Fig. 9
From: Numerical modeling of the geothermal hydrology of the Volcanic Island of Basse-Terre, Guadeloupe
Temperature-depth curves for a simple model setup following Hayba and Ingebritsen (1997) with a 300 m thick, horizontal caprock having the same width as the intrusion. The curves represent the onset of the hottest phase in the system’s evolution and occur at different times (\(1 \cdot 10^{-15} \, \text {m}^2\)–10,000 years; \(5 \cdot 10^{-15} \, \text {m}^2\)–7000 years; \(8 \cdot 10^{-15} \, \text {m}^2\)–4800 years; \(1 \cdot 10^{-14} \, \text {m}^2\)–2500 years)