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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 1980-03

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 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 1980-02

Hydrogeology of the Steen River-Whitesand River Area, Alberta

Evaluations of geology, topography, groundwater and surface water chemistry were fundamental in estimating hydrogeologic characteristics.The 20-year safe yields for half the area are over 0.4 l/sec (5 igpm) and only for a small area of very thick ... Show Abstract

Ozoray, G.F.  1980-01-01

ESR 1975-01

Hydrogeology of the Wainwright Area, Alberta

The Wainwright map area lies southeast of Edmonton between longitudes 110 degrees and 112 degrees west and latitudes 52 degrees and 53 degrees north. Precipitation is about 14 inches 136 cm) annually, while potential evapotranspiration is about 21 ... Show Abstract

Hackbarth, D.A.  1975-01-01

ESR 1975-02

Hydrogeology of the Medicine Hat area, Alberta

Hydrogeology of the Medicine Hat area, Alberta The Medicine Hat map area is predominantly flat, with rolling hills in the central, eastern and northern parts of the region; the South Saskatchewan, Red Deer and Bow Rivers cut deeply incised valleys ... Show Abstract

Stevenson, D.R.  Borneuf, D.M.  1977-01-01

ESR 1976-05

Hydrogeology of the Mount Robson-Wapiti area, Alberta

Flow systems are thought to be generally shallow and are bounded by major thrust fault zones which form highly permeable conduits for groundwater movement in both horizontal and vertical planes. Discharge from shallow bedrock aquifers is most ... Show Abstract

Barnes, R.G.  1977-01-01