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- W4313157346 abstract "I t is considered that a preglacial plains landscape in S. E. Alberta has been modified by glacial deposition and drainage arrangement. Most of the minor landforms, however, are the result of distinctive processes which occurred during deglaciation of the area. Of these processes, those associated with stagnating ice and glacial melt-water were especially important, for the variety of features they produced. Sufficient variation occurs within the landforms to have influenced both the general development of soils and vegetation, as well as the present pattern of land utilization in the area." @default.
- W4313157346 created "2023-01-06" @default.
- W4313157346 creator A5072298140 @default.
- W4313157346 date "1962-01-01" @default.
- W4313157346 modified "2023-09-30" @default.
- W4313157346 title "The geomorphology of the Medicine Hat area" @default.
- W4313157346 doi "https://doi.org/10.4095/331084" @default.
- W4313157346 hasPublicationYear "1962" @default.
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