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 .
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.
The cracks in an ice glacier are called crevasses. They form due to the movement of the glacier over uneven terrain, causing the ice to fracture and crack. Crevasses can be dangerous to climbers and hikers as they can be deep and difficult to see.
The ice expands in the crack and may split the rock, as will eventually the roots of a plant.
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.
In the cycle of ice wedging, water seeps into cracks in rocks during warm periods, freezes and expands when temperatures drop, putting pressure on the cracks, widening them. This repeated freeze-thaw cycle causes the rock to break apart over time, leading to the formation of progressively larger cracks and ultimately the breakdown of the rock into smaller fragments.
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.
No way hose!
Ice cracks when put into water because the sudden change in temperature causes the ice to contract and expand rapidly, leading to stress on the ice structure and resulting in cracks forming.
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.
Ice wedging
Ice wedging
Cracks in the ice sheet, which covers 98% of the continent, are called crevasses.
Ice wedging is a form of mechanical weathering.
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.
The process by which ice widens and deepens cracks in a rock is called frost wedging. This occurs when water seeps into the cracks in the rock, freezes, and expands, causing the crack to widen and deepen over time.
The general term for this is "erosion".
Frostwegging