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- W1849002423 abstract "the Yellowstone Caldera, the 0.11 km 2 Obsidian Pool Thermal Area (OPTA) and the 0.25 km 2 Solfatara Plateau Thermal Area (SPTA). Conductive heat flux through a low permeability layer capping large vapor reservoirs is calculated from soil temperature measurements at >600 locations and from laboratory measurements of soil properties. The conductive heat output is 3.6 � 0.4 MW and 7.5 � 0.4 MW from the OPTA and the SPTA, respectively. The advective heat output from soils is 1.3 � 0.3 MW and 1.2 � 0.3 MW from the OPTA and the SPTA, respectively and the heat output from thermal pools in the OPTA is 6.8 � 1.4 MW. These estimates result in a total heat output of 11.8 � 1.4 MW and 8.8 � 0.4 MW from OPTA and SPTA, respectively. Focused zones of high heat flux in both thermal areas are roughly aligned with regional faults suggesting that faults in both areas serve as conduits for the rising acid vapor. �� ;" @default.
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- W1849002423 date "2012-10-01" @default.
- W1849002423 modified "2023-10-09" @default.
- W1849002423 title "Heat flow in vapor dominated areas of the Yellowstone Plateau Volcanic Field: Implications for the thermal budget of the Yellowstone Caldera" @default.
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- W1849002423 doi "https://doi.org/10.1029/2012jb009463" @default.
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