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Radon-hazard potential of the southern St. George basin, Washington County, and Ogden, Weber County, Utah (SS-87)Vendor: Utah Geological SurveyBy: B. J. Solomon Radon derived from the radioactive decay of uranium migrates in soil gas and, after penetrating foundation openings, can accumulate indoors in sufficient quantities to pose a health hazard. Geologic factors that influence radon emanation and migration, including uranium concentration, ground-water...
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The radon-hazard-potential map of Utah (M-149)Vendor: Utah Geological SurveyBy: B. D. Black Radon is a naturally occurring radioactive gas formed by the decay of uranium which can be found in small concentrations in nearly all geologic materials. When radon is inhaled, its decay products are a significant cause of lung cancer. Radon...
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Radon Hazard Potential Map of Southern Davis County, Utah (OFR-655)Vendor: Utah Geological SurveyBy: Jessica J. Castleton, Ben A. Erickson, and Emily J. KleberAs requested by the Davis County Health Department, the Utah Geological Survey has mapped radon hazard potential for southern Davis County, Utah. This 1:24,000-scale map covers the southern portion of Davis County, including the...
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Radon-hazard potential of Beaver basin area, Beaver County, Utah (SS-94)Vendor: Utah Geological SurveyBy: C. E. Bishop Indoor-radon levels in the Beaver basin of southwestern Utah are the highest recorded to date in Utah. Measured indoor-radon concentrations range from 17.5 to 495pCi/L. These levels are well above those considered a health risk by the U.S. Environmental Protection...
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Radon-hazard potential of western Salt Lake Valley, Salt Lake County, Utah (SS-91)Vendor: Utah Geological SurveyBy: B. D. Black Radon is a radioactive gas of geologic origin that is an environmental concern because of its link to lung cancer. Radon is derived from the decay of uranium and can accumulate indoors in sufficient quantities to pose a health hazard...
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Radon-hazard potential of the lower Weber River area, Tooele Valley, and southeastern Cache Valley, Cache, Davis, Tooele, and Weber Counties, Utah (SS-90)Vendor: Utah Geological SurveyBy: B. D. Black and B. J. Solomon Radon is a radioactive gas of geologic origin that is an environmental concern because of its link to lung cancer. Radon is derived from the decay of uranium, and can accumulate indoors in sufficient quantities to...
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Radon-hazard potential of the central Sevier Valley, Sevier County, Utah (SS-89)Vendor: Utah Geological SurveyBy: B. J. Solomon Radon, a radioactive gas derived from the decay of uranium, occurs naturally in rock and soil. The gas migrates through the ground and, after penetrating foundation openings, can accumulate indoors in sufficient quantities to cause lung cancer. Both non-geologic and...
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Radon-hazard-potential areas in Sandy, Salt Lake County, and Provo, Utah County, Utah (SS-85)Vendor: Utah Geological SurveyBy: B. J. Solomon, B. D. Black, D. L. Nielson, D. L. Finerfrock, and J. D. Hultquist Average indoor-radon levels in two areas of the Wasatch Front region of north-central Utah are considerably higher than the national average of 1.7 picocuries per liter. The...
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Radon-hazard potential in the central Sevier Valley, Sevier County, Utah (PI-47)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of central Sevier Valley is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is common in the south end of the valley and along the valley margins. This soil is derived...
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Radon-hazard potential in southeastern Cache Valley, Cache County, Utah (PI-46)Vendor: Utah Geological SurveyBy: B. J. Solomon and B. D. Black The radon-hazard potential of southeastern Cache Valley is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is generally found along the mountain front. This soil is derived from local conglomerate...
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Radon-hazard potential in the lower Weber River area, Weber and Davis Counties, Utah (PI-45)Vendor: Utah Geological SurveyBy: B. D. BlackThe radon-hazard potential of lower Weber River area is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is found in the Weber delta and along the mountain front. This soil is deltaic sediment deposited by...
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Radon-hazard potential in Tooele Valley, Tooele County, Utah (PI-44)Vendor: Utah Geological SurveyBy: B. D. Black The radon-hazard potential of Tooele Valley is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is found locally along the valley margin. This soil is sediment deposited by Lake Bonneville, or alluvium locally derived...
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Radon-hazard potential in western Salt Lake Valley, Salt Lake County, Utah (PI-43)Vendor: Utah Geological SurveyBy: B. D. Black Color pamphlet that answers questions about the Great Salt Lake and Lake Bonneville such as when did Lake Bonneville exist and what kinds of animals lived around it, why is the Great Salt Lake salty, what islands are in the...
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Radon-hazard potential in the Ogden Valley, Weber County, Utah (PI-36)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of Ogden Valley is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is common west of Liberty. This soil is derived from metamorphic rock on the northwest valley margin. Answers are...
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Radon-hazard potential in the St. George area, Washington County, Utah (PI-35)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of the St. George area is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is common south of St. George. This soil is derived from local shale outcrops and from granitic...
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Radon-hazard potential in the Provo-Orem area, Utah County, Utah (PI-21)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of the Provo-Orem area is mapped based on geologic factors. Soil with potential for higher indoor-radon levels is common on the east bench and on alluvial fans along the Wasatch Range front. This soil is derived from...
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Radon-hazard potential in the Sandy-Draper area, Salt Lake County, Utah (PI-18)Vendor: Utah Geological SurveyBy: B. J. Solomon The radon-hazard potential of the Sandy-Draper area is mapped based on geologic factors. Soil with the greatest potential for high indoor-radon levels is common on the east bench at the mouth of Little Cottonwood Canyon. This soil is derived from...
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Engineering geologic map folio, Springdale, Washington County, Utah (OFR-340)Vendor: Utah Geological SurveyBy: B. J. Solomon This publication is an engineering folio for the Springdale area. Three of the six plates deal with different hazards, which are: landslide hazards; flood hazards and problem soils; and earthquake hazards, shallow ground-water, rock-fall hazards, and indoor-radon hazards. One of...
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Places with hazards; a teacher's handbook on natural hazards in Utah: The radon hazard in Utah (OFR-211D)Vendor: Utah Geological SurveyBy: S. N. Eldredge The Places with Hazards curriculum was developed for secondary-level earth science teachers as a means of preparing students to live more safely in a world that can pose problems from natural hazards. Students should be able to make wise choices...
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