A range of very high mountains.
two pieces of continental crust meeting at a convergent boundary
A range of very high mountains.
The colder, more dense plate is the one that subducts in a collision between two plates. In an oceanic to oceanic plate collision it is the older of the two plates that will subduct due to its higher density. In an oceanic to continental plate collision, it's the oceanic plate that will subduct because of its higher density.
When two Continental plates come together, they both collide.This forms mountains.
It's referred to as a Convergent Boundary If 2 Continental Plates --> Mountains If 2 Oceanic Plates --> Subduction of Heavier (older) Plate If Continental-Oceanic --> Oceanic Plate slides under the Continental Plate (Subduction of Oceanic)
when two plates collide they form trenches.
According to the modern theory of plate tectonics, its formation is a result of a continental collision along the convergent boundary between the Indo-Australian Plate and the Eurasian Plate.
Convergent Continental collision is where two tectonic plates move towards each other and the plate that is more dense moves underneath the less dense plate.
Its when the oceanic crust and the continental crsut colide together.
mountain formation
two pieces of continental crust meeting at a convergent boundary
two pieces of continental crust meeting at a convergent boundary:) study island 2012
two seafloor plates and a seafloor plate and continental plate
A range of very high mountains.
Accretion from plate collision, and addition of crust from continental rifting.
There are mainly two kinds of mountains, namely fold mountains and block mountains. Fold mountains are formed when a continental plate collides with either another continental plate or an oceanic plate. One example of a continental-continental collision is the collision of the Eurasian plate and the Indo-Australian plate, forming the Himalayas fold mountains range which contains Mt. Everest and K2. One example of a oceanic continental collision is the collision of the Nazca plate and the South American plate, forming the Andes mountains. ---- Block mountains are formed when two plate diverge from each other and sink downwards, leaving a highland in the middle of them. That is a block mountain. You might find this useful, http://en.wikipedia.org/wiki/Mountains.
Mountain-building is a result of continental collision, so destructive plate boundaries. One plate is destroyed by subduction below the other, which undergoes compression, buckling and uplift as the collision continues. This is happening at present in Asia, raising the Himalayan Mountains.