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Kuhbonan Mountains
Kuhbonan Mountains or Kuhbonan Highlands, (Kuhbonan also pronounced as Kuhbanan), are a group of mountains that are located in the northern part of Kerman Province in Iran. Stretching in a northwest-southeast direction, the mountain range is situated in northwestern, eastern, and southeastern part of the city of Kerman, northeast of the town of Zarand, and southwest of the town of Ravar. With an elevation of 4233 metres, the highest point of the range is Mount Pelvar (Kuh-e Pelvar) or Mount Palvar (Kuh-e Palvar) that is located southeast of the city of Kerman and about 25 kilometres east of the town of Mahan. Geology Kuhbonan Mountain Range was formed mainly in the Miocene during the Alpine orogeny as the Arabian Plate finally collided with the Iranian Plate and consequently this region was pressed against the resistant Lut Block. Kuhbonan Range is made chiefly of Triassic and Jurassic rocks in the northwestern part, Jurassic rocks in the central section, and Upper Cretaceous roc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iran
Iran, officially the Islamic Republic of Iran, and also called Persia, is a country located in Western Asia. It is bordered by Iraq and Turkey to the west, by Azerbaijan and Armenia to the northwest, by the Caspian Sea and Turkmenistan to the north, by Afghanistan and Pakistan to the east, and by the Gulf of Oman and the Persian Gulf to the south. It covers an area of , making it the 17th-largest country. Iran has a population of 86 million, making it the 17th-most populous country in the world, and the second-largest in the Middle East. Its largest cities, in descending order, are the capital Tehran, Mashhad, Isfahan, Karaj, Shiraz, and Tabriz. The country is home to one of the world's oldest civilizations, beginning with the formation of the Elamite kingdoms in the fourth millennium BC. It was first unified by the Medes, an ancient Iranian people, in the seventh century BC, and reached its territorial height in the sixth century BC, when Cyrus the Great fo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kerman
Kerman ( fa, كرمان, Kermân ; also romanization of Persian, romanized as Kermun and Karmana), known in ancient times as the satrapy of Carmania, is the capital city of Kerman Province, Iran. At the 2011 census, its population was 821,394, in 221,389 households, making it the 10th most populous city of Iran. It is the largest and most developed city in Kerman Province and one of the most important cities in the southeast of Iran. It is also one of the largest cities of Iran in terms of area. Kerman is famous for its long history and strong cultural heritage. The city is home to many historic mosques and Zoroastrian fire temples. Kerman became the capital city of Iranian dynasties several times during its history. It is located on a large, flat plain, 800 km (500 mi) south-east of Tehran, the capital of Iran. History Kerman was founded as a defensive outpost, with the name Veh-Ardashir, by Ardashir I, founder of the Sasanian Empire, in the 3rd century AD. After th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zarand, Iran
Zarand ( fa, زرند) is a city and capital of Zarand County, Kerman Province, Iran. At the 2006 census, its population was 54,745, in 12,992 families. It is located about northwest of the provincial capital of Kerman. On February 22, 2005, a major earthquake killed hundreds of residents in the city of Zarand and several nearby villages in north Kerman. (See 2005 Zarand earthquake.) Southwest of Tehran, Iran, halfway between Tehran and Saveh, there is a plain also called Zarand. Zavyeh and Mamounieh are two small towns on this plain. A crater on Mars is named after this city.See List of craters on Mars. References Populated places in Zarand County Cities in Kerman Province {{Zarand-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ravar
Ravar ( fa, راور, also Romanized as Rāvar) is a city and capital of Ravar County, Kerman Province, Iran. Ravar is the national carpet city of Iran. At the 2006 census, its population was 22,910, in 5,921 families. Ravar produces a distinctive type of Kerman carpet Kerman carpets (sometimes "Kirman") are one of the traditional classifications of Persian carpets. Kerman is both a city and a province located in south central Iran, though the term sometimes describes a type which may have been made elsewhere. K .... Ravar is also well known for its vast pistachio fields. References Populated places in Ravar County Cities in Kerman Province {{Ravar-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mahan, Iran
Mahan ( fa, ماهان, also Romanized as Māhān or Mâhân; also known as Māhūn) is a city and capital of Mahan District, in Kerman County, Kerman Province, Iran. At the 2006 census, its population was 16,787, in 4,138 families. Mahan is well known for the tomb of the great Sufi leader Shah Ne'emat Ollah-e-Vali, as well as Shazdeh Garden (Prince Garden). The tomb of Shah Nur-eddin Nematollah Vali, poet, sage, Sufi and founder of an order of darvishes, has twin minarets covered with turquoise tiles from the bottom up to the cupola. The mausoleum was built by Ahmad Shah Kani; the rest of the building was constructed during the reigns of Shah Abbas I, Mohammad Shah Qajar and Nasser-al-Din Shah. Shah Nematallah Wali spent many years wandering through central Asia perfecting his spiritual gifts before finally settling at Mahan, twenty miles south-east of Kerman, where he passed the last twenty five years of his life. He died in 1431, having founded a Darvish order which continue ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. During the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arabian Plate
The Arabian Plate is a minor tectonic plate in the Northern and Eastern Hemispheres. It is one of the three continental plates (along with the African and the Indian Plates) that have been moving northward in geological history and colliding with the Eurasian Plate. That is resulting in a mingling of plate pieces and mountain ranges extending in the west from the Pyrenees, crossing Southern Europe to Iran, forming the Alborz and the Zagros Mountains, to the Himalayas and ranges of Southeast Asia. Lexicology The ''Arabian Plate'' is a designation of the region, and it is also sometimes referred to as the ''Arab Plate''. Borders The Arabian Plate consists mostly of the Arabian Peninsula; it extends westward to the Sinai Peninsula and the Red Sea and northward to the Levant. The plate borders are: *East, with the Indian Plate, at the Owen Fracture Zone *South, with the African Plate to the west and the Somali Plate and the Indian Plate to the east *West, a left lateral fa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iranian Plate
The Iranian Plate is a small tectonic plate thought to underlie the Persian plateau, covering the modern-day countries of Iran and Afghanistan, and parts of Iraq and Pakistan. It is compressed between the Arabian Plate to the southwest, the Eurasian Plate to the north, and the Indian Plate to the southeast. This compression is likely a cause for the very mountainous terrain of the area including the Alborz and Zagros Mountains The Zagros Mountains ( ar, جبال زاغروس, translit=Jibal Zaghrus; fa, کوههای زاگرس, Kuh hā-ye Zāgros; ku, چیاکانی زاگرۆس, translit=Çiyakani Zagros; Turkish: ''Zagros Dağları''; Luri: ''Kuh hā-ye Zāgro .... References * William Bayne Fisher''The Middle East: a Physical, Social, and Regional Geography'' Routledge 1978, , p. 15–16 Tectonic plates Geology of Afghanistan Geology of Iran Geology of Iraq Geology of Pakistan {{tectonics-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
