UPSC MainsGEOLOGY-PAPER-I202010 Marks150 Words
Q17.

Briefly describe the economic mineral deposits associated with the Tertiary rocks of India.

How to Approach

This question requires a focused answer detailing the economic mineral deposits found within Tertiary rocks in India. The approach should involve identifying the key Tertiary formations, the types of mineral deposits associated with them, and their geographical distribution. Structure the answer by first briefly outlining the Tertiary geological period and its rock formations in India, then categorizing and describing the economic mineral deposits. Include specific examples of locations and minerals. Avoid overly detailed geological descriptions; focus on the economic aspect.

Model Answer

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Introduction

The Tertiary period (66 to 2.6 million years ago) witnessed significant geological activity in India, resulting in the formation of sedimentary and volcanic rocks across various regions. These Tertiary formations are crucial hosts for several economically important mineral deposits. The Indo-Gangetic Plain, parts of the Himalayas, and the coastal regions are particularly rich in these resources. Understanding the association between Tertiary rocks and mineral deposits is vital for resource management and economic planning. This answer will briefly describe the key economic mineral deposits associated with these rocks, focusing on their occurrence and significance.

Economic Mineral Deposits in Tertiary Rocks of India

Tertiary rocks in India are broadly classified into Lower, Middle, and Upper Tertiary formations, each exhibiting varying mineral potential. The deposits are primarily sedimentary and volcanically derived.

1. Coal

Significant coal deposits are found in the Tertiary formations of North-Eastern India, particularly in Assam, Meghalaya, and Nagaland. These coals are typically lignite to bituminous in rank and are associated with the Numaligarh and Kopili formations. The Tertiary coalfields contribute substantially to the energy needs of the region.

2. Petroleum and Natural Gas

The most prominent economic mineral associated with Tertiary rocks is petroleum and natural gas. The Assam-Arakan basin, a foreland basin formed during the Tertiary period, is a major oil-producing region. Oil and gas are found in sandstones and shales of Oligocene and Miocene age. Major fields include Digboi, Naharkatiya, and Moran in Assam. The Krishna-Godavari basin also contains significant Tertiary oil and gas reserves.

3. Lignite

Lignite deposits are found in the Neyveli lignite fields in Tamil Nadu, associated with the Cuddalore Sandstone formation of the Miocene epoch. These lignite deposits are a crucial source of energy for power generation in South India.

4. Gypsum and Limestone

Tertiary sedimentary formations, particularly in Rajasthan and Gujarat, contain substantial gypsum and limestone deposits. These are used in cement production, fertilizer manufacturing, and other industrial applications. The gypsum deposits are often found as evaporites in lacustrine environments.

5. Iron Ore (Lateritic)

Lateritic iron ore deposits, formed due to weathering of basaltic rocks during the Tertiary period, are found in the Konkan coast of Maharashtra, Goa, and Karnataka. These deposits are relatively low in grade but are important for local iron and steel industries.

6. Bauxite

Bauxite, the primary ore of aluminum, is found in the Tertiary sediments of the Western Ghats and Eastern Ghats. These deposits are formed by the intense weathering of aluminum-rich rocks under tropical conditions.

7. Silica Sand

Tertiary sandstones provide a source of high-quality silica sand, used in glass manufacturing and other industries. These deposits are found in various parts of India, including Rajasthan and Gujarat.

Mineral Tertiary Formation Location
Coal Numaligarh, Kopili Assam, Meghalaya, Nagaland
Petroleum & Natural Gas Oligocene, Miocene Assam-Arakan Basin, Krishna-Godavari Basin
Lignite Cuddalore Sandstone Neyveli, Tamil Nadu
Gypsum & Limestone Miocene Rajasthan, Gujarat
Iron Ore (Lateritic) Tertiary Basalts Konkan Coast (Maharashtra, Goa, Karnataka)

Conclusion

In conclusion, Tertiary rocks of India are significant repositories of various economic mineral deposits, including coal, petroleum, lignite, gypsum, limestone, iron ore, bauxite, and silica sand. These resources play a crucial role in India’s economic development, particularly in the energy, construction, and manufacturing sectors. Further exploration and sustainable exploitation of these mineral resources are essential for ensuring long-term economic growth and energy security. Understanding the geological context of these deposits is vital for efficient resource management.

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

Tertiary Period
The Tertiary Period, spanning from approximately 66 to 2.6 million years ago, is a major division of the Cenozoic Era, characterized by the rise of mammals and significant geological changes.
Laterite
Laterite is a soil and rock type rich in iron and aluminum, formed in hot and wet tropical areas. It is commonly associated with Tertiary basaltic rocks and serves as a source of iron ore and bauxite.

Key Statistics

India holds approximately 3% of the world’s total coal reserves, with a significant portion occurring in Tertiary formations.

Source: Coal Directory of India 2023

As of 2022, India's proven reserves of bauxite are estimated to be around 333 million tonnes, with a significant portion found in Tertiary formations.

Source: Ministry of Mines, Annual Report 2022-23

Examples

Digboi Oilfield

The Digboi oilfield in Assam, discovered in 1889, is one of the oldest oilfields in the world and is located within Tertiary sedimentary rocks. It continues to produce oil even today.

Frequently Asked Questions

What is the significance of the Assam-Arakan basin?

The Assam-Arakan basin is a major oil and gas-producing region in India, formed during the Tertiary period. Its geological structure and sedimentary formations are highly favorable for hydrocarbon accumulation.