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,{"id":54611,"text":"wdrIN971 - 1998 - Water resources data, Indiana, water year 1997","interactions":[],"lastModifiedDate":"2014-06-12T06:14:10","indexId":"wdrIN971","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IN-97-1","title":"Water resources data, Indiana, water year 1997","docAbstract":"Water resources data for the 1997 water year for Indiana consists of records of discharge, stage, and water quality\nof streams and wells; reservoir stage and contents; and water levels in lakes and wells. This report contains records\nof discharge for 166 stream-gaging stations, stage for 6 stream stations, stage and contents for 1 reservoir, water\nquality for 2 streams, and water levels for 80 lakes and 95 observation wells. These data represent that part of the\nNational Water Data System operated by the U.S. Geological Survey in Indiana in cooperation with State and Federal\nagencies.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIN971","collaboration":"Prepared in cooperation with the State of Indiana and with other agencies","usgsCitation":"Stewart, J., Keeton, C.R., Benedict, B.L., Hammil, L.E., and Nguyen, H.T., 1998, Water resources data, Indiana, water year 1997: U.S. Geological Survey Water Data Report IN-97-1, xx, 334 p., https://doi.org/10.3133/wdrIN971.","productDescription":"xx, 334 p.","numberOfPages":"357","temporalStart":"1996-10-01","temporalEnd":"1997-09-30","costCenters":[],"links":[{"id":288370,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288369,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1997/in-97-1/report.pdf"}],"projection":"Albers Equal Area projection","country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb8d4","contributors":{"authors":[{"text":"Stewart, James A.","contributorId":49824,"corporation":false,"usgs":true,"family":"Stewart","given":"James A.","affiliations":[],"preferred":false,"id":250879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keeton, Charles R.","contributorId":71220,"corporation":false,"usgs":true,"family":"Keeton","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":250880,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Benedict, Brian L.","contributorId":94351,"corporation":false,"usgs":true,"family":"Benedict","given":"Brian","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":250881,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hammil, Lowell E.","contributorId":19198,"corporation":false,"usgs":true,"family":"Hammil","given":"Lowell","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":250878,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Nguyen, Hieu T.","contributorId":97179,"corporation":false,"usgs":true,"family":"Nguyen","given":"Hieu","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":250882,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":54579,"text":"wdrIA972 - 1998 - Water resources data, Iowa, water year 1997. Volume 2: Surface water - Missouri River Basin and ground water","interactions":[],"lastModifiedDate":"2016-03-22T11:40:40","indexId":"wdrIA972","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"IA-97-2","title":"Water resources data, Iowa, water year 1997. Volume 2: Surface water - Missouri River Basin and ground water","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City, IA","doi":"10.3133/wdrIA972","usgsCitation":"May, J., Gorman, J., Goodrich, R., and Miller, V., 1998, Water resources data, Iowa, water year 1997. Volume 2: Surface water - Missouri River Basin and ground water: U.S. Geological Survey Water Data Report IA-97-2, 296 p., https://doi.org/10.3133/wdrIA972.","productDescription":"296 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":181074,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Iowa","otherGeospatial":"Missouri River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96.61376953125, 43.492782808225 ], [ -95.020751953125, 43.46886761482923 ], [ -94.8779296875, 43.13306116240612 ], [ -94.866943359375, 42.93229601903058 ], [ -95.174560546875, 42.66628070564928 ], [ -95.00976562499999, 42.08191667830631 ], [ -94.844970703125, 41.86956082699455 ], [ -94.47143554687499, 41.48389104267175 ], [ -94.163818359375, 41.07935114946899 ], [ -93.8232421875, 40.871987756697415 ], [ -93.438720703125, 41.0130657870063 ], [ -92.98828125, 40.863679665481676 ], [ -92.63671875, 40.57224011776902 ], [ -95.78979492187499, 40.58058466412764 ], [ -95.91064453125, 40.70562793820592 ], [ -95.877685546875, 40.85537053192494 ], [ -95.888671875, 41.054501963290505 ], [ -95.943603515625, 41.3025710943056 ], [ -95.965576171875, 41.4509614012039 ], [ -96.141357421875, 41.57436130598913 ], [ -96.097412109375, 41.77131167976407 ], [ -96.240234375, 42.01665183556825 ], [ -96.3720703125, 42.21224516288584 ], [ -96.427001953125, 42.42345651793833 ], [ -96.56982421875, 42.62587560259137 ], [ -96.65771484375, 42.71473218539458 ], [ -96.51489257812499, 42.97250158602597 ], [ -96.492919921875, 43.16512263158296 ], [ -96.624755859375, 43.22118973298753 ], [ -96.6357421875, 43.31718491566708 ], [ -96.558837890625, 43.33316939281732 ], [ -96.61376953125, 43.492782808225 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb87d","contributors":{"authors":[{"text":"May, J.E.","contributorId":7741,"corporation":false,"usgs":true,"family":"May","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":250743,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gorman, J.G.","contributorId":32233,"corporation":false,"usgs":true,"family":"Gorman","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":250744,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Goodrich, R.D.","contributorId":83995,"corporation":false,"usgs":true,"family":"Goodrich","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":250746,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, V.E.","contributorId":43423,"corporation":false,"usgs":true,"family":"Miller","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":250745,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54597,"text":"wdrID971 - 1998 - Water Resources Data, Idaho, Water Year 1997. Volume 1. Great Basin and Snake River Basin Above King Hill","interactions":[],"lastModifiedDate":"2012-02-02T00:11:52","indexId":"wdrID971","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ID-97-1","title":"Water Resources Data, Idaho, Water Year 1997. Volume 1. Great Basin and Snake River Basin Above King Hill","language":"ENGLISH","doi":"10.3133/wdrID971","usgsCitation":"Brennan, T., Lehmann, A., O'Dell, I., and Tungate, A., 1998, Water Resources Data, Idaho, Water Year 1997. Volume 1. Great Basin and Snake River Basin Above King Hill: U.S. Geological Survey Water Data Report ID-97-1, 460 p., https://doi.org/10.3133/wdrID971.","productDescription":"460 p.","costCenters":[],"links":[{"id":175132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb9d2","contributors":{"authors":[{"text":"Brennan, T.S.","contributorId":56708,"corporation":false,"usgs":true,"family":"Brennan","given":"T.S.","email":"","affiliations":[],"preferred":false,"id":250830,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lehmann, A.K.","contributorId":8548,"corporation":false,"usgs":true,"family":"Lehmann","given":"A.K.","email":"","affiliations":[],"preferred":false,"id":250828,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"O'Dell, I.","contributorId":80336,"corporation":false,"usgs":true,"family":"O'Dell","given":"I.","affiliations":[],"preferred":false,"id":250831,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tungate, A.M.","contributorId":38638,"corporation":false,"usgs":true,"family":"Tungate","given":"A.M.","affiliations":[],"preferred":false,"id":250829,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54867,"text":"wdrNY971 - 1998 - Water Resources Data, New York, Water Year 1997; Volume 1. Eastern New York; Excluding Long Island","interactions":[],"lastModifiedDate":"2019-05-14T10:37:17","indexId":"wdrNY971","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-97-1","title":"Water Resources Data, New York, Water Year 1997; Volume 1. Eastern New York; Excluding Long Island","docAbstract":"<p>Water resources data for the 1997 water year for New York consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground-water levels; and precipitation quality. This volume contains records for water discharge at 117 gaging stations; stage only at 9 gaging stations; stage and contents at 4 gaging stations, and 18 other lakes and reservoirs; water quality at 35 gaging stations and 1 precipitation-quality station; and water levels at 5 observation wells. Also included are data for 38 crest-stage partial-record stations. Locations of all these sites are shown on figure 8. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements and analyses.These data together with the data in volumes 2 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey in cooperation with State, Municipal, and Federal agencies in New York.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNY971","collaboration":"Prepared in cooperation with the State of New York and with other agencies","usgsCitation":"Butch, G.K., Lumia, R., and Murray, P.M., 1998, Water Resources Data, New York, Water Year 1997; Volume 1. Eastern New York; Excluding Long Island: U.S. Geological Survey Water Data Report NY-97-1, xvi, 349 p., https://doi.org/10.3133/wdrNY971.","productDescription":"xvi, 349 p.","costCenters":[],"links":[{"id":363749,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1997/ny-97-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173815,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1997/ny-97-1/report-thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.25,\n              41\n            ],\n            [\n              -73.1,\n              41\n            ],\n            [\n              -73.1,\n              45\n            ],\n            [\n              -76.25,\n              45\n            ],\n            [\n              -76.25,\n              41\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb10d","contributors":{"authors":[{"text":"Butch, Gerard K. gkbutch@usgs.gov","contributorId":914,"corporation":false,"usgs":true,"family":"Butch","given":"Gerard","email":"gkbutch@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":251826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lumia, Richard rlumia@usgs.gov","contributorId":4579,"corporation":false,"usgs":true,"family":"Lumia","given":"Richard","email":"rlumia@usgs.gov","affiliations":[],"preferred":true,"id":251824,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Murray, Patricia M. pmurray@usgs.gov","contributorId":4863,"corporation":false,"usgs":true,"family":"Murray","given":"Patricia","email":"pmurray@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":251825,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":54742,"text":"wdrMT971 - 1998 - Water resources data, Montana, water year 1997","interactions":[],"lastModifiedDate":"2020-08-21T18:08:02.447442","indexId":"wdrMT971","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MT-97-1","title":"Water resources data, Montana, water year 1997","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrMT971","usgsCitation":"Shields, R., White, M.K., Ladd, P., Chambers, C.L., and Dodge, K.A., 1998, Water resources data, Montana, water year 1997: U.S. Geological Survey Water Data Report MT-97-1, xii, 474 p., https://doi.org/10.3133/wdrMT971.","productDescription":"xii, 474 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa75a","contributors":{"authors":[{"text":"White, Roger K.","contributorId":19624,"corporation":false,"usgs":true,"family":"White","given":"Roger","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":252526,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powell, Eugene D.","contributorId":80309,"corporation":false,"usgs":true,"family":"Powell","given":"Eugene","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":252527,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50273,"text":"ofr98404 - 1998 - Level II scour analysis for Bridge 42 (NEWFTH00350042) on Town Highway 35, crossing Stratton Hill Brook, Newfane, Vermont","interactions":[],"lastModifiedDate":"2016-08-25T15:22:43","indexId":"ofr98404","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","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":"98-404","title":"Level II scour analysis for Bridge 42 (NEWFTH00350042) on Town Highway 35, crossing Stratton Hill Brook, Newfane, Vermont","docAbstract":"<p>This report provides the results of a detailed Level II analysis of scour potential at structure NEWFTH00350042 on Town Highway 35 crossing Stratton Hill Brook, Newfane, Vermont (figures 1–8). A Level II study is a basic engineering analysis of the site, including a quantitative analysis of stream stability and scour (FHWA, 1993). Results of a Level I scour investigation also are included in appendix E of this report. A Level I investigation provides a qualitative geomorphic characterization of the study site. Information on the bridge, gleaned from Vermont Agency of Transportation (VTAOT) files, was compiled prior to conducting Level I and Level II analyses and is found in appendix D. </p><p>The site is in the New England Upland section of the New England physiographic province in southeastern Vermont. The 1.16-mi2 drainage area is in a predominantly rural and forested basin. In the vicinity of the study site, the surface cover is forested. </p><p>In the study area, Stratton Hill Brook has an incised, striaght channel with a slope of approximately 0.1 ft/ft, an average channel top width of 36 ft and an average bank height of 8 ft. The channel bed material ranges from gravel to boulders with a median grain size (D50) of 121 mm (0.396 ft). The geomorphic assessment at the time of the Level I and Level II site visit on August 20, 1996, indicated that the reach was stable. </p><p>The Town Highway 34 crossing of Stratton Hill Brook is a 34-ft-long, one-lane bridge consisting of a 32-foot steel-beam span (Vermont Agency of Transportation, written communication, April 6, 1995). The opening length of the structure parallel to the bridge face is 30.8 ft. The bridge is supported by vertical, concrete abutments with upstream wingwalls. The channel is skewed approximately 20 degrees to the opening while the computed opening-skew-to-roadway is 15 degrees. </p><p>During the Level I assessment, it was observed that the right abutment footing was exposed 1.5 feet. The only scour protection measure at the site was type-1 stone fill (less than 12 inches diameter) along the downstream left bank. Additional details describing conditions at the site are included in the Level II Summary and appendices D and E.</p><p>Scour depths and recommended rock rip-rap sizes were computed using the general guidelines described in Hydraulic Engineering Circular 18 (Richardson and Davis, 1995) for the 100- and 500-year discharges. Total scour at a highway crossing is comprised of three components: 1) long-term streambed degradation; 2) contraction scour (due to accelerated flow caused by a reduction in flow area at a bridge) and; 3) local scour (caused by accelerated flow around piers and abutments). Total scour is the sum of the three components. Equations are available to compute depths for contraction and local scour and a summary of the results of these computations follows. </p><p>Contraction scour for all modelled flows was zero ft. Abutment scour ranged from 2.3 to 3.3 ft. The worst-case abutment scour occurred at the 500-year discharge. Additional information on scour depths and depths to armoring are included in the section titled “Scour Results”. Scoured-streambed elevations, based on the calculated scour depths, are presented in tables 1 and 2. A cross-section of the scour computed at the bridge is presented in figure 8. Scour depths were calculated assuming an infinite depth of erosive material and a homogeneous particle-size distribution. </p><p>It is generally accepted that the Froehlich equation (abutment scour) gives “excessively conservative estimates of scour depths” (Richardson and Davis, 1995, p. 46). Usually, computed scour depths are evaluated in combination with other information including (but not limited to) historical performance during flood events, the geomorphic stability assessment, existing scour protection measures, and the results of the hydraulic analyses. Therefore, scour depths adopted by VTAOT may differ from the computed values documented herein.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Pembroke, NH","doi":"10.3133/ofr98404","collaboration":"Prepared in cooperation with Vermont Agency of Transportation and Federal Highway Administration","usgsCitation":"Wild, E.C., and Ivanoff, M.A., 1998, Level II scour analysis for Bridge 42 (NEWFTH00350042) on Town Highway 35, crossing Stratton Hill Brook, Newfane, Vermont: U.S. Geological Survey Open-File Report 98-404, iv, 48 p., https://doi.org/10.3133/ofr98404.","productDescription":"iv, 48 p.","costCenters":[],"links":[{"id":162363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr98404.JPG"},{"id":279987,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0404/report.pdf"}],"country":"United States","state":"Vermont","city":"Newfane","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6150","contributors":{"authors":[{"text":"Wild, Emily C. 0000-0001-6157-7629 ecwild@usgs.gov","orcid":"https://orcid.org/0000-0001-6157-7629","contributorId":1810,"corporation":false,"usgs":true,"family":"Wild","given":"Emily","email":"ecwild@usgs.gov","middleInitial":"C.","affiliations":[{"id":5081,"text":"Libraries","active":false,"usgs":true}],"preferred":false,"id":241068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ivanoff, Michael A.","contributorId":27105,"corporation":false,"usgs":true,"family":"Ivanoff","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":241067,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50268,"text":"ofr9823 - 1998 - Level II scour analysis for Bridge 46 (LINCTH00060046) on Town Highway 6, crossing the New Haven River, Lincoln, Vermont","interactions":[],"lastModifiedDate":"2016-08-25T13:59:57","indexId":"ofr9823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","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":"98-23","title":"Level II scour analysis for Bridge 46 (LINCTH00060046) on Town Highway 6, crossing the New Haven River, Lincoln, Vermont","docAbstract":"<p>This report provides the results of a detailed Level II analysis of scour potential at structure LINCTH00060046 on Town Highway 6 crossing the New Haven River, Lincoln, Vermont (figures 1–8). A Level II study is a basic engineering analysis of the site, including a quantitative analysis of stream stability and scour (FHWA, 1993). Results of a Level I scour investigation also are included in appendix E of this report. A Level I investigation provides a qualitative geomorphic characterization of the study site. Information on the bridge, gleaned from Vermont Agency of Transportation (VTAOT) files, was compiled prior to conducting Level I and Level II analyses and is found in appendix D. </p><p>The site is in the Green Mountain section of the New England physiographic province in west-central Vermont. The 45.9-mi<sup>2</sup> drainage area is in a predominantly suburban and forested basin. In the vicinity of the study site, the surface cover is forest upstream of the bridge. The downstream right overbank near the bridge is suburban with buildings, homes, lawns, and pavement (less than fifty percent). The downstream left overbank is brushland while the immediate banks have dense woody vegetation. </p><p>In the study area, the New Haven River has an incised, sinuous channel with a slope of approximately 0.01 ft/ft, an average channel top width of 95 ft and an average bank height of 7 ft. The channel bed material ranges from sand to bedrock with a median grain size (D<sub>50</sub>) of 120.7 mm (0.396 ft). The geomorphic assessment at the time of the Level I and Level II site visit on June 13, 1996, indicated that the reach was stable. </p><p>The Town Highway 34 crossing of the New Haven River is a 85-ft-long, two-lane bridge consisting of an 80-foot steel arch truss (Vermont Agency of Transportation, written communication, December 14, 1995). The opening length of the structure parallel to the bridge face is 69 feet. The bridge is supported by vertical, concrete abutments with wingwalls. The channel is skewed approximately 25 degrees to the opening while the opening-skew-to-roadway is 5 degrees. </p><p>A scour hole 2.0 ft deeper than the mean thalweg depth was observed in the downstream channel during the Level I assessment. Protection measures at the site include type-1 stone fill (less than 12 inches diameter) at the upstream left wingwall, type-2 stone fill (less than 36 inches diameter) at the downstream end of the downstream left wingwall, and type-3 stone fill (less than 48 inches diameter) at the upstream right wingwall and the downstream end of the downstream right wingwall. Additional details describing conditions at the site are included in the Level II Summary and appendices D and E. </p><p>Scour depths and recommended rock rip-rap sizes were computed using the general guidelines described in Hydraulic Engineering Circular 18 (Richardson and Davis, 1995). Total scour at a highway crossing is comprised of three components: 1) long-term streambed degradation; 2) contraction scour (due to accelerated flow caused by a reduction in flow area at a bridge) and; 3) local scour (caused by accelerated flow around piers and abutments). Total scour is the sum of the three components. Equations are available to compute depths for contraction and local scour and a summary of the results of these computations follows. </p><p>Contraction scour for all modelled flows ranged from 0.0 to 1.7 ft. The worst-case contraction scour occurred at the incipient roadway-overtopping discharge. Left abutment scour ranged from 12.9 to 17.8 ft. Right abutment scour ranged from 5.9 to 11.9 ft. The worst-case abutment scour occurred at the incipient roadway-overtopping discharge. Additional information on scour depths and depths to armoring are included in the section titled “Scour Results”. Scoured-streambed elevations, based on the calculated scour depths, are presented in tables 1 and 2. A cross-section of the scour computed at the bridge is presented in figure 8. Scour depths were calculated assuming an infinite depth of erosive material and a homogeneous particle-size distribution. </p><p>It is generally accepted that the Froehlich equation (abutment scour) gives “excessively conservative estimates of scour depths” (Richardson and Davis, 1995, p. 47). Usually, computed scour depths are evaluated in combination with other information including (but not limited to) historical performance during flood events, the geomorphic stability assessment, existing scour protection measures, and the results of the hydraulic analyses. Therefore, scour depths adopted by VTAOT may differ from the computed values documented herein.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Pembroke, NH","doi":"10.3133/ofr9823","collaboration":"Prepared in cooperation with Vermont Agency of Transportation and Federal Highway Administration","usgsCitation":"Wild, E.C., 1998, Level II scour analysis for Bridge 46 (LINCTH00060046) on Town Highway 6, crossing the New Haven River, Lincoln, Vermont: U.S. Geological Survey Open-File Report 98-23, iv, 51 p., https://doi.org/10.3133/ofr9823.","productDescription":"iv, 51 p.","costCenters":[],"links":[{"id":178631,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr9823.JPG"},{"id":279992,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0023/report.pdf"}],"country":"United States","state":"Vermont","city":"Lincoln","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6077","contributors":{"authors":[{"text":"Wild, Emily C. 0000-0001-6157-7629 ecwild@usgs.gov","orcid":"https://orcid.org/0000-0001-6157-7629","contributorId":1810,"corporation":false,"usgs":true,"family":"Wild","given":"Emily","email":"ecwild@usgs.gov","middleInitial":"C.","affiliations":[{"id":5081,"text":"Libraries","active":false,"usgs":true}],"preferred":false,"id":241059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50257,"text":"ofr98289 - 1998 - Level II scour analysis for Bridge 42 (BRNETH00810042) on Town Highway 81, crossing Stevens River, Barnet, Vermont","interactions":[],"lastModifiedDate":"2013-12-02T09:23:25","indexId":"ofr98289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","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":"98-289","title":"Level II scour analysis for Bridge 42 (BRNETH00810042) on Town Highway 81, crossing Stevens River, Barnet, Vermont","language":"ENGLISH","doi":"10.3133/ofr98289","usgsCitation":"Serra, M., 1998, Level II scour analysis for Bridge 42 (BRNETH00810042) on Town Highway 81, crossing Stevens River, Barnet, Vermont: U.S. Geological Survey Open-File Report 98-289, 51 p., https://doi.org/10.3133/ofr98289.","productDescription":"51 p.","costCenters":[],"links":[{"id":179415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":280003,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0289/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6166","contributors":{"authors":[{"text":"Serra, M.M.","contributorId":81974,"corporation":false,"usgs":true,"family":"Serra","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":241042,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50261,"text":"ofr9824 - 1998 - Level II scour analysis for Bridge 16 (STRATH00180016) on Town Highway 18, crossing the West Branch of the Ompompanoosuc River, Strafford, Vermont","interactions":[],"lastModifiedDate":"2013-12-02T09:21:53","indexId":"ofr9824","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","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":"98-24","title":"Level II scour analysis for Bridge 16 (STRATH00180016) on Town Highway 18, crossing the West Branch of the Ompompanoosuc River, Strafford, Vermont","language":"ENGLISH","doi":"10.3133/ofr9824","usgsCitation":"Striker, L., and Ivanoff, M., 1998, Level II scour analysis for Bridge 16 (STRATH00180016) on Town Highway 18, crossing the West Branch of the Ompompanoosuc River, Strafford, Vermont: U.S. Geological Survey Open-File Report 98-24, 52 p., https://doi.org/10.3133/ofr9824.","productDescription":"52 p.","costCenters":[],"links":[{"id":179505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":279999,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0024/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8294","contributors":{"authors":[{"text":"Striker, L.K.","contributorId":55872,"corporation":false,"usgs":true,"family":"Striker","given":"L.K.","email":"","affiliations":[],"preferred":false,"id":241050,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ivanoff, M.A.","contributorId":45758,"corporation":false,"usgs":true,"family":"Ivanoff","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":241049,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50264,"text":"ofr98157 - 1998 - Level II scour analysis for Bridge 13 (LINCTH00010013) on Town Highway 1, crossing Cota Brook, Lincoln, Vermont","interactions":[],"lastModifiedDate":"2016-08-25T13:40:36","indexId":"ofr98157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","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":"98-157","title":"Level II scour analysis for Bridge 13 (LINCTH00010013) on Town Highway 1, crossing Cota Brook, Lincoln, Vermont","docAbstract":"<p>This report provides the results of a detailed Level II analysis of scour potential at structure LINCTH00010013 on Town Highway 1 crossing Cota Brook, Lincoln, Vermont (figures 1–8). A Level II study is a basic engineering analysis of the site, including a quantitative analysis of stream stability and scour (FHWA, 1993). Results of a Level I scour investigation also are included in appendix E of this report. A Level I investigation provides a qualitative geomorphic characterization of the study site. Information on the bridge, gleaned from Vermont Agency of Transportation (VTAOT) files, was compiled prior to conducting Level I and Level II analyses and is found in appendix D. </p><p>The site is in the Green Mountain section of the New England physiographic province in west-central Vermont. The 3.0-mi2 drainage area is in a predominantly rural and forested basin. In the vicinity of the study site, the surface cover is forest along the upstream right bank and brushland along the upstream left bank. Downstream of the bridge, the surface cover is pasture along the left and right banks. </p><p>In the study area, Cota Brook has an sinuous channel with a slope of approximately 0.01 ft/ ft, an average channel top width of 30 ft and an average bank height of 2 ft. The channel bed material ranges from sand to cobble with a median grain size (D50) of 34.7 mm (0.114 ft). The geomorphic assessment at the time of the Level I and Level II site visit on June 10, 1996, indicated that the reach was laterally unstable due to cut-banks and wide, vegetated point bars upstream and downstream of the bridge. </p><p>The Town Highway 1 crossing of Cota Brook is a 38-ft-long, two-lane bridge consisting of a 36-foot steel-stringer span (Vermont Agency of Transportation, written communication, December 14, 1995). The opening length of the structure parallel to the bridge face is 34.4 ft. The bridge is supported by vertical, concrete abutments. The channel is skewed approximately 15 degrees to the opening while the opening-skew-to-roadway is zero degrees.</p><p>A scour hole 2.0 ft deeper than the mean thalweg depth was observed along the upstream right bank during the Level I assessment. Along the right abutment, it is 0.25 ft deeper than the mean thalweg depth. Scour protection measures at the site included type-1 stone fill (less than 12 inches diameter) along the upstream right bank and type-2 stone fill (less than 36 inches diameter) along the left and right abutments and along the downstream left bank. Additional details describing conditions at the site are included in the Level II Summary and appendices D and E. </p><p>Scour depths and recommended rock rip-rap sizes were computed using the general guidelines described in Hydraulic Engineering Circular 18 (Richardson and Davis, 1995) for the 100- and 500-year discharges. Total scour at a highway crossing is comprised of three components: 1) long-term streambed degradation; 2) contraction scour (due to accelerated flow caused by a reduction in flow area at a bridge) and; 3) local scour (caused by accelerated flow around piers and abutments). Total scour is the sum of the three components. Equations are available to compute depths for contraction and local scour and a summary of the results of these computations follows. </p><p>Contraction scour for all modelled flows ranged from 0.0 to 1.7 ft. The worst-case contraction scour occurred at the 500-year discharge. Abutment scour ranged from 9.1 to 11.3 ft. The worst-case abutment scour occurred at the 500-year discharge. Additional information on scour depths and depths to armoring are included in the section titled “Scour Results”. Scoured-streambed elevations, based on the calculated scour depths, are presented in tables 1 and 2. A cross-section of the scour computed at the bridge is presented in figure 8. Scour depths were calculated assuming an infinite depth of erosive material and a homogeneous particle-size distribution. </p><p>It is generally accepted that the Froehlich equation (abutment scour) gives “excessively conservative estimates of scour depths” (Richardson and Davis, 1995, p. 46). Usually, computed scour depths are evaluated in combination with other information including (but not limited to) historical performance during flood events, the geomorphic stability assessment, existing scour protection measures, and the results of the hydraulic analyses. Therefore, scour depths adopted by VTAOT may differ from the computed values documented herein.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Pembroke, NH","doi":"10.3133/ofr98157","collaboration":"Prepared in cooperation with Vermont Agency of Transportation and Federal Highway Administration","usgsCitation":"Wild, E.C., 1998, Level II scour analysis for Bridge 13 (LINCTH00010013) on Town Highway 1, crossing Cota Brook, Lincoln, Vermont: U.S. Geological Survey Open-File Report 98-157, iv, 49 p., https://doi.org/10.3133/ofr98157.","productDescription":"iv, 49 p.","costCenters":[],"links":[{"id":178627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr98157.JPG"},{"id":279996,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0157/report.pdf"}],"country":"United States","state":"Vermont","city":"Lincoln","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8483","contributors":{"authors":[{"text":"Wild, Emily C. 0000-0001-6157-7629 ecwild@usgs.gov","orcid":"https://orcid.org/0000-0001-6157-7629","contributorId":1810,"corporation":false,"usgs":true,"family":"Wild","given":"Emily","email":"ecwild@usgs.gov","middleInitial":"C.","affiliations":[{"id":5081,"text":"Libraries","active":false,"usgs":true}],"preferred":false,"id":241055,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50271,"text":"ofr9815 - 1998 - Level II scour analysis for Bridge 17 (NEWHTH00200017) on Town Highway 20, crossing Little Otter Creek, New Haven, Vermont","interactions":[],"lastModifiedDate":"2016-10-13T15:50:54","indexId":"ofr9815","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","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":"98-15","title":"Level II scour analysis for Bridge 17 (NEWHTH00200017) on Town Highway 20, crossing Little Otter Creek, New Haven, Vermont","docAbstract":"<p>This report provides the results of a detailed Level II analysis of scour potential at structure NEWHTH00200017 on Town Highway 20 crossing Little Otter Creek, New Haven, Vermont (figures 1–8). A Level II study is a basic engineering analysis of the site, including a quantitative analysis of stream stability and scour (U.S. Department of Transportation, 1993). Results of a Level I scour investigation also are included in appendix E of this report. A Level I investigation provides a qualitative geomorphic characterization of the study site. Information on the bridge, gleaned from Vermont Agency of Transportation (VTAOT) files, was compiled prior to conducting Level I and Level II analyses and is found in appendix D. </p><p>The site is in the Champlain section of the St. Lawrence Valley physiographic province in west-central Vermont. The 10.8-mi<sup>2</sup> drainage area is in a predominantly rural and wetland basin. In the vicinity of the study site, the surface cover is shrubland on the downstream right overbank. The surface cover of the downstream left overbank, the upstream right overbank and the upstream left overbank is wetland and pasture. </p><p>In the study area, Little Otter Creek has a meandering channel with a slope of approximately 0.0007 ft/ft, an average channel top width of 97 ft and an average bank height of 5 ft. The channel bed material ranges from silt and clay to cobble. Medium sized silt and clay is the channel material upstream of the approach cross-section and downstream of the exit cross-section. The median grain size (D<sub>50</sub>) of the silt and clay channel bed material is 1.52 mm (0.005 ft), which was used for contraction and abutment scour computations. From the approach cross-section, under the bridge, and to the exit cross-section, stone fill is the channel bed material. The median grain size (D<sub>50</sub>) of the stone fill channel bed material is 95.7 mm (0.314 ft). The stone fill median grain size was used solely for armoring computations. The geomorphic assessment at the time of the Level I and Level II site visit on June 11, 1996, indicated that the reach was stable.</p><p>The Town Highway 20 crossing of Little Otter Creek is a 32-ft-long, two-lane bridge consisting of a 28-ft steel-beam span (Vermont Agency of Transportation, written communication, December 15, 1995). The opening length of the structure parallel to the bridge face is 24.9 ft. The bridge is supported by almost vertical, concrete abutments. The channel is skewed approximately 15 degrees to the opening while the opening-skew-toroadway is zero degrees. </p><p>The scour countermeasures at the site consisted of type-1 stone fill (less than 12 inches diameter) along the left and right abutments, as well as along the upstream left and right banks. Type-2 stone fill (less than 36 inches diameter) was present along the downstream right bank. Additional details describing conditions at the site are included in the Level II Summary and appendices D and E. </p><p>Scour depths and recommended rock rip-rap sizes were computed using the general guidelines described in Hydraulic Engineering Circular 18 (Richardson and Davis, 1995) for the 100- and 500-year discharges. In addition, the incipient roadway-overtopping discharge was determined and analyzed as another potential worst-case scour scenario. Total scour at a highway crossing is comprised of three components: 1) long-term streambed degradation; 2) contraction scour (due to accelerated flow caused by a reduction in flow area at a bridge) and; 3) local scour (caused by accelerated flow around piers and abutments). Total scour is the sum of the three components. Equations are available to compute depths for contraction and local scour and a summary of the results of these computations follows. </p><p>Contraction scour for all modelled flows ranged from 9.7 to 13.8 ft. The worst-case contraction scour occurred at the 500-year discharge. Left abutment scour ranged from 6.9 to 7.9 ft. Right abutment scour ranged from 10.5 to 11.8 ft. The worst-case left and right abutment scour occurred at the 500-year discharge. Additional information on scour depths and depths to armoring are included in the section titled “Scour Results”. Scoured-streambed elevations, based on the calculated scour depths, are presented in tables 1 and 2. A cross-section of the scour computed at the bridge is presented in figure 8. Scour depths were calculated assuming an infinite depth of erosive material and a homogeneous particle-size distribution. </p><p>It is generally accepted that the Froehlich equation (abutment scour) gives “excessively conservative estimates of scour depths” (Richardson and Davis, 1995, p. 47). Usually, computed scour depths are evaluated in combination with other information including (but not limited to) historical performance during flood events, the geomorphic stability assessment, existing scour protection measures, and the results of the hydraulic analyses. Therefore, scour depths adopted by VTAOT may differ from the computed values documented herein.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Pembroke, NH","doi":"10.3133/ofr9815","collaboration":"Prepared in cooperation with Vermont Agency of Transportation and Federal Highway Administration","usgsCitation":"Wild, E.C., and Burns, R.L., 1998, Level II scour analysis for Bridge 17 (NEWHTH00200017) on Town Highway 20, crossing Little Otter Creek, New Haven, Vermont: U.S. Geological Survey Open-File Report 98-15, iv, 51 p., https://doi.org/10.3133/ofr9815.","productDescription":"iv, 51 p.","costCenters":[],"links":[{"id":162288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":279989,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0015/report.pdf"}],"country":"United States","state":"Vermont","city":"New Haven","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8222","contributors":{"authors":[{"text":"Wild, Emily C. 0000-0001-6157-7629 ecwild@usgs.gov","orcid":"https://orcid.org/0000-0001-6157-7629","contributorId":1810,"corporation":false,"usgs":true,"family":"Wild","given":"Emily","email":"ecwild@usgs.gov","middleInitial":"C.","affiliations":[{"id":5081,"text":"Libraries","active":false,"usgs":true}],"preferred":false,"id":241064,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burns, Ronda L.","contributorId":71602,"corporation":false,"usgs":true,"family":"Burns","given":"Ronda","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":241063,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56229,"text":"wdrOK971 - 1998 - Water resources data, Oklahoma, water year 1997, Volume 1, Arkansas River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:11:48","indexId":"wdrOK971","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"OK-97-1","title":"Water resources data, Oklahoma, water year 1997, Volume 1, Arkansas River Basin","language":"ENGLISH","doi":"10.3133/wdrOK971","usgsCitation":"Blazs, R., Walters, D., Coffey, T., White, D., Boyle, D., and Kerestes, J., 1998, Water resources data, Oklahoma, water year 1997, Volume 1, Arkansas River Basin: U.S. Geological Survey Water Data Report OK-97-1, 447 p., https://doi.org/10.3133/wdrOK971.","productDescription":"447 p.","costCenters":[],"links":[{"id":174442,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0cbc","contributors":{"authors":[{"text":"Blazs, R.L.","contributorId":27067,"corporation":false,"usgs":true,"family":"Blazs","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":255024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walters, D.M.","contributorId":41507,"corporation":false,"usgs":true,"family":"Walters","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":255026,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coffey, T.E.","contributorId":51368,"corporation":false,"usgs":true,"family":"Coffey","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":255027,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"White, D.K.","contributorId":30279,"corporation":false,"usgs":true,"family":"White","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":255025,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Boyle, D.L.","contributorId":55505,"corporation":false,"usgs":true,"family":"Boyle","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":255028,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kerestes, J.F.","contributorId":19219,"corporation":false,"usgs":true,"family":"Kerestes","given":"J.F.","affiliations":[],"preferred":false,"id":255023,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":44311,"text":"ofr97102 - 1998 - Hydrogeology and water quality of the Clinton Street-Ballpark Aquifer near Johnson City, New York","interactions":[],"lastModifiedDate":"2017-04-06T11:08:21","indexId":"ofr97102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","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":"97-102","title":"Hydrogeology and water quality of the Clinton Street-Ballpark Aquifer near Johnson City, New York","docAbstract":"<p>The Clinton Street-Ballpark aquifer, in the Susquehanna River valley in southern Broome County, N.Y., supplies drinking water to the Village of Johnson City near Binghamton. The hydrogeology and water quality of the aquifer were studied in 1994-95 to identify the source area of 1,1,1-trichloroethane, which was detected at the Johnson City Camden Street wellfield in 1991.</p><p>The aquifer is generally 100 to 150 ft thick and consists primarily of ice-contact deposits of silty sand and gravel that are overlain by outwash deposits of sand and gravel. These two types of deposits are separated by lacustrine silt and clay of variable thickness into an upper and a lower layer of the aquifer. The coarse deposits form a single aquifer in areas where the lacustrine deposits are absent.</p><p>Synoptic water-level surveys indicated that ground water moves from upgradient areas flanking the aquifer boundaries toward two major pumping centers?the Anitec wellfield in Binghamton and the Camden Street wellfield in Johnson City. Areas contributing recharge to municipal and industrial wells in the aquifer were delineated by a previously developed groundwater- flow model. The residence time of ground water within the area contributing recharge to Johnson City well no. 2 in the Camden Street wellfield was estimated to be less than 6 years.</p><p>1,1,1-Trichloroethane, trichloroethene, and their metabolites were detected in ground water at several locations in and near Johnson City. Relatively high concentrations of 1,1,1-trichloroethane were found in ground water about 3,000 ft north of the Camden Street wellfield. The suspected source is an area bordered on the south by Field Street, on the north by Harry L. Drive, on the east by New York State Route 201, and on the west by Marie Street. A trichloroethene metabolite, cis-1,2-dichloroethene, appears to be migrating westward from U.S. Air Force Plant 59 toward the Camden Street well-field, 1,000 ft southwest of the plant, although this compound has not been detected in water pumped by municipal wells, possibly because it has become diluted by ground water from other locations within the contributing area to the wells.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr97102","collaboration":"Prepared in cooperation with the U.S. Air Force","usgsCitation":"Coon, W.F., Yager, R.M., Surface, J.M., Randall, A.D., and Eckhardt, D.A., 1998, Hydrogeology and water quality of the Clinton Street-Ballpark Aquifer near Johnson City, New York: U.S. Geological Survey Open-File Report 97-102, Report: 63 p.; 5 Plates, https://doi.org/10.3133/ofr97102.","productDescription":"Report: 63 p.; 5 Plates","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":326220,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0102/ofr1997102_plate3.pdf","text":"Plate 3 ","size":"7.52 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1996-0102","linkHelpText":"- Areas contributing ground water to municipal and industrial wells, and travel times of selected flow lines near Johnson, City, N.Y., 1994"},{"id":326221,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0102/ofr1997102_plate4.pdf","text":"Plate 4 ","size":"5.67 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1996-0102","linkHelpText":"- Concentration of 1,1,1- Trichloroethane (1,1,1-TCA) and 1,1-Dichlorethane (1,1-DCA) in ground water, Johnson City, N.Y., 1994–95"},{"id":326218,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0102/ofr1997102_plate1.pdf","text":"Plate 1","size":"7.84 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1996-0102","linkHelpText":" - Location of wells and surface-water measurement sites in Binghamton and Johnson City, N.Y."},{"id":169353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0102/coverthb.jpg"},{"id":3724,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0102/ofr19970102.pdf","text":"Report","size":"644 KB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1996-0102"},{"id":326219,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0102/ofr1997102_plate2.pdf","text":"Plate 2 ","size":"637 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1996-0102","linkHelpText":"- Water-table and selected ground-water flow directions in the unconfined layer of the Clinton Street-Ballpark aquifer, Broome County, N.Y., May 1995"},{"id":326222,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0102/ofr1997102_plate5.pdf","text":"Plate 5 ","size":"4.37 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 1996-0102","linkHelpText":"- Concentrations of 1,1,1-Trichlorethene (TCE) and <i>cis</i>-1,2-Dichloroethene (<i>cis</i>-1,2-DCE) in ground water, Johnson City, N.Y., 1994–95"}],"contact":"<p>Director, New York Water Science Center<br>U.S. Geological Survey<br> 425 Jordan Rd<br> Troy, NY 12180<br> (518) 285-5695&nbsp;<br> <a href=\"http://ny.water.usgs.gov/\" data-mce-href=\"http://ny.water.usgs.gov/\">http://ny.water.usgs.gov/</a></p>","tableOfContents":"<ul>\n<li>Abstract</li>\n<li>Introduction</li>\n<li>Methods Of Investigation</li>\n<li>Hydrogeology</li>\n<li>Ground-water Quality</li>\n<li>Summary</li>\n<li>References Cited</li>\n</ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627727","contributors":{"authors":[{"text":"Coon, William F. 0000-0002-7007-7797 wcoon@usgs.gov","orcid":"https://orcid.org/0000-0002-7007-7797","contributorId":1765,"corporation":false,"usgs":true,"family":"Coon","given":"William","email":"wcoon@usgs.gov","middleInitial":"F.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":229540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yager, Richard M. 0000-0001-7725-1148 ryager@usgs.gov","orcid":"https://orcid.org/0000-0001-7725-1148","contributorId":950,"corporation":false,"usgs":true,"family":"Yager","given":"Richard","email":"ryager@usgs.gov","middleInitial":"M.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true},{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":229537,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Surface, Jan M.","contributorId":32204,"corporation":false,"usgs":true,"family":"Surface","given":"Jan","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":229541,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Randall, Allan D. arandall@usgs.gov","contributorId":1168,"corporation":false,"usgs":true,"family":"Randall","given":"Allan","email":"arandall@usgs.gov","middleInitial":"D.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":229539,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Eckhardt, David A. daeckhar@usgs.gov","contributorId":1079,"corporation":false,"usgs":true,"family":"Eckhardt","given":"David","email":"daeckhar@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":229538,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":50265,"text":"ofr98156 - 1998 - Level II scour analysis for Bridge 27 (WSTOTH00070027) on Town Highway 7, crossing Jenny Coolidge Brook, Weston, Vermont","interactions":[],"lastModifiedDate":"2016-08-25T13:46:05","indexId":"ofr98156","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","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":"98-156","title":"Level II scour analysis for Bridge 27 (WSTOTH00070027) on Town Highway 7, crossing Jenny Coolidge Brook, Weston, Vermont","docAbstract":"<p>This report provides the results of a detailed Level II analysis of scour potential at structure WSTOTH00070027 on Town Highway 7 crossing Jenny Coolidge Brook, Weston, Vermont (figures 1–8). A Level II study is a basic engineering analysis of the site, including a quantitative analysis of stream stability and scour (FHWA, 1993). Results of a Level I scour investigation also are included in appendix E of this report. A Level I investigation provides a qualitative geomorphic characterization of the study site. Information on the bridge, gleaned from Vermont Agency of Transportation (VTAOT) files, was compiled prior to conducting Level I and Level II analyses and is found in appendix D. </p><p>The site is in the Green Mountain section of the New England physiographic province in southwestern Vermont. The 2.9-mi<sup>2</sup> drainage area is in a predominantly rural and forested basin. In the vicinity of the study site, the surface cover is pasture downstream of the bridge while upstream of the bridge is forested. </p><p>In the study area, the Jenny Coolidge Brook has an incised, sinuous channel with a slope of approximately 0.04 ft/ft, an average channel top width of 51 ft and an average bank height of 6 ft. The channel bed material ranges from sand to boulders with a median grain size (D<sub>50</sub>) of 122 mm (0.339 ft). The geomorphic assessment at the time of the Level I and Level II site visit on August 20, 1996, indicated that the reach was stable. </p><p>The Town Highway 7 crossing of the Jenny Coolidge Brook is a 52-ft-long, two-lane bridge consisting of a 50-foot steel-beam span (Vermont Agency of Transportation, written communication, April 7, 1995). The opening length of the structure parallel to the bridge face is 49.2 ft. The bridge is supported by vertical, concrete abutments with wingwalls. The channel is skewed approximately 5 degrees to the opening while the computed opening-skew-to-roadway is 15 degrees. </p><p>The legs of the skeleton-type right abutment were exposed approximately 2 feet (vertically) and approximately 2 feet (horizontally) during the Level I assessment. Scour protection measures at the site include type-1 stone fill (less than 12 inches diameter) along the downstream right wingwall, and type-2 stone fill (less than 36 inches diameter) along the upstream banks, upstream left wingwall, left abutment, downstream left wingwall and downstream left bank. A stone wall levee extends along the downstream right bank. Additional details describing conditions at the site are included in the Level II Summary and appendices D and E. </p><p>Scour depths and recommended rock rip-rap sizes were computed using the general guidelines described in Hydraulic Engineering Circular 18 (Richardson and Davis, 1995) for the 100- and 500-year discharges. Total scour at a highway crossing is comprised of three components: 1) long-term streambed degradation; 2) contraction scour (due to accelerated flow caused by a reduction in flow area at a bridge) and; 3) local scour (caused by accelerated flow around piers and abutments). Total scour is the sum of the three components. Equations are available to compute depths for contraction and local scour and a summary of the results of these computations follows. </p><p>Contraction scour for all modelled flows was zero ft. Abutment scour ranged from 3.0 to 4.1 ft. The worst-case left abutment scour occurred at the 100-year discharge. The worst-case right abutment scour occurred at the 500-year discharge. Additional information on scour depths and depths to armoring are included in the section titled “Scour Results”. Scoured-streambed elevations, based on the calculated scour depths, are presented in tables 1 and 2. A cross-section of the scour computed at the bridge is presented in figure 8. Scour depths were calculated assuming an infinite depth of erosive material and a homogeneous particlesize distribution. </p><p>It is generally accepted that the Froehlich equation (abutment scour) gives “excessively conservative estimates of scour depths” (Richardson and Davis, 1995, p. 46). Usually, computed scour depths are evaluated in combination with other information including (but not limited to) historical performance during flood events, the geomorphic stability assessment, existing scour protection measures, and the results of the hydraulic analyses. Therefore, scour depths adopted by VTAOT may differ from the computed values documented herein.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Pembroke, NH","doi":"10.3133/ofr98156","collaboration":"Prepared in cooperation with Vermont Agency of Transportation and Federal Highway Administration","usgsCitation":"Wild, E.C., 1998, Level II scour analysis for Bridge 27 (WSTOTH00070027) on Town Highway 7, crossing Jenny Coolidge Brook, Weston, Vermont: U.S. Geological Survey Open-File Report 98-156, iv, 48 p., https://doi.org/10.3133/ofr98156.","productDescription":"iv, 48 p.","costCenters":[],"links":[{"id":178628,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr98156.JPG"},{"id":279995,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0156/report.pdf"}],"country":"United States","state":"Vermont","city":"Weston","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f95","contributors":{"authors":[{"text":"Wild, Emily C. 0000-0001-6157-7629 ecwild@usgs.gov","orcid":"https://orcid.org/0000-0001-6157-7629","contributorId":1810,"corporation":false,"usgs":true,"family":"Wild","given":"Emily","email":"ecwild@usgs.gov","middleInitial":"C.","affiliations":[{"id":5081,"text":"Libraries","active":false,"usgs":true}],"preferred":false,"id":241056,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":50180,"text":"ofr98273 - 1998 - Level II scour analysis for Bridge 28 (ROCHTH00370028) on Town Highway 37, crossing Brandon Brook, Rochester, Vermont","interactions":[],"lastModifiedDate":"2016-08-25T16:15:35","indexId":"ofr98273","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","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":"98-273","title":"Level II scour analysis for Bridge 28 (ROCHTH00370028) on Town Highway 37, crossing Brandon Brook, Rochester, Vermont","docAbstract":"<p>This report provides the results of a detailed Level II analysis of scour potential at structure ROCHTH00370028 on Town Highway 37 crossing Brandon Brook, Rochester, Vermont (figures 1–8). A Level II study is a basic engineering analysis of the site, including a quantitative analysis of stream stability and scour (FHWA, 1993). Results of a Level I scour investigation also are included in appendix E of this report. A Level I investigation provides a qualitative geomorphic characterization of the study site. Information on the bridge, gleaned from VTAOT files, was compiled prior to conducting Level I and Level II analyses and is found in appendix D. </p><p>The site is in the Green Mountain section of the New England physiographic province in central Vermont. The 8.0-mi<sup>2</sup> drainage area is in a predominantly rural and forested basin. In the vicinity of the study site, the surface cover is pasture on the upstream left overbank although the immediate banks have dense woody vegetation. The upstream right overbank and downstream left and right overbanks are forested. </p><p>In the study area, the Brandon Brook has an incised, sinuous channel with a slope of approximately 0.01 ft/ft, an average channel top width of 44 ft and an average bank height of 7 ft. The channel bed material ranges from gravel to cobbles with a median grain size (D<sub>50</sub>) of 84.2 mm (0.276 ft). The geomorphic assessment at the time of the Level I site visit on April 12, 1995 and Level II site visit on July 8, 1996, indicated that the reach was stable. </p><p>The Town Highway 37 crossing of the Brandon Brook is a 33-ft-long, one-lane bridge consisting of a 31-foot timber-stringer span (Vermont Agency of Transportation, written communication, March 22, 1995). The opening length of the structure parallel to the bridge face is 29.6 ft. The bridge is supported by vertical, timber log cribbing abutments with wingwalls. The channel is skewed approximately 5 degrees to the opening while the computed opening-skew-to-roadway is zero degrees. </p><p>A scour hole 1.0 ft deeper than the mean thalweg depth was observed along the upstream left wingwall and the left abutment during the Level I assessment. The only scour protection measure at the site was type-5 protection, an artificial levee, extending along the upstream right bank to the end of the upstream right wingwall. Additional details describing conditions at the site are included in the Level II Summary and appendices D and E.</p><p>Scour depths and recommended rock rip-rap sizes were computed using the general guidelines described in Hydraulic Engineering Circular 18 (Richardson and others, 1995) for the 100- and 500-year discharges. Total scour at a highway crossing is comprised of three components: 1) long-term streambed degradation; 2) contraction scour (due to accelerated flow caused by a reduction in flow area at a bridge) and; 3) local scour (caused by accelerated flow around piers and abutments). Total scour is the sum of the three components. Equations are available to compute depths for contraction and local scour and a summary of the results of these computations follows. </p><p>Contraction scour for all modelled flows was zero ft. Left abutment scour ranged from 7.1 to 9.9 ft where the worst-case scour occurred at the 500-year discharge. Right abutment scour ranged from 4.4 to 5.1 ft where the worst-case scour occurred at the 500-year discharge. Additional information on scour depths and depths to armoring are included in the section titled “Scour Results.” Scoured-streambed elevations, based on the calculated scour depths, are presented in tables 1 and 2. A cross-section of the scour computed at the bridge is presented in figure 8. Scour depths were calculated assuming an infinite depth of erosive material and a homogeneous particle-size distribution. </p><p>It is generally accepted that the Froehlich equation (abutment scour) gives “excessively conservative estimates of scour depths” (Richardson and Davis, 1995, p. 46). Usually, computed scour depths are evaluated in combination with other information including (but not limited to) historical performance during flood events, the geomorphic stability assessment, existing scour protection measures, and the results of the hydraulic analyses. Therefore, scour depths adopted by VTAOT may differ from the computed values documented herein</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Pembroke, NH","doi":"10.3133/ofr98273","collaboration":"Prepared in cooperation with Vermont Agency of Transportation and Federal Highway Administration","usgsCitation":"Wild, E.C., and Weber, M.A., 1998, Level II scour analysis for Bridge 28 (ROCHTH00370028) on Town Highway 37, crossing Brandon Brook, Rochester, Vermont: U.S. Geological Survey Open-File Report 98-273, iv, 51 p., https://doi.org/10.3133/ofr98273.","productDescription":"iv, 51 p.","costCenters":[],"links":[{"id":179102,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr98273.JPG"},{"id":280071,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0273/report.pdf"}],"country":"United States","state":"Vermont","city":"Rochester","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f60","contributors":{"authors":[{"text":"Wild, Emily C. 0000-0001-6157-7629 ecwild@usgs.gov","orcid":"https://orcid.org/0000-0001-6157-7629","contributorId":1810,"corporation":false,"usgs":true,"family":"Wild","given":"Emily","email":"ecwild@usgs.gov","middleInitial":"C.","affiliations":[{"id":5081,"text":"Libraries","active":false,"usgs":true}],"preferred":false,"id":240908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weber, Matthew A.","contributorId":41483,"corporation":false,"usgs":true,"family":"Weber","given":"Matthew","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":240907,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53917,"text":"bsr19980003_1998 - 1998 - Perspectives on the land use history of North America: A context for understanding our changing environment","interactions":[{"subject":{"id":70180831,"text":"70180831 - 1998 - Landscape changes in the southwestern United States: Techniques, long-term datasets, and trends: Chapter 9","indexId":"70180831","publicationYear":"1998","noYear":false,"chapter":"p","title":"Landscape changes in the southwestern United States: Techniques, long-term datasets, and trends: Chapter 9"},"predicate":"IS_PART_OF","object":{"id":53917,"text":"bsr19980003_1998 - 1998 - Perspectives on the land use history of North America: A context for understanding our changing environment","indexId":"bsr19980003_1998","publicationYear":"1998","noYear":false,"title":"Perspectives on the land use history of North America: A context for understanding our changing environment"},"id":1}],"lastModifiedDate":"2018-01-19T17:42:22","indexId":"bsr19980003_1998","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":9,"text":"Biological Science Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"1998-0003","title":"Perspectives on the land use history of North America: A context for understanding our changing environment","docAbstract":"Ecological change is constant and profound, yet it often occurs at temporal and spatial scales that are difficult to measure and interpret. This publication demonstrates how diverse data bases, archived in different formats and at numerous locations, can be brought together to provide an integrated perspective on the relationship between land use and landcover change. The authors provide the historical context for interpreting recent landcover change in several regions of North America and articulate the value of a comprehensive continental land-use history for guiding environmental policy and management decisions during the coming century and beyond.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"1998, Perspectives on the land use history of North America: A context for understanding our changing environment: Biological Science Report 1998-0003, vi, 104 p.","productDescription":"vi, 104 p.","numberOfPages":"110","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true}],"links":[{"id":176987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6883f0","contributors":{"editors":[{"text":"Sisk, Thomas D.","contributorId":68157,"corporation":false,"usgs":true,"family":"Sisk","given":"Thomas D.","affiliations":[],"preferred":false,"id":504040,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":54809,"text":"wdrNJ972 - 1998 - Water resources data, New Jersey, water year 1997. Volume 2. Ground-water data","interactions":[],"lastModifiedDate":"2020-12-15T17:05:45.668561","indexId":"wdrNJ972","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NJ-97-2","title":"Water resources data, New Jersey, water year 1997. Volume 2. Ground-water data","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNJ972","usgsCitation":"Jones, W., and DeLuca, M., 1998, Water resources data, New Jersey, water year 1997. Volume 2. 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,{"id":53920,"text":"bsr19970002 - 1998 - Copper hazards to fish, wildlife, and invertebrates: a synoptic review","interactions":[],"lastModifiedDate":"2012-02-02T00:11:43","indexId":"bsr19970002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":9,"text":"Biological Science Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"1997-0002","title":"Copper hazards to fish, wildlife, and invertebrates: a synoptic review","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Eisler, R., 1998, Copper hazards to fish, wildlife, and invertebrates: a synoptic review: Biological Science Report 1997-0002, iv, 98 p. ; 28 cm.","productDescription":"iv, 98 p. ; 28 cm.","costCenters":[],"links":[{"id":177073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685e9d","contributors":{"authors":[{"text":"Eisler, Ronald","contributorId":101303,"corporation":false,"usgs":true,"family":"Eisler","given":"Ronald","affiliations":[],"preferred":false,"id":248666,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":54641,"text":"wdrLA971 - 1998 - Water resources data, Louisiana, water year 1997","interactions":[],"lastModifiedDate":"2025-07-21T15:04:52.989495","indexId":"wdrLA971","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"LA-97-1","title":"Water resources data, Louisiana, water year 1997","docAbstract":"<p>Water resources data for the 1997 water year for Louisiana consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report contains records for water discharge at 67 gaging stations; stage only for 45 gaging stations and 6 lakes; water quality for 37 surface-water stations (including 22 gaging stations) and 95 wells; and water levels for 243 observation wells. Also included are data for 113 crest-stage and flood-profile partial-record stations. Additional water data were collected at various sites not included in the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Louisiana. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrLA971","collaboration":"Prepared in cooperation with the Louisiana Department of Transportation and Development and with other State and Federal agencies","usgsCitation":"Garrison, C., Goree, B., Lovelace, W., Montgomery, P., and Resweber, J., 1998, Water resources data, Louisiana, water year 1997: U.S. Geological Survey Water Data Report LA-97-1, xviii, 495 p., https://doi.org/10.3133/wdrLA971.","productDescription":"xviii, 495 p.","costCenters":[],"links":[{"id":492630,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1997/la-97-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177565,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1997/la-97-1/report-thumb.jpg"}],"country":"United 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,{"id":54560,"text":"wdrGA972 - 1998 - Water resources data, Georgia, water year 1997. Volume 2. Gulf of Mexico and Tennessee River Basin Regions","interactions":[],"lastModifiedDate":"2025-05-21T19:37:45.083675","indexId":"wdrGA972","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1998","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"GA-97-2","title":"Water resources data, Georgia, water year 1997. Volume 2. Gulf of Mexico and Tennessee River Basin Regions","docAbstract":"<p>Water-resources data for the 1997 water year for Georgia consists of discharge records for 123 gaging stations; stage for 23 gaging stations; stage and contents for 18 lakes and reservoirs; water quality for 202 continuing-record stations; and peak stage and discharge only for 77 crest-stage partial-record stations; and water levels of 24 observation wells.</p><p>The data for the Gulf of Mexico and Tennessee River Basin Regions in Georgia include discharge records of 50 gaging stations; stage for 14 gaging stations; stage and contents for 10 lakes and reservoirs; water quality for 82 continuing-record stations; and peak stage and discharge only for 38 crest-stage partial-record stations; and water levels for 12 observation wells.</p><p>These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agenceies in Georgia.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrGA972","collaboration":"Prepared in cooperation with the State of Georgia and other Federal agencies.","usgsCitation":"Stokes, W., and McFarlane, R., 1998, Water resources data, Georgia, water year 1997. Volume 2. 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