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GK24
GeographyMedium

The diamond-bearing conglomerates of India, including those of the Panna area, occur in which rock system?

  1. A.Archaean system
  2. B.Vindhyan system
  3. C.Gondwana system
  4. D.Tertiary system

Correct answer

B. Vindhyan system

Explanation

The correct answer is B, the Vindhyan system. The sandstones, shales and limestones of this Purana system, which stretch across central India into the Son valley, contain the conglomerate beds in which diamonds are found, and the Panna mines of Madhya Pradesh as well as the diamonds once traded from the Kurnool area are associated with them. The same system supplied the red sandstone used in the Qutub Minar, the Red Fort, Fatehpur Sikri and the Sanchi stupa. Option A is wrong because the Archaean rocks are gneisses and granites that form the Basement Complex of the Peninsula and carry no diamonds. Option C is wrong because the Gondwana system is the coal-bearing system. Option D is wrong because the Tertiary rocks are the fuel rocks of the Himalayan and coastal basins, holding petroleum and lignite. Pairing each system with one mineral is the fastest way to secure these marks.

Read the full article: Geological Structure and Rock Systems of India Notes

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Q3.GeographyMedium

Which rock system of India is the richest in metallic minerals such as iron ore, manganese and gold?

  1. A.Cuddapah system
  2. B.Dharwar system
  3. C.Vindhyan system
  4. D.Deccan Trap
Show answer
Correct answer: B. Dharwar system

Named after the Dharwar region of Karnataka, it is the oldest metamorphosed sedimentary system in India and is described as highly metalliferous, yielding iron ore, manganese, gold, copper, lead, zinc and mica; the Champion gneiss of the Kolar gold field belongs to it.

Q5.GeographyMedium

The Deccan Trap of peninsular India was formed by

  1. A.fissure eruptions of basaltic lava
  2. B.deposition of sediment in a shallow sea
  3. C.metamorphism of ancient gneisses
  4. D.explosive eruptions of a single central volcano
Show answer
Correct answer: A. fissure eruptions of basaltic lava

At the close of the Cretaceous, highly fluid lava welled out of long cracks in the crust in the north-western Deccan and spread as sheet after sheet over Maharashtra and parts of Gujarat and Madhya Pradesh; the flat, step-like arrangement of these flows is what the word trap describes.