Flat Features Of The Deep Ocean Floor

What was discovered was a large chain of mountains along the deep seafloor called mid ocean ridges.

Flat features of the deep ocean floor. Deep ocean water is divided into layers or zones each with typical features of salinity pressure temperature and marine life according to their depth. Finally large flat areas called abyssal plains we. The shifting plates may collide converge move away diverge or slide past transform each other. Many ocean floor features are a result of the interactions that occur at the edges of these plates.

Deep ocean basins deep ocean basins situated between the continen tal margins and oceanic ridges are abyssal plains parts of these regions consist of incredibly flat features deep ocean trenches ocean floor also contains extremely deep depressions seamounts dotting the ocean floor are submerged volcanic structure oceanic ridges oceanic ridge mid. Lying along the top of the abyssal plain is the abyssal zone whose lower boundary lies at about 6 000 m 20 000 ft. Scientists also discovered deep sea trenches along the edges of continents or in the sea near chains of active volcanoes. As plates converge one plate may move under the other causing earthquakes forming volcanoes or creating deep ocean trenches.

They are among the flattest smoothest and least explored regions on earth. Even scientist were amazed that the seafloor was not completely flat.