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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 the 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) which 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 Cre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kerman Province
Kerman province () is the largest of the 31 provinces of Iran. Its capital is the city of Kerman. The province is in the southeast of Iran. In 2014 it was placed in Region 5. Mentioned in ancient times as the Achaemenid satrapy of Carmania, Kerman province has an area of , encompassing nearly 11% of the land area of Iran.http://www.sci.org.ir/content/userfiles/_sci_en/sci_en/sel/year85/f1/CS_01_4.HTM History According to a text from the 8th century commontly attributed to the Armenian historian Movses Khorenatsi, present-day Kerman province was situated in the southern quarter of the Sasanian Empire. The main city of the region from the Sasanian era to the 10th century was Sirjan. Early Muslim geographers considered the area as part of the hot climatic zone and the mountainous interior as home of predatory people including the Kufečs (or Kofejān). Hamdallah Mustawfi stated that predatory beasts roamed the area which by then had undergone forestation. In the 13th c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iran
Iran, officially the Islamic Republic of Iran (IRI) and also known as Persia, is a country in West Asia. It borders Iraq to the west, Turkey, Azerbaijan, and Armenia to the northwest, the Caspian Sea to the north, Turkmenistan to the northeast, Afghanistan to the east, Pakistan to the southeast, and the Gulf of Oman and the Persian Gulf to the south. With a Ethnicities in Iran, multi-ethnic population of over 92 million in an area of , Iran ranks 17th globally in both List of countries and dependencies by area, geographic size and List of countries and dependencies by population, population. It is the List of Asian countries by area, sixth-largest country entirely in Asia and one of the world's List of mountains in Iran, most mountainous countries. Officially an Islamic republic, Iran is divided into Regions of Iran, five regions with Provinces of Iran, 31 provinces. Tehran is the nation's Capital city, capital, List of cities in Iran by province, largest city and financial ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kerman
Kerman (; ) is a city in the Central District (Kerman County), Central District of Kerman County, Kerman province, Kerman province, Iran, serving as capital of the province, the county, and the district. 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 the Battle of Nahāvand in 642, the city came under Muslim rule. At first, the city's relative isolation allowed Kharijites and Zoroastrianism, Zoroastrians to thrive there, but the Kharijites were wiped out in 698, and the population was mostly Muslim by 725. Already in the eighth century the city was famous for its manufacture of cashmere wool shawls and other textiles. The Abbasid Caliphate's authority Anarchy at Samarra, over the region was weak, and power passed in the tenth century to the Buyid dynasty, Buyid emirs. The region and city fell to Mahmud of Ghazni in the late tenth century. The name Kerman was adop ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zarand, Iran
Zarand () is a city in the Central District of Zarand County, Kerman province, Iran, serving as capital of both the county and the district. Demographics Population At the time of the 2006 National Census, the city's population was 54,745 in 12,992 households. The following census in 2011 counted 57,749 people in 15,461 households. The 2016 census measured the population of the city as 60,370 people in 16,722 households. Geography Location The city of Zarand is about northwest of the provincial capital of Kerman. Southwest of Tehran, Iran, halfway between Tehran and Saveh, there is a plain also called Zarand. A crater on Mars is named after this city.See List of craters on Mars __NOTOC__ This is a list of craters on Mars. Impact craters on Mars larger than exist by the hundreds of thousands, but only about one thousand of them have names. Names are assigned by the International Astronomical Union after petitioning .... Earthquakes On 22 February 2005, a major ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ravar
Ravar () is a city in the Central District of Ravar County, Kerman province, Iran, serving as capital of both the county and the district. Known as the national carpet city of Iran, 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. The term also sometimes describes a type which may have been made elsewhere. Ty ..., and is also well known for its vast pistachio fields. Demographics Population At the time of the 2006 National Census, the city's population was 18.500 in 5,921 households. The following census in 2011 counted 19.100 people in 6,260 households. The 2016 census measured the population of the city as 19,800 people in 6,874 households. See also Notes References Cities in Kerman province Populated places in Ravar County {{Ravar-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mahan, Iran
Mahan () is a city in, and the capital of, Mahan District of Kerman County, Kerman province, Iran. History 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 continues to be an active spiritual force today. The central domed burial vault at Mahan, completed in 1437 was erected by A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first epoch (geology), 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 followed the Oligocene and preceded 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 distinct global events but by regionally defined transitions from the warmer Oligocene to the cooler Pliocene Epoch. During the Early Miocene, Afro-Arabia collided with Eurasia, severing the connection between the Mediterranean and Indian Oceans, and allowing the interchange of fauna between Eurasia and Africa, including the dispersal of proboscideans and Ape, hominoids into Eurasia. During the late Miocene, the conn ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alpine Orogeny
The Alpine orogeny, sometimes referred to as the Alpide orogeny, is an orogenic phase in the Late Mesozoic and the current Cenozoic which has formed the mountain ranges of the Alpide belt. Cause The Alpine orogeny was caused by the African continent, the Arabian Peninsula, the Indian subcontinent, and the Cimmerian plate colliding with Eurasia in the north. Convergent movements between the African, Arabian and Indian plates from the south, and the Eurasian plate and the Anatolian sub-plate from the north – as well as many smaller (micro)plates – had already begun during the early Cretaceous, but the major phases of mountain building began during the Paleocene to the Eocene. The process continues currently in some of the Alpide mountain ranges. The Alpine orogeny is considered one of the three major phases of orogeny in Europe that define the geology of that continent, along with the Caledonian orogeny that formed the Old Red Sandstone Continent when the continents ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Iranian Plate
The Iranian plateau or Persian plateau is a geological feature spanning parts of the Caucasus, Central Asia, South Asia, and West Asia. It makes up part of the Eurasian plate, and is wedged between the Arabian plate and the Indian plate. The plateau is situated between the Zagros Mountains to the west, the Caspian Sea and the Köpet Dag to the north, the Armenian Highlands and the Caucasus Mountains to the northwest, the Strait of Hormuz and the Persian Gulf to the south, and the Indian subcontinent to the southeast. As a historical region, it includes Parthia, Media, Persis, and some of the previous territories of Greater Iran."Old Iranian Online" , University of Texas College of Liberal Arts (retrieved 10 February 2007) The Zagros form the plateau's western boundary, and its eastern slopes may also be in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ; sometimes symbolized 🝈) is a geologic period and system which spans 50.5 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.4 Mya. The Triassic is the first and shortest period of the Mesozoic Era and the seventh period of the Phanerozoic Eon. 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 ... [...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 143.1 Mya. The Jurassic constitutes the second and middle period of the Mesozoic, Mesozoic Era as well as the eighth period of the Phanerozoic, Phanerozoic Eon 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 (CAMP). The beginning of the Toarcian Age started around 183 million years ago and is marked by the Toarcian Oceanic Anoxic Event, a global episode of Anoxic event, oceanic anoxia, ocean acidification, and elevated global temperatures associated with extinctions, likely caused by the eruption of the Kar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
