🌏 Geography of Bihar Chapter 1: Location, Geological Structure & Alluvium (स्थिति एवं भूगर्भिक संरचना)

Module 2: Geological structure

📖 Chapter 1 of 17 🧩 Module 2 of 5 ⏱️ ~2 min read 💡 6 MCQs
Topic Part 1 of 2

Subtopic 2.1: Geological structure

  • Bihar's rocks range from the Quaternary back to the Pre-Cambrian era.
  • The alluvial plain is the newest structure. In the southern marginal plateau, Archean (very old) rocks are found.
  • Four distinct surfaces: (1) Tertiary Siwalik rocks in the north; (2) Pleistocene alluvium of the Ganga plain; (3) Kaimur plateau with Vindhyan limestone and sandstone; (4) Archean rocks of the southern marginal plateau.
  • The plain is about 95% of the state and developed over the ancient Tethys Sea.
  • By the geosyncline theory, the Himalaya formed from the compression of Tethys sediments.
  • A huge foredeep formed south of the Himalaya. Rivers coming from the plateau of Gondwanaland dumped sediments there, forming the Ganga plain in the Pleistocene.
  • The plain is made of loose clay, silt and sand of varying grain size. Plate-like layers at depth give the underground water a special character.
⭐ Key Points
  • The alluvial plain (Ganga plain) is the youngest structure.
  • The southern border plateau (Chotanagpur side) carries Archean rocks.
  • The plain, about 95% of the state, formed over the Tethys Sea.
  • Kaimur is Vindhyan-age limestone and sandstone.
  • Compression of Tethys Sea sediments raised the Himalaya.
  • Sediments of rivers from the Gondwanaland plateau filled the foredeep in the Pleistocene.
📌 One-line Q&A
  • Question: Which is the newest geological structure of Bihar? Answer: The alluvial plain.
  • Question: Archean rocks are found in: Answer: Southern marginal plateau.
  • Question: The Bihar plain developed over the ancient: Answer: Tethys Sea.
  • Question: The Kaimur plateau consists of: Answer: Vindhyan limestone and sandstone.
  • Question: According to the geosyncline theory the Himalaya formed by: Answer: Compression of Tethys sediments.
  • Question: The Ganga plain was built in which epoch? Answer: Pleistocene.
Topic
Questions

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Question 1: Which is the newest geological structure of Bihar?

The alluvial plain (Ganga plain) is the youngest structure.

Question 2: Archean rocks are found in:

The southern border plateau (Chotanagpur side) carries Archean rocks.

Question 3: The Bihar plain developed over the ancient:

The plain, about 95% of the state, formed over the Tethys Sea.

Question 4: The Kaimur plateau consists of:

Kaimur is Vindhyan-age limestone and sandstone.

Question 5: According to the geosyncline theory the Himalaya formed by:

Compression of Tethys Sea sediments raised the Himalaya.

Question 6: The Ganga plain was built in which epoch?

Sediments of rivers from the Gondwanaland plateau filled the foredeep in the Pleistocene.
Question 1 of 6

Write your answer, then submit to see the correct answer.

Which is the newest geological structure of Bihar?

The alluvial plain.

Archean rocks are found in:

Southern marginal plateau.

The Bihar plain developed over the ancient:

Tethys Sea.

The Kaimur plateau consists of:

Vindhyan limestone and sandstone.

According to the geosyncline theory the Himalaya formed by:

Compression of Tethys sediments.

The Ganga plain was built in which epoch?

Pleistocene.
Question 1 of 6