Glaciers melt via
vaporization thermal conduction Water expanding colder temperatures mountain sources internal combustion decreased wind Physical weathering
A B C D E F G H
When the glacier moves into warmer areas the ice melts and sediments are deposited.
glaciers melt via thermal conduction
Glaciers melt via (A) vaporization (B) thermal conduction (C) Water expanding (D) colder temperatures (E) mountain sources (F) internal combustion (G) decreased wind (H) Physical weathering