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Wainganga River
The Wainganga is a river in India originating in the Mahadeo Hills in Mundara near the village Gopalganj in Seoni, Madhya Pradesh. It is a key tributary of the Godavari. The river flows south in a winding course through the states of Madhya Pradesh and Maharashtra, roughly . After joining the Wardha River, the united stream, which is known as the Pranahita River, empties into the Godavari River at Kaleshwaram, Telangana. Course The main stream of the Wainganga originates at Mahadev hills near Gopalganj, Seoni District, on the southern slopes of the Satpura Range of Madhya Pradesh. The river has developed extensive floodplains characterized by sweeping graceful meanders, low alluvial flats, and slip-off slopes. The river has high banks, which measure from to on either side. The northern part is surrounded by the Mahadeo hills and Satpura Range, with an average elevation of 625 m (2,051 ft) above sea level. The valley of the Wainganga River is forested and sparsely p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pranhita River
The Pranhita River is the largest tributary of Godavari River covering about 34% of its drainage basin conveying the combined waters of the Penganga River, the Wardha River, and the Wainganga River. By virtue of its extensive network of tributaries, the river drains a large part of Vidarbha region in Maharashtra, as well as the southern slopes of the Satpura Range in southeast Madhya Pradesh. It flows along the border of Gadchiroli district in Maharashtra and Komaram Bheem Asifabad district in Telangana. The Pranahita sub-basin is the seventh largest in India, measuring about 109,078 km2, making it larger than the individual basins of significant rivers such as the Narmada River and Kaveri. Origin The Pranhita River begins at the confluence of two extensive rivers: the Wardha (catchment area: 46,237 km2) and the Wainganga (catchment area: 49,677 km2). This junction lies on the border between the states of Maharashtra and Telangana near TumdiHettty,Kouthala M ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pranahita River
The Pranhita River is the largest tributary of Godavari River covering about 34% of its drainage basin conveying the combined waters of the Penganga River, the Wardha River, and the Wainganga River. By virtue of its extensive network of tributaries, the river drains a large part of Vidarbha region in Maharashtra, as well as the southern slopes of the Satpura Range in southeast Madhya Pradesh. It flows along the border of Gadchiroli district in Maharashtra and Komaram Bheem Asifabad district in Telangana. The Pranahita sub-basin is the seventh largest in India, measuring about 109,078 km2, making it larger than the individual basins of significant rivers such as the Narmada River and Kaveri. Origin The Pranhita River begins at the confluence of two extensive rivers: the Wardha River, Wardha (catchment area: 46,237 km2) and the Wainganga River, Wainganga (catchment area: 49,677 km2). This junction lies on the border between the states of Maharashtra and Telangan ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wainganga
The Wainganga is a river in India originating in the Mahadeo Hills in Mundara near the village Gopalganj in Seoni, Madhya Pradesh. It is a key tributary of the Godavari River, Godavari. The river flows south in a winding course through the states of Madhya Pradesh and Maharashtra, roughly . After joining the Wardha River, the united stream, which is known as the Pranhita River, Pranahita River, empties into the River Godavari, Godavari River at Kaleshwaram, Telangana. Course The main stream of the Wainganga originates at Mahadev hills near Gopalganj, Seoni District, on the southern slopes of the Satpura Range of Madhya Pradesh. The river has developed extensive floodplains characterized by sweeping graceful meanders, low Alluvial plain, alluvial flats, and slip-off slopes. The river has high banks, which measure from to on either side. The northern part is surrounded by the Mahadeo Hills, Mahadeo hills and Satpura Range, with an average elevation of 625 m (2,051 ft) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
India
India, officially the Republic of India (Hindi: ), is a country in South Asia. It is the seventh-largest country by area, the second-most populous country, and the most populous democracy in the world. Bounded by the Indian Ocean on the south, the Arabian Sea on the southwest, and the Bay of Bengal on the southeast, it shares land borders with Pakistan to the west; China, Nepal, and Bhutan to the north; and Bangladesh and Myanmar to the east. In the Indian Ocean, India is in the vicinity of Sri Lanka and the Maldives; its Andaman and Nicobar Islands share a maritime border with Thailand, Myanmar, and Indonesia. Modern humans arrived on the Indian subcontinent from Africa no later than 55,000 years ago., "Y-Chromosome and Mt-DNA data support the colonization of South Asia by modern humans originating in Africa. ... Coalescence dates for most non-European populations average to between 73–55 ka.", "Modern human beings—''Homo sapiens''—originated in Africa. Then, int ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bramhapuri
Bramhapuri is a town and municipal council in Chandrapur district in the state of Maharashtra, India. Geography Bramhapuri is one of the six divisions located in the northeastern part of Chandrapur district, Maharashtra at and has an average elevation of 229.5 metres (753 feet). The town is located in the 73rd Vidhan Sabha constituency in Maharashtra. Demographics According to 2011 Indian census, Brahmapuri Municipal Council administers over 8,575 households composing a population of 36,025. Male population constitute 50.10% of the total population and females 49.90%. The population of children with an age of 0 to 6 is 3,283, which is 9.11 % of the total population of Brahmapuri. In Brahmapuri Municipal Council, the female sex ratio is of 996 against the state average of 929. The child sex ratio in Brahmapuri is around 990 compared to the Maharashtra state average of 894. The literacy rate of Brahmapuri city is 89.69 % higher than state average of 82.34 %. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pauni
Pauni is a town and a Municipal Council in Bhandara district in the Indian state of Maharashtra. Now it has National Highway NH-247. Pauni is also known as Kashi of Vidarbha due to its wide swath of temples. Geography Pauni is located at . It has an average elevation of 226 metres (741 feet). The town is surrounded on three sides by a moat and earthen rampart, and the fourth side by the Wainganga River. The main language of Pauni is Marathi, the regional language of the state of Maharashtra. Pauni is surrounded by Umred-Karhandla wildlife sanctuary, famous for tigers and other wild animals. Introduction Pauni (Pauni derived from the name of king "Pavan") is situated on the bank of river Wainganga known as South Ganga. It is a center of market and trade for the surrounding smaller villages and connects the smaller villages to cities like Nagpur, Chandrapur, Bhandara and Gondhia. In ancient times, Pauni was famous for the handloom textile industry. It is also a place ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gadchiroli
Gadchiroli ( əɖt͡ʃiɾoliː is a city and a municipal council in Gadchiroli district in the state of Maharashtra, central India. It is located on eastern side of Maharashtra, and is the administrative headquarters of the district. Gadchiroli is called a lung of Maharashtra as it has almost 35% of this district has forest cover. The main river flowing through city is the Wainganga River. The landscape is lush and green during the monsoon season which is prone to flooding. Gadchiroli is known for its forests. Teak is grown commercially and bamboos are used for various crafts. Notable places and Personalities Some notable places and personalities in the town include: * Chaprala Wildlife Sanctuary"Tourist Places , District Gadchiroli, Government of Maharashtra , India". Retrieved 21 July 2021. *Semana-Hanuman Temple – About from center of town (Gandhi Chowk) * Hemalkasa – Situated in Bhamragarh Block (east side of district), from Gadchiroli. *Allapalli – ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Balaghat
Balaghat is a city and a municipality in Balaghat district, in the state of Madhya Pradesh, India. It is the administrative headquarters of Balaghat District. Wainganga River flows beside the town. Geography Balaghat is located at . It has an average elevation of 288 metres (944 feet). Demographics As of the 2011 Census of India The 2011 Census of India or the 15th Indian Census was conducted in two phases, house listing and population enumeration. The House listing phase began on 1 April 2010 and involved the collection of information about all buildings. Information ..., Balaghat had a population of 84,216. Males constitute 51% of the population and females 49%. 11% of the population is under 6 years of age. References Further reading {{Authority control Cities and towns in Balaghat district sv:Balaghat (distrikt) ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sea Level
Mean sea level (MSL, often shortened to sea level) is an average surface level of one or more among Earth's coastal bodies of water from which heights such as elevation may be measured. The global MSL is a type of vertical datuma standardised geodetic datumthat is used, for example, as a chart datum in cartography and marine navigation, or, in aviation, as the standard sea level at which atmospheric pressure is measured to calibrate altitude and, consequently, aircraft flight levels. A common and relatively straightforward mean sea-level standard is instead the midpoint between a mean low and mean high tide at a particular location. Sea levels can be affected by many factors and are known to have varied greatly over geological time scales. Current sea level rise is mainly caused by human-induced climate change. When temperatures rise, Glacier, mountain glaciers and the Ice sheet, polar ice caps melt, increasing the amount of water in water bodies. Because most of human settlem ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Slip-off Slope
A slip-off slope is a depositional landform that occurs on the inside convex bank of a meandering river. The term can refer to two different features: one in a freely meandering river with a floodplain and the other in an entrenched river. Freely meandering rivers In a freely meandering river, a ''slip-off slope'' is characterized by a gentle slope composed of sand and pebbles on the inside convex bank of a meander loop, across the channel from a cut bank or river-cut cliff.Scheffers, A.M., May, S.M. and Kelletat, D.H., 2015. ''Forms by Flowing Water (Fluvial Features).'' In ''Landforms of the World with Google Earth.'' (pp. 183-244). Springer, Amsterdam, Netherlands. 391 pp. As water in a meandering river travels around a bend, it moves in a secondary corkscrew-like flow as it travels downstream, in a pattern called helicoidal flow. This phenomenon causes increased water velocity in the outside bend of the meander, driving lateral bank erosion. It is also responsible for slo ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Plain
An alluvial plain is a largely flat landform created by the deposition of sediment over a long period of time by one or more rivers coming from highland regions, from which alluvial soil forms. A floodplain is part of the process, being the smaller area over which the rivers flood at a particular period of time, whereas the alluvial plain is the larger area representing the region over which the floodplains have shifted over geological time. As the highlands erode due to weathering and water flow, the sediment from the hills is transported to the lower plain. Various creeks will carry the water further to a river, lake, bay, or ocean. As the sediments are deposited during flood conditions in the floodplain of a creek, the elevation of the floodplain will be raised. As this reduces the channel floodwater capacity, the creek will, over time, seek new, lower paths, forming a meander (a curving sinuous path). The leftover higher locations, typically natural levees at the margins ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Meanders
A meander is one of a series of regular sinuous curves in the channel of a river or other watercourse. It is produced as a watercourse erodes the sediments of an outer, concave bank (cut bank) and deposits sediments on an inner, convex bank which is typically a point bar. The result of this coupled erosion and sedimentation is the formation of a sinuous course as the channel migrates back and forth across the axis of a floodplain. The zone within which a meandering stream periodically shifts its channel is known as a meander belt. It typically ranges from 15 to 18 times the width of the channel. Over time, meanders migrate downstream, sometimes in such a short time as to create civil engineering challenges for local municipalities attempting to maintain stable roads and bridges.Neuendorf, K.K.E., J.P. Mehl Jr., and J.A. Jackson, J.A., eds. (2005) ''Glossary of Geology'' (5th ed.). Alexandria, Virginia, American Geological Institute. 779 pp. Charlton, R., 2007. ''Fundamentals o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
._Plan_of_the_historic_city.jpg "Click for more on -> Pauni")
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