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A theory for the formation of Saturn and its family of satellites, which is based on ideas of supersonic turbulent convection applied to the original Laplacian hypothesis, is presented. It is shown that if the primitive rotating cloud which gravitationally contracted to form Saturn possessed the same level of turbulent kinetic energy as the clouds which formed Jupiter and the Sun, given byf(&) = $ppGM(r)/r where p = 0.1065 f 0.0015, then it would shed a concentric system of orbiting gas rings each of about the same mass: namely, 1.0 X lo-"Ms. The orbital radii R, (n = 0, 1, 2,. . .) of these gas rings form a geometric sequence similar to the observed distances of the regular satellites. It is proposed that the satellites condensed from the gas rings one at a time, commencing with Iapetus which originally occupied a circular orbit at radius 11.4R~. As the temperatures of the gas rings T, increase with decreasing orbital size according as Tn 0~ l/R,, a uniform gradient should be evident amongst the satellite compositions: Mimas is expected to be the rockiest and Iapetus the least rocky satellite. The densities predicted by the model coincide with the Voyager-determined values. Iapetus contains some 8% by weight solid CH,. Titan is believed to be a captured satellite. It was probably responsible for driving Iapetus to its present distant orbit. Accretional time-scales and the postaccretional evolution of the satellites are briefly discussed.

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