Parts of the ocean sea floor are:
There could be a trench like the Mariana Trench, a mountain range like the Mid Atlantic Ridge. Also the Mid Atlantic Ridge is a divergent plate boundary where plates are moving away and widening the Atlantic Ocean.
Pacific, Indian, Atlantic, Arctic, And Antarctic.
actually there are many parts of ocean basin but there are 3 major parts namely the;
continental slope
continental shelf
and ocean floor
An ocean basin geologically are land forms and large basins that are below sea level. Some ocean basins do not fit this criteria and are just basins that are in salt water.
trench
In ocean basins
Ocean basins are primarily made of the igneous rock, basalt.
Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins.
Hydrologically, an oceanic basin may be anywhere on Earth that is covered by seawater, but geologicallyocean basins are large geologic basins that are below sea level. Geologically, there are other underseageomorphological features such as the continental shelves, the deep ocean trenches, and the underseamountain ranges (for example, the mid-Atlantic ridge) which are not considered to be part of the ocean basins; while hydrologically, oceanic basins include the flanking continental shelves and shallow, epeiric seas.
continental margins and ocean basins
In ocean basins
In ocean basins
No, Ocean basins form when land drifts away, for example "Pangea" (north america,Europe,Asia&Africa) were once together & now, are not, theirfor ocean basins were created
Ocean basins are primarily made of the igneous rock, basalt.
under the earth start to overlap one another causing things in the ocean called basins to occur which is where ocean basins comes from.
the earth.
Drilling.
the earth.
crust
Yes. Wind Belts, The Coriolis Effect, and the Position of the Continents all influence the ocean basins patterns
Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins.
Oceanic crust is the part of Earth's lithosphere that surfaces in the ocean basins.