Hillslope Materials and Processes¶
Selby, M. J., & Hodder, A. P. W. (1993). Hillslope Materials and Processes. Oxford University Press.
Cited by¶
2 citations across 2 artifacts.
Each citation links to the sentence it supports in the citing article.
Domain-specific¶
- Mass Wasting
- Mass wasting is the geomorphic process by which rock, regolith, or soil moves downslope under the direct pull of gravity once the driving forces — primarily the downslope component of gravitational stress on a candidate failure surface — exceed the resisting forces, which are shear strength composed of cohesion, internal friction, and pore-water pressure effects on effective normal stress
This sourceSelby's hillslope treatment grounding rock- and soil-strength analysis in gravitational stress and pore-water (effective) stress after Terzaghi.
Supported in partVerified against the work's full text
“and other forms of instability. [Gravitational] stresses [Gravitational] stresses at a point within a rock”
- Mass wasting is the geomorphic process by which rock, regolith, or soil moves downslope under the direct pull of gravity once the driving forces — primarily the downslope component of gravitational stress on a candidate failure surface — exceed the resisting forces, which are shear strength composed of cohesion, internal friction, and pore-water pressure effects on effective normal stress
- Slope-Former
- Bedding, joints, cement, pore water, climate, exposure time, base-level incision, and neighboring support all condition the result.
This sourceAuthoritative treatment of rock mass strength, weathering, hydrology, slope form, and mass movement.
- Bedding, joints, cement, pore water, climate, exposure time, base-level incision, and neighboring support all condition the result.
Verification¶
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Registry ID ref:a7aa7fa7c3e9 · see in the full table