About: Lake Puyallup     Goto   Sponge   NotDistinct   Permalink

An Entity of Type : dbo:Lake, within Data Space : dbpedia.demo.openlinksw.com associated with source document(s)
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Lake Puyallup developed along the south edge of the Puget Sound Glacier. The glacier was in retreat northward after having reached its most southerly point. Drainage off the north face of Mount Rainier and the melting ice of the glacier was trapped in the valley of the Puyallup River. As the glacier moved north, the lake grew until it reached its largest capacity with the glacier at the glacial front across the Puyallup valley just south of Commencement Bay at Tacoma and northern bend of the White River at Auburn. When the ice retreated further north, it was reduced in depth and volume and takes on the name of Lake Tacoma.

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  • Lake Puyallup (en)
rdfs:comment
  • Lake Puyallup developed along the south edge of the Puget Sound Glacier. The glacier was in retreat northward after having reached its most southerly point. Drainage off the north face of Mount Rainier and the melting ice of the glacier was trapped in the valley of the Puyallup River. As the glacier moved north, the lake grew until it reached its largest capacity with the glacier at the glacial front across the Puyallup valley just south of Commencement Bay at Tacoma and northern bend of the White River at Auburn. When the ice retreated further north, it was reduced in depth and volume and takes on the name of Lake Tacoma. (en)
foaf:name
  • Lake Puyallup (en)
name
  • Lake Puyallup (en)
geo:lat
geo:long
foaf:depiction
  • http://commons.wikimedia.org/wiki/Special:FilePath/01_Lake_Puyallup_&_Early_Lake_Russell.jpg
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  • Glacial lakes Lake Puyallup & Early Lake Russell (en)
inflow
lake type
  • Glacial lake (en)
location
outflow
  • Ohop channel (en)
pushpin map
  • Washington (en)
georss:point
  • 47.223655 -122.344414
has abstract
  • Lake Puyallup developed along the south edge of the Puget Sound Glacier. The glacier was in retreat northward after having reached its most southerly point. Drainage off the north face of Mount Rainier and the melting ice of the glacier was trapped in the valley of the Puyallup River. As the glacier moved north, the lake grew until it reached its largest capacity with the glacier at the glacial front across the Puyallup valley just south of Commencement Bay at Tacoma and northern bend of the White River at Auburn. When the ice retreated further north, it was reduced in depth and volume and takes on the name of Lake Tacoma. (en)
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page length (characters) of wiki page
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length (μ)
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country
type
foaf:isPrimaryTopicOf
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  • POINT(-122.34441375732 47.223655700684)
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