The relation of geology to dry‐weather stream flow in Ohio

Eos, Transactions, American Geophysical Union
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Abstract

The regime of dry‐weather flow of several streams in Ohio is presented by flow‐duration curves. For comparison, the index of ground‐water flow for each basin is the discharge in cubic feet per second per square mile which is exceeded 90 per cent of the time. These indices are shown on a map of Ohio, and are discussed with respect to known geological conditions. It is concluded that stream‐flow records provide useful inferences to ground‐water geology, but the converse is not true.

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Publication type Article
Publication Subtype Journal Article
Title The relation of geology to dry‐weather stream flow in Ohio
Series title Eos, Transactions, American Geophysical Union
DOI 10.1029/TR030i004p00563
Volume 30
Issue 4
Year Published 1949
Language English
Publisher American Geophysical Union
Description 4 p.
First page 563
Last page 566
Country United States
State Ohio
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