Slope Development-4 Elements, 3 Classification, 2 Approaches & 3 Theories YouTube Lecture Handouts
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Elements of Slope Profile
Classification of Slope
Approaches to Slope Development
Models of Slope Evolution
Slope Decline Theory (Davis) | Slope Replacement Theory (Penck) | Parallel Retreat Theory (King) | |
Region of Study | NW Europe & Northeast USA | Slopes of Andes & Alps | Slopes of South Africa |
Climate | Humid areas | Tectonic Areas | Semi-arid landscape; sea cliffs with wave-cut platform |
Description of Slope | Initially has steepest slope & with time angle decreases | Reduction in maximum angle as gentler lower slopes erode back | Maximum angle remains constant like slope facets apart from lower ones which increases concavity |
Davis | Penck | King | |
Process | By stage 4, land turns convex-concave slope | Scree slope B will replace slope A; slope C replaces slope B | Flash floods remove concave debris on slope pediment |
Changes over Time | Intermediate denudation assumes rapid land uplift. | Starts with straight rock slope with equal weathering overall. | Considering two facets of slope viz. , gentle concave lower slope, & convex upper slope. |
Slope Failure – Causes & Process
✍ Manishika