T308 Geology of Dwarf Planets: First Results from NASA's Dawn Mission to Ceres (Posters)
Wednesday, 4 November 2015
9:00 AM - 6:30 PM
Exhibit Hall
PRELIMINARY GEOLOGICAL MAP OF THE AC-H-1 ASARI QUADRANGLE OF CERES: AN INTEGRATED MAPPING STUDY USING DAWN SPACECRAFT DATA
Paper number: T308-1
Program: Technical Sessions
Time: 9:00 AM – 6:30 PM
Authors
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Lucy A. McFaddenNASA GSFC, Greenbelt, MD
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Harald HiesingerInstitut fuer Planetologie WWU, Muenster
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Jennifer E.C. ScullyJet Propulsion Laboratory, California Institute of Technology, Pasadena, CA
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Thomas KneisslFreie Universität Berlin, Berlin
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Kynan H.G. HughsonUniversity of California, Los Angeles, Los Angeles, CA
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David A. WilliamsArizona State University, Tempe, AZ
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Thomas RoatschInstitute of Planetary Research, Berlin
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Frank PreuskerInstitute of Planetary Research, Berlin
Abstract
We present a photo-geological map of the “Asari” quadrangle covering the North Pole area of Ceres (66°N-90°N), based on Dawn Framing Camera images and mosaics with a resolution of ~400 m/pixel. The mapping process is supported by a stereo-photogrammetric digital elevation model. We identified few isolated plateaus of up to ~5 km in altitude relative to the datum and topographic depressions interpreted to be highly degraded impact basins. At 85°N/8°E a cone-shaped positive relief is found, few tens of kms large. Overall, the entire quadrangle is heavily cratered, and our measurements of crater density (9.8E-04 km-2 for crater diameters >10 km) identify the area as the most cratered on Ceres. This suggest a different geological history of the quadrangle relative to, e.g., the equatorial regions. The morphology of impact craters is characterized by central peaks and mass wasting deposits. We identified a morphologically-fresh mass wasting deposit at 78°N/38°E, 20 km in length, with a lobate margin and striations on its surface. This deposit and the positive relief at 85°N/8°E will be the focus of future investigations when higher spatial resolution images will be acquired by the Dawn Framing Camera. Observations with a spatial resolution of up to 35 m/pixel are planned and will allow photo-geological mapping at higher details. Support by N. Schmedemann, S. Marchi, R. Jaumann, A. Nathues, C.A. Raymond, C.T. Russell, and the Dawn Instrument, Operations, and Science Teams is acknowledged.