{"pageNumber":"2542","pageRowStart":"63525","pageSize":"25","recordCount":184652,"records":[{"id":72476,"text":"sir20055211 - 2005 - Hydraulic characterization of overpressured tuffs in central Yucca Flat, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2019-09-10T08:44:47","indexId":"sir20055211","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5211","title":"Hydraulic characterization of overpressured tuffs in central Yucca Flat, Nevada Test Site, Nye County, Nevada","docAbstract":"A sequence of buried, bedded, air-fall tuffs has been used extensively as a host medium for underground nuclear tests detonated in the central part of Yucca Flat at the Nevada Test Site. Water levels within these bedded tuffs have been elevated hundreds of meters in areas where underground nuclear tests were detonated below the water table. Changes in the ground-water levels within these tuffs and changes in the rate and distribution of land-surface subsidence above these tuffs indicate that pore-fluid pressures have been slowly depressurizing since the cessation of nuclear testing in 1992. Declines in ground-water levels concurrent with regional land subsidence are explained by poroelastic deformation accompanying ground-water flow as fluids pressurized by underground nuclear detonations drain from the host tuffs into the overlying water table and underlying regional carbonate aquifer. A hydraulic conductivity of about 3 x 10-6 m/d and a specific storage of 9 x 10-6 m-1 are estimated using ground-water flow models. Cross-sectional and three-dimensional ground-water flow models were calibrated to measured water levels and to land-subsidence rates measured using Interferometric Synthetic Aperture Radar. Model results are consistent and indicate that about 2 million m3 of ground water flowed from the tuffs to the carbonate rock as a result of pressurization caused by underground nuclear testing. The annual rate of inflow into the carbonate rock averaged about 0.008 m/yr between 1962 and 2005, and declined from 0.005 m/yr in 2005 to 0.0005 m/yr by 2300.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055211","usgsCitation":"Halford, K.J., Laczniak, R.J., and Galloway, D.L., 2005, Hydraulic characterization of overpressured tuffs in central Yucca Flat, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Scientific Investigations Report 2005-5211, 55 p., https://doi.org/10.3133/sir20055211.","productDescription":"55 p.","onlineOnly":"Y","costCenters":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":191204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7535,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5211/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nevada","county":"Nye County","otherGeospatial":"central Yucca Flat","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-115.9082,39.1615],[-115.5191,38.9578],[-115.4725,38.9325],[-115.4433,38.9162],[-115.3694,38.8769],[-115.363,38.874],[-115.242,38.8093],[-115.0969,38.7309],[-115.0777,38.721],[-115.0604,38.7107],[-115.0291,38.6937],[-114.999,38.6777],[-114.9996,38.592],[-114.9997,38.4315],[-114.9994,38.3894],[-115.0004,38.0507],[-115.1185,38.0508],[-115.1436,38.0508],[-115.326,38.0515],[-115.3453,38.0514],[-115.4003,38.051],[-115.4587,38.0506],[-115.6394,38.0512],[-115.6581,38.051],[-115.8404,38.0504],[-115.8931,38.0507],[-115.8938,37.723],[-115.8969,37.5498],[-115.8975,37.2796],[-115.8982,37.1926],[-115.8942,36.8425],[-115.8941,36.686],[-115.8945,36.6702],[-115.8949,36.598],[-115.8949,36.5962],[-115.8946,36.5858],[-115.8947,36.5005],[-115.8945,36.4806],[-115.8949,36.462],[-115.8944,36.457],[-115.8948,36.3087],[-115.8945,36.2923],[-115.8943,36.1957],[-115.8945,36.1608],[-115.8948,36.1163],[-115.8948,36.0927],[-115.895,36.0015],[-115.9178,36.0192],[-115.9518,36.0457],[-115.9925,36.0773],[-116.049,36.1211],[-116.0624,36.1314],[-116.1039,36.1636],[-116.1287,36.1829],[-116.1702,36.2152],[-116.173,36.2174],[-116.2311,36.2626],[-116.2834,36.3028],[-116.2954,36.3122],[-116.3752,36.373],[-116.5107,36.4764],[-116.5247,36.4871],[-116.5589,36.5131],[-116.574,36.5245],[-116.5946,36.54],[-116.6556,36.5867],[-116.6583,36.5888],[-116.6764,36.6024],[-116.706,36.6248],[-116.7895,36.6877],[-116.8424,36.7276],[-116.8453,36.7298],[-116.8806,36.7568],[-116.8912,36.7648],[-116.9237,36.7891],[-116.9641,36.8193],[-116.9783,36.8299],[-116.981,36.8319],[-117.0046,36.8495],[-117.164,36.9688],[-117.1639,36.9698],[-117.1637,37.0182],[-117.164,37.0894],[-117.1642,37.171],[-117.1641,37.1909],[-117.1641,37.1936],[-117.1665,37.6995],[-117.1664,37.714],[-117.1663,37.7285],[-117.1663,37.7435],[-117.1662,37.7585],[-117.1657,38.0019],[-117.2198,38.0482],[-117.2397,38.0483],[-117.239,38.0641],[-117.2408,38.0705],[-117.2653,38.0932],[-117.6896,38.4731],[-118.0197,38.7599],[-118.197,38.9154],[-118.1972,38.9993],[-117.8559,39.0746],[-117.7748,39.092],[-117.7008,39.1058],[-117.6409,39.1149],[-117.5946,39.1231],[-117.4742,39.1431],[-117.3823,39.1562],[-117.3609,39.1585],[-117.3318,39.1629],[-117.3063,39.1634],[-117.2849,39.1633],[-117.1995,39.1632],[-117.0856,39.1628],[-117.0322,39.1626],[-117.0144,39.1626],[-116.9871,39.1625],[-116.9158,39.1631],[-116.7562,39.1622],[-116.7301,39.1625],[-116.5996,39.1616],[-116.5859,39.162],[-116.4815,39.1616],[-116.3497,39.1618],[-116.2358,39.1616],[-116.0548,39.1624],[-115.9082,39.1615]]]},\"properties\":{\"name\":\"Nye\",\"state\":\"NV\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6297be","contributors":{"authors":[{"text":"Halford, Keith J. 0000-0002-7322-1846 khalford@usgs.gov","orcid":"https://orcid.org/0000-0002-7322-1846","contributorId":1374,"corporation":false,"usgs":true,"family":"Halford","given":"Keith","email":"khalford@usgs.gov","middleInitial":"J.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Laczniak, Randell J.","contributorId":90687,"corporation":false,"usgs":true,"family":"Laczniak","given":"Randell","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":285718,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Galloway, Devin L. 0000-0003-0904-5355 dlgallow@usgs.gov","orcid":"https://orcid.org/0000-0003-0904-5355","contributorId":679,"corporation":false,"usgs":true,"family":"Galloway","given":"Devin","email":"dlgallow@usgs.gov","middleInitial":"L.","affiliations":[{"id":5058,"text":"Office of the Chief Scientist for Water","active":true,"usgs":true},{"id":5078,"text":"Southwest Regional Director's Office","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":509,"text":"Office of the Associate Director for Water","active":true,"usgs":true}],"preferred":true,"id":285716,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72480,"text":"sir20055147 - 2005 - Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland","interactions":[],"lastModifiedDate":"2017-07-10T10:35:12","indexId":"sir20055147","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5147","title":"Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland","docAbstract":"Natural-stream designs are commonly based on the dimensions of the bankfull channel, which is capable of conveying discharges that transport sediment without excessive erosion or deposition. Regional curves relate bankfull-channel geometry and discharge to drainage area in watersheds with similar runoff characteristics and commonly are utilized by practitioners of natural-stream design to confirm or refute selection of the field-identified bankfull channel. Data collected from 66 streamflow-gaging stations and associated stream reaches between December 1999 and December 2003 were used in one-variable ordinary least-squares regression analyses to develop regional curves relating drainage area to cross-sectional area, discharge, width, and mean depth of the bankfull channel. Watersheds draining to these stations are predominantly within the Piedmont, Ridge and Valley, and Appalachian Plateaus Physiographic Provinces of Pennsylvania and northern Maryland. \r\n\r\nStatistical analyses of physiography, percentage of watershed area underlain by carbonate bedrock, and percentage of watershed area that is glaciated indicate that carbonate bedrock, not physiography or glaciation, has a controlling influence on the slope of regional curves. Regional curves developed from stations in watersheds underlain by 30 percent or less carbonate bedrock generally had steeper slopes than the corresponding relations developed from watersheds underlain by greater than 30 percent carbonate bedrock. In contrast, there is little evidence to suggest that regional curves developed from stations in the Piedmont or Ridge and Valley Physiographic Province are different from the corresponding relations developed from stations in the Appalachian Plateaus Physiographic Province. On the basis of these findings, regional curves are presented to represent two settings that are independent of physiography: (1) noncarbonate settings characterized by watersheds with carbonate bedrock underlying 30 percent or less of watershed area, and (2) carbonate settings characterized by watersheds with carbonate bedrock underlying greater than 30 percent of watershed area. \r\n\r\nAll regional curves presented in this report have slopes that are significantly different from zero and normally distributed residuals that vary randomly with drainage area. Drainage area explains the most variability in bankfull cross-sectional area and bankfull discharge in the noncarbonate setting (R2 = 0.92 for both). Less variability is explained in bankfull width and depth (R2 = 0.81 and 0.72, respectively). Regional curves representing the carbonate setting are generally not as statistically robust as the corresponding noncarbonate relations because there were only 11 stations available to develop these curves and drainage area cannot explain variance resulting from karst features. The carbonate regional curves generally are characterized by less confidence, lower R2 values, and higher residual standard errors. Poor representation by watersheds less than 40 mi2 causes the carbonate regional curves for bankfull discharge, cross-sectional area, and mean depth to be disproportionately influenced by the smallest watershed (values of Cook's Distance range from 3.6 to 8.4). Additional bankfull discharge and channel-geometry data from small watersheds might reduce this influence, increase confidence, and generally improve regional curves representing the carbonate setting. \r\n\r\nLimitations associated with streamflow-gaging station selection and development of the curves result in some constraints for the application of regional curves presented in this report. These curves apply only to streams within the study area in watersheds having land use, streamflow regulation, and drainage areas that are consistent with the criteria used for station selection. Regardless of the setting, the regional curves presented here are not intended for use as the sole method for estimation of bankfull characteristics; however, th","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055147","usgsCitation":"Chaplin, J.J., 2005, Development of regional curves relating bankfull-channel geometry and discharge to drainage area for streams in Pennsylvania and selected areas of Maryland: U.S. Geological Survey Scientific Investigations Report 2005-5147, 40 p., https://doi.org/10.3133/sir20055147.","productDescription":"40 p.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":192903,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7538,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5147/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81,39.833333333333336 ], [ -81,42.833333333333336 ], [ -74,42.833333333333336 ], [ -74,39.833333333333336 ], [ -81,39.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de31","contributors":{"authors":[{"text":"Chaplin, Jeffrey J. 0000-0002-0617-5050 jchaplin@usgs.gov","orcid":"https://orcid.org/0000-0002-0617-5050","contributorId":147,"corporation":false,"usgs":true,"family":"Chaplin","given":"Jeffrey","email":"jchaplin@usgs.gov","middleInitial":"J.","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285721,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72482,"text":"ofr20051282 - 2005 - Preliminary investigations of wastewater-related contaminants near home sewage treatment systems in Ohio","interactions":[],"lastModifiedDate":"2022-08-31T18:15:18.949272","indexId":"ofr20051282","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","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":"2005-1282","title":"Preliminary investigations of wastewater-related contaminants near home sewage treatment systems in Ohio","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051282","usgsCitation":"Dumouchelle, D., and Stoeckel, D.M., 2005, Preliminary investigations of wastewater-related contaminants near home sewage 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,{"id":72483,"text":"sir20055210 - 2005 - Water, ice, and meteorological measurements at South Cascade glacier, Washington, balance year 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"sir20055210","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5210","title":"Water, ice, and meteorological measurements at South Cascade glacier, Washington, balance year 2003","docAbstract":"Winter snow accumulation and summer snow and ice ablation were measured at South Cascade Glacier, Washington, to estimate glacier mass-balance quantities for balance year 2003. The 2003 glacier-average maximum winter snow balance was 2.66 meters water equivalent, which was about equal to the average of such balances for the glacier since balance year 1959. The 2003 glacier summer balance (-4.76 meters water equivalent) was the most negative reported for the glacier, and the 2003 net balance (-2.10 meters water equivalent), was the second-most negative reported. The glacier 2003 annual (water year) balance was -1.89 meters water equivalent. \r\n\r\nThe area of the glacier near the end of the balance year was 1.89 square kilometers, a decrease of 0.03 square kilometer from the previous year. The equilibrium-line altitude was higher than any part of the glacier; however, because snow remained along part of one side of the upper glacier, the accumulation-area ratio was 0.07. During September 13, 2002-September 13, 2003, the glacier terminus retreated at a rate of about 15 meters per year. Average speed of surface ice, computed using a series of vertical aerial photographs dating back to 2001, ranged from 2.2 to 21.8 meters per year. \r\n\r\nRunoff from the subbasin containing the glacier and from an adjacent non-glacierized basin was gaged during part of water year 2003. Air temperature, precipitation, atmospheric water-vapor pressure, wind speed, and incoming solar radiation were measured at selected locations on and near the glacier. Summer 2003 at the glacier was among the warmest for which data are available.","language":"ENGLISH","doi":"10.3133/sir20055210","usgsCitation":"Bidlake, W.R., Josberger, E.G., and Savoca, M.E., 2005, Water, ice, and meteorological measurements at South Cascade glacier, Washington, balance year 2003: U.S. Geological Survey Scientific Investigations Report 2005-5210, 60 p., https://doi.org/10.3133/sir20055210.","productDescription":"60 p.","costCenters":[],"links":[{"id":192960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7540,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5210/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489b05","contributors":{"authors":[{"text":"Bidlake, William R. wbidlake@usgs.gov","contributorId":1712,"corporation":false,"usgs":true,"family":"Bidlake","given":"William","email":"wbidlake@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":285725,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Josberger, Edward G. ejosberg@usgs.gov","contributorId":1710,"corporation":false,"usgs":true,"family":"Josberger","given":"Edward","email":"ejosberg@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":285724,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Savoca, Mark E. mesavoca@usgs.gov","contributorId":1961,"corporation":false,"usgs":true,"family":"Savoca","given":"Mark","email":"mesavoca@usgs.gov","middleInitial":"E.","affiliations":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285726,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72478,"text":"ofr20051336 - 2005 - Known or suggested Quaternary tectonic faulting, central and eastern United States-new and updated assessments for 2005","interactions":[],"lastModifiedDate":"2012-02-02T00:13:57","indexId":"ofr20051336","displayToPublicDate":"2005-10-14T00:00:00","publicationYear":"2005","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":"2005-1336","title":"Known or suggested Quaternary tectonic faulting, central and eastern United States-new and updated assessments for 2005","language":"ENGLISH","doi":"10.3133/ofr20051336","usgsCitation":"Wheeler, R.L., 2005, Known or suggested Quaternary tectonic faulting, central and eastern United States-new and updated assessments for 2005 (Online only, Version 1.0): U.S. Geological Survey Open-File Report 2005-1336, 40 p., https://doi.org/10.3133/ofr20051336.","productDescription":"40 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":191205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7536,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1336/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only, Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4778","contributors":{"authors":[{"text":"Wheeler, Russell L. wheeler@usgs.gov","contributorId":858,"corporation":false,"usgs":true,"family":"Wheeler","given":"Russell","email":"wheeler@usgs.gov","middleInitial":"L.","affiliations":[],"preferred":false,"id":285719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70238383,"text":"70238383 - 2005 - Implications for prediction and hazard assessment from the 2004 Parkfield earthquake","interactions":[],"lastModifiedDate":"2022-11-18T18:18:55.697023","indexId":"70238383","displayToPublicDate":"2005-10-13T11:50:53","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Implications for prediction and hazard assessment from the 2004 Parkfield earthquake","docAbstract":"<p><span>Obtaining high-quality measurements close to a large earthquake is not easy: one has to be in the right place at the right time with the right instruments. Such a convergence happened, for the first time, when the 28 September 2004 Parkfield, California, earthquake occurred on the San Andreas fault in the middle of a dense network of instruments designed to record it. The resulting data reveal aspects of the earthquake process never before seen. Here we show what these data, when combined with data from earlier Parkfield earthquakes, tell us about earthquake physics and earthquake prediction. The 2004 Parkfield earthquake, with its lack of obvious precursors, demonstrates that reliable short-term earthquake prediction still is not achievable. To reduce the societal impact of earthquakes now, we should focus on developing the next generation of models that can provide better predictions of the strength and location of damaging ground shaking.</span></p>","language":"English","publisher":"Springer","doi":"10.1038/nature04067","usgsCitation":"Bakun, W.H., Aagaard, B.T., Dost, B., Ellsworth, W.L., Hardebeck, J.L., Harris, R.A., Ji, C., Johnston, M.J., Langbein, J.O., Lienkaemper, J.J., Michael, A.J., Murray, J.R., Nadeau, R., Reasenberg, P., Reichle, M., Roeloffs, E.A., Shakal, A., Simpson, R.W., and Waldhauser, F., 2005, Implications for prediction and hazard assessment from the 2004 Parkfield earthquake: Nature, v. 437, p. 969-974, https://doi.org/10.1038/nature04067.","productDescription":"6 p.","startPage":"969","endPage":"974","costCenters":[],"links":[{"id":477643,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://resolver.caltech.edu/CaltechAUTHORS:20150403-080028282","text":"External Repository"},{"id":409458,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Parkfield","otherGeospatial":"San Andreas Fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.4537640117938,\n              35.910700976762385\n            ],\n            [\n              -120.4537640117938,\n              35.88567088811958\n            ],\n            [\n              -120.41342358821001,\n              35.88567088811958\n            ],\n            [\n              -120.41342358821001,\n              35.910700976762385\n            ],\n            [\n              -120.4537640117938,\n              35.910700976762385\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"437","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bakun, W. H.","contributorId":67055,"corporation":false,"usgs":true,"family":"Bakun","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":857297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aagaard, Brad T. 0000-0002-8795-9833 baagaard@usgs.gov","orcid":"https://orcid.org/0000-0002-8795-9833","contributorId":192869,"corporation":false,"usgs":true,"family":"Aagaard","given":"Brad","email":"baagaard@usgs.gov","middleInitial":"T.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":857298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dost, B.","contributorId":299207,"corporation":false,"usgs":false,"family":"Dost","given":"B.","email":"","affiliations":[{"id":16158,"text":"Royal Netherlands Meteorological Institute","active":true,"usgs":false}],"preferred":false,"id":857299,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ellsworth, William L. ellsworth@usgs.gov","contributorId":787,"corporation":false,"usgs":true,"family":"Ellsworth","given":"William","email":"ellsworth@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857300,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hardebeck, Jeanne L. 0000-0002-6737-7780 jhardebeck@usgs.gov","orcid":"https://orcid.org/0000-0002-6737-7780","contributorId":841,"corporation":false,"usgs":true,"family":"Hardebeck","given":"Jeanne","email":"jhardebeck@usgs.gov","middleInitial":"L.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true}],"preferred":true,"id":857301,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Harris, Ruth A. 0000-0002-9247-0768 harris@usgs.gov","orcid":"https://orcid.org/0000-0002-9247-0768","contributorId":786,"corporation":false,"usgs":true,"family":"Harris","given":"Ruth","email":"harris@usgs.gov","middleInitial":"A.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857302,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ji, C.","contributorId":31093,"corporation":false,"usgs":true,"family":"Ji","given":"C.","email":"","affiliations":[],"preferred":false,"id":857303,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Johnston, Malcolm J. S. 0000-0003-4326-8368 mal@usgs.gov","orcid":"https://orcid.org/0000-0003-4326-8368","contributorId":622,"corporation":false,"usgs":true,"family":"Johnston","given":"Malcolm","email":"mal@usgs.gov","middleInitial":"J. S.","affiliations":[],"preferred":true,"id":857304,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Langbein, John O. 0000-0002-7821-8101 langbein@usgs.gov","orcid":"https://orcid.org/0000-0002-7821-8101","contributorId":3293,"corporation":false,"usgs":true,"family":"Langbein","given":"John","email":"langbein@usgs.gov","middleInitial":"O.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857305,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Lienkaemper, James J. 0000-0002-7578-7042 jlienk@usgs.gov","orcid":"https://orcid.org/0000-0002-7578-7042","contributorId":1941,"corporation":false,"usgs":true,"family":"Lienkaemper","given":"James","email":"jlienk@usgs.gov","middleInitial":"J.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857306,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Michael, Andrew J. 0000-0002-2403-5019 michael@usgs.gov","orcid":"https://orcid.org/0000-0002-2403-5019","contributorId":1280,"corporation":false,"usgs":true,"family":"Michael","given":"Andrew","email":"michael@usgs.gov","middleInitial":"J.","affiliations":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857307,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Murray, Jessica R. 0000-0002-6144-1681 jrmurray@usgs.gov","orcid":"https://orcid.org/0000-0002-6144-1681","contributorId":2759,"corporation":false,"usgs":true,"family":"Murray","given":"Jessica","email":"jrmurray@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857308,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Nadeau, R.M.","contributorId":93268,"corporation":false,"usgs":true,"family":"Nadeau","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":857309,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Reasenberg, P.A.","contributorId":19959,"corporation":false,"usgs":true,"family":"Reasenberg","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":857310,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Reichle, M.S.","contributorId":14845,"corporation":false,"usgs":true,"family":"Reichle","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":857311,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Roeloffs, Evelyn A. 0000-0002-4761-0469 evelynr@usgs.gov","orcid":"https://orcid.org/0000-0002-4761-0469","contributorId":2680,"corporation":false,"usgs":true,"family":"Roeloffs","given":"Evelyn","email":"evelynr@usgs.gov","middleInitial":"A.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":857312,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Shakal, A.","contributorId":20934,"corporation":false,"usgs":false,"family":"Shakal","given":"A.","email":"","affiliations":[{"id":12640,"text":"California Geological Survey","active":true,"usgs":false}],"preferred":false,"id":857313,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Simpson, Robert W. simpson@usgs.gov","contributorId":1053,"corporation":false,"usgs":true,"family":"Simpson","given":"Robert","email":"simpson@usgs.gov","middleInitial":"W.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":857314,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Waldhauser, F.","contributorId":31897,"corporation":false,"usgs":true,"family":"Waldhauser","given":"F.","affiliations":[],"preferred":false,"id":857315,"contributorType":{"id":1,"text":"Authors"},"rank":19}]}}
,{"id":72470,"text":"sim2841 - 2005 - Geologic map of the Stafford quadrangle, Stafford County, Virginia","interactions":[],"lastModifiedDate":"2022-04-14T18:57:29.415324","indexId":"sim2841","displayToPublicDate":"2005-10-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2841","title":"Geologic map of the Stafford quadrangle, Stafford County, Virginia","docAbstract":"Introduction\r\n\r\nThe Stafford 7.5-minute quadrangle, comprising approximately 55 square miles (142.5 square kilometers) of northeastern Virginia, is about 40 miles (mi) south of Washington, D.C. The region's main north-south transportation corridor, which connects Washington, D.C., and Richmond, Va., consists of Interstate 95, U.S. Highway 1, and the heavily used CSX and Amtrak railroads. Although the northern and eastern parts of the Stafford quadrangle have undergone extensive suburban development, the remainder of the area is still dominantly rural in character. The town of Stafford is the county seat.\r\n\r\nThe Stafford 7.5-minute quadrangle is located in the Fredericksburg 30'x60' quadrangle, where information on the regional stratigraphy and structure is available from Mixon and others' (2000) geologic map and multichapter explanatory text. In addition to straddling the 'Fall Zone' boundary between the Appalachian Piedmont and the Atlantic Coastal Plain provinces, this quadrangle contains the best preserved and best studied segment of the Stafford fault system, an important example of late Cenozoic faulting in eastern North America (Mixon and Newell, 1977). This 1:24,000-scale geologic map provides a detailed framework for interpreting and integrating topical studies of that fault system.\r\n\r\nOur geologic map integrates more than two decades of intermittent geologic mapping and related investigations by the authors in this part of the Virginia Coastal Plain. Earlier mapping in the Piedmont by Pavlides (1995) has been revised by additional detailed mapping in selected areas, particularly near Abel Lake and Smith Lake, and by field evaluation of selected contact relations.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sim2841","usgsCitation":"Mixon, R.B., Pavlides, L., Horton, J., Powars, D.S., and Schindler, J.S., 2005, Geologic map of the Stafford quadrangle, Stafford County, Virginia: U.S. Geological Survey Scientific Investigations Map 2841, 1 Plate: 57.00 x 34.00 inches, https://doi.org/10.3133/sim2841.","productDescription":"1 Plate: 57.00 x 34.00 inches","costCenters":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":191017,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110724,"rank":700,"type":{"id":7,"text":"Companion Files"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_81183.htm","linkFileType":{"id":5,"text":"html"},"description":"81183"},{"id":398745,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_81183.htm"},{"id":9491,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sim/2005/2841/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Virginia","county":"Stafford County","otherGeospatial":"Stafford quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.5,\n              38.375\n            ],\n            [\n              -77.375,\n              38.375\n            ],\n            [\n              -77.375,\n              38.5\n            ],\n            [\n              -77.5,\n              38.5\n            ],\n            [\n              -77.5,\n              38.375\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a841f","contributors":{"authors":[{"text":"Mixon, Robert B.","contributorId":50517,"corporation":false,"usgs":true,"family":"Mixon","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":285708,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pavlides, Louis","contributorId":79444,"corporation":false,"usgs":true,"family":"Pavlides","given":"Louis","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":285709,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horton, J. Wright Jr. 0000-0001-6756-6365 whorton@usgs.gov","orcid":"https://orcid.org/0000-0001-6756-6365","contributorId":423,"corporation":false,"usgs":true,"family":"Horton","given":"J. Wright","suffix":"Jr.","email":"whorton@usgs.gov","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":false,"id":285705,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Powars, David S. 0000-0002-6787-8964 dspowars@usgs.gov","orcid":"https://orcid.org/0000-0002-6787-8964","contributorId":1181,"corporation":false,"usgs":true,"family":"Powars","given":"David","email":"dspowars@usgs.gov","middleInitial":"S.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":285706,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schindler, J. Stephen 0000-0001-9550-5957 sschindl@usgs.gov","orcid":"https://orcid.org/0000-0001-9550-5957","contributorId":3270,"corporation":false,"usgs":true,"family":"Schindler","given":"J.","email":"sschindl@usgs.gov","middleInitial":"Stephen","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":285707,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72469,"text":"gip19 - 2005 - Living with a volcano in your backyard: An educator's guide with emphasis on Mount Rainier","interactions":[],"lastModifiedDate":"2019-05-01T11:33:41","indexId":"gip19","displayToPublicDate":"2005-10-13T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":315,"text":"General Information Product","code":"GIP","onlineIssn":"2332-354X","printIssn":"2332-3531","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"19","title":"Living with a volcano in your backyard: An educator's guide with emphasis on Mount Rainier","docAbstract":"<p>Today&rsquo;s residents, as well as residents of centuries past, consider Mount Rainier &ldquo;the spiritual and cultural icon of the Pacific Northwest.&rdquo; As a backdrop for many of the State&rsquo;s residents, Mount Rainier offers beauty, solace, inspiration, and challenge. The mountain sets the daily mood for thousands of people who gaze at and respect it. There is no mistaking this object of admiration when people smile and remark that, &ldquo;the mountain is out!&rdquo;</p>\n<p>&nbsp;</p>\n<p>Yet, the origin of Mount Rainier, formed by volcanic processes and now heavily laden with snow and ice, remains an enigma to many admirers. During the 1980s, volcanologists from around the world voted Mount Rainier as one of 17 volcanoes most worthy of additional study because of the hazard potential to large population centers nearby. Subsequent research indicates that Mount Rainier, though quiet since the nineteenth century, is very much an &ldquo;active volcano&rdquo; with potential to erupt again and disrupt the life of Pacific Northwest residents. Following days to months or more of warning, Mount Rainier could erupt lava and ash and melt snow and ice to form lahars (volcanic mudflows). Or, Mount Rainier could simply warm up briefly, jolt us from our apathy, and then return to slumber for many more years.</p>\n<p>&nbsp;</p>\n<p>Until such time, the mountain is ours to explore. Living with a Volcano in Your Backyard&mdash;An Educator&rsquo;s Guide with Emphasis on Mount Rainier invites educators and their students to learn what scientists are discovering about Mount Rainier&rsquo;s past, to explore its slopes during this period of quiescence, and to plan future responses to volcanic unrest. Mount Rainier National Park is a unique classroom, rich in resources for observing geologic change. The park staff encourages safe and knowledgeable use by educators and students and their families.</p>\n<p>&nbsp;</p>\n<p>The National Park Service and the U.S. Geological Survey&rsquo;s Volcano Hazards Program (USGS-VHP) support development and publication of this educator&rsquo;s guide as part of their mission to educate the public about volcanoes. The USGS-VHP studies the dynamics of volcanoes, investigates eruption histories, develops hazard assessments, monitors volcano-related activity, and collaborates with local officials to lower the risk of disruption when volcanoes become restless.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/gip19","usgsCitation":"Driedger, C.L., Doherty, A., Dixon, C., and Faust, L.M., 2005, Living with a volcano in your backyard: An educator's guide with emphasis on Mount Rainier (Originally posted 2005; Version 2.0: December 10, 2014): U.S. Geological Survey General Information Product 19, iii, 722 p., https://doi.org/10.3133/gip19.","productDescription":"iii, 722 p.","numberOfPages":"729","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":296587,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/19/downloads/gip19.pdf","size":"43.6 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":296588,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/gip19.gif"},{"id":296586,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/gip/19/"}],"country":"United States","state":"Washington","otherGeospatial":"Mount Rainier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121.91940307617188,\n              46.67394106549699\n            ],\n            [\n              -121.453857421875,\n              46.67394106549699\n            ],\n            [\n              -121.453857421875,\n              46.98587362966405\n            ],\n            [\n              -121.91940307617188,\n              46.98587362966405\n            ],\n            [\n              -121.91940307617188,\n              46.67394106549699\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Originally posted 2005; Version 2.0: December 10, 2014","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b124","contributors":{"authors":[{"text":"Driedger, Carolyn L. 0000-0002-4011-4112 driedger@usgs.gov","orcid":"https://orcid.org/0000-0002-4011-4112","contributorId":537,"corporation":false,"usgs":true,"family":"Driedger","given":"Carolyn","email":"driedger@usgs.gov","middleInitial":"L.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":285702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doherty, Anne","contributorId":23238,"corporation":false,"usgs":true,"family":"Doherty","given":"Anne","email":"","affiliations":[],"preferred":false,"id":285703,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dixon, Cheryl","contributorId":91948,"corporation":false,"usgs":true,"family":"Dixon","given":"Cheryl","email":"","affiliations":[],"preferred":false,"id":285704,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Faust, Lisa M. 0000-0001-6175-8999 lisaf@usgs.gov","orcid":"https://orcid.org/0000-0001-6175-8999","contributorId":5131,"corporation":false,"usgs":true,"family":"Faust","given":"Lisa","email":"lisaf@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":526926,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72466,"text":"fs20053047 - 2005 - USGS activities in the Lake Tahoe Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:14:01","indexId":"fs20053047","displayToPublicDate":"2005-10-12T00:00:00","publicationYear":"2005","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":"2005-3047","title":"USGS activities in the Lake Tahoe Basin","language":"ENGLISH","doi":"10.3133/fs20053047","usgsCitation":"Rowe, T.G., Halsing, D., Raines, G.L., Thacker, A.M., and Watermolen, S.C., 2005, USGS activities in the Lake Tahoe Basin: U.S. Geological Survey Fact Sheet 2005-3047, 2 p., https://doi.org/10.3133/fs20053047.","productDescription":"2 p.","costCenters":[],"links":[{"id":7495,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs20053047/","linkFileType":{"id":5,"text":"html"}},{"id":120888,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3047.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61107c","contributors":{"authors":[{"text":"Rowe, Timothy G.","contributorId":8455,"corporation":false,"usgs":true,"family":"Rowe","given":"Timothy","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":285698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Halsing, David","contributorId":75587,"corporation":false,"usgs":true,"family":"Halsing","given":"David","affiliations":[],"preferred":false,"id":285700,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Raines, Gary L.","contributorId":48162,"corporation":false,"usgs":true,"family":"Raines","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":285699,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thacker, Angelia M.","contributorId":96368,"corporation":false,"usgs":true,"family":"Thacker","given":"Angelia","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":285701,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Watermolen, Shannon C. scwaterm@usgs.gov","contributorId":3239,"corporation":false,"usgs":true,"family":"Watermolen","given":"Shannon","email":"scwaterm@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":285697,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72465,"text":"ds137 - 2005 - Geologic map of the Wenatchee 1:100,000 quadrangle, central Washington: A digital database","interactions":[],"lastModifiedDate":"2022-07-11T19:32:27.803531","indexId":"ds137","displayToPublicDate":"2005-10-12T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":310,"text":"Data Series","code":"DS","onlineIssn":"2327-638X","printIssn":"2327-0271","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"137","title":"Geologic map of the Wenatchee 1:100,000 quadrangle, central Washington: A digital database","docAbstract":"This digital map database has been prepared by R.W. Tabor from the published Geologic map of the Wenatchee 1:100,000 Quadrangle, Central Washington. Together with the accompanying text files as PDF, it provides information on the geologic structure and stratigraphy of the area covered. The database delineates map units that are identified by general age and lithology following the stratigraphic nomenclature of the U.S. Geological Survey. The authors mapped most of the bedrock geology at 1:100,000 scale, but compiled Quaternary units at 1:24,000 scale. The Quaternary contacts and structural data have been much simplified for the 1:100,000-scale map and database. The spatial resolution (scale) of the database is 1:100,000 or smaller. \r\n\r\nThis database depicts the distribution of geologic materials and structures at a regional (1:100,000) scale. The report is intended to provide geologic information for the regional study of materials properties, earthquake shaking, landslide potential, mineral hazards, seismic velocity, and earthquake faults. In addition, the report contains information and interpretations about the regional geologic history and framework. However, the regional scale of this report does not provide sufficient detail for site development purposes.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ds137","usgsCitation":"Tabor, R.W., Waitt, R., Frizzell, V.A., Swanson, D.A., Byerly, G.R., and Bentley, R.D., 2005, Geologic map of the Wenatchee 1:100,000 quadrangle, central Washington: A digital database (Version 1.0): U.S. Geological Survey Data Series 137, HTML Document, https://doi.org/10.3133/ds137.","productDescription":"HTML Document","costCenters":[],"links":[{"id":193165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403430,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73770.htm","linkFileType":{"id":5,"text":"html"}},{"id":7494,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/137/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Washington","otherGeospatial":"Wenatchee quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -121,\n              47\n            ],\n            [\n              -120,\n              47\n            ],\n            [\n              -120,\n              47.5\n            ],\n            [\n              -121,\n              47.5\n            ],\n            [\n              -121,\n              47\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a80ce","contributors":{"authors":[{"text":"Tabor, R. W.","contributorId":16002,"corporation":false,"usgs":true,"family":"Tabor","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":285692,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waitt, R. B.","contributorId":78766,"corporation":false,"usgs":true,"family":"Waitt","given":"R. B.","affiliations":[],"preferred":false,"id":285695,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frizzell, V. A. Jr.","contributorId":39376,"corporation":false,"usgs":true,"family":"Frizzell","given":"V.","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285694,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swanson, D. A.","contributorId":34102,"corporation":false,"usgs":true,"family":"Swanson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285693,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Byerly, G. R.","contributorId":6826,"corporation":false,"usgs":true,"family":"Byerly","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285691,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bentley, R. D.","contributorId":85561,"corporation":false,"usgs":true,"family":"Bentley","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":285696,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70205941,"text":"70205941 - 2005 - Late Devonian Alamo Impact, southern Nevada, USA: Evidence of size, marine site, and widespread effects","interactions":[],"lastModifiedDate":"2020-05-26T12:41:46.564191","indexId":"70205941","displayToPublicDate":"2005-10-10T14:42:23","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3459,"text":"Special Paper of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Late Devonian Alamo Impact, southern Nevada, USA: Evidence of size, marine site, and widespread effects","docAbstract":"<p><span>The early Late Devonian (early Frasnian) Alamo Impact targeted an oceanic, off-platform site in southern Nevada, excavating a crater with a final diameter of 44–65 km. The original crater is now dismembered and buried beneath younger rocks. Consequently, its size and site must be deduced through multiple converging lines of geological and paleontological evidence. Previous and new evidence includes the catastrophically emplaced Alamo Breccia, tsunamites, shock-metamorphosed quartz grains, carbonate accretionary lapilli, an iridium anomaly, sub-Breccia clastic injection, deep-water Breccia channels, and ejecta material. We now demonstrate, on the basis of conodont microfossils in carbonate ejecta clasts within lapillistone blocks and widely distributed shocked-quartz and lithic-clast ejecta within the upper part of the Breccia, that the Alamo Impact excavated down at least into Upper Cambrian strata, at a depth of 1.7 km, and possibly into the underlying Proterozoic–Lower Cambrian Prospect Mountain Quartzite, ∼2.5 km beneath the Late Devonian seafloor. Distal tsunamites and probable ejecta are now documented as far north as Devils Gate, northern Nevada, and as far northeast as the Confusion Range, western Utah. A charcoal-bearing, early Frasnian estuarine deposit in the Bighorn Mountains, Wyoming, may provide the first evidence of an Alamo Impact fallout-generated forest fire. Our new data further document the widespread effects and size of the Alamo Impact, and constrain the likely present position of the tectonically transported crater to an area between the Timpahute and Hot Creek Ranges, southern Nevada.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0-8137-2384-1.259","usgsCitation":"Morrow, J.R., Sandberg, C., and Harris, A.G., 2005, Late Devonian Alamo Impact, southern Nevada, USA: Evidence of size, marine site, and widespread effects: Special Paper of the Geological Society of America, p. 259-280, https://doi.org/10.1130/0-8137-2384-1.259.","productDescription":"22 p.","startPage":"259","endPage":"280","costCenters":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"links":[{"id":368244,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.257080078125,\n              37.1165261849112\n            ],\n            [\n              -114.63134765625001,\n              37.1165261849112\n            ],\n            [\n              -114.63134765625001,\n              40.12849105685408\n            ],\n            [\n              -117.257080078125,\n              40.12849105685408\n            ],\n            [\n              -117.257080078125,\n              37.1165261849112\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Morrow, Jared R.","contributorId":65934,"corporation":false,"usgs":true,"family":"Morrow","given":"Jared","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":772998,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sandberg, Charles sandberg@usgs.gov","contributorId":199124,"corporation":false,"usgs":true,"family":"Sandberg","given":"Charles","email":"sandberg@usgs.gov","affiliations":[{"id":35995,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":772999,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harris, Anita G.","contributorId":50162,"corporation":false,"usgs":true,"family":"Harris","given":"Anita","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":773000,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72435,"text":"sir20055079 - 2005 - Feasibility of using benthic invertebrates as indicators of stream quality in Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055079","displayToPublicDate":"2005-10-09T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5079","title":"Feasibility of using benthic invertebrates as indicators of stream quality in Hawaii","docAbstract":"Macroinvertebrates were collected from 19 sites on 14 streams on the island of Oahu and from 9 sites on 7 streams on the island of Kauai to evaluate associations between macroinvertebrate assemblages and environmental variables and to determine whether or not it would be feasible, in future studies, to develop macroinvertebrate metrics that would indicate stream quality based on the macroinvertebrate assemblages and/or components of the assemblages. The purpose of applying rapid bioassessment techniques is to identify stream quality problems and to document changes in stream quality. Samples were collected at 10 sites in 1999, 3 sites in 2000, and 5 sites in 2003 on Oahu and at 9 sites on Kauai in 2003. Additionally, multiple year and multiple reach samples were collected at 1 site on Oahu. Macroinvertebrates were collected primarily from boulder/cobble riffles or from the fastest flowing habitat when riffles were absent. Although most streams in Hawaii originate in mountainous, forested areas, the lower reaches often drain urban, agricultural, or mixed land-use areas. The macroinvertebrate community data were used to identify metrics that could best differentiate between sites according to levels of environmental impairment. Environmental assessments were conducted using land-use/land-cover data, bed-sediment and fish-tissue contaminant data, and reach-level environmental data using a calibration set of 15 sites. The final scores of the environmental assessments were used to classify the sites into three categories of impairment: mild, moderate or severe. A number of invertebrate metrics were then tested and calibrated to the environmental assessments scores. The individual metrics that were the best at discerning environmental assessments among the sites were combined into a multimetric benthic index of biotic integrity (BIBI). These metrics were: total invertebrate abundance, taxa richness, insect relative abundance, amphipod abundance, crayfish presence or absence, and native mountain shrimp presence or absence. Because this index is in the preliminary stage of development and additional 'pristine' sites need to be sampled and assessed to develop a more robust measure of biotic integrity, the index will be referred to as a Preliminary Hawaiian Benthic Index of Biotic Integrity (P-HBIBI). The P-HBIBI scores were then classified into three categories of impairment: mild, moderate, or severe. The P-HBIBI was then used to assess the remaining sites and classify them into impairment categories. The P-HBIBI was correlated (r2 = 0.72; p < 0.005) with a reduced environmental assessment determined without contaminants data. The results of this study suggest that the development of a reliable Hawaiian benthic index of biotic integrity (HBIBI), based on macroinvertebrate assemblages, is feasible; however, a much larger sample size, including more samples from 'pristine' sites and from the other islands, would be required.","language":"ENGLISH","doi":"10.3133/sir20055079","usgsCitation":"Wolff, R.H., 2005, Feasibility of using benthic invertebrates as indicators of stream quality in Hawaii: U.S. Geological Survey Scientific Investigations Report 2005-5079, viii, 78 p. : ill., https://doi.org/10.3133/sir20055079.","productDescription":"viii, 78 p. : ill.","costCenters":[],"links":[{"id":191878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7456,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5079/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4823e4b07f02db4e2402","contributors":{"authors":[{"text":"Wolff, Reuben H.","contributorId":35020,"corporation":false,"usgs":true,"family":"Wolff","given":"Reuben","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":285647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72436,"text":"ofr20051053 - 2005 - Water-quality data from two agricultural drainage basins in northwestern Indiana and northeastern Illinois: II. diel data, 1999-2001","interactions":[],"lastModifiedDate":"2021-01-15T22:13:30.672116","indexId":"ofr20051053","displayToPublicDate":"2005-10-09T00:00:00","publicationYear":"2005","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":"2005-1053","title":"Water-quality data from two agricultural drainage basins in northwestern Indiana and northeastern Illinois: II. diel data, 1999-2001","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051053","usgsCitation":"Antweiler, R.C., Smith, R.L., Voytek, M.A., and Bohlke, J., 2005, Water-quality data from two agricultural drainage basins in northwestern Indiana and northeastern Illinois: II. diel data, 1999-2001: U.S. Geological Survey Open-File Report 2005-1053, 124 p., https://doi.org/10.3133/ofr20051053.","productDescription":"124 p.","costCenters":[{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":191933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":382243,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1053/"},{"id":382171,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1053/pdf/OFR%2020051053.pdf"}],"country":"United States","state":"Indiana, Illinois","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.5,40.666666666666664 ], [ -87.5,40.833333333333336 ], [ -87.41666666666667,40.833333333333336 ], [ -87.41666666666667,40.666666666666664 ], [ -87.5,40.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e57c9","contributors":{"authors":[{"text":"Antweiler, Ronald C. 0000-0001-5652-6034 antweil@usgs.gov","orcid":"https://orcid.org/0000-0001-5652-6034","contributorId":1481,"corporation":false,"usgs":true,"family":"Antweiler","given":"Ronald","email":"antweil@usgs.gov","middleInitial":"C.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":285648,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Richard L. 0000-0002-3829-0125 rlsmith@usgs.gov","orcid":"https://orcid.org/0000-0002-3829-0125","contributorId":1592,"corporation":false,"usgs":true,"family":"Smith","given":"Richard","email":"rlsmith@usgs.gov","middleInitial":"L.","affiliations":[{"id":38175,"text":"Toxics Substances Hydrology Program","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true},{"id":36183,"text":"Hydro-Ecological Interactions Branch","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":285649,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Voytek, Mary A.","contributorId":91943,"corporation":false,"usgs":true,"family":"Voytek","given":"Mary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285651,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bohlke, John Karl 0000-0001-5693-6455","orcid":"https://orcid.org/0000-0001-5693-6455","contributorId":66293,"corporation":false,"usgs":true,"family":"Bohlke","given":"John Karl","affiliations":[],"preferred":false,"id":285650,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72434,"text":"sim2905 - 2005 - Ground-water levels in the Spokane valley - Rathdrum Prairie aquifer, Spokane County, Washington, and Bonner and Kootenai Counties, Idaho, September 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sim2905","displayToPublicDate":"2005-10-09T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":333,"text":"Scientific Investigations Map","code":"SIM","onlineIssn":"2329-132X","printIssn":"2329-1311","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2905","title":"Ground-water levels in the Spokane valley - Rathdrum Prairie aquifer, Spokane County, Washington, and Bonner and Kootenai Counties, Idaho, September 2004","language":"ENGLISH","doi":"10.3133/sim2905","usgsCitation":"Campbell, A.M., 2005, Ground-water levels in the Spokane valley - Rathdrum Prairie aquifer, Spokane County, Washington, and Bonner and Kootenai Counties, Idaho, September 2004 (Online only): U.S. Geological Survey Scientific Investigations Map 2905, 1 sheet, 41 x 29 in., https://doi.org/10.3133/sim2905.","productDescription":"1 sheet, 41 x 29 in.","onlineOnly":"Y","costCenters":[],"links":[{"id":191877,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7455,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2905/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675d9","contributors":{"authors":[{"text":"Campbell, Annette M. annettec@usgs.gov","contributorId":3933,"corporation":false,"usgs":true,"family":"Campbell","given":"Annette","email":"annettec@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":285646,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70205872,"text":"70205872 - 2005 - Remote sensing of coastal environments","interactions":[],"lastModifiedDate":"2019-10-09T07:11:38","indexId":"70205872","displayToPublicDate":"2005-10-08T18:37:24","publicationYear":"2005","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Remote sensing of coastal environments","docAbstract":"<p><span>Coastal ecosystems are transitional environments that are sensitively balanced between open water and upland landscapes. Worldwide, they exhibit extreme variations in areal extent, spatial complexity, and temporal variability. Sustaining these ecosystems requires the ability to monitor their biophysical features and controlling processes at high spatial and temporal resolutions but within a holistic context. Remote sensing is the only tool that can economically measure these features and processes over large areas at appropriate resolutions. Consequently, it offers the only holistic approach to understanding the variable forces shaping the dynamic coastal landscape. Remote sensing must be able to adjust to these spatially and temporally changing conditions and also be able to discriminate subtle differences in these systems. As a result, remote sensing of coastal ecosystems is a complex undertaking that needs to incorporate not only the ability to define the observable hydrologic and vegetation features, but also the scale of measurement.</span></p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Encyclopedia of Coastal Science","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Springer","doi":"10.1007/1-4020-3880-1_257","usgsCitation":"Ramsey III, E., 2005, Remote sensing of coastal environments, chap. <i>of</i> Encyclopedia of Coastal Science, p. 797-804, https://doi.org/10.1007/1-4020-3880-1_257.","productDescription":"8 p.","startPage":"797","endPage":"804","costCenters":[{"id":455,"text":"National Wetlands Research Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"links":[{"id":368139,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ramsey III, Elijah 0000-0002-4518-5796","orcid":"https://orcid.org/0000-0002-4518-5796","contributorId":212009,"corporation":false,"usgs":true,"family":"Ramsey III","given":"Elijah","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":772740,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70205865,"text":"70205865 - 2005 - National Acid Precipitation Assessment Program Report to Congress: An integrated assessment","interactions":[{"subject":{"id":70205862,"text":"70205862 - 2005 - Results of the acid rain program: Status and trends of emissions and environmental impacts (1990–2002)","indexId":"70205862","publicationYear":"2005","noYear":false,"chapter":"2","title":"Results of the acid rain program: Status and trends of emissions and environmental impacts (1990–2002)"},"predicate":"IS_PART_OF","object":{"id":70205865,"text":"70205865 - 2005 - National Acid Precipitation Assessment Program Report to Congress: An integrated assessment","indexId":"70205865","publicationYear":"2005","noYear":false,"title":"National Acid Precipitation Assessment Program Report to Congress: An integrated assessment"},"id":1},{"subject":{"id":70205863,"text":"70205863 - 2005 - Assessing acid deposition: Advances in the state of science","indexId":"70205863","publicationYear":"2005","noYear":false,"chapter":"3","title":"Assessing acid deposition: Advances in the state of science"},"predicate":"IS_PART_OF","object":{"id":70205865,"text":"70205865 - 2005 - National Acid Precipitation Assessment Program Report to Congress: An integrated assessment","indexId":"70205865","publicationYear":"2005","noYear":false,"title":"National Acid Precipitation Assessment Program Report to Congress: An integrated assessment"},"id":2}],"lastModifiedDate":"2019-10-09T07:15:17","indexId":"70205865","displayToPublicDate":"2005-10-08T16:27:32","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":5871,"text":"Report to Congress","active":true,"publicationSubtype":{"id":1}},"title":"National Acid Precipitation Assessment Program Report to Congress: An integrated assessment","docAbstract":"<p>Acid deposition, more commonly known as acid rain,&nbsp;occurs when emissions of sulfur dioxide (SO2) and nitrogen&nbsp;oxides (NOx) react in the atmosphere (with water, oxygen,&nbsp;and oxidants) to form various acidic compounds. These&nbsp;acidic compounds then fall to earth in either a wet form&nbsp;(rain, snow, and fog) or a dry form (gases, aerosols, and&nbsp;particles). Prevailing winds transport the acidic compounds&nbsp;hundreds of miles, often across state and national borders.&nbsp;At certain levels the acidic compounds, including small particles such as sulfates and nitrates can cause many negative&nbsp;human health and environmental effects. While ecosystems&nbsp;are subject to many stresses, including land-use changes,&nbsp;climate change, and variations in hydrologic and meteorologic cycles, the scientific literature has clearly demonstrated&nbsp;that these pollutants can:<br>• Degrade air quality,<br>• Impair visibility,<br>• Damage public health,<br>• Acidify lakes and streams,<br>• Harm sensitive forests,<br>• Harm sensitive coastal ecosystems, and<br>• Accelerate the decay of building materials, paints, and&nbsp;cultural artifacts such as buildings, statues, and&nbsp;sculptures.<br></p><p>Title IV was passed by Congress as part of the 1990 Clean&nbsp;Air Act Amendments to reduce emissions of SO<sub>2</sub> and NO<sub>x&nbsp;</sub>from fossil fuel-burning power plants in order to protect<br>ecosystems suffering damage from acid deposition and to&nbsp;improve air quality. At the same time, the National Acid&nbsp;Precipitation Assessment Program (NAPAP) was asked to&nbsp;periodically assess and report to Congress on the&nbsp;implementation of the Acid Rain Program, recent scientific&nbsp;knowledge surrounding acid deposition and its effects, and<br>the reduction in acid deposition necessary to prevent&nbsp;adverse ecological effects. This NAPAP Report focuses primarily on emission reductions from power plants, both in&nbsp;terms of assessing past reductions under the Acid Rain&nbsp;Program and in projecting the ecological effects of additional reductions of SO<sub>2</sub> and NO<sub>x</sub>. </p><p>It should be noted that power generation&nbsp;currently contributes approximately 69% of&nbsp;the SO<sub>2</sub> emissions and 22% of the NO<sub>x</sub> emissions nationwide. This contribution is&nbsp;decreasing as emissions from power generation continue to decrease, making the other&nbsp;sources of these pollutants more prominent.&nbsp;Modeling suggests that even if SO<sub>2</sub><br>emissions from power generation were&nbsp;reduced to zero, some lakes and streams&nbsp;would remain acidic due to acid deposition.&nbsp;However, there are several other regulations&nbsp;that reduce emissions of SO<sub>2</sub> and NO<sub>x</sub> from&nbsp;these non-power generation sources, such&nbsp;as the Tier II mobile source standards, the&nbsp;Heavy Duty Diesel standards, and the Clean&nbsp;Air Non-Road Diesel Rule, that have also&nbsp;been promulgated since 1990. These regulations, primarily designed to bring counties&nbsp;into attainment with fine particle and ozone&nbsp;air quality standards, also incidentally reduce&nbsp;emissions that contribute to acid deposition.</p><p>Implementation of Title IV has successfully&nbsp;and substantially reduced emissions of SO<sub>2&nbsp;</sub>and NO<sub>x</sub> from power generation at a significantly lower cost than expected:<br>• In 2002, SO<sub>2</sub> emissions were 10.2 million&nbsp;tons, 35% lower than 1990 emissions and&nbsp;40% lower than 1980 emissions.*<br>• In 2002, NO<sub>x</sub> emissions were 4.5 million&nbsp;tons, 33% lower than 1990 emissions.<br></p><p>In addition, SO<sub>2</sub> emissions from all sources&nbsp;have decreased by 32% since 1990 and&nbsp;emissions of NO<sub>x</sub> from all sources have&nbsp;decreased by 12% since 1990. Power generating sources continue to close in on the&nbsp;goal of reducing power plant SO<sub>2</sub> emissions&nbsp;from 1980 levels by 50% (to 8.95 million&nbsp;tons) as required by the 1990 Clean Air Act.&nbsp;Power generating sources have also exceed­ed the goal of a two million ton reduction in&nbsp;NO<sub>x</sub> emissions from projected 2000 levels&nbsp;as required by the 1990 Clean Air Act.<br></p><p>These emission reductions have contributed&nbsp;to measurable improvements in air quality,&nbsp;reductions in acid deposition, and the beginnings of recovery of acid-sensitive waters in&nbsp;some areas:<br>• SO2 concentrations in the atmosphere (a&nbsp;precursor to fine particles and acid deposition) have decreased since 1990. Average&nbsp;annual SO2 concentrations in the&nbsp;Northeast in 2000–2002 were 40% lower&nbsp;than they were in 1989–1991, concentrations in the mid-Atlantic were 30% lower,&nbsp;concentrations in the Southeast were 35%&nbsp;lower, and concentrations in the Midwest&nbsp;were 45% lower.<br>• Sulfate concentrations in the atmosphere (a major component of fine particles, especially in the East) have&nbsp;decreased since 1990 as well. Average&nbsp;annual sulfate concentrations in the&nbsp;Northeast and Midwest in 2000–2002&nbsp;were approximately 30% lower than they were in&nbsp;1989–1991, and concentrations in the mid-Atlantic and&nbsp;Southeast were 25% lower.<br>• Wet sulfate deposition, a major component of acid rain,&nbsp;has also decreased since 1990. Average annual sulfate&nbsp;deposition in the Northeast in 2000–2002 was 40% lower&nbsp;than it was in 1989–1991, deposition in the mid-Atlantic&nbsp;and Midwest was 35% lower, and deposition in the&nbsp;Southeast was 25% lower.<br>• Wet nitrate deposition has not decreased regionally from&nbsp;historical levels because of the relatively moderate NO<sub>x</sub>&nbsp;reduction from power plants and the continuing large contribution (over 50% of total NOx emissions) from other&nbsp;sources of NO<sub>x</sub> such as vehicles and nonroad vehicles.<br>• Although visibility has begun to improve in some parts&nbsp;of the U.S., there is still significant impairment of visibility in many national parks and other Class I areas&nbsp;throughout the U.S.<br>• Acid neutralizing capacity is beginning to rise in some&nbsp;surface waters in the Northeast, including lakes in the&nbsp;Adirondack Mountains (see graphic below). This is an&nbsp;indication that recovery from acidification is occurring in&nbsp;those areas.&nbsp;<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"NOAA","usgsCitation":"2005, National Acid Precipitation Assessment Program Report to Congress: An integrated assessment: Report to Congress, 85 p.","productDescription":"85 p.","costCenters":[{"id":466,"text":"New England Water Science Center","active":true,"usgs":true}],"links":[{"id":368131,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":368130,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://www.esrl.noaa.gov/csd/aqrsd/reports/napapreport05.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Burtraw, Dallas","contributorId":219624,"corporation":false,"usgs":false,"family":"Burtraw","given":"Dallas","email":"","affiliations":[],"preferred":false,"id":772705,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"Butler, Thomas","contributorId":219625,"corporation":false,"usgs":false,"family":"Butler","given":"Thomas","email":"","affiliations":[],"preferred":false,"id":772706,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Colburn, Kenneth","contributorId":219626,"corporation":false,"usgs":false,"family":"Colburn","given":"Kenneth","email":"","affiliations":[],"preferred":false,"id":772707,"contributorType":{"id":2,"text":"Editors"},"rank":3},{"text":"Driscoll, C.","contributorId":28784,"corporation":false,"usgs":true,"family":"Driscoll","given":"C.","affiliations":[],"preferred":false,"id":772708,"contributorType":{"id":2,"text":"Editors"},"rank":4},{"text":"Grigal, David","contributorId":219627,"corporation":false,"usgs":false,"family":"Grigal","given":"David","email":"","affiliations":[],"preferred":false,"id":772709,"contributorType":{"id":2,"text":"Editors"},"rank":5}]}}
,{"id":72427,"text":"fs20053088 - 2005 - Pesticides in ground water - Hot Springs County, Wyoming, 2003-04","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"fs20053088","displayToPublicDate":"2005-10-06T00:00:00","publicationYear":"2005","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":"2005-3088","title":"Pesticides in ground water - Hot Springs County, Wyoming, 2003-04","language":"ENGLISH","doi":"10.3133/fs20053088","usgsCitation":"Eddy-Miller, C., and Remley, K., 2005, Pesticides in ground water - Hot Springs County, Wyoming, 2003-04: U.S. Geological Survey Fact Sheet 2005-3088, 4 p., https://doi.org/10.3133/fs20053088.","productDescription":"4 p.","costCenters":[],"links":[{"id":121015,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3088.jpg"},{"id":7449,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3088/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688274","contributors":{"authors":[{"text":"Eddy-Miller, Cheryl A.","contributorId":86755,"corporation":false,"usgs":true,"family":"Eddy-Miller","given":"Cheryl A.","affiliations":[],"preferred":false,"id":285635,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Remley, Kendra J.","contributorId":26753,"corporation":false,"usgs":true,"family":"Remley","given":"Kendra J.","affiliations":[],"preferred":false,"id":285634,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72431,"text":"ofr20051321 - 2005 - Mercury concentrations in fishes from select water bodies in Trinity County, California, 2000-2002","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"ofr20051321","displayToPublicDate":"2005-10-06T00:00:00","publicationYear":"2005","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":"2005-1321","title":"Mercury concentrations in fishes from select water bodies in Trinity County, California, 2000-2002","language":"ENGLISH","doi":"10.3133/ofr20051321","usgsCitation":"May, J., Hothem, R.L., and Alpers, C.N., 2005, Mercury concentrations in fishes from select water bodies in Trinity County, California, 2000-2002 (Online only): U.S. Geological Survey Open-File Report 2005-1321, 22 p. : ill., https://doi.org/10.3133/ofr20051321.","productDescription":"22 p. : ill.","onlineOnly":"Y","costCenters":[],"links":[{"id":7453,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1321/","linkFileType":{"id":5,"text":"html"}},{"id":191875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624b79","contributors":{"authors":[{"text":"May, Jason T. 0000-0002-5699-2112","orcid":"https://orcid.org/0000-0002-5699-2112","contributorId":14791,"corporation":false,"usgs":true,"family":"May","given":"Jason T.","affiliations":[],"preferred":false,"id":285643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hothem, Roger L. roger_hothem@usgs.gov","contributorId":1721,"corporation":false,"usgs":true,"family":"Hothem","given":"Roger","email":"roger_hothem@usgs.gov","middleInitial":"L.","affiliations":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"preferred":true,"id":285642,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alpers, Charles N. 0000-0001-6945-7365 cnalpers@usgs.gov","orcid":"https://orcid.org/0000-0001-6945-7365","contributorId":411,"corporation":false,"usgs":true,"family":"Alpers","given":"Charles","email":"cnalpers@usgs.gov","middleInitial":"N.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285641,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72430,"text":"sir20055052 - 2005 - Hydrology and water quality of lakes and streams in Orange County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055052","displayToPublicDate":"2005-10-06T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5052","title":"Hydrology and water quality of lakes and streams in Orange County, Florida","docAbstract":"Orange County, Florida, is continuing to experience a large growth in population. In 1920, the population of Orange County was less than 20,000; in 2000, the population was about 896,000. The amount of urban area around Orlando has increased considerably, especially in the northwest part of the County. The eastern one-third of the County, however, had relatively little increase in urbanization from 1977-97. The increase of population, tourism, and industry in Orange County and nearby areas changed land use; land that was once agricultural has become urban, industrial, and major recreation areas. These changes could impact surface-water resources that are important for wildlife habitat, for esthetic reasons, and potentially for public supply. Streamflow characteristics and water quality could be affected in various ways.\r\n\r\nAs a result of changing land use, changes in the hydrology and water quality of Orange County's lakes and streams could occur. Median runoff in 10 selected Orange County streams ranges from about 20 inches per year (in/yr) in the Wekiva River to about 1.1 in/yr in Cypress Creek. The runoff for the Wekiva River is significantly higher than other river basins because of the relatively constant spring discharge that sustains streamflow, even during drought conditions. The low runoff for the Cypress Creek basin results from a lack of sustained inflow from ground water and a relatively large area of lakes within the drainage basin.\r\n\r\nStreamflow characteristics for 13 stations were computed on an annual basis and examined for temporal trends. Results of the trend testing indicate changes in annual mean streamflow, 1-day high streamflow, or 7-day low streamflow at 8 of the 13 stations. However, changes in 7-day low streamflow are more common than changes in annual mean or 1-day high streamflow.\r\n\r\nThere is probably no single reason for the changes in 7-day low streamflows, and for most streams, it is difficult to determine definite reasons for the flow increases. Low flows in the Econlockhatchee River at Chuluota have increased because of discharge of treated wastewater since 1982. However, trends in increasing 7-day low streamflow are evident before 1982, which cannot be attributed to wastewater discharge.\r\n\r\nSome of the increases in 7-day low flows may be related to drainage changes resulting from increased development in Orange County. Development for most purposes, including those as diverse as cattle grazing and residential construction, may involve modification of surface drainage through stream channelization and construction of canals. These changes in land drainage can lower the water table, resulting in reductions of regional evapotranspiration rates and increased streamflow. Another possible cause of increasing low flows in streams is use of water from the Floridan aquifer system for irrigation. Runoff of irrigation water or increased seepage from irrigated areas to streams could increase base streamflow compared to natural conditions.\r\n\r\nWater-level data were analyzed to determine temporal trends from 83 lakes that had more than 15 years of record. There were significant temporal trends in 33 of the 83 lakes (40 percent) over the entire period of record. Of these 33 lakes, 14 had increasing water levels and 19 lakes had decreasing water levels. The downward trends in long-term lake levels could in part be due to high rainfall accumulation in 1960-1961, which included precipitation from Hurricane Donna (September 1960). The high rainfall resulted in historical high-water levels in many lakes in 1960 or 1961.\r\n\r\nA large range of water-quality conditions exists in lakes and streams of Orange County (2000-01). Specific conductance in lake samples ranged from 57 to 1,185 microsiemens per centimeter. Values of pH ranged from 3.2 to 8.7 in stream samples and 4.6 to 9.6 in lake samples. Total nitrogen concentrations ranged from less than 0.2 to 7.1 milligrams per liter (mg/L) as nitrogen in stream samples, and","language":"ENGLISH","doi":"10.3133/sir20055052","usgsCitation":"German, E.R., and Adamski, J.C., 2005, Hydrology and water quality of lakes and streams in Orange County, Florida: U.S. Geological Survey Scientific Investigations Report 2005-5052, 109 p. : ill.; maps, https://doi.org/10.3133/sir20055052.","productDescription":"109 p. : ill.; maps","costCenters":[],"links":[{"id":191874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7452,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5052/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604c05","contributors":{"authors":[{"text":"German, Edward R.","contributorId":85567,"corporation":false,"usgs":true,"family":"German","given":"Edward","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285640,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adamski, James C.","contributorId":20316,"corporation":false,"usgs":true,"family":"Adamski","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285639,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72432,"text":"i2802 - 2005 - Geologic map of the Van Buren North quadrangle, Carter, Reynolds, and Shannon Counties, Missouri","interactions":[],"lastModifiedDate":"2012-02-10T00:11:36","indexId":"i2802","displayToPublicDate":"2005-10-06T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2802","title":"Geologic map of the Van Buren North quadrangle, Carter, Reynolds, and Shannon Counties, Missouri","language":"ENGLISH","doi":"10.3133/i2802","isbn":"0607975490","usgsCitation":"Weary, D.J., and Weems, R.E., 2005, Geologic map of the Van Buren North quadrangle, Carter, Reynolds, and Shannon Counties, Missouri (Version 1.0): U.S. Geological Survey IMAP 2802, 1 sheet, 60 x 41.75 in.; GIS vector data, https://doi.org/10.3133/i2802.","productDescription":"1 sheet, 60 x 41.75 in.; GIS vector data","costCenters":[],"links":[{"id":110582,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73920.htm","linkFileType":{"id":5,"text":"html"},"description":"73920"},{"id":191876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7454,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2802/","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.11749999999999,37 ], [ -91.11749999999999,37.1175 ], [ -91,37.1175 ], [ -91,37 ], [ -91.11749999999999,37 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a0f2","contributors":{"authors":[{"text":"Weary, David J. 0000-0002-6115-6397 dweary@usgs.gov","orcid":"https://orcid.org/0000-0002-6115-6397","contributorId":545,"corporation":false,"usgs":true,"family":"Weary","given":"David","email":"dweary@usgs.gov","middleInitial":"J.","affiliations":[{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true},{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true}],"preferred":true,"id":285644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weems, Robert E. 0000-0002-1907-7804 rweems@usgs.gov","orcid":"https://orcid.org/0000-0002-1907-7804","contributorId":2663,"corporation":false,"usgs":true,"family":"Weems","given":"Robert","email":"rweems@usgs.gov","middleInitial":"E.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":285645,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72426,"text":"fs20053089 - 2005 - Pesticides in ground water - Converse County, Wyoming, 2003-04","interactions":[],"lastModifiedDate":"2017-09-20T16:45:02","indexId":"fs20053089","displayToPublicDate":"2005-10-06T00:00:00","publicationYear":"2005","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":"2005-3089","title":"Pesticides in ground water - Converse County, Wyoming, 2003-04","language":"ENGLISH","doi":"10.3133/fs20053089","usgsCitation":"Eddy-Miller, C., and Remley, K., 2005, Pesticides in ground water - Converse County, Wyoming, 2003-04: U.S. Geological Survey Fact Sheet 2005-3089, 4 p., https://doi.org/10.3133/fs20053089.","productDescription":"4 p.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":121014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3089.jpg"},{"id":7448,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3089/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68826a","contributors":{"authors":[{"text":"Eddy-Miller, Cheryl A.","contributorId":86755,"corporation":false,"usgs":true,"family":"Eddy-Miller","given":"Cheryl A.","affiliations":[],"preferred":false,"id":285633,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Remley, Kendra J.","contributorId":26753,"corporation":false,"usgs":true,"family":"Remley","given":"Kendra J.","affiliations":[],"preferred":false,"id":285632,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72428,"text":"fs20053087 - 2005 - Pesticides in ground water - Albany County, Wyoming, 2003-04","interactions":[],"lastModifiedDate":"2017-09-20T16:45:01","indexId":"fs20053087","displayToPublicDate":"2005-10-06T00:00:00","publicationYear":"2005","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":"2005-3087","title":"Pesticides in ground water - Albany County, Wyoming, 2003-04","language":"ENGLISH","doi":"10.3133/fs20053087","usgsCitation":"Eddy-Miller, C., and Remley, K., 2005, Pesticides in ground water - Albany County, Wyoming, 2003-04: U.S. Geological Survey Fact Sheet 2005-3087, 4 p., https://doi.org/10.3133/fs20053087.","productDescription":"4 p.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":121016,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3087.jpg"},{"id":7450,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3087/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688261","contributors":{"authors":[{"text":"Eddy-Miller, Cheryl A.","contributorId":86755,"corporation":false,"usgs":true,"family":"Eddy-Miller","given":"Cheryl A.","affiliations":[],"preferred":false,"id":285637,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Remley, Kendra J.","contributorId":26753,"corporation":false,"usgs":true,"family":"Remley","given":"Kendra J.","affiliations":[],"preferred":false,"id":285636,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72429,"text":"ofr20051364 - 2005 - Science within the U.S. Geological Survey Florida Integrated Science Center (FISC): applications, integration, and new opportunities","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"ofr20051364","displayToPublicDate":"2005-10-06T00:00:00","publicationYear":"2005","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":"2005-1364","title":"Science within the U.S. Geological Survey Florida Integrated Science Center (FISC): applications, integration, and new opportunities","language":"ENGLISH","doi":"10.3133/ofr20051364","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, Science within the U.S. Geological Survey Florida Integrated Science Center (FISC): applications, integration, and new opportunities: U.S. Geological Survey Open-File Report 2005-1364, 30 p., https://doi.org/10.3133/ofr20051364.","productDescription":"30 p.","costCenters":[],"links":[{"id":191873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7451,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1364/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd2af","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":534748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72423,"text":"sir20055175 - 2005 - Analysis of ground-water levels and associated trends in Yucca Flat, Nevada Test Site, Nye County, Nevada, 1951-2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055175","displayToPublicDate":"2005-10-05T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5175","title":"Analysis of ground-water levels and associated trends in Yucca Flat, Nevada Test Site, Nye County, Nevada, 1951-2003","docAbstract":"Almost 4,000 water-level measurements in 216 wells in the Yucca Flat area from 1951 to 2003 were quality assured and analyzed. An interpretative database was developed that describes water-level conditions for each water level measured in Yucca Flat. Multiple attributes were assigned to each water-level measurement in the database to describe the hydrologic conditions at the time of measurement. General quality, temporal variability, regional significance, and hydrologic conditions are attributed for each water-level measurement. The database also includes narratives that discuss the water-level history of each well.\r\n\r\nWater levels in 34 wells were analyzed for variability and for statistically significant trends. An attempt was made to identify the cause of many of the water-level fluctuations or trends. Potential causes include equilibration following well construction or development, pumping in the monitoring well, withdrawals from a nearby supply well, recharge from precipitation, earthquakes, underground nuclear tests, land subsidence, barometric pressure, and Earth tides. \r\n\r\nSome of the naturally occurring fluctuations in water levels may result from variations in recharge. The magnitude of the overall water-level change for these fluctuations generally is less than 2 feet. Long-term steady-state hydrographs for most of the wells open to carbonate rock have a very similar pattern. Carbonate-rock wells without the characteristic pattern are directly west of the Yucca and Topgallant faults in the southwestern part of Yucca Flat. Long-term steady-state hydrographs from wells open to volcanic tuffs or the Eleana confining unit have a distinctly different pattern from the general water-level pattern of the carbonate-rock aquifers.\r\n\r\nAnthropogenic water-level fluctuations were caused primarily by water withdrawals and nuclear testing. Nuclear tests affected water levels in many wells. Trends in these wells are attributed to test-cavity infilling or the effects of depressurization following nuclear testing. The magnitude of the overall water-level change for wells with anthropogenic trends can be large, ranging from several feet to hundreds of feet.\r\n\r\nVertical water-level differences at 27 sites in Yucca Flat with multiple open intervals were compared. Large vertical differences were noted in volcanic rocks and in boreholes where water levels were affected by nuclear tests. Small vertical differences were noted within the carbonate-rock and valley-fill aquifers. Vertical hydraulic gradients generally are downward in volcanic rocks and from pre-Tertiary clastic rocks toward volcanic- or carbonate-rock units.","language":"ENGLISH","doi":"10.3133/sir20055175","usgsCitation":"Fenelon, J.M., 2005, Analysis of ground-water levels and associated trends in Yucca Flat, Nevada Test Site, Nye County, Nevada, 1951-2003 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5175, 97 p. [some 11 x 17 in.] : ill.; online databases; maps, https://doi.org/10.3133/sir20055175.","productDescription":"97 p. [some 11 x 17 in.] : ill.; online databases; maps","onlineOnly":"Y","costCenters":[],"links":[{"id":7446,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5175/","linkFileType":{"id":5,"text":"html"}},{"id":191242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db6803f0","contributors":{"authors":[{"text":"Fenelon, Joseph M. 0000-0003-4449-245X jfenelon@usgs.gov","orcid":"https://orcid.org/0000-0003-4449-245X","contributorId":2355,"corporation":false,"usgs":true,"family":"Fenelon","given":"Joseph","email":"jfenelon@usgs.gov","middleInitial":"M.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285628,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72424,"text":"sir20055142 - 2005 - Potential for formation of disinfection by-products from storage of chlorinated surface water in the Basalt aquifer near Fallon, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"sir20055142","displayToPublicDate":"2005-10-05T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":334,"text":"Scientific Investigations Report","code":"SIR","onlineIssn":"2328-0328","printIssn":"2328-031X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"2005-5142","title":"Potential for formation of disinfection by-products from storage of chlorinated surface water in the Basalt aquifer near Fallon, Nevada","docAbstract":"Increased pumpage from a basalt aquifer near Fallon, Nevada, has caused its water levels to decline and has induced changes in the quality of water pumped from the basalt. The aquifer is the sole source of water for municipal supply to the city of Fallon, the Naval Air Station Fallon, and the Fallon Paiute-Shoshone Tribe. These changes may be mitigated by storage of surface water in the basalt for subsequent use. Because chlorination of the surface water may be required for storage, the U.S. Geological Survey, in cooperation with the Fallon Paiute-Shoshone Tribe, made laboratory tests using laboratory carbon-organic-free water, surface-water, ground-water, and basaltic-rock samples to determine the potential for formation of disinfection by-products. \r\n\r\nExperiments with water samples only (no rock and no chlorine) indicated no change in dissolved-organic-carbon (DOC) concentrations over a 20-day reaction period; whereas, all experiments using rock, water, and no chlorine indicated an increase in DOC concentrations. The greatest increase in DOC concentrations for all three water samples occurred in experiments with the rock samples from outcrops on Rattlesnake Hill. Experiments with water only and chlorine yielded a total trihalomethane (THM) concentration of 97.4 ?g/L for the ground-water sample and 347 ?g/L for the surface-water sample. \r\n\r\nExperiments with mixtures of water, rocks, and chlorine indicated that reactions with the rock consumed chlorine and released significant amounts of organic carbon from the rock, increasing the DOC concentration in the water. The organic carbon in the rocks likely is associated with the secondary clay minerals that line vesicles and fractures in the rocks. THM concentrations were greatest, from 335 to 909 ?g/L, for surface water equilibrated with rock samples from Rattlesnake Hill. However, the concentration of chlorine required to produce these high THM concentrations ranged from 18 to 84 mg/L. \r\n\r\nThe results of the experiments suggest that the amount of organic carbon released from the rocks during successive cycles of recharge, storage, and recovery of chlorinated surface water may be relatively small. The chlorine demand of the rocks is so large that all of the free chlorine in the entire volume of recharged water likely would be consumed by only a very small volume of the aquifer surrounding an injection well, or beneath an infiltration bed. The majority of the volume of the aquifer filled by the stored water likely would never come in contact with free chlorine, and the increases in concentration of DOC observed in these experiments likely would occur in a very small volume of the stored water. For this reason, increases in concentration of THMs for the entire volume of water stored also likely would be considerably less than those measured in these experiments. To test this hypothesis, additional laboratory experiments using varying levels of chlorination, varying lengths of reaction periods, and repeated cycles of chlorination would be useful. A field experiment made at a small scale in an isolated part of the basalt aquifer would aid in the design of an operational system.","language":"ENGLISH","doi":"10.3133/sir20055142","usgsCitation":"Fram, M.S., Maurer, D.K., and Lico, M.S., 2005, Potential for formation of disinfection by-products from storage of chlorinated surface water in the Basalt aquifer near Fallon, Nevada (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5142, 30 p., https://doi.org/10.3133/sir20055142.","productDescription":"30 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":191303,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7447,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5142/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6836c3","contributors":{"authors":[{"text":"Fram, Miranda S. 0000-0002-6337-059X mfram@usgs.gov","orcid":"https://orcid.org/0000-0002-6337-059X","contributorId":1156,"corporation":false,"usgs":true,"family":"Fram","given":"Miranda","email":"mfram@usgs.gov","middleInitial":"S.","affiliations":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285629,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maurer, Douglas K. dkmaurer@usgs.gov","contributorId":2308,"corporation":false,"usgs":true,"family":"Maurer","given":"Douglas","email":"dkmaurer@usgs.gov","middleInitial":"K.","affiliations":[],"preferred":true,"id":285630,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lico, Michael S.","contributorId":75897,"corporation":false,"usgs":true,"family":"Lico","given":"Michael","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":285631,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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