{"pageNumber":"5172","pageRowStart":"129275","pageSize":"25","recordCount":165485,"records":[{"id":70035508,"text":"70035508 - 1979 - b values and ω<sup>−γ</sup> seismic source models: Implications for tectonic stress variations along active crustal fault zones and the estimation of high-frequency strong ground motion","interactions":[],"lastModifiedDate":"2015-06-15T10:17:18","indexId":"70035508","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"b values and ω<sup>−γ</sup> seismic source models: Implications for tectonic stress variations along active crustal fault zones and the estimation of high-frequency strong ground motion","docAbstract":"<p><span>In this study the tectonic stress along active crustal fault zones is taken to be of the form&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0001.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umu6MIzikkO5ymj%0ANDlW1G0%2F%2BQ%3D%3D\" alt=\"inline image\" /></span></span><span>, where&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0002.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umuiedpqT79PPhK%0AOsNB85uCWA%3D%3D\" alt=\"inline image\" /></span></span><span>&nbsp;is the average tectonic stress at depth&nbsp;</span><i>y</i><span>&nbsp;and &Delta;&sigma;</span><span><i>p</i></span><span>(</span><i>x, y</i><span>) is a seismologically observable, essentially random function of both fault plane coordinates; the stress differences arising in the course of crustal faulting are derived from &Delta;&sigma;</span><i><span>p</span></i><span>(</span><i>x, y</i><span>). Empirically known frequency of occurrence statistics, moment-magnitude relationships, and the constancy of earthquake stress drops may be used to infer that the number of earthquakes&nbsp;</span><i>N</i><span>&nbsp;of dimension &ge;</span><i>r</i><span>&nbsp;is of the form&nbsp;</span><i>N</i><span>&nbsp;&sim; 1/</span><i>r</i><span>2</span><span>&nbsp;and that the spectral composition of &Delta;&sigma;</span><i><span>p</span></i><span>(</span><i>x, y</i><span>) is of the form&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0003.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umusANOiMJ6380O%0AqOQppeWKzQ%3D%3D\" alt=\"inline image\" /></span></span><span>, where&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0004.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umuGlAzWdjz2K3Q%0AG1y6nb%2F%2FjA%3D%3D\" alt=\"inline image\" /></span></span><span>&nbsp;is the two-dimensional Fourier transform of &Delta;&sigma;</span><i><span>p</span></i><span>(</span><i>x, y</i><span>) expressed in radial wave number&nbsp;</span><i>k</i><span>. The &gamma; = 2 model of the far-field shear wave displacement spectrum is consistent with the spectral composition&nbsp;</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0005.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umunzw%2FWHTH5Y0K%0AFHvdyv0N%2Fw%3D%3D\" alt=\"inline image\" /></span></span><span>, provided that the number of contributions to the spectral representation of the radiated field at frequency &fnof; goes as (</span><i>k</i><span>/</span><i>k</i><span>0</span><span>)</span><span>2</span><span>, consistent with the quasi-static frequency of occurrence relation&nbsp;</span><i>N</i><span>&nbsp;&sim; 1/</span><i>r</i><span>2</span><span>;</span><i>k</i><span>0</span><span>&nbsp;is a reference wave number associated with the reciprocal source dimension. Separately, a variety of seismologic observations suggests that the &gamma; = 2 model is the one generally, although certainly not always, applicable to the high-frequency spectral decay of the far-field radiation of earthquakes. In this framework, then,&nbsp;</span><i>b</i><span>&nbsp;values near 1, the general validity of the &gamma; = 2 model, and the constancy of earthquake stress drops independent of size are all related to the average spectral composition of</span><span class=\"math-equation-construct\" data-equation-construct=\"true\"><span class=\"math-equation-image\" data-equation-image=\"true\"><img class=\"inlineGraphic\" src=\"http://api.onlinelibrary.wiley.com/asset/v1/doi/10.1029%2FJB084iB05p02235/asset/equation%2Fjgrb2891-math-0006.gif?l=Cgg2pVVsCMwLOww28sbn56fxTbx6GilFBMCsUrZMoRcYP%2B9NZI%2F0t%2B3p7VO59umuaobXgGTYfS%2Fs%0AAwMugfb30g%3D%3D\" alt=\"inline image\" /></span></span><span>. Should one of these change as a result of premonitory effects leading to failure, as has been specifically proposed for&nbsp;</span><i>b</i><span>&nbsp;values, it seems likely that one or all of the other characteristics will change as well from their normative values. Irrespective of these associations, the far-field, high-frequency shear radiation for the &gamma; = 2 model in the presence of anelastic attenuation may be interpreted as band-limited, finite duration white noise in acceleration. Its rms value,&nbsp;</span><i>a</i><span>rms</span><span>, is given by the expression&nbsp;</span><i>a</i><span>rms</span><span>&nbsp;= 0.85[2</span><span>1/2</span><span>(2&pi;)</span><span>2</span><span>/106] (&Delta;&sigma;/&rho;</span><i>R</i><span>)(&fnof;</span><span>max</span><span>/&fnof;</span><span>0</span><span>)</span><span>1/2</span><span>, where &Delta;&sigma; is the earthquake stress drop, &rho; is density,&nbsp;</span><i>R</i><span>&nbsp;is hypocentral distance, &fnof;</span><span>0</span><span>&nbsp;is the spectral corner frequency, and &fnof;</span><span>max</span><span>&nbsp;is determined by&nbsp;</span><i>R</i><span>&nbsp;and specific attenuation 1/</span><i>Q</i><span>. For several reasons, one of which is that it may be estimated in the absence of empirically defined ground motion correlations,&nbsp;</span><i>a</i><span>rms</span><span>&nbsp;holds considerable promise as a measure of high-frequency strong ground motion for engineering purposes.</span></p>","language":"English","publisher":"AGU Publications","doi":"10.1029/JB084iB05p02235","issn":"01480227","usgsCitation":"Hanks, T.C., 1979, b values and ω<sup>−γ</sup> seismic source models: Implications for tectonic stress variations along active crustal fault zones and the estimation of high-frequency strong ground motion, v. 84, no. B5, p. 2235-2242, https://doi.org/10.1029/JB084iB05p02235.","productDescription":"8 p.","startPage":"2235","endPage":"2242","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":244197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":216334,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1029/JB084iB05p02235"}],"volume":"84","issue":"B5","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"5059ef79e4b0c8380cd4a26e","contributors":{"authors":[{"text":"Hanks, Thomas C. 0000-0003-0928-0056 thanks@usgs.gov","orcid":"https://orcid.org/0000-0003-0928-0056","contributorId":3065,"corporation":false,"usgs":true,"family":"Hanks","given":"Thomas","email":"thanks@usgs.gov","middleInitial":"C.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":450977,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70164466,"text":"70164466 - 1979 - International Seismological Centre","interactions":[],"lastModifiedDate":"2016-03-22T11:40:12","indexId":"70164466","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"International Seismological Centre","docAbstract":"<p>The International Seismological Centre had its origins when the British seismologist Professor John Milne returned to England from Japan in 1895 to retire at Shide on the Isle of Eight. In cooperation with the British Association for the Advancement of Science, Milne had set up a number of seismographic stations around the world and, while Tokyo, had published a <i>Catalogue of 8,33 Earthquakes Recorded in Japan, 1885-1892.&nbsp;</i></p>","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Spall, H., and Hughes, A., 1979, International Seismological Centre: Earthquake Information Bulletin (USGS), v. 11, no. 5, p. 165-169.","productDescription":"5 p.","startPage":"165","endPage":"169","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316627,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b5d624e4b0cc79998172f3","contributors":{"authors":[{"text":"Spall, H.","contributorId":99290,"corporation":false,"usgs":true,"family":"Spall","given":"H.","affiliations":[],"preferred":false,"id":597520,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, A.","contributorId":156346,"corporation":false,"usgs":false,"family":"Hughes","given":"A.","affiliations":[],"preferred":false,"id":597521,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28123,"text":"wri78117 - 1979 - Geohydrology of Brooks, Lowndes, and western Echols Counties, Georgia","interactions":[],"lastModifiedDate":"2023-04-25T18:40:40.905324","indexId":"wri78117","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"78-117","title":"Geohydrology of Brooks, Lowndes, and western Echols Counties, Georgia","docAbstract":"The principal artesian aquifer, a limestone of Eocene to Miocene age, is the main source of water supply for Brooks, Lowndes, and western Echols Counties in south Georgia. Pumpage of about 22 million gallons perday from this prolific aquifer has not posed any problems regarding declining water levels or depletion of the reservoir. However, water-quality problems do occur in the Valdosta area. Seepage-run measurements indicate that the Withlacoochee River north of Valdosta contributes an average of 112 cubic feet per second of water to caverns and sinkholes that recharge the aquifer. Wells near the recharge area withdraw relatively unfiltered water with iron concentration and color intensity exceeding standards for drinking water. South of Valdosta, water from the aquifer contains as much as 3.0 milligrams per liter of hydrogen sulfide, rendering the water unfit for drinking. Water high in sulfate concentration occurs below 550 feet in the lower part of the aquifer in Valdosta, and is assumed to be present at that depth throughout the study area. Generally, sufficient quantities of freshwater can be obtained without drilling to this depth.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Doraville, GA","doi":"10.3133/wri78117","collaboration":"Prepared in cooperation with the Georgia Department of Natural Resources","usgsCitation":"Krause, R., 1979, Geohydrology of Brooks, Lowndes, and western Echols Counties, Georgia: U.S. Geological Survey Water-Resources Investigations Report 78-117, Report: vi, 48 p.; 8 Plates: 20.81  14.96 inches or smaller; Table, https://doi.org/10.3133/wri78117.","productDescription":"Report: vi, 48 p.; 8 Plates: 20.81  14.96 inches or smaller; Table","numberOfPages":"64","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":279053,"rank":11,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri78117.jpg"},{"id":416316,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35217.htm","linkFileType":{"id":5,"text":"html"}},{"id":277893,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0117/plate-5.PDF","linkFileType":{"id":1,"text":"pdf"}},{"id":277897,"rank":3,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/wri/1978/0117/table-2.PDF","linkFileType":{"id":1,"text":"pdf"}},{"id":277896,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0117/plate-8.PDF","linkFileType":{"id":1,"text":"pdf"}},{"id":277888,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0117/report.pdf"},{"id":277894,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0117/plate-6.PDF","linkFileType":{"id":1,"text":"pdf"}},{"id":277895,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0117/plate-7.PDF","linkFileType":{"id":1,"text":"pdf"}},{"id":277889,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0117/plate-1.PDF","linkFileType":{"id":1,"text":"pdf"}},{"id":277890,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0117/plate-2.PDF","linkFileType":{"id":1,"text":"pdf"}},{"id":277891,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0117/plate-3.PDF","linkFileType":{"id":1,"text":"pdf"}},{"id":277892,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0117/plate-4.PDF","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","county":"Brooks County, Echols County, Lowndes 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,{"id":9039,"text":"ofr791051 - 1979 - Lignite drilling during 1978 in western North Dakota: Adams, Billings, Bowman, Burke, Golden Valley, Hettinger, McKenzie, McLean, and Slope Counties","interactions":[],"lastModifiedDate":"2023-03-29T20:31:42.195458","indexId":"ofr791051","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1979","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":"79-1051","title":"Lignite drilling during 1978 in western North Dakota: Adams, Billings, Bowman, Burke, Golden Valley, Hettinger, McKenzie, McLean, and Slope Counties","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr791051","usgsCitation":"Water Resources Division, U.S. Geological Survey, and North Dakota Geological Survey, 1979, Lignite drilling during 1978 in western North Dakota: Adams, Billings, Bowman, Burke, Golden Valley, Hettinger, McKenzie, McLean, and Slope Counties: U.S. Geological Survey Open-File Report 79-1051, i, 519 p., https://doi.org/10.3133/ofr791051.","productDescription":"i, 519 p.","costCenters":[],"links":[{"id":414920,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71653.htm","linkFileType":{"id":5,"text":"html"}},{"id":36677,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/1051/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142855,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/1051/report-thumb.jpg"}],"country":"United States","state":"North Dakota","county":"Adams County, Billings County, Bowman County, Burke County, Golden Valley County, Hettinger County, McKenzie County, McLean County, Slope County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -101,\n              49\n            ],\n            [\n              -104.045,\n              49\n            ],\n            [\n              -104.045,\n              45.945\n            ],\n            [\n              -101,\n              45.945\n            ],\n            [\n              -101,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a52ea","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528884,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"North Dakota Geological Survey","contributorId":128250,"corporation":true,"usgs":false,"organization":"North Dakota Geological Survey","id":528885,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56409,"text":"wdrMDDE771 - 1978 - Water resources data for Maryland and Delaware, water year 1977","interactions":[],"lastModifiedDate":"2021-01-22T19:29:44.483116","indexId":"wdrMDDE771","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-77-1","displayTitle":"Water Resources Data for Maryland and Delaware, Water Year 1977","title":"Water resources data for Maryland and Delaware, water year 1977","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE771","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Water resources data for Maryland and Delaware, water year 1977: U.S. Geological Survey Water Data Report 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 \"}}]}","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f42fb","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70196004,"text":"70196004 - 1978 - Numerical simulation of steady state three-dimensional groundwater flow near lakes","interactions":[],"lastModifiedDate":"2018-03-13T11:48:38","indexId":"70196004","displayToPublicDate":"2018-03-13T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Numerical simulation of steady state three-dimensional groundwater flow near lakes","docAbstract":"<p><span>Numerical simulation of three-dimensional groundwater flow near lakes shows that the continuity of the boundary encompassing the local groundwater flow system associated with a lake is the key to understanding the interaction of a lake with the groundwater system. The continuity of the boundary can be determined by the presence of a stagnation zone coinciding with the side of the lake nearest the downgradient side of the groundwater system. For most settings modeled in this study the stagnation zone underlies the lakeshore, and it generally follows its curvature. The length of the stagnation zone is controlled by the geometry of the lake's drainage basin divide on the side of the lake nearest the downgradient side of the groundwater system. In the case of lakes that lose water to the groundwater system, three-dimensional modeling also allows for estimating the area of lake bed through which outseepage takes place. Analysis of the effects of size and lateral and vertical distribution of aquifers within the groundwater system on the outseepage from lakes shows that the position of the center point of the aquifer relative to the littoral zone on the side of the lake nearest the downgradient side of the groundwater system is a critical factor. If the center point is downslope from this part of the littoral zone, the local flow system boundary tends to be weak or outseepage occurs. If the center point is upslope from this littoral zone, the stagnation zone tends to be stronger (to have a higher head in relation to lake level), and outseepage is unlikely to occur.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/WR014i002p00245","usgsCitation":"Winter, T.C., 1978, Numerical simulation of steady state three-dimensional groundwater flow near lakes: Water Resources Research, v. 14, no. 2, p. 245-254, https://doi.org/10.1029/WR014i002p00245.","productDescription":"10 p.","startPage":"245","endPage":"254","costCenters":[{"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":352436,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5aff4d62e4b0da30c1bfdc22","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":730884,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012490,"text":"70012490 - 1978 - Age of the last major scabland flood of the Columbia Plateau in eastern Washington","interactions":[],"lastModifiedDate":"2025-07-14T15:18:37.546213","indexId":"70012490","displayToPublicDate":"2017-01-20T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"Age of the last major scabland flood of the Columbia Plateau in eastern Washington","docAbstract":"<p><span>Pumice layers of set S from Mount St. Helens can be correlated with certain ash beds associated with young flood deposits of the channeled scabland. The correlation points to an age of about 13,000&nbsp;</span><span class=\"sup\">14</span><span>C yr B.P. for the last major flood to have crossed the scabland. Until recently, the last major episode of flooding was thought to be closer to 20,000 yr B.P., an age inferred chiefly from the relation of the flood to glacial events of the northern Rocky Mountains. Several investigations within the last few years have suggested that the last major flood occurred well after 20,000 yr B.P. Tentative correlations of ash beds of the scabland with set S pumice layers, the relations of flood and glacial events along the northwestern margin of the Columbia Plateau, and a radiocarbon date from the Snake River drainage southeast of the plateau all indicate an age much younger than 20,000 yr. The postulated age of about 13,000 yr B.P. is further supported by a radiocarbon date in the Columbia River valley downstream from the scabland tract. Basal peat from a bog on the Portland delta of Bretz, which is a downvalley deposit of the last major scabland flood, has been dated as 13,080 ± 300 yr B.P. (W-3404).</span></p>","language":"English","publisher":"Cambridge University Press","doi":"10.1016/0033-5894(78)90099-6","issn":"00335894","usgsCitation":"Mullineaux, D.R., Wilcox, R., Ebaugh, W., Fryxell, R., and Rubin, M., 1978, Age of the last major scabland flood of the Columbia Plateau in eastern Washington: Quaternary Research, v. 10, no. 2, p. 171-180, https://doi.org/10.1016/0033-5894(78)90099-6.","productDescription":"10 p.","startPage":"171","endPage":"180","costCenters":[],"links":[{"id":222207,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Columbia Plateau, eastern Washington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.61626687535127,\n              48.094362272240716\n            ],\n            [\n              -119.61626687535127,\n              46.99900541842095\n            ],\n            [\n              -117.10617240070286,\n              46.99900541842095\n            ],\n            [\n              -117.10617240070286,\n              48.094362272240716\n            ],\n            [\n              -119.61626687535127,\n              48.094362272240716\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"10","issue":"2","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059e8f2e4b0c8380cd47fd0","contributors":{"authors":[{"text":"Mullineaux, D. R.","contributorId":64248,"corporation":false,"usgs":true,"family":"Mullineaux","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilcox, R.E.","contributorId":107348,"corporation":false,"usgs":true,"family":"Wilcox","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":363744,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ebaugh, W.F.","contributorId":89521,"corporation":false,"usgs":true,"family":"Ebaugh","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":363743,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fryxell, R.","contributorId":28369,"corporation":false,"usgs":true,"family":"Fryxell","given":"R.","email":"","affiliations":[],"preferred":false,"id":363740,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":363742,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70180027,"text":"70180027 - 1978 - Developing a state water plan: Ground-water conditions in Utah, spring of 1978","interactions":[],"lastModifiedDate":"2017-01-23T13:04:03","indexId":"70180027","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"17","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1978","docAbstract":"<p>This report is the fifteenth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.</p><p>This report, like the others (see References, p. 13), contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing water-table configuration are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>This report includes individual discussions of selected major areas of ground-water withdrawal in the State for the calendar year 1977. Water-level fluctuations, however, are described for the period spring 1977 to spring 1978. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Gates, J., Jibson, W., Herbert, L.R., Mower, R.W., Razem, A., Cordova, R., Jensen, V., ReMillard, M.D., Emett, D.C., Sumison, C., Carroll, P., DeGrand, M., and Sandberg, G.W., 1978, Developing a state water plan: Ground-water conditions in Utah, spring of 1978: Cooperative Investigations Report 17, vi, 63 p.","productDescription":"vi, 63 p.","numberOfPages":"70","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333719,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333718,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-187"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5887248be4b08aa8f945abf8","contributors":{"authors":[{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":659879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jibson, W.N.","contributorId":27928,"corporation":false,"usgs":true,"family":"Jibson","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":659880,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659881,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659882,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Razem, A. C.","contributorId":34924,"corporation":false,"usgs":true,"family":"Razem","given":"A. C.","affiliations":[],"preferred":false,"id":659883,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659884,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":659885,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"ReMillard, M. D.","contributorId":38645,"corporation":false,"usgs":true,"family":"ReMillard","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":659886,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Emett, D. C.","contributorId":21213,"corporation":false,"usgs":true,"family":"Emett","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":659887,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sumison, C.T.","contributorId":39057,"corporation":false,"usgs":true,"family":"Sumison","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":659888,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Carroll, P.A.","contributorId":178594,"corporation":false,"usgs":false,"family":"Carroll","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":659889,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"DeGrand, M.J.","contributorId":178595,"corporation":false,"usgs":false,"family":"DeGrand","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":659890,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659891,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70180237,"text":"70180237 - 1978 - New ages on intrusive rocks and altered zones in the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1977</i>","interactions":[{"subject":{"id":70180237,"text":"70180237 - 1978 - New ages on intrusive rocks and altered zones in the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1977</i>","indexId":"70180237","publicationYear":"1978","noYear":false,"title":"New ages on intrusive rocks and altered zones in the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1977</i>"},"predicate":"IS_PART_OF","object":{"id":4432,"text":"cir772B - 1978 - The United States Geological Survey in Alaska: Accomplishments during 1977","indexId":"cir772B","publicationYear":"1978","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1977"},"id":1}],"isPartOf":{"id":4432,"text":"cir772B - 1978 - The United States Geological Survey in Alaska: Accomplishments during 1977","indexId":"cir772B","publicationYear":"1978","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1977"},"lastModifiedDate":"2017-01-27T10:53:20","indexId":"70180237","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"772-B","title":"New ages on intrusive rocks and altered zones in the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1977</i>","docAbstract":"<p>Preliminary potassium-argon dating of intrusive rocks and altered zones in the Chignik and Sutwik Island quadrangles of the Alaska Peninsula seems to indicate at least three and possibly four Tertiary ages of alteration and mineralization.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The United States Geological Survey in Alaska: Accomplishments during 1977 (Circular 772-B)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70180237","usgsCitation":"Wilson, F.H., Detterman, R.L., and Silberman, M.L., 1978, New ages on intrusive rocks and altered zones in the Alaska Peninsula: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1977</i>: U.S. Geological Survey Circular 772-B, 3 p., https://doi.org/10.3133/70180237.","productDescription":"3 p.","startPage":"B63","endPage":"B65","numberOfPages":"3","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":334024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":334023,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0772b/report.pdf#page=70","text":"Start page in Larger Work"}],"country":"United States","state":"Alaska","otherGeospatial":"Alaska Peninsula","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7c7e4b0ba3b075e065a","contributors":{"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":660853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Detterman, Robert L.","contributorId":71526,"corporation":false,"usgs":true,"family":"Detterman","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":660854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Silberman, Miles L.","contributorId":23947,"corporation":false,"usgs":true,"family":"Silberman","given":"Miles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":660855,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176380,"text":"70176380 - 1978 - Earthquake history of Washington","interactions":[],"lastModifiedDate":"2019-11-14T12:59:38","indexId":"70176380","displayToPublicDate":"2016-03-16T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Earthquake history of Washington","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"U.S. Geological Survey, 1978, Earthquake history of Washington: Earthquake Information Bulletin (USGS), v. 10, no. 1, p. 28-33.","productDescription":"6 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,{"id":70176379,"text":"70176379 - 1978 - Behavior of different segments of the San Andreas fault","interactions":[],"lastModifiedDate":"2019-11-14T12:54:33","indexId":"70176379","displayToPublicDate":"2016-03-16T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"Behavior of different segments of the San Andreas fault","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"U.S. Geological Survey, 1978, Behavior of different segments of the San Andreas fault: Earthquake Information Bulletin (USGS), v. 10, no. 4, p. 126-130.","productDescription":"5 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,{"id":70157467,"text":"70157467 - 1978 - Ground-water resources and geology of Columbia County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:35:15","indexId":"70157467","displayToPublicDate":"2015-04-06T09:15:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"37","title":"Ground-water resources and geology of Columbia County, Wisconsin","docAbstract":"<p>The increasing need for water of good Quality in Columbia County, caused by a steadily increasing population, can be met from the sand-and-gravel and sandstone aquifers. As much as 15 gallons per minute can be obtained from wells almost everywhere. Yields of more than 1,000 gallons per minute are available from drift where it contains a sufficient thickness of saturated sand and gravel (the sand-and-gravel aquifer). The sandstone aquifer underlies nearly all the county except for areas west of the Wisconsin River and northwest of Pardeeville. It is more than 700 feet thick in the south-central part. The sandstone aquifer includes all bedrock younger than Precambrian age and is capable of yielding more than 1,000 gallons per minute to wells in about three-fourths of the county. It is the principal source of municipal-water supply.</p>\n<p>The chemical quality of water from the two aquifers is similar. It is very hard (mean concentration of about 300 milligrams per liter as calcium carbonate), and much of it contains excessive amounts of iron and manganese. Concentrations of dissolved solids and chloride are higher in areas underlain by bedrock of Ordovician age than elsewhere.</p>\n<p>About 5.0 million gallons per day of water was pumped in the county in 1974, 90 percent from the sandstone aQuifer. About 45 percent of the total water pumped was for industrial and commercial purposes~ 37 percent was for residential use, 16 percent for municipal use, and 2 percent for irrigation.</p>","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","usgsCitation":"Harr, C., Trotta, L.C., and Borman, R.G., 1978, Ground-water resources and geology of Columbia County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 37, vi, 30 p.","productDescription":"vi, 30 p.","numberOfPages":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308478,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350391,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic37/"}],"country":"United States","state":"Wisconsin","county":"Columbia County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.2453,43.643],[-89.127,43.6436],[-89.1271,43.6318],[-89.007,43.6332],[-89.0063,43.548],[-89.0044,43.4616],[-89.0038,43.3737],[-89.0088,43.3738],[-89.0094,43.286],[-89.1271,43.2827],[-89.246,43.2834],[-89.3624,43.2832],[-89.3617,43.2954],[-89.4819,43.2942],[-89.6008,43.2932],[-89.7209,43.2935],[-89.7235,43.2935],[-89.7292,43.3026],[-89.7279,43.3108],[-89.7254,43.3153],[-89.7229,43.3181],[-89.7185,43.3195],[-89.7129,43.3226],[-89.7078,43.3277],[-89.7028,43.3345],[-89.6909,43.3495],[-89.684,43.3573],[-89.6783,43.3586],[-89.6708,43.3582],[-89.6613,43.3577],[-89.6456,43.36],[-89.6311,43.3646],[-89.6166,43.371],[-89.6009,43.3806],[-89.6004,43.4688],[-89.5999,43.5544],[-89.6075,43.5603],[-89.6138,43.5626],[-89.6277,43.5617],[-89.6359,43.5603],[-89.6511,43.5621],[-89.658,43.5634],[-89.6643,43.5657],[-89.6707,43.5666],[-89.6783,43.5671],[-89.6877,43.5634],[-89.6934,43.5616],[-89.6991,43.562],[-89.706,43.5648],[-89.7187,43.5652],[-89.7288,43.5661],[-89.7351,43.5693],[-89.7364,43.5743],[-89.7326,43.5793],[-89.7288,43.5829],[-89.7244,43.587],[-89.7188,43.5929],[-89.7207,43.597],[-89.727,43.5979],[-89.7428,43.597],[-89.751,43.5997],[-89.7567,43.6029],[-89.7662,43.6029],[-89.7738,43.6092],[-89.7763,43.6161],[-89.7808,43.6215],[-89.7802,43.6274],[-89.7789,43.6343],[-89.784,43.6388],[-89.7866,43.6411],[-89.779,43.6411],[-89.7195,43.643],[-89.6,43.6427],[-89.4837,43.6423],[-89.3648,43.6427],[-89.2453,43.643]]]},\"properties\":{\"name\":\"Columbia\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ec7e4b058f706e512d2","contributors":{"authors":[{"text":"Harr, C.A.","contributorId":106920,"corporation":false,"usgs":true,"family":"Harr","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":573249,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trotta, L. C.","contributorId":63410,"corporation":false,"usgs":true,"family":"Trotta","given":"L.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573250,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573251,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047582,"text":"70047582 - 1978 - Geologic framework of lower Cook Inlet, Alaska","interactions":[{"subject":{"id":8823,"text":"ofr77136 - 1977 - Geologic framework of lower Cook Inlet, Alaska","indexId":"ofr77136","publicationYear":"1977","noYear":false,"title":"Geologic framework of lower Cook Inlet, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70047582,"text":"70047582 - 1978 - Geologic framework of lower Cook Inlet, Alaska","indexId":"70047582","publicationYear":"1978","noYear":false,"title":"Geologic framework of lower Cook Inlet, Alaska"},"id":1}],"lastModifiedDate":"2023-01-25T15:48:58.755919","indexId":"70047582","displayToPublicDate":"2013-01-01T15:27:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geologic framework of lower Cook Inlet, Alaska","docAbstract":"<p>Three seismic reflectors are present throughout the lower Cook Inlet basin and can be correlated with onshore geologic features. The reflections come from unconformities at the base of the Tertiary sequence, at the base of Upper Cretaceous rocks, and near the base of Upper Jurassic strata.</p><p>A contour map of the deepest horizon shows that Mesozoic rocks are formed into a northeast-trending syncline. Along the southeast flank of the basin, the northwest-dipping Mesozoic rocks are truncated at the base of Tertiary rocks.</p><p>The Augustine-Seldovia arch trends across the basin axis between Augustine Island and Seldovia. Tertiary rocks thin onto the arch from the north and south. Numerous anticlines, smaller in structural relief and breadth than the Augustine-Seldovia arch, trend northeast parallel with the basin, and intersect the arch at oblique angles.</p><p>The stratigraphic record shows four cycles of sedimentation and tectonism that are bounded by three regional unconformities in lower Cook Inlet and by four thrust faults and the modern Benioff zone in flysch rocks of the Kenai Peninsula and the Gulf of Alaska. The four cycles of sedimentation are, from oldest to youngest, the early Mesozoic, late Mesozoic, early Cenozoic, and late Cenozoic.</p><p>Data on organic geochemistry of the rocks from one well suggest that Middle Jurassic strata may be a source of hydrocarbons. Seismic data show that structural traps are formed by northeast-trending anticlines and by structures formed at the intersections of these anticlines with the transbasin arch. Stratigraphic traps may be formed beneath the unconformity at the base of Tertiary strata and beneath unconformities within Mesozoic strata.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/C1EA4851-16C9-11D7-8645000102C1865D","usgsCitation":"Fisher, M.A., and Magoon, L.B., 1978, Geologic framework of lower Cook Inlet, Alaska: American Association of Petroleum Geologists Bulletin, v. 62, no. 3, p. 373-402, https://doi.org/10.1306/C1EA4851-16C9-11D7-8645000102C1865D.","productDescription":"10 p.","startPage":"373","endPage":"402","costCenters":[],"links":[{"id":276552,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Cook Inlet","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -154.5,58.0 ], [ -154.5,60.0 ], [ -151.5,60.0 ], [ -151.5,58.0 ], [ -154.5,58.0 ] ] ] } } ] }","volume":"62","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03ebe4b0026c2bc11b5b","contributors":{"authors":[{"text":"Fisher, Michael A. mfisher@usgs.gov","contributorId":1991,"corporation":false,"usgs":true,"family":"Fisher","given":"Michael","email":"mfisher@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":482453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Magoon, Leslie B. lmagoon@usgs.gov","contributorId":2383,"corporation":false,"usgs":true,"family":"Magoon","given":"Leslie","email":"lmagoon@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":true,"id":482452,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047767,"text":"70047767 - 1978 - In situ analysis of coal using a <sup>252</sup>CF-Ge(Li) borehole sonde","interactions":[{"subject":{"id":9037,"text":"ofr77162 - 1977 - In situ analysis of coal using a <sup>252</sup>CF-Ge(Li) borehole sonde","indexId":"ofr77162","publicationYear":"1977","noYear":false,"title":"In situ analysis of coal using a <sup>252</sup>CF-Ge(Li) borehole sonde"},"predicate":"SUPERSEDED_BY","object":{"id":70047767,"text":"70047767 - 1978 - In situ analysis of coal using a <sup>252</sup>CF-Ge(Li) borehole sonde","indexId":"70047767","publicationYear":"1978","noYear":false,"title":"In situ analysis of coal using a <sup>252</sup>CF-Ge(Li) borehole sonde"},"id":1}],"lastModifiedDate":"2013-08-22T13:41:10","indexId":"70047767","displayToPublicDate":"2013-01-01T13:39:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2755,"text":"Mining Engineering","active":true,"publicationSubtype":{"id":10}},"title":"In situ analysis of coal using a <sup>252</sup>CF-Ge(Li) borehole sonde","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Mining Engineering","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"SME","usgsCitation":"Senftle, F.E., Tanner, A., Philbin, P.W., Boynton, G.R., and Schram, C., 1978, In situ analysis of coal using a <sup>252</sup>CF-Ge(Li) borehole sonde: Mining Engineering, v. 30, no. 6, p. 666-674.","productDescription":"9 p.","startPage":"666","endPage":"674","costCenters":[],"links":[{"id":276903,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"30","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521732e5e4b043bae8d2e5ec","contributors":{"authors":[{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tanner, A.B.","contributorId":44155,"corporation":false,"usgs":true,"family":"Tanner","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":482930,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Philbin, P. W.","contributorId":25915,"corporation":false,"usgs":true,"family":"Philbin","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482929,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482933,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schram, C.W.","contributorId":77154,"corporation":false,"usgs":true,"family":"Schram","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":482932,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70047449,"text":"70047449 - 1978 - Geology and groundwater resources of northern Berks County, Pennsylvania","interactions":[{"subject":{"id":49316,"text":"ofr77407 - 1977 - Ground-water resources of northern Berks County, Pennsylvania","indexId":"ofr77407","publicationYear":"1977","noYear":false,"title":"Ground-water resources of northern Berks County, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047449,"text":"70047449 - 1978 - Geology and groundwater resources of northern Berks County, Pennsylvania","indexId":"70047449","publicationYear":"1978","noYear":false,"title":"Geology and groundwater resources of northern Berks County, Pennsylvania"},"id":1}],"lastModifiedDate":"2013-08-06T12:59:08","indexId":"70047449","displayToPublicDate":"2013-01-01T12:48:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":143,"text":"Water Resource Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"44","title":"Geology and groundwater resources of northern Berks County, Pennsylvania","docAbstract":"The area of investigation comprises approximately 540 square miles and lies entirely within the Great Valley section of the Valley and Ridge physiographic province. The Great Valley is underlain chiefly by carbon ate rocks in the south and by shale and graywacke in the north. Most of the carbonate rocks are included in two great nappes that differ appreciably in stratigraphic detail.","language":"English","publisher":"Pennsylvania Geological Survey","publisherLocation":"Harrisburg, PA","collaboration":"Prepared by the United States Geological Survey, Water Resources Division, in cooperation with the Pennsylvania Geological Survey","usgsCitation":"Wood, C.R., and MacLachlan, D.B., 1978, Geology and groundwater resources of northern Berks County, Pennsylvania: Water Resource Report 44, vi, 91 p.; Maps: 2 Sheets.","productDescription":"vi, 91 p.; Maps: 2 Sheets","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276122,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047449.PNG"},{"id":276120,"type":{"id":11,"text":"Document"},"url":"https://www.dcnr.state.pa.us/cs/groups/public/documents/document/dcnr_016329.zip"}],"country":"United States","state":"Pennsylvania","county":"Berks County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.4412,40.1371 ], [ -76.4412,40.6761 ], [ -75.5279,40.6761 ], [ -75.5279,40.1371 ], [ -76.4412,40.1371 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae4e4b0e21cafa49c4f","contributors":{"authors":[{"text":"Wood, Charles R.","contributorId":30259,"corporation":false,"usgs":true,"family":"Wood","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacLachlan, David B.","contributorId":54281,"corporation":false,"usgs":true,"family":"MacLachlan","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":482061,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047716,"text":"70047716 - 1978 - Guidebook to Rio Grande rift in New Mexico","interactions":[{"subject":{"id":44053,"text":"ofr77750 - 1977 - Tectonic map of the Rio Grande Rift system in Colorado","indexId":"ofr77750","publicationYear":"1977","noYear":false,"title":"Tectonic map of the Rio Grande Rift system in Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70047716,"text":"70047716 - 1978 - Guidebook to Rio Grande rift in New Mexico","indexId":"70047716","publicationYear":"1978","noYear":false,"title":"Guidebook to Rio Grande rift in New Mexico"},"id":1}],"lastModifiedDate":"2018-01-08T15:56:32","indexId":"70047716","displayToPublicDate":"2013-01-01T12:29:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5594,"text":"New Mexico Bureau of Geology and Mineral Resources Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"163","title":"Guidebook to Rio Grande rift in New Mexico","docAbstract":"Discusses the details of geologic features along the rift zone. Included are short papers on topics relative to the overall region. These papers and the road logs are of special interest to any one pursuing further study of the rift. This book is a comprehensive guide to the middle and late Cenozoic geology of the Rio Grande region of Colorado and New Mexico. Though initially used on field trips for the International Symposium on Tectonics and Magmatism of the Rio Grande rift, the guidebook will be useful to anyone interested in the Cenozoic history of the 600-mi-long area extending from central Colorado to El Paso, Texas.","language":"English","publisher":"New Mexico Bureau of Geology and Mineral Resources","publisherLocation":"Socorro, NM","usgsCitation":"1978, Guidebook to Rio Grande rift in New Mexico (Reprinted 1981): New Mexico Bureau of Geology and Mineral Resources Circular 163, 241 p.; Maps: 2 Sheets.","productDescription":"241 p.; Maps: 2 Sheets","costCenters":[],"links":[{"id":276802,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047716.jpg"},{"id":276801,"type":{"id":15,"text":"Index Page"},"url":"https://geoinfo.nmt.edu/publications/monographs/circulars/163/"}],"country":"United States","state":"New Mexico","otherGeospatial":"Rio Grande Rift","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.05,31.33 ], [ -109.05,37.0 ], [ -103.0,37.0 ], [ -103.0,31.33 ], [ -109.05,31.33 ] ] ] } } ] }","edition":"Reprinted 1981","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52148fe3e4b06d85e08fb4ff","contributors":{"compilers":[{"text":"Hawley, J.W.","contributorId":51320,"corporation":false,"usgs":true,"family":"Hawley","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":725459,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":70047786,"text":"70047786 - 1978 - Ground-water resources in the Libby area, northwestern Montana","interactions":[{"subject":{"id":7967,"text":"ofr77397 - 1977 - Ground-water resources in the Libby area, northwestern Montana","indexId":"ofr77397","publicationYear":"1977","noYear":false,"title":"Ground-water resources in the Libby area, northwestern Montana"},"predicate":"SUPERSEDED_BY","object":{"id":70047786,"text":"70047786 - 1978 - Ground-water resources in the Libby area, northwestern Montana","indexId":"70047786","publicationYear":"1978","noYear":false,"title":"Ground-water resources in the Libby area, northwestern Montana"},"id":1}],"lastModifiedDate":"2013-08-23T10:38:10","indexId":"70047786","displayToPublicDate":"2013-01-01T10:33:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"106","title":"Ground-water resources in the Libby area, northwestern Montana","language":"English","publisher":"Montana Bureau of Mines and Geology","publisherLocation":"Butte, MT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Montana Bureau of Mines and Geology","usgsCitation":"Boettcher, A.J., and Wilke, K., 1978, Ground-water resources in the Libby area, northwestern Montana: Bulletin 106, iv, 36 p.; Maps: 2 Sheets.","productDescription":"iv, 36 p.; Maps: 2 Sheets","costCenters":[],"links":[{"id":276944,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":276943,"type":{"id":15,"text":"Index Page"},"url":"https://www.mbmg.mtech.edu/mbmgcat/public/ListCitation.asp?pub_id=10107&"}],"country":"United States","state":"Montana","city":"Libby","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.647171,48.32196 ], [ -115.647171,48.444719 ], [ -115.454961,48.444719 ], [ -115.454961,48.32196 ], [ -115.647171,48.32196 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52188467e4b0e27b926cc6aa","contributors":{"authors":[{"text":"Boettcher, A. J.","contributorId":25965,"corporation":false,"usgs":true,"family":"Boettcher","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":482964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilke, K.R.","contributorId":60687,"corporation":false,"usgs":true,"family":"Wilke","given":"K.R.","email":"","affiliations":[],"preferred":false,"id":482965,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043963,"text":"70043963 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah","interactions":[{"subject":{"id":7977,"text":"ofr78312 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab and Millard counties, Utah","indexId":"ofr78312","publicationYear":"1978","noYear":false,"title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab and Millard counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043963,"text":"70043963 - 1978 - Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah","indexId":"70043963","publicationYear":"1978","noYear":false,"title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:08:28","indexId":"70043963","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"64","title":"Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah","docAbstract":"The Fish Springs Flat area includes about 590 square miles (1,530 square kilometers) in western Utah. Total annual precipitation on the area averages about 7 inches (180 millimeters) and totals about 232,000 acre-feet (286 cubic hectometers). Fish Springs Wash is the major drainage in the area; and, along with numerous smaller washes, it flows only in direct response to precipitation. Runoff from the area is estimated to be about 2,000 acre-feet (2.5 cubic hectometers) per year.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with The Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Bolke, E., and Sumsion, C.T., 1978, Hydrologic reconnaissance of the Fish Springs Flat area, Tooele, Juab, and Millard Counties, Utah: Technical Publication 64, iv, 30 p.","productDescription":"iv, 30 p.","numberOfPages":"36","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268165,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009q.pdf"},{"id":331953,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-560"}],"country":"United States","state":"Utah","county":"Juab County, Millard County, Tooele County","otherGeospatial":"Fish Springs Flat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.65905761718749,\n              39.41497702499074\n            ],\n            [\n              -113.65905761718749,\n              40.000267972646796\n            ],\n            [\n              -112.9779052734375,\n              40.000267972646796\n            ],\n            [\n              -112.9779052734375,\n              39.41497702499074\n            ],\n            [\n              -113.65905761718749,\n              39.41497702499074\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512b44a5e4b0523e997a814a","contributors":{"authors":[{"text":"Bolke, E.L.","contributorId":52151,"corporation":false,"usgs":true,"family":"Bolke","given":"E.L.","affiliations":[],"preferred":false,"id":474556,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":474555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043779,"text":"70043779 - 1978 - Ground-water conditions in the Navajo Sandstone in the central Virgin River basin, Utah","interactions":[{"subject":{"id":8429,"text":"ofr77582 - 1977 - Ground-water conditions in the Navajo Sandstone in the central Virgin River Basin, Utah","indexId":"ofr77582","publicationYear":"1977","noYear":false,"title":"Ground-water conditions in the Navajo Sandstone in the central Virgin River Basin, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043779,"text":"70043779 - 1978 - Ground-water conditions in the Navajo Sandstone in the central Virgin River basin, Utah","indexId":"70043779","publicationYear":"1978","noYear":false,"title":"Ground-water conditions in the Navajo Sandstone in the central Virgin River basin, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:34:51","indexId":"70043779","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"61","title":"Ground-water conditions in the Navajo Sandstone in the central Virgin River basin, Utah","docAbstract":"The central Virgin River basin, Utah, includes about 1,000 square miles (2,600 square kilometers) in the drainage basin of the Virgin River downstream from the Hurricane Cliffs. The Navajo Sandstone of Late Triassic(?) and Jurassic age crops out in 234 square miles (606 square kilometers) of the basin and underlies younger rocks in about 450 square miles (1,200 square kilometers) of the basin.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Cordova, R., 1978, Ground-water conditions in the Navajo Sandstone in the central Virgin River basin, Utah: Technical Publication 61, vi, 66 p.","productDescription":"vi, 66 p.","numberOfPages":"72","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267805,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267804,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009n.pdf"},{"id":331967,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-500"}],"country":"United States","state":"Utah","county":"Washington County","otherGeospatial":"Virgin River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.1,\n              37\n            ],\n            [\n              -113.1,\n              37.45\n            ],\n            [\n              -114.1 ,\n              37.45\n            ],\n            [\n              -114.1,\n              37\n            ],\n            [\n              -113.1,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad36e4b0b6328103b419","contributors":{"authors":[{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":474228,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043282,"text":"70043282 - 1978 - Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","interactions":[{"subject":{"id":10425,"text":"ofr7815 - 1977 - Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","indexId":"ofr7815","publicationYear":"1977","noYear":false,"title":"Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water"},"predicate":"SUPERSEDED_BY","object":{"id":70043282,"text":"70043282 - 1978 - Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","indexId":"70043282","publicationYear":"1978","noYear":false,"title":"Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water"},"id":1}],"lastModifiedDate":"2016-12-12T14:46:33","indexId":"70043282","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"63","title":"Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water","docAbstract":"Beaver Valley includes 534 square miles in southwestern Utah, in the Basin and Range physiographic province. The project area consists of a valley plain underlain by unconsolidated to partly consolidated material. The valley plain is bounded by mountains that are composed of partly consolidated to consolidated rocks of Pennsylvanian through Tertiary age except for local thin unconsolidated surficial deposits of Quaternary age. The water needs of the valley are supplied mainly by four streams rising in the Tushar Mountains along the eastern side of the valley and by wells in the unconsolidated to partly consolidated materials of the valley plain. The objectives of this study were (1) to measure and analyze the discharge/recharges rates and (2) to measure and analyze the total amount of water in storage in the ground-water reservoirs.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Mower, R.W., 1978, Hydrology of the Beaver Valley area, Beaver County, Utah, with emphasis on ground water: Technical Publication 63, vi, 90 p.","productDescription":"vi, 90 p.","numberOfPages":"100","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267168,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331971,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009p.pdf"},{"id":331970,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-530"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Beaver Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.9,\n              38.15\n            ],\n            [\n              -112.9,\n              38.5\n            ],\n            [\n              -112.4,\n              38.5\n            ],\n            [\n              -112.4,\n              38.15\n            ],\n            [\n              -112.9,\n              38.15\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177e04e4b0893acf3fffc6","contributors":{"authors":[{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":473280,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043933,"text":"70043933 - 1978 - Water resources of the northern Uinta Basin area, Utah and Colorado, with special emphasis on ground water supply","interactions":[{"subject":{"id":9560,"text":"ofr77730 - 1977 - Water resources of the northern Uinta Basin area, Utah and Colorado, with special emphasis on ground-water supply","indexId":"ofr77730","publicationYear":"1977","noYear":false,"title":"Water resources of the northern Uinta Basin area, Utah and Colorado, with special emphasis on ground-water supply"},"predicate":"SUPERSEDED_BY","object":{"id":70043933,"text":"70043933 - 1978 - Water resources of the northern Uinta Basin area, Utah and Colorado, with special emphasis on ground water supply","indexId":"70043933","publicationYear":"1978","noYear":false,"title":"Water resources of the northern Uinta Basin area, Utah and Colorado, with special emphasis on ground water supply"},"id":1}],"lastModifiedDate":"2016-12-12T14:38:35","indexId":"70043933","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"62","title":"Water resources of the northern Uinta Basin area, Utah and Colorado, with special emphasis on ground water supply","docAbstract":"The northern Uinta Basin area covers about 5,200 square miles (13,470 square kilometers) in northeastern Utah and northwestern Colorado. Much of the lowlands are arid to semiarid, but the highest parts of the Uinta Mountains have a humid climate. During 1941-70, the average annual precipitation ranged from less than 8 inches (203 millimeters) in the lowest part of the area at the Green River to more than 38 inches (965 millimeters) in the high west-central Uinta Mountains.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Hood, J.W., and Fields, F., 1978, Water resources of the northern Uinta Basin area, Utah and Colorado, with special emphasis on ground water supply: Technical Publication 62, vi, 75 p.","productDescription":"vi, 75 p.","numberOfPages":"87","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268036,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331968,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-520"},{"id":268047,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009o.pdf"}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Uinta Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.796875,\n              39.39375459224348\n            ],\n            [\n              -111.796875,\n              41.0130657870063\n            ],\n            [\n              -108.43505859374999,\n              41.0130657870063\n            ],\n            [\n              -108.43505859374999,\n              39.39375459224348\n            ],\n            [\n              -111.796875,\n              39.39375459224348\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5129f34be4b04edf7e93f979","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fields, F.K.","contributorId":90826,"corporation":false,"usgs":true,"family":"Fields","given":"F.K.","email":"","affiliations":[],"preferred":false,"id":474511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043728,"text":"70043728 - 1978 - Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah","interactions":[{"subject":{"id":7913,"text":"ofr77312 - 1977 - Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah","indexId":"ofr77312","publicationYear":"1977","noYear":false,"title":"Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043728,"text":"70043728 - 1978 - Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah","indexId":"70043728","publicationYear":"1978","noYear":false,"title":"Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah"},"id":1}],"lastModifiedDate":"2016-12-09T11:24:07","indexId":"70043728","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"60","title":"Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah","docAbstract":"The Parowan-Cedar City drainage basin, Iron County, Utah, includes about 1,100 mi<sup>2</sup> (square miles)(2,800 km<sup>2</sup> [square kilometers])--520 mi<sup>2</sup> (1,300 km<sup>2</sup>) in the Parowan basin and 580 mi<sup>2</sup> (1,500 km<sup>2</sup>) in the Cedar City basin. Parowan and Cedar City Valleys are structural depressions formed by northeast-trending faults. Parowan Valley is essentially a closed basin, whereas Cedar City Valley is drained by two gaps in the mountains bordering the west side of the valley, and a small part of Cedar City Valley is drained at a gap at the south end. Water flowing into the basin from the highlands to the east is used to irrigate lands near Cedar City, Parowan, Paragonah, and Summit. The surface-water outflow from the basin is negligible.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Bjorklund, L., Sunsion, C., and Sandberg, G.W., 1978, Ground-water resources of the Parowan-Cedar City drainage basin, Iron County, Utah: Technical Publication 60, viii, 93 p.","productDescription":"viii, 93 p.","numberOfPages":"110","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267716,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331779,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-480"},{"id":267715,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009m.pdf"}],"country":"United States","state":"Utah","county":"Iron County","otherGeospatial":"Parowan-Cedar City Drainage Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0539,37.4744 ], [ -114.0539,38.151 ], [ -112.4696,38.151 ], [ -112.4696,37.4744 ], [ -114.0539,37.4744 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad3ee4b0b6328103b42e","contributors":{"authors":[{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":474176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sunsion, C.T.","contributorId":99846,"corporation":false,"usgs":true,"family":"Sunsion","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":474178,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474177,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70046281,"text":"70046281 - 1978 - Geologic map of Nevada","interactions":[{"subject":{"id":41166,"text":"ofr7468 - 1974 - Preliminary geologic map of Nevada","indexId":"ofr7468","publicationYear":"1974","noYear":false,"title":"Preliminary geologic map of Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":70046281,"text":"70046281 - 1978 - Geologic map of Nevada","indexId":"70046281","publicationYear":"1978","noYear":false,"title":"Geologic map of Nevada"},"id":1}],"lastModifiedDate":"2013-06-04T15:48:31","indexId":"70046281","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Geologic map of Nevada","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70046281","collaboration":"Prepared by the United States Geological Survey in cooperation with the Nevada Bureau of Mines and Geology","usgsCitation":"Stewart, J., and Carlson, J., 1978, Geologic map of Nevada, Map: 1 Sheet, https://doi.org/10.3133/70046281.","productDescription":"Map: 1 Sheet","costCenters":[],"links":[{"id":273277,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.01,35.0 ], [ -120.01,42.0 ], [ -114.0,42.0 ], [ -114.0,35.0 ], [ -120.01,35.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51af0c69e4b08a3322c2c2ce","contributors":{"authors":[{"text":"Stewart, John H.","contributorId":14383,"corporation":false,"usgs":true,"family":"Stewart","given":"John H.","affiliations":[],"preferred":false,"id":479368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlson, John E.","contributorId":19996,"corporation":false,"usgs":false,"family":"Carlson","given":"John E.","affiliations":[{"id":7260,"text":"Pennsylvania State University","active":true,"usgs":false}],"preferred":false,"id":479369,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043280,"text":"70043280 - 1978 - Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah","interactions":[{"subject":{"id":11325,"text":"ofr77263 - 1977 - Hydrologic reconnaissance of the Dugway Valley-Government Creek area, west-central Utah","indexId":"ofr77263","publicationYear":"1977","noYear":false,"title":"Hydrologic reconnaissance of the Dugway Valley-Government Creek area, west-central Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043280,"text":"70043280 - 1978 - Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah","indexId":"70043280","publicationYear":"1978","noYear":false,"title":"Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah"},"id":1}],"lastModifiedDate":"2016-12-12T14:26:49","indexId":"70043280","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"59","title":"Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah","docAbstract":"The Dugway Valley-Government Creek area covers about 890 square miles (2,300 square kilometers) in west-central Utah. Total annual precipitation on the area averages about 380,000 acre-feet (470 cubic hectometers). Most streams are ephemeral except for a few in their upper reaches--all are ephemeral below the altitude of about 6,000 feet (1,830 meters). Surface-water development and use in the area are insignificant.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Stephens, J.C., and Sumsion, C.T., 1978, Hydrologic reconnaissance of the Dugway Valley-Government Creek area, West-Central Utah: Technical Publication 59, vi, 42 p.","productDescription":"vi, 42 p.","numberOfPages":"50","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331963,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-450"},{"id":267165,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009l.pdf"}],"datum":"United States","country":"United States","state":"Utah","county":"Juab County, Tooele County","otherGeospatial":"Dugway Valley-Government Creek Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.27316284179688,\n              40.226072729473884\n            ],\n            [\n              -113.31573486328124,\n              40.15683567591309\n            ],\n            [\n              -113.27041625976562,\n              40.11799004890473\n            ],\n            [\n              -113.26766967773438,\n              40.065460682065535\n            ],\n            [\n              -113.22509765625,\n              40.01078714046552\n            ],\n            [\n              -113.16055297851562,\n              39.985538414809746\n            ],\n            [\n              -113.07952880859375,\n              39.93711893299021\n            ],\n            [\n              -113.06854248046875,\n              39.839122664473194\n            ],\n            [\n              -113.148193359375,\n              39.818029898770206\n            ],\n            [\n              -113.16329956054688,\n              39.74837783143156\n            ],\n            [\n              -113.11248779296874,\n              39.688167045890395\n            ],\n            [\n              -113.06304931640625,\n              39.675484393594814\n            ],\n            [\n              -112.78701782226562,\n              39.7642140375156\n            ],\n            [\n              -112.78152465820312,\n              39.842286020743394\n            ],\n            [\n              -112.73483276367188,\n              39.883396390093075\n            ],\n            [\n              -112.59887695312499,\n              39.88128876522249\n            ],\n            [\n              -112.664794921875,\n              39.9602803542957\n            ],\n            [\n              -112.68402099609374,\n              40.03182061333687\n            ],\n            [\n              -112.70736694335936,\n              40.127441029049486\n            ],\n            [\n              -112.78701782226562,\n              40.2313150803688\n            ],\n            [\n              -112.97241210937499,\n              40.364334716590214\n            ],\n            [\n              -113.17428588867188,\n              40.286859051369504\n            ],\n            [\n              -113.27316284179688,\n              40.226072729473884\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177dffe4b0893acf3fffb5","contributors":{"authors":[{"text":"Stephens, Jerry C.","contributorId":81493,"corporation":false,"usgs":true,"family":"Stephens","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":473278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":473277,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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