“…In a highly active comet, all of the overlaying dust may be blown off the surface, but for most comets, some of the dust will remain behind, building up over time to form the insulating mantle. As the gas flow is restricted (as little as 1 cm of mantle can reduce emission by a factor of 10 Ibadinov, 1999;Ibadinov and Rahmonov, 2002;Skorov et al, 2002)), even more dust will remain behind, further cutting of the activity. This is a self-limiting process, because eventually the layer gets thick enough to shut off activity altogether.…”