{"pageNumber":"4392","pageRowStart":"109775","pageSize":"25","recordCount":184885,"records":[{"id":60326,"text":"mf2138H - 1990 - Map showing the distribution of thorium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:28:21.963488","indexId":"mf2138H","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"H","title":"Map showing the distribution of thorium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle, Utah, shows the regional distribution of thorium in the less-than-0.180-mm (minus-80-mesh) fraction of stream-sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138H","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing the distribution of thorium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 41.84 x 24.31 inches, https://doi.org/10.3133/mf2138H.","productDescription":"1 Plate: 41.84 x 24.31 inches","costCenters":[],"links":[{"id":180199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138h.jpg"},{"id":283677,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-H/plate-1.pdf"},{"id":390779,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5749.htm"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a91c7","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263534,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263536,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":134,"text":"wsp2350 - 1990 - National water summary 1987: Hydrologic events and water supply and use","interactions":[],"lastModifiedDate":"2024-06-28T21:03:11.195151","indexId":"wsp2350","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2350","title":"National water summary 1987: Hydrologic events and water supply and use","docAbstract":"<p>Water use in the United States, as measured by freshwater withdrawals in 1985, averaged 338,000 Mgal/d (million gallons per day), which is enough water to cover the 48 conterminous States to a depth of about 2.4 inches. Only 92,300 Mgal/d, or 27.3 percent of the water withdrawn, was consumptive use and thus lost to immediate further use; the remainder of the withdrawals (72.7 percent) was return flow available for reuse a number of times as the water flowed to the sea. The 1985 freshwater withdrawals were much less than the average 30 inches of precipitation that falls on the conterminous States each year; consumptive use accounted for only 7 percent of the estimated annual runoff of 1,230,000 Mgal/d. Nonetheless, as the State summaries on water supply and use clearly show, water is not always available when and where it is needed. Balancing water demands with available water supplies constitutes one of the major resource allocation issues that will face the United States in the coming decade.</p><p>Of the 1985 freshwater withdrawals, 78.3 percent (265,000 Mgal/d) came from surface-water sources (streams and lakes), and 21.7 percent (73,300 Mgal/d) came from ground water. Surface water provided drinking water for about 47 percent of the Nation's total population. It was the source of 59.9 percent of the Nation's public-supply systems. For self-supplied withdrawals, surface water accounted for 1.6 percent of the domestic and commercial uses; 64.0 percent of the industrial and mining use; 99.4 percent of the thermoelectric generation withdrawals, mainly for cooling water; and 65.6 percent of the agricultural withdrawals. Eight States accounted for 43 percent of the surface-water use; California, Colorado, and Idaho used surface water primarily for irrigation, and Dlinois, Michigan, Ohio, Pennsylvania, and Texas used surface-water primarily for cooling condensers or reactors in thermoelectric plants.</p><p>Ground water provided drinking water for 53 percent of the Nation's total population and nearly all the rural population. It was the source of 40.1 percent of the public-supply systems withdrawals. For self-supplied withdrawals, ground water accounted for 11.3 percent of the domestic and commercial use, 17.3 percent of the industrial and mining withdrawals, less than 1 percent of the thermoelectric generation withdrawals, and 34.4 percent of the agricultural withdrawals (irrigation and livestock). Eight States Arizona, Arkansas, California, Florida, Idaho, Kansas, Nebraska, and Texas accounted for 66 percent of the ground water used. In each of those States, as in many other States, irrigation was the major use of ground water. Each offstream-use category described in the State summaries public supply, domestic and commercial, industrial and mining, thermoelectric power, and agriculture (irrigation and livestock) followed its own geographic pattern as described below.</p><p>Consumptive use of water effectively removes the water from immediate further use downstream of the withdrawal point. Of the total amount of consumptive water use in 1985, agricultural use accounted for about 82.5 percent. More than one-half (53 percent) of irrigation water is consumptively used by evapotranspiration or is incorporated into the crop. This is a good indication of the effect that irrigated agriculture can have in a river basin where irrigation is a major activity. The availability of return flows for reuse depends largely on where the water reenters the system. If the return flows are discharged to a stream, they usually can be reused; if they are discharged to a saltwater estuary, they are effectively lost to further use because of water-quality degradation just as if the water had been consumptively used. Similarly, water that recharges a highly transmissive aquifer can be available for reuse either through pumpage from a well or as discharge to a local stream. Thus, much of the water withdrawn for different uses can and does become available for further use although the quality might degrade with each additional use.</p><p>The allocation and the management of water resources are the responsibilities of the individual States and water institutions within the States. These institutions are evolving in response to the challenges of water management problems. As the individual State summaries indicate, recent State legislation deals with facilitating water transfers within the States as a means of reducing imbalances between water supplies and use, with emphasizing water conservation in times of drought and at places where groundwater depletion is a problem of long standing, and with reducing threats to public health and the environment from water pollution.</p><p>Most of the State summaries indicate the expectation that water use will continue to increase in the future and that water contamination will continue to be a major water concern. Both issues will require increasingly intensive water management in the future. Whether the water resources under management are considered to be fully appropriated or over appropriated, as in some Western States, or whether the resource could support additional development, as is the situation in most States, improved water-use information will play a key role in future water management efforts.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2350","usgsCitation":"United States Geological Survey, 1990, National water summary 1987: Hydrologic events and water supply and use: U.S. Geological Survey Water Supply Paper 2350, xii, 553 p., https://doi.org/10.3133/wsp2350.","productDescription":"xii, 553 p.","numberOfPages":"567","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science 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    \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.56640625,\n              18.771115062337024\n            ],\n            [\n              -154.68749999999997,\n              19.642587534013032\n            ],\n            [\n              -156.9287109375,\n              21.453068633086783\n            ],\n            [\n              -159.521484375,\n              22.43134015636061\n            ],\n            [\n              -160.5322265625,\n              21.983801417384697\n            ],\n            [\n              -159.9609375,\n              21.207458730482642\n            ],\n            [\n              -158.291015625,\n              20.92039691397189\n            ],\n            [\n              -156.97265625,\n              19.932041306115536\n            ],\n            [\n              -155.9619140625,\n              18.8543103618898\n            ],\n            [\n              -155.56640625,\n              18.771115062337024\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -67.060546875,\n              18.020527657852337\n            ],\n            [\n              -66.2255859375,\n              17.916022703877665\n            ],\n            [\n              -65.6103515625,\n              17.97873309555617\n            ],\n            [\n              -65.2587890625,\n              18.124970639386515\n            ],\n            [\n              -65.5224609375,\n              18.458768120015126\n            ],\n            [\n              -66.11572265625,\n              18.542116654448996\n            ],\n            [\n              -66.95068359374999,\n              18.60460138845525\n            ],\n            [\n              -67.34619140625,\n              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W.","contributorId":106861,"corporation":false,"usgs":true,"family":"Paulson","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":573848,"contributorType":{"id":3,"text":"Compilers"},"rank":3},{"text":"Moody, David W.","contributorId":84729,"corporation":false,"usgs":true,"family":"Moody","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":573849,"contributorType":{"id":3,"text":"Compilers"},"rank":4}],"authors":[{"text":"United States Geological Survey","contributorId":128013,"corporation":true,"usgs":false,"organization":"United States Geological Survey","id":905271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60321,"text":"mf2138D - 1990 - Map showing distribution of gold in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:20:07.170313","indexId":"mf2138D","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"D","title":"Map showing distribution of gold in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle, Utah, shows the regional distribution of gold in the less-than-0.180-mm (minus-80-mesh) fraction of stream sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the Selected References of this report.</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138D","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J.B., 1990, Map showing distribution of gold in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 41.29 x 24.79 inches, https://doi.org/10.3133/mf2138D.","productDescription":"1 Plate: 41.29 x 24.79 inches","costCenters":[],"links":[{"id":180138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138d.jpg"},{"id":283673,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-D/plate-1.pdf"},{"id":390773,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5745.htm"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660eef","contributors":{"authors":[{"text":"Miller, W. R.","contributorId":92239,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263521,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, J. M.","contributorId":8834,"corporation":false,"usgs":true,"family":"Motooka","given":"J.","middleInitial":"M.","affiliations":[],"preferred":false,"id":263519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, J. B.","contributorId":79462,"corporation":false,"usgs":true,"family":"McHugh","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":263520,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60322,"text":"mf2138E - 1990 - Map showing the distribution of molybdenum in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:22:35.435888","indexId":"mf2138E","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"E","title":"Map showing the distribution of molybdenum in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle, Utah, shows the regional distribution of lead in the less-than-0.180-mm (minus-80-mesh) fraction of stream sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138E","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing the distribution of molybdenum in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 41.31 x 23.35 inches, https://doi.org/10.3133/mf2138E.","productDescription":"1 Plate: 41.31 x 23.35 inches","costCenters":[],"links":[{"id":180139,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138e.jpg"},{"id":390776,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5746.htm"},{"id":283674,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-E/plate-1.pdf"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660f03","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263522,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263524,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60328,"text":"mf2138J - 1990 - Map showing the distribution of uranium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:31:49.5809","indexId":"mf2138J","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"J","title":"Map showing the distribution of uranium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle, Utah, shows the regional distribution of uranium in the less-than-0.180-mm (minus-80-mesh) fraction of stream-sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138J","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing the distribution of uranium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 41.42 x 24.39 inches, https://doi.org/10.3133/mf2138J.","productDescription":"1 Plate: 41.42 x 24.39 inches","costCenters":[],"links":[{"id":180201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138j.jpg"},{"id":390781,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5751.htm"},{"id":283679,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-J/plate-1.pdf"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db661017","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263540,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263542,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60327,"text":"mf2138I - 1990 - Map showing the distribution of tin in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:30:07.677904","indexId":"mf2138I","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"I","title":"Map showing the distribution of tin in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle, Utah, shows the regional distribution of tin in the less-than-0.180-mm (minus-80-mesh) fraction of stream-sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138I","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing the distribution of tin in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 41.05 x 24.15 inches, https://doi.org/10.3133/mf2138I.","productDescription":"1 Plate: 41.05 x 24.15 inches","costCenters":[],"links":[{"id":180200,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138i.jpg"},{"id":283678,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-I/plate-1.pdf"},{"id":390780,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5750.htm"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660fe5","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263538,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263537,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263539,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60317,"text":"mf2138A - 1990 - Map showing distribution of barium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:02:18.85479","indexId":"mf2138A","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"A","title":"Map showing distribution of barium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle shows the regional distribution of barium in the less-than-0.180-mm (minus-80-mesh) fraction of stream sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138A","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing distribution of barium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 41.85 x 24.52 inches, https://doi.org/10.3133/mf2138A.","productDescription":"1 Plate: 41.85 x 24.52 inches","costCenters":[],"links":[{"id":390769,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5742.htm"},{"id":283670,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-A/plate-1.pdf"},{"id":179827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138a.jpg"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660eaa","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263507,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263509,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60323,"text":"mf2138F - 1990 - Map showing the distribution of molybdenum in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:24:36.991604","indexId":"mf2138F","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"F","title":"Map showing the distribution of molybdenum in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle, Utah, shows the regional distribution of molybdenum in the less-than-0.180-mm (minus-80-mesh) fraction of stream-sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138F","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing the distribution of molybdenum in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 40.80 x 23.60 inches, https://doi.org/10.3133/mf2138F.","productDescription":"1 Plate: 40.80 x 23.60 inches","costCenters":[],"links":[{"id":180196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138f.jpg"},{"id":390777,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5747.htm"},{"id":283675,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-F/plate-1.pdf"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660f25","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263525,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263527,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60320,"text":"mf2138C - 1990 - Map showing distribution of copper in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:12:09.45464","indexId":"mf2138C","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"C","title":"Map showing distribution of copper in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle shows the regional distribution of copper in the less-than-0.180-mm (minus-80-mesh) fraction of stream sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138C","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J.B., 1990, Map showing distribution of copper in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 41.45 x 23.99 inches, https://doi.org/10.3133/mf2138C.","productDescription":"1 Plate: 41.45 x 23.99 inches","costCenters":[],"links":[{"id":180137,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138c.jpg"},{"id":390772,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5744.htm"},{"id":283672,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-C/plate-1.pdf"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114,\n              38\n            ],\n            [\n              -112,\n              38\n            ],\n            [\n              -112,\n              39\n            ],\n            [\n              -114,\n              39\n            ],\n            [\n              -114,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660ed3","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":511902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":511901,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John. B.","contributorId":116059,"corporation":false,"usgs":true,"family":"McHugh","given":"John.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":511903,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60324,"text":"mf2138G - 1990 - Map showing the distribution of silver in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:26:48.684931","indexId":"mf2138G","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"G","title":"Map showing the distribution of silver in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle, Utah, shows the regional distribution of silver in the less-than-0.180-mm (minus-80-mesh) fraction of stream-sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138G","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing the distribution of silver in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 40.36 x 24.79 inches, https://doi.org/10.3133/mf2138G.","productDescription":"1 Plate: 40.36 x 24.79 inches","costCenters":[],"links":[{"id":180197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138g.jpg"},{"id":283676,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-G/plate-1.pdf"},{"id":390778,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5748.htm"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660f8c","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263528,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263530,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60329,"text":"mf2138K - 1990 - Map showing the distribution of zinc in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:33:24.270453","indexId":"mf2138K","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"K","title":"Map showing the distribution of zinc in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle, Utah, shows the regional distribution of zinc in the less-than-0.180-mm (minus-80-mesh) fraction of stream-sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138K","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing the distribution of zinc in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 41.01 x 23.76 inches, https://doi.org/10.3133/mf2138K.","productDescription":"1 Plate: 41.01 x 23.76 inches","costCenters":[],"links":[{"id":179744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138k.jpg"},{"id":283680,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-K/plate-1.pdf"},{"id":390782,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5752.htm"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db661022","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263544,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263543,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263545,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60318,"text":"mf2138B - 1990 - Map showing distribution of bismuth and cadmium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-21T20:07:13.342115","indexId":"mf2138B","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2138","chapter":"B","title":"Map showing distribution of bismuth and cadmium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle shows the regional distribution of bismuth and cadimum in the less-than-0.180-mm (minus-80-mesh) fraction of stream sediments. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2138B","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing distribution of bismuth and cadmium in stream-sediment samples, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2138, 1 Plate: 41.45 x 23.93 inches, https://doi.org/10.3133/mf2138B.","productDescription":"1 Plate: 41.45 x 23.93 inches","costCenters":[],"links":[{"id":179828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2138b.jpg"},{"id":283671,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2138-B/plate-1.pdf"},{"id":390770,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5743.htm"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660eb0","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263510,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263512,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60325,"text":"mf2137B - 1990 - Map showing distribution of silver in the nonmagnetic fraction of heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-09-15T21:48:54.917916","indexId":"mf2137B","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2137","chapter":"B","title":"Map showing distribution of silver in the nonmagnetic fraction of heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah","docAbstract":"<p>This map of the Richfield 1° x 2° quadrangle, Utah, shows the regional distribution of silver in the nonmagnetic fraction of heavy-mineral concentrates of drainage-sediment samples. It is part of a folio of maps of the Richfield 1° x 2° quadrangle, Utah, prepared under the Conterminuous United States Mineral Assessment Program. Other published geochemical maps in this folio are listed in the references (this publication).</p>\n<br/>\n<p>The Richfield quadrangle is located in west-central Utah and includes the eastern part of the Pioche-Marysvale igneous and mineral belt, which extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 155 miles into central Utah. The western two-thirds of the Richfield quadrangle is part of the Basin and Range province, whereas the eastern third is part of the High Plateaus of Utah, a subprovince of the Colorado Plateau.</p>\n<br/>\n<p>Bedrock in the northern part of the Richfield quadrangle consists predominantly of Late Proterozoic and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks located in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrain into a series of north-trending fault blocks; the uplifted mountain areas were eroded to various degrees and the resulting debris was deposited in adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed as a result of igneous activity in the middle and late Cenozoic time. A more complete description of the geology and a mineral-resource appraisal of the Richfield quadrangle appears in Steven and Morris (1984 and 1987).</p>\n<br/>\n<p>The regional sampling program was designed to define broad geochemical patterns and trends that can be utilized along with geological and geophysical data to assess the mineral-resource potential for this quadrangle. Reconnaissance geochemical surveys are valuable tools in mineral exploration, especially when used in conjunction with data obtained from other earth science disciplines. Identifying specific exploration targets generally involves additional, more detailed investigations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/mf2137B","usgsCitation":"Miller, W.R., Motooka, J.M., and McHugh, J., 1990, Map showing distribution of silver in the nonmagnetic fraction of heavy-mineral concentrates, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2137, 1 Plate: 40.84 x 25.08 inches, https://doi.org/10.3133/mf2137B.","productDescription":"1 Plate: 40.84 x 25.08 inches","costCenters":[],"links":[{"id":180198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf2137b.jpg"},{"id":283666,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2137-B/plate-1.pdf"},{"id":389315,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5741.htm"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660f9b","contributors":{"authors":[{"text":"Miller, William R.","contributorId":53838,"corporation":false,"usgs":true,"family":"Miller","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Motooka, Jerry M.","contributorId":36611,"corporation":false,"usgs":true,"family":"Motooka","given":"Jerry","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":263531,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McHugh, John B.","contributorId":64651,"corporation":false,"usgs":true,"family":"McHugh","given":"John B.","affiliations":[],"preferred":false,"id":263533,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":59957,"text":"mf2131 - 1990 - Aeromagnetic anomaly map of the Paducah 1 degree by 2 degrees quadrangle, Missouri, Illinois, and Kentucky","interactions":[],"lastModifiedDate":"2025-06-02T16:08:39.043058","indexId":"mf2131","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2131","title":"Aeromagnetic anomaly map of the Paducah 1 degree by 2 degrees quadrangle, Missouri, Illinois, and Kentucky","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf2131","usgsCitation":"Kucks, R., 1990, Aeromagnetic anomaly map of the Paducah 1 degree by 2 degrees quadrangle, Missouri, Illinois, and Kentucky: U.S. Geological Survey Miscellaneous Field Studies Map 2131, 1 Plate: 41.93 x 24.65 inches, https://doi.org/10.3133/mf2131.","productDescription":"1 Plate: 41.93 x 24.65 inches","costCenters":[],"links":[{"id":489418,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5734.htm","linkFileType":{"id":5,"text":"html"}},{"id":364352,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/2131/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183737,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/2131/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Illinois, Kentucky, Missouri","city":"Paducah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90,37 ], [ -90,38 ], [ -88,38 ], [ -88,37 ], [ -90,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698489","contributors":{"authors":[{"text":"Kucks, R.P.","contributorId":53758,"corporation":false,"usgs":true,"family":"Kucks","given":"R.P.","affiliations":[],"preferred":false,"id":262899,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60455,"text":"mf2133 - 1990 - Geologic map and phosphate resources of the northeastern part of the Lower Valley Quadrangle, Caribou County, Idaho","interactions":[],"lastModifiedDate":"2012-02-10T00:10:39","indexId":"mf2133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2133","title":"Geologic map and phosphate resources of the northeastern part of the Lower Valley Quadrangle, Caribou County, Idaho","language":"ENGLISH","doi":"10.3133/mf2133","usgsCitation":"Oberlindacher, P., 1990, Geologic map and phosphate resources of the northeastern part of the Lower Valley Quadrangle, Caribou County, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 2133, 1 map ;sheet 125 x 71 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf2133.","productDescription":"1 map ;sheet 125 x 71 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105256,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5736.htm","linkFileType":{"id":5,"text":"html"},"description":"5736"},{"id":180146,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.43416666666667,42.784166666666664 ], [ -111.43416666666667,42.8675 ], [ -111.36749999999999,42.8675 ], [ -111.36749999999999,42.784166666666664 ], [ -111.43416666666667,42.784166666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4936","contributors":{"authors":[{"text":"Oberlindacher, Peter","contributorId":64717,"corporation":false,"usgs":true,"family":"Oberlindacher","given":"Peter","affiliations":[],"preferred":false,"id":263780,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16897,"text":"ofr90721 - 1990 - Anomalous chlorine in iron-rich strata; Yellowjacket formation, Lemhi County, Idaho: Analytical data and discussion","interactions":[],"lastModifiedDate":"2021-10-28T19:35:36.628535","indexId":"ofr90721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"90-721","title":"Anomalous chlorine in iron-rich strata; Yellowjacket formation, Lemhi County, Idaho: Analytical data and discussion","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr90721","usgsCitation":"Nash, J., Connor, J.J., Currey, K.J., and Papp, C.S., 1990, Anomalous chlorine in iron-rich strata; Yellowjacket formation, Lemhi County, Idaho: Analytical data and discussion: U.S. Geological Survey Open-File Report 90-721, 36 p., https://doi.org/10.3133/ofr90721.","productDescription":"36 p.","costCenters":[],"links":[{"id":391104,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18029.htm"},{"id":46007,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0721/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150206,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0721/report-thumb.jpg"}],"country":"United States","state":"Idaho","county":"Lemhi County","otherGeospatial":"Yellowjacket formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.5,\n              44.75\n            ],\n            [\n              -114,\n              44.75\n            ],\n            [\n              -114,\n              45.25\n            ],\n            [\n              -114.5,\n              45.25\n            ],\n            [\n              -114.5,\n              44.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b6a2","contributors":{"authors":[{"text":"Nash, J. T.","contributorId":31751,"corporation":false,"usgs":true,"family":"Nash","given":"J. T.","affiliations":[],"preferred":false,"id":174099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Connor, J. J.","contributorId":56224,"corporation":false,"usgs":true,"family":"Connor","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":174100,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Currey, K. J.","contributorId":8488,"corporation":false,"usgs":true,"family":"Currey","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":174098,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Papp, C. S.","contributorId":97923,"corporation":false,"usgs":true,"family":"Papp","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":174101,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":16898,"text":"ofr90593 - 1990 - Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota","interactions":[{"subject":{"id":16898,"text":"ofr90593 - 1990 - Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota","indexId":"ofr90593","publicationYear":"1990","noYear":false,"title":"Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":3,"text":"wsp2383 - 1992 - Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota","indexId":"wsp2383","publicationYear":"1992","noYear":false,"title":"Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota"},"id":1}],"supersededBy":{"id":3,"text":"wsp2383 - 1992 - Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota","indexId":"wsp2383","publicationYear":"1992","noYear":false,"title":"Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota"},"lastModifiedDate":"2021-02-23T12:43:19.197729","indexId":"ofr90593","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"90-593","title":"Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr90593","usgsCitation":"Wiche, G., Jenson, S., Baglio, J.V., and Domingue, J.O., 1990, Application of digital elevation models to delineate drainage areas and compute hydrologic characteristics for sites in the James River basin, North Dakota: U.S. Geological Survey Open-File Report 90-593, Report: vi, 39 p.; 6 Plates: 15.73 x 20.82 inches or smaller, https://doi.org/10.3133/ofr90593.","productDescription":"Report: vi, 39 p.; 6 Plates: 15.73 x 20.82 inches or smaller","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":150293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0593/report-thumb.jpg"},{"id":383553,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0593/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383554,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383555,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383556,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383558,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383559,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":383557,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0593/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","otherGeospatial":"James River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.0185546875,\n              45.89000815866184\n            ],\n            [\n              -96.6796875,\n              45.89000815866184\n            ],\n            [\n              -96.6796875,\n              48.951366470947725\n            ],\n            [\n              -104.0185546875,\n              48.951366470947725\n            ],\n            [\n              -104.0185546875,\n              45.89000815866184\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa52","contributors":{"authors":[{"text":"Wiche, G.J.","contributorId":90715,"corporation":false,"usgs":true,"family":"Wiche","given":"G.J.","affiliations":[],"preferred":false,"id":174103,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jenson, S.K.","contributorId":35291,"corporation":false,"usgs":true,"family":"Jenson","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":174102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Baglio, J. V. Jr.","contributorId":91831,"corporation":false,"usgs":true,"family":"Baglio","given":"J.","suffix":"Jr.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":174104,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Domingue, Julia O.","contributorId":91832,"corporation":false,"usgs":true,"family":"Domingue","given":"Julia","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":174105,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":16907,"text":"ofr90225 - 1990 - Assessment of regional earthquake hazards and risk along the Wasatch Front, Utah; Volume IV","interactions":[{"subject":{"id":16907,"text":"ofr90225 - 1990 - Assessment of regional earthquake hazards and risk along the Wasatch Front, Utah; Volume IV","indexId":"ofr90225","publicationYear":"1990","noYear":false,"title":"Assessment of regional earthquake hazards and risk along the Wasatch Front, Utah; Volume IV"},"predicate":"SUPERSEDED_BY","object":{"id":38372,"text":"pp1519 - 1993 - Applications of research from the U.S. Geological Survey program, assessment of regional earthquake hazards and risk along the Wasatch Front, Utah","indexId":"pp1519","publicationYear":"1993","noYear":false,"title":"Applications of research from the U.S. Geological Survey program, assessment of regional earthquake hazards and risk along the Wasatch Front, Utah"},"id":1}],"supersededBy":{"id":38372,"text":"pp1519 - 1993 - Applications of research from the U.S. Geological Survey program, assessment of regional earthquake hazards and risk along the Wasatch Front, Utah","indexId":"pp1519","publicationYear":"1993","noYear":false,"title":"Applications of research from the U.S. Geological Survey program, assessment of regional earthquake hazards and risk along the Wasatch Front, Utah"},"lastModifiedDate":"2021-03-17T00:31:28.45572","indexId":"ofr90225","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"90-225","title":"Assessment of regional earthquake hazards and risk along the Wasatch Front, Utah; Volume IV","docAbstract":"<div class=\"page\" data-page-number=\"10\" data-loaded=\"true\"></div><div class=\"page\" data-page-number=\"11\" data-loaded=\"true\"><div class=\"textLayer\"><span>Translation and transfer of complex scientific and engineering </span><span>studies to nontechnical users are necessary for their use in reducing </span><span>earthquake hazards in Utah. Three elements are needed for effective </span><span>translation: </span><span>likelihood of occurrence, location, and severity of </span><span>potential hazards. Several examples of translated information for Utah </span><span>are described and illustrated. Three elements are needed for effective </span><span>transfer to nontechnical users: delivery, assistance, and encouragement. </span><span>Numerous examples of transfer techniques in Utah are described and </span><span>illustrated. The importance of evaluating and revising earthquake-hazard </span><span>reduction programs and their components is emphasized. Over thirty </span><span>evaluations of various natural-hazard reduction programs and techniques </span><span>are introduced.</span></div><div class=\"textLayer\"><span><br data-mce-bogus=\"1\"></span></div><div class=\"textLayer\"><span>This report was prepared for research managers, funding sources, and evaluators of the Utah earthquake-hazard reduction program who are concerned about effectiveness. It provides an overview of the Utah program for those researchers, engineers, planners, and decisionmakers --public and private -- who are committed to reducing human casualties, property damage, and interruptions of socioeconomic systems.</span></div></div>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr90225","usgsCitation":"1990, Assessment of regional earthquake hazards and risk along the Wasatch Front, Utah; Volume IV: U.S. Geological Survey Open-File Report 90-225, 471 p., https://doi.org/10.3133/ofr90225.","productDescription":"471 p.","costCenters":[],"links":[{"id":384419,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0225/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149554,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0225/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Front","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.1044921875,\n              39.67337039176558\n            ],\n            [\n              -111.70898437499999,\n              39.67337039176558\n            ],\n            [\n              -111.70898437499999,\n              41.541477666790286\n            ],\n            [\n              -112.1044921875,\n              41.541477666790286\n            ],\n            [\n              -112.1044921875,\n              39.67337039176558\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671eb6","contributors":{"editors":[{"text":"Gori, P. 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,{"id":60537,"text":"mf2114 - 1990 - Preliminary surficial geologic map of the Salt Lake City segment and parts of adjacent segments of the Wasatch Fault zone, Davis, Salt Lake, and Utah counties, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:33","indexId":"mf2114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2114","title":"Preliminary surficial geologic map of the Salt Lake City segment and parts of adjacent segments of the Wasatch Fault zone, Davis, Salt Lake, and Utah counties, Utah","language":"ENGLISH","doi":"10.3133/mf2114","usgsCitation":"Personius, S., and Scott, W.E., 1990, Preliminary surficial geologic map of the Salt Lake City segment and parts of adjacent segments of the Wasatch Fault zone, Davis, Salt Lake, and Utah counties, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 2114, 1 map ;94 x 42 cm., on sheet 142 x 105 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf2114.","productDescription":"1 map ;94 x 42 cm., on sheet 142 x 105 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105244,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5714.htm","linkFileType":{"id":5,"text":"html"},"description":"5714"},{"id":180400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,40.45 ], [ -112,40.8675 ], [ -111.75,40.8675 ], [ -111.75,40.45 ], [ -112,40.45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669ac4","contributors":{"authors":[{"text":"Personius, S. F. 0000-0001-8347-7370","orcid":"https://orcid.org/0000-0001-8347-7370","contributorId":31408,"corporation":false,"usgs":true,"family":"Personius","given":"S. F.","affiliations":[],"preferred":false,"id":263934,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, W. E.","contributorId":22773,"corporation":false,"usgs":true,"family":"Scott","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":263933,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35019,"text":"b1812 - 1990 - Mineral resources of the Gospel-Hump Wilderness, Idaho County, Idaho","interactions":[],"lastModifiedDate":"2023-03-15T19:26:57.168041","indexId":"b1812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1812","title":"Mineral resources of the Gospel-Hump Wilderness, Idaho County, Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1812","usgsCitation":"Lund, K., and Esparza, L.E., 1990, Mineral resources of the Gospel-Hump Wilderness, Idaho County, Idaho: U.S. Geological Survey Bulletin 1812, Report: vi, 19 p.; 1 Plate: 41.50 x 34.50 inches, https://doi.org/10.3133/b1812.","productDescription":"Report: vi, 19 p.; 1 Plate: 41.50 x 34.50 inches","costCenters":[],"links":[{"id":414250,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21954.htm","linkFileType":{"id":5,"text":"html"}},{"id":62955,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1812/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62954,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1812/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164679,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1812/report-thumb.jpg"}],"country":"United States","state":"Idaho","county":"Idaho County","otherGeospatial":"Gospel-Hump Wilderness","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.033,\n              45.75\n            ],\n            [\n              -116.033,\n              45.417\n            ],\n            [\n              -115.5,\n              45.417\n            ],\n            [\n              -115.5,\n              45.75\n            ],\n            [\n              -116.033,\n              45.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2fb","contributors":{"authors":[{"text":"Lund, Karen 0000-0002-4249-3582 klund@usgs.gov","orcid":"https://orcid.org/0000-0002-4249-3582","contributorId":1235,"corporation":false,"usgs":true,"family":"Lund","given":"Karen","email":"klund@usgs.gov","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true},{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":213991,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Esparza, Leon E.","contributorId":70112,"corporation":false,"usgs":true,"family":"Esparza","given":"Leon","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":213992,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17067,"text":"ofr90354 - 1990 - Drilling and geohydrologic data for test hole USW UZ-1, Yucca Mountain, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr90354","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"90-354","title":"Drilling and geohydrologic data for test hole USW UZ-1, Yucca Mountain, Nye County, Nevada","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr90354","usgsCitation":"Whitfield, M., Hammermeister, D., Thordarson, W., and Warner, J., 1990, Drilling and geohydrologic data for test hole USW UZ-1, Yucca Mountain, Nye County, Nevada: U.S. Geological Survey Open-File Report 90-354, iv, 40 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90354.","productDescription":"iv, 40 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":148609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0354/report-thumb.jpg"},{"id":46198,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0354/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63558a","contributors":{"authors":[{"text":"Whitfield, M.S.","contributorId":69547,"corporation":false,"usgs":true,"family":"Whitfield","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":174806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hammermeister, D.P.","contributorId":27066,"corporation":false,"usgs":true,"family":"Hammermeister","given":"D.P.","affiliations":[],"preferred":false,"id":174805,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":174804,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Warner, J.B.","contributorId":87561,"corporation":false,"usgs":true,"family":"Warner","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":174807,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17068,"text":"ofr90304 - 1990 - Drilling records and logs for the Indus East area, coal resource exploration and assessment program, March 1987 to February 1988, southern Sind Province, Pakistan","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr90304","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"90-304","title":"Drilling records and logs for the Indus East area, coal resource exploration and assessment program, March 1987 to February 1988, southern Sind Province, Pakistan","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr90304","usgsCitation":"Thomas, R.E., Khan, R., Akhtar, S., Farriduddin, M., Fatmi, S., Idress, M., Jaffar, M., Salin, S., Jaffery, A., Khan, I., Khan, M., Khan, S., Khan, Z.M., Khan, M., Khan, M., Naimatullah, K., Rasheed, S., and Tariq, M., 1990, Drilling records and logs for the Indus East area, coal resource exploration and assessment program, March 1987 to February 1988, southern Sind Province, Pakistan: U.S. Geological Survey Open-File Report 90-304, 82 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90304.","productDescription":"82 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":148610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0304/report-thumb.jpg"},{"id":46199,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0304/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a3e4b07f02db49641f","contributors":{"authors":[{"text":"Thomas, R. 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