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Convergent boundaries are boundaries that form when two tectonic plates collide or converge on each other. Subduction can also occur at these boundaries where one plate slides beneath the other. When an oceanic plate collides with a continental plate, the dense oceanic plate will be pushed below the less dense continental plate (subduction). When a continental plate collides with another continental plate, they push up against each other forming mountains. When two oceanic plates collide, one will sink beneath the other. Click on the picture for a better view.

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DIvergent boundaries are boundaries that occur when tectonic plates move away from each other or diverge. Rifts are created when these plates diverge. Magma starts to rise and it cools forming new lithosphere. Seafloor spreading is a form of divergent boundaries. As said earlier, the magma rises and forms new seafloor pushing the older seafloor away. Rifts appear when continental plates diverge. They split apart causing rifts to appear.

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Click on the link to watch.

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

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Transform boundaries are boundaries that occur when two tectonic plates slide past one another in opposite directions. When the plates shift, they slowly scrape each other causing energy to build up. Then they suddenly shift causing the energy to be released. These movements break and distort rock.