-01

MAP 391

Aggregate Resources Horse River (NTS 74D/4)

Aggregate Resources Horse River (NTS 74D/4) The character of the material (ratio of sand to gravel and amount of fines) in the deposit is described and its attributes may be shown, such as the geological process that formed each deposit and deposit ... Show Abstract

Scafe, D.W.  Edwards, W.A.D.  Boisvert, D.R.  2009-07-29

MAP 389

Aggregate Resources Winefred Lake (NTS 73M)

The character of the material (ratio of sand to gravel and amount of fines) in the deposit is described and its attributes may be shown, such as the geological process that formed each deposit and deposit thickness. [...]this map displays the ... Show Abstract

Scafe, D.W.  Edwards, W.A.D.  Boisvert, D.R.  2009-07-29

MAP 392

Aggregate Resources of Hangingstone River (NTS 74D/5)

The character of the material (ratio of sand to gravel and amount of fines) in the deposit is described and its attributes may be shown, such as the geological process that formed each deposit and deposit thickness. [...]this map displays the ... Show Abstract

Scafe, D.W.  Edwards, W.A.D.  Boisvert, D.R.  2009-08-31

MAP 393

Aggregate Resources Fort McMurray (NTS 74D/11)

Aggregate Resources Fort McMurray (NTS 74D/11) The character of the material (ratio of sand to gravel and amount of fines) in the deposit is described and its attributes may be shown, such as the geological process that formed each deposit and ... Show Abstract

Scafe, D.W.  Edwards, W.A.D.  Boisvert, D.R.  2009-07-29