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 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.
Indo-Austrailan and the Eurasian Plates Stay in School Kids
When the Indian Plate crashed into the European Plate, the softer Indian Plate was forced underneath the European Plate. This mass building up below caused the up-thrust to form the Himalayan Mountain Range. It is believed that the Himalayas are still very slowly growing higher.
convergent continental-continental boundary
Continental /Oceanic Crust is being formed.
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.
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.
Japan sits on top of a destructive plate margin.
A physcadelic plate.
A convergent or constructive continental boundary formed the Himalayas.
The Himalayas resulted from the collision of the Indian Plate into the European plate. The softer Indian Plate was forced underneath the harder European Plate, which caused the European Plate to rise up and form the Himalayas.
Indo-Austrailan and the Eurasian Plates Stay in School Kids
The Himalayas are Fold Mountains
Convergent Boundary.
The Himalayas are found at a convergent plate boundary also known as a subduction zone where one plate slips under the other driving the land mass up.
it is on a convergent plate boundary also known as a subduction zone
Subduction