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These slide-shows are all on the blog if you wish to copy any notes from them; we will not be stopping in class for you to do this. ‘Mass movements’ is the term used to define the different ways that weathered material can alter the scenery. The two forces acting on the material are;-.
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These slide-shows are all on the blog if you wish to copy any notes from them; we will not be stopping in class for you to do this ‘Mass movements’ is the term used to define the different ways that weathered material can alter the scenery. The two forces acting on the material are;- Friction, which stops them sliding downhill too fast. Gravity, which pulls the particles down.
Four main factors that influence mass movements;- • How much water is involved in the action. • How much of an angle is needed on the slope. • How quickly the movement happens. • The amount of vegetation cover is also important in some types of movement.
ROCKFALLS;- read pages 1-4 and answer the questions on page 4 Then read higher notes on pages 78-86 Answer questions 1, 2bcd,3,5,6, on page 139-140 use pages 72-86 to help you
1. What angles are rockfalls most likely to happen at? 2. Which of the two forces is the dominant one? 3. Which secondary processes are very important too? 4. So what condition ought the rock face to be in if a rockfall is to happen? Four more questions after the answers to these!
2. Gravity is more effective here than friction. 1. The best angle is between 70 and 90 degrees from horizontal. 3. Freeze-thaw and frost-shattering are important processes. 4. The face should be well- jointed or cracked for rockfalls to happen.
5. What angle does scree usually initially settle at? 6. Explain what is meant by ‘size- sorting’ and why it happens. 8. What is the usual angle of an inactive scree slope? 7. Why will weathering of the rock face cease in time?
6. Particles travel down the slope depending on their weight and density. Lighter ones finish nearer to the face, heavier ones travel further, often moved by rolling over smaller ones. 5. Scree settles between 34 and 40 degrees, usually. 8. The inactive slope consolidates at 37 degrees where it usually grasses over. 7. If scree covers the rock face, freeze-thaw cannot act and weathering stops.
Climbers call these types of screes ‘stone chutes’. Their technical name is talus slope.
1.What two roles does heavy rainfall play? 2. Where can the slip plane/ a.k.a. glide plane be found? 3.How does the result of this movement look different to a rockfall? 4.Slumps- special kinds of slides- have a different kind of slip plane- in what way? 5. What is the difference in the motion of the material in slumps?
1. It lubricates the slip plane and makes the material heavier and likely to move. 2. The slip plane is below the surface. 3. There are ‘bald’ spots visible on the slip plane and there is no sorting. Material moves as a ‘oner’. 4. A shear is curved, steeper at the top than the bottom. 5. Slumped ground has rotated whereas slides travel down in a straight line.
The Quiraing in Skye shows spectacular rotational slumping. Spot the tourists?
1. How gentle a slope can mudflows start on? 2.What angles are more likely? 3. What shape does the material stop in? 5.How do you describe the speed of a mudflow? 4. Describe the two factors that help create mudflows. 6. What condition does the surface below the flow have to have?
1. They can start on a slope as gentle as 5 or 6 degrees. 3. The material stops in a lobe/fan shape. 2. Angles over 10 degrees are more common. 5. Mudflows happen very quickly indeed! 4. They need high rainfall and little vegetation cover. 6. The lower layers need to be impermeable to water.
This mudflow happened several years before the photo was taken- the scars are still very visible!
1.What angle of slope does this require? 3.Why do particles not travel back at the same angle as they heave? 2. Define the term ‘heave’. 4.Describe how biological activity may enhance the activity. 5. Describe what terracettes look like. 6.Describe four results of soil creep.
1. Angles over as little as 5o but >6 degrees are most susceptable. 3. Gravity (and the effects of contraction) are the dominant forces here. 2. Heave is the upward motion of particles. 4. Plant roots and burrowing animals help the soil to move. 5. Terracettes are small-scale ridges parallel to the slope. 6. See the next slide for the answer.
6. a). Fence and telegraph posts lean down-slope as their supports are undermined by the creep. ( note these are the same effect) b). Soil piles up behind walls, creating deeper pockets, pushing walls over in time. ( note there are two effects here!) c). Roads may crack open parallel to the slope angle, and will need frequent repair. d). Terracettes spoil the smooth surface of fields, and affect land use.
