Gotowe bibliografie tematyczne / Fluvial geomorphology

Gotowa bibliografia na temat „Fluvial geomorphology”

Autor: Grafiati
Data publikacji: 4 czerwca 2021
Data aktualizacji: 29 lipca 2024

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Artykuły w czasopismach na temat "Fluvial geomorphology"

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Dollar, Evan S. J. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 26, nr 1 (marzec 2002): 123–43. http://dx.doi.org/10.1191/0309133302pp328pr.

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Dollar, Evan S. J. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 28, nr 3 (wrzesień 2004): 405–50. http://dx.doi.org/10.1191/0309133304pp419pr.

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Hardy, Richard J. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 29, nr 3 (wrzesień 2005): 411–25. http://dx.doi.org/10.1191/0309133305pp457pr.

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Hardy, Richard J. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 30, nr 4 (sierpień 2006): 553–67. http://dx.doi.org/10.1191/0309133306pp498pr.

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Dollar, Evan S. J. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 24, nr 3 (wrzesień 2000): 385–406. http://dx.doi.org/10.1177/030913330002400305.

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Stott, Tim. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 34, nr 2 (26.01.2010): 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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Richards, Keith. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 10, nr 3 (wrzesień 1986): 401–20. http://dx.doi.org/10.1177/030913338601000304.

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Richards, Keith. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 11, nr 3 (wrzesień 1987): 432–57. http://dx.doi.org/10.1177/030913338701100309.

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Richards, Keith. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 12, nr 3 (wrzesień 1988): 435–56. http://dx.doi.org/10.1177/030913338801200307.

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Rhoads, Bruce L. "Fluvial geomorphology". Progress in Physical Geography: Earth and Environment 16, nr 4 (grudzień 1992): 456–77. http://dx.doi.org/10.1177/030913339201600404.

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Rozprawy doktorskie na temat "Fluvial geomorphology"

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Alqahtani, Faisal A. "3D seismic geomorphology of fluvial systems". Thesis, Imperial College London, 2010. http://hdl.handle.net/10044/1/6180.

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Fluvial sandstones constitute one of the major clastic petroleum reservoir types in many sedimentary basins around the world. This is especially true in the Tertiary basins of Southeast Asia, which display a wide range of fluvial channel reservoir types. This study is based on the analysis of high-resolution, shallow (seabed to ca. 500 m depth) 3D seismic data which provide exceptional imaging of the geometry, dimension and temporal and spatial distribution of fluvial channels. The Malay Basin comprises a thick (>8 km), rift to post-rift Oligo-Miocene to Pliocene basin-fill. The youngest (Miocene to Pliocene), post-rift succession is dominated by a thick (1-5 km), cyclic succession of coastal plain and coastal deposits, which accumulated in a humidtropical climatic setting. This study focuses on the Pleistocene to Recent (ca. 500 m thick) succession, which comprises a range of seismic facies, mainly reflecting changes in fluvial channel style and gross stratigraphic architecture. The succession has been divided into four seismic units (Unit 1-4), bounded by basin-wide stratal surfaces. Units 3 and 4 have been further divided into two sub-units. Two types of boundaries have been identified: 1) a boundary that is defined by a regionally-extensive erosion surface at the base of a prominent incised valley (e.g. Horizons C.1 and D.1); 2) a sequence boundary that is defined by more weakly-incised, straight and low-sinuosity channels which is interpreted as lowstand alluvial bypass channel systems (e.g. Horizons A, B, C, and D). Each unit displays a predictable vertical change of the channel pattern and scale, with wide low-sinuosity channels at the base passing gradationally upwards into narrow high-sinuosity channels at the top. The wide variation in channel style and size is interpreted to be controlled mainly by the sea-level fluctuations on the widely flat and tectonically-quiescent Sundaland Platform.
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Saville, Christopher. "Fluvial and tectonic geomorphology of orogenic plateaux". Thesis, Durham University, 2013. http://etheses.dur.ac.uk/7718/.

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Geomorphology is an expression of processes acting upon an area. The links between driving processes and the resulting geomorphology are far from being fully understood. This thesis investigates controls on the dynamics and behaviour of fluvial systems from the interior of orogenic plateaux to the tectonically active plateaux margins. Orogenic plateaux provide a good study area by juxtaposing different tectonic and climatic settings that are served by the same sediment transport systems, allowing for observation of different variables on the same or similar fluvial systems. This is the first time that rivers draining orogenic plateaux have been extensively investigated. The Turkish-Iranian and Tibetan plateaux are the study areas. Forms of rivers draining from plateaux interiors, through the plateaux margins are analysed, along with alluvial fans within both the plateaux interior and plateaux margins. Plateau draining rivers act as the major route for material leaving the plateau region and a first-order control on erosive processes retarding plateau growth. Alluvial fans redistribute material within the plateau interior, enhancing the low relief topography diagnostic of a plateau. It is found that rivers draining plateaux show a sigmoidal form associated with the edge of the plateaux. High gradients and curvatures occur within the mountain ranges at the plateaux margins, while low values are present within the plateau interiors. Modelling work demonstrates that such forms to be likely responses for all plateau-draining rivers, but are most sensitive to the effects of precipitation upon a river’s ability to incise in-to the underlying sedimentary cover and bedrock lithologies. Alluvial fans in orogenic plateau regions are larger and with a lower surface gradient within the plateau interior than those nearer the active tectonic margins. It is theorised that this is due to the lack of lateral control on the accommodation space of alluvial fans within the plateau interior.
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Warwick, Gail L. "The geomorphology and sedimentology of terminal fluvial systems". Thesis, University of Aberdeen, 2006. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.487421.

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The geomorphology and sedimentology of terminal fluvial systems. Fluvial systems operating within drylands commonly experience downstream discharge reduction due to infiltration, evaporation and limited tributary inputs. Sediment bodies developed within the distal zones of rivers that do not drain into the sea or a lake (terminal fluvial systems) are currently represented by the terminal fan facies model. This model summarises the development of a distally thinning and fining sedimentary wedge from a coeval network of low sinuosity distributary channels as induced by the sub aerial termination ofchannelised flow under a dryland climate regime.. Extensive review of sediment fan bodies located within modern drylands highlights pronounced disequilibrium between planform character and present ephemeral flow conditions. Out of eighty documented fluvial systems no convincing examples fit the terminal fan model, including two commonly cited analogues used to support this model. In order to fully evaluate the terminal fan concept and redress the current imbalance in modern analogue studies, field work was undertaken to characterise sub aerial fluvial system termination within a single physiographic province - the Basin and Range rift complex of the southwestern U.S.A. Documentation of the potential range in fluvial style and character within this modern dryland environment is provided by the detailed study of seven terminal fluvial systems. Basin and Range terminal fluvial systems demonstrate strong geomorphic form inheritance. Fan landforms observed within medial and distal reaches of these systems predominantly represent relic Late Pleistocene highstand delta bodies into which the modern system is inset. Active terminal reaches operate within basin centre playa environments where shallo~ gradients induce frequent avulsion and the generation of composite lowstand fan bodies located downstream of lateral system confinement. These terminal features record non-coeval channel activity and the dominance of sinuous channel forms. Morphometric trends distinguish a general downstream reduction in channel scale characterised by the development of progressively narrower and shallower channel forms. Channelised flow is maintained within proximal and medial reaches but does not dominate distal reaches where sheetflow discharge is readily attained. Concomitant reductions in channel capacity and competence control the volume and calibre of fluvial material supplied to basinal environments. Progressive downstream thinning is associated with selective deposition and general basinwards sediment fining and sorting. Terminal reaches transport negligible bedload material and display a comparable depositional record to that generated by background playa sedimentation. Identified similarities with the terminal fan model include downstream loss of channel definition, sediment thinning, fining and improved sorting. Conversely, coeval distributive flow is not observed, constituent channels record moderate to high sinuosity and negligible fluvial material reaches basin centre locations. Basin and Range systems are principally responding to streampower reduction controlled primarily by gradient and enhanced by discharge attenuation. Sub aerial termination dominates due to the absence of basin centre lacustrine bodies; a condition forced by limited discharge supply from catchment reaches, compounded by transmission losses and maintained by excessive evaporation from extensive, low elevation flat playa surfaces. In conclusion, fluvial fan landforms generated exclusively from discharge attenuation do not characterise modern dryland environments. Selection of modern analogue systems for use in the interpretation and prediction of ancient fluvial successions must acknowledge the influence of high frequency and high magnitude climate fluctuations upon modern fluvial geomorphology. Key to this is an appreciation of modern processform disequilibrium and the identification of inherited planform characteristics.
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Wilson, David William. "On the problem of indeterminacy in fluvial geomorphology". Thesis, University of Southampton, 2001. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.246883.

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Clement, David T. "Fluvial geomorphology of the Yukon River, Yukon Flats, Alaska". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape9/PQDD_0015/MQ47994.pdf.

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Dietrich, James. "Applications of Structure-from-Motion Photogrammetry to Fluvial Geomorphology". Thesis, University of Oregon, 2015. http://hdl.handle.net/1794/18701.

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Since 2011, Structure-from-Motion Multi-View Stereo Photogrammetry (SfM or SfM-MVS) has gone from an overlooked computer vision technique to an emerging methodology for collecting low-cost, high spatial resolution three-dimensional data for topographic or surface modeling in many academic fields. This dissertation examines the applications of SfM to the field of fluvial geomorphology. My research objectives for this dissertation were to determine the error and uncertainty that are inherent in SfM datasets, the use of SfM to map and monitor geomorphic change in a small river restoration project, and the use of SfM to map and extract data to examine multi-scale geomorphic patterns for 32 kilometers of the Middle Fork John Day River. SfM provides extremely consistent results, although there are systematic errors that result from certain survey patterns that need to be accounted for in future applications. Monitoring change on small restoration stream channels with SfM gave a more complete spatial perspective than traditional cross sections on small-scale geomorphic change. Helicopter-based SfM was an excellent platform for low-cost, large scale fluvial remote sensing, and the data extracted from the imagery provided multi-scalar perspectives of downstream patterns of channel morphology. This dissertation makes many recommendations for better and more efficient SfM surveys at all of the spatial scales surveyed. By implementing the improvements laid out here and by other authors, SfM will be a powerful tool that will make 3D data collection more accessible to the wider geomorphic community.
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Simpson, Christopher J. "Fluvial geomorphology of the sand bed Milk River, northern Montana". Thesis, National Library of Canada = Bibliothèque nationale du Canada, 1999. http://www.collectionscanada.ca/obj/s4/f2/dsk1/tape9/PQDD_0020/MQ48043.pdf.

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Schaney, Mitzy L. "Geologic and geomorphic controls of alluvial island location in Cheat River, West Virginia". Morgantown, W. Va. : [West Virginia University Libraries], 2005. https://eidr.wvu.edu/etd/documentdata.eTD?documentid=4159.

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Thesis (M.S.)--West Virginia University, 2005.
Title from document title page. Document formatted into pages; contains v, 130, [12] p. : ill. (some col.), maps (some col.). Includes abstract. Includes bibliographical references.
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Pietsch, Timothy J. "Fluvial geomorphology and late quaternary geochronology of the Gwydir fan-plain". Access electronically, 2005. http://www.library.uow.edu.au/adt-NWU/public/adt-NWU20060720.153247/index.html.

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Obaid, Ahmed Kadhim. "Tectonic and fluvial geomorphology of the Zagros fold-and-thrust belt". Thesis, Durham University, 2018. http://etheses.dur.ac.uk/12894/.

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The Zagros-fold-and thrust belt has been selected to explore landscape responses to tectonic and climatic drivers using river profile steepness (ksn), relief from topography, and basin scale Hypsometric Index (HI) extracted from Shuttle Radar Topography Mission (SRTM) 30 m dataset. There are differences in the ksn and the HI value from one area to another across the Zagros range. The northeastward presence of high HI values with respect to the seismicity cut-off in the combined Dezful/Bakhtyari region is attributed to wetter conditions, in turn driven by high strain and high topographic gradients in the Bakhtyari region. Drier climate and low power rivers in the Fars region promote plateau growth, and high HI values occur south of the thrust seismicity cut-off. In spite of the regional differences in ksn and HI, there is a similarity in the integrated relief along swath profiles, consistent with the similar rate of strain and total strain across different parts of the Zagros. Digital Elevation Model (DEM)-based geomorphic indices; Hypsometric Index (HI), Surface Roughness (SR) and their combination Surface Index (SI) have been applied to quantify landscape maturity in the Kirkuk Embayment of the Zagros. Landscape maturity suggests out of sequence deformation towards the hinterland in opposite sense to classical ‘piggyback’ thrusting model. The SI shows new previously undiscovered anticlines of hydrocarbon potential. New balanced cross-section indicates shortening in the order of ~5% in the Zagros foreland. Basin-scale values of HI exhibit sharp boundary of the low/high HI transition in the south of the Himalaya consistent with the zone of the Main Himalayan Thrust (MHT), and indicate the controls of the MHT on Himalayan topography. Smaller magnitude increases in HI value across the physiographic transition (PT2) do not support the out-of-sequence model of active deformation of Himalayan tectonics. Point-counting technique was conducted for modern river sand from the Zagros suture and the Neogene sandstones of the Zagros foreland. Results show recycled orogen provenance and litharenite composition and spatial increase in quartz content towards the northwest, which might refer to provenance change and/or drainage reorganization. The more lithic composition of river sand and the Neogene sandstone refers to an uplift of the Zagros suture area, which is partly caused by the out-of sequence deformation of the Mountain Front Fault.
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Książki na temat "Fluvial geomorphology"

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Paul, Mosley M., i Weaver William E, red. Experimental fluvial geomorphology. New York: Wiley, 1987.

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1924-, Wolman M. Gordon, i Miller John P. 1923-1961, red. Fluvial processes in geomorphology. New York: Dover Publications, 1995.

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Mathias, Kondolf G., i Piégay H, red. Tools in fluvial geomorphology. Chichester, England: Wiley, 2003.

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F, Warner Robin, red. Fluvial geomorphology of Australia. Sydney: Academic Press, 1988.

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Charlton, Ro. Fundamentals of fluvial geomorphology. Abingdon, Oxon: Routledge, 2007.

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Bennett, Sean J., i Andrew Simon, red. Riparian Vegetation and Fluvial Geomorphology. Washington, D. C.: American Geophysical Union, 2004. http://dx.doi.org/10.1029/ws008.

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Gregory, Ken J., red. Fluvial Geomorphology of Great Britain. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5816-9.

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Oklahoma Conservation Commission. Water Quality Division., red. Fluvial geomorphology projects of Oklahoma. [Oklahoma City, Okla.]: Oklahoma Conservation Commission, Water Quality Division, 2003.

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1962-, Bennett Sean J., i Simon Andrew, red. Riparian vegetation and fluvial geomorphology. Washington, D.C: American Geophysical Union, 2004.

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Plenum Geomorfologicheskoĭ komissii RAN (29th 2006 Izhevsk, Russia). Problemmy fli︠u︡vialʹnoĭ geomofologii: Materialy XXIX Plenuma Geomofologicheskoi komissii RAN : Izhevsk, 25-30 senti︠a︡bri︠a︡ 2006 g. Izhevsk: Assot︠s︡iat︠s︡ii︠a︡ "Nauchnai︠a︡ kniga", 2006.

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Części książek na temat "Fluvial geomorphology"

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Bora, A. K. "Fluvial Geomorphology". W The Brahmaputra Basin Water Resources, 88–112. Dordrecht: Springer Netherlands, 2004. http://dx.doi.org/10.1007/978-94-017-0540-0_6.

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Allan, J. David, Maria M. Castillo i Krista A. Capps. "Fluvial Geomorphology". W Stream Ecology, 45–73. Cham: Springer International Publishing, 2021. http://dx.doi.org/10.1007/978-3-030-61286-3_3.

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Huggett, Richard, i Emma Shuttleworth. "Fluvial Landscapes". W Fundamentals of Geomorphology, 245–307. Wyd. 5. London: Routledge, 2022. http://dx.doi.org/10.4324/9781003251156-14.

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Gilvear, D., i J. P. Bravard. "Geomorphology of temperate rivers". W The Fluvial Hydrosystems, 68–97. Dordrecht: Springer Netherlands, 1996. http://dx.doi.org/10.1007/978-94-009-1491-9_4.

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Darby, Stephen E., i Marco J. Van de Wiel. "Models in Fluvial Geomorphology". W Tools in Fluvial Geomorphology, 501–37. Chichester, UK: John Wiley & Sons, Ltd, 2005. http://dx.doi.org/10.1002/0470868333.ch17.

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Clément, Pierre, i Hervé Piégay. "Statistics and Fluvial Geomorphology". W Tools in Fluvial Geomorphology, 597–630. Chichester, UK: John Wiley & Sons, Ltd, 2005. http://dx.doi.org/10.1002/0470868333.ch20.

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Biedenharn, D. S., C. C. Watson i C. R. Thorne. "Fundamentals of Fluvial Geomorphology". W Sedimentation Engineering, 355–86. Reston, VA: American Society of Civil Engineers, 2008. http://dx.doi.org/10.1061/9780784408148.ch06.

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Werritty, A., L. J. McEwen, A. M. Harvey i J. E. Gordon. "Fluvial geomorphology of Scotland". W Fluvial Geomorphology of Great Britain, 19–114. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5816-9_2.

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Lewin, J., G. Higgs, R. D. Hey, A. M. Gurnell i J. A. A. Jones. "Fluvial geomorphology of Wales". W Fluvial Geomorphology of Great Britain, 115–71. Dordrecht: Springer Netherlands, 1997. http://dx.doi.org/10.1007/978-94-011-5816-9_3.

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Dey, Sourav, i Sujit Mandal. "Introduction to fluvial geomorphology". W Riverbank Erosion Hazards and Channel Morphodynamics, 1–31. London: Routledge India, 2022. http://dx.doi.org/10.4324/9781003276685-1.

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Streszczenia konferencji na temat "Fluvial geomorphology"

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Klotz, Jonathan R. "What Is Fluvial Geomorphology?" W World Water and Environmental Resources Congress 2003. Reston, VA: American Society of Civil Engineers, 2003. http://dx.doi.org/10.1061/40685(2003)381.

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Mirijovsky, Jakub. "UAV�PHOTOGRAMMETRY�IN�FLUVIAL�GEOMORPHOLOGY". W SGEM2012 12th International Multidisciplinary Scientific GeoConference and EXPO. Stef92 Technology, 2012. http://dx.doi.org/10.5593/sgem2012/s08.v2009.

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Milhous, Robert. "FLUVIAL GEOMORPHOLOGY AND INSTREAM FLOW WATER RIGHTS". W GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-379895.

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Wilkinson, Justin. "New mesoscale fluvial landscapes–Seismic geomorphology and exploration". W SEG Technical Program Expanded Abstracts 2013. Society of Exploration Geophysicists, 2013. http://dx.doi.org/10.1190/segam2013-1465.1.

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Welcome, Leiaka. "LINKAGES IN SEDIMENTOLOGY, FLUVIAL GEOMORPHOLOGY AND COMMUNITY RESEARCH". W GSA Connects 2022 meeting in Denver, Colorado. Geological Society of America, 2022. http://dx.doi.org/10.1130/abs/2022am-383516.

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Niyomborwornwat*, Nantaporn, i Philip Rowell. "Seismic Geomorphology of Fluvial Systems, Pattani Basin, Gulf of Thailand". W International Conference and Exhibition, Melbourne, Australia 13-16 September 2015. Society of Exploration Geophysicists and American Association of Petroleum Geologists, 2015. http://dx.doi.org/10.1190/ice2015-2209437.

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McPhillips, Munsell, Ben Higgins, Robert Prager, Andrea Stone i Brian Kwiatkowski. "The Practical Application of Fluvial Geomorphology in Watershed Master Planning". W World Water and Environmental Resources Congress 2004. Reston, VA: American Society of Civil Engineers, 2004. http://dx.doi.org/10.1061/40737(2004)439.

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Niculiţă, Mihai, Mihai Ciprian Mărgărint i Ionuţ Cristea. "Relict landslides, fluvial landforms and threatened geoheritage - Costești village". W Proceedings of the Romanian Geomorphology Symposium, 33rd edition, Iași, 11-14 May 2017. Iași: Alexandru Ioan Cuza University of Iași Press, 2017. http://dx.doi.org/10.15551/prgs.2017.126.

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Hosu, Maria, Delia Gheorghiu i Sheng Xu. "Burial dating of fluvial terraces using cosmogenic nuclides, ArieÛ River". W Proceedings of the Romanian Geomorphology Symposium, 33rd edition, Iași, 11-14 May 2017. Iași: Alexandru Ioan Cuza University of Iași Press, 2017. http://dx.doi.org/10.15551/prgs.2017.60.

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Rădoane, Maria, Ioana Perșoiu, Francisca Chiriloaei, Constantin Nechita, Delia Robu i Nicolae Rădoane. "History of Holocene fluvial activity in Romania: evidences based on absolute dating". W Proceedings of the Romanian Geomorphology Symposium, 33rd edition, Iași, 11-14 May 2017. Iași: Alexandru Ioan Cuza University of Iași Press, 2017. http://dx.doi.org/10.15551/prgs.2017.92.

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Raporty organizacyjne na temat "Fluvial geomorphology"

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Budzich, Jeffrey. PR-685-184506-R05 Fluvial Geomorphology Equations and Mechanics. Chantilly, Virginia: Pipeline Research Council International, Inc. (PRCI), kwiecień 2020. http://dx.doi.org/10.55274/r0011666.

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Channel hydrology, hydraulics, and sediment composition are key variables to calculating vertical and horizontal channel movement. A variety of methods are available for estimating channel bed scour, bank erosion, and channel migration with fewer available to predict avulsion potential. These methods vary in complexity from simplified empirical and theoretical equations to complex multi-dimensional models that may be used to understand potential hydrotechnical threats to pipelines and other structures. Furthermore, there are a variety of publicly available resources of relevant information to enhance pipeline operators' development and implementation of an effective water crossing program. The public resources include the United States Geological Survey, the National Weather Service within the National Oceanic and Atmospheric Administration, Federal Emergency Management Administration, United States Department of Agriculture, Natural Resource Conservation Service, and the Government of Canada.
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