{"pageNumber":"5291","pageRowStart":"132250","pageSize":"25","recordCount":184739,"records":[{"id":25963,"text":"wri8247 - 1982 - Ground-water resources of the White River basin, Delaware County, Indiana","interactions":[],"lastModifiedDate":"2020-11-05T21:15:00.164788","indexId":"wri8247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-47","title":"Ground-water resources of the White River basin, Delaware County, Indiana","docAbstract":"<p><span>The ground-water resources of the White River basin in and near Delaware </span><span>County, Indiana, were investigated by mapping the aquifers, calculating their </span><span>hydraulic properties, determining the distribution of potentiometric head, and </span><span>determining some of the components of the ground-water budget from data collect</span><span>ed in the field. This information was used to construct and calibrate a seven-</span><span>layer, digital ground-water-flow model. The model, constructed and calibrated </span><span>to water-level and seepage data collected during the study, simulates conditions </span><span>for the autumn of 1977. The model was used to assess ground-water potential in </span><span>terms of yield, drawdown, and streamflow depletion. </span></p><p><span>Drift covers nearly the entire area and generally ranges in thickness from 0 to 500 feet. Beneath the drift lie Silurian and Ordovician limestone, dolomite, and shale. A bedrock valley trends east-west through the center of the area. Bedrock surface relief is about 400 feet. </span></p><p><span>Six confined sand and gravel aquifers interbedded in the drift, a bedrock aquifer, and an unconfined outwash aquifer are the three major aquifer systems. The nearly horizontal, areally discontinuous, confined sand and gravel aquifers generally range in thickness from 5 to 40 feet and have an average hydraulic conductivity estimated to be 433 feet per day. The bedrock aquifer underlying all of Delaware County has a permeable thickness estimated to be 150 feet and an average transmissivity of 1,000 square feet per day. </span></p><p><span>Observation-well records indicate that water-level fluctuation is seasonal and has no long-term trends. Municipal and industrial ground-water pumpage for 1976 was 3.1 million gallons per day (4.8 cubic feet per second). On October 29, 1977, when the flow duration in the White River at Muncie was 80 percent, ground-water seepage to streams was 81 cubic feet per second. The water budget simulated in the model indicated that the rate of inflow to the ground-water system in the modeled area is 102 cubic feet per second: 80 percent from effective areal recharge of precipitation and 20 percent from ground-water flow across the area boundaries. Two percent of the ground-water discharge is pump-age, 66 percent is seepage to streams, and the remaining 32 percent is flow across the area boundaries. </span></p><p><span>Simulations of seven pumping plans provide a general assessment of the water-yielding potential of the three major aquifer systems. Model results indicate that as much as 3 million gallons per day can be developed from well fields where the average drawdown is 20 feet. Model simulations also indicate that 7 million gallons per day is available from a potential well field around Muncie. </span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8247","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources","usgsCitation":"Arihood, L.D., and Lapham, W.W., 1982, Ground-water resources of the White River basin, Delaware County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 82-47, vi, 69 p., https://doi.org/10.3133/wri8247.","productDescription":"vi, 69 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":380218,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0047/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0047/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Delaware County","otherGeospatial":"White River basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.4451,40.3792],[-85.2205,40.379],[-85.2182,40.3073],[-85.2168,40.2198],[-85.2165,40.135],[-85.2157,40.0765],[-85.5763,40.0769],[-85.5784,40.3794],[-85.4451,40.3792]]]},\"properties\":{\"name\":\"Delaware\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696a92","contributors":{"authors":[{"text":"Arihood, Leslie D. 0000-0001-5792-3699 larihood@usgs.gov","orcid":"https://orcid.org/0000-0001-5792-3699","contributorId":2357,"corporation":false,"usgs":true,"family":"Arihood","given":"Leslie","email":"larihood@usgs.gov","middleInitial":"D.","affiliations":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":35860,"text":"Ohio-Kentucky-Indiana Water Science Center","active":true,"usgs":true}],"preferred":true,"id":195554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lapham, Wayne W.","contributorId":74734,"corporation":false,"usgs":true,"family":"Lapham","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":195555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38637,"text":"pp1066L - 1982 - Some silicified strophomenacean brachiopods from the Ordovician of Kentucky, with comments on the genus Pionomena","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"pp1066L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1066","chapter":"L","title":"Some silicified strophomenacean brachiopods from the Ordovician of Kentucky, with comments on the genus Pionomena","docAbstract":"Eight species of silicified strophomenid brachiopods from Ordovician rocks of Kentucky are described in this report. Seven species are strophomenaceans, including six from the Middle Ordovician and one, Leptaena kentuckiana n. sp., from the Upper Ordovician. Pionomena recens Neuman from the Middle Ordovician is referred to the Davidsoniacea. Three of these species also occur in the Middle Ordovician of the northern Mississippi Valley region. Rafinesquina is abundant at many localities throughout the Middle Ordovician section of Kentucky. Other silicified strophomenaceans are rare and have been recovered only from the lower part of the Middle Ordovician section of the area. Oepikinia minnesotensis has a high degree of polymorphism of outline shape, profile, and ornament. Some Middle Ordovician species heretofore placed in Strophomena are reassigned to Tetraphalerella. Furcitella and Holtedahlina are differentiated only by the presence of a prominent fold in adult valves of Holtedaklina because a bifid dorsal medial ridge occurs in species of both genera and because the transmuscle ridges of both genera are similar. The possession by Pionomena recens of a perideltidium, dentifers, dorsal medial node, and impunctate shell indicates relationship of this genus to the Davidsoniacea.","language":"ENGLISH","doi":"10.3133/pp1066L","usgsCitation":"Pope, J., 1982, Some silicified strophomenacean brachiopods from the Ordovician of Kentucky, with comments on the genus Pionomena: U.S. Geological Survey Professional Paper 1066, p. L1-L30, https://doi.org/10.3133/pp1066L.","productDescription":"p. L1-L30","costCenters":[],"links":[{"id":124452,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1066l/report-thumb.jpg"},{"id":65468,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1066l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db544d2f","contributors":{"authors":[{"text":"Pope, J.K.","contributorId":41502,"corporation":false,"usgs":true,"family":"Pope","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":220198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10487,"text":"ofr82591 - 1982 - Proceedings of Workshop XVI; The dynamic characteristics of faulting inferred from recordings of strong ground motion","interactions":[],"lastModifiedDate":"2016-05-09T11:01:11","indexId":"ofr82591","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-591","title":"Proceedings of Workshop XVI; The dynamic characteristics of faulting inferred from recordings of strong ground motion","docAbstract":"<p>The strong ground motions radiated by earthquake faulting are controlled by the dynamic characteristics of the faulting process. Although this assertion seems self-evident, seismologists have only recently begun to derive and test quantitative relations between common measures of strong ground motion and the dynamic characteristics of faulting. Interest in this problem has increased dramatically in past several years, however, resulting in a number of important advances. The research presented in this workshop is a significant part of this scientific development. Watching this development occur through the work of many scientists is exciting; to be able to gather a number of these scientists together in one workshop is a remarkable opportunity.</p>","conferenceTitle":"Workshop XVI","conferenceDate":"October 21-23, 1981","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Meno Park, CA","doi":"10.3133/ofr82591","collaboration":"Sponsored by U.S. Nuclear Regulatory Commission","usgsCitation":"1982, Proceedings of Workshop XVI; The dynamic characteristics of faulting inferred from recordings of strong ground motion: U.S. Geological Survey Open-File Report 82-591, 976 p., https://doi.org/10.3133/ofr82591.","productDescription":"976 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":320995,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0591/report-2.pdf","text":"Volume II","linkFileType":{"id":1,"text":"pdf"}},{"id":143914,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0591/report-thumb.jpg"},{"id":320994,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0591/report-1.pdf","text":"Volume I","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660798","contributors":{"compilers":[{"text":"Jacobson, Muriel L.","contributorId":79094,"corporation":false,"usgs":true,"family":"Jacobson","given":"Muriel L.","affiliations":[],"preferred":false,"id":628928,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"editors":[{"text":"Boatwright, John 0000-0002-6931-5241 boat@usgs.gov","orcid":"https://orcid.org/0000-0002-6931-5241","contributorId":1938,"corporation":false,"usgs":true,"family":"Boatwright","given":"John","email":"boat@usgs.gov","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":628927,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":68837,"text":"oc116 - 1982 - Summary chart of geological data from Amoco Tierney Unit 1 well, SW 1/4, SE 1/4, Sec. 15, T 20 N., R. 94 W., Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2019-12-26T07:52:09","indexId":"oc116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"116","title":"Summary chart of geological data from Amoco Tierney Unit 1 well, SW 1/4, SE 1/4, Sec. 15, T 20 N., R. 94 W., Sweetwater County, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/oc116","isbn":"0607824182","usgsCitation":"Markovchick, D., Lanham, R., Bucurel, H., and Law, B.E., 1982, Summary chart of geological data from Amoco Tierney Unit 1 well, SW 1/4, SE 1/4, Sec. 15, T 20 N., R. 94 W., Sweetwater County, Wyoming: U.S. Geological Survey Oil and Gas Investigation Chart 116, HTML, https://doi.org/10.3133/oc116.","productDescription":"HTML","costCenters":[],"links":[{"id":191056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":104774,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5142.htm","linkFileType":{"id":5,"text":"html"},"description":"5142"}],"scale":"764000","country":"United States","state":"Wyoming","county":"Sweetwater 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D.J.","contributorId":12078,"corporation":false,"usgs":true,"family":"Markovchick","given":"D.J.","affiliations":[],"preferred":false,"id":279032,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lanham, R.E.","contributorId":32256,"corporation":false,"usgs":true,"family":"Lanham","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":279034,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bucurel, H.G.","contributorId":104461,"corporation":false,"usgs":true,"family":"Bucurel","given":"H.G.","affiliations":[],"preferred":false,"id":279035,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Law, B. E.","contributorId":17586,"corporation":false,"usgs":true,"family":"Law","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":279033,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":28409,"text":"wri824087 - 1982 - Suspended sediment in selected streams of southeastern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri824087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4087","title":"Suspended sediment in selected streams of southeastern Montana","docAbstract":"The relatively flat Badger Road area near Fairbanks occupies part of the alluvial plain of the Chena and Tanana Rivers and is underlain by scattered areas of permafrost. The water table of the high-transmissivity aquifer that underlies the area is generally shallower than 15 feet, fluctuates seasonally about 2 feet, and slopes northwesterly, the direction of ground-water flow. Private domestic-supply wells obtain water from the upper part of the aquifer. Septic systems used to dispose of waste water are installed at or only slightly above the water table in the same aquifer. Analyses of samples from 16 observation wells in undeveloped parts of the study area and from 33 domestic wells indicated that water quality has not been significantly degraded by on-site waste disposal. Three samples had detectable but minor contamination by fecal coliform bacteria. Anomalous values of chloride and ammonia in one third of the domestic wells may indicate incipient degradation of ground-water quality by septic-tank effluent. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824087","usgsCitation":"Litke, D.W., 1982, Suspended sediment in selected streams of southeastern Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4087, v, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824087.","productDescription":"v, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4087/report-thumb.jpg"},{"id":57213,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fe0","contributors":{"authors":[{"text":"Litke, D. W.","contributorId":94346,"corporation":false,"usgs":true,"family":"Litke","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":10230,"text":"ofr82685 - 1982 - Knik Glacier, Alaska; summary of 1979, 1980, and 1981 data and introduction of new surveying techniques","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr82685","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-685","title":"Knik Glacier, Alaska; summary of 1979, 1980, and 1981 data and introduction of new surveying techniques","docAbstract":"Knik Glacier in south-central Alaska has the potential to reform Lake George, Alaska 's largest glacier-dammed lake. Measurements of surface altitude, snow depth, terminus position, glacier speed, and ice depth are being made in an attempt to determine the mechanisms that could cause a significant re-advance of the glacier. New surveying and data reduction techniques were developed by the authors and employed successfully at Knik Glacier. These include precise geodetic surveying by the ' trisection ' technique, calculation of surface altitude at a specially-fixed ' index point ' from three point measurements on a rough, moving glacier surface, and calculation of ice thickness from low frequency radar measurements. In addition, this report summarizes the data collected from 1979 to 1981 in support of this goal. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82685","usgsCitation":"Mayo, L., and Trabant, D., 1982, Knik Glacier, Alaska; summary of 1979, 1980, and 1981 data and introduction of new surveying techniques: U.S. Geological Survey Open-File Report 82-685, vi, 32 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82685.","productDescription":"vi, 32 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":144323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0685/report-thumb.jpg"},{"id":38099,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0685/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48fe","contributors":{"authors":[{"text":"Mayo, L.R.","contributorId":21541,"corporation":false,"usgs":true,"family":"Mayo","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":161046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trabant, D.C.","contributorId":42209,"corporation":false,"usgs":true,"family":"Trabant","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":161047,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10417,"text":"ofr82143 - 1982 - Spectrographic analyses of subsurface Cambrian insoluble-residue samples from southern Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr82143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-143","title":"Spectrographic analyses of subsurface Cambrian insoluble-residue samples from southern Missouri","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82143","usgsCitation":"Mosier, E.L., Erickson, M.S., and McDanal, S., 1982, Spectrographic analyses of subsurface Cambrian insoluble-residue samples from southern Missouri: U.S. Geological Survey Open-File Report 82-143, 90 p., map ;28 cm., https://doi.org/10.3133/ofr82143.","productDescription":"90 p., map ;28 cm.","costCenters":[],"links":[{"id":145634,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0143/report-thumb.jpg"},{"id":38276,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0143/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e4b","contributors":{"authors":[{"text":"Mosier, E. L.","contributorId":71537,"corporation":false,"usgs":true,"family":"Mosier","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161353,"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":161352,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":161354,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7499,"text":"ofr82199 - 1982 - Sedimentology and stratigraphy of the Kanayut Conglomerate, central Brooks Range, Alaska: Report of 1980 field season","interactions":[],"lastModifiedDate":"2022-12-14T20:44:40.489153","indexId":"ofr82199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-199","title":"Sedimentology and stratigraphy of the Kanayut Conglomerate, central Brooks Range, Alaska: Report of 1980 field season","docAbstract":"The Upper Devonian Kanayut Conglomerate crops out along the crest of the Brooks Range of northern Alaska for a distance of almost 1000 km. It ranges in thickness from 2600 m in the Atigun River area to 700 m south of Anaktuvuk Pass and has been subdivided into four regionally persistent members: (a) the basal sandstone member, consisting of marine sandstone and shale with some conglomerate; (b) the lower shale member, consisting of nonmarine quartzite, conglomerate and shale; (c) the middle conglomerate member, consisting of nonmarine pebble and cobble conglomerate and quartzite; and (d) the Stuver Member, consisting of nonmarine sandstone and shale. The Kanayut conformably overlies the Upper Devonian marine Hunt Fork Shale and is conformably overlain by the Mississippian marine Kayak Shale. The Kanayut is wholly allochthonous and has probably been transported northward on a series of thrust plates. \r\n\r\nThe basal sandstone member of the Kanayut Conglomerate, which overlies prodelta turbidites of the Hunt Fork Shale, contains marginal-marine coarsening-upward channel-mouth bar sequences. It is conformably overlain by the lower shale member. \r\n\r\nMeasured sections of the nonmarine members of the Kanayut show that the lower shale member ranges in thickness from 120 m to 1115 m and consists of fining-upward cycles interpreted to have been deposited by meandering streams on a broad floodplain. These cycles contain, in ascending order, channelized basal conglomerate, trough cross-stratified sandstone, and ripple-marked siltstone. The cycles are interpreted to be channel and point-bar deposits. Individual cycles average about 10 m in thickness and are separated by intervals of black, brown or maroon floodplain shale deposits. These typically contain thin coarsening-upward units that probably represent prograding levee sequences and irregular and ungraded sandstone bodies interpreted to be crevasse-splay deposits. In the Okokmilaga River area, the lower shale member contains a distinctive coarse-grained unit which is burrowed and interpreted to represent a widespread marine incursion. \r\n\r\nThe middle conglomerate member, which ranges in thickness from 155 m to 525 m, consists of braidplain deposits. It contains fining-upward couplets of conglomerate and parallel-stratified or cross-stratified sandstone that average 2-7 m in thickness. The couplets record deposition in channels and on bars of braided streams. The middle conglomerate member contains the largest clasts, little or no shale, and represents the maximum progradation of nonmarine sedimentation in the Kanayut depositional system. \r\n\r\nThe Stuver Member consists of fining-upward cycles that resemble those of the lower shale member. It ranges in thickness from 160 m to 1400 m and grades upward into tidal and marginal-marine deposits of the Kayak Shale. \r\n\r\nConglomerate in the Kanayut is compositionally very mature, averaging 82 percent white, gray, black or red chert clasts, 14 percent vein quartz clasts, 3 percent quartzite clasts, and less than I percent other lithologies, mainly argillite. Although red chert is locally abundant in the Shainin Lake-Galbraith Lake area, there is little variation in conglomerate composition in the Kanayut, suggesting derivation from a single major source terrane.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82199","usgsCitation":"Nilsen, T.H., Moore, T., Balin, D.F., and Johnson, S.Y., 1982, Sedimentology and stratigraphy of the Kanayut Conglomerate, central Brooks Range, Alaska: Report of 1980 field season: U.S. Geological Survey Open-File Report 82-199, iv, 81 p., https://doi.org/10.3133/ofr82199.","productDescription":"iv, 81 p.","costCenters":[],"links":[{"id":410493,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75624.htm","linkFileType":{"id":5,"text":"html"}},{"id":34953,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0199/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0199/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"central Brooks Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -154.4667,\n              67.8333\n            ],\n            [\n              -148.5,\n              67.8333\n            ],\n            [\n              -148.5,\n              68.45\n            ],\n            [\n              -154.4667,\n              68.45\n            ],\n            [\n              -154.4667,\n              67.8333\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3c15","contributors":{"authors":[{"text":"Nilsen, T. H.","contributorId":93057,"corporation":false,"usgs":true,"family":"Nilsen","given":"T.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":155903,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Thomas E. 0000-0002-0878-0457","orcid":"https://orcid.org/0000-0002-0878-0457","contributorId":85592,"corporation":false,"usgs":true,"family":"Moore","given":"Thomas E.","affiliations":[],"preferred":false,"id":155902,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Balin, D. F.","contributorId":76988,"corporation":false,"usgs":true,"family":"Balin","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":155901,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, S. Y.","contributorId":48572,"corporation":false,"usgs":true,"family":"Johnson","given":"S.","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":155900,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":10419,"text":"ofr82587 - 1982 - The determination of total volatiles in rocks by loss-on-fusion","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr82587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-587","title":"The determination of total volatiles in rocks by loss-on-fusion","docAbstract":"A fast and accurate technique has been developed for the determination of the total volatile content of rocks. The loss on fusion (LOF) results are comparable to the conventional time-consuming wet-chemical procedure but require no additional effort or cost when conducted as part of the usual sample preparation procedure for quantitative X-ray fluorescence spectrometric analysis (XRF). The technique utilizes the weight loss of the rock when fused with a suitable blend of lithium tetraborate and lithium nitrate. A simple mass balance model is used to represent the thermogravimetric results and to identify the nature of the high temperature mass alteration reactions taking place in the fusion melt. Under the sample preparation conditions used in this study, sulfide appears to be retained quantitatively in the fusion disc sulfate, a phenomenon permitting the determination of sulfide in prepared by a conventional fusion procedure in the form of \r\nrock samples.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82587","usgsCitation":"Mossotti, V., and King, B., 1982, The determination of total volatiles in rocks by loss-on-fusion: U.S. Geological Survey Open-File Report 82-587, 23 p., ill. ;28 cm., https://doi.org/10.3133/ofr82587.","productDescription":"23 p., ill. ;28 cm.","costCenters":[],"links":[{"id":145652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0587/report-thumb.jpg"},{"id":38278,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0587/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6687ee","contributors":{"authors":[{"text":"Mossotti, V.G.","contributorId":43785,"corporation":false,"usgs":true,"family":"Mossotti","given":"V.G.","affiliations":[],"preferred":false,"id":161358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, B.","contributorId":78750,"corporation":false,"usgs":true,"family":"King","given":"B.","affiliations":[],"preferred":false,"id":161359,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28474,"text":"wri824072 - 1982 - A data-management system for areal interpretive data for the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri824072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4072","title":"A data-management system for areal interpretive data for the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","docAbstract":"The High Plains Regional Aquifer System Analysis has developed a regional water-resources (and related) data storage and retrieval system to organize and preserve areal interpretative data. The system is general and can easily be adapted for other studies. This report documents the High Plains data base as well as the general system that is independent of the High Plains area. The system is built around a hierarchically structured data base consisting of related latitude-longitude blocks. Various parameters in the data base are stored at different degrees of detail, with the finest detail being a block of 1 minute of latitude by 1 minute longitude (approximately 1 square mile). (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824072","usgsCitation":"Luckey, R.R., and Ferrigno, C., 1982, A data-management system for areal interpretive data for the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming: U.S. Geological Survey Water-Resources Investigations Report 82-4072, vii, 112 p. :ill. ;28 cm., https://doi.org/10.3133/wri824072.","productDescription":"vii, 112 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":118797,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4072/report-thumb.jpg"},{"id":57274,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af2a1","contributors":{"authors":[{"text":"Luckey, R. R.","contributorId":93055,"corporation":false,"usgs":true,"family":"Luckey","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":199867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferrigno, C.F.","contributorId":27092,"corporation":false,"usgs":true,"family":"Ferrigno","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":199866,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10506,"text":"ofr821016 - 1982 - Vertical movement of ground water under the Merrill Field landfill, Anchorage, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr821016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1016","title":"Vertical movement of ground water under the Merrill Field landfill, Anchorage, Alaska","docAbstract":"Shallow groundwater under the Merrill Field sanitary landfill at Anchorage is polluted by leachate. Wells, including three Municipal-supply wells, obtain water from two confined aquifers 100-300 feet beneath the landfill area. Aquifer-test data and information on subsurface geology, ground-water levels, and properties of materials were used to estimate vertical gradients and vertical permeabilities under the landfill. The authors ' best estimates ' of vertical permeabilities of two confining units are 1 x 10 super -2 foot per day and 2 x 10 super -4 foot per day. Theoretical travel-time calculations indicate that minor amounts of pollutants may reach the upper confined aquifer after many tens of years, but that water of the composition of the leachate probably would not reach the aquifer for more than three centuries. The range of error in the theoretical travel-time calculations is likely to be plus or minus a factor of two or three. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821016","usgsCitation":"Nelson, G.L., and Dearborn, L., 1982, Vertical movement of ground water under the Merrill Field landfill, Anchorage, Alaska: U.S. Geological Survey Open-File Report 82-1016, iv, 28 p. ill. ;28 cm., https://doi.org/10.3133/ofr821016.","productDescription":"iv, 28 p. ill. ;28 cm.","costCenters":[],"links":[{"id":144659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1016/report-thumb.jpg"},{"id":38360,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1016/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db6020ca","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161515,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dearborn, L.L.","contributorId":53376,"corporation":false,"usgs":true,"family":"Dearborn","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":161514,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10340,"text":"ofr82744 - 1982 - Documentation and user's guide for interactive spectral analysis and filter program package useful in the processing of seismic reflection data","interactions":[],"lastModifiedDate":"2012-02-02T00:06:23","indexId":"ofr82744","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-744","title":"Documentation and user's guide for interactive spectral analysis and filter program package useful in the processing of seismic reflection data","docAbstract":"The spectral analysis and filter program package is written in the BASIC language for the HP-9845T desktop computer. The program's main purpose is to perform spectral analyses on digitized time-domain data. In addition, band-pass filtering of the data can be performed in the time domain. Various other processes such as autocorrelation can be performed to the time domain data in order to precondition them for spectral analyses. The frequency domain data can also be transformed back into the time domain if desired. Any data can be displayed on the CRT in graphic form using a variety of plot routines. A hard copy can be obtained immediately using the internal thermal printer. Data can also be displayed in tabular form on the CRT or internal thermal printer or it can be stored permanently on a mass storage device like a tape or disk. A list of the processes performed in the order in which they occurred can be displayed at any time.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82744","usgsCitation":"Miller, J.J., 1982, Documentation and user's guide for interactive spectral analysis and filter program package useful in the processing of seismic reflection data: U.S. Geological Survey Open-File Report 82-744, 55 p., ill. ;28 cm., https://doi.org/10.3133/ofr82744.","productDescription":"55 p., ill. ;28 cm.","costCenters":[],"links":[{"id":143662,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0744/report-thumb.jpg"},{"id":38191,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0744/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d7a6","contributors":{"authors":[{"text":"Miller, J. J.","contributorId":54588,"corporation":false,"usgs":true,"family":"Miller","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":161220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26597,"text":"wri824123 - 1982 - Flood of June 15, 1981, in Great Bend and vicinity, central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:22","indexId":"wri824123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4123","title":"Flood of June 15, 1981, in Great Bend and vicinity, central Kansas","docAbstract":"Torrential precipitation, as much as 20 inches in 12 hours, resulted in unprecedented flooding on Dry Walnut Creek in southwestern Barton County, central Kansas. Runoff from the storm caused extensive flooding in the town of Great Bend on June 15, 1981. Estimates of total damages exceeded $42 million. Measurements of peak discharges made in the downstream part of the Dry Walnut Creek watershed were as much as 3 1/2 times the estimated magnitude of the 100-year flood and in some locations exceeded the maximum previously measured discharge for the area. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824123","usgsCitation":"Clement, R., and Johnson, D., 1982, Flood of June 15, 1981, in Great Bend and vicinity, central Kansas: U.S. Geological Survey Water-Resources Investigations Report 82-4123, iv, 12 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824123.","productDescription":"iv, 12 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":122706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4123/report-thumb.jpg"},{"id":55463,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eed55","contributors":{"authors":[{"text":"Clement, R.W.","contributorId":11247,"corporation":false,"usgs":true,"family":"Clement","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":196682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, D.G.","contributorId":40245,"corporation":false,"usgs":true,"family":"Johnson","given":"D.G.","email":"","affiliations":[],"preferred":false,"id":196683,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10339,"text":"ofr82774 - 1982 - Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota","interactions":[{"subject":{"id":10339,"text":"ofr82774 - 1982 - Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota","indexId":"ofr82774","publicationYear":"1982","noYear":false,"title":"Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":2314,"text":"wsp2243 - 1984 - Changes in flood response of the Red River of the North basin, North Dakota-Minnesota","indexId":"wsp2243","publicationYear":"1984","noYear":false,"title":"Changes in flood response of the Red River of the North basin, North Dakota-Minnesota"},"id":1}],"supersededBy":{"id":2314,"text":"wsp2243 - 1984 - Changes in flood response of the Red River of the North basin, North Dakota-Minnesota","indexId":"wsp2243","publicationYear":"1984","noYear":false,"title":"Changes in flood response of the Red River of the North basin, North Dakota-Minnesota"},"lastModifiedDate":"2018-03-09T13:58:25","indexId":"ofr82774","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-774","title":"Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota","docAbstract":"<p>The magnitude and frequency of large floods that have occurred in recent years in the basin of the Red River of the North have caused concern that land-use changes and manmade drainage have increased flooding. This study was undertaken to determine if any changes in flood response of the Red River basin can be documented. A review of the hydrologic setting, previous floods, flood-control measures, and probable effects of land-use changes shows that the flooding problem of the Red River basin is complex hydrologically, highly variable historically, and follows a regional pattern. Therefore, a change in flood response of the basin is difficult to identify. The flood-frequency, regression, normalized-hydrograph, and double-mass analyses show little indication of significant change in flood response of the Red River basin at locations on the main stem. However, the large variation in flood discharges may mask or dwarf small changes in response of the basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82774","usgsCitation":"Miller, J.E., and Frink, D.L., 1982, Changes in flood response of the Red River of the North Basin, North Dakota-Minnesota: U.S. Geological Survey Open-File Report 82-774, viii, 166 p., https://doi.org/10.3133/ofr82774.","productDescription":"viii, 166 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":94967,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0774/report.pdf","size":"8340","linkFileType":{"id":1,"text":"pdf"}},{"id":143661,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0774/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6cdb","contributors":{"authors":[{"text":"Miller, Jeffrey E.","contributorId":76717,"corporation":false,"usgs":true,"family":"Miller","given":"Jeffrey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frink, Dale L.","contributorId":59421,"corporation":false,"usgs":true,"family":"Frink","given":"Dale","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161218,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":10509,"text":"ofr82627 - 1982 - Streamflow and sediment transport in the Quillayute River basin, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:06:40","indexId":"ofr82627","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-627","title":"Streamflow and sediment transport in the Quillayute River basin, Washington","docAbstract":"From October 1976 to September 1978 the U.S. Geological Survey made a reconnaissance evaluation of the fluvial-sediment transport and documented the natural streamflow characteristics in the Quillayute River basin in northwestern Washington. Most of the flow originates from the tributaries, the Soleduck, Bogachiel, and Calawah Rivers. Flow in the summer months from the Calawah River is about half that from either the Bogachiel or Soleduck Rivers. In the winter months flow from the Soleduck River is about 1 1/2 times that of the Bogachiel or Calawah Rivers. In general, the highest monthly flows during the winter are about 10 times greater than the lowest monthly flows during the summer except for the Dickey River where winter flows are about 20 times greater. Annual mean discharges may vary greatly from year to year, ranging from about 1/2 to 1 1/2 times the mean annual discharge. For the study period, the observed suspended-sediment concentration ranged from less than 1 to 2 ,150 milligrams per liter. The estimated mean annual suspended-sediment discharges were: Bogachiel River--400,000 tons (includes Calawah River); Calawah River--120,000 tons; Soleduck River--120,000 tons; Dickey River--75,000 tons; and other tributaries--10,000 tons, for a total of 606,000 tons transported annually by the Quillayute River. The estimated annual bedload of 21,000 tons was transported into the Quillayute River by the Soleduck, Bogachiel, and Dickey Rivers. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82627","usgsCitation":"Nelson, L.M., 1982, Streamflow and sediment transport in the Quillayute River basin, Washington: U.S. Geological Survey Open-File Report 82-627, iv, 33 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82627.","productDescription":"iv, 33 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":145541,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0627/report-thumb.jpg"},{"id":38361,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0627/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a268","contributors":{"authors":[{"text":"Nelson, L. M.","contributorId":39773,"corporation":false,"usgs":true,"family":"Nelson","given":"L.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":161518,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47667,"text":"wri824042 - 1982 - Map showing total thickness of the Fox Hills-Lower Hell Creek aquifer, Montana","interactions":[],"lastModifiedDate":"2023-01-04T19:24:20.544416","indexId":"wri824042","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4042","title":"Map showing total thickness of the Fox Hills-Lower Hell Creek aquifer, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824042","usgsCitation":"Feltis, R.D., 1982, Map showing total thickness of the Fox Hills-Lower Hell Creek aquifer, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4042, 1 Plate: 34.92 x 22.23 inches, https://doi.org/10.3133/wri824042.","productDescription":"1 Plate: 34.92 x 22.23 inches","costCenters":[],"links":[{"id":161696,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411357,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35566.htm","linkFileType":{"id":5,"text":"html"}},{"id":84579,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Fox Hills-Lower Hell Creek aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.054,\n              49\n            ],\n            [\n              -110,\n              49\n            ],\n            [\n              -110,\n              45\n            ],\n            [\n              -104.054,\n              45\n            ],\n            [\n              -104.054,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b11e4b07f02db6a2498","contributors":{"authors":[{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":235978,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38638,"text":"pp1066M - 1982 - The brachiopod genera Hebertella, Dalmanella, and Heterorthina from the Ordovician of Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:10:35","indexId":"pp1066M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1066","chapter":"M","title":"The brachiopod genera Hebertella, Dalmanella, and Heterorthina from the Ordovician of Kentucky","docAbstract":"The orthid brachiopod genera Hebertella, Dalmanella, and Heterorthina are abundant in Middle and Upper Ordovician strata in Kentucky. 'Nine species are described: Hebertella frankfortensis Foerste; H. parksensis Foerste; H. occidentalis (Hall); Dalmanella bassleri Foerste; D. fertilis (Ulrich); D. meeki (Miller); D. multisecta (Meek); D. sulcata Cooper; and Heterorthina macfarlani Neuman. The species designations Hebertella sinuata (Hall), H. subjugata (Hall), and H. latasulcata Foerste are placed in synonymy with H. occidentalis (Hall). The stratigraphic distribution of each species is given. Large collections of silicified specimens allowed the recognition of the considerable variability characteristic of most of the species. External morphology distinguishes species of Hebertella, whereas internal features are critical to recognition of species of Dalmanella and Heterorthina.","language":"ENGLISH","doi":"10.3133/pp1066M","usgsCitation":"Walker, L., 1982, The brachiopod genera Hebertella, Dalmanella, and Heterorthina from the Ordovician of Kentucky: U.S. Geological Survey Professional Paper 1066, 17 p.; 5 plates, https://doi.org/10.3133/pp1066M.","productDescription":"17 p.; 5 plates","costCenters":[],"links":[{"id":126742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1066m/report-thumb.jpg"},{"id":65469,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1066m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669585","contributors":{"authors":[{"text":"Walker, L.G.","contributorId":28652,"corporation":false,"usgs":true,"family":"Walker","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":220199,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38648,"text":"pp813T - 1982 - Summary appraisals of the nation's ground-water resources – New England region","interactions":[],"lastModifiedDate":"2021-12-14T21:58:30.42222","indexId":"pp813T","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"T","title":"Summary appraisals of the nation's ground-water resources – New England region","docAbstract":"<p>The New England Region has a total area of about 62,400 square miles (160,000 km<sup>2</sup>) and includes the States of Maine and New Hampshire, eastern Vermont, most of Massachusetts and Connecticut, all of Rhode Island, and a small part of southeastern New York. The longest stream is the Connecticut River, which extends from northern Vermont and New Hampshire, through western Massachusetts and central Connecticut, and drains into Long Island Sound. Other major streams are the Penobscot and Kennebec Rivers in Maine, the Androscoggin in Maine and New Hampshire, the Merrimack in New Hampshire and Massachusetts, and the Housatonic in western Massachusetts and Connecticut. Of the smaller streams, some, like the Charles River in the Boston area, are widely known because of their proximity to large population centers.</p>\n<p>Ground water occurs in two types of geologic materials: consolidated rocks and unconsolidated sedimentary rocks. The consolidated rocks underlie the entire region. They include crystalline igneous and metamorphic rocks and consolidated sedimentary rocks-shale, sandstone, and limestone and other carbonate rocks. The most productive unconsolidated rocks are sand and gravel of glacial origin. These deposits occur all over Cape Cod and nearby islands in southeastern Massachusetts and in many valleys throughout the region.</p>\n<p>Ground water is derived from precipitation. It can be intercepted for use by pumping from wells (1) before it discharges to the streams as base flow and (2) before it drains directly into coastal wetlands, bays, Long Island Sound, or the ocean.</p>\n<p>Withdrawals of fresh ground water in 1975 aggregated about 220 billion gallons (830 hm<sup>3</sup>), or about 12 percent of the total freshwater withdrawals (from all sources) of 1,800 billion gallons (6,800 hm<sup>3</sup>). In view of the available ground-water reserves, considerable additional water, for the anticipated continuing increase in population and economic activity, could be developed.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813T","usgsCitation":"Sinnott, A., 1982, Summary appraisals of the nation's ground-water resources – New England region: U.S. Geological Survey Professional Paper 813, vi, 23 p., https://doi.org/10.3133/pp813T.","productDescription":"vi, 23 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":392898,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5074.htm"},{"id":65480,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813t/report.pdf","text":"Report","size":"6.64 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,{"id":47654,"text":"wri824029 - 1982 - Map showing altitude of the top of the Swift Formation, Montana","interactions":[],"lastModifiedDate":"2023-01-17T21:48:43.171744","indexId":"wri824029","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4029","title":"Map showing altitude of the top of the Swift Formation, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824029","usgsCitation":"Feltis, R.D., 1982, Map showing altitude of the top of the Swift Formation, Montana: U.S. Geological Survey Water-Resources Investigations Report 82-4029, 1 Plate: 35.40 x 22.46 inches, https://doi.org/10.3133/wri824029.","productDescription":"1 Plate: 35.40 x 22.46 inches","costCenters":[],"links":[{"id":169626,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411999,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35554.htm","linkFileType":{"id":5,"text":"html"}},{"id":84566,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1982/4029/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana, Wyoming","county":"Swift Formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.054,\n              49\n            ],\n            [\n              -113,\n              49\n            ],\n            [\n              -113,\n              45\n            ],\n            [\n              -104.054,\n              45\n            ],\n            [\n              -104.054,\n              49\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658ecc","contributors":{"authors":[{"text":"Feltis, Richard D.","contributorId":98773,"corporation":false,"usgs":true,"family":"Feltis","given":"Richard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":235965,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10385,"text":"ofr82409 - 1982 - Three-dimensional modeling of the Nevada Test Site and vicinity from teleseismic P-wave residuals","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr82409","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-409","title":"Three-dimensional modeling of the Nevada Test Site and vicinity from teleseismic P-wave residuals","docAbstract":"A teleseismic P-wave travel-time residual study is described which reveals the regional compressional-velocity structure of southern Nevada and neighboring parts of California to a depth of 280 km. During 1980, 98 teleseismic events were recorded at as many as 53 sites in this area. P-wave residuals were calculated relative to a network-wide average residual for each event and are displayed on maps of the stations for each of four event-azimuth quadrants. Fluctuations in these map-patterns of residuals with approach azimuth combined with results of linear, three-dimensional inversions of some 2887 residuals indicate the following characteristics of the velocity structure of the southern Nevada region: 1) a low-velocity body exists in the upper crust 50 km northeast of Beatty, Nevada, near the Miocene Timber Mountain-Silent Canyon caldera complex. Another highly-localized low-velocity anomaly occurs near the southwest corner of the Nevada Test Site (NTS). These two anomalies seem to be part of a low-velocity trough extending from Death Valley, California, to about 50 km north of NTS. 2) There is a high-velocity body in the mantle between 81 and 131 km deep centered about i0 km north of the edge of the Timber Mountain caldera, 3) a broad low-velocity body is delineated between 81 and 131 km deep centered about 30 km north of Las Vegas, 4) there is a monotonic increase in travel-time delays from west to east across the region, probably indicating an eastward decrease in velocity, and lower than average velocities in southeastern Nevada below 31 km, and 5) considerable complexity in three-dimensional velocity structure exists in this part of the southern Great Basin. \r\n\r\nInversions of teleseismic P-wave travel-time residuals were also performed on data from 12 seismometers in the immediate vicinity of the Nevada Test Site to make good use of the closer station spacing i in that area. Results of these inversions show more details of the velocity structure but generally the same features as those found in the regional study.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82409","usgsCitation":"Monfort, M.E., and Evans, J.R., 1982, Three-dimensional modeling of the Nevada Test Site and vicinity from teleseismic P-wave residuals: U.S. Geological Survey Open-File Report 82-409, 70 p. :ill. ;28 cm., https://doi.org/10.3133/ofr82409.","productDescription":"70 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":142336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0409/report-thumb.jpg"},{"id":38215,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0409/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b857","contributors":{"authors":[{"text":"Monfort, Mary E.","contributorId":93491,"corporation":false,"usgs":true,"family":"Monfort","given":"Mary","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161296,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evans, John R. jrevans@usgs.gov","contributorId":529,"corporation":false,"usgs":true,"family":"Evans","given":"John","email":"jrevans@usgs.gov","middleInitial":"R.","affiliations":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true}],"preferred":true,"id":161295,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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