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In this video by Geoscience videos, it uses real life photos to show how transform boundaries work today! By annotating and narrating you are able to get a good idea on how transform boundaries are in motion!

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This video by Khan Academy shows and goes in depth on how the convergent boundaries occur. The drawings, narration, and photos help you to understand how all of them occur.

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Plate Tectonics-- Geological features of Convergent Plate Boundaries

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In this video by Khan Academy, it describes and explains how divergent boundaries work. It shows the effects and how they work. This is all shown through pictures and drawings with audio narrating.

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Plate tectonics: Geological features of divergent plate boundaries | Khan Academy

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These plates slide past each-other and rub together. These make faults and Earthquakes. This occurs in the San Andreas Fault.

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This plate boundary occurs when 2 continental plates of the same density collide and crumble up. This forms mountains and Earthquakes can occur. This is occuring in the Himalayan Mountains.

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In this boundary, the older, colder, and denser ocean plate dives under. As in subduction, the ocean plate melts down to form underwater volcanoes. These volcanoes can form islands. This is shown in the Aleutian Islands.

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Here, there is a ocean and a continental plate. The ocean plate dives under the continental plate because it is more dense. The ocean plate melts down to form volcanoes. This occurs in the Andes Mountains.

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This plate boundary occurs when convection currents pull apart 2 oceanic plates. Magma rises and makes new seafloor. This is shown in the Mid-Atlantic Ridge.

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In this plate boundary, 2 continental plates pull apart due to convection currents. This results in magma rising in the center forming a volcano. An example of this is the Great Rift Valley in Africa.