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New York Water Science Center publications

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Filter Total Items: 674

Surficial geology of Mexico quadrangle, Oswego County, New York

No abstract available.
Authors
Ernest Hathaway Muller, David Andrews, Todd S. Miller

Infiltration from tributary streams in the Susquehanna River basin, New York

As tributary streams in the Susquehanna River basin leave narrow upland valleys and enter larger valleys floored with permeable stratified glacial drift, they lose water by infiltration through streambeds. The infiltration rate is generally slow near the point of entering a larger valley, but farther downstream it is much faster and is approximately constant per unit distance along a given stream.
Authors
Allan D. Randall