Processes (especially melting) by which a glacier loses ice and snow: melting, evaporation, calving, and erosion. The area of a glacier where ablation occurs.
Accumulation, Accumulation zone
Process (especially snowfall and compression) by which a glacier gains snow and ice. The area of a glacier where accumulation occurs.
Arete
Sharp, narrow ridges formed on a mountain by a glacier.
Basal Slip
The sliding of a glacier over its bed.
Bedrock
The solid rock under a glacier or ice sheet.
Boulder
Also called, "erratic boulder." Large boulders are sometimes left behind when a glacier recedes or retreats. Illustration by Amy Stubsjoen
Calving
Cows have calves, glaciers calve icebergs, which are chunks of ice that break off glaciers and fall into water. From Animation by Dorothy Hall
A large accumulation of many years of snow, ice, rock, sediment and water that originates on land and moves down slope under the influence of its own weight and
gravity. Photo by Alaska Geographic Society
The very finely ground particles of rock, silt, or clay created by a glacier when its rock-filled ice scrapes over bedrock and which flow out from beneath a glacier in the meltwater. Photo by Dr. Bruce Molnia, Alaska Geographic Society
Jumbled and broken ice which forms when a glacier flows over a steep drop-off.
Ice Sizzle
A crackling or sizzling sound, similar to soda or Rice Krispies, that is produced by an iceberg while it is melting. The sound is caused by the release of air bubbles
that were trapped in the glacier ice during its formation under high pressure. This is also called "bergy seltzer." Computer Graphic by Donna Sandberg
Ice worms are the only earthworms known to inhabit snow and ice. They thrive in temperatures just above freezing.
Illustration by Donna Redhead
Electron Scanning Micrograph, Wergin & Erbe
Interglacials
The relatively warmer periods between each ice age when the ice sheets retreat.
Isostatic rebound
Land that was once pushed down by the heavy weight of glacial ice may experience actual rising at the small rate of about a centimeter per year after the ice melts
away. Photo by McMillan
The result of a very large block of ice being left behind as a glacier recedes. The melting forms potholes which are sometimes filled with water in a glacier, till, or outwash plain. Vegetation may grow up around kettles.
Photo by James Roush
Photo by McMillan
Lateral Moraine
A large mass of glacial material on the sides of a glacier.
Mass Balance
The difference between the amount of material that a glacier accumulates and the amount lost during ablation is called its mass balance. The equilibrium line moves down (1) or up (2) a glacier as the mass balance changes.
Medial Moraine
A central moraine formed where two glaciers join to form a large glacier.
Meltwater
Water produced by melting glacier ice, firn, and surface snow. Meltwater flows down the bed of the glacier and emerges from the end as a stream often colored gray-green by the rock flour it contains. Photo by James Roush
Metamorphic
Something that undergoes changes in structure or composition, texture, or internal structure by (for glaciers) heat or pressure.
A hole or tube in a glacier into which water flows. Moulin is French for mill, so called because of the loud, roaring noise made by the falling water. Photo by James Roush
A short period when a glacier can go as much as one hundred times faster that it normally goes. This happens when a glacier slides downstream on water trapped beneath
it.
Surge Front
The leading edge of the wave or bulge of moving ice which represents the surge before it reaches the terminus of the glacier.
Tarn
A small lake filling a hollow which was eroded out by ice or dammed by a moraine. Frequently found with cirques.