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Mount Jahanbin
Mount Jahanbin (32°11′18″N 50°40′46″E) is a mountain in Chaharmahal and Bakhtiari Province, central Iran. Jahanbin mount is about 2 km west of the Hafshejan City, 15 km south of Shahrekord and 100 km in south-west of Isfahan Isfahan ( fa, اصفهان, Esfahân ), from its Achaemenid empire, ancient designation ''Aspadana'' and, later, ''Spahan'' in Sassanian Empire, middle Persian, rendered in English as ''Ispahan'', is a major city in the Greater Isfahan Regio .... Mount Jahanbin is part of Zagros mountain range which runs along the northwest to southeast of Iran. From the geological point of view Jahanbin mount in made of limestones from the Cretaceous period located in the folded Zagros geological structure. {{coord, 32, 11, 18, N, 50, 40, 46, E, display=title Mountains of Chaharmahal and Bakhtiari Provinces Landforms of Chaharmahal and Bakhtiari province Mountains of Iran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Iran ...
Central Iran consists of the southern slopes of the Alborz Mountains in the north, the Zagros Mountains in south, the Central Iranian Range, and the desert of Dasht-e Kavir. It includes the provinces of Esfahan, Yazd, Chahar Mahal and Bakhtiari, Markazi, Qazvin, Alborz, Tehran, Qom and Semnan. The major cities are Tehran, Isfahan, Arak, Yazd, Karaj, Qazvin, Qom, Kashan, Saveh and Shahr-e Kord. Climate *Hot desert climate in the deserts. *Cold desert climate in the central mountains. *Humid continental climate on the few rivers. *cold semi-arid climate in the high mountains. See also * Northern Iran * Western Iran * Northwestern Iran * Eastern Iran * Southern Iran References {{Reflist Subdivisions of Iran 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 Turkmeni ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shahrekord
Shahr-e Kord ( fa, شهركرد, also Romanized as Shahrekord and Shahr Kord) is the capital city of Chaharmahal and Bakhtiari Province, Iran. It is the largest city in the province, and is 90 km away from Iran's third largest city, Isfahan. At the time of the 2006 census, Shahrekord had a population of about 148,464 and the Shahrekord metropolitan area had a population of 380,312. The city is populated by Persians, Lurs and Turkic people. Etymology Shahr-e Kord, at face value, seems to mean "City of the Kurds". In antiquity, the place had been called "Dezh Gord" (دژگرد), where ''dezh'' (دژ) means "fortress" and ''gord'' (گرد) means "hero". After the Muslim conquest of Persia, the name changed to "Deh Kord" ( fa, دهكرد); ''dezh'' was reinterpreted as ''deh'' (ده) meaning "village" and ''gord'' became ''kord'' because the Arabic alphabet lacks the letters "g" (گ), and "zh" (ژ). Other examples of cities whose names changed partly due to the influence of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Isfahan
Isfahan ( fa, اصفهان, Esfahân ), from its Achaemenid empire, ancient designation ''Aspadana'' and, later, ''Spahan'' in Sassanian Empire, middle Persian, rendered in English as ''Ispahan'', is a major city in the Greater Isfahan Region, Isfahan Province, Iran. It is located south of Tehran and is the capital of Isfahan Province. The city has a population of approximately 2,220,000, making it the third-largest city in Iran, after Tehran and Mashhad, and the second-largest metropolitan area. Isfahan is located at the intersection of the two principal routes that traverse Iran, north–south and east–west. Isfahan flourished between the 9th and 18th centuries. Under the Safavids, Safavid dynasty, Isfahan became the capital of Achaemenid Empire, Persia, for the second time in its history, under Shah Abbas the Great. The city retains much of its history. It is famous for its Perso–Islamic architecture, grand boulevards, covered bridges, palaces, tiled mosques, and mina ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 Zāgros'' ''کویا زاگرس'') are a long mountain range in Iran, northern Iraq, and southeastern Turkey. This mountain range has a total length of . The Zagros mountain range begins in northwestern Iran and roughly follows Iran's western border while covering much of southeastern Turkey and northeastern Iraq. From this border region, the range continues to the southeast under also the waters of the Persian Gulf. It spans the southern parts of the Armenian highland, the whole length of the western and southwestern Iranian plateau, ending at the Strait of Hormuz. The highest point is Mount Dena, at . Geology The Zagros fold and thrust belt was mainly formed by the collision of two tectonic plates, the Eurasian Plate and the Arabian Plat ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestones
Limestone ( calcium carbonate ) is a type of carbonate sedimentary rock which is the main source of the material lime. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of . Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years. Limestone often contains fossils which provide scientists with information on ancient environments and on the evolution of life. About 20% to 25% of sedimentary rock is carbonate rock, and most of this is limestone. The remaining carbonate rock is mostly dolomite, a closely related rock, which contains a high percentage of the mineral dolomite, . ''Magnesian limestone'' is an obsolete and poorly-defined term used variously for dolomite, for limestone co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous Period
The Cretaceous ( ) is a geological period that lasted from about 145 to 66 million years ago (Mya). It is the third and final period of the Mesozoic Era, as well as the longest. At around 79 million years, it is the longest geological period of the entire Phanerozoic. The name is derived from the Latin ''creta'', "chalk", which is abundant in the latter half of the period. It is usually abbreviated K, for its German translation ''Kreide''. The Cretaceous was a period with a relatively warm climate, resulting in high eustatic sea levels that created numerous shallow inland seas. These oceans and seas were populated with now-extinct marine reptiles, ammonites, and rudists, while dinosaurs continued to dominate on land. The world was ice free, and forests extended to the poles. During this time, new groups of mammals and birds appeared. During the Early Cretaceous, flowering plants appeared and began to rapidly diversify, becoming the dominant group of plants across the Earth by t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Chaharmahal And Bakhtiari Provinces
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Chaharmahal And Bakhtiari Province
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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