We examine various mechanisms of erosion on Titan and their likely eff
ect on Titan's geomorphology. Specifically we evaluate the solubility
of likely crustal ices (water and ammonia) in liquid methane and ethan
e, and compare these with the solubility of rocks on Earth. Aeolian an
d diurnal weathering can be neglected, and glacial erosion is unlikely
unless the atmosphere has frozen out in the past. Erosion due to rain
fall is at most comparable to periglacial environments on Earth. We fi
nd that additional laboratory experiments are required if Cassini obse
rvations are to be adequately interpreted. (C) 1996 Academic Press, In
c.