Ocean Basins: Definition, Formation, Features & Types

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  • 0:08 Ocean Basins
  • 0:44 Types and Formation
  • 2:07 Ocean Basin Features
  • 4:00 Oceanic Trenches
  • 4:51 Lesson Summary
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Lesson Transcript
Instructor: Rebecca Gillaspy

Dr. Gillaspy has taught health science at University of Phoenix and Ashford University and has a degree from Palmer College of Chiropractic.

Ocean basins are those areas found under the sea. They can be relatively inactive areas where deposits of sediment slowly collect or active areas where tectonic plates meet. Learn how ocean basins form and about features such as oceanic ridges and trenches.

Ocean Basins

About 70% of the planet's surface is made up of ocean basins, which are the regions that are below sea level. These areas hold the majority of the planet's water. In fact, it will help you to recall this term if you remember that a 'basin' is a large bowl, much like your kitchen sink. So, an ocean basin can be thought of as a large bowl that holds ocean water. The floors of our world's oceans contain features that you might recognize as being similar to some structures on land. In this lesson, you will learn about these features, including undersea mountains and trenches and how they are formed.

Ocean Basin Types and Formation

Ocean basins can be either active, with a lot of new structures being created and shaped, or they can be inactive, where their surface is slow to change and does little more than collect sediment. The Gulf of Mexico is an example of an inactive ocean basin where the main change that happens is the slow depositing of sand and sediment.

Active ocean basins undergo change mainly due to plate tectonics. Plate tectonics is the theory used to explain the dynamics of the earth's surface resulting from the interaction of the overlying rigid plates with the underlying mantle. According to the theory, the earth has a rigid outer layer called the crust. This crust is somewhat fragile, and like the shell of a hard-boiled egg, it can crack and break into plates. The earth's crust breaks due to heat and pressure from the layer beneath the crust, called the mantle.

These plates move very slowly and meet at their boundaries. These boundaries are common areas of tectonic activity, which is the deformation of the earth's crust due to movement of tectonic plates resulting in activity (such as earthquakes, volcanoes and mountain building). So, an area of the world that is tectonically active, whether it be on land or under the water, would be a mountainous area with earthquakes and volcanic activity. This creates many of the ocean basins features.

Ocean Basin Features

Plates can spread apart by moving away from each other. This creates gaps where hot molten rock, called magma, from the earth's mantle can rise up. When the magma seeps through the gaps, it solidifies as it cools, creating a new layer of ocean crust. This creates structures, such as oceanic ridges, which are continuous mountain chains located under the surface of the sea.

You can think of their creation in much the same way as a scab gets created over a wound. For example, when you cut your finger, it bleeds. The blood flowing out of the cut relates to the magma flowing out of the gap between the spreading plates. The cut will form a raised scab on your finger, and as the magma cools, it will form a raised layer of crust on the sea floor.

An abyssal hill is another raised feature found within ocean basins. It is defined as a small elevated landform that rises from the great depths of the ocean. It might help you to recall this term by remembering that an 'abyss' is something that is very deep. So an abyssal hill is a hill found on the deep ocean floor. An abyssal hill has sharply-defined edges but will remain relatively small, generally growing not much larger than 500 feet in height and a few miles in width.

A seamount is a large submerged volcanic mountain rising from the ocean floor. Seamounts can be very large, reaching heights of up to 10,000 feet, yet they remain submerged under the surface of the water.

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