two pieces of continental crust meeting at a convergent boundary
Continental plate to continental plate collisions.
two pieces of continental crust meeting at a convergent boundary
mountain building
Usually in high temperature and high pressure environments associated with plate collisions and mountain building.
When subduction occurs at points of plates collision.
Continental plate to continental plate collisions.
two pieces of continental crust meeting at a convergent boundary
two pieces of continental crust meeting at a convergent boundary:) study island 2012
the formation of a mountain range
Volume is an extensive property.
The extensive mountain range is known as a mountain range, and the principal mountain system of a continent is referred to as a continental mountain range. They are characterized by their significant size and their role in shaping the landscape and climate of the continent. Examples include the Rocky Mountains in North America and the Andes in South America.
Mountain formation refers to the geological processes that underlie the formation and metamorphism are all parts of the orogenic process of mountain building.
A sedimentary rock formation
fafafa
Mountain
Orogensis is the process of mountain formation.
Inselberg Formation