Karst of the Fireside quadrangle and portions of the Flat Rock and Clyde quadrangles, Ohio

dc.altmetrics.displaytrueen
dc.contributor.authorAden, D. J.
dc.contributor.authorMartin, D. R.
dc.date.accessioned2014-09-16T19:47:14Z
dc.date.available2014-09-16T19:47:14Z
dc.date.issued2014
dc.description.abstractKarst terrain forms by dissolution of carbonate rocks, such as limestone or dolomite, or evaporites, such as gypsum or salt, and is characterized by features including sinkholes, disappearing streams, caves, and springs. Sinkholes (or sinks) are enclosed depressions that do not usually hold water; they often have a “throat” or opening at the bottom where they drain to the subsurface. When a stream flows into a sinkhole, it is known as a disappearing stream or losing stream. Water flowing into the ground can cause solution enlargement of natural fractures in the rock and eventually can grow into caves. In Ohio, a cave is defined as “…a naturally occurring void, cavity, recess, or system of interconnecting passages beneath the surface of the earth or within a cliff or ledge…” The many passageways formed in karst terrain allow for high connectivity between the land surface and the water table. These passageways permit water to bypass soil and rock layers that filter out contaminants. Consequently, when compounds such as fertilizers, pesticides, and waste enter sinkholes, they are rapidly transported to the water table and quickly pollute water wells, streams, and rivers. When water exits these solutional features, a spring is formed. Such springs enable release of these contaminants at the surface. The different types of karst features may pose infrastructure complications; roads, utilities, houses, and other facilities built in karst areas are at risk of subsidence, collapse, or other damage. In order to provide a reference for future planning on both the local and regional scale, the Ohio Geological Survey has produced this map book identifying the known and suspected karst areas in the vicinity of Bellevue, Ohio, including portions of Erie, Huron, Sandusky, and Seneca Counties.en
dc.identifier.citationKarst of the Fireside quadrangle and portions of the Flat Rock and Clyde quadrangles, Ohio: Ohio Department of Natural Resources, Division of Geological Survey Open File Report 2014 1, 4 p., 42 maps.en
dc.identifier.urihttps://hdl.handle.net/2022/18935
dc.language.isoen_USen
dc.publisherOhio Department of Natural Resources, Division of Geological Surveyen
dc.relation.ispartofseriesOpen-File Report;2014-1
dc.relation.isversionofhttp://geosurvey.ohiodnr.gov/portals/geosurvey/PDFs/OpenFileReports/OFR_2013-1.pdfen
dc.subjectkarsten
dc.subjectFireside quadrangleen
dc.subjectFlat Rock quadrangleen
dc.subjectClyde quadrangleen
dc.subjectmap booken
dc.subjectOhioen
dc.subjectBellevueen
dc.subjectErie Countyen
dc.subjectHuron Countyen
dc.subjectSandusky Countyen
dc.subjectSeneca Countyen
dc.subjectsinkholeen
dc.subjectdisappearing streamen
dc.subjectcaveen
dc.subjectspringen
dc.subjectsinken
dc.titleKarst of the Fireside quadrangle and portions of the Flat Rock and Clyde quadrangles, Ohioen
dc.typeTechnical Reporten
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