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PeriglacialPermafrost II

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Heat transfer through rock allows nucleation at base. Once nucleated, ... Yipes stripes! Soli-/Gelifluction. Well-drained boulders trap finer sediment. ... – PowerPoint PPT presentation

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Title: PeriglacialPermafrost II


1
Periglacial/Permafrost II
2
Processes of the Active Layer
  • Short summer season!
  • Saturation
  • Dessication
  • Dehydration
  • Frost tables

3
Needle Ice
4
Freeze-thaw cycles
  • Weathering
  • Frequency
  • Intensity
  • Maximum
  • Mountains
  • South!
  • Minimum
  • North
  • W. coast

5
Alpine Felsenmeer(CO Front Range)
6
Frost Sorting
  • Ubiquitous!
  • Stone walls fences
  • Multiple explanations
  • Frost table penetration

7
Frost Sorting
X
8
Frost Sorting
  • Ubiquitous!
  • Stone walls fences
  • Multiple explanations
  • Frost table penetration
  • Selective crystal growth
  • Heat transfer through rock allows nucleation at
    base
  • Once nucleated, crystals grow vertically
  • Stones are Jacked up!

9
Frost Sorting
  • Ubiquitous!
  • Stone walls fences
  • Multiple explanations
  • Frost table penetration
  • Selective crystal growth
  • Rapid process!

10
Tombstones
11
Patterned Ground
  • Frost wedging (after Lachenbruch, 1960)
  • Expand/contract
  • Add water
  • Repeat
  • Upon warming, fill in with noncohesive sediment

12
Fossil Frost Wedges
Cover sand (eolian)?
  • Big Horn Basin
  • Pipeline trench
  • Also evident in aerial photographs
  • Evidence of former MAAT lt-6C

Bkb (caliche)
Preglacial soil
13
Frost Boils
  • Sorting and circulation
  • Fines in center (dont step there!)
  • Stones around the margin

14
Upland sorted nets
15
Lowland sorted nets
  • Like mud cracks and columnar jointing
  • May be high-center or low (seasonal)
  • May be fine or coarse

16
Pingos
  • Cycle lt10,000 yr
  • Feedback loops?

17
Periglacial Slopes
  • Landscape f(
  • Freeze-thaw cycles)
  • Slope angle)
  • Water saturation)
  • Sediment size)
  • Sediment supply)
  • Snow/water/ice supply)

18
Frost heave/creep
  • Heave f(
  • Moisture)
  • Grain size)
  • Creep f(
  • Saturation)
  • Grain size)
  • Slope)

19
Frost heave/creep
Fine
  • Movement f(
  • Time)
  • Slope)

Coarse
Coarse
Fine
Transect across a flow lobe
20
Sorted nets on slopes - steps
21
Yipes stripes!
22
Soli-/Gelifluction
  • Well-drained boulders trap finer sediment.
  • Roll down hill like caterpillar track

2340130
23
Examples soli-fluction
Cryoplanation?
24
Stone lobes
  • Stones move?
  • Water?
  • Fines?

25
Block streams
  • Weird!

26
Avalanche/Debris Fans
  • Lateral levees
  • Terminal lobes
  • Undisturbed ground
  • Run on snow?
  • On/above the surface redistribute as lobes
    levees.

27
Talus
  • Ubiquitous slope deposit
  • Note natural levees

28
Case study Sacajawea cirque
NOTE talus adjacent to ongoing debris flows
why?
29
Protalus ramparts
  • Positioned below talus
  • Ridge transverse to slope
  • Composition talus
  • Origin ?

30
Protalus ramparts
  • Positioned below talus
  • Ridge transverse to slope
  • Composition talus
  • Origin ?

31
Rock-glaciers
  • Transition between ice-glaciers, protalus
    ramparts and talus cones
  • Lobate rock masses downhill from talus
  • Often totreeline
  • Orienteddue north Why?

32
Rock-glacier features head
  • Transitional to talus coarse surface

33
Evidence of flow
  • Arcuate ridges vegetation(?)

34
Rock-glacier toe
  • Angle of repose fine/frozen core

35
Lobate rock-glacier CO
36
Rock-glacier vs. talus
  • Comparable orientation, source area So?

37
Rock-glacier movement
38
Lava Lake rock-glacier(?)
39
Deflated Rock-Glaciers Why?
40
Mountain Basins
  • EX Sawatch Rge, CO
  • Name those features!
  • Talus
  • Debris flows
  • Lobes
  • Levees
  • Rock-glaciers
  • Active
  • Ancient

41
Application Alaska Pipeline
  • Permafrost regimes
  • Tectonics

42
145F
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