Investigation of the Benthic Marine Flora of Hood Canal, Washington

Date
1970-04
Authors
Phillips, Ronald C.
Fleenor, Bill
Journal Title
Journal ISSN
Volume Title
Publisher
University of Hawai'i Press
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
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Citation
Phillips RC, Fleenor B. 1970. Investigation of the benthic marine flora of Hood Canal, Washington. Pac Sci 24(2): 275-281.
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