Source: Ricardo André Frantz (User:Tetraktys)
La maggior parte delle rocce e dei suoli presenti a Naxos non sono eccellenti per catturare e immagazzinare acqua. Le rocce cristalline (scisti, gneiss, migmatite, granodiorite e marmi) che compongono la parte principale di Naxos hanno una bassa permeabilità primaria; la capacità di trasmettere acqua attraverso di esse dipende da una frattura e/o permeabilità secondaria indotta da soluzioni. Il parametro principale che controlla il regime di flusso delle acque sotterranee in acquiferi fratturati come le rocce cristalline è il modello di frattura.
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Address: Naxos, Naxos, Greece
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Source: Ricardo André Frantz (User:Tetraktys)
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Source: Ricardo André Frantz (User:Tetraktys)
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