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Warwan Valley
The Warwan Valley is a Himalayan sub-valley and a tehsil in Kishtwar District in the Jammu division in union territory of Jammu and Kashmir in India. The Valley lies northeast of Kishtwar and from Srinagar, the summer capital of Jammu and Kashmir. It falls under the jurisdiction of Kishtwar district in Marwah sub-Division of Jammu and Kashmir. Geology The Warwan Valley is drained by the Warwan River. It is a river formed by the confluence of the Batkot and Gumbar streams. The river is called Marusudar in the lower reaches of the valley and is the biggest right tributary of the Chenab River which in turn is a tributary of the Indus River system. A geological mapping survey has revealed that the Warwan Valley has experienced three distinct phases of folding in polyphase deformation. Geography The Warwan is a Himalayan valley situated at an altitude of above sea level. It is bordered by main Kashmir Valley in the north and Ladakh in the east. Its parent dist ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
States And Union Territories Of India
India is a federal union comprising 28 states and 8 union territories, with a total of 36 entities. The states and union territories are further subdivided into districts and smaller administrative divisions. History Pre-independence The Indian subcontinent has been ruled by many different ethnic groups throughout its history, each instituting their own policies of administrative division in the region. The British Raj mostly retained the administrative structure of the preceding Mughal Empire. India was divided into provinces (also called Presidencies), directly governed by the British, and princely states, which were nominally controlled by a local prince or raja loyal to the British Empire, which held ''de facto'' sovereignty ( suzerainty) over the princely states. 1947–1950 Between 1947 and 1950 the territories of the princely states were politically integrated into the Indian union. Most were merged into existing provinces; others were organised into ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kishtwar
Kishtwar is a town, municipality and administrative headquarter of the Kishtwar District in the Indian union territory of Jammu and Kashmir. The district was carved out of the Doda district in 2007. It is located in the Jammu division. The town of Kishtwar is situated at a distance of from the winter capital of Jammu. A large ground locally called as Chowgan is located in the heart of the town. Kishtwar is bordered by the Anantnag and Doda districts in the west and northwest, by the Chamba district of Himachal Pradesh in the south and the Kargil district of Ladakh in the east and northeast. In 2013 the municipality was the location the Kishtwar Riots, which claimed three lives and injured 80 more, and was a conflict between Muslim and Hindu communities that occurred in the aftermath of the Eid festival on 9 August 2013 at Kishtwar, Jammu and Kashmir. Demographics As of the 2011 Indian census, Kishtwar had a population of 14,865. Males constitute 63% of the popula ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Margan Formation
{{geodis ...
Margan ( fa, مرگن or مارگان or مرگان, link=no) may refer to: * Margan, Fars (مارگان - ''Mārgān'') * Margan, Sistan and Baluchestan (مارگان - ''Mārgān'') * Margan-e Azizabad (مرگن - ''Margan''), West Azerbaijan Province * Margan-e Esmail Kandi (مرگن - ''Margan''), West Azerbaijan Province * Margan-e Qadim (مرگن - ''Margan''), West Azerbaijan Province * Margan-e Vasat (مرگن - ''Margan''), West Azerbaijan Province * Margan (مرگن - ''Margan''), alternate name of Maraghan, West Azerbaijan Province * Margan Rural District (مارگان - ''Mārgān''), in Sistan and Baluchestan Province * Margan Top, a mountain pass in Kashmir Valley The Kashmir Valley, also known as the ''Vale of Kashmir'', is an intermontane valley concentrated in the Kashmir Division of the Indian- union territory of Jammu and Kashmir. The valley is bounded on the southwest by the Pir Panjal Range and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lolab Formation
The Lolab Valley is a Himalayan valley located in union territory of Jammu and Kashmir, India. The entrance to the valley lies east of Kupwara, and the centre of the valley lies northwest of Srinagar, the capital of Jammu and Kashmir. LOLAB is known as Land of Love and Beauty. It is an oval-shaped valley long with an average width of . Valley is at an altitude of 1,590 metres (5,215 ft) above the Sea level. An under-construction road from Bandipora to Lolab via Anderbugh Nagmarg Meadows will short cut the distance from Srinagar-to-Lolab by 50 kilometers. In Lolab Valley, there are a few tourist huts and many camping sites. It has the potential to become one of the best tourist destinations in Kashmir. Geography The Lolab Valley is situated within the jurisdiction of Sogam Lolab, a block of Kupwara. Lolab is Sub-District of Kupwara. It is bordered by the Kashmir Valley to the south and the Neelum River to the north, and is separated by Nagmarg meadows from Bandipore to t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jurassic
The Jurassic ( ) is a Geological period, geologic period and System (stratigraphy), stratigraphic system that spanned from the end of the Triassic Period million years ago (Mya) to the beginning of the Cretaceous Period, approximately Mya. The Jurassic constitutes the middle period of the Mesozoic, Mesozoic Era and is named after the Jura Mountains, where limestone strata from the period were first identified. The start of the Jurassic was marked by the major Triassic–Jurassic extinction event, associated with the eruption of the Central Atlantic magmatic province, Central Atlantic Magmatic Province. The beginning of the Toarcian Stage started around 183 million years ago and is marked by an extinction event associated with widespread Anoxic event, oceanic anoxia, ocean acidification, and elevated temperatures likely caused by the eruption of the Karoo-Ferrar, Karoo-Ferrar large igneous provinces. The end of the Jurassic, however, has no clear boundary with the Cretaceous and i ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Triassic
The Triassic ( ) is a geologic period and system which spans 50.6 million years from the end of the Permian Period 251.902 million years ago ( Mya), to the beginning of the Jurassic Period 201.36 Mya. The Triassic is the first and shortest period of the Mesozoic Era. Both the start and end of the period are marked by major extinction events. The Triassic Period is subdivided into three epochs: Early Triassic, Middle Triassic and Late Triassic. The Triassic began in the wake of the Permian–Triassic extinction event, which left the Earth's biosphere impoverished; it was well into the middle of the Triassic before life recovered its former diversity. Three categories of organisms can be distinguished in the Triassic record: survivors from the extinction event, new groups that flourished briefly, and other new groups that went on to dominate the Mesozoic Era. Reptiles, especially archosaurs, were the chief terrestrial vertebrates during this time. A specialized subgroup of archo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleozoic
The Paleozoic (or Palaeozoic) Era is the earliest of three geologic eras of the Phanerozoic Eon. The name ''Paleozoic'' ( ;) was coined by the British geologist Adam Sedgwick in 1838 by combining the Greek words ''palaiós'' (, "old") and ''zōḗ'' (), "life", meaning "ancient life" ). It is the longest of the Phanerozoic eras, lasting from , and is subdivided into six geologic periods (from oldest to youngest): # Cambrian # Ordovician # Silurian # Devonian # Carboniferous # Permian The Paleozoic comes after the Neoproterozoic Era of the Proterozoic Eon and is followed by the Mesozoic Era. The Paleozoic was a time of dramatic geological, climatic, and evolutionary change. The Cambrian witnessed the most rapid and widespread diversification of life in Earth's history, known as the Cambrian explosion, in which most modern phyla first appeared. Arthropods, molluscs, fish, amphibians, reptiles, and synapsids all evolved during the Paleozoic. Life began in the ocean ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Proterozoic
The Proterozoic () is a geological eon spanning the time interval from 2500 to 538.8million years ago. It is the most recent part of the Precambrian "supereon". It is also the longest eon of the Earth's geologic time scale, and it is subdivided into three geologic eras (from oldest to youngest): the Paleoproterozoic, Mesoproterozoic, and Neoproterozoic. The Proterozoic covers the time from the appearance of oxygen in Earth's atmosphere to just before the proliferation of complex life (such as trilobites or corals) on the Earth. The name ''Proterozoic'' combines two forms of ultimately Greek origin: meaning 'former, earlier', and , 'of life'. The well-identified events of this eon were the transition to an oxygenated atmosphere during the Paleoproterozoic; the evolution of eukaryotes; several glaciations, which produced the hypothesized Snowball Earth during the Cryogenian Period in the late Neoproterozoic Era; and the Ediacaran Period (635 to 538.8 Ma) which is characterize ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Indus River
The Indus ( ) is a transboundary river of Asia and a trans-Himalayan river of South and Central Asia. The river rises in mountain springs northeast of Mount Kailash in Western Tibet, flows northwest through the disputed region of Kashmir, Quote: "Kashmir, region of the northwestern Indian subcontinent. It is bounded by the Uygur Autonomous Region of Xinjiang to the northeast and the Tibet Autonomous Region to the east (both parts of China), by the Indian states of Himachal Pradesh and Punjab to the south, by Pakistan to the west, and by Afghanistan to the northwest. The northern and western portions are administered by Pakistan and comprise three areas: Azad Kashmir, Gilgit, and Baltistan, ... The southern and southeastern portions constitute the Indian state of Jammu and Kashmir. The Indian- and Pakistani-administered portions are divided by a "line of control" agreed to in 1972, although neither country recognizes it as an international boundary. In addition, China became ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
