If the water cools to the saturation point (or dew point), water will begin to condense into liquid water on some exposed objects.
Water vapor
Clouds are made out of atmospheric water vapor. They form in part due to cooling in the upper atmosphere.
The cooling of water vapor to form liquid water is called condensation. It occurs when the temperature of the water vapor decreases, causing the vapor molecules to come together and form liquid droplets.
Saturation occurs in the atmosphere when the air reaches its maximum capacity to hold water vapor. This can happen through processes like cooling, uplift, or mixing of air masses. Once saturation is reached, water vapor begins to condense into liquid water droplets, which form clouds.
Crystallization from water vapor in the atmosphere is not a method by which minerals form. Minerals typically form through processes such as cooling of magma, precipitation from solution, or organic activity.
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Water existing in gaseous form makes up the water found int the atmosphere and this is called Water-vapor.
Condensation mostly occurs in the hydrosphere, specifically in the form of water droplets that accumulate on surfaces due to cooling of water vapor in the air. This process is a key part of the water cycle, with water evaporating from bodies of water into the atmosphere and then condensing back into liquid form.
The most abundant liquid in Earth's atmosphere is water in the form of vapor. Water vapor can make up around 0-4% of the atmosphere, depending on location and weather conditions.
Water vapor from the atmosphere condenses to form clouds. When the air cools, it can no longer hold all the moisture it contains, causing the water vapor to condense into tiny water droplets or ice crystals, which then come together to form clouds.
Rain is formed when water vapour cools.
The Earth's atmosphere contains about 0.001 of water in the form of water vapor.