Steam isn't "less dense" water it is effectively "gaseous" water. Ice is "solidified" water. you have to compare these things at a given temperature and pressure. if we are going to pretend "air" is pure oxygen for the benefit of this, it is only a gas because of the temperature and pressure are correct on earth. Lower the temperature far enough it becomes liquid, then solid. this is why water on the top of everest would boil at a lower temperature - theres less atmospheric pressure, so the water molecules can "escape" easier
Avogadro law, entrophy, sounds a bit like this thread and my tackle box (certainly entrophotic), good stuff though, I'm keeping out of this one, but what about the cryospheric accumulation and ablation?!
So Ian I take it you are now going to try and explain Ice And steam, and how they are the same density and viscosity, without being personal of course.
I think the difference is that there has to be a change of state(ie water to ice) before there is a change of density. Do you think anyones still reading this thread??