Mid ocean ridge mountain range on the ocean floor where magma upwells and new ocean floor is formed.
Large flat bottom ocean floor that is completely dark.
The sloped bottom of the ocean that extends from the continental shelf down to the deep ocean bottom.
Seamount a mountain rising from the seafloor that does not reach above the surface of the water.
However winds and gravity actually cause sea level differences around the world.
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Abyssal plains are larger in the atlantic ocean than they are in the pacific.
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This can happen because of infaunal worms who mix the sediments.
In fact it has been said that we know more about the surface of the moon than about the deeper ocean trenches.
We know very little about the deep ocean floor and the life it holds due to the depth and the difficulties this creates for scientists.
The ocean floor covers 70 of the earth s surface.
The abyssal plains of the ocean are some of the deepest parts.
These are large flat areas on the ocean floor covered with a thick layer of sediment and decomposing organic ooze.
Usually formed from volcanoes.
The abyssal plains are very level very large areas of the ocean floor that stretch from the continental rise to the mid ocean ridges.
Staring out at the ocean from a beach it might be easy to imagine that the world s seas are completely flat.
The reason for this is that many of the world s major sediment carrying rivers empty into the atlantic and indian oceans.
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Marine life can change the bottom of the ocean.
The walls represent 4 sides of the room so the paint color you choose has a much bigger impact on how large or small your space looks.
Tubes created in the bottom of the ocean can be used by animals like anemones and worms to draw water with dissolved oxygen below the surface.
A large flat area on the ocean floor composed of sediments that originated mostly on the continents.
Some species especially worms cement the sediments together making very hard tubes.
Here are 15 crazy facts about the ocean floor.
Also called oceanic trench any long narrow steep sided depression in the ocean bottom where maximum oceanic depths occur.