Accretion of Ornamental Equatorial Ridges on Pan, Atlas and Daphnis
Alice C. Quillen, Fatima Zaidouni, Miki Nakajima, Esteban Wright

TL;DR
This paper investigates how ornamental equatorial ridges on Saturn's moons Pan, Atlas, and Daphnis could have formed through accretion from ring material, considering physical constraints and orbital dynamics.
Contribution
It introduces models for ridge formation via ring accretion, accounting for moon shape, orbit, and ring gap asymmetries, providing explanations for observed ridge features.
Findings
Accretion is feasible within tidal torque limits.
Asymmetric gaps can produce ridges with depressions or lobes.
Orbital resonance may facilitate ridge growth.
Abstract
We explore scenarios for the accretion of ornamental ridges on Saturn's moons Pan, Atlas, and Daphnis from material in Saturn's rings. Accretion of complex shaped ridges from ring material should be possible when the torque from accreted material does not exceed the tidal torque from Saturn that ordinarily maintains tidal lock. This gives a limit on the maximum accretion rate and the minimum duration for equatorial ridge growth. We explore the longitude distribution of ridges accreted from ring material, initially in circular orbits, onto a moon that is on a circular, inclined or eccentric orbit. Sloped and lobed ridges can be accreted if the moon tidally realigns during accretion due to its change in shape or because the disk edge surface density profile allows ring material originating at different initial semi-major axes to impact the moon at different locations on its equatorial…
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