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The Atlantis Massif is a prominent undersea massif in the North Atlantic Ocean.It is a dome-shaped region approximately 10 miles (16 km) across and rising about 14,000 feet (4,267 m) from the sea floor.
Not a trench, but more of an "underwater valley", it is estimated to be at most ~19,685 feet (3.7 miles; 6.0 km) in depth. The Laurentian Fan is a product of glaciation and water currents from the Gulf of Saint Lawrence. [2] It is part of the Laurentian cone region, bound by the Laurentian Channel and the Sohm Abyssal Plain.
The islet contains a few underwater caves. [3] The islet seen from São Miguel, with Farilhão on the left. The islet is located between 500 metres (1,600 ft) and 1 kilometre (0.62 mi) off the south-central coast of the island of São Miguel, adjacent the municipality, town, and port of Vila Franca do Campo.
The Bear Seamount is a guyot or flat-topped underwater volcano in the Atlantic Ocean. It is the oldest of the New England Seamounts , which was active more than 100 million years ago. It was formed when the North American Plate moved over the New England hotspot . [ 3 ]
The Northeast Canyons and Seamounts Marine National Monument is located within the New England and mid-Atlantic regions, 130 miles southeast of Cape Cod. [1] It comprises a total area of 4,913 square miles, [1] and protects four underwater seamounts (Bear, Mytilus, Physalia, and Retriever Seamounts) and three submarine canyons in the edge of the continental shelf (Oceanographer, Lydonia, and ...
Ampère Seamount is a seamount in the Atlantic Ocean, 410 km (250 mi) south-west of Portugal and 470 km (290 mi) west of Morocco. It is located at 35°02'N and 12°54'W. This seamount is about 90 x 40 km, its base is at a depth of approximately 4,500 m (14,800 ft). The summit topography is rather disturbed with a summit plateau that is 6 by 3 ...
On average, the Atlantic is the saltiest major ocean; surface water salinity in the open ocean ranges from 33 to 37 parts per thousand (3.3–3.7%) by mass and varies with latitude and season. Evaporation, precipitation, river inflow and sea ice melting influence surface salinity values.
The Grand Banks of Newfoundland are a series of underwater plateaus south-east of the island of Newfoundland on the North American continental shelf. The Grand Banks are one of the world's richest fishing grounds, supporting Atlantic cod, swordfish, haddock and capelin, as well as shellfish, seabirds and sea mammals.
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