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59-540: The Awash River is the main waterflow into the region, but it runs dry during the annual dry season, and ends as a chain of saline lakes . The northern part of the Afar Depression is also known as the Danakil Depression . The lowlands are affected by heat, drought , and minimal air circulation, and contain the hottest places (year-round average temperatures) of anywhere on Earth. The Afar Triangle

118-678: A 4.4 million-year-old likely human ancestor. Prior to that discovery, his early career was notable for his work on Lucy as Australopithecus afarensis with discoverer Donald Johanson . Timothy Douglas White was born on August 24, 1950, in Los Angeles County , California and raised in Lake Arrowhead in neighboring San Bernardino County . He majored in biology and anthropology at the University of California, Riverside . He received his Ph.D. in physical anthropology from

177-503: A cause of heavy metal pollution (As, Cd, Cu, Pb, U, and Zn) in aquatic bodies, and industrial disposal could also lead to high heavy metals concentrations such as As, Cd, Cr, Hg, Ni, Zn, and Pb concentrations. A study of river water quality in 2023 showed that high levels of heavy metals, such as Al, Mn, Mo, As, V, Fe, and Ba were exhibited with values of 1257 μg/L, 626.8 μg/L, 116.7 μg/L, 61.2 μg/L, 100.5 μg/L, 1082.7 μg/L, and 211.7 μg/L, respectively. Among 20 heavy metals analyzed, 20% of

236-665: A female hominin which he named " Ardi ", it took nearly 15 years to safely excavate, preserve, and describe the specimen and to prepare publication of the event. The Afar Depression is the product of a tectonic triple-rifts junction (the Afar triple junction), where the spreading ridges forming the Red Sea and the Gulf of Aden emerge on land and meet the East African Rift . The conjunction of these three plates of Earth's crust

295-429: A few exceptions of small eucalyptus plantations. Outside of Awash National Park the open and woody savannas have been almost completely cultivated with crops. This especially accounts for all escarpment terraces. Thereby the scattered tree cover remained similar to the primary state of the savannas, while the grass layer has been replaced by crops. Only highest altitudes still show connected woodlands. Partly reforestation

354-549: A job at the University of California, Berkeley in 1977 and collaborated with J. Desmond Clark and F. Clark Howell . In 1994, White discovered 4.4 million-year-old Ardipithecus ramidus , a likely human ancestor from an era which was previously empty of fossil evidence. Near the Awash River in Ethiopia, he found an almost complete fossilized female skeleton, named " Ardi ". He took nearly 15 years to prepare publication of

413-594: A role in the Main Ethiopian Rift and in southern Afar. The Awash Basin is a densely populated and industrialized area where numerous enterprises rely on groundwater for their operation. Therefore, the majority of human development initiatives in the basin will continue to depend heavily on the quantity and quality of groundwater. Groundwater management requires proactive measures due to the global challenges posed by rapid population growth, urbanization, climate change, and various human activities. Most of

472-474: A severe drought and a humanitarian response targeting over 10 million people nationally, with many priority districts located in the Awash basin. Municipal and industrial wastewater treatment plants are scant and inefficient in the Awash River basin. Where they exist, their effluents (often poorly treated) are channeled into nearby streams, thus polluting them. Growing industrialization and urbanization in

531-407: A study in 2023 in the river and shallow groundwater systems: "Pesticides, veterinary drugs , artificial sweeteners , and personal care products were detected in samples from all sources (surface, ground, and tap water). Endocrine disruptors and equine drugs were found in both surface and groundwater sources." The river water and shallow groundwater are intrinsically connected. Contaminants in

590-402: Is 'flood-centric' in its thinking and approach [...]. This means identifying (and protecting) flood zones near build-up areas and identifying zones that can be allowed to flood to absorb the impact of extreme events." Groundwater recharge varies between values exceeding 350 millimetres (14 in) per year in the upper highlands and no recharge at the bottom of the rift valley. Groundwater

649-689: Is a dry season, called Bega . Semi-arid to arid conditions prevail in the Rift Valley. In contrast, the highlands partly receive more than 1,600 millimetres (63 in) of rainfall in ca. six months per year. A study in 2018 investigated the effects of climate change on water resources in the Awash basin. They used three climate models from Coupled Models Intercomparison Project phase 5 (CMIP5) and for three future periods (2006–2030, 2031–2055, and 2056–2080). The models were selected based on their performance in capturing historical precipitation characteristics. The baseline period used for comparison

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708-419: Is a major river of Ethiopia . Its course is entirely contained within the boundaries of Ethiopia and empties into a chain of interconnected lakes that begin with Lake Gargori and end with Lake Abbe (or Abhe Bad) on the border with Djibouti , some 100 kilometres (60 or 70 miles) from the head of the Gulf of Tadjoura . The Awash River is the principal stream of an endorheic drainage basin covering parts of

767-830: Is bordered as follows (see the topographic map): on the west by the Ethiopian Plateau and escarpment ; to the north-east (between it and the Red Sea) by the Danakil block ; to the south by the Somali Plateau and escarpment; and to the south-east by the Ali-Sabieh block (adjoining the Somali Plateau). Many important fossil localities exist in the Afar region, including the Middle Awash region and

826-551: Is composed of lava , mostly basalt . One of Earth's five lava lakes , Erta Ale is found here, as well as Dabbahu Volcano. It has been proposed that the Afar Depression is underlain by a mantle plume , a great upwelling of mantle that melts to yield basalt as it approaches the surface. 11°30′N 41°00′E  /  11.5°N 41.0°E  / 11.5; 41.0 Awash River The Awash River (sometimes spelled Awaash ; Oromo : Awaash OR Hawaas , Amharic : ዐዋሽ, Afar : Hawaash We'ayot , Somali : Webiga Dir )

885-483: Is different for the upper, middle and lower Awash basin. Research has found that "the type and range of flooding in the Awash Basin varies widely reflecting the basin’s complex geography". For example, in urban areas, flash floods and river overflows are known to occur. Rapid growth of agriculture, industries and urbanization within the Awash basin, as well as population growth is placing increasing demands on

944-478: Is mostly confined to drought-resistant plants such as small trees (e.g. species of the dragon tree ), shrubs, and grasses. Wildlife includes many herbivores such as Grévy's zebra , Soemmerring's gazelle , beisa and, notably, the last viable population of African wild ass ( Equus africanus somalicus ). Birds include the ostrich , the endemic Archer's lark , the secretary bird , Arabian and Kori bustards , Abyssinian roller , and crested francolin . In

1003-484: Is near Lake Abbe . The Afar Depression is one of two places on Earth where a mid-ocean ridge can be studied on land, the other being Iceland . Within the triangle, the Earth's crust is slowly rifting apart at a rate of 1–2 cm (0.4–0.8 in) per year along each of the three rift zones forming the "legs" of the triple junction. The immediate consequences are recurring sequences of earthquakes with deep fissures in

1062-521: Is partly located in the Main Ethiopian Rift . The Awash River is 1,200 kilometers long. It starts in Ethiopia’s central highlands at an elevation of 3000 m and passes through a number of locations before joining Lake Abbe at a height of 250 m. The Awash River basin is divided into three sections: upper, middle, and lower. The Awash rises south of Mount Warqe , west of Addis Ababa in

1121-487: Is placing increasing demands on the basin’s water resources . The main sources of water pollution in the upper Awash River basin come from industrial and urban wastes, agricultural runoff ( pesticides , fertilizers ), and sewage discharge. Polluting industries in the Awash River basin include tanneries , paint factories, slaughterhouses , textiles , breweries , soft drink factories, sugar factories, hospitals, and pharmaceuticals. The Awash Valley (and especially

1180-425: Is predominantly recharged at the escarpments and highlands above 1,900 m a.s.l., where annual rainfall is higher than 1,000 millimetres (39 in). Localized small-scale recharge is also supposed to occur at the flanks of the rift valley volcanoes. Artificial groundwater recharge takes further place at irrigated plantations at the rift valley. Recharge from river channel losses and via infiltration from lakes plays

1239-627: Is then joined on its left bank by its chief affluent, the Germama (or Kasam) River, before turning northeast at approximately 11° N 40° 30' E as far north as 12° before turning completely east to reach lake Gargori. Other tributaries of the Awash include (in order upstream): the Logiya , Mille , Borkana , Ataye , Hawadi , Kabenna and Durkham Rivers . Towns and cities along its course include Metehara , Awash , Gewane and Asaita . There are tributary rivers, lakes, hot springs , and swamps in

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1298-521: The Amhara , Oromia and Somali Regions , as well as the southern half of the Afar Region . The Awash River basin, spanning 23 administrative zones, covers 10% of Ethiopia's area. The basin usually has two rainy seasons, a shorter one around March ( Belg ), and a longer one between June and September ( Kiremt ), which partly fall into one longer rainy season. Climate change is predicted to increase

1357-483: The Danakil Desert . About 128 kilometres (80 mi) from the Red Sea the Awash ends in a chain of salt lakes, where its waterflow evaporates as quickly as it is supplied. Some 1,200 km (460 sq mi) of the Afar Depression is covered by salt deposits, and mining salt is a major source of income for many Afar groups. The Afar Depression biome is characterized as desert scrubland . Vegetation

1416-498: The Gawis cranium hominin from Gona ; several sites of the world's oldest stone tools; Hadar , the site of Lucy , the fossilized specimen of Australopithecus afarensis ; and Dikika , the site of the fossilized child Selam , an australopithecine hominin. In 1994, near the Awash River in Ethiopia, Tim D. White found the then-oldest known human ancestor: 4.4 million-year-old Ar. ramidus . A fossilized almost complete skeleton of

1475-575: The Koka Reservoir ), has an area of about 180 square kilometres (69 sq mi). Both lake and dam are threatened by increasing sedimentation . The valley of the Awash from about 9° N downstream is the traditional home of the Afar people and Issa people . The valley of the Awash have been included as part of the Fatagar , Ifat , and Shewa . The Awash International Bank is named after

1534-615: The Middle Awash ) is internationally famous for its high density of hominin fossils, offering unparalleled insight into the early evolution of humans . " Lucy ", one of the most famous early hominin fossils, was discovered in the lower Awash Valley. For its paleontological and anthropological importance, the lower valley of the Awash was inscribed on the UNESCO World Heritage List in 1980. The Awash River basin, spanning 23 administrative zones, covers 10% of Ethiopia's area and hosts about 17% of its population. It

1593-718: The National Center for Science Education . White has been accused of mistreating and misappropriating Indigenous people's remains. Some representatives of Indigenous Nations of California protest that he failed to comply with the Native American Graves Protection and Repatriation Act (NAGPRA), though no court has made such a finding. Laura Miranda, chair of the California Native American Heritage Commission, opined that his breach of NAGPRA's codes

1652-628: The University of Michigan . White took a position in the Department of Anthropology at the University of California, Berkeley in 1977, later moving to the university's Department of Integrative Biology. White taught courses on human paleontology and human osteology. He is a professor emeritus having retired in the spring of 2022. He is director of the Human Evolution Research Center and co-director, with Berhane Asfaw , Yonas Beyene , and Giday WoldeGabriel , of

1711-558: The woreda of Dandi , close to the town of Ginchi , West Shewa Zone , Oromia . After entering the bottom of the Great Rift Valley , the Awash flows south to loop around Mount Zuqualla in an easterly then northeasterly direction, before entering Koka Reservoir . There, water is used for the irrigation of sugar cane plantations. Downstream, the Awash passes the city of Adama and the Awash National Park . It

1770-551: The Awash River basin has severely damaged the ecosystem due to the toxins discharged into water bodies. The main sources of water pollution in the upper Awash River basin come from industrial and urban wastes, agricultural runoff ( pesticides , fertilizers ), and sewage discharge. Both anthropogenic and geogenic activities contribute to the observed water quality degradation. The term geogenic refers to naturally occurring contamination through tectonic, clay, volcanic ash, and sand weathering phenomena. Heavy metal pollution in

1829-422: The Awash River. 11°06′00″N 40°34′46″E  /  11.10000°N 40.57944°E  / 11.10000; 40.57944 Tim D. White Tim D. White (born August 24, 1950) is an American paleoanthropologist and Professor of Integrative Biology at the University of California, Berkeley . He is best known for leading the team which discovered Ardi , the type specimen of Ardipithecus ramidus ,

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1888-593: The Awash basin is part of the Ethiopian montane forests ecoregion. At high altitudes the Ethiopian montane grasslands and woodlands and Ethiopian montane moorlands predominate. The Somali Acacia–Commiphora bushlands and thickets ecoregion occupies low elevations in the Rift. The basin's vegetation has a strong anthropogenic impact. All over the upper and central Awash basin, remains of different savanna types are still clearly visible. They range from thorn savannas in

1947-432: The Awash basin. Recurrent extreme wet and dry weather events challenge economic activities in the basin. The large portion of rural poor engaged in rainfed agriculture in the drought-prone marginal lands located in the middle and lower reaches of the basin suffer greatly from recurring drought. Climate variability already has a severe impact on populations and economic productivity in the Awash basin. Severe droughts in

2006-667: The Middle Awash Basin. The climate of the Awash River basin is mostly influenced by the movement of the intertropical convergence zone (ITCZ). During its movement northwards in March/April and its retreat southwards, ITCZ creates two rainy seasons, a shorter one around March ( Belg ), and a longer one between June and September ( Kiremt ), which partly fall into one longer rainy season. The rainy season tends to be bimodal towards eastern Ethiopia and almost unimodal towards western Ethiopia. The time between October and March

2065-611: The Middle Awash Research Project. White has taught and mentored many paleoanthropologists who have subsequently gone on to prominence in the field, including Berhane Asfaw , William Henry Gilbert, Yohannes Haile-Selassie , and Gen Suwa and thousands of undergraduate and graduate students at the University of California, Berkeley. Since 2013, White has been listed on the Advisory Council of

2124-636: The Red Sea to breach the highlands surrounding the Afar Depression and flood the valley. Geologists predict that in about 10 million years the whole 6,000 km (3,700 mi) length of the East African Rift will be submerged, forming a new ocean basin as large as today's Red Sea, and separating the Somali plate and the Horn of Africa from the rest of the continent. The floor of the Afar Depression

2183-426: The basin have led to a significant depression of crop yields and death of livestock, resulting in increases in food insecurity . A modest (5%) decrease in rainfall was estimated to reduce the basin’s gross domestic product (GDP) 5%, with a 10% decrease in agricultural productivity. Humanitarian assistance requests are relatively common due to climate shocks , such as the 2015/2016 El Niño events which resulted in

2242-578: The basin, further threatening water security for different sectors. Rainfall varies a lot in the basin from one year to the next (this is called high intra-annual variability ). Dry season water shortage is recognized as a challenge for various activities such as irrigation and domestic water supply by the Awash Basin Authority. However, flooding also occurs frequently during the main rainy season in July and August. The type of flooding

2301-408: The basin’s water resources. The basin is known for high climate variability involving droughts and floods, and climate change will likely intensify the existing challenges. Future water management strategies needs to be inclusive of all sectors and consider the equity for different users. Flood adaption measures have been investigated and one of the recommendations is to use " land-use planning that

2360-422: The basis for economic growth in the coming years. Crop production in particular is a major component of the basin's economy and has seen rapid growth in recent years, with the value of output expanding by 7.9% per year in real terms between 2004 and 2014. As of 2012, the total irrigated area of the basin is less than 2% of the total area under cultivation. Forestry hardly exists inside the Awash River basin, with

2419-567: The coast. Daily mean temperatures at Dallol ranged from 30 °C (86 °F) in January to 39 °C (102 °F) in July in six years of observations from 1960 to 1966. The Awash River , flowing north-eastward through the southern part of the Afar Region, provides a narrow green belt which enables life for the flora and fauna in the area and for the Afars , the nomadic people living in

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2478-574: The explorer L. M. Nesbitt had followed parts of the course of the Awash in 1928, he turned away from the river at Asaita and proceeded north through the Afar Depression to the Red Sea. ) In 1960, the Koka Dam was completed across the Awash River at a point around 75 kilometres (47 mi) from Addis Ababa. With its opening, it became a major source of hydroelectric power in the area. The resulting freshwater lake, Lake Gelila (also known as

2537-562: The groundwater sources were unsuitable for drinking, posing significant health risks to local communities that rely heavily on these sources due to limited access to clean surface water. In the Middle Awash Basin and the country at large, the water quality of most groundwater sources is inadequately monitored and insufficiently regulated. Consequently, areas within the upstream Awash Basin, particularly around Modjo, Bishoftu, Gelan, and Addis Ababa, are highly susceptible to unregulated abstraction and pollution of groundwater. Humans have lived in

2596-407: The irrigation waters for local and commercial agricultural lands (such as sugarcane plantation) depend on the Awash River and its tributaries. The Awash basin's economy is dominated by the agricultural and service sectors, with the latter prevailing in the large urban center of Addis Ababa . Agriculture dominates water use (about 89% of total water use in the basin) and is expected to continue to be

2655-631: The lower rift, bush, grass and open savannas above 800 m and woody savannas on the escarpments and the highlands. The lower Awash Valley is one of the last wildlife preserves for the African wild ass . The mammal is now extinct in Yangudi Rassa National Park , but still found in the adjacent Mille-Serdo Wildlife Reserve . Other large animals native to the area include Beisa Oryx , Soemmering's gazelle , Dorcas gazelle , gerenuk and Grevy's zebra . Crocodiles also flourish within

2714-636: The parameters within the study area were above the WHO limit for drinking water ; Al (157 μg/L), V (100.5 μg/L), Fe (1082.7 μg/L), Mn (626.8 μg/L), and Mo (103.8 μg/L) were exhibited at sites along the river system. This is a problem as water from the river is used as a source of drinking water and irrigation . The presence of emerging organic contaminants in the river water is another concern. These substances include pharmaceuticals, personal care products , industrial byproducts, and agricultural chemicals. High levels of emerging organic contaminants were detected in

2773-442: The river water can pollute the groundwater and vice versa. A study in 2024 investigated the characteristics of groundwater in a region of Middle Awash for multipurpose use. It found that contaminants such as arsenic, vanadium, gallium, lithium, rubidium, chromium, manganese, copper, and zinc were found enriched in groundwater near Lake Beseka, majorly influenced by geogenic activities, volcanic ash, and weathering of rocks. Over half of

2832-429: The river. The Awash basin is the most developed, utilized, abused, impacted, and most populous (over 15% or nearly 18.6 million out of 120 million) basin in Ethiopia. Middle Awash is known for having both large- and small-scale irrigation, as well as agroindustry and sugar factories (Wenji, Methara, and Kesem Sugar factories). The water supplies of the major urban centers like Addis Ababa, Mojo and Adama, and also,

2891-611: The site include Homo erectus and Ardipithecus . In the 16th century the Awash River was called the great Dir river and lay in the country of the Muslims. The first European to trace the course of the Awash to its end in the Aussa oasis was Wilfred Thesiger in 1933/1934, who started at the city of Awash, followed the river's course to its final end in Lake Abhebad, and continued his expedition east to Tadjoura . (Although

2950-518: The sites of Hadar , Dikika , and Woranso-Mille. These sites have produced specimens of the earliest (fossil) hominins and of human tool culture, as well as many fossils of various flora and fauna. Dallol in the Danakil Depression is one of the hottest places year-round anywhere on Earth. There is no rain for most of the year; the yearly rainfall averages range from 100 to 200 mm (4 to 8 in), with even less rain falling closer to

3009-493: The southern part of the plain lies the Mille-Serdo Wildlife Reserve . The Afar Triangle is a cradle source of the earliest hominins . It contains a paleo-archaeological district that includes the Middle Awash region and numerous prehistoric sites of fossil hominin discoveries, including: the hominids and possible hominins, Ardi , or Ardipithecus ramidus , and Ardipithecus kadabba , see below;

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3068-446: The surface water has become a growing concern for the environment and people’s health. Polluting industries in the Awash River basin include tanneries , paint factories, slaughterhouses , textiles , breweries , soft drink factories, sugar factories, hospitals, and pharmaceuticals. Wastewater enters the river from cities such as Addis Abeba , Awash 7 Kilo, Ambo, Sebeta , Bishoftu , Gelan, Adama , Modjo. Agricultural runoff may be

3127-549: The surface, known as the Dabbahu fissure . Related eruptions have taken place in Teru and Aura woredas . The rift has recently been recorded by means of three-dimensional laser mapping. The region's salt deposits were created over time as water from the Red Sea periodically flooded the depression and evaporated; the most recent such flood was roughly 30,000 years ago. Over the next millions of years, geologists expect erosion and

3186-481: The terrain hundreds of metres long, and the valley floor sinking broadly across the depression. During September and October 2005 some 163 earthquakes of magnitudes greater than 3.9 and a volcanic eruption occurred within the Afar rift at the Dabbahu and Erta Ale volcanoes. Some 2.5 cubic kilometers of molten rock was injected from below into the plate along a dyke between depths of 2 and 9 km (1 and 6 mi), forcing open an 8 m (26 ft) wide gap on

3245-499: The valley of the Awash almost since the beginning of the species. Numerous pre-human hominid remains have been found in the Middle Awash . The remains found in the Awash Valley date from the late Miocene , Pliocene , and early Pleistocene (roughly 5.6–2.5 million years ago), and include fossils of many Australopithecines , including "Lucy", the most famous individual Australopithecus . Other extinct hominids discovered at

3304-429: The water deficiency in all seasons and for parts of the basin, due to a projected increase in temperature and decrease in precipitation. The Awash River basin is the most developed, utilized, abused, impacted, and most populous (over 15% or nearly 18.6 million out of 120 million) basin in Ethiopia (as of 2021). Rapid growth of agriculture, industries and urbanization within the Awash basin, as well as population growth

3363-540: Was "a major moral, ethical, and potentially legal violation." He has used human skeletal remains as teaching tools in classrooms within the legal framework in place at the time of his teaching activities, but has been accused of careless and negligent treatment of human remains. In 1974, White worked with Richard Leakey 's team at Koobi Fora, Kenya . Leakey was so impressed with White's work that he recommended him to his mother, Mary Leakey , to help her with hominid fossils she had found at Laetoli, Tanzania . White took

3422-582: Was 1981–2005. The future water availability was estimated as the difference between precipitation and potential evapotranspiration projections using the Representative Concentration Pathway (RCP8.5) emission scenarios. The projections for the future three periods show an increase in water deficiency in all seasons and for parts of the basin, due to a projected increase in temperature and decrease in precipitation. This decrease in water availability will increase water stress in

3481-416: Was carried out on not cultivable altitudes with secondary coniferous forests. The cultivated crops are (endemic) teff , maize, sorghum , beans and vegetables. Pastures hardly exist where agriculture is possible. The cattle graze on field edges and waysides and on steep escarpments. This is one major reason for erosion , because vegetation cover is partly destroyed. Stubble-grazing is a common practice in

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