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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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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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