Quaternary stratigraphic of the low Gods River region, Hudson Bay lowlands, Manitoba ...
Bibliography: p. 54-63. ... : Four or more tills, commonly separated by nonglacial deposits, are exposed along the Gods River in northwestern Hudson Bay Lowland. The oldest till (Till A) overlies Paleozoic bedrock and is overlain by fossiliferous beds of fluvial, lacustrine, and organic origin (Gods...
| Main Author: | |
|---|---|
| Format: | Master Thesis |
| Language: | English |
| Published: |
University of Calgary
1974
|
| Subjects: | |
| Online Access: | https://dx.doi.org/10.11575/prism/15989 https://prism.ucalgary.ca/handle/1880/15109 |
| Summary: | Bibliography: p. 54-63. ... : Four or more tills, commonly separated by nonglacial deposits, are exposed along the Gods River in northwestern Hudson Bay Lowland. The oldest till (Till A) overlies Paleozoic bedrock and is overlain by fossiliferous beds of fluvial, lacustrine, and organic origin (Gods River sediments). Pollen, spores, seeds, wood, insects, and molluscs from within the Gods River sediments record a subarctic climate and a vegetational succession that began and ended with tundra. During the warmest part of the interval, a forest-tundra vegetation grew in the region. The Gods River sediments are correlative with the Missinaibi Formation in northern Ontario and a Sangamon age is inferred. Till B, which overlies the Gods River sediments, is usually separated from the younger Till C by stratified sand and gravel devoid of organic material (Twin Creeks sediments) . This glacial-nonglacialglacial sequence probably encompasses the greater part of Wisconsin. time. The uppermost till (Till D) was laid down during a glacial advance ... |
|---|