HKDSE Geography/E1/Mass Movement
What better way to start this section with another definition?
Stress and Strength
The occurrence of mass movement is determined by the interplay between two main factors:
Mass movement occurs when stress exceeds strength.
TODO: The triangle thingamajig goes here
Factors that affect the occurence of landslides affect stress, strength or both.
- Water acts as a lubricant to weathered materials and increases pore water pressure. It also adds weight to weathered materials. Thus both the coherence of slope materials and friction will drop during rainfall. When the amount of rainwater reaches a certain level the coherence of the slope materials will break, leading to mass movement.
- Slope angle is another factor. Slope materials move slower on slopes with gentler gradient as the stress is smaller, and faster on slopes with steeper gradient as the stress is greater.
- Some rocks are more resistant to mass movement than others. Granite is more resistant than siltstone.
- The degree of weathering is important. An area of active weathering has more loose weathered materials, which decreases the internal cohesion of slope materials and thus strength, and favours mass movement.
- Vegetation roots prevent mass movement as they strengthen the bonding between soil particles. However, they also secrete organic acid, which weathers rocks below. This will weaken the rocks, decreasing the internal cohesion of slope materials and thus strength.
- Strong earthquakes can trigger earthquakes. The 2008 Sichuan earthquake and 2011 Japanese earthquake are examples.
A scar is left when a landslide occurs. Landslides will be discussed in detail later.
The rocks vary in size, from small grains to huge rocks. Tors are a typical example. If they stand on steep slopes, their bases may be removed by rain, seawater, or some other agent. Strong winds and the construction of roads are also common culprits. They will lose support and the stress will increase greatly, exceeding the strength. Thus they will fall suddenly.
Rock fragments called screes are found at the foothill. A scree slope is formed.
Soil creep is caused by alternate wetting and drying, thermal expansion and contraction or freeze and thaw.
- When soil expands (i.e. wets/freezes/expands thermally), it expands at right angles to the slope.
- When soil contracts (i.e. dries/thaws/contracts thermally), it falls back vertically to the slope of the bedrock.
- The material is moved downslope after each successive movement.
Several good indicators of soil creep include terracettes, bent trees, bulging fences, tilted walls and soil accumulation.