Chott Melrhir: Difference between revisions
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|catchment = {{convert|68750|km2|sqmi|abbr=on}}<ref name=j1>{{cite journal|url=http://www.larhyss.net/pdf/journal/7/8_Benkhaled_et_al_Larhyss_Journal_7_Juin_2008.pdf|title=Detecting trends in annual discharge and precipitation in the Chott Melghir basin in Southeastern Algeria|author1=Benkhaled A. |
|catchment = {{convert|68750|km2|sqmi|abbr=on}}<ref name=j1>{{cite journal|url=http://www.larhyss.net/pdf/journal/7/8_Benkhaled_et_al_Larhyss_Journal_7_Juin_2008.pdf|title=Detecting trends in annual discharge and precipitation in the Chott Melghir basin in Southeastern Algeria|author1=Benkhaled A.|author2=Bouziane M.T|author3=Achour B.|journal=Larhyss Journal|issn=1112-3680|volume=7|date=June 2008|pages=103–119|deadurl=yes|archiveurl=https://web.archive.org/web/20100614023034/http://www.larhyss.net/pdf/journal/7/8_Benkhaled_et_al_Larhyss_Journal_7_Juin_2008.pdf|archivedate=2010-06-14|df=}}</ref><ref name=gov/> |
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==Hydrology, geology and geography== |
==Hydrology, geology and geography== |
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During the rain season in winter, the lake is filled by numerous [[wadi]] (periodically drying rivers), mostly from north and north-west. The largest of them are the [[Djedi River|Djedi]] and Arab<ref name=gov/><ref>[http://www.abhs.dz/new_site/chottmelghir.asp Chott Melhrir]</ref> running from west to east down the slopes of [[Aurès Mountains]].<ref>{{cite book|language=French|author=Jean-Louis Ballais|url=http://physio-geo.revues.org/1173|title=Des oueds mythiques aux rivières artificielles: l'hydrographie du Bas-Sahara algérien|pages=107–127}}</ref> Others include [[Abiod Valley|Abiod]], Beggour Mitta, [[Biskra Province|Biskra]], Bir Az Atrous, Cheria, Demmed, Dermoun, Derradj, Djedeida, Djemorah, Halail, Horchane, Ittel, Mechra, Melh, Mzi, Messad, Oum El Ksob, Soukies, Tadmit and Zeribet.<ref name=j1/><ref>[https://books.google.com/books?id=bxErAAAAYAAJ&pg=PA159 Annales des mines: Mémoires], Cadrilian-Gœury et Vor. Dalmont, 1880 pp. 154, 159, 172</ref> In summer, the lake and most the rivers feeding it dry out, and Chott Melrhir turns into a [[Dry lake|salt pan]].<ref name=bse/><ref>[http://www.cosmovisions.com/Algerie.htm Algérie. États et Territoires] (in French)</ref> The annual water evaporation varies between 9.6 and 20 km<sup>3</sup>, and evaporation from soil nearby the lake can reach 14 km<sup>3</sup>.<ref name=gov/> |
During the rain season in winter, the lake is filled by numerous [[wadi]] (periodically drying rivers), mostly from north and north-west. The largest of them are the [[Djedi River|Djedi]] and Arab<ref name=gov/><ref>[http://www.abhs.dz/new_site/chottmelghir.asp Chott Melhrir] {{webarchive|url=https://web.archive.org/web/20110405073204/http://www.abhs.dz/new_site/chottmelghir.asp |date=2011-04-05 }}</ref> running from west to east down the slopes of [[Aurès Mountains]].<ref>{{cite book|language=French|author=Jean-Louis Ballais|url=http://physio-geo.revues.org/1173|title=Des oueds mythiques aux rivières artificielles: l'hydrographie du Bas-Sahara algérien|pages=107–127}}</ref> Others include [[Abiod Valley|Abiod]], Beggour Mitta, [[Biskra Province|Biskra]], Bir Az Atrous, Cheria, Demmed, Dermoun, Derradj, Djedeida, Djemorah, Halail, Horchane, Ittel, Mechra, Melh, Mzi, Messad, Oum El Ksob, Soukies, Tadmit and Zeribet.<ref name=j1/><ref>[https://books.google.com/books?id=bxErAAAAYAAJ&pg=PA159 Annales des mines: Mémoires], Cadrilian-Gœury et Vor. Dalmont, 1880 pp. 154, 159, 172</ref> In summer, the lake and most the rivers feeding it dry out, and Chott Melrhir turns into a [[Dry lake|salt pan]].<ref name=bse/><ref>[http://www.cosmovisions.com/Algerie.htm Algérie. États et Territoires] (in French)</ref> The annual water evaporation varies between 9.6 and 20 km<sup>3</sup>, and evaporation from soil nearby the lake can reach 14 km<sup>3</sup>.<ref name=gov/> |
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Chott Melrhir is separated from the nearby Chott Meorouane, which lies south-west, by a stripe of permanently dry land which can be as narrow as 4 kilometers in some places.<ref name=b1/> The bottom of the lake is mostly composed of [[gypsum]] and mud and is covered in salt in summer. The lake emits a garlic-like odor.<ref>[https://books.google.com/books?id=uzgVAAAAYAAJ&pg=PA377 The Annals and magazine of natural history: zoology, botany, and geology], Taylor and Francis (1871) p. 377</ref> Although the dry soil in and around the lake appears arable, it is nearly barren due to the high concentration of salt. For the same reason, the soil absorbs much condensation overnight that keeps it partly humid during much of the day.<ref>Henry Woodward [https://books.google.com/books?id=wYcPAAAAIAAJ&pg=PA28 Geological magazine, Volume 1], Cambridge University Press., 1864, p. 28</ref> |
Chott Melrhir is separated from the nearby Chott Meorouane, which lies south-west, by a stripe of permanently dry land which can be as narrow as 4 kilometers in some places.<ref name=b1/> The bottom of the lake is mostly composed of [[gypsum]] and mud and is covered in salt in summer. The lake emits a garlic-like odor.<ref>[https://books.google.com/books?id=uzgVAAAAYAAJ&pg=PA377 The Annals and magazine of natural history: zoology, botany, and geology], Taylor and Francis (1871) p. 377</ref> Although the dry soil in and around the lake appears arable, it is nearly barren due to the high concentration of salt. For the same reason, the soil absorbs much condensation overnight that keeps it partly humid during much of the day.<ref>Henry Woodward [https://books.google.com/books?id=wYcPAAAAIAAJ&pg=PA28 Geological magazine, Volume 1], Cambridge University Press., 1864, p. 28</ref> |
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Revision as of 18:07, 25 January 2018
| Chott Melrhir | |
|---|---|
 View from space. Note that most of the lake is already dried up in this picture. | |
| Coordinates | 34°20′N 6°20′E / 34.333°N 6.333°E |
| Type | endorheic salt lake |
| Catchment area | 68,750 km2 (26,540 sq mi)[1][2] |
| Basin countries | Algeria |
| Surface area | 6,700 km2 (2,600 sq mi)[3] |
Chott Melrhir (Arabic: شط ملغيغ) also known as Chott Melghir or Chott Melhir is an endorheic salt lake in northeastern Algeria. It the westernmost part of a series of depressions, which extend from the Gulf of Gabès into the Sahara. They were created between Miocene and Early Pleistocene as a result of compression accompanying the formation of the Atlas Mountains.[4] With the maximum area of about 6,700 km2 (2,600 sq mi), Chott Melrhir is the largest lake in Algeria.[3] It lies almost entirely below the sea level and contains the lowest point in Algeria, −40 meters (−130 feet).[5] Its size varies over the year and is usually larger than 130 km (81 mi) from east to west.[6] The nearby cities are Biskra (60 km north-east), El Oued and Touggourt (85 km south).[7]
Hydrology, geology and geography
During the rain season in winter, the lake is filled by numerous wadi (periodically drying rivers), mostly from north and north-west. The largest of them are the Djedi and Arab[2][8] running from west to east down the slopes of Aurès Mountains.[9] Others include Abiod, Beggour Mitta, Biskra, Bir Az Atrous, Cheria, Demmed, Dermoun, Derradj, Djedeida, Djemorah, Halail, Horchane, Ittel, Mechra, Melh, Mzi, Messad, Oum El Ksob, Soukies, Tadmit and Zeribet.[1][10] In summer, the lake and most the rivers feeding it dry out, and Chott Melrhir turns into a salt pan.[3][11] The annual water evaporation varies between 9.6 and 20 km3, and evaporation from soil nearby the lake can reach 14 km3.[2]
Chott Melrhir is separated from the nearby Chott Meorouane, which lies south-west, by a stripe of permanently dry land which can be as narrow as 4 kilometers in some places.[7] The bottom of the lake is mostly composed of gypsum and mud and is covered in salt in summer. The lake emits a garlic-like odor.[12] Although the dry soil in and around the lake appears arable, it is nearly barren due to the high concentration of salt. For the same reason, the soil absorbs much condensation overnight that keeps it partly humid during much of the day.[13]
Climate
The climate in the Chott Melrhir is hot and arid with high evaporation and low precipitation. The average lowest and highest temperatures are 11.4 and 34.2 °C, respectively, and the minimum temperature is about 0 °C. Annual precipitation is below 160 mm. The winds have a speed between 2.7 and 5.3 m/s and are mostly directed south-east between June and September and north-west between autumn and early spring. Sandstorms are more frequent in winter and late summer and last 39 days per year on average.[1][2]
Flora and fauna
The shallow waters of the lake contain scarce vegetation composed of 72 species of plants which have adapted to salty water, such as Parish's glasswort (Arthrocnemum subterminale), sea lavender (Limonium), rushes (Juncus), glasswort (Salicornia), Sarcocornia, bulrush (Scirpus) and seepweeds (Suaeda). Some species are unique for Algeria and 14 are endemic, such as Fagonia microphylla, Oudneya africana, Zygophyllum cornutum, Limoniastrum feii and Ammosperma cinerea.[2] They grown up to 30 cm in height and host relatively rich avifauna, mostly ducks, sandgrouse, houbara bustard (Chlamydotis undulata) and greater flamingo (Phoenicopterus roseus).[7][14] Lake waters are saturated with salt with concentrations reaching 0.4 kg/L[2] and sustain only few animal species, such as brine shrimp.[15] Wild boars, golden jackals, hares and foxes were observed around the lake.[2] In June 2003, Chott Melrhir was included to the List of Ramsar wetlands of international importance.[16]
References
- ^ a b c Benkhaled A.; Bouziane M.T; Achour B. (June 2008). "Detecting trends in annual discharge and precipitation in the Chott Melghir basin in Southeastern Algeria" (PDF). Larhyss Journal. 7: 103–119. ISSN 1112-3680. Archived from the original (PDF) on 2010-06-14.
{{cite journal}}: Unknown parameter|deadurl=ignored (|url-status=suggested) (help) - ^ a b c d e f g Chott Melghir Archived November 23, 2009, at the Wayback Machine, Ministere de l’Agriculture. Direction Generale des Forets (in French)
- ^ a b c В. М. Котляков Мельгир (Chott Melrhir), Словарь современных географических названий (Dictionary of modern geographical names), 2003–2006
- ^ Andrew Goudie (2002) Great warm deserts of the world: landscapes and evolution, Oxford University Press, ISBN 0-19-924515-0, p. 113
- ^ CIA World Factbook 2010, Book 2010 ISBN 1-60239-727-9, p. 10
- ^ Chott Melrhir, Encyclopædia Britannica on-line
- ^ a b c Robert Mepham, R. H. Hughes, J. S. Hughes (1992) A directory of African wetlands, IUCN, ISBN 2-88032-949-3 pp. 23–24
- ^ Chott Melhrir Archived 2011-04-05 at the Wayback Machine
- ^ Jean-Louis Ballais. Des oueds mythiques aux rivières artificielles: l'hydrographie du Bas-Sahara algérien (in French). pp. 107–127.
- ^ Annales des mines: Mémoires, Cadrilian-Gœury et Vor. Dalmont, 1880 pp. 154, 159, 172
- ^ Algérie. États et Territoires (in French)
- ^ The Annals and magazine of natural history: zoology, botany, and geology, Taylor and Francis (1871) p. 377
- ^ Henry Woodward Geological magazine, Volume 1, Cambridge University Press., 1864, p. 28
- ^ Erik Carp (1980) Directory of wetlands of international importance in the Western Palearctic, IUCN, ISBN 2-88032-300-2, p. 28
- ^ Samraoui, Boudjéma; et al. (2006). "Large branchiopods (Branchiopoda: Anostraca, Notostraca and Spinicaudata) from the salt lakes of Algeria" (PDF). J. Limnol. 65 (2): 83–88.
- ^ The List of Wetlands of International Importance, p. 5
External links
- A detailed report on the lake by the Ministry of Agriculture of Algeria with the map of the area (in French)
