{"pageNumber":"3850","pageRowStart":"96225","pageSize":"25","recordCount":185189,"records":[{"id":24944,"text":"ofr95699 - 1995 - Preliminary geologic map of the Val Verde 7.5' quadrangle, southern California: A digital database","interactions":[],"lastModifiedDate":"2023-06-08T13:28:32.544215","indexId":"ofr95699","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-699","title":"Preliminary geologic map of the Val Verde 7.5' quadrangle, southern California: A digital database","docAbstract":"This Open-File report is a digital geologic map database. A pamphlet serves to introduce and describe the digital data. There is no paper map included in the Open-File report.\n\nThis digital map database is compiled from previously published sources combined with some new mapping and modifications in nomenclature. The geologic map database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U. S. Geological Survey. For detailed descriptions of the units, their stratigraphic relations and sources of geologic mapping consult Yerkes and Campbell (1995). More specific information about the units may be available in the original sources.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr95699","issn":"0094-9140","usgsCitation":"Yerkes, R.F., and Campbell, R., 1995, Preliminary geologic map of the Val Verde 7.5' quadrangle, southern California: A digital database: U.S. Geological Survey Open-File Report 95-699, README; Database: .GZ files; Geology: 1 .GZ file; Structure: 1 .GZ file; Wells: 1 .GZ file; Composite base map: 1 .GZ file, https://doi.org/10.3133/ofr95699.","productDescription":"README; Database: .GZ files; Geology: 1 .GZ file; Structure: 1 .GZ file; Wells: 1 .GZ file; Composite base map: 1 .GZ file","additionalOnlineFiles":"Y","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":157309,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr95699.jpg"},{"id":1917,"rank":8,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1995/0699/","linkFileType":{"id":5,"text":"html"}},{"id":284112,"rank":7,"type":{"id":20,"text":"Read Me"},"url":"https://pubs.usgs.gov/of/1995/0699/pdf/valvde.pdf"},{"id":284116,"rank":5,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0699/vv-wells.e00.gz"},{"id":284117,"rank":4,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0699/vv-topo.e00.gz"},{"id":284114,"rank":3,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0699/vv-geol.e00.gz"},{"id":284113,"rank":6,"type":{"id":9,"text":"Database"},"url":"https://pubs.usgs.gov/of/1995/0699/valvde.tar.gz"},{"id":284115,"rank":2,"type":{"id":7,"text":"Companion Files"},"url":"https://pubs.usgs.gov/of/1995/0699/vv-strc.e00.gz"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.750,34.375 ], [ -118.750,34.500 ], [ -118.625,34.500 ], [ -118.625,34.375 ], [ -118.750,34.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa09","contributors":{"authors":[{"text":"Yerkes, R. F.","contributorId":24754,"corporation":false,"usgs":true,"family":"Yerkes","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":192844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, Russell H.","contributorId":91074,"corporation":false,"usgs":true,"family":"Campbell","given":"Russell H.","affiliations":[],"preferred":false,"id":192845,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24264,"text":"ofr95805B - 1995 - Time drill; an introduction to geologic time","interactions":[],"lastModifiedDate":"2012-02-02T00:08:00","indexId":"ofr95805B","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-805","chapter":"B","title":"Time drill; an introduction to geologic time","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr95805B","issn":"0094-9140","usgsCitation":"Purcell, K.P., 1995, Time drill; an introduction to geologic time: U.S. Geological Survey Open-File Report 95-805, 1 computer disk ;3 1/2 in., https://doi.org/10.3133/ofr95805B.","productDescription":"1 computer disk ;3 1/2 in.","costCenters":[],"links":[{"id":154985,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b741","contributors":{"authors":[{"text":"Purcell, Kevin P.","contributorId":101279,"corporation":false,"usgs":true,"family":"Purcell","given":"Kevin","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":191592,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27410,"text":"wri944110 - 1995 - Water levels in the Calumet aquifer and their relation to surface-water levels in northern Lake County, Indiana, 1985-92","interactions":[],"lastModifiedDate":"2016-05-24T10:55:16","indexId":"wri944110","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-4110","title":"Water levels in the Calumet aquifer and their relation to surface-water levels in northern Lake County, Indiana, 1985-92","docAbstract":"<p>The U.S. Geological Survey made 2,328 water-level measurements at a total of 96 ground-water and surface-water sites in northern Lake County, Indiana, from August 1985 through September 1992. This report lists and summarizes the significance of the measurements. Northern Lake County is on the southern shore of Lake Michigan and includes the cities of East Chicago, Gary, Hammond, and Whiting. The study area is underlain by the unconfined Calumet aquifer and receives about 36 inches of precipitation per year.</p>\n<p>The U.S. Geological Survey investigated ground-water levels and flow in the Calumet aquifer and the effect of Lake Michigan levels on ground-water and surface-water levels throughout the study area. Summary statistics of the water-level data were computed for each site.</p>\n<p>Ground-water levels annually reach a maximum in June or July and a minimum in September or October. Measured groundwater fluctuations in the Calumet aquifer during the study period ranged from 0.40 to 5.01 feet, and the mean ground-water fluctuation was about 2.3 feet The largest surface-water fluctuations were affected by record setting Lake Michigan levels. Midmonth daily averages for the data-collection period show that Lake Michigan fluctuated 4.14 feet Water-level fluctuations on the Grand Calumet River were from 1.06 to 2.45 feet.</p>\n<p>Analysis of water-level data indicates that the 1988 drought did not substantially affect water levels in the Calumet aquifer, but the deficit in precipitation reversed vertical flow gradients in ground water at three paired deep and shallow wells. High water levels in Lake Michigan during 1985-87 created long-term backwater effects on the Grand Calumet River as far as 11.0 miles upstream from Lake Michigan.</p>\n<p>Analysis of water-level data from the data-collection network indicates that the water table normally slopes toward streams, ditches, sewers, the Indiana Harbor Canal, and Lake Michigan. The slope of the water table toward the Grand Calumet River is greatest in the winter and can decrease to being almost horizontal in the summer. Wells near streams respond quickly to nearby surface-water-level changes. Water-table maps indicate that sewers and dewatering systems are lowering ground-water levels in large areas. Ditches, the Grand Calumet River, and the Indiana Harbor Canal connect the Lake Michigan water level to large parts of the study area. The surface-water stage in the Indiana Harbor Canal, which functions as a ditch, can equal Lake Michigan's stage up to 3.75 miles inland from the lakeshore. Human activity, the stage of Lake Michigan, and the storage capacity of the Calumet aquifer combine to reduce vertical changes in the water table in the study area.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri944110","collaboration":"Indiana Department of Environmental Management","usgsCitation":"Greeman, T.K., 1995, Water levels in the Calumet aquifer and their relation to surface-water levels in northern Lake County, Indiana, 1985-92: U.S. Geological Survey Water-Resources Investigations Report 94-4110, v, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri944110.","productDescription":"v, 61 p. :ill., maps ;28 cm.","startPage":"1","endPage":"61","numberOfPages":"67","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":158683,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1994/4110/report-thumb.jpg"},{"id":56269,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1994/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Lake","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.2223,41.6248],[-87.2222,41.6152],[-87.2221,41.6039],[-87.2218,41.5698],[-87.22,41.4632],[-87.2198,41.3747],[-87.2196,41.3601],[-87.22,41.3388],[-87.2198,41.3188],[-87.2197,41.3043],[-87.2189,41.2893],[-87.2187,41.2744],[-87.2193,41.2671],[-87.219,41.2426],[-87.2184,41.2417],[-87.2263,41.2353],[-87.2762,41.2187],[-87.2859,41.2154],[-87.3241,41.1862],[-87.3313,41.1829],[-87.3405,41.1824],[-87.3448,41.1824],[-87.38,41.1726],[-87.394,41.1625],[-87.4,41.1625],[-87.4055,41.1625],[-87.4147,41.1619],[-87.4411,41.1731],[-87.4466,41.174],[-87.4484,41.1744],[-87.4587,41.1702],[-87.4801,41.1701],[-87.5263,41.1661],[-87.5261,41.267],[-87.5265,41.2983],[-87.527,41.4086],[-87.5265,41.4712],[-87.5255,41.5516],[-87.5239,41.6941],[-87.524,41.7135],[-87.5234,41.7131],[-87.5134,41.7054],[-87.5158,41.7027],[-87.5133,41.7004],[-87.4997,41.6914],[-87.4922,41.6865],[-87.4848,41.6843],[-87.4829,41.6811],[-87.4768,41.6789],[-87.4712,41.6753],[-87.4613,41.6718],[-87.4503,41.6741],[-87.4397,41.6647],[-87.436,41.6656],[-87.4355,41.6729],[-87.4245,41.6802],[-87.4177,41.6753],[-87.4396,41.6565],[-87.4228,41.6439],[-87.4167,41.6439],[-87.4099,41.644],[-87.4087,41.644],[-87.4044,41.6413],[-87.392,41.6382],[-87.3748,41.6329],[-87.3711,41.6315],[-87.3538,41.6285],[-87.3384,41.6259],[-87.3274,41.6259],[-87.3218,41.6219],[-87.315,41.6201],[-87.3101,41.6201],[-87.3058,41.6202],[-87.3003,41.6202],[-87.296,41.6198],[-87.2831,41.6203],[-87.2702,41.6208],[-87.2223,41.6248]]]},\"properties\":{\"name\":\"Lake\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9d21","contributors":{"authors":[{"text":"Greeman, Theodore K.","contributorId":30655,"corporation":false,"usgs":true,"family":"Greeman","given":"Theodore","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":198064,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23617,"text":"ofr95816 - 1995 - Re-examination of rock geochemistry in the Copper Canyon area, Lander County, Nevada","interactions":[],"lastModifiedDate":"2022-08-31T18:25:11.201831","indexId":"ofr95816","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-816","title":"Re-examination of rock geochemistry in the Copper Canyon area, Lander County, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95816","usgsCitation":"Kotlyar, B.B., Theodore, T.G., and Jachens, R., 1995, Re-examination of rock geochemistry in the Copper Canyon area, Lander County, Nevada: U.S. Geological Survey Open-File Report 95-816, 47 p., https://doi.org/10.3133/ofr95816.","productDescription":"47 p.","costCenters":[],"links":[{"id":406010,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18553.htm","linkFileType":{"id":5,"text":"html"}},{"id":52894,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0816/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0816/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Lander County","otherGeospatial":"Copper Canyon area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.15,\n              40.517\n            ],\n            [\n              -117.1179,\n              40.517\n            ],\n            [\n              -117.117,\n              40.567\n            ],\n            [\n              -117.15,\n              40.567\n            ],\n            [\n              -117.15,\n              40.517\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6486c3","contributors":{"authors":[{"text":"Kotlyar, B. B.","contributorId":74408,"corporation":false,"usgs":true,"family":"Kotlyar","given":"B.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":190423,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theodore, T. G.","contributorId":38122,"corporation":false,"usgs":true,"family":"Theodore","given":"T.","middleInitial":"G.","affiliations":[],"preferred":false,"id":190421,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jachens, R.C.","contributorId":55433,"corporation":false,"usgs":true,"family":"Jachens","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":190422,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23762,"text":"ofr95423 - 1995 - Water-resources activities in Arkansas, 1992-94","interactions":[],"lastModifiedDate":"2012-02-02T00:08:11","indexId":"ofr95423","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-423","title":"Water-resources activities in Arkansas, 1992-94","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Report Section [distributor],","doi":"10.3133/ofr95423","issn":"0094-9140","usgsCitation":"Louthian, B.L., 1995, Water-resources activities in Arkansas, 1992-94: U.S. Geological Survey Open-File Report 95-423, iv, 44 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr95423.","productDescription":"iv, 44 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":156370,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0423/report-thumb.jpg"},{"id":52992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0423/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa147","contributors":{"authors":[{"text":"Louthian, Bobbie L. louthian@usgs.gov","contributorId":737,"corporation":false,"usgs":true,"family":"Louthian","given":"Bobbie","email":"louthian@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":true,"id":190673,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23700,"text":"ofr95435 - 1995 - Bibliography for Hayes, Spurr, Crater Peak, Redoubt, Iliamna, Augustine, Douglas, and Aniakchak volcanoes, Alaska","interactions":[],"lastModifiedDate":"2019-06-05T12:34:31","indexId":"ofr95435","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-435","title":"Bibliography for Hayes, Spurr, Crater Peak, Redoubt, Iliamna, Augustine, Douglas, and Aniakchak volcanoes, Alaska","docAbstract":"Alaska has more than 40 active volcanoes, many of which are close to the major population centers of south-central Alaska. This bibliography was compiled to assist in the preparation of volcano hazard evaluations at Cook Inlet volcanoes. It lists articles, reports, and maps about the geology and hydrology of Hayes, Spurr, Redoubt, Iliamna, Augustine, and Douglas volcanoes in the Cook Inlet region as well as Aniakchak Volcano on the Alaska Peninsula. References on the biology and archaeology of areas surrounding each volcano also are included because they may provide useful background information.","language":"English","publisher":"U.S. Geological Survey ","publisherLocation":"Reston, VA","doi":"10.3133/ofr95435","issn":"0094-9140","usgsCitation":"Lemke, K., May, B., and Vanderpool, A., 1995, Bibliography for Hayes, Spurr, Crater Peak, Redoubt, Iliamna, Augustine, Douglas, and Aniakchak volcanoes, Alaska: U.S. Geological Survey Open-File Report 95-435, iii, 32 p. , https://doi.org/10.3133/ofr95435.","productDescription":"iii, 32 p. ","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":52948,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0435/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":156311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0435/report-thumb.jpg"}],"country":"United States","state":"Alaska","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629ac5","contributors":{"authors":[{"text":"Lemke, K.J.","contributorId":12519,"corporation":false,"usgs":true,"family":"Lemke","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":190566,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, B.A.","contributorId":8872,"corporation":false,"usgs":true,"family":"May","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":190565,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vanderpool, A.M.","contributorId":14451,"corporation":false,"usgs":true,"family":"Vanderpool","given":"A.M.","affiliations":[],"preferred":false,"id":190567,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21972,"text":"ofr95210 - 1995 - National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 1","interactions":[],"lastModifiedDate":"2012-02-02T00:07:45","indexId":"ofr95210","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-210","title":"National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 1","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"National Earthquake Hazards Reduction Program, annual project summaries, XXXVI","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr95210","issn":"0094-9140","usgsCitation":"Jacobson, M.L., 1995, National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 1 (Volume 1): U.S. Geological Survey Open-File Report 95-210, Volume 1 - Total: 592 p.; Report: Pages 1-574; Index: I1-I13, https://doi.org/10.3133/ofr95210.","productDescription":"Volume 1 - Total: 592 p.; Report: Pages 1-574; Index: I1-I13","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":152892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0210/report-thumb.jpg"},{"id":51448,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0210/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Volume 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69894b","contributors":{"authors":[{"text":"Jacobson, Muriel L. (compiler)","contributorId":42965,"corporation":false,"usgs":true,"family":"Jacobson","given":"Muriel","suffix":"(compiler)","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":186501,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21161,"text":"ofr95274 - 1995 - Potassium-argon apparent ages of rocks from the western Okanogan Range, the Methow Basin, and adjacent areas, north-central Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:07:41","indexId":"ofr95274","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-274","title":"Potassium-argon apparent ages of rocks from the western Okanogan Range, the Methow Basin, and adjacent areas, north-central Washington","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95274","usgsCitation":"Todd, V.R., 1995, Potassium-argon apparent ages of rocks from the western Okanogan Range, the Methow Basin, and adjacent areas, north-central Washington: U.S. Geological Survey Open-File Report 95-274, 10 p. ;28 cm., https://doi.org/10.3133/ofr95274.","productDescription":"10 p. ;28 cm.","costCenters":[],"links":[{"id":153363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0274/report-thumb.jpg"},{"id":50752,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0274/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683976","contributors":{"authors":[{"text":"Todd, V. R.","contributorId":89918,"corporation":false,"usgs":true,"family":"Todd","given":"V.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":183950,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22409,"text":"ofr95826 - 1995 - Some fluid-inclusion measurements for geothermal drill holes in California, Nevada, El Salvador, and Russia","interactions":[],"lastModifiedDate":"2019-03-15T10:41:01","indexId":"ofr95826","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-826","title":"Some fluid-inclusion measurements for geothermal drill holes in California, Nevada, El Salvador, and Russia","docAbstract":"<p>The purpose of this report is to make available fluid-inclusion information from drill holes in five geothermal areas: The Geysers and Long Valley caldera in northern California; Steamboat Springs, Nevada; the Ahuachapan field of El Salvador, Central America; and the Mutnovsky geothermal field, Kamchatka Peninsula, Russia. These data were produced at the request of various individuals to provide needed subsurface-temperature data for their investigations. The fluid-inclusion information presented in this report has not been previously published, and, since the author did not work in these geothermal areas, only a very minimal attempt is made at interpreting the data. Information on the location of the drill holes from which the core specimens originated ranges from very poor in the case of the Russian drill holes to very good for those in the USA. </p><p>Mineral specimens from drill-core samples in the five geothermal areas were utilized as cleavage chips, thin sections polished on a single side, or double polished thin sections (polished on both sides). Fluid inclusions from all three USA geothermal areas were found in either hydrothermal or primary quartz crystals. These fluid inclusions firstly were frozen and gradually thawed to determine the final melting-point temperatures (Tm) as the last piece of ice melted and secondly, were heated to the temperature at which the vapor phase disappeared to obtain homogenization temperatures (Tn). For the El Salvador and Russian core specimens the fluid inclusions were hosted in calcite, and the order of the two procedures was reversed because calcite is a much softer mineral than quartz and there is a greater danger of the fluid inclusions decrepitating as the ice expands during freezing. </p><p>A Chaixmeca microthermometry apparatus was used during studies of the Steamboat Springs and The Geysers fluid inclusions. For the remaining studies, a Linkam THM 600 heating/freezing stage and TMS 90 temperature control system were employed. Accuracy of the data generated from both instruments is similar, with values of about ±2°C for heating studies and about ±0.2°C for the freezing methods.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95826","issn":"0094-9140","usgsCitation":"Bargar, K.E., 1995, Some fluid-inclusion measurements for geothermal drill holes in California, Nevada, El Salvador, and Russia: U.S. Geological Survey Open-File Report 95-826, 14 p., https://doi.org/10.3133/ofr95826.","productDescription":"14 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":156487,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0826/report-thumb.jpg"},{"id":51954,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0826/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e9359","contributors":{"authors":[{"text":"Bargar, Keith E.","contributorId":9643,"corporation":false,"usgs":true,"family":"Bargar","given":"Keith","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":188191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22412,"text":"ofr95637 - 1995 - Organic geochemical analysis and thermochronologic modeling of potential petroleum source rocks in the Malheur, Jordan and Andrews resource areas, southeastern Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:08:05","indexId":"ofr95637","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-637","title":"Organic geochemical analysis and thermochronologic modeling of potential petroleum source rocks in the Malheur, Jordan and Andrews resource areas, southeastern Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\n[Books and Open-File Reports Section, distributor,","doi":"10.3133/ofr95637","issn":"0094-9140","usgsCitation":"Barker, C., 1995, Organic geochemical analysis and thermochronologic modeling of potential petroleum source rocks in the Malheur, Jordan and Andrews resource areas, southeastern Oregon: U.S. Geological Survey Open-File Report 95-637, 44 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr95637.","productDescription":"44 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":155610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0637/report-thumb.jpg"},{"id":51957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0637/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68ad84","contributors":{"authors":[{"text":"Barker, C.E.","contributorId":69991,"corporation":false,"usgs":true,"family":"Barker","given":"C.E.","affiliations":[],"preferred":false,"id":188196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22265,"text":"ofr95191 - 1995 - Water-quality assessment of the Albemarle-Pamlico drainage basin, North Carolina and Virginia: Characterization of suspended sediment, nutrients, and pesticides","interactions":[],"lastModifiedDate":"2022-12-13T21:05:16.987622","indexId":"ofr95191","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-191","title":"Water-quality assessment of the Albemarle-Pamlico drainage basin, North Carolina and Virginia: Characterization of suspended sediment, nutrients, and pesticides","docAbstract":"The 28,000-square-mile Albemarle-Pamlico drainage basin includes the Roanoke, Dan, Chowan Tar, and Neuse Rivers. The basin extends through four physiographic provinces in North Carolina and Virginia-Valley and Ridge, Blue Ridge, Piedmont and Coastal Plain. The spatial and temporal trends in ground-water and riverine water quality in the study area were characterized by using readily available data sources The primary data sources that were used included the U.S. Geological Survey's National Water Data Storage and Retrieval System (WATSTORE) database, the U.S. Environmental Protection Agency's Storage and Retrieval System (STORET) database, and results of a few investigations of pesticide occurrence. The principal water-quality constituents examined were suspended sediment, nutrients, and pesticides. The data examined generally spanned the period from 1950 to 1993.\r\n\r\nThe only significant trends in suspended sediment were detected at three Chowan River tributary sites which showed long-term decreases. Suspended- and total-solids concentrations have decreased throughout the Albemarle-Pamlico drainage basin. The decreases are probably a result of (1) construction of new lakes and ponds in the basin, which trap solids, (2) improved agricultural soil management, and (3) improved wastewater treatment. \r\n\r\nNutrient point sources are much less than nonpoint nutrient sources at the eight NASQAN basins examined for nutrient loads. The greatest nitrogen inputs are associated with crop fertilizer and biological nitrogen fixation by soybeans and peanuts, whereas atmospheric and animal-related nitrogen inputs are comparable in magnitude. The largest phosphorus inputs are associated with animal wastes.\r\n\r\nThe most commonly detected pesticides in surface water in the STORET database were atrazine and aldrin.Intensive organonitrogen herbicide sampling of Chicod Creek in 1992 showed seasonal variations in pesticide concentration. The most commonly detected herbicides were atrazine, alachlor, metolachlor, prometon, and metribuzin. No relation between streamflow and pesticide concentration was evident.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95191","usgsCitation":"Harned, D., McMahon, G., Spruill, T., and Woodside, M.D., 1995, Water-quality assessment of the Albemarle-Pamlico drainage basin, North Carolina and Virginia: Characterization of suspended sediment, nutrients, and pesticides: U.S. Geological Survey Open-File Report 95-191, x, 131 p., https://doi.org/10.3133/ofr95191.","productDescription":"x, 131 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":51691,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0191/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":154446,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0191/report-thumb.jpg"},{"id":410401,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18416.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"North Carolina, Virginia","otherGeospatial":"Albemarle-Pamlico drainage basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.406,\n              37.592\n            ],\n            [\n              -80.406,\n              34.531\n            ],\n            [\n              -75.281,\n              34.531\n            ],\n            [\n              -75.281,\n              37.592\n            ],\n            [\n              -80.406,\n              37.592\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e7077","contributors":{"authors":[{"text":"Harned, Douglas","contributorId":11195,"corporation":false,"usgs":true,"family":"Harned","given":"Douglas","affiliations":[],"preferred":false,"id":187853,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McMahon, Gerard 0000-0001-7675-777X gmcmahon@usgs.gov","orcid":"https://orcid.org/0000-0001-7675-777X","contributorId":191488,"corporation":false,"usgs":true,"family":"McMahon","given":"Gerard","email":"gmcmahon@usgs.gov","affiliations":[{"id":565,"text":"Southeast Climate Science Center","active":true,"usgs":true},{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"preferred":true,"id":187852,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Spruill, T.B.","contributorId":76747,"corporation":false,"usgs":true,"family":"Spruill","given":"T.B.","affiliations":[],"preferred":false,"id":187854,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Woodside, M. D.","contributorId":98722,"corporation":false,"usgs":true,"family":"Woodside","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":187855,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26008,"text":"wri924192 - 1995 - Geohydrology and water quality of stratified-drift aquifers in the middle Merrimack River basin, south-central New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:08:24","indexId":"wri924192","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"92-4192","title":"Geohydrology and water quality of stratified-drift aquifers in the middle Merrimack River basin, south-central New Hampshire","docAbstract":"The U.S. Geological Survey, in cooperation with the State of New Hampshire, Department of Environmental Services, Water Resources Division has assessed the geohydrology and water quality of stratified-drift aquifers in the middle Merrimack River basin in south-central New Hampshire. The middle Merrimack River basin drains 469 square miles; 98 square miles is underlain by stratified-drift aquifers. Saturated thickness of stratified drift within the study area is generally less than 40 feet but locally greater than 100 feet. Transmissivity of stratified-drift aquifers is generally less than 2,000 feet squared per day but locally exceeds 6, 000 feet squared per day. At present (1990), ground-water withdrawals from stratified drift for public supply are about 0.4 million gallons per day within the basin. Many of the stratified-drift aquifers within the study area are not developed to their fullest potential. The geohydrology of stratified-drift aquifers was investigated by focusing on basic aquifer properties, including aquifer boundaries; recharge, discharge, and direction of ground-water flow; saturated thickness and storage; and transmissivity. Surficial geologic mapping assisted in the determination of aquifer boundaries. Data from 757 wells and test borings were used to produce maps of water-table altitude, saturated thickness, and transmissivity of stratified drift. More than 10 miles of seismic-refraction profiling and 14 miles of seismic-reflection profiling were also used to construct the water table and saturated-thickness maps. Stratified-drift aquifers in the southern, western, and central parts of the study area are typically small and discontinuous, whereas aquifers in the eastern part along the Merrimack River valley are continuous. The Merrimack River valley aquifers formed in glacial Lakes Merrimack and Hooksett. Many other smaller discontinuous aquifers formed in small temporary ponds during deglaciation. A stratified-drift aquifer in Goffstown was analyzed for aquifer yield by use of a two-dimensional, finite-difference ground-water-flow model. Yield of the Goffstown aquifer was estimated to be 2.5 million gallons per day. Sensitivity analysis showed that the estimate of aquifer yield was most sensitive to changes in hydraulic conductivity. The amount of water induced into the aquifer from the Piscataquog River was most affected by changes in estimates of streambed conductance. Results of analysis of water samples from 10 test wells indicate that, with some exceptions, water in the stratified-drift aquifers generally meets U.S. Environmental Protection Agency primary and secondary drinking-water regulations. Water from two wells had elevated sodium concentrations, waterfront two wells had elevated concentrations of dissolved iron, and waterfront seven wells had elevated concentrations of manganese. Known areas of contamination were avoided during water-quality sampling.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri924192","usgsCitation":"Ayotte, J., and Toppin, K.W., 1995, Geohydrology and water quality of stratified-drift aquifers in the middle Merrimack River basin, south-central New Hampshire: U.S. Geological Survey Water-Resources Investigations Report 92-4192, 1 v. (various pagings) :ill., maps (some col.) ;28 cm.;  PGS - 149 p., 4 over-size sheets, scale 1:24,000, https://doi.org/10.3133/wri924192.","productDescription":"1 v. (various pagings) :ill., maps (some col.) ;28 cm.;  PGS - 149 p., 4 over-size sheets, scale 1:24,000","costCenters":[],"links":[{"id":2007,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri924192/","linkFileType":{"id":5,"text":"html"}},{"id":123655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_92_4192.jpg"},{"id":54767,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54768,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54769,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54770,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54771,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54772,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54773,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54774,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1992/4192/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b8c","contributors":{"authors":[{"text":"Ayotte, Joseph D. jayotte@usgs.gov","contributorId":1802,"corporation":false,"usgs":true,"family":"Ayotte","given":"Joseph D.","email":"jayotte@usgs.gov","affiliations":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"preferred":false,"id":195634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toppin, Kenneth W. ktoppin@usgs.gov","contributorId":3753,"corporation":false,"usgs":true,"family":"Toppin","given":"Kenneth","email":"ktoppin@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":195635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27608,"text":"wri954098 - 1995 - Water-quality characteristics of selected public recreational lakes and ponds in Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:08:42","indexId":"wri954098","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-4098","title":"Water-quality characteristics of selected public recreational lakes and ponds in Connecticut","docAbstract":"Reconnaissance limnological and lakebed-sediment surveys were conducted in Connecticut during 1989-91 by the U.S. Geological Survey, in cooperation with the Connecticut Department of Environmental Protec- tion, to evaluate water-quality characteristics of selected public recreational lakes and ponds in the State. Limnological surveys were conducted on 49 lakes and ponds selected from a list of 105 publicly owned waterbodies that qualified for water- quality assessments under Section 314 of the Federal Clean Water Act. Lakebed-sediment surveys were conducted in 9 river impoundments and 1 riverine lake below industrial areas and 2 headwater lakes in relatively pristine areas. The limnological surveys consisted of two sampling events--during spring turnover and during the summer stratifi- cation. Each sampling event included depth profiles of water temperature, specific conductance, hydrogen-ion activity, and dissolved oxygen concen- trations; measurements of Secchi disc transparency; and the collection of samples for the analyses of alkalinity, chlorophyll, phosphorus, and nitrogen concentrations. Areal extent and population density of the dominant aquatic macrophytes were qualita- tively noted during the summer sampling event. These water-quality data were used to determine the trophic classification and acidification status of the 49 lakes. The trophic classification yielded the following results: 2 oligotrophic, 8 early mesotrophic, 13 mesotrophic, 5 late mesotrophic, 10 eutrophic, and 11 highly eutrophic lakes. In terms of acidification status, 7 lakes were classified as acid threatened and 42 as not threatened. A Wilcoxon two-tailed signed rank test was used to compare data for 13 lakes and ponds from the present survey with data from the 1973-75 or 1978-79 surveys conducted by the Connecticut Agricultural Experiment Station and Connecticut Department of Environmental Protection. The test showed no significant difference at the 90 percent confidence level for spring nitrogen and summer chlorophyll-a concen- trations, a significant increase at the 90 percent confidence level in summer phosphorus concentra- tions, and a significant decrease at the 95 percent confidence level in summer transparency. For the lakebed-sediment surveys, composite-grab samples were collected from the deepest part of each lake. Samples were analyzed for arsenic, cyanide, organic and inorganic carbon, selected metals, and methylene-extractable, synthetic organic compounds classified by the U.S. Environmental Protection Agency as semi-volatile priority pollutants. Hanover Pond, Eagleville Lake, and West Thompson Lake had three of the four highest concentrations of cadmium, chromium, copper, lead, nickel, zinc, and cyanide. The four lakes with the highest concentrations of arsenic (Aspinook Pond, Fitchville Pond, Mashapaug Pond, and West Thompson Lake) are located in the eastern part of Connecticut. The three samples with the highest mercury concentrations were from Lake Lillinonah and Lake Zoar. There appears to be a positive correlation between the concentrations of cadmium, chromium, copper, lead, nickel, zinc, and cyanide. Only 15 of the 54 synthetic organic compounds analyzed for were detected in 9 of the 12 lakes sampled. Of these 15 compounds, 14 are polycyclic aromatic hydrocarbons and the 15th is a phthalate ester. Hanover Pond had the most compounds detected (9), and phenanthrene was the compound detected in the most lakes (8).","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954098","usgsCitation":"Healy, D.F., and Kulp, K., 1995, Water-quality characteristics of selected public recreational lakes and ponds in Connecticut: U.S. Geological Survey Water-Resources Investigations Report 95-4098, ix, 277 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri954098.","productDescription":"ix, 277 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159026,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4098/report-thumb.jpg"},{"id":56474,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4098/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fafec","contributors":{"authors":[{"text":"Healy, D. F.","contributorId":97120,"corporation":false,"usgs":true,"family":"Healy","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":198405,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kulp, K.P.","contributorId":49791,"corporation":false,"usgs":true,"family":"Kulp","given":"K.P.","email":"","affiliations":[],"preferred":false,"id":198404,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29519,"text":"wri924093 - 1995 - Simulation of streamflow and sediment transport in two surface-coal-mined basins in Fayette County, Pennsylvania","interactions":[],"lastModifiedDate":"2022-09-16T21:33:46.050946","indexId":"wri924093","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"92-4093","title":"Simulation of streamflow and sediment transport in two surface-coal-mined basins in Fayette County, Pennsylvania","docAbstract":"The Hydrological Simulation Program - Fortran (HSPF) was used to simulate streamflow and sediment transport in two surface-mined basins of Fayette County, Pa. Hydrologic data from the Stony Fork Basin (0.93 square miles) was used to calibrate HSPF parameters. The calibrated parameters were applied to an HSPF model of the Poplar Run Basin (8.83 square miles) to evaluate the transfer value of model parameters. The results of this investigation provide information to the Pennsylvania Department of Environmental Resources, Bureau of Mining and Reclamation, regarding the value of the simulated hydrologic data for use in cumulative hydrologic-impact assessments of surface-mined basins. \r\n     The calibration period was October 1, 1985, through September 30, 1988 (water years 1986-88). The simulated data were representative of the observed data from the Stony Fork Basin. Mean simulated streamflow was 1.64 cubic feet per second compared to measured streamflow of 1.58 cubic feet per second for the 3-year period. The difference between the observed and simulated peak stormflow ranged from 4.0 to 59.7 percent for 12 storms. The simulated sediment load for the 1987 water year was 127.14 tons (0.21 ton per acre), which compares to a measured sediment load of 147.09 tons (0.25 ton per acre). The total simulated suspended-sediment load for the 3-year period was 538.2 tons (0.30 ton per acre per year), which compares to a measured sediment load of 467.61 tons (0.26 ton per acre per year). \r\n\r\n     The model was verified by comparing observed and simulated data from October 1, 1988, through September 30, 1989. The results obtained were comparable to those from the calibration period. The simulated mean daily discharge was representative of the range of data observed from the basin and of the frequency with which specific discharges were equalled or exceeded.\r\n\r\n     The calibrated and verified parameters from the Stony Fork model were applied to an HSPF model of the Poplar Run Basin. The two basins are in a similar physical setting. Data from October 1, 1987, through September 30, 1989, were used to evaluate the Poplar Run model. In general, the results from the Poplar Run model were comparable to those obtained from the Stony Fork model. The difference between observed and simulated total streamflow was 1.1 percent for the 2-year period. The mean annual streamflow simulated by the Poplar Run model was 18.3 cubic feet per second. This compares to an observed streamflow of 18.15 cubic feet per second. For the 2-year period, the simulated sediment load was 2,754 tons (0.24 ton per acre per year), which compares to a measured sediment load of 3,051.2 tons (0.27 ton per acre per year) for the Poplar Run Basin. Cumulative frequency-distribution curves of the observed and simulated streamflow compared well. The comparison between observed and simulated data improved as the time span increased. Simulated annual means and totals were more representative of the observed data than hourly data used in comparing storm events.\r\n\r\n     The structure and organization of the HSPF model facilitated the simulation of a wide range of hydrologic processes. The simulation results from this investigation indicate that model parameters may be transferred to ungaged basins to generate representative hydrologic data through modeling techniques.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri924093","usgsCitation":"Sams, J.I., and Witt, E., 1995, Simulation of streamflow and sediment transport in two surface-coal-mined basins in Fayette County, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 92-4093, vi, 52 p., https://doi.org/10.3133/wri924093.","productDescription":"vi, 52 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":406891,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47658.htm","linkFileType":{"id":5,"text":"html"}},{"id":58357,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1992/4093/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159722,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1992/4093/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"Fayette County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.6,\n              39.75\n            ],\n            [\n              -79.425,\n              39.75\n            ],\n            [\n              -79.425,\n              40.0667\n            ],\n            [\n              -79.6,\n              40.0667\n            ],\n            [\n              -79.6,\n              39.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e492de4b07f02db57ef5c","contributors":{"authors":[{"text":"Sams, J. I. III","contributorId":50548,"corporation":false,"usgs":true,"family":"Sams","given":"J.","suffix":"III","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":201654,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witt, E. C. III","contributorId":105746,"corporation":false,"usgs":true,"family":"Witt","given":"E. C.","suffix":"III","affiliations":[],"preferred":false,"id":201655,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25523,"text":"wri944237 - 1995 - Geohydrology and water quality of the Durham Center Area, Durham, Connecticut","interactions":[],"lastModifiedDate":"2019-10-15T06:53:59","indexId":"wri944237","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"94-4237","title":"Geohydrology and water quality of the Durham Center Area, Durham, Connecticut","docAbstract":"Contaminated ground water is widespread and persistent beneath the Durham Center area in the town of Durham, Conn. Most of the contaminants are organic halides, usually trichloroethene, 1,1,1-trichloroethane, and tetrachloroethene. Less extensive chemical contamination of surface water, soil, and glacial sediments also has been detected. Two manufacturing companies, located at the northern and southern ends of this largely residential area, are believed to be the principal sources of the organic compounds detected in ground water. The contamination of water in the bedrock, the primary source of drinking water throughout the area, is the major environmental concern. Maximum concentrations of trichloroethene in three bed- rock wells range from 4,500 to about 5,500 mg/L (micrograms per liter). Concentrations of trichloroethene greater than 5 mg/L, the maximum contaminant level established for drinking water by the U.S Environmental Protection Agency, have regularly been detected in water samples from many other bedrock wells for at least 9 years. The geohydrology of the area is highly complex. Compact lodgment till that is up to 30 feet thick and probably fractured, overlies the bedrock. The bedrock is lithologically heterogeneous, and con- sists mostly of red fluvial sandstone, siltstone, and conglomerate; it is locally interbedded with black lacustrine shales and gray sandstones. Lithology and stratigraphy interpreted from borehole-geophysical logs at Durham Center are consistent with the Portland Formation subfacies described in earlier geologic studies. Beds strike nearly north-south and dip gently eastward. At least one high-angle normal fault transects the bedrock; it strikes northeast and dips northwest. Acoustic televiewer logs, measurements at out-crops, and azimuthal, square-array, resistivity data indicate a dominance of northeast-striking fractures that dip steeply northwest and southeast. Less prevalent strike directions are north to east-north-east. The till and sedimentary bedrock are dual-porosity, dual-permeability media. The hydraulic conductivity of the bulk mass of till is believed to be on the order of tenths of a foot per day to about 2.5 feet per day, with a total porosity of about 25 percent and an estimated average fracture porosity of less than 1 percent. The reported transmissivities of the bedrock range from less than 1 to about 17,000 feet squared per day and storativity is generally about 10-4, but the accuracy of these values is uncertain. The intergranular porosity of the sandstone units is estimated to average 5 percent, and estimates of fracture porosity from square-array, resistivity soundings at two sites were 1.1 and 2.7 percent. The bedrock has characteristics of both a single aquifer and a multi-unit, artesian or leaky aquifer system. A local ground-water-flow system that includes the upper part of the bedrock is unconfined. A large- scale flow system in deeper parts of the bedrock has transported organic compounds across topographic drainage divides. Borehole-geophysical logs and head measurements indicate that the natural ground- water-flow system in the bedrock has been altered by drilled wells that connect fractures and by with- drawals from wells. A conceptual model of the movement and fate of organic contaminants suggests that (1) nonaqueous phase organic halides are retained near their source; (2) flow is primarily through fractures in the till and through fractures and bedding-plane openings in the sedimentary rocks; (3) retardation of contaminants occurs primarily by diffusion from fractures into the aquifer matrix; and (4) transport directions of dissolved organic halides are controlled by a combination of natural hydraulic gradients, hydraulic gradients produced by the cyclical pumping of wells, and by the strike directions of bedrock faults, fractures, and bedding planes.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri944237","usgsCitation":"Melvin, R., Stone, J.R., Craft, P.A., Lane, J., and Davies, B., 1995, Geohydrology and water quality of the Durham Center Area, Durham, Connecticut: U.S. Geological Survey Water-Resources Investigations Report 94-4237, v, 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,{"id":29861,"text":"wri954206 - 1995 - Numerical Simulation of Regional Changes in Ground-Water Levels and in the Freshwater-Saltwater Interface Induced by Increased Pumpage at Barbers Point Shaft, Oahu, Hawaii","interactions":[],"lastModifiedDate":"2012-03-08T17:16:15","indexId":"wri954206","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-4206","title":"Numerical Simulation of Regional Changes in Ground-Water Levels and in the Freshwater-Saltwater Interface Induced by Increased Pumpage at Barbers Point Shaft, Oahu, Hawaii","docAbstract":"The effect on the regional ground-water system of southern Oahu from increased pumpage at Barbers Point shaft was estimated by a numerical ground-water model developed for the Oahu Regional Aquifer Systems Analysis (RASA) study. The RASA model was updated by revising pumping and ground-water recharge data. Pumpage data used in the new simulations were based on the allocated pumping rates for 1995 as set by the State Commission on Water Resource Management. On the basis of numerical simulation, Barbers Point shaft can sustain a withdrawal rate of 4.34 million gallons per day without adversely affecting wells in the Waianae aquifer.\r\n\r\nFrom results of numerical simulations, it is estimated that, as a result of increasing pumpage in Barbers Point shaft by 2 million gallons per day above the 1995-allocated rate of 2.337 million gallons per day, regional declines in ground-water levels will be about 0.4 to 0.7 feet throughout the Waianae aquifer and about 0.8 ft at the shaft. The corresponding rise of the freshwater-saltwater interface, as a result of declines in ground-water levels, is estimated to be about 20 to 30 feet. Numerical simulation also indicates that changes in ground-water levels greater than about 0.1 feet do not extend across either the Waianae-Koolau unconformity or the south Schofield barrier.\r\n\r\nThe model-estimated position of the freshwater-saltwater interface, as a result of additional pumpage, ranges from 500 to 860 feet below sea level in the southern and northern parts of the aquifer, respectively, and about 540 feet below sea level at the shaft. On the basis of an estimate of the thickness of the transition-zone, the freshwater lens would remain about 240 feet thick below the shaft. In addition, the estimated declines in ground-water levels throughout the aquifer are small compared with the thickness of the freshwater lens and these declines would not be expected to affect the yields of other wells in terms of quantity.\r\n\r\nChloride concentrations in the water pumped at Barbers Point shaft were about 240 milligrams per liter in 1992. The estimated background chloride concentration is 200 to 220 milligrams per liter because of low rainfall and the contamination of recharge water from natural salt accumulation in the soil. A reduction in irrigation through 1995 is expected to reduce recharge to the aquifer from irrigation-return water and chloride concentrations associated with the irrigation water throughout the Waianae aquifer. As a result of these combined effects, chloride concentrations of water pumped from the Barbers Point shaft will likely decrease, although the length of time required for this lowering is unknown.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri954206","usgsCitation":"Souza, W.R., and Meyer, W., 1995, Numerical Simulation of Regional Changes in Ground-Water Levels and in the Freshwater-Saltwater Interface Induced by Increased Pumpage at Barbers Point Shaft, Oahu, Hawaii: U.S. Geological Survey Water-Resources Investigations Report 95-4206, iv, 47 p., https://doi.org/10.3133/wri954206.","productDescription":"iv, 47 p.","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":123829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4206/report-thumb.jpg"},{"id":58672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4206/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696893","contributors":{"authors":[{"text":"Souza, William R.","contributorId":90295,"corporation":false,"usgs":true,"family":"Souza","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":202256,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, William","contributorId":87538,"corporation":false,"usgs":true,"family":"Meyer","given":"William","affiliations":[],"preferred":false,"id":202255,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":54113,"text":"ofr95210_V2 - 1995 - National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 2","interactions":[],"lastModifiedDate":"2012-02-02T00:11:38","indexId":"ofr95210_V2","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-210","title":"National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 2","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"National Earthquake Hazards Reduction Program, annual project summaries, XXXVI","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr95210_V2","issn":"0094-9140","usgsCitation":"Jacobson, M.L., 1995, National Earthquake Hazards Reduction Program, annual project summaries, XXXVI; Volume 2 (Volume 2): U.S. Geological Survey Open-File Report 95-210, Volume 2 - Total: 549 p.; Report: Pages 575-1101; Index: I1-I13, https://doi.org/10.3133/ofr95210_V2.","productDescription":"Volume 2 - Total: 549 p.; Report: Pages 575-1101; Index: I1-I13","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":178192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0210-v2/report-thumb.jpg"},{"id":87853,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0210-v2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Volume 2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698854","contributors":{"authors":[{"text":"Jacobson, Muriel L. (compiler)","contributorId":42965,"corporation":false,"usgs":true,"family":"Jacobson","given":"Muriel","suffix":"(compiler)","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":249232,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22940,"text":"ofr95323 - 1995 - Flood magnitude and frequency of Eightmile Branch tributary at the culvert on New Jersey route 72, at Stafford Township, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:55","indexId":"ofr95323","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-323","title":"Flood magnitude and frequency of Eightmile Branch tributary at the culvert on New Jersey route 72, at Stafford Township, New Jersey","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nUSGS Earth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/ofr95323","issn":"0094-9140","usgsCitation":"Dunne, P., 1995, Flood magnitude and frequency of Eightmile Branch tributary at the culvert on New Jersey route 72, at Stafford Township, New Jersey: U.S. Geological Survey Open-File Report 95-323, iv, 10 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr95323.","productDescription":"iv, 10 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":154281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0323/report-thumb.jpg"},{"id":52341,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0323/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eeff9","contributors":{"authors":[{"text":"Dunne, Paul","contributorId":86794,"corporation":false,"usgs":true,"family":"Dunne","given":"Paul","email":"","affiliations":[],"preferred":false,"id":189166,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22085,"text":"ofr95443 - 1995 - Quality assurance/quality control manual; National Water Quality Laboratory","interactions":[],"lastModifiedDate":"2021-05-28T17:31:18.828075","indexId":"ofr95443","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-443","title":"Quality assurance/quality control manual; National Water Quality Laboratory","docAbstract":"Quality-control practices are established for the operation of the U.S. Geological Survey's National Water Quality Laboratory. These practices specify how samples are preserved, shipped, and analyzed in the Laboratory. This manual documents the practices that are currently (1995) used in the Laboratory.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr95443","usgsCitation":"Pritt, J., and Raese, J., 1995, Quality assurance/quality control manual; National Water Quality Laboratory: U.S. Geological Survey Open-File Report 95-443, vii, 35 p., https://doi.org/10.3133/ofr95443.","productDescription":"vii, 35 p.","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":154827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0443/report-thumb.jpg"},{"id":51527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0443/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b2ee4b07f02db6b3f2c","contributors":{"authors":[{"text":"Pritt, J.W.","contributorId":10064,"corporation":false,"usgs":true,"family":"Pritt","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":187004,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raese, J.W.","contributorId":73634,"corporation":false,"usgs":true,"family":"Raese","given":"J.W.","affiliations":[],"preferred":false,"id":187005,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22435,"text":"ofr95460 - 1995 - Reference manual for data base on Nevada well logs","interactions":[],"lastModifiedDate":"2012-02-02T00:08:07","indexId":"ofr95460","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-460","title":"Reference manual for data base on Nevada well logs","docAbstract":"The U.S. Geological Survey and Nevada Division of Water Resources are cooperatively using a data base for are cooperatively using a data base for managing well-log information for the State of Nevada. The Well-Log Data Base is part of an integrated system of computer data bases using the Ingres Relational Data-Base Management System, which allows efficient storage and access to water information from the State Engineer's office. The data base contains a main table, two ancillary tables, and nine lookup tables, as well as a menu-driven system for entering, updating, and reporting on the data. This reference guide outlines the general functions of the system and provides a brief description of data tables and data-entry screens.","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/ofr95460","issn":"0094-9140","usgsCitation":"Bauer, E., and Cartier, K.D., 1995, Reference manual for data base on Nevada well logs: U.S. Geological Survey Open-File Report 95-460, iv, 29 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95460.","productDescription":"iv, 29 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":155627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0460/report-thumb.jpg"},{"id":51972,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0460/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635220","contributors":{"authors":[{"text":"Bauer, E.M.","contributorId":49816,"corporation":false,"usgs":true,"family":"Bauer","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":188248,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cartier, K. D.","contributorId":9236,"corporation":false,"usgs":true,"family":"Cartier","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":188247,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23690,"text":"ofr95697 - 1995 - Statistical property of the earth reflectivity and fractal seismic deconvolution","interactions":[],"lastModifiedDate":"2012-02-02T00:08:13","indexId":"ofr95697","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-697","title":"Statistical property of the earth reflectivity and fractal seismic deconvolution","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr95697","issn":"0094-9140","usgsCitation":"Lee, M.W., 1995, Statistical property of the earth reflectivity and fractal seismic deconvolution: U.S. Geological Survey Open-File Report 95-697, i, 21 p. :ill. ;28 cm., https://doi.org/10.3133/ofr95697.","productDescription":"i, 21 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":157070,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1995/0697/report-thumb.jpg"},{"id":52941,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1995/0697/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b958","contributors":{"authors":[{"text":"Lee, Myung W.","contributorId":84358,"corporation":false,"usgs":true,"family":"Lee","given":"Myung","middleInitial":"W.","affiliations":[],"preferred":false,"id":190554,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5028,"text":"fs18395 - 1995 - USGS Tracks Acid Rain","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"fs18395","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"183-95","title":"USGS Tracks Acid Rain","docAbstract":"The U.S. Geological Survey (USGS) has been actively studying acid rain for the past 15 years. When scientists learned that acid rain could harm fish, fear of damage to our natural environment from acid rain concerned the American public. Research by USGS scientists and other groups began to show that the processes resulting in acid rain are very complex. Scientists were puzzled by the fact that in some cases it was difficult to demonstrate that the pollution from automobiles and factories was causing streams or lakes to become more acidic. Further experiments showed how the natural ability of many soils to neutralize acids would reduce the effects of acid rain in some locations--at least as long as the neutralizing ability lasted (Young, 1991). The USGS has played a key role in establishing and maintaining the only nationwide network of acid rain monitoring stations. This program is called the National Atmospheric Deposition Program/National Trends Network (NADP/NTN). Each week, at approximately 220 NADP/NTN sites across the country, rain and snow samples are collected for analysis. NADP/NTN site in Montana. The USGS supports about 72 of these sites. The information gained from monitoring the chemistry of our nation's rain and snow is important for testing the results of pollution control laws on acid rain. ","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/fs18395","usgsCitation":"Gordon, J.D., Nilles, M.A., and Schroder, L., 1995, USGS Tracks Acid Rain: U.S. Geological Survey Fact Sheet 183-95, 2 p., https://doi.org/10.3133/fs18395.","productDescription":"2 p.","costCenters":[{"id":535,"text":"Precipitation Chemistry Quality Assurance Project","active":false,"usgs":true}],"links":[{"id":122848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/1995/0183/report-thumb.jpg"},{"id":13196,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://bqs.usgs.gov/precip/reports/arfs.php","linkFileType":{"id":5,"text":"html"}},{"id":31855,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/1995/0183/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f8dc","contributors":{"authors":[{"text":"Gordon, John D. 0000-0001-8396-8524 jgordon@usgs.gov","orcid":"https://orcid.org/0000-0001-8396-8524","contributorId":347,"corporation":false,"usgs":true,"family":"Gordon","given":"John","email":"jgordon@usgs.gov","middleInitial":"D.","affiliations":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"preferred":true,"id":150312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nilles, Mark A. manilles@usgs.gov","contributorId":3171,"corporation":false,"usgs":true,"family":"Nilles","given":"Mark","email":"manilles@usgs.gov","middleInitial":"A.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":150313,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schroder, LeRoy J.","contributorId":8454,"corporation":false,"usgs":true,"family":"Schroder","given":"LeRoy J.","affiliations":[],"preferred":false,"id":150314,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5062,"text":"fs21695 - 1995 - Mercury contamination of aquatic ecosystems","interactions":[],"lastModifiedDate":"2020-04-11T16:39:50.948014","indexId":"fs21695","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"216-95","title":"Mercury contamination of aquatic ecosystems","docAbstract":"<p>Mercury has been well known as an environmental pollutant for several decades. As early as the 1950's it was established that emissions of mercury to the environment could have serious effects on human health. These early studies demonstrated that fish and other wildlife from various ecosystems commonly attain mercury levels of toxicological concern when directly affected by mercury-containing emissions from human-related activities. Human health concerns arise when fish and wildlife from these ecosystems are consumed by humans. During the past decade, a new trend has emerged with regard to mercury pollution. Investigations initiated in the late 1980's in the northern-tier states of the U.S., Canada, and Nordic countries found that fish, mainly from nutrient-poor lakes and often in very remote areas, commonly have high levels of mercury. More recent fish sampling surveys in other regions of the U.S. have shown widespread mercury contamination in streams, wet-lands, reservoirs, and lakes. To date, 33 states have issued fish consumption advisories because of mercury contamination. These continental to global scale occurrences of mercury contamination cannot be linked to individual emissions of mercury, but instead are due to widespread air pollution. When scientists measure mercury levels in air and surface water, however, the observed levels are extraordinarily low. In fact, scientists have to take extreme precautions to avoid direct contact with water samples or sample containers, to avert sample contamination (Fig 3). Herein lies an apparent discrepancy: Why do fish from some remote areas have elevated mercury concentrations, when contamination levels in the environment are so low?</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/fs21695","usgsCitation":"Krabbenhoft, D.P., and Rickert, D.A., 1995, Mercury contamination of aquatic ecosystems: U.S. Geological Survey Fact Sheet 216-95, 4 p., https://doi.org/10.3133/fs21695.","productDescription":"4 p.","numberOfPages":"4","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science 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,{"id":30401,"text":"wri934209 - 1995 - Regression models of monthly water-level change in and near the Closed Basin Division of the San Luis Valley, south-central Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:57","indexId":"wri934209","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"93-4209","title":"Regression models of monthly water-level change in and near the Closed Basin Division of the San Luis Valley, south-central Colorado","docAbstract":"The Bureau of Reclamation is developing a water-resource project, the Closed Basin Division, in the San Luis Valley of south-central Colorado that is designed to salvage unconfined ground water that currently is discharged as evapotranspiration. The water table in and near the 130,000-acre Closed Basin Division area will be lowered by an annual withdrawal of as much as 100,000 acre-feet of ground water from the unconfined aquifer. The legislation authorizing the project limits resulting drawdown of the water table in preexisting irrigation and domestic wells outside the Closed Basin Division to a maximum of 2 feet. Water levels in the closed basin in the northern part of the San Luis Valley historically have fluctuated more than 2 feet in response to water-use practices and variation of climatically controlled recharge and discharge. Declines of water levels in nearby wells that are caused by withdrawals in the Closed Basin Division can be quantified if water-level fluctuations that result from other water-use practices and climatic variations can be estimated. This study was done to evaluate water-level change at selected observation wells in and near the Closed Basin Division. Regression models of monthly water-level change were developed to predict monthly water-level change in 46 selected observation wells. Predictions of monthly water-level change are based on one or more of the following: elapsed time, cosine and sine functions with an annual period, streamflow depletion of the Rio Grande, electrical use for agricultural purposes, runoff into the closed basin, precipitation, and mean air temperature. Regression models for five of the wells include only an intercept term and either an elapsed-time term or terms determined by the cosine and sine functions. Regression models for the other 41 wells include 1 to 4 of the 5 other variables, which can vary from month to month and from year to year. Serial correlation of the residuals was detected in 24 of the regression models. These models also include an autoregressive term to account for serial correlation in the residuals. The adjusted coefficient of determination (Ra2) for the 46 regression models range from 0.08 to 0.89, and the standard errors of estimate range from 0.034 to 2.483 feet. The regression models of monthly water- level change can be used to evaluate whether post-1985 monthly water-level change values at the selected observation wells are within the 95-percent confidence limits of predicted monthly water-level change.","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri934209","usgsCitation":"Watts, K.R., 1995, Regression models of monthly water-level change in and near the Closed Basin Division of the San Luis Valley, south-central Colorado: U.S. Geological Survey Water-Resources Investigations Report 93-4209, viii, 105 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri934209.","productDescription":"viii, 105 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1993/4209/report-thumb.jpg"},{"id":59171,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1993/4209/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":59172,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1993/4209/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c09a","contributors":{"authors":[{"text":"Watts, Kenneth R. krwatts@usgs.gov","contributorId":1647,"corporation":false,"usgs":true,"family":"Watts","given":"Kenneth","email":"krwatts@usgs.gov","middleInitial":"R.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":203190,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29985,"text":"wri954020 - 1995 - Discharge characteristics of four highway drainage systems in Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri954020","displayToPublicDate":"1996-06-01T00:00:00","publicationYear":"1995","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":"95-4020","title":"Discharge characteristics of four highway drainage systems in Ohio","docAbstract":"Excessive water in the subbase of high-way combined with large traffic volumes and heavy loads is a major cause of road deterioration. Prompt removal of any excess water in a subbase will decrease the road deterioration and extend the effective life of a highway. This study presents discharge characteristics of four highway subbase drainage systems. These systems consisted of shallow, longitudal trenches with geocomposite drain materials (edge drains made from a polyethylene core surrounded by a geotextile filter fabric) that underline the joint between the shoulder and the traffic lane of State Route 16, approximately 1.0 mile southeast of Granville, Ohio. For selected rainfall-runoff events the maximum discharge, discharge characteristics from April 1991 through November 1993 were computed for three geocomposite products- a post type, an oblong-pipe type, and a cusp type-and a conventional perforated pipe edge drain.\r\n\r\nIn general, the discharge characteristics of the conventional edge drain and that of the oblong-pipe edge drain were similar for most of the rainfall-runoff event characteristics. Both produced most of the highest maximum discharges and largest discharge volumes among the four longitudal edge drains. The post edge drain produced smaller maximum discharge and volumes than the conventional and oblong-pipe edge drains, but it had the shortest lag times for most of the event characteristics. The cusp edge drain produced small maximum discharges and small volumes similar to those from the post edge drain, but it had the longest lag times of all the edge drains for most of the event characteristics. The cusp edge drain may have also had some problems during installation which could have affected the discharge characteristics.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nEarth Science Information Center, Open-File Reports Section [distributor],","doi":"10.3133/wri954020","usgsCitation":"Straub, D., 1995, Discharge characteristics of four highway drainage systems in Ohio: U.S. Geological Survey Water-Resources Investigations Report 95-4020, iv, 20 p. :ill., map ;28 cm., https://doi.org/10.3133/wri954020.","productDescription":"iv, 20 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":126656,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4020/report-thumb.jpg"},{"id":58793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4020/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aa97","contributors":{"authors":[{"text":"Straub, D.E.","contributorId":23986,"corporation":false,"usgs":true,"family":"Straub","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":202482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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