| South polar impacts on Vesta. The map indicates that the Vesta surface is not uniform, with a sharp contrast between the northern and southern regions. These data suggest that the region around the Rheasilvia basin is richer in diogenites than the equatorial regions. The north-south variation in minerals indicates that the deep crust exposed in the southern Rheasilvia region is dominated by pyroxene-rich, diogenitic material while the equatorial region seems to retain the most ancient eucrite-rich mineralogy. In this image, blue shows a richer concentration of diogenite minerals and yellow shows a richer concentration of eucrite minerals. The visible and infrared mapping spectrometer collected the data used to create this mosaic image in August 2011, from an average altitude of about 1,700 miles or (2,700 kilometers). Credit: NASA/JPL-Caltech/UCLA/INAF/MPS/DLR/IDA |
