Palaeochannel: Difference between revisions
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[[File:Exhumed Paleochannel, Emery County, Utah2.jpg|thumb|Aerial view of exhumed fluvial palaeochannel, Emery County, Utah. The erosion of softer surrounding mudstone left this palaeochannel as a sandstone ridge.<ref name="HaydenOthers2019a">Hayden, A.T., Lamb, M.P., Fischer, W.W., Ewing, R.C., McElroy, B.J. and Williams, R.M., 2019. ''Formation of sinuous ridges by inversion of river-channel belts in Utah, USA, with implications for Mars''. ''Icarus'', 332, pp.92-110.</ref>]] |
[[File:Exhumed Paleochannel, Emery County, Utah2.jpg|thumb|Aerial view of exhumed fluvial palaeochannel, Emery County, Utah. The erosion of softer surrounding mudstone left this palaeochannel as a sandstone ridge.<ref name="HaydenOthers2019a">Hayden, A.T., Lamb, M.P., Fischer, W.W., Ewing, R.C., McElroy, B.J. and Williams, R.M., 2019. ''Formation of sinuous ridges by inversion of river-channel belts in Utah, USA, with implications for Mars''. ''Icarus'', 332, pp.92-110.</ref>]] |
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In the [[Earth]] sciences, a '''palaeochannel''', also spelled '''paleochannel''', is a significant length of a river or stream channel which no longer conveys [[fluvial]] discharge and part of an active fluvial system. The term ''palaeochannel'' is derived from the combination of two words, ''palaeo'' or ''old'', and ''[[Channel (geography)|channel]]''; i.e., a palaeochannel is an old channel. Palaeochannels may be preserved either as abandoned surface channels on river [[floodplain]]s and [[Terrace (geology)|terraces]] or infilled and buried by younger [[sediment]]s. The fill of a palaeochannel and its enclosing sedimentary deposits may consist of unconsolidated, semi-consolidated, or well-cemented [[sedimentary]] [[strata]] depending on the action of [[tectonic]]s and [[diagenesis]] during their geologic history after deposition. The abandonment of an active fluvial channel and the resulting formation of a palaeochannel can be the result of tectonic processes, geomorphologic processes, anthropogenic activities, climatic changes, or a variable and interelated combination of these factors.<ref name="Kumar2011a">Kumar, V., 2011. ''Palaeo-channel.'' In: Bishop, M.P., Björnsson, H., Haeberli, W., Oerlemans, J., Shroder, J.F. and Tranter, M., eds., p. 803, ''Encyclopedia of snow, ice and glaciers.'' Amsterdam, The Netherlands, Springer Science & Business Media. 1253 pp. ISBN |
In the [[Earth]] sciences, a '''palaeochannel''', also spelled '''paleochannel''', is a significant length of a river or stream channel which no longer conveys [[fluvial]] discharge and part of an active fluvial system. The term ''palaeochannel'' is derived from the combination of two words, ''palaeo'' or ''old'', and ''[[Channel (geography)|channel]]''; i.e., a palaeochannel is an old channel. Palaeochannels may be preserved either as abandoned surface channels on river [[floodplain]]s and [[Terrace (geology)|terraces]] or infilled and buried by younger [[sediment]]s. The fill of a palaeochannel and its enclosing sedimentary deposits may consist of unconsolidated, semi-consolidated, or well-cemented [[sedimentary]] [[strata]] depending on the action of [[tectonic]]s and [[diagenesis]] during their geologic history after deposition. The abandonment of an active fluvial channel and the resulting formation of a palaeochannel can be the result of tectonic processes, geomorphologic processes, anthropogenic activities, climatic changes, or a variable and interelated combination of these factors.<ref name="Kumar2011a">Kumar, V., 2011. ''Palaeo-channel.'' In: Bishop, M.P., Björnsson, H., Haeberli, W., Oerlemans, J., Shroder, J.F. and Tranter, M., eds., p. 803, ''Encyclopedia of snow, ice and glaciers.'' Amsterdam, The Netherlands, Springer Science & Business Media. 1253 pp. {{ISBN|978-90-481-2641-5}}</ref><ref name="Nash2000a">Nash, D.J., 2000. ''Palaeochannel.'' In Thomas, D.S.G., and Goudie, A., eds., p. 354. ''The Dictionary of Physical Geology'', 3rd ed. Oxford, United Kingdon, Blackwell Publising. 610 pp. {{ISBN|978-0-631-20472-5}}</ref> |
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== Formation == |
== Formation == |
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Revision as of 03:12, 31 December 2023
 | This article needs additional citations for verification. (January 2016) |
In the Earth sciences, a palaeochannel, also spelled paleochannel, is a significant length of a river or stream channel which no longer conveys fluvial discharge and part of an active fluvial system. The term palaeochannel is derived from the combination of two words, palaeo or old, and channel; i.e., a palaeochannel is an old channel. Palaeochannels may be preserved either as abandoned surface channels on river floodplains and terraces or infilled and buried by younger sediments. The fill of a palaeochannel and its enclosing sedimentary deposits may consist of unconsolidated, semi-consolidated, or well-cemented sedimentary strata depending on the action of tectonics and diagenesis during their geologic history after deposition. The abandonment of an active fluvial channel and the resulting formation of a palaeochannel can be the result of tectonic processes, geomorphologic processes, anthropogenic activities, climatic changes, or a variable and interelated combination of these factors.[2][3]
Formation
Palaeochannels form when river channels aggrade and so deposit sediment on their bed. For the channel deposits to be preserved, the flow must not occupy and erode them again. Examples of what may cause long-term preservation include the channels being in a net-depositional environment and/or being in a subsiding sedimentary basin. Palaeochannels may also be preserved in the short-term on non-net-depositional floodplains in which the river migrates or avulses away from its previous course. The preservation is short-term because unless the channel deposits are buried, flow will eventually reoccupy its formerly-occupied course, reworking and eroding the channel deposits.
Recognition
A palaeochannel is distinct from the overbank deposits of currently-active river channels, including ephemeral water courses that do not regularly flow (such as the Todd River, Central Australia) because the river bed is filled with sedimentary deposits unrelated to the normal bed load of the current drainage pattern.
Many palaeochannels are arranged on old drainage patterns, distinct from the current drainage system of a catchment. For example, palaeochannels may relate to a system of rivers and creeks that drained east–west while the current drainage direction is north–south.
Palaeochannels can be most easily identified as broad erosional channels into a basement that underlies a system of depositional sequences, which may contain several episodes of deposition and represent meandering peneplain streams.
Thereafter, a palaeochannel may form part of the regolith of a region and although it is unconsolidated or partly consolidated, it is currently part of the erosional surface.
Palaeochannels can also be identified according to their age. For example, there are deposits of Tertiary lignites in the Tertiary river systems preserved on top of Archaean basement in the Yilgarn Craton of Western Australia.[4] The river systems have laid in place for 15 to 50 million years and would be considered palaeochannels.
Palaeochannels can be identified using airborne electromagnetic surveys, as the coarse-grained sediments are more electrically resistive than surrounding materials.[5]
Geological importance
Palaeochannels are important to geology for a number of reasons:
- Understanding movements of faults, which may redirect river systems and so form stranded channels that are, in essence, palaeochannels.
- Preserving Tertiary, Eocene and Holocene sediments and fossils within them, important locations for palaeontology, palaeobotany and archaeology.
- Preserving evidence of older erosional surfaces and levels, which is useful for estimating the net erosional budget of older regolith.
- Preserving sedimentary records, which is useful for understanding climatic conditions, including various isotopic indicators of past rainfall, temperatures and climates, used to understand climate change and global warming.
Examples
There is a large palaeovalley underneath Anangu Pitjantjatjara Yankunytjatjara (APY lands) in the remote north-west of South Australia.[6]
Economic importance
Palaeochannels can host economic ore deposits of uranium,[7] lignite, precious metals such as gold and platinum, heavy minerals such as tin, tungsten, and iron ore preserved as palaeo-placer deposits.
Palaeochannels have been proposed as a mechanism for managed aquifer recharge in California.[5][8]
See also
References
- ^ Hayden, A.T., Lamb, M.P., Fischer, W.W., Ewing, R.C., McElroy, B.J. and Williams, R.M., 2019. Formation of sinuous ridges by inversion of river-channel belts in Utah, USA, with implications for Mars. Icarus, 332, pp.92-110.
- ^ Kumar, V., 2011. Palaeo-channel. In: Bishop, M.P., Björnsson, H., Haeberli, W., Oerlemans, J., Shroder, J.F. and Tranter, M., eds., p. 803, Encyclopedia of snow, ice and glaciers. Amsterdam, The Netherlands, Springer Science & Business Media. 1253 pp. ISBN 978-90-481-2641-5
- ^ Nash, D.J., 2000. Palaeochannel. In Thomas, D.S.G., and Goudie, A., eds., p. 354. The Dictionary of Physical Geology, 3rd ed. Oxford, United Kingdon, Blackwell Publising. 610 pp. ISBN 978-0-631-20472-5
- ^ Anand, R.; Paine, M. (2002). "Regolith Geology of the Yilgarn Craton, Western Australia". Australian Journal of Earth Sciences. 49 (1): 3–162. doi:10.1046/j.1440-0952.2002.00912.x. S2CID 129930657.
- ^ a b Knight, Rosemary; Steklova, Klara; Miltenberger, Alex; Kang, Seogi; Goebel, Meredith; Fogg, Graham (1 December 2022). "Airborne geophysical method images fast paths for managed recharge of California's groundwater". Environmental Research Letters. 17 (12): 124021. doi:10.1088/1748-9326/aca344. ISSN 1748-9326. S2CID 253605188.
- ^ Lysaght, Gary-Jon (28 January 2021). "Map of APY Lands translated to 'empower' First Nations people, giving them greater voice". ABC News. Australian Broadcasting Corporation. Retrieved 29 January 2021.
- ^ Douglas, G.B.; Butt, C.R.M.; Gray, D.J. (2003). "Mulga Rock Uranium and Multielement Deposits, Officer Basin, WA" (PDF). CRC LEME, CSIRO Exploration and Mining. Retrieved 7 March 2006.
- ^
- Gies, Erica (7 January 2023). "California Could Capture Its Destructive Floodwaters to Fight Drought". New York Times.
- Lansdale, Amy LeVan (2005). Influence of a coarse-grained incised-valley fill on groundwater flow in fluvial fan deposits, Stanislaus County, Modesto, California, USA (Masters). Michigan State University. doi:10.25335/M5G44J01D.
- He, Xiaogang; Bryant, Benjamin P.; Moran, Tara; Mach, Katharine J.; Wei, Zhongwang; Freyberg, David L. (2023). "Climate-informed hydrologic modeling and policy typology to guide managed aquifer recharge". Science Advances. 7 (17): eabe6025. doi:10.1126/sciadv.abe6025. PMC 8059926. PMID 33883132. S2CID 233349426.