hot spot volcanoes such as the Hawaiian island chain.
Fault-block
Mount Everest was formed by a convergent or collision boundary.
when plate boundaries converge folded mountains are formed.
One example is when the Indian Plate crashed into the European plate. As the Indian plate was driven beneath the European plate, the Himalayas was formed and is still increasing in height.
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.
fault-block
hot spot volcanoes such as the Hawaiian island chain.
The Andes mountain range was formed at a convergent boundary where the South American Plate and the Nazca Plate are colliding. This collision has caused the crust to be uplifted and folded, creating the impressive mountain range we see today.
Fault-block
Mount Everest was formed by a convergent or collision boundary.
Continental Collision Boundary
The collision boundary type modeled the formation of the Himalayan mountains, where the Indian tectonic plate collided with the Eurasian plate. This collision resulted in the uplift and formation of the massive mountain range.
when plate boundaries converge folded mountains are formed.
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.
Divergent: Created Collision\Subduction: Destroyed
the Himalayas were formed by a collision plate boundary, meaning that the plates collided and formed the Himalayas. The Himalayas are also referred to as 'fold mountains' because of the way in which they are made.
The type of boundary that the Andes mountains are, in South America, is a convergent plate boundary. This was formed from the collision of the South American plate boundary and the Nazca plate.