This close-up of Dione's icy surface shows deeply shadowed craters near the terminator, as well as a group of roughly linear faults above centre.
Expand (118kb, 936 x 1242) The terrain shown here is on the moon's leading hemisphere. North on Dione is up and tilted 21 degrees to the right.
The image was taken in visible green light with the Cassini spacecraft narrow-angle camera on Dec. 24, 2005 at a distance of approximately 152,000 kilometres from Dione and at a Sun-Dione-spacecraft, or phase, angle of 109 degrees. Resolution in the original image was 904 meters per pixel. The image has been magnified by a factor of two and contrast-enhanced to aid visibility.
This false colour image shows the leading hemisphere of Dione. To create this view, ultraviolet, green and infrared images were combined into a single black and white picture that isolates and maps regional colour differences.
This "colour map" was then superposed over a clear-filter image. The origin of the colour differences is not yet understood, but may be caused by subtle differences in the surface composition or the sizes of grains making up the icy soil. Terrain visible here is on the moon's leading hemisphere. North on Dione is up and rotated 17 degrees to the right.
All images were acquired with the Cassini spacecraft narrow-angle camera on Dec. 24, 2005 at a distance of approximately 597,000 kilometres from Dione and at a Sun-Dione-spacecraft, or phase, angle of 21 degrees. Image scale is 4 kilometres per pixel.
This global digital map of Saturn's moon Dione was created using data taken during Cassini and Voyager spacecraft flybys. The map is an equidistant projection and has a scale of 977 meters per pixel.
Expand (1.4Mb,5750 x 3244) The mean radius of Dione used for projection of this map is 560 kilometres. The resolution of the map is 10 pixels per degree.
To create this false-colour view, ultraviolet, green and infrared images were combined into a single black and white picture that isolates and maps regional colour differences. This "colour map" was then superimposed over a clear-filter image of the moon.
Credit: NASA/JPL/Space Science Institute
The combination of colour map and brightness image shows how the colours vary across the moon's surface in relation to geologic features. The origin of the colour differences is not yet understood, but may be caused by subtle differences in the surface composition or the sizes of grains making up the icy soil.
The images were acquired on August 1, 2005, at a mean distance of 267,600 kilometres from Dione. Image scale is 1.6 kilometres per pixel. The image shows terrain on the trailing hemisphere of Dione 1,126 kilometres across, and is centred on 41 degrees south latitude. North is up.
Dione's icy surface is scarred by craters and sliced up by multiple generations of geologically-young bright fractures. Numerous fine, roughly-parallel linear grooves run across the terrain in the upper left corner. Most of the craters seen here have bright walls and dark deposits of material on their floors. As on other Saturnian moons, rockslides on Dione may reveal cleaner ice, while the darker materials accumulate in areas of lower topography and lower slope (e.g. crater floors and the bases of scarps).
The terrain seen here is centred at 15.4 degrees north latitude, 330.3 degrees west longitude, in a region called Carthage Linea. North on Dione is up and rotated 50 degrees to the left. The image was taken in visible green light with the Cassini narrow-angle camera on Oct. 11, 2005, at a distance of approximately 19,600 kilometres from Dione. The image scale is about 230 meters per pixel.
The terrain seen here becomes notably darker toward the west, and is crosscut by the bright, fresh canyons that form wispy markings on Dione's trailing hemisphere. The image was taken in visible light with the Cassini wide-angle camera at a distance of approximately 24,500 kilometres from Dione and at a Sun-Dione-spacecraft, or phase, angle of 22 degrees. The image scale is about 2 kilometres per pixel.
Saturn's moon Dione is about to swing around the edge of the thin F ring in this colour view. More than one thin strand of the F ring's tight spiral can be seen here.
The terrain seen on Dione is on the moon's Saturn-facing hemisphere. The diameter of Dione is 1,126 kilometres.
Images taken using infrared, green and ultraviolet spectral filters were composited to create this colour view. The images were taken with the Cassini spacecraft narrow-angle camera on Sept. 20, 2005, at a distance of approximately 2 million kilometres from Dione and at a Sun-Dione-spacecraft, or phase, angle of 48 degrees. The image scale is 12 kilometres per pixel.
The cratered and cracked disk of Saturn's moon Dione looms ahead in this mosaic of images taken by Cassini on Oct. 11, 2005, as it neared its close encounter with the icy moon.
In this false-colour mosaic, the clear-filter images are overlain by colour composited from (compressed) infrared, green and ultraviolet images. The colours have been specially processed to accentuate subtle changes in the spectral properties of Dione's surface materials. To create the colour view, the colour images were combined into a single black and white picture that isolates and maps regional colour differences. This "colour map" was then superimposed over the clear-filter mosaic. Multiple generations of tectonics can be seen in this full-disk view. Near the eastern limb (at the right) are tectonic fractures, which may be similar to the bright, braided canyons that make up Dione's noted wispy terrain. Some of the bright, wispy markings can be seen at the left.
The softer ridges and troughs at the upper right appear to be about the same age as the cratering seen in that region. These appear to be older than the fracturing seen in the wispy terrain and the fractures seen at the right. Scientists continue to be intrigued by the strikingly linear features seen crisscrossing the southern latitudes. The fine latitudinal streaks appear to crosscut everything, and appear to be the youngest feature type in this region of Dione. A large impact basin hugs the south polar region (at the bottom, right of centre). Northeast of the basin is a region of terrain that is relatively smooth, compared to the rest of the moon. This view of Dione is centred on 1.3 degrees south latitude, 167.6 degrees west longitude.
The images in the mosaic were obtained with the Cassini spacecraft narrow-angle camera at distances ranging from of 55,280 to 27,180 kilometres from Dione. The full-size versions of the mosaics have an image scale of 316 meters per pixel.