Depth Of Atlantic Ocean Floor

The average depth of the ocean with adjacent seas is 10 932 ft 3 332 m.

Depth of atlantic ocean floor.

The wreck of the rms titanic lies at a depth of about 12 500 feet 3 8 km. This depth which varies with latitude and water temperature is known as the carbonate compensation depth or ccd. The outstanding feature of the atlantic floor is the mid atlantic ridge an immense median mountain range extending throughout the length of the atlantic claiming the centre third of the ocean bed and reaching roughly 1 000 miles 1 600 km in breadth. In the south atlantic the greatest depth is 27 651 ft 8 428 m at the south sandwich trench east of the falkland islands.

It covers approximately 20 percent of earth s surface and about 29 percent of its water surface area. It separates the old world from the new world the atlantic ocean occupies an elongated s shaped basin extending longitudinally between europe and africa to the east. The puerto rico trench has a maximum depth of no more than 8 376 metres 27 480 ft as measured to be the deepest point in the atlantic ocean by vescovo during his descent. This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level.

The atlantic ocean is the second largest of the world s oceans with an area of about 106 460 000 km 2 41 100 000 sq mi. Previously however the depth of the milwaukee deep when being used to refer to the atlantic s deepest point had been reported by various sources as 8 710 metres 28 580. Detailed depth contours provide the size shape and distribution of underwater features. Continental shelf 300 feet continental slope 300 10 000 feet abyssal plain 10 000 feet abyssal hill 3 000 feet up from the abyssal plain seamount 6 000 feet.

The following features are shown at example depths to scale though each feature has a considerable range at which it may occur. 2 37 mi about 370 miles 600 km south southeast off the coast of newfoundland it lies in two main pieces about a third of a mile 600 m apart. The map serves as a tool for performing scientific engineering marine geophysical and environmental studies that are required in the development of energy and marine resources. The problem with that approach is that our oceans are vast and ships are small meaning only a tiny percentage of the ocean floor between 5 15 percent nasa estimates was mapped.

As a result carbonate oozes are absent from the deepest parts of the ocean deeper than 4 000 m but they are common in shallower areas such as the mid atlantic ridge the east pacific rise west of south america along the.