What is faulting give examples of landforms formed by this process.
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Faulting can be defined as a natural phenomenon where the crust on the Earth's surface develops cracks and faults due to the movement of tectonic plates.
Examples of landforms formed by this process are:
- Anticlines (Ups) are formed due to the vertical displacement of rocks. These landforms include mountains, hills.
- Synclines (Downs) are formed due to horizontal displacement of the crustal rocks. These landforms include ridges, lakes, and valleys.
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The process that leads to an error is known as Faulting. The normal error formation is caused by the compressive force, while the negative error formation is caused by the compressive force.
The types of land associated with Faulting are:
- Block Mountains are produced when large crust blocks of land are raised or lowered due to normal Faulting. For example, in Germany, Black Forest, and Uganda, Ruwnzori.
- The Rift Valley is a valley or pit produced by crustal shift and the middle ground between two common faults.
- Plateaus and vessels are the results of the earth's crust. The raised areas are called plateaus, such as the Deccan Plateau in India, and the depressed areas are called vessels, such as the Victoria Basin in Australia (Africa).
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