Punjab Plain in the context of "Alluvial plain"

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⭐ Core Definition: Punjab Plain

The Punjab Plain is a large alluvial plain in northwestern India and eastern Pakistan. The plain includes the Indian states of Punjab and Haryana and the union territory of Delhi, excluding the Shahdara district, and the eastern part of Pakistani Punjab. This plain is around 200–300 meters above mean sea level. The plain is the western part of the Indo-Gangetic Plain, and is bounded by the Sivalik Hills in the north, the Yamuna River in the east, the Thar Desert of Rajasthan to the south, the Ravi River to the northwest and Sutlej River to the southwest. The plain is extensively farmed for cereals and cotton.

The land formed of alluvium in between two rivers known as Doab is found here. 'Doab' is made up of two words — 'do' meaning two and 'ab' meaning water. Similarly 'Punjab', is also made up of two words — 'Punj' meaning five and 'ab' meaning water.

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Punjab Plain in the context of Indus Valley

The Indus (/ˈɪndəs/ IN-dəs) is a transboundary river of Asia and a trans-Himalayan river of South and Central Asia. The 3,180 km (1,980 mi) river rises in western China, flows northwest through the disputed Kashmir region, first through the Indian-administered Ladakh, and then the Pakistani-administered Gilgit-Baltistan, bends sharply to the left after the Nanga Parbat massif, and flows south-by-southwest through Pakistan, before bifurcating and emptying into the Arabian Sea, its main stem located near the port city of Karachi.

The Indus River has a total drainage area of circa 1,120,000 km (430,000 sq mi). Its estimated annual flow is around 175 km/a (5,500 m/s), making it one of the 50 largest rivers in the world in terms of average annual flow. Its left-bank tributary in Ladakh is the Zanskar River, and its left-bank tributary in the plains is the Panjnad River which is formed by the successive confluences of the five Punjab rivers, namely the Chenab, Jhelum, Ravi, Beas, and Sutlej rivers. Its principal right-bank tributaries are the Shyok, Gilgit, Kabul, Kurram, and Gomal rivers. Beginning in a mountain spring and fed with glaciers and rivers in the Himalayan, Karakoram, and Hindu Kush ranges, the river supports the ecosystems of temperate forests, plains, and arid countryside.

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Punjab Plain in the context of Jhelum District

Jhelum District is a district within the Rawalpindi Division of Punjab, Pakistan, located on both the Pothohar Plateau and the Indus Plain of northern Punjab. It is one of the oldest districts of Punjab, being established on 23 March 1849. It borders the districts of Chakwal, and Rawalpindi to the west; Khushab to the south; Gujrat, Mandi Bahauddin, and Sargodha to the east, along the Jhelum River; and Mirpur to the north.

Jhelum is known for providing many soldiers to the British and later to the Pakistan armed forces due to which it is also known as the 'city of soldiers' or 'land of martyrs and warriors'. Salt is quarried at the Khewra Salt Mine in the Salt Range. There are two coal mines in the district from which the North-Western railway used to obtain part of its supply. These are the only coal mines in Punjab province which are in working condition. The chief center of the salt trade is Pind Dadan Khan. The district is crossed by the main line of the North-Western railway and also traversed along the south by a branch line.

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Punjab Plain in the context of Murree

Murree is a mountain resort city in the northernmost region of the Punjab province of Pakistan. Lying in the Galyat region of the Pir Panjal Range under the western Himalayas, it is located in the northeast of the capital city of Islamabad. The town was built in the mid-19th century and served as the summer capital of the British Punjab, allowing British troops to escape the scorching heat of the plains of Punjab. It has an average altitude of 2,291 metres (7,516 ft).

Construction of the town was started in 1851 on the hills of Murree as a sanatorium for British troops. The permanent town of Murree was constructed in 1853 and a church was consecrated shortly thereafter. One main road was established, commonly referred to as "Mall Road". Murree was the headquarters of the colonial Government of the Punjab Province during the 1873–1875 summer; later the summer capital was moved to Shimla.

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Punjab Plain in the context of Indus valley

The Indus (/ˈɪndəs/ IN-dəs) is a transboundary river of Asia and a trans-Himalayan river of South and Central Asia. The 3,180 km (1,980 mi) river rises in western China where it is known as Sengge Zangbo, flows northwest through the disputed Kashmir region, first through the Indian-administered Ladakh, and then the Pakistani-administered Gilgit-Baltistan, bends sharply to the left after the Nanga Parbat massif, and flows south-by-southwest through Pakistan, before bifurcating and emptying into the Arabian Sea, its main stem located near the port city of Karachi.

The Indus River has a total drainage area of circa 1,120,000 km (430,000 mi). Its estimated annual flow is around 175 km/a (5,500 m/s), making it one of the 50 largest rivers in the world in terms of average annual flow. Its left-bank tributary in Ladakh is the Zanskar River, and its left-bank tributary in the plains is the Panjnad River which is formed by the successive confluences of the five Punjab rivers, namely the Chenab, Jhelum, Ravi, Beas, and Sutlej rivers. Its principal right-bank tributaries are the Shyok, Gilgit, Kabul, Kurram, and Gomal rivers. Beginning in a mountain spring and fed with glaciers and rivers in the Himalayan, Karakoram, and Hindu Kush ranges, the river supports the ecosystems of temperate forests, plains, and arid countryside.

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