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Seymour Narrows is notable also because the flowing current can be sufficiently turbulent to realize a Reynolds number of about , i.e. one hundred million, which is possibly the largest Reynolds number regularly attained in natural water channels on Earth (the current speed is about 8 m/s, 26 ft/s, the nominal depth about 100 m, 330 ft). [4]
Puget Sound's shoreline is 1,332 miles (2,144 km) long, encompassing a water area of 1,020 square miles (2,600 km 2) and a total volume of 26.5 cubic miles (110 km 3) at mean high water. The average volume of water flowing in and out of Puget Sound during each tide is 1.26 cubic miles (5.3 km 3).
This lake now drains both to Cases Inlet and Hood Canal. Gravel terraces exist along the channel, and one terrace on the east side continues as a small channel directly eastward to Cases Inlet. The Clifton channel ends in the forest west of Allyn, 160 feet (49 m) above tide, corresponding with the dominant water plane of Lake Russell. [1]
The Puget Sound region is a coastal area of the Pacific Northwest in the U.S. state of Washington, including Puget Sound, the Puget Sound lowlands, and the surrounding region roughly west of the Cascade Range and east of the Olympic Mountains. It is characterized by a complex array of saltwater bays, islands, and peninsulas carved out by ...
The Colvos Passage is a tidal strait within Puget Sound in the American state of Washington running west of Vashon Island between the island and the Kitsap Peninsula. It lies just north of the Dalco Passage. Colvos Passage has a permanent predominantly northbound current, in contrast to the rest of Puget Sound which varies with the tide.
The city of Seattle, Washington, is located on a narrow isthmus between Puget Sound on the west and Lake Washington on the east; water comprises approximately 41% of the total area of the city. [1] It was founded on the harbor of Elliott Bay , home to the Port of Seattle —in 2002, the 9th busiest port in the United States by TEUs of container ...
The Montlake Cut, part of the Lake Washington Ship Canal, connects the lake to Lake Union and ultimately Puget Sound. Concrete floating bridges are employed to span the lake because Lake Washington's depth and muddy bottom prevented the emplacement of the pilings or towers necessary for the construction of a causeway or suspension bridge. The ...
In the Puget Sound depression, a series of lakes developed, of which Lake Russell was the largest and the longest lasting. Early Lake Russell’s surface was at 160 ft (49 m) above sea level, draining across the divide at Shelton, Washington into early Glacial Lake Russell.