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A divergent boundary forms when tow tectonic plates move away from each other. New lithosphere is formed at divergent boundaries while old lithosphere is destroyed in parts where subduction happens and it eventually melts.

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Volcano: volcanoes can form on a convergent boundary: as the oceanic lithosphere sinks, it hits higher temperatures and starts to melt, this magma rises up to the Earth's surface.

Trenches: trenches can occur when a plate subducts beneath another

Rifts: rifts form along divergent boundaries, occurs when Earth's lithosphere pulls apart to form narrow valleys. Eventually, rifts will become a new divergent boundary.

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lithosphere: outermost physical layer of Earth's crust, rigid and solid layer made of rock

asthenosphere: solid layer made of rock although the rock is weak and flows slowly

tectonic plates: large moving pieces of the lithosphere

continental: parts of the lithosphere that contain land mass (continents, duh)

oceanic: parts of the lithosphere that contain water (oceans)

compression: a stress that squeezes or shortens material

tension: a stress that lengthens a material or pulls a material apart

sheer stress: causes material to twist or become distorted

deformation: the bending, tilting, or breaking of rock

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A transform boundary is a boundary formed when two tectonic plates move parallel to each other and touch sides. The plates then shift suddenly, releasing energy.

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This video goes in depth with transform boundaries. It provides examples and shows how they have affected the past.

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-most transform boundaries are found on the ocean floor although the San Andreas fault in found on land in California.

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This video shows a divergent boundary and gives information regarding the topic.

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-most divergent boundaries are below the ocean

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A convergent boundary is a boundary formed when two tectonic plates move towards each other and collide.

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This video shows a convergent boundary

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subduction: the process of one plate sinking below another (seen in the photo below; oceanic lithosphere)
-denser plate sinks below less-dense plate (oceanic-oceanic)
-in a continental-continental convergent boundary, the two plates collide and buckle

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got you