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• W2328022823 abstract "Isotopic measurements of the 34 m3/s discharge from the Fall River Springs of northern California indicate recharge from 50 km upgradient in high elevation regions of Medicine Lake Volcano. Age determinations suggest less than 20-year travel time. Data demonstrate Klamath Basin further north cannot be a recharge source. Mass balance calculations support that annual precipitation on the volcano supplies observed spring discharge, requiring 50%–75% recharge rates. Radiocarbon and δ13C of dissolved inorganic carbon indicate 30%–40% is derived from magmatic CO2. Measured excess 3He is also consistent with the presence of magmatic gas derived from the Quaternary Age Medicine Lake Volcano." @default.
• W2328022823 created "2016-06-24" @default.
• W2328022823 creator A5043500739 @default.
• W2328022823 creator A5070378466 @default.
• W2328022823 date "2014-01-02" @default.
• W2328022823 modified "2023-09-26" @default.
• W2328022823 title "Recharge and Flow in the Medicine Lake Volcano–Fall River Springs Groundwater Basin, California" @default.
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• W2328022823 doi "https://doi.org/10.1080/15275922.2013.873097" @default.
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