I have no idea, have a good day
Sediment left after weathering and erosion can be found in a variety of places such as riverbeds, beaches, deltas, and the ocean floor. It can also accumulate in valleys, lakes, and areas where wind deposition occurs.
When sediment sinks into the ocean floor, it is called sedimentation. Over time, layers of sediment build up and compress to form sedimentary rocks.
The top layer of the ocean floor is called the "abyssal zone" or "abyssal plain." This region is characterized by flat, sediment-covered areas that lie below the continental shelf. The abyssal zone is the deepest part of the ocean floor and is typically found at depths greater than 4,000 meters.
The ocean floor is primarily made up of basaltic rock, which is formed from solidified lava from volcanic activity. It also contains sediment such as sand, mud, and organic material that has accumulated over time.
turbidity currents, which are fast-moving underwater currents that carry sediment down into the deep ocean basins. These currents can transport large volumes of sediment over long distances before depositing them on the ocean floor.
No, due to plate shifting, earthquakes, volcanoes, erosion, and sediment settling it will most definitely be very different in a million years.
Sediment left after weathering and erosion can be found in a variety of places such as riverbeds, beaches, deltas, and the ocean floor. It can also accumulate in valleys, lakes, and areas where wind deposition occurs.
Lithogenous sediment is made up of fragments of rocks and minerals that have been eroded and transported by various geological processes before settling on the ocean floor. These sediments typically originate from continental sources and can include materials such as quartz, feldspar, and clay minerals. Lithogenous sediment forms a significant component of marine sedimentary deposits.
When sediment sinks into the ocean floor, it is called sedimentation. Over time, layers of sediment build up and compress to form sedimentary rocks.
Large flat areas of the ocean floor are called abyssal plains. These regions are typically covered in thick layers of fine sediment and are among the flattest, most featureless parts of the ocean floor. Abyssal plains are found at depths between 3,000 and 6,000 meters.
broken up rocks
the thickest accumulation of sediment on the ocean floor is at the CONTINENTAL SLOPES AND RISES. :)
Biogenous
i just dont know !
Fine sediments can reach the ocean floor through various ways, such as river runoff carrying sediment from land, currents transporting sediments offshore, and particles settling from the water column. Once these fine sediments reach the ocean floor, they can accumulate over time to form sediment layers.
Large areas of sea floor are covered with thick layers of sediment containing calcium due to the accumulation of calcium carbonate shells and skeletons from marine organisms over time. This process, known as biomineralization, contributes to the formation of limestone and other calcium-rich sediments.
The midwest was once an inland sea. Over time organic sediment that sunk to the bottom of the sea created a uniformly flat surface on the sea floor. When the sea dried the sediment was left uniformly flat.