Raghunathganj I
Raghunathganj I is a Community development block in India, community development block that forms an administrative division in the Jangipur subdivision of Murshidabad district in the Indian States and territories of India, state of West Bengal. Geography Raghunathganj is located at Raghunathganj I CD block lies in the Rarh region in Murshidabad district. The Hooghly River, Bhagirathi River splits the district into two natural physiographic regions – Rarh on the west and Bagri on the east. The Rarh region is undulating and contains mostly clay and laterite, lateritic clay based soil. As the Rajmahal hills slopes gently down from adjoining Jharkhand it forms the Nabagram plain at the lowest edge of its elevation in this region. The eastern slope of the region is characterised by the existence of numerous cliffs and Beach ridge, bluffs. Raghunathganj I CD block is bounded by Suti I CD block in the north, Raghunathganj II CD block in the east, Sagardighi (community development blo ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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States And 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]   |
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Jangipur Subdivision
Jangipur subdivision is an administrative subdivision of Murshidabad district in the state of West Bengal, India. Overview The Bhagirathi River splits the district into two natural physiographic regions – Rarh on the west and Bagri on the east. Jangipur subdivision lies in the Rarh region in Murshidabad district. The Rarh region spreads over from the adjoining Santhal Pargana division of Jharkhand on the west. The land is slightly higher in altitude than the surrounding plains and is undulating. The Padma River, on the east, separates Murshidabad district from Malda district and Chapai Nawabganj and Rajshahi districts of Bangladesh in the north. Geography Subdivisions Murshidabad district is divided into the following administrative subdivisions: Administrative units Jangipur subdivision has 5 police stations, 7 community development blocks, 7 panchayat samitis, 61 gram panchayats, 561 mouzas, 420 inhabited villages, 2 municipalities and 52 census towns. The municipal ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pakuria Block
Pakuria is a community development block that forms an administrative division in the Pakur subdivision of the Pakur district, Jharkhand state, India. Geography Pakuria, the eponymous CD block headquarters, is located at . It is located 52 km from Pakur, the district headquarters. A predominantly hilly area, Pakur district has pockets of plain land. A long but narrow stretch between the Farakka Feeder Canal, located outside the district, and the Sahibganj loop line is very fertile. The Littipara and Amrapara CD blocks are largely covered by the Rajmahal hills. The rest of the district is rolling uplands. The district, once famous for its forests, have lost all of it, except a few hill tops in the Damin-i-koh area. Pakuria CD block is bounded by Maheshpur block on the north, Nalhati I CD block in Birbhum district of West Bengal on the east, Shikaripara CD block in Dumka district on the south, and Kathikund and Gopikandar CD blocks in Dumka district on the west. Pakuria ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Sagardighi (community Development Block)
Sagardighi is a community development block that forms an administrative division in the Jangipur subdivision of Murshidabad district in the Indian state of West Bengal. History Stone Age Small weapons made of stone, which are around 15,000-20,000 years old, have been discovered by archaeologists of the State Archaeology Department at Ekani Chandpara in Sagardighi. Apart from the weapons they also discovered raw materials and scrap, which indicates that the weapons were made at this place itself. Pala period Sagardighi has many remains of the Pala dynasty. There is a lake of the name, which is the largest in the district. It was dug up by Mahipala. Gauda Sultanate Hussain Shah, the greatest of Sultans of Gauda, was associated with Chandpara or Ekani Chandpara in Sagardighi block. Sekherdighi is a large lake excavated by him. British Period During the British Raj, the Murshidabad leadership of the Nawabs became weak and the British gave charge of revenue collections to a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Raghunathganj II
Raghunathganj II is a community development block that forms an administrative division in the Jangipur subdivision of Murshidabad district in the Indian state of West Bengal. Geography Jot Kamal, a census town in Raghunathganj II block, is located at Raghunathganj II CD block lies in the Rarh region in Murshidabad district. The Bhagirathi River splits the district into two natural physiographic regions – Rarh on the west and Bagri on the east. The Padma River separates Murshidabad district from Malda district and Chapai Nawabganj and Rajshahi districts of Bangladesh in the north. The Rarh region is undulating and contains mostly clay and lateritic clay based soil. As the Rajmahal hills slopes gently down from adjoining Jharkhand it forms the Nabagram plain at the lowest edge of its elevation in this region. The eastern slope of the region is characterised by the existence of numerous cliffs and bluffs. Raghunathganj II CD block is bounded by Suti I CD block in the north, Lal ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Suti I
Suti I is a community development block that forms an administrative division in the Jangipur subdivision of Murshidabad district in the Indian state of West Bengal. Geography Suti I is located at Suti I CD block lies in the Rarh region in Murshidabad district. The Bhagirathi River splits the district into two natural physiographic regions – Rarh on the west and Bagri on the east. The Padma River separates Murshidabad district from Malda district and Chapai Nawabganj and Rajshahi districts of Bangladesh in the north. The Rarh region is undulating and contains mostly clay and lateritic clay based soil. As the Rajmahal hills slopes gently down from adjoining Jharkhand it forms the Nabagram plain at the lowest edge of its elevation in this region. The eastern slope of the region is characterised by the existence of numerous cliffs and bluffs. Suti I CD block is bounded by Suti II CD block in the north, Chapai Nawabganj Sadar Upazila in Chapai Nawabganj District of Bangladesh, ac ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Beach Ridge
A beach ridge is a wave-swept or wave-deposited ridge running parallel to a shoreline. It is commonly composed of sand as well as sediment worked from underlying beach material. The movement of sediment by wave action is called ''littoral transport''. Movement of material parallel to the shoreline is called ''longshore transport''. Movement perpendicular to the shore is called ''on-offshore transport''. A beach ridge may be capped by, or associated with, sand dunes. The height of a beach ridge is affected by wave size and energy. A fall in water level (or an uplift of land) can isolate a beach ridge from the body of water that created it. Isolated beach ridges may be found along dry lakes in the western United States and inland of the Great Lakes of North America, where they formed at the end of the last ice age when lake levels were much higher due to glacial melting and obstructed outflow caused by glacial ice. Some isolated beach ridges are found in parts of Scandinavia, ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cliff
In geography and geology, a cliff is an area of rock which has a general angle defined by the vertical, or nearly vertical. Cliffs are formed by the processes of weathering and erosion, with the effect of gravity. Cliffs are common on coasts, in mountainous areas, escarpments and along rivers. Cliffs are usually composed of rock that is resistant to weathering and erosion. The sedimentary rocks that are most likely to form cliffs include sandstone, limestone, chalk, and dolomite. Igneous rocks such as granite and basalt also often form cliffs. An escarpment (or scarp) is a type of cliff formed by the movement of a geologic fault, a landslide, or sometimes by rock slides or falling rocks which change the differential erosion of the rock layers. Most cliffs have some form of scree slope at their base. In arid areas or under high cliffs, they are generally exposed jumbles of fallen rock. In areas of higher moisture, a soil slope may obscure the talus. Many cliffs also fea ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Jharkhand
Jharkhand (; ; ) is a state in eastern India. The state shares its border with the states of West Bengal to the east, Chhattisgarh to the west, Uttar Pradesh to the northwest, Bihar to the north and Odisha to the south. It has an area of . It is the 15th largest state by area, and the 14th largest by population. Hindi is the official language of the state. The city of Ranchi is its capital and Dumka its sub-capital. The state is known for its waterfalls, hills and holy places; Baidyanath Dham, Parasnath, Dewri and Rajrappa are major religious sites. The state was formed on 15 November 2000, after carving out what was previously the southern half of Bihar. Jharkhand suffers from what is sometimes termed a resource curse: it accounts for more than 40% of the mineral resources of India, but 39.1% of its population is below the poverty line and 19.6% of children under five years of age are malnourished. Jharkhand is primarily rural, with about 24% of its population living in ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rajmahal Hills
The Rajmahal Hills are located in the Santhal Pargana division of Jharkhand, India. They were located on the northern margin of the Gondwana supercontinent, and its hills are today inhabited by the Sauria Paharia people whilst its valleys are dominated by the Santhal people. The hills span over an area of . Volcanic activity during the Jurassic resulted in the formation of the Rajmahal Traps. The hills are approximately located at . The Rajmahal hills are named after the town of Rajmahal which lies in the eastern Jharkhand. The hills trend north-south with an average elevation of , from the Sahibganj district to the Dumka district. The River Ganges wanders around the hills changing the direction of flow from east to south. Francis Buchanan-Hamilton travelled through the Rajmahal hills in the early 19th century. He described the hills that seemed impenetrable in a zone where few travellers had been. He wrote that everywhere people were hostile, apprehensive of officials and unwil ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Laterite
Laterite is both a soil and a rock type rich in iron and aluminium and is commonly considered to have formed in hot and wet tropical areas. Nearly all laterites are of rusty-red coloration, because of high iron oxide content. They develop by intensive and prolonged weathering of the underlying parent rock, usually when there are conditions of high temperatures and heavy rainfall with alternate wet and dry periods. Tropical weathering (''laterization'') is a prolonged process of chemical weathering which produces a wide variety in the thickness, grade, chemistry and ore mineralogy of the resulting soils. The majority of the land area containing laterites is between the tropics of Cancer and Capricorn. Laterite has commonly been referred to as a soil type as well as being a rock type. This and further variation in the modes of conceptualizing about laterite (e.g. also as a complete weathering profile or theory about weathering) has led to calls for the term to be abandoned alto ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Clay
Clay is a type of fine-grained natural soil material containing clay minerals (hydrous aluminium phyllosilicates, e.g. kaolin, Al2 Si2 O5( OH)4). Clays develop plasticity when wet, due to a molecular film of water surrounding the clay particles, but become hard, brittle and non–plastic upon drying or firing. Most pure clay minerals are white or light-coloured, but natural clays show a variety of colours from impurities, such as a reddish or brownish colour from small amounts of iron oxide. Clay is the oldest known ceramic material. Prehistoric humans discovered the useful properties of clay and used it for making pottery. Some of the earliest pottery shards have been dated to around 14,000 BC, and clay tablets were the first known writing medium. Clay is used in many modern industrial processes, such as paper making, cement production, and chemical filtering. Between one-half and two-thirds of the world's population live or work in buildings made with clay, often ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |