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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]
Survey of Pakistan, which emerged as successor to pre-partition Royal Survey of India, is a National Surveying and Mapping Organization of the country. [2] It is primarily responsible for all sorts of topographical land surveys of cis-frontier areas of the entire country. The basic products include map sheets on scale 1:50,000 and 1:250,000.
The Geological Survey of Pakistan is an autonomous and independent institution under Ministry of Petroleum and Natural Resources which is tasked and mandate with advancing the geoscience knowledge and carrying out systematic studies on official mapping and area surveying. [3]
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.
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:
Geological Survey of Pakistan; Pre-collisional Himalaya; R. Rawat Fault This page was last edited on 2 January 2020, at 01:09 (UTC). ...
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.