PASADENA, Calif. -- These Dawn FC
(framing camera) images show part of the south polar basin. A large
scarp (eg. cliff) is visible in the top right of the images, grooves and
hummocky (eg. wavy/undulating) terrane are visible in the center of the
images and the mountain/central complex is visible in the bottom left
of the images. 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 various colors
correspond to the height of the area that they color. For example, the
white in the top left of the right image is the highest area and the
blue areas in the bottom right of the image are the lowest. The scarp
and surrounding area are some of the highest regions in the image. Then
there is a blue colored depression in between this area and the
mountain/ central complex. This is a green color which corresponds to a
height in between that of the scarp area and the depression area. The
topography is calculated from a set of images that were observed from
different viewing directions, these are called stereo images.
NASA’s
Dawn spacecraft obtained the albedo image with its framing camera on
August 11, 2011. This image was taken through the camera’s clear filter.
The distance to the surface of Vesta is 2740 km the image has a
resolution of about 250 meters per pixel. The images are projected using
a lambert-azimuthal map projection.
Image Credit: NASA/ JPL-Caltech/ UCLA/ MPS/ DLR/ IDA
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