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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

Correct answer

B. Dharwar system

Explanation

The correct answer is B, the 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. Option A is wrong because the Cuddapah system is poor in metals and is worked instead for cement-grade limestone, asbestos and barytes. Option C is wrong because the Vindhyan system is famous for diamonds and red sandstone rather than for ores. Option D is wrong because the Deccan Trap is a basalt formation whose chief value lies in the black cotton soil it weathers into and in building stone. If a question offers four systems and asks about metals, Dharwar is the answer; if it asks about cement, the answer shifts to Cuddapah.

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

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Q3.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
Show answer
Correct answer: B. 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.

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.