This zone is divided further into three subzones.
The ocean floor is which ocean zone.
This heat is responsible for the wide range of temperatures that occur in this zone.
Epipelagic zone the surface layer of the ocean is known as the epipelagic zone and extends from the surface to 200 meters 656 feet.
Most animals living in the open ocean live in the sunlit zone.
The hadalpelagic zone lies between 19 686 feet to 36 100 feet.
The deep zone is also known as.
The sunlit zone is where photosynthesis takes place.
The hadalpelagic zone is also called the trenches and is found from the ocean basin and below.
The abyss because it is a zone of complete darkness no sunlight enters at all.
Shallow area of ocean floor that extends from continents.
It is also known as the sunlight zone because this is where most of the visible light exists.
The area of the ocean beyond the continental shelf that includes the water column and the deepest darkest parts of the ocean deep zone from 1 km to the ocean floor this layer of the water column is the darkest coldest and harshest.
Ocean zone that includes all of the ocean floor deep and shallow parts continental shelf.
Ocean zone with no light very cold water and high pressure.
Plankton and jellyfish are drifters that inhabit this zone.
Scientists basically divide the ocean depths into 5 main layers of the ocean or ocean zones which extend from the surface to very deep we re talking 36 000 feet which is more than a mile deeper than mount everest is tall.
Japan s marina trench is the deepest part of the ocean ever to be explored by man and it sits at 35 797 feet.
Below the sunlit zone is the twilight zone where some light penetrates the ocean to a depth of 3000 feet.
A gently sloping shallow area of the ocean floor that extends outward from the edge of a continent.
An abyssal plain is an underwater plain on the deep ocean floor usually found lying between the foot of a continental rise and a mid ocean ridge.
With the light come heat.
The depth depends on the trenches and valleys in the area.
Area where ocean water heated by magma rises through cracks in the ocean floor.