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Suraj Tal
Suraj Tal, also called Tso Kamtsi or Surya Tal, is an long lake that lies just below the high Bara-lacha-la pass in Lahaul and Spiti district of the Indian state of Himachal Pradesh. It is the third highest lake in India, and the 21st-highest in the world. Suraj Tal Lake is just below the source of the Bhaga River that joins the Chandra River downstream at Tandi to form the Chandrabhaga River in Himachal Pradesh. The Chandrabhaga River is known as the Chenab as it enters the Jammu region of Jammu and Kashmir. The other major tributary of the Chandrabhaga, the Chandra originates and flows south-east of the Bara-lacha La. Access Suraj Tal is from Keylong, the district headquarters of the Lahaul Spiti district. It is approachable by National Highway NH 21, also known as the Leh-Manali Highway. The road skirts Suraj Tal which is just short of the Bara-lacha-la pass. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lahaul And Spiti District
The Lahaul and Spiti district in the Indian state of Himachal Pradesh consists of the two formerly separate districts of Lahaul () and Spiti (; or ). The present administrative centre is Kyelang in Lahaul. Before the two districts were merged, Kardang was the capital of Lahaul, and Dhankar the capital of Spiti. The district was formed in 1960, and is the fourth least populous district in India (out of 640). It is the least densely populated district of India, according to the Census of India 2011. Geography Geologically located on the Tibetan Plateau, Lahaul and Spiti district is connected to Manali through the Rohtang Pass. ''Kunzum la'' or the Kunzum Pass (altitude ) is the entrance pass to the Spiti Valley from Lahaul. It is from Chandra Tal. To the south, Spiti ends from Tabo, at the Sumdo where the road enters Kinnaur and joins National Highway 5. Spiti is barren and difficult to cross, with an average elevation of the valley floor of . It is surrounded by lofty ran ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ladakh
Ladakh () is a region administered by India as a union territory which constitutes a part of the larger Kashmir region and has been the subject of dispute between India, Pakistan, and China since 1947. (subscription required) Quote: "Jammu and Kashmir, state of India, located in the northern part of the Indian subcontinent in the vicinity of the Karakoram and westernmost Himalayan mountain ranges. From 1947 to 2019, Ladakh was part of the Indian state of Jammu and Kashmir, which has been the subject of dispute between India, Pakistan, and China since the partition of the subcontinent in 1947." Quote: "Jammu and Kashmir: Territory in northwestern India, subject to a dispute between India and Pakistan. It has borders with Pakistan and China." Ladakh is bordered by the Tibet Autonomous Region to the east, the Indian state of Himachal Pradesh to the south, both the Indian-administered union territory of Jammu and Kashmir (union territory), Jammu and Kashmir and the Pakistan-administ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sacred Lakes Of India
Sacred describes something that is dedicated or set apart for the service or worship of a deity; is considered worthy of spiritual respect or devotion; or inspires awe or reverence among believers. The property is often ascribed to objects (a " sacred artifact" that is venerated and blessed), or places (" sacred ground"). French sociologist Émile Durkheim considered the dichotomy between the sacred and the profane to be the central characteristic of religion: "religion is a unified system of beliefs and practices relative to ''sacred things'', that is to say, things set apart and forbidden." Durkheim, Émile. 1915. ''The Elementary Forms of the Religious Life''. London: George Allen & Unwin. . In Durkheim's theory, the sacred represents the interests of the group, especially unity, which are embodied in sacred group symbols, or using team work to help get out of trouble. The profane, on the other hand, involve mundane individual concerns. Etymology The word ''sacred'' desce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tourist Attractions In Himachal Pradesh
Tourism is travel for pleasure or business; also the theory and practice of touring (other), touring, the business of attracting, accommodating, and entertaining tourists, and the business of operating tour (other), tours. The World Tourism Organization defines tourism more generally, in terms which go "beyond the common perception of tourism as being limited to holiday activity only", as people "travelling to and staying in places outside their usual environment for not more than one consecutive year for leisure and not less than 24 hours, business and other purposes". Tourism can be Domestic tourism, domestic (within the traveller's own country) or International tourism, international, and international tourism has both incoming and outgoing implications on a country's balance of payments. Tourism numbers declined as a result of a strong economic slowdown (the late-2000s recession) between the second half of 2008 and the end of 2009, and in consequence of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lakes Of Himachal Pradesh
Reservoirs *Maharana Pratap Sagar *Pandoh Lake *Gobind Sagar *Chamera Dam Low Altitude Lakes *Renuka Lake *Macchial Lake Mid Altitude Lakes *Dal Lake (HP), Dal Lake District kangra *Khajjiar, Khajjiar Lake District Chamba *Kumarwah Lake District Mandi *Rewalsar Lake, Rewalsar Lake District mandi High Altitude Lakes *Prashar Lake (2730m)- Mandi district *Dehnasar Lake (4280m) -Kangra district *Nako Lake (3662m) - Kinnaur district *Chandra Tal (4300m) -Lahaul & Spiti district *Suraj Tal (4883m) -Lahaul & Spiti district *Dhankar Lake *Dashair (4270m) *Bhrighu Lake (4235m) - Kullu district *Manimahesh Lake (4080m) -Chamba district *Gadasru Lake (3470m) - Chamba district *Mahakali Lake (4080m) -Chamba district *Lama Dal (3960m) -Chamba district *Chander Naun (4260m) *Kareri Lake (2934m) -Kangra district *Nag Dal Lake (4150m) *Kamrunag lake (3334m) Mandi in district.mandi In the Shimla area lie the small rain water fed lakes of Tani Jubbar, Kunihar and Karwali that lie ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zingzingbar
Zingzingbar is a Border Roads Organization road-building camp and tea house way-station situated from Darcha on the Manali to Leh road in the Lahaul and Spiti district of Himachal Pradesh. It is situated at an altitude of around . The location has temporary shelters and dhaba A dhaba is a roadside restaurant in the Indian subcontinent, primarily across Pakistan and India. They are on highways, generally serve local cuisine, and also serve as truck stops. They are most commonly found next to petrol stations, and mos ...s that can be used by trekkers and tourists for accommodation. Zingzingbar is the proposed south portal of the Bara-lacha-la tunnel, situated approximately from Manali. The north portal of this tunnel is expected to be at Keylong Sarai. The tunnel will reduce the transit time on the avalanche and landslide prone route by up to 2 hrs. References Cities and towns in Lahaul and Spiti district {{HimachalPradesh-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Suraj Tal
Suraj Tal, also called Tso Kamtsi or Surya Tal, is an long lake that lies just below the high Bara-lacha-la pass in Lahaul and Spiti district of the Indian state of Himachal Pradesh. It is the third highest lake in India, and the 21st-highest in the world. Suraj Tal Lake is just below the source of the Bhaga River that joins the Chandra River downstream at Tandi to form the Chandrabhaga River in Himachal Pradesh. The Chandrabhaga River is known as the Chenab as it enters the Jammu region of Jammu and Kashmir. The other major tributary of the Chandrabhaga, the Chandra originates and flows south-east of the Bara-lacha La. Access Suraj Tal is from Keylong, the district headquarters of the Lahaul Spiti district. It is approachable by National Highway NH 21, also known as the Leh-Manali Highway. The road skirts Suraj Tal which is just short of the Bara-lacha-la pass. [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Continental Crust
Continental crust is the layer of igneous, sedimentary, and metamorphic rocks that forms the geological continents and the areas of shallow seabed close to their shores, known as continental shelves. This layer is sometimes called ''sial'' because its bulk composition is richer in aluminium silicates (Al-Si) and has a lower density compared to the oceanic crust, called ''sima'' which is richer in magnesium silicate (Mg-Si) minerals. Changes in seismic wave velocities have shown that at a certain depth (the Conrad discontinuity), there is a reasonably sharp contrast between the more felsic upper continental crust and the lower continental crust, which is more mafic in character. The continental crust consists of various layers, with a bulk composition that is intermediate (SiO2 wt% = 60.6). The average density of continental crust is about , less dense than the ultramafic material that makes up the mantle, which has a density of around . Continental crust is also less dense ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Basalt
Basalt (; ) is an aphanite, aphanitic (fine-grained) extrusive igneous rock formed from the rapid cooling of low-viscosity lava rich in magnesium and iron (mafic lava) exposed at or very near the planetary surface, surface of a terrestrial planet, rocky planet or natural satellite, moon. More than 90% of all volcanic rock on Earth is basalt. Rapid-cooling, fine-grained basalt is chemically equivalent to slow-cooling, coarse-grained gabbro. The eruption of basalt lava is observed by geologists at about 20 volcanoes per year. Basalt is also an important rock type on other planetary bodies in the Solar System. For example, the bulk of the plains of volcanism on Venus, Venus, which cover ~80% of the surface, are basaltic; the lunar mare, lunar maria are plains of flood-basaltic lava flows; and basalt is a common rock on the surface of Mars. Molten basalt lava has a low viscosity due to its relatively low silica content (between 45% and 52%), resulting in rapidly moving lava flo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geology
Geology () is a branch of natural science concerned with Earth and other astronomical objects, the features or rocks of which it is composed, and the processes by which they change over time. Modern geology significantly overlaps all other Earth sciences, including hydrology, and so is treated as one major aspect of integrated Earth system science and planetary science. Geology describes the structure of the Earth on and beneath its surface, and the processes that have shaped that structure. It also provides tools to determine the relative and absolute ages of rocks found in a given location, and also to describe the histories of those rocks. By combining these tools, geologists are able to chronicle the geological history of the Earth as a whole, and also to demonstrate the age of the Earth. Geology provides the primary evidence for plate tectonics, the evolutionary history of life, and the Earth's past climates. Geologists broadly study the properties and processes of E ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wind
Wind is the natural movement of air or other gases relative to a planet's surface. Winds occur on a range of scales, from thunderstorm flows lasting tens of minutes, to local breezes generated by heating of land surfaces and lasting a few hours, to global winds resulting from the difference in absorption of solar energy between the climate zones on Earth. The two main causes of large-scale atmospheric circulation are the differential heating between the equator and the poles, and the rotation of the planet (Coriolis effect). Within the tropics and subtropics, thermal low circulations over terrain and high plateaus can drive monsoon circulations. In coastal areas the sea breeze/land breeze cycle can define local winds; in areas that have variable terrain, mountain and valley breezes can prevail. Winds are commonly classified by their spatial scale, their speed and direction, the forces that cause them, the regions in which they occur, and their effect. Winds have various asp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precipitation (meteorology)
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called showers. Moisture that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condense ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
