Groundwater flow refers to the movement of water that is found beneath the Earth's surface. This water is stored in soil and rocks and slowly moves through spaces and cracks underground. Groundwater flow is an important part of the water cycle because it helps supply water to rivers, lakes, and springs. It occurs when rainwater soaks into the ground and travels through the layers of soil and rock, eventually reaching aquifers, which are underground layers of water-bearing rock. Understanding groundwater flow is crucial in geography as it affects how humans use water resources and how landscapes are formed.
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