1. Mass Movement Hazards Mass Wasting:
Mass wasting is the downslope movement of regolith and masses of rock under the pull of gravity
Mass wasting is a basic part of the rock cycle. Weathering, mass-wasting, and other aspects of erosion constitute a continuum of interacting processes
the most widespread geological hazard
does not account for many deaths
cost in damages is over three times that of all other catastrophes combined

2. Reduces internal friction in regolith
Mass Movement Hazards
Role of Water in Mass Movement
Reduces internal friction in regolith
If sand, silt, or clay becomes saturated with water, and the fluid pressure of this water rises above a critical limit, the fine-grained sediment will lose strength and begin to flow

3. Classification of Mass Movement
Mass Movement Hazards
Classification of Mass Movement
Mass-movement events are classified on the speed and manner in which materials move downslope:
Slow mass movement
Creep is a very slow type of granular flow measured in millimeters or centimeters per year.
Rates higher on steep slopes than on gentle slopes
Rates tend to increase as soil moisture increases.
Alternating freezing and thawing cause Creep
Solifluction occurs in arctic regions as consequence of freeze and thaw cycle – melted top layers slides over bottom
frozen layer.

4. Example of Creep

5. Rapid Mass Movement
Falls: rock and debris drop from steep slopes
Slides move downslope along preexisting plane of weakness as a single, intact mass
Slumps move downslope along a concave slip surface - both downward and outward motion
Flow: mixture moves downslope as a viscous fluid

6. Types of Rapid Mass Movement

7. Optimal Conditions for Falls, Slides, Flows
Rock falls require fractured bedrock exposures.
Slides commonly originate along contacts between layers of rock, soil, etc. with contrasting mechanical properties.
Major areas of concern are where surface vegetation cover is destroyed by fires, followed by rainfall.
Roadcuts or other areas of altered or excavated slopes are common targets (this includes sites of old landslides).
Volcanoes are common targets for such mass wasting because of the wealth of fine, unconsolidated sediment.
All of these are made more prevalent by seismic activity, that can act as a trigger mechanism.

8. Mass Movement Hazards
Rockfall is the free falling of detached bodies of rock, common in precipitous mountainous terrain, where slopes are to steep for loose material to remain on the surface.
A debris fall is similar to a rockfall, but it consists of a mixture of rock and weathered regolith, as well as vegetation.

9. Yosemite, CA
A rock fall in this area in July, 1996, had rather amazing consequences.
A single granite block weighing ~200 tons broke free and disintegrated upon impact.
The burst of air from the impact flattened some 2000 trees and the area was showered with dust from the obliterated boulder.
Only one person was killed.
The debris at the base of a steep slope such as this is called talus.

10. - Associated with heavy rains or sudden shocks, such as earthquakes.
Mass Movement Hazards
A slump is slope failure in which a downward and outward rotational movement of rock or regolith occurs along a curved concave-up surface.
- Associated with heavy rains or sudden shocks, such as earthquakes.
The top of the displaced block usually is tilted backward, producing a reversed slope.

11. Slumping and Scarps in Dorset
Mass Movement Hazards
Slumping and Scarps in Dorset

12. Mass Movement Hazards
Slides
commonly originate along contacts between layers of rock, soil, etc. with contrasting mechanical properties

13. Landslide This is a typical landslide.
Mass Movement Hazards
Landslide
This is a typical landslide.
Note that materials hold together in more-or-less singular blocks.
As is common, when the slide blocks reach a lower slope, they break up (becoming a debris flow in this case).
The La Conchita landslide, near Santa Barbara, CA, Spring, 1995.

14. Mass Movement Hazards
Flow Types
Flows: A movement of water-saturated sediment which move downslope as a thick fluid.
Mudflow
Def. – A quick movement of material that results from a heavy downpour of rain or rapid snowmelt.
After heavy rain in a mountain canyon, a mudflow can start as a muddy stream that becomes a moving dam of mud and rubble.
Mudflows produce sediments fans at the base of mountain slopes.

15. Mass Movement Hazards

16. Mass Movement Hazards
Mudflow in Sarno, Italy, 1998

17. Earthflows – relatively slow mvts.
Mass Movement Hazards
Earthflows – relatively slow mvts.
most common mass-wasting process.
At the top of a typical earthflow is a steep scarp.
A special type of earthflow called liquefaction occurs in wet, highly porous sediment consisting of clay to sand-size particles weakened by an earthquake.
An abrupt shock increases shear stress and may cause a momentary buildup of water pressure in pore spaces which decreases the shear strength.
A rapid fluidization of the sediment causes abrupt failure.

18. Mass Movement Hazards
Earthflow
Figure 13.16

19. Mass Movement Hazards
3. Debris avalanche
a huge mass of falling rock and debris that breaks up, pulverizes on impact, and continues to travel downslope
The flanks of steep stratovolcanoes are especially susceptible to collapse that can lead to the production of pyrolclastic debris avalanches

20. Before the Yungay Avalanche
Mass Movement Hazards
Before the Yungay Avalanche
Source: Lloyd S. Cluff

21. After the Yungay Avalanche
Mass Movement Hazards
After the Yungay Avalanche
Source: Lloyd S. Cluff

22. Natural triggers of mass-movement hazards include:
torrential rainstorms
earthquakes
volcanic eruptions
Oversteepened slopes
Human triggers of mass movement hazards include:
excessive irrigation
clear-cutting of steep slopes
slope oversteepening or overloading
mining practices

23. Mass movement Hazards To Life And Property
In the United States alone, landslides in a typical year cause more than $1 billion in economic looses and 25 to 50 deaths
Careful planning can often reduce or even eliminate the impact of mass-wasting processes on human environment
Slopes subject to creep can be stabilized by draining or pumping water from saturated sediment