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Journal articles on the topic 'Fluvial geomorphology'

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Published: 4 June 2021
Last updated: 29 July 2024

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1

Dollar, Evan S. J. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 26, no. 1 (March 2002): 123–43. http://dx.doi.org/10.1191/0309133302pp328pr.

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2

Dollar, Evan S. J. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 28, no. 3 (September 2004): 405–50. http://dx.doi.org/10.1191/0309133304pp419pr.

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3

Hardy, Richard J. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 29, no. 3 (September 2005): 411–25. http://dx.doi.org/10.1191/0309133305pp457pr.

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4

Hardy, Richard J. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 30, no. 4 (August 2006): 553–67. http://dx.doi.org/10.1191/0309133306pp498pr.

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5

Dollar, Evan S. J. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 24, no. 3 (September 2000): 385–406. http://dx.doi.org/10.1177/030913330002400305.

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6

Stott, Tim. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 34, no. 2 (January 26, 2010): 221–45. http://dx.doi.org/10.1177/0309133309357284.

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This progress report on the discipline of fluvial geomorphology reviews 147 papers published in 21 key journals during the calendar years of 2006 and 2007. Papers are grouped by themes to cover 10 subject areas. The themes were chosen by classifying all geomorphological articles published in a single leading journal for the same period, of which (44%) were within the subject area of fluvial geomorphology. Themes (in order of number contributing to the total) were: ‘River management, restoration and effects of vegetation on fluvial systems’; ‘Soil erosion and control’; ‘Fluvial hydraulics’; ‘Fluvial sediment transport’; ‘Gully and hillslope sediment transfer’; ‘Modelling the fluvial environment’; ‘River regulation, channel change and human influences’; ‘Advances in methodology in fluvial geomorphology’; ‘Bank erosion in fluvial systems’; and ‘Holocene fluvial chronology’.
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7

Richards, Keith. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 10, no. 3 (September 1986): 401–20. http://dx.doi.org/10.1177/030913338601000304.

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8

Richards, Keith. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 11, no. 3 (September 1987): 432–57. http://dx.doi.org/10.1177/030913338701100309.

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9

Richards, Keith. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 12, no. 3 (September 1988): 435–56. http://dx.doi.org/10.1177/030913338801200307.

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10

Rhoads, Bruce L. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 16, no. 4 (December 1992): 456–77. http://dx.doi.org/10.1177/030913339201600404.

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11

Rhoads, Bruce L. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 18, no. 1 (March 1994): 103–23. http://dx.doi.org/10.1177/030913339401800107.

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12

Rhoads, Bruce L. "Fluvial geomorphology." Progress in Physical Geography: Earth and Environment 18, no. 4 (December 1994): 588–608. http://dx.doi.org/10.1177/030913339401800409.

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13

Marcus, W. Andrew. "Experimental fluvial geomorphology." Geomorphology 3, no. 1 (January 1990): 96–97. http://dx.doi.org/10.1016/0169-555x(90)90038-r.

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14

Hadley, Richard F. "Experimental Fluvial Geomorphology." Eos, Transactions American Geophysical Union 69, no. 32 (1988): 773. http://dx.doi.org/10.1029/88eo01058.

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15

BAKER, VICTOR R. "Geological fluvial geomorphology." Geological Society of America Bulletin 100, no. 8 (August 1988): 1157–67. http://dx.doi.org/10.1130/0016-7606(1988)100<1157:gfg>2.3.co;2.

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16

Stott, Tim. "Fluvial geomorphology 2008–2009." Progress in Physical Geography: Earth and Environment 35, no. 6 (August 22, 2011): 810–30. http://dx.doi.org/10.1177/0309133311415785.

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This progress report on the discipline of fluvial geomorphology reviews 134 papers, 112 of which were published in Earth Surface Processes and Landforms ( ESPL) during the calendar years of 2008 and 2009. It continues where the last report for 2006 and 2007 ( Stott, 2010 ) ended. Papers are again grouped by themes to cover 10 subdisciplines within the subject area. The themes were chosen by classifying all geomorphological articles published in ESPL for the same period, of which 38% were within the subject area of fluvial geomorphology. Themes (in order of number contributing to the total) were: fluvial sediment transport; soil erosion and control; modelling the fluvial environment; river management, restoration and effects of vegetation on fluvial systems; gully and hillslope sediment transfer; river regulation, channel change and human influences; advances in methodology in fluvial geomorphology; fluvial hydraulics; fluvial chronology; and bank erosion in fluvial systems. The 2006–2007 and 2008–2009 periods are compared and it was found that broadly the same themes retained their popularity (in terms of numbers of papers published) as in the previous report for 2006–2007.
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17

Giano, Salvatore Ivo. "Fluvial Geomorphology, River Management and Restoration." Water 16, no. 3 (January 29, 2024): 432. http://dx.doi.org/10.3390/w16030432.

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This Special Issue follows a previous SI titled “Fluvial geomorphology and river management”, published in 2021, which addressed the role of fluvial geomorphology in landscape evolution and the impact produced by human activities on fluvial systems [...]
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18

Dollar, E. S. J. "Progress reports, Fluvial geomorphology." Progress in Physical Geography 24, no. 3 (September 1, 2000): 385–407. http://dx.doi.org/10.1191/030913300701542697.

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19

Chin, Anne. "Tools in Fluvial Geomorphology." Annals of the Association of American Geographers 95, no. 3 (September 2005): 713–15. http://dx.doi.org/10.1111/j.1467-8306.2005.00482_10.x.

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20

Giano, Salvatore Ivo. "Fluvial Geomorphology and River Management." Water 13, no. 11 (June 7, 2021): 1608. http://dx.doi.org/10.3390/w13111608.

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21

Andrews, E. D., T. P. Burt, and D. E. Walling. "Catchment Experiments in Fluvial Geomorphology." Arctic and Alpine Research 17, no. 3 (August 1985): 349. http://dx.doi.org/10.2307/1551025.

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22

Wharton, Geraldene, and K. J. Gregory. "Fluvial Geomorphology of Great Britain." Geographical Journal 165, no. 3 (November 1999): 336. http://dx.doi.org/10.2307/3060466.

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23

Newman, W. I., and D. L. Turcotte. "Cascade model for fluvial geomorphology." Geophysical Journal International 100, no. 3 (March 1990): 433–39. http://dx.doi.org/10.1111/j.1365-246x.1990.tb00696.x.

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24

Douglas, I. "Fluvial Geomorphology and River Management." Australian Geographical Studies 38, no. 3 (November 2000): 253–62. http://dx.doi.org/10.1111/1467-8470.00114.

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25

Goudie, Andrew S. "Global warming and fluvial geomorphology." Geomorphology 79, no. 3-4 (September 2006): 384–94. http://dx.doi.org/10.1016/j.geomorph.2006.06.023.

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26

BAKER, V. R. "Fluvial Geomorphology: The Colorado River." Science 229, no. 4711 (July 26, 1985): 376–77. http://dx.doi.org/10.1126/science.229.4711.376.

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27

Behnke, J. J. "Catchment experiments in fluvial geomorphology." Earth-Science Reviews 22, no. 2 (September 1985): 157. http://dx.doi.org/10.1016/0012-8252(85)90022-4.

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28

Nicholas, Andrew P. "Cellular modelling in fluvial geomorphology." Earth Surface Processes and Landforms 30, no. 5 (2005): 645–49. http://dx.doi.org/10.1002/esp.1231.

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29

Tooth, Stephen, and Gerald C. Nanson. "The geomorphology of Australia's fluvial systems: retrospect, perspect and prospect." Progress in Physical Geography: Earth and Environment 19, no. 1 (March 1995): 35–60. http://dx.doi.org/10.1177/030913339501900103.

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This article provides a review of the study and geomorphology of Australia's fluvial systems by offering comment on the development, concerns and future of the subject. Trends in the history of fluvial landform studies in Australia are traced from the observations and comments of the early explorers and visiting scientists through to the emergence and growth of fluvial geomorphology as a study discipline. Subsequent development of the idea of a distinctive geomorphology of Australian fluvial systems that often contrast with Anglo-American observations is outlined and illustrated with particular reference to fluvial studies in south-east Australia. Key features of the Australian setting include low long-term denudation rates, the absence of extensive Quaternary glaciation and the predominance of low gradient fluvial systems over much of the continent. Some of the most important themes in contemporary Australian fluvial research are discussed and include long-term landscape evolution, thresholds and riverine response to secular trends in climate, Quaternary environmental change, arid-environment systems, bedrock channels and applied approaches to study. Consideration is also given to present deficiencies in research and to future priorities. Particular attention is focused on the need firstly to collect additional process data, secondly to shift the bias in research away from south-east Australia, and thirdly to develop links between fluvial process and alluvial stratigraphy/chronology. It is concluded that, given the variety of hydrogeomorphological environments in Australia and the diversity of approaches to study, ongoing research will provide further indications of the unusual nature of many of the continent's fluvial systems.
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30

Arnaud-Fassetta, Gilles, Laurent Astrade, Éric Bardou, Jeannine Corbonnois, Daniel Delahaye, Monique Fort, Emmanuèle Gautier, et al. "Fluvial geomorphology and flood-risk management." Géomorphologie : relief, processus, environnement 15, no. 2 (July 1, 2009): 109–28. http://dx.doi.org/10.4000/geomorphologie.7554.

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31

Everard, Mark, and Nevil Quinn. "Realizing the value of fluvial geomorphology." International Journal of River Basin Management 13, no. 4 (June 10, 2015): 487–500. http://dx.doi.org/10.1080/15715124.2015.1048457.

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32

Oguchi, Takashi, Kyoji Saito, Hiroshi Kadomura, and Michael Grossman. "Fluvial geomorphology and paleohydrology in Japan." Geomorphology 39, no. 1-2 (July 2001): 3–19. http://dx.doi.org/10.1016/s0169-555x(01)00048-4.

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33

Kasvi, Elina, Janet Hooke, Matti Kurkela, Matti T. Vaaja, Juho-Pekka Virtanen, Hannu Hyyppä, and Petteri Alho. "Modern empirical and modelling study approaches in fluvial geomorphology to elucidate sub-bend-scale meander dynamics." Progress in Physical Geography: Earth and Environment 41, no. 5 (July 12, 2017): 533–69. http://dx.doi.org/10.1177/0309133317715870.

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Major developments in theory and modelling techniques have taken place within the past couple of decades in the field of the fluvial geomorphology. In this review, we examine the state-of-the-art empirical and modelling approaches and discuss their potential benefits and shortcomings in deepening understanding of the sub-bend-scale fluvial geomorphology of meander bends. Meandering rivers represent very complex 3D flow and sedimentary processes. We focus on high-resolution techniques which have improved the spatial and temporal resolution of the data and thereby enabled investigation of processes, which have been thus far beyond the capacity of the measurement techniques. This review covers the measurement techniques applied in the field and in laboratory circumstances as well as the close-range remote sensing techniques and computational approaches. We discuss the key research questions in fluvial geomorphology of meander bends and demonstrate how the contemporary approaches have been and could be applied to solve these questions.
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34

Morón, Sara, Kathryn Amos, and Sandra Mann. "Fluvial reservoirs in dryland endorheic basins: the Lake Eyre Basin as a world-class modern analogue." APPEA Journal 54, no. 1 (2014): 119. http://dx.doi.org/10.1071/aj13014.

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Intracratonic dryland basins have been common throughout geological time and significant hydrocarbon reservoirs are contained in these basins. Based on a literature compilation of fluvial dryland reservoirs, the authors demonstrate the need for new modern analogue data from dryland fluvial systems, and present new field data from the Neales River, in the Lake Eyre catchment. The selected study reach has a complex planform, with a downstream transition from single channel to anabranching. Results of the observations of the channel bed grain size, the geomorphology and the channel geometry (width and depth) allow the authors to infer that the channel bed grain size is more strongly related to planform geomorphology than the channel geometry (width to depth ratios). Based on the grain size and channel geometry data the authors present, the authors conclude that the planform geomorphology exerts a greater control on channel bed material size than channel geometry. This interpretation is based on the analysis of satellite imagery, topographic survey data and grain size descriptions. In this paper, the authors provide channel geometry data and grain size data that will improve understanding of dryland fluvial sedimentology. The authors hope this contributes to enhancing hydrocarbon exploration and production in petroleum reservoirs developed in dryland fluvial settings.
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35

Assine, Mario Luis, Eder Renato Merino, Fabiano do Nascimento Pupim, Hudson de Azevedo Macedo, and Mauricio Guerreiro Martinho dos Santos. "The Quaternary alluvial systems tract of the Pantanal Basin, Brazil." Brazilian Journal of Geology 45, no. 3 (September 2015): 475–89. http://dx.doi.org/10.1590/2317-4889201520150014.

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ABSTRACT The Pantanal Basin is an active sedimentary basin in central-west Brazil that consists of a complex alluvial systems tract characterized by the interaction between different river systems developed in one of the largest wetlands in the world. The Paraguay River is the trunk river system that drains the water and part of the sediment load received from areas outside of the basin. Depositional styles vary considerably along the river profiles throughout the basin, with the development of entrenched meandering belts, anastomosing reaches, and floodplain ponds. Paleodrainage patterns are preserved on the surface of abandoned lobes of fluvial fans, which also exhibit many degradational channels. Here, we propose a novel classification scheme according to which the geomorphology, hydrological regime and sedimentary dynamics of these fluvial systems are determined by the geology and geomorphology of the source areas. In this way, the following systems are recognized and described: (I) the Paraguay trunk-river plains; (II) fluvial fans sourced by the tablelands catchment area; (III) fluvial fans sourced by lowlands; and (IV) fluvial interfans. We highlight the importance of considering the influences of source areas when interpreting contrasting styles of fluvial architectures in the rock record.
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36

Lazzari, Maurizio. "GIS Application in Fluvial Geomorphology and Landscape Changes." Water 12, no. 12 (December 10, 2020): 3481. http://dx.doi.org/10.3390/w12123481.

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The main purpose of this Special Issue of Water is to propose on overview of studies and researches, in which the use of GIS is functional to the representation of fluvial geomorphology and river dynamics, linear erosion processes, erosion rates, ancient landscapes reshaped by the fluvial action, flooding areas, and historical anthropic changes of the river landscape and land use [...]
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37

Smith, L., and P. Rogers. "Applied fluvial geomorphology in the 21st century." Water e-Journal 4, no. 1 (April 1, 2019): 1–6. http://dx.doi.org/10.21139/wej.2019.009.

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38

Douglas, Ian. "Fundamentals of Fluvial Geomorphology- by Ro Charlton." Geographical Research 47, no. 1 (March 2009): 86–87. http://dx.doi.org/10.1111/j.1745-5871.2008.00565.x.

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39

Kale, Vishwas S. "Fluvial geomorphology of Indian rivers: an overview." Progress in Physical Geography: Earth and Environment 26, no. 3 (September 2002): 400–433. http://dx.doi.org/10.1191/0309133302pp343ra.

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The rivers of India reveal certain special characteristics because they undergo large seasonal fluctuations in flow and sediment load. The rivers are adjusted to an array of discharges, and most rivers exhibit morphologies that are related to high-magnitude floods. In the last 100 years primarily hydraulic engineers have contributed to the understanding of the fluvial forms and processes. Though this trend has continued even today, in recent decades some interesting fluvial research has also been carried out by earth scientists. Four large rivers, namely Brahmaputra, Kosi, Indus and Narmada, have received greater attention from fluvial geomorphologists. The major themes in Indian fluvial geomorphology include the hydrology of monsoonal rivers; forms and processes in alluvial channels; causes of avulsion, channel migration; and anomalous variations in channel patterns; dynamics of suspended sediment; and the geomorphic impacts of floods. Studies of bedrock channels are far less than similar studies in alluvial channels. Only a few rivers have been investigated in this respect. Studies indicate that the Himalayan rivers are different in many respects from those of the Indian Peninsula. The former occupy a highly dynamic environment with extreme variability in discharge and sediment load. Earthquakes and landslides also have a great impact on these rivers from time to time. Consequently, the rivers are characterized by frequent changes in shape, size, position and planform. In comparison, the adjustments in Peninsular rivers are less frequent and of a much smaller magnitude. An inescapable conclusion is that in the tropical monsoonal environment, large floods are important geomorphic agents that temporarily affect the forms and behavioural characteristics of some rivers, but leave a lasting effect on others. In magnitude-frequency terms, large floods are major formative events in many rivers of the Indian region in general and the Indian Peninsula in particular.
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40

Vandenberghe, Jef, and Darrel Maddy. "The significance of fluvial archives in geomorphology." Geomorphology 33, no. 3-4 (June 2000): 127–30. http://dx.doi.org/10.1016/s0169-555x(99)00119-1.

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41

Fuller, Ian. "Fundamentals of fluvial geomorphology - By Ro Charlton." New Zealand Geographer 66, no. 1 (April 2010): 93–94. http://dx.doi.org/10.1111/j.1745-7939.2010.01176_4.x.

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42

Graf, William L. "Natural and anthropogenic influences in fluvial geomorphology." Journal of Hydrology 190, no. 1-2 (March 1997): 165–67. http://dx.doi.org/10.1016/s0022-1694(97)83309-4.

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43

Macdonald, Neil. "Fundamentals of fluvial geomorphology - by Ro Charlton." Area 41, no. 2 (June 2009): 225. http://dx.doi.org/10.1111/j.1475-4762.2009.883_5.x.

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44

Richards, Keith, and Nicholas Clifford. "Fluvial geomorphology: structured beds in gravelly rivers." Progress in Physical Geography: Earth and Environment 15, no. 4 (December 1991): 407–22. http://dx.doi.org/10.1177/030913339101500404.

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45

Vita-Finzi, Claudio. "River history." Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences 370, no. 1966 (May 13, 2012): 2029–39. http://dx.doi.org/10.1098/rsta.2011.0604.

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During the last half century, advances in geomorphology—abetted by conceptual and technical developments in geophysics, geochemistry, remote sensing, geodesy, computing and ecology—have enhanced the potential value of fluvial history for reconstructing erosional and depositional sequences on the Earth and on Mars and for evaluating climatic and tectonic changes, the impact of fluvial processes on human settlement and health, and the problems faced in managing unstable fluvial systems.
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46

Dollar, Evan S. J. "Palaeofluvial geomorphology in southern Africa: a review." Progress in Physical Geography: Earth and Environment 22, no. 3 (September 1998): 325–49. http://dx.doi.org/10.1177/030913339802200302.

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This article presents an overview of palaeofluvial geomorphology research in southern Africa. For the purposes of this article this includes South Africa, Zimbabwe, Namibia, Lesotho, Swaziland and Botswana. Although interest in fluvial systems has a long history in southern Africa, the scientific study of rivers was initiated by the discovery of the first alluvial diamond along the banks of the Orange River in 1867. Since then, significant progress has been made in unravelling the fluvial history of southern Africa from the early Archaean Ventersdorp Contact Reef River to modern channel process studies. The development of an understanding of palaeofluvial systems has occurred along two main lines. The first was alluvial diamond exploration work undertaken by the large mining houses. The second line was of a more ‘academic’ interest and included determining the impact of superimposition, tectonics, base level and climate changes. The review suggests that southern Africa fluvial systems have shown large-scale changes in drainage pattern, discharge and sediment yield and that these can be related to a complex set of causative factors including the geological template, the Jurassic rifting of Gondwana, tectonic episodes and climate change.
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47

Gilvear, David J. "Fluvial geomorphology and river engineering: future roles utilizing a fluvial hydrosystems framework." Geomorphology 31, no. 1-4 (December 1999): 229–45. http://dx.doi.org/10.1016/s0169-555x(99)00086-0.

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48

Stott, Tim. "Review of research in fluvial geomorphology 2010–2011." Progress in Physical Geography: Earth and Environment 37, no. 2 (February 15, 2013): 248–58. http://dx.doi.org/10.1177/0309133313477124.

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This progress report on the discipline of fluvial geomorphology for the calendar years 2010–2011 extends the analysis carried out by Stott (2010, 2011) of papers published in Earth Surface Processes and Landforms ( ESPL) during the calendar years 2006–2007 and 2008–2009 to include the period of 2010–2011. A total of 327 papers were published in the 30 issues of ESPL during the review period, up from 284 during 2006–2007 and 300 in 2008–2009. Of these papers, 175 (54%) were within the subject area of fluvial geomorphology, compared to 125 out of 284 (44%) in the 2006–2007 period, and 113 out of 297 (38%) in the 2008–2009 period. In comparing the three two-year periods covering 2006–2011, the numbers of papers in each of 10 subdisciplines within fluvial geomorphology (e.g. bank erosion, hydraulics, soil erosion) changed markedly. For example, river management, restoration and the effects of vegetation on fluvial systems changed from first in rank in 2006–2007 to tied in fourth place in 2008–2009 and eighth in 2010–2011. In contrast, the subdiscipline of soil erosion was consistently the second-ranked topic in each of the three two-year periods. Following the analysis of patterns of publications in ESPL, selected papers from each of the 10 subdisciplines are reviewed. The articles discussed were selected by searching using keywords from the 10 subdisciplines using http://scholar.google.co.uk, then selecting a relevant journal article from the first 10 hits returned. In this way, 33 papers drawn from 22 journals were sampled and their key findings are summarized.
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49

Goswami, Kaushalendra Prakash, and Himanshu Shekher. "Hydro-geomorphological research in earth sciences: A systematic review of literature." National Geographical Journal of India 68, no. 4 (December 31, 2022): 266–73. http://dx.doi.org/10.48008/ngji.1815.

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Water is the most important geomorphic agent for geomorphological action. Hydro-geomorphology is a sub-field of geomorphology that provides a scientific description of the evolution of landforms. The former deals with the study of the spatial interaction of water with the earth's surface. The introduction and implementation of new techniques make descriptions more useful and informative. Remote sensing and GIS provide highly dynamic space through which assessment and analysis of these geomorphic forms become feasible. The application of hydro-geomorphological study is most useful in management and planning. The present paper focuses on a systematic review of literature on geomorphology, hydro-geomorphology, and mapping, and explains how sub-discipline such as fluvial geomorphology is different from hydro- geomorphological.
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50

Rosanov, L. L. "THE DEVELOPMENT OF SOME IDEAS OF FLUVIAL GEOMORPHOLOGY." Geomorphology RAS, no. 1 (July 20, 2015): 20. http://dx.doi.org/10.15356/0435-4281-2007-1-20-28.

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