Chitrakoot Falls
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Chitrakoot Falls
The Chitrakote Falls (also spelled Chitrakote, Chitrakot, and Chitrakoot) is a natural waterfall on the Indravati River, located approximately to the west of Jagdalpur, in Bastar district in the Indian state of Chhattisgarh. The height of the falls is about . It is the widest fall in India, reaching a width of nearly during the monsoon season. Because of its width and its widespread horseshoe shape during the monsoon season, it is often called the "Niagara Falls of India". Topography The Chitrakote Falls is located on the Indravati River. The river originates in the Kalahandi district of Odisha, in the Vindhya Range of hills, flows westward, and then forms a fall at Chitrakote, after which it finally flows into the Godavari River at Bhadrakali, after traversing in the state. The free drop of the falls is a sheer height of about . Because of its horseshoe shape, it is often compared with the world-famous Niagara Falls in the United States, and is given the sobriquet "the Sm ...
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Bastar District
Bastar is a district in the state of Chhattisgarh in Central India. Jagdalpur is the district headquarters. Bastar is bounded on the northwest by Narayanpur District, on the north by Kondagaon district, on the east by Nabarangpur and Koraput Districts of Odisha State, on the south and southwest by Dantewada and Sukma. The district possesses a unique blend of tribal and Odia culture. Bastar and Dantewada districts were formerly part of the princely state of Bastar. Bastar was founded in the early 14th century, by Annama Deva, the brother of Kakatiya King Pratapa Rudra Deva of Warangal in Telangana. After India achieved independence in 1947, the princely states of Bastar and Kanker acceded to the Government of India, and were merged to form Bastar district of Madhya Pradesh. The district, which had an area of , was one of the largest in India when formed. In 1999, the district was divided into the present-day districts of Bastar, Dantewada, and Kanker. In 2000, Bastar was one ...
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Parvati
Parvati ( sa, पार्वती, ), Uma ( sa, उमा, ) or Gauri ( sa, गौरी, ) is the Hindu goddess of power, energy, nourishment, harmony, love, beauty, devotion, and motherhood. She is a physical representation of Mahadevi in her complete form. She is also revered in her appearances as Durga and Kali.Suresh Chandra (1998), Encyclopedia of Hindu Gods and Goddesses, , pp 245–246 She is one of the central deities of the goddess-oriented sect called Shaktism, and the chief goddess in Shaivism. Along with Lakshmi and Saraswati, she forms the Tridevi. Parvati is the wife of the Hindu god Shiva. She is the reincarnation of Sati, the first wife of Shiva who immolated herself during a yajna (fire-sacrifice).Edward Balfour, , The Encyclopaedia of India and of Eastern and Southern Asia, pp 153 Parvati is the daughter of the mountain-king Himavan and queen Mena.H.V. Dehejia, Parvati: Goddess of Love, Mapin, , pp 11 Parvati is the mother of the Hindu deities Ganesha and ...
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International Union Of Geological Sciences
The International Union of Geological Sciences (IUGS) is an international non-governmental organization devoted to international cooperation in the field of geology. About The IUGS was founded in 1961 and is a Scientific Union member of the International Science Council (ISC), formerly the International Council for Science (ICSU), which it recognizes as the co-ordinating body for the international organization of science. Currently geologists from 121 countries (and regions) are represented in the IUGS. A broad range of scientific topics are covered by its commission, task groups, joint programmes and affiliated organizations. IUGS promotes and encourages the study of geological problems, especially those of worldwide significance, and supports and facilitates international and inter-disciplinary co-operation in the earth sciences. The Union's Secretariat is currently located at the Chinese Academy of Geological Sciences in Beijing, China. Activities IUGS is a joint partner with ...
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International Union For Conservation Of Nature
The International Union for Conservation of Nature (IUCN; officially International Union for Conservation of Nature and Natural Resources) is an international organization working in the field of nature conservation and sustainable use of natural resources. It is involved in data gathering and analysis, research, field projects, advocacy, and education. IUCN's mission is to "influence, encourage and assist societies throughout the world to conserve nature and to ensure that any use of natural resources is equitable and ecologically sustainable". Over the past decades, IUCN has widened its focus beyond conservation ecology and now incorporates issues related to sustainable development in its projects. IUCN does not itself aim to mobilize the public in support of nature conservation. It tries to influence the actions of governments, business and other stakeholders by providing information and advice and through building partnerships. The organization is best known to the wider pu ...
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United Nations Educational, Scientific And Cultural Organization
The United Nations Educational, Scientific and Cultural Organization is a specialized agency of the United Nations (UN) aimed at promoting world peace and security through international cooperation in education, arts, sciences and culture. It has 193 member states and 12 associate members, as well as partners in the non-governmental, intergovernmental and private sector. Headquartered at the World Heritage Centre in Paris, France, UNESCO has 53 regional field offices and 199 national commissions that facilitate its global mandate. UNESCO was founded in 1945 as the successor to the League of Nations's International Committee on Intellectual Cooperation.English summary). Its constitution establishes the agency's goals, governing structure, and operating framework. UNESCO's founding mission, which was shaped by the Second World War, is to advance peace, sustainable development and human rights by facilitating collaboration and dialogue among nations. It pursues this objective th ...
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Geomorphological
Geomorphology (from Ancient Greek: , ', "earth"; , ', "form"; and , ', "study") is the scientific study of the origin and evolution of topographic and bathymetric features created by physical, chemical or biological processes operating at or near Earth's surface. Geomorphologists seek to understand why landscapes look the way they do, to understand landform and terrain history and dynamics and to predict changes through a combination of field observations, physical experiments and numerical modeling. Geomorphologists work within disciplines such as physical geography, geology, geodesy, engineering geology, archaeology, climatology, and geotechnical engineering. This broad base of interests contributes to many research styles and interests within the field. Overview Earth's surface is modified by a combination of surface processes that shape landscapes, and geologic processes that cause tectonic uplift and subsidence, and shape the coastal geography. Surface processes ...
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Geoheritage
Geoheritage is the geological aspect of natural and cultural heritage. A geosite is a particular geoheritage asset. The word is a blend of ''geological'' and ''heritage''. It is thus a heritage category comparable to other forms of natural heritage, such as biodiversity. History of the concept The first reference to geoheritage as such was at a 1993 conference held in the UK, the Malvern International Conference on Geological and Landscape Conservation. The term geological heritage was first mentioned at the First International Symposium on the Conservation of our Geological Heritage at Digne, France in 1991. The matter is further discussed in 2002 by Sharples. Conceptually, geoheritage derives from various writings of Busby et al. 2001 and Hallam 1989). In Sharples 1995 the original concept of geoheritage further developed to include the protection of dynamic geological processes and geodiversity. In Sadry 2021 the concept of geoheritage have more developed to include the ...
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Gneisses
Gneiss ( ) is a common and widely distributed type of metamorphic rock. It is formed by high-temperature and high-pressure metamorphic processes acting on formations composed of igneous or sedimentary rocks. Gneiss forms at higher temperatures and pressures than schist. Gneiss nearly always shows a banded texture characterized by alternating darker and lighter colored bands and without a distinct cleavage. Gneisses are common in the ancient crust of continental shields. Some of the oldest rocks on Earth are gneisses, such as the Acasta Gneiss. Description Orthogneiss from the Czech Republic In traditional English and North American usage, a gneiss is a coarse-grained metamorphic rock showing compositional banding (gneissic banding) but poorly developed schistosity and indistinct cleavage. In other words, it is a metamorphic rock composed of mineral grains easily seen with the unaided eye, which form obvious compositional layers, but which has only a weak tendency to fracture ...
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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 ...
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Archean
The Archean Eon ( , also spelled Archaean or Archæan) is the second of four geologic eons of Earth's history, representing the time from . The Archean was preceded by the Hadean Eon and followed by the Proterozoic. The Earth Earth is the third planet from the Sun and the only astronomical object known to harbor life. While large volumes of water can be found throughout the Solar System, only Earth sustains liquid surface water. About 71% of Earth's surfa ... during the Archean was mostly a water world: there was continental crust, but much of it was under an ocean deeper than today's ocean. Except for some trace minerals, today's oldest continental crust dates back to the Archean. Much of the geological detail of the Archean has been destroyed by subsequent activity. The Earliest known life forms, earliest known life started in the Archean. Life was simple throughout the Archean, mostly represented by shallow-water microbial mats called stromatolites, and the a ...
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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 ...
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Quartzitic
Quartzite is a hard, non- foliated metamorphic rock which was originally pure quartz sandstone.Essentials of Geology, 3rd Edition, Stephen Marshak, p 182 Sandstone is converted into quartzite through heating and pressure usually related to tectonic compression within orogenic belts. Pure quartzite is usually white to grey, though quartzites often occur in various shades of pink and red due to varying amounts of hematite. Other colors, such as yellow, green, blue and orange, are due to other minerals. The term ''quartzite'' is also sometimes used for very hard but unmetamorphosed sandstones that are composed of quartz grains thoroughly cemented with additional quartz. Such sedimentary rock has come to be described as orthoquartzite to distinguish it from metamorphic quartzite, which is sometimes called metaquartzite to emphasize its metamorphic origins. Quartzite is very resistant to chemical weathering and often forms ridges and resistant hilltops. The nearly pure silica cont ...
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