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Go visit Samatar Ali Petroleum Engineer's videosfor me

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Plate Boundaries  Convergent, Divergent, and Transform Boundaries 2

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A Transform Plate Boundary occurs when 2 Tectonic plates slide past each other creating fault lines. An example of this is the San Francisco Fault Line. Magma doesn't fill the gap in between the plates.

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Convergent Plate Boundary without Subduction

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Convergent Plate Boundary without Subduction

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A Convergent Plate Boundary without subduction is where 2 tectonic plates are pushed together and they fold together which creates mountain ranges. An example of this is the Himalayan Mountains which is caused by the Indian Plate colliding into the Eurasian Plate

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Convergent Plate Boundary with Subduction

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Convergent Plate Boundary with Subduction

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A Convergent Plate Boundary with subduction is where 2 tectonic plates are pushed together and one sinks below the other. When this occurs it is usually dense, Oceanic crust being shoved under less dense, Continental crust. Volcanoes form because of the sinking plate being melted

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A Divergent Plate Boundary is where 2 tectonic plates are pushed apart by magma that is being forced up by convection currents. An example of this is the Mid-Atlantic ridge, which runs down through Iceland and the middle of the Atlantic ocean.