The Two Major Regions Of The Ocean Floor

Two major regions of the ocean floor the ocean floor has two major regions.

The two major regions of the ocean floor.

This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. Located principally in two major zones circum pacific belt region surrounding the pacific ocean includes the mountains of the western americas and continues into the western pacific in the form of volcanic islands other major mountainous belt extends eastward from the alps through iran and the himalayas and then dips southward into. One region the continental margin is the edge of the continent that is covered by ocean water. How does the topography of the ocean floor compare to that on land.

The ocean floor or seabed can be divided into three major regions. Shields expansive flat regions composed of mostly igneous and metamorphic rocks stable platforms very deformed rocks are covered by a thin layer of sedimentary rocks 1 9 what are the three major regions of the ocean floor and what are some features associated with each. The ocean floor regions are the continental margins the ocean basin floor and the mid ocean ridge. The world ocean can be divided into four main ocean basins the pacific ocean the atlantic ocean the indian ocean and the arctic ocean.

Continental shelf is the shallow portion of the ocean which lies close to the continental margin. The three major regions of the ocean floor is the continental margin the deep ocean basin and the ocean floor. In general the ocean floor can be divided into four major divisions. The two major regions of the ocean floor include the continental margin and the deep ocean basin.

The continental margins abyssal plains and mid ocean ridges. The continental shelf the continental slope and the continental rise are sections of the continental margin based on depth and changes in slope. The other region the deep ocean basin begins at the end of the continental margin and extends under the deepest parts. The following features are shown at example depths to scale though each feature has a considerable range at which it may occur.