Abyssal plain. It is the very level area of the deep ocean floor, usually lying at the foot of the continental rise.
The flat part of the ocean floor is called the abyssal plain. It is a smooth, flat region that lies between the continental rise and the mid-ocean ridges.
At deep-ocean trenches, subduction allows part of the ocean floor to sink back into the mantle. The ocean floor does not just keep spreading. Instead, it sinks beneath deep underwater canyons called deep-ocean trenches. Where there are trenches, subduction takes place.
At deep-ocean trenches, subduction allows part of the ocean floor to sink back into the mantle. The ocean floor does not just keep spreading. Instead, it sinks beneath deep underwater canyons called deep-ocean trenches. Where there are trenches, subduction takes place.
Rift zone- Site of crust formationAbyssal plain- Very flat part of ocean floorSubmarine canyon- Part of the continental marginGuyot- Flat-topped, underwater mountain.
Rift Zone: Site of crust formation Abyssal Plain: Very flat part of ocean floor Guyots: Flat-topped, underwater mountains Submarine canyons: Part of the continental margins :D
False, continental shelves are part of the Coastal Plain
The deepest parts of the ocean floor are caused by plate tectonic subduction and occur where the sea floor sinks back into the mantle in a subduction zone. These areas are called deep sea trenches and the Challenger Deep in the Mariana Trench in the Pacific is the deepest known point in Earth's oceans.
In a process taking tens of millions of years, part of the ocean floor sinks back into the mantle at deep ocean trenches.
Beyond the continental shelf, the seafloor drops off abruptly into the deep ocean, forming the continental slope. This slope extends down to the abyssal plain, which makes up a large part of the ocean floor. The abyssal plain is characterized by flat, sediment-covered expanses that are home to a variety of deep-sea organisms.
The ocean in certain points can be 11,030 meters deep.
The flat part of the seafloor is called the abyssal plain. It is a smooth, flat area of the ocean floor that lies between the continental margins and the oceanic ridges. The abyssal plain is typically covered with sediments and is home to a diverse range of marine life.
Yes, ocean trenches are a long, narrow, deep depression in the ocean bed.They typically run parallel to a plate boundary.The Marianas Trench is the deepest part of the world's oceans.