Submarine Canyons
The part of the sea level that is known as continent is the continental shelf, which is the submerged region of a continent that extends from the shoreline to the continental slope. The continental shelf is relatively shallow compared to the deeper oceanic waters beyond it.
continental shelves
The area between the continental shelf and the ocean floor is known as the continental slope. This region marks the transition from the relatively shallow waters of the continental shelf to the deeper oceanic depths. The continental slope is characterized by a steep gradient and is often where sediment from the shelf accumulates, leading to an important zone for marine life and geological processes.
rift valley Answer 2 Continents are formed when continental plates pull apart.
Sonar shows that the edges of continental shelves match the underwater slope known as the continental slope. This underwater feature marks the boundary between the continental shelf and the deeper ocean floor. The continental slope is steeper than the continental shelf and descends into the abyssal plain.
valleys some of the tallest mountains and deepest valleys known in the solar system.
A shallow area near the coast of a continent is known as a continental shelf. It is an underwater landmass that extends from the shoreline to the deeper ocean. The continental shelf is rich in marine life and is important for various ecological processes.
what is this
The area between the continental shelf and the ocean floor is known as the continental slope. This region marks the transition from the shallower, more biologically productive continental shelf to the deeper, less accessible oceanic depths. The continental slope typically features a steep gradient and can host unique geological formations and ecosystems. It plays a crucial role in ocean currents and sediment transport.
This is known as a thermocline. It is a layer where the temperature decreases rapidly with depth. The thermocline often separates the warm surface waters from the colder deeper waters in a lake or ocean.
This region is known as the continental shelf. It is a gently sloping area of land between the shoreline and the deep ocean. The continental shelf is rich in marine life and is an important area for commercial fishing and oil exploration.
The strength of continental crust generally increases with depth due to higher pressure and temperature. The top layer of continental crust, known as the brittle upper crust, is more prone to fracturing and faulting, while the deeper layers become more ductile and can deform plastically under stress.