Water is formed in the atmosphere through the process of condensation, where water vapor cools and turns into liquid droplets. These droplets then combine to form clouds and eventually fall to the Earth's surface as precipitation, such as rain, snow, sleet, or hail.
Precipitation that falls on land can accumulate in bodies of water like lakes, rivers, and streams. These surface water sources are replenished by rainfall and runoff from surrounding areas.
Some precipitation seeps into the ground and is stored in underground reservoirs called aquifers. These aquifers are made up of porous rocks or soil that can hold and transmit water. Groundwater can be accessed through wells and springs.
In polar regions and high-altitude areas, water is stored in the form of ice in glaciers and ice caps. When these ice formations melt, they release water into rivers and oceans.
Water can also be obtained through the process of desalination, where saltwater from oceans or saline groundwater is treated to remove the salt and make it suitable for drinking or irrigation.
Overall, water is constantly cycling through the Earth's atmosphere, land, and oceans in a process known as the water cycle or hydrological cycle.
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