Greater Des Moines River During Waning Glaciation

With the lower Minnesota valley blocked with ice, drainage from the waning Keewatin glacier, in southern Minnesota, would naturally be released into the Des Moines River, as indicated by the deep, gorge-like valley of the present stream above Des Moines City. Some recent observations on this phase o...

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Main Author: Keyes, Charles
Format: Text
Language:English
Published: UNI ScholarWorks 1936
Subjects:
Online Access:https://scholarworks.uni.edu/pias/vol43/iss1/62
https://scholarworks.uni.edu/context/pias/article/4527/viewcontent/061_Greater_Des_Moines_River_During_Waning_Glaciation.pdf
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spelling ftunortherniowa:oai:scholarworks.uni.edu:pias-4527 2023-08-20T04:07:43+02:00 Greater Des Moines River During Waning Glaciation Keyes, Charles 1936-01-01T08:00:00Z application/pdf https://scholarworks.uni.edu/pias/vol43/iss1/62 https://scholarworks.uni.edu/context/pias/article/4527/viewcontent/061_Greater_Des_Moines_River_During_Waning_Glaciation.pdf en eng UNI ScholarWorks https://scholarworks.uni.edu/pias/vol43/iss1/62 https://scholarworks.uni.edu/context/pias/article/4527/viewcontent/061_Greater_Des_Moines_River_During_Waning_Glaciation.pdf ©1936 Iowa Academy of Science, Inc. Proceedings of the Iowa Academy of Science text 1936 ftunortherniowa 2023-07-29T22:44:54Z With the lower Minnesota valley blocked with ice, drainage from the waning Keewatin glacier, in southern Minnesota, would naturally be released into the Des Moines River, as indicated by the deep, gorge-like valley of the present stream above Des Moines City. Some recent observations on this phase of Iowa drainage are explained and charts presented. A now filled ancient channel is to be sought along the line of former long prairie lakes and the Blue Earth River, which in pioneer days formed part of the canoe-route of the trappers, from the head-waters of the Saskatchewan, in the Canadian Rockies, to the market in St. Louis. Text Keewatin University of Northern Iowa: UNI ScholarWorks St. Louis ENVELOPE(-67.496,-67.496,-67.132,-67.132)
institution Open Polar
collection University of Northern Iowa: UNI ScholarWorks
op_collection_id ftunortherniowa
language English
description With the lower Minnesota valley blocked with ice, drainage from the waning Keewatin glacier, in southern Minnesota, would naturally be released into the Des Moines River, as indicated by the deep, gorge-like valley of the present stream above Des Moines City. Some recent observations on this phase of Iowa drainage are explained and charts presented. A now filled ancient channel is to be sought along the line of former long prairie lakes and the Blue Earth River, which in pioneer days formed part of the canoe-route of the trappers, from the head-waters of the Saskatchewan, in the Canadian Rockies, to the market in St. Louis.
format Text
author Keyes, Charles
spellingShingle Keyes, Charles
Greater Des Moines River During Waning Glaciation
author_facet Keyes, Charles
author_sort Keyes, Charles
title Greater Des Moines River During Waning Glaciation
title_short Greater Des Moines River During Waning Glaciation
title_full Greater Des Moines River During Waning Glaciation
title_fullStr Greater Des Moines River During Waning Glaciation
title_full_unstemmed Greater Des Moines River During Waning Glaciation
title_sort greater des moines river during waning glaciation
publisher UNI ScholarWorks
publishDate 1936
url https://scholarworks.uni.edu/pias/vol43/iss1/62
https://scholarworks.uni.edu/context/pias/article/4527/viewcontent/061_Greater_Des_Moines_River_During_Waning_Glaciation.pdf
long_lat ENVELOPE(-67.496,-67.496,-67.132,-67.132)
geographic St. Louis
geographic_facet St. Louis
genre Keewatin
genre_facet Keewatin
op_source Proceedings of the Iowa Academy of Science
op_relation https://scholarworks.uni.edu/pias/vol43/iss1/62
https://scholarworks.uni.edu/context/pias/article/4527/viewcontent/061_Greater_Des_Moines_River_During_Waning_Glaciation.pdf
op_rights ©1936 Iowa Academy of Science, Inc.
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