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ESR 1979-02

Sand and Gravel Deposits in the Canmore Corridor Area, Alberta

The deposits described are mappable at a scale of 1:50,000, have a thickness of at least 1 m, and have a ratio of overburden to gravel and sand of no more than 1:1. Volume or tonnage figures are general estimates based on a geological ... Show Abstract

Edwards, W.A.D.  1979-01-01

ESR 1957-03

Glacial Geology Galahad-Hardisty District, Alberta

The topography of the district has been modified by debris-filled meltwater channels (stream trenches) which are numerous in the eastern portion of the area. The western portion of the Hardisty district is composed of gently rolling ground moraine ... Show Abstract

Bayrock, L.A.  1958-01-01

ESR 1957-02

Glacial Geology Alliance-Brownfield District Alberta

The eastern part of the Alliance-Brownfield district is made up of hummocky dead-ice moraine and the western part is a relatively flat till plain, the Torlea flats (Warren, 1937). [...]covers most of the surface of the area, and other glacial and ... Show Abstract

Bayrock, L.A.  1958-01-01

ESR 1967-04

Surficial Geology of the Wainwright Area (East Half), Alberta

The Wainwright area lies within the east-central Alberta Plains, a relatively flat, glaciated area underlain by gentle dipping detrital strata of Late Cretaceous age. In most parts of the area, bedrock is overlain by till, as ground or hummocky ... Show Abstract

Bayrock, L.A.  1967-01-01