When two plates slide apart from each other, it is known as divergent boundaries. As the continent splits, a ridge forms at the spreading center, stretches the ocean basin, causing it to expand and the plate area increases causing many small volcanoes or light earthquakes.
A divergent plate boundary, with tensional stress.
they are formed by two tectonic plates pulling away from each other
The place where two tectonic plates move away from each other horizontally are called divergent plate boundaries.
Tectonic movement
When two tectonic plates collide, it is called compressional stress at convergent boundaries. Rocks and plates usually have stronger compressional strength than tensional strength (which would happen at divergent boundaries). This means the higher the likelihood of developing mountains for continent-continent convergence or being subducted for oceanic-oceanic/oceanic-continental boundaries.
convergent
they are formed by two tectonic plates pulling away from each other
they are formed by two tectonic plates pulling away from each other
Divergent Plate Boundary. A Rift Valley forms between the two plates.
Convergent tectonic plates are plates that are moving toward each other.
Fault lines
Continental plates are tectonic plates. They are tectonic plates upon which continents rest, and they move as do all tectonic plates. Basically, there is no difference, other than the fact that oceanic plates are another type of tectonic plate.
Convergent Boundary
Plates rubbing past each other is known as a transform boundary.
They are called a Plate Boundaries :)
The place where two tectonic plates move away from each other horizontally are called divergent plate boundaries.
Mid-ocean ridges
A divergent plate boundary.