| Reference Type | Journal (article/letter/editorial) |
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| Title | Groundwater flow systems in the crystalline rocks of the Okanagan Highland, British Columbia |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Lawson, D. W. | Author |
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| Year | 1968 (August 1) | Volume | 5 |
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| Issue | 4 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e68-079Search in ResearchGate |
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| Generate Citation Formats |
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| Mindat Ref. ID | 472023 | Long-form Identifier | mindat:1:5:472023:6 |
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| GUID | 0 |
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| Full Reference | Lawson, D. W. (1968) Groundwater flow systems in the crystalline rocks of the Okanagan Highland, British Columbia. Canadian Journal of Earth Sciences, 5 (4) 813-824 doi:10.1139/e68-079 |
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| Plain Text | Lawson, D. W. (1968) Groundwater flow systems in the crystalline rocks of the Okanagan Highland, British Columbia. Canadian Journal of Earth Sciences, 5 (4) 813-824 doi:10.1139/e68-079 |
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| In | (1968, August) Canadian Journal of Earth Sciences Vol. 5 (4) Canadian Science Publishing |
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| Abstract/Notes | An investigation of the groundwater flow systems associated with the most prominent topographic expression in the Okanagan Highland (a U-shaped valley) revealed that the hydraulic conductivity of the crystalline rock varies exponentially with depth, and that the local flow systems within the upper 125 to 150βft of the crystalline rock conduct an estimated 10 to 17 Imperial gallons per day per foot thickness in a two-dimensional flow system. These local flow systems are quantitatively the most significant in the Okanagan Highland. |
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