Residual Mountains and their Examples

Answer: The shape and structure of the rocks influence the erosion process.

The softer rocks of the upland are eroded considerably more quickly than the harder rock sections due to erosion agents. Soft rocks are worn down into the sand over thousands of years, leaving hard rocks standing tall in the area that has been decreased in height. These are referred to as “residual mountains.” Relict mountains are another name for residual mountains.

Examples of Residual mountains include the Sierras of central Spain and the Mesas of the United States. The Aravalli Mountain and the Parasnath Mountain in Bihar are examples of this type in India.