Glacier Mist

Glacier

A glacier is a persistent body of natural ice, a form of rock, that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It slowly flows and deforms under stresses induced by gravity, undergoing both ductile and brittle deformation, and acquiring distinguishing surface features, such as crevasses and seracs. As a glacier moves, it abrades underlying rock and debris to create glacial landforms, such as cirques, moraines, and fjords. Although a glacier may flow into a body of water, and can include ice shelves and ice tongues, it originates only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of freezing bodies of water.

Mist

Mist is a natural phenomenon caused by small droplets of water aerosols suspended in the cold air, usually by condensation. Physically, it is an example of a dispersion, most commonly seen where water vapor in warm, moist air meets sudden cooling, such as in exhaled air in the winter, or when hot sauna steam is suddenly released outside. Mist occurs naturally as part of weather, typically when humid air comes into contact with surfaces that are much cooler. It can also be created artificially with aerosol spray dispensers if the humidity and temperature conditions are right.

glacier

Noun

1. A large body of ice which flows under its own mass, usually downhill.
2. An area of a mountain where snow is present year-round.

mist

Noun

1. Water or other liquid finely suspended in air.
2. A layer of fine droplets or particles.

Verb

1. To form mist.
2. To spray fine droplets on, particularly of water.