340 Sentences With "alluvial plains" | Random Sentence Generator

Three years after seizing control of the great alluvial plains of the Tigris and the Euphrates, Islamic State, which has claimed so many victims in north-western Iraq, Syria and beyond, is finally dying.

Khasi men and women sit by roadsides with ball-peen hammers reducing boulders to pebbles the size of peas that will descend to the plains not by stream but by lorry, there to feed an infrastructure boom on the alluvial plains of Bangladesh.

Alluvial plains (Sumer/Elam). Low rainfall makes irrigation systems necessary. Ubaid culture from 6,900 BC.

The area is composed of flat alluvial plains that form a part of the Gangetic Delta.

Darappur is located at . Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati. With these rivers getting silted up, floods are a recurring feature.

Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichamati. With these rivers getting silted up, floods are a recurring feature.Gangopadhyay, Basudev, Paschimbanga Parichay, 2001, , p.

Other islands include Hwanggumpyong, Ssarisŏm, Kanŭnsŏm, Munbakto, and Wihwa. There are various alluvial plains and extensive reed fields.

The agricultural landscape consists of: 13.4% alluvial plains of the Yuanjiang River, 49.3% hillocks, and 36.0% hills and mountains.

Jagatnagar is located at: The area is composed of flat alluvial plains that form a part of the Gangetic Delta.

Nasibpur is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta.

Balarambati is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta.

Bargachhia is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta.

Borai is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta.

Dhaniakhali is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta.

Kuki is located in northeastern Saitama Prefecture, approximately 50 kilometers from downtown Tokyo in the alluvial plains of the Tone River.

Its typical habitat is sandy deserts, alluvial plains and especially arid sandy areas in hilly deserts with a scattering of scrub.

It has a carrying capacity of 10,500 sheep. The country is mostly alluvial plains with duplex soils and many sandy rises. The vegetation is mixed shrubland of currant bush, many acacias and some Gascoyne bluebush. The western portion of the station is made up of flat, saline alluvial plains that support salt bush, blue bush and taller acacia species.

The area lies on Matangi soils, formed on the edge of the Komakorau Bog and the Waikato's alluvial plains of sands and gravels.

Environmental Protection Agency, Queensland. Four regional ecosystems listed as of concern are easily encountered by visitors to Carnarvon Gorge: Queensland blue gum woodland on alluvial plains; silver-leaved ironbark woodland on alluvial plains; Queensland blue gum, river she-oak fringing woodland on alluvial plains; and tall open forest in sheltered gorges and moist habitats. Two plant species, in particular, are considered Carnarvon Gorge icons; the cycad Macrozamia moorei (no common name) and the Carnarvon fan palm (Livistona nitida). Macrozamia moorei is closely associated with the Tertiary basalt flows of the Buckland Volcanic Province, and is endemic to Central Queensland.

Serampore is located at . The area consists of flat alluvial plains, that form a part of the Gangetic Delta. This belt is highly industrialised.

The alluvial plains of Teonthar are 100 metres (330 ft) in elevation. Due to its location and elevation, the area around Teonthar is flood prone.

Baruipara is located at in Hooghly district, West Bengal. The area is composed of flat alluvial plains that form a part of the Gangetic Delta.

Lopburi lies on the Lopburi River at an elevation of mostly surrounded by alluvial plains, although some hills rise to between and to the north-east.

Hanguk-eui Chungjeok Pyeongya [Alluvial Plains of Korea]. Gyohak Yeongusa, Seoul. making it the third longest in South Korea. The area of the Geum River Basin is .

In southern Mesopotamia were the alluvial plains of Sumer and Elam. Since there was little rainfall, irrigation systems were necessary. The Ubaid culture flourished from 5500 BCE.

Maheshganj is located at . Nabadwip CD Block is bounded by Krishnanagar II CD Block in the north, Krishnanagar I CD Block in the east, Santipur in the south and Purbasthali I CD Block in Bardhaman district in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

The shrub grows generally on alluvial plains, in California montane chaparral and woodlands and temperate coniferous forest habitats, among Tecate cypress (Cupressus forbesii) trees.Federal Register October 3, 2006.

The Sierra Chica de Zonda is located about four kilometres west. However, all the ejido of the town is settled in the alluvial plains formed east of the same.

The height decreases from south to north. The Kaimur Range is more than . The alluvial plains of Teonthar are just around .A series of plateaux runs along the Kaimur Range.

Ecosystems include a variety of rainforest types, wet sclerophyll forests, mixed eucalypt woodlands, melaleuca gallery forest, and lakes on alluvial plains. Brooklyn also contains a relict population of Bunya Pine.

Arroyo belongs to the alluvial plains sub-region of Ponce-Patillas known as the Southern Coastal Valley. The area is very dry although its plains are productive thanks to artificial irrigation.

The palea has a rounded tip and the anthers are long. The grass flowers from August to September. The grass occurs in wet woods and prairies, stream banks, and alluvial plains.

Chapra is located at . Chapra CD Block is bounded by Tehatta I CD Block in the north, Damurhuda Upazila in Chuadanga District of Bangladesh in the east, Krishnaganj and Krishnanagar I CD Blocks, in the south and Krishnanagar II and Nakashipara CD Blocks in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Subarnapur is located at . Haringhata CD Block is bounded by Chakdaha CD Block in the north and west, Bangaon and Gaighata CD Blocks, in North 24 Parganas district, in the east, Amdanga, Habra I and Habra II CD Blocks, in North 24 Parganas district, in the south. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Dhubulia is located at . Krishnanagar II CD Block is bounded by Nakshipara CD Block in the north, Chapra CD Block in the east, Krishnanagar I and Nabadwip CD Blocks in the south and Purbasthali II CD Block in Bardhaman district, across the Hooghly, in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Habibpur is located at . Ranaghat I CD Block is bounded by Hanskhali CD Block in the north, Ranaghat II CD Block in the east, Chakdaha CD Block in the south and Santipur CD Block and Balagarh CD Block in Hooghly district across the Hooghly River in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Nokari is located at . Ranaghat II CD Block is bounded by Hanskhali in the north, Jhikargachha Upazila in Jessore District of Bangladesh and Bagdah CD Block in North 24 Parganas district, in the east, Chakdaha CD Block in the south and Ranaghat I CD Block in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Bhaluka, a constituent panchayat in this block, is located at . Krishnanagar I CD Block is bounded by Krishnanagar II and Chapra CD Blocks in the north, Krishnaganj and Hanskhali CD Blocks in the east, Santipur CD Block in the south and Nabadwip CD Block in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Raghunathpur is located at The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised.

Madhusudanpur is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised.

Dakshin Rajyadharpur is located at . Belumilki and Dakshin Rajyadharpur are close to Serampore. The area consists of flat alluvial plains, that form a part of the Gangetic Delta. This belt is highly industrialised.

The town is situated near the coast. A confluence of the Haddas, Aligide and Comaile River's runs through the district. During the 1960s, there was significant agricultural development on the district's alluvial plains.

Karimpur is located at . Karimpur I CD Block is bounded by Jalangi and Domkal CD Blocks, in Murshidabad district, in the north, Daulatpur Upazila in Kushtia District of Bangladesh in the east, Karimpur II CD Block in the south and Naoda CD Block, in Murshidabad district, in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Tehatta is located at . at Tehatta Tehatta I CD Block is bounded by Naoda, in Murshidabad district, and Karimpur II CD Block, in the north, Gangni Upazila, Meherpur Sadar Upazila and Mujibnagar Upazila of Meherpur District of Bangladesh in the east, Chapra CD Block in the south and Tehatta II CD Block in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Prachinburi is on the banks of the Prachinburi River, about northeast of Bangkok. Most of the city's environs are flats alluvial plains, but the foothills of the Sankamphaeng Range begin to rise about to the north.

The maps of Ranaghat I and Ranaghat II CD blocks, in the District Census Handbook 2011, Nadia, shows the census towns of Kamgachhi, Raghabpur, Panpara, Aistala, Satigachha, Anulia, Halalpur Krishnapur, Hijuli and Ranaghat (CT) forming a cluster around Ranaghat. Certain other localitites such as Nokari, Nasra, Cooper's Camp, Birnagar, Habibpur, Gopalpur and Parbbatipur are also linked with this cluster. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Nakashipara is located at . Nakasipara CD Block is bounded by Tehatta II and Kaliganj CD Blocks in the north, Tehatta I and Chapra CD Blocks in the east, Nabadwip CD Block and Purbasthali II CD Block, in Bardhaman district across the Bhagirathi, in the south and Katwa II CD Block, in Bardhaman district across the Bhagirathi, in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Phulia is located at . Santipur CD Block is bounded by Nabadwip and Krishnanagar I CD Blocks in the north, Ranaghat I CD Block in the east, Balagarh CD Block in Hooghly district, across the Hooghly River, in the south, and Kalna I and Kalna II CD Blocks in Bardhaman district, across the Hooghly River, in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Kaliganj is located at . Kaliganj CD Block is bounded by Beldanga II CD Block, in Murshidabad district, in the north, Tehatta II and Nakashipara CD Blocks in the east, Katwa II CD Block, in Bardhaman district across the Bhagirathi, in the south and Katwa I and Ketugram II CD Blocks, in Bardhaman district across the Bhagirathi, in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

View of the Thar Desert The Thar Desert extends between the Aravalli Hills in the north-east, the Great Rann of Kutch along the coast and the alluvial plains of the Indus River in the west and north-west. Most of the desert area is covered by huge shifting sand dunes that receive sediments from the alluvial plains and the coast. The sand is highly mobile due to strong winds occurring before the onset of the monsoon. The Luni River is the only river integrated into the desert.

Psoralidium lanceolatum. Integrated Taxonomic Information System (ITIS). Great Sand Dunes National Park, Colorado USA It is native to western North America from central Canada to California to Texas, where it grows in sandy habitat, such as alluvial plains and sagebrush.Laedeania lanceolata.

Irrigation is strongly dependent on the river's baseflow. Such irrigated agriculture is important in meeting the demands for food security and poverty reduction. Irrigated lands are established in the lower alluvial plains of Korowya River, and near springs at the headwaters.

Krishnaganj police station serves this block. Headquarters of this CD Block is at Majhdia. It is located 24 km from Krishnanagar, the district headquarters. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi.

The forest contains the Caquetá River's alluvial plains, their upland terraces, a sedimentary plain from the Tertiary and sandstone table mountains from the Paleozoic that rise to elevations of over . Some soils are rich in nutrients and others are poor.

Murutia, a constituent village in Karimpur II CD Block, is located at . (presently police station) Karimpur II CD Block is bounded by Karimpur I CD Block, in the north, Daulatpur Upazila in Kushtia District and Gangni Upazila in Meherpur District of Bangladesh in the east, Tehatta I and Tehatta II CD Blocks in the south and Naoda CD Block, in Murshidabad district, in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

Chakdaha is located at . Chakdaha CD Block is bounded by Ranaghat I and Ranaghat II CD Blocks in the north, Bangaon CD Block, in North 24 Parganas district, in the east, Haringhata CD Block and Kanchrapara, Halisahar and Barrackpore I CD Block, in the North 24 Parganas district, in the south and Chinsurah-Mogra CD Block in Hooghly district, across the Hooghly River, in the west. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi. The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati.

A small city located near the coast, Foro was built at the confluence of the Haddas, Aligide and Comaile rivers. In the 1960s, there was significant agricultural development on its alluvial plains. The Aksumite ruins of Adulis are situated about to the east.

Besides springs and reservoirs, irrigation is strongly dependent on the river’s baseflow. Such irrigated agriculture is important in meeting the demands for food security and poverty reduction. Irrigated lands are established in the narrow alluvial plains along the river in several places.

The river system has a number of spectacular waterfalls, including the Jim Jim Falls on Jim Jim Creek and the Twin Falls on Twin Falls Creek. The rivers have created the alluvial plains, including the mangrove swamps, in the past 20,000 years.

Bishnupur is located at . It has an average elevation of 59 metres (194 feet). This area has fertile, low -lying alluvial plains. It is a predominantly rural area with 90.06% of the population living in rural areas and only 8.94% living in the urban areas.

Soluri, Banana Culture pp. 43-45.Mario Argueta Banana y politica: Samuel Zemurray y la Cuyamel Fruit Company, pp. 24-37 After the first concessions in 1912, US concerns achieved more or less complete control of the productive alluvial plains of Honduras' Atlantic coast.

Durgapur is located at . It has an average elevation of . Map of Paschim Bardhaman district Durgapur is in the Paschim Bardhaman district of West Bengal, on the bank of the Damodar River, just before it enters the alluvial plains of Bengal. The topography is undulating.

Besides springs and reservoirs, irrigation is strongly dependent on the river's baseflow. Such irrigated agriculture is important in meeting the demands for food security and poverty reduction. Irrigated lands are established in the narrow alluvial plains all along the river and pump irrigation is used.

The Bagri or eastern half belongs to alluvial plains of eastern Bengal. There are few permanent swamps; but the whole country is low-lying, and liable to annual inundation. In the north-west are a few small detached hillocks, said to be of basaltic formation.

It then extends southeast into northern Bolivia and in a narrow band south along the base of the Andes Mountains. Elevations range from in the west to on the eastern edge of the region. Landforms present in this region include the upland terra firme (non-flooded) mostly on nutrient-poor lateritic soils, ancient alluvial plains (mostly non-flooded) on nutrient-rich soils, and present alluvial plains (várzea, seasonally flooded) of super-rich sediments renewed with each annual flood. Floristically, distinct lowland humid forest types occur on each of these landforms with the terra firme mature forests and late successional, seasonally flooded forest being the two major types.

Dera Bhattian is part of the alluvial plains between the Himalayan foothills and the central core of the Indian subcontinent. The alluvial deposits are typically over a thousand feet thick. The interfluves are believed to have been formed during the Late Pleistocene and feature river terraces.

Semi-arid districts; on red sandy soils, sand rises and dunes. Occurs on sandplains and low sandy rises, dunefields, fertile alluvial plains, Mulga-dominated red earth plains, intermittent watercourses and run-on areas, and rocky or gravelly ranges, hills or rises composed of neutral or acidic rocks.

Hugli-Chuchura is located at . This city is on the flood plain on the right bank of river Bhagirathi-Hooghly. The area is composed of flat alluvial plains that forms part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised.

Besides springs and reservoirs, irrigation is strongly dependent on the river's baseflow. Such irrigated agriculture is important in meeting the demands for food security and poverty reduction. Irrigated lands are established in the narrow alluvial plains all along the river, mainly through use of pump irrigation.

Iris spuria grows on seasonally damp grasslands, damp meadows (or pastures), marshes, alluvial plains, swamps, bogs, maquis, and salty flats. It also grows in saline soils. Wild Iris Spuria in Behbahan It can be found naturalised in damp, grassy places, by ditches, on banks and on roadside verges.

Subbhabhumi was a part of Rarh in ancient times. It is located in what is now Birbhum district in the Indian state of West Bengal. The more fertile eastern part of the district, consisting of alluvial plains, was known as Subbhabhumi.O,Malley, L.S.S., Bengal District Gazetteers - Birbhum, Govt.

It typically grows in deciduous or mixed deciduous woods, as well as on slopes or alluvial plains. Basic to neutral soils are usually preferred. Its flower heads emerge in the late summer to early fall and show white to lavender rays with pale yellow centres sometimes tinged with purple.

The map alongside shows the Bishnupur subdivision of Bankura district. Physiographically, this area has fertile low lying alluvial plains. It is a predominantly rural area with 90.06% of the population living in rural areas and only 8.94% living in the urban areas. It was part of the core area of Mallabhum.

Mersin Province is a Mediterraneran province of Turkey. The south eastern plain of the province is a part of Çukurova (or historically Cilicia Pedias ). But most of the province is mountainous with a number of small alluvial plains at the coastal band. Below are the transport facilities of the province.

The Chatra Gorge is about 10 km long and is about 5–8 km wide. Downstream of the gorge, the river enters the alluvial plains forming a huge megafan covering around 16,000 km2. The gorge is located at . The initial or northern portion of the gorge is at an altitude of .

The highland areas feature alpine grasslands, jagged bare peaks, montane forests, rainforests, fast-flowing rivers, and gorges. Swamps and low-lying alluvial plains with fertile soil dominate the southeastern section around the town of Merauke. Swamps also extend around the Asmat region. The rugged and hilly topography of Western New Guinea.

The most striking feature of Japanese agriculture is the shortage of farmland. The under cultivation constituted just 13.2% of the total land area in 1988. However, the land is intensively cultivated. Rice paddies occupy most of the countryside, whether on the alluvial plains, the terraced slopes, or wetlands and coastal bays.

Dome-like rounded mogotes in Viñales Valley, Cuba A mogote () is a generally- isolated steep-sided residual hill composed of either limestone, marble, or dolomite. Mogotes are surrounded by nearly flat alluvial plains. The hills typically have a rounded, tower-like form. Several mogotes along a ridge are called pepinos.

The map alongside shows the Bishnupur subdivision of Bankura district. Physiographically, this area has fertile low lying alluvial plains. It is a predominantly rural area with 90.06% of the population living in rural areas and only 8.94% living in the urban areas. It was a part of the core area of Mallabhum.

Samudragarh is located on the agriculturally rich alluvial plains between the Bhagirathi, Ajay and Damodar rivers.Chattopadhyay, Akkori, Bardhaman Jelar Itihas O Lok Sanskriti (History and Folk lore of Bardhaman District.), , Vol I, p. 15, Radical Impression. Temperatures in this region varies from 17-18 °C in winter to 30-32 °C in summer.

The map alongside shows the Bishnupur subdivision of Bankura district. Physiographically, this area has fertile low lying alluvial plains. It is a predominantly rural area with 90.06% of the population living in rural areas and only 8.94% living in the urban areas. It was a part of the core area of Mallabhum.

In Siberia, an area containing a high density of close system pingos can be found near Yakutsk located on the Lena River. In this area there are more than 500 pingos next to the Lena River. The area consists of alluvial plains areas of thick permafrost, allowing pingos to form and develop.

Honduras' topography. Honduras has three distinct topographical regions: an extensive interior highland area and two narrow coastal lowlands. The interior, which constitutes approximately 80 percent of the country's terrain, is mountainous. The larger Caribbean lowlands in the north and the Pacific lowlands bordering the Gulf of Fonseca are characterized by alluvial plains.

Purbasthali is located on the agriculturally rich alluvial plains between the Bhagirathi, Ajay and Damodar rivers.Chattopadhyay, Akkori, Bardhaman Jelar Itihas O Lok Sanskriti (History and Folk lore of Bardhaman District.), , Vol I, p. 15, Radical Impression. Temperatures in this region varies from 17-18 °C in winter to 30-32 °C in summer.

Kulihanda is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Keota, Manushpur, Naldanga, Kodalia, Kulihanda, Dharmapur and Simla form a cluster of census towns on the eastern side of Hugli-Chuchura.

Kodalia is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Keota, Manushpur, Naldanga, Kodalia, Kulihanda, Dharmapur and Simla form a cluster of census towns on the eastern side of Hugli-Chuchura.

Dharmapur is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Keota, Manushpur, Naldanga, Kodalia, Kulihanda, Dharmapur and Simla form a cluster of census towns on the eastern side of Hugli-Chuchura.

The western and northern portions of the state are part of the Chota Nagpur plateau. The coasts composed of fertile alluvial plains and the valleys of the Mahanadi, Brahmani, and Baitarani rivers, which empty into the Bay of Bengal. 31.41% of Odisha has forest cover. There are many wildlife sanctuaries in Odisha.

Manushpur is located at . Keota, Manushpur, Naldanga, Kodalia, Kulihanda, Dharmapur and Simla form a cluster of census towns on the eastern side of Hugli-Chuchura. The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised.

Dhatrigram is located on the agriculturally rich alluvial plains between the Bhagirathi, Ajay and Damodar rivers.Chattopadhyay, Akkori, Bardhaman Jelar Itihas O Lok Sanskriti (History and Folk lore of Bardhaman District.), , Vol I, p. 15, Radical Impression. Temperatures in this region varies from 17-18 °C in winter to 30-42 °C in summer.

Keota is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Keota, Manushpur, Naldanga, Kodalia, Kulihanda, Dharmapur and Simla form a cluster of census towns on the eastern side of Hugli-Chuchura.

Naldanga is located at . Keota, Manushpur, Naldanga, Kodalia, Kulihanda, Dharmapur and Simla form a cluster of census towns on the eastern side of Hugli-Chuchura. The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised.

The alluvial plains are cut across by such distributaries as Jalangi, Churni and Ichhamati. With these rivers getting silted up, floods are a recurring feature.Gangopadhyay, Basudev, Paschimbanga Parichay, 2001, , p. 70, Sishu Sahitya Sansad Gram panchayats of Krishnaganj block/ panchayat samiti are: Bhajanghat Tungi, Gobindapur, Joyghata, Krishnaganj, Matiary Banpur, Shibnibas and Taldah Majdia.

Diversion dam on Genfel for irrigation near Wukro Besides springs and reservoirs, irrigation is strongly dependent on the river's baseflow. Such irrigated agriculture is important in meeting the demands for food security and poverty reduction. Irrigated lands are established in the narrow alluvial plains along the river, particularly up- and downstream of Wukro.

Simla is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Keota, Manushpur, Naldanga, Kodalia, Kulihanda, Dharmapur and Simla form a cluster of census towns on the eastern side of Hugli-Chuchura.

They are found on level and slightly sloping alluvial plains, terraces and gently sloping piedmont plains in arid, semi-arid and Mediterranean regions. The soils have AC or ABC profile. Eroded Durisols with exposed hard horizons (a petroduric horizon) are common in (gently) sloping terrain. Most Durisols can only be used for extensive grazing.

Uttar Goara is located on the agriculturally rich alluvial plains between the Bhagirathi, Ajay and Damodar rivers.Chattopadhyay, Akkori, Bardhaman Jelar Itihas O Lok Sanskriti (History and Folk lore of Bardhaman District.), , Vol I, p. 15, Radical Impression. Temperatures in this region varies from 17-18 °C in winter to 30-32 °C in summer.

The Dhaniakhali CD Block is part of the Hooghly-Damodar Plain, one of the three natural regions in the district of the flat alluvial plains that forms part of the Gangetic Delta. The region has many depressions which receive water from the surrounding lands during the rainy season and discharge the water through small channels.

They have their own specific type of plant and animal populations. The next phase is erosion—which the drainage simulates. Rivers are created by tracing their paths from the mountains (which get eroded) to its end which is usually an ocean; some form into lakes. The salinity field defines oceans, mangroves or alluvial plains.

Hatsimla is located at . Hatsimla is also shown in the map of Purbasthali I CD block in the District Census Handbook. Hatsimla is located on the agriculturally rich alluvial plains between the Bhagirathi, Ajay and Damodar rivers.Chattopadhyay, Akkori, Bardhaman Jelar Itihas O Lok Sanskriti (History and Folk lore of Bardhaman District.), , Vol I, p.

This contains plant and animal material collected over centuries. The morass can be mined as peat, an excellent source of energy. The marsh serves as a natural and unique sanctuary for a wide variety of Jamaican wildlife and birds. The remaining area consists of several hills of moderate elevation, and alluvial plains along the coast.

The Singur CD Block is part of the Hooghly-Damodar Plain, one of the three natural regions in the district, of the flat alluvial plains that forms part of the Gangetic Delta. The region has many depressions which receive water from the surrounding lands during the rainy season and discharge the water through small channels.

Northern Territory Flora online, Northern Territory Government. Retrieved 11 May 2019. The species is found on the edges of swamps and creek beds and damp flats in the Kimberley region of Western Australia where it grows in sandy-loam soils. In the Territory it is found on mulga-dominated plains, alluvial plains and intermittent watercourses.

Fareed Gate Alluvial plains form much of the immediate region around Bahawalpur. The main crops for which Bahawalpur is recognised are cotton, sugarcane, wheat, sunflower seeds, rape/mustard seed and rice. Bahawalpur mangoes, citrus, dates and guavas are some of the fruits exported out of the country. Vegetables include onions, tomatoes, cauliflower, potatoes and carrots.

Pandua CD Block is part of the Hooghly-Damodar Plain, one of the three natural regions in the district of the flat alluvial plains that forms part of the Gangetic Delta. The region has many depressions which receive water from the surrounding lands during the rainy season and discharge the water through small channels.

Smith's vole lives in forests, plantations and farmland in montane areas above about 400 metres. It is absent from alluvial plains. It makes burrows in leaf litter and prefers damp conditions. It is a common species in chosen habitat but some of its populations are fragmented by road development, land reclamation, dam building and deforestation.

The Jangipara CD Block is part of the Hooghly- Damodar Plain, one of the three natural regions in the district of the flat alluvial plains, that forms part of the Gangetic Delta. The region has many depressions which receive water from the surrounding lands during the rainy season and discharge the water through small channels.

The Haripal CD Block is part of the Hooghly-Damodar Plain, one of the three natural regions in the district of the flat alluvial plains that form a part of the Gangetic Delta. The region has many depressions which receive water from the surrounding lands during the rainy season and discharge the water through small channels.

The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Hansghara, Kola, Gajaghanta, Alikhoja, Amodghata, Shankhanagar and Chak Bansberia form a cluster of census towns on the eastern side of Bansberia and includes Mogra and Bara Khejuria (outgrowth).

The Tehsil of Tandlianwala is part of the alluvial plains between the Himalayan foothills and the central core of the Indian subcontinent. The alluvial deposits are typically over 1000 thick.Geology Study of Pakistan: Study Area and Sampling. hec.gov.pk The scalloped interfluves are believed to have been formed during the Late Pleistocene and feature flat-topped river terraces.

Kondopozhsky District covers the forested lake area to the northwest of Lake Onega. The terrain is a combination of lakes, rocky ridges, glacial moraines, and glacial alluvial plains. The lakes and rivers are oriented northwest to southeast to flow into Lake Onega, and eventually into the Baltic Sea. The Kivach Nature Reserve is located in the District.

The reserve lies at the confluence of the arid and semi-arid zones. It contains strips of River Red Gum forest and Black Box floodplain woodlands along the Murray and its associated wetlands. Much of the rest of the property consists of flat alluvial plains with mallee woodlands, chenopod shrublands, semi-arid grasslands and ephemeral lignum wetlands.

Shankhanagar is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Hansghara, Kola, Alikhoja, Amodghata, Shankhanagar and Chak Bansberia form a cluster of census towns on the eastern side of Bansberia and includes Mogra and Bara Khejuria (outgrowth).

The Chanditala II CD Block is part of the Hooghly- Damodar Plain, one of the three natural regions in the district of the flat alluvial plains, that form a part of the Gangetic Delta. The region has many depressions which receive water from the surrounding lands during the rainy season and discharge the water through small channels.

Nabagram Colony is located at . It has an average elevation of . Rishra (CT), Bamunari, Nawapara, Nabagram Colony, Kanaipur , Basai and Raghunathpur (PS- Dankuni) form a cluster of census towns on the eastern side of the series of statutory towns/ cities – Rishra, Konnagar and Uttarpara. The area consists of flat alluvial plains, that form a part of the Gangetic Delta.

Bamunari is located at . Rishra (CT), Bamunari, Nawapara, Nabagram Colony, Kanaipur , Basai and Raghunathpur (PS-Dankuni) form a cluster of census towns on the eastern side of the series of statutory towns/ cities – Rishra, Konnagar and Uttarpara. The area consists of flat alluvial plains, that form a part of the Gangetic Delta. This belt is highly industrialised.

Bansberia is located at . The area is composed of flat alluvial plains that forms part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Hansghara, Kola, Alikhoja, Amodghata, Shankhanagar and Chak Bansberia form a cluster of census towns on the eastern side of Bansberia and includes Mogra and Bara Khejuria (outgrowth).

Amodghata is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Hansghara, Kola, Alikhoja, Amodghata, Shankhanagar and Chak Bansberia form a cluster of census towns on the eastern side of Bansberia and includes Mogra and Bara Khejuria (outgrowth).

The ecoregion covers upland alluvial plains formed in the Tertiary period. The terrain includes floodplains, rolling hills, steep banks and plateaus. Elevations are typically from , but in Colombia the sandstone plateaus rise to . The Putumayo River, which defines the border between Peru and Colombia, runs through the region, which is also drained by the Caquetá, Napo and Solimões.

Alikhoja is located at . Hansghara, Kola, Alikhoja, Amodghata, Shankhanagar and Chak Bansberia form a cluster of census towns on the eastern side of Bansberia and includes Mogra and Bara Khejuria (outgrowth). The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised.

Hansghara is located at . Hansghara, Kola, Alikhoja, Amodghata, Shankhanagar and Chak Bansberia form a cluster of census towns on the eastern side of Bansberia and includes Mogra and Bara Khejuria (outgrowth). The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised.

Kola is located at . Hansghara, Kola, Alikhoja, Amodghata, Shankhanagar and Chak Bansberia form a cluster of census towns on the eastern side of Bansberia and includes Mogra and Bara Khejuria (outgrowth). The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised.

Rishra (CT) is located at Rishra (CT), Bamunari, Nawapara, Nabagram Colony, Kanaipur , Basai and Raghunathpur (PS-Dankuni) form a cluster of census towns on the eastern side of the series of statutory towns/ cities – Rishra, Konnagar and Uttarpara. The area consists of flat alluvial plains, that form a part of the Gangetic Delta. This belt is highly industrialised.

The Chanditala I CD Block is part of the Hooghly- Damodar Plain, one of the three natural regions in the district of the flat alluvial plains, that forms part of the Gangetic Delta. The region has many depressions which receive water from the surrounding lands during the rainy season and discharge the water through small channels.

Besides springs and reservoirs, irrigation is strongly dependent on the river’s baseflow. Such irrigated agriculture is important in meeting the demands for food security and poverty reduction. Irrigated lands are established in the narrow alluvial plains along the river in Rubaksa, and additional gardens have been installed in the lower gorge through the May Zegzeg project.

The catchment area of the lake occupies approximately . A large proportion has been cleared for agricultural purposes. The landscape is composed of lakes and swamps with small lunettes, alluvial plains, swales and dunes on alluvial and aeolian deposits in the Beaufort River and upper Blackwood River catchment. The lake is located along an ancient drainage line.

This term is used for hills, isolated or linked, with very steep, almost vertical, walls, surrounded by alluvial plains in the tropics, regardless or not the carbonate strata in which they have formed is folded.Neuendorf, K. K. E., J. P. Mehl, Jr., and J. A. Jackson, 2005, Glossary of Geology, 5th ed. American Geological Institute, Alexandria, Virginia. 779 p.

250px Atakent is a Mediterranean coastal town in Silifke district which itself is a part of Mersin Province. Alluvial plains of Silifke lie in the west of the town and hilly coastline is in the east of the town. The town is on the D 400 highway. The distance to Mersin is and to Silifke is .

The Polba Dadpur CD Block is part of the Hooghly- Damodar Plain, one of the three natural regions in the district of the flat alluvial plains that forms part of the Gangetic Delta. The region has many depressions which receive water from the surrounding lands during the rainy season and discharge the water through small channels.

The good natural fertility of most fluvisols and their attractive dwelling sites on river levees and higher parts in marine landscapes were recognized in prehistoric times. Fluvisols are found on alluvial plains, river fans, valleys and tidal marshes on all continents and in all climate zones. Under natural conditions periodical flooding is fairly common. The soils have a clear evidence of stratification.

The homestead is situated on the southern block. This block consists of the broad alluvial plains of Turee Creek flanked by hardpan plains. The northern block is made up of a narrow river valley flanked by jagged hills and undulating plains. The station was owned by Piesse and Maguire in 1932 who were trading in bullocks to the sale yards in Meekatharra.

Badhagachhi is located at The Balagarh CD Block is mostly part of the Hooghly Flats, one of the three natural regions in the district of the flat alluvial plains that form a part of the Gangetic Delta. The region is a narrow strip of land along the 80 km long stretch of the Hooghly River, that forms the eastern boundary of the district.

Bari Brahmana is located at .Falling Rain Genomics, Inc - Bari Brahmana It has an average elevation of 340 metres (1115 feet). The city is just south of Jammu Tawi city and is situated on the banks of Devika river at a flat alluvial plains on the foot hills of the Shiwaliks which surround it on the East and North-east.

Besides springs and reservoirs, irrigation is strongly dependent on the river’s baseflow. Such irrigated agriculture is important in meeting the demands for food security and poverty reduction. Irrigated lands are established in the narrow alluvial plains all along the river, mostly using pump irrigation. Very often tropical fruits are grown in these gorges as the climate is warmer than the overall surrounding highlands.

Other habitats are brackish or salt lagoons, brackish herbaceous swamps, swamp woods and swamp forests. The swamps are a source of fresh water to the mangroves. The alluvial plains in the northwest have different characteristics. The San Juan delta has swamps with marine- fluvial sediment deposits, the Gulf of Paria has marine sediments and the Orinoco delta has mainly fluvial sediments.

Badulia is at an average elevation of 35 meters. It lies to the south of the Damodar River, on the alluvial plains between the Damodar and the Dwarakeswar River rivers. As a result, it has been a flood- prone area.Chattopadhyay, Akkori, Bardhaman Jelar Itihas O Lok Sanskriti (History and Folk lore of Bardhaman District.), , Vol I, pp15-18, Radical Impression.

The Rewa Plateau covers a portion of Rewa district in the Indian state of Madhya Pradesh. The Rewa Plateau lies between the Kaimur Range in the south and Vindhya Range or Binj Pahar in the north. To the north of the Binj Pahar are the alluvial plains known as Uprihar. The plateau covers the Huzur, Sirmaur and Mauganj tehsils of Rewa district.

The Balochistan Plateau lies in the west and the Thar Desert in the east. The Indus River and its tributaries flow through the country from the Kashmir region to the Arabian Sea. There is an expanse of alluvial plains along it in the Punjab and Sindh. The climate varies from tropical to temperate, with arid conditions in the coastal south.

Chak Bansberia is located at . The area is composed of flat alluvial plains that form a part of the Gangetic Delta. The high west bank of the tidal Hooghly River is highly industrialised. Hansghara, Kola, Alikhoja, Amodghata, Shankhanagar and Chak Bansberia form a cluster of census towns on the eastern side of Bansberia and includes Mogra and Bara Khejuria (outgrowth).

Camden white gum grows on alluvial plains on sand or loam over clay along the Nepean River and its tributaries, in tall open forest, where it either forms a pure stand or is found with other eucalypts such as mountain blue gum (E. deanei) and river peppermint (E. elata). Other associated trees include grey box (E. moluccana), forest red gum (E.

A major portion of Chandannagore subdivion is part of the Hooghly-Damodar Plain, the agriculturally rich alluvial plains lying between the Hooghly and the Damodar. The narrow strip of land along the Hooghly is part of the Hooghly Flats. The entire area is a part of the Gangetic Delta. The Hooghly is a tidal river and has a high west bank.

The catchment area of the Sabarmati basin is out of which lies in Rajasthan State and the remaining in Gujarat. The basin is located in a semi-arid zone with rainfall ranging from in different parts of the basin. The river traverses three geomorphic zones: rocky uplands, middle alluvial plains, and lower estuarine zone. The major tributaries are the Watrak, Wakal, Hathmati, Harnav, and Sei rivers.

A. mollifolia is endemism to the central tablelands and central western slopes of New South Wales with the bulk of the population found to the west of Peakhill, Boorowa and Bathurst areas to around Rankins Springs where it is often situated on sandstone ridges and on alluvial plains a part of dry sclerophyll forest or woodland communities dominated by species of Eucalyptus and Callitris.

The area consists of two different tracts. The western portion marks the gradual descent from the table land of Chota Nagpur to the delta of lower Bengal, consisting largely of spurs projecting from the western tableland and of low swelling ridges. However, there is no marked ridge of hills. In the central portion of the district there are rolling downs eventually merging with the alluvial plains.

Terminalia fitzgeraldii is a tree of the family Combretaceae native to Western Australia. The tree typically grows to a height of in height but can reach up to and is deciduous. It blooms between July and December producing white- yellow flowers. It is found in rocky creek beds and on alluvial plains in the Kimberley region of Western Australia growing in lateritic clay soils.

Kankar or kunkur is a sedimentological term derived from Hindi, occasionally applied in India and the United States to detrital or residual rolled, often nodular calcium carbonate formed in soils of semi-arid regions. It forms sheets across alluvial plains and can occur as discontinuous lines of nodular kankar or as indurated layers in stratigraphic profiles more commonly referred to as calcrete, hardpan or duricrust.

The features of the landscape include alluvial plains, small lunettes, dunes and swales on alluvial and aeolian deposits. The lake is situated along a major ancient drainage line. The catchment has an average annual rainfall of and an annual evaporation of . The northern shore of the lake is part of a crown reserve with an area of designated for the protection of native fauna and flora.

The terrain is flat, mostly about above sea level but rising to in levees along the coast. Soils are almost all alluvial deposits, carried from the Andes far to the west. The coastline of the delta moves east into the Atlantic ocean by about annually. The delta region has many large and small distributary rivers and streams, permanent wetlands and marshes, oxbow lakes, levees and alluvial plains.

Anserimimus was recovered from the Nemegt Formation of Mongolia. The Nemegt is thought to represent alluvial plains containing meandering rivers. The layer Anserimimus was found, is dating from the early Maastrichtian stage of the Late Cretaceous, or about 70 million years ago. Aside from Gallimimus, other theropods found in the Nemegt Formation include the gigantic Tarbosaurus and Deinocheirus, as well as smaller dromaeosaurids, oviraptorosaurs, troodontids, and birds.

Sripur is located at . The Balagarh CD Block is mostly part of the Hooghly Flats, one of the three natural regions in the district composed of the flat alluvial plains that form a part of the Gangetic Delta. The region is a narrow strip of land along the 80 km long stretch of the Hooghly River, that forms the eastern boundary of the district.

Mirdhanga is located at . The Balagarh CD Block is mostly part of the Hooghly Flats, one of the three natural regions in the district composed of the flat alluvial plains that form a part of the Gangetic Delta. The region is a narrow strip of land along the 80 km long stretch of the Hooghly River, that forms the eastern boundary of the district.

The city has an urban area of , while together with its metropolitan area it covers . On the right bank of the Sava, central Belgrade has a hilly terrain, while the highest point of Belgrade proper is Torlak hill at . The mountains of Avala () and Kosmaj () lie south of the city. Across the Sava and Danube, the land is mostly flat, consisting of alluvial plains and loessial plateaus.

Ben Lugmore's geology is what is known as the Mweelrea Formation, and is very different from that of the Twelve Bens, on the other side of Killary Harbour. At a summary level, the Mweelrea Formation consists of Ordovician period sandstones originally deposited on large alluvial fans, and distally‐equivalent alluvial plains and delta fans. Interbedded with these sandstones are tufts, being ash deposits from Ordovician period volcanos.

The geology of what is known as the Mweelrea Formation is very different from that of the Twelve Bens, on the other side of Killary Harbour. At a summary level, the Mweelrea Formation consists of Ordovician period sandstones originally deposited on large alluvial fans, and distally‐equivalent alluvial plains and delta fans. Interbedded with these sandstones are tufts, being ash deposits from Ordovician period volcanos.

The district of Faisalabad is part of the alluvial plains between the Himalayan foothills and the central core of the Indian subcontinent. The alluvial deposits are typically over a thousand feet thick. The interfluves are believed to have been formed during the Late Pleistocene and feature river terraces. These were later identified as old and young floodplains of the Ravi River on the Kamalia and Chenab Plains.

Colorado has an area of km² which corresponds to about 48% of the cantonal area and an elevation of metres. Within the limits of the district is the Calero Island (151.6 km², the largest in the country). Another important and near fluvial island is the Brava Island (44.4 km²). The territory of the district is a continuation of the alluvial plains of the north of the country.

Balagarh is located at . The Balagarh CD Block is mostly part of the Hooghly Flats, one of the three natural regions in the district composed of the flat alluvial plains that form a part of the Gangetic Delta. The region is a narrow strip of land along the 80 km long stretch of the Hooghly River, that forms the eastern boundary of the district.

Unlike the rest of Bardhaman district, which lies to the north of the Damodar River, the Khandaghosh- Jamalpur-Raina area lies on the alluvial plains between the Damodar on its southern/ eastern side and the Dwarakeswar River. As a result, it has been a flood prone area.Chattopadhyay, Akkori, Bardhaman Jelar Itihas O Lok Sanskriti (History and Folk lore of Bardhaman District.), , Vol I, pp. 15–18, Radical Impression.

Altitudes range from . Hilly and mountainous with large alluvial plains and some low tabular plateaus. Separating the two basins of Rio Ucayali (Peru) and Juruá (Brazil), the Park shelters main sources of Jurua 's left margin affluent. It is structured in four main hill massifs (Serras da Jaquirana, do Moa, do Jurua-Mirim & do Rio Branco), separated by flat plains and valleys of the corresponding affluent of the Juruá basin.

The longest distance from east to west is 63 km and from north to south is 74 km. From the mountain areas downwards, the land falls in altitude in the stages of mountains, alleys, alluvial plains, lowlands, swamps, sand hills and finally coastline. Yilan's Toucheng Township includes Guishan Island and Guiluan Island. The Senkaku Islands, known in Mandarin as the Diaoyu Islands, are claimed as part of the township.

The area consists of Aichi, Mie, Shizuoka, and southern Gifu prefectures. A number of small alluvial plains are found in the corridor section. A mild climate, favorable location relatively close to the great metropolitan complexes, and availability of fast transportation have made this area a center for truck- gardening and out-of-season vegetables. Upland areas of rolling hills are extensively given over to the growing of mandarin oranges and tea.

Agriculture contributes a major role to the economy of the municipality of Nabua given its vast alluvial plains. Its agricultural contribution consists of crop production, livestock, and fishery. Crop production is more intense rather than livestock and fishery. Rice production, both irrigated and non-irrigated occupies about 87.26% of the total agricultural land devoted to crop production while corn and other types of crops occupies merely 7.96% and 4.78% respectively.

Joypur jungle Bankura district has been described as the “connecting link between the plains of Bengal on the east and Chota Nagpur plateau on the west.” The areas to the east and north-east are low lying alluvial plains, similar to predominating rice lands of Bengal. To the west the surface gradually rises, giving way to undulating country, interspersed with rocky hillocks. Much of the country is covered with jungles.

The City Municipality of Novi Sad is situated in the southern part of the Bačka region. Total area of City of Novi Sad is 699 km², and the area of the city municipality is 671.8 km². Municipality lies in one of the southern lowest parts of the Pannonian Plain. Alluvial plains along Danube are well formed, especially on the left bank, in some parts 10 km from the river.

Amburla Station is a pastoral lease that operates as a cattle station in Northern Territory, Australia. The property is situated approximately north of Hermannsburg and west of Alice Springs. Amburla occupies an area of . The most productive area of the property are the Mitchell grass plains at the foot of Mount Hay and the relict alluvial plains of the floodout areas of Amburla, Charley and 16 mile Creeks.

It affects mainly ungulates, but also carnivores and humans. As anthrax inhibits blood clotting, the blood of deceased animals seep into the soil. The spores survive for decades in substrates with elevated calcium content or neutral-to-alkaline pH levels. The immediate vicinity of Shingwedzi camp contains some riparian vegetation with large trees, and narrow alluvial plains created by centuries of flooding, flank the river on each side.

The coast in this ecoregion is a series of alluvial plains separated by ridges extending down from the Annamite Range on the west. The separating hills rise to 1,000 meters, and are typically granite or rhyolite. The region stretches for 750 km from Da Nang in the north to the edge of the Mekong River delta in the south, and averages about 50 km wide. Mean elevation is 200 meters.

Dams have been built on the Middle and Upper Geum to facilitate water for agriculture and industry. They include the Daecheong Dam and the Yongdam Dam. The city of Greater Daejeon and the farms and industries of South Chungcheong Province rely heavily on the Geum River and its tributaries. The alluvial plains formed by the Geum and its tributaries are the locations of significant agricultural production in Korea.

Lower ranges of hills run parallel to the mountains. The Lower Himalayan Range runs from north of Rawalpindi through Jammu and Kashmir, Himachal Pradesh, and further south. The mountains are relatively young, and are eroding rapidly. The Indus and the five rivers of the Punjab have their sources in the mountain range and carry loam, minerals and silt down to the rich alluvial plains, which consequently are very fertile.

Downstream from the Yanguo Gorge, the provincial capital of Lanzhou is built upon the Yellow River's banks. The Yellow River flows northeasterly out of Gansu and into Ningxia before the Qingtong Gorge. After emerging from the Qingtong Gorge, the river comes into a section of vast alluvial plains, the Yinchuan Plain and Hetao Plain. In this section, the regions along the river are mostly deserts and grasslands, with very few tributaries.

200px Located west of St. Louis along the Missouri River, the area is known for its river bottoms and alluvial plains that follow the winding river. The soil in this area is a type of loam known as Hayne Silt-Loam which is heaviest in clay composition in the areas closest to the river but has more silt concentration in the higher elevations where most of the vineyards are now located.

The district head quarter is located in Bankura town. The district has been described as the "connecting link between the plains of Bengal on the east and Chota Nagpur plateau on the west." The areas to the east and north-east are low-lying alluvial plains while to the west the surface gradually rises, giving way to undulating country, interspersed with rocky hillocks.O’Malley, L.S.S., ICS, Bankura, Bengal District Gazetteers, pp.

Rainfall is slightly higher in the San Gabriel Valley than the coastal plain due to its proximity to the mountains. However, the climate as a whole is very arid, with only moderate precipitation in winter and nearly none in summer. The lower watershed essentially consists of alluvial plains that once experienced seasonal flooding from the San Gabriel River, creating vast swamps and wetlands. Today very little of this original environment remains.

The district of Toba Tek Singh is part of the alluvial plains between the Himalayan foothills and the central core of the Indian subcontinent. The alluvial deposits are typically over 1,000 feet thick. The interfluves are believed to have been formed during the Late Pleistocene and feature river terraces. These were later identified as old and young floodplains of the Ravi River on the Kamalia and Chenab Plains.

The Lodgepole Limestone was deposited during the Mississippian, followed by the Madison Group and the Big Snowy Group. The Tyler Formation was deposited in the Pennsylvanian, and consists of interbedded sandstone, siltstone, shale, and limestone. The overlying Minnelusa Formation is characterized by deposition in alluvial plains, prograding river delta, and barrier island environments. The Minnekahta Formation was deposited during the Permian, followed by the Spearfish Formation and the Nesson Formation.

Kanoya is located approximately at the heart of Ōsumi Peninsula with its city limits running approximately east and west and north and south. The Takakuma Mountains stretch out into the northwestern part of the city and the Kimotsuki Mountains in the southeast. Between both mountain ranges lie the Kasanohara and Kanoyahara plateaus. The Kimotsuki Plains spread through the alluvial plains of the Kimotsuki River that runs through central Kanoya.

Irrigation scheme in Upper Gabat Besides springs and reservoirs, irrigation is strongly dependent on the river's baseflow. Such irrigated agriculture is important in meeting the demands for food security and poverty reduction. Irrigated lands are established in the narrow alluvial plains along the river in many places; the farmers use motor pumps to pump baseflow water generated by seepage from Hiza'iti Wedi Cheber, Gereb Segen and Gereb Bi'ati reservoirs.

The Shashe River is a highly ephemeral river, with flow generally restricted to a few days of the year. The river contributes 12.2% of the mean annual runoff of the Limpopo Basin. Major tributaries of the Shashe River include the Simukwe, Shashani, Thuli, Tati and Ramokgwebana rivers. The lower Shashe is a sand filled channel, with extensive alluvial aquifers in the river channel and below the alluvial plains.

Journal of South American Earth Sciences 22(2): 116-129. Amargasuchus inhabited a terrestrial paleoenvironment that existed during the Early Cretaceous in the Neuquén basin that was characterized by a system of braided rivers, lakes, and alluvial plains. Sauropod, abelisauroid, and stegosaurian dinosaurs have also been found existing in the Neuquén basin at this time. The holotype was discovered in 1984 in association with the dicraeosaurid sauropod dinosaur Amargasaurus'.

Kneeling Bull with Vessel. Kneeling bull holding a spouted vessel, Proto-Elamite period, (3100–2900 BC) Metropolitan Museum of Art, ref. 66.173 Proto-Elamite civilization grew up east of the Tigris and Euphrates alluvial plains; it was a combination of the lowlands and the immediate highland areas to the north and east. At least three proto-Elamite states merged to form Elam: Anshan (modern Fars Province), Awan (modern Lorestan Province) and Shimashki (modern Kerman).

Jodhpur district comprises three distinct physiography units, the alluvial plains, sand dunes and escarpments. The western and north-western parts of Jodhpur district are characterized by sand dunes. With exception of some parts of Bilara and Osian tehsil, land surface of the district is nearly flat and sandy. Luni is the only important river in the district, it enters Jodhpur district near Bilara and flows for a distance of over 75 km.

Silver coin of Magadha mahajanapada (c. 350 BCE) The Magadha was one of the most prominent and prosperous of mahajanapadas. The capital city Pataliputra (Patna, Bihar) was situated on the confluence of major rivers like the Ganga, Son, Punpun and Gandak. The alluvial plains of this region and its proximity to the copper and iron rich areas of Bihar and Jharkhand helped the kingdom to develop good quality weapons and support the agrarian economy.

Hsinchu County is located at the northwest part of Taiwan Island. It borders Taoyuan City to the north, Miaoli County to the south, the Taiwan Strait to the west, and Xueshan and Dabajian Mountain to the east. With an area spanning up to , Hsinchu County area composed mainly of uplands, tablelands and mountains, except for the alluvial plains of the Fengshan River and Touqian River mouth area and some ancient river land.

The southern "panhandle" of the country contains large level areas in Savannakhét and Champasak provinces that are well suited for extensive paddy rice cultivation and livestock raising. Much of Khammouan Province and the eastern part of all the southern provinces are mountainous. Together, the alluvial plains and terraces of the Mekong and its tributaries cover only about 20% of the land area. Only about 4% of the total land area is classified as arable.

The two largest parts of the park are the Serranía del Darién mountains, which lie to the west, and the Atrato River floodplains in the east. The floodplains hold exceptionally fertile soil and consist of alluvial plains of two types. One consists of low- lying terraces that flood often and the other has high terraces that seldom flood. There are also low hills of up to in elevation and others that are high.

Map of Bankura District showing CD blocks and municipalities Kotulpur is located at . Kotulpur CD block is located in the eastern part of the district and belongs to the fertile low lying alluvial plains, similar to the predominating rice lands in the adjacent districts of West Bengal. Here, the eye constantly rests on wide expanses of rice fields, green in the rains but parched and dry in summer.O’Malley, L.S.S., ICS, Bankura, Bengal District Gazetteers, pp.

Map of Bankura District showing CD blocks and municipalities Indas is located at . Indas CD block is located in the eastern part of the district and belongs to the fertile low lying alluvial plains, similar to the predominating rice lands in the adjacent districts of West Bengal. Here, the eye constantly rests on wide expanses of rice fields, green in the rains but parched and dry in summer.O’Malley, L.S.S., ICS, Bankura, Bengal District Gazetteers, pp.

The park is famed for its coast redwoods (Sequoia sempervirens), many of which grow to over in height. The forests on alluvial plains are almost pure redwood forest, but the forests on the slopes also contain Douglas-fir. Over 100 of the 137 known trees over tall—all coast redwoods—occur in Humboldt Redwoods State Park. It is home to the 4th-tallest measured living redwood, the Stratosphere Giant, which was measured at in 2004.

Cantalupo is a frazione of Bevagna in the Italian region Umbria located at an elevation of 201 m on the Torrente Attone, a tributary of the Topino River. It is a small farming community in the low alluvial plains of central Umbria; its principal crop is grapes for wine. About 2 km north of the village is the roadside shrine of Pian d' Arca commemorating the miracle of St. Francis of Assisi and the birds.

The Main sector occurs near Acfarcid, with an exposure of ~800 m, recovering the most detritic sector. Along this expossure, the Wazzant member appears at the right lateral, along massive calcareous dolomites, over the Latest Pliensbachian strata, where the lower Toarcian strata is missing. The Wazzant facies never exceed 50 m, getting its maximum exposure at the north of the Guettioua Formation. The facies of the formation follow a deposition typical of Alluvial Plains.

The Tapiche River basin in the area of the reserve exhibits a landscape containing alluvial plains and associated floodplains. The floodplains of the alluvial landscape encompass swamps or aguajales; while the non-flooded plains appear as undulating terraces. There are hilly landscapes within the reserve which appear as gently sloping lowland terrain. Swamps have developed on flat land and in depressions formed by fibric histosol soils with pH values varying between 3.5 and 5.

In Siddha medicine of the Tamils in southern India, Dichrostachys cinerea is called vidathther and used for gonorrhea, syphilis and eczema. As they are rich in nutrients, the plants are often used as fertiliser, particularly in the Sahel region of Africa along riverbanks. The plant is widely used for soil conservation, particularly in India, for shallow soils, and in arid western and subhumid alluvial plains. It is also cultivated as an indoor bonsai specimen.

Chen Yu (), Governor of Guangdong in 1957–1967, was the first to have proposed an underground metro system for Guangzhou. In the summer of 1960, he ordered a secret geological survey of groundwater levels of Guangzhou. Six holes with an accumulated depth of were drilled in the plateaus and alluvial plains in the city. The geological conditions of Guangzhou, despite their complexity, did not preclude the possibility of an underground metro system.

Two of the most interesting are arguably the southern helmeted curassow and the military macaw. Finally, 109 species of fish species have been identified by the IMNA alone, with a clear dependence on altitude. The largest specimens, which are the principal targets of commercial and subsistence fishing - such as sábalo, barred surubim, and pacú - are restricted to the alluvial plains, below 700 m. Above just 1000 m, the fish diversity diminishes dramatically.

The eastern portion of Chinsurah subdivision is part of the Hooghly Flats, a natural physiographic region, that is a narrow strip of land along the Hooghly. The interior of the subdivision is part of the Hooghly-Damodar Plain, the agriculturally rich alluvial plains lying between the Hooghly and the Damodar. The entire area is a part of the Gangetic Delta. The Hooghly is a tidal river and has a high west bank.

The Dugway Range is a 13-mile (21 km) longUtah DeLorme Atlas & Gazetteer, pp. 23, 31. mountain range located in central-south Tooele County, Utah, on the Juab County north border. The Dugway Range extends northwesterly into the south of the Great Salt Lake Desert, the region at the west and southwest of the Great Salt Lake, about three times its area, a region of a flat white, salt flat, flat alluvial plains, and some alluvial mountain range pediments.

A well-marked trail leads from the village of San Bernardino in several stages to the Alpine hut Cassina de Vignun (), where the real Alpine valley begins. The valley rises evenly to the pass of Strec de Vignun (), where it connects to the Val Curciusa. The European Watershed runs across the Strec de Vignun pass. Motta Caslasc The mighty rock Motta Caslasc rises to a height of 2300 m in the middle of the valley, between two alluvial plains.

The landform is composed of a raised plateau that has eroded to form granitic breakaways and the alluvial plains of the surrounding valleys. Acacia woodlands (dominated by Acacia aneura) and shrublands with spinifex grasslands (Triodia basedowii) dominate the vegetation. The area is located toward the inland extreme of two separate weather systems. The main influence on the climate is the east-west belt of high pressure systems which lies over the southern portions of Australia throughout the year.

Fertile valleys are framed by high mountain ridges, creating a scenic landscape. The north of the province adjoins Cao Bằng Province. The Kỳ or Kyu River flows through Lạng Sơn town and alluvial plains are formed in the valley that is surrounded by high mountains of about height. The Kỳ has a basin area of , and has its source in the mountainous area of Bắc Xa at an altitude of in the district of Đình Lập.

To the north lies the Teonther tehsil which is quite different in its physical and other features from the plateau tehsils. The Rewa plateau decreases in height from south to north. In the south, the Kaimur Range rises to more than 450 meters above sea level, whereas the alluvial plain of Teonthor is just 100 meters above sea level. The district has a varied terrain that includes alluvial plains, hills, ravines, scarp, rivers, and water-falls.

Biostratigraphic Series 1. Pretoria, Council for Geoscience. The depositional environment of the Tapinocephalus Assemblage Zone was formed by sedimentary material being deposited in the Karoo Basin (a retro-arc foreland basin) by vast, low-energy alluvial plains flowing northwards from a southerly source area in the rising Gondwanide mountains. The Gondwanides were the result of crustal uplift that had previously begun to take course due to subduction of the Palaeo-pacific plate beneath the Gondwanan Plate.

Basai is located at Note: Basai is not shown in the Google maps. Its location is based on the map published in the District Census Handbook, linked above. Rishra (CT), Bamunari, Nawapara, Nabagram Colony, Kanaipur, Basai and Raghunathpur (PS-Dankuni) form a cluster of census towns on the eastern side of the series of statutory towns/ cities – Rishra, Konnagar and Uttarpara. The area consists of flat alluvial plains, that form a part of the Gangetic Delta.

The most famous scenery in China is found in the karst landscapes of Guangxi and Yunnan provinces. The alluvial Sichuan basin is surrounded by mountains, the Qinling mountains to the north and the Himalaya to the west and southwest. Much of Northeast China, or Manchuria, is dominated by alluvial plains, but the border regions with Korea are also highly mountainous. In the west, most of the Tibetan Plateau is in China, and averages over 4000 metres in elevation.

The Kirthars consist of a series of parallel rock hill ridges oriented mostly north-south, with piedmont and piedmont-alluvial plains located between ridges, with dry riverbeds. The ridges rise rapidly over short distances between valleys and ridges. From the Arabian Sea coast, they rise to nearly in the north. The Kirthars are part of the Kirthar-Sulaiman geologic province, which stretches from the Arabian Sea coast north to northwestern Pakistan along the western boundary of the Indus Valley.

Mondal, Dipanwita, Ek Najare Birbhum Jela, Paschim Banga, Birbhum Special Issue (in Bengali), February 2006, pp. 7–10 Geographically, this area lies at the northeastern end of the Chota Nagpur Plateau, as it slopes down and merges with the alluvial plains of the Ganges. In the district there is only hilly area of natural rock formation situated near Dubrajpur town called Mama Bhagne Pahar (Hill). The western portion of the district is historically known as Vajjabhumi or Bajrabhumi.

The presence of these rocks reveal much about the past environment that they were deposited in. They were formed by sedimentary material being deposited in the Karoo Basin - a retro- arc foreland basin - by vast, low-energy alluvial plains flowing northwards from the south. The lowermost deposits are considered to be deltaic and grade laterally into the underlying Ecca Group deposits in its southern localities. Deposits grade steadily younger in the northeast where the sedimentary facies turn fully terrestrial.

This creeps up into the Wentnor Group where alluvial plains occur latterly with fluvial and alluvial deposits noted in the uppermost (youngest) Bridges Formation.Pharaoh, T. C., Gibbons, W., Precambrian Rocks in England and Wales south of the Menai Strait Fault System, 1987 A Revised Correlation of the Precambrian Rocks in the British IslesW. Compston, A. E. Wright, P. Toghill, "Dating the Late Precambrian volcanicity of England and Wales". 2002, Journal of the Geological Society of London.

The property occupies an area of . The country varies from the alluvial plains flanking the river that support various native grasses to the rugged mountain and dolomite hills that support tall shrubland and spinifex plains. It has an estimated carrying capacity of 4,150 cattle and in 1979 was carrying 1,200 head of cattle. In 1928 Mount Vernon was put up for auction, at this time it occupied an area of and was stocked with 900 cattle and 150 horses.

Map of Bankura District showing CD blocks and municipalities Bishnupur is located at . Bishnupur CD block is located in the north-eastern part of the district and belongs to the fertile low lying alluvial plains, similar to the predominating rice lands in the adjacent districts of West Bengal. Here, the eye constantly rests on wide expanses of rice fields, green in the rains but parched and dry in summer.O’Malley, L.S.S., ICS, Bankura, Bengal District Gazetteers, pp.

Zhongshan is located along the west side of the mouth of the Pearl River, directly opposite Shenzhen and Hong Kong. It lies south of Guangzhou and Foshan and north of Zhuhai and Macau. The northern part of Zhongshan, including most of the urbanized area, lies on the alluvial plains of the Pearl River Delta, while the southern part of the city's territory reaches into a range of coastal hills. The most notable of these are the Wugui Hills ().

Sibu is located near the Rajang delta at the confluence of Rajang and Igan rivers. Peat swamp forests and alluvial plains are particularly prevalent in the Sibu Division. Sibu is located on a deep peat soil, which has caused problems in infrastructure development because buildings and roads slowly sink into the ground after its completion. The location of Sibu in lowland peat swamps have subjected it to frequent floods, about 1 to 3 times per year.

In general humans have not caused adverse impact to the Merriam's kangaroo rat through most of its range. However, in southern California one subspecies, the San Bernardino kangaroo rat, Dipodomys merriami parvus, is at risk due primarily to urban development including construction of dams and alteration of hydrologic regimes throughout its range. Once common on alluvial plains in the washes of San Bernardino and Riverside counties, the United States Fish and Wildlife Service listed the San Bernardino kangaroo rat as endangered in 1998.

Satigachha is located at . The maps of Ranaghat I and Ranaghat II CD blocks, in the District Census Handbook 2011, Nadia, shows the census towns of Kamgachhi, Raghabpur, Panpara, Aistala, Satigachha, Anulia, Halalpur Krishnapur, Hijuli and Ranaghat (CT) forming a cluster around Ranaghat. Certain other localitites such as Nokari, Nasra, Cooper's Camp, Birnagar, Habibpur, Gopalpur and Parbbatipur are also linked with this cluster. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi.

Gopalpur is located at . The maps of Ranaghat I and Ranaghat II CD blocks, in the District Census Handbook 2011, Nadia, shows the census towns of Kamgachhi, Raghabpur, Panpara, Aistala, Satigachha, Anulia, Halalpur Krishnapur, Hijuli and Ranaghat (CT) forming a cluster around Ranaghat. Certain other localitites such as Nokari, Nasra, Cooper's Camp, Birnagar, Habibpur, Gopalpur and Parbbatipur are also linked with this cluster. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi.

However, the land is intensively cultivated. Paddy fields occupy much of the countryside, whether on the alluvial plains, the terraced slopes, or the swampland and coastal bays. Nonrice farmland share the terraces and lower slopes and are planted with wheat and barley in the autumn and with sweet potatoes, vegetables, and dry rice in the summer. Japan's strategy to protect the flooding of its rice market is to offer compensation to those who own land and agree to grow other commodities.

Cooper's Camp is located at . The maps of Ranaghat I and Ranaghat II CD blocks, in the District Census Handbook 2011, Nadia, shows the census towns of Kamgachhi, Raghabpur, Panpara, Aistala, Satigachha, Anulia, Halalpur Krishnapur, Hijuli and Ranaghat (CT) forming a cluster around Ranaghat. Certain other localitites such as Nokari, Nasra, Cooper's Camp, Birnagar, Habibpur, Gopalpur and Parbbatipur are also linked with this cluster. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi.

Low samphire and saltbush shrublands cover the saline alluvial plains, snakewood scrublands cover the clay flats, Bowgada low woodland covers sandy ridges and plains, red sand dune fields are interspersed or overlain with tree to shrub steppe over hummock grasslands, and Acacia startii/A. bivenosa shrublands cover limestone outcrops in the north. Other trees in the area include limestone wattle (Acacia sclerosperma) with an undergrowth of dead finish (Acacia tetragonophylla). The sheltered embayments and extensive tidal flats along the coast support mangroves.

The coast is generally low, and punctuated by the deltas of several large rivers, including the Kaveri, Palar, Penner, and Krishna River, which rise in the highlands of the Western Ghats and flow across the Deccan Plateau to drain into the Bay of Bengal. The alluvial plains created by these rivers are fertile and favour agriculture. The rivers remain dry during most of the year. There is little forest cover, but marshes, swamps, scrub woodlands, and thorny thickets are common.

Srirampore subdivision is the most urbanised, and the one with the highest density of population, of all the subdivisions of Hooghly district. Urbanisation started with industrialisation of the Hooghly Flats, the narrow strip of land along the Hooghly and spread inland covering a large portion of Hooghly-Damodar Plain, the agriculturally rich alluvial plains lying between the Hooghly and the Damodar. The entire area is a part of the Gangetic Delta. The Hooghly is a tidal river and has a high west bank.

Permanent swamp forests are common on the alluvial plains. Pockets of nutrient-poor white sand soils are found here that host forests of lower height, a more open forest canopy, and lower alpha diversity, but with many endemics. The forests are mostly dense tropical rain forest, but some patches of open forest exist. The ecoregion contains stretches of Iquitos várzea along the main rivers, blending into Purus várzea near the eastern border, where it adjoins the Juruá-Purus moist forests ecoregion.

The Mekong Delta was the heartland of agricultural South Vietnam, it encompassed the fertile alluvial plains formed by the Mekong River and its main tributary, the Bassac River. With its sixteen provinces, the Delta contained about two- thirds of the nation's population and yielded the same proportion in rice production. The terrain of IV Corps differed radically from other regions. Flat and mostly uncovered, it consisted of mangrove swamps and ricefields crisscrossed by an interlocking system of canals, natural and artificial.

Nasra is located at . The maps of Ranaghat I and Ranaghat II CD blocks, in the District Census Handbook 2011, Nadia, shows the census towns of Kamgachhi, Raghabpur, Panpara, Aistala, Satigachha, Anulia, Halalpur Krishnapur, Hijuli and Ranaghat (CT) forming a cluster around Ranaghat. Certain other localitites such as Nokari, Nasra, Cooper's Camp, Birnagar, Habibpur, Gopalpur and Parbbatipur are also linked with this cluster. Nadia district is mostly alluvial plains lying to the east of Hooghly River, locally known as Bhagirathi.

Prehistoric Daepyeong incorporates in area formed by the curves of the Nam River in a single area of several small, linked alluvial plains that are semi- circumscribed by steep hills of 100–1100 metres. In the north, Daepyeong includes Sonam-ni and Eoeun, and in the south Okbang and Sangchon-ni are included. Eoeun and Okbang make up the central area and are partially protected by a natural levee formed by terracing and changes in the flow of the Nam River.

In freshwater ecology, upland rivers and streams are the fast-flowing rivers and streams that drain elevated or mountainous country, often onto broad alluvial plains (where they become lowland rivers). However, altitude is not the sole determinant of whether a river is upland or lowland. Arguably the most important determinants are those of stream power and stream gradient. Rivers with a course that drops rapidly in altitude will have faster water flow and higher stream power or "force of water".

By road, the town can be accessed from Krishnanagar, Katwa, Bandel, Pandua, Boinchi, Memari and Barddhaman. Though part of the Burdwan district of West Bengal, it is located near the border with Nadia and Hooghly District, and is close to Nabadwip and Mayapur, known for the ISKCON center. Kalna is located on the agriculturally rich alluvial plains between the Bhagirathi, Ajay and Damodar rivers.Chattopadhyay, Akkori, Bardhaman Jelar Itihas O Lok Sanskriti (History and Folklore of Bardhaman District.), , Vol I, p.

The Balagarh CD Block is mostly part of the Hooghly Flats, one of the three natural regions in the district of the flat alluvial plains that forms part of the Gangetic Delta. The region is a narrow strip of land along the 80 km long stretch of the Hooghly River, that forms the eastern boundary of the district. The region has been physiographically influenced by the course of the river. The western part of the block gradually merges into the Hooghly-Damodar Plain.

Geologically, basalt terraces account for 43% of the peninsula's area. The rest is divided up between marine terraces (27%) and alluvial plains (17%). Leizhou Peninsula is dotted with a few dormant volcanoes, beaches, and low-lying diluvial plains. Leizhou has two separate volcanic fields: a Pleistocene-Holocene field at the northern end of the peninsula west of Zhanjiang Leibei Huoshanqun) and the northern end of the Qionglei or Leiqiong volcanic field, which extends across the strait into northern Hainan Leinan Huoshanqun).

The Sreerampur Uttarpara CD Block is part of the Hooghly Flats, one of the three natural regions in the district of the flat alluvial plains, that forms part of the Gangetic Delta. The region is a narrow strip of land along the 80 km long stretch of the Hooghly River, that forms the eastern boundary of the district. The region has been physiographically influenced by the course of the river. The Hooghly is a tidal river and has a high west bank.

The Gomti in Sitapur district The Gomti River is polluted at several points of its course through the stretch of alluvial plains in Uttar Pradesh. The major sources of pollution are industrial waste and effluent from sugar factories and distilleries and residential wastewater and sewage. The river and its tributaries, such as Kukrail Drainage, collect large amounts of human and industrial pollutants as they flow through an area of about 18 million people. High pollution levels threaten the Gomti's aquatic life.

The Chinsurah Mogra CD Block is part of the Hooghly Flats, one of the three natural regions in the district of the flat alluvial plains that forms part of the Gangetic Delta. The region is a narrow strip of land along the 80 km long stretch of the Hooghly River, that forms the eastern boundary of the district. The region has been physiographically influenced by the course of the river. The Hooghly is a tidal river and has a high west bank.

The city's current geography is typical of southern China: numerous steep mountains and hills with alluvial plains in between down to the coastline. The main summit of the Wugui Hills is the highest point in the city, at above sea level. Like nearly all of southern China, Zhongshan's climate is warm and humid most of the year, with an average temperature of and of rainfall each year. Southern China experiences fairly frequent typhoons and thunderstorms, and most rain falls between April and September.

Alluvial plains along the Danube are well-formed, especially on the left bank, and in some parts from the river. A large part of Novi Sad lies on a fluvial terrace with an elevation between . The northern part of Fruška Gora is composed of massive landslide zones, although they are largely inactive with the exception of the Ribnjak neighbourhood between Sremska Kamenica and Petrovaradin Fortress.Завод за урбанизам: "Еколошки Атлас Новог Сада" ("Ecological Atlas of Novi Sad"), page 14-15, 1994.

Palaeobotanical research at the Joggins Formation suggests vegetation played a vital role in maintaining the ecosystem's water balance and shaping the waterways of Palaeozoic Joggins. The deep roots of tree-like plants like lycopsids and calamitaceaens stabilized river banks and formed river bars. This behaviour is more common in younger deposits of the Joggins Formation than in older strata. Gymnosperm forests covered much of the alluvial plains and the basin-margin highlands and were occasionally devastated by forest fires, possibly a result of high atmospheric oxygen.

Jirat is the Main Administrative Center (Sadar) of Balagarh Block. Balagarh Bijoy Krishna Mahavidyalaya, Balagarh BDO Office, and Jirat Hospital are located in Jirat. The Balagarh CD Block is mostly part of the Hooghly Flats, one of the three natural regions in the district composed of the flat alluvial plains that form a part of the Gangetic Delta. The region is a narrow strip of land along the 80 km long stretch of the Hooghly River, that forms the eastern boundary of the district.

It is comparable in size to the US state of California, and somewhat larger than Paraguay. Iraq mainly consists of desert, but near the two major rivers (Euphrates and Tigris) are fertile alluvial plains, as the rivers carry about of silt annually to the delta. The north of the country is mostly composed of mountains; the highest point being at point, unnamed on the map opposite, but known locally as Cheekah Dar (black tent). Iraq has a small coastline measuring along the Persian Gulf.

Map of Bankura District showing CD blocks and municipalities Patrasayer is located at . Patrasayer CD block is located in the eastern part of the district and belongs to the fertile low lying alluvial plains, similar to the predominating rice lands in the adjacent districts of West Bengal. The area is also referred to as Patrasayer plains. Here, the eye constantly rests on wide expanses of rice fields, green in the rains but parched and dry in summer.O’Malley, L.S.S., ICS, Bankura, Bengal District Gazetteers, pp.

Unlike the rest of Bardhaman district, which lies to the north of the Damodar River, the Khandaghosh-Jamalpur-Raina area lies on the alluvial plains between the Damodar on its southern/ eastern side and the Dwarakeswar River. As a result, it has been a flood prone area.Chattopadhyay, Akkori, pp. 15-18 Raina I CD Block is bounded by Burdwan II CD Block on the north, Jamalpur CD Block on the east, Raina II CD Block in the south, and Khandaghosh CD Block on the west.

Stone is rare in the central and southern alluvial plains that formed the heartland of Abbasid territory, so many of the buildings were of mud-brick, faced with plaster and frequently repaired or rebuilt. Sometimes fired brick was used. When the caliph al-Mansur built the round city of Baghdad, called Madinat al-Salam, which contained the caliphal palace, mosque and administrative buildings, he may have been following earlier traditions such as the round city of Gur built by Ardashir I (r. 224-241) at Firuzabad.

About 56% of the total forest is within the Permanent Forest Estate. This includes almost the full range of forest types found in Malaysia, although some of the unusual types, heath forest or forest on ultrabasic rocks, exist only in tiny areas of Pahang. The totally protected forest within Taman Negara and Krau Wildlife Reserve includes small areas of extreme lowland alluvial plains. Elsewhere, most of the dryland forest in Pahang is on steep slopes and therefore has both catchment protection and slope protection functions.

It is native to Pilbara, Gascoyne and Mid West regions of Western Australia where it is known to grow in quartzite, and granitic soils and is often found along watercourses and swampy areas. It has a discontinuous distribution and is found from around Pingandy Station along the Ashburton River in the north down to around Murgoo Station and the Murchison River in the south where it is often situated on loamy alluvial plains as a part of shrubland communities where it is usually associated with Acacia aneura.

The ecoregion is between the Pacific Ocean and the Western Ranges of the Andes, with elevations from sea level to about . It includes the western slopes of the Andes and the Cerro Torrá, Serranía del Darién, Sierra Llorona de San Blas and Serranía del Baudó massifs. Terrain includes recently formed alluvial plains, hills formed in the Tertiary and Pleistocene from dissection of sediments, and older Mesozoic era rocks in the mountains. The soils are typically red clay laterite, leached of most nutrients by the heavy rain.

69 The depositional environment has been interpreted as alluvial plains and alluvial fans, formed during the main phase of tectonic uplift of the Eastern Ranges in the Late Pliocene.Montoya & Reyes, 2005, p.67 Dutch geologist Salomon Kroonenberg, who studied the Neogene uplift of the Eastern Andes in Colombia, defines the main stage of uplift between six and four million years ago. Other Dutch geologists Helmens, Van der Hammen and Hooghiemstra have pushed back this uplift phase to between 4.5 and 3 Ma.Molnar, 2004, p.

On the south-east it is bounded by Hooghly district, on the south by Paschim Medinipur district and on the west by Purulia district. Bankura district has been described as the "connecting link between the plains of Bengal on the east and Chota Nagpur plateau on the west." The areas to the east and north-east are low-lying alluvial plains, similar to predominating rice lands of Bengal. To the west the surface gradually rises, giving way to undulating country, interspersed with rocky hillocks.

Habiganj is located at . Its area is 2,636.58 km² and bounded by Sunamganj District to the north, Tripura of India and Maulvibazar District to the east, Balaganj Upazila of Sylhet to the north- east, Brahmanbaria and Kishoreganj districts to the west. This part of Bangladesh is characterized by alluvial plains which are dissected by various connecting rivers as well as streams, lakes; and it is vulnerable to both flood and drought. The land is devoted mainly to agriculture due to its fertile alluvial soils.

Below the western foothills of the ranges, such as the Hsinchu Hills and the Miaoli Hills, lie raised terraces formed of material eroded from the ranges. These include the Linkou Plateau, the Taoyuan Plateau and the Dadu Plateau. About 23% of Taiwan's land area consists of fertile alluvial plains and basins watered by rivers running from the eastern mountains. Over half of this land lies in the Chianan Plain in southwest Taiwan, with lesser areas in the Pingtung Plain, Taichung Basin and Taipei Basin.

The river contributes 9.3% of the mean annual runoff of the Limpopo Basin, making it the third largest tributary to the Limpopo basin. Major tributaries of the Mzingwane River include the Insiza, Inyankuni, Ncema, Umchabezi (not to be confused with Mtshabezi) and Mtetengwe Rivers. The lower Mzingwane River is a sand filled channel, with extensive alluvial aquifers in the river channel and below the alluvial plains. Estimated water resources potential of these aquifers ranges between 175,000 m3 and 5,430,0003 in the channels and between 80,000 m3 and 6,920,0003 in the plains.

Lane of Huanglongxi In Chinese, western Sichuan is called Chuanxi, which refers to the western plain of Sichuan and is located in the western part of the Sichuan Basin. It is also called as Chengdu Plain or Basin West Plain. The narrow western Sichuan plain refers to the alluvial plains with an area of approximately 8,000 m2 of Min River, Tuo River, and their tributaries bordered by Dujiangyan City, Mianzhu, Luojiang, Jintang, Xinjin and Qionglai. Vernacular residential architecture style in Western Sichuan became relatively mature in Qing dynasty.

He County is located on the northern bank of the Yangtze River. He County borders Chuzhou to the northwest, Nanjing to the northeast, the three urban districts of Ma'anshan to the east, Wuhu to the south, and Hanshan County to the west. He County has a total area of 1318.6 square kilometers (509 sq mi), of which 48% is arable land. He County is situated on the Yangtze Plain and has relatively flat terrain in the southeast, with ponds dotting the alluvial plains, with the northwest of the county consisting of rolling hills.

Archaeologists found 11 polishing pebbles and a mushroom-shaped pottery anvil in the grave of a woman at the Nodena Site. Both amateur collectors as well as professional archeologists have long known that shell-tempered pottery is characteristic of the middle and lower Mississippi Valley. "Grave diggers" and amateur collectors have plundered many Mississippian mounds for the fine funerary effigies and other vessels placed as grave goods within mounds and surrounding village areas. Early professional surveys in the valley noted the preponderance of shell-tempered wares in large village sites throughout the valley alluvial plains.

The two most substantial aquifers are the Pacific Coastal Plain alluvium and the karstic and fractured limestone that extend beneath the Sierra de los Cuchumatanes, Sierra de Chama, and Peten Lowlands. Other more limited aquifers are important for small-scale local demands. The mountains and hills of Guatemala contain many other types of aquifers, including volcanic pyroclastic and lava deposits, low permeability sediments, igneous, and metamorphic aquifers. Alluvial plains, valleys and lowlands make up about 50% of the countries territory and contain about 70% of the available ground water reserves.

The homes were built of local field stones from the alluvial plains around Claremont, as well as salvaged and recycled materials including the sides from railroad cars, debris remaining after the 1933 Long Beach earthquake, and materials from wrecking yards.Russian Village, Claremont CA hubpages > education > fieldstone_homes Many of Stys's friends were unemployed during the Great Depression and several lost their homes. Stys sold off portions of his land for low prices, often asking for no down payment, and helped them build inexpensive houses out of salvaged and recycled materials.

The Office du Niger is a semi-autonomous government agency in Mali that administers a large irrigation scheme in the Ségou Region of the country. Water from the Niger River is diverted into a system of canals at the Markala dam downstream of Ségou. The water is used to irrigate nearly of the flat alluvial plains to the north and northeast of Markala that form part of the Delta mort. Although the French colonial administration constructed the system to produce cotton for the textile industry, the main agricultural product is now rice.

In the late 1800s the alluvial plains near the lake were occupied by the Njemps people, an ethnic group related to the Maasai. They used a brushwood barrier to raise the level of the river and let the water flow over the flat ground. The barrier would be destroyed by the seasonal floods, needing to be replaced, but the system was stable. The British explorer Joseph Thomson visited the Perkerra in the nineteenth century with his caravan and bought grain from the local people, grown using their proven system of irrigation using basins and canals.

In addition, many of the best-preserved specimens that can accurately be classified as Robertia were collected without precise location documentation. As a result, the range of Robertia may also extend further than is currently known. Robertia fossil specimens have been uncovered in mudstone and sandstone, which have been formed by river flow across the alluvial plains. It is thought that the paleoenvironment of the Beaufort Karoo consisted of large rivers around 350 meters wide and 11 meters deep running into a system of lakes that were no more than 50 meters deep.

A portion of the alluvial plain of the lower Burdekin River is located in the north and north west of the subregion. Smaller alluvial plains are located on the Bowen and Bogie rivers which flow through the subregion into the Burdekin River. The Don River which flows into the sea near Bowen has an alluvial plain and a small delta. To the north of the Don River is a narrow coastal plain across which several small coastal streams flow, this is analogous to but smaller than the Townsville coastal plain to the north.

The Southwest Amazon moist forests (NT0166) is an ecoregion located in the Upper Amazon basin. The forest is characterized by a relatively flat landscape with alluvial plains dissected by undulating hills or high terraces. The biota of the southwest Amazon moist forest is very rich because of these dramatic edaphic and topographical variations at both the local and regional levels. This ecoregion has the highest number of both mammals and birds recorded for the Amazonian biogeographic realm: 257 with 11 endemic species for mammals and 782 and 17 endemics for birds.

Geologic map of the Santa Barbara coastal plain area, Santa Barbara County, California: US Geological Survey Scientific Investigations Map 3001, scale 1: 25,000, 1 sheet, pamphlet 38 p. Notable features along the fault which mark the boundary of the range include Jalama Creek and the Santa Ynez River to the west and Matilija Creek in the far east. To the north of the range are the San Rafael Mountains. The southern slopes of the range drop off into a series of alluvial plains adjoining the Santa Barbara Channel.

This year it will be conducted on 23 September. Sasthamkottah lake is the largest fresh water lake in kerala and provides drinking water for most of the places in Kollam district. Except for an earthen embankment of 1.5 km length which separates the lake from the paddy fields on its southern side, bordering the alluvial plains of the Kallada River, all other sides of the lake are surrounded by hills which are steep and form narrow valleys. Sooranad, Chakkuvally, Kunnathur, Mynagappally, Poruvazhy, West Kallada, Karunagappally, East Kallada are the important places in and around Sasthamcotta.

Jo 1987:35 The upper part of the river flows slowly through part of the Noryeong Mountains and is marked by extensive stream meandering. On the other hand, river curves on middle and lower parts of the river are more gradual and there is comparatively less stream meandering. Tributary streams of the Geum include the Gap-cheon, Yugu-cheon, Miho-cheon, Unsan-cheon, Seokseong-cheon, and Nonsan-cheon. Several small alluvial plains including the Honam and Nonsan Plain have been formed by the flow of the Geum and its tributaries.

Malik's son, Ismail Khan, is traditionally believed to have founded the city of Dera Ismail Khan, though the Emperor Babur passed through the region in 1506 and made no mention of the city.Aminullah Khan Gandpar, Tarikh-i-Sar Zamin-i-Gomal, National Book Foundation Islamabad, page 45. Baloch settlers were assimilated through the, later waves of Pashtun settlement, although villagers along the alluvial plains are typically Baloch or Jat. The city was along the major Multan-to-Kandahar trade route, though it never attained a station of great power or importance before the British period.

Unlike the rest of Bardhaman district, which lies to the north of the Damodar River, the Khandaghosh-Jamalpur-Raina area lies on the alluvial plains between the Damodar on its northern/ eastern side and the Dwarakeswar River. As a result, it has been a flood prone area.Chattopadhyay, Akkori, pp. 15-18 Raina II CD Block is bounded by Raina I CD Block on the north, Jamalpur CD Block on the east, Pursurah, Aramabgh and Goghat I CD Blocks, in Hooghly district, in the south, and Khandaghosh CD Block on the west.

Located between the Lisboa and Alentejo VRs, the region is dominated by the influence of the Tagus river. The river moderates the region's climate, making it more temperate than other areas of Portugal. Vineyards are planted on the fertile alluvial plains along the river and can be prone to producing excessive yields.T. Stevenson "The Sotheby's Wine Encyclopedia" pg 329-333 Dorling Kindersley 2005 In 2009, the region was renamed from Ribatejo to Tejo, the same name as the river flowing through the region, as part of a drive to increase the wine region's international reputation.

These smaller regions are located on alluvial plains with soils composed of gravel and sand. The wines made here are lighter and less elegant than the Friuli wines made in the major southern wine regions. Unlike other Friuli regions which require 100%, a varietal wine in the Graves and Aquileia zones only need 85% of the grape variety with the Latisana and Annia zones requiring 90%. More red wine is produced in these zones than in the rest of the Friuli with Merlot, Cabernet franc and Cabernet Sauvignon being the leading varietals.

Rous Creek runs north to south through the property for a distance of and the flanking alluvial plains have the highest pastoral value. About one third of the property is made up of sandy plain country that supports spinifex grasslands dived by rugged hills and ridges. Established at some time prior to 1901, the property was owned by Joseph McCarthy at that time. The store at Uaroo was important to the many prospectors in the area as it was the only place they could obtain provisions, the next nearest being at Onslow.

A group of Taiwanese indigenous children Taiwanese indigenous peoples are the indigenous peoples of Taiwan. They speak languages that belongs to the Austronesian language family, and are culturally, genetically and linguistically closely related to the ethnic groups of Maritime Southeast Asia and Oceania. Their ancestors are believed to have been living on the islands for approximately 8,000 years before major Han Chinese immigration began in the 17th century . Taiwan's Austronesian speakers were traditionally distributed over much of the island's rugged central mountain range and concentrated in villages along the alluvial plains.

The district of Dera Ismail Khan is bounded on the east by the Bhakkar and Dera Ghazi Khan districts of Punjab. Eastern portions of the district along the Indus River are characterized by fertile alluvial plains, while lands farther from the river consist of clay soil cut by ravines from rainfall. The district is bounded on the southwest by a thin strip of the South Waziristan district of the Federally Administered Tribal Areas, which separates D.I Khan from the Takht-e-Sulaiman Mountain in the neighboring Baluchistan province. In the northwest is the Tank District.

It is native to an area in the Pilbara and Mid West regions of Western Australia where it is commonly found in river beds, hardpans and floodplains where it grows in loam, clay, alluvium and red sandy soils. It has a discontinuous distribution and is often found around the headwaters and upper catchment areas of the Fortescue, Gascyone and Murchison Rivers where it is found on alluvial plains growing in loamy soils as a part of low woodland or shrubland communities and are known to form pure stands.

Namsan, a mountain composed of two peaks (466 m, 495 m), cuts the Gyeongju Basin into two parts at the southern end. The streams that flow from these mountains have formed a number of interlinked alluvial plains in the Basin. The city center of Gyeongju, which was also the capital of the ancient Silla kingdom, occupies much of the basin. Various watershed management projects were undertaken even during Silla times, due to continuous flooding in the basin, caused by runoff from the neighboring mountains combined with inflow from the upper Hyeongsan River watershed.

Even in this zone, however, only one crop a year can be grown, and shortages of rain have often led to crop failures. Mean minimum temperatures in the winter range from near freezing (just before dawn) in the northern and northeastern foothills and the western desert to and in the alluvial plains of southern Iraq. They rise to a mean maximum of about in the western desert and the northeast, and in the south. In the summer mean minimum temperatures range from about and rise to maxima between roughly .

Bathurst Harbour is a large, rectangular, almost landlocked body of water located in the southwest corner of Tasmania. The harbour is surrounded by low-lying alluvial plains with mountain ranges running along the western and eastern shores. The North River, Old River, Ray River and Melaleuca Creek all drain into the harbour either directly or into one of the many offshoot bays and inlets connected to the harbour. Almost all of the harbour is navigable by sailing vessels with no submerged rocks or navigational hazards except for a small area around Black Swan Island at Old Bay in the harbours north.

Unlike the rest of Bardhaman district, which lies to the north of the Damodar River, the Khandaghosh-Jamalpur-Raina area lies on the alluvial plains between the Damodar on its northern/ eastern side and the Dwarakeswar River. As a result, it has been a flood prone area.Chattopadhyay, Akkori, pp. 15-18 Khandaghosh CD Block is bounded by Galsi II and Burdwan I CD Blocks on the north, Raina I and Raina II CD Blocks on the east, Goghat II CD Block, in Hooghly district, in a small section of the south, and Indas CD Block, in Bankura district, on the south and west.

At higher altitudes, there are fewer maples and the dominant trees are hawthorn, Juniperus turcomanica and Celtis caucasica. On the mountain tops, grasses and cushion plants are the main members of the plant community. In the steep sided ravines, there are walnut trees, Syrian ash, Thelycrania meyeri, Prunus divaricata, Lonicera floribunda, Rubus sanguinoides and Rosa lacerans. Takirs of Karakum Desert Much of the rest of the country makes up the Central Asian Southern Desert ecoregion, which includes the Karakum Desert, the southern part of the Kyzylkum Desert and other areas with rolling dunes, sandy plateaus and alluvial plains.

The layer was 180 centimeters below the ground, which is covered with lake deposits such as thick black and gray silt clay. Three archeological excavations have been carried out so far by institutions such as the Department of Archaeology in Peking University, the Department of History in Hebei University, the Hebei Provincial Institute of Cultural Relics and other cultural institutions in the city and county level. The Early Neolithic period (7,000 BC-5,000 BC) succeeds Nanzhuangtou, and is characterized by the rise of farming villages across the alluvial plains of China, as seen in the site of Peiligang.

In 1873, a settler named J.L. Hilton built a small house situated half-way between Greeley and Fort Collins. The “half-way” house, as it became known, directed travelers along a route, which was soon adopted by the Greeley, Salt Lake and Pacific railway. The railroad brought investors and farmers to Windsor in increasing numbers. Windsor's rich alluvial plains lent themselves to extensive wheat production and the establishment of one of the town's first commercial enterprises, a flour mill, which through a subsequent fire in 1899, was rebuilt and became the Windsor Milling and Elevator Company.

The Cistecephalus Assemblage Zone is located in the lower portion of the Teekloof Formation west of 24°E, in the upper Middleton Formation and lower Balfour Formation east of 24°E. These formations all fall within the Adelaide Subgroup of the Beaufort Group, sediments of which were formed in a large retroarc foreland basin in southwestern Gondwana. The sedimentary rocks are mainly sandstone, mudrock layers containing mudstone, siltstone, and fine sandstone. The sandstones are thought to have been deposited in broad alluvial plains where low-sinuosity streams flowed, while the mudrock accumulated on the floodplains that flanked these streams.

The IV Corps () was a corps of the Army of the Republic of Vietnam (ARVN), the army of the nation state of South Vietnam that existed from 1955 to 1975. It was one of four corps in the ARVN, and it oversaw the Mekong Delta region of the country. The Mekong Delta was the heartland of agricultural South Vietnam, it encompassed the fertile alluvial plains formed by the Mekong River and its main tributary, the Bassac River. With its sixteen provinces, the Delta contained about two-thirds of the nation's population and yielded the same proportion in rice production.

The administrative headquarters and chief town is Bijapur. Geographically, the district lies in the tract of the Deccan Plateaus. The lands of the district can be broadly divided into three zones: the northern belt consisting of the northern parts of Bijapur Taluks of Indi and Sindagi; the central belt consisting of Bijapur city; the southern belt consisting of the rich alluvial plains of the Krishna Rivers parted from the central belt by a stretch of barren Trap. The northern belt is a succession of low rolling uplands without much vegetation, gently rounded and falling into intermediate narrow valleys.

It is a foreland basin which consists of the sediments brought down from the northern part of Nepal. It is the Nepalese extension of the Indo-Gangetic Plains, which covers most of northern and eastern India, the most populous parts of Pakistan, and virtually all of Bangladesh. The Plains get their names from the rivers Ganges and Indus. The vast alluvial plains of the Indo-Gangetic Basin evolved as a foreland basin in the southern part of the rising Himalaya, before breaking up along a series of steep faults known as the Himalayan Frontal Fault or the Main Frontal Thrust .

The Yangtze Plain (Chinese: 長江中下游平原/长江中下游平原; Wade-Giles: Ch'ang Chiang P'ing- yüan; Pinyin: Chang Jiang Pingyuan) is made up of a series of alluvial plains of along the Yangtze River and its major tributaries. It is the best place in the world judging as a plateau. The Yangtze Plain starts east of Yichang (Hubei province), China. The Middle Yangtze Plain is made up of parts of the north-eastern and south-eastern Hunan, Hubei, and north-central Jiangxi provinces, and includes the Dongting, Poyang, and Hong lakes.

It is navigable for about , and is supported by many tributaries including Y.S., Broad, Grass and Horse Savannah. The river has its source in the mountains of Manchester where it rises and flows west as the border between Manchester and Trelawny then goes underground. It reappears briefly in several surrounding towns, but reemerges near Balaclava and tumbles down gorges to the plain known as the Savannah, through the Great Morass and to the sea at Black River, the capital of the parish. The geology of the parish is primarily alluvial plains to the south, and karstic limestone to the north.

The Bicol River is the eighth largest river in the Philippines in terms of drainage basin size with an estimated catchment area of . The river drains a large part of southwestern Bicol Peninsula of the island of Luzon and passes through Camarines Sur province. The river starts from Lake Bato, above sea level, and flows downstream to its estuarine mouth at San Miguel Bay. It passes through Naga City, the alluvial and coastal plains of the vast Bicol Valley, an elongated, northwesterly trending depression in the Bicol Region, which contains alluvial plains to the coastal plain.

Map of Hooghly district, with CD blocks and municipal areas Map of Tarakeswar The CD block is part of the Hooghly-Damodar Plain, one of the district's three natural regions of flat alluvial plains which form part of the Ganges Delta. It has many depressions which receive water from tributaries of the surrounding lands during the rainy season and discharge it in smaller channels. Tarakeshwar is bordered by Dhaniakhali CD block on the north, Haripal CD block on the east, Jangipara CD block on the south, and Pursurah CD block on the west. It is from Chinsurah, the district headquarters.

On the slightly rolling small plains along the Pivka and the Nanoščica, there are wet meadows, and small fields are found on the surrounding gentle rounded slopes. Settlements lie in elevated places among the alluvial plains. The location of villages was mainly determined by the agricultural orientation of the population because the settlements are connected to land that can be farmed. Kalec Castle near Zagorja, Pivka Basin The largest settlement is Postojna, located at the entrance to the Postojna Gate, and on the opposite side lies Razdrto, which played a key role in transportation in the past.

Geomorphologists believe that the island of New Guinea is part of the Australian continent, both lies on Sahul Shelf and once joined via a land bridge during the Last glacial period. The tectonic movement of the Australian Plate created towering, snowcapped mountain peaks lining the island's central east-west spine and hot, humid alluvial plains along the coasts. The New Guinea Highlands range some east to west along the island, forming a mountainous spine between the northern and southern portion of the island. Due to its tectonic movement, New Guinea experienced many earthquakes and tsunamis, especially in its northern and western part.

With this name, they historically identified themselves as the inhabitants of the alluvial plains, river valleys, and plateaus of their native area, where they lived in local communities called muang and cultivated rice on paddy fields. This distinguished them from the indigenous peoples of the area ("hill tribes"), like the Lua', who lived in the wooded mountains practicing slash- and-burn agriculture. Membership of the ethnicity was therefore defined by lifestyle rather than by genetics. At the same time, it was a term of dissociation from the Burmese and Siamese, who held suzerainty over the Lanna Kingdom for centuries and who were not "people of our muang".

The territory of China lies between latitudes 18° and 54° N, and longitudes 73° and 135° E. The geographical center of China is marked by the Center of the Country Monument at . China's landscapes vary significantly across its vast territory. In the east, along the shores of the Yellow Sea and the East China Sea, there are extensive and densely populated alluvial plains, while on the edges of the Inner Mongolian plateau in the north, broad grasslands predominate. Southern China is dominated by hills and low mountain ranges, while the central-east hosts the deltas of China's two major rivers, the Yellow River and the Yangtze River.

Restoration of two alt=Artistic reconstruction of the habitat of Limusaurus'' All known Limusaurus fossils were recovered from the Shishugou Formation, a succession of sedimentary rocks that were deposited at the northeastern margin of the Junggar foreland basin and is about in thickness. The formation is dated to the Late Jurassic, around 161 to 157 million years ago. Limusaurus occurs in the upper part of the formation, which represents a variety of environments, including alluvial fans and alluvial plains, streams, wetlands, and shallow lakes. During the time when Limusaurus lived, the environment would have been relatively warm and dry, judging by the abundance of coal and carbon-rich deposits.

Except for an earthen embankment of 1.5 km length which separates the lake from the paddy fields on its southern side, bordering the alluvial plains of the Kallada River, all other sides of the lake are surrounded by hills which are steep and form narrow valleys. In the south and southwestern parts of the lake there are a number of smaller water bodies and waterlogged areas. The present area of the lake is 375 ha since large part of the lake is reported to have been occupied for agriculture. Rock formation of mainly archaean origin are recorded with intrusions of charnockite, biotite gneiss and dolerite dyke rocks.

With the exception of the mountainous northeastern region, however, most areas of Kaesong consist of low hills with the height less than 100 meters. The Imjin River flows along the northeastern border line of the city and the Ryesong River (禮成江) (Ryeseong-gang; 례성강) (transliterated in South Korea as Yeseong- gang; 예성강) runs along the western border to the mouth of the Han River. In addition to the two rivers, small and large rivers and streams such as the Samich'ŏn, Wŏlamch'ŏn, Chukbaech'ŏn, Kŭmsŏngch'ŏn, and Sach'ŏn rivers drain into the Han. The river basin located in the southwest of Kaesong has spacious alluvial plains such as P'ungdŏkbŏl, Singwangbŏl, and Samsŏngbŏl.

The depositional environment of the Eodicynodon Assemblage Zone was formed by sedimentary material being deposited in the Karoo Basin - a retro-arc foreland basin - by vast, low-energy alluvial plains flowing northwards from a southerly source area in the rising the Gondwanide mountains. The Gondwanides were the result of crustal uplift that had previously begun to take course due to subduction of the Palaeo-pacific plate beneath the Gondwanan Plate. Orogenic pulses from the growing Gondwanides mountain chain and associated subduction created accommodation space for sedimentation in the Karoo Basin where the deposits of the Eodicynodon Assemblage zone, and all other succeeding assemblage zones, were deposited over millions of years.

A debate has arise of whether the Dagshai Formation overlies conformably or unconformably on top of the Subathu formation. recent research by dating detrital micas and fission track dating of detrital zircons shows conclusively that there is an unconformable nature between the Subathu and Dagshai Formation. Magnetostratigraphic data suggests that the Daghsai formation was deposited at approximately 27 Ma with 2 Ma uncertainty. Previously, multiple studies of facies interpretation of the Dagshai formation has been conducted with varying results regarding the past depositional environment; the presence of quartzitic sandstones was thought to be leftovers of an extensive and prolonged weathering in alluvial plains in which time tropical weathering was intensifying.

These large plateaus are divided into smaller ones by shallow river valleys. One of the common features of the plateaus is that their surfaces are covered with a thick layer of loam of volcanic origin. Volcanic ashes from surrounding volcanoes, Mounts Asama, Haruna, and Akagi to the north and Mounts Hakone and Fuji to the southwest, are thought to have been deposited on these plateaus.Nihon Daihyakka Jiten, Shōgakkan Among the plateaus, the Musashino Plateau has the largest stretch of land, extending from the western edge of Ōme to the eastern edge of Yamanote which borders the alluvial plains of the Arakawa and Sumida Rivers.

Village in the central highlands The Central Highlands, which range from in altitude, contain a wide variety of topographies: rounded and eroded hills, massive granite outcrops, extinct volcanoes, eroded peneplains, and alluvial plains and marshes, which have been converted into irrigated rice fields. The Central Highlands extend from the Tsaratanana Massif in the north to the Ivakoany Massif in the south. They are defined rather clearly by the escarpments along the east coast, and they slope gently to the west coast. The Central Highlands include the Anjafy High Plateaux; the volcanic formations of Itasy (Lake Itasy is in a volcanic crater) and the Ankaratra Massif, reaching a height of .

The Dundwa Range (Hindi and dundwā shrinkhalā) is a subrange of the Sivalik Hills in western Nepal and northern Uttar Pradesh, India. It separates the Outer Terai of Balarampur and Shravasti districts in Uttar Pradesh from Deukhuri Valley in Nepal's Dang-Deukhuri and eastern Banke districts. The international border follows the southern edge of this range, leaving a zone of forested Bhabar inside Uttar Pradesh. The Dundwas diverge from other Sivalik ranges at 27°52'N, 83°14'Ein western Kapilvastu, extending 160 km W and WNW across Dang Deukhuri District and into Banke -- within 20 km of Nepalganj -- before descending into the alluvial plains.

Picture from Hume and Marshall. The > swamp partridge, as its name implies, has a habitat quite different from our > other species, affecting high grass and cane-brakes near the edges of rivers > and jheels, though it will come into cultivated ground to feed. It haunts > the alluvial plains of the Ganges and Brahmaputra, extending from Pilibhit > to the extremity of Assam and Cachar, and even occurs occasionally on the > Khasi plateau; but it is not found in the Sundarbans. Very little is known > about its breeding, but on two occasions five eggs of the species have been > taken in April; they were cream-coloured and slightly speckled.

India's agriculture has an extensive background which goes back to at least 9 thousand years. In India, Agriculture was established throughout most of the subcontinent by 6000–5000 BP. During the 5th millennium BP, in the alluvial plains of the Indus River in Pakistan, the old cities of Mohenjo-Daro and Harappa experienced an apparent establishment of an organized farming urban culture. That society, known as the Harappan or Indus civilization, flourished until shortly after 4000 BP; it was much more comprehensive than those of Egypt or Babylonia and appeared earlier than analogous societies in northern China. Currently, the country holds the second position in agricultural production in the world.

Located south-east of Saigon, Phước Tuy Province lay on the coast between the mountains of southern central Vietnam and the alluvial plains of the Mekong Delta, dominating the approaches to Vũng Tàu and the main highway to the capital. Approximately east to west and north to south, it was roughly rectangular. Mostly flat, it gradually sloped north, while the Nui Thi Vai, Mây Tào and Long Hải mountains rose in the south-west, north-east and south. The province was bounded to the north by Biên Hòa, Long Khánh, and Bình Tuy Provinces, and to the south-east by the South China Sea.

Montgomery Woods State Natural Reserve is a 1,323-acre (535 ha) state-owned park located in the Coastal Range in Mendocino County, California, United States. The Reserve occupies the headwaters of Montgomery Creek, a tributary of Big River, which flows into the Pacific Ocean at Mendocino Headlands State Park. The virgin groves of Coast Redwood (Sequoia sempervirens) in Montgomery Woods are examples of a now rare upland riparian meadow habitat; most other preserved redwood groves are on broad alluvial plains. The Reserve is accessed from a parking area along Orr Springs Road 13 miles (21 km) west of Ukiah, California, or 15 miles (24 km) east of Comptche, California.

Utah State Route 21 (SR‑21)borders the north of the range following the Beaver River from Minersville Reservoir; at the center-north foothills, SR‑21 turns northeast towards Beaver and Greenville. The range is dissected west of center, by the north-south Utah State Route 130 (SR‑130), from Minersville at the range's northwest region, (and the northeast Escalante Desert); SR-130 goes south through Parowan Canyon, and then across an alluvial plains region of Long Hollow, between two southwest-trending ridgelines. The route meets the north of Cedar Valley, and the site of Rush Lake, a dry lake; the valley turns northwest into the Escalante Desert. The route continues to Enoch, and I‑15 at Cedar City.

The Mulato-Getudo Fault, in some parts called Jetudo Fault,Plancha 5-09, 2015 extends along the eastern foothills of the Central Ranges of the Colombian Andes, where it marks the abrupt break in slope of the east-tilted Tertiary erosion surface of the Cordillera and the flat alluvial plains of the Magdalena River in the Middle Magdalena Valley. The fault forms a regional- scale degraded fault escarpment with an outstanding break in slope. It offsets Pliocene to Quaternary deposits and an extensive tilted erosional surface of probable Miocene to Pliocene age (pre-Mesa Formation, older than 1.5 Ma). The northern half of the fault is characterised by aligned drainages and broad valleys.

Location of the Waikato Plains The Waikato Plains form a large area of low- lying land in the northwest of the North Island of New Zealand. They are the alluvial plains of the ancient Waikato River, the country's longest river that over the last 1800 years has changed course many times. In the distant past the river flowed northeast from the current Lake Karapiro, exiting near Thames, but in recent times it has flowed northwest to empty into the Tasman Sea near Port Waikato. The plains can be divided roughly into the Waikato Basin (or Middle Waikato Plain), extending in all directions around the city of Hamilton, and the Lower Waikato Plain, nearer the river's mouth.

It loops northwest, then northeast through Yamanashi, before following a generally southerly course to exit into Sagami Bay of the Pacific Ocean between the cities of Hiratsuka and Chigasaki. It is dammed at several locations along the way, forming a number of reservoir lakes, the largest of which are Lake Sagami and Lake Tsukui. The river has had to re-cut its course several times due to repeated eruptions of Mount Fuji, and river terraces are in evidence along its upper reaches in Yamanashi. As the river crosses Kanagawa, it forms natural levees in the soft soils of the alluvial plains of central Kanagawa's Sagamino plateau, and forms almost no river delta as it exits into the ocean.

The Shire of Wagin contains many large lakes and wetlands, including western parts of Lake Dumbleyung, Parkeyerring Lake, Lake Little Parkeyerring, Lake Quarbing, Lake Norring, Lake Little Norring, Lake Gundaring and Lake Wagin. The lakes are part of the catchment system of the Blackwood River but as a result of the flat topography, low average rainfall and existence of an extensive network of salt lakes, the eastern creeks and rivers rarely contribute any flows to the river. The catchment area has an average rainfall of per annum and an evaporation rate of per annum. The landscape is a mixture of alluvial plains, dunes, small lunettes and swales found over alluvial and aeolian deposits.

Map showing the entire Santa Ana River Basin The drainage basin of Chino Creek spans in parts of Los Angeles, San Bernardino and Riverside Counties, with the vast majority within southwestern San Bernardino County. The broad, flat watershed comprises much of the southeastern slopes of the San Gabriel Mountains and alluvial plains that lie to the south of the range. Almost 55 percent of the basin is heavy urban development, and major cities include Rancho Cucamonga, Ontario, Upland, Pomona and Chino. ~20% of the watershed is wild land, mostly in the mountainous north within the Angeles National Forest, and the remaining quarter in the south is used for agriculture, much for the raising of livestock.

As the Ravi flows past Lahore in Pakistan ( below Amritsar in India) it is called "The river of Lahore" since that city is on its eastern bank. After passing through Lahore the river takes a turn at Kamalia and then debouches into the Chenab River, south of the town of Ahmadpur Sial. On its western bank is the town of Shahdara Bagh with the tomb of Jahangir and the Tomb of Noor Jahan. ;Change of river course According to satellite imagery studies carried out over a period of 20 years (between 1972–1973 and 1991–1993), the river coursing along the India–Pakistan border meanders substantially in the alluvial plains of the Amritsar, pathankot and Gurdaspur districts of Punjab.

The highway passes through the alluvial plains of the Yarra River and the rich Yarra Valley vineyards near Yarra Glen. At Yarra Glen, the road diverts from the main town street (Bell Street) and follows a recently completed bypass of the township. After rejoining the main highway north of Yarra Glen, the road rises up a steep grade between Dixons Creek and Glenburn to the top of the Great Dividing Range at a road junction that links the highway with the nearby towns of Kinglake and Toolangi, a former home of Australian author C. J. Dennis. From there, the road passes through forest and open agricultural land before reaching Yea, a small pastoral town.

The lower section of the river spans from the town of Novi Grad to the river mouth. After exiting the town of Novi Grad, the river flows in a general northeast direction until its confluence with the Sava river near Jasenovac. Major towns and villages on the river in this section are Novi Grad, Kostajnica and Kozarska Dubica on the right bank in Bosnia and Dvor na Uni, Hrvatska Kostajnica and Hrvatska Dubica on the left bank in Croatia. The waterfalls, rapids and tufa rock that were common in previous sections are almost completely nonexistent in the lower section as the Una takes up the characteristics of a mature river, meandering through alluvial plains and having a low gradient.

View of Marche countryside A view of Monte Conero Marche extends over an area of of the central Adriatic slope between Emilia- Romagna to the north, Tuscany and Umbria to the west, and Lazio and Abruzzo to the south, the entire eastern boundary being formed by the Adriatic. Most of the region is mountainous or hilly, the main features being the Apennine chain along the internal boundary and an extensive system of hills descending towards the Adriatic. With the sole exception of Monte Vettore, high, the mountains do not exceed . The hilly area covers two-thirds of the region and is interrupted by wide gullies with numerous – albeit short – rivers and by alluvial plains perpendicular to the principal chain.

Rivers of Japan are characterized by their relatively short lengths and considerably steep gradients due to the narrow and mountainous topography of the country. An often-cited quote is 'this is not a river, but a waterfall' by the Dutch engineer (o-yatoi gaikokujin) Johannis de Rijke who had visited the Jōganji River, Toyama Prefecture. The Mogami, the Fuji and the Kuma are regarded as the three most rapid rivers of Japan. Typical rivers of Japan rise from mountainous forests and cut out deep V-shaped valleys in their upper reaches, and form alluvial plains in their lower reaches which enable the Japanese to cultivate rice fields and to set up cities.

106f There are a number of wetland areas of significance within the district. The most westerly of these is situated on the Kyttyk Peninsula and the mouth of the Rauchua River.Andreev, p. 41 This area is dominated by the Lower Rauchua delta and the alluvial plains of the Kyttyk Peninsula, from which Ayon Island is separated by the Maly Chaunsky Strait. The peninsula is almost completely covered in a complex system of lakes, ranging in size from small saline pools lying on a recently exposed marine terrace 1 to 2 m above sea level, near the coast, to lakes up to 1 km wide and 12 m deep on high level surfaces 10–15 m above sea level.

Restoration of two Guanlong and a Yinlong, contemporaries of the unnamed crocodyliform in the Shishugou Formation The specimen was recovered from the Shishugou Formation, a succession of sedimentary rocks that was deposited at the northeastern margin of the Junggar foreland basin and is about in thickness. The formation is dated to the Late Jurassic, around 161 to 157 million years ago. The unnamed crocodyliform occurs in the upper part of the formation, which represents a variety of environments, including alluvial fans and alluvial plains, streams, wetlands, and shallow lakes. During the time when The unnamed crocodyliform lived, the environment would have been consistently warm and dry, judging by the abundance of coal and carbon-rich deposits.

The true deepest point in the harbour is where the three channels meet between Platypus Point and Nixon Point which reaches due to the dredging action of the tide. Bathurst Harbour, like the rest of the Bathurst Channel, is a ria formation caused by the inundation of a large valley and its associated alluvial plains. The glacially carved landscape of the region has resulted in the shape of the estuarine system being greatly different to other ria formations around Tasmania such as the Derwent Estuary, instead bearing close resemblance to artificial impoundments like Lake Pedder, to the north. Bathurst Harbour is one of only two places in the world where the Maugean Skate, endemic to Tasmania, has been reported from.

Bumbunga lies in the state electoral district of Narungga and in the federal electoral division of Grey. An east-facing 2006 photograph of an entrance to the former micronation, Province of Bumbunga The South Australian Government's Atlas of South Australia describes the Bumbunga environmental subregion as being a low- lying (mean altitude alluvial plains "with salt lakes and occasional dunes." The atlas further describes the subregion as having "grassland cover used for rotation cereal cultivation and livestock grazing" and "low shrubland used for livestock grazing" on salt lake margins. Located on what was traditionally the land of the Kaurna (indigenous) people, the first pioneers arrived sometime between 1847 and 1849 due to the rapid expansion of farming to the north of the area.

Animal-powered irrigation, Upper Egypt, ca. 1846 Archaeological investigation has found evidence of irrigation in areas lacking sufficient natural rainfall to support crops for rainfed agriculture. The earliest known use of the technology dates to the 6th millennium BCE in Khuzistan in the south-west of present-day Iran. Irrigation was used as a means of manipulation of water in the alluvial plains of the Indus valley civilization, the application of it is estimated to have begun around 4500 BC and drastically increased the size and prosperity of their agricultural settlements. The Indus Valley Civilization developed sophisticated irrigation and water-storage systems, including artificial reservoirs at Girnar dated to 3000 BCE, and an early canal irrigation system from 2600 BCE.

Dalupirip section of Agno River within the forest reserve in Itogon The Lower Agno reserve protects a -long valley along the Agno River from just downstream of Binga Dam in the mountain village of Tinongdan to the foothills and alluvial plains of San Roque in San Manuel immediately below the San Roque dam and reservoir. The reservation is located primarily in Itogon in the southern Cordillera Central, with small areas extending westward into Baguio and Tuba and southward into San Roque village, San Manuel and San Felipe East in San Nicolas. About 90 percent of the total land area of Itogon lies within the reservation. The protected area has a mean elevation of with peaks rising to above sea level.

Punjab features mountainous terrain near the hill station of Murree. Punjab's landscape consists mostly consists of fertile alluvial plains of the Indus River and its four major tributaries in Pakistan, the Jhelum, Chenab, Ravi, and Sutlej rivers which traverse Punjab north to south – the fifth of the "five waters" of Punjab, the Beas River, lies exclusively in the Indian state of Punjab. The landscape is amongst the most heavily irrigated on earth and canals can be found throughout the province. Punjab also includes several mountainous regions, including the Sulaiman Mountains in the southwest part of the province, the Margalla Hills in the north near Islamabad, and the Salt Range which divides the most northerly portion of Punjab, the Pothohar Plateau, from the rest of the province.

The Danubian Plain encompasses the Moesian plate and extends from the river Timok in the west to the Black Sea in the east and from the river Danube in the north to the Balkan Mountains in the south, covering 31,520 km2, or almost 1/3 of Bulgaria's total area. Its width varies from 25–30 km in the west to 120 km in the east. The highest point is Tarnov Dyal (502 m) on the Shumen Plateau; the average altitude is 178 m. As a result of the rock weathering processes the relief is uneven with fertile alluvial plains along the Danube (Vidinska, Chernopolska, Zlatia, Belenska, Pobrezhie, Aidemirska), and hilly terrain in the remaining area, including plateaus in the east.

The bison were introduced to the island in 1893, and Antelope Island bison herd has proven to be a valuable genetic pool for bison breeding and conservation purposes. The bison do well, because much of the island is covered by dry, native grassland. The geology of Antelope Island consists mostly of alluvial plains with prairie grassland on the north, east and south of the island, along with a mountainous central area of older Precambrian metamorphic and igneous rocks and late Precambrian to Paleozoic sedimentary rocks, covered by a thin layer of Quaternary lake deposits, colluvium and alluvium.physiography The Precambrian deposits on Antelope Island are some of the oldest rocks in the United States, older even than the Precambrian rocks at the bottom of the Grand Canyon.

Niono is an important town of the Office du Niger irrigation scheme which was established during the last decades of French colonial rule and continued after independence by the Malian state.. Water from the Niger River is diverted into a system of canals at the Markala dam 35 km downstream of Ségou. The water flows north for 65 km in the Canal du Sahel and is then used to irrigate the flat alluvial plains around Niono that form part of the 'Delta Mort' (Dead Delta). Although the French colonial administration constructed the system to produce cotton for the textile industry, the main agricultural product is now rice. Each year around 2.7 km3 of water are diverted from the Niger corresponding to 8.3 percent of the total flow.

When the region was covered with marshland lycopsid would put down roots on the solid ground of newly made alluvial plains where young individuals faced little competition but were at risk of flooding. If the river banks burst before the forest floor had accumulated a significant amount of peat the lycopsids would be swamped by sand carried overland in a crevasse splay, burying the trunk and killing the tree as well as any other living thing in or around it. One such event of this kind buried the Fundy forest, a section of the Joggins Formation located in Cycle 6, around 419 m (1,374.7 ft) from the base of the formation. Once dead, the section of trunk not submerged in sand would rot and decay while the section buried underground had a chance at fossilization.

The Alpine orogeny caused extensive folding and faulting of Mesozoic and early Tertiary sediments from the Tethys geosyncline. The Tibetan and Mongolian plateaux, and the structural basins of Tarim, Qaidam, and Junggar, are delimited by major east–west lithospheric faults that were probably the results of stresses caused by the impact of the Indian Plate against Laurasia. Erosion of the mountains caused by this orogeny has created a large amount of sediment, which has been transported southwards to produce the alluvial plains of India, China, and Cambodia, and which has also been deposited in large amounts in the Tarim and Dzungarian basins. Northern Asia was glaciated in the Pleistocene, but this played a less significant part in the geology of the area compared to the part that it played in North America and Europe.

Map of Bankura District showing CD blocks and municipalities. The only CD block not marked on the map is Joypur Joypur is located at . Joypur CD block is located in the eastern part of the district and belongs to the fertile low lying alluvial plains, similar to the predominating rice lands in the adjacent districts of West Bengal. Here, the eye constantly rests on wide expanses of rice fields, green in the rains but parched and dry in summer.O’Malley, L.S.S., ICS, Bankura, Bengal District Gazetteers, pp. 1-20, first published 1908, 1995 reprint, Government of West Bengal Joypur CD block is bounded by Patrasayer CD block on the north, Indas and Kotulpur CD blocks on the east, Garhbeta I CD block in Paschim Medinipur district, on the south and Bishnupur CD block on the west.

From Chapu near Lhatse, the Friendship Highway maintains the Hwy 318 route number and turns southwest and crosses the main Brahmaputra-Ganges divide at Gyatso La (), the highest pass on the road. Descending 1,000 meters onto alluvial plains of the Bum-Chu, also known as the Arun river in Nepal, the highway passes near Shelkar (New Tingri) then through Old Tingri, both gateways to Rongbuk Monastery and the north side of Mount Everest. Continuing southwest, the highway climbs over Lalung La () and crosses shortly after the Tong La (also known as Thong La, Yakri Shung La or Yakrushong La) (), which marks the water divide between the Bum-Chu / Arun and the (Matsang Tsangpo / Sun Kosi) rivers. The Friendship Highway then descends along the Matsang Tsangpo through Nyalam, then more steeply through a canyon to Zhangmu.

While Mackin considered himself a geomorphologist, his bibliography reveals far greater scope to his actual research activities. In his doctoral thesis on the origin of surface features of the Big Horn Basin in Wyoming, he introduced the concept of lateral plantation by a stream essentially at grade, producing gravel-mantled terraces as the stream gradually deepens its valley, as opposed to formation of terraces by stream dissection of earlier alluvial plains. Mackin's further analysis led to publication in 1948 of the classic paper, Concept of the Graded River, which has been cited over 700 times. In this paper Mackin refers to the rapidity with which a graded stream responds to artificial changes - a warning of profound importance to stream engineers against altering natural equilibrium by diversion or damming or channel- improvements.

This concept still has value when applied within the framework of modern soil science, although a useful understanding of soils goes beyond the removal of nutrients from soil by harvested crops and their return in manure, lime, and fertilizer. The early geologists generally accepted the balance-sheet theory of soil fertility and applied it within the framework of their own discipline. They described soil as disintegrated rock of various sorts—granite, sandstone, glacial till, and the like. They went further, however, and described how the weathering processes modified this material and how geologic processes shaped it into landforms such as glacial moraines, alluvial plains, loess plains, and marine terraces. Geologist Nathaniel Shaler (1841–1906) monograph (1891) on the origin and nature of soils summarized the late 19th century geological concept of soils.

Map of Bankura District showing CD blocks and municipalities Sonamukhi is located at . Sonamukhi CD block is located in the eastern part of the district and belongs to the fertile low lying alluvial plains, similar to the predominating rice lands in the adjacent districts of West Bengal. Here, the eye constantly rests on wide expanses of rice fields, green in the rains but parched and dry in summer.O’Malley, L.S.S., ICS, Bankura, Bengal District Gazetteers, pp. 1-20, first published 1908, 1995 reprint, Government of West Bengal Sonamukhi CD block is bounded by the Kanksa and Galsi I CD blocks, in Bardhaman district across the Damodar, on the north, Patrasayer CD block on the east, Bishnupur and Onda CD blocks on the south and Gangajalghati and Barjora CD blocks on the west.

The Alluvial Plains of the centre of the island are for the most part the product of successive rain-storms and floods which have brought down from the mountains immense quantities of light debris which has been spread over the lower lands, principally by human agency exerted in the system of colmatage, which has been practised from time immemorial. This has resulted in the general raising of the land surface and incidentally in the natural reclamation of many acres of land in the lower parts of the Mesaoria, which once were arms of the sea.Hutchinson. Page 3 The word "Mesaoria" (sometimes spelled "Mesarya"), means "between the mountains" in Greek. For the most part, the Mesaoria is a flat, bare plain, with few trees except for those planted as windbreaks.

The west coast, composed of sedimentary formations, is more indented than the east coast, thus offering a number of harbors sheltered from cyclones, such as the harbor at Mahajanga. Deep bays and well-protected harbors have attracted explorers, traders, and pirates from Europe, Africa, and the Middle East since ancient times; thus, the area has served as an important bridge between Madagascar and the outside world. Silting up of harbors on this coast, caused by sediment from the high levels of erosion suffered inland in Madagascar, is a major problem. The broad alluvial plains found on the coast between Mahajanga and Toliara, which are believed to have great agricultural potential, are thinly inhabited, in many places covered with swamps of Madagascar mangroves, and remain largely unexplored, although they are the subject of mineral and hydrocarbon exploration activity.

Al Khatim Desert is a desert on the way to Al Ain from Abu Dhabi, Al Khatim desert is amazing location to do off-road riding experiences, United Arab Emirates. The local tour haris operators those who conduct 4x4 tours from Abu Dhabi created many fabulous track that meanders between untouched ranges of sand dunes, following the valleys that naturally occur where alluvial plains gently percolate underground run-off water from the Omani mountains in the direction of Abu Dhabi city. The beauty of this area is its quiet, rolling landscape, virgin dunes and the openness of the desert. Al Khatim Desert Road rock is a nice old desert high way with one lien each side it is in Al Khatim deserts in Abu Dhabi, It lies near the Road E22 in the middle between Abu Dhabi and Al Ain.

The first influx of migrants were the Hakkas and Hokkiens who came during the Dutch period, in which merchants and traders from the mainland Chinese coast sought to purchase hunting licenses from the Dutch or hide out in aboriginal villages to escape the Qing authorities. Most of the immigrants were young single males who were discouraged from staying on the island often referred to by Han as "The Gate of Hell" for its reputation in taking the lives of sailors and explorers. The Dutch originally sought to use their castle Zeelandia at Tayowan as a trading base between Japan and China, but soon realized the potential of the huge deer populations that roamed in herds of thousands along the alluvial plains of Taiwan's western regions. Deer were in high demand by the Japanese, who were willing to pay exorbitant prices for use of the hides in samurai armor.

The Hauraki Plains are a geographical feature and non-administrative area (though Hauraki Plains County Council existed from 1920 to 1989 and a statistical Area Unit remains) located in the northern North Island of New Zealand, at the lower (northern) end of the Thames Valley. They are located 75 kilometres south-east of Auckland, at the foot of the Coromandel Peninsula and occupy the southern portion of a rift valley bounded on the north-west by the Hunua Ranges, to the east by the Coromandel and Kaimai ranges and the west by a series of undulating hills which separate the plains from the much larger plains of the Waikato River. Broadly, the northern and southern parts of the Hauraki Plains are administered by the Hauraki District and the Matamata-Piako District respectively. The alluvial plains have been built up by sediment deposited by the Piako and Waihou rivers, which flow north to reach the sea at the Firth of Thames, and earlier by the ancestral Waikato River.

The most common animal in the park is by far the white-nosed coati, which one can expect to encounter dozens of times on the beach hike between La Leona and Sirena, digging for and feeding on the abundant moon crabs. Other animals in the park include Central American squirrel monkeys, mantled howler monkeys, both two-toed and three- toed sloths, agoutis, giant anteaters, great curassows, black hawks, spectacled owls, hummingbirds, 220 species of butterflies, golden orb spiders (who build huge webs), otters and raccoons. Four species of sea turtle (green, Pacific ridley, hawksbill, and leatherback) nest on the beaches. The abundance in wildlife can in part be explained by the variety of vegetation types, at least 13, including montane forest (more than half the park), cloud forest, jolillo forest (palm swamp), prairie forest, alluvial plains forest, swamp forest, freshwater herbaceous swamp and mangrove, together holding over 500 tree species, including purple heart, poponjoche, nargusta, banak, cow tree, espave and crabwood.

Other trace fossils from the Late Ordovician a little over probably represent land invertebrates, and there is clear evidence of numerous arthropods on coasts and alluvial plains shortly before the Silurian-Devonian boundary, about , including signs that some arthropods ate plants. Arthropods were well pre-adapted to colonise land, because their existing jointed exoskeletons provided protection against desiccation, support against gravity and a means of locomotion that was not dependent on water. The fossil record of other major invertebrate groups on land is poor: none at all for non-parasitic flatworms, nematodes or nemerteans; some parasitic nematodes have been fossilized in amber; annelid worm fossils are known from the Carboniferous, but they may still have been aquatic animals; the earliest fossils of gastropods on land date from the Late Carboniferous, and this group may have had to wait until leaf litter became abundant enough to provide the moist conditions they need.Selden 2001, "Terrestrialization of Animals," pp.

Guanzhong (, formerly romanised as Kwanchung) region, also known as the Guanzhong Basin, Wei River Basin, or uncommonly as the Shaanzhong region, is a historical region of China corresponding to the crescentic graben basin within present-day central Shaanxi, bounded between the Qinling Mountains in the south (known as Guanzhong's "South Mountains"), and the Huanglong Mountain, Meridian Ridge and Long Mountain ranges in the north (collectively known as its "North Mountains"). The central flatland area of the basin, known as the Guanzhong Plain, is made up of alluvial plains along the lower Wei River and its numerous tributaries and thus also called the Wei River Plain. The region is part of the Jin-Shaan Basin Belt, and is separated from its geological sibling — the Yuncheng Basin to its northeast — by the Yellow River section southwest of the Lüliang Mountains and north of the river's bend at the tri- provincial junction among Shaanxi, Shanxi and Henan. The name Guanzhong means "within the passes", referring to the four major mountain pass fortresses historically defending the region.

A most serious objection to the formation of continuous, high embankments along rivers bringing down considerable quantities of detritus, especially near a place where their fall has been abruptly reduced by descending from mountain slopes onto alluvial plains, is the danger of their bed being raised by deposit, producing a rise in the flood-level, and necessitating a raising of the embankments if inundations are to be prevented. Longitudinal sections of the Po River, taken in 1874 and 1901, show that its bed was materially raised during this period from the confluence of the Ticino to below Caranella, despite the clearance of sediment effected by the rush through breaches. Therefore, the completion of the embankments, together with their raising, would only eventually aggravate the injuries of the inundations they have been designed to prevent, as the escape of floods from the raised river must occur sooner or later. In the UK, problems of flooding of domestic properties around the turn of the 21st century have been blamed on inadequate planning controls which have permitted development on floodplains.

The Indus Valley Civilisation is named after the Indus river system in whose alluvial plains the early sites of the civilisation were identified and excavated. Following a tradition in archaeology, the civilisation is sometimes referred to as the Harappan, after its type site, Harappa, the first site to be excavated in the 1920s; this is notably true of usage employed by the Archaeological Survey of India after India's independence in 1947. Aryan indigenist writers like David Frawley use the terms "Sarasvati culture", the "Sarasvati Civilisation", the "Indus-Sarasvati Civilisation" or the "Sindhu-Saraswati Civilisation", because they consider the Ghaggar-Hakra river to be the same as the Sarasvati, a river mentioned several times in the Rig Veda, a collection of ancient Sanskrit hymns composed in the second millennium BCE. Recent geophysical research suggests that unlike the Sarasvati, whose descriptions in the Rig Veda are those of a snow- fed river, the Ghaggar-Hakra was a system of perennial monsoon-fed rivers, which became seasonal around the time that the civilisation diminished, approximately 4,000 years ago.

The Ribnik river is a short but significant tributary of the Sana The Sana in its upper course is fast mountain river with upland freshwater ecology, and its waters being very clear and cold. Gushing out of the karst plateau with Ovčara as most prominent summit (1576 m), between Klekovača and Vitorog mountains, and flows toward alluvial plains of the Bosanska Krajina with lowland freshwater ecology. Well-spring areal is located in the vicinity of Marići village, between surrounding villages of Gornja and Donja Pečka, Gornji and Donji Vrbljani, and Medna, on the territories of Ribnik and Mrkonjić Grad municipality not far from the town of Šipovo. The source itself consists of four major and water abundant karstic well-springs, with relatively high average discharge, and after about hundred meters first three individual wellsprings merge with a main course, which is set by the small stream of Korana coming from the right form direction of Gornja Pečka village, receiving the Sana springs one-by-one, with first three supplementing it from the left and, after just a little more than one kilometre downstream, with the fourth from the right.