CICLOPS: Cassini Imaging Central Laboratory for OPerationS
Ancient Plains of Rhea

Ancient Plains of Rhea
PIA 09895

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  Densely cratered plains cover the ancient surface of Saturn's moon Rhea.

Following the Voyager spacecraft encounters with Saturn, cryovolcanism was suggested as a source for the wispy markings on both Rhea and Dione. Cassini has shown that Rhea's bright streaks are, like those on Dione, tectonic features. Planetary scientists now think it is unlikely that cryovolcanic activity has ever occurred on this moon.

This view looks toward the trailing hemisphere of Rhea (1,528 kilometers, 949 miles across). North is up.

The image was taken in visible light with the Cassini spacecraft narrow-angle camera on April 4, 2008. The view was acquired at a distance of approximately 1.2 million kilometers (735,000 miles) from Rhea and at a Sun-Rhea-spacecraft, or phase, angle of 39 degrees. Image scale is 7 kilometers (4 miles) per pixel.

The Cassini-Huygens mission is a cooperative project of NASA, the European Space Agency and the Italian Space Agency. The Jet Propulsion Laboratory, a division of the California Institute of Technology in Pasadena, manages the Cassini-Huygens mission for NASA's Science Mission Directorate, Washington, D.C. The imaging team consists of scientists from the US, England, France, and Germany. The imaging operations center and team lead (Dr. C. Porco) are based at the Space Science Institute in Boulder, Colo.

For more information about the Cassini-Huygens mission, visit and the Cassini imaging team home page,

Credit: NASA/JPL/Space Science Institute
Released: May 6, 2008 (PIA 09895)
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