Geology lecture 20

2,573 views

Published on

0 Comments
0 Likes
Statistics
Notes
  • Be the first to comment

  • Be the first to like this

No Downloads
Views
Total views
2,573
On SlideShare
0
From Embeds
0
Number of Embeds
7
Actions
Shares
0
Downloads
108
Comments
0
Likes
0
Embeds 0
No embeds

No notes for slide

Geology lecture 20

  1. 1. Chapter22Glaciers and Ice Ages
  2. 2. Chapter22Outline• Ice and glacial ice, glaciers and their formation.• Glaciers-Types: mountain and continental-Thermal categories: temperate and polar-Ice movement, glacial advance & retreat-Ice in the sea• Effects of glaciers:-Erosion, sediment transport, deposition-Depositional landforms• Glaciation-Theory of glaciation and ice ages-Subsidence & rebound, sea level change, drainage modification.-The Pleistocene Glaciation and earlier ones-CausesChapter 22
  3. 3. Chapter22Ice: The Water Mineral• Ice is solid water (H2O).• Forms when water cools below freezing point.• Natural ice is a mineral; grows in hexagonal forms.
  4. 4. Chapter22Formation of Glacial Ice• Snow is transformed into ice.• Flakes accumulate.• Buried by later falls.• Compression expels air.• Pressure causes melting &recrystallization.• Snow turns into granular firn.• Over time, firn melds intointerlocking crystals of ice.
  5. 5. Chapter22Glaciers & Their Formation• Thick masses of recrystallized (glacial) ice.• Last all year long, flow via gravity.• 3 conditions necessary:• Cold local climate• Snow must be abundant; more snow must fall than melts• Snow must not be removed by avalanches or wind
  6. 6. Chapter22Forming a Glacier• Glacier-sustaining elevation is latitude controlled• Polar regions -> glaciers form at sea level• Equatorial regions -> glaciers form >5km elevation• This elevation is marked by the “snow line”
  7. 7. Chapter22Outline• Ice and glacial ice, glaciers and their formation.• Glaciers-Types: mountain and continental-Thermal categories: temperate and polar-Ice movement, glacial advance & retreat-Ice in the sea• Effects of glaciers:-Erosion, sediment transport, deposition-Depositional landforms• Glaciation-Theory of glaciation and ice ages-Subsidence & rebound, sea level change, drainage modification.-The Pleistocene Glaciation and earlier ones-CausesChapter 22
  8. 8. Chapter22Glaciers2 main types: Continental and mountain.
  9. 9. Chapter22Mountain Glaciers• Flow from high to low elevation in mountains• Include a variety of types.• Ice caps cover mountain peaks• Cirque glaciers fill mountain top bowls
  10. 10. Chapter22Mountain Glaciers• Valley glaciers flow like rivers down valleys
  11. 11. Chapter22Mountain Glaciers• Piedmont glaciers spread out at valley terminusGreenlandAlaska
  12. 12. Chapter22Continental Glaciers• Ice sheets covering large land areas.• Flows outward from thickest portion• 2 major ice sheets on Earth:Greenland, AntarcticaMinor: Iceland
  13. 13. Chapter22Thermal Categories• Used to classify glaciers; determined by climate.• Temperate glaciers – ice at/near melting temperature• Polar glaciers – ice well below melting temperature
  14. 14. Chapter22Glacial Ice Movement• How do glaciers move?• Wet-bottom glaciers – water flows along base• Basal sliding – ice slips over a meltwater/sediment slurry• Dry-bottom glaciers – cold base is frozen to substrate• Movement is by internal plastic deformation of the ice
  15. 15. Chapter22Glacial Ice Movement• 2 types of mechanical behavior.• Brittle – Uppermost 60 m• Tension initiates cracking• Crevasses open and close with movement• Plastic – Lower than 60 m• Ductile flow occurs in deeper ice• Ice flow heals cracks
  16. 16. Chapter22• Ice flows downhill via gravity.• Gravity (g) can be resolved into 2 vectors• Parallel to slope component (gs) drives flowGlacial Ice Movement
  17. 17. Chapter22• Ice flows downhill via gravity.• Ice flows from thickest part of continental glaciers• Analogous to honey flowing…Glacial Ice Movement
  18. 18. Chapter22• Variable flow rates (10 to 300 m/yr).• Rarely, glaciers surge (20 to 110 m/day)• Flow rate controlled by:• Slope -> steeper = faster• Basal water: wet-bottom = faster• Location within glacier• Greater velocity in ice center• Friction slows ice at marginsGlacial Ice Movement
  19. 19. Chapter22• Glaciers behave like bank accounts• Accumulation zone – Area of new snow addition• Colder T prevent melting• Snow remains even in summer• Ablation zone – Area of net ice loss• Zones abut at equilibrium lineGlacial Advance and Retreat
  20. 20. Chapter22Glacial Advance and Retreat• Toe (leading edge) position:• If accumulation = ablation the toe is stable Note curved path of ice flow.
  21. 21. Chapter22Glacial Advance and Retreat• Toe position:• If accumulation < ablation, toe retreats upslope
  22. 22. Chapter22Glacial Advance and Retreat• Toe position:• If accumulation > ablation, the toe advances
  23. 23. Chapter22Glacial Advance and RetreatGlacial advance and retreat is determined by the balance between theaccumulation of snow and the removal of ice by sublimation, melting,and calving (ablation). When the rate of ablation below the snowlineequals the rate of accumulation above it, the glacier is stationary, as inView 1. During glacial retreat, View 2, the rate of ablation exceeds therate of accumulation, and the position of the toe retreats toward theorigin of the glacier. Glacial advance, View 3, occurs when the rate ofaccumulation exceeds the rate of ablation. For all views, pay attention tothe motion of the stones. Note that in all cases, ice flows downhill. Formore information, see Section 22.2 Ice and the Nature of Glaciersstarting on p. 758 and Figure 22.14 on p. 768 in your textbook.Glacial Advance and Retreat
  24. 24. Chapter22Ice in the Sea• In polar regions, glaciers flow out over ocean water.• Tidewater glaciers – valley glaciers entering sea• Ice shelves – continental glaciers entering sea• Sea ice – non-glacial ice formed on frozen seawater
  25. 25. Chapter22Ice in the Sea• Large areas of the polar seas are covered with ice.
  26. 26. Chapter22Ice in the Sea• Marine glaciers have both grounded and floating ice• Ice debris calves off edge forming icebergs
  27. 27. Chapter22Outline• Ice and glacial ice, glaciers and their formation.• Glaciers-Types: mountain and continental-Thermal categories: temperate and polar-Ice movement, glacial advance & retreat-Ice in the sea• Effects of glaciers:-Erosion, sediment transport, deposition-Depositional landforms• Glaciation-Theory of glaciation and ice ages-Subsidence & rebound, sea level change, drainage modification.-The Pleistocene Glaciation and earlier ones-CausesChapter 22
  28. 28. Chapter22Glacial Erosion• Glaciers erode substrates in1. Incorporation – rock surrounded and carried off
  29. 29. Chapter22Glacial Erosion2. Plucking – ice breaks off and removes bedrock fragments• Ice melts by pressure against up-ice side of obstruction• Enters cracks in bedrock, water re-freezes to the ice• Glacial movement “plucks” away bedrock chunks
  30. 30. Chapter22Glacial Erosion3. Abrasion – a “sandpaper” effect on substrate• Rock fragments in moving ice abrades and polishes bedrock• Leaves scratches called striations
  31. 31. Chapter22• Various erosional features of glaciated valleys.Glacial Erosion
  32. 32. Chapter22Glacial Erosion• Cirque – bowl-shaped basin near mountain top• Forms at uppermost portion of valley• Erosion at glacier base over-steepens into bowl• After ice melts, cirque is often filled with a lake (tarn)Glacier, Nat’l Park, MT
  33. 33. Chapter22Glacial Erosion• Arête – a “knife-edge” ridge• Formed by 2 adjacent cirques or• Valley glaciers
  34. 34. Chapter22Glacial Erosion• Horn – a pointed mountain peak• Formed by 3 or more cirques that coalesce
  35. 35. Chapter22Glacial Erosion• U-shaped valleys.• Glacial erosion createsvery steep walls• Unlike V-shaped fluvialvalleys
  36. 36. Chapter22Glacial Erosion• Hanging valleys.• -Intersection of tributary glacier• With trunk glacier• -Trunk glacier incises deeper• -Trough bases at different• -Elevations• -A waterfall results
  37. 37. Chapter22Glacial Sediment Transport• Glaciers carry sediment of all sizes (lots of it!)• Some falls onto from adjacent cliffs• Some entrained from substrate erosion• When ice melts, material is dropped
  38. 38. Chapter22Glacial Sediment Transport• Moraines – unsorted debris carried/dumped by glaciers• Lateral – along valley glacier flank• Medial – mid-ice merging lateral moraines
  39. 39. Chapter22Glacial Sediment Transport• Glaciers are large-scale conveyor belts• Pick up, transport, deposit sediment.• Transport is always downhill• Debris at toe is an end moraine
  40. 40. Chapter22Glacial Deposition• Many sediment types derive from glaciation.• Called glacial drift, these include...• Till.• Erratics.• Marine sediments.• Outwash.• Others (lake seds, loess)• Stratified drift is water-sorted; unstratified driftisn’t.
  41. 41. Chapter22Glacial Deposition• Glacial till – Sediment dropped by glacial ice.• Consists of all grain sizes• Unmodified by liquid water, hence:• Unsorted• Unstratified• Accumulates…• Beneath glacial ice• At glacial toe• Along glacial flanks
  42. 42. Chapter22Glacial Deposition• Erratics – boulders dropped by glacial ice• Different than underlying bedrock• Often carried from long distances
  43. 43. Chapter22Glacial Deposition• Glacial marine – sediments from an oceanic glacier• Calving icebergs raft sediments away from ice• Melting bergs drop stones into marine muds• Dropstones…• Differ from ambient sediment• Indicate glaciation
  44. 44. Chapter22Glacial Deposition• Glacial outwash – sediment transported in meltwater• Muds removed• Abraded and rounded• Dominated by sand and gravel
  45. 45. Chapter22Depositional Landforms• Glacial sediments create distinctive landforms.• Moraines.• Drumlins.• Ground moraine.• Kettle lakes.• Eskers.
  46. 46. Chapter22Depositional Landforms• End moraines form at stable glacier toe• Terminal moraines form at farthest edge of flow• Recessional moraines form as retreating ice stalls
  47. 47. Chapter22Depositional Landforms• Drumlins – long aligned hills of molded till• Asymmetric form – steep up-ice; tapered down-ice• Aligned parallel to ice flow direction
  48. 48. Chapter22Depositional Landforms• Eskers – long, sinuous ridges of land and gravel• Form from meltwater channels below ice
  49. 49. Chapter22Outline• Ice and glacial ice, glaciers and their formation.• Glaciers-Types: mountain and continental-Thermal categories: temperate and polar-Ice movement, glacial advance & retreat-Ice in the sea• Effects of glaciers:-Erosion, sediment transport, deposition-Depositional landforms• Glaciation-Theory of glaciation and ice ages-Subsidence & rebound, sea level change, drainage modification.-The Pleistocene Glaciation and earlier ones-CausesChapter 22
  50. 50. Chapter22The Theory of Glaciation• European farmers broke plows on large rocks.• Buried in fine-grained soils, often of enormous size.• Unlike local bedrock, they were from 100s of km away.• Rocks became known as erratics• Origins were a mystery…
  51. 51. Chapter22The Theory of Glaciation• Louis Agassiz, a Swiss geologist, observed glaciers.• Saw glaciers as landscape change agents• They carried snad, mud, huge boulders long distances• They dropped these materials, unsorted, upon melting• Realized glaciers could explain the erratics
  52. 52. Chapter22The Theory of Glaciation• Agassiz proposed an ice age had frozen Europe• Ice sheets covered land• Ice carried and dropped…• Erratics and• Unsorted soil (till)
  53. 53. Chapter22Ice Ages• Glaciers presently cover ~10% of Earth• During ice ages, coverage expands to ~30%• Most recent ice age ended ~11 kyrs ago• Covered New York, Montreal, London, Paris, Seattle• Ice sheets were 100s to 1,000s of m thick.
  54. 54. Chapter22Glacial Consequences• Subsidence & rebound.• -Ice sheets depress lithosphereinto mantle• -Subsidence followsasthenosphere flow• -Ice melts, depressedlithosphere rebounds• -Continues slowly today
  55. 55. Chapter22Glacial Consequences• Sea level changes due to ice ages• Water stored on land during ice age –> sea level fall• Deglaciation returns water to oceans –> sea level rise• Sea level was ~100 m lower during last glacial maximum
  56. 56. Chapter22Glacial Consequences• Can cause drainage basin reorganization.• N. America: Glaciation completely changed drainage.
  57. 57. Chapter22The Pleistocene Glaciation• Young (< 2 Ma) glacialremnants are abundant.• North America• Scandanavia and Europe• Siberia• Distinctive glaciallandscapes.
  58. 58. Chapter22The Pleistocene Glaciation• Glaciation chronology.• Several Pleistocene glacial advances• In North America, 4 recognized – youngest to oldest…• Wisconsinan, Illinoian, Kansan, Nebraskan• Ice ages are separatedby interglacials
  59. 59. Chapter22The Pleistocene Glaciation• Glaciation chronology.• Oxygen isotopes from planktonsuggest more ice ages• They reveal 20 or moreglaciations• Higher 18O/16O = colder.• Lower 18O/16O = warmer.• The “original 4” ice agesmay simply be the largest
  60. 60. Chapter22Earlier Glaciations• Glaciation recurs across Earth history.• Evidence? Fossil til (tillite), striated bedrock• Tillite at equatorial latitiudes suggest an ice-covered world:Snowball Earth
  61. 61. Chapter22Causes of Glaciation• Long-term causes – set stage for ice ages1. Plate tectonics – controls factors that influence glaciation• Continents at high latitudes• Sea level flux by mid-ocean ridge volume changes• Oceanic currents2. Atmospheric chemistry.• Changes in greenhouse gas concentrations• Carbon dioxide (CO2)• Methane (CH4)
  62. 62. Chapter22Causes of Glaciation• Short-term causes – govern advances and retreats• Milankovitch cycles – climate variation over 10-100s kyrspredicted by cyclic changes in orbital geometry1. Earth’s orbit shape varies (~100,000 year cyclicity)2. Earth’s axis tilt caries from 22.5degrees to 24.5degrees (~41,000years)3. Earth’s axis wobbles (23,000 years)
  63. 63. Chapter22Causes of Glaciation• Milankovitch – cyclic changes in orbital geometry.• Variations lead to excess warming/cooling.• Ice ages result when cooling effects coincide.

×