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Geological Survey of Pakistan (GSP) is an independent executive scientific agency to explore the natural resources of Pakistan. Main tasks GSP perform are Geological, Geophysical and Geo-chemical Mapping of Pakistan. Target of these mapping are resources exploration, Geo-Engineering assessment, Geo-hazard prediction/prevention and addressing ...
Rawat Fault line near Islamabad. The geology of Pakistan encompasses the varied landscapes that make up the land constituting modern-day Pakistan, which are a blend of its geological history, and its climate over the past few million years. The Geological Survey of Pakistan is the premier agency responsible for studying the country's geology. [1]
Inter State Gas Systems (Private) Limited (ISGS) was established in 1996 as a private limited company. In order to meet the growing energy deficit in the country , the Government of Pakistan (GOP), besides encouraging local exploration and production, plans to import natural gas from across its borders from Iran and Turkmenistan .
As a result, earthquakes in Pakistan occur often and are destructive. Geology Pakistan ... Islamabad: 5.1 M w: V 3 2014-05-08: Sindh: 4.5 M w: 2 50 2013-09-28:
To survey, print and publish topographical maps of cis-frontier terrain of Pakistan on scale 1:50,000 and derived maps on scales 1:250,000 and 1:1,000,000 for general public use and the defence forces of Pakistan. To establish and maintain geodetic network in the entire country. To delineate and demarcate international borders of Pakistan.
Geological Survey of Pakistan; Pre-collisional Himalaya; R. Rawat Fault This page was last edited on 2 January 2020, at 01:09 (UTC). ...
This page shows the province-wise list of dams and reservoirs in Pakistan. According to the International Commission on Large Dams, 73 dams and reservoirs in Pakistan are over 15 m (49 ft) in height. [1] Tarbela Dam in Pakistan's Khyber Pakhtunkhwa is the largest earth-filled dam in the world and is the second largest by the structural volume.
The Chaman Fault is a major, active geological fault in Pakistan and Afghanistan that runs for over 850 km. [1] Tectonically, it is actually a system of related geologic faults that separates the Eurasian Plate from the Indo-Australian Plate. It is a terrestrial, primarily transform, left-lateral strike-slip fault.