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Polar Spiral Troughs, Mars

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Encyclopedia of Planetary Landforms

Definition

Curvilinear troughs or depressions arranged along spiral trends on the northern and southern polar cap of Mars, perpendicular to large chasmata.

Synonyms

Accublation trough; Scarp/trough complex

Description

The polar caps and polar layered deposits of Mars at both hemispheres display pinwheel-shaped dark spiral troughs in helical arrangement (Fig. 1). Troughs in the north have a clear clockwise spiraling pattern; they extend and spiral from the highest region of the cap, located near the rotational pole. They have asymmetric cross-sectional profiles with steeper equatorward-facing slopes (Pathare and Paige 2005) (high sides) (Smith et al. 2013). Polar spiral trough systems in the south are parallel sets of curvilinear grooves perpendicular to the larger curvilinear canyons, trending down canyon, e.g., Australe Sulci (Kolb and Tanaka 2006). Large spirals have an opposite sense in opposite hemispheres (e.g., Smith et al. 2013).

Fig. 1
figure 1

The residual polar ice caps, showing the...

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References

  • Cutts JA (1973) Wind erosion in the Martian polar regions. J Geophys Res 78(20):4211–4221. doi:10.1029/JB078i020p04211

    Article  Google Scholar 

  • Fishbaugh KE, Head JW (2002) Chasma Boreale, Mars: topographic characterization from Mars Orbiter Laser Altimeter data and implications for mechanisms of formation. J Geophys Res 107(E3). doi:10.1029/2000JE001351

    Google Scholar 

  • Fisher D (1993) If Martian ice caps flow: ablation mechanisms and appearance. Icarus 105:501–511

    Article  Google Scholar 

  • Fisher DA (2000) Internal layers in an “accublation” ice cap: a test for flow. Icarus 144:289–294

    Article  Google Scholar 

  • Grima C, Kofman W, Mouginot J, Phillips RJ, Hérique A, Biccari D, Seu R, Cutigni M (2009) North polar deposits of Mars: extreme purity of the water ice. Geophys Res Lett 36:L03203. doi:10.1029/2008GL036326

    Article  Google Scholar 

  • Herkenhoff KE, Plaut JJ (2000) Surface ages and resurfacing rates of the polar layered deposits on Mars. Icarus 144(2):243–253

    Article  Google Scholar 

  • Howard AD (1978) Origin of the stepped topography of the Martian poles. Icarus 34:581–599

    Article  Google Scholar 

  • Howard AD (2000) The role of eolian processes in forming surface features of the Martian polar layered deposits. Icarus 144:267–288

    Article  Google Scholar 

  • Howard AD, Cutts JA, Blasius KR (1982) Stratigraphic relationships within Martian Polar Cap Deposits. Icarus 50:161–215

    Article  Google Scholar 

  • Hvidberg CS, Fishbaugh KE, Winstrup M, Svensson A, Byrne S, Herkenhoff KE (2012) Reading the climate record of the Martian polar layered deposits. Icarus 221:405–419

    Article  Google Scholar 

  • Karlsson NB, Holt JW, Hindmarsh RCA (2011) Testing for flow in the north polar layered deposits of Mars using radar stratigraphy and a simple 3D ice-flow model. Geophys Res Lett 38:L24204. doi:10.1029/2011GL049630

    Article  Google Scholar 

  • Kolb EJ, Tanaka KL (2001) Geologic history of the polar regions of Mars based on Mars Global Surveyor data. Icarus 154:22–39

    Article  Google Scholar 

  • Kolb EJ, Tanaka KL (2006) Accumulation and erosion of south polar layered deposits in the Promethei Lingula region, Planum Australe, Mars. MARS 2:1–9. doi:10.1555/mars.2006.0001

    Google Scholar 

  • Murray BC, Soderblom LA, Cutts JA, Sharp RP, Milton DJ, Leighton RB (1972) Geological framework of the south polar region of Mars. Icarus 17(2):328–345

    Article  Google Scholar 

  • Pathare VA, Paige DA (2005) The effects of Martian orbital variations upon the sublimation and relaxation of north polar troughs and scarps. Icarus 174(2):419–443

    Article  Google Scholar 

  • Siegert MJ, Fisher DA (2002) A terrestrial analogy for Martian “accublation zones” revealed by airborne ice-penetrating radar from the east Antarctic ice sheet. Icarus 157:264–267

    Article  Google Scholar 

  • Smith IB, Holt JW (2010) Onset and migration of spiral troughs on Mars revealed by orbital radar. Nature 465(7297):450–453

    Article  Google Scholar 

  • Smith IB, Holt JW (2012) The northern spiral troughs of Mars as cyclic steps: a theoretical framework for calculating average migration and accumulation rates. In: 43rd LPSC, The Woodland Texas #2116

    Google Scholar 

  • Smith IB, Holt JW, Spiga A, Howard AD, Parker G (2013) The spiral troughs of Mars as cyclic steps. J Geophys Res Planets 118:1835–1857. doi:10.1002/jgre.20142

    Article  Google Scholar 

  • Squyres SW (1979) The evolution of dust deposits in the Martian north polar region. Icarus 40:244–261

    Article  Google Scholar 

  • Weijermars R (1986) The polar spirals of Mars may be due to glacier surges deflected by Coriolis forces. Earth Planet Sci Lett 76(3–4):227–240

    Article  Google Scholar 

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Correspondence to Ákos Kereszturi .

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Kereszturi, Á., Hargitai, H. (2014). Polar Spiral Troughs, Mars. In: Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_279-1

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  • DOI: https://doi.org/10.1007/978-1-4614-9213-9_279-1

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