An ultra-prominent peak, or Ultra for short, is a mountain summit with a topographic prominence of 1,500 metres or more. There are 1,524 such peaks on Earth; some peaks, such as the Matterhorn and Eiger, are not Ultras because they are connected to higher mountains by high cols and therefore do not achieve enough topographic prominence. The term "Ultra" originated with earth scientist Stephen Fry, from his studies of the prominence of peaks in Washington in the 1980s, his original term was "ultra major mountain", referring to peaks with at least 1,500 metres of prominence. 1,515 Ultras have been identified above sea level: 637 in Asia, 353 in North America, 209 in South America, 119 in Europe, 84 in Africa, 69 in Australasia and 39 in Antarctica. Many of the world's largest mountains are Ultras, including Mount Everest, K2, Mont Blanc, Mount Olympus. On the other hand, others such as the Eiger and the Matterhorn are not Ultras because they do not have sufficient prominence. Many Ultras lie in visited and inhospitable parts of the world, including 39 in Greenland, the high points of the Arctic islands of Novaya Zemlya, Jan Mayen and Spitsbergen, many of the peaks of the Greater ranges of Asia.
In British Columbia, some of the mountains listed do not have recognized names. Thirteen of the fourteen 8,000m summits are Ultras, there are a further 64 Ultras over 7,000 metres in height. There are 90 Ultras with a prominence of over 3,000 metres, but only 22 with more than 4,000 metres prominence. A number of Ultras have yet to be climbed, with Sauyr Zhotasy, Mount Siple, Gangkar Puensum being the most candidates for the most prominent unclimbed mountain in the world. All of the Seven Summits are Ultras by virtue of the fact that they are the high points of large landmasses; each has its key col at or near sea level, resulting in a prominence value equal to its elevation. List of peaks by prominence gives the 125 most prominent peaks worldwide. List of islands by highest point gives the 75 highest island highpoints, all of which are Ultras List of Alpine peaks by prominence List of non-Alpine European Ultras, including Atlantic islands and the Caucasus List of Ultras in West Asia List of Ultras in Central Asia List of Ultras of the Karakoram and Hindu Kush List of Ultras of the Himalayas, including Sino-Nepal Provinces List of Ultras of Tibet, East Asia and neighbouring areas, including India List of Ultras in Northeast Asia List of Ultras in Japan List of Ultras in Southeast Asia List of Ultras in the Philippines List of Ultras of Malay Archipelago List of African Ultras List of Ultras in Oceania, including the Southern Indian Ocean List of ultra-prominent summits of Australia List of ultra-prominent summits of Indonesian New Guinea List of ultra-prominent summits of New Zealand List of ultra-prominent summits of Papua New Guinea List of ultra-prominent summits of the Hawaiian Islands List of ultra-prominent summits of the Pacific Islands List of ultra-prominent summits of the Southern Indian Ocean List of Ultras in Antarctica, including South Atlantic islands List of Ultras in North America List of Ultras in Canada List of Ultras in the United States List of Ultras in Alaska List of Ultras in Greenland List of Ultras in Mexico List of Ultras in Central America List of Ultras in the Caribbean List of Ultras in South America List of mountain lists List of peaks by prominence Prominence
Buni is the headquarters of Upper [[Chitral District in Khyber Pakhtunkhwa, Pakistan. The residents of Buni are Khos, a minority Shina are present. Urdu, the national language of Pakistan, is spoken and understood; the climate is considered to be a local steppe climate. During the year there is little rainfall; this climate is considered to be BSK according to the Köppen-Geiger climate classification. The average annual temperature in Buni is 15.6 °C. About 418 mm of precipitation falls annually. There's a number of educational institution in Buni. Aga Khan High School Buni Govt Degree College Buni Govt High School Buni Govt Girls Degree College Buni Pamir School & College Buni Space Era Model School Buni Oxford Public School Buni Pearl College Buni Buni Zom Mastuj Media related to Booni at Wikimedia Commons
Tirich Mir is the highest mountain of the Hindu Kush range, the highest mountain in the world outside of the Himalayas-Karakoram range, located in Chitral District of Pakistan. The mountain was first climbed on 21 July 1950 by a Norwegian expedition consisting of Arne Næss, P. Kvernberg, H. Berg, Tony Streather. Tirich Mir overlooks Chitral town, can be seen from the main bazaar; the last village in Chitral before reaching Tirich Mir is the village of Tirich. It is located in Mulkow; the people there speak the Khowar language. The residents are available for hire as porters and tourist guides and will lead trekkers part way up the mountain, but there is a point beyond which they will not go, it is believed the origin of the name Tirich Mir is "King of Tirich" as Tirich is the name of a side valley of the Mulkhow valley of Chitral which leads up to Tirich Mir. An alternative etymology derives this name from the Wakhi language. In Wakhi, trich means shadow or darkness and mir means king, so Tirich Mir means king of darkness.
It could have gotten this name. The weather station 4,245 m above sea level lies in the Tundra climate/Alpine climate zone according to Köppen Climate Classification. On this specific altitude we find moderately cold winters and cool summers above freezing. Annual mean temperature is −5.25 °C, which puts the station well inside the range of continuous permafrost. The average temperature in the coldest month of January is −17.5 °C and the two hottest months of July and August have mean temperatures of 6.5 °C. Average low temperatures range from − 23 °C in January to 0 °C in August. On higher elevations near the summit however, one can find the ice cap climate, marked by no month having an daily mean temperature of above freezing. Here ice and snow never melt and average daily temperatures range from around −35 °C in winter to −15 °C in summer. Khyber-Pakhtunkhwa List of mountains in Pakistan List of highest mountains List of Ultras of the Karakoram and Hindu Kush Keay, John, "The Gilgit Game": The Explorers of the Western Himalayas, 1865-95, Oxford University Press, 1985, ISBN 0-19-577466-3 Robertson, Sir George Scott, The Kafirs of the Hindukush, Oxford University Press, ISBN 0-19-577127-3 Tirich Mir on SummitPost
The Hindu Raj is a mountain range in northern Pakistan, between the Hindu Kush and the Karakoram ranges. Its highest peak is 6,872 m. Other notable peaks include Ghamubar Zom and Gul Lasht Zom; the range is less well-known than its neighbors because of the absence of any 8000 or 7000 meter peaks
The Hindu Kush known in Ancient Greek as the Caucasus Indicus or Paropamisadae, is an 800-kilometre-long mountain range that stretches near the Afghan-Pakistan border, from central Afghanistan to northern Pakistan. It forms the western section of the Hindu Kush Himalayan Region, it divides the valley of the Amu Darya to the north from the Indus River valley to the south. The Hindu Kush range has numerous high snow-capped peaks, with the highest point in the Hindu Kush being Tirich Mir or Terichmir at 7,708 metres in the Chitral District of Khyber Pakhtunkhwa, Pakistan. To the north, near its northeastern end, the Hindu Kush buttresses the Pamir Mountains near the point where the borders of China and Afghanistan meet, after which it runs southwest through Pakistan and into Afghanistan near their border; the eastern end of the Hindu Kush in the north merges with the Karakoram Range. Towards its southern end, it connects with the Spin Ghar Range near the Kabul River; the Hindu Kush range region was a significant centre of Buddhism with sites such as the Bamiyan Buddhas.
The range and communities settled in it hosted ancient monasteries, important trade networks, travelers between Central Asia and South Asia. The Hindu Kush range has been the passageway during the invasions of the Indian subcontinent, continues to be important during modern-era warfare in Afghanistan. Geologically, the range is rooted in the formation of a subcontinent from a region of Gondwana that drifted away from East Africa about 160 million years ago, around the Middle Jurassic period; the Indian subcontinent and islands of the Indian Ocean rifted further, drifting northeastwards, with the Indian subcontinent colliding with the Eurasian plate nearly 55 million years ago, towards the end of Palaeocene. This collision created the Himalayas, including the Hindu Kush; the Hindu Kush range is still rising. It is prone to earthquakes; the origins of the name Hindu Kush are uncertain, with various theories being propounded by different scholars and writers. According to Hobson-Jobson, the name might be a possible corruption of Indicus Caucasus, with another explanation mentioned first by Ibn Batuta remaining popular despite doubts upon it, the modification of the name by some writers into Hindu Koh is factitious and throws no light on the name's origin.
In the time of Alexander the Great, the Hindu Kush range was referred to as the Caucasus Indicus or the "Caucasus of the Indus River", in the time of Islam in India, the regular invasions derived Hind Kash as Hindu Kush Hindū Kūh and Kūh-e Hind applied to the entire range separating the basins of the Kabul and Helmand Rivers from that of the Amu Darya, or, more to that part of the range lying northwest of Kabul. Sanskrit documents refer to the Hindu Kush as Hind kshetra in short Hind Kash as frontier lands of India. "Kash as in Kashmir" word synonym of frontier part of a "Kusha" grass. Hind Kash all around from Amu Darya to Kashmir was Kshetra for meditation and teaching by founders of Hinduism; the mountain range was called "Paropamisadae" by Hellenic Greeks in the late first millennium BC. The word Koh or Kuh means "mountain" in Khowar. According to Nigel Allan, Hindu Kush meant both "mountains of India" and "sparkling snows of India", as he notes, from a Central Asian perspective. A Persian-English dictionary indicates that the suffix'koš' is the present stem of the verb "to kill".
According to Francis Joseph Steingass, the word and suffix "-kush" means "a male. A Practical Dictionary of the Persian Language gives the meaning of the word kush as "hotbed". According to one interpretation, the name Hindu Kush means "kills the Hindu" or "Hindu killer" and is a reminder of the days when slaves from the Indian subcontinent died in the harsh weather typical of the Afghan mountains while being taken to Central Asia; the World Book Encyclopedia states that the word kush means death, was given to the mountains because of their dangerous passes. In his travel memoirs about India, the 14th century Moroccan traveller Muhammad Ibn Battuta mentioned crossing into India via the mountain passes of the Hindu Kush. In his Rihla, he mentions the history of the range in slave trading. Alexander von Humboldt stated that it can be learned from his work that the name only referred to a single mountain pass upon which many Indian slaves died of the cold weather. Battuta wrote, After this I proceeded to the city of Barwan, in the road to, a high mountain, covered with snow and exceedingly cold.
The name Hindu Kush is young, states Ervin Grötzbach, it is "missing from the accounts of the early Arab geographers and occurs for the first time in Ibn Baṭṭuṭa". Ibn Baṭṭuṭa, states Grötzbach, saw the "origin of the name Hindu Kush in the fact that numerous Hindu slaves died crossing the pass on their way from India to Turkestan". In contrast, state Fosco Maraini and Nigel Allan, the earliest known usage occurs on a map published about 1000 CE. According to Allan, the term Hindu Kush has been seen to mean "Hindu killer", but two other meaning
American Alpine Journal
The American Alpine Journal is an annual magazine published by the American Alpine Club. Its mission is "to document and communicate mountain exploration." The headquarters is in Colorado. Subtitled as a compilation of "The World's Most Significant Climbs," the magazine contains feature stories about notable new routes and ascents, written by the climbers, as well as a large "Climbs and Expeditions" section containing short notes by climbers about new and noteworthy achievements; some general articles about mountaineering, mountain medicine, the mountain environment, or other topics are sometimes included. Each issue includes book reviews, memorials of deceased members, club activities; the journal was established in 1929. In 1957 and 1958, the editor was Francis P. Farquhar. From 1960 to 1995, the editor was H. Adams Carter, who brought the journal to international pre-eminence. From 1996 to 2001, the editor was Christian Beckwith. Since 2002, the editor has been John Harlin III; the overall format of the journal has changed little since at least the 1970s, but current plans include more complete worldwide coverage and electronic/online access.
Other journals of record for climbing include the Alpine Journal published by the UK Alpine Club, the Canadian Alpine Journal published by the Alpine Club of Canada, the Himalayan Journal, Iwa To Yuki, a Japanese magazine. All of these magazines are used by climbers planning expeditions those who wish to verify that a proposed route would be a new one. Entries in these journals concerning major Himalayan peaks are indexed in the Himalayan Index. In March 2007, the American Alpine Journal inaugurated free, searchable online access for its issues dating back to 1966. All earlier issues will be added. A complete index is available for free download. A complete set of the journal on DVD may be available for purchase. National Geographic Adventure Outside Official website Searchable online access Himalayan Index
A mountain range or hill range is a series of mountains or hills ranged in a line and connected by high ground. A mountain system or mountain belt is a group of mountain ranges with similarity in form and alignment that have arisen from the same cause an orogeny. Mountain ranges are formed by a variety of geological processes, but most of the significant ones on Earth are the result of plate tectonics. Mountain ranges are found on many planetary mass objects in the Solar System and are a feature of most terrestrial planets. Mountain ranges are segmented by highlands or mountain passes and valleys. Individual mountains within the same mountain range do not have the same geologic structure or petrology, they may be a mix of different orogenic expressions and terranes, for example thrust sheets, uplifted blocks, fold mountains, volcanic landforms resulting in a variety of rock types. Most geologically young mountain ranges on the Earth's land surface are associated with either the Pacific Ring of Fire or the Alpide Belt.
The Pacific Ring of Fire includes the Andes of South America, extends through the North American Cordillera along the Pacific Coast, the Aleutian Range, on through Kamchatka, Taiwan, the Philippines, Papua New Guinea, to New Zealand. The Andes is 7,000 kilometres long and is considered the world's longest mountain system; the Alpide belt includes Indonesia and Southeast Asia, through the Himalaya, Caucasus Mountains, Balkan Mountains fold mountain range, the Alps, ends in the Spanish mountains and the Atlas Mountains. The belt includes other European and Asian mountain ranges; the Himalayas contain the highest mountains in the world, including Mount Everest, 8,848 metres high and traverses the border between China and Nepal. Mountain ranges outside these two systems include the Arctic Cordillera, the Urals, the Appalachians, the Scandinavian Mountains, the Great Dividing Range, the Altai Mountains and the Hijaz Mountains. If the definition of a mountain range is stretched to include underwater mountains the Ocean Ridges form the longest continuous mountain system on Earth, with a length of 65,000 kilometres.
The mountain systems of the earth are characterized by a tree structure, where mountain ranges can contain sub-ranges. The sub-range relationship is expressed as a parent-child relationship. For example, the White Mountains of New Hampshire and the Blue Ridge Mountains are sub-ranges of the Appalachian Mountains. Equivalently, the Appalachians are the parent of the White Mountains and Blue Ridge Mountains, the White Mountains and the Blue Ridge Mountains are children of the Appalachians; the parent-child expression extends to the sub-ranges themselves: the Sandwich Range and the Presidential Range are children of the White Mountains, while the Presidential Range is parent to the Northern Presidential Range and Southern Presidential Range. The position of mountains influences climate, such as snow; when air masses move up and over mountains, the air cools producing orographic precipitation. As the air descends on the leeward side, it warms again and is drier, having been stripped of much of its moisture.
A rain shadow will affect the leeward side of a range. Mountain ranges are subjected to erosional forces which work to tear them down; the basins adjacent to an eroding mountain range are filled with sediments which are buried and turned into sedimentary rock. Erosion is at work while the mountains are being uplifted until the mountains are reduced to low hills and plains; the early Cenozoic uplift of the Rocky Mountains of Colorado provides an example. As the uplift was occurring some 10,000 feet of Mesozoic sedimentary strata were removed by erosion over the core of the mountain range and spread as sand and clays across the Great Plains to the east; this mass of rock was removed as the range was undergoing uplift. The removal of such a mass from the core of the range most caused further uplift as the region adjusted isostatically in response to the removed weight. Rivers are traditionally believed to be the principal cause of mountain range erosion, by cutting into bedrock and transporting sediment.
Computer simulation has shown that as mountain belts change from tectonically active to inactive, the rate of erosion drops because there are fewer abrasive particles in the water and fewer landslides. Mountains on other planets and natural satellites of the Solar System are isolated and formed by processes such as impacts, though there are examples of mountain ranges somewhat similar to those on Earth. Saturn's moon Titan and Pluto, in particular exhibit large mountain ranges in chains composed of ices rather than rock. Examples include the Mithrim Montes and Doom Mons on Titan, Tenzing Montes and Hillary Montes on Pluto; some terrestrial planets other than Earth exhibit rocky mountain ranges, such as Maxwell Montes on Venus taller than any on Earth and Tartarus Montes on Mars, Jupiter's moon Io has mountain ranges formed from tectonic processes including Boösaule Montes, Dorian Montes, Hi'iaka Montes and Euboea Montes. Peakbagger Ranges Home Page Bivouac.com