Canning II
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Canning II
Canning II is a community development block that forms an administrative division in Canning subdivision of South 24 Parganas district in the Indian State of West Bengal. Geography Canning II CD block is located at . It has an average elevation of . Canning II CD block is bounded by Bhangar I CD block in the north, Sandeshkhali I, Sandeshkhali II and Hingalganj CD blocks in North 24 Parganas district in the east, Basanti CD block in the south, Canning I, Baruipur and Sonarpur CD blocks in the west. South 24 Parganas district is divided into two distinct physiographic zones: the marine-riverine delta in the north and the marine delta zone in the south. As the sea receded southwards, in the sub-recent geological period, a large low-lying plain got exposed. Both tidal inflows and the rivers have been depositing sediments in this plain. The periodical collapse of both the natural levees and man-made embankments speed up the process of filling up of the depressions containing br ...
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West Bengal
West Bengal (, Bengali: ''Poshchim Bongo'', , abbr. WB) is a state in the eastern portion of India. It is situated along the Bay of Bengal, along with a population of over 91 million inhabitants within an area of . West Bengal is the fourth-most populous and thirteenth-largest state by area in India, as well as the eighth-most populous country subdivision of the world. As a part of the Bengal region of the Indian subcontinent, it borders Bangladesh in the east, and Nepal and Bhutan in the north. It also borders the Indian states of Odisha, Jharkhand, Bihar, Sikkim and Assam. The state capital is Kolkata, the third-largest metropolis, and seventh largest city by population in India. West Bengal includes the Darjeeling Himalayan hill region, the Ganges delta, the Rarh region, the coastal Sundarbans and the Bay of Bengal. The state's main ethnic group are the Bengalis, with the Bengali Hindus forming the demographic majority. The area's early history featured a succession ...
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Sandeshkhali II
Sandeshkhali-II is a Community development block in India, community development block that forms an administrative division in Basirhat subdivision of North 24 Parganas district in the Indian States and territories of India, state of West Bengal. Geography Sandeshkhali is located at . Sandeshkhali II CD Block is bounded by Sandeshkhali I CD Block in the north, Hingalganj CD Block towards east, Basanti (community development block), Basanti, Gosaba (community development block), Gosaba CD Blocks and Sundarbans in South 24 Parganas district in the south and Canning II CD Block in South 24 Parganas district in the west. Sandeshkhali II CD Block is part of the North Bidyadhari Plain, one of the three physiographic regions in the district located in the lower Ganges Delta. The area is full of marshes and salt water lakes. The Bidyadhari River, Bidyadhari has a long course through the central part of the district. The wide Dansa, Kalindi and Raimangal rivers flow through the area. ...
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Panchayat Samiti (Block)
Panchayat samiti is a rural local government (panchayat) body at the intermediate tehsil (taluka/mandal) level in India. It works for the villages of the tehsil that together are called a development block. It has been said to be the "panchayat of panchayats". The 73rd Amendment defines the levels of panchayati raj institution as : * No Level * Intermediate level * Base level The panchayat samiti is the link between the gram panchayat (village council) and the zila parishad (district board). The name varies across states: ''mandal parishad'' in Andhra Pradesh, ''taluka panchayat'' in Gujarat, and ''mandal panchayat'' in Karnataka. Composition Typically, a taluka panchayat is composed of elected members of the area: the block development officer, members of the state's legislative assembly, members of parliament belonging to that area, otherwise unrepresented groups ( Scheduled Castes, Scheduled Tribes and women), associate members (such as a farmer, a representative of t ...
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Monsoon
A monsoon () is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with annual latitudinal oscillation of the Intertropical Convergence Zone (ITCZ) between its limits to the north and south of the equator. Usually, the term monsoon is used to refer to the rainy phase of a seasonally changing pattern, although technically there is also a dry phase. The term is also sometimes used to describe locally heavy but short-term rains. The major monsoon systems of the world consist of the West African, Asia–Australian, the North American, and South American monsoons. The term was first used in English in British India and neighboring countries to refer to the big seasonal winds blowing from the Bay of Bengal and Arabian Sea in the southwest bringing heavy rainfall to the area. Etymology The etymology of the word monsoon is not wholl ...
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Brackish Water
Brackish water, sometimes termed brack water, is water occurring in a natural environment that has more salinity than freshwater, but not as much as seawater. It may result from mixing seawater (salt water) and fresh water together, as in estuaries, or it may occur in brackish fossil aquifers. The word comes from the Middle Dutch root '' brak''. Certain human activities can produce brackish water, in particular civil engineering projects such as dikes and the flooding of coastal marshland to produce brackish water pools for freshwater prawn farming. Brackish water is also the primary waste product of the salinity gradient power process. Because brackish water is hostile to the growth of most terrestrial plant species, without appropriate management it is damaging to the environment (see article on shrimp farms). Technically, brackish water contains between 0.5 and 30 grams of salt per litre—more often expressed as 0.5 to 30 parts per thousand (‰), which is a specific gr ...
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Levee
A levee (), dike (American English), dyke (English in the Commonwealth of Nations, Commonwealth English), embankment, floodbank, or stop bank is a structure that is usually soil, earthen and that often runs parallel (geometry), parallel to the course of a river in its floodplain or along low-lying coastlines. The purpose of a levee is to keep the course of rivers from changing and to protect against flooding of the area adjoining the river or coast. Levees can be naturally occurring ridge structures that form next to the bank of a river, or be an artificially constructed fill dirt, fill or wall that regulates water levels. Ancient civilizations in the Indus Valley civilisation, Indus Valley, ancient Egypt, Mesopotamia and China all built levees. Today, levees can be found around the world, and failures of levees due to erosion or other causes can be major disasters. Etymology Speakers of American English (notably in the Midwestern United States, Midwest and Deep South) u ...
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Tide
Tides are the rise and fall of sea levels caused by the combined effects of the gravity, gravitational forces exerted by the Moon (and to a much lesser extent, the Sun) and are also caused by the Earth and Moon orbiting one another. Tide tables can be used for any given locale to find the predicted times and amplitude (or "tidal range"). The predictions are influenced by many factors including the alignment of the Sun and Moon, the #Phase and amplitude, phase and amplitude of the tide (pattern of tides in the deep ocean), the amphidromic systems of the oceans, and the shape of the coastline and near-shore bathymetry (see ''#Timing, Timing''). They are however only predictions, the actual time and height of the tide is affected by wind and atmospheric pressure. Many shorelines experience semi-diurnal tides—two nearly equal high and low tides each day. Other locations have a diurnal cycle, diurnal tide—one high and low tide each day. A "mixed tide"—two uneven magnitude ...
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Period (geology)
The geologic time scale, or geological time scale, (GTS) is a representation of time based on the rock record of Earth. It is a system of chronological dating that uses chronostratigraphy (the process of relating strata to time) and geochronology (scientific branch of geology that aims to determine the age of rocks). It is used primarily by Earth scientists (including geologists, paleontologists, geophysicists, geochemists, and paleoclimatologists) to describe the timing and relationships of events in geologic history. The time scale has been developed through the study of rock layers and the observation of their relationships and identifying features such as lithologies, paleomagnetic properties, and fossils. The definition of standardized international units of geologic time is the responsibility of the International Commission on Stratigraphy (ICS), a constituent body of the International Union of Geological Sciences (IUGS), whose primary objective is to precisely define ...
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South 24 Parganas District
South 24 Parganas (Pron: pɔrɡɔnɔs; abbr. 24 PGS (S)), or sometimes South Twenty Four Parganas and Dakshin 24 Parganas, is a district in the Indian state of West Bengal, headquartered in Alipore. It is the largest district of West Bengal by area and second largest by population. It is the sixth most populous district in India (out of 640). On one side of the district there is the urban fringe of Kolkata, and on the other the remote riverine villages in the Sundarbans. History Originally, the capital of Raja Bikramaditya and Maharaja Pratapaditya was at Dhumghat. Later it was transferred to Ishwaripur (Originated from the name Jeshoreshwaripur). Maharaja Pratapaditya declared the independence of South Bengal from the Mughal Empire. Pratapaditya's father Shrihari (Shridhar), a Kayastha, was an influential officer in the service of Daud Khan Karrani. Upon the fall of Daud, he fled with the government treasure in his custody. He then, in 1574, set up a kingdom for himself in th ...
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Sonarpur (community Development Block)
Sonarpur is a community development block (CD block) that forms an administrative division in the Baruipur subdivision of the South 24 Parganas district in the Indian state of West Bengal. Geography The Sonarpur CD block is located at . It has an average elevation of . The Sonarpur CD block is bounded by Garia neighbourhood of Kolkata in the north, the Bhangar I, Bhangar II and Canning II CD blocks in the east, the Baruipur CD block in the south, the Thakurpukur Maheshtala and Bishnupur I CD blocks in the west. The South 24 Parganas district is divided into two distinct physiographic zones: the marine-riverine delta in the north and the marine delta zone in the south. As the sea receded southwards, in the sub-recent geological period, a large low-lying plain got exposed. Both tidal inflows and rivers have deposited sediments in this plain. The periodical collapse of both the natural Levees and man-made embankments speed up the process of filling up of the depressions contain ...
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Baruipur (community Development Block)
Baruipur is a community development block that forms an administrative division in the Baruipur subdivision of the South 24 Parganas district in the Indian state of West Bengal. Geography The Baruipur CD block is located at . It has an average elevation of . The Baruipur CD block is bounded by the Sonarpur CD block in the north, the Canning I CD block in the east, the Jaynagar I CD block in the south, the Magrahat II and Bishnupur I CD blocks in the west. The South 24 Parganas district is divided into two distinct physiographic zones: the marine-riverine delta in the north and the marine delta zone in the south. As the sea receded southwards, in the sub-recent geological period, a large low-lying plain got exposed. Both tidal inflows and the rivers have been depositing sediments in this plain. The periodical collapse of both the natural levees and man-made embankments speed up the process of filling up of the depressions containing brackish water wetlands. The marine delta in t ...
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Canning I
Canning I is a community development block that forms an administrative division in Canning subdivision of South 24 Parganas district in the Indian State of West Bengal. Geography Canning I CD block is located at . It has an average elevation of . Canning I CD block is bounded by Canning II CD block in the north, Basanti CD block in the east and south, Kultali, Jaynagar I and Baruipur CD blocks in the west. South 24 Parganas district is divided into two distinct physiographic zones: the marine-riverine delta in the north and the marine delta zone in the south. As the sea receded southwards, in the sub-recent geological period, a large low-lying plain got exposed. Both tidal inflows and the rivers have been depositing sediments in this plain. The periodical collapse of both the natural levees and man-made embankments speed up the process of filling up of the depressions containing brackish water wetlands. The marine delta in the south is formed of interlacing tidal channels. ...
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