UPSC MainsGEOLOGY-PAPER-II201210 Marks
Q35.

Meteorite crater in India and its age.

How to Approach

This question requires a descriptive answer focusing on identified meteorite craters in India and their estimated ages. The answer should begin by defining meteorite craters and briefly explaining their formation. It should then detail known craters, including their location, diameter, estimated age, and any associated geological or historical significance. A structured approach, potentially using a table, will enhance clarity. The answer should demonstrate an understanding of impact events and dating techniques used in geology.

Model Answer

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Introduction

Meteorite craters are geological formations created when a meteorite, asteroid, or comet impacts the surface of a planet or moon. These impacts release immense energy, excavating a bowl-shaped depression. While Earth has been subjected to numerous such impacts throughout its history, erosion, sedimentation, and tectonic activity have obscured many older craters. India, with its diverse geological landscape, hosts several confirmed and suspected meteorite craters, providing valuable insights into the planet’s impact history and the processes shaping its surface. Identifying and dating these craters is crucial for understanding Earth’s geological evolution and potential future impact risks.

Known Meteorite Craters in India

Currently, five meteorite impact structures have been confirmed in India. Several other potential sites are under investigation. The identification and dating of these craters rely on various geological and geochemical techniques, including shock metamorphic features in minerals, breccia analysis, and radiometric dating.

1. Lonar Crater Lake, Maharashtra

Location: Lonar, Buldhana district, Maharashtra. Diameter: Approximately 1.8 km. Age: Estimated to be 52,000 ± 6,500 years (late Pleistocene epoch). This dating is based on Argon-Argon dating of basaltic rocks surrounding the crater. Significance: Lonar Crater Lake is a unique ecosystem, supporting microbial life and attracting significant scientific interest. The lake’s alkaline water and unusual mineral composition are attributed to the impact event. It is a declared National Geo-heritage Monument.

2. Shiva Crater, Rajasthan (Proposed)

Location: Near Lonar, Rajasthan. Diameter: Estimated to be 21 km. Age: Proposed to be approximately 650 million years old (late Neoproterozoic era). Significance: This is a controversial structure, proposed as a potential impact site linked to the Deccan Traps volcanism and possibly contributing to the Cretaceous-Paleogene extinction event. However, its impact origin is still debated, with some geologists attributing it to volcanic activity.

3. Zhamala Crater, Rajasthan

Location: Churu District, Rajasthan. Diameter: Approximately 1.75 km. Age: Estimated to be around 1.2 million years old (Pleistocene epoch). Significance: This crater is relatively well-preserved and exhibits clear evidence of impact, including shock metamorphic features in quartz grains.

4. Ramgarh Crater, Rajasthan

Location: Baran District, Rajasthan. Diameter: Approximately 3.5 km. Age: Estimated to be between 140-470 million years old (Mesozoic era). Significance: This is a highly eroded crater, making precise dating difficult. It is characterized by a circular magnetic anomaly and the presence of breccia.

5. Sirsi Crater, Karnataka

Location: Near Sirsi, Karnataka. Diameter: Approximately 0.4 km. Age: Estimated to be around 1.72 billion years old (Proterozoic era). Significance: This is one of the oldest impact structures in India, identified through the presence of shock metamorphic features in quartz and feldspar.

Dating Techniques

Determining the age of meteorite craters is a complex process. Several techniques are employed:

  • Radiometric Dating: Techniques like Argon-Argon dating are used to date the rocks surrounding the crater, providing a minimum age for the impact event.
  • Shock Metamorphism: The presence of shock metamorphic features (e.g., planar deformation features in quartz) is a strong indicator of an impact event.
  • Breccia Analysis: Studying the composition and structure of breccia (fragmented rock) can provide clues about the impactor and the target rocks.
  • Magnetic Anomalies: Impact craters often create circular magnetic anomalies due to the disruption of the Earth’s magnetic field.
Crater Name Location Diameter (km) Estimated Age
Lonar Maharashtra 1.8 52,000 years
Shiva Rajasthan 21 650 million years (Proposed)
Zhamala Rajasthan 1.75 1.2 million years
Ramgarh Rajasthan 3.5 140-470 million years
Sirsi Karnataka 0.4 1.72 billion years

Conclusion

India’s meteorite craters represent valuable geological archives, offering insights into the planet’s impact history and the processes that have shaped its surface. While Lonar Crater is the most well-known and studied, ongoing research continues to reveal and characterize other potential impact sites. Accurate dating and detailed analysis of these craters are crucial for understanding Earth’s geological evolution, assessing impact hazards, and potentially linking impact events to major geological or biological changes in the past. Further exploration and research are needed to fully understand the impact record of the Indian subcontinent.

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

Impact Crater
A depression in the surface of a planet, moon, or other solid body formed by the hypervelocity impact of a projectile, such as a meteorite, asteroid, or comet.
Shock Metamorphism
Alterations in the mineral structure of rocks caused by the extreme pressure and temperature generated during a high-velocity impact event.

Key Statistics

Approximately 190 impact craters have been confirmed on Earth as of 2023.

Source: Earth Impact Database (as of knowledge cutoff)

The estimated rate of impact events on Earth is one large impact (diameter > 5 km) every 10-20 million years.

Source: NASA Near Earth Object Program (as of knowledge cutoff)

Examples

Chicxulub Crater

The Chicxulub crater, located beneath the Yucatán Peninsula in Mexico, is widely believed to be the impact site associated with the Cretaceous-Paleogene extinction event, which wiped out the dinosaurs approximately 66 million years ago.

Frequently Asked Questions

Why are meteorite craters rare on Earth?

Meteorite craters are relatively rare on Earth due to several factors, including erosion by wind and water, sedimentation, tectonic activity (plate movements), and vegetation cover, which obscure or destroy impact structures over time.