{"pageNumber":"4744","pageRowStart":"118575","pageSize":"25","recordCount":165605,"records":[{"id":70231498,"text":"70231498 - 1983 - Combining Landsat and geophysical data for mineral and groundwater exploration in the Tucson area, Arizona, and Sonora","interactions":[],"lastModifiedDate":"2022-05-11T16:28:46.304482","indexId":"70231498","displayToPublicDate":"1983-01-01T11:17:24","publicationYear":"1983","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Combining Landsat and geophysical data for mineral and groundwater exploration in the Tucson area, Arizona, and Sonora","docAbstract":"

No abstract available.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"SEG Technical Program Expanded Abstracts 1983","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"53rd Annual International Meeting and Exposition of Society of Exploration Geophysicists","conferenceDate":"September 11-15, 1983","conferenceLocation":"Las Vegas, Nevada, United States","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1893806","usgsCitation":"Hastings, D.A., 1983, Combining Landsat and geophysical data for mineral and groundwater exploration in the Tucson area, Arizona, and Sonora, in SEG Technical Program Expanded Abstracts 1983, Las Vegas, Nevada, United States, September 11-15, 1983, p. 194-197, https://doi.org/10.1190/1.1893806.","productDescription":"4 p.","startPage":"194","endPage":"197","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":400514,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico, United States","state":"Arizona, Sonora","city":"Tucson","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.96142578125,\n 30.62845887475364\n ],\n [\n -109.00634765625,\n 30.62845887475364\n ],\n [\n -109.00634765625,\n 33.458942753687644\n ],\n [\n -112.96142578125,\n 33.458942753687644\n ],\n [\n -112.96142578125,\n 30.62845887475364\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationDate":"2012-03-22","publicationStatus":"PW","contributors":{"authors":[{"text":"Hastings, D. A.","contributorId":48197,"corporation":false,"usgs":true,"family":"Hastings","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":842788,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70120416,"text":"70120416 - 1983 - The physical habitat simulation system and instream flow considerations","interactions":[],"lastModifiedDate":"2023-12-19T00:35:30.808567","indexId":"70120416","displayToPublicDate":"1983-01-01T11:16:54","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The physical habitat simulation system and instream flow considerations","docAbstract":"No abstract available.","language":"English","publisher":"American Geophysical Union","usgsCitation":"Milhous, R.T., 1983, The physical habitat simulation system and instream flow considerations: Eos, Transactions, American Geophysical Union, v. 64, no. 45, 1 p.","productDescription":"1 p.","numberOfPages":"1","costCenters":[],"links":[{"id":292186,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"64","issue":"45","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53edcd54e4b0f61b386d24ae","contributors":{"authors":[{"text":"Milhous, Robert T.","contributorId":28646,"corporation":false,"usgs":true,"family":"Milhous","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":498177,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70202407,"text":"70202407 - 1983 - Topographic map of the island of Tinian, Commonwealth of the Northern Mariana Islands","interactions":[],"lastModifiedDate":"2019-03-04T10:17:02","indexId":"70202407","displayToPublicDate":"1983-01-01T11:16:46","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Topographic map of the island of Tinian, Commonwealth of the Northern Mariana Islands","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70202407","usgsCitation":"U.S. Geological Survey, 1983, Topographic map of the island of Tinian, Commonwealth of the Northern Mariana Islands, 1 Plate: 33.00 x 54.29 inches, https://doi.org/10.3133/70202407.","productDescription":"1 Plate: 33.00 x 54.29 inches","costCenters":[],"links":[{"id":361666,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70202407/report-thumb.jpg"},{"id":361667,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70202407/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","otherGeospatial":"Tinian","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 145.51666667,\n 14.82500000\n ],\n [\n 145.69166667,\n 14.82500000\n ],\n [\n 145.69166667,\n 15.11666667\n ],\n [\n 145.51666667,\n 15.11666667\n ],\n [\n 145.51666667,\n 14.82500000\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":202815,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":758653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70200535,"text":"70200535 - 1983 - Channels and valleys on Mars","interactions":[],"lastModifiedDate":"2018-10-23T11:12:50","indexId":"70200535","displayToPublicDate":"1983-01-01T11:12:08","publicationYear":"1983","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":"Channels and valleys on Mars","docAbstract":"

The discovery of channels, valleys, and related features of aqueous origin on Mars is of profound importance in comparative planetology. Models of the evolution of planetary surfaces and atmospheres must be reconciled with the diversity, abundance, and origins of channels and valleys on Mars. The term “channel” is properly restricted to those Martian troughs that display at least some evidence of large-scale fluid flow on their floors. Outflow channels show evidence of flows emanating from zones of chaotic terrain. The term “valley” applies to those elongate Martian troughs, or systems of troughs, that also appear to have formed by fluid flow, but which lack a suite of bed forms on their floors. The Martian valleys of greatest interest consist of interconnected, digitate networks that dissect extensive areas of heavily cratered uplands on the planet. The diversity of Martian channels and valleys is nearly as great as that of their terrestrial counterparts. Even though polygenetic and highly modified features abound, water was a necessary ingredient in the various channel- and valley-forming processes. The outflow channels involved large-scale fluid flow, entailing as yet unresolved percentages of liquid and solid phases, entrained sediment, and debris flowage. The formation of valley networks required ground water or ground ice, contributing to sapping and various other hillslope phenomena. Channels and valley networks probably require an ancient epoch with surface temperatures and pressures higher than at present. The aqueous formation of channels is release-limited, requiring short-duration floods of immense volumes. The origin of valley networks is perseverance-limited, requiring the maintenance of prolonged seepage and surface flow. Both phenomena are consistent with a thick, ice-rich Martian permafrost formed either during a volatile-rich early epoch or by very effective recycling of planetary water.

","language":"English","publisher":"The Geological Society of America","doi":"10.1130/0016-7606(1983)94<1035:CAVOM>2.0.CO;2","usgsCitation":"Mars Channel Working Group, 1983, Channels and valleys on Mars: GSA Bulletin, v. 94, no. 9, p. 1035-1054, https://doi.org/10.1130/0016-7606(1983)94<1035:CAVOM>2.0.CO;2.","productDescription":"20 p.","startPage":"1035","endPage":"1054","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":358669,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mars Channel Working Group","contributorId":209982,"corporation":true,"usgs":false,"organization":"Mars Channel Working Group","id":749399,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":917,"text":"917 - 1983 - Water resources data: Tennessee","interactions":[],"lastModifiedDate":"2014-07-09T10:25:35","indexId":"917","displayToPublicDate":"1983-01-01T10:21:02","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Water resources data: Tennessee","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":"10.3133/917","issn":"0163-9447","collaboration":"Prepared in cooperation with the Tennessee, Division of Water Resources, 1982; the Tennessee Valley Authority, 1982-198 ; the U.S. Geological Survey, Water Resources Division, 1983- ; the Tennessee, Division of Water Management, 1983-198u; and with other state, municipal, and federal agencies, 1983-","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Water resources data: Tennessee, https://doi.org/10.3133/917.","costCenters":[],"links":[{"id":289600,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Tennessee","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.3103,34.9829 ], [ -90.3103,36.678 ], [ -81.6469,36.678 ], [ -81.6469,34.9829 ], [ -90.3103,34.9829 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53be6498e4b0527d5d409801","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":527832,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70265478,"text":"wri834205 - 1983 - Atmospheric deposition: Sample handling, storage, and analytical procedures for chemical characterization of event-based samples in North Dakota","interactions":[],"lastModifiedDate":"2025-07-17T13:35:42.159342","indexId":"wri834205","displayToPublicDate":"1983-01-01T10:13:22","publicationYear":"1983","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":"83-4205","title":"Atmospheric deposition: Sample handling, storage, and analytical procedures for chemical characterization of event-based samples in North Dakota","docAbstract":"

The North Dakota atmospheric-deposition network uses HASL-type collectors to sample wet and dry deposition on an event basis for analysis of 8 principal mineral, 3 nutrient, and 15 trace constituents. Comparison of the compositions of wet deposition collected in adjacent collectors sampled on weekly and event bases indicates that weekly sampling leads to significant contamination of wet deposition samples with dry deposition. Elevation of the collectors 10 feet above ground surface may decrease wind-blown soil contamination significantly.

This manual presents a summary of the research procedures adopted by the North Dakota District of the U.S. Geological Survey to investigate the consequences of increased fossil-fuel combustion on the quality of atmospheric deposition. The manual has been tested by field operatives for 3 years and shown to be an effective field guide and management tool.

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No abstract available.

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This chapter examines the eolian sand bodies of the world. Analyses regarding grain size and sorting distribution at Great Sand Dunes indicate that the higher dunes contain much more fine-grained sand and much less medium-grained sand than do the lower dunes, and, in addition, they are definitely better sorted. Cross-stratification in eolian deposits is the product of several distinct processes of transport. These processes are saltation or ripple migration that include various amounts of surface creep, grainfall (a dropping of grains from sand in suspension), and avalanching either by mass movement or by grain flowage which involves the downhill rolling or sliding of discrete particles. Penecontemporaneous deformational structures including various types of faults and folds, flames, break aparts, and rotated blocks are sufficiently numerous in most eolian deposits to serve as useful tools in determining genesis. These structures are good indicators of the nature of the stress and therefore provide information on the part of a sand body involved. Sufficient observations have been recorded to establish that the lee side (or slipface) of most modern dunes stands at 30° or slightly more and that the length of the foresets developed on it may be 8 or 10 m and often much more. © 1983, Elsevier Science & Technology. All rights reserved.

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No abstract available.

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California","interactions":[],"lastModifiedDate":"2019-10-24T09:52:47","indexId":"70206168","displayToPublicDate":"1983-01-01T09:29:42","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2309,"text":"Journal of Geology","active":true,"publicationSubtype":{"id":10}},"title":"A tale of two plutons: petrographic and mineralogic constraints on the petrogenesis of the Red Lake and Eagle Peak plutons, central Sierra Nevada, California","docAbstract":"

The two plutons are similar in age (K/Ar, 87-89 m.y.) and range in composition from granodiorite to granite. The Red Lake pluton is equigranular, has a locally greisened marginal zone, and shows only minor mineralogical and chemical zoning, whereas the Eagle Peak pluton is mineralogically, compositionally and texturally zoned, with an equigranular margin and a porphyritic core. Modal and normative trends within each pluton are consistent with separation of plagioclase and mafic minerals leading to a residual liquid enriched in quartz and alkali feldspar. The presence of homogeneous cores in the plagioclase, early titanite crystallization in the Red Lake magma and irregular hornblende compositions suggest that refractory material was present when the magmas were intruded. Inferred source regions for the two plutons are amphibolite for the Red Lake magma and a more biotite-rich amphibolite for the Eagle Peak magma.

","language":"English ","doi":"10.1086/628784","issn":"00221376","usgsCitation":"Noyes, J., Wones, D.R., and Frey, F., 1983, A tale of two plutons: petrographic and mineralogic constraints on the petrogenesis of the Red Lake and Eagle Peak plutons, central Sierra Nevada, California: Journal of Geology, v. 91, no. 4, p. 353-379, https://doi.org/10.1086/628784.","productDescription":"26 p. ","startPage":"353","endPage":"379","costCenters":[],"links":[{"id":368552,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"California 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\"}}]}","volume":"91","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Noyes, J.H.","contributorId":66636,"corporation":false,"usgs":true,"family":"Noyes","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":773755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wones, D. R.","contributorId":104079,"corporation":false,"usgs":true,"family":"Wones","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":773756,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frey, F.A.","contributorId":12618,"corporation":false,"usgs":true,"family":"Frey","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":773757,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70175650,"text":"70175650 - 1983 - Groundwater resources of the Dallas-Monmouth area, Polk, Benton, and Marion counties, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T14:36:14","indexId":"70175650","displayToPublicDate":"1983-01-01T07:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Groundwater resources of the Dallas-Monmouth area, Polk, Benton, and Marion counties, Oregon","docAbstract":"

No abstract available.

","language":"English","publisher":"American Geosciences Institute","issn":"0473-1883","usgsCitation":"Young, W., 1983, Groundwater resources of the Dallas-Monmouth area, Polk, Benton, and Marion counties, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326744,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"scale":"62500","country":"United States","state":"Oregon","county":"Benton, Marion, Polk","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ad5e4b03bcb0104bbe3","contributors":{"authors":[{"text":"Young, William","contributorId":138842,"corporation":false,"usgs":false,"family":"Young","given":"William","email":"","affiliations":[{"id":12542,"text":"Washington Dept. of Fish and Wildlife, Snake River Laboratory, 401 South Cottonwood St., Dayton WA 99328","active":true,"usgs":false}],"preferred":false,"id":645929,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175044,"text":"70175044 - 1983 - Anaerobic oxalate degradation: Widespread natural occurrence in aquatic sediments","interactions":[],"lastModifiedDate":"2023-01-26T18:33:35.793734","indexId":"70175044","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":850,"text":"Applied and Environmental Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Anaerobic oxalate degradation: Widespread natural occurrence in aquatic sediments","docAbstract":"

Significant concentrations of oxalate (dissolved plus particulate) were present in sediments taken from a diversity of aquatic environments, ranging from 0.1 to 0.7 mmol/liter of sediment. These included pelagic and littoral sediments from two freshwater lakes (Searsville Lake, Calif., and Lake Tahoe, Calif.), a hypersaline, meromictic, alkaline lake (Big Soda Lake, Nev.), and a South San Francisco Bay mud flat and salt marsh. The oxalate concentration of several plant species which are potential detrital inputs to these aquatic sediments ranged from 0.1 to 5.0% (wt/wt). In experiments with litter bags, the oxalate content of Myriophyllum sp. samples buried in freshwater littoral sediments decreased to 7% of the original value in 175 days. This suggests that plant detritus is a potential source of the oxalate within these sediments. [14C]oxalic acid was anaerobically degraded to14CO2 in all sediment types tested, with higher rates evident in littoral sediments than in the pelagic sediments of the lakes studied. The turnover time of the added [14C]oxalate was less than 1 day in Searsville Lake littoral sediments. The total sediment oxalate concentration did not vary significantly between littoral and pelagic sediments and therefore did not appear to be controlling the rate of oxalate degradation. However, depth profiles of [14C]oxalate mineralization and dissolved oxalate concentration were closely correlated in freshwater littoral sediments; both were greatest in the surface sediments (0 to 5 cm) and decreased with depth. The dissolved oxalate concentration (9.1 μmol/liter of sediment) was only 3% of the total extractable oxalate (277 μmol/liter of sediment) at the sediment surface. These results suggest that anaerobic oxalate degradation is a widespread phenomenon in aquatic sediments and may be limited by the dissolved oxalate concentration within these sediments.

","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/aem.46.1.106-113.1983","usgsCitation":"Smith, R.L., and Oremland, R.S., 1983, Anaerobic oxalate degradation: Widespread natural occurrence in aquatic sediments: Applied and Environmental Microbiology, v. 46, no. 1, p. 106-113, https://doi.org/10.1128/aem.46.1.106-113.1983.","productDescription":"8 p.","startPage":"106","endPage":"113","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":480232,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/aem.46.1.106-113.1983","text":"Publisher Index Page"},{"id":325727,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, 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Seabirds were observed between Alaska and Hawaii along 158°W longitude from 24 October to 6 November 1976. Their distributions and abundances corresponded remarkably well to oceanographic regions. Indices of seabird density dropped in a series of plateaus from 44 birds/km2 in the Alaska Current System to less than 1 bird/km2 in subtropic waters. Northern distribution records were found for six species. The Subarctic Boundary marked the center of the separation between subarctic and subtropic pelagic avifaunas.

","language":"English","publisher":"Cooper Ornithological Society","doi":"10.2307/1367061","usgsCitation":"Gould, P.J., 1983, Seabirds between Alaska and Hawaii: The Condor, v. 85, no. 3, p. 286-291, https://doi.org/10.2307/1367061.","productDescription":"6 p.","startPage":"286","endPage":"291","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":503097,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/condor/vol85/iss3/4","text":"External Repository"},{"id":335662,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska, Hawaii","otherGeospatial":"North Pacific 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\"}}]}","volume":"85","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a5770ce4b057081a24eec0","contributors":{"authors":[{"text":"Gould, Patrick J.","contributorId":11667,"corporation":false,"usgs":true,"family":"Gould","given":"Patrick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":669485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011964,"text":"70011964 - 1983 - Improper use of regression equations in earth sciences","interactions":[],"lastModifiedDate":"2024-01-31T01:29:13.934732","indexId":"70011964","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1796,"text":"Geology","active":true,"publicationSubtype":{"id":10}},"title":"Improper use of regression equations in earth sciences","docAbstract":"

A regression equation used to estimate a variable is appropriately used only to estimate the dependent variable of that equation; the equation is inappropriately used when solved for an independent variable. Examples given here of this misuse of regression equations are based on actual cases in sedimentologic, geomorphologic, and paleohydrologic literature. The error involved can amount to several hundred percent.

","language":"English","publisher":"Geological Society of America","doi":"10.1130/0091-7613(1983)11<195:IUOREI>2.0.CO;2","issn":"00917613","usgsCitation":"Williams, G.P., 1983, Improper use of regression equations in earth sciences: Geology, v. 11, no. 4, p. 195-197, https://doi.org/10.1130/0091-7613(1983)11<195:IUOREI>2.0.CO;2.","productDescription":"3 p.","startPage":"195","endPage":"197","numberOfPages":"3","costCenters":[],"links":[{"id":221482,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a394ee4b0c8380cd61896","contributors":{"authors":[{"text":"Williams, G. P.","contributorId":97472,"corporation":false,"usgs":true,"family":"Williams","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":362401,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46989,"text":"ofr821030 - 1983 - Geologic map of the Mitten Lake, Half Dome Crag, Hyde Creek, East Glacier Park, Big Rock, and Magee Range quadrangles, Pondera and Glacier Counties, Montana","interactions":[],"lastModifiedDate":"2023-08-25T18:26:40.347672","indexId":"ofr821030","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","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":"82-1030","title":"Geologic map of the Mitten Lake, Half Dome Crag, Hyde Creek, East Glacier Park, Big Rock, and Magee Range quadrangles, Pondera and Glacier Counties, Montana","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr821030","usgsCitation":"Mudge, M.R., Earhart, R., Perry, W.J., and Bohannon, R.G., 1983, Geologic map of the Mitten Lake, Half Dome Crag, Hyde Creek, East Glacier Park, Big Rock, and Magee Range quadrangles, Pondera and Glacier Counties, Montana: U.S. Geological Survey Open-File Report 82-1030, 1 Plate: 34.92 x 32.46 inches, https://doi.org/10.3133/ofr821030.","productDescription":"1 Plate: 34.92 x 32.46 inches","costCenters":[],"links":[{"id":108422,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13625.htm","linkFileType":{"id":5,"text":"html"},"description":"13625"},{"id":83892,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/1030/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172698,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","county":"Glacier County, Pondera County","otherGeospatial":"Mitten Lake, Half Dome Crag, Hyde Creek, East Glacier Park, Big Rock, and Magee Ranch quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113.25,\n 48.5\n ],\n [\n -113.25,\n 48.25\n ],\n [\n -112.875,\n 48.25\n ],\n [\n -112.875,\n 48.5\n ],\n [\n -113.25,\n 48.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696904","contributors":{"authors":[{"text":"Mudge, Melville Rhodes","contributorId":77119,"corporation":false,"usgs":true,"family":"Mudge","given":"Melville","email":"","middleInitial":"Rhodes","affiliations":[],"preferred":false,"id":234447,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Earhart, R.L.","contributorId":73175,"corporation":false,"usgs":true,"family":"Earhart","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":234446,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Perry, W. J. Jr.","contributorId":64266,"corporation":false,"usgs":true,"family":"Perry","given":"W.","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":234445,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bohannon, R. G.","contributorId":61808,"corporation":false,"usgs":true,"family":"Bohannon","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":234444,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":38584,"text":"pp1277 - 1983 - Hydrologic and geomorphic studies of the Platte River basin","interactions":[{"subject":{"id":8117,"text":"ofr811116 - 1981 - Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska","indexId":"ofr811116","publicationYear":"1981","noYear":false,"title":"Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":38584,"text":"pp1277 - 1983 - Hydrologic and geomorphic studies of the Platte River basin","indexId":"pp1277","publicationYear":"1983","noYear":false,"title":"Hydrologic and geomorphic studies of the Platte River basin"},"id":1}],"lastModifiedDate":"2025-08-22T19:13:25.616513","indexId":"pp1277","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1277","title":"Hydrologic and geomorphic studies of the Platte River basin","docAbstract":"The channels of the Platte River and its major tributaries, the South Platte and North Platte Rivers in Colorado, Wyoming, and Nebraska, have undergone major changes in hydrologic regime and morphology since about 1860, when the water resources of the basin began to be developed for agricultural, municipal, and industrial uses. These water uses have continued to increase with growth in population and land development. Diversion of flow from channels, storage of water in reservoirs, and increased use of ground water have affected the distribution and timing of streamflows and the transport of fluvial sediments. All these factors have contributed to changes in channel geometry and the riverine environment.\r\n\r\nIn 1979, the U.S. Geological Survey began investigations in the Platte River basin to determine the effects of water use on the hydrology and morphology of the Platte River and its major tributaries. These investigations also considered the relationship of hydrologic regime to factors that control or affect the habitat of migratory waterfowl in the Platte River valley.\r\n\r\nThis volume brings together the results of several research studies on historical changes in channel morphology, surface-water hydrology, hydraulic geometry, sediment-transport and bedform processes, ground-water and surface-water relations, stochastic models of streamflow and precipitation, and methods for estimating discharge required to maintain channel width. In each of the studies, data on some segment of the Platte River hydrologic system were collected and interpreted. All the studies are interrelated; together they provide some degree of understanding of regime changes that are occurring. The hydrologic research described in the following chapters will be useful in decision-making pertaining to the management of water resources and migratory waterfowl habitats.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1277","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Hydrologic and geomorphic studies of the Platte River basin: U.S. Geological Survey Professional Paper 1277, 297 p., https://doi.org/10.3133/pp1277.","productDescription":"297 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":120025,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1277/report-thumb.jpg"},{"id":65397,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1277/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":416915,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74514.htm","text":"Hydrologic and morphologic changes in channels of the Platte River Basin in Colorado, Wyoming, and Nebraska: a historical perspective","linkFileType":{"id":5,"text":"html"}},{"id":494561,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74520.htm","text":"Simulated hydrologic effects of possible ground-water and surface-water management alternatives in and near the Platte River, south-central Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494560,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74519.htm","text":"A stochastic streamflow model and precipitation model for the Platte River from Gothenburg to Grand Island, Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494559,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74518.htm","text":"Relation of channel-width maintenance to sediment transport and river morphology: Platte River, south-central Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494562,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74521.htm","text":"Ground-water hydrology of the Mormon Island Crane Meadows Wildlife area near Grand Island, Hall County, Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494558,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74517.htm","text":"Interpretation of sediment data for the South Platte River in Colorado and Nebraska, and the North Platte and Platte Rivers in Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494557,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74516.htm","text":"Hydraulic geometry of the Platte River near Overton, south-central Nebraska","linkFileType":{"id":5,"text":"html"}},{"id":494556,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74515.htm","text":"Effects of water development on surface-water hydrology, Platte River Basin in Colorado, Wyoming, and Nebraska upstream from Duncan Nebraska","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado, Nebraska, Wyoming","otherGeospatial":"Platte River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -105.06337546697512,\n 39.229893136534116\n ],\n [\n -102.18895980010433,\n 40.144489715784374\n ],\n [\n -100.8494900961135,\n 40.3909684886664\n ],\n [\n -97.26109805609099,\n 40.4570069139221\n ],\n [\n -95.81030659908853,\n 40.76732232232118\n ],\n [\n -96.23779355385292,\n 42.11319257035615\n ],\n [\n -96.82014771860239,\n 42.56341058787868\n ],\n [\n -102.92550353390914,\n 42.57699651556365\n ],\n [\n -105.05465161293671,\n 43.44397434759969\n ],\n [\n -107.66814025908258,\n 43.491370497698284\n ],\n [\n -107.35007550814393,\n 42.01749793928926\n ],\n [\n -105.81098030047286,\n 39.62779224334653\n ],\n [\n -105.06337546697512,\n 39.229893136534116\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6118e1","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":529861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70184255,"text":"70184255 - 1983 - Detection of infectious hematopoietic necrosis virus in river water and demonstration of waterborne transmission","interactions":[],"lastModifiedDate":"2017-03-06T09:59:58","indexId":"70184255","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2286,"text":"Journal of Fish Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Detection of infectious hematopoietic necrosis virus in river water and demonstration of waterborne transmission","docAbstract":"

In a study of the possible role of waterborne infectious haematopoietic necrosis virus in transmission of the disease among spawning sockeye salmon, Oncorhynchus nerka (Walbaum), both infection rates and virus titres were higher in fish held at high density in a side channel than in fish in the adjacent river. Virus was never isolated from river water, but was found in water from the side channel at levels ranging from 32.5 to 1600 plaque-forming units (p.f.u.)/ml. Uninfected yearling sockeye salmon held in a box in the side channel developed localized gill infections with IHN virus. The disease did not progress to the viscera until a threshold titre of about 105 p.f.u./g was reached in the gill. The effectiveness of the gill as a barrier limiting development of systemic infections means that waterborne IHN virus probably does not greatly increase the infection rate in a sockeye salmon population during spawning.

","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-2761.1983.tb00083.x","usgsCitation":"Mulcahy, D.M., Pascho, R.J., and Jenes, C., 1983, Detection of infectious hematopoietic necrosis virus in river water and demonstration of waterborne transmission: Journal of Fish Diseases, v. 6, no. 4, p. 321-330, https://doi.org/10.1111/j.1365-2761.1983.tb00083.x.","productDescription":"10","startPage":"321","endPage":"330","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":336847,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Cedar River","volume":"6","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-04-07","publicationStatus":"PW","scienceBaseUri":"58be8350e4b014cc3a3a9a53","contributors":{"authors":[{"text":"Mulcahy, Daniel M. dmulcahy@usgs.gov","contributorId":3102,"corporation":false,"usgs":true,"family":"Mulcahy","given":"Daniel","email":"dmulcahy@usgs.gov","middleInitial":"M.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":680752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pascho, Ronald J.","contributorId":177070,"corporation":false,"usgs":false,"family":"Pascho","given":"Ronald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":680753,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jenes, C.K.","contributorId":152262,"corporation":false,"usgs":false,"family":"Jenes","given":"C.K.","email":"","affiliations":[],"preferred":false,"id":680754,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70184434,"text":"70184434 - 1983 - Populations and habitat use of marine birds in the Semidi Islands, Alaska","interactions":[],"lastModifiedDate":"2017-03-08T15:27:08","indexId":"70184434","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2793,"text":"Murrelet","active":true,"publicationSubtype":{"id":10}},"title":"Populations and habitat use of marine birds in the Semidi Islands, Alaska","docAbstract":"

About one-quarter of the resident seabirds in the Gulf of Alaska breed on the Semidi Islands. In terms of biomass, the proportion is closer to one-third. The most abundant birds are Common and Thick-billed Murres, with a combined population exceeding 1 million birds. Hundreds of thousands of Horned Puffins breed in burrows on two islands. Other species numbering more than 100,000 individuals include the Northern Fulmar, Fork-tailed and Leach's Storm-Petrels, and possibly also the Black-legged Kittiwake and Tufted Puffin. Both species of storm-petrels commonly nest in side chambers of puffin burrows. Parasitic Jaegers nest in a loose colony on Chowiet Island. This behavior has not been reported elsewhere in the Gulf of Alaska. Red-faced and Pelagic Cormorants commonly change breeding colony location from year to year. The Semidi Islands are the easternmost breeding site for Least Auklets.

","language":"English","publisher":"Society for Northwestern Vertebrate Biology","doi":"10.2307/3534688","usgsCitation":"Hatch, S.A., and Hatch, M.A., 1983, Populations and habitat use of marine birds in the Semidi Islands, Alaska: Murrelet, v. 64, no. 2, p. 39-46, https://doi.org/10.2307/3534688.","productDescription":"8 p.","startPage":"39","endPage":"46","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":337134,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Gulf of Alaska, Semidi Islands","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -156.91978454589844,\n 55.96419132294944\n ],\n [\n -156.55792236328122,\n 55.96419132294944\n ],\n [\n -156.55792236328122,\n 56.25441316154926\n ],\n [\n -156.91978454589844,\n 56.25441316154926\n ],\n [\n -156.91978454589844,\n 55.96419132294944\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"64","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c12664e4b014cc3a3d353d","contributors":{"authors":[{"text":"Hatch, Scott A. 0000-0002-0064-8187 shatch@usgs.gov","orcid":"https://orcid.org/0000-0002-0064-8187","contributorId":2625,"corporation":false,"usgs":true,"family":"Hatch","given":"Scott","email":"shatch@usgs.gov","middleInitial":"A.","affiliations":[{"id":116,"text":"Alaska Science Center Biology MFEB","active":true,"usgs":true}],"preferred":true,"id":681476,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatch, Martha A.","contributorId":181576,"corporation":false,"usgs":false,"family":"Hatch","given":"Martha","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":681477,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1003875,"text":"1003875 - 1983 - Capture myopathy in a free-flying greater sandhill crane (Grus canadensis tabida) from Wisconsin","interactions":[],"lastModifiedDate":"2023-09-23T04:36:40.824013","indexId":"1003875","displayToPublicDate":"1983-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Capture myopathy in a free-flying greater sandhill crane (Grus canadensis tabida) from Wisconsin","title":"Capture myopathy in a free-flying greater sandhill crane (Grus canadensis tabida) from Wisconsin","docAbstract":"

No abstract available.

","language":"English","publisher":"Allen Press","doi":"10.7589/0090-3558-19.3.289","usgsCitation":"Windingstad, R.M., Hurley, S., and Sileo, L., 1983, Capture myopathy in a free-flying greater sandhill crane (Grus canadensis tabida) from Wisconsin: Journal of Wildlife Diseases, v. 19, no. 3, p. 289-290, https://doi.org/10.7589/0090-3558-19.3.289.","productDescription":"2 p.","startPage":"289","endPage":"290","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":135932,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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