Duwatsun Hajar
Dutsen Hajar (Larabci: جِبَال ٱلْحَجَر, romanized: Jibāl al-Ḥajar, The Rocky Mountains ko Dutsen Duwatsu) ɗaya ne daga cikin tudu mafi tsayi a yankin Larabawa, wanda aka raba tsakanin arewacin Oman da gabacin Hadaddiyar Daular Larabawa. Hakanan ana kiranta da "Dutsen Oman", suna raba ƙananan filin bakin teku na Oman daga babban tudun hamada, kuma suna kwance 50-100 km (31-62 mi) daga ciki daga Tekun Oman.
| Duwatsun Hajar | |
|---|---|
| Dutsen Oman [1] Dutsen Rocky [2] Dutsen Asabon[3][4] | |
 Hajar ta Tsakiya da Yamma ta tashi a bayan Nakhal Fort, Gwamnatin Al Batinah ta Kudu, Oman
| |
| Mafi Girma | |
| Mafi girma | Jebel Shams, Oman |
| Hawan sama | 3,009 m (9,872 ft) |
| Sunayen | |
| Sunan asali | Jibāl al-Ḥajar (جِبَال أْحَر (Arabic) ) |
| Yanayin ƙasa | |
Page Module:Location map/styles.css has no content.   Duwatsun Hajar  Duwatsun Hajar  Duwatsun Hajar | |
| Kasashe | Oman da Hadaddiyar Daular Larabawa 
|
| Yankin | Asiya |
| Yanayin kewayon | Page Module:Coordinates/styles.css has no content.23°18′N 57°06′E/__hau____hau____hau__23.3°N 57.1°E |
Al (اَلْ) yana nufin "dutse", kuma Ḥajar (حَجَر) yana nufin" dutse" ko "dutse". Don haka ana kiran al-Ḥajar (اَلْحَجَر) "dutse" ko "dutse".
Ilimin ƙasa
gyara sashe
Duwatsun Hajar sun kai kilomita 700 (mil 430) ta hanyar Hadaddiyar Daular Larabawa da Oman.[5] Suna kan kusurwar arewa maso gabashin Larabawa, suna zuwa daga Yankin Musandam zuwa gabar gabashin Oman. Yankin yana da kusan kilomita 100 kilometres (62 mi) (62 a fadin, tare da Jabal Shams kasancewa mafi girma a 3,009 metres (9,872 ft) a tsakiyar yankin tsaunuka.[6][7]
Manazarta
gyara sashe- ↑ Allen, Calvin H. Jr. (2016-02-05). "1: Land and People". Oman: the Modernization of the Sultanate. Abingdon, New York: Routledge. pp. 1–8. ISBN 978-1-3172-9164-0.
- ↑ Geukens, F. (1966). Bowers, S. D. (ed.). United States Geological Survey Professional Paper. Washington, D.C.: U.S. Government Printing Office.
- ↑ Al-Yahyai, Sultan; Charabi, Yassine; Al-Sarmi, Said; Al-Maskari, Juma (2017-05-09). "3: Scenarios Based Climate Projection for Oman's Water Resources". In Abdalla, Omar; Kacimov, Anvar; Chen, Mingjie; Al-Maktoumi, Ali; Al-Hosni, Talal; Clark, Ian (eds.). Water Resources in Arid Areas: The Way Forward. Springer. p. 49. ISBN 978-3-3195-1856-5.
- ↑ Megdiche-Kharrat, Fairouz; Ragala, Rachid; Moussa, Mohamed (2016-11-25). "12: The Aqueducts of the Sultanate of Oman: Sustainable Water-Supplying Irrigating Oases Cities". In Angelakis, Andreas N.; Chiotis, Eustathios; Eslamian, Saeid; Weingartner, Herbert (eds.). Underground Aqueducts Handbook. CRC Press. p. 206. ISBN 978-1-4987-4831-5.
- ↑ Searle, M. P.; Cooper, D. J. W. (1986). "Structure of the Hawasina Window culmination, central Oman Mountains". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 77 (2): 143–156. doi:10.1017/S0263593300010798. ISSN 1473-7116. S2CID 130270339.
- ↑ Breton, Jean-Paul; Béchennec, François; Métour, Joël Le; Moen-Maurel, Laure; Razin, Philippe (2004-04-01). "Eoalpine (Cretaceous) evolution of the Oman Tethyan continental margin: insights from a structural field study in Jabal Akhdar (Oman Mountains)". GeoArabia. 9 (2): 41–58. Bibcode:2004GeoAr...9...41B. doi:10.2113/geoarabia090241. ISSN 1025-6059. S2CID 197865202.
- ↑ Kusky, Timothy; Robinson, Cordula; El-Baz, Farouk (September 2005). "Tertiary–Quaternary faulting and uplift in the northern Oman Hajar Mountains". Journal of the Geological Society. 162 (5): 871–888. Bibcode:2005JGSoc.162..871K. doi:10.1144/0016-764904-122. ISSN 0016-7649. S2CID 59467623.