Harrat al-Sham
Ḥarrat al-Shām
Black Desert | |
---|---|
Coordinates: 32°37′53″N 36°45′52″E / 32.63139°N 36.76444°E | |
Part of | Syrian Desert |
Offshore water bodies | |
Age | Oligocene, Neogene, Quaternary |
Geology | Basaltic volcanic field |
Volcanic field | Harrat Ash Shaam Volcanic Province (HASV) |
The Ḥarrat al-Shām (Arabic: حَرَّة ٱلشَّام),[1][nb 1] also known as the Harrat al-Harra or Harrat al-Shaba,[2] and sometimes the Black Desert in English,[3] is a region of rocky, basaltic desert straddling southern Syrian region and the northern Arabian Peninsula. It covers an area of some 40,000 km2 (15,000 sq mi)[citation needed] in the modern-day Syrian Arab Republic, Jordan, and Saudi Arabia. Vegetation is characteristically open acacia shrubland with patches of juniper at higher altitudes.[4]
The Harrat has been occupied by humans since at least the Late Epipalaeolithic (c. 12,500–9500 BCE).[5] One of the earliest known sites is Shubayqa 1 (occupied c. 12,600–10,000 BCE),[5][6] a Natufian site where archaeologists have discovered the remains of the oldest known bread.[7]
Geology
[edit]The Harrat comprises volcanic fields formed by tectonic activity from the Oligocene through to the Quaternary.[8] It is the largest of several volcanic fields on the Arabian Plate,[9] containing more than 800 volcanic cones and around 140 dikes.[8] Activity began during the Miocene; an earlier eruptive stage at the southeastern end of the volcanic field, occurred during the late Pleistocene and the Holocene.[10] It is known to have erupted in historic times.[11][12]
The Jabal al-Druze, al-Safa and Dirat al-Tulul volcanic fields, among others, form the northern and Syrian part of the ḥarra. The Saudi Arabian portion of the Harrat Ash Shamah volcanic field extends across a 210 km (130 miles)-long, roughly 75 km (47 miles)-wide northwest-southeast-trending area on the northeastern flanks of the Wadi Sirhan and reaches its 1,100 metres (3,600 ft) high point at Jabal al-Amud. It is in the Tabuk Province of northwest Saudi Arabia.[13][14] and is one of a series of Quaternary volcanic fields paralleling the Red Sea coast.
History and economy
[edit]The Harrat has traditionally been occupied by nomadic Bedouin of the Anizah confedaration.[15][16] It It is primarily associated with the Ahl al-Jabal tribe, who graze sheep, goats, donkeys and camels there, but the Rwala, Zbaid, Ghayyath, Sardiyya and other tribes also use the area at times.[16] Although the region as a whole is too dry for rainfed agriculture, seasonal wetlands such as the Qa' Shubayqa are used for growing cereals after they are flooded by winter rains.[16][17] In the second half of the 20th century, many Bedouin settled in the village of Safawi, which grew up around a pumping station on the Kirkuk–Haifa oil pipeline (H5).[18]
Archaeological sites
[edit]Jordan
[edit]- Jawa, Jordan, Early Bronze Age proto-urban settlement
- Qasr al-Azraq and Qasr 'Ain es-Sil, ancient desert castles in the Azraq oasis
- Qasr Burqu', ancient "desert castle"
- Qasr Usaykhim, an ancient fort northeast of Azraq
- Shubayqa 1, Natufian hunter-gatherer site with the oldest bread-making find in the world
See also
[edit]- Syrian Desert
- Hauran, a historical region partially overlapping with the Harrat al-Sham
- List of volcanoes in Saudi Arabia
- Sarawat Mountains
Notes
[edit]- ^ Variously transcribed as the harra, Ḥarrat ash-Shāmah (حَرَّة ٱلشَّامَة) or Ḥarrate-Shāmah (حَرَّةِ شَامَة).[citation needed]
References
[edit]- ^ Ibrahim, K. (1993), The geological framework for the Harrat Ash-Shaam Basaltic Super-Group and its volcanotectonic evolution, Jordan: Bulletin 24, Geological Mapping Division, Natural Resources Authority
- ^ Edgell, H. Stewart (2006). Arabian Deserts: Nature, Origin and Evolution. Dordrecht: Springer. pp. 327–329, 347. ISBN 978-1-4020-3969-0.
{{cite book}}
: CS1 maint: date and year (link) - ^ Betts, Alison (1982). "A Natufian site in the Black Desert, Eastern Jordan". Paléorient. 8 (2): 79–82. doi:10.3406/paleo.1982.4322. ISSN 0153-9345.
- ^ S.A. Ghazanfar, Vegetation of the Arabian Peninsula (Springer Science & Business Media, 1998) p 272.
- ^ a b Richter, Tobias (2017). "Natufian and early Neolithic in the Black Desert". In Enzel, Yehouda; Bar-Yosef, Ofer (eds.). Quaternary of the Levant: Environments, Climate Change, and Humans. Cambridge: Cambridge University Press. pp. 715–722. ISBN 978-1-107-09046-0.
- ^ Richter, Tobias; Arranz-Otaegui, Amaia; Yeomans, Lisa; Boaretto, Elisabetta (5 December 2017). "High Resolution AMS Dates from Shubayqa 1, northeast Jordan Reveal Complex Origins of Late Epipalaeolithic Natufian in the Levant". Scientific Reports. 7 (1): 17025. Bibcode:2017NatSR...717025R. doi:10.1038/s41598-017-17096-5. ISSN 2045-2322. PMC 5717003. PMID 29208998.
- ^ Arranz-Otaegui, Amaia; Carretero, Lara Gonzalez; Ramsey, Monica N.; Fuller, Dorian Q.; Richter, Tobias (31 July 2018). "Archaeobotanical evidence reveals the origins of bread 14,400 years ago in northeastern Jordan". Proceedings of the National Academy of Sciences. 115 (31): 7925–7930. doi:10.1073/pnas.1801071115. ISSN 0027-8424. PMC 6077754. PMID 30012614.
- ^ a b Al Kwatli, Mohamad Amer; Gillot, Pierre Yves; Lefèvre, Jean Claude; Hildenbrand, Anthony (2015-09-01). "Morpho-structural analysis of Harrat Al Sham volcanic field Arabian plate (Syria, Jordan, and Saudi Arabia): methodology and application". Arabian Journal of Geosciences. 8 (9): 6867–6880. doi:10.1007/s12517-014-1731-1. ISSN 1866-7538. S2CID 129569824.
- ^ Krienitz, M.-S.; Haase, K. M.; Mezger, K.; Shaikh-Mashail, M. A. (2007-08-01). "Magma Genesis and Mantle Dynamics at the Harrat Ash Shamah Volcanic Field (Southern Syria)". Journal of Petrology. 48 (8): 1513–1542. doi:10.1093/petrology/egm028. ISSN 0022-3530.
- ^ H. Stewart Edgell, Arabian Deserts: Nature, Origin and Evolution (Springer Science & Business Media, 21Jul.,2006 ) p329-330
- ^ Geological Survey Professional Paper. U.S. Government Printing Office. 1989. p. 153.
- ^ Peter Vincent, Saudi Arabia: An Environmental Overview (CRC Press, 2008) p22.
- ^ U.S. Geological Survey Professional Paper (U.S. Government Printing Office, 1989) pA152
- ^ Geological Survey Professional Paper, Volume 560, Part 1 (U.S. Government Printing Office, 1989)
- ^ Lancaster, William; Lancaster, Fidelity (1997-02-01). "Indigenous resource management systems in the Bâdia of the Bilâd ash-Shâm". Journal of Arid Environments. 35 (2): 367–378. doi:10.1006/jare.1996.0169. ISSN 0140-1963.
- ^ a b c Lancaster, William; Lancaster, Fidelity (1999). People, Land and Water in the Arab Middle East. London: Routledge. pp. 100–102. ISBN 9781315079257.
- ^ Jones, Matthew D.; Richter, Tobias; Rollefson, Gary; Rowan, Yorke; Roe, Joe; Toms, Phillip; Wood, Jamie; Wasse, Alexander; Ikram, Haroon; Williams, Matthew; AlShdaifat, Ahmad; Pedersen, Patrick Nørskov; Esaid, Wesam (2022-10-20). "The palaeoenvironmental potential of the eastern Jordanian desert basins (Qe'an)". Quaternary International. Geoarchaeology from Mediterranean Areas to Arid Margins. 635: 73–82. doi:10.1016/j.quaint.2021.06.023. ISSN 1040-6182.
- ^ "Arid Land Resources and Their Management: Jordan's Desert Margin". Routledge & CRC Press. Retrieved 2024-12-17.
Further reading
[edit]- Ilani, S., Harlavan, Y., Tarawneh, K., Rabba, I., Weinberger, R., Khalil, I., and Peltz, S. (2001), "New K-Ar ages of basalts from the Harrat Ash Shaam volcanic field in Jordan: Implications for the span and duration of the upper-mantle upwelling beneath the western Arabian plate" Geology 29(2):171–174
- Kempe, S. and Al-Malabeh, A. (2005), "Newly discovered lava tunnels of the Al-Shaam plateau basalts", Geophysical Research Abstracts 7, European Geosciences Union
- Salf, S.I. (1988), "Field and petrographic characteristics of Cenozoic basaltic rocks, Northwestern Saudi Arabia" Journal of African Earth Sciences, 7(5):805–809
- Weinstein, Y., Navon, O., Altherr, R., and Stein, M., (2006) "The role of lithospheric mantle heterogeneity in the generation of Plio-Pleistocene alkali basalt suites from NW Harrat Ash Shaam (Israel)", Journal of Petrology 47(5):1017–1050
- Al Kwatli, M.A., Gillot, P.Y., Zeyen, H., Hildenbrand, A., and Al Gharib, I., 2012. Volcano-tectonic evolution of the northern part of the Arabian plate in the light of new K-Ar ages and remote sensing: Harrat Ash Shaam volcanic province (Syria). Tectonophysics, 580, 192–207.