Overview of Ground Water Situation in India

Authors

  • khatri P Associate professor Department of Geography, GCW Rohtak

Keywords:

Hard-rock aquifers of peninsular India, Alluvial aquifers of the Indo-Gangetic plains

Abstract

Ground water is the water that seeps through rocks and soil and is stored below the ground. The rocks in which ground water is stored are called aquifers. Aquifers are typically made up of gravel, sand, sandstone or limestone. Water moves through these rocks because they have large connected spaces that make them permeable. The area where water fills the aquifer is called the saturated zone. The depth from the surface at which ground water is found is called the water table. The water table can be as shallow as a foot below the ground or it can be a few hundred meters deep. Heavy rains can cause the water table to rise and conversely, continuous extraction of ground water can cause the level to fall.

References

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Published

2023-09-30

How to Cite

khatri, P. R. (2023). Overview of Ground Water Situation in India. Universal Research Reports, 10(3), 83–93. Retrieved from https://urr.shodhsagar.com/index.php/j/article/view/1125

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Section

Original Research Article