The robust design of Pollock (1982) was used to estimate parameters of a Maryland M. pennsylvanicus population. Closed model tests provided strong evidence of heterogeneity of capture probability, and model M eta (Otis et al., 1978) was selected as the most appropriate model for estimating population size. The Jolly-Seber model goodness-of-fit test indicated rejection of the model for this data set, and the M eta estimates of population size were all higher than the Jolly-Seber estimates. Both of these results are consistent with the evidence of heterogeneous capture probabilities. The authors thus used M eta estimates of population size, Jolly-Seber estimates of survival rate, and estimates of birth-immigration based on a combination of the population size and survival rate estimates. Advantages of the robust design estimates for certain inference procedures are discussed, and the design is recommended for future small mammal capture-recapture studies directed at estimation.
","language":"English","publisher":"Polska Akademia Nauk","doi":"10.4098/AT.arch.84-34","usgsCitation":"Nichols, J.D., Pollock, K.H., and Hines, J., 1984, The use of a robust capture-recapture design in small mammal population studies: A field example with Microtus pennsylvanicus: Acta Theriologica, v. 29, no. 30, p. 357-365, https://doi.org/10.4098/AT.arch.84-34.","productDescription":"9 p.","startPage":"357","endPage":"365","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":480187,"rank":3,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4098/at.arch.84-34","text":"Publisher Index Page"},{"id":197295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":351387,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://rcin.org.pl/dlibra/docmetadata?id=11103"}],"volume":"29","issue":"30","noUsgsAuthors":false,"publicationDate":"1984-12-20","publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db6349e4","contributors":{"authors":[{"text":"Nichols, James D. 0000-0002-7631-2890 jnichols@usgs.gov","orcid":"https://orcid.org/0000-0002-7631-2890","contributorId":140652,"corporation":false,"usgs":true,"family":"Nichols","given":"James","email":"jnichols@usgs.gov","middleInitial":"D.","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":336359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pollock, Kenneth H.","contributorId":8590,"corporation":false,"usgs":false,"family":"Pollock","given":"Kenneth","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":336361,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hines, James E. jhines@usgs.gov","contributorId":3506,"corporation":false,"usgs":true,"family":"Hines","given":"James E.","email":"jhines@usgs.gov","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":336360,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5221926,"text":"5221926 - 1984 - Home-range formation and dispersal of deer in northeastern Minnesota","interactions":[],"lastModifiedDate":"2024-07-01T11:21:43.261736","indexId":"5221926","displayToPublicDate":"2010-06-16T12:19:24","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"Home-range formation and dispersal of deer in northeastern Minnesota","docAbstract":"Eleven white-tailed (Odocoileus virginianus) does and their offspring (10 male and 6 female fawns) were radio-tracked for up to 56 months (2,725 total deer locations) in Minnesota's Superior National Forest from November 1974 through August 1983. All fawns wintered in yards with their does and migrated in spring to their does' summer ranges where they then separated from the does. By 17 months of age, seven males had established new summer ranges up to 9.6 km away, whereas the other three used the same summer ranges as their does, up to at least 29 months of age. One male established a new winter range, but six others continued to use the winter ranges of their does. The female fawns used the same summer range as their does, or areas immediately adjacent, and migrated to and from the same winter ranges, some with their does, for up to 3 years of age. The one female that we followed beyond this age migrated separately to and from the same winter yard during her fifth year. The data fit a hypothesis that non-incestuous inbreeding is common in vertebrates.
","language":"English","publisher":"Oxford Academic","doi":"10.2307/1380839","usgsCitation":"Nelson, M., and Mech, L., 1984, Home-range formation and dispersal of deer in northeastern Minnesota: Journal of Mammalogy, v. 65, no. 4, p. 567-575, https://doi.org/10.2307/1380839.","productDescription":"9 p.","startPage":"567","endPage":"575","numberOfPages":"9","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194153,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"65","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62beb7","contributors":{"authors":[{"text":"Nelson, M.E.","contributorId":102021,"corporation":false,"usgs":true,"family":"Nelson","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":335046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mech, L.D. 0000-0003-3944-7769","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":75466,"corporation":false,"usgs":false,"family":"Mech","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":335045,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5223690,"text":"5223690 - 1984 - Estimating prey size and number in crayfish-eating snakes, genus Regina","interactions":[],"lastModifiedDate":"2012-02-02T00:15:43","indexId":"5223690","displayToPublicDate":"2010-06-16T12:19:21","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1892,"text":"Herpetologica","active":true,"publicationSubtype":{"id":10}},"title":"Estimating prey size and number in crayfish-eating snakes, genus Regina","docAbstract":" Snakes of the genus Regina feed almost exclusively on crayfish. The paired, symmetrical gastroliths of crayfish are not digested and are detectable from x-rays of the snake. Gastrolith length is directly proportional to carapace length and can be obtained from x-rays. Carapace length can be converted to kcal of ingested energy. Using these relationships and repeated captures of radio-telemetered Regina, estimates of food consumption and energy intake by freeliving snakes are feasible. New information on prey selectivity, feeding behavior, and predator-prey size relations in Regina grahami and R. septemvittata are presented and compared with similar data for other snakes.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Herpetologica","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Godley, J., McDiarmid, R., and Rojas, N., 1984, Estimating prey size and number in crayfish-eating snakes, genus Regina: Herpetologica, v. 40, no. 1, p. 82-88.","productDescription":"82-88","startPage":"82","endPage":"88","numberOfPages":"7","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18247,"rank":200,"type":{"id":11,"text":"Document"},"url":"https://www.jstor.org/stable/3892464","linkFileType":{"id":5,"text":"html"}}],"volume":"40","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc8cd","contributors":{"authors":[{"text":"Godley, J.S.","contributorId":15731,"corporation":false,"usgs":true,"family":"Godley","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":339273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDiarmid, R.W.","contributorId":15130,"corporation":false,"usgs":true,"family":"McDiarmid","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":339272,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rojas, N.N.","contributorId":41555,"corporation":false,"usgs":true,"family":"Rojas","given":"N.N.","email":"","affiliations":[],"preferred":false,"id":339274,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5222870,"text":"5222870 - 1984 - Testing for variation in taxonomic extinction probabilities: A suggested methodology and some results","interactions":[],"lastModifiedDate":"2025-06-05T16:31:57.200057","indexId":"5222870","displayToPublicDate":"2010-06-16T12:19:19","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3001,"text":"Paleobiology","active":true,"publicationSubtype":{"id":10}},"title":"Testing for variation in taxonomic extinction probabilities: A suggested methodology and some results","docAbstract":"Several important questions in evolutionary biology and paleobiology involve sources of variation in extinction rates. In all cases of which we are aware, extinction rates have been estimated from data in which the probability that an observation (e.g., a fossil taxon) will occur is related both to extinction rates and to what we term encounter probabilities. Any statistical method for analyzing fossil data should at a minimum permit separate inferences on these two components. We develop a method for estimating taxonomic extinction rates from stratigraphic range data and for testing hypotheses about variability in these rates. We use this method to estimate extinction rates and to test the hypothesis of constant extinction rates for several sets of stratigraphic range data. The results of our tests support the hypothesis that extinction rates varied over the geologic time periods examined. We also present a test that can be used to identify periods of high or low extinction probabilities and provide an example using Phanerozoic invertebrate data. Extinction rates should be analyzed using stochastic models, in which it is recognized that stratigraphic samples are random variates and that sampling is imperfect.
","language":"English","publisher":"Cambridge University Press","doi":"10.1017/S0094837300008307","usgsCitation":"Conroy, M., and Nichols, J., 1984, Testing for variation in taxonomic extinction probabilities: A suggested methodology and some results: Paleobiology, v. 10, no. 3, p. 328-337, https://doi.org/10.1017/S0094837300008307.","productDescription":"10 p.","startPage":"328","endPage":"337","numberOfPages":"10","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193468,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationDate":"2016-02-08","publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b8a9","contributors":{"authors":[{"text":"Conroy, M.J.","contributorId":84690,"corporation":false,"usgs":true,"family":"Conroy","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":337348,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nichols, J.D. 0000-0002-7631-2890","orcid":"https://orcid.org/0000-0002-7631-2890","contributorId":14332,"corporation":false,"usgs":true,"family":"Nichols","given":"J.D.","affiliations":[],"preferred":false,"id":337347,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5221980,"text":"5221980 - 1984 - DDE in birds' eggs: Comparisons of two methods for estimating critical levels","interactions":[],"lastModifiedDate":"2012-02-02T00:15:10","indexId":"5221980","displayToPublicDate":"2010-06-16T12:19:19","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"DDE in birds' eggs: Comparisons of two methods for estimating critical levels","docAbstract":"The sample egg technique and eggshell thickness-residue regression analysis were comparatively evaluated as tools in estimating critical levels of DDE in birds? eggs that seriously affect reproductive successa nd population starts....In comparing critical values of DDE that were derived from the two methods, the estimates were lower using the sample egg technique for both the Brown Pelican (3 ?g/g vs 8 ?g/g) and the Black-crowned Night-Heron (12?g/g/ vs 54 ?g/g) assuming a critical value of eggshell thinning at 20%....Extension of the regression line beyond the eggshell thickness-DDE residue data base is likely to result in spurious critical values of DDE. When sufficient thickness and residue data are available for estimating critical values of DDE from the regression equation, the estimates are meaningful but are likely to be inflated because adverse effects unrelated to eggshell thinning such as parental behavior and embryotoxicity unrelated to eggshell deficiencies are not taken into account.....Establishing critical levels of pollutants in eggs and tissues is a necessary procedure in assessing effects of these chemicals on individuals and populations of sensitive species. There are inherent difficulties in quantifying the effects of any pollutant on population trends and declines in productivity. The sample egg technique is apparently a more sensitive method for estimating critical levels of DDE, but some subjective interpretation is required for results obtained by both methods.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Blus, L.J., 1984, DDE in birds' eggs: Comparisons of two methods for estimating critical levels: The Wilson Bulletin, v. 96, no. 2, p. 268-276.","productDescription":"268-276","startPage":"268","endPage":"276","numberOfPages":"9","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":18196,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://elibrary.unm.edu/sora/Wilson/v096n02/p0268-p0276.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":196333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"96","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e539","contributors":{"authors":[{"text":"Blus, L. J.","contributorId":38116,"corporation":false,"usgs":true,"family":"Blus","given":"L.","middleInitial":"J.","affiliations":[],"preferred":false,"id":335188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5221972,"text":"5221972 - 1984 - A general methodology for maximum likelihood inference from band-recovery data","interactions":[],"lastModifiedDate":"2023-11-06T12:59:29.433193","indexId":"5221972","displayToPublicDate":"2010-06-16T12:19:19","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1039,"text":"Biometrics","active":true,"publicationSubtype":{"id":10}},"title":"A general methodology for maximum likelihood inference from band-recovery data","docAbstract":"A numerical procedure is described for obtaining maximum likelihood estimates and associated maximum likelihood inference from band- recovery data. The method is used to illustrate previously developed one-age-class band-recovery models, and is extended to new models, including the analysis with a covariate for survival rates and variable-time-period recovery models. Extensions to R-age-class band- recovery, mark-recapture models, and twice-yearly marking are discussed. A FORTRAN program provides computations for these models.","language":"English","publisher":"International Biometric Society","doi":"10.2307/2530917","usgsCitation":"Conroy, M., and Williams, B.K., 1984, A general methodology for maximum likelihood inference from band-recovery data: Biometrics, v. 40, no. 3, p. 739-748, https://doi.org/10.2307/2530917.","productDescription":"10 p.","startPage":"739","endPage":"748","numberOfPages":"10","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196905,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae73f","contributors":{"authors":[{"text":"Conroy, M.J.","contributorId":84690,"corporation":false,"usgs":true,"family":"Conroy","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":335163,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, B. Kenneth","contributorId":107798,"corporation":false,"usgs":true,"family":"Williams","given":"B.","email":"","middleInitial":"Kenneth","affiliations":[],"preferred":false,"id":335164,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":5221981,"text":"5221981 - 1984 - Simulation analyses of space use: Home range estimates, variability, and sample size","interactions":[],"lastModifiedDate":"2018-01-02T20:22:04","indexId":"5221981","displayToPublicDate":"2010-06-16T12:19:16","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":979,"text":"Behavior Research Methods, Instruments, and Computers","onlineIssn":"1532-5970","printIssn":"0743-3808","active":true,"publicationSubtype":{"id":10}},"title":"Simulation analyses of space use: Home range estimates, variability, and sample size","docAbstract":"Simulations of space use by animals were run to determine the relationship among home range area estimates, variability, and sample size (number of locations). As sample size increased, home range size increased asymptotically, whereas variability decreased among mean home range area estimates generated by multiple simulations for the same sample size. Our results suggest that field workers should ascertain between 100 and 200 locations in order to estimate reliably home range area. In some cases, this suggested guideline is higher than values found in the few published studies in which the relationship between home range area and number of locations is addressed. Sampling differences for small species occupying relatively small home ranges indicate that fewer locations may be sufficient to allow for a reliable estimate of home range. Intraspecific variability in social status (group member, loner, resident, transient), age, sex, reproductive condition, and food resources also have to be considered, as do season, habitat, and differences in sampling and analytical methods. Comparative data still are needed.
","language":"English","publisher":"Springer","doi":"10.3758/BF03201046","usgsCitation":"Bekoff, M., and Mech, L.D., 1984, Simulation analyses of space use: Home range estimates, variability, and sample size: Behavior Research Methods, Instruments, and Computers, v. 16, no. 1, p. 32-37, https://doi.org/10.3758/BF03201046.","productDescription":"6 p.","startPage":"32","endPage":"37","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":480188,"rank":1,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3758/bf03201046","text":"Publisher Index Page"},{"id":197590,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"16","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49aee4b07f02db5c7a1f","contributors":{"authors":[{"text":"Bekoff, Marc","contributorId":113207,"corporation":false,"usgs":true,"family":"Bekoff","given":"Marc","email":"","affiliations":[],"preferred":false,"id":335189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mech, L. David 0000-0003-3944-7769 david_mech@usgs.gov","orcid":"https://orcid.org/0000-0003-3944-7769","contributorId":2518,"corporation":false,"usgs":true,"family":"Mech","given":"L.","email":"david_mech@usgs.gov","middleInitial":"David","affiliations":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"preferred":true,"id":335190,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70039514,"text":"70039514 - 1984 - Geographic Names Information System","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039514","displayToPublicDate":"2008-01-23T16:11:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Geographic Names Information System","docAbstract":"The Geographic Names Information System (GNIS) is an automated data system developed by the U.S. Geological Survey (USGS) to standardize and disseminate information on geographic names. GNIS provides primary information for all known places, features, and areas in the United States identified by a proper name. The information in the system can be manipulated to meet varied needs. You can incorporate information from GNIS into your own data base for special applications.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039514","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Geographic Names Information System, 2 p., https://doi.org/10.3133/70039514.","productDescription":"2 p.","numberOfPages":"2","costCenters":[{"id":409,"text":"National Cartographic Information Center","active":false,"usgs":true}],"links":[{"id":261642,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039514/report.pdf"},{"id":261643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039514/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1756e4b0c8380cd5548d","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":535337,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":80063,"text":"wri82508 - 1984 - Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington","interactions":[],"lastModifiedDate":"2012-02-10T00:11:44","indexId":"wri82508","displayToPublicDate":"2007-06-28T00:00:00","publicationYear":"1984","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":"82-508","title":"Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington","docAbstract":"This study provides basic data on ground-water quality throughout the State. It is intended for uses in planning and management by agencies and individuals who have responsibility for or interest in, public health and welfare. It also provides a basis for directing future studies of ground-water quality toward areas where ground-water quality problems may already exist. The information presented is a compilation of existing data from numerous sources including: the Washington Departments of Ecology and Social and Health Services, the Environmental Protection Agency, as well as many other local, county, state and federal agencies and private corporations. Only data on fluoride, nitrate, and dissolved-solids concentrations in ground water are presented, as these constituents are among those commonly used to determine the suitability of water for drinking or other purposes. They also reflect both natural and man-imposed effects on water quality and are the most readily available water-quality data for the State of Washington. The percentage of wells with fluoride, nitrate, or dissolved-solids concentrations exceeding U.S. Environmental Protection Agency Primary and Secondary Drinking Water Regulations were about 1, about 3, and about 3, respectively. Most high concentrations occurred in widely separated wells. Two exceptions were: high concentrations of nitrate and dissolved solids in wells on the Hanford Department of Energy Facility and high concentrations of nitrate in the lower Yakima River basin. (USGS)","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri82508","collaboration":"Prepared in cooperation with the State of Washington Department of Ecology","usgsCitation":"Lum, W.E., and Turney, G.L., 1984, Fluoride, Nitrate, and Dissolved-Solids Concentrations in Ground Waters of Washington (WRI/OFR 82-508): U.S. Geological Survey Water-Resources Investigations Report 82-508, 4 Sheets (3 maps and 1 data sheet; each sheet 21 x 27 inches), https://doi.org/10.3133/wri82508.","productDescription":"4 Sheets (3 maps and 1 data sheet; each sheet 21 x 27 inches)","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":194716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":264344,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/0508/plate-1.pdf","size":"3794","linkFileType":{"id":1,"text":"pdf"}},{"id":264345,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/0508/plate-2.pdf","size":"3646","linkFileType":{"id":1,"text":"pdf"}},{"id":264346,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/0508/plate-3.pdf","size":"3745","linkFileType":{"id":1,"text":"pdf"}},{"id":264347,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/0508/plate-4.pdf","size":"3568","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -125,45 ], [ -125,49 ], [ -116,49 ], [ -116,45 ], [ -125,45 ] ] ] } } ] }","edition":"WRI/OFR 82-508","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec01","contributors":{"authors":[{"text":"Lum, W. E. II","contributorId":81504,"corporation":false,"usgs":true,"family":"Lum","given":"W.","suffix":"II","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":291610,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turney, Gary L.","contributorId":72446,"corporation":false,"usgs":true,"family":"Turney","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":291609,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":80038,"text":"wri83698 - 1984 - Hydrology of Area 62, Northern Great Plains and Rocky Mountain Coal Provinces, New Mexico and Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:41","indexId":"wri83698","displayToPublicDate":"2007-06-20T00:00:00","publicationYear":"1984","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":"83-698","title":"Hydrology of Area 62, Northern Great Plains and Rocky Mountain Coal Provinces, New Mexico and Arizona","docAbstract":"This report summarizes available hydrologic data for Area 62 and will aid leasing decisions, and the preparation and appraisal of environmental impact studies and mine-permit applications. Area 62 is located at the southern end of the Rocky Mountain Coal Province in parts of New Mexico and Arizona and includes approximately 9,500 square miles. Surface mining alters, at least temporarily, the environment; if the areas are unreclaimed, there can be long-term environmental consequences.\r\n\r\nThe land-ownership pattern in Area 62 is complicated. The checkerboard pattern created by several types of ownership makes effective management of these lands difficult.\r\n\r\nThe climate generally is semiarid with average annual precipitation ranging from 10 to 20 inches. Pinons, junipers, and grasslands cover most of the area, and much of it is used for grazing by livestock. Soils vary with landscape, differing from flood plains and hillslopes to mountain slopes.\r\n\r\nThe major structural features of this area were largely developed during middle Tertiary time. The main structural features are the southern San Juan Basin and the Mogollon slope. Coal-bearing rocks are present in four Cretaceous rock units of the Mesaverde Group: the Gallup Sandstone, the Dileo Coal Member, and the Gibson Coal Member of the Crevasse Canyon Formation, and the Cleary Coal Member of the Menefee Formation.\r\n\r\nArea 62 is drained by Black Creek, the Puerco River, the Zuni River, Carrizo Wash-Largo Creek, and the Rio San Jose. Only at the headwaters of the Zuni River is the flow perennial. The streamflow-gaging station network consists of 25 stations operated for a variety of needs. Streamflow changes throughout the year with variation related directly to rainfall and snowmelt. Base flow in Area 62 is zero indicating no significant ground-water discharge. Mountainous areas contribute the highest mean annual runoff of 1.0 inch. Very few water-quality data are available for the surface-water stations. Of the nine surface-water stations that have water-quality data, only one has chemical analyses from more than 10 samples. Therefore, sufficient data to characterize the area in detail are not available. Suspended sediment data are available only for a few surface-\r\nwater stations in the area. Erosion rates generally are less than 1 acre-foot per square mile per year. Greater erosion rates are found within the badland areas.\r\n\r\nWater levels are periodically measured at 21 selected wells in Area 62. These observation wells are located mostly along the Rio San Jose and northeast of Gallup, New Mexico. The recharge to ground-water aquifers generally coincide with areas of greater precipitation in the mountainous areas. Depth to water below land surface is generally less than 200 feet. Well yields of 100 gallons per minute are common in most of the area.\r\n\r\nGround-water quality is variable both within each aquifer and between aquifers. Water quality generally is best near recharge areas.\r\n\r\nHistorical and current data related to stream discharge, water quality, and suspended sediment are available from computer files in the U.S. Geological Survey's National Water Data Storage and Retrieval System (WATSTORE) and through the National Water Data Exchange (NAWDEX).","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri83698","usgsCitation":"Roybal, F., Wells, J., Gold, R., and Flager, J., 1984, Hydrology of Area 62, Northern Great Plains and Rocky Mountain Coal Provinces, New Mexico and Arizona (WRI/OFR 83-698): U.S. Geological Survey Water-Resources Investigations Report 83-698, v, 66 p., https://doi.org/10.3133/wri83698.","productDescription":"v, 66 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0698/report-thumb.jpg"},{"id":91373,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0698/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110,34 ], [ -110,36 ], [ -107.5,36 ], [ -107.5,34 ], [ -110,34 ] ] ] } } ] }","edition":"WRI/OFR 83-698","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604a3c","contributors":{"authors":[{"text":"Roybal, F.E.","contributorId":62998,"corporation":false,"usgs":true,"family":"Roybal","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":291539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wells, J.G.","contributorId":85198,"corporation":false,"usgs":true,"family":"Wells","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":291541,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gold, R.L.","contributorId":97918,"corporation":false,"usgs":true,"family":"Gold","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":291542,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Flager, J.V.","contributorId":72799,"corporation":false,"usgs":true,"family":"Flager","given":"J.V.","email":"","affiliations":[],"preferred":false,"id":291540,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":77059,"text":"fwsobs82_10_73 - 1984 - Habitat Suitability Index Models: Gray partridge","interactions":[],"lastModifiedDate":"2022-02-09T15:12:21.326003","indexId":"fwsobs82_10_73","displayToPublicDate":"2006-07-19T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.73","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Gray partridge","docAbstract":"This report is part of the Habitat Suitability Index model series which provides\r\nhabitat information useful for impact assessment and habitat management. The\r\nHabitat Use Information section is largely constrained to those data that can be\r\nused to derive quantitative relationships between key environmental variables\r\nand habitat suitability. The habitat use information provides the foundation for\r\nthe HSI model that follows. In addition, this same information may be useful in\r\nthe development of other models more appropriate to specific assessment or\r\nevaluation needs for the gray partridge (Perdix perdix).\r\n\r\nThe HSI model section documents a habitat model and information pertinent to its\r\napplication. The model synthesizes the habitat use information into a framework\r\nappropriate for field application and is scaled to produce an index value\r\nbetween 0.0 (unsuitable habitat) and 1.0 (optimum habitat).","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Allen, A.W., 1984, Habitat Suitability Index Models: Gray partridge: FWS/OBS 82/10.73, vi, 23 p.","productDescription":"vi, 23 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":190839,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6498ad","contributors":{"authors":[{"text":"Allen, Arthur W.","contributorId":40648,"corporation":false,"usgs":true,"family":"Allen","given":"Arthur","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":288423,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71002,"text":"wdrFL824 - 1984 - Water resources data, Florida, water year 1982, Volume 4: Northwest Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:13:46","indexId":"wdrFL824","displayToPublicDate":"2005-08-09T00:00:00","publicationYear":"1984","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":"FL-82-4","title":"Water resources data, Florida, water year 1982, Volume 4: Northwest Florida","language":"ENGLISH","doi":"10.3133/wdrFL824","usgsCitation":"Geological Survey, U., 1984, Water resources data, Florida, water year 1982, Volume 4: Northwest Florida: U.S. Geological Survey Water Data Report FL-82-4, 310 p., https://doi.org/10.3133/wdrFL824.","productDescription":"310 p.","costCenters":[],"links":[{"id":185748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/fl-82-4/report-thumb.jpg"},{"id":90530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/fl-82-4/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f146d","contributors":{"authors":[{"text":"Geological Survey, U.S.","contributorId":26017,"corporation":false,"usgs":true,"family":"Geological Survey","given":"U.S.","affiliations":[],"preferred":false,"id":283473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013138,"text":"70013138 - 1984 - Evaluation of the efficiency of streamflow data collection strategies for alluvial rivers","interactions":[],"lastModifiedDate":"2025-04-15T15:32:03.110121","indexId":"70013138","displayToPublicDate":"2003-04-23T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of the efficiency of streamflow data collection strategies for alluvial rivers","docAbstract":"Streamflow discharge is usually determined indirectly from measurements of the river stage at gaging stations and through the use of stage-discharge relationships (rating curves). However, in alluvial streams, stage-discharge relationships change continually and, sometimes, quite markedly. Such changes may be caused by major floods, seasonal variations, or long-term secular trends associated with changes in the river channel. Consequently, reliable estimates of discharge using rating curves are not possible unless frequent direct measurements of discharge are made. Such measurements involve appreciable costs, and it is important to evaluate their contribution in increasing the accuracy of estimation of quantities of interest such as mean daily, monthly or annual flow. A methodology for the evaluation of the efficiency of data-collection strategies for alluvial rivers is developed and applied to stations on the Missouri River, U.S.A. A flexible and expedient model describing the variability of discharges and shifts in the stage-discharge relationship is developed. Procedures for the estimation of parameters and the validation of the model using actual data are presented. The calibrated and validated model is then employed in simulations to evaluate the effect of sampling strategies (such as frequency and accuracy of discharge measurements) on the accuracy of estimated mean daily, monthly and annual flow. Curves relating the cost of sampling to the achieved accuracy can be generated, and the optimization of sampling strategies given accuracy or budget objectives or constraints can be achieved.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(84)90186-0","issn":"00221694","usgsCitation":"Kitanidis, P., Lara, O.G., and Lane, R., 1984, Evaluation of the efficiency of streamflow data collection strategies for alluvial rivers: Journal of Hydrology, v. 72, no. 1-2, p. 85-103, https://doi.org/10.1016/0022-1694(84)90186-0.","productDescription":"19 p.","startPage":"85","endPage":"103","costCenters":[],"links":[{"id":220409,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0ce2e4b0c8380cd52d2a","contributors":{"authors":[{"text":"Kitanidis, P.K.","contributorId":63274,"corporation":false,"usgs":true,"family":"Kitanidis","given":"P.K.","affiliations":[],"preferred":false,"id":365378,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lara, O. G.","contributorId":31001,"corporation":false,"usgs":true,"family":"Lara","given":"O.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":365377,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lane, R.W.","contributorId":86228,"corporation":false,"usgs":true,"family":"Lane","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":365379,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70014083,"text":"70014083 - 1984 - Age and correlation of emerged pliocene and pleistocene deposits, U.S. Atlantic Coastal Plain","interactions":[],"lastModifiedDate":"2025-06-16T15:01:27.053261","indexId":"70014083","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Age and correlation of emerged pliocene and pleistocene deposits, U.S. Atlantic Coastal Plain","docAbstract":"Paleontologic and paleomagnetic investigations were conducted on several hundred Pliocene and Pleistocene marine samples from five regions of the emerged Atlantic Coastal Plain: (1) the Delmarva Peninsula, (2) eastern Virginia, (3) central and northern North Carolina, (4) southern North Carolina and northeastern South Carolina, and (5) the Charleston area, South Carolina. Molluscan and ostracode interval and assemblage zonations, which are the primary means of regional correlation, have been calibrated using planktic biochronologic, paleomagnetic, radiometric and amino-acid recemization data. These multiple dating criteria were used to determine the age and, where possible, the duration of marine transgressive/regressive sequences. A correlation chart illustrates the age relationships of 27 formations from five regions. One important conclusion is some of the Yorktown Formation of Virginia and North Carolina (including the “Duplin” Formation), and some of the Raysor of South Carolina are late Pliocene in age. The late Pliocene Chowan River Formation of North Carolina is older than the early Pleistocene Waccamaw Formation of South Carolina, which in turn may be older than the James City Formation of North Carolina. During the last 1.0 million years, multiple marine transgressions occurred in each region, but the age of these middle and late Pleistocene formations often may differ from one area to the next.
A significant result of the study is the evidence for the lack of time equivalence of formations in the five different regions; that is, the sequence of marine transgressions in one region does not necessarily correspond to that in another. This appears to be the result of differing subsidence and uplift histories, the patchiness of the depositional record, and the limitations of the dating techniques in light of the rapidity and frequency of sea-level fluctuations.
","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(84)90079-8","usgsCitation":"Cronin, T.M., Bybell, L., Poore, R., Blackwelder, B.W., Liddicoat, J.C., and Hazel, J.E., 1984, Age and correlation of emerged pliocene and pleistocene deposits, U.S. Atlantic Coastal Plain: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 47, no. 1-2, p. 21-51, https://doi.org/10.1016/0031-0182(84)90079-8.","productDescription":"31 p.","startPage":"21","endPage":"51","costCenters":[],"links":[{"id":225812,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Delaware, Maryland, North Carolina, South Carolina, Virginia","otherGeospatial":"Atlantic Coastal Plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.234375,\n 39.13006024213511\n ],\n [\n -75.65185546874999,\n 39.690280594818034\n ],\n [\n -78.06884765624999,\n 39.53793974517628\n ],\n [\n -81.6943359375,\n 33.394759218577995\n ],\n [\n -81.36474609375,\n 32.58384932565662\n ],\n [\n -80.74951171875,\n 32.045332838858506\n ],\n [\n -76.97021484375,\n 34.32529192442733\n ],\n [\n -75.56396484375,\n 35.746512259918504\n ],\n [\n -75.60791015625,\n 37.28279464911045\n ],\n [\n -74.970703125,\n 38.41055825094609\n ],\n [\n -75.234375,\n 39.13006024213511\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"47","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8d7e4b0c8380cd47eeb","contributors":{"authors":[{"text":"Cronin, T. M. 0000-0002-2643-0979","orcid":"https://orcid.org/0000-0002-2643-0979","contributorId":42613,"corporation":false,"usgs":true,"family":"Cronin","given":"T.","email":"","middleInitial":"M.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":false,"id":367529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bybell, L.M. 0000-0002-4760-7542","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":11220,"corporation":false,"usgs":true,"family":"Bybell","given":"L.M.","affiliations":[],"preferred":false,"id":367527,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Poore, R.Z.","contributorId":35314,"corporation":false,"usgs":true,"family":"Poore","given":"R.Z.","email":"","affiliations":[],"preferred":false,"id":367528,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blackwelder, B. W.","contributorId":104136,"corporation":false,"usgs":true,"family":"Blackwelder","given":"B.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":367532,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Liddicoat, J. C.","contributorId":76781,"corporation":false,"usgs":false,"family":"Liddicoat","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":367530,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hazel, J. E.","contributorId":89187,"corporation":false,"usgs":false,"family":"Hazel","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":367531,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70013358,"text":"70013358 - 1984 - A note on drillhole depths required for reliable heat flow determinations","interactions":[],"lastModifiedDate":"2025-08-27T16:01:29.417985","indexId":"70013358","displayToPublicDate":"2003-04-09T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"A note on drillhole depths required for reliable heat flow determinations","docAbstract":"In general, there is a limiting depth in a drillhole above which the reliability of a single determination of heat flow decreases rapidly with decreasing depth and below which the statistical uncertainty of a heat flow determination does not change perceptibly with increasing depth. This feature has been established empirically for a test case comprising a group of twelve heat flow sites in the Republic of Zambia. The technique consists of constructing heat flow versus depth curves for individual sites by progressively discarding data from the lower part of the hole and recomputing heat flow from the remaining data. For the Zambian test case, the curves converge towards a uniform value of 67 ± 3 mW m−2 when all available data are used, but values of heat flow calculated for shallow(< 100 m) parts of the same holes range from 45 to 95 mW m−2. The heat flow versus depth curves are enclosed by a perturbation envelope which has an amplitude of 40 mW m−2 at the surface and decreases linearly to the noise level at 190 m. For the test region of Zambia a depth of 170 m is needed to guarantee a heat flow measurement within ± 10% of the background regional value. It is reasonable to expect that this depth will be shallower in some regions and deeper in others. Features of heat flow perturbation envelopes can be used as quantitative reliability indices for heat flow studies.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(84)90070-2","issn":"00401951","usgsCitation":"Chapman, D.S., Howell, J., and Sass, J.H., 1984, A note on drillhole depths required for reliable heat flow determinations: Tectonophysics, v. 103, no. 1-4, p. 11-18, https://doi.org/10.1016/0040-1951(84)90070-2.","productDescription":"8 p.","startPage":"11","endPage":"18","costCenters":[],"links":[{"id":220196,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"103","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4c2e4b0c8380cd468d7","contributors":{"authors":[{"text":"Chapman, David S.","contributorId":93192,"corporation":false,"usgs":true,"family":"Chapman","given":"David","middleInitial":"S.","affiliations":[],"preferred":false,"id":365894,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howell, Jack","contributorId":92990,"corporation":false,"usgs":true,"family":"Howell","given":"Jack","affiliations":[],"preferred":false,"id":365893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sass, John H.","contributorId":69596,"corporation":false,"usgs":true,"family":"Sass","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":365892,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70014047,"text":"70014047 - 1984 - A review of crust and upper mantle structure studies of the Snake River Plain-Yellowstone volcanic system: A major lithospheric anomaly in the western U.S.A.","interactions":[],"lastModifiedDate":"2025-08-26T16:52:03.221469","indexId":"70014047","displayToPublicDate":"2003-04-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"A review of crust and upper mantle structure studies of the Snake River Plain-Yellowstone volcanic system: A major lithospheric anomaly in the western U.S.A.","docAbstract":"The Snake River Plain-Yellowstone volcanic system is one of the largest, basaltic, volcanic field in the world. Here, there is clear evidence for northeasterly progression of rhyolitic volcanism with its present position in Yellowstone. Many theories have been advanced for the origin of the Snake River Plain-Yellowstone system. Yellowstone and Eastern Snake River Plain have been studied intensively using various geophysical techniques. Some sparse geophysical data are available for the Western Snake River Plain as well. Teleseismic data show the presence of a large anomalous body with low P- and S-wave velocities in the crust and upper mantle under the Yellowstone caldera. A similar body in which compressional wave velocity is lower than in the surrounding rock is present under the Eastern Snake River Plain. No data on upper mantle anomalies are available for the Western Snake River Plain. Detailed seismic refraction data for the Eastern Snake River Plain show strong lateral heterogeneities and suggest thinning of the granitic crust from below by mafic intrusion. Available data for the Western Snake River Plain also show similar thinning of the upper crust and its replacement by mafic material. The seismic refraction results in Yellowstone show no evidence of the low-velocity anomalies in the lower crust suggested by teleseismic P-delay data and interpreted as due to extensive partial melting. However, the seismic refraction models indicate lower-than-normal velocities and strong lateral inhomogeneities in the upper crust. Particularly obvious in the refraction data are two regions of very low seismic velocities near the Mallard Eake and Sour Creek resurgent domes in the Yellowstone caldera. The low-velocity body near the Sour Creek resurgent dome is interpreted as partially molten rock. Together with other geophysical and thermal data, the seismic results indicate that a sub-lithospheric thermal anomaly is responsible for the time-progressive volcanism along the Eastern Snake River Plain. However, the exact mechanism responsible for the volcanism and details of magma storage and migration are not yet fully understood.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(84)90209-9","issn":"00401951","usgsCitation":"Iyer, H.M., 1984, A review of crust and upper mantle structure studies of the Snake River Plain-Yellowstone volcanic system: A major lithospheric anomaly in the western U.S.A.: Tectonophysics, v. 105, no. 1-4, p. 291-308, https://doi.org/10.1016/0040-1951(84)90209-9.","productDescription":"18 p.","startPage":"291","endPage":"308","costCenters":[],"links":[{"id":226198,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Idaho, Montana, Nevada, Oregon, Washington, Wyoming","otherGeospatial":"Snake River Plain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.75522630969246,\n 48.99647522967908\n ],\n [\n -121.34357181116266,\n 40.94856106036778\n ],\n [\n -120.51316857399542,\n 40.82964955876772\n ],\n [\n -116.84272791453125,\n 41.89549551259576\n ],\n [\n -115.64848818410448,\n 41.3864499907779\n ],\n [\n -113.86318033209798,\n 41.953660184765866\n ],\n [\n -110.16687892122758,\n 43.55396021584184\n ],\n [\n -110.88285627702768,\n 48.99647522967908\n ],\n [\n -120.75522630969246,\n 48.99647522967908\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"105","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e54fe4b0c8380cd46c9a","contributors":{"authors":[{"text":"Iyer, H. M.","contributorId":17997,"corporation":false,"usgs":true,"family":"Iyer","given":"H.","middleInitial":"M.","affiliations":[],"preferred":false,"id":367448,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013271,"text":"70013271 - 1984 - Groundwater-flow parameter estimation and quality modeling of the Equus Beds aquifer in Kansas, U.S.A.","interactions":[],"lastModifiedDate":"2025-04-14T16:53:54.718216","indexId":"70013271","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Groundwater-flow parameter estimation and quality modeling of the Equus Beds aquifer in Kansas, U.S.A.","docAbstract":"The salinity problems created in the Burrton area as a result of poor oil-field brine disposal practices of the past continue to be a major concern to the area depending on the Equus Beds aquifer for water, including the City of Wichita, Kansas. In this paper, an attempt is made to predict where and how fast the brine plume will move in this area, and what the average chloride concentrations in different parts of the aquifer are. In order to make such predictions, it was necessary to get a calibrated model of the groundwater-flow velocity field. Multiple regression analysis is used for parameter estimation of the steady-state groundwater-flow equation applied in the most critical area of the Equus Beds aquifer. Results of such an analysis produced a correlation coefficient of 0.992 between calculated and observed values of hydraulic head. A chloride transport modeling effort is then carried out despite some serious data deficiencies, the significance of which are evaluated through sensitivity analysis. Thus, starting with the quasi steady-state conditions of the early 1940's, it was possible to match the present chloride distribution satisfactorily. Chloride concentration predictions made for the year 2000 indicate that the quality of the Wichita well-field waters will not generally deteriorate from their present condition by that time.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(84)90164-1","issn":"00221694","usgsCitation":"Sophocleous, M., 1984, Groundwater-flow parameter estimation and quality modeling of the Equus Beds aquifer in Kansas, U.S.A.: Journal of Hydrology, v. 69, no. 1-4, p. 197-222, https://doi.org/10.1016/0022-1694(84)90164-1.","productDescription":"26 p.","startPage":"197","endPage":"222","costCenters":[],"links":[{"id":219846,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Equus Beds aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -97.75234872951685,\n 38.17839167762153\n ],\n [\n -97.75234872951685,\n 37.4855633758371\n ],\n [\n -96.79405394886194,\n 37.4855633758371\n ],\n [\n -96.79405394886194,\n 38.17839167762153\n ],\n [\n -97.75234872951685,\n 38.17839167762153\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"69","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2dcde4b0c8380cd5c02c","contributors":{"authors":[{"text":"Sophocleous, M.A.","contributorId":18032,"corporation":false,"usgs":true,"family":"Sophocleous","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":365692,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70013618,"text":"70013618 - 1984 - Transport and concentration controls for chloride, strontium, potassium and lead in Uvas Creek, a small cobble-bed stream in Santa Clara County, California, U.S.A.: 2. Mathematical modeling","interactions":[],"lastModifiedDate":"2025-04-15T16:00:11.629528","indexId":"70013618","displayToPublicDate":"2003-03-27T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Transport and concentration controls for chloride, strontium, potassium and lead in Uvas Creek, a small cobble-bed stream in Santa Clara County, California, U.S.A.: 2. Mathematical modeling","docAbstract":"Three models describing solute transport of conservative ion species and another describing transport of species which adsorb linearly and reversibly on bed sediments are developed and tested. The conservative models are based on three different conceptual models of the transient storage of solute in the bed. One model assumes the bed to be a well-mixed zone with flux of solute into the bed proportional to the difference between stream concentration and bed concentration. The second model assumes solute in the bed is transported by a vertical diffusion process described by Fick's law. The third model assumes that convection occurs in a selected portion of the bed while the mechanism of the first model functions everywhere. The model for adsorbing species assumes that the bed consists of particles of uniform size with the rate of uptake controlled by an intraparticle diffusion process.
All models are tested using data collected before, during and after a 24-hr. pulse injection of chloride, strontium, potassium and lead ions into Uvas Creek near Morgan Hill, California, U.S.A. All three conservative models accurately predict chloride ion concentrations in the stream. The model employing the diffusion mechanism for bed transport predicts better than the others.
The adsorption model predicts both strontium and potassium ion concentrations well during the injection of the pulse but somewhat overestimates the observed concentrations after the injection ceases. The overestimation may be due to the convection of solute deep into the bed where it is retained longer than the 3-week post-injection observation period. The model, when calibrated for strontium, predicts potassium equally well when the adsorption equilibrium constant for strontium is replaced by that for potassium.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(84)90047-7","issn":"00221694","usgsCitation":"Jackman, A.P., Walters, R.A., and Kennedy, V.C., 1984, Transport and concentration controls for chloride, strontium, potassium and lead in Uvas Creek, a small cobble-bed stream in Santa Clara County, California, U.S.A.: 2. 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A. P.","contributorId":46957,"corporation":false,"usgs":true,"family":"Jackman","given":"A.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":366495,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, R. A.","contributorId":34174,"corporation":false,"usgs":true,"family":"Walters","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":366493,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennedy, V. C.","contributorId":46080,"corporation":false,"usgs":true,"family":"Kennedy","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":366494,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70013221,"text":"70013221 - 1984 - Experimental studies in natural groundwater recharge dynamics: Assessment of recent advances in instrumentation","interactions":[],"lastModifiedDate":"2025-04-14T17:00:46.569772","indexId":"70013221","displayToPublicDate":"2003-03-25T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2342,"text":"Journal of Hydrology","active":true,"publicationSubtype":{"id":10}},"title":"Experimental studies in natural groundwater recharge dynamics: Assessment of recent advances in instrumentation","docAbstract":"To quantify and model the natural groundwater-recharge process, two sites in south-central Kansas, U.S.A., were instrumented with various modern sensors and data microloggers. The atmospheric-boundary layer and the unsaturated and saturated soil zones were monitored as a unified regime. Data from the various sensors were collected using microloggers in combination with magnetic-cassette tape, graphical and digital recorders, analog paper-tape recorders, and direct observations to evaluate and automate data collection and processing.
Atmospheric sensors included an anemometer, a tipping-bucket raingage, an air-temperature thermistor, a relative-humidity probe, a net radiometer, and a barometric-pressure transducer. Sensors in the unsaturated zone consisted of soil-temperature thermocouples, tensiometers coupled with pressure transducers and dial gages, gypsum blocks, and a neutron moisture probe operated by an observer. The saturated-zone sensors consisted of a water-level pressure transducer, a conventional float gage connected to a variable potentiometer, soil thermocouples, and a number of multiple-depth piezometers.
Evaluation of the operation of these sensors and recorders indicated that certain types of equipment such as pressure transducers are very sensitive to environmental conditions. Extraordinary steps had to be taken to protect some of the equipment, whereas other equipment seemed to be reliable under all conditions. Based on such experiences, a number of suggestions aimed at improving such investigations are outlined.
","language":"English","publisher":"Elsevier","doi":"10.1016/0022-1694(84)90133-1","issn":"00221694","usgsCitation":"Sophocleous, M., and Perry, C.A., 1984, Experimental studies in natural groundwater recharge dynamics: Assessment of recent advances in instrumentation: Journal of Hydrology, v. 70, no. 1-4, p. 369-382, https://doi.org/10.1016/0022-1694(84)90133-1.","productDescription":"14 p.","startPage":"369","endPage":"382","costCenters":[],"links":[{"id":220081,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -99.1748871630371,\n 38.507940104645996\n ],\n [\n -99.1748871630371,\n 37.64917420455242\n ],\n [\n -97.68600447634276,\n 37.64917420455242\n ],\n [\n -97.68600447634276,\n 38.507940104645996\n ],\n [\n -99.1748871630371,\n 38.507940104645996\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"70","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0ddfe4b0c8380cd53226","contributors":{"authors":[{"text":"Sophocleous, M.","contributorId":13373,"corporation":false,"usgs":true,"family":"Sophocleous","given":"M.","email":"","affiliations":[],"preferred":false,"id":365571,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perry, C. A.","contributorId":106149,"corporation":false,"usgs":true,"family":"Perry","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":365572,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10301,"text":"ofr84704 - 1984 - Streamflow and basin characteristics at selected sites in Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr84704","displayToPublicDate":"1997-04-01T00:00:00","publicationYear":"1984","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":"84-704","title":"Streamflow and basin characteristics at selected sites in Kentucky","docAbstract":"Common basin and streamflow characteristics for sites in Kentucky are presented. Basin characteristics include quantified drainage basin parameters and statistics on areal rainfall. Streamflow characteristics include tables for mean, high and low flow frequencies and partial duration discharge. The data listed in this report are for continuous and low-flow partial-record sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84704","usgsCitation":"Melcher, N., and Ruhl, K., 1984, Streamflow and basin characteristics at selected sites in Kentucky: U.S. Geological Survey Open-File Report 84-704, v, 80 p. :ill., maps (some folded) ;28 cm., https://doi.org/10.3133/ofr84704.","productDescription":"v, 80 p. :ill., maps (some folded) ;28 cm.","costCenters":[],"links":[{"id":144092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0704/report-thumb.jpg"},{"id":38159,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db626eda","contributors":{"authors":[{"text":"Melcher, N.B.","contributorId":71554,"corporation":false,"usgs":true,"family":"Melcher","given":"N.B.","email":"","affiliations":[],"preferred":false,"id":161163,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruhl, K.J.","contributorId":35322,"corporation":false,"usgs":true,"family":"Ruhl","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":161162,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":60252,"text":"mf1246L - 1984 - Maps showing distribution of pH, copper, zinc, fluoride, uranium, molybdenum, arsenic, and sulfate in water, Richfield 1° x 2° quadrangle, Utah","interactions":[],"lastModifiedDate":"2021-10-25T19:02:48.751765","indexId":"mf1246L","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1246","chapter":"L","title":"Maps showing distribution of pH, copper, zinc, fluoride, uranium, molybdenum, arsenic, and sulfate in water, Richfield 1° x 2° quadrangle, Utah","docAbstract":"These maps show the regional distribution of copper, zinc, arsenic, molybdenum, uranium, fluoride, sulfate, and pH in surface and ground water from the Richfield 1° x 2° quadrangle. This study supplements (Miller and others, 1984a-j) the regional drainage geochemical study done for the Richfield quadrangle under the U.S. Geological Survey’s Conterminuous United States Mineral Assessment Program (CUSMAP). Regional sampling was designed to define broad geochemical patterns and trends which can be used, along with geologic and geophysical data, to assess the mineral resource potential of the Richfield quadrangle. Analytical data used in compiling this report were published previously (McHugh and others, 1981).
\nThe Richfield quadrangle in west-central Utah covers the eastern part of the Pioche-Marysvale igneous and mineral belt that extends from the vicinity of Pioche in southeastern Nevada, east-northeastward for 250 km into central Utah. The western two-thirds of the Richfield quadrangle is in the Basin and Range Province, and the eastern third in the High Plateaus of Utah subprovince of the Colorado Plateau.
\nBedrock in the northern part of the Richfield quadrangle consists predominantly of latest Precambrian and Paleozoic sedimentary strata that were thrust eastward during the Sevier orogeny in Cretaceous time onto an autochthon of Mesozoic sedimentary rocks in the eastern part of the quadrangle. The southern part of the quadrangle is largely underlain by Oligocene and younger volcanic rocks and related intrusions. Extensional tectonism in late Cenozoic time broke the bedrock terrane into a series of north-trending fault blocks; the uplifted mountain areas were deeply eroded and the resulting debris deposited in the adjacent basins. Most of the mineral deposits in the Pioche-Marysvale mineral belt were formed during igneous activity in the middle and late Cenozoic time.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver CO","doi":"10.3133/mf1246L","usgsCitation":"McHugh, J.B., Miller, W.R., and Ficklin, W.H., 1984, Maps showing distribution of pH, copper, zinc, fluoride, uranium, molybdenum, arsenic, and sulfate in water, Richfield 1° x 2° quadrangle, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1246, 1 Plate: 40.89 x 32.77 inches, https://doi.org/10.3133/mf1246L.","productDescription":"1 Plate: 40.89 x 32.77 inches","costCenters":[],"links":[{"id":182629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1246l.jpg"},{"id":283659,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1246-L/plate-1.pdf"},{"id":390899,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6856.htm"}],"scale":"500000","country":"United States","state":"Utah","otherGeospatial":"Richfield 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,38.0 ], [ -114.0,39.0 ], [ -112.0,39.0 ], [ -112.0,38.0 ], [ -114.0,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db60578b","contributors":{"authors":[{"text":"McHugh, J. B.","contributorId":79462,"corporation":false,"usgs":true,"family":"McHugh","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":263391,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. R.","contributorId":92239,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":263393,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ficklin, W. H.","contributorId":89517,"corporation":false,"usgs":true,"family":"Ficklin","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":263392,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":55229,"text":"wdrME831 - 1984 - Water resources data, Maine, water year 1983","interactions":[],"lastModifiedDate":"2025-07-28T16:43:40.517617","indexId":"wdrME831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"ME-83-1","title":"Water resources data, Maine, water year 1983","docAbstract":"Water resources data for the 1983 water year for Maine consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water quality of wells. This report contains discharge records for 56 gaging stations; stage only for 2 gaging stations; contents for 17 lakes and reservoirs; water quality for 11 gaging stations; and water levels for 32 observation wells. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrME831","collaboration":"Prepared in cooperation with the State of Maine and with other agencies","usgsCitation":"Morrill, R., Haskell, C., Adamik, J., and Higgins, W., 1984, Water resources data, Maine, water year 1983: U.S. Geological Survey Water Data Report ME-83-1, vii, 152 p., https://doi.org/10.3133/wdrME831.","productDescription":"vii, 152 p.","costCenters":[],"links":[{"id":493028,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/me-83-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174495,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/me-83-1/report-thumb.jpg"}],"country":"United 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