Geology 12 Presents Outline: Outline: Chp 14 Mass Wasting (Landslides)Chp 14 Mass Wasting...
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Transcript of Geology 12 Presents Outline: Outline: Chp 14 Mass Wasting (Landslides)Chp 14 Mass Wasting...
Outline:Outline:• Chp 14 Mass Wasting (Landslides)Chp 14 Mass Wasting (Landslides)• Chp 15 Running WaterChp 15 Running Water• Chp 16 GroundwaterChp 16 Groundwater• Chp 17 Glaciers and GlaciationChp 17 Glaciers and Glaciation• Chp 18 Wind and DesertsChp 18 Wind and Deserts
A: Introduction/Glaciers
• Glacier: mass of ice composed of compacted snow and recrystallized snow flowing under its own weight under the force of gravity.
• Move via:1. plastic deformation below 40m just from the
shear weight of ice.
2. basal slip: sometimes with the presence of melt water the glacier may slide.
Types of Glaciers1. Valley/Alpine Glaciers: confined to
mountain valleys (yoodle leh)
• Flow down hill
• Few km wide by 10’s of km long by several 100 m thick
• Ex: Alaskan Alpine Glaciers
2 km wide x 120 km long x 400 m thick
ice
Types of Glaciers2. Ice Sheets: BIG
• Flow out horizontally in every direction from where the snow accumulates the mosta) Continental Glaciers:
• Largest: 100s of km long/wide by 3-5 km thick
• Ex: Greenland, Antarctica (now) and N. Amer’ during the last ice age 25,000 yrs ago (most of Canada)
Types of Glaciers
2. Ice Sheets: b) Ice Caps
• <50,000 km2
• Ex: Penny Ice Cap (Baffin Isld), Iceland, Spitsberg Isld.
ice
crustisostacy
• Glacial Movement
Zone of accumulation
Firn limit
snow
ice
Zone of wastage
Ice front
Firn: pebbles of ice; intermediate stage between snow and ice
Glacial MovementGlacial advance: when accumulation > wastage
Glacial Retreat: when accumulation < wastage
Glacial MovementGlacial Movement
Glacial advance: when accumulation > wastage
Glacial Retreat: when accumulation < wastage
B: Glacial Erosion & Transport• Weathering: a glacier
is a combination of ice and rock (silt,sand, pebbles, boulders). The primary weathering is mechanical; ice/frost wedging (plucking or quarrying)
Glacial Eroded Landforms
• Erosion: glaciers carry the sediment within the ice AND grind/polish bedrock via abrasion (rock within the ice grinds below the glacier).
• The plucking and grinding creates the following landforms (become visible after the ice is gone):
8. U-Shaped Valley/Trough: valley scoured by a valley glacier
• *Fjords: sea-level was 130m lower during the ice age allowing alpine glaciers to gouge out valleys, then after the ice melted and sea level raised it flooded the valleys to make fiords (Ex. Howe Sound)
10. Ice Scoured Plain: glacier stripped unconsolidated sediment leaving scoured bedrock with little lakes/swamps and small hills (northern Manitoba & Quebec, NWT).
C: Glacial Deposits:
Drift = all glacial sedimentDrift = all glacial sediment2 types:2 types:1. Till: unsorted and unstratified1. Till: unsorted and unstratified
Directly deposited by the glacier Directly deposited by the glacier (like a bulldozer) so it is unsorted and (like a bulldozer) so it is unsorted and unstratified (no layers)unstratified (no layers)
2. Outwash = Stratified Drift: depsoited 2. Outwash = Stratified Drift: depsoited by glacial meltwater so it tends to be by glacial meltwater so it tends to be sorted and stratifiedsorted and stratified
ii) Recessional End Moraine: smaller end moraines behind the terminal moraine that
form as the glacier recedes
1. Till Landformsf) Drumlins: canoe-shaped hill of till formed as glacier over-runs a moraine forming it into a swarm of drumlins.
More common with ice sheets.
Ice direction??
Mtn’Mtn’Mtn’
End moraines
Medial moraine
Ground moraine (underneath ice)
Lateral moraines
ice ice Lateral moraine
Lateral moraine
recessional moraines
terminal moraine
drumlins
Draw
2. Outwash = Stratified Drift Landforms a) Varves: mud deposits in lakes < 1cm
thick
1 year: spring-summer: silt + clay = light colour
Fall-winter: clay + OM = dark layer
1 year
Drop stone: fell out of melting iceberg.
2. Outwash = Stratified Drift Landforms a) a) Varves: mud deposits in lakes < 1cm thick
1 year spring-summer: light colour
Fall-winter: dark layer
2. Outwash = Stratified Drift*Kettle: block of ice is buried by outwash ( or in a moraine). When it melts a depression is
formed.
*Kettle: block of ice is buried by outwash ( or in a moraine). When it melts a depression is
formed.
e) Kame Terrace: remnant terrace after glacier melts
Before, near end of ice age
Stagnant glacier -ice
Stream & sedimentsLake and clay sediments
Ice melts
esker
Kame terrace
lake
2. Outwash = Stratified Drift Landforms 2. Outwash = Stratified Drift Landforms e) Kame Terracee) Kame Terrace
Provincial Exam question: name and Provincial Exam question: name and label four glacial features.label four glacial features.
Use the photograph of an ancient glacial lake deposit to answer this question. Each pair of dark (clay rich) and light (silt rich) layers represents one year of deposition. (4 marks)a) Describe a process which would have resulted in the deposition of the pairs of layers. (2 marks)b) Describe a process which could account for the presence of the twenty centimetre diameter boulder X on the right-hand side of the deposit. (2 marks)
Use the photograph to answer question this question. The large, isolated, darkly-coloured boulder shown in the picture is obviously composed of a different type of rock from the lightly-coloured limestone on which it is lying.a) Account for the presence of the boulder in this locality. Give evidence for your answer.(2 marks)Presence of the boulder:b) Explain why the boulder is elevated above the general surface level. (2 marks)Elevation of the boulder:
Causes of Ice Ages
• Cool summers causing less melting of snow (snow has a high albedo (light reflection) which results in colder weather, less melting, more snow, etc…
• 3 Major Ice Ages:1. 2,300 myrs
2. 700 myr
3. Last 1.6 myrs (Pleistocene Epoch)
• Pleistocene Epoch
• Glacial Interglacial Years
(now)
Wisconsin
Sangamon
Illinoan
Yarmouth
Kansan
Aftonian
Nebraskan
10,000
500,000
1 million
1.5 million
• Causes of Ice Ages:– 1. Position of continents blocking ocean
current flow (Central America formed 1.5 m yrs ago)
– 2. Changes in Earth’ rotation and revolution around the Sun (Milankovitch Theory)
– 3. Volcanic Eruptions– 4. Meteorite Impact– 5. Sun’s output changes
– 6. CO2 Levels vary