The type of tectonic plates grind past each other are Transform plates Option(c) is correct.
Plate tectonics from the Ancient is the for the most part acknowledged logical hypothesis that considers the Earth's lithosphere to involve various huge structural plates which have been gradually moving since around 3.4 a long time back.
Structural plates are made out of the maritime lithosphere and the thicker mainland lithosphere, each beat by its own sort of covering. Along joined limits, the course of subduction, or one plate moving under another, conveys the edge of the lower one down into the mantle; the area of material lost is adjusted by the development of new (maritime) hull along unique edges via ocean bottom spreading.
Structural plates can move since Earth's lithosphere has more prominent mechanical strength than the hidden asthenosphere. Sidelong thickness varieties in the mantle bring about convection; that is, the sluggish crawling movement of Earth's strong mantle.
Therefore Option(c) is correct.
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