Chapter 1: Geomorphology
The Study of Landforms and Earth’s Internal Processes
1.1 Structure of the Earth
- Earth has concentric layers:
- Crust: 5–70 km thick; continental (sial) and oceanic (sima)
- Mantle: Extends to 2900 km; asthenosphere is part of upper mantle
- Core: Outer (liquid), Inner (solid); iron-nickel composition
Discontinuities:
- Moho: Crust–mantle
- Gutenberg: Mantle–outer core
- Lehmann: Outer–inner core
UPSC Angle: “Why S-waves do not travel through outer core?” → They can’t pass through liquid.
1.2 Earth Movements
Endogenic (internal forces): Build landforms
- Folding (Himalayas), Faulting (Rift Valleys), Volcanism
Exogenic (external forces): Degrade landforms
- Weathering, Erosion, Mass wasting, Deposition
1.3 Plate Tectonics Theory
- Developed from Continental Drift (Wegener) + Sea Floor Spreading
- Lithosphere divided into 7 major plates and several minor ones
- Plate boundaries:
- Divergent: Mid-Atlantic Ridge
- Convergent: Himalayas (continent–continent), Andes (ocean–continent)
- Transform: San Andreas Fault (USA)
Important: Subduction zones = volcanic + earthquake activity
Prelims MCQ Trend: Plate matching with landforms
1.4 Earthquakes
- Sudden energy release → seismic waves
- Focus: Origin point, Epicenter: Surface point
- Richter Scale: Measures magnitude
- Mercalli Scale: Measures intensity (damage)
Seismic Waves:
- P-waves: Fast, through solid & liquid
- S-waves: Through solids only
- Surface waves: Most destructive
Seismic Zones in India:
- Zone V: Kashmir, NE India
- Zone IV: Delhi, parts of Bihar
- Zone III: Mumbai, Kolkata
Mains Relevance: “Urban earthquakes are deadlier due to human vulnerability. Discuss.”
1.5 Volcanoes
- Opening in Earth’s crust emitting lava/gases/ash
- Types by Activity:
- Active (Barren Island), Dormant (Vesuvius), Extinct (Deccan Traps)
Volcanic Landforms:
- Intrusive: Batholith, Laccolith, Sill
- Extrusive: Shield volcano, Composite cone
Pacific Ring of Fire = Most active volcanic belt
Prelims Favorite: Match volcano type with location
Mains Angle: “Volcanism and plate tectonics are linked – explain with examples.”
1.6 Weathering and Mass Wasting
- Weathering: Disintegration of rocks in place
- Mechanical (frost, exfoliation)
- Chemical (oxidation, hydration)
- Biological (roots, lichens)
Mass Wasting: Downhill movement (landslide, soil creep)
Prelims Alert: Match type of weathering with climate
Mains Angle: “Landslides are increasing in Western Ghats – explain with geography”
1.7 Erosional and Depositional Landforms
Fluvial (River):
- Erosional: V-shaped valley, gorges, waterfall
- Depositional: Meanders, floodplains, delta, ox-bow lake
Aeolian (Wind):
- Erosional: Mushroom rock
- Depositional: Sand dunes (barchans)
Glacial:
- Erosional: U-shaped valley, cirque, arête
- Depositional: Moraines, drumlins
Coastal:
- Erosional: Cliffs, arches, stacks
- Depositional: Beaches, spits, bars
Karst (Limestone):
- Sinkholes, stalactites, stalagmites, caves
Prelims Pick: Delta type – arcuate (Ganga), bird-foot (Mississippi)
Mains Task: “River systems shape the Indian landscape – discuss with examples.”
Chapter 2: Climatology
2.1 Introduction to Climatology
- Definition: Climatology is the scientific study of climate, analyzing long-term weather patterns and trends.
- Importance: Understanding climate is crucial for agriculture, disaster management, and planning in India.
2.2 Factors Influencing India’s Climate
- Latitude: India’s position between 8°N and 37°N affects its tropical to subtropical climate.
- Himalayas: Act as a barrier, preventing cold Central Asian winds, thus influencing the climate of the northern plains.
- Thar Desert: Contributes to the development of the monsoon system by creating low-pressure zones.
- Indian Ocean: Influences the monsoon winds and provides moisture for rainfall.
- Altitude: Varied elevations lead to diverse climatic conditions across regions.
2.3 Climatic Zones of India (Köppen Classification)
India’s climate can be categorized into several zones based on the Köppen system:
- Tropical Wet (Af): Found in the Western Ghats and northeastern states; characterized by high rainfall and humidity.
- Tropical Wet and Dry (Aw): Covers central and southern India; marked by distinct wet and dry seasons.
- Semi-Arid (BSh): Located in parts of Gujarat and the Deccan plateau; receives moderate rainfall.
- Arid (BWh): Encompasses the Thar Desert region; experiences very low rainfall.
- Humid Subtropical (Cwa): Includes the northern plains; hot summers and cool winters with moderate rainfall.
- Mountain (H): Covers the Himalayan region; characterized by cold temperatures and snowfall.
Note: For a detailed map illustrating these climatic zones, refer to the official resources provided by the Survey of India.India Government
2.4 Seasons in India (As per Indian Meteorological Department)
- Winter (January – February): Cool and dry conditions prevail.
- Pre-Monsoon/Summer (March – May): High temperatures and occasional thunderstorms.
- Southwest Monsoon (June – September): Major rainfall period due to monsoon winds.
- Post-Monsoon/Retreating Monsoon (October – December): Withdrawal of monsoon with decreasing rainfall.
2.5 Monsoons in India
- Southwest Monsoon:
- Onset: Early June over Kerala.
- Coverage: Progresses northward, covering the entire country by mid-July.
- Significance: Accounts for about 75% of India’s annual rainfall.
- Northeast Monsoon:
- Occurrence: October to December.
- Impact: Primarily affects the southeastern coast, especially Tamil Nadu.
2.6 Climatic Regions (Stamp’s Classification)
Stamp’s classification divides India into the following climatic regions
- Tropical Rainy Climate: Western Ghats, northeastern states.
- Tropical Savanna Climate: Central and parts of southern India.
- Humid Subtropical Climate: Northern plains and foothills of the Himalayas.
- Mountain Climate: Himalayan region.
- Arid and Semi-Arid Climate: Rajasthan, parts of Gujarat.
2.7 Climatic Data of Major Cities
City | Avg Temp (°C) | Annual Rainfall (mm) |
---|---|---|
Delhi | 25 | 774 |
Mumbai | 27 | 2,200 |
Kolkata | 26 | 1,582 |
Chennai | 28 | 1,400 |
Bengaluru | 24 | 970 |
Guwahati | 24 | 1,722 |
Jaipur | 25 | 650 |
2.8 Impact of Climate on Agriculture
- Crop Patterns: Monsoon-dependent crops like rice and pulses dominate.
- Irrigation Needs: Regions with low rainfall rely heavily on irrigation.
- Climate Change Effects: Altered rainfall patterns affect sowing and harvesting cycles.
2.9 Climate Change and India
- Rising Temperatures: Increase in average temperatures affects ecosystems.
- Glacial Retreat: Himalayan glaciers are receding, impacting river flows.
- Extreme Weather Events: Increased frequency of floods, droughts, and cyclones