The flat area of ocean floor covered in mud, sand, and plant and animal remains is known as the continental shelf. This area extends from the shoreline to the beginning of the steeper continental slope and is characterized by relatively shallow waters. The sediments found on the continental shelf provide important habitats for marine organisms and play a crucial role in nutrient cycling.
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.
Approximately 2.5% of the ocean bottom is covered by trenches, which are deep depressions in the ocean floor that form where tectonic plates collide and one plate is forced beneath the other. These trenches can be incredibly deep, with the Mariana Trench being the deepest known point in the ocean.
A seamount forms through volcanic activity, where magma rises from beneath the Earth's crust to create a mountain-like structure on the ocean floor. Over time, as the volcano becomes inactive and cools, it sinks below the ocean surface but remains as a seamount.
Abyssal plain. Abyssal plains are flat, sediment-covered areas of the ocean floor that lie between the continental margins and oceanic ridge systems. They are typically found at depths of 4 to 6 km below sea level.
A crustal shift in the ocean floor can trigger underwater disturbances like tsunamis or underwater landslides, which can cause significant damage to coastal wildlife habitats on land. These events can lead to flooding, destruction of habitats, and displacement of plant and animal species, impacting the overall ecosystem health.
its covered with rock and stones
Ooze on the ocean floor is formed from the remains of marine organisms like phytoplankton and zooplankton, as well as shells and skeletons of marine animals. Over time, these organic materials accumulate and form sediment on the ocean floor.
dead organisms A+
Trilobites
Sexual coment
It is believed that old rocks are rare on ocean floors bevause the floor has manny remains and we are not unable to reach them
The ocean floor is located on the Earth's outermost layer called the crust. It is part of the crust that is covered by water, forming the ocean basins.
Biogenous are dominant on deep-ocean floors.
The relationship between the existence of the plume influence and ocean floor topography.
mid ocean ridge
Oil is a concentrated by-product from the decay of ancient plant and animal remains on the ocean floor and is considered a natural resource but not a mineral. Coal deposits are composed of the remains of mostly plant life that has undergone sedimentation and lithification. It is not considered a mineral, but a sedimentary rock.
They both come from the ocean floor? That and it probably has to do with both allowing some type of plant or animal life to survive on the ocean floor.