The geological and hydrological environment of the Whitewater Lake basin, Manitoba / Alan P. Kohut
Material type:
TextPublication details: Winnipeg, MB : University of Manitoba, 1972.Description: xvi, 295 leaves : ill. ; 29 cmOnline resources: Abstract: The Whitewater Lake Basin is located in southwestern Manitoba within the Interior Plains region of western Canada. The main hydrologic feature of the basin is Whitewater Lake, a shallow closed basin lake less than 5 feet deep occupying 25 square miles in the centre of the basin. The lake lies within the Boissevain Till Plain and is underlain by Cretaceous Shales of the Riding Mountain Formation. A Late Cretaceous-Tertiary outlier of Boissevain Formation sandstone overlain by sanstones and shales of the Turtle Mountain Formation occurs on Turtle Mountain immediately south of the lake. The origin of the basin is due to a collapse feature caused by the solution of salt from Devonian evaporite deposits and/or to a Pre-Jurassic erosion feature on the Mississippian escarpment underlying the basin. During Tertiary- Early pleistocene time a major preglacial river existed under the present location of Whitewater Lake. Three till sheets were deposited in the basin during the Pleistocene separat
| Item type | Current library | Collection | Call number | Status | Date due | Barcode |
|---|---|---|---|---|---|---|
Electronic Report
|
Electronic Library | Non-fiction | KOH (Browse shelf(Opens below)) | Available | 1513 |
Browsing Electronic Library shelves Close shelf browser (Hides shelf browser)
Thesis(M.Sc.)--University of Manitoba, 1972.
Includes bibliographical references (leaves 129-135).
The Whitewater Lake Basin is located in southwestern Manitoba within the Interior Plains region of western Canada. The main hydrologic feature of the basin is Whitewater Lake, a shallow closed basin lake less than 5 feet deep occupying 25 square miles in the centre of the basin. The lake lies within the Boissevain Till Plain and is underlain by Cretaceous Shales of the Riding Mountain Formation. A Late Cretaceous-Tertiary outlier of Boissevain Formation sandstone overlain by sanstones and shales of the Turtle Mountain Formation occurs on Turtle Mountain immediately south of the lake. The origin of the basin is due to a collapse feature caused by the solution of salt from Devonian evaporite deposits and/or to a Pre-Jurassic erosion feature on the Mississippian escarpment underlying the basin. During Tertiary- Early pleistocene time a major preglacial river existed under the present location of Whitewater Lake. Three till sheets were deposited in the basin during the Pleistocene separat