Slope Processes and Development Flashcards
describe a slope in an arid area?
jagged or straight due to mechanical weathering or shestwash
describe a slope in a humid area?
rounder
due to ecumenical weathering
soil creep
and fluvial transport
describe a slope in the tropics?
humid weather means domination of chemical weathering
due to hot wet conditions and avalibility of organic acids
deep flat produced favouring low slope angles
what is revoking?
the superficial and unconsolidated material at earths surface
including soil scree weathered bedrock and deposited material
prone to downslope movement (due to unconsolidated nature)
clay rich are particularly unstable due to ability to hold water
how can soil structure and texture influence slope development?
clay soils hold more water
dee clay on a slope where vegetation has been removed will offer very little resistance to mass movement
how can vegetation affect slope development?
can decrease surface runoff through storage and interception
deforested slopes are exposed to intense erosion and filleting
vegetarion can increase chance of major landslides
dry mass movement
rock fall
fluid mass movement
mud flow
very slow mass movement
soil creep
fast mass movement
avalanche
what is mass movement
large scale movements on the earths surface not accompanied by a moving agent such as a river or ocean wave
what are the most important factors in determining mass movement
gravity
slope angle
pore pressure
what factors influence slope development
rock type climate regality soil aspect vegetation
what two factors cause slope failure
reduction in internal resistance SHEAR STRENGTH of slope
Increase in SHEAR STRESS of the slope (the forces attemption to pull the material downslope)
what is the effect of gravity on mass movement
moves material downslope
sticks partciles to slope
where do slip planes occur
at the junction of two layers at fault lines at a joint along a bedding plane when shear stress is rested than shear strength
Heave/creep
slow
small scale
occurs mostly in winter
indidcual soil particles are pushed to surface by wetting heating or freezing of water
particles move at right angles to the surface as it is the path of least resistance
fall under the influence of gravity when the particles have dried, cooled or water has thawed
net movement downslope
Talus creep
slow movement of fragments on scree slope