Types:
Cirque glacier: a glacier that has carved a cirque and is wholly
contained within the cirque.
Cirque: an amphitheatre-shaped depression scoured by a glacier into the side of a mountain.
Horn: A mountain peak between 2 or more cirques. Example: The Matterhorn
Arete: A knife-edge ridge between two cirques, usually connecting 2 horns.
Tarn: a lake occupying a cirque.
Alpine or valley glacier: a glacier originating in a cirque or
high altitude snow field that flows within a pre-existing valley. Glacial
erosion greatly modifies the valley into a characteristic U-shaped valley.
Piedmont glacier: A glacier formed by the coalescing of valley glaciers that flowed onto the
pediment, a flat low-lying erosional surface at the foot of a mountain range.
Piedmont glaciers were important in forming ice sheets in the U.S. western
interior during the Pleistocene (epoch of geologic time of the most recent
ice ages).
Ice Sheet: A thick, extensive body of glacial ice that is not
confined to valleys. Ice sheets cover an area 106 to 107
square kilometers. Ice flow is radial from the centers of ice domes that
merge to form an ice divide. Modern examples include Greenland and the
East and West Antarctic Ice Sheets of Antarctica.
Ice Cap: A thick, extensive body of glacial ice that is not confined
to valleys. Ice caps cover an area 102 to 104 square
kilometers. Ice flow is radial from the center of 1 or more ice domes that
may merge to form an ice divide. Modern examples include the Barnes and
Penny Ice Caps on Baffin Island, ice caps on Spitsbergen, and Vatnajokull,
Hofsjokull, Langjokull, and
Myrdalsjokull ice caps on Iceland.
Ice Shelf: a floating glacier derived from a land based ice sheet. An ice shelf is thick enough to have internal flow, but is over water. Modern examples include the Ross and Ronne/Filchner Ice shelves in Antarctica.
C.f. Pack Ice = frozen seawater that is not a glacier, but seasonally covers most of the Arctic ocean, and large portions of the South Atlantic, South Pacific, and Southern Indian oceans surrounding the continent of Antarctica.
Outlet glacier: a segment of a continental glacier (ice cap
or ice sheet) that advances rapidly through a mountain pass.
Ice Stream: A linear zone within an ice sheet, measured in 10's
of kilometers across and 100's of kilometers in length, that is flowing
significantly faster than the surrounding ice.