The most shallow part is the near-shore zone.
The most shallow end of the water is the Continental Shelf. The most deepest end is the Continental Margin. It is flat and smooth from the bottom.
The Arctic Ocean is most shallow.
continential shelves
conglomerate
sediment on the ocean floor
As it turns out, most of the ocean floor is basalt, and most of the continents are granite.
on the ocean floor
the ocean
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.
Biogenous are dominant on deep-ocean floors.
Most of the ocean floor is made up of ocean plains.
conglomerate
Farther
Most plants and animals live in the Sunlit Zone.
Because Most Energy is EXCHANGED at the surface!
The ocean floor is the most anaerobic zone in the ocean.
The most abundant mineral in the ocean floor is basalt. There are also some other minerals like sand, gravel and granite that are found in the ocean floor.