Titlebook: Geological Setting, Palaeoenvironment and Archaeology of the Red Sea; Najeeb M.A. Rasul,Ian C.F. Stewart Book 2019 Springer Nature Switzer

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Origin of Submarine Channel North of Hanish Sill, Red Sea,ottom waters passing between the basins form gravity currents. In the southernmost Red Sea, in contrast, an 8 km-wide and 100- to 250-m deep channel lies on the north side of Hanish Sill, in an area where the strongest bottom currents flow southward, associated with winter expulsion of dense saline

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Cenozoic Faults and Seismicity in Northwest Saudi Arabia and the Gulf of Aqaba Region,identify the youngest geological faults in the area. These faults have been termed Cenozoic faults, although most are Neogene in age, being younger than 23 Ma. A number of previously unknown structures have been identified. These include a zone of shattered and intensely faulted rocks 25 km wide tha

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FLIP

Variations in Plio-Pleistocene Deposition in the Red Sea,es in the south and with input of aeolian and fluvial sediments through the Tokar Gap in the Sudanese hills. Otherwise, however, the sediment distribution does not obviously reflect the likely pattern of sediment input (from the positions of wind gaps through the Red Sea hills and fluvial drainage b

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Pleistocene Coral Reef Terraces on the Saudi Arabian Side of the Gulf of Aqaba, Red Sea,Aqaba. Those bordering the Saudi Arabian sector have received little attention thus far, and are comparatively less known than their counterparts in the Sinai sector of the Gulf and in the Red Sea. As is the rule in the Red Sea region, the best developed marine terrace system is reefal and pertains

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Mollusc Fauna Associated with Late Pleistocene Coral Reef Systems of the Saudi Arabian Side of the tified and sampled for macrofossils. Terraces ascribable to the last interglacial, the Marine Isotope Stage 5e (MIS5e, ~125kyr BP), predominate and contain a well preserved fossil legacy of sea life at the time. Molluscs proved to represent the most diverse component in the macrobenthos, overwhelmin

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Palaeomagnetism and Geochronology of the Harrats Lunayyir and Khaybar Lava Fields, Saudi Arabia,tudy on volcanic rocks from the Khaybar and Lunayyir Harrats plus a site of sediments deposited below the Miocene rocks in the former area. Progressive thermal or alternating field demagnetization successfully isolated stable characteristic magnetizations (ChRM) that are consistent with a primary ma

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Princip der Untersuchungsmethode,n of mid-ocean ridges. Competing theories for how spreading begins—either by quasi-instantaneous formation of a whole spreading segment or by initiation of spreading at multiple discrete “nodes” separated by thinned continental lithosphere—have been put forward based, until recently, on the observat