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Dahna
Ad-Dahna Desert is the central division of the Arabian Desert. It is a corridor of sandy terrain forming a bow-like shape that connects an-Nafud desert in the north to Rub' al-Khali desert in the south. Its length is more than siding Twaik Mountains from the east and does not exceed in width. It is also considered the geographical margin separating Al-Ahsa Province from Najd. Al-Dahna Desert is therefore the string that connects the great deserts of Saudi Arabia. The desert is a series of seven successive deserts, separated from one another by plains. Roads pass through Al-Dahnā, linking Kuwait with Al-Zilfī and Riyadh and connecting Riyadh with Hasa. Ad-Dahna desert is formed of high sand dunes spreading horizontally which are called veins (), mostly red in color since it contains Iron Oxides. Caves Beneath the harsh deserts of Saudi Arabia lie dark chambers and complex mazes filled with crystalline structures, stalactites and stalagmites. The limestone floor o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Al-Dahna
Ad-Dahna Desert is the central division of the Arabian Desert. It is a corridor of sandy terrain forming a bow-like shape that connects an-Nafud desert in the north to Rub' al-Khali desert in the south. Its length is more than siding Twaik Mountains from the east and does not exceed in width. It is also considered the geographical margin separating Al-Ahsa Province from Najd. Al-Dahna Desert is therefore the string that connects the great deserts of Saudi Arabia. The desert is a series of seven successive deserts, separated from one another by plains. Roads pass through Al-Dahnā, linking Kuwait with Al-Zilfī and Riyadh and connecting Riyadh with Hasa. Ad-Dahna desert is formed of high sand dunes spreading horizontally which are called veins (), mostly red in color since it contains Iron Oxides. Caves Beneath the harsh deserts of Saudi Arabia lie dark chambers and complex mazes filled with crystalline structures, stalactites and stalagmites. The limestone floor of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Najd
Najd is a Historical region, historical region of the Arabian Peninsula that includes most of the central region of Saudi Arabia. It is roughly bounded by the Hejaz region to the west, the Nafud desert in Al-Jawf Province, al-Jawf to the north, ad-Dahna Desert in Al-Ahsa Governorate, al-Ahsa to the east, and Rub' al Khali, Rub' al-Khali to the south, although its exact boundaries cannot be determined due to varying geographical and political limits throughout history. Administratively, Najd is divided into three main Provinces of Saudi Arabia, regions: the Riyadh Province, Riyadh region which features Wadi Hanifa and the Tuwaiq escarpment, which houses easterly Al-Yamama, Yamama with the Saudi capital, Riyadh since Emirate of Nejd, 1824, and the Sudairi region, which has its capital in Al Majma'ah, Majmaah. The second region, Al-Qassim Province, Al-Qassim, houses the fertile oases and date palm orchards spread out in the region's highlands along Wadi al-Rummah, Wadi Rummah in c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arabian Desert And East Sahero-Arabian Xeric Shrublands
The Arabian Desert () is a vast desert wilderness in West Asia that occupies almost the entire Arabian Peninsula with an area of . It stretches from Yemen to the Persian Gulf and Oman to Jordan and Iraq. It is the fourth largest desert in the world and the largest in Asia. At its center is ''Ar-Rub' al-Khali'' (The Empty Quarter), one of the largest continuous bodies of sand in the world. It is an extension of the Sahara Desert. Gazelles, oryx, sand cats, and spiny-tailed lizards are just some of the desert-adapted species that survive in this extreme environment, which features everything from red dunes to deadly quicksand. The climate is mostly dry (the major part receives around of rain per year, but some very rare places receive as little as 50 mm), and temperatures oscillate between very high heat and seasonal night time freezes. It is part of the deserts and xeric shrublands biome and lie in biogeographical realms of the Palearctic (northern part) and Afrotropical ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
An-Nafud
The Nafud desert or simply The Nafud () is a desert in the northern part of the Arabian Peninsula is , occupying a great oval depression. It is long and wide, with an area of . The Nafud is an erg, a desert region located in north-central Saudi Arabia. It is noted for its sudden violent winds, which account for the large crescent-shaped dunes. The sand in the Nafud is a brick-reddish color. Rain comes once or twice per year. In some lowland areas, namely those near the Hejaz Mountains, there are oases where dates, vegetables, barley, and fruits are grown. The Nafud is connected to the Rub' al Khali by the Dahna, a corridor of gravel plains and sand dunes, long and wide. During the Arab Revolt in 1917, forces led by Auda ibu Tayi attacked the Turkish-held coastal town of Aqaba on its poorly defended eastern flank. The approach was via a long and wide desert route, passing close to the edge of the Nafud. Colonel T. E. Lawrence asked Auda ibu Tayi to allow their group to stray f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rub' Al-Khali
The Rub' al KhaliOther standardized transliterations include: /. The ' is the assimilated Arabic definite article, ', which can also be transliterated as '. (; , ) or Empty Quarter is a desert encompassing most of the southern third of the Arabian Peninsula. The desert covers some (the area of long. 44.5°−56.5°E, and lat. 16.5°−23.0°N), including parts of Saudi Arabia, Oman, the United Arab Emirates, and Yemen. It is part of the larger Arabian Desert. Description Terrain The desert is long, and wide. Its surface elevation varies from in the southwest to around sea level in the northeast. Most of the terrain is ergs, with sand dunes up to high, interspersed with gravel and gypsum plains. The sand is reddish-orange due to the presence of feldspar. There are also brackish salt flats in some areas, such as the Umm al Samim area on the desert's eastern edge. Ali Al-Naimi reports that the sand dunes do not drift. He goes on to say, Sand blows off the surface, of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tuwaiq
Jabal Tuwaiq (, Tuwaiq Mountain) is a narrow escarpment that cuts through the plateau of Najd in central Arabia, running approximately 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 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. 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 an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arabian Desert
The Arabian Desert () is a vast desert wilderness in West Asia that occupies almost the entire Arabian Peninsula with an area of . It stretches from Yemen to the Persian Gulf and Oman to Jordan and Iraq. It is the fourth largest desert in the world and the largest in Asia. At its center is ''Ar-Rub' al-Khali'' (The Empty Quarter), one of the largest continuous bodies of sand in the world. It is an extension of the Sahara Desert. Gazelles, oryx, sand cats, and spiny-tailed lizards are just some of the desert-adapted species that survive in this extreme environment, which features everything from red dunes to deadly quicksand. The climate is mostly dry (the major part receives around of rain per year, but some very rare places receive as little as 50 mm), and temperatures oscillate between very high heat and seasonal night time freezes. It is part of the deserts and xeric shrublands biome and lie in biogeographical realms of the Palearctic (northern part) and Afrotro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rub' Al Khali
The Rub' al KhaliOther standardized transliterations include: /. The ' is the assimilated Arabic definite article, ', which can also be transliterated as '. (; , ) or Empty Quarter is a desert encompassing most of the southern third of the Arabian Peninsula. The desert covers some (the area of long. 44.5°−56.5°E, and lat. 16.5°−23.0°N), including parts of Saudi Arabia, Oman, the United Arab Emirates, and Yemen. It is part of the larger Arabian Desert. Description Terrain The desert is long, and wide. Its surface elevation varies from in the southwest to around sea level in the northeast. Most of the terrain is ergs, with sand dunes up to high, interspersed with gravel and gypsum plains. The sand is reddish-orange due to the presence of feldspar. There are also brackish salt flats in some areas, such as the Umm al Samim area on the desert's eastern edge. Ali Al-Naimi reports that the sand dunes do not drift. He goes on to say, Sand blows off the surface, of c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Stalagmites
A stalagmite (, ; ; ) is a type of rock formation that rises from the floor of a cave due to the accumulation of material deposited on the floor from ceiling drippings. Stalagmites are typically composed of calcium carbonate, but may consist of lava, mud, peat, pitch, sand, sinter, and amberat (crystallized urine of pack rats). The corresponding formation hanging down from the ceiling of a cave is a stalactite. Formation and type Limestone stalagmites The most common stalagmites are speleothems, which usually form in limestone caves. Stalagmite formation occurs only under certain pH conditions within the cavern. They form through deposition of calcium carbonate and other minerals, which is precipitated from mineralized water solutions. Limestone is the chief form of calcium carbonate rock, which is dissolved by water that contains carbon dioxide, forming a calcium bicarbonate solution in caverns. The partial pressure of carbon dioxide in the water must be greater than ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deserts Of Saudi Arabia
A desert is a landscape where little precipitation occurs and, consequently, living conditions create unique biomes and ecosystems. The lack of vegetation exposes the unprotected surface of the ground to denudation. About one-third of the land surface of the Earth is arid or semi-arid. This includes much of the polar regions, where little precipitation occurs, and which are sometimes called polar deserts or "cold deserts". Deserts can be classified by the amount of precipitation that falls, by the temperature that prevails, by the causes of desertification or by their geographical location. Deserts are formed by weathering processes as large variations in temperature between day and night strain the rocks, which consequently break in pieces. Although rain seldom occurs in deserts, there are occasional downpours that can result in flash floods. Rain falling on hot rocks can cause them to shatter, and the resulting fragments and rubble strewn over the desert floor are further e ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ancient Towns In Saudi Arabia
Thirteen ancient towns have been discovered in Saudi Arabia up to the present day. These include Qaryat al-Fāw, the Al-Ukhdūd archeological area, Hegra (Madā'in Ṣālih), Jubbah, Tārūt, Al-Shuwayḥaṭiyah, Thāj, Taimaa and Dūmat Al-Jandal. There are still more ancient towns in Saudi Arabia, but little information is currently available on them. Saudi Arabia occupies a unique and distinctive geographic location, bridging civilizations between continents. In ancient times the Arabian peninsula served as a corridor for trade; therefore it saw the beginning of many civilizations, the relics of which are still evident today. The Saudi government has recently established the Saudi Commission for Tourism and Antiquities, which is responsible for the preservation of these cities. Qaryat al-Fāw Qaryat al-Fāw (Arabic: قرية الفاو) also appears in the southern text as Qaryat Dhu Kahl (in association with the god Kahl), Qaryat al-Hamraa and Dhat al-Jnan. The name deri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saudi Geological Survey
The Saudi Geological Survey (SGS; ) is the national geological survey of the Kingdom of Saudi Arabia. History and profile The SGS was established as an independent entity attached to the ministry of petroleum and mineral resources following a council of ministers decision in 1999. It is built from other governmental agencies, including the former directorate general for mineral resources, the US Geological Survey (USGS) mission (1963–1999) and the Bureau de Recherches Géologiques et Minières (BRGM) mission (1972–1999). Activities The Saudi Geological Survey activities covers a broad range of strategic and applied earth science topics, with emphasis on understanding the geologic, economic, and engineering factors that affect sustainable management of mineral and groundwater resources, detection and mitigation of earthquakes and other geohazards, protection and management of the environment, and safe development of engineering and construction sites. The bulk of the wor ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
