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ESR 1956-02

Glacial Geology of Castor District, Alberta

Glacial Geology of Castor District, Alberta The Castor district lies within the Torlea flats which is a north-south belt of relatively featureless ground moraine in east-central Alberta. Gently dipping Upper Cretaceous rocks are close to the ... Show Abstract

Gravenor, C.P.  1956-01-01

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 1956-04

Stream-Trench Systems of East-Central Alberta

Recently there has been found in the Alliance-Kinsella district of east-central Alberta a confused system of interconnected debris-filled channels which are intimately tied to the drainage problems of the larger stream courses of Alberta. Similar ... Show Abstract

Gravenor, C.P.  Bayrock, L.A.  1956-01-01

ESR 1965-02

Surficial Geology of the Cypress Hills Area, Alberta

Surficial Geology of the Cypress Hills Area, Alberta The surficial deposits of the Cypress Hills area consist predominantly of till, mainly in the form of ground moraine, hummocky disintegration moraine and end moraine. Glaciofluvial deposits of ... Show Abstract

West, E.W.  1965-01-01

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 1956-05

Air Photographs of the Plains Region of Alberta

Over the past 20 years air photographs have been used extensively by the geologist, soil scientist, forester, geographer, topographer and engineer. While air photographs have been used by the different professions for a wide variety of purposes, ... Show Abstract

Gravenor, C.P.  1956-01-01

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