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Tide tables, sometimes called tide charts, are used for tidal prediction and show the daily times and levels of high and low tides, usually for a particular location. [1] Tide heights at intermediate times (between high and low water) can be approximated by using the rule of twelfths or more accurately calculated by using a published tidal ...
Rawsonville is an unincorporated community on the boundary of Washtenaw and Wayne County in the U.S. state of Michigan. [1] Small parts of the historic community of Rawsonville lie under Belleville Lake, which is an artificial reservoir created in 1925 when the Eastern Michigan Edison Company built the French Landing Dam and Powerhouse along the Huron River. [2]
Welcome to Belleville Sign. Belleville is a city in Wayne County in the U.S. state of Michigan.A western suburb of Detroit, Belleville is located roughly 29 miles (46.7 km) southwest of downtown Detroit, and 18 miles (29.0 km) southeast of Ann Arbor, and is completely surrounded by Van Buren Township.
The construction of the French Landing Dam and Powerhouse in 1925 led to the creation of Belleville Lake. Belleville Lake is an artificial reservoir created by the hydroelectric French Landing Dam and Powerhouse in 1925. The lake was originally named Edison Lake, because the dam was constructed by the Detroit Edison Company.
Van Buren Township is a charter township in Wayne County in the U.S. state of Michigan.A western suburb of Detroit, Van Buren Township is located roughly 28 miles (45.1 km) southwest of downtown Detroit, and 17 miles (27.4 km) southeast of Ann Arbor.
As of the 2010 census Sumpter Township had a population of 9,549. The ethnic and racial makeup of the population was 82.1% non-Hispanic white, 12.0% African American, 0.6% Native American, 0.3% Asian, 0.1% from some other race, 2.9% reporting two or more races and 2.6% Hispanic or Latino.
Tides are the rise and fall of sea levels caused by the combined effects of the gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range").
At neap tides the semi-diurnal tide is virtually absent, resulting in the phenomenon known as a "dodge tide" [6] [7] —a day-long period of slack water—occurring twice a month; this effect is accentuated near the equinoxes when the diurnal component also vanishes, resulting in a period of 2–3 days of slack water. [8] [9] [10]