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Coastal Plain
A coastal plain is flat, low-lying land adjacent to a sea coast. A fall line commonly marks the border between a coastal plain and a piedmont area. Some of the largest coastal plains are in Alaska and the southeastern United States. The Gulf Coastal Plain of North America extends northwards from the Gulf of Mexico along the Lower Mississippi River to the Ohio River, which is a distance of about . The Atlantic Coastal Plain runs from the New York Bight to Florida. The Coastal Plains of India lie on either side of the Deccan Plateau, along the western and eastern coasts of India. They extend for about 6,150 km from the Rann of Kutch in the west to West Bengal in the east. They are broadly divided into the Western Coastal Plains and the Eastern Coastal Plains. The two coastal plains meet at Kanyakumari, the southernmost tip of the Indian mainland. The eastern coastal plain is located between The Bay of Bengal and the eastern Ghats and the western coastal plain is located between ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Everglades Sawgrass Prairie Moni3
The Everglades is a natural region of tropical climate, tropical wetlands in the southern portion of the U.S. state of Florida, comprising the southern half of a large drainage basin within the Neotropical realm. The system begins near Orlando, Florida, Orlando with the Kissimmee River, which discharges into the vast but shallow Lake Okeechobee. Water leaving the lake in the wet season forms a slow-moving river wide and over long, flowing southward across a limestone shelf to Florida Bay at the southern end of the state. The Everglades experiences a wide range of weather patterns, from frequent flooding in the wet season to drought in the dry season. Throughout the 20th century, the Everglades suffered significant loss of habitat and environmental degradation. Human habitation in the southern portion of the Florida peninsula dates to 15,000 years ago. Before European colonization, the region was dominated by the native Calusa and Tequesta tribes. With Spanish colonizati ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
North European Plain
The North European Plain (german: Norddeutsches Tiefland – North German Plain; ; pl, Nizina Środkowoeuropejska – Central European Plain; da, Nordeuropæiske Lavland and nl, Noord-Europese Laagvlakte ; French : ''Plaine d'Europe du Nord'') is a geomorphological region in Europe, mostly in Poland, Denmark, Germany, Belgium, the Netherlands (Low Countries), along with small parts of northern France and the Czech Republic. It consists of the low plains between the Hercynian Europe ( Central European Highlands) to the south and coastlines of the North Sea and the Baltic Sea to the north. These two seas are separated by the Jutland Peninsula (Denmark). The North European Plain is connected to the East European Plain, together forming the majority of the Great European Plain (European Plain). Geography Elevations vary between 0 and 200 m (0 to about 650 ft). While mostly used as farmland, the region also contains bogs, heath and lakes. The Wadden Sea, a large tidal area, ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mississippi Embayment
The Mississippi embayment is a physiographic feature in the south-central United States, part of the Mississippi Alluvial Plain. It is essentially a northward continuation of the fluvial sediments of the Mississippi River Delta to its confluence with the Ohio River at Cairo, Illinois. The current sedimentary area was formed in the Cretaceous and early Cenozoic by the filling with sediment of a pre-existing basin. An explanation for the embayment's formation was put forward by Van Arsdale and Cox in 2007: movement of the earth's crust brought this region over a volcanic " hotspot" in the Earth's mantle causing an upthrust of magma which formed the Appalachian-Ouachita range. Subsequent erosion caused a deep trough that was flooded by the Gulf of Mexico and eventually filled with sediment from the Mississippi River. Geography The embayment is a topographically low-lying basin that is filled with Cretaceous to recent sediments. The northern end of the embayment appears as a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Israeli Coastal Plain
Israeli coastal plain ( he, מישור החוף, ''Mishor HaḤof'') is the coastal plain along Israel's Mediterranean Sea coast, extending north to south. It is a geographical region defined morphologically by the sea, in terms of topography and soil, and also in its climate, flora and fauna. It is narrow in the north and broadens considerably towards the south, and is continuous with the exception of the short section where Mount Carmel reaches almost all the way to the sea. The Coastal Plain is bordered to the east by – north to south – the topographically higher regions of the Galilee, the low and flat Jezreel Valley, the Carmel range, the mountains of Samaria, the hill country of Judea known as the Shephelah, and the Negev Mountains in the south. To the north it is separated from the coastal plain of Lebanon by the cliffs of Rosh HaNikra, which jut out into the sea from the Galilee mountains, but to the south it continues into the Egyptian Sinai Peninsula. The plain ca ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cumberland Plain
The Cumberland Plain, an IBRA biogeographic region, is a relatively flat region lying to the west of Sydney CBD in New South Wales, Australia. Cumberland Basin is the preferred physiographic and geological term for the low-lying plain of the Permian-Triassic Sydney Basin found between Sydney and the Blue Mountains, and it is a structural sub-basin of the Sydney Basin. The Cumberland Plain has an area of roughly , which lies on Triassic shales and sandstones. Shaping the geography of Sydney, it extends from north of Windsor in the north, to Picton in the south; and from the Nepean-Hawkesbury River in the west almost to Sydney City's Inner West in the east. Much of the Sydney metropolitan area is located on the Plain. The Hornsby Plateau is located to the north and is dissected by steep valleys. The plain takes its name from Cumberland County, in which it is situated, one of the cadastral land divisions of New South Wales. The name ''Cumberland'' was conferred on the County ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coastal Plains Of Chile
The coastal plains of Chile ( es, Planicies litorales) are a series of discontinuous coastal plains found over much of Chile. Together with the Chilean Coast Range, the Chilean Central Valley and the Andes proper the coastal plains are one of the main landscape units of Chile. In Coquimbo and Valparaíso regions these plains are of fluvial or marine origin, and sometimes of combined fluvial and marine origin. See also *Coastal Cliff of northern Chile 250px, View of the arid mountains near Iquique ending abruptly in the Pacific Ocean. The Coastal Cliff of northern Chile ( es, Acantilado Costero) stretches over a length of more than 1000 km along the Atacama Desert. It makes up a large part of ... References {{reflist Geography of Chile Coasts of Chile Plains of Chile ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Atlantic Plain
The Atlantic Plain is one of eight distinct United States physiographic regions. The Atlantic Coast of the United States comprises the coastal states of Delaware, Florida, Georgia, Maine, Maryland, New Jersey, New York, North Carolina, South Carolina, Virginia, and Puerto Rico. The lands adjacent to the Atlantic coastline are made up of sandy beaches, marshlands, bays, and barrier islands. This major division consists of the Continental Shelf and Coastal Plain physiographic provinces. It is the flattest of the U.S. physiographic divisions and stretches over in length from Cape Cod to the Mexican border and southward an additional to the Yucatán Peninsula. The central and southern Atlantic Coast is characterized by barrier and drowned valley coasts. The coastal Atlantic plain features nearly continuous barriers interrupted by inlets, large embayments with drowned river valleys, and extensive wetlands and marshes. The Atlantic plain slopes gently seaward from the inland highla ... [...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] |
Kanyakumari
Kanniyakumari (; , referring to Devi Kanya Kumari), also known as Cape Comorin, is a city in Kanniyakumari district in the state of Tamil Nadu, India. It is the southern tip of the Indian subcontinent and the southernmost city in mainland India, thus referred to as 'The Land's End'. The city is situated south of Thiruvananthapuram city, and about south of Nagercoil, the headquarters of Kanniyakumari district. Kanniyakumari is a popular tourist destination and pilgrimage centre in India. Notable tourist spots include its unique sunrise and sunset points, the Thiruvalluvar Statue and Vivekananda Rock Memorial off the coast. Lying at the tip of peninsular India, the town is bordered on the west, south and east by the Laccadive Sea. It has a coastal line of stretched on the three sides. On the shores of the city is a temple dedicated to Goddess Kanniyakumari (the virgin Goddess), after which the town is named.https://thehinduimages.com/details-page.php?id=157918128 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Eastern Coastal Plains
The Eastern Coastal Plains is a wide stretch of landmass of India, lying between the Eastern Ghats and the Bay of Bengal. It is wider and leveled than the Western Coastal Plains and stretches from Tamil Nadu in the south to West Bengal in the north through Andhra Pradesh and Odisha. Chilka Lake is a brackish water lake along the eastern coastal plain. It lies in the state of Odisha and stretches to the south of the Mahanadi Delta. Deltas of many of India's rivers form a major portion of these plains. The Mahanadi, Godavari, Krishna and Kaveri rivers drain these plains. The region receives both the Northeast & Southwest monsoon rains with its annual rainfall averaging between . The width of the plains varies between 100 and 120 km (62 to 80 miles). It is locally known as Utkal Plains in the Northern part between Cossye and Rushikulya Rivers, Northern Circars in the Central part between Rushikulya and Krishna Rivers and, as Coromandel Coast in the Southern part from ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Western Coastal Plains
The Western Coastal Plains is a strip of coastal plain 50 kilometres (31 mi) in width between the west coast of India and the Western Ghats hills, which starts near the south of the Tapi River. The plains are located between the Western Ghats and the Arabian Sea. The plains begin at Gujarat in the north and end at Tamil Nadu in the south. It includes the states of Gujarat, Maharashtra, Goa, Karnataka, Kerala, and Tamil Nadu. The region consists of three sections: the Northern part of the coast is called the Konkan (Mumbai to Goa), the central stretch is called the Kanara or the "Karavali", while the southern stretch is referred to as the Malabar Coast. On its northern side there are two gulfs: the Gulf of Khambat and the Gulf of Kutch. The rivers along the coast form estuaries and provide conditions ideal for pisciculture. Because of the presence of less coastal land in this part, it will be affected more by the global warming. The northern portion of the west c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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