Geomorphic Processes

The earth's crust is constantly being reshaped by a dynamic balance of opposing forces:

• Geomorphic Processes: Physical and chemical actions that induce changes in the configuration of the Earth's surface.
• 1. Endogenic Forces (Internal Constructive Forces): Energy originating from deep within the Earth (radioactive decay, rotational and tidal friction, primordial heat):
  • Diastrophism: Slow, gradual movements of the crust:
    • Orogenic Processes: Mountain-building movements acting tangentially (horizontal compression causing severe folding, thrusting, and faulting).
    • Epeirogenic Processes: Continent-building movements acting radially (vertical uplift or subsidence of large continental landmasses without structural folding).
  • Sudden Movements: Earthquakes and explosive volcanic eruptions causing rapid catastrophic surface dislocation.
• 2. Exogenic Forces (External Denudational Forces): Energy derived from solar radiation and gravity acting on surface rocks: $$\mathbf{\text{Denudation} = \text{Weathering} + \text{Mass Wasting} + \text{Erosion} + \text{Transportation}}$$

Weathering: The mechanical disintegration and chemical decomposition of rocks in situ (on the spot) without active transportation by an agent:

A. Physical / Mechanical Weathering:

• Thermal Expansion & Contraction (Exfoliation): In hot deserts with extreme diurnal temperature ranges, outer rock layers heat up and expand during the day, then cool and contract at night faster than the interior. This generates internal shear stresses, causing outer curved rock sheets to peel off like the skin of an onion (Exfoliation Domes).
• Frost Wedging (Freeze-Thaw): In temperate and high alpine zones, water fills rock crevices. When water freezes into ice, its volume expands by 9%, exerting immense bursting pressure ($>2,000 \text{ kg/cm}^2$), shattering rocks into angular fragments (scree/talus).
• Salt Weathering: Crystallization of sodium and calcium salts in arid rocks forces pore spaces open, disintegrating granular grains.

B. Chemical Weathering:

• Solution: Soluble minerals (halite/rock salt) dissolve directly in water.
• Carbonation: Rainwater absorbs atmospheric $CO_2$ to form weak carbonic acid ($H_2CO_3$), which dissolves calcium carbonate rocks (limestone/marble), carving out underground caves, sinkholes, and Karst Topography.
• Hydration: Minerals absorb water into their crystal lattices, expanding in volume and breaking down (e.g., anhydrous calcium sulfate absorbing water to form gypsum).
• Oxidation: Chemical reaction of oxygen dissolved in water with iron-rich minerals, forming iron oxides ("rusting"), crumbling the rock.

Mass Movement (Mass Wasting): The downslope movement of rock debris and soil under the direct gravitational pull, without being carried by an independent geomorphic medium (like river water, wind, or ice):

A. Slow Mass Movements:

• Soil Creep: The extremely slow, imperceptible continuous downslope movement of soil along moderate slopes. Evidenced by tilted utility telephone poles, bent tree trunks, and tilted fence lines.
• Solifluction: The slow downslope flow of saturated water-logged soil slurry over an impermeable frozen bedrock layer (permafrost) in sub-polar tundra regions.

B. Rapid Mass Movements:

• Slump: The slipping of one or several rock/soil units downward along a distinct curved, concave-upward slip plane.
• Debris Slide & Rockslide: Rapid catastrophic sliding of un-consolidated earth material along a planar slip surface without backward rotation.
• Mudflow: Heavy torrential cloudbursts turn thick soil and clay on deforested slopes into a fluid liquid mud slurry that roars down valleys at high speed.

C. Landslide Comparison: Himalayas vs Western Ghats:

• The Himalayas: Geologically young, structurally weak, seismically active, composed of crushed sedimentary strata, with torrential monsoon cloudbursts, making landslides extraordinarily frequent and devastating.
• The Western Ghats: Geologically ancient, stable basaltic plateau with zero tectonic activity; however, steep vertical escarpments, heavy rainfall (3,000 mm), and human deforestation trigger destructive debris slides during peak monsoons.

Soil: The thin, dynamic, organic-mineral surface layer of the Earth's crust supporting plant life, formed through the interaction of five independent pedogenic factors:

The 5 Fundamental Pedogenic Factors:

1. 1. Parent Material (P): The underlying geological bedrock. Governs the physical texture (sand vs clay), mineral composition, and chemical permeability of the young soil (e.g., Deccan basalt weathers into black cotton soil rich in clay and iron).
2. 2. Relief / Topography (R): Steep mountain slopes promote rapid runoff, preventing water infiltration, resulting in thin, poorly developed soils. Flat alluvial plains and valleys allow deep water retention, yielding thick, mature, fertile soil horizons.
3. 3. Climate (C): The most important single factor. Temperature and precipitation govern the rate and depth of chemical weathering and biological activity:
   • Hot, humid tropics accelerate leaching, forming acidic Laterite soils.
   • Cold tundra climates inhibit chemical weathering, forming thin, peaty soils.
4. 4. Biological Activity / Organisms (O): Microorganisms (bacteria, fungi) decompose dead leaves and animal residues, producing dark, nutrient-rich Humus. Earthworms and termites aerate the soil.
5. 5. Time (T): Determines the maturity of the soil profile. Young soils on steep slopes lack clear layering; mature soils on stable plains feature fully differentiated A, B, and C Horizons.