Tarvos is a moon of Saturn, part of the Solar System in the universe. Saturn is a planet associated with the Sun, our star, and this space encyclopedia describes the moon’s identity and place in its planetary system.

Tarvos — A natural satellite of Saturn. Its physical properties and orbital motion are shown from the available catalogue and ephemeris data.

No object-specific chemical/elemental dataset has been verified and imported for this record. This does not mean none is publicly available. Appearance may be imagined; chemistry is not.

Discovery and designation
Tarvos was discovered in 2000. JPL credits B. Gladman, J. Kavelaars, J.-M. Petit, H. Scholl, M. Holman, B.G. Marsden, P. Nicholson, J.A. Burns. Its provisional designation is S/2000 S4. The name and discovery entry identify this particular satellite of Saturn; similarly named asteroids are separate objects.

Tarvos was discovered on Sept. 23, 2000, by Brett J. Gladman, John J. Kavelaars, Jean-Marc Petit, Hans Scholl, Matthew J. Holman, Brian G. Marsden, Phillip D. Nicholson, and Joseph A. Burns using the 3.6-m Canada-France-Hawaii reflector on Mauna Kea, Hawaii, with adaptive optics. They discovered seven other Saturnian moons at the same time: Siarnaq, Ijiraq, Thrymr, Skathi, Mundilfari, Erriapus and Suttungr.

Tarvos has a mean radius of about 4.7 miles (7.5 kilometers), assuming an albedo (a measure of how reflective the surface is) of 0.06. At a mean distance of 11.4 million miles (18.3 million kilometers) from Saturn, the moon takes about 926 Earth days to complete one orbit.

Tarvos is one of the four known members of the Gallic group of moons. These moons have prograde orbits (they travel around Saturn in the same direction as the planet's rotation), but their egg-shaped, angled orbits classify them as "irregular" moons. Like Saturn's other irregular moons, they are thought to be objects that were captured by Saturn's gravity, rather than having accreted from the dusty disk that surrounded the newly formed planet, as the regular moons are thought to have done.

The similarities among the orbits of moons in the Gallic group suggest a common origin – they may be fragments of a single object that shattered in a collision. The other members of this group are Albiorix, Bebhionn and Erriapus.

Observations by Tommy Grav and James Bauer using telescopes on Mauna Kea, Hawaii in 2006 found that the color of Albiorix varies over its surface. They hypothesize that Tarvos and Erriapus, which were both seen to be light red, are the largest fragments from an impact on Albiorix, leaving a less-red crater. (These observations did not include Bebhionn.)

Originally called S/2000 S4, Tarvos was named for a bull in Celtic mythology. It is known from two stone sculptures, found in Paris and Trier, of a bull with three cranes and a tree, which is presumed to be a willow. The narrative behind this imagery is lost to antiquity, but it has been hypothesized that the tree represents the cycle of life, the birds are spirits released when life has ended, and the bull represents the vigor and sexual potency that keeps the cycle spinning.