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34 Cards in this Set

  • Front
  • Back
a moving body of ice on land that flows downslope or outward from an area of accumulation
glacier
confined to mountain valleys where they flow from higher to lower elevation
valley glacier
vast, covering at least 50,000 km2 and are unconfined by topography
continental glacier
all glacial activity including the origin, expansion, and retreat of glaciers as well as their impact on earth's surface
glaciation
what is glacial ice composed of?
90% solids 10% air
partially thawed refrozen accumulated compacted snow
firn
a type of permanent deformation involving no fracturing
plastic flow
sliding over underlying surface
basal slip
a balance sheet of expansion and contraction in response to accumulation and wastage
glacial budget
addition exceed losses/ always snow covered
zone of accumulation
losses from melting, sublimination, and carving of icebergs exceed rate of accumulation
zone of wastage
a short lived episode of accelerated flow in a glacier during which its surface breaks into a maze of crevasses and its terminus advances noticeably
glacial surge
when glaciers shove or push unconsolidated material in its path
bulldozing
glacial ice freezes in the cracks and crevasses of a bedrock projection and eventually pulls it loose
plucking
bedrock over which sediment laden glacial ice moves is eroded and developes glacial polish and striations
abrasion
long, steepwalled embayments
fiord
a tributary valley whose floor is at a higher level than that of the main valley
hanging valley
steep wall/ bowl shaped depressions
cirque
narrow, serrated ridges
aretes
steep walled, pyramidal peaks formed by headward erosion of cirques
horns
a general term for all deposits resulting from glacial activity
glacial drift
rocks derived from a distance source but move with glaciers
glacial erratics
sediments deposited by glacial ice directly
till drift
layered and invariably exhibits some degree of sorting by particle size
stratified drift
any sediment transported within a stationary glacier that is dumped at glaciers terminus
end moraine
till deposited as ice melts in a later on ground
ground moraine
deposited till if ice front has receded
recessional moraine
outermost end moraine
terminal moraine
sediment deposited along margin
lateral moraine
continental glaciers deposit till in the shape of elongated hills
drumlin
blanket of sediment in streams flowing from glacier
outwash plain
long narrow deposits of stratified drift
valley train
conical hills of stratified drift
kames
long sinuous ridges of stratified drift
esker