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Journal articles on the topic 'Geomorphology and earth surface processes'

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Author: Grafiati

Published: 10 December 2022

Last updated: 28 January 2023

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1

Dadson, Simon. "Geomorphology and Earth system science." Progress in Physical Geography: Earth and Environment 34, no. 3 (June 2010): 385–98. http://dx.doi.org/10.1177/0309133310365031.

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Earth system science (ESS) is an approach to: ‘obtain a scientific understanding of the entire Earth system on a global scale by describing how its component parts and their interactions have evolved, how they function, and how they may be expected to continue to evolve on all timescales’ (Bretherton, 1998). The aim of this review is to introduce some key examples showing the role of Earth surface processes, the traditional subject of geomorphology, within the interacting Earth system. The paper considers three examples of environmental systems in which geomorphology plays a key role: (1) links between topography, tectonics, and atmospheric circulation; (2) links between geomorphic processes and biogeochemical cycles; and (3) links between biological processes and the Earth’s surface. Key research needs are discussed, including the requirement for better opportunities for interdisciplinary collaboration, clearer mathematical frameworks for Earth system models, and more sophisticated interaction between natural and social scientists.

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2

Bardají, Teresa, and Adrian Harvey. "Dryland geomorphology and interacting processes." Geomorphology 102, no. 2 (December 2008): 205–6. http://dx.doi.org/10.1016/j.geomorph.2008.05.001.

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3

Semmel, Arno. "Soil geomorphology." CATENA 20, no. 6 (December 1993): 597–98. http://dx.doi.org/10.1016/0341-8162(93)90022-h.

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4

Ruffell, Alastair, and Jennifer McKinley. "Forensic geomorphology." Geomorphology 206 (February 2014): 14–22. http://dx.doi.org/10.1016/j.geomorph.2013.12.020.

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5

Melhorn, Wilton N. "Appalachian geomorphology." Geomorphology 4, no. 5 (March 1992): 364–65. http://dx.doi.org/10.1016/0169-555x(92)90030-r.

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6

Sawyer, Carol F. "Mountain geomorphology." Geomorphology 83, no. 1-2 (January 2007): 195–96. http://dx.doi.org/10.1016/j.geomorph.2006.07.004.

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7

Harbor, Jonathan M. "Glacial geomorphology: modeling processes and landforms." Geomorphology 7, no. 1-3 (July 1993): 129–40. http://dx.doi.org/10.1016/0169-555x(93)90014-s.

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8

Clague, John J., and Olav Slaymaker. "Canadian geomorphology 2000." Geomorphology 32, no. 3-4 (March 2000): 203–11. http://dx.doi.org/10.1016/s0169-555x(99)00097-5.

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9

Keller, Edward, Chandler Adamaitis, Paul Alessio, Sarah Anderson, Erica Goto, Summer Gray, Larry Gurrola, and Kristin Morell. "Applications in geomorphology." Geomorphology 366 (October 2020): 106729. http://dx.doi.org/10.1016/j.geomorph.2019.04.001.

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10

Craig, Richard G. "Computing Applachian geomorphology." Geomorphology 2, no. 1-3 (September 1989): 197–207. http://dx.doi.org/10.1016/0169-555x(89)90012-3.

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11

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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12

Twidale, C. R. "Arid zone geomorphology." Geomorphology 4, no. 2 (June 1991): 155–56. http://dx.doi.org/10.1016/0169-555x(91)90026-7.

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13

Parker, Timothy J., and Donald R. Currey. "Extraterrestrial coastal geomorphology." Geomorphology 37, no. 3-4 (April 2001): 303–28. http://dx.doi.org/10.1016/s0169-555x(00)00089-1.

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14

Stephenson, W. J., and L. A. Naylor. "Rock coast geomorphology." Geomorphology 114, no. 1-2 (January 2010): 1–2. http://dx.doi.org/10.1016/j.geomorph.2009.02.013.

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15

Janke, Jason R., John R. Giardino, and John D. Vitek. "The Binghamton Geomorphology Symposium (BGS): 50 years of Enhancing Geomorphology." Geomorphology 366 (October 2020): 107191. http://dx.doi.org/10.1016/j.geomorph.2020.107191.

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16

Thouret, Jean-Claude. "Avijit Gupta, Tropical geomorphology." Géomorphologie : relief, processus, environnement 18, no. 4 (December 31, 2012): 477–78. http://dx.doi.org/10.4000/geomorphologie.10072.

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17

Jackson, Nancy L., Karl F. Nordstrom, Rusty A. Feagin, and William K. Smith. "Coastal geomorphology and restoration." Geomorphology 199 (October 2013): 1–7. http://dx.doi.org/10.1016/j.geomorph.2013.06.027.

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18

Migoń, Piotr. "Sandstone geomorphology – Recent advances." Geomorphology 373 (January 2021): 107484. http://dx.doi.org/10.1016/j.geomorph.2020.107484.

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19

Embleton, C. "Geomorphology in environmental planning." Geomorphology 4, no. 3-4 (October 1991): 301. http://dx.doi.org/10.1016/0169-555x(91)90012-y.

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20

Baker, V. R., and C. R. Twidale. "The reenchantment of geomorphology." Geomorphology 4, no. 2 (June 1991): 73–100. http://dx.doi.org/10.1016/0169-555x(91)90021-2.

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21

Rapp, Anders. "Advances in periglacial geomorphology." Geomorphology 4, no. 2 (June 1991): 157–59. http://dx.doi.org/10.1016/0169-555x(91)90028-9.

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22

Walker, H. J. "Geomorphology of rocky coasts." Geomorphology 11, no. 2 (December 1994): 174–75. http://dx.doi.org/10.1016/0169-555x(94)90084-1.

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23

Mercier, Denis. "Compte rendu d'ouvrage : Periglacial Geomorphology." Géomorphologie : relief, processus, environnement 24, no. 3 (December 15, 2018): 321–23. http://dx.doi.org/10.4000/geomorphologie.12409.

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24

Ollier, C. D., and C. F. Pain. "Neotectonic mountain uplift and geomorphology." Geomorphology RAS, no. 4 (November 8, 2019): 3–26. http://dx.doi.org/10.31857/s0435-4281201943-26.

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Mountains are topographic features caused by erosion after vertical uplift or mountain building. Mountain building is often confused with orogeny, which today means the formation of structures in fold belts. The common assumption that folding and mountain building go together is generally untrue. Many mountains occur in unfolded rocks, granites and volcanic rocks, so there is no direct association of folding and mountain building. In those places where mountains are underlain by folded rocks the folding pre-dates planation and uplift. The age of mountains is therefore not the age of the last folding (if any) but the age of vertical uplift. Since mountains are not restricted to folded rocks, lateral compression is not required to explain the uplift. A compilation of times of uplift of mountains around the world shows that a major phase of tectonic uplift started about 6 Ma, and much uplift occurred in the last 2 Ma. This period is known as the Neotectonic Period. It is a global phenomenon including mountains on passive continental margins, and those in deep continental interiors. Several hypotheses of mountain building have problems with this timing. Some fail by being only able to make mountains out of folded rock at continental margins. Many translate the vertical uplift into lateral compression, but vertical uplift alone can create mountains. The Neotectonic Period has important implications for geomorphology, climate and global tectonics. In geomorphology it does not fit into conventional theories of geomorphology such as Davisian or King cycles of erosion. Neotectonic uplift might initiate several cycles of erosion, but most planation surfaces are much older than the Neotectonic Period. The increasing relief associated with Neotectonic uplift affected rates of erosion and sedimentation, and also late Cenozoic climate. The Neotectonic Period does not fit within plate tectonics theory, in which mountains are explained as a result of compression at active margins: mountains in other locations are said to have been caused by the same process but further back in time. This is disproved by the young age of uplift of mountains in intercontinental and passive margin positions. Subduction is supposed to have been continuous for hundreds of millions of years, so fails to explain the world-wide uplifts in just a few million years. Geomorphologists should be guided by their own findings, and refrain from theory-driven hypotheses of plate collision or landscape evolution.

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25

McGlashan, Derek J. "Geomorphology and Environmental Impact Assessment." Geomorphology 54, no. 3-4 (September 2003): 350–51. http://dx.doi.org/10.1016/s0169-555x(02)00343-4.

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26

Burger, K. C., J. J. Degenhardt, and J. R. Giardino. "Engineering geomorphology of rock glaciers." Geomorphology 31, no. 1-4 (December 1999): 93–132. http://dx.doi.org/10.1016/s0169-555x(99)00074-4.

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27

Slaymaker, Olav, and Christine Embleton-Hamann. "Advances in global mountain geomorphology." Geomorphology 308 (May 2018): 230–64. http://dx.doi.org/10.1016/j.geomorph.2018.02.016.

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28

Rhoads, Bruce L. "Process models and theoretical geomorphology." Geomorphology 11, no. 3 (February 1995): 256–57. http://dx.doi.org/10.1016/0169-555x(95)90005-e.

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29

Bauer, B. O. "Contemporary research in aeolian geomorphology." Geomorphology 105, no. 1-2 (April 2009): 1–5. http://dx.doi.org/10.1016/j.geomorph.2008.02.014.

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30

Butler, David R., Stephen J. Walsh, and George P. Malanson. "Introduction to the special issue: mountain geomorphology—integrating earth systems." Geomorphology 55, no. 1-4 (September 2003): 1–4. http://dx.doi.org/10.1016/s0169-555x(03)00128-4.

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31

Trudgill, Stephen, Richard J. Chorley, Stanley A. Schumm, and David E. Sugden. "Geomorphology." Transactions of the Institute of British Geographers 11, no. 3 (1986): 373. http://dx.doi.org/10.2307/621798.

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32

Slaymaker, O., T. Spencer, and C. Embleton-Hamann. "Recasting geomorphology as a landscape science." Geomorphology 384 (July 2021): 107723. http://dx.doi.org/10.1016/j.geomorph.2021.107723.

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33

Mercier, Denis. "Paraglacial geomorphology: Conceptual and methodological revival." Géomorphologie : relief, processus, environnement 14, no. 4 (December 31, 2008): 219–22. http://dx.doi.org/10.4000/geomorphologie.7395.

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34

Gielstra, Dianna Alsup. "Principles of Glacial Geomorphology and Geology." Geomorphology 54, no. 3-4 (September 2003): 348–49. http://dx.doi.org/10.1016/s0169-555x(02)00342-2.

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35

Barsch, Dietrich. "Periglacial geomorphology in the 21st century." Geomorphology 7, no. 1-3 (July 1993): 141–63. http://dx.doi.org/10.1016/0169-555x(93)90015-t.

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36

Sherman, Douglas J., and Bernard O. Bauer. "Coastal geomorphology through the looking glass." Geomorphology 7, no. 1-3 (July 1993): 225–49. http://dx.doi.org/10.1016/0169-555x(93)90018-w.

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37

Dubois, J. M. M. "Functional geomorphology: Landform analysis and models." Geomorphology 9, no. 4 (June 1994): 344–45. http://dx.doi.org/10.1016/0169-555x(94)90055-8.

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38

Ahnert, Frank. "Equilibrium, scale and inheritance in geomorphology." Geomorphology 11, no. 2 (December 1994): 125–40. http://dx.doi.org/10.1016/0169-555x(94)90077-9.

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39

Shroder, John F., Michael P. Bishop, Jeffrey Olsenholler, and J. Philip Craiger. "Geomorphology and the World Wide Web." Geomorphology 47, no. 2-4 (October 2002): 343–63. http://dx.doi.org/10.1016/s0169-555x(02)00097-1.

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40

Doyle, Martin W., and Jason P. Julian. "The most-cited works in Geomorphology." Geomorphology 72, no. 1-4 (December 2005): 238–49. http://dx.doi.org/10.1016/j.geomorph.2005.04.016.

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41

González-Díez, Alberto, Lothar Schrott, and Denys Brunsden. "Theories and methods in geomorphology: Introduction." Geomorphology 110, no. 1-2 (September 2009): 1. http://dx.doi.org/10.1016/j.geomorph.2009.02.023.

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42

Glade, Thomas, and Michael J. Crozier. "Landslide geomorphology in a changing environment." Geomorphology 120, no. 1-2 (August 2010): 1–2. http://dx.doi.org/10.1016/j.geomorph.2009.09.018.

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43

Maestro, Adolfo, Jerónimo López-Martínez, Estefanía Llave, Fernando Bohoyo, Juan Acosta, F. Javier Hernández-Molina, Araceli Muñoz, and Gloria Jané. "Geomorphology of the Iberian Continental Margin." Geomorphology 196 (August 2013): 13–35. http://dx.doi.org/10.1016/j.geomorph.2012.08.022.

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44

Butler, David R. "The field tradition in mountain geomorphology." Geomorphology 200 (October 2013): 42–49. http://dx.doi.org/10.1016/j.geomorph.2013.03.021.

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45

SMART, P. L. "Karst Geomorphology." Geology Today 3, no. 2 (March 1987): 71–72. http://dx.doi.org/10.1111/j.1365-2451.1987.tb00847.x.

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46

Brocklehurst, Simon H. "Tectonics and geomorphology." Progress in Physical Geography: Earth and Environment 34, no. 3 (June 2010): 357–83. http://dx.doi.org/10.1177/0309133309360632.

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The field of tectonic geomorphology is in a state of tension. The widespread availability of high-quality, high-resolution digital topographic data encourages the development of simple morphological ‘tools’ which can be used to deduce recent tectonic evolution. Meanwhile, process geomorphologists recognize that current models have a significant empirical basis, and lack insight into the underlying physics of erosion processes. Most tectonic geomorphology research is concerned with rivers, but glaciers, debris flows and hillslope processes also play a key role in hypotheses linking climate to tectonics, via surface processes, while submarine geomorphology has barely been investigated in a tectonic context. Studies combining field data collection, exposure, burial and low-temperature thermochronologic dating, digital topographic analysis, laboratory experiments and numerical models are successfully incorporating physics into geomorphic process ‘laws’, and demonstrating key tectonic geomorphology hypotheses. The approaches required for further progress have been outlined, but many exciting challenges remain.

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47

Helene, Burningham. "Introduction to Coastal Processes & Geomorphology." Journal of Coastal Research 226 (November 2006): 1589–90. http://dx.doi.org/10.2112/1551-5036(2006)22[1589:br]2.0.co;2.

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48

Brierley, Gary, Kirstie Fryirs, Helen Reid, and Richard Williams. "The dark art of interpretation in geomorphology." Geomorphology 390 (October 2021): 107870. http://dx.doi.org/10.1016/j.geomorph.2021.107870.

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49

Hesp, Patrick. "Foredunes and blowouts: initiation, geomorphology and dynamics." Geomorphology 48, no. 1-3 (November 2002): 245–68. http://dx.doi.org/10.1016/s0169-555x(02)00184-8.

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50

McGlashan, Derek J. "Review on “Applied Geomorphology: theory and practice”." Geomorphology 57, no. 3-4 (February 2004): 441–43. http://dx.doi.org/10.1016/s0169-555x(03)00233-2.

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