Analysis of linear parameters of morphology of the dunes of the Herschel cratera on mars through HIRISE images
DOI:
https://doi.org/10.5007/2177-5230.2023.e81182Keywords:
Planetary Geomorphology, Mars, Dunes, CratersAbstract
The Aeolian processes are key elements to understand the surfaces of celestial bodies with atmosphere. This paper performs an analysis of aeolian activity on Herschel crater, from two dune fields in different topographical settings. At East field, between small simple craters, and at West, the dune field is located inside a large impact crater near to uplifted central peak. As source of data will be employed high resolution images (spatial resolution 0,25 m/pixel) and digital terrain models (DTM), with 1m / pixel spatial resolution, generated by HiRISE sensor of orbital probe Mars Reconnaissance Orbiter (MRO).Were measured horizontal parameters (Area,Azimuth length, width , and length/width ratio) and vertical parameters (height of crest (Hc), height of slipface (Hs),slipface slope, curvature) of 10 dunes in each field.
References
Baker, V.R & Twidale, C R. The Reenchantment of geomorphology. Geomorphology 4, 73-100,1991.
Bourke, M.C. & Goudie, A.S.Varieties of barchan form in the Namib Desert and on Mars. Aeolian Research 1 (2009) 45–54
Bigarella, J.J.The Lagoa dune field In: Mckee, E.D.A study of global sand seas.Geological Survey Professional Paper 1052. Washington D.C: United States Government Printing Office, 1979.p 114-134.
Bishop,M.A. Nearest neighbor analysis of mega-barchanoid dunes, Ar Rub' al Khali, sand sea: The application of geographical indices to the understanding of dune field self-organization, maturity and environmental change. Geomorphology 120 (2010) 186–194.
Cardinale et al. Dunes in: Hargitai, H. & Kereszturi, A. Encyclopedia of Planetary Landforms. New York : Springer Science+Business Media,2015,2460p.
Bridges,N.T.& Laity, J.E., Fundamentals of Aeolian Sediment Transport: Aeolian Abrasion In: Lancaster, N.& Sherman,D.J. (Eds).Treatise of Geomorphology,Vol 11, Aeolian Geomorphology.San Diego: Academic Press, 2013.437p.
Edgett,K.S. The ejecta deposit of the ancient basin Herschel - an example of a generally unrecognized Martian sedimentological unit. Houston, TX, Lunar and Planetary Institute, 1991, p.657-667.
El-Sayed,M.I. The nature and possible origin of mega-dunes in Liwa, Ar, Rub' Al Khali, UAE. Sedimentary Geology 134(3), 2000, p.305-330.
Greeley,R & Guest J.E. Geologic Map of the Eastern Equatorial Region of Mars. U.S Geological Survey Miscellaneous Investigations Series Map 1-1802-B, scale 1:15.000.000. U.S Geological Survey, 1987.
Hargitai,H. Dune-Field Patterns in Hargitai, H. & Kereszturi, A. Encyclopedia of Planetary Landforms. New York: Springer Science+Business Media, 2015, 2460p.
McEwan,A.S, et al. (2007) Mars Reconnaissance Orbiter's High Resolution Imaging Science Experiment (HiRISE) J. Geophys. Res., 112, E05S02
Melosh H. J. Planetary Surface Processes, Cambridge Univ. Press, Cambridge, 2011, 416 p.
Parker, T.J A reassetemen of Mars Ocean Hypotesis, Second Conference on Early Mars, Houston, TX: Lunar and Planetary Institute 3054, 2005
Parteli.E.J. Sand Dunes on Mars and on Earth. Ph.D. Thesis. Institut fur Computerphysik der Universität Stuttgart 2007.p.171.
Pye, K & Tsoar, H. Aeolian Sand and Sand Dunes. Berlin: Springer-Verlag, 2009, 475p.
Saunders, R. S, et al. 2001 Mars Odyssey Mission summary, Space Sci. Rev., 110, No. 1-2, 1-36, 2004.
Seidelmann, P.K et al. Report of the IAU/ IAG working group on cartographic coordinates and rotational elements of the planets and satellites. 2000. Celest. Mech. Dyn. Astron. 82 (1), 83–111, 2002.
Tsoar,H & Blumberg,D.Elongation and Migration of sand dunes. Geomorphology 57,2004, p.293-302.
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Este trabalho está licenciado com uma Licença Creative Commons - Atribuição 4.0 Internacional.