![Fig.5-19 A conceptual representation of a three-dimensional groundwater flow in a research area](img/honbun/large/e2009_5-19.jpg)
Fig.5-19 A conceptual representation of a three-dimensional groundwater flow in a research area
Groundwater is recharged at Mt. Daifuku which consists of a highly permeable sandstone. The groundwater flows through a shallow stratum and flows out at a relatively early stage into the Umegase and the Imohara rivers.
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