Uploaded by Tiffini AnáMaria Thomas

Landslide Handout

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Name:
Date: 20/ / .
Geography
Form 3:
Mass Movements
Definition: The movement of soil and rock debris down a slope, due to gravity and the lubricating action of
water.
This movement is both fast and slow and the degree of movement is influenced by:
1. The angle of the slope
2. The nature of the material
3. The structure of the rocks
Mass wasting is induced by:
1. Steep slopes
2. Heavy rainfall
3. Human interference with natural vegetation
Slow Movement: Soil Creep
֎ Define what is soil creep.
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What are some indicators of soil creep?
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Factors affecting soil creep
In temperate environments soil can creep downhill at between 1mm and 2mm per year, but in tropical regions
it is quicker, perhaps 3-6mm. In cold semi-arid areas, it is even faster. Soil creep is caused by:
 The alternate wetting and drying of the soil
 The alternate freezing and thawing of the soil
The expansion and contraction in soil is the main cause of soil creep. The wetter the soil is, the faster it is able
to flow. Therefore, soil creep is much more active in wet areas of the world. In regions of seasonal wetting and
drying the soil contracts when dry and expands when wet; wet soil moves more easily. Rain-wash and rain
splash can also move soil downslope.
֎ What is the difference between rain-wash and rain splash?
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Rapid Movement – Landslide
 Define what is a landslide.
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Ms. T. Thomas
1
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Physical/Natural Causes of Landslides
1. Unconsolidated material on a slope: In 1998, the rains from Hurricane Mitch caused devastating
mudflows from the unconsolidated ash slopes of the Casita volcano which killed 1900 people and
destroyed the town of Posoltega in Nicaragua.
2. Slippery rocks like shale and clay: Shale and clay are both slippery, esp. when wet. Wet clay acts as a
lubricant, so rock beds above it slip down more easily while shale is made of very thin layers, so it slides
easily.
3. Bedding planes being roughly parallel to the slope surface: This makes it easy for material to slip
downwards along the bedding plane. Gravity can exert its force easily on the rock beds. The effects are
even greater if the rock layer below is impermeable. This keeps all the moisture in the top layer of the
rock, so it becomes saturated quickly.
4. The base of a slope being undercut by river or coastal erosion: Rivers meander and undercut their
valley sides. If the slope above is made of unconsolidated material or very wet material and becomes
unsupported it is much more likely to collapse. Coastal erosion can produce a similar effect.
5. Earthquakes: 1977, a 7.7 earthquake shook parts of Peru. Ice and snow near the summit of Huascaran
formed an avalanche which picked up rocks and boulders along the way. It hit the town of Yungay in the
Rio Santo Valley killing and destroyed the town.
6. Volcanic eruptions: Volcanic ash and mudflow (lahars) move rapidly destroying and killing anything in
their paths.
7. Heavy rainfall: all of the mentioned are made worse by the surface material becoming saturated, which
makes it heavier and reduces friction. Water does two things; it adds weight to the material, making the
slope less stable and it decreases friction which helps movement downslope.
Human causes of landslides
1. Building on unstable slopes: _____________________________________________________________________________________
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2. Undercutting the base of a slope by road building: _____________________________________________________________
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3. Dumping waste material: _________________________________________________________________________________________
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4. Building dams: _____________________________________________________________________________________________________
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ACTIVITY: MASS WASTING
Ms. T. Thomas
2
1. What measures can be taken to minimize the effects of soil creep?
2. Discuss the causes and consequences of a particular landslide in the Caribbean region.
3. Why do you think that a landslide is more likely to occur in a less developed country versus that of a
more developed county?
Ms. T. Thomas
3
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