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Al Hoota Cave
Al Hoota Cave ( ar, كَهْف ٱلْهُوْتَه, Kahf Al-Hūtah) is a cave located in Al-Hamra', Ad Dakhiliyah Governorate, Oman Oman ( ; ar, عُمَان ' ), officially the Sultanate of Oman ( ar, سلْطنةُ عُمان ), is an Arabian country located in southwestern Asia. It is situated on the southeastern coast of the Arabian Peninsula, and spans the mouth of ..., that is long. The cave was first discovered by locals several hundred years ago and was officially opened as a tourist destination in December 2006. The Omani blind cave fish lives in this cave system. Stalagmites from this cave yield data on the palaeoclimate.FLEITMANN, D., J. Haldon, R. Bradley, S. Burns, Hai Cheng, R. Edwards, C. Raible, M. Jacobson, A. Matter 2022. Droughts and societal change: The environmental context for the emergence of Islam in late antique Arabia, Science 376, 1317–21. References External links Official website {{Authority control Caves of Oman Wild caves ...
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Al Hajar Mountains
The Hajar Mountains ( ar, جِبَال ٱلْحَجَر, Jibāl al-Ḥajar, ''The Rocky Mountains'' or ''The Stone Mountains'') in northeastern Oman and also the eastern United Arab Emirates are the highest mountain range in the eastern Arabian peninsula. Also known as "Oman Mountains", they separate the low coastal plain of Oman from the high desert plateau, and lie inland from the Gulf of Oman. ''Al'' () means "the", and ''Ḥajar'' () means "stone" or "rock". So ''al-Ḥajar'' () is named as "the stone" or "the rock". Geology Orography and tectonic setting The Hajar Mountains extend for through the UAE and Oman. They are located on the north-east corner of the Arabian Plate, reaching from the Musandam Peninsula through to the east coast of Oman. The range is about wide, with Jabal Shams being the highest peak at 3,009 m (9,872 ft) in the central region of the mountains. Currently, the Arabian Plate is moving north relative to the Eurasian Plate at per ye ...
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Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ...
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Electric
Electricity is the set of physical phenomena associated with the presence and motion of matter that has a property of electric charge. Electricity is related to magnetism, both being part of the phenomenon of electromagnetism, as described by Maxwell's equations. Various common phenomena are related to electricity, including lightning, static electricity, electric heating, electric discharges and many others. The presence of an electric charge, which can be either positive or negative, produces an electric field. The movement of electric charges is an electric current and produces a magnetic field. When a charge is placed in a location with a non-zero electric field, a force will act on it. The magnitude of this force is given by Coulomb's law. If the charge moves, the electric field would be doing work on the electric charge. Thus we can speak of electric potential at a certain point in space, which is equal to the work done by an external agent in carrying a unit of positiv ...
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Al Hamra, Oman
Al Hamra ( ar, ٱلْحَمْرَاء, Al-Ḥamrāʾ) is a 400-year-old town in the region Ad Dakhiliyah, in northeastern Oman. As a province (wilayat), it is home to a number of villages including the mountainside village of Misfat Al Abryeen, with the village of Ghul to the northwest of the town, and Bimah to the north-northeast. The town and province lie on the southern slopes of the Akhdar Mountains. Al Hamra is also known as Hamra Al Abryeen with reference to the Al Abri tribe who live there. Near the center of the town is a plaza and the souq. Some of the oldest preserved houses in Oman can be found in Al Hamra, a town built on a tilted rock slab. Many of the houses have two, three and even four stories, with ceilings made of palm beams and fronds topped by mud and straw. Visitors to the nearby souq can watch a halwa maker at work in the only halwa shop still operating in the old souq. Mount Shams (the sun mountain), the highest mountain in Oman, sits northeast of the ...
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Ad Dakhiliyah Governorate
Ad Dakhiliyah ( ar, الداخلية, Ad-Dāḫilīyah, meaning: The Interior) is one of the governorates (''muhafazah'') of Oman with Nizwa town as the regional center. It was previously a region (''mintaqah''). It became a governorate on 28 October 2011. Provinces Ad Dakhiliyah Governorate consists of eight provinces (wilayat): *Nizwa *Samail * Bahla *Adam Adam; el, Ἀδάμ, Adám; la, Adam is the name given in Genesis 1-5 to the first human. Beyond its use as the name of the first man, ''adam'' is also used in the Bible as a pronoun, individually as "a human" and in a collective sense as " ... * Al Hamra * Manah * Izki * Bid Bid Demographics References Governorates of Oman {{Oman-geo-stub ...
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Oman
Oman ( ; ar, عُمَان ' ), officially the Sultanate of Oman ( ar, سلْطنةُ عُمان ), is an Arabian country located in southwestern Asia. It is situated on the southeastern coast of the Arabian Peninsula, and spans the mouth of the Persian Gulf. Oman shares land borders with Saudi Arabia, the United Arab Emirates, and Yemen, while sharing Maritime boundary, maritime borders with Iran and Pakistan. The coast is formed by the Arabian Sea on the southeast, and the Gulf of Oman on the northeast. The Madha and Musandam Governorate, Musandam exclaves are surrounded by the United Arab Emirates on their land borders, with the Strait of Hormuz (which it shares with Iran) and the Gulf of Oman forming Musandam's coastal boundaries. Muscat is the nation's capital and largest city. From the 17th century, the Omani Sultanate was Omani Empire, an empire, vying with the Portuguese Empire, Portuguese and British Empire, British empires for influence in the Persian Gulf and Indian ...
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Omani Blind Cave Fish
''Garra barreimiae'', the Oman garra, is a species of ray-finned fish in the family Cyprinidae. It is found in the mountains of northern Oman and in the United Arab Emirates. Most populations inhabit wadis, streams, pools and springs, but one population which lives in a cave system, is known as Omani blind cave fish, and has lost its sight and pigmentation. The only other cave fish in the Arabian Peninsula is the Tawi Atair garra (''G. dunsirei''), but it has normal eyes.Romero, A., editor (2001). The Biology of Hypogean Fishes, p. 17. Developments in Environmental Biology of Fishes. Taxonomy The Oman garra was first described in 1956 by the American zoologist Henry Weed Fowler and the Israeli zoologist Heinz Steinitz as ''Garra barreimiae''. The following subspecies are recognised: * ''G. b. barreimiae'' Fowler & Steinitz, 1956 * ''G. b. gallagheri'' Krupp, 1988 * ''G. b. shawkahensis'' Banister & Clarke, 1977 * ''G. b. wurayahi'' Khalaf, 2009 The blind cave form has been ...
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Caves Of Oman
A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word ''cave'' can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called ''exogene'' caves. Caves which extend further underground than the opening is wide are called ''endogene'' caves. Speleology is the science of exploration and study of all aspects of caves and the cave environment. Visiting or exploring caves for recreation may be called ''caving'', ''potholing'', or ''spelunking''. Formation types The formation and development of caves is known as ''speleogenesis''; it can occur over the course of millions of years. Caves can range widely in size, and are formed by various geological processes. These may involve a combination of chemical processes, erosion by water, tectonic forces, microorgani ...
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