Lay flat and try to spread you weight out as much as possible . Carefully try to to wiggle your way back to thicker ice. Yell for help . Pray .
Crevasses.
The ice expands in the crack and may split the rock, as will eventually the roots of a plant.
Icebergs calving off the Antarctic ice sheet is a normal phenomenon that has occurred for eons and will continue to occur. The weight of ice on the continent forms glaciers that push the ice sheets out over the ocean. In recent years warming waters are undermining the ice shelves at the point where they reach the sea. This is known as basal melting.
Most of the time it is a good thing that ice expands. But sometimes water may get into cracks in streets and roads. If the water freezes, the pressure caused by the expanding ice can break the pavement. Then the holes and cracks are expensive to repair. And if we put a full bottle of soda into the freezer to get cold quick and then and then forget about it, we may find the expanding ice has shattered the bottle and ruined our treat.
Water goes in a cracks. When it gets cold it thaws and freezes. It also turns into a crystal form. Then it takes a lot of space and cracks a rock.
Ice naturally makes cracks when it is frozen. Not large cracks, but cracks. Water seeps in through these cracks and freezes them. The crack expands due to the frozen water, or new ice. The cycle continues over and over again until the piece of ice finally breaks.
Crevasses.
No way hose!
The ice expands, forcing the crack to widen. As an effect the cracks get bigger every time ice freezes inside. The thing with a crack eventually breaks.
Cracks in the ice sheet, which covers 98% of the continent, are called crevasses.
Ice wedging
Ice wedging
ice wedging
If rain water seeps into cracks in rocks, and becomes frozen, the water turns to ice. As the ice expands it can force the cracks wider, even splitting the rock in two.
Ice wedging is a form of mechanical weathering.
Ice makes cracks in rocks laeger as it expands
Frostwegging