The Sinai Peninsula is located in a hyper-arid climate environment, which affects drainage, development of coastal fan deltas and the growth of coral reef along the Gulf of Suez and Gulf of Aqaba. The recent extension of Gulf of Suez and the strike-slip tectonics of the Gulf of Aqaba give the possibility to contrast two different tectonic settings under the same arid conditions. The purpose of this study is to identify relationships and trends between catchment areas, fan deltas and coral reefs in the shallow-water area. Additionally two flash flood events, from 2002 and 2016, and the delivery of sediments to the coastal area have been studied. This thesis is based on mapped catchments, fan deltas, coral reefs and shallow-water (to 5 m dept...
Hurghada coastal reefs have encountered a huge modification in the last three decades, associated wi...
Northern Safaga Bay is a mixed siliciclastic/carbonate environment with both Aeolian and fluvial sed...
Wadis emerging from the southeastern Sinai Mountains (Egypt) westwards to the Gulf of Suez are fille...
The Sinai Peninsula is located in a hyper-arid climate environment, which affects drainage, developm...
The main geomorphological features of the coral shores of the eastern and southern Sinai Peninsula a...
Localisation and internai organisation of immature coral reefs on an Early Quaternary alluvial fan, ...
The possible causes and consequences of changes to the coral reefs in different sites of Dahab, Sout...
Patterns of sedimentation in the Red Sea offer a contemporary analog for carbonate deposition in mar...
International audienceCoral reefs developed within the Gulf of Suez-northern Red Sea region during a...
Sea floor types, biota and sedimentary facies were mapped in northern Safaga Bay, Red Sea Egypt. Aft...
Copyright © 2013 Abdel Hamid A. Taha et al. This is an open access article distributed under the Cre...
The Wadi Kubbaniya in the Western Desert of Egypt north of the City of Aswan has been interpreted as...
Two kms north-east of Dahab, the northernmost remnant of emerged Pleistocene terraces display well p...
Modem reefs in the Red Sea exhibit different controls on their formation. The majority of the reefs ...
The Red Sea is typified by expansive fringing-reefs affixed to a narrow and steep coastal shelf. We ...
Hurghada coastal reefs have encountered a huge modification in the last three decades, associated wi...
Northern Safaga Bay is a mixed siliciclastic/carbonate environment with both Aeolian and fluvial sed...
Wadis emerging from the southeastern Sinai Mountains (Egypt) westwards to the Gulf of Suez are fille...
The Sinai Peninsula is located in a hyper-arid climate environment, which affects drainage, developm...
The main geomorphological features of the coral shores of the eastern and southern Sinai Peninsula a...
Localisation and internai organisation of immature coral reefs on an Early Quaternary alluvial fan, ...
The possible causes and consequences of changes to the coral reefs in different sites of Dahab, Sout...
Patterns of sedimentation in the Red Sea offer a contemporary analog for carbonate deposition in mar...
International audienceCoral reefs developed within the Gulf of Suez-northern Red Sea region during a...
Sea floor types, biota and sedimentary facies were mapped in northern Safaga Bay, Red Sea Egypt. Aft...
Copyright © 2013 Abdel Hamid A. Taha et al. This is an open access article distributed under the Cre...
The Wadi Kubbaniya in the Western Desert of Egypt north of the City of Aswan has been interpreted as...
Two kms north-east of Dahab, the northernmost remnant of emerged Pleistocene terraces display well p...
Modem reefs in the Red Sea exhibit different controls on their formation. The majority of the reefs ...
The Red Sea is typified by expansive fringing-reefs affixed to a narrow and steep coastal shelf. We ...
Hurghada coastal reefs have encountered a huge modification in the last three decades, associated wi...
Northern Safaga Bay is a mixed siliciclastic/carbonate environment with both Aeolian and fluvial sed...
Wadis emerging from the southeastern Sinai Mountains (Egypt) westwards to the Gulf of Suez are fille...