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Relevant bibliographies by topics / Geomorphic processes

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Academic literature on the topic 'Geomorphic processes'

Author: Grafiati

Published: 4 June 2021

Last updated: 20 February 2023

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Journal articles on the topic "Geomorphic processes"

1

Turcotte, Donald L. "Modeling geomorphic processes." Physica D: Nonlinear Phenomena 77, no. 1-3 (October 1994): 229–37. http://dx.doi.org/10.1016/0167-2789(94)90136-8.

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Burtin, A., N. Hovius, and J. M. Turowski. "Seismic monitoring of geomorphic processes." Earth Surface Dynamics Discussions 2, no. 2 (December 15, 2014): 1217–67. http://dx.doi.org/10.5194/esurfd-2-1217-2014.

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Abstract. In seismology, the signal is usually analysed for earthquake data, but these represent less than 1% of continuous recording. The remaining data are considered as seismic noise and were for a long time ignored. Over the past decades, the analysis of seismic noise has constantly increased in popularity, and this has led to develop new approaches and applications in geophysics. The study of continuous seismic records is now open to other disciplines, like geomorphology. The motion of mass at the Earth's surface generates seismic waves that are recorded by nearby seismometers and can be used to monitor its transfer through the landscape. Surface processes vary in nature, mechanism, magnitude and space and time, and this variability can be observed in the seismic signals. This contribution aims to give an overview of the development and current opportunities for the seismic monitoring of geomorphic processes. We first describe the common principles of seismic signal monitoring and introduce time-frequency analysis for the purpose of identification and differentiation of surface processes. Second, we present techniques to detect, locate and quantify geomorphic events. Third, we review the diverse layout of seismic arrays and highlight their advantages and limitations for specific processes, like slope or channel activity. Finally, we illustrate all these characteristics with the analysis of seismic data acquired in a small debris-flow catchment where geomorphic events show interactions and feedbacks. Further developments must aim to fully understand the richness of the continuous seismic signals, to better quantify the geomorphic activity and improve the performance of warning systems. Seismic monitoring may ultimately allow the continuous survey of erosion and transfer of sediments in the landscape on the scales of external forcing.

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Timofeyev, D. A. "PRINCIPLES OF GEOMORPHIC PROCESSES CLASSIFICATION." Geomorphology RAS, no. 4 (August 25, 2015): 16. http://dx.doi.org/10.15356/0435-4281-2004-4-16-20.

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Malinowski, J. "Aridic soils and geomorphic processes." Geoderma 37, no. 3 (July 1986): 258–60. http://dx.doi.org/10.1016/0016-7061(86)90055-8.

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Warburton, Jeff. "Energenetics of Alpine Proglacial Geomorphic Processes." Transactions of the Institute of British Geographers 18, no. 2 (1993): 197. http://dx.doi.org/10.2307/622362.

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Wendland, Wayne M. "Climate changes: impacts on geomorphic processes." Engineering Geology 45, no. 1-4 (December 1996): 347–58. http://dx.doi.org/10.1016/s0013-7952(96)00021-x.

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Yang, Xiaoping, and Andrew Goudie. "Geomorphic processes and palaeoclimatology in deserts." Quaternary International 175, no. 1 (December 2007): 1–2. http://dx.doi.org/10.1016/j.quaint.2007.06.021.

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Malanson, George P., David R. Butler, and Konstantine P. Georgakakos. "Nonequilibrium geomorphic processes and deterministic chaos." Geomorphology 5, no. 3-5 (August 1992): 311–22. http://dx.doi.org/10.1016/0169-555x(92)90011-c.

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Hupp, Cliff R., and W. R. Osterkamp. "Riparian vegetation and fluvial geomorphic processes." Geomorphology 14, no. 4 (January 1996): 277–95. http://dx.doi.org/10.1016/0169-555x(95)00042-4.

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Olav, SLAYMAKER. "The implications of disconnectivity for the study of contemporary geomorphic processes." Revista de Geomorfologie 19, no. 1 (December 29, 2017): 5–15. http://dx.doi.org/10.21094/rg.2017.008.

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The emphasis on the understanding of contemporary geomorphic processes that has dominated Anglophone geomorphological literature over the past 50 years has seen huge progress but also some set-backs. We now have reliable measurements of mean rates of operation of all subaerial processes responsible for modification of landforms and landscapes and have made good progress in estimating the role of human activities as compared with “natural” processes. Some limited progress has been achieved in understanding the scale problem but problems remain. Perhaps the single most surprising development has been the recognition of the ubiquity of disconnectivity in geomorphic systems, the need to calculate virtual velocities of whole geomorphic systems and the relevance of this understanding to the general spatio-temporal scale problem. We have always known that most geomorphic processes operate intermittently but we have continued to depend on models that imply that mass and energy move freely through geomorphic systems and that conservation of mass and energy occurrs uninterruptedly at all temporal and spatial scales.

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Dissertations / Theses on the topic "Geomorphic processes"

1

Abu-Maila, Y. S. "Geomorphic and hydrologic processes in Coombs Brook, Macclesfield Forest." Thesis, University of Manchester, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.378012.

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Williams, Bethany Lynn. "The Role of Ecological Interactions in Saltmarsh Geomorphic Processes." W&M ScholarWorks, 2018. https://scholarworks.wm.edu/etd/1530192504.

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Accelerated sea-level rise poses a significant threat to coastal habitats. Salt marshes are critical coastal ecosystems, providing a host of services such as storm protection, food production, and carbon storage. Persistence of salt marshes in the face of rising sea levels relies, in part, on vertical accretion. Current ecogeomorphic models and empirical studies emphasize the importance of the positive relationship between plant production and vertical accretion via sediment trapping by stems aboveground and belowground organic matter production. Thus, changes in plant production influence salt marsh persistence with sea-level rise. However, studies and models of marsh accretion do not consider the effects of animal-mediated changes in plant production. Here, I tested how two co-occurring marsh crustaceans, Uca pugnax (marsh fiddler crab) and Sesarma reticulatum (purple marsh crab), which have contrasting effects on smooth cordgrass (Spartina alterniflora) production, indirectly influence sediment deposition and belowground organic matter contribution, through observational surveys and field manipulation. S. reticulatum feeds directly on S. alterniflora, while U. pugnax facilitates S. alterniflora production through burrowing and biodeposits. I found that U. pugnax facilitated S. alterniflora biomass in some marshes, but not others. However, this facilitation of S. alterniflora biomass did not enhance sediment deposition. U. pugnax had no effect on belowground components of vertical accretion (i.e. root production and decomposition). These results suggest that in isolation, U. pugnax has little impact on saltmarsh geomorphic processes. S. reticulatum reduced S. alterniflora above- and belowground biomass; however, sediment deposition increased as S. alterniflora biomass decreased, contrary to models of ecogeomorphology. This trend was likely due to sediment being resuspended by crab bioturbation, as U. pugnax abundances were higher in S. reticulatum-grazed areas than in non-grazed areas. When U. pugnax occurred in areas of low S. reticulatum grazing, S. alterniflora biomass and sedimentation was similar to areas with only U. pugnax. I suggest that the negative impacts of S. reticulatum are exaggerated when intense grazing results in completely unvegetated areas and subsequent increases in U. pugnax density, where bioturbation erodes sediments. Thus, while S. reticulatum can increase the susceptibility of marsh sediments to physical erosion by removing vegetation, it may also do so by facilitating U. pugnax bioturbation. However, when S. reticulatum grazing intensity is low, facilitation of S. alterniflora growth by U. pugnax can mitigate the negative effect of grazing, which suggests that the net effect of these species may depend on their relative abundance. This study demonstrates that ecological interactions, in addition to physical processes, have significant effects on marsh persistence as sea level rises, and merit incorporation into ecogeomorphic models and empirical studies of marsh accretion.

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Anorov, Julie Margaret, and n/a. "Integrated Study of Coastal Wetland Characteristics and Geomorphic Processes in a South East Queensland Catchment." Griffith University. Australian School of Environmental Studies, 2004. http://www4.gu.edu.au:8080/adt-root/public/adt-QGU20060223.153104.

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Coastal wetlands are dynamic ecosystems that are highly susceptible to change due to natural and human factors. The study area, located within the Native Dog Creek sub-catchment of the Logan River - which drains into Moreton Bay, south east Queensland - holds a detailed history of environmental change spanning most of the Holocene epoch. This history is preserved in the estuarine sedimentary record and is a valuable indicator of natural environmental change. More recently, human-induced changes within the study area have been superimposed on the natural process of environmental change. In order to develop a conceptual bio-geomorphic model of the coastal wetlands of Native Dog Creek, this thesis examined - on an integrated catchment basis - the evolution and connectivity of four coastal wetland community types (Melaleuca, Casuarina, saltmarsh and mangroves). The research consisted of four discrete studies within the study area: a geomorphic investigation that provided a framework for understanding how the wetlands evolved during the Holocene epoch; an acid sulfate soil (ASS) study that surveyed the distribution and concentration of sulfides; a palynological study that examined the natural directions of ecosystem change; and an investigation of the impact of specific human activities on these ecosystems. Detailed stratigraphic modelling found that the Logan River system (and its Native Dog Creek sub-catchment) has evolved from an infilling estuary since the peak of the Holocene transgression 6500 years before present. Recognition of the major controls that influenced geomorphic coastal development during the Holocene, provided important insights into the distribution and genesis of estuarine pyritic sediments which strongly influence the soils within the study area. In general, the estuarine central basin and fluvial delta sediments posed the greatest risk to the environment from acidification if disturbed. The major focus of the ASS study was to survey the distribution of ASS and to identify other areas most vulnerable to acidification. A predictive approach that combined chemical and stratigraphic analysis was used. Results showed that these areas are intrinsically related to their environment of deposition. The study found, for example, that the alternation of excessively wet and dry conditions - combined with high organic carbon levels and variations in microtopography - provided ideal conditions for the re-formation of pyrite in the stream channel within the Melaleuca wetlands. The palaeo-environmental study reconstructed the evolution of Holocene coastal wetland vegetation during the marine transgression and subsequent shoreline progradation. Pollen records from the four representative wetland communities (previously mentioned) were examined. The results found the mid-late Holocene vegetation history was controlled by the development of geomorphic features that have affected freshwater input, drainage and salinity. In response to the progradation of the shoreline after sea level stabilised, changes in fossil pollen from mangroves and saltmarsh taxa during the early-mid Holocene, to freshwater taxa during the late Holocene, are estimated to have taken 800 years. Thus, pollen analysis when used in combination with stratigraphic modelling, provided an important point of reference for rates of natural ecological change in response to evolutionary changes to the physical environment. The wetlands within the study area have suffered varying degrees of disturbance since European settlement in the 1820s. The most significant changes occurred during early European settlement, when vast areas of coastal lowlands were cleared for timber, sheep and cattle grazing and for agricultural purposes. A second period of change occurred from 1989 to 1995, when the Melaleuca community suffered dieback in response to hydrological modifications to Native Dog Creek for the development of a golf course. Results indicate that human-induced changes over the past 170 years have occurred at a rate far beyond the ability of the natural ecosystem to adapt or move to a more ecologically sustainable state, at least in the short-term. Hence the current environment is experiencing degradation through both decline in health and loss of indigenous species. The development of a conceptual bio-geomorphic model was based on the integration of results from all four studies, in an effort to provide a holistic understanding of the coastal wetland environment and of the impact of human-induced changes upon that environment. If these vulnerable ecosystems are to be maintained, successful and sustainable coastal management strategies must rely on a sound scientific understanding of the response of a coastal ecosystem to both human and environmental changes.

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Anorov, Julie Margaret. "Integrated Study of Coastal Wetland Characteristics and Geomorphic Processes in a South East Queensland Catchment." Thesis, Griffith University, 2004. http://hdl.handle.net/10072/365955.

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change due to natural and human factors. The study area, located within the Native Dog Creek sub-catchment of the Logan River - which drains into Moreton Bay, south east Queensland - holds a detailed history of environmental change spanning most of the Holocene epoch. This history is preserved in the estuarine sedimentary record and is a valuable indicator of natural environmental change. More recently, human-induced changes within the study area have been superimposed on the natural process of environmental change. In order to develop a conceptual bio-geomorphic model of the coastal wetlands of Native Dog Creek, this thesis examined - on an integrated catchment basis - the evolution and connectivity of four coastal wetland community types (Melaleuca, Casuarina, saltmarsh and mangroves). The research consisted of four discrete studies within the study area: a geomorphic investigation that provided a framework for understanding how the wetlands evolved during the Holocene epoch; an acid sulfate soil (ASS) study that surveyed the distribution and concentration of sulfides; a palynological study that examined the natural directions of ecosystem change; and an investigation of the impact of specific human activities on these ecosystems. Detailed stratigraphic modelling found that the Logan River system (and its Native Dog Creek sub-catchment) has evolved from an infilling estuary since the peak of the Holocene transgression 6500 years before present. Recognition of the major controls that influenced geomorphic coastal development during the Holocene, provided important insights into the distribution and genesis of estuarine pyritic sediments which strongly influence the soils within the study area. In general, the estuarine central basin and fluvial delta sediments posed the greatest risk to the environment from acidification if disturbed. The major focus of the ASS study was to survey the distribution of ASS and to identify other areas most vulnerable to acidification. A predictive approach that combined chemical and stratigraphic analysis was used. Results showed that these areas are intrinsically related to their environment of deposition. The study found, for example, that the alternation of excessively wet and dry conditions - combined with high organic carbon levels and variations in microtopography - provided ideal conditions for the re-formation of pyrite in the stream channel within the Melaleuca wetlands. The palaeo-environmental study reconstructed the evolution of Holocene coastal wetland vegetation during the marine transgression and subsequent shoreline progradation. Pollen records from the four representative wetland communities (previously mentioned) were examined. The results found the mid-late Holocene vegetation history was controlled by the development of geomorphic features that have affected freshwater input, drainage and salinity. In response to the progradation of the shoreline after sea level stabilised, changes in fossil pollen from mangroves and saltmarsh taxa during the early-mid Holocene, to freshwater taxa during the late Holocene, are estimated to have taken 800 years. Thus, pollen analysis when used in combination with stratigraphic modelling, provided an important point of reference for rates of natural ecological change in response to evolutionary changes to the physical environment. The wetlands within the study area have suffered varying degrees of disturbance since European settlement in the 1820s. The most significant changes occurred during early European settlement, when vast areas of coastal lowlands were cleared for timber, sheep and cattle grazing and for agricultural purposes. A second period of change occurred from 1989 to 1995, when the Melaleuca community suffered dieback in response to hydrological modifications to Native Dog Creek for the development of a golf course. Results indicate that human-induced changes over the past 170 years have occurred at a rate far beyond the ability of the natural ecosystem to adapt or move to a more ecologically sustainable state, at least in the short-term. Hence the current environment is experiencing degradation through both decline in health and loss of indigenous species. The development of a conceptual bio-geomorphic model was based on the integration of results from all four studies, in an effort to provide a holistic understanding of the coastal wetland environment and of the impact of human-induced changes upon that environment. If these vulnerable ecosystems are to be maintained, successful and sustainable coastal management strategies must rely on a sound scientific understanding of the response of a coastal ecosystem to both human and environmental changes.
Thesis (PhD Doctorate)
Doctor of Philosophy (PhD)
Australian School of Environmental Studies
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Michaelides, Katerina. "The effects of hillslope-channel coupling on catchment hydrological response in Mediterranean areas." Thesis, King's College London (University of London), 2000. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.326964.

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Lambert, Jeanne. "Coastal Processes and Anthropogenic Factors Influencing the Geomorphic Evolution of Weedon Island, Florida." Scholar Commons, 2006. http://scholarcommons.usf.edu/etd/3784.

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Weedon Island, a peninsula located on the western inner shoreline of Tampa Bay, Florida, is the location of a collaborative geological and archaeological project that aims to relate the present day geomorphology to natural processes and human occupational activity during the middle to late Holocene. The area is known for extensive archaeological sites, which were originally investigated in the 1920s, although they have received relatively little scientific attention during most of the last century. We hypothesize that activities associated with pre-historic human occupation of Weedon Island at various times during the last ca. 5,000 years influenced the geomorphic evolution of the peninsula. An interdisciplinary approach, including geomorphic mapping, sediment-coring, and archaeological survey and excavation, is being used to test our hypothesis and is expected to reveal the extent to which natural processes and human activities interacted to shape the present-day configuration of the peninsula. More recent human impacts on the peninsula have impeded our efforts in some areas. During the twentieth century, dredging, mosquito ditching, and road construction, have disturbed the surface and portions of the upper sediment record in many locations. Sediments below obvious disturbances or in unimpacted areas of the peninsula, along with radiocarbon dating, have helped reconstruct the mid to late Holocene paleoenvironments and paleolandscape of Weedon Island.

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Hester, Erich T. Doyle Martin W. "Impact of geomorphic structures on hyporheic exchange, temperature, and ecological processes in streams." Chapel Hill, N.C. : University of North Carolina at Chapel Hill, 2008. http://dc.lib.unc.edu/u?/etd,2641.

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Thesis (Ph. D.)--University of North Carolina at Chapel Hill, 2008.
Title from electronic title page (viewed Oct. 5, 2009). "... in partial fulfillment of the requirements for the degree of Doctor of Philosophy in the Curriculum in Ecology." Discipline: Ecology; Department/School: Ecology.

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Phillips, Sally Elizabeth. "The interaction of geological, geomorphic and pedogenic processes in the genesis of calcrete." Title page, table of contents and abstract only, 1988. http://hdl.handle.net/2440/19052.

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Spizale, Jordyn A. "Geomorphic Evolution of Caminada Pass in Southeast Louisiana." ScholarWorks@UNO, 2013. http://scholarworks.uno.edu/td/1705.

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Tidal inlets play a significant role in barrier island sustainability along the barrier islands of southern Louisiana. With increasing tidal prism, major changes are taking place within and adjacent to the inlets. The purpose of this thesis is to examine how Caminada Pass, a tidal inlet along the Caminada-Moreau headland, has evolved through time. Fundamental to this effort is evaluating which processes have contributed toward inlet evolution and what is the response of the inlet-bordering barrier island shorelines of Grand Isle and Elmer’s Island. This effort summarizes previous results and utilizes published bathymetric data, aerial photographs, vector shorelines, satellite images, and seafloor grab samples. The intent of this research is to document the variety of data that are available for future studies of Caminada Pass, an evaluation of long and short-term changes to the system, and an overall better understanding of the inlet dynamics of Caminada Pass.

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Londono, Ana Cristina. "Arid geomorphic processes revealed by erosion of pre-Columbian archaeological earthworks in Southern Peru." Cincinnati, Ohio : University of Cincinnati, 2008. http://rave.ohiolink.edu/etdc/view.cgi?acc_num=ucin1217365896.

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Thesis (Ph. D. )--University of Cincinnati, 2008.
Advisors: David Nash PhD (Committee Chair), Lewis Owen PhD (Committee Member), Mark Bowers PhD (Committee Member), Thomas Lowell PhD (Committee Member), David Keefer PhD (Committee Member) Title from electronic thesis title page (viewed Sept. 25, 2008). Includes abstract. Includes bibliographical references.

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Books on the topic "Geomorphic processes"

1

Dorava, Joseph M., David R. Montgomery, Betty B. Palcsak, and Faith A. Fitzpatrick, eds. Geomorphic Processes and Riverine Habitat. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004.

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Damm, Bodo, Heinrich Thiemeyer, and Birgit Terhorst. Hillslope processes in geomorphic systems on varying temporal and spatial scales. Stuttgart: Gebrüder Borntraeger, 2012.

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Simon, Andrew. Geomorphic and vegetative recovery processes along modified stream channels of west Tennessee. Nashville, Tenn: U.S. Geological Survey, 1992.

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Gustavson, Thomas C. Geomorphic processes and rates of retreat affecting the Caprock Escarpment, Texas Panhandle. Austin, Tex: Bureau of Economic Geology, University of Texas at Austin, 1989.

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Simon, Andrew. Geomorphic and vegetative recovery processes along modified stream channels of west Tennessee. Nashville, Tenn: U.S. Geological Survey, 1992.

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Simon, Andrew. Geomorphic and vegetative recovery processes along modified stream channels of west Tennessee. Nashville, Tenn: U.S. Geological Survey, 1992.

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Simon, Andrew. Geomorphic and vegetative recovery processes along modified stream channels of west Tennessee. Washington, D.C: U.S. G.P.O., 1994.

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Gustavson, Thomas C. Geomorphic processes and rates of retreat affecting the Caprock Escarpment, Texas Panhandle. Austin, TX: University of Texas at Austin, 1989.

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Molinelli, Joseph Antonio. Geomorphic processes along the Autopista Las Americas in North Central Puerto Rico: Implications for highway construction, design and maintenance. Ann Arbor, Mich: University Microfilms International, 1990.

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Branson, Farrel Allen. Contrasts of vegetation, soils, microclimates, and geomorphic processes between north- and south-facing slopes on Green Mountain near Denver, Colorado. Denver, Colo: Dept. of the Interior, U.S. Geological Survey, 1990.

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Book chapters on the topic "Geomorphic processes"

1

Lancaster, Stephen T., Shannon K. Hayes, and Gordon E. Grant. "Modeling sediment and wood storage and dynamics in small mountainous watersheds." In Geomorphic Processes and Riverine Habitat, 85–102. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0085.

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Frothingham, Kelly M., Bruce L. Rhoads, and Edwin E. Herricks. "Stream geomorphology and fish community structure in channelized and meandering reaches of an agricultural stream." In Geomorphic Processes and Riverine Habitat, 105–17. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0105.

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Larsen, Matthew C., and Abigail Santiago Román. "Mass wasting and sediment storage in a small montane watershed: An extreme case of anthropogenic disturbance in the humid tropics." In Geomorphic Processes and Riverine Habitat, 119–38. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0119.

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Pasternack, Gregory B. "Animal response to river evolution in the tidal freshwater zone." In Geomorphic Processes and Riverine Habitat, 139–57. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0139.

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McDowell, Patricia F. "Spatial variations in channel morphology at segment and reach scales, Middle Fork John Day River, northeastern Oregon." In Geomorphic Processes and Riverine Habitat, 159–72. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0159.

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Nakamura, Futoshi, and Nozomi Shin. "The downstream effects of dams on the regeneration of riparian tree species in northern Japan." In Geomorphic Processes and Riverine Habitat, 173–81. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0173.

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Pitlick, John, and Peter Wilcock. "Relations between streamflow, sediment transport, and aquatic habitat in regulated rivers." In Geomorphic Processes and Riverine Habitat, 185–98. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0185.

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Jacobson, Robert B., Mark S. Laustrup, and Michael D. Chapman. "Fluvial processes and passive rehabilitation of the Lisbon bottom side-channel chute, Lower Missouri River." In Geomorphic Processes and Riverine Habitat, 199–216. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0199.

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Dorava, Joseph M. "Mitigating Boatwake-induced erosion along the Kenai River, Alaska." In Geomorphic Processes and Riverine Habitat, 217–26. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0217.

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Collins, Brian D., and David R. Montgomery. "Importance of archival and process studies to characterizing pre-settlement riverine geomorphic processes and habitat in the Puget Lowland." In Geomorphic Processes and Riverine Habitat, 227–43. Washington, D. C.: American Geophysical Union, 2001. http://dx.doi.org/10.1029/ws004p0227.

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Conference papers on the topic "Geomorphic processes"

1

Greco, M., C. Di, S. Evangelista, A. Leopardi, M. Iervolino, and A. Vacca. "Experimental investigation of embankment erosion during fast geomorphic processes." In The International Conference On Fluvial Hydraulics (River Flow 2016). Taylor & Francis Group, 6000 Broken Sound Parkway NW, Suite 300, Boca Raton, FL 33487-2742: CRC Press, 2016. http://dx.doi.org/10.1201/9781315644479-77.

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Southworth, Scott. "GEOMORPHIC FEATURES AND PROCESSES ACROSS THE CENTRAL AND SOUTHERN APPALACHIANS." In 67th Annual Southeastern GSA Section Meeting - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018se-312673.

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Suursaar, Ü., and T. Kullas. "Decadal changes in wave climate and sea level regime: the main causes of the recent intensification of coastal geomorphic processes along the coasts of Western Estonia?" In COASTAL PROCESSES 2009. Southampton, UK: WIT Press, 2009. http://dx.doi.org/10.2495/cp090101.

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Phinney, April, Lyman P. Persico, Andrew Luhmann, Chantal Iosso, Alice Hinzmann, Trent Foky, and Eliza Van Wetter. "GEOMORPHIC CONTROLS ON HYDRAULIC PROCESSES OF BLACKTAIL DEER CREEK, YELLOWSTONE NATIONAL PARK." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-360039.

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Boyer, Elizabeth W., Heather E. Golden, James N. Galloway, Richard B. Alexander, Gregory E. Schwarz, Jesus D. Gomez-Velez, Judson W. Harvey, Durelle Scott, and Noah Schmadel. "COUPLED HYDROLOGICAL, BIOGEOCHEMICAL, AND GEOMORPHIC PROCESSES AFFECTING NUTRIENT LOADINGS IN FLUVIAL NETWORKS." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-307833.

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Jakob, Matthias, Michael Porter, K. Wayne Savigny, and Eugene Yaremko. "A Geomorphic Approach to the Design of Pipeline Crossings of Mountain Streams." In 2004 International Pipeline Conference. ASMEDC, 2004. http://dx.doi.org/10.1115/ipc2004-0239.

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Several hydrological methods are available to determine flood discharge and scour of streams at pipeline crossings. These methods are appropriate for streams dominated by purely hydrological processes, but fail where other, more hazardous processes occur within the design recurrence interval. Several investigations have shown that scour, impact and aggradation associated with debris flows, outburst floods or related phenomena may fundamentally change the parameters needed for proper pipeline crossing design. Depending on the process type, the peak discharge of the hazardous process can exceed that of the design flood (typically 50 to 200 year return period) by a factor of 2 to 50. Similarly, scour or aggradation by a non-fluvial process can exceed the hydrologically-derived estimates by several factors. It is therefore recommended that a geomorphic approach be taken in recognizing and quantifying the potential for non-fluvial processes and that the findings be integrated in the design of pipeline crossings.

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Yanites, Brian J., Nathaniel Mitchell, and Brigid M. Lynch. "GEOMORPHIC RECORDS OF LITHOSPHERIC PROCESSES: CASE STUDIES IN THE NORTH AND SOUTH AMERICAN CORDILLERA." In GSA Annual Meeting in Indianapolis, Indiana, USA - 2018. Geological Society of America, 2018. http://dx.doi.org/10.1130/abs/2018am-319200.

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Тониссон, Х., H. Tonisson, К. Орвикку, and K. Orvikku. "COASTAL GEOMORPHIC PROCESSES AND THEIR RELATION TO HYDRODYNAMIC CONDITIONS ON OSMUSSAAR ISLAND, THE BALTIC SEA." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce3c771d6a2.87718513.

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9

East, Amy, and Joel B. Sankey. "HOW ARE SEDIMENTARY AND GEOMORPHIC PROCESSES IN THE WESTERN U.S. RESPONDING TO MODERN CLIMATE CHANGE?" In GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-331403.

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Кравчуновская, Е., E. Kravchunovskaya, И. Тембрел, I. Tembrel, С. Горин, and S. Gorin. "EXTREME STORM EVENTS ON OKTYABR’SKAYA SPIT." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce3ad22e234.55317758.

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Extreme storm events occur on Oktyabr’skaya spit (Kamchatka) every year and destroy the only road connecting Oktyabr’skii village with the mainland. 30.11.2011 and 2.04.2012 we had a unique possibility to be on the spit at the time of such events. Significant geomorphic change occurred and the road was damaged. We documented the processes, as well as the effects.

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Reports on the topic "Geomorphic processes"

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Evans, S. G. Other Geomorphic Processes - Geomorphic Response To Endogenic Processes [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131648.

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Slaymaker, H. O. Physiography of Canada and Its Effects On Geomorphic Processes [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131640.

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Carson, M. A., and M. J. Bovis. Slope Processes [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131642.

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Day, T. J. River Processes [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131644.

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Ford, D. C. Solution Processes [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131652.

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David, P. P. Eolian Processes [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131654.

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French, H. M. Cold Climate Processes [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131646.

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G. Valentine, D.J. Krier, F.V. Perry, and G. Heiken. Eruptive and Geomorphic Processes at the Lathrop Wells Scoria Cone. US: Yucca Mountain Project, Las Vegas, Nevada, August 2006. http://dx.doi.org/10.2172/894816.

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Heginbottom, J. A. Summary [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131634.

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Heginbottom, J. A. Introduction [Chapter 9: a Survey of Geomorphic Processes in Canada]. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/131636.

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