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Valles Caldera - Redondo Geothermal Area
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"Unocal drilled 24 wells into a portion of
"Unocal drilled 24 wells into a portion of the Redondo Peak Resurgent Dome from 1959 to 1983 as a part of a geothermal exploration and development program within what was known as the Baca Project Area (now referred to as the Redondo Geothermal Area). In 1984, Nielson and Hulen described the intracaldera volcanic stratigraphy in the vicinity of Redondo Peak based on detailed logging of subsurface samples from these wells, which provided insights that improved interpretation of the internal structure of the resurgent dome. Maximum temperatures of 342°C were encountered in the deepest Unocal well, Baca-12, which was drilled to a depth of 3.2 km. The VC-1 core hole drilled at Redondo Creek and the VC-2A and VC-2B core holes drilled at [[Valles Caldera - Sulphur Springs Geothermal Area|Sulphur Springs]] as part of the CSDP from 1984 to 1988 have been the subject of numerous studies of the stratigraphy, structure, hydrothermal alteration, and subsurface architecture of the Valles Caldera.'"`UNIQ--ref-0000004F-QINU`"''"`UNIQ--ref-00000050-QINU`"''"`UNIQ--ref-00000051-QINU`"' '"`UNIQ--ref-00000052-QINU`"''"`UNIQ--ref-00000053-QINU`"' '"`UNIQ--ref-00000054-QINU`"''"`UNIQ--ref-00000055-QINU`"''"`UNIQ--ref-00000056-QINU`"''"`UNIQ--ref-00000057-QINU`"' '"`UNIQ--ref-00000058-QINU`"''"`UNIQ--ref-00000059-QINU`"' '"`UNIQ--ref-0000005A-QINU`"' '"`UNIQ--ref-0000005B-QINU`"' '"`UNIQ--ref-0000005C-QINU`"' An additional core hole, VC-3, was drilled in 2004 as part of the GLAD5 project to investigate major climatic changes and glacial/interglacial cycles recorded in lacustrine sediments below Valle Grande. While the findings of this shallow core hole are significant with respect to paleoclimate research, they pose little relevance to the exploration for geothermal resources." cannot be used as a page name in this wiki. The given value was not understood.
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Valles Caldera - Redondo Geothermal Area + Has processing error
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