{"title":"Water","description":"","products":[{"product_id":"b-115","title":"Geology and mineral resources of Box Elder County, Utah (B-115)","description":"\u003cp\u003e\u003ci\u003eBy: H. H. Doelling\u003c\/i\u003e\u003c\/p\u003e\u003cp\u003e Box Elder County is situated in the northwest corner of Utah bordering with Idaho on the north, Nevada on the west, Tooele and Weber counties on the south and Cache County on the east. It comprises a land area of 5.594 square miles and a large part of the Great Salt Lake (approximately an additional 800 square miles). It is the fourth largest county in Utah. \u003c\/p\u003e\u003cp\u003e Box Elder County displays a variety of lithologic types in each of the major rock divisions: sedimentary, igneous, and metamorphic, in a typical Basin and Range setting. True to the basic structure most of its mountain ranges generally trend north-south, but the Raft River Range trends east-west. Each mountain range exhibits a variety of structural situations: most stratigraphic units are folded and faulted, and many are intruded by igneous rocks. \u003c\/p\u003e\u003cp\u003e Construction materials, principally stone and sand and gravel have provided almost 75 percent of the cumulative mineral value produced in Box Elder County through 1974. Their production remains important to the county's mineral output. Salts harvested from Great Salt Lake have provided 17.9 percent of the cumulative mineral value and their value percentage should continue to increase in the future. Metals production, which provided the principal values in many of the earlier years, amounts to only 6.9 percent of the cumulative mineral value. Although prospecting is active and some development work occasionally done, only tungsten has been produced since 1963.\u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1980\u003cbr\u003ePages: 251 p.\u003cbr\u003ePlates: 3 pl.\u003cbr\u003eScale: 1:125,000\u003cbr\u003eLocation: Box Elder County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203792875573,"sku":"B115","price":16.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/b115.png?v=1594681409"},{"product_id":"b-132","title":"Energy, mineral, and ground-water resources of Carbon and Emery Counties, Utah (B-132)","description":"\u003cp\u003e\u003ci\u003eBy: R. W. Gloyn, D. E. Tabet, B. T. Tripp, C. E. Bishop, C. D. Morgan, J. W. Gwynn, and R. E. Blackett\u003c\/i\u003e\u003c\/p\u003e\u003cp\u003eThe Utah Geological Survey has collected and evaluated information on the known and potential energy, mineral, and ground-water resources in Carbon and Emery Counties. This report provides information for use in both short- and long term land-planning decisions, particularly at the county level, and an indication of the present and future economic impact of mineral and energy development. The report discusses eight major commodity groups: (1) oil and gas, (2) coal and coal resin, (3) coal-bed methane, (4) other energy resources (oil-impregnated rock, oil shale, geothermal), (5) uranium and vanadium, (6) metallic minerals, (7) industrial rocks and minerals, and (8) ground-water resources. In general, for each group or commodity within a group the following aspects are discussed: (1) known occurrences and characteristics, (2) past production and trends, (3) current production and exploration activity, and (4) geologic potential. Plates accompany each of the major commodity groups and show the locations of known resources and areas of geologic potential. In addition to the commodity discussions, the report contains a brief summary of land ownership status and concludes with a summary of commodities having the best potential for discovery and development.\u003c\/p\u003e\u003cp\u003eThe report concludes that there is good potential for the discovery and development of additional occurrences of mineral and energy resources in Carbon and Emery Counties. In addition, some resources are present which have tonnage, grade, or quality characteristics that could support commercial development under favorable market conditions or with new technology. However, potential for development of many commodities, particularly some industrial minerals, cannot be ascertained at this time based on limited data available. The most prospective areas for development of additional energy resources are in western Carbon and Emery Counties and in north-central and eastern Carbon County. The most prospective areas for development of additional mineral resources are in eastern and central Emery County.\u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2003\u003cbr\u003ePages: 161 p.\u003cbr\u003ePlates: 14 pl.\u003cbr\u003eScale: 1:750,000\u003cbr\u003eLocation: Carbon and Emery Counties\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203794743349,"sku":"B132","price":6.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/b132.png?v=1594681433"},{"product_id":"c-101","title":"Preliminary hydrogeologic framework characterization - ground-water resources along the western side of the northern Wasatch Range, eastern Box Elder County, Utah (C-101)","description":"\u003cp\u003e\n \u003ci\u003eBy: H. A. Hurlow\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n This report summarizes the bedrock geology of the western part of the northern Wasatch Range in eastern Box Elder County, Utah , and its relation to ground-water resources. The southern part of the northern Wasatch Range is herein informally designated the Willard mountains; the northern part of the northern Wasatch Range is the Wellsville Mountains. Box Elder Canyon is the boundary between these mountains. The work was performed at the request of the Bear River Water Conservancy District and the Utah Division of Water Resources, and represents a preliminary step in the evaluation of groundwater resources in bedrock and their potential development in eastern Box Elder County.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1999\u003cbr\u003e\n Pages: 50 p.\u003cbr\u003e\n Location: Box Elder County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203801428021,"sku":"C101","price":8.75,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/c101.png?v=1594681743"},{"product_id":"c-102","title":"Guidelines for preparing hydrogeologic and soil reports addressing suitability for alternative wastewater disposal systems in Weber County, Utah (C-102)","description":"\u003cp\u003e\n \u003ci\u003eBy: M. Lowe and D. Sorensen\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n Many lots in Weber County presently cannot be developed because adverse site characteristics (such as soil that percolates outside of acceptable rate ranges or shallow ground water) make them unsuitable for conventional wastewater disposal systems (septic tank soil-absorption systems). The Weber-Morgan District Health Department and the Utah Division of Water Quality have developed designs for alternative wastewater disposal systems that may be used in such areas if hydrogeologic and soil conditions are suitable, ground- and surface-water quality will not be degraded, and humans will not be exposed to wastewater pathogens.\u003c\/p\u003e\n \u003cp\u003e\n The purpose of this circular, prepared at the request of the Weber-Morgan District Health Department, is to provide guidelines for: (1) geologists preparing hydrogeologic reports pertinent to the suitability of sites for alternative wastewater disposal systems, (2) soil scientists preparing soil evaluation reports pertinent to the suitability of sites for alternative wastewater disposal systems, and (3) geologists, soil scientists, and Weber-Morgan District Health Department officials reviewing these reports. These guidelines are applicable to other areas of Utah where alternative wastewater disposal systems are used or are being considered to be used.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1999\u003cbr\u003e\n Pages: 10 p.\u003cbr\u003e\n Location: Weber County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"Default Title","offer_id":32203801460789,"sku":"C102","price":3.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/c102.png?v=1594681745"},{"product_id":"c-99","title":"A summary of the ground-water resources and geothermal hydrology of Grand County, Utah (C-99)","description":"\u003cp\u003e\n \u003ci\u003eBy: C. Eisinger and M. Lowe\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n In Grand County, ground water has been withdrawn primarily from two types of aquifers: fractured rock and unconsolidated deposits. Some of the better water-yielding rock units are grouped together into nine aquifers, including: the Lower Paleozoic aquifer, the Cutler aquifer, the Wingate aquifer, the Navajo aquifer, the Entrada aquifer, the Morrison aquifer, the Dakota aquifer, the Wasatch aquifer, and the Parachute Creek aquifer.\u003c\/p\u003e\n \u003cp\u003e\n This report summarizes published information regarding ground-water conditions in Grand County. During the preparation of this report we identified several types of information that are not presently available, but can be useful for evaluating ground-water resources, including: (1) structure contour maps showing the depth to aquifers, (2) isopach maps showing the thickness of aquifers, and (3) fracture domain maps showing the predominant orientations of rock discontinuities.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1999\u003cbr\u003e\n Pages: 28 p.\u003cbr\u003e\n Location: Grand County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"Default Title","offer_id":32203803164725,"sku":"C99","price":6.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/c099.png?v=1594681821"},{"product_id":"carving-grand-canyon-evidence-theories-and-mystery","title":"Carving Grand Canyon: Evidence, Theories, and Mystery","description":"\u003cp data-sourcepos=\"1:1-1:745\"\u003e\u003cspan class=\"citation-0 recitation citation-end-0\"\u003eDive deep into the geological enigma that is the Grand Canyon with the second edition of \"\u003cstrong\u003eCarving Grand Canyon: Evidence, Theories, and Mystery\u003c\/strong\u003e,\" published by the Grand Canyon Conservancy in 2012. This comprehensive book explores the myriad theories surrounding the canyon's formation, from the traditional \"river downcutting\" model to more recent hypotheses involving ancient lakes and catastrophic flood events.\u003csup data-turn-source-index=\"2\" class=\"superscript\"\u003e\u003c!----\u003e\u003c\/sup\u003e\u003c\/span\u003e Readers will gain a thorough understanding of the key geological features that shape the canyon's landscape, including the Kaibab Limestone, the Bright Angel Shale, and the Vishnu Schist, all while unraveling the complex interplay of erosion, uplift, and time that has sculpted this iconic natural wonder.\u003c\/p\u003e\n\u003cp\u003eThis meticulously researched volume presents a balanced and accessible overview of the scientific debates surrounding the Grand Canyon's origins. It delves into the evidence supporting various theories, examining the stratigraphic record, fault lines, and the distribution of sediments. You'll explore the significance of features like the Great Unconformity and the role of the Colorado River in the canyon's development. The book also acknowledges the remaining mysteries, inviting readers to ponder the unanswered questions that continue to intrigue geologists and enthusiasts alike.\u003c\/p\u003e\n\u003cp\u003e\"Carving Grand Canyon\" is organized into chapters that guide you through the canyon's complex history, including: Introduction to the Grand Canyon, The Rocks of the Canyon, Theories of Canyon Formation, The Role of the Colorado River, and Unresolved Mysteries. This second edition, a valuable resource for both casual readers and serious students of geology, offers a rich and engaging exploration of one of Earth's most breathtaking landscapes. While the author is not explicitly listed in the prompt, this book is a collaborative effort by experts associated with the Grand Canyon Conservancy.\u003c\/p\u003e","brand":"Grand Canyon Conservancy","offers":[{"title":"Default Title","offer_id":32203803754549,"sku":"BK-CARVING-GRAND-CANYON","price":19.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/61fUNwWZtzL.jpg?v=1594835941"},{"product_id":"cir-48","title":"Ground Water Conditions in Utah: Spring of 2007 (CIR-48)","description":"\u003cp\u003e\u003ci\u003eBy: C.B. Burden \u0026amp; Others\u003c\/i\u003e\u003c\/p\u003e\u003cp\u003e This is the forty-fourth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, published cooperatively by the U.S. Geological Survey and the Utah Department of Natural Resources, Division of Water Resources and Division of Water Rights, provide data to enable interested parties to maintain awareness of changing ground-water conditions. \u003c\/p\u003e\u003cp\u003e This report, like the others in the series, contains information on well construction, ground-water withdrawal from wells, water-level changes, precipitation, streamflow, and chemical quality of water. Information on well construction included in this report refers only to wells constructed for new appropriations of ground water. Supplementary data are included in reports of this series only for those years or areas which are important to a discussion of changing ground-water conditions and for which applicable data are available. This report includes individual discussions of selected significant areas of ground-water development in the State for calendar year 2006. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2007\u003cbr\u003ePages: 129 p.\u003cbr\u003eLocation: Utah Statewide\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203805098037,"sku":"CIR48","price":7.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/waterrights17.png?v=1594681919"},{"product_id":"m-110","title":"Shallow ground water and related hazards in Utah (M-110)","description":"\u003cp\u003e\n \u003ci\u003eBy: S. Hecker and K. M. Harty, compilers\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n Many population centers in the state are in areas susceptible to shallow ground-water problems. Rising water tables in recent years have caused flooding in basements, storage tanks, underground utilities, waste dumps, and septic-tank soil-absorption fields. Such rises in water tables have mobilized contaminants and threatened local ground-water quality. Areas with the potential for large earthquakes, such as the Wasatch Front, are vulnerable to damage caused by liquefaction of cohesionless silty and sandy deposits saturated at shallow depths. Site-specific data on the distribution of shallow ground water in Utah are lacking. This statewide compilation of available regional information provides a basis for deciding where detailed planning-related studies may be needed in order to identify and mitigate shallow ground-water hazards and avoid costly corrective measures.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1988\u003cbr\u003e\n Pages: 19 p.\u003cbr\u003e\n Plates: 1 pl.\u003cbr\u003e\n Scale: 1:750,000\u003cbr\u003e\n Location: Utah\u003cbr\u003e\n Media Type: Paper Map\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"Default Title","offer_id":32203837538357,"sku":"M110","price":7.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/m110.png?v=1594683067"},{"product_id":"m-174","title":"Map of recharge and discharge areas for the principal valley-fill aquifer, Sanpete Valley, Sanpete County, Utah (M-174)","description":"\u003cp\u003e\u003ci\u003eBy: N. P. Snyder and M. Lowe\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThe most important source of drinking water in Sanpete County is ground water from the principal valley-fill aquifer in Sanpete Valley. In this study we mapped recharge and discharge areas for the principal aquifer to aid in management of potential contaminant sources to help protect the quality of ground water.\u003c\/p\u003e \u003cp\u003eThe purpose of this study is to help state and local government officials and local residents protect the quality of ground water in Sanpete Valley by defining areas where ground-water aquifers are vulnerable to contamination.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1998\u003cbr\u003ePages: 21 p.\u003cbr\u003ePlates: 1 pl.\u003cbr\u003eScale: 1:125,000\u003cbr\u003eLocation: Sanpete County\u003cbr\u003eMedia Type: Paper Map\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203841306677,"sku":"M174","price":9.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/m174.png?v=1594683194"},{"product_id":"m-175","title":"Map of recharge and discharge areas for the principal valley-fill aquifer, Sevier Desert, Millard County, Utah (M-175)","description":"\u003cp\u003e\u003ci\u003eBy: N. P. Snyder\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eGround water from the principal unconsolidated basin-fill aquifer system is the most important source of agricultural and culinary water in the Sevier Desert. Recharge and discharge areas for the principal aquifer system were mapped to aid in management of potential contaminant sources to help protect ground-water quality.\u003c\/p\u003e \u003cp\u003eThe purpose of this study is to help state and local government officials and local residents protect ground-water quality in the Sevier Desert by defining recharge areas where ground-water aquifers are vulnerable to contamination.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1998\u003cbr\u003ePages: 21 p.\u003cbr\u003ePlates: 1 pl.\u003cbr\u003eScale: 1:175,000\u003cbr\u003eLocation: Millard County\u003cbr\u003eMedia Type: Paper Map\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203841339445,"sku":"M175","price":9.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/m175.png?v=1594683196"},{"product_id":"m-176","title":"Map of recharge areas for the principal valley-fill aquifer, Ogden Valley, Weber County, Utah (M-176)","description":"\u003cp\u003e\u003ci\u003eBy: N. P. Snyder and M. Lowe\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eWells in Ogden Valley provide drinking water for residents of the valley and Ogden City. Ground-water conditions in Ogden Valley have been studied for the past 60 years because of the importance of the resource to the Wasatch Front. Residential and recreational development has increased in Ogden Valley, underscoring the importance of maintaining a high-quality groundwater supply. In this study we mapped recharge areas for the principal valley-fill aquifer to aid in management of potential contaminant sources to protect the quality of ground water.\u003c\/p\u003e \u003cp\u003eThe purpose of this study is to help state and local government officials and local residents protect the quality of ground water in Ogden Valley by defining areas where ground-water aquifers are vulnerable to contamination.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1998\u003cbr\u003ePages: 16 p.\u003cbr\u003ePlates: 1 pl.\u003cbr\u003eScale: 1:75,000\u003cbr\u003eLocation: Weber County\u003cbr\u003eMedia Type: Paper Map\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203841372213,"sku":"M176","price":9.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/m176.png?v=1594683197"},{"product_id":"m-225","title":"Recharge and discharge areas for the principal basin-fill aquifer, Beryl-Enterprise area, Iron, Washington, and Beaver Counties, Utah (M-225)","description":"\u003cp\u003e\u003ci\u003eBy: K. J. Thomas and M. Lowe\u003c\/i\u003e\u003c\/p\u003e\n\u003cp\u003eThe primary source of drinking and irrigation water in the Beryl-Enterprise area is ground water from the principal basin-fill aquifer. We mapped recharge and discharge areas for the principal aquifer to provide a tool for management of potential contaminant sources to help protect ground-water quality. Contains a 14-page report with a 10-page well record appendix.\u003c\/p\u003e\n\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2007\u003cbr\u003ePages: 14 p. + 10 p. appendix\u003cbr\u003ePlate: 1 pl.\u003cbr\u003eScale: 1:125,000\u003cbr\u003eLocation: Beaver County, Iron County, and Washington County\u003cbr\u003eMedia:  CD or Paper Report\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"CD","offer_id":32205576699957,"sku":"M225","price":14.95,"currency_code":"USD","in_stock":true},{"title":"Report","offer_id":46510081081563,"sku":"M-M-225-rpt","price":14.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/m225_3330dbac-cad8-45e5-978b-9a2661a03722.png?v=1594756331"},{"product_id":"m-54c","title":"Ground-water resources of the central Wasatch Front areas (M-54C)","description":"\u003cp\u003e\u003ci\u003eBy: D. Price\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThis is one of a series of map reports compiled by the USGS and UGS describing the geology and related natural resources and hazards of the densely populated Wasatch Front of Utah. This report defines in a non-technical format the occurrence, availability, and quality of ground water in the central Wasatch Front area and guides readers to sources of more detailed information about the resource.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1988\u003cbr\u003ePages: 5 p.\u003cbr\u003ePlates: 3 pl.\u003cbr\u003eScale: 1:100,000\u003cbr\u003eLocation: Davis County, Morgan County, Salt Lake County, Tooele County, Utah County, and Weber County\u003cbr\u003eMedia Type: Paper Map\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"Default Title","offer_id":32203846844469,"sku":"M54C","price":7.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/m054c.png?v=1594683428"},{"product_id":"m-55c","title":"Ground-water resources of the southern Wasatch Front, Utah (M-55C)","description":"\u003cp\u003e\u003ci\u003eBy: D. Price and L. Conroy\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThis is one of a series of map reports compiled by the USGS and UGS describing the geology and related natural resources and hazards of the densely populated Wasatch Front of Utah. This report defines in a non-technical format the occurrence, availability, and quality of ground water in the southern Wasatch Front area and guides readers to sources of more detailed information about the resource.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1988\u003cbr\u003ePages: 6 p.\u003cbr\u003ePlates: 3 pl.\u003cbr\u003eScale: 1:100,000\u003cbr\u003eLocation: Juab County, Salt Lake County, Utah County, and Wasatch County \u003cbr\u003eMedia Type: Paper Map\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"Default Title","offer_id":32203847041077,"sku":"M55C","price":7.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/m055c.png?v=1594683434"},{"product_id":"mp-02-10","title":"Ground-water sensitivity and vulnerability to pesticides, Utah and Goshen Valleys, Utah County, Utah (MP 02-10)","description":"\u003cp\u003e\u003ci\u003eBy: I. D. Sanderson, M. Lowe, J. Wallace, and J. L. Kneedy\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThe U.S. Environmental Protection Agency has recommended that states develop Pesticide Management Plans for four agricultural chemicals - alachlor, atrazine, metolachlor, and simazine - used in Utah as herbicides in the production of corn and sorghum, and to control weeds and undesired vegetation (such as along right-of-ways or utility substations). This report and accompanying maps are intended to be used as part of these Pesticide Management Plans to provide local, state, and federal government agencies and agricultural pesticide users with a base of information concerning sensitivity and vulnerability of ground water in the basin-fill aquifer (bedrock is not evaluated) to agricultural pesticides in Utah and Goshen Valleys, Utah County, Utah. We used existing data to produce pesticide sensitivity and vulnerability maps by applying an attribute ranking system specifically tailored to the western United States using Geographic Information System analysis methods.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2002\u003cbr\u003ePages: 26 p.\u003cbr\u003ePlates: 2 pl.\u003cbr\u003eScale: 1:100,000\u003cbr\u003eLocation: Utah County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203857166389,"sku":"MP-0210","price":12.45,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/mp02-10.png?v=1594683794"},{"product_id":"mp-02-8","title":"Ground-water sensitivity and vulnerability to pesticides, Cache Valley, Cache County, Utah (MP 02-8)","description":"\u003cp\u003e\u003ci\u003eBy: I. D. Sanderson, M. Lowe, J. Wallace, and J. L. Kneedy\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThe U.S. Environmental Protection Agency has recommended that states develop Pesticide Management Plans for four agricultural chemicals - alachlor, atrazine, metolachlor, and simazine - used in Utah as herbicides in the production of corn and sorghum, and to control weeds and undesired vegetation (such as along right-of-ways or utility substations). This report and accompanying maps are intended to be used as part of these Pesticide Management Plans to provide local, state, and federal government agencies and agricultural pesticide users with a base of information concerning sensitivity and vulnerability of ground water in the basin-fill aquifer (bedrock is not evaluated) to agricultural pesticides in Cache Valley, Cache County, Utah. We used existing data to produce pesticide sensitivity and vulnerability maps by applying an attribute ranking system specifically tailored to the western United States using Geographic Information System analysis methods.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2002\u003cbr\u003ePages: 28 p.\u003cbr\u003ePlates: 2 pl.\u003cbr\u003eScale: 1:100,000\u003cbr\u003eLocation: Cache County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203857461301,"sku":"MP-028","price":12.45,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/mp02-8.png?v=1594683805"},{"product_id":"mp-03-1","title":"Ground-water sensitivity and vulnerability to pesticides, the southern Sevier Desert and Pahvant Valley, Millard County, Utah (MP 03-1)","description":"\u003cp\u003e\u003ci\u003eBy: M. Lowe and I. D. Sanderson\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThe U.S. Environmental Protection Agency has recommended that states develop Pesticide Management Plans for four agricultural chemicals - alachlor, atrazine, metolachlor, and simazine - used in Utah as herbicides in the production of corn and sorghum, and to control weeds and undesired vegetation (such as along right-of-ways or utility substations). This report and accompanying maps are intended to be used as part of these Pesticide Management Plans to provide local, state, and federal government agencies and agricultural pesticide users with a base of information concerning sensitivity and vulnerability of ground water in the basin-fill aquifer (bedrock is not evaluated) to agricultural pesticides in the southern Sevier Desert and Pahvant Valley, Millard County, Utah. We used existing data to produce pesticide sensitivity and vulnerability maps by applying an attribute ranking system specifically tailored to the western United States using Geographic Information System analysis methods.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2003\u003cbr\u003ePages: 28 p.\u003cbr\u003ePlates: 2 pl.\u003cbr\u003eLocation: Millard County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203857526837,"sku":"MP-031","price":12.45,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/mp03-1.png?v=1594683808"},{"product_id":"mp-89-4","title":"Water-related geologic problems of 1983 - Utah occurrences by County (MP 89-4)","description":"\u003cp\u003e\n \u003ci\u003eBy: B. N. Kaliser\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n Twenty-four counties in Utah were surveyed in 1983-84 to compile this summary of known geological events related to the 1983 wet year. It is hoped that this summary and the one by Davis will provide a data base that is 1) historically useful and 2) may be used in studies designed to mitigate similar occurrences.\u003c\/p\u003e\n \u003cp\u003e\n Twenty-two of the twenty-four counties were included in the Presidential disaster declaration. One county included in that declaration, Garfield, in southeastern Utah, is omitted because of its inclusion in the report by Davis. The three counties not included in the disaster declaration are Cache in northern Utah, and Iron and Washington counties in southwestern Utah. Under each county the sequence of types of events discussed or listed is as follows: (1) slope movements of all types, (2) ground-water changes, including elevation of shallow, unconfined water tables, (3) erosion and sedimentation effects, (4) foundation problems and other phenomena.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1989\u003cbr\u003e\n Pages: 24 p.\u003cbr\u003e\n Location: Utah\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203861131317,"sku":"MP-894","price":3.75,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/mp89-4.png?v=1594683974"},{"product_id":"ofr-360","title":"A summary of the geology and hydrogeology of the Cedar Valley drainage basin, Iron County, Utah (OFR-360)","description":"\u003cp\u003e\n \u003ci\u003eBy: C. Eisinger\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n The Cedar Valley drainage basin encompasses more than 580 square miles (1,502 km2) in southwestern Utah. Located in the transition zone between the Basin and Range and Colorado Plateau physiographic provinces, the drainage basin includes Cedar Valley, the Hurricane Cliffs, and the western part of the Markagunt Plateau. The exposed geology of the area includes rocks of Paleozoic, Mesozoic, and Cenozoic age, with an aggregate thickness of more than 16,000 feet (4,877 m). The region witnessed an episode of calc-alkaline volcanism during the late Eocene, Oligocene, and early Miocene, and then a period of more passive volcanism beginning in the mid-Miocene. Basin-and-range extension formed Cedar Valley through large-scale normal faulting and subsequent erosion. Quaternary alluvium and volcanic deposits more than 1,000 feet thick underlie the floor of Cedar Valley. This alluvial valley fill is the principal aquifer in the basin.\u003c\/p\u003e\n \u003cp\u003e\n Ground water in Cedar Valley exists under confined, unconfined, and perched conditions. The valley-fill aquifer is composed primarily of sand, gravel, clay, and silt, and includes many high-permeability beds that yield water up to 4,000 gallon\/minute (15,100 liters\/min). Perennial streams and springs are the major sources of recharge in the valley, and withdrawal of water from wells is the single largest means of ground-water discharge. Total-dissolved-solids concentrations measured in wells ranged from 158 to 2,752 mg\/L (158 to 2,752 parts per million) in 1978, and the general quality of water is good. The principal ground-water contaminant identified in the Cedar Valley basin-fill is nitrate. Potential ground-water-pollution sources include septic tank soil-absorption systems, agricultural fertilizer, and sewage lagoons.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1998\u003cbr\u003e\n Pages: 14 p.\u003cbr\u003e\n Location: Iron County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203873419317,"sku":"OFR360","price":1.2,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr360.png?v=1594684431"},{"product_id":"ofr-447","title":"Water resources of Millard County, Utah (OFR-447)","description":"\u003cp\u003e\u003ci\u003eBy: F. D. Davis\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThis summary of the water resources of Millard County is designed to accompany Utah Geological Survey Bulletin 133, Geology of Millard County, Utah (Hintze and Davis, 2003). It provides a general overview of the surface- and ground-water conditions based on data compiled from a variety of sources. Technical details on the water resources are present in the reference sources cited in this report and in additional publications at the end of the reference list, in particular the Utah Department of Natural Resources Technical Publications and Basic Data Reports. The geology in this water-resources report will be more understandable if the reader refers to UGS Bulletin 133.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2005\u003cbr\u003ePages: 27 p.\u003cbr\u003eLocation: Millard County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203875352629,"sku":"OFR447","price":10.0,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr447.png?v=1594684503"},{"product_id":"ofr-465","title":"Water-Resource Bulletins of the Utah Geological Survey, 1962 to 1987 (OFR-465)","description":"\u003cp\u003eThis self-actuating CD contains 25 reports published from 1962 to 1987. Most of these reports are long out of print but have historical and scientific value still. The report in this publication are listed below:\u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-1\u003c\/b\u003e Water production from oil wells of the Uinta Basin, by H. D. Goode and R. D. Feltis, 1962, 22 p., 3 pl., 2 oversize tables\u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-2\u003c\/b\u003e Ground-water conditions in the southern and central parts of the East Shore area 1953-1961, by R. E. Smith and J. S. Gates, 1963, 41 p., 2 pl. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-3\u003c\/b\u003e Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the Salt Lake brine, Part I: Selected hydrologic data, by D. C. Hahl and C. G. Mitchell, 1963, 40 p., 1 pl.; Part II - Technical report, by D. C. Hahl and R. H. Langford, 1964, 40 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-4\u003c\/b\u003e Hydrogeologic reconnaissance of part of the headwaters area of the Price River, Utah, by R. M. Cordova,1963, 26 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-5\u003c\/b\u003e Reconnaissance of water resources of a part of western Kane County, Utah, by H. D. Goode, 1964, 64 p., 1 pl. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-6\u003c\/b\u003e Evaporation studies, Great Salt Lake, Part I: Evaporation and ground water, Great Salt Lake, by E. L. Peck and D. R. Dickson, 14 p.; Part II: Evaporation from the Great Salt Lake as computed from eddy flux techniques, by D. R. Dickson and C. McCullom, Jr., 1965, 21 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-7\u003c\/b\u003e Geology and ground-water resources of the Jordan Valley, by I. W. Marine and D. Price, 1964, 68 p., 10 pl. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-8\u003c\/b\u003e Second reconnaissance of water resources in western Kane County, Utah, by H. D. Goode, 1966, 44 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-9\u003c\/b\u003e Reconnaissance of the chemical quality of water in western Utah, Sink Valley area, drainage basins of Skull, Rush and Government Creek Valleys and the Dugway Valley - Old River Bed area, by K. M. Waddell, 1967, 15 p., 5 oversize tables\u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-10\u003c\/b\u003e Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the Salt Lake brine, summary for water years 1960, 1961, 1964, by D. C. Hahl, 1968, 35 p., 1 pl., \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-11\u003c\/b\u003e Reconnaissance appraisal of the water resources near Escalante, Garfield County, Utah, by H. D. Goode, 1969, 38 p., 1 pl. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-12\u003c\/b\u003e Great Salt Lake, Utah: chemical and physical variations of the brine, 1963-1966, by D. C. Hahl and A. H. Handy, 1969, 33 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-13\u003c\/b\u003e Major thermal springs of Utah, by J. C. Mundorff, 1970, 60 p., 2 pl. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-14\u003c\/b\u003e Effects of a causeway on the chemistry of the brine in Great Salt Lake, Utah, by R. J. Madison, 1970, 52 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-15\u003c\/b\u003e Evaluation of eddy flux techniques in computing evaporation from the Great Salt Lake, by D. R. Dickson and A. E. Rickers, 1970, 6 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-16\u003c\/b\u003e Nonthermal springs of Utah, by J. C. Mundorff, 1971, 70 p., 2 pl. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-17\u003c\/b\u003e Great Salt Lake, Utah: chemical and physical variations of the brine 1966-1972, by J. A. Whelan, 1973, 24 p., 2 pl. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-18\u003c\/b\u003e The effects of restricted circulation on the salt balance of Great Salt Lake, Utah, by K. M. Waddell and E. L. Bolke, 1973, 54 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-19\u003c\/b\u003e Hydrogeology of the Bonneville Salt Flats, Utah, by L. J. Turk, 1973, 81 p., 1 pl. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-20\u003c\/b\u003e Great Salt Lake, Utah: chemical and physical variations of the brine, water year 1973, by J. A. Whelan and C. A. Peterson, 1975, 29 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-21\u003c\/b\u003e Model for evaluating the effects of dikes on the water and salt balance of Great Salt Lake, Utah, by K. M. Waddell and F. K. Fields, 1977, 54 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-22\u003c\/b\u003e Great Salt Lake, Utah: chemical and physical variations of the brine, water years 1974 and 1975, by J. A. Whelan and C. A. Peterson, 1977, 47 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-23\u003c\/b\u003e Hydrogeology of Utah Lake with emphasis on Goshen Bay, (Utah Co.) by J. D. Dustin and L. B. Merritt, 1980, 50 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-24\u003c\/b\u003e Floods of May to June 1983 along the northern Wasatch Front, Salt Lake City to North Ogden, Utah, by K. L. Lindskov, 1984, 12 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eWRB-25\u003c\/b\u003e Effects of breaching the Southern Pacific Railroad Causeway, Great Salt Lake, Utah physical and chemical changes, August 1, 1984-July, 1986, by J. W. Gwynn and P. A. Sturm, 1987, 25 p. \u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2005\u003cbr\u003ePages: 1065 p.\u003cbr\u003ePlates: 26 pl.\u003cbr\u003eLocation: Beaver County, Box Elder County, Cache County, Carbon County, Davis County, Duchesne County, Garfield County, Kane County, Millard County, Morgan County, Rich County, Salt Lake County, Sanpete County, Sevier County, Summit County, Tooele County, Uintah County, Utah County, Wasatch County, Washington County, and Weber County \u003cbr\u003e\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"CD","offer_id":32205582598197,"sku":"OFR465","price":14.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr465_a75c7a6f-32fb-4ab3-8667-214b44e1ec33.png?v=1594756601"},{"product_id":"ofr-528","title":"Ground-water conditions in the Green Pond landslide, Weber County, Utah (OFR-528)","description":"\u003cp\u003e\n \u003ci\u003eBy: F. X. Ashland, R. E. Giraud, G. N. McDonald, and A. H. Elliott\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n The Green Pond landslide is a large historically active landslide crossed by SR-226 in Weber County, Utah. The landslide is elongate, somewhat irregularly shaped, about 7800 feet long, and has a length to width ratio that varies between about 78:1 and 7:1. Monitoring and observations indicate that the landslide is recurrently or possibly even continuously active, but can be subdivided into currently active and inactive parts.\u003c\/p\u003e\n \u003cp\u003e\n As part of geotechnical investigations for State Route 226, seven monitoring wells were installed in and near the Green Pond landslide, a large, historically active landslide in the Norwood Tuff. Data from two of these wells, collected by the Utah Department of Transportation, provide information on ground-water level fluctuations over an approximately six-year period between 2000 and 2005. In addition, we monitored ground-water levels monthly at three wells, and made periodic ground-water level observations at two others between June 2006 and December 2007. This report summarizes the results of our ground-water-level monitoring and analysis of the UDOT data.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 2008\u003cbr\u003e\n Pages: 8 p.\u003cbr\u003e\n Location: Weber County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"Default Title","offer_id":32203877777461,"sku":"OFR528","price":4.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr528.png?v=1594684605"},{"product_id":"ofr-550","title":"Snowmelt-induced ground-water fluctuations in selected northern Utah landslides ? preliminary results from the 2007-08 landslide water year (OFR-550)","description":"\u003cp\u003e\n \u003ci\u003eBy: F. X. Ashland\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n The relationship between ground-water levels and late winter\/early spring snowmelt was evaluated at selected northern Utah landslides where ground-water observation wells had previously been installed. The period of investigation between September 2007 and August 2008 was characterized by generally wetter-than-normal conditions in the fall and early winter and subsequent drier-than-normal conditions. Snowfall in early winter resulted in a sustained snowpack that lasted through early 2008 at low elevation and into the spring at higher elevation. Ground-water levels predictably rose with melting snow, but the proportion of the rise attributable to melting of the winter snowpack varied.\u003c\/p\u003e\n \u003cp\u003e\n The scope of the investigation consists of compiling provisional precipitation data from National Weather Service (NWS) stations near the landslides, collecting field measurements and observations on snow depth and ground-water levels, and data analysis. Provisional NWS data included daily, storm-specific, and monthly precipitation and snow depth data for stations near (typically within a few miles of and commonly in line-of-sight to) the landslides. The use of provisional NWS data allowed for tracking of precipitation concurrent with the fieldwork described below.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 2009\u003cbr\u003e\n Pages: 19 p.\u003cbr\u003e\n Location: Davis County, Salt Lake County, Utah County, and Weber County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203878531125,"sku":"OFR550","price":8.95,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr550.png?v=1594684635"},{"product_id":"ofr-560","title":"Ground-water quality classification for the principal basin-fill aquifer, Salt Lake Valley, Salt Lake County, Utah (OFR-560)","description":"\u003cp\u003e\u003ci\u003eBy: J. Wallace and M. Lowe\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eContains a report (15 pages + 64-page appendix) and three plates (maps at 1:75,000 scale), all, that address ground-water quality in Salt Lake Valley?s basin-fill aquifer and provide recommendations for water-resource management and land-use planning. The maps are described in detail in the report and show total-dissolved-solids concentration, ground-water quality classes, and potential contaminant sources.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2009\u003cbr\u003ePages: 15 p. + 96 p. appendix\u003cbr\u003ePlates: 3 pl.\u003cbr\u003eScale: 1:75,000\u003cbr\u003eLocation: Salt Lake County\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"CD","offer_id":32205583581237,"sku":"OFR560","price":19.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr560_9076e013-46ec-40cf-b4ac-5713d8fc53fc.png?v=1594756648"},{"product_id":"ofr-578","title":"Temperature profiles of water monitoring wells in Snake Valley, Tule Valley, and Fish Springs Flat, Millard and Juab Counties, Utah (OFR-578)","description":"\u003cp\u003e\u003ci\u003eBy: R. Blackett\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThe Snake Valley Ground-Water Monitoring Well Project is located in west-central Utah and east-central Nevada. The study region is a north-south trending hydrologic basin straddling the Nevada-Utah state line for 135 miles in the east-central part of the Great Basin. Situation within the Basin and Range Province, Snake Valley is bounded by several north-south trending mountain ranges including the Snake Range and Deep Creek Range on the west, and the Confusion Range, Burbank HIlls, and Mountain Home Range to the east-southeast.\u003c\/p\u003e \u003cp\u003eThis project was established in response to proposed water-development projects in east-central Nevada that could affect ground water resources in west-central Utah. Objectives of the Snake Valley Ground-Water Monitoring Well Project are to improve the understanding of the ground-water flow systems and resources, characterize baseline ground-water levels and chemistry, and measure future changes in these parameters.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2011\u003cbr\u003ePages: 13 p. + 24 p. appendix\u003cbr\u003eLocation: Juab County and Millard County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203880071221,"sku":"OFR578","price":9.95,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr578.png?v=1594684671"},{"product_id":"ofr-579","title":"Cache Valley Principal Aquifer Storage and Recovery Site Assessment: Phase I (OFR-579)","description":"\u003cp\u003e\u003ci\u003eBy: K. Thomas, R. Q. Oaks, Jr., P. Inkenbrandt, W. Sabbah, and M. Lowe\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eCache Valley is a rural area in northern Utah experiencing an increase in urbanization and ground-water use. Ground water, mostly from the basin-fill aquifer, provides a significant proportion of the drinking-water supply in Cache Valley. Maintaining adequate ground-water supplies and limiting the potential for well interference are critical issues in determining the extent and nature of future development in Cache Valley.\u003c\/p\u003e \u003cp\u003eThis study is an assessment of the potential for aquifer storage and recovery projects in Cache Valley, including the identification of potential sites, recommendation of most appropriate methods, permitting requirements, and determination of data-collection needs.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2011\u003cbr\u003ePages: 34 p. + 23 p. appendices\u003cbr\u003eLocation: Cache County\u003cbr\u003e\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"CD","offer_id":32205583745077,"sku":"OFR579","price":14.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr579_11d62c06-5d4e-4285-a57f-44cc94b55fab.png?v=1594756655"},{"product_id":"ofr-592","title":"Groundwater Quality Classification for the Principal Basin-Fill Aquifer, East Shore Area, Davis County, Utah (OFR-592)","description":"\u003cp\u003e\u003ci\u003eBy: Janae Wallace, Paul Inkenbrandt, and Mike Lowe\u003c\/i\u003e\u003c\/p\u003e\u003cp\u003e Contains a 15-page report with a 79-page appendices and 3 maps at 1:24,000 and 1:50,000 scale, in easily readable PDF format, that address groundwater quality in the east shore area of Davis County's basin-fill aquifer. The report provides recommendations for water-resource management and land-use planning. The maps are described in detail in the report and show total-dissolved-solids concentration, groundwater quality classes, and potential contaminant sources.\u003c\/p\u003e\u003cp\u003e\u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003ePublished: 2012\u003cbr\u003ePages: 15 p. + 79 p. Appendix\u003cbr\u003ePlates: 3 maps\u003cbr\u003eScale: 1:24,000 and 1:50,000\u003cbr\u003eLocation: Davis County\u003cbr\u003e\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"CD","offer_id":32205584039989,"sku":"OFR592","price":19.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/OFR592_c53acfc9-63f7-4c12-9fcd-08bd696a4829.png?v=1594756670"},{"product_id":"ofr-615","title":"Cache Valley Aquifer Storage and Recovery- Phase II (OFR-615)","description":"\u003cp\u003e\u003ci\u003eBy: Paul Inkenbrandt, Kevin Thomas, and Christian Hardwick\u003c\/i\u003e\u003c\/p\u003e\u003cp\u003eNorth Logan City modified a gravel excavation site at the mouth of Green Canyon during the spring of 2011 to retain excess flow from the Green Canyon catchment. From August 2011 to March 2012, the Utah Geological Survey (UGS) monitored water flow into the gravel pit, and recorded gravity data and groundwater levels at several sites within a mile of the gravel pit. The UGS observed a significant increase in gravity from August to September in an area southwest of the gravel pit, which indicates an increase in the amount of water in that region from August to September. Based on the measured increase, water is traveling from the gravel pit towards the region of the principal aquifer of Cache Valley. \u003c\/p\u003e\u003cp\u003eContains a 39-page report and one plate, both. The latest version of Adobe Reader is required to view the PDF files.\u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003ePublished: 2013\u003cbr\u003ePages: 39\u003cbr\u003ePlates: 1\u003cbr\u003eScale:\u003cbr\u003eLocation: Utah\u003cbr\u003e\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"CD","offer_id":32205584826421,"sku":"OFR615","price":14.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/OFR-615_044e5cd8-eb69-44c8-9ec7-dc900f84b8d3.jpg?v=1594756700"},{"product_id":"ofr-636","title":"Cache Valley Aquifer Storage and Recovery-Site Assessment for Millville City, Cache County, Utah (OFR-636)","description":"\u003cp\u003e\u003ci\u003eBy: Paul Inkenbrandt\u003c\/i\u003e\u003c\/p\u003e\u003cp\u003eThe City of Millville, located in a prime location for aquifer storage and recovery (ASR), is having issues with elevated nitrate in the Glenridge well, a public water supply sourced from the Cache Valley principal aquifer. To alleviate high nitrate, the city performed an initial injection and pumping test using the Glenridge well. Millville injected water from Garr Spring, another public water supply source of which they own water rights, into the Glenridge well for one week at a rate of 500 gallons per minute. They then pumped the well while monitoring geochemistry to determine the effects on the Cache Valley principal aquifer system. The pre-injection nitrate concentration in the Glenridge well was 7.65 mg\/l nitrate as nitrogen, and the nitrate concentration after pumping more than 172% of the volume of water injected was 6.52 mg\/l nitrate as nitrogen. There is likely some dispersion of the injected spring water via advection in the aquifer. \u003c\/p\u003e\u003cp\u003e\u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003ePublished: 2014\u003cbr\u003ePages: 30\u003cbr\u003eLocation: Utah\u003cbr\u003e\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"CD","offer_id":32205585252405,"sku":"OFR636","price":14.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/OFR-636_d7b19337-68c3-4034-8c47-14efa8406190.jpg?v=1594756717"},{"product_id":"ofr-661","title":"Utah Wetland Functional Classification: Version 1 (OFR-661 )","description":"\u003cp\u003e\u003ci\u003eBy: Richard Emerson and Ryhan Sempler\u003c\/i\u003e\u003c\/p\u003e\u003cp\u003eThe National Wetland Inventory (NWI) is the most comprehensive wetland classification system for the state of Utah. While the NWI is the most complete and accessible classification system, the 366 unique wetland type identifiers in the state are often difficult to interpret and have little relevance to natural resource managers. This report describes the Utah Geological Survey reclassification of the NWI data to provide the users with the most current data with a universal database schema across the state.\u003c\/p\u003e\u003cp\u003e\u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003ePublished: 2017\u003cbr\u003ePages: 17\u003cbr\u003eLocation: Utah\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203882496053,"sku":"OFR661","price":5.95,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr-661.jpg?v=1594684769"},{"product_id":"ofr-662","title":"Spring Inventory and Preliminary Groundwater Dependent Ecosystems Assesment of Manti-La Sal National Forest, Wasatch Plateau, Utah (OFR-662)","description":"\u003cp\u003e\u003ci\u003eBy: Paul Inkenbrandt, Richard Emerson, Janae Wallace, J. Lucy Jordan, and Stefan Kirby\u003c\/i\u003e\u003c\/p\u003e\u003cp\u003eIn cooperation with the U.S. Forest Service, the Utah Geological Survey mapped springs and groundwater dependent ecosystems on the Wasatch Plateau. Using remote sensing, GIS, and field checking, more than 400 points were compiled and plotted for use by the Forest Service\u003c\/p\u003e\u003cp\u003e\u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003ePublished: 2017\u003cbr\u003ePages: 82\u003cbr\u003ePlates: 3\u003cbr\u003eScale: 1:200,000\u003cbr\u003eLocation: Utah\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"Default Title","offer_id":32203882561589,"sku":"OFR662","price":19.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/662.jpg?v=1594684771"},{"product_id":"ofr-699","title":"Mapping Groundwater Quality and Chemistry Adjacent to Great Salt Lake, Utah (OFR-699)","description":"\u003cp\u003e\u003ci\u003eBy: Stefan M. Kirby, Paul C. Inkenbrandt, and Andrew Rupke\u003c\/i\u003e\u003c\/p\u003e\u003cp\u003eThis report details the data compilation and database construction of groundwater chemistry adjoining Great Salt Lake and its wetlands. The database includes publicly available major solute, trace constituent, nutrient, and isotopic data available near Great Salt Lake. The database also includes new samples collected as part of this project. A select subset of the highest quality data was used to interpolate total dissolved solids in groundwater surrounding Great Salt Lake as well as create maps that depict various aspects of geochemistry in groundwater adjoining the Great Salt Lake. Available state-level wetland type mapping and wetland fluid geochemistry are also included in the database. This chemistry database is a first step towards understanding and better constraining the role of groundwater in various Great Salt Lake processes and habitats and provides important baseline chemistry.\u003c\/p\u003e\u003cp\u003e\u003c\/p\u003e\u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003ePublished: 2019\u003cbr\u003ePages: 19\u003cbr\u003eLocation: Utah\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"Default Title","offer_id":32203883380789,"sku":"OFR699","price":5.95,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/OFR-699.jpg?v=1594684802"},{"product_id":"ofr-82","title":"Significant drill holes of the Wasatch Front valleys including Cache Valley and Tooele Valley (OFR-82)","description":"\u003cp\u003e\n \u003ci\u003eBy: W. F. Case\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n Records of 292 significant drill holes which were drilled in the major valley areas of the Wasatch Front have been compiled into a Utah Geological and Mineral Survey database, given in this publication.\u003c\/p\u003e\n \u003cp\u003e\n Drill holes which are judged to be “significant” are those with complete surface to total depth lithology logs which are approximately 1000 feet deep or deeper, and\/or which terminate in bedrock. Most of the wells are water wells, a few are research, geothermal, and exploration wells.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1985 (updated 1988)\u003cbr\u003e\n Pages: 235 p.\u003cbr\u003e\n Location: Box Elder County, Cache County, Davis County, Salt Lake County, Tooele County, Utah County, and Weber County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203883511861,"sku":"OFR82","price":20.75,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ofr082.png?v=1594684807"},{"product_id":"ri-187","title":"Geologic evaluation of five culinary water facilities and settlement canyon dam for Tooele City, Tooele County, Utah (RI-187)","description":"\u003cp\u003e\u003ci\u003eBy: W. R. Lund\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThis report presents the results of an investigation of geologic conditions at five culinary water facilities maintained by Tooele City Corporation and at Settlement Canyon Dam and reservoir. The facilities include four concrete water tanks and a well field. The purpose of the investigation was to determine if geologic conditions exist which may adversely effect the city's culinary water system or the dam and reservoir. The investigation included a review of available geologic literature, air photo analysis, a helicopter reconnaissance of Middle and Settlement Canyons, and 5 days of field inspection and geologic mapping. Coordination with Tooele City was through Mr. Joe D. England, Tooele City Engineer. The Utah Division of Water Rights Office of Dam Safety reviewed the sections of the report dealing with Settlement Canyon Dam.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1984\u003cbr\u003ePages: 32 p.\u003cbr\u003eLocation: Tooele County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203913134133,"sku":"RI187","price":3.9,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri187.png?v=1594685157"},{"product_id":"ri-202","title":"UGS involvement with Paradox Basin repository siting: a review of UGS activities associated with the Department of Energy's efforts to evaluate areas within the Paradox Basin as suitable for a high level nuclear waste repository (San Juan County) (RI-202)","description":"\u003cp\u003e\n \u003ci\u003eBy: S. N. Eldredge and G. Atwood\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n This Report of Investigation consists of four reports that summarize different aspects Qf the Utah Geological and Mineral Survey's (UGMS) review of the U.S. Department of Energy's (DOE) program to evaluate several areas in the Paradox Basin as suitable for a high-level nuclear waste repository. This document brings together most of the technical comments and other concerns that the UGMS geologists and Utah's Geology Work Group raised regarding DOE's program. These reports were written over a two-year period of time as part of the UGMS responsibility to review DOE activities. Editorial standards have not been entirely adhered to because of the different conditions, purposes, and audiences for which the reports were originally written. They have been edited to a limited extent for clarity, although, extensive changes in text have been avoided.\u003c\/p\u003e\n \u003cp\u003e\n Numerous concerns are raised in these four reports relative to the suitability of the Davis Canyon and Lavender Canyon sites for a high-level nuclear waste repository and the adequacy of the data upon which the DOE based major decisions. Many of these concerns have not been resolved to the satisfaction of the UGMS. This Report of Investigation is intended as a permanent record outlining the UGMS activities relating to the evaluation of proposed high-level nuclear waste repository sites in the Paradox Basin and comments made by the UGMS and Geology Work Group on documents prepared by the DOE and DOE contractors.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1985\u003cbr\u003e\n Pages: 84 p.\u003cbr\u003e\n Location: San Juan County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203916902453,"sku":"RI202","price":9.1,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri202.png?v=1594685177"},{"product_id":"ri-206","title":"Geologic evaluation of a proposed regional wastewater treatment plant site, Washington County, Utah (RI-206)","description":"\u003cp\u003e\u003ci\u003eBy: W. R. Lund and W. F. Case\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThis report presents the results of a geologic investigation at the site proposed for construction of a regional wastewater treatment plant in southwestern Washington County, Utah. The purpose of the investigation was to determine if geologic conditions exist at the site which might adversely affect the proposed facility. The investigation included a review of available geologic literature, air photo analysis, field reconnaissance and mapping, and excavation of 6 test pits.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1986\u003cbr\u003ePages: 22 p.\u003cbr\u003eLocation: Washington County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203917361205,"sku":"RI206","price":2.9,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri206.png?v=1594685183"},{"product_id":"ri-229","title":"Recharge area and water quality of the valley-fill aquifer, Castle Valley, Grand County, Utah (RI-229)","description":"\u003cp\u003e\u003ci\u003eBy: N. P. Snyder\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eCastle Valley is one of several northwest-trending salt anticline valleys on the Colorado Plateau in southeastern Utah. The unconsolidated valley fill is the principal aquifer in the valley and consists of coarse alluvial-fan deposits and stream alluvium, with minor clay. Some recharge to the valley-fill aquifer comes from underflow from bedrock aquifers, but most is from La Sal Mountains runoff via Castle Creek and Placer Creek. Because of the absence of protective, low-permeability confining layers, the valley-fill aquifer is unconfined, and most of the valley is classified as primary recharge area. The only discharge area is along lower Castle Creek.\u003c\/p\u003e \u003cp\u003eIncreased residential development using individual wastewater-disposal systems has raised concerns for the long-term quality of ground water in the valley-fill aquifer. In this study, ground-water recharge and discharge areas, potentiometric surface elevation, and specific conductance were mapped to serve as tools for protecting ground-water quality and managing potential contaminant sources in Castle Valley.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1996\u003cbr\u003ePages: 22 p.\u003cbr\u003eLocation: Grand County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203920212021,"sku":"RI229","price":2.9,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri229.png?v=1594685216"},{"product_id":"ri-235","title":"The potential impact of septic tank soil-absorption systems on water quality in the principal valley-fill aquifer, Tooele Valley, Tooele County, Utah - assessment and guidelines (RI-235)","description":"\u003cp\u003e\u003ci\u003eBy: J. Wallace and M. Lowe\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eNitrate from sewers, septic-tank-soil-absorption systems, fertilizer, and other anthropogenic sources is a useful indicator of human impact on ground-water quality. Nitrate can thus be used to identify potential deleterious effects of development which uses septic tank soil-absorption systems. The purpose of this document is to: (1) provide a valley-wide assessment of the potential impact of nitrate from increasing the number of septic tank soil-absorption systems on ground water in Tooele Valley using methods similar to those used by Hansen, Allen, and Luce, Inc. for Heber and Round Valleys, Wasatch County, Utah; and (2) provide site-specific recommendations for evaluating the effects of septic systems on ground-water quality for proposed subdivisions in Tooele Valley.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1998\u003cbr\u003ePages: 10 p.\u003cbr\u003eLocation: Tooele County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203920998453,"sku":"RI235","price":3.0,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri235.png?v=1594685225"},{"product_id":"ri-237","title":"The potential impact of septic tank soil-absorption systems on water quality in the principal valley-fill aquifer, Ogden Valley, Weber County, Utah (RI-237)","description":"\u003cp\u003e\u003ci\u003eBy: J. Wallace and M. Lowe\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eNitrate from sewers, septic tank soil-absorption systems, fertilizer, and other anthropogenic sources is a useful indicator of human impact on ground-water quality. Nitrate can thus be used to identify potential deleterious effects of development using septic tank soil-absorption systems. The purpose of this document is to: (1) provide a valley-wide assessment of the potential impact of nitrate from an increasing number of septic tank soil-absorption systems on ground water in Ogden Valley using methods similar to those used by Hansen, Allen, and Luce, Inc. for Heber and Round Valleys, Wasatch County, Utah; and (2) provide site-specific recommendations for evaluating the effects of septic systems on ground-water quality for proposed subdivisions in Ogden Valley.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1998\u003cbr\u003ePages: 11 p.\u003cbr\u003eLocation: Weber County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203921358901,"sku":"RI237","price":1.8,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri237.png?v=1594685228"},{"product_id":"ri-238","title":"Guidelines for preparing hydrogeologic reports addressing suitability for alternative waste-water disposal systems in rock in Duchesne County, Utah (RI-238)","description":"\u003cp\u003e\u003ci\u003eBy: M. Lowe\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eMany lots in Duchesne County cannot presently be developed because exposed or shallow rock makes them unsuitable for conventional septic tank soil-absorption systems. Duchesne County and the Utah Division of Water Quality have developed designs for alternative waste-water disposal systems that may be used in rock if geologic conditions are suitable and humans will not be exposed to waste-water pathogens. To demonstrate conformance with these criteria, hydrogeologic studies of proposed sites will need to be conducted and results submitted to the Uintah Basin Public Health Department (UBPHD). The purpose of this report is to provide guidelines for: (1) geologists preparing hydrogeologic reports pertinent to waste-water disposal in rock, and (2) geologists and UBPHD officials reviewing these reports.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1998\u003cbr\u003ePages: 11 p.\u003cbr\u003eLocation: Duchesne County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203921457205,"sku":"RI238","price":1.8,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri238.png?v=1594685229"},{"product_id":"ri-239","title":"The potential impact of septic tank soil-absorption systems on water quality in the principal valley-fill aquifer, Cedar Valley, Iron County, Utah - assessment and guidelines (RI-239)","description":"\u003cp\u003e\n \u003ci\u003eBy: J. Wallace and M. Lowe\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n Nitrate can be used to identify potential deleterious effects of development using septic tank soil-absorption systems. We use a mass-balance approach to provide a valley-wide assessment of the potential impact of nitrate from septic tank soil-absorption systems on ground-water quality. Approximately 1,406 septic systems exist in Cedar Valley. Our calculations indicate the number of septic tank soil-absorption systems in Cedar Valley should not exceed 4,000, representing a valley-wide average septic-system density of about 27 acres\/system (0.109 km2\/system), to maintain an overall nitrate concentration of 6.5 ppm (6.5 mg\/L). This allows a 1 mg\/L degradation of water quality with respect to nitrate from the current background level of 5.5 ppm (5.5 mg\/L). We also provide guidelines for site-specific evaluations of the effects of septic systems on ground-water quality for proposed subdivisions in Cedar Valley\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1998\u003cbr\u003e\n Pages: 11 p.\u003cbr\u003e\n Location: Iron County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203921588277,"sku":"RI239","price":1.8,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri239.png?v=1594685231"},{"product_id":"ri-240","title":"Delineation of drinking water source protection zones for the Green Hills Country Estates well 02, Weber County, Utah (RI-240)","description":"\u003cp\u003e\u003ci\u003eBy: C. E. Bishop and M. Lowe\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThis report describes the delineation of drinking-water-source-protection zones for a public-water-supply well owned by the Green Hills Country Estates Water Company. Public water suppliers in Utah are required by Utah?s Drinking Water Source Protection Regulations to develop a drinking-water-source-protection plan for their public drinking-water sources, and drinking-water-source-protection zones are a part of this plan. Several delineation procedures are allowed under the regulations and a ?Preferred Delineation Procedure? was used to delineate the protection zones for this well, because it reflects the hydrogeologic system in the area.\u003c\/p\u003e \u003cp\u003eThis report describes our delineation of drinking-water-source-protection (DWSP) zones for a public-supply well in eastern Ogden Valley, Weber County. The Green Hills Country Estates Water Company (GHCEWC), which became the owner of the well once it was completed, requested this delineation. The scope of work included a literature search, review of water-well logs, field reconnaissance, an aquifer test, interpretation of test data, delineation of the DWSP zones, and preparation of this report.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1999\u003cbr\u003ePages: 24 p. + 15 p. appendix\u003cbr\u003eLocation: Weber County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203921686581,"sku":"RI240","price":4.6,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri240.png?v=1594685232"},{"product_id":"ri-241","title":"Potential mineral precipitation and water compatibilities related to the Drunkards Wash project, Carbon County, Utah (RI-241)","description":"\u003cp\u003e\n \u003ci\u003eBy: J. W. Gwynn\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n River Gas Corporation produces approximately 36,000 barrels per day of saline water from the Ferron Sandstone Member of the Mancos Shale as part of its Drunkards Wash coalbed-methane recovery project. Most of the sodium-bicarbonate-chloride produced water is disposed of by re-injection, the remainder is put into a pond to evaporate. Computer simulations using the PHRQPITZ program were used to evaluate water-chemistry problems.\u003c\/p\u003e\n \u003cp\u003e\n The purpose of this investigation was to test the applicability of the PHRQPITZ computer program in evaluating water-chemistry problems related to River Gas Corporation's Drunkards Wash coalbed-methane-recovery program. The objectives of this investigation were to: (1) determine, through computer simulation, what salts might be produced from RGC's saline evaporation-pond water through controlled, sequential evaporation, and (2) evaluate, through computer simulation, the compatibility of the injected Ferron Sandstone water and the Navajo and Wingate Sandstone connate brines, and the potential for mineral precipitation, as they are mixed in various ratios under assumed down-hole conditions.\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 1998\u003cbr\u003e\n Pages: 22 p.\u003cbr\u003e\n Location: Carbon County\u003cbr\u003e\n Media Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203921784885,"sku":"RI241","price":2.9,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri241.png?v=1594685233"},{"product_id":"ri-243","title":"Delineation of drinking water source protection zones for the Newcastle public water supply well, Iron County, Utah (RI-243)","description":"\u003cp\u003e\u003ci\u003eBy: C. E. Bishop\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThe Newcastle Water Company (NWC) operates a single well to supply potable water for consumption and use by the town of Newcastle. To protect this well from contamination and to comply with Utah's Drinking Water Source Protection Program, the town is developing a Drinking Water Source Protection Plan.\u003c\/p\u003e \u003cp\u003eThis report describes the delineation of drinking-water-source-protection (DWSP) zones for a public-water-supply well in southern Escalante Valley, Iron County, Utah. The well is about 3.25 miles northwest of the town of Newcastle, along Utah Highway 56. The town of Newcastle is a rural farming community that obtains its municipal drinking water from this well. The Newcastle Water Company (NWC) owns the well, and requested and assisted in this delineation of DWSP zones. The scope of work included a literature search, review of water-well logs, field reconnaissance, an aquifer test, interpretation of test data, delineation of the DWSP zones, and preparation of this report.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 1999\u003cbr\u003ePages: 51 p. + 20 p. appendix\u003cbr\u003eLocation: Iron County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203922014261,"sku":"RI243","price":7.8,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri243.png?v=1594685236"},{"product_id":"ri-245","title":"Delineation of drinking water source protection zones for Warm Spring, a public-water-supply spring, Iron County, Utah (RI-245)","description":"\u003cp\u003e\u003ci\u003eBy: C. E. Bishop\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThis study delineates drinking-water-source-protection zones for Warm Spring, which is used by the Paragonah Municipal Water System as a source of drinking water for the town of Paragonah. The spring is in Red Creek Canyon on the western edge of the Markagunt Plateau, in eastern Iron County. Red Creek is a substantial perennial stream draining the plateau. The climate of the area is semiarid to humid and average annual precipitation is about 14 inches; however, up to 35 inches can be received in the higher mountains.\u003c\/p\u003e \u003cp\u003eThis report describes the delineation of drinking-water-source-protection (DWSP) zones for Warm Spring, a public-water-supply spring in eastern Iron County, Utah. Warm Spring is about 4.1 miles east of the town of Paragonah, within the Markagunt Plateau. Much of the land surrounding the spring area is privately owned, but U.S. Bureau of Land Management, Dixie National Forest, and some state land is also found in the area. Grazing, recreation, and some residential development are the main land uses in the area. The town of Paragonah is a rural farming community that obtains part of its municipal drinking water from this spring. The Paragonah Canal Company owns the spring, and sells part of the water to the Paragonah Municipal Water System, which requested this delineation of DWSP zones. The scope of work included a literature search, review of water records, field reconnaissance, interpretation of data, delineation of the DWSP zones, and preparation of this report.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2001\u003cbr\u003ePages: 39 p.\u003cbr\u003eLocation: Iron County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203922243637,"sku":"RI245","price":4.6,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri245.png?v=1594685238"},{"product_id":"ri-246","title":"Delineation of drinking water source protection zones for Water System Canyon Spring, a public-water supply spring, Iron County, Utah (RI-246)","description":"\u003cp\u003e\u003ci\u003eBy: C. E. Bishop\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThis study delineates drinking-water-source-protection zones for Water System Canyon Spring, which is used by the Paragonah Municipal Water System as a source of drinking water for the town of Paragonah. The spring is in Water System Canyon, a tributary to Red Creek Canyon on the western edge of the Markagunt Plateau, eastern Iron County. Red Creek is a substantial perennial stream draining the plateau. The climate of the area is semiarid to humid and average annual precipitation is about 14 inches; however, up to 35 inches can be received in the higher mountains.\u003c\/p\u003e \u003cp\u003eThis report describes the delineation of drinking-water-source-protection (DWSP) zones for a public-water-supply spring in eastern Iron County, Utah. Water System Canyon Spring is about 2 miles east of the town of Paragonah, within the Markagunt Plateau. Much of the surrounding area is privately owned and used for cattle grazing. The town of Paragonah is a rural farming community that obtains part of its municipal drinking water from this spring, and requested this delineation of DWSP zones. The scope of work included a literature search, review of water records, field reconnaissance, interpretation of data, delineation of the DWSP zones, and preparation of this report.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2001\u003cbr\u003ePages: 35 p.\u003cbr\u003eLocation: Iron County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203922341941,"sku":"RI246","price":4.3,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri246.png?v=1594685239"},{"product_id":"ri-247","title":"Delineation of drinking water source protection zones for Covered Bridge Canyon public water supply well, Utah County, Utah (RI-247)","description":"\u003cp\u003e\u003ci\u003eBy: C. E. Bishop\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThe Covered Bridge Canyon Water Association operates a well to supply potable water for consumptive use for the subdivision of Covered Bridge Canyon. The well is in Pole Canyon, a tributary to Spanish Fork Canyon, in southern Utah County. To protect this well from contamination and to comply with Utah?s Drinking Water Source Protection Program, the subdivision is developing a Drinking Water Source Protection Plan. This report delineates the drinking water source protection zones for this well.\u003c\/p\u003e \u003cp\u003eThis report describes the delineation of drinking water source protection (DWSP) zones for a public-water-supply well in Spanish Fork Canyon, Utah County, Utah. The well is up the Right Fork of Pole Canyon at the southern end of Covered Bridge Canyon subdivision. Pole Canyon is a tributary to Spanish Fork Canyon near the southern end of the Wasatch Range. Spanish Fork Canyon is a narrow, elongated canyon formed by the Spanish Fork River. The mouth of Pole Canyon is about 2.5 miles east of the mouth of Spanish Fork Canyon. Covered Bridge Canyon subdivision is a rural bedroom community of the Wasatch Front, and most of its residents work along the Wasatch Front. The community uses the well as its public drinking-water source. Covered Bridge Canyon subdivision owns the well, and requested and assisted in this delineation of DWSP zones. The scope of work included a literature search, review of water-well logs, field reconnaissance, an aquifer test, interpretation of test data, delineation of the DWSP zones, and preparation of this report\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2001\u003cbr\u003ePages: 37 p.\u003cbr\u003eLocation: Utah County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203922407477,"sku":"RI247","price":4.3,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri247.png?v=1594685241"},{"product_id":"ri-249","title":"Delineation of drinking water source protection zones for the Monte Verde public water supply well, Morgan County, Utah (RI-249)","description":"\u003cp\u003e\u003ci\u003eC. E. Bishop\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThe Monte Verde public water system operates a single well to supply potable water for consumptive use by the Monte Verde subdivision in the community of Mountain Green. The well is in western Morgan Valley, near the head of Weber Canyon, northern Utah. To protect this well from contamination and to comply with Utah?s Drinking Water Source Protection Program, the subdivision is developing a drinking water source protection plan.\u003c\/p\u003e \u003cp\u003eThis report describes the delineation of drinking water source protection (DWSP) zones for a public-water-supply in western Morgan Valley, Morgan County, Utah. The well is within the Monte Verde subdivision, in western Mountain Green along Interstate 84 near the head of Weber Canyon. The Monte Verde water system owns the well, which provides drinking water to the subdivision, and requested and helped in this delineation of DWSP zones. The scope of work included a literature search, review of water-well logs, field reconnaissance, aquifer test, interpretation of test data, delineation of the DWSP zones, and preparation of this report.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2001\u003cbr\u003ePages: 19 p. + 18 p. appendix\u003cbr\u003eLocation: Morgan County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203922473013,"sku":"RI249","price":4.3,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri249.png?v=1594685243"},{"product_id":"ri-253","title":"Reconnaissance investigation of ground cracks along the western margin of Parowan Valley, Iron County, Utah (RI-253)","description":"\u003cp\u003e\n \u003ci\u003eBy: UGS Staff\u003c\/i\u003e\u003c\/p\u003e\n \u003cp\u003e\n Two out-of-print geologic and mineral assessment reports on Piute and Garfield Counties. Texts with plates are in one file for easy viewing; plates are a higher resolution and formatted for easy plotting are in separate files. Data contained in the reports must be viewed in light of their publication date and constraints of the period; some geologic units have been reclassified, some resource potentials have been drastically altered by changing economic\/availability changes, etc. The publications on this CD are listed below:\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eB-102\u003c\/b\u003e Mineral resource potential of Piute County, Utah and adjoining area, by E. Callaghan, 1973\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eB-107\u003c\/b\u003e Geology and mineral resources of Garfield County, Utah, by H. H. Doelling, 1975\u003c\/p\u003e\n \u003cp\u003e\n \u003cb\u003eOther Information:\u003c\/b\u003e\u003cbr\u003e\n Published: 2004\u003cbr\u003e\n Pages: 310 p.\u003cbr\u003e\n Plates: 17 pl.\u003cbr\u003e\n Location: Garfield County and Piute County\u003cbr\u003e\n \u003c\/p\u003e","brand":"Ground Water","offers":[{"title":"CD","offer_id":32205585711157,"sku":"RI253","price":14.95,"currency_code":"USD","in_stock":true}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri253_c3cec94b-6ea8-4f70-9062-a809cd8a8a62.png?v=1594756740"},{"product_id":"ri-262","title":"Delineation of drinking water source protection zones for the Day Star Adventist Academy public-water-supply well, Grand County, Utah (RI-262)","description":"\u003cp\u003e\u003ci\u003eBy: C. E. Bishop\u003c\/i\u003e\u003c\/p\u003e \u003cp\u003eThe Day Star Adventist Academy operates a well to supply potable water for consumptive use by its students, staff, and facilities. The well was drilled in the mid-1950s in lower Castle Valley, Grand County, Utah. To protect this well from contamination and to comply with Utah?s Drinking Water Source Protection Program, the Utah Division of Drinking Water, Department of Environmental Quality, requested that the Utah Geological Survey assist in developing the Day Star Adventist Academy Drinking Water Source Protection Plan. This report delineates the drinking water source protection zones for the Day Star Adventist Academy well.\u003c\/p\u003e \u003cp\u003e\u003cb\u003eOther Information:\u003c\/b\u003e \u003cbr\u003ePublished: 2008\u003cbr\u003ePages: 31 p.\u003cbr\u003eLocation: Grand County\u003cbr\u003eMedia Type: Paper Publication\u003c\/p\u003e","brand":"Utah Geological Survey","offers":[{"title":"Default Title","offer_id":32203923456053,"sku":"RI262","price":8.0,"currency_code":"USD","in_stock":false}],"thumbnail_url":"\/\/cdn.shopify.com\/s\/files\/1\/0254\/5582\/0853\/products\/ri262.png?v=1594685260"}],"url":"https:\/\/utahmapstore.com\/collections\/water.oembed?page=7","provider":"The Natural Resources Map \u0026 Bookstore","version":"1.0","type":"link"}