ICE SHEETS
GLACIER ELEVATION/ICE SHEET ELEVATION
GLACIER FACIES
ICEBERGS
GLACIER THICKNESS/ICE SHEET THICKNESS
FIRN
ICE SHELVES
BASAL SHEAR STRESS
GLACIERS
DEPTHS AT SPECIFIC AGES
GLACIER MOTION/ICE SHEET MOTION
COASTLINE
BASINS
2015-05-01 15:50:51.0 [aaleman] Insert Concept add narrower relation (GLACIERS/ICE SHEETS [8603db51-3484-4439-8b3b-a06f48e8c686,83513] - AGE OF INTERNAL REFLECTIONS [9ce536e1-06c8-4817-af5f-b625cfe571a7,157911]);
2015-05-01 15:51:16.0 [aaleman] Insert Concept add narrower relation (GLACIERS/ICE SHEETS [8603db51-3484-4439-8b3b-a06f48e8c686,83513] - AGE AT ICE-THICKNESS-NORMALIZED DEPTHS [ab4b800d-820f-40cc-bb01-4e8835368d04,157915]);
2015-05-01 15:50:18.0 [aaleman] Insert Concept add narrower relation (GLACIERS/ICE SHEETS [8603db51-3484-4439-8b3b-a06f48e8c686,83513] - GEOMETRY OF INTERNAL REFLECTIONS [ab319cdf-a34c-446c-9fc0-27605048364e,157907]);
Glaciers are masses of land ice, formed by the further recrystallization of firn, flowing continuously from higher to lower elevations. Ice sheets are a continuous sheet of land ice that covers a very large area and moves outward in many directions. This type of ice mass is so thick as to mask the land surface contours, in contrast to the smaller and thinner highland ice. The continental glacier of Greenland is sometimes called the Inland Ice. This term is often used to describe the great ice masses that characterized the ice ages.
GLACIERS/ICE SHEETS
ABLATION ZONES/ACCUMULATION ZONES
AGE OF INTERNAL REFLECTIONS
GLACIER MASS BALANCE/ICE SHEET MASS BALANCE
GEOMETRY OF INTERNAL REFLECTIONS
AGE AT ICE-THICKNESS-NORMALIZED DEPTHS
GLACIER TOPOGRAPHY/ICE SHEET TOPOGRAPHY
CRYOSPHERE