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Dena2
Dena (in Luri and fa, ) is the name for a sub-range within the Zagros Mountains, Iran. Mount Dena, with length and average width, is situated on the boundary of the Isfahan, Kohgiluyeh and Boyer-Ahmad and Chaharmahal and Bakhtiari Provinces of Iran. Mount Dena has more than 40 peaks higher than . With an elevation of 4,409 metres above sea level, Qash-Mastan is the highest peak in the Dena Range and in the Zagros Mountains in general. Another known peak in this range is Hose-Daal close to the city of Sisakht, to the north of Yasuj. Annual precipitation in Mount Dena ranges from and various rivers including a branch of the Karun rise in this range. Geologically, Mount Dena is located in the Sanandaj-Sirjan geologic and structural zone of Iran and is mainly made of Cretaceous limestone. On 18 February 2018, Iran Aseman Airlines Flight 3704 crashed into Mount Dena, killing all 65 people on board. Gallery Dena2.jpg, Dena3.jpg, Denaltgh6.jpg, Denaltgh4.jpg, Den ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Yasuj
Yasuj ( fa, ; also romanized as Yāsūj, Yasooj, and Yesūj; Luri language, Luri: ''Jasuc'' or ''Jasyç'') is a city and capital of Kohgiluyeh and Boyer-Ahmad Province, Iran. At the 2006 census, its population was 96,786, in 20,297 families. Yasuj is an industrial city in the Zagros, Zagros Mountains of southwestern Iran. The term ''Yasuj'' is also used to refer to the entire region. Yasuj has a sugar processing plant. History The area of Yasuj has been settled since as early as the Bronze Age. Findings include the Martyrs Hills (dating from 3rd millennium BC), the Khosravi Hill from the Achaemenid Empire, Achaemenian period, the ancient site of Gerd, the Pataveh bridge, and the Pay-e Chol cemetery. Yasuj is the place where Alexander III of Macedon and his Macedonian forces stormed the ''Persian Gates'' (''Darvazeh-ye Fars''), and found a way into the Fars Province, Persian heartland (331 BC). The Yasuj Museum, which opened in 2002, displays coins, statues, pottery, and bronze ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous
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 Ear ... [...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 the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Isfahan 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 ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Landforms Of Kohgiluyeh And Boyer-Ahmad 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 the fou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountaineering In Iran
Mountaineering or alpinism, is a set of outdoor activities that involves ascending tall mountains. Mountaineering-related activities include traditional outdoor climbing, skiing, and traversing via ferratas. Indoor climbing, sport climbing, and bouldering are also considered variants of mountaineering by some. Unlike most sports, mountaineering lacks widely applied formal rules, regulations, and governance; mountaineers adhere to a large variety of techniques and philosophies when climbing mountains. Numerous local alpine clubs support mountaineers by hosting resources and social activities. A federation of alpine clubs, the International Climbing and Mountaineering Federation (UIAA), is the International Olympic Committee-recognized world organization for mountaineering and climbing. The consequences of mountaineering on the natural environment can be seen in terms of individual components of the environment (land relief, soil, vegetation, fauna, and landscape) and location ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Biosphere Reserves Of Iran
The biosphere reserves of Iran have a total land area of 1.64 million km2. They support more than 8,000 recorded species of plants (almost 2,421 are endemic), 502 species of birds, 164 species of mammals, 209 species of reptiles, and 375 species of butterflies. Iran has taken many steps to protect its natural resources, biodiversity, and landscapes. The country has established national parkss, natural monuments, wildlife sanctuaries, and protected areas. The country has also identified and registered 13 areas as biosphere reserves since 1976. List * Arasbaran, 1976 * Arjan Protected Area and Lake Parishan, 1976 * Geno, 1976 * Golestan, 1976 * Hara, 1976 * Kavir, 1977 * Lake Oromeeh, 1976 * Miankaleh, 1976 * Touran, 1976 * Dena, 2010 * Tang-e-Sayad & Sabzkuh, 2015 * Hamoun, 2016 * Kopet Dag, 2018 See also * Geography of Iran * Iranian Plateau * List of national parks and protected areas of Iran The National parks and protected areas, and wildlife refuges, of Iranse ... [...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] |
Mountains Of Kohgiluyeh And Boyer-Ahmad Province
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] |
Mountains Of Isfahan Province
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] |
List Of Ultras Of West Asia
This is a list of all 101 of the ultra-prominent peaks (with topographic prominence greater than 1,500 metres) in West Asia. It includes peaks on the islands of Cyprus and Socotra. It also includes the 10 ultras of the Caucasus (also listed under Europe) as they are geographically more connected to the mountains of West Asia. Two of these peaks (Mount Aragats and Kapudzhukh Lerr) are on the Asian side of the ridge of the Greater Caucasus, which forms the boundary between Asia and Europe, and four more are on the border itself and so in both Europe and Asia. List / Georgia , , Greater Caucasus , , 2348 , , - , 4.05 , , Mount Aragats , , 4,090 , , 2,143 , , Armenia , , Lesser Caucasus , , 1947 , , - , 4.06 , , Dykh-Tau , , 5,205 , , 2,002, , Russia , , Greater Caucasus , , 3203 , , - , 4.07 , , Dyultydag , , 4,127 , , 1,834 , , Russia , , Greater Caucasus , , 2293 , , - , 4.08 , , Kapudzhukh Lerr , , 3,905 , , 1,820, , Armenia / ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Iranian Four-thousanders
This list contains all of the summits and subsidiary tops of or more above sea level in Iran. Since there is no precise or formal definition of a mountain summit, the number of 4000-metre summits or four-thousanders is arbitrary. Topographic prominence is an important factor in deciding the official nomination of a summit. The list here is based not only on prominence but also on other criteria, such as morphology (general appearance) and mountaineering interest. A minimum prominence criterion of 500 metres would considerably reduce the number of four-thousanders. List The table shows the four-thousanders in Iran. There are several summits in the list with multiple peaks, where only the highest is listed. ''Clicking the symbol at the head of the column sorts the table by that column's data.'' See also * Iranian plateau * List of Ultras of West Asia * Four-thousanders References Bibliography * Ali Moghim, ''Mountaineering in Iran'', Rozaneh, 3rd edition, 2006, (in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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