Lake Milh

The lake is located in a depression into which excess water from Lake Habbaniyah, which comes from the Euphrates River, is diverted through a controlled escape channel or canal. The lake is listed as a wetland of international importance. The lake is rather shallow and the water level changes seasonally. Due to its salt content and changing water level, this largest freshwater^{[contradictory]} lake in Iraq has lost its important stock of fish species and only a few recreational areas exist around the lake.

Lake Milh
From space, June 1996
Lake Milh
Coordinates	32°45′09″N 43°38′06″E / 32.75250°N 43.63500°E / 32.75250; 43.63500
Type	Saline
Primary inflows	Canal from Lake Habbaniyah, ultimately the Euphrates
Primary outflows	Euphrates River
Basin countries	Iraq
Surface area	1,562.34 km2 (603.22 sq mi)

 

The lake, also termed the Karbala Gap, covers an area of 156,234 hectares (386,060 acres) enclosed by deserts with a few low hills on the shoreline. The lake and its surrounding area lie in an elevation range of 28 to 56 metres (92 to 184 ft). It is a deep closed lake in a sand and silt basin. The western part of the valley surrounding the lake has thick forest cover, as well as orchards. In the eastern and southern surroundings, the terrain is flat desert and semi-desert. Mud flats are a common feature in the lake.

The geological formations in and around the lake consist of marl, siltstone, gypsum and anhydrite, and limestone bands, but mostly silt.

The lake is 95 kilometres (59 mi) south-west of Baghdad, and 10 kilometres (6.2 mi) west of Karbala in Karbala Governorate.

The lake was constructed during the latter half of the 1970s, downstream of the Hawr al Habbaniyah as a flood control measure to regulate the floodwaters of the Euphrates River.

The lake is fed from the excess floodwater diverted from the Majora escape of Lake Habbaniyah. The flow from the escape is diverted through the Sin al Thibban canal, which is a narrow channel that is aligned through a semi-desert area. This diversion prevents flooding in the northern areas. The salinity of the lake is increasing as result of inadequate water supply from the linked canal. According to a USGS study of satellite imagery of the area it is noted that the water level of the lake fluctuates with the seasons, and in 1995, 2003, and 2013 the area of the lake was reduced considerably. The local people said that the lake's depth has been reduced to about 5–10 metres (16–33 ft) since 1993, during the regime of Saddam Hussein. The reason for this reduction is mainly due to inadequate diversion of water from Lake Habbaniyah, where the priority of use is irrigation. Diversion has been limited to once every 15 days only. This has also affected fishing operations in the lake which used to be throughout the year. As a result, the only fish species surviving in the lake is reported to be al-Shanik or Shanak (Acanthopagrus arabicus) of marine origin, stocked in the lake by the government. During the Gulf War the area was a military establishment.

The vegetation around the periphery of the lake consists of Aeluropus lagopoides, Juncus acutus, Phragmites australis, Salicornia herbacea, and Schoenoplectus litoralis. Also reported are shrublands made up of the desert species Haloxylon salicornicum, Nitraria retusa, Prosopis farcta, Tamarix aucherana, Tamarix macrocarpa, and Zygophyllum fabago.

The lake area has a large number of wintering waterfowl. Some of the species reported are Marmaronetta angustirostris, Podiceps cristatus, Podiceps nigricollis, Phalacrocorax carbo, Pelecanus onocrotalus, Mergellus albellus and Fulica atra. According to a survey 42 bird species have been recorded.

The mammal species reported are the Rüppell's fox (Vulpes rueppellii), golden jackal (Canis aureus), Indian grey mongoose (Urva edwardsii), jungle cat (Felis chaus), and European wildcat (Felis silvestris).

• Lake Tharthar
• Lake Habbaniyah
• Lake Qadisiyah
• List of dams and reservoirs in Iraq
• Mosul Dam
• Wildlife of Iraq