constuctive
Folded mountains are formed by the tectonic forces of compression, where rock layers are squeezed together and folded, such as in convergent plate boundaries. Unwarped mountains, also known as block mountains, are formed by faulting and tectonic forces that uplift and break the Earth's crust, creating steep topography without folding.
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.
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.
The Cohutta mountains were formed by constructive forces. They are part of the Appalachian mountain chain that was formed by the collision of tectonic plates, leading to uplift and the creation of mountain ranges.
The mountains which are formed by by the blocks earth's crust or rock-bed developed by the tensional forces and faulting are known as Relict Mountains.It is also known as Block mountains.
constuctive
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Folded mountains are formed by the tectonic forces of compression, where rock layers are squeezed together and folded, such as in convergent plate boundaries. Unwarped mountains, also known as block mountains, are formed by faulting and tectonic forces that uplift and break the Earth's crust, creating steep topography without folding.
Mountains are typically formed by tectonic plates colliding, leading to the crust being pushed upwards. This can cause the crust to fold and buckle, creating mountain ranges. Additionally, volcanic activity can also contribute to the formation of mountains when magma forces its way to the surface and solidifies.
Upwarped mountains are formed.
Upwarped mountains
Forces that erode mountains are called erosion forces. These forces include processes like weathering, mass wasting, and erosion by water, ice, or wind, which gradually wear down mountain landscapes over time.
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LaRae
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upwarped mountains