Historical bathymetric changes near the entrance to Grays Harbor, Washington
Large changes in the distribution of sediment near the entrance to Grays Harbor, Washington, have occurred since the long rock jetties were built to confine flow. Spits to the north and south of the entrance have grown, the entrance channel has deepened, and the outer bar has eroded and moved offsho...
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Format: | Report |
Language: | English |
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Pacific Northwest Laboratory
1992
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Online Access: | https://doi.org/10.2172/6615253 https://digital.library.unt.edu/ark:/67531/metadc1193426/ |