Cover. Map showing the 16 geologic-unit study area with geologic units shaded to indicate median radon concentrations in groundwater in Pennsylvania, 1986Pennsylvania, -2015. Green shading represents median radon concentration of less than 300 picocuries per liter (pCi/L); orange shading represents median radon concentration greater than or equal to 300 pCi/L and less than 4,000 pCi/L; red shading represents median radon concentration greater than or equal to 4,000 pCi/L. Geologic unit digital data from Miles and Whitfield, 2001. For more information on the USGS-the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment-visit http://www.usgs.gov or call 1-888-ASK-USGS.
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AbstractResults from 1,041 groundwater samples collected during 1986-2015 from 16 geologic units in Pennsylvania, associated with 25 or more groundwater samples with concentrations of radon-222, were evaluated in an effort to identify variations in radon-222 activities or concentrations and to classify potential radon-222 exposure from groundwater and indoor air. Radon-222 is hereafter referred to as "radon." Radon concentrations in groundwater greater than or equal to the proposed U.S. Environmental Protection Agency (EPA) maximum contaminant level (MCL) for public-water supply systems of 300 picocuries per liter (pCi/L) were present in about 87 percent of the water samples, whereas concentrations greater than or equal to the proposed alternative MCL (AMCL) for public watersupply systems of 4,000 pCi/L were present in 14 percent. The highest radon concentrations were measured in groundwater from the schists, gneisses, and quartzites of the Piedmont Physiographic Province.