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Subjects

Geography

Plate Tectonics and the movement of the Indian plate

प्लेट विवर्तनिकी और भारतीय प्लेट की गति

In this Class 11 Geography topic from “Distribution of Oceans and Continents,” students learn how plate tectonics explains the changing arrangement of continents and ocean basins. They study the structure and movement of lithospheric plates, the major types of plate boundaries, and the forces linked to their motion. The topic traces the Indian plate’s journey from Gondwana, its northward movement, and its collision with the Eurasian plate, connecting these processes with the formation of the Himalayas, earthquakes, and volcanism.

TOPIC PRACTICE

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Up to 25 questions from this page. Select your focus, then start.

25 questions

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Medium · Level 5
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  1. They were compressed and involved in fold mountain building
  2. They completely became vapour
  3. They flowed into the Pacific Ocean
  4. They turned into desert sand
Medium · Level 5
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  1. It was the final collision zone of the Indian Plate
  2. India was earlier a part of this southern continental group
  3. It is the present name of the Himalayas
  4. It was only an oceanic trench
Medium · Level 5
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  1. Complete flattening of the sea floor
  2. Drying of the Arabian Sea
  3. Formation and uplift of the Himalayas
  4. Rivers flowing reverse from north to south
Medium · Level 5
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  1. Two plates separating to form a new ocean
  2. Two plates sliding parallel
  3. One plate remaining completely fixed
  4. Convergence of the Indian Plate toward the Eurasian Plate
Medium · Level 5
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  1. Stress still accumulates between the Indian and Eurasian plates
  2. There are no rocks below the Himalayas
  3. Earthquakes are caused only by rainfall
  4. Earthquakes are caused only by ocean salinity
Medium · Level 5
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  1. The Indian Plate submerged Tibet into the sea
  2. Compression from the Indian Plate uplifted the Eurasian region
  3. Tibet formed only by river deposition
  4. Tibet is completely away from plate boundaries
Medium · Level 5
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  1. Formation of an oceanic trench
  2. Freezing in the Tethys Sea
  3. Massive volcanic eruptions
  4. Deposition by Himalayan rivers
Medium · Level 5
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  1. It says India never moved
  2. It only describes coastline shape
  3. It gives daily weather forecast
  4. It explains plate motion and boundary processes
Medium · Level 5
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  1. The condition for India Asia collision would not arise
  2. The Himalayas would become even higher
  3. The Tethys Sea would dry immediately
  4. The Eurasian Plate would disappear
Medium · Level 5
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  1. Only number of marine organisms
  2. Formation of new oceanic crust and plate movement
  3. Only rainfall on coasts
  4. River erosion of the Himalayas
Medium · Level 5
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  1. Closing of Tethys formed no landform
  2. Tethys was only a part of the Pacific Ocean
  3. Tethys sediments were compressed and linked with Himalayan formation
  4. Closing of Tethys moved India southward
Medium · Level 5
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  1. They only show rainfall amount
  2. They show the taste of seawater
  3. They show river direction
  4. They can indicate old latitudinal positions in rocks
Medium · Level 5
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  1. It is mainly continental collision where crust folded and uplifted
  2. Only seawater sank in it
  3. No compression occurred in it
  4. Plates moved apart in it
Medium · Level 5
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  1. Because it alone forms the Indian monsoon
  2. Because India’s collision and Himalayan formation are linked with it
  3. Because it is the smallest plate of the Indian Ocean
  4. Because it is made only of seawater
Medium · Level 5
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  1. Plate boundaries are geologically active zones
  2. Plate boundaries are inactive because unrelated to weather
  3. All plate boundaries are only in oceans
  4. There are no rocks at plate boundaries
Medium · Level 5
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  1. Himalayan formation then separation from Gondwana then Tethys Sea
  2. Separation from Gondwana then northward movement then collision with Asia
  3. Collision with Asia then southward movement then Gondwana
  4. Formation of Tethys then India staying fixed then Himalayas
Medium · Level 5
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  1. The Himalayas were always a desert
  2. The sea still lies above the Himalayas
  3. Himalayan rocks may include old marine sediments
  4. Fossils formed only from air
Medium · Level 5
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  1. Deposition of sand in desert
  2. Formation of coastal marsh
  3. Decrease in sea salinity
  4. Folding and mountain building
Medium · Level 5
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  1. Seismic activity and continuing stress
  2. Constant colour of the sea
  3. Absence of coastline
  4. Complete end of desert
Medium · Level 5
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  1. It immediately melts the crust completely
  2. It allows crust to fold and uplift instead of sinking completely
  3. It stops all earthquakes
  4. It makes the Tethys Sea wider
Medium · Level 5
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  1. River deposition
  2. Coastal erosion
  3. Sea-floor spreading
  4. Rainfall cycle
Medium · Level 5
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  1. It contributed to expansion of the marine region behind India
  2. It changed the Indian Ocean into mountains
  3. It completely closed the Indian Ocean
  4. It changed the Indian Ocean into North America
Medium · Level 5
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  1. It provides a relatively plastic base for plates to move
  2. It is an atmospheric cloud above plates
  3. It is only the ocean surface
  4. It is the solid inner core of Earth
Medium · Level 5
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  1. Only number of trees on coast
  2. Regional concentration of earthquakes and mountain building
  3. Only name of a river
  4. Only distance between cities
Medium · Level 5
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  1. It is only a result of rainfall
  2. It is linked with plate interactions and regional pressure
  3. It is made by sea waves
  4. It occurs due to absence of rocks

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