Glaciers, Glaciation & Permafrost Flashcards

1
Q

How does glacial ice form – on Earth? On Mars?

A

On Earth- Snow accumulates, compacts, melts and
refreezes - changes into firn; firn melts, compacts, and refreezes further and transforms into ice. Ice needs time to form. The forst step is glacier ice

On Mars- Ice is not just composed of water. It is completely different to ice on earth. It depends on the tilt of the axis

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2
Q

Where have glaciers been identified on Mars?

A

At the poles

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3
Q

How does glacial ice move? What factors affect rates of glacier movement?

A
  • Gravity makes ice move
  • Ice moves in responce to stress
  • Movement or deformation of ice is called strain
  • Ice moves the fastest in the center at the top
  • friction of sides and bottom slow down movement there which is why the midle and top are faster
  • not constant in velocity or speed
    Types of movement: basal sliding, internal deformation, crevassing
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4
Q

What is a glacier budget?

A
  • relationship between gain and loss of mass
  • If more mass GAINED: positive buget and glacier terminus will advance
  • if more mass LOST: negative budget and glacier terminus will retreat
  • Mass gained in the accumulation area. zone of accumulation is usually up slope, new mass gained
  • Mass lost in the ablation (wastage) area. Lost ice goes right to evaportation (skips melting)
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5
Q

How do we classify glaciers? What communities/regions are most impacted by
rapid glacier retreat?**

A
  • continetal ice sheet
  • ice cap
  • outlet glacier
  • valley glacier
  • pidemont glacier
  • cirque glacier
  • ice shelf
  • communties on the ocean front are most impacted by glacier retreat because rising water levels. andes impacted
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6
Q

What processes are involved in glacial erosion and glacial deposition?

A
  • abrasion: debris in ice dragged across substrate; form striations (scratches), smooths the rock. Smoothed and streamlined landforms are formed for example, roche mountonee, whaleback. abrasion creates shapes stones (faceting) which are bullet-shaped boulders with a pointed end and a blunt end; this reduced grain sixe and produces silt
  • occurs on bedrock, not made of sediment
  • glacier erosion occurs at the base. Clean ice does not erode, it needs and abrasive device
  • erosion by plucking which is debris released by fracturing of bedrock; frozen into glacer bed
  • water seeps into cracks, freezes, and, mechanically breaks up the bedrocks. These fragements are plucked out by the glacier. Pressure causes change in melting point
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7
Q

What features of a landscape indicate cold climate conditions?

A
  • glacier landforms (U-shaped valleys, cirqures, moraines)
  • permafrost
  • tundra ecosystem (low-lying vegatation, polygons)
  • Alpine Glacial Features (horns, arrets, cirque lakes)
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8
Q

Firn

A

snow which has survived a summer melt season and has begun to change into ice

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9
Q

basal sliding

A
  • requires water at ice base
  • need ‘warm’ ice
  • e.g. Alaska, Rockies
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10
Q

internal deformation

A

ice deforms as a plastic material

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11
Q

crevassing

A
  • upper surface of ice is brittle
  • fractures, or crevasses form to allow movement
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12
Q

how quickly does glacier ice move

A

3 to 300m/year

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13
Q

where are the fastest glaciers found

A
  • Alaska, Rockies
  • ‘warm’ glaciers where ice is close to 0C
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14
Q

where are the slowest glaciers found?

A
  • Antarctica
  • Cold Ice
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15
Q

Ogives

A
  • dirt bands in ice
  • show differential movemen
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16
Q

ablation

A

dirty ice, old, downslope

17
Q

equilibrium line (snow line)

A
  • Point on the glacier where there is neither gain or loss of mass
  • will move for places with seasion, ex. closer to ablation in summer
18
Q

what determines how quickly ice moves?

A
  • slope of glacier
  • ice thickness
  • Temperature
  • Valley geometry
  • Bedrock conditions
  • Subglacial hydrology
19
Q

how does ice flow?

A
  • ice flows from accumulation area to abaltion area
  • never flows “backwards”
    -ex. south casacde glacier washington- ice front has retreated due to increased melt, it has not flowed backwards
20
Q

contiental ice sheet

A
  • bigger than 50000km^2
  • Antarctica
  • greenland,
  • lauerntie ice sheet (used to be on top of hamilton 1200-1400 years ago)
21
Q

ice caps

A
  • smaller than ice sheets (less than 50000 km^2)
  • often in mountainous areas
  • ex. vatnajokull, iceland, southern patagonian ice field.
  • Martian ice caps fall under this
22
Q

outlet glacier

A
  • radiate from the edge of an ice cap
  • ex. breiamerkurjokull, iceland
  • there are lots around the world
23
Q

valley glacier

A
  • flow in bedrock valleys
  • ex. athabasca glacier (this one is melting which is alarming)
24
Q

pidemont glacier

A
  • valley glaciers that extend out onto lowlands
  • ex. malaspina glacier, alaska
25
Q

cirquce glaciers

A
  • occupy small, semi-circular hollows in mountainous reigions
  • ex, rockies, alps
26
Q

ice shelf

A
  • floating part of ice sheet or ice cap
  • ex. ross ice shelf, antarctica
  • they are evicence that we can see melting
27
Q

ice field glacier

A
  • relatively flat expanse of glacial ice that covers a mountainous area, often feeding multiple glaciers
28
Q

tidewater glacier

A
  • an outlet glacier that flows into the ocean
29
Q

rochee mountee

A
  • A glacially eroded asymmetric hill that becomes
    elongate in the direction of flow; glacial rasping smooths the upstream part of the hill into a gentle slope, while glacial plucking erodes the downstream edge into a steep slope
30
Q

whaleback

A

A streamlined rock knob with symmetrical longitudinal profiles caused by abrasion of both stoss and lee sides