Aquifer Information Table Aquifer 808 ATTRIBUTE VALUE/DESCRIPTION 10REFERENCE(S) 1Aquifer Identification BC MOE Number: 808 WRA, BC MOE, 2007 South Okanagan, East of Osoyoos Lake, Descriptive Location (Name): ACW, BC MOE, 2007 Anarchist Mountain. 2BC MOE Classification: IIB WRA, BC MOE, 2007 Aquifer Type: Bedrock ACW, BC MOE, 2007 Aquifer Dimensions 1 2 Approximate Size (km ): 10 km2 ACW, BC MOE, 2007 3 Estimated Avg. Thickness (m): Unconfirmed 3 Est. Avg. Bottom Depth (m): Unconfirmed Stratigraphy and Geology Fractured bedrock (granite or 3Aquifer Materials: ACW, BC MOE, 2007 metamorphic schist). Sand, gravel, silt, till, and boulder 3Overlying Materials: ACW, BC MOE, 2007 mixtures (thickness unconfirmed) 3Underlying Materials: Bedrock Inferred for this report 4Aquifer Bedrock Type: 6b ACW, BC MOE, 2007 5Water Well Statistics Number of Wells in Aquifer: Approximately 32 ACW, BC MOE, 2007 Average Well Depth (m): 105 m (range: 47 m to 184 m) ACW, BC MOE, 2007 Average Yield (L/s): 0.4 L/s (max = 9 L/s) ACW, BC MOE, 2007 Average Depth to Water (m): Approximately 18 m ACW, BC MOE, 2007 Aquifer Hydraulic Properties and Information 6Hydraulic Conductivity (m/s): Unconfirmed 6Transmissivity (m2/s): Unconfirmed 6Storativity or Specific Yield: Unconfirmed 7Hydraulic Communication with Possibly aquifer 194 to west. Inferred for this report Other Aquifers: Inferred for this report. 8Recharge Processes: Inferred types: A, B, C, D, E, and/or F 9Other Aquifer Information Models: None identified Geochemical Data: None identified Flow Direction/Gradient: Unconfirmed Associated Watersheds: None, Residual Area E‐17 Map 7, Appendix I of this report. ACW = Draft Aquifer Classification Worksheets, WRA = Water Resources Atlas, WL = well logs (from Wells Database) The above Aquifer Information Table is part of the report: Groundwater and Hydrogeological Conditions in the Okanagan Basin, British Columbia, A State‐of‐the‐Basin Report, by L. Neilson‐Welch and D.M. Allen, December, 2007. Aquifer Information Tables are subject to all limitations discussed in the report as well as limitations and footnotes listed at the end of this appendix. .
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