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Chagai Hills

Mountain range in Pakistan

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Through Pakistan, British Raj and Queen Victoria

The highest peak, Malik Naru, at the Chagai Hills is measured at 7,915 feet (2,412 m) and is a site of volcanic Koh-i-Sultan.

Overview

Location and topography

During its time as part of the India under the British Queen Victoria, the British Geological Survey conducted the geological survey of the Chagai Hills, which was able to provide its coordinates lies between 28°46′N 63°18′E / 28.767°N 63.300°E in 1908. The more precise coordinates were provided by the extensive geological survey by the Geological Survey of Pakistan (GSP) which provided the coordinates at 29°00′35.65″N 64°00′17.26″E / 29.0099028°N 64.0047944°E in 1983.

The Chagai Hills terrain is mostly consists of dry desert and located in the northernmost area of Chagai District at the international Durand Line– the official name of Afghanistan–Pakistan border. The region where Chagai Hills are located is reported by the extremely dry with no prospect of water, which the GSP conducted a survey in search of water in 1975.

The Chagai Hills are stretched over an area that is approximately 130 kilometres (81 mi) and 95 kilometres (59 mi) wide. The highest peak, Malik Naru, at the Chagai Hills is measured at 7,915 feet (2,412 m) and is a site of volcanic Koh-i-Sultan.

Geology

Since 1901, the geology of Chagai Hills have been studied first by the European geologists and later by Pakistani geologists since 1960. The Chagai Hills are mostly granite mountains, some with average height of 200 m (660 ft)

The Pakistani investigations discovered the occurrences of copper, iron, zinc, molybdenum, sulfur, and limestones, the travertine, which is an interest of economic importance. The geological survey to explore uranium was also conducted in the region in 1957.

The Chagai Hills are continuous subject of interest of Volcanology which the Geological Survey of Pakistan (GSP) has commissioned its studies in a joint venture with the United States since 1997. The Koh-i-Sultan (lit. Mountain of the King) is a prominent site where its activity has provided scientific opportunity to the Pakistani seismologists and volcanologists. The fission carbon dating studies were first conducted on rocks and geological structure in 1997, which provided the age of Chagai Hills in Miocene-Late Pleistocene period.

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