The most shallow part is the near-shore zone.
The two major regions of land under the water are the continental shelf, which is the relatively shallow area surrounding continents, and the ocean basins, which are deeper areas beyond the continental shelf that make up most of the ocean floor.
Conglomerate rock is most likely formed from pebble-sized sediment deposited in shallow water at an ocean shoreline. The pebbles are typically rounded due to erosion in water, and they can become cemented together to form the conglomerate rock.
As it turns out, most of the ocean floor is basalt, and most of the continents are granite.
the ocean
Ocean water is warmed most by the sun in the tropics, particularly in regions close to the equator. Areas like the Caribbean Sea and the western Pacific Ocean experience higher temperatures due to direct sunlight year-round. Additionally, shallow coastal regions can heat up more quickly than deeper waters, contributing to localized warming.
Coral reefs are found in salt water, on the ocean floor. Most often they are found in warm, shallow water.
It depends on how deep the bottom is. Coral can only survive in relatively shallow water, so most of the ocean floor is coral free.
Because ocean plants need sunlight, most are either designed to float on the surface of the water, or grow on the ocean floor in water that is shallow enough to receive adequate sunlight. They also have adapted to salty water. Some are: kelp, seaweed. seagrass and algae.
Most landmasses lie on what is known as 'the continetal shelf' - a region of relatively shallow water extending up to some hundred of kilometres off the coast. This gives way, either gradually or suddenly, to the true ocean floor.
The two major regions of land under the water are the continental shelf, which is the relatively shallow area surrounding continents, and the ocean basins, which are deeper areas beyond the continental shelf that make up most of the ocean floor.
Biogenous are dominant on deep-ocean floors.
Most of the ocean floor is made up of ocean plains.
Conglomerate rock is most likely formed from pebble-sized sediment deposited in shallow water at an ocean shoreline. The pebbles are typically rounded due to erosion in water, and they can become cemented together to form the conglomerate rock.
Most plants and animals live in the Sunlit Zone.
Conglomerate rock is most likely formed from pebble-sized sediment deposited in shallow water at an ocean shoreline. As the pebbles accumulate, they cement together to form the rock.
Because Most Energy is EXCHANGED at the surface!
The ocean floor is the most anaerobic zone in the ocean.