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- W2147402657 abstract "Pb dating of five cores from Crystal Bay, Lake Minnetonka, was used to examine the geologic history of the basin during the last century. A lakewide 210Pb budget and the basinwide average cumulative activities of 210Pb within time-stratigraphic units were estimated from multiple cores, Ages of time-stratigraphic markers and sediment accumulation rates of time-stratigraphic units were calculated from a constant-flux 210Pb-dating model. The basinwide bulk-sediment accumulation rate was found to have increased from 0.003 g cm-2 yr-I before settlement to 0.07 g cm-2 yr-i for the period from 1962 to 1983. Since settlement of the surrounding area, profundal sediment became highly calcareous and accumulation of littoral marl began. Intensity of focusing of sediment to the center of Crystal Bay decreased as basinwide sediment accumulation rates increased. Light organic sediment was also found to be more intensely focused than heavier siliceous or calcareous sediment. Accumulation of sediment spread to regions shal- lower than 5 m as the rate of sedimentation exceeded the rate of sediment resuspension at that depth, about 4 mm yr-I." @default.
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- W2147402657 date "1985-11-01" @default.
- W2147402657 modified "2023-10-06" @default.
- W2147402657 title "210 Pb dating and the recent geologic history of Crystal Bay, Lake Minnetonka, Minnesota1" @default.
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- W2147402657 doi "https://doi.org/10.4319/lo.1985.30.6.1154" @default.
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