{"pageNumber":"3718","pageRowStart":"92925","pageSize":"25","recordCount":185258,"records":[{"id":65786,"text":"i2367 - 1996 - Revised shaded relief map and controlled color photomosaic of the Eridania Quadrangle (MC-29) of Mars","interactions":[],"lastModifiedDate":"2019-12-23T12:17:50","indexId":"i2367","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2367","title":"Revised shaded relief map and controlled color photomosaic of the Eridania Quadrangle (MC-29) of Mars","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i2367","isbn":"0607870540","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1996, Revised shaded relief map and controlled color photomosaic of the Eridania Quadrangle (MC-29) of Mars: U.S. Geological Survey IMAP 2367, 2 Plates: 33.19 x 29.29 inches and 31.56 x 24.26 inches, https://doi.org/10.3133/i2367.","productDescription":"2 Plates: 33.19 x 29.29 inches and 31.56 x 24.26 inches","costCenters":[],"links":[{"id":101144,"rank":399,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2367/plate-1.pdf","size":"12551","linkFileType":{"id":1,"text":"pdf"}},{"id":101145,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/2367/plate-2.pdf","size":"11607","linkFileType":{"id":1,"text":"pdf"}},{"id":255523,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/2367/report-thumb.jpg"}],"scale":"46000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602e02","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29557,"text":"wri964039 - 1996 - Estimation of the recharge areas contributing water to the South Well Field, Columbus, Ohio","interactions":[],"lastModifiedDate":"2023-04-07T21:39:45.717016","indexId":"wri964039","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4039","title":"Estimation of the recharge areas contributing water to the South Well Field, Columbus, Ohio","docAbstract":"The city of Columbus, Ohio, operates four radial collector wells, designed to yield 42 Mgal/d (million gallons per day), in southern Franklin County, Ohio, as part of their municipal supply of water. The collector wells are adjacent to, and designed to induce infiltration from, Big Walnut Creek and Scioto River. A previously constructed, three-dimensional, steady-state and transient ground-water-flow model of this river-aquifer system was used to estimate contributing recharge areas (CRA's) and calculate particle flowpaths in southern Franklin County. The simulations were of two steady-state periods (October 1979 and March 1986) and one 5-year transient period (March 1986---June 1991). The first simulation (1979) was of conditions before construction of the collector wells. The second simulation (1986) was of conditions when the collector wells were producing 8 Mgal/d. During the 5 years covered in the transient simulation, production at the well field averaged 18.5 Mgal/d. \r\n\r\nUnder the 1979 conditions, the largest ground-water contributing areas were of the quarries and Scioto River (41 and 47 percent of the study area, respectively). During 1986, when 8 Mgal/d was withdrawn, the primary contributing areas were of the quarries (40 percent), collector wells (34 percent), and rivers (8 percent). Travel times associated with simulated particles of water tracked from cells along Big Walnut Creek to their discharge points in cells along Scioto River were about 5 to 60 years in the 1979 simulation and about 7 to 41 years in the 1986 simulation. The endpoints of these particles varied as simulated pumping rates were increased to 22 Mgal/d. \r\n\r\nThe 1986, 10-year CRA's of the collector wells under 8 Mgal/d-conditions totalled about 4.5 mi2. As the pumping rate was increased to 22 Mgal/d in a predictive simulation, 10-year CRA's of the collector wells increased to 6.7mi2. \r\n\r\nBecause the transient simulation encompassed only 5 years, the 10-year CRA's could not be estimated from the transient simulation. However, the size of the 1- to 5-year CRA's for the transient simulation was similar to the size of the 1- to 5-year CRA's for a steady-state predictive simulation if well-field production were 16 Mgal/d. The transient simulations predicted discontinuous CRA's, especially adjacent to the rivers, due to changes in hydrologic stresses. Analyses of the steady-state and transient models showed that sizes of CRA's were most sensitive to changes in porosity, pumping rate, riverbed conductance, and horizontal hydraulic conductivity.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964039","usgsCitation":"Schalk, C.W., 1996, Estimation of the recharge areas contributing water to the South Well Field, Columbus, Ohio: U.S. Geological Survey Water-Resources Investigations Report 96-4039, iv, 26 p., https://doi.org/10.3133/wri964039.","productDescription":"iv, 26 p.","costCenters":[],"links":[{"id":415480,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48407.htm","linkFileType":{"id":5,"text":"html"}},{"id":58386,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4039/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124541,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4039/report-thumb.jpg"}],"country":"United States","state":"Ohio","city":"Columbus","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -83.0417,\n              39.8972\n            ],\n            [\n              -83.0417,\n              39.8192\n            ],\n            [\n              -82.9583,\n              39.8192\n            ],\n            [\n              -82.9583,\n              39.8972\n            ],\n            [\n              -83.0417,\n              39.8972\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb1aa","contributors":{"authors":[{"text":"Schalk, C. W.","contributorId":64286,"corporation":false,"usgs":true,"family":"Schalk","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":201713,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22400,"text":"ofr96458 - 1996 - Quality of Wisconsin stormwater, 1989-94","interactions":[],"lastModifiedDate":"2015-10-15T14:41:53","indexId":"ofr96458","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-458","title":"Quality of Wisconsin stormwater, 1989-94","docAbstract":"<p>Water-quality data were compiled from four urban stormwater monitoring projects conducted in Wisconsin between 1989 and 1994. These projects included monitoring in both storm-sewer pipes and urban streams. A total of 147 constitu ents were analyzed for in stormwater sampled from 10 storm-sewer pipes and four urban streams. Land uses represented by the storm-sewer watersheds included residential, commercial, industrial, and mixed. For about one-half the con stituents, at least 10 percent of the event mean con centrations exceeded the laboratory's minimum reporting limit. Detection frequencies were greater than 75 percent for many of the heavy metals and polycyclic aromatic hydrocarbons in both the storm sewer and stream samples, whereas detec tion frequencies were about 20 percent or greater for many of the pesticides in both types of sam ples. Stormwater concentrations for conventional constituents, such as suspended solids, chloride, total phosphorus, and fecal coliform bacteria were greater than minimum reporting limits almost 100 percent of the time. Concentrations of many of the constituents were high enough to say that stormwater in the storm sewers and urban streams might be contrib uting to the degradation of the streams. In this report, constituents defined as potential contami nants are those for which the laboratory minimum report limit was exceeded for at least 10 percent of the sampled storm events, and for which at least one event mean concentration exceeded an estab lished water-quality standard. Storm-sewer sam ples had event mean concentrations of lead, copper, zinc, cadmium, and silver that frequently exceeded Wisconsin's acute toxicity criteria for cold water fisheries. Wisconsin's human cancer criteria was exceeded almost 100 percent of the time for polycyclic aromatic hydrocarbons in stormwater samples from storm sewers and streams. Maximum concentrations of diazinon found in storm sewers exceeded recommended levels of diazinon. Storm-sewer samples also exceeded Wisconsin's ground-water enforcement standards for pesticides, PCB's, phthalates, and chloride. Defined by criteria in this report, poten tial contaminants included five metals (lead, zinc, copper, silver, and cadmium), nine polycyclic aro matic hydrocarbons, Bis(2-ethylhexyl)phthalate, four pesticides (DDT, atrazine, alachlor, and 2,4 D), suspended solids, chlorides, total phosphorus, BOD 5-day, and bacteria. Wisconsin stormwater quality was similar to stormwater quality monitored in other states. Nearly one-half of median concentrations of con stituents in Wisconsin stormwater were within 30 percent of the medians from other states. The clos est agreement was seen for biochemical oxygen demand, total phosphorus, and total recoverable zinc. Similarities in stormwater quality for the storm sewer and urban streams indicated the storm sewers were a major source of water to the streams during storm events. Concentrations of potential contaminants in urban streams increased dramati cally during storm events as compared to baseflow concentrations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96458","issn":"0094-9140","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Bannerman, R.T., Legg, A.D., and Greb, S.R., 1996, Quality of Wisconsin stormwater, 1989-94: U.S. Geological Survey Open-File Report 96-458, iv, 26 p., https://doi.org/10.3133/ofr96458.","productDescription":"iv, 26 p.","numberOfPages":"30","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science 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,{"id":23081,"text":"ofr96522 - 1996 - Mineralogy, geochemistry, metamorphism, and provenance of the early Proterozoic metamorphic rocks of the central Front Range, Colorado","interactions":[],"lastModifiedDate":"2018-09-19T17:45:16","indexId":"ofr96522","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-522","title":"Mineralogy, geochemistry, metamorphism, and provenance of the early Proterozoic metamorphic rocks of the central Front Range, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr96522","issn":"0094-9140","usgsCitation":"Gable, D.J., 1996, Mineralogy, geochemistry, metamorphism, and provenance of the early Proterozoic metamorphic rocks of the central Front Range, Colorado: U.S. Geological Survey Open-File Report 96-522, 186 p. (some folded) :ill., maps ;28 cm., https://doi.org/10.3133/ofr96522.","productDescription":"186 p. (some folded) :ill., maps ;28 cm.","costCenters":[],"links":[{"id":52448,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0522/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52449,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0522/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156942,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0522/report-thumb.jpg"},{"id":52447,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0522/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d9a","contributors":{"editors":[{"text":"Johnson, W. D. Jr.","contributorId":53421,"corporation":false,"usgs":true,"family":"Johnson","given":"W. D.","suffix":"Jr.","affiliations":[],"preferred":false,"id":745664,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Gable, D. J.","contributorId":36569,"corporation":false,"usgs":true,"family":"Gable","given":"D.","middleInitial":"J.","affiliations":[],"preferred":false,"id":189399,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22428,"text":"ofr96496 - 1996 - Radionuclides, stable isotopes, inorganic constituents, and organic compounds in water from selected wells and springs from the southern boundary of the Idaho National Engineering Laboratory to the Hagerman area, Idaho, 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr96496","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-496","title":"Radionuclides, stable isotopes, inorganic constituents, and organic compounds in water from selected wells and springs from the southern boundary of the Idaho National Engineering Laboratory to the Hagerman area, Idaho, 1995","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96496","issn":"0094-9140","usgsCitation":"Bartholomay, R.C., Williams, L.M., and Campbell, L., 1996, Radionuclides, stable isotopes, inorganic constituents, and organic compounds in water from selected wells and springs from the southern boundary of the Idaho National Engineering Laboratory to the Hagerman area, Idaho, 1995: U.S. Geological Survey Open-File Report 96-496, iv, 29 p. :maps ;28 cm., https://doi.org/10.3133/ofr96496.","productDescription":"iv, 29 p. :maps ;28 cm.","costCenters":[],"links":[{"id":156459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0496/report-thumb.jpg"},{"id":51967,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0496/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649b02","contributors":{"authors":[{"text":"Bartholomay, R. C.","contributorId":66271,"corporation":false,"usgs":true,"family":"Bartholomay","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":188236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, L. M.","contributorId":63045,"corporation":false,"usgs":true,"family":"Williams","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":188235,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Campbell, L.J.","contributorId":59820,"corporation":false,"usgs":true,"family":"Campbell","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":188234,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23289,"text":"ofr96485 - 1996 - User's documentation for MODFLOW-96, an update to the U.S. Geological Survey modular finite-difference ground-water flow model","interactions":[],"lastModifiedDate":"2012-02-02T00:08:03","indexId":"ofr96485","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-485","title":"User's documentation for MODFLOW-96, an update to the U.S. Geological Survey modular finite-difference ground-water flow model","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96485","issn":"0094-9140","usgsCitation":"Harbaugh, A., and McDonald, M., 1996, User's documentation for MODFLOW-96, an update to the U.S. Geological Survey modular finite-difference ground-water flow model: U.S. Geological Survey Open-File Report 96-485, vi, 56 p. ;28 cm., https://doi.org/10.3133/ofr96485.","productDescription":"vi, 56 p. ;28 cm.","costCenters":[],"links":[{"id":156054,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0485/report-thumb.jpg"},{"id":52574,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0485/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604034","contributors":{"authors":[{"text":"Harbaugh, A.W.","contributorId":15208,"corporation":false,"usgs":true,"family":"Harbaugh","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":189820,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDonald, M.G.","contributorId":37716,"corporation":false,"usgs":true,"family":"McDonald","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":189821,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22963,"text":"ofr96560 - 1996 - Floods of July 12, 1972, March 19, 1979, and June 15, 1991, in the Turkey River Basin, northeast Iowa","interactions":[],"lastModifiedDate":"2016-03-21T14:12:42","indexId":"ofr96560","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-560","title":"Floods of July 12, 1972, March 19, 1979, and June 15, 1991, in the Turkey River Basin, northeast Iowa","docAbstract":"<p>Water-surface-elevation profiles and peak discharges for the floods of July 12, 1972, March 19, 1979, and June 15, 1991, in the Turkey River Basin, northeast Iowa, are presented in this report. The profiles illustrate the 1979 and 1991 floods along the Turkey River in Fayette and Clayton Counties and along the Volga River in Clayton County; the 1991 flood along Roberts Creek in Clayton County and along Otter Creek in Fayette County; and the 1972 flood along the Turkey River in Winneshiek and Fayette Counties. Watersurface elevations for the flood of March 19,1979, were collected by the Iowa Natural Resources Council. The June 15, 1991, flood on the Turkey River at Garber (station number 05412500) is the largest known flood-peak discharge at the streamflow-gaging station for the period 1902-95. The peak discharge for June 15, 1991, of 49,900 cubic feet per second was 1.4 times larger than the 100-year recurrence-interval discharge. The report provides information on flood stages and discharges and floodflow frequencies for streamflow-gaging stations in the Turkey River Basin using flood information collected during 1902-95. Information on temporary bench marks and reference points established in the Turkey River Basin during 1981, 1992, and 1996 also is included in the report. A flood history describes rainfall conditions for floods that occurred during 1922, 1947, 1972, 1979, and 1991.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City, IA","doi":"10.3133/ofr96560","issn":"0094-9140","collaboration":"Prepared in cooperation with the Iowa Highway Research Board and the Project Development Division of the Iowa Department of Transportation (Iowa DOT Research Project HR-140)","usgsCitation":"Eash, D.A., and Koppensteiner, B., 1996, Floods of July 12, 1972, March 19, 1979, and June 15, 1991, in the Turkey River Basin, northeast Iowa: U.S. Geological Survey Open-File Report 96-560, iv, 55 p., https://doi.org/10.3133/ofr96560.","productDescription":"iv, 55 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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A.","contributorId":60237,"corporation":false,"usgs":true,"family":"Eash","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":189206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Koppensteiner, B.A.","contributorId":108144,"corporation":false,"usgs":true,"family":"Koppensteiner","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":189207,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23288,"text":"ofr96486 - 1996 - Programmer's documentation for MODFLOW-96, an update to the U.S. Geological Survey modular finite-difference ground-water flow model","interactions":[],"lastModifiedDate":"2012-02-02T00:08:03","indexId":"ofr96486","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-486","title":"Programmer's documentation for MODFLOW-96, an update to the U.S. Geological Survey modular finite-difference ground-water flow model","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96486","issn":"0094-9140","usgsCitation":"Harbaugh, A., and McDonald, M., 1996, Programmer's documentation for MODFLOW-96, an update to the U.S. Geological Survey modular finite-difference ground-water flow model: U.S. Geological Survey Open-File Report 96-486, vii, 220 p. ;28 cm., https://doi.org/10.3133/ofr96486.","productDescription":"vii, 220 p. ;28 cm.","costCenters":[],"links":[{"id":156053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0486/report-thumb.jpg"},{"id":52573,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0486/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e0db","contributors":{"authors":[{"text":"Harbaugh, A.W.","contributorId":15208,"corporation":false,"usgs":true,"family":"Harbaugh","given":"A.W.","email":"","affiliations":[],"preferred":false,"id":189818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDonald, M.G.","contributorId":37716,"corporation":false,"usgs":true,"family":"McDonald","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":189819,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23809,"text":"ofr96648 - 1996 - Ground-water levels in Wyoming, January 1986 through September 1995","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr96648","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-648","title":"Ground-water levels in Wyoming, January 1986 through September 1995","docAbstract":"Water levels were measured in a network of 81 observation wells in Wyoming as of September 1995.  The wells are located mainly in areas where ground water is used in large quantities for irrigation or municipal purposes.  Water-level data were collected at 74 of the 81  observation wells by Wyoming State Engineer personnel; data at theremaining 7 wells were collected by the U.S. Geological Survey.  This report contains hydrographs for 81 observation wells showing water-level fluctuations from January 1986 through September 1995.  Included in the report are maps showing location of the observation wells and tableslisting observation-well depths, use of water, principal geologic source, records available, and highest and lowest water levels for the period ofrecord.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr96648","issn":"0094-9140","usgsCitation":"Mason, J.P., and Green, S.L., 1996, Ground-water levels in Wyoming, January 1986 through September 1995: U.S. Geological Survey Open-File Report 96-648, iv, 119 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96648.","productDescription":"iv, 119 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0648/report-thumb.jpg"},{"id":53023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0648/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667928","contributors":{"authors":[{"text":"Mason, J. P.","contributorId":27491,"corporation":false,"usgs":true,"family":"Mason","given":"J.","middleInitial":"P.","affiliations":[],"preferred":false,"id":190769,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, S. L.","contributorId":83525,"corporation":false,"usgs":true,"family":"Green","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":190770,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26472,"text":"wri964050 - 1996 - Ground-water hydrology, historical water use, and simulated ground-water flow in Cretaceous-age Coastal Plain aquifers near Charleston and Florence, South Carolina","interactions":[],"lastModifiedDate":"2019-12-30T12:53:36","indexId":"wri964050","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4050","title":"Ground-water hydrology, historical water use, and simulated ground-water flow in Cretaceous-age Coastal Plain aquifers near Charleston and Florence, South Carolina","docAbstract":"A quasi-three-dimensional, transient, digital, ground-water flow model representing the Coastal Plain aquifers of South Carolina, has been constructed to assist in defining the ground- water-flow system of Cretaceous aquifers near Charleston and Florence, S.C. Both cities are near the centers of large (greater than 150 feet) potentiometric declines in the Middendorf aquifer. In 1989, the diameter of the depressions was approximately 40 miles at Charleston and 15 miles at Florence. The potentiometric decline occurred between predevelopment (1926) and 1982 near Florence, and between predevelopment (1879) and 1989 near Charleston. The city of Charleston does not withdraw water from these aquifers; however, some of the small communities in the area use these aquifers for a potable water supply. The model simulates flow in and between four aquifer systems. The model has a variable-cell-size grid, and spans the Coastal Plain from the Savannah River in the southwest to the Cape Fear Arch in the northeast, and from the Fall Line in the northwest to approximately 30 miles offshore to the southeast. Model-grid cell size is 1 by 1 mile in a 48 by 48 mile area centered in Charleston, and in a 36 by 48 mile area centered in Florence. The model cell size gradually increases to a maximum of 4 by 4 miles outside the two study areas. The entire grid consists of 115 by 127 cells and covers an area of 39,936 square miles. The model was calibrated to historical water-level data. The calibration relied on three techniques: (1) matching simulated and observed potentiometric map surfaces, (2) statistical comparison of observed and simulated heads, and (3) comparison of observed and simulated well hydrographs. Systematic changes in model parameters showed that simulated heads are most sensitive to changes in aquifer transmissivity. Eight predictive ground-water-use scenarios were simulated for the Mount Pleasant area, which presently (1993) uses the Middendorf aquifer as a sole-source of potable water. These simulations use various combinations of spatial distribution, and injection of treated wastewater effluent for existing and future Middendorf aquifer wells.","language":"English","publisher":"U.S. Geological Survey ","doi":"10.3133/wri964050","usgsCitation":"Campbell, B.G., and van Heeswijk, M., 1996, Ground-water hydrology, historical water use, and simulated ground-water flow in Cretaceous-age Coastal Plain aquifers near Charleston and Florence, South Carolina: U.S. Geological Survey Water-Resources Investigations Report 96-4050, viii, 100 p. , https://doi.org/10.3133/wri964050.","productDescription":"viii, 100 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":55291,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4050/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124971,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4050/report-thumb.jpg"}],"country":"United States","state":"South Carolina","city":"Charleston, Florence","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.18920898437499,\n              32.59310597426537\n            ],\n            [\n              -79.65087890624999,\n              32.59310597426537\n            ],\n            [\n              -79.65087890624999,\n              33.03169299978312\n            ],\n            [\n              -80.18920898437499,\n              33.03169299978312\n            ],\n            [\n              -80.18920898437499,\n              32.59310597426537\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.013427734375,\n              34.043556504127444\n            ],\n            [\n              -79.6014404296875,\n              34.043556504127444\n            ],\n            [\n              -79.6014404296875,\n              34.334364487026306\n            ],\n            [\n              -80.013427734375,\n              34.334364487026306\n            ],\n            [\n              -80.013427734375,\n              34.043556504127444\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b10cb","contributors":{"authors":[{"text":"Campbell, B. G.","contributorId":68764,"corporation":false,"usgs":true,"family":"Campbell","given":"B.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":196453,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"van Heeswijk, Marijke heeswijk@usgs.gov","contributorId":1537,"corporation":false,"usgs":true,"family":"van Heeswijk","given":"Marijke","email":"heeswijk@usgs.gov","affiliations":[],"preferred":true,"id":196452,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32013,"text":"ofr96506 - 1996 - Coastal zone hazards map of Puerto Rico: Hurricane Hugo impacted portion of the shoreline, Cibuco (Punta Garaza) to Punta Viento","interactions":[],"lastModifiedDate":"2022-09-07T18:10:08.815407","indexId":"ofr96506","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-506","title":"Coastal zone hazards map of Puerto Rico: Hurricane Hugo impacted portion of the shoreline, Cibuco (Punta Garaza) to Punta Viento","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96506","usgsCitation":"Bush, D.M., Richmond, B.R., and Neal, W.J., 1996, Coastal zone hazards map of Puerto Rico: Hurricane Hugo impacted portion of the shoreline, Cibuco (Punta Garaza) to Punta Viento: U.S. Geological Survey Open-File Report 96-506, 19 p., https://doi.org/10.3133/ofr96506.","productDescription":"19 p.","costCenters":[],"links":[{"id":406325,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19396.htm","linkFileType":{"id":5,"text":"html"}},{"id":60171,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0506/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161486,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0506/report-thumb.jpg"}],"country":"United States","state":"Puerto Rico","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -66.4178466796875,\n              17.926475979176438\n            ],\n            [\n              -65.533447265625,\n              17.926475979176438\n            ],\n            [\n              -65.533447265625,\n              18.516074596589366\n            ],\n            [\n              -66.4178466796875,\n              18.516074596589366\n            ],\n            [\n              -66.4178466796875,\n              17.926475979176438\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aea3f","contributors":{"authors":[{"text":"Bush, D. M.","contributorId":104986,"corporation":false,"usgs":true,"family":"Bush","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":207458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richmond, B. R.","contributorId":11876,"corporation":false,"usgs":true,"family":"Richmond","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":207456,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Neal, W. J.","contributorId":40472,"corporation":false,"usgs":true,"family":"Neal","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":207457,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29337,"text":"wri964038C - 1996 - Benthic invertebrates of benchmark streams in agricultural areas of eastern Wisconsin — Western Lake Michigan drainages","interactions":[],"lastModifiedDate":"2022-01-21T21:01:57.760672","indexId":"wri964038C","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4038","chapter":"C","title":"Benthic invertebrates of benchmark streams in agricultural areas of eastern Wisconsin — Western Lake Michigan drainages","docAbstract":"<p>This study describes the benthic invertebrate communities of 20 benchmark streams in agricultural areas of eastern Wisconsin. Streams with minimal adverse effects from human activity were selected from four agricultural areas with differing surficial deposits and bedrock types (relatively homogeneous units, or RHU's). Most aquatic invertebrate orders were well represented in the 20 benchmark stream samples; 217 species and 151 genera within 56 families were identified. Diptera was the best represented order (96 species), followed by Trichoptera (42 species) and Ephemeroptera (26 species). Diptera were the most abundant organisms in terms of numbers of individuals in the sample (28 percent of the total) followed by Trichoptera (25 percent) and Ephemeroptera (13 percent). Nine species of freshwater mussels were found, but only in 5 of the 20 benchmark streams.</p>\n<p>Community measures were calculated for the following: total number of individuals; number of species; number of families; Margalef's diversity index; percent dominant family; percent Ephemeroptera-Plecoptera-Trichoptera (EPT); ratio of EPT to Chironomidae; percent shredders; ratio of scrapers to collectors-gatherers-filterers; Hilsenhoff's Biotic Index; Hilsenhoff's family level biotic index; and mean tolerance value. The S AS statistical software package was used for calculations of variance and correlations, normality checks, and principal components analysis of these measures and to find relations between benthic-invertebrate data and environmental-setting, habitat, and water-quality data.</p>\n<p>Coefficients of variation within the RHU's were as great or greater than those for all 20 streams for most measures and RHU's. The specific taxa assemblages present at the sites did not show distinct differences between RHU's or similarities within the RHU's. The covariance and the Kruskal-Wallis tests showed that the benthic invertebrate measures were not related to RHU. These results all indicate that the combined effect of the RHU variables (bedrock geology, texture of surficial deposits, and land use/land cover) were not elemental in describing invertebrate communities in the study-area streams.</p>\n<p>A principal components analysis (PCA) was done on the 20 benchmark streams which used the invertebrate population measures as variables. A three-dimensional ordination plot of these components revealed that 18 of the 20 streams could be divided into three groups relative to stream size, available habitat, and water quality. The three classifications of streams include large, warmer streams with slight pollution; deep, mixed-water streams with minimal pollution; and small, cold, pristine headwater streams. The two streams not defined by the three PCA groupings were not suitable to represent benchmark conditions. One site lacked suitable quality habitat or sufficient nutrients to support a healthy population of invertebrates, causing low measures of diversity. The other site appeared to be affected by sedimentation and low flows.</p>\n<p>The classification groupings did not show any significant relations to percentage agricultural land use. Percentage of agricultural land use varied greatly within each group and the means for each group were similar. All streams in this study had some level of protection from agricultural practices in their basins. Although the intensity of agriculture is known to be a factor causing deterioration of invertebrate populations in past studies, the finding in this study indicated that the level of protection the stream received and other factors such as environmental setting and habitat could be more important to benthic invertebrates than the percentage of agriculture in the basin.</p>\n<p>Information gathered from these benchmark streams can be used as a regional reference for comparison with other streams in agricultural areas, based on communities of aquatic biota, habitat, and water quality.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964038C","usgsCitation":"Rheaume, S.J., Lenz, B.N., and Scudder, B.C., 1996, Benthic invertebrates of benchmark streams in agricultural areas of eastern Wisconsin — Western Lake Michigan drainages: U.S. Geological Survey Water-Resources Investigations Report 96-4038, vi, 39 p., https://doi.org/10.3133/wri964038C.","productDescription":"vi, 39 p.","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":394722,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48405.htm"},{"id":58180,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4038c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4038c/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Lake Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.483642578125,\n              43.1090040242731\n            ],\n            [\n              -89.483642578125,\n              45.46783598133375\n            ],\n            [\n              -86.737060546875,\n              45.46783598133375\n            ],\n            [\n              -86.737060546875,\n              43.1090040242731\n            ],\n            [\n              -89.483642578125,\n              43.1090040242731\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b4bb","contributors":{"authors":[{"text":"Rheaume, S. J.","contributorId":70804,"corporation":false,"usgs":true,"family":"Rheaume","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":201366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lenz, B. N.","contributorId":106164,"corporation":false,"usgs":true,"family":"Lenz","given":"B.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":201368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scudder, B. C.","contributorId":71588,"corporation":false,"usgs":true,"family":"Scudder","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201367,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28044,"text":"wri964163 - 1996 - Estimated 100-year peak flows and flow volumes in the Big Lost River and Birch Creek at the Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:25","indexId":"wri964163","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4163","title":"Estimated 100-year peak flows and flow volumes in the Big Lost River and Birch Creek at the Idaho National Engineering Laboratory, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/wri964163","usgsCitation":"Kjelstrom, L., and Berenbrock, C., 1996, Estimated 100-year peak flows and flow volumes in the Big Lost River and Birch Creek at the Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 96-4163, iv, 23 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri964163.","productDescription":"iv, 23 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118703,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4163/report-thumb.jpg"},{"id":56882,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4163/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdd10","contributors":{"authors":[{"text":"Kjelstrom, L.C.","contributorId":89104,"corporation":false,"usgs":true,"family":"Kjelstrom","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":199121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berenbrock, Charles","contributorId":30598,"corporation":false,"usgs":true,"family":"Berenbrock","given":"Charles","email":"","affiliations":[],"preferred":false,"id":199120,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32023,"text":"ofr96589 - 1996 - Potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1996","interactions":[],"lastModifiedDate":"2022-10-04T20:47:47.045124","indexId":"ofr96589","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-589","title":"Potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1996","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96589","usgsCitation":"Phelps, G.G., O’Reilly, A.M., Bradner, L.A., and Knowles, L., 1996, Potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1996: U.S. Geological Survey Open-File Report 96-589, 1 Plate: 30.00 × 54.00 inches, https://doi.org/10.3133/ofr96589.","productDescription":"1 Plate: 30.00 × 54.00 inches","costCenters":[],"links":[{"id":161012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":407885,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18649.htm","linkFileType":{"id":5,"text":"html"}},{"id":19594,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0589/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83,\n              26.5\n            ],\n            [\n              -80,\n              26.5\n            ],\n            [\n              -80,\n              31.5\n            ],\n            [\n              -83,\n              31.5\n            ],\n            [\n              -83,\n              26.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682e62","contributors":{"authors":[{"text":"Phelps, G. G.","contributorId":82346,"corporation":false,"usgs":true,"family":"Phelps","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":207475,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"O’Reilly, A. M.","contributorId":71219,"corporation":false,"usgs":true,"family":"O’Reilly","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":207474,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":207473,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Knowles, Leel Jr.","contributorId":14857,"corporation":false,"usgs":true,"family":"Knowles","given":"Leel","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":207472,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":24775,"text":"ofr96516 - 1996 - Provisional geologic map of Augustine Volcano, Alaska","interactions":[],"lastModifiedDate":"2022-03-28T18:39:58.261827","indexId":"ofr96516","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-516","title":"Provisional geologic map of Augustine Volcano, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr96516","usgsCitation":"Waitt, R., Beget, J.E., and Kienle, J., 1996, Provisional geologic map of Augustine Volcano, Alaska: U.S. Geological Survey Open-File Report 96-516, Report: 44 p.; 1 Plate: 26.14 × 24.69 inches, https://doi.org/10.3133/ofr96516.","productDescription":"Report: 44 p.; 1 Plate: 26.14 × 24.69 inches","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":53799,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0516/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53798,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0516/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0516/report-thumb.jpg"},{"id":397730,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19173.htm"}],"scale":"25000","country":"United States","state":"Alaska","otherGeospatial":"Augustine Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -153.60122680664062,\n              59.30796423218468\n            ],\n            [\n              -153.30459594726562,\n              59.30796423218468\n            ],\n            [\n              -153.30459594726562,\n              59.43390314475794\n            ],\n            [\n              -153.60122680664062,\n              59.43390314475794\n            ],\n            [\n              -153.60122680664062,\n              59.30796423218468\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687e7a","contributors":{"authors":[{"text":"Waitt, R. B.","contributorId":78766,"corporation":false,"usgs":true,"family":"Waitt","given":"R. B.","affiliations":[],"preferred":false,"id":192544,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beget, J. E.","contributorId":63392,"corporation":false,"usgs":true,"family":"Beget","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":192543,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kienle, Juergen","contributorId":45343,"corporation":false,"usgs":true,"family":"Kienle","given":"Juergen","email":"","affiliations":[],"preferred":false,"id":192542,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32020,"text":"ofr96547 - 1996 - Geologic map of the Hellertown Quadrangle, Northampton, Bucks, and Lehigh counties, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"ofr96547","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-547","title":"Geologic map of the Hellertown Quadrangle, Northampton, Bucks, and Lehigh counties, Pennsylvania","language":"ENGLISH","doi":"10.3133/ofr96547","usgsCitation":"Drake, A.A., 1996, Geologic map of the Hellertown Quadrangle, Northampton, Bucks, and Lehigh counties, Pennsylvania: U.S. Geological Survey Open-File Report 96-547, 27 p., 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet).  , https://doi.org/10.3133/ofr96547.","productDescription":"27 p., 1 over-size sheet, scale 1:24,000 (1 inch = 2,000 feet).  ","costCenters":[],"links":[{"id":161009,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0547/report-thumb.jpg"},{"id":60177,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1996/0547/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60178,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0547/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6981d9","contributors":{"authors":[{"text":"Drake, Avery A. Jr.","contributorId":81090,"corporation":false,"usgs":true,"family":"Drake","given":"Avery","suffix":"Jr.","middleInitial":"A.","affiliations":[],"preferred":false,"id":207468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29777,"text":"wri964047 - 1996 - Geohydrology of the Stockton Formation and cross-contamination through open boreholes, Hatboro Borough and Warminster Township, Pennsylvania","interactions":[],"lastModifiedDate":"2018-12-20T10:40:33","indexId":"wri964047","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4047","title":"Geohydrology of the Stockton Formation and cross-contamination through open boreholes, Hatboro Borough and Warminster Township, Pennsylvania","docAbstract":"The study area consists of a 9-square-mile area underlain by sedimentary rocks of the middle arkose member of the Stockton Formation of Upper Triassic age. In the Hatboro area, the Stockton Formation strikes approximately N. 65 degrees E. and dps approximately 9 degrees NW. The rocks are chiefly arkosic sandstone and siltstone. Rocks of the Stocton Formation form a complex, heterogeneous, multiaquifer system consisting of a series of gently dipping lithologic units with different hydraulic properties. Most ground water in the unweathered zone moves through a network of interconnecting secondary openigns-fractures, bedding plans, and joints. Ground water is unconfined in the shallower part of the aquifer and semiconfined or confined in the deeper part of the aquifer. Nearly all deep wells in the Stockton Formation are open to several water-bearing zones and are multiaquifer wells. Each water-bearing zone usually has a different hydraulic head. Where differences in hydraulic head exist between water-bearing zones, water in the well bore flows under nonpumping conditions in the direction of decreasing head.\r\n\r\n      Determination of the potential for borehole flow was based on caliper, natural-gamma, single- point-resistance, fluid-resistivity, and (or) fluid-temperature logs that were run in 162 boreholes 31 to 655 feet deep. The direction and rate of borehole-fluid movement were determined in 83 boreholes by the bring-tracing method and in 10 boreholes by use of a heat-pulse flowmeter. Borehole flow was measurable in 65 of the 93 boreholes (70 percent). Fluid movement at rates up to 17 gallons per minute was measured. Downward flow was measured in 36 boreholes, and upward flow was measured in 23 boreholes, not including those boreholes in which two directions of flow were measured. Both upward and downward vertical flow was measured in six boreholes; these boreholes are 396 to 470 feet deep and were among the deepest boreholes logged. Fluid movement was upward in the upper part of the borehole and downward in the lower part of the borehole in two boreholes. Fluid movement wad downward in the upper part of the borehole and upward in the lower part of the borehole in three boreholes.\r\n\r\n      Groung-water contamination by volatile organic compounds (VOC's) is widespread in the study area. Detectable concentrations of VOC's were present in water samples from 24 wells sampled in Hatboro Brough and in water samples for 10 of 14 wells (71 percent) samples in Warminster Township. Samples of borehole flow from nine boreholes in the industrial area of Hatboro were collected for laboratory analysis to estimate the quantity of VOC's in borehole flow. Downward flow was measured in all of these boreholes. Concentrations of TCE, TCA, and 1,1-DCE as great at 5,800, 1,400 and 260 micrograms per liter, respectively, show that some water moving downward in the aquifer through these open boreholes is highly contaminated and that open boreholes may contribute substantially to ground-water contamination. An estimated 14.7 gallons per year of VOC's were moving downward through the nine open boreholes sampled from the contaminated, upper part of the aquifer to the lower part, which is tapped by public supply wells.\r\n\r\n      Borehole geophysical logs were used as a guide to design and construct monitor-well networks at three National Priorities List sites in the area. An open borehole was dirlled, and a suite of geophysical logs was run. Interpretation of geophysical logs enabled the identification of water-bearing zones that produce and receive water; these are zones that should not be connected. From the logs, discrete intervals to be monitored were selected. In the Stockton Formation, the same water-bearing zone may not be intersected in adjacent boreholes, especially if it is a vertical fracture with a diffident magnetic orientation than that of the adjacent boreholes. In most areas of the stockton Formation, depth of water-bearing zones in an are","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri964047","usgsCitation":"Sloto, R.A., Macchiaroli, P., and Towle, M.T., 1996, Geohydrology of the Stockton Formation and cross-contamination through open boreholes, Hatboro Borough and Warminster Township, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 96-4047, Report: v, 49 p.; 2 Plates: 17.00 x 11.04 inches, https://doi.org/10.3133/wri964047.","productDescription":"Report: v, 49 p.; 2 Plates: 17.00 x 11.04 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":122226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4047/report-thumb.jpg"},{"id":58579,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4047/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360607,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":360608,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1996/4047/plate-2.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              -75.16666667,\n              40.16666667\n            ],\n            [\n              -75.05000000,\n              40.16666667\n            ],\n            [\n             -75.05000000,\n              40.28333333\n            ],\n            [\n             -75.16666667,\n              40.28333333\n            ],\n            [\n              -75.16666667,\n             40.16666667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a88ce","contributors":{"authors":[{"text":"Sloto, Ronald A. rasloto@usgs.gov","contributorId":424,"corporation":false,"usgs":true,"family":"Sloto","given":"Ronald","email":"rasloto@usgs.gov","middleInitial":"A.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":202105,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Macchiaroli, Paola","contributorId":96309,"corporation":false,"usgs":true,"family":"Macchiaroli","given":"Paola","email":"","affiliations":[],"preferred":false,"id":202107,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Towle, Michael T.","contributorId":211743,"corporation":false,"usgs":true,"family":"Towle","given":"Michael","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":202106,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":6584,"text":"fs18396 - 1996 - Hazard maps help save lives and property","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"fs18396","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"183-96","title":"Hazard maps help save lives and property","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs18396","usgsCitation":"Brown, W.M., Perkins, D.M., Leyendecker, E.V., Frankel, A.D., Hendley, J.W., and Stauffer, P.H., 1996, Hazard maps help save lives and property: U.S. Geological Survey Fact Sheet 183-96, 2 p., https://doi.org/10.3133/fs18396.","productDescription":"2 p.","costCenters":[],"links":[{"id":121767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_183_96.bmp"},{"id":875,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/1996/fs183-96/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d77b","contributors":{"authors":[{"text":"Brown, William M. III","contributorId":72365,"corporation":false,"usgs":true,"family":"Brown","given":"William","suffix":"III","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":152968,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Perkins, David M. perkins@usgs.gov","contributorId":2114,"corporation":false,"usgs":true,"family":"Perkins","given":"David","email":"perkins@usgs.gov","middleInitial":"M.","affiliations":[{"id":301,"text":"Geologic Hazards Team","active":false,"usgs":true}],"preferred":true,"id":152966,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leyendecker, Edgar V.","contributorId":75142,"corporation":false,"usgs":true,"family":"Leyendecker","given":"Edgar","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":152969,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Frankel, Arthur D. 0000-0001-9119-6106 afrankel@usgs.gov","orcid":"https://orcid.org/0000-0001-9119-6106","contributorId":1363,"corporation":false,"usgs":true,"family":"Frankel","given":"Arthur","email":"afrankel@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":152965,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hendley, James W. II jhendley@usgs.gov","contributorId":2547,"corporation":false,"usgs":true,"family":"Hendley","given":"James","suffix":"II","email":"jhendley@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":false,"id":152967,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stauffer, Peter H. pstauffe@usgs.gov","contributorId":1219,"corporation":false,"usgs":true,"family":"Stauffer","given":"Peter","email":"pstauffe@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":152964,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":5198,"text":"fs20196 - 1996 - Interpretive U.S. Geological Survey programs with municipalities in Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"fs20196","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":313,"text":"Fact Sheet","code":"FS","onlineIssn":"2327-6932","printIssn":"2327-6916","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"201-96","title":"Interpretive U.S. Geological Survey programs with municipalities in Iowa","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/fs20196","usgsCitation":"Buchmiller, R.C., 1996, Interpretive U.S. Geological Survey programs with municipalities in Iowa: U.S. Geological Survey Fact Sheet 201-96, 1 sheet (4 p.) : col. ill., col. map ; 28 cm. col. ill., col. map ;, https://doi.org/10.3133/fs20196.","productDescription":"1 sheet (4 p.) : col. ill., col. map ; 28 cm. col. ill., col. map ;","costCenters":[],"links":[{"id":125328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1996/0201/report-thumb.jpg"},{"id":31933,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1996/0201/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dff09","contributors":{"authors":[{"text":"Buchmiller, Robert C.","contributorId":72372,"corporation":false,"usgs":true,"family":"Buchmiller","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":150592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30608,"text":"wri964058 - 1996 - Interpretation of chemical and isotopic data from boreholes in the unsaturated zone at Yucca Mountain, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:09:13","indexId":"wri964058","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-4058","title":"Interpretation of chemical and isotopic data from boreholes in the unsaturated zone at Yucca Mountain, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBranch of Information Services [distributor],","doi":"10.3133/wri964058","usgsCitation":"Yang, I., Rattray, G., and Yu, P., 1996, Interpretation of chemical and isotopic data from boreholes in the unsaturated zone at Yucca Mountain, Nevada: U.S. Geological Survey Water-Resources Investigations Report 96-4058, v, 58 p. :ill., maps ;28 cm. [PGS - 57 p.], https://doi.org/10.3133/wri964058.","productDescription":"v, 58 p. :ill., maps ;28 cm. [PGS - 57 p.]","costCenters":[],"links":[{"id":121827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4058/report-thumb.jpg"},{"id":59375,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4058/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e057f","contributors":{"authors":[{"text":"Yang, I.C.","contributorId":88777,"corporation":false,"usgs":true,"family":"Yang","given":"I.C.","email":"","affiliations":[],"preferred":false,"id":203532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rattray, G.W.","contributorId":87584,"corporation":false,"usgs":true,"family":"Rattray","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":203531,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Yu, Pei","contributorId":14458,"corporation":false,"usgs":true,"family":"Yu","given":"Pei","email":"","affiliations":[],"preferred":false,"id":203530,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26900,"text":"wri954244 - 1996 - Ground-water quality in the Calumet Region of northwestern Indiana and northeastern Illinois, June 1993","interactions":[],"lastModifiedDate":"2016-05-16T09:41:55","indexId":"wri954244","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"95-4244","title":"Ground-water quality in the Calumet Region of northwestern Indiana and northeastern Illinois, June 1993","docAbstract":"<p>Water samples were collected from 128 wells in a large industrial and urban area in northwestern Indiana and northeastern Illinois during June 1993. Samples were collected from wells completed in one of four geohydrologic units: surficial sand aquifer (Calumet aquifer), clay confining unit, confined sand aquifers, and a carbonate-bedrock aquifer (Silurian-Devonian aquifer). Samples were analyzed by U.S. Environmental Protection Agency contract laboratories for selected water-quality properties, common ions, trace elements, volatile and semivolatile organic compounds, pesticides, and polychlorinated biphenyls.</p>\n<p>Water from wells in the Silurian-Devonian aquifer is predominantly a sodium bicarbonate type. Water types in confined sand aquifers and the confining unit are varied. Water types from wells in the Calumet aquifer also are varied, although approximately 42 percent of the wells in this geohydrologic unit produced water in which calcium and bicarbonate were the dominant cation-anion pair. Samples from several shallow wells in the confining unit and the Calumet aquifer, and one well in a confined sand aquifer, were classified as sodium chloride-type water.</p>\n<p>The largest concentrations of trace elements and organic compounds were detected in samples from wells located in or near industrial areas or areas of waste disposal. A total of 14 volatile organic compounds and 23 semivolatile organic compounds on the U.S. Environmental Protection Agency's target compound list was detected in 20 and 56 samples. A total of 18 pesticide compounds was detected in 29 samples. Compounds containing polychlorinated biphenyls were detected in three samples.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri954244","collaboration":"U.S. Environmental Protection Agency","usgsCitation":"Duwelius, R.F., Kay, R.T., and Prinos, S.T., 1996, Ground-water quality in the Calumet Region of northwestern Indiana and northeastern Illinois, June 1993: U.S. Geological Survey Water-Resources Investigations Report 95-4244, vii, 179 p., [8] folded p. of plates :ill., maps ;28 cm., https://doi.org/10.3133/wri954244.","productDescription":"vii, 179 p., [8] folded p. of plates :ill., maps ;28 cm.","startPage":"1","endPage":"179","numberOfPages":"185","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":2004,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://il.water.usgs.gov/pubsearch/reports.cgi/view?series=WRIR&number=95-4244","linkFileType":{"id":5,"text":"html"}},{"id":123527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4244/report-thumb.jpg"},{"id":55781,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4244/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois, Indiana","otherGeospatial":"Calumet Region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.75,\n              41.75\n            ],\n            [\n              -87.75,\n              41.55\n            ],\n            [\n              -87,\n              41.55\n            ],\n            [\n              -87,\n              41.75\n            ],\n            [\n              -87.75,\n              41.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db658731","contributors":{"authors":[{"text":"Duwelius, Richard F.","contributorId":31378,"corporation":false,"usgs":true,"family":"Duwelius","given":"Richard","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kay, Robert T. 0000-0002-6281-8997 rtkay@usgs.gov","orcid":"https://orcid.org/0000-0002-6281-8997","contributorId":1122,"corporation":false,"usgs":true,"family":"Kay","given":"Robert","email":"rtkay@usgs.gov","middleInitial":"T.","affiliations":[{"id":344,"text":"Illinois Water Science Center","active":true,"usgs":true}],"preferred":true,"id":197214,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prinos, Scott T. 0000-0002-5776-8956 stprinos@usgs.gov","orcid":"https://orcid.org/0000-0002-5776-8956","contributorId":4045,"corporation":false,"usgs":true,"family":"Prinos","given":"Scott","email":"stprinos@usgs.gov","middleInitial":"T.","affiliations":[{"id":156,"text":"Caribbean Water Science Center","active":true,"usgs":true},{"id":269,"text":"FLWSC-Ft. 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,{"id":23848,"text":"ofr96670 - 1996 - A closed-path Fourier transform infrared spectrometer for measuring volcanic gases","interactions":[],"lastModifiedDate":"2012-02-02T00:08:08","indexId":"ofr96670","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-670","title":"A closed-path Fourier transform infrared spectrometer for measuring volcanic gases","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr96670","issn":"0094-9140","usgsCitation":"McGee, K., 1996, A closed-path Fourier transform infrared spectrometer for measuring volcanic gases: U.S. Geological Survey Open-File Report 96-670, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr96670.","productDescription":"20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0670/report-thumb.jpg"},{"id":53068,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0670/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd498ae4b0b290850ef426","contributors":{"authors":[{"text":"McGee, K.A.","contributorId":6059,"corporation":false,"usgs":true,"family":"McGee","given":"K.A.","email":"","affiliations":[],"preferred":false,"id":190850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24655,"text":"ofr96662A - 1996 - Total dissolved gas, barometric pressure, and water temperature data, lower Columbia River, Oregon and Washington, 1996","interactions":[],"lastModifiedDate":"2017-02-07T10:01:37","indexId":"ofr96662A","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-662","chapter":"A","title":"Total dissolved gas, barometric pressure, and water temperature data, lower Columbia River, Oregon and Washington, 1996","docAbstract":"<p>Increased levels of total dissolved gas pressure can cause gas-bubble trauma in fish downstream from dams on the Columbia River. In cooperation with the U.S. Army Corps of Engineers, the U.S. Geological Survey collected data on total dissolved gas pressure, barometric pressure, water temperature, and dissolved oxygen pressure at 11 stations on the lower Columbia River from the John Day forebay (river mile 215.6) to Wauna Mill (river mile 41.9) from March to September 1996. Methods of data collection, review, and processing are described in this report. Summaries of daily minimum, maximum, and mean hourly values are presented for total dissolved gas pressure, barometric pressure, and water temperature. Hourly values for these parameters are presented graphically. Dissolved oxygen data are not presented in this report because the quality-control data show that the data have poor precision and high bias. Suggested changes to monitoring procedures for future studies include (1) improved calibration procedures for total dissolved gas and dissolved oxygen to better define accuracy at elevated levels of supersaturation and (2) equipping dissolved oxygen sensors with stirrers because river velocities at the shoreline monitoring stations probably cannot maintain an adequate flow of water across the membrane surface of the dissolved oxygen sensor.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr96662A","issn":"0094-9140","collaboration":"Prepared in cooperation with the U.S. Army Corps of Engineers","usgsCitation":"Tanner, D.Q., Harrison, H.E., and McKenzie, S.W., 1996, Total dissolved gas, barometric pressure, and water temperature data, lower Columbia River, Oregon and Washington, 1996: U.S. Geological Survey Open-File Report 96-662, vi, 85 p., https://doi.org/10.3133/ofr96662A.","productDescription":"vi, 85 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E.","contributorId":8485,"corporation":false,"usgs":true,"family":"Harrison","given":"Howard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":192330,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenzie, Stuart W.","contributorId":27841,"corporation":false,"usgs":true,"family":"McKenzie","given":"Stuart","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":192331,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21714,"text":"ofr96614 - 1996 - Data from synoptic water-quality studies on the Colorado River in the Grand Canyon, Arizona, November 1990 and June 1991","interactions":[],"lastModifiedDate":"2018-02-15T12:53:33","indexId":"ofr96614","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-614","title":"Data from synoptic water-quality studies on the Colorado River in the Grand Canyon, Arizona, November 1990 and June 1991","docAbstract":"Two water-quality synoptic studies were made on the Colorado River in the Grand Canyon, Arizona. Field measurements and the collection of water samples for laboratory analysis were made at 10 mainstem and 6 tributary sites every 6 hours for a 48-hour period on November 5-6, 1990, and again on June 18-20, 1991. Field\r\nmeasurements included discharge, alkalinity, water temperature, light penetration, pH, specific conductance, and dissolved oxygen. Water samples were collected for the laboratory analysis of major and minor ions (calcium, magnesium, sodium, potassium, strontium, chloride, sulfate, silica as SiO2), trace elements (aluminum, arsenic, boron, barium, beryllium, cadmium, cobalt, chromium, copper, iron, lead, lithium, manganese, molybdenum, nickel, selenium, thallium, uranium, vanadium and zinc), and nutrients (phosphate, nitrate, ammonium, nitrite, total\r\ndissolved nitrogen, total dissolved phosphorus and dissolved organic carbon). Biological measurements included drift (benthic invertebrates and detrital material), and benthic invertebrates from the river bottom.","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/ofr96614","issn":"0566-8174","usgsCitation":"Taylor, H.E., Peart, D., Antweiler, R.C., Brinton, T., Campbell, W.L., Barbarino, J., Roth, D., Hart, R.J., and Averett, R., 1996, Data from synoptic water-quality studies on the Colorado River in the Grand Canyon, Arizona, November 1990 and June 1991: U.S. Geological Survey Open-File Report 96-614, iv, 176 p. :ill. ; 28 cm., https://doi.org/10.3133/ofr96614.","productDescription":"iv, 176 p. :ill. ; 28 cm.","temporalStart":"1990-11-01","temporalEnd":"1991-06-30","costCenters":[],"links":[{"id":8225,"rank":9999,"type":{"id":18,"text":"Project Site"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_inorganic/","linkFileType":{"id":5,"text":"html"}},{"id":154546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0614/report-thumb.jpg"},{"id":8224,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_inorganic/download/Synoptic.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51241,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0614/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c87f","contributors":{"authors":[{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":185377,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peart, D.B.","contributorId":45304,"corporation":false,"usgs":true,"family":"Peart","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":185379,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Antweiler, Ronald C. 0000-0001-5652-6034 antweil@usgs.gov","orcid":"https://orcid.org/0000-0001-5652-6034","contributorId":1481,"corporation":false,"usgs":true,"family":"Antweiler","given":"Ronald","email":"antweil@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":185381,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Brinton, T.I.","contributorId":93922,"corporation":false,"usgs":true,"family":"Brinton","given":"T.I.","affiliations":[],"preferred":false,"id":185383,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Campbell, W. L.","contributorId":46939,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":185380,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barbarino, J.R.","contributorId":94336,"corporation":false,"usgs":true,"family":"Barbarino","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":185384,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Roth, D.A.","contributorId":100864,"corporation":false,"usgs":true,"family":"Roth","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":185385,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hart, R. J.","contributorId":62607,"corporation":false,"usgs":true,"family":"Hart","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":185382,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Averett, R. C.","contributorId":35709,"corporation":false,"usgs":true,"family":"Averett","given":"R. C.","affiliations":[],"preferred":false,"id":185378,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":22900,"text":"ofr96554 - 1996 - A modified index for assessment of potential scour at bridges over waterways","interactions":[],"lastModifiedDate":"2012-02-02T00:07:56","indexId":"ofr96554","displayToPublicDate":"1997-07-01T00:00:00","publicationYear":"1996","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":"96-554","title":"A modified index for assessment of potential scour at bridges over waterways","docAbstract":"The modified potential-scour index described in this report is based on a  potential-scour index used by the U.S. Geological Survey Maryland  District (Maryland index), and a prototype index developed by the U.S.  Geological Survey Tennessee District (Tennessee index).  The  modifications were made to (1) improve the technical content of theMaryland index, and (2) provide a more extensive set of index variables  for assessment of potential scour at bridges.  The report demonstrates  and describes problems that were encountered when using the Maryland  index in a study of county- maintained bridges in Maryland from 1993 to  1995.The modifications made to specific index variables and ranking  values in the Maryland index are presented and discussed.  A comparison  of potential-scour ratings from the modified potential- scour index, as  applied to two bridges, is presented.This comparison indicates that the  modified potential-scour index produces potential-scour ratings that most  consistently reflect scour conditions observed at these bridges.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr96554","issn":"0094-9140","usgsCitation":"Doheny, E.J., 1996, A modified index for assessment of potential scour at bridges over waterways: U.S. Geological Survey Open-File Report 96-554, iv, 16 p. ;28 cm., https://doi.org/10.3133/ofr96554.","productDescription":"iv, 16 p. ;28 cm.","costCenters":[],"links":[{"id":154231,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1996/0554/report-thumb.jpg"},{"id":52307,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1996/0554/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adead","contributors":{"authors":[{"text":"Doheny, Edward J. 0000-0002-6043-3241 ejdoheny@usgs.gov","orcid":"https://orcid.org/0000-0002-6043-3241","contributorId":4495,"corporation":false,"usgs":true,"family":"Doheny","given":"Edward","email":"ejdoheny@usgs.gov","middleInitial":"J.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":false,"id":189099,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}