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- W2024321812 abstract "ABSTRACT Dams decrease stream gradient and flow velocity, and often trap a stream's sediment load. For 188 years, sedimentation in the Munroe Falls dam pool on the Cuyahoga River, Ohio created a sediment record of both natural and anthropogenic variability. A wooden dam, first constructed in 1817, was replaced with a 3.66-m-high stone dam in 1902 to better serve local industrial needs. Before this dam was removed in 2005, a coring and transect profiling study was undertaken to characterize the dam pool sediments. To a distance of 600 m upstream of the Munroe Falls Dam, only ~30 cm of sediment overlaid the bedrock in the thalweg, indicating that the deep-water channel was an area of sediment transport. However, in the low-velocity shallow-water margins of the dam pool, up to 3 m of organic-rich, clayey silt had accumulated above pre-dam floodplain deposits. Past flooding events are recorded in these dam pool sediment deposits by an increase in woody debris and sand. A distinctive lithology having an oily s..." @default.
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- W2024321812 date "2007-09-01" @default.
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- W2024321812 title "The Legacy Sediment Record within the Munroe Falls Dam Pool, Cuyahoga River, Summit County, Ohio" @default.
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- W2024321812 doi "https://doi.org/10.3394/0380-1330(2007)33[127:tlsrwt]2.0.co;2" @default.
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