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Titlebook: Geology of the Oman Mountains, Eastern Arabia; Mike Searle Book 2019 Springer Nature Switzerland AG 2019 Al Hajar Mountains.Oman Geoparks.

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Exploration of the Oman–UAE Mountainsulf through the Straits of Hormuz between Musandam and the Iranian coast to the north. The seas off Oman teem with fish, attracted by the upwelling of plankton-rich currents along the western side of the Indian Ocean. Omani traders used the monsoon winds to sail large ocean-going dhows south to East
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Muscat–As Sifaheposited unconformably above the ophiolite and all underlying units, have been folded around huge anticlines with north-south axes at right angles to the regional trend of the Mesozoic shelf carbonates inland. These limestones are beautifully exposed around Qurum and Ras al Hamra, and are folded ove
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Saih Hatatuctile shear zones and top-north ductile S-C fabrics reflect uplift and exhumation of deeper thrust sheets beneath ‘passive roof faults’. A major phase of uplift occurred after deposition of the Paleocene–Eocene limestones when normal faulting occurred around its perimeter reflecting uplift of the f
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Sharkiyah, Eastern Oman Mountainsparts of the high mountains, and Arabian tahr are restricted to the high peaks around the Wadi Serin reserve. The construction of a major highway linking Quriat to Sur with several large new bridges spanning Wadi Daykah, Wadi Ash Shab and Wadi Tiwi has now opened up the region for development. The e
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