Definition
Crosshatched lineated and striated regolith texture on sloping and horizontal surfaces.
Synonyms
Description
Fine-scale wrinkle texture (lineations and striations). Striations frequently follow contours of surface topography, but there are generally several orientations of striations, with one dominant orientation and another more subdued orientation (Mattingly and El-Baz 1973).
Formation Models
- (1)
Creep: formed by the slow, cumulative downslope movement of the regolith caused by micrometeorite impacts (Pleascia and Robinson 2010). This model does not explain the occurrence of the texture in horizontal surfaces (Mattingly and El-Baz 1973; Antonenko 2012).
- (2)
Seismic shaking: reworking of unconsolidated regolith driven by horizontal surface oscillations generated by impacts that produce craters greater than 1 km in diameter, affecting a zone up to 10 crater radii away (Schultz and Gault 1975; Antonenko 2012). This is the most widely...
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References
Antonenko I (2012) Leathery texture in the Bose, Bhabha, and Stoney Crater Region of South Pole-Aitken Basin on the Moon. 43rd Lunar Planet Sci Conf, abstract #2581, Houston
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Mattingly TK, El-Baz F (1973) Impressions of the lunar highlands from the Apollo 16 Command Module. Proc 4th Lunar Sci Conf V1:49–56, Houston
Mest SC (2011) The geology of Schrodinger basin: insights from post-Lunar Orbiter data. In: Ambrose WA, Williams DA (eds) Recent advances and current research issues in lunar stratigraphy. Geological Society of America special paper 477. Geological Society of America, Boulder, SPE477-04
Pleascia J, Robinson MS (2010) Character of the Lunar regolith: the view from LROC EPSC Abstracts vol 5, EPSC2010-731
Schultz PH, Gault DE (1975) Seismically induced modification of Lunar surface features. Lunar Planet Sci VI:724–726, Houston
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Antonenko, I., Hargitai, H. (2014). Tree Bark Texture. In: Encyclopedia of Planetary Landforms. Springer, New York, NY. https://doi.org/10.1007/978-1-4614-9213-9_635-1
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DOI: https://doi.org/10.1007/978-1-4614-9213-9_635-1
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