1
Q

What is Hillslope?

A

The elevated land between valley bottoms

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2
Q

What are hillslope processes?

A

Movement of rock and soil by mass wasting, rain splash and overland flow

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3
Q

Characteristics of bedrock slopes?

A

Soil production < erosion
Little to no soil cover with bedrock at surface
Sediment transport is weathering limited
Slope form controlled by rock properties

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4
Q

Characteristics of soil-mantled slopes?

A

Soil production > erosion
A surficial layer of soil covers the bedrock
Sediment transport is transported limited
Slope form controlled by soil properties, production & transport rates

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5
Q

What are bedrock hillslopes?

A

WEATHERING LIMITED
- With steep slopes
- Thin to absent soil mantle

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6
Q

Where are bedrock hillslopes found?

A

Arid climates
Common in humid areas with low weathering rates

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7
Q

What are the processes of bedrock hillslopes?

A
  • Falls and slides
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8
Q

What are the physical characteristics of bedrock hillslopes?

A

Parallel retreat at threshold angles

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9
Q

What are soil-mantled hillslopes?

A

Transport-limited
With thick soil mantle

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10
Q

Where are soil-mantled hillslopes found?

A

Humid climates

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11
Q

What are processes of soil-mantled hillslopes?

A

Soil creep and slides

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12
Q

what are the physical characteristics of soil-mantled slopes?

A

Convex profiles
Typically parabolic

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13
Q

What does surface erosion impact?

A

Individual grains, detached separately and transported over the slope surface

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14
Q

What are some examples of surface erosion?

A
  • Rain-splash
  • Overland flow
  • Rills
  • Gully
  • Reactivated ancient gullies
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15
Q

What are the types of overland flow?

A

Horton Overland flow
Slope foot saturation - termed saturation overland flow

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16
Q

What is the Horton Overland Flow?

A

Rainfall rate excess of infiltration capacity

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17
Q

What is overland flow?

A

Water flowing over the soil surface

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18
Q

What infiltration rate?

A

The rate that’s actually taking place

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19
Q

What is the infiltration capacity?

A

A hypothetical maximum rate

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20
Q

What does the Horton Overland Flow depend on?

A

Rainfall rate and surface

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21
Q

What does the saturation overland flow depend on?

A

Rainfall amount

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22
Q

What increases in both Horton Overland Flow and Saturation overland flow?

A

Damage increase with gradient

23
Q

What are the four major styles of mass wasting?

A

1/ Fall
2/ Slide
3/ Flow
4/ Creep

24
Q

Where are rock falls most common?

A

Arid and semi-arid lands
and along shorelines

25
What can trigger rock falls?
Earthquakes
26
Factors of a rock fall?
Rapid and observable
27
What happened on Monday 7th Jan 2020?
5.8 magnitude earthquake destroying Punta Ventana Puerto Rico
28
What is rock fall?
Downward motion of rock or soil through the air
29
On what kind of slope does rock fall occur?
Very steep faces or cliffs
30
What is slide/ slumps?
Slipping of coherent roc or soil units often with a backwards rotation
31
What happened to the A625?
Large parts were removed during a large landslide in 1977 (following the dry summer of 1976 and heavy rain in the winter of 1976/77) the road developed large steps in the carriageway. The road finally closed in 1979
32
What are debris flows?
- Slow to the very rapid flow - Saturated soil & rock debris down distinct channels - Typically coarse-grained materials - Lots of internal deformation - Relatively high water content/ fluid-like flow - Failure typically along a well-defined shear plane at the soil-bedrock interface.
33
Where does water-logged material moving slowly typically occur?
Fine-grained soil or rock
34
What can bedrock slides limit?
The relief of mountain ranges
35
What happened to Mt. Cook, New Zealand?
Top 10 meters of summit fell away in a massive debris avalanche on December 14, 1991
36
What does soil creep impact?
Whole soil mass rather than individual grains
37
What is soil creep?
Continuous gravity driven process with no discrete boundaries
38
What is soil creep?
The continuous gravity-driven process with no discrete boundaries
39
What is soil creep caused by?
- Seasonal processes such as thermal- or moisture-driven expansion/contraction - Bioturbation
40
What is bioturbation?
The disturbance of the mixing of sediment by living organisms
41
What is solifluction?
A type of creep particularly associated with periglacial conditions and freeze-thaw cycles - Faster than most other forms of creep
42
What is stress?
The force acting over a cross-sectional area within a solid or liquid
43
What is normal stress?
Force acting perpendicular to the principle plane within a mass
44
What is shear stress
The force acts perpendicular to normal stress = slippage
45
What happens if the two stress exceed the strength or resistance of the slope material?
slope failure
46
What factors influence the balance between stress and strength?
Angle of the slope, cohesion of the materials, presence of water, and geological characteristics
47
When do failures occur?
When the gravitational force exceeds the resistance offered by the slope materials, causing movement and deformation
48
What is the role of water?
Adds weight to the slope: air in pore space is replaced by water
49
How does water impact the angle of repose>
- Low amounts of water causes cohesion - Saturation causes buoyancy, reduction N and thus friction - Over pressuring can cause liquefaction - Angle of repose maximal with least water - Angle of repose strongly reduced - Generally initiated by shock
50
What is the role of vegetation on a slope?
- Plant roots, trees in particular, substantially increase slope strength, reducing shallow slides and slumps Planting is an effective tool in slope stabilisation
51
What are the triggers for failure
- Shocks eg earthquakes - Slope modification (removal of vegetation) - Undercutting - Changes in hydrology - Volcanic eruptions
52
How can earthquakes impact slopes?
- They have destructive potential A secondary effect of earthquakes
53
What happened on 12th January 2001 in El Salvador?
Las Colinas slide claimed the lives of more than 500 people
54
What happened in the Regolith landslides?
The upper layer of soil slipped due to heavy rainfall Striking Manawatu, New Zealand In Feb 2004 Compared to the area of steep pasture with the scrub-covered gullies (upper right), where protective vegetation reduced the number of slips