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Transversions occur on the transform fault lines between two plates. The motion of transversions is a sliding motion where both the plates are either dextral or sinistral. Dextral is when the plate block farthest from the observer is sliding to the right and sinistral is when the block farthest from the observer is sliding to the left. In this grinding process, the plates are neither constructive or destructive like in converging and diverging plates. Neither plate subducts in a transversion. They merely slide past each other.
A transverse boundary is when two plates collide, causing great amounts of pressure. The plates crumble, and usually get destroyed. This is a very destructive type of boundary. This is also know as a transform boundary, or a sliding boundary- even though this action is the opposite of sliding.
where plates slide past each other and crust is neither made nor destroyed by swethan
Transform boundary is when the plates are sliding past each other: ↑ ↓; Divergent is when plates are sliding away from each other: ← →; and convergent is when plates are sliding towards each other: → ←. Those are the three main plate boundaries.
Many strong earthquakes are caused by plates sliding apart.
they will be destroyed.
Transversions occur on the transform fault lines between two plates. The motion of transversions is a sliding motion where both the plates are either dextral or sinistral. Dextral is when the plate block farthest from the observer is sliding to the right and sinistral is when the block farthest from the observer is sliding to the left. In this grinding process, the plates are neither constructive or destructive like in converging and diverging plates. Neither plate subducts in a transversion. They merely slide past each other.
If you mean tetonic plates, then no, sliding tetonic plates cause earthquakes.
A transverse boundary is when two plates collide, causing great amounts of pressure. The plates crumble, and usually get destroyed. This is a very destructive type of boundary. This is also know as a transform boundary, or a sliding boundary- even though this action is the opposite of sliding.
where plates slide past each other and crust is neither made nor destroyed by swethan
Sliding plates release tension and energy to cause earthquakes.
They are sliding on the worldly 13 plates of all th continent
Transform boundary is when the plates are sliding past each other: ↑ ↓; Divergent is when plates are sliding away from each other: ← →; and convergent is when plates are sliding towards each other: → ←. Those are the three main plate boundaries.
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Many strong earthquakes are caused by plates sliding apart.
The tectonic plates
The worlds tectonic plates slide on the earths mantle.