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A transform boundary occurs when two plates move past each other in opposite directions. When the two plates move its almost always a horizontal movement. When the plates move its a slow scrape against each other which allows energy to build up within the rocks. They eventually shift all the sudden and they release all their energy causing the movements to break or distort the rock. The San Andrea fault is an example of a transform boundary located between the North American plate and pacific plate. But on thing to keep in mind is that a transform boundary is most likely to happen on the ocean floor.

https://www.youtube.com/watch?v=tuKNtQ7Hupg

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A divergent boundary forms when two plates move away from each other. When the plates move apart tension allows for the lithosphere to thin resulting in the asthenophere to melt to the Earths surface where it cools and solidifies. This process is what causes seafloor spreading. A divergent boundaries is most likely going to be found under the ocean. One example of a divergent boundary is between the North American and Eurasian plates.

https://www.youtube.com/watch?v=0bx57pjt4qE

# data[].attributes.body
A convergent boundary forms when two plates move toward each other and collide. Subduction is a one thing that can happen when a convergent boundary forms, its when one plate (more dense plate usually oceanic) slides under another less dense plate (usually a continental plate). Another thing that can happen when a convergent boundary forms is two continental plates meet and push up against each other resulting rocks to buckle. This can be seen where the Indian plate meet the Eurasian plate.

https://www.youtube.com/watch?v=75di2vdSg5U