It depends on the type of crust involved. If both plates carry oceanic crust, an ocean trench is formed along with a volcanic island are on the overriding plate. If one plate carries oceanic crust and the other continental, you will get an ocean trench, a continental volcanic arc, and a mountain range. If both plates carry continental crust, then a mountain range is formed.
Convergent boundaries are classified according to the type of tectonic plates involved. There are three main types of convergent boundaries: oceanic-continental, oceanic-oceanic, and continental-continental. The classification is based on whether the plates involved are oceanic or continental and the resulting geological features that are formed.
Mountain ranges are formed when two continental plates collide. When they converge one plate will be forced slightly under the other one.
At a continental-continental convergence, two tectonic plates carrying continental crust collide, leading to the uplift of land and the formation of mountain ranges. This process can result in intense seismic activity and the creation of complex geological structures. Unlike oceanic-continental convergence, there is no subduction, as both plates are buoyant, leading to a compressional environment. Notable examples include the Himalayas, formed by the collision of the Indian and Eurasian plates.
Oceanic plates are denser and thinner than continental plates, which causes them to be lower in elevation. The denser oceanic plates are effectively pulled downward by gravity, causing them to sink beneath the less dense continental plates. This difference in density and thickness results in oceanic plates being lower than continental plates.
When two continental plates collide,fold mountains are formed.
The Matterhorn in the Alps was formed through the movement of tectonic plates, specifically the African and European plates colliding. This collision caused the Earth's crust to fold and thrust upwards, creating the iconic pyramid shape of the Matterhorn. Additionally, glacial erosion over millions of years helped sculpt the mountain to its current form.
rift valley Answer 2 Continents are formed when continental plates pull apart.
Deep-ocean trenches are formed where seafloor tectonic plates subduct under continental plates.
fold mountains
In theory, tectonic plates. http://www.ucmp.berkeley.edu/geology/tectonics.html
Some examples of mountain ranges created by continental-continental convergence are the Himalayas (resulting from the collision of the Indian and Eurasian plates) and the Alps (formed by the collision of African and Eurasian plates).
When it is two continental plates, new oceanic crust is formed, and when this continues, more oceanic crust is formed between the plates.
rift valley Answer 2 Continents are formed when continental plates pull apart.
They were formed on the edges of two ancient continental plates that collided with each other in the geological past.
Subduction zones are formed when oceanic plates slide beneath continental plates. The process leads to the oceanic plate being forced into the Earth's mantle. This can result in the formation of deep oceanic trenches and volcanic activity at the surface.
It depends on the type of crust involved. If both plates carry oceanic crust, an ocean trench is formed along with a volcanic island are on the overriding plate. If one plate carries oceanic crust and the other continental, you will get an ocean trench, a continental volcanic arc, and a mountain range. If both plates carry continental crust, then a mountain range is formed.