{"pageNumber":"1636","pageRowStart":"40875","pageSize":"25","recordCount":46644,"records":[{"id":70199512,"text":"70199512 - 1982 - Geologic estimates and future costs of strip mining coal","interactions":[],"lastModifiedDate":"2018-09-20T15:26:51","indexId":"70199512","displayToPublicDate":"1982-09-01T16:39:35","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5749,"text":"Energy Systems and Policy","active":true,"publicationSubtype":{"id":10}},"title":"Geologic estimates and future costs of strip mining coal","docAbstract":"<p>Geologic coal-resource appraisals, which typically describe the location and general characteristics of coalbeds, do not generally provide enough information to estimate the cost of developing the resource or to predict the escalation of costs expected to result from physical depletion. This paper considers the nature of data and methods of appraisal required to provide this cost information to policymakers. Illinois is used as a prototype area for analysis because of its long history of coal mining and its demonstrated coal reserve base of strippable coal that exceeds all but two of the States in the United States. Evidence of gradual depletion of Illinois strippable coal reserves is provided by declining labor productivity, decreasing average mine size, and increasing overburden depth. The procedures used to estimate the costs of mining remaining deposits indicate that the physical characteristics that will affect mining costs most significantly are depth of overburden, thickness of coal seam, and areal extent of coal of the minable reserve blocks. Findings presented here provide guidelines for the collection of economic and geologic data in order to improve coal appraisals, particularly those currently in progress in the Western United States. <br><br></p>","language":"English","publisher":"Taylor & Francis Inc.","usgsCitation":"Attanasi, E., and Green, E., 1982, Geologic estimates and future costs of strip mining coal: Energy Systems and Policy, v. 6, no. 3, p. 193-212.","productDescription":"20 p.","startPage":"193","endPage":"212","costCenters":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"links":[{"id":357526,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Attanasi, Emil 0000-0001-6845-7160 attanasi@usgs.gov","orcid":"https://orcid.org/0000-0001-6845-7160","contributorId":1809,"corporation":false,"usgs":true,"family":"Attanasi","given":"Emil","email":"attanasi@usgs.gov","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":745654,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, E.K.","contributorId":15760,"corporation":false,"usgs":true,"family":"Green","given":"E.K.","email":"","affiliations":[],"preferred":false,"id":745655,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039454,"text":"70039454 - 1982 - Earth Science Information System (ESIS)","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039454","displayToPublicDate":"1982-08-01T16:17:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Earth Science Information System (ESIS)","docAbstract":"The Earth Science Information System (ESIS) was developed in 1981 by the U.S. Geological Survey's Office of the Data Administrator. ESIS serves as a comprehensive data management facility designed to support the coordination, integration, and standardization of scientific, technical, and bibliographic data of the U.S. Geological Survey (USGS). ESIS provides, through an online interactive computer system, referral to information about USGS data bases, data elements which are fields in the records of data bases, and systems. The data bases contain information about many subjects from several scientific disciplines such as: geology, geophysics, geochemistry, hydrology, cartography, oceanography, geography, minerals exploration and conservation, and satellite data sensing.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039454","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Earth Science Information System (ESIS), 11 p., https://doi.org/10.3133/70039454.","productDescription":"11 p.","numberOfPages":"6","costCenters":[],"links":[{"id":261590,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039454/report.pdf"},{"id":261591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039454/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0496e4b0c8380cd50a8c","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":535307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70120390,"text":"70120390 - 1982 - Capture-recapture and removal methods for sampling closed populations","interactions":[],"lastModifiedDate":"2014-08-14T09:08:52","indexId":"70120390","displayToPublicDate":"1982-08-01T09:07:04","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Capture-recapture and removal methods for sampling closed populations","docAbstract":"The problem of estimating animal abundance is common in wildlife management and environmental impact asessment. Capture-recapture and removal methods are often used to estimate population size. Statistical Inference From Capture Data On Closed Animal Populations, a monograph by Otis et al. (1978), provides a comprehensive synthesis of much of the wildlife and statistical literature on the methods, as well as some extensions of the general theory. In our primer, we focus on capture-recapture and removal methods for trapping studies in which a population is assumed to be closed and do not treat open-population models, such as the Jolly-Seber model, or catch-effort methods in any detail. The primer, written for students interested in population estimation, is intended for use with the more theoretical monograph.","language":"English","publisher":"Los Alamos National Laboratory","publisherLocation":"Los Alamos, NM","usgsCitation":"White, G.C., Anderson, D.R., Burnham, K.P., and Otis, D.L., 1982, Capture-recapture and removal methods for sampling closed populations, 13 p.","productDescription":"13 p.","numberOfPages":"14","costCenters":[],"links":[{"id":292143,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53edcd44e4b0f61b386d23ac","contributors":{"authors":[{"text":"White, Gary C.","contributorId":66831,"corporation":false,"usgs":false,"family":"White","given":"Gary","email":"","middleInitial":"C.","affiliations":[{"id":6621,"text":"Colorado State University","active":true,"usgs":false}],"preferred":false,"id":498121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, David R.","contributorId":92722,"corporation":false,"usgs":true,"family":"Anderson","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":498123,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burnham, Kenneth P.","contributorId":95025,"corporation":false,"usgs":true,"family":"Burnham","given":"Kenneth","email":"","middleInitial":"P.","affiliations":[{"id":189,"text":"Colorado Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":498124,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Otis, David L.","contributorId":78455,"corporation":false,"usgs":true,"family":"Otis","given":"David","email":"","middleInitial":"L.","affiliations":[{"id":350,"text":"Iowa Cooperative Fish and Wildlife Research Unit","active":false,"usgs":true}],"preferred":false,"id":498122,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70120251,"text":"70120251 - 1982 - Wilderness permit accuracy: differences between reported and actual use","interactions":[],"lastModifiedDate":"2014-08-13T13:23:43","indexId":"70120251","displayToPublicDate":"1982-07-01T13:22:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1547,"text":"Environmental Management","active":true,"publicationSubtype":{"id":10}},"title":"Wilderness permit accuracy: differences between reported and actual use","docAbstract":"Wilderness permits are valuable tools for recording backcountry use patterns. They provide a valuable basis upon which management decisions are made. Unfortunately, significant inaccuracies in reporting permit data result from noncompliance, transmission errors, and changes in visitor plans. Data from Sequoia and Kings Canyon National Parks in California show that in 1978, 97 percent of the parties obtained wilderness permits. Changes in visitor plans resulted in an over-reporting of total persons by 8 percent and of visitor nights by 23 percent. The latter was due primarily to shortening of trip length. Over-reporting was greatest when permits were issued well in advance of the trip. Backcountry managers should be aware of possible inaccuracies in permit data and may want to adjust for them under certain circumstances.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Management","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","publisherLocation":"New York, NY","doi":"10.1007/BF01875064","usgsCitation":"Parsons, D.J., Stohlgren, T.J., and Kraushaar, J.M., 1982, Wilderness permit accuracy: differences between reported and actual use: Environmental Management, v. 6, no. 4, p. 329-335, https://doi.org/10.1007/BF01875064.","productDescription":"7 p.","startPage":"329","endPage":"335","numberOfPages":"7","costCenters":[],"links":[{"id":292096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":292095,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01875064"}],"volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ec7bd4e4b02bf5a76740c6","contributors":{"authors":[{"text":"Parsons, David J.","contributorId":39249,"corporation":false,"usgs":true,"family":"Parsons","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":498056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stohlgren, Thomas J. 0000-0001-9696-4450 stohlgrent@usgs.gov","orcid":"https://orcid.org/0000-0001-9696-4450","contributorId":2902,"corporation":false,"usgs":true,"family":"Stohlgren","given":"Thomas","email":"stohlgrent@usgs.gov","middleInitial":"J.","affiliations":[{"id":291,"text":"Fort Collins Science Center","active":true,"usgs":true}],"preferred":true,"id":498055,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kraushaar, James M.","contributorId":48493,"corporation":false,"usgs":true,"family":"Kraushaar","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":498057,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011708,"text":"70011708 - 1982 - Uraniferous opal, Virgin Valley, Nevada: Conditions of formation and implications for uranium exploration","interactions":[],"lastModifiedDate":"2025-04-08T17:10:15.793994","indexId":"70011708","displayToPublicDate":"1982-06-04T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Uraniferous opal, Virgin Valley, Nevada: Conditions of formation and implications for uranium exploration","docAbstract":"<p><span>Uraniferous, fluorescent opal, which occurs in tuffaceous sedimentary rocks at Virgin Valley, Nevada, records the temperature and composition of uranium-rich solutions as well as the time of uranium-silica coprecipitation. Results are integrated with previous geologic and geochronologic data for the area to produce a model for uranium mobility that may be used to explore for uranium deposits in similar geologic settings.</span></p><p><span>Uraniferous opal occurs as replacements of diatomite, or silicic air-fall ash layers in tuffaceous lakebeds of the Virgin Valley Formation (Miocene) of Merriam (1907). Fission-track radiography shows uranium to be homogeneously dispersed throughout the opal structure, suggesting coprecipitation of dissolved uranium and silica gel. Fluid inclusions preserved within opal replacements of diatomite have homogenization temperatures in the epithermal range and are of low salinity. Four samples of opal from one locality all have U-Pb apparent ages which suggest uraniferous opal precipitation in late Pliocene time. These ages correspond to a period of local, normal faulting, and highangle faults may have served as vertical conduits for transport of deep, thermalized ground water to shallower levels. Lateral migration of rising solutions occurred at intersections of faults with permeable strata. Silica and some uranium were dissolved from silica-rich host strata of 5–20 ppm original uranium content and reprecipitated as the solutions cooled. The model predicts that in similar geologic settings, ore-grade concentrations of uranium will occur in permeable strata that intersect high-angle faults and that contain uranium source rocks as well as efficient reductant traps for uranium. In the absence of sufficient quantities of reductant materials, uranium will be flushed from the system or will accumulate in low-grade disseminated hosts such as uraniferous opal.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(82)90010-3","usgsCitation":"Zielinski, R.A., 1982, Uraniferous opal, Virgin Valley, Nevada: Conditions of formation and implications for uranium exploration: Journal of Geochemical Exploration, v. 16, no. 3, p. 197-216, https://doi.org/10.1016/0375-6742(82)90010-3.","productDescription":"20 p.","startPage":"197","endPage":"216","costCenters":[],"links":[{"id":221384,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","county":"Humboldt County","otherGeospatial":"Virgin Valley","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-117.0293,42.0003],[-117.0175,42.0003],[-117.0171,41.6942],[-117.0173,41.667],[-117.0174,41.6457],[-117.0177,41.5167],[-117.0177,41.5113],[-117.0172,41.5018],[-117.0174,41.4732],[-117.0175,41.4586],[-117.0174,41.3842],[-117.0175,41.3697],[-117.0176,41.3556],[-117.0177,41.3411],[-117.0172,41.3266],[-117.0173,41.3107],[-117.0174,41.2971],[-117.0175,41.283],[-117.0176,41.268],[-117.0173,41.2249],[-117.0173,41.2109],[-117.0169,41.1954],[-117.0169,41.1809],[-117.017,41.1668],[-117.0177,41.1519],[-117.0173,41.1364],[-117.0169,41.0929],[-117.017,41.0779],[-117.0171,41.0639],[-117.0172,41.0493],[-117.0173,41.0344],[-117.0168,41.0203],[-117.0169,41.0058],[-117.017,41.0003],[-117.0164,40.9899],[-117.0171,40.9754],[-117.0166,40.9609],[-117.0167,40.9454],[-117.0168,40.9318],[-117.0169,40.9169],[-117.0176,40.9019],[-117.0171,40.8865],[-117.0172,40.8715],[-117.0173,40.8583],[-117.0168,40.8447],[-117.0175,40.8302],[-117.017,40.8148],[-117.0179,40.7712],[-117.0183,40.7123],[-117.019,40.6978],[-117.0179,40.6846],[-117.0174,40.6687],[-117.0169,40.6542],[-117.0164,40.6415],[-117.0357,40.642],[-117.0551,40.6417],[-117.0733,40.6417],[-117.0921,40.6418],[-117.1115,40.6414],[-117.1302,40.6414],[-117.1502,40.641],[-117.1684,40.6406],[-117.1866,40.6402],[-117.2078,40.6398],[-117.2272,40.6399],[-117.2459,40.6399],[-117.249,40.6358],[-117.2539,40.6254],[-117.2606,40.6105],[-117.2624,40.6064],[-117.2673,40.5964],[-117.274,40.5819],[-117.2807,40.567],[-117.2874,40.5525],[-117.2935,40.538],[-117.2977,40.5334],[-117.3008,40.5244],[-117.3007,40.5674],[-117.3,40.5815],[-117.3012,40.5965],[-117.3011,40.6105],[-117.3011,40.6259],[-117.3011,40.64],[-117.3016,40.655],[-117.3016,40.6699],[-117.3016,40.6827],[-117.4137,40.6828],[-117.4525,40.6833],[-117.4694,40.6833],[-117.4906,40.6833],[-117.5088,40.6837],[-117.5258,40.6837],[-117.5488,40.6837],[-117.5682,40.6837],[-117.5882,40.6837],[-117.6076,40.6837],[-117.6428,40.6836],[-117.6428,40.7122],[-117.6423,40.7281],[-117.6423,40.7439],[-117.6423,40.7571],[-117.6423,40.7703],[-117.6431,40.8438],[-117.6431,40.8574],[-117.6595,40.8573],[-117.679,40.8573],[-117.6984,40.8568],[-117.7185,40.8573],[-117.7373,40.8572],[-117.7549,40.8572],[-117.8497,40.8574],[-117.8691,40.8574],[-117.8898,40.8573],[-117.9092,40.8572],[-117.9293,40.8572],[-117.9487,40.8571],[-117.9676,40.857],[-117.9828,40.857],[-118.0046,40.8569],[-118.0229,40.8568],[-118.0423,40.8567],[-118.063,40.8567],[-118.0818,40.857],[-118.0988,40.8569],[-118.1183,40.8573],[-118.1365,40.8572],[-118.1553,40.8571],[-118.1754,40.857],[-118.1991,40.8569],[-118.2142,40.8573],[-118.2349,40.8567],[-118.255,40.8566],[-118.2738,40.8564],[-118.2932,40.8563],[-118.3127,40.8562],[-118.3291,40.8561],[-118.3509,40.856],[-118.3692,40.8563],[-118.388,40.8557],[-118.4081,40.856],[-118.4275,40.8559],[-118.4439,40.8558],[-118.4646,40.8556],[-118.4834,40.8555],[-118.5028,40.8553],[-118.5235,40.8551],[-118.5411,40.855],[-118.5435,40.855],[-118.6717,40.8548],[-118.6906,40.8546],[-118.7781,40.8556],[-118.7872,40.8555],[-118.7869,40.9049],[-118.7871,40.9172],[-118.7869,40.9426],[-118.7879,40.9607],[-118.8414,40.9606],[-118.9546,40.9607],[-119.0903,40.9591],[-119.1627,40.9591],[-119.3088,40.9589],[-119.3288,40.9586],[-119.3305,40.9999],[-119.3305,41.235],[-119.317,41.2352],[-119.3042,41.2354],[-119.3038,41.2676],[-119.3033,41.2957],[-119.3028,41.3225],[-119.302,41.3888],[-119.3021,41.4133],[-119.3229,41.413],[-119.323,41.443],[-119.3227,41.5256],[-119.3226,41.5905],[-119.3262,41.5905],[-119.3287,41.5905],[-119.3287,41.5918],[-119.3278,41.6963],[-119.3275,41.7103],[-119.3279,41.7703],[-119.3276,41.8566],[-119.3227,41.8571],[-119.3244,41.9936],[-119.1449,41.9942],[-119.0478,41.9946],[-118.9076,41.9935],[-118.7764,41.993],[-118.7723,41.993],[-118.5914,41.9943],[-118.4287,41.9952],[-118.3891,41.9954],[-118.3496,41.9956],[-118.3125,41.9958],[-118.2341,41.9963],[-118.2137,41.9964],[-118.1952,41.9965],[-118.155,41.9967],[-118.1352,41.9968],[-118.0784,41.9971],[-118.0426,41.9974],[-118.0191,41.9974],[-117.9264,41.9979],[-117.8289,41.9981],[-117.8066,41.9981],[-117.7733,41.9982],[-117.7726,41.9982],[-117.7152,41.9982],[-117.7083,41.9983],[-117.6694,41.9983],[-117.6509,41.9984],[-117.6164,41.9984],[-117.612,41.9984],[-117.5582,41.9987],[-117.53,41.9987],[-117.5038,41.9988],[-117.4899,41.9988],[-117.4003,41.9984],[-117.2864,41.9985],[-117.2307,41.9991],[-117.0298,42.0003],[-117.0293,42.0003]]]},\"properties\":{\"name\":\"Humboldt\",\"state\":\"NV\"}}]}","volume":"16","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbd7fe4b08c986b32905f","contributors":{"authors":[{"text":"Zielinski, R. A. 0000-0002-4047-5129","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":106930,"corporation":false,"usgs":true,"family":"Zielinski","given":"R.","email":"","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":361778,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70011860,"text":"70011860 - 1982 - Hydrogeochemical prospecting for porphyry copper deposits in the tropical-marine climate of Puerto Rico","interactions":[],"lastModifiedDate":"2025-04-09T15:02:15.596022","indexId":"70011860","displayToPublicDate":"1982-06-04T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2302,"text":"Journal of Geochemical Exploration","active":true,"publicationSubtype":{"id":10}},"title":"Hydrogeochemical prospecting for porphyry copper deposits in the tropical-marine climate of Puerto Rico","docAbstract":"<p>A hydrogeochemical survey utilizing waters from streams and springs was conducted in the area of two known porphyry copper deposits in the tropical-marine climate of westcentral Puerto Rico. The most important pathfinder for regional hydrogeochemical surveys is sulfate which reflects the associated pyrite mineralization. Because of increased mobility due to intense chemical weathering and the low pH environment, dissolved copper can also be used as a pathfinder for regional surveys and has the advantage of distinguishing barren pyrite from pyrite associated with copper mineralization. For follow-up surveys, the most important pathfinders are copper, sulfate, pH, zinc, and fluoride. High concentrations of dissolved copper and moderate concentrations of sulfate is a diagnostic indication of nearby sources of copper minerals. </p><p>An understanding of the geochemical processes taking place in the streambeds and the weathering environment, such as the precipitation of secondary copper minerals, contributes to the interpretation of the geochemical data and the selection of the most favorable areas for further exploration.&nbsp;</p>","largerWorkType":{"id":2,"text":"Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0375-6742(82)90011-5","usgsCitation":"Miller, W.R., Ficklin, W.H., and Learned, R.E., 1982, Hydrogeochemical prospecting for porphyry copper deposits in the tropical-marine climate of Puerto Rico: Journal of Geochemical Exploration, v. 16, no. 3, p. 217-233, https://doi.org/10.1016/0375-6742(82)90011-5.","productDescription":"17 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R.","contributorId":92239,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":362141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ficklin, W. H.","contributorId":89517,"corporation":false,"usgs":true,"family":"Ficklin","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":362140,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Learned, R. E.","contributorId":9638,"corporation":false,"usgs":true,"family":"Learned","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":362139,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70209997,"text":"70209997 - 1982 - Application of wave field continuation to the inversion of refraction data","interactions":[],"lastModifiedDate":"2020-05-08T14:10:32.738175","indexId":"70209997","displayToPublicDate":"1982-05-08T09:04:36","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2314,"text":"Journal of Geophysical Research B: Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Application of wave field continuation to the inversion of refraction data","docAbstract":"<div class=\"article-section__content en main\"><p>Three examples of the inversion of refraction data by downward continuation illustrate the applicability of the method to field data. The first example is a refraction profile from the Mojave Desert, California. These data are spatially aliased and contain clear evidence of lateral inhomogeneity. The inversion in this case produces a broken image in the slowness‐depth domain due to the lateral inhomogeneity, but a useful average velocity model is still obtained. The second example is a shallow marine reflection profile. Here, the truncation effects due to the finite horizontal aperture of the recording cable produce artifacts in the slowness‐depth domain. The velocity model is, however, distinct from these artifacts, and the presence of strong precritical reflections aids in the inversion. The third example is another shallow marine reflection profile. The inversion of these data illustrate the utilization of constraints provided by multiples as well as primary arrivals.</p></div>","conferenceLocation":"","language":"English","publisher":"Wiley","doi":"10.1029/JB087iB02p00927","usgsCitation":"McMechan, G.A., Clayton, R.W., and Mooney, W.D., 1982, Application of wave field continuation to the inversion of refraction data: Journal of Geophysical Research B: Solid Earth, v. 87, no. B2, p. 927-935, https://doi.org/10.1029/JB087iB02p00927.","productDescription":"9 p.","startPage":"927","endPage":"935","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"links":[{"id":480252,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1029/jb087ib02p00927","text":"External Repository"},{"id":374574,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"B2","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","contributors":{"authors":[{"text":"McMechan, G. A.","contributorId":54647,"corporation":false,"usgs":true,"family":"McMechan","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":788749,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clayton, Robert W.","contributorId":202752,"corporation":false,"usgs":false,"family":"Clayton","given":"Robert","email":"","middleInitial":"W.","affiliations":[{"id":7218,"text":"California Institute of Technology","active":true,"usgs":false}],"preferred":false,"id":788750,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mooney, Walter D. 0000-0002-5310-3631 mooney@usgs.gov","orcid":"https://orcid.org/0000-0002-5310-3631","contributorId":3194,"corporation":false,"usgs":true,"family":"Mooney","given":"Walter","email":"mooney@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":788751,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70208962,"text":"70208962 - 1982 - Mid-Paleozoic age of the Roberts thrust unsettled by new data from northern Nevada ","interactions":[],"lastModifiedDate":"2020-03-09T13:22:00","indexId":"70208962","displayToPublicDate":"1982-03-09T13:10:01","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Mid-Paleozoic age of the Roberts thrust unsettled by new data from northern Nevada ","docAbstract":"<p><span>The Roberts thrust is a major thrust in Nevada on which Ordovician to Devonian siliceous facies rocks were carried more than 80 km eastward over contemporaneous carbonate facies. For more than two decades, a mid-Paleozoic age for this structure has been widely accepted. The bases for dating the thrust are (1) the assumption that the Roberts thrust formed at the time of the Antler orogeny—a reliably dated mid-Paleozoic event, and (2) the concept of an overlapping assemblage consisting of sedimentary strata deposited on both the allochthon and autochthon. The first assumption is unproved, and the second relies on another assumption: that the overlap assemblage was not cut and telescoped by the Roberts thrust. In the years since a mid-Paleozoic age for the Roberts thrust became widely accepted, much new information on the stratigraphy and facies relations of Mississippian rocks in northern Nevada has accumulated. One interpretation of these new data suggests that in the Pinon Range, where a mid-Paleozoic age for the thrust was most convincingly displayed, the overlap assemblage actually may have been cut by a major thrust that juxtaposed contrasting facies of Mississippian rocks. If so, the principal evidence used to date the Roberts thrust is compromised, and the time has come for an agonizing reappraisal of all evidence bearing on the question. A mid-Paleozoic age can no longer be taken for granted, and a post-Paleozoic age cannot be ruled out.</span></p>","language":"English","publisher":"GSA","doi":"10.1130/0091-7613(1982)10<298:MAOTRT>2.0.CO;2","usgsCitation":"Ketner, K.B., and Smith, F.J., 1982, Mid-Paleozoic age of the Roberts thrust unsettled by new data from northern Nevada : Geology, v. 10, no. 6, p. 298-303, https://doi.org/10.1130/0091-7613(1982)10<298:MAOTRT>2.0.CO;2.","productDescription":"6 p.","startPage":"298","endPage":"303","costCenters":[],"links":[{"id":373016,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Northern Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.52099609375,\n              39.317300373271024\n            ],\n            [\n              -113.99414062499999,\n              39.26628442213066\n            ],\n            [\n              -114.12597656249999,\n              42.01665183556825\n            ],\n            [\n              -117.48779296875,\n              42.00032514831621\n            ],\n            [\n              -117.72949218749999,\n              39.11301365149975\n            ],\n            [\n              -116.52099609375,\n              39.317300373271024\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"10","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ketner, Keith B.","contributorId":957,"corporation":false,"usgs":true,"family":"Ketner","given":"Keith","email":"","middleInitial":"B.","affiliations":[],"preferred":true,"id":784207,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Fred J. Jr.","contributorId":30864,"corporation":false,"usgs":true,"family":"Smith","given":"Fred","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":784208,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221778,"text":"5221778 - 1982 - Use of blood levels to infer carcass levels of contaminants","interactions":[],"lastModifiedDate":"2023-12-12T17:35:34.427962","indexId":"5221778","displayToPublicDate":"1982-03-01T12:19:26","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":887,"text":"Archives of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"Use of blood levels to infer carcass levels of contaminants","docAbstract":"<p><span>Inferences may be made about the carcass levels of a contaminant based on the contaminant level in blood samples. A method is given for comparing such populations that utilizes bivariate normal distributions and their principal axes, thereby avoiding a dilemma arising from the use of regression techniques. Confidence intervals and power calculations are given. Data from captive barn owls provide partial justification for the use of this method.</span></p>","language":"English","publisher":"Springer","doi":"10.1007/BF01054901","usgsCitation":"Hensler, G.L., and Stout, W., 1982, Use of blood levels to infer carcass levels of contaminants: Archives of Environmental Contamination and Toxicology, v. 11, no. 2, p. 235-238, https://doi.org/10.1007/BF01054901.","productDescription":"4 p.","startPage":"235","endPage":"238","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197418,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e272a","contributors":{"authors":[{"text":"Hensler, Gary L.","contributorId":23111,"corporation":false,"usgs":true,"family":"Hensler","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":334659,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stout, William C.","contributorId":56756,"corporation":false,"usgs":false,"family":"Stout","given":"William C.","affiliations":[],"preferred":false,"id":334660,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70208103,"text":"70208103 - 1982 - A late Pleistocene glacial chronology for the southern Brooks Range: Stratigraphic record and regional significance","interactions":[],"lastModifiedDate":"2020-01-27T14:52:38","indexId":"70208103","displayToPublicDate":"1982-01-27T14:44:37","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"A late Pleistocene glacial chronology for the southern Brooks Range: Stratigraphic record and regional significance","docAbstract":"<p>Radiocarbon dates from 11 measured sections in the Koyukuk region provide a chronology of the last Pleistocene glaciation. Glaciers were advancing strongly by 24,000 yr ago; they built moraines near the south flank of the Brooks Range, retreated briefly about 22,000 to 20,000 yr B.P., then readvanced at least one more time into their terminal zones. Glaciation was accompanied by alluviation of the Koyukuk and Kobuk drainage systems and by periglacial processes that resemble those taking place today farther north and at higher altitudes. Moraines near the south flank of the range were being revegetated by 13,500 yr B.P. A strong final readvance into end-moraine belts of some northern valleys occurred about 13,000 to 12,500 yr ago, and this event may be synchronous with less extensive glacier readvances in upper valleys of the Koyukuk region. Upper valleys were largely deglaciated by 11,800 yr B.P.</p><p>Dated Stratigraphic sections from the northern Alaska Range show similar ages for initiation and close of glaciation and also suggest a possible interstadial episode about 20,000 yr ago. Scanty records of fluctuations during ice wastage probably reflect the general scarcity of datable wood, peat, and organic soils between about 19,500 and 13,500 yr ago. The Brooks Range and Alaska Range chronologies closely approximate glacial successions determined else-where in eastern Beringia and in Siberia. Advance and retreat of glaciers throughout this region evidently were associated with widespread climatic changes that also controlled the late Wisconsin history of the Laurentide ice sheet.</p><p>The Itkillik II and late Itkillik phases of former usage are part of a single glaciation that was entirely separate from the preceding Itkillik I ice advance. For this reason, the local term \"Walker Lake Glaciation\" is here extended to the last major glaciation of the entire southern Brooks Range, and use of Itkillik phases should be discontinued. The term \"Itkillik Glaciation\" is hereby restricted to the next older ice advance, in accord with its original definition.</p><p>Cold and dry conditions during the last glaciation of eastern Beringia are indicated by (1) relatively small mountain glaciers, (2) slight (200-m) depression of glaciation limits below modern values, (3) periglacial features indicating severe frost action on slopes with little protective plant cover, (4) widespread accretion of eolian sand, (5) low pollen influx rates, (6) scarcity of radiocarbon-datable organic remains, and (7) general absence of carbonaceous paleosols. Plant growth may have been much more restricted than generally believed, with relatively low capacity to support grazing animals and human hunting bands.</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1982)93<700:ALPGCF>2.0.CO;2","usgsCitation":"Hamilton, T.D., 1982, A late Pleistocene glacial chronology for the southern Brooks Range: Stratigraphic record and regional significance: GSA Bulletin, v. 93, no. 8, p. 700-716, https://doi.org/10.1130/0016-7606(1982)93<700:ALPGCF>2.0.CO;2.","productDescription":"17 p.","startPage":"700","endPage":"716","costCenters":[],"links":[{"id":371601,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Southern Brooks Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.796875,\n              66.51326044311185\n            ],\n            [\n              -148.88671874999997,\n              66.51326044311185\n            ],\n            [\n              -148.88671874999997,\n              68.65655498475735\n            ],\n            [\n              -156.796875,\n              68.65655498475735\n            ],\n            [\n              -156.796875,\n              66.51326044311185\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"93","issue":"8","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hamilton, T. D.","contributorId":36921,"corporation":false,"usgs":true,"family":"Hamilton","given":"T.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":780471,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8841,"text":"ofr82772 - 1982 - Hydrologic data from monitoring of saline-water intrusion in the Cape Coral area, Lee County, Florida","interactions":[],"lastModifiedDate":"2022-01-05T16:13:49.843023","indexId":"ofr82772","displayToPublicDate":"1982-01-01T22:05:00","publicationYear":"1982","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":"82-772","title":"Hydrologic data from monitoring of saline-water intrusion in the Cape Coral area, Lee County, Florida","docAbstract":"<p>As a result of declining water levels and saline-water intrusion in the Cape Coral area, the U.S. Geological Survey in cooperation with the City of Cape Coral established a monitoring well network in Cape Coral and adjacent areas in 1978-79. The network was designed to provide indication of lateral movement of saline water in the upper part of the Hawthorn Formation; to provide trends in water levels; and to provide background data from: (1) the aquifer in the upper part of the Hawthorn Formation; (2) the aquifer in the lower part of the Hawthorn Formation and upper part of the Tampa Limestone; and (3) the surficial aquifer. The monitoring well network consists of 77 wells.</p><p>Data collected in this network since 1978, as well as data collected from selected wells in the network prior to 1978, are compiled in this report. These data include water-quality data from 69 wells, water-level data from 29 wells, and lithologic logs from 18 wells. Other data compiled in this report include municipal pumpage and rainfall data supplied by the City of Cape Coral.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82772","collaboration":"Prepared in cooperation with the City of Cape Coral","usgsCitation":"Fitzpatrick, D.J., 1982, Hydrologic data from monitoring of saline-water intrusion in the Cape Coral area, Lee County, Florida: U.S. Geological Survey Open-File Report 82-772, v, 48 p., https://doi.org/10.3133/ofr82772.","productDescription":"v, 48 p.","numberOfPages":"53","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":142006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0772/report-thumb.jpg"},{"id":36416,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0772/ofr82772.pdf","text":"Report","size":"635 KB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Florida","county":"Lee County","city":"Cape Coral","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.28759765625,\n              26.35988109485539\n            ],\n            [\n              -81.54327392578125,\n              26.35988109485539\n            ],\n            [\n              -81.54327392578125,\n              26.814266197561462\n            ],\n            [\n              -82.28759765625,\n              26.814266197561462\n            ],\n            [\n              -82.28759765625,\n              26.35988109485539\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607761","contributors":{"authors":[{"text":"Fitzpatrick, Daniel J.","contributorId":31367,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Daniel","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":158420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":901,"text":"901 - 1982 - Water resources data","interactions":[],"lastModifiedDate":"2014-07-08T15:51:29","indexId":"901","displayToPublicDate":"1982-01-01T15:48:56","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":345,"text":"Annual Report","active":false,"publicationSubtype":{"id":6}},"title":"Water resources data","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"U.S. Geological Survey water-supply paper","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S Geological Survey","doi":"10.3133/901","issn":"0363-1974","collaboration":"Prepared in cooperation with the Nebraska Dept. of Water Resources, the Conservation and Survey Division of the University of Nebraska, the Nebraska Dept. of Environmental Control, and with other state and federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data: Annual Report, https://doi.org/10.3133/901.","costCenters":[],"links":[{"id":289569,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nebraska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.0535,39.9999 ], [ -104.0535,43.0017 ], [ -95.3083,43.0017 ], [ -95.3083,39.9999 ], [ -104.0535,39.9999 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bd130ce4b00cbf31f72386","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":527816,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":900,"text":"900 - 1982 - Water resources data","interactions":[],"lastModifiedDate":"2014-07-08T15:46:57","indexId":"900","displayToPublicDate":"1982-01-01T15:43:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":345,"text":"Annual Report","active":false,"publicationSubtype":{"id":6}},"title":"Water resources data","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"U.S. Geological Survey water-supply paper","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/900","issn":"0364-4073","collaboration":"Prepared in cooperation with the state of Montana and other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data: Annual Report, https://doi.org/10.3133/900.","costCenters":[],"links":[{"id":289568,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,44.3582 ], [ -116.05,49.0014 ], [ -104.0396,49.0014 ], [ -104.0396,44.3582 ], [ -116.05,44.3582 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bd130ce4b00cbf31f72384","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":527815,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":899,"text":"899 - 1982 - Water resources data","interactions":[],"lastModifiedDate":"2014-07-08T15:41:46","indexId":"899","displayToPublicDate":"1982-01-01T15:39:22","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":345,"text":"Annual Report","active":false,"publicationSubtype":{"id":6}},"title":"Water resources data","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"U.S. Geological Survey water-supply paper","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/899","issn":"0741-6296","collaboration":"In cooperation with Missouri Dept. of Natural Resources, Division of Geology and Land Survey and Division of Environmental Quality, Missouri State Highway Commission and other State and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data: Annual Report, https://doi.org/10.3133/899.","costCenters":[],"links":[{"id":289567,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Missouri","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.7747,35.9957 ], [ -95.7747,40.6136 ], [ -89.1045,40.6136 ], [ -89.1045,35.9957 ], [ -95.7747,35.9957 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bd130be4b00cbf31f72382","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":527814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":897,"text":"897 - 1982 - Water resources data","interactions":[],"lastModifiedDate":"2014-07-08T15:32:17","indexId":"897","displayToPublicDate":"1982-01-01T15:29:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":345,"text":"Annual Report","active":false,"publicationSubtype":{"id":6}},"title":"Water resources data","docAbstract":"No abstract available.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"U.S. Geological Survey water-supply paper","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/897","issn":"0364-4383","collaboration":"Prepared in cooperation with the Minnesota Dept. of Natural Resources, Division of Waters; the Minnesota Dept. of Transportation; and with other state, municipal, and federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data: Annual Report, https://doi.org/10.3133/897.","costCenters":[],"links":[{"id":289563,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Minnesota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.24,43.5 ], [ -97.24,49.38 ], [ -89.49,49.38 ], [ -89.49,43.5 ], [ -97.24,43.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53bd1309e4b00cbf31f7237e","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":527812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":70039237,"text":"70039237 - 1982 - Land Use and land cover and associated maps","interactions":[],"lastModifiedDate":"2012-08-03T01:02:04","indexId":"70039237","displayToPublicDate":"1982-01-01T11:55:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Land Use and land cover and associated maps","docAbstract":"The Geological Survey is compiling land use and land cover and associated maps for the entire United States. Land use refers to man's activities which are directly related to the land. Land cover describes the vegetation, water, natural surface, and artificial constructions at the land surface. These maps will help satisfy a longstanding need for a consistent level of detail, standardization of categories, and appropriate use of scales of compilation for a type of data frequently used by land use planners, land managers, resource management planners, and others.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039237","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Land Use and land cover and associated maps: General Information Product, 5 p. (9 columns), https://doi.org/10.3133/70039237.","productDescription":"5 p. (9 columns)","costCenters":[],"links":[{"id":261445,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039237/report.pdf"},{"id":261446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039237/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4198e4b0c8380cd6563d","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":535267,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":27386,"text":"wri8222 - 1982 - A technique for estimating time of concentration and storage coefficient values for Illinois streams","interactions":[],"lastModifiedDate":"2021-07-13T21:36:39.900045","indexId":"wri8222","displayToPublicDate":"1982-01-01T11:30:00","publicationYear":"1982","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":"82-22","displayTitle":"A Technique for Estimating Time of Concentration and Storage Coefficient Values for Illinois Streams","title":"A technique for estimating time of concentration and storage coefficient values for Illinois streams","docAbstract":"<p>Values of the unit hydrograph parameters time of concentration (<i>TC</i>) and storage coefficient (<i>R</i>) can be estimated for streams in Illinois by a two-step technique developed from data for 98 gaged basins in the State. 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B.","contributorId":59005,"corporation":false,"usgs":true,"family":"Graf","given":"Julia","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":198025,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garklavs, George","contributorId":87139,"corporation":false,"usgs":true,"family":"Garklavs","given":"George","email":"","affiliations":[],"preferred":false,"id":198026,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oberg, Kevin A. kaoberg@usgs.gov","contributorId":928,"corporation":false,"usgs":true,"family":"Oberg","given":"Kevin","email":"kaoberg@usgs.gov","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":198024,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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