Difference between revisions of "Transverse Aeolian ridges (TARs)"
(created article with images, info, and ref) |
m |
||
| Line 1: | Line 1: | ||
| − | Transverse Aeolian ridges (TARs) are light-toned features typically found in spots on Mars, especially on the floors of channels. Thus they sever as markers for where channels are located. They were first seen in narrow-angle images from the Mars Global Surveyor Mars Orbiter Camera (MOC | + | Transverse Aeolian ridges (TARs) are light-toned features typically found in spots on Mars, especially on the floors of channels. Thus they sever as markers for where channels are located. They were first seen in narrow-angle images from the Mars Global Surveyor Mars Orbiter Camera (MOC. Even though TARs are widespread on Mars, their formation, age, composition are not totally understood. |
| − | Even though TARs are widespread on Mars, their formation, age, composition are not totally understood. | ||
<ref>Berman, Daniel C.; Balme, Matthew R.; Rafkin, Scot C.R.; Zimbelman, James R. (2011). "Transverse Aeolian Ridges (TARs) on Mars II: Distributions, orientations, and ages". Icarus. 213 (1): 116–130. Bibcode:2011Icar..213..116B. doi:10.1016/j.icarus.2011.02.014. ISSN 0019-1035.</ref> | <ref>Berman, Daniel C.; Balme, Matthew R.; Rafkin, Scot C.R.; Zimbelman, James R. (2011). "Transverse Aeolian Ridges (TARs) on Mars II: Distributions, orientations, and ages". Icarus. 213 (1): 116–130. Bibcode:2011Icar..213..116B. doi:10.1016/j.icarus.2011.02.014. ISSN 0019-1035.</ref> | ||
<ref> Balme, Matt; Berman, Daniel C.; Bourke, Mary C.; Zimbelman, James R. (2008). "Transverse Aeolian Ridges (TARs) on Mars". Geomorphology. 101 (4): 703–720. Bibcode:2008Geomo.101..703B. doi:10.1016/j.geomorph.2008.03.011. ISSN 0169-555X. </ref> | <ref> Balme, Matt; Berman, Daniel C.; Bourke, Mary C.; Zimbelman, James R. (2008). "Transverse Aeolian Ridges (TARs) on Mars". Geomorphology. 101 (4): 703–720. Bibcode:2008Geomo.101..703B. doi:10.1016/j.geomorph.2008.03.011. ISSN 0169-555X. </ref> | ||
| Line 7: | Line 6: | ||
Geissler, Paul E.; Wilgus, Justin T. (2017). "The morphology of transverse aeolian ridges on Mars". Aeolian Research. 26: 63–71. Bibcode:2017AeoRe..26...63G. doi:10.1016/j.aeolia.2016.08.008. </ref> | Geissler, Paul E.; Wilgus, Justin T. (2017). "The morphology of transverse aeolian ridges on Mars". Aeolian Research. 26: 63–71. Bibcode:2017AeoRe..26...63G. doi:10.1016/j.aeolia.2016.08.008. </ref> | ||
<ref> Geissler, Paul E. (2014). "The birth and death of transverse aeolian ridges on Mars: Transverse Aeolian Ridges on Mars". Journal of Geophysical Research: Planets. 119 (12): 2583–2599. doi:10.1002/2014JE004633. </ref> | <ref> Geissler, Paul E. (2014). "The birth and death of transverse aeolian ridges on Mars: Transverse Aeolian Ridges on Mars". Journal of Geophysical Research: Planets. 119 (12): 2583–2599. doi:10.1002/2014JE004633. </ref> | ||
| − | <ref> Wilson, Sharon A. (2015), "Transverse Aeolian Ridge (TAR)", in Hargitai, Henrik; Kereszturi, Ákos (eds.), Encyclopedia of Planetary Landforms, New York, NY: Springer, pp. 2177–2185, doi:10.1007/978-1-4614-3134-3_380, ISBN 978-1-4614-3134-3, retrieved 2020-09-16 </ref> | + | <ref> Wilson, Sharon A. (2015), "Transverse Aeolian Ridge (TAR)", in Hargitai, Henrik; Kereszturi, Ákos (eds.), Encyclopedia of Planetary Landforms, New York, NY: Springer, pp. 2177–2185, doi:10.1007/978-1-4614-3134-3_380, ISBN 978-1-4614-3134-3, retrieved 2020-09-16 </ref> |
| + | |||
<gallery class="center" widths="380px" heights="360px"> | <gallery class="center" widths="380px" heights="360px"> | ||
| + | |||
File:Com59515 2160meander.jpg|Channels of a meander, most show TAR’s | File:Com59515 2160meander.jpg|Channels of a meander, most show TAR’s | ||
File:59515 2160tarswidearrows.jpg|TAR’s indicated with arrows | File:59515 2160tarswidearrows.jpg|TAR’s indicated with arrows | ||
File:59515 2160tarslabeled.jpg|Close view of TAR’s om a channel | File:59515 2160tarslabeled.jpg|Close view of TAR’s om a channel | ||
| + | |||
</gallery> | </gallery> | ||
== Aeolian bedforms == | == Aeolian bedforms == | ||
| + | |||
Features that used the wind for their formation, Aeolian bedforms, are usually classified as dunes or ripple marks, which are much smaller.<ref> https://www.sciencedirect.com/science/article/pii/S0019103521003079</ref> <ref>Day, M. and J. Zimbelan. 2021. Ripples, megaripples, and TARs, Oh, My! Recommendations regarding Mars aeolian bedform terminology. Icarus. Volume 369, 114647</ref> Dunes are taller than 0.5 m or taller on Earth and usually display an asymmetrical cross section. Wind ripples are much smaller—being only 0.6 - 15 mm high. They are more symmetrical in profile and are created by sand grains bouncing along: this process is called “saltation” by geologists. But, TARs are several orders of magnitude larger than wind ripples observed on Mars or Earth. | Features that used the wind for their formation, Aeolian bedforms, are usually classified as dunes or ripple marks, which are much smaller.<ref> https://www.sciencedirect.com/science/article/pii/S0019103521003079</ref> <ref>Day, M. and J. Zimbelan. 2021. Ripples, megaripples, and TARs, Oh, My! Recommendations regarding Mars aeolian bedform terminology. Icarus. Volume 369, 114647</ref> Dunes are taller than 0.5 m or taller on Earth and usually display an asymmetrical cross section. Wind ripples are much smaller—being only 0.6 - 15 mm high. They are more symmetrical in profile and are created by sand grains bouncing along: this process is called “saltation” by geologists. But, TARs are several orders of magnitude larger than wind ripples observed on Mars or Earth. | ||
<ref> Vriend, N. M.; Jarvis, P. A. (2018). "Between a ripple and a dune". Nature Physics. 14 (7): 641–642. Bibcode:2018NatPh..14..641V. doi:10.1038/s41567-018-0113-0. ISSN 1745-2473. S2CID 125921951.</ref> | <ref> Vriend, N. M.; Jarvis, P. A. (2018). "Between a ripple and a dune". Nature Physics. 14 (7): 641–642. Bibcode:2018NatPh..14..641V. doi:10.1038/s41567-018-0113-0. ISSN 1745-2473. S2CID 125921951.</ref> | ||
| Line 29: | Line 32: | ||
Furthermore, while TARs and dunes both seem to be composed of the dark volcanic mineral basalt. | Furthermore, while TARs and dunes both seem to be composed of the dark volcanic mineral basalt. | ||
| − | + | TARs are generally lighter in color and have lower thermal inertias than dunes. Hard, rocky materials have a higher thermal inertia. Scientists believe that the lower thermal inertia means that the surface of TARs is composed of smaller particles than dunes. | |
<ref> Fenton, Lori K.; Bandfield, Joshua L.; Ward, A. Wesley (2003). "Aeolian processes in Proctor Crater on Mars: Sedimentary history as analyzed from multiple data sets". Journal of Geophysical Research: Planets. 108 (E12): 5129. Bibcode:2003JGRE..108.5129F. doi:10.1029/2002je002015. ISSN 0148-0227. </ref> | <ref> Fenton, Lori K.; Bandfield, Joshua L.; Ward, A. Wesley (2003). "Aeolian processes in Proctor Crater on Mars: Sedimentary history as analyzed from multiple data sets". Journal of Geophysical Research: Planets. 108 (E12): 5129. Bibcode:2003JGRE..108.5129F. doi:10.1029/2002je002015. ISSN 0148-0227. </ref> | ||
<ref> Fenton, Lori K.; Mellon, Michael T. (2006). "Thermal properties of sand from Thermal Emission Spectrometer (TES) and Thermal Emission Imaging System (THEMIS): Spatial variations within the Proctor Crater dune field on Mars". Journal of Geophysical Research. 111 (E6): E06014. Bibcode:2006JGRE..111.6014F. doi:10.1029/2004je002363. ISSN 0148-0227. </ef> | <ref> Fenton, Lori K.; Mellon, Michael T. (2006). "Thermal properties of sand from Thermal Emission Spectrometer (TES) and Thermal Emission Imaging System (THEMIS): Spatial variations within the Proctor Crater dune field on Mars". Journal of Geophysical Research. 111 (E6): E06014. Bibcode:2006JGRE..111.6014F. doi:10.1029/2004je002363. ISSN 0148-0227. </ef> | ||
| Line 35: | Line 38: | ||
Although a 2020 study found evidence that some isolated TARs could still be moving a small amount, but most studies suggests they do not move .<ref> Silvestro, S.; Chojnacki, M.; Vaz, D. A.; Cardinale, M.; Yizhaq, H.; Esposito, F. (2020). "Megaripple Migration on Mars". Journal of Geophysical Research: Planets. 125 (8): e2020JE006446. Bibcode:2020JGRE..12506446S. doi:10.1029/2020JE006446. ISSN 2169-9097. PMC 7583471. PMID 33133993.</ref> | Although a 2020 study found evidence that some isolated TARs could still be moving a small amount, but most studies suggests they do not move .<ref> Silvestro, S.; Chojnacki, M.; Vaz, D. A.; Cardinale, M.; Yizhaq, H.; Esposito, F. (2020). "Megaripple Migration on Mars". Journal of Geophysical Research: Planets. 125 (8): e2020JE006446. Bibcode:2020JGRE..12506446S. doi:10.1029/2020JE006446. ISSN 2169-9097. PMC 7583471. PMID 33133993.</ref> | ||
| + | |||
== Images of TARs== | == Images of TARs== | ||
| + | |||
<gallery class="center" widths="380px" heights="360px"> | <gallery class="center" widths="380px" heights="360px"> | ||
WikiESP 039563 1730yardangsclose.jpg| Arrows point to "transverse aeolian ridges" (TAR's). They lie between ridges called yardangs. The location is Arsinoes Chaos. | WikiESP 039563 1730yardangsclose.jpg| Arrows point to "transverse aeolian ridges" (TAR's). They lie between ridges called yardangs. The location is Arsinoes Chaos. | ||
| Line 43: | Line 48: | ||
File:55149 1765tarscolorsurface.jpg|Close view of TAR's with waves, as seen by HiRISE under HiWish program | File:55149 1765tarscolorsurface.jpg|Close view of TAR's with waves, as seen by HiRISE under HiWish program | ||
File:55149 1765tarscolor2.jpg|Close, color view of TAR's in a channel,as seen by HiRISE under HiWish program Only part of the image is in color because HiRISE only takes a 1 km wide color strip. | File:55149 1765tarscolor2.jpg|Close, color view of TAR's in a channel,as seen by HiRISE under HiWish program Only part of the image is in color because HiRISE only takes a 1 km wide color strip. | ||
| + | |||
</gallery> | </gallery> | ||
| + | |||
==References== | ==References== | ||
{{reflist}} | {{reflist}} | ||
Revision as of 06:45, 21 September 2021
Transverse Aeolian ridges (TARs) are light-toned features typically found in spots on Mars, especially on the floors of channels. Thus they sever as markers for where channels are located. They were first seen in narrow-angle images from the Mars Global Surveyor Mars Orbiter Camera (MOC. Even though TARs are widespread on Mars, their formation, age, composition are not totally understood. [1]
[2] [3] [4] Geissler, Paul E.; Wilgus, Justin T. (2017). "The morphology of transverse aeolian ridges on Mars". Aeolian Research. 26: 63–71. Bibcode:2017AeoRe..26...63G. doi:10.1016/j.aeolia.2016.08.008. </ref> [5] [6]
Channels of a meander, most show TAR’s
TAR’s indicated with arrows
Close view of TAR’s om a channel
Aeolian bedforms
Features that used the wind for their formation, Aeolian bedforms, are usually classified as dunes or ripple marks, which are much smaller.[7] [8] Dunes are taller than 0.5 m or taller on Earth and usually display an asymmetrical cross section. Wind ripples are much smaller—being only 0.6 - 15 mm high. They are more symmetrical in profile and are created by sand grains bouncing along: this process is called “saltation” by geologists. But, TARs are several orders of magnitude larger than wind ripples observed on Mars or Earth.
[9]
[11] [12]
[13] On Mars, TARs represent some intermediate form with characteristics of both ripple marks and dunes. [14]
[15] [16] [17] [18]
Furthermore, while TARs and dunes both seem to be composed of the dark volcanic mineral basalt. TARs are generally lighter in color and have lower thermal inertias than dunes. Hard, rocky materials have a higher thermal inertia. Scientists believe that the lower thermal inertia means that the surface of TARs is composed of smaller particles than dunes. [19]
Cite error: Closing </ref> missing for <ref> tag
Although a 2020 study found evidence that some isolated TARs could still be moving a small amount, but most studies suggests they do not move .[20]
Images of TARs
Arrows point to "transverse aeolian ridges" (TAR's). They lie between ridges called yardangs. The location is Arsinoes Chaos.
Close, color view of unusual transverse aeolian ridges, TAR's, as seen by HiRISE under HiWish program These features may have had variable local winds to make the wavy tops.
Close view of TAR's with waves, as seen by HiRISE under HiWish program
Close, color view of TAR's in a channel,as seen by HiRISE under HiWish program Only part of the image is in color because HiRISE only takes a 1 km wide color strip.
References
- ↑ Berman, Daniel C.; Balme, Matthew R.; Rafkin, Scot C.R.; Zimbelman, James R. (2011). "Transverse Aeolian Ridges (TARs) on Mars II: Distributions, orientations, and ages". Icarus. 213 (1): 116–130. Bibcode:2011Icar..213..116B. doi:10.1016/j.icarus.2011.02.014. ISSN 0019-1035.
- ↑ Balme, Matt; Berman, Daniel C.; Bourke, Mary C.; Zimbelman, James R. (2008). "Transverse Aeolian Ridges (TARs) on Mars". Geomorphology. 101 (4): 703–720. Bibcode:2008Geomo.101..703B. doi:10.1016/j.geomorph.2008.03.011. ISSN 0169-555X.
- ↑ Wilson, Sharon A. (2004). "Latitude-dependent nature and physical characteristics of transverse aeolian ridges on Mars". Journal of Geophysical Research. 109 (E10): E10003. Bibcode:2004JGRE..10910003W. doi:10.1029/2004JE002247. ISSN 0148-0227.
- ↑ Bridges, N. T.; Bourke, M. C.; Geissler, P. E.; Banks, M. E.; Colon, C.; Diniega, S.; Golombek, M. P.; Hansen, C. J.; Mattson, S.; McEwen, A. S.; Mellon, M. T. (2012). "Planet-wide sand motion on Mars". Geology. 40 (1): 31–34. Bibcode:2012Geo....40...31B. doi:10.1130/G32373.1. ISSN 0091-7613.
- ↑ Geissler, Paul E. (2014). "The birth and death of transverse aeolian ridges on Mars: Transverse Aeolian Ridges on Mars". Journal of Geophysical Research: Planets. 119 (12): 2583–2599. doi:10.1002/2014JE004633.
- ↑ Wilson, Sharon A. (2015), "Transverse Aeolian Ridge (TAR)", in Hargitai, Henrik; Kereszturi, Ákos (eds.), Encyclopedia of Planetary Landforms, New York, NY: Springer, pp. 2177–2185, doi:10.1007/978-1-4614-3134-3_380, ISBN 978-1-4614-3134-3, retrieved 2020-09-16
- ↑ https://www.sciencedirect.com/science/article/pii/S0019103521003079
- ↑ Day, M. and J. Zimbelan. 2021. Ripples, megaripples, and TARs, Oh, My! Recommendations regarding Mars aeolian bedform terminology. Icarus. Volume 369, 114647
- ↑ Vriend, N. M.; Jarvis, P. A. (2018). "Between a ripple and a dune". Nature Physics. 14 (7): 641–642. Bibcode:2018NatPh..14..641V. doi:10.1038/s41567-018-0113-0. ISSN 1745-2473. S2CID 125921951.
- ↑ Anderson, R (1990). "Eolian ripples as examples of self-organization in geomorphological systems". Earth-Science Reviews. 29 (1–4): 77–96. doi:10.1016/0012-8252(0)90029-U.
- ↑ Boulton, J. Wayne (1997). Quantifying the morphology of aeolian impact ripples formed in a natural dune setting. National Library of Canada = Bibliothèque nationale du Canada. OCLC 654186636.
- ↑ Sharp, Robert P. (1963). "Wind Ripples". The Journal of Geology. 71 (5): 617–636. Bibcode:1963JG.....71..617S. doi:10.1086/626936. ISSN 0022-1376. S2CID 225043269.
- ↑ Wang, Peng; Zhang, Jie; Huang, Ning (2019). "A theoretical model for aeolian polydisperse-sand ripples". Geomorphology. 335: 28–36. Bibcode:2019Geomo.335...28W. doi:10.1016/j.geomorph.2019.03.013.
- ↑ Zimbelman, J. R.; Williams, S. H. (2007-07-01). "An Evaluation of Formation Processes for Transverse Aeolian Ridges on Mars". Seventh International Conference on Mars. 1353: 3047. Bibcode:2007LPICo1353.3047Z.
- ↑ Shockey, K. M.; Zimbelman, J. R. (2012-09-20). "Analysis of transverse aeolian ridge profiles derived from HiRISE images of Mars". Earth Surface Processes and Landforms. 38 (2): 179–182. doi:10.1002/esp.3316. ISSN 0197-9337.
- ↑ Bourke, M.C.; Balme, M.; Beyer, R.A.; Williams, K.K.; Zimbelman, J. (2006). "A comparison of methods used to estimate the height of sand dunes on Mars". Geomorphology. 81 (3–4): 440–452. Bibcode:2006Geomo..81..440B. doi:10.1016/j.geomorph.2006.04.023. ISSN 0169-555X.
- ↑ Claudin, Philippe; Andreotti, Bruno (2006). "A scaling law for aeolian dunes on Mars, Venus, Earth, and for subaqueous ripples". Earth and Planetary Science Letters. 252 (1–2): 30–44. arXiv:cond-mat/0603656. Bibcode:2006E&PSL.252...30C. doi:10.1016/j.epsl.2006.09.004. ISSN 0012-821X. S2CID 13910286.
- ↑ Williams, S. H.; Zimbelman, J. R.; Ward, A. W. (2002). "Large Ripples on Earth and Mars". Lunar and Planetary Science Conference. 33: 1508. Bibcode:2002LPI....33.1508W.
- ↑ Fenton, Lori K.; Bandfield, Joshua L.; Ward, A. Wesley (2003). "Aeolian processes in Proctor Crater on Mars: Sedimentary history as analyzed from multiple data sets". Journal of Geophysical Research: Planets. 108 (E12): 5129. Bibcode:2003JGRE..108.5129F. doi:10.1029/2002je002015. ISSN 0148-0227.
- ↑ Silvestro, S.; Chojnacki, M.; Vaz, D. A.; Cardinale, M.; Yizhaq, H.; Esposito, F. (2020). "Megaripple Migration on Mars". Journal of Geophysical Research: Planets. 125 (8): e2020JE006446. Bibcode:2020JGRE..12506446S. doi:10.1029/2020JE006446. ISSN 2169-9097. PMC 7583471. PMID 33133993.
