Type F: Oceanic-ridge, Basaltic Resource

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Type F: Oceanic-ridge, Basaltic Resource:
No definition has been provided for this term.


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

Want to add an example to this list? Select a Geothermal Resource Area to edit its "Brophy Model" property using the "Edit with Form" option.

CSV

Geothermal
Resource
Area
Geothermal
Region
Control
Structure
Host
Rock
Age
Host
Rock
Lithology
Mean
Capacity
Mean
Reservoir
Temp
Aluto-Langano Geothermal AreaEast African Rift System - Ethiopian Rift ValleyMajor Normal FaultBasalt7.5 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 AreaMid Atlantic RidgeBasalt3 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 AreaSouth Iceland Seismic Zone - Mid Atlantic RidgeBasalt303 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 AreaMid Atlantic RidgeBasalt2 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 AreaHawaii Geothermal RegionIntrusion Margins and Associated Fractures
Fissure Swarms
QuaternaryTholeiitic Basalt47 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 AreaMid Atlantic RidgeBasalt60 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 AreaSouth Iceland Seismic Zone - Mid Atlantic RidgeBasalt120 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 AreaEast African Rift System - Kenya Rift602 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 AreaMid Atlantic RidgeBasalt28.5 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 AreaMid Atlantic RidgeBasalt100 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 AreaMid Atlantic RidgeFault IntersectionBasalt76 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

  1. 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