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555:) is a type of fluvial-dominated delta formed from coarse sediments, as opposed to gently-sloping muddy deltas such as that of the Mississippi. For example, a mountain river depositing sediment into a freshwater lake would form this kind of delta. It is commonly a result of homopycnal flow. Such deltas are characterized by a tripartite structure of topset, foreset, and bottomset beds. River water entering the lake rapidly deposits its coarser sediments on the submerged face of the delta, forming steeping dipping foreset beds. The finer sediments are deposited on the lake bottom beyond this steep slope as more gently dipping bottomset beds. Behind the delta front, braided channels deposit the gently dipping beds of the topset on the delta plain.
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886:. As the river channels meander laterally across the top of the delta, the river is lengthened and its gradient is reduced, causing the suspended load to settle out in nearly horizontal beds over the delta's top. Topset beds are subdivided into two regions: the upper delta plain and the lower delta plain. The upper delta plain is unaffected by the tide, while the boundary with the lower delta plain is defined by the upper limit of tidal influence.
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416:, basin area, and basin elevation. Topography along passive margins tend to be more gradual and widespread over a greater area enabling sediment to pile up and accumulate over time to form large river deltas. Topography along active margins tends to be steeper and less widespread, which results in sediments not having the ability to pile up and accumulate due to the sediment traveling into a steep subduction trench rather than a shallow
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the receiving basin. With a high wave energy near shore and a steeper slope offshore, waves will make river deltas smoother. Waves can also be responsible for carrying sediments away from the river delta, causing the delta to retreat. For deltas that form further upriver in an estuary, there are complex yet quantifiable linkages between winds, tides, river discharge, and delta water levels.
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is laid down in this fashion, the shape of these deltas approximates a fan. The more often the flow changes course, the shape develops closer to an ideal fan because more rapid changes in channel position result in a more uniform deposition of sediment on the delta front. The
Mississippi and Ural River deltas, with their bird's feet, are examples of rivers that do not
365:(mid-channel sand and/or gravel bars at the mouth of a river). When this mid-channel bar is deposited at the mouth of a river, the flow is routed around it. This results in additional deposition on the upstream end of the mouth bar, which splits the river into two distributary channels. A good example of the result of this process is the
354:(such as during a flood), it spills out into a new course with a shorter route to the ocean, thereby obtaining a steeper, more stable gradient. Typically, when the river switches channels in this manner, some of its flow remains in the abandoned channel. Repeated channel-switching events build up a mature delta with a
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and ridges. This tends to produce a "dendritic" structure. Tidal deltas behave differently from river-dominated and wave-dominated deltas, which tend to have a few main distributaries. Once a wave-dominated or river-dominated distributary silts up, it is abandoned, and a new channel forms elsewhere.
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In wave-dominated deltas, wave-driven sediment transport controls the shape of the delta, and much of the sediment emanating from the river mouth is deflected along the coastline. The relationship between waves and river deltas is quite variable and largely influenced by the deepwater wave regimes of
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In both of these cases, depositional processes force redistribution of deposition from areas of high deposition to areas of low deposition. This results in the smoothing of the planform (or map-view) shape of the delta as the channels move across its surface and deposit sediment. Because the sediment
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up to the fresh stream feeding the head of tidal propagation. As a result, the tributaries are considered to be "subestuaries". The origin and evolution of a tidal freshwater delta involves processes that are typical of all deltas as well as processes that are unique to the tidal freshwater setting.
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that the river moves downstream by rolling and bouncing along the channel bottom. When the bed load reaches the edge of the delta front, it rolls over the edge, and is deposited in steeply dipping layers over the top of the existing bottomset beds. Underwater, the slope of the outermost edge of the
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The modern
Mississippi River delta is a good example of a fluvial-dominated delta whose outflow is buoyancy-dominated. Channel abandonment has been frequent, with seven distinct channels active over the last 5000 years. Other fluvial-dominated deltas include the Mackenzie delta and the Alta delta.
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rather than active margins. Along active margins, orogenic sequences cause tectonic activity to form over-steepened slopes, brecciated rocks, and volcanic activity resulting in delta formation to exist closer to the sediment source. When sediment does not travel far from the source, sediments that
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While some authors describe both lacustrine and marine locations of
Gilbert deltas, others note that their formation is more characteristic of the freshwater lakes, where it is easier for the river water to mix with the lakewater faster (as opposed to the case of a river falling into the sea or a
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At the mouth of a river, the change in flow conditions can cause the river to drop any sediment it is carrying. This sediment deposition can generate a variety of landforms, such as deltas, sand bars, spits, and tie channels. Landforms at the river mouth drastically alter the geomorphology and
432:, delta lobe switching, and auto cyclicity. Active margin river deltas tend to be much smaller and less abundant but may transport similar amounts of sediment. However, the sediment is never piled up in thick sequences due to the sediment traveling and depositing in deep subduction trenches.
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Historical data documents show that during the Roman Empire and Little Ice Age (times when there was considerable anthropogenic pressure), there was significant sediment accumulation in deltas. The industrial revolution has only amplified the impact of humans on delta growth and retreat.
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landslides occur and readjust overall slope stability. The foreset slope, thus created and maintained, extends the delta lobe outward. In cross section, foresets typically lie in angled, parallel bands, and indicate stages and seasonal variations during the creation of the
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in which the river water is slow to mix with the denser basin water and spreads out as a surface fan. This allows fine sediments to be carried a considerable distance before settling out of suspension. Beds in a hypocynal delta dip at a very shallow angle, around 1 degree.
1026:, buildings, sidewalks, and even landscaping. More than 1 billion tons of sand and gravel are produced in the United States alone. Not all sand and gravel quarries are former deltas, but for ones that are, much of the sorting is already done by the power of water.
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The formation of a delta is complicated, multiple, and cross-cutting over time, but in a simple delta three main types of bedding may be distinguished: the bottomset beds, foreset/frontset beds, and topset beds. This three-part structure may be seen on small scale by
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The combination of processes that create a tidal freshwater delta result in a distinct morphology and unique environmental characteristics. Many tidal freshwater deltas that exist today are directly caused by the onset of or changes in historical land use, especially
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The topset beds of an advancing delta are deposited in turn over the previously laid foresets, truncating or covering them. Topsets are nearly horizontal layers of smaller-sized sediment deposited on the top of the delta and form an extension of the landward
1485:
Hage, Sophie; Romans, Brian W.; Peploe, Thomas G. E.; Poyatos-Moré, Miquel; Haeri
Ardakani, Omid; Bell, Daniel; Englert, Rebecca G.; Kaempfe-Droguett, Sebastian A.; Nesbit, Paul R.; Sherstan, Georgia; Synnott, Dane P.; Hubbard, Stephen M. (24 October 2022).
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Dadson, Simon J.; Ashpole, Ian; Harris, Phil; Davies, Helen N.; Clark, Douglas B.; Blyth, Eleanor; Taylor, Christopher M. (4 December 2010). "Wetland inundation dynamics in a model of land surface climate: Evaluation in the Niger inland delta region".
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build up are coarser grained and more loosely consolidated, therefore making delta formation more difficult. Tectonic activity on active margins causes the formation of river deltas to form closer to the sediment source which may affect channel
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A tidal freshwater delta is a sedimentary deposit formed at the boundary between an upland stream and an estuary, in the region known as the "subestuary". Drowned coastal river valleys that were inundated by rising sea levels during the late
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The bottomset beds are created from the lightest suspended particles that settle farthest away from the active delta front, as the river flow diminishes into the standing body of water and loses energy. This suspended load is deposited by
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tends to form
Gilbert-type deltas. Outflow dominated by turbulent friction is prone to channel bifurcation, while buoyancy-dominated outflow produces long distributaries with narrow subaqueous natural levees and few channel bifurcations.
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Galloway, W.E., 1975, Process framework for describing the morphologic and stratigraphic evolution of deltaic depositional systems, in
Brousard, M.L., ed., Deltas, Models for Exploration: Houston Geological Society, Houston, Texas, pp.
510:, in which the river water rapidly mixes with basin water and abruptly dumps most of its sediment load. Where the river water has a higher density than basin water, typically from a heavy load of sediment, the delta is characterized by
1065:, and sea access for trade. Deltas often host extensive industrial and commercial activities as well as agricultural land which are often in conflict. Some of the world's largest regional economies are located on deltas such as the
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KUENZER C. and RENAUD, F. 2012: Climate Change and
Environmental Change in River Deltas Globally. In (eds.): Renaud, F. and C. Kuenzer 2012: The Mekong Delta System – Interdisciplinary Analyses of a River Delta, Springer,
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Goodbred, S. L.; Kuehl, S. A. (2000). "The significance of large sediment supply, active tectonism, and eustasy on margin sequence development: Late
Quaternary stratigraphy and evolution of the Ganges-Brahmaputra delta".
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Syvitski, James P. M.; Kettner, Albert J.; Overeem, Irina; Hutton, Eric W. H.; Hannon, Mark T.; Brakenridge, G. Robert; Day, John; Vörösmarty, Charles; Saito, Yoshiki; Giosan, Liviu; Nicholls, Robert J. (2009-10-01).
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construction in the basins feeding deltas have reduced river sediment delivery to many deltas in recent decades. This change means that there is less sediment available to maintain delta landforms, and compensate for
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Nienhuis, J.H., Ashton, A.D., Edmonds, D.A., Hoitink, A.J.F., Kettner, A.J., Rowland, J.C. and Törnqvist, T.E., 2020. Global-scale human impact on delta morphology has led to net land area gain. Nature, 577(7791),
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along the east coastline of the United States. Research has demonstrated that the accumulating sediments in this estuary derive from post-European settlement deforestation, agriculture, and urban development.
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The foreset beds in turn are deposited in inclined layers over the bottomset beds as the active lobe advances. Foreset beds form the greater part of the bulk of a delta, (and also occur on the lee side of
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processes, depending on the strength of each. The other two factors that play a major role are landscape position and the grain size distribution of the source sediment entering the delta from the river.
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Day, John W.; Agboola, Julius; Chen, Zhongyuan; D’Elia, Christopher; Forbes, Donald L.; Giosan, Liviu; Kemp, Paul; Kuenzer, Claudia; Lane, Robert R.; Ramachandran, Ramesh; Syvitski, James (2016-12-20).
2097:"Geological and Petrophysical Characterization of the Ferron Sandstone for 3-D Simulation of a Fluvial-deltaic Reservoir". By Thomas C. Chidsey, Thomas C. Chidsey Jr (ed), Utah Geological Survey, 2002.
113:, and receiving basin processes that redistribute, sequester, and export that sediment. The size, geometry, and location of the receiving basin also plays an important role in delta evolution.
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Irwin III, R. et al. 2005. An intense terminal epoch of widespread fluvial activity on early Mars: 2. Increased runoff and paleolake development. Journal of
Geophysical Research: 10. E12S15
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into the sea and the convexly curved seaward side of the triangle. Despite making comparisons to other river systems deltas, Herodotus did not describe them as "deltas". The Greek historian
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Fluvial-dominated deltas are further distinguished by the relative importance of the inertia of rapidly flowing water, the importance of turbulent bed friction beyond the river mouth, and
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Petráš, Rudolf; Mecko, Julian; Oszlányi, Július; Petrášová, Viera; Jamnická, Gabriela (August 2013). "Landscape of Danube inland-delta and its potential of poplar bioenergy production".
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Fluvial-dominated deltas are found in areas of low tidal range and low wave energy. Where the river water is nearly equal in density to the basin water, the delta is characterized by
5523:
6015:
1351:
Pasternack, Gregory B.; Brush, Grace S.; Hilgartner, William B. (2001-04-01). "Impact of historic land-use change on sediment delivery to a
Chesapeake Bay subestuarine delta".
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Darby, Stephen E.; Hackney, Christopher R.; Leyland, Julian; Kummu, Matti; Lauri, Hannu; Parsons, Daniel R.; Best, James L.; Nicholas, Andrew P.; Aalto, Rolf (November 2016).
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Pasternack, Gregory B; Brush, Grace S (2002-03-01). "Biogeomorphic controls on sedimentation and substrate on a vegetated tidal freshwater delta in upper Chesapeake Bay".
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Hackney, Christopher R.; Darby, Stephen E.; Parsons, Daniel R.; Leyland, Julian; Best, James L.; Aalto, Rolf; Nicholas, Andrew P.; Houseago, Robert C. (2020-03-01).
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1406:"Rice production and food security in Asian Mega deltas—A review on characteristics, vulnerabilities and agricultural adaptation options to cope with climate change"
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Orson, R. A.; Simpson, R. L.; Good, R. E. (1992). "The paleoecological development of a late Holocene, tidal freshwater marsh of the upper Delaware River estuary".
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1142:. Finding deltas is a major sign that Mars once had large amounts of water. Deltas have been found over a wide geographical range. Below are pictures of a few.
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Backert, Nicolas; Ford, Mary; Malartre, Fabrice (February 2010). "Architecture and sedimentology of the Kerinitis Gilbert-type fan delta, Corinth Rift, Greece".
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Pasternack, Gregory B.; Hilgartner, William B.; Brush, Grace S. (2000-09-01). "Biogeomorphology of an upper Chesapeake Bay river-mouth tidal freshwater marsh".
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Ottinger, M.; Kuenzer, C.; LIU; Wang, S.; Dech, S. (2013). "Monitoring Land Cover Dynamics in the Yellow River Delta from 1995 to 2010 based on Landsat 5 TM".
105:, or (more rarely) another river that cannot carry away the supplied sediment. It is so named because its triangle shape resembles the uppercase Greek letter
3377:
Eslami, Sepehr; Hoekstra, Piet; Nguyen Trung, Nam; Ahmed Kantoush, Sameh; Van Binh, Doan; Duc Dung, Do; Tran Quang, Tho; van der Vegt, Maarten (2019-12-10).
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Seto, Karen C. (December 2011). "Exploring the dynamics of migration to mega-delta cities in Asia and Africa: Contemporary drivers and future scenarios".
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Milliman, J. D.; Syvitski, J. P. M. (1992). "Geomorphic/Tectonic Control of Sediment Discharge to the Ocean: The Importance of Small Mountainous Rivers".
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tend to have dendritic estuaries with many feeder tributaries. Each tributary mimics this salinity gradient from its brackish junction with the mainstem
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Most large river deltas discharge to intra-cratonic basins on the trailing edges of passive margins due to the majority of large rivers such as the
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for the landform at the mouth of the river, the word delta is first attested in the English-speaking world in the late 18th century, in the work of
1987:
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316:, which builds up to form the river delta. Over time, this single channel builds a deltaic lobe (such as the bird's-foot of the Mississippi or
522:. When the river water is less dense than the basin water, as is typical of river deltas on an ocean coastline, the delta is characterized by
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Orton, G.J.; Reading, H.G. (1993). "Variability of deltaic processes in terms of sediment supply, with particular emphasis on grain size".
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1061:. This makes deltas a common location for civilizations to flourish due to access to flat land for farming, freshwater for sanitation and
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salt lake, where less dense fresh water brought by the river stays on top longer). Gilbert himself first described this type of delta on
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723:. Sometimes a river divides into multiple branches in an inland area, only to rejoin and continue to the sea. Such an area is called an
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3815:
3076:"Projections of declining fluvial sediment delivery to major deltas worldwide in response to climate change and anthropogenic stress"
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Neuenschwander, A.L.; Crawford, M.M.; Ringrose, S. (2002). "Monitoring of seasonal flooding in the Okavango Delta using EO-1 data".
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Fagherazzi S., 2008, Self-organization of tidal deltas, Proceedings of the National Academy of Sciences, vol. 105 (48): 18692–18695,
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Hart, Jeff; Hunter, John (2004). "Restoring Slough and River Banks with Biotechnical Methods in the Sacramento-San Joaquin Delta".
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on the bed decreases, which results in the deposition of sediment within the channel and a rise in the channel bed relative to the
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920:, causing some deltas to start losing land. Declines in river sediment delivery are projected to continue in the coming decades.
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Elliot, T. 1986. Deltas. in H. G. Reading (ed.). Sedimentary environments and facies. Backwell Scientific Publications, Oxford.
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In some cases, a river flowing into a flat arid area splits into channels that evaporate as it progresses into the desert. The
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rivers to the Nile Delta, referring to both as islands, but did not apply the word delta. According to the Greek geographer
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Brush, G. S. (1984). "Patterns of recent sediment accumulation in Chesapeake Bay (Virginia-Maryland, U.S.A.) tributaries".
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Anthony, Edward J. (2015-03-01). "Wave influence in the construction, shaping and destruction of river deltas: A review".
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3448:"Impact of human interventions and coastal processes along the Nile Delta coast, Egypt during the past twenty-five years"
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Dunn, Frances E; Darby, Stephen E; Nicholls, Robert J; Cohen, Sagy; Zarfl, Christiane; Fekete, Balázs M (2019-08-06).
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In a tidal delta, new distributaries are formed during times when there is a lot of water around – such as floods or
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Blum, M.D.; Törnqvist, T.E. (2000). "Fluvial responses to climate and sea-level change: a review and look forward".
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Miall, A. D. 1979. Deltas. in R. G. Walker (ed) Facies Models. Geological Association of Canada, Hamilton, Ontario.
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Renaud, F. and C. Kuenzer 2012: The Mekong Delta System – Interdisciplinary Analyses of a River Delta, Springer,
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of the river channel becomes lower because the river channel is longer but has the same change in elevation (see
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2120:"Dr. Gregory B. Pasternack – Watershed Hydrology, Geomorphology, and Ecohydraulics :: TFD Hydrometeorology"
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2219:"Gregory B. Pasternack – Watershed Hydrology, Geomorphology, and Ecohydraulics :: Tidal Freshwater Deltas"
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Deltas are typically classified according to the main control on deposition, which is a combination of river,
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are some of the most extreme examples of the devastation caused to deltas by damming and diversion of water.
864:). The sediment particles within foreset beds consist of larger and more variable sizes, and constitute the
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in 1885. Elsewhere, similar structures occur, for example, at the mouths of several creeks that flow into
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Urban areas and human habitation tend to be located in lowlands near water access for transportation and
109:, Δ. The size and shape of a delta are controlled by the balance between watershed processes that supply
3379:"Tidal amplification and salt intrusion in the Mekong Delta driven by anthropogenic sediment starvation"
1664:"Dr. Gregory B. Pasternack – Watershed Hydrology, Geomorphology, and Ecohydraulics :: TFD Modeling"
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River deltas form when a river carrying sediment reaches a body of water, such as a lake, ocean, or a
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Perillo, G. M. E. 1995. Geomorphology and Sedimentology of Estuaries. Elsevier Science B.V., New York.
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There are many other lesser factors that could explain why the majority of river deltas form along
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Minderhoud, P S J; Erkens, G; Pham, V H; Bui, V T; Erban, L; Kooi, H; Stouthamer, E (2017-06-01).
2150:"Hydrometeorological controls on water level in a vegetated Chesapeake Bay tidal freshwater delta"
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deltas, as seen by their name, avulse frequently and more closely approximate an ideal fan shape.
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983:. There are small-scale efforts to correct these issues, improve delta environments and increase
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Meade, Robert H. (January 1994). "Suspended sediments of the modern Amazon and Orinoco rivers".
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Slingerland, R. and N. D. Smith (1998), "Necessary conditions for a meandering-river avulsion",
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discharging along passive continental margins. This phenomenon is due mainly to three factors:
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1488:"High rates of organic carbon burial in submarine deltas maintained on geological timescales"
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640:. These distributaries slowly silt up at a more or less constant rate until they fizzle out.
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120:, as they are major agricultural production centers and population centers. They can provide
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WISDOM Water-related Information System for the Sustainable Development of the Mekong Delta
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Gottschalk, L. C. (1945). "Effects of soil erosion on navigation in upper Chesapeake Bay".
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3185:"Impacts of 25 years of groundwater extraction on subsidence in the Mekong delta, Vietnam"
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important, with different species' assemblages depending on their landscape position. On
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2822:"Fluvial sediment supply to a mega-delta reduced by shifting tropical-cyclone activity"
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674:. These ideas are well illustrated by the many tidal freshwater deltas prograding into
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856:. These beds are laid down in horizontal layers and consist of the finest grain sizes.
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deltas), pushing its mouth into the standing water. As the deltaic lobe advances, the
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1022:. Sand and gravel are often quarried from these old deltas and used in concrete for
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is the largest delta in the world, and one of the most fertile regions in the world.
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6030:
5722:
5626:
5578:
5490:
5383:
5081:
4932:
4766:
4741:
4736:
4711:
4661:
4487:
4347:
4265:
4230:
3896:
3824:
3757:
3737:
3717:
3573:
3557:
3508:
3459:
3418:
3400:
3330:
3322:
3271:
3222:
3206:
3138:
3097:
3035:
3027:
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2846:
2829:
2802:
2757:
2738:
2734:
2697:
2650:
2621:
2590:
2554:
2503:
2474:
2457:
2429:
2367:
2334:
2281:
2174:
2069:
1920:
1853:
1798:
1696:(4th ed.). Upper Saddle River, N.J.: Pearson Prentice Hall. pp. 289–306.
1569:
1509:
1467:
1417:
1370:
1322:
1270:
1246:
568:
429:
374:
161:
6517:
196:
19:
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6797:
6734:
6492:
6487:
6343:
6234:
6000:
5967:
5828:
5780:
5656:
5631:
5440:
5393:
5318:
5163:
5148:
4969:
4751:
4696:
4563:
4472:
4467:
4352:
4235:
4124:
3911:
3873:
3858:
3761:
3309:"River bank instability from unsustainable sand mining in the lower Mekong River"
2106:
2007:
1471:
1232:
904:
900:
870:
807:
799:
775:
719:
In rare cases, the river delta is located inside a large valley and is called an
560:
515:
256:
46:
2761:
2608:
Leconte, Robert; Pietroniro, Alain; Peters, Daniel L.; Prowse, Terry D. (2001).
1558:
Celoria, Francis (1966). "Delta as a geographical concept in Greek literature".
1034:
874:
6993:
6872:
6679:
6353:
5864:
5818:
5813:
5785:
5752:
5621:
5480:
5408:
5398:
5248:
5193:
5111:
5106:
5101:
4362:
4357:
4320:
4260:
4240:
4114:
3981:
3931:
3883:
3843:
3838:
3609:
3464:
3447:
3405:
3210:
3102:
3075:
2967:
2353:
1560:
1513:
964:
960:
917:
883:
767:
675:
458:
424:
366:
297:
149:
106:
3741:
3721:
3326:
3276:
3251:
3142:
2702:
2685:
1267: – Delta produced by the Nile River at its mouth in the Mediterranean Sea
6947:
6882:
6636:
6207:
6078:
5972:
5937:
5838:
5833:
5808:
5338:
5303:
5278:
5128:
5091:
4974:
4957:
4907:
4848:
4823:
4686:
4613:
4285:
4119:
4001:
3961:
3906:
3569:
3473:
3414:
3344:
3285:
3218:
3150:
3111:
3049:
2975:
2684:
van Beek, Eelco; Bozorgy, Babak; Vekerdy, Zoltán; Meijer, Karen (June 2008).
2379:
2293:
1431:
1382:
1139:
1115:
1108:
1074:
936:
932:
924:
732:
663:
564:
301:
273:
3126:
2610:"Effects of flow regulation on hydrologic patterns of a large, inland delta"
2256:
6867:
6653:
6568:
6303:
6293:
6256:
6187:
6162:
6064:
5843:
5823:
5727:
5465:
5348:
5268:
5228:
5218:
5188:
4838:
4726:
4598:
4593:
4492:
4482:
4427:
4052:
3863:
3587:
3522:
3432:
3236:
2858:
1749:(2nd ed.). Chichester, West Sussex, UK: Wiley-Blackwell. p. 388.
1249: – Rapid abandonment of a river channel and formation of a new channel
1240:
1096:
1050:
980:
975:
rise. Anthropogenic activities can also destabilise river channels through
840:
831:
811:
803:
671:
628:
604:
409:
393:
378:
355:
343:
317:
296:. When the flow enters the standing water, it is no longer confined to its
269:
216:
117:
35:
23:
3005:
445:
6892:
6754:
6744:
6643:
6522:
6505:
6392:
6373:
6202:
6192:
6182:
5977:
5952:
5947:
5917:
5700:
5676:
5641:
5450:
5353:
5273:
5233:
5086:
4989:
4803:
4776:
4771:
4633:
4623:
4618:
4573:
4568:
4558:
4507:
4497:
4220:
4068:
4019:
3986:
3976:
2662:
2594:
1127:
1104:
994:
While nearly all deltas have been impacted to some degree by humans, the
976:
952:
896:
688:
650:
637:
350:. This destabilizes the river channel. If the river breaches its natural
262:
224:
179:
mentions the Delta fourteen times, as "the Delta, as it is called by the
169:
refers to it as the "triangular Nilotic land", though not as a "delta".
133:
82:
30:
3376:
2850:
2654:
1810:
6852:
6548:
6532:
6512:
6378:
6368:
6271:
6239:
6222:
6217:
6212:
5957:
5892:
5681:
5661:
5445:
5418:
5203:
5116:
4917:
4853:
4813:
4731:
4656:
4447:
4305:
4109:
4073:
4014:
3941:
3921:
3335:
2686:"Limits to agricultural growth in the Sistan Closed Inland Delta, Iran"
2515:
2387:
1264:
1100:
1062:
1058:
995:
968:
944:
861:
756:
612:
413:
362:
361:
Another way these distributary networks form is from the deposition of
347:
300:
and expands in width. This flow expansion results in a decrease in the
145:
54:
6246:
6073:
3561:
2627:
10.1002/1099-1646(200101/02)17:1<51::AID-RRR588>3.0.CO;2-V
2441:
1998:
Bernard Biju-Duval, J. Edwin Swezey. "Sedimentary Geology". Page 183.
1581:
1422:
1405:
1126:
is the largest delta emptying into a body of fresh water, in its case
6674:
6648:
6383:
6197:
6172:
6152:
5982:
5887:
5671:
5435:
5428:
5403:
5313:
5018:
4858:
4818:
4646:
4583:
4502:
4432:
3946:
3936:
3891:
3040:
1138:
Researchers have found a number of examples of deltas that formed in
1046:
1014:
Ancient deltas are a benefit to the economy due to their well-sorted
923:
The extensive anthropogenic activities in deltas also interfere with
853:
727:, and often occurs on former lake beds. The term was first coined by
584:
572:
519:
490:
293:
170:
166:
102:
4168:
3513:
3488:
3031:
2507:
2371:
1374:
899:
upstream of deltas can radically alter delta environments. Upstream
6862:
6857:
6847:
6669:
6621:
6616:
6599:
6457:
6437:
6402:
6281:
6276:
5932:
5742:
5288:
5283:
5208:
4786:
4781:
4608:
4523:
4382:
4207:
4042:
3916:
3793:
2942:"Approaches to defining deltaic sustainability in the 21st century"
2433:
1802:
1573:
1123:
1023:
865:
790:
can be used to describe very large Asian river deltas, such as the
771:
654:
627:
is also an important control in tide-dominated deltas, such as the
531:
321:
313:
220:
188:
152:. The triangular shape of the Nile Delta was known to audiences of
110:
74:
66:
6318:
1747:
Sedimentology and sedimentary basins: from turbulence to tectonics
284:
192:
6897:
6877:
6442:
6407:
6229:
6131:
5942:
5902:
5872:
5850:
5470:
5258:
5158:
4922:
4796:
4641:
4517:
4512:
4422:
4417:
4407:
4327:
4029:
3991:
3926:
3853:
1252:
948:
928:
913:
735:, which he visited in 1800. Other prominent examples include the
692:
658:
624:
535:
405:
261:
states that "the delta of the land of the Indians is made by the
180:
125:
94:
5691:
5061:
3252:"Regional hydrological research perspectives in the Niger Delta"
1029:
711:
6631:
6422:
6412:
6308:
5927:
5253:
4947:
4942:
4477:
4457:
4412:
4397:
4255:
4009:
3956:
3951:
3781:
1019:
752:
748:
691:, do not form a delta but enter into the sea in the form of an
397:
252:
200:
2751:
2354:"Sedimentation cycles in a river-mouth tidal freshwater marsh"
760:
342:
As the gradient of the river channel decreases, the amount of
6472:
6427:
6417:
6397:
6348:
6313:
6288:
6261:
6157:
4828:
4791:
4550:
4452:
4402:
4387:
4377:
4342:
4337:
4332:
4280:
4275:
4225:
2607:
1258:
755:
has one in the valley on the Slovak–Hungarian border between
700:
632:
608:
401:
351:
325:
121:
86:
81:
and enters slower-moving or stagnant water. This occurs at a
78:
3002:
2724:
2683:
1484:
873:
of these sediments. As the foresets accumulate and advance,
687:
Other rivers, particularly those on coasts with significant
124:
defence and can impact drinking water supply. They are also
6626:
6447:
6323:
6100:
5423:
4962:
4952:
4927:
4437:
4367:
4315:
4310:
4047:
2286:
10.1672/0277-5212(2000)020<0520:boaucb>2.0.co;2
1042:
1015:
494:
389:
184:
98:
50:
39:
3306:
2754:
IEEE International Geoscience and Remote Sensing Symposium
6266:
6177:
5485:
5475:
4442:
4245:
4037:
2571:
2269:
2148:
Pasternack, Gregory B.; Hinnov, Linda A. (October 2003).
1350:
1255: – Partially enclosed coastal body of brackish water
931:
delta processes. People living on deltas often construct
908:
251:'he calls the island a delta'). The Roman author
239:
90:
2819:
1960:
1049:. Its delta, where the delta islands remain between the
3790:– A coastalwiki.org page on wave-dominated river deltas
3182:
1938:
1936:
1934:
1728:
1726:
3747:
3073:
2352:
Pasternack, Gregory B.; Brush, Grace S. (1998-09-01).
2249:
Physical dynamics of tidal freshwater delta evolution
2938:
1948:
1931:
1723:
1222:
514:
in which the river water hugs the basin bottom as a
2051:
2029:. US Government Printing Office. pp. 104–107.
144:A river delta is so named because the shape of the
3536:Maselli, Vittorio; Trincardi, Fabio (2013-05-31).
2251:(PhD dissertation). The Johns Hopkins University.
308:. As a result, sediment drops out of the flow and
3661:"Appendix A: The Major River Deltas Of The World"
2950:. Sustainability of Future Coasts and Estuaries.
2204:
2202:
967:, and constructing infrastructure all accelerate
6945:
3535:
2929:. Tokyo, Japan: Tokyo Geographical Society, 2003
2491:
2147:
1877:
1778:
1710:
939:from floods on deltas, and therefore means that
890:
631:, which may be mainly submarine, with prominent
16:Silt deposition landform at the mouth of a river
3446:Ali, Elham M.; El-Magd, Islam A. (2016-03-01).
2351:
2314:
1869:
1867:
1443:
1441:
6703:A Directory of Important Wetlands in Australia
3788:Wave-dominated river deltas on coastalwiki.org
2927:Morphology and Sediments of Large River Deltas
2199:
377:often enough to form a symmetrical fan shape.
304:, which diminishes the ability of the flow to
265:no less than is the case with that of Egypt".
6788:Bangladesh Haor and Wetland Development Board
6713:Ramsar Classification System for Wetland Type
6116:
5324:Stable isotope analysis in aquatic ecosystems
5034:
4184:
3809:
1834:
1604:"Word Stories: Unexpected Relatives for Xmas"
1403:
1312:
1209:, as seen by Mars Global Surveyor. Image in
3489:"Water returns to arid Colorado River delta"
2905:
2903:
1902:
1864:
1694:Principles of sedimentology and stratigraphy
1438:
5389:Freshwater environmental quality parameters
4140:List of rivers that have reversed direction
2614:Regulated Rivers: Research & Management
1830:
1828:
1774:
1772:
1770:
1768:
1766:
501:
6123:
6109:
5041:
5027:
4191:
4177:
3816:
3802:
3445:
2640:
2419:
2246:
2093:
2091:
1633:"How a Delta Forms Where River Meets Lake"
643:
3577:
3512:
3463:
3422:
3404:
3334:
3275:
3226:
3101:
3039:
2900:
2701:
2625:
1421:
951:. In addition to interference with delta
336:Sacramento–San Joaquin (California) Delta
288:A delta forms where a river meets a lake.
3632:"Why are cities located where they are?"
3452:The Egyptian Journal of Aquatic Research
3124:
3006:"Sinking deltas due to human activities"
1979:
1977:
1975:
1825:
1763:
1261: – Ridge or wall to hold back water
1028:
1009:
895:Human activities in both deltas and the
825:
821:
710:
619:
598:
590:
444:
330:
283:
45:
29:
18:
2998:
2996:
2088:
2026:The topographic features of lake shores
2019:
1557:
1447:
183:", including describing the outflow of
69:shaped like a triangle, created by the
6946:
6808:Meadowview Biological Research Station
6740:Greenhouse gas emissions from wetlands
5048:
1744:
1404:Schneider, Pia; Asch, Folkard (2020).
1243: – Fan-shaped deposit of sediment
148:approximates the triangular uppercase
6104:
5577:
5576:
5060:
5022:
4198:
4172:
3797:
3486:
2536:
2454:
1972:
1966:
1954:
1942:
1732:
1691:
1354:Earth Surface Processes and Landforms
907:and hydrological engineering such as
3823:
3249:
3125:Syvitski, James P. M. (2008-04-01).
2993:
2947:Estuarine, Coastal and Shelf Science
2792:
2158:Estuarine, Coastal and Shelf Science
1553:
1551:
1549:
1547:
1545:
1543:
1410:Journal of Agronomy and Crop Science
1346:
1344:
116:River deltas are important in human
6803:Irish Peatland Conservation Council
5652:Oceanic physical-biological process
5514:List of freshwater ecoregions (WWF)
2909:Robert L. Bates, Julia A. Jackson,
2756:. Vol. 6. pp. 3124–3126.
1278:– Complex delta in south-east China
905:anti-erosion agricultural practices
13:
4887:Integrated coastal zone management
3776:Louisiana State University Geology
3629:
3602:"Mineral Photos – Sand and Gravel"
1925:10.1111/j.1365-3091.1993.tb01347.x
1528:from the original on 20 April 2023
989:sedimentation enhancing strategies
745:Sacramento–San Joaquin River Delta
14:
7005:
3769:
2895:The Penguin Dictionary of Geology
1540:
1341:
1133:
546:
6928:
6927:
6916:
6085:
6084:
6072:
6058:
5690:
5362:
5179:Colored dissolved organic matter
5003:
5002:
4540:
4533:
4153:
4152:
2074:10.1111/j.1365-3091.2009.01105.x
2033:from the original on 25 May 2024
1327:10.1046/j.1365-3091.2000.00008.x
1225:
1198:
1182:
1166:
1147:
1111:, is the world's largest delta.
706:
695:. Notable examples include the
338:at flood stage, early March 2009
6299:Flooded grasslands and savannas
5524:Latin America and the Caribbean
3849:Drainage system (geomorphology)
3702:
3690:
3679:from the original on 2022-02-22
3653:
3623:
3594:
3529:
3487:Witze, Alexandra (2014-03-20).
3480:
3439:
3370:
3359:from the original on 2021-06-13
3300:
3243:
3176:
3165:from the original on 2024-05-25
3118:
3067:
3056:from the original on 2021-05-05
2982:from the original on 2024-05-25
2932:
2919:
2887:
2876:from the original on 2021-06-13
2813:
2807:10.1016/j.gloenvcha.2011.08.005
2786:
2745:
2718:
2690:Irrigation and Drainage Systems
2677:
2634:
2601:
2575:Journal of Geophysical Research
2565:
2530:
2485:
2448:
2413:
2402:from the original on 2019-02-07
2345:
2308:
2263:
2240:
2229:from the original on 2018-09-30
2211:
2188:from the original on 2018-07-24
2141:
2130:from the original on 2018-10-03
2112:
2045:
2013:
1992:
1896:
1887:
1738:
1685:
1674:from the original on 2018-09-30
1656:
1645:from the original on 2017-12-12
1625:
1614:from the original on 2020-10-22
518:that deposits its sediments as
173:'s description of Egypt in his
6006:Ecological values of mangroves
5549:North Pacific Subtropical Gyre
4985:Region of freshwater influence
3859:Strahler number (stream order)
3190:Environmental Research Letters
3081:Environmental Research Letters
2911:Dictionary of Geological Terms
2739:10.1016/j.biombioe.2012.05.022
1596:
1478:
1397:
1306:
1297:
1288:
781:
731:for the middle reaches of the
1:
6823:Wildfowl & Wetlands Trust
6813:Society of Wetland Scientists
4747:Large-scale coastal behaviour
4579:Beaches in estuaries and bays
3606:Mineral Information Institute
3256:Hydrological Sciences Journal
3250:ABAM, T. K. S. (2001-02-01).
2339:10.1016/s0169-555x(01)00139-8
2179:10.1016/s0272-7714(03)00106-9
1858:10.1016/S0037-0738(00)00041-5
1282:
1211:Margaritifer Sinus quadrangle
1191:Margaritifer Sinus quadrangle
891:Existential threats to deltas
551:A Gilbert delta (named after
191:likened the land between the
6438:Peatland, mire, and quagmire
6130:
6026:Marine conservation activism
6011:Fisheries and climate change
3782:http://www.wisdom.eoc.dlr.de
3762:10.1016/j.apgeog.2013.07.003
2559:10.1016/1040-6182(94)90019-1
2479:10.1016/0009-2541(84)90074-3
1472:10.1016/j.margeo.2014.12.004
1041:) flows through the city of
985:environmental sustainability
682:
449:Delta lobe switching in the
279:
240:
139:
53:satellite photograph of the
7:
6708:National Wetlands Inventory
6021:Human impact on marine life
5898:Davidson Seamount § Ecology
5134:Aquatic population dynamics
2795:Global Environmental Change
2762:10.1109/IGARSS.2002.1027105
1218:
1084:
10:
7010:
6793:Delta Waterfowl Foundation
3669:Louisiana State University
3465:10.1016/j.ejar.2016.01.002
3406:10.1038/s41598-019-55018-9
2968:10.1016/j.ecss.2016.06.018
2247:Pasternack, G. B. (1998).
2006:. Editions TECHNIP, 2002.
1514:10.1038/s41561-022-01048-4
1088:
232:
132:, they are also important
6911:
6835:
6780:
6730:
6721:
6693:
6662:
6609:
6581:
6541:
6145:
6138:
6052:
5991:
5863:
5799:
5761:
5708:
5699:
5688:
5637:Marine primary production
5589:
5585:
5572:
5531:List of marine ecoregions
5506:
5371:
5360:
5074:
5070:
5056:
4998:
4900:
4867:
4672:
4632:
4549:
4531:
4206:
4148:
4097:
4061:
4028:
4000:
3882:
3831:
3742:10.1007/978-94-007-3962-8
3722:10.1007/978-94-007-3962-8
3630:A., Stefan (2017-05-22).
3327:10.1038/s41893-019-0455-3
3277:10.1080/02626660109492797
3143:10.1007/s11625-008-0043-3
2703:10.1007/s10795-008-9045-7
1986:. (Available archived at
1984:Characteristics of deltas
1638:Jet Propulsion Laboratory
1156:Ismenius Lacus quadrangle
1053:, starts near the centre.
209:Onesicritus of Astypalaea
6772:Wetland indicator status
5883:Coastal biogeomorphology
5878:Marine coastal ecosystem
4692:Coastal biogeomorphology
3211:10.1088/1748-9326/aa7146
3103:10.1088/1748-9326/ab304e
2539:Quaternary International
1097:Ganges–Brahmaputra Delta
869:delta is created at the
502:Fluvial-dominated deltas
440:
241:kalei de tēn nēson délta
233:καλεῖ δὲ τὴν νῆσον δέλτα
6483:Freshwater swamp forest
5791:Paradox of the plankton
5602:Diel vertical migration
5496:Freshwater swamp forest
5214:GIS and aquatic science
5062:General components and
3972:River channel migration
2925:Hori, K. and Saito, Y.
1720:(Boulder), 26, 435–438.
943:can not compensate for
644:Tidal freshwater deltas
534:. Outflow dominated by
34:Satellite image of the
6818:Wetlands International
6589:List of wetland plants
5617:Large marine ecosystem
5309:Shoaling and schooling
4589:Coastal morphodynamics
3902:Bar (river morphology)
3608:. 2011. Archived from
3131:Sustainability Science
2643:Ecological Restoration
2223:pasternack.ucdavis.edu
2124:pasternack.ucdavis.edu
1782:The Journal of Geology
1745:Leeder, M. R. (2011).
1668:pasternack.ucdavis.edu
1175:Lunae Palus quadrangle
1099:, which spans most of
1075:European Low Countries
1054:
835:
729:Alexander von Humboldt
716:
697:Gulf of Saint Lawrence
616:
486:
339:
289:
58:
57:(shown in false color)
43:
27:
6463:Salt pannes and pools
6036:Marine protected area
5963:Salt pannes and pools
5738:Marine larval ecology
5713:Census of Marine Life
5597:Deep scattering layer
5554:San Francisco Estuary
5519:Africa and Madagascar
5344:Underwater camouflage
5124:Aquatic biomonitoring
5064:freshwater ecosystems
4980:Physical oceanography
4084:Erosion and tectonics
4079:Degradation (geology)
3314:Nature Sustainability
2727:Biomass and Bioenergy
1107:and empties into the
1091:Category:River deltas
1032:
1010:Deltas in the economy
850:sediment gravity flow
829:
822:Sedimentary structure
741:Peace–Athabasca Delta
714:
668:intensive agriculture
620:Tide-dominated deltas
602:
591:Wave-dominated deltas
448:
334:
287:
77:that is carried by a
49:
33:
22:
5771:Marine bacteriophage
5733:Marine invertebrates
4809:Submergent coastline
4762:Marine transgression
4717:Discordant coastline
4702:Concordant coastline
4105:Deposition (geology)
3832:Large-scale features
2595:10.1029/2010JD014474
2495:Estuaries and Coasts
2359:Estuaries and Coasts
1989:– checked Dec 2008.)
1000:Colorado River Delta
774:is one example. See
721:inverted river delta
85:, when it enters an
6923:Wetlands portal
6554:Constructed wetland
6139:Types and landforms
5647:Ocean fertilization
5456:Trophic state index
5414:Lake stratification
5144:Aquatic respiration
4913:Coastal engineering
3554:2013NatSR...3E1926M
3505:2014Natur.507..286W
3397:2019NatSR...918746E
3268:2001HydSJ..46...13A
3203:2017ERL....12f4006M
3094:2019ERL....14h4034D
3024:2009NatGe...2..681S
2960:2016ECSS..183..275D
2851:10.1038/nature19809
2843:2016Natur.539..276D
2655:10.3368/er.22.4.262
2587:2010JGRD..11523114D
2551:1994QuInt..21...29M
2471:1984ChGeo..44..227B
2422:Geographical Review
2331:2002Geomo..43..293P
2171:2003ECSS...58..367P
2066:2010Sedim..57..543B
1969:, pp. 293–294.
1917:1993Sedim..40..475O
1850:2000SedG..133..227G
1838:Sedimentary Geology
1795:1992JG....100..525M
1692:Boggs, Sam (2006).
1506:2022NatGe..15..919H
1464:2015MGeol.361...53A
1367:2001ESPL...26..409P
1177:, as seen by THEMIS
1071:Yangtze River Delta
981:saltwater intrusion
941:sediment deposition
751:delta of Iran. The
571:and form prominent
213:Alexander the Great
130:geologic timescales
6767:Salt marsh die-off
6685:Salt marsh dieback
6594:List of fen plants
6433:Palustrine wetland
6334:Intertidal wetland
6329:Interdunal wetland
5913:Intertidal wetland
5908:Intertidal ecology
5776:Marine prokaryotes
5718:Deep-sea community
5612:Iron fertilization
5535:Specific examples
5461:Upland and lowland
5379:Freshwater biology
5244:Microbial food web
5154:Aquatic toxicology
5097:Aquatic adaptation
5050:Aquatic ecosystems
4882:Coastal management
4722:Emergent coastline
4393:Intertidal wetland
4296:Continental margin
4135:Sediment transport
4089:River rejuvenation
4062:Regional processes
3542:Scientific Reports
3384:Scientific Reports
1205:Probable delta in
1079:Greater Tokyo Area
1055:
1047:Satakunta, Finland
973:relative sea level
836:
812:Ganges-Brahmaputra
717:
617:
553:Grove Karl Gilbert
487:
340:
306:transport sediment
290:
223:(the delta of the
211:, who accompanied
154:classical Athenian
150:Greek letter delta
59:
44:
28:
6979:Fluvial landforms
6969:Coastal geography
6941:
6940:
6843:Aquatic ecosystem
6831:
6830:
6750:Ramsar Convention
6577:
6576:
6559:Converted wetland
6501:Peat swamp forest
6364:Inland salt marsh
6098:
6097:
6079:Oceans portal
6048:
6047:
6044:
6043:
5923:Hydrothermal vent
5859:
5858:
5748:Seashore wildlife
5579:Marine ecosystems
5568:
5567:
5564:
5563:
5334:Thermal pollution
5299:Ramsar Convention
5239:Microbial ecology
5199:Fisheries science
5139:Aquatic predation
5016:
5015:
4844:Wave-cut platform
4757:Marine regression
4301:Continental shelf
4291:Coastal waterfall
4200:Coastal geography
4166:
4165:
3967:River bifurcation
3750:Applied Geography
3734:978-94-007-3961-1
3714:978-94-007-3961-1
3562:10.1038/srep01926
3538:"Man made deltas"
3499:(7492): 286–287.
3011:Nature Geoscience
2837:(7628): 276–279.
1493:Nature Geoscience
1423:10.1111/jac.12415
1276:Pearl River Delta
1207:Eberswalde crater
1193:as seen by THEMIS
1067:Pearl River Delta
786:The generic term
737:Inner Niger Delta
451:Mississippi Delta
418:continental shelf
250:
238:
227:) was "a delta" (
7001:
6931:
6930:
6921:
6920:
6919:
6903:Will-o'-the-wisp
6836:Related articles
6728:
6727:
6528:Whitewater river
6478:Coniferous swamp
6359:Freshwater marsh
6252:Clearwater river
6168:Blackwater river
6143:
6142:
6125:
6118:
6111:
6102:
6101:
6088:
6087:
6081:
6077:
6076:
6067:
6065:Lakes portal
6063:
6062:
6061:
6031:Marine pollution
5723:Deep-water coral
5706:
5705:
5694:
5627:Marine chemistry
5587:
5586:
5574:
5573:
5491:Freshwater marsh
5384:Freshwater biome
5366:
5082:Acoustic ecology
5072:
5071:
5058:
5057:
5043:
5036:
5029:
5020:
5019:
5006:
5005:
4767:Raised shoreline
4742:Ingression coast
4737:Graded shoreline
4712:Cuspate foreland
4544:
4537:
4488:Submarine canyon
4348:Freshwater marsh
4193:
4186:
4179:
4170:
4169:
4156:
4155:
3897:Avulsion (river)
3825:River morphology
3818:
3811:
3804:
3795:
3794:
3765:
3697:
3694:
3688:
3687:
3685:
3684:
3678:
3665:
3657:
3651:
3650:
3648:
3647:
3638:. Archived from
3627:
3621:
3620:
3618:
3617:
3598:
3592:
3591:
3581:
3533:
3527:
3526:
3516:
3484:
3478:
3477:
3467:
3443:
3437:
3436:
3426:
3408:
3374:
3368:
3367:
3365:
3364:
3338:
3304:
3298:
3297:
3279:
3247:
3241:
3240:
3230:
3180:
3174:
3173:
3171:
3170:
3127:"Deltas at risk"
3122:
3116:
3115:
3105:
3071:
3065:
3064:
3062:
3061:
3043:
3000:
2991:
2990:
2988:
2987:
2936:
2930:
2923:
2917:
2907:
2898:
2891:
2885:
2884:
2882:
2881:
2875:
2826:
2817:
2811:
2810:
2790:
2784:
2783:
2749:
2743:
2742:
2722:
2716:
2715:
2705:
2681:
2675:
2674:
2638:
2632:
2631:
2629:
2605:
2599:
2598:
2569:
2563:
2562:
2534:
2528:
2527:
2489:
2483:
2482:
2465:(1–3): 227–242.
2458:Chemical Geology
2452:
2446:
2445:
2417:
2411:
2410:
2408:
2407:
2349:
2343:
2342:
2325:(3–4): 293–311.
2312:
2306:
2305:
2267:
2261:
2260:
2244:
2238:
2237:
2235:
2234:
2215:
2209:
2206:
2197:
2196:
2194:
2193:
2187:
2154:
2145:
2139:
2138:
2136:
2135:
2116:
2110:
2109:on Google Books.
2095:
2086:
2085:
2049:
2043:
2042:
2040:
2038:
2017:
2011:
2010:on Google Books.
1996:
1990:
1981:
1970:
1964:
1958:
1952:
1946:
1940:
1929:
1928:
1900:
1894:
1891:
1885:
1881:
1875:
1871:
1862:
1861:
1844:(3–4): 227–248.
1832:
1823:
1822:
1776:
1761:
1760:
1742:
1736:
1730:
1721:
1714:
1708:
1707:
1689:
1683:
1682:
1680:
1679:
1660:
1654:
1653:
1651:
1650:
1629:
1623:
1622:
1620:
1619:
1610:. January 2020.
1600:
1594:
1593:
1555:
1538:
1537:
1535:
1533:
1482:
1476:
1475:
1445:
1436:
1435:
1425:
1401:
1395:
1394:
1348:
1339:
1338:
1310:
1304:
1301:
1295:
1292:
1271:Regressive delta
1247:Avulsion (river)
1235:
1230:
1229:
1228:
1202:
1186:
1170:
1151:
1120:Russian republic
925:geomorphological
569:British Columbia
512:hyperpycnal flow
484:
480:
476:
472:
468:
464:
456:
245:
243:
237:romanized:
236:
234:
219:, reported that
215:'s conquests in
162:Prometheus Bound
7009:
7008:
7004:
7003:
7002:
7000:
6999:
6998:
6989:Bodies of water
6954:Aquatic ecology
6944:
6943:
6942:
6937:
6917:
6915:
6907:
6827:
6798:Ducks Unlimited
6776:
6735:Clean Water Act
6717:
6695:Classifications
6689:
6658:
6605:
6573:
6537:
6488:Mangrove forest
6134:
6129:
6099:
6094:
6071:
6070:
6059:
6057:
6056:
6040:
6001:Coral bleaching
5987:
5968:Seagrass meadow
5865:Marine habitats
5855:
5829:Coral reef fish
5795:
5781:Marine protists
5757:
5695:
5686:
5657:Ocean turbidity
5632:Marine food web
5581:
5560:
5502:
5441:River ecosystem
5394:Freshwater fish
5367:
5358:
5164:Bioluminescence
5149:Aquatic science
5066:
5052:
5047:
5017:
5012:
4994:
4970:Intertidal zone
4896:
4863:
4752:Longshore drift
4697:Coastal erosion
4668:
4628:
4564:Beach evolution
4545:
4539:
4538:
4529:
4216:Anchialine pool
4202:
4197:
4167:
4162:
4144:
4125:Helicoidal flow
4093:
4057:
4024:
3996:
3912:Channel pattern
3884:Alluvial rivers
3878:
3874:River sinuosity
3827:
3822:
3772:
3744:, pp. 7–48
3724:, pp. 7–48
3705:
3700:
3695:
3691:
3682:
3680:
3676:
3663:
3659:
3658:
3654:
3645:
3643:
3636:This City Knows
3628:
3624:
3615:
3613:
3600:
3599:
3595:
3534:
3530:
3514:10.1038/507286a
3485:
3481:
3444:
3440:
3375:
3371:
3362:
3360:
3305:
3301:
3248:
3244:
3181:
3177:
3168:
3166:
3123:
3119:
3072:
3068:
3059:
3057:
3032:10.1038/ngeo629
3018:(10): 681–686.
3001:
2994:
2985:
2983:
2937:
2933:
2924:
2920:
2908:
2901:
2893:D.G.A Whitten,
2892:
2888:
2879:
2877:
2873:
2824:
2818:
2814:
2791:
2787:
2772:
2750:
2746:
2723:
2719:
2682:
2678:
2639:
2635:
2606:
2602:
2581:(D23): D23114.
2570:
2566:
2535:
2531:
2508:10.2307/1352687
2490:
2486:
2453:
2449:
2418:
2414:
2405:
2403:
2372:10.2307/1352839
2350:
2346:
2313:
2309:
2268:
2264:
2245:
2241:
2232:
2230:
2217:
2216:
2212:
2207:
2200:
2191:
2189:
2185:
2152:
2146:
2142:
2133:
2131:
2118:
2117:
2113:
2096:
2089:
2050:
2046:
2036:
2034:
2018:
2014:
1997:
1993:
1982:
1973:
1965:
1961:
1953:
1949:
1941:
1932:
1901:
1897:
1892:
1888:
1882:
1878:
1872:
1865:
1833:
1826:
1777:
1764:
1757:
1743:
1739:
1731:
1724:
1715:
1711:
1704:
1690:
1686:
1677:
1675:
1662:
1661:
1657:
1648:
1646:
1631:
1630:
1626:
1617:
1615:
1602:
1601:
1597:
1556:
1541:
1531:
1529:
1483:
1479:
1446:
1439:
1402:
1398:
1375:10.1002/esp.189
1349:
1342:
1311:
1307:
1302:
1298:
1293:
1289:
1285:
1233:Wetlands portal
1231:
1226:
1224:
1221:
1214:
1203:
1194:
1187:
1178:
1171:
1162:
1152:
1136:
1093:
1087:
1012:
901:land use change
893:
871:angle of repose
824:
784:
776:endorheic basin
709:
685:
653:and subsequent
646:
622:
593:
561:Lake Bonneville
549:
524:hypopycnal flow
516:density current
508:homopycnal flow
504:
482:
478:
474:
470:
466:
462:
454:
443:
435:
425:passive margins
282:
142:
17:
12:
11:
5:
7007:
6997:
6996:
6991:
6986:
6981:
6976:
6971:
6966:
6961:
6956:
6939:
6938:
6936:
6935:
6925:
6912:
6909:
6908:
6906:
6905:
6900:
6895:
6890:
6885:
6880:
6875:
6873:Drainage basin
6870:
6865:
6860:
6855:
6850:
6845:
6839:
6837:
6833:
6832:
6829:
6828:
6826:
6825:
6820:
6815:
6810:
6805:
6800:
6795:
6790:
6784:
6782:
6778:
6777:
6775:
6774:
6769:
6764:
6763:
6762:
6752:
6747:
6742:
6737:
6731:
6725:
6719:
6718:
6716:
6715:
6710:
6705:
6699:
6697:
6691:
6690:
6688:
6687:
6682:
6680:Paludification
6677:
6672:
6666:
6664:
6660:
6659:
6657:
6656:
6651:
6646:
6641:
6640:
6639:
6634:
6632:Sapric or muck
6629:
6619:
6613:
6611:
6610:Soil mechanics
6607:
6606:
6604:
6603:
6596:
6591:
6585:
6583:
6579:
6578:
6575:
6574:
6572:
6571:
6566:
6561:
6556:
6551:
6545:
6543:
6539:
6538:
6536:
6535:
6530:
6525:
6520:
6515:
6510:
6509:
6508:
6503:
6498:
6490:
6485:
6480:
6470:
6465:
6460:
6455:
6450:
6445:
6440:
6435:
6430:
6425:
6420:
6415:
6410:
6405:
6400:
6395:
6390:
6389:
6388:
6387:
6386:
6381:
6371:
6366:
6361:
6356:
6354:Brackish marsh
6346:
6341:
6336:
6331:
6326:
6321:
6316:
6311:
6306:
6301:
6296:
6291:
6286:
6285:
6284:
6279:
6274:
6264:
6259:
6254:
6249:
6244:
6243:
6242:
6232:
6227:
6226:
6225:
6220:
6215:
6210:
6205:
6200:
6195:
6190:
6185:
6175:
6170:
6165:
6160:
6155:
6149:
6147:
6140:
6136:
6135:
6128:
6127:
6120:
6113:
6105:
6096:
6095:
6093:
6092:
6082:
6068:
6053:
6050:
6049:
6046:
6045:
6042:
6041:
6039:
6038:
6033:
6028:
6023:
6018:
6013:
6008:
6003:
5997:
5995:
5989:
5988:
5986:
5985:
5980:
5975:
5970:
5965:
5960:
5955:
5950:
5945:
5940:
5935:
5930:
5925:
5920:
5915:
5910:
5905:
5900:
5895:
5890:
5885:
5880:
5875:
5869:
5867:
5861:
5860:
5857:
5856:
5854:
5853:
5848:
5847:
5846:
5841:
5836:
5831:
5826:
5819:Saltwater fish
5816:
5814:Marine reptile
5811:
5805:
5803:
5797:
5796:
5794:
5793:
5788:
5786:Marine viruses
5783:
5778:
5773:
5767:
5765:
5763:Microorganisms
5759:
5758:
5756:
5755:
5753:Wild fisheries
5750:
5745:
5740:
5735:
5730:
5725:
5720:
5715:
5709:
5703:
5697:
5696:
5689:
5687:
5685:
5684:
5679:
5674:
5669:
5667:Thorson's rule
5664:
5659:
5654:
5649:
5644:
5639:
5634:
5629:
5624:
5622:Marine biology
5619:
5614:
5609:
5604:
5599:
5593:
5591:
5583:
5582:
5570:
5569:
5566:
5565:
5562:
5561:
5559:
5558:
5557:
5556:
5551:
5546:
5541:
5533:
5528:
5527:
5526:
5521:
5510:
5508:
5504:
5503:
5501:
5500:
5499:
5498:
5493:
5488:
5483:
5481:Brackish marsh
5478:
5468:
5463:
5458:
5453:
5448:
5443:
5438:
5433:
5432:
5431:
5421:
5416:
5411:
5409:Lake ecosystem
5406:
5401:
5399:Hyporheic zone
5396:
5391:
5386:
5381:
5375:
5373:
5369:
5368:
5361:
5359:
5357:
5356:
5351:
5346:
5341:
5336:
5331:
5326:
5321:
5316:
5311:
5306:
5301:
5296:
5291:
5286:
5281:
5276:
5271:
5266:
5261:
5256:
5251:
5249:Microbial loop
5246:
5241:
5236:
5231:
5226:
5221:
5216:
5211:
5206:
5201:
5196:
5194:Eutrophication
5191:
5186:
5181:
5176:
5174:Cascade effect
5171:
5166:
5161:
5156:
5151:
5146:
5141:
5136:
5131:
5126:
5121:
5120:
5119:
5114:
5109:
5102:Aquatic animal
5099:
5094:
5089:
5084:
5078:
5076:
5068:
5067:
5054:
5053:
5046:
5045:
5038:
5031:
5023:
5014:
5013:
5011:
5010:
4999:
4996:
4995:
4993:
4992:
4987:
4982:
4977:
4972:
4967:
4966:
4965:
4960:
4955:
4950:
4945:
4940:
4935:
4930:
4925:
4915:
4910:
4904:
4902:
4898:
4897:
4895:
4894:
4889:
4884:
4879:
4873:
4871:
4865:
4864:
4862:
4861:
4856:
4851:
4846:
4841:
4836:
4831:
4826:
4821:
4816:
4811:
4806:
4801:
4800:
4799:
4789:
4784:
4779:
4774:
4769:
4764:
4759:
4754:
4749:
4744:
4739:
4734:
4729:
4724:
4719:
4714:
4709:
4704:
4699:
4694:
4689:
4684:
4678:
4676:
4670:
4669:
4667:
4666:
4665:
4664:
4659:
4649:
4644:
4638:
4636:
4630:
4629:
4627:
4626:
4621:
4616:
4611:
4606:
4601:
4596:
4591:
4586:
4581:
4576:
4571:
4566:
4561:
4555:
4553:
4547:
4546:
4532:
4530:
4528:
4527:
4520:
4515:
4510:
4505:
4500:
4495:
4490:
4485:
4480:
4475:
4470:
4465:
4460:
4455:
4450:
4445:
4440:
4435:
4430:
4425:
4420:
4415:
4410:
4405:
4400:
4395:
4390:
4385:
4380:
4375:
4370:
4365:
4360:
4355:
4350:
4345:
4340:
4335:
4330:
4325:
4324:
4323:
4313:
4308:
4303:
4298:
4293:
4288:
4283:
4278:
4273:
4268:
4263:
4261:Brackish marsh
4258:
4253:
4248:
4243:
4241:Barrier island
4238:
4233:
4228:
4223:
4218:
4212:
4210:
4204:
4203:
4196:
4195:
4188:
4181:
4173:
4164:
4163:
4161:
4160:
4149:
4146:
4145:
4143:
4142:
4137:
4132:
4130:Playfair's law
4127:
4122:
4117:
4115:Exner equation
4112:
4107:
4101:
4099:
4095:
4094:
4092:
4091:
4086:
4081:
4076:
4071:
4065:
4063:
4059:
4058:
4056:
4055:
4053:Current ripple
4050:
4045:
4040:
4034:
4032:
4026:
4025:
4023:
4022:
4017:
4012:
4006:
4004:
3998:
3997:
3995:
3994:
3989:
3984:
3982:Slip-off slope
3979:
3974:
3969:
3964:
3959:
3954:
3949:
3944:
3939:
3934:
3932:Meander cutoff
3929:
3924:
3919:
3914:
3909:
3904:
3899:
3894:
3888:
3886:
3880:
3879:
3877:
3876:
3871:
3866:
3861:
3856:
3851:
3846:
3844:Drainage basin
3841:
3839:Alluvial plain
3835:
3833:
3829:
3828:
3821:
3820:
3813:
3806:
3798:
3792:
3791:
3785:
3779:
3778:– World Deltas
3771:
3770:External links
3768:
3767:
3766:
3745:
3725:
3704:
3701:
3699:
3698:
3689:
3652:
3622:
3593:
3528:
3479:
3438:
3369:
3321:(3): 217–225.
3299:
3242:
3175:
3117:
3066:
2992:
2931:
2918:
2899:
2886:
2812:
2785:
2770:
2744:
2717:
2696:(2): 131–143.
2676:
2633:
2600:
2564:
2529:
2502:(2): 130–146.
2484:
2447:
2434:10.2307/211476
2428:(2): 219–238.
2412:
2366:(3): 407–415.
2344:
2307:
2280:(3): 520–537.
2262:
2239:
2210:
2198:
2165:(2): 367–387.
2140:
2111:
2105:. Pages 2–17.
2087:
2060:(2): 543–586.
2044:
2012:
1991:
1971:
1959:
1957:, p. 294.
1947:
1945:, p. 293.
1930:
1911:(3): 475–512.
1895:
1886:
1876:
1863:
1824:
1803:10.1086/629606
1789:(5): 525–544.
1762:
1755:
1737:
1735:, p. 295.
1722:
1709:
1702:
1684:
1655:
1641:. 2014-08-12.
1624:
1595:
1574:10.1086/350146
1568:(3): 385–388.
1539:
1500:(1): 919–924.
1477:
1451:Marine Geology
1437:
1416:(4): 491–503.
1396:
1361:(4): 409–427.
1340:
1305:
1296:
1286:
1284:
1281:
1280:
1279:
1273:
1268:
1262:
1256:
1250:
1244:
1237:
1236:
1220:
1217:
1216:
1215:
1204:
1197:
1195:
1188:
1181:
1179:
1172:
1165:
1163:
1153:
1146:
1135:
1134:Deltas on Mars
1132:
1086:
1083:
1051:distributaries
1035:Kokemäki River
1011:
1008:
935:which prevent
933:flood defences
918:sea level rise
892:
889:
888:
887:
884:alluvial plain
879:
857:
823:
820:
783:
780:
768:Okavango Delta
715:Okavango Delta
708:
705:
684:
681:
676:Chesapeake Bay
645:
642:
621:
618:
592:
589:
548:
547:Gilbert deltas
545:
503:
500:
442:
439:
367:Wax Lake Delta
281:
278:
159:; the tragedy
141:
138:
15:
9:
6:
4:
3:
2:
7006:
6995:
6992:
6990:
6987:
6985:
6984:Water streams
6982:
6980:
6977:
6975:
6974:Sedimentology
6972:
6970:
6967:
6965:
6962:
6960:
6957:
6955:
6952:
6951:
6949:
6934:
6926:
6924:
6914:
6913:
6910:
6904:
6901:
6899:
6896:
6894:
6891:
6889:
6886:
6884:
6883:Riparian zone
6881:
6879:
6876:
6874:
6871:
6869:
6866:
6864:
6861:
6859:
6856:
6854:
6851:
6849:
6846:
6844:
6841:
6840:
6838:
6834:
6824:
6821:
6819:
6816:
6814:
6811:
6809:
6806:
6804:
6801:
6799:
6796:
6794:
6791:
6789:
6786:
6785:
6783:
6781:Organizations
6779:
6773:
6770:
6768:
6765:
6761:
6758:
6757:
6756:
6753:
6751:
6748:
6746:
6743:
6741:
6738:
6736:
6733:
6732:
6729:
6726:
6724:
6720:
6714:
6711:
6709:
6706:
6704:
6701:
6700:
6698:
6696:
6692:
6686:
6683:
6681:
6678:
6676:
6673:
6671:
6668:
6667:
6665:
6661:
6655:
6652:
6650:
6647:
6645:
6642:
6638:
6637:Tropical peat
6635:
6633:
6630:
6628:
6625:
6624:
6623:
6620:
6618:
6615:
6614:
6612:
6608:
6602:
6601:
6597:
6595:
6592:
6590:
6587:
6586:
6584:
6580:
6570:
6567:
6565:
6562:
6560:
6557:
6555:
6552:
6550:
6547:
6546:
6544:
6540:
6534:
6531:
6529:
6526:
6524:
6521:
6519:
6518:Várzea forest
6516:
6514:
6511:
6507:
6504:
6502:
6499:
6497:
6495:
6491:
6489:
6486:
6484:
6481:
6479:
6476:
6475:
6474:
6471:
6469:
6466:
6464:
6461:
6459:
6456:
6454:
6451:
6449:
6446:
6444:
6441:
6439:
6436:
6434:
6431:
6429:
6426:
6424:
6421:
6419:
6416:
6414:
6411:
6409:
6406:
6404:
6401:
6399:
6396:
6394:
6391:
6385:
6382:
6380:
6377:
6376:
6375:
6372:
6370:
6367:
6365:
6362:
6360:
6357:
6355:
6352:
6351:
6350:
6347:
6345:
6342:
6340:
6337:
6335:
6332:
6330:
6327:
6325:
6322:
6320:
6317:
6315:
6312:
6310:
6307:
6305:
6302:
6300:
6297:
6295:
6292:
6290:
6287:
6283:
6280:
6278:
6275:
6273:
6270:
6269:
6268:
6265:
6263:
6260:
6258:
6255:
6253:
6250:
6248:
6245:
6241:
6238:
6237:
6236:
6233:
6231:
6228:
6224:
6221:
6219:
6216:
6214:
6211:
6209:
6208:Polygonal bog
6206:
6204:
6201:
6199:
6196:
6194:
6191:
6189:
6186:
6184:
6181:
6180:
6179:
6176:
6174:
6171:
6169:
6166:
6164:
6161:
6159:
6156:
6154:
6151:
6150:
6148:
6144:
6141:
6137:
6133:
6126:
6121:
6119:
6114:
6112:
6107:
6106:
6103:
6091:
6083:
6080:
6075:
6069:
6066:
6055:
6054:
6051:
6037:
6034:
6032:
6029:
6027:
6024:
6022:
6019:
6017:
6014:
6012:
6009:
6007:
6004:
6002:
5999:
5998:
5996:
5994:
5990:
5984:
5981:
5979:
5976:
5974:
5973:Sponge ground
5971:
5969:
5966:
5964:
5961:
5959:
5956:
5954:
5951:
5949:
5946:
5944:
5941:
5939:
5938:Marine biomes
5936:
5934:
5931:
5929:
5926:
5924:
5921:
5919:
5916:
5914:
5911:
5909:
5906:
5904:
5901:
5899:
5896:
5894:
5891:
5889:
5886:
5884:
5881:
5879:
5876:
5874:
5871:
5870:
5868:
5866:
5862:
5852:
5849:
5845:
5842:
5840:
5839:Demersal fish
5837:
5835:
5834:Deep-sea fish
5832:
5830:
5827:
5825:
5822:
5821:
5820:
5817:
5815:
5812:
5810:
5809:Marine mammal
5807:
5806:
5804:
5802:
5798:
5792:
5789:
5787:
5784:
5782:
5779:
5777:
5774:
5772:
5769:
5768:
5766:
5764:
5760:
5754:
5751:
5749:
5746:
5744:
5741:
5739:
5736:
5734:
5731:
5729:
5726:
5724:
5721:
5719:
5716:
5714:
5711:
5710:
5707:
5704:
5702:
5698:
5693:
5683:
5680:
5678:
5675:
5673:
5670:
5668:
5665:
5663:
5660:
5658:
5655:
5653:
5650:
5648:
5645:
5643:
5640:
5638:
5635:
5633:
5630:
5628:
5625:
5623:
5620:
5618:
5615:
5613:
5610:
5608:
5605:
5603:
5600:
5598:
5595:
5594:
5592:
5588:
5584:
5580:
5575:
5571:
5555:
5552:
5550:
5547:
5545:
5542:
5540:
5537:
5536:
5534:
5532:
5529:
5525:
5522:
5520:
5517:
5516:
5515:
5512:
5511:
5509:
5505:
5497:
5494:
5492:
5489:
5487:
5484:
5482:
5479:
5477:
5474:
5473:
5472:
5469:
5467:
5464:
5462:
5459:
5457:
5454:
5452:
5449:
5447:
5444:
5442:
5439:
5437:
5434:
5430:
5427:
5426:
5425:
5422:
5420:
5417:
5415:
5412:
5410:
5407:
5405:
5402:
5400:
5397:
5395:
5392:
5390:
5387:
5385:
5382:
5380:
5377:
5376:
5374:
5370:
5365:
5355:
5352:
5350:
5347:
5345:
5342:
5340:
5339:Trophic level
5337:
5335:
5332:
5330:
5327:
5325:
5322:
5320:
5317:
5315:
5312:
5310:
5307:
5305:
5304:Sediment trap
5302:
5300:
5297:
5295:
5292:
5290:
5287:
5285:
5282:
5280:
5279:Phytoplankton
5277:
5275:
5272:
5270:
5267:
5265:
5262:
5260:
5257:
5255:
5252:
5250:
5247:
5245:
5242:
5240:
5237:
5235:
5232:
5230:
5227:
5225:
5222:
5220:
5217:
5215:
5212:
5210:
5207:
5205:
5202:
5200:
5197:
5195:
5192:
5190:
5187:
5185:
5182:
5180:
5177:
5175:
5172:
5170:
5167:
5165:
5162:
5160:
5157:
5155:
5152:
5150:
5147:
5145:
5142:
5140:
5137:
5135:
5132:
5130:
5129:Aquatic plant
5127:
5125:
5122:
5118:
5115:
5113:
5110:
5108:
5105:
5104:
5103:
5100:
5098:
5095:
5093:
5092:Anoxic waters
5090:
5088:
5085:
5083:
5080:
5079:
5077:
5073:
5069:
5065:
5059:
5055:
5051:
5044:
5039:
5037:
5032:
5030:
5025:
5024:
5021:
5009:
5001:
5000:
4997:
4991:
4988:
4986:
4983:
4981:
4978:
4976:
4975:Littoral zone
4973:
4971:
4968:
4964:
4961:
4959:
4956:
4954:
4951:
4949:
4946:
4944:
4941:
4939:
4936:
4934:
4931:
4929:
4926:
4924:
4921:
4920:
4919:
4916:
4914:
4911:
4909:
4908:Bulkhead line
4906:
4905:
4903:
4899:
4893:
4890:
4888:
4885:
4883:
4880:
4878:
4875:
4874:
4872:
4870:
4866:
4860:
4857:
4855:
4852:
4850:
4849:Wave shoaling
4847:
4845:
4842:
4840:
4837:
4835:
4832:
4830:
4827:
4825:
4824:Surge channel
4822:
4820:
4817:
4815:
4812:
4810:
4807:
4805:
4802:
4798:
4795:
4794:
4793:
4790:
4788:
4785:
4783:
4780:
4778:
4775:
4773:
4770:
4768:
4765:
4763:
4760:
4758:
4755:
4753:
4750:
4748:
4745:
4743:
4740:
4738:
4735:
4733:
4730:
4728:
4725:
4723:
4720:
4718:
4715:
4713:
4710:
4708:
4705:
4703:
4700:
4698:
4695:
4693:
4690:
4688:
4687:Cliffed coast
4685:
4683:
4680:
4679:
4677:
4675:
4671:
4663:
4660:
4658:
4655:
4654:
4653:
4650:
4648:
4645:
4643:
4640:
4639:
4637:
4635:
4631:
4625:
4622:
4620:
4617:
4615:
4614:Shingle beach
4612:
4610:
4607:
4605:
4602:
4600:
4597:
4595:
4592:
4590:
4587:
4585:
4582:
4580:
4577:
4575:
4572:
4570:
4567:
4565:
4562:
4560:
4557:
4556:
4554:
4552:
4548:
4543:
4536:
4526:
4525:
4521:
4519:
4516:
4514:
4511:
4509:
4506:
4504:
4501:
4499:
4496:
4494:
4491:
4489:
4486:
4484:
4481:
4479:
4476:
4474:
4471:
4469:
4466:
4464:
4461:
4459:
4456:
4454:
4451:
4449:
4446:
4444:
4441:
4439:
4436:
4434:
4431:
4429:
4426:
4424:
4421:
4419:
4416:
4414:
4411:
4409:
4406:
4404:
4401:
4399:
4396:
4394:
4391:
4389:
4386:
4384:
4381:
4379:
4376:
4374:
4371:
4369:
4366:
4364:
4361:
4359:
4356:
4354:
4351:
4349:
4346:
4344:
4341:
4339:
4336:
4334:
4331:
4329:
4326:
4322:
4319:
4318:
4317:
4314:
4312:
4309:
4307:
4304:
4302:
4299:
4297:
4294:
4292:
4289:
4287:
4286:Coastal plain
4284:
4282:
4279:
4277:
4274:
4272:
4269:
4267:
4264:
4262:
4259:
4257:
4254:
4252:
4249:
4247:
4244:
4242:
4239:
4237:
4234:
4232:
4229:
4227:
4224:
4222:
4219:
4217:
4214:
4213:
4211:
4209:
4205:
4201:
4194:
4189:
4187:
4182:
4180:
4175:
4174:
4171:
4159:
4151:
4150:
4147:
4141:
4138:
4136:
4133:
4131:
4128:
4126:
4123:
4121:
4118:
4116:
4113:
4111:
4110:Water erosion
4108:
4106:
4103:
4102:
4100:
4096:
4090:
4087:
4085:
4082:
4080:
4077:
4075:
4072:
4070:
4067:
4066:
4064:
4060:
4054:
4051:
4049:
4046:
4044:
4041:
4039:
4036:
4035:
4033:
4031:
4027:
4021:
4018:
4016:
4013:
4011:
4008:
4007:
4005:
4003:
4002:Bedrock river
3999:
3993:
3990:
3988:
3985:
3983:
3980:
3978:
3975:
3973:
3970:
3968:
3965:
3963:
3962:Riparian zone
3960:
3958:
3955:
3953:
3950:
3948:
3945:
3943:
3940:
3938:
3935:
3933:
3930:
3928:
3925:
3923:
3920:
3918:
3915:
3913:
3910:
3908:
3907:Braided river
3905:
3903:
3900:
3898:
3895:
3893:
3890:
3889:
3887:
3885:
3881:
3875:
3872:
3870:
3867:
3865:
3862:
3860:
3857:
3855:
3852:
3850:
3847:
3845:
3842:
3840:
3837:
3836:
3834:
3830:
3826:
3819:
3814:
3812:
3807:
3805:
3800:
3799:
3796:
3789:
3786:
3783:
3780:
3777:
3774:
3773:
3763:
3759:
3755:
3751:
3746:
3743:
3739:
3735:
3731:
3726:
3723:
3719:
3715:
3711:
3707:
3706:
3693:
3675:
3671:
3670:
3662:
3656:
3642:on 2019-06-06
3641:
3637:
3633:
3626:
3612:on 2011-10-06
3611:
3607:
3603:
3597:
3589:
3585:
3580:
3575:
3571:
3567:
3563:
3559:
3555:
3551:
3547:
3543:
3539:
3532:
3524:
3520:
3515:
3510:
3506:
3502:
3498:
3494:
3490:
3483:
3475:
3471:
3466:
3461:
3457:
3453:
3449:
3442:
3434:
3430:
3425:
3420:
3416:
3412:
3407:
3402:
3398:
3394:
3390:
3386:
3385:
3380:
3373:
3358:
3354:
3350:
3346:
3342:
3337:
3332:
3328:
3324:
3320:
3316:
3315:
3310:
3303:
3295:
3291:
3287:
3283:
3278:
3273:
3269:
3265:
3261:
3257:
3253:
3246:
3238:
3234:
3229:
3224:
3220:
3216:
3212:
3208:
3204:
3200:
3197:(6): 064006.
3196:
3192:
3191:
3186:
3179:
3164:
3160:
3156:
3152:
3148:
3144:
3140:
3136:
3132:
3128:
3121:
3113:
3109:
3104:
3099:
3095:
3091:
3088:(8): 084034.
3087:
3083:
3082:
3077:
3070:
3055:
3051:
3047:
3042:
3037:
3033:
3029:
3025:
3021:
3017:
3013:
3012:
3007:
2999:
2997:
2981:
2977:
2973:
2969:
2965:
2961:
2957:
2953:
2949:
2948:
2943:
2935:
2928:
2922:
2915:
2912:
2906:
2904:
2896:
2890:
2872:
2868:
2864:
2860:
2856:
2852:
2848:
2844:
2840:
2836:
2832:
2831:
2823:
2816:
2808:
2804:
2800:
2796:
2789:
2781:
2777:
2773:
2771:0-7803-7536-X
2767:
2763:
2759:
2755:
2748:
2740:
2736:
2732:
2728:
2721:
2713:
2709:
2704:
2699:
2695:
2691:
2687:
2680:
2672:
2668:
2664:
2660:
2656:
2652:
2649:(4): 262–68.
2648:
2644:
2637:
2628:
2623:
2619:
2615:
2611:
2604:
2596:
2592:
2588:
2584:
2580:
2576:
2568:
2560:
2556:
2552:
2548:
2544:
2540:
2533:
2525:
2521:
2517:
2513:
2509:
2505:
2501:
2497:
2496:
2488:
2480:
2476:
2472:
2468:
2464:
2460:
2459:
2451:
2443:
2439:
2435:
2431:
2427:
2423:
2416:
2401:
2397:
2393:
2389:
2385:
2381:
2377:
2373:
2369:
2365:
2361:
2360:
2355:
2348:
2340:
2336:
2332:
2328:
2324:
2320:
2319:
2318:Geomorphology
2311:
2303:
2299:
2295:
2291:
2287:
2283:
2279:
2275:
2274:
2266:
2258:
2254:
2250:
2243:
2228:
2224:
2220:
2214:
2205:
2203:
2184:
2180:
2176:
2172:
2168:
2164:
2160:
2159:
2151:
2144:
2129:
2125:
2121:
2115:
2108:
2104:
2103:1-55791-668-3
2100:
2094:
2092:
2083:
2079:
2075:
2071:
2067:
2063:
2059:
2055:
2054:Sedimentology
2048:
2032:
2028:
2027:
2022:
2021:Gilbert, G.K.
2016:
2009:
2005:
2004:2-7108-0802-1
2001:
1995:
1988:
1985:
1980:
1978:
1976:
1968:
1963:
1956:
1951:
1944:
1939:
1937:
1935:
1926:
1922:
1918:
1914:
1910:
1906:
1905:Sedimentology
1899:
1890:
1880:
1870:
1868:
1859:
1855:
1851:
1847:
1843:
1839:
1831:
1829:
1820:
1816:
1812:
1808:
1804:
1800:
1796:
1792:
1788:
1784:
1783:
1775:
1773:
1771:
1769:
1767:
1758:
1756:9781405177832
1752:
1748:
1741:
1734:
1729:
1727:
1719:
1713:
1705:
1699:
1695:
1688:
1673:
1669:
1665:
1659:
1644:
1640:
1639:
1634:
1628:
1613:
1609:
1605:
1599:
1591:
1587:
1583:
1579:
1575:
1571:
1567:
1563:
1562:
1554:
1552:
1550:
1548:
1546:
1544:
1527:
1523:
1519:
1515:
1511:
1507:
1503:
1499:
1495:
1494:
1489:
1481:
1473:
1469:
1465:
1461:
1457:
1453:
1452:
1444:
1442:
1433:
1429:
1424:
1419:
1415:
1411:
1407:
1400:
1392:
1388:
1384:
1380:
1376:
1372:
1368:
1364:
1360:
1356:
1355:
1347:
1345:
1336:
1332:
1328:
1324:
1320:
1316:
1315:Sedimentology
1309:
1300:
1291:
1287:
1277:
1274:
1272:
1269:
1266:
1263:
1260:
1257:
1254:
1251:
1248:
1245:
1242:
1239:
1238:
1234:
1223:
1212:
1208:
1201:
1196:
1192:
1185:
1180:
1176:
1169:
1164:
1161:
1158:, as seen by
1157:
1150:
1145:
1144:
1143:
1141:
1140:Martian lakes
1131:
1129:
1125:
1121:
1118:delta in the
1117:
1116:Selenga River
1112:
1110:
1109:Bay of Bengal
1106:
1102:
1098:
1092:
1082:
1080:
1076:
1072:
1068:
1064:
1060:
1052:
1048:
1044:
1040:
1036:
1031:
1027:
1025:
1021:
1017:
1007:
1003:
1001:
997:
992:
990:
986:
982:
978:
974:
971:, increasing
970:
966:
962:
958:
955:, pumping of
954:
950:
946:
942:
938:
937:sedimentation
934:
930:
926:
921:
919:
915:
910:
906:
902:
898:
885:
880:
876:
872:
867:
863:
858:
855:
852:, creating a
851:
846:
845:
844:
842:
833:
828:
819:
817:
813:
809:
805:
801:
797:
793:
789:
779:
777:
773:
769:
764:
762:
758:
754:
750:
746:
742:
738:
734:
733:Orinoco River
730:
726:
722:
713:
707:Inland deltas
704:
702:
698:
694:
690:
680:
677:
673:
669:
665:
664:deforestation
660:
656:
652:
641:
639:
634:
630:
626:
614:
610:
606:
601:
597:
588:
586:
582:
578:
574:
570:
566:
565:Okanagan Lake
562:
556:
554:
544:
540:
537:
533:
528:
525:
521:
517:
513:
509:
499:
496:
492:
481:500 yrs BP,×
473:1000 yrs BP,
469:2800 yrs BP,
465:3500 yrs BP,
460:
452:
447:
438:
433:
431:
426:
421:
419:
415:
411:
407:
403:
399:
395:
391:
387:
382:
380:
376:
370:
368:
364:
359:
357:
353:
349:
345:
337:
333:
329:
327:
323:
319:
315:
311:
307:
303:
302:flow velocity
299:
295:
286:
277:
275:
274:Edward Gibbon
271:
266:
264:
260:
259:
254:
248:
242:
230:
226:
222:
218:
214:
210:
206:
202:
198:
194:
190:
186:
182:
178:
177:
172:
168:
164:
163:
158:
155:
151:
147:
137:
135:
131:
127:
123:
119:
114:
112:
108:
104:
100:
96:
92:
88:
84:
80:
76:
72:
68:
64:
56:
52:
48:
41:
37:
32:
25:
21:
6964:River deltas
6887:
6868:List of bogs
6723:Conservation
6654:Ombrotrophic
6598:
6569:Water-meadow
6493:
6304:Grass valley
6294:Flood-meadow
6257:Cypress dome
6188:Cataract bog
6163:Beach meadow
5993:Conservation
5844:Pelagic fish
5824:Coastal fish
5728:Marine fungi
5466:Water garden
5349:Water column
5294:Productivity
5269:Pelagic zone
5229:Macrobenthos
5219:Hydrobiology
5189:Ecohydrology
4839:Volcanic arc
4727:Feeder bluff
4651:
4634:River mouths
4599:Raised beach
4594:Pocket beach
4522:
4493:Tidal island
4483:Strand plain
4428:Natural arch
3868:
3864:River valley
3753:
3749:
3703:Bibliography
3692:
3681:. Retrieved
3667:
3655:
3644:. Retrieved
3640:the original
3635:
3625:
3614:. Retrieved
3610:the original
3605:
3596:
3545:
3541:
3531:
3496:
3492:
3482:
3455:
3451:
3441:
3391:(1): 18746.
3388:
3382:
3372:
3361:. Retrieved
3318:
3312:
3302:
3262:(1): 13–25.
3259:
3255:
3245:
3194:
3188:
3178:
3167:. Retrieved
3137:(1): 23–32.
3134:
3130:
3120:
3085:
3079:
3069:
3058:. Retrieved
3015:
3009:
2984:. Retrieved
2951:
2945:
2934:
2926:
2921:
2910:
2894:
2889:
2878:. Retrieved
2834:
2828:
2815:
2801:: S94–S107.
2798:
2794:
2788:
2753:
2747:
2730:
2726:
2720:
2693:
2689:
2679:
2646:
2642:
2636:
2620:(1): 51–65.
2617:
2613:
2603:
2578:
2574:
2567:
2542:
2538:
2532:
2499:
2493:
2487:
2462:
2456:
2450:
2425:
2421:
2415:
2404:. Retrieved
2363:
2357:
2347:
2322:
2316:
2310:
2277:
2271:
2265:
2248:
2242:
2231:. Retrieved
2222:
2213:
2190:. Retrieved
2162:
2156:
2143:
2132:. Retrieved
2123:
2114:
2107:Partial text
2057:
2053:
2047:
2035:. Retrieved
2025:
2015:
2008:Partial text
1994:
1962:
1950:
1908:
1904:
1898:
1889:
1879:
1841:
1837:
1786:
1780:
1746:
1740:
1717:
1712:
1693:
1687:
1676:. Retrieved
1667:
1658:
1647:. Retrieved
1636:
1627:
1616:. Retrieved
1607:
1598:
1565:
1559:
1530:. Retrieved
1497:
1491:
1480:
1455:
1449:
1413:
1409:
1399:
1358:
1352:
1318:
1314:
1308:
1299:
1290:
1241:Alluvial fan
1137:
1113:
1094:
1056:
1039:Kokemäenjoki
1038:
1013:
1004:
993:
979:, and cause
922:
897:river basins
894:
841:crossbedding
837:
832:Kachemak Bay
787:
785:
765:
725:inland delta
724:
718:
686:
672:urbanization
647:
638:storm surges
629:Ganges Delta
623:
605:Ganges Delta
594:
557:
550:
541:
529:
523:
511:
507:
505:
488:
477:300 yrs BP,
434:
422:
410:Yellow River
383:
379:Alluvial fan
371:
360:
356:distributary
344:shear stress
341:
310:is deposited
291:
270:generic term
267:
257:
207:philosopher
175:
160:
143:
134:carbon sinks
126:ecologically
118:civilization
115:
62:
60:
38:captured by
36:Amazon Delta
6893:Telmatology
6888:River delta
6755:Ramsar site
6745:Marsh organ
6644:Hydric soil
6523:Vernal pool
6506:Shrub swamp
6374:Tidal marsh
6203:Plateau bog
6193:Coastal bog
6183:Blanket bog
5978:Sponge reef
5953:Rocky shore
5948:Oyster reef
5918:Kelp forest
5801:Vertebrates
5701:Marine life
5677:Viral shunt
5642:Marine snow
5544:Maharashtra
5451:Stream pool
5354:Zooplankton
5274:Photic zone
5234:Meiobenthos
5087:Algal bloom
4990:River plume
4804:Steep coast
4777:Rocky shore
4772:Rip current
4652:River delta
4624:Wash margin
4619:Storm beach
4609:Shell beach
4574:Beach wrack
4569:Beach ridge
4559:Beach cusps
4508:Tied island
4498:Tidal marsh
4221:Archipelago
4069:Aggradation
4020:Plunge pool
3987:Stream pool
3977:River mouth
3869:River delta
3493:Nature News
3458:(1): 1–10.
3336:10871/40127
2954:: 275–291.
2037:23 February
1884:pp.514-518.
1128:Lake Baikal
1105:West Bengal
977:sand mining
957:groundwater
953:aggradation
834:at low tide
782:Mega deltas
689:tidal range
651:Pleistocene
437:ecosystem.
386:Mississippi
263:Indus river
229:Koinē Greek
225:Indus River
83:river mouth
63:river delta
6948:Categories
6853:Bog butter
6549:Bog garden
6542:Artificial
6513:Wet meadow
6379:High marsh
6369:Salt marsh
6272:Fen-meadow
6240:Alder carr
6223:Upland bog
6218:String bog
6213:Raised bog
5958:Salt marsh
5893:Coral reef
5682:Whale fall
5662:Photophore
5539:Everglades
5507:Ecoregions
5446:Stream bed
5419:Macrophyte
5372:Freshwater
5204:Food chain
5117:Water bird
4918:Grain size
4892:Submersion
4869:Management
4854:Wind fetch
4814:Surf break
4732:Flat coast
4662:regressive
4448:Salt marsh
4306:Coral reef
4120:Hack's law
4074:Base level
4015:Knickpoint
3942:Oxbow lake
3922:Floodplain
3683:2022-02-22
3646:2020-01-05
3616:2011-11-02
3363:2021-03-13
3169:2021-03-13
3060:2021-03-13
2986:2021-03-13
2880:2020-12-22
2406:2018-09-08
2233:2017-06-12
2192:2019-08-29
2134:2017-06-12
1967:Boggs 2006
1955:Boggs 2006
1943:Boggs 2006
1733:Boggs 2006
1703:0131547283
1678:2017-06-12
1649:2017-12-12
1618:2020-12-21
1283:References
1265:Nile Delta
1101:Bangladesh
1089:See also:
1063:irrigation
1059:sanitation
996:Nile Delta
969:subsidence
945:subsidence
929:ecological
875:subaqueous
862:sand dunes
788:mega delta
757:Bratislava
747:, and the
613:Bangladesh
581:Summerland
573:peninsulas
520:turbidites
414:topography
363:mouth bars
348:floodplain
318:Ural river
146:Nile Delta
71:deposition
55:Nile Delta
24:Lena river
6675:Hydrosere
6663:Processes
6649:Marsh gas
6494:Myristica
6384:Low marsh
6198:Kermi bog
6173:Bofedales
6153:Backswamp
5983:Tide pool
5888:Cold seep
5672:Upwelling
5436:Rheotaxis
5429:Fish pond
5404:Limnology
5329:Substrate
5314:Siltation
5184:Dead zone
4877:Accretion
4859:Wind wave
4819:Surf zone
4674:Processes
4647:Mouth bar
4604:Recession
4584:Beachrock
4503:Tide pool
4433:Peninsula
4321:cliff-top
4208:Landforms
4098:Mechanics
3947:Point bar
3937:Mouth bar
3892:Anabranch
3756:: 53–68.
3570:2045-2322
3474:1687-4285
3415:2045-2322
3353:210166330
3345:2398-9629
3294:129784677
3286:0262-6667
3219:1748-9326
3159:128976925
3151:1862-4057
3112:1748-9326
3050:1752-0908
3041:1912/3207
2976:0272-7714
2867:205251150
2733:: 68–72.
2712:111027461
2663:43442774.
2545:: 29–39.
2380:0160-8347
2294:0277-5212
2082:129299341
1590:143811840
1522:253145418
1458:: 53–78.
1432:1439-037X
1391:129080402
1383:1096-9837
1335:140714394
1189:Delta in
1173:Delta in
1154:Delta in
854:turbidite
830:Delta on
808:Irrawaddy
703:estuary.
683:Estuaries
585:Peachland
457:4600 yrs
358:network.
294:reservoir
280:Formation
176:Histories
171:Herodotus
167:Aeschylus
140:Etymology
122:coastline
103:reservoir
6933:Category
6863:Bog-wood
6858:Bog iron
6848:Bog body
6670:Halosere
6622:Histosol
6617:Acrotelm
6600:Sphagnum
6458:Reed bed
6403:Moorland
6282:Rich fen
6277:Poor fen
6132:Wetlands
6090:Category
6016:HERMIONE
5933:Mangrove
5743:Seagrass
5289:Pleuston
5284:Plankton
5264:Particle
5209:Food web
5008:Category
4834:Undertow
4787:Sea foam
4782:Sea cave
4682:Blowhole
4524:Windwatt
4383:Headland
4231:Avulsion
4158:Category
4043:Antidune
4030:Bedforms
3917:Cut bank
3674:Archived
3588:23722597
3548:: 1926.
3523:24646976
3433:31822705
3357:Archived
3237:30344619
3163:Archived
3054:Archived
2980:Archived
2871:Archived
2859:27760114
2780:33284178
2671:84968414
2524:85128464
2400:Archived
2396:85961542
2302:25962433
2273:Wetlands
2257:49850378
2227:Archived
2183:Archived
2128:Archived
2031:Archived
2023:(1885).
1819:22727856
1811:30068527
1672:Archived
1643:Archived
1612:Archived
1532:19 April
1526:Archived
1321:: 2–48.
1219:See also
1124:Buryatia
1085:Examples
1077:and the
1024:highways
987:through
903:such as
866:bed load
772:Botswana
699:and the
655:Holocene
633:sandbars
577:Naramata
532:buoyancy
430:avulsion
322:gradient
314:alluvium
221:Patalene
189:Polybius
111:sediment
75:sediment
67:landform
42:in 2005.
6959:Ecology
6898:Turbary
6878:Estuary
6453:Pothole
6443:Pocosin
6408:Mudflat
6247:Ciénega
6230:Callows
6146:Natural
5943:Mudflat
5903:Estuary
5873:Bay mud
5851:Seabird
5607:f-ratio
5590:General
5471:Wetland
5259:Neuston
5224:Hypoxia
5169:Biomass
5159:Benthos
5075:General
4958:shingle
4938:granule
4923:boulder
4901:Related
4797:peresyp
4707:Current
4642:Debouch
4551:Beaches
4518:Waituna
4513:Tombolo
4423:Mudflat
4418:Machair
4408:Isthmus
4328:Estuary
4271:Channel
3992:Thalweg
3927:Meander
3854:Estuary
3579:3668317
3550:Bibcode
3501:Bibcode
3424:6904557
3393:Bibcode
3264:Bibcode
3228:6192430
3199:Bibcode
3090:Bibcode
3020:Bibcode
2956:Bibcode
2839:Bibcode
2583:Bibcode
2547:Bibcode
2516:1352687
2467:Bibcode
2388:1352839
2327:Bibcode
2167:Bibcode
2062:Bibcode
1913:Bibcode
1846:Bibcode
1791:Bibcode
1718:Geology
1502:Bibcode
1460:Bibcode
1363:Bibcode
1253:Estuary
949:erosion
914:erosion
792:Yangtze
693:estuary
659:estuary
625:Erosion
536:inertia
485:current
483:
479:
475:
471:
467:
463:
455:
406:Yangtze
298:channel
249:
181:Ionians
95:estuary
6468:Slough
6423:Pakihi
6413:Muskeg
6339:Kettle
6309:Guelta
5928:Lagoon
5254:Nekton
5112:Mammal
5107:Insect
4948:pebble
4943:gravel
4933:cobble
4478:Strait
4458:Skerry
4413:Lagoon
4398:Island
4353:Fundus
4256:Bodden
4010:Canyon
3957:Rapids
3952:Riffle
3732:
3712:
3586:
3576:
3568:
3521:
3472:
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3351:
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2916:(1984)
2897:(1972)
2865:
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2830:Nature
2778:
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2522:
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2442:211476
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1817:
1809:
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1608:Druide
1588:
1582:228368
1580:
1520:
1430:
1389:
1381:
1333:
1160:THEMIS
1020:gravel
963:, and
878:delta.
814:, and
804:Mekong
753:Danube
749:Sistan
743:, the
670:, and
583:, and
493:, and
408:, and
398:Ganges
394:Amazon
375:avulse
352:levees
258:Indica
253:Arrian
203:, the
201:Strabo
6994:Water
6564:Swale
6533:Yaéré
6496:swamp
6473:Swamp
6428:Palsa
6418:Oasis
6398:Misse
6349:Marsh
6319:Igapó
6314:Hamun
6289:Flark
6262:Dambo
6158:Bayou
5319:Spawn
4829:Swash
4792:Shoal
4473:Stack
4463:Sound
4453:Shoal
4403:Islet
4388:Inlet
4378:Hapua
4343:Fjord
4338:Fjard
4333:Firth
4281:Coast
4276:Cliff
4251:Bight
4226:Atoll
3677:(PDF)
3664:(PDF)
3349:S2CID
3290:S2CID
3155:S2CID
2874:(PDF)
2863:S2CID
2825:(PDF)
2776:S2CID
2708:S2CID
2667:S2CID
2659:JSTOR
2520:S2CID
2512:JSTOR
2438:JSTOR
2392:S2CID
2384:JSTOR
2298:S2CID
2186:(PDF)
2153:(PDF)
2078:S2CID
1815:S2CID
1807:JSTOR
1586:S2CID
1578:JSTOR
1518:S2CID
1387:S2CID
1331:S2CID
1259:Levee
816:Indus
796:Pearl
701:Tagus
609:India
495:tidal
441:Types
402:Indus
326:slope
268:As a
217:India
205:Cynic
197:Isère
193:Rhône
157:drama
107:delta
87:ocean
79:river
65:is a
26:delta
6760:List
6627:Peat
6582:Life
6448:Pond
6393:Mere
6344:Lagg
6324:Ings
6235:Carr
5424:Pond
4963:silt
4953:sand
4928:clay
4657:mega
4468:Spit
4438:Reef
4368:Gulf
4316:Dune
4311:Cove
4266:Cape
4236:Ayre
4048:Dune
3730:ISBN
3710:ISBN
3584:PMID
3566:ISSN
3519:PMID
3470:ISSN
3429:PMID
3411:ISSN
3341:ISSN
3282:ISSN
3233:PMID
3215:ISSN
3147:ISSN
3108:ISSN
3046:ISSN
2972:ISSN
2855:PMID
2766:ISBN
2376:ISSN
2290:ISSN
2253:OCLC
2099:ISBN
2039:2022
2000:ISBN
1751:ISBN
1698:ISBN
1561:Isis
1534:2023
1428:ISSN
1379:ISSN
1114:The
1103:and
1095:The
1043:Pori
1033:The
1018:and
1016:sand
998:and
947:and
927:and
916:and
759:and
611:and
603:The
491:wave
390:Nile
247:lit.
195:and
185:silt
99:lake
51:NASA
40:NASA
6267:Fen
6178:Bog
5486:Fen
5476:Bog
4443:Ria
4373:Gut
4363:Geo
4358:Gat
4246:Bay
4038:Ait
3758:doi
3738:doi
3718:doi
3574:PMC
3558:doi
3509:doi
3497:507
3460:doi
3419:PMC
3401:doi
3331:hdl
3323:doi
3272:doi
3223:PMC
3207:doi
3139:doi
3098:doi
3036:hdl
3028:doi
2964:doi
2952:183
2914:AGI
2847:doi
2835:539
2803:doi
2758:doi
2735:doi
2698:doi
2651:doi
2622:doi
2591:doi
2579:115
2555:doi
2504:doi
2475:doi
2430:doi
2368:doi
2335:doi
2282:doi
2175:doi
2070:doi
1921:doi
1854:doi
1842:133
1799:doi
1787:100
1570:doi
1510:doi
1468:doi
1456:361
1418:doi
1414:206
1371:doi
1323:doi
1122:of
1045:in
965:gas
961:oil
909:dam
800:Red
770:in
761:Iža
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