False.
There are a number of processes that could fit this description including mud / debris flows and solifluction (both types of "mass wasting"). In pelagic / benthic (marine) settings turbidity currents would also fit this description. Please see the related links.
Slope canyons are narrow, deep channels carved into the seafloor on the continental slope. They are typically formed by a combination of erosional processes like underwater landslides, turbidity currents, and the movement of sediment down the continental slope. Slope canyons play a crucial role in transporting sediment and nutrients from the continental shelf to the deep ocean.
Cell plate is formed in plant cell division.It is characteristic feature of plants.
A substance that is formed from one type of atoms with a characteristic set of physical and chemical properties is called an element.
Turbidity currents usually originate along the continental slope and continue across the continental rise, still cutting channels. Eventually they lose momentum and come to rest along the floor of the deepest ocean basin. As these currents slow, suspended sediments begin to settle out. First, the coarser sand is dropped, followed by successively finer accumulations of silt and then clay. these deposits, called turbidites, display a decrease in sediment grain size from bottom to top.
Graded beds of sediment are typically formed by turbidity currents in water environments or by debris flows on land. These currents transport a mixture of different-sized sediments, with larger particles settling first as the flow slows down, creating the graded bedding pattern.
An ocean submarine canyon is typically formed through a combination of processes such as erosion by currents, turbidity flows, and underwater landslides. These can carve deep, V-shaped valleys in the seafloor, similar to canyons on land. Over time, the canyon can deepen and widen as sediment is transported and deposited within it.
A submarine canyon refers to a steep-sided valley cut into the sea floor of the continental slope. It is formed through turbidity currents that carve out the submarine canyons in the continental shelf.
A submarine canyon refers to a steep-sided valley cut into the sea floor of the continental slope. It is formed through turbidity currents that carve out the submarine canyons in the continental shelf.
There are a number of processes that could fit this description including mud / debris flows and solifluction (both types of "mass wasting"). In pelagic / benthic (marine) settings turbidity currents would also fit this description. Please see the related links.
A difference between gyres and currents is that currents are formed by the wind, but gyres are formed by currents.
A calciturbidite is a turbidite - a sedimentary deposit formed by a turbidity current - composed of calcium carbonate.
from winds :)
the ocean .
A submarine canyon refers to a steep-sided valley cut into the sea floor of the continental slope. It is formed through turbidity currents that carve out the submarine canyons in the continental shelf.
V-shaped valleys in the continental shelf and slope are called submarine canyons. These are deep, steep-sided valleys that cut across the continental margin and are often formed by underwater processes such as turbidity currents or erosion by underwater currents. Submarine canyons can be comparable in scale to canyons found on land.
Submarine canyons. These are steep-sided valleys that cut into the continental slope and sometimes extend onto the continental shelf. Submarine canyons can be formed by various processes, including erosion from turbidity currents or underwater landslides.