Field Studies of Crater Gradation in Gusev Crater and Meridiani Planum Using the Mars Exploration RoversThe Mars Exploration Rovers Spirit and Opportunity investigated numerous craters since landing in Gusev crater (14.569degS, 175.473degE) and Meridiani Planum (1.946degS, 354.473degE) over the first 400 sols of their missions [1-4]. Craters at both sites are simple structures and vary in size and preservation state. Comparing observed and expected pristine morphology and using process-specific gradational signatures around terrestrial craters as a template [5-7] allows distinguishing gradation processes whose relative importance fundamentally differs from those responsible for most crater modification on the Earth.
Document ID
20050201825
Acquisition Source
Headquarters
Document Type
Conference Paper
Authors
Grant, J. A. (Smithsonian Institution Washington, DC, United States)
Golombek, M. P. (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Haldemann, A. F. C. (Jet Propulsion Lab., California Inst. of Tech. Pasadena, CA, United States)
Crumpler, L. (New Mexico Museum of Natural History and Science Albuquerque, NM, United States)
Li, R. (Ohio State Univ. Columbus, OH, United States)
Watters, W. A. (Massachusetts Inst. of Tech. Cambridge, MA, United States)
Date Acquired
September 7, 2013
Publication Date
January 1, 2005
Publication Information
Publication: Workshop on The Role of Volatile and Atmospheres on Martian Impact Craters
IDRelationTitle20050201815Collected WorksWorkshop on The Role of Volatile and Atmospheres on Martian Impact Craters20050201815Collected WorksWorkshop on The Role of Volatile and Atmospheres on Martian Impact Craters