- 2064 Jestha (old course) · 3 marks
Slope orientation and discontinuities for stability
Short answer
Stability depends on discontinuity orientation relative to slope face. Plane sliding is likely when a discontinuity strikes parallel (±20°) to the face and dips out with slope angle > dip > φ. Opposite dips and dips less than φ are stable; two intersecting joints plunging out with line of intersection between slope angle and φ produce wedge failure.
Discuss in brief the relation between hill slope and orientation of discontinuities to investigate the slope stability condition.
Stability of a rock slope depends on how the discontinuities are oriented relative to the slope face (dip and dip direction), and on the friction angle of the discontinuities.
| Relation | Condition | Stability |
|---|---|---|
| Dip direction same as slope, discontinuity dip less than slope face angle but more than | Unstable (plane sliding) | |
| Dip direction same as slope, dip less than | Stable | |
| Dip direction opposite to the slope (dipping into the hill) | Generally stable, but toppling is possible in steep dips | |
| Dip steeper than slope (dip > face angle) | Stable (no daylight) | |
| Strike parallel to the slope | within | Most critical |
| Strike perpendicular to the slope | Stable | |
| Two joints whose intersection plunges out of the face | Wedge failure |
UNSTABLE (dip out of slope) STABLE (dip into slope)
\ /
\ bedding / bedding
______\______ ____/_______
In road cuts, the cut slope should not be steeper than the dip of bedding or foliation when these dip out of the slope. This is investigated using a stereonet (kinematic analysis) before design.
✓ Answer checked by Claude Opus 5.5 (high effort)
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