Investigation of the Benthic Marine Flora of Hood Canal, Washington
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
Description
Keywords
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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