Glaciers
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Glaciers

Imagine you are trekking in the high Himalayas. As you ascend, the air gets colder, the terrain turns from lush green to rocky, and finally, you reach a point where snow never melts. This is the snow line—the altitude above which temperatures never rise above freezing, even in the hottest month of the year. So,…

Arid Cycle of Erosion
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Arid Cycle of Erosion

In 1905, W.M. Davis introduced the concept of the Arid Cycle of Erosion, which explains how desert landscapes gradually change over time due to erosion and deposition. However, this concept applies only to mountain deserts (like the Thar Desert) and not to low-level open deserts. The cycle passes through four stages — Initial, Youth, Maturity,…

Water Eroded Arid Landforms
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Water Eroded Arid Landforms

Suppose you’re standing in a vast, arid desert. The land appears dry and lifeless most of the year, but occasionally, a sudden torrential downpour occurs. Water gushes through the barren landscape, shaping it in unique ways. Unlike humid regions where rivers continuously erode land, in arid regions, water erosion happens sporadically but intensely, giving rise…