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The Broad River is a tidal channel in Beaufort and Jasper counties, South Carolina. [1] The channel flows between the mainland on the west and Port Royal and Parris islands on the east. The Coosawhatchie River flows into the Broad River at the head. It joins Coosaw River channel Northeast and continues Southeast to the Atlantic Ocean as Port ...
USGS Hydrologic Unit Map - State of South Carolina (1974) This page was last edited on 17 February 2024, at 22:19 (UTC). ... List of rivers of South Carolina.
In 1675 Cooper was granted 12,000 acres (4,900 ha) of land along the river after a permanent settlement was made at Albemarle Point in 1670. This settlement was the “first permanent European settlement” in South Carolina and today Albemarle Point is known as Charles Towne Landing. The settlement would be moved to its current peninsular ...
The Charleston Harbor gauge clocked 3.47 feet of inundation, with a tide at 9.23 feet — the fifth-highest value since 1921.
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.
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[1] In terms of tides, tidal rivers are classified as microtidal (<2 m), mesotidal (2-4 m), and macrotidal (>4 m). [2] Areas of brackish water seaward of the tidal river section are often called estuaries. A phenomenon commonly associated with tidal rivers is a tidal bore, where a wall of water travels upriver during a flood tide. [1]
King tides are the highest tides. They are naturally occurring, predictable events. Tides are the movement of water across Earth's surface caused by the combined effects of the gravitational forces exerted by the Moon, Sun, and the rotation of Earth which manifest in the local rise and fall of sea levels.