Fissure Swarms
Controlling Structures

Fissure swarms typically result from tensional forces in volcanic regions and are predominantly host to geothermal systems in Iceland.
Examples
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Geothermal Resource Area | Geothermal Region | Tectonic Setting | Host Rock Age | Host Rock Lithology | Mean Capacity | Mean Reservoir Temp |
---|---|---|---|---|---|---|
Kilauea East Rift Geothermal Area | Hawaii Geothermal Region | Hot Spot | Quaternary | Tholeiitic Basalt | 47 MW47,000 kW <br />47,000,000 W <br />47,000,000,000 mW <br />0.047 GW <br />4.7e-5 TW <br /> | 575.15 K302 °C <br />575.6 °F <br />1,035.27 °R <br /> |