Light-toned patches on the closest flank of the cone, and the entire field of light-toned material on the left of the cone (see annotated image) are hydrothermal deposits.
The cone is about 5 kilometers (3 miles) in diameter at the base.
The deposits are evidence for a past local environment that was warm and wet or steamy, possibly hospitable to microbial life, as reported in a November 2010 Nature Geoscience paper by J.R. Skok, of Brown University, Providence, R.I., and co-authors.
This image is in false color derived from observation in infrared wavebands with the Compact Reconnaissance Imaging Spectrometer for Mars (CRISM) on NASA's Mars Reconnaissance Orbiter.
The CRISM spectral data is overlaid on imagery from the Context Camera on that orbiter.
A stereo pair of Context Camera images provided topographic information for a digital terrain model produced with NASA Ames Stereo Pipeline software. The image uses no vertical exaggeration.
NASA's Jet Propulsion Laboratory, a division of the California Institute of Technology, Pasadena, manages the Mars Reconnaissance Orbiter for the NASA Science Mission Directorate, Washington. Lockheed Martin Space Systems, Denver, built the spacecraft.
The Johns Hopkins University Applied Physics Laboratory led the effort to build the CRISM instrument and operates CRISM in coordination with an international team of researchers from universities, government and the private sector.
Malin Space Science Systems, San Diego, built and operates the Context Camera.
Image Credit: NASA/JPL-Caltech/MSSS/JHU-APL/Brown Univ.
› See annotated image
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