The headwaters for Puget Sound’s famously rich waters lie far below the surface, in a submarine canyon that draws nutrient-rich water up from the deep ocean. New measurements may explain how the Pacific Northwest’s inland waters are able to support so many shellfish, salmon runs and even the occasional pod of whales.
The Juan de Fuca Canyon reaches the opening of the strait that separates the U.S. and Canada. The canyon is just under 4 miles wide and at least 450 yards deep, or twice the depth of the surrounding seafloor.
University of Washington oceanographers made the first detailed measurements at the headwater’s source, a submarine canyon offshore from the strait that separates the U.S. and Canada. Observations show water surging up through the canyon and mixing at surprisingly high rates, according to a paper published in March in Geophysical Research Letters. Read more
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