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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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Continental collision of Indian and Eurasian plates
Eastward movement of the Pacific Plate
Closure of the Atlantic Ocean
Stability of the African Plate
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Fold mountain formation
Volcanic island formation
Mid-oceanic ridge formation
Rift valley formation
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Gondwana landmass
Laurasia landmass
Panthalassa Ocean
Arctic Shield
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Earlier and stronger collision with Eurasia
Stopping of Atlantic expansion
Complete erosion of the Himalaya
India remaining near the South Pole
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Compression and convergence still continue
Both plates have become completely stable
The region has become a divergent boundary
The Tethys Sea has reopened
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Passage of the Indian Plate over a hotspot
Melting of Himalayan glaciers
Quiet deposition in the Tethys Sea
Complete closure of the Arabian Sea
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Preserved ancient magnetic direction in rocks
Present direction of river flow
Amount of monsoon rainfall
Present colour of soil
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Path of plate motion in the Indian Ocean
Agricultural yield of the Ganga Plain
Desert climate of Rajasthan
Snowline height of the Himalaya
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Its area shrank and sediments were folded
It changed into the Pacific Ocean
It suddenly became a desert
It underwent no geological change
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New crust at southern oceanic ridges pushed the plate northward
Himalayan rivers pulled the plate
Monsoon winds pushed the plate
Desertification stabilized the plate
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It is a continent-continent convergence zone
It is an ocean-ocean divergence zone
It is a completely inactive intraplate zone
It is formed only by erosion
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Himalayan compression and uplift
Earth’s rotation
Solar radiation
Ocean water salinity
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Plate boundaries are defined by geological boundaries, not political borders
Political boundaries are always plate boundaries
The Indian Plate is limited only to the Ganga Plain
Plates have no physical existence
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Continued convergence of the Indian Plate
Complete disappearance of the Indian Plate
Eurasian Plate becoming oceanic
Submergence of the Deccan Plateau
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Tethys Sea
Arctic Ocean
Pacific Ocean
Southern Ocean
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Because ridges, fractures and magnetic stripes show motion history
Because political capitals are found on the ocean floor
Because seawater keeps plates fixed
Because there is no crust on the ocean floor
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To the south
To the north
Fully attached to the west
Above Eurasia
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Convergence stores stress that is released along faults
Monsoon makes rocks magnetic
River deposits separate plates
Vegetation load melts the crust
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Changing paleomagnetic latitudinal positions in Indian rocks
Seasonal floods in the Ganga
Dust storms in Rajasthan
Number of marine fish
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Because compression folded and uplifted them
Because rainfall immediately solidified them
Because wind pushed them northward
Because ocean water burned them
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New crust at a mid-oceanic ridge pushing a plate away
Ice from the Himalaya pulling the plate southward
River water cutting the plate
Desert sand stopping the plate
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Pulling of a plate by the weight of subducting dense oceanic lithosphere
Pushing of a plate due to new crust formation at a mid-ocean ridge
Lateral movement of a plate due to the weight of river-borne sediments
Uplift of mountains due to atmospheric pressure
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Similar densities limit deep subduction and favor crustal thickening
Both continents easily sink into the mantle
Only an oceanic island arc forms
No earthquakes are possible
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Plate crust and boundaries linked with the Indian Ocean
Only glacial plains
Completely non-volcanic zones
Centre of the Pacific Plate
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This region was once linked with Tethys Sea sediments
The Himalaya is entirely volcanic
The Indian Plate never moved
The Ganga Plain is an ocean floor
Question 1ExpertLevel 1
Which process most directly links the northward movement of the Indian Plate with Himalayan formation?
Correct answer: A
The Indian Plate collided with the Eurasian Plate, uplifting Tethys sediments into the Himalayas. Exam tip: treat the Himalaya as a result of a convergent boundary.
In the context of the Indian Plate, slab pull is considered related to what?
Correct answer: A
Slab pull occurs when cold, dense oceanic lithosphere subducts into the mantle at a convergent boundary. The gravitational weight of the sinking slab pulls the rest of the plate along, so option A is correct. Option B describes ridge push, which is associated with mid-ocean ridges rather than slab pull. Exam tip: link slab pull with subduction and gravity, and ridge push with divergent boundaries.
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