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The water cycle, also known as the hydrological cycle, is a continuous process that moves water around our planet. It plays a critical role in sustaining life and maintaining the Earth's climate. The cycle starts when the sun heats up oceans, lakes, and rivers. This heat causes water to evaporate, turning it into invisible water vapor. Plants also release water vapor through their leaves in a process called transpiration.

Once in the atmosphere, the water vapor cools down and condenses into tiny droplets, forming clouds. This stage is called condensation. As more and more water droplets join together, the clouds become heavier and eventually release the water back to the Earth in the form of precipitation. Precipitation can be rain, snow, sleet, or hail, depending on the temperature.

After precipitation, the water travels back to lakes, rivers, and oceans. Some of it flows along the surface in streams and rivers, known as surface runoff. Other water seeps into the ground to replenish underground reservoirs called aquifers, which people and plants often tap for drinking and irrigation. This process is called infiltration. From there, groundwater slowly makes its way to rivers, lakes, and oceans.

The water cycle ensures that the Earth never runs out of fresh water. Each step is vital, maintaining the balance of life across ecosystems. This natural process purifies water and helps distribute essential nutrients and minerals. By understanding the water cycle, people can better appreciate the importance of conserving water and protecting the environment.