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Dhauladhar Sanctuary
Dhauladhar ( hi, धौलाधार) () is a mountain range which is part of a lesser Himalayan chain of mountains. It rises from the Shivalik hills, to the north of Kangra and Mandi. Dharamsala, the headquarters of Kangra district and the winter capital of Himachal Pradesh, lies on its southern spur in the Kangra Valley.Dhaula Dhar '''', v. 11, ''p. 287.'' lies to the North of this range. Overview The Dhauladhar range is one of ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dhauladhar
Dhauladhar ( hi, धौलाधार) () is a mountain range which is part of a lesser Himalayan chain of mountains. It rises from the Shivalik hills, to the north of Kangra and Mandi. Dharamsala, the headquarters of Kangra district and the winter capital of Himachal Pradesh, lies on its southern spur in the Kangra Valley.Dhaula Dhar '''', v. 11, ''p. 287.'' lies to the North of this range. Overview The Dhauladhar range is one of the ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manali, Himachal Pradesh
Manali is a town, near Kullu town in Kullu district in the Indian state of Himachal Pradesh. It is situated in the northern end of the Kullu Valley, formed by the Beas River. The town is located in the Kullu district, approximately north of the state capital of Shimla and northeast of the national capital of New Delhi. With a population of 8,096 people recorded in the 2011 Indian census Manali is the beginning of an ancient trade route through Lahaul (H.P) and Ladakh, over the Karakoram Pass and onto Yarkand and Hotan in the Tarim Basin of China. Manali is a popular tourist destination in India and serves as the gateway to the Lahaul and Spiti district as well as the city of Leh in Ladakh.''Paper also Presented at the International Seminar on Disasters, Environment and Development, 9–12 December 1994, New Delhi, India'' –by History Manali is named after the Sanātanī lawgiver Manu (see Manusmriti). The name ''Manali'' is regarded as the derivative of ''Manu-Alaya'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Manimahesh Kailash Peak
The Manimahesh Kailash Peak, , also known as Chamba Kailash, which stands towering high over the Manimahesh Lake, is believed to be the abode of Lord Shiva, the (Hindu deity). It is located in the Bharmour subdivision of the Chamba district in the Indian state of Himachal Pradesh. The peak is from Bharmour in the Budhil valley. It is one of the major pilgrimage sites as well as a popular trekking destination in Himachal Pradesh. The Manimahesh Lake is at the base of the Kailash peak at and is also held in deep veneration by people of Himachal Pradesh, particularly the Gaddi tribe of the region. In the month of Bhadon, on the eighth day of the new moon period a fair is held in the precincts of the lake that attracts thousands of pilgrims. Manimahesh Kailash has not been successfully summitted by mountaineers and is thus remains a virgin peak. An attempt to climb the peak in 1968 by an Indo–Japanese team led by Nandini Patel was aborted. This failure is attributed to the divin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
McLeod Ganj
McLeod Ganj, also spelt McLeodganj, (pronounced ''Mc-loud-gunj'') is a suburb of Dharamshala in the Kangra district of Himachal Pradesh, India. It is known as "Little Lhasa" or "Dhasa" (a short form of Dharamshala used mainly by Tibetans) because of its large population of Tibetans. The Tibetan government-in-exile is headquartered in McLeod Ganj. Etymology McLeod Ganj was named after Sir Donald Friell McLeod, a Lieutenant Governor of Punjab; the suffix ''ganj'' is a common Persian word used for "neighbourhood".Dharamshala '''', v. 11, p. 301. History In March 1850, the area was annexed by th ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triund
Triund is a small hill station in the Kangra district in the state of Himachal Pradesh, India. Triund is a part of Dharamkot. Triund is at the foot of the Dhauladhar ranges and is at a height of . See also *List of hill stations in India *Dharamshala *McLeodGanj *Kangra district Kangra is the most populous district of the Indian state of Himachal Pradesh. Dharamshala is the administrative headquarters of the district. History Kangra is known for having the oldest serving Royal Dynasty in the world, the Katoch. In 1758 ... References Government website Other websites {{Kangra district Villages in Kangra district Hill stations in Himachal Pradesh Dharamshala ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gaddi People
The Gaddi is a semi-pastoral Indo-Aryan ethno-linguistic tribe living mainly in the Indian states of Himachal Pradesh and Jammu and Kashmir. Overview The origin of the Gaddi Tribe is Gaderiya ( Dhangar) they also additionally believe that their ancestors fled from plains because of lack of security or foreign Invasions. The fact regarding their origination lies within the popular myths in the state. There is no accord of the views from where Gaddis migrated to this hilly state. Bharmour is additionally known as the abode of Gaddis. Some views are commonly held among these folks like Kailash is the throne (gadi) of the Lord Shiva. Therefore, those people who took refuge and settled in Brahmaur also came to be referred as Gaddis. Gaddis are semi nomadic, semi-agricultural and a semi-pastoral tribe. They have a defined culture, expressed through language, dress, food, marriage, song, and devout celebrations. Gaddis have their empyreal history deep- rooted in their endemic c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Limestone
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 limes ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slate
Slate is a fine-grained, foliated, homogeneous metamorphic rock derived from an original shale-type sedimentary rock composed of clay or volcanic ash through low-grade regional metamorphism. It is the finest grained foliated metamorphic rock. Foliation may not correspond to the original sedimentary layering, but instead is in planes perpendicular to the direction of metamorphic compression. The foliation in slate is called "slaty cleavage". It is caused by strong compression causing fine grained clay flakes to regrow in planes perpendicular to the compression. When expertly "cut" by striking parallel to the foliation, with a specialized tool in the quarry, many slates will display a property called fissility, forming smooth flat sheets of stone which have long been used for roofing, floor tiles, and other purposes. Slate is frequently grey in color, especially when seen, en masse, covering roofs. However, slate occurs in a variety of colors even from a single locality; for ex ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Granite
Granite () is a coarse-grained (phaneritic) intrusive igneous rock composed mostly of quartz, alkali feldspar, and plagioclase. It forms from magma with a high content of silica and alkali metal oxides that slowly cools and solidifies underground. It is common in the continental crust of Earth, where it is found in igneous intrusions. These range in size from dikes only a few centimeters across to batholiths exposed over hundreds of square kilometers. Granite is typical of a larger family of ''granitic rocks'', or ''granitoids'', that are composed mostly of coarse-grained quartz and feldspars in varying proportions. These rocks are classified by the relative percentages of quartz, alkali feldspar, and plagioclase (the QAPF classification), with true granite representing granitic rocks rich in quartz and alkali feldspar. Most granitic rocks also contain mica or amphibole minerals, though a few (known as leucogranites) contain almost no dark minerals. Granite is nearly alway ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dhauladhar Peak From McLeod Ganj
Dhauladhar ( hi, धौलाधार) () is a mountain range which is part of a lesser Himalayan chain of mountains. It rises from the Shivalik hills, to the north of Kangra and Mandi. Dharamsala, the headquarters of Kangra district and the winter capital of Himachal Pradesh, lies on its southern spur in the Kangra Valley.Dhaula Dhar '' The Imperial Gazetteer of India'', v. 11, ''p. 287.'' Chamba lies to the North of this range. Overview The Dhauladhar range is one of the ranges of the[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pir Panjal Range
The Pir Panjal Range (Kashmiri: ) is a group of mountains in the Lesser Himalayan region, running from east-southeast (ESE) to west-northwest (WNW) across the Indian territories of Himachal Pradesh and Jammu and Kashmir and then Pakistan's Azad Kashmir and Punjab. The average elevation varies from to . The Himalayas show a gradual elevation towards the Dhauladhar and Pir Panjal ranges. Pir Panjal is the largest range of the Lesser Himalayas. Near the bank of the Sutlej River, it dissociates itself from the Himalayas and forms a divide between the Beas and Ravi rivers on one side and the Chenab on the other. The renowned Galyat mountains are also located in this range. Etymology The Pir Panjal range is named after the Pir Panjal Pass, whose original name as recorded by Srivara, is ''Panchaladeva'' (IAST: ''Pāñcāladeva'', meaning the deity of ''Panchala''). Panchala is a country mentioned in the Mahabharata in the northwest Uttar Pradesh. However, there are also tradition ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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