powerpace
Platinum Member
Almost missed this one. The actual Glacier Ice does not mix and churn. It flows as a continuous mass.
But surely does mix, churn and bulldoze the strata's it travels over. Just think of all the lateral and terminal moraine or float deposited along the glaciers path.
The shelf ice is probably made up of mostly fresh glacier melt water that is of lower density than the seawater and will freeze at higher temperatures than saline seawater. All that cold fresh meltwater may also muck up the normal current flows and when that happens th Merry Breezes may be angered into deviant behaviour.![]()
If you have ever seen a glacier the streaks in the ice are sections of the flow traveling at different speeds. The center of the flow travels fastest. The uneven travel speed creates crevasses. Opening and closing at different travel speeds.
The meltwater is minimal in the Antarctic, only occurring in small areas along the coast. The pack ice is seawater that gradually loses most of the salinity during the freezing cycle.. Your right about the aberrant ocean current. The currents coming into the coastal areas melt large areas of the ice every year. Wind has an affect on the ice movement.