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In Conclusion

Divergent, Convergent, and Transform plate boundaries are the three types of plate

movement theories that explain natural disasters like earthquakes, tsunamis, and volcanic

eruptions. The movements of each plate boundary can be away from each other causing a

separation, or continental drift; the plates can move parallel to each other and also move across

the plates. The theories involving plate tectonics and continental drift include a magnetic like

structure along the Earth’s crust or each continent has an anchor like structure that slowly pulls

the continents away from each other

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What is Transform plate boundaries base on searching on Google/books

A transform fault or transform boundary, sometimes called a strike-slip boundary, is a fault along a plate boundary where the motion is predominantly horizontal.

It ends abruptly where it connects to another plate boundary, either another transform, a spreading ridge, or a subduction zone.

A transform fault is a special case of a strike-slip fault that also forms a plate boundary

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What is divergent plate boundaries base on searching on Google/books

In plate tectonic, a divergent boundary or divergent plate boundary(also known as a constructive boundary or an extensional boundary) is a linear feature that exists between two tectonic plates  that are moving away from each other.

Divergent boundaries within continents initially produce rifts, which eventually become rift Valleys.

Most active divergent plate boundaries occur between oceanic plates and exist

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What is convergent plate boundaries base on searching on Google/books

A convergent boundary is an area on Earth where two or more lithospheric plates collide.

One plate eventually slide beneath the other, a process known as subduction.

The subduction zone can be defined by plane where many earthquake occur, called Wadati-Benioff zone.

These collision happen on scales of millions to tens of millions of year and can lead to volcanism, earthquakes, orogenesis, destruction of lithosphere, and deformation.

Convergent boundaries occur between oceanic-oceanic lithosphere , oceanic-continental lithosphere, and continental-continental lithosphere. The geologic features related to convergent boundaries vary depending on crust types.