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INF 124

Alberta Geological Survey Contributions to the CSPG Annual Convention June 18 - 22, 2001

Alberta Geological Survey Contributions to the CSPG Annual Convention June 18 - 22, 2001 Five presentations from Alberta Geological Survey that were presented at the 2001 CSPG Annual Convention. Place Keywords 72e 72l 72m 73d 73e 73l 73m 74d 74e ... Show Abstract

Beaton, A.P.  Chen, D.  Richardson, R.J.H.  Andriashek, L.D.  Pawlowicz, J.G.  Fenton, M.M.  Ranger, I.  Langenberg, C.W.  Hein, F.J.  Pana, C.  Lemay, T.G.  Stewart, S.A.  Campbell, J.D.  2001-06-22

INF 140

Edmonton-Calgary Corridor Groundwater Atlas

Edmonton-Calgary Corridor Groundwater Atlas Place Keywords 82o 82p 83a 83b 83g 83h 83i 83j alberta calgary canada edmonton edmonton calgary corridor red deer Theme Keywords bedrock chemistry geology geophysics groundwater hydrochemistry hydrology ... Show Abstract

Alberta EnvironmentBarker, A.A.  Riddell, J.T.F.  Slattery, S.R.  Andriashek, L.D.  Moktan, H.  Wallace, S.  Lyster, S.  Jean, G.  Huff, G.F.  Stewart, S.A.  Lemay, T.G.  2011-11-10

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 1975-05

Hydrogeology of the Vermillion area, Alberta

The Vermilion map area lies in the plains-parkland transition zone of east-central Alberta and covers approximately 5660 square miles (14,660 square km). Average annual precipitation is 16 inches (41 cm) and potential evaporation exceeds ... Show Abstract

Currie, D.V.  Zacharko, N.  1975-01-01

ESR 1974-10

Hydrogeology of the Edmonton Area (Northwest Segment), Alberta

In the bedrock, yields are typically less than 5 igpm.Groundwater flow systems in the upper 300 feet are largely controlled by the connection between the river and buried valley sand and gravel deposits, and by the incised nature of the valleys In ... Show Abstract

Bibby, R.  1974-01-01

ESR 1974-04

Hydrogeology of the Foremost Area, Alberta

In the western half of the map area, sandstone of the lower member of the Milk River Formation (hereafter referred to as the lower Milk River sandstone) is the main aquifer; in the eastern half permeable lenses in the drift are the main sources of ... Show Abstract

Borneuf, D.M.  1976-01-01

ESR 1974-01

Hydrogeology of the Lethbridge-Fernie Area, Alberta

Clastic rocks, largely non-marine, of Upper Cretaceous age and some of Tertiary age underlie the plains in the Lethbridge-Fernie map area. Closely spaced, high-angle thrust faulting has deformed the Upper and Lower Cretaceous clastics of the ... Show Abstract

Tokarsky, O.  1974-01-01

ESR 1972-11

Hydrogeology of the Tawatinaw Area, Alberta

The drift is the water-bearing zone in most of the Tawatinaw area except for the southwest and the south-central part of the map area, where wells obtain water from the Wapiti Formation. The yields range from less than 1 igpm (imperial gallon per ... Show Abstract

Borneuf, D.M.  1973-01-01

ESR 1972-08

Hydrogeology of the Wabamun Lake Area, Alberta

The maps and profiles were constructed from existing data and from data collected by a field survey and drilling operations. The best aquifers are Paskapoo sandstones and Quaternary sands and gravels .Water quality is good. The total dissolved ... Show Abstract

Ozoray, G.F.  1972-01-01