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Divergent Plate Boundaries (or How do you make an ocean?)

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Our Earth's lithosphere is broken into 15 different plates that fit together like puzzle pieces. Plates are are large, irregularly shaped slabs of solid rock, which generally  are composed of both continental and oceanic lithosphere.

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How many types of plate boundaries are there?

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How many types of plate boundaries are there?

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There are three main types of plate boundaries, although there are different types within each category. The three main boundaries are, convergent, divergent, and transform.

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There are three different types of convergent boundaries. The three categories they could fall into are: Ocean-Continental with Subduction, Ocean-Ocean with Subduction, and Continental-Continental with no subduction.

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There are only two types of divergent boundaries which includes: Ocean-Ocean (seafloor spreading) and Continental-Continental.

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There is one type of Transform boundary therefore, there is only one name. The two plates, either Oceanic or Continental slide past each other in the same direction at different speeds or in opposite directions

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Two continental plates are pulled apart by convection currents. Magma rise in between the plates, cools, hardens, then sinks forming a valley. The valley eventually becomes a rift valley like the Great Rift Valley in Africa.

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Divergent ~ Ocean-Ocean (seafloor spreading)

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Divergent ~ Ocean-Ocean (seafloor spreading)

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The Convection currents pull both of the ocean plates apart. Hot, less dense magma rises in the middle, cools and hardens, pushing the old seafloor out. This plate boundary forms Mid-Ocean Ridges, in which you can find in the middle of the Atlantic Ocean.

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Convergent ~ Continental-Continental with no subduction

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Convergent ~ Continental-Continental with no subduction

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Convection currents cause 2 continental plates to move towards each other. Both plates are the same density, therefore no subduction occurs, the two plates crumble together. The two plates that crumble together create mountains in which we see at the Himalayan mountains.

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Convergent ~  Ocean-Continental with subduction

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Convergent ~  Ocean-Continental with subduction

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These two plates are moving towards each other, in which can create land forms such as mountains, volcanoes, and ocean trenches. Convection currents cause denser ocean plates to dive under a continental plate, the ocean plate melts, forming magma and when the magma rises it causes volcanoes. This type of of boundary exist at the Andes Mountains.

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Convergent ~ Ocean-Ocean with subduction

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Convergent ~ Ocean-Ocean with subduction

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This type of boundary exist at the Aleutian Islands. Convection currents cause 2 ocean plates to move towards each other. The plate is that always older, colder, and more dense, is the plate that dives under. (subduction)