Different Parts Of The Ocean Floor

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.

Different parts of the ocean floor.

The layers range from the surface layer where most ocean activities occur to the deep dark depths of the water that have yet to be fully explored. There are four parts of the ocean floor. The continental shelf is the part of the ocean floor that is a long plain beginning at the shore line which stretches towards the ocean. The deepest parts of the ocean floor are caused by plate tectonic subduction and occur where the sea floor sinks back into the mantle in a subduction zone.

Organisation with a mandate to map the entire ocean floor. In other parts of the ocean floor you ll find king crabs and flounders. The four parts are the continental shelf continental slope continental rise and the abyssal plains. Deep ocean drilling and radiometric dating in the late 1960s gave an accurate stratigraphy and precise date of the ocean floor.

Start studying parts of the ocean floor. Close to shore coral forests are. The following features are shown at example depths to scale though each feature has a considerable range at which it may occur. The ocean has 5 different and distinct layers that each have their own unique characteristics.

Shelves can be found around most continents. The deep layers have unique sea creatures freezing temperatures and high pressure. This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. The mariana trench the world s deepest submarine de pression is more than 11 000m below sea level in some parts about 7 000m below the mean depth of the ocean floor.

And if you want to understand precisely how sea levels will rise in different parts of the world good ocean floor maps are a must. From studying the oxygen isotopes of the shells of microfossils in these cores scientists were able to begin studying the earth s past climates in a study known as paleoclimatology.