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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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Expert · Level 3
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  1. Convergent collision of Indian and Eurasian plates
  2. Divergent separation of Indian and Antarctic plates
  3. Formation of a stable craton within the Indian Plate
  4. Effect of only tidal currents in the Indian Ocean
Expert · Level 3
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  1. Convergence of the Indian Plate toward the Eurasian Plate
  2. Pacific Plate moving away from North America
  3. African Plate remaining fixed toward the South Pole
  4. South American Plate spreading from west to east
Expert · Level 3
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  1. Plate forces generated by seafloor spreading and mantle convection
  2. Continental pulling only by monsoon winds
  3. Pushing of the plate by Himalayan glaciers
  4. Automatic breaking of the plate by river erosion
Expert · Level 3
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  1. Continental rifting and plate divergence
  2. Continental stability and absence of plates
  3. Complete disappearance of oceanic trenches
  4. Expansion of only fluvial deposition
Expert · Level 3
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  1. Active convergent and collision zone
  2. Completely inactive plate interior
  3. Zone of only desert expansion
  4. Zone of stable oceanic plain
Expert · Level 3
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  1. Passage of the Indian Plate over the Réunion hotspot
  2. Only coral growth in the Tethys Sea
  3. Glacial erosion in the Himalaya
  4. Modern alluvial deposition in the Ganga plain
Expert · Level 3
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  1. Himalayan mountain system
  2. Southern Peninsular Plateau
  3. General coast of the Arabian Sea
  4. Ancient craton of the Deccan
Expert · Level 3
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  1. Northeast India and the Arakan Yoma region of Myanmar
  2. Only the Thar Desert of Rajasthan
  3. Only the lagoon zone of the Malabar Coast
  4. Only the salt flats of Kachchh
Expert · Level 3
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  1. It is linked with a divergent boundary and seafloor spreading in the Indian Ocean
  2. It is the central fault of continental collision in the Himalaya
  3. It is a fluvial alluvial fan of the Ganga plain
  4. It is a terrestrial crater of Deccan lava
Expert · Level 3
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  1. Continental collision with the Eurasian Plate
  2. Sudden decrease in solar radiation intensity
  3. Increase in water discharge of the Ganga
  4. Change in monsoon direction
Expert · Level 3
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  1. They provide the sequence of age and direction of seafloor spreading
  2. They measure only annual monsoon rainfall
  3. They show fertility of river valley soils
  4. They show present ice thickness of the Himalaya
Expert · Level 3
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  1. Himalayan rocks include sediments of the Tethys Sea
  2. The Himalaya was always an arid desert
  3. The Indian Plate never moved
  4. No deposits form on the ocean floor
Expert · Level 3
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  1. Plate convergence and subduction store energy here
  2. There is no plate boundary here
  3. It is only a zone of glacier melting
  4. It is a stable intraplate plain
Expert · Level 3
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  1. Because plate tectonics also includes seafloor spreading and subduction
  2. Because continental drift does not mention any motion
  3. Because the Indian Plate is only a part of the atmosphere
  4. Because oceans are not affected by plates
Expert · Level 3
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  1. By thickening and compression of continental crust
  2. By complete melting of oceanic crust
  3. By stopping of Earth's rotation
  4. Only by increased deposition from river floods
Expert · Level 3
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  1. Because it is part of old rigid cratonic crust
  2. Because it lies on an active convergent boundary
  3. Because it contains only new Tethyan sediments
  4. Because it lies in an oceanic trench
Expert · Level 3
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  1. Continued convergence of the Indian Plate toward Eurasia
  2. Himalaya being completely free from erosion
  3. Indian monsoon remaining identical every year
  4. Deccan lava still spreading across all India
Expert · Level 3
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  1. Seafloor spreading
  2. Static Earth theory
  3. Only river erosion theory
  4. Only glacial deposition theory
Expert · Level 3
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  1. They were compressed, folded and uplifted
  2. They remained unchanged in the deep ocean
  3. They completely changed into atmosphere
  4. They changed only into river deltas
Expert · Level 3
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  1. It shows the shape of active plate boundaries
  2. It determines the rainy season
  3. It shows chemical fertility of soils
  4. It completely controls river courses
Expert · Level 3
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  1. Compressional forces
  2. Tensional forces
  3. Only wind weathering forces
  4. Only tidal forces
Expert · Level 3
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  1. They indicate the latitudinal position at the time of rock formation
  2. They show annual crop production quantity
  3. They show present population density
  4. They show river water quality
Expert · Level 3
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  1. Because it crossed a large oceanic gap in a relatively short time
  2. Because it never passed through any ocean
  3. Because it moved only due to atmospheric pressure
  4. Because it is completely stationary today
Expert · Level 3
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  1. This causes crustal thickening and Himalayan uplift
  2. This turns an oceanic trench directly into a desert
  3. This completely stops the monsoon
  4. This makes plate motion permanently zero
Expert · Level 3
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  1. Divergent motion
  2. Convergent collision
  3. Transform stability
  4. Complete plate inactivity

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