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Subjects

Geography

Hydrological cycle

जल चक्र

In this Class 11 Geography topic from the chapter Water (Oceans), students learn how water continuously moves between oceans, the atmosphere, land and living organisms. The topic explains key processes such as evaporation, condensation, precipitation, transpiration, infiltration, surface runoff and groundwater flow. It also shows how solar energy drives the hydrological cycle, how oceans influence the global water balance, and why these processes matter for rainfall, freshwater availability and environmental systems.

TOPIC PRACTICE

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Up to 25 questions from this page. Select your focus, then start.

25 questions

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Medium · Level 1
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  1. Because it participates only in respiration
  2. Because it is linked with heat retention and precipitation formation
  3. Because it is the main source of nitrogen
  4. Because it is more permanent than argon
Medium · Level 1
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  1. It supplies major moisture to the atmosphere
  2. It immediately makes oceans fresh
  3. It completely stops groundwater
  4. It removes clouds
Medium · Level 1
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  1. Dry and hot air
  2. Cool and saturated air
  3. Below ocean floor
  4. Near very hot lava
Medium · Level 1
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  1. Transpiration
  2. Ocean tide
  3. Seismic vibration
  4. Ocean salinity
Medium · Level 1
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  1. It always becomes infinite
  2. It may decrease
  3. It becomes ocean tide
  4. It stops condensation
Medium · Level 1
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  1. Winds
  2. Age of rocks
  3. Earth's core
  4. Colour of sea salt
Medium · Level 1
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  1. Surface runoff
  2. Solar radiation
  3. Seismic wave
  4. Ocean salinity
Medium · Level 1
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  1. They store water as ice for long periods
  2. They immediately empty oceans
  3. They turn clouds into soil
  4. They completely stop evaporation
Medium · Level 1
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  1. Ocean waves
  2. Groundwater storage
  3. Colour of clouds
  4. Sea salt
Medium · Level 1
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  1. The Sun causes evaporation and gravity makes water fall and flow
  2. Both only increase salinity
  3. Both cause earthquakes
  4. Both make clouds permanent
Medium · Level 1
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  1. Surface runoff
  2. Condensation
  3. Oceanic evaporation
  4. Salinity becoming zero
Medium · Level 1
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  1. When moist air rises and cools
  2. When ocean salt disappears
  3. When rivers flow backward
  4. When the soil becomes completely dry
Medium · Level 1
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  1. On steep slopes and during heavy rainfall
  2. In a completely calm ocean
  3. During dry conditions with little available water
  4. Only in deep underground layers
Medium · Level 1
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  1. Porous soil
  2. Concrete surface
  3. Very steep slope
  4. Highly impermeable rock
Medium · Level 1
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  1. When droplets become large enough to fall by gravity
  2. When clouds are completely empty
  3. When oceans have no water
  4. When air has no moisture at all
Medium · Level 1
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  1. Snowmelt and groundwater flow
  2. Colour of sea salt
  3. Shine of rocks
  4. Sound of earthquakes
Medium · Level 1
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  1. Evaporation, precipitation, river flow, and ice melt
  2. Only colour of clouds
  3. Only desert dust
  4. Only rock texture
Medium · Level 1
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  1. Precipitation and runoff
  2. Tide and salinity
  3. Earthquake and weathering
  4. Transpiration and lava
Medium · Level 1
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  1. Low precipitation for a long time
  2. More earthquakes
  3. Change in colour of sea salt
  4. Rocks becoming harder
Medium · Level 1
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  1. During heavy rainfall and low infiltration
  2. During light rainfall and high infiltration
  3. In moistureless air
  4. When there are no waves in the sea
Medium · Level 1
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  1. Because atmospheric circulation can carry moisture far away
  2. Because water vapour always stays in the ocean
  3. Because rainfall occurs only over oceans
  4. Because winds have no relation with moisture
Medium · Level 1
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  1. Both can transfer land water onward
  2. Both are found only in clouds
  3. Both produce sea salt
  4. Both stop solar heat
Medium · Level 1
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  1. Transpiration
  2. Salinity
  3. Ocean current
  4. Seismic wave
Medium · Level 1
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  1. Surface water reservoir
  2. Earthquake source
  3. Sea salt source
  4. Lava flow
Medium · Level 1
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  1. Concrete surfaces reduce infiltration and increase runoff
  2. Groundwater becomes infinite everywhere
  3. Cloud formation becomes impossible
  4. Ocean water immediately decreases

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