Publication Date:
2013-08-31
Description:
Analysis of high spatial resolution (down to 2 to 5 km) thermal data that shows the presence of aeolian debris mantling in topographic traps such as some channels is presented. In cases where this occurs, even if the mantle is thin, it can prevent remote sensing analysis of actual compositional differences that may characterize the true floors of the features.
Keywords:
LUNAR AND PLANETARY EXPLORATION
Type:
MECA Symposium on Mars: Evolution of its Climate and Atmosphere; p 126-128
Format:
application/pdf