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The only outflow from the lake was through a swamp that became the Lake Worth Creek as it approached the Loxahatchee River and Jupiter Inlet. In 1866 travelers reported that fresh water was pouring out of the lake into the ocean at a point about ten miles south of the Jupiter Inlet. One report is that a settler named Lang had dug the channel to ...
In 1917 the South Lake Worth Inlet was created in a failed effort to improve tidal circulation and provide flushing to the south end of the Lagoon. The completion of the West Palm Beach Canal (which connected to Lake Okeechobee , draining land west of West Palm Beach as well as the Everglades ) in 1925 resulted in significant freshwater inflow ...
The South Lake Worth Inlet, also known as the Boynton Inlet, is an artificial cut through a barrier beach connecting the south end of the Lake Worth Lagoon in Palm Beach County, Florida with the Atlantic Ocean. The inlet is 130 feet (40 m) wide and 6 to 12 feet (1.8 to 3.7 m) deep.
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 ...
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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.
Lake Worth Beach, previously named Lake Worth, is a city in east-central Palm Beach County, Florida, United States, located about 63 miles (101 km) north of Miami.The city's name is derived from the body of water along its eastern border known as the Lake Worth Lagoon, which was named for General William J. Worth, who led United States Army forces during the last part of the Second Seminole War.
Tide flow information is most commonly seen on nautical charts, presented as a table of flow speeds and bearings at hourly intervals, with separate tables for spring and neap tides. The timing is relative to high water at some harbour where the tidal behaviour is similar in pattern, though it may be far away.