UPSC MainsGEOGRAPHY-PAPER-I202415 Marks
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Q8.

With suitable sketches elaborate the bottom topography of the Indian Ocean.

How to Approach

This question requires a detailed understanding of the Indian Ocean's bottom topography. The approach should involve first defining key terms, then systematically describing the major features – continental shelf, continental slope, deep-sea plains, oceanic ridges, trenches, seamounts, and guyots. Sketches are crucial for illustrating these features. The answer should be structured geographically, moving from the margins towards the center of the ocean. Focus on the unique features of the Indian Ocean compared to other oceans.

Model Answer

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Introduction

The Indian Ocean, covering approximately 20% of the Earth’s water surface, is the third largest ocean globally. Its unique hydrological characteristics and geological setting contribute to a complex bottom topography. Understanding this topography is crucial for comprehending ocean currents, marine biodiversity, resource distribution, and even seismic activity. The Indian Ocean’s floor is characterized by a diverse range of features, from shallow continental shelves to deep abyssal plains and prominent mid-ocean ridges, shaped by tectonic processes and sedimentation over millions of years. This answer will elaborate on these features with illustrative sketches.

Major Features of the Indian Ocean Bottom Topography

The bottom topography of the Indian Ocean can be broadly divided into four major zones: the continental margin, the deep-sea plains, the mid-ocean ridge system, and the island arcs and trenches.

1. Continental Margin

The continental margin represents the transition zone between the continents and the deep ocean basin. It comprises the continental shelf, continental slope, and continental rise.

  • Continental Shelf: Relatively shallow, gently sloping submerged extension of the continent. It’s widest off the coast of India and Australia. Average depth is around 100 meters.
  • Continental Slope: A steeper incline connecting the continental shelf to the deep-sea plain. It marks the boundary between continental and oceanic crust.
  • Continental Rise: A gently sloping accumulation of sediments at the base of the continental slope.
Continental Margin

2. Deep-Sea Plains (Abyssal Plains)

These are vast, flat, sediment-covered areas located at depths exceeding 3000-6000 meters. They constitute a significant portion of the Indian Ocean floor.

  • Central Indian Basin: A major abyssal plain in the central Indian Ocean, formed by the accumulation of sediments from surrounding landmasses and biogenic sources.
  • Crozet Basin & Kerguelen Plateau: Located in the southern Indian Ocean, these basins are characterized by thick sediment deposits.

3. Mid-Ocean Ridge System

The Indian Ocean is bisected by a prominent mid-ocean ridge system, a chain of underwater mountains formed by volcanic activity and tectonic plate divergence.

  • Central Indian Ridge (CIR): Extends from the Red Sea to the Australian-Antarctic Basin. It’s a seismically active zone with numerous hydrothermal vents.
  • Southwest Indian Ridge (SWIR): Located in the southwestern Indian Ocean, it’s characterized by a complex fracture zone system.
  • Ninety East Ridge: A prominent aseismic ridge extending north-south, believed to be a hotspot track.
Mid-Ocean Ridge

4. Island Arcs and Trenches

These features are associated with subduction zones, where one tectonic plate slides beneath another.

  • Java-Sumatra Trench: A deep-sea trench formed by the subduction of the Indo-Australian Plate beneath the Eurasian Plate. This is a highly seismically active zone.
  • Andaman-Nicobar Trench: Another significant trench formed by the subduction of the Indo-Australian Plate.
  • Island Arcs: Chains of volcanic islands formed parallel to trenches, such as the Andaman and Nicobar Islands and the Indonesian archipelago.

5. Other Significant Features

  • Seamounts: Submarine mountains rising from the seafloor, often volcanic in origin.
  • Guyots: Flat-topped seamounts, formed by wave erosion when they were at or near sea level.
  • Chagos Ridge: A linear feature associated with hotspot volcanism.

Conclusion

The bottom topography of the Indian Ocean is a complex mosaic of features shaped by tectonic activity, sedimentation, and volcanic processes. Understanding these features is vital for comprehending the ocean’s circulation patterns, biological productivity, and geological hazards. Continued research, utilizing advanced technologies like multi-beam sonar and satellite altimetry, is crucial for refining our knowledge of this vast and important oceanic basin. The increasing focus on deep-sea mining also necessitates a thorough understanding of the ocean floor’s topography and its ecological sensitivity.

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 Statistics

The average depth of the Indian Ocean is approximately 3,741 meters (12,274 feet).

Source: National Ocean Service, NOAA (as of knowledge cutoff 2023)

Approximately 65% of the Indian Ocean floor is covered by abyssal plains.

Source: Oceanographic studies (as of knowledge cutoff 2023)

Examples

The Chagos Archipelago

The Chagos Archipelago is a prime example of a hotspot volcanic island chain in the Indian Ocean, formed by the Réunion hotspot. Its formation illustrates the process of seamount and guyot development.

Frequently Asked Questions

How does the Indian Ocean’s topography influence monsoon patterns?

The topography, particularly the presence of ridges and basins, influences ocean currents and upwelling, which in turn affect atmospheric circulation and monsoon rainfall patterns. For example, the Somali Current is intensified by the topography along the East African coast.

Topics Covered

GeographyOceanographyOcean TopographyIndian OceanGeological Features