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9-520: The lake's banks and vicinity are home to ancient archaeological sites Ghazi Shah , Wahi Pandhi and Ali Murad Mound . The sites of Lal Chatto, Mashak Lohri and Lakhiyo situated along the bank of Lake Manchar are the most ancient sites, which date from the Harappan culture . The lake was formed when a branch of the Indus River flowed from Kashmore . In 1921, it was connected to Hamal Lake via

18-499: A breach in the lake to assist its drainage to protect the city of Sehwan and the town of Bhan Syedabad , at the cost of flooding many villages that are home to 150,000 people. Officials had hoped the ploy would protect up to 500,000 people from flooding. Lake Manchar is directly south of Hamal Lake , and the two are connected by the Main Nara Valley Drain built in 1921. Manchar lake's surface area fluctuates with

27-592: The "Boat People." The lake supports thousands of fisherfolk, who depend on the freshwater fish in the lake. Ghazi Shah Mound The Ghazi Shah Mound is most ancient archaeological site located in Johi Tehsil of Dadu District in Sindh, Pakistan . It was explored by N. G. Majumdar and Louis Flam has also studied and surveyed this ancient site. It is among the earliest site of Indus Valley civilization and dates back to 4000 to 6000 years. This place

36-468: The Indus flyway for Siberian migratory birds, but the numbers have fallen from 25,000 birds counted in 1988 to 2,800 birds counted in 2002, because the lake no longer provides the birds' main food, the lake fish. In the place of the birds, the lake now hosts a saline water reed. The lake also provided large volumes of water for irrigation, but this has also been reduced and has resulted in a great reduction in

45-413: The Main Nara Valley Drain. In 1958, the lake completely evaporated due to drought. Between 10 August and 23 August 2009, 700 cu ft/s (20 m/s) of water was introduced in the lake via Indus River . In the 2010 Pakistan floods , the lake overflowed due to a high inflow of water. During the 2022 Pakistan floods it again overflowed, and efforts were made to assist its drainage. Engineers made

54-526: The area irrigated by the lake. Right Bank Outfall Drain is being built to save the lake from contamination through inflow of sewage. Construction of the Nai Gaj Dam upstream from the lake will result in freshwater being discharged into the lake throughout the year, instead of seasonally, which should improve the lake's waters. Lake Manchar is populated by the Mohana tribe, who are sometimes referred to as

63-454: The lake has been degraded. The diversion of water from the Indus and a diminished storm runoff from the Kirthar mountains have contributed to the reduction in fresh water supplies, resulting in the water becoming saline, and killing off fish. At the same time, saline drainage water from agricultural fields of Balochistan and surrounding areas flows into Lake Manchar. The lake was a stop-off on

72-583: The lake is at the base of the Laki Hills, a branch of the Kirthar Mountains , and water flows to the Indus via the Aral channel, and Danister Canal. The lake supports thousands of fisherfolk, who depend on the freshwater fish in the lake. The lake since construction of the Main Nara Valley Drain in 1921 has undergone environmental degradation with inflow of sewage. Consequently, the water quality of

81-445: The seasons - from as little as 200 km to as much as 500 km during monsoon rains. The average depth is only 2.5 to 3.75 metres. It is 6 metres lower than the bed of the Indus, and sometimes catches floodwater from the river, while in winter when the river is low, water flows from the lake into the Indus. Freshwater flow from canals amounts to 1.54 MAF, and rainfall in the area averages only 4.46 inches annual. The southern end of

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