Delta Marsh conceptual review / Phil Ould.
Material type:
TextPublication details: Winnipeg, MB : 1980. Ducks Unlimited Canada,Description: xiii, 280 p. : ill. (some col.) ; 28 cmOnline resources: Abstract: Delta marsh was formed behind an elevated beach ridge at the south end of Lake Manitoba. Water levels in the marsh are maintained by 2 processes: a. runoff from adjacent uplands, b. flow of water between Delta Marsh and Lake Manitoba. When water levels are low in Lake Manitoba, water flows from Delta marsh into the Lake. When water levels are high in Lake Manitoba (or wind tides build up water at the south end), the flow is reversed.
| Item type | Current library | Collection | Call number | Status | Date due | Barcode |
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Electronic Report
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Electronic Library | Non-fiction | OUL (Browse shelf(Opens below)) | Available | 3642 |
Includes bibliographical references (p. 229-231).
Delta marsh was formed behind an elevated beach ridge at the south end of Lake Manitoba. Water levels in the marsh are maintained by 2 processes: a. runoff from adjacent uplands, b. flow of water between Delta Marsh and Lake Manitoba. When water levels are low in Lake Manitoba, water flows from Delta marsh into the Lake. When water levels are high in Lake Manitoba (or wind tides build up water at the south end), the flow is reversed.