answersLogoWhite

0

The formation of fog is a physical change, not a chemical one.

User Avatar

Wiki User

16y ago

What else can I help you with?

Related Questions

What are the examples of condensation?

Examples of condensation include water droplets forming on the outside of a cold glass of water, fog forming on a cool morning, and clouds forming in the atmosphere when warm air rises and cools down.


Is fog a physical or chemical weathering?

Fog is a chemical weathering.


What is the process that changes water vapor into clouds of fog?

The process that changes water vapor into clouds of fog is called condensation. When warm, moist air comes into contact with cooler air or a cooler surface, the water vapor in the air condenses into tiny water droplets, forming fog.


What is the process that changes cloud into fog?

Fog is a cloud on the ground.


Is dry ice changing into theatrical smoke physical or chemical change?

Dry ice doesn't "turn into smoke". Dry ice causes moisture in the air to condense, forming fog. This is a purely physical, not chemical, change.


What is mist and fog examples of?

aerosols


What water droplets are forming and hovering over the ground because the air is being cooled underlying ground what is it?

Fog


Why is Fog forming at night a physical change?

because is liquid to gas


What are examples of water condensing?

when we take a bath the mirror has on it some gas, the steam on the sauna, and maybe fire


How do salt and chemical grains help make fog and rain?

Salt and chemical grains can act as cloud condensation nuclei, providing a surface for water vapor to condense on and form cloud droplets. These droplets can eventually coalesce and grow large enough to fall as rain. In fog formation, these particles can also help water vapor condense into tiny droplets, creating the fog.


What is the process by which material is worn away by forces?

fog forming pataway up the sides of mountains


When Does condenstion form?

Condensation forms when water vapor in the air cools and changes into liquid water. This typically occurs when warm, moist air comes into contact with cooler surfaces or when the air reaches its dew point temperature, where it can no longer hold all the moisture. Common examples include dew forming on grass in the morning and fog developing in cooler temperatures.