Articles | Volume 382
https://doi.org/10.5194/piahs-382-595-2020
https://doi.org/10.5194/piahs-382-595-2020
Pre-conference publication
 | 
22 Apr 2020
Pre-conference publication |  | 22 Apr 2020

Land subsidence caused by groundwater exploitation in Quetta and surrounding region, Pakistan

Najeebullah Kakar, Din Muhammad Kakar, and Sadia Barrech

Cited articles

Ahmad, S.: Persistent drought of Balochistan and impacts on water availability and Agriculture, Water for Balochistan: Policy Briefings, 3, 2010–2011, 2007. 
Alam, K. and Ahmad, N.: Determination of aquifer geometry through geophysical methods: A case study from Quetta Valley, Pakistan, Acta Geophys., 62, 142–163, 2014. 
Galloway, D. L., Jones, D. R., and Ingebritsen, S. E.: Land subsidence in the United States, US Geological Survey, 1999. 
Halcrow and Cameos Consultant Companies: Effectiveness of Delay Action/Storage Dams in Balochistan, TA-4560(PAK) Project, Asian Development Bank, Quetta, 2008. 
Haque, B.: Water level behavior in northern part of Quetta valley, Hydrogeology Project Quetta, WAPDA, 1986. 
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Short summary
In Quetta, Pakistan where I have worked. Land Subsidence has created large scale fractures on the surface of the land, these fissures have damaged a lot of structures inside the city. According to our research work, the annual recorded subsidence rate in Quetta city is about 120 mm per year and the groundwater decline level is about 5 m per year. We measured land Subsidence using GPS units. These GPS units are capable of recording land deformation with sub-centimeter accuracy.