The Himalayas were formed by the convergence of the Indian and Eurasian tectonic plates, with the Indian plate pushing against the Eurasian plate, causing the land to rise and form the mountain range.
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.
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.
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.
if i thing if gago abno yudipota ka
Andes, convergence between South American Plate and Pacific Plate
oceanic convergence is when two oceanic plates subduct beneath one another.
oceanic convergence is when two oceanic plates subduct beneath one another.
oceanic convergence is when two oceanic plates subduct beneath one another.
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.
The Andes mountain range is being formed by the convergence of the Nazca and South American plates. This process involves the oceanic Nazca Plate subducting beneath the South American Plate, leading to the uplift of the Andes mountains.
The Andes Mountains :) ***** I would like to add the Himalayas, which rose when the Indian Plate collided with the European plate.
non boundary mountains
The Andes mountain range was not formed as a result of continental-continental convergence; instead, it resulted from oceanic-continental convergence. Specifically, the Andes were created by the subduction of the Nazca Plate beneath the South American Plate. In contrast, the Himalayas, Alps, and Appalachians are primarily the result of continental-continental tectonic interactions.
The Aleutian Islands
convergence between a continetal plate and an oceanic plate
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.
Continental crust cannot form as a result of oceanic-oceanic convergence. This process typically results in the formation of volcanic island arcs or deep-sea trenches. Continental crust is formed through processes like continental collision and accretion of terranes.