DLR Institute of Planetary Research - 06.11.2011 - Topography of a scarp and hummocky terrain in Vesta’s south polar region

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06.11.2011 - Topography of a scarp and hummocky terrain in Vesta’s south polar region

PASADENA, Calif. -- These Dawn FC (framing camera) images show part of the rim of the south polar basin, which is dominated by a large scarp (eg. cliff) that runs vertically across the center of the images. The piled-up material at the scarp’s base is likely due to landsliding. There is also some hummocky (eg. wavy/ undulating) terrain to the left of the scarp. The left image is an albedo image, which is taken directly through the clear filter of the FC. Such an image shows the albedo (eg. brightness/ darkness) of the surface. The right image uses the same albedo image as its base but then a color-coded height representation of the topography is overlain onto it. The topography is calculated from a set of images that were observed from different viewing directions, called stereo images. The various colors correspond to the height of the area that they color. For example, white and red areas on the right are the highest regions and the blue areas on the left are the lowest. The change in color-coded height on the scarp from red to green illustrates its dramatic topographic profile. The blue color-coded hummocky terrain is located on the base of the south polar basin, which is the lowest region in this image.

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