The Nottawaseppi Huron Band of Potawatomi Indians in Calhoun County, Michigan is concerned about the water quality and quantity of streams in and around tribal lands and of shallow ground water. The tribe wanted to establish a database that included streamflow, stage, and water quality of local streams and quality of ground water from wells belonging to the tribe and its members. Concerned about the effects of long-term agricultural activity and increasing numbers of singlefamily dwellings being constructed within the watershed both on and off the reservation, the tribe wants to develop a water-resources management plan.
U.S. Geological Survey (USGS) measured streamflow and installed staff gages tied into local datum on three tributaries of the St. Joseph River that cross tribal lands. Water-quality samples were collected from the sites under a variety of flow regimes from spring to fall during 2000-03. Stage-streamflow rating curves were constructed for Pine Creek and Athens & Indian Creek Drain after a number of discharge measurements were made and a thorough basin analysis was completed. Daily streamflow for Pine Creek near Athens was estimated for the period from May 2000 through September 2003.
USGS collected 12 water samples at Pine Creek near Athens, Athens & Indian Creek Drain, and an unnamed tributary to Pine Creek during October 2000 through September 2003. Physical properties were measured, and the streams were sampled for major ions, nutrients, trace elements, caffeine, and herbicides/pesticides and their breakdown products (degradates). The tribe also measured physical properties weekly at the three sites during each growing season for the study period. Surface water at the three sites can be classified as hard, with calcium carbonate concentrations exceeding 180 milligrams per liter (mg/L). Concentrations of calcium, magnesium, chloride, and dissolved solids are typical of the area. There were 68 detections of 17 pesticides, degradates, and caffeine. Atrazine and metolachlor were detected in all samples, and the atrazine degradate deethylatrazine was detected in all samples from Pine Creek and Athens & Indian Creek Drain. Another atrazine degradate (2-hydroxy-atrazine, or OIET) was detected five of the six times that it was included in the analyses. A single sample collected from Athens & Indian Creek Drain in May 2001 had relatively higher concentrations of acetochlor, atrazine, CIAT (deethylatrazine), and diuron than the other sampling sites did during the study. Analysis for various species of mercury was completed on samples collected at Pine Creek and Athens & Indian Creek Drain in July 2003, and results were similar to those typical of unimpaired streams in the Midwest. None of the surface-water sites had major ion, nutrient, or trace-element concentrations that exceeded Michigan Department of Environmental Quality standards for nonpotable surface water.
USGS also collected 11 ground-water samples from 7 wells on or adjacent to the traditional reservation in 2003. Two wells were sampled twice, and a single well was sampled three times, in order to document any chemical changes that might have occurred as a result of aquifer recharge, which most typically occurs in late winter to spring in the southern Lower Peninsula of Michigan. Samples were analyzed for 184 pesticides and degradates and caffeine. There were five detections of four pesticides or degradates, but none of the detected chemicals are included in current U.S. Environmental Protection Agency drinking-water standards. The remaining 181 analytes were below laboratory reporting limits.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041406","collaboration":"Prepared in cooperation with the Nottawaseppi Huron Band of Potawatomi Indians","usgsCitation":"Weaver, T.L., Healy, D., and Sabin, T., 2005, Water resources on and near the Nottawaseppi Huron band of Potawatomi indian tribal lands, Calhoun County, Michigan, 2000-03: U.S. Geological Survey Open-File Report 2004-1406, ix, 40 p., https://doi.org/10.3133/ofr20041406.","productDescription":"ix, 40 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":193281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041406.JPG"},{"id":6667,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1406/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Michigan","county":"Calhoun County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.308333,\n 42.158333\n ],\n [\n -85.308333,\n 42.066667\n ],\n [\n -85.220833,\n 42.066667\n ],\n [\n -85.220833,\n 42.158333\n ],\n [\n -85.308333,\n 42.158333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efd37","contributors":{"authors":[{"text":"Weaver, T. L.","contributorId":24339,"corporation":false,"usgs":true,"family":"Weaver","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Healy, D.","contributorId":101754,"corporation":false,"usgs":true,"family":"Healy","given":"D.","affiliations":[],"preferred":false,"id":282938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sabin, T.G.","contributorId":42310,"corporation":false,"usgs":true,"family":"Sabin","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":282937,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70716,"text":"sir20055040 - 2005 - Comparison of preconstruction and 2003 bathymetric and topographic surveys of Lake McConaughy, Nebraska","interactions":[],"lastModifiedDate":"2022-01-07T19:39:04.856421","indexId":"sir20055040","displayToPublicDate":"2005-06-18T00:00:00","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":"2005-5040","title":"Comparison of preconstruction and 2003 bathymetric and topographic surveys of Lake McConaughy, Nebraska","docAbstract":"The U.S. Geological Survey, in cooperation with The Central Nebraska Public Power and Irrigation District, conducted a study that used bathymetric and topographic surveying in conjunction with Geographical Information Systems techniques to determine the 2003 physical shape, current storage capacity, and the changes in storage capacity of Lake McConaughy that have occurred over the past 62 years. By combining the bathymetric and topographic survey data, the current surface area of Lake McConaughy was determined to be 30,413.0 acres, with a volume of 1,756,300 acre-feet at the lake conservation-pool elevation of 3,266.4 feet above North American Vertical Datum of 1988 (3,265.0 feet above Central datum). To determine the changes in storage of Lake McConaughy, the 2003 survey Digital Elevation Model (DEM) was compared to a preconstruction DEM compiled from historical contour maps. This comparison showed an increase in elevation at the dam site due to the installation of Kingsley Dam. Immediately to the west of the Kingsley Dam is an area of decline where a borrow pit for Kingsley Dam was excavated. The comparison of the preconstruction survey to the 2003 survey also was used to estimate the gross storage capacity reduction that occurred between 1941 and 2002. The results of this comparison indicate a gross storage capacity reduction of approximately 42,372 acre-feet, at the lake conservation-pool elevation of 3,266.4 feet in NAVD 88 (3,265.0 feet in Central datum). By comparing preconstruction and 2003 survey data and subtracting the Kingsley Dam and borrow pit, the total estimated net volume of sediment deposited over the past 62 years is 53,347,124 cubic yards, at an annual average rate of 860,437 cubic yards per year. The approximate decrease in the net storage capacity occurring over the past 62 years is 33,066 acre-feet, at an annual average decrease of approximately 533 acre-feet per year, which has resulted in a 1.8 percent decrease in storage capacity of Lake McConaughy. The lake has accumulated most of the sediment in the original river channel and in the west end of the delta area on the upstream end of the lake.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055040","usgsCitation":"Kress, W.H., Sebree, S.K., Littin, G.R., Drain, M.A., and Kling, M.E., 2005, Comparison of preconstruction and 2003 bathymetric and topographic surveys of Lake McConaughy, Nebraska: U.S. Geological Survey Scientific Investigations Report 2005-5040, 27 p., https://doi.org/10.3133/sir20055040.","productDescription":"27 p.","costCenters":[],"links":[{"id":192728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":394047,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_72215.htm"},{"id":6664,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5040/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Nebraska","otherGeospatial":"Lake McConaughy","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102.01080322265624,\n 41.192089674364105\n ],\n [\n -101.65374755859375,\n 41.192089674364105\n ],\n [\n -101.65374755859375,\n 41.31701278537454\n ],\n [\n -102.01080322265624,\n 41.31701278537454\n ],\n [\n -102.01080322265624,\n 41.192089674364105\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae2ae","contributors":{"authors":[{"text":"Kress, Wade H.","contributorId":100475,"corporation":false,"usgs":true,"family":"Kress","given":"Wade","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":282933,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sebree, Sonja K.","contributorId":36622,"corporation":false,"usgs":true,"family":"Sebree","given":"Sonja","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":282932,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Littin, Gregory R. grlittin@usgs.gov","contributorId":1732,"corporation":false,"usgs":true,"family":"Littin","given":"Gregory","email":"grlittin@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":282929,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Drain, Michael A.","contributorId":29526,"corporation":false,"usgs":true,"family":"Drain","given":"Michael","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282930,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kling, Michael E.","contributorId":35409,"corporation":false,"usgs":true,"family":"Kling","given":"Michael","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282931,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70720,"text":"ofr20041417 - 2005 - Water resources data, Oakland County, Michigan 2001-2004","interactions":[],"lastModifiedDate":"2017-11-10T19:15:51","indexId":"ofr20041417","displayToPublicDate":"2005-06-18T00:00:00","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":"2004-1417","title":"Water resources data, Oakland County, Michigan 2001-2004","docAbstract":"The U.S. Geological Survey (USGS), in cooperation with Oakland County, the Huron-Clinton Metropark Authority, the Michigan Department of Environmental Quality (MDEQ), and the Rouge Program Office, collected streamflow, water-quality, and ground-water-level data in watersheds across Oakland County during water years 2001, 2002, 2003, and 2004. Water years begin October 1 and end September 30.
\nThis report presents water resources data used to produce a series of interpretive reports on the quantity and quality of water in Oakland County for Oakland County, Michigan. Some of these data have been published elsewhere, but are provided here in one report. This report has two main sections. The first section provides an overview of the methods used to collect the various types of data. The second section is a series of data tables containing ground-water-level data, synoptically measured stream-water-quality data, synoptically measured lake-water-quality data, and the results of a macroinvertebrate and habitat assessment.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041417","collaboration":"In cooperation with Oakland County, Michigan","usgsCitation":"Aichele, S., Crowley, S.L., Tariska, C., and Stopar, J., 2005, Water resources data, Oakland County, Michigan 2001-2004: U.S. Geological Survey Open-File Report 2004-1417, iv, 75 p., https://doi.org/10.3133/ofr20041417.","productDescription":"iv, 75 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":192517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20041417.JPG"},{"id":6668,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1417/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Michigan","county":"Oakland County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-83.4546,42.8798],[-83.2227,42.887],[-83.1025,42.8884],[-83.0986,42.801],[-83.0905,42.6238],[-83.0867,42.5355],[-83.0843,42.4463],[-83.3264,42.4416],[-83.4403,42.4393],[-83.553,42.4351],[-83.6669,42.4312],[-83.6733,42.5196],[-83.6863,42.7822],[-83.6902,42.871],[-83.5737,42.8744],[-83.4541,42.8766],[-83.4546,42.8798]]]},\"properties\":{\"name\":\"Oakland\",\"state\":\"MI\"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0d5d","contributors":{"authors":[{"text":"Aichele, Stephen S. 0000-0002-3397-7921 saichele@usgs.gov","orcid":"https://orcid.org/0000-0002-3397-7921","contributorId":194508,"corporation":false,"usgs":true,"family":"Aichele","given":"Stephen S.","email":"saichele@usgs.gov","affiliations":[{"id":430,"text":"National Mapping Program","active":false,"usgs":true}],"preferred":false,"id":282941,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crowley, S. L.","contributorId":77614,"corporation":false,"usgs":true,"family":"Crowley","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282942,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tariska, C.K.","contributorId":26380,"corporation":false,"usgs":true,"family":"Tariska","given":"C.K.","email":"","affiliations":[],"preferred":false,"id":282939,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stopar, J.","contributorId":26381,"corporation":false,"usgs":true,"family":"Stopar","given":"J.","affiliations":[],"preferred":false,"id":282940,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70710,"text":"tm11B1 - 2005 - Selection of colors and patterns for geologic maps of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2018-01-04T09:39:43","indexId":"tm11B1","displayToPublicDate":"2005-06-17T00:00:00","publicationYear":"2005","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":335,"text":"Techniques and Methods","code":"TM","onlineIssn":"2328-7055","printIssn":"2328-7047","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"11-B1","title":"Selection of colors and patterns for geologic maps of the U.S. Geological Survey","docAbstract":"U.S. Geological Survey (USGS) color and pattern standards and conventions for geologic maps have evolved since the USGS published its first set of standards in 1881. Since that time, USGS personnel have continuously updated and revised the standards in response to the need to show increasingly complex geologic map data and in response to changing technology. The color and pattern standards and conventions contained in this book enable geologists, cartographers, and editors to produce geologic maps that have consistent geologic-age color schemes and patterns. Such consistency enables geologists and other users of geologic maps to obtain a wealth of geologic information at a glance and to produce maps that can easily be used and compared to other published maps that follow the color and pattern standards and conventions.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tm11B1","collaboration":"Modified and updated from USGS Technical Standards Paper No. 9.03.1, September 30, 1971","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2005, Selection of colors and patterns for geologic maps of the U.S. Geological Survey (Version 1.0): U.S. Geological Survey Techniques and Methods 11-B1, 19 p.; 1 plate, https://doi.org/10.3133/tm11B1.","productDescription":"19 p.; 1 plate","costCenters":[],"links":[{"id":350291,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2005/11B01/pdf/TM11-B1.pdf","text":"Report","size":"14.3 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":6660,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/tm/2005/11B01/","linkFileType":{"id":5,"text":"html"}},{"id":7847,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tm/2005/11B01/pdf/plate.pdf","size":"5.2 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":124842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tm_11_b1.gif"},{"id":350292,"rank":5,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tm/2005/11B01/05tm11b01.html","text":"Text-Only HTML Version","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a00e4b07f02db5f7db3","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":534702,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70702,"text":"wdrNM041 - 2005 - Water resources data, New Mexico, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:05","indexId":"wdrNM041","displayToPublicDate":"2005-06-16T00:00:00","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":"NM-04-1","title":"Water resources data, New Mexico, water year 2004","docAbstract":"Water-resources data for the 2004 water year for New Mexico consist of records of discharge and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality in wells and springs. This report contains discharge records for 185 gaging stations; stage and contents for 22 lakes and reservoirs; water quality for 39 gaging stations, 108 wells, and 9 partial-record stations and miscellaneous sites; and water levels at 128 observation wells. Also included are 80 crest-stage, partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program and are published as miscellaneous measurements. Two seepage investigations were made during the year. These data represent that part of the National Water Data System collected by the U.S. Geological Survey and cooperating Federal, State, and local agencies in New Mexico.","language":"ENGLISH","doi":"10.3133/wdrNM041","usgsCitation":"Byrd, D., Allen, H.R., and Montano, M., 2005, Water resources data, New Mexico, water year 2004: U.S. Geological Survey Water Data Report NM-04-1, 469 p., https://doi.org/10.3133/wdrNM041.","productDescription":"469 p.","costCenters":[],"links":[{"id":192712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6657,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2004/wdr-nm-04-1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f5e4b07f02db5f0f12","contributors":{"authors":[{"text":"Byrd, Dave","contributorId":59114,"corporation":false,"usgs":true,"family":"Byrd","given":"Dave","email":"","affiliations":[],"preferred":false,"id":282909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, Harriet R.","contributorId":94683,"corporation":false,"usgs":true,"family":"Allen","given":"Harriet","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":282910,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Montano, Mary","contributorId":102950,"corporation":false,"usgs":true,"family":"Montano","given":"Mary","email":"","affiliations":[],"preferred":false,"id":282911,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70703,"text":"sir20045262 - 2005 - Median and Low-Flow Characteristics for Streams under Natural and Diverted Conditions, Northeast Maui, Hawaii","interactions":[],"lastModifiedDate":"2012-03-08T17:16:18","indexId":"sir20045262","displayToPublicDate":"2005-06-16T00:00:00","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":"2004-5262","title":"Median and Low-Flow Characteristics for Streams under Natural and Diverted Conditions, Northeast Maui, Hawaii","docAbstract":"Flow-duration statistics under natural (undiverted) and diverted flow conditions were estimated for gaged and ungaged sites on 21 streams in northeast Maui, Hawaii. The estimates were made using the optimal combination of continuous-record gaging-station data, low-flow measurements, and values determined from regression equations developed as part of this study. Estimated 50- and 95-percent flow duration statistics for streams are presented and the analyses done to develop and evaluate the methods used in estimating the statistics are described. Estimated streamflow statistics are presented for sites where various amounts of streamflow data are available as well as for locations where no data are available.\r\n\r\nDaily mean flows were used to determine flow-duration statistics for continuous-record stream-gaging stations in the study area following U.S. Geological Survey established standard methods. Duration discharges of 50- and 95-percent were determined from total flow and base flow for each continuous-record station. The index-station method was used to adjust all of the streamflow records to a common, long-term period. The gaging station on West Wailuaiki Stream (16518000) was chosen as the index station because of its record length (1914-2003) and favorable geographic location. Adjustments based on the index-station method resulted in decreases to the 50-percent duration total flow, 50-percent duration base flow, 95-percent duration total flow, and 95-percent duration base flow computed on the basis of short-term records that averaged 7, 3, 4, and 1 percent, respectively.\r\n\r\nFor the drainage basin of each continuous-record gaged site and selected ungaged sites, morphometric, geologic, soil, and rainfall characteristics were quantified using Geographic Information System techniques. Regression equations relating the non-diverted streamflow statistics to basin characteristics of the gaged basins were developed using ordinary-least-squares regression analyses. Rainfall rate, maximum basin elevation, and the elongation ratio of the basin were the basin characteristics used in the final regression equations for 50-percent duration total flow and base flow. Rainfall rate and maximum basin elevation were used in the final regression equations for the 95-percent duration total flow and base flow. The relative errors between observed and estimated flows ranged from 10 to 20 percent for the 50-percent duration total flow and base flow, and from 29 to 56 percent for the 95-percent duration total flow and base flow.\r\n\r\nThe regression equations developed for this study were used to determine the 50-percent duration total flow, 50-percent duration base flow, 95-percent duration total flow, and 95-percent duration base flow at selected ungaged diverted and undiverted sites. Estimated streamflow, prediction intervals, and standard errors were determined for 48 ungaged sites in the study area and for three gaged sites west of the study area. Relative errors were determined for sites where measured values of 95-percent duration discharge of total flow were available. East of Keanae Valley, the 95-percent duration discharge equation generally underestimated flow, and within and west of Keanae Valley, the equation generally overestimated flow. Reduction in 50- and 95-percent flow-duration values in stream reaches affected by diversions throughout the study area average 58 to 60 percent.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/sir20045262","collaboration":"Prepared in cooperation with the State of Hawaii Commission on Water Resource Management","usgsCitation":"Gingerich, S.B., 2005, Median and Low-Flow Characteristics for Streams under Natural and Diverted Conditions, Northeast Maui, Hawaii: U.S. Geological Survey Scientific Investigations Report 2004-5262, Report: vi, 72 p.; Plate: 26 x 32 inches, https://doi.org/10.3133/sir20045262.","productDescription":"Report: vi, 72 p.; Plate: 26 x 32 inches","costCenters":[{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"links":[{"id":192713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6658,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5262/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db60ff43","contributors":{"authors":[{"text":"Gingerich, Stephen B. 0000-0002-4381-0746 sbginger@usgs.gov","orcid":"https://orcid.org/0000-0002-4381-0746","contributorId":1426,"corporation":false,"usgs":true,"family":"Gingerich","given":"Stephen","email":"sbginger@usgs.gov","middleInitial":"B.","affiliations":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":525,"text":"Pacific Islands Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282912,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70696,"text":"ofr20051186 - 2005 - Particle-size, CaCO3, chemical, magnetic, and age data from surficial deposits in and around Canyonlands National Park, Utah","interactions":[],"lastModifiedDate":"2026-02-03T16:58:36.072514","indexId":"ofr20051186","displayToPublicDate":"2005-06-14T00:00:00","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":"2005-1186","displayTitle":"Particle-Size, CaCO3, chemical, magnetic, and age data from surficial deposits in and around Canyonlands National Park, Utah","title":"Particle-size, CaCO3, chemical, magnetic, and age data from surficial deposits in and around Canyonlands National Park, Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20051186","usgsCitation":"Goldstein, H.L., Reynolds, R.L., Reheis, M.C., Yount, J., Lamothe, P., Roberts, H., and McGeehin, J., 2005, Particle-size, CaCO3, chemical, magnetic, and age data from surficial deposits in and around Canyonlands National Park, Utah (Version 1.0): U.S. Geological Survey Open-File Report 2005-1186, 201 p., https://doi.org/10.3133/ofr20051186.","productDescription":"201 p.","costCenters":[],"links":[{"id":192664,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6654,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1186/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adfea","contributors":{"authors":[{"text":"Goldstein, Harland L. 0000-0002-6092-8818 hgoldstein@usgs.gov","orcid":"https://orcid.org/0000-0002-6092-8818","contributorId":807,"corporation":false,"usgs":true,"family":"Goldstein","given":"Harland","email":"hgoldstein@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":282899,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reynolds, Richard L. 0000-0002-4572-2942 rreynolds@usgs.gov","orcid":"https://orcid.org/0000-0002-4572-2942","contributorId":139068,"corporation":false,"usgs":true,"family":"Reynolds","given":"Richard","email":"rreynolds@usgs.gov","middleInitial":"L.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":282905,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reheis, Marith C. 0000-0002-8359-323X mreheis@usgs.gov","orcid":"https://orcid.org/0000-0002-8359-323X","contributorId":1196,"corporation":false,"usgs":true,"family":"Reheis","given":"Marith","email":"mreheis@usgs.gov","middleInitial":"C.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":false,"id":282900,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Yount, James","contributorId":65172,"corporation":false,"usgs":true,"family":"Yount","given":"James","affiliations":[],"preferred":false,"id":282904,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lamothe, Paul","contributorId":18728,"corporation":false,"usgs":true,"family":"Lamothe","given":"Paul","affiliations":[],"preferred":false,"id":282901,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Roberts, Helen","contributorId":49878,"corporation":false,"usgs":true,"family":"Roberts","given":"Helen","affiliations":[],"preferred":false,"id":282903,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"McGeehin, John","contributorId":23235,"corporation":false,"usgs":true,"family":"McGeehin","given":"John","affiliations":[],"preferred":false,"id":282902,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}} ,{"id":70691,"text":"sim2814 - 2005 - Geologic and geophysical maps of the Las Vegas 30' x 60' quadrangle, Clark and Nye counties, Nevada, and Inyo County, California","interactions":[],"lastModifiedDate":"2017-01-24T13:56:13","indexId":"sim2814","displayToPublicDate":"2005-06-11T00:00:00","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":"2814","title":"Geologic and geophysical maps of the Las Vegas 30' x 60' quadrangle, Clark and Nye counties, Nevada, and Inyo County, California","docAbstract":"Las Vegas and Pahrump are two of the fastest growing cities in the US, and the shortage of water looms as among the greatest future problems for these cities. These new maps of the Las Vegas 30 x 60-minute quadrangle provide a geologic and geophysical framework and fundamental earth science database needed to address societal issues such as ground water supply and contamination, surface flood, landslide, and seismic hazards, and soil properties and their changing impact by and on urbanization.\r\n The mountain ranges surrounding Las Vegas and Pahrump consist of Mesozoic, Paleozoic and Proterozoic rocks. A majority of these rocks are Paleozoic carbonate rocks that are part of Nevada's carbonate rock aquifer province. The Spring Mountains represent a major recharge site in the province, where maximum altitude is 3,632 m (Charleston Peak) above sea level. Rocks in the Sheep and Las Vegas Ranges and Spring Mountains contain correlative, northeast-striking, southeast-verging thrust faults that are part of the Cretaceous, Sevier orogenic belt. These thrusts were offset during the Miocene by the Las Vegas Valley shear system (LVVSZ). We conducted new mapping in the Blue Diamond area, highlighting refined work on the Bird Spring thrust, newly studied ancient landslides, and gravity-slide blocks. We conducted new mapping in the Las Vegas Range and mapped previously unrecognized structures such as the Valley thrust and fold belt; recognition of these structures has led to a refined correlation of Mesozoic thrust faults across the LVVSZ. New contributions in the quadrangle also include a greatly refined stratigraphy of Paleozoic bedrock units based on conodont biostragraphy. We collected over 200 conodont samples in the quadrangle and established stratigraphic reference sections used to correlate units across the major Mesozoic thrust faults.\r\n Quaternary deposits cover about half of the map area and underlie most of the present urbanized area. Deposits consist of large coalescing alluvial fans that grade downslope to extensive areas of fine-grained sediment indicative of groundwater-discharge during the Pleistocene. In the central areas of Las Vegas and Pahrump valleys, Quaternary fault scarps associated with past ground-water discharge deposits suggest a genetic relationship. In collaboration with NBMG and University of Nevada, a variety of ages of gravelly alluvium are newly mapped using surficial characteristics and soil development, along with reassessment of previously published mapping during compilation. Reconnaissance geochronology (thermoluminescence and U-series) of eolian and authigenic components of surficial and buried soils and spring deposits is applied to test hypotheses of geomorphic and hydrologic response to climate change over the past 100 k.y.). The major structure in the Las Vegas quadrangle is the LVVSZ. Because the LVVSZ is concealed by thick basin-fill deposits of Quaternary and Tertiary age, it was characterized primarily based on geophysics. Likewise, the newly described State line fault system in Pahrump Valley has also been characterized by geophysics, where geophysically inferred structures correlate remarkably with surface structures defined by our new geologic mapping in the Mound Spring and Hidden Hills Ranch 7.5-minute quadrangles.","language":"English","doi":"10.3133/sim2814","usgsCitation":"Page, W.R., Lundstrom, S.C., Harris, A.G., Langenheim, V., Workman, J.B., Mahan, S., Paces, J.B., Dixon, G.L., Rowley, P.D., Burchfiel, B., Bell, J.W., and Smith, E.I., 2005, Geologic and geophysical maps of the Las Vegas 30' x 60' quadrangle, Clark and Nye counties, Nevada, and Inyo County, California (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2814, 58 p.; 2 sheets, https://doi.org/10.3133/sim2814.","productDescription":"58 p.; 2 sheets","costCenters":[],"links":[{"id":186634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6745,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2814/","linkFileType":{"id":5,"text":"html"}},{"id":110565,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71661.htm","linkFileType":{"id":5,"text":"html"},"description":"71661"}],"scale":"5000000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8263","contributors":{"authors":[{"text":"Page, William R. 0000-0002-0722-9911 rpage@usgs.gov","orcid":"https://orcid.org/0000-0002-0722-9911","contributorId":1628,"corporation":false,"usgs":true,"family":"Page","given":"William","email":"rpage@usgs.gov","middleInitial":"R.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":282883,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lundstrom, Scott C. 0000-0003-4149-2219 sclundst@usgs.gov","orcid":"https://orcid.org/0000-0003-4149-2219","contributorId":2446,"corporation":false,"usgs":true,"family":"Lundstrom","given":"Scott","email":"sclundst@usgs.gov","middleInitial":"C.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":282884,"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":282890,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Langenheim, Victoria E. 0000-0003-2170-5213 zulanger@usgs.gov","orcid":"https://orcid.org/0000-0003-2170-5213","contributorId":1526,"corporation":false,"usgs":true,"family":"Langenheim","given":"Victoria E.","email":"zulanger@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":false,"id":282882,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Workman, Jeremiah B. 0000-0001-7816-6420 jworkman@usgs.gov","orcid":"https://orcid.org/0000-0001-7816-6420","contributorId":714,"corporation":false,"usgs":true,"family":"Workman","given":"Jeremiah","email":"jworkman@usgs.gov","middleInitial":"B.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":282880,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mahan, Shannon 0000-0001-5214-7774 smahan@usgs.gov","orcid":"https://orcid.org/0000-0001-5214-7774","contributorId":1215,"corporation":false,"usgs":true,"family":"Mahan","given":"Shannon","email":"smahan@usgs.gov","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":282881,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Paces, James B. 0000-0002-9809-8493 jbpaces@usgs.gov","orcid":"https://orcid.org/0000-0002-9809-8493","contributorId":2514,"corporation":false,"usgs":true,"family":"Paces","given":"James","email":"jbpaces@usgs.gov","middleInitial":"B.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":282885,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Dixon, Gary L.","contributorId":23571,"corporation":false,"usgs":true,"family":"Dixon","given":"Gary","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":282886,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Rowley, Peter D.","contributorId":27435,"corporation":false,"usgs":true,"family":"Rowley","given":"Peter","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":282887,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Burchfiel, B.C.","contributorId":30262,"corporation":false,"usgs":true,"family":"Burchfiel","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":282888,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Bell, John W.","contributorId":61411,"corporation":false,"usgs":true,"family":"Bell","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":282891,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Smith, Eugene I.","contributorId":35185,"corporation":false,"usgs":true,"family":"Smith","given":"Eugene","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":282889,"contributorType":{"id":1,"text":"Authors"},"rank":12}]}} ,{"id":70693,"text":"wdrFL041A - 2005 - Water resources data for Florida water year 2004volume 1A. northeast Florida surface water","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"wdrFL041A","displayToPublicDate":"2005-06-11T00:00:00","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":"FL-04-1A","title":"Water resources data for Florida water year 2004volume 1A. northeast Florida surface water","docAbstract":"Water resources data for the 2004 water year in Florida consist of continuous or daily discharge for 405 streams, periodic discharge for 12 streams, continuous or daily stage for 159 streams, periodic stage for 19 streams, peak stage and discharge for 30 streams; continuous or daily elevations for 14 lakes, periodic elevations for 23 lakes; continuous ground-water levels for 408 wells, periodic ground-water levels for 1,157 wells; quality-of-water data for 140 surface-water sites and 239 wells.\r\n\r\nThe data for northeast Florida include continuous or daily discharge for 140 streams, periodic discharge for 4 streams, continuous or daily stage for 58 streams, periodic stage for 3 streams; peak stage and discharge for 0 streams; continuous or daily elevations for 10 lakes, periodic elevations for 20 lakes; continuous ground water levels for 50 wells, periodic ground-water levels for 522 wells; quality-of-water data for 40 surface-water sites and 66 wells.\r\n\r\nThese data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, State and Federal agencies in Florida.","language":"ENGLISH","doi":"10.3133/wdrFL041A","usgsCitation":"Herrett, T.A., Hess, G.W., House, J.G., Ruppert, G.P., and Courts, M., 2005, Water resources data for Florida water year 2004volume 1A. northeast Florida surface water: U.S. Geological Survey Water Data Report FL-04-1A, 401 p., https://doi.org/10.3133/wdrFL041A.","productDescription":"401 p.","costCenters":[],"links":[{"id":6747,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-fl-04-1a/","linkFileType":{"id":5,"text":"html"}},{"id":185504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49b8e4b07f02db5cd2a6","contributors":{"authors":[{"text":"Herrett, Thomas A. herrett@usgs.gov","contributorId":3505,"corporation":false,"usgs":true,"family":"Herrett","given":"Thomas","email":"herrett@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":282894,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Glen W.","contributorId":19136,"corporation":false,"usgs":true,"family":"Hess","given":"Glen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":282895,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"House, Jon G.","contributorId":85266,"corporation":false,"usgs":true,"family":"House","given":"Jon","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":282897,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ruppert, Gregory P.","contributorId":46616,"corporation":false,"usgs":true,"family":"Ruppert","given":"Gregory","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282896,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Courts, Mary-Lorraine","contributorId":104151,"corporation":false,"usgs":true,"family":"Courts","given":"Mary-Lorraine","email":"","affiliations":[],"preferred":false,"id":282898,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70684,"text":"ofr20051172 - 2005 - The New Hampshire watershed tool: a geographic information system tool to estimate streamflow statistics and ground-water-recharge rates","interactions":[],"lastModifiedDate":"2012-02-02T00:13:44","indexId":"ofr20051172","displayToPublicDate":"2005-06-07T00:00:00","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":"2005-1172","title":"The New Hampshire watershed tool: a geographic information system tool to estimate streamflow statistics and ground-water-recharge rates","docAbstract":"Estimates of low-flow statistics, flow durations, and ground-water-recharge rates are needed to assist water-resource managers in assessing surface-water resources and ground-water availability. Often these estimates are required at ungaged sites where no observed streamflow data are available for analysis. Regression equations for estimating low-flow statistics and flow durations, and for estimating ground-water-recharge rates at ungaged sites have been developed for New Hampshire. However, use of these equations requires numerous input parameters, such as basin and climatic characteristics. This report describes a customized geographic information system (GIS) application, the New Hampshire Watershed Tool, that automates the measurement of the characteristics used for input to the regression equations and calculates the corresponding flow statistics and ground-water-recharge rates.","language":"ENGLISH","doi":"10.3133/ofr20051172","usgsCitation":"Olson, S.A., Flynn, R.H., Johnston, C.M., and Tasker, G.D., 2005, The New Hampshire watershed tool: a geographic information system tool to estimate streamflow statistics and ground-water-recharge rates (Online only): U.S. Geological Survey Open-File Report 2005-1172, 20 p., https://doi.org/10.3133/ofr20051172.","productDescription":"20 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":185652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6718,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2005-1172/","linkFileType":{"id":5,"text":"html"}}],"edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67af8f","contributors":{"authors":[{"text":"Olson, Scott A. 0000-0002-1064-2125 solson@usgs.gov","orcid":"https://orcid.org/0000-0002-1064-2125","contributorId":2059,"corporation":false,"usgs":true,"family":"Olson","given":"Scott","email":"solson@usgs.gov","middleInitial":"A.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282871,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flynn, Robert H. rflynn@usgs.gov","contributorId":2137,"corporation":false,"usgs":true,"family":"Flynn","given":"Robert","email":"rflynn@usgs.gov","middleInitial":"H.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282872,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnston, Craig M. cmjohnst@usgs.gov","contributorId":1814,"corporation":false,"usgs":true,"family":"Johnston","given":"Craig","email":"cmjohnst@usgs.gov","middleInitial":"M.","affiliations":[{"id":405,"text":"NH/VT office of New England Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282870,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tasker, Gary D.","contributorId":95035,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":282873,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70676,"text":"ofr20051171 - 2005 - Vitrinite reflectance data for the Permian Basin, west Texas and southeast New Mexico","interactions":[],"lastModifiedDate":"2017-03-02T13:13:27","indexId":"ofr20051171","displayToPublicDate":"2005-06-06T00:00:00","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":"2005-1171","title":"Vitrinite reflectance data for the Permian Basin, west Texas and southeast New Mexico","docAbstract":"This report presents a compilation of vitrinite reflectance (Ro) data based on analyses of samples of drill cuttings collected from 74 boreholes spread throughout the Permian Basin of west Texas and southeast New Mexico (fig. 1). The resulting data consist of 3 to 24 individual Ro analyses representing progressively deeper stratigraphic units in each of the boreholes (table 1). The samples, Cambrian-Ordovician to Cretaceous in age, were collected at depths ranging from 200 ft to more than 22,100 ft.
The R0 data were plotted on maps that depict three different maturation levels for organic matter in the sedimentary rocks of the Permian Basin (figs. 2-4). These maps show depths at the various borehole locations where the R0 values were calculated to be 0.6 (fig. 2), 1.3 (fig. 3), and 2.0 (fig. 4) percent, which correspond, generally, to the onset of oil generation, the onset of oil cracking, and the limit of oil preservation, respectively.
The four major geologic structural features within the Permian Basin–Midland Basin, Delaware Basin, Central Basin Platform, and Northwest Shelf (fig. 1) differ in overall depth, thermal history and tectonic style. In the western Delaware Basin, for example, higher maturation is observed at relatively shallow depths, resulting from uplift and eastward basin tilting that began in the Mississippian and ultimately exposed older, thermally mature rocks. Maturity was further enhanced in this basin by the emplacement of early and mid-Tertiary intrusives. Volcanic activity also appears to have been a controlling factor for maturation of organic matter in the southern part of the otherwise tectonically stable Northwest Shelf (Barker and Pawlewicz, 1987). Depths to the three different Ro values are greatest in the eastern Delaware Basin and southern Midland Basin. This appears to be a function of tectonic activity related to the Marathon-Ouachita orogeny, during the Late-Middle Pennsylvanian, whose affects were widespread across the Permian Basin. The Central Basin Platform has been a positive feature since the mid to-late Paleozoic, during which time sedimentation occurred along its flanks. This nonsubsidence, along with the lack of supplemental heating (volcanism), implies lower maturation levels.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20051171","usgsCitation":"Pawlewicz, M., Barker, C., and McDonald, S., 2005, Vitrinite reflectance data for the Permian Basin, west Texas and southeast New Mexico (Version 1.0): U.S. Geological Survey Open-File Report 2005-1171, 25 p., https://doi.org/10.3133/ofr20051171.","productDescription":"25 p.","costCenters":[],"links":[{"id":185936,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6713,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1171/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New Mexico, Texas","otherGeospatial":"Permian Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.05078125,\n 28.76765910569123\n ],\n [\n -99.49218749999999,\n 28.76765910569123\n ],\n [\n -99.49218749999999,\n 35.22767235493586\n ],\n [\n -107.05078125,\n 35.22767235493586\n ],\n [\n -107.05078125,\n 28.76765910569123\n ]\n ]\n ]\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fda69","contributors":{"authors":[{"text":"Pawlewicz, Mark","contributorId":69212,"corporation":false,"usgs":true,"family":"Pawlewicz","given":"Mark","email":"","affiliations":[],"preferred":false,"id":282857,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barker, Charles E.","contributorId":93070,"corporation":false,"usgs":true,"family":"Barker","given":"Charles E.","affiliations":[],"preferred":false,"id":282859,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McDonald, Sargent","contributorId":74456,"corporation":false,"usgs":true,"family":"McDonald","given":"Sargent","email":"","affiliations":[],"preferred":false,"id":282858,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70678,"text":"sir20055012 - 2005 - S-wave refraction survey of alluvial aggregate","interactions":[],"lastModifiedDate":"2012-02-02T00:13:47","indexId":"sir20055012","displayToPublicDate":"2005-06-06T00:00:00","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":"2005-5012","title":"S-wave refraction survey of alluvial aggregate","docAbstract":"An S-wave refraction survey was conducted in the Yampa River valley near Steamboat Springs, Colo., to determine how well this method could map alluvium, a major source of construction aggregate. At the field site, about 1 m of soil overlaid 8 m of alluvium that, in turn, overlaid sedimentary bedrock. The traveltimes of the direct and refracted S-waves were used to construct velocity cross sections whose various regions were directly related to the soil, alluvium, and bed-rock. The cross sections were constrained to match geologic logs that were developed from drill-hole data. This constraint minimized the ambiguity in estimates of the thickness and the velocity of the alluvium, an ambiguity that is inherent to the S-wave refraction method. In the cross sections, the estimated S-wave velocity of the alluvium changed in the horizontal direction, and these changes were attributed to changes in composition of the alluvium. The estimated S-wave velocity of the alluvium was practically constant in the vertical direc-tion, indicating that the fine layering observed in the geologic logs could not be detected. The S-wave refraction survey, in conjunction with independent information such as geologic logs, was found to be suitable for mapping the thickness of the alluvium.","language":"ENGLISH","doi":"10.3133/sir20055012","usgsCitation":"Ellefsen, K.J., Tuttle, G.J., Williams, J.M., and Lucius, J.E., 2005, S-wave refraction survey of alluvial aggregate (Version 1.0): U.S. Geological Survey Scientific Investigations Report 2005-5012, 14 p. and 3 plates, https://doi.org/10.3133/sir20055012.","productDescription":"14 p. and 3 plates","costCenters":[],"links":[{"id":185938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6715,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2005/5012/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe115","contributors":{"authors":[{"text":"Ellefsen, Karl J. 0000-0003-3075-4703 ellefsen@usgs.gov","orcid":"https://orcid.org/0000-0003-3075-4703","contributorId":789,"corporation":false,"usgs":true,"family":"Ellefsen","given":"Karl","email":"ellefsen@usgs.gov","middleInitial":"J.","affiliations":[{"id":82803,"text":"Geology, Geophysics, and Geochemistry Science Center","active":true,"usgs":false}],"preferred":true,"id":282861,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tuttle, Gary J.","contributorId":67165,"corporation":false,"usgs":true,"family":"Tuttle","given":"Gary","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":282864,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Williams, Jackie M.","contributorId":11217,"corporation":false,"usgs":true,"family":"Williams","given":"Jackie","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":282863,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lucius, Jeffrey E. lucius@usgs.gov","contributorId":817,"corporation":false,"usgs":true,"family":"Lucius","given":"Jeffrey","email":"lucius@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":282862,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70674,"text":"sir20045268 - 2005 - Effects of aquifer heterogeneity on ground-water flow and chloride concentrations in the Upper Floridan aquifer near and within an active pumping well field, west-central Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:13:47","indexId":"sir20045268","displayToPublicDate":"2005-06-06T00:00:00","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":"2004-5268","title":"Effects of aquifer heterogeneity on ground-water flow and chloride concentrations in the Upper Floridan aquifer near and within an active pumping well field, west-central Florida","docAbstract":"Chloride concentrations have been increasing over time in water from wells within and near the Eldridge-Wilde well field, near the coast in west-central Florida. Variable increases in chloride concentrations from well to well over time are the combined result of aquifer heterogeneity and ground-water pumping within the Upper Floridan aquifer. Deep mineralized water and saline water associated with the saltwater interface appear to move preferentially along flow zones of high transmissivity in response to ground-water withdrawals. The calcium-bicarbonate-type freshwater of the Upper Floridan aquifer within the study area is variably enriched with ions by mixing with introduced deep and saline ground water. The amount and variability of increases in chloride and sulfate concentrations at each well are related to well location, depth interval, and permeable intervals intercepted by the borehole.\r\n\r\nZones of high transmissivity characterize the multilayered carbonate rocks of the Upper Floridan aquifer. Well-developed secondary porosity within the Tampa/Suwannee Limestones and the Avon Park Formation has created producing zones within the Upper Floridan aquifer. The highly transmissive sections of the Avon Park Formation generally are several orders of magnitude more permeable than the Tampa/Suwannee Limestones, but both are associated with increased ground-water flow. The Ocala Limestone is less permeable and is dominated by primary, intergranular porosity. Acoustic televiewer logging, caliper logs, and borehole flow logs (both electromagnetic and heat pulse) indicate that the Tampa/Suwannee Limestone units are dominated by porosity owing to dissolution between 200 and 300 feet below land surface, whereas the porosity of the Avon Park Formation is dominated by fractures that occur primarily from 600 to 750 feet below land surface and range in angle from horizontal to near vertical. Although the Ocala Limestone can act as a semiconfining unit between the Avon Park Formation and the Tampa/Suwannee Limestones, seismic-reflection data and photolinear analyses indicate that fractures and discontinuities in the Ocala Limestone are present within the southwestern part of the well field. It is possible that some fracture zones extend upward from the Avon Park Formation through the Ocala, Suwannee, and Tampa Limestones to land surface. These fractures may provide a more direct hydrologic connection between transmissive zones that are vertically separated by less permeable stratigraphic units.\r\n\r\nGround water moves along permeable zones within the Upper Floridan aquifer in response to changes in head gradients as a result of pumping. Borehole geophysical measurements, including flow logs, specific conductance logs, and continuous monitoring of specific conductance at selected fixed depths, indicate that borehole specific conductance varies substantially with time and in response to pumping stresses. Ground-water mixing between hydrogeologic units likely occurs along highly transmissive zones and within boreholes of active production wells. Ground-water movement and water-quality changes were greatest along the most transmissive zones.\r\n\r\nVariable mixing of three water-type end members (freshwater, deepwater, and saltwater) occurs throughout the study area. Both deepwater and saltwater are likely sources for elevated chloride and sulfate concentrations in ground water. Mass-balance calculations of mixtures of the three end members indicate that deepwater is found throughout the aquifer units. Samples from wells within the southwestern part of the well field indicate that deepwater migrates into the shallow permeable units in the southwestern part of the well field. Deepwater contributes to elevated sulfate and chloride concentrations, which increase with depth and are elevated in wells less than 400 feet deep.\r\n\r\nThe greatest increases in chloride concentrations over time are found in water from wells closest to the saltwater interface. Gro","language":"ENGLISH","doi":"10.3133/sir20045268","usgsCitation":"Tihansky, A., 2005, Effects of aquifer heterogeneity on ground-water flow and chloride concentrations in the Upper Floridan aquifer near and within an active pumping well field, west-central Florida: U.S. Geological Survey Scientific Investigations Report 2004-5268, 81 p., https://doi.org/10.3133/sir20045268.","productDescription":"81 p.","costCenters":[],"links":[{"id":186643,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6711,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5268/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db624a6e","contributors":{"authors":[{"text":"Tihansky, A. B. 0000-0003-1681-1601","orcid":"https://orcid.org/0000-0003-1681-1601","contributorId":77956,"corporation":false,"usgs":true,"family":"Tihansky","given":"A. B.","affiliations":[],"preferred":false,"id":282855,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70657,"text":"ofr20051041 - 2005 - Geodatabase of environmental information for Air Force Plant 4 and Naval Air Station-Joint Reserve Base Carswell Field, Fort Worth, Texas, 1990-2004","interactions":[],"lastModifiedDate":"2022-11-03T18:57:10.917599","indexId":"ofr20051041","displayToPublicDate":"2005-06-04T00:00:00","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":"2005-1041","title":"Geodatabase of environmental information for Air Force Plant 4 and Naval Air Station-Joint Reserve Base Carswell Field, Fort Worth, Texas, 1990-2004","docAbstract":"Air Force Plant 4 (AFP4) and adjacent Naval Air Station-Joint Reserve Base (NAS-JRB) at Fort Worth, Tex., constitute a government-owned, contractor-operated (GOCO) facility that has been in operation since 1942. Contaminants from the facility, primarily volatile organic compounds (VOCs) and metals, have entered the groundwater-flow system through leakage from waste-disposal sites (landfills and pits) and from manufacturing processes (U.S. Air Force, Aeronautical Systems Center, 1995).
The U.S. Geological Survey (USGS), in cooperation with the U.S. Air Force (USAF), Aeronautical Systems Center, Environmental Management Directorate (ASC/ENVR), developed a comprehensive database (or geodatabase) of temporal and spatial environmental information associated with the geology, hydrology, and water quality at AFP4 and NAS-JRB. The database of this report provides information about the AFP4 and NAS-JRB study area including sample location names, identification numbers, locations, historical dates, and various measured hydrologic data. This database does not include every sample location at the site, but is limited to an aggregation of selected digital and hardcopy data of the USAF, USGS, and various consultants who have previously or are currently working at the site.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr20051041","usgsCitation":"Shah, S., and Quigley, S.M., 2005, Geodatabase of environmental information for Air Force Plant 4 and Naval Air Station-Joint Reserve Base Carswell Field, Fort Worth, Texas, 1990-2004: U.S. Geological Survey Open-File Report 2005-1041, Report: 5 p.; ReadMe; Zipped CD Files; Data Dictionary, https://doi.org/10.3133/ofr20051041.","productDescription":"Report: 5 p.; ReadMe; Zipped CD Files; Data Dictionary","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327707,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr20051041.JPG"},{"id":409125,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_72070.htm","linkFileType":{"id":5,"text":"html"}},{"id":6754,"rank":99,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2005/1041/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Texas","city":"Fort Worth","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -97.42554321003897,\n 32.780688573146605\n ],\n [\n -97.42554321003897,\n 32.74218303078236\n ],\n [\n -97.38269461761818,\n 32.74218303078236\n ],\n [\n -97.38269461761818,\n 32.780688573146605\n ],\n [\n -97.42554321003897,\n 32.780688573146605\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6aa048","contributors":{"authors":[{"text":"Shah, Sachin D.","contributorId":60174,"corporation":false,"usgs":true,"family":"Shah","given":"Sachin D.","affiliations":[],"preferred":false,"id":282837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quigley, Sean M.","contributorId":22435,"corporation":false,"usgs":true,"family":"Quigley","given":"Sean","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":282836,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70665,"text":"ofr20041247 - 2005 - Lake Mohave Geophysical Survey 2002: GIS Data Release","interactions":[],"lastModifiedDate":"2012-02-10T00:11:37","indexId":"ofr20041247","displayToPublicDate":"2005-06-04T00:00:00","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":"2004-1247","title":"Lake Mohave Geophysical Survey 2002: GIS Data Release","docAbstract":"This CD-ROM contains sidescan-sonar imagery, sub-bottom reflection profiles, and an interpretive map derived from these data. These data were collected in Lake Mohave, a reservoir behind the Davis Dam and below the Hoover Dam on the Colorado River. These data are veiwable within an Environmental system Research Institute, Inc. (ESRI) Geographic Information system (GIS) ArcView 3.2 project file stored on this CD-ROM","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr20041247","isbn":"0607962631","usgsCitation":"Cross, V.A., Foster, D.S., and Twichell, D.C., 2005, Lake Mohave Geophysical Survey 2002: GIS Data Release: U.S. Geological Survey Open-File Report 2004-1247, Available on CD-ROM and online, https://doi.org/10.3133/ofr20041247.","productDescription":"Available on CD-ROM and online","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":680,"text":"Woods Hole Science Center","active":false,"usgs":true}],"links":[{"id":193063,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9833,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1247/","linkFileType":{"id":5,"text":"html"}}],"scale":"0","projection":"Universal Transverse Mercator","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.8,34.53333333333333 ], [ -115.8,36.56666666666667 ], [ -113.51666666666667,36.56666666666667 ], [ -113.51666666666667,34.53333333333333 ], [ -115.8,34.53333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1520","contributors":{"authors":[{"text":"Cross, VeeAnn A.","contributorId":103311,"corporation":false,"usgs":true,"family":"Cross","given":"VeeAnn","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foster, David S. 0000-0003-1205-0884 dfoster@usgs.gov","orcid":"https://orcid.org/0000-0003-1205-0884","contributorId":1320,"corporation":false,"usgs":true,"family":"Foster","given":"David","email":"dfoster@usgs.gov","middleInitial":"S.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":282852,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Twichell, David C.","contributorId":37730,"corporation":false,"usgs":true,"family":"Twichell","given":"David","email":"","middleInitial":"C.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":282853,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70650,"text":"sim2883 - 2005 - Seismic-hazard maps for the conterminous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sim2883","displayToPublicDate":"2005-06-03T00:00:00","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":"2883","title":"Seismic-hazard maps for the conterminous United States","docAbstract":"This publication consists of six map sheets (titles and text included in this document, below), geospatial datasets, and metadata. The geospatial datasets consist of ArcInfo export files for the seismic-hazard point and polygon data shown on the sheets.\r\nProbabilistic seismic-hazard maps were prepared for the conterminous United States portraying peak horizontal acceleration and horizontal spectral response acceleration for 0.2- and 1.0-second periods with probabilities of exceedance of 10 percent in 50 years and 2 percent in 50 years. All of the maps were prepared by combining the hazard derived from spatially smoothed historic seismicity with the hazard from fault-specific sources. The acceleration values contoured are the random horizontal component. The reference site condition is firm rock, defined as having an average shear-wave velocity of 760 m/sec in the top 30 meters corresponding to the boundary between NEHRP (National Earthquake Hazards Reduction program) site classes B and C.\r\nThis data set represents the results of calculations of hazard curves for a grid of points with a spacing of 0.05 degrees in latitude and longitude. The points were contoured to produce the final representation of the seismic hazard.","language":"ENGLISH","doi":"10.3133/sim2883","usgsCitation":"Frankel, A.D., Petersen, M.D., Mueller, C.S., Haller, K., Wheeler, R.L., Leyendecker, E.V., Wesson, R.L., Harmsen, S., Cramer, C.H., Perkins, D.M., and Rukstales, K.S., 2005, Seismic-hazard maps for the conterminous United States (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2883, 5 p. : 6 map sheets (col.), https://doi.org/10.3133/sim2883.","productDescription":"5 p. : 6 map sheets (col.)","costCenters":[],"links":[{"id":110561,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_71426.htm","linkFileType":{"id":5,"text":"html"},"description":"71426"},{"id":185659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6752,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2005/2883/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3f49","contributors":{"authors":[{"text":"Frankel, Arthur D. 0000-0001-9119-6106 afrankel@usgs.gov","orcid":"https://orcid.org/0000-0001-9119-6106","contributorId":1363,"corporation":false,"usgs":true,"family":"Frankel","given":"Arthur","email":"afrankel@usgs.gov","middleInitial":"D.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":false,"id":282826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Petersen, Mark D. 0000-0001-8542-3990 mpetersen@usgs.gov","orcid":"https://orcid.org/0000-0001-8542-3990","contributorId":1163,"corporation":false,"usgs":true,"family":"Petersen","given":"Mark","email":"mpetersen@usgs.gov","middleInitial":"D.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":282824,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mueller, Charles S. 0000-0002-1868-9710 cmueller@usgs.gov","orcid":"https://orcid.org/0000-0002-1868-9710","contributorId":955,"corporation":false,"usgs":true,"family":"Mueller","given":"Charles","email":"cmueller@usgs.gov","middleInitial":"S.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":282823,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Haller, Kathleen M. haller@usgs.gov","contributorId":1331,"corporation":false,"usgs":true,"family":"Haller","given":"Kathleen M.","email":"haller@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":282825,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"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":282822,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Leyendecker, E. V.","contributorId":87162,"corporation":false,"usgs":true,"family":"Leyendecker","given":"E.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":282830,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Wesson, Robert L. 0000-0003-2702-0012 rwesson@usgs.gov","orcid":"https://orcid.org/0000-0003-2702-0012","contributorId":850,"corporation":false,"usgs":true,"family":"Wesson","given":"Robert","email":"rwesson@usgs.gov","middleInitial":"L.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":282821,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Harmsen, Stephen C. harmsen@usgs.gov","contributorId":1795,"corporation":false,"usgs":true,"family":"Harmsen","given":"Stephen C.","email":"harmsen@usgs.gov","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":false,"id":282827,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Cramer, Chris H.","contributorId":32196,"corporation":false,"usgs":true,"family":"Cramer","given":"Chris","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":282829,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Perkins, David M. perkins@usgs.gov","contributorId":2114,"corporation":false,"usgs":true,"family":"Perkins","given":"David","email":"perkins@usgs.gov","middleInitial":"M.","affiliations":[{"id":301,"text":"Geologic Hazards Team","active":false,"usgs":true}],"preferred":true,"id":282828,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Rukstales, Kenneth S. 0000-0003-2818-078X rukstales@usgs.gov","orcid":"https://orcid.org/0000-0003-2818-078X","contributorId":775,"corporation":false,"usgs":true,"family":"Rukstales","given":"Kenneth","email":"rukstales@usgs.gov","middleInitial":"S.","affiliations":[{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"preferred":true,"id":282820,"contributorType":{"id":1,"text":"Authors"},"rank":11}]}} ,{"id":70648,"text":"fs20053063 - 2005 - Availability of ground-water data for California, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"fs20053063","displayToPublicDate":"2005-06-02T00:00:00","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":"2005-3063","title":"Availability of ground-water data for California, water year 2004","language":"ENGLISH","doi":"10.3133/fs20053063","usgsCitation":"Huff, J., 2005, Availability of ground-water data for California, water year 2004: U.S. Geological Survey Fact Sheet 2005-3063, 2 p. : map, https://doi.org/10.3133/fs20053063.","productDescription":"2 p. : map","costCenters":[],"links":[{"id":121143,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2005_3063.bmp"},{"id":6751,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2005/3063/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d868","contributors":{"authors":[{"text":"Huff, Julia A.","contributorId":23130,"corporation":false,"usgs":true,"family":"Huff","given":"Julia A.","affiliations":[],"preferred":false,"id":282819,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70646,"text":"i2811 - 2005 - Geologic map of Cydonia Mensae - southern Acidalia Planitia, Mars, quadrangles MTM 40007, 40012, 40017, 45007, 45012, and 45017","interactions":[],"lastModifiedDate":"2023-07-05T11:09:20.903456","indexId":"i2811","displayToPublicDate":"2005-06-02T00:00:00","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":"2811","title":"Geologic map of Cydonia Mensae - southern Acidalia Planitia, Mars, quadrangles MTM 40007, 40012, 40017, 45007, 45012, and 45017","docAbstract":"Cydonia Mensae lie adjacent to the boundary separating the highland terrain of western Arabia Terra from the northern lowlands (the dichotomy boundary), where this boundary is gradational rather than abrupt, as is generally the case. Cydonia Mensae are characterized by abundant knobs and mesas, most of which occur in well defined clusters that commonly are long and narrow. The adjacent lowland of Acidalia Planitia contains abundant troughs that define a crude, very large scale polygonal pattern. This pattern, and the troughs, are similar in size and spacing to those in Utopia Planitia (for example, McGill and Hills, 1992; Hiesinger and Head, 2000). The six 1:500,000-scale quadrangles mapped are MTM 40007, 40012, 40017, 45007, 45012, and 45017, which include northern Cydonia Mensae, part of southern Acidalia Planitia, and a small area of Arabia Terra highlands. These six quadrangles are combined into a single map at 1:1,000,000 scale for this publication. Issues of interest addressed by this mapping include the crustal history implied by the knobs and mesas of Cydonia Mensae, the implications of the gradational dichotomy boundary, the age of the Acidalia plains materials, the origin and age of the giant polygons, the validity of putative shorelines inferred to be present in this area, and the origin of the very abundant small cones and domes, specifically if these imply the past presence of water or ice within the plains materials. Earlier maps (Witbeck and Underwood, 1984; Scott and Tanaka, 1986; Tanaka and others, 2003) that included the area mapped for this study addressed some or all of these issues, but these maps were more regional in coverage and were at smaller scales. In addition, new orbital data from Mars Global Surveyor and Mars Odyssey missions were available only to Tanaka and others (2003). The intent of this present study is to address the issues listed by mapping at a scale large enough to permit greater map detail and to better understand the areal distribution of the materials and features of interest.
","language":"English","publisher":"U.S Geological Survey","doi":"10.3133/i2811","usgsCitation":"McGill, G.E., 2005, Geologic map of Cydonia Mensae - southern Acidalia Planitia, Mars, quadrangles MTM 40007, 40012, 40017, 45007, 45012, and 45017: U.S. Geological Survey IMAP 2811, HTML Document, https://doi.org/10.3133/i2811.","productDescription":"HTML Document","costCenters":[],"links":[{"id":6749,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i2811/","linkFileType":{"id":5,"text":"html"}},{"id":185578,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"5000000","otherGeospatial":"Mars","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a33b1","contributors":{"authors":[{"text":"McGill, George E.","contributorId":47462,"corporation":false,"usgs":true,"family":"McGill","given":"George","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282813,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70634,"text":"sir20055030 - 2005 - Trends in streamflow, sedimentation, and sediment chemistry for the Wolf River, Menominee Indian Reservation, Wisconsin, 1850-1999","interactions":[],"lastModifiedDate":"2015-11-16T08:44:46","indexId":"sir20055030","displayToPublicDate":"2005-06-02T00:00:00","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":"2005-5030","title":"Trends in streamflow, sedimentation, and sediment chemistry for the Wolf River, Menominee Indian Reservation, Wisconsin, 1850-1999","docAbstract":"Historical trends in streamflow, sedimentation, and sediment chemistry of the Wolf River were examined for a 6-mile reach that flows through the southern part of the Menominee Indian Reservation and the northern part of Shawano County, Wis. Trends were examined in the context of effects from dams, climate, and land-cover change. Annual flood peaks and mean monthly flow for the Wolf River were examined for 1907-96 and compared to mean annual and mean monthly precipitation. Analysis of trends in sedimentation (from before about 1850 through 1999) involved collection of cores and elevation data along nine valley transects spanning the Wolf River channel, flood plain, and backwater and impounded areas; radioisotope analyses of impounded sediment cores; and analysis of General Land Office Survey Notes (1853-91). Trends in sediment chemistry were examined by analyzing samples from an impoundment core for minor and trace elements. Annual flood peaks for the Wolf River decreased during 1907-49 but increased during 1950-96, most likely reflecting general changes in upper-atmospheric circulation patterns from more zonal before 1950 to more meridional after 1950. The decrease in flood peaks during 1907-49 may also, in part, be due to forest regrowth. Mean monthly streamflow during 1912-96 increased for the months of February and March but decreased for June and July, suggesting that spring snowmelt occurs earlier in the season than it did in the past. Decreases in early summer flows may be a reflection earlier spring snowmelt and large rainstorms in early spring rather than early summer. These trends also may reflect upper-atmospheric circulation patterns. The Balsam Row Dam impoundment contains up to 10 feet of organic-rich silty clay and has lost much of its storage capacity. Fine sediment has accumulated for 1.8 miles upstream from the Balsam Row Dam. Historical average linear and mass sedimentation rates in the Balsam Row impoundment were 0.09 feet per year and 1.15 pounds per square foot per year for 1927-62 and 0.10 feet per year and 1.04 pounds per square foot per year for 1963-99. Sedimentation in the impoundment was episodic and was associated with large floods, especially the flood-related failure of the Keshena Falls Dam in 1972 and a large flood in 1973. Sand deposition is common in the Wolf River upstream from the impounded reach for 2.5 miles and is caused by the base-level increase associated with the Balsam Row Dam. Some sand deposition also may have been associated with logging and log drives in the late 1800s and the failure of the Keshena Falls Dam. In the upstream 1.5-mile part of the studied reach, the substrate is mainly rocky; however, about 2,000 feet downstream from Keshena Falls, the channel has narrowed and incised since the 1890s, likely related to human alterations associated with logging, log drives, and (or) changes in hydraulics and sediment characteristics associated with completion of the Keshena Falls Dam and head race in 1908. Minor- and trace-element concentrations in sediment from Balsam Row impoundment and other depositional areas along the Wolf River generally reflect background conditions as affected by watershed geology and historical inputs from regional and local atmospheric deposition.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20055030","collaboration":"In cooperation with the Menominee Indian Tribe of Wisconsin","usgsCitation":"Fitzpatrick, F.A., 2005, Trends in streamflow, sedimentation, and sediment chemistry for the Wolf River, Menominee Indian Reservation, Wisconsin, 1850-1999: U.S. Geological Survey Scientific Investigations Report 2005-5030, vi, 47 p., https://doi.org/10.3133/sir20055030.","productDescription":"vi, 47 p.","numberOfPages":"55","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1849-12-30","temporalEnd":"1999-01-01","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":191281,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":311329,"rank":101,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2005/5030/pdf/SIR_2005-5030.pdf"},{"id":6843,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2005-5030/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","country":"United States","state":"Wisconsin","county":"Menominee County","otherGeospatial":"Menominee Indian Reservation","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.6399,45.1171],[-88.6109,45.1174],[-88.5598,45.1175],[-88.4836,45.117],[-88.4862,45.0302],[-88.4881,44.9435],[-88.4894,44.8554],[-88.6117,44.8563],[-88.736,44.8561],[-88.7356,44.9429],[-88.7982,44.9432],[-88.8588,44.943],[-88.9516,44.943],[-88.9812,44.9427],[-88.9812,45.0299],[-88.9818,45.118],[-88.9301,45.1182],[-88.8623,45.1175],[-88.8118,45.1177],[-88.7343,45.1172],[-88.6826,45.1174],[-88.6574,45.1172],[-88.6399,45.1171]]]},\"properties\":{\"name\":\"Menominee\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69606b","contributors":{"authors":[{"text":"Fitzpatrick, Faith A. fafitzpa@usgs.gov","contributorId":1182,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Faith","email":"fafitzpa@usgs.gov","middleInitial":"A.","affiliations":[{"id":476,"text":"North Carolina Water Science Center","active":true,"usgs":true}],"preferred":false,"id":282779,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70637,"text":"sir20045241 - 2005 - Remote sensing for environmental site screening and watershed evaluation in Utah Mine lands: East Tintic mountains, Oquirrh mountains, and Tushar mountains","interactions":[],"lastModifiedDate":"2022-12-22T20:08:18.850387","indexId":"sir20045241","displayToPublicDate":"2005-06-02T00:00:00","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":"2004-5241","title":"Remote sensing for environmental site screening and watershed evaluation in Utah Mine lands: East Tintic mountains, Oquirrh mountains, and Tushar mountains","docAbstract":"Imaging spectroscopy-a powerful remote-sensing tool for mapping subtle variations in the composition of minerals, vegetation, and man-made materials on the Earth's surface-was applied in support of environmental assessments and watershed evaluations in several mining districts in the State of Utah. Three areas were studied through the use of Landsat 7 ETM+ and Airborne Visible/Infrared Imaging Spectrometer (AVIRIS) data: (1) the Tintic mining district in the East Tintic Mountains southwest of Provo, (2) the Camp Floyd mining district (including the Mercur mine) and the Stockton (or Rush Valley) mining district in the Oquirrh Mountains south of the Great Salt Lake, and (3) the Tushar Mountains and Antelope Range near Marysvale.
The Landsat 7 ETM+ data were used for initial site screening and the planning of AVIRIS surveys. The AVIRIS data were analyzed to create spectrally defined maps of surface minerals with special emphasis on locating and characterizing rocks and soils with acid-producing potential (APP) and acid-neutralizing potential (ANP). These maps were used by the United States Environmental Protection Agency (USEPA) for three primary purposes: (1) to identify unmined and anthropogenic sources of acid generation in the form of iron sulfide and (or) ferric iron sulfate-bearing minerals such as jarosite and copiapite; (2) to seek evidence for downstream or downwind movement of minerals associated with acid generation, mine waste, and (or) tailings from mines, mill sites, and zones of unmined hydrothermally altered rocks; and (3) to identify carbonate and other acid-buffering minerals that neutralize acidic, potentially metal bearing, solutions and thus mitigate potential environmental effects of acid generation.
Calibrated AVIRIS surface-reflectance data were spectrally analyzed to identify and map selected surface materials. Two maps were produced from each flightline of AVIRIS data: a map of iron-bearing minerals and water having absorption features in the spectral region from 0.35 µm to 1.35 µm and a map of minerals (including clays, sulfates, micas, and carbonates) having absorptions in the spectral region from 1.45 µm to 2.51 µm. Several methods were used to verify the AVIRIS mapping results, including field checking of selected locations with a portable spectrometer, visual inspection of the AVIRIS reflectance spectra, and X-ray diffraction (XRD) analysis of field samples.
The maps of iron-bearing minerals derived from analysis of the visible (VIS) and near-infrared (NIR) regions of the electromagnetic spectrum were shown to be more consistently reliable in indicating the presence of jarosite than were the maps generated from analysis of the short-wave infrared (SWIR) region. When present in abundance, phyllosilicate minerals tend to dominate the SWIR and mask the spectral features of jarosite in that wavelength region. The crystal field absorptions of jarosite in the VIS and NIR spectral regions will commonly be present regardless of whether the Fe-OH absorption feature near 2.27 µm can be detected. For this reason, the VIS and NIR were preferable to the SWIR for the remote spectroscopic identification of jarosite (and other iron-bearing minerals).
Large exposures of unmined hydrothermally altered rocks occur throughout the three study areas. These rocks commonly contain sulfide or sulfate minerals that produce sulfuric acid upon subaerial oxidation. The acid may be introduced into local surface and ground water and thus lower the baseline (that is, the premining) pH for a watershed.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045241","usgsCitation":"Rockwell, B.W., McDougal, R., and Gent, C.A., 2005, Remote sensing for environmental site screening and watershed evaluation in Utah Mine lands: East Tintic mountains, Oquirrh mountains, and Tushar mountains (Version 1.2): U.S. Geological Survey Scientific Investigations Report 2004-5241, Report: viii, 84 p.; Figures, https://doi.org/10.3133/sir20045241.","productDescription":"Report: viii, 84 p.; Figures","costCenters":[],"links":[{"id":410962,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_73988.htm","linkFileType":{"id":5,"text":"html"}},{"id":8924,"rank":3,"type":{"id":25,"text":"Version History"},"url":"https://pubs.usgs.gov/sir/2004/5241/sirHist.html","linkFileType":{"id":5,"text":"html"}},{"id":191808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6846,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5241/","linkFileType":{"id":5,"text":"html"}},{"id":7886,"rank":2,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/sir/2004/5241/figures.html","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Utah","otherGeospatial":"East Tintic Mountains, Oquirrh Mountains, Tushar Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -113.29022483358571,\n 40.93599326796834\n ],\n [\n -113.29022483358571,\n 37.86776389090204\n ],\n [\n -111.17415878264146,\n 37.86776389090204\n ],\n [\n -111.17415878264146,\n 40.93599326796834\n ],\n [\n -113.29022483358571,\n 40.93599326796834\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf7d","contributors":{"authors":[{"text":"Rockwell, Barnaby W. 0000-0002-9549-0617 barnabyr@usgs.gov","orcid":"https://orcid.org/0000-0002-9549-0617","contributorId":2195,"corporation":false,"usgs":true,"family":"Rockwell","given":"Barnaby","email":"barnabyr@usgs.gov","middleInitial":"W.","affiliations":[{"id":171,"text":"Central Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":282792,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McDougal, Robert R.","contributorId":53418,"corporation":false,"usgs":true,"family":"McDougal","given":"Robert R.","affiliations":[],"preferred":false,"id":282794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gent, Carol A.","contributorId":40646,"corporation":false,"usgs":true,"family":"Gent","given":"Carol","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":282793,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70623,"text":"fs20043067 - 2005 - Ground-water vulnerability to nitrate contamination in the mid-atlantic region","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"fs20043067","displayToPublicDate":"2005-06-01T00:00:00","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":"2004-3067","title":"Ground-water vulnerability to nitrate contamination in the mid-atlantic region","docAbstract":"The U.S. Environmental Protection Agency?s (USEPA) Regional Vulnerability Assessment (ReVA) Program has developed a set of statistical tools to support regional-scale, integrated ecological risk-assessment studies. One of these tools, developed by the U.S. Geological Survey (USGS), is used with available water-quality data obtained from USGS National Water-Quality Assessment (NAWQA) and other studies in association with land cover, geology, soils, and other geographic data to develop logistic-regression equations that predict the vulnerability of ground water to nitrate concentrations exceeding specified thresholds in the Mid-Atlantic Region. The models were developed and applied to produce spatial probability maps showing the likelihood of elevated concentrations of nitrate in the region. These maps can be used to identify areas that currently are at risk and help identify areas where ground water has been affected by human activities. This information can be used by regional and local water managers to protect water supplies and identify land-use planning solutions and monitoring programs in these vulnerable areas.","language":"ENGLISH","doi":"10.3133/fs20043067","usgsCitation":"Greene, E.A., LaMotte, A.E., Cullinan, K., and Smith, E.R., 2005, Ground-water vulnerability to nitrate contamination in the mid-atlantic region: U.S. Geological Survey Fact Sheet 2004-3067, 4 p., https://doi.org/10.3133/fs20043067.","productDescription":"4 p.","costCenters":[],"links":[{"id":6805,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://md.water.usgs.gov/publications/fs-2004-3067/html/","linkFileType":{"id":5,"text":"html"}},{"id":125084,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/fs/2004/3067/report-thumb.jpg"},{"id":90526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/fs/2004/3067/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db65556b","contributors":{"authors":[{"text":"Greene, Earl A. 0000-0002-9479-0829 eagreene@usgs.gov","orcid":"https://orcid.org/0000-0002-9479-0829","contributorId":3518,"corporation":false,"usgs":true,"family":"Greene","given":"Earl","email":"eagreene@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":282734,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"LaMotte, Andrew E. 0000-0002-1434-6518 alamotte@usgs.gov","orcid":"https://orcid.org/0000-0002-1434-6518","contributorId":2842,"corporation":false,"usgs":true,"family":"LaMotte","given":"Andrew","email":"alamotte@usgs.gov","middleInitial":"E.","affiliations":[{"id":374,"text":"Maryland Water Science Center","active":true,"usgs":true}],"preferred":true,"id":282733,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cullinan, Kerri-Ann","contributorId":90821,"corporation":false,"usgs":true,"family":"Cullinan","given":"Kerri-Ann","email":"","affiliations":[],"preferred":false,"id":282736,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Smith, Elizabeth R.","contributorId":76023,"corporation":false,"usgs":true,"family":"Smith","given":"Elizabeth","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":282735,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70608,"text":"wdrMS041 - 2005 - Water resources data Mississippi water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"wdrMS041","displayToPublicDate":"2005-06-01T00:00:00","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":"MS-04-1","title":"Water resources data Mississippi water year 2004","docAbstract":"Water resources data for this water year for Mississippi consists of records of surface water and ground water in the State. Specifically, it contains: (1) Discharge records for 90 streamflow-gaging stations, stage records for 18 of these gaging stations, discharge records for 97 partial-record stations or miscellaneous streamflow sites, including 6 flood hydrograph partial-record stations, 91 crest-stage partial-record stations and 0 special study and miscellaneous sites; (2) stage only at 1 gaging station; (3) water-quality records for 12 streamflow-gaging stations, 0 stage-only stations, 13 water-quality monitor stations, 0 partial-record stations or miscellaneous sites, 0 short-term study sites, and 26 wells; and (4) water-level records for 19 observation wells. Records obtained from water-resources investigations are also included in special sections of the report. Records included for stream stages are only a small fraction of those obtained during the water year.","language":"ENGLISH","doi":"10.3133/wdrMS041","usgsCitation":"Morris, F., Runner, M., and Storm, J., 2005, Water resources data Mississippi water year 2004 (Online only): U.S. Geological Survey Water Data Report MS-04-1, 300 p., https://doi.org/10.3133/wdrMS041.","productDescription":"300 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6798,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ms-04-1/","linkFileType":{"id":5,"text":"html"}},{"id":192772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a02e4b07f02db5f80b0","contributors":{"authors":[{"text":"Morris, F. III","contributorId":76395,"corporation":false,"usgs":true,"family":"Morris","given":"F.","suffix":"III","email":"","affiliations":[],"preferred":false,"id":282718,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Runner, M.S.","contributorId":28630,"corporation":false,"usgs":true,"family":"Runner","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":282716,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Storm, J.B.","contributorId":51838,"corporation":false,"usgs":true,"family":"Storm","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":282717,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70610,"text":"sir20055061 - 2005 - External quality-assurance results for the National Atmospheric Deposition Program/National Trends Network, 2002-03","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"sir20055061","displayToPublicDate":"2005-06-01T00:00:00","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":"2005-5061","title":"External quality-assurance results for the National Atmospheric Deposition Program/National Trends Network, 2002-03","docAbstract":"Six external quality-assurance programs were operated by the U.S. Geological Survey (USGS) External Quality-Assurance (QA) Project for the National Atmospheric Deposition Program/National Trends Network (NADP/NTN) from 2002 through 2003. Each program measured specific components of the overall error inherent in NADP/NTN wet-deposition measurements.\r\n\r\nThe intersite-comparison program assessed the variability and bias of pH and specific conductance determinations made by NADP/NTN site operators twice per year with respect to accuracy goals. The percentage of site operators that met the pH accuracy goals decreased from 92.0 percent in spring 2002 to 86.3 percent in spring 2003. In these same four intersite-comparison studies, the percentage of site operators that met the accuracy goals for specific conductance ranged from 94.4 to 97.5 percent.\r\n\r\nThe blind-audit program and the sample-handling evaluation (SHE) program evaluated the effects of routine sample handling, processing, and shipping on the chemistry of weekly NADP/NTN samples. The blind-audit program data indicated that the variability introduced by sample handling might be environmentally significant to data users for sodium, potassium, chloride, and hydrogen ion concentrations during 2002. In 2003, the blind-audit program was modified and replaced by the SHE program. The SHE program was designed to control the effects of laboratory-analysis variability. The 2003 SHE data had less overall variability than the 2002 blind-audit data. The SHE data indicated that sample handling buffers the pH of the precipitation samples and, in turn, results in slightly lower conductivity. Otherwise, the SHE data provided error estimates that were not environmentally significant to data users.\r\n\r\nThe field-audit program was designed to evaluate the effects of onsite exposure, sample handling, and shipping on the chemistry of NADP/NTN precipitation samples. Field-audit results indicated that exposure of NADP/NTN wet-deposition samples to onsite conditions tended to neutralize the acidity of the samples by less than 1.0 microequivalent per liter. Onsite exposure of the sampling bucket appeared to slightly increase the concentration of most of the analytes but not to an extent that was environmentally significant to NADP data users.\r\n\r\nAn interlaboratory-comparison program was used to estimate the analytical variability and bias of the NADP Central Analytical Laboratory (CAL) during 2002-03. Bias was identified in the CAL data for calcium, magnesium, sodium, potassium, ammonium, chloride, nitrate, sulfate, hydrogen ion, and specific conductance, but the absolute value of the bias was less than analytical minimum detection limits for all constituents except magnesium, nitrate, sulfate, and specific conductance. Control charts showed that CAL results were within statistical control approximately 90 percent of the time. Data for the analysis of ultrapure deionized-water samples indicated that CAL did not have problems with laboratory contamination.\r\n\r\nDuring 2002-03, the overall variability of data from the NADP/NTN precipitation-monitoring system was estimated using data from three collocated monitoring sites. Measurement differences of constituent concentration and deposition for paired samples from the collocated samplers were evaluated to compute error terms. The medians of the absolute percentage errors (MAEs) for the paired samples generally were larger for cations (approximately 8 to 50 percent) than for anions (approximately 3 to 33 percent). MAEs were approximately 16 to 30 percent for hydrogen-ion concentration, less than 10 percent for specific conductance, less than 5 percent for sample volume, and less than 8 percent for precipitation depth.\r\nThe variability attributed to each component of the sample-collection and analysis processes, as estimated by USGS quality-assurance programs, varied among analytes. Laboratory analysis variability accounted for approximately 2 percent of the","language":"ENGLISH","doi":"10.3133/sir20055061","usgsCitation":"Wetherbee, G.A., Latysh, N.E., and Burke, K.P., 2005, External quality-assurance results for the National Atmospheric Deposition Program/National Trends Network, 2002-03 (Online only): U.S. Geological Survey Scientific Investigations Report 2005-5061, 69 p., https://doi.org/10.3133/sir20055061.","productDescription":"69 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":6800,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20055061/","linkFileType":{"id":5,"text":"html"}},{"id":192774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e65ff","contributors":{"authors":[{"text":"Wetherbee, Gregory A. 0000-0002-6720-2294 wetherbe@usgs.gov","orcid":"https://orcid.org/0000-0002-6720-2294","contributorId":1044,"corporation":false,"usgs":true,"family":"Wetherbee","given":"Gregory","email":"wetherbe@usgs.gov","middleInitial":"A.","affiliations":[{"id":143,"text":"Branch of Quality Systems","active":true,"usgs":true}],"preferred":true,"id":282722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Latysh, Natalie E.","contributorId":39860,"corporation":false,"usgs":true,"family":"Latysh","given":"Natalie","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":282723,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burke, Kevin P.","contributorId":101333,"corporation":false,"usgs":true,"family":"Burke","given":"Kevin","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282724,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70604,"text":"ofr20041387 - 2005 - Ground-water/surface-water relations along Honey Creek, Washtenaw County, Michigan, 2003","interactions":[],"lastModifiedDate":"2016-10-06T12:08:32","indexId":"ofr20041387","displayToPublicDate":"2005-06-01T00:00:00","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":"2004-1387","title":"Ground-water/surface-water relations along Honey Creek, Washtenaw County, Michigan, 2003","docAbstract":"The U.S. Geological Survey (USGS), in cooperation with the city of Ann Arbor, Mich., investigated the ground-water/ surface-water relations along the lower reaches of Honey Creek, Washtenaw County, Mich., and an unnamed tributary to Honey Creek (the discharge tributary) from June through October 2003. Streamflow in these reaches was artificially high during a naturally low-flow period due to an anthropogenic discharge. Ground-water/surface-water relations were examined by seepage runs (series of streamflow measurements for the computation of streams gains or losses) and measurements of the difference in head between the stream surface and shallow aquifer. Specific conductance and water-temperature measurements were used as ancillary data to help identify gaining and losing reaches. Three seepage runs and four runs in which hydraulic-head differences between the stream and shallow aquifer were measured (piezometer runs) were made during periods of base flow.
Streamflow measurements were made at 18 sites for the seepage runs. Instream piezometers were installed at 16 sites and bank piezometers were installed at 2 sites. Two deeper instream piezometers were installed at site 13 on September 4, 2003 to collect additional data on the ground-water/surface-water relations at that site.
The seepage runs indicate that the main stem of Honey Creek and the discharge tributary in the study area are overall gaining reaches. The seepage runs also indicate that smaller reaches of Honey Creek and the discharge tributary may be losing reaches and that this relation may change over time with changing hydraulic conditions. The piezometer-run measurements support the seepage-run results on the main stem, whereas piezometer-run measurements both support and conflict with seepage-run measurements on the discharge tributary. Seepage runs give an average for the reach, whereas piezometer head-difference measurements are for a specific area around the piezometer. Data that may appear to be conflicting actually may be showing that within a gaining reach there are localized areas that lose streamflow.
The overall gain in streamflow along with specific measurements of head differences, specific conductance, and water temperature indicate that ground water is discharging to Honey Creek and the discharge tributary. Although reaches and areas that lose streamflow have been identified, data collected during this study cannot confirm or disprove that the loss is to the regional ground-water system.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr20041387","collaboration":"Prepared in cooperation with the city of Ann Arbor, Michigan","usgsCitation":"Healy, D.F., 2005, Ground-water/surface-water relations along Honey Creek, Washtenaw County, Michigan, 2003: U.S. Geological Survey Open-File Report 2004-1387, iv, 17 p., https://doi.org/10.3133/ofr20041387.","productDescription":"iv, 17 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":192615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6797,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/ofr2004-1387/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","country":"United States","state":"Michigan","county":"Washtenaw County","otherGeospatial":"Honey Creek","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -83.858333,\n 42.333333\n ],\n [\n -83.858333,\n 42.25\n ],\n [\n -83.775,\n 42.25\n ],\n [\n -83.775,\n 42.333333\n ],\n [\n -83.858333,\n 42.333333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659ffd","contributors":{"authors":[{"text":"Healy, Denis F.","contributorId":46514,"corporation":false,"usgs":true,"family":"Healy","given":"Denis","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":282715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70603,"text":"wdrOR041 - 2005 - Water resources data for Oregon, water year 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"wdrOR041","displayToPublicDate":"2005-06-01T00:00:00","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":"OR-04-1","title":"Water resources data for Oregon, water year 2004","docAbstract":"The annual Oregon water data report is one of a series of annual reports that document hydrologic data gathered from the U.S. Geological Survey's surface- and ground-water data-collection networks in each State, Puerto Rico, and the Trust Territories. These records of streamflow, ground-water levels, and quality of water provide the hydrologic information needed by State, local, Tribal, and Federal agencies and the private sector for developing and managing our Nation's land and water resources.\r\n\r\nThis report contains water year 2004 data for both surface and ground water, including discharge records for 209 streamflow-gaging stations, 42 partial-record or miscellaneous streamflow stations, and 9 crest-stage partial-record streamflow stations; stage-only records for 6 gaging stations; stage and content records for 15 lakes and reservoirs; water-level records from 12 long-term observation wells; and water-quality records collected at 133 streamflow-gaging stations and 1 atmospheric deposition station.","language":"ENGLISH","doi":"10.3133/wdrOR041","usgsCitation":"Herrett, T.A., Hess, G.W., House, J.G., Ruppert, G.P., and Courts, M., 2005, Water resources data for Oregon, water year 2004: U.S. Geological Survey Water Data Report OR-04-1, 968 p., https://doi.org/10.3133/wdrOR041.","productDescription":"968 p.","costCenters":[],"links":[{"id":192614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6796,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wdr/2004/wdr-or-04/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629a04","contributors":{"authors":[{"text":"Herrett, Thomas A. herrett@usgs.gov","contributorId":3505,"corporation":false,"usgs":true,"family":"Herrett","given":"Thomas","email":"herrett@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":282710,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, Glenn W.","contributorId":33411,"corporation":false,"usgs":true,"family":"Hess","given":"Glenn","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":282711,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"House, Jon G.","contributorId":85266,"corporation":false,"usgs":true,"family":"House","given":"Jon","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":282713,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ruppert, Gregory P.","contributorId":46616,"corporation":false,"usgs":true,"family":"Ruppert","given":"Gregory","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":282712,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Courts, Mary-Lorraine","contributorId":104151,"corporation":false,"usgs":true,"family":"Courts","given":"Mary-Lorraine","email":"","affiliations":[],"preferred":false,"id":282714,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ]}