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MAP 287

Sand and Gravel Deposits with Aggregate Potential, Lethbridge, Alberta (NTS 82H)

The map is a compilation of all existing Alberta Geological Survey sand and gravel geology and resource data for the NTS area. Data sources include Alberta Geological Survey maps and reports produced between 1976 and 2002. The deposit colour ... Show Abstract

Edwards, W.A.D.  Budney, H.D.  Berezniuk, T.  Cadrin, M.  Stoyko, G.  2005-10-17

MAP 435

Aggregate Resources Lethbridge (NTS 82H/10)

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

Shetsen, I.  2009-07-29

MAP 206

Surficial geology of Lethbridge, Alberta, NTS 82H and NTS 82I

Surficial geology of Lethbridge, Alberta, NTS 82H and NTS 82I Deposits are classified by age, genesis and lithologic type. Place Keywords 82h 82i alberta canada lethbridge Theme Keywords geology surficial geology Deposits are classified by age, ... Show Abstract

Shetsen, I.  2005-10-17

ESR 1981-04

Sand and Gravel Resources of the Lethbridge Area

The most important sources of gravel and sand in the Lethbridge area are high and low level alluvial terraces associated with the Oldman River valley. The low terraces commonly have up to 3 m of fine sand and silt overlying the sand and ... Show Abstract

Shetsen, I.  1980-01-01

MAP 105

Hydrogeological map of the Lethbridge - Fernie area, Alberta, NTS 82G and NTS 82H

Hydrogeological map of the Lethbridge - Fernie area, Alberta, NTS 82G and NTS 82H The Hydrogeological Map Series of Alberta provides 1:250000-scale hydrogeological maps over much of Alberta.� Through the use of colour, the maps and ... Show Abstract

Tokarsky, O.  2005-10-17

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