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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.
Dozens of homes were left unstable in the Daytona Beach area after Hurricane Nicole's erosion. Joe Raedle/Getty ImagesBack-to-back hurricanes left an unnerving scene on the Florida coast in ...
Long Beach, nicknamed "The City By the Sea" and once known as "The Riviera of the East", boasts a 2.2-mile (3.5-km) boardwalk east of New York Avenue, which was planned and developed in 1906-1907 by Tammany Hall-connected real estate developer and former New York senator William H. Reynolds.
Murrells Inlet is located in northeastern Georgetown County at (33.551593, -79.048794 The northern edge of the CDP follows the Horry County line. U.S. Route 17 (Ocean Highway) runs through the center of the community, leading northeast 13 miles (21 km) to Myrtle Beach and southwest 21 miles (34 km) to Georgetown, the seat of Georgetown County.
Murrells Inlet Historic District is a national historic district located at Murrells Inlet, Georgetown County, South Carolina.The district encompasses 37 contributing buildings and contains a significant concentration of buildings that visually reflect the transition of the area from adjoining estates of two 19th-century rice planters into a 20th-century resort community.
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Murrells Inlet, Georgetown County, South Carolina: Coordinates: Area: 2,500 acres (10.1 km 2) Camp sites: 107 30 Amp standard campsites 21 30 Amp full service campsites 42 50 Amp full service campsites 6 walk-in tent sites: Hiking trails: 2: Website: Official website
A tidal creek or tidal channel is a narrow inlet or estuary that is affected by the ebb and flow of ocean tides. [1] Thus, it has variable salinity and electrical conductivity over the tidal cycle, and flushes salts from inland soils. Tidal creeks are characterized by slow water velocity, resulting in buildup of fine, organic sediment in wetlands.
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