Paleomagnetic studies of 25 oriented bedrock specimens from Jabal Mahd adh Dhahab, located 160 km southeast of Al Madinah, Kingdom of Saudi Arabia, have yielded important structural information relating to the geologic history of this base and precious metal deposit. Samples were collected along one traverse away from the mineralized zones, across the northeast-plunging antiform that constitutes the dominant regional structure of the area, and along another traverse down the axis of the mineralized zones. Lithologies range from andesite flows through andesitic to rhyodacitic tuffs, lapilli tuffs, and volcaniclastic sediments. Measurements of remanent magnetization direction and intensity before and after stepwise alternating-field demagnetization ranging from 25 Oersted (Oe) to 1000 Oe were carried out on all samples. Three classes of demagnetization behavior were observed: A very stable class with little change in direction and intensity of magnetization; a class in which rapid changes were observed at first but which then settled on a high coercivity stable component of magnetization; and a class in which the magnetization was composed of a spectrum of low coervicity components, and continuous variation of direction and intensity of magnetization occurred.
\nA structural correction restoring the bedding to horizontal resulted in a significant reduction in dispersion of magnetization directions, and implies that the magnetization was acquired before the northeast-trending deformation. At least one geomagnetic reversal is recorded and, together with drillhole electric logs, suggests structural repetition of some parts of the area.
\nThe determined paleopole location, after correction for Tertiary rotation of Arabia from Africa, falls on the apparent polar wander path for Gondwanaland at an age of 600-590 Ma, which is younger than the mineralization age of about 680 Ma and the age of the Mahd group of rocks (772 Ma) determined from geochronologic studies, and implies that the rocks have been remagnetized during the middle Pan African times.
\nThe results of this work suggest that more extensive paleomagnetic investigations of the felsic volcanic and volcanic-derived rocks of the northern Arabian shield should provide greater insight into the structural evolution of the shield, and these investigations are recommended.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr8515","usgsCitation":"Gettings, M.E., 1985, Paleomagnetic investigations at Mahd adh Dhahab, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 85-15, i, 43 p., ill., map: 28 cm., https://doi.org/10.3133/ofr8515.","productDescription":"i, 43 p., ill., map: 28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":36730,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0015/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0015/report-thumb.jpg"}],"country":"Saudi Arabia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 40,\n 23\n ],\n [\n 40,\n 24\n ],\n [\n 41,\n 24\n ],\n [\n 41,\n 23\n ],\n [\n 40,\n 23\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c3b","contributors":{"authors":[{"text":"Gettings, M. E.","contributorId":25148,"corporation":false,"usgs":true,"family":"Gettings","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159129,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29956,"text":"wri854020 - 1985 - Determination of diffusivities in the Rustler Formation from exploratory-shaft construction at the Waste Isolation Pilot Plant in southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri854020","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":"85-4020","title":"Determination of diffusivities in the Rustler Formation from exploratory-shaft construction at the Waste Isolation Pilot Plant in southeastern New Mexico","docAbstract":"The construction of an exploratory shaft 12 feet in diameter into the Salado Formation (repository horizon for transuranic waste material) at the Waste Isolation Pilot Plant site in southeastern New Mexico affected water-levels in water-bearing zones above the repository horizon. By reading the construction history of the exploratory shaft, an approximation of construction-generated hydraulic stresses at the shaft was made. The magnitude of the construction-generated stresses was calibrated using the hydrographs from one hydrologic test pad. Whereas flow rates from the Magenta Dolomite and Culebra Dolomite Members in the Rustler Formation into the exploratory shaft were unknown, the ratio of transmissivity to storage (diffusivity) was determined by mathematically simulating the aquifers and the hydrologic stresses with flood-wave-response digital model. These results indicate that the Magenta Dolomite and Culebra Dolomite Members of the Rustler Formation can be modeled as homogeneous, isotropic, and confined water-bearing zones. One simple and consistent explanation, but by no means the only explanation, of the lack of a single diffusivity value in the Culebra aquifer is that the open-hole observation wells at the hydrologic test pads dampen the amplitude of water-level changes. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854020","usgsCitation":"Stevens, K., and Beyeler, W., 1985, Determination of diffusivities in the Rustler Formation from exploratory-shaft construction at the Waste Isolation Pilot Plant in southeastern New Mexico: U.S. Geological Survey Water-Resources Investigations Report 85-4020, v, 32 p. :ill., map ;28 cm., https://doi.org/10.3133/wri854020.","productDescription":"v, 32 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4020/report-thumb.jpg"},{"id":58775,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4020/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66789e","contributors":{"authors":[{"text":"Stevens, Ken","contributorId":101264,"corporation":false,"usgs":true,"family":"Stevens","given":"Ken","email":"","affiliations":[],"preferred":false,"id":202426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beyeler, Walt","contributorId":92306,"corporation":false,"usgs":true,"family":"Beyeler","given":"Walt","email":"","affiliations":[],"preferred":false,"id":202425,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":57364,"text":"wdrTX842 - 1985 - Water resources data, Texas, water year 1984; Volume 2. San Jacinto River basin, Brazos River basin, San Bernard River basin, and intervening coastal basins","interactions":[],"lastModifiedDate":"2023-03-07T22:34:50.271795","indexId":"wdrTX842","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":"TX-84-2","title":"Water resources data, Texas, water year 1984; Volume 2. San Jacinto River basin, Brazos River basin, San Bernard River basin, and intervening coastal basins","docAbstract":"Surface-water data for the 1984 water year for Texas are presented in three volumes, appropriately identified as to content by river basins. Data in each volume consist of records of stage, discharge, and water quality of streams and canals; and stage, contents, and water quality of lakes and reservoirs. Also included are crest-stage and flood-hydrograph partial-record stations, reconnaissance partial-record stations, and low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. Records for a few pertinent stations in bordering States are also included. 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 Texas.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrTX842","collaboration":"Prepared in cooperation with the State of Texas and with other agencies","usgsCitation":"Buckner, H., Carrillo, E., and Davidson, H., 1985, Water resources data, Texas, water year 1984; Volume 2. San Jacinto River basin, Brazos River basin, San Bernard River basin, and intervening coastal basins: U.S. Geological Survey Water Data Report TX-84-2, x, 427 p., https://doi.org/10.3133/wdrTX842.","productDescription":"x, 427 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":184282,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/tx-84-2/report-thumb.jpg"},{"id":413824,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/tx-84-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.0517578125,\n 35.003003395276714\n ],\n [\n -103.0517578125,\n 34.06176136129718\n ],\n [\n -102.667236328125,\n 33.797408767572485\n ],\n [\n -101.84326171875,\n 33.4955977448657\n ],\n [\n -101.1181640625,\n 33.073130945006625\n ],\n [\n -100.118408203125,\n 32.602361666817515\n ],\n [\n -98.96484375,\n 31.840232667909365\n ],\n [\n -97.767333984375,\n 30.968189296794247\n ],\n [\n -97.14111328125,\n 30.44867367928756\n ],\n [\n -96.52587890625,\n 29.707139348134145\n ],\n [\n -96.21826171874999,\n 29.219302076779456\n ],\n [\n -95.95458984375,\n 28.545925723233477\n ],\n [\n -95.526123046875,\n 28.70986084394286\n ],\n [\n -95.00976562499999,\n 28.8831596093235\n ],\n [\n -94.757080078125,\n 29.248063243796576\n ],\n [\n -94.85595703125,\n 29.649868677972304\n ],\n [\n -95.03173828125,\n 29.983486718474694\n ],\n [\n -95.614013671875,\n 30.80791068136646\n ],\n [\n -96.35009765625,\n 31.5504526754715\n ],\n [\n -97.086181640625,\n 32.045332838858506\n ],\n [\n -98.06396484375,\n 32.861132322810946\n ],\n [\n -99.2724609375,\n 33.65120829920497\n ],\n [\n -100.72265625,\n 34.243594729697406\n ],\n [\n -101.458740234375,\n 34.615126683462194\n ],\n [\n -103.0517578125,\n 35.003003395276714\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc873","contributors":{"authors":[{"text":"Buckner, H.D.","contributorId":49783,"corporation":false,"usgs":true,"family":"Buckner","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":256808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carrillo, E.R.","contributorId":77924,"corporation":false,"usgs":true,"family":"Carrillo","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":256809,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davidson, H.J.","contributorId":108177,"corporation":false,"usgs":true,"family":"Davidson","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":256810,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1918,"text":"wsp2277 - 1985 - A primer on trace metal-sediment chemistry","interactions":[{"subject":{"id":9582,"text":"ofr84709 - 1984 - A primer on trace metal-sediment chemistry","indexId":"ofr84709","publicationYear":"1984","noYear":false,"title":"A primer on trace metal-sediment chemistry"},"predicate":"SUPERSEDED_BY","object":{"id":1918,"text":"wsp2277 - 1985 - A primer on trace metal-sediment chemistry","indexId":"wsp2277","publicationYear":"1985","noYear":false,"title":"A primer on trace metal-sediment chemistry"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp2277","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":"2277","title":"A primer on trace metal-sediment chemistry","docAbstract":"In most aquatic systems, concentrations of trace metals in suspended sediment and the top few centimeters of bottom sediment are far greater than concentrations of trace metals dissolved in the water column. Consequently, the distribution, transport, and availability of these constituents can not be intelligently evaluated, nor can their environmental impact be determined or predicted solely through the sampling and analysis of dissolved phases. This Primer is designed to acquaint the reader with the basic principles that govern the concentration and distribution of trace metals associated with bottom and suspended sediments. \r\n\r\nThe sampling and analysis of suspended and bottom sediments are very important for monitoring studies, not only because trace metal concentrations associated with them are orders of magnitude higher than in the dissolved phase, but also because of several other factors. Riverine transport of trace metals is dominated by sediment. In addition, bottom sediments serve as a source for suspended sediment and can provide a historical record of chemical conditions. This record will help establish area baseline metal levels against which existing conditions can be compared. \r\n\r\nMany physical and chemical factors affect a sediment's capacity to collect and concentrate trace metals. The physical factors include grain size, surface area, surface charge, cation exchange capacity, composition, and so forth. Increases in metal concentrations are strongly correlated with decreasing grain size and increasing surface area, surface charge, cation exchange capacity, and increasing concentrations of iron and manganese oxides, organic matter, and clay minerals. Chemical factors are equally important, especially for differentiating between samples having similar bulk chemistries and for inferring or predicting environmental availability. Chemical factors entail phase associations (with such sedimentary components as interstitial water, sulfides, carbonates, and organic matter) and ways in which the metals are entrained by the sediments (such as adsorption, complexation, and within mineral lattices).","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2277","usgsCitation":"Horowitz, A.J., 1985, A primer on trace metal-sediment chemistry: U.S. Geological Survey Water Supply Paper 2277, v, 67 p. :ill. ;28 cm., https://doi.org/10.3133/wsp2277.","productDescription":"v, 67 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":137702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2277/report-thumb.jpg"},{"id":27244,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2277/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f1bd9","contributors":{"authors":[{"text":"Horowitz, Arthur J. 0000-0002-3296-730X horowitz@usgs.gov","orcid":"https://orcid.org/0000-0002-3296-730X","contributorId":1400,"corporation":false,"usgs":true,"family":"Horowitz","given":"Arthur","email":"horowitz@usgs.gov","middleInitial":"J.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":144363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57455,"text":"wdrMT841 - 1985 - Water resources data for Montana, water year 1984. Volume 1. Hudson Bay and Missouri River Basins","interactions":[],"lastModifiedDate":"2020-08-21T17:36:34.225153","indexId":"wdrMT841","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":"MT-84-1","title":"Water resources data for Montana, water year 1984. Volume 1. Hudson Bay and Missouri River Basins","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrMT841","usgsCitation":"Shields, R., Knapton, J.R., White, M.K., Jacobson, M., and Kasman, M., 1985, Water resources data for Montana, water year 1984. Volume 1. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcd87","contributors":{"authors":[{"text":"Shields, R.R.","contributorId":106916,"corporation":false,"usgs":true,"family":"Shields","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":257060,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knapton, J. 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R.","contributorId":84385,"corporation":false,"usgs":true,"family":"Knapton","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":257063,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, M. K.","contributorId":74395,"corporation":false,"usgs":true,"family":"White","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":257062,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jacobson, M.A.","contributorId":7279,"corporation":false,"usgs":true,"family":"Jacobson","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":257061,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kasman, M.L.","contributorId":85254,"corporation":false,"usgs":true,"family":"Kasman","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":257064,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":3027,"text":"wsp2256B - 1985 - Effects of low-level dams on the distribution of sediment, trace metals, and organic substances in the lower Schuylkill River basin, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-06T14:02:12","indexId":"wsp2256B","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":"2256","chapter":"B","title":"Effects of low-level dams on the distribution of sediment, trace metals, and organic substances in the lower Schuylkill River basin, Pennsylvania","docAbstract":"Heavy use of the Schuylkill River for municipal water supplies and a history of accidental spills and discharges of trace metals and organic substances have been a concern of State and local officials for many years. The U.S. Geological Survey, as part of their River Quality Assessment Program, developed a study to assess the occurrence and distribution of trace substances that pose a threat to human health and aquatic life. This report presents the results of the part of the study that evaluates the effects of low-level dams in the lower basin on the distribution and transport of sediment and trace substances. \r\n\r\nA combination of historical and current data were used in the assessment. Suspended-sediment data collected at several mainstem and tributary sites from 1954 to 1979 and sedimentation surveys of the six pools in the lower basin were used to define the sediment-transport characteristics of the river. These data provided a base for assessing the transport of trace substances, which are associated closely with riverbed sediments and suspended particles. Water and riverbed samples were collected for analyses of trace substances at numerous sites in the lower basin from 1978 to 1980. \r\n\r\nThe six dams on the river between Pottstown and Philadelphia have had a significant effect on the transport of sediment and trace substances. Between 1954 and 1970, more than 4.7 million cubic yards of sediment accumulated in the pools formed by the dams. The quantity of sediment deposited in the pools ranged from 150,000 cubic yards in Plymouth Pool to 1.6 million cubic yards in Fairmount Pool. The rate of accumulation in the pools was a function of pool size and geometry and the frequency of storms. About 35 percent of the total sediment discharged by the river was stored in the six pools from 1954 to 1970. Since 1970, the net change in sediment accumulation has been minimal. More than 24 percent of the sediment in Fairmount Pool in 1970 was scoured from the pool during Hurricane Agnes in 1972; however, total sediment accumulation returned to the 1970 level within 2 years. \r\n\r\nAnalyses of water samples showed that some trace substances are associated closely with particulate material transported by the river. The concentration of suspended and total cadmium, chromium, copper, lead, nickel, and zinc correlated well with the concentration of suspended sediment and suspended organic carbon. The average annual discharge of metals in suspension as a percentage of total average annual discharge ranged from 46 percent for nickel to 94 percent for lead for the Schuylkill River at Manayunk. The average annual discharge of each metal remained about the same or decreased between Pottstown and Philadelphia. Synoptic sampling of the inflow and outflow of several pools during storm runoff showed that the pools limit the transport of trace metals. More than 50 percent of the suspended copper transported by the river at Pottstown was deposited in Vincent Pool during the storm of May 12-15, 1980. Similar reductions were observed between Port Kennedy and Manayunk as the storm runoff passed through Norristown, Plymouth, and Flat Rock Pools. \r\n\r\nAnalyses of riverbed sediments showed that concentrations of trace substances were higher in sediments that included all particles finer than 0.062 millimeter than in sediments that included only particles finer than 0.016 millimeter. This suggests that medium and coarse silt particles or conglomerates of finer particles sorb as much or more trace constituents as the individual fine silts and clay particles. Concentrations of trace metals were as much as 90 percent higher in the sediments that included coarse silt. Concentrations of trace organic substances were several times higher in the sediments that included coarse silt than in sediments consisting of only fine silt or clay. \r\n\r\nSurficial and core samples of riverbed sediments were used to define the present and historical distribution of trace substances in ","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp2256B","usgsCitation":"Yorke, T.H., Stamer, J.K., and Pederson, G.L., 1985, Effects of low-level dams on the distribution of sediment, trace metals, and organic substances in the lower Schuylkill River basin, Pennsylvania: U.S. Geological Survey Water Supply Paper 2256, vii, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2256B.","productDescription":"vii, 53 p. :ill., maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":29858,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2256b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2256b/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ecc5","contributors":{"authors":[{"text":"Yorke, Thomas H.","contributorId":83109,"corporation":false,"usgs":true,"family":"Yorke","given":"Thomas","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stamer, John K.","contributorId":104481,"corporation":false,"usgs":true,"family":"Stamer","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":146170,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pederson, Gary L.","contributorId":81084,"corporation":false,"usgs":true,"family":"Pederson","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146168,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25508,"text":"wri844145 - 1985 - Fishery survey and related limnological conditions of Williams Lake, Hubbard County, Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T11:36:14","indexId":"wri844145","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":"84-4145","title":"Fishery survey and related limnological conditions of Williams Lake, Hubbard County, Minnesota","docAbstract":"Bluegill (Lepomis macrochirus), pumpkinseed sunfish (Lepomis gibbosus), largemouth bass (Micropterus salmoides), yellow perch (Perca flavescens) rock bass (Amploplites rupestris), black crappie (Pomozis nigromaculatus), and northern pike (Esox lucius) were found in Williams Lake, Hubbard County, Minnesota, during a fishery survey of the lake in late August 1982. The most abundant fish were the bluegills. These fish live in the large littoral zone of the lake; this zone underlies 55% of the surface area of the lake. The most ubiquitous benthic invertebrate in the littoral zone (amphipods) and the most abundant benthic invertebrate (chironomid larvae) were major food sources for the bluegill. Other organisms found in the stomach contents of fish collected in this survey were zooplankton, gastropods, Diptera larvae, odonates, terrestrial insects, and other fish. Daphnia were the only zooplankters of a diverse plankton community that were found in stomach contents. The abundance of fish other than bluegill was typical for a system in which northern pike is the major predator.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lakewood, CO","doi":"10.3133/wri844145","usgsCitation":"Taylor, W., LaBaugh, J.W., Freeberg, M., and Dowling, D., 1985, Fishery survey and related limnological conditions of Williams Lake, Hubbard County, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 84-4145, iv, 25 p., https://doi.org/10.3133/wri844145.","productDescription":"iv, 25 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":123645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4145/report-thumb.jpg"},{"id":54225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Hubbard County","otherGeospatial":"Williams Lake","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-95.1817,47.4124],[-94.6911,47.4106],[-94.6711,47.4103],[-94.6708,47.3225],[-94.6628,47.3221],[-94.6624,47.1498],[-94.6623,47.1429],[-94.664,46.9771],[-94.6554,46.9772],[-94.6597,46.8041],[-94.7856,46.8058],[-94.8752,46.8063],[-95.1643,46.8072],[-95.1646,46.9789],[-95.1713,46.9788],[-95.1724,47.049],[-95.1696,47.1496],[-95.1694,47.3238],[-95.1827,47.3241],[-95.1817,47.4124]]]},\"properties\":{\"name\":\"Hubbard\",\"state\":\"MN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef339","contributors":{"authors":[{"text":"Taylor, W.W.","contributorId":61002,"corporation":false,"usgs":true,"family":"Taylor","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":193984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaBaugh, J. W.","contributorId":23484,"corporation":false,"usgs":true,"family":"LaBaugh","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":193983,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Freeberg, M.H.","contributorId":71209,"corporation":false,"usgs":true,"family":"Freeberg","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":193985,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dowling, D.C.","contributorId":84796,"corporation":false,"usgs":true,"family":"Dowling","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":193986,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25515,"text":"wri844304 - 1985 - Geochemical controls on dissolved sodium in basalt aquifers of the Columbia Plateau, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"wri844304","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":"84-4304","title":"Geochemical controls on dissolved sodium in basalt aquifers of the Columbia Plateau, Washington","docAbstract":"Miocene basaltic aquifers of the Columbia Plateau are the principal source of water for agricultural, domestic, and municipal use in Washington State. Irrigation with groundwaters with relatively high sodium concentrations has been cause for concern in recent years, because of the tendency of such waters to reduce soil permeability. Chemical reactions involving groundwater and the basalts are the primary mechanisms responsible for the input of sodium to groundwater in the plateau. This conclusion is supported by the sequence of secondary alteration products found and by progressive changes in groundwater chemistry with depth and position along regional flow paths. Upgradient and shallow groundwaters have low sodium concentrations and sodium-adsorption ratios (SAR's), and are predominantly calcium sodium bicarbonate waters. Groundwaters from deeper and downgradient locations have higher sodium concentrations and SAR 's and are predominantly sodium bicarbonate water. Volcanic glass and cryptocrystalline matrix are the major sources of groundwater sodium, and are dissolved by a combination of silicate hydrolysis and dissolution by carbonic acid. Magnesium, iron, and calcium are removed from solution by the formation of an iron magnesium smectite, calcite , and amorphous iron oxyhydroxide. The addition of sodium, silicon, and potassium by dissolution of basalt exceeds their removal by the precipitation of secondary minerals, and their concentrations increase in the initial stages of this process. In later stages, these continued increases produce a water saturated with clinoptilolite and silica phases, and these begin to precipitate. While the timing of these processes is unclear, the mineralogy of secondary alteration and estimated cooling rates of the basalt flows suggest that observed alteration products formed primarily at low temperature, under conditions similar to those existing at the present time. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844304","usgsCitation":"Hearn, P., Steinkampf, W., Bortleson, G.C., and Drost, B., 1985, Geochemical controls on dissolved sodium in basalt aquifers of the Columbia Plateau, Washington: U.S. Geological Survey Water-Resources Investigations Report 84-4304, v, 38 p. :ill., maps (one col.) ;28 cm., https://doi.org/10.3133/wri844304.","productDescription":"v, 38 p. :ill., maps (one col.) ;28 cm.","costCenters":[],"links":[{"id":123433,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4304/report-thumb.jpg"},{"id":54231,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4304/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54232,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4304/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae499","contributors":{"authors":[{"text":"Hearn, P.P.","contributorId":18380,"corporation":false,"usgs":true,"family":"Hearn","given":"P.P.","affiliations":[],"preferred":false,"id":194007,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinkampf, W.C.","contributorId":8137,"corporation":false,"usgs":true,"family":"Steinkampf","given":"W.C.","affiliations":[],"preferred":false,"id":194006,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bortleson, Gilbert C.","contributorId":57472,"corporation":false,"usgs":true,"family":"Bortleson","given":"Gilbert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":194009,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Drost, B. W.","contributorId":38526,"corporation":false,"usgs":true,"family":"Drost","given":"B. W.","affiliations":[],"preferred":false,"id":194008,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":2532,"text":"wsp2232 - 1985 - Ground water in Utah's densely populated Wasatch Front area - The challenge and the choices","interactions":[],"lastModifiedDate":"2017-08-31T17:11:23","indexId":"wsp2232","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":"2232","title":"Ground water in Utah's densely populated Wasatch Front area - The challenge and the choices","docAbstract":"Utah's Wasatch Front area comprises about 4,000 square miles in the north-central part of the State. I n 1980, the area had a population of more than 1.1 million, or about 77 percent of Utah's total population. It contains several large cities, including Salt Lake City, Ogden, and Provo, and is commonly called Utah's urban corridor.
Most of the water supply for the Wasatch Front area comes from streams that originate in the Wasatch Range and nearby Uinta Mountains; however, ground water has played an important role in the economic growth of the area. The principal source of ground water is the unconsolidated fill (sedimentary deposits) in the valleys of the Wasatch Front area northern Juab, Utah, Goshen, and Salt Lake Valleys; the East Shore area (a valley area east of the Great Salt Lake), and the Bear River Bay area. Maximum saturated thickness of the fill in the principal ground-water reservoirs in these valleys exceeds 6,000 feet, and the estimated volume of water that can be withdrawn from just the upper 100 feet of the saturated fill is about 8 million acre-feet. In most places the water is fresh, containing less than 1,000 milligrams per liter of dissolved solids; in much of the Bear River Bay area and most of Goshen Valley (and locally in the other valleys), the water is slightly to moderately saline, with 1,000 to 10,000 milligrams per liter of dissolved solids.
The principal ground-water reservoirs receive recharge at an annual rate that is estimated to exceed 1 million acre-feet chiefly as seepage from consolidated rocks in the adjacent mountains from canals, ditches, and irrigated land, directly from precipitation, and from streams. Discharge during 1980 (which was chiefly from springs, seepage to streams, evapotranspiration, and withdrawal by wells) was estimated to be about 1.1 million acre-feet. Withdrawal from wells, which began within a few years after the arrival of the Mormon pioneers in the Salt Lake Valley in 1847, and had increased to about 320,000 acre-feet during 1979. Additional withdrawals from wells may cause water levels to decline, possibly leading to such problems as conflicts among water-right owners, increased pumping costs, land subsidence, and deterioration of ground-water quality. Some of these problems cannot be avoided if the principal ground-water reservoirs are to be fully used; however, management practices such as artificial ground-water recharge in intensivelypumped areas may help to alleviate those problems.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2232","usgsCitation":"Price, D., 1985, Ground water in Utah's densely populated Wasatch Front area - The challenge and the choices: U.S. Geological Survey Water Supply Paper 2232, vii, 71 p., https://doi.org/10.3133/wsp2232.","productDescription":"vii, 71 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":139112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2232/report-thumb.jpg"},{"id":28758,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2232/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Front","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dacb","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":145356,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25444,"text":"wri854111 - 1985 - Development and testing of highway storm-sewer flow measurement and recording system","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri854111","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":"85-4111","title":"Development and testing of highway storm-sewer flow measurement and recording system","docAbstract":"A comprehensive study and development of measuring instruments and techniques for measuring all components of flow in a storm-sewer drainage system was undertaken by the U.S. Geological Survey under the sponsorship of the Federal Highway Administration. The study involved laboratory and field calibration and testing of measuring flumes, pipe insert meters, weirs, electromagnetic velocity meters as well as the development and calibration of pneumatic-bubbler pressure transducer head measuring systems. Tracer-dilution and acoustic flow meter measurements were used in field verification tests. A single micrologger was used to record data from all the above instruments as well as from a tipping-bucket rain gage and also to activate on command the electromagnetic velocity meter and tracer-dilution systems. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri854111","usgsCitation":"Kilpatrick, F.A., Kaehrle, W., Hardee, J., Cordes, E.H., and Landers, M.N., 1985, Development and testing of highway storm-sewer flow measurement and recording system: U.S. Geological Survey Water-Resources Investigations Report 85-4111, xiii, 98 p. :ill. ;28 cm., https://doi.org/10.3133/wri854111.","productDescription":"xiii, 98 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118776,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4111/report-thumb.jpg"},{"id":54179,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4111/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db686725","contributors":{"authors":[{"text":"Kilpatrick, F. A.","contributorId":22319,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":193719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaehrle, W.R.","contributorId":17650,"corporation":false,"usgs":true,"family":"Kaehrle","given":"W.R.","affiliations":[],"preferred":false,"id":193718,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hardee, Jack","contributorId":99554,"corporation":false,"usgs":true,"family":"Hardee","given":"Jack","email":"","affiliations":[],"preferred":false,"id":193722,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cordes, E. H.","contributorId":49002,"corporation":false,"usgs":true,"family":"Cordes","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":193720,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Landers, M. N.","contributorId":63428,"corporation":false,"usgs":true,"family":"Landers","given":"M.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":193721,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":2522,"text":"wsp2274 - 1985 - Relation between ground-water quality and mineralogy in the coal-producing Norton Formation of Buchanan County, Virginia","interactions":[],"lastModifiedDate":"2022-02-22T22:19:03.367618","indexId":"wsp2274","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":"2274","title":"Relation between ground-water quality and mineralogy in the coal-producing Norton Formation of Buchanan County, Virginia","docAbstract":"The geochemical processes controlling ground-water chemistry in the coal-producing strata of southwestern Virginia include hydrolysis of silicates, dissolution of carbonates, oxidation of pyrite, cation exchange, and precipitation of secondary minerals, kaolinite and goethite. \r\n\r\nCore material from the Norton Formation of the Pennsylvania Period is composed of slightly more than one-half sandstone; siltstone and minor amounts of shale, clay, and coal account for the majority of the remainder. Petrographic analyses and x-ray diffraction studies indicate that the sandstone is about 75 percent quartz, 15 percent plagioclase feldspar, 2 percent potassium feldspar, 2 percent muscovite, 4 percent chlorite, and 1 percent siderite. Calcite is present in small amounts and in a few strata as clasts or cement. No limestone strata were identified. The siltstone is about 50 percent quartz, 10 percent plagioclase feldspar, 10 percent mica, 20 percent chlorite, and from 0 to 25 percent siderite. Pyrite is associated with some siltstone and, where present, generally accounts for less than 1 percent. Total sulfur generally constitutes less than 0.1 percent of core samples but about 4 percent in the more pyrite-rich layers. \r\n\r\nThree reaction models are used to account for the observed water chemistry. The models derive sulfate from pyrite, iron from pyrite and siderite, calcium from plagioclase and calcite, sodium from plagioclase and cation exchange, magnesium from chlorite, and carbon from carbon dioxide, calcite, and siderite. Kaolinite, chalcedony, and goethite are formed authigenically. Carbon-13 data define the relative contributions of carbon sources to models. \r\n\r\nComparison of adjacent unmined and mined basins indicates that surface mining significantly increases the weathering reaction of pyrite in contrast to weathering reactions of other minerals. However, in the area studied, reactive pyrite does not appear to be present in sufficient quantities in strata associated with mined coal seams to cause acid mine drainage.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2274","usgsCitation":"Powell, J.D., and Larson, J.D., 1985, Relation between ground-water quality and mineralogy in the coal-producing Norton Formation of Buchanan County, Virginia: U.S. Geological Survey Water Supply Paper 2274, iv, 30 p., https://doi.org/10.3133/wsp2274.","productDescription":"iv, 30 p.","costCenters":[],"links":[{"id":396293,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25416.htm"},{"id":28725,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2274/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138811,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2274/report-thumb.jpg"}],"country":"United States","state":"Virginia","county":"Buchanan County","otherGeospatial":"Norton Formation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.0830,\n 37.0500\n ],\n [\n -82.033,\n 37.0500\n ],\n [\n -82.033,\n 37.087\n ],\n [\n -82.0830,\n 37.087\n ],\n [\n -82.0830,\n 37.0500\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c32f","contributors":{"authors":[{"text":"Powell, John D.","contributorId":6045,"corporation":false,"usgs":true,"family":"Powell","given":"John","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":145339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larson, Jerry D.","contributorId":90703,"corporation":false,"usgs":true,"family":"Larson","given":"Jerry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":145340,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25526,"text":"wri854030 - 1985 - Geohydrology of rocks penetrated by test well USW H-4, Yucca Mountain, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:21","indexId":"wri854030","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":"85-4030","title":"Geohydrology of rocks penetrated by test well USW H-4, Yucca Mountain, Nye County, Nevada","docAbstract":"Test well USW H-4 is one of several wells drilled in the southwestern part of the Nevada Test Site for hydraulic testing, hydrologic monitoring, and geophysical logging. The work was performed in cooperation with the U.S. Department of Energy. The rocks penetrated by the well to a total depth of 1,219 m were volcanic tuffs of Tertiary age. Hydraulic coefficients calculated from pumping test data indicate that transmissivity ranged from 200 to 790 sq m/day. A radioactive tracer, borehole flow survey indicated that the two most productive zones during this borehole flow survey occurred in the upper part of the Bullfrog Member of the Crater Flat Tuff, depth interval from 721 to 731.5m, and in the underlying part of the Tram Member, depth interval from 864 to 920m. The water is predominantly a sodium biocarbonate type with small concentrations of calcium, magnesium, and sulfate. The apparent age of this composite water sample was determined by carbon-14 date of 17,200 years before present. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri854030","usgsCitation":"Whitfield, M., Eshom, E., Thordarson, W., and Schaefer, D.H., 1985, Geohydrology of rocks penetrated by test well USW H-4, Yucca Mountain, Nye County, Nevada: U.S. Geological Survey Water-Resources Investigations Report 85-4030, iv, 33 p. :ill., map ;28 cm., https://doi.org/10.3133/wri854030.","productDescription":"iv, 33 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":118981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4030/report-thumb.jpg"},{"id":54242,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a3f","contributors":{"authors":[{"text":"Whitfield, M.S.","contributorId":69547,"corporation":false,"usgs":true,"family":"Whitfield","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":194048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eshom, E.P.","contributorId":83127,"corporation":false,"usgs":true,"family":"Eshom","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":194049,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":194047,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Schaefer, D. H.","contributorId":84763,"corporation":false,"usgs":true,"family":"Schaefer","given":"D.","middleInitial":"H.","affiliations":[],"preferred":false,"id":194050,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":65642,"text":"i1760 - 1985 - Controlled photomosaics of the Sidon Flexus Region of Europa","interactions":[],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i1760","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":"1760","subseriesTitle":"NONE","title":"Controlled photomosaics of the Sidon Flexus Region of Europa","language":"ENGLISH","doi":"10.3133/i1760","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Controlled photomosaics of the Sidon Flexus Region of Europa: U.S. Geological Survey IMAP 1760, 2 remote-sensing images ;on sheets 78 x 59 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1760.","productDescription":"2 remote-sensing images ;on sheets 78 x 59 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":189245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101079,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1760/plate-1.pdf","size":"3349","linkFileType":{"id":1,"text":"pdf"}},{"id":101080,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1760/plate-2.pdf","size":"2420","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6865e4","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":534030,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65126,"text":"i1570 - 1985 - Geologic map and structure sections of the Dos Cabezas Quadrangle, Cochise County, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:05","indexId":"i1570","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":"1570","subseriesTitle":"NONE","title":"Geologic map and structure sections of the Dos Cabezas Quadrangle, Cochise County, Arizona","language":"ENGLISH","doi":"10.3133/i1570","usgsCitation":"Drewes, H., 1985, Geologic map and structure sections of the Dos Cabezas Quadrangle, Cochise County, Arizona: U.S. Geological Survey IMAP 1570, 1 map :col. ;49 x 58 cm., on sheet 99 x 111 cm., https://doi.org/10.3133/i1570.","productDescription":"1 map :col. ;49 x 58 cm., on sheet 99 x 111 cm.","costCenters":[],"links":[{"id":189928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":106811,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9320.htm","linkFileType":{"id":5,"text":"html"},"description":"9320"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.61749999999999,32.1175 ], [ -109.61749999999999,32.25 ], [ -109.5,32.25 ], [ -109.5,32.1175 ], [ -109.61749999999999,32.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a37f6","contributors":{"authors":[{"text":"Drewes, Harald","contributorId":52567,"corporation":false,"usgs":true,"family":"Drewes","given":"Harald","affiliations":[],"preferred":false,"id":272697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65511,"text":"i1673 - 1985 - Controlled photomosaic of the Mare Boreum I Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i1673","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":"1673","subseriesTitle":"NONE","title":"Controlled photomosaic of the Mare Boreum I Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1673","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Controlled photomosaic of the Mare Boreum I Quadrangle of Mars: U.S. Geological Survey IMAP 1673, 1 remote sensing image ;41 x 58 cm., on sheet 86 x 64 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1673.","productDescription":"1 remote sensing image ;41 x 58 cm., on sheet 86 x 64 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":251361,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1673/report.pdf","size":"24","linkFileType":{"id":1,"text":"pdf"}},{"id":251362,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1673/plate-1.pdf","size":"6740","linkFileType":{"id":1,"text":"pdf"}},{"id":252235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1673/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68819f","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":533898,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":13565,"text":"ofr85706 - 1985 - User's manual for MAPGEN (UNIX version); a method of transforming digital cartographic data to a map","interactions":[],"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr85706","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":"85-706","title":"User's manual for MAPGEN (UNIX version); a method of transforming digital cartographic data to a map","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85706","usgsCitation":"Evenden, G., and Botbol, J., 1985, User's manual for MAPGEN (UNIX version); a method of transforming digital cartographic data to a map: U.S. Geological Survey Open-File Report 85-706, ii, 140 p. ;28 cm., https://doi.org/10.3133/ofr85706.","productDescription":"ii, 140 p. ;28 cm.","costCenters":[],"links":[{"id":147182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0706/report-thumb.jpg"},{"id":42042,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0706/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603df3","contributors":{"authors":[{"text":"Evenden, G. I.","contributorId":52960,"corporation":false,"usgs":true,"family":"Evenden","given":"G. I.","affiliations":[],"preferred":false,"id":168032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Botbol, J.M.","contributorId":46944,"corporation":false,"usgs":true,"family":"Botbol","given":"J.M.","affiliations":[],"preferred":false,"id":168031,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":65510,"text":"i1668 - 1985 - Controlled photomosaic of the Mare Boreum D Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i1668","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":"1668","subseriesTitle":"NONE","title":"Controlled photomosaic of the Mare Boreum D Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1668","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Controlled photomosaic of the Mare Boreum D Quadrangle of Mars: U.S. Geological Survey IMAP 1668, 1 remote sensing image ;38 x 58 cm., on sheet 86 x 65 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1668.","productDescription":"1 remote sensing image ;38 x 58 cm., on sheet 86 x 65 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":251359,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1668/report.pdf","size":"24","linkFileType":{"id":1,"text":"pdf"}},{"id":251360,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1668/plate-1.pdf","size":"6938","linkFileType":{"id":1,"text":"pdf"}},{"id":252234,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1668/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68821a","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":533897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65509,"text":"i1667 - 1985 - Controlled photomosaic of the Mare Boreum C Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:18","indexId":"i1667","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":"1667","subseriesTitle":"NONE","title":"Controlled photomosaic of the Mare Boreum C Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1667","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Controlled photomosaic of the Mare Boreum C Quadrangle of Mars: U.S. Geological Survey IMAP 1667, 1 remote sensing image ;38 x 58 cm., on sheet 86 x 65 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1667.","productDescription":"1 remote sensing image ;38 x 58 cm., on sheet 86 x 65 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":260774,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1667/plate-1.pdf"},{"id":251358,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1667/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":252233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1667/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881b7","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":533896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":65508,"text":"i1703 - 1985 - Controlled photomosaic of the Mare Boreum A and B Regions of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:10","indexId":"i1703","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":"1703","subseriesTitle":"NONE","title":"Controlled photomosaic of the Mare Boreum A and B Regions of Mars","language":"ENGLISH","doi":"10.3133/i1703","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Controlled photomosaic of the Mare Boreum A and B Regions of Mars: U.S. Geological Survey IMAP 1703, 1 remote sensing image ;74 cm. in diam., on sheet 108 x 81 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1703.","productDescription":"1 remote sensing image ;74 cm. in diam., on sheet 108 x 81 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":251356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1703/report.pdf","size":"24","linkFileType":{"id":1,"text":"pdf"}},{"id":251357,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1703/plate-1.pdf","size":"12918","linkFileType":{"id":1,"text":"pdf"}},{"id":252232,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1703/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6881ae","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":533895,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55924,"text":"wdrNV851 - 1985 - Water resources data, Nevada, water year 1985","interactions":[],"lastModifiedDate":"2024-07-22T21:04:56.522018","indexId":"wdrNV851","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":"NV-85-1","title":"Water resources data, Nevada, water year 1985","docAbstract":"Water-resources data published herein for the 1984 water year comprise the following records:
o Water discharge for 89 gaging stations on streams, canals, and drains.
o Discharge data for 43 peak-flow stations, 2 low-flow stations on streams, and 41 springs.
o Stage and contents for 14 lakes and reservoirs.
o Water levels for 298 observation wells.
o Water-quality data for 23 stream, canal, and drain sites, 3 lake and reservoir sites, and 5 wells.
o Precipitation totals for 10 stations.
Additional water data, collected at various sites that are not part of the systematic data-collection program, are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Nevada.
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