There are three types of convergent boundaries: Oceanic, continental, and continental-oceanic convergent boundaries. Continental-continental convergent boundaries form mountain ranges.
Continental-oceanic boundaries result in subduction zones and the recycling of lithosphere. The continental side of the boundary may form a mountain range.
Oceanic-oceanic form deep oceanic trenches and sometimes volcanoes.
coliding boundary
the mid ocean ridges cause the magma to form at a convergent plate boundary.
convergant
A convergant boundary is destructive because the plates approach one another.
The type of plate boundary the Vesuvius is located on it a subduction zone in latitude 40.9n and 14e. It lies on the convergant boundry of the African and Euasian plates.
Mt Fuji is located on three plates. Those three plates are: Amurian, Okhotsk, and the Filipino located directly below Fuji.
Naturally, Compression! Converge= Collide, Compress= Force together, put it all together; CONVERGANT BOUNDRY!!!!
convergant boundary and divergant boundary
Felsic rocks, such as granite, primarily originate from convergent plate boundaries where continental crust collides and undergoes partial melting to form silica-rich magmas. These magmas then cool and solidify to create felsic rocks.
A stratovolcano, also known as a composite volcano, is the type of volcano that occurs along a convergent plate boundary. These volcanoes are typically steep-sided and have explosive eruptions due to the presence of viscous magma.
When convergent plates collide one is pushed beneath the other plate and sinks into the Earth's mantle. This process is known as subduction. Subduction creates trenches in the ocean, which is why trenches and associated with convergent plates.
The plate boundary that causes mountains to form is called a convergent boundary.