What are the two major regions of land under the water?

What are the two major regions of land under the water?

Two major regions of the ocean floor are the continental margin and the deep-ocean basin.

What are the 2 major provinces of the ocean floor?

The pelagic zone is divided into two provinces: the neritic province corresponds to all of the water from the low tide line to the shelf break, while the oceanic province represents all of the other water in the open ocean regions.

What are the two divisions of the ocean floor?

In general, the ocean floor can be divided into four major divisions: 1. Continental Shelf 2. Continental Slope 3. Continental Rise 4.

What are the 3 major ocean floor provinces?

Physiography and bathymetry (submarine landscape) allow the sea floor to be subdivided into three distinct provinces: (1) continental margins, (2) deep ocean basins and (3) mid-oceanic ridges.

What are the two major regions of the ocean floor?

Two Major Regions of the Ocean Floor The ocean floor has two major regions. One region, the continental margin,is the edge of the continent that is covered by ocean water. The other region, the deep-ocean basin,begins at the end of the continental margin and extends under the deepest parts of the ocean.

Which is an example of an underwater body of water?

(October 2011) Underwater refers to the region below the surface of water where the water exists in a swimming pool or a natural feature (called a body of water) such as an ocean, sea, lake, pond, or river.

What kind of currents are under the surface of the ocean?

Thermohaline circulation is also known as the ocean’s conveyor belt (which refers to deep ocean density driven ocean basin currents). These currents, called submarine rivers, flow under the surface of the ocean and are hidden from immediate detection.

Which is the flattest part of the ocean?

The large, flat, almost level area of the deep-ocean basin is called the abyssal plain. Abyssal plains are the flattest regions on Earth. They are covered with layers of fine sediment. Wind and ocean currents carry some of this sediment from the continental margins. Other sediment is made of the remains of marine organisms.

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