- Afar Depression
The Afar Depression (also called the Danakil Depression or the Afar Triangle) is a
geological depression in theHorn of Africa , where it overlapsEritrea , the Afar Region ofEthiopia , andDjibouti . Afar is well known as one of the cradles ofhominid s, containing theMiddle Awash , site of many fossil hominid discoveries; Gona, site of the world's oldest stone tools; and Hadar, site of Lucy, the fossilized specimen of "Australopithecus afarensis ".The Afar Depression includes the
Danakil Desert and the lowest point inAfrica , Lake Asal (–155meter s or –500 ft). Dallol is also part of the Depression, one of the hottest places year-round anywhere onEarth . The climate varies from around 25 °C (77 °F) during therainy season (September –March ) to 48 °C (118 °F) during thedry season (March–September). Only theAwash River flows into the depression, where it ends in a chain of lakes that increase insalinity .Environment
The lowlands of the Afar Depression are dominated by heat and
drought . There is no rain for most of the year, and yearly rainfall averages range from 100 to 200 millimetres (4 to 7 in), with less rain falling closer to the coast. TheAwash River , flowing north-eastward through southern Afar, provides a narrow green belt and enables life for the flora and fauna in the area and for theAfars , the nomadic people living in the Danakil desert. About 128 kilometres (79 miles) from theRed Sea , the Awash ends in a chain of salt lakes, where its water evaporates as quickly as it is supplied. About 1200 km² (463 sq mi) of the Afar Depression is covered bysalt , and salt mining is still a major source of income for many Afar tribes.The Afar Depression
biome is characterized as desert scrubland. Vegetation is mostly confined to drought-resistant plants such as small trees (e.g. species of thedragon tree ), shrubs, and grasses. Wildlife includes manyherbivore s such asGrevy's Zebra , Soemmering’s Gazelle, Oryx Beisa and, notably, the last viable population ofAfrican wild ass ("Equus africanus somalicus"). Birds include theostrich , the endemic Archer'slark ("Heteromirafra archeri"), theSecretary Bird , Arabian and Koribustard s,Abyssinian Roller and Crested Francolin. In the southern part of the plain, in Ethiopia, lies theMille-Sardo Wildlife Reserve (established 1973). Many fossils have been found in the Awash region, not onlyhominid s but also elephantoids,crocodile s andhippopotamus .According to proponents of the
aquatic ape hypothesis , the depression formed a small sea roughly 8 million years ago. The theory proposes to explain certain human characteristics (e.g.hairlessness ,biped ality) in terms ofadaptation to this semi-aquatic environment. [http://www.primitivism.com/aquatic-ape.htm]Geology
The Afar Depression results from the presence of a tectonic
triple junction (theAfar Triple Junction ) where the spreading ridges that are forming theRed Sea and theGulf of Aden emerge on land and meet the East African Rift. The central meeting place for these three pieces of Earth's crust is aroundLake Abbe . The Afar Depression is one of two places on Earth where amid-ocean ridge can be studied on land, the other beingIceland .In the Depression, the earth's crust is slowly rifting apart at a rate of 1–2 centimetres (0.3–0.8 in) per year along each of the three rifts which form the "legs" of the triple junction. The immediate consequence of this is that there are (as of late 2005) a continuous sequence of earthquakes, fissures hundreds of metres long and deep appearing in the ground, and the valley floor sinking as much as 100 metres. Between September and October 2005, 163 earthquakes of magnitudes greater than 3.9 and a volcanic eruption occurred within the Afar rift. 2.5 cubic kilometers of molten rock was injected into the plate along a dyke between depths of 2 and 9 km, forcing open an 8 meter wide gap on the surface. [cite journal | last = Wright | first = T.J. | coauthors = et al. | year = 2006 | month = July | title = Magma-maintained rift segmentation at continental rupture in the 2005 Afar dyking episode | journal = Nature | volume = 442 | pages = 291–294 | doi = 10.1038/nature04978]
Over millions of years, geologists expect the
Red Sea to erode through the highlands surrounding the Afar Depression and flood the valley. In about 10 million years, geologists predict that the whole 6,000 km length of the East African Rift will be submerged, forming a new sea as large as the Red Sea is now. At that point, Africa will have lost its horn. [Bojanowski 2006]The floor of the Afar Depression is composed of
lava , mostlybasalt . One of Earth's great active volcanoes,Erta Ale , is found here. The Afar Depression is, in the views of some geologists, underlain by amantle plume , a great upwelling of mantle that melts to yield basalt as it approaches the surface.ee also
*
List of fossil sites "(with link directory)"
* List of hominina (hominid) fossils "(with images)"Footnotes
References
* Alebachew Beyene and Mohamed G. Abdelsalam, 2005. "Tectonics of the Afar Depression: A review and synthesis." "
Journal of African Earth Sciences ", Volume 41, Issues 1-2, pp 41-59
* Kloos, Helmut (1982) 'Development, drought and famine in the Awash valley of Ethiopia', "African Studies Review ", vol. 25, no. 4, p. 21-48.
*World Wildlife Fund (2001) 'Ethiopian xeric grasslands and shrublands (AT1305)' [http://www.worldwildlife.org/wildworld/profiles/terrestrial/at/at1305_full.html online version] .
* Includes a photo essay of the region and its geologic changes.External links
* [http://www.erta-ale.org/photos_volcan.html Photos of Erta Ale]
* [http://www.erta-ale.org/photos_dallol.html Hotsprings at Dallol]
* [http://www.ethiopar.net/type/English/basinfo/infoafar.htm#TopClimate The Ethiopian state of Afar: Topography and Climate]
* [http://www.newscientist.com/channel/opinion/mg18725162.000.html Danakil in New Scientist]
* [http://danakil.ethiopia.free.fr Photos of Afar Depression: between Ethiopia and Djibouti]
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