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27 Cards in this Set

  • Front
  • Back

% of freshwater that is frozen

77%

Glaciers classified by 3 things

morphology


flow dynamics


thermal properties

Glacial mass balance

balance between inputs/outputs of snow, ice and water




bm = accumulation - ablation




bm> 0 , growth, advancing terminus


bm < 0, shrinking, retreating terminus

terminus

end of the glacier at any given time

4 types of materials in glacier

snow


firn (between snow and ice) - granulated crystals


impure glacial ice (has air in it)


true glacial ice (no air in it)




density goes top to bottom, cause intuition

glacial ice formation

1. snow survives summer


2. more snow falls, compacts previous years snow


3. repeat until yous got a glacier

glacial flow - 3 types

basal sliding - sliding at base, warm glaciers only, sporadic




plastic flow - typical flow lol




shearing- shear movement along fractures

firn line

basically the snow line on mountains, but glaciers

accumulation zone

area where snow is accumulating, is above the firn line

ablation

loss of mass due to: melting, sublimation, and deflation

deflation

erosion due to wind blowing things away

ice flow as geomorphic process

scours/ erodes rock


traps other rocks and stuff and bull dozes stuff and drags along the surface of things

cirques

amphitheater shaped basin at the head of an alpine glacier

erosional landforms

horns


aretes


u shaped valleys


grooves/striations


roche moutonees



horns

formed from several cirques gouging a peak

aretes

formed from erosion on both sides

u shaped valleys

glacier going hella deep then retreating, and having a stream running through it helps

roche moutonees

asymmetric slope of bedrock - steep on one side, not so much on the other

depositional landforms

glacial outwash plain


moraines


eskers


drumlin


kettle lakes


erratics


proglacial lakes

glacial outwash plain

basically a braided stream from glacier run off

moraines

when glaciers deposit rock they were carrying




terminus moraine - furthest advance


recessional - built while terminus recedes


lateral- on the side of a moraine


medial- between two glaciers that be moving beside eachother

eskers

long curving ridge of gravel that forms by filling up stream channel in a glacier

drumlin

hill of unsorted till, shaped like a mini sperm

kettle lakes

ice that was penetrating the ground, melts and fills with water

glacial erratics

carries a rock hella far and leaves it there like hey dude you can stay here please

proglacial lakes

formed by the damming action of a moraine or ice dam

things that erosional/depositional land forms tell us

reveal past flow rates and ice extent