The tectonic plates pushing each other cause mountain ranges. Like when a towel is folded, you get the ridges. That's exactly what happens.
Plates crumple up to form mountain ranges due to the intense forces of tectonic activity, such as collision or subduction. When plates collide, the immense pressure forces the edges of the plates to crumple and uplift, creating mountain ranges like the Himalayas.
Mountain ranges are often formed by tectonic plate movements that can also cause earthquakes and volcanic activity. Thus, areas with prominent mountain ranges are more likely to have earthquake epicenters and volcanoes due to the tectonic forces at work. The distribution of mountain ranges can serve as an indication of potential earthquake and volcanic activity in a region.
continental drifts
Colliding plates cause mountain ranges to grow.
Mountain ranges are typically associated with convergent plate boundaries, where two tectonic plates collide. The collision forces the plates to crumple and fold, leading to the uplift of rock layers and the formation of mountain ranges.
The San Andreas fault has caused the basins and mountain ranges to form.
Major mountain ranges are formed when crustal plates collide. The intense pressure and forces generated by the collision force the Earth's crust to buckle and uplift, forming mountain ranges.
Mountain ranges often form when large terranes and continents collide due to the intense pressure and tectonic forces generated during the collision. The tectonic forces cause the rocks to deform and uplift, leading to the creation of mountain ranges. Examples include the Himalayas, which formed as a result of the collision between the Indian plate and the Eurasian plate.
convergent forces
Mountain ranges are formed when tectonic plates collide or converge. This collision forces one plate to fold and push upwards, creating elevated landforms. The immense pressure and movement between the plates can also cause earthquakes and volcanic activity, contributing to the formation of mountain ranges.
Fold mountains typically form at convergent plate boundaries, where tectonic forces cause the Earth's crust to fold and uplift. Examples of fold mountain ranges include the Himalayas, Andes, Alps, and Rockies.
Deposition and erosion can wear down a mountain and cause it to shrink.