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The North Sea lies between Great ... For the most part, the sea lies on the European continental shelf ... This was the deepest dinosaur fossil ever found and the ...
Off the Rogaland coast, it is 250–300 m (820–980 ft) deep, and at its deepest point, off Arendal, it reaches 700 m (2,300 ft) deep as compared to the average depth of the North Sea, about 100 m (330 ft). [5] The trench is not a subduction-related oceanic trench, where one tectonic plate is being forced under another.
The basin floor measures about 220 km 2 (85 sq mi) and is the deepest point in the Arctic Ocean. [9] [10] The only person to have reached the bottom of the Molloy Deep is American explorer Victor Vescovo as part of his Five Deeps Expedition.
The deepest point of the trench is more than 2 km (1.2 mi) farther from sea level than the peak of Mount Everest. [a] At the bottom of the trench, the water column above exerts a pressure of 1,086 bar (15,750 psi), more than 1,071 times the standard atmospheric pressure at sea level. At this pressure, the density of water is increased by 4.96%.
Milwaukee Deep, also known as the Milwaukee Depth, is the deepest part of the Puerto Rico Trench, constituting the deepest points in the Atlantic Ocean. [1] Together with the surrounding seabed area, known as Brownson Deep, the Milwaukee Deep forms an elongated depression that constitutes the floor of the trench. As there is no geomorphological ...
The purple sea floor at the center of the view is the Puerto Rico Trench, the deepest part of the Atlantic Ocean. The Puerto Rico Trench is located on the boundary between the North Atlantic Ocean and Caribbean Sea, parallel to and north of Puerto Rico, where the oceanic trench reaches the deepest points in the Atlantic Ocean.
During interglacial periods (when sea levels were high) between the initial flooding 450,000 years ago until around 180,000 years ago, the Channel would still have been separated from the North Sea by a land bridge to the north of the Strait of Dover (the Strait of Dover at this time formed part of a estuary fed by the Thames and Scheldt ...
Beaufort's Dyke is a natural glacial-formed trench within the North Channel between Northern Ireland and Scotland. The dyke is 50 kilometres (25 nautical miles) long, 3.5 kilometres (2 nautical miles) wide and 200–312 m (700–1,000 ft) deep. The Dyke is one of the deepest areas of the European continental shelf. [1]