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The Himalayan Mountains are a result of the collision between the Indian Plate and the Eurasian Plate. This collision has led to the uplift of the mountains through convergent tectonic processes. The movement of the plates continues to push the mountains higher over time.
No. It is the collision between two tectonic plates that can cause mountains. For example: when the Indian plate collided into the European plate, the Himalayan mountains were formed.
A convergent boundary where two tectonic plates collide causes mountains to form. The intense pressure and friction between the plates force them to move upwards, resulting in the formation of mountain ranges. Examples of this are the Himalayas, where the Indian Plate is colliding with the Eurasian Plate.
Convergent boundary mountains are formed where two tectonic plates collide, causing one plate to be forced beneath the other in a process called subduction. This collision can lead to the formation of mountain ranges due to the intense pressure and folding of the Earth's crust. The Himalayas are a notable example of convergent boundary mountains, formed by the collision of the Indian Plate with the Eurasian Plate.
A transform boundary occurs when tectonic plates slide past each other horizontally, causing earthquakes. On the other hand, a convergent boundary forms when two tectonic plates collide, leading to the formation of mountains, trenches, and volcanic activity.
A complex plate boundary is a tectonic boundary where three or more plates meet. These boundaries can be sites of intense geologic activity, including seismic activity, volcanic eruptions, and mountain-building. Examples include the Himalayan region where the Indian, Eurasian, and Pacific plates interact.