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Gangotri Glacier
Gangotri glacier (Sanskrit and ) is located in Uttarkashi District, Uttarakhand, India in a region bordering Tibet. This glacier, one of the primary sources of the Ganges, has a volume of over 27 cubic kilometers. The glacier is about long and wide. Around the glacier are the peaks of the Gangotri Group, including several peaks notable for extremely challenging climbing routes, such as Shivling, Thalay Sagar, Meru, and Bhagirathi III. It flows roughly northwest, originating in a cirque below Chaukhamba, the highest peak of the group. The terminus of the Gangotri Glacier is said to resemble a cow's mouth, and the place is called Gomukh or Gaumukh (''gou'', cow + ''mukh'', face). Gomukh, which is about from the town of Gangotri, is the precise source of the Bhagirathi river, an important tributary of the Ganges. Gomukh is situated near the base of Shivling; in between lies the Tapovan meadow. The Gangotri glacier is a traditional Hindu pilgrimage site. Devout Hindus c ...
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Gomukh
Gomukh, also known as "Gaumukh" or "Gomukhi" (Hindi: गौमुख or गौमुखी ; Assamese and Bengali: গোমুখ or গোমুখী), is the terminus or snout of the Gangotri Glacier and the source of the Bhagirathi River, one of the primary headstreams of the Ganga River. The word ''Gomukh/Gaumukh'' (''go/gau''=cow, ''mukh''= mouth) literally means "Mouth of a Cow." The place is situated at a height of 13,200 ft (4,023 m) in the Uttarkashi district in the state of Uttarakhand, India. It is one of the largest glaciers in the Himalayas with an estimated volume of over 27 cubic kilometers. It is a Hindu holy pilgrimage site, visited by many who visit Gangotri. It is around 20 km away from Gangotri and can be reached by trekking. First Visit to Gomukh Gomukh is mentioned in the Puranas. It is said there that, searching a lost sheep, a boy reached near a glacier in Gangotri, the snout of which exactly looked like the face of a cow, and thus it g ...
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Ganges River
The Ganges ( ; in India: Ganga, ; in Bangladesh: Padma, ). "The Ganges Basin, known in India as the Ganga and in Bangladesh as the Padma, is an international which goes through India, Bangladesh, Nepal and China." is a trans-boundary river of Asia which flows through India and Bangladesh. The river rises in the western Himalayas in the States and union territories of India, Indian state of Uttarakhand. It flows south and east through the Gangetic Plain, Gangetic plain of North India, receiving the right-bank tributary, the Yamuna, which also rises in the western Indian Himalayas, and several left-bank tributaries from Nepal that account for the bulk of its flow. In West Bengal state, India, a feeder canal taking off from its right bank diverts 50% of its flow southwards, artificially connecting it to the Hooghly River. The Ganges continues into Bangladesh, its name changing to the Padma River, Padma. It is then joined by the Jamuna River (Bangladesh), Jamuna, the lower str ...
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Gangotri Glacier, Retreat From 1780 To 2001
Gangotri is a town and a ''Nagar Panchayat'' (municipality) in Uttarkashi district in the state of Uttarakhand, India. It is 99 km from Uttarkashi, the main district headquarter. It is a Hindu pilgrim town on the banks of the river Bhagirathi – the origin of the river Ganges. The town is located on the Greater Himalayan Range, at a height of . According to a popular Hindu legend, the goddess Ganga descended here when Shiva released the mighty river from the locks of his hair. Significance Ganga River Gangotri is one of the four sites in the Chota Char Dham pilgrimage circuit. It is also the origin of the Ganges river and, per Hinduism, the seat of the goddess Ganga. The source of the Ganges river is the Bhagirathi River, originating from the Gangotri Glacier. Once the river confluences with the Alakananda River at a town called Devprayag it finally acquires the name ''Ganga''. Near the river is a stone where King Bhagiratha performed penance to Shiva in order ...
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Supraglacial Lake
A supraglacial lake is any pond of liquid water on the top of a glacier. Although these pools are ephemeral, they may reach kilometers in diameter and be several meters deep. They may last for months or even decades at a time, but can empty in the course of hours. Lifetime Lakes may be created by surface melting during summer months, or over the period of years by rainfall, such as monsoons. They may dissipate by overflowing their banks, or creating a moulin. Effects on ice masses Lakes of a diameter greater than ~300 m are capable of driving a fluid-filled crevasse to the glacier/bed interface, through the process of hydrofracture. A surface-to-bed connection made in this way is referred to as a moulin. When these crevasses form, it can take a mere 2–18 hours to empty a lake, supplying warm water to the base of the glacier - lubricating the bed and causing the glacier to surge. The rate of emptying such a lake is equivalent to the rate of flow of the Niagara Fal ...
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Snow-bridge
A snow bridge is an arc formed by snow across a crevasse, a crack in rock, a creek, or some other opening in terrain. It is typically formed by snow drift, which first creates a cornice, which may then grow to reach the other side of the opening. Dangers A snow bridge may completely cover the opening and thus present a danger by creating an illusion of unbroken surface under which the opening is concealed by an unknown thickness of snow, possibly only a few centimetres. Snow bridges may also form inside a crevasse, making it appear shallow. A snow bridge is thicker and stronger at the edge of a crevasse; therefore, a fall through a bridge usually happens at some distance from the edge.''Mountain Operations'' (September 1947) United States War Department Field Manual FM-10,p. 204/ref> See also *Ice bridge An ice bridge is a frozen natural structure formed over seas, bays, rivers or lake surfaces. They facilitate migration of animals or people over a water body that was ...
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Avalanche
An avalanche is a rapid flow of snow down a Grade (slope), slope, such as a hill or mountain. Avalanches can be triggered spontaneously, by factors such as increased precipitation or snowpack weakening, or by external means such as humans, other animals, and earthquakes. Primarily composed of flowing snow and air, large avalanches have the capability to capture and move ice, rocks, and trees. Avalanches occur in two general forms, or combinations thereof: slab avalanches made of tightly packed snow, triggered by a collapse of an underlying weak snow layer, and loose snow avalanches made of looser snow. After being set off, avalanches usually accelerate rapidly and grow in mass and volume as they capture more snow. If an avalanche moves fast enough, some of the snow may mix with the air, forming a powder snow avalanche. Though they appear to share similarities, avalanches are distinct from slush flows, Mudflow, mudslides, Landslide#Debris landslide, rock slides, and serac collap ...
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Himalaya
The Himalayas, or Himalaya ( ), is a mountain range in Asia, separating the plains of the Indian subcontinent from the Tibetan Plateau. The range has some of the Earth's highest peaks, including the highest, Mount Everest. More than 100 peaks exceeding elevations of above sea level lie in the Himalayas. The Himalayas abut on or cross territories of six countries: Nepal, China, Pakistan, Bhutan, India and Afghanistan. The sovereignty of the range in the Kashmir region is disputed among India, Pakistan, and China. The Himalayan range is bordered on the northwest by the Karakoram and Hindu Kush ranges, on the north by the Tibetan Plateau, and on the south by the Indo-Gangetic Plain. Some of the world's major rivers, the Indus, the Ganges, and the Tsangpo– Brahmaputra, rise in the vicinity of the Himalayas, and their combined drainage basin is home to some 600 million people; 53 million people live in the Himalayas. The Himalayas have profoundly shaped the cultures of ...
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Gaumukh Gangotri Glacier
Gomukh, also known as "Gaumukh" or "Gomukhi" (Hindi: गौमुख or गौमुखी ; Assamese language, Assamese and Bengali language, Bengali: গোমুখ or গোমুখী), is the Glacier terminus, terminus or snout of the Gangotri Glacier and the source of the Bhagirathi River, one of the primary headstreams of the Ganga River. The word ''Gomukh/Gaumukh'' (''go/gau''=cow, ''mukh''= mouth) literally means "Mouth of a Cow." The place is situated at a height of 13,200 ft (4,023 m) in the Uttarkashi district in the state of Uttarakhand, India. It is one of the largest glaciers in the Himalayas with an estimated volume of over 27 cubic kilometers. It is a Hindu holy pilgrimage site, visited by many who visit Gangotri. It is around 20 km away from Gangotri and can be reached by trekking. First Visit to Gomukh Gomukh is mentioned in the Puranas. It is said there that, searching a lost sheep, a boy reached near a glacier in Gangotri, the snout of which ex ...
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Gaumukh (gangotri Glaciar) May 28 2007
Gomukh, also known as "Gaumukh" or "Gomukhi" (Hindi: गौमुख or गौमुखी ; Assamese and Bengali: গোমুখ or গোমুখী), is the terminus or snout of the Gangotri Glacier and the source of the Bhagirathi River, one of the primary headstreams of the Ganga River. The word ''Gomukh/Gaumukh'' (''go/gau''=cow, ''mukh''= mouth) literally means "Mouth of a Cow." The place is situated at a height of 13,200 ft (4,023 m) in the Uttarkashi district in the state of Uttarakhand, India. It is one of the largest glaciers in the Himalayas with an estimated volume of over 27 cubic kilometers. It is a Hindu holy pilgrimage site, visited by many who visit Gangotri. It is around 20 km away from Gangotri and can be reached by trekking. First Visit to Gomukh Gomukh is mentioned in the Puranas. It is said there that, searching a lost sheep, a boy reached near a glacier in Gangotri, the snout of which exactly looked like the face of a cow, and thus it got ...
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2013 North Indian Floods
In June 2013, a mid-day cloudburst centered on the North Indian state of Uttarakhand caused devastating floods and landslides, becoming the country's worst natural disaster since the 2004 tsunami. The rainfall received that month was far greater than the rainfall the state usually received. Debris blocked the rivers, causing major overflow. The main day of the flood was 16 June 2013. Some parts of Himachal Pradesh, Haryana, Delhi and Uttar Pradesh in India experienced the heavy rainfall, as well as regions of Western Nepal and some parts of Western Tibet. Over 89% of the casualties occurred in Uttarakhand. , according to figures provided by the Government of Uttarakhand, more than 5,700 people were "presumed dead." This total included 934 local residents. The death toll was later placed at 6,054. Destruction of bridges and roads left about 300,000 pilgrims and tourists trapped in the valleys leading to three of the four Hindu Chota Char Dham pilgrimage sites. The Indian Air F ...
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