{"pageNumber":"4443","pageRowStart":"111050","pageSize":"25","recordCount":184828,"records":[{"id":26247,"text":"wri894087 - 1990 - Determination of flood hydrographs for streams in South Carolina: Volume 1. Simulation of flood hydrographs for rural watersheds in South Carolina","interactions":[],"lastModifiedDate":"2021-12-30T21:24:06.808398","indexId":"wri894087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-4087","title":"Determination of flood hydrographs for streams in South Carolina: Volume 1. Simulation of flood hydrographs for rural watersheds in South Carolina","docAbstract":"A method is given for simulating a typical (average) flood hydrograph corresponding to a peak discharge of specific recurrence interval for ungaged rural basins having drainage areas less than 500 sq mi in South Carolina. Dimensionless hydrographs were developed for three regions on the basis of 188 storm events at 49 stations that represent a wide range of drainage area sizes and basin conditions. The design peak discharge and a basin lagtime (which has been adjusted to produce correct hydrograph volume) are required to apply the technique. The standard errors of estimate for simulated hydrograph widths at 50 and 75%, respectively, of observed stormflow were +/-14.1 and +/-18.3% for basins in the Blue Ridge physiographic province, +/-29.2 and +/-36.2% for basins in the Piedmont province, and +/-17.8 and +/-22.8% for basins in the Coastal Plain provinces. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894087","usgsCitation":"Bohman, L.R., 1990, Determination of flood hydrographs for streams in South Carolina: Volume 1. Simulation of flood hydrographs for rural watersheds in South Carolina: U.S. Geological Survey Water-Resources Investigations Report 89-4087, Report: vi, 53 p.; 1 Plate: 20.82 × 19.44 inches, https://doi.org/10.3133/wri894087.","productDescription":"Report: vi, 53 p.; 1 Plate: 20.82 × 19.44 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":393706,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47195.htm"},{"id":55045,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4087/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4087/report-thumb.jpg"},{"id":55046,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South 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,{"id":26087,"text":"wri904147 - 1990 - Mineralogical correlation of surficial sediment from area drainages with selected sedimentary interbeds at the Idaho National Engineering Laboratory, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:08:34","indexId":"wri904147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4147","title":"Mineralogical correlation of surficial sediment from area drainages with selected sedimentary interbeds at the Idaho National Engineering Laboratory, Idaho","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904147","usgsCitation":"Bartholomay, R.C., 1990, Mineralogical correlation of surficial sediment from area drainages with selected sedimentary interbeds at the Idaho National Engineering Laboratory, Idaho: U.S. Geological Survey Water-Resources Investigations Report 90-4147, iv, 18 p. :ill. ;28 cm. [PGS - 17p.], https://doi.org/10.3133/wri904147.","productDescription":"iv, 18 p. :ill. ;28 cm. [PGS - 17p.]","costCenters":[],"links":[{"id":123058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4147/report-thumb.jpg"},{"id":54856,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4147/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699f0c","contributors":{"authors":[{"text":"Bartholomay, R. C.","contributorId":66271,"corporation":false,"usgs":true,"family":"Bartholomay","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":195776,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26059,"text":"wri894113 - 1990 - Effects of acidic precipitation on the water quality of streams in the Laurel Hill area, Somerset County, Pennsylvania, 1983-86","interactions":[],"lastModifiedDate":"2017-07-17T10:47:40","indexId":"wri894113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-4113","title":"Effects of acidic precipitation on the water quality of streams in the Laurel Hill area, Somerset County, Pennsylvania, 1983-86","docAbstract":"Five headwater streams in the Laurel Hill area in southwestern Pennsylvania were investigated from September 1983 through February 1986 to determine possible effects of acidic precipitation on water quality. Precipitation in the Laurel Hill area is among the most acidic in the Nation, with a mean volume-weighted pH of 4.06. Sulfate is the dominant acid-forming anion, averaging 3.6 milligrams per liter or about 50 kilograms per hectare in wet deposition alone. Nitrate averages about 2 milligrams per liter or 7 kilograms per hectare in the study area.\r\n\r\n      Stream chemistry in the five streams is quite variable and apparently is influenced to a large degree by the bedrock geology and by small amounts of alkaline material in watershed soils. Three of the five streams with no or little acid-neutralizing capacity presently are devoid of fish because of low pH and elevated aluminum concentrations. Aluminum concentrations increase in the other two streams during rainfall and snowmelt despite comparatively higher base flow and acid-neutralizing capacities.\r\n\r\n      Comparison of the chemistry of streamflow during 14 storm events at South Fork Bens Creek and North Fork Bens Creek reveals similar chemical responses when discharge suddenly increases. Concentrations of dissolved metals and sulfate increased during stormflow and snowmelt runoff, whereas concentrations of base cations, silica, and chloride decreased. Nitrate concentrations were not affected by rainfall runoff by tended to increase with snowmelt runoff.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894113","usgsCitation":"Barker, J.L., and Witt, E., 1990, Effects of acidic precipitation on the water quality of streams in the Laurel Hill area, Somerset County, Pennsylvania, 1983-86: U.S. Geological Survey Water-Resources Investigations Report 89-4113, viii, 72 p. :ill. ;28 cm., https://doi.org/10.3133/wri894113.","productDescription":"viii, 72 p. :ill. ;28 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":124545,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4113/report-thumb.jpg"},{"id":54839,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4113/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","county":"Sommerset County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-78.6569,40.2429],[-78.6603,40.2351],[-78.6627,40.2315],[-78.6639,40.2297],[-78.6674,40.2219],[-78.6744,40.2114],[-78.6791,40.2019],[-78.6808,40.1987],[-78.682,40.1968],[-78.6849,40.1891],[-78.6907,40.1795],[-78.6948,40.1691],[-78.6971,40.1641],[-78.6989,40.1613],[-78.7047,40.1517],[-78.7053,40.1504],[-78.7065,40.1481],[-78.7076,40.1463],[-78.7111,40.1381],[-78.7197,40.114],[-78.7243,40.1017],[-78.7272,40.093],[-78.7394,40.0725],[-78.7467,40.0747],[-78.7485,40.076],[-78.7614,40.0596],[-78.7629,40.0401],[-78.7634,40.0342],[-78.7649,40.0192],[-78.7631,40.0174],[-78.7628,40.0011],[-78.7627,39.9925],[-78.762,39.9544],[-78.7617,39.9353],[-78.7605,39.9004],[-78.7598,39.8646],[-78.758,39.8633],[-78.758,39.8619],[-78.7579,39.8601],[-78.7597,39.8578],[-78.7592,39.8275],[-78.7608,39.8166],[-78.7631,39.8116],[-78.7665,39.8029],[-78.7682,39.7979],[-78.7688,39.7965],[-78.7693,39.7915],[-78.7705,39.7888],[-78.771,39.7865],[-78.7733,39.7829],[-78.7787,39.7783],[-78.7816,39.7737],[-78.7827,39.7701],[-78.7844,39.766],[-78.7873,39.761],[-78.7891,39.7578],[-78.7983,39.7414],[-78.8048,39.7318],[-78.81,39.7236],[-78.8524,39.7234],[-78.9146,39.7232],[-79.0408,39.7225],[-79.3213,39.7222],[-79.3889,39.7221],[-79.3901,39.722],[-79.3902,39.7252],[-79.3903,39.7279],[-79.3915,39.7302],[-79.3946,39.7333],[-79.397,39.7337],[-79.4018,39.7341],[-79.4066,39.7345],[-79.4078,39.7367],[-79.4073,39.7404],[-79.4056,39.7418],[-79.4032,39.7436],[-79.3985,39.7437],[-79.3949,39.7442],[-79.3937,39.7456],[-79.3944,39.7487],[-79.3969,39.7523],[-79.3975,39.755],[-79.397,39.7573],[-79.3965,39.76],[-79.3929,39.7606],[-79.3905,39.7615],[-79.3858,39.7625],[-79.3822,39.7639],[-79.3805,39.7666],[-79.3788,39.7689],[-79.38,39.7721],[-79.3813,39.7739],[-79.3855,39.7765],[-79.3892,39.7774],[-79.3922,39.7787],[-79.3928,39.7805],[-79.3935,39.7818],[-79.3917,39.7828],[-79.3881,39.7833],[-79.3846,39.7843],[-79.3828,39.7847],[-79.3816,39.7861],[-79.3817,39.7888],[-79.3787,39.7893],[-79.3769,39.7893],[-79.3708,39.7867],[-79.3581,39.7815],[-79.3558,39.7824],[-79.3541,39.7856],[-79.3529,39.7879],[-79.3553,39.7879],[-79.3601,39.7878],[-79.3643,39.7895],[-79.3656,39.7922],[-79.3675,39.7949],[-79.3681,39.7976],[-79.3676,39.8004],[-79.3671,39.8027],[-79.3654,39.8068],[-79.3643,39.81],[-79.3656,39.814],[-79.3651,39.8186],[-79.3682,39.8235],[-79.37,39.8253],[-79.3725,39.8266],[-79.3749,39.827],[-79.3785,39.8274],[-79.3809,39.8283],[-79.3809,39.8297],[-79.3811,39.8342],[-79.3805,39.8365],[-79.3823,39.8373],[-79.3921,39.8426],[-79.4169,39.8536],[-79.4023,39.8914],[-79.3984,39.9006],[-79.3984,39.9015],[-79.3816,39.9244],[-79.3735,39.9345],[-79.3271,39.9973],[-79.3253,39.9992],[-79.3248,40.0001],[-79.3242,40.001],[-79.294,40.04],[-79.2753,40.0625],[-79.2665,40.0735],[-79.2619,40.0803],[-79.2584,40.0863],[-79.2561,40.0886],[-79.2531,40.0904],[-79.2496,40.0918],[-79.2436,40.0919],[-79.2424,40.0924],[-79.24,40.0942],[-79.2382,40.0956],[-79.2352,40.0966],[-79.2281,40.0976],[-79.2233,40.1008],[-79.2222,40.104],[-79.2217,40.1072],[-79.2211,40.109],[-79.2176,40.1122],[-79.2147,40.1154],[-79.2105,40.1169],[-79.2081,40.1169],[-79.205,40.116],[-79.2032,40.1161],[-79.2021,40.117],[-79.2009,40.1179],[-79.1991,40.1175],[-79.1984,40.1166],[-79.1965,40.1116],[-79.1953,40.1089],[-79.1928,40.1085],[-79.188,40.1095],[-79.1821,40.1136],[-79.1745,40.1214],[-79.1716,40.1255],[-79.1676,40.1333],[-79.1653,40.1383],[-79.1636,40.1451],[-79.162,40.1533],[-79.1615,40.1583],[-79.161,40.1597],[-79.1598,40.1602],[-79.1549,40.1598],[-79.1471,40.1599],[-79.1447,40.1613],[-79.1436,40.1636],[-79.1443,40.1703],[-79.1475,40.178],[-79.1314,40.1828],[-79.1285,40.1891],[-79.128,40.1919],[-79.1246,40.2001],[-79.1228,40.2015],[-79.1138,40.2052],[-79.108,40.2134],[-79.1039,40.2171],[-79.0986,40.224],[-79.0963,40.229],[-79.094,40.2327],[-79.0887,40.2404],[-79.0846,40.2446],[-79.0793,40.2514],[-79.0765,40.2587],[-79.0759,40.2606],[-79.0724,40.2651],[-79.0665,40.2711],[-79.0612,40.2771],[-79.0572,40.2857],[-79.0174,40.2853],[-78.9999,40.2851],[-78.9643,40.285],[-78.9445,40.2853],[-78.927,40.285],[-78.9275,40.2832],[-78.9275,40.2823],[-78.9275,40.2814],[-78.925,40.2787],[-78.9244,40.2782],[-78.9232,40.2778],[-78.9208,40.2774],[-78.9172,40.277],[-78.9099,40.2761],[-78.9045,40.2753],[-78.896,40.2713],[-78.8947,40.27],[-78.8947,40.2686],[-78.8947,40.2677],[-78.897,40.2654],[-78.897,40.2636],[-78.897,40.2627],[-78.8958,40.2622],[-78.8946,40.2613],[-78.8933,40.2595],[-78.8927,40.2573],[-78.892,40.2537],[-78.8913,40.2505],[-78.8907,40.2496],[-78.8889,40.2482],[-78.8877,40.2473],[-78.887,40.2469],[-78.8846,40.2456],[-78.8822,40.2456],[-78.8804,40.2479],[-78.8786,40.2488],[-78.8745,40.2493],[-78.8726,40.2489],[-78.8672,40.2471],[-78.8611,40.2458],[-78.8563,40.2454],[-78.8533,40.2455],[-78.8473,40.246],[-78.8189,40.2445],[-78.8002,40.2442],[-78.7894,40.2443],[-78.7575,40.2433],[-78.753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J. L.","contributorId":83518,"corporation":false,"usgs":true,"family":"Barker","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witt, E. C. III","contributorId":105746,"corporation":false,"usgs":true,"family":"Witt","given":"E. C.","suffix":"III","affiliations":[],"preferred":false,"id":195730,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26033,"text":"wri904053 - 1990 - Flow characteristics of streams that drain the Fort Apache and San Carlos Indian reservations, east-central Arizona, 1930-86","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri904053","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4053","title":"Flow characteristics of streams that drain the Fort Apache and San Carlos Indian reservations, east-central Arizona, 1930-86","docAbstract":"Streamflow characteristics of the Salt River and Gila River basins in the Fort Apache and San Carlos Indian Reservations, were studied in response to pending adjudication of water resources in those basins. Statistical summaries were compiled for 28 streamflow-gaging stations in and near the reservation. Mean annual streamflow for 1930-86 was computed for stations with complete records for the period; for those stations with records that did not completely cover the 1930-86 period, record extension techniques were used. Mean annual streamflow for ungaged sites on streams with gaging stations was estimated by interpolation between data points using drainage-area ratios. Two regional-regression equations were derived to estimate mean annual streamflow at sites on ungaged natural streams. The standard error of the regression for estimation of mean annual flow for sites in the Salt River basin is -37 to +59%. The standard error of the regression for estimation of mean annual flow for sites in the Gila River basins is -18 to +21%. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904053","usgsCitation":"Baldys, S., and Bayles, J., 1990, Flow characteristics of streams that drain the Fort Apache and San Carlos Indian reservations, east-central Arizona, 1930-86: U.S. Geological Survey Water-Resources Investigations Report 90-4053, iv, 59 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904053.","productDescription":"iv, 59 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119075,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4053/report-thumb.jpg"},{"id":54813,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4053/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54814,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4053/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df1f1","contributors":{"authors":[{"text":"Baldys, Stanley sbaldys@usgs.gov","contributorId":3366,"corporation":false,"usgs":true,"family":"Baldys","given":"Stanley","email":"sbaldys@usgs.gov","affiliations":[],"preferred":true,"id":195677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bayles, J.A.","contributorId":23179,"corporation":false,"usgs":true,"family":"Bayles","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":195678,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26026,"text":"wri904177 - 1990 - Summary and analysis of water-use data collection in eastern Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:27","indexId":"wri904177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4177","title":"Summary and analysis of water-use data collection in eastern Arkansas","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri904177","usgsCitation":"Baker, N., 1990, Summary and analysis of water-use data collection in eastern Arkansas: U.S. Geological Survey Water-Resources Investigations Report 90-4177, v, 25 p. :ill. ;28 cm., https://doi.org/10.3133/wri904177.","productDescription":"v, 25 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":158000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4177/report-thumb.jpg"},{"id":54803,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4177/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6996f8","contributors":{"authors":[{"text":"Baker, N.T.","contributorId":32519,"corporation":false,"usgs":true,"family":"Baker","given":"N.T.","email":"","affiliations":[],"preferred":false,"id":195664,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25979,"text":"wri874213 - 1990 - Cost effectiveness of the stream-gaging program in Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri874213","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"87-4213","title":"Cost effectiveness of the stream-gaging program in Nevada","docAbstract":"The stream-gaging network in Nevada was evaluated as part of a nationwide effort by the U.S. Geological Survey to define and document the most cost-effective means of furnishing streamflow information. Specifically, the study dealt with 79 streamflow gages and 2 canal-flow gages that were under the direct operation of Nevada personnel as of 1983. Cost-effective allocations of resources, including budget and operational criteria, were studied using statistical procedures known as Kalman-filtering techniques. The possibility of developing streamflow data at ungaged sites was evaluated using flow-routing and statistical regression analyses. Neither of these methods provided sufficiently accurate results to warrant their use in place of stream gaging. The 81 gaging stations were being operated in 1983 with a budget of $465,500. As a result of this study, all existing stations were determined to be necessary components of the program for the foreseeable future. At the 1983 funding level, the average standard error of streamflow records was nearly 28%. This same overall level of accuracy could have been maintained with a budget of approximately $445,000 if the funds were redistributed more equitably among the gages. The maximum budget analyzed, $1,164 ,000 would have resulted in an average standard error of 11%. The study indicates that a major source of error is lost data. If perfectly operating equipment were available, the standard error for the 1983 program and budget could have been reduced to 21%. (Thacker-USGS, WRD)","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey ;\r\nU.S. Geological Survey, Books and Open-File Reports Section [distributor],","doi":"10.3133/wri874213","usgsCitation":"Arteaga, F., 1990, Cost effectiveness of the stream-gaging program in Nevada: U.S. Geological Survey Water-Resources Investigations Report 87-4213, v, 68 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874213.","productDescription":"v, 68 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4213/report-thumb.jpg"},{"id":54733,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4213/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683ebd","contributors":{"authors":[{"text":"Arteaga, F.E.","contributorId":50918,"corporation":false,"usgs":true,"family":"Arteaga","given":"F.E.","affiliations":[],"preferred":false,"id":195579,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25733,"text":"wri894105 - 1990 - Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in and near Stillwater Wildlife Management Area, Churchill County, Nevada, 1986-87","interactions":[],"lastModifiedDate":"2012-02-02T00:08:13","indexId":"wri894105","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"89-4105","title":"Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in and near Stillwater Wildlife Management Area, Churchill County, Nevada, 1986-87","docAbstract":"A reconnaissance was initiated in 1986 to determine whether the quality of irrigation-drainage water in and near the Stillwater Wildlife Management Area, Nevada, has caused or has potential to cause harmful effects on human health, fish, wildlife, or other beneficial uses of water. Samples of surface and groundwater, bottom sediment, and biota were collected from sites upstream and downstream from the Fallon agricultural area in the Carson Desert, and analyzed for potentially toxic trace elements. Other analysis included radioactive substances, major dissolved constituents, and nutrients in water, and pesticide residues in bottom sediment and biota. In areas affected by irrigation drainage, the following constituents were found to commonly exceed baseline concentrations or recommended criteria for protection of aquatic life or propagation of wildlife: In water, arsenic, boron, dissolved solids, molybdenum, sodium, and un-ionized ammonia; in bottom sediments, arsenic, lithium, mercury, molybdenum, and selenium; and in biota, arsenic, boron, chromium, copper, mercury, selenium, and zinc. In some wetlands, selenium and mercury appeared to be biomagnified, and arsenic bioaccumulated. Pesticides contamination in bottom sediments and biota was insignificant. Adverse biological effects observed during this reconnaissance included gradual vegetative changes and species loss, fish die-offs, waterfowl disease epidemics, and persistent and unexplained deaths of migratory birds. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894105","usgsCitation":"Hoffman, R., Hallock, R., Rowe, T., Lico, M., Burge, H., and Thompson, S., 1990, Reconnaissance investigation of water quality, bottom sediment, and biota associated with irrigation drainage in and near Stillwater Wildlife Management Area, Churchill County, Nevada, 1986-87: U.S. Geological Survey Water-Resources Investigations Report 89-4105, viii, 150 p. :ill., map ;28 cm., https://doi.org/10.3133/wri894105.","productDescription":"viii, 150 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":157001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4105/report-thumb.jpg"},{"id":54494,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4105/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54495,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4105/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63eb5c","contributors":{"authors":[{"text":"Hoffman, R.J.","contributorId":38582,"corporation":false,"usgs":true,"family":"Hoffman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":194842,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hallock, R.J.","contributorId":100413,"corporation":false,"usgs":true,"family":"Hallock","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":194845,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowe, T.G.","contributorId":105732,"corporation":false,"usgs":true,"family":"Rowe","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":194846,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lico, M.S.","contributorId":36573,"corporation":false,"usgs":true,"family":"Lico","given":"M.S.","affiliations":[],"preferred":false,"id":194841,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Burge, H.L.","contributorId":57104,"corporation":false,"usgs":true,"family":"Burge","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":194843,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Thompson, S.P.","contributorId":66731,"corporation":false,"usgs":true,"family":"Thompson","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":194844,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":25727,"text":"wri904029 - 1990 - Programs and analytical methods for the US Geological Survey Acid Rain Quality-Assurance Project","interactions":[],"lastModifiedDate":"2012-02-02T00:08:12","indexId":"wri904029","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4029","title":"Programs and analytical methods for the US Geological Survey Acid Rain Quality-Assurance Project","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904029","usgsCitation":"See, R., Willoughby, T.C., Brooks, M.H., and Gordon, J., 1990, Programs and analytical methods for the US Geological Survey Acid Rain Quality-Assurance Project: U.S. Geological Survey Water-Resources Investigations Report 90-4029, v, 57 p. :ill. ;28 cm., https://doi.org/10.3133/wri904029.","productDescription":"v, 57 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":157120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4029/report-thumb.jpg"},{"id":54489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4029/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e07f","contributors":{"authors":[{"text":"See, R.B.","contributorId":67910,"corporation":false,"usgs":true,"family":"See","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":194816,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willoughby, T. C.","contributorId":31791,"corporation":false,"usgs":true,"family":"Willoughby","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":194815,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brooks, M. H.","contributorId":107735,"corporation":false,"usgs":true,"family":"Brooks","given":"M.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":194817,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gordon, J.D.","contributorId":26684,"corporation":false,"usgs":true,"family":"Gordon","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":194814,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25585,"text":"wri884179 - 1990 - Hydrogeology, water quality, and effects of increased municipal pumpage of the Saco River valley glacial aquifer: Bartlett, New Hampshire to Fryeburg, Maine","interactions":[],"lastModifiedDate":"2022-02-03T20:46:59.720332","indexId":"wri884179","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"88-4179","title":"Hydrogeology, water quality, and effects of increased municipal pumpage of the Saco River valley glacial aquifer: Bartlett, New Hampshire to Fryeburg, Maine","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri884179","usgsCitation":"Tepper, D.H., Morrissey, D.J., Johnson, C., and Maloney, T.J., 1990, Hydrogeology, water quality, and effects of increased municipal pumpage of the Saco River valley glacial aquifer: Bartlett, New Hampshire to Fryeburg, Maine: U.S. Geological Survey Water-Resources Investigations Report 88-4179, Report: vii, 113 p.; 6 Plates: 37.28 × 36.39 inches or smaller, https://doi.org/10.3133/wri884179.","productDescription":"Report: vii, 113 p.; 6 Plates: 37.28 × 36.39 inches or smaller","costCenters":[],"links":[{"id":54324,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4179/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54323,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4179/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54322,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4179/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54321,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4179/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54320,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4179/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4179/report-thumb.jpg"},{"id":54319,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1988/4179/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54325,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4179/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":395407,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47083.htm"}],"country":"United States","state":"Maine, New Hampshire","otherGeospatial":"Saco River valley glacial aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.20788574218749,\n              43.87611806075357\n            ],\n            [\n              -70.8233642578125,\n              43.87611806075357\n            ],\n            [\n              -70.8233642578125,\n              44.143783302207424\n            ],\n            [\n              -71.20788574218749,\n              44.143783302207424\n            ],\n            [\n              -71.20788574218749,\n              43.87611806075357\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae04a","contributors":{"authors":[{"text":"Tepper, D. H.","contributorId":27466,"corporation":false,"usgs":true,"family":"Tepper","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":194295,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morrissey, D. J.","contributorId":51305,"corporation":false,"usgs":true,"family":"Morrissey","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":194296,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, C. D.","contributorId":8120,"corporation":false,"usgs":true,"family":"Johnson","given":"C. D.","affiliations":[],"preferred":false,"id":194294,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Maloney, T. J.","contributorId":56660,"corporation":false,"usgs":true,"family":"Maloney","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":194297,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54965,"text":"wdrSC891 - 1990 - Water resources data, South Carolina, water year 1989","interactions":[],"lastModifiedDate":"2020-10-23T18:47:12.461249","indexId":"wdrSC891","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"SC-89-1","title":"Water resources data, South Carolina, water year 1989","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrSC891","usgsCitation":"Bennett, C., Cooney, T., Jones, K., Church, B., and Murray, G., 1990, Water resources data, South Carolina, water year 1989: U.S. Geological Survey Water Data Report SC-89-1, viii, 585 p., 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,{"id":25403,"text":"wri904057 - 1990 - Assessment of contamination of ground water and surface water in the area of building 24, Picatinny Arsenal, New Jersey, 1986-87","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"wri904057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-4057","title":"Assessment of contamination of ground water and surface water in the area of building 24, Picatinny Arsenal, New Jersey, 1986-87","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904057","usgsCitation":"Sargent, B., Fusillo, T., Storck, D.A., and Smith, J.A., 1990, Assessment of contamination of ground water and surface water in the area of building 24, Picatinny Arsenal, New Jersey, 1986-87: U.S. Geological Survey Water-Resources Investigations Report 90-4057, vii, 120 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904057.","productDescription":"vii, 120 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118757,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4057/report-thumb.jpg"},{"id":54132,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672760","contributors":{"authors":[{"text":"Sargent, B. P.","contributorId":61827,"corporation":false,"usgs":true,"family":"Sargent","given":"B. P.","affiliations":[],"preferred":false,"id":193539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fusillo, T. V.","contributorId":91845,"corporation":false,"usgs":true,"family":"Fusillo","given":"T. V.","affiliations":[],"preferred":false,"id":193540,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Storck, D. A.","contributorId":59468,"corporation":false,"usgs":true,"family":"Storck","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":193538,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, J. A.","contributorId":101646,"corporation":false,"usgs":true,"family":"Smith","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":193541,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":54372,"text":"wdrAL891 - 1990 - Water resources data, Alabama, water year 1989","interactions":[],"lastModifiedDate":"2022-11-23T19:48:02.352099","indexId":"wdrAL891","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AL-89-1","title":"Water resources data, Alabama, water year 1989","docAbstract":"<p>The Water Resources Division of the U.S. Geological Survey, in cooperation with State and Federal agencies, obtains a large amount of data pertaining to the water resources of Alabama each water year. These data, accumulated during many water years, constitute a valuable data base for developing an improved understanding of the water resources of the State. 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,{"id":19684,"text":"ofr90641 - 1990 - Geologic map of the Loudoun County portion of the Middleburg Quadrangle, Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:07:38","indexId":"ofr90641","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-641","title":"Geologic map of the Loudoun County portion of the Middleburg Quadrangle, Virginia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr90641","usgsCitation":"Kline, S., Lyttle, P., and Froelich, A., 1990, Geologic map of the Loudoun County portion of the Middleburg Quadrangle, Virginia: U.S. Geological Survey Open-File Report 90-641, 18 p. :map ;28 cm., https://doi.org/10.3133/ofr90641.","productDescription":"18 p. :map ;28 cm.","costCenters":[],"links":[{"id":152057,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0641/report-thumb.jpg"},{"id":49167,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1990/0641/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":49168,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0641/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696d8c","contributors":{"authors":[{"text":"Kline, S.W.","contributorId":13262,"corporation":false,"usgs":true,"family":"Kline","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":181329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lyttle, P. T.","contributorId":93078,"corporation":false,"usgs":true,"family":"Lyttle","given":"P. T.","affiliations":[],"preferred":false,"id":181331,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Froelich, A.J.","contributorId":13593,"corporation":false,"usgs":true,"family":"Froelich","given":"A.J.","email":"","affiliations":[],"preferred":false,"id":181330,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3233,"text":"cir1041 - 1990 - Digitization of a geologic map for the Quebec-Maine-Gulf of Maine global geoscience transect","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir1041","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1041","title":"Digitization of a geologic map for the Quebec-Maine-Gulf of Maine global geoscience transect","docAbstract":"The Bedrock Geologic Map of Maine was digitized and combined with digital geologic data for Quebec and the Gulf of Maine for the Quebec-Maine-Gulf of Maine Geologic Transect Project. This map is being combined with digital geophysical data to produce three-dimensional depictions of the subsurface geology and to produce cross sections of the Earth's crust. It is an essential component of a transect that stretches from the craton near Quebec City, Quebec, to the Atlantic Ocean Basin south of Georges Bank. The transect is part of the Global Geosciences Transect Project of the International Lithosphere Program. \r\n\r\nThe Digital Line Graph format is used for storage of the digitized data. A coding scheme similar to that used for base category planimetric data was developed to assign numeric codes to the digitized geologic data. These codes were used to assign attributes to polygon and line features to describe rock type, age, name, tectonic setting of original deposition, mineralogy, and composition of igneous plutonic rocks, as well as faults and other linear features. \r\n\r\nThe digital geologic data can be readily edited, rescaled, and reprojected. The attribute codes allow generalization and selective retrieval of the geologic features. The codes allow assignment of map colors based on age, lithology, or other attribute. The Digital Line Graph format is a general transfer format that is supported by many software vendors and is easily transferred between systems.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nBooks and Open-file Reports Section, U.S. Geological Survey,","doi":"10.3133/cir1041","usgsCitation":"Wright, B.E., and Stewart, D.B., 1990, Digitization of a geologic map for the Quebec-Maine-Gulf of Maine global geoscience transect: U.S. Geological Survey Circular 1041, vi, 16 p. :ill. ;28 cm., https://doi.org/10.3133/cir1041.","productDescription":"vi, 16 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":124676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1990/1041/report-thumb.jpg"},{"id":30225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1990/1041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aecf9","contributors":{"authors":[{"text":"Wright, Bruce E.","contributorId":93885,"corporation":false,"usgs":true,"family":"Wright","given":"Bruce","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146481,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, David B.","contributorId":79864,"corporation":false,"usgs":true,"family":"Stewart","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146480,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2772,"text":"wsp2292 - 1990 - Geohydrology and simulated effects of large ground-water withdrawals on the Mississippi River alluvial aquifer in northwestern Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp2292","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2292","title":"Geohydrology and simulated effects of large ground-water withdrawals on the Mississippi River alluvial aquifer in northwestern Mississippi","docAbstract":"The 7,000-square-mile Mississippi River alluvial plain in northwestern Mississippi, locally known as the 'Delta,' is underlain by a prolific aquifer that yielded about 1,100 million gallons per day of water to irrigation wells in 1983. About 20 feet of clay underlying the Delta land surface commonly is underlain by about 80 to 180 feet of sand and gravel that forms the Mississippi River alluvial aquifer. This study of the alluvial aquifer was prompted by recent declines of water levels. The study was designed to better define the hydrology of the aquifer and to quantify availability of water from the aquifer. \r\n\r\nThe Mississippi River is in good hydraulic connection with the alluvial aquifer. Generally, smaller streams are less likely to recharge the aquifer than larger streams. Direct vertical recharge to the alluvial aquifer from the 52 inches per year of precipitation is small, especially in the central part of the Delta. \r\n\r\nA two-dimensional finite-difference computer model of the alluvial aquifer was constructed, calibrated, and verified using water levels observed for five dates from April 1981 to September 1983. The values of some of the calibration-derived parameters are hydraulic conductivity, 400 feet per day; specific yield, 0.30; and infiltration of precipitation to the aquifer, 0.5 inch per year. \r\n\r\nThe model showed that the aquifer had a net loss in storage of about 360 million gallons per day from April 1981 to April 1983. During this period, pumpage was about 1,100 million gallons per day (1,270,000 acre-feet per year), and the net inflows from the sources of recharge were as follows, in million gallons per day: Mississippi River, 390; recharge along the east edge of the Delta, 170; streams within the Delta, 57; areal recharge from infiltration, 180; and oxbow lakes, 24. \r\n\r\nThe effects of several levels of pumpage by wells--0, 670, 1,100, 1,900, and 4,000 million gallons per day--were projected 20 years into the future. In 2003, the 1,100-milliongallon-per-day pumping rate, about average for the early 1980's, would take 46 percent of the water withdrawn from aquifer storage, water levels would be lowered more than 20 feet in a large area in the central part of the Delta, and groundwater levels would continue to decline in future years.","language":"ENGLISH","publisher":"U.S. G.P.O. ;\r\nFor sale by the Books and Open-File Reports Section, U.S. Geological Survey,","doi":"10.3133/wsp2292","usgsCitation":"Sumner, D.M., and Wasson, B.E., 1990, Geohydrology and simulated effects of large ground-water withdrawals on the Mississippi River alluvial aquifer in northwestern Mississippi: U.S. Geological Survey Water Supply Paper 2292, vi, 60 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2292.","productDescription":"vi, 60 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":138668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2292/report-thumb.jpg"},{"id":29220,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2292/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c76","contributors":{"authors":[{"text":"Sumner, D. M.","contributorId":100827,"corporation":false,"usgs":true,"family":"Sumner","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":145758,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wasson, Billie E.","contributorId":85571,"corporation":false,"usgs":true,"family":"Wasson","given":"Billie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145757,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2441,"text":"wsp2365 - 1990 - Methods for estimating monthly streamflow characteristics at ungaged sites in western Montana","interactions":[],"lastModifiedDate":"2023-01-09T22:45:26.642346","indexId":"wsp2365","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2365","title":"Methods for estimating monthly streamflow characteristics at ungaged sites in western Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2365","usgsCitation":"Parrett, C., and Cartier, K.D., 1990, Methods for estimating monthly streamflow characteristics at ungaged sites in western Montana: U.S. Geological Survey Water Supply Paper 2365, iv, 30 p., https://doi.org/10.3133/wsp2365.","productDescription":"iv, 30 p.","costCenters":[],"links":[{"id":411599,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25387.htm","linkFileType":{"id":5,"text":"html"}},{"id":28511,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2365/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138624,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2365/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116,\n              49\n            ],\n            [\n              -116,\n              45.817\n            ],\n            [\n              -112,\n              45.817\n            ],\n            [\n              -112,\n              49\n            ],\n            [\n              -116,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a3b7","contributors":{"authors":[{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":145210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cartier, Kenn D.","contributorId":39766,"corporation":false,"usgs":true,"family":"Cartier","given":"Kenn","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":145211,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":49306,"text":"ofr90609A - 1990 - Earthquake Data Report, September 1990","interactions":[],"lastModifiedDate":"2012-02-02T00:11:11","indexId":"ofr90609A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-609","chapter":"A","title":"Earthquake Data Report, September 1990","language":"ENGLISH","doi":"10.3133/ofr90609A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1990, Earthquake Data Report, September 1990: U.S. Geological Survey Open-File Report 90-609, 266 p., https://doi.org/10.3133/ofr90609A.","productDescription":"266 p.","costCenters":[],"links":[{"id":176115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0609a/report-thumb.jpg"},{"id":85997,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0609a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696b0f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20050,"text":"ofr90479 - 1990 - Deterioration of building stones in Washington, DC; a field trip guide","interactions":[],"lastModifiedDate":"2012-02-02T00:07:54","indexId":"ofr90479","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-479","title":"Deterioration of building stones in Washington, DC; a field trip guide","language":"ENGLISH","publisher":"Dept. of the Interior, U.S. Geological Survey,","doi":"10.3133/ofr90479","usgsCitation":"McGee, E.S., 1990, Deterioration of building stones in Washington, DC; a field trip guide: U.S. Geological Survey Open-File Report 90-479, 16 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90479.","productDescription":"16 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0479/report-thumb.jpg"},{"id":49607,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0479/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6679cc","contributors":{"authors":[{"text":"McGee, E. S.","contributorId":75927,"corporation":false,"usgs":true,"family":"McGee","given":"E.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":181968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20300,"text":"ofr87547 - 1990 - Estimates of dissolved solids and major dissolved constituents for 70 streamflow-gaging stations in the Upper Colorado River basin, Arizona, Colorado, New Mexico, Utah, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:07:38","indexId":"ofr87547","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"87-547","title":"Estimates of dissolved solids and major dissolved constituents for 70 streamflow-gaging stations in the Upper Colorado River basin, Arizona, Colorado, New Mexico, Utah, and Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey :\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/ofr87547","usgsCitation":"Nordlund, B., and Liebermann, T., 1990, Estimates of dissolved solids and major dissolved constituents for 70 streamflow-gaging stations in the Upper Colorado River basin, Arizona, Colorado, New Mexico, Utah, and Wyoming: U.S. Geological Survey Open-File Report 87-547, iv, 441 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87547.","productDescription":"iv, 441 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":152081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0547/report-thumb.jpg"},{"id":49835,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0547/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcbae","contributors":{"authors":[{"text":"Nordlund, B.D.","contributorId":18795,"corporation":false,"usgs":true,"family":"Nordlund","given":"B.D.","email":"","affiliations":[],"preferred":false,"id":182416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Liebermann, T.D.","contributorId":23569,"corporation":false,"usgs":true,"family":"Liebermann","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":182417,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17174,"text":"ofr90294 - 1990 - Geology and mineralization at the Ishmas Kabir gold prospect, Ishmas gold district, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2015-09-02T16:12:13","indexId":"ofr90294","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1990","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":"90-294","title":"Geology and mineralization at the Ishmas Kabir gold prospect, Ishmas gold district, Kingdom of Saudi Arabia","docAbstract":"<p>Ishmas Kabir ancient gold mine is located approximately 60 km southeast of the city of Ranyah and 9 km northwest of Jabal Ishmas in the southwestern part of the Ishmas gold district. The mine workings are located near the eastern edge of a flat plain covered by eolian sand and drained by Wadi Bishah. Two elongate dumps, 75 m wide and 530 m long (combined length), comprise the workings. Rising 4 m above the plain, they are prominent features in this area of low relief.</p>\n<p>Core drilling (1,023 m total depth drilled) was conducted to define the extent of potential gold occurrences at the prospect. The two northeasternmost of the four holes drilled unequivocally intersected the gold-bearing main vein zone. Drill hole 1, the northeasternmost hole drilled, passed through significant lengths of altered wall rocks + quartz veins containing &gt; 100 ppb Au (threshold value). The average gold concentration of all intercepts in drill holes 1 through 4 is 278 ppb; the total length of drill core that assayed above the gold threshold value is 13.46 m. The highest gold concentration (1,620 ppb) reported in geochemical assay results was obtained from a 0.33 m length of core in drill hole 1. Gold-intercept occurrences are not economic in the rocks drilled; no further deep drilling is recommended at this time.</p>\n<p>Gold concentrations in samples obtained from mine dumps are much higher than in drill-core samples. Samples collected by earlier workers assayed 3-7 g/t, and tonnage estimates of mine spoil have been estimated to be as high as 120,000 tons. A possible sampling bias in earlier studies may favor larger gold-enriched, samples relative to samples from quartz tailings. Further work at Ishmas Kabir should be limited to defining gold resource potential in the dumps and in the oxidized, near-surface quartz-vein system.</p>\n<p>Primary gold at the Ishmas Kabir gold prospect occurs with quartz veins and associated sericite + pyrite alteration hosted by quartz diorite and mafic dikes. The highest gold concentrations both in dumps (earlier studies) and drill core (this investigation) are found with limonite + hematite in breccia zones, in stringer veins, and in sericitic alteration envelopes surrounding quartz veins. Secondary gold is significant in this system and attests to the importance of oxidizing, acidic solutions.</p>\n<p>Quartz veins intersected by drill holes are surrounded by mylonite schist. Quartz and carbonate veins less than 5 mm thick are boudined, whereas thick quartz veins (&pound; 1.2 m) have disrupted and brecciated margins; mylonitized country rock envelops quartz-vein fragments. Sulfide mineralization associated with vein formation predates this rock-deformation event. Contemporaneous brittle and ductile deformation of quartz veins and country rocks occurred during the Nabitah orogeny. Supergene gold enrichment took place much later.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr90294","usgsCitation":"Walker, B., Ben Talib, M., El Komi, M., Hussain, M., and Christian, R., 1990, Geology and mineralization at the Ishmas Kabir gold prospect, Ishmas gold district, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 90-294, iii, 91 p. :ill. ;28 cm., https://doi.org/10.3133/ofr90294.","productDescription":"iii, 91 p. :ill. ;28 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":150196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1990/0294/report-thumb.jpg"},{"id":46316,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1990/0294/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Saudi Arabia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              43,\n              20\n            ],\n            [\n              43,\n              30\n            ],\n            [\n              44,\n              30\n            ],\n            [\n              44,\n              20\n            ],\n            [\n              43,\n             20\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4734","contributors":{"authors":[{"text":"Walker, B.M.","contributorId":26820,"corporation":false,"usgs":true,"family":"Walker","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":175259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ben Talib, Majed","contributorId":100242,"corporation":false,"usgs":true,"family":"Ben Talib","given":"Majed","email":"","affiliations":[],"preferred":false,"id":175262,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"El Komi, Mohamed","contributorId":38418,"corporation":false,"usgs":true,"family":"El Komi","given":"Mohamed","email":"","affiliations":[],"preferred":false,"id":175260,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hussain, M.A.","contributorId":104492,"corporation":false,"usgs":true,"family":"Hussain","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":175263,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Christian, R.P.","contributorId":51313,"corporation":false,"usgs":true,"family":"Christian","given":"R.P.","email":"","affiliations":[],"preferred":false,"id":175261,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
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