38:
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30:"Red Sea Hills" redirects here. For the mountains in Saudi Arabia on the opposite coast of the Red Sea, sometimes also called the Red Sea Hills, see
145:, the most significant of the few seasonal streams that flow into the Red Sea, rises in the Red Sea Hills of Sudan and empties into the sea at the
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130:. The Red Sea Hills rise almost to 3,000 metres (9,800 ft) today, but in the past were much higher. The Oligocene uplift caused the
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M. Sultan, S. Sefry and M. AbuAbdallah, "Impacts of
Climate Change on the Red Sea Region and its Watersheds, Saudi Arabia",
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The Itbāy is arid, receiving less than 200 millimetres (7.9 in) of rainfall each year with high variability. The
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of their streams and the increased erosion removed most of the limestone and sandstone to expose the
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W. Bosworth, "Geological
Evolution of the Red Sea: Historical Background, Review, and Synthesis",
118:, only some 23–34 million years ago. The Red Sea Hills are thus part of the same formation as the
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The Red Sea: The
Formation, Morphology, Oceanography and Environment of a Young Oceanic Basin
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The Red Sea: The
Formation, Morphology, Oceanography and Environment of a Young Oceanic Basin
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Managing pastoral adaptations in the Red Sea Hills of the Sudan: Challenges and
Dilemmas
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110:. Although the rock itself is 550–900 million years old, the mountains were created by
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Stevens, Chris J.; Nixon, Sam; Murray, Mary Anne; Fuller, Dorian Q. (July 2016).
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and their presence in the hills is detected archaeologically by the presence of
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190:, where there is limited vegetation. In antiquity, the Beja were known as the
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206:'s sphere of influence. Extensive mining settlements have been found in the
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In prehistoric times, the Red Sea Hills were likely the area where the
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168:, which was being mined as early as the fourth millennium BC.
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149:. In prehistoric times it was probably a permanent river.
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84:. The hills separate the narrow coastal plain from the
279:(American University in Cairo Press, 2003), pp. 27–28.
218:(flat-topped burial mounds), and the appearance of
76:. It is characterized by a chain of mountains, the
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Region of southeastern Egypt and northeastern Sudan
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253:(online 7 May 2012), accessed 31 December 2018.
96:The Red Sea Hills are composed of the exposed
349:The Nubian Past: An Archaeology of the Sudan
186:, that flow seasonally into the sea and the
80:, running north–south and parallel with the
49:Closer view of the arid, rocky Red Sea Hills
277:The Geology of Egypt: A Traveler's Handbook
179:. They mainly live near the dry riverbeds,
175:who speak a Cushitic language and practice
114:when the Red Sea itself was formed in the
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351:(Routledge, 2004), pp. 64, 209, 251–52.
171:The Red Sea Hills are inhabited by the
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202:of the hills places it firmly within
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164:The Red Sea Hills are a source of
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321:Archaeology of African Plant Use
198:from the fourth century AD. The
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222:to mark burials in the late
68:is a region of southeastern
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214:. The early Blemmyes built
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266:(Springer, 2015), p. 364.
126:and the mountains of the
308:(Springer, 2015), p. 50.
251:Encyclopædia Britannica
159:Proto-Cushitic language
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41:Red Sea Hills in Egypt
108:Arabian-Nubian Shield
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275:Bonnie M. Sampsell,
376:25.6611°N 33.9533°E
372: /
295:(IIED, 1994), p. 2.
196:Eastern Desert Ware
101:volcano-sedimentary
405:Geography of Sudan
400:Geography of Egypt
347:David N. Edwards,
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415:Regions of Africa
331:978-1-315-43400-1
226:may be linked to
120:Sarawat Mountains
72:and northeastern
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224:Middle Ages
208:Wadi Allaqi
177:pastoralism
173:Beja people
147:Tokar Delta
143:Barka River
394:Categories
367:33°57′12″E
364:25°39′40″N
234:References
116:Oligocene
410:Blemmyes
210:and the
192:Blemmyes
166:porphyry
136:basement
247:"Itbāy"
153:History
138:layer.
106:of the
92:Geology
82:Red Sea
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220:cairns
112:uplift
66:ʿAtbāy
58:Arabic
249:, in
74:Sudan
70:Egypt
64:) or
62:اطبيه
54:Itbāy
326:ISBN
188:Nile
182:wādī
104:rock
122:of
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