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Hisper Glacier
Hispar Glacier ( ur, ) is a long glacier in the Karakoram Mountains of Gilgit–Baltistan, Pakistan which meets the long Biafo Glacier at the Hispar La (Pass) at an altitude of to create the world's longest glacial system outside of the polar regions. Details This highway of ice connects two ancient mountain kingdoms, Nagar in the west with Baltistan in the east. The extreme steepness of the hillsides and strenuous nature of the boulder hopping on the lateral moraines and hillsides make this route's upper half the most difficult part of the Biafo - Hispar traverse. Only the Hispar La day includes walking on the Hispar Glacier. The crossing of four major tributary glaciers from the north is most taxing, and potentially high nullah crossings can be dangerous. The views of peaks and of the snow-covered cliffs and mountains on the south side of the glacier are particularly impressive. Rivers The Hispar River, a tributary of the Hunza River, rises from the meltwater of th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hispar Muztagh
Hispar Muztagh is a sub-range of the Karakoram mountain range. It is located in the Nagar District of Gilgit-Baltistan, Pakistan, north of Hispar Glacier, south of Shimshal Valley, and east of the Hunza Valley. It is the second highest sub-range of the Karakoram, the highest being the Baltoro Muztagh. The highest mountain in the range is Distaghil Sar Disteghil Sar or Distaghil Sar ( ur, ) is the highest mountain in the Shimshal Valley, part of the Karakoram mountain range in Gilgit-Baltistan, Pakistan. It is the 19th-highest mountain on Earth and the 7th-highest in Pakistan. ''Disteghil ... (7,885m/25,869 ft). Selected peaks in the Hispar Muztagh Note # These are from thHimalayan Index which may not be completely accurate, as some climbs may not have been recorded in the climbing literature or indexed properly. Sources Jerzy Wala, ''Orographical Sketch Map of the Karakoram'', Swiss Foundation for Alpine Research, Zurich, 1990. External links Blankonthemap ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Baltistan
Baltistan ( ur, ; bft, སྦལ་ཏི་སྟཱན, script=Tibt), also known as Baltiyul or Little Tibet ( bft, སྦལ་ཏི་ཡུལ་།, script=Tibt), is a mountainous region in the Pakistani-administered territory of Gilgit–Baltistan. It is located near the Karakoram (south of K2) and borders Gilgit to the west, China's Xinjiang to the north, Indian-administered Ladakh to the southeast, and the Indian-administered Kashmir Valley to the southwest. The average altitude of the region is over . Baltistan is largely administered under the Baltistan Division. Prior to the partition of British India in 1947, Baltistan was part of the princely state of Jammu and Kashmir, having been conquered by Gulab Singh's armies in 1840. Baltistan and Ladakh were administered jointly under one ''wazarat'' (district) of the state. The region retained its identity in this setup as the Skardu ''tehsil'', with Kargil and Leh being the other two ''tehsils'' of the district. A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Glaciers
A glacier ( ) or () is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly deform and flow due to stresses induced by their weight, creating crevasses, seracs, and other distinguishing features. Because glacial mass is affected by long-term climate changes, e.g., precipitation, mean temperature, and cloud cover, glacial mass changes are considered among the most sensitive indicators of climate change. There are about 198,000 to 200,000 glaciers in the world. Glaciers by continent Africa Africa, specifically East Africa, has contained glacial regions, possibly as far back as the last glacier maximum 10 to 15 thousand years ago. Seasonal snow does exist on the highest peaks of East Africa as well as in the Drakensberg Range of South Africa, the Stormberg Mountains, and the Atlas Mountains in Morocco. Currently, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Highest Mountains
Currently, There are at least 108 mountains on Earth with elevations of or greater above sea level. The vast majority of these mountains are located on the edge of the Indian plate, Indian and Eurasian plate, Eurasian plates in China, India, Nepal and Pakistan. The dividing line between a mountain with multiple peaks and separate mountains is not always clear (see also Highest unclimbed mountain). A popular and intuitive way to distinguish mountains from subsidiary peaks is by their height above the highest saddle connecting it to a higher summit, a measure called topographic prominence or re-ascent (the higher summit is called the "parent peak"). A common definition of a mountain is a summit with prominence. Alternatively, a relative prominence (prominence/height) is used (usually 7–8%) to reflect that in higher mountain ranges everything is on a larger scale. The table below lists the highest 100 summits with at least prominence, approximating a 7% relative prominence ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
List Of Mountains In Pakistan
Pakistan is home to 108 peaks above 7,000 metres and 4555 above 6,000 m. There is no count of the peaks above 5,000 and 4,000 m. Five of the 14 highest independent peaks in the world (the eight-thousanders) are in Pakistan (four of which lie in the surroundings of Concordia; the confluence of Baltoro Glacier and Godwin Austen Glacier). Most of the highest peaks in Pakistan lie in the Karakoram mountain range (which lies almost entirely in the Gilgit–Baltistan region of Pakistan, and is considered to be a separate range from Himalayan range) but some peaks above 7,000 m are included in the Himalayan and Hindu Kush ranges. Moreover, Pakistan is home to over 7,000 glaciers, more than anywhere except the polar regions. Considerations The list is an incomplete list of mountains in Pakistan. There are many named and unnamed peaks in Pakistan that are currently not included in this list. The list also includes many peaks that are not usually classed as independent mountains, but i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Central Karakoram National Park
Central Karakoram National Park ( ur, ) is a national park located in Skardu district of Gilgit-Baltistan in Pakistan. It encompasses some of the world’s highest peaks and largest glaciers. Internationally renowned for mountaineering, rock climbing and trekking opportunities, it covers an area of about 10,000 sq. km and contains the greatest concentration of high mountains on earth. It has four peaks over 8,000 m including K2 (8611 m), Gasherbrum-I (8068 m), Gasherbrum-II (8035 m) and Broad Peak (8051 m), and sixty peaks higher than 7,000 m. The park was placed on the World Heritage Site Tentative List in 2016. Features The Central Karakoram National Park is the highest national park in the world and the largest protected area in Pakistan. It covers about in the Central Karakoram mountain range. It varies in altitude from above sea level to the summit of chogori K2, the world's second highest mountain at . There are three other ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hunza River
Hunza River ( ur, ) is the principal river of Hunza in Gilgit–Baltistan, Pakistan It is formed by the confluence of the Chapursan and Khunjerab ''nalas'' (gorges) which are fed by glaciers. It is joined by the Gilgit River and the Naltar River, before it flows into the Indus River. The river cuts through the Karakoram range, flowing from north to south. The Karakoram Highway (N-35) runs along the Hunza River valley, switching to the Khunjerab River valley at the point of confluence, eventually reaching the Khunjerab Pass at the border with China Xinjiang. The river is dammed for part of its route. The Attabad landslide disaster in January 2010 completely blocked the Hunza Valley. A new lake — now called the Attabad Lake or Gojal Lake — which extends 30 kilometers and rose to a depth of 400 feet, was formed as the Hunza River backed-up. Karakorum Area Development Organization (KADO), Aliabad The landslide completely covered sections of the Karakoram Highway. The Hunz ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hispar River
The Hispar River ( ur, ) forms from the melt water of the Hispar Glacier - a 49 kilometer-long glacier in the Karakoram mountains of Gilgit-Baltistan, Pakistan. The Hispar Glacier and river both flow northwest, passing through Hispar, Hopar and Nagar (Nagir) villages until the confluence with the Hunza River in the Hunza Valley. Road conditions are spectacular at best, treacherous at worst. In August 2006, a bridge below Hispar village was condemned, and the Hunza River washed the road away at the confluence, eliminating all vehicular access to the entire valley for some months. See also * Hispar The Hispar Valley or Hispar (Urdu.وادی ہسپر) is the last Valley of Nagar Valley in the Gilgit-Baltistan region of Pakistan. The valley is located two kilometers below the snout of the 49 kilometer-long Hispar Glacier. It is about 28 ... Rivers of Gilgit-Baltistan Indus basin Karakoram Rivers of Pakistan {{Pakistan-river-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Snow Lake Pakistan
Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
A Glacial Stream On Hispar Glacier, 49km
A, or a, is the first letter and the first vowel of the Latin alphabet, used in the modern English alphabet, the alphabets of other western European languages and others worldwide. Its name in English is ''a'' (pronounced ), plural ''aes''. It is similar in shape to the Ancient Greek letter alpha, from which it derives. The uppercase version consists of the two slanting sides of a triangle, crossed in the middle by a horizontal bar. The lowercase version can be written in two forms: the double-storey a and single-storey ɑ. The latter is commonly used in handwriting and fonts based on it, especially fonts intended to be read by children, and is also found in italic type. In English grammar, " a", and its variant " an", are indefinite articles. History The earliest certain ancestor of "A" is aleph (also written 'aleph), the first letter of the Phoenician alphabet, which consisted entirely of consonants (for that reason, it is also called an abjad to distinguish it fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nullah
A nullah or nala ( Hindustani or "nallah" in Punjabi) is an 'arm of the sea', stream, or watercourse, a steep narrow valley. Like the wadi of the Arabs, the nullah is characteristic of mountainous or hilly country where there is little rainfall. In the drier parts of India and Pakistan, and in many parts of Australia, there are small steep-sided valleys penetrating the hills, clothed with rough brushwood or small trees growing in the stony soil. During occasional heavy rains, torrents rush down the nullahs and quickly disappear. There is little local action upon the sides, while the bed is lowered, and consequently these valleys are narrow and steep. In cities on the Delhi plain in India, nullahs are concrete or brick-lined ditches about deep and wide, used to divert monsoon rain away from the cities. Encroachment into nullahs is a significant problem in many South Asian cities, since it hampers the drainage of stormwater and can exacerbate floods. Canal In East Asia, a n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Nagar (princely State)
Nagar ( ur, , ''Riyasat Nagar'') was a princely state, princely salute state in the northern part of Gilgit–Baltistan, Pakistan. Until August 1947, it was in a subsidiary alliance with British India. It bordered the states of the Gilgit Agency to the south and west, and the princely state of Hunza (princely state), District Hunza to the north and east. From November 1947 to 1974 it was a Princely states of Pakistan, princely state of Pakistan. The state capital was the town of Nagar. The territory previously covered by Nagar forms three tehsils of the Nagar District of Northern Pakistan. History Nagar, founded in the fourteenth century, was an autonomous principality until the United Kingdom, British gained control of the state following the Hunza–Nagar Campaign (1889-1893). It was a colonial princely states, princely state under the administration of the Gilgit Agency until 1947, but from 1868 it was a vassal of the Maharaja of Jammu and Kashmir (princely state), Jammu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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