The total water supply is approximately 332.5 million cubic miles of water, which covers approximately 70% of the Earth's surface. With so much water inhabiting our planet, there obviously has to be a way to keep the water moving. We call this the water cycle, which has been around for longer than we know. The great thing about the water cycle is that it can never stop working because the water is always evaporating. In fact, we now use the same water as we did on the early Earth, thanks to the water cycle. Growing up, we all learned about the water cycle and its three simple steps. These stages were evaporation, condensation and precipitation. Come and discover that there is much more to the cycle than we originally learned. Deposition occurs when a vapor is directly transformed into a solid. Deposits are most often seen in the form of frost or snowflakes. Although this process is relevant to the water cycle, it is not as common as some other processes and is certainly not as distinct. The third stage of the water cycle is precipitation. Once the molecule becomes a liquid again, something must happen. This “something” is precipitation. According to an article from usgs.gov, in 2015, precipitation is water released from clouds in the form of rain, freezing rain, sleet, snow, or hail. It is the part of the water cycle that connects water in the atmosphere to the earth. The most common type of precipitation we experience is rain. Infiltration is another minor process in the water cycle. Infiltration is the process by which water seeps into the soil and moves through the area to rocks and pores. When water lands on shallow ground, it moves horizontally and vertically. If the ground is deeper, water could begin to recharge underground aquifers. If this were to happen, people could dig a hole in the ground and start using it as a water source. Many factors impact infiltration, such as rainfall intensity, soil characteristics, soil slope, etc. Soil can only absorb a limited amount of water at a time. Excess water is considered runoff water, which is surface water that drains from the

Essay / The total water supply is approximately 332.5 million cubic miles of water, which covers approximately 70% of the Earth's surface. With so much water inhabiting our planet, there obviously has to be a way to keep the water moving. We call this the water cycle, which has been around for longer than we know. The great thing about the water cycle is that it can never stop working because the water is always evaporating. In fact, we now use the same water as we did on the early Earth, thanks to the water cycle. Growing up, we all learned about the water cycle and its three simple steps. These stages were evaporation, condensation and precipitation. Come and discover that there is much more to the cycle than we originally learned. Deposition occurs when a vapor is directly transformed into a solid. Deposits are most often seen in the form of frost or snowflakes. Although this process is relevant to the water cycle, it is not as common as some other processes and is certainly not as distinct. The third stage of the water cycle is precipitation. Once the molecule becomes a liquid again, something must happen. This “something” is precipitation. According to an article from usgs.gov, in 2015, precipitation is water released from clouds in the form of rain, freezing rain, sleet, snow, or hail. It is the part of the water cycle that connects water in the atmosphere to the earth. The most common type of precipitation we experience is rain. Infiltration is another minor process in the water cycle. Infiltration is the process by which water seeps into the soil and moves through the area to rocks and pores. When water lands on shallow ground, it moves horizontally and vertically. If the ground is deeper, water could begin to recharge underground aquifers. If this were to happen, people could dig a hole in the ground and start using it as a water source. Many factors impact infiltration, such as rainfall intensity, soil characteristics, soil slope, etc. Soil can only absorb a limited amount of water at a time. Excess water is considered runoff water, which is surface water that drains from the

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