Boundaries, or faults, are locations on the edges of plates, crustal masses that are very slowly moving atop the convective outer mantle (asthenosphere).
At convergent boundaries, two crustal masses (plates) are pushing into each other. This can result in subduction, so may be a destructive boundary.
At divergent boundaries, two masses of rock are pulling away from each other. This can be a constructive boundary when it produces rifting and seafloor spreading.
At transform boundaries, or transform faults, rock masses move past one another. These are known as conservativeboundaries because crust is neither destroyed or created.
(these can cause earthquakes when accumulated strain is released)
convergent boundaries collide but divergent boundaries move away from each other.
convergent boundaries collide but divergent boundaries move away from each other.
There are divergent, convergent, and transform plate boundaries.
Earthquakes can, and do, occur at divergent, convergent, and transform plate boundaries.
The four types of plate boundaries are divergent boundaries (plates moving apart), convergent boundaries (plates moving together), transform boundaries (plates sliding past each other), and subduction zones (one plate sinking beneath another).
Yes, volcanism is found at both convergent and divergent boundaries of tectonic plates. At convergent boundaries, subduction zones can result in the formation of volcanoes due to the melting of subducted crust. At divergent boundaries, magma rises to the surface to create new crust, leading to volcanic activity as seen in mid-ocean ridges.
Convergent, divergent, and transformal
Volcanoes and earthquakes
divergent, transform and convergent
Convergent,Divergent, and Transform Boundaries
Underwater volcanoes and mountains can form at both convergent and divergent boundaries.
Convergent divergent transform,