Fig. 4From: Contention between supply of hydrothermal fluid and conduit obstruction: inferences from numerical simulationsTemporal change in a temperature at the crater (red line) and the observation point (black line) and b pressure at the observation point after doubling the flux of hydrothermal fluid (Run 10, Mʹ = 2000 kg s−1, kʹPCB = 1.0 × 10−10 m2)Back to article page