Tufa Rock

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dc.contributor.author Niebergall, Ernst en_US
dc.coverage.spatial Erie County (Ohio) en_US
dc.coverage.spatial Castalia (Ohio) en_US
dc.coverage.temporal 1901-1919 en_US
dc.date.accessioned 2008-04-28T19:01:42Z
dc.date.available 2008-04-28T19:01:42Z
dc.date.created 1909-1919 en_US
dc.date.issued 2008-04-28T19:01:42Z
dc.identifier.other 348.20.u158 en_US
dc.identifier.other 20 en_US
dc.identifier.uri http://hdl.handle.net/2374.OX/2018
dc.description Tufa rock is a porous rock formed when water with a heavy lime content evaporates. Abundant limestone deposits, lots of underground rivers, sink holes - like the Blue Hole - and marshes around Castalia made a fertile ground for the growth of tufa rock. Evaporating water left mineral deposits that encrusted twigs, small pebbles, etc. and grew into unique rock formations. en_US
dc.format.extent 5" x 7" en_US
dc.language.iso eng en_US
dc.relation.ispartof Charles E. Frohman Collection en_US
dc.rights Rutherford B. Hayes Presidential Center en_US
dc.rights.uri http://www.rbhayes.org/hayes/photographs/display.asp?id=497&subj=photographs en_US
dc.subject Erie County (Ohio) en_US
dc.subject Castalia (Ohio) en_US
dc.subject Cold Creek (Ohio) en_US
dc.subject Rivers - Ohio - Erie County en_US
dc.subject Springs - Ohio - Erie County en_US
dc.title Tufa Rock en_US
dc.type Photographic print; black and white en_US
dc.publisher.digital Rutherford B. Hayes Presidential Center en_US
dc.contributor.photographer Niebergall, Ernst en_US
dc.contributor.repository Rutherford B. Hayes Presidential Center en_US
dc.repository.place Fremont, Ohio en_US
dc.repository.place Fremont, Ohio en_US
dc.repository.place Sandusky County, Ohio en_US

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