Investigation of the Benthic Marine Flora of Hood Canal, Washington

Item Description

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