Variations in sediment sources and yields in the Finger Lakes and Catskills regions of New York.

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dc.contributor.author	Nagle, G.N.
dc.contributor.author	Fahey, T.J.
dc.contributor.author	Ritchie, J.C.
dc.contributor.author	Woodbury, P.B.
dc.date.accessioned	2013-07-01T19:52:53Z
dc.date.available	2013-07-01T19:52:53Z
dc.date.issued	2007
dc.identifier.citation	Nagle, G.N., Fahey, T.J., Ritchie, J.C., Woodbury, P.B., 2007. Variations in sediment sources and yields in the Finger Lakes and Catskills regions of New York. Hydrological Processes 21(6): 828-838.	en_US
dc.description.abstract	This study used radionuclide tracer analysis to quantify proportional contributions of land surface and stream bank erosion to fine sediment loads in streams. Results for two streams within the Schoharie Creek basin yielded relatively high rates of bank erosion, indicating the importance of glaciolacustrine deposits as importance sources of stream sediment.	en_US
dc.language.iso	en_US	en_US
dc.publisher	Hydrological Processes	en_US
dc.relation.ispartofseries	Turbidity;B4
dc.subject	bank erosion	en_US
dc.subject	sediment sources	en_US
dc.subject	tracers	en_US
dc.subject	New York State	en_US
dc.title	Variations in sediment sources and yields in the Finger Lakes and Catskills regions of New York.	en_US
dc.type	Article	en_US