A ground-water-flow model was developed to investigate the ground-water resources of Kalamazoo County. Ground water is widely used as a source of water for drinking and industry in Kalamazoo County and the surrounding area. Additionally, lakes and streams are valued for their recreational and aesthetic uses. Stresses on the ground-water system, both natural and human-induced, have raised concerns about the long-term availability of ground water for people to use and for replenishment of lakes and streams. Potential changes in these stresses, including withdrawals and recharge, were simulated using a ground-water-flow model.
Simulations included steady-state conditions (in which stresses remained constant and changes in storage were not included) and transient conditions (in which stresses changed in seasonal and monthly time scales and storage within the system was included). Steady-state simulations were used to investigate the long-term effects on water levels and streamflow of a reduction in recharge or an increase in pumping to projected 2010 withdrawal rates, withdrawal and application of water for irrigation, and a reduction in recharge in urban areas caused by impervious surfaces. Transient simulations were used to investigate changes in withdrawals to match seasonal and monthly patterns under various recharge conditions, and the potential effects of the use of water for irrigation over the summer months.
With a reduction in recharge, simulated water levels declined over most of the model area in Kalamazoo County; with an increase in pumping, water levels declined primarily near pumping centers. Because withdrawals by wells intercept water that would have discharged possibly to a stream or lake, model simulations indicated that streamflow was reduced with increased withdrawals. With withdrawal and consumption of water for irrigation, simulated water levels declined. Assuming a reduction in recharge due to urbanization, water levels declined and flow to streams was reduced based on steady-state simulation results. Transient results indicated a reduction of water levels with the simulated use of water for irrigation over the summer months. Generally the transient simulation with recharge only in the winter provided the best fit to observed water levels collected during synoptic water-level measurements in some wells and to the trends observed in water levels for other wells.
Analysis of the regional hydrologic budgets provides an increased understanding of water movement within the ground-water-flow system in Kalamazoo County. Budgets for the steady-state simulations indicated that with reduced recharge, less water was available for streamflow and less water left the model area through the model boundaries. Similarly, with an increase in pumping rates, less water was available to enter streams and become streamflow. When recharge was assumed to remain constant and when it was allowed to vary throughout the year, the amount of water that entered storage was greater than that which left storage. However, when recharge was distributed through October?May only or when recharge rates were reduced from October to May, the amount of water that entered storage was less than that which left storage. Thus, on the basis of model simulations, with reduced recharge or increased withdrawals, water must come from storage, rivers, or from ground-flow-system boundaries to meet withdrawal demands.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/sir20045054","collaboration":"Prepared in cooperation with the city of Kalamazoo, city of Portage, Kalamazoo County Human Services Department, and Michigan Department of Environmental Quality","usgsCitation":"Luukkonen, C.L., Blumer, S.P., Weaver, T.L., and Jean, J., 2004, Simulation of the ground-water-flow system in the Kalamazoo County area, Michigan: U.S. Geological Survey Scientific Investigations Report 2004-5054, vii, 65 p., https://doi.org/10.3133/sir20045054.","productDescription":"vii, 65 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":6832,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045054/","linkFileType":{"id":5,"text":"html"}},{"id":352751,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/sir/2004/5054/SIR2004-5054.pdf"},{"id":191592,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/sir20045054.JPG"}],"scale":"100000","country":"United States","state":"Michigan","county":"Kalamazoo County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86,\n 42.616667\n ],\n [\n -86,\n 41.866667\n ],\n [\n -85,\n 41.866667\n ],\n [\n -85,\n 42.616667\n ],\n [\n -86,\n 42.616667\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6974e0","contributors":{"authors":[{"text":"Luukkonen, Carol L. clluukko@usgs.gov","contributorId":3489,"corporation":false,"usgs":true,"family":"Luukkonen","given":"Carol","email":"clluukko@usgs.gov","middleInitial":"L.","affiliations":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blumer, Stephen P. spblumer@usgs.gov","contributorId":2419,"corporation":false,"usgs":true,"family":"Blumer","given":"Stephen","email":"spblumer@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":281902,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weaver, T. L.","contributorId":24339,"corporation":false,"usgs":true,"family":"Weaver","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281904,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jean, Julie","contributorId":75640,"corporation":false,"usgs":true,"family":"Jean","given":"Julie","email":"","affiliations":[],"preferred":false,"id":281905,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70124,"text":"ofr20041238 - 2004 - User's manual for the national water information system of the U.S. Geological Survey: Ground-water site-inventory system","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"ofr20041238","displayToPublicDate":"2005-02-24T00:00:00","publicationYear":"2004","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":"2004-1238","title":"User's manual for the national water information system of the U.S. Geological Survey: Ground-water site-inventory system","docAbstract":"The Ground-Water Site-Inventory (GWSI) System is a ground-water data storage and retrieval system that is part of the National Water Information System (NWIS) developed by the U.S. Geological Survey (USGS). The NWIS is a distributed water database in which data can be processed over a network of workstations and file servers at USGS offices throughout the United States. This system comprises the GWSI, the Automated Data Processing System (ADAPS), the Water-Quality System (QWDATA), and the Site-Specific Water-Use Data System (SWUDS).\r\n\r\nThe GWSI System provides for entering new sites and updating existing sites within the local database. In addition, the GWSI provides for retrieving and displaying ground-water and sitefile data stored in the local database. Finally, the GWSI provides for routine maintenance of the local and national data records. This manual contains instructions for users of the GWSI and discusses the general operating procedures for the programs found within the GWSI Main Menu.","language":"ENGLISH","doi":"10.3133/ofr20041238","usgsCitation":"Water Resources Division, U.S. Geological Survey, 2004, User's manual for the national water information system of the U.S. Geological Survey: Ground-water site-inventory system (Version 4.3): U.S. Geological Survey Open-File Report 2004-1238, 275 p., https://doi.org/10.3133/ofr20041238.","productDescription":"275 p.","costCenters":[],"links":[{"id":191700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6835,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1238/","linkFileType":{"id":5,"text":"html"}}],"scale":"100000","edition":"Version 4.3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603d61","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":534692,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70114,"text":"wdrNY031 - 2004 - Water resources data New York water year 2003, volume 1: eastern New York excluding Long Island","interactions":[],"lastModifiedDate":"2012-02-02T00:14:05","indexId":"wdrNY031","displayToPublicDate":"2005-02-24T00:00:00","publicationYear":"2004","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":"NY-03-1","title":"Water resources data New York water year 2003, volume 1: eastern New York excluding Long Island","docAbstract":"Water resources data for the 2003 water year for Eastern New York Excluding Long Island consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and ground-water levels. This volume contains records for water discharge at 150 gaging stations; stage only at 8 gaging stations; stage and contents at 4 gaging stations, and 18 other lakes and reservoirs; water quality at 29 gaging stations; and water levels at 21 observation wells. Also included are data for 31 crest-stage partial-record stations. Locations of all these sites are shown on figue 8. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements and analyses. These data together with the data in volumes 2 and 3 represent that part of the National Water Data System operated by the U.S. Geological Survey in cooperation with State, Municipal, and Federal agencies in New York.","language":"ENGLISH","doi":"10.3133/wdrNY031","usgsCitation":"Butch, G., Murray, P., Lumia, R., and Corse, M., 2004, Water resources data New York water year 2003, volume 1: eastern New York excluding Long Island: U.S. Geological Survey Water Data Report NY-03-1, 599 p., https://doi.org/10.3133/wdrNY031.","productDescription":"599 p.","costCenters":[],"links":[{"id":6826,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ny-03-1/","linkFileType":{"id":5,"text":"html"}},{"id":193285,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7f38","contributors":{"authors":[{"text":"Butch, G.K.","contributorId":63849,"corporation":false,"usgs":true,"family":"Butch","given":"G.K.","affiliations":[],"preferred":false,"id":281880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murray, P.M.","contributorId":33358,"corporation":false,"usgs":true,"family":"Murray","given":"P.M.","email":"","affiliations":[],"preferred":false,"id":281879,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lumia, R.","contributorId":70465,"corporation":false,"usgs":true,"family":"Lumia","given":"R.","email":"","affiliations":[],"preferred":false,"id":281881,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Corse, M.D.","contributorId":12943,"corporation":false,"usgs":true,"family":"Corse","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":281878,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70116,"text":"wdrNY033 - 2004 - Water resources data New York water year 2003, volume 3: western New York","interactions":[],"lastModifiedDate":"2012-02-02T00:14:00","indexId":"wdrNY033","displayToPublicDate":"2005-02-24T00:00:00","publicationYear":"2004","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":"NY-03-3","title":"Water resources data New York water year 2003, volume 3: western New York","docAbstract":"Water resources data for the 2003 water year for Western New York consist of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; water levels and water quality of ground-water wells; and quantity and chemical quality of precipitation. This volume contains records for water discharge at 72 gaging stations; stage only at 14 gaging stations; stage and contents at 6 gaging stations, water quality at 7 gaging stations; 62 wells, and 19 partial record stations; water levels at 27 observation wells; daily precipitation totals at 3 sites, and chemical quality of precipitation at 1 site. Also included are data for 39 crest-stage partial record stations. Locations of all these sites are shown on figue 1. Additional water data were collected at various sites not involved in the systematic data collection program and are published as miscellaneous measurements. These data together with the data in volumes 1 and 2 represent that part of the National Water Data System operated by the U.S. Geological Survey in cooperation with State, local, and Federal agencies in New York.","language":"ENGLISH","doi":"10.3133/wdrNY033","usgsCitation":"Hornlein, J., Szabo, C., and Sherwood, D.A., 2004, Water resources data New York water year 2003, volume 3: western New York: U.S. Geological Survey Water Data Report NY-03-3, 4 p. online; 378 p. report, https://doi.org/10.3133/wdrNY033.","productDescription":"4 p. online; 378 p. report","costCenters":[],"links":[{"id":6828,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wdr-ny-03-3/","linkFileType":{"id":5,"text":"html"}},{"id":192911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7fa1","contributors":{"authors":[{"text":"Hornlein, J.F.","contributorId":102554,"corporation":false,"usgs":true,"family":"Hornlein","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":281888,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Szabo, Carolyn O.","contributorId":75210,"corporation":false,"usgs":true,"family":"Szabo","given":"Carolyn O.","affiliations":[],"preferred":false,"id":281887,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherwood, D. A.","contributorId":65824,"corporation":false,"usgs":true,"family":"Sherwood","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":281886,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70118,"text":"sir20045243 - 2004 - Quality of water on the Prairie Band Potawatomi Reservation, northeastern Kansas, May 2001 through August 2003","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"sir20045243","displayToPublicDate":"2005-02-24T00:00:00","publicationYear":"2004","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":"2004-5243","title":"Quality of water on the Prairie Band Potawatomi Reservation, northeastern Kansas, May 2001 through August 2003","docAbstract":"Water-quality samples were collected from 20 surface-water sites and 11 ground-water sites on the Prairie Band Potawatomi Reservation in northeastern Kansas in an effort to describe existing water-quality conditions on the reservation and to compare water-quality conditions to results from previous reports published as part of a multiyear cooperative study with the Prairie Band Potawatomi Nation. Water is a valuable resource to the Prairie Band Potawatomi Nation as tribal members use the streams draining the reservation, Soldier, Little Soldier, and South Cedar Creeks, to fulfill subsistence hunting and fishing needs and as the tribe develops an economic base on the reservation. Samples were collected once at 20 surface-water monitoring sites during June 2001, and quarterly samples were collected at 5 of the 20 monitoring sites from May 2001 through August 2003. Ground-water-quality samples were collected once from seven wells and twice from four wells during April through May 2003 and in August 2003. \r\n\r\nSurface-water-quality samples collected from May through August 2001 were analyzed for physical properties, nutrients, pesticides, fecal indicator bacteria, and total suspended solids. In November 2001, an additional analysis for dissolved solids, major ions, trace elements, and suspended-sediment concentration was added for surface-water samples. Ground-water samples were analyzed for physical properties, dissolved solids, major ions, nutrients, trace elements, pesticides, and fecal indicator bacteria. Chemical oxygen demand and volatile organic compounds were analyzed in a sample from one monitoring well located near a construction and demolition landfill on the reservation. \r\n\r\nPrevious reports published as a part of this ongoing study identified total phosphorus, triazine herbicides, and fecal coliform bacteria as exceeding their respective water-quality criteria in surface water on the reservation. Previous ground-water assessments identified occasional sample concentrations of dissolved solids, sodium, sulfate, boron, iron, and manganese as exceeding their respective water-quality criteria. \r\n\r\nForty percent of the 65 surface-water samples analyzed for total phosphorus exceeded the aquatic-life goal of 0.1 mg/L (milligrams per liter) established by the U.S. Environmental Protection Agency (USEPA). Concentrations of dissolved solids and sodium occasionally exceeded USEPA Secondary Drinking-Water Regulations and Drinking-Water Advisory Levels, respectively. One of the 20 samples analyzed for atrazine concentrations exceeded the Maximum Contaminant Level (MCL) of 3.0 ?g/L (micrograms per liter) as an annual average established for drinking water by USEPA. A triazine herbicide screen was used on 63 surface-water samples, and triazine compounds were frequently detected. Triazine herbicides and their degradates are listed on the USEPA Contaminant Candidate List. \r\n\r\nNitrite plus nitrate concentrations in two ground-water samples from one monitoring well exceeded the MCL of 10 mg/L established by USEPA for drinking water. Arsenic concentrations in two samples from one monitoring well also exceeded the proposed MCL of 10 ?g/L established by the USEPA for drinking water. Concentrations of dissolved solids and sulfate in some ground-water samples exceeded their respective Secondary Drinking-Water Regulations, and concentrations exceeded the taste threshold of the USEPA?s \r\n\r\nDrinking-Water Advisory Level for sodium. Consequently, in the event that ground water on the reservation is to be used as a drinking-water source, additional treatment may be necessary to remove excess dissolved solids, sulfate, and sodium.","language":"ENGLISH","doi":"10.3133/sir20045243","usgsCitation":"Ross Schmidt, H.C., 2004, Quality of water on the Prairie Band Potawatomi Reservation, northeastern Kansas, May 2001 through August 2003: U.S. Geological Survey Scientific Investigations Report 2004-5243, 69 p., https://doi.org/10.3133/sir20045243.","productDescription":"69 p.","costCenters":[],"links":[{"id":6830,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045243/","linkFileType":{"id":5,"text":"html"}},{"id":191539,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636364","contributors":{"authors":[{"text":"Ross Schmidt, Heather C.","contributorId":85671,"corporation":false,"usgs":true,"family":"Ross Schmidt","given":"Heather","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":281891,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70107,"text":"sir20045207 - 2004 - Assessment of soil and water contaminants from selected locations in and near the Idaho Army National Guard Orchard Training Area, Ada County, Idaho, 2001-2003","interactions":[],"lastModifiedDate":"2012-02-02T00:14:04","indexId":"sir20045207","displayToPublicDate":"2005-02-22T00:00:00","publicationYear":"2004","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":"2004-5207","title":"Assessment of soil and water contaminants from selected locations in and near the Idaho Army National Guard Orchard Training Area, Ada County, Idaho, 2001-2003","docAbstract":"In 2001, the National Guard Bureau and the U.S. Geological Survey began a project to compile hydrogeologic data and determine presence or absence of soil, surface-water, and ground-water contamination at the Idaho Army National Guard Orchard Training Area in southwestern Idaho. Between June 2002 and April 2003, a total of 114 soil, surface-water, ground-water, precipitation, or dust samples were collected from 68 sample sites (65 different locations) in the Orchard Training Area (OTA) or along the vehicle corridor to the OTA. Soil and water samples were analyzed for concentrations of selected total trace metals, major ions, nutrients, explosive compounds, semivolatile organics, and petroleum hydrocarbons. Water samples also were analyzed for concentrations of selected dissolved trace metals and major ions.\r\n\r\nDistinguishing naturally occurring large concentrations of trace metals, major ions, and nutrients from contamination related to land and water uses at the OTA was difficult. There were no historical analyses for this area to compare with modern data, and although samples were collected from 65 locations in and near the OTA, sampled areas represented only a small part of the complex OTA land-use areas and soil types. For naturally occurring compounds, several assumptions were made?anomalously large concentrations, when tied to known land uses, may indicate presence of contamination; naturally occurring concentrations cannot be separated from contamination concentrations in mid- and lower ranges of data; and smallest concentrations may represent the lowest naturally occurring range of concentrations and (or) the absence of contaminants related to land and water uses. Presence of explosive, semivolatile organic (SVOC), and petroleum hydrocarbon compounds in samples indicates contamination from land and water uses.\r\n\r\nIn areas along the vehicle corridor and major access roads within the OTA, most trace metal, major ion, and nutrient concentrations in soil samples were not in the upper 10th percentile of data, but concentrations of 25 metals, ions, or nutrients were in the upper 10th percentile in a puddle sample near the heavy equipment maneuvering area, MPRC-H. The largest concentrations of tin, ammonia, and nitrite plus nitrate (as nitrogen) in water from the OTA were detected in a sample from this puddle. Petroleum hydrocarbons were the most common contaminant, detected in all soil and surface-water samples. An SVOC, bis (2-ethylhexyl) phthalate, a plasticizer, was detected at a site along the vehicle corridor.\r\n\r\nIn Maneuver Areas within the OTA, many soil samples contained at least one trace metal, major ion, or nutrient in the upper 10th percentile of data, and the largest concentrations of cobalt, iron, mercury, titanium, sodium, ammonia, or total phosphorus were detected in 6 of 13 soil samples outside the Tadpole Lake area. The largest concentrations of aluminum, arsenic, beryllium, nickel, selenium, silver, strontium, thallium, vanadium, chloride, potassium, sulfate, and nitrite plus nitrate were detected in soil samples from the Tadpole Lake area. Water from Tadpole Lake contained the largest total concentrations of 19 trace metals, 4 major ions, and 1 nutrient. Petroleum hydrocarbons were detected in 5 soil samples and water from Tadpole Lake. SVOCs related to combustion of fuel or plasticizers were detected in 1 soil sample. Explosive compounds were detected in 1 precipitation sample.In the \r\n\r\nImpact Area within the OTA, most soil samples contained at least one trace metal, major ion, or nutrient in the upper 10th percentile of data, and the largest concentrations of barium, chromium, copper, manganese, lead, or orthophosphate were detected in 6 of the 18 soil samples. Petroleum hydrocarbons were detected in 4 soil samples, SVOCs in 6 samples, and explosive compounds in 4 samples.\r\n\r\nIn the mobilization and training equipment site (MATES) compound adjacent to the OTA, all soil and water samples contained at lea","language":"ENGLISH","doi":"10.3133/sir20045207","usgsCitation":"Parliman, D., 2004, Assessment of soil and water contaminants from selected locations in and near the Idaho Army National Guard Orchard Training Area, Ada County, Idaho, 2001-2003 (Online only): U.S. Geological Survey Scientific Investigations Report 2004-5207, 78 p., https://doi.org/10.3133/sir20045207.","productDescription":"78 p.","onlineOnly":"Y","costCenters":[],"links":[{"id":193060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6793,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir2004-5207/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","edition":"Online only","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669420","contributors":{"authors":[{"text":"Parliman, D. J.","contributorId":64220,"corporation":false,"usgs":true,"family":"Parliman","given":"D. J.","affiliations":[],"preferred":false,"id":281874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70103,"text":"ofr20041426 - 2004 - RayGUI 2.0: a graphical user interface for interactive forward and inversion ray-tracing","interactions":[{"subject":{"id":23761,"text":"ofr98203 - 1998 - RayGUI; a graphical user interface for interactive ray-tracing (rayinvr)","indexId":"ofr98203","publicationYear":"1998","noYear":false,"title":"RayGUI; a graphical user interface for interactive ray-tracing (rayinvr)"},"predicate":"SUPERSEDED_BY","object":{"id":70103,"text":"ofr20041426 - 2004 - RayGUI 2.0: a graphical user interface for interactive forward and inversion ray-tracing","indexId":"ofr20041426","publicationYear":"2004","noYear":false,"title":"RayGUI 2.0: a graphical user interface for interactive forward and inversion ray-tracing"},"id":1}],"lastModifiedDate":"2017-11-18T12:01:30","indexId":"ofr20041426","displayToPublicDate":"2005-02-22T00:00:00","publicationYear":"2004","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":"2004-1426","title":"RayGUI 2.0: a graphical user interface for interactive forward and inversion ray-tracing","language":"ENGLISH","doi":"10.3133/ofr20041426","usgsCitation":"Song, J., and ten Brink, U., 2004, RayGUI 2.0: a graphical user interface for interactive forward and inversion ray-tracing: U.S. Geological Survey Open-File Report 2004-1426, 33 p., https://doi.org/10.3133/ofr20041426.","productDescription":"33 p.","costCenters":[],"links":[{"id":192997,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6790,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1426/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db64876f","contributors":{"authors":[{"text":"Song, Jian-Li","contributorId":74089,"corporation":false,"usgs":true,"family":"Song","given":"Jian-Li","email":"","affiliations":[],"preferred":false,"id":281860,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"ten Brink, Uri S. 0000-0001-6858-3001 utenbrink@usgs.gov","orcid":"https://orcid.org/0000-0001-6858-3001","contributorId":127560,"corporation":false,"usgs":true,"family":"ten Brink","given":"Uri S.","email":"utenbrink@usgs.gov","affiliations":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true},{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":281861,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70089,"text":"sir20045076 - 2004 - Stratigraphy and tectonic history of the Tucson Basin, Pima County, Arizona, based on the Exxon state (32)-1 well","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"sir20045076","displayToPublicDate":"2005-02-17T00:00:00","publicationYear":"2004","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":"2004-5076","title":"Stratigraphy and tectonic history of the Tucson Basin, Pima County, Arizona, based on the Exxon state (32)-1 well","docAbstract":"The Tucson Basin is a relatively large late Cenozoic extensional basin developed in the upper plate of the Catalina detachment fault in the southern Basin and Range Province, southeastern Arizona. In 1972, Exxon Company, U.S.A., drilled an exploration well (Exxon State (32)-1) near the center of the Tucson Basin that penetrated 3,658 m (12,001 ft) of sedimentary and volcanic rocks above granitoid basement. Detailed study of cuttings and geophysical logs of the Exxon State well has led to revision of the previously reported subsurface stratigraphy for the basin and provided new insight into its depositional and tectonic history. There is evidence that detachment faulting and uplift of the adjacent Catalina core complex on the north have affected the subsurface geometry of the basin. The gravity anomaly map of the Tucson Basin indicates that the locations of subbasins along the north-trending axis of the main basin coincide with the intersection of this axis with west-southwest projections of synforms in the adjacent core complex. In other words, the subbasins overlie synforms and the ridges between subbasins overlie antiforms. The Exxon State well was drilled near the center of one of the subbasins. The Exxon well was drilled to a total depth of 3,827 m (12,556 ft), and penetrated the following stratigraphic section: Pleistocene(?) to middle(?) Miocene upper basin-fill sedimentary rocks (0-908 m [0-2,980 ft]) lower basin-fill sedimentary rocks (908-1,880 m [2,980-6,170 ft]) lower Miocene and upper Oligocene Pantano Formation (1,880-2,516 m [6,170-8,256 ft]) upper Oligocene to Paleocene(?) volcanic and sedimentary rocks (2,516-3,056 m [8,256-10,026 ft]) Lower Cretaceous to Upper Jurassic Bisbee Group (3,056-3,658 m [10,026-12,001 ft]) pre-Late Jurassic granitoid plutonic rock (3,658-3,827 m [12,001- 12,556 ft]). Stratigraphy and Tectonic History of the Tucson Basin, Pima County, Arizona, Based on the Exxon State (32)-1 Well The 1,880 m (6,170 ft) of basin-fill sedimentary rocks consist of alluvial-fan, alluvial-plain, and playa facies. The uppermost unit, a 341-m-thick (1,120-ft) lower Pleistocene and upper Pliocene alluvial-fan deposit (named the Cienega Creek fan in this study), is an important aquifer in the Tucson basin. The facies change at the base of the alluvial fan may prove to be recognizable in well data throughout much of the basin. The well data show that a sharp boundary at 908 m (2,980 ft) separates relatively unconsolidated and undeformed upper basin fill from denser, significantly faulted lower basin fill, indicating that there were two stages of basin filling in the Tucson basin as in other basins of the region. The two stages apparently occurred during times of differing tectonic style in the region. In the Tucson area the Pantano Formation, which contains an andesite flow dated at about 25 Ma, fills a syntectonic basin in the hanging wall of the Catalina detachment fault, reflecting middle Tertiary extension on the fault. The formation in the well is 636 m thick (2,086 ft) and consists of alluvial-fan, playa, and lacustrine sedimentary facies, a lava flow, and rock- avalanche deposits. Analysis of the geophysical logs indicates that a K-Ar date of 23.4 Ma reported previously for the Pantano interval of the well was obtained on selected cuttings collected from a rock-avalanche deposit near the base of the unit and, thus, does not date the Pantano Formation. The middle Tertiary volcanic and sedimentary rocks have an aggregate thickness of 540 m (1,770 ft). We obtained a new 40Ar/ 39Ar age of 26.91+0.18 Ma on biotite sampled at a depth of 2,584-2,609 m (8,478-8,560 ft) from a 169-m-thick (554-ft) silicic tuff in this interval. The volcanic rocks probably correlate with other middle Tertiary volcanic rocks of the area, and the sedimentary rocks may correlate with the Cloudburst and Mineta Formations exposed on the flanks of the San Pedro Basin to the northeast. The Bisbee Group in the Exxon well is 602 m (1,975 f","language":"ENGLISH","doi":"10.3133/sir20045076","usgsCitation":"Houser, B.B., Peters, L., Esser, R.P., and Gettings, M.E., 2004, Stratigraphy and tectonic history of the Tucson Basin, Pima County, Arizona, based on the Exxon state (32)-1 well: U.S. Geological Survey Scientific Investigations Report 2004-5076, 42 p., https://doi.org/10.3133/sir20045076.","productDescription":"42 p.","costCenters":[],"links":[{"id":193221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6785,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sir/2004/5076/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8168","contributors":{"authors":[{"text":"Houser, Brenda B.","contributorId":20772,"corporation":false,"usgs":true,"family":"Houser","given":"Brenda","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":281834,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, Lisa","contributorId":26770,"corporation":false,"usgs":true,"family":"Peters","given":"Lisa","affiliations":[],"preferred":false,"id":281835,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Esser, Richard P.","contributorId":13323,"corporation":false,"usgs":true,"family":"Esser","given":"Richard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":281833,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gettings, Mark E. 0000-0002-2910-2321 mgetting@usgs.gov","orcid":"https://orcid.org/0000-0002-2910-2321","contributorId":602,"corporation":false,"usgs":true,"family":"Gettings","given":"Mark","email":"mgetting@usgs.gov","middleInitial":"E.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":281832,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70092,"text":"sim2824 - 2004 - Maps of Hawaiian Islands exclusive economic zone interpreted from GLORIA sidescan-sonar imagery","interactions":[],"lastModifiedDate":"2023-01-11T22:00:37.973246","indexId":"sim2824","displayToPublicDate":"2005-02-17T00:00:00","publicationYear":"2004","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":"2824","title":"Maps of Hawaiian Islands exclusive economic zone interpreted from GLORIA sidescan-sonar imagery","docAbstract":"The map is geology around the Hawaiian Islands derived from GLORIA data collected in 1986-1989 from the southeastern Hawaiian Ridge EEZ (Exclusive Economic Zone), which covers more than 1,000,000 km2 of sea floor. The seafloor is characterized by a variety of volcanic and sedimentary processes. Cretaceous age seafloor underlies both subaerial and subaqueous erupted lava forming the Hawaiian Ridge and various Cretaceous seamounts. Subaerial lava quenches and brecciates as it enters the ocean forming smooth slopes. The mobile flanks of the islands have given way into slumps and debris avalanches.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sim2824","usgsCitation":"Holcomb, R.T., and Robinson, J., 2004, Maps of Hawaiian Islands exclusive economic zone interpreted from GLORIA sidescan-sonar imagery (Version 1.0): U.S. Geological Survey Scientific Investigations Map 2824, Report: 9 p.; 1 Plate: 49.01 x 35.65 inches; Metadata; Data Download, https://doi.org/10.3133/sim2824.","productDescription":"Report: 9 p.; 1 Plate: 49.01 x 35.65 inches; Metadata; Data Download","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":193222,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6786,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/sim/2004/2824","linkFileType":{"id":5,"text":"html"}},{"id":110544,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70165.htm","linkFileType":{"id":5,"text":"html"},"description":"70165"}],"scale":"5000000","country":"United States","state":"Hawaii","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -154.9936756321275,\n 15.315035175420434\n ],\n [\n -151.9850748699214,\n 20.35516245647287\n ],\n [\n -153.7557836225372,\n 23.225453084150047\n ],\n [\n -163.76032839486115,\n 26.239657139129463\n ],\n [\n -166.07646831070537,\n 19.262013911556778\n ],\n [\n -154.9936756321275,\n 15.315035175420434\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3ecd","contributors":{"authors":[{"text":"Holcomb, Robin T.","contributorId":46938,"corporation":false,"usgs":true,"family":"Holcomb","given":"Robin","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":281837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Joel E. 0000-0002-5193-3666 jrobins@usgs.gov","orcid":"https://orcid.org/0000-0002-5193-3666","contributorId":2757,"corporation":false,"usgs":true,"family":"Robinson","given":"Joel E.","email":"jrobins@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":281836,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70093,"text":"fs20043121 - 2004 - Oil and gas assessment of Yukon Flats, East-Central Alaska, 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"fs20043121","displayToPublicDate":"2005-02-17T00:00:00","publicationYear":"2004","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":"2004-3121","title":"Oil and gas assessment of Yukon Flats, East-Central Alaska, 2004","language":"ENGLISH","doi":"10.3133/fs20043121","usgsCitation":"Stanley, R.G., Ahlbrandt, T.S., Charpentier, R., Cook, T.A., Crews, J.M., Klett, T., Lillis, P.G., Morin, R.L., Phillips, J.D., Pollastro, R.M., Rowan, E.L., Saltus, R.W., Schenk, C.J., Simpson, M.K., Till, A.B., Troutman, S.M., and Hendley, J.W., 2004, Oil and gas assessment of Yukon Flats, East-Central Alaska, 2004: U.S. Geological Survey Fact Sheet 2004-3121, 2 p. (online) , https://doi.org/10.3133/fs20043121.","productDescription":"2 p. (online) ","costCenters":[],"links":[{"id":122452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2004_3121.bmp"},{"id":6787,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/fs/2004/3121/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd69d5e4b0b29085102dad","contributors":{"authors":[{"text":"Stanley, Richard G. 0000-0001-6192-8783 rstanley@usgs.gov","orcid":"https://orcid.org/0000-0001-6192-8783","contributorId":1832,"corporation":false,"usgs":true,"family":"Stanley","given":"Richard","email":"rstanley@usgs.gov","middleInitial":"G.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":281844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ahlbrandt, Thomas S.","contributorId":57836,"corporation":false,"usgs":true,"family":"Ahlbrandt","given":"Thomas","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":281851,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Charpentier, Ronald R. charpentier@usgs.gov","contributorId":934,"corporation":false,"usgs":true,"family":"Charpentier","given":"Ronald R.","email":"charpentier@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":281841,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cook, Troy A.","contributorId":52519,"corporation":false,"usgs":true,"family":"Cook","given":"Troy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":281850,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crews, Jesse M.","contributorId":96540,"corporation":false,"usgs":true,"family":"Crews","given":"Jesse","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281854,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Klett, Timothy R. 0000-0001-9779-1168 tklett@usgs.gov","orcid":"https://orcid.org/0000-0001-9779-1168","contributorId":709,"corporation":false,"usgs":true,"family":"Klett","given":"Timothy R.","email":"tklett@usgs.gov","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":false,"id":281838,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lillis, Paul G. 0000-0002-7508-1699 plillis@usgs.gov","orcid":"https://orcid.org/0000-0002-7508-1699","contributorId":1817,"corporation":false,"usgs":true,"family":"Lillis","given":"Paul","email":"plillis@usgs.gov","middleInitial":"G.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":281843,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Morin, Robert L.","contributorId":82671,"corporation":false,"usgs":true,"family":"Morin","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":281852,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Phillips, Jeffrey D. 0000-0002-6459-2821 jeff@usgs.gov","orcid":"https://orcid.org/0000-0002-6459-2821","contributorId":1572,"corporation":false,"usgs":true,"family":"Phillips","given":"Jeffrey","email":"jeff@usgs.gov","middleInitial":"D.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":false,"id":281842,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Pollastro, Richard M.","contributorId":25100,"corporation":false,"usgs":true,"family":"Pollastro","given":"Richard","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281848,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Rowan, Elisabeth L. 0000-0001-5753-6189 erowan@usgs.gov","orcid":"https://orcid.org/0000-0001-5753-6189","contributorId":2075,"corporation":false,"usgs":true,"family":"Rowan","given":"Elisabeth","email":"erowan@usgs.gov","middleInitial":"L.","affiliations":[{"id":241,"text":"Eastern Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":281845,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Saltus, Richard W. saltus@usgs.gov","contributorId":777,"corporation":false,"usgs":true,"family":"Saltus","given":"Richard","email":"saltus@usgs.gov","middleInitial":"W.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":281839,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Schenk, Christopher J. 0000-0002-0248-7305 schenk@usgs.gov","orcid":"https://orcid.org/0000-0002-0248-7305","contributorId":826,"corporation":false,"usgs":true,"family":"Schenk","given":"Christopher","email":"schenk@usgs.gov","middleInitial":"J.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true},{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"preferred":true,"id":281840,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Simpson, Megan K.","contributorId":82987,"corporation":false,"usgs":true,"family":"Simpson","given":"Megan","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":281853,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Till, Alison B. atill@usgs.gov","contributorId":2482,"corporation":false,"usgs":true,"family":"Till","given":"Alison","email":"atill@usgs.gov","middleInitial":"B.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":281846,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Troutman, Sandra M.","contributorId":46601,"corporation":false,"usgs":true,"family":"Troutman","given":"Sandra","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":281849,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Hendley, James W. II jhendley@usgs.gov","contributorId":2547,"corporation":false,"usgs":true,"family":"Hendley","given":"James","suffix":"II","email":"jhendley@usgs.gov","middleInitial":"W.","affiliations":[],"preferred":false,"id":281847,"contributorType":{"id":1,"text":"Authors"},"rank":17}]}} ,{"id":70072,"text":"sir20045214 - 2004 - Water resources of Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"sir20045214","displayToPublicDate":"2005-02-11T00:00:00","publicationYear":"2004","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":"2004-5214","title":"Water resources of Sweetwater County, Wyoming","docAbstract":"Sweetwater County is located in the southwestern part of Wyoming and is the largest county in the State. A study to quantify the availability and describe the chemical quality of surface-water and ground-water resources in Sweetwater County was conducted by the U.S. Geological Survey in cooperation with the Wyoming State Engineer\u0019s Office. Most of the county has an arid climate. For this reason a large amount of the flow in perennial streams within the county is derived from outside the county. Likewise, much of the ground-water recharge to aquifers within the county is from flows into the county, and occurs slowly. Surface-water data were not collected as part of the study. Evaluations of streamflow and stream-water quality were limited to analyses of historical data and descriptions of previous investigations. Forty-six new ground-water-quality samples were collected as part of the study and the results from an additional 782 historical ground-water-quality samples were reviewed. Available hydrogeologic characteristics for various aquifers throughout the county also are described.\r\n\r\nFlow characteristics of streams in Sweetwater County vary substantially depending on regional and local basin characteristics and anthropogenic factors. Because precipitation amounts in the county are small, most streams in the county are ephemeral, flowing only as a result of regional or local rainfall or snowmelt runoff. Flows in perennial streams in the county generally are a result of snowmelt runoff in the mountainous headwater areas to the north, west, and south of the county. Flow characteristics of most perennial streams are altered substantially by diversions and regulation.\r\nWater-quality characteristics of selected streams in and near Sweetwater County during water years 1974 through 1983 were variable. Concentrations of dissolved constituents, suspended sediment, and bacteria generally were smallest at sites on the Green River because of resistant geologic units, increased vegetative cover, large diluting streamflows, and large reservoirs. Concentrations of dissolved constituents, suspended sediment, and bacteria generally were largest at sites in the Big Sandy River and Bitter Creek Basins. Some nutrient concentrations and bacteria counts exceeded various State and Federal water-quality criteria. Historical and recent anthropogenic activities contributed to natural sources of many dissolved constituents and suspended sediment.\r\n\r\nBoth water-table and artesian conditions occur in aquifers within the county. Shallow ground water is available throughout the county, although much of it is only marginally suitable or is unsuitable for domestic and irrigation uses mainly because of high total dissolved solids (TDS) concentrations. Suitable ground water for livestock use can be found in most areas of the county. Ground-water quality tends to deteriorate with increasing distance from recharge areas and with increasing depth below land surface. Ground water from depths of greater than a few thousand feet tends to have TDS concentrations that make it moderately saline to briny. In some areas even shallow ground water has moderately saline TDS concentrations. Specific constituents in parts of some aquifers in the county occur in relatively high concentrations when compared to U.S. Environmental Protection Agency drinking-water standards. Relatively high concentrations of sulfate, fluoride, boron, iron, and manganese were found in several aquifers. Many ground-water samples from the Battle Spring aquifer in the Great Divide Structural Basin had high radionuclide concentrations.\r\n\r\nThe estimated mean daily water use in Sweetwater County in 2000 was 170.73 million gallons per day. Irrigation was the largest single use of water in the county with an estimated mean use of more than 92 million gallons per day. Surface water irrigation accounted for nearly 90 percent of the total irrigation water used in 2000. Although ground water is used to a much ","language":"ENGLISH","doi":"10.3133/sir20045214","usgsCitation":"Mason, J., and Miller, K.A., 2004, Water resources of Sweetwater County, Wyoming: U.S. Geological Survey Scientific Investigations Report 2004-5214, 196 p. and 4 plates, https://doi.org/10.3133/sir20045214.","productDescription":"196 p. and 4 plates","costCenters":[],"links":[{"id":6743,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045214/","linkFileType":{"id":5,"text":"html"}},{"id":186557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4835e4b07f02db4ed484","contributors":{"authors":[{"text":"Mason, Jon P.","contributorId":26758,"corporation":false,"usgs":true,"family":"Mason","given":"Jon P.","affiliations":[],"preferred":false,"id":281811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, Kirk A. 0000-0002-8141-2001 kmiller@usgs.gov","orcid":"https://orcid.org/0000-0002-8141-2001","contributorId":3959,"corporation":false,"usgs":true,"family":"Miller","given":"Kirk","email":"kmiller@usgs.gov","middleInitial":"A.","affiliations":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281810,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70071,"text":"fs20043133 - 2004 - Water use in Kansas, 1990-2000","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"fs20043133","displayToPublicDate":"2005-02-11T00:00:00","publicationYear":"2004","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":"2004-3133","title":"Water use in Kansas, 1990-2000","docAbstract":"This fact sheet compares water use in 1990, 1995, and 2000 for the 12 major river basins in Kansas. Of these 3 years, irrigation water use was largest in 1990 and smallest in 1995, largely because of differing climatic conditions. Irrigation averaged about 85 percent of total water use in Kansas each year, and ground water pumped in the western part of the State provided most of the irrigation water used. Water use for public supply, industry, and livestock increased between 1990 and 2000. Total State population increased 8 percent between 1990 and 2000, and the number of people served by public water suppliers increased 12 percent. Surface water withdrawn for public supply increased 24 percent because of population growth in the northeastern and south-central parts of the State and decreasing reliance on ground water by the city of Wichita. From 1990 to 2000, ground-water withdrawals for livestock and meat processing increased in western Kansas, and surface-water withdrawals for sand dredging increased in eastern Kansas. This fact sheet was produced as part of an ongoing cooperative program supported in part by the Kansas State Water Plan Fund.","language":"ENGLISH","doi":"10.3133/fs20043133","usgsCitation":"Kenny, J., and Hansen, C.V., 2004, Water use in Kansas, 1990-2000: U.S. Geological Survey Fact Sheet 2004-3133, 4 p., https://doi.org/10.3133/fs20043133.","productDescription":"4 p.","costCenters":[],"links":[{"id":6742,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/fs2004-3133/","linkFileType":{"id":5,"text":"html"}},{"id":124489,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/fs_2004_3133.bmp"}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd1c8","contributors":{"authors":[{"text":"Kenny, Joan F.","contributorId":69132,"corporation":false,"usgs":true,"family":"Kenny","given":"Joan F.","affiliations":[],"preferred":false,"id":281809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hansen, Cristi V. chansen@usgs.gov","contributorId":435,"corporation":false,"usgs":true,"family":"Hansen","given":"Cristi","email":"chansen@usgs.gov","middleInitial":"V.","affiliations":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"preferred":false,"id":281808,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70062,"text":"sir20045219 - 2004 - Environmental factors and chemical and microbiological water-quality constituents related to the presence of enteric viruses in ground water from small public water supplies in southeastern Michigan","interactions":[],"lastModifiedDate":"2023-01-10T20:07:43.049671","indexId":"sir20045219","displayToPublicDate":"2005-02-11T00:00:00","publicationYear":"2004","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":"2004-5219","title":"Environmental factors and chemical and microbiological water-quality constituents related to the presence of enteric viruses in ground water from small public water supplies in southeastern Michigan","docAbstract":"A study of small public ground-water-supply wells that produce water from discontinuous sand and gravel aquifers was done from July 1999 through July 2001 in southeastern Michigan. Samples were collected to determine the occurrence of viral pathogens and microbiological indicators of fecal contamination (“indicators”), determine whether indicators are adequate predictors of the presence of enteric viruses, and determine the factors that affect the presence of enteric viruses. Small systems are those that serve less than 3,300 people. Samples were analyzed for specific enteric viruses by reverse transcriptase-polymerase chain reaction (RT-PCR), for culturable viruses by cell culture, and for the indicators total coliforms, Escherichia coli (E. coli), enterococci, and F-specific and somatic coliphage. Ancillary environmental and water-quality data were collected or compiled.
A total of 169 regular samples and 32 replicate pairs were collected from 38 wells. Replicate pairs were samples collected at the same well on the same date. One well was sampled 6 times, 30 wells were sampled five times, 6 wells were sampled twice, and 1 well was sampled once. By use of RT-PCR, enterovirus was found in four wells (10.5 percent) and hepatitis A virus (HAV) in five wells (13.2 percent). In two of these wells, investigators found both enterovirus and HAV, but on different sampling dates. Culturable viruses were found one time in two wells (5.9 percent), and neither of these wells was positive for viruses by use of RT-PCR on any sampling date. If results for all viruses are combined, 9 of the 38 small public-supply wells were positive for enteric viruses (23.7 percent) by either cell culture or RT-PCR.
One or more indicators were found in 18 of 38 wells. Total coliforms, E. coli, enterococci, and F-specific and somatic coliphage were found in 34.2, 10.5, 15.8, 5.9, and 5.9 percent, respectively, of the wells tested. In only 3 out of 18 wells were samples positive for an indicator on more than one date at the same well. The co-occurrence of enteric viruses and any indicator was 55.6 percent; five out of the nine virus-positive wells were also found to be positive for an indicator. Two wells with detections of viruses had a detection of total coliforms, one well had a detection of E. coli, one of enterococci, and one of F-specific coliphage. On a per sample basis, of 11 samples that were positive for enteric viruses, indicator bacteria co-occurred in only 2 samples, and coliphage were not present in any.
More virus-positive samples were found at sites served by septic systems than those served by sewerlines. Sampling condition (ground water or a mixture of tank and ground water), distance to septic system, type of and distance to nearest surface-water body, well characteristics, or land use were not related to the presence of viruses or indicators. Among continuous water-quality variables, statistically significant relations were found between total coliforms and dissolved organic carbon and between total coliforms and iron. There was a statistically significant relation between chloride concentrations >20 mg/L and detections of total coliforms. Presence of nitrate and nitrite was related to the presence of other indicators (E. coli, enterococci, and F-specific and somatic coliphage) or enteric viruses, but not to total coliforms. The data indicated that chloride-to-bromide (C1:Br) ratios may be useful as a screening tool for total coliforms and enteric viruses but not for E. coli, enterococci, and F-specific and somatic coliphage.
This study provides evidence for fecal contamination of ground water from small public-supply wells, at least on an intermittent basis. Collecting data on multiple lines of evidence would be needed to reliably predict the presence of enteric viruses and protect public health. Future data collection toward this end could include repeat sampling several times a year for different indicators, measuring dissolved-organic carbon, nitrate plus nitrite, and (or) chloride concentrations, or determining C1:Br ratios. The presence of a site served by a septic system is an indication that the well may be more vulnerable to contamination than a site served by a sewerline.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/sir20045219","usgsCitation":"Francy, D.S., Bushon, R.N., Stopar, J., Luzano, E.J., and Fout, G.S., 2004, Environmental factors and chemical and microbiological water-quality constituents related to the presence of enteric viruses in ground water from small public water supplies in southeastern Michigan: U.S. Geological Survey Scientific Investigations Report 2004-5219, v, 54 p., https://doi.org/10.3133/sir20045219.","productDescription":"v, 54 p.","costCenters":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":186407,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411658,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70795.htm","linkFileType":{"id":5,"text":"html"}},{"id":6738,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/sir20045219/","linkFileType":{"id":5,"text":"html"}}],"scale":"5000000","country":"United States","state":"Michigan","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -83,\n 42.25\n ],\n [\n -83,\n 42.85\n ],\n [\n -84.0014,\n 42.85\n ],\n [\n -84.0014,\n 42.25\n ],\n [\n -83,\n 42.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602381","contributors":{"authors":[{"text":"Francy, Donna S. 0000-0001-9229-3557 dsfrancy@usgs.gov","orcid":"https://orcid.org/0000-0001-9229-3557","contributorId":1853,"corporation":false,"usgs":true,"family":"Francy","given":"Donna","email":"dsfrancy@usgs.gov","middleInitial":"S.","affiliations":[{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true},{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bushon, Rebecca N. rnbushon@usgs.gov","contributorId":2304,"corporation":false,"usgs":true,"family":"Bushon","given":"Rebecca","email":"rnbushon@usgs.gov","middleInitial":"N.","affiliations":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"preferred":true,"id":281794,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stopar, Julie","contributorId":97990,"corporation":false,"usgs":true,"family":"Stopar","given":"Julie","email":"","affiliations":[],"preferred":false,"id":281796,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Luzano, Emma J.","contributorId":108196,"corporation":false,"usgs":true,"family":"Luzano","given":"Emma","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":281797,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fout, G. Shay","contributorId":44999,"corporation":false,"usgs":true,"family":"Fout","given":"G.","email":"","middleInitial":"Shay","affiliations":[],"preferred":false,"id":281795,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70055,"text":"ofr20041033 - 2004 - 1999 Volcanic activity in Alaska and Kamchatka: Summary of events and response of the Alaska Volcano Observatory","interactions":[],"lastModifiedDate":"2024-07-17T21:05:21.15412","indexId":"ofr20041033","displayToPublicDate":"2005-02-10T00:00:00","publicationYear":"2004","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":"2004-1033","title":"1999 Volcanic activity in Alaska and Kamchatka: Summary of events and response of the Alaska Volcano Observatory","docAbstract":"The Alaska Volcano Observatory (AVO) monitors 41 historically active volcanoes along the Aleutian Arc. Twenty are seismically monitored and for the rest, the AVO monitoring program relies mainly on daily analysis of satellite images, pilot reports, and observations of local residents and ship's crews. In 1999, AVO responded to eruptive activity or suspect volcanic activity at 7 volcanic centers: Wrangell, Shrub mud volcano, Iliamna, Veniaminof, Pavlof, Shishaldin, and Vsevidof volcanoes. Of these, in 1999, AVO had real-time, continuously recording seismic networks at Iliamna, and Shishaldin. The phrase “suspect volcanic activity” (SVA), used to characterize several responses, is an eruption report or report of unusual activity that is subsequently determined to be normal or enhanced fumarolic activity, weather-related phenomena, or a non-volcanic event.
In addition to responding to eruptive activity at Alaska volcanoes, AVO also disseminated information for the Kamchatkan Volcanic Eruption Response Team (KVERT) about the 1999 activity of four Russian volcanoes: Sheveluch, Klyuchevskoy, Bezimianny, and Karymsky volcanoes.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041033","usgsCitation":"McGimsey, R.G., Neal, C., and Girina, O., 2004, 1999 Volcanic activity in Alaska and Kamchatka: Summary of events and response of the Alaska Volcano Observatory: U.S. Geological Survey Open-File Report 2004-1033, 45 p., https://doi.org/10.3133/ofr20041033.","productDescription":"45 p.","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":431200,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70120.htm","text":"Vsevidof, Shishaldin, Pavlof, and Veniaminof Volcanoes"},{"id":431199,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70119.htm","text":"Shishaldin Volcano","linkFileType":{"id":5,"text":"html"}},{"id":431198,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_70118.htm","text":"Shrub Mud Volcano","linkFileType":{"id":5,"text":"html"}},{"id":186629,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6735,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1033/","linkFileType":{"id":5,"text":"html"}}],"country":"Russia, United States","state":"Alaska","otherGeospatial":"Kamchatka Peninsula","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -141.07432048552,\n 64.31013591087381\n ],\n [\n -168.160235291931,\n 64.83831129681298\n ],\n [\n -170.40374415238404,\n 55.630188934225885\n ],\n [\n -179.9,\n 51.30691891935581\n ],\n [\n -174.92509387239826,\n 51.12271831308922\n ],\n [\n -166.01806404653644,\n 52.28385783194997\n ],\n [\n -147.52132672981213,\n 56.96202485336042\n ],\n [\n -140.71114468843984,\n 59.20190453481136\n ],\n [\n -141.07432048552,\n 64.31013591087381\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 165.4871552289449,\n 58.01237121857304\n ],\n [\n 157.2678748585049,\n 58.94640775098463\n ],\n [\n 154.87368761680005,\n 56.1679163844061\n ],\n [\n 153.64449792252162,\n 49.863785363319494\n ],\n [\n 155.84502645042463,\n 49.88235300641058\n ],\n [\n 161.42220932950391,\n 51.97361910012589\n ],\n [\n 165.4871552289449,\n 58.01237121857304\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd491ae4b0b290850eee38","contributors":{"authors":[{"text":"McGimsey, Robert G. 0000-0001-5379-7779 mcgimsey@usgs.gov","orcid":"https://orcid.org/0000-0001-5379-7779","contributorId":2352,"corporation":false,"usgs":true,"family":"McGimsey","given":"Robert","email":"mcgimsey@usgs.gov","middleInitial":"G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":281773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neal, Christina A. 0000-0002-7697-7825","orcid":"https://orcid.org/0000-0002-7697-7825","contributorId":82660,"corporation":false,"usgs":true,"family":"Neal","given":"Christina A.","affiliations":[],"preferred":false,"id":281775,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Girina, Olga","contributorId":37406,"corporation":false,"usgs":true,"family":"Girina","given":"Olga","affiliations":[],"preferred":false,"id":281774,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70049,"text":"ofr20041301 - 2004 - Preliminary physical stratigraphy and geophysical data of the USGS Elizabethtown core (BL-244/BL-C-1-2003), Bladen County, North Carolina","interactions":[],"lastModifiedDate":"2026-03-02T18:52:09.366569","indexId":"ofr20041301","displayToPublicDate":"2005-02-10T00:00:00","publicationYear":"2004","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":"2004-1301","title":"Preliminary physical stratigraphy and geophysical data of the USGS Elizabethtown core (BL-244/BL-C-1-2003), Bladen County, North Carolina","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr20041301","usgsCitation":"Self-Trail, J.M., Wrege, B., Prowell, D., Seefelt, E., and Weems, R., 2004, Preliminary physical stratigraphy and geophysical data of the USGS Elizabethtown core (BL-244/BL-C-1-2003), Bladen County, North Carolina (Version 1.0): U.S. Geological Survey Open-File Report 2004-1301, 1 CD-ROM : ill. 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Carolina\",\"nation\":\"USA \"}}]}","edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cce2","contributors":{"authors":[{"text":"Self-Trail, Jean M. jstrail@usgs.gov","contributorId":2205,"corporation":false,"usgs":true,"family":"Self-Trail","given":"Jean","email":"jstrail@usgs.gov","middleInitial":"M.","affiliations":[{"id":596,"text":"U.S. Geological Survey National Center","active":false,"usgs":true}],"preferred":false,"id":281757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wrege, B.M.","contributorId":100405,"corporation":false,"usgs":true,"family":"Wrege","given":"B.M.","affiliations":[],"preferred":false,"id":281761,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prowell, D.C.","contributorId":95475,"corporation":false,"usgs":true,"family":"Prowell","given":"D.C.","affiliations":[],"preferred":false,"id":281760,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Seefelt, E.L.","contributorId":93977,"corporation":false,"usgs":true,"family":"Seefelt","given":"E.L.","affiliations":[],"preferred":false,"id":281759,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Weems, R.E.","contributorId":44920,"corporation":false,"usgs":true,"family":"Weems","given":"R.E.","affiliations":[],"preferred":false,"id":281758,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":70019,"text":"ofr20041447 - 2004 - A preliminary assessment of geologic framework and sediment thickness studies relevant to prospective US submission on extended continental shelf","interactions":[],"lastModifiedDate":"2012-02-02T00:13:36","indexId":"ofr20041447","displayToPublicDate":"2005-02-10T00:00:00","publicationYear":"2004","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":"2004-1447","title":"A preliminary assessment of geologic framework and sediment thickness studies relevant to prospective US submission on extended continental shelf","docAbstract":"Under the provisions of Articles 76 and 77 of the United Nations Convention on the Law of the Sea (UNCLOS), coastal States have sovereign rights over the continental shelf territory beyond 200-nautical mile (nm) from the baseline from which the territorial sea is measured if certain conditions are met regarding the geologic and physiographic character of the legal continental shelf as defined in those articles. These claims to an extended continental shelf must be supported by relevant bathymetric, geophysical and geological data according to guidelines established by the Commission on the Limits of the Continental Shelf (CLCS, 1999). In anticipation of the United States becoming party to UNCLOS, Congress in 2001 directed the Joint Hydrographic Center/Center for Coastal and Ocean Mapping at the University of New Hampshire to conduct a study to evaluate data relevant to establishing the outer limit of the juridical continental shelf beyond 200 nm and to recommend what additional data might be needed to substantiate such an outer limit (Mayer and others, 2002). The resulting report produced an impressive and sophisticated GIS database of data sources. Because of the short time allowed to complete the report, all seismic reflection data were classified together; the authors therefore recommended that USGS perform additional analysis on seismic and related data holdings. The results of this additional analysis are the substance of this report, including the status of geologic framework, sediment isopach research, and resource potential in the eight regions1 identified by Mayer and others (2002) where analysis of seismic data might be crucial for establishing an outer limit .\r\n\r\nSeismic reflection and refraction data are essential in determining sediment thickness, one of the criteria used in establishing the outer limits of the juridical continental shelf. Accordingly, the initial task has been to inventory public-domain seismic data sources, primarily those regionally extensive data held within the Department of the Interior (DOI). The numerous seismic reflection and refraction surveys collected prior to 1970 by academic and governmental institutions are generally not included in this compilation, except where they provide unique data in a region. These data sources were omitted from this report because they were deemed to be of insufficient quality (poorly navigated or low resolution) to meet the CLCS standards for a submission, or they were redundant with higher-quality, more modern data. Hence, this report attempts to identify those data sets of highest utility for establishing the outer limits of the juridical continental shelf. If there was any ambiguity or uncertainty about the relevance of a data set to a continental shelf submission, either by its quality, location, or other parameter, it was included in this compilation. This report does not summarize other geophysical data (such as marine magnetics or gravity) that might be relevant to understanding crustal provenance and geological continuity.\r\n\r\nDetailed metadata tables and maps are included to facilitate the location and utilization of these sources when a comprehensive assessment (?desktop study?) is undertaken.","language":"ENGLISH","doi":"10.3133/ofr20041447","usgsCitation":"Hutchinson, D.R., Childs, J.R., Hammar-Klose, E., Dadisman, S., Edgar, N.T., and Barth, G., 2004, A preliminary assessment of geologic framework and sediment thickness studies relevant to prospective US submission on extended continental shelf: U.S. Geological Survey Open-File Report 2004-1447, CD-ROM only, https://doi.org/10.3133/ofr20041447.","productDescription":"CD-ROM only","costCenters":[],"links":[{"id":187449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6249,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1447/","linkFileType":{"id":5,"text":"html"}}],"scale":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab29d","contributors":{"authors":[{"text":"Hutchinson, Deborah R. 0000-0002-2544-5466 dhutchinson@usgs.gov","orcid":"https://orcid.org/0000-0002-2544-5466","contributorId":521,"corporation":false,"usgs":true,"family":"Hutchinson","given":"Deborah","email":"dhutchinson@usgs.gov","middleInitial":"R.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":281677,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Childs, Jonathan R. jchilds@usgs.gov","contributorId":3155,"corporation":false,"usgs":true,"family":"Childs","given":"Jonathan","email":"jchilds@usgs.gov","middleInitial":"R.","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":true,"id":281678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hammar-Klose, Erika","contributorId":36227,"corporation":false,"usgs":true,"family":"Hammar-Klose","given":"Erika","email":"","affiliations":[],"preferred":false,"id":281680,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dadisman, Shawn","contributorId":56735,"corporation":false,"usgs":true,"family":"Dadisman","given":"Shawn","affiliations":[],"preferred":false,"id":281681,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Edgar, N. Terrence","contributorId":102149,"corporation":false,"usgs":true,"family":"Edgar","given":"N.","email":"","middleInitial":"Terrence","affiliations":[],"preferred":false,"id":281682,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Barth, Ginger A. gbarth@usgs.gov","contributorId":3595,"corporation":false,"usgs":true,"family":"Barth","given":"Ginger A.","email":"gbarth@usgs.gov","affiliations":[{"id":520,"text":"Pacific Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":281679,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70024,"text":"ofr20041437 - 2004 - Digital database of faulting accompanying the 1966 Parkfield, California, earthquake","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"ofr20041437","displayToPublicDate":"2005-02-10T00:00:00","publicationYear":"2004","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":"2004-1437","title":"Digital database of faulting accompanying the 1966 Parkfield, California, earthquake","language":"ENGLISH","doi":"10.3133/ofr20041437","usgsCitation":"Crosby, C.J., 2004, Digital database of faulting accompanying the 1966 Parkfield, California, earthquake (Version 1.0): U.S. Geological Survey Open-File Report 2004-1437, 1 online sheet with DOQ, DEM, GIS zip with metadata, https://doi.org/10.3133/ofr20041437.","productDescription":"1 online sheet with DOQ, DEM, GIS zip with metadata","costCenters":[],"links":[{"id":191751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6692,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1437/","linkFileType":{"id":5,"text":"html"}}],"edition":"Version 1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d4cc","contributors":{"authors":[{"text":"Crosby, Christopher J. 0000-0003-2522-4193","orcid":"https://orcid.org/0000-0003-2522-4193","contributorId":68415,"corporation":false,"usgs":true,"family":"Crosby","given":"Christopher","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":281699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70034,"text":"ofr20041399 - 2004 - Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 2004","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"ofr20041399","displayToPublicDate":"2005-02-10T00:00:00","publicationYear":"2004","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":"2004-1399","title":"Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 2004","language":"ENGLISH","doi":"10.3133/ofr20041399","usgsCitation":"Blanchard, R., Seidenfeld, A., and McCulloch, D.S., 2004, Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 2004: U.S. Geological Survey Open-File Report 2004-1399, 1 map ; 72 x 69 cm., on sheet 87 x 86 cm., folded to 22 x 26 cm., https://doi.org/10.3133/ofr20041399.","productDescription":"1 map ; 72 x 69 cm., on sheet 87 x 86 cm., folded to 22 x 26 cm.","costCenters":[],"links":[{"id":191108,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90490,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/2004/1399/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682bbc","contributors":{"authors":[{"text":"Blanchard, R.A.","contributorId":35389,"corporation":false,"usgs":true,"family":"Blanchard","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":281727,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seidenfeld, A.V.","contributorId":90377,"corporation":false,"usgs":true,"family":"Seidenfeld","given":"A.V.","email":"","affiliations":[],"preferred":false,"id":281728,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":281726,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70035,"text":"ofr20041391 - 2004 - Airborne Digital Sensor System and GPS-aided inertial technology for direct geopositioning in rough terrain","interactions":[],"lastModifiedDate":"2012-04-15T17:28:14","indexId":"ofr20041391","displayToPublicDate":"2005-02-10T00:00:00","publicationYear":"2004","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":"2004-1391","title":"Airborne Digital Sensor System and GPS-aided inertial technology for direct geopositioning in rough terrain","docAbstract":"High-resolution airborne digital cameras with onboard data collection based on the Global Positioning System (GPS) and inertial navigation systems (INS) technology may offer a real-time means to gather accurate topographic map information by reducing ground control and eliminating aerial triangulation. Past evaluations of this integrated system over relatively flat terrain have proven successful. The author uses Emerge Digital Sensor System (DSS) combined with Applanix Corporation?s Position and Orientation Solutions for Direct Georeferencing to examine the positional mapping accuracy in rough terrain. The positional accuracy documented in this study did not meet large-scale mapping requirements owing to an apparent system mechanical failure. Nonetheless, the findings yield important information on a new approach for mapping in Antarctica and other remote or inaccessible areas of the world.","language":"ENGLISH","doi":"10.3133/ofr20041391","usgsCitation":"Sanchez, R.D., 2004, Airborne Digital Sensor System and GPS-aided inertial technology for direct geopositioning in rough terrain: U.S. Geological Survey Open-File Report 2004-1391, 10 p., https://doi.org/10.3133/ofr20041391.","productDescription":"10 p.","costCenters":[],"links":[{"id":191109,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6699,"rank":300,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1391/","linkFileType":{"id":5,"text":"html"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6888d1","contributors":{"authors":[{"text":"Sanchez, Richard D.","contributorId":66296,"corporation":false,"usgs":true,"family":"Sanchez","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":281729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70036,"text":"ofr20041389 - 2004 - GPS-aided inertial technology and navigation-based photogrammetry for aerial mapping the San Andreas fault system","interactions":[],"lastModifiedDate":"2012-04-15T17:28:14","indexId":"ofr20041389","displayToPublicDate":"2005-02-10T00:00:00","publicationYear":"2004","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":"2004-1389","title":"GPS-aided inertial technology and navigation-based photogrammetry for aerial mapping the San Andreas fault system","docAbstract":"Aerial mapping of the San Andreas Fault System can be realized more efficiently and rapidly without ground control and conventional aerotriangulation. This is achieved by the direct geopositioning of the exterior orientation of a digital imaging sensor by use of an integrated Global Positioning System (GPS) receiver and an Inertial Navigation System (INS). A crucial issue to this particular type of aerial mapping is the accuracy, scale, consistency, and speed achievable by such a system. To address these questions, an Applanix Digital Sensor System (DSS) was used to examine its potential for near real-time mapping. Large segments of vegetation along the San Andreas and Cucamonga faults near the foothills of the San Bernardino and San Gabriel Mountains were burned to the ground in the California wildfires of October-November 2003. A 175 km corridor through what once was a thickly vegetated and hidden fault surface was chosen for this study. Both faults pose a major hazard to the greater Los Angeles metropolitan area and a near real-time mapping system could provide information vital to a post-disaster response.","language":"ENGLISH","doi":"10.3133/ofr20041389","usgsCitation":"Sanchez, R.D., and Hudnut, K.W., 2004, GPS-aided inertial technology and navigation-based photogrammetry for aerial mapping the San Andreas fault system: U.S. Geological Survey Open-File Report 2004-1389, 12 p., https://doi.org/10.3133/ofr20041389.","productDescription":"12 p.","costCenters":[],"links":[{"id":191110,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":6700,"rank":300,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/2004/1389/","linkFileType":{"id":5,"text":"html"}}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1524","contributors":{"authors":[{"text":"Sanchez, Richard D.","contributorId":66296,"corporation":false,"usgs":true,"family":"Sanchez","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":281731,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hudnut, Kenneth W. 0000-0002-3168-4797 hudnut@usgs.gov","orcid":"https://orcid.org/0000-0002-3168-4797","contributorId":2550,"corporation":false,"usgs":true,"family":"Hudnut","given":"Kenneth","email":"hudnut@usgs.gov","middleInitial":"W.","affiliations":[{"id":508,"text":"Office of the AD Hazards","active":true,"usgs":true},{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":281730,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70022,"text":"ofr20041444 - 2004 - 40Ar/39Ar dating studies of minerals and rocks in various areas in Mexico: USGS/CRM scientific collaboration. 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