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The Pothohar Plateau (Punjabi: پوٹھوہار پٹھار, romanized: Pо̄ṭhoā̀r Paṭhār; Urdu: سطح مرتفع پوٹھوہار, romanized: Satāh Murtafā Pо̄ṭhohār), also spelled Pothwar, is a plateau in the Sind Sagar Doab of northern Punjab, Pakistan, located between the Indus and Jhelum rivers.
2012-03-02 19:15 Elraja1988 2365×1890× (804699 bytes) More accurate mapping, previous map was locations of constituent districts, this map is a better representation of where exactly the plateau lies within the greater pothohar region.
Tilla Jogian, second highest peak in Potwar The Potwar Plateau (also Potowar or Potohar) is a plateau in the province of Punjab, Pakistan and the western parts of Pakistan administered Kashmir. The area was the home of the Soanian Culture, which is evidenced by the discovery of fossils, tools, coins, and remains of ancient archaeological sites.
The Tarbela Dam is located on the Indus River near the village of Tarbela in Bara, approximately 30 kilometers from the town of Attock. Positioned where the Indus River emerges from the foothills of the Himalayas and enters the Potwar Plateau, the dam features a reservoir for water storage.
Tilla Jogian, second highest peak in the Pothohar plateau. The Pothohar Plateau is a plateau and historical sub-region in northern parts of the Punjab region, present-day Punjab, Pakistan. Ethnic Punjabis are the native people of the area and are subdivided into many tribes and clans . [1]
Oil production was entirely confined to the Potwar Plateau till 1981, when Union Texas Pakistan subsidiary discovered its first oil-field in Lower Sindh. By 1998-1999, the Lower Sindh gas-fields were producing more oil than the Potohar Plateau. Since then, new deposits have also been found here.
Earthquake hazard zones of Pakistan. Pakistan geologically overlaps both with the Indian and the Eurasian tectonic plates where its Sindh and Punjab provinces lie on the north-western corner of the Indian plate while Balochistan and most of the Khyber-Pakhtunkhwa lie within the Eurasian plate which mainly comprises the Iranian plateau, some parts of the Middle East and Central Asia.
The Thal desert is a subtropical sandy region with severe climatic conditions that are prone to temperature extremes. [17] Approximately 50% of the region sees hyper-arid climatic conditions (annual rainfall less than 200mm) and the remaining half sees semi-arid climatic conditions (annual rainfall between 200mm and 500mm). [18]