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TitleReport on 1978 field work - Meager Creek geothermal area, upper Lillooet River, British Columbia
DownloadDownloads
AuthorFairbank, B; Shore, G A; Werner, L J; Nevin, A E; Sadlier-Brown, T L
SourceEarth Physics Branch, Open File 79-10, 1979, 145 pages (4 sheets), https://doi.org/10.4095/8357
Year1979
PublisherEnergy, Mines and Resources Canada (Ottawa, Canada)
Documentopen file
Lang.English
MapsPublication contains 4 maps
Map Info.geological, bedrock geology, 1:20,000
Map Info.geological, bedrock geology, 1:40,000
Map Info.geophysical, resistivity, 1:20,000
Map Info.geophysical, resistivity, 1:40,000
Mediapaper; on-line; digital
File formatpdf
ProvinceBritish Columbia
NTS92I; 92J
AreaLillooet Valley; Meager Creek; Meager Mountain
Lat/Long WENS-124.0000 -120.0000 51.0000 50.0000
Subjectsgeophysics; geothermal energy; geothermal gradient; geothermal potential; geothermal research; geothermal resources
Illustrationssketch maps; tables; stratigraphic charts; graphs; profiles; lithologic sections; cross-sections; schematic representations; sample forms; schematic diagrams; histograms
Released1979 01 01; 2018 11 13
Abstractencouraging new subsurface information. Two wells were drilled and both recorded temperatures in excess of l00°c. One of these confirmed a new target area. Geophysical surveys refined earlier concepts of the boundaries of the three areas of interest and allowed a division into:
a. the South Reservoir
b. the North Reservoir
c. the Lillooet Valley resistivity anomaly. ·
The South Reservoir is the best-defined. It has been under specific study since 1974. Seven diamond drill holes have been put down within or near its boundaries. Exploratory work on the North Reservoir and the Lillooet Valley resistivity anomaly is not as advanced as that on the South Reservoir.
GEOSCAN ID8357