Surfaces can be freshly fractured or smoothly melted below old waterlines:

Icebergs are pieces broken from glaciers, which are ancient compressed snow, white from the trapped air bubbles. Cracks that fill with meltwater freeze into translucent blue ice.

I guess the ice layers in the glacier must vary in hardness, so they can melt into something like this:

Meltwater can form underground rivers through glaciers that become iceberg caves:

This one has embedded flat dirty layers that I assume were originally deposited on the surface of the glacier; I'd love to learn more about it:

See the full gallery for more bergs and larger versions: http://www.pbase.com/plbh/greenland_2003 -- Peter