What is the process of continental collision?

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What is the process of continental collision?

The process of continental collision refers to the collision and subsequent convergence of two continental plates. It occurs when two tectonic plates carrying continental crust collide due to the movement of the Earth's lithosphere.

During continental collision, the leading edges of the two plates collide, causing intense compression and deformation of the crust. As the plates continue to converge, the continental crust buckles and folds, forming mountain ranges. This process is responsible for the creation of some of the world's largest mountain systems, such as the Himalayas and the Alps.

The collision between continental plates is a slow and gradual process that can take millions of years to complete. As the plates continue to collide, the crust thickens and deep-seated rocks are uplifted, leading to the formation of high mountain ranges. The collision also results in intense pressure and heat, causing metamorphism and the formation of new rocks.

Continental collision plays a crucial role in shaping the Earth's surface and influencing the distribution of landmasses. It is responsible for the formation of major mountain belts, the closure of ancient oceans, and the creation of new continental crust. Additionally, the collision between continental plates can have significant geological and environmental impacts, including the formation of earthquakes, volcanic activity, and the redistribution of natural resources.