Glaciers and ice ages Flashcards

1
Q

What evidence was found for glaciation?

A

erratics: fine sediment of large boulders found 100s of km in local bedrock
unsorted sediments

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2
Q

what are glaciers?

A

thick masses of recrystallized ice. last all year long. flow via gravity. cover about 10% of the earth.

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3
Q

when did the most recent ice age end?

A

11000 years ago. ice sheets were hundreds to thousands of metres thick.

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4
Q

is ice a mineral?

A

yes

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5
Q

how is snow transformed into ice?

A

can form slowly (thousands of years) or quickly (tens of years)
Snow is buried by later falls. Compression reduces volume. Burial pressure causes melting
and recrystallization. Snow turns into granular firn.
Over time, firn becomes
interlocking crystals of ice.

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6
Q

what conditions are necessary for glacier formation?

A

cold local climate (polar latitudes or high elevations)
lots of snow in winter and can’t all melt in summer

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7
Q

what are the two types of glaciers?

A

mountain and continental

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8
Q

describe mountain glaciers

A

flow from high to low elev in mountain settings

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9
Q

name and describe 4 types of mountain glaciers

A

cirque: fill mountain top bowls
valley: flow like rivers down valleys
mountain ice caps cover peaks
piedmont: spread out at end of valley

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10
Q

descrive continental glaciers

A

Greenland and Antartica
Vast ice sheets covering large land areas. Ice flows outward from thickest part of sheet.

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11
Q

what is basal sliding?

A

meltwater forms at base of glacier, it decreases friction and ice slides along substrate
movement of glacier

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12
Q

what is plastic deformation?

A

movement of glacier
occurs below, about 60m depth. grains of ice change shape slowly. new grains form while old grain disappear. crevasses form at surface, upper zone too brittle to flow

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13
Q

why do glaciers move?

A

gravity is strong makes ice flow.
glacier moves in the direction of its surface slope.
ice base can flow up a local incline.
In continental glaciers, ice spreads away from center of
accumulation. because
ice sheet always thicker in the middle, so it spreads
toward the edges.

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14
Q

what control’s a glacier’s rate of flow?

A

The severity of slope angle: steeper = faster
Basal water: wet-bottom = faster
Location within glacier:
faster in ice center, slower due to Friction at margins.

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15
Q

what is zone of accumulation vs of ablation?

A

accumulation: net snow addition
colder temps prevent melting, snow remains in summer
ablation: net ice loss
zones meet at equilibrium line

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16
Q

what is toe?

A

leading edge of a glacier

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17
Q

what are toe positions based on accumulation and ablation?

A

accumulation = ablation: stays in the same place
accumulation > ablation: advances
accumulation < ablation: retreat upslope

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18
Q

what are tidewater glaciers?

A

valley glaciers entering the sea

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19
Q

what are ice shelves?

A

continental glaciers entering the sea

20
Q

what is glacial abrasion?

A

a “sandpaper” effect on substrate
Substrate is pulverized to fine “rock flour” which abrades and polishes bedrock. Large rocks are dragged across bedrock gouge striations causing striations parallel to ice motion direction

21
Q

what are cirques?

A

bowl-shaped basins high on a mountain. form at uppermost portion of glacial valley. after ice melt, will become a tarn (lake)

22
Q

what is an arete?

A

a knife-edge ridge formed by 2 cirques that have eroded toward one another

23
Q

what is horn?

A

a pointed mountain peak. formed by 3+ cirques that surround the peak

24
Q

what are u-shaped valleys?

A

glacial erosion creates a distinctive trough. likeV-shaped fluvial valleys

25
Q

what are hanging valleys?

A

look at slide lol idk what this is

26
Q

what is glacial plucking?

A

Ice freezes around bedrock fragments and plucks chunks as glacier advances.
Forms asymmetric hill called a roche moutonée

27
Q

what is a fjord?

A

U-shaped glacial troughs flooded by the sea

28
Q

what can glaciers be compared with in terms of deposition?

A

large-scale conveyor belt. pick up, transport, deposit sediment. sediment transport always downhill

29
Q

what is moraine?

A

unsorted debris deposited at toe of a glacier

30
Q

what is glacial till?

A

sediment dropped by glacial ice. consists of all grain sizes. unmodified by water there4 unsorted, unstratified
accumulates beneath glacial ice, at toe of glacier, along glacial flanks

31
Q

what are erratics?

A

boulders dropped by glacial ice. rocks are different from underlying bedrock. been carried long distances in ice.

32
Q

what is glacial marine?

A

sediments from an oceanic glacier. melting icebergs drop stones into bottom mud

33
Q

what is glacial outwash?

A

sediment transported by meltwater. muds are removed, sizes graded and stratified, grains abraded and rounded. outwash dominated by sand and gravel

34
Q

what type of muds are formed in winter vs summer months?

A

winter: finest silt and clay
summer: coarser silt and sand

35
Q

what is loess?

A

“luss”
wind-transported silt.
fine sediments produced abundantly by glaciers. Strong winds over ice blow
the rock flour away, it settles out near glaciated areas as
loess deposits.
Deposits are unstratified and distinct in color.

36
Q

where are different types of moraines formed?

A

end: stable toe of a glacier
terminal: farthest edge of flow
recessional: retreating ice stalls

37
Q

what is ground moraine?

A

till left behind by rapid ice retreat. hummocky mostly flat land surface. kettle lakes form from stranded ice blocks

38
Q

what are drumlins?

A

long, aligned hills of molded lodgement till
steep up-ice; tapered down-ice
parallel to ice-flow direction

39
Q

what are eskers?

A

long, sinuous ridges of sand and gravel
form as meltwater channels within or below ice. channel sediment released when the ice melts

40
Q

what are consequences of continental glaciation?

A

ice loading and glacial rebound (ice sheets depress, rebounds after melting)
sea level rise and fall (fall when water stored on land, rise when water returns to oceans)

41
Q

lakes and glacial consequences

A

Gigantic proglacial lakes formed near the ice margin.
Pluvial features—large lakes formed during ice age. lakes where today’s deserts are

42
Q

what is unique about periglacial environments?

A

“near-ice”
year-round frozen ground (permafrost).
Freeze-thaw cycles generate unusual patterned ground

43
Q

approximately how many glaciations throughout earth history?

A

20 or more. 4 largest. indicated by fossil tills and striated bedrock

44
Q

what are causes of glaciation?

A

plate tectonics
atmospheric chemistry (changes in GHG concentrations)

45
Q

how do plate tectonics cause glaciation?

A

tectonics move higher latitudinally. uplift leads to absorbance of CO2 from atmosphere (and CO2 keeps Earth warm), blocking warm water flow.

46
Q

what is milankovitch hypothesis?

A

Earth climate variation predicted by orbital movements.
1. temp drops, glaciers form
2. glaciers grow, albedo cools more
3. temp warms, interglacial begins

47
Q

we have forestalled the next glaciation

A

human-induced warming
last 150 years, temperatures have risen and most mountain glaciers have dramatically retreated.
“super-interglacial”
period