Extreme mountain ranges
Oceanic-continental convergent boundary: Where oceanic plates subduct beneath continental plates, creating deep ocean trenches and volcanic arcs on the overriding plate. Continental-continental convergent boundary: Where two continental plates collide, causing intense folding and faulting to create mountain ranges. An example is the collision of the Indian Plate with the Eurasian Plate, forming the Himalayas.
A convergent boundary is when two plates collide with each other forming landforms like trenches, or mountains (depends which type of plates converge.)
A convergent boundary is formed when two tectonic plates collide. This collision can result in one plate being forced beneath the other in a process called subduction, where the denser plate sinks into the mantle. This can lead to the formation of mountain ranges, deep ocean trenches, and volcanic activity.
the boundry formed by the collision of 2 lithosphere plates
convergent boundaries form when 2 plates collide, causing moutains to form over millions of years.
1. Oceanic-oceanic convergent plate boundary. 2. Continental-continental convergent plate boundary. and 3. Oceanic-continental convergent plate boundary.
convergent boundaries form when 2 plates collide, causing moutains to form over millions of years.
when two plates push together, it could either cause mountains or a subduction zone. When they cause mountains it's when two
1. Convergent movement 2. Divergent movement 3. Shear movement
earthquakes
Mountain plates. when 2 mountain plates crashes together, they go all the way up and forms mountains.
Rebound tendency is when 2 plates from a convergent boundary slide past one another to form a trench