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Tidal range is the difference in height between high tide and low tide. Tides are the rise and fall of sea levels caused by gravitational forces exerted by the Moon and Sun, by Earth's rotation and by centrifugal force caused by Earth's progression around the Earth-Moon barycenter. Tidal range depends on time and location.
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).
High tide on Mud Bay in the spring. Mud Bay is the southernmost reach of Puget Sound, at Eld Inlet just outside the city limits of Olympia, Washington. [1] [2] [3] The name Eld Inlet was officially bestowed after a member of the U.S. Navy's Wilkes Expedition, but "Mud Bay" is a local, informal adoption.
This 1909 topographical map of Greater Seattle shows the old route of the Duwamish (lower center). Maps showing the changes of course and nomenclature of rivers in the Duwamish Valley, 1899–1959. Survey of the river in 1862, note the mouth of the river in its natural state.
A king tide is an especially high tide that brings unusually high water levels and can cause local tidal flooding. Some images taken around #GigHarbor at approximately 9:00 a.m. on 12/27/22 ...
The East Waterway is crossed by a causeway supported a few feet above high tide by pilings. Vigor Industrial operates a 27-acre (10.9 ha) shipyard on the island, which is also the site of some of the Port of Seattle's terminals and the publishing branch of The Mountaineers (Mountaineering: The Freedom of the Hills, among others).
Lake Washington (Lushootseed: x̌ačuʔ) [3] [a] is a large freshwater lake adjacent to the city of Seattle, Washington, United States. [4] It is the largest lake in King County and the second largest natural lake in the state of Washington, after Lake Chelan.
[5]: 7–8 The construction of the locks profoundly reshaped the topography of Seattle and the surrounding area, lowering the water level of Lake Washington and Lake Union by 8.8 feet (2.7 m), adding miles of new waterfront land, reversing the flow of rivers, and leaving piers in the eastern half of Salmon Bay high and dry. [5]