Historic stream flow data were compiled and record extension techniques were used, when necessary, to develop a monthly stream flow record for 1953-82 at streamflow-gaging stations on the James River in North Dakota and South Dakota. The record extension techniques included both Maintenance of Variance Extension Type 1 and Ordinary Least Squares.
In addition to the historic stream flow record, synthesized unregulated streamflow was computed for gaging stations on the James River for 1953-82 by eliminating the effects of Jamestown Reservoir, Pipestem Reservoir, Sand Lake National Wildlife Refuge, and the consumptive surface-water withdrawals. Maintenance of Variance Extension Type 1, Ordinary Least Squares regression, water-balance procedures, and drainage-area ratio methods were used to compute the unregulated streamflows.
Mean annual historic stream flow of the James River at Jamestown is about 7,000 acre-feet less than the mean annual unregulated streamflow. Mean monthly unregulated streamflow is greater than mean monthly historic streamflow during March, April, and May; during all other months, unregulated stream flow is less than historic streamflow.
The climate during 1953-82 was compared to the climate records, which range in length from 53 to 102 years, in the James River basin to determine if the climate during 1953-82 was similar to the climate that has occurred during the last 90 years. On the basis of the climate analysis, the data-development period (1953-82) does not represent an abnormally wet or dry period. Thus, the streamflow during the data-development period represents a range of streamflows that might be expected to occur during the last 90 years.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894039","usgsCitation":"Wiche, G.J., Benson, R.D., and Emerson, D.G., 1989, Streamflow at selected gaging stations on the James River in North Dakota and South Dakota, 1953-82, with a section on climatology: U.S. Geological Survey Water-Resources Investigations Report 89-4039, Report: v, 99 p.; Plate: 10.34 x 16.30 inches, https://doi.org/10.3133/wri894039.","productDescription":"Report: v, 99 p.; Plate: 10.34 x 16.30 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":159983,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4039/report-thumb.jpg"},{"id":59262,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4039/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59263,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4039/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4e91","contributors":{"authors":[{"text":"Wiche, Gregg J. gjwiche@usgs.gov","contributorId":1675,"corporation":false,"usgs":true,"family":"Wiche","given":"Gregg","email":"gjwiche@usgs.gov","middleInitial":"J.","affiliations":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":203321,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benson, Rick D.","contributorId":60303,"corporation":false,"usgs":true,"family":"Benson","given":"Rick","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":203319,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":203320,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":63313,"text":"gq1624 - 1989 - Geologic map of the Buckhorn Mountain quadrangle, Larimer County, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:44","indexId":"gq1624","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1624","title":"Geologic map of the Buckhorn Mountain quadrangle, Larimer County, Colorado","language":"ENGLISH","doi":"10.3133/gq1624","usgsCitation":"Braddock, W.A., O’Connor, J.T., and Curtin, G.C., 1989, Geologic map of the Buckhorn Mountain quadrangle, Larimer County, Colorado: U.S. Geological Survey Geologic Quadrangle 1624, 1 map :col. ;58 x 44 cm., on sheet 74 x 81 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1624.","productDescription":"1 map :col. ;58 x 44 cm., on sheet 74 x 81 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102698,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1148.htm","linkFileType":{"id":5,"text":"html"},"description":"1148"},{"id":249416,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1624/report.pdf","size":"71","linkFileType":{"id":1,"text":"pdf"}},{"id":252815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1624/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.36749999999999,40.5 ], [ -105.36749999999999,40.6175 ], [ -105.25,40.6175 ], [ -105.25,40.5 ], [ -105.36749999999999,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d70b","contributors":{"authors":[{"text":"Braddock, William A.","contributorId":61010,"corporation":false,"usgs":true,"family":"Braddock","given":"William","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":268660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connor, Joseph T.","contributorId":61832,"corporation":false,"usgs":true,"family":"O’Connor","given":"Joseph","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":268661,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curtin, Gary C.","contributorId":89109,"corporation":false,"usgs":true,"family":"Curtin","given":"Gary","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":268662,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27810,"text":"wri894107 - 1989 - Estimating pumping time and ground-water withdrawals using energy- consumption data","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri894107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4107","title":"Estimating pumping time and ground-water withdrawals using energy- consumption data","docAbstract":"Evaluation of the hydrology of an aquifer requires knowledge about the volume of groundwater in storage and also about the volume of groundwater withdrawals. Totalizer flow meters may be installed at pumping plants to measure withdrawals; however, it generally is impractical to equip all pumping plants in an area with meters. A viable alternative is the use of rate-time methods. Rate-time methods may be used at individual pumping plants to decrease the data collection necessary for determining withdrawals. At sites where pumping-time measurement devices are not installed, pumping time may be determined on the basis of energy consumption and power demand. At pumping plants where energy consumption is metered, data acquired by reading of meters is used to estimate pumping time. Care needs to be taken to read these meters correctly. At pumping plants powered by electricity, the calculations need to be modified if transformers are present. At pumping plants powered by natural gas, the effects of the pressure-correction factor need to be included in the calculations. At pumping plants powered by gasoline, diesel oil, or liquid petroleum gas, the geometry of storage tanks needs to be analyzed as part of the calculations. The relation between power demand and pumping rate at a pumping plant can be described through the use of the power-consumption coefficient. Where equipment and hydrologic conditions are stable, this coefficient can be applied to total energy consumption at a site to estimate total groundwater withdrawals. Random sampling of power consumption coefficients can be used to estimate area-wide groundwater withdrawal. 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T.","contributorId":20713,"corporation":false,"usgs":true,"family":"Hurr","given":"R. T.","affiliations":[],"preferred":false,"id":198721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Litke, D. W.","contributorId":94346,"corporation":false,"usgs":true,"family":"Litke","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":198722,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":27851,"text":"wri894027 - 1989 - A numerical solution for the diffusion equation in hydrogeologic systems","interactions":[],"lastModifiedDate":"2018-01-30T20:57:46","indexId":"wri894027","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4027","title":"A numerical solution for the diffusion equation in hydrogeologic systems","docAbstract":"The documentation of a computer code for the numerical solution of the linear diffusion equation in one or two dimensions in Cartesian or cylindrical coordinates is presented. Applications of the program include molecular diffusion, heat conduction, and fluid flow in confined systems. The flow media may be anisotropic and heterogeneous. The model is formulated by replacing the continuous linear diffusion equation by discrete finite-difference approximations at each node in a block-centered grid. The resulting matrix equation is solved by the method of preconditioned conjugate gradients. The conjugate gradient method does not require the estimation of iteration parameters and is guaranteed convergent in the absence of rounding error. The matrixes are preconditioned to decrease the steps to convergence. The model allows the specification of any number of boundary conditions for any number of stress periods, and the output of a summary table for selected nodes showing flux and the concentration of the flux quantity for each time step. The model is written in a modular format for ease of modification. The model was verified by comparison of numerical and analytical solutions for cases of molecular diffusion, two-dimensional heat transfer, and axisymmetric radial saturated fluid flow. Application of the model to a hypothetical two-dimensional field situation of gas diffusion in the unsaturated zone is demonstrated. The input and output files are included as a check on program installation. The definition of variables, input requirements, flow chart, and program listing are included in the attachments. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies of the report can be purchased from Books and Open-File Reports Section,","doi":"10.3133/wri894027","usgsCitation":"Ishii, A.L., Healy, R.W., and Striegl, R.G., 1989, A numerical solution for the diffusion equation in hydrogeologic systems: U.S. Geological Survey Water-Resources Investigations Report 89-4027, viii, 86 p. :ill. ;28 cm., https://doi.org/10.3133/wri894027.","productDescription":"viii, 86 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":56672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4027/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":2169,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=WRIR&number=89-4027","linkFileType":{"id":5,"text":"html"}},{"id":124299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4027/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ab940","contributors":{"authors":[{"text":"Ishii, A. L.","contributorId":61464,"corporation":false,"usgs":true,"family":"Ishii","given":"A.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":198779,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, R. W.","contributorId":89872,"corporation":false,"usgs":true,"family":"Healy","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":198781,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Striegl, Robert G. 0000-0002-8251-4659 rstriegl@usgs.gov","orcid":"https://orcid.org/0000-0002-8251-4659","contributorId":1630,"corporation":false,"usgs":true,"family":"Striegl","given":"Robert","email":"rstriegl@usgs.gov","middleInitial":"G.","affiliations":[{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":200,"text":"Coop Res Unit Seattle","active":true,"usgs":true}],"preferred":false,"id":198780,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":63418,"text":"gq1659 - 1989 - Geologic map of the Twin Lakes quadrangle, McKinley County, New Mexico","interactions":[{"subject":{"id":42930,"text":"ofr8077 - 1980 - Preliminary geologic map of the Twin Lakes Quadrangle, McKinley County, New Mexico","indexId":"ofr8077","publicationYear":"1980","noYear":false,"title":"Preliminary geologic map of the Twin Lakes Quadrangle, McKinley County, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":63418,"text":"gq1659 - 1989 - Geologic map of the Twin Lakes quadrangle, McKinley County, New Mexico","indexId":"gq1659","publicationYear":"1989","noYear":false,"title":"Geologic map of the Twin Lakes quadrangle, McKinley County, New Mexico"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:47","indexId":"gq1659","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1659","title":"Geologic map of the Twin Lakes quadrangle, McKinley County, New Mexico","language":"ENGLISH","doi":"10.3133/gq1659","usgsCitation":"Zech, R.S., 1989, Geologic map of the Twin Lakes quadrangle, McKinley County, New Mexico: U.S. Geological Survey Geologic Quadrangle 1659, 1 map :col. ;58 x 47 cm., on sheet 84 x 96 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1659.","productDescription":"1 map :col. ;58 x 47 cm., on sheet 84 x 96 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102725,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1175.htm","linkFileType":{"id":5,"text":"html"},"description":"1175"},{"id":249512,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1659/report.pdf","size":"68","linkFileType":{"id":1,"text":"pdf"}},{"id":252994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1659/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.86749999999999,35.6175 ], [ -108.86749999999999,35.75 ], [ -108.75,35.75 ], [ -108.75,35.6175 ], [ -108.86749999999999,35.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a2d4","contributors":{"authors":[{"text":"Zech, R. 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At each site, one deep well was completed below the first confining clay encountered in the upper Tehama Formation to determine hydraulic gradients between water-bearing deposits in the Tehama Formation and overlying channel deposits. At three sites along Cottonwood Creek, two shallow wells were drilled at each site on a line perpendicular to the stream channel to determine if groundwater in channel deposits is moving toward or away from the stream channel and to monitor water levels. Geophysical logs were correlated with lithologic logs compiled from analyses of drill cuttings to determine depths for setting well screens. After pumping to confirm hydraulic connection between each well and the Tehama Formation, water levels were monitored monthly from June 1984 to June 1985; at two sites, water levels were above the altitude of the stream channel bottom during all streamflow conditions. Tritium dating indicates two wells have water more than 100 years old; one well has either a mixture of old and new water or an intermediate-aged water. 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J.","contributorId":52988,"corporation":false,"usgs":true,"family":"Johnson","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198882,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houston, E.R.","contributorId":67551,"corporation":false,"usgs":true,"family":"Houston","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":198883,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Neil, J. M.","contributorId":27464,"corporation":false,"usgs":true,"family":"Neil","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":198881,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27533,"text":"wri884172 - 1989 - Aquifer-system compaction, Tucson Basin and Avra Valley, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri884172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4172","title":"Aquifer-system compaction, Tucson Basin and Avra Valley, Arizona","docAbstract":"Groundwater declines of several ft/yr since the 1940 's have induced aquifer-system compaction and land subsidence of as much as 0.5 ft in the Tucson basin and 1.1 ft in Avra Valley, Arizona. Aquifer system compaction is affected by the layering, hydraulic diffusivity, preconsolidation-stress threshold, and stress history of the aquifer system. Layering at extensometer sites can be categorized into three general groups that typify the fine-grained and coarse-grained layering within the Fort Lowell Formation and upper Tinaja beds. Data from the first group show almost as much elastic as inelastic compaction, a layering frequency of six layers/100 ft, and weighted-average aquitard thicknesses of 20 to 50 ft. Data from the second group show inelastic compaction, a layering frequency of two to three layers/100 ft, an average aquitard thickness of less than 20 ft. Data from the third group show inelastic compaction, a layering frequency of fewer than two layers/100 ft, an average aquitard thickness of more than 30 ft. A one-dimensional compaction model was applied to data from six extensometers to simulate aquifer-system compaction of less than 0.1 ft. Values of elastic and some values of inelastic specific storage are comparable to values estimated in California. Parts of the aquifer system appear to be in transition from predominantly elastic to inelastic compaction. Water level declines since 1940 at six extensometer sites are within an estimated preconsolidation-stress threshold of 50 to 150 ft. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri884172","usgsCitation":"Hanson, R.T., 1989, Aquifer-system compaction, Tucson Basin and Avra Valley, Arizona: U.S. Geological Survey Water-Resources Investigations Report 88-4172, vi, 69 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884172.","productDescription":"vi, 69 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4172/report-thumb.jpg"},{"id":56392,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4172/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48abe4b07f02db52d0c1","contributors":{"authors":[{"text":"Hanson, R. T.","contributorId":91148,"corporation":false,"usgs":true,"family":"Hanson","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":198272,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27551,"text":"wri884188 - 1989 - Streamflow, sediment discharge, and streambank erosion in Cache Creek, Yolo County, California, 1953-86","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri884188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4188","title":"Streamflow, sediment discharge, and streambank erosion in Cache Creek, Yolo County, California, 1953-86","docAbstract":"This report defines cross-section geometry, slope, sinuosity, bed and bank material size, and sediment discharge for Cache Creek, Capay Valley, Yolo County, California; it also relates streambank erosion to daily volumes of flow greater than 6,000 acre-ft. Mean bed elevations at six cross sections during 1983-86 and at two cross sections over several years indicate general stability of elevations in the gravel-bed channel. Water-surface slope ranged from 0.13% to 0.51% in four reaches during two flood peaks. Aerial photographs indicate that the Cache Creek channel is sinuous. About 67% of bed material at 45 cross sections is gravel, and 23% is coarser than gravel. Bank material at 27 cross sections contain sands, silt, and clay, except at one cross section where cobbles and gravel form the left bank. The sediment-discharge rate was lower during 1984-86 than in 1960-63. Streambank erosion was measured by comparing aerial photographs taken over several years. Eroded areas total about 13.2 million sq ft (300 acres) from 1953 to 1984. Net migration is toward the right bank. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nCopies can be purchased from U.S. Geological Survey Books and Open-File Reports Section,","doi":"10.3133/wri884188","usgsCitation":"Harmon, J., 1989, Streamflow, sediment discharge, and streambank erosion in Cache Creek, Yolo County, California, 1953-86: U.S. Geological Survey Water-Resources Investigations Report 88-4188, v, 40 p. :ill. ;28 cm., https://doi.org/10.3133/wri884188.","productDescription":"v, 40 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":158970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4188/report-thumb.jpg"},{"id":56406,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4188/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4ca6","contributors":{"authors":[{"text":"Harmon, J.G.","contributorId":90753,"corporation":false,"usgs":true,"family":"Harmon","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":198307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67097,"text":"i1894 - 1989 - Historic trail maps of the Sterling 1° x 2° quadrangle, northeastern Colorado","interactions":[],"lastModifiedDate":"2021-10-22T21:55:20.903255","indexId":"i1894","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1894","title":"Historic trail maps of the Sterling 1° x 2° quadrangle, northeastern Colorado","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1894","usgsCitation":"Scott, G., 1989, Historic trail maps of the Sterling 1° x 2° quadrangle, northeastern Colorado: U.S. Geological Survey IMAP 1894, Report: 23 p.; 2 Plates: 29.22 x 22.68 inches and 28.25 x 22.20 inches, https://doi.org/10.3133/i1894.","productDescription":"Report: 23 p.; 2 Plates: 29.22 x 22.68 inches and 28.25 x 22.20 inches","costCenters":[],"links":[{"id":390877,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9973.htm"},{"id":189385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1894/report-thumb.jpg"},{"id":91646,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1894/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256451,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1894/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256452,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1894/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Colorado","otherGeospatial":"Sterling 1° x 2° quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104,40 ], [ -104,41 ], [ -102,41 ], [ -102,40 ], [ -104,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6885ac","contributors":{"authors":[{"text":"Scott, G. R.","contributorId":61398,"corporation":false,"usgs":true,"family":"Scott","given":"G. R.","affiliations":[],"preferred":false,"id":275595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67108,"text":"i1803A - 1989 - Map showing exposures of limonitic rocks and hydrothermally altered rocks in the Dillon 1 degree by 2 degrees Quadrangle, Idaho and Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"i1803A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1803","subseriesTitle":"NONE","chapter":"A","title":"Map showing exposures of limonitic rocks and hydrothermally altered rocks in the Dillon 1 degree by 2 degrees Quadrangle, Idaho and Montana","language":"ENGLISH","doi":"10.3133/i1803A","usgsCitation":"Segal, D.B., and Rowan, L.C., 1989, Map showing exposures of limonitic rocks and hydrothermally altered rocks in the Dillon 1 degree by 2 degrees Quadrangle, Idaho and Montana: U.S. Geological Survey IMAP 1803, 1 map :col. ;45 x 63 cm., on sheet 59 x 104 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1803A.","productDescription":"1 map :col. ;45 x 63 cm., on sheet 59 x 104 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107132,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9924.htm","linkFileType":{"id":5,"text":"html"},"description":"9924"},{"id":188041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114,45 ], [ -114,46 ], [ -112,46 ], [ -112,45 ], [ -114,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c869","contributors":{"authors":[{"text":"Segal, D. B.","contributorId":60236,"corporation":false,"usgs":true,"family":"Segal","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":275616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rowan, L. C.","contributorId":40584,"corporation":false,"usgs":true,"family":"Rowan","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":275615,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":38304,"text":"ofr89300H - 1989 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:49","indexId":"ofr89300H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-300","chapter":"H","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska","language":"ENGLISH","doi":"10.3133/ofr89300H","usgsCitation":"Townshend, J.B., O’Connell, R.V., and Varner, C.A., 1989, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: U.S. Geological Survey Open-File Report 89-300, 19 p.:ill. ;28 cm., https://doi.org/10.3133/ofr89300H.","productDescription":"19 p.:ill. ;28 cm.","costCenters":[],"links":[{"id":164779,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0300h/report-thumb.jpg"},{"id":64676,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0300h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2d9","contributors":{"authors":[{"text":"Townshend, John B.","contributorId":70383,"corporation":false,"usgs":true,"family":"Townshend","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":219574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connell, R. V.","contributorId":88755,"corporation":false,"usgs":true,"family":"O’Connell","given":"R.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":219575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Varner, Carol Ann","contributorId":66705,"corporation":false,"usgs":true,"family":"Varner","given":"Carol","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":219573,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":66243,"text":"i1874 - 1989 - Geologic map of Yosemite National Park and vicinity, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"i1874","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1874","subseriesTitle":"NONE","title":"Geologic map of Yosemite National Park and vicinity, California","docAbstract":"This digital map database represents the general distribution of bedrock and surficial deposits of the Yosemite National Park vicinity. It was produced directly from the file used to create the print version in 1989. The Yosemite National Park region is comprised of portions of 15 7.5 minute quadrangles. The original publication of the map in 1989 included the map, described map units and provided correlations, as well as a geologic summary and references, all on the same sheet. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The scale of the source maps limits the spatial resolution (scale) of the database to 1:125,000 or smaller.","language":"ENGLISH","doi":"10.3133/i1874","usgsCitation":"Huber, N., Bateman, P.C., and Wahrhaftig, C., 1989, Geologic map of Yosemite National Park and vicinity, California: U.S. Geological Survey IMAP 1874, 1 map :col. ;66 x 53 cm., on sheet 86 x 111 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1874.","productDescription":"1 map :col. ;66 x 53 cm., on sheet 86 x 111 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":101972,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_318.htm","linkFileType":{"id":5,"text":"html"},"description":"318"},{"id":187763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6129,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i1874/","linkFileType":{"id":5,"text":"html"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.91666666666667,37.46666666666667 ], [ -119.91666666666667,38.21666666666667 ], [ -119.16666666666667,38.21666666666667 ], [ -119.16666666666667,37.46666666666667 ], [ -119.91666666666667,37.46666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2ac7","contributors":{"authors":[{"text":"Huber, N.K.","contributorId":73610,"corporation":false,"usgs":true,"family":"Huber","given":"N.K.","affiliations":[],"preferred":false,"id":274229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bateman, P. C.","contributorId":27851,"corporation":false,"usgs":true,"family":"Bateman","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":274228,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wahrhaftig, Clyde","contributorId":102473,"corporation":false,"usgs":true,"family":"Wahrhaftig","given":"Clyde","email":"","affiliations":[],"preferred":false,"id":274230,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":38302,"text":"ofr89300F - 1989 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:49","indexId":"ofr89300F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-300","chapter":"F","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska","language":"ENGLISH","doi":"10.3133/ofr89300F","usgsCitation":"Townshend, J.B., O’Connell, R.V., and Varner, C.A., 1989, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: U.S. Geological Survey Open-File Report 89-300, 19 p. ill. ;28 cm., https://doi.org/10.3133/ofr89300F.","productDescription":"19 p. ill. ;28 cm.","costCenters":[],"links":[{"id":164777,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0300f/report-thumb.jpg"},{"id":64674,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0300f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a2d4","contributors":{"authors":[{"text":"Townshend, John B.","contributorId":70383,"corporation":false,"usgs":true,"family":"Townshend","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":219568,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Connell, R. V.","contributorId":88755,"corporation":false,"usgs":true,"family":"O’Connell","given":"R.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":219569,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Varner, Carol Ann","contributorId":66705,"corporation":false,"usgs":true,"family":"Varner","given":"Carol","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":219567,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27587,"text":"wri884234 - 1989 - Geohydrology of the alluvial and terrace deposits of the North Canadian River from Oklahoma City to Eufaula Lake, central Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri884234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4234","title":"Geohydrology of the alluvial and terrace deposits of the North Canadian River from Oklahoma City to Eufaula Lake, central Oklahoma","docAbstract":"This investigation was undertaken to describe the geohydrology of the alluvial and terrace deposits along the North Canadian River between Lake Overholser and Eufaula Lake, an area of about 1,835 square miles, and to determine the maximum annual yield of ground water.\r\nA 1982 water-level map of the alluvial and terrace aquifer was prepared using field data and published records. Data from test holes and other data from the files of the U.S. Geological Survey and the Oklahoma Water Resources Board were used to establish the approximate thickness of the alluvial and terrace deposits.\r\n\r\nThe North Canadian River from Lake Overholser, near Oklahoma City, to Eufaula Lake is paralleled by a 2- to 3-mile wide band of alluvium. Scattered terrace deposits on either side of the alluvium reach an extreme width of 8 miles. Rocks of Permian age bound the alluvial and terrace deposits from the west to the midpoint of the study area; Pennsylvanian rocks bound the alluvial and terrace deposits from that point eastward.\r\n\r\nThree major aquifers are present in the study area: the alluvial and terrace aquifer, consisting of alluvium and terrace deposits of Quaternary age in a narrow band on either side of the North Canadian River; the Garber-Wellington aquifer of Permian age, consisting of an upper unconfined zone and a lower confined zone separated by relatively impermeable shales; and the Ada-Vamoosa aquifer of Pennsylvanian age. At locations were the alluvial and terrace aquifer overlies either of the other aquifers, there is hydraulic continuity between the alluvial and terrace aquifer and the other aquifers, and water levels are the same.\r\n\r\nMost large-scale municipal and industrial pumping from the Garber-Wellington aquifer is from the lower zone and has little discernible effect upon the alluvial and terrace aquifer.\r\n\r\nThe total estimated base flow of the North Canadian River for the studied reach is 264 cubic feet per second. Evapotranspiration from the basin in August is about 60 cubic feet per second for the North Canadian River from Lake Overholser to a measuring station above Eufaula Lake. Estimated recharge rates to the alluvial and terrace aquifer in the basin range from 1.7 inches at the west edge of the study area to 7.0 inches at the east edge.\r\n\r\nTotal permitted withdrawal from the aquifer, according to records of the Oklahoma Water Resources Board, ranged from 2,107 acre-feet per year in 1942 to about 21,415 acre-feet per year in 1982.\r\n\r\nSimulations of the alluvial and terrace aquifer from Lake Overholser to Eufaula Lake were made using a finite-difference model developed by McDonald and Harbaugh (1984). The area of the aquifers was subdivided into a finite-difference grid having 30 rows and 57 columns with cells measuring 1 mile in the north-south direction and 2 miles in the east-west direction. The model was calibrated in two steps: A steady-state calibration simulated head distribution prior to extensive pumping of the aquifer in 1942, and a transient calibration simulated head distribution after extensive pumpage. The final horizontal hydraulic conductivity used for the alluvial and terrace aquifer was 0.0036 feet per second (310 feet per day) at all locations. The recharge rate for the alluvial and terrace aquifer ranged from 1.7 inch per year in the west to 7.0 inches per year in the east, and averaged about 3.3 inches per year. A specific yield of 15 percent was used for the transient simulation.\r\n\r\nPermitted pumpage for 1942 through 1982 was used in the digital model to estimate the annual volume of water in storage in the alluvial and terrace aquifer for the years for this time period. The 1982 permitted pumpage rates were used for projections for 1983 to 2020. The estimated volume of water in storage was 1,940,000 acre-feet in 1982. Because the estimated recharge rate is equal to the allowed pumpage rate in 1982, the projected volume of water in storage in both 1993 and 2020 was 1,890,000 acre-feet.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-file reports, Federal Center,","doi":"10.3133/wri884234","usgsCitation":"Havens, J., 1989, Geohydrology of the alluvial and terrace deposits of the North Canadian River from Oklahoma City to Eufaula Lake, central Oklahoma: U.S. Geological Survey Water-Resources Investigations Report 88-4234, vii, 32 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri884234.","productDescription":"vii, 32 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4234/report-thumb.jpg"},{"id":56439,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56440,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56441,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56442,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56443,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56444,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56445,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56446,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56447,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56448,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56449,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56450,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4234/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56451,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4234/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8888","contributors":{"authors":[{"text":"Havens, J.S.","contributorId":12043,"corporation":false,"usgs":true,"family":"Havens","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":198372,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67121,"text":"i1924 - 1989 - Geologic map of Precambrian rocks of Rice Lake 1 degree by 2 degrees Quadrangle, northern Wisconsin","interactions":[],"lastModifiedDate":"2012-02-10T00:11:03","indexId":"i1924","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1924","subseriesTitle":"NONE","title":"Geologic map of Precambrian rocks of Rice Lake 1 degree by 2 degrees Quadrangle, northern Wisconsin","language":"ENGLISH","doi":"10.3133/i1924","usgsCitation":"Sims, P., 1989, Geologic map of Precambrian rocks of Rice Lake 1 degree by 2 degrees Quadrangle, northern Wisconsin: U.S. Geological Survey IMAP 1924, 1 map :col. ;44 x 63 cm., on sheet 78 x 102 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1924.","productDescription":"1 map :col. ;44 x 63 cm., on sheet 78 x 102 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107182,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10002.htm","linkFileType":{"id":5,"text":"html"},"description":"10002"},{"id":189405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92,45 ], [ -92,46 ], [ -90,46 ], [ -90,45 ], [ -92,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2c42","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":275631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27827,"text":"wri894079 - 1989 - Analysis of the effect of pumping on ground-water flow in the Springfield Plateau and Ozark aquifers near Springfield, Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri894079","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-4079","title":"Analysis of the effect of pumping on ground-water flow in the Springfield Plateau and Ozark aquifers near Springfield, Missouri","docAbstract":"Pumpage of water from the Ozark aquifer for public supply and industry use by the city of Springfield and surrounding communities in southwestern Missouri has significantly altered the potentiometric surface of the aquifer. Springfield is located on a regional groundwater divide that trends east and west across southern Missouri. Groundwater that once flowed north and south from the divide now moves toward Springfield. Drawdown in the Ozark aquifer beneath Springfield has increased about 50 ft near the center of the city since 1974. The area of well influence also has increased, most notably to the south and southwest, because of increased pumpage by Springfield and new groundwater withdrawals in rapidly increasing communities, such as Republic and Nixa. Changes in the potentiometric surface of the Ozark aquifer, and to a lesser extent the Springfield Plateau aquifer, resulting from stresses applied by pumpage of water supply wells has altered the hydrologic budget of the Springfield area. Downward leakage of groundwater through the Ozark confining unit has increased from about 10 cu ft/sec to about 18 cu ft/sec because drawdown in the Ozark aquifer has resulted in an increased vertical hydraulic gradient across the confining unit. Minimal quantities of water are supplied by increased upward leakage through the St. Francois confining unit. Model simulations indicate substantial quantities of water are still (1987) being removed from storage within the Ozark and Springfield Plateau aquifers and the hydrologic system is not in equilibrium at this time. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports, U.S. Geological Survey,","doi":"10.3133/wri894079","usgsCitation":"Imes, J., 1989, Analysis of the effect of pumping on ground-water flow in the Springfield Plateau and Ozark aquifers near Springfield, Missouri: U.S. Geological Survey Water-Resources Investigations Report 89-4079, vii, 63 p. :ill. ;28 cm., https://doi.org/10.3133/wri894079.","productDescription":"vii, 63 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":124040,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4079/report-thumb.jpg"},{"id":56660,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f5d4","contributors":{"authors":[{"text":"Imes, J. L.","contributorId":61428,"corporation":false,"usgs":true,"family":"Imes","given":"J. L.","affiliations":[],"preferred":false,"id":198746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26603,"text":"wri884217 - 1989 - Sources and concentrations of dissolved solids and selenium in the San Joaquin River and its tributaries, California, October 1985 to March 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"wri884217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"88-4217","title":"Sources and concentrations of dissolved solids and selenium in the San Joaquin River and its tributaries, California, October 1985 to March 1987","docAbstract":"Sources and concentrations of dissolved solids and selenium in the San Joaquin River and its tributaries, California, were assessed by a mass-balance approach to determine the effects of tile-drain water and irrigation-return flows on the river. The study included low-flow periods from October 1985 to mid-February 1986 and mid-May 1986 through March 1987, and a high-flow period from mid-February to mid-May 1985. During the combined low-flow period, the dissolved-solids load from eastside tributaries and the upper San Joaquin River accounted for only 18% of the total load at Vernalis, located farthest downstream, even though they accounted for 71% of the streamflow. Salt and Mud Sloughs contributed 40% of the dissolved-solids load but only 9% of streamflow. Unmeasured sources of dissolved solids contributed about 42% of the total load during low flow. In contrast, Salt and Mud Sloughs, which receive most of the tile-drain water that enters the river, contributed almost 80% of the total selenium load to the river, and loading of selenium concentrations were highest in Salt and Mud Sloughs and decreased downstream in the San Joaquin River with dilution from eastside tributaries. A State standard for dissolved solids of 500 mg/L was exceeded 11% of the time in the San Joaquin River at Vernalis. The U.S. Environmental Protection Agency 's 4-day average aquatic-life criterion of 5 micrograms/L of selenium was exceeded in more than 60% of the samples from the sloughs and in about 20% of the samples from the San Joaquin River, just downstream of the Merced River. (USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri884217","usgsCitation":"Clifton, D., and Gilliom, R.J., 1989, Sources and concentrations of dissolved solids and selenium in the San Joaquin River and its tributaries, California, October 1985 to March 1987: U.S. Geological Survey Water-Resources Investigations Report 88-4217, v, 33 p. :ill. ;28 cm., https://doi.org/10.3133/wri884217.","productDescription":"v, 33 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":157810,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4217/report-thumb.jpg"},{"id":55468,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699fb8","contributors":{"authors":[{"text":"Clifton, D.G.","contributorId":103292,"corporation":false,"usgs":true,"family":"Clifton","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":196691,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilliom, R. J.","contributorId":60650,"corporation":false,"usgs":true,"family":"Gilliom","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196690,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":67188,"text":"i1939 - 1989 - Geologic map of the Montrose 30' x 60' Quadrangle, southwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:21","indexId":"i1939","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1939","subseriesTitle":"NONE","title":"Geologic map of the Montrose 30' x 60' Quadrangle, southwestern Colorado","language":"ENGLISH","doi":"10.3133/i1939","usgsCitation":"Steven, T.A., and Hail, W., 1989, Geologic map of the Montrose 30' x 60' Quadrangle, southwestern Colorado: U.S. Geological Survey IMAP 1939, 1 map :col. ;88 x 55 cm., on sheet 86 x 137 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1939.","productDescription":"1 map :col. ;88 x 55 cm., on sheet 86 x 137 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107193,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10013.htm","linkFileType":{"id":5,"text":"html"},"description":"10013"},{"id":188850,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108,38 ], [ -108,38.5 ], [ -107,38.5 ], [ -107,38 ], [ -108,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696841","contributors":{"authors":[{"text":"Steven, T. A.","contributorId":42575,"corporation":false,"usgs":true,"family":"Steven","given":"T.","middleInitial":"A.","affiliations":[],"preferred":false,"id":275738,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hail, W. J. Jr.","contributorId":35332,"corporation":false,"usgs":true,"family":"Hail","given":"W. J.","suffix":"Jr.","affiliations":[],"preferred":false,"id":275737,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13776,"text":"ofr89169 - 1989 - U.S. Geological Survey - Missouri Geological Survey symposium; mineral-resource potential of the Midcontinent; program and abstracts","interactions":[{"subject":{"id":13776,"text":"ofr89169 - 1989 - U.S. Geological Survey - Missouri Geological Survey symposium; mineral-resource potential of the Midcontinent; program and abstracts","indexId":"ofr89169","publicationYear":"1989","noYear":false,"title":"U.S. Geological Survey - Missouri Geological Survey symposium; mineral-resource potential of the Midcontinent; program and abstracts"},"predicate":"SUPERSEDED_BY","object":{"id":4426,"text":"cir1043 - 1990 - U.S. Geological Survey-Missouri Geological Survey symposium; Mineral-resource potential of the Midcontinent; program and abstracts, St. Louis, Missouri, April 11-12, 1989","indexId":"cir1043","publicationYear":"1990","noYear":false,"title":"U.S. Geological Survey-Missouri Geological Survey symposium; Mineral-resource potential of the Midcontinent; program and abstracts, St. Louis, Missouri, April 11-12, 1989"},"id":1}],"supersededBy":{"id":4426,"text":"cir1043 - 1990 - U.S. Geological Survey-Missouri Geological Survey symposium; Mineral-resource potential of the Midcontinent; program and abstracts, St. Louis, Missouri, April 11-12, 1989","indexId":"cir1043","publicationYear":"1990","noYear":false,"title":"U.S. Geological Survey-Missouri Geological Survey symposium; Mineral-resource potential of the Midcontinent; program and abstracts, St. Louis, Missouri, April 11-12, 1989"},"lastModifiedDate":"2019-11-26T13:13:49","indexId":"ofr89169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-169","title":"U.S. Geological Survey - Missouri Geological Survey symposium; mineral-resource potential of the Midcontinent; program and abstracts","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr89169","usgsCitation":"Goldhaber, M.B., 1989, U.S. Geological Survey - Missouri Geological Survey symposium; mineral-resource potential of the Midcontinent; program and abstracts: U.S. Geological Survey Open-File Report 89-169, viii, 45 p., https://doi.org/10.3133/ofr89169.","productDescription":"viii, 45 p.","costCenters":[],"links":[{"id":145374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0169/report-thumb.jpg"},{"id":369667,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0169/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Midcontinent","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.94140625,\n 30.259067203213018\n ],\n [\n -82.30957031249999,\n 30.259067203213018\n ],\n [\n -82.30957031249999,\n 44.809121700077355\n ],\n [\n -104.94140625,\n 44.809121700077355\n ],\n [\n -104.94140625,\n 30.259067203213018\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6998b9","contributors":{"editors":[{"text":"Pratt, Walden P.","contributorId":88342,"corporation":false,"usgs":true,"family":"Pratt","given":"Walden","email":"","middleInitial":"P.","affiliations":[],"preferred":true,"id":749338,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Goldhaber, Martin B. 0000-0002-1785-4243 mgold@usgs.gov","orcid":"https://orcid.org/0000-0002-1785-4243","contributorId":1339,"corporation":false,"usgs":true,"family":"Goldhaber","given":"Martin","email":"mgold@usgs.gov","middleInitial":"B.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":168364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":31104,"text":"ofr89461 - 1989 - Gold, platinum, and silver analytical results and gold signatures from the Bonnifield mining district, Fairbanks and Healy quadrangles, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:13","indexId":"ofr89461","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-461","title":"Gold, platinum, and silver analytical results and gold signatures from the Bonnifield mining district, Fairbanks and Healy quadrangles, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89461","usgsCitation":"Cathrall, J.B., Antweiler, J., VanTrump, G., and Mosier, E.L., 1989, Gold, platinum, and silver analytical results and gold signatures from the Bonnifield mining district, Fairbanks and Healy quadrangles, Alaska: U.S. Geological Survey Open-File Report 89-461, 23 p. :ill. ;28 cm., https://doi.org/10.3133/ofr89461.","productDescription":"23 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":161113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0461/report-thumb.jpg"},{"id":59681,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0461/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673fdd","contributors":{"authors":[{"text":"Cathrall, J. B.","contributorId":29400,"corporation":false,"usgs":true,"family":"Cathrall","given":"J.","middleInitial":"B.","affiliations":[],"preferred":false,"id":205003,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Antweiler, J.C.","contributorId":35722,"corporation":false,"usgs":true,"family":"Antweiler","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":205004,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"VanTrump, George Jr.","contributorId":54193,"corporation":false,"usgs":true,"family":"VanTrump","given":"George","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":205005,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mosier, E. L.","contributorId":71537,"corporation":false,"usgs":true,"family":"Mosier","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":205006,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":31102,"text":"ofr89375 - 1989 - Analytical results and sample locality map of stream-sediment heavy-mineral-concentrate, and rock samples from the Continental Divide (NM- 020-044) and Horse Mountain (NM-020-043) Wilderness Study Areas, Catron County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:09:12","indexId":"ofr89375","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1989","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":"89-375","title":"Analytical results and sample locality map of stream-sediment heavy-mineral-concentrate, and rock samples from the Continental Divide (NM- 020-044) and Horse Mountain (NM-020-043) Wilderness Study Areas, Catron County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr89375","usgsCitation":"Adrian, B.M., Turner, R.L., Briggs, P., Bradley, L.A., and Delaney, T.A., 1989, Analytical results and sample locality map of stream-sediment heavy-mineral-concentrate, and rock samples from the Continental Divide (NM- 020-044) and Horse Mountain (NM-020-043) Wilderness Study Areas, Catron County, New Mexico: U.S. Geological Survey Open-File Report 89-375, 26 p. :maps ;28 cm., https://doi.org/10.3133/ofr89375.","productDescription":"26 p. :maps ;28 cm.","costCenters":[],"links":[{"id":161381,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1989/0375/report-thumb.jpg"},{"id":59679,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1989/0375/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67eb73","contributors":{"authors":[{"text":"Adrian, B. M.","contributorId":71535,"corporation":false,"usgs":true,"family":"Adrian","given":"B.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":204996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turner, R. L.","contributorId":93903,"corporation":false,"usgs":true,"family":"Turner","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":204997,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Briggs, Paul H.","contributorId":107691,"corporation":false,"usgs":true,"family":"Briggs","given":"Paul H.","affiliations":[],"preferred":false,"id":204998,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bradley, L. A.","contributorId":35738,"corporation":false,"usgs":true,"family":"Bradley","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204995,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Delaney, T. A.","contributorId":12049,"corporation":false,"usgs":true,"family":"Delaney","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204994,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ]}