From the creation of crust by magma at divergent plate boundaries. It has been proposed that when the above crust is created, it creates in the form of an upward pointing wedge of basalt and this wedge forces the plates apart. For a more extensive discussion of this proposal see http://members.tripod.com/~charles_W/ridge.html
Yes, but no with each other. They can meet other plates.
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.
If two plates crashed into each other two possible things can happen: 1 The plates bump into each other and can cause an earthquake. 2 The plates crash, then they go upwards to form a mountain or a volcano. ~Doraexplorer
The three types of crustal plate movements are convergent (plates move towards each other), divergent (plates move away from each other), and transform (plates slide past each other horizontally). These movements are driven by the interactions of tectonic plates at plate boundaries.
Tectonic Plates move by trying to push past each other and by trying to slide past each other.
A convergent boundary is when two plates collide with each other forming landforms like trenches, or mountains (depends which type of plates converge.)
Yes, but no with each other. They can meet other plates.
When plates slide past each other, move toward each other, and move away from each other.
Plates either move towards each other (convergent plates), away from each other (divergent plates) or slide next to each other (transform plates).
The three types of Earth's plates are convergent plates, where two plates move towards each other; divergent plates, where two plates move away from each other; and transform plates, where two plates slide past each other horizontally.
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.
If two plates crashed into each other two possible things can happen: 1 The plates bump into each other and can cause an earthquake. 2 The plates crash, then they go upwards to form a mountain or a volcano. ~Doraexplorer
The three types of crustal plate movements are convergent (plates move towards each other), divergent (plates move away from each other), and transform (plates slide past each other horizontally). These movements are driven by the interactions of tectonic plates at plate boundaries.
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.
Tectonic Plates move by trying to push past each other and by trying to slide past each other.
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.
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.