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Choctawhatchee Bay is a bay in the Emerald Coast region of the Florida Panhandle. The bay, located within Okaloosa and Walton counties , is an inlet of the Gulf of Mexico and has a surface area of 334 square kilometres (129 sq mi). [ 2 ]
A section of the Intracoastal Waterway in Pamlico County, North Carolina, crossed by the Hobucken Bridge Inland Waterways, Intracoastal Waterways, and navigable waterways. The Intracoastal Waterway (ICW) is a 3,000-mile (4,800 km) inland waterway along the Atlantic and Gulf of Mexico coasts of the United States, running from Massachusetts southward along the Atlantic Seaboard and around the ...
The term tidewater may be correctly applied to all portions of any area, including Virginia, where the water level is affected by the tides (more specifically, where the water level rises when the tide comes in). In the case of Virginia, the Tidewater region includes the land east of the Fall Line, the
The Choctawhatchee River is a 141-mile-long (227 km) [1] river in the southern United States, flowing through southeast Alabama and the Panhandle of Florida before emptying into Choctawhatchee Bay in Okaloosa and Walton counties. The river, the bay and their adjacent watersheds collectively drain 5,350 square miles (13,900 km 2). [2]
Santa Rosa Sound is a sound connecting Pensacola Bay and Choctawhatchee Bay in Florida.The northern shore consists of the Fairpoint Peninsula and portions of the mainland in Santa Rosa County and Okaloosa County.
A chart datum is the water level surface serving as origin of depths displayed on a nautical chart and for reporting and predicting tide heights. A chart datum is generally derived from some tidal phase, in which case it is also known as a tidal datum. [1] Common chart datums are lowest astronomical tide (LAT) [1] and mean lower low water (MLLW).
A bore in Morecambe Bay, in the United Kingdom Video of the Arnside Bore, in the United Kingdom The tidal bore in Upper Cook Inlet, in Alaska. A tidal bore, [1] often simply given as bore in context, is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travels up a river or narrow bay, reversing the direction of the river or bay's current.
1.1 Atlantic Ocean north of Chesapeake Bay. 1.2 Chesapeake Bay. 1.3 Atlantic Ocean south of Chesapeake Bay. ... Richmond, VA: Virginia Office of Graphic Communications.
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