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49 Cards in this Set
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Bubble Rock!! Acadia Maine
It was the result of a glacier << concluded by The Father of Glaciology aka Louis Agassiz |
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.....and how was it placed up there?! |
L. A.
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How does snow become ice?
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packs together, b/c gravity, less and less % air
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4 steps
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continental glacier aka ice sheets
--1 mill sq miles --upsidedown bowl --flows outward in all directions fr center |
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flows outward in all directions fr center...
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ice shelf
--when a continental glacier reaches and spreads out over the ocean |
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look at the pic
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iceland--Vatnajokull
ice cap |
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iceland
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alpine/valley/mountain glacier
--confined to a valley --ie Mt. Ranier |
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3 diff names!
morraine stripes |
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Piedmont glacier
--a valley glacier that reaches the valley floor and spreads out |
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it peed everywhere
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tidewater glacier
--a valley glacier that ends in a lake or ocean |
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it meets the tide
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snowline?
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elevation above which snow remains year round
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glacial movement--how?
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Gravity!! they move b/c their own weight
--sliding on meltwater layer on base above bedrock --sliding is much faster than internal flow --valley glacier--downhill, stakes.. |
sliding on what?
moves bc of what? |
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crevasse
--a crack in the ice due to the uneven movement of a glacier --only found to a depth of 165 ft, above the plastic flow |
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due to ___ movement of a glacier
only found to a depth of ___ above ____ |
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cirque
--bowl-shaped depression at the head of a glacial valley |
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at the head
b...shaped |
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arete
--sharp edged ridge --created when 2 cirques are located back to back |
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ridge
starts w an "a" |
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col
--an arete that takes on a saddle shape --caused when 2 cirques begin to erode backwards and begin to connect |
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saddle
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horn
--a pyramid shaped peak created by the presence of 3+ cirques |
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pointy!
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Glacial valleys/troughs
--u-shaped ie Doubtful Sound, NZ **can have hanging valleys (waterfalls) --on the sides: cirques w aretes and horns + tarns(pools of water) + pater noster lakes (leading into streams) --v-shaped bf glaciation, fills w snow, then u |
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fjord
--flooded glacial valley |
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starts w "F"
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nunatak
--a mtn peak that sticks out of a glacier |
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it attacks fr within the glacier!!
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erratic
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any boulder moved by a glacier
ie bubble rock |
ie bubble rock
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morraines
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-a mound, ridge, or other distinct accumulation of glacial till; often pushed
1.medial 2lateral 3 ground 4end (terminal and recessional) |
till
4 types |
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medial morraine
--form where glaciers join --debris mostly on top of ice --may b many in a very large glacier |
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mm
join |
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lateral morraine
--debris that accumulate along the sides of a glacier + deposit along these margins |
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ground moraine
--when a valley glacier melts completely away, the debris carried on or w/in it are dropped on the valley floor, creating a deposit--gr moraine --has NO distinct morphology |
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no distinct morphology
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end moraine
TERMINAL: marks the farthest forward progression of a glacier RECESSIONAL: are created when a glacier ahs begun to recede, but then moves forward again w/o ever reaching its furthest point |
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ogives
--alternating bands of light (winter) and dark (summer) ice that form ridges and swales at the base of some falls |
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light vs dark
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ablation hollows
--irregular features created in the surf of a glacier due to differences in wind and temp on the glacier's surf |
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cryoconites
--during the day the black rock absorbs heat and melts the glacial ice, causing the depression |
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rock >>depression
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sun cups
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sun cups
--ablation hollows that develop during intense sunshine |
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penitents
--due to extreme relief of ablation hollows found at most often high altitudes in the tropics --they're created as a result of differential snow ice evap and sublimation rates --spikes of snow <<resemble repetent souls |
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repetent souls
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moulin
--a nearly vertical channel thats formed by flowing water --if u fall in goodbye! |
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channel like a mole
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rock/glacial flour
--rock that has been pulverized by the grinding of glaciers glacial milk --when rock flour mixes w water |
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striations
--lines made in rock by stones beneath the glacier scratching the rock's surf as the glacier moved --they indicate the direction the glacier was moving |
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scratching
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Grooves
--deep striations, made by rocks underneath the glacier |
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deep s___'s
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chatter marks + crescentic gouges
--caused by short, abrupt movement |
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Roche Montonnee (Sheepback)
--plucking on one side>rough (lee) + abrasion/ice polishes the other surf side |
sheepback mtn
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Drumlins
--gen grouped together --lee slope is more gentle --made of till |
hills
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Kame
--a cone shaped deposit of sediment, formed by a river flowing over the surf of a glacier into a crevasse |
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Kame
--a cone shaped deposit of sediment, formed by a river flowing over the surf of a glacier into a crevasse |
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Eskers
--a winding ridge of sedm material (us. gravel or sand) deposited by streams that cut channels under or thru the glacier ice |
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winding ridge
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till
--any material carreid by a glacier and dropped on land (unstratified) |
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stratified drift
--any material deposited by a glacier in water --layers!! |
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dep in wataaa
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varve
--couplets of sedm layers indicating cyclic deposion --thick/light = sand/summer thin/dark = clay/winter |
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couplets
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outwash plains
--that area at the end of glacier where meltwater flows and deposits sediment |
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at the end of a glacier
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Pater noster lakes
--our father, rosary beads --a series of lakes connected by streams |
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rosary beads
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moraine damned lake
--a glacial lake damned by a moraine |
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damned
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kettle pond
--kettles that fill in w water --icebergs get buried by outwash, then melt |
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kettle pond
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kettle pond
--kettles that fill in w water --icebergs get buried by outwash, then melt ie walden pond |
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kettle pond
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cirque lake aka tarn
--cirque fills in w water |
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lake in a cirque
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calving
--when a glacier reaches the ocean or any large body of water and large pieces of the glacier break off |
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