continental volcanic arc. :)
Ocean-continental convergent boundaries can produce earthquakes and volcanic activity. As the ocean plates shift under each other they near their melting temperature and can form magma and solidify to form underwater mountain ranges.
The three types of convergent plate boundaries are oceanic-oceanic, oceanic-continental, and continental-continental. Oceanic-oceanic convergence occurs when two oceanic plates collide, resulting in the formation of volcanic island arcs. Oceanic-continental convergence happens when an oceanic plate subducts beneath a continental plate, creating volcanic mountain ranges. Continental-continental convergence involves the collision of two continental plates, leading to the formation of large mountain ranges.
Both oceanic-oceanic and continental-continental convergent boundaries involve the collision of tectonic plates, leading to geological features such as mountains and earthquakes. In oceanic-oceanic convergence, one oceanic plate subducts beneath another, often creating deep ocean trenches and volcanic island arcs. In contrast, continental-continental convergence occurs when two continental plates collide, resulting in the formation of extensive mountain ranges, like the Himalayas, without significant subduction. The main difference lies in the types of plates involved and the resulting geological features.
A deep ocean trench is commonly formed at a plate boundary where oceanic crust converges with continental crust. The oceanic crust is denser and is forced beneath the lighter continental crust, creating a deep trench.
The three main regions of the ocean floor are the continental margins, the ocean basins, and the mid-ocean ridges. Continental margins are the shallow, submerged edges of continents. Ocean basins are the deeper areas of the ocean floor beyond the continental margins. Mid-ocean ridges are underwater mountain ranges where tectonic plates move apart and magma rises to create new oceanic crust.
Parallel belts of folded mountains and volcanic mountains
Ocean-continental convergent boundaries can produce earthquakes and volcanic activity. As the ocean plates shift under each other they near their melting temperature and can form magma and solidify to form underwater mountain ranges.
Ocean-continental convergent boundaries can produce earthquakes and volcanic activity. As the ocean plates shift under each other they near their melting temperature and can form magma and solidify to form underwater mountain ranges.
Parallel belts of folded mountains and volcanic mountains
Parallel belts of folded mountains and volcanic mountains
Ocean convergence occurs when two ocean currents come together. This can lead to the uplift of deep water and the formation of upwelling zones, which can bring nutrients to the surface and support marine productivity.
Mountains like the Andes, fold mountains with Volcanoes,.
Convergence can occur between oceanic-oceanic, oceanic-continental, and continental-continental plates. This process typically leads to the formation of mountain ranges, deep ocean trenches, and volcanic arcs.
continental volcanic arc
In oceanic-continental convergence, the denser oceanic plate is forced beneath the continental plate in a process called subduction. This creates a deep ocean trench and can lead to volcanic activity and the formation of mountain ranges on the continental plate. The collision can also cause earthquakes.
ujnjenfrn
The Andes Mountains :) ***** I would like to add the Himalayas, which rose when the Indian Plate collided with the European plate.