{"pageNumber":"1597","pageRowStart":"39900","pageSize":"25","recordCount":46651,"records":[{"id":7612,"text":"ofr83251 - 1983 - Water resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1983","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"ofr83251","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":"83-251","title":"Water resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1983","docAbstract":"Water-resources investigations of the U.S. Geological Survey in Missouri consist of collecting hydrologic data and making interpretive investigations. These data and the results of the investigations are published or released by either the U.S. Geological Survey or by cooperating agencies. This report describes the data-collection activities and investigations in Missouri for the 1983 fiscal year and provides an extensive list of water-resources references for the State of Missouri. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83251","usgsCitation":"Kratzer, W.M., 1983, Water resources investigations of the U.S. Geological Survey in Missouri, fiscal year 1983: U.S. Geological Survey Open-File Report 83-251, ii, 55 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83251.","productDescription":"ii, 55 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0251/report-thumb.jpg"},{"id":35101,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0251/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faf42","contributors":{"authors":[{"text":"Kratzer, Wanietia M.","contributorId":40978,"corporation":false,"usgs":true,"family":"Kratzer","given":"Wanietia","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":156302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29520,"text":"wri834074 - 1983 - Effects of ground-water development in the North Fort Hood area, Coryell County, Texas","interactions":[],"lastModifiedDate":"2016-08-09T13:48:15","indexId":"wri834074","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":"83-4074","title":"Effects of ground-water development in the North Fort Hood area, Coryell County, Texas","docAbstract":"

The U.S. Army Corps of Engineers is studying the adequacy of the existing ground-water supplies of North Fort Hood, located in Coryell County in central Texas and an important part of the U.S. Army's Fort Hood Military Reservation. The U.S. Geological Survey was requested to compile the available ground-water data, collect additional data, and assess the effects of the long-term development of ground water in the North Fort Hood area.

\n

Nearly all ground water in the North Fort Hood area is withdrawn from the Hensell and Hosston Members of the Travis Peak Formation. The total average annual rates of ground-water withdrawals, mostly for public supply, has steadily increased from nearly 0.5 million gallons per day during 1955 to mare than 1.5 million gallons per day during 1980.

\n

The principal effect of the long-term development of ground water in the area has been a large decline of water levels in wells. The water level in a well near Narth Fort Hood declined from a depth of 100 feet during 1943 to nearly 480 feet during 1982. The water level in a well at Gatesville was above ground level during 1898. A nearby well had a water level of 476 feet below land surface during 1982. The long-term average of water-level declines for wells in the area ranges from 8 to more than 9 feet per year.

\n

The historical confined (artesian) conditions of the principal aquifer have changed to water-table conditions in some areas as the artesian head 9 drops below the base of the confining layer due to pumping. The greater storage property of the unconfined system will decrease the rate of water-level declines. However, well yields will continue to decrease in relation to the general decline of hydraulic head in the aquifer.

\n

The ground water in the area is slightly saline and concentrations of some constituents generally exceed chemical-quality limits set by the U.S. Environmental Protection Agency for public water supplies. Hie historical chemical changes in the ground water generally are insignificant and appear unrelated to the large declines of water levels in wells of the area.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri834074","usgsCitation":"Sandeen, W., 1983, Effects of ground-water development in the North Fort Hood area, Coryell County, Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4074, Report: v, 48 p.; 2 Plates: 12.16 x 16.33 inches and 11.85 x 16.58 inches, https://doi.org/10.3133/wri834074.","productDescription":"Report: v, 48 p.; 2 Plates: 12.16 x 16.33 inches and 11.85 x 16.58 inches","numberOfPages":"53","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":110159,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35705.htm","linkFileType":{"id":5,"text":"html"},"description":"35705"},{"id":58358,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4074/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58359,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4074/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":58360,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4074/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119416,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4074/report-thumb.jpg"}],"country":"United States","state":"Texas","county":"Coryell County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db615317","contributors":{"authors":[{"text":"Sandeen, W.M.","contributorId":102488,"corporation":false,"usgs":true,"family":"Sandeen","given":"W.M.","affiliations":[],"preferred":false,"id":201656,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9607,"text":"ofr83713 - 1983 - RDARL4, a Fortran interface for transferring chemical analytical data from an Applied Research Laboratories electron microprobe to a PDP-11 computing system","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr83713","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":"83-713","title":"RDARL4, a Fortran interface for transferring chemical analytical data from an Applied Research Laboratories electron microprobe to a PDP-11 computing system","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83713","usgsCitation":"Huebner, J., 1983, RDARL4, a Fortran interface for transferring chemical analytical data from an Applied Research Laboratories electron microprobe to a PDP-11 computing system: U.S. Geological Survey Open-File Report 83-713, 40 p. ;28 cm., https://doi.org/10.3133/ofr83713.","productDescription":"40 p. ;28 cm.","costCenters":[],"links":[{"id":141714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0713/report-thumb.jpg"},{"id":37338,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0713/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db649fc7","contributors":{"authors":[{"text":"Huebner, J.S.","contributorId":41422,"corporation":false,"usgs":true,"family":"Huebner","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":159990,"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":27381,"text":"wri834010 - 1983 - Hydrogeologic evaluation of selected stratified-drift deposits in Connecticut","interactions":[],"lastModifiedDate":"2025-01-10T19:57:57.67083","indexId":"wri834010","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":"83-4010","title":"Hydrogeologic evaluation of selected stratified-drift deposits in Connecticut","docAbstract":"

Test borings at 28 sites and seismic-refraction profiles at 16 sites provide data on the saturated thickness and grain-size characteristics of stratified-drift deposits in five areas of Connecticut. These data, together with information on the areal extent of the deposits and their proximity to sources of induced recharge, can be used to estimate the water-yielding potential of the stratified-drift deposits. Individual wells could potentially yield moderate to possibly very large quantities of water (50 to 2000 gallons per minute) at some locations in all five areas where saturated, dominantly coarse-grained stratified drift is 40 feet thick or greater and hydraulically connected to nearby surface-water bodies. Coarse-grained stratified drift is most extensive in the Glastonbury, Haddam, and Simsbury, Connecticut areas. Saturated thickness exceeds 150 feet in parts of the Glastonbury and Haddam areas, but is less than 100 feet in most places. The best sites for developing large quantities of water are in the Glastonbury and Haddam areas where thick, saturated, coarse-grained stratified drift is hydraulically connected to the Connecticut River. Water in the stratified drift is generally of good chemical quality except for excessive iron (0.64 to 20 mg/L) and manganese (0.1 to 10 mg/L) in some samples. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834010","usgsCitation":"Grady, S.J., and Handman, E., 1983, Hydrogeologic evaluation of selected stratified-drift deposits in Connecticut: U.S. Geological Survey Water-Resources Investigations Report 83-4010, v, 56 p., https://doi.org/10.3133/wri834010.","productDescription":"v, 56 p.","costCenters":[],"links":[{"id":119860,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4010/report-thumb.jpg"},{"id":56240,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4010/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":466036,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35655.htm","text":"Bladens River area","linkFileType":{"id":5,"text":"html"}},{"id":466037,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35656.htm","text":"Glastonbury area","linkFileType":{"id":5,"text":"html"}},{"id":466038,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35657.htm","text":"Haddam area","linkFileType":{"id":5,"text":"html"}},{"id":466039,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35658.htm","text":"Simsbury area","linkFileType":{"id":5,"text":"html"}},{"id":466040,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35659.htm","text":"Willimantic River area","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Connecticut","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -73.24769490339403,\n 42.00620095205019\n ],\n [\n -73.24769490339403,\n 41.3245840419726\n ],\n [\n -71.96119276504564,\n 41.3245840419726\n ],\n [\n -71.96119276504564,\n 42.00620095205019\n ],\n [\n -73.24769490339403,\n 42.00620095205019\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db62873f","contributors":{"authors":[{"text":"Grady, S. J.","contributorId":69962,"corporation":false,"usgs":true,"family":"Grady","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Handman, E. H.","contributorId":63407,"corporation":false,"usgs":true,"family":"Handman","given":"E.","middleInitial":"H.","affiliations":[],"preferred":false,"id":198014,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61507,"text":"mf1381C - 1983 - Map and interpretation of aeromagnetic data for the Wild Rogue Wilderness, Coos and Curry Counties, Oregon","interactions":[],"lastModifiedDate":"2016-08-23T10:35:31","indexId":"mf1381C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1381","chapter":"C","title":"Map and interpretation of aeromagnetic data for the Wild Rogue Wilderness, Coos and Curry Counties, Oregon","docAbstract":"

The Wild Rogue Wilderness is located in Coos and Curry Counties, southwestern Oregon and covers part of the Bone Mountain, Marial, and Agness 15-minute quadrangles (fig. 1). It is an elongate area 19 mi by 1 to 3 mi (31 km by 1.3 to 5 km) and covers approximately 35,818 acres extending from the town of Agness to Mount Bolivar.

\n

The mapped geology of the Wild Rogue Wilderness (Gray and others, 1982) consists of a tectonic wedge of volcanic and intrusive rocks of Jurassic age surrounded on all sides by thick sequences of Jurassic, Creacetous, and Tertiary sedimentary rocks. Normally, volcanic and intrusive rocks are more magnetic than sedimentary rocks, a property which should be reflected by the areomagnetic data. We conclude, however, that most of the magnetic anomalies of the Wild Rogue Wilderness are caused by magnetic rocks that are not exposed but which occur at relatively shallow depth below the topographic surface. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1381C","usgsCitation":"Blakely, R.J., and Senior, L., 1983, Map and interpretation of aeromagnetic data for the Wild Rogue Wilderness, Coos and Curry Counties, Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1381, 36.37 x 34.88 inches, https://doi.org/10.3133/mf1381C.","productDescription":"36.37 x 34.88 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":180497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1381C.PNG"},{"id":327598,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1381-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Oregon","county":"Coos, Curry","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.08333333333333,42.583333333333336 ], [ -124.08333333333333,42.833333333333336 ], [ -123.83333333333333,42.833333333333336 ], [ -123.83333333333333,42.583333333333336 ], [ -124.08333333333333,42.583333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db655409","contributors":{"authors":[{"text":"Blakely, Richard J. 0000-0003-1701-5236 blakely@usgs.gov","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":1540,"corporation":false,"usgs":true,"family":"Blakely","given":"Richard","email":"blakely@usgs.gov","middleInitial":"J.","affiliations":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":265841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senior, Lisa","contributorId":81989,"corporation":false,"usgs":true,"family":"Senior","given":"Lisa","affiliations":[],"preferred":false,"id":265842,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":10917,"text":"ofr83566 - 1983 - Time series analysis of Cenozoic era sea level and paleotemperature data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr83566","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":"83-566","title":"Time series analysis of Cenozoic era sea level and paleotemperature data","docAbstract":"A statistical analysis of Cenozoic era sea level and paleotemperature data was performed to determine the cycles of each data set and the correspondence between them. Accordingly, each of the four time series were first analyzed independently in the univariate mode of a spectral analysis. The two basic data sets were then analyzed in a paired cross-spectral analysis. \r\n\r\nThe prominent periodic cycles remaining in the data sets after linear trend removal, were: sea level surface from seismic stratigraphy--9.6 million years, updated version of sea level surface from seismic stratigraphy--9.5 million years, continental paleotemperatures from paleobotanical interpretations--9.6 million years, and marine paleotemperatures from foraminiferal isotopic data--12.7 million years. The cross-correlation properties between the data sets of continental paleotemperatures from paleobotanical interpretations and sea level surface from seismic stratigraphy at the common prominent period of 9.6 million years were: (1) The squared coherency value which measures cross correlation between the two data sets has the value 0.30, and (2) the amount by which the continental paleotemperatures from paleobotanical interpretations data lags the sea level surface from seismic stratigraphy data is 2.70 million years.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr83566","usgsCitation":"Rosenfield, G.H., and Huffman, T.E., 1983, Time series analysis of Cenozoic era sea level and paleotemperature data: U.S. Geological Survey Open-File Report 83-566, iv, 42 p., https://doi.org/10.3133/ofr83566.","productDescription":"iv, 42 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":142435,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0566/report-thumb.jpg"},{"id":38684,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0566/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b6ce","contributors":{"authors":[{"text":"Rosenfield, George H.","contributorId":103282,"corporation":false,"usgs":true,"family":"Rosenfield","given":"George","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":162206,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Huffman, Tod E.","contributorId":14823,"corporation":false,"usgs":true,"family":"Huffman","given":"Tod","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":162205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7277,"text":"ofr83296 - 1983 - Late Proterozoic island-arc complexes and tectonic belts in the southern part of the Arabian Shield, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"ofr83296","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":"83-296","title":"Late Proterozoic island-arc complexes and tectonic belts in the southern part of the Arabian Shield, Kingdom of Saudi Arabia","docAbstract":"Two main subdivisions of layered rocks are recognized in the southern Arabian Shield south of lat 22? N. These are an older ensimatic-arc complex, which formed 1100-800 m.y. ago, and a younger marginal-arc complex, which formed 800-690 m.y. ago. The older ensimatic-arc complex, located in the southwestern part of the Shield, includes graywacke and mafic to intermediate volcanic rocks of the essentially contemporaneous Baish, Bahah, and Jiddah groups. Although the younger arc complex is also dominantly ensimatic in character, it is also partly superimposed over the older ensimaticarc complex. The superimposed portions of the younger arc complex are represented by the Ablah, Samran, and possibly the Ararat groups. The ensimatic portion of the younger arc group is represented by the Halaban group, which was deposited to the east and northeast of the older ensimatic-arc complex. The Halaban group includes andesitic and dacitic volcanic rocks and associated clastic sedimentary rocks. The layered rocks of both arc complexes are intruded by dioritic (quartz diorite, tonalite, trondhjemite) plutonic rocks. \r\n\r\nThe southern Shield is also subdivided into a number of structurally bounded, north-trending tectonic belts. Within the older ensimatic complex, three belts are recognized. From west to east, these are the Lith, Bidah, and Tayyah belts. Within these three belts, progressive facies changes indicate a gradation from deep-water facies in the south to shallow-water or-terrestrial facies in the north. The distribution of dioritic batholiths, as well as the distribution of layered-rock facies, suggests a northwest-trending axis for the older ensimatic-arc complex. The younger arc complex is present within six belts, the Makkah source papers. In Fleck and others (1980), the term 'quartz diorite' includes both tonalite and quartz diorite as defined in the International Union of Geological Sciences (IUGS) system of plutonic rock classification (Streckeisen, 1973). \r\n\r\nInitial 87Sr/86Sr ratios are not included in the appendix, but all rocks more than 660 m.y. old have initial ratios in the range 0.7021-0.7035, with only two greater than 0.7030. Thus, nothing in the Rb-Sr data suggests involvement of an older continental crust during the evolution of the southern Shield. A lead isotope study of ore minerals and potassium feldspars of the Arabian Shield by Stacey and others (1980) also suggests that no older (Archean to early Proterozoic) evolved continental-type crust underlies the southern Shield. An early summary of mapping (Schmidt and others, 1973) suggests that older sialic basement underlies the late Proterozoic layered rocks in the southern Shield. However, subsequent-mapping and the isotopic studies cited above have established that all of these rocks are of late Proterozoic age and that all rocks of the southern Shield that are more than 660 m.y. old have ensimatic or mantle isotopic characteristics. \r\n\r\nFigure 2 shows, with only two exceptions, that rocks more than 800 m.y. old are present west of the boundary separating the Tayyah and Khadra belts. The exceptions are two poorly controlled Rb-Sr ages obtained by Fleck (1980) on two quartz diorite plutons in the Malahah region (appendix 1, localities 26 and 27). Preliminary uranium-thorium zircon data of Stacey now suggest that one of these quartz diorite plutons (locality 26) has an age of approximately 640 m.y. Therefore, we prefer to discount the two dates of Fleck until further information is available. \r\n\r\nAs noted earlier and as described below, most of the rocks of the southern Arabian Shield have characteristics typical of those formed in the island-arc environment by subduction-related processes. We shall refer to the group of rocks in the western part of the southern Shield, which formed from 1100 to 800 m.y. ago, as the 'older ensimatic-arc complex' and those in the eastern and northwestern parts, which formed from 800 to 690 m.y. ago, as the 'younger marginal-arc compl","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83296","usgsCitation":"Greenwood, W., Stoeser, D.B., Fleck, R., and Stacey, J.S., 1983, Late Proterozoic island-arc complexes and tectonic belts in the southern part of the Arabian Shield, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 83-296, 49 p. maps ;28 cm., https://doi.org/10.3133/ofr83296.","productDescription":"49 p. maps ;28 cm.","costCenters":[],"links":[{"id":140032,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0296/report-thumb.jpg"},{"id":34654,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0296/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b9a","contributors":{"authors":[{"text":"Greenwood, William R.","contributorId":53789,"corporation":false,"usgs":true,"family":"Greenwood","given":"William R.","affiliations":[],"preferred":false,"id":155009,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoeser, D. B.","contributorId":18735,"corporation":false,"usgs":true,"family":"Stoeser","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":155007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fleck, R.J.","contributorId":25147,"corporation":false,"usgs":true,"family":"Fleck","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":155008,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155010,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7946,"text":"ofr83435 - 1983 - Oregon; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83435","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":"83-435","title":"Oregon; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83435","usgsCitation":"Bliss, J.D., 1983, Oregon; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-435, iv, 342 leaves ;28 cm., https://doi.org/10.3133/ofr83435.","productDescription":"iv, 342 leaves ;28 cm.","costCenters":[],"links":[{"id":140871,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0435/report-thumb.jpg"},{"id":35517,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0435/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db691238","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57270,"text":"wdrMN822 - 1983 - Water Resources Data, Minnesota Water Year 1982, Volume 2: Upper Mississippi and Missouri River Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:12:17","indexId":"wdrMN822","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":"MN-82-2","title":"Water Resources Data, Minnesota Water Year 1982, Volume 2: Upper Mississippi and Missouri River Basins","language":"ENGLISH","doi":"10.3133/wdrMN822","usgsCitation":"Gunard, K., Hess, J., Zirbel, J., and Cornelius, C., 1983, Water Resources Data, Minnesota Water Year 1982, Volume 2: Upper Mississippi and Missouri River Basins: U.S. Geological Survey Water Data Report MN-82-2, 449 p., 9 fig., https://doi.org/10.3133/wdrMN822.","productDescription":"449 p., 9 fig.","costCenters":[],"links":[{"id":184911,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/mn-82-2/report-thumb.jpg"},{"id":88255,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/mn-82-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb631","contributors":{"authors":[{"text":"Gunard, K.T.","contributorId":103733,"corporation":false,"usgs":true,"family":"Gunard","given":"K.T.","affiliations":[],"preferred":false,"id":256530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hess, J.H.","contributorId":100465,"corporation":false,"usgs":true,"family":"Hess","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":256529,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zirbel, J.L.","contributorId":70837,"corporation":false,"usgs":true,"family":"Zirbel","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":256528,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cornelius, C.E.","contributorId":106190,"corporation":false,"usgs":true,"family":"Cornelius","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":256531,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7953,"text":"ofr83439 - 1983 - Wyoming; basic data for thermal springs and wells as recorded in Geotherm","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"ofr83439","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":"83-439","title":"Wyoming; basic data for thermal springs and wells as recorded in Geotherm","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83439","usgsCitation":"Bliss, J.D., 1983, Wyoming; basic data for thermal springs and wells as recorded in Geotherm: U.S. Geological Survey Open-File Report 83-439, iv, 216 p. ;28 cm., https://doi.org/10.3133/ofr83439.","productDescription":"iv, 216 p. ;28 cm.","costCenters":[],"links":[{"id":140742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0439/report-thumb.jpg"},{"id":35524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0439/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4933","contributors":{"authors":[{"text":"Bliss, James D. jbliss@usgs.gov","contributorId":2790,"corporation":false,"usgs":true,"family":"Bliss","given":"James","email":"jbliss@usgs.gov","middleInitial":"D.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":156881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44505,"text":"wri834063 - 1983 - Identification and classification of perennial streams of Arkansas","interactions":[],"lastModifiedDate":"2023-12-12T21:53:14.81486","indexId":"wri834063","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":"83-4063","title":"Identification and classification of perennial streams of Arkansas","docAbstract":"Perennial streams are identified in a map and classified according to the relative magnitude of their 7-day, 10-year low flows. Perennial streams are identified for the entire State of Arkansas with the exception of the Mississippi Alluvial Plain. Also presented are the 7-day, 10-year low flow values at continuous-record and low-flow partial-record stations statewide. Perennial streams are defined in this report as having 7-day, 10-year low flows greater than zero. The perennial stream drainage was delineated using data from continuous-record and low-flow partial-record stations, and reconnaissance-site observations. The reconnaissance was conducted during the unusually dry summer of 1980. In analysis, the State was divided into hydrologic regions; they were used in conjunction with index stations to establish the recurrence intervals of flow observed, during the reconnaissance. When necessary, relations were developed by region to adjust observed flow to 10-year recurrence interval flows. 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Water resources data for the 1981 water year for Arizona consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; measurements of ground-water levels; and quality of water from selected wells. Also included are discharge data for crest-stage partial-record stations and water-quality data for partial-record stations. Locations of the gaging stations are shown in figures 4, 6, and 7, and of water-quality stations in figures 5 and 6. Additional water data were collected at various sites, which are not part of the systematic data-collection program, and are published as miscellaneous measurements or miscellaneous water-quality analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Arizona.

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No abstract available.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc426","contributors":{"authors":[{"text":"Lamb, T.E.","contributorId":58272,"corporation":false,"usgs":true,"family":"Lamb","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":256637,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porter, J.E.","contributorId":51779,"corporation":false,"usgs":true,"family":"Porter","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":256636,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lambert, B.F.","contributorId":30292,"corporation":false,"usgs":true,"family":"Lambert","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":256635,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edds, J.","contributorId":27549,"corporation":false,"usgs":true,"family":"Edds","given":"J.","email":"","affiliations":[],"preferred":false,"id":256634,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":57293,"text":"wdrWV821 - 1983 - Water resources data West Virginia, water year 1982","interactions":[],"lastModifiedDate":"2025-02-26T20:00:54.138059","indexId":"wdrWV821","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":"WV-82-1","title":"Water resources data West Virginia, water year 1982","docAbstract":"

Water resources data for the 1982 water year for West Virginia consist of records of stage, discharge, and water quality of streams and springs; stage and contents of lakes and reservoirs; and water levels in wells. This report contains discharge records for 116 gaging stations; stage only records for 9 gaging stations; stage and contents for 8 lakes and reservoirs; contents for 1 reservoir; change in contents for 1 reservoir; water quality for 55 gaging stations; and water levels for 29 observation wells. Also included are 2 crest-stage partial-record stations, and 1 low-flow partial record station. Additional water data were collected at various sites, not part of the systematic data collections program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal Agencies in West Virginia.

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L.L.","contributorId":81513,"corporation":false,"usgs":true,"family":"Hubbard","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":257016,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parks, T.D.","contributorId":17257,"corporation":false,"usgs":true,"family":"Parks","given":"T.D.","email":"","affiliations":[],"preferred":false,"id":257014,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weiss, D.L.","contributorId":68812,"corporation":false,"usgs":true,"family":"Weiss","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":257015,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hubbard, L.E.","contributorId":104945,"corporation":false,"usgs":true,"family":"Hubbard","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":257017,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":27014,"text":"wri834089 - 1983 - Investigation of Waikele well no. 2401-01, Oahu, Hawaii: Pumping test, well logs and water quality","interactions":[],"lastModifiedDate":"2022-01-20T20:42:32.261575","indexId":"wri834089","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":"83-4089","title":"Investigation of Waikele well no. 2401-01, Oahu, Hawaii: Pumping test, well logs and water quality","docAbstract":"Field tests indicate that an abandoned well (No. 2401-01) near the confluence of Waikele and Kipapa Streams, Oahu, Hawaii, can be reactivated to produce potable water at a rate of 400-500 gallons per minute. Previous tests in 1946 and 1954 indicated that the well tapped the brackish transition zone which inderlies the Ghyben-Herzberg lens of the Pearl Harbor aquifer. Results of this study, based on geologic and geophysical logs of the wall, as well as on pumping test and water-quality data, indicate that the slightly brackish water produced by the well results from brackish irrigation return water. It does not appear that pumping from this well will cause seawater upconing or intrusion. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834089","usgsCitation":"Eyre, P.R., 1983, Investigation of Waikele well no. 2401-01, Oahu, Hawaii: Pumping test, well logs and water quality: U.S. Geological Survey Water-Resources Investigations Report 83-4089, iv, 42 p., https://doi.org/10.3133/wri834089.","productDescription":"iv, 42 p.","costCenters":[],"links":[{"id":394614,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35717.htm"},{"id":55899,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4089/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121809,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4089/report-thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Oahu, Waikele well no. 2401-01","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -158.017,\n 21.383\n ],\n [\n -158.008,\n 21.383\n ],\n [\n -158.008,\n 21.417\n ],\n [\n -158.017,\n 21.417\n ],\n [\n -158.017,\n 21.383\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4887e4b07f02db519f44","contributors":{"authors":[{"text":"Eyre, P. 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Sediment and stream-velocity data were gathered from May 1978 to September 1981 over several magnitudes of streamflow at four cross sections near Hood. This report, prepared in cooperation with the California Department of Water Resources, contains data that show the vertical distribution and size of sediment, and the magnitude and direction of stream velocity measured at 25 points in each of the four cross sections on several occasions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83135","usgsCitation":"Harmon, J.G., 1983, Sediment and stream-velocity data for the Sacramento River near Hood, California, May 1978 to September 1981: U.S. Geological Survey Open-File Report 83-135, iv, 83 p. ill., map ;28 cm., https://doi.org/10.3133/ofr83135.","productDescription":"iv, 83 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":140856,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0135/report-thumb.jpg"},{"id":37071,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0135/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc148","contributors":{"authors":[{"text":"Harmon, Jerry G.","contributorId":30220,"corporation":false,"usgs":true,"family":"Harmon","given":"Jerry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":159541,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57355,"text":"wdrUT821 - 1983 - Water resources data for Utah, water year 1982","interactions":[],"lastModifiedDate":"2020-11-17T20:58:49.120692","indexId":"wdrUT821","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":"UT-82-1","title":"Water resources data for Utah, water year 1982","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrUT821","usgsCitation":"ReMillard, M.D., Anderson, G., Hookano, E., and Sandberg, G.W., 1983, Water resources data for Utah, water year 1982: U.S. Geological Survey Water Data Report UT-82-1, xiv, 497 p., https://doi.org/10.3133/wdrUT821.","productDescription":"xiv, 497 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":380556,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/ut-82-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/ut-82-1/report-thumb.jpg"}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd1bb","contributors":{"authors":[{"text":"ReMillard, M. D.","contributorId":38645,"corporation":false,"usgs":true,"family":"ReMillard","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":256782,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, G.C.","contributorId":64729,"corporation":false,"usgs":true,"family":"Anderson","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":256784,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hookano, E. Jr.","contributorId":70479,"corporation":false,"usgs":true,"family":"Hookano","given":"E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":256785,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":256783,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":9378,"text":"ofr83350 - 1983 - Coal-seismic, desktop computer programs in BASIC; Part 5, Perform X-square T-square analysis and plot normal moveout lines on seismogram overlay","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr83350","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":"83-350","title":"Coal-seismic, desktop computer programs in BASIC; Part 5, Perform X-square T-square analysis and plot normal moveout lines on seismogram overlay","docAbstract":"Processing of data taken with the U.S. Geological Survey's coal-seismic system is done with a desktop, stand-alone computer. Programs for this computer are written in the extended BASIC language used by the Tektronix 4051 Graphic System. This report presents computer programs to perform X-square/T-square analyses and to plot normal moveout lines on a seismogram overlay.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83350","usgsCitation":"Hasbrouck, W., 1983, Coal-seismic, desktop computer programs in BASIC; Part 5, Perform X-square T-square analysis and plot normal moveout lines on seismogram overlay: U.S. Geological Survey Open-File Report 83-350, 22 p. ;28 cm., https://doi.org/10.3133/ofr83350.","productDescription":"22 p. ;28 cm.","costCenters":[],"links":[{"id":141460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0350/report-thumb.jpg"},{"id":37095,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0350/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec97","contributors":{"authors":[{"text":"Hasbrouck, W.P.","contributorId":56646,"corporation":false,"usgs":true,"family":"Hasbrouck","given":"W.P.","affiliations":[],"preferred":false,"id":159574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}