The Geomorphic Implications of the Geo-Hydrology of Gypsum Karst Areas

Gypsum karst areas in British Columbia and Wood Buffalo National Park, Alta.-N.W.T. are described. Investigation of the geo-hydrology of these areas, particularly specifically the saturation states of rising waters, is demonstrated to be a valuable tool in defining the major geomorphic processes act...

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Bibliographic Details
Main Author: Drake, Julian John
Other Authors: Ford, D.C., Geography
Format: Thesis
Language:English
Published: 1970
Subjects:
Gypsum Karst
geo-hydrology
rising waters
geomorphic
rock solution
Alta
Wood Buffalo
Wood Buffalo National Park
Online Access:http://hdl.handle.net/11375/17673
Description
Summary:Gypsum karst areas in British Columbia and Wood Buffalo National Park, Alta.-N.W.T. are described. Investigation of the geo-hydrology of these areas, particularly specifically the saturation states of rising waters, is demonstrated to be a valuable tool in defining the major geomorphic processes acting. The combination of thermo-dynamic equilibrium studies of the gypsum and limestone processes serves to define zones within which the dominant controls of rock solution can be inferred. The commonly accepted parameters of limestone solution equilibria (Picknett's curves) are examined and shown to be incorrect. Use of the parameters and indices presented in this thesis gives much better accordance with observed characteristics of karst waters. Thesis Master of Science (MSc)

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