{"pageNumber":"395","pageRowStart":"9850","pageSize":"25","recordCount":16506,"records":[{"id":21568,"text":"ofr97640 - 1997 - Activities of the United States Geological Survey in Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-06T14:14:22","indexId":"ofr97640","displayToPublicDate":"1998-07-01T00:00:00","publicationYear":"1997","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":"97-640","title":"Activities of the United States Geological Survey in Pennsylvania","docAbstract":"<p>Since the late 1800's, when the U.S. Geological Survey first established a presence in Pennsylvania, the focus of our work has changed from general hydrologic and geologic appraisals to issue-oriented investigations; from predominantly data collection to a balanced program of data collection, interpretation, and research; and from traditional, hand-drawn mapping to digitally produced coverages with specialized themes. Yet our basic mission has not changed. It is as relevant to the resource issues of today as it was when our geologists first arrived in western Pennsylvania in 1884. Continuing in this proud heritage and tradition, the U.S. Geological Survey is moving confidently toward the next century, evolving organizationally and technologically to better meet the needs of our many constituencies. One major organizational change is the recent accession of employees from the former National Biological Service, who now form the Survey's fourth program division, the Biological Resources Division. These employees join forces with colleagues in our other three divisions: Water Resources, Geologic, and National Mapping. More than any other change in decades, the addition of this biological expertise creates new and exciting opportunities for scientific research and public service. This report provides an overview of recent activities in Pennsylvania conducted by the four program divisions and is intended to inform those interested in U.S. Geological Survey products and services. Additional information is available on our home page (at http://wwwpah2o.er.usgs.gov/). Together with numerous Federal, State, and local agencies and organizations who are our customers and partners, we at the U.S. Geological Survey look forward to providing continued scientific contributions and public service to Pennsylvania and the Nation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr97640","usgsCitation":"Wood, C.R., 1997, Activities of the United States Geological Survey in Pennsylvania: U.S. Geological Survey Open-File Report 97-640, 32 p. :col. ill., col. maps ;28 cm., https://doi.org/10.3133/ofr97640.","productDescription":"32 p. :col. ill., col. maps ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science 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,{"id":22188,"text":"ofr97598 - 1997 - Studies of the San Francisco Bay, California, estuarine ecosystem regional monitoring program results, 1996","interactions":[],"lastModifiedDate":"2019-12-05T09:21:24","indexId":"ofr97598","displayToPublicDate":"1998-06-01T00:00:00","publicationYear":"1997","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":"97-598","title":"Studies of the San Francisco Bay, California, estuarine ecosystem regional monitoring program results, 1996","docAbstract":"<p>As part of a regional monitoring program, water samples were collected in the San Francisco Bay estuary during 21 cruises from January through December 1996. Conductivity, temperature, light attenuation, turbidity, oxygen, and in-vivo chlorophyll fluorescence were measured longitudinally and vertically in the main channel of the estuary from south of the Dumbarton Bridge in the southern part of the Bay to Rio Vista on the Sacramento River. Discrete water samples were analyzed for chlorophyll a, phaeopigments, suspended participate matter, and dissolved oxygen. Water density was calculated from salinity, temperature, and pressure (depth), and is included in the data summaries.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr97598","issn":"0094-9140","usgsCitation":"Baylosis, J.I., Edmunds, J.L., Cole, B.E., and Cloern, J.E., 1997, Studies of the San Francisco Bay, California, estuarine ecosystem regional monitoring program results, 1996: U.S. Geological Survey Open-File Report 97-598, iv, 203 p., https://doi.org/10.3133/ofr97598.","productDescription":"iv, 203 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":51624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0598/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155020,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0598/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.52365112304688,\n              37.41925395973696\n            ],\n            [\n              -122.52365112304688,\n              38.15831665744203\n            ],\n            [\n              -121.44012451171874,\n              38.15831665744203\n            ],\n            [\n              -121.44012451171874,\n              37.41925395973696\n            ],\n            [\n              -122.52365112304688,\n              37.41925395973696\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e04","contributors":{"authors":[{"text":"Baylosis, Jelriza I.","contributorId":72820,"corporation":false,"usgs":true,"family":"Baylosis","given":"Jelriza","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":187538,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edmunds, Jody L.","contributorId":10452,"corporation":false,"usgs":true,"family":"Edmunds","given":"Jody","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":597612,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cole, Brian E.","contributorId":18357,"corporation":false,"usgs":true,"family":"Cole","given":"Brian","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":597613,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":597614,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":23210,"text":"ofr97811 - 1997 - Low-flow water-quality and discharge data for lined channels in Northeast Albuquerque, New Mexico, 1990 to 1994","interactions":[],"lastModifiedDate":"2012-02-02T00:07:55","indexId":"ofr97811","displayToPublicDate":"1998-06-01T00:00:00","publicationYear":"1997","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":"97-811","title":"Low-flow water-quality and discharge data for lined channels in Northeast Albuquerque, New Mexico, 1990 to 1994","docAbstract":"The water resources of the Albuquerque metropolitan area are under \r\nincreasing scrutiny by Federal and State regulators. Because of a lack \r\nof available low-flow data for use in addressing potential water-quality \r\nproblems, a project was established to collect low-flow water-quality \r\nand discharge data. The project was initiated under a current cooperative \r\nprogram between the U.S. Geological Survey and the Albuquerque Metropolitan \r\nArroyo Flood Control Authority. This report summarizes hydrologic data for \r\nthat project collected between October 31, 1990, and September 3, 1994, at \r\nthree sites in the lined channel network in northeast Albuquerque. \r\n     The data collection network consisted of three sampling sites on \r\nCampus Wash, Embudo Arroyo, and the North Floodway Channel. The sites on \r\nCampus Wash and the North Floodway Channel were established at existing \r\ncontinuous-record streamflow-gaging stations; the Embudo Arroyo site was \r\nestablished at the site of an abandoned streamflow-gaging station. Data \r\npresented include site descriptions, instantaneous stream discharges \r\nmeasured at the time of sampling, and the results of the chemical analyses \r\nof the water-quality samples.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr97811","issn":"0094-9140","usgsCitation":"Gold, R., and McBreen, R., 1997, Low-flow water-quality and discharge data for lined channels in Northeast Albuquerque, New Mexico, 1990 to 1994: U.S. Geological Survey Open-File Report 97-811, iii, 60 p. :map ;28 cm., https://doi.org/10.3133/ofr97811.","productDescription":"iii, 60 p. :map ;28 cm.","costCenters":[],"links":[{"id":154479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0811/report-thumb.jpg"},{"id":52523,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0811/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6487e2","contributors":{"authors":[{"text":"Gold, R.L.","contributorId":97918,"corporation":false,"usgs":true,"family":"Gold","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":189639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McBreen, Robert","contributorId":43226,"corporation":false,"usgs":true,"family":"McBreen","given":"Robert","email":"","affiliations":[],"preferred":false,"id":189638,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24136,"text":"ofr97641 - 1997 - Results of soil, ground-water, surface-water, and streambed-sediment sampling at Air Force Plane 85, Columbus, Ohio, 1996","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"ofr97641","displayToPublicDate":"1998-06-01T00:00:00","publicationYear":"1997","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":"97-641","title":"Results of soil, ground-water, surface-water, and streambed-sediment sampling at Air Force Plane 85, Columbus, Ohio, 1996","docAbstract":"The U.S. Geological Survey (USGS), in cooperation with Aeronautical Systems Center, Environmental Management Directorate, Restoration Division, prepared the Surface- and Ground- Water Monitoring Work Plan for Air Force Plant 85 (AFP 85 or Plant), Columbus, Ohio, under the Air Force Installation Restoration Program to characterize any ground-water, surface-water, and soil contamination that may exist at AFP 85. The USGS began the study in November 1996.\r\n\r\nThe Plant was divided into nine sampling areas, which included some previously investi gated study sites. The investigation activities included the collection and presentation of data taken during drilling and water-quality sampling. Data collection focused on the saturated and unsatur ated zones and surface water. Twenty-three soil borings were completed. Ten monitoring wells (six existing wells and four newly constructed monitoring wells) were selected for water-quality sam pling. Surface-water and streambed-sediment sampling locations were chosen to monitor flow onto and off of the Plant. Seven sites were sampled for both surface-water and streambed-sediment quality.\r\n\r\nThis report presents data on the selected inorganic and organic constituents in soil, ground water, surface water, and streambed sediments at AFP 85. The methods of data collection and anal ysis also are included. Knowledge of the geologic and hydrologic setting could aid Aeronautical Systems Center, Environmental Management Directorate, Restoration Division, and its governing regulatory agencies in future remediation studies.","language":"ENGLISH","publisher":"U.S. Department of the Interior, U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr97641","issn":"0094-9140","usgsCitation":"Parnell, J.M., 1997, Results of soil, ground-water, surface-water, and streambed-sediment sampling at Air Force Plane 85, Columbus, Ohio, 1996: U.S. Geological Survey Open-File Report 97-641, v, 107 p. : ill., maps ;28 cm., https://doi.org/10.3133/ofr97641.","productDescription":"v, 107 p. : ill., maps ;28 cm.","costCenters":[],"links":[{"id":157167,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0641/report-thumb.jpg"},{"id":53288,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0641/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056c6","contributors":{"authors":[{"text":"Parnell, J. M.","contributorId":13656,"corporation":false,"usgs":true,"family":"Parnell","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":191384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22172,"text":"ofr97669 - 1997 - Spatial and temporal trends of trace metals in surface water, bed sediment, and biota of the upper Clark Fork Basin, Montana, 1985-95","interactions":[],"lastModifiedDate":"2019-12-05T09:50:29","indexId":"ofr97669","displayToPublicDate":"1998-06-01T00:00:00","publicationYear":"1997","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":"97-669","title":"Spatial and temporal trends of trace metals in surface water, bed sediment, and biota of the upper Clark Fork Basin, Montana, 1985-95","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr97669","issn":"0094-9140","usgsCitation":"Hornberger, M.I., Lambing, J., Luoma, S., and Axtmann, E., 1997, Spatial and temporal trends of trace metals in surface water, bed sediment, and biota of the upper Clark Fork Basin, Montana, 1985-95: U.S. Geological Survey Open-File Report 97-669, 127 p. , https://doi.org/10.3133/ofr97669.","productDescription":"127 p. 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H.","contributorId":100860,"corporation":false,"usgs":true,"family":"Lambing","given":"J. H.","affiliations":[],"preferred":false,"id":187469,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Luoma, S. N.","contributorId":86353,"corporation":false,"usgs":true,"family":"Luoma","given":"S. N.","affiliations":[],"preferred":false,"id":187468,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Axtmann, E.V.","contributorId":30652,"corporation":false,"usgs":true,"family":"Axtmann","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":187467,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":29154,"text":"wri974152 - 1997 - Spring contributions to water quantity and nitrate loads in the Suwannee River during base flow in July 1995","interactions":[],"lastModifiedDate":"2021-11-18T20:39:17.241338","indexId":"wri974152","displayToPublicDate":"1998-06-01T00:00:00","publicationYear":"1997","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":"97-4152","title":"Spring contributions to water quantity and nitrate loads in the Suwannee River during base flow in July 1995","docAbstract":"The Suwannee River flows through an area of north-central Florida where ground water has elevated nitrate concentrations. A study was conducted to determine how springs and other ground-water inflow affect the quantity and quality of water in the Suwannee River. The study was done on a 33-mile (mi) reach of the lower Suwannee River from just downstream of Dowling Park, Fla., to Branford, Fla. Water samples for nitrate concentrations (dissolved nitrite plus nitrate as nitrogen) and discharge data were collected at 11 springs and 3 river sites during the 3-day period in July 1995 during base flow in the river. \r\n\r\nIn the study reach, all inflow to the river is derived from ground water. Measured springs and other ground-water inflow, such as unmeasured springs and upward diffuse leakage through the riverbed, increased the river discharge 47 percent over the 33-mi reach. The 11 measured springs contributed 41 percent of the increased discharge and other ground-water inflow contributed the remaining 59 percent. River nitrate loads increased downstream from 2,300 to 6,000 kilograms per day (kg/d), an increase of 160 percent in the 33-mi study reach. Measured springs contributed 46 percent of this increase and other ground-water inflow contributed the remaining 54 percent. \r\n\r\nThe study reach was divided at Luraville, Fla., into an 11-mi upper segment and a 22-mi lower segment to determine whether the ground-water inflows and nitrate concentrations were uniform throughout the entire study reach (fig. 1). The two segments were dissimilar. The amount of water added to the river by measured springs more than tripled from the upper to the lower segment. Even though the median nitrate concentration for the three springs in the upper segment (1.7 milligrams per liter (mg/L)) was similar to the median for the eight springs in the lower segment (1.8 mg/L), nitrate concentrations in the river almost doubled from 0.46 to 0.83 mg/L in the lower segment. Only 11 percent of the increase in nitrate load for the study reach occurred in the upper segment; the remaining 89 percent occurred in the lower segment. Measured springs were the major source of nitrate load in the upper reach and other ground-water inflow was the major source in the lower segment. \r\n\r\nDifferences in nitrate loads between the upper and lower river segments are probably controlled by such factors as differences in the magnitude of the spring discharges, the size and location of spring basins, and the hydrologic characteristics of ground water in the study area.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri974152","usgsCitation":"Pittman, J.R., Hatzell, H.H., and Oaksford, E., 1997, Spring contributions to water quantity and nitrate loads in the Suwannee River during base flow in July 1995: U.S. Geological Survey Water-Resources Investigations Report 97-4152, 12 p., https://doi.org/10.3133/wri974152.","productDescription":"12 p.","costCenters":[],"links":[{"id":58028,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4152/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4152/report-thumb.jpg"},{"id":391883,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_48768.htm"}],"country":"United States","state":"Florida","otherGeospatial":"Suwannee River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.25,\n              29.9444\n            ],\n            [\n              -82.9167,\n              29.9444\n            ],\n            [\n              -82.9167,\n              30.25\n            ],\n            [\n              -83.25,\n              30.25\n            ],\n            [\n              -83.25,\n              29.9444\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4814e4b07f02db4db248","contributors":{"authors":[{"text":"Pittman, J. R.","contributorId":71571,"corporation":false,"usgs":true,"family":"Pittman","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201039,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hatzell, H. H.","contributorId":7732,"corporation":false,"usgs":true,"family":"Hatzell","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":201037,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oaksford, E. T.","contributorId":64284,"corporation":false,"usgs":true,"family":"Oaksford","given":"E. T.","affiliations":[],"preferred":false,"id":201038,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27031,"text":"wri954132 - 1997 - Effect of faulting on ground-water movement in the Death Valley Region, Nevada and California","interactions":[],"lastModifiedDate":"2015-10-06T14:43:18","indexId":"wri954132","displayToPublicDate":"1998-06-01T00:00:00","publicationYear":"1997","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":"95-4132","title":"Effect of faulting on ground-water movement in the Death Valley Region, Nevada and California","docAbstract":"<p>This study characterizes the hydrogeologic system of the Death Valley region, an area covering approximately 100,000 square kilometers. The study also characterizes the effects of faults on ground-water movement in the Death Valley region by synthesizing crustal stress, fracture mechanics, and structural geologic data. The geologic conditions are typical of the Basin and Range Province; a variety of sedimentary and igneous intrusive and extrusive rocks have been subjected to both compressional and extensional deformation. Faulting and associated fracturing is pervasive and greatly affects ground-water flow patterns. Faults may become preferred conduits or barriers to flow depending on whether they are in relative tension, compression, or shear and other factors such as the degree of dislocations of geologic units caused by faulting, the rock types involved, the fault zone materials, and the depth below the surface.</p>\n<p>The current crustal stress field was combined with fault orientations to predict potential effects of faults on the regional groundwater flow regime. Numerous examples of faultcontrolled ground-water flow exist within the study area. Hydrologic data provided an independent method for checking some of the assumptions concerning preferential flow paths.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri954132","collaboration":"Prepared in cooperation with the Nevada Operations Office, U.S. Department of Energy","usgsCitation":"Faunt, C., 1997, Effect of faulting on ground-water movement in the Death Valley Region, Nevada and California: U.S. Geological Survey Water-Resources Investigations Report 95-4132, Report: v, 42 p.; 1 Plate: 27.83 x 31.39 inches, https://doi.org/10.3133/wri954132.","productDescription":"Report: v, 42 p.; 1 Plate: 27.83 x 31.39 inches","numberOfPages":"51","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":309693,"rank":301,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4132/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55909,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4132/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4132/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Death Valley Region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.49853515625,\n              35.28150065789119\n            ],\n            [\n              -118.49853515625,\n              38.77121637244273\n            ],\n            [\n              -114.58740234375,\n              38.77121637244273\n            ],\n            [\n              -114.58740234375,\n              35.28150065789119\n            ],\n            [\n              -118.49853515625,\n              35.28150065789119\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db6256c1","contributors":{"authors":[{"text":"Faunt, Claudia C. 0000-0001-5659-7529 ccfaunt@usgs.gov","orcid":"https://orcid.org/0000-0001-5659-7529","contributorId":1491,"corporation":false,"usgs":true,"family":"Faunt","given":"Claudia C.","email":"ccfaunt@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":197438,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28563,"text":"wri974142 - 1997 - Snow and ice volume on Mount Spurr Volcano, Alaska, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:08:52","indexId":"wri974142","displayToPublicDate":"1998-06-01T00:00:00","publicationYear":"1997","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":"97-4142","title":"Snow and ice volume on Mount Spurr Volcano, Alaska, 1981","docAbstract":"Mount Spurr (3,374 meters altitude) is an active volcano 130 kilometers west of Anchorage, Alaska, with an extensive covering of seasonal and perennial snow, and glaciers. Knowledge of the volume and distribution of snow and ice on a volcano aids in assessing hydrologic hazards such as floods, mudflows, and debris flows. \r\n\r\nIn July 1981, ice thickness was measured at 68 locations on the five main glaciers of Mount Spurr: 64 of these measurements were made using a portable 1.7 megahertz monopulse ice-radar system, and 4 measurements were made using the helicopter altimeter where the glacier bed was exposed by ice avalanching. The distribution of snow and ice derived from these measurements is depicted on contour maps and in tables compiled by altitude and by drainage basins. \r\n\r\nBasal shear stresses at 20 percent of the measured locations ranged from 200 to 350 kilopascals, which is significantly higher than the 50 to 150 kilopascals commonly referred to in the literature as the 'normal' range for glaciers. Basal shear stresses higher than 'normal' have also been found on steep glaciers on volcanoes in the Cascade Range in the western United States. \r\n\r\nThe area of perennial snow and ice coverage on Mount Spurr was 360 square kilometers in 1981, with an average thickness of 190?50 meters. Seasonal snow increases the volume about 1 percent and increases the area about 30 percent with a maximum in May or June. Runoff from Mount Spurr feeds the Chakachatna River and the Chichantna River (a tributary of the Beluga River). The Chakachatna River drainage contains 14 cubic kilometers of snow and ice and the Chichantna River drainage contains 53 cubic kilometers. \r\n\r\nThe snow and ice volume on the mountain was 67?17 cubic kilometers, approximately 350 times more snow and ice than was on Mount St. Helens before its May 18, 1980, eruption, and 15 times more snow and ice than on Mount Rainier, the most glacierized of the measured volcanoes in the Cascade Range. On the basis of these relative quantities, hazard-producing glaciovolcanic phenomena at Mount Spurr could be significantly greater than similar phenomena at Cascade Volcanoes.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/wri974142","usgsCitation":"March, R.S., Mayo, L.R., and Trabant, D.C., 1997, Snow and ice volume on Mount Spurr Volcano, Alaska, 1981: U.S. Geological Survey Water-Resources Investigations Report 97-4142, vi, 36 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri974142.","productDescription":"vi, 36 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4142/report-thumb.jpg"},{"id":57392,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1997/4142/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57393,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1997/4142/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57394,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4142/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5edea0","contributors":{"authors":[{"text":"March, Rod S. rsmarch@usgs.gov","contributorId":416,"corporation":false,"usgs":true,"family":"March","given":"Rod","email":"rsmarch@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":200032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayo, Lawrence R.","contributorId":98344,"corporation":false,"usgs":true,"family":"Mayo","given":"Lawrence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":200034,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trabant, Dennis C.","contributorId":13965,"corporation":false,"usgs":true,"family":"Trabant","given":"Dennis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":200033,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70019456,"text":"70019456 - 1997 - Dynamic deformations and the M6.7, Northridge, California earthquake","interactions":[],"lastModifiedDate":"2025-08-15T16:23:23.977686","indexId":"70019456","displayToPublicDate":"1998-05-17T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3418,"text":"Soil Dynamics and Earthquake Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Dynamic deformations and the M6.7, Northridge, California earthquake","docAbstract":"<p><span>A method of estimating the complete time-varying dynamic formation field from commonly available three-component single station seismic data has been developed and applied to study the relationship between dynamic deformation and ground failures and structural damage using observations from the 1994 Northridge, California earthquake. Estimates from throughout the epicentral region indicate that the horizontal strains exceed the vertical ones by more than a factor of two. The largest strains (exceeding ∼100 pstrain) correlate with regions of greatest ground failure. There is a poor correlation between structural damage and peak strain amplitudes. The smallest strains,∼35 pstrain, are estimated in regions of no damage or ground failure. Estimates in the two regions with most severe and well mapped permanent deformation, Potrero Canyon and the Granada-Mission Hills regions, exhibit the largest strains; peak horizontal strains estimates in these regions equal ∼1351 and ∼229 μstrain respectively. Of note, the dynamic principal strain axes have strikers consistent with the permanent failure features suggesting that, while gravity, sub-surface materials, and hydrologic conditions undoubtedly played fundamental roles in determining where and what types of failures occurred, the dynamic deformation field may have been favorably sized and oriented to initiate failure processes. These results support other studies that conclude that the permanent deformation resulted from ground shaking, rather than from static strains associated with primary or secondary faulting. They also suggest that such an analysis, either using data or theoretical calculations, may enable observations of paleo-ground failure to be used as quantitative constraints on the size and geometry of previous earthquakes.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0267-7261(97)00011-0","issn":"02677261","usgsCitation":"Gomberg, J.S., 1997, Dynamic deformations and the M6.7, Northridge, California earthquake: Soil Dynamics and Earthquake Engineering, v. 16, no. 7-8, p. 471-494, https://doi.org/10.1016/S0267-7261(97)00011-0.","productDescription":"24 p.","startPage":"471","endPage":"494","costCenters":[],"links":[{"id":226836,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Northridge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.63912192273753,\n              34.31335236387632\n            ],\n            [\n              -118.63912192273753,\n              34.158572942513956\n            ],\n            [\n              -118.46109137594402,\n              34.158572942513956\n            ],\n            [\n              -118.46109137594402,\n              34.31335236387632\n            ],\n            [\n              -118.63912192273753,\n              34.31335236387632\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"16","issue":"7-8","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0424e4b0c8380cd507e7","contributors":{"authors":[{"text":"Gomberg, Joan S. 0000-0002-0134-2606 gomberg@usgs.gov","orcid":"https://orcid.org/0000-0002-0134-2606","contributorId":1269,"corporation":false,"usgs":true,"family":"Gomberg","given":"Joan","email":"gomberg@usgs.gov","middleInitial":"S.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":382794,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24705,"text":"ofr97418 - 1997 - Status of ground-water resources at U.S. Navy support facility, Diego Garcia; summary of hydrologic and climatic data, January 1995 through June 1997","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"ofr97418","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","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":"97-418","title":"Status of ground-water resources at U.S. Navy support facility, Diego Garcia; summary of hydrologic and climatic data, January 1995 through June 1997","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr97418","issn":"0094-9140","usgsCitation":"Torikai, J., 1997, Status of ground-water resources at U.S. Navy support facility, Diego Garcia; summary of hydrologic and climatic data, January 1995 through June 1997: U.S. Geological Survey Open-File Report 97-418, v, 43 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr97418.","productDescription":"v, 43 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0418/report-thumb.jpg"},{"id":53738,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0418/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de7c2","contributors":{"authors":[{"text":"Torikai, J.D.","contributorId":93926,"corporation":false,"usgs":true,"family":"Torikai","given":"J.D.","affiliations":[],"preferred":false,"id":192408,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28466,"text":"wri974162 - 1997 - Evaluation of drawdown and sources of water in the Mississippi River alluvium caused by hypothetical pumping, Muscatine, Iowa","interactions":[],"lastModifiedDate":"2016-03-21T15:25:47","indexId":"wri974162","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","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":"97-4162","title":"Evaluation of drawdown and sources of water in the Mississippi River alluvium caused by hypothetical pumping, Muscatine, Iowa","docAbstract":"<p>A study was conducted to evaluate drawdown and volumetric changes in sources of water in the Mississippi River alluvium caused by hypothetical pumping. A steady-state, ground-water flow model was constructed for a previous study to simulate February 1993 hydrologic conditions, which were assumed to be an acceptable estimate of the ground-water system at equilibrium. The flow model was modified for this study to simulate six hypothetical pumping scenarios: five pumping scenarios to simulate hypothetical pumping at five pumping scenario sites, and a total pumping scenario to simulate cumulative hypothetical pumping from the five pumping scenario sites.</p>\n<p>The evaluation of drawdown for the six hypothetical pumping scenarios indicates that hypothetical pumping causes simulated drawdown that varies from about 10 ft to greater than 50 ft relative to February 1993 conditions at the five hypothetical pumping scenario sites. The simulated drawdown is less than half of the estimated saturated thickness of the alluvium during February 1993 at these sites.</p>\n<p>The primary sources of water (inflows) to the alluvium needed to balance the increased ground-water withdrawals (outflows) caused by hypothetical pumping are a combination of increased river leakage and decreased leakage to Muscatine Slough. Compared to February 1993 conditions, larger inflow rates occur as river leakage from the Mississippi River for the six hypothetical pumping scenarios. However, smaller outflow rates to Muscatine Slough compared to February 1993 conditions indicate that an important source of water for hypothetical pumping is ground-water discharge that would have become streamflow in the slough.</p>\n<p>Increased pumping at the hypothetical pumping scenario sites could affect long-term water quality and hydrology in the study area. The greater amounts of river leakage might affect overall ground-water quality in the alluvium. The lesser amounts of ground water being discharged to streamflow could have a long-term impact on the hydrology of the slough and adjacent wetland areas.</p>\n<p>The simplified steady-state flow model does not account for dynamic (transient) conditions (natural or development-related). The steady-state model does not indicate time needed to reach new equilibrium conditions. Attaining equilibrium might take many years and is complicated by varying climatic and hydrologic conditions; noncontinuous pumping and pumping that is cycled among well fields; and changing and seasonally varying irrigation pumpage.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City, IA","doi":"10.3133/wri974162","collaboration":"Prepared in cooperation with Muscatine Power and Water, Muscatine, Iowa","usgsCitation":"Lucey, K., 1997, Evaluation of drawdown and sources of water in the Mississippi River alluvium caused by hypothetical pumping, Muscatine, Iowa: U.S. Geological Survey Water-Resources Investigations Report 97-4162, iv, 18 p., https://doi.org/10.3133/wri974162.","productDescription":"iv, 18 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":119673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4162/report-thumb.jpg"},{"id":57268,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4162/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Illinois, Iowa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.2083333333333333,\n              41.43333333333333\n            ],\n            [\n              -91.2083333333333333,\n              41.25\n            ],\n            [\n              -91,\n              41.25\n            ],\n            [\n              -91,\n              41.43333333333333\n            ],\n            [\n              -91.2083333333333333,\n              41.43333333333333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fae3c","contributors":{"authors":[{"text":"Lucey, K.J.","contributorId":70002,"corporation":false,"usgs":true,"family":"Lucey","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":199850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26648,"text":"wri964269 - 1997 - Hydrology, sedimentology, and biology of Ellison Park wetland at the mouth of Irondequoit Creek near Rochester, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri964269","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"96-4269","title":"Hydrology, sedimentology, and biology of Ellison Park wetland at the mouth of Irondequoit Creek near Rochester, New York","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nU.S. Geological Survey, Branch of Information Services [distributor],","doi":"10.3133/wri964269","usgsCitation":"Coon, W., 1997, Hydrology, sedimentology, and biology of Ellison Park wetland at the mouth of Irondequoit Creek near Rochester, New York: U.S. Geological Survey Water-Resources Investigations Report 96-4269, v, 41 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri964269.","productDescription":"v, 41 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119069,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1996/4269/report-thumb.jpg"},{"id":55525,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1996/4269/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc763","contributors":{"authors":[{"text":"Coon, W.F.","contributorId":102524,"corporation":false,"usgs":true,"family":"Coon","given":"W.F.","email":"","affiliations":[],"preferred":false,"id":196768,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27032,"text":"wri954016 - 1997 - A Hydrogeologic Map of the Death Valley Region, Nevada and California, Developed Using GIS Techniques","interactions":[],"lastModifiedDate":"2012-02-10T00:10:08","indexId":"wri954016","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","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":"95-4016","title":"A Hydrogeologic Map of the Death Valley Region, Nevada and California, Developed Using GIS Techniques","docAbstract":"In support of Yucca Mountain site characterization studies, a hydrogeologic framework was developed, and a hydrogeologic map was constructed for the Death Valley region. The region, covering approximately 100,000 km 2 along the Nevada-California border near Las Vegas, is characterized by isolated mountain ranges juxtaposed against broad, alluvium-filled valleys. Geologic conditions are typical of the Basin and Range Province; a variety of sedimentary and igneous intrusive and extrusive rocks have been subjected to both compressional and extensional deformation. The regional ground-water flow system can best be described as a series of connected intermontane basins in which ground-water flow occurs in basin-fill deposits, carbonate rocks, clastic rocks, and volcanic rocks. Previous investigations have developed more site-specific hydrogeologic relationships; however, few have described all the lithologies within the Death Valley regional ground-water flow system.\r\n\r\nInformation required to characterize the hydrogeologic units in the region was obtained from regional geologic maps and reports. Map data were digitized from regional geologic maps and combined into a composite map using a geographic information system. This map was simplified to show 10 laterally extensive hydrogeologic units with distinct hydrologic properties. The hydraulic conductivity values for the hydrogeologic units range over 15 orders of magnitude due to the variability in burial depth and degree of fracturing. ","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/wri954016","collaboration":"Prepared in cooperation with the Nevada Operations Office, U.S. Department of Energy","usgsCitation":"Faunt, C., D’Agnese, F.A., and Turner, A.K., 1997, A Hydrogeologic Map of the Death Valley Region, Nevada and California, Developed Using GIS Techniques: U.S. Geological Survey Water-Resources Investigations Report 95-4016, Report: iv, 18 p.; Plate: 32 x 30 inches, https://doi.org/10.3133/wri954016.","productDescription":"Report: iv, 18 p.; Plate: 32 x 30 inches","additionalOnlineFiles":"Y","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":124528,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1995/4016/report-thumb.jpg"},{"id":55910,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1995/4016/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55911,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1995/4016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118,35 ], [ -118,38 ], [ -115,38 ], [ -115,35 ], [ -118,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4959e4b0b290850ef155","contributors":{"authors":[{"text":"Faunt, Claudia C. 0000-0001-5659-7529 ccfaunt@usgs.gov","orcid":"https://orcid.org/0000-0001-5659-7529","contributorId":1491,"corporation":false,"usgs":true,"family":"Faunt","given":"Claudia C.","email":"ccfaunt@usgs.gov","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":197439,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"D’Agnese, Frank A.","contributorId":47810,"corporation":false,"usgs":true,"family":"D’Agnese","given":"Frank","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":197441,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Turner, A. Keith","contributorId":39400,"corporation":false,"usgs":true,"family":"Turner","given":"A.","email":"","middleInitial":"Keith","affiliations":[],"preferred":false,"id":197440,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":30580,"text":"wri974145 - 1997 - Eutrophication potential of Payette Lake, Idaho","interactions":[],"lastModifiedDate":"2013-11-22T14:51:31","indexId":"wri974145","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","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":"97-4145","title":"Eutrophication potential of Payette Lake, Idaho","docAbstract":"<p>Payette Lake was studied during water years \n1995-96 to determine the 20.5-square-kilometer \nlake's assimilative capacity for nutrients and, thus, \nits eutrophication potential. The study included \nquantification of hydrologic and nutrient budgets, \ncharacterization of water quality in the limnetic \nand littoral zones, development of an empirical nutrient load/lake response model, and estimation of \nthe limnological effects of a large-scale forest fire \nin the lake's 373-square-kilometer watershed during the autumn of 1994.</p>\n<br/>\n<p>Streamflow from the North Fork Payette \nRiver, the lake's primary tributary, delivered about \n73 percent of the lake's inflow over the 2 years. \nOutflow from the lake, measured since 1908, was \n128 and 148 percent of the long-term average in \n1995 and 1996, respectively. The larger volumes \nof outflow reduced the long-term average water-\nresidence time of 2.35 years to 1.84 and 1.42 years \nfor 1995 and 1996, respectively. The lake retained \n54 percent of its 1995-96 influent load of nitrogen \nand 79 percent of its influent load of phosphorus. \nThe North Fork Payette River contributed an average of 69.4 percent of the lake's nitrogen load and \n28.2 percent of its phosphorus load. The 1994 forest fires substantially increased the loads of nitrogen and phosphorus delivered to the lake; however, only nitrogen concentrations were noticeably increased in the lake.</p>\n<br/>\n<p>Payette Lake was classified as oligotrophic \non the basis of annual geometric mean concentrations, in micrograms per liter, of total phosphorus \n(4.7), total nitrogen (225), and chlorophyll-<i>a</i> (1.3)\nduring 1995-96. Secchi-disc transparencies ranged \nfrom 2.3 to 8.0 meters, indicative of mesotrophic \nconditions. Median ratios of dissolved inorganic \nnitrogen to dissolved orthophosphorus ranged from \n38 to 254, thereby indicating phosphorus limitation \nof phytoplankton growth. Phytoplankton populations were taxonomically dominated by diatoms; \nblue-green algae were rare. One diatom, <i>Tabellaria \nfenestrata</i>, contributed 52 percent of the biovolume. Within the littoral zone, median periphyton \nproduction, normalized to photosynthetically active \nradiation input, ranged from 0.0007 to 0.02 milligrams of chlorophyll-<i>a</i> per square meter per Einstein, a difference of 28.6 times. Multiple linear regression analysis failed to detect any significant relation between periphyton production and various \nindices of nearshore development. Nine genera of \naquatic macrophytes were identified, including \nEurasian milfoil (<i>Myriophyllum spicatum</i> var. <i>spicatum</i>), which is considered a nuisance aquatic \nplant.</p>\n<br/>\n<p>Despite its oligotrophy, Payette Lake had \nsubstantial dissolved-oxygen deficits in 1995-96, \nwhich led to 4-month periods of anoxia in the near-bottom waters of its southwest basin. The hypolimnetic dissolved-oxygen deficit was much larger than \nthat predicted by the nutrient load/lake response \nmodel. The southwest basin's propensity for developing anoxia was related to the lengthy water-residence time and incomplete water-column circulation and reaeration during the spring and autumn, \ncoupled with a long-term accumulation of oxygen-\ndemanding organic matter produced within the \nlake or delivered by its watershed.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boise, ID","doi":"10.3133/wri974145","collaboration":"Prepared in cooperation with the Idaho Division of Environmental Quality","usgsCitation":"Woods, P.F., 1997, Eutrophication potential of Payette Lake, Idaho: U.S. Geological Survey Water-Resources Investigations Report 97-4145, v, 39 p., https://doi.org/10.3133/wri974145.","productDescription":"v, 39 p.","numberOfPages":"44","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":119292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1997/4145/report-thumb.jpg"},{"id":59339,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1997/4145/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Albers Equal-Area projection","country":"United States","state":"Idaho","otherGeospatial":"North Fork Payette River;Payette Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.141529,44.903939 ], [ -116.141529,45.199354 ], [ -115.911589,45.199354 ], [ -115.911589,44.903939 ], [ -116.141529,44.903939 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fb104","contributors":{"authors":[{"text":"Woods, Paul F.","contributorId":82273,"corporation":false,"usgs":true,"family":"Woods","given":"Paul","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":203488,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24229,"text":"ofr97399 - 1997 - Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1996 water year","interactions":[],"lastModifiedDate":"2013-12-19T12:49:37","indexId":"ofr97399","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","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":"97-399","title":"Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1996 water year","docAbstract":"The computed annual yield and deficiency of the subbasins as defined in the Arkansas River Basin Compact, Arkansas-Oklahoma, are given in tables for the 1996 water year. Actual runoff from the subbasins and depletion caused by major reservoirs in the compact area also are given in tabular form. Computed monthly mean discharges are shown for the 21 streamflow stations in the Arkansas River Basin. Water-quality data are shown for 16 water-quality stations sampled in the Arkansas River Basin.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Little Rock, AR","doi":"10.3133/ofr97399","issn":"0094-9140","collaboration":"Prepared in cooperation with Arkansas River Compact Commission Arkansas-Oklahoma","usgsCitation":"Porter, J.E., 1997, Annual yield and selected hydrologic data for the Arkansas River Basin Compact, Arkansas-Oklahoma, 1996 water year: U.S. Geological Survey Open-File Report 97-399, iv, 62 p., https://doi.org/10.3133/ofr97399.","productDescription":"iv, 62 p.","numberOfPages":"66","costCenters":[],"links":[{"id":155448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0399/report-thumb.jpg"},{"id":53363,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0399/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas;Oklahoma","otherGeospatial":"Arknasas River Basin Compact","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.75,34.75 ], [ -95.75,36.25 ], [ -94.0,36.25 ], [ -94.0,34.75 ], [ -95.75,34.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a7fc3","contributors":{"authors":[{"text":"Porter, J. Elton","contributorId":91138,"corporation":false,"usgs":true,"family":"Porter","given":"J.","email":"","middleInitial":"Elton","affiliations":[],"preferred":false,"id":191531,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22874,"text":"ofr97478 - 1997 - Preliminary characterization of acid-generating potential and toxic metal solubility of some abandoned metal-mining related wastes in the Boulder River headwaters, northern Jefferson County, Montana","interactions":[],"lastModifiedDate":"2019-12-05T08:27:19","indexId":"ofr97478","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","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":"97-478","title":"Preliminary characterization of acid-generating potential and toxic metal solubility of some abandoned metal-mining related wastes in the Boulder River headwaters, northern Jefferson County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr97478","issn":"0094-9140","usgsCitation":"Desborough, G.A., and Fey, D.L., 1997, Preliminary characterization of acid-generating potential and toxic metal solubility of some abandoned metal-mining related wastes in the Boulder River headwaters, northern Jefferson County, Montana: U.S. Geological Survey Open-File Report 97-478, ii, 21 p. , https://doi.org/10.3133/ofr97478.","productDescription":"ii, 21 p. ","costCenters":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":153775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8101,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1997/ofr-97-0478/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Montana","county":"Jefferson 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George A.","contributorId":101661,"corporation":false,"usgs":true,"family":"Desborough","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":189046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fey, David L. dfey@usgs.gov","contributorId":713,"corporation":false,"usgs":true,"family":"Fey","given":"David","email":"dfey@usgs.gov","middleInitial":"L.","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":189045,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":21889,"text":"ofr97414 - 1997 - Information on hydrologic and physical properties of water to assess transient hydrology of the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:07:44","indexId":"ofr97414","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","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":"97-414","title":"Information on hydrologic and physical properties of water to assess transient hydrology of the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr97414","issn":"0566-8174","usgsCitation":"Harte, P., Flynn, R., Kiah, R., and Severance, T., 1997, Information on hydrologic and physical properties of water to assess transient hydrology of the Milford-Souhegan glacial-drift aquifer, Milford, New Hampshire: U.S. Geological Survey Open-File Report 97-414, vi, 96 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr97414.","productDescription":"vi, 96 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0414/report-thumb.jpg"},{"id":51378,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0414/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0414/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee537","contributors":{"authors":[{"text":"Harte, P. T. 0000-0002-7718-1204","orcid":"https://orcid.org/0000-0002-7718-1204","contributorId":36143,"corporation":false,"usgs":true,"family":"Harte","given":"P. T.","affiliations":[],"preferred":false,"id":186125,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flynn, R.J.","contributorId":59060,"corporation":false,"usgs":true,"family":"Flynn","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":186126,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kiah, R.G.","contributorId":76770,"corporation":false,"usgs":true,"family":"Kiah","given":"R.G.","affiliations":[],"preferred":false,"id":186127,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Severance, Timothy","contributorId":104927,"corporation":false,"usgs":true,"family":"Severance","given":"Timothy","email":"","affiliations":[],"preferred":false,"id":186128,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":23376,"text":"ofr97425 - 1997 - Floods of July 18-20, 1996, in northern Illinois","interactions":[],"lastModifiedDate":"2013-03-27T07:06:32","indexId":"ofr97425","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","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":"97-425","title":"Floods of July 18-20, 1996, in northern Illinois","docAbstract":"Record flooding occurred on many streams in northern Ilinois during July 18-20, 1996. Over 16 inches of rain fell at some locations during and just prior to this period. Peak of record discharges were recorded at 19 U.S. Geological Survey (USGS) streamflow-gaging stations. The USGS, in cooperation with the Illinois Department of Natural Resources, Office of Water Resources (IDNROWR), has compiled the available hydrologic data from the July 1996 flood in northern Illinois, and the data are presented in this report.","language":"ENGLISH","publisher":"U.S. Geological Survey ;Branch of Information Services [distributor],","doi":"10.3133/ofr97425","issn":"0094-9140","collaboration":"The USGS does not support this software or technical questions for the software associated with the publication.","usgsCitation":"Holmes, R., and Kupka, A., 1997, Floods of July 18-20, 1996, in northern Illinois: U.S. Geological Survey Open-File Report 97-425, iv, 29 p. (some folded) :ill., maps (some col.) ;28 cm. +1 computer disc (3 1/2 in.), https://doi.org/10.3133/ofr97425.","productDescription":"iv, 29 p. (some folded) :ill., maps (some col.) ;28 cm. +1 computer disc (3 1/2 in.)","costCenters":[],"links":[{"id":156962,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0425/report-thumb.jpg"},{"id":19459,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1997/0425/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52666,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0425/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":270240,"type":{"id":4,"text":"Application Site"},"url":"https://pubs.usgs.gov/of/1997/0425/application.zip"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfcb8","contributors":{"authors":[{"text":"Holmes, Robert R. Jr. 0000-0002-5060-3999","orcid":"https://orcid.org/0000-0002-5060-3999","contributorId":70429,"corporation":false,"usgs":true,"family":"Holmes","given":"Robert R.","suffix":"Jr.","affiliations":[],"preferred":false,"id":190002,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kupka, Amanda","contributorId":105336,"corporation":false,"usgs":true,"family":"Kupka","given":"Amanda","email":"","affiliations":[],"preferred":false,"id":190003,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22449,"text":"ofr97398 - 1997 - Trace-element concentrations and transport in the Coeur d'Alene river, Idaho, water years 1993-94","interactions":[],"lastModifiedDate":"2013-12-19T12:53:17","indexId":"ofr97398","displayToPublicDate":"1998-05-01T00:00:00","publicationYear":"1997","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":"97-398","title":"Trace-element concentrations and transport in the Coeur d'Alene river, Idaho, water years 1993-94","docAbstract":"for almost a century, the U.S. Geological Survey has collected hydrologic data at a network of stream-gaging stations throughout the Coeur d'Alene Lake and River drainage basin. Since 1990, extensive water-quality data have been collected for a comprehensive study of potential eutrophication of Coeur d'Alene Lake and for assessment of the environmental effects of past mining and ore-processing activities in the South Fork Coeur d'Alene River valley. Although the South Fork Coeur d'Alene River provided only about 20 percent of the Coeur d'Alene River's annual discharge to Coeur d'Alene Lake, it contributed as much as 84 percent of the annual cadmium and 83 percent of the annual zinc loads entering the Lake. The South Fork contributed at most 14 percent of the annual lead and 21 percent of the copper loads carried by the Coeur d'Alene River to Coeur d'Alene Lake. Cadmium, copper, and zinc loads more than doubled between the upstream and downstream boundaries of the Bunker Hill (Kellogg, Idaho) Superfund site in water years 1993 and 1994; lead load increased 24 percent and 33 percent, respectively, in water years 1993 and 1994. Zinc was transported primarily in a dissolved or colloidal phase, the major source being the South Fork Coeur d'Alene River valley, downstream from the Elizabeth Park gaging station. Lead was transported primarily as particulate material, the major source being sediments eroded from the main-stem Coeur d'Alene River channel and flood plain. Annual lead and zinc loads at Rose Lake were significantly larger than at Harrison or Cataldo, indicating entrainment of trace elements in the reach between Cataldo and Rose Lake, and subsequent deposition or loss in the reach between Rose Lake and Harrison.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boise, Idaho","doi":"10.3133/ofr97398","usgsCitation":"Beckwith, M.A., Woods, P.F., and Berenbrock, C., 1997, Trace-element concentrations and transport in the Coeur d'Alene river, Idaho, water years 1993-94: U.S. Geological Survey Open-File Report 97-398, iii, 7 p., https://doi.org/10.3133/ofr97398.","productDescription":"iii, 7 p.","numberOfPages":"10","temporalStart":"1993-01-01","temporalEnd":"1994-12-31","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":155051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0398/report-thumb.jpg"},{"id":51978,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0398/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","otherGeospatial":"Coeur D'alene River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,47.0 ], [ -117.0,48.0 ], [ -115.0,48.0 ], [ -115.0,47.0 ], [ -117.0,47.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db627321","contributors":{"authors":[{"text":"Beckwith, Michael A.","contributorId":66670,"corporation":false,"usgs":true,"family":"Beckwith","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":188277,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Woods, Paul F.","contributorId":82273,"corporation":false,"usgs":true,"family":"Woods","given":"Paul","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":188278,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Berenbrock, Charles","contributorId":30598,"corporation":false,"usgs":true,"family":"Berenbrock","given":"Charles","email":"","affiliations":[],"preferred":false,"id":188276,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23905,"text":"ofr97319 - 1997 - Modified level II streambed-scour analysis for structure I-64-108-5658 crossing Indian Creek in Harrison County, Indiana","interactions":[],"lastModifiedDate":"2016-06-21T10:40:38","indexId":"ofr97319","displayToPublicDate":"1998-04-01T00:00:00","publicationYear":"1997","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":"97-319","title":"Modified level II streambed-scour analysis for structure I-64-108-5658 crossing Indian Creek in Harrison County, Indiana","docAbstract":"<p>Level II scour evaluations follow a process in which hydrologic, hydraulic, and sedient-transport data are evaluated to calculate the depth of scour that may result when given discharge is routed through a bridge opening. the results of the modified Levell II analysis for structure I-64-108-5658 on Interstate 64 crossing Indian Creek in Harrison County, Indiana, are presented. The site is near the town of Corydon in the central part of Harrison County. Scour depths were computed with the Water Surface PROfile model, version V050196, which incorporates the scour-calculation procedures outlined in Hydraulic Engineering Circular No. 18. Total scour depths at the piers were approximately 6.6 feet for the modeled discharge of 26,000 cubic feet per second and approximately 8.0 feet for the modeled discharge of 34,000 cubic feet per second.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr97319","issn":"0094-9140","collaboration":"Indiana Department of Transporation","usgsCitation":"Miller, R.L., Robinson, B., and Voelker, D.C., 1997, Modified level II streambed-scour analysis for structure I-64-108-5658 crossing Indian Creek in Harrison County, Indiana: U.S. Geological Survey Open-File Report 97-319, iv, 20 p. ;28 cm., https://doi.org/10.3133/ofr97319.","productDescription":"iv, 20 p. ;28 cm.","startPage":"1","endPage":"20","numberOfPages":"24","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":155508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0319/report-thumb.jpg"},{"id":53109,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0319/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Harrison","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-86.2544,38.4224],[-86.0324,38.4177],[-86.033,38.3307],[-86.0295,38.3307],[-86.0248,38.3306],[-86.0148,38.3306],[-86.0144,38.3025],[-85.9956,38.3024],[-85.9947,38.2752],[-85.9735,38.2756],[-85.9737,38.2606],[-85.9549,38.2606],[-85.9508,38.1857],[-85.8987,38.1855],[-85.8987,38.1786],[-85.8996,38.177],[-85.9044,38.1676],[-85.906,38.1428],[-85.9032,38.1148],[-85.9024,38.1064],[-85.9028,38.0926],[-85.9063,38.0825],[-85.91,38.0718],[-85.9125,38.0641],[-85.9136,38.0599],[-85.9144,38.0557],[-85.9195,38.032],[-85.9224,38.0257],[-85.9382,38.0103],[-85.9398,38.0089],[-85.9443,38.0076],[-85.9485,38.0065],[-85.9567,38.0042],[-85.9659,38.0029],[-85.9673,38.0027],[-85.9967,37.9984],[-85.9981,37.9982],[-86.0145,37.9958],[-86.0296,37.9913],[-86.0343,37.9864],[-86.0352,37.9853],[-86.0354,37.9846],[-86.0353,37.9733],[-86.0353,37.9665],[-86.037,37.9631],[-86.04,37.9604],[-86.0464,37.9586],[-86.057,37.9649],[-86.0639,37.9725],[-86.0811,37.9987],[-86.0928,38.0077],[-86.0933,38.0079],[-86.111,38.014],[-86.1236,38.0154],[-86.1267,38.0155],[-86.1319,38.0151],[-86.148,38.0134],[-86.1571,38.0115],[-86.1629,38.0103],[-86.1682,38.0093],[-86.1702,38.0095],[-86.1781,38.0109],[-86.2055,38.0207],[-86.2067,38.0214],[-86.2351,38.0387],[-86.2548,38.0481],[-86.2586,38.0503],[-86.2603,38.0514],[-86.2728,38.0625],[-86.2732,38.063],[-86.2767,38.0694],[-86.2776,38.0724],[-86.2813,38.0887],[-86.2812,38.0984],[-86.2788,38.109],[-86.2729,38.1341],[-86.2758,38.1432],[-86.2805,38.1496],[-86.2824,38.1514],[-86.2923,38.1601],[-86.2963,38.1632],[-86.3005,38.1653],[-86.3077,38.1683],[-86.3219,38.1741],[-86.3314,38.18],[-86.3261,38.1828],[-86.3173,38.1782],[-86.3126,38.1782],[-86.3097,38.1818],[-86.3185,38.1882],[-86.3167,38.1895],[-86.3114,38.1891],[-86.3085,38.2009],[-86.3061,38.2031],[-86.2997,38.2027],[-86.2938,38.2013],[-86.2903,38.2018],[-86.2956,38.2095],[-86.2903,38.2108],[-86.2891,38.214],[-86.2985,38.2194],[-86.2979,38.2217],[-86.2932,38.2249],[-86.2844,38.2208],[-86.2797,38.2235],[-86.2774,38.2271],[-86.2761,38.2529],[-86.2755,38.257],[-86.2749,38.2783],[-86.2696,38.2783],[-86.266,38.2865],[-86.2596,38.2833],[-86.2578,38.2837],[-86.2555,38.2905],[-86.2531,38.2914],[-86.2525,38.295],[-86.2543,38.2964],[-86.2601,38.2973],[-86.2648,38.2946],[-86.2642,38.3041],[-86.2619,38.3041],[-86.2589,38.305],[-86.2589,38.3064],[-86.2677,38.3087],[-86.2707,38.3078],[-86.2765,38.3091],[-86.2894,38.3164],[-86.2829,38.3246],[-86.2818,38.3232],[-86.2794,38.3214],[-86.2747,38.32],[-86.2741,38.325],[-86.2735,38.3295],[-86.2764,38.3386],[-86.2764,38.3404],[-86.2741,38.3409],[-86.2711,38.3413],[-86.2741,38.3472],[-86.2758,38.3499],[-86.2735,38.3563],[-86.2705,38.3617],[-86.2641,38.3612],[-86.2629,38.3572],[-86.257,38.3544],[-86.2529,38.3558],[-86.2482,38.3603],[-86.2482,38.363],[-86.2488,38.3644],[-86.2582,38.3667],[-86.2593,38.3775],[-86.2616,38.3812],[-86.2552,38.3843],[-86.2522,38.383],[-86.2464,38.3861],[-86.2458,38.3879],[-86.2493,38.3907],[-86.2516,38.3947],[-86.251,38.3979],[-86.2533,38.402],[-86.2522,38.407],[-86.258,38.4102],[-86.2627,38.4097],[-86.2645,38.412],[-86.2592,38.4152],[-86.2544,38.4224]]]},\"properties\":{\"name\":\"Harrison\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69946c","contributors":{"authors":[{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":190949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, B.A.","contributorId":63035,"corporation":false,"usgs":true,"family":"Robinson","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":190950,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Voelker, D. C.","contributorId":36572,"corporation":false,"usgs":true,"family":"Voelker","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":190948,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23910,"text":"ofr97321 - 1997 - Modified level II streambed-scour analysis for structure I-74-32-4946 crossing Sugar Creek in Montgomery County, Indiana","interactions":[],"lastModifiedDate":"2016-06-21T10:53:49","indexId":"ofr97321","displayToPublicDate":"1998-04-01T00:00:00","publicationYear":"1997","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":"97-321","title":"Modified level II streambed-scour analysis for structure I-74-32-4946 crossing Sugar Creek in Montgomery County, Indiana","docAbstract":"<p>Level II scour evaluations follow a process in which hydrologic, hydraulic, and sedient-transport data are evaluated to calculate the depth of scour that may result when given discharge is routed through a bridge opening. The results of the modified Levell II analysis for structure I-74-32-4946 on Interstate 74 crossing Sugar Creek in Montgomery County, Indiana are presented. The site is near the town of Crawfordsville in the central part of Montgomery County. Scour depths were computed with the Water Surface PROfile model, version V050196, which incorporates the scour-calculation procedures outlined in Hydraulic Engineering Circular No. 18. Total scour depths at the piers were approximately 13.0 feet for the modeled discharge of 3,000&nbsp; cubic feet per second and approximately 15.1 feet for the modeled discharge of 41,900 cubic feet per second.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr97321","issn":"0094-9140","collaboration":"Indiana Department of Transportation","usgsCitation":"Miller, R.L., Robinson, B., and Voelker, D.C., 1997, Modified level II streambed-scour analysis for structure I-74-32-4946 crossing Sugar Creek in Montgomery County, Indiana: U.S. Geological Survey Open-File Report 97-321, iv, 23 p. ;28 cm., https://doi.org/10.3133/ofr97321.","productDescription":"iv, 23 p. ;28 cm.","startPage":"1","endPage":"23","numberOfPages":"27","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":155527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0321/report-thumb.jpg"},{"id":53114,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0321/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Montgomery","city":"Crawfordsville","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-86.6957,40.2144],[-86.6962,40.1785],[-86.6961,40.1282],[-86.6946,40.0402],[-86.6938,39.9528],[-86.6937,39.9228],[-86.6929,39.8643],[-86.7918,39.8651],[-86.8056,39.865],[-86.8967,39.8666],[-86.9182,39.8674],[-87.0087,39.8685],[-87.0333,39.8683],[-87.0914,39.8685],[-87.0909,39.9538],[-87.0919,40.2172],[-87.0353,40.2165],[-86.9221,40.2161],[-86.8095,40.2146],[-86.6957,40.2144]]]},\"properties\":{\"name\":\"Montgomery\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fad","contributors":{"authors":[{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":190964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, B.A.","contributorId":63035,"corporation":false,"usgs":true,"family":"Robinson","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":190965,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Voelker, D. C.","contributorId":36572,"corporation":false,"usgs":true,"family":"Voelker","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":190963,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":23909,"text":"ofr97313 - 1997 - Modified level II streambed-scour analysis for structure I-70-148-4528 crossing West Fork of East Fork Whitewater River in Wayne County, Indiana","interactions":[],"lastModifiedDate":"2016-06-21T10:59:25","indexId":"ofr97313","displayToPublicDate":"1998-04-01T00:00:00","publicationYear":"1997","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":"97-313","title":"Modified level II streambed-scour analysis for structure I-70-148-4528 crossing West Fork of East Fork Whitewater River in Wayne County, Indiana","docAbstract":"<p>Level II scour evaluations follow a process in which hydrologic, hydraulic, and sedient-transport data are evaluated to calculate the depth of scour that may result when given discharge is routed through a bridge opening. the results of the modified Levell II analysis for structure I-70-148-4528 on Interstate 70 crossing West Fork of East Fork Whitewater River in Wayne County, Indiana, are presented. The site is near the city of Richmond in the eastern part of Wayne County. Scour depths were computed with the Water Surface PROfile model, version V050196, which incorporates the scour-calculation procedures outlined in Hydraulic Engineering Circular No. 18. Total scour depths at the piers were approximately 19.8 feet for the modeled discharge of 6,000 cubic feet per second and approximately 26.5 feet for the modeled discharge of 7,900 cubic feet per second.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr97313","issn":"0094-9140","collaboration":"Indiana Department of Transportation","usgsCitation":"Miller, R.L., Robinson, B., and Voelker, D.C., 1997, Modified level II streambed-scour analysis for structure I-70-148-4528 crossing West Fork of East Fork Whitewater River in Wayne County, Indiana: U.S. Geological Survey Open-File Report 97-313, iv, 18 p. ;28 cm., https://doi.org/10.3133/ofr97313.","productDescription":"iv, 18 p. ;28 cm.","startPage":"1","endPage":"18","numberOfPages":"22","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":155526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0313/report-thumb.jpg"},{"id":53113,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0313/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Wayne","city":"Richmond","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.8131,40.006],[-84.8136,39.9502],[-84.8138,39.9169],[-84.8146,39.7267],[-84.9708,39.7269],[-84.9701,39.7291],[-85.0347,39.729],[-85.0344,39.7145],[-85.1851,39.7152],[-85.1837,39.7891],[-85.2214,39.7895],[-85.2205,39.8748],[-85.2133,39.8751],[-85.2013,39.875],[-85.2014,40.0042],[-84.8952,40.0061],[-84.8603,40.0066],[-84.8131,40.006]]]},\"properties\":{\"name\":\"Wayne\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6993b4","contributors":{"authors":[{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":190961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, B.A.","contributorId":63035,"corporation":false,"usgs":true,"family":"Robinson","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":190962,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Voelker, D. C.","contributorId":36572,"corporation":false,"usgs":true,"family":"Voelker","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":190960,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":21575,"text":"ofr97358 - 1997 - Air temperature and precipitation data, Gulkana Glacier, Alaska, 1968-96","interactions":[],"lastModifiedDate":"2012-02-02T00:07:41","indexId":"ofr97358","displayToPublicDate":"1998-04-01T00:00:00","publicationYear":"1997","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":"97-358","title":"Air temperature and precipitation data, Gulkana Glacier, Alaska, 1968-96","docAbstract":"Daily, monthly, and annual average air temperature and precipitation-catch data were recorded at Gulkana Glacier basin, Alaska, between October 1967 and September 1996. The data set is important because it provides long-term climate information from the highest year-round climatological recording site in Alaska.\r\nThe daily air temperature data set is 96 percent complete. The daily precipitation data set is 83 percent complete; precipitation data for 1993-96 are missing. Annual data summaries are calculated for each hydrologic year, October 1 through September 30, for years that have 12 months of data. Monthly precipitation-catch and average air temperature summaries are calculated for months with nine or fewer daily records missing.\r\nThe average annual air temperature recorded at the site from hydrologic year 1968 through 1996 was -4.1 degrees Celsius. The coldest recorded year was 1972 with an average annual temperature of -6.7 degrees Celsius. The warmest year was 1981 with an average annual temperature of -2.6 degrees Celsius. January 1971 was the coldest month with an average temperature of -20.8 degrees Celsius. July 1989 was the warmest month with an average temperature of 8.7 degrees Celsius. January 17, 1971, was the coldest day with an average temperature of -35.0 degrees Celsius. June 15, 1969, was the warmest day with an average temperature of 16.4 degrees Celsius.\r\nThe average annual precipitation catch recorded at the site from hydrologic year 1968 through 1992 was 1,020 millimeters. The highest annual precipitation catch recorded was 1,572 millimeters in 1981; the lowest was 555 millimeters in 1969. The highest recorded monthly precipitation catch was 448 millimeters in July 1981 and in several different months no precipitation was recorded. The highest daily precipitation catch was 99 millimeters on September 12, 1972, and on many different dates no precipitation was recorded. Because of low gage-catch efficiency the reported annual precipitation-catch data are estimated to represent about 62 percent of the actual annual basin precipitation. Snowfall is the dominant form of precipitation on the glacier from September through mid-June.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBranch of Information Services [distributor],","doi":"10.3133/ofr97358","usgsCitation":"Kennedy, B., Mayo, L.R., Trabant, D.C., and March, R.S., 1997, Air temperature and precipitation data, Gulkana Glacier, Alaska, 1968-96: U.S. Geological Survey Open-File Report 97-358, iv, 144 p. :ill., maps ;28 cm.; 4 illus.; 6 plates; 132 tables, https://doi.org/10.3133/ofr97358.","productDescription":"iv, 144 p. :ill., maps ;28 cm.; 4 illus.; 6 plates; 132 tables","costCenters":[],"links":[{"id":153413,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0358/report-thumb.jpg"},{"id":51160,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48a7e4b07f02db52a9b1","contributors":{"authors":[{"text":"Kennedy, Ben W.","contributorId":104519,"corporation":false,"usgs":true,"family":"Kennedy","given":"Ben W.","affiliations":[],"preferred":false,"id":184720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayo, Lawrence R.","contributorId":98344,"corporation":false,"usgs":true,"family":"Mayo","given":"Lawrence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":184719,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Trabant, Dennis C.","contributorId":13965,"corporation":false,"usgs":true,"family":"Trabant","given":"Dennis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":184718,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"March, Rod S. rsmarch@usgs.gov","contributorId":416,"corporation":false,"usgs":true,"family":"March","given":"Rod","email":"rsmarch@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":184717,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":6763,"text":"fs11897 - 1997 - Source characterization of disinfection byproduct precursors in two Arkansas water-supply reservoirs","interactions":[],"lastModifiedDate":"2019-12-05T10:08:06","indexId":"fs11897","displayToPublicDate":"1998-04-01T00:00:00","publicationYear":"1997","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":"118-97","title":"Source characterization of disinfection byproduct precursors in two Arkansas water-supply reservoirs","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/fs11897","usgsCitation":"Pomes, M.L., Green, W.R., Thurman, E., Orem, W., and Lerch, H., 1997, Source characterization of disinfection byproduct precursors 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,{"id":24350,"text":"ofr97324 - 1997 - Modified level II streambed-scour analysis for structure I-465-131-5256 crossing Williams Creek in Hamilton County, Indiana","interactions":[],"lastModifiedDate":"2016-07-12T13:50:55","indexId":"ofr97324","displayToPublicDate":"1998-04-01T00:00:00","publicationYear":"1997","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":"97-324","title":"Modified level II streambed-scour analysis for structure I-465-131-5256 crossing Williams Creek in Hamilton County, Indiana","docAbstract":"<p>Level II scour evaluations follow a process in which hydrologic, hydraulic, and sediment transport data are evaluated to calculate the depth of scour that may result when a given discharge is routed through a bridge opening. The results of the modified Level II analysis for structure 1-465-131-5256 on Interstate 465 crossing Williams Creek in Hamilton County, Indiana, are presented. The site is near the city of Indianapolis and is in the southwestern part of Hamilton County. Scour depths were computed with the Water Surface PROfile model, version V050196, which incorporates the scour-calculation procedures outlined in Hydraulic Engineering Circular No. 18. Total scour depths at the piers were approximately 6.5 feet for the modeled discharge of 4,300 cubic feet per second and approximately 9.8 feet for the modeled discharge of 7,310 cubic feet per second.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr97324","issn":"0094-9140","usgsCitation":"Robinson, B., Voelker, D.C., and Miller, R.L., 1997, Modified level II streambed-scour analysis for structure I-465-131-5256 crossing Williams Creek in Hamilton County, Indiana: U.S. Geological Survey Open-File Report 97-324, iv, 22 p. ;28 cm., https://doi.org/10.3133/ofr97324.","productDescription":"iv, 22 p. ;28 cm.","startPage":"1","endPage":"18","numberOfPages":"22","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":156768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1997/0324/report-thumb.jpg"},{"id":53448,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1997/0324/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Hamilton County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699449","contributors":{"authors":[{"text":"Robinson, B.A.","contributorId":63035,"corporation":false,"usgs":true,"family":"Robinson","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":191739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Voelker, D. C.","contributorId":36572,"corporation":false,"usgs":true,"family":"Voelker","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":191737,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":191738,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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