When an oceanic plate collides with a continental plate, the denser oceanic plate typically subducts beneath the lighter continental plate due to the difference in density. This subduction can lead to the formation of volcanic mountain ranges along the continental margin. The oceanic plate may also undergo partial melting, leading to the formation of magma that can erupt to the surface.
The three categories of convergent boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergent boundaries result in volcanic island arcs. Oceanic-continental convergent boundaries create volcanic mountain ranges. Continental-continental convergent boundaries give rise to large mountain ranges.
At a convergent plate boundary between an oceanic and continental plate, the oceanic plate is usually denser and subducts beneath the continental plate. This can lead to the formation of deep oceanic trenches, volcanic arcs on the continental plate, and earthquakes due to the intense pressure and friction. Over time, the oceanic plate can melt and create magma that rises to form volcanic mountain ranges on the continental plate.
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced to subduct beneath the lighter continental plate. As the oceanic plate descends into the mantle, it creates a deep ocean trench at the boundary. The subduction process can result in volcanic activity, earthquakes, and the formation of mountain ranges on the overriding continental plate.
if i thing if gago abno yudipota ka
Andes, convergence between South American Plate and Pacific Plate
An oceanic plate colliding with a continental plate formed the Sierra Nevada. That collision is no longer happening, though, as that oceanic plate. the Farallon Plate, is mostly gone, with remnants to the north and south.
The answer is subduction.
Andean
The three categories of convergent boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergent boundaries result in volcanic island arcs. Oceanic-continental convergent boundaries create volcanic mountain ranges. Continental-continental convergent boundaries give rise to large mountain ranges.
Fold mountains.
At a convergent plate boundary between an oceanic and continental plate, the oceanic plate is usually denser and subducts beneath the continental plate. This can lead to the formation of deep oceanic trenches, volcanic arcs on the continental plate, and earthquakes due to the intense pressure and friction. Over time, the oceanic plate can melt and create magma that rises to form volcanic mountain ranges on the continental plate.
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced to subduct beneath the lighter continental plate. As the oceanic plate descends into the mantle, it creates a deep ocean trench at the boundary. The subduction process can result in volcanic activity, earthquakes, and the formation of mountain ranges on the overriding continental plate.
At this type of convergent boundary the oceanic plate will be subducted, or sink into the mantle underneath the continental plate. Volcanoes often form near these boundaries.
Fold mountains.
no se cual es la respuesta
Andes, convergence between South American Plate and Pacific Plate
if i thing if gago abno yudipota ka