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dc.contributor.author Phillips, Ronald C en_US
dc.contributor.author Fleenor, Bill en_US
dc.date.accessioned 2008-11-26T07:23:34Z en_US
dc.date.available 2008-11-26T07:23:34Z en_US
dc.date.issued 1970-04 en_US
dc.identifier.citation Phillips RC, Fleenor B. 1970. Investigation of the benthic marine flora of Hood Canal, Washington. Pac Sci 24(2): 275-281. en_US
dc.identifier.issn 0030-8870 en_US
dc.identifier.uri http://hdl.handle.net/10125/4047 en_US
dc.description.abstract Hood Canal is a fjord (Kollmeyer, 1965) connected to Puget Sound (Fig. 1) . Water in the canal was reported as highly stratified owing to a large volume of freshwater runoff from the Olympic Mountains (Kollmeyer, 1965). The water mass is relatively isolated from that of Puget Sound proper by an entrance sill at Vinland, 44 meters deep, 22.36 km (12 nautical miles) south of Admiralty Inlet. Owing to a lack of investigation en_US
dc.language.iso en-US en_US
dc.publisher University of Hawai'i Press en_US
dc.title Investigation of the Benthic Marine Flora of Hood Canal, Washington en_US
dc.type Article en_US
dc.type.dcmi Text en_US

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