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Subjects

Geography

Mass movements, erosion, and deposition

In Class 11 Geography, this topic within “Geomorphic Processes” explains how weathering, gravity, running water, wind, glaciers, waves, and underground water reshape the land. Students learn to distinguish mass movements such as landslides and soil creep from erosion, examine how sediments are transported, and understand deposition that builds features such as fans, floodplains, dunes, moraines, and deltas. It connects processes, landforms, and environmental impacts through clear geographical examples.

Hard · Level 3 · 25 questions

TOPIC PRACTICE

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25 questions

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  1. Cut steep slope and continuous rainfall
  2. Flat dry plain
  3. Stable rock and dense roots
  4. Gentle slope and good drainage
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  1. It permanently cements particles
  2. It can reduce friction on a slip surface and increase movement
  3. It reverses gravity
  4. It completely stops deposition
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  1. Both have the same speed
  2. Both occur only on coasts
  3. Soil creep is slow while debris flow is a water-rich rapid flow
  4. Debris flow has no gravity
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  1. They make a strong staircase
  2. They completely stop rainfall
  3. They form a river mouth
  4. They can form a possible slip plane
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  1. Undercutting at the base and collapse of hard cap rock
  2. Only loess deposition by wind
  3. Lime deposition in caves
  4. Sorting by marine currents
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  1. The valley always remains narrow and deep
  2. The valley widens and a floodplain may develop
  3. The valley instantly turns into a glacier
  4. The valley only becomes a sea cave
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  1. Strong deposition
  2. Strong vertical erosion
  3. Glacial plucking
  4. Sea arch
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  1. Both form only by glaciers
  2. Alluvial fan forms at mountain foot and delta forms at river mouth
  3. Delta always forms in deserts
  4. Alluvial fan forms only by sea waves
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  1. Continuously dissolved in water
  2. Only pressed under a glacier
  3. In short jumps near the surface
  4. Down from a sea cave roof
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  1. They freeze inside a glacier
  2. They form a marine delta
  3. They form lime columns
  4. They are removed by deflation
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  1. One-directional wind and limited sand supply
  2. Dense forest and continuous snowfall
  3. Sea cliff and high tide
  4. Limestone cave and groundwater
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  1. Rock abraded and polished by wind
  2. Meander cut by a river
  3. Moraine formed by glacier
  4. Cave made by groundwater
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  1. They are made only of salt
  2. They consist of fine mineral particles that can retain moisture
  3. They are always glacial ice
  4. They are marine coral
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  1. A tributary glacier erodes less deeply than the main glacier
  2. Wind deposits sand upward
  3. River forms delta at mouth
  4. Sea waves form cave
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  1. Where rock is jointed and ice freezes into cracks to pull blocks
  2. Where a delta forms in the sea
  3. Where dust deposits in wind
  4. Where river only deposits silt
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  1. Moraine is unsorted glacial debris while esker is a long sorted meltwater deposit
  2. Moraine forms by waves and esker by wind
  3. Both form only in limestone caves
  4. Esker is a triangle at river mouth
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  1. Sharp ridge between two glacial valleys
  2. Deposit at a river mouth
  3. Crescent dune made by wind
  4. Sand strip on coast
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  1. Waves force air and water pressure into cracks
  2. Wind changes sand into snow
  3. River deposits dissolved salt
  4. Glacier colors the rock
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  1. Gorge
  2. Spit
  3. U-shaped valley
  4. Stalagmite
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  1. Where uniform hard rock has no joints
  2. Where weak joints and fault zones exist
  3. Where only sandy delta exists
  4. Where glacier deposits moraine
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  1. Surface water disappearing into underground channels
  2. Glacier freezing all water
  3. Sea waves forming valleys
  4. Wind lifting the river upward
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  1. They deposit minerals from the roof and grow the feature downward
  2. They cut river meanders
  3. They form horns of barchans
  4. They push glaciers backward
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  1. It dissolves limestone to form caves and later deposits minerals
  2. It only changes wind direction
  3. It always burns soil
  4. It creates sea tides
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  1. Because they are heavy and settle immediately near the bank
  2. Because they are light and can travel farther with floodwater
  3. Because they remain locked in glaciers
  4. Because they form only in caves
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  1. Presence of river terraces
  2. Column inside sea cave
  3. Limited sand in barchan
  4. Unsorted debris in moraine

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