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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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Hard · Level 3
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  1. Because plate tectonics also explains sea-floor spreading and boundary processes
  2. Because continental drift considered India fixed
  3. Because no sea-floor evidence is available
  4. Because the Himalayas have no relation with plates
Hard · Level 3
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  1. Because both regions are completely oceanic
  2. Because it is mainly a collision of continental crust
  3. Because no compression occurred there
  4. Because the Indian Plate moved southward
Hard · Level 3
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  1. Coral reef formation
  2. Quiet deposition on ocean floor
  3. Crustal shortening and thickening due to the push of the Indian Plate
  4. Only river erosion
Hard · Level 3
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  1. Himalayan formation then India moved south then Tethys expanded
  2. Tethys expanded then India remained fixed then Eurasia broke
  3. India separated from Gondwana then moved north then Tethys sediments were compressed
  4. Tethys sediments formed then the Pacific Ocean dried
Hard · Level 3
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  1. Formation of new oceanic crust behind the Indian Plate clarifies its movement path
  2. Sea-floor spreading only controls rainfall
  3. Sea-floor spreading always keeps plates fixed
  4. Sea-floor spreading is related only to coastal fish
Hard · Level 3
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  1. The Himalayas are made only of volcanic ash
  2. Old Tethys Sea sediments were folded and uplifted
  3. India never moved northward
  4. The Eurasian Plate was completely oceanic
Hard · Level 3
View options
  1. Old latitudinal position of rocks and plate journey
  2. Daily sea waves
  3. Direction of present monsoon
  4. Salinity of river water
Hard · Level 3
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  1. Because compression can cause both bending and breaking of rocks
  2. Because the Himalayas formed only by wind
  3. Because rocks always remain liquid
  4. Because plates are completely fixed there
Hard · Level 3
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  1. Local crop cycle
  2. Only river bends
  3. Stress at different depths in the plate contact zone
  4. Only ocean salinity
Hard · Level 3
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  1. Collision uplifted the Himalayas and rivers deposited its sediments in plains
  2. The Indian Plate directly filled the plains with lava
  3. The plains formed only from oceanic trenches
  4. The plains are unrelated to plate movement
Hard · Level 3
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  1. Because it is linked with a major geological phase of the Indian Plate’s northward journey
  2. Because the Deccan Traps are above the Himalayas
  3. Because they are only river sediments
  4. Because they have no volcanic relation
Hard · Level 3
View options
  1. Erosion immediately destroys the mountain
  2. Erosion and uplift together keep modifying Himalayan relief
  3. Erosion has no relation with mountains
  4. Erosion occurs only on the sea floor
Hard · Level 3
View options
  1. It shows the height of sea waves
  2. It shows when crust formed and in which direction spreading occurred
  3. It only shows the age of coastal cities
  4. It directly measures current height of the Himalayas
Hard · Level 3
View options
  1. Northward push of the Indian Plate and seismic stress
  2. Complete reopening of the Tethys Sea
  3. Sinking of the Himalayas into the sea
  4. Immediate reconstruction of Gondwana
Hard · Level 3
View options
  1. Because their density and behaviour change the result of collision
  2. Because both always remain at the same depth
  3. Because both are made only of soil
  4. Because both have no relation with plate movement
Hard · Level 3
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  1. They show the path of rain clouds
  2. They indicate new oceanic crust and plate spreading
  3. They stop all earthquakes
  4. They directly cut the Himalayas
Hard · Level 3
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  1. The folded mountain character of the Himalayas would not develop
  2. The Himalayas would become higher
  3. India would reach the South Pole
  4. The Indian Ocean would close completely
Hard · Level 3
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  1. Stress accumulation due to friction and compression between plates
  2. Change in colour of seawater
  3. Spread of vegetation
  4. Only day and night change
Hard · Level 3
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  1. Long-term marine deposits were later compressed and included in mountain building
  2. Sediments immediately stopped plate movement
  3. Sediments formed only by air and flew away
  4. Sediments have no relation with the Himalayas
Hard · Level 3
View options
  1. Daily rain gauge
  2. Soil fertility test
  3. Satellite based positioning
  4. Ordinary thermometer
Hard · Level 3
View options
  1. Detailed relation of Tethys sediment compression Tibetan uplift and active seismicity
  2. The fact that the Himalayas are in the middle of the sea
  3. The fact that India is fixed
  4. The fact that plates are in the atmosphere
Hard · Level 3
View options
  1. Only by one straight passive boundary
  2. By combined effects of several plate contacts compression and sliding
  3. Only by deposition of coastal sand
  4. Only by monsoon clouds
Hard · Level 3
View options
  1. Deccan Traps are linked with volcanic eruptions while the Himalayas with continental collision
  2. Both are only river deposits
  3. Deccan Traps are collision mountains and Himalayas are lava plains
  4. Both have no relation with the Indian Plate
Hard · Level 3
View options
  1. Because active uplift slopes and seismic shocks increase instability
  2. Because the mountains are completely flat
  3. Because there is no rainfall there
  4. Because rocks never break
Hard · Level 3
View options
  1. Marine expansion occurred behind while continental collision occurred ahead
  2. Both formed only due to weather
  3. The Indian Ocean is a river plain of the Himalayas
  4. India was never mobile

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