Ocean bottoms are not plain as believed earlier; they reveal many complex and varied features which rival the relief features on land.
The oceans are confined to the great depressions of the earth’s outer layer.
The oceans, unlike the continents, merge so naturally into one another that it is hard to demarcate them.
The geographers have divided the oceanic part of the earth into four oceans, namely the Pacific, the Atlantic, the Indian and the Arctic.
The various seas, bays, gulfs and other inlets are parts of these four large oceans. A major portion of the ocean floor is found between 3-6 km below the sea level.
The ‘land’ under the waters of the oceans, that is, the ocean floor exhibits complex and varied features as those observed over the land .
The floors of the oceans are rugged with the world’s largest mountain ranges, deepest trenches and the largest plains.
These features are formed, like those of the continents, by the factors of tectonic, volcanic and depositional processes.
Divisions of the Ocean Floors
The ocean floors can be divided into four major divisions:
(i) the Continental Shelf;
(ii) the Continental Slope;
(iii) the Deep Sea Plain;
(iv) the Oceanic Deeps.
Besides, these divisions there are also major and minor relief features in the ocean floors like ridges, hills, seamounts, guyots, trenches, canyons, etc.
The continental shelf is the extended margin of each continent occupied by relatively shallow seas and gulfs. It is the shallowest part of the ocean showing an average gradient of 1° or even less.
The shelf typically ends at a very steep slope, called the shelf break. The width of the continental shelves vary from one ocean to another.
The average width of continental shelves is about 80 km. The shelves are almost absent or very narrow along some of the margins like the coasts of Chile, the west coast of Sumatra, etc. On the contrary, the Siberian shelf in the Arctic Ocean, the largest in the world, stretches to 1,500 km in width. The depth of the shelves also varies.
It may be as shallow as 30 m in some areas while in some areas it is as deep as 600 m. The continental shelves are covered with variable thicknesses of sediments brought down by rivers, glaciers, wind, from the land and distributed by waves and currents.
Massive sedimentary deposits received over a long time by the continental shelves, become the sourceof fossil fuel
The continental slope connects the continental shelf and the ocean basins.
It begins where the bottom of the continental shelf sharply drops off into a steep slope.
The gradient of the slope region varies between 2-5°. The depth of the slope region varies between 200 and 3,000 m.
The slope boundary indicates the end of the continents. Canyons and trenches are observed in this region.
Deep Sea Plain
Deep sea plains are gently sloping areas of the ocean basins.
These are the flattest and smoothest regions of the world.
The depths vary between 3,000 and 6,000m. These plains are covered with fine-grained sediments like clay and silt.
Oceanic Deeps or Trenches
These areas are the deepest parts of the oceans. The trenches are relatively steep-sided, narrow basins.
They are some 3-5 km deeper than the surrounding ocean floor.
That is why they are very significant in the study of plate movements. As many as 57 deeps have been explored so far; of which 32 are in the Pacific Ocean; 19 in the Atlantic Ocean and 6 in the Indian Ocean.
Minor Relief Features
Apart from the above-mentioned major relief features of the ocean floor, some minor but significant features predominate in different parts of the oceans.
A mid-oceanic ridge is composed of two chains of mountains separated by a large depression.
The mountain ranges can have peaked as high as 2,500 m and some even reach above the ocean’s surface. Iceland, a part of the mid-Atlantic Ridge, is an example.
It is a mountain with pointed summits, rising from the seafloor that does not reach the surface of the ocean. Seamounts are volcanic in origin.
These can be 3,000-4,500 m tall. The Emperor seamount, an extension of the Hawaiian Islands in the Pacific Ocean, is a good example.
These are deep valleys, some comparable to the Grand Canyon of the Colorado River.
They are sometimes found cutting across the continental shelves and slopes, often extending from the mouths of large rivers.
The Hudson Canyon is the best-known submarine canyon in the world.
It is a flat-topped seamount. They show evidence of gradual subsidence through stages to become flat-topped submerged mountains.
It is estimated that more than 10,000 seamounts and guyots exist in the Pacific Ocean alone.
These are low islands found in the tropical oceans consisting of coral reefs surrounding a central depression.
It may be a part of the sea (lagoon), or sometimes form enclosing a body of fresh, brackish, or highly saline water.