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Daylighting Bedding and a Fault Gouge in an Idukki Road Cut

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Daylighting Bedding and a Fault Gouge in an Idukki Road Cut

A 12 m high road cut near Idukki exposes garnet-biotite gneiss. Bedding S0 strikes N30°E and dips 40°SE. A spaced cleavage S1 strikes N60°E and dips 70°NW. The cut face strikes N30°E and dips 75°SE. Quartz veins are folded, and a 30 cm thick fault gouge zone strikes N80°E and dips 60°S; slickensides on its surface plunge 20° toward N60°E. The slope is above a two-lane highway, and monsoon rainfall exceeds 2500 mm/year. During the last monsoon, a 20 m3 wedge of rock and soil slid onto the shoulder. Joints parallel to the cut face are open and clay-filled. No drainage measures are present, and gully erosion is active. The highway authority plans to remove the toe and steepen the cut to widen the road.

1. Assess the kinematic feasibility of planar sliding on bedding and on the fault. Use the orientation data and state what additional data you would need.

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For planar sliding, a discontinuity must strike nearly parallel to the slope face, dip out of the slope, and dip less steeply than the face, and there must be a release surface. Bedding S0 strikes N30°E, the same as the cut face, and dips 40°SE; the face dips 75°SE. Bedding therefore daylights in the face and is kinematically feasible for planar sliding. The open joints parallel to the face can act as release surfaces.

The fault strikes N80°E, about 50° from the face, and dips 60°S. It is not parallel to the face and is more likely to form a lateral release or one boundary of a wedge than a simple planar sliding plane. The slickenside plunge gives the slip direction but not the sense of movement.

Additional data needed: friction angle and cohesion of bedding and joints, persistence and infilling of the joints, water pressure along the sliding plane, and whether the 20 m3 failure was a planar slide or a wedge. Without those data, the orientation analysis shows feasibility, not failure probability.

2. Reconstruct the deformation history from S0, S1, folding, fault gouge, and joints, and explain which structures most likely controlled the 20 m3 failure.

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S0 is primary bedding. The quartz veins are folded, so folding postdates vein emplacement. S1 strikes N60°E, oblique to S0; if it is axial planar to the folds, cleavage formed during the same folding event. The fault gouge cuts cleavage and is therefore later than the folding and cleavage. The open joints parallel to the cut face are youngest; they are likely stress-release joints formed during excavation and unloading.

The failure is best explained by daylighting bedding plus clay-filled release joints. Monsoon water entering the open joints raises water pressure, reduces effective normal stress on the bedding plane, and allows a wedge to slide. The fault gouge may have provided a weak lateral boundary, but its orientation does not favour it as the main sliding plane. The active gully erosion and absence of drainage increased water availability.

3. Recommend a stabilization and monitoring programme before widening. Include structural and hydrogeological measures and explain the priority order.

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The first priority is to abandon the plan to remove the toe and steepen the cut; that would remove support and increase daylighting. Stabilization should proceed in this order:

  1. Surface drainage: intercept runoff above the cut with drains, seal gullies, and line channels so water does not enter open joints.
  2. Subsurface drainage: install horizontal drains and weep holes in the slope to lower water pressure on the bedding plane.
  3. Support: use benching, rock bolts, mesh, and shotcrete where necessary; retain the toe with a buttress or gabion wall rather than removing it.
  4. Protection: erect a catch fence or rockfall barrier above the highway and limit blast vibration during widening.
  5. Monitoring: install piezometers, crack meters, and survey markers; inspect during and after monsoon; set trigger levels for movement and water pressure.

The sequence matters because drainage and toe support reduce driving forces before expensive structural support is added. Monitoring must continue through at least one monsoon.