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Current Crescent and Scour Flute

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Encyclopedia of Planetary Landforms
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Definition, Description, and Subtypes

  1. (1)

    Erosional: Scour zone/crescentic furrow – a deposit-free U-shaped or moat-like depression encircling a topographic obstacle in an area otherwise covered by deposits (e.g., aeolian) (Bishop 2011). The deepest part of the moat is typically upwind (e.g., between a possible echo dune and the obstacle). Its arms extend leeward in a pair of furrows that become shallower and wider downflow (Sharpe and Shaw 1989) (Figs. 1 and 3a–c).

  2. (2)

    Depositional: Horseshoe (U) shaped or paired accumulations in front of an obstacle (on the windward or up-current side) and on the two sides appearing as two wings, formed by the airflow or streamflow deflected around and over the obstacle (Pye and Tsoar 1990 and references therein) (double lee dunes) (Fig. 3d).

Current Crescent and Scour Flute, Fig. 1
figure 3249 figure 3249

Initial stages of the erosion of friable Medusae Fossae materials at 10°S 182°E, Mars. These current crescents may evolve into yardangs (Mandt et al. 2009). Scale bar 2...

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References

  • Allen JRL (1965) Scour marks in snow. J Sediment Petrol 35(2):331–338

    Google Scholar 

  • Allen JRL (1982) Sedimentary structures: their character and physical basis II. In: Developments in sedimentology 30b. Elsevier, Amsterdam

    Google Scholar 

  • Bishop MA (2010) Obstacle marks: evidence of variable wind erosion and sediment transport, Hellespontus, Mars. In: Second international planetary dunes workshop #2020 LPI

    Google Scholar 

  • Bishop MA (2011) Aeolian scours as putative signatures of wind erosion and sediment transport direction on Mars. Geophys J Roy Astron Soc 125:569–574

    Google Scholar 

  • Euler T (2009) Fluvial obstacle marks as complex geomorphic systems: a comparison between physically modelled and natural forms. Geophys Res Abstr 11, EGU2009-4035, EGU General Assembly

    Google Scholar 

  • Greeley R (1999) Mars pathfinder landing site: simulations of wind erosion and deposition. Lunar Planet Sci Conf XXX, abstract #1300, Houston

    Google Scholar 

  • Greeley R, Bridges NT, Kuzmin RO, Laity JE (2002) Terrestrial analogs to wind-related features at the Viking and pathfinder landing sites on Mars. J Geophys Res 107:E1. doi:10.1029/2000JE001481

    Google Scholar 

  • Herget J (2005) Reconstruction of Pleistocene ice-dammed lake outburst floods in the Altai Mountains, Siberia. The Geological Society of America Special Paper 386

    Google Scholar 

  • Karcz I (1968) Fluviatile obstacle marks from the wadis of the Negev (Southern Israel). J Sediment Petrol 38(4):1000–1012

    Google Scholar 

  • Komar PD (1985) Experiments and analyses of the formation of erosional scour marks with implications to the origin of the Martian outflow channels. NASA, Washington Reports of Planetary Geol Geophys Program, 22–324 (SEE N85-23474 13-91)

    Google Scholar 

  • Kor PSG, Shaw J, Sharpe DR (1991) Erosion of bedrock by subglacial meltwater, Georgian Bay, Ontario: a regional view. Can J Earth Sci 28:623–642

    Article  Google Scholar 

  • Mandt K, de Silva S, Zimbelman J, Wyrick D (2009) Distinct erosional progressions in the Medusae Fossae Formation, Mars, indicate contrasting environmental conditions. Icarus 204:471–477

    Article  Google Scholar 

  • Metzger SM (2000) Shifting wind regimes at MPF as evidenced by wind tail bedding. Lunar Planet Sci Conf XXXI, abstract #2095, Houston

    Google Scholar 

  • Munro-Stasiuk MJ, Shaw J, Sjogren DB, Brennand TA, Fisher TG, Sharpe DR, Kor PSG, Beaney CL, Rains BB (2009) The morphology and sedimentology of landforms created by subglacial megafloods. In: Carling PA, Baker VR, Burr DM (eds) Megaflooding on earth and mars. Cambridge University Press, Cambridge, pp 78–103

    Chapter  Google Scholar 

  • Peabody FE (1947) Current crescents in the Triassic Moenkopi formation [Arizona]. J Sediment Res 17(2):73–76

    Article  Google Scholar 

  • Pye K, Tsoar H (1990) Aeolian sand and sand dunes. Unwin Hyman, London

    Book  Google Scholar 

  • Reineck HE, Singh IB (1973) Depositional sedimentary environments. Springer, Berlin, 439 pp

    Book  Google Scholar 

  • Rygel MC, Calder JH, Gibling MR, Gingras MK, Melrose CSA (2006) Tournaisian forested wetlands in the Horton Group of Atlantic Canada. GSA Spec Pap 399:103–126. doi:10.1130/2006.2399(05)

    Google Scholar 

  • Sharpe DR, Shaw J (1989) Erosion of bedrock by subglacial meltwater, Cantley, Quebec. Geol Soc Am Bull 101:1011–1020

    Article  Google Scholar 

  • Shaw J, Pugin A, Young RR (2008) A meltwater origin for Antarctic shelf bedforms with special attention to megalineations. Geomorphology 102(3–4):364–375

    Article  Google Scholar 

  • Tsoar H (1983) Wind tunnel modeling of echo and climbing dunes. In: Brookfield ME, Ahlbrandt TS (eds) Eolian sediments and processes. Developments in sedimentology. Elsevier, Amsterdam, pp 247–259

    Chapter  Google Scholar 

  • Werner F, Unsöld G, Koopmann B, Stefanon A (1980) Field observations and flume experiments on the nature of comet marks. Sediment Geol 26:233–262

    Article  Google Scholar 

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Correspondence to Henrik Hargitai .

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Hargitai, H. (2015). Current Crescent and Scour Flute. In: Hargitai, H., Kereszturi, Á. (eds) Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-3134-3_116

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