Rift Zone
Tectonic Settings

Rift valleys occur at divergent plate boundaries, resulting in large graben structures and increased volcanism. The East African Rift is an example of a continental rift zone with increased volcanism, while the Atlantic’s spreading Mid-Ocean Ridge is host to an enormous amount of geothermal activity in Iceland.
Some rift zones, like that of the Gulf of California, exhibit transtensional strains exemplified by strike-slip regions like that of the San Andreas fault. Rift zones may also give way to leaky transform faults that may contribute to increased volcanism as is thought to be the case with Las Tres Virgenes in Baja California, Mexico and the Azores Islands which are located on a triple junction.
Examples
Want to add an example to this list? Select a Geothermal Resource Area to edit its "Tectonic Setting" property using the "Edit with Form" option.
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 /> | ||
Bruchsal Geothermal Area | Upper Rhine Valley | Major Normal Fault | Triassic | Sandstone | 0.6 MW600 kW <br />600,000 W <br />600,000,000 mW <br />6.0e-4 GW <br />6.0e-7 TW <br /> | 413.15 K140 °C <br />284 °F <br />743.67 °R <br /> |
Cerro Prieto Geothermal Area | Gulf of California Rift Zone Geothermal Region | Sandstone | 720 MW720,000 kW <br />720,000,000 W <br />720,000,000,000 mW <br />0.72 GW <br />7.2e-4 TW <br /> | 588.15 K315 °C <br />599 °F <br />1,058.67 °R <br /> | ||
East Mesa Geothermal Area | Gulf of California Rift Zone | sandstone | 115 MW115,000 kW <br />115,000,000 W <br />115,000,000,000 mW <br />0.115 GW <br />1.15e-4 TW <br /> | 443.15 K170 °C <br />338 °F <br />797.67 °R <br /> | ||
Eburru Geothermal Area | East African Rift System - Kenya Rift | Basalt | 2.5 MW2,500 kW <br />2,500,000 W <br />2,500,000,000 mW <br />0.0025 GW <br />2.5e-6 TW <br /> | 578.15 K305 °C <br />581 °F <br />1,040.67 °R <br /> | ||
Fenton Hill HDR Geothermal Area | Rio Grande Rift | Lithologically Controlled | Precambrian | Crystalline basement “pCu” (undifferentiated in map units); Biotite Granodiorite (Phase I Reservoir); Gneiss, Schist, Granodiorite, Granite, Metavolcanic Rocks (Phase II Reservoir) | 20 MW20,000 kW <br />20,000,000 W <br />20,000,000,000 mW <br />0.02 GW <br />2.0e-5 TW <br /> | 508.15 K235 °C <br />455 °F <br />914.67 °R <br /> |
Heber Geothermal Area | Gulf of California Rift Zone | Pull-Apart in Strike-Slip Fault Zone | sandstone | 180 MW180,000 kW <br />180,000,000 W <br />180,000,000,000 mW <br />0.18 GW <br />1.8e-4 TW <br /> | 447.15 K174 °C <br />345.2 °F <br />804.87 °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 /> | ||
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 /> | ||
Landau Geothermal Area | Upper Rhine Valley | Major Normal Fault | 3.6 MW3,600 kW <br />3,600,000 W <br />3,600,000,000 mW <br />0.0036 GW <br />3.6e-6 TW <br /> | 413.15 K140 °C <br />284 °F <br />743.67 °R <br /> | ||
Las Tres Virgenes Geothermal Area | Baja Peninsula Geothermal Region | Granodiorite | 10 MW10,000 kW <br />10,000,000 W <br />10,000,000,000 mW <br />0.01 GW <br />1.0e-5 TW <br /> | 553.15 K280 °C <br />536 °F <br />995.67 °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 /> | ||
Salton Sea Geothermal Area | Gulf of California Rift Zone | Pull-Apart in Strike-Slip Fault Zone | Pleistocene | sandstone | 437 MW437,000 kW <br />437,000,000 W <br />437,000,000,000 mW <br />0.437 GW <br />4.37e-4 TW <br /> | 575.15 K302 °C <br />575.6 °F <br />1,035.27 °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 /> | |
Valles Caldera - Redondo Geothermal Area | Rio Grande Rift | Fault Intersection Stratigraphic Boundaries Caldera Rim Margins | Mississippian-Pennsylvanian; Pleistocene, 1.6 to 1.25 Ma | Limestone-Madera Formation “MIPu”; Rhyolitic tuff-Intracaldera Bandelier Tuff (upper Tshirege “Qbt” and lower Otowi “Qbo” members); Caldera Fill Rhyolite (shallow) | ||
Valles Caldera - Sulphur Springs Geothermal Area | Rio Grande Rift | Fault Intersection Stratigraphic Boundaries Caldera Rim Margins | Precambrian; Mississippian-Pennsylvanian; Pleistocene, 1.6 to 1.25 Ma; Pliocene; Miocene | Crystalline basement “pCu”; Limestone-Madera Formation “MIPu”; Rhyolitic tuff-Bandelier Tuff (upper Tshirege “Qbt” and lower Otowi “Qbo” members); Caldera Fill Rhyolite (shallow); Dacitic/Andesitic to Rhyolitic lavas and tuffs-Keres Group Volcanics (shallow); Santa Fe Group volcaniclastics “Tsf” |