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Geomorphic Processes

1. Introduction to Geomorphic Processes

  • Definition: Geomorphic processes are natural mechanisms that shape the Earth's surface through the interaction of endogenic (internal) and exogenic (external) forces. These processes create and modify landforms over time.

  • Landforms: Physical features like mountains, valleys, plateaus, and plains are the result of these processes.

  • Example: The Himalayas (formed by endogenic forces) and the Grand Canyon (shaped by exogenic erosion).


2. Types of Geomorphic Processes

A. Endogenic Processes

  • Definition: Processes originating from within the Earth, driven by internal energy (radioactive decay and primordial heat).

  • Types:

    1. Diastrophism:

    • Definition: Deformation of the Earth's crust leading to the formation of mountains, plateaus, and basins.

    • Types:

      • Orogenic Processes: Mountain-building through folding and faulting.

        • Example: Himalayas formed by the collision of the Indian and Eurasian plates.

      • Epeirogenic Processes: Vertical uplift or subsidence of large continental landmasses.

        • Example: Uplift of the Deccan Plateau in India.

    2. Volcanism:

    • Definition: Movement of magma from the Earth's interior to the surface.

    • Types:

      • Intrusive Volcanism: Magma cools and solidifies below the surface (e.g., granite batholiths).

      • Extrusive Volcanism: Lava erupts onto the surface (e.g., shield volcanoes like Mauna Loa, Hawaii).

    3. Earthquakes:

    • Definition: Sudden shaking of the Earth's crust caused by the release of energy along fault lines.

    • Example: 2001 Bhuj earthquake (India) caused by the subduction of the Indian Plate.

B. Exogenic Processes

  • Definition: Processes originating from outside the Earth, driven by solar energy and gravity.

  • Types:

    1. Weathering:

    • Definition: The breakdown of rocks at or near the Earth's surface due to physical, chemical, or biological processes.

    • Example: Freeze-thaw cycles in the Alps (physical weathering).

    2. Erosion:

    • Definition: The wearing away of the Earth's surface by natural agents like water, wind, ice, and waves.

    • Example: Ganga River eroding the Himalayas.

    3. Transportation:

    • Definition: The movement of eroded materials by natural agents.

    • Example: Sediment carried by the Ganga River.

    4. Deposition:

    • Definition: The accumulation of eroded materials in new locations.

    • Example: Formation of the Sundarbans delta by sediment deposition from the Ganga-Brahmaputra rivers.


3. Weathering

  • Definition: The breakdown of rocks at or near the Earth's surface due to physical, chemical, or biological processes.

A. Physical (Mechanical) Weathering

  • Frost Action:

    • Definition: Water freezes in rock cracks, expanding and breaking rocks.

    • Example: Tors (rock formations) in the Himalayas.

  • Thermal Expansion:

    • Definition: Rocks expand by day and contract at night, leading to cracking.

    • Example: Exfoliation domes in Yosemite National Park, USA.

  • Salt Crystallization:

    • Definition: Salt crystals grow in rock pores, causing disintegration.

    • Example: Arid regions like the Thar Desert.

B. Chemical Weathering

  • Oxidation:

    • Definition: Rocks react with oxygen (e.g., iron turns to rust).

    • Example: Red soil in Odisha (high iron content).

  • Carbonation:

    • Definition: Rainwater (CO₂-rich) dissolves limestone.

    • Example: Limestone caves in Mawsmai, Meghalaya.

  • Hydration:

    • Definition: Minerals absorb water and expand.

    • Example: Feldspar converting to clay.

C. Biological Weathering

  • Plant Roots:

    • Definition: Roots grow into rock cracks, causing splitting.

    • Example: Banyan tree roots splitting rocks in tropical regions.

  • Burrowing Animals:

    • Definition: Animals create pores in soil and rocks.

    • Example: Earthworms in agricultural fields.


4. Mass Movements

  • Definition: The downslope movement of material under the influence of gravity.

A. Slow Movements

  • Soil Creep:

    • Definition: Gradual movement of soil (1–2 mm/year).

    • Example: Bent tree trunks on slopes in the Western Ghats.

  • Solifluction:

    • Definition: Saturated soil flows over permafrost.

    • Example: Arctic tundra regions.

B. Rapid Movements

  • Landslides:

    • Definition: Sudden movement of rock and soil down a slope.

    • Example: 2013 Kedarnath landslide (Uttarakhand) triggered by heavy rain.

  • Mudflows:

    • Definition: Rapid flow of water-saturated soil.

    • Example: 1999 Vargas tragedy (Venezuela) caused by heavy rainfall.


5. Erosion and Deposition

  • Erosion:

    • Definition: Removal of surface material by natural agents like water, wind, ice, and waves.

    • Agents of Erosion:

      1. Water: Rivers, rainfall, and ocean waves.

        • Example: Ganga River eroding the Himalayas.

      2. Wind: Common in arid regions.

        • Example: Sandstorms in Rajasthan.

      3. Glaciers: Ice erodes land by plucking and abrasion.

        • Example: U-shaped valleys in the Alps.

      4. Waves: Coastal erosion.

        • Example: Cliffs in Dover, UK.

  • Deposition:

    • Definition: The laying down of eroded material in new locations.

    • Examples:

      1. Deltas: Formed at river mouths (e.g., Sundarbans delta).

      2. Sand Dunes: Formed by wind deposition (e.g., Thar Desert).

      3. Glacial Moraines: Deposits of glacial debris (e.g., Himalayan moraines).


6. Significance of Geomorphic Processes

  • Landform Development: Creates mountains, valleys, plateaus, plains, etc.

    • Example: Himalayas (endogenic) and Grand Canyon (exogenic).

  • Soil Formation: Weathering of rocks contributes to soil formation.

    • Example: Laterite soil in Kerala.

  • Natural Hazards: Processes like earthquakes, landslides, and volcanic eruptions can cause disasters.

    • Example: 2004 Indian Ocean tsunami.

  • Ecological Balance: Influences ecosystems and biodiversity.

    • Example: River deltas supporting rich ecosystems.



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