Type F: Oceanic-ridge, Basaltic Resource
Brophy Occurrence Models
Basaltic resources typically occur at oceanic-ridges, continental rifts, and hot spots. These geothermal systems are heated by magmatic activity and the exploited fluids are typically very high temperatures.
Examples of such resources include those in Hawaii, Iceland, and along the East African Rift.
According to Brophy, ocean-ridge, basaltic resources typically have the following properties:
- Topography – Rugged to flat
- Climate – Island – high precipitation
- Depth to resource –Shallow (1000-2000m)
- Surface manifestations - Common
- Permeability – High horizontal permeability, variable vertical permeability
Examples
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Geothermal Resource Area | Geothermal Region | Control Structure | Host Rock Age | Host Rock Lithology | Mean Capacity | Mean Reservoir Temp |
---|---|---|---|---|---|---|
Aluto-Langano Geothermal Area | East African Rift System - Ethiopian Rift Valley | Major Normal Fault | Basalt | 7.5 MW7,500 kW <br />7,500,000 W <br />7,500,000,000 mW <br />0.0075 GW <br />7.5e-6 TW <br /> | 561.15 K288 °C <br />550.4 °F <br />1,010.07 °R <br /> | |
Bjarnaflag Geothermal Area | Mid Atlantic Ridge | Basalt | 3 MW3,000 kW <br />3,000,000 W <br />3,000,000,000 mW <br />0.003 GW <br />3.0e-6 TW <br /> | 573.15 K300 °C <br />572 °F <br />1,031.67 °R <br /> | ||
Hellisheidi Geothermal Area | South Iceland Seismic Zone - Mid Atlantic Ridge | Basalt | 303 MW303,000 kW <br />303,000,000 W <br />303,000,000,000 mW <br />0.303 GW <br />3.03e-4 TW <br /> | 533.15 K260 °C <br />500 °F <br />959.67 °R <br /> | ||
Husavik (Hveravellir) Geothermal Area | Mid Atlantic Ridge | Basalt | 2 MW2,000 kW <br />2,000,000 W <br />2,000,000,000 mW <br />0.002 GW <br />2.0e-6 TW <br /> | 395.15 K122 °C <br />251.6 °F <br />711.27 °R <br /> | ||
Kilauea East Rift Geothermal Area | Hawaii Geothermal Region | Intrusion Margins and Associated Fractures Fissure Swarms | 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 /> |
Krafla Geothermal Area | Mid Atlantic Ridge | Basalt | 60 MW60,000 kW <br />60,000,000 W <br />60,000,000,000 mW <br />0.06 GW <br />6.0e-5 TW <br /> | 538.15 K265 °C <br />509 °F <br />968.67 °R <br /> | ||
Nesjavellir Geothermal Area | South Iceland Seismic Zone - Mid Atlantic Ridge | Basalt | 120 MW120,000 kW <br />120,000,000 W <br />120,000,000,000 mW <br />0.12 GW <br />1.2e-4 TW <br /> | 568.15 K295 °C <br />563 °F <br />1,022.67 °R <br /> | ||
Olkaria Geothermal Area | East African Rift System - Kenya Rift | 602 MW602,000 kW <br />602,000,000 W <br />602,000,000,000 mW <br />0.602 GW <br />6.02e-4 TW <br /> | 548.15 K275 °C <br />527 °F <br />986.67 °R <br /> | |||
Pico Vermelho-Ribeira Grande Geothermal Area | Mid Atlantic Ridge | Basalt | 28.5 MW28,500 kW <br />28,500,000 W <br />28,500,000,000 mW <br />0.0285 GW <br />2.85e-5 TW <br /> | 511.15 K238 °C <br />460.4 °F <br />920.07 °R <br /> | ||
Reykjanes Geothermal Area | Mid Atlantic Ridge | Basalt | 100 MW100,000 kW <br />100,000,000 W <br />100,000,000,000 mW <br />0.1 GW <br />1.0e-4 TW <br /> | 583.15 K310 °C <br />590 °F <br />1,049.67 °R <br /> | ||
Svartsengi Geothermal Area | Mid Atlantic Ridge | Fault Intersection | Basalt | 76 MW76,000 kW <br />76,000,000 W <br />76,000,000,000 mW <br />0.076 GW <br />7.6e-5 TW <br /> | 513.15 K240 °C <br />464 °F <br />923.67 °R <br /> |
References
- ↑ Colin F. Williams, Marshall J. Reed and Arlene F. Anderson. 2011. Updating the Classification of Geothermal Resources - Presentation. In: Thirty-Sixth Workshop on Geothermal Reservoir Engineering; 2011/02/02; Stanford, California. Stanford, California: Stanford University; p. 23