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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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Medium · Level 3
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  1. Formation of Himalayas and shrinking of Tethys Sea
  2. Complete closure of the Pacific Ocean
  3. Conversion of Sahara Desert into sea
  4. Antarctica joining northern India
Medium · Level 3
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  1. It was part of the Pacific Plate
  2. Its sediments were compressed between Indian and Eurasian plates and linked with Himalayan formation
  3. It still separates India and Asia
  4. It was made only of volcanic islands
Medium · Level 3
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  1. Because both plates moved away from each other
  2. Because both plates remained completely stationary
  3. Because both plates moved toward each other
  4. Because both plates dissolved in seawater
Medium · Level 3
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  1. Himalayan earthquakes occur only due to monsoon
  2. Indian Plate movement has no relation with the Himalayas
  3. Earthquakes occur only on the ocean floor
  4. The moving Indian Plate presses against the Eurasian Plate, creating stress
Medium · Level 3
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  1. Amazon Basin
  2. Tibetan Plateau
  3. Sahara Plain
  4. Great Barrier Reef
Medium · Level 3
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  1. Sea-floor spreading helped explain plate motion and oceanic crust formation
  2. Sea-floor spreading immediately erased all mountains
  3. Sea-floor spreading only increases rainfall
  4. Sea-floor spreading has no relation with plates
Medium · Level 3
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  1. Northward movement of the Indian Plate toward the Eurasian Plate
  2. Retreat of the Indian Plate toward Antarctica
  3. Subduction of the Eurasian Plate into the Pacific Ocean
  4. Only vertical volcanic uplift of the Indian Plate
Medium · Level 3
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  1. It protects plates from weather
  2. It carries river water to oceans
  3. It only creates sea waves
  4. It creates material movement due to internal heat and affects plates
Medium · Level 3
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  1. Himalayas and adjoining areas
  2. Only the southern peninsular stable region
  3. Only the western coastal sea
  4. All parts equally risk-free
Medium · Level 3
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  1. It completely blew them into air
  2. It compressed and folded them, leading to mountain building
  3. It only changed them into fresh water
  4. It sent them to the Pacific Ocean
Medium · Level 3
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  1. Lack of a clear mechanism for movement of continents
  2. Lack of names of continents
  3. Lack of water in oceans
  4. Lack of colours in maps
Medium · Level 3
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  1. Because it involves separation from Gondwana, ocean formation, collision and uplift
  2. Because the Indian Plate never moved
  3. Because it is only a topic of river erosion
  4. Because plates exist only in the atmosphere
Medium · Level 3
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  1. Continued northward movement of the Indian Plate
  2. Southward movement of the Pacific Plate
  3. African Plate joining Antarctica
  4. Stabilisation of sea tides
Medium · Level 3
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  1. Only formation of a deep ocean trench
  2. Folding of thick crustal parts and mountain building
  3. Complete evaporation of ocean water
  4. Lithosphere turning into atmosphere
Medium · Level 3
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  1. Two continental crustal parts
  2. Two atmospheric layers
  3. Two river valleys
  4. Two glacier tongues
Medium · Level 3
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  1. At convergent boundaries plates come together, and at divergent boundaries plates move apart
  2. At convergent boundaries plates disappear, and at divergent boundaries they become air
  3. In both, plates always remain stationary
  4. Both form only along river banks
Medium · Level 3
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  1. Oceanic area developed through separation from Gondwana and sea-floor spreading
  2. The Indian Ocean formed above the Himalayas
  3. The Indian Ocean is only an old name of a river
  4. It was only a weather event
Medium · Level 3
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  1. First Himalayan uplift occurred, then rivers deposited sediments to form plains
  2. First Northern Plains uplifted, then they became Himalayas
  3. Both formed only by volcanic eruption
  4. Both have no relation with plates
Medium · Level 3
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  1. Himalayan earthquakes and continuing crustal stress
  2. Stable ocean tides
  3. Colour of desert sand
  4. Waves of the Southern Ocean
Medium · Level 3
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  1. Breakup process of Pangaea and Gondwana
  2. Only erosion process of the Himalayas
  3. Wave process of the Arabian Sea
  4. Process of monsoon arrival
Medium · Level 3
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  1. It made the collision between India and Asia possible
  2. It stopped Earth's rotation
  3. It made oceans fresh
  4. It ended all plate boundaries
Medium · Level 3
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  1. Earthquake
  2. Rainbow
  3. Sea salinity
  4. Soil fertility
Medium · Level 3
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  1. Plate movement can connect continents, oceans, mountains and earthquakes
  2. All continents remain fixed
  3. Mountains form only by river deposition
  4. Earthquakes occur only due to weather
Medium · Level 3
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  1. Indian Plate moving toward the Eurasian Plate
  2. Pacific Plate moving to the South Pole
  3. Sahara sinking into the sea
  4. Meeting of atmospheric layers
Medium · Level 3
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  1. In subduction one plate sinks below another, while in continental collision thick crust can fold into mountains
  2. Both mean only rainfall
  3. Subduction occurs only in rivers
  4. There is no crust in continental collision

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