IS 14243 Part 11995AI Search Enabled✦ AI Generated

Guidelines for selection and development of the site for building in hill areas, Part 1: Microzonation of urban centres

IS 14243 Part 1 (1995) provides comprehensive guidelines for microzonation of urban centres in hill areas, focusing on assessing geological, geomorphological, hydrological, and seismic factors to identify zones prone to ground failures and inundations. It aids engineers, planners, and developers in selecting and developing safe building sites by delineating stable and unstable areas, considering natural and human-induced hazards to minimize structural damage and enhance urban resilience.

15Sections
49Clauses Indexed
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1995Edition
Rock MechanicsCategory
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What This Standard Covers

IS 14243 Part 1 (1995) provides comprehensive guidelines for microzonation of urban centres in hill areas, focusing on assessing geological, geomorphological, hydrological, and seismic factors to identify zones prone to ground failures and inundations. It aids engineers, planners, and developers in selecting and developing safe building sites by delineating stable and unstable areas, considering natural and human-induced hazards to minimize structural damage and enhance urban resilience.

Who Uses This Standard

  • Geotechnical Engineers
  • Urban Planners
  • Civil Engineers
  • Disaster Management Professionals
  • Geologists
  • Structural Engineers
  • Environmental Consultants

Key Topics Covered

Microzonation mapping of urban centres
Assessment of seismic hazard classes
Evaluation of geological and geomorphological conditions
Hydrological analysis including flood and inundation risks
Identification of ground failure types (landslides, rock falls, debris flows)
Impact of human activities on slope stability
Slope stability criteria and classification
Effects of extreme hydro-meteorological events
Site selection criteria for building development
Preparation of topographic, slope, and hydrological maps
Evaluation of reclaimed and waste disposal areas
Guidelines for safe construction in hill terrains

Table of Contents

1Scope

IS 14243 (Part 1) - Scope & Key Specifications

1. Seismic Hazard Classification (Clause 4.2 & Table 1)

  • Based on Peak Ground Acceleration (PGA) at urban center:
PGA RangeSeismic Hazard ClassCondition
PGA < 0.10 gI (Low)-
0.10 g < PGA < 0.25 gII (Moderate)No active faults within 10 km
PGA > 0.25 gIII (High)No active faults within 10 km
PGA > 0.25 gIV (Extreme)Active fault within or within 10 km
  • Design earthquake and stability analysis must be based on this classification.

2. Ground & Soil Considerations (Clause 4.7)

  • Check long-term settlements in reclaimed/solid waste disposal areas.
  • Settlement effects due to soil consolidation and organic material must be evaluated under in-situ seasonal conditions.

3. Geomorphology (Clause 3.4.1.1.2)

  • Terrain evaluation based on:
    • Slope categories:
      • Very gentle: 0°–15°
      • Gentle: 15°–25°
      • Moderately steep: 25°–35°
      • Steep: 35°–45°
      • Very steep: >45°
    • Relative relief: scarp faces, valley shape, depression zones, inundation areas.

Summary Diagram: Seismic Hazard Classification Flow

flowchart TD
    A[PGA Measurement] --> B{PGA Value}
    B -->|<0.10g| C[Class I - Low]
    B -->|0.10g to 0.25g| D{Active Fault?}
    D -->|No| E[Class II - Moderate]
    D -->|Yes| F[Class III - High]
    B -->|>0.25g| G{Active Fault within 10 km?}
    G -->|No| H[Class III - High]
    G -->|Yes| I[Class IV - Extreme]

Note: Use seismic hazard class to determine design

2Primary Factors for Microzonation Maps

Primary Factors for Microzonation Maps (IS 14243 Part 1)

Key Parameters (Clauses 2.2, 3.1)

  • Scale of base maps depends on:
    • Size of urban center
    • Relief/topography
    • Surficial soil and rock strata
    • Drainage pattern and density
  • Recommended topographic map scales:
    • 1:10,000 scale with 2 m contour intervals for mountainous/high relief areas
    • 1:25,000 scale with 3-5 m contour intervals for moderate relief
  • Base maps must be prepared if unavailable.

Primary Factors Governing Microzonation (Clause 3.1)

  • Regional and local geology
  • Hydrological conditions (water table, drainage)
  • Human activities (mining, construction)
  • Urban size and building types

Seismic Hazard Classification (Clause 4.2, Table 1)

PGA Range (g)Seismic Hazard ClassNotes
< 0.10I (Low)
0.10 – 0.25II (Moderate)No active faults within 10 km
> 0.25III (High)No active faults within 10 km
> 0.25IV (Extreme)Active fault within or within 10 km distance

Stability Assessment (Clause 4.3)

  • Demarcate homogeneous lithology zones (hard rock, soft rock, terraces, fans, flood plains, slide debris).
  • Slope stability criteria:
    • Rocky terrain: slopes < 25° generally stable
    • Surficial deposits: dry slopes < 20° generally stable
  • Identify high water table zones prone to liquefaction or settlement.

Summary Diagram: Microzonation Factors

graph TD
  A[Microzonation Maps] --> B[Base Map Scale]
  A --> C[Geology & Lithology]
  A --> D[Hydrology & Water Table]
  A --> E[Seismic Hazard Class]
  A --> F[Topography & Slope]
  A --> G[Human Activities]

  B --> B1[1:10,000 (High Relief)]
 
3Regional and Local Geology

IS 14243 Part 1: Key Points on Regional and Local Geology


1. Regional Geology (Clause 3.2)

  • Study area around urban center for hazard intensity (earthquakes, floods).
  • Include:
    • Physiography: landforms, drainage.
    • Geological history.
    • Geological formations & surficial deposits.
    • Structural features: folds, faults, fractures, joints.
    • Active faults/shear zones.
    • Hydrological conditions: groundwater table configuration.

2. Local Geology (Clause 3.3)

  • Data collection via literature, site inspection, field exploration.
  • Include:
    • Geomorphology: slope, relief, landforms, drainage, springs, land use.
    • Soil/rock type, thickness, stability.
    • Hydrology: water table, seepage, permeability.
    • Local structural features.
    • Past disaster effects.
    • Geotechnical properties of materials.

3. Slope Stability & Terrain Classification (Clause 4.3 & 3.4.1.1.2)

Slope CategoryGradient (°)Stability Notes
Very Gentle0° - 15°Generally stable
Gentle15° - 25°Stable in rocky terrain
Moderately Steep25° - 30°Requires detailed study
Steep35° - 45°Requires detailed study
Very Steep> 45°Requires detailed study
  • Rocky terrain slopes < 25° generally stable.
  • Surficial deposits slopes < 20° generally stable.
  • Areas with high water table or saturation need liquefaction/settlement evaluation.

4. Geomorphology Parameters (Clause 3.4.1.1.2)

  • Slope character & relative relief for terrain evaluation.
  • Relief indicates scarps, valleys, depressions, inundation zones.

flowchart TD
    A[Regional Geology Study] --> B[Physiography & Drainage]
    A --> C[Geological History & Formations]
    A --> D[Structural Features & Faults]
    A --> E[Hydrological Conditions
4Procedures for Microzonation

IS 14243 Part 1: Procedures for Microzonation - Key Points

1. Map Scale Selection (Clause 2.2)

  • Based on:
    • Urban center size
    • Relief of area
    • Nature of surficial soil/rock strata
    • Drainage pattern & density
  • Scale & contour intervals:
    • High relief/mountainous: 1:10,000 scale, 2m contour interval
    • Moderate relief: up to 1:25,000 scale, 3-5m contour interval
  • Prepare topographic base maps if unavailable.

2. Primary Factors for Microzonation (Clause 3.1)

  • Regional geology
  • Hydrological conditions
  • Local geology
  • Human activity hazards (mining, construction)
  • Consider size and purpose of urban sectors.

3. Objectives of Microzonation

  • Identify unstable zones prone to:
    • Ground failures
    • Inundation/water-logging
    • Earthquake amplification
  • Demarcate:
    • High-risk areas
    • Negligible risk zones
  • Aid in land-use planning, building siting, and hazard mitigation.

4. Map Content & Reporting (Clause 4.7)

  • Show areas likely inundated during 100-year floods.
  • Indicate ground failure types and extents.
  • Include reclaimed/solid waste areas with long-term settlement checks.
  • Provide explanatory report on methodology and evaluation.

Summary Table: Map Scale & Contour Interval

Terrain TypeMap ScaleContour Interval
High relief/mountain1:10,0002 m
Moderate/low reliefUp to 1:25,0003 - 5 m

Conceptual Flow of Microzonation Procedure

flowchart TD
    A[Start: Define Urban Area] --> B[Collect Geological & Hydrological Data]
    B --> C[Prepare Topographic Base Maps]
    C --> D[Analyze Soil, Rock & Drainage Patterns]
    D --> E[Identify Hazard Zones (Ground Failures, Floods)]
    E --> F[Demarcate Risk Zones on Microzonation Map]
    F --> G[Prepare Report with Methodology & Recommendations]
    G
4.1Preparation of Topographic Maps

Key Specifications for Preparation of Topographic Maps (IS 14243 Part 1):

1. Scale & Contour Interval (Clause 2.2)

  • Mountainous/high relief areas:
    • Scale: 1:10,000
    • Contour interval: 2 m
  • Moderate relief areas:
    • Scale: up to 1:25,000
    • Contour interval: 3 to 5 m
  • Maps must be prepared if unavailable, as they form the base for further mapping.

2. Slope Classification (Clauses 3.4.1.1.2 & 4.1)

Slope CategoryGradient (Degrees)
Very gentle slope< 15°
Gentle slope15° - 25°
Moderate slope25° - 35°
Steep slope35° - 45°
Very steep slope> 45°
  • Prepare slope maps delineating these categories.

3. Map Types to Prepare (Clause 4.1)

  • Topographic map (base map)
  • Slope map (using above slope categories)
  • Geology map (rock outcrops, surficial deposits)
  • Land use/land cover map
  • Hydrological map showing:
    • Perennial/seasonal streams
    • Irrigation canals, open drains
    • Runoff levels (normal, monsoon, 100-year flood)
    • Groundwater table contours

4. Stability Guidelines (Clause 4.3)

  • Rocky terrain: slopes < 25° generally stable.
  • Surficial deposits: dry slopes < 20° generally stable.
  • Areas with high water table or saturated soils require detailed study for liquefaction and settlement risks.

flowchart TD
    A[Prepare Topographic Map] --> B[Slope Map]
    A --> C[Geology Map]
    A --> D[Land Use & Cover Map]
    A --> E[Hydrological Map]
    B --> F{Slope Categories}
    F --> G[Very gentle <15°]
    F --> H[Gentle 15°-
4.2Seismic Hazard Classification

Seismic Hazard Classification (IS 14243 Part 1, Clause 4.2 & Table 1)

Seismic hazard class is determined based on Peak Ground Acceleration (PGA) at the urban center:

PGA RangeSeismic Hazard ClassConditions
PGA < 0.10gI (Low)-
0.10g ≤ PGA < 0.25gII (Moderate)No active faults within 10 km
PGA > 0.25gIII (High)No active faults within 10 km
PGA > 0.25gIV (Extreme)Active fault within or ≤10 km from urban center

Key Specifications:

  • Active faults within 10 km increase hazard class to IV.
  • Geological, slope, and hydrological maps must be used to identify stable zones.
  • Slopes < 25° (rocky terrain) and < 20° (surficial deposits) are generally stable.
  • Areas with high water table or saturated soils require detailed liquefaction and settlement studies.

Summary Diagram:

flowchart TD
    A[PGA Measurement] --> B{PGA Range}
    B -->|<0.10g| C[Class I: Low]
    B -->|0.10g to <0.25g| D{Active Faults?}
    D -->|No| E[Class II: Moderate]
    D -->|Yes| F[Class IV: Extreme]
    B -->|≥0.25g| G{Active Faults?}
    G -->|No| H[Class III: High]
    G -->|Yes| F

Use this classification for design earthquake parameters and stability analysis of soil/rock as per IS 14243 Part 1.

4.3Geological and Slope Stability Assessment

Geological and Slope Stability Assessment per IS 14243 Part 1:

Key Specifications:

  • Slope Stability by Terrain Type (Clause 4.3):

    • Rocky terrain: slopes < 25° generally stable.
    • Surficial deposits (dry slopes): slopes < 20° generally stable.
    • Slopes exceeding these require detailed factor of safety (FoS) analysis.
  • Material Classification (Clause 3.4.1.1.1):

    1. Natural materials (rocks, terraces, alluvial fans, etc.)
    2. Disturbed materials (due to ground failures)
    3. Reclaimed land and waste dumps
  • Hydrological Conditions (Clause 3.4.1.1.3):

    • Evaluate surface runoff, water spread, marshy areas, groundwater table, springs.
    • Consider pore water pressure effect on shear strength.
    • Account for normal, seasonal, and 100-year flood levels.

Stability Evaluation:

  • Factor of Safety (FoS) against sliding:

[ FoS = \frac{C' + (\sigma - u) \tan \phi'}{\tau} ]

Where:

  • ( C' ) = effective cohesion

  • ( \sigma ) = normal stress

  • ( u ) = pore water pressure

  • ( \phi' ) = effective angle of internal friction

  • ( \tau ) = shear stress on failure plane

  • Slope Stability Zones:

Terrain TypeStable Slope AngleNotes
Hard rock terrain< 25°Generally stable
Surficial deposits< 20° (dry slopes)Stable if dry; wet slopes need analysis
Saturated soilsN/AStudy for liquefaction risk

Recommendations:

  • Mark zones of homogeneous lithology.
  • Superimpose slope and hydrological maps for stability mapping.
  • Identify high water table zones for liquefaction and settlement risk.
  • Plan open cut slopes considering local stability (Clause 3.4.1.3.1).
flowchart TD
    A[Geological Map] --> B[Demarcate Lithology Zones]
    C[Slope Map] --> D[Identify Stable Slopes (<25
4.4Evaluation of Rocky Terrain Stability

Key Specifications & Evaluation Criteria for Rocky Terrain Stability (IS 14243 Part 1):

1. Slope Stability Classification (Clause 4.3 & 3.4.1.1.2)

  • Rocky terrain slopes < 25° → Generally stable.
  • Surficial deposits slopes < 20° (dry) → Generally stable.
  • Slopes beyond these limits require detailed stability analysis (Factor of Safety).
Slope CategoryGradient Range (°)Stability Condition
Very Gentle0° – 15°Stable
Gentle15° – 25°Stable (rocky terrain)
Moderate25° – 30°Needs detailed study
Steep35° – 45°High risk, detailed study
Very Steep> 45°High risk, unstable

2. Material Classification (Clause 3.4.1.1.1)

  • Natural materials: rocks, terraces, alluvial fans, flood plains.
  • Disturbed materials: due to ground failures.
  • Reclaimed land and solid waste dumps.
  • Strength parameters and structural weaknesses must be assessed.

3. Failure Mode Identification (Clause 4.4)

  • Identify zones prone to:
    • Rock falls
    • Rock slides
    • Creeps
    • Debris flows

4. Factor of Safety (FoS) Evaluation

  • For slopes > stable limits, calculate FoS considering:
    • Shear strength parameters (cohesion c, friction angle φ)
    • Slope geometry and groundwater conditions
    • Use standard slope stability methods (e.g., Limit Equilibrium Method)

Simplified FoS Formula (for planar slip):

[ FoS = \frac{c' \cdot L + (W \cos \alpha - uL) \tan \phi'}{W \sin \alpha} ]

Where:

  • ( c' ) = effective cohesion
  • ( \phi' ) = effective friction angle
  • ( W ) = weight of sliding mass
  • ( \alpha ) = slope angle
  • ( u ) = pore water pressure
  • ( L
4.5Assessment of Glacial Materials

Assessment of Glacial Materials as per IS 14243 Part 1

Key Points & Specifications:

  • Degree of Saturation (Clause 4.5):
    Evaluate saturation to assess loss of strength and potential debris flow in glacial materials.
    [ S_r = \frac{V_w}{V_v} \times 100% ]
    where (S_r) = degree of saturation, (V_w) = volume of water, (V_v) = volume of voids.

  • Material Classification (Clause 3.4.1.1.1):

    • Natural materials (including glacial deposits)
    • Disturbed materials (due to ground failures)
    • Reclaimed land and solid waste dumps
  • Stability Parameters (Clause 4.3):

    • Slope stability depends on lithology and slope angle.
    • Rocky terrain: slopes < 25° generally stable.
    • Surficial deposits (including glacial till): dry slopes < 20° generally stable.
    • Areas with high water table or saturation require detailed factor of safety (FoS) analysis.
  • Avalanche & Landslide Debris (Clause 3.4.1.2.5):
    Study debris characteristics for hazard evaluation.


Recommended Stability Check Formula (FoS):

[ FoS = \frac{c' + (\sigma - u) \tan \phi'}{\tau} ]

  • (c') = effective cohesion
  • (\sigma) = normal stress
  • (u) = pore water pressure
  • (\phi') = effective angle of internal friction
  • (\tau) = shear stress

Summary Table: Stability of Slopes in Glacial Materials

Terrain TypeSlope Angle for StabilityNotes
Rocky Terrain< 25°Generally stable
Surficial Deposits< 20°Stable if dry
Saturated SoilsRequires detailed studyRisk of liquefaction & debris flow

flowchart TD
    A[Glacial Material] --> B{Degree of Saturation}
    B -->|Low Saturation| C[Stable
4.6Study of Terrace and Fan Deposits

Study of Terrace and Fan Deposits as per IS 14243 Part 1

Key Specifications:

  • Classification (3.4.1.1.1):

    • Natural materials include terraces, fans, flood plains, alluvial deposits, etc.
    • Strength parameters and structural weaknesses must be analyzed for stability.
  • Stability Assessment (4.3 & 4.6):

    • Identify homogeneous lithology zones (terraces, fans, etc.) using geological, slope, and hydrological maps.
    • Stable slopes:
      • Rocky terrain: slope < 25°
      • Surficial deposits (terraces/fans): dry slopes < 20°
    • Areas with high water table or saturation require liquefaction and settlement analysis under earthquake loading.

Stability Evaluation:

  • Calculate Factor of Safety (FOS) for slopes > stable limits using shear strength parameters:
    [ FOS = \frac{c' + (\sigma - u) \tan \phi'}{\tau} ] where:
    • (c') = effective cohesion
    • (\phi') = effective angle of internal friction
    • (\sigma) = normal stress
    • (u) = pore water pressure
    • (\tau) = shear stress on failure plane

Other Considerations:

  • Identify previous ground failures and debris zones (3.4.1.2.5) for hazard evaluation.
  • Study earthquake effects on stability and potential liquefaction.

flowchart TD
    A[Geological Map] --> B[Identify Lithology Zones]
    B --> C[Slope Map & Hydrological Map]
    C --> D{Slope Stability Check}
    D -->|Slope < 20° (Surficial)| E[Generally Stable]
    D -->|Slope < 25° (Rocky)| E
    D -->|Slope > Limits| F[Detailed FOS Analysis]
    F --> G[Consider Strength Parameters & Water Table]
    G --> H[Estimate Stability under Earthquake]

This approach ensures a comprehensive stability assessment of terrace and fan deposits per IS 14243 Part 1.

4.7Considerations for Reclaimed and Waste Disposal Areas

Considerations for Reclaimed and Waste Disposal Areas (IS 14243 Part 1)

Key Points from Clauses:

  • Clause 3.4.1.3.5:

    • Unstable foundations on slopes with reclaimed land or waste dumps cause unequal settlements and failures.
    • Dumps often contain organic materials that decay, creating voids and differential settlements.
    • Presence of contaminants and empty spaces reduces soil strength and stability.
  • Clause 4.7:

    • Long-term settlements due to soil consolidation and organic decomposition must be evaluated under in-situ conditions across seasons.
    • Use microzonation maps to identify flood-prone and ground failure-prone areas for safe construction zones.

Design & Evaluation Guidelines:

  • Settlement Estimation:
    Consider primary consolidation and secondary compression for organic fills:
    [ S = S_c + S_s ]
    where

    • ( S_c ) = primary consolidation settlement
    • ( S_s ) = secondary (creep) settlement due to organic decay
  • Consolidation Settlement (Terzaghi’s Theory):
    [ S_c = \frac{H}{1+e_0} \log \frac{\sigma'_0 + \Delta \sigma'}{\sigma'_0} ]
    where

    • ( H ) = thickness of compressible layer
    • ( e_0 ) = initial void ratio
    • ( \sigma'_0 ) = initial effective stress
    • ( \Delta \sigma' ) = increase in effective stress
  • Recommendations:

    • Conduct seasonal field monitoring for settlements.
    • Use geotechnical investigations to characterize waste material properties.
    • Avoid heavy structures on highly organic or loosely filled dumps.
    • Employ ground improvement or deep foundations if necessary.

Summary Table: Key Considerations

AspectSpecification/Action
Material TypeOrganic, contaminated, loose fill
Settlement AssessmentPrimary + secondary consolidation
MonitoringIn-situ seasonal settlement checks
Stability ConcernsUnequal settlement, slope failure
5Causative Factors of Land Hazards

IS 14243 Part 1 — Causative Factors of Land Hazards

Key Points from Clauses 3.4, 4.3, and 3.4.1.1.1:

1. Categories of Land Hazards:

  • Ground Failures: Landslides, slope failures, liquefaction, settlement.
  • Floods and Inundations: Waterlogging, flooding hazards.

2. Stability Criteria Based on Terrain and Slope (Clause 4.3):

Terrain TypeStable Slope Limit
Rocky TerrainSlope < 25°
Surficial DepositsDry slope < 20°
  • Areas with slopes beyond these limits require detailed factor of safety (FoS) analysis.
  • High water table and saturated soils need liquefaction and settlement assessment.

3. Material Classification (Clause 3.4.1.1.1):

  • Natural materials: Rocks, terraces, alluvial fans, flood plains, glacial deposits.
  • Disturbed materials: Due to ground failures.
  • Reclaimed land: Solid waste dumps, reclaimed soils.

4. Factor of Safety (FoS) for Slope Stability (General Formula):

[ FoS = \frac{\text{Shear Strength of Soil (c + \sigma \tan \phi)}}{\text{Shear Stress due to slope}} ]

Where:

  • ( c ) = cohesion,
  • ( \phi ) = angle of internal friction,
  • ( \sigma ) = normal stress.

FoS > 1.5 generally indicates stable slopes.


Summary Diagram of Hazard Identification Process

flowchart TD
    A[Geological Map] --> B[Identify Homogeneous Lithology]
    B --> C[Superimpose Slope Map]
    C --> D{Slope Criteria}
    D -->|Rocky < 25°| E[Stable Area]
    D -->|Surficial < 20°| E
    D -->|Others| F[Detailed FoS Study]
    E --> G[Mark Stable Zones]
    F --> G
    G --> H[Hydrological Map Overlay]
    H --> I[Identify High Water Table Zones]
    I --> J[Assess
6Instabilities due to Human Activities

Instabilities Due to Human Activities (IS 14243 Part 1, Clause 3.4.1.3):

  • Causes:
    • Mining and excavations without proper planning.
    • Unplanned urban development.
    • Construction interfering with existing drainage systems.
    • Building on flood plains or near shorelines.
    • Construction on weak/unstable foundations.

Key Specifications & Considerations:

  • Planning & Execution: Proper site investigation and planning to avoid interference with natural drainage and unstable zones.
  • Foundation Assessment: Use geotechnical investigations to identify weak soils.
  • Drainage: Maintain or improve natural drainage to prevent waterlogging and erosion.
  • Urban Development: Follow zoning and land-use regulations to avoid construction on vulnerable lands.

Important Formulas & Checks (General Guidance):

  • Factor of Safety (FoS) against slope failure:

[ FoS = \frac{\text{Shear Strength of Soil}}{\text{Shear Stress due to Loads}} ]

  • Allowable bearing capacity check:

[ q_{allow} = \frac{q_{ult}}{FS} ]

Where:

  • (q_{ult}) = ultimate bearing capacity (from soil tests)
  • (FS) = factor of safety (usually 2.5 to 3 for human activity zones)

Summary Table (Conceptual):

Human ActivityInstability RiskMitigation Measures
Mining/excavationGround collapse, subsidenceControlled excavation, monitoring
Urban developmentSoil erosion, drainage blockageProper zoning, drainage planning
Construction near waterFlooding, foundation failureSoil stabilization, deep foundations

flowchart TD
    A[Human Activities] --> B[Mining/Excavation]
    A --> C[Unplanned Urban Development]
    A --> D[Drainage Interference]
    A --> E[Construction on Weak Foundations]
    B --> F[Ground Collapse]
    C --> G[Soil Erosion & Instability]
    D --> H[Waterlogging & Erosion]
    E --> I[Foundation Failure]

Note: IS 14243 Part 1 emphasizes prevention through planning and geotechnical assessment rather than prescribing fixed formulas for human activity-induced instabilities.

7Floods and Inundations

IS 14243 Part 1: Floods and Inundations — Key Points & Specifications

Classification of Floods (Clause 3.4.2)

  • Inland floods: Floods on rivers.
  • Deltaic floods: Flooding in delta areas.
  • Sea waves: Due to cyclones.
  • Excessive precipitation: From cyclones/cloud bursts.

Design Considerations

  • Establish maximum flood level from historical data.
  • Construction must be above max flood level to avoid inundation.
  • Near shorelines/flood plains, consider:
    • High tide levels
    • Sea waves
    • Backflow through drains

Extreme Conditions (Clause 3.4.1.2.2 & 3.4.1.2.4)

  • Consider effects of:
    • Cloud bursts, cyclones, tsunamis.
    • Collapse of upstream water-retaining structures.
    • Sudden debris flow from bursting debris dams (e.g., landslides, glacial debris).

Recommended Formula for Flood Level Estimation

[ H_{max} = H_{historic} + S + C ]

Where:

  • (H_{max}) = Design flood level
  • (H_{historic}) = Highest recorded flood level
  • (S) = Freeboard (safety margin, typically 0.5 to 1.0 m)
  • (C) = Climate change allowance (if applicable)

Summary Table: Flood Hazard Parameters

ParameterTypical Values/Notes
Freeboard (S)0.5 to 1.0 m
Design flood return period50 to 100 years
Debris flow considerationRequired if debris dams upstream
Tide & wave height (coastal)Use local tide data + cyclone surge

flowchart TD
    A[Flood Hazard Types] --> B[Inland Floods]
    A --> C[Deltaic Floods]
    A --> D[Sea Waves (Cyclones)]
    A --> E[Excessive Precipitation]
    F[Design Considerations] --> G[Max Flood Level]
    F --> H[Freeboard]
    F --> I[Backflow & Drainage]
   
8Guidelines for Site Selection and Development

IS 14243 Part 1 (1995) — Guidelines for Site Selection & Development in Hill Areas

Key Specifications for Microzonation & Site Development

  • Microzonation Maps:

    • Delineate areas prone to:
      • Ground failures (landslides, rock falls, avalanches)
      • Flood inundation (100-year flood zones)
      • Water-logging and soil consolidation settlements
    • Identify stable, unstable, and potentially hazardous zones.
    • Used for planning building complexes, green belts, and open spaces.
  • Assessment Parameters:

    • Local geomorphology, geology, hydrology.
    • Natural hazards: earthquakes, floods, cyclones.
    • Procreated hazards: mining, unplanned excavation.
    • Long-term soil settlement checks in reclaimed/solid waste areas.
  • Development Guidelines:

    • Avoid construction in high-risk zones.
    • Design green belts and open spaces as buffers.
    • Use microzonation data for master planning & land use.

Important Considerations

AspectDetails
Flood InundationMap 100-year flood extent of streams
Ground FailuresIdentify nature, type, and aerial extent
Soil ConsolidationMonitor settlements seasonally in reclaimed sites
Natural & Procreated HazardsEarthquakes, erosion, mining impacts

Summary Flowchart of Site Selection Process

flowchart TD
    A[Start: Urban Centre Planning] --> B[Collect Geological & Hydrological Data]
    B --> C[Prepare Microzonation Maps]
    C --> D{Identify Zones}
    D -->|Stable| E[Suitable for Construction]
    D -->|Unstable| F[Restrict Construction; Plan Green Belts]
    D -->|Flood Prone| G[Plan Flood Mitigation & Open Spaces]
    E & F & G --> H[Finalize Master Plan & Land Use]
    H --> I[Site Development & Monitoring]

Note: For detailed procedures, refer to Clause 4.7 and related sections of IS 14243-1 (1995). Always round off values per IS 2:1960 rules.

Popular Questions About IS 14243 Part 1

?What are the key geological factors considered in microzonation of urban centres in hill areas?

Key geological factors for microzonation of urban centres in hill areas per IS 14243 Part 1:

  • Regional Geology:

    • Physiography (landforms, drainage)
    • Geological history and formations (rock masses, surficial deposits)
    • Structural features (folds, faults, fractures, joints)
    • Active faults and shear zones prone to seismic activity
    • Hydrological conditions including groundwater table configuration
  • Local Geology & Terrain:

    • Lithology homogeneity (hard rock, soft rock, terraces, fans, flood plains, slide debris)
    • Slope stability:
      • Rocky terrain slopes < 25° generally stable
      • Surficial deposits slopes < 20° generally stable
    • Areas with high water table or saturated soils prone to liquefaction and settlement during earthquakes
  • Mapping Scales:

    • High relief: 1:10,000 scale with 2m contour intervals
    • Moderate relief: up to 1:25,000 scale with 3-5m contours

These factors guide hazard assessment and safe urban planning in hilly terrains.

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?How does IS 14243 Part 1 classify seismic hazard zones based on peak ground acceleration?

IS 14243 Part 1 classifies seismic hazard zones based on Peak Ground Acceleration (PGA) as follows:

PGA RangeSeismic Hazard ClassCondition
PGA < 0.10gI (Low)-
0.10g ≤ PGA < 0.25gII (Moderate)No active faults within 10 km
PGA > 0.25gIII (High)No active faults within 10 km
PGA > 0.25gIV (Extreme)Active fault within or within 10 km of urban centre

Key points:

  • PGA is the estimated peak ground acceleration at the urban centre.
  • Presence of active faults within 10 km elevates the hazard class to IV (Extreme).
  • This classification guides design earthquake evaluation and structural stability analysis.
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This classification is essential for microzonation, urban planning, and seismic design per IS 14243 Part 1.

?What types of ground failures are addressed by this standard for safe site selection?

IS 14243 Part 1 addresses ground failures for safe site selection by classifying materials and failure types as follows:

Types of Ground Failures Covered:

  • Inherent instabilities: Natural weaknesses in soil/rock materials.
  • Instabilities due to external forces: Such as slope failures, earthquakes, floods.
  • Instabilities due to human activities: Excavation, loading, reclamation, waste dumping.

Key Ground Failure Types:

  • Slope failures: Identified by breaks in ground profiles, especially on slopes >25° in rock terrain or >20° in surficial deposits.
  • Liquefaction and settlement: In areas with high water tables and saturated soils during earthquakes.
  • Inundation and flooding: From monsoons, poor drainage, or industrial discharge causing foundation failures.

Site Selection Guidance:

  • Demarcate homogeneous lithology zones.
  • Use geological, slope, and hydrological maps to identify stable/unstable areas.
  • Avoid previously failed slopes or reclaimed/waste dump sites without detailed study.

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Summary: IS 14243 Part 1 emphasizes detailed geological and geotechnical evaluation, especially for slopes, saturated soils, and reclaimed lands, to ensure safe site selection against ground failures.

?How should hydrological conditions and flood risks be evaluated according to this standard?

According to IS 14243 Part 1, hydrological conditions and flood risks should be evaluated as follows:

Hydrological Conditions (Clause 3.4.1.1.3)

  • Study surface run-off characteristics: nature of streams (perennial/seasonal), inlet/outlet levels, and terrain.
  • Assess water spread and marshy conditions (seasonal or permanent water logging).
  • Determine groundwater table/phreatic level, springs, and seepages, as these affect pore water pressure and shear strength.
  • Consider normal water levels, seasonal flood levels, and 100-year flood levels for siting structures near water bodies.
  • Account for seepages on slopes which may reduce stability.

Flood Risks (Clause 3.4.2)

  • Classify floods into:
    1. Inland river floods,
    2. Deltaic area floods,
    3. Sea waves from cyclones,
    4. Excessive precipitation (cyclones/cloud bursts).
  • Establish maximum flood levels from historical data and restrict construction above these levels.

Additional Considerations

  • Include effects of extreme hydro-meteorological events (cloud bursts, cyclones, tsunamis).
  • For flood plains and coastal areas, consider sea waves, high tides, backflows, and water spreading during floods.

Summary Table

ParameterConsideration
Surface Run-offStream type, inlet/outlet levels, terrain
Water Spread & MarshinessSeasonal/permanent water logging
Groundwater & SeepagesPhreatic level, springs, seepage effects
Flood LevelsNormal, seasonal, 100-year flood levels
Flood TypesInland, deltaic, cyclone waves, heavy rain
Extreme EventsCloud bursts, cyclones, tsunamis, dam collapse
Construction LocationAbove max flood level, consider backflows

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?What human activities can contribute to slope instability and how are they accounted for in microzonation?

Human Activities Causing Slope Instability (IS 14243 Part 1):

  • Mining and Excavations: Disturb natural ground, weaken slope integrity.
  • Unplanned Urban Development: Excessive construction in certain zones causes slope overload and instability.
  • Interference with Drainage: Altered hydrological regime leads to waterlogging, erosion, and slope failure.
  • Construction on Weak Foundations: Builds on unstable or flood-prone areas, increasing failure risk.
  • Building in Flood Plains/Shorelines: Increases vulnerability to inundation and ground failure.

Accounting in Microzonation:

  • Microzonation maps delineate zones prone to ground failures and inundation.
  • They incorporate regional/local geology, hydrology, and human-induced hazards.
  • Areas with unplanned development or mining are identified as high-risk.
  • Helps in planning safer urban growth and construction practices by avoiding unstable zones.
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Summary: IS 14243 Part 1 emphasizes identifying and mitigating slope instability from human activities through detailed microzonation considering geology, hydrology, and urbanization patterns.

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