STRATIGRAPHIC ARCHITECTURE OF BEDROCK REFERENCE SECTION, VICTORIA CRATER, MERIDIANI PLANUM, MARS LAUREN A. EDGAR, JOHN P. GROTZINGER, AND ALEX G. HAYES Division of Geological and Planetary Sciences, California Institute of Technology, Pasadena, California 91125 USA e-mail:
[email protected] DAVID M. RUBIN US Geological Survey Pacific Science Center, Santa Cruz, California 95060 USA STEVE W. SQUYRES AND JAMES F. BELL Astronomy Department, Cornell University, Ithaca, New York 14853 USA AND KEN E. HERKENHOFF US Geological Survey Astrogeology Science Center, Flagstaff, Arizona 86001 USA ABSTRACT: The Mars Exploration Rover Opportunity has investigated bedrock outcrops exposed in several craters at Meridiani Planum, Mars, in an effort to better understand the role of surface processes in its geologic history. Opportunity has recently completed its observations of Victoria crater, which is 750 m in diameter and exposes cliffs up to ;15 m high. The plains surrounding Victoria crater are ;10 m higher in elevation than those surrounding the previously explored Endurance crater, indicating that the Victoria crater exposes a stratigraphically higher section than does the Endurance crater; however, Victoria strata overlap in elevation with the rocks exposed at the Erebus crater. Victoria crater has a well-developed geomorphic pattern of promontories and embayments that define the crater wall and that reveal thick bedsets (3–7 m) of large-scale cross-bedding, interpreted as fossil eolian dunes. Opportunity was able to drive into the crater at Duck Bay, located on the western margin of Victoria crater. Data from the Microscopic Imager and Panoramic Camera reveal details about the structures, textures, and depositional and diagenetic events that influenced the Victoria bedrock.