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1. Three different kinds of stress can occur in the crust—tension, compression, and shearing.
2. In geology, epeirogenic movement (from Greek epeiros, land, and genesis, birth) is upheavals or depressions of land exhibiting long wavelengths and little folding apart from broad undulations. The broad central parts of continents are called cratons, and are subject to epeirogeny.
3. An orogeny is an event that leads to a large structural deformation of the Earth's lithosphere (crust and uppermost mantle) due to the interaction between plate tectonics. ... Orogeny is the primary mechanism by which mountains are built on continents.
4. A large natural elevation of the earth's surface rising abruptly from the surrounding level.
5.Young fold mountains-The Himalayas and The Andes.
6.Old fold mountains-The Aravali Range,The Ural Mountains.
7.Block mountains-Sierra Nevada in California and Nevada.
8. These mountains form when faults or cracks in the earth's crust force some materials or blocks of rock up and others down. Instead of the earth folding over, the earth's crust fractures (pulls apart). ... Examples of fault-block mountains include: the Sierra Nevada mountains in North America.
9. An area of fairly level high ground.Examples-Intermontane plateaus. Mountain border plateaus. Domed plateaus, Volcanic plateaus.
10. A plateau which is enclosed or surrounded by mountain ranges is known as an intermontane plateau.
11. A plain is a flat, sweeping landmass that generally does not change much in elevation.
12. Sundarban delta and Nile delta are examples of delta plains.
13. Loess is an aeolian sediment formed by the accumulation of wind-blown silt, typically in the 20–50 micrometer size range, twenty percent or less clay and the balance equal parts sand and silt that are loosely cemented by calcium carbonate.
14. The drift plains are forms when a sheet of ice becomes detached from the main body of glacier and melts in place depositing the sediments it carried.
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