{"pageNumber":"2546","pageRowStart":"63625","pageSize":"25","recordCount":184652,"records":[{"id":72254,"text":"ofr20051006_2005 - 2005 - Potentiometric surface map of the Magothy aquifer in southern Maryland, September, 2003","interactions":[],"lastModifiedDate":"2023-03-09T20:49:22.817505","indexId":"ofr20051006_2005","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1006","title":"Potentiometric surface map of the Magothy aquifer in southern Maryland, September, 2003","docAbstract":"This report presents a map showing the potentiometric surface of the Magothy aquifer in the Magothy Formation of Upper Cretaceous age in Southern Maryland during September 2002. The map is based on water-level measurements in 79 wells. The highest measured water level was 83 feet above sea level near the northern boundary and outcrop area of the aquifer in the north-central part of Anne Arundel County.\r\n\r\nThe potentiometric surface declined towards the south and east. Local gradients were directed toward the centers of two cones of depression that developed in response to pumping. These cones of depression were centered around well fields in the Waldorf area and at the Chalk Point power plant. Measured ground-water levels were as low as 81 feet below sea level in the Waldorf area and 75 feet below sea level at Chalk Point.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051006_2005","usgsCitation":"Curtin, S.E., Andreasen, D., and Wheeler, J.C., 2005, Potentiometric surface map of the Magothy aquifer in southern Maryland, September, 2003: U.S. Geological Survey Open-File Report 2005-1006, 1 p., https://doi.org/10.3133/ofr20051006_2005.","productDescription":"1 p.","temporalStart":"2003-09-01","temporalEnd":"2003-09-30","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia  Water Science Center","active":true,"usgs":true}],"links":[{"id":191623,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8906,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1006/","linkFileType":{"id":5,"text":"html"}},{"id":409012,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_78439.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Maryland","otherGeospatial":"Magothy aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.0667,\n              38.26667\n            ],\n            [\n              -76,\n              38.2667\n            ],\n            [\n              -76,\n              39.2197\n            ],\n            [\n              -77.0667,\n              39.2197\n            ],\n            [\n              -77.0667,\n              38.2667\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68310d","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285271,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":285273,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285272,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72270,"text":"ofr20051317 - 2005 - Compressional and shear wave velocity versus depth in the San Francisco Bay area, California: Rules for USGS Bay Area Velocity Model 05.0.0","interactions":[],"lastModifiedDate":"2022-07-05T18:09:57.461823","indexId":"ofr20051317","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1317","title":"Compressional and shear wave velocity versus depth in the San Francisco Bay area, California: Rules for USGS Bay Area Velocity Model 05.0.0","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051317","usgsCitation":"Brocher, T.M., 2005, Compressional and shear wave velocity versus depth in the San Francisco Bay area, California: Rules for USGS Bay Area Velocity Model 05.0.0: U.S. Geological Survey Open-File Report 2005-1317, 58 p., https://doi.org/10.3133/ofr20051317.","productDescription":"58 p.","costCenters":[],"links":[{"id":193145,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":402996,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73603.htm","linkFileType":{"id":5,"text":"html"}},{"id":7141,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1317/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.947998046875,\n              36.85325222344018\n            ],\n            [\n              -120.89355468749999,\n              36.85325222344018\n            ],\n            [\n              -120.89355468749999,\n              38.75408327579141\n            ],\n            [\n              -122.947998046875,\n              38.75408327579141\n            ],\n            [\n              -122.947998046875,\n              36.85325222344018\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7ef9","contributors":{"authors":[{"text":"Brocher, Thomas M. 0000-0002-9740-839X brocher@usgs.gov","orcid":"https://orcid.org/0000-0002-9740-839X","contributorId":262,"corporation":false,"usgs":true,"family":"Brocher","given":"Thomas","email":"brocher@usgs.gov","middleInitial":"M.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":285321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72292,"text":"sir20055185 - 2005 - Pre- and post-reservoir ground-water conditions and assessment of artificial recharge at Sand Hollow, Washington County, Utah, 1995-2005","interactions":[],"lastModifiedDate":"2017-01-27T16:04:53","indexId":"sir20055185","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-5185","title":"Pre- and post-reservoir ground-water conditions and assessment of artificial recharge at Sand Hollow, Washington County, Utah, 1995-2005","docAbstract":"<p>Sand Hollow, Utah, is the site of a surface-water reservoir completed in March 2002, which is being operated by the Washington County Water Conservancy District primarily as an aquifer storage and recovery project. The reservoir is an off-channel facility receiving water from the Virgin River, diverted near the town of Virgin, Utah. It is being operated conjunctively, providing both surface-water storage and artificial recharge to the underlying Navajo aquifer. The U.S. Geological Survey and the Bureau of Reclamation conducted a study to document baseline ground-water conditions at Sand Hollow prior to the operation of the reservoir and to evaluate changes in ground-water conditions caused by the reservoir.</p><p>Pre-reservoir age dating using tritium/helium, chlorofluorocarbons, and carbon-14 shows that shallow ground water in the Navajo Sandstone in some areas of Sand Hollow entered the aquifer from 2 to 25 years before sample collection. Ground water in low-recharge areas and deeper within the aquifer may have entered the aquifer more than 8,000 years ago. Ground-water levels in the immediate vicinity of Sand Hollow Reservoir have risen by as much as 80 feet since initial filling began in March 2002. In 2005, ground water was moving laterally away from the reservoir in all directions, whereas the pre-reservoir direction of ground-water flow was predominantly toward the north.</p><p>Tracers, or attributes, of artificial recharge include higher specific conductance, higher dissolved-solids concentrations, higher chloride-to-bromide ratios, more-depleted stable isotopes (<img src=\"https://pubs.usgs.gov/sir/2005/5185/images/snake.gif\" alt=\"Snake\" width=\"16\" height=\"15\" data-mce-src=\"https://pubs.usgs.gov/sir/2005/5185/images/snake.gif\"><sup>2</sup>H and <img src=\"https://pubs.usgs.gov/sir/2005/5185/images/snake.gif\" alt=\"Snake\" width=\"16\" height=\"15\" data-mce-src=\"https://pubs.usgs.gov/sir/2005/5185/images/snake.gif\"><sup>18</sup>O), and higher total-dissolved gas pressures. These tracers have been detected at observation and production wells close to the reservoir. About 15,000 tons of naturally occurring salts that previously accumulated in the vadose zone beneath the reservoir are being flushed into the aquifer. Except for the shallowest parts of the aquifer, this is generally not affecting water quality, largely because of the large saturated thickness of the Navajo aquifer. Since the initial filling of Sand Hollow Reservoir, arsenic concentrations have risen to exceed U.S. Environmental Protection Agency standards only in some shallow observation wells. These increases in arsenic concentration are likely caused by increasing pH associated with artificial recharge beneath the reservoir, rather than flushing of previously accumulated salts in the vadose zone. There has been no trend of increasing arsenic concentration in deeper production wells.</p><p>Estimated evaporation rates for Sand Hollow Reservoir, calculated by the Jensen-Haise method with data from the Sand Hollow weather station, range from about 55 to 61 inches per year and result in a total evaporative loss of about 6,000 acre-feet of water from March 2002 to September 2004. Rates of artificial recharge of ground water beneath Sand Hollow Reservoir have ranged from about 0.02 to 0.44 feet per day, with an average rate excluding the initial 3-month wetting period of about 0.06 feet per day. A total of about 28,000 acre-feet of recharge to the underlying Navajo aquifer occurred from March 2002 to September 2004.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/sir20055185","collaboration":"Prepared in cooperation with the Washington County water conservancy district, Bureau of Reclamation, and the University of Utah Department of Geology and Geophysics","usgsCitation":"Heilweil, V.M., Susong, D.D., Gardner, P.M., and Watt, D.E., 2005, Pre- and post-reservoir ground-water conditions and assessment of artificial recharge at Sand Hollow, Washington County, Utah, 1995-2005 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5185, viii, 74 p., https://doi.org/10.3133/sir20055185.","productDescription":"viii, 74 p.","numberOfPages":"85","onlineOnly":"Y","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":191824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":334243,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5185/pdf/SIR2005_5185.pdf"},{"id":7204,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5185/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","county":"Washington County","otherGeospatial":"Sand Hollow","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.393499,37.102437 ], [ -113.393499,37.127407 ], [ -113.359917,37.127407 ], [ -113.359917,37.102437 ], [ -113.393499,37.102437 ] ] ] } } ] }","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681dc2","contributors":{"authors":[{"text":"Heilweil, Victor M. heilweil@usgs.gov","contributorId":837,"corporation":false,"usgs":true,"family":"Heilweil","given":"Victor","email":"heilweil@usgs.gov","middleInitial":"M.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285364,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Susong, David D. ddsusong@usgs.gov","contributorId":1040,"corporation":false,"usgs":true,"family":"Susong","given":"David","email":"ddsusong@usgs.gov","middleInitial":"D.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285366,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gardner, Philip M. 0000-0003-3005-3587 pgardner@usgs.gov","orcid":"https://orcid.org/0000-0003-3005-3587","contributorId":962,"corporation":false,"usgs":true,"family":"Gardner","given":"Philip","email":"pgardner@usgs.gov","middleInitial":"M.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285365,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Watt, Dennis E.","contributorId":55286,"corporation":false,"usgs":true,"family":"Watt","given":"Dennis","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":285367,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72291,"text":"b2204E - 2005 - Transylvanian Composite Total Petroleum System of the Transylvanian Basin Province, Romania, Eastern Europe","interactions":[],"lastModifiedDate":"2018-08-28T16:47:53","indexId":"b2204E","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2204","chapter":"E","title":"Transylvanian Composite Total Petroleum System of the Transylvanian Basin Province, Romania, Eastern Europe","docAbstract":"The Transylvanian Composite Total Petroleum System and the Transylvanian Neogene Suprasalt Gas Assessment Unit were identified in the Transylvanian Basin Province (4057), which lies entirely within the country of Romania. The assessment unit is composed of middle Miocene (Badenian) to Pliocene strata. Gas from the assessment unit is biogenic and originated from bacterial activity on dispersed organic matter in shales and siltstones. Gas migration is believed to be minimal, both vertically and laterally, with gases trapped in local stratigraphic traps and in structural traps (most likely domes and anticlinal folds created by salt diapirism) in the central part of the basin. For this reason, the gas fields also are concentrated in the central part of the basin. Reservoirs are isolated and composed of vertically stacked sandstones and siltstones sealed by shales and possibly by evaporite layers. Traps result from stratigraphic and facies changes within the entire assessment unit stratigraphic section. Some gas fields contain as much or more than a trillion cubic feet, but in most, the estimated resources are between 6 billion and 96 billion cubic feet. Petroleum exploration in the province is in the mature stage, which, combined with the geologic complexity of the region, is considered to limit future discoveries to a relatively few small fields. The undiscovered resources for the Transylvanian Basin Neogene Suprasalt Composite AU in the Transylvanian Hybrid Total Petroleum System (4057) are, at the mean, 2.083 trillion cubic feet of gas. No oil is produced in the basin. Rocks underlying the salt layers were not assessed for hydrocarbon potential.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"World Petroleum Assessment 2000","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b2204E","usgsCitation":"Pawlewicz, M., 2005, Transylvanian Composite Total Petroleum System of the Transylvanian Basin Province, Romania, Eastern Europe (Version 1.0): U.S. Geological Survey Bulletin 2204, iii, 10 p., https://doi.org/10.3133/b2204E.","productDescription":"iii, 10 p.","onlineOnly":"Y","costCenters":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":174,"text":"Central Region Energy Resources Program","active":false,"usgs":true}],"links":[{"id":191770,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7203,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/2204/e/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 14,43 ], [ 14,52 ], [ 30,52 ], [ 30,43 ], [ 14,43 ] ] ] } } ] }","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626b71","contributors":{"authors":[{"text":"Pawlewicz, Mark","contributorId":69212,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"Mark","email":"","affiliations":[],"preferred":false,"id":285363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72272,"text":"ds124 - 2005 - Mining Claim Activity on Federal Land for the Period 1976 through 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"ds124","displayToPublicDate":"2005-09-19T00:00:00","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":"124","title":"Mining Claim Activity on Federal Land for the Period 1976 through 2003","docAbstract":"Previous reports on mining claim records provided information and statistics (number of claims) using data from the U.S. Bureau of Land Management's (BLM) Mining Claim Recordation System. Since that time, BLM converted their mining claim data to the Legacy Repost 2000 system (LR2000). \r\n\r\nThis report describes a process to extract similar statistical data about mining claims from LR2000 data using different software and procedures than were used in the earlier work. A major difference between this process and the previous work is that every section that has a mining claim record is assigned a value. This is done by proportioning a claim between each section in which it is recorded. Also, the mining claim data in this report includes all BLM records, not just the western states. \r\n\r\nLR2000 mining claim database tables for the United States were provided by BLM in text format and imported into a Microsoft? Access2000 database in January, 2004. Data from two tables in the BLM LR2000 database were summarized through a series of database queries to determine a number that represents active mining claims in each Public Land Survey (PLS) section for each of the years from 1976 to 2002. For most of the area, spatial databases are also provided. The spatial databases are only configured to work with the statistics provided in the non-spatial data files. They are suitable for geographic information system (GIS)-based regional assessments at a scale of 1:100,000 or smaller (for example, 1:250,000).","language":"ENGLISH","doi":"10.3133/ds124","usgsCitation":"Causey, J.D., 2005, Mining Claim Activity on Federal Land for the Period 1976 through 2003: U.S. Geological Survey Data Series 124, 28 p. text + data files, https://doi.org/10.3133/ds124.","productDescription":"28 p. text + data files","costCenters":[],"links":[{"id":193205,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7142,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/ds/124/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb727","contributors":{"authors":[{"text":"Causey, J. Douglas","contributorId":41398,"corporation":false,"usgs":true,"family":"Causey","given":"J.","email":"","middleInitial":"Douglas","affiliations":[],"preferred":false,"id":285325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72290,"text":"sir20055158 - 2005 - Trends in surface-water quality at selected National Stream Quality Accounting Network (NASQAN) stations, in Michigan","interactions":[],"lastModifiedDate":"2017-02-06T09:35:02","indexId":"sir20055158","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-5158","title":"Trends in surface-water quality at selected National Stream Quality Accounting Network (NASQAN) stations, in Michigan","docAbstract":"<p>To demonstrate the value of long-term, water-quality monitoring, the Michigan Department of Environmental Quality (MDEQ), in cooperation with the U.S. Geological Survey (USGS), initiated a study to evaluate potential trends in water-quality constituents for selected National Stream Quality Accounting Network (NASQAN) stations in Michigan. The goal of this study is to assist the MDEQ in evaluating the effectiveness of water-pollution control efforts and the identification of water-quality concerns. </p><p>The study included a total of nine NASQAN stations in Michigan. Approximately 28 constituents were analyzed for trend tests. Station selection was based on data availability, land-use characteristics, and station priority for the MDEQ Water Chemistry Monitoring Project. Trend analyses were completed using the uncensored Seasonal Kendall Test in the computer program Estimate Trend (ESTREND), a software program for the detection of trends in water-quality data. The parameters chosen for the trend test had (1) at least a 5-year period of record (2) about 5 percent of the observations censored at a single reporting limit, and (3) 40 percent of the values within the beginning one-fifth and ending one-fifth of the selected period. In this study, a negative trend indicates a decrease in concentration of a particular constituent, which generally means an improvement in water quality; whereas a positive trend means an increase in concentration and possible degradation of water quality. </p><p>The results of the study show an overall improvement in water quality at the Clinton River at Mount Clemens, Manistee River at Manistee, and Pigeon River near Caseville. The detected trend for these stations show decreases in concentrations of various constituents such as nitrogen compounds, conductance, sulfate, fecal coliform bacteria, and fecal streptococci bacteria. The negative trend may indicate an overall improvement in agricultural practices, municipal and industrial wastewater-treatment processes, and effective regulations. </p><p>Phosphorus data for most of the study stations could not be analyzed because of the data limitations for trend tests. The only station with a significant negative trend in total phosphorus concentration is the Clinton River at Mount Clemens. However, scatter-plot analyses of phosphorus data indicate decreasing concentrations with time for most of the study stations. </p><p>Positive trends in concentration of nitrogen compounds were detected at the Kalamazoo River near Saugatuck and Muskegon River near Bridgeton. Positive trends in both fecal coliform and total fecal coliform were detected at the Tahquamenon River near Paradise. Various different point and nonpoint sources could produce such positive trends, but most commonly the increase in concentrations of nitrogen compounds and fecal coliform bacteria are associated with agricultural practices and sewage-plant discharges. </p><p>The constituent with the most numerous and geographically widespread significant trend is pH. The pH levels increased at six out of nine stations on all the major rivers in Michigan, with no negative trend at any station. The cause of pH increase is difficult to determine, as it could be related to a combination of anthropogenic activities and natural processes occurring simultaneously in the environment. </p><p>Trends in concentration of major ions, such as calcium, sodium, magnesium, sulfate, fluoride, chloride, and potassium, were detected at eight out of nine stations. A negative trend was detected only in sulfate and fluoride concentrations; a positive trend was detected only in calcium concentration. The major ions with the most widespread significant trends are sodium and chloride; three positive and two negative trends were detected for sodium, and three negative and two positive trends were detected for chloride. The negative trends in chloride concentrations outnumbered the positive trends. This result indicates a slight improvement in surface-water quality because chloride as a point source in natural water comes from deicing salt, sewage effluents, industrial wastes, and oil fields. </p><p>For other major ions, such as magnesium and potassium, both positive and negative trends were detected. These changes in trends indicate changes in surface-water quality caused by a variety of point and non-point sources throughout Michigan, as well as natural changes in the environment.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20055158","collaboration":"In cooperation with the Michigan Department of Environmental Quality","usgsCitation":"Syed, A.U., and Fogarty, L., 2005, Trends in surface-water quality at selected National Stream Quality Accounting Network (NASQAN) stations, in Michigan: U.S. Geological Survey Scientific Investigations Report 2005-5158, v, 38 p., https://doi.org/10.3133/sir20055158.","productDescription":"v, 38 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":191769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20055158.JPG"},{"id":7202,"rank":100,"type":{"id":15,"text":"Index 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 \"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697aa0","contributors":{"authors":[{"text":"Syed, Atiq U.","contributorId":14898,"corporation":false,"usgs":true,"family":"Syed","given":"Atiq","email":"","middleInitial":"U.","affiliations":[],"preferred":false,"id":285361,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fogarty, Lisa R.","contributorId":74074,"corporation":false,"usgs":true,"family":"Fogarty","given":"Lisa R.","affiliations":[],"preferred":false,"id":285362,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72285,"text":"sir20055075 - 2005 - Changes in ground-water levels in the Carlin Trend area, north-central Nevada, 1989-2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"sir20055075","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-5075","title":"Changes in ground-water levels in the Carlin Trend area, north-central Nevada, 1989-2003","docAbstract":"Ground-water pumpage in support of gold mining activities, including mine dewatering, has resulted in water-level declines and rises in different parts of the Carlin Trend area in north-central Nevada. Total annual pumpage at the Gold Quarry, Carlin, Genesis, and Betze Mines has ranged from about 5,000 acre-feet in 1989 to almost 130,000 acre-feet in 1994 and 1998. Excess water from the mines is stored in the TS Ranch and Maggie Creek Reservoirs.\r\n\r\nAquifers in the Carlin Trend area are comprised of carbonate rocks of Cambrian to Permian age and basin-fill deposits and interbedded volcanic rocks of Tertiary and Quaternary age. Since 1992, water levels in carbonate-rock aquifers near the Gold Quarry Mine have declined as much as 680 feet below an elongate area 12 miles long and 6 miles wide northwest and southeast from the mine. Since 1990, water levels have declined by more than 1,600 feet in the deepest part of the cone of depression at the Betze Mine. The area encompassed by the main part of the cone, which is 7 miles long by 4 miles wide, did not change much during 1993-2003, although its depth had doubled. Near both mines, the cones of depression are bounded by faults acting as barriers to ground-water flow. \r\n\r\nWater levels in the volcanic rocks of northern Boulder Flat began to rise soon after the TS Ranch Reservoir began filling in 1990 because of infiltration. Since 1990, the net water-level rise around the reservoir has been 50 feet or more over an area of about 2 square miles, and 20 feet or more over an area of about 60 square miles. \r\n\r\nSince 1992, water levels in basin-fill deposits in Boulder Flat have risen 5 feet or more over an estimated area of 20 square miles as a result of (1) use of water from the Betze Mine as a substitute for irrigation pumpage, (2) water from the TS Ranch Reservoir infiltrating volcanic rocks and then flowing southward into adjacent basin-fill deposits, (3) secondary recharge of water from the mine for irrigating about 10,000 acres, and (4) discharge from three new springs in northeastern Boulder Flat.\r\n\r\nWater-level declines in carbonate rocks near the Gold Quarry Mine have not affected water levels in overlying basin-fill deposits. Declines were no more than a few feet north and west of the mine because older basin-fill deposits at the base of the Carlin Formation consist of fine-grained poorly permeable sediments. Water levels rose 5 feet to more than 20 feet over an area of 6-7 square miles around the Maggie Creek Reservoir in response to infiltration. A few miles farther south, water levels rose as much as 5 feet over an area of 3 square miles as a combined result of the infiltration of irrigation water and flow of Maggie Creek into permeable volcanic rocks in the stream channel. \r\n\r\nAn area of 1,900 acres about 10 miles north of Battle Mountain in the Clovers Area has been pumped for irrigation since the early 1970's. Since 1989, water levels have declined 5-15 feet over an area of 15 square miles.","language":"ENGLISH","doi":"10.3133/sir20055075","usgsCitation":"Plume, R.W., 2005, Changes in ground-water levels in the Carlin Trend area, north-central Nevada, 1989-2003: U.S. Geological Survey Scientific Investigations Report 2005-5075, iv, 14 p. : ill., col. maps ; 28 cm.; one map on 1 folded leaf in pocket, https://doi.org/10.3133/sir20055075.","productDescription":"iv, 14 p. : ill., col. maps ; 28 cm.; one map on 1 folded leaf in pocket","costCenters":[],"links":[{"id":193253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7154,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5075/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6cbf","contributors":{"authors":[{"text":"Plume, Russell W. rwplume@usgs.gov","contributorId":2303,"corporation":false,"usgs":true,"family":"Plume","given":"Russell","email":"rwplume@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":true,"id":285354,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72284,"text":"sir20055149 - 2005 - Questa baseline and pre-mining ground-water quality investigation. 12. Geochemical and reactive-transport modeling based on tracer injection-synoptic sampling studies for the Red River, New Mexico, 2001-2002","interactions":[],"lastModifiedDate":"2024-10-30T19:00:48.391857","indexId":"sir20055149","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-5149","title":"Questa baseline and pre-mining ground-water quality investigation. 12. Geochemical and reactive-transport modeling based on tracer injection-synoptic sampling studies for the Red River, New Mexico, 2001-2002","docAbstract":"<p>Reactive-transport processes in the Red River, downstream from the town of<span>&nbsp;</span>Red River<span>&nbsp;</span>in north-central New Mexico, were simulated using the OTEQ reactive-transport model. The simulations were calibrated using physical and chemical data from synoptic studies conducted during low-flow conditions in August 2001 and during March/April 2002. Discharge over the 20-km reach from the town of Red River to the USGS streamflow-gaging station near the town of Questa ranged from 395 to 1,180 L/s during the 2001 tracer and from 234 to 421 L/s during the 2002 tracer. The pH of the<span>&nbsp;</span>Red River<span>&nbsp;</span>ranged from 7.4 to 8.5 during the 2001 tracer and from 7.1 to 8.7 during the 2002 tracer, and seep and tributary samples had pH values of 2.8 to 9.0 during the 2001 tracer and 3.8 to 7.2 during the 2002 tracer.</p><p>Mass-loading calculations allowed identification of several specific locations where elevated concentrations of potential contaminants entered the<span>&nbsp;</span>Red River<span>&nbsp;</span>. These locations, characterized by features on the north side of the Red River that are known to be sources of low-pH water containing elevated metal and sulfate concentrations, are: the initial 2.4 km of the study reach, including Bitter Creek, the stream section from 6.2 to 7.8 km, encompassing La Bobita well and the Hansen debris fan, Sulphur Gulch, at about 10.5 km, the area near Portal Springs, from 12.2 to 12.6 km, and the largest contributors of mass loading, the 13.7 to 13.9 km stream section near Cabin Springs and the 14.7 to 17.5 km stream section from Shaft Spring to Thunder Bridge, Goathill Gulch, and Capulin Canyon.</p><p>Speciation and saturation index calculations indicated that although solubility limits the concentration of aluminum above pH 5.0, at pH values above 7 and aluminum concentrations below 0.3 mg/L inorganic speciation and mineral solubility controls no longer dominate and aluminum-organic complexing may occur.</p><p>The August 2001 reactive-transport simulations included dissolved iron(II) oxidation, constrained using measured concentrations of dissolved iron(II) and dissolved iron(total). Both simulations included precipitation of amorphous Al(OH)<sub>3</sub><span>&nbsp;</span>and hydrous ferric oxide as Fe(OH)<sub>3</sub>, and sorption of copper and zinc to the precipitated hydrous ferric oxide. Simulations revealed that hydrogen, iron, aluminum, copper, and zinc were non-conservative and that mineral precipitation can account for iron and aluminum concentrations. Copper and zinc concentrations can be accounted for by simulating their sorption to hydrous ferric oxide forming in the water column of the<span>&nbsp;</span>Red River<span>&nbsp;</span>, although hydrous manganese oxides also may be important sorption substrates.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055149","usgsCitation":"Ball, J.W., Runkel, R.L., and Nordstrom, D.K., 2005, Questa baseline and pre-mining ground-water quality investigation. 12. Geochemical and reactive-transport modeling based on tracer injection-synoptic sampling studies for the Red River, New Mexico, 2001-2002: U.S. Geological Survey Scientific Investigations Report 2005-5149, vii, 68 p., https://doi.org/10.3133/sir20055149.","productDescription":"vii, 68 p.","temporalStart":"2001-01-01","temporalEnd":"2002-12-31","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":589,"text":"Toxic Substances Hydrology Program","active":true,"usgs":true}],"links":[{"id":193252,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7153,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5149/","linkFileType":{"id":5,"text":"html"}},{"id":463441,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_86714.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico","otherGeospatial":"Red River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.55,36.63333333333333 ], [ -105.55,36.733333333333334 ], [ -105.4,36.733333333333334 ], [ -105.4,36.63333333333333 ], [ -105.55,36.63333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685afe","contributors":{"authors":[{"text":"Ball, James W.","contributorId":38946,"corporation":false,"usgs":true,"family":"Ball","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":285352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runkel, Robert L. 0000-0003-3220-481X runkel@usgs.gov","orcid":"https://orcid.org/0000-0003-3220-481X","contributorId":685,"corporation":false,"usgs":true,"family":"Runkel","given":"Robert","email":"runkel@usgs.gov","middleInitial":"L.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285351,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nordstrom, D. Kirk 0000-0003-3283-5136 dkn@usgs.gov","orcid":"https://orcid.org/0000-0003-3283-5136","contributorId":749,"corporation":false,"usgs":true,"family":"Nordstrom","given":"D.","email":"dkn@usgs.gov","middleInitial":"Kirk","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":false,"id":285353,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72247,"text":"ofr20051090 - 2005 - Geomorphic Data Collected Within Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:58","indexId":"ofr20051090","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1090","title":"Geomorphic Data Collected Within Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2004","language":"ENGLISH","doi":"10.3133/ofr20051090","usgsCitation":"Kinzel, P.J., Parker, R.S., Nelson, J.M., Burman, A.R., and Heckman, A.K., 2005, Geomorphic Data Collected Within Nebraska Public Power District's Cottonwood Ranch Property, Platte River, Nebraska, Water Year 2004: U.S. Geological Survey Open-File Report 2005-1090, 23 p. text + additional files, https://doi.org/10.3133/ofr20051090.","productDescription":"23 p. text + additional files","costCenters":[],"links":[{"id":191524,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7099,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://wwwbrr.cr.usgs.gov/projects/SW_Env_Fluid/downloads.html","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c55f","contributors":{"authors":[{"text":"Kinzel, Paul J. 0000-0002-6076-9730 pjkinzel@usgs.gov","orcid":"https://orcid.org/0000-0002-6076-9730","contributorId":743,"corporation":false,"usgs":true,"family":"Kinzel","given":"Paul","email":"pjkinzel@usgs.gov","middleInitial":"J.","affiliations":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true},{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true}],"preferred":true,"id":285244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, Randolph S.","contributorId":58638,"corporation":false,"usgs":true,"family":"Parker","given":"Randolph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":285246,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelson, Jonathan M. 0000-0002-7632-8526 jmn@usgs.gov","orcid":"https://orcid.org/0000-0002-7632-8526","contributorId":2812,"corporation":false,"usgs":true,"family":"Nelson","given":"Jonathan","email":"jmn@usgs.gov","middleInitial":"M.","affiliations":[{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true},{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":285245,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Burman, Aaron R.","contributorId":102960,"corporation":false,"usgs":true,"family":"Burman","given":"Aaron","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285247,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Heckman, Ashley K.","contributorId":103748,"corporation":false,"usgs":true,"family":"Heckman","given":"Ashley","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":285248,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72251,"text":"ofr20051011 - 2005 - The difference between the potentiometric surfaces of the Lower Patapsco Aquifer, September 1990 and September 2003 in Southern Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:13:58","indexId":"ofr20051011","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1011","title":"The difference between the potentiometric surfaces of the Lower Patapsco Aquifer, September 1990 and September 2003 in Southern Maryland","docAbstract":"This report presents a map showing the change in the potentiometric surface of the Lower Patapsco aquifer in the Lower Patapsco Formation of Cretaceous age in Southern Maryland for September 1990 and September 2003. The map, based on water level measurements in 45 wells, shows that the change of the potentiometric surface during the 13- year period ranged from rises of 17 feet at Indian Head and 9 feet near the outcrop area in Glen Burnie, to declines of 40 feet at Arnold, 44 feet at Severndale, 48 feet at Waldorf, 69 feet at LaPlata, and 31 feet at the Morgantown powerplant.","language":"ENGLISH","doi":"10.3133/ofr20051011","usgsCitation":"Curtin, S.E., Andreasen, D., and Wheeler, J.C., 2005, The difference between the potentiometric surfaces of the Lower Patapsco Aquifer, September 1990 and September 2003 in Southern Maryland: U.S. Geological Survey Open-File Report 2005-1011, 1 p., https://doi.org/10.3133/ofr20051011.","productDescription":"1 p.","temporalStart":"1990-09-01","temporalEnd":"2003-09-30","costCenters":[],"links":[{"id":191577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8913,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1011/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668526","contributors":{"authors":[{"text":"Curtin, Stephen E. securtin@usgs.gov","contributorId":3703,"corporation":false,"usgs":true,"family":"Curtin","given":"Stephen","email":"securtin@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, David C.","contributorId":59003,"corporation":false,"usgs":true,"family":"Andreasen","given":"David C.","affiliations":[],"preferred":false,"id":285264,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wheeler, Judith C.","contributorId":13620,"corporation":false,"usgs":true,"family":"Wheeler","given":"Judith","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":285263,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72261,"text":"ofr20051252 - 2005 - The geologic map of Seattle — A progress report","interactions":[],"lastModifiedDate":"2022-07-15T20:17:21.334219","indexId":"ofr20051252","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1252","title":"The geologic map of Seattle — A progress report","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051252","usgsCitation":"Troost, K.G., Booth, D.B., Wisher, A.P., and Shimel, S.A., 2005, The geologic map of Seattle — A progress report (Version 1.0): U.S. Geological Survey Open-File Report 2005-1252, 1 Plate: 36.00 × 60.00 inches, https://doi.org/10.3133/ofr20051252.","productDescription":"1 Plate: 36.00 × 60.00 inches","costCenters":[],"links":[{"id":7105,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1252/","linkFileType":{"id":5,"text":"html"}},{"id":192533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":110574,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_72190.htm","linkFileType":{"id":5,"text":"html"},"description":"72190"}],"country":"United States","state":"Washington","city":"Seattle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.4372,\n              47.4958\n            ],\n            [\n              -122.2333,\n              47.4958\n            ],\n            [\n              -122.2333,\n              47.75\n            ],\n            [\n              -122.4372,\n              47.75\n            ],\n            [\n              -122.4372,\n              47.4958\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7ef","contributors":{"authors":[{"text":"Troost, Kathy Goetz","contributorId":35023,"corporation":false,"usgs":true,"family":"Troost","given":"Kathy","email":"","middleInitial":"Goetz","affiliations":[],"preferred":false,"id":285288,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Booth, Derek B.","contributorId":100873,"corporation":false,"usgs":false,"family":"Booth","given":"Derek","email":"","middleInitial":"B.","affiliations":[{"id":6934,"text":"University of Washington","active":true,"usgs":false}],"preferred":false,"id":285290,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wisher, Aaron P.","contributorId":60728,"corporation":false,"usgs":true,"family":"Wisher","given":"Aaron","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":285289,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Shimel, Scott A.","contributorId":25252,"corporation":false,"usgs":true,"family":"Shimel","given":"Scott","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285287,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72293,"text":"wdrMDDEDC041 - 2005 - Water resources data Maryland, Delaware, and Washington, D.C., water year 2004, Volume 1. Surface-water data","interactions":[],"lastModifiedDate":"2012-02-02T00:13:55","indexId":"wdrMDDEDC041","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-DC-04-1","title":"Water resources data Maryland, Delaware, and Washington, D.C., water year 2004, Volume 1. Surface-water data","language":"ENGLISH","doi":"10.3133/wdrMDDEDC041","usgsCitation":"Saffer, R.W., Pentz, R.H., and Tallman, A.J., 2005, Water resources data Maryland, Delaware, and Washington, D.C., water year 2004, Volume 1. Surface-water data: U.S. Geological Survey Water Data Report MD-DE-DC-04-1, 572 p., https://doi.org/10.3133/wdrMDDEDC041.","productDescription":"572 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":191825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7205,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2004/wdr-md-de-dc-04-1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7fce","contributors":{"authors":[{"text":"Saffer, Richard W.","contributorId":79951,"corporation":false,"usgs":true,"family":"Saffer","given":"Richard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":285370,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pentz, Robert H.","contributorId":15276,"corporation":false,"usgs":true,"family":"Pentz","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":285368,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tallman, Anthony J.","contributorId":56275,"corporation":false,"usgs":true,"family":"Tallman","given":"Anthony","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":285369,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":72283,"text":"sir20055106 - 2005 - Quality of nutrient data from streams and ground water sampled during water years 1992-2001","interactions":[],"lastModifiedDate":"2012-02-02T00:13:59","indexId":"sir20055106","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-5106","title":"Quality of nutrient data from streams and ground water sampled during water years 1992-2001","docAbstract":"Proper interpretation of water-quality data requires consideration of the effects that bias and variability might have on measured constituent concentrations. In this report, methods are described to estimate the bias due to contamination of samples in the field or laboratory and the variability due to sample collection, processing, shipment, and analysis. Contamination can adversely affect interpretation of measured concentrations in comparison to standards or criteria. Variability can affect interpretation of small differences between individual measurements or mean concentrations. Contamination and variability are determined for nutrient data from quality-control samples (field blanks and replicates) collected as part of the National Water-Quality Assessment (NAWQA) Program during water years 1992-2001. Statistical methods are used to estimate the likelihood of contamination and variability in all samples. Results are presented for five nutrient analytes from stream samples and four nutrient analytes from ground-water samples. Ammonia contamination can add at least 0.04 milligram per liter in up to 5 percent of all samples. This could account for more than 22 percent of measured concentrations at the low range of aquatic-life criteria (0.18 milligram per liter). Orthophosphate contamination, at least 0.019 milligram per liter in up to 5 percent of all samples, could account for more than 38 percent of measured concentrations at the limit to avoid eutrophication (0.05 milligram per liter). Nitrite-plus-nitrate and Kjeldahl nitrogen contamination is less than 0.4 milligram per liter in 99 percent of all samples; thus there is no significant effect on measured concentrations of environmental significance. Sampling variability has little or no effect on reported concentrations of ammonia, nitrite-plus-nitrate, orthophosphate, or total phosphorus sampled after 1998. The potential errors due to sampling variability are greater for the Kjeldahl nitrogen analytes and for total phosphorus sampled before 1999. The uncertainty in a mean of 10 concentrations caused by sampling variability is within a small range (1 to 7 percent) for all nutrients. These results can be applied to interpretation of environmental data collected during water years 1992-2001 in 52 NAWQA study units. ","language":"ENGLISH","doi":"10.3133/sir20055106","usgsCitation":"Mueller, D.K., and Titus, C.J., 2005, Quality of nutrient data from streams and ground water sampled during water years 1992-2001: U.S. Geological Survey Scientific Investigations Report 2005-5106, v, 27 p. : ill. (some col.), col. map ; 28 cm., https://doi.org/10.3133/sir20055106.","productDescription":"v, 27 p. : ill. (some col.), col. map ; 28 cm.","costCenters":[],"links":[{"id":192864,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7152,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5106/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a68e4b07f02db63b24b","contributors":{"authors":[{"text":"Mueller, David K. mueller@usgs.gov","contributorId":1585,"corporation":false,"usgs":true,"family":"Mueller","given":"David","email":"mueller@usgs.gov","middleInitial":"K.","affiliations":[{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":285349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Titus, Cindy J.","contributorId":61913,"corporation":false,"usgs":true,"family":"Titus","given":"Cindy","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":285350,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72280,"text":"pp1707 - 2005 - The orphan tsunami of 1700—Japanese clues to a parent earthquake in North America","interactions":[],"lastModifiedDate":"2023-04-10T14:30:26.904775","indexId":"pp1707","displayToPublicDate":"2005-09-19T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1707","title":"The orphan tsunami of 1700—Japanese clues to a parent earthquake in North America","docAbstract":"<h1>Summary</h1>\n<p>A puzzling tsunami entered Japanese history in January 1700. Samurai, merchants, and villagers wrote of minor flooding and damage. Some noted that no parent earthquake had been felt; they were wondering what had set off the waves. They had no way knowing that the tsunami had been spawned during an earthquake along the coast of northwestern North America. This orphan tsunami would not be linked to its parent earthquake until the middle 1990s, through an extraordinary series of discoveries in both North America and Japan.</p>\n<p><i>The Orphan Tsunami of 1700</i>, now in its second edition, tells this scientific detective story through its North American and Japanese clues. The discoveries underpin many of today&rsquo;s precautions against earthquakes and tsunamis in the Cascadia region of northwestern North America. The Japanese tsunami of March 2011 called attention to those hazards as a mirror image of the transpacific waves of January 1700.</p>","language":"English, Japanese","doi":"10.3133/pp1707","collaboration":"Prepared in cooperation with the Geological Survey of Japan (National Institute of Advanced Industrial Science and Technology), the University of Tokyo, and the University of Washington","usgsCitation":"Atwater, B.F., Musumi-Rokkaku, S., Satake, K., Tsuji, Y., Ueda, K., and Yamaguchi, D.K., 2015, The orphan tsunami of 1700—Japanese clues to a parent earthquake in North America, 2nd ed.: Seattle, University of Washington Press, U.S. Geological Survey Professional Paper 1707, 135 p.","productDescription":"vii, 135 p.","numberOfPages":"146","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":311372,"rank":16,"type":{"id":20,"text":"Read Me"},"url":"https://www.washington.edu/uwpress/search/books/ATWOR2.html","text":"A paperback copy of this book may be purchased from University of Washington Press"},{"id":311269,"rank":9,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_otsuchi.pdf","text":"Report Piece - Otsuchi","size":"4 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Otsuchi"},{"id":311268,"rank":8,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_tsugaruishi.pdf","text":"Report Piece - Tsugaruishi","size":"4.2 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Tsugaruishi"},{"id":311267,"rank":7,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_kuwagasaki.pdf","text":"Report Piece - Kuwagasaki","size":"5.8 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Kuwagasaki"},{"id":311266,"rank":6,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_part2.pdf","text":"Report Piece - Part 2","size":"5.5 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Part 2"},{"id":311265,"rank":5,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_part1.pdf","text":"Report Piece - Part 1","size":"10.4 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Part 1"},{"id":311264,"rank":4,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_front.pdf","text":"Report Piece - Front matter","size":"3.3 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Front matter"},{"id":311263,"rank":3,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_covers.pdf","text":"Report Piece - Covers","size":"685 KB","description":"PP 1707 PDF - Covers only"},{"id":311275,"rank":15,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_versionHist.txt"},{"id":7150,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707.pdf","text":"Full Report","size":"74.9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF- Full report"},{"id":311274,"rank":14,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_back.pdf","text":"Report Piece - Back matter","size":"6.3 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Back matter"},{"id":311273,"rank":13,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_part3.pdf","text":"Report Piece - Part 3","size":"4.1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Part 3"},{"id":311272,"rank":12,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_tanabe.pdf","text":"Report Piece - Tanabe","size":"4.2 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Tanabe"},{"id":311271,"rank":11,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_miho.pdf","text":"Report Piece - Miho","size":"6.7 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Miho"},{"id":311270,"rank":10,"type":{"id":2,"text":"Additional Report Piece"},"url":"https://pubs.usgs.gov/pp/pp1707/pp1707_nakaminato.pdf","text":"Report Piece - Nakaminato","size":"5.9 MB","linkFileType":{"id":1,"text":"pdf"},"description":"PP 1707 PDF - Nakaminato"},{"id":192813,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/pp1707/cover.jpg"}],"country":"Japan, United States","edition":"First Edition: Originally posted 2005; 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,{"id":72265,"text":"ofr20051271 - 2005 - Abstracts of the Annual Meeting of Planetary Geologic Mappers, Washington, D.C. 2005","interactions":[],"lastModifiedDate":"2018-09-19T19:01:27","indexId":"ofr20051271","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1271","title":"Abstracts of the Annual Meeting of Planetary Geologic Mappers, Washington, D.C. 2005","language":"ENGLISH","doi":"10.3133/ofr20051271","usgsCitation":"Tanaka, K.L., and Saunders, R.S., 2005, Abstracts of the Annual Meeting of Planetary Geologic Mappers, Washington, D.C. 2005 (Version 1.0): U.S. Geological Survey Open-File Report 2005-1271, 50 p., https://doi.org/10.3133/ofr20051271.","productDescription":"50 p.","costCenters":[],"links":[{"id":7137,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1271/","linkFileType":{"id":5,"text":"html"}},{"id":193140,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a38e5","contributors":{"editors":[{"text":"Gregg, Tracy K. P.","contributorId":57937,"corporation":false,"usgs":true,"family":"Gregg","given":"Tracy K. P.","affiliations":[],"preferred":false,"id":745707,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Tanaka, Kenneth L. ktanaka@usgs.gov","contributorId":610,"corporation":false,"usgs":true,"family":"Tanaka","given":"Kenneth","email":"ktanaka@usgs.gov","middleInitial":"L.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":true,"id":285299,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saunders, R. Stephen","contributorId":70842,"corporation":false,"usgs":true,"family":"Saunders","given":"R.","email":"","middleInitial":"Stephen","affiliations":[],"preferred":false,"id":285301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72281,"text":"sir20055041 - 2005 - Foreign Nonindigenous Carps and Minnows (Cyprinidae) in the United States - A Guide to their Identification, Distribution, and Biology","interactions":[],"lastModifiedDate":"2018-07-11T09:12:32","indexId":"sir20055041","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-5041","title":"Foreign Nonindigenous Carps and Minnows (Cyprinidae) in the United States - A Guide to their Identification, Distribution, and Biology","language":"ENGLISH","doi":"10.3133/sir20055041","usgsCitation":"Schofield, P., Williams, J.D., Nico, L.G., Fuller, P.L., and Thomas, M.R., 2005, Foreign Nonindigenous Carps and Minnows (Cyprinidae) in the United States - A Guide to their Identification, Distribution, and Biology: U.S. Geological Survey Scientific Investigations Report 2005-5041, 103 p., https://doi.org/10.3133/sir20055041.","productDescription":"103 p.","startPage":"0","endPage":"103","costCenters":[{"id":275,"text":"Florida Integrated Science Center","active":false,"usgs":true}],"links":[{"id":254727,"rank":200,"type":{"id":15,"text":"Index Page"},"url":"https://archive.usgs.gov/archive/sites/fl.biology.usgs.gov/Carp_ID/index.html","linkFileType":{"id":5,"text":"html"}},{"id":192814,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":355597,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://archive.usgs.gov/archive/sites/fl.biology.usgs.gov/sir2005_5041_report_LowRez.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de450","contributors":{"authors":[{"text":"Schofield, Pamela J. 0000-0002-8752-2797","orcid":"https://orcid.org/0000-0002-8752-2797","contributorId":30306,"corporation":false,"usgs":true,"family":"Schofield","given":"Pamela J.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":true,"id":285346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, James D.","contributorId":17690,"corporation":false,"usgs":false,"family":"Williams","given":"James","email":"","middleInitial":"D.","affiliations":[{"id":12556,"text":"Florida Fish and Wildlife Conservation Commission","active":true,"usgs":false}],"preferred":false,"id":285344,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nico, Leo G. 0000-0002-4488-7737 lnico@usgs.gov","orcid":"https://orcid.org/0000-0002-4488-7737","contributorId":2913,"corporation":false,"usgs":true,"family":"Nico","given":"Leo","email":"lnico@usgs.gov","middleInitial":"G.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":285342,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fuller, Pamela L. 0000-0002-9389-9144 pfuller@usgs.gov","orcid":"https://orcid.org/0000-0002-9389-9144","contributorId":3217,"corporation":false,"usgs":true,"family":"Fuller","given":"Pamela","email":"pfuller@usgs.gov","middleInitial":"L.","affiliations":[{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true}],"preferred":false,"id":285343,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Thomas, Matthew R.","contributorId":25650,"corporation":false,"usgs":true,"family":"Thomas","given":"Matthew","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":285345,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72267,"text":"ofr20051290 - 2005 - Pacific Island Ecosystems Research Center: Annotated Bibliography 1994 - 2004","interactions":[],"lastModifiedDate":"2013-05-23T10:02:24","indexId":"ofr20051290","displayToPublicDate":"2005-09-19T00:00:00","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":"2005-1290","title":"Pacific Island Ecosystems Research Center: Annotated Bibliography 1994 - 2004","language":"ENGLISH","doi":"10.3133/ofr20051290","usgsCitation":"Helweg, D.A., 2005, Pacific Island Ecosystems Research Center: Annotated Bibliography 1994 - 2004: U.S. Geological Survey Open-File Report 2005-1290, 86 p., https://doi.org/10.3133/ofr20051290.","productDescription":"86 p.","temporalStart":"1994-01-01","temporalEnd":"2004-12-31","costCenters":[{"id":521,"text":"Pacific Island Ecosystems Research Center","active":false,"usgs":true}],"links":[{"id":193142,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20051290.GIF"},{"id":272653,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/2005/1290/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d78","contributors":{"authors":[{"text":"Helweg, David A. (compiler)","contributorId":8943,"corporation":false,"usgs":true,"family":"Helweg","given":"David","suffix":"(compiler)","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":285310,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70209133,"text":"70209133 - 2005 - Using laser technology to characterize substrate morphology and Geology of selected lake trout spawing habitat in Northern Lake Michigan","interactions":[],"lastModifiedDate":"2020-03-18T10:33:46","indexId":"70209133","displayToPublicDate":"2005-09-18T10:29:29","publicationYear":"2005","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":718,"text":"American Fisheries Society Symposium","active":true,"publicationSubtype":{"id":10}},"title":"Using laser technology to characterize substrate morphology and Geology of selected lake trout spawing habitat in Northern Lake Michigan","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Fisheries Society","usgsCitation":"Barnes, P.W., Fleischer, G.W., Gardner, J.V., and Lee, K.M., 2005, Using laser technology to characterize substrate morphology and Geology of selected lake trout spawing habitat in Northern Lake Michigan: American Fisheries Society Symposium, v. 41, p. 165-169.","productDescription":"5 p.","startPage":"165","endPage":"169","costCenters":[],"links":[{"id":373342,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":373341,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://fisheries.org/bookstore/all-titles/afs-symposia/x54041xm/"}],"country":"United States","otherGeospatial":"Northern Lake Michigan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.0224609375,\n              43.929549935614595\n            ],\n            [\n              -85.869140625,\n              43.929549935614595\n            ],\n            [\n              -84.3310546875,\n              45.55252525134013\n            ],\n            [\n              -84.8583984375,\n              46.28622391806706\n            ],\n            [\n              -86.3525390625,\n              46.28622391806706\n            ],\n            [\n              -87.4951171875,\n              45.920587344733654\n            ],\n            [\n              -88.2861328125,\n              44.77793589631623\n            ],\n            [\n              -88.0224609375,\n              43.929549935614595\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"41","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Barnes, Peter W.","contributorId":223441,"corporation":false,"usgs":false,"family":"Barnes","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":785056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleischer, Guy W.","contributorId":89478,"corporation":false,"usgs":true,"family":"Fleischer","given":"Guy","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":785057,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gardner, James V.","contributorId":93035,"corporation":false,"usgs":true,"family":"Gardner","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":785058,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lee, Kristen M.","contributorId":49855,"corporation":false,"usgs":true,"family":"Lee","given":"Kristen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":785059,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":72236,"text":"sir20055161 - 2005 - Hydrogeology and ground-water availability in the carbonate aquifer system of Frederick County, Virginia","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"sir20055161","displayToPublicDate":"2005-09-17T00:00:00","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":"2005-5161","title":"Hydrogeology and ground-water availability in the carbonate aquifer system of Frederick County, Virginia","docAbstract":"The carbonate aquifer system of the northern Shenandoah Valley provides an important water supply to local communities, including Frederick County, Va., which depends on ground water as a source of water supply. The county and surrounding area are undergoing increased urbanization, and increased demands on the carbonate aquifer system are expected. A study was conducted between October 2000 and March 2004 by the U.S. Geological Survey (USGS), in cooperation with the County of Frederick, Va., to describe the hydrogeology and ground-water availability in the carbonate aquifer system underlying the county. The study area encompasses about 25 percent (105 square miles) of the county that is underlain by carbonate bedrock. \r\n\r\nThe carbonate aquifer system of Frederick County is in the Shenandoah Valley region of the Valley and Ridge Physiographic Province. Approximately 10,000 feet of folded and fractured Middle Cambrian to Upper Ordovician sedimentary rocks are exposed and are overlain by Pleistocene (?) and Holocene surficial deposits. All geologic units in the study area are considered to be aquifers. The geologic units are generally unconfined, fractured-rock aquifers that are recharged by precipitation and discharge locally to streams and springs, and by evapotranspiration.\r\n\r\nStream density in the carbonate study area is less than in the remainder of the county, which is underlain by siliciclastic rock units. Most streams flow normal to strike (from the northwest towards the southeast) across the study area. These streams are characterized by shallow incisement and are usually limited to a single stream channel. In the southern third of the study area, streams flow parallel to strike (from the northeast towards the southwest) towards the deeply intrenched Cedar Creek. Springs are commonly located at the start of flows for all streams in the carbonate study area, and spring discharges are often a large portion of the streamflow (especially during drought conditions).\r\n\r\nThe general direction of ground-water flow is from the hills in the west of the study area into and across the carbonate valley. A ground-water divide may occur north of Round Hill in the vicinity of the Apple Pie Ridge fault where the North Mountain fault zone cuts out the resistant Silurian and Devonian sandstone units and results in surface drainage from the carbonate rocks toward the west and out of the carbonate valley.\r\n\r\nEstimates of effective ground-water recharge for 2001-02 range from 5.8 to 6.2 inches in the Cedar Creek Basin, with base flow accounting for between 60 and 64 percent of streamflow, and from 3.2 to 3.8 inches in the Opequon Creek Basin, with base flow accounting for between 86 and 92 percent of streamflow.\r\n\r\nWater budgets calculated for 2001, a year of below-normal precipitation (33.1 inches), and 2002, a year of above-normal precipitation (41.2 inches), include a streamflow of 9.0 inches in 2001 and 9.2 inches in 2002 in Cedar Creek. Evapotranspiration ranged from 25.9 to 30.7 inches, and ground-water storage decreased 1.8 inches in 2001 and increased 1.3 inches in 2002. Streamflow was 3.7 inches in 2001 and 2002 in Opequon Creek. Evapotranspiration ranged from 29.8 to 37.5 inches, and ground-water storage decreased 0.4 inch in 2001 and did not change in 2002.","language":"ENGLISH","doi":"10.3133/sir20055161","usgsCitation":"Harlow, G., Orndorff, R.C., Nelms, D.L., Weary, D.J., and Moberg, R.M., 2005, Hydrogeology and ground-water availability in the carbonate aquifer system of Frederick County, Virginia: U.S. Geological Survey Scientific Investigations Report 2005-5161, v, 30 p. : ill.; maps, https://doi.org/10.3133/sir20055161.","productDescription":"v, 30 p. : ill.; maps","costCenters":[],"links":[{"id":192830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":7058,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5161/","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.13333333333334,39 ], [ -79.13333333333334,39.833333333333336 ], [ -78,39.833333333333336 ], [ -78,39 ], [ -79.13333333333334,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6276a1","contributors":{"authors":[{"text":"Harlow, George E. Jr. geharlow@usgs.gov","contributorId":383,"corporation":false,"usgs":true,"family":"Harlow","given":"George E.","suffix":"Jr.","email":"geharlow@usgs.gov","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true}],"preferred":false,"id":285221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Orndorff, Randall C. 0000-0002-8956-5803 rorndorf@usgs.gov","orcid":"https://orcid.org/0000-0002-8956-5803","contributorId":2739,"corporation":false,"usgs":true,"family":"Orndorff","given":"Randall","email":"rorndorf@usgs.gov","middleInitial":"C.","affiliations":[{"id":40020,"text":"Florence Bascom Geoscience Center","active":true,"usgs":true},{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true},{"id":243,"text":"Eastern Geology and Paleoclimate Science Center","active":true,"usgs":true}],"preferred":true,"id":285224,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nelms, David L. 0000-0001-5747-642X dlnelms@usgs.gov","orcid":"https://orcid.org/0000-0001-5747-642X","contributorId":1892,"corporation":false,"usgs":true,"family":"Nelms","given":"David","email":"dlnelms@usgs.gov","middleInitial":"L.","affiliations":[{"id":614,"text":"Virginia Water Science Center","active":true,"usgs":true},{"id":37759,"text":"VA/WV Water Science Center","active":true,"usgs":true}],"preferred":true,"id":285223,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"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":285222,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Moberg, Roger M. rmmoberg@usgs.gov","contributorId":3655,"corporation":false,"usgs":true,"family":"Moberg","given":"Roger","email":"rmmoberg@usgs.gov","middleInitial":"M.","affiliations":[],"preferred":true,"id":285225,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":72235,"text":"fs20053104 - 2005 - A NOAA-USGS demonstration flash-flood and debris-flow early-warning system","interactions":[],"lastModifiedDate":"2012-02-02T00:14:02","indexId":"fs20053104","displayToPublicDate":"2005-09-17T00:00:00","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":"2005-3104","title":"A NOAA-USGS demonstration flash-flood and debris-flow early-warning system","language":"ENGLISH","doi":"10.3133/fs20053104","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, A NOAA-USGS demonstration flash-flood and debris-flow early-warning system (Version 1.0): U.S. Geological Survey Fact Sheet 2005-3104, 2 p., https://doi.org/10.3133/fs20053104.","productDescription":"2 p.","costCenters":[],"links":[{"id":7057,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3104/","linkFileType":{"id":5,"text":"html"}},{"id":122330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3104.jpg"}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd495de4b0b290850ef1a1","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":534734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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