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Little Lagoon Nautical Chart. Little Lagoon is located on the western side of Gulf Shores, Alabama, and is situated between the Gulf of Mexico and Bon Secour Bay.The lagoon has four small fresh/brackish water lakes that drain into it, Lake Shelby (678 acres), Middle Lake (250 acres), Little Lake (45 acres), and Gator Lake (45 acres). [1]
The Gulf Intracoastal Waterway (GIWW [1]) is the portion of the Intracoastal Waterway located along the Gulf Coast of the United States. It is a navigable inland waterway running approximately 1,300 mi (2,100 km) [ 1 ] from Saint Marks, Florida , to Brownsville , Texas .
Keel depth (sometimes given as Depth to keel) is the depth (or draft) of water from the water surface to the keel of a vessel, the deepest part. The keel establishes a commonly defined reference point to measure to. Keel depth is useful for determining safe operating depth in shallow water.
Gulf Shores is located on the Gulf of Mexico, and is the southernmost settlement in the state of Alabama. [2] It is served by Alabama State Route 59 (Gulf Shores Parkway), which leads north to Foley. Route 182 (Beach Boulevard) runs east-west along the shore front, while Route 180 (Fort Morgan Road) runs parallel to it, north of Little Lagoon.
Continental shelves teem with life because of the sunlight available in shallow waters, in contrast to the biotic desert of the oceans' abyssal plain. The pelagic (water column) environment of the continental shelf constitutes the neritic zone, and the benthic (sea floor) province of the shelf is the sublittoral zone. [35]
A depth finder may refer to any of the following: Sonar: use of underwater sound propagation to measure depth; Fathometer or fishfinder: a device to locate fish at various water depths; Echo sounding: a technique using sound pulses to measure depth; sounding line: a length of rope used to measure water depth
Surge risk rises on Florida’s Gulf Coast. The wide stretch of shallow water west of Florida is a perfect breeding ground for storm surge. When a hurricane passes over the ocean, its strong winds ...
Many shallow marine environments are associated with carbonate factory zones, where processes that remove CO 2 from the water change bicarbonate ions into carbonate ions, supporting lime precipitation. These processes include increasing temperature, intense evaporation, and mixing water that is high in CO 3 and low in calcium cations with seawater.
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