The type of forces that dominate at convergent plate margins are compressive forces. The tensional forces are tectonic forces that tend to push two sides of body in opposite directions so that they slide horizontally past one another.
(A+LS) Convergent Boundary
Contenental/contenental
A convergent boundary adds to the lithosphere by bringing new material to the crust through subduction or continental collision. This process helps in the formation of mountain ranges and volcanic arcs.
It forms a convergent boundary with the South American Plate, divergent.
It is on a convergent plate boundry forming a subduction zone which build pressure in the volcano causing them to erupt.
Convergent boundry
Tension
the boundry formed by the collision of 2 lithosphere plates
Naturally, Compression! Converge= Collide, Compress= Force together, put it all together; CONVERGANT BOUNDRY!!!!
Predominantly.... Convergent Boundary.
Mount Nyamuragira is on a convergent boundry
(A+LS) Convergent Boundary
Contenental/contenental
Compression
The three main types of plate boundaries are divergent, convergent, and transform. Divergent boundaries occur where plates move apart, creating new crust. Convergent boundaries occur where plates collide and can result in subduction zones or mountain formation. Transform boundaries occur where plates slide past each other horizontally.
A convergent boundry is creating the shiveluch volcano in Russia. The Eurasian plate collides with the Pacific plate
its convergent!