An Entity of Type: Glacial lake, from Named Graph: http://dbpedia.org, within Data Space: dbpedia.org

Before the Pleistocene Ice Age, circa two million years before present (YBP), the rivers in North, South Dakota and eastern Montana drained northeast into Canada and then into Hudson Bay. The Keewatin Lobe of the continental ice sheet, block the flow of water northward and impounded it along the ice front. Lakes formed, until the waters could find a new way to drain. Initially, the north flowing rivers followed the front of the glacier eastward and into a valley that passed between Garrison and Riverdale, to the Turtle Lake area, and on into Sheridan County. This is known as the preglacial McClean River. This valley became blocked by the glacier and the glacial lake identified as Lake McKenzie formed. Eventually, water level rose to crest the south ridge a point near Riverdale — at the sit

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dbo:abstract
  • Before the Pleistocene Ice Age, circa two million years before present (YBP), the rivers in North, South Dakota and eastern Montana drained northeast into Canada and then into Hudson Bay. The Keewatin Lobe of the continental ice sheet, block the flow of water northward and impounded it along the ice front. Lakes formed, until the waters could find a new way to drain. Initially, the north flowing rivers followed the front of the glacier eastward and into a valley that passed between Garrison and Riverdale, to the Turtle Lake area, and on into Sheridan County. This is known as the preglacial McClean River. This valley became blocked by the glacier and the glacial lake identified as Lake McKenzie formed. Eventually, water level rose to crest the south ridge a point near Riverdale — at the site of the modern Garrison Dam and a diversion trench was cut. The modern Missouri River follows this pathway. (en)
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  • 1940.000000 (xsd:double)
dbo:inflow
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  • 225308.160000 (xsd:double)
dbo:location
dbo:outflow
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  • 64373.760000 (xsd:double)
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  • 56641312 (xsd:integer)
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  • 4551 (xsd:nonNegativeInteger)
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  • 1041947821 (xsd:integer)
dbo:wikiPageWikiLink
dbp:area
  • varied (en)
dbp:basinCountries
dbp:inflow
dbp:lakeType
  • Glacial lake (en)
dbp:length
  • about (en)
dbp:location
  • McLean, Mercer, and Dunn, Counties, North Dakota (en)
dbp:name
  • Lake McKenzie (en)
dbp:outflow
  • Over the divide to the Yellowstone River or along the face of the Ice sheet. (en)
dbp:pushpinMap
  • North Dakota (en)
dbp:wikiPageUsesTemplate
dcterms:subject
georss:point
  • 47.528614 -101.406182
rdf:type
rdfs:comment
  • Before the Pleistocene Ice Age, circa two million years before present (YBP), the rivers in North, South Dakota and eastern Montana drained northeast into Canada and then into Hudson Bay. The Keewatin Lobe of the continental ice sheet, block the flow of water northward and impounded it along the ice front. Lakes formed, until the waters could find a new way to drain. Initially, the north flowing rivers followed the front of the glacier eastward and into a valley that passed between Garrison and Riverdale, to the Turtle Lake area, and on into Sheridan County. This is known as the preglacial McClean River. This valley became blocked by the glacier and the glacial lake identified as Lake McKenzie formed. Eventually, water level rose to crest the south ridge a point near Riverdale — at the sit (en)
rdfs:label
  • Glacial Lake McKenzie (en)
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  • POINT(-101.40618133545 47.528614044189)
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  • 47.528614 (xsd:float)
geo:long
  • -101.406181 (xsd:float)
prov:wasDerivedFrom
foaf:isPrimaryTopicOf
foaf:name
  • Lake McKenzie (en)
is dbo:wikiPageWikiLink of
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