{"pageNumber":"1526","pageRowStart":"38125","pageSize":"25","recordCount":46677,"records":[{"id":55694,"text":"wdrMI851 - 1986 - Water resources data for Michigan, water year 1985","interactions":[],"lastModifiedDate":"2017-08-10T14:42:09","indexId":"wdrMI851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"MI-85-1","title":"Water resources data for Michigan, water year 1985","docAbstract":"<p>Water resources data for the 1985 water year for Michigan consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels and water temperature of ground water. This report contains discharge records for 135 gaging stations; stage only records for 1 gaging station; stage and contents for 5 lakes and reservoirs; water-quality records for 52 gaging stations; water-level records for 53 observation wells; and water-temperature records for 6 observation wells. Also included are 52 crest-stage partial-record stations and 30 low-flow partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program. Miscellaneous data were collected at 41 measuring sites and 1 water-quality sampling site. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State, Local, and Federal agencies in Michigan.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMI851","usgsCitation":"Miller, J.B., Oberg, J., and Failing, J., 1986, Water resources data for Michigan, water year 1985: U.S. Geological Survey Water Data Report MI-85-1, ix, 297 p., https://doi.org/10.3133/wdrMI851.","productDescription":"ix, 297 p.","numberOfPages":"312","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":181913,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/mi-85-1/report-thumb.jpg"},{"id":344733,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/mi-85-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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B.","contributorId":70423,"corporation":false,"usgs":true,"family":"Miller","given":"J.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":254028,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oberg, J.L.","contributorId":54669,"corporation":false,"usgs":true,"family":"Oberg","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":254027,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Failing, J.C.","contributorId":76822,"corporation":false,"usgs":true,"family":"Failing","given":"J.C.","affiliations":[],"preferred":false,"id":254029,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":16099,"text":"ofr86166 - 1986 - U-Pb isotopic evidence for accretion of a continental microplate in the Zalm region of the Saudi Arabian Shield","interactions":[],"lastModifiedDate":"2015-09-02T18:49:06","indexId":"ofr86166","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-166","title":"U-Pb isotopic evidence for accretion of a continental microplate in the Zalm region of the Saudi Arabian Shield","docAbstract":"<p>The region covered by this work includes three of the main tectonic units of the Arabian Shield: the Afif continental terrane, the Nabitah suture with its associated mobile belt, and the Asir ensimatic arc terrane. The geology of the area is well understood, and this geochronologic and isotopic study confirms that the Afif terrane was a continental microplate in the late Proterozoic. The study also provides a time frame for the crustal evolution of this part of the Shield. U-Pb zircon age data from a pelitic garnet-sillimanite gneiss of the Kabid formation shows that this part of the continental basement in the Afif terrane may be as old as 1830 Ma. Isotope data indicate that lead from the Kabid gneiss resided in the upper continental crust for a long period before 1830 Ma, and require that Archean rocks exist at depth beneath the Afif terrane.</p>\n<p>Lead isotope data reveal a change in the nature of the underlying crust, from continental basement in the northeast, to less radiogenic, marginal arc rocks in the southwest. This change is coincident with both aeromagnetic data, and a fades change within a pre-collision marginal basin. Miogeosynclinal continental shelf fades of the Siham group lie unconcormably over the Kabid formation, and are in the area of continental lead signatures. Eugeosynclinal deep water sediments and volcanics, in association with ultramafic rocks, occur in the area of marginal arc signatures.</p>\n<p>U-Pb zircon age determinations show that this \"Andean\" continental margin developed before about 720 Ma, and emplacement of calc-alkaline plutonic rocks continued until about 690 Ma. During the period 690-640 Ma, the continental Afif microplate collided with the Asir terrane as part of the Nabitah orogeny. At approximately 640 Ma ago, the Najd strike-slip orogen commenced with a dextral phase that controlled the emplacement of granitic plutons as well as the development of a series of large pull-apart grabens. Some of these grabens were floored by new oceanic crust and were filled with volcano-sedimentary rocks of the Bani Ghayy group. Subsequently, the Najd fault system changed to sinistral strike slip motion at about 620 Ma ago.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr86166","usgsCitation":"Stacey, J.S., and Agar, R., 1986, U-Pb isotopic evidence for accretion of a continental microplate in the Zalm region of the Saudi Arabian Shield: U.S. Geological Survey Open-File Report 86-166, ii, 2p. :ill., map ;28 cm., https://doi.org/10.3133/ofr86166.","productDescription":"ii, 2p. :ill., map ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":149093,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0166/report-thumb.jpg"},{"id":45021,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0166/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"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              35,\n              28\n            ],\n            [\n              35,\n              16\n            ],\n            [\n              45,\n              16\n            ],\n            [\n              45,\n              28\n            ],\n            [\n              35,\n              28\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db62375f","contributors":{"authors":[{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":172232,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Agar, R.A.","contributorId":13645,"corporation":false,"usgs":true,"family":"Agar","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":172231,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15231,"text":"ofr86360 - 1986 - Summary of vitrinite reflectance and rock-eval pyrolysis data, Eagle Basin, northwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr86360","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-360","title":"Summary of vitrinite reflectance and rock-eval pyrolysis data, Eagle Basin, northwestern Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86360","usgsCitation":"Nuccio, V., Schenk, C.J., and Daws, T., 1986, Summary of vitrinite reflectance and rock-eval pyrolysis data, Eagle Basin, northwestern Colorado: U.S. Geological Survey Open-File Report 86-360, 5 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr86360.","productDescription":"5 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":146678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0360/report-thumb.jpg"},{"id":44179,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0360/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44180,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0360/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698893","contributors":{"authors":[{"text":"Nuccio, V. F.","contributorId":7713,"corporation":false,"usgs":true,"family":"Nuccio","given":"V. F.","affiliations":[],"preferred":false,"id":170782,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schenk, Christopher J. 0000-0002-0248-7305","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":72344,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":170784,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Daws, T.A.","contributorId":56651,"corporation":false,"usgs":true,"family":"Daws","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":170783,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14703,"text":"ofr86487 - 1986 - Hydrologic data for urban studies in the Houston metropolitan area, Texas, 1983","interactions":[],"lastModifiedDate":"2017-06-14T11:20:52","indexId":"ofr86487","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-487","title":"Hydrologic data for urban studies in the Houston metropolitan area, Texas, 1983","docAbstract":"<p>Hydro!ogic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in the Austin and Houston areas, and have been completed in the Dallas-Fort Worth and San Antonio areas.</p>\n<p>The U.S. Geological Survey, in cooperation with the city of Houston, began studies in the Houston metropolitan area in 1964. The program was expanded in 1968 to include collection of water-quality data. The objectives of the Houston urban-hydrology study are as follows:</p>\n<ol>\n<li>To determine, on the basis of historical data and hydrologic analyses, the magnitude and frequency of flood peaks and flood volumes.</li>\n<li>To determine the effect of urban development on flood peaks and volumes.</li>\n<li>To ascertain the variation in water quality for different flow conditions and different seasons.</li>\n</ol>\n<p>This report, the twentieth in a series of reports to be published annually, is primarily applicable to objective No. 2. The report presents hydrologic data collected in the Houston urban area for the 1983 water year (October 1, 1982, to September 30, 1983).</p>\n<p>A report by Johnson and Sayre (1973) utilized records collected from 1965 to 1969 to study the effects of urbanization on floods in the Houston area. That report also summarized various basin parameters. A report by Waddell, Massey, and Jennings (1979) presented data on runoff from the Houston area and computed concentrations and loads of selected water-quality constituents discharged to Galveston Bay. The study utilized a variation of the \"STORM\" model developed by the Hydrologic Engineering Center of the U.S. Army Corps of Engineers. A report prepared by Li scum and Massey (1980) presented a technique for estimating the magnitude and frequency of floods in the Houston area from drainage areas, bank-full conveyance, and percentage )f urban development.</p>\n<p>A definition of terms related to streamflow, water quality, and other hydrologic data, as used in this report, are defined in \" U.S. Geological Survey, Water-resources data for Texas, water year 1983, volume 2.\"</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr86487","collaboration":"Prepared in cooperation with the City of Houston","usgsCitation":"Liscum, F., 1986, Hydrologic data for urban studies in the Houston metropolitan area, Texas, 1983: U.S. Geological Survey Open-File Report 86-487, viii, 287 p., https://doi.org/10.3133/ofr86487.","productDescription":"viii, 287 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":30478,"text":"wri864320 - 1986 - Hydrologic and climatologic factors affecting water levels of Devils Lake, North Dakota","interactions":[],"lastModifiedDate":"2018-03-14T16:35:11","indexId":"wri864320","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-4320","title":"Hydrologic and climatologic factors affecting water levels of Devils Lake, North Dakota","docAbstract":"<p>High water levels of Devils Lake, North Dakota, and other terminal lakes, have, in recent years, threatened highways, agricultural land, recreational cabins, and communities located near these lakes. This study was undertaken to describe the hydrology of the Devils Lake basin and to determine how to estimate future water level probabilities. </p><p>Analysis of the available hydrologic and climatologic data indicates the water level of Devils Lake fluctuates largely in response to climatic variability. Average annual net storage gain has varied from 70 ,000 acre-feet for 1969-83 to as little as 4,530 acre-feet for 1931-40. In addition to the influence of climatic variability on the inflow to Devils Lake, an interconnected chain of lakes upstream of Devils Lake retains runoff and acts as an evaporation basin for runoff from the Devils Lake basin. During 1965-67, at least 112,000 acre-feet of water was stored in this upstream chain of lakes. </p><p>A review of research conducted on other terminal lakes indicated that the water level in these lakes fluctuated primarily in response to climate variability. There is agreement between water level fluctuations of terminal lakes in Western North America and water level fluctuations of Devils lake during times of climatic extremes. </p><p>No standardized methods are available for computing water level probabilities of terminal lakes. Most of the development of a method for determining future water level probabilities has been focused on Great Salt Lake, Utah. A number of techniques have been used to estimate the future water-level probabilities for Great Salt Lake; however, they provide a wide range in probability of occurrence for any given water level. (Author 's abstract)</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864320","usgsCitation":"Wiche, G.J., 1986, Hydrologic and climatologic factors affecting water levels of Devils Lake, North Dakota: U.S. Geological Survey Water-Resources Investigations Report 86-4320, iv, 62 p., https://doi.org/10.3133/wri864320.","productDescription":"iv, 62 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":59261,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4320/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4320/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611886","contributors":{"authors":[{"text":"Wiche, Gregg J. gjwiche@usgs.gov","contributorId":1675,"corporation":false,"usgs":true,"family":"Wiche","given":"Gregg","email":"gjwiche@usgs.gov","middleInitial":"J.","affiliations":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true}],"preferred":true,"id":203318,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29259,"text":"wri854099 - 1986 - Aquifer model of the Susquehanna River valley in southwestern Broome County, New York","interactions":[],"lastModifiedDate":"2019-08-16T13:58:00","indexId":"wri854099","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4099","title":"Aquifer model of the Susquehanna River valley in southwestern Broome County, New York","docAbstract":"<p>A finite-difference model of ground-water flow within stratified drift in the 14-mile reach of the Susquehanna River valley from Binghamton west to the Tioga County line (including Johnson City, Endicott, and Vestal) has been developed. Outwash is the most permeable and extensive type of stratified drift in the valley but has only small saturated thickness except where it is downwarped beneath ice-block depressions. The outwash is commonly underlain by extensive beds of silt and clay deposited in proglacial lakes. Older ice-contact deposits are also extensive and provide the largest yields to wells but are highly variable in thickness and commonly siltier than the outwash. The ice-contact deposits seem to occur mainly as ridges that parallel the axis of major valleys and are buried beneath later lacustrine and outwash sediments.</p><p>The model simulates horizontal flow in two layers; the upper layer generally represents outwash, and the lower layer generally represents older ice-contact deposits. The model also simulates vertical flow between those layers through the beds of silt and clay or, where the two aquifer layers are in direct contact, through sand and gravel.</p><p>The model has been calibrated to reproduce observed water levels that represent steady-state conditions. Aquifer properties, recharge from several sources, river stage, and pumpage from several municipal and industrial well fields were calculated from data collected largely in 1981. Major streams were treated as constant specified heads in the upper layer. Data are available to refine the calibration. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854099","usgsCitation":"Randall, A.D., 1986, Aquifer model of the Susquehanna River valley in southwestern Broome County, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4099, Report: vi, 38 p.; 4 Plates: 41.02 x 19.73 or smaller, https://doi.org/10.3133/wri854099.","productDescription":"Report: vi, 38 p.; 4 Plates: 41.02 x 19.73 or smaller","costCenters":[],"links":[{"id":58107,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4099/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58108,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4099/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4099/report-thumb.jpg"},{"id":58109,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4099/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58110,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4099/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366617,"rank":6,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4099/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","county":"Broome County","otherGeospatial":"Susquehanna River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.13250732421875,\n              42.00542768820574\n            ],\n            [\n              -75.84548950195312,\n              42.00542768820574\n            ],\n            [\n              -75.84548950195312,\n              42.188846538629164\n            ],\n            [\n              -76.13250732421875,\n              42.188846538629164\n            ],\n            [\n              -76.13250732421875,\n              42.00542768820574\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679f92","contributors":{"authors":[{"text":"Randall, Allan D. arandall@usgs.gov","contributorId":1168,"corporation":false,"usgs":true,"family":"Randall","given":"Allan","email":"arandall@usgs.gov","middleInitial":"D.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":201233,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15151,"text":"ofr86551H - 1986 - Earthquake data report, August 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:05","indexId":"ofr86551H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-551","chapter":"H","title":"Earthquake data report, August 1985","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86551H","usgsCitation":"National Earthquake Information Center, 1986, Earthquake data report, August 1985: U.S. Geological Survey Open-File Report 86-551, 275 p. ;28 cm., https://doi.org/10.3133/ofr86551H.","productDescription":"275 p. ;28 cm.","costCenters":[],"links":[{"id":148732,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0551h/report-thumb.jpg"},{"id":44070,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0551h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62ab35","contributors":{"authors":[{"text":"National Earthquake Information Center","contributorId":128066,"corporation":true,"usgs":false,"organization":"National Earthquake Information Center","id":528975,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13917,"text":"ofr85693 - 1986 - Availability of selected meteorological data in computer-based files of the U.S. Geological Survey, Montana, North Dakota, South Dakota, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:45","indexId":"ofr85693","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-693","title":"Availability of selected meteorological data in computer-based files of the U.S. Geological Survey, Montana, North Dakota, South Dakota, and Wyoming","docAbstract":"Meteorological data were located, acquired, and stored from selected stations in Montana and North Dakota coal regions and adjacent areas including South Dakota and Wyoming. Data that were acquired have potential use in small watershed modeling studies. Emphasis was placed on acquiring data that was collected during the period 1970 to the present (1984). A map shows the location and type of stations selected. A narration summarizing conventions used in acquiring and storing the meteorological data is provided along with the various retrieval options available. Individual station descriptions are followed by tables listing the meteorological variables collected, period of obtained record, percentage of data recovery, and the instruments used and their description. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85693","usgsCitation":"Link, B.L., and Cary, L.E., 1986, Availability of selected meteorological data in computer-based files of the U.S. Geological Survey, Montana, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Open-File Report 85-693, v, 36 p. :map ;28 cm., https://doi.org/10.3133/ofr85693.","productDescription":"v, 36 p. :map ;28 cm.","costCenters":[],"links":[{"id":146285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0693/report-thumb.jpg"},{"id":42587,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0693/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d85c","contributors":{"authors":[{"text":"Link, Brenda L.","contributorId":33971,"corporation":false,"usgs":true,"family":"Link","given":"Brenda","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":168633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cary, L. E.","contributorId":47369,"corporation":false,"usgs":true,"family":"Cary","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":168634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13889,"text":"ofr86268 - 1986 - VARMAG; a Fortran program to implement the variable-magnetization terrain-correction method for aeromagnetic data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr86268","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-268","title":"VARMAG; a Fortran program to implement the variable-magnetization terrain-correction method for aeromagnetic data","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86268","usgsCitation":"Grauch, V., 1986, VARMAG; a Fortran program to implement the variable-magnetization terrain-correction method for aeromagnetic data: U.S. Geological Survey Open-File Report 86-268, ii, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr86268.","productDescription":"ii, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":144448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0268/report-thumb.jpg"},{"id":42507,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0268/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d4d","contributors":{"authors":[{"text":"Grauch, V.J. 0000-0002-0761-3489","orcid":"https://orcid.org/0000-0002-0761-3489","contributorId":70362,"corporation":false,"usgs":true,"family":"Grauch","given":"V.J.","affiliations":[],"preferred":false,"id":168579,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13242,"text":"ofr86317 - 1986 - January 1986 water levels, and data related to water-level changes, western and south-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:56","indexId":"ofr86317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-317","title":"January 1986 water levels, and data related to water-level changes, western and south-central Kansas","docAbstract":"Hydrologic data related to water level measurements were made in observation wells in western and south-central Kansas. The measurements were made in midwinter when pumping was minimal and water levels had recovered, for the most part, from the effects of pumping during the previous irrigation season. Annual hydrologic data are provided for relating water-level changes from a ' base-reference year ' (predevelopment year), a year of abnormally large amounts of rainfall and minimum pumpage (1966 or 1974), and each of 7 consecutive years of measurement (1980-86). The ' base-reference year ' is designated as 1940 for the southwestern area, 1944 for the south-central area, and 1950 for the northwestern, west-central, and Equus beds areas. Data also are provided for relating the average annual water level changes, saturated thicknesses of the deposits, and percentage changes in saturated thickness. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86317","usgsCitation":"Dague, B., 1986, January 1986 water levels, and data related to water-level changes, western and south-central Kansas: U.S. Geological Survey Open-File Report 86-317, iv, 165 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86317.","productDescription":"iv, 165 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":146922,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0317/report-thumb.jpg"},{"id":41627,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0317/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f4069","contributors":{"authors":[{"text":"Dague, B.J.","contributorId":45723,"corporation":false,"usgs":true,"family":"Dague","given":"B.J.","affiliations":[],"preferred":false,"id":167458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30243,"text":"wri844262 - 1986 - Quality of ground water in southeastern and south-central Washington, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri844262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"84-4262","title":"Quality of ground water in southeastern and south-central Washington, 1982","docAbstract":"In 1982 groundwater was sampled at over 100 sites in the southeastern-south central region of Washington and analyzed for pH, specific conductance, and concentrations of fecal-coliform bacteria, major dissolved irons, and dissolved iron, manganese, and nitrate. Twenty percent of the samples were analyzed for concentrations of dissolved aluminum, arsenic, barium, cadmium, chromium, cooper, lead, mercury, selenium, silver, and zinc. The predominant water type was calcium bicarbonate. Some sodium bicarbonate water was found in samples from the Lower Yakima, Horse Heaven Hills, and Walla Walla-Tucannon subregions. Dissolved solids concentrations were typically less than 500 mg/L (milligrams per liter). Median iron and manganese concentrations were less than 20 micrograms/L except in the Palouse subregion, where the median concentration of iron was 200 micrograms/L and the median concentrations of manganese was 45 micrograms/L. Generally, trace-metal concentrations were also less than 10 micrograms/L except for barium, copper, and zinc. Nitrate concentrations were less than 1.0 mg/L in waters from half the wells sampled. Concentrations greater than 5.0 mg/L were found in areas of the Lower Yakima, Walla Walla-Tucannon and Hanford subregions. No fecal-coliform bacteria were detected. U.S. Environmental Protection Agency drinking water regulation limits were generally not exceeded, except for occasional high concentrations of nitrate or dissolved solids. The historical data for the region were evaluated for these same constituents. Quantitative differences were found, but the historical and 1982 data led to similar qualitative conclusions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844262","usgsCitation":"Turney, G.L., 1986, Quality of ground water in southeastern and south-central Washington, 1982: U.S. Geological Survey Water-Resources Investigations Report 84-4262, v, 158 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri844262.","productDescription":"v, 158 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159823,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4262/report-thumb.jpg"},{"id":59020,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59021,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59022,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59023,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59024,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1984/4262/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59025,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4262/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c012","contributors":{"authors":[{"text":"Turney, G. L.","contributorId":95070,"corporation":false,"usgs":true,"family":"Turney","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15234,"text":"ofr86427 - 1986 - Analytical and stratigraphic data on the Retort Phosphatic Shale Member of the Phosphoria Formation in the Hawley Creek area, Lehmi County, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr86427","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-427","title":"Analytical and stratigraphic data on the Retort Phosphatic Shale Member of the Phosphoria Formation in the Hawley Creek area, Lehmi County, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86427","usgsCitation":"Oberlindacher, H., and Hovland, R.D., 1986, Analytical and stratigraphic data on the Retort Phosphatic Shale Member of the Phosphoria Formation in the Hawley Creek area, Lehmi County, Idaho: U.S. Geological Survey Open-File Report 86-427, 12 p. :map ;28 cm., https://doi.org/10.3133/ofr86427.","productDescription":"12 p. :map ;28 cm.","costCenters":[],"links":[{"id":146741,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0427/report-thumb.jpg"},{"id":44182,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0427/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f4e8","contributors":{"authors":[{"text":"Oberlindacher, H.P.","contributorId":44928,"corporation":false,"usgs":true,"family":"Oberlindacher","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":170788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hovland, R. D.","contributorId":17620,"corporation":false,"usgs":false,"family":"Hovland","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":7217,"text":"Bureau of Land Management","active":true,"usgs":false}],"preferred":false,"id":170787,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15182,"text":"ofr8673 - 1986 - Dissolved-selenium data for wells in the western San Joaquin Valley, California, February to July 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:07:00","indexId":"ofr8673","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-73","title":"Dissolved-selenium data for wells in the western San Joaquin Valley, California, February to July 1985","docAbstract":"Water samples were collected for selenium analysis from 63 wells in western San Joaquin Valley, California, during February to July 1985. Results of the data collection indicate that dissolved selenium concentrations ranged from less than 1 to 120 micrograms per liter; more than 50 percent of the wells sampled had concentrations of less than 1 microgram per liter. Four additional samples collected from public supply wells in the western valley had concentrations ranging from less than 1 to 2 micrograms per liter. All samples from five public supply wells east of the study area had concentrations less than 1 microgram per liter. The U.S. Environmental Protection Agency 's drinking-water standard of 10 micrograms per liter for selenium was slightly exceeded in 2 of 39 domestic wells (11 and 13 micrograms per liter) and substantially exceeded in 2 of 11 irrigation and agricultural wells (55 and 120 micrograms per liter). (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8673","usgsCitation":"Neil, J.M., 1986, Dissolved-selenium data for wells in the western San Joaquin Valley, California, February to July 1985: U.S. Geological Survey Open-File Report 86-73, iv, 10 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr8673.","productDescription":"iv, 10 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":148214,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0073/report-thumb.jpg"},{"id":44096,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0073/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3a1","contributors":{"authors":[{"text":"Neil, J. M.","contributorId":27464,"corporation":false,"usgs":true,"family":"Neil","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":170700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14711,"text":"ofr86200 - 1986 - BASIC program to reduce audio-magnetotelluric data and calculate apparent resistivity","interactions":[],"lastModifiedDate":"2012-02-02T00:06:58","indexId":"ofr86200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-200","title":"BASIC program to reduce audio-magnetotelluric data and calculate apparent resistivity","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86200","usgsCitation":"Long, C.L., and Pierce, H.A., 1986, BASIC program to reduce audio-magnetotelluric data and calculate apparent resistivity: U.S. Geological Survey Open-File Report 86-200, 17 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86200.","productDescription":"17 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":148128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0200/report-thumb.jpg"},{"id":43476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ae21","contributors":{"authors":[{"text":"Long, C. L.","contributorId":98699,"corporation":false,"usgs":true,"family":"Long","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":169890,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, H. A.","contributorId":99951,"corporation":false,"usgs":true,"family":"Pierce","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":169891,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14705,"text":"ofr86417 - 1986 - Laboratory measurements of velocity-dependent frictional strength","interactions":[],"lastModifiedDate":"2012-02-02T00:07:03","indexId":"ofr86417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-417","title":"Laboratory measurements of velocity-dependent frictional strength","docAbstract":"Water levels, location, depths, and aquifers tapped are given for 113 observation wells in Michigan. Tabulated data include extremes of water levels for 1985 and for the period of record, pumpage of most major groundwater users in the state, and water quality data from selected wells. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86417","usgsCitation":"Lockner, D., and Byerlee, J., 1986, Laboratory measurements of velocity-dependent frictional strength: U.S. Geological Survey Open-File Report 86-417, 84 p. :ill. ;28 cm., https://doi.org/10.3133/ofr86417.","productDescription":"84 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":147607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0417/report-thumb.jpg"},{"id":43473,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0417/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47fde4b07f02db4c98dc","contributors":{"authors":[{"text":"Lockner, D.A. 0000-0001-8630-6833","orcid":"https://orcid.org/0000-0001-8630-6833","contributorId":85603,"corporation":false,"usgs":true,"family":"Lockner","given":"D.A.","affiliations":[],"preferred":false,"id":169879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":169878,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30246,"text":"wri854254 - 1986 - Water quality of selected lakes in Mount Rainier National Park, Washington with respect to lake acidification","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri854254","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4254","title":"Water quality of selected lakes in Mount Rainier National Park, Washington with respect to lake acidification","docAbstract":"Thirteen lakes in Mount Rainier National Park were evaluated for general chemical characteristics, sensitivity to acidification by acidic precipitation, and degree of existing acidification. The lakes studies were Allen, one of the Chenuis group, Crescent , Crystal, Eleanor, Fan, one of the Golden group, Marsh, Mowich, Mystic, Shriner, and two unnamed lakes. The lakes were sampled in August 1983. Specific conductance values were generally 21 microsiemens/cm at 25 C or less, and dissolved solids concentrations were generally 20 mg/L or less. The major cations were calcium and sodium, and the major anion was bicarbonate. Alkalinity concentrations ranged from 2.1 to 9.0 mg/L in 12 of the lakes. Allen Lake was the exception, having an alkalinity concentration of 27 mg/L. The pH values for all of the lakes ranged from 5.8 to 6.5. In most of the lakes, vertical profiles of temperature, dissolved oxygen, pH, and specific conductance were relatively uniform. In the deeper lakes, temperature decreased with depth and dissolved-oxygen concentrations increased to about 20 feet, remained constant to 80 ft, then decreased with increasing depth. Exceptions to general water quality patterns were observed in three lakes. Allen Lake had a specific conductance value of 58 Microsiemens/cm. The lake of the Golden group was anaerobic at the bottom and had relatively high concentrations of dissolved organic carbon and dissolved metals, and a lower light transmission than the other lakes studied. One of the unnamed lakes had relatively high concentrations of phytoplankton and dissolved organic carbon and relatively low levels of light transmission. Comparisons of lake data to acid-sensitivity thresholds for specific conductance and alkalinity indicated that all of the lakes except Allen would be sensitive to acidic precipitation. The small sizes of the lakes, and their locations in basins of high precipitation and weathering-resistant rock types, enhance their sensitivity. None of the lakes in this study appeared to be presently acidified. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854254","usgsCitation":"Turney, G.L., Dion, N.P., and Sumioka, S.S., 1986, Water quality of selected lakes in Mount Rainier National Park, Washington with respect to lake acidification: U.S. Geological Survey Water-Resources Investigations Report 85-4254, v, 45 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854254.","productDescription":"v, 45 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4254/report-thumb.jpg"},{"id":59035,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4254/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bc963","contributors":{"authors":[{"text":"Turney, G. L.","contributorId":95070,"corporation":false,"usgs":true,"family":"Turney","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":202927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dion, N. P.","contributorId":33302,"corporation":false,"usgs":true,"family":"Dion","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":202926,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sumioka, S. S.","contributorId":20747,"corporation":false,"usgs":true,"family":"Sumioka","given":"S.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":202925,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60997,"text":"mf1856 - 1986 - Seismicity map of the state of Utah","interactions":[],"lastModifiedDate":"2017-05-11T14:38:38","indexId":"mf1856","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1856","title":"Seismicity map of the state of Utah","docAbstract":"<p>This map is one of a series of seismicity maps produced by the U. S. Geological Survey that show earthquake data of individual states or groups of states at the scale of 1:1,000,000. This map shows only those earthquakes with epicenters located within the boundaries of Utah, even though earthquakes in nearby states or countries may have been felt or may have caused damage in Utah.</p><p>The data in table 1 were used to compile the seismicity map; these data are a corrected, expanded, and updated (through 1982) version of the data used by Algermissen (1969) for a study of seismic risk in the United States. The locations and intensities of some earthquakes were revised and intensities were assigned where none had been before. Many earthquakes were added to the original list from new data sources as well as from some old data sources that had not been previously used. The data in table 1 represent best estimates of the location of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for earthquakes that occurred before seismic instruments were universally used.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1856","usgsCitation":"Stover, C.W., Reagor, B., and Algermissen, S.T., 1986, Seismicity map of the state of Utah: U.S. Geological Survey Miscellaneous Field Studies Map 1856, 57.79 x 38.29 inches, https://doi.org/10.3133/mf1856.","productDescription":"57.79 x 38.29 inches","costCenters":[],"links":[{"id":341151,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1856/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1856/mf1856.JPG"}],"country":"United States","state":"Utah","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"47\",\"properties\":{\"name\":\"Utah\",\"nation\":\"USA  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C. W.","contributorId":70369,"corporation":false,"usgs":true,"family":"Stover","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":264799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reagor, B.G.","contributorId":99121,"corporation":false,"usgs":true,"family":"Reagor","given":"B.G.","affiliations":[],"preferred":false,"id":264800,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Algermissen, S. T.","contributorId":39790,"corporation":false,"usgs":true,"family":"Algermissen","given":"S.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":264798,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57457,"text":"wdrMT851 - 1986 - Water resources data, Montana, water year 1985; Volume 1. Hudson Bay Basin, Missouri River Basin","interactions":[],"lastModifiedDate":"2023-02-10T16:38:48.392523","indexId":"wdrMT851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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-85-1","title":"Water resources data, Montana, water year 1985; Volume 1. Hudson Bay Basin, Missouri River Basin","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with State and other Federal agencies, obtain a large amount of data pertaining to the water resources of Montana each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved under-standing of the water resources of the State. To make these data readily available to interested parties outside the Geological Survey, the data are published annually in this report series entitled, \"Water Resources Data, Montana.\"</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMT851","collaboration":"Prepared in cooperation with the State of Montana and with other agencies","usgsCitation":"Shields, R., Knapton, J.R., White, M.K., Brosten, T., and Kasman, M., 1986, Water resources data, Montana, water year 1985; Volume 1. Hudson Bay Basin, Missouri River Basin: U.S. Geological Survey Water Data Report MT-85-1, xvi, 483 p., https://doi.org/10.3133/wdrMT851.","productDescription":"xvi, 483 p.","costCenters":[],"links":[{"id":412960,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/mt-85-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181804,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/mt-85-1/report-thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Hudson Bay Basin, Missouri River 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,{"id":27002,"text":"wri854171 - 1986 - Water-quality appraisal of NASQAN stations below impoundments, eastern Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri854171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"85-4171","title":"Water-quality appraisal of NASQAN stations below impoundments, eastern Tennessee","docAbstract":"The National Stream Quality Accounting Network (NASQAN) is a network of stations at which systematic and continuing water quality data are collected. Major objectives of this U.S. Geological Survey program are: (1) to depict areal variability of streamflow and water quality conditions nationwide on a year-by-year basis and (2) to detect long-term changes in streamflow and stream quality. Several NASQAN stations in East Tennessee are downstream from impoundments which have a significant effect on water quality. NASQAN data obtained from the Tennessee River below Watts Bar Dam and the Clinch River below Melton Hill Dam were compared to water quality data from the basins upstream. The comparison indicates that NASQAN data obtained below impoundments may not be adequate to describe a composite picture of water quality in the accounting unit. Detention time of storage in the impoundments is believed to moderate the range of constituent values observed at the NASQAN stations. Data obtained upstream and downstream from Watts Bar Dam indicate that the water sampled at the NASQAN station comes from stratified layers of the impoundment and is not representative of an integrated sample of water from the impoundment. Values of total recoverable iron suggest that, because of adsorption onto sediments in impoundments, some constituents are not accurately described by sampling below impoundments. Relations between water quality constituents and flow at stations on the Clinch River and Tennessee River are not well defined due to regulation. Direct load computations for many constituents were therefore not possible, which diminished the utility of data from these NASQAN stations to account for quantity versus quality of the water. Load computations were only possible for ionic constituents through use of a continuous specific conductance record as an intermediary. Rivers might reflect the decreasing trend in discharge during the 1972-82 water years. Thus the stations below Watts Bar Dam and below Melton Hill Dam do not adequately meet the NASQAN objective to detect and assess long-term changes in stream quality. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854171","usgsCitation":"Evaldi, R., and Lewis, J., 1986, Water-quality appraisal of NASQAN stations below impoundments, eastern Tennessee: U.S. Geological Survey Water-Resources Investigations Report 85-4171, v, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854171.","productDescription":"v, 50 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2180,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri85-4171","linkFileType":{"id":5,"text":"html"}},{"id":124347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4171/report-thumb.jpg"},{"id":55889,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4171/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4870","contributors":{"authors":[{"text":"Evaldi, R. D.","contributorId":93909,"corporation":false,"usgs":true,"family":"Evaldi","given":"R. D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":197390,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, J.G.","contributorId":32570,"corporation":false,"usgs":true,"family":"Lewis","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":197389,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60974,"text":"mf1857_1986 - 1986 - Seismicity map of the state of Idaho","interactions":[{"subject":{"id":60974,"text":"mf1857_1986 - 1986 - Seismicity map of the state of Idaho","indexId":"mf1857_1986","publicationYear":"1986","noYear":false,"title":"Seismicity map of the state of Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":60975,"text":"mf1857 - 1991 - Seismicity map of the state of Idaho","indexId":"mf1857","publicationYear":"1991","noYear":false,"title":"Seismicity map of the state of Idaho"},"id":1}],"supersededBy":{"id":60975,"text":"mf1857 - 1991 - Seismicity map of the state of Idaho","indexId":"mf1857","publicationYear":"1991","noYear":false,"title":"Seismicity map of the state of Idaho"},"lastModifiedDate":"2017-05-11T13:55:04","indexId":"mf1857_1986","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1857","title":"Seismicity map of the state of Idaho","docAbstract":"<p>This map is one of a series of seismicity maps produced by the U.S. Geological Survey that show earthquake data of individual states or groups of states at the scale of 1:1,000,000. This map shows only those earthquakes with epicenters located within the boundaries of Idaho, even though earthquakes in nearby states or countries may have been felt or may have caused damage in Idaho. The USGS and the Idaho Geological Survey are continuing to research historical data with the objective of improving the pre-instrumental data listed below.</p><p>The data in table 1 were used to compile the seismicity map; these data are a corrected, expanded, and updated (through 1983) version of the data used by Algermissen (1969) for a study of seismic risk in the United States. The locations and intensities of some earthquakes were revised and intensities were assigned where none had been before. Many earthquakes were added to the original list from new data sources as well as from some old data sources that had not been previously used. The data in table 1 represent earthquake on the basis of historical and current information. Some of the aftershocks from large earthquake are listed, but not all, especially for earthquakes that occurred before seismic instruments were universally used.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1857_1986","usgsCitation":"Stover, C.W., Reagor, B., and Algermissen, S.T., 1986, Seismicity map of the state of Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 1857, 55.70 x 41.37 inches, https://doi.org/10.3133/mf1857_1986.","productDescription":"55.70 x 41.37 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":186904,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1857_1986/mf1857_1986.JPG"},{"id":341132,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1857_1986/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":57527,"text":"wdrAR851 - 1986 - Water resource data--Arkansas, water year 1985","interactions":[],"lastModifiedDate":"2020-09-15T20:02:26.621313","indexId":"wdrAR851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"AR-85-1","title":"Water resource data--Arkansas, water year 1985","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrAR851","usgsCitation":"Lamb, T., Porter, J., Lambert, B., and Edds, J., 1986, Water resource data--Arkansas, water year 1985: U.S. Geological Survey Water Data Report AR-85-1, viii, 523 p., https://doi.org/10.3133/wdrAR851.","productDescription":"viii, 523 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,{"id":14957,"text":"ofr8669 - 1986 - Discharge and water quality of Horse Creek, southeastern Wyoming, May-November, 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr8669","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-69","title":"Discharge and water quality of Horse Creek, southeastern Wyoming, May-November, 1985","docAbstract":"This report presents stream-discharge and water-quality data collected at five sites in the lower Horse Creek drainage of southeastern Wyoming, May through November, 1985. Data include stream-discharge measurements; field measurements of specific conductance, pH, and water temperature; and computer changes in stream discharge. Measured discharge in Horse Creek ranged from 0.91 to 172 cu ft/sec. Values of pH averaged 8.4. Water temperature ranged from 0 to 27 C. The data are presented in graphs and tables. A map of the study reach shows the location of the data collection sites. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8669","usgsCitation":"Meyer, J., and Lenfest, L., 1986, Discharge and water quality of Horse Creek, southeastern Wyoming, May-November, 1985: U.S. Geological Survey Open-File Report 86-69, iv, 16 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8669.","productDescription":"iv, 16 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0069/report-thumb.jpg"},{"id":43771,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0069/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aac0","contributors":{"authors":[{"text":"Meyer, J.F.","contributorId":39793,"corporation":false,"usgs":true,"family":"Meyer","given":"J.F.","affiliations":[],"preferred":false,"id":170315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lenfest, L.W. Jr.","contributorId":54604,"corporation":false,"usgs":true,"family":"Lenfest","given":"L.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":170316,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1712,"text":"wsp2269 - 1986 - Traveltime and longitudinal dispersion in Illinois streams","interactions":[{"subject":{"id":9201,"text":"ofr84468 - 1984 - Traveltime and longitudinal dispersion in Illinois streams","indexId":"ofr84468","publicationYear":"1984","noYear":false,"title":"Traveltime and longitudinal dispersion in Illinois streams"},"predicate":"SUPERSEDED_BY","object":{"id":1712,"text":"wsp2269 - 1986 - Traveltime and longitudinal dispersion in Illinois streams","indexId":"wsp2269","publicationYear":"1986","noYear":false,"title":"Traveltime and longitudinal dispersion in Illinois streams"},"id":1}],"lastModifiedDate":"2022-09-19T18:32:36.31144","indexId":"wsp2269","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"2269","title":"Traveltime and longitudinal dispersion in Illinois streams","docAbstract":"Twenty-seven measurements of traveltime and longitudinal dispersion in 10 Illinois streams made from 1975 to 1982 provide data needed for estimating traveltime of peak concentration of a conservative solute, traveltime of the leading edge of a solute cloud, peak concentration resulting from injection of a given quantity of solute, and passage time of solute past a given point on a stream. These four variables can be estimated graphically for each stream from distance of travel and either discharge at the downstream end of the reach or flow-duration frequency. From equations developed from field measurements, the traveltime and dispersion characteristics also can be estimated for other unregulated streams in Illinois that have drainage areas less than about 1,500 square miles. For unmeasured streams, traveltime of peak concentration and of the leading edge of the cloud are related to discharge at the downstream end of the reach and to distance of travel. For both measured and unmeasured streams, peak concentration and passage time are best estimated from the relation of each to traveltime. In measured streams, dispersion efficiency is greater than that predicted by Fickian diffusion theory. The rate of decrease in peak concentration with traveltime is about equal to the rate of increase in passage time. Average velocity in a stream reach, given by the velocity of the center of solute mass in that reach, can be estimated from an equation developed from measured values. The equation relates average reach velocity to discharge at the downstream end of the reach. Average reach velocities computed for 9 of the 10 streams from available equations that are based on hydraulic-geometry relations are high relative to measured values. The estimating equation developed from measured velocities provides estimates of average reach velocity that are closer to measured velocities than are those computed using equations developed from hydraulic-geometry relations.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2269","usgsCitation":"Graf, J.B., 1986, Traveltime and longitudinal dispersion in Illinois streams: U.S. Geological Survey Water Supply Paper 2269, vi, 65 p., https://doi.org/10.3133/wsp2269.","productDescription":"vi, 65 p.","costCenters":[],"links":[{"id":406991,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25457.htm","linkFileType":{"id":5,"text":"html"}},{"id":26788,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2269/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2269/report-thumb.jpg"}],"country":"United 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,{"id":25723,"text":"wri824091 - 1986 - Preliminary delineation and description of the regional aquifers of Tennessee: the East Tennessee aquifer system","interactions":[],"lastModifiedDate":"2022-12-21T22:56:36.359639","indexId":"wri824091","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"82-4091","title":"Preliminary delineation and description of the regional aquifers of Tennessee: the East Tennessee aquifer system","docAbstract":"<p>The east Tennessee aquifer system occurs in the Valley and Ridge and the Blue Ridge provinces of Tennessee. These areas are underlain by rocks of Precambrian to Pennsylvanian age which have been structurally deformed and faulted during the Appalachian orogeny. Groundwater in the Valley and Ridge occurs primarily in solution openings in carbonate rocks and in fractures in sandstone and shale. Fractures in the crystalline rocks store and transmit most of the groundwater in the Blue Ridge province. The east Tennessee aquifer system is important as a source of rural and municipal drinking water. Within 300 ft of land surface, groundwater generally contains less than 500 milligrams/L dissolved solids. At greater depths, fractures and solution openings are smaller and fewer in number. There are very little data to define groundwater occurrence at depths greater than about 300 ft. Groundwater flow may be restricted and the dissolved solids concentrations in the groundwater may reach thousands or even ten thousands of milligrams/L.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824091","usgsCitation":"Brahana, J., Mulderink, D., Macy, J.A., and Bradley, M.W., 1986, Preliminary delineation and description of the regional aquifers of Tennessee: the East Tennessee aquifer system: U.S. Geological Survey Water-Resources Investigations Report 82-4091, iv, 30 p., https://doi.org/10.3133/wri824091.","productDescription":"iv, 30 p.","costCenters":[],"links":[{"id":156170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410909,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35602.htm","linkFileType":{"id":5,"text":"html"}},{"id":1854,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri824091","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Tennessee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -85.5,\n              36.594\n            ],\n            [\n              -85.5,\n              35\n            ],\n            [\n              -81.667,\n              35\n            ],\n            [\n              -81.667,\n              36.594\n            ],\n            [\n              -85.5,\n              36.594\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6c3","contributors":{"authors":[{"text":"Brahana, J. V.","contributorId":32926,"corporation":false,"usgs":true,"family":"Brahana","given":"J. V.","affiliations":[],"preferred":false,"id":194802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mulderink, Dolores","contributorId":64667,"corporation":false,"usgs":true,"family":"Mulderink","given":"Dolores","email":"","affiliations":[],"preferred":false,"id":194804,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Macy, J. A.","contributorId":10047,"corporation":false,"usgs":true,"family":"Macy","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194801,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bradley, M. W.","contributorId":40610,"corporation":false,"usgs":true,"family":"Bradley","given":"M.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":194803,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25721,"text":"wri82762 - 1986 - Preliminary delineation and description of the regional aquifers of Tennessee: Basal sandstone west of the Valley and Ridge Province","interactions":[],"lastModifiedDate":"2022-12-21T22:49:29.850891","indexId":"wri82762","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"82-762","title":"Preliminary delineation and description of the regional aquifers of Tennessee: Basal sandstone west of the Valley and Ridge Province","docAbstract":"The basal sandstone is a poorly sorted, well indurated sandstone, which lies below the Conasauga Group and above the Precambrian crystalline rocks. It is an unknown resource defined by limited data, with only 14 data points (wells) for the entire State of Tennessee. The basal sandstone is thought to occur throughout most of the State west of the Valley and Ridge province at depths of generally more than 5,500 feet below land surface. The basal sandstone probably does not receive significant vertical recharge because the sandstone is overlain by such a thick sequence of flat-lying, low-porosity lower Paleozoic carbonates and shales. Data from two sites indicate that the rocks of the basal sandstone have relatively low porosity and permeability.\r\n\r\nThe concentrations of dissolved solids in water from the basal sandstone range from less than 40,000 milligrams per liter to more than 200,000 milligrams per liter. The basal sandstone is not being used as a source of drinking water because of its great depth, the presence of shallower sources of drinking water, and possible concentrations of more than 10,000 milligrams per liter dissolved solids throughout its area of occurrence.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri82762","usgsCitation":"Brahana, J., Bradley, M., Macy, J.A., and Mulderink, D., 1986, Preliminary delineation and description of the regional aquifers of Tennessee: Basal sandstone west of the Valley and Ridge Province: U.S. Geological Survey Water-Resources Investigations Report 82-762, iv, 21 p., https://doi.org/10.3133/wri82762.","productDescription":"iv, 21 p.","costCenters":[],"links":[{"id":156685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":1837,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri82-0762","linkFileType":{"id":5,"text":"html"}},{"id":410907,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35646.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Tennessee","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.5,\n              36.712\n            ],\n            [\n              -89.5,\n              35\n            ],\n            [\n              -84,\n              35\n            ],\n            [\n              -84,\n              36.712\n            ],\n            [\n              -89.5,\n              36.712\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b2a9","contributors":{"authors":[{"text":"Brahana, J. V.","contributorId":32926,"corporation":false,"usgs":true,"family":"Brahana","given":"J. V.","affiliations":[],"preferred":false,"id":194794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradley, Mike 0000-0002-2979-265X mbradley@usgs.gov","orcid":"https://orcid.org/0000-0002-2979-265X","contributorId":582,"corporation":false,"usgs":true,"family":"Bradley","given":"Mike","email":"mbradley@usgs.gov","affiliations":[{"id":581,"text":"Tennessee Water Science Center","active":true,"usgs":true},{"id":24708,"text":"Lower Mississippi-Gulf Water Science Center","active":true,"usgs":true}],"preferred":true,"id":194793,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Macy, Jo Ann","contributorId":107314,"corporation":false,"usgs":true,"family":"Macy","given":"Jo","email":"","middleInitial":"Ann","affiliations":[],"preferred":false,"id":194796,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mulderink, Dolores","contributorId":64667,"corporation":false,"usgs":true,"family":"Mulderink","given":"Dolores","email":"","affiliations":[],"preferred":false,"id":194795,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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