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The Sea of Abaco (sometimes Abaco Sound), located in The Bahamas, is an approximately 100 kilometres (62 miles) long saltwater lagoon separating Great Abaco Island (known locally as the 'mainland') from a chain of barrier islands known as the Abaco Cays. Depths in the Sea of Abaco are generally a few metres, and shallow reefs and shoals can ...
In the video, Cuba is mostly covered by clouds, but the reefs in the Bahamas stand out. The Bahamas are a group of about 700 islands and cays in the western Atlantic Ocean, of which only between 30 and 40 are inhabited. The largest of the islands is Andros Island, located north of Cuba and 200 kilometres (120 miles) southeast of Florida.
The sport fishing in Chub Cay is well known due to its proximity to the Tongue of the Ocean. The Tongue of the Ocean is a deep underwater trench that attracts varying species of marine life. [13] Chub Cay’s water offers a variety of different types of fishing including bone fishing, deep sea fishing, and bottom fishing. [14]
Scientists have mapped the largest coral reef deep in the ocean, stretching hundreds of miles off the U.S. Atlantic coast. While researchers have known since the 1960s that some coral were present ...
The lagoon is mostly 20–30 ft deep with scattered coral heads. Good light is needed to navigate it. Once at the head of the lagoon, there is a large field of 10 ft sand to anchor in. The charts indicate areas of the reef dry at low water, which suggests good protection from surge at low tide, but as of 2009, little of the reef actually dries.
The Florida Reef Tract—largest continental US reef and the third-largest coral barrier reef, extends from Soldier Key, located in Biscayne Bay, to the Dry Tortugas in the Gulf of Mexico [68] Blake Plateau has the world's largest known deep-water coral reef , comprising a 6.4 million acre reef that stretches from Miami to Charleston, S. C.
On a recent expedition, a group of ocean researchers discovered 85 miles of deep-sea coral reef off the coast of the southeastern US.
This channel and the Providence Channels are the two main branches of the Great Bahama Canyon, a submerged geological feature formed by erosion during periods of lower sea level. During their early history the Tongue of the Ocean and the Providence Channel were broad, relatively shallow basins flanked by growing carbonate banks .