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Two tectonic plates move past each other moving in opposition directions which would form a transform boundary. The movement is usually horizontal. Shear stress is common at this kind of boundary. They scrape against each other, which causes energy to build. Then. they suddenly shift, releasing energy. These movements break or distort rock. https://www.youtube.com/watch?v=tuKNtQ7Hupg

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When two tectonic plates diverge from each other, it's a divergent boundary. As they move apart, tension occurs. This causes the lithosphere to become thinner. This allows the asthenosphere to rise to Earth's surface and melt. The melting produces magma, which moves to the surface and solidifies. This process forms new lithosphere at divergent boundaries. This does not mean that the lithosphere gets bigger however. The old lithosphere is destroyed in subduction zones at convergent boundaries when one plate sinks below the other and melts. https://www.youtube.com/watch?v=aTE49IOsFJ4

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Convergent Boundaries form when two tectonic plates collide with each other. These collisions can have different kinds of plates. For example, if a oceanic plate and continental plate were to collide with each other, the denser oceanic plate would sinks below the less dense continental plate. If two continental plates were to meet. The two plates would push up against each other and the compression causes the rocks to buckle. If two oceanic plates were to meet, where subduction would occur. The densest of the two oceanic plates would sink under the less dense oceanic plate. https://www.youtube.com/watch?v=75di2vdSg5U