Originally Posted by
kunes
In northern climates the warmest water in the lake is sometimes found on the bottom. Like most substances water becomes denser as it becomes colder. However this only occurs until the water reaches 39 degrees, at which point it starts to become less dense for some reason. That's why ice floats on top of warmer water.
Just in case someone is itching for a simple explanation as to why ice floats, here goes....
I recall from my chemistry classes that the crystal structure for water changes as it gets very cold. The crystal structure for ice takes slightly more space (is less dense) than the crystal structure for warmer water. The two crystal structures are face-centered-cubic (FCC) and body-centered cubic (BCC). I can't recall which one ice is. I think it is BCC. The energy level of the water molecules determine the crystal structure.
Keith
2008 NWR Bash Crappie Champion
2010 NWR Bash Yellow Perch Champion
2010 Buggs Bash Smallest Crappie Award