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Glaciers and Glaciation
Chapter 12
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Glaciers and Earth’s Systems
• A glacier is a large, long-lasting mass of ice, formed on land, that moves downhill under its own weight
• Glaciers are part of Earth’s hydrosphere
• About 75% of the world’s supply of fresh water is locked up in glacial ice
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*Paleozoic glacial age shows evidence for continental drift.
*Glaciers when present are more effective in transportation and deposition than running water
*Yosemite, Great Lakes, Glacier National Park, Greenland, Antarctica
Glaciation
*Ice Age covered 1/3 of land surface only a couple million years ago.
*Rock record shows other older glaciations.
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Formation of Glaciers• Glaciers develop as snow is compacted
and recrystallized, first into firn and then
glacial ice
• A glacier can only form where more snow accumulates during the winter than melts
away during the spring and summer
– Glaciation occurs in areas cold enough
to allow accumulated snow to
persist from year to year
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Formation of Glaciers
• Two types of glaciated terrains on Earth: – Alpine glaciation occurs in mountainous regions in the form of valley
glaciers
– Continental glaciation covers large land masses in Earth’s polar regions
in the form of ice sheets
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Anatomy of a Glacier
• An advancing glacier gains more snow than it loses, has a positive budget– End or terminus of glacier advances downslope
• A receding glacier has a negative budget– Terminus of glacier shrinks back upslope
• Snow is added in the zone of accumulation of glaciers, whereas melting (and calving of icebergs) occurs in the zone of ablation
• The equilibrium line, which separates accumulation and ablation zones, will advance or retreat depending on the climate
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Receding Glacier
South Cascade Glacier, Washington
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Movement of Glaciers
• Valley glaciers move downslope under the force of gravity • Movement occurs by basal sliding and plastic flow
– Crevasses are fractures formed n the upper rigid zone
• Due to friction, glacier flow is fastest at the top center of a glacier and slowest along its margins
slow
fast
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Glacial Erosion
• Glaciers erode underlying rock by plucking of rock fragments and abrasion as they are dragged along – Basal abrasion polishes and
striates the underlying rock surface and produces abundant fine rock powder known as rock flour
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Erosional Landscapes
• Erosional landforms produced by valley glaciers include: – U-shaped valleys
– Hanging valleys
• Smaller tributary glacial valleys left stranded above more quickly eroded central valleys
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Erosional Landscapes
U-shaped valleys
Hanging valleys
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Glacial Deposition
• General name for unsorted, unlayered glacial sediment is till
• Lateral moraines are elongate, low mounds of till along sides of valley glaciers
• Medial moraines are lateral moraines trapped between adjacent ice streams
Terminal moraines are ridges of till piled up along the front end of a glacier
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Glacial Deposition
• Medial moraines are lateral moraines trapped between adjacent ice streams
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Glacial Deposition• Large amounts of liquid water flow
over, beneath and away from the ice at the end of a glacier
• Sediment deposited by this water is known as glacial outwash
• Sediment-laden streams emerging from ends of glaciers have braided channel drainage patterns
• Outwash landforms include drumlins, eskers, kettles and kames
• Drumlins give direction information
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Antarctic Ice Sheet
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Past Glaciationfrom Ice Cores
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Direct Effects of Past Glaciation
• Large-scale glaciation of North America during the recent ice age produced the following effects: – Soil and sedimentary rocks were scraped off in northern and
eastern Canada, and lake basins were gouged out of the bedrock
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Indirect Effects of Past Glaciation
• Large pluvial lakes (formed in a period of abundant rainfall) existed in closed basins in Utah, Nevada and eastern California– Great Salt Lake is remnant of much larger
pluvial Lake Bonneville
– Huge floods emanated as ice-dammed lakes (e.g., Lake Missoula) drained catastrophically
• Sea level was lowered by water locked up into ice sheets, allowing stream channels and glaciers to erode valleys below present-day sea level– Fiords are coastal inlets formed by drowning
of glacially carved valleys by rising sea level
Giant gravel ripples formed during draining of Lake Missoula
Norway
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Meteorites found in Arctic Glaciers• The easiest place to locate dark, rocky meteorites is in Antarctic Ice Sheet
• A small number of meteorites appear to have come from the Moon and Mars
• Several of these appear to have come from Mars
martian meteorite
lunar meteorite
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The Global Energy ChallengeRoel Snieder
Photo: USFWS/Susanne Miller
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Developing countries
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… and our energy use
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Our energy-dependence (1)
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Energy use by type
(International Energy Outlook 2006)
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Peak oilPeak oil
N.B. based on USGS estimates, these are among the most optimistic
(Energy Information administration)
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Peak oil (again)
http://info.energyscenariosireland.com/Overview
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Declining production (1)
resource depleted
Time
Pro
duct
ion
supply
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Declining production (2)
production gap!
Time
Pro
duct
ion demand
supply
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Oil Peak, Oil Panic ?(Study by Amos Nur - Stanford)
U.S., Canada, Japan, Germany, France, Italy, UK, are the biggestconsumers of oil reserves worldwide.
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Countries with highest per capita income seeking oil from countries holding the oil wells/reservoirs (Saudi Arabia, Iraq, Venezuala).
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New find in GOM(Jack No. 2 test well)
• up to 3-15 billion barrels of oil
• US consumption 20 million barrels/day
• 5 months - 2 years
• reservoir is 8 km under sea level
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Non-convenional reserves(excluding gas and coal)
Produced (gone)
Proved Reserves
Undiscovered(?)
EORExtra Heavy Oil& Tar Sands Shale Oil
0 1 2 3 4 5 6 7 8 9 10
Trillions of Barrels Recoverable
Years Supply at2005 Production
Unconventional petroleum resources:(more difficult & dirty, and therefore expen$ive)
Conventional(“easy”)
0 25 50
(Courtesy of Joe Stefani)
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Non-conventional oil
from National Geographic, June 2004
Tar Sand
HeavyOil
Oilshale
2 tons of tar sands produce 1 barrel of bitumen (~asphalt)
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Other Energy Resources• The metal uranium is used to power nuclear power generators
– Found with organic matter in sedimentary rocks
– Accounts for 10% of U.S. energy production
– Leaves radioactive waste as by-product
• Hydroelectric power provides about 4% of U.S. energy needs– Renewable and non-polluting
• Geothermal power provides about 0.2% of U.S. energy needs
• Other renewable, non-polluting energy sources are wave/current power, solar power, wind power, and hydrogen fuel cells– As fossil fuel supplies dwindle, these sources become more important
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A New, Global Oil Quandary: Costly Fuel Means Costly Calories
(NYT, January 19, 2008)
Rising prices for cooking oil are forcing residents of Asia’s largest slum, in Mumbai, India, to ration every drop. Bakeries in the United States are fretting over higher shortening costs.
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Carbohydrates and biofuel
Do we feed humans or cars?
Is it a good idea to compete with our machines for calories?
glucose cellulose
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Research: biofuel from cellulose
0 5 10 15 20 25 Feed cost ($/GJ)
25
20
15
10
5
Pro
cess
ing
cost
s ($
/GJ)
oil (100$/barrel)
gas
starch(glucose)
cellulose
vegetableoil
http://gcep.stanford.edu/research/biomass.html(Figure adapted from Lange, J.P., Biofuels, Bioproducts and Biorefining, 1: 39-48, 2007)
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First solar 2 MW arrayFt. Carson, CO
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Research: efficient solar cells
ᅠ
1 mm
http://gcep.stanford.edu/research/solar.html
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Alternative Energy Sources: Wind power
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Past Glaciationfrom Ice Cores
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Arctic sea ice 1995-2007
(National Snow and Ice Data Center, Boulder)
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Arctic sea ice 2005-2007
(National Snow and Ice Data Center, Boulder)
4.3 million sq km4.3 million sq km
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What can I do as consumer?
Lighting Transportation Appliances
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What can I do as citizen?
• Ask: what is our energy plan?
• Start a discussion in your community.
• Demand that the United States becomes a world-leader in responsible use of energy.
“That which we are, we shall teach, not voluntarily but involuntarily.” [Emerson]
z
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Temperature and CO2 records
1 350 300 250 200 150 100 50 now
Thousands of year before present
20
-2-4-6-8
-10
Tem
pera
ture
cha
nge
(o C)
400
350
300
250
200
Car
bon
Dio
xode
(pp
mv)