Analysis of the panoramas of the Venera 13 and Venera 14 landing sites
Abstract
Geological and morphological analysis demonstrates that rock outcrops with thin horizontal bedding occur at the Venera 13 and Venera 14 landing sites. These rocks have much the same distinctive morphology as those at the Venera 9 and Venera 10 sites, and are most likely of sedimentary origin - tuff, in particular.
- Publication:
-
Pisma v Astronomicheskii Zhurnal
- Pub Date:
- August 1982
- Bibcode:
- 1982PAZh....8..429B
- Keywords:
-
- Geomorphology;
- Landing Sites;
- Panoramic Cameras;
- Planetary Geology;
- Venus Surface;
- Planetology;
- Sedimentary Rocks;
- Venera Satellites;
- Lunar and Planetary Exploration