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Glacial Ice

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Title: Glacial Ice


1
Glacial Ice
  • Lecture Outline
  • Introduction to glacial geology
  • Water
  • Ice as a mineral
  • Ice as a rock
  • Metamorphism of snow
  • Snow hazards and resources

2
Introduction to Glacial Geology
  • We live in an interglacial period
  • Ice covers 11 of continents
  • Outside of glaciated areas 11 of earth is
    permafrost
  • 12 of surface water is frozen
  • Ice in atmosphere
  • Global changes of just a few degrees one way or
    other can move earth into interglacial period or
    ice age

3
Introduction to Glacial Geology
  • Glacial studies
  • Sensitive recorder of paleoclimates
  • Sensitive indicators of current climate change
  • Significant portion of earths surface has been
    modified directly/indirectly by glaciers

4
Introduction to Glacial Geology
  • Glacial studies
  • Glaciology How glaciers form and behave
  • Glacial geomorphology
  • how glaciers and glacial meltwater erode,
    transport, deposit sediments
  • Landforms created by glaciers and glacial
    meltwater
  • Glacial geology
  • sediment left behind by glaciers
  • History of glaciation recorded by glaciers

5
Introduction to Glacial Geology
  • Glacial record on Earth

6
Water
  • The water molecule
  • 2 positive univalent hydrogen ions asymmetrically
    bonded to one bivalent oxygen ion (covalent
    bond)
  • Causes small residual negative charges at oxygen
    end and slight positive charges at hydrogen end
    (polar)
  • Hydrogen end of one molecule attracts oxygen end
    of another molecule ? weak electrostatic bond
    (hydrogen bond)

7
Ice as a Mineral
  • Ice differs from water in structure, physical
    properties, isotopic composition
  • Crystallice ice that forms glaciers is
  • Hexagonal
  • Exists at temps 0oC. to 70oC. And at pressures
    as high as 2000 atm
  • Other types of ice not found on earth

8
Ice as a Mineral
  • Ice is a mineral
  • Relatively stable crystalline structure within
    certain range of pressure-temperature
  • Hexagonal structure revealed by X-ray diffraction
    analysis of position of oxygen atoms in space (H
    atoms too small)

9
Ice as a Mineral
  • Physical properties of ice defined at pressure
    melting point (0oC. At 1 atm)
  • Melting point decreases with increasing pressure
  • Specific gravity of ice lt water, but volume is
    higher
  • Because ice has a 3-D structure more open than
    that of water
  • water is well-packed chains of H2O)

10
Ice as a Mineral
  • See text for discussion of
  • Specific heat
  • Thermal conductivity
  • Heat content (enthalpy)
  • Latent heat heat absorbed/freed by unit weight
    of water or ice during phase change

11
Ice as a Mineral
  • Hardness of ice crystals increases as temperature
    decreases
  • At pressure melting point ice hardness 1.5 on
    Mohs Scale (similar to talc, gypsum)
  • At 15oC. hardness 2-3 (similar to
    gypsum-calcite)
  • Thus, too soft to abrade most rocks

12
Ice as a Mineral
  • Nature of ice deformation depends on amount
    rate that stress is applied
  • With increasing stress elastic deformation
    followed by breakage
  • With constant stress applied over long time ?
    plastic deformation
  • Deformation of ice crystal depends on direction
    that stress is applied

13
Ice as a Sediment and Rock
  • Two major forms of ice rock
  • Congelation ice formed from freezing of water
  • Metamorphic glacier ice formed through
    densification of snow

14
Ice as a Rock
  • Gas impurities
  • Mostly as air but can also trap CH4, H2S, CO2
  • Percent volume as air
  • Up to 99 in fresh snow
  • Up to 56 in firn
  • Air reduces thermal conductivity of snow and ice
    snow is a good insulator
  • Air reduces transparency of ice

15
Ice as a Rock
  • Liquid impurities
  • Liquids found in ice as a response to heat,
    pressure, salt
  • As ice melts water initially develops between
    ice crystals

16
Ice as a Rock
  • As ice melts into water water temperature
    remains at 0oC. until all of ice is gone
  • Only after that will water temperature rise

17
Ice as a Rock
  • Salt impurities
  • Salts lower freezing point of water
  • Until eutectic point (see E in figure) when
    everything freezes

18
Ice as a Rock
  • Rock impurities in ice
  • Rocks absorb radiant energy ? heat up and melt
    surrounding ice

19
Ice as a Rock
  • Rock impurities in ice
  • Thick deposits of rock serve as an insulator and
    protect ice from melting

20
Ice as a Rock
  • Rock impurities in ice
  • Melting occurs when basal ice is at pressure
    melting point and glacier passes over rock
  • Rock in ice increases rigidity of glacier

21
Metamorphism of Snow
  • Snow
  • Snowflakes are ice crystals that have combined in
    hexagonal structure
  • New snow density is 0.1 (90 air) to 0.3 g/cc
  • Old snow
  • Coarse granular snow rounded-off crystals
  • Density 0.3 to 0.45 g/cc

22
Metamorphism of Snow
  • Firn
  • Snow that has survived at least one melt season
  • Loosely consolidated, randomly-oriented ice
    crystals, 1-4 mm diameter
  • Interconnected air pockets
  • Density 0.45 to 0.75 g/cc

23
Metamorphism of Snow
  • Firn ice
  • Mix of partially altered firn and white bubbly
    glacier ice
  • Density 0.75 to 0.88 g/cc

24
Metamorphism of Snow
  • Glacier ice
  • Crystals in firn grow and air pockets become
    isolated air cannot be blown into it!

25
Metamorphism of Snow
  • Glacier ice
  • Crystals can grow quite large gt10 cm

26
Metamorphism of Snow
  • Glacier ice
  • Crystals can grow quite large gt10 cm
  • Density 0.88 to 0.90 g/cc
  • Less than water
  • As more air is expelled white bubbly ice becomes
    blue and eventually black ice
  • Water molecules between ice refract blue
    wavelengths
  • Other colors are refracted but they interfere and
    we dont see them

27
Metamorphism of Snow
28
Metamorphism of Snow
29
Metamorphism of Snow
  • Depth of firn needed to form glacier ice depends
    on temperature and water equivalent of snow
  • 80 meters in Antarctica
  • 13 meters in SE Alaska

30
Snow Hazards and Resources
  • Snow hazards
  • Hazard for humans road ice, white-outs, snow
    bridges, snowmelt flooding
  • Hazard for animals
  • Hazard for plants abrasion, bending of branches,
    reduced soil productivity

31
Snow Hazards and Resources
  • Costs of snow removal

32
Snow Hazards and Resources
  • 25 deaths per year in Switzerland from snow
    avalanches
  • Hannibals Army of 18,000 wiped-out by avalanches
    in Alps in 218 B.C.
  • During WWII 40,000 Italian Austrian troops
    killed by avalanches in Dolomite Mts., Italy

33
Snow Hazards and Resources
  • Avalanches can start at a point or as a slab
  • May reach high velocity 300 kph
  • 10,000 per year in mountains of western USA
  • 1 of USA avalanches cause fatalities and/or
    damage 7 deaths 300,000 in damage per year

34
Snow Hazards and Resources
  • Contributing factors
  • Cornice overhang
  • 1-2 feet of new snow ? weight
  • Sun crust forms ? future sliding plane
  • Rounding-off of crystals in old snow ? loose
    interlocking crystals
  • Depth hoar crystals from sublimation of water
    vapor (sugar snow) ? act like ball bearings

35
Snow Hazards and Resources
  • Avalanches of 1951 in Alps
  • Heavy snowfall for 3 weeks in Jan.-Feb.
  • Up to 4 feet in one day
  • 500,000 tonnes of wet snow let loose above
    village of Vallascia
  • Killed 10 who had ignored instructions to
    evacuate

36
Snow Hazards and Resources
  • Collapse of ice summit on Huascaran (21,831 ft.)
    in Peru
  • Rock displaced by falling ice
  • Debris flow in valley with ice-rock-water moved
    200 mph
  • Demolished 3 towns 25,000 died
  • Smaller scale event in 1962 had claimed 4000
    deaths

37
Snow Hazards and Resources
  • Juneau, Alaska
  • 6 major avalanches in last 100 years
  • None in last 25 years
  • New subdivision has been constructed across
    avalanche chute
  • Threat to 30 homes, school, hotel, marina

38
Snow Hazards and Resources
  • Prediction mitigation
  • Need adequate network of weather stations for
    real-time prediction
  • Avalanche mapping
  • Artificial triggering with explosives
  • Avalanche barriers or energy dissipaters

39
Snow Hazards and Resources
  • Snowmelt and flooding esp. from regional warm
    rain-on-snow events

40
Snow Hazards and Resources
  • Snow as a resource
  • Insulation inhibits deep frost penetration and
    prevents damage to crops, gardens, buried
    pipelines
  • Water supply
  • Transportation skis, snowmobiles, packed snow
    roads in arctic
  • Recreation
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