Solution:Meghalaya plateau is an extension of the Peninsular plateau . It is believed that due to the force exerted by the north eastward movement of the Indian plate at the time of the Himalayan origin , a huge fault was crested between the Raajmahal hills and the Meghalaya plateau .Later, this depression got filled up by the deposition activity of numerous rivers. Today the Meghalaya and Karbi Anglong plateau stand detached from the main Peninsular Block. Thus statement (1) is correct . The Valley of Kashmir was formed in a synclinorium . The Indo-Gangetic basin is an active foreland basin having east -west elongated shape .
The basin formed is response to the uplift of Himalaya after the collision of India and China plates ( Dewey and bird , 1970 ). Suess ( 1893-1909) was the first geologist to suggest that the Indo- Gangetic depression is A 'fore deep ' and was formed in front of the high crust - waves of the Himalayas as their southward migration was resisted by the Himalayas as their southward migration was resisted by the rigid Landmass of the Peninsula.
Thus statements (3) is also correct . The Himalayas mountain range and Tibetan plateau have formed as a result of the collision between The Indian plate and the Eurasian plate . Chinese plate is not mentioned in the theory of plate tectonics . Thus statements (4) is wrong .