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dc.contributor.advisorWhite, Sidney E.en_US
dc.creatorJost, Donalden_US
dc.date.accessioned2016-10-28T16:19:50Z
dc.date.available2016-10-28T16:19:50Z
dc.date.issued1970-03en_US
dc.identifier.urihttp://hdl.handle.net/1811/78814
dc.description.abstractA study of a recent rockfall in Conkles Hollow indicates that rockfall was not an important form of mass movement in the development of the Hollow. The local lithology, however, suggests that rockfall was an important form of mass movement in the development of the Hollow. The total mass of rock involved in the rockfall was determined by using two methods: (1) calculating the dimensions of the original sheet of rock, and (2) measuring the volume of the boulders comprising the talus.en_US
dc.language.isoen_USen_US
dc.publisherThe Ohio State Universityen_US
dc.relation.ispartofseriesThe Ohio State University. Department of Geology Senior Theses; 1970en_US
dc.titleRockfall in Conkles Hollow, Hocking County, Ohioen_US
dc.typeThesisen_US
dc.description.embargoNo embargoen_US


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