{"pageNumber":"4985","pageRowStart":"124600","pageSize":"25","recordCount":184563,"records":[{"id":2698,"text":"wsp2239 - 1985 - Ground-water resources and potential hydrologic effects of surface coal mining in the northern Powder River basin, southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"wsp2239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2239","title":"Ground-water resources and potential hydrologic effects of surface coal mining in the northern Powder River basin, southeastern Montana","docAbstract":"The shallow ground-water system in the northern Powder River Basin consists of Upper Cretaceous to Holocene aquifers overlying the Bearpaw Shale--namely, the Fox Hills Sandstone; Hell Creek, Fort Union, and Wasatch Formations; terrace deposits; and alluvium. Ground-water flow above the Bearpaw Shale can be divided into two general flow patterns. An upper flow pattern occurs in aquifers at depths of less than about 200 feet and occurs primarily as localized flow controlled by the surface topography. A lower flow pattern occurs in aquifers at depths from about 200 to 1,200 feet and exhibits a more regional flow, which is generally northward toward the Yellowstone River with significant flow toward the Powder and Tongue Rivers. \r\n\r\nThe chemical quality of water in the shallow ground-water system in the study area varies widely, and most of the ground water does not meet standards for dissolved constituents in public drinking water established by the U.S. Environmental Protection Agency. Water from depths less than 200 feet generally is a sodium sulfate type having an average dissolved-solids concentration of 2,100 milligrams per liter. Sodium bicarbonate water having an average dissolved-solids concentration of 1,400 milligrams per liter is typical from aquifers in the shallow ground-water system at depths between 200 and 1,200 feet. \r\n\r\nEffects of surface coal mining on the water resources in the northern Powder River Basin are dependent on the stratigraphic location of the mine cut. Where the cut lies above the water-yielding zone, the effects will be minimal. Where the mine cut intersects a water-ielding zone, effects on water levels and flow patterns can be significant locally, but water levels and flow patterns will return to approximate premining conditions after mining ceases. Ground water in and near active and former mines may become more mineralized, owing to the placement of spoil material from the reducing zone in the unsaturated zone where the minerals are subject to oxidation. Regional effects probably will be small because of the limited areal extent of ground-water flow systems where mining is feasible. \r\n\r\nResults of digital models are presented to illustrate the effects of varying hydraulic properties on water-level changes resulting from mine dewatering. The model simulations were designed to depict maximum-drawdown situations. One simulation indicates that after 20 years of continuous dewatering of an infinite, homogeneous, isotropic aquifer that is 10 feet thick and has an initial potentiometric surface 10 feet above the top of the aquifer, water-level declines greater than 1 foot would generally be limited to within 7.5 miles of the center of the mine excavation; declines greater than 2 feet to within about 6 miles; declines greater than 5 feet to within about 3.7 miles; declines greater than 10 feet to within about 1.7 miles; and declines greater than 15 feet to within 1.2 miles.","language":"ENGLISH","publisher":"U.S. G.P.O :\r\nFor sale by the Supt. of Docs., U.S. G.P.O.,","doi":"10.3133/wsp2239","usgsCitation":"Slagle, S.E., Lewis, B.D., and Lee, R.W., 1985, Ground-water resources and potential hydrologic effects of surface coal mining in the northern Powder River basin, southeastern Montana: U.S. Geological Survey Water Supply Paper 2239, iv, 34 p. :ill., maps ;28 cm.; 2 plates in pocket, https://doi.org/10.3133/wsp2239.","productDescription":"iv, 34 p. :ill., maps ;28 cm.; 2 plates in pocket","costCenters":[],"links":[{"id":138838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2239/report-thumb.jpg"},{"id":247236,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2239/plate-1.pdf","size":"10143","linkFileType":{"id":1,"text":"pdf"}},{"id":247237,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2239/plate-2.pdf","size":"6388","linkFileType":{"id":1,"text":"pdf"}},{"id":29067,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2239/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e13d","contributors":{"authors":[{"text":"Slagle, Steven E.","contributorId":35284,"corporation":false,"usgs":true,"family":"Slagle","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145629,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, Barney D.","contributorId":93873,"corporation":false,"usgs":true,"family":"Lewis","given":"Barney","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":145630,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, Roger W.","contributorId":105273,"corporation":false,"usgs":true,"family":"Lee","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145631,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28398,"text":"wri854129 - 1985 - Comparison of two methods for estimating ground-water recharge in 1978-80, Santa Maria Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:49","indexId":"wri854129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4129","title":"Comparison of two methods for estimating ground-water recharge in 1978-80, Santa Maria Valley, California","docAbstract":"Infiltration from the Santa Maria River and the lower part of the Sisquoc River constitutes most of the groundwater recharge to the aquifer system of Santa Maria Valley, California. The annual recharge volumes commonly are much greater or smaller than the long-term average annual recharge. A comparison of two methods of estimating annual recharge indicates that, in Santa Maria Valley, a seepage-loss method is comparable to a water-level-change method. Both methods indicate that recharge was about 600,000 acre-feet during 1978-80. By the seepage-loss method, annual recharges for 1978, 1979, and 1980 are estimated as 290,000, 130,000, and 190,000 acre-feet. Using the water-level-change method, annual recharges during 1978, 1979, and 1980 are estimated at 230,000, 190,000, and 160,000 acre-feet. A log-Pearson Type III probability distribution of annual flows gaged on the Sisquoc River indicates that average annual recurrence intervals of recharge events equal to those of 1978, 1979, and 1980 are 20, 4, and 10 years. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854129","usgsCitation":"Lipinski, P., 1985, Comparison of two methods for estimating ground-water recharge in 1978-80, Santa Maria Valley, California: U.S. Geological Survey Water-Resources Investigations Report 85-4129, iv, 17 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854129.","productDescription":"iv, 17 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4129/report-thumb.jpg"},{"id":57204,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4129/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab648","contributors":{"authors":[{"text":"Lipinski, Paul","contributorId":34144,"corporation":false,"usgs":true,"family":"Lipinski","given":"Paul","affiliations":[],"preferred":false,"id":199728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1817,"text":"wsp2205 - 1985 - Mathematical model of the Tesuque aquifer system near Pojoaque, New Mexico","interactions":[{"subject":{"id":9419,"text":"ofr801023 - 1980 - Mathematical model of the Tesuque aquifer system underlying Pojoaque River basin and vicinity, New Mexico","indexId":"ofr801023","publicationYear":"1980","noYear":false,"title":"Mathematical model of the Tesuque aquifer system underlying Pojoaque River basin and vicinity, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":1817,"text":"wsp2205 - 1985 - Mathematical model of the Tesuque aquifer system near Pojoaque, New Mexico","indexId":"wsp2205","publicationYear":"1985","noYear":false,"title":"Mathematical model of the Tesuque aquifer system near Pojoaque, New Mexico"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp2205","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2205","title":"Mathematical model of the Tesuque aquifer system near Pojoaque, New Mexico","docAbstract":"A three-dimensional digital model of ground-water flow was constructed to represent the dipping anisotropic beds of the Tesuque aquifer system underlying the Pojoaque River basin and vicinity, New Mexico. Simulations of steady-state conditions and historical ground-water withdrawals were consistent with observed data. The model was used to simulate the response of the aquifer system to an irrigation-development plan in the Pojoaque River basin. Storage is the main source of water; 34.05 cubic feet per second (86 percent of the withdrawal rate) was simulated to be withdrawn from storage after 50 years of withdrawals for irrigation development. The maximum simulated water-level decline was 334 feet, and the net simulated streamflow capture from the Rio Grande and the Santa Cruz, Pojoaque, and Santa Fe Rivers was 5.63 cubic feet per second (14 percent of the withdrawal rate). The sensitivity of the model was tested by varying aquifer characteristics to the limits of the plausible range. Change in hydraulic head in the Pojoaque River basin is most sensitive to hydraulic conductivity. In all simulations, after 50 years of withdrawals, the maximum simulated decline in hydraulic head ranged between 210 and 474 feet, storage in the aquifer system was the source of 80 to 90 percent of the water withdrawn from wells, and streamflow capture from the Rio Grande and its tributaries plus irrigation diversions from the tributaries of the Pojoaque River simulated a decrease in the flow of the Rio Grande of between 17.13 and 21.11 cubic feet per second.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2205","usgsCitation":"Hearne, G.A., 1985, Mathematical model of the Tesuque aquifer system near Pojoaque, New Mexico: U.S. Geological Survey Water Supply Paper 2205, vii, 75 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2205.","productDescription":"vii, 75 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":137216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2205/report-thumb.jpg"},{"id":27013,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2205/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db60ffd1","contributors":{"authors":[{"text":"Hearne, Glenn A.","contributorId":50882,"corporation":false,"usgs":true,"family":"Hearne","given":"Glenn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144204,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29018,"text":"wri844247 - 1985 - Estimation of selected flow and water-quality characteristics of Alaskan streams","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri844247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4247","title":"Estimation of selected flow and water-quality characteristics of Alaskan streams","docAbstract":"Although hydrologic data are either sparse or nonexistent for large areas of Alaska, the drainage area, area of lakes, glacier and forest cover, and average precipitation in a hydrologic basin of interest can be measured or estimated from existing maps. Application of multiple linear regression techniques indicates that statistically significant correlations exist between properties of basins determined from maps and measured streamflow characteristics. This suggests that corresponding characteristics of ungaged basins can be estimated. Streamflow frequency characteristics can be estimated from regional equations developed for southeast, south-central and Yukon regions. Statewide or modified regional equations must be used, however, for the southwest, northwest, and Arctic Slope regions where there is a paucity of data. Equations developed from basin characteristics are given to estimate suspended-sediment values for glacial streams and, with less reliability, for nonglacial streams. Equations developed from available specific conductance data are given to estimate concentrations of major dissolved inorganic constituents. Suggestions are made for expanding the existing data base and thus improving the ability to estimate hydrologic characteristics for Alaskan streams. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844247","usgsCitation":"Parks, B., and Madison, R.J., 1985, Estimation of selected flow and water-quality characteristics of Alaskan streams: U.S. Geological Survey Water-Resources Investigations Report 84-4247, v, 64 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844247.","productDescription":"v, 64 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4247/report-thumb.jpg"},{"id":57883,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4247/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d5e3","contributors":{"authors":[{"text":"Parks, Bruce","contributorId":87542,"corporation":false,"usgs":true,"family":"Parks","given":"Bruce","email":"","affiliations":[],"preferred":false,"id":200799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Madison, R. J.","contributorId":84734,"corporation":false,"usgs":true,"family":"Madison","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":80302,"text":"fwsobs82_10_106 - 1985 - Habitat Suitability Index Models: Eastern wild turkey","interactions":[],"lastModifiedDate":"2022-02-09T15:00:51.29419","indexId":"fwsobs82_10_106","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.106","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Eastern wild turkey","docAbstract":"A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model for the eastern wild turkey (Meleagris gallopavo sylvestris). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum habitat). HSI models are designed to be used with Habitat Evaluation Procedures previously developed by the U.S. Fish and Wildlife Service.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Schroeder, R.L., 1985, Habitat Suitability Index Models: Eastern wild turkey: FWS/OBS 82/10.106, vi, 33 p.","productDescription":"vi, 33 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":194800,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6498bd","contributors":{"authors":[{"text":"Schroeder, Richard L.","contributorId":10368,"corporation":false,"usgs":true,"family":"Schroeder","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":292209,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4438,"text":"cir967 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1984","interactions":[{"subject":{"id":70180306,"text":"70180306 - 1985 - Summary of data on the age of the Orca Group, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1984</i>","indexId":"70180306","publicationYear":"1985","noYear":false,"title":"Summary of data on the age of the Orca Group, Alaska: A section in <i>The United States Geological Survey in Alaska: Accomplishments during 1984</i>"},"predicate":"IS_PART_OF","object":{"id":4438,"text":"cir967 - 1985 - The United States Geological Survey in Alaska: Accomplishments during 1984","indexId":"cir967","publicationYear":"1985","noYear":false,"title":"The United States Geological Survey in Alaska: Accomplishments during 1984"},"id":1}],"lastModifiedDate":"2024-11-13T22:25:29.788145","indexId":"cir967","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"967","title":"The United States Geological Survey in Alaska: Accomplishments during 1984","docAbstract":"This circular contains short reports about many of the geologic studies carried out in Alaska by the U.S. Geological Survey and cooperating agencies during 1984. The topics cover a wide range in scientific and economic interest.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Alexandria, VA","doi":"10.3133/cir967","usgsCitation":"1985, The United States Geological Survey in Alaska: Accomplishments during 1984: U.S. Geological Survey Circular 967, xi, 97 p., https://doi.org/10.3133/cir967.","productDescription":"xi, 97 p.","numberOfPages":"114","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":31541,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0967/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139534,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0967/report-thumb.jpg"},{"id":402351,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23811.htm","text":"Preliminary study of lode gold deposits, Seward Peninsula","linkFileType":{"id":5,"text":"html"}},{"id":463976,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23954.htm","text":"Ophiolitic ultramafic rocks of the Jade Mountains - Cosmos Hills area, southwestern Brooks Range","linkFileType":{"id":5,"text":"html"}},{"id":463977,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24017.htm","text":"Gravity lows may indicate Pleistocene deposits beneath glacial Lake Noatak","linkFileType":{"id":5,"text":"html"}},{"id":463978,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24029.htm","text":"Preliminary interpretation of factor analysis of geochemical data from the Healy quadrangle","linkFileType":{"id":5,"text":"html"}},{"id":463979,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24033.htm","text":"Summary of data on the age of the Orca Group, Alaska","linkFileType":{"id":5,"text":"html"}},{"id":463980,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24035.htm","text":"Late Quaternary glaciation of the Paulof Bay and Port Moller areas, Alaska","linkFileType":{"id":5,"text":"html"}},{"id":463981,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24038.htm","text":"New evidence for activity on the Talkeetna segment, Castle Mountain-Caribou fault system: the 1984 Sutton earthquake","linkFileType":{"id":5,"text":"html"}},{"id":463982,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24073.htm","text":"Fossiliferous Middle and(or) Upper Triassic rocks within the Coast plutonic-metamorphic complex southeast of Skagway","linkFileType":{"id":5,"text":"html"}},{"id":463983,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24084.htm","text":"Preliminary study of shear sense in mylonites, eastern Ray Mountains, Tanana quadrangle","linkFileType":{"id":5,"text":"html"}},{"id":463984,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24090.htm","text":"Summary of 1984 TACT geologic studies in the northern Chugach Mountains and southern Copper River basin","linkFileType":{"id":5,"text":"html"}},{"id":463985,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24099.htm","text":"Early Pennsylvanian conodonts from the Strelna Formation, Chitina Valley","linkFileType":{"id":5,"text":"html"}},{"id":463986,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24120.htm","text":"Reconnaissance hydrology and suspended sediment analysis, Turnagain Arm estuary, upper Cook 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,{"id":28910,"text":"wri834263 - 1985 - Calibration procedure for a daily flow model of small watersheds with snowmelt runoff in the Green River coal region of Colorado","interactions":[],"lastModifiedDate":"2023-01-06T20:34:32.885086","indexId":"wri834263","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"83-4263","title":"Calibration procedure for a daily flow model of small watersheds with snowmelt runoff in the Green River coal region of Colorado","docAbstract":"<p>A calibration procedure was developed for the U.S. Geological Survey 's Precipitation-Runoff Modeling System for watersheds in which snowmelt is the major contributor to runoff. The model uses daily values of air temperature and precipitation as input and the output is mean daily discharge. The procedure appears sufficient to calibrate both streamflow volume and the timing of mean daily discharge if other model parameters are reasonably estimated. Model structure and sensitivity analysis suggest that one of the most important parameters is the available water-holding capacity of the soil (SMAX). Changing this parameter through a series of iterations, the calibration procedure minimizes the error between observed and predicted annual discharge. The calibration suggests that the single parameter SMAX may be sufficient for optimizing both the volumes and the timing of runoff, assuming other model parameters are adequately estimated. Additional optimization on parameters sensitive to timing does not appear to improve prediction. This indicates that these parameters were estimated accurately prior to calibration. Further investigation is needed on more watersheds to determine SMAX 's ability to calibrate volume and timing with a constant set of other model parameter values.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834263","usgsCitation":"Norris, J.M., and Parker, R.S., 1985, Calibration procedure for a daily flow model of small watersheds with snowmelt runoff in the Green River coal region of Colorado: U.S. Geological Survey Water-Resources Investigations Report 83-4263, iv, 32 p., https://doi.org/10.3133/wri834263.","productDescription":"iv, 32 p.","costCenters":[],"links":[{"id":411518,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35891.htm","linkFileType":{"id":5,"text":"html"}},{"id":57780,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4263/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124055,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4263/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Green River coal region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.433,\n              40.683\n            ],\n            [\n              -107.433,\n              40.183\n            ],\n            [\n              -106.75,\n              40.183\n            ],\n            [\n              -106.75,\n              40.683\n            ],\n            [\n              -107.433,\n              40.683\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e703c","contributors":{"authors":[{"text":"Norris, J. M.","contributorId":87953,"corporation":false,"usgs":true,"family":"Norris","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, R. S.","contributorId":104510,"corporation":false,"usgs":true,"family":"Parker","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":200604,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67481,"text":"i1310C - 1985 - Geologic map of the Silver City 1 degree by 2 degrees Quadrangle, New Mexico and Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"i1310C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1310","subseriesTitle":"NONE","chapter":"C","title":"Geologic map of the Silver City 1 degree by 2 degrees Quadrangle, New Mexico and Arizona","language":"ENGLISH","doi":"10.3133/i1310C","usgsCitation":"Drewes, H., Houser, B.B., Hedlund, D.C., Richter, D., Thorman, C., and Finell, T., 1985, Geologic map of the Silver City 1 degree by 2 degrees Quadrangle, New Mexico and Arizona: U.S. Geological Survey IMAP 1310, 1 map :col ;45 x 75 cm., on sheet 83 x 129 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1310C.","productDescription":"1 map :col ;45 x 75 cm., on sheet 83 x 129 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106687,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9132.htm","linkFileType":{"id":5,"text":"html"},"description":"9132"},{"id":187848,"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\": [ [ [ -110,32 ], [ -110,33 ], [ -108,33 ], [ -108,32 ], [ -110,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a7d1","contributors":{"authors":[{"text":"Drewes, Harald","contributorId":52567,"corporation":false,"usgs":true,"family":"Drewes","given":"Harald","affiliations":[],"preferred":false,"id":276327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Houser, B. B.","contributorId":46092,"corporation":false,"usgs":true,"family":"Houser","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":276326,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hedlund, D. C.","contributorId":101624,"corporation":false,"usgs":true,"family":"Hedlund","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":276330,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Richter, D.H.","contributorId":43325,"corporation":false,"usgs":true,"family":"Richter","given":"D.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":276325,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thorman, C.H.","contributorId":67524,"corporation":false,"usgs":true,"family":"Thorman","given":"C.H.","affiliations":[],"preferred":false,"id":276328,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Finell, T.L.","contributorId":100481,"corporation":false,"usgs":true,"family":"Finell","given":"T.L.","email":"","affiliations":[],"preferred":false,"id":276329,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":80295,"text":"fwsobs82_10_109 - 1985 - Habitat Suitability Index Models and Instream Flow Suitability Curves: Pink salmon","interactions":[],"lastModifiedDate":"2022-02-09T15:01:28.098049","indexId":"fwsobs82_10_109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.109","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models and Instream Flow Suitability Curves: Pink salmon","docAbstract":"A review and synthesis of existing information were used to develop a Habitat Suitability Index (HSI) model and instream flow suitability curves for the pink salmon (Oncorhynchus gorbuscha). The model consolidates habitat use information into a framework appropriate for field application, and is scaled to produce an index between 0.0 (unsuitable habitat) to 1.0 (optimum habitat). HSI models are designed to be used with Habitat Evaluation Procedures previously developed by the U.S. Fish and Wildlife Service.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Raleigh, R.F., and Nelson, P.C., 1985, Habitat Suitability Index Models and Instream Flow Suitability Curves: Pink salmon: FWS/OBS 82/10.109, vi, 36 p.","productDescription":"vi, 36 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649e46","contributors":{"authors":[{"text":"Raleigh, Robert F.","contributorId":49841,"corporation":false,"usgs":true,"family":"Raleigh","given":"Robert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":292199,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, Patrick C.","contributorId":68799,"corporation":false,"usgs":true,"family":"Nelson","given":"Patrick","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":292200,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15952,"text":"ofr85732 - 1985 - Assessment of undiscovered phosphate resource potential of the Dominican Republic","interactions":[],"lastModifiedDate":"2012-02-02T00:07:11","indexId":"ofr85732","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-732","title":"Assessment of undiscovered phosphate resource potential of the Dominican Republic","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85732","usgsCitation":"Sheldon, R., and McDowell, R., 1985, Assessment of undiscovered phosphate resource potential of the Dominican Republic: U.S. Geological Survey Open-File Report 85-732, ii, 65 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85732.","productDescription":"ii, 65 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149521,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0732/report-thumb.jpg"},{"id":44912,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0732/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab2e4b07f02db66f363","contributors":{"authors":[{"text":"Sheldon, R.P.","contributorId":71158,"corporation":false,"usgs":true,"family":"Sheldon","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":172002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDowell, R. C.","contributorId":30206,"corporation":false,"usgs":true,"family":"McDowell","given":"R. C.","affiliations":[],"preferred":false,"id":172001,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28269,"text":"wri844172 - 1985 - Water quality of the North Platte River, east-central Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri844172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4172","title":"Water quality of the North Platte River, east-central Wyoming","docAbstract":"This report is a statistical summary of 40 different constituents and physical characteristics that describe the water quality of the North Platter River between Alcova Dam and Orin, Wyoming, a distance of 143 river miles. Data from seven stations are summarized for 1970-79. Water entering the North Platte River upstream from Casper generally is more mineralized and degraded than the water in the North Platte River or in the tributaries entering the river downstream from Casper. The average dissolved solids concentration was about 320 mg/L at the upper sampling station and about 430 mg/L just downstream from Casper. This increase is typical of many other constituents. The mean fecal-coliform concentration at the upper station was about 8 colonies/ml and about 4,000 colonies/100 ml at the station downstream from Casper. Concentrations of some constituents periodically were greater than maximum recommended for drinking water supplies. About 24% of the dissolved solids concentrations were more than 500 mg/L. Some selenium concentrations exceeded the limit of 10 micrograms/L mandated for public water supplies. Large concentrations of copper, zinc, and ammonia indicate that these constituents might be a problem for sensitive aquatic life. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844172","usgsCitation":"Larson, L.R., 1985, Water quality of the North Platte River, east-central Wyoming: U.S. Geological Survey Water-Resources Investigations Report 84-4172, vii, 85 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844172.","productDescription":"vii, 85 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":159601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4172/report-thumb.jpg"},{"id":57091,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4172/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9878","contributors":{"authors":[{"text":"Larson, L. R.","contributorId":41421,"corporation":false,"usgs":true,"family":"Larson","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199501,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28169,"text":"wri844302 - 1985 - Documentation of a numerical code for the simulation of variable density ground-water flow in three dimensions","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri844302","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4302","title":"Documentation of a numerical code for the simulation of variable density ground-water flow in three dimensions","docAbstract":"A numerical code is documented for the simulation of variable density time dependent groundwater flow in three dimensions. The groundwater density, although variable with distance, is assumed to be constant in time. The Integrated Finite Difference grid elements in the code follow the geologic strata in the modeled area. If appropriate, the determination of hydraulic head in confining beds can be deleted to decrease computation time. The strongly implicit procedure (SIP), successive over-relaxation (SOR), and eight different preconditioned conjugate gradient (PCG) methods are used to solve the approximating equations. The use of the computer program that performs the calculations in the numerical code is emphasized. Detailed instructions are given for using the computer program, including input data formats. An example simulation and the Fortran listing of the program are included. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844302","usgsCitation":"Kuiper, L., 1985, Documentation of a numerical code for the simulation of variable density ground-water flow in three dimensions: U.S. Geological Survey Water-Resources Investigations Report 84-4302, 90 p. :ill. ;28 cm., https://doi.org/10.3133/wri844302.","productDescription":"90 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":121578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4302/report-thumb.jpg"},{"id":57003,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4302/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db63628c","contributors":{"authors":[{"text":"Kuiper, L.K.","contributorId":34557,"corporation":false,"usgs":true,"family":"Kuiper","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":199327,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28724,"text":"wri844237 - 1985 - Occurrence of natural radium-226 radioactivity in ground water of Sarasota County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri844237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4237","title":"Occurrence of natural radium-226 radioactivity in ground water of Sarasota County, Florida","docAbstract":"Water that contains radium-226 radioactivity in excess of the 5.0-picocurie-per-liter limit set in the National Interim Primary Drinking Water Regulations was found in the majority of wells sampled throughout Sarasota County. Highest levels were found areally near the coast or near rivers and vertically in the Tamiami-upper Hawthorn aquifer where semiconsolidated phosphate pebbles occur. Analysis of data suggests that part of the radium-226 in ground water of Sarasota County is dissolved by alpha particle recoil. In slightly mineralized water, radium-226 concentrations are decreased by ion exchange or sorption. In more mineralized water, other ions compete with radium-226 for ion exchange or sorption sites. Dissolution of minerals containing radium-226 by mineralized water probably contributes a significant fraction of the dissolved radium-226. Two types of mineralized water were present in Sarasota County. One type is a marine-like water, presumably associated with saltwater encroachment in coastal areas; the other is a calcium magnesium strontium surfate bicarbonate type. In general, water that contains high radium-226 radioactivities also contains too much water hardness or dissolved solids to be used for public supply without treatment that would also reduce radium-226 radioactivities. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844237","usgsCitation":"Miller, R.L., and Sutcliffe, H., 1985, Occurrence of natural radium-226 radioactivity in ground water of Sarasota County, Florida: U.S. Geological Survey Water-Resources Investigations Report 84-4237, vi, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844237.","productDescription":"vi, 34 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118905,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4237/report-thumb.jpg"},{"id":57553,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4237/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1e5d","contributors":{"authors":[{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":200294,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sutcliffe, Horace","contributorId":28598,"corporation":false,"usgs":true,"family":"Sutcliffe","given":"Horace","affiliations":[],"preferred":false,"id":200293,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28155,"text":"wri854288_1985 - 1985 - Hydrogeology of the southwestern part of the Town of Hempstead, Nassau County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri854288_1985","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4288","title":"Hydrogeology of the southwestern part of the Town of Hempstead, Nassau County, New York","docAbstract":"The groundwater resources of the southwestern part of the Town of Hempstead in Nassau County, NY were investigated in 1984. The area studied encompasses 85 sq mi, or 68% of the town 's 125-sq mi area. The groundwater reservoir underlying the area consists of unconsolidated gravel, sand, silt, and clay of Holocene, Pleistocene, and Late Cretaceous age that have been divided into eight geologic units. The maximum total thickness of the unconsolidated deposits is about 1,500 ft. Precipitation is the sole source of groundwater recharge in the area. The average annual precipitation, as recorded at Valley Stream during 1927-83, was 42.62 in. The water table altitude in the 1980 's has recovered and equalled or exceeded that before the regional drought of 1962-66. The potentiometric surfaces in the Magothy and Lloyd aquifers are still somewhat below those before the drought but are recovering throughout most of the area. The report presents 10 maps showing the surface altitude of the geologic units as well as the potentiometric altitudes of the three major aquifers. Also included are six geologic sections, four hydrographs, and several graphs presenting the data that was collected. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854288_1985","usgsCitation":"Krulikas, R., 1985, Hydrogeology of the southwestern part of the Town of Hempstead, Nassau County, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4288, iv, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854288_1985.","productDescription":"iv, 20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_85_4288.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614b49","contributors":{"authors":[{"text":"Krulikas, R.K.","contributorId":81102,"corporation":false,"usgs":true,"family":"Krulikas","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":199310,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28869,"text":"wri844293 - 1985 - Water-surface elevations for the high tide of December 15, 1977, in the Puget Sound region, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri844293","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4293","title":"Water-surface elevations for the high tide of December 15, 1977, in the Puget Sound region, Washington","docAbstract":"An unusually high oceanic tide on December 15, 1977, caused flooding of lowlying, nearshore parts of western Washington, including several areas in the Puget Sound region. At Seattle, the December 15 high tide of 14.8 feet above MLLW (mean lower low water datum; 8.55 feet above the National Geodetic Vertical Daltum of 1929, or NGVD) was 0.1 foot higher than the 100-year high tide. At Neah Bay, near the western end of the Straits of Juan de Fuca, however, the high tide of 8.77 feet MLLW (4.55 feet NGVD) on that date was 3.2 feet lower than the 100-year high tide. This study has identified the observed December 15 high-tide elevations at many locations in the Puget Sound region. The observed high tide then was much higher than predicted in most of the Puget Sound region, primarily as the result of a very low barametric pressure. Little damage from wind waves was reported. Elevation profiles for the predicted and observed high tides on December 15 and for several other selected tide levels indicate an increase in the maximum height in the inland direction, except near Port Angeles, and show abrupt changes in tidal elevations at three constrictions - Admiralty Inlet, Tacoma Narrows, and Deception Pass. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844293","usgsCitation":"Nelson, L.M., 1985, Water-surface elevations for the high tide of December 15, 1977, in the Puget Sound region, Washington: U.S. Geological Survey Water-Resources Investigations Report 84-4293, iii, 15 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844293.","productDescription":"iii, 15 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123887,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4293/report-thumb.jpg"},{"id":57747,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4293/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9a00","contributors":{"authors":[{"text":"Nelson, L. M.","contributorId":39773,"corporation":false,"usgs":true,"family":"Nelson","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":200530,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30251,"text":"wri854064 - 1985 - Ground-water contamination in East Bay Township, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T10:15:47","indexId":"wri854064","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4064","title":"Ground-water contamination in East Bay Township, Michigan","docAbstract":"<p>Glacial deposits, as much as 360 feet thick, underlie the study area. The upper 29 to 118 feet, a sand and gravel unit, is the aquifer tapped for water by all wells in the area. This unit is underlain by impermeable clay that is at least 100 feet thick. </p><p>Ground-water flow is northeastward at an estimated rate of 3 to 6 feet per day. Hydraulic conductivities in the aquifer range from 85 to 150 feet per day; 120 feet per day provided the best match of field data in a ground-water flow model. The depth to water ranged from 1 to 20 feet. </p><p>Chemical anlayses indicate that ground water is contaminated with organic chemicals from near the Hangar/Administration building at the U.S. Coast Guard Air Station to East Bay, about 4,300 feet northeast. The plume, which follows ground-water flow lines, ranges from 180 to 400 feet wide. In the upper reach of the plume, hydrocarbons less dense than water occur at the surface of the water table; they move downward in the aquifer as they move toward East Bay. Maximum concentrations of the major organic compounds include: benzene, 3,390 micrograms per liter; toluene, 55,500 micrograms per liter; xylene, 3,900 micrograms per liter; tetrachloroethylene, 3,410 micrograms per liter; and bis (2-ethyl hexyl) phthalate, 2,100 micrograms per liter. Soils are generally free of these hydrocarbons; however, in the vicinity of past drum storage, aircraft maintenance operations, and fuel storage and dispensing, as much as 1,100 micrograms per kilogram of tetrachloroethylene and 1,500 micrograms per kilogram of bis (2-ethyl hexyl) phthalate were detected. At a few locations higher molecular weight hydrocarbons, characteristic of petroleum distillates, were found.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri854064","collaboration":"Prepared in cooperation with the U.S. Coast Guard","usgsCitation":"Twenter, F.R., Cummings, T., and Grannemann, N., 1985, Ground-water contamination in East Bay Township, Michigan: U.S. Geological Survey Water-Resources Investigations Report 85-4064, Document: ix, 63 p.; 5 Plates: 23.24 x 35.59 inches or smaller, https://doi.org/10.3133/wri854064.","productDescription":"Document: ix, 63 p.; 5 Plates: 23.24 x 35.59 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":59038,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59039,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123443,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4064/report-thumb.jpg"},{"id":59040,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59041,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59042,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4064/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59043,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4064/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","otherGeospatial":"East Bay Township","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.57439804077148,\n              44.74164292754147\n            ],\n            [\n              -85.56602954864502,\n              44.75276788055599\n            ],\n            [\n              -85.5673599243164,\n              44.7531640722716\n            ],\n            [\n              -85.56911945343018,\n              44.753986923310066\n            ],\n            [\n              -85.57062149047852,\n              44.75490118850054\n            ],\n            [\n              -85.57225227355957,\n              44.75599828763615\n            ],\n            [\n              -85.57353973388672,\n              44.75706489182693\n            ],\n            [\n              -85.57529926300047,\n              44.7584971579133\n            ],\n            [\n              -85.57585716247559,\n              44.7592894600709\n            ],\n            [\n              -85.57611465454102,\n              44.760234113828844\n            ],\n            [\n              -85.58675765991211,\n              44.746885637908065\n            ],\n            [\n              -85.57439804077148,\n              44.74164292754147\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699997","contributors":{"authors":[{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202934,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. R.","contributorId":104082,"corporation":false,"usgs":true,"family":"Cummings","given":"T. R.","affiliations":[],"preferred":false,"id":202935,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grannemann, N.G.","contributorId":11221,"corporation":false,"usgs":true,"family":"Grannemann","given":"N.G.","affiliations":[],"preferred":false,"id":202933,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30179,"text":"wri844113 - 1985 - Simulation of ground-water flow in the water-table aquifer near Barceloneta, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri844113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4113","title":"Simulation of ground-water flow in the water-table aquifer near Barceloneta, Puerto Rico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844113","usgsCitation":"Torres-Gonzalez, A., 1985, Simulation of ground-water flow in the water-table aquifer near Barceloneta, Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 84-4113, v, 39 p. :maps ;28 cm., https://doi.org/10.3133/wri844113.","productDescription":"v, 39 p. :maps ;28 cm.","costCenters":[],"links":[{"id":159486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4113/report-thumb.jpg"},{"id":58977,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4113/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f261c","contributors":{"authors":[{"text":"Torres-Gonzalez, Arturo","contributorId":70769,"corporation":false,"usgs":true,"family":"Torres-Gonzalez","given":"Arturo","email":"","affiliations":[],"preferred":false,"id":202814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67127,"text":"i1527 - 1985 - Geologic map of Archean rocks, western Vermilion District, northern Minnesota","interactions":[],"lastModifiedDate":"2012-02-10T00:11:20","indexId":"i1527","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1527","subseriesTitle":"NONE","title":"Geologic map of Archean rocks, western Vermilion District, northern Minnesota","language":"ENGLISH","doi":"10.3133/i1527","usgsCitation":"Sims, P., and Southwick, D.L., 1985, Geologic map of Archean rocks, western Vermilion District, northern Minnesota: U.S. Geological Survey IMAP 1527, 1 map :col. ;87 x 117 cm., on sheet 101 x 147 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1527.","productDescription":"1 map :col. ;87 x 117 cm., on sheet 101 x 147 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106790,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9294.htm","linkFileType":{"id":5,"text":"html"},"description":"9294"},{"id":187786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.61749999999999,47.6175 ], [ -92.61749999999999,48 ], [ -91.86749999999999,48 ], [ -91.86749999999999,47.6175 ], [ -92.61749999999999,47.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a32ae","contributors":{"authors":[{"text":"Sims, P.K.","contributorId":30191,"corporation":false,"usgs":true,"family":"Sims","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":275641,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Southwick, D. L.","contributorId":57130,"corporation":false,"usgs":true,"family":"Southwick","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":275642,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26417,"text":"wri854014 - 1985 - Hydrologic description of the Tamarack Wildlife area and vicinity, Logan County, Colorado, and simulated effects of possible water-management activities","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri854014","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4014","title":"Hydrologic description of the Tamarack Wildlife area and vicinity, Logan County, Colorado, and simulated effects of possible water-management activities","docAbstract":"The stream-aquifer system of the Tamarack Wildlife Area and vicinity in Logan County, Colorado, is described using analyses of water level, water temperature, and specific conductance data. Correlation analysis indicated that water levels in the flood plain relate better to those in the river than those in the upgradient valley meadow. Water table surfaces showed that water moves parallel to the river with a small gradient toward the river. Water temperature data for the river had a large annual fluctuation. The temperature of well water from 0 feet below land surface had no fluctuation. The temperature of sloughs and shallow groundwater had intermediate fluctuations. Specific conductance data ranged from 264 microsiemens/cm at 25 C in sandhill wells to 1,540 microsiemens in the river. A groundwater flow model and simplified slough-temperature model showed that additional groundwater pumpage or lower river stage caused by upstream diversions would decrease groundwater inflow to the slough, with a corresponding water temperature decrease. A simulated artificial recharge project would increase groundwater inflow to the slough and increase water temperature in the slough. The simulation of a plan to pump groundwater to create wildlife-habitat ponds indicated that this would cause stream depletions each month, except during the nonpumping period, June through August. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854014","usgsCitation":"Burns, A., 1985, Hydrologic description of the Tamarack Wildlife area and vicinity, Logan County, Colorado, and simulated effects of possible water-management activities: U.S. Geological Survey Water-Resources Investigations Report 85-4014, v, 42 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854014.","productDescription":"v, 42 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4014/report-thumb.jpg"},{"id":55211,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4014/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55212,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4014/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607059","contributors":{"authors":[{"text":"Burns, A.W.","contributorId":65498,"corporation":false,"usgs":true,"family":"Burns","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":196350,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30279,"text":"wri844307 - 1985 - Preliminary assessment of the ground-water resources of the alluvial aquifer, White River valley, Rio Blanco County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri844307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4307","title":"Preliminary assessment of the ground-water resources of the alluvial aquifer, White River valley, Rio Blanco County, Colorado","docAbstract":"A preliminary study of the alluvial aquifer in the White River Valley was conducted to assess aquifer extent and the occurrence , availability, and chemical quality of water in the aquifer. The aquifer in the study area underlies 35 square miles. Aquifer width ranges from 0.1 to 1.5 miles and averages 0.5 miles. Saturated thickness ranges from zero to more than 140 feet and averages 22 feet. The aquifer is unconfined except west of the Grand Hogback, where artesian conditions were observed at several locations. Well yields usually are less than 25 gallons per minute. At the Meeker municipal well field in Agency Park, wells reportedly could yield more than 1,000 gallons per minute each. Based on nine aquifer tests, transmissivity ranges from 860 to 93,000 feet squared per day, and hydraulic conductivity ranges from 70 to 1,550 feet per day. The estimated total volume of water in storage in the aquifer in the study area is 103,000 acre-feet. Groundwater type in the eastern part of the study area is calcium bicarbonate; to the west, water type is sodium sulfate. Water in the aquifer is classified as very hard throughout the study area. Specific conductance generally increases from east to west. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri844307","usgsCitation":"Van Liew, W.P., and Gesink, M., 1985, Preliminary assessment of the ground-water resources of the alluvial aquifer, White River valley, Rio Blanco County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 84-4307, vii, 82 p. :ill., maps (some col.) ;28 cm., https://doi.org/10.3133/wri844307.","productDescription":"vii, 82 p. :ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":159340,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4307/report-thumb.jpg"},{"id":59063,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4307/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59064,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4307/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59065,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4307/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59066,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4307/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59067,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4307/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59068,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4307/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4870","contributors":{"authors":[{"text":"Van Liew, W. P.","contributorId":78370,"corporation":false,"usgs":true,"family":"Van Liew","given":"W.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":202976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gesink, M.L.","contributorId":6489,"corporation":false,"usgs":true,"family":"Gesink","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":202975,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57551,"text":"wdrCA834 - 1985 - Water Resources Data for California, Water Year 1983, Volume 4. Northern California Valley Basins and the Great Basin from Honey Lake Basin to Oregon State Line","interactions":[],"lastModifiedDate":"2012-06-20T01:01:36","indexId":"wdrCA834","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-83-4","title":"Water Resources Data for California, Water Year 1983, Volume 4. Northern California Valley Basins and the Great Basin from Honey Lake Basin to Oregon State Line","docAbstract":"Water-resources data for the 1983 water year for California consists of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 4 contains discharge records for 153 gaging stations; stage and contents for 25 lakes and reservoirs; precipitation data for 2 stations; water quality for 7 stations; and water levels for 147 observation wells. Also included is one low-flow partial-record station. Additional water data are collected at various sites, not part of the systematic data collection program, and are published as special investigations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA834","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies","usgsCitation":"Fogelman, R.P., Mullen, J., Shelton, W., Simpson, R., and Grillo, D., 1985, Water Resources Data for California, Water Year 1983, Volume 4. Northern California Valley Basins and the Great Basin from Honey Lake Basin to Oregon State Line (Legacy Reports): U.S. Geological Survey Water Data Report CA-83-4, xiii, 361 p., https://doi.org/10.3133/wdrCA834.","productDescription":"xiii, 361 p.","temporalStart":"1982-10-01","temporalEnd":"1983-09-30","costCenters":[{"id":631,"text":"Water Resources Division-California District","active":false,"usgs":true}],"links":[{"id":257684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_83_4.jpg"},{"id":182015,"rank":0,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/ca-83/WDR-1983-vol4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Northern California Valley Basins;Great Basin;Honey Lake Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.4,32.5 ], [ -124.4,42 ], [ -114.13333333333334,42 ], [ -114.13333333333334,32.5 ], [ -124.4,32.5 ] ] ] } } ] }","edition":"Legacy Reports","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b012","contributors":{"authors":[{"text":"Fogelman, R. P.","contributorId":96688,"corporation":false,"usgs":true,"family":"Fogelman","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":257322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullen, J.R.","contributorId":92683,"corporation":false,"usgs":true,"family":"Mullen","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":257321,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shelton, W.F.","contributorId":48241,"corporation":false,"usgs":true,"family":"Shelton","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":257320,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Simpson, R.G.","contributorId":16016,"corporation":false,"usgs":true,"family":"Simpson","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":257318,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Grillo, D.A.","contributorId":45727,"corporation":false,"usgs":true,"family":"Grillo","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":257319,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":57552,"text":"wdrCA842 - 1985 - Water Resources Data for California, Water Year 1984; Volume 2. Pacific Slope Basins from Arroyo Grande to Oregon State Line except Central Valley","interactions":[],"lastModifiedDate":"2012-06-21T01:01:41","indexId":"wdrCA842","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-84-2","title":"Water Resources Data for California, Water Year 1984; Volume 2. Pacific Slope Basins from Arroyo Grande to Oregon State Line except Central Valley","docAbstract":"Water resources data for the 1984 water year for California consists of records of stage, discharge, and water quality of streams; stage and contents in lakes and reservoirs; and water levels and water quality in wells. Volume 2 contains discharge records for 132 gaging stations; stage and contents for 18 lakes and reservoirs; water quality for 11 stations; water levels for 9 observation wells. Also included are 2 low-flow partial-record stations and 19 water-quality partial-record stations. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA842","collaboration":"Prepared in cooperation with the California Department of Water Resources and with other agencies","usgsCitation":"Anderson, S., Markham, K., Piro, V., Shelton, W., and Grillo, D., 1985, Water Resources Data for California, Water Year 1984; Volume 2. Pacific Slope Basins from Arroyo Grande to Oregon State Line except Central Valley (Legacy Report): U.S. Geological Survey Water Data Report CA-84-2, xi, 315 p., https://doi.org/10.3133/wdrCA842.","productDescription":"xi, 315 p.","temporalStart":"1983-10-01","temporalEnd":"1984-09-30","costCenters":[{"id":631,"text":"Water Resources Division-California District","active":false,"usgs":true}],"links":[{"id":257724,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_84_2.jpg"},{"id":182016,"rank":0,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/ca-84/WDR-1984-vol2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Pacific Slope Basins;Arroyo Grande","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.4,32.5 ], [ -124.4,42 ], [ -114.13333333333334,42 ], [ -114.13333333333334,32.5 ], [ -124.4,32.5 ] ] ] } } ] }","edition":"Legacy Report","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd162","contributors":{"authors":[{"text":"Anderson, S.","contributorId":45779,"corporation":false,"usgs":true,"family":"Anderson","given":"S.","affiliations":[],"preferred":false,"id":257325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Markham, K.L.","contributorId":14041,"corporation":false,"usgs":true,"family":"Markham","given":"K.L.","email":"","affiliations":[],"preferred":false,"id":257323,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Piro, V.","contributorId":53883,"corporation":false,"usgs":true,"family":"Piro","given":"V.","email":"","affiliations":[],"preferred":false,"id":257327,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shelton, W.F.","contributorId":48241,"corporation":false,"usgs":true,"family":"Shelton","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":257326,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Grillo, D.A.","contributorId":45727,"corporation":false,"usgs":true,"family":"Grillo","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":257324,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":29918,"text":"wri854085 - 1985 - Hydraulic and sediment characteristics at the North Channel Bridge, Jamaica Bay, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:09:03","indexId":"wri854085","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4085","title":"Hydraulic and sediment characteristics at the North Channel Bridge, Jamaica Bay, New York","docAbstract":"Data were collected during the spring of 1984 in the vicinity of North Channel Bridge in Jamaica Bay, New York to define the hydraulic regime and the physical characteristics and chemical quality of bottom sediments. The data were used in a semiquantitative analysis to predict the effects of bridge replacement and the attendant resuspension of bottom sediments, on the hydraulics and quality of water and bottom sediments. The bay-bottom configuration at the bridge site was defined, and continuous tidal stage and tidal velocity data were collected for about a month. In addition, eight bottom-sediment samples were collected near the bridge and analyzed. Results of the hydraulic analysis show that the proposed bridge should not have any measurable effect on the net water transport at the bridge cross section. The sediment data indicate that bottom sediments are relatively unpolluted in the vicinity of the bridge. Seventy-five percent of the resuspended bottom sediments will probably settle within 186 m of the bridge during an average ebb tide. Metals and nutrients released from the sediments to the water column are expected to be diluted far below detection limits. The extra oxygen demand exerted by the resuspended bottom sediments is also expected to be far less than ambient biochemical oxygen demand of the water column. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854085","usgsCitation":"Staubitz, W., and Wolcott, S., 1985, Hydraulic and sediment characteristics at the North Channel Bridge, Jamaica Bay, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4085, vi, 49 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854085.","productDescription":"vi, 49 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123495,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4085/report-thumb.jpg"},{"id":58735,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4085/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698a1c","contributors":{"authors":[{"text":"Staubitz, W. W.","contributorId":73209,"corporation":false,"usgs":true,"family":"Staubitz","given":"W. W.","affiliations":[],"preferred":false,"id":202358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolcott, S.W.","contributorId":14453,"corporation":false,"usgs":true,"family":"Wolcott","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":202357,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43759,"text":"ofr8567 - 1985 - Land use and land cover and associated maps for Eagle Pass, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"ofr8567","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-67","title":"Land use and land cover and associated maps for Eagle Pass, Texas","language":"ENGLISH","doi":"10.3133/ofr8567","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Land use and land cover and associated maps for Eagle Pass, Texas: U.S. Geological Survey Open-File Report 85-67, maps :photocopy ;45 x 65 cm., on sheet 76 x 107 cm., https://doi.org/10.3133/ofr8567.","productDescription":"maps :photocopy ;45 x 65 cm., on sheet 76 x 107 cm.","costCenters":[],"links":[{"id":161821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b14ab","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":531347,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44094,"text":"ofr85444 - 1985 - Surficial geologic map of the Palen-McCoy Wilderness Study area, Riverside County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:12","indexId":"ofr85444","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-444","title":"Surficial geologic map of the Palen-McCoy Wilderness Study area, Riverside County, California","language":"ENGLISH","doi":"10.3133/ofr85444","usgsCitation":"Yeend, W.E., 1985, Surficial geologic map of the Palen-McCoy Wilderness Study area, Riverside County, California: U.S. Geological Survey Open-File Report 85-444, 1 map :photocopy ;43 x 35 cm., on sheet 77 x 52 cm., https://doi.org/10.3133/ofr85444.","productDescription":"1 map :photocopy ;43 x 35 cm., on sheet 77 x 52 cm.","costCenters":[],"links":[{"id":161827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81485,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0444/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688e79","contributors":{"authors":[{"text":"Yeend, Warren E.","contributorId":65053,"corporation":false,"usgs":true,"family":"Yeend","given":"Warren","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}