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Geography

Endogenic and exogenic forces

In this Class 11 Geography topic from the chapter Geomorphic Processes, students learn how endogenic forces originate within the Earth and shape its surface through tectonic movements, folding, faulting, earthquakes, and volcanism. They also examine exogenic forces acting at or near the surface, including weathering, erosion, mass movement, and deposition. The topic explains how these internal and external processes interact over time to create and modify landforms such as mountains, valleys, plains, and plateaus.

Hard · Level 2 · 25 questions

TOPIC PRACTICE

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25 questions

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  1. Climate and rock nature
  2. Only Earth’s core
  3. Only colour of magma
  4. Only names of plates
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  1. Deposition and low gradient
  2. Vertical erosion and high potential energy
  3. Volcanism and magma eruption
  4. Isostasy and crustal balance
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  1. Earthquake endogenic
  2. Weathering exogenic
  3. Crustal uplift exogenic
  4. Deposition exogenic
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  1. Only wind deposition
  2. Rejuvenation of the plateau or base-level change followed by erosion
  3. Only immediate volcanic eruption
  4. Complete absence of weathering
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  1. Endogenic because it is driven by magma
  2. Endogenic because it folds the crust
  3. Exogenic because an external agent erodes the surface
  4. Endogenic because it is only an earthquake
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  1. When transport energy decreases
  2. When slope suddenly becomes very steep
  3. When river carrying capacity increases
  4. When the crust uplifts rapidly
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  1. They keep it unchanged forever
  2. They only create new magma chambers
  3. They modify it through weathering, erosion and deposition
  4. They stop giving energy to plates
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  1. They occur only suddenly
  2. They occur only over millions of years
  3. They never form landforms
  4. They may occur as slow crustal movements and sudden earthquakes
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  1. Limestone in warm and humid climate
  2. Very low moisture in dry desert
  3. Permanent freezing in glaciated area
  4. Crust melting in magma chamber
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  1. Humid tropical forest
  2. Mountain area with repeated freezing and thawing
  3. Warm swampy area
  4. Deep ocean floor
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  1. Wind depositing sand to form a dune
  2. Fault formation by earthquake
  3. Cone formation by lava
  4. Folding of crust
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  1. They always level the surface
  2. They can form mountains, plateaus and volcanic forms
  3. They only chemically dissolve rocks
  4. They only deposit sediments in river beds
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  1. Because climate changes the nature of weathering, runoff and erosion
  2. Because climate directly changes the number of plates
  3. Because no process acts on similar rocks
  4. Because endogenic forces disappear
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  1. Weathering, erosion, transport, deposition
  2. Volcanism, earthquake, folding, faulting
  3. Deposition, crustal uplift, magma, earthquake
  4. Faulting, folding, weathering, crust formation
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  1. Rivers may incise more deeply
  2. River water will immediately disappear
  3. All rivers will only deposit
  4. River erosion will become an endogenic process
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  1. Formation of only magma by endogenic forces
  2. Cutting down of highs and filling of lows by exogenic processes
  3. Sudden breaking of crust by earthquake
  4. Only convergence of plates
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  1. Glacier carrying rock fragments down a valley
  2. Magma rising in the mantle
  3. Faulting of the crust
  4. Generation of earthquake waves
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  1. Endogenic forces create relief, exogenic forces modify and reduce relief
  2. Endogenic forces only form soil, exogenic forces uplift mountains
  3. Both only perform marine deposition
  4. Neither has any relation with landforms
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  1. Water enters jointed rocks and accelerates weathering
  2. Magma colour decides river velocity
  3. Plate name decides rainfall
  4. Earthquake always stops weathering
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  1. Exogenic deposition followed by endogenic folding
  2. Endogenic volcanic deposit followed by exogenic water erosion
  3. Only chemical weathering
  4. Only marine deposition
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  1. Long-term exogenic erosion and leveling
  2. Sudden inward folding of crust
  3. Only propagation of earthquake waves
  4. Only solidification of magma
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  1. Landslides increase on steep slopes after seismic uplift
  2. Magma forms from river deposition
  3. Wind erosion forms a plate boundary
  4. Crustal folding by sea waves
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  1. Some processes are instantaneous while others continue for millions of years
  2. All processes finish in one day
  3. All exogenic processes occur only in one second
  4. Timescale has no relation with landforms
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  1. Weathering breaks rock and provides loose material for erosion
  2. Weathering always uplifts the crust
  3. Weathering only makes magma
  4. Weathering completely stops a river
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  1. Endogenic processes build relief and exogenic processes continually reshape it
  2. Exogenic processes remain limited inside Earth
  3. Endogenic processes only form sand dunes
  4. Both processes always remain without change

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