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Then mean longitude is also [1] L = ϖ + M. Another form often seen is the mean longitude at epoch, ε. This is simply the mean longitude at a reference time t 0, known as the epoch. Mean longitude can then be expressed, [2] L = ε + n(t − t 0), or L = ε + nt, since t = 0 at the epoch t 0. where n is the mean angular motion and t is any ...
Sun City was a success, with the company selling 237 homes within its first three days of opening. [12] It was followed by Sun City, California, the Kern City, Sun City Center, Florida, and similar developments in Nevada, Illinois, and Massachusetts. [13]
Downtown Canyon. Canyon is a city in, and the county seat of, Randall County, Texas, United States. The population was 14,836 at the 2020 census. [5] It is part of the Amarillo, Texas, metropolitan statistical area. Canyon is the home of the Panhandle–Plains Historical Museum, and the outdoor musical drama Texas.
The development has plans to add nearly 10,000 homes and apartments, 1.5 million square feet of retail and office space and 1,330 acres of passive and recreational park space.
Geodetic latitude and geocentric latitude have different definitions. Geodetic latitude is defined as the angle between the equatorial plane and the surface normal at a point on the ellipsoid, whereas geocentric latitude is defined as the angle between the equatorial plane and a radial line connecting the centre of the ellipsoid to a point on the surface (see figure).
Sun City is an unincorporated community and census-designated place in Maricopa County, Arizona, United States, that is located within the Phoenix metropolitan area. The population was 39,931 as of the 2020 census. [3] Its adjoining sister city is Sun City West. Both Sun Cities are retirement communities popular with snowbirds.
Sun City Texas is a 4,750-acre (19.2 km 2) [1] age-restricted community located in Georgetown, Texas, a city 35 miles north of Austin off Interstate 35. It is part of the chain of Sun City communities started by Del Webb .
Also amphidrome and tidal node. A geographical location where there is little or no tide, i.e. where the tidal amplitude is zero or nearly zero because the height of sea level does not change appreciably over time (meaning there is no high tide or low tide), and around which a tidal crest circulates once per tidal period (approximately every 12 hours). Tidal amplitude increases, though not ...