Geology of the City of Edmonton Part 1: Central Edmonton

Publication Type
Earth Sciences Report
Published Date
Topic
Oil and Gas
Publication ID
ESR 1966-01
Publication ID Extended
Earth Sciences Report 1966-01
Publication
Abstract

The City of Edmonton is built upon surficial deposits of variable thickness underlain by Upper Cretaceous strata. The surficial deposits, of late Pleistocene age, consist of well-sorted preglacial sands and gravels, glacial till, and proglacial lake sediments, in ascending order. The surficial deposits generally thicken towards the northern part of the area due to the relief developed on the bedrock surface. Maximum relief on the upper surfaces of the map-units ranges from 120 feet on the bedrock surface to 32 feet on the till surface.

The area covered by this report is the central business section of Edmonton, bounded by 114th Street on the west, 114th Avenue on the north, 92nd Street on the east, and Jasper Avenue on the south.

Citation

Bayrock, L.A. and Berg, T.E. (1966): Geology of the City of Edmonton part 1: central Edmonton; Research Council of Alberta, RCA/AGS Earth Sciences Report 1966-01, 33 p.

Place Keywords
alberta, edmonton
Place Keywords NTS
83h
Theme Keywords
bedrock, edmonton group, glacial lake edmonton, glacial sediment, saskatchewan sands and gravels, surficial deposit, till