This detail of a Dawn FC (framing camera) image shows many fresh
craters, several with bright ejecta rays, which were formed by impacts
into the floor of Vesta’s south polar basin. The three most distinctive
rayed craters are in the top and middle of the image and each has a
clear raised crater rim. Ejecta rays form when material is thrown out
of a crater during an impact. These ejecta rays most commonly have a
higher albedo (are brighter) than the surrounding surface, as is the
case here. Sometimes larger masses of ejecta form small secondary
craters near these ejecta rays. Even though this image resolves numerous
small craters, only a few hundred meters across, higher resolution
imagery is necessary to identify secondary craters in this case. The
rayed craters also contain enigmatic low albedo dark material, which is
seen across Vesta. The distinctive hummocky (eg. wavy/ undulating)
terrane of Vesta’s south polar region is evident throughout this image
as well.
NASA’s Dawn spacecraft obtained this image with its framing camera on September 9th
2011. This image was taken through the camera’s clear filter. The
distance to the surface is 1390km and the image resolution is about 130
meters per pixel.
Image Credit: NASA/ JPL-Caltech/ UCLA/ MPS/ DLR/ IDA
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