Tuwaiq

Tuwaiq
A view of the Tweig (Tuwaiq) Escarpment from the west. The Saudi capital Riyadh lies just beyond the horizon
Highest point
Elevation600 metres (2,000 ft)
Coordinates19°54′51″N 45°15′6″E / 19.91417°N 45.25167°E / 19.91417; 45.25167 (Jabal e-Malaika)
Naming
Native nameجَبَل طُوَيْق (Arabic)
Geography
Tuwaiq is located in Saudi Arabia
Tuwaiq
Tuwaiq
Location in Saudi Arabia
Tuwaiq is located in West and Central Asia
Tuwaiq
Tuwaiq
Tuwaiq (West and Central Asia)
LocationNajd, Saudi Arabia
ProvinceRiyadh Province

Jabal Tuwaiq (Arabic: جَبَل طُوَيْق, lit.'Tuwaiq Mountain') or Tuwaiq Escarpment is a narrow escarpment that cuts through the plateau of Najd in central Arabia,[1] running approximately 800 km (500 miles)[2] from the southern border of Al-Qasim in the north, to the northern edge of the Rub' al Khali desert near Wadi ad-Dawasir in the south. It is 600 m (2,000 ft) high and also has a Middle Jurassic stratigraphic section. The eastern side slopes downwards gradually, while the western side ends in an abrupt manner. The escarpment can be thought of as a narrow plateau, though the locals refer to it as a jebel ("mount"). Marshall Cavendish used the name "Tuwayr Mountains" to describe mountains of central Arabia, distinct from the Shammar in the north, the Dhofar in the south, and the Hajar to the east.[3]

Many narrow valleys (wadis) run along its sides, such as Wadi Hanifa, and a group of towns lie on its central section, including the Saudi capital, Riyadh. Many settlements have historically existed on either side of it as well, such as those of Sudair and Al-Washm. The Tweig escarpment is mentioned in Yaqut's 13th century geographical encyclopedia under the name "Al-'Aridh", though for the past few centuries that name has applied only to the central section of it, around Riyadh.

Jebel Fihrayn

Jebel Fihrayn or Edge of the World is a cliff of 1.131 m height that lies some 100 km northwest from Riyadh. Formed by tectonic movements of the Arabian plate, the cliffs drop down 300 m into an ancient ocean bed. They are a popular touritic spot offering wide views of a vast desert landscape.[4]

Petroleum geology

The Arab-D (Upper Jurassic) unit of the Riyadh Group makes up one of the largest petroleum reservoirs in the world. Bureau and Saudi Aramco researchers conducted a high-resolution LIDAR survey of Middle Jurassic outcrops of the Tuwaiq Mountain limestone along the Tuwaiq Mountain Escarpment near the city of Riyadh, Saudi Arabia. This study was a first step towards building a quantitative 3-D geologic model for use as an analog to the lower Arab-D reservoir. Outcrop analogs like this one are critical to understanding reservoir performance on the flow-unit scale (1 to 30 m (98 ft)). Although seismic data allow geologists to gain information about large-scale reservoir compartmentalization (>30 metres (98 feet)), flow-unit scale reservoir parameters are far below seismic imaging capability and inter-well spacing.[5]

High-precision laser scans were used as a template upon which stratigraphic interpretation were made allowing researchers to characterize sub-seismic, flow-unit scale reservoir properties of Jurassic bioherms in an effort to better understand optimum production techniques of this enormous reservoir.

See also

References

  1. ^ Scoville, Sheila A. (2006). Gazetteer of Arabia: a geographical and tribal history of the Arabian Peninsula. Vol. 2. Akademische Druck- u. Verlagsanstalt. pp. 117–122. ISBN 0-7614-7571-0.
  2. ^ Ghazanfar, Shahina A.; Fisher, Martin (17 April 2013). "11–13". Vegetation of the Arabian Peninsula. Sultan Qaboos University, Muscat, Oman: Springer Science & Business Media. pp. 270–345. ISBN 978-9-4017-3637-4.
  3. ^ "Geography and climate". World and Its Peoples. Vol. 1. Marshall Cavendish. 2007. pp. 8–19. ISBN 978-0-7614-7571-2.
  4. ^ "Edge of the World". Retrieved 20 February 2026.
  5. ^ Rosales, Idoia; Pomar, Luis; Al-Awwad, Saad Fahd (2018). "Microfacies, diagenesis and oil emplacement of the Upper Jurassic Arab-D carbonate reservoir in an oil field in central Saudi Arabia (Khurais Complex)". Marine and Petroleum Geology. 96: 551–576. doi:10.1016/j.marpetgeo.2018.05.010.