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| Uweinat | |
|---|---|
| Name | Uweinat |
| Other names | جبل العوينات, Jabal al-ʿUwaynāt, Jebel Oweinat |
| Elevation m | 1,934 |
| Range | Gilf Kebir, Sahara |
| Location | Libya–Egypt–Sudan border region |
| Coordinates | 22°N 24°E |
Uweinat is a sandstone massif located at the tri-border area of northeastern Africa, straddling the Libya, Egypt, and Sudan frontiers. The plateau is noted for its isolated mountain block, dramatic rock art, and paleohydrological features that have drawn explorers, archaeologists, and geologists. It sits near the Gilf Kebir and Western Desert, serving as a focal point for trans-Saharan routes, scientific expeditions, and nomadic pastoralists.
The massif lies within the Western Desert region adjacent to the Gilf Kebir, the Sahara Desert, and the Kebir Plateau. Uweinat's summit area reaches about 1,934 metres above sea level and forms part of the greater Saharan highland system near the Qattara Depression, the Murzuq Basin, and the Wadi Howar corridor. The mountain's position on the Libya–Egypt–Sudan margins places it near international boundaries recognized by the United Nations and referenced in historical agreements such as colonial-era accords between the United Kingdom, Italy, and Egypt. Cartographically it appears on maps produced by institutions like the Royal Geographical Society and the British Museum-era expedition charts.
Geologically, the massif is a remnant of Paleozoic and Mesozoic sedimentation, with exposed sandstone, conglomerate, and inselberg structures comparable to formations studied at the Aïr Mountains and the Hoggar Mountains. Stratigraphy includes silcretes and fossiliferous layers examined by researchers from the Natural History Museum, London and the Institut Français d'Archéologie Orientale. Paleohydrological evidence—rock basins, gueltas, and relict drainage channels—ties to paleo-river systems like the ancient courses feeding the Nile via paleochannels similar to Wadi Howar. Hydrogeological studies led by teams from the University of Khartoum and the University of Cairo have modeled water retention in tafoni and solution basins that supported prehistoric human occupation.
The massif experiences hyper-arid Saharan climate conditions influenced by the Saharan heat low, subtropical high-pressure cells, and episodic Atlantic-derived plumes studied by climatologists at NASA and the Max Planck Institute for Meteorology. Paleoclimate reconstructions linking African Humid Period fluctuations to orbital forcing conducted by researchers at the Lamont–Doherty Earth Observatory help explain periods of enhanced monsoonal activity that created lakes and savanna patches. Modern microclimates in sheltered wadis support isolated biota, a subject of ecological surveys by teams from the Royal Botanic Gardens, Kew and the Smithsonian Institution.
Archaeological investigations have revealed extensive rock art panels, stone tools, and archaeological assemblages attributed to Saharan pastoralist and hunter-gatherer groups contemporaneous with cultural phases recognized at sites like Tassili n'Ajjer, Nabta Playa, and Gilf Kebir. Rock arts include depictions of cattle, giraffes, and anthropomorphic figures, motifs paralleled in the corpus cataloged by the British Institute in Eastern Africa and the University of Oxford's archaeological missions. Explorers such as Gertrude Bell-era contemporaries, twentieth-century surveyors including László Almásy and scientific teams from the Royal Geographical Society conducted mapping and recorded inscriptions. Chronologies derive from comparative typology and radiocarbon dating methods refined at laboratories like the Oxford Radiocarbon Accelerator Unit and the Max Planck Institute for Evolutionary Anthropology.
Flora in sheltered gullies mirrors elements cataloged by botanists from the International Union for Conservation of Nature inventories and the Royal Botanic Gardens, Kew with species adapted to episodic moisture such as acacias also recorded in studies at Nabta Playa. Faunal remains and rock art images reference species like giraffe, hartebeest, and ostrich that correlate with paleontological finds in regions investigated by teams from the Natural History Museum, London and the University of Cambridge. Contemporary faunal presence is limited and monitored by conservation biologists affiliated with institutions such as the Zoological Society of London and regional wildlife authorities.
Access is remote and regulated by the governments of Libya, Egypt, and Sudan, with permits often required and logistics coordinated through border authorities and organizations like the United Nations Educational, Scientific and Cultural Organization when heritage concerns arise. Conservation initiatives reference frameworks from the World Heritage Convention and are informed by risk assessments carried out by teams from the International Council on Monuments and Sites and the European Association of Archaeologists. Expeditions historically mounted by private explorers and institutions such as the Royal Geographical Society have given way to collaborative scientific missions and heritage protection programs involving national research councils.
The massif holds cultural importance for nomadic groups including Tuareg-linked communities and Bedouin groups associated with trans-Saharan routes documented by anthropologists at the London School of Economics and the School of Oriental and African Studies. Oral traditions recorded by researchers from the University of Khartoum and the American University in Cairo reference pilgrimage routes, seasonal grazing, and place-based narratives. The site features in scholarly works published by the British Museum, the Journal of African Archaeology, and monographs from the Institute of Archaeology, University College London.
Category:Mountains of Africa