The Deccan Trap of peninsular India was formed by
- A.fissure eruptions of basaltic lava
- B.deposition of sediment in a shallow sea
- C.metamorphism of ancient gneisses
- D.explosive eruptions of a single central volcano
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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.
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