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CRISMCompact Reconnaissance Imaging Spectrometer for Mars Even though some landforms provide evidence that liquid water may have flowed on the surface of Mars long ago, evidence of mineral deposits created by long-term interaction between water and rock has been limited. CRISM's visible and infrared spectrometers track regions on the dusty martian surface and map them at scales as small as 18 meters (60 feet) across, from an altitude of 300 kilometers (186 miles). CRISM reads the hundreds of "colors" in reflected sunlight to detect patterns that indicate certain minerals on the surface, including signature traces of past water. The principal investigator (lead scientist) for CRISM is Scott Murchie from the Applied Physics Lab at Johns Hopkins University. Visit the instrument site:
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