IS 14496 Part 21998AI Search Enabled✦ AI Generated
Guidelines for the preparation of landslide - Hazard zonation maps in mountainous terrains, Part 2: Macro-zonation
IS 14496 Part 2: 1998 provides comprehensive guidelines for preparing macro-scale landslide hazard zonation (LHZ) maps in mountainous terrains at scales of 1:25,000 or 1:50,000. It outlines a systematic approach to assess slope instability by evaluating key causative factors such as lithology, geological structure, slope morphometry, relative relief, land use, and hydrogeological conditions. This standard is essential for planners, geotechnical engineers, and environmental professionals involved in regional planning, hazard assessment, and mitigation of landslide risks in hill and mountain areas.
10Sections
77Clauses Indexed
✓AI Search Ready
1998Edition
Hill Area Development EngineeringCategory
Alternative search terms: IS 14496 Part 2 PDF, IS 14496 Part 2 pdf free download, IS 14496 Part 2 free download pdf, IS14496Part2 PDF, IS-14496-Part-2 PDF, IS 14496 Part 2 1998 PDF, IS 14496 Part 2:1998 PDF, IS 14496 Part 2-1998 PDF, IS 14496 Part 2 (1998) PDF, IS 14496 Part 2 1998 edition PDF, IS 14496 Part 2 edition 1998 PDF
Overview
What This Standard Covers
IS 14496 Part 2: 1998 provides comprehensive guidelines for preparing macro-scale landslide hazard zonation (LHZ) maps in mountainous terrains at scales of 1:25,000 or 1:50,000. It outlines a systematic approach to assess slope instability by evaluating key causative factors such as lithology, geological structure, slope morphometry, relative relief, land use, and hydrogeological conditions. This standard is essential for planners, geotechnical engineers, and environmental professionals involved in regional planning, hazard assessment, and mitigation of landslide risks in hill and mountain areas.
Audience
Who Uses This Standard
Geotechnical Engineers
Geologists
Urban and Regional Planners
Environmental Consultants
Civil Engineers
Disaster Management Authorities
Infrastructure Developers in Mountainous Regions
Contents
Key Topics Covered
✓Landslide hazard zonation mapping methodology
✓Macro-zonation scale and mapping techniques
✓Identification and rating of causative factors
✓Lithology and rock/soil classification
✓Structural discontinuities and slope relationships
✓Slope morphometry and relative relief evaluation
✓Land use and land cover impact on slope stability
✓Hydrogeological conditions affecting landslides
✓Total Estimated Hazard Degree (TEHD) calculation
✓Preparation and interpretation of LHZ maps
✓Symbol conventions for geological and hazard maps
✓Guidelines for field investigations and desk studies
✓Revision protocols post-natural events
✓Application of LHZ maps for developmental planning
✓Safety and mitigation recommendations for hazard zones
Structure
Table of Contents
1Scope▼
IS 14496 Part 2: Scope & Key Specifications
This part of IS 14496 focuses on landslide hazard zonation (LHZ) mapping using geological and geomorphological data.
Superimpose these maps to calculate Total Estimated Hazard Degree (TEHD) for each facet.
Use TEHD values to create a Landslide Hazard Zonation (LHZ) Map with zones:
High Hazard (HH)
Very High Hazard (VHH)
Suggested Symbols for Slope Morphometry (Clause 6.3):
Slope Category
Slope Angle (°)
Very gentle slope
≤ 15
Gentle slope
16 to 25
Moderately steep slope
26 to 35
Steep slope
36 to 45
Escarpment/Cliff
> 45
Procedure for Macro Zonation (Fig. 1 Summary):
flowchart TD
A[Acquire Topographic Maps 1:50000] --> B[Acquire Aerial Photos & Satellite Imageries]
B --> C[Acquire Regional Geological Map]
C --> D[Identify Hazard Evaluation Factors]
D --> E[Prepare Pre-field Geological Map 1:50000]
E --> F[Lithological & Structural Map 1:50000]
F --> G[Slope Morphometric Map]
G --> H[Relative Relief Map]
H --> I[Assign Land Hazard Evaluation Factor (LHEF)]
I --> J[Rock Outcrop & Soil Cover Map]
J --> K[Land Use & Land Cover Map]
K --> L[Hydrogeological Map]
L --> M[Calculate TEHD]
M --> N[Prepare Landslide Hazard Zonation (LHZ) Map]
References for Symbols and Abbreviations (IS 7422):
Part 1: Abbreviations
Part 2: Igneous Rocks
Part 3: Sedimentary Rocks
Part 4: Metamorphic Rocks
Part 5: Line Symbols for Contacts & Structures
Summary: Present terrain and hazard data as layered maps, calculate TEHD facet
7Interpretation of Macro-Zonation LHZ Map▼
Interpretation of Macro-Zonation Landslide Hazard Zonation (LHZ) Map (IS 14496 Part 2)
Key Hazard Zones & Their Meaning (Clause 6.7 & 7.1)
Hazard Level
Description
Very Low Hazard (VLH)
Generally safe for development
Low Hazard (LH)
Generally safe for development
Moderate Hazard (MH)
May contain unstable slope pockets; requires detailed geotechnical investigation
High Hazard (HH)
Mostly unstable slopes; detailed slope mapping at 1:1000 or 1:2000 scale needed
Very High Hazard (VHH)
Highly unstable slopes, often active; requires detailed geotechnical appraisal and mitigation
Factors Considered (Clause 7.1)
Hazard rating based on slope stability
Modes of failure: boulder jumping, debris flow, toe erosion, choked drainage, gully meandering
Damage risk to life and property
Preparation Steps (Annex A)
Slope Facet Map: Divide topographic map into slope facets.
Pre-Field Maps: Transfer geological, morphometric, relief, land use, and hydrogeological data.
Factorial Maps: Prepare lithological, structural, slope morphometric, relative relief, land use, and hydrogeological maps; analyze structural discontinuities.
LHZ Map: Combine desk study and field data (scale 1:25,000 or 1:50,000).
Revision of LHZ Map (Clause 9)
Update after major earthquakes (>5 Richter), floods, cyclones, mining, or cloud bursts.
Summary Flowchart of LHZ Mapping Process
flowchart TD
A[Topographical Map] --> B[Slope Facet Division]
B --> C[Pre-Field Maps Preparation]
C --> D[Field Verification & Modification]
D --> E[Factorial Maps Preparation]
E --> F[Structural Analysis & Stability Assessment]
F --> G[Landslide Hazard Zonation Map]
G --> H[Periodic Revision after Major Events]
Note: Use scale 1:25,000 or 1:50,000 for macro-zonation; detailed slope mapping at 1:100
8Revision of Macro-Zonation LHZ Map▼
Revision of Macro-Zonation LHZ Map (IS 14496 Part 2)
Key Specifications:
Revision triggers: After major events like earthquakes (>5 Richter), floods, cyclones, mining, developmental activities, or cloud bursts affecting the watershed.
Scale for detailed slope mapping: 1:1000 or 1:2000 for unstable slopes (HH, VHH zones).
Hazard assessment basis: Hazard rating, failure modes (boulder jumping, debris flow, toe erosion, etc.), and damage type.
Update after major earthquakes (>5 Richter), floods, cyclones, mining, cloud bursts.
Procedure Flowchart (Simplified):
flowchart TD
A[Acquire Topographic Maps 1:50000] --> B[Acquire Aerial Photos/Satellite Imageries]
B --> C[Acquire Regional Geological Map]
C --> D[Prepare Pre-field Geological Map]
D
Annex BComposition of Technical Committee▼
Composition of Technical Committee (IS 14496 Part 2)
The Technical Committee responsible for this standard is the Hill Area Development Engineering Sectional Committee, CED 56. The detailed composition is given in Annex B and includes:
Role
Representative Organization
Chairman
Dr. Gopal Ranjan, University of Roorkee
Members
Public Works Dept. J&K, Indian Institute of Remote Sensing, National Buildings Construction Corporation, Uttar Pradesh Irrigation Design Organization, Ministry of Surface Transport, Indian Roads Congress, Central Water Commission, Indian Meteorological Dept., Society for Integrated Development of Himalayas, Forest Survey of India, Ministry of Railways, Geological Survey of India, Army Headquarters, Sikkim Hill Area Development Board, Central Road Research Institute, Directorate General Border Roads, Central Mining Research Institute, University of Roorkee, Department of Science and Technology, National Institute of Hydrology, Structural Engineering Research Centre, HUDCO, and others
Alternates are nominated for many members ensuring continuity.
Key Notes:
The committee includes experts from government departments, research institutes, universities, and industry.
This multi-disciplinary composition ensures comprehensive coverage of hill area development and landslide hazard zonation.
Refer to Annex B of IS 14496 Part 2 for the full detailed list.
Related Reference Table (for geological symbols & maps):
IS No.
Title
7422 (Part 1 to 5)
Symbols and abbreviations for geological maps and features
This composition ensures expert inputs for landslide hazard zonation and hill area engineering standards.
Frequently Asked
Popular Questions About IS 14496 Part 2
?What are the primary causative factors considered in macro-zonation landslide hazard mapping?▼
Primary Causative Factors in Macro-Zonation Landslide Hazard Mapping (IS 14496 Part 2)
According to Clause 3.1, the key factors governing macro-zonation landslide hazard (LHZ) mapping are:
Lithology: Rock type and its weathering characteristics.
Structure: Geological discontinuities such as faults, joints, and bedding planes.
Slope Morphometry: Slope angle, shape, and length.
Land Use and Land Cover: Vegetation, urbanization, and surface conditions.
Hydrogeological Conditions: Groundwater presence, seepage, and wet patches.
These factors collectively influence slope stability and are mapped facet-wise to prepare factorial maps, which are then integrated into the LHZ map.
Summary Table of Factors
Factor
Role in Instability
Lithology
Determines rock strength and weathering
Structure
Controls potential failure planes
Slope Morphometry
Steeper slopes have higher failure risk
Relative Relief
Influences gravitational driving forces
Land Use & Cover
Affects surface runoff and root reinforcement
Hydrogeological
Water pressure reduces effective stress
Loading diagram...
This systematic approach ensures comprehensive hazard assessment for safer development planning.
?How is the Total Estimated Hazard Degree (TEHD) calculated for slope facets?▼
Calculation of Total Estimated Hazard Degree (TEHD) for Slope Facets (IS 14496 Part 2)
TEHD is calculated facet-wise because adjoining slope facets may have different stability.
For each slope facet, TEHD is the sum of ratings from individual causative factors based on the Landslide Hazard Evaluation Factor (LHEF) rating scheme.
The causative factors include:
Lithology
Structure
Slope Morphometry
Relative Relief
Land Use and Land Cover
Hydrogeological Conditions
Formula:
[
\text{TEHD} = \sum \text{LHEF ratings of all causative factors for the facet}
]
Interpretation of TEHD values (Table 3):
Zone
TEHD Value
Hazard Description
I
< 3.5
Very Low Hazard (VLH)
II
3.5 – 5.0
Low Hazard (LH)
III
5.1 – 6.0
Moderate Hazard (MH)
IV
6.1 – 7.5
High Hazard (HH)
V
> 7.5
Very High Hazard (VHH)
Summary
Delimit slope facets by natural boundaries (ridges, gullies, rivers).
Assign ratings for each factor per facet using LHEF.
Sum ratings to get TEHD.
Classify hazard zone based on TEHD value.
Loading diagram...
?What scales are recommended for preparing macro-zonation landslide hazard zonation maps?▼
Recommended Scales for Macro-Zonation Landslide Hazard Zonation Maps (IS 14496 Part 2):
Detailed Geotechnical Slope Mapping (for unstable zones): 1:1,000 to 1:2,000
Summary:
Macro-zonation mapping uses 1:50,000 scale for broad regional mapping and hazard evaluation.
For detailed slope instability assessment in High Hazard (HH) and Very High Hazard (VHH) zones, finer scales of 1:1,000 or 1:2,000 are recommended.
These scales help identify slope facets, structural discontinuities, and hazard factors effectively.
Loading diagram...
This approach ensures efficient hazard zoning and guides appropriate mitigation measures.
?How does land use and vegetation cover influence landslide hazard ratings in this standard?▼
Influence of Land Use and Vegetation Cover on Landslide Hazard Ratings (IS 14496 Part 2)
Land use and vegetation cover are indirect indicators of slope stability (Clause 4.2.5).
Vegetation effects:
Thick forest cover protects slopes by reducing weathering and erosion.
Root systems increase shear resistance, stabilizing the soil.
Sparse or barren areas have faster erosion and higher instability.
Agricultural lands are generally stable due to repeated artificial watering, usually on gentle slopes.
Hazard ratings based on vegetation intensity (Table 2, Clause 4.2):
Land Use / Vegetation Cover
Rating
Agricultural land / populated flat land
0.6
Thickly vegetated forest area
0.8
Moderately vegetated area
1.2
Sparsely vegetated area with lesser ground cover
1.5
Barren land
2.0
In thickly populated areas, smaller facets are considered for detailed hazard evaluation.
This rating contributes up to 2.0 in the overall Landslide Hazard Evaluation Factor (LHEF), reflecting the significant role of land cover in slope stability.
?What procedures are suggested for revising landslide hazard zonation maps after major natural events?▼
Revision Procedures for Landslide Hazard Zonation (LHZ) Maps after Major Natural Events (IS 14496 Part 2)
When to Revise:
The LHZ maps must be revised after major natural events such as:
Earthquakes with magnitude > 5 (Richter scale)
Major floods, cyclones, cloud bursts
Significant developmental or mining activities
These events can trigger new landslides affecting watershed stability.
Revision Approach:
Conduct field verification and mapping of new landslides and slope changes.
Update factorial maps (lithology, structure, slope morphology, hydrogeology, land use) based on fresh data.
Reassess hazard ratings considering new instabilities and failure modes (e.g., debris flow, toe erosion).
Use detailed mapping at scales 1:1000 or 1:2000 for unstable zones (HH, VHH).
Integrate satellite imagery/aerial photos for rapid detection of wet patches and slope changes.
Outcome:
A revised LHZ map reflecting updated hazard zones to guide safer development and mitigation.
Loading diagram...
This ensures dynamic, risk-informed land use decisions in mountainous terrains.
✦
Need Detailed Clause Answers?
Ask AI about any clause, requirement, or provision in IS 14496 Part 2. Get instant, clause-cited responses powered by our indexed library.