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During its historic close encounter with Phoebe, the Cassini spacecraft captured a series of high resolution images of the small moon, six of which have been put together to create this mosaic. Phoebe shows an unusual variation in brightness over its surface due to the existence on some crater slopes and floors of bright material -- thought to contain ice -- on what is otherwise one of the darkest known bodies in the solar system. Bright streaks on the rim of the large crater in the North (up in this image) may have been revealed by the collapse of overlying darker material from the crater wall. The large crater below right-of-center shows evidence of layered deposits of alternating bright and dark material. A possible mechanism for this apparent layering was discussed in an earlier image release

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      EUN,LOM,LRE4,hdl:10494/254268,work-cmr-id:254268,http://photojournal.jpl.nasa.gov:http://photojournal.jpl.nasa.gov/catalog/PIA06073,ilox,learning resource exchange,LRE metadata application profile,LRE

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