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ESR 1982-04

Hydrogeology of the Clear Hills-Chinchaga River area, Alberta

The 20-year safe yield for about four-fifths of the area is 0.1 to 0.4 l/sec (1 to 5 igpm). Only in small isolated alluvial areas along the Peace River is the potential yield greater than 8 l/sec (100 igpm). A 20-year safe yield of even 0.1 l/sec ... Show Abstract

Ozoray, G.F.  1982-01-01

ESR 1980-01

Hydrogeology of the Pelican-Algar Lake Area, Alberta

Maps and profiles were constructed from existing data and from data collected in a field survey. The 20-year safe yields are mostly over 0.4 l/sec (5 igpm). Most bedrock aquifers, however, yield saline water unsuitable for human ... Show Abstract

Ozoray, G.F.  Lytviak, A.T.  1980-01-01

ESR 1980-03

Hydrogeology of the Zama-Bistcho Lakes Area, Alberta

The Zama-Bistcho Lakes map area, in northwestern Alberta, shares common boundaries with the province of British Columbia to the west and with the Northwest Territories to the north. The main discharge area is in the Zama-Hay Lakes lowland. The map ... Show Abstract

Borneuf, D.M.  Pretula, B.  1980-01-01

ESR 1979-07

Hydrogeology of the Edson area, Alberta

The hydrogeology of the Edson map area can be discussed with respect to three physiographic regions: the Interior Plains, the Rocky Mountain Foothills, and the front ranges of the Rocky Mountains.In the interior Plains, fractured sandstones of the ... Show Abstract

Vogwill, R.I.J.  1983-01-01

ESR 1982-02

Groundwater hydrology of the Pine Lake Research Basin, Alberta

Various types of geologic, geophysical, and hydrologic data were used to evaluate the hydrogeology of the research basin.Permeable sandstone, mudstone, and coals of the thick Paskapoo Formation underlie the study area. Natural basin yield was ... Show Abstract

Garven, G.  1982-01-01

ESR 1981-02

Hydrogeology of the Peace River Area, Alberta

Hydrogeology of the Peace River Area, Alberta The Peace River area, located in northwestern Alberta, has little relief with the exception of the Whitemud Hills in the northwestern quarter of the map area. The Peace River valley cuts deeply into ... Show Abstract

Borneuf, D.M.  1981-01-01

ESR 1979-03

Hydrogeology of the Winagami area, Alberta

The Winagami map area is underlain by the sediments of the Shaftesbury, Dunvegan, Kaskapau, Bad Heart, Puskwaskau and Wapiti Formations of Lower and Upper Cretaceous age. The groundwater yields of the area vary from less 0.07 L/s (100 igpm). The ... Show Abstract

Borneuf, D.M.  1980-01-01

ESR 1979-06

Hydrogeology of the Edmonton area (southeast segment), Alberta

Within these deposits, aquifers consisting of sand and gravel, sandstone, and fractured coal are capable of yielding groundwater at rates of up to 8 l/sec (100 igpm). Groundwater flow is generally from a western upland area to the east, but ... Show Abstract

Stein, R.  1982-01-01

ESR 1979-05

Hydrogeology of the Peerless Lake area, Alberta

The area is sparsely populated and access is poor.The area is covered by thick surficial deposits, primarily of glacial origin, overlying Cretaceous shales. The greatest yields are available from preglacial sands and gravels located in portions of ... Show Abstract

Ceroici, W.J.  1979-01-01

ESR 1979-04

Hydrogeology of the Kananaskis Lake Area, Alberta

The Kananaskis map area, in southwestern Alberta, falls within the Rocky Mountains, the Foothills, the Porcupine Hills and the Plains physiographic regions. Sodium bicarbonate and calcium-magnesium bicarbonate are the main chemical types and ... Show Abstract

Borneuf, D.M.  1980-01-01