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dc.contributor.author Aden, D. J.
dc.date.accessioned 2013-10-07T18:43:35Z
dc.date.available 2013-10-07T18:43:35Z
dc.date.issued 2013
dc.identifier.citation Aden, D. J., 2013, Karst of the Bellevue quadrangle and portions of the Clyde and Castalia quadrangles, Ohio: Columbus, Ohio Department of Natural Resources, Division of Geological Survey Open-File Report 2013-1, 4 p., 59 maps. en_US
dc.identifier.uri http://hdl.handle.net/2022/16882
dc.description.abstract Karst 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…” (State of Ohio, 1989). 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. References State of Ohio, 1989, Ohio Revised Code 1517.21 Cave definitions, in chap. 1517 of Title 15 Conservation of Natural Resources: State of Ohio, Ohio Revised Code, accessible at <http://codes.ohio.gov/orc/1517.21>. en_US
dc.language.iso en_US en_US
dc.publisher ODNR Division of Geological Survey en_US
dc.relation.ispartofseries OFR;2013-1
dc.subject Ohio en_US
dc.subject ODNR - Division of Geological Survey en_US
dc.subject karst en_US
dc.subject Bellevue Quadrangle en_US
dc.subject Clyde Quadrangle en_US
dc.subject Castalia Quadrangle en_US
dc.title Karst of the Bellevue quadrangle and portions of the Clyde and Castalia quadrangles, Ohio en_US
dc.type Technical Report en_US


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