The answer is subduction.
When an oceanic plate collides with a continental plate, the denser oceanic plate is forced beneath the lighter continental plate in a process called subduction. This leads to the formation of deep ocean trenches and volcanic arcs on the continental plate. As the oceanic plate descends into the mantle, it generates magma, which can result in volcanic activity. Over time, this tectonic interaction can also cause earthquakes along the subduction zone.
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.
Fold mountains.
As the oceanic crust descends beneath the continental crust, the mantle rock is subjected to high pressure and temperature. This causes the mantle rock to partially melt, producing magma that can rise to the surface and form volcanoes. The interaction of the descending oceanic crust with the continental crust can also lead to earthquake activity.
Its when the oceanic crust and the continental crsut colide together.
This process is known as subduction. When an oceanic plate collides with and is forced underneath a continental plate, it creates a subduction zone. The descending oceanic plate melts due to the intense heat and pressure, causing volcanic activity and the formation of mountain ranges on the continental plate.
The categories are a continental and a continental plate colliding, continental and oceanic plates colliding, and oceanic and oceanic plates colliding. The two continental plates form mountains. The continental and oceanic plated colliding cause subduction zones and volcanoes. Oceanic and oceanic plates colliding form a trench.
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.
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.
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.
Andean
Fold mountains.
As the oceanic crust descends beneath the continental crust, the mantle rock is subjected to high pressure and temperature. This causes the mantle rock to partially melt, producing magma that can rise to the surface and form volcanoes. The interaction of the descending oceanic crust with the continental crust can also lead to earthquake activity.
When an oceanic plate and a continental plate collide, it forms a volcano. The oceanic plate subducts underneath the continental plate. As the oceanic plate slides underneath, a magma chamber is formed. This magma chamber is what feeds the volcano.
Its when the oceanic crust and the continental crsut colide together.
They are fold mountains as it is a mountain range. It is caused by either 2 continental plates or an oceanic and a continental plate colliding into each other.
Oceanic-Oceanic.