{"pageNumber":"353","pageRowStart":"8800","pageSize":"25","recordCount":11004,"records":[{"id":70011225,"text":"70011225 - 1983 - Strain accumulation along the San Andreas fault system east of San Francisco Bay, California","interactions":[],"lastModifiedDate":"2025-08-27T16:49:29.58543","indexId":"70011225","displayToPublicDate":"2003-04-08T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Strain accumulation along the San Andreas fault system east of San Francisco Bay, California","docAbstract":"<p><span>The occurrence of several large earthquakes to the east of San Francisco Bay during historical times, and present high levels of microseismicity, indicate that a significant part of the relative plate motion may be occurring east of San Francisco Bay. Furthermore, the Hayward fault is known to be slipping aseismically at the surface, and the Calaveras fault may be slipping aseismically also. These facts raise an important question: Is the observed creep rate accommodating all of the east bay deformation or is there a significant amount of strain accumulating along these faults?</span></p><div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id4\" class=\"abstract author\"><div id=\"aep-abstract-sec-id5\"><div class=\"u-margin-s-bottom\">Several small survey networks (&lt; 2 km diameter) located along the Hayward and Calaveras faults, have been measured occasionally since 1965. Recent observations of these and other networks have been made by the U.S. Geological Survey. These observations imply a surface slip rate on the Hayward fault at Fremont, Hayward, Berkeley, and Richmond of about 6 mm/yr. On the Calaveras fault, north of the Hayward-Calaveras fault junction, surface slip rates have been determined from only four data sets. Three of which give a rate of 3 mm/yr. The U.S. Geological Survey annually measures 32 longer lines (10–30 km) in the east bay. Observations of these lines extend back to 1977 for most and to 1970 for some of the lines. The observed creep rates and the data for the longer east-bay lines provide constraints on the amount and position of deeper slip on the Hayward and Calaveras faults. After correcting for line-length changes due to fault slip, we calculated the strain accumulation rate. The shear strain rate parallel to east bay faults is 0.07 ± 0.02<span>&nbsp;</span><i>μstrain</i>/<i>yr</i>, a rate well below that of other areas along the San Andreas fault system, suggesting that creep is relieving a large part of the strain in this area.</div></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(83)90124-5","issn":"00401951","usgsCitation":"Prescott, W., and Lisowski, M., 1983, Strain accumulation along the San Andreas fault system east of San Francisco Bay, California: Tectonophysics, v. 97, no. 1-4, p. 41-56, https://doi.org/10.1016/0040-1951(83)90124-5.","productDescription":"16 p.","startPage":"41","endPage":"56","costCenters":[],"links":[{"id":220965,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"east of San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.5633105684395,\n              38.14960602120442\n            ],\n            [\n              -122.10094430081702,\n              37.459359967317894\n            ],\n            [\n              -121.72846974008448,\n              37.49292072037382\n            ],\n            [\n              -122.26483903868393,\n              38.24942942468891\n            ],\n            [\n              -122.5633105684395,\n              38.14960602120442\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"97","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9891e4b08c986b31c0a2","contributors":{"authors":[{"text":"Prescott, W.H.","contributorId":96337,"corporation":false,"usgs":true,"family":"Prescott","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":360609,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lisowski, M.","contributorId":70381,"corporation":false,"usgs":true,"family":"Lisowski","given":"M.","email":"","affiliations":[],"preferred":false,"id":360608,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":11552,"text":"ofr83417 - 1983 - Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:44","indexId":"ofr83417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-417","title":"Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado","docAbstract":"The Schwartzwalder uranium deposit, in the Front Range west of Denver, Colorado, is the largest vein-type uranium deposit in the United States. The deposit is situated in a steeply dipping fault system that cuts Proterozoic metamorphic rocks. The host rocks represent a submarine volcanic system with associated chert and iron- and sulfide-rich pelitic rocks. Where faulted, the more competent garnetiferous and quartzitic units behaved brittlely and created a deep, narrow conduit. \r\n\r\nThe ores formed 70-72 m.y. ago beneath 3 km of Phanerozoic sedimentary rocks. Mineralization included two episodes of alteration and three stages of vein-mineralization. Early carbonate-sericite alteration pseudomorphically replaced mafic minerals, whereas the ensuing hematite-adularia episode replaced only the earlier alteration assemblage. Early vein mineralization produced a minor sulfide-adularia-carbonate assemblage. Later vein mineralization generated the uranium ores in two successive stages. Carbonates, sulfides, and adularia filled the remaining voids. Clastic dikes composed of fault gouge and, locally, ore were injected into new and existing fractures. \r\n\r\nGeologic and chemical evidence suggest that virtually all components of the deposit were derived from major hornblende gneiss units and related rocks. The initial fluids were evolved connate/metamorphic water that infiltrated and resided along the extensive fault zones. Complex fault movements in the frontal zone of the eastern Front Range caused the fluids to migrate to the most permeable segments of the fault zones. Heat was supplied by increased crustal heat flow related to igneous activity in the nearby Colorado mineral belt. Temperatures decreased from 225?C to 125?C during later mineralization, and the pressure episodically dropped from 1000 bars. The CO2 fugacity was initially near 100 bars, and uranium was carried as a dicarbonate complex. Sudden decreases in confining pressure during fault movement caused evolution of CO2 and a consequent increase in pH. Uranium was released with destruction of the uranyl complexes; it was subsequently reduced by aqueous sulfur species, thereby leading to the precipitation of pitchblende.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83417","usgsCitation":"Wallace, A.R., 1983, Alteration and vein mineralization, Schwartzwalder uranium deposit, Front Range, Colorado: U.S. Geological Survey Open-File Report 83-417, 186 p. ill. ;28 cm., https://doi.org/10.3133/ofr83417.","productDescription":"186 p. ill. ;28 cm.","costCenters":[],"links":[{"id":145473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0417/report-thumb.jpg"},{"id":39426,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0417/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adee4b07f02db68751b","contributors":{"authors":[{"text":"Wallace, Alan R.","contributorId":6024,"corporation":false,"usgs":true,"family":"Wallace","given":"Alan","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":163345,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20306,"text":"ofr83848 - 1983 - Analytical results for 2244 stream-sediment samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire","interactions":[],"lastModifiedDate":"2021-10-22T19:01:13.844526","indexId":"ofr83848","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-848","title":"Analytical results for 2244 stream-sediment samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83848","usgsCitation":"Nowlan, G., Howd, F.H., and Nakagawa, H.M., 1983, Analytical results for 2244 stream-sediment samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire: U.S. Geological Survey Open-File Report 83-848, Report: i, 117 p.; 1 Plate: 30.53 × 47.40 inches, https://doi.org/10.3133/ofr83848.","productDescription":"Report: i, 117 p.; 1 Plate: 30.53 × 47.40 inches","costCenters":[],"links":[{"id":152191,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0848/report-thumb.jpg"},{"id":49840,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0848/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0848/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390840,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14244.htm"}],"country":"United States","state":"Maine, New Hampshire","otherGeospatial":"Lewiston 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.211,\n              44\n            ],\n            [\n              -70,\n              44\n            ],\n            [\n              -70,\n              45\n            ],\n            [\n              -71.211,\n              45\n            ],\n            [\n              -71.211,\n              44\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca6d","contributors":{"authors":[{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":182426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howd, F. H.","contributorId":52965,"corporation":false,"usgs":true,"family":"Howd","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":182425,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nakagawa, H. M.","contributorId":106475,"corporation":false,"usgs":true,"family":"Nakagawa","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":182427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":20265,"text":"ofr83334 - 1983 - High-resolution seismic-reflection profiles and sidescan-sonar records collected on eastern Long Island Sound and Block Island Sound","interactions":[],"lastModifiedDate":"2019-10-01T14:20:51","indexId":"ofr83334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-334","title":"High-resolution seismic-reflection profiles and sidescan-sonar records collected on eastern Long Island Sound and Block Island Sound","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83334","usgsCitation":"Needell, S.W., and Lewis, R., 1983, High-resolution seismic-reflection profiles and sidescan-sonar records collected on eastern Long Island Sound and Block Island Sound: U.S. Geological Survey Open-File Report 83-334, 4 p. , https://doi.org/10.3133/ofr83334.","productDescription":"4 p. ","costCenters":[],"links":[{"id":152066,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0334/report-thumb.jpg"},{"id":367645,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0334/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New York","otherGeospatial":"Long Island Sound, Block Island Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.970947265625,\n              40.245991504199026\n            ],\n            [\n              -70.8123779296875,\n              40.245991504199026\n            ],\n            [\n              -70.8123779296875,\n              41.430371882652814\n            ],\n            [\n              -73.970947265625,\n              41.430371882652814\n            ],\n            [\n              -73.970947265625,\n              40.245991504199026\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f435","contributors":{"authors":[{"text":"Needell, Sally W.","contributorId":106874,"corporation":false,"usgs":true,"family":"Needell","given":"Sally","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":182351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, Ralph S.","contributorId":9288,"corporation":false,"usgs":true,"family":"Lewis","given":"Ralph S.","affiliations":[],"preferred":false,"id":182350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28087,"text":"wri824122 - 1983 - Artificial recharge in the northern part of Chino ground-water basin, upper Santa Ana Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:43","indexId":"wri824122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4122","title":"Artificial recharge in the northern part of Chino ground-water basin, upper Santa Ana Valley, California","docAbstract":"This study was made to help management design and implement a recharge-recapture system for State Water Project water in Chino Basin. Nine test holes were drilled in the study area. Analyses of data from these test holes and drillers ' logs of water wells indicate the presence of clay deposits. The clay deposits cannot be correlated between holes which indicates that they are in the form of discontinuous beds or lenses. The existence and location of two ground-water barriers (Barrier ' J ' and Red Hill Barrier) have been postulated in previous reports. Water-level data indicate that Barrier ' J ' is probably not effectively stopping the movement of ground water. Data are insufficient to determine the effectiveness of the Red Hill barrier. Five existing recharge facilities in the study area were previously constructed to control floodflow. Infiltration tests were conducted at three of the facilities, and results of these tests indicate infiltration rates of 2.6 feet per day at Day Creek, 2.0 feet per day at East Etiwanda, and 1.3 feet per day at San Sevaine. A total of about 9,000 acre-feet of State Water Project water was recharged between June 1980 and July 1981. Rising water levels in wells indicate that recharge water is percolating down to the water table. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824122","usgsCitation":"Koehler, J.H., 1983, Artificial recharge in the northern part of Chino ground-water basin, upper Santa Ana Valley, California: U.S. Geological Survey Water-Resources Investigations Report 82-4122, iv, 27 p. :ill., maps ;26 cm., https://doi.org/10.3133/wri824122.","productDescription":"iv, 27 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":123868,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4122/report-thumb.jpg"},{"id":56907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4122/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672bfe","contributors":{"authors":[{"text":"Koehler, J. H.","contributorId":108108,"corporation":false,"usgs":true,"family":"Koehler","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":199196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19847,"text":"ofr83816 - 1983 - The Emma Bell deposit, Siskiyou Co., California: A possible low-grade source of chromite","interactions":[],"lastModifiedDate":"2021-11-16T20:29:28.488564","indexId":"ofr83816","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-816","title":"The Emma Bell deposit, Siskiyou Co., California: A possible low-grade source of chromite","docAbstract":"<p>The Emma Bell chromite deposit in Siskiyou County, California contains over 5 million tons of dunite averaging about 4 percent Cr<sub>2</sub>O<sub>3</sub>. Chromite is not evenly disseminated throughout the dunite, however. For the most part the deposit consists of many chromite-rich bands in sharp contact with, and separated by, common dunite containing 1 to 2 percent accessory chromite. Electron microprobe and petrographic analysis of accessory chromite shows that it is fine grained (average grain size 0.14 mm), generally lower in Cr<sub>2</sub>O<sub>3</sub>, and has a lower Cr/Fe ratio than segregated chromite. In addition, unusual patchy zoning is exhibited by some accessory chromite. These patchy zones are extremely rich in iron (&gt;60 percent total iron oxide). The negative factors such as the fine-grained nature of the accessory chromite and high iron content compared to segregated chromite, could be overcome by the very large tonnage in the deposit.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83816","usgsCitation":"Lipin, B., Wetzel, N., and Heinrich, S.M., 1983, The Emma Bell deposit, Siskiyou Co., California: A possible low-grade source of chromite: U.S. Geological Survey Open-File Report 83-816, i, 16 p., https://doi.org/10.3133/ofr83816.","productDescription":"i, 16 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":391761,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14237.htm"},{"id":152420,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0816/report-thumb.jpg"},{"id":49326,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0816/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Siskiyou County","otherGeospatial":"Emma Bell deposit","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.176,\n              41.905\n            ],\n            [\n              -123.125,\n              41.905\n            ],\n            [\n              -123.125,\n              41.95\n            ],\n            [\n              -123.176,\n              41.95\n            ],\n            [\n              -123.176,\n              41.905\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c8b5","contributors":{"authors":[{"text":"Lipin, B. R.","contributorId":61031,"corporation":false,"usgs":true,"family":"Lipin","given":"B. R.","affiliations":[],"preferred":false,"id":181621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wetzel, Nicholas","contributorId":37357,"corporation":false,"usgs":true,"family":"Wetzel","given":"Nicholas","email":"","affiliations":[],"preferred":false,"id":181620,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heinrich, S. M.","contributorId":95892,"corporation":false,"usgs":true,"family":"Heinrich","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":181622,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":19790,"text":"ofr83931 - 1983 - Public-supply pumpage in Wisconsin","interactions":[],"lastModifiedDate":"2015-10-08T13:30:56","indexId":"ofr83931","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-931","title":"Public-supply pumpage in Wisconsin","docAbstract":"<p>This report summarizes the amounts and distribution of the pumpage of ground water for public supplies from four aquifers in Wisconsin. The data are for 1979 and reflect the pumpage from about 1,100 wells in 485 communities. The distribution and amount of pumpage is estimated to be similar for subsequent years.</p>\n<p>Of the water pumped for public supplies, 95 percent comes from two major aquifers--the sand-and-gravel and the sandstone aquifers. Lesser amounts of water come from the Silurian dolomite, which is present onlyl in a narrow band in eastern Wisconsin, and from the generally low-yielding Precambrian basement rock that underlies the entire state.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83931","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Lawrence, C., Ellefson, B., and Cotter, R.D., 1983, Public-supply pumpage in Wisconsin: U.S. Geological Survey Open-File Report 83-931, iv, 40 p., https://doi.org/10.3133/ofr83931.","productDescription":"iv, 40 p.","numberOfPages":"44","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":49269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0931/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0931/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-90.403306,47.026693],[-90.411972,47.014958],[-90.425351,47.007526],[-90.464079,46.994636],[-90.465465,47.002593],[-90.457688,47.012484],[-90.4553,47.02375],[-90.455502,47.051331],[-90.449572,47.064965],[-90.438734,47.072557],[-90.417272,47.07757],[-90.395367,47.077175],[-90.393342,47.066204],[-90.403306,47.026693]]],[[[-90.730883,46.873096],[-90.677989,46.897527],[-90.667776,46.890037],[-90.675239,46.881029],[-90.718547,46.864531],[-90.745356,46.83566],[-90.756052,46.830595],[-90.760991,46.838277],[-90.749816,46.861806],[-90.730883,46.873096]]],[[[-90.764857,46.946524],[-90.741417,46.9636],[-90.71511,46.957332],[-90.694487,46.93671],[-90.689302,46.918563],[-90.737107,46.914712],[-90.764857,46.946524]]],[[[-90.568938,46.847391],[-90.58505,46.839789],[-90.613569,46.837958],[-90.673838,46.819684],[-90.683356,46.813275],[-90.685753,46.805003],[-90.652916,46.797755],[-90.65892,46.7885],[-90.696465,46.78204],[-90.716456,46.785418],[-90.7625,46.755547],[-90.787751,46.753301],[-90.783086,46.772939],[-90.790965,46.781373],[-90.790231,46.786103],[-90.733231,46.800183],[-90.720932,46.815897],[-90.656946,46.843476],[-90.622048,46.872872],[-90.602619,46.872715],[-90.568938,46.847391]]],[[[-90.572383,46.958835],[-90.528182,46.968396],[-90.508157,46.956836],[-90.524018,46.935714],[-90.539947,46.92785],[-90.543852,46.918289],[-90.549104,46.915461],[-90.569169,46.920309],[-90.637124,46.906724],[-90.64412,46.908373],[-90.654796,46.919249],[-90.634507,46.942944],[-90.572383,46.958835]]],[[[-87.335299,45.211327],[-87.331962,45.199251],[-87.33622,45.173174],[-87.327284,45.157363],[-87.376777,45.177298],[-87.375403,45.199296],[-87.335299,45.211327]]],[[[-90.962901,46.962028],[-90.980316,46.971578],[-90.98222,46.985417],[-90.949383,46.991208],[-90.939866,47.001321],[-90.928563,47.000726],[-90.923764,46.987928],[-90.932132,46.962655],[-90.962901,46.962028]]],[[[-90.757147,47.03372],[-90.688544,47.043347],[-90.643623,47.041177],[-90.608824,47.007558],[-90.560936,47.037013],[-90.544875,47.017383],[-90.552867,46.999686],[-90.609715,46.991208],[-90.634105,46.970983],[-90.671581,46.948973],[-90.712032,46.98526],[-90.767985,47.002327],[-90.776921,47.024324],[-90.757147,47.03372]]],[[[-87.405658,44.860098],[-87.384821,44.865532],[-87.385396,44.889964],[-87.406199,44.90449],[-87.393752,44.933751],[-87.374805,44.956631],[-87.360288,44.987643],[-87.322117,45.034201],[-87.264877,45.081361],[-87.257449,45.121644],[-87.240813,45.137559],[-87.242924,45.149377],[-87.238426,45.166492],[-87.224065,45.174551],[-87.21437,45.165735],[-87.195876,45.163201],[-87.17517,45.173],[-87.163169,45.185331],[-87.13303,45.192843],[-87.119972,45.191103],[-87.122708,45.221786],[-87.109541,45.255397],[-87.078316,45.265723],[-87.071035,45.280355],[-87.057627,45.292838],[-87.0517,45.285888],[-87.043895,45.284767],[-87.017036,45.299254],[-86.994112,45.298061],[-86.97778,45.290684],[-86.970355,45.278455],[-86.984938,45.259036],[-86.983066,45.250764],[-86.973287,45.246381],[-86.985973,45.215872],[-87.002806,45.211773],[-87.00754,45.222127],[-87.032521,45.222274],[-87.040909,45.211535],[-87.045242,45.158798],[-87.030225,45.147382],[-87.03292,45.141963],[-87.045748,45.134987],[-87.054282,45.120074],[-87.049346,45.110122],[-87.048213,45.089124],[-87.057415,45.087472],[-87.064864,45.078427],[-87.079552,45.070783],[-87.081866,45.059103],[-87.090849,45.055465],[-87.121156,45.058311],[-87.139384,45.012565],[-87.163477,45.004913],[-87.189134,44.969078],[-87.188399,44.94856],[-87.17524,44.939753],[-87.1717,44.931476],[-87.204238,44.916819],[-87.215808,44.906744],[-87.217171,44.898013],[-87.206285,44.885928],[-87.204815,44.877199],[-87.267061,44.847025],[-87.282561,44.814729],[-87.304824,44.804603],[-87.313363,44.794237],[-87.320397,44.784963],[-87.319903,44.769672],[-87.353789,44.701915],[-87.401629,44.631191],[-87.437751,44.604559],[-87.467089,44.553557],[-87.483696,44.511354],[-87.490024,44.477224],[-87.498662,44.460686],[-87.506362,44.423804],[-87.517965,44.394356],[-87.517597,44.375696],[-87.533583,44.351111],[-87.545382,44.321385],[-87.541382,44.294018],[-87.508457,44.229755],[-87.507419,44.210803],[-87.512903,44.192808],[-87.51966,44.17987],[-87.53994,44.15969],[-87.563181,44.144195],[-87.603572,44.13039],[-87.6458,44.105222],[-87.654935,44.082552],[-87.656062,44.051919],[-87.683361,44.020139],[-87.695053,43.990715],[-87.69892,43.965936],[-87.71817,43.939498],[-87.735436,43.882219],[-87.728698,43.852524],[-87.726408,43.810454],[-87.700251,43.76735],[-87.702985,43.749695],[-87.709885,43.735795],[-87.702685,43.687596],[-87.789105,43.564844],[-87.797608,43.52731],[-87.793239,43.492783],[-87.807799,43.461136],[-87.855608,43.405441],[-87.872504,43.380178],[-87.882392,43.352099],[-87.889207,43.307652],[-87.901847,43.284117],[-87.911787,43.250406],[-87.896286,43.197108],[-87.881085,43.170609],[-87.900285,43.13731],[-87.900496,43.126],[-87.893185,43.114011],[-87.876084,43.099011],[-87.866487,43.074419],[-87.870184,43.064412],[-87.894813,43.042497],[-87.898184,43.030689],[-87.896157,43.017486],[-87.887789,43.000715],[-87.857182,42.978015],[-87.845181,42.962015],[-87.842786,42.944865],[-87.847745,42.889595],[-87.824,42.836649],[-87.766675,42.784896],[-87.781949,42.74857],[-87.778824,42.728432],[-87.783489,42.705164],[-87.802377,42.676651],[-87.814674,42.64402],[-87.819407,42.617327],[-87.819374,42.60662],[-87.810873,42.58732],[-87.812273,42.52982],[-87.800477,42.49192],[-88.115285,42.496219],[-88.786681,42.491983],[-89.690088,42.505191],[-90.640927,42.508302],[-90.636727,42.518702],[-90.645627,42.5441],[-90.654127,42.5499],[-90.661527,42.567999],[-90.685487,42.589614],[-90.693999,42.614509],[-90.709204,42.636078],[-90.769495,42.651443],[-90.88743,42.67247],[-90.921155,42.685406],[-90.949213,42.685573],[-90.977735,42.696816],[-91.000128,42.716189],[-91.026786,42.724228],[-91.035418,42.73734],[-91.053733,42.738238],[-91.056297,42.747341],[-91.065783,42.753387],[-91.060261,42.761847],[-91.069549,42.769628],[-91.078097,42.806526],[-91.078665,42.827678],[-91.09406,42.830813],[-91.091402,42.84986],[-91.097656,42.859871],[-91.100565,42.883078],[-91.115512,42.894672],[-91.14556,42.90798],[-91.144315,42.926592],[-91.149784,42.940244],[-91.14655,42.963345],[-91.156562,42.978226],[-91.15749,42.991475],[-91.174692,43.038713],[-91.179457,43.067427],[-91.175193,43.103771],[-91.177932,43.128875],[-91.175253,43.134665],[-91.1562,43.142945],[-91.1462,43.152405],[-91.12217,43.197255],[-91.066398,43.239293],[-91.059684,43.248566],[-91.058644,43.257679],[-91.072649,43.262129],[-91.07371,43.274746],[-91.107237,43.313645],[-91.137343,43.329757],[-91.181115,43.345926],[-91.201847,43.349103],[-91.21477,43.365874],[-91.19767,43.395334],[-91.203144,43.419805],[-91.22875,43.445537],[-91.233367,43.455168],[-91.216035,43.481142],[-91.217353,43.512474],[-91.232941,43.523967],[-91.243183,43.540309],[-91.24382,43.54913],[-91.232812,43.564842],[-91.231865,43.581822],[-91.268748,43.615348],[-91.268457,43.627352],[-91.262397,43.64176],[-91.270767,43.65308],[-91.273252,43.666623],[-91.268455,43.709824],[-91.255932,43.729849],[-91.255431,43.744876],[-91.243955,43.773046],[-91.262436,43.792166],[-91.277695,43.837741],[-91.284138,43.847065],[-91.310991,43.867381],[-91.320605,43.888491],[-91.338141,43.897664],[-91.346271,43.910074],[-91.356741,43.916564],[-91.366642,43.937463],[-91.385785,43.954239],[-91.406011,43.963929],[-91.43738,43.999962],[-91.463515,44.009041],[-91.478498,44.00803],[-91.507121,44.01898],[-91.580019,44.026925],[-91.59207,44.031372],[-91.610487,44.04931],[-91.638115,44.063285],[-91.647873,44.064109],[-91.667006,44.086964],[-91.68153,44.0974],[-91.707491,44.103906],[-91.710597,44.12048],[-91.721552,44.130342],[-91.751747,44.134786],[-91.774486,44.147539],[-91.808064,44.159262],[-91.817302,44.164235],[-91.829167,44.17835],[-91.875158,44.200575],[-91.877429,44.212921],[-91.892698,44.231105],[-91.88704,44.251772],[-91.896008,44.262871],[-91.895652,44.273008],[-91.924613,44.291815],[-91.913534,44.311392],[-91.918625,44.322671],[-91.92559,44.333548],[-91.941311,44.340978],[-91.9636,44.362112],[-92.038147,44.388731],[-92.056486,44.402729],[-92.078605,44.404869],[-92.111085,44.413948],[-92.124513,44.422115],[-92.195378,44.433792],[-92.232472,44.445434],[-92.291005,44.485464],[-92.302215,44.500298],[-92.302466,44.516487],[-92.314071,44.538014],[-92.336114,44.554004],[-92.361518,44.558935],[-92.399281,44.558292],[-92.431101,44.565786],[-92.455105,44.561886],[-92.481001,44.568276],[-92.493808,44.566063],[-92.518358,44.575183],[-92.54806,44.567792],[-92.55151,44.571607],[-92.549777,44.58113],[-92.569434,44.603539],[-92.577148,44.605054],[-92.584711,44.599861],[-92.601516,44.612052],[-92.621456,44.615017],[-92.619779,44.634195],[-92.632105,44.649027],[-92.660988,44.660884],[-92.700948,44.693751],[-92.737259,44.717155],[-92.787906,44.737432],[-92.807317,44.750364],[-92.805287,44.768361],[-92.785206,44.792303],[-92.78043,44.812589],[-92.766102,44.834966],[-92.76909,44.861997],[-92.764133,44.875905],[-92.773946,44.889997],[-92.774571,44.898084],[-92.758701,44.908979],[-92.750645,44.937299],[-92.754603,44.955767],[-92.769445,44.97215],[-92.771231,45.001378],[-92.76206,45.02432],[-92.770362,45.033803],[-92.793282,45.047178],[-92.803079,45.060978],[-92.800851,45.069477],[-92.791528,45.079647],[-92.746749,45.107051],[-92.739528,45.116515],[-92.745694,45.123112],[-92.757707,45.155466],[-92.752542,45.171772],[-92.764872,45.182812],[-92.767408,45.190166],[-92.763908,45.204866],[-92.751708,45.218666],[-92.760249,45.2496],[-92.751659,45.26591],[-92.760615,45.278827],[-92.761013,45.289028],[-92.737122,45.300459],[-92.709968,45.321302],[-92.698967,45.336374],[-92.703705,45.35633],[-92.679193,45.37271],[-92.669505,45.389111],[-92.650422,45.398507],[-92.646602,45.441635],[-92.652698,45.454527],[-92.680234,45.464344],[-92.702224,45.493046],[-92.726677,45.514462],[-92.726082,45.541112],[-92.770223,45.566939],[-92.785741,45.567888],[-92.823309,45.560934],[-92.871082,45.567581],[-92.883749,45.575483],[-92.886442,45.598679],[-92.882529,45.610216],[-92.888035,45.624959],[-92.887929,45.639006],[-92.875488,45.689014],[-92.870145,45.696757],[-92.869193,45.717568],[-92.809837,45.744172],[-92.784621,45.764196],[-92.776496,45.790014],[-92.757815,45.806574],[-92.765146,45.830183],[-92.739991,45.846283],[-92.734039,45.868108],[-92.712503,45.891705],[-92.676607,45.90637],[-92.676807,45.91093],[-92.659549,45.922937],[-92.639116,45.924555],[-92.640115,45.932478],[-92.636316,45.934634],[-92.614314,45.934529],[-92.60246,45.940815],[-92.551933,45.951651],[-92.549806,45.967986],[-92.527052,45.983245],[-92.469354,45.973811],[-92.46126,45.979427],[-92.464512,45.985038],[-92.453373,45.992913],[-92.442259,46.016177],[-92.428555,46.024241],[-92.410649,46.027259],[-92.372717,46.014198],[-92.35176,46.015685],[-92.344244,46.02743],[-92.343604,46.040917],[-92.332912,46.062697],[-92.294033,46.074377],[-92.292192,46.666042],[-92.287392,46.667342],[-92.286192,46.660342],[-92.274392,46.657441],[-92.270592,46.650741],[-92.256592,46.658741],[-92.242493,46.649241],[-92.228492,46.652941],[-92.216392,46.649841],[-92.207092,46.651941],[-92.202292,46.655041],[-92.204092,46.666941],[-92.176091,46.686341],[-92.183091,46.695241],[-92.198491,46.696141],[-92.205192,46.698341],[-92.205692,46.702541],[-92.189091,46.717541],[-92.167291,46.719941],[-92.146291,46.71594],[-92.141291,46.72524],[-92.14329,46.73464],[-92.13789,46.73954],[-92.108777,46.749105],[-92.08949,46.74924],[-92.03399,46.708939],[-92.020289,46.704039],[-92.007989,46.705039],[-91.961889,46.682539],[-91.942988,46.679939],[-91.886963,46.690211],[-91.820027,46.690176],[-91.790473,46.694624],[-91.74965,46.709129],[-91.646146,46.734575],[-91.590684,46.754331],[-91.511077,46.757453],[-91.489125,46.766997],[-91.44957,46.773252],[-91.411799,46.78964],[-91.369387,46.793745],[-91.33825,46.817704],[-91.315061,46.826729],[-91.256873,46.836833],[-91.226796,46.86361],[-91.207524,46.865835],[-91.200107,46.854017],[-91.178292,46.844259],[-91.168297,46.844727],[-91.140301,46.873105],[-91.133337,46.870341],[-91.134977,46.859023],[-91.107323,46.857469],[-91.096565,46.86153],[-91.090916,46.88267],[-91.080951,46.883609],[-91.069331,46.878772],[-91.052991,46.881325],[-91.03989,46.88923],[-91.034518,46.903053],[-91.019141,46.911502],[-90.995149,46.917577],[-90.968419,46.94391],[-90.92204,46.931372],[-90.914044,46.933346],[-90.908654,46.941221],[-90.880358,46.957661],[-90.855874,46.962232],[-90.838814,46.957728],[-90.786595,46.927019],[-90.75563,46.899247],[-90.751151,46.887863],[-90.77017,46.876296],[-90.798545,46.823922],[-90.825696,46.803858],[-90.835008,46.790366],[-90.854916,46.788952],[-90.863542,46.780565],[-90.859724,46.774433],[-90.862333,46.768135],[-90.885021,46.756341],[-90.870396,46.723293],[-90.853225,46.70028],[-90.853644,46.694464],[-90.870079,46.679449],[-90.914619,46.659054],[-90.924487,46.625417],[-90.93831,46.608768],[-90.951418,46.600774],[-90.942101,46.588573],[-90.906058,46.58343],[-90.873154,46.601223],[-90.794775,46.624941],[-90.770192,46.636127],[-90.755381,46.646225],[-90.756495,46.664591],[-90.74809,46.669817],[-90.73726,46.692267],[-90.627885,46.623839],[-90.558141,46.586384],[-90.538346,46.581182],[-90.505909,46.589614],[-90.437596,46.561492],[-90.418136,46.566094],[-90.39332,46.532615],[-90.369964,46.540549],[-90.350121,46.537337],[-90.344338,46.552087],[-90.331887,46.553278],[-90.326686,46.54615],[-90.320428,46.546287],[-90.310859,46.539365],[-90.316983,46.517319],[-90.285707,46.518846],[-90.277131,46.524487],[-90.272599,46.521127],[-90.274721,46.515416],[-90.270684,46.508237],[-90.263018,46.502777],[-90.231587,46.509842],[-90.230324,46.501732],[-90.216594,46.501759],[-90.204009,46.478175],[-90.188996,46.469015],[-90.193294,46.463143],[-90.180336,46.456746],[-90.17786,46.440548],[-90.166919,46.439851],[-90.158603,46.422656],[-90.157851,46.409291],[-90.144359,46.390255],[-90.13225,46.381249],[-90.133871,46.371828],[-90.116844,46.355153],[-90.12138,46.338131],[-89.09163,46.138505],[-88.85027,46.040274],[-88.837991,46.030176],[-88.811948,46.021609],[-88.79646,46.023605],[-88.80067,46.030036],[-88.796182,46.033712],[-88.779221,46.031869],[-88.783891,46.020934],[-88.779915,46.015436],[-88.765208,46.022086],[-88.756295,46.020173],[-88.746422,46.025798],[-88.730675,46.026535],[-88.721125,46.022013],[-88.718397,46.013284],[-88.704687,46.018154],[-88.679132,46.013538],[-88.661312,45.988819],[-88.6375,45.98496],[-88.616405,45.9877],[-88.611466,46.003332],[-88.60144,46.017599],[-88.59386,46.015132],[-88.589755,46.005602],[-88.565485,46.015708],[-88.550756,46.012896],[-88.541078,46.013763],[-88.533825,46.020915],[-88.514601,46.019926],[-88.507188,46.0183],[-88.498108,45.99636],[-88.492495,45.992157],[-88.476002,45.992826],[-88.470855,46.001004],[-88.458658,45.999391],[-88.450325,45.990181],[-88.439733,45.990456],[-88.416914,45.975323],[-88.388847,45.982675],[-88.380183,45.991654],[-88.330137,45.965951],[-88.330296,45.956625],[-88.326953,45.955071],[-88.316894,45.960969],[-88.292381,45.951115],[-88.250133,45.963147],[-88.246307,45.962983],[-88.242518,45.950363],[-88.23314,45.947405],[-88.201852,45.945173],[-88.202116,45.949836],[-88.191991,45.95274],[-88.170096,45.93947],[-88.146352,45.935314],[-88.121864,45.92075],[-88.104686,45.922121],[-88.096496,45.917273],[-88.095354,45.913895],[-88.105677,45.904387],[-88.101814,45.883504],[-88.095841,45.880042],[-88.083965,45.881186],[-88.073944,45.875593],[-88.075146,45.864832],[-88.081641,45.865087],[-88.13611,45.819029],[-88.129461,45.809288],[-88.105355,45.800104],[-88.103247,45.791361],[-88.072091,45.780261],[-88.050634,45.780972],[-88.040221,45.789236],[-87.991447,45.795393],[-87.98087,45.776977],[-87.989829,45.772945],[-87.96697,45.764021],[-87.963452,45.75822],[-87.905873,45.759364],[-87.896032,45.752285],[-87.875813,45.753888],[-87.864141,45.745697],[-87.86432,45.737139],[-87.85548,45.726943],[-87.805867,45.706841],[-87.809181,45.700337],[-87.782226,45.683053],[-87.780737,45.675458],[-87.823164,45.662732],[-87.824102,45.647138],[-87.810194,45.638732],[-87.79588,45.618846],[-87.780845,45.614599],[-87.777199,45.588499],[-87.787534,45.581376],[-87.790874,45.564096],[-87.806104,45.562863],[-87.829346,45.568776],[-87.833591,45.562529],[-87.80339,45.538272],[-87.802267,45.514233],[-87.792769,45.499967],[-87.812971,45.4661],[-87.861697,45.434473],[-87.860432,45.423504],[-87.849322,45.403872],[-87.859131,45.398967],[-87.859418,45.388227],[-87.875424,45.379373],[-87.871789,45.373557],[-87.884855,45.362792],[-87.888052,45.354697],[-87.881114,45.351278],[-87.86856,45.360537],[-87.860871,45.351192],[-87.850418,45.347492],[-87.848368,45.340676],[-87.832612,45.352249],[-87.790324,45.353444],[-87.783076,45.349725],[-87.754104,45.349442],[-87.751626,45.354169],[-87.738352,45.358243],[-87.718891,45.377462],[-87.693956,45.389893],[-87.675017,45.382454],[-87.674403,45.378065],[-87.657349,45.368752],[-87.656632,45.358617],[-87.648476,45.352243],[-87.648126,45.339396],[-87.662029,45.326434],[-87.663666,45.318257],[-87.687498,45.298055],[-87.698248,45.281512],[-87.69878,45.26942],[-87.709137,45.260341],[-87.711339,45.239965],[-87.724156,45.233236],[-87.721935,45.228444],[-87.726952,45.218949],[-87.726198,45.209391],[-87.741732,45.198201],[-87.736509,45.173389],[-87.683902,45.144135],[-87.675816,45.135059],[-87.678511,45.131204],[-87.672447,45.121294],[-87.661296,45.112566],[-87.661211,45.108279],[-87.631535,45.106224],[-87.59188,45.094689],[-87.587147,45.089495],[-87.587992,45.085271],[-87.601849,45.082297],[-87.610395,45.075617],[-87.625748,45.045157],[-87.624693,45.014176],[-87.630298,44.976865],[-87.661964,44.973035],[-87.696492,44.974233],[-87.766115,44.965351],[-87.817551,44.951986],[-87.837647,44.933091],[-87.844299,44.918524],[-87.827751,44.891229],[-87.832764,44.880939],[-87.852789,44.86486],[-87.865898,44.840988],[-87.878218,44.839016],[-87.899787,44.828051],[-87.941453,44.75608],[-87.964714,44.74357],[-87.983065,44.72073],[-87.990081,44.669791],[-88.002085,44.664035],[-88.009766,44.637081],[-87.998836,44.609523],[-88.001943,44.603909],[-88.012395,44.602438],[-88.027103,44.578992],[-88.039092,44.574324],[-88.042261,44.567344],[-88.005518,44.539216],[-87.970702,44.530292],[-87.943801,44.529693],[-87.929001,44.535993],[-87.901206,44.568887],[-87.899368,44.573043],[-87.903689,44.581317],[-87.901179,44.584545],[-87.867941,44.607606],[-87.809076,44.636189],[-87.77516,44.639281],[-87.756048,44.649117],[-87.748409,44.667122],[-87.71978,44.693246],[-87.720312,44.725073],[-87.610063,44.838384],[-87.581635,44.851638],[-87.550288,44.85129],[-87.530999,44.857437],[-87.515142,44.869596],[-87.502431,44.864619],[-87.478489,44.863572],[-87.437084,44.892718],[-87.421007,44.887869],[-87.419951,44.87594],[-87.405658,44.860098]]],[[[-86.880572,45.331467],[-86.895055,45.329035],[-86.899488,45.322588],[-86.896667,45.307275],[-86.899891,45.295185],[-86.925681,45.3242],[-86.95499,45.34128],[-86.956192,45.351179],[-86.946297,45.35869],[-86.95497,45.383194],[-86.943041,45.41525],[-86.934724,45.421123],[-86.928045,45.411273],[-86.917686,45.40789],[-86.892893,45.40898],[-86.877502,45.413981],[-86.862174,45.412151],[-86.853145,45.405547],[-86.830353,45.410852],[-86.828731,45.428461],[-86.810055,45.422619],[-86.805415,45.407324],[-86.824383,45.406135],[-86.841432,45.389601],[-86.853103,45.370861],[-86.863367,45.365],[-86.869031,45.333244],[-86.880572,45.331467]]]]},\"properties\":{\"name\":\"Wisconsin\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a90e4b07f02db656113","contributors":{"authors":[{"text":"Lawrence, C.L.","contributorId":58263,"corporation":false,"usgs":true,"family":"Lawrence","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":181515,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ellefson, B.R.","contributorId":83927,"corporation":false,"usgs":true,"family":"Ellefson","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":181516,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":181517,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":19670,"text":"ofr83815 - 1983 - Geoelectric structure of the Gila-San Francisco Wilderness Area, Graham and Greenlee Counties, Arizona, from audio-magnetotelluric data","interactions":[],"lastModifiedDate":"2022-09-01T21:00:22.928432","indexId":"ofr83815","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-815","title":"Geoelectric structure of the Gila-San Francisco Wilderness Area, Graham and Greenlee Counties, Arizona, from audio-magnetotelluric data","docAbstract":"Electromagnetic induction data using distant field sources, mostly of natural origin, in the frequency range of 4.5-27,000 Hz are analyzed to depict the geoelectric structure in an area of volcanic-rock cover located in southeastern Arizona between the Morenci and Safford porphyry copper deposits. The data for each station consist of scalar electromagnetic measurements at descrete frequencies for two-orthogonal magnetic and electric field pairs. Observations spaced about 5-km apart indicate resistivities in the range of 100-700 ohm-m for the unweathered Tertiary volcanic rocks to a depth of 200 to 500 m. Beneath this zone the data indicate resistivities in the range of 10-100 ohm-m that suggest the existence of an older volcanic rock unit. The less resistive unit appears to be displaced upward beneath Turtle Mountain, an area bounded to the northeast and southwest by mapped Basin and Range faults, and bounded to the southeast by an unmapped fault of older origin that trends northeast. Lateral changes in the resistivity of the two main geoelectric layers result in lowered resistivity in an area of known hot-springs near the confluence of the Gila and San Francisco Rivers, as well as along a north-south trending zone located on the east flank of Turtle Mountain, about 5-km (3-mi) west-northwest of the hot springs. This second anomaly is at a probable depth of 400-500 m and is interpreted to indicate a buried fault or fracture zone.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83815","usgsCitation":"Klein, D.P., and Baer, M.J., 1983, Geoelectric structure of the Gila-San Francisco Wilderness Area, Graham and Greenlee Counties, Arizona, from audio-magnetotelluric data: U.S. Geological Survey Open-File Report 83-815, 109 p., https://doi.org/10.3133/ofr83815.","productDescription":"109 p.","costCenters":[],"links":[{"id":406098,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14236.htm","linkFileType":{"id":5,"text":"html"}},{"id":49135,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0815/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152182,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0815/report-thumb.jpg"}],"country":"United States","state":"Arizona","county":"Graham County, Greenlee County","otherGeospatial":"Gila-San Francisco Wilderness Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.566,\n              33.076\n            ],\n            [\n              -109.32,\n              33.076\n            ],\n            [\n              -109.32,\n              32.833\n            ],\n            [\n              -109.566,\n              32.833\n            ],\n            [\n              -109.566,\n              33.076\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9b4e","contributors":{"authors":[{"text":"Klein, D. P.","contributorId":36555,"corporation":false,"usgs":true,"family":"Klein","given":"D.","email":"","middleInitial":"P.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":181308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Baer, M. J.","contributorId":102487,"corporation":false,"usgs":true,"family":"Baer","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":181309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19423,"text":"ofr83774 - 1983 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","interactions":[{"subject":{"id":19423,"text":"ofr83774 - 1983 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"ofr83774","publicationYear":"1983","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":1899,"text":"wsp2258 - 1985 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"wsp2258","publicationYear":"1985","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"id":1}],"supersededBy":{"id":1899,"text":"wsp2258 - 1985 - Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","indexId":"wsp2258","publicationYear":"1985","noYear":false,"title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico"},"lastModifiedDate":"2021-01-26T19:53:48.989552","indexId":"ofr83774","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-774","title":"Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico","docAbstract":"<p>The Papago Farms-Great Plain and upper Rio Sonoyta study area includes about 490 square miles in south-central Arizona and north-central Sonora, Mexico. In the study area 23,700 acre-feet of ground water from the basin-fill deposits was used to irrigate more than 5,000 acres in 1981. Surface water is not a reliable source for irrigation or public supply. Ground water enters the area as underflow from the north and east and as recharge from the mountains, moves through basin-margin sediments, around the basin-center clays, and exits the area to the west beneath the Rio Sonoyta. Ground-water withdrawals in the upper Rio Sonoyta area do not appear to have an effect on water levels in the Papago Farms-Great Plain area. Depth to water ranges from 500 feet near the southern boundary to 150 feet in the center of study area. About 10 million acre-feet of recoverable ground water is stored in the upper 400 feet of the aquifer. Storage is being depleted at a rate of 19,000 acre-feet per year. The ground water is a sodium and bicarbonate type and has an anomalously high content of arsenic and fluoride. (USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83774","usgsCitation":"Hollett, K., 1983, Geohydrology and water resources of the Papago Farms-Great Plain area, Papago Indian Reservation, Arizona, and the upper Rio Sonoyta area, Sonora, Mexico: U.S. Geological Survey Open-File Report 83-774, vi, 76 p., https://doi.org/10.3133/ofr83774.","productDescription":"vi, 76 p.","costCenters":[],"links":[{"id":382608,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0774/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0774/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Papago Indian Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.2470703125,\n              31.765537409484374\n            ],\n            [\n              -111.236572265625,\n              31.765537409484374\n            ],\n            [\n              -111.236572265625,\n              33.0178760185549\n            ],\n            [\n              -113.2470703125,\n              33.0178760185549\n            ],\n            [\n              -113.2470703125,\n              31.765537409484374\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b25","contributors":{"authors":[{"text":"Hollett, K.J.","contributorId":23570,"corporation":false,"usgs":true,"family":"Hollett","given":"K.J.","affiliations":[],"preferred":false,"id":180879,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27998,"text":"wri834007 - 1983 - Application of remote-sensing techniques to hydrologic studies in selected coal-mined areas of southeastern Kansas","interactions":[],"lastModifiedDate":"2022-01-10T20:04:36.318938","indexId":"wri834007","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4007","title":"Application of remote-sensing techniques to hydrologic studies in selected coal-mined areas of southeastern Kansas","docAbstract":"<p>Disturbances resulting from intensive coal mining in the Cherry Creek basin of southeastern Kansas were investigated using color and color-infrared aerial photography in conjunction with water-quality data from simultaneously acquired samples. Imagery was used to identify the type and extent of vegetative cover on strip-mined lands and the extent and success of reclamation practices. Drainage patterns, point sources of acid mine drainage, and recharge areas for underground mines were located for onsite inspection. Comparison of these interpretations with water-quality data illustrated differences between the eastern and western parts of the Cherry Creek basin. Contamination in the eastern part is due largely to circulation of water from unreclaimed strip mines and collapse features through the network of underground mines and subsequent discharge of acidic drainage through seeps. Contamination in the western part is primarily caused by runoff and seepage from strip-mined lands in which surfaces have frequently been graded and limed but are generally devoid of mature stands of soil-anchoring vegetation. The successful use of aerial photography in the study of Cherry Creek basin indicates the potential of using remote-sensing techniques in studies of other coal-mined regions.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834007","usgsCitation":"Kenny, J.F., and McCauley, J.R., 1983, Application of remote-sensing techniques to hydrologic studies in selected coal-mined areas of southeastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 83-4007, Report: iv, 33 p.; 1 Plate: 16.01 × 18.60 inches, https://doi.org/10.3133/wri834007.","productDescription":"Report: iv, 33 p.; 1 Plate: 16.01 × 18.60 inches","costCenters":[],"links":[{"id":56824,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4007/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394124,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35653.htm"},{"id":56825,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4007/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123358,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4007/report-thumb.jpg"}],"country":"United States","state":"Kansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.9720,\n              37.158\n            ],\n            [\n              -94.5730,\n              37.158\n            ],\n            [\n              -94.5730,\n              37.333\n            ],\n            [\n              -94.9720,\n              37.333\n            ],\n            [\n              -94.9720,\n              37.158\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a8ad","contributors":{"authors":[{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCauley, J. R.","contributorId":97533,"corporation":false,"usgs":true,"family":"McCauley","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18803,"text":"ofr82864 - 1983 - Hydrology of area 10, Eastern Coal Province, West Virginia and Virginia","interactions":[],"lastModifiedDate":"2023-12-13T21:02:30.442332","indexId":"ofr82864","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-864","title":"Hydrology of area 10, Eastern Coal Province, West Virginia and Virginia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82864","usgsCitation":"Ehlke, T.A., McCauley, S.D., Schultz, R.A., Bader, J., Runner, G.S., and Downs, S.C., 1983, Hydrology of area 10, Eastern Coal Province, West Virginia and Virginia: U.S. Geological Survey Open-File Report 82-864, v, 73 p., https://doi.org/10.3133/ofr82864.","productDescription":"v, 73 p.","costCenters":[],"links":[{"id":95416,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0864/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152920,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0864/report-thumb.jpg"},{"id":423532,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13845.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Virginia, West Virginia","otherGeospatial":"Area 10","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.2305875752171,\n              37.237962508166916\n            ],\n            [\n              -81.07592965369068,\n              37.00253435336218\n            ],\n            [\n              -80.09174288034123,\n              37.21277309392809\n            ],\n            [\n              -79.61370930471458,\n              37.40288462880359\n            ],\n            [\n              -80.13743726624699,\n              37.86218294165562\n            ],\n            [\n              -79.49420064369879,\n              38.6790003602099\n            ],\n            [\n              -79.73673238427408,\n              38.80785124653647\n            ],\n            [\n              -80.17961643228112,\n              38.409585365316985\n            ],\n            [\n              -81.2868289170625,\n              37.45033682465838\n            ],\n            [\n              -81.34658311401566,\n              37.32745615996632\n            ],\n            [\n              -81.43094198030279,\n              37.25195244255953\n            ],\n            [\n              -81.2305875752171,\n              37.237962508166916\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6046e7","contributors":{"authors":[{"text":"Ehlke, T. A.","contributorId":106477,"corporation":false,"usgs":true,"family":"Ehlke","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179770,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCauley, S. D.","contributorId":63036,"corporation":false,"usgs":true,"family":"McCauley","given":"S.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":179767,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schultz, R. A.","contributorId":108126,"corporation":false,"usgs":true,"family":"Schultz","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":179771,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bader, J. S.","contributorId":65830,"corporation":false,"usgs":true,"family":"Bader","given":"J. S.","affiliations":[],"preferred":false,"id":179768,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Runner, G. S.","contributorId":74405,"corporation":false,"usgs":true,"family":"Runner","given":"G.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":179769,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Downs, S. C.","contributorId":36956,"corporation":false,"usgs":true,"family":"Downs","given":"S.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":179766,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":1098,"text":"wsp2210 - 1983 - Connector well experiment to recharge the Floridan aquifer, east Orange County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp2210","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"2210","title":"Connector well experiment to recharge the Floridan aquifer, east Orange County, Florida","docAbstract":"An experimental connector well, screened in the shallow sand aquifer, finished with open hole in the Floridan aquifer and cased through the confining layer between the two aquifers, was drilled in east Orange County, Fla., to obtain information on the nature and function of the shallow aquifer as related to connector well operation. The potentiometric surface of the shallow aquifer is about 45 feet higher than the potentiomettic surface of the Floridan aquifer; hence water flows by gravity from the shallow aquifer to the Floridan aquifer through the well 'connecting' the two aquifers. Continuous flow measurement over 10 months shows the well discharge varies seasonally and averages slightly more than 50 gallons per minute. Observation wells show that, except for seasonal variation, water levels within the area of influence have reached steady state within measurable limits. Vertical anisotropy in the shallow aquifer is apparently caused by the shape and (or) arrangement of the sand grains that comprise the shallow aquifer, rather than because of distinct confining layers of different lithology. Transmissivity of the shallow aquifer at the site is about 600 square feet per clay. Extensive dewatering of wetlands in east Orange County by connector wells alone probably is not feasible. Nevertheless, large amounts of water could be channeled to the Floridan aquifer by connector wells. The results of the connector well experiment imply that water is being captured from evapotranspiration and interception of water that would have discharged to swamps in the vicinity of the connector well. However, the data available from this experiment do not permit a quantitative expression of the net gain in recharge to the Floridan aquifer resulting from operation of the connector well.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wsp2210","usgsCitation":"Bush, P.W., 1983, Connector well experiment to recharge the Floridan aquifer, east Orange County, Florida: U.S. Geological Survey Water Supply Paper 2210, iii, 26 p. :ill., map ;28 cm., https://doi.org/10.3133/wsp2210.","productDescription":"iii, 26 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":138094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2210/report-thumb.jpg"},{"id":25828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2210/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f59","contributors":{"authors":[{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143173,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18705,"text":"ofr83739 - 1983 - Analyses of heavy-mineral-concentrate samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire","interactions":[],"lastModifiedDate":"2022-05-04T21:23:22.720667","indexId":"ofr83739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-739","title":"Analyses of heavy-mineral-concentrate samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83739","usgsCitation":"Domenico, J.A., Howd, F.H., and Nowlan, G., 1983, Analyses of heavy-mineral-concentrate samples, east half of the Lewiston 1° x 2° quadrangle, Maine and New Hampshire: U.S. Geological Survey Open-File Report 83-739, i, 25 p., https://doi.org/10.3133/ofr83739.","productDescription":"i, 25 p.","costCenters":[],"links":[{"id":48063,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0739/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48062,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0739/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0739/report-thumb.jpg"},{"id":400191,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14203.htm"}],"country":"United States","state":"Maine, New Hampshire","otherGeospatial":"Lewiston 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.063,\n              44\n            ],\n            [\n              -70,\n              44\n            ],\n            [\n              -70,\n              45\n            ],\n            [\n              -71.063,\n              45\n            ],\n            [\n              -71.063,\n              44\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683838","contributors":{"authors":[{"text":"Domenico, J. A.","contributorId":12028,"corporation":false,"usgs":true,"family":"Domenico","given":"J.","middleInitial":"A.","affiliations":[],"preferred":false,"id":179592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howd, F. H.","contributorId":52965,"corporation":false,"usgs":true,"family":"Howd","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":179593,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":179594,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":18599,"text":"ofr83695 - 1983 - Annual water-resources review, White Sands Missile Range, New Mexico, 1982","interactions":[],"lastModifiedDate":"2022-01-07T21:35:47.318265","indexId":"ofr83695","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-695","title":"Annual water-resources review, White Sands Missile Range, New Mexico, 1982","docAbstract":"<p>Ground-water data were collected in 1982 at White Sands Missile Range in south-central New Mexico. Depth-to-water measurements in the Post Headquarters supply wells continued to show seasonal declines. Test wells east of the Headquarters well field continue to show long-term declines as well as seasonal fluctuations. The total amount of water pumped from White Sands Missile Range supply wells was 66,226,600 gallons more in 1982 than in 1981. The difference in the specific-conductance values of the water samples collected from the Post Headquarters supply wells in the winter and summer increased in 1982.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83695","usgsCitation":"Cruz, R.R., 1983, Annual water-resources review, White Sands Missile Range, New Mexico, 1982: U.S. Geological Survey Open-File Report 83-695, iv, 20 p., https://doi.org/10.3133/ofr83695.","productDescription":"iv, 20 p.","costCenters":[],"links":[{"id":47944,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0695/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394070,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14176.htm"},{"id":150690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0695/report-thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"White Sands Missile Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.816,\n              32.316\n            ],\n            [\n              -106.041,\n              32.316\n            ],\n            [\n              -106.041,\n              34.325\n            ],\n            [\n              -106.816,\n              34.325\n            ],\n            [\n              -106.816,\n              32.316\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b77e","contributors":{"authors":[{"text":"Cruz, R. R.","contributorId":97496,"corporation":false,"usgs":true,"family":"Cruz","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":179407,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17758,"text":"ofr83694 - 1983 - Surface water and climatologic data, Salt Lake County, Utah, water year 1981, with selected data for water years 1980 and 1982","interactions":[],"lastModifiedDate":"2017-09-01T14:33:23","indexId":"ofr83694","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-694","title":"Surface water and climatologic data, Salt Lake County, Utah, water year 1981, with selected data for water years 1980 and 1982","docAbstract":"<p>This report contains precipitation, atmospheric-deposition, water- discharge and water-quality data collected in Salt Lake County as part of two investigations by the U.S. Geological Survey. The purpose of this report is to release data collected mainly during the 1981 water year. Selected data collected during the 1980 water year not previously published or revised and the 1982 water year also are included in this report.</p><p>The first investigation, which was carried out from September 1979 to August 1982, was an urban-runoff study done in cooperation with the Salt Lake County Division of Flood Control and Water Quality. The objectives of the urban-runoff study were to identify the impact of urban runoff on the quantity and quality of the water in the canals east of the Jordan River and on the major tributaries to the river.</p><p>The second investigation, which was carried out from December 1979 to September 1983, is a study of water-quality problems in the Jordan River. The study was done primarily to provide information about toxic substances, dissolved-oxygen depletion, sanitary quality, and turbidity and suspended sediment in the Jordan River. It also was funded in part by the Salt Lake County Division of Flood Control and Water Quality.</p><p>Several Salt Lake County employees assisted in the collection of water- quality samples from storm runoff. Of those employees, Lee R. Armstrong, Gilbert H. Heal, Steven J. Mitckes, and Ben Santistevan worked on a daily basis with the authors and made a significant contribution in the collection of the data contained in this report. Organizations that furnished data are acknowledged in the station descriptions in tables 1 and 4.</p><p>Information for previously published water-discharge, water-quality, atmospheric-deposition, and precipitation data for Salt Lake County are reported by Pyper and others (1981); Dustin (1977); Hely and others (1971) and references that they cited; and Feth and others (1964). Additional water- discharge and water-quality data, published annually by the U.S. Geological Survey, and climatologic data, published monthly by the National Oceanic and Atmospheric Administration, are available for Salt Lake County. (See for example, U.S. Geological Survey, 1982 and National Oceanic and Atmospheric Administration, 1982.)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr83694","collaboration":"Prepared in cooperation with the Salt Lake County Division of Flood Control and Water Quality","usgsCitation":"McCormack, H., Christensen, R., Stephens, D.W., Pyper, G., Weigel, J.F., and Conroy, L., 1983, Surface water and climatologic data, Salt Lake County, Utah, water year 1981, with selected data for water years 1980 and 1982: U.S. Geological Survey Open-File Report 83-694, Report: iv, 586 p.; Plate: 25.89 in. x 19.85 in., https://doi.org/10.3133/ofr83694.","productDescription":"Report: iv, 586 p.; Plate: 25.89 in. x 19.85 in.","numberOfPages":"590","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":150927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0694/report-thumb.jpg"},{"id":46986,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0694/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":46987,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0694/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","county":"Salt Lake County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697b87","contributors":{"authors":[{"text":"McCormack, H.F.","contributorId":93453,"corporation":false,"usgs":true,"family":"McCormack","given":"H.F.","email":"","affiliations":[],"preferred":false,"id":177712,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christensen, R.C.","contributorId":56670,"corporation":false,"usgs":true,"family":"Christensen","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":177709,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stephens, D. W.","contributorId":68335,"corporation":false,"usgs":true,"family":"Stephens","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":177710,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pyper, G. E.","contributorId":35337,"corporation":false,"usgs":true,"family":"Pyper","given":"G. E.","affiliations":[],"preferred":false,"id":177708,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Weigel, J. F.","contributorId":74394,"corporation":false,"usgs":true,"family":"Weigel","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":177711,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Conroy, L.S.","contributorId":6051,"corporation":false,"usgs":true,"family":"Conroy","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":177707,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":17370,"text":"ofr83507 - 1983 - Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","interactions":[{"subject":{"id":17370,"text":"ofr83507 - 1983 - Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","indexId":"ofr83507","publicationYear":"1983","noYear":false,"title":"Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":33390,"text":"b1766 - 1988 - Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","indexId":"b1766","publicationYear":"1988","noYear":false,"title":"Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana"},"id":1}],"supersededBy":{"id":33390,"text":"b1766 - 1988 - Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","indexId":"b1766","publicationYear":"1988","noYear":false,"title":"Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana"},"lastModifiedDate":"2019-09-26T13:27:09","indexId":"ofr83507","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-507","title":"Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr83507","usgsCitation":"Pearson, R.C., Berger, B.R., Kaufmann, H.E., Hanna, W.F., and Zen, E., 1983, Mineral resources of the eastern Pioneer Mountains, Beaverhead County, Montana: U.S. Geological Survey Open-File Report 83-507, ii, 56 p., https://doi.org/10.3133/ofr83507.","productDescription":"ii, 56 p.","costCenters":[],"links":[{"id":151103,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Montana","county":"Beaverhead County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-113.083,45.8651],[-113.074,45.852],[-113.062,45.849],[-113.054,45.8451],[-113.036,45.8326],[-113.026,45.8323],[-113.021,45.8283],[-113.019,45.826],[-113.018,45.8219],[-113.013,45.8188],[-113.004,45.8167],[-112.998,45.8141],[-112.986,45.8079],[-112.965,45.8046],[-112.947,45.7994],[-112.933,45.802],[-112.927,45.8012],[-112.921,45.7981],[-112.921,45.7935],[-112.915,45.7913],[-112.895,45.7889],[-112.89,45.7895],[-112.879,45.7892],[-112.87,45.7811],[-112.864,45.7803],[-112.83,45.7777],[-112.823,45.7765],[-112.819,45.7733],[-112.813,45.7698],[-112.802,45.7617],[-112.787,45.761],[-112.773,45.7521],[-112.764,45.75],[-112.758,45.7469],[-112.755,45.7419],[-112.757,45.735],[-112.747,45.7329],[-112.753,45.7131],[-112.748,45.7041],[-112.736,45.6896],[-112.733,45.6842],[-112.727,45.6806],[-112.724,45.6784],[-112.715,45.6758],[-112.699,45.6756],[-112.697,45.6614],[-112.692,45.6565],[-112.692,45.6547],[-112.693,45.6496],[-112.697,45.6386],[-112.695,45.6349],[-112.691,45.63],[-112.684,45.626],[-112.681,45.6155],[-112.68,45.6054],[-112.686,45.599],[-112.686,45.566],[-112.686,45.5596],[-112.698,45.537],[-112.702,45.5274],[-112.699,45.5215],[-112.695,45.5151],[-112.688,45.5093],[-112.689,45.5061],[-112.688,45.4814],[-112.68,45.4756],[-112.671,45.4698],[-112.662,45.4599],[-112.651,45.4505],[-112.644,45.4469],[-112.632,45.4444],[-112.626,45.4422],[-112.621,45.4391],[-112.616,45.4355],[-112.611,45.4305],[-112.605,45.4274],[-112.575,45.4297],[-112.566,45.434],[-112.541,45.444],[-112.526,45.4419],[-112.507,45.4431],[-112.464,45.3907],[-112.465,45.3495],[-112.459,45.3492],[-112.458,45.2615],[-112.458,45.1733],[-112.457,45.0998],[-112.457,45.0865],[-112.419,45.0866],[-112.333,45.0873],[-112.333,45.0755],[-112.333,45.0312],[-112.332,45.0166],[-112.333,45.0019],[-112.293,45.002],[-112.247,45.0017],[-112.233,45.0019],[-112.191,45.002],[-112.194,44.9125],[-112.167,44.9123],[-112.168,44.8877],[-112.168,44.8827],[-112.168,44.8384],[-112.169,44.826],[-112.147,44.8259],[-112.067,44.7826],[-111.782,44.781],[-111.781,44.7368],[-111.781,44.7231],[-111.782,44.7085],[-111.761,44.7082],[-111.74,44.7084],[-111.66,44.7087],[-111.64,44.7079],[-111.483,44.7077],[-111.487,44.7041],[-111.487,44.7001],[-111.479,44.6843],[-111.476,44.6812],[-111.472,44.6709],[-111.474,44.6647],[-111.486,44.6494],[-111.489,44.6471],[-111.491,44.6442],[-111.494,44.6428],[-111.497,44.6433],[-111.516,44.6421],[-111.515,44.6397],[-111.512,44.6373],[-111.509,44.6339],[-111.506,44.6316],[-111.505,44.6295],[-111.507,44.6261],[-111.511,44.6222],[-111.512,44.6211],[-111.521,44.6147],[-111.523,44.6077],[-111.523,44.6044],[-111.521,44.5919],[-111.521,44.5905],[-111.515,44.5815],[-111.512,44.579],[-111.506,44.568],[-111.508,44.563],[-111.502,44.5612],[-111.499,44.5615],[-111.493,44.5613],[-111.476,44.555],[-111.465,44.5406],[-111.469,44.5402],[-111.495,44.5421],[-111.512,44.5356],[-111.514,44.5361],[-111.517,44.5373],[-111.521,44.5411],[-111.552,44.5563],[-111.554,44.5555],[-111.565,44.556],[-111.595,44.5597],[-111.627,44.5516],[-111.631,44.552],[-111.636,44.5517],[-111.667,44.5547],[-111.672,44.5566],[-111.685,44.5594],[-111.698,44.5585],[-111.699,44.5586],[-111.71,44.5533],[-111.746,44.5395],[-111.763,44.5281],[-111.764,44.528],[-111.786,44.5251],[-111.79,44.5249],[-111.793,44.5255],[-111.808,44.5212],[-111.81,44.5157],[-111.811,44.5143],[-111.816,44.5115],[-111.826,44.5136],[-111.873,44.5659],[-111.894,44.5624],[-111.907,44.5579],[-111.953,44.5518],[-111.954,44.5505],[-111.967,44.5448],[-111.988,44.537],[-112.004,44.538],[-112.011,44.5416],[-112.03,44.5446],[-112.037,44.5439],[-112.04,44.5407],[-112.038,44.5394],[-112.029,44.5282],[-112.033,44.5279],[-112.035,44.5284],[-112.056,44.5376],[-112.07,44.5367],[-112.094,44.53],[-112.114,44.5254],[-112.117,44.5265],[-112.137,44.5378],[-112.156,44.5382],[-112.173,44.5416],[-112.191,44.5368],[-112.195,44.5376],[-112.225,44.5467],[-112.23,44.5593],[-112.247,44.5681],[-112.254,44.5687],[-112.262,44.5676],[-112.286,44.5691],[-112.289,44.5675],[-112.29,44.5627],[-112.304,44.5597],[-112.314,44.5519],[-112.313,44.5415],[-112.317,44.5392],[-112.331,44.5384],[-112.333,44.5387],[-112.342,44.5393],[-112.356,44.533],[-112.358,44.5083],[-112.357,44.5024],[-112.358,44.4977],[-112.392,44.45],[-112.397,44.4533],[-112.404,44.4561],[-112.407,44.4566],[-112.411,44.4559],[-112.431,44.4559],[-112.433,44.4582],[-112.439,44.4644],[-112.441,44.4654],[-112.454,44.4687],[-112.46,44.4765],[-112.47,44.4785],[-112.504,44.4645],[-112.507,44.4658],[-112.518,44.4764],[-112.545,44.4859],[-112.555,44.4859],[-112.624,44.4859],[-112.629,44.4903],[-112.632,44.4916],[-112.638,44.4918],[-112.652,44.4895],[-112.655,44.489],[-112.688,44.4977],[-112.725,44.5047],[-112.736,44.4995],[-112.764,44.4896],[-112.768,44.4883],[-112.779,44.4848],[-112.787,44.4791],[-112.794,44.4719],[-112.795,44.4703],[-112.798,44.4663],[-112.801,44.4623],[-112.803,44.4602],[-112.82,44.4508],[-112.828,44.444],[-112.829,44.4406],[-112.837,44.4267],[-112.837,44.4254],[-112.835,44.42],[-112.828,44.4146],[-112.819,44.4033],[-112.814,44.3948],[-112.814,44.3894],[-112.816,44.3775],[-112.819,44.3725],[-112.821,44.3706],[-112.833,44.3647],[-112.846,44.3577],[-112.848,44.358],[-112.856,44.3616],[-112.861,44.3647],[-112.877,44.3777],[-112.88,44.3824],[-112.89,44.4045],[-112.907,44.4001],[-112.911,44.4009],[-112.913,44.4019],[-112.921,44.409],[-112.925,44.4105],[-112.946,44.4151],[-112.948,44.4161],[-112.959,44.424],[-112.981,44.4352],[-112.996,44.4473],[-113.009,44.4597],[-113.009,44.4629],[-113.01,44.4746],[-113.012,44.4766],[-113.023,44.4908],[-113.021,44.5032],[-113.017,44.5075],[-113.016,44.5093],[-113.014,44.5145],[-113.012,44.519],[-113.009,44.525],[-113.03,44.5363],[-113.048,44.5473],[-113.048,44.5481],[-113.039,44.5605],[-113.038,44.5649],[-113.043,44.5681],[-113.065,44.5889],[-113.069,44.591],[-113.077,44.5958],[-113.085,44.6013],[-113.085,44.6031],[-113.084,44.6078],[-113.082,44.609],[-113.074,44.6158],[-113.067,44.6202],[-113.052,44.6291],[-113.051,44.6334],[-113.054,44.6407],[-113.059,44.6453],[-113.066,44.6577],[-113.069,44.6725],[-113.068,44.6775],[-113.08,44.6884],[-113.083,44.6925],[-113.085,44.6934],[-113.1,44.7071],[-113.1,44.7168],[-113.104,44.7306],[-113.119,44.7392],[-113.126,44.7499],[-113.135,44.7558],[-113.137,44.7594],[-113.137,44.7627],[-113.132,44.7698],[-113.132,44.7722],[-113.135,44.7754],[-113.14,44.7774],[-113.158,44.7826],[-113.162,44.7831],[-113.206,44.808],[-113.254,44.8213],[-113.296,44.8044],[-113.319,44.7939],[-113.323,44.7918],[-113.33,44.7886],[-113.344,44.788],[-113.349,44.7895],[-113.353,44.7984],[-113.35,44.8006],[-113.346,44.8039],[-113.347,44.8074],[-113.349,44.8143],[-113.391,44.8384],[-113.397,44.8385],[-113.402,44.8391],[-113.423,44.8405],[-113.425,44.8442],[-113.427,44.8534],[-113.434,44.8557],[-113.45,44.8652],[-113.46,44.8786],[-113.477,44.9007],[-113.473,44.9076],[-113.475,44.9126],[-113.476,44.9138],[-113.492,44.926],[-113.494,44.931],[-113.495,44.9355],[-113.496,44.9452],[-113.491,44.9492],[-113.488,44.9495],[-113.464,44.9509],[-113.455,44.9524],[-113.449,44.9556],[-113.447,44.958],[-113.447,44.9749],[-113.447,44.9917],[-113.446,44.9964],[-113.445,44.9994],[-113.442,45.0012],[-113.439,45.0078],[-113.441,45.0118],[-113.443,45.0159],[-113.447,45.0255],[-113.449,45.0345],[-113.451,45.0553],[-113.455,45.0599],[-113.459,45.0609],[-113.472,45.0615],[-113.481,45.0615],[-113.489,45.0662],[-113.488,45.072],[-113.489,45.0742],[-113.497,45.0794],[-113.522,45.0923],[-113.521,45.0932],[-113.506,45.1096],[-113.508,45.1118],[-113.516,45.1146],[-113.53,45.1153],[-113.544,45.111],[-113.552,45.1129],[-113.554,45.1146],[-113.571,45.1249],[-113.575,45.1311],[-113.573,45.1345],[-113.57,45.145],[-113.592,45.1584],[-113.593,45.1646],[-113.59,45.18],[-113.62,45.2025],[-113.638,45.214],[-113.647,45.225],[-113.649,45.2278],[-113.657,45.2404],[-113.669,45.2485],[-113.676,45.2497],[-113.679,45.2507],[-113.687,45.2574],[-113.69,45.2726],[-113.68,45.2747],[-113.682,45.2787],[-113.691,45.2876],[-113.714,45.3092],[-113.721,45.3149],[-113.733,45.3222],[-113.739,45.3336],[-113.738,45.3441],[-113.737,45.346],[-113.734,45.3534],[-113.732,45.3567],[-113.732,45.3593],[-113.734,45.3621],[-113.736,45.3689],[-113.733,45.3754],[-113.736,45.3924],[-113.774,45.4081],[-113.775,45.4161],[-113.774,45.4165],[-113.765,45.422],[-113.762,45.4299],[-113.763,45.43],[-113.774,45.435],[-113.774,45.4421],[-113.778,45.4494],[-113.775,45.4635],[-113.773,45.4692],[-113.767,45.4728],[-113.762,45.4774],[-113.759,45.4859],[-113.767,45.5032],[-113.778,45.5234],[-113.803,45.5229],[-113.826,45.5204],[-113.831,45.518],[-113.834,45.5196],[-113.833,45.5214],[-113.828,45.5328],[-113.824,45.5433],[-113.815,45.5628],[-113.814,45.5714],[-113.801,45.58],[-113.799,45.5817],[-113.797,45.5849],[-113.799,45.588],[-113.803,45.5948],[-113.817,45.6084],[-113.821,45.6107],[-113.829,45.6113],[-113.845,45.6139],[-113.861,45.6229],[-113.874,45.6202],[-113.888,45.617],[-113.905,45.6215],[-113.906,45.6264],[-113.9,45.6323],[-113.897,45.6483],[-113.93,45.6735],[-113.932,45.6785],[-113.934,45.6942],[-113.922,45.7037],[-113.913,45.7003],[-113.908,45.7023],[-113.91,45.7113],[-113.903,45.7216],[-113.907,45.7275],[-113.91,45.7379],[-113.913,45.7465],[-113.905,45.755],[-113.898,45.7629],[-113.887,45.7687],[-113.877,45.7749],[-113.863,45.7794],[-113.85,45.7595],[-113.849,45.7504],[-113.839,45.7493],[-113.83,45.7513],[-113.824,45.757],[-113.817,45.7571],[-113.797,45.7622],[-113.801,45.7699],[-113.797,45.7732],[-113.794,45.792],[-113.772,45.7903],[-113.77,45.7972],[-113.739,45.8149],[-113.726,45.8271],[-113.713,45.8347],[-113.697,45.841],[-113.678,45.8374],[-113.662,45.8345],[-113.649,45.8367],[-113.641,45.8378],[-113.627,45.8395],[-113.622,45.841],[-113.612,45.8503],[-113.602,45.8501],[-113.593,45.8508],[-113.593,45.8636],[-113.587,45.8683],[-113.579,45.8717],[-113.56,45.874],[-113.55,45.8756],[-113.541,45.8762],[-113.534,45.8782],[-113.531,45.8801],[-113.532,45.8837],[-113.537,45.8942],[-113.539,45.9014],[-113.535,45.9125],[-113.533,45.9185],[-113.526,45.9278],[-113.518,45.9353],[-113.519,45.9376],[-113.508,45.942],[-113.503,45.9425],[-113.499,45.9389],[-113.491,45.9263],[-113.49,45.9204],[-113.486,45.9118],[-113.47,45.8961],[-113.467,45.8861],[-113.451,45.8631],[-113.44,45.8473],[-113.441,45.8441],[-113.434,45.8319],[-113.431,45.8256],[-113.433,45.8131],[-113.434,45.804],[-113.423,45.7923],[-113.417,45.7869],[-113.411,45.7857],[-113.405,45.7799],[-113.4,45.7722],[-113.391,45.7632],[-113.379,45.7521],[-113.374,45.749],[-113.365,45.7537],[-113.363,45.762],[-113.362,45.7703],[-113.355,45.7855],[-113.345,45.8045],[-113.331,45.8125],[-113.317,45.8069],[-113.296,45.8156],[-113.285,45.8167],[-113.273,45.817],[-113.258,45.8319],[-113.253,45.8453],[-113.247,45.8495],[-113.235,45.8589],[-113.215,45.874],[-113.21,45.8741],[-113.19,45.8758],[-113.177,45.8829],[-113.165,45.885],[-113.143,45.8813],[-113.111,45.8801],[-113.096,45.8786],[-113.091,45.8727],[-113.089,45.8709],[-113.087,45.8696],[-113.083,45.8651]]]},\"properties\":{\"name\":\"Beaverhead\",\"state\":\"MT\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699fcb","contributors":{"authors":[{"text":"Pearson, R. C.","contributorId":30978,"corporation":false,"usgs":true,"family":"Pearson","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":176133,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berger, B. R.","contributorId":77914,"corporation":false,"usgs":true,"family":"Berger","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":176136,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaufmann, H. E.","contributorId":40215,"corporation":false,"usgs":true,"family":"Kaufmann","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":176135,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hanna, W. F.","contributorId":6835,"corporation":false,"usgs":true,"family":"Hanna","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":176132,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zen, E-an","contributorId":38564,"corporation":false,"usgs":true,"family":"Zen","given":"E-an","affiliations":[],"preferred":false,"id":176134,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":17252,"text":"ofr83223 - 1983 - Hydrology of Area 1, eastern coal province, Pennsylvania [West Branch Susquehanna River, Sinnemahoning Creek, Upper Juniata River, Clearfield Creek]","interactions":[],"lastModifiedDate":"2022-02-07T21:20:37.876385","indexId":"ofr83223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-223","title":"Hydrology of Area 1, eastern coal province, Pennsylvania [West Branch Susquehanna River, Sinnemahoning Creek, Upper Juniata River, Clearfield Creek]","docAbstract":"<p>Provisions of the Surface Mining Control and Reclamation Act of 1977 recognized a nationwide need for hydrologic information in mined and potentially mined areas. This report is designed to be useful to mine owners, operators, regulatory authorities, citizens groups, and others by presenting information on existing hydrologic conditions and by identifying additional sources of hydrologic information. General hydrologic information is presented in a brief text accompanied by a map, chart, graph, or other illustration for each of a series of water resources-related topics. The summation of the topical discussions provides a description of the hydrology of the area.</p><p>The Eastern Coal Province has been divided into 24 hydrologic study areas which are shown on the cover of this report. The divisions are based on hydrologic factors, location, and size. Hydrologic units (surface drainage basins) or parts of units are combined to form each study area.</p><p>Area 1 covers 7,400 square miles of the Eastern Coal Province in part or all of 18 counties in west-central Pennsylvania. The major streams in the area are the West Branch Susquehanna and Juniata Rivers. Area 1 counties produced more than 20,000,000 tons of coal during 1979. About 66,000 acres of disturbed coal land in Area 1 counties are in need of reclamation.</p><p>Streamflow data have been collected at 146 locations in the area, and water-quality data have been collected at 123 locations. Interpretations of water quality in this report are generally based on a series of four water-quality samples collected at each of 113 locations during the 1979-80 water years. Water-quality data collected at these sites included: specific conductance; dissolved solids; pH; acidity; alkalinty; total and dissolved iron; total and dissolved manganese; sulfate; and bed-material iron, manganese, coal, and organic carbon. Most sites had benthic invertebrate populations sampled and analyses of bed-material constituents. A smaller set of sites was sampled for common constituents and minor elements.</p><p>Streams in Clearfield and Cambria Counties, the two leading coal producers in the area, had median specific conductances and dissolved-solids concentrations three to five times greater than those from other area counties. Clearfield County streams had the lowest median stream pH in the area. Most streams sampled in the area had acidity in excess of alkalinity. Streams in the three major coal producing counties in the area had median total-iron concentrations two to three times higher than those for other area counties, and the same general pattern was found for total manganese. The median sulfate concentration of a county's streams showed a close positive correlation with the amount of coal mined in the county. Iron and coal concentrations in bed material were higher in coal-producing counties, but manganese concentrations in bed material were not higher. Twenty-eight streams did not have a benthic biological community as defined by the Office of Surface Mining. Three-fourths of the sites with no biological community had levels of pH, acidity, iron, manganese, and sulfate indicative of acid mine drainage.</p><p>Statistics on low flow, mean flow, peak flow, and flow-duration can be computed from gaging station records for gaged streams. The same statistics can be estimated for ungaged streams through the use of regression or graphical techniques. This information may be useful in preparing and evaluating mine-permit applications.</p><p>Aquifers in the area receive most recharge from precipitation on outcrop areas. Highest ground-water levels generally occur in spring, decline during the summer, and begin to rise again during the fall. Water levels in valleys generally show less fluctuation than on hills. Median well yields in the area range from 5 to 50 gallons per minute. Ground-water supplies are obtained from more than 40 formations. Ground-water quality is generally suitable for most uses.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83223","usgsCitation":"Herb, W.J., Brown, D.E., Shaw, L.C., and Becher, A.E., 1983, Hydrology of Area 1, eastern coal province, Pennsylvania [West Branch Susquehanna River, Sinnemahoning Creek, Upper Juniata River, Clearfield Creek]: U.S. Geological Survey Open-File Report 83-223, vi, 89 p., https://doi.org/10.3133/ofr83223.","productDescription":"vi, 89 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":149364,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0223/report-thumb.jpg"},{"id":94516,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0223/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.31579589843749,\n              39.87601941962116\n            ],\n            [\n              -77.47558593749999,\n              39.87601941962116\n            ],\n            [\n              -77.47558593749999,\n              41.93088998442502\n            ],\n            [\n              -79.31579589843749,\n              41.93088998442502\n            ],\n            [\n              -79.31579589843749,\n              39.87601941962116\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604b72","contributors":{"authors":[{"text":"Herb, William J.","contributorId":79454,"corporation":false,"usgs":true,"family":"Herb","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":175611,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Deborah E.","contributorId":92255,"corporation":false,"usgs":true,"family":"Brown","given":"Deborah","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":175614,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shaw, Lewis C.","contributorId":84433,"corporation":false,"usgs":true,"family":"Shaw","given":"Lewis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":175612,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Becher, Albert E.","contributorId":82979,"corporation":false,"usgs":true,"family":"Becher","given":"Albert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":175613,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1348,"text":"wsp2216 - 1983 - Daily water and sediment discharges from selected rivers of the eastern United States; a time-series modeling approach","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp2216","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"2216","title":"Daily water and sediment discharges from selected rivers of the eastern United States; a time-series modeling approach","docAbstract":"Time-series models were constructed for analysis of daily runoff and sediment discharge data from selected rivers of the Eastern United States. Logarithmic transformation and first-order differencing of the data sets were necessary to produce second-order, stationary time series and remove seasonal trends. \r\n\r\nCyclic models accounted for less than 42 percent of the variance in the water series and 31 percent in the sediment series. Analysis of the apparent oscillations of given frequencies occurring in the data indicates that frequently occurring storms can account for as much as 50 percent of the variation in sediment discharge. \r\n\r\nComponents of the frequency analysis indicate that a linear representation is reasonable for the water-sediment system. Models that incorporate lagged water discharge as input prove superior to univariate techniques in modeling and prediction of sediment discharges. The random component of the models includes errors in measurement and model hypothesis and indicates no serial correlation. An index of sediment production within or between drain-gage basins can be calculated from model parameters.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wsp2216","usgsCitation":"Fitzgerald, M.G., and Karlinger, M.R., 1983, Daily water and sediment discharges from selected rivers of the eastern United States; a time-series modeling approach: U.S. Geological Survey Water Supply Paper 2216, vi, 24 p. :ill., 1 map ;27 cm., https://doi.org/10.3133/wsp2216.","productDescription":"vi, 24 p. :ill., 1 map ;27 cm.","costCenters":[],"links":[{"id":137526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2216/report-thumb.jpg"},{"id":26423,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2216/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65acb2","contributors":{"authors":[{"text":"Fitzgerald, Michael G.","contributorId":42942,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"Michael","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":143606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karlinger, Michael R.","contributorId":10777,"corporation":false,"usgs":true,"family":"Karlinger","given":"Michael","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143605,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29224,"text":"wri824065 - 1983 - Numerical simulation of ground-water flow in lower Satus Creek Basin, Yakima Indian Reservation, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri824065","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4065","title":"Numerical simulation of ground-water flow in lower Satus Creek Basin, Yakima Indian Reservation, Washington","docAbstract":"A multilayer numerical model of steady-state ground-water flow in lower Satus Creek basin was constructed, calibrated using time-averaged data, and used to estimate the long-term effects of proposed irrigation-water management plans on ground-water levels in the area. Model computations showed that irrigation of new lands in the Satus uplands would raise ground-water levels in lower Satus Creek basin and thereby increase the size of the waterlogged areas. The model also demonstrated that pumping water from wells, reducing the amount of irrigation water used in the lowlands, and stopping leakage from Satus No. 2 and 3 Pump Canals were all effective methods to alleviate present waterlogging in some parts of the basin and to counteract some of the anticipated ground-water-level rises that would be caused by irrigating the uplands. The proposed changes in water use affected model-computed ground-water levels most in the eastern part of the basin between Satus No. 2 and No. 3 Pump Canals. The effects on ground-water levels in the western part of the basin between Satus Creek and Satus No. 2 Pump Canal were smaller. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824065","usgsCitation":"Prych, E., 1983, Numerical simulation of ground-water flow in lower Satus Creek Basin, Yakima Indian Reservation, Washington: U.S. Geological Survey Water-Resources Investigations Report 82-4065, xi, 89 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824065.","productDescription":"xi, 89 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4065/report-thumb.jpg"},{"id":58077,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4065/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58078,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4065/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69680c","contributors":{"authors":[{"text":"Prych, E. A.","contributorId":36163,"corporation":false,"usgs":true,"family":"Prych","given":"E. A.","affiliations":[],"preferred":false,"id":201175,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38149,"text":"ofr82445 - 1983 - Aquifer systems in the Great Basin region of Nevada, Utah, and adjacent states: A study plan","interactions":[],"lastModifiedDate":"2022-10-17T15:30:33.03952","indexId":"ofr82445","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-445","title":"Aquifer systems in the Great Basin region of Nevada, Utah, and adjacent states: A study plan","docAbstract":"<p>The Great Basin Regional Aquifer Study includes about 140,000 square miles in parts of Nevada, Utah, California, Idaho, Oregon, and Arizona. Within that area, 240 hydrographic areas occupy structural depressions formed primarily by basin-and-range faulting. The principal aquifers are in basin- fill deposits; however, permeable carbonate rocks underlie valleys in much of eastern Nevada and western Utah and are significant regional aquifers. Anticipated future water needs require a better understanding of the resource so that wise management will be possible. In October 1980, the U.S Geological Survey started a 4-year study to (1) describe the ground-water systems as they existed under natural conditions and as they exist today, (2) analyze the changes that have led to the systems' present condition, (3) tie the results of this and previous studies together in a regional analysis, and (4) provide means by which effects of future ground-water development can be estimated.</p><p>A plan of work is presented that describes the general approach to be taken in this study. It defines (1) the major task necessary to meet objectives and (2) constraints on the scope of work. The approach has been strongly influenced by the diverse nature of ground-water flow systems and the large number of basins. A detailed appraisal of 240 individual areas would require more resources than are available. Consequently, the general approach is to study selected \"typical\" areas and key hydrologic processes. Effort during the first 3 years will be directed toward describing the regional hydrology, conducting detailed studies of \"type\" areas, and studying selected hydrologic processes. Effort during the final year will be directed toward developing a regional analyses of results.</p><p>Special studies that will address hydrologic processes, key components of the ground-water system, and improved use of technology include evaluations of regional geochemistry, regional hydrogeology, recharge, ground-water discharge, and the use of remote sensing. Areas selected for study using ground-water flow models include the regional carbonate-rock province in eastern Nevada and western Utah, six valleys Las Vegas, Carson, Paradise, Dixie, Smith Creek, and Stagecoach in Nevada, plus Jordan Valley, the Milford area, and Tule Valley in Utah.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Carson City, NV","doi":"10.3133/ofr82445","usgsCitation":"Harrill, J.R., Welch, A., Prudic, D.E., Thomas, J.M., Carman, R.L., Plume, R.W., Gates, J., and Mason, J.L., 1983, Aquifer systems in the Great Basin region of Nevada, Utah, and adjacent states: A study plan: U.S. Geological Survey Open-File Report 82-445, Report: v, 49 p.; Plate: 24.00 in. x 20.00 in., https://doi.org/10.3133/ofr82445.","productDescription":"Report: v, 49 p.; Plate: 24.00 in. x 20.00 in.","numberOfPages":"54","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":64410,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0445/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0445/report-thumb.jpg"},{"id":20564,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0445/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada, Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679f6b","contributors":{"authors":[{"text":"Harrill, James R.","contributorId":99533,"corporation":false,"usgs":true,"family":"Harrill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":219211,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Welch, Alan H.","contributorId":45286,"corporation":false,"usgs":true,"family":"Welch","given":"Alan H.","affiliations":[],"preferred":false,"id":219205,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":219206,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thomas, James M.","contributorId":195094,"corporation":false,"usgs":false,"family":"Thomas","given":"James","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":219210,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Carman, Rita L.","contributorId":6468,"corporation":false,"usgs":true,"family":"Carman","given":"Rita","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":219207,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Plume, Russell W. rwplume@usgs.gov","contributorId":2303,"corporation":false,"usgs":true,"family":"Plume","given":"Russell","email":"rwplume@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":219208,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":219212,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Mason, James L.","contributorId":14397,"corporation":false,"usgs":true,"family":"Mason","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":219209,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":26904,"text":"wri81215 - 1983 - Effects on water quality of coal mining in the basin of the North Fork Kentucky River, eastern Kentucky","interactions":[],"lastModifiedDate":"2021-01-27T19:43:43.31003","indexId":"wri81215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"81-215","title":"Effects on water quality of coal mining in the basin of the North Fork Kentucky River, eastern Kentucky","docAbstract":"A study of the effects on water quality of coal mining in the basin of the North Fork Kentucky River shows increases in the mean annual total dissolved solids concentrations from about 8 to 50 milligrams per liter. It shows that the Hazard Number 9 coal seam produces the largest quantities of acid and sulfate. The study also shows that most of the acid mine drainage is neutralized by carbonate minerals or is replaced by exchangeable bases from the aquifer materials before it reaches the streams. The generation of sediment is probably the most damaging effect of strip mining on water quality in the basin. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri81215","usgsCitation":"Dyer, K.L., 1983, Effects on water quality of coal mining in the basin of the North Fork Kentucky River, eastern Kentucky: U.S. Geological Survey Water-Resources Investigations Report 81-215, Report: vi, 94 p.; 3 Plates: 18.00 x 18.68 inches or smaller, https://doi.org/10.3133/wri81215.","productDescription":"Report: vi, 94 p.; 3 Plates: 18.00 x 18.68 inches or smaller","costCenters":[],"links":[{"id":382716,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/0215/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382715,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/0215/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382714,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/0215/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382713,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0215/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157777,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0215/report-thumb.jpgg"}],"country":"United States","state":"Kentucky","otherGeospatial":"North Fork Kentucky River","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-89.485106,36.497692],[-89.5391,36.498201],[-89.570071,36.544387],[-89.571509,36.552569],[-89.563185,36.568749],[-89.546113,36.579989],[-89.527583,36.581147],[-89.480893,36.569771],[-89.465445,36.536163],[-89.47246,36.513741],[-89.485106,36.497692]]],[[[-82.333044,37.740969],[-82.319686,37.734404],[-82.307235,37.707669],[-82.298074,37.704143],[-82.301964,37.696223],[-82.297126,37.684228],[-82.303867,37.678392],[-82.296724,37.678071],[-82.291773,37.669143],[-82.284687,37.675277],[-82.257111,37.656749],[-82.23939,37.661465],[-82.226111,37.653092],[-82.209691,37.625103],[-82.187298,37.626935],[-82.191444,37.644378],[-82.174688,37.646529],[-82.172762,37.634008],[-82.18143,37.621842],[-82.164191,37.620192],[-82.168137,37.608495],[-82.158554,37.609546],[-82.156718,37.59279],[-82.131977,37.593537],[-82.127321,37.586667],[-82.127303,37.572681],[-82.144648,37.568315],[-82.133954,37.562245],[-82.133299,37.552996],[-82.121985,37.552763],[-82.116584,37.559588],[-82.103127,37.560097],[-82.098924,37.5533],[-82.07503,37.555824],[-82.064792,37.539021],[-82.049584,37.535222],[-82.048205,37.528972],[-82.042397,37.533916],[-82.04478,37.546713],[-82.038972,37.547926],[-82.028826,37.537667],[-82.021006,37.540526],[-82.009194,37.533243],[-81.999844,37.542579],[-81.992597,37.538323],[-81.970147,37.546504],[-81.964971,37.543026],[-82.309415,37.300066],[-82.324619,37.28318],[-82.341849,37.280886],[-82.342068,37.274109],[-82.350948,37.267077],[-82.449164,37.243908],[-82.486439,37.231204],[-82.491486,37.225086],[-82.498858,37.227044],[-82.520117,37.212906],[-82.528746,37.213742],[-82.592451,37.182847],[-82.633493,37.154264],[-82.651646,37.151908],[-82.676765,37.134965],[-82.722097,37.120168],[-82.726201,37.115882],[-82.721617,37.101276],[-82.724954,37.091905],[-82.717204,37.079544],[-82.727022,37.073019],[-82.722254,37.057948],[-82.724714,37.042758],[-82.742454,37.04298],[-82.747981,37.025214],[-82.759175,37.027333],[-82.782144,37.008242],[-82.828592,37.005707],[-82.836008,36.988837],[-82.866019,36.978272],[-82.870274,36.965993],[-82.855705,36.953808],[-82.861282,36.944848],[-82.857965,36.929529],[-82.876215,36.910218],[-82.873213,36.897263],[-82.878569,36.889585],[-82.910315,36.874055],[-82.970253,36.857686],[-82.998376,36.85663],[-83.006086,36.847889],[-83.021887,36.849989],[-83.025887,36.855289],[-83.07259,36.854589],[-83.07519,36.840889],[-83.101792,36.829089],[-83.098492,36.814289],[-83.103092,36.806689],[-83.131694,36.781488],[-83.131245,36.767105],[-83.125655,36.761407],[-83.127833,36.750828],[-83.136395,36.743088],[-83.194597,36.739487],[-83.311403,36.710287],[-83.386099,36.686589],[-83.423707,36.667385],[-83.466483,36.6647],[-83.498011,36.670485],[-83.531912,36.664984],[-83.577312,36.641784],[-83.607913,36.637083],[-83.628913,36.624083],[-83.648314,36.622683],[-83.649513,36.616683],[-83.673114,36.604682],[-83.690714,36.582581],[-84.543138,36.596277],[-84.843091,36.605127],[-85.024627,36.619354],[-85.195372,36.625498],[-85.290627,36.62645],[-85.488353,36.614994],[-85.677789,36.618157],[-86.03277,36.630367],[-86.333051,36.648778],[-86.507771,36.652445],[-86.543777,36.640536],[-86.550054,36.644817],[-86.551292,36.637985],[-86.564143,36.633472],[-86.589906,36.652486],[-87.853204,36.633247],[-87.849567,36.663701],[-88.070532,36.678118],[-88.068208,36.659747],[-88.045127,36.602939],[-88.032489,36.540662],[-88.037822,36.51385],[-88.053205,36.497129],[-89.300284,36.507147],[-89.417293,36.499033],[-89.382762,36.583603],[-89.376367,36.613868],[-89.365548,36.625059],[-89.327589,36.632194],[-89.27171,36.571387],[-89.259994,36.565149],[-89.236542,36.566824],[-89.213563,36.580119],[-89.202607,36.601576],[-89.197654,36.628936],[-89.15908,36.666352],[-89.168723,36.671892],[-89.169522,36.688878],[-89.19948,36.716045],[-89.199798,36.734217],[-89.184523,36.753638],[-89.169106,36.759473],[-89.130399,36.751702],[-89.119198,36.759802],[-89.116067,36.772423],[-89.123481,36.785258],[-89.155891,36.789126],[-89.171069,36.798119],[-89.179229,36.812915],[-89.178888,36.831368],[-89.1704,36.841522],[-89.137969,36.847349],[-89.117567,36.887356],[-89.099007,36.961389],[-89.11503,36.980335],[-89.132685,36.9822],[-89.17112,37.008072],[-89.180849,37.026843],[-89.181369,37.046305],[-89.168087,37.074218],[-89.154504,37.088907],[-89.14132,37.093865],[-89.111189,37.119052],[-89.086526,37.165602],[-89.029981,37.211144],[-89.000968,37.224401],[-88.966831,37.229891],[-88.933077,37.227749],[-88.80572,37.188595],[-88.732105,37.143956],[-88.693983,37.141155],[-88.625889,37.119458],[-88.545403,37.070003],[-88.504437,37.065265],[-88.458948,37.073796],[-88.424776,37.149901],[-88.447764,37.203527],[-88.471753,37.220155],[-88.487277,37.244077],[-88.508031,37.260261],[-88.515939,37.284043],[-88.484462,37.345609],[-88.476592,37.386875],[-88.456,37.408482],[-88.408808,37.425216],[-88.365471,37.401663],[-88.312585,37.440591],[-88.281667,37.452596],[-88.135142,37.471626],[-88.087664,37.471059],[-88.064234,37.484548],[-88.061292,37.505232],[-88.069018,37.525297],[-88.131622,37.572968],[-88.139973,37.586451],[-88.142225,37.603737],[-88.156827,37.632801],[-88.159372,37.661847],[-88.122412,37.709685],[-88.059588,37.742608],[-88.02803,37.799224],[-87.997102,37.797672],[-87.95259,37.771742],[-87.944506,37.775256],[-87.932554,37.797672],[-87.90681,37.807624],[-87.903804,37.817762],[-87.910276,37.843416],[-87.936228,37.867937],[-87.941021,37.879168],[-87.938365,37.890802],[-87.904789,37.924892],[-87.892471,37.92793],[-87.87254,37.920999],[-87.830578,37.876516],[-87.7909,37.875714],[-87.76226,37.890906],[-87.717971,37.89257],[-87.67573,37.90193],[-87.666481,37.895786],[-87.66282,37.881449],[-87.681633,37.855917],[-87.679188,37.836321],[-87.666522,37.827455],[-87.635806,37.827015],[-87.612426,37.83384],[-87.588729,37.860984],[-87.591582,37.887194],[-87.620272,37.906922],[-87.62896,37.926714],[-87.606216,37.949642],[-87.601416,37.972542],[-87.585916,37.975442],[-87.574715,37.967742],[-87.57203,37.947466],[-87.559342,37.931146],[-87.511499,37.906426],[-87.447786,37.942427],[-87.418585,37.944763],[-87.380247,37.935596],[-87.344933,37.911164],[-87.302599,37.898558],[-87.220944,37.849134],[-87.158878,37.837871],[-87.14195,37.816176],[-87.129629,37.786608],[-87.111133,37.782512],[-87.090636,37.787808],[-87.067836,37.806065],[-87.043854,37.870796],[-87.045101,37.893775],[-87.033444,37.906593],[-86.969044,37.932858],[-86.919329,37.936664],[-86.85595,37.987292],[-86.820071,37.999392],[-86.794985,37.988982],[-86.765054,37.93251],[-86.73146,37.89434],[-86.718462,37.893123],[-86.680929,37.91501],[-86.647081,37.908621],[-86.644754,37.894806],[-86.661233,37.862761],[-86.661637,37.849714],[-86.655286,37.842505],[-86.638265,37.842718],[-86.609163,37.855408],[-86.598108,37.867382],[-86.599848,37.906754],[-86.588581,37.921159],[-86.534156,37.917007],[-86.507831,37.928829],[-86.50939,37.942492],[-86.525174,37.968228],[-86.521825,38.038327],[-86.51176,38.044448],[-86.452192,38.05049],[-86.432789,38.067171],[-86.430091,38.078638],[-86.434046,38.086763],[-86.463858,38.101177],[-86.463248,38.119278],[-86.449793,38.127223],[-86.431749,38.126121],[-86.401653,38.105396],[-86.379775,38.129274],[-86.335145,38.129242],[-86.323453,38.139032],[-86.321274,38.147418],[-86.325941,38.154317],[-86.37174,38.164183],[-86.377434,38.171379],[-86.373801,38.193352],[-86.360377,38.198796],[-86.287773,38.15805],[-86.271802,38.137874],[-86.27872,38.089303],[-86.273584,38.067443],[-86.261273,38.052721],[-86.220371,38.027922],[-86.178983,38.011308],[-86.12757,38.016011],[-86.095766,38.00893],[-86.075393,37.996948],[-86.053912,37.963571],[-86.038188,37.95935],[-86.029509,37.99264],[-85.951467,38.005608],[-85.925418,38.023456],[-85.906163,38.08617],[-85.908764,38.161169],[-85.894764,38.188469],[-85.845464,38.23027],[-85.829364,38.276769],[-85.780963,38.288469],[-85.761062,38.27257],[-85.744862,38.26717],[-85.683561,38.295469],[-85.653641,38.327108],[-85.638777,38.361443],[-85.632937,38.395666],[-85.607629,38.439295],[-85.587758,38.450495],[-85.536542,38.456083],[-85.498866,38.468242],[-85.474354,38.504074],[-85.423077,38.531581],[-85.4156,38.546341],[-85.415821,38.563558],[-85.437446,38.601724],[-85.438742,38.659319],[-85.456978,38.689135],[-85.452114,38.709348],[-85.434065,38.729455],[-85.410925,38.73708],[-85.363827,38.730477],[-85.306049,38.741649],[-85.275454,38.741172],[-85.246505,38.731821],[-85.213257,38.695446],[-85.172528,38.688082],[-85.13868,38.699168],[-85.103313,38.725323],[-84.990006,38.778383],[-84.941071,38.775627],[-84.887919,38.794652],[-84.814641,38.784488],[-84.813939,38.800209],[-84.829958,38.830632],[-84.791002,38.860572],[-84.785234,38.880439],[-84.812746,38.895132],[-84.867778,38.899133],[-84.877029,38.909016],[-84.877762,38.920357],[-84.83516,38.957961],[-84.829857,38.969385],[-84.83712,38.988059],[-84.889065,39.04082],[-84.897364,39.057378],[-84.831197,39.10192],[-84.78768,39.115297],[-84.766749,39.138558],[-84.750749,39.147358],[-84.718548,39.137059],[-84.684847,39.100459],[-84.657246,39.09546],[-84.632446,39.07676],[-84.620112,39.073457],[-84.572144,39.08206],[-84.550844,39.09936],[-84.524644,39.09216],[-84.510076,39.093606],[-84.470542,39.12146],[-84.449793,39.117754],[-84.435541,39.102261],[-84.427913,39.054962],[-84.406941,39.045662],[-84.346039,39.036963],[-84.326539,39.027463],[-84.304698,39.006455],[-84.288164,38.955789],[-84.234453,38.893226],[-84.231306,38.830552],[-84.212904,38.805707],[-84.071491,38.770475],[-84.044486,38.770572],[-83.962123,38.787384],[-83.917217,38.769665],[-83.873168,38.762418],[-83.852085,38.751433],[-83.836696,38.717857],[-83.787113,38.699489],[-83.769347,38.65522],[-83.720779,38.646704],[-83.679484,38.630036],[-83.663911,38.62793],[-83.649737,38.632753],[-83.637377,38.66793],[-83.626922,38.679387],[-83.520953,38.703045],[-83.493342,38.694187],[-83.468059,38.67547],[-83.384755,38.663171],[-83.356445,38.654009],[-83.327636,38.637489],[-83.319101,38.612233],[-83.307832,38.600824],[-83.294193,38.596588],[-83.264011,38.621535],[-83.245572,38.627936],[-83.202453,38.616956],[-83.142836,38.625076],[-83.112372,38.671685],[-83.053104,38.695831],[-83.027917,38.727143],[-82.979395,38.725976],[-82.923694,38.750076],[-82.894193,38.756576],[-82.879492,38.751476],[-82.869892,38.728177],[-82.877592,38.690177],[-82.859391,38.660378],[-82.854291,38.613454],[-82.844306,38.590862],[-82.820161,38.572703],[-82.789776,38.559951],[-82.724846,38.5576],[-82.696621,38.542112],[-82.657051,38.496816],[-82.608202,38.468049],[-82.593673,38.421809],[-82.599737,38.39037],[-82.593008,38.375082],[-82.597979,38.344909],[-82.576936,38.328275],[-82.572691,38.318801],[-82.583056,38.296829],[-82.574656,38.263873],[-82.581796,38.248592],[-82.60423,38.247303],[-82.61226,38.236087],[-82.608944,38.22366],[-82.600353,38.218949],[-82.599326,38.197231],[-82.611343,38.171548],[-82.642997,38.16956],[-82.637306,38.13905],[-82.622125,38.133414],[-82.621164,38.123239],[-82.606589,38.120843],[-82.587782,38.108879],[-82.584039,38.090663],[-82.551259,38.070799],[-82.517351,38.001204],[-82.48978,37.998869],[-82.483871,37.984505],[-82.464257,37.983412],[-82.46938,37.973059],[-82.483836,37.971566],[-82.484758,37.965752],[-82.472669,37.960721],[-82.475096,37.954906],[-82.48512,37.946044],[-82.495294,37.946612],[-82.491182,37.93581],[-82.501948,37.934756],[-82.49814,37.9283],[-82.480338,37.925836],[-82.487616,37.919905],[-82.475534,37.911945],[-82.474574,37.900295],[-82.469058,37.90222],[-82.464297,37.915038],[-82.421484,37.885652],[-82.417679,37.870658],[-82.409799,37.865392],[-82.422127,37.863952],[-82.423513,37.860313],[-82.414651,37.85626],[-82.420484,37.847496],[-82.39968,37.829935],[-82.39871,37.808785],[-82.385259,37.81741],[-82.377393,37.803009],[-82.340455,37.786058],[-82.335981,37.7745],[-82.323004,37.773907],[-82.333816,37.765391],[-82.331162,37.763125],[-82.312824,37.765027],[-82.310893,37.762005],[-82.333044,37.740969]]]]},\"properties\":{\"name\":\"Kentucky\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f934","contributors":{"authors":[{"text":"Dyer, Kenneth L.","contributorId":82353,"corporation":false,"usgs":true,"family":"Dyer","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33235,"text":"b1537C - 1983 - The Fishburne Formation (lower Eocene), a newly defined subsurface unit in the South Carolina coastal plain","interactions":[],"lastModifiedDate":"2020-03-27T07:12:00","indexId":"b1537C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1537","chapter":"C","title":"The Fishburne Formation (lower Eocene), a newly defined subsurface unit in the South Carolina coastal plain","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1537C","usgsCitation":"Gohn, G., Hazel, J.E., Bybell, L.M., and Edwards, L.E., 1983, The Fishburne Formation (lower Eocene), a newly defined subsurface unit in the South Carolina coastal plain: U.S. Geological Survey Bulletin 1537, iii, 16 p., https://doi.org/10.3133/b1537C.","productDescription":"iii, 16 p.","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"links":[{"id":61018,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1537c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1537c/report-thumb.jpg"}],"country":"United States","state":"South Carolina","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.7275390625,\n              31.98944183792288\n            ],\n            [\n              -78.0029296875,\n              33.358061612778876\n            ],\n            [\n              -78.75,\n              34.52466147177172\n            ],\n            [\n              -80.6396484375,\n              35.209721645221386\n            ],\n            [\n              -82.353515625,\n              35.10193405724606\n            ],\n            [\n              -83.0126953125,\n              34.95799531086792\n            ],\n            [\n              -82.79296874999999,\n              33.7243396617476\n            ],\n            [\n              -81.7822265625,\n              32.62087018318113\n            ],\n            [\n              -80.7275390625,\n              31.98944183792288\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c832","contributors":{"authors":[{"text":"Gohn, Gregory 0000-0003-2000-479X ggohn@usgs.gov","orcid":"https://orcid.org/0000-0003-2000-479X","contributorId":219822,"corporation":false,"usgs":true,"family":"Gohn","given":"Gregory","email":"ggohn@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":210246,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hazel, J. E.","contributorId":89187,"corporation":false,"usgs":false,"family":"Hazel","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":210247,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bybell, Laurel M. 0000-0002-4760-7542 lbybell@usgs.gov","orcid":"https://orcid.org/0000-0002-4760-7542","contributorId":1760,"corporation":false,"usgs":true,"family":"Bybell","given":"Laurel","email":"lbybell@usgs.gov","middleInitial":"M.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":210245,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edwards, Lucy E. 0000-0003-4075-3317 leedward@usgs.gov","orcid":"https://orcid.org/0000-0003-4075-3317","contributorId":2647,"corporation":false,"usgs":true,"family":"Edwards","given":"Lucy","email":"leedward@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":210244,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":32570,"text":"pp1170E - 1983 - A sillimanite gneiss dome in the Yukon crystalline terrane, east-central Alaska: Petrography and garnet-biotite geothermometry","interactions":[],"lastModifiedDate":"2022-12-20T19:46:25.517242","indexId":"pp1170E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1170","chapter":"E","title":"A sillimanite gneiss dome in the Yukon crystalline terrane, east-central Alaska: Petrography and garnet-biotite geothermometry","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1170E","usgsCitation":"Dusel-Bacon, C., and Foster, H., 1983, A sillimanite gneiss dome in the Yukon crystalline terrane, east-central Alaska: Petrography and garnet-biotite geothermometry: U.S. Geological Survey Professional Paper 1170, iii, 25 p., https://doi.org/10.3133/pp1170E.","productDescription":"iii, 25 p.","costCenters":[],"links":[{"id":60395,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1170e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1170e/report-thumb.jpg"},{"id":410805,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74409.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -146.180,\n              64.8106\n            ],\n            [\n              -146.180,\n              64.2978\n            ],\n            [\n              -145.1628,\n              64.2978\n            ],\n            [\n              -145.1628,\n              64.8106\n            ],\n            [\n              -146.180,\n              64.8106\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6546","contributors":{"authors":[{"text":"Dusel-Bacon, Cynthia 0000-0001-8481-739X cdusel@usgs.gov","orcid":"https://orcid.org/0000-0001-8481-739X","contributorId":2797,"corporation":false,"usgs":true,"family":"Dusel-Bacon","given":"Cynthia","email":"cdusel@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":208701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, H.L.","contributorId":34894,"corporation":false,"usgs":true,"family":"Foster","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":208702,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29871,"text":"wri824109 - 1983 - Appraisal of the interconnection between the St Johns River and the surficial aquifer, east-central Duval County, Florida","interactions":[],"lastModifiedDate":"2024-01-08T23:01:11.323275","indexId":"wri824109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-4109","title":"Appraisal of the interconnection between the St Johns River and the surficial aquifer, east-central Duval County, Florida","docAbstract":"The proposed deepening of the navigation channel in the St. Johns River to about 46-48 feet below sea level (45 feet below mean low water) may breach up to 11 feet of limestone unit of the lower part of the surficial aquifer along a 25-mile channel. The limestone supplies water to numerous domestic wells along the river in the Jacksonville area. Recent channel improvements to about 39 feet below sea level have already breached the limestone at many locations. Where breaching has not yet occurred, less than 1 to 6 feet of undifferentiated sediments overlie the limestone. These sediments, consisting predominantly of sand, are generally too permeable to form an effective confining layer. Chloride concentrations determined from water in wells tapping the limestone unit range from 8 to 6,600 milligrams per liter. However, chloride concentrations in water from wells located more than 500 feet from the river, were generally less than 30 milligrams per liter. The proposed dredging operation is not expected to alter significantly the present hydrologic system. The current position of the interface most likely represents conditions that will be present after future channel improvements. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824109","usgsCitation":"Spechler, R., and Stone, R.B., 1983, Appraisal of the interconnection between the St Johns River and the surficial aquifer, east-central Duval County, Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4109, iv, 38 p., https://doi.org/10.3133/wri824109.","productDescription":"iv, 38 p.","costCenters":[],"links":[{"id":424204,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35616.htm","linkFileType":{"id":5,"text":"html"}},{"id":58685,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4109/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123308,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4109/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Duval County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.72156565133055,\n              30.471947232313866\n            ],\n            [\n              -81.72156565133055,\n              30.27618396890138\n            ],\n            [\n              -81.39844829812067,\n              30.27618396890138\n            ],\n            [\n              -81.39844829812067,\n              30.471947232313866\n            ],\n            [\n              -81.72156565133055,\n              30.471947232313866\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a369","contributors":{"authors":[{"text":"Spechler, R. M.","contributorId":85961,"corporation":false,"usgs":true,"family":"Spechler","given":"R. M.","affiliations":[],"preferred":false,"id":202279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stone, R. B. Jr.","contributorId":71598,"corporation":false,"usgs":true,"family":"Stone","given":"R.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":202278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29911,"text":"wri834002 - 1983 - Ground-water contamination at Wurtsmith Air Force Base, Michigan","interactions":[],"lastModifiedDate":"2017-01-25T14:09:18","indexId":"wri834002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4002","title":"Ground-water contamination at Wurtsmith Air Force Base, Michigan","docAbstract":"<p>A sand and gravel aquifer of glacial origin underlies Wurtsmith Air Force Base in northeastern lower Michigan. The aquifer overlies a thick clay layer at an average depth of 65 feet. The water table is about 10 feet below land surface in the western part of the Base and about 25 feet below land surface in the eastern part. A ground-water divide cuts diagonally across the Base from northwest to southeast. South of the divide, ground water flows to the Au Sable River; north of the divide, it flows to Van Etten Creek and Van Etten Lake. Mathematical models were used to aid in calculating rates of groundwater flow. Rates range from about 0.8 feet per day in the eastern part of the Base to about 0.3 feet per day in the western part. Models also were used as an aid in making decisions regarding purging of contaminated water from the aquifer. </p><p>In 1977, trichloroethylene was detected in the Air Force Base water-supply system. It had leaked from a buried storage tank near Building 43 in the southeastern part of the Base and moved northeastward under the influence of the natural ground-water gradient and the pumping of Base water-supply wells. In the most highly contaminated part of the plume, concentrations are greater than 1,000 micrograms per liter. Current purge pumping is removing some of the trichloroethylene, and seems to have arrested its eastward movement. Pumping of additional purge wells could increase the rate of removal. </p><p>Trichloroethylene has also been detected in ground water in the vicinity of the Base alert apron, where a plume from an unknown source extends northeastward off Base. A smaller, less well-defined area of contamination also occurs just north of the larger plume. Trichloroethylene, identified near the waste-treatment plant, seepage lagoons, and the northern landfill area, is related to activities and operations in these areas. Dichloroethylene and trichloroethylene occur in significant quantities westward of Building 43, upgradient from the major spill site. Benzene, indicative of ground-water contamination by a fuel substance, occurs in an area northeast of the bulk-fuel storage area. Analysis of a variety of chemical, physical, and biologic characteristics of water on the Base indicate that there is a measurable affect on ground-water quality from landfills, the seepage lagoon, and the waste-treatment plant.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/wri834002","collaboration":"Prepared in cooperation with the U.S. Air Force","usgsCitation":"Stark, J., Cummings, T., and Twenter, F.R., 1983, Ground-water contamination at Wurtsmith Air Force Base, Michigan: U.S. Geological Survey Water-Resources Investigations Report 83-4002, Document: ix, 93 p.; Plate: 41.58 x 35.42 inches, https://doi.org/10.3133/wri834002.","productDescription":"Document: ix, 93 p.; Plate: 41.58 x 35.42 inches","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":58728,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4002/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58729,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4002/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4002/report-thumb.jpg"}],"country":"United States","state":"Michigan","otherGeospatial":"Wurtsmith Air Force Base","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.416667,\n              44.483333\n            ],\n            [\n              -83.416667,\n              44.425\n            ],\n            [\n              -83.325,\n              44.425\n            ],\n            [\n              -83.325,\n              44.483333\n            ],\n            [\n              -83.416667,\n              44.483333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d05d","contributors":{"authors":[{"text":"Stark, J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":202340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. R.","contributorId":104082,"corporation":false,"usgs":true,"family":"Cummings","given":"T. R.","affiliations":[],"preferred":false,"id":202341,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Twenter, F. R.","contributorId":81080,"corporation":false,"usgs":true,"family":"Twenter","given":"F.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202339,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}