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Question 1
ప్రశ్న 1
A proposed water-supply installation lies below a slope mapped as highly susceptible to landsliding. Which statement correctly distinguishes landslide susceptibility from landslide risk?
Explanation:
Landslide susceptibility expresses the relative tendency of terrain to experience landsliding based on relevant conditions. Such conditions can include geology, slope geometry, drainage and evidence of previous movement. Landslide risk concerns the potential consequences of hazardous landslide events for exposed people, structures and infrastructure. A highly susceptible but unoccupied slope may have different risk implications from a similar slope supporting an important water-supply facility. Susceptibility mapping alone does not specify the exact timing of a future failure.
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Question 2
ప్రశ్న 2
A highway authority uses a Geological Survey of India landslide-susceptibility map to screen a proposed hill-road corridor. Which interpretation of the map is most appropriate?
Explanation:
Landslide-susceptibility maps identify areas having relatively favorable or unfavorable conditions for slope instability. The Geological Survey of India prepares susceptibility information for landslide-prone areas using geological and terrain-related factors. Regional maps are useful for preliminary route planning and identifying locations requiring special attention. Their scale and input data may not resolve individual weak seams, localized seepage or small excavation-related failures. Detailed field mapping and site-specific stability evaluation remain necessary for important engineering works.
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Question 3
ప్రశ్న 3
A soil slope develops a spoon-shaped failure surface concave upward, and the displaced mass moves downward while rotating backward near its head. Which mass-movement mechanism is indicated?
Explanation:
A rotational slide develops along a curved failure surface that is generally concave upward. The moving mass undergoes rotational displacement rather than simple translation along a planar surface. Backward tilting near the head is a common feature of this movement. Rotational failures frequently occur in soil slopes and weak geological materials. Their investigation requires assessment of slope geometry, material shear strength and groundwater conditions.
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Question 4
ప్రశ్న 4
A rock mass on a hillside moves downslope approximately as a coherent slab along a persistent, nearly planar bedding surface. Which classification is most appropriate?
Explanation:
A translational slide involves movement along a comparatively planar failure surface. Persistent bedding, joints or fault planes may provide such surfaces in rock masses. The displaced material can move as a coherent block or become fragmented during movement. Its stability depends on discontinuity orientation, shear strength, water pressure and external loading. Recognition of the controlling plane is necessary before designing anchors, drainage or other stabilization works.
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Question 5
ప్రశ్న 5
Following intense rainfall, a steep drainage channel carries a rapidly moving mixture of water, soil, rock fragments and organic material toward a road crossing. Which hazard and mitigation approach are most appropriate?
Explanation:
Debris flows involve rapid downslope movement of mixtures containing water and substantial solid material. Intense rainfall can mobilize loose deposits and increase water flow in steep channels. These flows may travel beyond their source slopes and affect roads, culverts and settlements downstream. Engineering protection can include source-area management, channel works, suitable debris barriers or avoidance of dangerous flow paths. The measures must be designed for plausible flow volume, impact and deposition rather than assuming that an ordinary storm-water drain will contain every debris flow.
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Question 6
ప్రశ్న 6
A highway cutting in jointed rock experiences occasional detachment of blocks that fall, bounce and roll toward the carriageway. Which combination of measures is most appropriate for managing this hazard?
Explanation:
Rockfall commonly develops when blocks detach along joints, fractures or bedding surfaces. The detached material may fall freely, bounce or roll downslope. Scaling and suitable anchoring can reduce the likelihood of release from particular source areas. Protective mesh, barriers and catch ditches can help control the consequences of falling material. Their selection requires assessment of rock-block dimensions, trajectories, impact energies and available space.
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Question 7
ప్రశ్న 7
A steep rock cut contains tall, narrow rock columns separated by persistent near-vertical joints. Several columns are inclined outward and show potential forward rotation about their lower edges. What instability mechanism should be investigated?
Explanation:
Toppling occurs when a rock block or column rotates forward about a pivot near its lower part. Steep discontinuities can divide a rock mass into columns susceptible to this movement. Joint orientation, block dimensions and contact forces influence the possibility of rotation. Water pressure or disturbance at the base may contribute to instability. Appropriate investigation should establish the geometry before selecting anchorage, slope modification or protective measures.
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Question 8
ప్రశ్న 8
A river progressively erodes the toe of a natural hillside containing weathered rock and soil. What is the most important effect of continued toe erosion on slope stability?
Explanation:
The toe of a slope can provide important support to the material above it. River erosion may progressively remove this supporting material. The resulting geometry can increase driving forces or reduce resistance along potential failure surfaces. Weathered or fractured ground may be particularly vulnerable to such changes. Erosion control, toe protection and slope-stability analysis should therefore be considered together.
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Question 9
ప్రశ్న 9
A hillside remains stable during dry weather but develops tension cracks and movement after prolonged rainfall. Piezometers indicate that groundwater pressure has risen along a potential sliding surface. Which mechanism most directly explains the reduction in stability?
Explanation:
Shear resistance along a soil or rock discontinuity depends partly on effective normal stress. Increasing pore-water pressure reduces effective normal stress when the total normal load remains unchanged. Lower effective normal stress can reduce frictional resistance and favor movement. Rainfall may also increase seepage forces or soften susceptible geological materials. Drainage and monitoring are therefore important elements of slope stabilization where groundwater is influential.
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Question 10
ప్రశ్న 10
For a simplified planar slope-stability assessment, the total weight of a potentially sliding block is W = 1000 kN on a plane inclined at 30 degrees. Take sin(30 degrees) = 0.500 and cos(30 degrees) = 0.866. The total pore-water force normal to the plane is U = 200 kN, the cohesive resistance along the plane is cA = 100 kN, and tan(phi) = 0.50. Neglect other forces and use FS = [cA + (W cos(theta) - U)tan(phi)]/[W sin(theta)]. What is the factor of safety?
Explanation:
The driving force parallel to the slope is W sin(theta) = 1000(0.500) = 500 kN. The total normal force is W cos(theta) = 1000(0.866) = 866 kN. Subtracting the specified pore-water force gives an effective normal force of 866 - 200 = 666 kN. The available resisting force is 100 + 666(0.50) = 433 kN. Therefore FS = 433/500 = 0.866, or approximately 0.87, indicating inadequate stability under the explicitly stated simplified conditions.
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Question 11
ప్రశ్న 11
A road embankment has developed movement along a wet, weak foundation layer. Investigation identifies surface-water entry, elevated internal pore pressure and excessive fill loading near the slope crest. Which combination of remedial measures is most defensible?
Explanation:
Slope remediation should address the actual causes of movement rather than merely conceal surface cracks. Surface drainage can reduce avoidable infiltration into the unstable mass. Subsurface drainage may lower pore pressure where the hydrogeological conditions permit it. Slope regrading, unloading or properly designed toe support can improve the balance between driving and resisting forces. The combination must be selected through stability analysis and a safe construction sequence.
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Question 12
ప్రశ్న 12
A rock slope contains potentially detachable blocks bounded by persistent joints. A stabilization design proposes installing rock bolts. Which arrangement most directly improves the stability of the identified blocks?
Explanation:
Rock bolts can connect potentially unstable blocks to more competent portions of the rock mass. Their orientation should consider the geometry of the relevant discontinuities. Adequate anchorage length and capacity are needed beyond potential release surfaces. Joint filling, groundwater and the possibility of larger-scale movement also influence the design. Rock bolting may be combined with mesh, drainage and other measures where appropriate.
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Question 13
ప్రశ్న 13
Geological investigation identifies evidence of geologically recent surface displacement along a fault crossing a proposed critical water-treatment facility. What hazard requires particular consideration beyond ordinary earthquake ground shaking?
Explanation:
Earthquakes may produce ground shaking over broad regions. Fault rupture reaching the surface can additionally create concentrated horizontal or vertical displacement. A structure crossing the rupture zone may experience severe differential ground movement. Conventional strengthening against shaking does not automatically eliminate this direct rupture hazard. Fault investigation and consideration of suitable siting or avoidance are therefore important for critical infrastructure.
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Question 14
ప్రశ్న 14
Two sites experience the same regional earthquake, but one is founded on stiff rock and the other on deep soft sediments. The soft-sediment site records stronger shaking over a frequency range relevant to its structures. Which explanation is most appropriate?
Explanation:
Earthquake magnitude characterizes the size of a seismic event rather than the shaking at a particular site. Local geological conditions influence how seismic waves propagate and interact near the ground surface. Soft sediments and sedimentary basins may amplify motion within particular frequency ranges. Such amplification can affect the dynamic response of structures founded on the ground. Site-specific seismic and geotechnical investigation is therefore important when evaluating earthquake-related hazards.
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Question 15
ప్రశ్న 15
A proposed pumping-station foundation lies on loose, saturated sand in an earthquake-prone area. Which statement correctly explains the basic liquefaction mechanism?
Explanation:
Loose saturated granular soils can be susceptible to liquefaction during sufficiently strong cyclic loading. Under conditions where drainage is restricted, shaking can generate excess pore-water pressure. The rise in pore pressure reduces effective stress carried by the soil skeleton. This may cause substantial loss of stiffness and shear resistance. Liquefaction susceptibility depends on soil characteristics, groundwater conditions and the severity and duration of shaking.
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Question 16
ప్రశ్న 16
An idealized saturated sand element has an initial vertical effective stress of 80 kPa. During undrained earthquake shaking, excess pore-water pressure rises by 60 kPa while total vertical stress is assumed constant. Using ru = excess pore-water pressure/initial effective stress, determine ru and the remaining vertical effective stress.
Explanation:
The excess pore-pressure ratio is defined in the question as the excess pore pressure divided by the initial effective stress. Substituting the given values gives ru = 60/80 = 0.75. Because the total vertical stress remains constant, the increase in pore pressure reduces effective stress by the same amount. The remaining effective stress is therefore 80 - 60 = 20 kPa. This indicates a major reduction in effective stress but does not by itself establish complete liquefaction of the soil.
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Question 17
ప్రశ్న 17
After an earthquake, a riverbank founded on loose saturated sand shows lateral cracks and permanent horizontal ground displacement toward the river, although the original ground slope was gentle. Which mechanism is most likely?
Explanation:
Liquefaction can cause substantial reduction in the strength of saturated granular soils. Where a free face such as a riverbank exists, overlying ground may move laterally toward it. This movement is known as lateral spreading. It can damage foundations, roads, pipelines and buried utilities even on gently sloping ground. Hazard assessment should consider the soil profile, groundwater level, seismic demand and the geometry of nearby slopes or free faces.
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Question 18
ప్రశ్న 18
A proposed reservoir pumping station is underlain by loose saturated sand with assessed liquefaction susceptibility. Which mitigation strategy is most defensible before final foundation design?
Explanation:
Liquefaction mitigation should be selected using site-specific soil and earthquake information. Appropriate densification can reduce liquefaction susceptibility in suitable granular deposits. Some drainage or ground-improvement systems may help control pore-pressure response or associated deformation. Foundation design must also address possible settlement and lateral ground movement. No single mitigation method should be assumed effective for every soil profile or seismic condition without investigation.
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Question 19
ప్రశ్న 19
A proposed underground water-storage structure lies over limestone containing solution cavities, with surface depressions and evidence of past sinkhole activity. Which geological hazard is most relevant?
Explanation:
Limestone can undergo dissolution where groundwater chemistry and flow conditions are favorable. Progressive dissolution may enlarge joints and form underground cavities. Collapse of material above such voids can create sinkholes or other ground depressions. The hazard depends on cavity dimensions, cover material, groundwater changes and geological structure. Investigation may require geological mapping, suitable geophysics and boreholes before considering avoidance or engineered treatment.
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Question 20
ప్రశ్న 20
An urban area on thick alluvial deposits has experienced prolonged intensive groundwater abstraction. Monitoring shows groundwater-head decline and gradual regional land subsidence. Which explanation is most appropriate?
Explanation:
Groundwater extraction can lower hydraulic heads within aquifer systems. Lower pore-water pressure can increase effective stress in compressible sediments. Fine-grained layers may consolidate or compact under the increased loading. Compaction can produce gradual lowering of the land surface and damage infrastructure. Groundwater management and deformation monitoring are important because some aquifer-system compaction may be irreversible.
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Question 21
ప్రశ్న 21
Historical records indicate abandoned shallow underground mine workings beneath a proposed road alignment. What is the most appropriate engineering-geological response?
Explanation:
Abandoned mine openings may remain as underground voids or partially collapsed zones. The overlying rock and soil can deform or collapse if support is inadequate. Surface conditions alone may not reveal the location or condition of buried workings. Historical records, appropriate geophysical surveys and targeted drilling can help characterize the hazard. Remediation may involve avoidance, engineered filling or other measures based on the actual subsurface conditions.
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Question 22
ప్రశ్న 22
A municipality suspects gradual ground subsidence near a group of production wells. Which monitoring strategy is most appropriate for assessing the spatial extent and possible groundwater-related causes?
Explanation:
Land subsidence can affect a broad area and may develop gradually. Repeated leveling, GNSS measurements or InSAR observations can help identify spatial and temporal deformation patterns. Groundwater-head records provide information about changes in hydraulic conditions. Geological and geotechnical data help establish which strata may be compacting. Monitoring results should be interpreted together because surface displacement alone does not uniquely establish the cause.
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Question 23
ప్రశ్న 23
A road embankment in highly erodible soil is experiencing progressive gully erosion because runoff is concentrated at an unprotected drainage outlet. Which preventive measure is most appropriate?
Explanation:
Concentrated runoff can detach and transport soil particles from vulnerable slopes. Repeated erosion may deepen a gully and undermine roads or embankment toes. Proper drainage design should control the location and energy of discharged water. Lining, grade-control structures and suitable vegetation can help limit erosion where appropriate. The selected measures should consider soil erodibility, catchment runoff and possible downstream effects.
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Question 24
ప్రశ్న 24
A monitored landslide shows 15 mm of downslope displacement over a 30-day observation interval. Assuming an average movement rate over this interval, what is the rate, and what conclusion can reasonably be drawn?
Explanation:
Average displacement rate is calculated by dividing the measured movement by the observation interval. The recorded displacement is 15 mm over 30 days. Therefore the average movement rate is 15/30 = 0.50 mm/day. A measured rate provides useful information about slope behavior but cannot alone establish the timing of failure. Interpretation should consider changes in rate, rainfall, groundwater pressure, measurement accuracy and the established monitoring action levels.
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Question 25
ప్రశ్న 25
A major landslide in a narrow mountain valley temporarily blocks a river and forms an impounded lake upstream. Which additional geological-hazard consequence requires particular attention?
Explanation:
Large landslides can obstruct rivers and create temporary natural dams. Water may accumulate upstream of the blockage and increase the hydraulic loading on the debris. Overtopping, erosion or internal instability can cause the blockage to fail. Sudden release of stored water can produce dangerous downstream flooding. This is an example of a cascading geological hazard that requires monitoring, assessment of dam stability and suitable risk-reduction measures.
వివరణ:
Answer Key సమాధానాల పట్టిక
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Question 1 ప్రశ్న 1Answer: B. Susceptibility describes the relative tendency of ground to undergo landsliding, while risk also considers hazardous events, exposed assets and their vulnerability. సమాధానం: B.
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Question 2 ప్రశ్న 2Answer: C. The map can identify areas requiring more detailed investigation, but local geology, slope conditions and construction effects must be assessed before design. సమాధానం: C.
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Question 3 ప్రశ్న 3Answer: A. Rotational slide or slump. సమాధానం: A.
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Question 4 ప్రశ్న 4Answer: D. Translational rock slide controlled by a geological discontinuity. సమాధానం: D.
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Question 5 ప్రశ్న 5Answer: C. A debris flow; investigate source areas, drainage paths and possible interception, diversion or appropriately designed protective structures. సమాధానం: C.
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Question 6 ప్రశ్న 6Answer: B. Assess scaling of unstable blocks, rock anchoring where suitable, protective mesh or barriers and adequately designed catch ditches. సమాధానం: B.
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Question 7 ప్రశ్న 7Answer: A. Rock toppling controlled by discontinuity geometry and rotational instability. సమాధానం: A.
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Question 8 ప్రశ్న 8Answer: D. It can remove supporting material and modify slope geometry, increasing the possibility of sliding or collapse. సమాధానం: D.
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Question 9 ప్రశ్న 9Answer: C. Increased pore-water pressure can reduce effective normal stress and available frictional resistance along the sliding surface. సమాధానం: C.
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Question 10 ప్రశ్న 10Answer: B. Approximately 0.87. సమాధానం: B.
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Question 11 ప్రశ్న 11Answer: D. Evaluate surface and subsurface drainage, suitable reduction or redistribution of driving loads, and engineered toe support or reinforcement where required. సమాధానం: D.
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Question 12 ప్రశ్న 12Answer: A. Install appropriately oriented bolts that cross potential release surfaces and develop adequate anchorage in more stable surrounding rock. సమాధానం: A.
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Question 13 ప్రశ్న 13Answer: C. Potential direct surface fault rupture and differential ground displacement across the facility footprint. సమాధానం: C.
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Question 14 ప్రశ్న 14Answer: B. Local soil and basin conditions can modify seismic-wave motion and amplify shaking at some frequencies, even during the same earthquake. సమాధానం: B.
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Question 15 ప్రశ్న 15Answer: D. Strong cyclic loading may generate excess pore-water pressure in susceptible saturated soil, reducing effective stress and shear resistance. సమాధానం: D.
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Question 16 ప్రశ్న 16Answer: A. ru = 0.75 and remaining effective stress = 20 kPa. సమాధానం: A.
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Question 17 ప్రశ్న 17Answer: C. Liquefaction-induced lateral spreading toward a free face. సమాధానం: C.
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Question 18 ప్రశ్న 18Answer: B. Investigate appropriate soil densification, drainage or other ground-improvement measures and evaluate foundation performance under potential liquefaction-induced deformation. సమాధానం: B.
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Question 19 ప్రశ్న 19Answer: D. Karst-related ground subsidence or localized collapse due to dissolution cavities and loss of supporting ground. సమాధానం: D.
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Question 20 ప్రశ్న 20Answer: A. Lower pore pressure can increase effective stress in compressible aquifer-system sediments and cause compaction and ground-surface lowering. సమాధానం: A.
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Question 21 ప్రశ్న 21Answer: B. Investigate the location and condition of voids, possible roof collapse and ground subsidence before selecting avoidance, ground treatment or structural measures. సమాధానం: B.
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Question 22 ప్రశ్న 22Answer: C. Combine repeated geodetic or InSAR displacement observations with groundwater-head monitoring and appropriate subsurface information. సమాధానం: C.
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Question 23 ప్రశ్న 23Answer: D. Provide properly designed runoff collection and outlet protection, with appropriate erosion-control lining, vegetation or grade-control measures. సమాధానం: D.
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Question 24 ప్రశ్న 24Answer: A. 0.50 mm/day; the slope is moving, but the rate alone does not establish when or whether rapid failure will occur. సమాధానం: A.
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Question 25 ప్రశ్న 25Answer: C. Failure or overtopping of the landslide dam may produce rapid downstream flooding, so monitoring, hazard assessment and appropriate emergency measures are necessary. సమాధానం: C.
