The depth of the Indian Ocean's continental slope is 4,000 meters
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The seaward edge of the continental shelf is marked by the shelf break, which is the steep slope that descends from the continental shelf to the deep ocean floor. This is where the ocean depth abruptly increases, indicating the boundary between the continental shelf and the continental slope.
Continental shelves typically end where the seafloor drops off into the open ocean, known as the continental slope. This transition point can vary in depth but is usually around 200 meters (656 feet) deep. Beyond the continental slope lies the deep ocean floor known as the abyssal plain.
The temperature of the continental rise is the temp of your dick
The transition between the shelf and the deep seafloor is known as the continental slope. This area is characterized by a steep descent from the continental shelf to the deep ocean, usually at a depth of around 200 meters to 2,000 meters.
You can't have a continent rise from land, but you can have land rise from the continental shelf, which may be under water, and that is called an island.
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The average depth of the continental slope in the Atlantic Ocean is around 700 to 2,000 meters (2,300 to 6,560 feet). It can vary depending on the specific location and geological features in the region.
The slope is the steep transitional area between the shelf and rise. The continental slope depth for the Atlantic Ocean is 3900 meters or in other words 12800 feet.
The steep area between the continental shelf and the ocean floor is called the continental margin. A continental margin is usually composed of a steep continental slope that is followed by the flatter continental rise.
The seaward edge of the continental shelf is marked by the shelf break, which is the steep slope that descends from the continental shelf to the deep ocean floor. This is where the ocean depth abruptly increases, indicating the boundary between the continental shelf and the continental slope.
A sharp drop from a continent to an ocean basin is called a continental slope. This feature marks the boundary between the continental shelf and the deep ocean floor.
Continental slope, Continental Rise, Continental Slope, Seamont, Trench
The continental slope is the area of the ocean floor in which gently drops and is connected to the oceanic crust and continental shelf. This slope is caused by waves within the ocean.
The depth of the continental rise typically ranges from 3,300 to 13,200 feet (1,000 to 4,000 meters). It marks the boundary between the continental slope and the deep ocean floor, where sediment from the continent accumulates.
The area between the continental slope and the ocean basin is known as the continental rise. It is a gradual incline where sediments transported from the continental shelf and slope accumulate before settling in the abyssal plain of the ocean basin.
The two major regions of the ocean floor are the continental margin and the deep ocean basin. The continental shelf is the submerged extension of the continent, characterized by shallow waters, while the continental slope marks the transition between the shelf and the deep ocean, featuring a steep descent. Below the slope lies the continental rise, a more gradual incline formed by sediment accumulation. Together, these features represent a continuum from the landmass to the deep ocean, illustrating the gradual change in depth and geological characteristics of the ocean floor.
continental slope. :)