{"pageNumber":"6382","pageRowStart":"159525","pageSize":"25","recordCount":184689,"records":[{"id":70038405,"text":"wdrCA682 - 1970 - Water Resources Data for California, 1968; Part 2: Water Quality Records","interactions":[],"lastModifiedDate":"2012-05-22T01:01:41","indexId":"wdrCA682","displayToPublicDate":"2012-05-13T15:21:00","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":"CA-68-2","title":"Water Resources Data for California, 1968; Part 2: Water Quality Records","docAbstract":"<p>Water-resources investigations of the U.S. Geological Survey include the collection of water-quality data on the chemical and physical characteristics of surface- and ground-water supplies of the Nation. These data for the 1968 water year for the quality of surface water in California are presented in this report. Data for a few water-quality stations in bordering States are also included. The data were collected by the Water Resources Division of the Geological Survey under the direction of R. Stanley Lord, district chief, Menlo Park, Calif.</p>\n<p>Water-quality information is presented for chemical quality, fluvial sediment, and water temperatures. The chemical-quality information includes concentrations of individual dissolved constituents and certain properties or characteristics such as hardness, sodium-adsorption ratio, specific conductance, and pH. Fluvial-sediment information includes suspended-sediment discharges and concentrations and the particle-size distribution of suspended sediment and bed material. Water-temperature data represent once daily observations except for stations where a continuous record of temperature is obtained. Daily minimums and maximums are reported for the continuous temperature stations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA682","usgsCitation":"U.S. Geological Survey, 1970, Water Resources Data for California, 1968; Part 2: Water Quality Records: U.S. Geological Survey Water Data Report CA-68-2, xi, 416 p., https://doi.org/10.3133/wdrCA682.","productDescription":"xi, 416 p.","temporalStart":"1967-10-01","temporalEnd":"1968-09-30","costCenters":[],"links":[{"id":256925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":256923,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1968/ca-68/WDR-1968-wq.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc496e4b08c986b32b732"}
,{"id":70038251,"text":"70038251 - 1970 - Hydrogeologic data for the Upper Housatonic River basin, Connecticut","interactions":[],"lastModifiedDate":"2014-04-09T12:41:33","indexId":"70038251","displayToPublicDate":"2012-04-22T16:51:00","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":"22","title":"Hydrogeologic data for the Upper Housatonic River basin, Connecticut","docAbstract":"The upper Housatonic River basin covers an area of about 700 square miles in western Connecticut and includes the towns of Bridgewater, Brookfield, Canaan, Cornwall, Kent, New Fairfield, New Hilford, North Canaan, Salisbury, Sharon, Sherman and Warren and parts of Bethel, Bethlehem, Danbury, Goshen, Litchfield, Morris, Newtown, Norfolk, Ridgefield, Roxbury, Southbury, Torrington and Washington. The U.S. Geological Survey in cooperation with the Connecticut Water Resources Commission conducted a water resources investigation of this basin from July 1966 to November 1968. The interpretive results of this study are published separately in Connecticut Water Resources Bulletin No. 21.\nStreamflow and water-quality data and measurements of water levels In observation\nwells collected during the investigative period have been published in the\n1967, 1968 and 1969 volumes of the annual series of U.S. Geological Survey reports\nentitled \"Water Resources Data for Connecticut\". The remaining significant information,\nconsisting of records of 284 wells and 5 springs, logs of 322 wells and test\nholes, mechanical analyses of 58 sediment samples of stratified drift and records\nof 3 pumping tests is contained in this report. The locations of all sites at\nwhich hydrogeologic data were collected are shown on plate A (in pocket at back of\nreport). The Information contained on the following pages together with data\npreviously published~ document the companion interpretive report and should facilitate\nthe planned development of water resources at specific localities.","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Water Resources Commission","usgsCitation":"Melvin, R., 1970, Hydrogeologic data for the Upper Housatonic River basin, Connecticut: Connecticut Water Resources Bulletin 22, Report: 33 p.; 3 Plates: 31.47 x 38.64 inches and smaller.","productDescription":"Report: 33 p.; 3 Plates: 31.47 x 38.64 inches and smaller","numberOfPages":"37","costCenters":[],"links":[{"id":258811,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0022/report.pdf","size":"1542","linkFileType":{"id":1,"text":"pdf"}},{"id":258812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0022/report-thumb.jpg"},{"id":285997,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038251/plate-a-3.pdf"},{"id":285995,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038251/plate-a-1.pdf"},{"id":285996,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038251/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\": [ [ [ -73.583333,41.283333 ], [ -73.583333,41.633333 ], [ -73.25,41.633333 ], [ -73.25,41.283333 ], [ -73.583333,41.283333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a33b4e4b0c8380cd5f1c9","contributors":{"authors":[{"text":"Melvin, Robert L.","contributorId":96277,"corporation":false,"usgs":true,"family":"Melvin","given":"Robert L.","affiliations":[],"preferred":false,"id":463741,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":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":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":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":70001663,"text":"70001663 - 1970 - Elastic shocks and earthquakes","interactions":[],"lastModifiedDate":"2012-03-08T17:16:39","indexId":"70001663","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":"Elastic shocks and earthquakes","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Die Naturwissenschaften","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Springer-Verlag","doi":"10.1007/BF00590684","issn":"00281042","usgsCitation":"Byerlee, J., and Peselnick, L., 1970, Elastic shocks and earthquakes: Die Naturwissenschaften, v. 57, no. 2, p. 82-85, https://doi.org/10.1007/BF00590684.","startPage":"82","endPage":"85","costCenters":[],"links":[{"id":203417,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":19133,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00590684"}],"volume":"57","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ee4d","contributors":{"authors":[{"text":"Byerlee, J.D.","contributorId":69982,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.D.","affiliations":[],"preferred":false,"id":346812,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peselnick, L.","contributorId":66825,"corporation":false,"usgs":true,"family":"Peselnick","given":"L.","affiliations":[],"preferred":false,"id":346811,"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":70001561,"text":"70001561 - 1970 - Water content of basalt erupted on the ocean floor","interactions":[],"lastModifiedDate":"2020-11-30T16:42:59.538015","indexId":"70001561","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":"Water content of basalt erupted on the ocean floor","docAbstract":"<p>Deep sea pillow basalts dredged from the ocean floor show that vesicularity changes with composition as well as with depth. Alkalic basalts are more vesicular than tholeiitic basalts erupted at the same depth. The vesicularity data, when related to experimentally determined solubility of water in basalt, indicate that K-poor oceanic tholeiites originally contained about 0.25 percent water, Hawaiian tholeiites of intermediate K-content, about 0.5 percent water, and alkali-rich basalts, about 0.9 percent water. Analyses of fresh basalt pillows show a systematic increase of H<sub>2</sub>O<sup>+</sup><span>&nbsp;</span>as the rocks become more alkalic. K-poor oceanic tholeiites contain 0.06–0.42 percent H<sub>2</sub>O<sup>+</sup>, Hawaiian tholeiites, 0.31–0.60 percent H<sub>2</sub>O<sup>+</sup>, and alkali rich basalts 0.49–0.98 percent H<sub>2</sub>O<sup>+</sup>. The contents of K<sub>2</sub>O, P<sub>2</sub>O<sub>5</sub>, F, and Cl increase directly with an increase in H<sub>2</sub>O<sup>+</sup><span>&nbsp;</span>content such that at 1.0 weight percent H<sub>2</sub>O<sup>+</sup>, K<sub>2</sub>O is 1.58 percent, P<sub>2</sub>O<sub>5</sub><span>&nbsp;</span>is 0.55 percent, F is 0.07 percent, and Cl is 0.1 percent. The measured weight percent of deuterium on the rim of one Hawaiian pillow is −6.0 (relative to SMOW); this value, which is similar to other indications of magmatic water, suggests that no appreciable sea water was absorbed by the pillow during or subsequent to eruption on the ocean floor.</p><p>Concentrations of volatile constituents in the alkali basalt melts relative to tholeiitic melts can be explained by varying degrees of partial melting of mantle material or by fractional crystallization of a magma batch.</p>","language":"English","publisher":"Springer","doi":"10.1007/BF00388949","issn":"00107999","usgsCitation":"Moore, J., 1970, Water content of basalt erupted on the ocean floor: Contributions to Mineralogy and Petrology, v. 28, no. 4, p. 272-279, https://doi.org/10.1007/BF00388949.","productDescription":"8 p.","startPage":"272","endPage":"279","costCenters":[],"links":[{"id":203746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"28","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db489f4f","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":346801,"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 States","state":"Hawaii","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-155.778234,20.245743],[-155.772734,20.245409],[-155.746893,20.232325],[-155.737004,20.222773],[-155.735822,20.212417],[-155.732704,20.205392],[-155.653966,20.16736],[-155.630382,20.146916],[-155.624565,20.145911],[-155.607797,20.137987],[-155.600909,20.126573],[-155.598033,20.124539],[-155.590923,20.122497],[-155.58168,20.123617],[-155.568368,20.130545],[-155.558933,20.13157],[-155.523661,20.120028],[-155.516795,20.11523],[-155.502561,20.114155],[-155.468211,20.104296],[-155.443957,20.095318],[-155.405459,20.078772],[-155.4024,20.075541],[-155.387578,20.067119],[-155.33021,20.038517],[-155.29548,20.024438],[-155.282629,20.021969],[-155.270316,20.014525],[-155.240933,19.990173],[-155.204486,19.969438],[-155.194593,19.958368],[-155.179939,19.949372],[-155.149215,19.922872],[-155.144394,19.920523],[-155.131235,19.906801],[-155.124618,19.897288],[-155.12175,19.886099],[-155.107541,19.872467],[-155.098716,19.867811],[-155.095032,19.867882],[-155.086341,19.855399],[-155.084357,19.849736],[-155.085674,19.838584],[-155.088979,19.826656],[-155.094414,19.81491],[-155.09207,19.799409],[-155.091216,19.776368],[-155.093517,19.771832],[-155.093387,19.737751],[-155.087118,19.728013],[-155.079426,19.726193],[-155.063972,19.728917],[-155.045382,19.739824],[-155.006423,19.739286],[-154.997278,19.72858],[-154.987168,19.708524],[-154.981102,19.690687],[-154.984718,19.672161],[-154.983778,19.641647],[-154.974342,19.633201],[-154.963933,19.627605],[-154.950359,19.626461],[-154.947874,19.62425],[-154.947718,19.621947],[-154.951014,19.613614],[-154.947106,19.604856],[-154.93394,19.597505],[-154.928205,19.592702],[-154.924422,19.586553],[-154.903542,19.570622],[-154.875,19.556797],[-154.852618,19.549172],[-154.837384,19.538354],[-154.826732,19.537626],[-154.814417,19.53009],[-154.809561,19.522377],[-154.809379,19.519086],[-154.822968,19.48129],[-154.838545,19.463642],[-154.86854,19.438126],[-154.887817,19.426425],[-154.928772,19.397646],[-154.944185,19.381852],[-154.964619,19.365646],[-154.980861,19.349291],[-155.020537,19.331317],[-155.061729,19.316636],[-155.113272,19.290613],[-155.1337,19.276099],[-155.159635,19.268375],[-155.172413,19.26906],[-155.187427,19.266156],[-155.19626,19.261295],[-155.205892,19.260907],[-155.243961,19.271313],[-155.264619,19.274213],[-155.296761,19.266289],[-155.303808,19.261835],[-155.31337,19.250698],[-155.341268,19.234039],[-155.349148,19.217756],[-155.360631,19.20893],[-155.378638,19.202435],[-155.390701,19.201171],[-155.417369,19.187858],[-155.427093,19.179546],[-155.432519,19.170623],[-155.453516,19.151952],[-155.465663,19.146964],[-155.505281,19.137908],[-155.51474,19.132501],[-155.51214,19.128174],[-155.512137,19.124296],[-155.519652,19.117025],[-155.526136,19.115889],[-155.528902,19.11371],[-155.544806,19.091059],[-155.551129,19.08878],[-155.557817,19.08213],[-155.555326,19.069377],[-155.555177,19.053932],[-155.557371,19.046565],[-155.566446,19.032531],[-155.576599,19.027412],[-155.581903,19.02224],[-155.596032,18.998833],[-155.596521,18.980654],[-155.601866,18.971572],[-155.613966,18.970399],[-155.625256,18.961951],[-155.625,18.959934],[-155.638054,18.941723],[-155.658486,18.924835],[-155.672005,18.917466],[-155.681825,18.918694],[-155.687716,18.923358],[-155.690171,18.932195],[-155.693117,18.940542],[-155.726043,18.969437],[-155.763598,18.981837],[-155.806109,19.013967],[-155.853943,19.023762],[-155.88155,19.036644],[-155.884077,19.039266],[-155.886278,19.05576],[-155.903693,19.080777],[-155.908355,19.081138],[-155.921389,19.121183],[-155.917292,19.155963],[-155.903339,19.217792],[-155.90491,19.230147],[-155.902565,19.258427],[-155.895435,19.274639],[-155.890842,19.298905],[-155.887356,19.337101],[-155.888701,19.348031],[-155.898792,19.377984],[-155.913849,19.401107],[-155.909087,19.415455],[-155.921707,19.43055],[-155.924269,19.438794],[-155.925166,19.468081],[-155.922609,19.478611],[-155.924124,19.481406],[-155.930523,19.484921],[-155.935641,19.485628],[-155.936403,19.481905],[-155.939145,19.481577],[-155.95149,19.486649],[-155.952897,19.488805],[-155.953663,19.510003],[-155.960457,19.546612],[-155.962264,19.551779],[-155.965211,19.554745],[-155.96935,19.555963],[-155.970969,19.586328],[-155.978206,19.608159],[-155.997728,19.642816],[-156.028982,19.650098],[-156.032928,19.653905],[-156.034994,19.65936],[-156.033326,19.66923],[-156.027427,19.672154],[-156.029281,19.678908],[-156.036079,19.690252],[-156.04796,19.698938],[-156.051652,19.703649],[-156.052485,19.718667],[-156.064364,19.730766],[-156.05722,19.742536],[-156.052315,19.756836],[-156.049651,19.780452],[-156.021732,19.8022],[-156.006267,19.81758],[-155.982821,19.845651],[-155.976651,19.85053],[-155.964817,19.855183],[-155.949251,19.857034],[-155.945297,19.853443],[-155.940311,19.852305],[-155.925843,19.858928],[-155.926938,19.870221],[-155.92549,19.875],[-155.915662,19.887126],[-155.901987,19.912081],[-155.894099,19.923135],[-155.894474,19.926927],[-155.892533,19.932162],[-155.866919,19.954172],[-155.856588,19.968885],[-155.840708,19.976952],[-155.838692,19.975527],[-155.835312,19.976078],[-155.831948,19.982775],[-155.828965,19.995542],[-155.825473,20.025944],[-155.828182,20.035424],[-155.850385,20.062506],[-155.866931,20.078652],[-155.88419,20.10675],[-155.899149,20.145728],[-155.906035,20.205157],[-155.901452,20.235787],[-155.890663,20.25524],[-155.882631,20.263026],[-155.873921,20.267744],[-155.853293,20.271548],[-155.811459,20.26032],[-155.783242,20.246395],[-155.778234,20.245743]]],[[[-157.789581,21.438396],[-157.789734,21.437679],[-157.789276,21.435833],[-157.790543,21.434313],[-157.791718,21.434881],[-157.793045,21.43391],[-157.793167,21.43574],[-157.791565,21.43651],[-157.791779,21.437752],[-157.793289,21.437658],[-157.791779,21.438435],[-157.791092,21.438442],[-157.790741,21.43874],[-157.789581,21.438396]]],[[[-160.125,21.95909],[-160.122262,21.962881],[-160.112746,21.995245],[-160.09645,22.001489],[-160.072123,22.003334],[-160.058543,21.99638],[-160.051992,21.983681],[-160.052729,21.980321],[-160.056336,21.977939],[-160.060549,21.976729],[-160.063349,21.978354],[-160.065811,21.976562],[-160.078393,21.955153],[-160.085787,21.927295],[-160.080012,21.910808],[-160.079065,21.89608],[-160.098897,21.884711],[-160.124283,21.876789],[-160.147609,21.872814],[-160.16162,21.864746],[-160.174796,21.846923],[-160.189782,21.82245],[-160.205211,21.789053],[-160.200427,21.786479],[-160.205851,21.779518],[-160.218044,21.783755],[-160.23478,21.795418],[-160.24961,21.815145],[-160.244943,21.848943],[-160.231028,21.886263],[-160.228965,21.889117],[-160.21383,21.899193],[-160.205528,21.907507],[-160.202716,21.912422],[-160.190158,21.923592],[-160.167471,21.932863],[-160.13705,21.948632],[-160.127302,21.955508],[-160.125,21.95909]]],[[[-159.431707,22.220015],[-159.40732,22.230555],[-159.388119,22.223252],[-159.385977,22.220009],[-159.367563,22.214906],[-159.359842,22.214831],[-159.357227,22.217744],[-159.353795,22.217669],[-159.339964,22.208519],[-159.315613,22.186817],[-159.308855,22.155555],[-159.297808,22.149748],[-159.295875,22.144547],[-159.295271,22.13039],[-159.297143,22.113815],[-159.317451,22.080944],[-159.321667,22.063411],[-159.324775,22.05867],[-159.333267,22.054639],[-159.337996,22.046575],[-159.341401,22.028978],[-159.333224,21.973005],[-159.333109,21.964176],[-159.334714,21.961099],[-159.350828,21.950817],[-159.356613,21.939546],[-159.382349,21.924479],[-159.408284,21.897781],[-159.425862,21.884527],[-159.446599,21.871647],[-159.471962,21.88292],[-159.490914,21.888898],[-159.517973,21.890996],[-159.555415,21.891355],[-159.574991,21.896585],[-159.577784,21.900486],[-159.584272,21.899038],[-159.610241,21.898356],[-159.637849,21.917166],[-159.648132,21.93297],[-159.671872,21.957038],[-159.681493,21.960054],[-159.705255,21.963427],[-159.72014,21.970789],[-159.758218,21.980694],[-159.765735,21.986593],[-159.788139,22.018411],[-159.790932,22.031177],[-159.786543,22.06369],[-159.780096,22.072567],[-159.748159,22.100388],[-159.741223,22.115666],[-159.733457,22.142756],[-159.726043,22.152171],[-159.699978,22.165252],[-159.66984,22.170782],[-159.608794,22.207878],[-159.591596,22.219456],[-159.583965,22.22668],[-159.559643,22.229185],[-159.554166,22.228212],[-159.548594,22.226263],[-159.54115,22.216764],[-159.534594,22.219403],[-159.523769,22.217602],[-159.51941,22.215646],[-159.518348,22.211182],[-159.515574,22.208008],[-159.507811,22.205987],[-159.501055,22.211064],[-159.500821,22.225538],[-159.488558,22.23317],[-159.480158,22.232715],[-159.467007,22.226529],[-159.45619,22.228811],[-159.441809,22.226321],[-159.431707,22.220015]]],[[[-157.014553,21.185503],[-156.999108,21.182221],[-156.991318,21.18551],[-156.987768,21.18935],[-156.982343,21.207798],[-156.984464,21.210063],[-156.984032,21.212198],[-156.974002,21.218503],[-156.969064,21.217018],[-156.962847,21.212131],[-156.951654,21.191662],[-156.950808,21.182636],[-156.946159,21.175963],[-156.918248,21.168279],[-156.903466,21.16421],[-156.898174,21.16594],[-156.89613,21.169561],[-156.896537,21.172208],[-156.867944,21.16452],[-156.841592,21.167926],[-156.821944,21.174693],[-156.771495,21.180053],[-156.742231,21.176214],[-156.738341,21.17202],[-156.736648,21.16188],[-156.719386,21.163911],[-156.712696,21.161547],[-156.714158,21.152238],[-156.726033,21.13236],[-156.748932,21.1086],[-156.775995,21.089751],[-156.790815,21.081686],[-156.794136,21.075796],[-156.835351,21.06336],[-156.865795,21.057801],[-156.877137,21.0493],[-156.891946,21.051831],[-156.89517,21.055771],[-156.953719,21.067761],[-157.00295,21.083282],[-157.02617,21.089015],[-157.032045,21.091094],[-157.037667,21.097864],[-157.079696,21.105835],[-157.095373,21.10636],[-157.125,21.1026],[-157.143483,21.096632],[-157.254061,21.090601],[-157.298054,21.096917],[-157.313343,21.105755],[-157.299187,21.132488],[-157.299471,21.135972],[-157.293774,21.146127],[-157.284346,21.157755],[-157.276474,21.163175],[-157.274504,21.162762],[-157.259911,21.174875],[-157.254709,21.181376],[-157.251007,21.190952],[-157.25026,21.207739],[-157.256935,21.215665],[-157.261457,21.217661],[-157.263163,21.220873],[-157.26069,21.225684],[-157.257085,21.227268],[-157.241534,21.220969],[-157.226445,21.220185],[-157.212082,21.221848],[-157.202125,21.219298],[-157.192439,21.207644],[-157.185553,21.205602],[-157.157103,21.200706],[-157.148125,21.200745],[-157.144627,21.202555],[-157.128207,21.201488],[-157.113438,21.197375],[-157.097971,21.198012],[-157.064264,21.189076],[-157.053053,21.188754],[-157.047757,21.190739],[-157.039987,21.190909],[-157.014553,21.185503]]],[[[-156.544169,20.522802],[-156.550016,20.520273],[-156.559994,20.521892],[-156.586238,20.511711],[-156.603844,20.524372],[-156.631143,20.514943],[-156.642347,20.508285],[-156.647464,20.512017],[-156.668809,20.504738],[-156.682939,20.506775],[-156.703673,20.527237],[-156.702265,20.532451],[-156.696662,20.541646],[-156.6801,20.557021],[-156.651567,20.565574],[-156.614598,20.587109],[-156.610734,20.59377],[-156.576871,20.60657],[-156.56714,20.604895],[-156.553604,20.594729],[-156.543034,20.580115],[-156.542808,20.573674],[-156.548909,20.56859],[-156.556021,20.542657],[-156.553018,20.539382],[-156.540189,20.534741],[-156.539643,20.527644],[-156.544169,20.522802]]],[[[-156.612012,21.02477],[-156.612065,21.027273],[-156.606238,21.034371],[-156.592256,21.03288],[-156.580448,21.020172],[-156.562773,21.016167],[-156.549813,21.004939],[-156.546291,21.005082],[-156.528246,20.967757],[-156.518707,20.954662],[-156.512226,20.95128],[-156.510391,20.940358],[-156.507913,20.937886],[-156.49948,20.934577],[-156.495883,20.928005],[-156.493263,20.916011],[-156.481055,20.898199],[-156.474796,20.894546],[-156.422668,20.911631],[-156.386045,20.919563],[-156.374297,20.927616],[-156.370729,20.932669],[-156.352649,20.941414],[-156.345655,20.941596],[-156.342365,20.938737],[-156.332817,20.94645],[-156.324578,20.950184],[-156.307198,20.942739],[-156.286332,20.947701],[-156.275116,20.937361],[-156.263107,20.940888],[-156.242555,20.937838],[-156.230159,20.931936],[-156.230089,20.917864],[-156.226757,20.916677],[-156.222062,20.918309],[-156.217953,20.916573],[-156.216341,20.907035],[-156.173103,20.876926],[-156.170458,20.874605],[-156.166746,20.865646],[-156.132669,20.861369],[-156.129381,20.847513],[-156.115735,20.827301],[-156.100123,20.828502],[-156.090291,20.831872],[-156.059788,20.81054],[-156.033287,20.808246],[-156.003532,20.795545],[-156.002947,20.789418],[-155.987944,20.776552],[-155.984587,20.767496],[-155.986851,20.758577],[-155.985413,20.744245],[-155.987216,20.722717],[-155.991534,20.713654],[-156.00187,20.698064],[-156.01415,20.685681],[-156.020044,20.686857],[-156.030702,20.682452],[-156.040341,20.672719],[-156.043786,20.664902],[-156.053385,20.65432],[-156.059753,20.652044],[-156.081472,20.654387],[-156.089365,20.648519],[-156.120985,20.633685],[-156.129898,20.627523],[-156.142665,20.623605],[-156.144588,20.624032],[-156.148085,20.629067],[-156.156772,20.629639],[-156.169732,20.627358],[-156.173393,20.6241],[-156.184556,20.629719],[-156.192938,20.631769],[-156.210258,20.628518],[-156.225338,20.62294],[-156.236145,20.61595],[-156.265921,20.601629],[-156.284391,20.596488],[-156.288037,20.59203],[-156.293454,20.588783],[-156.302692,20.586199],[-156.322944,20.588273],[-156.351716,20.58697],[-156.359634,20.581977],[-156.370725,20.57876],[-156.377633,20.578427],[-156.415313,20.586099],[-156.417523,20.589728],[-156.415746,20.594044],[-156.417799,20.598682],[-156.423141,20.602079],[-156.427708,20.598873],[-156.431872,20.598143],[-156.438385,20.601337],[-156.444242,20.607941],[-156.442884,20.613842],[-156.450651,20.642212],[-156.445894,20.64927],[-156.443673,20.656018],[-156.448656,20.704739],[-156.451038,20.725469],[-156.452895,20.731287],[-156.458438,20.736676],[-156.462242,20.753952],[-156.462058,20.772571],[-156.464043,20.781667],[-156.473562,20.790756],[-156.489496,20.798339],[-156.501688,20.799933],[-156.506026,20.799463],[-156.515994,20.794234],[-156.525215,20.780821],[-156.537752,20.778408],[-156.631794,20.82124],[-156.678634,20.870541],[-156.688969,20.888673],[-156.687804,20.89072],[-156.688132,20.906325],[-156.691334,20.91244],[-156.697418,20.916368],[-156.69989,20.920629],[-156.69411,20.952708],[-156.680905,20.980262],[-156.665514,21.007054],[-156.652419,21.008994],[-156.645966,21.014416],[-156.642592,21.019936],[-156.644167,21.022312],[-156.642809,21.027583],[-156.619581,21.027793],[-156.612012,21.02477]]],[[[-157.010001,20.929757],[-156.989813,20.932127],[-156.971604,20.926254],[-156.937529,20.925274],[-156.91845,20.922546],[-156.897169,20.915395],[-156.837047,20.863575],[-156.825237,20.850731],[-156.809576,20.826036],[-156.808469,20.820396],[-156.809463,20.809169],[-156.817427,20.794606],[-156.838321,20.764575],[-156.846413,20.760201],[-156.851481,20.760069],[-156.869753,20.754701],[-156.890295,20.744855],[-156.909081,20.739533],[-156.949009,20.738997],[-156.96789,20.73508],[-156.984747,20.756677],[-156.994001,20.786671],[-156.988933,20.815496],[-156.991834,20.826603],[-157.006243,20.849603],[-157.010911,20.854476],[-157.054552,20.877219],[-157.059663,20.884634],[-157.061128,20.890635],[-157.062511,20.904385],[-157.05913,20.913407],[-157.035789,20.927078],[-157.025626,20.929528],[-157.010001,20.929757]]],[[[-158.044485,21.306011],[-158.0883,21.2988],[-158.1033,21.2979],[-158.1127,21.3019],[-158.1211,21.3169],[-158.1225,21.3224],[-158.111949,21.326622],[-158.114196,21.331123],[-158.119427,21.334594],[-158.125459,21.330264],[-158.13324,21.359207],[-158.1403,21.3738],[-158.149719,21.385208],[-158.161743,21.396282],[-158.1792,21.4043],[-158.181274,21.409626],[-158.181,21.420868],[-158.182648,21.430073],[-158.192352,21.44804],[-158.205383,21.459793],[-158.219446,21.46978],[-158.233,21.4876],[-158.231171,21.523857],[-158.23175,21.533035],[-158.234314,21.540058],[-158.250671,21.557373],[-158.27951,21.575794],[-158.277679,21.578789],[-158.254425,21.582684],[-158.190704,21.585892],[-158.17,21.5823],[-158.12561,21.586739],[-158.10672,21.596577],[-158.106689,21.603024],[-158.1095,21.6057],[-158.108185,21.607487],[-158.079895,21.628101],[-158.0668,21.6437],[-158.066711,21.65234],[-158.0639,21.6584],[-158.0372,21.6843],[-158.018127,21.699955],[-157.9923,21.708],[-157.98703,21.712494],[-157.968628,21.712704],[-157.947174,21.689568],[-157.939,21.669],[-157.9301,21.6552],[-157.924591,21.651183],[-157.9228,21.6361],[-157.9238,21.6293],[-157.910797,21.611183],[-157.900574,21.605885],[-157.87735,21.575277],[-157.878601,21.560181],[-157.872528,21.557568],[-157.8669,21.5637],[-157.85614,21.560661],[-157.85257,21.557514],[-157.836945,21.529945],[-157.837372,21.512085],[-157.849579,21.509598],[-157.852625,21.499971],[-157.84549,21.466747],[-157.84099,21.459483],[-157.82489,21.455379],[-157.8163,21.4502],[-157.8139,21.4403],[-157.8059,21.4301],[-157.786513,21.415633],[-157.779846,21.417309],[-157.774455,21.421352],[-157.772209,21.431236],[-157.774905,21.453698],[-157.772209,21.457741],[-157.764572,21.461335],[-157.754239,21.461335],[-157.737617,21.459089],[-157.731777,21.455944],[-157.731328,21.444713],[-157.73582,21.438424],[-157.740762,21.424048],[-157.741211,21.414614],[-157.7386,21.4043],[-157.730191,21.401871],[-157.728221,21.402104],[-157.726421,21.402845],[-157.724324,21.403311],[-157.723794,21.40329],[-157.723286,21.403227],[-157.722735,21.403121],[-157.722544,21.403036],[-157.721845,21.401596],[-157.721083,21.399541],[-157.7189,21.3961],[-157.7089,21.3833],[-157.7087,21.3793],[-157.7126,21.3689],[-157.7106,21.3585],[-157.7088,21.3534],[-157.6971,21.3364],[-157.6938,21.3329],[-157.6619,21.3131],[-157.6518,21.3139],[-157.652629,21.308709],[-157.6537,21.302],[-157.6946,21.2739],[-157.6944,21.2665],[-157.7001,21.264],[-157.7097,21.2621],[-157.7139,21.2638],[-157.7142,21.2665],[-157.7114,21.272],[-157.7122,21.2814],[-157.7143,21.2845],[-157.7213,21.2869],[-157.7572,21.278],[-157.765,21.2789],[-157.7782,21.2735],[-157.7931,21.2604],[-157.8096,21.2577],[-157.8211,21.2606],[-157.8241,21.2646],[-157.8253,21.2714],[-157.8319,21.2795],[-157.8457,21.29],[-157.89,21.3065],[-157.894518,21.319632],[-157.898969,21.327391],[-157.90482,21.329172],[-157.918939,21.318615],[-157.917921,21.313781],[-157.913469,21.310983],[-157.910925,21.305768],[-157.952263,21.306531],[-157.950736,21.312509],[-157.951881,21.318742],[-157.967971,21.327986],[-157.973334,21.327426],[-157.989424,21.317984],[-158.0245,21.3093],[-158.044485,21.306011]]]]},\"properties\":{\"name\":\"Hawaii\",\"nation\":\"USA  \"}}]}","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":70001639,"text":"70001639 - 1970 - The strontium isotopic composition of basalts from the Gordo and Juan de Fuca Rises, northeastern Pacific Ocean","interactions":[],"lastModifiedDate":"2020-11-30T16:31:17.047938","indexId":"70001639","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":"The strontium isotopic composition of basalts from the Gordo and Juan de Fuca Rises, northeastern Pacific Ocean","docAbstract":"<div id=\"Abs1-section\" class=\"c-article-section\"><div id=\"Abs1-content\" class=\"c-article-section__content\"><p>The strontium isotopic compositions have been determined for twelve tholeiitic basalts dredged from the Gordo and Juan de Fuca Rises. Sr<sup>87</sup>/Sr<sup>86</sup><span>&nbsp;</span>ratios range from 0.7012 to 0.7031 and average 0.7026. These data, combined with other data from the East Pacific Rise indicate that tholeiite basalts being erupted along the active rises, in the Pacific Ocean, contain less radiogenic Sr<sup>87</sup><span>&nbsp;</span>than basalts erupted on the islands. These isotopic differences between the ocean-ridge tholeiite and the more alkali island basalts indicate that variations in Rb/Sr have persisted in the mantle for billions of years. The possible origins and distribution of these heterogeneties are discussed.</p></div></div><div id=\"cobranding-and-download-availability-text\" class=\"note test-pdf-link\"><br></div>","language":"English","publisher":"Springer","doi":"10.1007/BF00371978","issn":"00107999","usgsCitation":"Hedge, C., and Peterman, Z.E., 1970, The strontium isotopic composition of basalts from the Gordo and Juan de Fuca Rises, northeastern Pacific Ocean: Contributions to Mineralogy and Petrology, v. 27, no. 2, p. 114-120, https://doi.org/10.1007/BF00371978.","productDescription":"7 p.","startPage":"114","endPage":"120","costCenters":[],"links":[{"id":203457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db6357f4","contributors":{"authors":[{"text":"Hedge, C. E.","contributorId":73611,"corporation":false,"usgs":true,"family":"Hedge","given":"C. E.","affiliations":[],"preferred":false,"id":346808,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterman, Z. E.","contributorId":63781,"corporation":false,"usgs":true,"family":"Peterman","given":"Z.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":346807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":5222027,"text":"5222027 - 1970 - Winter wing molt in the western grebe","interactions":[],"lastModifiedDate":"2023-11-27T13:04:33.990416","indexId":"5222027","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":"Winter wing molt in the western grebe","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Oxford Academic","doi":"10.2307/1366028","usgsCitation":"Sibley, F., 1970, Winter wing molt in the western grebe: Condor, v. 72, no. 3, p. 373-373, https://doi.org/10.2307/1366028.","productDescription":"1 p.","startPage":"373","endPage":"373","numberOfPages":"1","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":503023,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/condor/vol72/iss3/31","text":"External Repository"},{"id":197425,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"72","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dae4b07f02db5e01f1","contributors":{"authors":[{"text":"Sibley, F.C.","contributorId":79971,"corporation":false,"usgs":true,"family":"Sibley","given":"F.C.","email":"","affiliations":[],"preferred":false,"id":335306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220178,"text":"5220178 - 1970 - Spring record of the yellow-headed blackbird in Maryland","interactions":[],"lastModifiedDate":"2012-02-02T00:14:40","indexId":"5220178","displayToPublicDate":"2010-06-16T12:18:02","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2687,"text":"Maryland Birdlife","active":true,"publicationSubtype":{"id":10}},"title":"Spring record of the yellow-headed blackbird in Maryland","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Maryland Birdlife","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Sharp, B., 1970, Spring record of the yellow-headed blackbird in Maryland: Maryland Birdlife, v. 26, no. 3.","productDescription":"95","startPage":"95","numberOfPages":"95","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4bf0","contributors":{"authors":[{"text":"Sharp, Brian","contributorId":34606,"corporation":false,"usgs":true,"family":"Sharp","given":"Brian","affiliations":[],"preferred":false,"id":331463,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5221266,"text":"5221266 - 1970 - Recovery of DDT and dieldrin from tissues of Coturnix japonica stepwise during residue analysis","interactions":[],"lastModifiedDate":"2023-10-20T15:48:53.573885","indexId":"5221266","displayToPublicDate":"2010-06-16T12:18:02","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Recovery of DDT and dieldrin from tissues of <i>Coturnix japonica</i> stepwise during residue analysis","title":"Recovery of DDT and dieldrin from tissues of Coturnix japonica stepwise during residue analysis","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/es60044a006","usgsCitation":"Prouty, R.M., and Cromartie, E., 1970, Recovery of DDT and dieldrin from tissues of Coturnix japonica stepwise during residue analysis: Environmental Science & Technology, v. 4, no. 9, p. 768-769, https://doi.org/10.1021/es60044a006.","productDescription":"2 p.","startPage":"768","endPage":"769","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193907,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"9","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db63547f","contributors":{"authors":[{"text":"Prouty, R. M.","contributorId":31349,"corporation":false,"usgs":true,"family":"Prouty","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":333441,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cromartie, E.","contributorId":13926,"corporation":false,"usgs":true,"family":"Cromartie","given":"E.","email":"","affiliations":[],"preferred":false,"id":333440,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5220067,"text":"5220067 - 1970 - Mass movement of black fly larvae on silken threads (Diptera: Simuliidae)","interactions":[],"lastModifiedDate":"2023-02-21T17:09:10.94562","indexId":"5220067","displayToPublicDate":"2010-06-16T12:18:02","publicationYear":"1970","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":798,"text":"Annals of the Entomological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Mass movement of black fly larvae on silken threads (Diptera: Simuliidae)","docAbstract":"<p><span>Stoppage of waterflow in a stream resulted in the migration of massive numbers of black fly larvae on silken threads. Larvae were found on single silken threads, but the heaviest concentrations were on “cables” composed of 25-50 individual silken threads. The larvae were attached in concentric rings around the silken threads and cables.</span></p>","language":"English","publisher":"Oxford Academic Press","doi":"10.1093/aesa/63.2.607","usgsCitation":"Tarshis, I., and Neil, W., 1970, Mass movement of black fly larvae on silken threads (Diptera: Simuliidae): Annals of the Entomological Society of America, v. 63, no. 2, p. 607-610, https://doi.org/10.1093/aesa/63.2.607.","productDescription":"4 p.","startPage":"607","endPage":"610","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193574,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"2","noUsgsAuthors":false,"publicationDate":"1970-03-16","publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fd98","contributors":{"authors":[{"text":"Tarshis, I.B.","contributorId":83625,"corporation":false,"usgs":true,"family":"Tarshis","given":"I.B.","email":"","affiliations":[],"preferred":false,"id":331286,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Neil, W.","contributorId":86063,"corporation":false,"usgs":true,"family":"Neil","given":"W.","email":"","affiliations":[],"preferred":false,"id":331287,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}