Search results
Results from the WOW.Com Content Network
The convergent boundary started about 200 million years ago as India moved north towards the Eurasian Plate. Around 40 to 50 million years ago, the Indian Plate collided with the Eurasian Plate ...
The location of a convergent boundary stays reasonably constant. When an ocean plate converges with a continental plate. The Ocean plate is driven down creating a subduction zone. The subduction zone often creates an ocean trench at the point the two plates meet. The continental plate is pushed upward as the ocean plate is pushed under the continental plate. The longer the motion bringing the ...
Convergent boundaries can form volcanos, trenches, islands, and mountains. An example of a convergent boundary is the Himalayan mountains. Divergent boundaries occur when two plates move apart ...
When crustal plates are pushed together. Convergent boundaries occur when pieces of crust are pushed together and one is subducted over the other, or continental crust piles up into mountain chains. See the three most common types in the pic below.
Learn the definition of a convergent plate boundary and explore the different types of convergent boundaries, where they occur, and see detailed...
Convergent Boundary: A convergent boundary is a place where two tectonic plates collide when moving toward each other in opposite directions. Tectonic plates are large pieces of the Earth's lithosphere. Answer and Explanation: 1
The buildup of friction (thus potential energy) between both converging plates. Convergent boundaries are where two plates come together. The plate that is the most dense will subduct beneath the other plate (see the image below) creating uplift (mountain building) or plates with comparable densities will mash into each other, creating uplift, even though there is still going to be at least ...
convergent boundary is formed where two tectonic plates collide with each other. features formed are Deep trenches Active volcanoes arcs of islands along the tectonic boundary in some cases, mountain ranges.
When the two expanding plates of crust meet a convergent boundary is formed. When one plate is an oceanic crust made mainly of shallow dense basalt meets another plate that is a thick less dense continental crust, the ocean crust is pushed and pulled down. The convergent boundary of a an ocean crust and a continental crust forms a subduction zone,
The convergent boundary along the northern edge is a subduction zone (convergent boundaries and where they collide, one plate dives below the other) where the African plate is diving below the ...