The Ḥarrat al-Shām (Arabic: حَرَّة ٱلشَّام),[1][nb 1] also known as the Black Desert,[2] is a region of rocky, basaltic desert straddling southern Syria and the northern Arabian Peninsula. It covers an area of some 40,000km2 (15,000sqmi)[citation needed] in the modern-day Syrian Arab Republic, Jordan, Israel and Saudi Arabia. Vegetation is characteristically open acacia shrubland with patches of juniper at higher altitudes[3]
Desert region in Syria and northern Arabia
Ḥarrat al-Shām
Black Desert
Location within the Levant of the wider volcanic province it is part of
Part of
Syrian Desert
Offshore water bodies
Lake Burqu' (see Qasr Burqu')
Qa Shubayqa
Age
Oligocene, Neogene, Quaternary
Geology
Basaltic volcanic field
Volcanic field
Harrat Ash Shaam Volcanic Province (HASV)
The Harrat near Jawa in eastern Jordan
The Harrat has been occupied by humans since at least the Late Epipalaeolithic period (c.12,500–9500 BCE).[4] One of the earliest known sites is Shubayqa 1 (occupied c.12,600–10,000 BCE),[4][5] where archaeologists have discovered the remains of the oldest known bread.[6]
Geology
Harrah region from the Space Shuttle
The Harrat comprises volcanic fields formed by tectonic activity from the Oligocene through to the Quaternary period.[7] It is the largest of several volcanic fields on the Arabian Plate,[8] containing more than 800 volcanic cones and around 140 dikes.[7] Activity began during the Miocene; a younger eruptive stage, at the SE end of the volcanic field, occurred during the late-Pleistocene and Holocene.[9] It is known to have erupted in historic times.[10][11]
The Jabal al-Druze, al-Safa and Dirat al-Tulul volcanic fields, among others, form the northern and Syrian part of the harrat. The Saudi Arabian portion of the Harrat Ash Shamah volcanic field extends across a 210km (130mi)-long, roughly 75km (47mi)-wide NW-SE-trending area on the NE flanks of the Sirhan Valley and reaches its 1,100 metres (3,600ft) high point at Jabal Al-Amud. It is in the Tabuk Region of northwest Saudi Arabia.[12][13] and is one of a series of Quaternary volcanic fields paralleling the Red Sea coast.
Archaeological sites
Desert kites
Jordan
Jawa, Early Bronze Age proto-urban settlement
Qasr Azraq and Qasr 'Ain es-Sil, ancient fortified sites in the Azraq Oasis
Qasr Burqu', ancient "desert castle"
Qasr Usaykhim, ancient fort northeast of Azraq
Shubayqa 1, Stone Age (Natufian) hunter-gatherer site with oldest bread-making find in the world
See also
Badia region
Hauran, historical region partially overlapping with Harrat al-Sham
Variously transcribed as the harra, Ḥarrat ash-Shāmah (حَرَّة ٱلشَّامَة) or Ḥarrate-Shāmah (حَرَّةِ شَامَة).[citation needed]
References
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
Betts, Alison (1982). "A Natufian site in the Black Desert, Eastern Jordan". Paléorient. 8 (2): 79–82. doi:10.3406/paleo.1982.4322. ISSN0153-9345.
S.A. Ghazanfar, Vegetation of the Arabian Peninsula (Springer Science & Business Media, 1998) p 272.
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. ISBN978-1-107-09046-0.
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. ISSN1866-7538. S2CID129569824.
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)
Further reading
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
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.
External links
Wikimedia Commons has media related to Black Desert.
Note: Mountains are sorted in alphabetical order, unless where it concerns ranges. The highest confirmed mountains in each country are indicated with 'HP', and those with the highest peak are indicated with 'HP', bearing in mind that in the UAE, the highest mountain and the mountain with the highest peak are different. Outcrops are indicated with 'OC', and outliers with 'OL', and anticlines with 'AC'. Volcanoes are indicated with 'V', volcanic craters with 'VC', lava fields with 'LF', and volcanic fields with 'VF'.
Other notes:
Shared with the UAE
Also regarded as being of the Western Hajar
Also regarded as being of the Western Hajar
Shared with the UAE
Shared with the UAE
Sensu lato, shared with Yemen
Shared with Yemen
Sensu lato
Sensu lato
Shared with Oman
Shared with Oman
Highest mountain in the UAE, but the peak is in Oman
Due to the peak of Jebel Jais being in Oman, this mountain has the highest confirmed peak in the UAE
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