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...

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Main Author: Netterville, J. A.
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
id ftdatacite:10.11575/prism/15989
record_format openpolar
spelling ftdatacite:10.11575/prism/15989 2023-11-05T03:42:29+01:00 Quaternary stratigraphic of the low Gods River region, Hudson Bay lowlands, Manitoba ... Netterville, J. A. 1974 https://dx.doi.org/10.11575/prism/15989 https://prism.ucalgary.ca/handle/1880/15109 en eng University of Calgary University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission. QE 696 N46 1974 Microfiche Geology, Stratigraphic - Quaternary Geology - Manitoba - Gods River region article master thesis CreativeWork Other 1974 ftdatacite https://doi.org/10.11575/prism/15989 2023-10-09T10:52:02Z 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 ... Master Thesis Hudson Bay Subarctic Tundra DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic QE 696 N46 1974 Microfiche
Geology, Stratigraphic - Quaternary
Geology - Manitoba - Gods River region
spellingShingle QE 696 N46 1974 Microfiche
Geology, Stratigraphic - Quaternary
Geology - Manitoba - Gods River region
Netterville, J. A.
Quaternary stratigraphic of the low Gods River region, Hudson Bay lowlands, Manitoba ...
topic_facet QE 696 N46 1974 Microfiche
Geology, Stratigraphic - Quaternary
Geology - Manitoba - Gods River region
description 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 ...
format Master Thesis
author Netterville, J. A.
author_facet Netterville, J. A.
author_sort Netterville, J. A.
title Quaternary stratigraphic of the low Gods River region, Hudson Bay lowlands, Manitoba ...
title_short Quaternary stratigraphic of the low Gods River region, Hudson Bay lowlands, Manitoba ...
title_full Quaternary stratigraphic of the low Gods River region, Hudson Bay lowlands, Manitoba ...
title_fullStr Quaternary stratigraphic of the low Gods River region, Hudson Bay lowlands, Manitoba ...
title_full_unstemmed Quaternary stratigraphic of the low Gods River region, Hudson Bay lowlands, Manitoba ...
title_sort quaternary stratigraphic of the low gods river region, hudson bay lowlands, manitoba ...
publisher University of Calgary
publishDate 1974
url https://dx.doi.org/10.11575/prism/15989
https://prism.ucalgary.ca/handle/1880/15109
genre Hudson Bay
Subarctic
Tundra
genre_facet Hudson Bay
Subarctic
Tundra
op_rights University of Calgary graduate students retain copyright ownership and moral rights for their thesis. You may use this material in any way that is permitted by the Copyright Act or through licensing that has been assigned to the document. For uses that are not allowable under copyright legislation or licensing, you are required to seek permission.
op_doi https://doi.org/10.11575/prism/15989
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