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Water is held in the soil and seeps out over time.

Earth/soil holds water depending on its absorbancy ('sponginess'). Even though the ratio of the volume of water seeping out from a volume of soil is generally quite small, it is compounded by the catchment area of the stream - and hence there is a flow of water in the stream for some time after precipitation.

The amount of water in a stream is a factor of the the amount of water being released by the soil, depth of soil, whether there is a non-permiable layer undergound that feeds the catchment, the size of the catchment and amount of recent precipitation.

You could experiment to create streams of different water flow long after precipitation by filling in a valley between two mountains with various types of clay, soil, gravel, sand etc and notice the difference of stream flow in each case after precipitation. Of course, such an exercise would take many months/years to undertake and many millions, if not billions of dollars. There might also be government legislation and local environmental groups who might oppose such an activity.

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