The Geology of Gaspra

M. H. Carr, R. L. Kirk, Alfred S. McEwen, J. Veverka, P. Thomas, J. W. Head, S. Murchie

Research output: Contribution to journalArticle

75 Citations (Scopus)

Abstract

The surface of Gaspra can be divided into several facets separated by ridges. Superimposed on the facets and ridges are two populations of craters. Type 1 craters are crisply defined and constitute a production function of impact origin. Type 2 craters are mostly irregular shallow depressions and probably of various origins. Some of the type 2 craters may have formed by impact and be remnants of a crater population that predates the type 1 population. The number of type 1 craters suggests that they started to accumulate 2 × 107 to 3 × 108 years ago. The freshest craters have a depth/diameter ratio of 1:7, as compared with 1:5 typically observed on other bodies. The craters appear to have become shallower with age at a rate of 10-6 to 10-7 m/year. The shallow depth of newly formed craters and the progressive degradation with age are ascribed to downslope movement of poorly coherent surface materials, the movement being aided by seismic shaking as a result of impact. The surface shows subtle color differences. The most prominent differences are observed around craters on ridges, where the surface has a stronger 1-μm absorption than elsewhere. The contrast is not observed around craters on the facets. The color differences are attributed to alteration of the materials brought to the surface. The unaltered material is estimated to be located at least 50 m below the surface on the facets. Only on the ridges is unaltered material at a shallow enough depth to be excavated by the observed craters. The rate of degradation of craters, the rounded form of the ridges, the depth of altered material on the facets, and the presence of old degraded craters all suggest that Gaspra is covered with a regolith a few tens to several tens of meters thick.

Original languageEnglish (US)
Pages (from-to)61-71
Number of pages11
JournalIcarus
Volume107
Issue number1
DOIs
StatePublished - Jan 1994
Externally publishedYes

Fingerprint

geology
craters
crater
ridges
flat surfaces
degradation
color
regolith
shaking
material

ASJC Scopus subject areas

  • Astronomy and Astrophysics
  • Space and Planetary Science

Cite this

Carr, M. H., Kirk, R. L., McEwen, A. S., Veverka, J., Thomas, P., Head, J. W., & Murchie, S. (1994). The Geology of Gaspra. Icarus, 107(1), 61-71. https://doi.org/10.1006/icar.1994.1006

The Geology of Gaspra. / Carr, M. H.; Kirk, R. L.; McEwen, Alfred S.; Veverka, J.; Thomas, P.; Head, J. W.; Murchie, S.

In: Icarus, Vol. 107, No. 1, 01.1994, p. 61-71.

Research output: Contribution to journalArticle

Carr, MH, Kirk, RL, McEwen, AS, Veverka, J, Thomas, P, Head, JW & Murchie, S 1994, 'The Geology of Gaspra', Icarus, vol. 107, no. 1, pp. 61-71. https://doi.org/10.1006/icar.1994.1006
Carr MH, Kirk RL, McEwen AS, Veverka J, Thomas P, Head JW et al. The Geology of Gaspra. Icarus. 1994 Jan;107(1):61-71. https://doi.org/10.1006/icar.1994.1006
Carr, M. H. ; Kirk, R. L. ; McEwen, Alfred S. ; Veverka, J. ; Thomas, P. ; Head, J. W. ; Murchie, S. / The Geology of Gaspra. In: Icarus. 1994 ; Vol. 107, No. 1. pp. 61-71.
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