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,{"id":66185,"text":"i687 - 1972 - Geologic map of the lower Cache La Poudre River basin, north-central Colorado","interactions":[],"lastModifiedDate":"2014-01-30T11:47:34","indexId":"i687","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"687","subseriesTitle":"NONE","title":"Geologic map of the lower Cache La Poudre River basin, north-central Colorado","language":"ENGLISH","doi":"10.3133/i687","usgsCitation":"Hershey, L., and Schneider, P.A., 1972, Geologic map of the lower Cache La Poudre River basin, north-central Colorado: U.S. Geological Survey IMAP 687, 1 map :col. ;80 x 90 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i687.","productDescription":"1 map :col. ;80 x 90 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106917,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9462.htm","linkFileType":{"id":5,"text":"html"},"description":"9462"},{"id":188474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0687/report-thumb.jpg"},{"id":281733,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0687/plate-1.pdf"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.16666666666667,40.416666666666664 ], [ -105.16666666666667,40.833333333333336 ], [ -104.5,40.833333333333336 ], [ -104.5,40.416666666666664 ], [ -105.16666666666667,40.416666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688a6c","contributors":{"authors":[{"text":"Hershey, L.A.","contributorId":22000,"corporation":false,"usgs":true,"family":"Hershey","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":274124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schneider, P. A. Jr.","contributorId":18771,"corporation":false,"usgs":true,"family":"Schneider","given":"P.","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":274123,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5796,"text":"pp645 - 1972 - Stratigraphy and ammonite fauna of the Graneros Shale and Greenhorn Limestone near Pueblo, Colorado","interactions":[],"lastModifiedDate":"2020-07-01T15:29:48.73254","indexId":"pp645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"645","title":"Stratigraphy and ammonite fauna of the Graneros Shale and Greenhorn Limestone near Pueblo, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp645","usgsCitation":"Cobban, W.A., and Scott, G., 1972, Stratigraphy and ammonite fauna of the Graneros Shale and Greenhorn Limestone near Pueblo, Colorado: U.S. Geological Survey Professional Paper 645, Report: v, 108 p.; 2 Plates: 20.50 x 33.50 inches and 25.00 x 24.00 inches, https://doi.org/10.3133/pp645.","productDescription":"Report: v, 108 p.; 2 Plates: 20.50 x 33.50 inches and 25.00 x 24.00 inches","costCenters":[],"links":[{"id":32481,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0645/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":32480,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0645/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":32479,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0645/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":117716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0645/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Pueblo","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -104.94140625,\n              37.996162679728116\n            ],\n            [\n              -104.27124023437499,\n              37.996162679728116\n            ],\n            [\n              -104.27124023437499,\n              38.54816542304656\n            ],\n            [\n              -104.94140625,\n              38.54816542304656\n            ],\n            [\n              -104.94140625,\n              37.996162679728116\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6aba9f","contributors":{"authors":[{"text":"Cobban, William Aubrey","contributorId":78317,"corporation":false,"usgs":true,"family":"Cobban","given":"William","email":"","middleInitial":"Aubrey","affiliations":[],"preferred":false,"id":151596,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, G. R.","contributorId":61398,"corporation":false,"usgs":true,"family":"Scott","given":"G. R.","affiliations":[],"preferred":false,"id":151595,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42942,"text":"ofr72417 - 1972 - Preliminary Mars chart, Equatorial Region (Mercator Projection)","interactions":[],"lastModifiedDate":"2014-06-11T08:07:48","indexId":"ofr72417","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"72-417","title":"Preliminary Mars chart, Equatorial Region (Mercator Projection)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72417","collaboration":"Prepared in cooperation with the Jet Propulsion Laboratory, California Institute of Technology; National Aeronautics and Space Administration","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Preliminary Mars chart, Equatorial Region (Mercator Projection): U.S. Geological Survey Open-File Report 72-417, 10.11 x 5.89 inches, https://doi.org/10.3133/ofr72417.","productDescription":"10.11 x 5.89 inches","costCenters":[],"links":[{"id":288245,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288244,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0417/plate-1.pdf"}],"scale":"25000000","projection":"Mercator Projection","otherGeospatial":"Mars","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -180.0,-65.0 ], [ -180.0,65.0 ], [ 180.0,65.0 ], [ 180.0,-65.0 ], [ -180.0,-65.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968f0","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":530946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61944,"text":"gq1009 - 1972 - Geologic map of the Halls Gap quadrangle, Lincoln County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:49","indexId":"gq1009","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1009","title":"Geologic map of the Halls Gap quadrangle, Lincoln County, Kentucky","language":"ENGLISH","doi":"10.3133/gq1009","usgsCitation":"Weir, G.W., 1972, Geologic map of the Halls Gap quadrangle, Lincoln County, Kentucky: U.S. Geological Survey Geologic Quadrangle 1009, 1 map., https://doi.org/10.3133/gq1009.","productDescription":"1 map.","costCenters":[],"links":[{"id":107456,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10557.htm","linkFileType":{"id":5,"text":"html"},"description":"10557"},{"id":248230,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1009/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":253056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1009/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.75,37.3675 ], [ -84.75,37.5 ], [ -84.61749999999999,37.5 ], [ -84.61749999999999,37.3675 ], [ -84.75,37.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6985d6","contributors":{"authors":[{"text":"Weir, Gordon Whitney","contributorId":59790,"corporation":false,"usgs":true,"family":"Weir","given":"Gordon","email":"","middleInitial":"Whitney","affiliations":[],"preferred":false,"id":266586,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66423,"text":"i770C - 1972 - Map showing transportation routes in the Parker Quadrangle, Arapahoe and Douglas counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:11:21","indexId":"i770C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"770","subseriesTitle":"NONE","chapter":"C","title":"Map showing transportation routes in the Parker Quadrangle, Arapahoe and Douglas counties, Colorado","language":"ENGLISH","doi":"10.3133/i770C","usgsCitation":"Maberry, J., 1972, Map showing transportation routes in the Parker Quadrangle, Arapahoe and Douglas counties, Colorado: U.S. Geological Survey IMAP 770, 1 map :col. ;58 x 45 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i770C.","productDescription":"1 map :col. ;58 x 45 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":255896,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0770c/plate-1.pdf","size":"4575","linkFileType":{"id":1,"text":"pdf"}},{"id":255897,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0770c/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":255898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0770c/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.86749999999999,39.5 ], [ -104.86749999999999,39.6175 ], [ -104.75,39.6175 ], [ -104.75,39.5 ], [ -104.86749999999999,39.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b11e4b07f02db6a2408","contributors":{"authors":[{"text":"Maberry, J. O.","contributorId":56636,"corporation":false,"usgs":true,"family":"Maberry","given":"J. O.","affiliations":[],"preferred":false,"id":274510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65884,"text":"i710 - 1972 - Surficial geologic map of the Yellowstone National Park","interactions":[],"lastModifiedDate":"2012-02-10T00:11:09","indexId":"i710","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"710","subseriesTitle":"NONE","title":"Surficial geologic map of the Yellowstone National Park","language":"ENGLISH","doi":"10.3133/i710","usgsCitation":"Richmond, G., Pierce, K.L., and Waldrop, H., 1972, Surficial geologic map of the Yellowstone National Park: U.S. Geological Survey IMAP 710, 1 map :col. ;88 x 88 cm., https://doi.org/10.3133/i710.","productDescription":"1 map :col. ;88 x 88 cm.","costCenters":[],"links":[{"id":106925,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9474.htm","linkFileType":{"id":5,"text":"html"},"description":"9474"},{"id":190283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.16666666666667,44.13333333333333 ], [ -111.16666666666667,45.11666666666667 ], [ -109.8,45.11666666666667 ], [ -109.8,44.13333333333333 ], [ -111.16666666666667,44.13333333333333 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688d14","contributors":{"authors":[{"text":"Richmond, G.L.","contributorId":93981,"corporation":false,"usgs":true,"family":"Richmond","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":273700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, K. L.","contributorId":12404,"corporation":false,"usgs":true,"family":"Pierce","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":273699,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waldrop, H.A.","contributorId":105279,"corporation":false,"usgs":true,"family":"Waldrop","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":273701,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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,{"id":70112313,"text":"70112313 - 1972 - ERTS and EROS","interactions":[],"lastModifiedDate":"2017-03-27T14:15:16","indexId":"70112313","displayToPublicDate":"1990-06-12T14:26:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1829,"text":"Geotimes","active":true,"publicationSubtype":{"id":10}},"title":"ERTS and EROS","docAbstract":"<p>In June the National Aeronautics & Space Administration is to launch its first experimental satellite designed to view the Earth systematically with remote-sensing instruments that will provide new information about our resources and environment. The launching will culminate more than 8 years of planning and research by resource agencies of the Federal Government in cooperation with NASA, state and local governments, universities, and industry. The first Earth Resources Technology Satellite, ERTS-A, will be followed a year later by ERTS-B. Analyses of data from them, it is hoped, will lead to design of operational satellites for Earth resources investigations in the future. In the belief that satellite systems will be of significant assistance in meeting its responsibilities to map, monitor, and manage the vast resources and the public lands of the United States, the Department of the Interior assumed a major role in the ERTS-A Experiment.</p>","language":"English","publisher":"American Geological Institute","publisherLocation":"Alexandria, GA","usgsCitation":"Staff, E.P., 1972, ERTS and EROS: Geotimes, v. 17, no. 3, p. 20-23.","productDescription":"4 p.","startPage":"20","endPage":"23","numberOfPages":"4","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288524,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbf2e4b0e83db6d08f01","contributors":{"authors":[{"text":"Staff, EROS Program","contributorId":105233,"corporation":false,"usgs":true,"family":"Staff","given":"EROS","email":"","middleInitial":"Program","affiliations":[],"preferred":false,"id":494658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175925,"text":"70175925 - 1972 - Ground-water data in the Corvallis-Albany area, central Willamette Valley, Oregon","interactions":[],"lastModifiedDate":"2016-08-22T08:45:40","indexId":"70175925","displayToPublicDate":"1974-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":115,"text":"Ground Water Report","active":false,"publicationSubtype":{"id":2}},"title":"Ground-water data in the Corvallis-Albany area, central Willamette Valley, Oregon","docAbstract":"<p><span>THE CORVALLIS-ALBANY AREA IS PART OF THE ALLUVIAL PLAIN THAT LIES BETWEEN THE CASCADE AND COAST RANGES IN THE CENTRAL WILLAMETTE VALLEY IN NORTHWESTERN OREGON. THE ALLUVIAL DEPOSITS (SAND AND GRAVEL) OF THE VALLEY PLAIN CONTAIN THE MOST PRODUCTIVE AQUIFERS IN THE AREA AND ARE CONSIDERED TO BE THE ONLY UNITS FEASIBLE FOR LARGE-SCALE DEVELOPMENT OF GROUNDWATER SUPPLIES. DURING 1971 THE SEASONAL DECLINE OF WATER LEVELS FROM WINTER TO LATE SUMMER AVERAGED ABOUT 10 FEET FOR THE ALLUVIAL DEPOSITS. THE SEASONAL CHANGE OF STORAGE WAS ESTIMATED TO BE ABOUT 130,000 ACRE-FEET. OF THIS VOLUME, ABOUT 14,000 ACRE-FEET WAS PUMPED FROM WELLS; THE REST WAS DISCHARGED THROUGH SEEPS AND SPRINGS BY EVAPOTRANSPIRATION. THE DIFFERENCE BETWEEN PUMPAGE AND NATURAL DISCHARGE INDICATES THAT A GREAT QUANTITY OF ADDITIONAL WATER IS AVAILABLE FOR DEVELOPMENT. THE STORAGE CAPACITY OF THE ALLUVIAL AQUIFERS IS ESTIMATED TO BE ABOUT 750,000 ACRE-FEET BETWEEN DEPTHS OF 10 AND 100 FEET. WATER FROM THE ALLUVIAL DEPOSITS IS CHEMICALLY SUITABLE FOR ALL USES, AS IS MOST OF THE WATER FROM PERCHED-WATER BODIES IN THE OLDER SEDIMENTARY AND VOLCANIC ROCKS.</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Frank, F.J., and Johnson, N.A., 1972, Ground-water data in the Corvallis-Albany area, central Willamette Valley, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":327129,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","city":"Corvallis-Albany","otherGeospatial":"Willamette Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bc228ce4b03fd6b7de17cd","contributors":{"authors":[{"text":"Frank, F. J.","contributorId":95037,"corporation":false,"usgs":true,"family":"Frank","given":"F.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":646559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, N. A.","contributorId":74406,"corporation":false,"usgs":true,"family":"Johnson","given":"N.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":646560,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70173978,"text":"70173978 - 1972 - Falling-stream turbidimeter as a means of measuring sediment concentrations in streams","interactions":[],"lastModifiedDate":"2016-06-22T08:10:31","indexId":"70173978","displayToPublicDate":"1973-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Falling-stream turbidimeter as a means of measuring sediment concentrations in streams","docAbstract":"<p>An optical (photocell) sensing device was used to measure the relative transparency characteristics of sediment suspensions with a view toward improving our ability to measure the temporal variations of suspended-sediment concentration moving in streams. The instrument used was a commercial \"falling stream\" turbidimeter that measured the relative transparency of a gravity induced smooth flat sample stream formed as the flow drops vertically from an orifice.</p>\n<p>Output results were recorded on a strip-chart recorder as a function of concentration, up to about 100,000 mg/2, for a range of particle sizes and for three kinds of sediment--a fine sand, a silty alluvial soil, and a clayey residual soil. The sensitivity range was improved by use of both the 1/8- and 1/16-inch thick orifices. The use of the two orifice or nozzle sizes provided data useful in evaluation of the effect of particle size and type of sediment at different concentrations. The unique relative transparency-concentration relationships were more linear for coarse than for fine sediments of a given kind. It was concluded that curvature in this relationship resulted from light reflections from the surface of the particles and (or) the fact that some particles moved through the system while in the \"shadow\" of other particles closer to the light source.</p>\n<p>The ratio of suspended-sediment concentration to the square root of the median particle size of sand-sized sediments was found to be a useful parameter for elimination of the effect of particle size in the relative transparency-concentration relationships. Thus it was possible to evaluate the effect of the different type of sediment on the relative transparency independent of particle size. The use of this parameter to eliminate the effect of particle size was unsuccessful for finer sediments. -</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/70173978","usgsCitation":"Guy, H., and Olson, R., 1972, Falling-stream turbidimeter as a means of measuring sediment concentrations in streams: Open-File Report, 58 p., https://doi.org/10.3133/70173978.","productDescription":"58 p.","numberOfPages":"62","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":324035,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70173978.jpg"},{"id":324183,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70173978/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913bae4b07657d19ff052","contributors":{"authors":[{"text":"Guy, Harold P.","contributorId":6434,"corporation":false,"usgs":true,"family":"Guy","given":"Harold P.","affiliations":[],"preferred":false,"id":639911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, Richard C.","contributorId":172202,"corporation":false,"usgs":false,"family":"Olson","given":"Richard C.","affiliations":[],"preferred":false,"id":639912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207472,"text":"70207472 - 1972 - Interstitial water studies on small core samples, leg 14 ","interactions":[],"lastModifiedDate":"2019-12-19T17:49:21","indexId":"70207472","displayToPublicDate":"1972-12-31T17:47:21","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, leg 14 ","docAbstract":"<p>The interstitial waters from the sediments cored on Leg 14 exhibit characteristic compositional trends with three important exceptions. At most of the sites, the changes in Na and Cl are very small while enrichment of Ca and Sr and depletion of Mg and SO<sub>4</sub> is typical of patterns observed in similar types of sediment recovered on previous legs. At Sites 139 and 140, off the African coast, and Site 144, off the coast of South America, systematic increases in concentration with depth are found for Na and Cl. At these sites, the concentration changes, in Ca, Mg, SO<sub>4</sub> and Sr generally follow diagenic patterns observed previously, but there is some indication of other factors affecting Mg concentrations. All analyses reported here, with the exception of bulk water content and pH, were carried out on water samples which were squeezed from the sediments on board ship and preserved by heat-sealing in lengths of polyethylene tubing. Analytical methods were identical to those outlined in earlier volumes of this series. We wish to thank Wen Chang, James O'Neill and Irene Uhlitzsch for their assistance in conducting the laboratory determinations and data reduction</p>","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.14.121.1972","usgsCitation":"Waterman, L., Sayles, F., and Manheim, F.T., 1972, Interstitial water studies on small core samples, leg 14 : Initial reports of the Deep Sea Drilling Project, v. 14, p. 753-761, https://doi.org/10.2973/dsdp.proc.14.121.1972.","productDescription":"9 p.","startPage":"753","endPage":"761","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488852,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.14.121.1972","text":"Publisher Index Page"},{"id":370531,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Waterman, L.S.","contributorId":25474,"corporation":false,"usgs":true,"family":"Waterman","given":"L.S.","affiliations":[],"preferred":false,"id":778179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":778180,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778181,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70207470,"text":"70207470 - 1972 - Interstitial water studies on small core samples, leg XI","interactions":[],"lastModifiedDate":"2019-12-19T17:37:42","indexId":"70207470","displayToPublicDate":"1972-12-31T17:27:41","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1997,"text":"Initial reports of the Deep Sea Drilling Project","active":true,"publicationSubtype":{"id":10}},"title":"Interstitial water studies on small core samples, leg XI","docAbstract":"<p>The sediments cored at Sites 98, 99 and 100 are predominantly biogenic; those cored at Sites 101 through 106 are composed mainly of terrigenous material. As reported previously, most constituents in pore waters from the biogenic oozes exhibit minor changes in chemistry relative to sea water. In the terrigenous-hemipelagic sediments interstitial solutions initially of sea water composition have undergone considerable reaction. These reactions have produced large changes in the concentrations of calcium (Ca), magnesium (Mg), sulfate (SO<sub>4</sub>) and HCO<sub>3</sub> relative to sea water. In addition, this set of samples documents significant diagenetic alteration of sodium (Na) and chloride (Cl). Potassium exhibits little change in most samples, but in a few instances is depleted at depth. </p><p>The analytical techniques employed are identical to those described in earlier volumes of the Initial Reports of the Deep Sea Drilling Project. In an effort to identify alteration of sample composition during storage, salinity determinations<sup>2</sup> are made on the pore solution immediately upon their recovery from the sediments. The same measurement is made in the laboratory when the sample containers are opened for analysis. Occasionally evidence of evaporation is found as in Sample 104-2-5; the shipboard salinity was 32%o, while the laboratory measurement yielded 38%o. Changes of 3 to 4 per cent were also noted in several other samples as noted in the tables. </p><p>Adjustment of the analytically determined concentrations has been made and the corrected values presented in Tables 1 and 2. A large part of the work involved in the analyses of these samples has been done by Irene Uhlitzsch; we are indebted to her for the invaluable assistance she has rendered.</p>","language":"English","publisher":"National Science Foundation","doi":"10.2973/dsdp.proc.11.134.1972","usgsCitation":"Sayles, F., Manheim, F.T., and Waterman, L., 1972, Interstitial water studies on small core samples, leg XI: Initial reports of the Deep Sea Drilling Project, v. 11, p. 997-1007, https://doi.org/10.2973/dsdp.proc.11.134.1972.","productDescription":"12 p.","startPage":"997","endPage":"1007","costCenters":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"links":[{"id":488419,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"http://doi.org/10.2973/dsdp.proc.11.134.1972","text":"Publisher Index Page"},{"id":370529,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Sayles, F.L.","contributorId":77657,"corporation":false,"usgs":true,"family":"Sayles","given":"F.L.","email":"","affiliations":[],"preferred":false,"id":778170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Manheim, Frank T. 0000-0003-4005-4524","orcid":"https://orcid.org/0000-0003-4005-4524","contributorId":20770,"corporation":false,"usgs":true,"family":"Manheim","given":"Frank","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":778171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waterman, L.S.","contributorId":25474,"corporation":false,"usgs":true,"family":"Waterman","given":"L.S.","affiliations":[],"preferred":false,"id":778172,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70207141,"text":"70207141 - 1972 - Pliocene uplift of the grand canyon region - time of drainage adjustment","interactions":[],"lastModifiedDate":"2019-12-09T10:10:15","indexId":"70207141","displayToPublicDate":"1972-12-31T10:05:29","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Pliocene uplift of the grand canyon region - time of drainage adjustment","docAbstract":"<p><span>Tertiary gravel deposits in ancient stream channels along the southern margin of the Colorado Plateaus of northern Arizona show by composition and structure that these deposits came from sources to the south and southwest at a time when central Arizona stood higher than the present Grand Canyon region. Three cobbles of basalt included in the gravel deposits have K-Ar ages of about 10.0 m.y., 12.2, and 12.4 m.y. showing that the major uplift of the plateau in northern Arizona had not taken place at that time. The present south-flowing drainage of the Verde River and neighboring streams resulted from final elevation of the northern Arizona region relative to central Arizona, and must have developed well before about 5 m.y. - the age of some basalts that flowed into the Verde Valley. Thus, the major relative uplift of the southern part of the Colorado Plateaus must have occurred within the 5 to 10 m.y. interval, or in early to middle Pliocene time. This time of uplift also was the time of major canyon erosion, including the cutting of Grand Canyon, within the Plateaus province. © 1972, The Geological Society of America, Inc.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1972)83[1923:PUOTGC]2.0.CO;2","issn":"00167606","usgsCitation":"McKee, E., and McKee, E., 1972, Pliocene uplift of the grand canyon region - time of drainage adjustment: Geological Society of America Bulletin, v. 83, no. 7, p. 1923-1932, https://doi.org/10.1130/0016-7606(1972)83[1923:PUOTGC]2.0.CO;2.","productDescription":"10 p. 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 \"}}]}","volume":"83","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"McKee, E. D.","contributorId":105802,"corporation":false,"usgs":true,"family":"McKee","given":"E. D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":776940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, E.H.","contributorId":20736,"corporation":false,"usgs":true,"family":"McKee","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":776941,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70206730,"text":"70206730 - 1972 - Hawaiian-emperor chain and its relation to cenozoic circumpacific tectonics","interactions":[],"lastModifiedDate":"2019-11-19T07:48:26","indexId":"70206730","displayToPublicDate":"1972-12-31T07:43:57","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Hawaiian-emperor chain and its relation to cenozoic circumpacific tectonics","docAbstract":"<p><span>The Hawaiian Ridge and Emperor Seamounts appear to form a single chain of tholeiitic shield volcanoes that erupted sequentially on the sea floor of the central Pacific Ocean during Tertiary and Quaternary time. The chain cuts obliquely across the older Cretaceous structural patterns of that sea floor. While the pattern of the chain as a whole is linear, the individual volcanoes lie on short, sigmoidal, en echelon loci that are subparallel with respect to each other and that may represent extensional features in the crust and upper mantle. In general, the order of eurption progressed from northwest to southeaśt along the chain, but the rate of progression of volcanism along individual loci is nonlinear where best studied in the southeastern part of the chain. Furthermore, simultaneous eruptions appear to have occurred within a distance along the chain of about 200 to 400 km. The available data are consistent with a genesis related to the motion of the Pacific crust over a melting spot in the mantle. This melting spot, which may be due to either excess heat or pressure release, appears to have a diameter of about 300 km and is presently centered slightly north of the island of Hawaii. We concur with the idea that the bend in the Hawaiian-Emperor chain probably reflects a significant change in the motion of the Pacific plate. Our best estimate of the age of the Hawaiian-Emperor bend, based on the existing radiometric data, is 24.6 ± 2.5 m.y., which correlates with a time of increased tectonic activity in the western Pacific island arcs and along the northern and eastern boundaries of the Pacific plate. The vector change in the motion of the Pacific plate (with respect to the melting spot) that is required to produce the bend is about 12 cm/yr in a west-southwest-ward direction. © 1972, The Geological Society of America, Inc.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1972)83[601:HCAIRT]2.0.CO;2","issn":"00167606","usgsCitation":"Jackson, E., Silver, E.A., and Dalrymple, G.B., 1972, Hawaiian-emperor chain and its relation to cenozoic circumpacific tectonics: Geological Society of America Bulletin, v. 83, no. 3, p. 601-618, https://doi.org/10.1130/0016-7606(1972)83[601:HCAIRT]2.0.CO;2.","productDescription":"18 p. 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 \"}}]}","volume":"83","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Jackson, E.D.","contributorId":99524,"corporation":false,"usgs":true,"family":"Jackson","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":775574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silver, E. A.","contributorId":18491,"corporation":false,"usgs":true,"family":"Silver","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":775575,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dalrymple, G. B.","contributorId":10407,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":775576,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70198184,"text":"70198184 - 1972 - Structure of Sierra Madera, Texas, as a guide to central peaks of lunar craters","interactions":[],"lastModifiedDate":"2018-07-18T15:24:14","indexId":"70198184","displayToPublicDate":"1972-12-31T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Structure of Sierra Madera, Texas, as a guide to central peaks of lunar craters","docAbstract":"<p>Like hundreds of other lunar craters of probable impact origin, Copernicus contains central peaks presumed to expose rocks uplifted from beneath the crater floor. A possible analog of these peaks on Earth is the central uplift of the Sierra Madera cryptoexplosion structure, a probable impact scar (astrobleme) in stratified Permian and Cretaceous rocks of west Texas. The most conspicuous part of this 12-km-wide structure is its central uplift, 6 to 8 km across, in which the oldest rocks have been raised 1,200 m above their normal position. The uplift is surrounded by a structural depression, beyond which is a concentric rim containing some folds and circumferential normal faults with downthrow toward the center. The intensity of folding and faulting increases inward from the flanks of the central uplift toward a central zone about 2 km across where dips and fold plunges are near vertical or overturned. As in salt domes, the beds moved inward as well as upward to occupy their present positions, causing faulting and radial folding due to crowding in the center. Repetition by folding due to inward movement of upper beds over lower appears to have been followed by upward movement of the core of the uplift pulling away from the flanks by faulting. Minor outward-directed thrusting may have been caused by gravitational spreading of the rising dome. The structural depression surrounding the uplift resulted from tectonic thinning accompanying the inward movement of rocks in the uplift.</p><p>Analogy with experimental craters and with other cryptoexplosion structures indicates that the uplift at Sierra Madera protruded into a crater (since destroyed by erosion) that was about 12 km across. Inasmuch as the rocks forming such uplifts are derived from below the crater floors, analogous peaks in lunar craters such as Copernicus may offer samples of lunar crust uplifted from distances below the crater floor on the order of one-tenth of the crater diameter.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1972)83[2795:SOSMTA]2.0.CO;2","usgsCitation":"Howard, K.A., Offield, T.W., and Wilshire, H.G., 1972, Structure of Sierra Madera, Texas, as a guide to central peaks of lunar craters: GSA Bulletin, v. 83, no. 9, p. 2795-2808, https://doi.org/10.1130/0016-7606(1972)83[2795:SOSMTA]2.0.CO;2.","productDescription":"14 p.","startPage":"2795","endPage":"2808","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355810,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Sierra Madera crater","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.326416015625,\n              29.878755346037977\n            ],\n            [\n              -101.25,\n              29.878755346037977\n            ],\n            [\n              -101.25,\n              31.662732913235317\n            ],\n            [\n              -103.326416015625,\n              31.662732913235317\n            ],\n            [\n              -103.326416015625,\n              29.878755346037977\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"83","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":740470,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Offield, Terry W.","contributorId":15196,"corporation":false,"usgs":true,"family":"Offield","given":"Terry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":740471,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilshire, H. G.","contributorId":36125,"corporation":false,"usgs":false,"family":"Wilshire","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":740472,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70197654,"text":"70197654 - 1972 - Paleomagnetic correlations and Potassium-Argon dating of Middle Tertiary ash-flow sheets in the eastern Great Basin, Nevada and Utah","interactions":[],"lastModifiedDate":"2018-06-15T11:38:42","indexId":"70197654","displayToPublicDate":"1972-12-31T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Paleomagnetic correlations and Potassium-Argon dating of Middle Tertiary ash-flow sheets in the eastern Great Basin, Nevada and Utah","docAbstract":"<p><span>Directions of natural remanent magnetization are used to identify and correlate individual cooling units in the middle Tertiary ash-flow province in central and eastern Nevada and western Utah. Potassium-argon dating indicates that the minimum time between eruptions of individual but genetically related ash-flow cooling units is on the order of 0.8 m.y. As this interval is long in comparison with the secular variation of the direction of the geomagnetic field, in a given volcanic province the direction of natural thermoremanent magnetization is a unique characteristic of each cooling unit. Ash-flow sheets investigated include the Stone Cabin Formation, the tuff of Pancake Summit, the Windous Butte Formation, the Needles Range Formation, the Bates Mountain Tuff, and the tuff of Clipper Gap, of Oliogcene to early Miocene age. The original areas of individual ash-flow cooling units are as great as 8,000 km</span><sup>2</sup><span>; the volumes, 1,300 km</span><sup>3</sup><span>. The paleomagnetic correlations, made over distances up to 200 km, confirm most of the previously made lithologic correlations and allow more accurate delineation of single cooling units. These correlations are particularly useful in those parts of the Basin and Range province where the Tertiary stratigraphic section consists mainly of ash-flow sheets, and the outcrops are confined to mountain ranges that are separated by alluvium-filled valleys.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1972)83[1619:PCAPDO]2.0.CO;2","usgsCitation":"Grommé, C., McKee, E., and Blake, M.C., 1972, Paleomagnetic correlations and Potassium-Argon dating of Middle Tertiary ash-flow sheets in the eastern Great Basin, Nevada and Utah: GSA Bulletin, v. 83, no. 6, p. 1619-1638, https://doi.org/10.1130/0016-7606(1972)83[1619:PCAPDO]2.0.CO;2.","productDescription":"20 p.","startPage":"1619","endPage":"1638","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355073,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada, Utah","volume":"83","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Grommé, C. S.","contributorId":38558,"corporation":false,"usgs":true,"family":"Grommé","given":"C. S.","affiliations":[],"preferred":false,"id":738084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, E.H.","contributorId":20736,"corporation":false,"usgs":true,"family":"McKee","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":738085,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blake, M. Clark Jr.","contributorId":56675,"corporation":false,"usgs":true,"family":"Blake","given":"M.","suffix":"Jr.","email":"","middleInitial":"Clark","affiliations":[],"preferred":false,"id":738086,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70198181,"text":"70198181 - 1972 - Geologic setting of the Apollo 15 samples","interactions":[],"lastModifiedDate":"2018-07-19T09:49:39","indexId":"70198181","displayToPublicDate":"1972-12-31T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geologic setting of the Apollo 15 samples","docAbstract":"<p><span>The samples and photographs returned from the Apollo 15 site show that Hadley Delta is largely underlain by breccias whose clasts are mainly fragments of coarse-grained feldspathic rocks and nonmare-type basalt. Conspicuous sets of lineaments, visible in surface and orbital photographs of Mount Hadley and Hadley Delta, may represent systematic layering or fracture sets. The mare surface, with regolith about 5 meters thick, is underlain by two major basalt types, at least one of which has extensive lateral continuity and is exposed in the upper wall of Hadley Rille. Gradual erosional recession of the edges and filing of the interior of the rille by talus have contributed to the present cross sectional profile.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.175.4020.407","usgsCitation":"Swann, G., Bailey, N.G., Batson, R.M., Freeman, V.L., Hait, M., Holt, H.E., Larson, K., Reed, V.S., Schaber, G.G., Sutton, R.L., Wolfe, E., Howard, K.A., Wilshire, H.G., Head, J., Irwin, J., Scott, D., Muehlberger, W., Silver, L.T., and Rennilson, J.J., 1972, Geologic setting of the Apollo 15 samples: Science, v. 175, no. 4020, p. 407-415, https://doi.org/10.1126/science.175.4020.407.","productDescription":"9 p.","startPage":"407","endPage":"415","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355809,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"175","issue":"4020","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Swann, G.A.","contributorId":8859,"corporation":false,"usgs":true,"family":"Swann","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":740445,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bailey, N. G.","contributorId":14408,"corporation":false,"usgs":true,"family":"Bailey","given":"N.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":740446,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Batson, R. M.","contributorId":76714,"corporation":false,"usgs":true,"family":"Batson","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":740447,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Freeman, V. L.","contributorId":52958,"corporation":false,"usgs":true,"family":"Freeman","given":"V.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":740448,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hait, M. H.","contributorId":59052,"corporation":false,"usgs":true,"family":"Hait","given":"M. H.","affiliations":[],"preferred":false,"id":740449,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Holt, H. E.","contributorId":64694,"corporation":false,"usgs":true,"family":"Holt","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":740450,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Larson, K.B.","contributorId":55410,"corporation":false,"usgs":true,"family":"Larson","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":740451,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Reed, V. S.","contributorId":58255,"corporation":false,"usgs":true,"family":"Reed","given":"V.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":740452,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Schaber, G. G.","contributorId":68300,"corporation":false,"usgs":true,"family":"Schaber","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":740453,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sutton, R. L.","contributorId":24364,"corporation":false,"usgs":true,"family":"Sutton","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":740454,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Wolfe, E.W.","contributorId":57470,"corporation":false,"usgs":true,"family":"Wolfe","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":740455,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Howard, Keith A. 0000-0002-6462-2947 khoward@usgs.gov","orcid":"https://orcid.org/0000-0002-6462-2947","contributorId":3439,"corporation":false,"usgs":true,"family":"Howard","given":"Keith","email":"khoward@usgs.gov","middleInitial":"A.","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":740456,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Wilshire, H. G.","contributorId":36125,"corporation":false,"usgs":false,"family":"Wilshire","given":"H.","middleInitial":"G.","affiliations":[],"preferred":false,"id":740457,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Head, J.W.","contributorId":67982,"corporation":false,"usgs":true,"family":"Head","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":740458,"contributorType":{"id":1,"text":"Authors"},"rank":14},{"text":"Irwin, J.B.","contributorId":39270,"corporation":false,"usgs":true,"family":"Irwin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":740459,"contributorType":{"id":1,"text":"Authors"},"rank":15},{"text":"Scott, D.R.","contributorId":86508,"corporation":false,"usgs":true,"family":"Scott","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":740460,"contributorType":{"id":1,"text":"Authors"},"rank":16},{"text":"Muehlberger, W.R.","contributorId":66732,"corporation":false,"usgs":true,"family":"Muehlberger","given":"W.R.","affiliations":[],"preferred":false,"id":740461,"contributorType":{"id":1,"text":"Authors"},"rank":17},{"text":"Silver, L. T.","contributorId":46968,"corporation":false,"usgs":true,"family":"Silver","given":"L.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":740462,"contributorType":{"id":1,"text":"Authors"},"rank":18},{"text":"Rennilson, J. J.","contributorId":107336,"corporation":false,"usgs":true,"family":"Rennilson","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":740463,"contributorType":{"id":1,"text":"Authors"},"rank":19}]}}
,{"id":5223308,"text":"5223308 - 1972 - Eastward migration of blue-winged teal","interactions":[],"lastModifiedDate":"2025-02-21T16:54:53.760943","indexId":"5223308","displayToPublicDate":"1972-10-06T00:00:00","publicationYear":"1972","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":"Eastward migration of blue-winged teal","docAbstract":"<p>Of 3,789 recoveries of blue-winged teal (<i>Anas discors</i>) banded prior to the hunting season in the prairie pothole region, 183 (4.8 percent) were recovered, due east in New England, Ontario, Quebec, and the Maritime Provinces during the subsequent hunting season. Of 19 recoveries looked at in detail, all were banded as either hatching-year (flying young) or local (flightless young) birds. A blue-winged teal banded in Minnesota in September was retrapped in October in South Carolina, before being shot later that month in Colombia, South America.</p>","language":"English","publisher":"Wiley","doi":"10.2307/3799262","usgsCitation":"Sharp, B., 1972, Eastward migration of blue-winged teal: Journal of Wildlife Management, v. 36, no. 4, p. 1273-1277, https://doi.org/10.2307/3799262.","productDescription":"5 p.","startPage":"1273","endPage":"1277","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199687,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"North Dakota, Minnesota","otherGeospatial":"Alberta, Saskatchewan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.1520732984464,\n              59.92509917759563\n            ],\n            [\n              -120.1690210759753,\n              53.861418873618376\n            ],\n            [\n              -114.30334555422223,\n              49.729112484974586\n            ],\n            [\n              -103.89236975427357,\n              45.747832694335045\n            ],\n            [\n              -97.466221646018,\n              45.75362612194698\n            ],\n            [\n              -96.3112252567795,\n              43.66239757659807\n            ],\n            [\n              -90.47288416474126,\n              43.623425078704315\n            ],\n            [\n              -92.64696983604352,\n              46.08348138659872\n            ],\n            [\n              -89.99666740104907,\n              47.88552887744924\n            ],\n            [\n              -94.73762141579002,\n              49.07380418744488\n            ],\n            [\n              -101.43958666144323,\n              49.24157507682183\n            ],\n            [\n              -102.70581818256466,\n              59.65559957942301\n            ],\n            [\n              -120.1520732984464,\n              59.92509917759563\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"36","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627f15","contributors":{"authors":[{"text":"Sharp, Brian","contributorId":34606,"corporation":false,"usgs":true,"family":"Sharp","given":"Brian","affiliations":[],"preferred":false,"id":338376,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220959,"text":"5220959 - 1972 - Migration patterns and wintering localities of American ospreys","interactions":[],"lastModifiedDate":"2025-02-21T17:00:42.624605","indexId":"5220959","displayToPublicDate":"1972-10-06T00:00:00","publicationYear":"1972","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":"Migration patterns and wintering localities of American ospreys","docAbstract":"<p>North American ospreys (<i>Pandion haliaetus carolinensis</i>), banded primarily in the Middle Atlantic States and in New England, apparently migrate to their winter grounds in the West Indies and South America on a broad front. Ospreys do not return to the United States as 1-year-olds, but an estimated 28 to 55 percent return to their natal vicinity (state where hatched or an adjacent state) as 2-year-olds. The 2-year-olds (presumably nonbreeders) are estimated to represent 5 to 10 percent of the population on the northern breeding grounds. Nest studies suggest that about 6 percent of the population on the breeding grounds consists of nonbreeders (presumably the 2-year-olds). These birds are associated with nests but do not lay eggs or exhibit brooding behavior. The point to be made to individuals conducting nest studies on ospreys is that nests should not be classified as active if eggs are not laid, even though a pair is present. If nests with no eggs are excluded from studies, we believe the observed recruitment rates can be validly compared with the recruitment standard (production rate required to maintain a stable population) of Henny and Wight (1969).</p>","language":"English","publisher":"Wiley","doi":"10.2307/3799242","usgsCitation":"Henny, C.J., and Van Velzen, W., 1972, Migration patterns and wintering localities of American ospreys: Journal of Wildlife Management, v. 36, no. 4, p. 1133-1141, https://doi.org/10.2307/3799242.","productDescription":"9 p.","startPage":"1133","endPage":"1141","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198217,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635540","contributors":{"authors":[{"text":"Henny, Charles J.","contributorId":12578,"corporation":false,"usgs":true,"family":"Henny","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":332757,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Velzen, W.T.","contributorId":72080,"corporation":false,"usgs":true,"family":"Van Velzen","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":332758,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70205796,"text":"70205796 - 1972 - Massive sulfide copper deposits of the Ergani-Maden area, Southeastern Turkey","interactions":[],"lastModifiedDate":"2019-10-03T13:20:37","indexId":"70205796","displayToPublicDate":"1972-10-03T13:15:30","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Massive sulfide copper deposits of the Ergani-Maden area, Southeastern Turkey","docAbstract":"<p>The copper deposits of the Ergani-Maden area, in the Taurus Mountains of southeastern Turkey, have been a major source of copper for more than 4,000 years. The area is underlain by gently dipping mudstones interlayered with mafic volcanic rocks and lenticular beds of limestone, mainly of Eocene age. The layered rocks were intruded and slightly metamorphosed by large masses of gabbro and related mafic rocks that are now largely serpentinized. The copper deposits are in an east-trending belt about 20 km long, near the center of which is the town of Maden. A broad geochemical anomaly extends north-northwest and south-southeast from this belt, its axis passing near Maden. Near the mines the main igneous mass has a gently dipping roof and steep sides. Around and south of Maden, where the mass has barely been unroofed, are many roof pendants and remnants of sedimentary and volcanic material. One of these contains the largest mine in the area--the Ana Yatak. The largest deposit, the Aria Yatak ore body, occurs in a canoe-shaped pendant of mudstone that occupies atrough about 1 km long and 1/2 km wide in the top of the intrusive. The present vertical extent is about 170 meters. In the central and western parts of the trough the mudstone is chloritized and partly replaced by ore minerals. The main ore body is about 550 X 300 X 50 m in maximum dimensions. It consists mainly of pyrite and chalcopyrite, and locally it contains abundant magnetite or pyrrhotite. The gangue consists predominantly of chlorite, smaller amounts of quartz, and very minor amounts of calcite and barite. The massive sulfide ore body is underlain by \"impregnation ore\" in which veinlets and irregular small masses of sulfides are embedded in chloritized mudstone. A zone rich in supergene chalcocite, corellite, and bornite lies between the sulfide mass and the well-developed gossan in many places, and this was extensively mined in ancient times. The Mihrap Dagi mine, about 1 km northwest of the Aria Yatak deposit, is also near a contact between the intrusive and the sedimentary rock. It too contains a massive sulfide ore body accompanied by chloritized rock, but it contains little \"impregnation ore.\" In the Ergani-Maden area, ore deposition followed a long history of sedimentation, lithification, faulting, intrusion of mafic igneous rocks, serpentinization, and further faulting, and was part of a broad-scale introduction of metal into the sedimentary, extrusive, and intrusive rocks. Thus it is epigenetic. The major ore bodies are fracturecontrolled replacement masses. Adularia which occurs in veins a few hundred meters south of the main sulfide ore bodies is inferred to have formed contemporaneously with the sulfide and shows a potassium-argon age of 31.5 +/- 0.8 m.y. If this inference is correcthe deposits formed during middle Oligocene or slightly later. </p>","language":"English","publisher":" Economic Geology Publishing Company","doi":"10.2113/gsecongeo.67.6.701","issn":" 0361-0128","usgsCitation":"Griffitts, W., Albers, J.P., and Oener, O., 1972, Massive sulfide copper deposits of the Ergani-Maden area, Southeastern Turkey: Economic Geology, v. 67, no. 6, p. 701-716, https://doi.org/10.2113/gsecongeo.67.6.701.","productDescription":"16 p.","startPage":"701","endPage":"716","costCenters":[],"links":[{"id":367972,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Turkey","otherGeospatial":"Ergani-Maden ","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              39.364013671875,\n              38.09998264736481\n            ],\n            [\n              40.36376953125,\n              38.09998264736481\n            ],\n            [\n              40.36376953125,\n              38.74551518488265\n            ],\n            [\n              39.364013671875,\n              38.74551518488265\n            ],\n            [\n              39.364013671875,\n              38.09998264736481\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"67","issue":"6","noUsgsAuthors":false,"publicationDate":"1972-10-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Griffitts, W. R.","contributorId":116293,"corporation":false,"usgs":true,"family":"Griffitts","given":"W. R.","affiliations":[],"preferred":false,"id":772381,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Albers, J. P.","contributorId":81505,"corporation":false,"usgs":true,"family":"Albers","given":"J.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":772382,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oener, Oemer","contributorId":219495,"corporation":false,"usgs":false,"family":"Oener","given":"Oemer","email":"","affiliations":[],"preferred":false,"id":772383,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70230464,"text":"70230464 - 1972 - Summary of data collected for the Miami River Restoration Project during March and September, 1971","interactions":[],"lastModifiedDate":"2025-04-25T15:49:22.705736","indexId":"70230464","displayToPublicDate":"1972-10-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"FL 72-020","displayTitle":"Summary of Data Collected for the Miami River Restoration Project During March and September, 1971","title":"Summary of data collected for the Miami River Restoration Project during March and September, 1971","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70230464","collaboration":"Prepared in cooperation with the Florida Department of Natural Resources, Bureau of Geology, Central and Southern Florida Flood Control District, Dade County, Water Control Division, and City of Miami, Department of Water and Sewers","usgsCitation":"Meyer, F., and Wimberly, E., 1972, Summary of data collected for the Miami River Restoration Project during March and September, 1971: Open-File Report FL 72-020, 15 p., https://doi.org/10.3133/70230464.","productDescription":"15 p.","numberOfPages":"15","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":398640,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70230464/coverthb.jpg"},{"id":398641,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70230464/ofr-fl-72020.pdf","text":"Report","size":"2.33 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR FL 72-020"}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.35186080617744,\n              25.87475299004177\n            ],\n            [\n              -80.35186080617744,\n              25.72746259685377\n            ],\n            [\n              -80.16140768662913,\n              25.72746259685377\n            ],\n            [\n              -80.16140768662913,\n              25.87475299004177\n            ],\n            [\n              -80.35186080617744,\n              25.87475299004177\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"1972-10-01","noUsgsAuthors":false,"publicationDate":"1972-10-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Meyer, F.W.","contributorId":25150,"corporation":false,"usgs":true,"family":"Meyer","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":840487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wimberly, E.T.","contributorId":50180,"corporation":false,"usgs":true,"family":"Wimberly","given":"E.T.","email":"","affiliations":[],"preferred":false,"id":840488,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5222233,"text":"5222233 - 1972 - Normal yeast flora of the upper digestive tract of some wild columbids","interactions":[],"lastModifiedDate":"2025-04-04T16:17:18.328874","indexId":"5222233","displayToPublicDate":"1972-10-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"title":"Normal yeast flora of the upper digestive tract of some wild columbids","docAbstract":"<p><span>Seven species of pigeons and doves were cultured for yeasts in the upper digestive tract. The following list gives the isolation rate for each columbid species and the yeasts cultured from them: feral pigeon&nbsp;</span><i>Colwnha livia</i><span>&nbsp;(Gmelin) 95% —&nbsp;</span><i>Candida albicans</i><span>&nbsp;(Robin) Berkhout,&nbsp;</span><i>C. tropicalis</i><span>&nbsp;(Castellani) Berkhout,&nbsp;</span><i>C. krusei</i><span>&nbsp;(Cast.) Berkhout,&nbsp;</span><i>C. guilliermondii</i><span>&nbsp;(Cast.) Langeron et Guerra,&nbsp;</span><i>Torulopsis glabrata</i><span>&nbsp;(Anderson) Lodder et De Vries,&nbsp;</span><i>Saccharomyces telluris</i><span>&nbsp;Van der Walt, and&nbsp;</span><i>Geotrichum</i><span>&nbsp;sp.; white-crowned pigeon (</span><i>C. leucocephala</i><span>&nbsp;Linnaeus) 56% —&nbsp;</span><i>S. telluris</i><span>; mourning dove (</span><i>Zenaidura macroura</i><span>&nbsp;Linnaeus) 24% —&nbsp;</span><i>C. albicans</i><span>,&nbsp;</span><i>C. tropicalis</i><span>,&nbsp;</span><i>C. guilliermondii</i><span>, and&nbsp;</span><i>Geotrichum</i><span>&nbsp;sp.; passerine ground dove (</span><i>Collumbigallina passerina</i><span>&nbsp;Linnaeus) 20% —&nbsp;</span><i>C. parapsilosis</i><span>&nbsp;(Ashford) Langeron et Talice,&nbsp;</span><i>Kloeckera apiculata</i><span>&nbsp;(Reess Emend. Klocker) Janke; zenaida dove (</span><i>Zenaida auritu</i><span>&nbsp;Temminck) 16% —&nbsp;</span><i>C. albicans</i><span>,&nbsp;</span><i>C. guilliermondii</i><span>, and&nbsp;</span><i>T. glabrata</i><span>; one moustasche dove (</span><i>Geotrygon mystacea</i><span>&nbsp;Gosse) —&nbsp;</span><i>C. guilliermondii</i><span>; ringed turtle dove (</span><i>Streptopelia rizoria</i><span>&nbsp;Linnaeus) 14% —&nbsp;</span><i>C. albicans</i><span>&nbsp;and&nbsp;</span><i>Geotrichum</i><span>&nbsp;sp. No signs of disease could be seen in the 139 birds that were examined, and it was concluded that these yeasts comprise a part of the columbid's normal microbial flora.</span></p>","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-8.4.365","usgsCitation":"Kocan, R.M., and Hasenclever, H., 1972, Normal yeast flora of the upper digestive tract of some wild columbids: Journal of Wildlife Diseases, v. 8, no. 4, p. 365-368, https://doi.org/10.7589/0090-3558-8.4.365.","productDescription":"4 p.","startPage":"365","endPage":"368","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196386,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e21","contributors":{"authors":[{"text":"Kocan, R. M.","contributorId":41783,"corporation":false,"usgs":true,"family":"Kocan","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":335865,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hasenclever, H.F.","contributorId":37027,"corporation":false,"usgs":true,"family":"Hasenclever","given":"H.F.","email":"","affiliations":[],"preferred":false,"id":335864,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1013846,"text":"1013846 - 1972 - Monitoring channel catfish use of a demand feeder","interactions":[],"lastModifiedDate":"2025-08-05T15:46:11.503384","indexId":"1013846","displayToPublicDate":"1972-10-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Monitoring channel catfish use of a demand feeder","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1972)34[204:MCCUOA]2.0.CO;2","usgsCitation":"Hastings, W., Hinson, B., Tackett, D., and Simco, B., 1972, Monitoring channel catfish use of a demand feeder: Progressive Fish-Culturist, v. 34, no. 4, p. 204-206, https://doi.org/10.1577/1548-8659(1972)34[204:MCCUOA]2.0.CO;2.","productDescription":"3 p.","startPage":"204","endPage":"206","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131686,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699175","contributors":{"authors":[{"text":"Hastings, W.H.","contributorId":58969,"corporation":false,"usgs":true,"family":"Hastings","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":319338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hinson, B.","contributorId":38939,"corporation":false,"usgs":true,"family":"Hinson","given":"B.","email":"","affiliations":[],"preferred":false,"id":319337,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tackett, D.","contributorId":36089,"corporation":false,"usgs":true,"family":"Tackett","given":"D.","affiliations":[],"preferred":false,"id":319336,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Simco, B.","contributorId":22728,"corporation":false,"usgs":true,"family":"Simco","given":"B.","affiliations":[],"preferred":false,"id":319335,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70210093,"text":"70210093 - 1972 - Observation of nighttime feeding behavior of ducks","interactions":[],"lastModifiedDate":"2020-05-13T20:37:57.720537","indexId":"70210093","displayToPublicDate":"1972-07-31T15:26:37","publicationYear":"1972","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":"Observation of nighttime feeding behavior of ducks","docAbstract":"<p><span>A night vision scope was used during 1969-71 to study the nighttime feeding behavior of ducks on prairie wetlands of south-central North Dakota. Adult and immature ducks were observed feeding between 9:00 PM and 4:00 AM, predominantly on midges (Chironomidae) and mayflies (Ephemeroptera). The emergence pattern of these insects appeared to be a major factor influencing duck activity and feeding behavior at night.</span></p>","language":"English","publisher":"Wiley","doi":"10.2307/3799457","usgsCitation":"Swanson, G.A., and Sargeant, A.B., 1972, Observation of nighttime feeding behavior of ducks: Journal of Wildlife Management, v. 36, no. 3, p. 959-961, https://doi.org/10.2307/3799457.","productDescription":"3 p.","startPage":"959","endPage":"961","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":374804,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","city":"Jamestown","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.96209716796874,\n              46.78501604269254\n            ],\n            [\n              -98.558349609375,\n              46.78501604269254\n            ],\n            [\n              -98.558349609375,\n              47.26991141830741\n            ],\n            [\n              -98.96209716796874,\n              47.26991141830741\n            ],\n            [\n              -98.96209716796874,\n              46.78501604269254\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"36","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Swanson, George A.","contributorId":49654,"corporation":false,"usgs":true,"family":"Swanson","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":789075,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sargeant, Alan B.","contributorId":89185,"corporation":false,"usgs":true,"family":"Sargeant","given":"Alan","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":789076,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}