Titan is the fifteenth of Saturn's known satellites and the largest. Discovered in 1655 by Dutch physicist and astronomer, Christiaan Huygens. The orangy haze seen in the picture above is due to Titan's thick atmosphere, and we have no direct images of the surface-YET. Soon the Huygens Mission will visit! Click here, too.
Titan's low density
Earth has a dense iron rich core, giving it its high density. Even the
Moon has a significantly higher density, 3 x water, and is made
mostly of silicate rock (little iron). Titan's low density suggests
it contains a lot of frozen water, methane, carbon dioxide and ammonia.
Water ices are
common and ubiquitous all over the outer solar system, in Jupiter,
on the icy rings of Saturn and are the predominant ice found in Comets.
Saturn's remaining moons
The remaining moons show heavy cratering, though Enceladus appears to show
evidence of more recent geological activity, having a relatively crater-free
region on its surface. All of the moons, including Titan, are tidally locked
to Saturn. See ground based image here.
Interactions between Rings and Moons
There are complex tidal resonances between some of Saturn's moons and the ring
system: some of the moons, the so-called "shepherding satellites" (i.e. Atlas,
Prometheus and Pandora) are clearly important in keeping the rings in place.
Shepherd satellites or moons move just inside or outside of a ring
system, and confine the narrow rings through their gravitational effect.
Moons can also clear out sections of the rings: Mimas
seems to be responsible for the paucity of material in the Cassini division;
Pan is located inside yet another gap (Encke Division). The
whole system is very complex and as yet poorly understood. A diagram
of the ring and moon system is shown
HERE.