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As a final observation, there are three different types of plate boundaries with different specifications, specifically: Convergent Plate Boundary, Divergent Plate Boundary, and Transform Plate Boundary.
What's more is that there is only one type of plate boundary where subduction is present and that is the Convergent Plate Boundary. The reason why subduction is only present in Convergent Plate Boundary is because subduction talks about collision of plates and collision only exists in convergence.
The occurrence of the three types of plate boundaries forms different kinds of landforms like mountain ranges, volcanoes, valleys, etc.

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A boundary produced when two plates slide past each other.

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Maria Khimberly De Rama:
In this kind of plate boundary, plates are sliding past each other. In addition, subduction is also not present for the reason that the plates are not colliding, however, they are gliding.

Prince Francis Guevarra:
It is a slide-slip motion that causes a fault in the plates of lithospere. It appears when two tectonic plate moves with one another.

King Daryll Abe:
A transform fault boundary forms when oceanic or continental plates slide past one other in opposing directions or move in the same direction but at different speeds. While no new crust is produced, subducted, or formed, and no volcanoes are formed, the fault produces earthquakes.

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A boundary in which two plates move toward each other, causing one of the slabs of the lithosphere to subduct beneath an overriding plate.

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Maria Khimberly De Rama:
In this kind of plate boundary, plates are moving or pushing towards each other. Moreover, subduction occurs in Convergent Plate Boundary because the plates are colliding – one is forced downward (oceanic crust) because of its higher density and one is forced upward (continental crust) because of its buoyancy (less dense).

Prince Francis Guevarra:
It is where two lithosphere collide by moving forward.

King Daryll Abe:
Where two plates collide to produce a subduction zone or other boundary, convergence occurs. The oceanic plate, which is denser, descends into the mantle below to supersede it.

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A region where the crustal plates are moving apart.

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Maria Khimberly De Rama:
In this kind of plate boundary, plates are moving far away from each other. The plates in Divergent Boundary does not subduct since there is no collision existing.

Prince Francis Guevarra:
It is a liniar that exist between two plates moved away from each other.

King Daryll Abe:
When plates move apart, new sea floor forms and rift valleys can be created.