Differences between normal cycle and arid cycle of davis
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In the late 1800s, U.S. geographer and Harvard professor William Morris Davis developed his “cycle of erosion” theory, holding that features like valleys and plains were shaped by physical forces such as water. ... * Then, in a stage he called “youth,” water flowing through the landscape carves out sharp, steep valleys.
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The normal cycle of erosion starts with formation of landforms by the river and and arid cycle with the impacts age of the river.
Explanation:
- The geographical cycle of erosion was given by William Morris Davis and that states that erosion follows the upliftment of land.
- The normal cycle of erosion by the fluvial processes is the most widespread and most significant geomorphic agents.
- likewise, the normal cycle begins with the rate of upliftment of the landmass with the reference to the sea and rate of erosion in the starting far exceeds the rate of erosion that results in the absolute relief and the relative relief registers an increase.
- After the upliftment and remains stable and the process of the river, development takes place through the youth, maturity, and old age.
- The arid cycle is a modification of the humidity cycle and it exists in the desert, especially in the western USA and around tracks of savanna of Africa.
- The differences in the runoff, maximum relief at the youth, and the mature stage the relief decreases as the cycle progressed, consequent drainage forms various landforms like salt-pans oasis and inselbergs.
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- brainly.in/question/15235232 answered by Deleted account.
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