Qattara Depression

For other uses, see Qattara (disambiguation).
Qattara Depression
Qattara Depression
Location of the Qattara Depression in Egypt
Location Egypt in the Matruh Governorate
Coordinates 30°0′N 27°30′E / 30.000°N 27.500°E / 30.000; 27.500Coordinates: 30°0′N 27°30′E / 30.000°N 27.500°E / 30.000; 27.500
Type Endorheic basin
Primary inflows Groundwater
Primary outflows Evaporation
Basin countries Egypt
Max. length 300 kilometres (190 mi)
Max. width 135 kilometres (84 mi)
Surface area 19,605 square kilometres (7,570 sq mi)
Average depth −60 metres (−200 ft)
Max. depth −133 metres (−436 ft)
Water volume 1,213 cubic kilometres (291 cu mi)
Settlements Qara Oasis
References [1][2]

The Qattara Depression (Arabic: منخفض القطارة‎‎ Munḫafaḍ al-Qaṭṭārah) is a depression in the north west of Egypt in the Matruh Governorate and is part of the Western Desert. It lies below sea level and is covered with salt pans, sand dunes and salt marshes. The region extends between latitudes of 28°35' and 30°25' north and longitudes of 26°20' and 29°02' east.[3] The region was created by the interplay of salt weathering and wind erosion. Some 20 kilometres west of the depression lie the oases of Siwa and Jaghbub in smaller but similar depressions.

The Qattara Depression contains the second lowest point in Africa at −133 metres (−436 ft) below sea level, the lowest being Lake Assal in Djibouti. The depression covers about 19,605 square kilometres (7,570 sq mi), a size comparable to Lake Ontario or twice as large as Lebanon. Due to its size and proximity to the Mediterranean Sea shore, it has been studied for its potential to generate hydroelectricity.

Geography

Map of the Qattara Depression.
Lower left bound: 28°36'30.74"N 26°14'31.08"E.
Upper right bound: 30°31'1.74"N 29° 8'51.83"E.

The depression has the shape of a teardrop, with its point facing east and the broad deep area facing the south west. The northern side of the depression is characterised by steep escarpments up to 280 meters high, marking the edge of the adjacent El Diffa plateau. To the south the depression slopes gently up to the Great Sand Sea.

Within the Depression are salt marshes, under the northwestern and northern escarpment edges, and extensive dry lake beds that flood occasionally. The marshes occupy approximately 300 square kilometres (120 sq mi), although wind-blown sands are encroaching in some areas. About a quarter of the region is occupied by dry lakes composed of hard crust and sticky mud, and occasionally filled with water.

The depression was initiated by either wind or fluvial erosion in the late Neogene, but during the Quaternary the dominant mechanism has been a combination of salt weathering and wind erosion working together. First, the salts break up the depression floor, then the wind blows away the resulting sands. This process is less effective in the eastern part of the depression, due to lower salinity groundwater.[4]

Ecology

View of the Qattara Depression
Sand dunes in the Qattara Depression

Groves of Acacia raddiana, growing in shallow sandy depressions, and Phragmites swamps represent the only permanent vegetation. The acacia groves vary widely in biodiversity and rely on runoff from rainfall and groundwater to survive. The Moghra Oasis in the northeast of the Depression has a 4 km2 brackish lake and a Phragmites swamp.[5][6]

The south western corner of the depression is part of the Siwa Protected Area which protects the wild oasis in and around the Siwa Oasis.

The Depression is an important habitat for the cheetah, with the largest number of recent sightings being in areas in the northern, western and northwestern part of the Qattara Depression, including the highly isolated, wild oases of Ain EI Qattara and Ein EI Ghazzalat and numerous acacia groves both inside and outside the depression.[7]

Gazelles (Gazella dorcas and Gazella leptoceros) also inhabit the Qattara Depression, being an important food source for the cheetah. The largest gazelle population exists in the southwestern part of the Qattara Depression within a vast area of wetlands and soft sand. The area of 900 square kilometres (350 sq mi), includes the wild oases of Hatiyat Tabaghbagh and Hatiyat Umm Kitabain, and is a mosaic of lakes, salt marshes, scrubland, wild palm groves and Desmostachya bipinnata grassland.[7]

Other common fauna include the Cape hare (Lepus capensis), Egyptian jackal (Canis aureus hupstar), sand fox (Vulpes rueppelli) and more rarely the fennec fox (Vulpes zerda). Barbary sheep (Ammotragus lervia) were once common throughout but now are few in numbers.

Extinct species from the area include the scimitar oryx (Oryx dammah), addax (Addax nasomaculatus) and bubal hartebeest (Alcelaphus buselaphus).[8] Also the Droseridites baculatus, an extinct plant known only from fossils of its pollen, was found at the Ghazalat-1 Well.[9]

Climate

The climate of the Qattara Depression is highly arid with annual precipitation between 25 and 50 mm on the northern rim to less than 25 mm in the south of the depression. The average daily temperature averages between 36.2 to 6.2 °C (97.2 to 43.2 °F) during summer and winter months. The prevailing wind comes from the north varying between north easterly and westerly directions. Wind speeds peak in March with of 11.5 m/s (25.7 mph) and minimal in December with 3.2 m/s (7.2 mph).[4] The average wind speed is about 5–6 m/s (11.2-13.4 mph).[10]

Land use

There is one permanent settlement in the Qattara Depression, the Qara Oasis. The oasis is located in the westernmost part of the depression and is inhabited by about 300 people.[11] The Depression is also inhabited by the nomadic Bedouin people and their flocks, with the uninhabited Moghra oasis being important in times of water scarcity during the dry seasons.

The Qattara Depression contains many oil concessions and several operating fields. Drillers include Royal Dutch Shell and the Apache Corporation.

History

Measurement

The altitude of the depression was first measured in 1917 by an officer of the British Army leading a light car patrol into the region. The officer took readings of the height of the terrain with an aneroid barometer on behalf of Dr. John Ball, who later would also publish on the region. He discovered that the spring Ain EI Qattara lay about 60 metres (200 ft) below sea level. Because the barometer got lost and the readings were so unexpected, this find had to be verified. In 1924-25, Ball again organised a survey party, this time with the sole purpose to triangulate the elevation on a westerly line from Wadi El Natrun. The survey was led by G.F. Walpole who had already distinguished himself by triangulating the terrain across 500 km from the Nile to Siwa via Bahariya. He confirmed earlier readings and proved the presence of a huge area below sea level, with places as deep as -133 m.[3]

Knowledge about the geology of the Qattara Depression was greatly extended by Ralph Alger Bagnold, a British military commander and explorer, through numerous journeys in the 1920s and 1930s. Most notable was his 1927 journey during which he crossed the depression east to west and visited the oasis of Qara and Siwa. Many of these trips used motor vehicles (Ford Model-Ts) which used special techniques for driving in desert conditions. These techniques were an important asset of the Long Range Desert Group which Bagnold founded in 1940.[12]

After the discovery of the depression, Ball published the triangulation findings about the region on October 1927 in The Geographical Journal. He also gave the region its name 'Qattara' after the spring Ain EI Qattara where the first readings were taken. The name literally means 'dripping' in Arabic. Six years later in 1933, Ball was the first to publish a proposal for flooding the region to generate hydro power in his article "The Qattara Depression of the Libyan Desert and the possibility of its utilisation for power-production".[3]

WWII

During World War II, the depression's presence shaped the 1st and 2nd Battles of El Alamein. It was considered impassable by tanks and most other military vehicles because of features such as salt lakes, high cliffs and/or escarpments, and fech fech (very fine powdered sand). The cliffs in particular acted as an edge of the El Alamein battlefield, which meant the British position could not be outflanked. Both Axis and Allied forces built their defences in a line from the Mediterranean Sea to the Qattara Depression. These defences became known as the Devil's gardens and are for the most part still there, especially the extensive minefields. No large army units entered the Depression, although German Afrika Korps patrols and the British Long Range Desert Group did operate in the area, as these small units had considerable experience in desert travel.[12][13] The RAF's repair and salvage units (e.g. 58 RSU) used a route through the depression in order to salvage or recover aircraft that had put down in the Western desert away from the coastal plain. The RSUs included a 6-wheel drive truck, Coles crane, and large trailer, and were particularly active from mid-1941 when Air Vice-Marshal G.G. Dawson arrived in Egypt to address the lack of serviceable aircraft.[14]

The German officer stationed in the depression was cited by Gordon Welchman as helpful in the breaking of the Enigma machine code, due to his regular transmissions stating there was "nothing to report".[15]

Qattara Depression Project

The large size of the Qattara Depression and the fact that it falls to a depth of 133 m below mean sea level has led to several proposals to create a massive hydroelectric project in northern Egypt rivalling the Aswan High Dam. This project is known as the Qattara Depression Project. The proposals call for a large canal or tunnel being excavated from the Qattara due north of 55 to 80 kilometres (34 to 50 mi) depending on the route chosen to the Mediterranean Sea to bring seawater into the area.[16] An alternative plan involved running a 320 kilometre (200 mile) pipeline north-east to the freshwater Nile River at Rosetta.[17][18] Water would flow into a series of hydro-electric penstocks which would generate electricity by releasing the water at 60 m below sea level. Because the Qattara Depression is in a very hot dry region with very little cloud cover, the water released at the −70 metres (−230 ft) level would spread out from the release point across the basin and evaporate from solar influx. Because of evaporation, more water can flow into the depression, thus forming a constant source of energy. Eventually this would result in a hyper-saline lake or a salt pan as the water evaporates and leaves the salt it contains behind.

Plans to use the Qattara Depression for the generation of electricity date back to 1912 from Berlin geographer Professor Penck.[19] The subject was discussed in more detail by Dr. John Ball in 1927.[20] In 1957 the American Central Intelligence Agency proposed to President Dwight Eisenhower that peace in the Middle East could be achieved by flooding the Qattara Depression. The resulting lagoon, according to the CIA, would have four benefits:[21]

In the 1970s and early 1980s, several proposals to flood the area were made by Friedrich Bassler and the Joint Venture Qattara, a group of mainly German companies. They wanted to make use of peaceful nuclear explosions to construct a tunnel, drastically reducing construction costs compared to conventional methods. This project proposed to use 213 devices, with yields of 1 to 1.5 megatons detonated at depths of 100 to 500 metres (330 to 1,640 ft). This fit within the Atoms for Peace program proposed by President Dwight Eisenhower in 1953. Because of this frightening solution, the Egyptian government turned down the plan.[22]

Planning experts and scientists intermittently put forward potentially viable options, whether of a tunnel or canal, as an economic, ecological and energy solution in Egypt, often coupled with the idea of new settlements.[23]

References

  1. ↑ Dr. Andrew, J. 2007. Report on the Qattara Depression CIAT Land Use project
  2. ↑ Dr. Ball, J. 1933. http://www.jstor.org/pss/1785898 "The Qattara Depression of the Libyan Desert and the Possibility of Its Utilization for Power Production" The Geographical Journal.
  3. 1 2 3 El Bassyony, Abdou. 1995. "Introduction to the geology of the Qattara Depression," International Conference on the Studies and Achievements of Geosciences in Egypt, 69 (85-eoa)
  4. 1 2 Aref M.A.M., El-Khoriby E., Hamdan M.A. 15 June 2002. The role of salt weathering in the origin of the Qattara Depression, Western Desert, Egypt. Geomorphology, Volume 45, Issues 3-4, Pages 181-195.
  5. ↑ Hughes, R. H. and J. S. Hughes. 1992. A Directory of African Wetlands. IUCN, Gland, Switzerland. ISBN 2-88032-949-3.
  6. ↑ Nora Berrahmouni and Burgess, Neil. 2001. "Saharan halophytics". Terrestrial Ecoregions. World Wildlife Fund.
  7. 1 2 Saleh, M.A., Helmy, I. and Giegengack. 2001. The Cheetah, "Acinonyx jubatus" (Schreber, 1776) in Egypt (Felidae, Acinonychinae). "Mammalia" 65 (2): 177-194.
  8. ↑ Manlius, M., Menardi-Noguera, A. and Andras Zboray, A. 2003. Decline of the Barbary sheep (Ammotragus lervia) in Egypt during the 20th century: literature review and recent observations. J. Zool. (London) 259: 403–409.
  9. ↑ Ibrahim, M.I.A. (1996). "Aptian-Turonian palynology of the Ghazalat-1 Well (GTX-1), Qattara Depression, Egypt". Review of Palaeobotany and Palynology. 94 (1–2): 137–168. doi:10.1016/0034-6667(95)00135-2.
  10. ↑ Mortensen N.G, Said U.S, Badger J. 2006. Wind Atlas for Egypt: Measurements, Micro- and Mesoscale Modeling. New and Renewable Energy Authority, Cairo, Egypt
  11. ↑ Kjeilen, Tore Looklex report on the Qara oasis, date unknown
  12. 1 2 Bagnold, R.A. 1931. Journeys in the Libyan Desert, 1929 and 1930. The Geographical Journal 78(1): 13-39; (6):524-533.
  13. ↑ Jorgensen, C. (2003). Rommel's panzers: Rommel and the Panzer forces of the Blitzkrieg, 1940-1942 (pp. 78–79). St. Paul, MN: MBI.
  14. ↑ Richards, D., Saunders, H. (1975). Royal Air Force 1939-45 Vol II (pp 160-167). Stationery Office Books
  15. ↑ Lee, Lloyd (1991). WWII: Crucible of the Contemporary World : Commentary and Readings. M.E. Sharpe. p. 240.
  16. ↑ Ragheb, M. 2010. Pumped Storage Qattara Depression Solar Hydroelectric Power Generation.pdf Archived 18 December 2012 at the Wayback Machine.. Published on 28 October 2010.
  17. ↑ Mahmoud, Mohamed. The River Nile - Qattara Depression Pipeline, June 2009
  18. ↑ User:TGCP Great Circle Mapper - Rosetta to Qattara, 2011
  19. ↑ Murakami M. Managing water for peace in the Middle East United Nations University Press. p.64-66
  20. ↑ Ball, John. 1927. "Problems of the Libyan Desert: Geographical Journal"
  21. ↑ MI: Gale. 2009. Farmington Hills, CIA Suggestions, Document Number CK3100127026. Reproduced in "Declassified Documents Reference System"
  22. ↑ Badescu, Viorel. 2011. Macro-Engineering Seawater In Unique Environments 1st Edition., 2011, XXXIX, 790 p. Springer
  23. ↑ Kelada, Maher. Global Hyper Saline Power Generation Qattara Depression Potential MIK Technology

Further reading

Wikimedia Commons has media related to Qattara Depression.
This article is issued from Wikipedia - version of the 11/18/2016. The text is available under the Creative Commons Attribution/Share Alike but additional terms may apply for the media files.