UPSC MainsGEOLOGY-PAPER-I202120 Marks150 Words
Q7.

Discuss the geomorphic processes. Cite any four aggradational and four degradational land forms associated with fluvial processes.

How to Approach

This question requires a demonstration of understanding of geomorphic processes and their resulting landforms. A good answer will define geomorphic processes, categorize them into degradational and aggradational types, and then provide four examples of each associated with fluvial (river) processes. Structure the answer by first defining geomorphic processes, then explaining degradational and aggradational processes separately with examples. Focus on clarity and precision in describing the landforms.

Model Answer

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Introduction

Geomorphic processes are the natural forces that shape the Earth's surface, leading to the creation of various landforms. These processes can be broadly categorized into endogenic (internal forces like plate tectonics and volcanism) and exogenic (external forces like weathering, erosion, and deposition). Fluvial processes, specifically those related to rivers and streams, are a significant component of exogenic processes, responsible for both eroding and building up land surfaces. Understanding these processes is crucial for comprehending landscape evolution and associated hazards. This answer will discuss these processes and illustrate them with relevant landforms.

Geomorphic Processes: An Overview

Geomorphic processes are the physical, chemical, and biological actions that modify the Earth’s surface. They operate at different scales, from microscopic weathering to large-scale tectonic movements. Exogenic processes, driven by solar energy, gravity, and atmospheric forces, are particularly important in shaping landscapes over time. These processes can be further divided into degradational (erosional) and aggradational (depositional) processes.

Degradational Landforms (Fluvial)

Degradational processes involve the wearing away and removal of earth material. In fluvial systems, these processes lead to the formation of landforms characterized by erosion and downcutting. Four examples are:

  • V-Shaped Valleys: Formed in the upper course of rivers where vertical erosion dominates. The river cuts downwards, creating steep sides and a narrow valley floor.
  • Potholes: Cylindrical depressions eroded into the bedrock of riverbeds due to the abrasive action of pebbles and boulders carried by the river current.
  • Meanders: Develop in the middle and lower courses of rivers as lateral erosion becomes more prominent. These are winding curves formed due to variations in channel gradient and sediment load.
  • Rapids and Waterfalls: Created where a river flows over resistant bedrock. Differential erosion leads to a steep gradient and turbulent flow, forming rapids. If the resistant layer is undercut, a waterfall develops.

Aggradational Landforms (Fluvial)

Aggradational processes involve the building up of land surfaces through deposition of sediment. In fluvial systems, these processes result in landforms created by the accumulation of eroded material. Four examples are:

  • Alluvial Fans: Fan-shaped deposits of sediment formed at the base of mountains or hills where a stream emerges onto a plain. The stream loses its velocity and deposits its load.
  • Floodplains: Flat areas adjacent to a river channel that are periodically inundated during floods. They are formed by the deposition of sediment during flood events.
  • Levees: Natural embankments formed along the banks of a river due to the deposition of coarser sediment during floods. They help to contain the river within its channel.
  • Deltas: Landforms created at the mouth of a river where it enters a lake or sea. The river's velocity decreases, causing it to deposit its sediment load, forming a triangular or fan-shaped landform. The Ganges-Brahmaputra delta is a prime example.

The interplay between degradational and aggradational processes determines the overall landscape evolution. For instance, a river might erode a V-shaped valley in its upper course (degradation) and then deposit sediment to form a floodplain in its lower course (aggradation).

Conclusion

In conclusion, geomorphic processes, particularly fluvial ones, are fundamental in shaping the Earth’s surface. Degradational processes erode and remove material, creating features like V-shaped valleys and waterfalls, while aggradational processes deposit sediment, forming landforms such as deltas and floodplains. The dynamic interaction between these processes results in a constantly evolving landscape. Understanding these processes is vital for effective river management, hazard mitigation, and sustainable land use planning.

Answer Length

This is a comprehensive model answer for learning purposes and may exceed the word limit. In the exam, always adhere to the prescribed word count.

Additional Resources

Key Definitions

Geomorphology
The scientific study of the origin, evolution, and distribution of landforms. It integrates aspects of geology, geography, climatology, and hydrology.
Base Level
The lowest level to which a stream can erode its channel. It can be sea level, a lake, or another stream.

Key Statistics

Approximately 78% of India’s land area is prone to flooding, highlighting the significance of fluvial processes and associated landforms.

Source: National Disaster Management Authority (NDMA), India (as of 2023 knowledge cutoff)

India has approximately 14 major river basins, covering about 85% of the country’s geographical area, making fluvial landforms dominant.

Source: Central Water Commission (CWC), India (as of 2023 knowledge cutoff)

Examples

The Sundarbans Delta

The Sundarbans delta, formed by the confluence of the Ganges, Brahmaputra, and Meghna rivers, is the world’s largest mangrove forest and a classic example of a deltaic landform. It demonstrates the extensive depositional power of fluvial systems.

Frequently Asked Questions

How does human activity influence fluvial geomorphic processes?

Human activities like deforestation, urbanization, and dam construction significantly alter fluvial processes. Deforestation increases erosion, urbanization increases runoff, and dams trap sediment, disrupting natural deposition patterns and potentially leading to increased erosion downstream.

Topics Covered

GeographyGeologyErosionDepositionFluvial ProcessesLandform Development