{"pageNumber":"2562","pageRowStart":"64025","pageSize":"25","recordCount":68807,"records":[{"id":1001811,"text":"1001811 - 1964 - Numbered nasal discs for waterfowl","interactions":[],"lastModifiedDate":"2025-02-05T16:56:06.547022","indexId":"1001811","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Numbered nasal discs for waterfowl","docAbstract":"<p>Numbered nasal discs were successfully used in studies requiring large numbers of individually marked waterfowl. The procedure for constructing these discs is outlined. Blue-winged teal (<i>Anas discors</i>) with 5/8-inch discs, and canvasback (<i>Aythya valisineria</i>) and redhead (<i>A. americana</i>) with 3/4-inch discs can be individually identified up to 50 and 80 yards, respectively, with a gunstock-mounted, 20-power spotting scope. The particular value of these markers is their durability, the number of combinations possible, and the apparent absence of behavioral or mortality influence among such species as the blue-winged teal.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3798783","usgsCitation":"Bartonek, J., and Dane, C., 1964, Numbered nasal discs for waterfowl: Journal of Wildlife Management, v. 28, no. 4, p. 688-692, https://doi.org/10.2307/3798783.","productDescription":"5 p.","startPage":"688","endPage":"692","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":130488,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696878","contributors":{"authors":[{"text":"Bartonek, James C.","contributorId":38085,"corporation":false,"usgs":true,"family":"Bartonek","given":"James C.","affiliations":[],"preferred":false,"id":311836,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dane, C.W.","contributorId":95003,"corporation":false,"usgs":true,"family":"Dane","given":"C.W.","email":"","affiliations":[],"preferred":false,"id":311837,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1003310,"text":"1003310 - 1964 - Toxicological effects of herbicides on the fish environment Part 1","interactions":[],"lastModifiedDate":"2012-02-02T00:11:24","indexId":"1003310","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3727,"text":"Water and Sewage Works","active":true,"publicationSubtype":{"id":10}},"title":"Toxicological effects of herbicides on the fish environment Part 1","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water and Sewage Works","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Walker, C., 1964, Toxicological effects of herbicides on the fish environment Part 1: Water and Sewage Works, v. 111, no. 3, p. 113-116.","productDescription":"pp. 113-116","startPage":"113","endPage":"116","numberOfPages":"4","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":179277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627f0f","contributors":{"authors":[{"text":"Walker, C.R.","contributorId":69097,"corporation":false,"usgs":true,"family":"Walker","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":313096,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1003311,"text":"1003311 - 1964 - Toxicological effects of herbicides on the fish environment Part 2","interactions":[],"lastModifiedDate":"2012-02-02T00:11:25","indexId":"1003311","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3727,"text":"Water and Sewage Works","active":true,"publicationSubtype":{"id":10}},"title":"Toxicological effects of herbicides on the fish environment Part 2","docAbstract":"Abstract has not been submitted","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Water and Sewage Works","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Walker, C., 1964, Toxicological effects of herbicides on the fish environment Part 2: Water and Sewage Works, v. 111, no. 4, p. 173-175.","productDescription":"pp. 173-175","startPage":"173","endPage":"175","numberOfPages":"3","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":179527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"111","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627f14","contributors":{"authors":[{"text":"Walker, C.R.","contributorId":69097,"corporation":false,"usgs":true,"family":"Walker","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":313097,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190800,"text":"70190800 - 1964 - Selected hydrologic data, upper Sevier River basin, Utah","interactions":[],"lastModifiedDate":"2017-09-14T12:50:52","indexId":"70190800","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"8","title":"Selected hydrologic data, upper Sevier River basin, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during 1961-63 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of ground-water conditions in the upper Sevier River basin, in parts of Garfield, Iron, Kane, Piute, and Sevier Counties, Utah. The interpretive material will be published in a companion report by Carl H. Carpenter, Gerald B. Robinson, Jr., and Louis J. Bjorklund.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells and springs as shown in the tables. From table 1 he can find information on wells, including depth, diameter, water level, yield, drawdown, use of water, temperature of water, and depth of perforations. Table 2 gives information on springs such as yield, use of water, temperature, and improvements. From tables 1 and 2 he can note the type of material that yields water in the vicinity. Table 3 shows the historic fluctuations and trends of water levels. Table 4 shows the type of material penetrated by wells. From table 5 he can note the chemical quality of water from wells and springs, and from table 6, the chemical quality of surface water. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Carpenter, C.H., Robinson, G.B., and Bjorklund, L.J., 1964, Selected hydrologic data, upper Sevier River basin, Utah: Utah Basic-Data Report 8, 29 p.","productDescription":"29 p.","numberOfPages":"37","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345769,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-160&Title=Basic+Data+Report+8"}],"country":"United States","state":"Utah","county":"Garfield County, Iron County, Kane County, Piute County, Sevier County","otherGeospatial":"Sevier River basi","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ae4b091459a578226","contributors":{"authors":[{"text":"Carpenter, Carl H.","contributorId":46074,"corporation":false,"usgs":true,"family":"Carpenter","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":710428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Gerald B. Jr.","contributorId":91837,"corporation":false,"usgs":true,"family":"Robinson","given":"Gerald","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":710429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bjorklund, Louis Jay","contributorId":21138,"corporation":false,"usgs":true,"family":"Bjorklund","given":"Louis","email":"","middleInitial":"Jay","affiliations":[],"preferred":false,"id":710430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70185698,"text":"70185698 - 1964 - Water in the world","interactions":[],"lastModifiedDate":"2017-03-27T16:44:51","indexId":"70185698","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5341,"text":"The UNESCO Courier","active":true,"publicationSubtype":{"id":10}},"title":"Water in the world","docAbstract":"<p>The earth, Including Its oceans and atmosphere, ls a giant distillation system whose operation brings about the distribution of fresh water throughout the world, from the frozen wastes of polar regions to the burning equatorial deserts. Stated in the simplest terms, distillation, condensation and liquid flow are the elemental processes which, on a grand scale, distribute and circulate throughout the world the water which ls essential for all life.</p><p>Water in liquid form absorbs heat energy, chiefly from the sun, and the absorbed energy changes the water from liquid to gaseous form. Transported in the atmosphere, the vapour later meets cooler conditions and condenses as precipitation, some of which replenishes the water in land areas.</p><p>Because water is continually being transformed from liquid to vapour and back to liquid again, the whole sequence of events ends where It began. That ls, the condensed moisture in the form of precipitation runs Into or off the surface of the earth, and a part of It collects in rivers which flow to the ocean. The events together form what is called the hydrological cycle.</p>","largerWorkTitle":"Water and Life","language":"English","publisher":"UNESCO","usgsCitation":"Leopold, L.B., 1964, Water in the world: The UNESCO Courier, v. 17, p. 11-13.","startPage":"11","endPage":"13","costCenters":[],"links":[{"id":338428,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338427,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.unesco.org/new/en/unesco-courier/archives/","text":"Journal Archives","linkHelpText":"Article is findable using the search function"}],"volume":"17","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da2540e4b0543bf7fda87f","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190980,"text":"70190980 - 1964 - Quality of surface waters in Utah, October 1962 to September 1963","interactions":[],"lastModifiedDate":"2017-09-19T16:02:03","indexId":"70190980","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Quality of surface waters in Utah, October 1962 to September 1963","docAbstract":"<p><span>This data release is a compilation that presents water-quality data for the period October 1962 to September 1963 for the sites listed on page 2. These preliminary data are subject to revision before final publication in the annual series of U.S. Geological Survey Water-supply papers entitled Quality of surface waters of the United States. Most of the data were obtained as part of the Geological Survey's continuing program for the investigation of the nation's water resources or as part of a cooperative program with the U.S. Bureau of Reclamation; some data were obtained as part of cooperative programs with the State Engineer of Utah and with the Soil Conservation Service.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/70190980","usgsCitation":"U.S. Geological Survey, 1964, Quality of surface waters in Utah, October 1962 to September 1963: Open-File Report, v, 77 p., https://doi.org/10.3133/70190980.","productDescription":"v, 77 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345895,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","publicComments":"Data Release 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59c22cb6e4b091459a61b756","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":127955,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":710811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190796,"text":"70190796 - 1964 - Ground-water data, Sevier Desert, Utah","interactions":[],"lastModifiedDate":"2017-09-14T11:38:12","indexId":"70190796","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"9","title":"Ground-water data, Sevier Desert, Utah","docAbstract":"<p>This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.</p><p>Records were collected during the period 1935-64 by the U.S. Geological survey in cooperation with the Utah State Engineer as part of the investigation of ground-water conditions in the Sevier Desert, in Juab and Millard Counties, Utah. The interpretive material will be published in a companion report by R. W. Mower and R. D. Feltis.</p><p>This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells as shown in the tables and figures. From table 1 he can note such things as depth, diameter, water level, yield, use of water, temperature of water, and depth of perforations. By comparing the depth of perforations with the drillers' logs in table 3 he can note the type of material that yields water to the wells. Table 2 and figure 2 show the historic fluctuations and trends of water levels in the vicinity. From table 4 he can note the chemical quality of the water from wells in the vicinity. Table 5 shows the amount of water discharged during 1951-63 from the pumped irrigation, public supply, and industrial wells. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the state Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.</p><p>The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Mower, R.W., and Feltis, R.D., 1964, Ground-water data, Sevier Desert, Utah: Utah Basic-Data Report 9, 34 p.","productDescription":"34 p.","numberOfPages":"41","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345766,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345765,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-180&Title=Basic+Data+Report+9"}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Desert","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ae4b091459a578228","contributors":{"authors":[{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":710423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":710424,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185667,"text":"70185667 - 1964 - [Book review] Politics and water resources","interactions":[],"lastModifiedDate":"2017-03-27T12:55:04","indexId":"70185667","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"[Book review] Politics and water resources","docAbstract":"<p>Arizona is a state in which development has proceeded sufficiently rapidly relative to the available water supply that its water problems are as acute as those of nearly any other state in the Union. Owing to the fact that, in the past, the principal use of water was for irrigation, and that the areas where the water has been utilized were geographically separated from the mountain zones where the water originated, surface water resources were developed fairly early in the state’s history.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.144.3617.402-b","usgsCitation":"Leopold, L.B., 1964, [Book review] Politics and water resources: Science, v. 144, no. 3617, p. 402-403, https://doi.org/10.1126/science.144.3617.402-b.","productDescription":"2 p.","startPage":"402","endPage":"403","costCenters":[],"links":[{"id":338376,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","volume":"144","issue":"3617","publicComments":"This is a review of \"<u>The Politics of Water in Arizona</u>. Dean E. Mann. University of Arizona Press, Tucson, 1963. xviii + 317 pp. Illus.\"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da2540e4b0543bf7fda881","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185663,"text":"70185663 - 1964 - Fluvial processes in geomorphology","interactions":[],"lastModifiedDate":"2017-03-27T12:36:09","indexId":"70185663","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":4,"text":"Book"},"publicationSubtype":{"id":15,"text":"Monograph"},"title":"Fluvial processes in geomorphology","docAbstract":"<p><span>This excellent text is a pioneering work in the study of landform development under processes associated with running water. Its primary emphasis is on subjects that were the focus of the authors' studies in both field and laboratory. Part I deals with the process of change in the evolving landscape. Part II explores process and form, and Part III, the effects of time.</span></p><p><span>In Part I, the relation of geomorphology to field problems is analyzed in studies of a mountain block in a semiarid climate, a meandering river cut into bedrock, and benches along a sea coast. Part Two contains studies of weathering, climate, and such denudational processes as flooding and erosion. Here, too, are examinations of the drainage basin as a geomorphic unit, water and sediment in channels, channel form and process, and hillslope characteristics and processes.</span></p><p><span>In Part III, the authors cover geochronology, drainage pattern evolution, channel changes with time, and the evolution of hillslopes. Two appendixes will help readers convert units and equivalents, and identify symbols and nomenclature.</span></p>","language":"English","publisher":"Dover Publications, Inc.","publisherLocation":"New York, NY","isbn":"0486685888","usgsCitation":"Leopold, L.B., Wolman, M.G., and Miller, J.P., 1964, Fluvial processes in geomorphology, 544 p.","productDescription":"544 p.","costCenters":[],"links":[{"id":338371,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338370,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://store.doverpublications.com/0486685888.html"}],"publicComments":"This book was originally published by W. H. Freeman & Company, San Francisco, California.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da2540e4b0543bf7fda883","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolman, M. Gordon","contributorId":85163,"corporation":false,"usgs":true,"family":"Wolman","given":"M.","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":686276,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, John P.","contributorId":33696,"corporation":false,"usgs":true,"family":"Miller","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":686277,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70191371,"text":"70191371 - 1964 - Developing a State Water Plan: A basic water resource data program for Utah","interactions":[],"lastModifiedDate":"2017-10-09T08:52:31","indexId":"70191371","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"1","title":"Developing a State Water Plan: A basic water resource data program for Utah","docAbstract":"<p>Reliable data on Utah's water resources are essential to development of a State Water plan. While the need for such data was outlined in the report entitles \"Developing a State Water Plan - Utah's water resources, problems, and needs - A challenge\" published by the Utah Water and Power Board and Utah State University in 1963, the discussion was, of necessity, brief. Further definition and scheduling of data collection and related investigations were known to be needed.<br data-mce-bogus=\"1\"></p><p>The report which follows was prepared by the U.S. Geological Survey as part of that agency's cooperative program with the State of Utah. It outlines, in greater detail, what the Geological Survey feels is an appropriate long-range program of investigations to provide part of the basic data which will be needed during the course of the State's water planning program. Some of these investigations already are underway, and others will be undertaken in the immediate future.<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"Utah Water and Power Board","collaboration":"Prepared by the United States Geological Survey in cooperation with the State of Utah","usgsCitation":"Arnow, T., Langford, R., and Wilson, M.T., 1964, Developing a State Water Plan: A basic water resource data program for Utah: Cooperative Investigations Report 1, 23 p.","productDescription":"23 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":346467,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a61583de4b06e28e9c260a7","contributors":{"authors":[{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":712122,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langford, R.H.","contributorId":59426,"corporation":false,"usgs":true,"family":"Langford","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":712123,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, M. T.","contributorId":102116,"corporation":false,"usgs":true,"family":"Wilson","given":"M.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":712124,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175579,"text":"70175579 - 1964 - Records of wells and springs, water levels, and chemical quality of ground water in the East Portland area, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T11:24:53","indexId":"70175579","displayToPublicDate":"1963-12-29T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Records of wells and springs, water levels, and chemical quality of ground water in the East Portland area, Oregon","docAbstract":"<p><span class=\"EXLDetailsDisplayVal\">Data are presented on more than 300 <span class=\"searchword\">wells</span>, including many new ones whose <span class=\"searchword\">records</span> will not be a part of a forthcoming interpretative report on the occurrence of <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span> in this <span class=\"searchword\">area</span>. A brief description of the geomorphic features is given, and the characteristics of the rock units are summarized in a table. Principal aquifers are beds of loose sand and gravel in the early Pliocene Troutdale Formation, late Pleistocene fluviolacustrine deposits, and Recent alluvium. Locally, Columbia River Basalt (Miocene) and the Boring Lava (late Pliocene to Pleistocene) yield substantial amounts of wate.. In addition to well <span class=\"searchword\">records</span> there are 124 driller's logs and a table of <span class=\"searchword\">chemical</span> analyses of the <span class=\"searchword\">ground</span> <span class=\"searchword\">water</span>.</span></p>","language":"English","usgsCitation":"Foxworthy, B., Hogenson, G., and Hampton, E.R., 1964, Records of wells and springs, water levels, and chemical quality of ground water in the East Portland area, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326649,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b57e4b03bcb0104bc4d","contributors":{"authors":[{"text":"Foxworthy, B. L.","contributorId":45686,"corporation":false,"usgs":true,"family":"Foxworthy","given":"B. L.","affiliations":[],"preferred":false,"id":645748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hogenson, G.M.","contributorId":69957,"corporation":false,"usgs":true,"family":"Hogenson","given":"G.M.","affiliations":[],"preferred":false,"id":645749,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":645750,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70221125,"text":"70221125 - 1964 - Origin of precambrian iron formations","interactions":[],"lastModifiedDate":"2021-06-02T17:51:31.990895","indexId":"70221125","displayToPublicDate":"1963-09-01T12:48:10","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Origin of precambrian iron formations","docAbstract":"<p><span>A statistical study of the chemical composition of the&nbsp;</span>Precambrian<span>&nbsp;</span>iron<span>&nbsp;</span>formations<span>&nbsp;of the Canadian Shield affords a new approach to the&nbsp;</span>origin<span>&nbsp;of these unusual&nbsp;</span>formations<span>. The average total&nbsp;</span>iron<span>&nbsp;content of 2,200 samples from the literature and from unpublished mining company analyses is 26.7 percent Fe. The average Fe content for 16&nbsp;</span>iron<span>&nbsp;</span>formations<span>&nbsp;in the United States and Canada ranges from 24.5 to 34.1 percent. Low contents of A1203, Ti02, P2O5, and CaO characterize the&nbsp;</span>Precambrian<span>&nbsp;</span>iron<span>&nbsp;</span>formations<span>&nbsp;compared to the relatively large amounts of these constituents in the post-</span>Precambrian<span>&nbsp;</span>iron<span>-bearing sediments. The chemical data emphasize that whereas&nbsp;</span>iron<span>, manganese, and silica were transported and deposited together in the cherty&nbsp;</span>iron<span>&nbsp;</span>formations<span>&nbsp;of the&nbsp;</span>Precambrian<span>, these same elements were chemically differentiated in younger geological time in large but separate deposits of&nbsp;</span>iron<span>&nbsp;and silica. Isotopic age determinations indicate that cherty&nbsp;</span>iron<span>&nbsp;</span>formations<span>&nbsp;were deposited during a long interval of geologic time from approximately 1,700 to 3,000 million years ago. A model is proposed to explain the&nbsp;</span>origin<span>&nbsp;of the&nbsp;</span>iron<span>&nbsp;</span>formations<span>&nbsp;of the Lake Superior type based on the absence or marked deficiency of free oxygen in the atmosphere prior to the Late&nbsp;</span>Precambrian<span>. Lateritic weathering under these conditions permitted the transport of&nbsp;</span>iron<span>&nbsp;and manganese together with silica. The weathered mantle effectively retained aluminum, titanium, phosphorus, and colloidal clay. Graphitic material of biogenic&nbsp;</span>origin<span>&nbsp;is closely associated with the&nbsp;</span>Precambrian<span>&nbsp;</span>iron<span>&nbsp;</span>formations<span>. Although it is uncertain whether&nbsp;</span>iron<span>&nbsp;was precipitated directly through biologic processes, the removal of C02 and the liberation of oxygen to the sea water through photosynthesis of primitive plants undoubtedly influenced the energy relationships among the&nbsp;</span>iron<span>&nbsp;minerals. As a result of the variable conditions the&nbsp;</span>iron<span>&nbsp;</span>formations<span>&nbsp;commonly are characterized by nonequilibrium mineral assemblages. In Late&nbsp;</span>Precambrian<span>&nbsp;time a critical level of free oxygen in the atmosphere was attained permitting a marked acceleration in plant growth and in accretion of oxygen. This stage in the development of an oxygenated atmosphere was reached at least 1,200 million years ago and effectively curtailed the development of cherty&nbsp;</span>iron<span>&nbsp;</span>formations<span>&nbsp;of the Lake Superior type.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.59.6.1025","usgsCitation":"Lepp, H., and Goldich, S., 1964, Origin of precambrian iron formations: Economic Geology, v. 59, no. 6, p. 1025-1060, https://doi.org/10.2113/gsecongeo.59.6.1025.","productDescription":"36 p.","startPage":"1025","endPage":"1060","costCenters":[],"links":[{"id":386141,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"6","noUsgsAuthors":false,"publicationDate":"1964-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lepp, H.","contributorId":259204,"corporation":false,"usgs":false,"family":"Lepp","given":"H.","email":"","affiliations":[],"preferred":false,"id":816811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldich, S. S.","contributorId":65536,"corporation":false,"usgs":true,"family":"Goldich","given":"S. S.","affiliations":[],"preferred":false,"id":816812,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70217324,"text":"wdrMDDE63 - 1963 - Surface water records of Maryland and Delaware, water year 1963","interactions":[],"lastModifiedDate":"2021-01-22T19:13:18.810771","indexId":"wdrMDDE63","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1963","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-63","displayTitle":"Surface Water Records of Maryland and Delaware, Water Year 1963","title":"Surface water records of Maryland and Delaware, water year 1963","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE63","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Surface water records of Maryland and Delaware, water year 1963: U.S. Geological Survey Water Data Report MD-DE-63, 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,{"id":70180201,"text":"70180201 - 1963 - Floods in southeastern Michigan, magnitude and frequency","interactions":[],"lastModifiedDate":"2017-01-25T14:59:42","indexId":"70180201","displayToPublicDate":"2017-01-25T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Floods in southeastern Michigan, magnitude and frequency","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/70180201","usgsCitation":"Stoimenoff, L., 1963, Floods in southeastern Michigan, magnitude and frequency: Open-File Report, 9 p., https://doi.org/10.3133/70180201.","productDescription":"9 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":333930,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Michigan","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5889c7c7e4b0ba3b075e065c","contributors":{"authors":[{"text":"Stoimenoff, L.E.","contributorId":34157,"corporation":false,"usgs":true,"family":"Stoimenoff","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":660748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179734,"text":"70179734 - 1963 - Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data","interactions":[],"lastModifiedDate":"2017-09-06T17:19:25","indexId":"70179734","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"3-I","title":"Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data","docAbstract":"<p>This report presents the data collected for a study of the dissolved-mineral load contributed by surficial sources to Great Salt Lake, Utah. The study was conducted by the U.S. Geological Survey in cooperation with the University of Utah during the period from July 1959 through June 1962, and is part of an overall investigation of the Great Salt Lake basin by the University. Financial support for the study was provided by the U.S. Geological Survey and by the University of Utah Research Fund and Uniform School Fund. Some of the data presented in this report were obtained as part of cooperative programs between the Geological Survey and other agencies.</p>","language":"English","publisher":"Utah Geological and Minerological Society","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with The College of Mines and Mineral Industries, University of Utah, Salt Lake City, Utah","usgsCitation":"Hahl, D.C., and Mitchell, C., 1963, Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data: Utah Geological and Mineralogical Survey Water-Resources Bulletin 3-I, 39 p.","productDescription":"39 p.","numberOfPages":"51","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345533,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179736","text":"Part II: Technical report"},{"id":345532,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-3part1.pdf"},{"id":333225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.2305908203125,\n              40.59727063442024\n            ],\n            [\n              -113.2305908203125,\n              41.795888098191426\n            ],\n            [\n              -111.81884765624999,\n              41.795888098191426\n            ],\n            [\n              -111.81884765624999,\n              40.59727063442024\n            ],\n            [\n              -113.2305908203125,\n              40.59727063442024\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d6","contributors":{"authors":[{"text":"Hahl, D. C.","contributorId":57436,"corporation":false,"usgs":true,"family":"Hahl","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":658473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mitchell, C.G.","contributorId":177183,"corporation":false,"usgs":true,"family":"Mitchell","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":658474,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179901,"text":"70179901 - 1963 - Effects on the shallow artesian aquifer of withdrawing water from the deep artesian aquifer near Sugarville, Millard County, Utah","interactions":[],"lastModifiedDate":"2017-01-19T17:44:45","indexId":"70179901","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5258,"text":"Utah State Engineer Water Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"10","title":"Effects on the shallow artesian aquifer of withdrawing water from the deep artesian aquifer near Sugarville, Millard County, Utah","docAbstract":"<p>Ground water occurs in a shallow (unconfined) aquifer and in at least two artesian (confined) aquifers in the unconsolidated alluvial material composing the valley fill near Sugarville, Utah. No wells are known to withdraw water from the unconfined aquifer, and this report is limited to a discussion of the effects of pumping a well tapping one artesian aquifer on the piezometric surfaces of the water in both artesian aquifers.</p>","language":"English","publisher":"Utah State Engineer's Office","publisherLocation":"Salt Lake City, UT","usgsCitation":"Mower, R.W., 1963, Effects on the shallow artesian aquifer of withdrawing water from the deep artesian aquifer near Sugarville, Millard County, Utah: Utah State Engineer Water Circular 10, 9 p.","productDescription":"9 p.","numberOfPages":"12","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333519,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333518,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-4-190"}],"country":"United States","state":"Utah","city":"Sugarville","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881def9e4b01192927d9ffd","contributors":{"authors":[{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659147,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179902,"text":"70179902 - 1963 - Test drilling in the upper Sevier River drainage basin, Garfield and Piute Counties, Utah","interactions":[],"lastModifiedDate":"2017-01-19T17:51:02","indexId":"70179902","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5258,"text":"Utah State Engineer Water Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"12","title":"Test drilling in the upper Sevier River drainage basin, Garfield and Piute Counties, Utah","docAbstract":"<p>A test-drilling program was conducted by the U.S. Geological Survey in the upper Sevier River drainage basin (fig. 1) in the summer of 1962. The program was part of a ground-water investigation made in cooperation with the Utah State Engineer. The drilling was financed cooperatively through the State Engineer by the U.S. Geological Survey, Garfield, Piute, Sevier, Sanpete, and Millard Counties, and various water users within those counties. Drilling began in May and continued through September 1962, and 21 test holes were drilled.</p>","language":"English","publisher":"Utah State Engineer's Office","publisherLocation":"Salt Lake City, UT","usgsCitation":"Feltis, R., and Robinson, G., 1963, Test drilling in the upper Sevier River drainage basin, Garfield and Piute Counties, Utah: Utah State Engineer Water Circular 12, 32 p.","productDescription":"32 p.","numberOfPages":"36","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333521,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333520,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=21-4-230"}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5881def9e4b01192927d9ffb","contributors":{"authors":[{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":659148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, G.B.","contributorId":178487,"corporation":false,"usgs":true,"family":"Robinson","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":659149,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70179721,"text":"70179721 - 1963 - Hydrogeologic reconnaissance of part of the headwaters area of the Price River, Utah","interactions":[],"lastModifiedDate":"2017-09-06T17:27:11","indexId":"70179721","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"4","title":"Hydrogeologic reconnaissance of part of the headwaters area of the Price River, Utah","docAbstract":"<p>The area investigated comprises 33 square miles in the Price River drainage basin ad is in the High Plateaus section of Utah. Precipitation on most of the area ranges from about 20 to 23 inches per year, and the average annual precipitation for the entire area was assumed to be 22 inches, of which approximately 65 percent is lost by evapotranspiration. The geologic formations underlying the area are the Blackhawk and Price River Formations of Cretaceous age, the North Horn Formation of Cretaceous and Tertiary age, the Flagstaff Limestone and Colton Formation of tertiary age, and unconsolidated deposits of probable Quaternary age.</p><p>Some ground water issues from springs and seeps and is used by stock and the cities of Price and Helper. The annual discharge from the springs and seeps in the area averages about 3,000 acre-feet. Two deep wells supply about 400 acre-feet per year for use at a steam-generating plant. The aquifers penetrated by the wells are in the Flagstaff Limestone and the North Horn formation, the deepest aquifer being about 1,500 feet below the land surface. Most of the ground water in the area is suitable for municipal and industrial use.</p><p>The surface discharge from the area is approximately 6,000 acre-feet per year. By means of a water budget, it is calculated that approximately 4,000 acre-feet per year leaves the area by subsurface flow. Further development of ground water on a large scale can be accomplished only by the use of wells. It is possible, however, that part of any newly developed supply from wells may be drawn from existing spring discharge or streamflow.</p>","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State Engineer of Utah and the Price River Water Improvement District","usgsCitation":"Cordova, R.M., 1963, Hydrogeologic reconnaissance of part of the headwaters area of the Price River, Utah: Utah Geological and Mineralogical Survey Water-Resources Bulletin 4, 26 p.","productDescription":"26 p.","numberOfPages":"28","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333196,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333192,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-4.pdf"}],"country":"United States","state":"Utah","county":"Carbon County, Utah County","otherGeospatial":"Price River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.13700866699219,\n              39.761047087593965\n            ],\n            [\n              -111.13700866699219,\n              39.87127666240552\n            ],\n            [\n              -110.98526000976562,\n              39.87127666240552\n            ],\n            [\n              -110.98526000976562,\n              39.761047087593965\n            ],\n            [\n              -111.13700866699219,\n              39.761047087593965\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d8","contributors":{"authors":[{"text":"Cordova, Robert M.","contributorId":178302,"corporation":false,"usgs":true,"family":"Cordova","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":658427,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70179720,"text":"70179720 - 1963 - Ground-water conditions in the southern and central parts of the East Shore area, Utah, 1953-61","interactions":[],"lastModifiedDate":"2017-09-06T17:27:46","indexId":"70179720","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Ground-water conditions in the southern and central parts of the East Shore area, Utah, 1953-61","docAbstract":"<p>The East Shore area is in north-central Utah between the Wasatch Range and Great Salt Lake, and it has been divided into the Bountiful, Weber Delta, and Brigham ground-water districts, from south to north. The area described in this report includes the Bountiful and Weber Delta districts and the southernmost part of the Brigham district. Long-term mean annual precipitation at Ogden is 17.07 inches, and the average annual temperature over the area is about 50°F. The population of the project area increased by 54 per cent from 1950 to 1960 and should increase rapidly in the future.</p>","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State Engineer of Utah","usgsCitation":"Smith, R., and Gates, J., 1963, Ground-water conditions in the southern and central parts of the East Shore area, Utah, 1953-61: Utah Geological and Mineralogical Survey Water-Resources Bulletin 2, 41 p.","productDescription":"41 p.","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333191,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333190,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-2.pdf"}],"country":"United 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E.","contributorId":178301,"corporation":false,"usgs":true,"family":"Smith","given":"Ralph E.","affiliations":[],"preferred":false,"id":658425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":658426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71791,"text":"tei840 - 1963 - A summary of the ground-water hydrology of the area between the Las Vegas Valley and the Amargosa Desert, Nevada, with special reference to the effects of possible new withdrawals of ground water","interactions":[],"lastModifiedDate":"2014-07-16T14:13:44","indexId":"tei840","displayToPublicDate":"2013-07-16T14:10:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"840","title":"A summary of the ground-water hydrology of the area between the Las Vegas Valley and the Amargosa Desert, Nevada, with special reference to the effects of possible new withdrawals of ground water","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei840","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Winograd, I.J., 1963, A summary of the ground-water hydrology of the area between the Las Vegas Valley and the Amargosa Desert, Nevada, with special reference to the effects of possible new withdrawals of ground water: U.S. Geological Survey Trace Elements Investigations 840, Report: 79 p.; 1 Map, https://doi.org/10.3133/tei840.","productDescription":"Report: 79 p.; 1 Map","costCenters":[],"links":[{"id":290305,"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\": [ [ [ -116.4011,36.2803 ], [ -116.4011,36.6184 ], [ -115.2713,36.6184 ], [ -115.2713,36.2803 ], [ -116.4011,36.2803 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ee2e4b0194841642416","contributors":{"authors":[{"text":"Winograd, Isaac Judah","contributorId":9233,"corporation":false,"usgs":true,"family":"Winograd","given":"Isaac","email":"","middleInitial":"Judah","affiliations":[],"preferred":false,"id":284759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71788,"text":"tei836 - 1963 - Ground-water test well 2, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and well construction","interactions":[],"lastModifiedDate":"2014-07-16T14:03:58","indexId":"tei836","displayToPublicDate":"2013-07-16T14:01:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"836","title":"Ground-water test well 2, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and well construction","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei836","collaboration":"Work done on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Moore, J.E., and Carroll, R.D., 1963, Ground-water test well 2, Nevada test site, Nye County, Nevada : a summary of lithologic data, aquifer tests, and well construction: U.S. Geological Survey Trace Elements Investigations 836, 73 p., https://doi.org/10.3133/tei836.","productDescription":"73 p.","costCenters":[],"links":[{"id":290301,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Nye County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.1972,35.9618 ], [ -118.1972,39.1634 ], [ -114.999,39.1634 ], [ -114.999,35.9618 ], [ -118.1972,35.9618 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ef7e4b0194841642456","contributors":{"authors":[{"text":"Moore, John Ezra","contributorId":93582,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"Ezra","affiliations":[],"preferred":false,"id":284756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carroll, Roderick D.","contributorId":93395,"corporation":false,"usgs":true,"family":"Carroll","given":"Roderick","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":284755,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047455,"text":"70047455 - 1963 - Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania","interactions":[{"subject":{"id":52352,"text":"ofr6397 - 1963 - Geology and hydrology of the carbonate rocks of the Lebanon Valley, Pennsylvania","indexId":"ofr6397","publicationYear":"1963","noYear":false,"title":"Geology and hydrology of the carbonate rocks of the Lebanon Valley, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047455,"text":"70047455 - 1963 - Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania","indexId":"70047455","publicationYear":"1963","noYear":false,"title":"Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania"},"id":1}],"lastModifiedDate":"2013-08-06T15:18:39","indexId":"70047455","displayToPublicDate":"2013-01-01T13:51:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"18","title":"Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania","docAbstract":"The Lebanon Valley, which is part of the Great Valley in southeastern Pennsylvania, is underlain by carbonate rocks in the southern part and by shale in the northern part. The carbonate rocks consist of alternating beds of limestone and dolomite of Cambrian and Ordovician age. Although the beds generally dip to the south, progressively younger beds crop out to the north, because the rocks are overturned. The stratigraphic units, from oldest to youngest, are: the Buffalo Springs Formation, Snitz Creek, Schaefferstown, Millbach, and Richland Formations of the Conococheague Group; the Stonehenge, Rickenbach, Epler, and Ontelaunee Formations of the Beekmantown Group; and the Annville, Myerstown, and Hershey Limestones.","language":"English","publisher":"Pennsylvania Geological Survey","publisherLocation":"Harrisburg, PA","collaboration":"Prepared by the United States Geological Survey, Ground Water Branch in cooperation with the Pennsylvania Geological Survey","usgsCitation":"Meisler, H., 1963, Hydrogeology of the carbonate rocks of the Lebanon Valley, Pennsylvania: Ground Water Report 18, 81 p.; Maps: 3 Sheets.","productDescription":"81 p.; Maps: 3 Sheets","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276131,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047455.PNG"},{"id":276129,"type":{"id":11,"text":"Document"},"url":"https://www.dcnr.state.pa.us/cs/groups/public/documents/document/dcnr_016307.zip"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Lebanon Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.625,40.25 ], [ -76.625,40.416667 ], [ -76.25,40.416667 ], [ -76.25,40.25 ], [ -76.625,40.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae6e4b0e21cafa49c66","contributors":{"authors":[{"text":"Meisler, Harold","contributorId":34103,"corporation":false,"usgs":true,"family":"Meisler","given":"Harold","email":"","affiliations":[],"preferred":false,"id":482072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047480,"text":"70047480 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","interactions":[{"subject":{"id":52309,"text":"ofr6316 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","indexId":"ofr6316","publicationYear":"1963","noYear":false,"title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047480,"text":"70047480 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","indexId":"70047480","publicationYear":"1963","noYear":false,"title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida"},"id":1}],"lastModifiedDate":"2017-09-13T17:55:27","indexId":"70047480","displayToPublicDate":"2013-01-01T13:24:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5489,"text":"Florida Geological Survey Report of Investigations","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"33","title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida","docAbstract":"Brooklyn Lake receded about 20 feet during 1954-58 and reached its lowest stage of record (97.2 feet) in February 1958; this was the lowest stage in the memory of longtime residents. This unusually large recession was a result of deficient rainfall during more than a 3-year period, January 1954 to May 1957. However, by October 1959, after 2 1/2 years of above normal rainfall, the lake had recovered and water was flowing through the surface outlet.","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by the United States Geological Survey in cooperation with the Florida Geological Survey","usgsCitation":"Clark, W.E., Musgrove, R.H., Menke, C.G., and Cagle, J.W., 1963, Hydrology of Brooklyn Lake near Keystone Heights, Florida: Florida Geological Survey Report of Investigations 33, viii, 43 p.","productDescription":"viii, 43 p.","costCenters":[],"links":[{"id":276166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047480.PNG"},{"id":276162,"type":{"id":11,"text":"Document"},"url":"https://ufdc.ufl.edu/UF00001220/00001/pdf?search=report+%3dinvestigations"}],"country":"United States","state":"Florida","otherGeospatial":"Brooklyn Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.16,29.71 ], [ -82.16,29.86 ], [ -81.95,29.86 ], [ -81.95,29.71 ], [ -82.16,29.71 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5203a37be4b02bdb1bc63fc4","contributors":{"authors":[{"text":"Clark, William E.","contributorId":105365,"corporation":false,"usgs":true,"family":"Clark","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Musgrove, Rufus H.","contributorId":20245,"corporation":false,"usgs":true,"family":"Musgrove","given":"Rufus","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":482146,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Menke, Clarence G.","contributorId":25450,"corporation":false,"usgs":true,"family":"Menke","given":"Clarence","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":482147,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cagle, Joseph W. Jr.","contributorId":78640,"corporation":false,"usgs":true,"family":"Cagle","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482148,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70047675,"text":"70047675 - 1963 - Geology and ground-water resources of northwestern King County, Washington","interactions":[{"subject":{"id":47153,"text":"ofr60116 - 1960 - Geologic map and sections of northwestern King County, Washington","indexId":"ofr60116","publicationYear":"1960","noYear":false,"title":"Geologic map and sections of northwestern King County, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":70047675,"text":"70047675 - 1963 - Geology and ground-water resources of northwestern King County, Washington","indexId":"70047675","publicationYear":"1963","noYear":false,"title":"Geology and ground-water resources of northwestern King County, Washington"},"id":1}],"lastModifiedDate":"2020-09-09T13:05:00.38711","indexId":"70047675","displayToPublicDate":"2013-01-01T10:02:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":148,"text":"Water Supply Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"20","title":"Geology and ground-water resources of northwestern King County, Washington","docAbstract":"King County, in the west-central part of the State of Washington, includes about 2,135 square miles. The eastern part of the county lies in the Sierra-Cascade Mountains province and the remainder is in the Puget Trough of the Pacific Border province. The area covered by the present investigation is almost entirely within the Puget Trough and includes about 450 square miles.","language":"English","publisher":"Washington State Division of Water Resources","publisherLocation":"Olympia, WA","collaboration":"Prepared in cooperation with United States Geological Survey Ground-Water Branch","usgsCitation":"Liesch, B.A., Price, C.E., and Walters, K., 1963, Geology and ground-water resources of northwestern King County, Washington: Water Supply Bulletin 20, Report: 241 p.; 3 Plates: 46.00 x 31.00 inches or smaller.","productDescription":"Report: 241 p.; 3 Plates: 46.00 x 31.00 inches or smaller","costCenters":[],"links":[{"id":276742,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047675.JPG"},{"id":276741,"type":{"id":17,"text":"Plate"},"url":"https://fortress.wa.gov/ecy/publications/parts/wsb20part2.pdf","text":"Plate 1-3","description":"Plates 1-3"},{"id":378175,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://fortress.wa.gov/ecy/publications/SummaryPages/WSB20.html"}],"country":"United States","state":"Washington","county":"King County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.5431,47.0814 ], [ -122.5431,47.7824 ], [ -121.0682,47.7824 ], [ -121.0682,47.0814 ], [ -122.5431,47.0814 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52136e33e4b0b08f446198de","contributors":{"authors":[{"text":"Liesch, Bruce A.","contributorId":71208,"corporation":false,"usgs":true,"family":"Liesch","given":"Bruce","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":482695,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, Charles E.","contributorId":38523,"corporation":false,"usgs":true,"family":"Price","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482694,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walters, Kenneth L.","contributorId":104099,"corporation":false,"usgs":true,"family":"Walters","given":"Kenneth L.","affiliations":[],"preferred":false,"id":482696,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70046301,"text":"70046301 - 1963 - Geology and ground water resources of Kidder County, North Dakota","interactions":[],"lastModifiedDate":"2024-08-29T16:54:21.876403","indexId":"70046301","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"36","title":"Geology and ground water resources of Kidder County, North Dakota","docAbstract":"Kidder County was covered with glacial ice at least three times during the Wisconsin Stage of the Pleistocene, but the entire sequence of drifts has not been observed in one exposure. The drift which covers the area was deposited during three ice advances termed the Long Lake, Burnstad and Streeter advances. The position of the drift border of the Long Lake advance is marked by the prominent Long Lake end moraine on the western border of the county.","language":"English","publisher":"North Dakota Geological Survey","publisherLocation":"Grand Forks, ND","collaboration":"Prepared cooperatively by the U.S. Geological Survey, the North Dakota Geological Survey, and the North Dakota State Water Conservation Commission; This report was also published as North Dakota County and Ground Water Studies 1","usgsCitation":"Rau, J.L., Bakken, W.E., Chmelik, J., Williams, B.J., Randich, P., Petri, L.R., Adolphson, D.G., and Bradley, E., 1963, Geology and ground water resources of Kidder County, North Dakota: Bulletin 36, 3 Parts; Variously Paginated; Maps.","productDescription":"3 Parts; Variously Paginated; Maps","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":433324,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71160.htm","text":"Part III","linkFileType":{"id":5,"text":"html"}},{"id":273350,"rank":4,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046301.png"},{"id":433323,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71159.htm","text":"Part II","linkFileType":{"id":5,"text":"html"}},{"id":433322,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71158.htm","text":"Part I","linkFileType":{"id":5,"text":"html"}},{"id":273351,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://www.swc.nd.gov/info_edu/reports_and_publications/county_groundwater_studies/pdfs/Kidder_Part_III.pdf","text":"Part III","linkFileType":{"id":1,"text":"pdf"}},{"id":273352,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://www.swc.nd.gov/info_edu/reports_and_publications/county_groundwater_studies/pdfs/Kidder_Part_II.pdf","text":"Part II","linkFileType":{"id":1,"text":"pdf"}},{"id":273353,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.swc.nd.gov/info_edu/reports_and_publications/county_groundwater_studies/pdfs/Kidder_Part_I.pdf","text":"Part I","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North Dakota","county":"Kidder County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100.12,46.63 ], [ -100.12,47.33 ], [ -99.45,47.33 ], [ -99.45,46.63 ], [ -100.12,46.63 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b1bbd0e4b022a6a540f9bf","contributors":{"authors":[{"text":"Rau, Jon L.","contributorId":97989,"corporation":false,"usgs":true,"family":"Rau","given":"Jon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":479423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bakken, Wallace E.","contributorId":34811,"corporation":false,"usgs":true,"family":"Bakken","given":"Wallace","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":479418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chmelik, James","contributorId":92958,"corporation":false,"usgs":true,"family":"Chmelik","given":"James","email":"","affiliations":[],"preferred":false,"id":479422,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, Barrett J.","contributorId":16306,"corporation":false,"usgs":true,"family":"Williams","given":"Barrett","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":479417,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Randich, P.G.","contributorId":69953,"corporation":false,"usgs":true,"family":"Randich","given":"P.G.","affiliations":[],"preferred":false,"id":479421,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Petri, L. 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