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Geography

Forms of condensation: dew, frost, fog, and mist

This Class 12 Geography topic from “Water in the Atmosphere” explains how water vapour changes into visible forms near Earth’s surface. Students learn how cooling, the dew point, relative humidity, and the availability of condensation nuclei produce dew, frost, fog, and mist. The topic distinguishes these forms by temperature, physical state, visibility, and formation conditions, including the role of surface cooling, calm air, and suspended droplets or ice crystals. It also helps students understand their effects on weather, visibility, agriculture, and daily life.

Easy · Level 4 · 25 questions

TOPIC PRACTICE

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

25 questions

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  1. Wind direction
  2. Cloud colour
  3. Ocean depth
  4. Amount of visibility
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  1. Dew point
  2. Boiling point
  3. Sea level
  4. Earthquake focus
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  1. When the surface is very hot
  2. When the surface temperature is below freezing
  3. When air is completely dry
  4. When there is tide in the sea
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  1. Frost
  2. Dust
  3. Dew
  4. Smoke
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  1. Temperature always rises
  2. Rivers dry up
  3. Oxygen ends in the air
  4. Visibility decreases
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  1. Clear sky and calm air
  2. Strong dust storm
  3. Very hot surface
  4. Completely dry air
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  1. Because it immediately increases soil fertility
  2. Because it can damage tender plant cells
  3. Because it always increases rainfall
  4. Because it raises air temperature
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  1. Denser
  2. Completely dry
  3. Less dense
  4. Always icy
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  1. Tiny water droplets
  2. Large stones
  3. Dry sand
  4. Hot lava
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  1. Dew is water vapour formed in the atmosphere, whereas frost is a deposit of dust
  2. Dew is a deposit of liquid water droplets, whereas frost is a deposit of ice crystals
  3. Dew forms only over the sea surface, whereas frost forms only in deserts
  4. Dew forms at high temperature, whereas frost forms without water vapour
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  1. Underground fire
  2. Earthquake
  3. Condensation of water vapour in the air
  4. Melting of rocks
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  1. In strong afternoon heat
  2. During an earthquake
  3. During a sea storm
  4. In the morning
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  1. Near the ground
  2. Above mountain peaks
  3. In the stratosphere
  4. In outer space
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  1. Desert storm
  2. Dew formation
  3. Volcanic eruption
  4. Undersea earthquake
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  1. Dew
  2. Frost
  3. Fog
  4. Mist
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  1. Liquid state
  2. Vapour state
  3. Solid state
  4. Plasma state
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  1. Very dry and hot air
  2. Cooling of moist air
  3. Melting of rocks
  4. Strong underground stream
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  1. It is generally greater
  2. It is always zero
  3. It is always lower
  4. It has no relation with visibility
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  1. Into icy mountains
  2. Into liquid water droplets
  3. Into dry dust
  4. Into salt grains
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  1. Enough water vapour
  2. Only smoke
  3. Only sand
  4. Lava
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  1. Evaporation
  2. Condensation
  3. Weathering
  4. Deposition
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  1. Fog
  2. Dew
  3. Frost
  4. Clear sky
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  1. On cool grass and leaves
  2. On deep ocean floor
  3. Inside a volcano
  4. At the centre of Earth
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  1. Rainfall
  2. Frost
  3. Hot wind
  4. Dust
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  1. When very tiny water droplets are suspended in the air
  2. When the air is completely dry
  3. When the temperature is far above the dew point
  4. When atmospheric pressure suddenly rises greatly

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