Composite cone volcanos are the most common.. Shielding and other types are results from a divergent boundary.
The lavas that are erupted at convergent plate boundaries are mostly intermediate (andesitic). Convergent plate boundaries also erupt mafic (basaltic) lavas
Most volcanoes at convergent boundaries are stratovolcanoes.
They are typically basaltic in composition.
Yes. Pinatubo and the other volcanoes of the Philippines are the result of he convergence between the Philippine Plate and the Eurasian plate.
Converging Plate Boundaries
they are both formed by converging plates at a BOUNDARY THAT PUSH UP THE EARTH
Continental and Oceanic plates.
no its along a divering boundary
Most are found on converging
Volcanoes may form where two oceanic plates collide or where an oceanic plate collides with a continental plate.
Volcanoes may form where two oceanic plates collide or where an oceanic plate collides with a continental plate.
Yes. Pinatubo and the other volcanoes of the Philippines are the result of he convergence between the Philippine Plate and the Eurasian plate.
Converging Plate Boundaries
they are both formed by converging plates at a BOUNDARY THAT PUSH UP THE EARTH
they are both formed by converging plates at a BOUNDARY THAT PUSH UP THE EARTH
hotspot volcanoes are formed away from the edge of plate boundaries. Plate boundary volcanoes are near a plate boundary
Continental and Oceanic plates.
Two continental plates meet here plus a great number of faults
no its along a divering boundary
Shield volcanoes may occur far from any plate boundaries.