{"pageNumber":"5186","pageRowStart":"129625","pageSize":"25","recordCount":184563,"records":[{"id":8965,"text":"ofr83517 - 1983 - Mineralogical and sedimentological data collected on the shelf and upper slope adjacent to the Russian River, Northern California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr83517","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-517","title":"Mineralogical and sedimentological data collected on the shelf and upper slope adjacent to the Russian River, Northern California","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83517","usgsCitation":"Gardner, J.V., and Klise, D.H., 1983, Mineralogical and sedimentological data collected on the shelf and upper slope adjacent to the Russian River, Northern California: U.S. Geological Survey Open-File Report 83-517, 35 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr83517.","productDescription":"35 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":141144,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0517/report-thumb.jpg"},{"id":36585,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0517/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e88","contributors":{"authors":[{"text":"Gardner, James V.","contributorId":93035,"corporation":false,"usgs":true,"family":"Gardner","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":158636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klise, David H.","contributorId":13977,"corporation":false,"usgs":true,"family":"Klise","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":158635,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3653,"text":"cir886 - 1983 - Analysis of the world distribution of metal-rich subsea manganese nodules","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir886","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"886","title":"Analysis of the world distribution of metal-rich subsea manganese nodules","docAbstract":"Publicly available data on the composition of subsea manganese nodules extend previous reports of differences in average metal contents from ocean to ocean and of variations related to latitude and depth. Pacific Ocean nodules have the highest average manganese, nickel, and copper contents, and Atlantic Ocean nodules have the highest average iron content. The average manganese, nickel, and copper contents generally increase toward the equator in both hemispheres, and iron content generally decreases. The variation of metal content with water depth is not linear; instead, there appears to be a threshold depth of about 2,900 to 3,000 m, above which combined nickel and copper contents are generally less than 1 percent and below which cobalt content is generally less than about 0.6 percent. \r\n\r\nThe composition of the nodules varies widely, but three rarely overlapping types that are of possible economic interest can be recognized. (1) Nodules containing more than about 1 percent combined nickel and copper only exceptionally contain more than 0.5 percent cobalt and 35 percent manganese. (2) Nodules containing more than 0.5 percent cobalt rarely contain more than 1 percent combined nickel and copper and 35 percent manganese. (3) Nodules containing more than 35 percent manganese only exceptionally contain more than 0.5 percent cobalt, although they average nearly 1.1 percent combined nickel and copper. Current economic interest in nodule mining is focused on the Clarion-Clipperton zone in the northeastern equatorial Pacific Ocean, the largest known area in which nodules average 1.8 percent or more combined nickel and copper. Several other areas in which nodules are rich in these metals are found in the Pacific and Indian Oceans and may be viewed as targets for exploration. \r\n\r\nNearly 60 chemical elements have been found in manganese nodules, many in concentrations far exceeding their crustal abundances. The amounts in which many minor elements are present vary with the amounts of principal metals present, but the three metal types described above do not include the maximum reported values for several other elements, such as titanium (8.9 percent), vanadium (0.5), zinc (9.0), and lead (0.75). It seems possible, therefore, that there may be other kinds of metal-rich types, some of which may have p6tential economic value. \r\n\r\nMany of the variations in nodule composition are in large part a function of variations in mineral composition, to which many factors contribute. Some of the regional variations can be broadly related to oceanic circulation, basin morphology, and depth, but a better understanding of ocean processes and regional oceanography and geology is needed to explain all the variations observed in the composition of manganese nodules.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir886","usgsCitation":"McKelvey, V.E., Wright, N.A., and Bowen, R.W., 1983, Analysis of the world distribution of metal-rich subsea manganese nodules: U.S. Geological Survey Circular 886, iv, 55 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir886.","productDescription":"iv, 55 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":124693,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0886/report-thumb.jpg"},{"id":30694,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0886/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e778","contributors":{"authors":[{"text":"McKelvey, Vincent Ellis","contributorId":92650,"corporation":false,"usgs":true,"family":"McKelvey","given":"Vincent","email":"","middleInitial":"Ellis","affiliations":[],"preferred":false,"id":147340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, Nancy A.","contributorId":28586,"corporation":false,"usgs":true,"family":"Wright","given":"Nancy","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147339,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowen, Roger W.","contributorId":21142,"corporation":false,"usgs":true,"family":"Bowen","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":147338,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4474,"text":"cir902P - 1983 - Estimates of the potential petroleum resources in wilderness lands; petroleum potential of wilderness lands in the Western United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"cir902P","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"902","chapter":"P","title":"Estimates of the potential petroleum resources in wilderness lands; petroleum potential of wilderness lands in the Western United States","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological  Survey,","doi":"10.3133/cir902P","usgsCitation":"Miller, B., 1983, Estimates of the potential petroleum resources in wilderness lands; petroleum potential of wilderness lands in the Western United States: U.S. Geological Survey Circular 902, iii, P1-P15 p. :ill. ;26 cm.26 cm., https://doi.org/10.3133/cir902P.","productDescription":"iii, P1-P15 p. :ill. ;26 cm.26 cm.","costCenters":[],"links":[{"id":139667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0902p/report-thumb.jpg"},{"id":112511,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0902p/report.pdf","size":"1118","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fca74","contributors":{"authors":[{"text":"Miller, Betty M.","contributorId":92231,"corporation":false,"usgs":true,"family":"Miller","given":"Betty M.","affiliations":[],"preferred":false,"id":149302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4523,"text":"cir908 - 1983 - Annual report on Alaska's mineral resources","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"cir908","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"908","title":"Annual report on Alaska's mineral resources","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir908","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Annual report on Alaska's mineral resources: U.S. Geological Survey Circular 908, iv, 48 p. :ill., maps ;28 cm.28 cm., https://doi.org/10.3133/cir908.","productDescription":"iv, 48 p. :ill., maps ;28 cm.28 cm.","costCenters":[],"links":[{"id":117550,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1983/0908/report-thumb.jpg"},{"id":31581,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1983/0908/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b916","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":528227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5772,"text":"pp946 - 1983 - Geologic principles for prudent land use; a decisionmaker's guide for the San Francisco Bay region","interactions":[{"subject":{"id":9868,"text":"ofr80124 - 1980 - Examples of the use of earth-science information by decisionmakers in the San Francisco Bay region, California","indexId":"ofr80124","publicationYear":"1980","noYear":false,"title":"Examples of the use of earth-science information by decisionmakers in the San Francisco Bay region, California"},"predicate":"SUPERSEDED_BY","object":{"id":5772,"text":"pp946 - 1983 - Geologic principles for prudent land use; a decisionmaker's guide for the San Francisco Bay region","indexId":"pp946","publicationYear":"1983","noYear":false,"title":"Geologic principles for prudent land use; a decisionmaker's guide for the San Francisco Bay region"},"id":1}],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"pp946","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"946","title":"Geologic principles for prudent land use; a decisionmaker's guide for the San Francisco Bay region","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp946","usgsCitation":"Brown, R.D., and Kockelman, W.J., 1983, Geologic principles for prudent land use; a decisionmaker's guide for the San Francisco Bay region: U.S. Geological Survey Professional Paper 946, 97 p., https://doi.org/10.3133/pp946.","productDescription":"97 p.","costCenters":[],"links":[{"id":118013,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0946/report-thumb.jpg"},{"id":32438,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0946/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6884f8","contributors":{"authors":[{"text":"Brown, Robert David","contributorId":67084,"corporation":false,"usgs":true,"family":"Brown","given":"Robert","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":151562,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kockelman, William J.","contributorId":34510,"corporation":false,"usgs":true,"family":"Kockelman","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":151561,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27381,"text":"wri834010 - 1983 - Hydrogeologic evaluation of selected stratified-drift deposits in Connecticut","interactions":[],"lastModifiedDate":"2025-01-10T19:57:57.67083","indexId":"wri834010","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4010","title":"Hydrogeologic evaluation of selected stratified-drift deposits in Connecticut","docAbstract":"<p>Test borings at 28 sites and seismic-refraction profiles at 16 sites provide data on the saturated thickness and grain-size characteristics of stratified-drift deposits in five areas of Connecticut. These data, together with information on the areal extent of the deposits and their proximity to sources of induced recharge, can be used to estimate the water-yielding potential of the stratified-drift deposits. Individual wells could potentially yield moderate to possibly very large quantities of water (50 to 2000 gallons per minute) at some locations in all five areas where saturated, dominantly coarse-grained stratified drift is 40 feet thick or greater and hydraulically connected to nearby surface-water bodies. Coarse-grained stratified drift is most extensive in the Glastonbury, Haddam, and Simsbury, Connecticut areas. Saturated thickness exceeds 150 feet in parts of the Glastonbury and Haddam areas, but is less than 100 feet in most places. The best sites for developing large quantities of water are in the Glastonbury and Haddam areas where thick, saturated, coarse-grained stratified drift is hydraulically connected to the Connecticut River. Water in the stratified drift is generally of good chemical quality except for excessive iron (0.64 to 20 mg/L) and manganese (0.1 to 10 mg/L) in some samples.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834010","usgsCitation":"Grady, S.J., and Handman, E., 1983, Hydrogeologic evaluation of selected stratified-drift deposits in Connecticut: U.S. Geological Survey Water-Resources Investigations Report 83-4010, v, 56 p., https://doi.org/10.3133/wri834010.","productDescription":"v, 56 p.","costCenters":[],"links":[{"id":119860,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4010/report-thumb.jpg"},{"id":56240,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4010/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":466036,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35655.htm","text":"Bladens River area","linkFileType":{"id":5,"text":"html"}},{"id":466037,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35656.htm","text":"Glastonbury area","linkFileType":{"id":5,"text":"html"}},{"id":466038,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35657.htm","text":"Haddam area","linkFileType":{"id":5,"text":"html"}},{"id":466039,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35658.htm","text":"Simsbury area","linkFileType":{"id":5,"text":"html"}},{"id":466040,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35659.htm","text":"Willimantic River area","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Connecticut","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.24769490339403,\n              42.00620095205019\n            ],\n            [\n              -73.24769490339403,\n              41.3245840419726\n            ],\n            [\n              -71.96119276504564,\n              41.3245840419726\n            ],\n            [\n              -71.96119276504564,\n              42.00620095205019\n            ],\n            [\n              -73.24769490339403,\n              42.00620095205019\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db62873f","contributors":{"authors":[{"text":"Grady, S. J.","contributorId":69962,"corporation":false,"usgs":true,"family":"Grady","given":"S.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":198015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Handman, E. H.","contributorId":63407,"corporation":false,"usgs":true,"family":"Handman","given":"E.","middleInitial":"H.","affiliations":[],"preferred":false,"id":198014,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":60991,"text":"mf1660 - 1983 - Seismicity map of the State of New Mexico","interactions":[{"subject":{"id":60991,"text":"mf1660 - 1983 - Seismicity map of the State of New Mexico","indexId":"mf1660","publicationYear":"1983","noYear":false,"title":"Seismicity map of the State of New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":60990,"text":"mf2035 - 1988 - Seismicity map of the state of New Mexico","indexId":"mf2035","publicationYear":"1988","noYear":false,"title":"Seismicity map of the state of New Mexico"},"id":1}],"supersededBy":{"id":60990,"text":"mf2035 - 1988 - Seismicity map of the state of New Mexico","indexId":"mf2035","publicationYear":"1988","noYear":false,"title":"Seismicity map of the state of New Mexico"},"lastModifiedDate":"2017-05-11T14:15:07","indexId":"mf1660","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1660","title":"Seismicity map of the State of New Mexico","docAbstract":"<p><span>The data shown on this map and listed in table 1 are for earthquakes that were originally included in a study of seismic risk in the United States (Algermissen, 1969). This data file has been recompiled and updated through 1980. Some revisions of epicenters and intensities in the original file have been made, and intensities have been assigned to earthquakes that previously had none assigned. Only earthquakes that had epicenters within the boundary of the state are listed in table 1, even though earthquakes that had epicenters in bordering states or countries may have been felt or may have caused damage in the state. Intensity values were updated from data sources that were not available at the time or original compilation. Some epicenters were relocated on the basis of new information. The data shown in table 1 represent best estimates of the epicenter, magnitude, and intensity of each earthquake on the basis of historical and current information. Some of the aftershocks from large earthquakes are listed, but not all, especially for the earthquakes that occurred before seismic instruments were universally used.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1660","usgsCitation":"Stover, C.W., Reagor, B., and Algermissen, S.T., 1983, Seismicity map of the State of New Mexico: U.S. Geological Survey Miscellaneous Field Studies Map 1660, 52.37 x 32.81 inches, https://doi.org/10.3133/mf1660.","productDescription":"52.37 x 32.81 inches","costCenters":[],"links":[{"id":341145,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1660/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":179975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1660/mf1660.JPG"}],"country":"United States","state":"New Mexico","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"id\":\"35\",\"properties\":{\"name\":\"New 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,{"id":61008,"text":"mf1536 - 1983 - Geologic map of the Wenaha Tucannon Wilderness, Washington and Oregon","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf1536","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1536","title":"Geologic map of the Wenaha Tucannon Wilderness, Washington and Oregon","language":"ENGLISH","doi":"10.3133/mf1536","usgsCitation":"Swanson, D.A., and Wright, T.L., 1983, Geologic map of the Wenaha Tucannon Wilderness, Washington and Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1536, 1 map ;122 x 96 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1536.","productDescription":"1 map ;122 x 96 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106096,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7512.htm","linkFileType":{"id":5,"text":"html"},"description":"7512"},{"id":182784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.91666666666667,45.8675 ], [ -117.91666666666667,46.200833333333335 ], [ -117.5,46.200833333333335 ], [ -117.5,45.8675 ], [ -117.91666666666667,45.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a076","contributors":{"authors":[{"text":"Swanson, D. A.","contributorId":34102,"corporation":false,"usgs":true,"family":"Swanson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":264820,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, T. L.","contributorId":11188,"corporation":false,"usgs":true,"family":"Wright","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":264819,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61145,"text":"mf1425C - 1983 - Geochemical maps of Bunk Robinson Peak and Whitmire Canyon Roadless Areas, Hidalgo County, New Mexico, and Cochise County, Arizona","interactions":[],"lastModifiedDate":"2016-08-23T10:04:12","indexId":"mf1425C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1425","chapter":"C","title":"Geochemical maps of Bunk Robinson Peak and Whitmire Canyon Roadless Areas, Hidalgo County, New Mexico, and Cochise County, Arizona","docAbstract":"<p>Geochemical sampling of the Bunk Robinson Peak and Whitmire Canyon Roadless Areas was completed in the spring of 1980. The purpose of the geochemical sampling was to determine if certain metals, and \"pathfinder\" elements in heavy-mineral concentrates and stream sediments are enriched beyond normal black-ground amounts. The enrighment of elemental contents above background amounts in these samples can be importatn clue to the presence of a potential mineral deposit. These geochemical investigations are of part of an intergrated mineral resource investigation of the Bunk Robinson Peak and Whitmire Canyon Roadless Areas that also include geologic mapping (Hayes, 1982) and an evaluation of mineral resource potential (Hayes and others, in press).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1425C","usgsCitation":"Watts, K., Hassemer, J.R., and Day, G.W., 1983, Geochemical maps of Bunk Robinson Peak and Whitmire Canyon Roadless Areas, Hidalgo County, New Mexico, and Cochise County, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1425, 51.25 x 30.51 inches, https://doi.org/10.3133/mf1425C.","productDescription":"51.25 x 30.51 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1425C.PNG"},{"id":327550,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1425-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"Arizona, New Mexico","county":"Cochise, Hidalgo","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.08333333333333,31.333333333333332 ], [ -109.08333333333333,31.583333333333332 ], [ -109,31.583333333333332 ], [ -109,31.333333333333332 ], [ -109.08333333333333,31.333333333333332 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae09e","contributors":{"authors":[{"text":"Watts, Kenneth C.","contributorId":101180,"corporation":false,"usgs":true,"family":"Watts","given":"Kenneth C.","affiliations":[],"preferred":false,"id":265064,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hassemer, Jerry R.","contributorId":173451,"corporation":false,"usgs":false,"family":"Hassemer","given":"Jerry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":265063,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Day, Gordon W.","contributorId":21520,"corporation":false,"usgs":true,"family":"Day","given":"Gordon","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265065,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":60918,"text":"mf1507B - 1983 - Mineral resource potential map of the Sky Lakes Roadless Area and Mountain Lakes Wilderness, Jackson and Klamath counties, Oregon","interactions":[],"lastModifiedDate":"2012-02-10T00:10:22","indexId":"mf1507B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1507","chapter":"B","title":"Mineral resource potential map of the Sky Lakes Roadless Area and Mountain Lakes Wilderness, Jackson and Klamath counties, Oregon","language":"ENGLISH","doi":"10.3133/mf1507B","usgsCitation":"Smith, J., Benham, J.R., and Johnson, F.L., 1983, Mineral resource potential map of the Sky Lakes Roadless Area and Mountain Lakes Wilderness, Jackson and Klamath counties, Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1507, 1 map ;95 x 55 cm., on sheet 114 x 91 cm. folded in envelope 25 x 32 cm. +1 pamphlet (6 p. : maps ; 28 cm.), https://doi.org/10.3133/mf1507B.","productDescription":"1 map ;95 x 55 cm., on sheet 114 x 91 cm. folded in envelope 25 x 32 cm. +1 pamphlet (6 p. : maps ; 28 cm.)","costCenters":[],"links":[{"id":105938,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7299.htm","linkFileType":{"id":5,"text":"html"},"description":"7299"},{"id":183216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1983/1507b/report-thumb.jpg"},{"id":88892,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1983/1507b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88893,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1983/1507b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.33333333333333,42.333333333333336 ], [ -122.33333333333333,42.75 ], [ -122.08333333333333,42.75 ], [ -122.08333333333333,42.333333333333336 ], [ -122.33333333333333,42.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f7f76","contributors":{"authors":[{"text":"Smith, James G.","contributorId":44534,"corporation":false,"usgs":true,"family":"Smith","given":"James G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":264615,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benham, J. R.","contributorId":81934,"corporation":false,"usgs":true,"family":"Benham","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":264616,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, F. L.","contributorId":28236,"corporation":false,"usgs":true,"family":"Johnson","given":"F.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":264614,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8459,"text":"ofr83405 - 1983 - Major, minor, and trace elements in samples from the Wheeler Wilderness Study Area, Colorado, as determined by inductively coupled argon plasma-atomic emission spectrometry","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr83405","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-405","title":"Major, minor, and trace elements in samples from the Wheeler Wilderness Study Area, Colorado, as determined by inductively coupled argon plasma-atomic emission spectrometry","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83405","usgsCitation":"Crock, J., Raymond, W.H., and Lichte, F., 1983, Major, minor, and trace elements in samples from the Wheeler Wilderness Study Area, Colorado, as determined by inductively coupled argon plasma-atomic emission spectrometry: U.S. Geological Survey Open-File Report 83-405, 26 p.  ;28 cm., https://doi.org/10.3133/ofr83405.","productDescription":"26 p.  ;28 cm.","costCenters":[],"links":[{"id":140582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0405/report-thumb.jpg"},{"id":36028,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0405/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64981c","contributors":{"authors":[{"text":"Crock, J.G.","contributorId":58236,"corporation":false,"usgs":true,"family":"Crock","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":157756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raymond, William H.","contributorId":48555,"corporation":false,"usgs":true,"family":"Raymond","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":157755,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lichte, F.E.","contributorId":99108,"corporation":false,"usgs":true,"family":"Lichte","given":"F.E.","affiliations":[],"preferred":false,"id":157757,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61103,"text":"mf1558A - 1983 - Mineral resource potential and geologic map of the Wet Beaver Roadless Area, Coconino and Yavapai counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:10:48","indexId":"mf1558A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1558","chapter":"A","title":"Mineral resource potential and geologic map of the Wet Beaver Roadless Area, Coconino and Yavapai counties, Arizona","language":"ENGLISH","doi":"10.3133/mf1558A","usgsCitation":"Ulrich, G., Bielski, A.M., and Bywaters, J., 1983, Mineral resource potential and geologic map of the Wet Beaver Roadless Area, Coconino and Yavapai counties, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1558, 1 map ;32 x 74 cm., folded in envelope 25 x 32 cm. +1 pamphlet (5 p. : maps ; 28 cm.), https://doi.org/10.3133/mf1558A.","productDescription":"1 map ;32 x 74 cm., folded in envelope 25 x 32 cm. +1 pamphlet (5 p. : maps ; 28 cm.)","costCenters":[],"links":[{"id":106159,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7634.htm","linkFileType":{"id":5,"text":"html"},"description":"7634"},{"id":186850,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1983/1558a/report-thumb.jpg"},{"id":88917,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1983/1558a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88918,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1983/1558a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.66666666666667,34.65 ], [ -111.66666666666667,34.7 ], [ -111.5,34.7 ], [ -111.5,34.65 ], [ -111.66666666666667,34.65 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6834c9","contributors":{"authors":[{"text":"Ulrich, G. E.","contributorId":88737,"corporation":false,"usgs":true,"family":"Ulrich","given":"G. E.","affiliations":[],"preferred":false,"id":264993,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bielski, A. M.","contributorId":67534,"corporation":false,"usgs":true,"family":"Bielski","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":264992,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bywaters, J.S.","contributorId":55909,"corporation":false,"usgs":true,"family":"Bywaters","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":264991,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26159,"text":"wri834077 - 1983 - A preliminary assessment of the hydrologic characteristics of the James River in South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri834077","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4077","title":"A preliminary assessment of the hydrologic characteristics of the James River in South Dakota","docAbstract":"The James River in South Dakota has very restricted channel capacities within the Lake Dakota Plain. Channel capacities in Brown County are as little as 200 cubic feet per second, and spring flooding can be expected on an average of every other year. The river has potential for extended periods of flooding an average of once in 10 years. Extended periods of no flow during late-summer and winter also can be expected. Excluding flows of a very large magnitude, average travel time between Columbia and Scotland (a distance of 382 river miles) is estimated to be 25-30 days for most flows. The upstream reach of the James River within the Lake Dakota Plain generally loses discharge with distance whereas the downstream reach generally gains discharge with distance. Ground water - surface water interaction does not appear to be significant along upstream reaches of the James River. Some interaction, although not quantified, does occur in Hanson, Davison, and Yankton Counties. Sand Lake National Wildlife Refuge, located just downsteam from the State line and containing Sand and Mud Lakes (combined capacity = 24,600 acre-feet), is a major source of water loss between LaMoure, N. Dak. and Columbia, S. Dak. Gross evaporation losses from the lakes during 1969-81 is estimated to have been slightly more than 29,000 acre-feet per year. Unaccounted-for losses in the lake system are estimated to have been slightly more than 19,000 acre-feet per year. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834077","usgsCitation":"Benson, R., 1983, A preliminary assessment of the hydrologic characteristics of the James River in South Dakota: U.S. Geological Survey Water-Resources Investigations Report 83-4077, viii, 122 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834077.","productDescription":"viii, 122 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4077/report-thumb.jpg"},{"id":54953,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4077/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b88","contributors":{"authors":[{"text":"Benson, R.D.","contributorId":23955,"corporation":false,"usgs":true,"family":"Benson","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":195919,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2838,"text":"wsp2249 - 1983 - An evaluation of trends in the acidity of precipitation and the related acidification of surface water in North America","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp2249","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2249","title":"An evaluation of trends in the acidity of precipitation and the related acidification of surface water in North America","docAbstract":"The acidity of precipitation in the Northeastern United States and Southeastern Canada has increased in the past, probably as a result of anthropogenic emissions. The increase in New England and New York occurred primarily before the mid-1950's. Since the mid1960's, there has been no significant change in the acidity of precipitation in this region; however, sulfate concentrations have decreased and nitrate concentrations may have increased. The time of initial acidification in Southeastern Canada is not known because of a lack of historical data. In the Southeastern United States, the evaluation of whether precipitation has been acidified is complicated by meager data. The available data show that precipitation is more acidic than would be expected for sites unaffected by anthropogenic emissions. In addition, comparison of recent data with the meager historical data suggests, but does not unambiguously prove, increased acidification since the 1950's. In the Western United States, available data indicate that precipitation at individual sites has been acidified by anthropogenic emissions. The acidification generally has been attributable to localized sources, and the time of initial acidification is undefined. \r\n\r\nAcidification of lakes and streams in the Northeastern United States has occurred in a time frame compatible with the hypothesis that acidification of precipitation was the cause. The acidification of surface waters appears to have occurred before the mid- to late 1960's. In Southeastern Canada, the best-documented cases of acidified lakes point to localized sources of acidic emissions as the cause. Sparse evidence of recent regional acidification of lakes and streams exists, but evidence for acidification of precipitation as the cause is largely lacking. In the Southeastern United States, most data on acidification of surface waters are ambiguous, and in the West, most of the data reflect local conditions. However, recent analysis of a national network of remote stream sampling stations indicates that, since the mid- to late 1960's, sulfate concentrations have increased in the Southeast and the West, with a concurrent decrease in alkalinity. Additional work is needed to test the hypothesis that regional acidification of surface waters is occurring in the Southeastern and Western United States.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2249","usgsCitation":"Turk, J.T., 1983, An evaluation of trends in the acidity of precipitation and the related acidification of surface water in North America: U.S. Geological Survey Water Supply Paper 2249, iii, 18 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2249.","productDescription":"iii, 18 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":138979,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2249/report-thumb.jpg"},{"id":29404,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2249/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db6848a4","contributors":{"authors":[{"text":"Turk, John T.","contributorId":53363,"corporation":false,"usgs":true,"family":"Turk","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":145880,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60917,"text":"mf1507A - 1983 - Geologic map of the Sky Lakes roadless area and Mountain Lakes Wilderness, Jackson and Klamath counties, Oregon","interactions":[],"lastModifiedDate":"2012-02-10T00:10:22","indexId":"mf1507A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1507","chapter":"A","title":"Geologic map of the Sky Lakes roadless area and Mountain Lakes Wilderness, Jackson and Klamath counties, Oregon","language":"ENGLISH","doi":"10.3133/mf1507A","usgsCitation":"Smith, J., 1983, Geologic map of the Sky Lakes roadless area and Mountain Lakes Wilderness, Jackson and Klamath counties, Oregon: U.S. Geological Survey Miscellaneous Field Studies Map 1507, 1 map ;95 x 54 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1507A.","productDescription":"1 map ;95 x 54 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":105937,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7298.htm","linkFileType":{"id":5,"text":"html"},"description":"7298"},{"id":183215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.33333333333333,42.333333333333336 ], [ -122.33333333333333,42.75 ], [ -122.08333333333333,42.75 ], [ -122.08333333333333,42.333333333333336 ], [ -122.33333333333333,42.333333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a75a","contributors":{"authors":[{"text":"Smith, James G.","contributorId":44534,"corporation":false,"usgs":true,"family":"Smith","given":"James G.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":264613,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25056,"text":"pp1296 - 1983 - Evidence of floods on the Potomac River from anatomical abnormalities in the wood of flood-plain trees","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"pp1296","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"1296","title":"Evidence of floods on the Potomac River from anatomical abnormalities in the wood of flood-plain trees","docAbstract":"Ash trees along the Potomac River flood plain near Washington, D.C., were studied to determine changes in wood anatomy related to flood damage, and anomalous growth was compared to flood records for April 15 to August 31, 1930-79. Collectively, anatomical evidence was detected for 33 of the 34 growing-season floods during the study period. Evidence of 12 floods prior to 1930 was also noted, including catastrophic ones in 1889 and 1924. Trees damaged after the transition from earlywood to latewood growth typically formed ' flood rings ' of enlarged vessels within the latewood zone. Trees damaged near the beginning of the growth year developed flood rings within, or contiguous with, the earlywood. Both patterns are assumed to have developed when flood-damaged trees produced a second crop of leaves. Trees damaged by high-magnitude floods developed well formed flood rings along the entire height and around the entire circumference of the stem. Small floods were generally associated wtih diffuse or discontinuous anomalies restricted to stem apices. Frequency of flood rings was positively related to flood magnitude, and time of flood generation during the tree-growth season was estimated from the radial position of anomalous growth relative to annual ring width. Reconstructing tree heights in a year of flood-ring formation gives a minimum stage estimate along local stream reaches. Some trees provided evidence of numerous floods. Those with the greatest number of flood rings grew on frequently flooded surfaces subject to flood-flow velocities of at least 1 m/s, and more typically greater than 2 m/s. Tree size, more than age, was related to flood-ring formation. Trees kept small by frequent flood damage had more flood rings than taller trees of comparable age. (USGS)","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/pp1296","usgsCitation":"Yanosky, T.M., 1983, Evidence of floods on the Potomac River from anatomical abnormalities in the wood of flood-plain trees: U.S. Geological Survey Professional Paper 1296, 42 p., https://doi.org/10.3133/pp1296.","productDescription":"42 p.","costCenters":[],"links":[{"id":123451,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1296/report-thumb.jpg"},{"id":54071,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1296/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672ce","contributors":{"authors":[{"text":"Yanosky, Thomas M.","contributorId":40589,"corporation":false,"usgs":true,"family":"Yanosky","given":"Thomas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193143,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57342,"text":"wdrID822 - 1983 - Water Resources Data Idaho, Water Year 1982: Volume 2. Upper Columbia River Basin and Snake River Basin below King Hill","interactions":[],"lastModifiedDate":"2012-02-02T00:12:20","indexId":"wdrID822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ID-82-2","title":"Water Resources Data Idaho, Water Year 1982: Volume 2. Upper Columbia River Basin and Snake River Basin below King Hill","language":"ENGLISH","doi":"10.3133/wdrID822","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Water Resources Data Idaho, Water Year 1982: Volume 2. Upper Columbia River Basin and Snake River Basin below King Hill: U.S. Geological Survey Water Data Report ID-82-2, 292 p., 22 Fig., https://doi.org/10.3133/wdrID822.","productDescription":"292 p., 22 Fig.","costCenters":[],"links":[{"id":185251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd285","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":533063,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25885,"text":"wri824018 - 1983 - Determination of dissolved aluminum in water samples","interactions":[],"lastModifiedDate":"2012-02-02T00:08:38","indexId":"wri824018","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"82-4018","title":"Determination of dissolved aluminum in water samples","docAbstract":"A technique has been modified for determination of a wide range of concentrations of dissolved aluminum (Al) in water and has been tested. In this technique, aluminum is complexed with 8-hydroxyquinoline at pH 8.3 to minimize interferences, then extracted with methyl isobutyl ketone (MIBK). The extract is analyzed colorimetrically at 395 nm. This technique is used to analyze two forms of monomeric Al, nonlabile (organic complexes) and labile (free, Al, Al sulfate, fluoride and hydroxide complexes). A detection limit 2 ug/L is possible with 25-ml samples and 10-ml extracts. The detection limit can be decreased by increasing the volume of the sample and (or) decreasing the volume of the methyl isobutyl ketone extract. The analytical uncertainty of this method is approximately + or - 5 percent. The standard addition technique provides a recovery test for this technique and ensures precision in samples of low Al concentrations. The average percentage recovery of the added Al plus the amount originally present was 99 percent. Data obtained from analyses of filtered standard solutions indicated that Al is adsorbed on various types of filters. However, the relationship between Al concentrations and adsorption remains linear. A test on standard solutions also indicated that Al is not adsorbed on nitric acid-washed polyethylene and polypropylene bottle wells. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824018","usgsCitation":"Afifi, A., 1983, Determination of dissolved aluminum in water samples: U.S. Geological Survey Water-Resources Investigations Report 82-4018, iii, 16 p. :ill. ;28 cm., https://doi.org/10.3133/wri824018.","productDescription":"iii, 16 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4018/report-thumb.jpg"},{"id":54647,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4018/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6677f2","contributors":{"authors":[{"text":"Afifi, A.A.","contributorId":98768,"corporation":false,"usgs":true,"family":"Afifi","given":"A.A.","email":"","affiliations":[],"preferred":false,"id":195423,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":21079,"text":"ofr83259 - 1983 - Influence of climate on progressive hillslope failure in Redwood Creek Valley, northwestern California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:46","indexId":"ofr83259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"83-259","title":"Influence of climate on progressive hillslope failure in Redwood Creek Valley, northwestern California","docAbstract":"Both creep and earthflow processes control hillslope erosion over large parts of the Redwood Creek basin. The type of process and displacement rates are largely dependent on underlying bedrock type and precipitation input. Progressive creep with rates ranging from 1.0 to 2.5 mm/a dominates on slopes west of the Grogen fault underlain by sheared and foliated schists. Movement appears to respond primarily to annual increments of precipitation. Complex earthflows occur predominantly on slopes east of the Grogen fault underlain by sheared graywacke and mudstone. Movement rates range from 3.0 to 131.0 mm/a and characteristically display dominant rainy season movement.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nOpen-File Services Section [distributor],","doi":"10.3133/ofr83259","usgsCitation":"Swanston, D.N., Ziemer, R.R., and Janda, R.J., 1983, Influence of climate on progressive hillslope failure in Redwood Creek Valley, northwestern California: U.S. Geological Survey Open-File Report 83-259, 49 p. :ill. ;28 cm., https://doi.org/10.3133/ofr83259.","productDescription":"49 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":154078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0259/report-thumb.jpg"},{"id":50673,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0259/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee7bd","contributors":{"authors":[{"text":"Swanston, Douglas N.","contributorId":81930,"corporation":false,"usgs":true,"family":"Swanston","given":"Douglas","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":183805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ziemer, Robert Ruhl","contributorId":9290,"corporation":false,"usgs":true,"family":"Ziemer","given":"Robert","email":"","middleInitial":"Ruhl","affiliations":[],"preferred":false,"id":183803,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Janda, Richard J.","contributorId":13235,"corporation":false,"usgs":true,"family":"Janda","given":"Richard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":183804,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26126,"text":"wri834141 - 1983 - Floods in Kansas City, Missouri and vicinity, August 12-13, 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri834141","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4141","title":"Floods in Kansas City, Missouri and vicinity, August 12-13, 1982","docAbstract":"On August 12-13, 1982, a nearly stationary weather front in the vicinity of Kansas City, MO, produced intense thunderstorms. Excessive rainfall (12.6 inches in Raytown, MO) caused flash flooding during the nighttime and early daylight hours. Four deaths and damages unofficially estimated in excess of $30 million, occurred in the three-county area of Jackson, Cass, and Clay counties. Peak discharges were determined at 12 current or discontinued streamflow-gaging stations and 17 miscellaneous sites. Flood peaks and volumes at many locations exceeded estimated 100-year recurrence-interval floods and equaled or exceeded the 1977 floods in some drainage basins. Significant flooding occurred in the Blue, East Fork Little Blue, and Little Blue River basins and in the Rock, Wilkerson, Sni-A-Bar, Shoal, and Big Creek drainage basins. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834141","usgsCitation":"Becker, L., Alexander, T., and Waite, L., 1983, Floods in Kansas City, Missouri and vicinity, August 12-13, 1982: U.S. Geological Survey Water-Resources Investigations Report 83-4141, iv, 35 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834141.","productDescription":"iv, 35 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4141/report-thumb.jpg"},{"id":54926,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4141/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e498de4b07f02db5b060e","contributors":{"authors":[{"text":"Becker, L.D.","contributorId":84797,"corporation":false,"usgs":true,"family":"Becker","given":"L.D.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":195862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, T.W.","contributorId":9680,"corporation":false,"usgs":true,"family":"Alexander","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":195860,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waite, L.A.","contributorId":40995,"corporation":false,"usgs":true,"family":"Waite","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":195861,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":57274,"text":"wdrMT822 - 1983 - Water resources data, Montana, water year 1982, volume 2: Columbia River Basin","interactions":[],"lastModifiedDate":"2019-10-01T15:52:37","indexId":"wdrMT822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MT-82-2","title":"Water resources data, Montana, water year 1982, volume 2: Columbia River Basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U. S. 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,{"id":64617,"text":"i1508A - 1983 - Shaded relief, oblique view map, vicinity of Going-to-the-Sun Road, Glacier National Park, Montana","interactions":[],"lastModifiedDate":"2025-08-04T19:46:51.205984","indexId":"i1508A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1508","chapter":"A","title":"Shaded relief, oblique view map, vicinity of Going-to-the-Sun Road, Glacier National Park, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i1508A","usgsCitation":"Isom, A.L., Raup, O.B., Brumley, D.A., and Binder, S.G., 1983, Shaded relief, oblique view map, vicinity of Going-to-the-Sun Road, Glacier National Park, Montana: U.S. Geological Survey IMAP 1508, 1 Plate: 24.88 x 17.26 inches, https://doi.org/10.3133/i1508A.","productDescription":"1 Plate: 24.88 x 17.26 inches","costCenters":[],"links":[{"id":493484,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9269.htm","linkFileType":{"id":5,"text":"html"}},{"id":91410,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1508a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":187078,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"65000","country":"United States","state":"Montana","otherGeospatial":"Glacier National Park, Going-to-the-Sun Road","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -114,\n              48.75\n            ],\n            [\n              -114,\n              48.333\n            ],\n            [\n              -113.5,\n              48.333\n            ],\n            [\n              -113.5,\n              48.75\n            ],\n            [\n              -114,\n              48.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4879","contributors":{"authors":[{"text":"Isom, A. L.","contributorId":7777,"corporation":false,"usgs":true,"family":"Isom","given":"A.","middleInitial":"L.","affiliations":[],"preferred":false,"id":271756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raup, O. B.","contributorId":19175,"corporation":false,"usgs":true,"family":"Raup","given":"O.","middleInitial":"B.","affiliations":[],"preferred":false,"id":271758,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brumley, D. A.","contributorId":15282,"corporation":false,"usgs":true,"family":"Brumley","given":"D.","middleInitial":"A.","affiliations":[],"preferred":false,"id":271757,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Binder, S. G.","contributorId":73280,"corporation":false,"usgs":true,"family":"Binder","given":"S.","middleInitial":"G.","affiliations":[],"preferred":false,"id":271759,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25940,"text":"wri834196 - 1983 - Water quality of Lake Arlington on Village Creek, north-central Texas; 1973 to 1981","interactions":[],"lastModifiedDate":"2022-10-31T21:40:25.308282","indexId":"wri834196","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"83-4196","title":"Water quality of Lake Arlington on Village Creek, north-central Texas; 1973 to 1981","docAbstract":"<p>Water in Lake Arlington on Village Creek in north-central Texas had volume-weighted average concentrations of less than 240 milligrams per liter of dissolved solids, less than 30 milligrams per liter of dissolved chloride, and less than 40 milligrams per liter of dissolved sulfate between January 29, 1973, and August 20, 1981. The water was moderately hard (hardness greater than 60 but less than 120 milligrams per liter as calcium carbonate). The concentrations of each of these constituents were usually greatest during winter, especially during the first few years of the study, but decreased significantly as discharges of municipal wastes were systematically and progressively diverted to treatment facilities downstream from the reservoir.</p>\n<p>Thermal stratification in Lake Arlington usually begins during March or April and persists until October. Thermal stratification has resulted in significant seasonal and areal variations in the concentration of dissolved oxygen, dissolved iron, dissolved manganese, total inorganic nitrogen, and total phosphorus. Oxygen utilized in the decay of organic matter is not replenished during periods of summer stagnation, and water below depths of 30 to 40 feet usually contains less than 2 milligrams per liter of dissolved oxygen during stagnation. Even though heated effluent from an electrical generating plant is returned to the reservoir at site GC and causes an elevation of water temperature, average dissolved oxygen levels at this site are not significantly different from levels at other sites.</p>\n<p>During summer stagnation, reducing conditions result in the dissolution of iron and manganese from bottom deposits at deep sites in the reservoir. At site AQ, a deep site near Arlington Dam, dissolved iron concentrations in water near the bottom during summer stagnation ranged from less than 10 to 1,100 micrograms per liter and averaged about 640 micrograms per liter. Dissolved manganese concentrations near the bottom at site AC during summer staynation ranged from 20 to 2,700 micrograms per liter and averaged about 1,500 micrograms per liter. The concentrations of dissolved iron and dissolved manganese in water throughout the reservoir during winter circulation and in water near the reservoir surface during summer stagnation averaged less than 50 micrograms per liter.</p>\n<p>Seasonal temperature and dissolved oxygen cycles resulted in the recycling of dissolved iron and dissolved manganese between the water and bottom sediments. However, no significant accumulation of these constituents within the reservoir was detected during the study.</p>\n<p>The concentrations of total inorganic nitrogen and total phosphorus are greatest during summer stagnation in water near the bottom at deep sites. At site AC during the summer, the concentrations of total inorganic nitrogen in the hypolimnion averaged about 0.9 milligram per liter, and the concentration of total phosphorus near the bottom averaged about 0.2 milligram per liter. The concentrations of total inorganic nitrogen in the epilimnion at site AC averaged about 0.1 milligram per liter; the concentrations of total phosphorus averaged less than 0.1 milligram per liter.</p>\n<p>The densities and composition of algal populations varied seasonally. At site AC, total algae counts ranged from 200 to 240,000 cells per mi Hi liter and averaged about 50,000 cells per milliliter. At site FC, total algae counts ranged from 1,000 to 290,000 cells per milliliter and averaged about 56,000 cells per milliliter. Algal densities were greatest during the summer with blue-green algae being the predominant phyla.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/wri834196","usgsCitation":"Andrews, F.L., and Gibbons, W.J., 1983, Water quality of Lake Arlington on Village Creek, north-central Texas; 1973 to 1981: U.S. Geological Survey Water-Resources Investigations Report 83-4196, vi, 126 p., https://doi.org/10.3133/wri834196.","productDescription":"vi, 126 p.","numberOfPages":"132","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":408941,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35843.htm","linkFileType":{"id":5,"text":"html"}},{"id":157166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4196/report-thumb.jpg"},{"id":54696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4196/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Lake Arlington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -97.24342346191406,\n              32.66278938534136\n            ],\n            [\n              -97.24342346191406,\n              32.73646168396554\n            ],\n            [\n              -97.17716217041014,\n              32.73646168396554\n            ],\n            [\n              -97.17716217041014,\n              32.66278938534136\n            ],\n            [\n              -97.24342346191406,\n              32.66278938534136\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa982","contributors":{"authors":[{"text":"Andrews, Freeman L.","contributorId":91486,"corporation":false,"usgs":true,"family":"Andrews","given":"Freeman","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195518,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gibbons, Willard J.","contributorId":173568,"corporation":false,"usgs":false,"family":"Gibbons","given":"Willard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":195517,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57296,"text":"wdrAL821 - 1983 - Water resources data, Alabama, water year 1982","interactions":[],"lastModifiedDate":"2023-03-06T20:23:55.707691","indexId":"wdrAL821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AL-82-1","title":"Water resources data, Alabama, water year 1982","docAbstract":"<p>Water resources data for the 1982 water year for Alabama consist 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 85 gaging stations; stage only for 16 gaging stations, stage and contents for 12 lakes and reservoirs; water quality for 67 gaging stations and 76 wells, and water levels for 52 observation wells. Also included are 10 crest-stage partial-record stations, 8 flood hydrograph partial-record stations and 91 water-quality 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 and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Alabama.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAL821","collaboration":"Prepared in cooperation with the Geological Survey of Alabama, the Alabama Highway Department, and with other State, municipal, and Federal agencies","usgsCitation":"Rollins, H., Sedberry, F., Ming, E., and Giles, I., 1983, Water resources data, Alabama, water year 1982: U.S. Geological Survey Water Data Report AL-82-1, x, 467 p., https://doi.org/10.3133/wdrAL821.","productDescription":"x, 467 p.","costCenters":[],"links":[{"id":413737,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/al-82-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":181986,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/al-82-1/report-thumb.jpg"}],"country":"United 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,{"id":57273,"text":"wdrMT821 - 1983 - Water resources data, Montana, water year 1982: Volume 1. Hudson Bay and Missouri River Basins","interactions":[],"lastModifiedDate":"2020-08-21T18:12:25.596237","indexId":"wdrMT821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MT-82-1","title":"Water resources data, Montana, water year 1982: Volume 1. Hudson Bay and Missouri River Basins","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrMT821","usgsCitation":"Shields, R., Knapton, J.R., White, M.K., Jacobson, M., and Kasman, M., 1983, Water resources data, Montana, water year 1982: Volume 1. 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