A mountain is a large landform that rises prominently above its surroundings, typically exhibiting steep slopes, a relatively confined summit area, and considerable height. Mountains are formed through tectonic processes, volcanic activity, or erosion and weathering over long periods of time.
Mountains can be formed through tectonic processes such as the collision of tectonic plates. When two continental plates collide, the land is pushed upwards, forming mountain ranges. The Himalayas, for example, were formed by the collision of the Indian and Eurasian plates.
Volcanic mountains are formed when molten rock (magma) erupts onto the Earth's surface. As the lava cools and solidifies, it builds up, forming a mountain. Examples include Mount Kilimanjaro in Tanzania and Mount Fuji in Japan.
Erosion and weathering can also shape mountains over time. The gradual wearing away of rock by wind, water, and ice can create mountainous landscapes, such as the Rocky Mountains in North America.