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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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25 questions

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Expert · Level 2
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  1. Uplift of the Himalaya and Tibetan Plateau
  2. Formation of the Amazon Basin
  3. Complete glaciation of Sahara
  4. Disappearance of the Mid-Atlantic Ridge
Expert · Level 2
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  1. Actual movement of the lithospheric plate
  2. Only change in sea level
  3. Only change in rainfall zones
  4. Only change in human boundaries
Expert · Level 2
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  1. Divergent boundary
  2. Convergent boundary
  3. Transform boundary only
  4. Passive political boundary
Expert · Level 2
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  1. Convergence with the Eurasian Plate
  2. Moving away from Antarctica alone
  3. Southward movement of the Pacific Plate
  4. Atmospheric pressure of the African Plate
Expert · Level 2
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  1. Because convergence is still continuing
  2. Because plate tectonics has now ended
  3. Because the Himalaya has submerged into the sea
  4. Because India has rejoined Gondwana
Expert · Level 2
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  1. Mantle convection and boundary forces are major in plate motion
  2. Monsoon alone moves plates
  3. Cyclones change plate direction
  4. Rainfall turns mountains into plates
Expert · Level 2
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  1. Slow flow of mantle material moves lithospheric plates
  2. Ocean water directly floats the plate away
  3. Earth’s shadow pushes plates
  4. Rivers cut and move plates forward
Expert · Level 2
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  1. It is mainly formed by compression and folding
  2. It is made only of lava piles
  3. It lies on a divergent ridge
  4. It formed by freezing of seawater
Expert · Level 2
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  1. Separating from Gondwana and moving north over millions of years
  2. Formation of the Himalaya in one monsoon season
  3. Closure of the Tethys Sea in one day
  4. Disappearance of the Tibetan Plateau in one year
Expert · Level 2
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  1. Crustal thickening and mountain uplift
  2. Complete dissolution of crust
  3. Ocean floor remaining unchanged
  4. Elimination of all faults
Expert · Level 2
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  1. Convergence of the Indian and Eurasian plates
  2. Atlantic sea-floor spreading
  3. Pacific island arc formation
  4. Stability of the Arabian Plate
Expert · Level 2
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  1. Because modern explanation includes plate boundaries, sea-floor spreading and mantle processes
  2. Because continents never move
  3. Because only rivers move continents
  4. Because mountains are separate from plates
Expert · Level 2
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  1. Daily temperature change
  2. Plate convergence
  3. Folding of sediments
  4. Crustal compression
Expert · Level 2
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  1. Continued convergence and stress accumulation
  2. Complete stability
  3. Divergent oceanic expansion
  4. Political boundary change
Expert · Level 2
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  1. Sea-floor spreading
  2. Glacial erosion
  3. River meandering
  4. Desertification
Expert · Level 2
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  1. Rifting and sea-floor spreading
  2. Himalayan folding only
  3. River alluvial deposition only
  4. Vegetation expansion
Expert · Level 2
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  1. It marked India’s independent northward motion
  2. It instantly formed the Himalaya
  3. It rejoined Gondwana
  4. It enlarged the Tethys Sea
Expert · Level 2
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  1. Continental crust is lighter and less dense
  2. Continental crust is always liquid
  3. Continental crust has no rocks
  4. Continental crust is made only of water
Expert · Level 2
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  1. Active plate boundaries and fault zones
  2. Only high rainfall areas
  3. Only old cities
  4. Only agricultural land
Expert · Level 2
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  1. The Himalaya is the result of convergent continental collision
  2. The Himalaya is a mid-oceanic ridge
  3. The Himalaya is only a volcanic island
  4. The Himalaya is unrelated to plate boundaries
Expert · Level 2
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  1. Evidence of sea-floor spreading
  2. Evidence of monsoon change
  3. Evidence of river erosion
  4. Evidence of soil formation
Expert · Level 2
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  1. Paleomagnetism, ocean-floor stripes and plate reconstructions
  2. Only legends and weather reports
  3. Only names of rivers
  4. Only administrative maps
Expert · Level 2
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  1. Push from south toward north and resistance from the north
  2. East to west river current only
  3. Downward rainfall pressure
  4. West to east sea wave
Expert · Level 2
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  1. It is a major example of crustal thickening and uplift due to collision
  2. It is the deepest part of the Pacific Ocean
  3. It is the unchanged centre of Gondwana
  4. It is only a river delta
Expert · Level 2
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  1. Separation from Gondwana, northward movement, closure of Tethys, Himalayan formation
  2. Himalayan formation, joining Gondwana, southward movement, Tethys expansion
  3. Tethys closure, Pacific expansion, India remaining fixed, Himalayan erosion
  4. India remaining fixed, Ganga Plain formation, Gondwana formation, ocean disappearance

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