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Sharavathi
Sharavati is a river which originates and flows entirely within the state of Karnataka in India. It is one of the few westward flowing rivers of India and a major part of the river basin lies in the Western Ghats. The famous Jog Falls, located about 25km from Siddapura, Uttara Kannada, Siddapura, are formed by this river. The river itself and the region around it are rich in biodiversity and are home to many rare species of flora and fauna. Origin and topography The river Sharavati originates at a place called Ambutheertha in the Thirthahalli taluk. According to ancient legend, the god Rama shot at the ground with his Ambu (translates to bow and arrow) because his wife, Sita, was thirsty. When his arrow hit the ground, water poured out (translates to Thirtha) and quenched her thirst. Because the river, according to the legend, originated with this event, the river is called "Sharavati" as "Shara" translates to arrow. The total length of the river is around and it joins the Ara ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Shimoga District
Shimoga district, officially known as Shivamogga district, is a district in the Karnataka state of India. A major part of Shimoga district lies in the Malnad region or the Sahyadri. Shimoga city is its administrative centre. Jog Falls view point is a major tourist attraction. As of 2011 Shimoga district has a population of 17,52,753. There are seven taluks: Soraba, Sagara, Hosanagar, Shimoga, Shikaripura, Thirthahalli, and Bhadravathi. Channagiri and Honnali were part of Shimoga district until 1997 when they became part of the newly formed Davanagere district. Origin of name ''Shivamogga'' was previously known as Mandli. There are legends about how the name ''Shivamogga'' has evolved. According to one, the name ''Shivamogga'' is related to the Hindu God Shiva. ''Shiva-Mukha'' (Face of Shiva), ''Shivana-Moogu'' (Nose of Shiva) or ''Shivana-Mogge'' (Flowers to be offered to Shiva) can be the origins of the name "Shivamogga". Another legend indicates that the name ''Shimoga'' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ambutheertha
Ambuthirtha is a mountain located from the village of Thirthahalli, Shimoga District of the state of Karnataka, India. It is the headwaters of the Sharavathi river. History Etymology The name "Ambuthirtha" refers to a part of Hindu mythology that legend says happened here, which is the reason a temple to Rama is located in the area. The Legend According to ancient legend, the god Rama shot at the ground with his Ambu (translates to bow & arrow) because his wife, Sita, was thirsty (translates to Thirtha). When his arrow hit the ground, water poured out and quenched her thirst. Because the river, according to the legend, originated with this event, the river is called "Sharavathi" as "Shara" translates to arrow. A Shivalinga is installed at Ambuthirtha, under which river Sharavathi originates to start her journey. Hydroelectric Power Plants The river has two Hydroelectric plants built on it that supply electricity for much of the state of Karnataka. The first plant, which is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sharavathi River Karnataka India
Sharavati is a river which originates and flows entirely within the state of Karnataka in India. It is one of the few westward flowing rivers of India and a major part of the river basin lies in the Western Ghats. The famous Jog Falls, located about 25km from Siddapura, are formed by this river. The river itself and the region around it are rich in biodiversity and are home to many rare species of flora and fauna. Origin and topography The river Sharavati originates at a place called Ambutheertha in the Thirthahalli taluk. According to ancient legend, the god Rama shot at the ground with his Ambu (translates to bow and arrow) because his wife, Sita, was thirsty. When his arrow hit the ground, water poured out (translates to Thirtha) and quenched her thirst. Because the river, according to the legend, originated with this event, the river is called "Sharavati" as "Shara" translates to arrow. The total length of the river is around and it joins the Arabian Sea at Honnavar in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Jog Falls
Jog Falls is a waterfall on the Sharavati river located in the Western Ghats running between Uttara Kannada and Shimoga districts of Karnataka, India. It is the third highest plunge waterfall in India. It is a segmented waterfall which depends on rain and season to become a plunge waterfall. The falls are major attractions for tourists and is ranked 36th in the list of free-falling waterfalls, 490th in the world by list of waterfalls by total height, 128th in the list of single-drop waterfalls in the World by the waterfall database. Description Jog Falls is created by the Sharavati dropping , making it the third-highest waterfall in India after the Nohkalikai Falls with a drop of in Meghalaya and the Dudhsagar Falls with a drop of in Goa. Sharavathi, a river which rises at Ambutirtha, next to Nonabur, in the Thirthahalli taluk takes a northwesterly course by Fatte petta, receives the Haridravati on the right below Pattaguppe and the Yenne Hole on the left above Barangi. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sagara, Karnataka
Sagara is a city located in the Indian state of Karnataka. It is also a sub divisional and a taluk headquarters. Located in the Sahyadri Mountain range on the banks of river Varada, it is known for its proximity to Jog Falls and to the historical places of Ikkeri, Keladi and Varadamoola. The river Varada originates near Varada-moola. Sagara subdivision consists of Sagara, Soraba, Hosanagara and Shikaripur taluks. City Municipal Council Sagara city is one of the 74 Karnataka Municipal Reforms Project (KMRP) City in Karnataka. Sagara ULB was started in 1931 and became a City Municipal Council (CMC) grade two in the year 2007. The ULB consist of 31 wards with the respective number of councillors. The population of the city was 64,550 at the 2011 census and total area is 19.71 sq. km. Etymology Sagara derives its name from ''Sadashiva Sagara''. Sadashiva Nayaka, ruler of Keladi dynasty built a lake in between Keladi and Ikkeri. Sadashiva Sagara is now called Ganapathi Kere (G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Linganamakki
The Linganamakki Dam (Kannada : ಲಿಂಗನಮಕ್ಕಿ ಜಲಾಶಯ) was constructed by the Karnataka State Government in 1964. Located in the Kargal village of Sagara taluk, the dam has a length of stretching across the Sharavathi river. It is located about 9 km from Jog Falls Jog Falls is a waterfall on the Sharavati river located in the Western Ghats running between Uttara Kannada and Shimoga districts of Karnataka, India. It is the third highest plunge waterfall in India. It is a segmented waterfall which depends .... It has a storage capacity of 4.29 cubic kms or 151.52 tmc ft of water. References Hydroelectric power stations in Karnataka Dams in Karnataka Buildings and structures in Shimoga district Dams completed in 1964 1964 establishments in Mysore State {{India-powerstation-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Karnataka
Karnataka (; ISO: , , also known as Karunāḍu) is a state in the southwestern region of India. It was formed on 1 November 1956, with the passage of the States Reorganisation Act. Originally known as Mysore State , it was renamed ''Karnataka'' in 1973. The state corresponds to the Carnatic region. Its capital and largest city is Bengaluru. Karnataka is bordered by the Lakshadweep Sea to the west, Goa to the northwest, Maharashtra to the north, Telangana to the northeast, Andhra Pradesh to the east, Tamil Nadu to the southeast, and Kerala to the southwest. It is the only southern state to have land borders with all of the other four southern Indian sister states. The state covers an area of , or 5.83 percent of the total geographical area of India. It is the sixth-largest Indian state by area. With 61,130,704 inhabitants at the 2011 census, Karnataka is the eighth-largest state by population, comprising 31 districts. Kannada, one of the classical languages of India, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Conglomerate (geology)
Conglomerate () is a clastic sedimentary rock that is composed of a substantial fraction of rounded to subangular gravel-size clasts. A conglomerate typically contains a matrix of finer-grained sediments, such as sand, silt, or clay, which fills the interstices between the clasts. The clasts and matrix are typically cemented by calcium carbonate, iron oxide, silica, or hardened clay. Conglomerates form by the consolidation and lithification of gravel. They can be found in sedimentary rock sequences of all ages but probably make up less than 1 percent by weight of all sedimentary rocks. In terms of origin and depositional mechanisms, they are closely related to sandstones and exhibit many of the same types of sedimentary structures, e.g., tabular and trough cross-bedding and graded bedding.Boggs, S. (2006) ''Principles of Sedimentology and Stratigraphy.'', 2nd ed. Prentice Hall, New York. 662 pp. Friedman, G.M. (2003) ''Classification of sediments and sedimentary rocks.'' In G ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dharwar
Dharwad (), also known as Dharwar, is a city located in the north western part of the Indian state of Karnataka. It is the headquarters of the Dharwad district of Karnataka and forms a contiguous urban area with the city of Hubballi. It was merged with Hubballi in 1962 to form the twin cities of Hubballi-Dharwad. It covers an area of and is located northwest of Bangalore, on NH-48, between Bangalore and Pune. Etymology The word "Dharwad" is derived from the Sanskrit word 'dwarawata', 'dwara' meaning "door" and 'wata' or 'wada' meaning "town". It means a place of rest in a long travel or a small habitation. For centuries, Dharwad acted as a resting place for travellers and a gateway between the ''Malenadu'' (western mountains) and the ''Bayalu Seeme'' (plains). History The Chalukyas ruled Dharwad during the 12th century. A stone inscription indicates that there was a ruler by the name of BhaskaraDeva in 1117. In the 14th century, the district was first overrun by the Bahmani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gneiss
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distorti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Schist
Schist ( ) is a medium-grained metamorphic rock showing pronounced schistosity. This means that the rock is composed of mineral grains easily seen with a low-power hand lens, oriented in such a way that the rock is easily split into thin flakes or plates. This texture (geology), texture reflects a high content of platy minerals, such as micas, talc, chlorite group, chlorite, or graphite. These are often interleaved with more granular minerals, such as feldspar or quartz. Schist typically forms during regional metamorphism accompanying the process of mountain building (orogeny) and usually reflects a medium Metamorphism#Metamorphic grades, grade of metamorphism. Schist can form from many different kinds of rocks, including sedimentary rocks such as mudstones and igneous rocks such as tuffs. Schist metamorphosed from mudstone is particularly common and is often very rich in mica (a ''mica schist''). Where the type of the original rock (the protolith) is discernible, the schist is us ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
