Geob 103 topic 9

42 cards

Glaciers


 
  
Created Apr 18, 2012
by
mendonca_liera

 

 
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1
Glacierstwo types?
 
A large mass of perennial ice resting on land or floating on waterAlpine Glaciers on mountains...
2
When and how to glaciers formHow do they move
 
when snow accumulation>snow melt, compaction and pressure increases with depth, increasing...
3
Alpine glaciersContinental
 
narrow and thin and there are four types: valley, cirque, piedmont and tidewaterunconfined...
4
Valley glaciersCirque Glaciers
 
Rivers of ice confined in valleys which transport debris downstreambowl shaped pit located...
5
Piedmont GlaciersTide Water
 
Glaciers formed by coalescing valley glaciersglaciers which end in a body of water
6
Ice SheetsIce caps
 
Most extensive form (50,000km2 in area) Round domes that cover peaks
7
Ice fieldsIce shelvesice front
 
Not enough ice to cover peaks and does not form domeice sheet attached to land, extends over...
8
Conversion of snow to iceFirn
 
fresh snow doesnt have a lot of density, over time porosity decreases and density increases,...
9
Accumulation zoneEquilibrium lineAblation Zone
 
upper part of glacier where accumulation>abalationseparates two zonesabalation>accumulation...
10
Glacier mass balanceWhy do Glaciers move?
 
Change in mass of glacier over time= total accumulation-ablationWeight and flow
11
WeightFlow
 
ice at depth is under a lot of pressure which forces ice to spread outice is slippery and flows...
12
What does glacier velocity depend onin general what is glacier velocity like
 
distance from bed and valley, steepness and free water at the bed providing lubricationfaster...
13
Supraglacial meltwaterMoulin
 
water flow on top of glaciersupraglacial melts a vertical tunnel through ice
14
Subglacial meltwaterWhat are the functions
 
water below the glacier generated in two ways: at the surface and flows through moulin or tunnels...
15
Ice pluckingPlucking
 
a way erosion can take place where the glacier acts as a bulldozer capable of pushing a limited...
16
AbrasionEvidence of Abrasion
 
Rocks held by ice scrape and grind over bedrockpolish, striations, grooves
17
Factors which influence abrasion
 
Amount of debris, basal sliding velocity, ice thickness , hardness of bedrock, basal water...
18
Cirquearete
 
semi-circular shaped bedrock formed when glacier scours back to mountainsharp-edged bed rock...
19
ColHorn
 
low areas or passes that once had glaciers on either sideThree or more cirques adjacent to...
20
TarneWhat does the shape of a cirque depend on
 
A small lake that occupies a rock basin in a circque or glacial trough-shape before-level of...
21
U-shaped trough fjord
 
formed by glacier that has retreated and could be occupied by streams or lakes but also alluvium...
22
What do glaciers move
 
loose fragmented rock: either eroded or deposited by glacial advancesRocks that fall-in from...
23
What is some evidence of glaciation
 
striations, polished bedrock, erratic: different sized boulders and different rock than surrounding,...
24
Lodgement tillAblation till
 
deposited under the ice consisting of clay and is compacted by ice on topDeposited in front...
25
Moraineground moraine
 
glacially-deposited sediment piles or landformsdeposited under the glacier
26
lateral moraineMedial moraine
 
pile-up along side glaciermaterial in middle of glacier (two laterals come together)
27
End morainerecessional moraine
 
occurs at the ice front marks the farthest advance of the glacierslow retreat of terminus leaves
28
Drumlin
 
Depositional feature of moving ice which is a low oval hill made of tillupstream side is steep,...
29
ESker
 
depositional feature of stagnant ice which is a narrow ridge of coarse sand and gravel formed...
30
KettleKame
 
steep-sided hole formed by gradual melting of an ice block left behindany stratified ice deposit,...
31
OutwashIce contacted stratified drift
 
depositional plain of  stratified driftdeposited by meltwater in contact with ice
32
roche mountonnees
 
striated on the stoss (up side) and plucked on the leeward side
33
Peri-glacial
 
climate and geomorphology of cold regions. Lanscapes along the margins of past and present...
34
Frost actionFrost heavingFrost thrusting
 
as water expands when it freezes it breaks a part rock and soilvertical movement of rock and...
35
PermafrostContinuousDiscontinuous
 
ground frozen for more than two yearsall areas frozen except under rivers and lakesslopes facing...
36
Active layertalik
 
Seasonally unfrozena pocket or region within a permafrost which is unfrozen
37
Patterned groundIce Wedges
 
Stone polygon nets (produced by frost heaving), circles or netsvertical body of ice penetrating...
38
Thermokarst lakesPingo
 
Lakes formed in depression as permafrost thaws, causes CH4 to be released Heaved, circular...
39
Ice ageGlaciation
 
series of glaciations and interglaciations spanning 1-3 million yearsPeriod of cold where glaciers...
40
interglaciationsDeglaciation
 
warm phasewidespread recession during a warm period
41
causes of ice age
 
earths orbital variations (Milankovich cycles) axial wobble (precession of equinox) and axial...
42
What was the name of our last glacier (in Canada)
 
cordillera ice sheet 15,00 yrs ago

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