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Geothermal Energy

Science – Society – Technology

Table 1 In situ measurements of the temperature [°C] in the wells of Krafla (K) at specific depths [m] for permeable horizons presented in Guðmundsson and Arnórsson (2002) (Table 3)

From: A multicomponent geothermometer for high-temperature basalt settings

K-11

K-24

K-28

1330 m

> 240 °C

580 m

190 °C

500 m

230 °C

1600 m

> 240 °C

780 m

195 °C

800 m

240 °C

1700 m

> 240 °C

920 m

210 °C

  

2180 m

> 300 °C

1150 m

225 °C

  
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