{"pageNumber":"5741","pageRowStart":"143500","pageSize":"25","recordCount":165653,"records":[{"id":70038247,"text":"70038247 - 1970 - Hydrogeologic data for the lower Housatonic River basin, Connecticut","interactions":[],"lastModifiedDate":"2014-04-09T12:39:42","indexId":"70038247","displayToPublicDate":"2012-04-22T15:28:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"20","title":"Hydrogeologic data for the lower Housatonic River basin, Connecticut","docAbstract":"This report contains hydrologic and geologic data collected for an investigation of the lower Housatonic River basin by the U.S. Geological Survey in financial cooperation with the Connecticut Water Resources Commission. The report also summarizes data that are available in other publications. The towns within the 557 square mile area of the basin in western Connecticut include all of Beacon Falls, Middlebury, Naugatuck, Oxford, Seymour, Thomaston, Waterbury, Watertown, and Woodbury; and parts of Ansonia, Bethany, Bethlehem, Bristol, Burlington, Cheshire, Derby, Easton, Goshen, Narwinton, Litchfield, Milford, Monroe, Morris, New Hartford, Newtown, Norfolk, Orange, Plymouth, Prospect, Roxbury, Shelton, Southbury, Stratford, Torrington, Trumbull, Washington, Winchester, Wolcott, and Woodbridge. The factual information on the following pages was the basis for a companion interpretive report, Connecticut Water Resources Bulletin No. 19 (Wilson, W. E., and others, in preparation, 1970). The basic-data report can be used alone for detailed information needed in planning water resources development at specific sites or it can be used to supplement the interpretive report.\nData were collected for this investigation from 1965 to 1967. Water\nlevels measured in wells as part of this investigation were published in\nConnecticut Water Resources Bulletin No. 7 (Meikle and Baker, 1965) and No. 13\n(Meikle, 1967) with water-level data from other wells throughout the State.\nPublications containing relevant ground-water information are listed on page\nthose concerned with streamflow are on page 5 and those on quality of water,\nare on page 6.\nThe locations of sites at which data were collected are shown on plate A\nin the back pocket of this report. Data presented here were collected by the\nU.S. Geological Survey unless otherwise noted.","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Water Resource Commission","usgsCitation":"Grossman, I., and Wilson, W.E., 1970, Hydrogeologic data for the lower Housatonic River basin, Connecticut: Connecticut Water Resources Bulletin 20, Report: 50 p.; 3 Plates: 28.80 x 46.56 inches and smaller.","productDescription":"Report: 50 p.; 3 Plates: 28.80 x 46.56 inches and smaller","numberOfPages":"55","costCenters":[],"links":[{"id":258807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0020/report.pdf","size":"2300","linkFileType":{"id":1,"text":"pdf"}},{"id":258808,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0020/report-thumb.jpg"},{"id":285988,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038247/plate-a-3.pdf"},{"id":285986,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038247/plate-a-1.pdf"},{"id":285987,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038247/plate-a-2.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Housatonic River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.258333,41.5 ], [ -73.258333,41.883333 ], [ -72.916667,41.883333 ], [ -72.916667,41.5 ], [ -73.258333,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a33b6e4b0c8380cd5f1dc","contributors":{"authors":[{"text":"Grossman, I.G.","contributorId":52574,"corporation":false,"usgs":true,"family":"Grossman","given":"I.G.","email":"","affiliations":[],"preferred":false,"id":463730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, William E.","contributorId":46478,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463729,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038238,"text":"70038238 - 1970 - Water resources inventory of Connecticut Part 4: Southwestern coastal river basins","interactions":[],"lastModifiedDate":"2014-03-28T09:53:16","indexId":"70038238","displayToPublicDate":"2012-04-22T11:25:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"17","title":"Water resources inventory of Connecticut Part 4: Southwestern coastal river basins","docAbstract":"The 44O square miles of the southwestern coastal river basins (394 square miles of which are in Connecticut) yield about 183 billion gallons, or 23.9 inches of runoff during an average year. This amount of runoff is almost entirely derived from precipitation falling on the basins, and is eventually discharged into Long Island Sound. In 1965, some streamflow originated from 5.5 billion gallons of water imported from the Housatonic River basin. Mean annual runoff is generally an index of the water potentially available for development; however, in the basins, large-scale impoundment and diversion of streamflow has preempted most of the surface water available.","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared in cooperation with the Connecticut Water Resources Commission","usgsCitation":"Ryder, R.B., Cervione, M.A., Thomas, C.E., and Thomas, M.P., 1970, Water resources inventory of Connecticut Part 4: Southwestern coastal river basins: Connecticut Water Resources Bulletin 17, ix, 49 p.; Abbreviations; Glossary; Plate A: 24.57 x 23.68 inches; Plate B: 24.20 x 22.86 inches; Plate C: 24.20 x 24.05 inches.","productDescription":"ix, 49 p.; Abbreviations; Glossary; Plate A: 24.57 x 23.68 inches; Plate B: 24.20 x 22.86 inches; Plate C: 24.20 x 24.05 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":258798,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ctwrb/0017/plate-a.pdf","size":"7110","linkFileType":{"id":1,"text":"pdf"}},{"id":258799,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ctwrb/0017/plate-b.pdf","size":"7228","linkFileType":{"id":1,"text":"pdf"}},{"id":258800,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ctwrb/0017/plate-c.pdf","size":"7361","linkFileType":{"id":1,"text":"pdf"}},{"id":258801,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0017/report.pdf","size":"16969","linkFileType":{"id":1,"text":"pdf"}},{"id":258802,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0017/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Southwestern Coastal River Basins","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.75,40.93333333333333 ], [ -73.75,41.38333333333333 ], [ -73.1,41.38333333333333 ], [ -73.1,40.93333333333333 ], [ -73.75,40.93333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb7ae4b08c986b32d68d","contributors":{"authors":[{"text":"Ryder, Robert B. rryder@usgs.gov","contributorId":68294,"corporation":false,"usgs":true,"family":"Ryder","given":"Robert","email":"rryder@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":463716,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cervione, Michael A. Jr.","contributorId":23988,"corporation":false,"usgs":true,"family":"Cervione","given":"Michael","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463714,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Chester E. Jr.","contributorId":37182,"corporation":false,"usgs":true,"family":"Thomas","given":"Chester","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463715,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463717,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70006934,"text":"70006934 - 1970 - The effect of anesthetization and urinary bladder catheterization on renal function of rainbow trout","interactions":[],"lastModifiedDate":"2017-05-05T16:36:08","indexId":"70006934","displayToPublicDate":"2012-01-01T19:05:26","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1287,"text":"Comparative Biochemistry and Physiology","active":false,"publicationSubtype":{"id":10}},"title":"The effect of anesthetization and urinary bladder catheterization on renal function of rainbow trout","docAbstract":"1. Rainbow trout were anesthetized with MS-222 (Sandoz) or  methylpentynol and catheterized. Urine was collected at selected intervals up to 48 hr. 2. Effects of MS-222 anesthesia on urine flow and composition were isolated from the stress of catheterization by re-anesthetizing the fish 18 to 20 hr post catheterization. 3. Urine output patterns were similar following MS-222 or methylpentynol anesthesia and catheterization. Highest urine flows were measured 4 to 8 hr post treatment. The highest urine output after re-anesthetization with MS-222 was observed 2 to 4 hr post-anesthesia. 4. Highest concentrations of  Na<sup>2+</sup>, K<sup>+</sup>, Ca<sup>2+</sup>, Cl<sup>-</sup> and inorganic PO<sub>4</sub> in the urine were measured in the first 2 hr after anesthesia and catheterization. 5. Flow rates and chemical composition of urine indicate that \"normal\" renal function is re-established 12 to 24 hr post-treatment.","language":"English","publisher":"Elsevier","doi":"10.1016/0010-406X(70)90029-0","usgsCitation":"Hunn, J.B., and Willford, W., 1970, The effect of anesthetization and urinary bladder catheterization on renal function of rainbow trout: Comparative Biochemistry and Physiology, v. 33, no. 4, p. 805-812, https://doi.org/10.1016/0010-406X(70)90029-0.","productDescription":"8 p.","startPage":"805","endPage":"812","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":258258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bab14e4b08c986b322bde","contributors":{"authors":[{"text":"Hunn, J. B.","contributorId":15133,"corporation":false,"usgs":true,"family":"Hunn","given":"J.","middleInitial":"B.","affiliations":[],"preferred":false,"id":355497,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Willford, W. A.","contributorId":105256,"corporation":false,"usgs":true,"family":"Willford","given":"W. A.","affiliations":[],"preferred":false,"id":355498,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70039100,"text":"70039100 - 1970 - Base-flow study of Suamico River basin, Oconto, Brown, Shawano and Outagamie counties, Wisconsin","interactions":[],"lastModifiedDate":"2012-07-19T01:01:49","indexId":"70039100","displayToPublicDate":"2012-01-01T12:40:38","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":280,"text":"Report","active":false,"publicationSubtype":{"id":4}},"title":"Base-flow study of Suamico River basin, Oconto, Brown, Shawano and Outagamie counties, Wisconsin","docAbstract":"The Suamico River is a gaining stream throughout its entire reach. No loss of water from the streams was noted between any measuring sites. The August 12 measurements were made during base-flow period when flow duration was about 50 to 55 percent (table 2). The August 28 measurements were made during a lower base-flow period when flow duration was about 70 to 80 percent. Flow duration at about 80 percent is more representative of low-flow conditions during the summer.","language":"English","publisher":"Wisconsin Department of Natural Resources","publisherLocation":"Madison, WI","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Devaul, R.W., 1970, Base-flow study of Suamico River basin, Oconto, Brown, Shawano and Outagamie counties, Wisconsin: Report, 7 p.; 1 Plate: 56 x 29 cm.","productDescription":"7 p.; 1 Plate: 56 x 29 cm.","costCenters":[],"links":[{"id":261309,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/othergov/70039100/plate-2.pdf"},{"id":261310,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/othergov/70039100/report.pdf"},{"id":261311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/othergov/70039100/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Wisconsin","city":"Brown;Oconto;Outagamie;Shawano","otherGeospatial":"Suamico River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.33333333333333,44.5 ], [ -88.33333333333333,44.71666666666667 ], [ -88,44.71666666666667 ], [ -88,44.5 ], [ -88.33333333333333,44.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059efd3e4b0c8380cd4a486","contributors":{"authors":[{"text":"Devaul, Robert W.","contributorId":48432,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"W.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":465616,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039099,"text":"70039099 - 1970 - Base-flow study of Little Suamico River basin Oconto, Brown and Shawano counties, Wisconsin","interactions":[],"lastModifiedDate":"2012-07-19T01:01:49","indexId":"70039099","displayToPublicDate":"2012-01-01T12:29:55","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":280,"text":"Report","active":false,"publicationSubtype":{"id":4}},"title":"Base-flow study of Little Suamico River basin Oconto, Brown and Shawano counties, Wisconsin","docAbstract":"The Little Suamico River is a gaining stream throughout its entire reach. No loss of water from the streams was noted between any measuring sites. The August 13 measurements were made during a base-flow period when flow duration was about 50 to 55 percent (table 2). The August 27, 28 measurements were made during a lower base-flow period when flow duration was about 70 to 80 percent. Flow duration at about 80 percent is more representative of low-flow conditions during the summer.","language":"English","publisher":"Wisconsin Department of Natural Resources","publisherLocation":"Madison, WI","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Devaul, R.W., 1970, Base-flow study of Little Suamico River basin Oconto, Brown and Shawano counties, Wisconsin: Report, 7 p.; 1 Plate: 54 x 29 cm.","productDescription":"7 p.; 1 Plate: 54 x 29 cm.","costCenters":[],"links":[{"id":261306,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/othergov/70039099/plate-2.pdf"},{"id":261307,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/othergov/70039099/report.pdf"},{"id":261308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/othergov/70039099/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Wisconsin","county":"Brown;Oconto;Shawano","otherGeospatial":"Little Suamico River;Tibbet Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.33333333333333,44.583333333333336 ], [ -88.33333333333333,44.8 ], [ -87.98333333333333,44.8 ], [ -87.98333333333333,44.583333333333336 ], [ -88.33333333333333,44.583333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059efd3e4b0c8380cd4a483","contributors":{"authors":[{"text":"Devaul, Robert W.","contributorId":48432,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"W.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":465615,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039097,"text":"70039097 - 1970 - Base-flow study of East River basin Brown and Calumet counties, Wisconsin","interactions":[],"lastModifiedDate":"2012-07-19T01:01:49","indexId":"70039097","displayToPublicDate":"2012-01-01T12:17:25","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":280,"text":"Report","active":false,"publicationSubtype":{"id":4}},"title":"Base-flow study of East River basin Brown and Calumet counties, Wisconsin","docAbstract":"Streams in the East River basin gain ground water throughout most of their reaches, however, ground-water pumping of the Green Bay - DePere area may reduce the water being gained by the streams from ground water. The August 13, 14 measurements were made during base-flow period when flow duration was about 50 to 55 percent (table 2). The August 28 measurements were made during a lower base-flow period when flow duration was about 70 to 80 percent. About 80 percent duration is more representative of low-flow conditions during the summer.","language":"English","publisher":"Wisconsin Department of Natural Resources","publisherLocation":"Madison, WI","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Devaul, R.W., 1970, Base-flow study of East River basin Brown and Calumet counties, Wisconsin: Report, 7 p.; 1 Plate: 59 x62 cm.","productDescription":"7 p.; 1 Plate: 59 x62 cm.","costCenters":[],"links":[{"id":261303,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/othergov/70039097/plate-1.pdf"},{"id":261304,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/othergov/70039097/report.pdf"},{"id":261305,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/othergov/70039097/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Wisconsin","county":"Brown;Outagamie","otherGeospatial":"Baird Creek;Bower Creek;East River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.16666666666667,43.166666666666664 ], [ -88.16666666666667,43.583333333333336 ], [ -87.75,43.583333333333336 ], [ -87.75,43.166666666666664 ], [ -88.16666666666667,43.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059efd3e4b0c8380cd4a480","contributors":{"authors":[{"text":"Devaul, Robert W.","contributorId":48432,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"W.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":465611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039096,"text":"70039096 - 1970 - Base-flow study of Duck Creek basin Brown and Outagamie counties, Wisconsin","interactions":[],"lastModifiedDate":"2012-07-19T01:01:49","indexId":"70039096","displayToPublicDate":"2012-01-01T11:49:50","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":280,"text":"Report","active":false,"publicationSubtype":{"id":4}},"title":"Base-flow study of Duck Creek basin Brown and Outagamie counties, Wisconsin","docAbstract":"Streams in the Duck Creek basin gain ground water throughout most of their reaches, however, ground-water pumping of the Green Bay - DePere area may reduce the water being gained by the streams from ground water. The August 11, 12 measurements were made during base-flow period when flow duration was about 50 to 55 percent (table 2), The August 27 measurements were made during a lower base-flow period when flow duration was about 70 to 80 percent. About 80 percent duration is, more representative of low-flow conditions during the summer.","language":"English","publisher":"Wisconsin Department of Natural Resources","publisherLocation":"Madison, WI","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Devaul, R.W., 1970, Base-flow study of Duck Creek basin Brown and Outagamie counties, Wisconsin: Report, 15 p. : map.","productDescription":"15 p. : map","costCenters":[],"links":[{"id":261301,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/othergov/70039096/report.pdf"},{"id":261302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/othergov/70039096/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Wisconsin","county":"Brown;Outagamie","otherGeospatial":"Beaver Dam Creek;Duck Creek;Trout Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.5,43.25 ], [ -88.5,44.666666666666664 ], [ -87.83333333333333,44.666666666666664 ], [ -87.83333333333333,43.25 ], [ -88.5,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059efd3e4b0c8380cd4a47d","contributors":{"authors":[{"text":"Devaul, Robert W.","contributorId":48432,"corporation":false,"usgs":true,"family":"Devaul","given":"Robert","email":"","middleInitial":"W.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":465610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039539,"text":"70039539 - 1970 - Serial publications commonly cited in technical bibliographies of the United States Geological Survey","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039539","displayToPublicDate":"2012-01-01T10:46:05","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Serial publications commonly cited in technical bibliographies of the United States Geological Survey","docAbstract":"A list of serial publications commonly cited by USGS technical bibliographies.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039539","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Serial publications commonly cited in technical bibliographies of the United States Geological Survey, 100 p., https://doi.org/10.3133/70039539.","productDescription":"100 p.","numberOfPages":"102","costCenters":[],"links":[{"id":261664,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039539/report.pdf"},{"id":261665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039539/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8d58e4b08c986b31835a","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":535344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040710,"text":"70040710 - 1970 - Ground-water resources in the eastern Oswego River basin, New York","interactions":[],"lastModifiedDate":"2012-11-13T12:35:16","indexId":"70040710","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":241,"text":"Basin Planning Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"ORB-2","title":"Ground-water resources in the eastern Oswego River basin, New York","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"Kantrowitz, I., 1970, Ground-water resources in the eastern Oswego River basin, New York: Basin Planning Report ORB-2, 129 p.; 6 Plates.","productDescription":"129 p.; 6 Plates","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263104,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a3ba68e4b0855e233c074a","contributors":{"authors":[{"text":"Kantrowitz, I.H.","contributorId":15646,"corporation":false,"usgs":true,"family":"Kantrowitz","given":"I.H.","affiliations":[],"preferred":false,"id":468856,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040754,"text":"70040754 - 1970 - Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics","interactions":[{"subject":{"id":52458,"text":"ofr6547 - 1965 - Time of travel studies, Fall Creek basin, Tompkins County, New York","indexId":"ofr6547","publicationYear":"1965","noYear":false,"title":"Time of travel studies, Fall Creek basin, Tompkins County, New York"},"predicate":"SUPERSEDED_BY","object":{"id":70040754,"text":"70040754 - 1970 - Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics","indexId":"70040754","publicationYear":"1970","noYear":false,"title":"Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics"},"id":1}],"lastModifiedDate":"2017-09-13T18:25:06","indexId":"70040754","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5495,"text":"New York State Department of Environmental Conservation Report of Investigations","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"RI-11","title":"Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"Dunn, B., 1970, Time-of-travel studies in the Fall Creek basin, Tompkins County, New York, including low-flow characteristics: New York State Department of Environmental Conservation Report of Investigations RI-11, 21 p.","productDescription":"21 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263188,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70040754.png"},{"id":274890,"type":{"id":15,"text":"Index Page"},"url":"https://archive.org/details/usgswaterresourcesnewyork-ri_11"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a61d6be4b0d446a665ca0e","contributors":{"authors":[{"text":"Dunn, Bernard","contributorId":61423,"corporation":false,"usgs":true,"family":"Dunn","given":"Bernard","email":"","affiliations":[],"preferred":false,"id":468961,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046327,"text":"wdrNM691 - 1970 - Water resources data for New Mexico, water year 1969; Part 1. Surface water records","interactions":[],"lastModifiedDate":"2013-07-08T10:53:36","indexId":"wdrNM691","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1970","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":"NM-69-1","title":"Water resources data for New Mexico, water year 1969; Part 1. Surface water records","docAbstract":"Surface-water records for the 1969 water year for New Mexico, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report and their locations shown in figures 1, 2. Records for a few pertinent gaging stations in bordering states also are included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of W. E. Hale, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in New Mexico. Through September 30, 1960, the records of discharge and stage of streams and canals and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled Surface Water Supply of the United States.\"\nBeginning with the 1961 water year, surface-water records have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these reports is limited; they are designed primarily for rapid release of data shortly after the end of the water year to meet local needs. The discharge and reservoir storage records for 1961-65 also will be published in a Geological Survey water-supply paper series entitled \"Surface Water Supply of the United States 1961-65.\"","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Santa Fe, NM","doi":"10.3133/wdrNM691","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1970, Water resources data for New Mexico, water year 1969; Part 1. Surface water records: U.S. Geological Survey Water Data Report NM-69-1, 268 p., https://doi.org/10.3133/wdrNM691.","productDescription":"268 p.","costCenters":[],"links":[{"id":273456,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274525,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1969/nm-69/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.052,31.3322 ], [ -109.052,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.052,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300eae4b01368e589e424","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":535537,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042512,"text":"70042512 - 1970 - Biostratigraphy and dolomite porosity trends of the Lisburne Group","interactions":[{"subject":{"id":17993,"text":"ofr6913 - 1969 - Preliminary carbonate lithofacies maps and possible dolomite porosity trends, Mississippian-Pennsylvanian Lisburne Group, North Slope, Alaska","indexId":"ofr6913","publicationYear":"1969","noYear":false,"title":"Preliminary carbonate lithofacies maps and possible dolomite porosity trends, Mississippian-Pennsylvanian Lisburne Group, North Slope, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70042512,"text":"70042512 - 1970 - Biostratigraphy and dolomite porosity trends of the Lisburne Group","indexId":"70042512","publicationYear":"1970","noYear":false,"title":"Biostratigraphy and dolomite porosity trends of the Lisburne Group"},"id":1}],"lastModifiedDate":"2013-01-10T13:40:56","indexId":"70042512","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1970","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Biostratigraphy and dolomite porosity trends of the Lisburne Group","docAbstract":"This preliminary study is based on measured and carefully collected sections of the Lisburne Group (fig. 1, sees. 1-29). The outcrops extend from Cape Lisburne (sec. 1) in the west to Egaksrak River (sec. 29) in northeastern Alaska and are used as the basic building blocks for the carbonate facies maps and the cross section. Lithologic and foraminifera samples were collected at 10-foot intervals and rugose corals were collected within each section where found. The rock material was cut into thin section, and petrographic and microfossil studies were made to determine environments of deposition, facies, diagenetic changes, and microfossil content. Coral collections were studied in thin section.","largerWorkTitle":"Proceedings of the geological seminar on the North Slope of Alaska, 1970","language":"English","publisher":"American Association of Petroleum Geologists","publisherLocation":"Tulsa, OK","usgsCitation":"Armstrong, A.K., and Mamet, B.L., 1970, Biostratigraphy and dolomite porosity trends of the Lisburne Group, chap. <i>of</i> Proceedings of the geological seminar on the North Slope of Alaska, 1970, p. N1-N15.","productDescription":"15 p.","startPage":"N1","endPage":"N15","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":265512,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265511,"type":{"id":11,"text":"Document"},"url":"https://archives.datapages.com/data/pacific/data/028/028001/pdfs/N1.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"Lisburne Group","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.5,51.2 ], [ 172.5,71.4 ], [ -130.0,71.4 ], [ -130.0,51.2 ], [ 172.5,51.2 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4f87e4b0b290850f2c25","contributors":{"authors":[{"text":"Armstrong, Augustus K.","contributorId":68282,"corporation":false,"usgs":true,"family":"Armstrong","given":"Augustus","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":471675,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mamet, Bernard L.","contributorId":32524,"corporation":false,"usgs":true,"family":"Mamet","given":"Bernard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":471674,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70001661,"text":"70001661 - 1970 - Tholeiitic basalt magmatism of Kilauea and Mauna Loa volcanoes of Hawaii","interactions":[],"lastModifiedDate":"2020-11-30T16:18:06.178112","indexId":"70001661","displayToPublicDate":"2010-09-28T23:09:23","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1390,"text":"Die Naturwissenschaften","active":true,"publicationSubtype":{"id":10}},"title":"Tholeiitic basalt magmatism of Kilauea and Mauna Loa volcanoes of Hawaii","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>The primitive magmas of Kilauca and Mauna Loa are generated by partial melting of mantle peridotite at depths of −60 km or more. Results of high-pressure melting experiments indicate that the primitive melt must contain at least 20% MgO in order to have olivine as a liquidus mineral. The least fractionated lavas of both volcanoes have olivine (Fa<sub>13</sub>) on the liquidus at 1 atmosphere, suggesting that the only substance lost from the primitive melt, during a rather rapid ascent to the surface, is olivine. This relation allows the primitive composition to be computed by adding olivine to the composition of an erupted lava until total MgO is at least 20 percent.</p><p>Although roughly similar, historic lavas of the two volcanoes show a consistent difference in composition. The primitive melt of Mauna Loa contains 20% more dissolved orthopyroxene, a high-temperature melting phase in the mantle, and is deficient in elements such as potassium, uranium, and niobium, which presumably occur in minor low-melting phases. Mauna Loa appears to be the older volcano, deriving its magma at higher temperature and greater depth from a more depleted source rock.</p></div></div>","language":"English","publisher":"Springer","doi":"10.1007/BF00600044","issn":"00281042","usgsCitation":"Murata, K.J., 1970, Tholeiitic basalt magmatism of Kilauea and Mauna Loa volcanoes of Hawaii: Die Naturwissenschaften, v. 57, no. 3, p. 108-113, https://doi.org/10.1007/BF00600044.","productDescription":"6 p.","startPage":"108","endPage":"113","costCenters":[],"links":[{"id":203377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kilauea volcano, Mauna Loa volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.29586791992188,\n              19.368158505739146\n            ],\n            [\n              -155.19699096679688,\n              19.368158505739146\n            ],\n            [\n              -155.19699096679688,\n              19.441989391028706\n            ],\n            [\n              -155.29586791992188,\n              19.441989391028706\n            ],\n            [\n              -155.29586791992188,\n              19.368158505739146\n            ]\n          ]\n        ]\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.67489624023438,\n              19.41867799583191\n            ],\n            [\n              -155.53756713867188,\n              19.41867799583191\n            ],\n            [\n              -155.53756713867188,\n              19.536495698592987\n            ],\n            [\n              -155.67489624023438,\n              19.536495698592987\n            ],\n            [\n              -155.67489624023438,\n              19.41867799583191\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"57","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bdaa","contributors":{"authors":[{"text":"Murata, K. J.","contributorId":18759,"corporation":false,"usgs":true,"family":"Murata","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":346810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70001640,"text":"70001640 - 1970 - Relationship between subsidence and volcanic load, Hawaii","interactions":[],"lastModifiedDate":"2020-11-30T16:21:07.621196","indexId":"70001640","displayToPublicDate":"2010-09-28T23:09:22","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"Relationship between subsidence and volcanic load, Hawaii","docAbstract":"<p>A computer analysis of tide-gage records in the northeast Pacific indicates that the active volcanic islands of eastern Hawaii are subsiding at a rate considerably faster than the eustatic rise of sea level. The rate of absolute subsidence increases progressively toward the center of current activity on the Island of Hawaii. Honolulu, Oahu, appears to be stable; Kahului, Maui, is subsiding at 1.7 mm per year; and Hilo, Hawaii, is subsiding at 4.8 mm per year. This subsidence is apparently related to downbowing of the crust throughout a zone 400 km in diameter by the weight of volcanic material added to the crust by active volcanoes, principally Mauna Loa and Kilauea on the Island of Hawaii. The Hawaiian Arch encircles the subsiding zone and may be uplifted by material moving down and outward from the zone of subsidence.</p><p>The annual volume of subsidence is about 270×10<sup>6</sup><span>&nbsp;</span>m<sup>3</sup>, whereas the average annual volume of erupted basalt on the Island of Hawaii (based on historic records back to about 1820) is about 50×10<sup>6</sup><span>&nbsp;</span>m<sup>3</sup>. The great excess of subsidence over volcanic addition cannot be reconciled by isostatic models, and is apparently the result of other processes operating in the volcano and its basement thet are poorly understood. Probably the more important of these processes are intrusions and submarine volcanism, both of which are providing additional unseen load on the volcanoes. Furthermore, the rate of eruption may be uplifted by material moving down and outward from the zone of subsidence may be overestimated due to localized downslope movement of the margins of the islands.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF02596771","issn":"0366483X","usgsCitation":"Moore, J., 1970, Relationship between subsidence and volcanic load, Hawaii: Bulletin Volcanologique, v. 34, no. 2, p. 562-576, https://doi.org/10.1007/BF02596771.","productDescription":"15 p.","startPage":"562","endPage":"576","costCenters":[],"links":[{"id":203458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"34","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c17e","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":346809,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70001637,"text":"70001637 - 1970 - Lead and strontium isotopes in rocks of the Absaroka volcanic field, Wyoming","interactions":[],"lastModifiedDate":"2020-11-30T16:37:46.058763","indexId":"70001637","displayToPublicDate":"2010-09-28T23:09:22","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Lead and strontium isotopes in rocks of the Absaroka volcanic field, Wyoming","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>The Absaroka volcanic field is comprised of predominant andesitic volcaniclastic rocks and less abundant potassium-rich mafic lavas (shoshonites and absarokites). Strontium and lead isotopic variations preclude a simple derivation from an isotopically uniform source: Sr<sup>87</sup>/Sr<sup>86</sup>, 0.7042 to 0.7090; Pb<sup>206</sup>/Pb<sup>204</sup>, 16.31 to 17.30; Pb<sup>208</sup>/Pb<sup>204</sup>, 36.82 to 37.64. We postulate that these rocks were derived from a lower crust or upper mantle which underwent a preferential loss of uranium relative to lead approximately 2800±200 m.y. ago. Variations in lead and strontium isotopic compositions are thought to reflect small inhomogeneities in U/Pb and Rb/Sr ratios in the source.</p></div></div>","language":"English","publisher":"Springer","doi":"10.1007/BF00371979","issn":"00107999","usgsCitation":"Peterman, Z.E., Doe, B.R., and Prostka, H., 1970, Lead and strontium isotopes in rocks of the Absaroka volcanic field, Wyoming: Contributions to Mineralogy and Petrology, v. 27, no. 2, p. 121-130, https://doi.org/10.1007/BF00371979.","productDescription":"10 p.","startPage":"121","endPage":"130","costCenters":[],"links":[{"id":203420,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Absaroka volcanic field","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.93994140625,\n              42.01665183556825\n            ],\n            [\n              -108.720703125,\n              42.01665183556825\n            ],\n            [\n              -108.720703125,\n              43.75522505306928\n            ],\n            [\n              -110.93994140625,\n              43.75522505306928\n            ],\n            [\n              -110.93994140625,\n              42.01665183556825\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"27","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a891c","contributors":{"authors":[{"text":"Peterman, Z. E.","contributorId":63781,"corporation":false,"usgs":true,"family":"Peterman","given":"Z.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":346806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doe, B. R.","contributorId":52173,"corporation":false,"usgs":true,"family":"Doe","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":346805,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Prostka, H.J.","contributorId":31369,"corporation":false,"usgs":true,"family":"Prostka","given":"H.J.","affiliations":[],"preferred":false,"id":346804,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70001625,"text":"70001625 - 1970 - Distribution of rubidium between sodic sanidine and natural silicic liquid","interactions":[],"lastModifiedDate":"2020-11-30T16:47:42.924264","indexId":"70001625","displayToPublicDate":"2010-09-28T23:09:21","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of rubidium between sodic sanidine and natural silicic liquid","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>Phenocrysts of sodic sanidine from twelve upper Cenozoic units of silicic ash-flow tuff and lava from the Western United States contain from 0.25 to 0.45 the Rb present in the associated groundmass materials. The ratios of potassium to rubidium in the sanidines are, on the average, about four times greater than those of the groundmass. Separation of phenocrystic sanidine from salic melts provides an efficient method for raising the Rb content and lowering the K/Rb ratio of the melts, although the amount of differentiation probably is limited by continuous reequilibration of the alkalis between crystal and liquid phases through ion exchange. Syenites of cumulate origin will have appreciably lower Rb contents and higher K/Rb ratios than the melts from which they precipitated. Available data on the distribution of Rb between synthetic biotite and K-sanidine demonstrate that the separation of biotite probably will not deplete salic melts in Rb relative to K.</p></div></div>","language":"English","publisher":"Springer","doi":"10.1007/BF00373307","issn":"00107999","usgsCitation":"Noble, D.C., and Hedge, C., 1970, Distribution of rubidium between sodic sanidine and natural silicic liquid: Contributions to Mineralogy and Petrology, v. 29, no. 3, p. 234-241, https://doi.org/10.1007/BF00373307.","productDescription":"8 p.","startPage":"234","endPage":"241","costCenters":[],"links":[{"id":203706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f6dc","contributors":{"authors":[{"text":"Noble, D. C.","contributorId":60627,"corporation":false,"usgs":true,"family":"Noble","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":346802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hedge, C. E.","contributorId":73611,"corporation":false,"usgs":true,"family":"Hedge","given":"C. E.","affiliations":[],"preferred":false,"id":346803,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221246,"text":"5221246 - 1970 - The effect of putrefaction of eggs upon residue analysis of DDT and metabolites","interactions":[],"lastModifiedDate":"2023-11-01T11:33:01.226658","indexId":"5221246","displayToPublicDate":"2010-06-16T12:18:02","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1103,"text":"Bulletin of Environmental Contamination and Toxicology","active":true,"publicationSubtype":{"id":10}},"title":"The effect of putrefaction of eggs upon residue analysis of DDT and metabolites","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF01558315","usgsCitation":"Mulhern, B., and Reichel, W.L., 1970, The effect of putrefaction of eggs upon residue analysis of DDT and metabolites: Bulletin of Environmental Contamination and Toxicology, v. 5, no. 3, p. 222-225, https://doi.org/10.1007/BF01558315.","productDescription":"4 p.","startPage":"222","endPage":"225","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196597,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","issue":"3","noUsgsAuthors":false,"publicationDate":"2013-08-24","publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66763b","contributors":{"authors":[{"text":"Mulhern, B.M.","contributorId":98683,"corporation":false,"usgs":true,"family":"Mulhern","given":"B.M.","email":"","affiliations":[],"preferred":false,"id":333393,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reichel, W. L.","contributorId":50482,"corporation":false,"usgs":true,"family":"Reichel","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":333392,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5220055,"text":"5220055 - 1970 - A note on the stomach contents of two whooping cranes","interactions":[],"lastModifiedDate":"2023-11-27T12:59:45.581654","indexId":"5220055","displayToPublicDate":"2010-06-16T12:18:02","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1318,"text":"Condor","active":true,"publicationSubtype":{"id":10}},"title":"A note on the stomach contents of two whooping cranes","docAbstract":"<p>On 4 January 1968 an adult female Whooping Crane (<span id=\"_mce_caret\" data-mce-bogus=\"true\"><i>Grus americana</i><span id=\"_mce_caret\" data-mce-bogus=\"true\">) was illegally shot by a hunter near the Aransas National Wildlife Refuge, Texas. The carcass was immediately frozen and subsequently shipped to the Patuxent Wildlife Research Center for autopsy.</span></span><br></p>","language":"English","publisher":"American Ornithological Society","doi":"10.2307/1366652","usgsCitation":"Uhler, F.M., and Locke, L.N., 1970, A note on the stomach contents of two whooping cranes: Condor, v. 72, no. 2, p. 246-246, https://doi.org/10.2307/1366652.","productDescription":"1 p.","startPage":"246","endPage":"246","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193567,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ab909","contributors":{"authors":[{"text":"Uhler, Francis M.","contributorId":49838,"corporation":false,"usgs":true,"family":"Uhler","given":"Francis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":331265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Locke, Louis N.","contributorId":71233,"corporation":false,"usgs":true,"family":"Locke","given":"Louis","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":331264,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221251,"text":"5221251 - 1970 - Toxicity of DDT to Japanese quail as influenced by body weight, breeding condition, and sex","interactions":[],"lastModifiedDate":"2026-03-12T14:47:37.711735","indexId":"5221251","displayToPublicDate":"2010-06-16T12:18:01","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3612,"text":"Toxicology and Applied Pharmacology","active":true,"publicationSubtype":{"id":10}},"title":"Toxicity of DDT to Japanese quail as influenced by body weight, breeding condition, and sex","docAbstract":"<p><span>Controlled experiments were utilized to simulate the stresses on wild birds of breeding condition and of weight loss due to migration. Light conditions in the laboratory were manipulated to produce Japanese quail (</span><i>Coturnix coturnix japonica</i><span>) in breeding condition and not in breeding condition. Within each of these groups, some birds were partially starved before dosage and some were fully fed. Birds were then fed dietary levels of 0, 700, 922, 1214, or 1600 ppm dry weight of&nbsp;</span><i>p,p′</i><span>-DDT for a period of 20 days or until death.</span></p><p><span>Birds partially starved before dosage were more susceptible to DDT intoxication than nonstarved ones, and birds not in breeding condition were slightly more so than birds in breeding condition. Similarly, males died earlier than females, and the birds of the lighter weight strain used in the second half of the study died earlier than the birds of the heavier strain used in the first half. The heavier birds of each sex not only survived longer than lighter individuals receiving the same treatments, but they also lost a greater proportion of their weight before death.</span></p><p><span>During the early portion of the dosage period, females in breeding condition were less sensitive to DDT than were females not in breeding condition and males. After 10 days on dosage, however, the cumulative mortality of females in breeding condition rapidly approached that of males and of females not in breeding condition. Food restriction prior to dosage, strains of quail, breeding conditions, and sexes resulted in weight differences and a corresponding accentuation or delay of the effects of the different levels of DDT.</span></p>","language":"English","publisher":"Elsevier","doi":"10.1016/0041-008X(70)90049-9","usgsCitation":"Gish, C., and Chura, N., 1970, Toxicity of DDT to Japanese quail as influenced by body weight, breeding condition, and sex: Toxicology and Applied Pharmacology, v. 17, no. 3, p. 740-751, https://doi.org/10.1016/0041-008X(70)90049-9.","productDescription":"12 p.","startPage":"740","endPage":"751","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194117,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499ee4b07f02db5bcc2d","contributors":{"authors":[{"text":"Gish, C.D.","contributorId":21651,"corporation":false,"usgs":true,"family":"Gish","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":333407,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chura, N.J.","contributorId":8571,"corporation":false,"usgs":true,"family":"Chura","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":333406,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221252,"text":"5221252 - 1970 - Organochlorine insecticide residues in soils and soil invertebrates from agricultural lands","interactions":[],"lastModifiedDate":"2013-03-20T13:03:21","indexId":"5221252","displayToPublicDate":"2010-06-16T12:18:01","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3038,"text":"Pesticides Monitoring Journal","onlineIssn":" 0031-615","printIssn":" 0031-615","active":true,"publicationSubtype":{"id":10}},"title":"Organochlorine insecticide residues in soils and soil invertebrates from agricultural lands","docAbstract":"Soils and earthworms and other soil invertebrates were collected from 67 agricultural fields in eight States.  Samples were analyzed by gas chromatography for DDE, DDD, DDT, aldrin, dieldrin, endrin, heptachlor, heptachlor epoxide, and gamma-chlordane insecticides.  Organochlorine insecticides in soils averaged 1.5 ppm, dry weight, and in earthworms, 13.8 ppm.  Residues in earthworms averaged nine times that in soils.  Residues ranged from a trace to 19.1 ppm in soils and from a trace to 159.4 ppm in earthworms.  Residues in beetle larvae from two fields averaged 0.6 ppm; in snails from two fields, 3.5 ppm; and in slugs from four fields, 89.0 ppm.  Amounts of insecticides in earthworms varied directly with amounts in soils.  Coefficients of correlation between residues in soils and residues in earthworms usually were significant for DDE, DDD, and DDT regardless of crop or soil type.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Pesticides Monitoring Journal","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Gish, C., 1970, Organochlorine insecticide residues in soils and soil invertebrates from agricultural lands: Pesticides Monitoring Journal, v. 3, no. 4, p. 241-252.","productDescription":"241-252","startPage":"241","endPage":"252","numberOfPages":"12","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197263,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269746,"type":{"id":11,"text":"Document"},"url":"https://biodiversitylibrary.org/page/26094215"}],"volume":"3","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a8c1","contributors":{"authors":[{"text":"Gish, C.D.","contributorId":21651,"corporation":false,"usgs":true,"family":"Gish","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":333408,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220401,"text":"5220401 - 1970 - Head-scratching method of the Swainson's warbler","interactions":[],"lastModifiedDate":"2017-06-07T14:49:43","indexId":"5220401","displayToPublicDate":"2010-06-16T12:18:01","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Head-scratching method of the Swainson's warbler","docAbstract":"<p>Ficken and Ficken (Auk, 85: 136, 1968) suggest that the \"Head-scratching method may prove a valuable addition to the set of complex characters that can be used in defining genera,\" and that field observers should continue to fill gaps in our knowledge of this behavior. In the course of a series of observations of Swainson's Warblers (<i>Limnothlypis swainsonii</i>) in the Dismal Swamp, Virginia, I saw head-scratching in three individuals, four times in one, three in another, and once in the third. All three birds used the direct method, bringing the foot forward and under the wing.</p>","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4083673","usgsCitation":"Meanley, B., 1970, Head-scratching method of the Swainson's warbler: The Auk, v. 87, no. 1, p. 163-163, https://doi.org/10.2307/4083673.","productDescription":"1 p.","startPage":"163","endPage":"163","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":503139,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/auk/vol87/iss1/24","text":"External Repository"},{"id":194089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"87","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d347","contributors":{"authors":[{"text":"Meanley, Brooke","contributorId":79938,"corporation":false,"usgs":true,"family":"Meanley","given":"Brooke","email":"","affiliations":[],"preferred":false,"id":331771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221250,"text":"5221250 - 1970 - Soil-food chain-pesticide wildlife relationships in aldrin-treated fields","interactions":[],"lastModifiedDate":"2025-02-19T17:32:41.865259","indexId":"5221250","displayToPublicDate":"2010-06-16T12:18:01","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Soil-food chain-pesticide wildlife relationships in aldrin-treated fields","docAbstract":"<p>Soil-food-chain-pesticide wildlife relationships were investigated to learn the concentration of pesticide residues present in soils, macro-invertebrates, vertebrates, and seeds as a result of annual applications of aldrin at recommended rates for pest control. Two central Missouri cornfields treated with aldrin at 1 lb/acre, for 16 and 15 of the past 17 years, were selected for study during 1965-67. Primary samples collected for residue analyses included soils, earthworms (Lumbricidae), crickets (Gryllidae), and two kinds of ground beetles (Carabidae) obtained during early April, June, August, and October. Vertebrates and plant seeds collected during 1967 included white-footed mice (<i>Peromyscus maniculatus</i>), toads (<i>Bufo americanus</i>), snakes (<i>Thamnophis sirtalis</i> and <i>Pituophis sayi</i>), corn (<i>Zea Mays</i>), foxtail (<i>Setaria Faberii</i>), and annual sunflower (<i>Helianthus annuus</i>). Pesticide residues consisted primarily of dieldrin, the degradation product of aldrin. Combined aldrin and dieldrin residues, as two field all-season averages, wet weight basis, were: soils, 0.31 ppm; earthworms, 1.49 ppm; crickets, 0.23 ppm; <i>Harpalus</i> ground beetles, 1.10 ppm; <i>Poecilus</i> ground beetles, 9.67 ppm; white-footed mice, 0.98 ppm; toads, 3.53 ppm; garter snakes, 12.35 ppm; and corn, foxtail, and sunflower seeds less than 0.02 ppm each. Unusually high average residues (37.48 ppm) in <i>Poecilus</i> beetles during June, 1967, were attributed to abnormally high soil moisture and predacious feeding habits of these insects.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3799508","usgsCitation":"Korschgen, L., 1970, Soil-food chain-pesticide wildlife relationships in aldrin-treated fields: Journal of Wildlife Management, v. 34, no. 1, p. 186-199, https://doi.org/10.2307/3799508.","productDescription":"14 p.","startPage":"186","endPage":"199","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":489943,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3799508","text":"Publisher Index Page"},{"id":194113,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Missouri","county":"Saline County","city":"Malta Bend","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.481,39.2914],[-93.4799,39.2919],[-93.4781,39.2924],[-93.4703,39.291],[-93.4661,39.2861],[-93.4589,39.2794],[-93.4522,39.2708],[-93.4451,39.269],[-93.4439,39.2686],[-93.4421,39.2682],[-93.4403,39.2677],[-93.4379,39.2677],[-93.429,39.2673],[-93.426,39.2674],[-93.4231,39.2674],[-93.4159,39.2665],[-93.4135,39.2656],[-93.4111,39.2648],[-93.4099,39.2639],[-93.4087,39.263],[-93.4075,39.2612],[-93.4069,39.2598],[-93.4069,39.2575],[-93.4075,39.2553],[-93.4086,39.2539],[-93.4098,39.2521],[-93.411,39.2512],[-93.415,39.2416],[-93.4156,39.2375],[-93.4137,39.2335],[-93.4107,39.2308],[-93.4077,39.2285],[-93.4006,39.2267],[-93.394,39.2268],[-93.3863,39.2278],[-93.3757,39.2301],[-93.365,39.232],[-93.352,39.2362],[-93.3379,39.2471],[-93.3314,39.2576],[-93.3285,39.2617],[-93.3297,39.2649],[-93.331,39.2685],[-93.3334,39.2712],[-93.334,39.2721],[-93.3376,39.2757],[-93.3406,39.2798],[-93.3436,39.2847],[-93.3449,39.2892],[-93.3443,39.2929],[-93.3444,39.2956],[-93.3432,39.2983],[-93.3414,39.302],[-93.3397,39.3038],[-93.3373,39.3061],[-93.3367,39.307],[-93.3344,39.3079],[-93.3308,39.3097],[-93.3291,39.3102],[-93.3267,39.3107],[-93.3243,39.3111],[-93.322,39.3116],[-93.3196,39.3112],[-93.316,39.3112],[-93.3118,39.3108],[-93.31,39.3108],[-93.3071,39.3103],[-93.3041,39.3099],[-93.3023,39.3095],[-93.2975,39.3095],[-93.294,39.3091],[-93.288,39.3091],[-93.2833,39.3096],[-93.2809,39.3105],[-93.2773,39.3114],[-93.2762,39.3124],[-93.2738,39.3137],[-93.2726,39.3147],[-93.2674,39.3256],[-93.2668,39.3265],[-93.2662,39.3274],[-93.2645,39.3288],[-93.2639,39.3301],[-93.2633,39.331],[-93.2621,39.3319],[-93.2562,39.3379],[-93.2544,39.3379],[-93.2533,39.3383],[-93.2526,39.3388],[-93.2503,39.3388],[-93.2479,39.3388],[-93.2449,39.3379],[-93.2431,39.3375],[-93.2413,39.3371],[-93.2401,39.3366],[-93.2389,39.3353],[-93.2371,39.3339],[-93.2359,39.3326],[-93.2347,39.3316],[-93.2341,39.3307],[-93.2335,39.3307],[-93.2329,39.3298],[-93.2324,39.3298],[-93.2305,39.3285],[-93.2299,39.328],[-93.2293,39.328],[-93.2282,39.3281],[-93.2258,39.3285],[-93.2246,39.329],[-93.2216,39.3313],[-93.221,39.3313],[-93.2152,39.3381],[-93.2122,39.3427],[-93.2093,39.3486],[-93.2064,39.3522],[-93.1993,39.3586],[-93.1952,39.3627],[-93.1917,39.3659],[-93.1893,39.37],[-93.1888,39.375],[-93.1888,39.3772],[-93.1894,39.3795],[-93.19,39.3813],[-93.1912,39.384],[-93.193,39.3858],[-93.1948,39.3881],[-93.1966,39.3903],[-93.1985,39.3931],[-93.1997,39.3958],[-93.2009,39.3989],[-93.2003,39.4016],[-93.1992,39.4044],[-93.1968,39.4067],[-93.1933,39.4094],[-93.1897,39.4103],[-93.1849,39.4113],[-93.1808,39.4117],[-93.1772,39.4118],[-93.1742,39.4109],[-93.1724,39.41],[-93.1694,39.4086],[-93.167,39.4073],[-93.164,39.405],[-93.1616,39.4028],[-93.161,39.4005],[-93.1592,39.3992],[-93.1586,39.3974],[-93.1574,39.3946],[-93.1562,39.3928],[-93.1544,39.3897],[-93.152,39.387],[-93.149,39.3843],[-93.146,39.382],[-93.1424,39.3802],[-93.1394,39.3784],[-93.1352,39.3775],[-93.1317,39.3775],[-93.1269,39.3776],[-93.1251,39.3776],[-93.112,39.3822],[-93.1091,39.3826],[-93.1061,39.3836],[-93.1037,39.3836],[-93.0977,39.3813],[-93.0912,39.3764],[-93.0894,39.3746],[-93.0876,39.3732],[-93.0875,39.3723],[-93.0864,39.3714],[-93.0852,39.3701],[-93.0834,39.3678],[-93.0822,39.3656],[-93.0815,39.3628],[-93.0809,39.3597],[-93.0809,39.356],[-93.0796,39.3461],[-93.076,39.3402],[-93.0754,39.3388],[-93.0754,39.337],[-93.0742,39.3357],[-93.0724,39.3339],[-93.0694,39.3316],[-93.0652,39.3284],[-93.0616,39.3253],[-93.0568,39.3231],[-93.0521,39.3208],[-93.0479,39.319],[-93.0443,39.3172],[-93.0419,39.3168],[-93.0383,39.3159],[-93.0336,39.315],[-93.03,39.3146],[-93.0205,39.3132],[-93.0163,39.3133],[-93.0121,39.3128],[-93.0116,39.3128],[-93.0062,39.3133],[-93.0038,39.3133],[-93.0003,39.3133],[-92.9985,39.3133],[-92.9979,39.3129],[-92.9688,39.3139],[-92.964,39.3116],[-92.9604,39.3085],[-92.958,39.3053],[-92.9556,39.2999],[-92.9549,39.294],[-92.9567,39.2904],[-92.9573,39.2886],[-92.9585,39.2845],[-92.959,39.2822],[-92.9584,39.2799],[-92.9572,39.2777],[-92.956,39.2759],[-92.9548,39.2745],[-92.953,39.2736],[-92.9507,39.2718],[-92.9471,39.27],[-92.9435,39.2687],[-92.9387,39.2673],[-92.9352,39.2664],[-92.9304,39.2646],[-92.9256,39.2637],[-92.9227,39.2628],[-92.9197,39.2615],[-92.9185,39.2601],[-92.9167,39.2579],[-92.9161,39.2556],[-92.9161,39.2538],[-92.9178,39.252],[-92.919,39.2492],[-92.922,39.2434],[-92.9213,39.2325],[-92.9189,39.2289],[-92.9153,39.2234],[-92.9135,39.223],[-92.9094,39.2225],[-92.9064,39.2225],[-92.9052,39.2226],[-92.9022,39.2217],[-92.8993,39.2217],[-92.8963,39.2217],[-92.8927,39.2226],[-92.8892,39.2235],[-92.8868,39.2244],[-92.8844,39.2249],[-92.8785,39.2285],[-92.875,39.2313],[-92.8726,39.2331],[-92.8702,39.234],[-92.8679,39.2349],[-92.8631,39.2349],[-92.8524,39.2295],[-92.8553,39.2159],[-92.857,39.2109],[-92.8582,39.2082],[-92.86,39.2055],[-92.8612,39.2041],[-92.8612,39.2032],[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L.J.","contributorId":29910,"corporation":false,"usgs":true,"family":"Korschgen","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":333405,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220531,"text":"5220531 - 1970 - Passive immunization of pigeons against trichomoniasis","interactions":[],"lastModifiedDate":"2025-05-09T15:45:50.520244","indexId":"5220531","displayToPublicDate":"2010-06-16T12:18:01","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2434,"text":"Journal of Protozoology","active":true,"publicationSubtype":{"id":10}},"title":"Passive immunization of pigeons against trichomoniasis","docAbstract":"<p>Nonimmune homing pigeons<span>&nbsp;</span><i>Columba livia</i><span>&nbsp;</span>were infected with the Jones' Barn strain of<span>&nbsp;</span><i>Trichomonas gallinae</i><span>&nbsp;</span>and subsequently transfused with plasma from acute or chronically infected pigeons harboring one of 3 different strains of<span>&nbsp;</span><i>T. gallinae.</i><span>&nbsp;</span>The transfusions were either a single 2 ml dose given one day after inoculation or three 1 ml doses given 0, 5, and 10 days after inoculation. Plasma from pigeons harboring any of the 3 strains was capable of passively immunizing nonimmune birds. All birds which were immunized with plasma from infected pigeons survived until killed at the end of the test period and no visceral lesions were found on necropsy but trichomonads were present in the oropharynx. All controls (untreated or transfused with normal plasma) died of visceral trichomoniasis.</p><p>Immune plasma produced some lysis of trichomonads<span>&nbsp;</span><i>in vitro,</i><span>&nbsp;</span>and inhibition of motility and vacuolization occurred in some of the non-lysed organisms. The overall lytic activity<span>&nbsp;</span><i>in vitro</i><span>&nbsp;</span>affected less than 10% of the suspended trichomonads.</p>","language":"English","publisher":"Wiley","doi":"10.1111/j.1550-7408.1970.tb04726.x","usgsCitation":"Kocan, R.M., 1970, Passive immunization of pigeons against trichomoniasis: Journal of Protozoology, v. 17, no. 4, p. 551-553, https://doi.org/10.1111/j.1550-7408.1970.tb04726.x.","productDescription":"3 p.","startPage":"551","endPage":"553","numberOfPages":"3","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":197980,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"4","noUsgsAuthors":false,"publicationDate":"2007-04-30","publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c33","contributors":{"authors":[{"text":"Kocan, R. M.","contributorId":41783,"corporation":false,"usgs":true,"family":"Kocan","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":331966,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220437,"text":"5220437 - 1970 - Bronzed cowbird taken in Florida","interactions":[],"lastModifiedDate":"2017-06-07T12:57:02","indexId":"5220437","displayToPublicDate":"2010-06-16T12:18:01","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Bronzed cowbird taken in Florida","docAbstract":"<p>On 8 November 1968 in Gainesville, Florida, I removed a male Bronzed Cowbird (<i>Tangavius a. aeneus</i>) from a blackbird decoy trap containing a large number of Brown-headed Cowbirds (<i>Malothrus ater</i>). Oliver L. Austin, Jr., at the Florida State Museum, verified the species identification by noting the notched inner webs of the outer three primaries, a characteristic of the genus. The subspecific identification was made at the U. S. National Museum where the bird is now specimen number 531666. The subspecies normally ranges from southcentral Texas and the Yucatan Peninsula south through Central America to Panama (Check-list of North American birds, fifth ed., Baltimore, Amer. Ornithol. Union, 1957, p. 542). This Gainesville specimen apparently is the first Bronzed Cow- bird taken in Florida. Alexander Sprunt, Jr., (Florida bird life. In Addendum to Florida bird life, New York, Coward-McCann, 1963, p. 18) lists three photographed sightings at Sarasota, Florida, in April 196</p>","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4083812","usgsCitation":"Matteson, R., 1970, Bronzed cowbird taken in Florida: The Auk, v. 87, no. 3, p. 588-588, https://doi.org/10.2307/4083812.","productDescription":"1 p.","startPage":"588","endPage":"588","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":503138,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/auk/vol87/iss3/30","text":"External Repository"},{"id":193485,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","volume":"87","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb317","contributors":{"authors":[{"text":"Matteson, R.E.","contributorId":86061,"corporation":false,"usgs":true,"family":"Matteson","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":331811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5223225,"text":"5223225 - 1970 - Molt and taxonomy of red-breasted nuthatches","interactions":[],"lastModifiedDate":"2012-02-02T00:15:05","indexId":"5223225","displayToPublicDate":"2010-06-16T12:18:00","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3783,"text":"The Wilson Bulletin","printIssn":"0043-5643","active":true,"publicationSubtype":{"id":10}},"title":"Molt and taxonomy of red-breasted nuthatches","docAbstract":"The postnuptial and postjuvenal molts of Red-breasted Nuthatches occur from middle June to late September. Some birds may be nearly finished with the complete molt before other individuals begin, so that specimens taken at any given time may differ by as much as two months in the age of their plumage. No characters useful in ageing birds after the completion of the autumn molt were found.....The proposed racial subdivision of Sitta canadensis was based on misleading evidence resulting from variation of plumage age in birds assumed to be seasonally comparable, sooting of birds in industrialized parts of the country, and variation in quality of prepared specimens.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Wilson Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Banks, R., 1970, Molt and taxonomy of red-breasted nuthatches: The Wilson Bulletin, v. 82, no. 2, p. 201-205.","productDescription":"201-205","startPage":"201","endPage":"205","numberOfPages":"5","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":16281,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://elibrary.unm.edu/sora/Wilson/v082n02/p0201-p0205.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":198309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699259","contributors":{"authors":[{"text":"Banks, Richard C.","contributorId":20440,"corporation":false,"usgs":true,"family":"Banks","given":"Richard C.","affiliations":[],"preferred":false,"id":338152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}