Krylov Seamount | |
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Krylov Seamount Krylov Seamount (North Atlantic) | |
Summit depth | 1,240 metres (4,070 ft) |
Location | |
Coordinates | 17°31′N 30°07.5′W / 17.517°N 30.1250°W[1] |
Krylov Seamount (also known as Albatross Seamount[2] or Krylou Seamount[3]) is a volcanic seamount in the Atlantic Ocean, west of the Cape Verde islands. It is formed by one seamount and one ridge which are separated by a 5 kilometres (3.1 mi) wide depression, and it rises to a minimum depth of 1,240 metres (4,070 ft); formerly the depression was interpreted to be a caldera. The seamount probably formed no later than 70-75 million years ago before sinking to its current depth.
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