{"pageNumber":"2111","pageRowStart":"52750","pageSize":"25","recordCount":68919,"records":[{"id":5210292,"text":"5210292 - 1982 - Bedrock geologic control of sensitivity of aquatic ecosystems in the United States to acidic deposition","interactions":[],"lastModifiedDate":"2012-02-02T00:15:15","indexId":"5210292","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1982","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Bedrock geologic control of sensitivity of aquatic ecosystems in the United States to acidic deposition","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Distribution of Surface Waters Sensitive to Acidic Precipitation: A State-Level Atlas ","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"University of Maine","publisherLocation":"Orono","usgsCitation":"Norton, S.A., Akielaszek, J., Haines, T., Stromborg, K., and Longcore, J.R., 1982, Bedrock geologic control of sensitivity of aquatic ecosystems in the United States to acidic deposition, chap. of Distribution of Surface Waters Sensitive to Acidic Precipitation: A State-Level Atlas .","productDescription":"[66 leaves]","startPage":"Unnumbered","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63da26","contributors":{"authors":[{"text":"Norton, S. A.","contributorId":32223,"corporation":false,"usgs":true,"family":"Norton","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":328147,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Akielaszek, J.J.","contributorId":24731,"corporation":false,"usgs":true,"family":"Akielaszek","given":"J.J.","affiliations":[],"preferred":false,"id":328146,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Haines, T.A.","contributorId":83062,"corporation":false,"usgs":true,"family":"Haines","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":328150,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stromborg, K. L.","contributorId":34466,"corporation":false,"usgs":true,"family":"Stromborg","given":"K. L.","affiliations":[],"preferred":false,"id":328148,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Longcore, J. R. 0000-0003-4898-5438","orcid":"https://orcid.org/0000-0003-4898-5438","contributorId":43835,"corporation":false,"usgs":true,"family":"Longcore","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":328149,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":5200056,"text":"5200056 - 1982 - An atlas and census of Texas waterbird colonies, 1973-1980","interactions":[],"lastModifiedDate":"2012-02-02T00:15:21","indexId":"5200056","displayToPublicDate":"2009-06-08T16:49:39","publicationYear":"1982","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"An atlas and census of Texas waterbird colonies, 1973-1980","language":"English","publisher":"Texas Colonial Waterbird Society. Caesar Kleberg Wildlife Research Institute, Texas A&I University","publisherLocation":"Kingsville, Texas","usgsCitation":"Mullins, L., Slack, R., Chaney, A., Telfair, R., Paul, R., Blankinship, D., Blacklock, G.W., King, K.A., Kennedy, S., and Smith, J., 1982, An atlas and census of Texas waterbird colonies, 1973-1980, x, 358.","productDescription":"x, 358","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200986,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684c96","contributors":{"authors":[{"text":"Mullins, L.M.","contributorId":24469,"corporation":false,"usgs":true,"family":"Mullins","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":326902,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slack, R.D.","contributorId":101769,"corporation":false,"usgs":true,"family":"Slack","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":326910,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chaney, A.H.","contributorId":34233,"corporation":false,"usgs":true,"family":"Chaney","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":326903,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Telfair, R.C.","contributorId":85299,"corporation":false,"usgs":true,"family":"Telfair","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":326908,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Paul, R.T.","contributorId":50250,"corporation":false,"usgs":true,"family":"Paul","given":"R.T.","email":"","affiliations":[],"preferred":false,"id":326905,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Blankinship, D.R.","contributorId":82010,"corporation":false,"usgs":true,"family":"Blankinship","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":326907,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Blacklock, Gene W.","contributorId":98849,"corporation":false,"usgs":true,"family":"Blacklock","given":"Gene","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":326909,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"King, Kirk A.","contributorId":9203,"corporation":false,"usgs":true,"family":"King","given":"Kirk","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":326901,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Kennedy, S.","contributorId":39908,"corporation":false,"usgs":true,"family":"Kennedy","given":"S.","affiliations":[],"preferred":false,"id":326904,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Smith, J.C.","contributorId":53498,"corporation":false,"usgs":true,"family":"Smith","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":326906,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":80037,"text":"ofr811103 - 1982 - Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States","interactions":[],"lastModifiedDate":"2012-02-10T00:11:39","indexId":"ofr811103","displayToPublicDate":"2007-06-20T00:00:00","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":"81-1103","title":"Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States","docAbstract":"INTRODUCTION\r\n\r\nThe tertiary limestone aquifer system of the southeastern United States is a sequence of carbonate rocks referred to as the Floridan aquifer in Florida and the principal artesian aquifer in Georgia, Alabama, and South Carolina. More than 3 billion gallons of water are pumped daily from the limestone aquifer; and the system is the principal source of municipal, industrial, and agricultural water supply in south Georgia and most of Florida.\r\n\r\nThe aquifer system includes units of Paleocene to early Miocene age that combine to form a continuous carbonate sequence that is hydraulically connected in varying degrees. In a small area near Brunswick, Ga., a thin sequence of rocks of Late Cretaceous age is part of the system. In and directly downdip from much of the outcrop area, the system consists of one continuous permeable unit. Further downdip the aquifer system generally consists of two major permeable zones separated by a less-permeable unit of highly variable hydraulic properties (very leaky to virtually nonleaky). Conditions for the system vary from unconfined to confined depending upon whether the argillaceous Miocene and younger rocks that form the upper confining unit have been removed by erosion.\r\n\r\nThis report is one of a series of preliminary products depicting the hydrogeologic framework, water chemistry, and hydrology of the aquifer system. The map shows the distribution of chloride ions in water from the upper permeable zone of the limestone aquifer system. The upper permeable zone consists of several formations, primarily the Tampa, Suwannee, Ocala, and Avon Park Limestones (Miller 1981a, b).\r\n\r\nChloride concentrations of water within the upper permeable zone vary from nearly zero in recharge areas to many thousands of milligrams per liter (mg/L) in coastal discharge areas. Where the aquifer system discharges into the sea, the upper permeable zone contains increasing amounts of seawater. In these areas, wells that fully penetrate the upper permeable zone will yield water with chloride concentrations that approach that of seawater, about 19500 mg/L.","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/ofr811103","usgsCitation":"Sprinkle, C.L., 1982, Chloride Concentration in Water from the Upper Permeable Zone of the Tertiary Limestone Aquifer System, Southeastern United States (WRI/OFR 81-1103): U.S. Geological Survey Open-File Report 81-1103, Map: 35 x 44 inches, https://doi.org/10.3133/ofr811103.","productDescription":"Map: 35 x 44 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":192151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1103/report-thumb.jpg"},{"id":91219,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1103/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,24 ], [ -89,34 ], [ -80,34 ], [ -80,24 ], [ -89,24 ] ] ] } } ] }","edition":"WRI/OFR 81-1103","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e253c","contributors":{"authors":[{"text":"Sprinkle, Craig L.","contributorId":41802,"corporation":false,"usgs":true,"family":"Sprinkle","given":"Craig","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":291538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011707,"text":"70011707 - 1982 - A climate-related oxidizing event in deep-sea sediment from the Bering Sea","interactions":[],"lastModifiedDate":"2025-07-11T13:17:14.795318","indexId":"70011707","displayToPublicDate":"2004-11-19T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3218,"text":"Quaternary Research","active":true,"publicationSubtype":{"id":10}},"title":"A climate-related oxidizing event in deep-sea sediment from the Bering Sea","docAbstract":"

Many cores from the deep basins of the Bering Sea have a thin oxidized zone within otherwise reduced sediment. This oxidized zone began to form about 6000 yr ago and represents an interval of about 3200 yr. Mineralogically, the oxidized and reduced sediments are similar, but chemically they differ. Concentrations of Fe and C are lower, and concentrations of Mn, Ba, Co, Mo, and Ni are higher in the oxidized than in the reduced sediment. Mn is enriched about 10-fold in the oxidized zone relative to its concentration in the reduced sediment, Mo about threefold, and Ba, Co, and Ni about twofold. These data suggest that the oxidized zone developed diagenetically as the result of the balance between the flux of organic matter and the available dissolved oxygen in bottom and interstitial waters.

We propose that the Bering Sea was substantially ice covered when global glacial conditions prevailed. during the transition to global interglacial conditions, seasonal meltwater from thawing sea ice formed a lens of fresh water that decreased organic productivity. During the winter seasons, however, sea ice reformed and caused downwelling of dense, oxygen-rich waters to recharge bottom waters. The combination of lower organic productivity and more oxygen-rich bottom water allowed oxidized sediment to accumulate. Once full interglacial conditions were established, the volume of sea ice produced was insufficient to affect either productivity or the supply of dissolved oxygen and so bottom conditions again became reducing.

Similar events probably occurred during the onset of global glacial conditions, and similar oxidized layers probably formed at these times. Such oxidized zones are highly unstable, however, in a reducing environment and, once buried beyond the influence of bacterial and infaunal activities, are depleted of their available oxygen and converted to reduced sediment.

","language":"English","publisher":"Elsevier","doi":"10.1016/0033-5894(82)90023-0","issn":"00335894","usgsCitation":"Gardner, J., Dean, W., Klise, D., and Baldauf, J., 1982, A climate-related oxidizing event in deep-sea sediment from the Bering Sea: Quaternary Research, v. 18, no. 1, p. 91-107, https://doi.org/10.1016/0033-5894(82)90023-0.","productDescription":"17 p.","startPage":"91","endPage":"107","costCenters":[],"links":[{"id":221383,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bering Sea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -179.43447622186315,\n 66.03716814295933\n ],\n [\n -179.9,\n 52.18346144027916\n ],\n [\n -157.448243609558,\n 52.18346144027916\n ],\n [\n -165.90706351388224,\n 61.801670477796904\n ],\n [\n -161.33262095123737,\n 64.27396844279207\n ],\n [\n -165.98991273192667,\n 64.46043441454259\n ],\n [\n -169.5221977836011,\n 66.0415498224066\n ],\n [\n -173.0349006985722,\n 64.09395801361447\n ],\n [\n -179.43447622186315,\n 66.03716814295933\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 179.83934565752284,\n 64.81744080068066\n ],\n [\n 178.00118962320346,\n 64.61627483409542\n ],\n [\n 179.38507782495674,\n 62.24228337394402\n ],\n [\n 163.59594051029097,\n 59.269627569503484\n ],\n [\n 165,\n 52.519259996483186\n ],\n [\n 179.9,\n 52.519259996483186\n ],\n [\n 179.83934565752284,\n 64.81744080068066\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"18","issue":"1","noUsgsAuthors":false,"publicationDate":"2017-01-20","publicationStatus":"PW","scienceBaseUri":"5059e344e4b0c8380cd45f0d","contributors":{"authors":[{"text":"Gardner, J.V.","contributorId":76705,"corporation":false,"usgs":true,"family":"Gardner","given":"J.V.","affiliations":[],"preferred":false,"id":361775,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dean, W.E.","contributorId":97099,"corporation":false,"usgs":true,"family":"Dean","given":"W.E.","email":"","affiliations":[],"preferred":false,"id":361776,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Klise, D.H.","contributorId":97105,"corporation":false,"usgs":true,"family":"Klise","given":"D.H.","affiliations":[],"preferred":false,"id":361777,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baldauf, J.G.","contributorId":67655,"corporation":false,"usgs":true,"family":"Baldauf","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":361774,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":40864,"text":"ofr82259 - 1982 - Potentiometric surface of the Floridan Aquifer in central Sumter County, Florida, September 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:10:51","indexId":"ofr82259","displayToPublicDate":"1998-02-01T00:00:00","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":"82-259","title":"Potentiometric surface of the Floridan Aquifer in central Sumter County, Florida, September 1981","docAbstract":"This map presents the potentiometric surface of the Floridan aquifer in central Sumter County, Florida, for September 1981. The Floridan aquifer is the principal source of potable water in the area. The focus of the map is the potentiometric surface in the Jumper Creek Canal area for the high water-level period. Water-level measurements were made on approximately 60 wells. The potentiometric surface ranged in altitude from more than 85 feet in the southeast part of the county to less than 35 feet northwest of Lake Panasoffkee in the west-central area. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82259","usgsCitation":"Bradner, L.A., 1982, Potentiometric surface of the Floridan Aquifer in central Sumter County, Florida, September 1981: U.S. Geological Survey Open-File Report 82-259, 1 map :photocopy ;73 x 51 cm., https://doi.org/10.3133/ofr82259.","productDescription":"1 map :photocopy ;73 x 51 cm.","costCenters":[],"links":[{"id":171530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78741,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0259/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682ff7","contributors":{"authors":[{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":224068,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37151,"text":"rp149 - 1982 - Mitigation and enhancement techniques for the Upper Mississippi River system and other large river systems","interactions":[],"lastModifiedDate":"2016-11-16T13:28:07","indexId":"rp149","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":79,"text":"Resource Publication","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"149","title":"Mitigation and enhancement techniques for the Upper Mississippi River system and other large river systems","docAbstract":"

Extensive information is provided on techniques that can reduce or eliminate the negative impact of man's activities (particularly those related to navigation) on large river systems, with special reference to the Upper Mississippi River. These techniques should help resource managers who are concerned with such river systems to establish sound environmental programs.

\n
\n

Discussion of each technique or group of techniques include (1) situation to be mitigated or enhanced; (2) description of technique; (3) impacts on the environment; (4) costs; and (5) evaluation for use on the Upper Mississippi River Systems. The techniques are divided into four primary categories: Bank Stabilization Techniques, Dredging and Disposal of Dredged Material, Fishery Management Techniques, and Wildlife Management Techniques. Because techniques have been grouped by function, rather than by structure, some structures are discussed in several contexts. For example, gabions are discussed for use in revetments, river training structures, and breakwaters.

\n
\n

The measures covered under Bank Stabilization Techniques include the use of riprap revetments, other revetments, bulkheads, river training structures, breakwater structures, chemical soil stabilizers, erosion-control mattings, and filter fabrics; the planting of vegetation; the creation of islands; the creation of berms or enrichment of beaches; and the control of water level and boat traffic. The discussions of Dredging and the Disposal of Dredged Material consider dredges, dredging methods, and disposal of dredged material. The following subjects are considered under Fishery Management Techniques: fish attractors; spawning structures; nursery ponds, coves, and marshes; fish screens and barriers; fish passage; water control structures; management of water levels and flows; wing dam modification; side channel modification; aeration techniques; control of nuisance aquatic plants; and manipulated of fish populations. Wildlife Management Techniques include treatments of artificial nest structures, island creation or development, marsh creation or development, greentree reservoirs and mast management, vegetation control, water level control, and revegetation.

","language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, D.C.","usgsCitation":"Schnick, R.A., Morton, J.M., Mochalski, J.C., and Beall, J.T., 1982, Mitigation and enhancement techniques for the Upper Mississippi River system and other large river systems: Resource Publication 149, xxiv, 714 p.","productDescription":"xxiv, 714 p.","numberOfPages":"742","costCenters":[],"links":[{"id":331079,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":290219,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/37151/report.pdf"}],"country":"United States","otherGeospatial":"Upper Mississippi River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ac0","contributors":{"authors":[{"text":"Schnick, Rosalie A.","contributorId":34565,"corporation":false,"usgs":true,"family":"Schnick","given":"Rosalie","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":511192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morton, John M.","contributorId":17097,"corporation":false,"usgs":true,"family":"Morton","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":511190,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mochalski, Jeffrey C.","contributorId":10673,"corporation":false,"usgs":true,"family":"Mochalski","given":"Jeffrey","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":511189,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beall, Jonathan T.","contributorId":23815,"corporation":false,"usgs":true,"family":"Beall","given":"Jonathan","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":511191,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":47552,"text":"wdrIN811 - 1982 - Water resources data, Indiana, water year 1981","interactions":[],"lastModifiedDate":"2014-06-26T11:08:09","indexId":"wdrIN811","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1982","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":"IN-81-1","title":"Water resources data, Indiana, water year 1981","docAbstract":"

Water resources data for the 1981 water year for Indiana consists of records of stage, discharge, and water quality of streams; stage and contents of lakes and reservoirs; and water levels in wells. This report contains discharge records for 195 gaging stations, stage and contents for 12 lakes and reservoirs, releases from 6 flood control reservoirs, water quality for 51 gaging stations, and water levels for 84 observation wells. Also included are 95 crest-stage partial-record stations and 42 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements. 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 Indiana.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrIN811","collaboration":"Prepared in cooperation with the State of Indiana and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Water resources data, Indiana, water year 1981: U.S. Geological Survey Water Data Report IN-81-1, xiv, 448 p., https://doi.org/10.3133/wdrIN811.","productDescription":"xiv, 448 p.","numberOfPages":"465","temporalStart":"1980-10-01","temporalEnd":"1981-09-30","costCenters":[],"links":[{"id":288330,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdrIN811.jpg"},{"id":288329,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1981/in-81-1/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f70b0","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8947,"text":"ofr82571 - 1982 - Ground-water withdrawals and land-surface subsidence in the Houston-Galveston region, Texas, 1906-80","interactions":[],"lastModifiedDate":"2016-08-11T15:04:10","indexId":"ofr82571","displayToPublicDate":"1994-01-01T01:00:00","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":"82-571","title":"Ground-water withdrawals and land-surface subsidence in the Houston-Galveston region, Texas, 1906-80","docAbstract":"

The withdrawal of larqe amounts of ground water in the Houston-Galveston region, Texas, has resulted in water-level declines of as much as 250 feet (76 meters) in wells completed in the Chicot aquifer and as much as 300 feet (91 meters) in wells completed in the Evangeline aquifer during 1943-77. Since late 1976, changes in pumping distribution resulting from efforts to control subsidence and the introduction of surface water from Lake Livingston have altered the pattern of water-level changes. In the Johnson Space Center and Baytown-La Porte areas (Chicot aquifer), and in the Pasadena area (Evangeline aquifer), water levels rose about 20 feet (6.1 meters) during 1973-77. However, in the western Houston area (Evangeline aquifer), water levels have continued to decline at an increasing rate through 1977.

\n

The declines in water levels have caused pronounced regional subsidence of the land surface. The center of regional subsidence is the Pasadena area, where more than 9 feet (2.7 meters) and possibly as much as 10 feet (3.0 meters) of subsidence occurred between 1906 and 1978. Almost 9 feet (2.7 meters) of subsidence occurred between 1943 and 1978. Localized centers of subsidence exist throughout the region, especially in the Baytown-La Porte and Texas City areas.

\n

Evaluation of tide records from five gages in Galveston Bay and the tidal reaches of Buffalo Bayou indicates that changes in elevations of significantly less than 0.5 foot (150 millimeters) and possibly as little as 0.1 foot (30 millimeters) can be detected.

\n

The unit measure of compressibility, specific-unit compaction, ranged from 1.0 x 10-5 to 4.0 x 10-5 feet-1 (3.28 x 10-5 to 1.31 x 10-4 m-1) of compaction per foot of clay thickness per foot of average water-level change for 1906-78. The greatest compressibility was at the Clear Lake site and the least compressibility was at the Lake Houston site. The data indicate that the compressibility is related to the age of the sediments and the depth of burial of the sediments.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82571","usgsCitation":"Gabrysch, R., 1982, Ground-water withdrawals and land-surface subsidence in the Houston-Galveston region, Texas, 1906-80: U.S. Geological Survey Open-File Report 82-571, vi, 68 p., https://doi.org/10.3133/ofr82571.","productDescription":"vi, 68 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":36575,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0571/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0571/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672bf","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":158605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10894,"text":"ofr82678 - 1982 - Water quality of Canyon Lake, central Texas","interactions":[],"lastModifiedDate":"2016-08-11T15:24:12","indexId":"ofr82678","displayToPublicDate":"1994-01-01T01:00:00","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":"82-678","title":"Water quality of Canyon Lake, central Texas","docAbstract":"

The volume-weighted average concentrations of the principal dissolved constituents in Canyon Lake on the Guadalupe River in central Texas are usually less than 240 milligrams per liter of dissolved solids, 20 milligrams per liter of chloride, and 30 milligrams per liter of sulfate. The water, which is very hard, has a volume-weighted average concentration of hardness of about 200 milligrams per liter. There is little seasonal variation in the volume-weighted average concentrations of the principal dissolved constituents.

\n

Thermal stratification of the lake usually begins during March and persists until September or October. Stratification results in significant seasonal and areal variations in dissolved oxygen, which in turn result in higher concentrations of dissolved iron, dissolved manganese, and total ammonia during the summer. Oxygen used in the stabilization of unoxidized material in the lake is not replaced during summer stagnation. The depth-integrated concentration of dissolved oxygen averaged less than 4.0 milligrams per liter during summer stagnation and about 9.0 milligrams per liter during winter circulation.

\n

The concentrations of dissolved iron and dissolved manganese, which varied seasonally, were closely related to the concentrations of dissolved oxygen. Reducing conditions in the hypolimnion often result in the dissolution of iron and manganese from bottom sediments in the deep parts of the lake. At site Dc, a deep site on an arm of Canyon Lake, the summer concentrations of dissolved iron averaged 860 micrograms per liter and the concentration of dissolved manganese averaged 390 micrograms per liter. The concentrations of total ammonia in the lake usually were less than 0.2 milligram per liter except in the hypolimnion (bottom stratum) during summer stagnation when nitrate and nitrite are reduced to ammonia.

\n

The closure of Canyon Dam resulted in a change in the monthly average water temperature of the Guadalupe River downstream from the dam. Prior to closure, the maximum monthly average water temperature for the Guadalupe River near Sattler, which was 29.0? degrees Celsius, occurred during June or July. Since closure of the dam, the maximum monthly average water temperature, which is 19.0? degrees Celsius, occurs during September or November.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82678","usgsCitation":"Roddy, W., and Waddell, K., 1982, Water quality of Canyon Lake, central Texas: U.S. Geological Survey Open-File Report 82-678, Report: v, 68 p.; Plate: 9.62 x 16.72 inches, https://doi.org/10.3133/ofr82678.","productDescription":"Report: v, 68 p.; Plate: 9.62 x 16.72 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":143002,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0678/report-thumb.jpg"},{"id":38668,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0678/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":38669,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0678/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489ee4","contributors":{"authors":[{"text":"Roddy, W.R.","contributorId":27453,"corporation":false,"usgs":true,"family":"Roddy","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":162155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":162156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":65460,"text":"i1438 - 1982 - Controlled photomosaic of the Iapygia Northeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:17","indexId":"i1438","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1438","subseriesTitle":"NONE","title":"Controlled photomosaic of the Iapygia Northeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1438","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Controlled photomosaic of the Iapygia Northeast Quadrangle of Mars: U.S. Geological Survey IMAP 1438, 1 photomosaic ;40 x 59 cm., on sheet 86 x 67 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1438.","productDescription":"1 photomosaic ;40 x 59 cm., on sheet 86 x 67 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":114945,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1438/report.pdf","size":"30","linkFileType":{"id":1,"text":"pdf"}},{"id":114946,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1438/plate-1.pdf","size":"7219","linkFileType":{"id":1,"text":"pdf"}},{"id":189149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1438/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688af7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533847,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27597,"text":"wri824110 - 1982 - Hydrology of the sand-and-gravel aquifer, southern Okaloosa and Walton Counties, northwest Florida","interactions":[],"lastModifiedDate":"2022-02-22T19:34:05.117776","indexId":"wri824110","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":"82-4110","title":"Hydrology of the sand-and-gravel aquifer, southern Okaloosa and Walton Counties, northwest Florida","docAbstract":"

The sand-and-gravel aquifer in southern Okaloosa and Walton Counties, northwest Florida, extends from land surface to depth of 50 to 150 feet. Intervening layers of clay generally separate the aquifer into an unconfined surficial zone, composed principally of fine to medium sand, and a lower confined zone, consisting of variable amounts of medium to coarse sand and gravel. Well yields of 50 to 500 gallons per minute are possible in most of the area, and yields of 500 to 1,000 gallons per minute can be developed in parts of southwestern Okaloosa County.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824110","usgsCitation":"Hayes, L.R., and Barr, D.E., 1982, Hydrology of the sand-and-gravel aquifer, southern Okaloosa and Walton Counties, northwest Florida: U.S. Geological Survey Water-Resources Investigations Report 82-4110, vi, 49 p., https://doi.org/10.3133/wri824110.","productDescription":"vi, 49 p.","costCenters":[],"links":[{"id":158870,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4110/report-thumb.jpg"},{"id":56467,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4110/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396266,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35617.htm"}],"country":"United States","state":"Florida","county":"Okaloosa County, Walton County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -86.70135498046875,\n 30.379983796443767\n ],\n [\n -86.19873046875,\n 30.379983796443767\n ],\n [\n -86.19873046875,\n 30.590637026892917\n ],\n [\n -86.70135498046875,\n 30.590637026892917\n ],\n [\n -86.70135498046875,\n 30.379983796443767\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc79d","contributors":{"authors":[{"text":"Hayes, L. R.","contributorId":50931,"corporation":false,"usgs":true,"family":"Hayes","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198387,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barr, D. E.","contributorId":55469,"corporation":false,"usgs":true,"family":"Barr","given":"D.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198388,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":41679,"text":"ofr82356 - 1982 - Arsenic, nitrate, iron, and hardness in ground water, Chena Hot Springs Road, Steele Creek Road, and Gilmore Trail areas, (T.1N., R.1E., FM), Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2022-11-02T20:10:16.813379","indexId":"ofr82356","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":"82-356","title":"Arsenic, nitrate, iron, and hardness in ground water, Chena Hot Springs Road, Steele Creek Road, and Gilmore Trail areas, (T.1N., R.1E., FM), Fairbanks, Alaska","docAbstract":"This report presents all data on arsenic, nitrate, iron, and hardness in well water in the Chena Hot Springs Road, Steele Creek Road, and Gilmore Trail area of Fairbanks, Alaska, collected through October 1981. Concentrations range as follows: arsenic - 0 to 5,100 micrograms per liter; nitrate - 0 to 53 milligrams per liter; iron - 0 to 50 milligrams per liter, and hardness - 12 to 1,000 milligrams per liter. The percentage of samples exceeding limits set by the U.S. Environmental Protection Agency are as follows: arsenic - 13%; nitrate - 14%, and iron - 80%. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82356","usgsCitation":"Krumhardt, A.P., 1982, Arsenic, nitrate, iron, and hardness in ground water, Chena Hot Springs Road, Steele Creek Road, and Gilmore Trail areas, (T.1N., R.1E., FM), Fairbanks, Alaska: U.S. Geological Survey Open-File Report 82-356, 2 Plates: 18.90 × 29.67 inches and 18.82 × 30.36 inches, https://doi.org/10.3133/ofr82356.","productDescription":"2 Plates: 18.90 × 29.67 inches and 18.82 × 30.36 inches","costCenters":[],"links":[{"id":135488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79401,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0356/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79400,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0356/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409080,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13706.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","city":"Fairbanks","otherGeospatial":"Chena Hot Springs Road, Steele Creek Road, and Gilmore Trail areas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -147.55,\n 64.864\n ],\n [\n -147.55,\n 64.95\n ],\n [\n -147.417,\n 64.95\n ],\n [\n -147.417,\n 64.864\n ],\n [\n -147.55,\n 64.864\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c7f","contributors":{"authors":[{"text":"Krumhardt, Andrea P.","contributorId":71946,"corporation":false,"usgs":true,"family":"Krumhardt","given":"Andrea","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":225368,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11009,"text":"ofr82341 - 1982 - Report of the River Master of the Delaware River for the period of December 1, 1980 to November 30, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:29","indexId":"ofr82341","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":"82-341","title":"Report of the River Master of the Delaware River for the period of December 1, 1980 to November 30, 1981","docAbstract":"Water supply conditions at the beginning of the year were marginal in marked contrast to those for the preceeding nine years. Discharge of the Delaware River at Montague, New Jersey, was only 72% of median as compared to 68% in excess of median the previous year. In December, with reservoir storage again declining, further reductions in both diversions and releases were imposed. With consent of all the parties, reductions were effected on December 20 limiting New York City diversions to 560 mgd, New Jersey to 65 mgd, and the required discharge at Montague was targeted at 1550 cfs. To conserve supplies, additional reductions were imposed in January when the Delaware River basin Commission formally declared a drought. New York City 's limitations was set at 520 mgd and that for New Jersey at 62 mgd. Montague flows were targeted between 1100 cfs, depending upon the location of the salt front in the estuary. Water quality of the Delaware River and Estuary was monitored on a continuous basis at eight sites for most of the year and on a monthly basis at ten sites to accurately locate the salt front. Highest concentrations observed at the Benjamin Franklin Bridge site was 133 mg/l (milligram per liter) on February 2. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82341","usgsCitation":"Schaefer, F.T., and Fish, R., 1982, Report of the River Master of the Delaware River for the period of December 1, 1980 to November 30, 1981: U.S. Geological Survey Open-File Report 82-341, 110 p. :ill., maps (some col.) ;27 cm., https://doi.org/10.3133/ofr82341.","productDescription":"110 p. :ill., maps (some col.) ;27 cm.","costCenters":[],"links":[{"id":144073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0341/report-thumb.jpg"},{"id":38778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0341/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bcfd","contributors":{"authors":[{"text":"Schaefer, Francis T.","contributorId":48184,"corporation":false,"usgs":true,"family":"Schaefer","given":"Francis","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":162369,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fish, Robert E.","contributorId":51296,"corporation":false,"usgs":true,"family":"Fish","given":"Robert E.","affiliations":[],"preferred":false,"id":162370,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":41955,"text":"ofr82546 - 1982 - Aeromagnetic map of Mt. Washington, Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr82546","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":"82-546","title":"Aeromagnetic map of Mt. Washington, Oregon","language":"ENGLISH","doi":"10.3133/ofr82546","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Aeromagnetic map of Mt. Washington, Oregon: U.S. Geological Survey Open-File Report 82-546, 1 map ;52 x 47 cm., https://doi.org/10.3133/ofr82546.","productDescription":"1 map ;52 x 47 cm.","costCenters":[],"links":[{"id":136525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79717,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0546/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e92","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":27624,"text":"wri8178 - 1982 - Automation of an ion chromatograph for precipitation analysis with computerized data reduction","interactions":[],"lastModifiedDate":"2017-10-03T10:15:54","indexId":"wri8178","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":"81-78","title":"Automation of an ion chromatograph for precipitation analysis with computerized data reduction","docAbstract":"

Interconnection of an ion chromatograph, an autosampler, and a computing integrator to form an analytical system for simultaneous determination of fluoride, chloride, orthophosphate, bromide, nitrate, and sulfate in precipitation samples is described. Computer programs provided with the integrator are modified to implement ionchromatographic data reduction and data storage. The liquid-flow scheme for the ion chromatograph is changed by addition of a second suppressor column for greater analytical capacity. An additional vave enables selection of either suppressor column for analysis, as the other column is regenerated and stabilized with concentrated eluent.

Minimum limits of detection and quantitation for each anion are calculated; these limits are a function of suppressor exhaustion. Precision for replicate analyses of six precipitation samples for fluoride, chloride, orthophosphate, nitrate, and sulfate ranged from 0.003 to 0.027 milligrams per liter. To determine accuracy of results, the same samples were spiked with known concentrations of the above mentioned anions. Average recovery was 108 percent.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8178","usgsCitation":"Hedley, A.G., and Fishman, M., 1982, Automation of an ion chromatograph for precipitation analysis with computerized data reduction: U.S. Geological Survey Water-Resources Investigations Report 81-78, iv, 33 p., https://doi.org/10.3133/wri8178.","productDescription":"iv, 33 p.","numberOfPages":"41","costCenters":[],"links":[{"id":159000,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0078/report-thumb.jpg"},{"id":346293,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0078/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668079","contributors":{"authors":[{"text":"Hedley, Arthur G.","contributorId":17876,"corporation":false,"usgs":true,"family":"Hedley","given":"Arthur","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":198429,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fishman, Marvin J.","contributorId":87110,"corporation":false,"usgs":true,"family":"Fishman","given":"Marvin J.","affiliations":[],"preferred":false,"id":198430,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36492,"text":"fwsobs82_13_3 - 1982 - A guidance manual for the input of biological information to water intake structure design","interactions":[],"lastModifiedDate":"2012-02-02T00:09:35","indexId":"fwsobs82_13_3","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"82/13.3","title":"A guidance manual for the input of biological information to water intake structure design","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Neitzel, D., Simmons, M., and McKenzie, D., 1982, A guidance manual for the input of biological information to water intake structure design: FWS/OBS 82/13.3, viii, 37 p. : ill.; 28 cm.","productDescription":"viii, 37 p. : ill.; 28 cm.","costCenters":[],"links":[{"id":167155,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae5d4","contributors":{"authors":[{"text":"Neitzel, D.A.","contributorId":100905,"corporation":false,"usgs":true,"family":"Neitzel","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":216414,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simmons, M.A.","contributorId":34576,"corporation":false,"usgs":true,"family":"Simmons","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":216412,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McKenzie, D.H.","contributorId":89195,"corporation":false,"usgs":true,"family":"McKenzie","given":"D.H.","email":"","affiliations":[],"preferred":false,"id":216413,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":27634,"text":"wri8240 - 1982 - Method for estimating historical irrigation requirements from ground water in the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","interactions":[],"lastModifiedDate":"2018-08-08T14:01:49","indexId":"wri8240","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":"82-40","title":"Method for estimating historical irrigation requirements from ground water in the High Plains in parts of Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, and Wyoming","docAbstract":"

Historical information on ground-water pumpage for irrigation is required for use with a computer model of the High Plains aquifer. Available historical data on ground-water pumpage in the High Plains were inadequate for use with the computer model. Consequently, a method was developed to estimate historical pumpage data.

Two principal components were used to develop estimates of ground-water pumpage: (1) Acreage irrigated; and (2) irrigation demand. The Blaney-Criddle formula was used to calculate consumptive-use requirements for irrigated crops grown on the High Plains. The irrigation demand for each crop was estimated by subtracting precipitation available to the crop from the consumptive-use requirement of the crop. Irrigation demands were combined with irrigated acreages to estimate the volume of irrigation water required for areas in the High Plains. Estimates of irrigation water requirements were compiled for 1949, 1954, 1959, 1964, 1969, 1974, and 1978. Irrigation pumpage for use with the computer model can be estimated from the irrigation water requirements by applying a factor to account for irrigation system efficiency.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8240","usgsCitation":"Heimes, F.J., and Luckey, R.R., 1982, Method for estimating historical irrigation requirements from ground water in 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 82-40, iii, 64 p., https://doi.org/10.3133/wri8240.","productDescription":"iii, 64 p.","numberOfPages":"71","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true},{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":356336,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0040/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0040/report-thumb.jpg"}],"country":"United States","state":"Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106,\n 32\n ],\n [\n -96,\n 32\n ],\n [\n -96,\n 43.5\n ],\n [\n -106,\n 43.5\n ],\n [\n -106,\n 32\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629ed0","contributors":{"authors":[{"text":"Heimes, Frederick J.","contributorId":20787,"corporation":false,"usgs":true,"family":"Heimes","given":"Frederick","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198451,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Luckey, Richard R.","contributorId":17980,"corporation":false,"usgs":true,"family":"Luckey","given":"Richard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":198450,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":67620,"text":"l87 - 1982 - Land use and land cover, 1974-75, Atlanta, Georgia; Alabama","interactions":[],"lastModifiedDate":"2012-02-10T00:11:24","indexId":"l87","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87","title":"Land use and land cover, 1974-75, Atlanta, Georgia; Alabama","language":"ENGLISH","doi":"10.3133/l87","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Land use and land cover, 1974-75, Atlanta, Georgia; Alabama: U.S. Geological Survey Land Use and Land Cover 87, -, https://doi.org/10.3133/l87.","productDescription":"-","costCenters":[],"links":[{"id":188007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260925,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/087/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86,33 ], [ -86,34 ], [ -84,34 ], [ -84,33 ], [ -86,33 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae32d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534366,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11219,"text":"ofr82987 - 1982 - Leaching characteristics of ash from the May 18, 1980, eruption of Mount St. Helens Volcano, Washington","interactions":[],"lastModifiedDate":"2025-05-14T19:42:17.843167","indexId":"ofr82987","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":"82-987","title":"Leaching characteristics of ash from the May 18, 1980, eruption of Mount St. Helens Volcano, Washington","docAbstract":"Leaching of freshly erupted air-fall ash, unaffected by rain, from the May 18, 1.980,eruption of Mount St. Helens volcano, Washington, shows that Ca 2+, Na+, Mg+, SO4 2-, and Cl- are the predominant chemical species released on first exposure of the ash to water. Extremely high correlation of Ca with SO4 and Na with Cl in water leachates suggests the presence of CaSO4 and NaCl salts on the ash. The amount of water soluble material on ash increases with distance from source and with the weight fraction of small (less than 63 micrometers) ash particles of high-surface area. This suggests that surface reactions such as adsorption are responsible for concentrating the soluble material. CaSO4, NaCl, and other salts are probably formed as microscopic crystals in the high-temperature core of the eruption column and are then adsorbed by silicate ash particles. \r\n\r\nThe environmentally important elements Zn, Cu, Cd, F, Pb, and Ba are released by a water leach in concentrations which could pose short-term hazards to some forms of aquatic life. However, calculated concentrations are based on a water-to-ash ratio of 4:1 or less, which is probably an underestimation of the regionally operative ratio. A subsequent leach of ash by warm alkaline solution shows dramatic increases in the amount of dissolved SiO2, U, and V, which are probably caused by increased dissolution of the glassy component of ash. Glass dissolution by alkaline ground water is a mechanism for providing these three elements to sedimentary traps where they may co-accumulate as uraniferous silica or U-V minerals. \r\n\r\nLeaching characteristics of ash from Mount St. Helens are comparable to characteristics of ash of similar composition from volcanoes in Guatemala. Ashes from each locality show similar ions predominating for a given leachate and similar fractions of a particular element in the ash removed on contact with the leach solution.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82987","usgsCitation":"Smith, D.B., Zielinski, R.A., and Taylor, H.E., 1982, Leaching characteristics of ash from the May 18, 1980, eruption of Mount St. Helens Volcano, Washington: U.S. Geological Survey Open-File Report 82-987, 30 p., ill., map ;28 cm., https://doi.org/10.3133/ofr82987.","productDescription":"30 p., ill., map ;28 cm.","costCenters":[],"links":[{"id":144548,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0987/report-thumb.jpg"},{"id":39010,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0987/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89b9","contributors":{"authors":[{"text":"Smith, David Burl","contributorId":90738,"corporation":false,"usgs":true,"family":"Smith","given":"David","email":"","middleInitial":"Burl","affiliations":[],"preferred":false,"id":162755,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zielinski, Robert A. 0000-0002-4047-5129 rzielinski@usgs.gov","orcid":"https://orcid.org/0000-0002-4047-5129","contributorId":1593,"corporation":false,"usgs":true,"family":"Zielinski","given":"Robert","email":"rzielinski@usgs.gov","middleInitial":"A.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":162753,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Taylor, Howard E. hetaylor@usgs.gov","contributorId":1551,"corporation":false,"usgs":true,"family":"Taylor","given":"Howard","email":"hetaylor@usgs.gov","middleInitial":"E.","affiliations":[{"id":5044,"text":"National Research Program - Central Branch","active":true,"usgs":true}],"preferred":true,"id":162754,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":11616,"text":"ofr82352 - 1982 - A model for the simulation of flow of variable-density ground water in three dimensions under steady-state conditions","interactions":[],"lastModifiedDate":"2012-02-02T00:06:44","indexId":"ofr82352","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":"82-352","title":"A model for the simulation of flow of variable-density ground water in three dimensions under steady-state conditions","docAbstract":"A computer program has been developed as part of the U.S. Geological Survey's national program of Regional Aquifer System Analysis (RASA) that generates input to ground-water flow models to enable them to simulate variable-density ground-water flow. Information required for the program's operation is: aquifer elevation, thickness, and ground-water density. Included in the report is a computer program for calculating ground-water density from aquifer depth, temperature, and dissolved solids concentration. The 60-page report describes the theoretical development and documents two FORTRAN programs used to generate the necessary flow-model input. An example for a symmetrical basin is fully worked out.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82352","usgsCitation":"Weiss, E., 1982, A model for the simulation of flow of variable-density ground water in three dimensions under steady-state conditions: U.S. Geological Survey Open-File Report 82-352, vii, 66 p., ill. ;28 cm., https://doi.org/10.3133/ofr82352.","productDescription":"vii, 66 p., ill. ;28 cm.","costCenters":[],"links":[{"id":145283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0352/report-thumb.jpg"},{"id":39476,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0352/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6adf42","contributors":{"authors":[{"text":"Weiss, Emanuel","contributorId":74383,"corporation":false,"usgs":true,"family":"Weiss","given":"Emanuel","affiliations":[],"preferred":false,"id":163451,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68419,"text":"ha645 - 1982 - Dissolved-solids concentrations of ground water in the Sacramento Valley, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:12","indexId":"ha645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"645","title":"Dissolved-solids concentrations of ground water in the Sacramento Valley, California","docAbstract":"The general quality of the ground water in the Sacramento Valley , Calif., in terms of dissolved-solids concentration is considered good for irrigation, domestic, and most other uses. This map shows the distribution of dissolved-solids concentrations and is based on about 1,330 chemical analyses collected from about 900 wells between 1974 and 1978. On the west side of the valley some of the smaller streams contribute water of higher dissolved-solids concentrations to the ground water. The sources of these waters are thought to be the upper Cretaceous Chico Formation or marine deposits of Early Cretaceous age that are exposed in the Coast Ranges. (USGS)","language":"ENGLISH","doi":"10.3133/ha645","usgsCitation":"Fogelman, R.P., 1982, Dissolved-solids concentrations of ground water in the Sacramento Valley, California: U.S. Geological Survey Hydrologic Atlas 645, 1 map :col. ;70 x 99 cm., on sheet 76 x 112 cm., folded in envelope 32 x 24 cm., https://doi.org/10.3133/ha645.","productDescription":"1 map :col. ;70 x 99 cm., on sheet 76 x 112 cm., folded in envelope 32 x 24 cm.","costCenters":[],"links":[{"id":188901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89942,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/645/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.75,38.083333333333336 ], [ -122.75,40.333333333333336 ], [ -120.75,40.333333333333336 ], [ -120.75,38.083333333333336 ], [ -122.75,38.083333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1ed","contributors":{"authors":[{"text":"Fogelman, Ronald P.","contributorId":62597,"corporation":false,"usgs":true,"family":"Fogelman","given":"Ronald","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":278186,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":29270,"text":"wri8241 - 1982 - Quadratic spline subroutine package","interactions":[],"lastModifiedDate":"2019-08-05T11:50:38","indexId":"wri8241","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":"82-41","title":"Quadratic spline subroutine package","docAbstract":"A continuous piecewise quadratic function with continuous first derivative is devised for approximating a single-valued, but unknown, function represented by a set of discrete points. The quadratic is proposed as a treatment intermediate between using the angular (but reliable, easily constructed and manipulated) piecewise linear function and using the smoother (but occasionally erratic) cubic spline. Neither iteration nor the solution of a system of simultaneous equations is necessary to determining the coefficients. Several properties of the quadratic function are given. A set of five short FORTRAN subroutines is provided for generating the coefficients (QSC), finding function value and derivatives (QSY), integrating (QSI), finding extrema (QSE), and computing arc length and the curvature-squared integral (QSK). (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8241","usgsCitation":"Rasmussen, L.A., 1982, Quadratic spline subroutine package: U.S. Geological Survey Water-Resources Investigations Report 82-41, 16 p. , https://doi.org/10.3133/wri8241.","productDescription":"16 p. ","costCenters":[],"links":[{"id":366263,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158306,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/0041/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a340","contributors":{"authors":[{"text":"Rasmussen, Lowell A.","contributorId":36930,"corporation":false,"usgs":true,"family":"Rasmussen","given":"Lowell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":201250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7523,"text":"ofr82323B - 1982 - Stacked magnetic and radiometric profiles of flight lines in the McDermitt calderas area, Nevada-Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr82323B","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":"82-323","chapter":"B","title":"Stacked magnetic and radiometric profiles of flight lines in the McDermitt calderas area, Nevada-Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82323B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Stacked magnetic and radiometric profiles of flight lines in the McDermitt calderas area, Nevada-Oregon: U.S. Geological Survey Open-File Report 82-323, 96 sheets :all ill. ;77 x 109 cm. or smaller folded to 37 x 27 cm. or smaller., https://doi.org/10.3133/ofr82323B.","productDescription":"96 sheets :all ill. ;77 x 109 cm. or smaller folded to 37 x 27 cm. or smaller.","costCenters":[],"links":[{"id":140201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4916","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41995,"text":"ofr82548 - 1982 - Aeromagnetic map of the Dome Peak area, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:02","indexId":"ofr82548","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":"82-548","title":"Aeromagnetic map of the Dome Peak area, Washington","language":"ENGLISH","doi":"10.3133/ofr82548","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Aeromagnetic map of the Dome Peak area, Washington: U.S. Geological Survey Open-File Report 82-548, 1 map ;76 x 77 cm., https://doi.org/10.3133/ofr82548.","productDescription":"1 map ;76 x 77 cm.","costCenters":[],"links":[{"id":135457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79752,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0548/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69695a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530761,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9354,"text":"ofr811113 - 1982 - Hydrology of Area 24, Eastern Coal Province, Alabama and Georgia","interactions":[],"lastModifiedDate":"2016-12-14T12:01:54","indexId":"ofr811113","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":"81-1113","title":"Hydrology of Area 24, Eastern Coal Province, Alabama and Georgia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811113","usgsCitation":"Harkins, J.R., and and others, 1982, Hydrology of Area 24, Eastern Coal Province, Alabama and Georgia: U.S. Geological Survey Open-File Report 81-1113, v, 81 p. :ill., col. maps ;28 cm., https://doi.org/10.3133/ofr811113.","productDescription":"v, 81 p. :ill., col. maps ;28 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":144150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1113/report-thumb.jpg"},{"id":94919,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1113/report.pdf","size":"24196","linkFileType":{"id":1,"text":"pdf"}},{"id":94510,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://hdl.handle.net/2027/mdp.39015048192861?urlappend=%3Bseq=3"}],"country":"United States","state":"Alabama, Georgia","otherGeospatial":"Eastern Coal Province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.4351806640625,\n 34.800272350556824\n ],\n [\n -85.31982421875,\n 34.836349990763864\n ],\n [\n -85.14404296875,\n 34.74161249883172\n ],\n [\n -85.242919921875,\n 34.50655662164561\n ],\n [\n -85.20996093749999,\n 34.40237742424137\n ],\n [\n -85.1495361328125,\n 34.279914398549934\n ],\n [\n -85.089111328125,\n 34.161818161230386\n ],\n [\n -85.242919921875,\n 33.95247360616282\n ],\n [\n -85.3912353515625,\n 33.947916898356404\n ],\n [\n -85.4791259765625,\n 33.76544869849223\n ],\n [\n -85.6494140625,\n 33.568861182555565\n ],\n [\n -85.814208984375,\n 33.27543541298162\n ],\n [\n -85.792236328125,\n 33.165145408240285\n ],\n [\n -86.0009765625,\n 33.100745405144245\n ],\n [\n -86.1712646484375,\n 33.18353672893615\n ],\n [\n -86.1602783203125,\n 33.27543541298162\n ],\n [\n -86.253662109375,\n 33.31216783738619\n ],\n [\n -86.319580078125,\n 33.35347332342168\n ],\n [\n -86.7425537109375,\n 33.31675830290707\n ],\n [\n -86.7315673828125,\n 33.43602551072033\n ],\n [\n -86.27014160156249,\n 33.73347670599252\n ],\n [\n -86.3580322265625,\n 33.88865750124075\n ],\n [\n -86.37451171875,\n 33.988918483762156\n ],\n [\n -86.209716796875,\n 34.048108084909835\n ],\n [\n -86.1602783203125,\n 34.13908837343849\n ],\n [\n -86.0614013671875,\n 34.261756524459805\n ],\n [\n -85.9185791015625,\n 34.31168124115256\n ],\n [\n -85.6658935546875,\n 34.45674800347809\n ],\n [\n -85.4351806640625,\n 34.800272350556824\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604b86","contributors":{"authors":[{"text":"Harkins, Joe R.","contributorId":28982,"corporation":false,"usgs":true,"family":"Harkins","given":"Joe","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":159534,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528902,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}