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• W12912104 abstract "Abstract Boreholes were drilled in South Cascade Glacier to investigate the hydraulics of subglacial water flow. Results indicate that subglacial water pressures are generally close to local ice-overburden pressures and that a subglacial debris layer probably exists. Calculations indicate that the range of hydraulic conductivity of this layer is 10 −7 -10 −4 m −1 . The borehole water levels generally increased during the ablation season and may be caused by a seasonal evolution in the permeability of the debris layer. Water in the debris layer drains to a subglacial conduit, the existence of which is inferred by large diurnal variations in the water level of one borehole. These levels commonly reached the bottom of the glacier, indicating near-atmospheric pressures in the conduit." @default.
• W12912104 created "2016-06-24" @default.
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• W12912104 date "1994-01-01" @default.
• W12912104 modified "2023-10-03" @default.
• W12912104 title "Borehole water-level variations and implications for the subglacial hydraulics of South Cascade Glacier, Washington State, U.S.A." @default.
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• W12912104 doi "https://doi.org/10.1017/s0022143000007383" @default.
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