Venus's shield terrain

Vicki L. Hansen

Research output: Contribution to journalReview articlepeer-review

22 Scopus citations


Plains, planitiae, or lowlands - expanses of gentle, long-wavelength (∼1000 km) basins - cover ∼80% of Venus's surface. These regions are widely accepted as covered by volcanic flows, although the mechanism(s) responsible for resurfacing remains elusive; in addition, a volcanic origin for the lowland surface may be open to question. Lowland resurfacing is typically attributed to catastrophic emplacement (10-100 m.y.) of globally extensive, thick (1-3 km) flood-type lava. This model of resurfacing has been postulated on the basis of impact crater distribution, taken together with a lack of obvious volcanic flows or edifices, and a lack of viable alternative models. Ongoing geologic mapping of ∼15,000,000 km2 (0-25N/90-150E) using 225 m/ pixel and 75 m/pixel NASA Magellan SAR (synthetic aperture radar) data indicates that small edifices, called shields (1-15-km-diameter edifices, «1 km high), play a major role in lowland resurfacing. Individual shields are radar-smooth or - rough, quasi-circular to circular features with or without a central pit. Shield shapes, which have been previously documented, range from shield, dome, or cone, to flat-topped or flat. Shield deposits typically coalesce, forming a thin, regionally extensive but discontinuous, mechanically strong layer, herein called shield paint. Shield paint conforms to delicate local topography, providing evidence of its thin character and indicating generally low viscosity during emplacement. Shield terrain (shields and shield paint) covers more than 10,000,000 km2 within the study area. Detailed mapping of five 2° × 2° regions using coregistered normal and inverted right- and left-illumination SAR imagery indicates shield densities of 3500-33,500 shields/106 km2; thus, the map area hosts more than 35,000-335,000 shields. Shield terrain generally postdates, but is also locally deformed by, fractures and wrinkle ridges, indicating time-transgressive formation relative to local deformation and/or reactivation. The regional scale crust was strong throughout shield-terrain formation. Shield terrain may extend across much of Venus's surface.

Original languageEnglish (US)
Pages (from-to)808-822
Number of pages15
JournalBulletin of the Geological Society of America
Issue number5-6
StatePublished - May 2005


  • Flood lava
  • Mud volcano
  • Partial melt
  • Resurfacing
  • Shields
  • Venus


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