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Harrat al-Sham

Desert region in Syria and northern Arabia From Wikipedia, the free encyclopedia

Harrat al-Shammap

The Ḥarrat al-Shām (Arabic: حَرَّة ٱلشَّام),[1][nb 1] also known as the Harrat al-Harra, Harrat al-Shaba,[2] Syro-Jordanian Harrah,[3] and sometimes the Black Desert in English,[4] is a region of rocky, basaltic desert stretching from southern Syria starting at the Hauran region all the way down to the northern Arabian Peninsula.[3] 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.[5]

Quick Facts Ḥarrat al-Shām Black Desert, Part of ...
Ḥarrat al-Shām
Black Desert
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Location within the Levant of the wider volcanic province it is part of
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Coordinates: 32°37′53″N 36°45′52″E / 32.63139; 36.76444][[Category:Pages using gadget WikiMiniAtlas]]"},"html":"Coordinates: </templatestyles>\"}' data-mw='{\"name\":\"templatestyles\",\"attrs\":{\"src\":\"Module:Coordinates/styles.css\"},\"body\":{\"extsrc\":\"\"}}'/>32°37′53″N 36°45′52″E / 32.63139°N 36.76444°E / 32.63139; 36.76444"}">
Part ofSyrian Desert
Offshore water bodies
AgeOligocene, Neogene, Quaternary
GeologyBasaltic volcanic field
Volcanic fieldHarrat Ash Shaam Volcanic Province (HASV)
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The Harrat near Jawa in eastern Jordan

The Harrat has been occupied by humans since at least the Late Epipalaeolithic (c.12,500–9500 BCE).[6] One of the earliest known sites is Shubayqa 1 (occupied c.12,600–10,000 BCE),[6][7] a Natufian site where archaeologists have discovered the remains of the oldest known bread.[8]

Geology

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Harrah region from the Space Shuttle

The Harrat comprises volcanic fields formed by tectonic activity from the Oligocene through to the Quaternary.[9] It is the largest of several volcanic fields on the Arabian Plate,[10] containing more than 800 volcanic cones and around 140 dikes.[9] 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.[11] It is known to have erupted in historic times.[12][13]

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.[14][15] and is one of a series of Quaternary volcanic fields paralleling the Red Sea coast.

History and economy

The Harrat has traditionally been occupied by nomadic Bedouin of the Anizah confedaration.[16][17] 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.[17] 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.[17][18] 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).[19]

Archaeological sites

Jordan

See also

Notes

  1. Variously transcribed as the harra, Ḥarrat ash-Shāmah (حَرَّة ٱلشَّامَة) or Ḥarrate-Shāmah (حَرَّةِ شَامَة).[citation needed]

References

Further reading

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