{"pageNumber":"2052","pageRowStart":"51275","pageSize":"25","recordCount":68919,"records":[{"id":27879,"text":"wri844050 - 1984 - An evaluation of rainfall-runoff data for the Denver Federal Center, Lakewood, Jefferson County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri844050","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4050","title":"An evaluation of rainfall-runoff data for the Denver Federal Center, Lakewood, Jefferson County, Colorado","docAbstract":"An investigation was made to monitor the storm runoff in McIntyre Gulch basin to determine the rainfall-runoff chracteristics. Results may now be used to evaluate the effects of future development on storm runoff from the Denver Federal Center, which is located in the McIntyre Gulch basin in Lakewood , CO. Rainfall and runoff data were collected at eight streamflow stations and three auxiliary rainfall stations in and adjacent to the Denver Federal Center. The outflow peak discharges from McIntyre Gulch in the Denver Federal Center were higher than the inflow peak discharges for eight of the storms by an average of 38 percent. Outflow peak discharges for eight of the storms were lower by an average of 12 percent. The study demonstrated that runoff varies with location of a storm--even for a relatively small basin. Peak discharges of McIntyre Gulch outflow from the Denver Federal Center were 27 percent greater than the inflow for all storms, but only 15 percent greater for evenly distributed storms. Runoff from the Denver Federal Center increased storm-runoff volumes in McIntyre Gulch by an average of 46 percent. Proper management of storm runoff in the Denver Federal Center requires that proposed improvements to the existing storm-runoff system maintain peak flows at their present levels. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844050","usgsCitation":"Jarrett, R., and Veenhuis, J., 1984, An evaluation of rainfall-runoff data for the Denver Federal Center, Lakewood, Jefferson County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 84-4050, v, 29 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844050.","productDescription":"v, 29 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122689,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4050/report-thumb.jpg"},{"id":56702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4050/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684964","contributors":{"authors":[{"text":"Jarrett, R.D.","contributorId":36551,"corporation":false,"usgs":true,"family":"Jarrett","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":198835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Veenhuis, J.E.","contributorId":6850,"corporation":false,"usgs":true,"family":"Veenhuis","given":"J.E.","affiliations":[],"preferred":false,"id":198834,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27874,"text":"wri844203 - 1984 - Time of travel and dispersion in the Jones Falls, Baltimore, Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri844203","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4203","title":"Time of travel and dispersion in the Jones Falls, Baltimore, Maryland","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844203","usgsCitation":"James, R., and Helinsky, B., 1984, Time of travel and dispersion in the Jones Falls, Baltimore, Maryland: U.S. Geological Survey Water-Resources Investigations Report 84-4203, v, 29 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844203.","productDescription":"v, 29 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4203/report-thumb.jpg"},{"id":56698,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4203/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b778","contributors":{"authors":[{"text":"James, R.W.","contributorId":70434,"corporation":false,"usgs":true,"family":"James","given":"R.W.","affiliations":[],"preferred":false,"id":198825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Helinsky, B.M.","contributorId":82344,"corporation":false,"usgs":true,"family":"Helinsky","given":"B.M.","affiliations":[],"preferred":false,"id":198826,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27871,"text":"wri844201 - 1984 - Hydrogeology of eastern Michaud Flats, Fort Hall Indian Reservation, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri844201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4201","title":"Hydrogeology of eastern Michaud Flats, Fort Hall Indian Reservation, Idaho","docAbstract":"Groundwater in Michaud Flats, southeastern Idaho, is developed extensively for irrigation and industry. Extensive clay beds overlie the Bighole Basalt and Sunbeam Formation, which yield most of the water for irrigation and industrial wells; artesian aquifers in these rock units have heads below land surface and near those in the shallow water-table aquifer in the overlying Michaud Gravel. Transmissivities in artesian aquifers range from 19,6000 to 444,000 feet squared per day. High levels of arsenic were detected in groundwater in the Flats in 1972. During 1982, concentrations of arsenic twice exceeded the recommended drinking water limit of 50 micrograms per liter. Concentrations of other chemical constituents were generally within drinking water limits. Stable-isotope data suggest more than one source of aquifer recharge and indicate some mixing between waters from industrial ponds and local groundwater. Management alternatives are being implemented by two industries for control of groundwater contamination. These include reduction of effluent, installation of liners and leachate recovery systems in ponds, and removal and reclamation of precipitates in old slurry and evaporation ponds. Six sites will be monitored through 1985 to determine changes in groundwater chemistry and migration of contaminants. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri844201","usgsCitation":"Jacobson, N., 1984, Hydrogeology of eastern Michaud Flats, Fort Hall Indian Reservation, Idaho: U.S. Geological Survey Water-Resources Investigations Report 84-4201, iv, 31 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844201.","productDescription":"iv, 31 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4201/report-thumb.jpg"},{"id":56695,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4201/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624698","contributors":{"authors":[{"text":"Jacobson, N.D.","contributorId":105302,"corporation":false,"usgs":true,"family":"Jacobson","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":198820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27865,"text":"wri844041 - 1984 - Low-flow transport models for conservative and sorbed solutes — Uvas Creek, near Morgan Hill, California","interactions":[],"lastModifiedDate":"2022-01-20T21:02:14.126583","indexId":"wri844041","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4041","title":"Low-flow transport models for conservative and sorbed solutes — Uvas Creek, near Morgan Hill, California","docAbstract":"<p>Models describing low-flow transport of conservative (nonreactive) and reactive solutes, which adsorb on the streambed, are developed and tested. Temporary storage within the bed plays an important role in solute movement. Three different models of bed-storage processes are developed for conservative solutes. One model assumes the bed is a well-mixed, nondiffusing, nonreacting zone. Solute flux into the bed is then proportional to the difference between stream and bed-solute concentrations. A second model assumes that solute is transported within the bed by a vertical diffusion process. The bed-solute concentration, which matches the stream concentration at the interface, varies with depth in the bed according to Fick 's law. A third model assumes convection in the downstream direction occurs in certain parts of the bed, while the mechanism of the first model functions elsewhere. Storage of absorbing species is assumed to occur by equilibrium adsorption within streambed particles. Uptake rate is described by an intraparticle diffusion process. Model equations were solved using finite element numerical methods. Models were calibrated using data from a 24-hour injection of conservative chloride and adsorptive Sr ions at Uvas Creek near Morgan Hill, California. All models predict well except for some overestimation by the adsorption model during dieaway.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri844041","usgsCitation":"Jackman, A.P., Walters, R.A., and Kennedy, V.C., 1984, Low-flow transport models for conservative and sorbed solutes — Uvas Creek, near Morgan Hill, California: U.S. Geological Survey Water-Resources Investigations Report 84-4041, 82 p., https://doi.org/10.3133/wri844041.","productDescription":"82 p.","costCenters":[],"links":[{"id":394617,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35942.htm"},{"id":123415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4041/report-thumb.jpg"},{"id":56689,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Uvas Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.75,\n              37.05\n            ],\n            [\n              -121.667,\n              37.05\n            ],\n            [\n              -121.667,\n              37.167\n            ],\n            [\n              -121.75,\n              37.167\n            ],\n            [\n              -121.75,\n              37.05\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6487d9","contributors":{"authors":[{"text":"Jackman, A. P.","contributorId":46957,"corporation":false,"usgs":true,"family":"Jackman","given":"A.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":198809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, R. A.","contributorId":34174,"corporation":false,"usgs":true,"family":"Walters","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":198807,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kennedy, V. C.","contributorId":46080,"corporation":false,"usgs":true,"family":"Kennedy","given":"V.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198808,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27933,"text":"wri834235 - 1984 - An assessment of cumulative impacts of coal mining on the hydrology in part of the Powder River structural basin, Wyoming: A progress report","interactions":[],"lastModifiedDate":"2025-04-09T14:12:54.54617","indexId":"wri834235","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4235","title":"An assessment of cumulative impacts of coal mining on the hydrology in part of the Powder River structural basin, Wyoming: A progress report","docAbstract":"<p>The U.S. Geological Survey and the Wyoming Department of Environmental Quality are involved in a cooperative effort to assess the probable cumulative impacts of coal mining on the hydrology of a part of the Powder River Structural Basin in Wyoming. It was assumed that the principal impacts on the ground-water system due to mining will occur in the relatively shallow aquifers which can be grouped into three homogeneous aquifers, namely, the Wyodak coal, the overburden, and the under burden. Emphasis of this report is on the results of analysis of surface-water resources in the Caballo Creek drainage. A surface-water model of the Caballo Creek drainage was developed using the Hydrological Simulation Program-Fortran model to help assess the impacts of mining activities on streamflow. The Caballo Creek drainage was divided into 10 land segments and 6 stream reaches in the modeling process. Three simulation runs show little, if any, change in streamflow between pre- and post-mining conditions and very little change between pre-mining and during-mining conditions. The principal reason for the absence of change is the high infiltration rate used in the model for all three conditions.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834235","usgsCitation":"Jordan, P.R., Bloyd, R., and Daddow, P., 1984, An assessment of cumulative impacts of coal mining on the hydrology in part of the Powder River structural basin, Wyoming: A progress report: U.S. Geological Survey Water-Resources Investigations Report 83-4235, iv, 29 p., https://doi.org/10.3133/wri834235.","productDescription":"iv, 29 p.","costCenters":[],"links":[{"id":394363,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35874.htm"},{"id":56748,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4235/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123888,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4235/report-thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.75,\n              44\n            ],\n            [\n              -105.25,\n              44\n            ],\n            [\n              -105.25,\n              44.217\n            ],\n            [\n              -105.75,\n              44.217\n            ],\n            [\n              -105.75,\n              44\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684e08","contributors":{"authors":[{"text":"Jordan, P. R.","contributorId":7282,"corporation":false,"usgs":true,"family":"Jordan","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bloyd, R. M.","contributorId":34549,"corporation":false,"usgs":true,"family":"Bloyd","given":"R. M.","affiliations":[],"preferred":false,"id":198929,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Daddow, P. B.","contributorId":26700,"corporation":false,"usgs":true,"family":"Daddow","given":"P. B.","affiliations":[],"preferred":false,"id":198928,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":41669,"text":"ofr84786 - 1984 - Aeromagnetic map of the northern and central Sierra Nevada foothills and adjacent Sacramento Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr84786","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-786","title":"Aeromagnetic map of the northern and central Sierra Nevada foothills and adjacent Sacramento Valley, California","language":"ENGLISH","doi":"10.3133/ofr84786","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Aeromagnetic map of the northern and central Sierra Nevada foothills and adjacent Sacramento Valley, California: U.S. Geological Survey Open-File Report 84-786, 7 maps :photocopy ;88 x 115 cm. and smaller, on sheets 108 x 126 cm. and smaller., https://doi.org/10.3133/ofr84786.","productDescription":"7 maps :photocopy ;88 x 115 cm. and smaller, on sheets 108 x 126 cm. and smaller.","costCenters":[],"links":[{"id":135651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21064,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0786/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21065,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0786/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21066,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0786/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21067,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0786/plate-4_east.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21068,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0786/plate-4_west.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21069,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0786/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21070,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0786/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":21071,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0786/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b44e","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":530556,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38571,"text":"pp1307 - 1984 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","interactions":[{"subject":{"id":10046,"text":"ofr83216 - 1983 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","indexId":"ofr83216","publicationYear":"1983","noYear":false,"title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":38571,"text":"pp1307 - 1984 - Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","indexId":"pp1307","publicationYear":"1984","noYear":false,"title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado"},"id":1}],"lastModifiedDate":"2017-08-31T17:15:10","indexId":"pp1307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1307","title":"Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado","docAbstract":"<p>Proposed oil-shale mining in northeastern Utah is expected to impact the water resources of a 3,000-square-mile area. This report summarizes a comprehensive hydrologic investigation of the area which resulted in 13 published reports. Hydrologic information obtained during 1974-80 was used to evaluate the availability of water and to evaluate potential impacts of an oil-shale industry on the water resources.</p><p>The study area is the southeastern part of the Uinta Basin, Utah and Colorado, where the hydrology is extremely variable. The normal annual precipitation averages 11 inches and varies with altitude. It ranges from less than 8 inches at altitudes below 5,000 feet along the White and Green Rivers to more than 20 inches where altitudes exceed 9,000 feet on the Roan Plateau.</p><p>The White and Green Rivers are large streams that flow through the area. They convey an average flow of 4.3 million acre-feet per year from outside drainage areas of about 34,000 square miles, which is more than 150 times as much flow as that originating within the area. Streams originating in areas where precipitation is less than 10 inches are ephemeral. Mean annual runoff from the study area is about 28,000 acre-feet and ranges from less than 0.1 to 1.6 inches, depending on the location. At any given site, runoff varies greatly-from year to year and season to season. Potential evapotranspiration is large, exceeding precipitation in all years. </p><p>Three major aquifers occur in the area. They are alluvial deposits of small areal extent along the major stream valleys; the bird's-nest aquifer of the Parachute Creek Member of the Green River Formation, which is limited to the central part of the study area; and the Douglas Creek aquifer of the Douglas Creek Member of the Green River Formation, which underlies most of the area. Total recoverable water in storage in the three aquifers is about 18 million acre-feet. Yields of individual wells and interference between wells limit the maximum practical withdrawal to about 20,000 acre-feet per year.</p><p>An oil-shale industry in the southeastern Uinta Basin with a peak production of 400,000 barrels of oil per day would require a water supply of about 70,000 acre-feet per year. Sources of water supply considered for such an industry were: diversion from the natural flow of the White River, a proposed reservoir on the White River, diversion from the White River combined with proposed off-stream storage in Hells Hole Canyon, diversion from the Green River, and conjunctive use of ground and surface water.</p><p>The proposed reservoir on the White River would trap about 90 percent of the sediment moving in the river and in turn would release almost sediment-free water. Possible impacts are changes in channel gradient in the downstream 18 miles of the White River and changes in bank stability. In some parts of the area, annual sheet-erosion rates are as great as 2.2 acre-feet per square mile but sediment yield to the White River is less than might be expected because the runoff is small. If process water from retort operations or water used in the construction of surface facilities is discharged into a normally dry streambed, increased channel erosion and sediment in tributary streams could result in increased sediment loads in the White River. In addition, sediment yields from retorted-shale piles with minimum slopes could exceed 0.1 acrefoot per square mile during a common storm. Thus, without safeguards, the useful life of any proposed reservoir or holding pond could be decreased considerably.</p><p>Leachate water from retorted-shale piles has large concentrations of sodium and sulfate, and the chemical composition of retort waters differs considerably from that of the natural waters of the area. The retort waters contain a greater concentration of dissolved solids and more organic carbon and nutrients. Without proper disposal or impoundment of retort and leachate waters, the salinity of downstream waters in the Colorado River Basin would be increased. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp1307","usgsCitation":"Lindskov, K., and Kimball, B.A., 1984, Water resources and potential hydrologic effects of oil-shale development in the southeastern Uinta Basin, Utah and Colorado: U.S. Geological Survey Professional Paper 1307, iv, 32 p., https://doi.org/10.3133/pp1307.","productDescription":"iv, 32 p.","numberOfPages":"38","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":123808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1307/report-thumb.jpg"},{"id":65347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1307/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Utah","otherGeospatial":"Uinta Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d2e4b07f02db5487cd","contributors":{"authors":[{"text":"Lindskov, K.L.","contributorId":91077,"corporation":false,"usgs":true,"family":"Lindskov","given":"K.L.","affiliations":[],"preferred":false,"id":220087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimball, B. A.","contributorId":87583,"corporation":false,"usgs":false,"family":"Kimball","given":"B.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":220086,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33363,"text":"b1538 - 1984 - Mineral resources of the Charles Sheldon Wilderness Study Area, Humboldt and Washoe Counties, Nevada, and Lake and Harney Counties, Oregon","interactions":[{"subject":{"id":30804,"text":"ofr781002 - 1978 - Mineral resources of the Charles Sheldon wilderness study area, Humboldt and Washoe Counties, Nevada, and Lake and Harney Counties, Oregon","indexId":"ofr781002","publicationYear":"1978","noYear":false,"title":"Mineral resources of the Charles Sheldon wilderness study area, Humboldt and Washoe Counties, Nevada, and Lake and Harney Counties, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":33363,"text":"b1538 - 1984 - Mineral resources of the Charles Sheldon Wilderness Study Area, Humboldt and Washoe Counties, Nevada, and Lake and Harney Counties, Oregon","indexId":"b1538","publicationYear":"1984","noYear":false,"title":"Mineral resources of the Charles Sheldon Wilderness Study Area, Humboldt and Washoe Counties, Nevada, and Lake and Harney Counties, Oregon"},"id":1}],"lastModifiedDate":"2025-03-03T19:48:06.329047","indexId":"b1538","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1538","title":"Mineral resources of the Charles Sheldon Wilderness Study Area, Humboldt and Washoe Counties, Nevada, and Lake and Harney Counties, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1538","usgsCitation":"Water Resources Division, U.S. Geological Survey, and U.S. Bureau of Mines, 1984, Mineral resources of the Charles Sheldon Wilderness Study Area, Humboldt and Washoe Counties, Nevada, and Lake and Harney Counties, Oregon: U.S. Geological Survey Bulletin 1538, Report: v, 139 p.; 2 Plates: 34.68 x 33.52 inches and 42.86 x 30.16 inches, https://doi.org/10.3133/b1538.","productDescription":"Report: v, 139 p.; 2 Plates: 34.68 x 33.52 inches and 42.86 x 30.16 inches","costCenters":[],"links":[{"id":482754,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92740.htm","text":"Geologic appraisal of the Charles Sheldon Wilderness Study Area, Nevada and Oregon","linkFileType":{"id":5,"text":"html"}},{"id":482753,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21621.htm","text":"Mineral resources of the Charles Sheldon Wilderness Study Area, Humboldt and Washoe Counties, Nevada, and Lake and Harney Counties, Oregon","linkFileType":{"id":5,"text":"html"}},{"id":61205,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1538/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61204,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1538/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251830,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1538/report-thumb.jpg"},{"id":247389,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1538/report.pdf","size":"13661","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada, Oregon","county":"Harney County, Humboldt County, Lake County, Washoe County","otherGeospatial":"Charles Sheldon Wilderness Study Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -119.70246614561646,\n              42.16172358581122\n            ],\n            [\n              -119.70246614561646,\n              41.54833743395767\n            ],\n            [\n              -118.68859224784083,\n              41.54833743395767\n            ],\n            [\n              -118.68859224784083,\n              42.158844460387456\n            ],\n            [\n              -119.70246614561646,\n              42.16172358581122\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b07e4b07f02db69adee","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":529479,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"U.S. Bureau of Mines","contributorId":128223,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Mines","id":529480,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36538,"text":"fwsobs82_10_75 - 1984 - Habitat Suitability Index Models: Spotted seatrout","interactions":[],"lastModifiedDate":"2022-02-09T15:20:37.161233","indexId":"fwsobs82_10_75","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/10.75","subseriesTitle":"Habitat Suitability Index","title":"Habitat Suitability Index Models: Spotted seatrout","docAbstract":"<p>The estuarine spotted seatrout, a primarily estuarine species, is one of the most important sport and commercial fishes in coastal Gulf of Mexico waters (Arnold et a1. 1976). Spotted seatrout rank second by weight in catches by U.S. saltwater sport fishermen (National Marine Fisheries Services 1981) .</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Kostecki, P.T., 1984, Habitat Suitability Index Models: Spotted seatrout: FWS/OBS 82/10.75, vi, 22 p.","productDescription":"vi, 22 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":166203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649743","contributors":{"authors":[{"text":"Kostecki, Paul T.","contributorId":55060,"corporation":false,"usgs":true,"family":"Kostecki","given":"Paul","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":216495,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42041,"text":"ofr84512 - 1984 - Aeromagnetic map of east-central Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr84512","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-512","title":"Aeromagnetic map of east-central Oregon","language":"ENGLISH","doi":"10.3133/ofr84512","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Aeromagnetic map of east-central Oregon: U.S. Geological Survey Open-File Report 84-512, 1 map on 2 sheets :photocopy ;46 x 61 cm. and 87 x 77 cm., https://doi.org/10.3133/ofr84512.","productDescription":"1 map on 2 sheets :photocopy ;46 x 61 cm. and 87 x 77 cm.","costCenters":[],"links":[{"id":136580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79792,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0512/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79793,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0512/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e23","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":530791,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40656,"text":"ofr84689 - 1984 - Buried or abandoned drainage in the Harlem 30ʹ x 60ʹ quadrangle, Montana [sheet 1]. Selected well data: Water quality, quantity, and depth to bedrock in the Harlem 30ʹ x 60ʹ quadrangle, Montana [sheet 2]","interactions":[],"lastModifiedDate":"2022-04-27T21:55:15.864701","indexId":"ofr84689","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-689","title":"Buried or abandoned drainage in the Harlem 30ʹ x 60ʹ quadrangle, Montana [sheet 1]. Selected well data: Water quality, quantity, and depth to bedrock in the Harlem 30ʹ x 60ʹ quadrangle, Montana [sheet 2]","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84689","usgsCitation":"Patton, T.W., and Colton, R.B., 1984, Buried or abandoned drainage in the Harlem 30ʹ x 60ʹ quadrangle, Montana [sheet 1]. Selected well data: Water quality, quantity, and depth to bedrock in the Harlem 30ʹ x 60ʹ quadrangle, Montana [sheet 2]: U.S. Geological Survey Open-File Report 84-689, 2 Plates: 36.57 × 27.28 inches and 36.57 × 26.85 inches, https://doi.org/10.3133/ofr84689.","productDescription":"2 Plates: 36.57 × 27.28 inches and 36.57 × 26.85 inches","costCenters":[],"links":[{"id":136829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":77742,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0689/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":77741,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0689/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","country":"United States","state":"Montana","otherGeospatial":"Harlem 30ʹ x 60ʹ quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109,\n              48.5\n            ],\n            [\n              -108,\n              48.5\n            ],\n            [\n              -108,\n              49\n            ],\n            [\n              -109,\n              49\n            ],\n            [\n              -109,\n              48.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f999e","contributors":{"authors":[{"text":"Patton, Thomas W.","contributorId":65322,"corporation":false,"usgs":true,"family":"Patton","given":"Thomas","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":223661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colton, Roger B.","contributorId":17967,"corporation":false,"usgs":true,"family":"Colton","given":"Roger","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":223660,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38647,"text":"pp1151D - 1984 - Stratigraphy and structure of the western Kentucky fluorspar district","interactions":[],"lastModifiedDate":"2012-02-02T00:09:58","indexId":"pp1151D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1151","chapter":"D","title":"Stratigraphy and structure of the western Kentucky fluorspar district","docAbstract":"The western Kentucky fluorspar district is part of the larger Illinois-Kentucky fluorspar district, the largest producer of fluorspar in the United States. This report is based largely on data gathered from 1960 to 1974 during the U.S. Geological Survey-Kentucky Geological Survey cooperative geologic mapping program of Kentucky. It deals chiefly with the stratigraphy and structure of the district and, to a lesser extent, with the fluorspar-zinc-lead-barite deposits. \r\n\r\nSedimentary rocks exposed in the district range in age from Early Mississippian (Osagean) to Quaternary. Most rocks exposed at the surface are Mississippian in age; two-thirds are marine fossiliferous limestones, and the remainder are shales, siltstones, and sandstones. Osagean deep-water marine silty limestone and chert are present at the surface in the southwestern corner of the district. Meramecian marine limestone is exposed at the surface in about half the area. Chesterian marine and fluvial to fluviodeltaic clastic sedimentary rocks and marine limestone underlie about one-third of the area. The total sequence of Mississippian rocks is about 3,000 ft thick. \r\n\r\nPennsylvanian rocks are dominantly fluvial clastic sedimentary rocks that change upward into younger fluviodeltaic strata. Pennsylvanian strata of Morrowan and Atokan age are locally thicker than 600 ft along the eastern and southeastern margin and in the major grabens of the district where they have been preserved from erosion. \r\n\r\nCretaceous and Tertiary sediments of the Mississippi embayment truncate Paleozoic formations in and near the southwestern corner of the district and are preserved mostly as erosional outliers. The deposits are Gulfian nonmarine gravels, sands, and clays as much as 170 ft thick and upper Pliocene fluvial continental deposits as thick as 45 ft. Pleistocene loess deposits mantle the upland surface of the district, and Quaternary fluvial and fluviolacustrine deposits are common and widespread along the Ohio and Cumberland Rivers and their major tributaries. \r\n\r\nMany mafic dikes and a few mafic sills are present. The mafic rocks are mostly altered mica peridotites or lamprophyres that are composed of carbonate minerals, serpentine, chlorite, and biotite and contain some hornblende, pyroxene, and olivine. Most of the dikes are in a north-north west-trending belt 6 to 8 mi wide and strike N. 20 0 -30 0 W. The dikes dip from 80 0 to 90 0 and are commonly 5 to 10 ft wide. Radioisotopic study indicates that the dikes are Early Permian in age. \r\n\r\nThe district is just southeast of the intersection of the east-trending Rough Creek-Shawneetown and northeast-trending New Madrid fault systems. The district's principal structural features are a northwest-trending domal anticline, the Tolu Arch, and a series of steeply dipping to nearly vertical normal faults and fault zones that trend dominantly northeastward and divide the area into elongated northeast-trending grabens and horsts. Formation of these grabens and horsts was one of the major tectonic events in the district. Vertical displacement may be as much as 3,000 ft but commonly ranges from a few feet to a few hundred feet; no substantial horizontal movement is believed to have taken place. Many cross faults having only a few feet of displacement trend northwestward and are occupied at places by mafic dikes. Faulting was mostly post-Early Permian to pre-middle Cretaceous in age. \r\n\r\nMany theories have been advanced to explain the structural history of the district. A generally acceptable overall hypothesis that would account for all the structural complexities, however, is still lacking. Useful structural data, such as the structural differences between the grabens and the horsts, have been obtained, however, from the recently completed geologic mapping. Mapping also has more clearly shown the alinement of the Tolu Arch, the belt of dikes, and an unusually deep graben (the Griffith Bluff graben); this alinement suggests that possibl","language":"ENGLISH","doi":"10.3133/pp1151D","usgsCitation":"Trace, R.D., and Amos, D., 1984, Stratigraphy and structure of the western Kentucky fluorspar district: U.S. Geological Survey Professional Paper 1151, p. D1-D41; 1 plate in pocket, https://doi.org/10.3133/pp1151D.","productDescription":"p. D1-D41; 1 plate in pocket","costCenters":[],"links":[{"id":119900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1151d/report-thumb.jpg"},{"id":65478,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1151d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65479,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1151d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a7fee","contributors":{"authors":[{"text":"Trace, R. D.","contributorId":47004,"corporation":false,"usgs":true,"family":"Trace","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":220215,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Amos, D.H.","contributorId":75600,"corporation":false,"usgs":true,"family":"Amos","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":220216,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38635,"text":"pp1066J - 1984 - Leperditicopid ostracodes from Ordovician rocks of Kentucky and nearby states and characteristic features of the order Leperditicopida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"pp1066J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1066","chapter":"J","title":"Leperditicopid ostracodes from Ordovician rocks of Kentucky and nearby states and characteristic features of the order Leperditicopida","docAbstract":"Leperditicopid ostracodes from the Ordovician formations of Kentucky occur in micritic to fine-grained carbonate rocks believed to represent shallow-water facies. They are found at widely separated horizons in the Middle Ordovician High Bridge Group, the Middle and Upper Ordovician Lexington Limestone, and the Upper Ordovician Ashlock, Bull Fork, and Drakes Formations. In this sequence, the leperditicopes are represented by two genera of leperditiids, Eoleperditia Swartz, 1949 and Bivia Berdan, 1976, and six isochilinid genera, Isochilina Jones, 1858, Teichochilina Swartz, 1949, Ceratoleperditia Harris, 1960, Parabriartina n. gen., Kenodontochilina n. gen., and Saffordellina Bassler and Kellett, 1934; the type species of the hitherto poorly known genus Saffordellina, S. muralis (Ulrich and Bassler, 1923), is redescribed and refigured. In all, 18 taxa, of which 2 are in open nomenclature, are described and illustrated. In addition, the family Isochilinidae Swartz, 1949 is redefined to include genera without marginal brims and with straight ventral contact margins. The morphological characteristics of leperditicopid genera are discussed, and a table listing described genera and their diagnostic features is included.","language":"ENGLISH","doi":"10.3133/pp1066J","usgsCitation":"Berdan, J., 1984, Leperditicopid ostracodes from Ordovician rocks of Kentucky and nearby states and characteristic features of the order Leperditicopida: U.S. Geological Survey Professional Paper 1066, p. J1 - J40, https://doi.org/10.3133/pp1066J.","productDescription":"p. J1 - J40","costCenters":[],"links":[{"id":120365,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1066j/report-thumb.jpg"},{"id":65466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1066j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a631d","contributors":{"authors":[{"text":"Berdan, J.M.","contributorId":27913,"corporation":false,"usgs":true,"family":"Berdan","given":"J.M.","affiliations":[],"preferred":false,"id":220196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42042,"text":"ofr84208 - 1984 - Aeromagnetic map of east-central Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr84208","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-208","title":"Aeromagnetic map of east-central Texas","language":"ENGLISH","doi":"10.3133/ofr84208","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Aeromagnetic map of east-central Texas: U.S. Geological Survey Open-File Report 84-208, 1 map :photocopy ;44 x 91 cm., https://doi.org/10.3133/ofr84208.","productDescription":"1 map :photocopy ;44 x 91 cm.","costCenters":[],"links":[{"id":136581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79794,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0208/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e32","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":530792,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41049,"text":"ofr84865 - 1984 - Potentiometric surface of the upper Floridan Aquifer in the St. Johns River Water Management District and vicinity, Florida, September 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:05:01","indexId":"ofr84865","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-865","title":"Potentiometric surface of the upper Floridan Aquifer in the St. Johns River Water Management District and vicinity, Florida, September 1984","docAbstract":"This map shows the potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity for September 1984. The Upper Floridan aquifer is the principal source of potable water in the area. Water-level measurements were made on approximately 1,000 wells and on several springs. The potentiometric surface is shown mostly by 5-foot contour intervals. In the Fernandina Beach area of Nassau County a 40-foot interval is used to show a deep cone of depression. The potentiometric surface ranged from 130 feet above sea level in Polk County to 83 feet below sea level in Nassau County. Water levels in key wells ranged from slightly above average to several feet below average for September in response to diverse area rainfall patterns. Most levels in the district were about the same as the levels of September 1983. However, in Nassau County levels were generally below those of September 1983, and levels in Volusia County were mostly higher than September 1983 levels. (USGS)","language":"ENGLISH","doi":"10.3133/ofr84865","usgsCitation":"Schiner, G.R., and Hayes, E.C., 1984, Potentiometric surface of the upper Floridan Aquifer in the St. Johns River Water Management District and vicinity, Florida, September 1984: U.S. Geological Survey Open-File Report 84-865, 1 map :photocopy ;104 x 62 cm., https://doi.org/10.3133/ofr84865.","productDescription":"1 map :photocopy ;104 x 62 cm.","costCenters":[],"links":[{"id":135295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78924,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0865/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682cdc","contributors":{"authors":[{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, Eugene C.","contributorId":46918,"corporation":false,"usgs":true,"family":"Hayes","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":224388,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36444,"text":"fwsobs84_15 - 1984 - Instream water temperature model. Instream Flow Information Paper 16","interactions":[],"lastModifiedDate":"2012-02-02T00:09:38","indexId":"fwsobs84_15","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"84/15","title":"Instream water temperature model. Instream Flow Information Paper 16","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Theurer, F.D., Voos, K.A., and Miller, W., 1984, Instream water temperature model. Instream Flow Information Paper 16: FWS/OBS 84/15, 1 v. (various pagings) : ill., maps; 28 cm.","productDescription":"1 v. (various pagings) : ill., maps; 28 cm.","costCenters":[],"links":[{"id":166569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49efe4b07f02db5eddef","contributors":{"authors":[{"text":"Theurer, Fred D.","contributorId":41699,"corporation":false,"usgs":true,"family":"Theurer","given":"Fred","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":216336,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Voos, Kenneth A.","contributorId":80962,"corporation":false,"usgs":true,"family":"Voos","given":"Kenneth","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":216337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, William J.","contributorId":18069,"corporation":false,"usgs":true,"family":"Miller","given":"William J.","affiliations":[],"preferred":false,"id":216335,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":36429,"text":"fwsobs84_01 - 1984 - Feasibility of using oil shale wastewater for waterfowl wetlands","interactions":[],"lastModifiedDate":"2012-02-02T00:09:36","indexId":"fwsobs84_01","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"84/01","title":"Feasibility of using oil shale wastewater for waterfowl wetlands","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Snyder, B.D., and Snyder, J.L., 1984, Feasibility of using oil shale wastewater for waterfowl wetlands: FWS/OBS 84/01, xxii, 290 p. : ill., maps ; 28 cm.","productDescription":"xxii, 290 p. : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":167672,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbc35","contributors":{"authors":[{"text":"Snyder, Bruce D.","contributorId":70824,"corporation":false,"usgs":true,"family":"Snyder","given":"Bruce","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":216307,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snyder, Janet L.","contributorId":82770,"corporation":false,"usgs":true,"family":"Snyder","given":"Janet","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":216308,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30815,"text":"ofr84624 - 1984 - The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington","interactions":[{"subject":{"id":30815,"text":"ofr84624 - 1984 - The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington","indexId":"ofr84624","publicationYear":"1984","noYear":false,"title":"The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":38516,"text":"pp1345 - 1985 - The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington","indexId":"pp1345","publicationYear":"1985","noYear":false,"title":"The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington"},"id":1}],"supersededBy":{"id":38516,"text":"pp1345 - 1985 - The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington","indexId":"pp1345","publicationYear":"1985","noYear":false,"title":"The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington"},"lastModifiedDate":"2021-01-21T18:29:27.346835","indexId":"ofr84624","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-624","title":"The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr84624","usgsCitation":"Meyer, W., Sabol, M.A., Glicken, H., and Voight, B., 1984, The effects of ground water, slope stability, and seismic hazard on the stability of the South Fork Castle Creek blockage in the Mount St. Helens area, Washington: U.S. Geological Survey Open-File Report 84-624, vi, 72 p., https://doi.org/10.3133/ofr84624.","productDescription":"vi, 72 p.","costCenters":[],"links":[{"id":161238,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0624/report-thumb.jpg"},{"id":382378,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0624/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Mount St. Helens","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.4920654296875,\n              46.118941506107056\n            ],\n            [\n              -121.92626953124999,\n              46.118941506107056\n            ],\n            [\n              -121.92626953124999,\n              46.32986150334176\n            ],\n            [\n              -122.4920654296875,\n              46.32986150334176\n            ],\n            [\n              -122.4920654296875,\n              46.118941506107056\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65df00","contributors":{"authors":[{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":204039,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sabol, M. A.","contributorId":36178,"corporation":false,"usgs":true,"family":"Sabol","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":204037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Glicken, H. X.","contributorId":8902,"corporation":false,"usgs":true,"family":"Glicken","given":"H. X.","affiliations":[],"preferred":false,"id":204036,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Voight, Barry","contributorId":73653,"corporation":false,"usgs":true,"family":"Voight","given":"Barry","email":"","affiliations":[],"preferred":false,"id":204038,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":40836,"text":"ofr84620 - 1984 - Potentiometric surface of the Floridan Aquifer, Southwest Florida Water Management District, May 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:10:49","indexId":"ofr84620","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-620","title":"Potentiometric surface of the Floridan Aquifer, Southwest Florida Water Management District, May 1984","docAbstract":"A May 1984 potentiometric surface map of the Southwest Florida Water Management District depicts the annual low water-level period. Water levels in most wells measured in May 1984 were lower than in September 1983. May levels averaged about 1 foot lower than September levels in areas north of latitude 28 07'10' ' and about 9 feet lower in southern areas. Generally, water levels in May 1984 were lower when compared to May 1983. Water levels in most wells measured in May 1984 averaged less than 1 foot lower than May 1983 levels in the north and about 2 feet lower in the south. (USGS)","language":"ENGLISH","doi":"10.3133/ofr84620","usgsCitation":"Barr, G., and Schiner, G.R., 1984, Potentiometric surface of the Floridan Aquifer, Southwest Florida Water Management District, May 1984: U.S. Geological Survey Open-File Report 84-620, 1 map :photocopy ;79 x 56 cm., https://doi.org/10.3133/ofr84620.","productDescription":"1 map :photocopy ;79 x 56 cm.","costCenters":[],"links":[{"id":171085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78708,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0620/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bfc0","contributors":{"authors":[{"text":"Barr, G. L.","contributorId":22312,"corporation":false,"usgs":true,"family":"Barr","given":"G. L.","affiliations":[],"preferred":false,"id":224019,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224020,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41179,"text":"ofr84801 - 1984 - Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1984","interactions":[],"lastModifiedDate":"2021-11-17T20:38:11.632367","indexId":"ofr84801","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-801","title":"Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1984","docAbstract":"<p>This map shows the potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity for May 1984. The Upper Floridan aquifer is the principal source of potable water in the area. Water-level measurements were made on approximately 1,000 wells and on several springs. The potentiometric surface is shown mostly by 5-foot contour intervals. In the Fernandina Beach area a 40-foot interval is used to show a deep cone of depression. The potentiometric surface ranged from 126 feet above sea level in Polk County to 84 feet below sea level in Nassau County. Water levels in key wells were mostly above, or less frequently, slightly below averages for May in response to diverse area rainfall patterns. Most levels in the district were about the same, or more commonly, 1 to 2 feet lower than May 1983 levels.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84801","usgsCitation":"Schiner, G.R., and Hayes, E.C., 1984, Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1984: U.S. Geological Survey Open-File Report 84-801, 1 Plate: 28.69 × 46.14 inches, https://doi.org/10.3133/ofr84801.","productDescription":"1 Plate: 28.69 × 46.14 inches","costCenters":[],"links":[{"id":391820,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13569.htm"},{"id":79011,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0801/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"St. Johns River Water Management District and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.75,\n              26.75\n            ],\n            [\n              -80,\n              26.75\n            ],\n            [\n              -80,\n              30.75\n            ],\n            [\n              -82.75,\n              30.75\n            ],\n            [\n              -82.75,\n              26.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6863da","contributors":{"authors":[{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224612,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayes, Eugene C.","contributorId":46918,"corporation":false,"usgs":true,"family":"Hayes","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":224613,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41980,"text":"ofr84207 - 1984 - Aeromagnetic map of the Lockhart area, Texas","interactions":[],"lastModifiedDate":"2022-01-10T21:47:50.488275","indexId":"ofr84207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-207","title":"Aeromagnetic map of the Lockhart area, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr84207","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Aeromagnetic map of the Lockhart area, Texas: U.S. Geological Survey Open-File Report 84-207, 1 Plate: 14.86 × 23.74 inches, https://doi.org/10.3133/ofr84207.","productDescription":"1 Plate: 14.86 × 23.74 inches","costCenters":[],"links":[{"id":135403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79738,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0207/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394150,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13309.htm"}],"country":"United States","state":"Texas","otherGeospatial":"Lockhart area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98,\n              29\n            ],\n            [\n              -97.25,\n              29\n            ],\n            [\n              -97.25,\n              30\n            ],\n            [\n              -98,\n              30\n            ],\n            [\n              -98,\n              29\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698183","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":530749,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41989,"text":"ofr84393 - 1984 - Aeromagnetic map of the Mt. Jefferson area, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:02","indexId":"ofr84393","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-393","title":"Aeromagnetic map of the Mt. Jefferson area, Nevada","language":"ENGLISH","doi":"10.3133/ofr84393","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Aeromagnetic map of the Mt. Jefferson area, Nevada: U.S. Geological Survey Open-File Report 84-393, 1 map :photocopy ;33 x 70 cm., https://doi.org/10.3133/ofr84393.","productDescription":"1 map :photocopy ;33 x 70 cm.","costCenters":[],"links":[{"id":135430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79746,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0393/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d23","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":530756,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42059,"text":"ofr84666 - 1984 - Aeromagnetic map of the Craig area, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:02","indexId":"ofr84666","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-666","title":"Aeromagnetic map of the Craig area, Alaska","language":"ENGLISH","doi":"10.3133/ofr84666","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Aeromagnetic map of the Craig area, Alaska: U.S. Geological Survey Open-File Report 84-666, 3 maps :photocopy ;70 x 64 cm. and smaller, on sheets 92 x 90 cm. and 46 x 61 cm., https://doi.org/10.3133/ofr84666.","productDescription":"3 maps :photocopy ;70 x 64 cm. and smaller, on sheets 92 x 90 cm. and 46 x 61 cm.","costCenters":[],"links":[{"id":135516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79808,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0666/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79809,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0666/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79807,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0666/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696c24","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":530806,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42061,"text":"ofr84392 - 1984 - Aeromagnetic map of the Thunder Mountain area, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:02","indexId":"ofr84392","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-392","title":"Aeromagnetic map of the Thunder Mountain area, Nevada","language":"ENGLISH","doi":"10.3133/ofr84392","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1984, Aeromagnetic map of the Thunder Mountain area, Nevada: U.S. Geological Survey Open-File Report 84-392, 1 map :photocopy ;48 x 53 cm., https://doi.org/10.3133/ofr84392.","productDescription":"1 map :photocopy ;48 x 53 cm.","costCenters":[],"links":[{"id":135518,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79811,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0392/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c3ee","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":530807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41022,"text":"ofr84812 - 1984 - Potentiometric surface of the upper Floridan aquifer, Southwest Florida Water Management District, September 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:05:04","indexId":"ofr84812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"84-812","title":"Potentiometric surface of the upper Floridan aquifer, Southwest Florida Water Management District, September 1984","docAbstract":"A September 1984 potentiometric surface map of the Southwest Florida Water Management District depicts the annual high water level period. Water levels in most wells measured in September 1984 were higher than in May 1984. September levels averaged less than 1 foot higher than May levels in areas north of latitude 28 degrees 7 feet and about 6 feet higher in southern areas. Generally, water levels in September 1984 were lower when compared to September 1983. Water levels in most wells measured in September 1984 averaged less than 1 foot lower than September 1983 levels in the north and about 2.6 feet lower in the south. (USGS)","language":"ENGLISH","doi":"10.3133/ofr84812","usgsCitation":"Barr, G., 1984, Potentiometric surface of the upper Floridan aquifer, Southwest Florida Water Management District, September 1984: U.S. Geological Survey Open-File Report 84-812, 1 map :photocopy ;79 x 56 cm., on sheet 92 x 61 cm., https://doi.org/10.3133/ofr84812.","productDescription":"1 map :photocopy ;79 x 56 cm., on sheet 92 x 61 cm.","costCenters":[],"links":[{"id":136723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78903,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0812/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697409","contributors":{"authors":[{"text":"Barr, G. L.","contributorId":22312,"corporation":false,"usgs":true,"family":"Barr","given":"G. L.","affiliations":[],"preferred":false,"id":224344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}