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Duwatsun Hajar

An daina tallafawa sigar da ake bugawa kuma tana iya samun kurakurai na fassarar. Da fatan za a sabunta alamun binciken mai binciken ku kuma da fatan za a yi amfani da aikin bugun tsoffin ayyukan a maimakon.
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
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Hajar Mountains is located in Oman
Hajar Mountains
Duwatsun Hajar
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Hajar Mountains is located in Middle East
Hajar Mountains
Duwatsun Hajar
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Hajar Mountains is located in West and Central Asia
Hajar Mountains
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 / 23.3; 57.1

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.

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

Taswirar taswirar tsaunukan Hajar tare da yankuna na tectonic da geological

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

  1. 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.
  2. Geukens, F. (1966). Bowers, S. D. (ed.). United States Geological Survey Professional Paper. Washington, D.C.: U.S. Government Printing Office.
  3. 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.
  4. 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.
  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.
  6. 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.
  7. 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.