The glacial geomorphology of West-Central Newfoundland; Halls Bay to the Topsails
During the late Wisconsin glaciation, ice flow in west-central Newfoundland was to the north-northeast and northeast, sub-parallel to structural lineations. Constructional forms at this stage included drumlins, drumlinoid forms and ribbed moraine. -- The coast of Halls Bay was deglaciated about 12,0...
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| Format: | Thesis |
| Language: | English |
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Memorial University of Newfoundland
1973
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| Online Access: | https://research.library.mun.ca/5532/ https://research.library.mun.ca/5532/1/Tucker_ChristopherM.pdf https://research.library.mun.ca/5532/3/Tucker_ChristopherM.pdf |