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dc.creatorAli, Syed A.en_US
dc.creatorWeiss, Malcolm P.en_US
dc.date.accessioned2005-10-01T03:04:17Z
dc.date.available2005-10-01T03:04:17Z
dc.date.issued1971-05en_US
dc.identifier.citationThe Ohio Journal of Science. v71 n3 (May, 1971), 129-149en_US
dc.identifier.issn0030-0950en_US
dc.identifier.urihttp://hdl.handle.net/1811/5612
dc.descriptionAuthor Institution: Rennsselaer Polytechnic Institute, Troy, N. Y. ; Northern Illinois University, DeKalb, Illinoisen_US
dc.description.abstractThe directional data of cross-laminae and ripple marks in the Kope and Fairview Formations in Brown and Adams Counties, Ohio, show no statistically significant difference in mean orientation. The prevailing paleocurrent direction was towards the northnorthwest. A significant difference, however, exists between the wave lengths of the ripples in the Kope and Fairview. Ripple marks are larger in the Kope Formation and gradually decrease in size upward into the overlying Fairview Formation. This may well have resulted from gradual local shallowing of the Cincinnatian sea as carbonate detritus accumulated. The ripple marks are interpreted to have been formed by currents and modified by waves.en_US
dc.format.extent3953852 bytes
dc.format.mimetypeapplication/pdf
dc.language.isoen_US
dc.rightsReproduction of articles for non-commercial educational or research use granted without request if credit to The Ohio State University and The Ohio Academy of Science is given.en_US
dc.titleKope and Fairview Ripple Marks : Brown and Adams Counties, Ohioen_US


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