{"pageNumber":"5211","pageRowStart":"130250","pageSize":"25","recordCount":184617,"records":[{"id":30048,"text":"wri824125 - 1983 - Mudflow hazards along the Toutle and Cowlitz Rivers from a hypothetical failure of Spirit Lake blockage","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri824125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4125","title":"Mudflow hazards along the Toutle and Cowlitz Rivers from a hypothetical failure of Spirit Lake blockage","docAbstract":"The debris avalanche accompanying the May 18, 1980, eruption of Mount St. Helens, in southwestern Washington, buried the former outlet of Spirit Lake, located 5 miles north of the volcano, to a depth ranging to 500 feet. Since that time, Spirit Lake has had no natural outlet and its lake level and contents have increased significantly. Erosion at the crest of the debris dam on the surface of the blockage and recent studies of theblockage stratigraphy and soil properties showing that the effective crest elevation is lower than the surface crest have led to concern that the lake may someday breach through or spill over the top of the blockage. A study was made by the U.S. Geological Survey to determine the extent of inundation that might result downstream in the Toutle and Cowlitz Rivers if a hypothetical breach should occur and generate a mudflow flood of catastrophic proportions. A hypothetical breach of Spirit Lake produced a hypothetical mudflow hydrograph with a peak discharge of 2.65 million cu ft/s and a sediment concentration of 65 percent by volume at Camp Baker on the North Fork Toutle River. Elevations determined by the hydraulic routing of the mudflow were used to prepare inundation maps, indicating depths of inundation to be about 60 feet at Castle Rock and Lexington; 30-40 feet at Toutle, Toutle Lake at Silver Lake, Kelson, and Longview; and 15-20 feet at Toledo. Travel times for the peak elevation were estimated to be about 15 hours to Kid Valley on the North Fork Toutle River, 21 hours to Castle Rock, 22 hours to Toledo, and 23 hours to Kelso and Longview on the Cowlitz River. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824125","usgsCitation":"Swift, C., and Kresch, D., 1983, Mudflow hazards along the Toutle and Cowlitz Rivers from a hypothetical failure of Spirit Lake blockage: U.S. Geological Survey Water-Resources Investigations Report 82-4125, v, 15 p. :maps ;28 cm., https://doi.org/10.3133/wri824125.","productDescription":"v, 15 p. :maps ;28 cm.","costCenters":[],"links":[{"id":123441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4125/report-thumb.jpg"},{"id":58847,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58848,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58849,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58850,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58851,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58852,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58853,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58854,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58855,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58856,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4125/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58857,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4125/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b484e","contributors":{"authors":[{"text":"Swift, C.H.","contributorId":61821,"corporation":false,"usgs":true,"family":"Swift","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":202593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kresch, D. L.","contributorId":52559,"corporation":false,"usgs":true,"family":"Kresch","given":"D. L.","affiliations":[],"preferred":false,"id":202592,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29871,"text":"wri824109 - 1983 - Appraisal of the interconnection between the St Johns River and the surficial aquifer, east-central Duval County, Florida","interactions":[],"lastModifiedDate":"2024-01-08T23:01:11.323275","indexId":"wri824109","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4109","title":"Appraisal of the interconnection between the St Johns River and the surficial aquifer, east-central Duval County, Florida","docAbstract":"The proposed deepening of the navigation channel in the St. Johns River to about 46-48 feet below sea level (45 feet below mean low water) may breach up to 11 feet of limestone unit of the lower part of the surficial aquifer along a 25-mile channel. The limestone supplies water to numerous domestic wells along the river in the Jacksonville area. Recent channel improvements to about 39 feet below sea level have already breached the limestone at many locations. Where breaching has not yet occurred, less than 1 to 6 feet of undifferentiated sediments overlie the limestone. These sediments, consisting predominantly of sand, are generally too permeable to form an effective confining layer. Chloride concentrations determined from water in wells tapping the limestone unit range from 8 to 6,600 milligrams per liter. However, chloride concentrations in water from wells located more than 500 feet from the river, were generally less than 30 milligrams per liter. The proposed dredging operation is not expected to alter significantly the present hydrologic system. The current position of the interface most likely represents conditions that will be present after future channel improvements. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824109","usgsCitation":"Spechler, R., and Stone, R.B., 1983, Appraisal of the interconnection between the St Johns River and the surficial aquifer, east-central Duval County, Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4109, iv, 38 p., https://doi.org/10.3133/wri824109.","productDescription":"iv, 38 p.","costCenters":[],"links":[{"id":424204,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35616.htm","linkFileType":{"id":5,"text":"html"}},{"id":58685,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4109/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123308,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4109/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Duval County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.72156565133055,\n              30.471947232313866\n            ],\n            [\n              -81.72156565133055,\n              30.27618396890138\n            ],\n            [\n              -81.39844829812067,\n              30.27618396890138\n            ],\n            [\n              -81.39844829812067,\n              30.471947232313866\n            ],\n            [\n              -81.72156565133055,\n              30.471947232313866\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a369","contributors":{"authors":[{"text":"Spechler, R. M.","contributorId":85961,"corporation":false,"usgs":true,"family":"Spechler","given":"R. M.","affiliations":[],"preferred":false,"id":202279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stone, R. B. Jr.","contributorId":71598,"corporation":false,"usgs":true,"family":"Stone","given":"R.","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":202278,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8116,"text":"ofr83139 - 1983 - Hydrologic data from the Tamarack Wildlife Area and vicinity, Logan County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr83139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-139","title":"Hydrologic data from the Tamarack Wildlife Area and vicinity, Logan County, Colorado","docAbstract":"Hydrologic data were collected from the Tamarack Ranch Wildlife area and vicinity near Crook, Colo., during the period September 1979 to August 1981. These data will aid in the analysis of the effects of proposed water-development projects on the hydrologic system of the wildlife area. The data collected included a reconnaissance evaluation of specific conductance, a 24-hour sampling of air and water temperature at 6 sites, and periodic measurements of water levels, temperature, and specific conductance at 57 sites.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83139","usgsCitation":"Burns, A.W., 1983, Hydrologic data from the Tamarack Wildlife Area and vicinity, Logan County, Colorado: U.S. Geological Survey Open-File Report 83-139, 126 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83139.","productDescription":"126 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140649,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0139/report-thumb.jpg"},{"id":35719,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0139/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35720,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0139/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35721,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0139/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6076dc","contributors":{"authors":[{"text":"Burns, Alan W.","contributorId":41419,"corporation":false,"usgs":true,"family":"Burns","given":"Alan","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157177,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7494,"text":"ofr83390 - 1983 - Saudi Arabian seismic deep-refraction profiles; final project report","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr83390","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-390","title":"Saudi Arabian seismic deep-refraction profiles; final project report","docAbstract":"In February 1978 a seismic deep-refraction profile was recorded by the U.S. Geological Survey along a 1000-km line across the Arabian Shield in western Saudi Arabia. The line begins in Mesozoic cover rocks near Riyadh on the Arabian Platform, leads southwesterly across three major Precambrian tectonic provinces, traverses Cenozoic rocks of the coastal plain near Jizan (Tihamat-Asir), and terminates at the outer edge of the Farasan Bank in the southern Red Sea. More than 500 surveyed recording sites were occupied, including 19 in the Farasan Islands. Six shot points were used: five on land, with most charges placed below the water table in drill holes, and one at sea, with charges placed on the sea floor and detonated from a ship. Slightly more than 61 metric tons of explosives were used in 19 discrete firings. \r\n\r\nSeismic energy was recorded by 100 newly-developed portable seismic stations deployed in approximately 200 km-long arrays for each firing. Each station consisted of a standard 2-Hz vertical component geophone coupled to a self-contained analog recording instrument equipped with a magnetic-tape cassette.\r\n\r\nIn this final report, we fully document the field and data-processing procedures and present the final seismogram data set as both a digital magnetic tape and as record sections for each shot point. Record sections include a normalized set of seismograms, reduced at 6 km/s, and a true-amplitude set, reduced at 8 km/s, which have been adjusted for amplifier gain, individual shot size, and distance from the shot point.\r\n\r\nAppendices give recorder station and shot information, digital data set descriptions, computer program listings, arrival times used in the interpretation, and a bibliography of reports published as a result of this project.\r\n\r\nWe used two-dimensional ray-tracing techniques in the data analysis, and our interpretation is based primarily on horizontally layered models. The Arabian Shield is composed, to first-order, of two layers, each about 20 km thick, with average velocities of 6.3 km/s and 7.0 km/s, respectively. At the western shield margin the crust thins to less than 20 km total thickness, beyond which the Red Sea shelf and coastal plain are interpreted to be underlain by oceanic crust.\r\n\r\nA major crustal lateral velocity inhomogeneity northeast of Sabhah in the Shammar Tectonic Province is interpreted as the suture zone of two crustal blocks of different composition. Several high-velocity anomalies in the upper crust correlate with mapped gneissic dome structures. Two intra-crustal reflectors at13 km depth are interpreted as the tops of mafic intrusives.\r\n\r\nThe Mohorovicic discontinuity beneath the shield varies from 43 km depth in the northeast with 8.2 km/s mantle velocity to 38 km depth in the southwest with 8.0 km/s mantle velocity. Two velocity discontinuities are identified in the upper mantle, at 59 and 70 km depth.\r\n\r\nWe suggest further work, including refined analyses of the data employing filtering and synthetic seismogram techniques, as well as consideration of attenuation properties. Extension of the seismic refraction profile to the Arabian Gulf and some short profiles perpendicular to the existing profile would be fruitful areas for future field work.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83390","usgsCitation":"Healy, J.H., Mooney, W.D., Blank, H., Gettings, M.E., Kohler, W., Lamson, R., and Leone, L., 1983, Saudi Arabian seismic deep-refraction profiles; final project report: U.S. Geological Survey Open-File Report 83-390, 434 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83390.","productDescription":"434 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140466,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0390/report-thumb.jpg"},{"id":34937,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34938,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34939,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34940,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34941,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34942,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34943,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34944,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34945,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0390/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34946,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0390/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdb74","contributors":{"authors":[{"text":"Healy, J. H.","contributorId":48968,"corporation":false,"usgs":true,"family":"Healy","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":155877,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mooney, W. D.","contributorId":72376,"corporation":false,"usgs":true,"family":"Mooney","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":155881,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blank, H. R.","contributorId":50516,"corporation":false,"usgs":true,"family":"Blank","given":"H. R.","affiliations":[],"preferred":false,"id":155878,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gettings, M. E.","contributorId":25148,"corporation":false,"usgs":true,"family":"Gettings","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155876,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kohler, W.M.","contributorId":62999,"corporation":false,"usgs":true,"family":"Kohler","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":155879,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lamson, R.J.","contributorId":86762,"corporation":false,"usgs":true,"family":"Lamson","given":"R.J.","affiliations":[],"preferred":false,"id":155882,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Leone, L.E.","contributorId":71969,"corporation":false,"usgs":true,"family":"Leone","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":155880,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":7467,"text":"ofr8383 - 1983 - Quantitative microfossil, sedimentologic, and geochemical data on cores V1-80-P3, V1-80-G1, and V1-80-P8 from the continental slope off Northern California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:08","indexId":"ofr8383","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-83","title":"Quantitative microfossil, sedimentologic, and geochemical data on cores V1-80-P3, V1-80-G1, and V1-80-P8 from the continental slope off Northern California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8383","usgsCitation":"Gardner, J.V., Barron, J., Dean, W., Heusser, L., Klise, D., Poore, R., Quinterno, P., and Stone, S., 1983, Quantitative microfossil, sedimentologic, and geochemical data on cores V1-80-P3, V1-80-G1, and V1-80-P8 from the continental slope off Northern California: U.S. Geological Survey Open-File Report 83-83, 54 p. ill. ;28 cm., https://doi.org/10.3133/ofr8383.","productDescription":"54 p. ill. ;28 cm.","costCenters":[],"links":[{"id":141255,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0083/report-thumb.jpg"},{"id":34886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0083/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a86e4b07f02db64daf9","contributors":{"authors":[{"text":"Gardner, James V.","contributorId":93035,"corporation":false,"usgs":true,"family":"Gardner","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":155753,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barron, J.A. 0000-0002-9309-1145","orcid":"https://orcid.org/0000-0002-9309-1145","contributorId":95461,"corporation":false,"usgs":true,"family":"Barron","given":"J.A.","affiliations":[],"preferred":false,"id":155754,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dean, W.E.","contributorId":97099,"corporation":false,"usgs":true,"family":"Dean","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":155755,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Heusser, L.E.","contributorId":92667,"corporation":false,"usgs":true,"family":"Heusser","given":"L.E.","affiliations":[],"preferred":false,"id":155752,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Klise, D.H.","contributorId":97105,"corporation":false,"usgs":true,"family":"Klise","given":"D.H.","affiliations":[],"preferred":false,"id":155756,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Poore, R.Z.","contributorId":35314,"corporation":false,"usgs":true,"family":"Poore","given":"R.Z.","email":"","affiliations":[],"preferred":false,"id":155749,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Quinterno, P. J.","contributorId":65465,"corporation":false,"usgs":true,"family":"Quinterno","given":"P. J.","affiliations":[],"preferred":false,"id":155750,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Stone, S.M.","contributorId":87136,"corporation":false,"usgs":true,"family":"Stone","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":155751,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":30277,"text":"wri824082 - 1983 - Water resources of the Truk Islands","interactions":[],"lastModifiedDate":"2012-02-02T00:08:51","indexId":"wri824082","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4082","title":"Water resources of the Truk Islands","docAbstract":"The Truk Islands, part of the Caroline Islands in the western Pacific, consist of 19 volcanic islands and about 65 coral islets. The volcanic islands and some of the coral islets are scattered in an 820-square-mile lagoon enclosed by a 125-mile long barrier reef. Moen, although not the largest, is by far the most developed island and is the adminstrative, commercial, educational, and transporation center of the islands. Monthly rainfall records for most years are available since 1903. Rainfall-runoff comparisons show that about half the annual rainfall runs off as surface water into Truk Lagoon. Flow characteristics of the major streams, based on more than 11 years of record, are provided and the application of data for possible use in the design of reservoirs and rain catchments is included. Historical and present development of all water sources is given. The chemical analyses of surface and ground water on Moen, with the exception of water from well 9, show the good quality of the water sources. This report summarizes all hydrologic data collected and provides interpretations that can be used for development and management of the water resources. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824082","usgsCitation":"Van der Brug, O., 1983, Water resources of the Truk Islands: U.S. Geological Survey Water-Resources Investigations Report 82-4082, xvii, 240 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824082.","productDescription":"xvii, 240 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4082/report-thumb.jpg"},{"id":59060,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4082/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f02fe","contributors":{"authors":[{"text":"Van der Brug, Otto","contributorId":37347,"corporation":false,"usgs":true,"family":"Van der Brug","given":"Otto","email":"","affiliations":[],"preferred":false,"id":202972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8134,"text":"ofr83180 - 1983 - Final report on the permeability of geopressured Gulf Coastal shale cores","interactions":[],"lastModifiedDate":"2012-02-02T00:06:13","indexId":"ofr83180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-180","title":"Final report on the permeability of geopressured Gulf Coastal shale cores","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83180","usgsCitation":"Byerlee, J., and Morrow, C., 1983, Final report on the permeability of geopressured Gulf Coastal shale cores: U.S. Geological Survey Open-File Report 83-180, 9 p. ill. ;28 cm., https://doi.org/10.3133/ofr83180.","productDescription":"9 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0180/report-thumb.jpg"},{"id":35738,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0180/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4707","contributors":{"authors":[{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":157204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morrow, C.A.","contributorId":99977,"corporation":false,"usgs":true,"family":"Morrow","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":157205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7248,"text":"ofr83132 - 1983 - Hydrology of Area 61, Northern Great Plains and Rocky Mountain Coal Provinces, Colorado and New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:49","indexId":"ofr83132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-132","title":"Hydrology of Area 61, Northern Great Plains and Rocky Mountain Coal Provinces, Colorado and New Mexico","docAbstract":"Area 61 is located on the Colorado-New Mexico boundary in Huerfano and Las Animas Counties, Colorado, and Colfax County, New Mexico, and includes the Raton Mesa coal region. The 5 ,900-square-mile area is an asymmetrical structural trough bounded by the Rocky Mountains on the west and the Great Plains on the east. The area is drained by the Huerfano, Apishapa, Purgatoire, and Canadian Rivers (and their tributaries), all tributary to the Arkansas River. The principal coal-bearing formations are the Vermejo Formation of Late Cretaceous age and the Raton Formation of Late Cretaceous and Paleocene age. Much of the coal in the area is of coking quality, important to the metallurgical industry. Topographic relief in the area is greater than 8,700 feet, and this influences the climate which in turn affects the runoff pattern of area streams. Summer thunderstorms often result in flash floods. Virtually all geologic units in the region yield water. Depth to ground water ranges from land surface to 400 feet. Surface and ground water in the area contain mostly bicarbonate and sulfate ions; locally in the ground water, chloride ions predominate. Potential hydrologic problems associated with surface coal mining in the area are water-quality degradation, water-table decline, and increased erosion and sedimentation.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr83132","usgsCitation":"Abbott, P., Geldon, A.L., Cain, D., Hall, A.P., and Edelmann, P., 1983, Hydrology of Area 61, Northern Great Plains and Rocky Mountain Coal Provinces, Colorado and New Mexico (WRI/OFR): U.S. Geological Survey Open-File Report 83-132, vi, 99 p., https://doi.org/10.3133/ofr83132.","productDescription":"vi, 99 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":139915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0132/report-thumb.jpg"},{"id":34628,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604add","contributors":{"authors":[{"text":"Abbott, P.O.","contributorId":21154,"corporation":false,"usgs":true,"family":"Abbott","given":"P.O.","email":"","affiliations":[],"preferred":false,"id":154893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Geldon, Arthur L.","contributorId":16395,"corporation":false,"usgs":true,"family":"Geldon","given":"Arthur","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":154892,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cain, Doug","contributorId":101655,"corporation":false,"usgs":true,"family":"Cain","given":"Doug","email":"","affiliations":[],"preferred":false,"id":154895,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hall, Alan P.","contributorId":8464,"corporation":false,"usgs":true,"family":"Hall","given":"Alan","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":154891,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Edelmann, Patrick","contributorId":86305,"corporation":false,"usgs":true,"family":"Edelmann","given":"Patrick","affiliations":[],"preferred":false,"id":154894,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":7514,"text":"ofr83524 - 1983 - Spectrographic analyses of panned concentrate from stream-sediment samples from the Mazatzal Wilderness and Mazatzal Wilderness Contiguous Roadless Area, Gila, Maricopa, and Yavapai Counties, Arizona","interactions":[],"lastModifiedDate":"2021-09-28T18:06:30.205922","indexId":"ofr83524","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-524","title":"Spectrographic analyses of panned concentrate from stream-sediment samples from the Mazatzal Wilderness and Mazatzal Wilderness Contiguous Roadless Area, Gila, Maricopa, and Yavapai Counties, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83524","usgsCitation":"Marsh, S.P., Erickson, M.S., Forn, C., and McDougal, C.M., 1983, Spectrographic analyses of panned concentrate from stream-sediment samples from the Mazatzal Wilderness and Mazatzal Wilderness Contiguous Roadless Area, Gila, Maricopa, and Yavapai Counties, Arizona: U.S. Geological Survey Open-File Report 83-524, Report: 38 p.; 1 Plate: 36.06 × 53.58 inches, https://doi.org/10.3133/ofr83524.","productDescription":"Report: 38 p.; 1 Plate: 36.06 × 53.58 inches","costCenters":[],"links":[{"id":34981,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0524/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34980,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0524/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0524/report-thumb.jpg"},{"id":108461,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14089.htm","linkFileType":{"id":5,"text":"html"},"description":"14089"}],"country":"United States","state":"Arizona","county":"Gila County, Maricopa County, Yavapai County","otherGeospatial":"Mazatzal Wilderness, Mazatzal Wilderness Contiguous Roadless Area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.7810,\n              33.8920\n            ],\n            [\n              -111.4080,\n              33.8920\n            ],\n            [\n              -111.4080,\n              34.4010\n            ],\n            [\n              -111.7810,\n              34.4010\n            ],\n            [\n              -111.7810,\n              33.8920\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e2b","contributors":{"authors":[{"text":"Marsh, Sherman P.","contributorId":42950,"corporation":false,"usgs":true,"family":"Marsh","given":"Sherman","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":155956,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, M. S.","contributorId":35302,"corporation":false,"usgs":true,"family":"Erickson","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155955,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forn, C.L.","contributorId":46935,"corporation":false,"usgs":true,"family":"Forn","given":"C.L.","affiliations":[],"preferred":false,"id":155957,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McDougal, C. M.","contributorId":21129,"corporation":false,"usgs":true,"family":"McDougal","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":155954,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":64596,"text":"i1420(NL15) - 1983 - Quaternary geologic map of the Minneapolis 4 degrees x 6 degrees quadrangle, United States","interactions":[],"lastModifiedDate":"2018-09-18T18:39:14","indexId":"i1420(NL15)","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1420(NL-15)","subseriesTitle":"GAUS","title":"Quaternary geologic map of the Minneapolis 4 degrees x 6 degrees quadrangle, United States","language":"ENGLISH","doi":"10.3133/i1420(NL15)","usgsCitation":"Fullerton, D.S., Goebel, J., Mickelson, D.M., Farrand, W.R., Clayton, L., Knox, J.C., Cahow, A., Hobbs, H.C., and Walton, M.S., 1983, Quaternary geologic map of the Minneapolis 4 degrees x 6 degrees quadrangle, United States: U.S. Geological Survey IMAP 1420(NL-15), 1 map :col. ;44 x 48 cm., on sheet 76 x 118 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1420(NL15).","productDescription":"1 map :col. ;44 x 48 cm., on sheet 76 x 118 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":187192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":9227,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/imap/i-1420/nl-15/","linkFileType":{"id":5,"text":"html"}},{"id":106745,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9223.htm","linkFileType":{"id":5,"text":"html"},"description":"9223"}],"scale":"1000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96,44 ], [ -96,48 ], [ -90,48 ], [ -90,44 ], [ -96,44 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a24c","contributors":{"editors":[{"text":"Richmond, Gerald Martin","contributorId":89908,"corporation":false,"usgs":true,"family":"Richmond","given":"Gerald","email":"","middleInitial":"Martin","affiliations":[],"preferred":false,"id":745428,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Fullerton, David S. fullerton@usgs.gov","contributorId":448,"corporation":false,"usgs":true,"family":"Fullerton","given":"David","email":"fullerton@usgs.gov","middleInitial":"S.","affiliations":[{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":271653,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goebel, Joseph E.","contributorId":78822,"corporation":false,"usgs":true,"family":"Goebel","given":"Joseph E.","affiliations":[],"preferred":false,"id":271661,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mickelson, David M.","contributorId":57544,"corporation":false,"usgs":true,"family":"Mickelson","given":"David","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":271658,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Farrand, William R.","contributorId":65542,"corporation":false,"usgs":true,"family":"Farrand","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":271660,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Clayton, Lee","contributorId":95960,"corporation":false,"usgs":true,"family":"Clayton","given":"Lee","email":"","affiliations":[],"preferred":false,"id":271662,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Knox, James C.","contributorId":62247,"corporation":false,"usgs":true,"family":"Knox","given":"James","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":271659,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Cahow, Adam","contributorId":41084,"corporation":false,"usgs":true,"family":"Cahow","given":"Adam","email":"","affiliations":[],"preferred":false,"id":271656,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Hobbs, Howard C.","contributorId":43439,"corporation":false,"usgs":true,"family":"Hobbs","given":"Howard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":271657,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Walton, Matt S. Jr.","contributorId":33335,"corporation":false,"usgs":true,"family":"Walton","given":"Matt","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":271655,"contributorType":{"id":1,"text":"Authors"},"rank":9}]}}
,{"id":29615,"text":"wri834206 - 1983 - Trends in polychlorinated biphenyl concentrations in Hudson River water five years after elimination of point sources","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri834206","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4206","title":"Trends in polychlorinated biphenyl concentrations in Hudson River water five years after elimination of point sources","docAbstract":"Industrial discharge of polychlorinated biphenyls (PCBs) to the Hudson River from 1950 to the mid-1970 's has resulted in serious degradation of the water. Contaminated river-bottom sediments continue to contribute PCBs to the river water. Concentrations in the sediment range from several hundred micrograms per gram near the outfall to less than 10 micrograms per gram in the lower estuary. PCBs are supplied by bottom sediments to the overlying water by two mechanisms--desorption and resuspension. Because desorption is a relatively constant process, concentrations of PCBs decrease as water discharge increases. At high flow, however, scouring by turbulence causes resuspension of PCB-laden sediment. Transport rates indicate that most PCBs enter the water from the most contaminated sediments, which are within 20 kilometers of the outfall. Mean daily transport from the upper river (except during high discharges) has decreased from 10 kilograms in 1976 to 5 kilograms in the late 1970 's and to 1 kilogram in 1981. This decrease probably results from the burial of highly contaminated sediments by cleaner sediments originating upstream. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834206","usgsCitation":"Schroeder, R.A., and Barnes, C., 1983, Trends in polychlorinated biphenyl concentrations in Hudson River water five years after elimination of point sources: U.S. Geological Survey Water-Resources Investigations Report 83-4206, v, 33 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834206.","productDescription":"v, 33 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":160114,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4206/report-thumb.jpg"},{"id":58439,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4206/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969fe","contributors":{"authors":[{"text":"Schroeder, R. A.","contributorId":15554,"corporation":false,"usgs":true,"family":"Schroeder","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201819,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, C.R.","contributorId":85625,"corporation":false,"usgs":true,"family":"Barnes","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":201820,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8206,"text":"ofr83685 - 1983 - Floods of April 1983 in southern Mississippi and southeastern Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:05:59","indexId":"ofr83685","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-685","title":"Floods of April 1983 in southern Mississippi and southeastern Louisiana","docAbstract":"Extreme flooding occurred in April 1983 in southern Mississippi and southeastern Louisiana. The floods resulted from a near-stationary cold front, which moved slowly across Louisiana and Mississippi. Flood heights and discharges of many streams exceeded previously known maximums of record, and for many the recurrence interval of peak discharge exceeded 100 years. On Black Creek, near Brooklyn, Miss., the previous maximum stage (since 1961) was exceeded by 4.26 ft, and the April 7 peak discharge of 42,500 cu ft/sec was about two times the previous maximum discharge. This flood exceeded the 100-yr event. In southeastern Louisiana, the area with the most severe flooding was in the Bogue Chitto basin. At the Franklinton, LA, Station, the April 7 peak discharge of 125,000 cu ft/sec was more than two times the previous maximum discharge. In April 1900 the stage at this site was 29.6 ft, 4.9 ft higher than the April 1981 peak. An extreme event also occurred on the Tchefuncta River near Franklinton, LA. The previous maximum stage (since 1949) was exceeded by 3.75 ft, and the April 6 discharge of 26 ,900 cu ft/sec is more than three times the previous maximum. This discharge also exceeded the 100-yr event. Combined flood damages for both States totaled in the hundred of millions of dollars. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83685","usgsCitation":"Carlson, D.D., and Firda, G.D., 1983, Floods of April 1983 in southern Mississippi and southeastern Louisiana: U.S. Geological Survey Open-File Report 83-685, v, 37 p., 2 over-size sheets, ill., maps ;28 cm., https://doi.org/10.3133/ofr83685.","productDescription":"v, 37 p., 2 over-size sheets, ill., maps ;28 cm.","costCenters":[],"links":[{"id":139979,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0685/report-thumb.jpg"},{"id":35815,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0685/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35816,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0685/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":35817,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0685/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b0f9b","contributors":{"authors":[{"text":"Carlson, Darrell D.","contributorId":63000,"corporation":false,"usgs":true,"family":"Carlson","given":"Darrell","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Firda, Gary D. gfirda@usgs.gov","contributorId":1552,"corporation":false,"usgs":true,"family":"Firda","given":"Gary","email":"gfirda@usgs.gov","middleInitial":"D.","affiliations":[],"preferred":true,"id":157337,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29611,"text":"wri834188 - 1983 - Polychlorinated biphenyl concentrations in Hudson River water and treated drinking water at Waterford, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri834188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4188","title":"Polychlorinated biphenyl concentrations in Hudson River water and treated drinking water at Waterford, New York","docAbstract":"Past discharge of PCBs into the Hudson River has resulted in contaminant concentrations of a few tenths of a microgram per liter in the water. Waterford is one of two large municipal users of the Hudson River for drinking-water supply. The treatment scheme at the Waterford plant, which processes approximately 1 million gallons per day, is similar to that of most conventional treatment plants except for the addition of powdered activated carbon during flocculation. Comparison of PCB concentrations in river water and intake water at the plant to concentrations in treated drinking-water samples indicates that purification processes remove 80 to 90 percent of the PCBs and that final concentrations seldom exceed 0.1 microgram per liter. No significant difference was noted between the removal efficiencies during periods of high river discharge, when PCBs are associated with suspended sediment, and low discharge, when PCBs are generally dissolved. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834188","usgsCitation":"Schroeder, R.A., and Barnes, C., 1983, Polychlorinated biphenyl concentrations in Hudson River water and treated drinking water at Waterford, New York: U.S. Geological Survey Water-Resources Investigations Report 83-4188, iv, 17 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834188.","productDescription":"iv, 17 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4188/report-thumb.jpg"},{"id":58434,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4188/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db68446b","contributors":{"authors":[{"text":"Schroeder, R. A.","contributorId":15554,"corporation":false,"usgs":true,"family":"Schroeder","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201811,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, C.R.","contributorId":85625,"corporation":false,"usgs":true,"family":"Barnes","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":201812,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":18741,"text":"ofr82648 - 1983 - Water resources of the Tulalip Indian Reservation, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:07:24","indexId":"ofr82648","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"82-648","title":"Water resources of the Tulalip Indian Reservation, Washington","docAbstract":"Water will play a significant role in the future development of the Tulalip Indian Reservation. Ground-water resources are sufficient to supply several times the 1978 population. Potential problems associated with increased ground-water development are saltwater encroachment in the coastal areas and septic-tank contamination of shallow aquifers. There are sufficient good-quality surface-water resources to allow for significant expansion of the tribe)s fisheries activities. \r\n\r\nThe tribal well field is the only place where the ground-water system has been stressed) resulting in declining water levels (1,5 feet per year), The well field has a useful life of at least 1.5-20 years, This can be increased by drilling additional wells to expand the present well field, \r\n\r\nInflow of water to the reservation is in the form of precipitation (103 cubic feet per second) ft3/s)) surface-water inflow (13 ft3/s)) and ground-water inflow (4 ft3/s), Outflow is as evapotranspiration (62 ft3/s)) surface-water outflow (40 ft3/s)) and ground-water outflow (18 ft3/s), Total inflow and outflow are equal (120 ft3/s). \r\n\r\nGround water is generally suitable for domestic use without treatment) but a serious quality problem is the presence of coliform bacteria in some shallow wells, High values of turbidity and color and large concentrations of iron and manganese are common problems regarding the esthetic quality of the water, In a few places, large concentrations of chloride and dissolved solids indicate the possibility of saltwater encroachment, but no ongoing trend has been identified, \r\n\r\nSurface waters have been observed to contain undesirably high concentrations of total phosphorus and total and fecal-coliform bacteria) and to have temperatures too high for fish-rearing. The concentration of nutrients appears to be related to flow conditions. Nitrate and total nitrogen are greater in wet-season runoff than during low-flow periods) and total phosphorus shows an inverse relationship. Total phosphorus and ammonia concentrations are greatest in dry-season storm runoff. Generally) surface-water quality is adequate for fish-rearing and (with treatment) for public supply,","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82648","usgsCitation":"Drost, B., 1983, Water resources of the Tulalip Indian Reservation, Washington: U.S. Geological Survey Open-File Report 82-648, vii, 106 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr82648.","productDescription":"vii, 106 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":150951,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0648/report-thumb.jpg"},{"id":48100,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0648/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48101,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0648/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee3e2","contributors":{"authors":[{"text":"Drost, B. W.","contributorId":38526,"corporation":false,"usgs":true,"family":"Drost","given":"B. W.","affiliations":[],"preferred":false,"id":179657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2474,"text":"wsp2236 - 1983 - Guide to North Dakota's ground-water resources","interactions":[],"lastModifiedDate":"2018-03-09T13:24:53","indexId":"wsp2236","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2236","title":"Guide to North Dakota's ground-water resources","docAbstract":"Ground water, the water we pump from the Earth through wells or that which flows naturally from springs, is one of North Dakota's most valuable resources. More than 60 percent of the people living in the State use ground water for one purpose of another. It is the only source of water for thousands of farm families and their livestock. Almost all smaller cities and villages depend solely on groudn water as a source of supply. Increasingly, ground water is being used to irrigate crops and grasslands (fig. 1) during protracted dry spells so common in North Dakota. During recent years there has been a rapid development of rural water ditribution systems in which thousands of farms and rurals residences are connected via underground pipeline to a single water source, usually wells pumping ground water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2236","usgsCitation":"Paulson, Q., 1983, Guide to North Dakota's ground-water resources: U.S. Geological Survey Water Supply Paper 2236, iv, 25 p., https://doi.org/10.3133/wsp2236.","productDescription":"iv, 25 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":138747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2236/report-thumb.jpg"},{"id":28550,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2236/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648756","contributors":{"authors":[{"text":"Paulson, Q.F.","contributorId":107259,"corporation":false,"usgs":true,"family":"Paulson","given":"Q.F.","email":"","affiliations":[],"preferred":false,"id":145253,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4380,"text":"cir817 - 1983 - Scientific and technical, spatial, and bibliographic data bases and systems of the U.S. Geological Survey, 1983; including other Federal agencies","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir817","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"817","title":"Scientific and technical, spatial, and bibliographic data bases and systems of the U.S. Geological Survey, 1983; including other Federal agencies","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir817","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Scientific and technical, spatial, and bibliographic data bases and systems of the U.S. Geological Survey, 1983; including other Federal agencies (Revised edition 1983): U.S. Geological Survey Circular 817, 434 p. in various pagings ;26 cm., https://doi.org/10.3133/cir817.","productDescription":"434 p. in various pagings ;26 cm.","costCenters":[],"links":[{"id":121264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0817/report-thumb.jpg"},{"id":31489,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0817/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Revised edition 1983","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd270","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":528199,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2838,"text":"wsp2249 - 1983 - An evaluation of trends in the acidity of precipitation and the related acidification of surface water in North America","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp2249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2249","title":"An evaluation of trends in the acidity of precipitation and the related acidification of surface water in North America","docAbstract":"The acidity of precipitation in the Northeastern United States and Southeastern Canada has increased in the past, probably as a result of anthropogenic emissions. The increase in New England and New York occurred primarily before the mid-1950's. Since the mid1960's, there has been no significant change in the acidity of precipitation in this region; however, sulfate concentrations have decreased and nitrate concentrations may have increased. The time of initial acidification in Southeastern Canada is not known because of a lack of historical data. In the Southeastern United States, the evaluation of whether precipitation has been acidified is complicated by meager data. The available data show that precipitation is more acidic than would be expected for sites unaffected by anthropogenic emissions. In addition, comparison of recent data with the meager historical data suggests, but does not unambiguously prove, increased acidification since the 1950's. In the Western United States, available data indicate that precipitation at individual sites has been acidified by anthropogenic emissions. The acidification generally has been attributable to localized sources, and the time of initial acidification is undefined. \r\n\r\nAcidification of lakes and streams in the Northeastern United States has occurred in a time frame compatible with the hypothesis that acidification of precipitation was the cause. The acidification of surface waters appears to have occurred before the mid- to late 1960's. In Southeastern Canada, the best-documented cases of acidified lakes point to localized sources of acidic emissions as the cause. Sparse evidence of recent regional acidification of lakes and streams exists, but evidence for acidification of precipitation as the cause is largely lacking. In the Southeastern United States, most data on acidification of surface waters are ambiguous, and in the West, most of the data reflect local conditions. However, recent analysis of a national network of remote stream sampling stations indicates that, since the mid- to late 1960's, sulfate concentrations have increased in the Southeast and the West, with a concurrent decrease in alkalinity. Additional work is needed to test the hypothesis that regional acidification of surface waters is occurring in the Southeastern and Western United States.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2249","usgsCitation":"Turk, J.T., 1983, An evaluation of trends in the acidity of precipitation and the related acidification of surface water in North America: U.S. Geological Survey Water Supply Paper 2249, iii, 18 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2249.","productDescription":"iii, 18 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":138979,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2249/report-thumb.jpg"},{"id":29404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2249/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6848a4","contributors":{"authors":[{"text":"Turk, John T.","contributorId":53363,"corporation":false,"usgs":true,"family":"Turk","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":145880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57532,"text":"wdrCO821 - 1983 - Water Resources Data Colorado, Water Year 1982: Volume 1. Missouri River Basin, Arkansas River Basin, and Rio Grande Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:12:05","indexId":"wdrCO821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"CO-82-1","title":"Water Resources Data Colorado, Water Year 1982: Volume 1. Missouri River Basin, Arkansas River Basin, and Rio Grande Basin","language":"ENGLISH","doi":"10.3133/wdrCO821","usgsCitation":"Ugland, R., Steinheimer, J., Blattner, J., and Steger, R., 1983, Water Resources Data Colorado, Water Year 1982: Volume 1. Missouri River Basin, Arkansas River Basin, and Rio Grande Basin: U.S. Geological Survey Water Data Report CO-82-1, 403 p., 6 Fig., 5 Tab., https://doi.org/10.3133/wdrCO821.","productDescription":"403 p., 6 Fig., 5 Tab.","costCenters":[],"links":[{"id":182085,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/co-82-1/report-thumb.jpg"},{"id":88277,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/co-82-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd2cc","contributors":{"authors":[{"text":"Ugland, R.C.","contributorId":14044,"corporation":false,"usgs":true,"family":"Ugland","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":257270,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinheimer, J.T.","contributorId":81121,"corporation":false,"usgs":true,"family":"Steinheimer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":257273,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blattner, J.L.","contributorId":44541,"corporation":false,"usgs":true,"family":"Blattner","given":"J.L.","affiliations":[],"preferred":false,"id":257271,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steger, R.D.","contributorId":78008,"corporation":false,"usgs":true,"family":"Steger","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":257272,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":17804,"text":"ofr83906 - 1983 - Underwater gravity meter survey of San Francisco and San Pablo bays, California, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr83906","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-906","title":"Underwater gravity meter survey of San Francisco and San Pablo bays, California, 1982","docAbstract":"Seafloor gravity measurements were made at 281 bottom stations in San Francisco and San Pablo Bays, California, on a series of lines oriented approximately NNE.. Line spacing was approximately 2.8 km and stations along the lines mere spaced 0.5 to 1.5 km apart, between 0.5 and 1.5 km perpendicular to the axis. Sample Bouguer anomalies in the San Francisco Bay range from -15 to +15 mGals (?0.1 mgal), while anomalies in the San Pablo Bay are consistently negative, ranging from +4.0 to -40.0 mGal (?0.2 mGal).","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83906","usgsCitation":"Childs, J.R., Beyer, L.A., McCulloch, D.S., McHendrie, G., and Steele, W., 1983, Underwater gravity meter survey of San Francisco and San Pablo bays, California, 1982: U.S. Geological Survey Open-File Report 83-906, 28 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83906.","productDescription":"28 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":149192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0906/report-thumb.jpg"},{"id":47044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0906/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f645","contributors":{"authors":[{"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":177897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beyer, L. A.","contributorId":63403,"corporation":false,"usgs":true,"family":"Beyer","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":177900,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McCulloch, D. S.","contributorId":78315,"corporation":false,"usgs":true,"family":"McCulloch","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":177901,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McHendrie, G.A.","contributorId":40599,"corporation":false,"usgs":true,"family":"McHendrie","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":177899,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Steele, W. C.","contributorId":34117,"corporation":false,"usgs":true,"family":"Steele","given":"W. C.","affiliations":[],"preferred":false,"id":177898,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":57533,"text":"wdrCO823 - 1983 - Water Resources Data Colorado, Water Year 1982: Volume 3. Dolores River Basin, Green River Basin, and San Juan River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:12:05","indexId":"wdrCO823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"CO-82-3","title":"Water Resources Data Colorado, Water Year 1982: Volume 3. Dolores River Basin, Green River Basin, and San Juan River Basin","language":"ENGLISH","doi":"10.3133/wdrCO823","usgsCitation":"Steinheimer, J., Ugland, R., Burch, H., and Wilson, E., 1983, Water Resources Data Colorado, Water Year 1982: Volume 3. Dolores River Basin, Green River Basin, and San Juan River Basin: U.S. Geological Survey Water Data Report CO-82-3, 366 p., 6 Fig., 5 Tab, https://doi.org/10.3133/wdrCO823.","productDescription":"366 p., 6 Fig., 5 Tab","costCenters":[],"links":[{"id":182086,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/co-82-3/report-thumb.jpg"},{"id":88278,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/co-82-3/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd2df","contributors":{"authors":[{"text":"Steinheimer, J.T.","contributorId":81121,"corporation":false,"usgs":true,"family":"Steinheimer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":257276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ugland, R.C.","contributorId":14044,"corporation":false,"usgs":true,"family":"Ugland","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":257274,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Burch, H.E.","contributorId":27936,"corporation":false,"usgs":true,"family":"Burch","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":257275,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wilson, E.A.","contributorId":92334,"corporation":false,"usgs":true,"family":"Wilson","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":257277,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1329,"text":"wsp2201 - 1983 - Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","interactions":[{"subject":{"id":8772,"text":"ofr81911 - 1981 - Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","indexId":"ofr81911","publicationYear":"1981","noYear":false,"title":"Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":1329,"text":"wsp2201 - 1983 - Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","indexId":"wsp2201","publicationYear":"1983","noYear":false,"title":"Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp2201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2201","title":"Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona","docAbstract":"The N aquifer is the main source of water in the 5,400-square-mile Black Mesa area in the Navajo and Hopi Indian Reservations in northeastern Arizona. The N aquifer consists of the Navajo Sandstone and parts of the underlying Kayenta Formation and Wingate Sandstone of Jurassic and Triassic age. Maximum saturated thickness of the aquifer is about 1,050 feet in the northwestern part of the area, and the aquifer thins to extinction to the southeast. Water is under confined conditions in the central 3,300 square miles of the area. To the east, north, and west of Black Mesa, the aquifer is exposed at the surface, and water is unconfined. The aquifer was in equilibrium before about 1965. Recharge of about 13,000 acre-feet per year was balanced primarily by discharge near Moenkopi Wash and Laguna Creek and by evapotranspiration. At least 180 million acre-feet of water was in storage. The estimated average hydraulic conductivity of the aquifer is 0.65 foot per day. The confined storage coefficient is estimated to be about 0.0004 where the aquifer is thickest, and the estimated unconfined storage coefficient ranges from 0.10 to 0.15. \r\n\r\nGround-water withdrawals that averaged 5,300 acre-feet per year from 1976 to 1979 have caused water levels to decline in wells in the confined part of the aquifer. Withdrawals include an average of 3,700 acre-feet per year to supply a coal-slurry pipeline from a coal mine on Black Mesa. Six observation wells equipped with water-level recorders have been used to monitor aquifer response. The water level in one well 32 miles south of the mine declined 17 feet from 1972 through 1979 and 3.5 feet during 1979. \r\n\r\nA mathematical model of the N aquifer was developed and calibrated for equilibrium and nonequilibrium conditions. The model was used in part to improve estimates of aquifer characteristics and the water budget, and it successfully reproduced the observed response of the aquifer through 1979. The model results indicate that about 95 percent of the 44,000 acre-feet of water pumped from 1965 to 1979 was withdrawn from storage, but the reduction amounted to less than 0.03 percent of total storage. Water-level declines through 1979 were estimated to be more than 100 feet in an area of 200 square miles. Four projections of future water-level changes were made using the model. The most probable projection indicates that water-level declines would exceed 100 feet in an area of 440 square miles by 2001. Most of the decline would be recovered within a few years if withdrawals at the mine ceased. By 1990, however, municipal-supply pumpage is expected to exceed pumpage at the mine, and this pumpage would continue to have significant impacts on water levels in the Black Mesa area.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2201","usgsCitation":"Eychaner, J.H., 1983, Geohydrology and effects of water use in the Black Mesa area, Navajo and Hopi Indian Reservations, Arizona: U.S. Geological Survey Water Supply Paper 2201, vi, 26 p. :ill. ;28 cm., https://doi.org/10.3133/wsp2201.","productDescription":"vi, 26 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":138019,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2201/report-thumb.jpg"},{"id":26384,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2201/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a731","contributors":{"authors":[{"text":"Eychaner, James H.","contributorId":102050,"corporation":false,"usgs":true,"family":"Eychaner","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":982,"text":"wsp2200 - 1983 - Analysis and computer simulation of stream-aquifer hydrology, Arkansas River Valley, southwestern Kansas","interactions":[{"subject":{"id":7811,"text":"ofr81686 - 1981 - Analysis and computer simulation of stream-aquifer hydrology, Arkansas River valley, southwestern Kansas","indexId":"ofr81686","publicationYear":"1981","noYear":false,"title":"Analysis and computer simulation of stream-aquifer hydrology, Arkansas River valley, southwestern Kansas"},"predicate":"SUPERSEDED_BY","object":{"id":982,"text":"wsp2200 - 1983 - Analysis and computer simulation of stream-aquifer hydrology, Arkansas River Valley, southwestern Kansas","indexId":"wsp2200","publicationYear":"1983","noYear":false,"title":"Analysis and computer simulation of stream-aquifer hydrology, Arkansas River Valley, southwestern Kansas"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp2200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2200","title":"Analysis and computer simulation of stream-aquifer hydrology, Arkansas River Valley, southwestern Kansas","docAbstract":"A study was made, in cooperation with the Division of Water Resources, Kansas State Board of Agriculture, to determine geohydrologic conditions underlying nearly 110,000 acres of the Arkansas River Valley between the Colorado-Kansas State line and the Bear Creek Fault zone in southwestern Kansas. The Arkansas River meanders atop and interacts hydraulically with the area's unconfined sand and gravel aquifer. Owing to decreasing recharge and increasing discharge during the 1970's, water levels declined an average of 4 feet during 1970-79. Average annual streamflow at Syracuse, Kansas, also decreased from 232 cubic feet per second during 1951-69 to 85 cubic feet per second during 1970-79. \r\n\r\nA digital-computer model was calibrated to simulate the trends of historic water levels and streamflow during 1970-79. Simulated 1975-79 conditions depict an annual recharge to the aquifer of 15,000 acre-ft (acre-feet) from river leakage, 9,000 acre-ft from boundary inflow, and 50,000 acre-ft from deep percolation. Simulated annual discharge consists of 12,000 acre-ft to boundary outflow across the Bear Creek Fault zone, 1,000 acre-ft as leakage to the Arkansas River, 11,000 acre-ft to groundwater evaporation, and 57,000 acre-ft to pumpage. Simulated annual recharge was 7,000 acre-ft less than simulated annual discharge of 81,000 acre-ft. \r\n\r\nSimulation indicates that: (1) The long-term effects of less recharge from smaller than average amounts of annual precipitation during the 1970's were offset by more recharge during brief, timely periods of much greater than the mean monthly amounts of precipitation, and (2) the effects of the increased pumpage were partly offset by increased recharge resulting from increased irrigation. Model results indicate that the water-level decline and streamflow shortage during 1970-79 were affected more directly by departures from historic (1951-69) rates of incoming streamflow than by either the smaller than average amounts of precipitation or the increased pumpage during the 1970's. Results also indicate that waterlevel declines and streamflow reduction would stabilize or reverse during 1980-82 if one of the following conditions prevailed: (1) Monthly precipitation increased to 25 percent greater than the normal for 3 years. (2) pumpage decreased to 50 percent of the 1979 rate or, (3) incoming streamflow increased to the 1951-69 rate.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2200","usgsCitation":"Barker, R., Sauer, C.G., and Dunlap, L.E., 1983, Analysis and computer simulation of stream-aquifer hydrology, Arkansas River Valley, southwestern Kansas: U.S. Geological Survey Water Supply Paper 2200, vii, 59 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2200.","productDescription":"vii, 59 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":137876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2200/report-thumb.jpg"},{"id":25553,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2200/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25554,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680ca5","contributors":{"authors":[{"text":"Barker, R.A.","contributorId":28952,"corporation":false,"usgs":true,"family":"Barker","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":142963,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sauer, C. G.","contributorId":52548,"corporation":false,"usgs":true,"family":"Sauer","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":142965,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunlap, L. E.","contributorId":45685,"corporation":false,"usgs":true,"family":"Dunlap","given":"L.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":142964,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43299,"text":"ofr83565 - 1983 - Land use series, Aztec [quadrangle], New Mexico-Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr83565","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-565","title":"Land use series, Aztec [quadrangle], New Mexico-Colorado","language":"ENGLISH","doi":"10.3133/ofr83565","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Land use series, Aztec [quadrangle], New Mexico-Colorado: U.S. Geological Survey Open-File Report 83-565, maps :photocopy ;45 x 73 cm., on sheets 77 x 107 cm., https://doi.org/10.3133/ofr83565.","productDescription":"maps :photocopy ;45 x 73 cm., on sheets 77 x 107 cm.","costCenters":[],"links":[{"id":161607,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a109","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":531103,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53500,"text":"fwsobs82_11_13 - 1983 - Species profiles: life histories and environmental requirements of coastal fishes and invertebrates (mid Atlantic): surf clam","interactions":[],"lastModifiedDate":"2012-02-02T00:11:39","indexId":"fwsobs82_11_13","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/11.13","title":"Species profiles: life histories and environmental requirements of coastal fishes and invertebrates (mid Atlantic): surf clam","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Fay, C.W., Neves, R.J., and Pardue, G.B., 1983, Species profiles: life histories and environmental requirements of coastal fishes and invertebrates (mid Atlantic): surf clam: FWS/OBS 82/11.13, v, 23 p. : ill., 1 map; 28 cm.","productDescription":"v, 23 p. : ill., 1 map; 28 cm.","costCenters":[],"links":[{"id":177824,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e7d","contributors":{"authors":[{"text":"Fay, Clemon W.","contributorId":60293,"corporation":false,"usgs":true,"family":"Fay","given":"Clemon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":247709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neves, Richard J.","contributorId":8909,"corporation":false,"usgs":true,"family":"Neves","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":247707,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pardue, Garland B.","contributorId":53014,"corporation":false,"usgs":true,"family":"Pardue","given":"Garland","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":247708,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44527,"text":"wri824120 - 1983 - Hydrogeology for land-use planning: the Peters Creek area, Municipality of Anchorage, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"wri824120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4120","title":"Hydrogeology for land-use planning: the Peters Creek area, Municipality of Anchorage, Alaska","docAbstract":"Wells currently provide all water supplies in the area. Most wells obtain enough water for individual household needs from unconsolidated, principally glacial and glacioalluvial deposits. In some places, however, wells must be drilled into the underlying bedrock to obtain adequate supplies. It may be possible to develop small community supplies--for individual trailer courts or subdivisions--in areas where yields of 20 gallons per minute or greater are reported for private, domestic wells. Peters Creek is a potential source of surface-water supply, but it would have to be treated to remove glacial silt during summer months. The chemical quality of both ground water and surface water in the area in generally acceptable for most uses. Foundation and excavation conditions, the potential for water pollution from onsite disposal of wastewater through septic tank systems, and the suitability of specific areas for certain types of development may be affected by the following factors: wetlands and areas of shallow ground water underlie about 30 percent of the study area; landslope exceeds 20 percent in about a third of the area; areas of fine-grained, low-permeability sediments are present locally; bedrock is within 25 feet of the land surface in about a third of the area. (USGS)","language":"ENGLISH","doi":"10.3133/wri824120","usgsCitation":"Brunett, J.O., and Lee, M., 1983, Hydrogeology for land-use planning: the Peters Creek area, Municipality of Anchorage, Alaska: U.S. Geological Survey Water-Resources Investigations Report 82-4120, 7 maps on 3 sheets : both sides, some col. ; 58 x 80 cm. and smaller, sheets 61 x 89 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri824120.","productDescription":"7 maps on 3 sheets : both sides, some col. ; 58 x 80 cm. and smaller, sheets 61 x 89 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":161719,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db625195","contributors":{"authors":[{"text":"Brunett, Jilann O.","contributorId":92230,"corporation":false,"usgs":true,"family":"Brunett","given":"Jilann","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":229936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, Michael 0000-0002-8260-8794","orcid":"https://orcid.org/0000-0002-8260-8794","contributorId":7334,"corporation":false,"usgs":true,"family":"Lee","given":"Michael","affiliations":[],"preferred":false,"id":229935,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}