Ocean Floor Features

Many ocean floor features are a result of the interactions that occur at the edges of these plates.

Ocean floor features. Because of the extreme pressure these fish have evolved a gelatinous texture of flesh with a density slightly less than sea water. The ocean floor is populated by bottom feeders that look somewhat like blobs. As plates converge one plate may move under the other causing earthquakes forming volcanoes or creating deep ocean trenches. The ocean floor is called the abyssal plain.

Features of the ocean include the continental shelf slope and rise. This video examines the different types of features in the ocean primarily on the ocean floor. Mid ocean ridge underwater on the sea floor that are made up of magma and run all around the ocean. In other parts of the ocean floor you ll find king.

Features rising up from the ocean floor include seamounts volcanic islands and the mid oceanic ridges and rises. This video examines the different types of features in the ocean primarily on the ocean floor. The blobfish first discovered off the coast of australia is an example. In the atlantic ocean thick layers of undisturbed sediment cover the continental margin.

Below the ocean floor there are a few small deeper areas called ocean trenches. On the sea floor made up of rocks minerals sediments and sand a steep cliff like slope increases water pressure and is where the continent connects with the ocean floor. Continental shelf continental slope and rise mid oceanic ridge ocean trench and abyssal plain. What are three obstacles to studying the seafloor.

A bathymetric profile cross section of a major ocean basin like the pacific ocean shows the typical features of the seafloor. Three quarters of the earth consists of ocean water. Submarine sediments are of two main types. The zone between the continent and the adjacent ocean basin floor is the continental margin.

Science has established that the topography of the ocean floor is similar to the ground topography with features such as valleys mountains and plateaus. All these details are incorporated on underwater topography maps. The features of the ocean floor are covered by a layer of sediments the thickness of which depends on the age of the feature the local topography and on the abundance of the sediment sup ply. Continental margin and oceanic divisions.

The shifting plates may collide converge move away diverge or slide past transform each other.