About: Lake Skokomish

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During the Vashon Glaciation a series of lakes formed along the southern margin of the Cordilleran Ice Cap. In the Hood Canal depression, two significant lake stages existed, Lake Skokomish and Lake Hood. Early Lake Skokomish’s surface was at 350 ft (110 m) above sea level, draining across the divide at Shelton, Washington into early Glacial Lake Russell. As the glacier receded northward, this freshwater lake grew in size, until the ice was north of the Clifton channel. With the opening of the Clifton channel, the water dropped to 160 m (520 ft) above sea level. This longer and lower level lake is referred to as Lake Hood. The glacier continued to recede northward until it reached the Poulsbo channel. Here, the water level equalized to Glacial Lake Russell nolonger having a separate identi

Attributes	Values
rdf:type	Thing place dbo:Location schema:BodyOfWater schema:LakeBodyOfWater schema:Place natural place Lake geo:SpatialThing body of water lake
rdfs:label	Lake Skokomish (en)
rdfs:comment	During the Vashon Glaciation a series of lakes formed along the southern margin of the Cordilleran Ice Cap. In the Hood Canal depression, two significant lake stages existed, Lake Skokomish and Lake Hood. Early Lake Skokomish’s surface was at 350 ft (110 m) above sea level, draining across the divide at Shelton, Washington into early Glacial Lake Russell. As the glacier receded northward, this freshwater lake grew in size, until the ice was north of the Clifton channel. With the opening of the Clifton channel, the water dropped to 160 m (520 ft) above sea level. This longer and lower level lake is referred to as Lake Hood. The glacier continued to recede northward until it reached the Poulsbo channel. Here, the water level equalized to Glacial Lake Russell nolonger having a separate identi (en)
foaf:name	Lake Skokomish, Lake Hood (en)
name	Lake Skokomish, Lake Hood (en)
geo:lat	47.363323 (xsd:float)
geo:long	-123.127487 (xsd:float)
foaf:depiction
location	Hood Canal Kitsap County, Washington
dct:subject	Former lakes of the United States Thurston County, Washington King County, Washington Glacial lakes of the United States Proglacial lakes Geography of Washington (state) Pierce County, Washington
Wikipage page ID	54542891 (xsd:integer)
Wikipage revision ID	1095437067 (xsd:integer)
Link from a Wikipage to another Wikipage	Former lakes of the United States Thurston County, Washington Poulsbo, Washington King County, Washington Cordilleran Ice Cap Big Quilcene River Glacial lakes of the United States United States Cordilleran Ice Sheet Proglacial lakes Glacial Lake Russell Skokomish River Geography of Washington (state) Glacial lake Lake Hood Canal Kitsap County, Washington Pierce County, Washington Shelton, Washington Vashon Glaciation
reference	Washington Geological Survey, Bulletin No. 8; Glaciation of the Puget Sound Region; J. Harlen Bretz; Olympia, Wash, Frank M. Lamborn Public Printer; 1913 (en)
sameAs	Lake Skokomish Lake Skokomish
dbp:wikiPageUsesTemplate	dbt:Infobox_lake dbt:! dbt:About dbt:Convert dbt:Coord dbt:Reflist dbt:Pleistocene_Lakes_and_Seas dbt:Puget_Sound
thumbnail	wiki-commons:Special:FilePath/03_Lake_Skokomish_&_Russell_(1913)_fig_11.jpg?width=300
basin countries	United States
caption	Glacial Lakes Skokomish & Russell in the Puget Sound basin. (en)
inflow	Cordilleran Ice Sheet
lake type	Glacial lake (en)
location	Hood Canal Kitsap County, Washington
outflow	Shelton Delta, Shelton, Washington; Clifton Channel, North Bay of Case Inlet; Poulsbo Channel, Poulsbo, Washington (en)
pushpin map	Washington (en)
georss:point	47.363322 -123.127485
has abstract	During the Vashon Glaciation a series of lakes formed along the southern margin of the Cordilleran Ice Cap. In the Hood Canal depression, two significant lake stages existed, Lake Skokomish and Lake Hood. Early Lake Skokomish’s surface was at 350 ft (110 m) above sea level, draining across the divide at Shelton, Washington into early Glacial Lake Russell. As the glacier receded northward, this freshwater lake grew in size, until the ice was north of the Clifton channel. With the opening of the Clifton channel, the water dropped to 160 m (520 ft) above sea level. This longer and lower level lake is referred to as Lake Hood. The glacier continued to recede northward until it reached the Poulsbo channel. Here, the water level equalized to Glacial Lake Russell nolonger having a separate identify. (en)
catchment	Hood Canal
maximum depth (μ)	106.680000 (xsd:double)
inflow	Cordilleran Ice Sheet
outflow	Poulsbo, Washington Shelton, Washington
average depth (μ)	48.768000 (xsd:double)
quote	Washington Geological Survey, Bulletin No. 8; Glaciation of the Puget Sound Region; J. Harlen Bretz; Olympia, Wash, Frank M. Lamborn Public Printer; 1913
prov:wasDerivedFrom	wikipedia-en:Lake_Skokomish?oldid=1095437067&ns=0
page length (characters) of wiki page	6546 (xsd:nonNegativeInteger)
elevation (μ)	350.000000 (xsd:double)
country	United States
type	Glacial lake
foaf:isPrimaryTopicOf	wikipedia-en:Lake_Skokomish
geo:geometry	POINT(-123.12748718262 47.36332321167)
is Link from a Wikipage to another Wikipage of	List of prehistoric lakes Skokomish
is Wikipage disambiguates of	Skokomish
is foaf:primaryTopic of	wikipedia-en:Lake_Skokomish

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