Web1. nov 1998 · The Tertiary to Recent Red Sea rift forms part of a rift system that includes the Gulf of Aden and East African rift in the south and the Gulf of Suez in the north (Fig. 2). These rifts initiated in the Late Oligocene–Miocene time and fragment the once continuous Arabian–Nubian Shield (Cochran and Martinez, 1988).
Afar Triangle - Wikipedia
Web10. apr 2024 · The Central Red Sea Rift is a natural laboratory to study the transition from rifting to spreading. Based on new reflection seismic profiles and gravity modeling, we examined the crustal structure, tectonic evolution, breakup mechanism, and future evolution of the Central Red Sea Rift. Along this rift axis, the breakup of continental lithosphere is … WebAbout 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 2 (460 sq mi) … set up private internet access unraid
Dead Sea Transform - Wikipedia
WebThe Gulf of Suez is an abandoned rift basin with less than 100-meter water depths. The Gulf of Aqaba is a younger, rapidly subsiding wrench basin with maximum water depth of 1850 meters. The remaining Red Sea Basin Province is an active rift where sea-floor spreading has occurred for the last 5 m.y. and where water depths locally exceed 2300 ... Web15. okt 2008 · The Red Sea is one of the youngest oceans in the world and one of the warmest. The northern region, with its diverse array of marine life, is one of the most visited dive locations on earth while ... The Red Sea (Arabic: البحر الأحمر - بحر القلزم, romanized: Modern: al-Baḥr al-ʾAḥmar, Medieval: Baḥr al-Qulzum; Hebrew: יַם-סוּף, romanized: yam sūf or Hebrew: הַיָּם הָאָדְוֹם, romanized: hayyām hāʾāḏōm; Coptic: ⲫⲓⲟⲙ ⲛ̀ϩⲁϩ Phiom Enhah or ⲫⲓⲟⲙ ⲛ̀ϣⲁⲣⲓ Phiom ǹšari; Tigrinya: ቀይሕ ባሕሪ Qeyih Bahri; Somali: Badda Cas) is a seawater inlet of the Indian Ocean, lying between Africa and Asia. Its connection t… set up private limited company