The place were two plates move past each other is called a transform boundary. This motion does not produce any mountains, but it can create large earthquakes.
Tectonic Plates move by trying to push past each other and by trying to slide past each other.
When plates slide past each other, move toward each other, and move away from each other.
The tectonic plates move divergent when they move away from each other, convergent when they are colliding with each other, and trasform when they slide past each other.
It where to plates rub past each other; move away from each other; or move towards each other.
The three types of plate tectonic boundaries are divergent boundaries, where plates move apart; convergent boundaries, where plates collide; and transform boundaries, where plates slide past each other horizontally.
rift zone
Plates tectonics move past each other at transform boundaries, where two plates slide horizontally past each other. This movement can cause earthquakes as the plates grind against each other. An example of a transform boundary is the San Andreas Fault in California.
When two plates move past each other, a transform fault boundary is formed. This boundary is characterized by horizontal motion, and the friction between the plates causes earthquakes along the fault line.
Plates either move towards each other (convergent plates), away from each other (divergent plates) or slide next to each other (transform plates).
the answer is tension
Tension is the force that causes plates to move sideways past each other. This can cause built up stress that releases suddenly and causes earthquakes.
Plates that move past each other are called transform boundaries. These boundaries are where two tectonic plates slide horizontally past each other, causing earthquakes. An example of a transform boundary is the San Andreas Fault in California.