When an earthquake happens the tectonic plates slide up rubbing on each other. Then they slide up and form huge rocks that are eroded in time. These formations are called mountains
Folded mountains are formed when the Earth's crust is squeezed together. This process causes the rock layers to fold and buckle, creating prominent ridges and peaks. The Appalachian Mountains in the eastern United States are an example of folded mountains.
Upwarped mountains
The tallest mountains on Earth are formed by the collision of tectonic plates. This collision forces rock layers to be pushed upward, creating towering mountain ranges such as the Himalayas and the Andes. Additionally, the process of erosion and weathering over millions of years can also contribute to the height of these mountains.
Mountains formed by magma that reaches the Earth's surface are called volcanoes.
Mountains and plateaus are landforms that are typically formed by the forces of tectonic plates pushing against each other, causing the Earth's crust to uplift. This process is known as crustal deformation and results in the creation of large elevated landmasses.
Residual mountains are formed by the plates in the earth moving
Mountains formed by magma that reach the Earth's surface are called volcanoes. These volcanic mountains are created through the eruption of lava, ash, and gases from the Earth's mantle and crust. Over time, repeated eruptions build up the volcano, forming a distinct peak.
Upwarped mountains are formed.
When forces inside the Earth push up the crust, fold mountains are formed. Examples of fold mountains include the Himalayas, the Alps, and the Andes. These mountains are typically characterized by long linear ridges and valleys.
A upwarped mountain is a mountain consisting of a broad area of the Earth's crust that has moved gently upward without much apparent deformation, and usually containing sedimentary, igneous, and metamorphic rocks
Mountains formed by pressure on layers of the Earth are typically the result of tectonic forces that create folds and faults in the Earth's crust. This process, known as orogeny, often occurs at convergent plate boundaries where two tectonic plates collide, causing the crust to buckle and rise. Examples of such mountains include the Himalayas, which were formed by the collision of the Indian and Eurasian plates. These mountains can be characterized by steep slopes and rugged terrain due to the intense geological processes involved in their formation.
Fold mountains are formed due to the collision of plates and earth movements.