Silvex, [2-(2,4,5-trichlorophenoxy)propionic acid], impregnated (20% ae) on clay granules, applied at a rate as low as 20 lb/A ae gave excellent control of well-rooted alligatorweed [Alternanthera philoxeroides (Mart.) Grieb] growing in less than 18 inches of water. The 2-ethylhexyl ester of silvex was more effective than the potassium salt. Silvex was not effective on floating-mat alligatorweed or in water over 18 inches deep.
","language":"English","publisher":"Cambridge University Press","doi":"10.2307/4041102","usgsCitation":"McGilvrey, F., and Steenis, J., 1965, Control of alligatorweed in South Carolina with granular silvex: Weeds, v. 13, no. 1, p. 66-68, https://doi.org/10.2307/4041102.","productDescription":"3 p.","startPage":"66","endPage":"68","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194316,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South 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Carolina\",\"nation\":\"USA \"}}]}","volume":"13","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68991f","contributors":{"authors":[{"text":"McGilvrey, Frank B.","contributorId":14908,"corporation":false,"usgs":true,"family":"McGilvrey","given":"Frank B.","affiliations":[],"preferred":false,"id":331798,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steenis, J.H.","contributorId":73694,"corporation":false,"usgs":true,"family":"Steenis","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":331799,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68443,"text":"ha195 - 1965 - Hydrogeology of the glacial drift in the Skunk Creek-Lake Madison drainage basin, southeastern South Dakota","interactions":[],"lastModifiedDate":"2023-03-14T19:17:51.83257","indexId":"ha195","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"195","title":"Hydrogeology of the glacial drift in the Skunk Creek-Lake Madison drainage basin, southeastern South Dakota","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha195","usgsCitation":"Ellis, M.J., and Adolphson, D.G., 1965, Hydrogeology of the glacial drift in the Skunk Creek-Lake Madison drainage basin, southeastern South Dakota: U.S. Geological Survey Hydrologic Atlas 195, 1 Plate: 52.00 x 34.50 inches, https://doi.org/10.3133/ha195.","productDescription":"1 Plate: 52.00 x 34.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":414119,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15559.htm","linkFileType":{"id":5,"text":"html"}},{"id":186219,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89973,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/195/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"South Dakota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -96.75,\n 43.478\n ],\n [\n -96.75,\n 44.081\n ],\n [\n -97.3,\n 44.081\n ],\n [\n -97.3,\n 43.478\n ],\n [\n -96.75,\n 43.478\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db614eec","contributors":{"authors":[{"text":"Ellis, M. J.","contributorId":27840,"corporation":false,"usgs":true,"family":"Ellis","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278228,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1013643,"text":"1013643 - 1965 - Characteristics and identification of oxidative Pseudomonads isolated from diseased fish","interactions":[],"lastModifiedDate":"2025-02-05T16:18:27.467682","indexId":"1013643","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2300,"text":"Journal of General Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Characteristics and identification of oxidative Pseudomonads isolated from diseased fish","docAbstract":"Several characteristics of 20 strains of oxidative pseudomonads, all but one of which were isolated from freshwater fish, were determined. All strains oxidized glucose and gluconate, produced NH3 from 1 % peptone, grew at 6, 12, 20 and 30° and produced cytochrome oxidase. Lipase was produced by 17 of the strains, while 15 produced gelatinase, and 16 produced fluorescent pigment. These and other characteristics used to identify fish-spoilage pseudomonads are also useful for identification of fish-pathogenic pseudomonads. Species determinations from the present data were not attempted. However, from previously published data on speciation of Pseudomonas, most of the 20 strains appeared to be closely related to or identical with P. fluorescens.
","language":"English","publisher":"Microbiology Society","doi":"10.1099/00221287-38-1-1","usgsCitation":"Bullock, G.L., Snieszko, S.F., and Dunbar, C.E., 1965, Characteristics and identification of oxidative Pseudomonads isolated from diseased fish: Journal of General Microbiology, v. 38, p. 1-7, https://doi.org/10.1099/00221287-38-1-1.","productDescription":"7 p.","startPage":"1","endPage":"7","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":486903,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1099/00221287-38-1-1","text":"Publisher Index Page"},{"id":131914,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"38","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e539f","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":318949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":318948,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunbar, C. E.","contributorId":96623,"corporation":false,"usgs":true,"family":"Dunbar","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":318950,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1013747,"text":"1013747 - 1965 - Eimeria aurati n. sp. (Protozoa:Eimeriidae) from goldfish (Carassius auratus) in North America","interactions":[],"lastModifiedDate":"2025-05-09T15:51:47.108634","indexId":"1013747","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2434,"text":"Journal of Protozoology","active":true,"publicationSubtype":{"id":10}},"title":"Eimeria aurati n. sp. (Protozoa:Eimeriidae) from goldfish (Carassius auratus) in North America","docAbstract":"Eimeria aurati n. sp. is described from the intestine of the goldfish, Carassius auratus, from Pennsylvania, U.S.A. Oocysts were very numerous in long, whitish, opaque fecal casts. They were 16 to 24 by 14 to 17 μ (mean, 20.1 by 16.3) and were non-sporulated when passed but sporulated 2 to 5 days later.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1550-7408.1965.tb01850.x","usgsCitation":"Hoffman, G.L., 1965, Eimeria aurati n. sp. (Protozoa:Eimeriidae) from goldfish (Carassius auratus) in North America: Journal of Protozoology, v. 12, no. 2, p. 273-275, https://doi.org/10.1111/j.1550-7408.1965.tb01850.x.","productDescription":"3 p.","startPage":"273","endPage":"275","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":129473,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"12","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-04-30","publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60eec0","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70176114,"text":"70176114 - 1965 - Surface water records of Texas, 1964","interactions":[],"lastModifiedDate":"2017-04-19T10:37:54","indexId":"70176114","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5196,"text":"Water Data Report","active":true,"publicationSubtype":{"id":6}},"title":"Surface water records of Texas, 1964","docAbstract":"The surface-water records for the 1964 water year for gaging stations, partial-record stations, miscellaneous sites, and base-flow studies within the State of Texas are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U. S. Geological Survey, under the direction of Trigg Twichell, district chief, Water Resources Division.
Through September 30, 1960, the records of discharge and stage of streams 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.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Texas were contained in Parts 7 and 8 of that series.
Beginning with the 1961 water year, streamflow records and related data have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports is limited and primarily for local needs. Records will be published in Geological Survey water-supply papers at 5-year intervals.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57c1683ee4b0f2f0ceb90861","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128037,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":647150,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1718,"text":"wsp1809I - 1965 - Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61","interactions":[],"lastModifiedDate":"2023-03-13T20:10:12.868331","indexId":"wsp1809I","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1809","chapter":"I","title":"Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61","docAbstract":"Artesian water pressure in the deep sandstone aquifer continued to decline throughout most of the Milwaukee-Waukesha area, Wisconsin between 1950 and 1961. Areas of greatest water-level decline were in northeast Waukesha County and in northwest Milwaukee County. The chief cause of the decline was continued heavy pumpage. The major aquifers of southeastern Wisconsin are the Niagara aquifer, which is primarily Niagara Dolomite of Silurian age, and the sandstone aquifer, which consists of sandstones of Cambrian and Ordovician ages. Locally, the glacial sands and gravels ,of Pleistocene age also are important aquifers. In the Milwaukee-Waukesha area, the sandstone aquifer is completely artesian, confined above by the Maquoketa Shale. The Niagara aquifer is generally unconfined. Pumpage from the sandstone aquifer in the Milwaukee-Waukesha area de- creased from about 23.3 million gallons per day in 1950 to about 20.9 million gallons per day in 1961. The principal reason for decreased pumpage was sub- stitution of surface-water supply from Lake Michigan. Between 1950 and 1961, the water-level changes in wells in the sandstone aquifer ranged from plus 10 feet at Town of Lake to minus 98 feet in northwest Milwaukee. Except for a small area near Town of Lake, water levels in wells in the Milwaukee-Waukesha area were lower in 1961 than in 1950. Water-level changes were directly related to the pumpage pattern and pump- age changes. Increased pumpage at Waukesha and in northwest Milwaukee and continued heavy pumpage at Wauwatosa caused widespread water-level declines in northeast Waukesha County and in northwest Milwaukee County. Locally, decreased pumpage at West Milwaukee allowed limited recovery of water levels since 1957. Estimates of pumpage through the year 1975 indicate a pumpage decrease in the middle 1960's, followed by an increase in the late 1960's and early 1970's. Additional conversion to surface-water supply in Milwaukee County will account for most pumpage decreases. Increased pumpage is most likely in Waukesha County where the population is expanding rapidly and an adequate surface-water supply is not readily accessible. The westward shift of the pumpage pattern may cause an additional water-level decline of about 50 feet at Waukesha but will permit water levels to recover about 100 feet at West Allis by 1975. Partial or complete conversion to surface-water supplies by municipalities that depend entirely on water from the sandstone aquifer would allow greater use of the sandstone aquifer by isolated suburban developments and industries.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809I","collaboration":"Prepared in cooperation with the University of Wisconsin, Geological and Natural History Survey","usgsCitation":"Green, J.H., and Hutchinson, R.D., 1965, Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61: U.S. Geological Survey Water Supply Paper 1809, Report: iii, 19 p. ; 2 Plates: 19.50 x 24.00 inches and 18.50 x 24.00 inches, https://doi.org/10.3133/wsp1809I.","productDescription":"Report: iii, 19 p. ; 2 Plates: 19.50 x 24.00 inches and 18.50 x 24.00 inches","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":26806,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136940,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809i/report-thumb.jpg"},{"id":26805,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26804,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414041,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25008.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wisconsin","city":"Milwaukee, Waukesha","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -88.82011978710044,\n 43.6048598948214\n ],\n [\n -88.82011978710044,\n 42.619688745253114\n ],\n [\n -87.76500461016991,\n 42.619688745253114\n ],\n [\n -87.76500461016991,\n 43.6048598948214\n ],\n [\n -88.82011978710044,\n 43.6048598948214\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673ff","contributors":{"authors":[{"text":"Green, J. H.","contributorId":43312,"corporation":false,"usgs":true,"family":"Green","given":"J.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":144010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, R. D.","contributorId":99112,"corporation":false,"usgs":true,"family":"Hutchinson","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":144011,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000291,"text":"1000291 - 1965 - Movements of hatchery-reared lake trout in Lake Superior","interactions":[],"lastModifiedDate":"2016-02-25T10:45:56","indexId":"1000291","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Movements of hatchery-reared lake trout in Lake Superior","docAbstract":"The history of stocking of lake trout (Salvelinus namaycush) in the Great Lakes is reviewed. The study of movements is based on capture of 24,275 fin-clipped lake trout taken in experimental gill nets and trawls and commercial gill nets. Yearling lake trout planted from shore dispersed to 15-fath (27-m) depths in 3A? hr. Most fish remained within 2 miles (3.2 km) of the planting site 2 months, but within 4 months some fish had moved as much as 17 miles (27 km). The highest abundance of planted lake trout was in areas 2-4 miles (3.2-6.4 km) from the planting site even 3 years after release. Distance moved and size of fish were not correlated. Dispersal of lake trout begins at planting and probably continues until the fish are mature. Most movement was eastward in southern Lake Superior and followed the counterclockwise surface currents. Movement is most rapid in areas of strong currents and slowest in areas of weak currents or eddies. Movement to areas west of the Keweenaw Peninsula was insignificant from plantings in Keweenaw Bay and nil from other plantings farther east. Lake trout planted in the eastern third of the lake dispersed more randomly than those planted farther west. Few fish moved farther offshore than the 50-fath (91-m) contour. Lake trout planted in Canadian waters made insignificant contributions to populations in US waters.
","language":"English","publisher":"NRC Research Press","doi":"10.1139/f65-093","usgsCitation":"Pycha, R.L., Dryer, W.R., and King, G.R., 1965, Movements of hatchery-reared lake trout in Lake Superior: Journal of the Fisheries Research Board of Canada, v. 22, no. 4, p. 999-1024, https://doi.org/10.1139/f65-093.","productDescription":"26 p.","startPage":"999","endPage":"1024","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63ee14","contributors":{"authors":[{"text":"Pycha, Richard L.","contributorId":17175,"corporation":false,"usgs":true,"family":"Pycha","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dryer, William R.","contributorId":71921,"corporation":false,"usgs":true,"family":"Dryer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308347,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"King, George R.","contributorId":74721,"corporation":false,"usgs":true,"family":"King","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308348,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2529,"text":"wsp1594C - 1965 - Artificial recharge in Oregon and Washington 1962","interactions":[{"subject":{"id":56108,"text":"ofr5845 - 1957 - Artificial recharge to ground water in Oregon and Washington","indexId":"ofr5845","publicationYear":"1957","noYear":false,"title":"Artificial recharge to ground water in Oregon and Washington"},"predicate":"SUPERSEDED_BY","object":{"id":2529,"text":"wsp1594C - 1965 - Artificial recharge in Oregon and Washington 1962","indexId":"wsp1594C","publicationYear":"1965","noYear":false,"chapter":"C","title":"Artificial recharge in Oregon and Washington 1962"},"id":1}],"lastModifiedDate":"2023-03-21T21:43:14.859497","indexId":"wsp1594C","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1594","chapter":"C","title":"Artificial recharge in Oregon and Washington 1962","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1594C","usgsCitation":"Price, D., Hart, D.H., and Foxworthy, B., 1965, Artificial recharge in Oregon and Washington 1962: U.S. Geological Survey Water Supply Paper 1594, Report: iv, 65 p.; 2 Plates: 13.00 x 16.00 inches and 15.50 x 22.50 inches, https://doi.org/10.3133/wsp1594C.","productDescription":"Report: iv, 65 p.; 2 Plates: 13.00 x 16.00 inches and 15.50 x 22.50 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":414513,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24780.htm","linkFileType":{"id":5,"text":"html"}},{"id":28750,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1594c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28751,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1594c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28752,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1594c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1594c/report-thumb.jpg"}],"country":"United States","state":"Oregon, Washington","city":"Richland","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.46350315641314,\n 46.4426973178723\n ],\n [\n -119.46350315641314,\n 45.7221983183116\n ],\n [\n -118.77099010172134,\n 45.7221983183116\n ],\n [\n -118.77099010172134,\n 46.4426973178723\n ],\n [\n -119.46350315641314,\n 46.4426973178723\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c3e","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":145352,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, D. H.","contributorId":16811,"corporation":false,"usgs":true,"family":"Hart","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145351,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Foxworthy, B. L.","contributorId":45686,"corporation":false,"usgs":true,"family":"Foxworthy","given":"B. L.","affiliations":[],"preferred":false,"id":145353,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":67263,"text":"i451 - 1965 - Map showing relation of land and submarine topography, Nova Scotia to Florida","interactions":[],"lastModifiedDate":"2023-02-01T17:12:44.682049","indexId":"i451","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"451","title":"Map showing relation of land and submarine topography, Nova Scotia to Florida","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i451","usgsCitation":"Uchupi, E., 1965, Map showing relation of land and submarine topography, Nova Scotia to Florida: U.S. Geological Survey IMAP 451, 3 Plates: 41.21 x 31.28 inches or smaller, https://doi.org/10.3133/i451.","productDescription":"3 Plates: 41.21 x 31.28 inches or smaller","costCenters":[],"links":[{"id":256270,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0451/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":256269,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0451/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":189025,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0451/plate-1-thumb.jpg"},{"id":412538,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0451/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660793","contributors":{"authors":[{"text":"Uchupi, Elazar","contributorId":79853,"corporation":false,"usgs":true,"family":"Uchupi","given":"Elazar","email":"","affiliations":[],"preferred":false,"id":275871,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64241,"text":"gp509 - 1965 - Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont","interactions":[{"subject":{"id":44227,"text":"ofr6110 - 1961 - Total intensity aeromagnetic map of parts of Bolton, Whitehall, Glens Falls, and Fort Ann quadrangles, New York","indexId":"ofr6110","publicationYear":"1961","noYear":false,"title":"Total intensity aeromagnetic map of parts of Bolton, Whitehall, Glens Falls, and Fort Ann quadrangles, New York"},"predicate":"SUPERSEDED_BY","object":{"id":64241,"text":"gp509 - 1965 - Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont","indexId":"gp509","publicationYear":"1965","noYear":false,"title":"Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont"},"id":1}],"lastModifiedDate":"2025-04-28T17:13:30.023397","indexId":"gp509","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"509","title":"Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp509","usgsCitation":"Balsley, J.R., and Bromery, R.W., 1965, Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont: U.S. Geological Survey Geophysical Investigations Map 509, Report: 1 p.; 1 Plate: 22.31 x 34.57 inches, https://doi.org/10.3133/gp509.","productDescription":"Report: 1 p.; 1 Plate: 22.31 x 34.57 inches","costCenters":[],"links":[{"id":254280,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0509/report-thumb.jpg"},{"id":250809,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0509/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250808,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0509/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414488,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3460.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"62500","country":"United States","state":"New York, Vermont","county":"Rutland County, Warren County, Washington County","otherGeospatial":"Bolton Landing, Glens Falls, and Whitehall quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.75,\n 43.333\n ],\n [\n -73.75,\n 43.75\n ],\n [\n -73.3667,\n 43.75\n ],\n [\n -73.3667,\n 43.333\n ],\n [\n -73.75,\n 43.333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697670","contributors":{"authors":[{"text":"Balsley, James R.","contributorId":10010,"corporation":false,"usgs":true,"family":"Balsley","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270291,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bromery, R. W.","contributorId":11676,"corporation":false,"usgs":true,"family":"Bromery","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":270292,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":64149,"text":"gp546 - 1965 - Aeromagnetic map of the Uncasville quadrangle and part of the New London quadrangle, New London County, Connecticut","interactions":[],"lastModifiedDate":"2023-03-21T20:06:33.503288","indexId":"gp546","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"546","title":"Aeromagnetic map of the Uncasville quadrangle and part of the New London quadrangle, New London County, Connecticut","docAbstract":"No abstract available.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha161","usgsCitation":"Morgan, J.H., 1965, Availability of ground water in the Cuba quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 161, 1 Plate: 47.50 x 34.50 inches, https://doi.org/10.3133/ha161.","productDescription":"1 Plate: 47.50 x 34.50 inches","costCenters":[],"links":[{"id":186376,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89449,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/161/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413583,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15522.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Cuba quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.75,\n 36.5\n ],\n [\n -88.75,\n 36.625\n ],\n [\n -88.625,\n 36.625\n ],\n [\n -88.625,\n 36.5\n ],\n [\n -88.75,\n 36.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e54b","contributors":{"authors":[{"text":"Morgan, J. H.","contributorId":9243,"corporation":false,"usgs":true,"family":"Morgan","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277727,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70171153,"text":"70171153 - 1965 - Field application methods for recovery of the selective lampricide, 3-trifluoromethyl-4-nitrophenol","interactions":[],"lastModifiedDate":"2016-05-24T09:56:22","indexId":"70171153","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Field application methods for recovery of the selective lampricide, 3-trifluoromethyl-4-nitrophenol","docAbstract":"Colorimetric methods are described for the detection of residues of the selective lampricide, 3-trifluoromethyl-4-nitrophenol (TFM), in natural waters and fish tissues. Solvent extraction and anion exchange were used to separate and concentrate the lampricide, and to reduce high background colors which often interfere with the determinations. Data from the Pentwater and Muskegon Rivers (Michigan) showed an exponential rate of disappearance of TFM from the water immediately after treatments to eradicate larvae of the sea lamprey (Petromyzon marinus). No TFM was recovered from fish exposed in their natural environment to low levels of the lampricide during treatment; residues were recovered, however, from fish exposed to high concentrations in the laboratory.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 8th Conference on Great Lakes Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"8th Conference on Great Lakes Research","conferenceDate":"March 29-30","conferenceLocation":"Ann Arbor, MI","language":"English","publisher":"University of Michigan","usgsCitation":"Billy, T.J., Daniels, S.L., Kempe, L.L., and Beeton, A.M., 1965, Field application methods for recovery of the selective lampricide, 3-trifluoromethyl-4-nitrophenol, in Proceedings of the 8th Conference on Great Lakes Research, Ann Arbor, MI, March 29-30, p. 17-24.","productDescription":"8 p.","startPage":"17","endPage":"24","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321589,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d6505e4b07e28b6683e7b","contributors":{"authors":[{"text":"Billy, Thomas J.","contributorId":76853,"corporation":false,"usgs":true,"family":"Billy","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daniels, Stacy L.","contributorId":105821,"corporation":false,"usgs":true,"family":"Daniels","given":"Stacy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630122,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kempe, Lloyd L.","contributorId":55117,"corporation":false,"usgs":true,"family":"Kempe","given":"Lloyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630123,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630124,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1000089,"text":"1000089 - 1965 - Length-weight relationship of northern pike, Esox lucius, from East Harbor, Ohio","interactions":[],"lastModifiedDate":"2016-02-25T11:11:27","indexId":"1000089","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Length-weight relationship of northern pike, Esox lucius, from East Harbor, Ohio","docAbstract":"The northern pike is one of Ohio's largest game fish but is well known to comparatively few anglers. Large numbers of the big fish spawn in the Ohio marshes adjacent to Lake Erie. Movements related to spawning reach a peak in late March or early April. Later the spawning population disperses and is seldom represented in catches by experimental gear or by anglers. The short period of availability was used to obtain life history information in March of 1951 through 1953. No comprehensive length-weight data for this species have previously been published from this area. East Harbor is a sandspit pond separated from Lake Erie by a large sand bar. Waters and fish populations of the harbor and lake can mix freely through a permanent connecting channel. The larger part of the 850 surface acres of the harbor is normally less than 8 feet deep. The male northern pike averaged 20.5 inches in length and ranged from 13.5 to 28.5 inches. The conspicuously larger females averaged 26.0 inches and ranged from 15.5 to 37.5 inches.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1965)94[404:LRONPE]2.0.CO;2","usgsCitation":"Brown, E.H., and Clark, C.F., 1965, Length-weight relationship of northern pike, Esox lucius, from East Harbor, Ohio: Transactions of the American Fisheries Society, v. 94, no. 4, p. 404-405, https://doi.org/10.1577/1548-8659(1965)94[404:LRONPE]2.0.CO;2.","productDescription":"2 p.","startPage":"404","endPage":"405","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6108","contributors":{"authors":[{"text":"Brown, Edward H. Jr.","contributorId":33251,"corporation":false,"usgs":true,"family":"Brown","given":"Edward","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Clarence F.","contributorId":99101,"corporation":false,"usgs":true,"family":"Clark","given":"Clarence","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308059,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010446,"text":"70010446 - 1965 - A new Rosalina (foraminifera) parasitic on a bivalve","interactions":[],"lastModifiedDate":"2020-11-24T00:29:52.432387","indexId":"70010446","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1372,"text":"Deep-Sea Research and Oceanographic Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"A new Rosalina (foraminifera) parasitic on a bivalve","docAbstract":"In a collection of pelecypods from deep water off the west coast of Africa, several specimens of a new species of the foraminifer, Rosalina, are attached to the umbonal area of the bivalve. In addition, numerous attachment scars are observed on the exterior surface with interconnected penetration scars on the interior surface of the valves. It is speculated that the foraminifer made the partial or complete penetration of the clam shell in connection with its search for calcium carbonate for shell-building. From the nature of the scars on the interior of the valves, it is clear that the clam was alive, because there are mounded up shell deposits around some of the openings and others are completely sealed shut by shell material deposited by the clam.
Because of its direct relation to total dissolved solids content, sodium concentration is the most useful single hydrochemical parameter of closed basin waters in the western United States. Therefore, it is advantageous to have a rapid method for sodium determination which could be readily adapted to field use. Accordingly, thirty waters of highly variable concentration and anionic composition from the western Great Basin have been analyzed with a sodium-sensitive glass electrode. Na+ values ranged from 10 to 130,000 ppm in waters containing from 102 to 401,000 ppm total dissolved solids. The electrode values were compared with conventional sodium determinations; results differed by as much as 11 per cent, although over two-thirds were within 5 per cent. No significant relation was found between the glass electrode and conventional method differences and the total dissolved solids or sodium concentration. The comparative accuracy of electrode and conventional procedures was checked, employing solutions of known sodium concentration. It was concluded that for the analysis of sodium in natural waters the glass electrode method offers results comparable in accuracy to those obtained by conventional methods, but with increased simplicity, and therefore the possibility of rapid, accurate field measurements.
The lower limit of abundance of sodium and potassium in ultramafic rocks is less than the threshold amount detectable by conventional analytical methods. By a dilutionaddition modification of the flame-spectrophotometric method, sodium and potassium have been determined in 40 specimens of alpine ultramafic rocks. Samples represent six regions in the United States and one in Australia, and include dunite, peridotite, pyroxenite, and their variably serpentinized and metamorphosed derivatives.
The median value found for Na2O is 0.004 per cent, and the range of Na2O is 0.001–0.19. The median value for K2O is 0.0034 per cent and the range is 0.001–0.031 per cent. Alkali concentrations are below 0.01 per cent Na2O in 28 samples and below 0.01 per cent K2O in 35.
Derivation of basalt magma from upper-mantle material similar to such ultramafic rocks, as has been postulated, is precluded by the relative amounts of sodium and potassium, which are from 200 to 600 times more abundant in basalt than in the ultramafic rocks. Similar factors apply to a number of other elements. No reasonable process could produce such concentrations in, for example, tens of thousands of cubic miles of uniform tholeiitic basalt. The ultramafic rocks might have originated either as magmatic crystal precipitates or as mantle residues left after fusion and removal of basaltic magma. Injection of ultramafic rocks to exposed positions is tectonic rather than magmatic.
The average concentrations of potassium, rubidium, strontium, thorium, and uranium in oceanic tholeiitic basalt are (in parts per million) K, 1400; Rb, 1.2; Sr, 120; Th, 0.2; and U, 0.1. The ratio Sr87 to Sr86 is about 0.702, that of K to U is 1.4 x 104, and of Th to U is 1.8. These amounts of K, Th, U, and radiogenic Sr87 are less than in other common igneous rocks. The ratios of Th to U and Sr87 to Sr86 suggest that the source region of the oceanic tholeiites was differentiated from the original mantle material some time in the geologic past.
Occurrence, quality, and availability of ground water differ considerably from place to place in the Eola-Amity Hills area because of the highly diversified geologic and hydrologic conditions. A table relates the geologic situation to the availability of ground water for four areas--Eola-Amity Hills, east and west valley plains, and Willamette River flood plain. Tables show well and spring records, drillers' logs, and chemical analyses of ground water. The final interpretive report will be published by the U.S. Geological Survey.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, DC","usgsCitation":"Price, D., and Johnson, N.A., 1965, Selected ground water data in the Eola-Amity Hills area, northern Willamette Valley, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326670,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Willamette Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b58e4b03bcb0104bc68","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":645787,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, Nyra A.","contributorId":173771,"corporation":false,"usgs":false,"family":"Johnson","given":"Nyra","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":645788,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175584,"text":"70175584 - 1965 - Oregon ground-water levels, 1964","interactions":[],"lastModifiedDate":"2016-08-17T11:35:47","indexId":"70175584","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"Oregon ground-water levels, 1964","docAbstract":"No abstract available.
","language":"English","usgsCitation":"Sceva, J.E., and DeBow, R., 1965, Oregon ground-water levels, 1964: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326657,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b53e4b03bcb0104bc2e","contributors":{"authors":[{"text":"Sceva, Jack E.","contributorId":79086,"corporation":false,"usgs":true,"family":"Sceva","given":"Jack","email":"","middleInitial":"E.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":645760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeBow, Robert","contributorId":173757,"corporation":false,"usgs":false,"family":"DeBow","given":"Robert","email":"","affiliations":[],"preferred":false,"id":645761,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70175590,"text":"70175590 - 1965 - Add to e-Shelf \t Records of wells, water levels and chemical quality of water in Baker Valley, Baker County, Oregon","interactions":[],"lastModifiedDate":"2016-08-17T11:47:07","indexId":"70175590","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"Add to e-Shelf \t Records of wells, water levels and chemical quality of water in Baker Valley, Baker County, Oregon","docAbstract":"Records from 135 representative wells, and chemical analyses of water from 49 wells and 2 springs are tabulated. Drillers' logs of representative wells comprise most of the report.
","largerWorkType":{"id":2,"text":"Article"},"usgsCitation":"Ducret, G., and Anderson, D., 1965, Add to e-Shelf \t Records of wells, water levels and chemical quality of water in Baker Valley, Baker County, Oregon: Ground Water Report.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":326663,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon","county":"Baker","otherGeospatial":"Baker Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58abce4b03bcb0104bb55","contributors":{"authors":[{"text":"Ducret, G.L. Jr.","contributorId":107703,"corporation":false,"usgs":true,"family":"Ducret","given":"G.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":645780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Anderson, D.B.","contributorId":47762,"corporation":false,"usgs":true,"family":"Anderson","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":645781,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":34683,"text":"b1202B - 1965 - Regional structure of the southeast Missouri and Illinois-Kentucky mineral districts","interactions":[],"lastModifiedDate":"2023-03-16T21:13:14.671067","indexId":"b1202B","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1202","chapter":"B","title":"Regional structure of the southeast Missouri and Illinois-Kentucky mineral districts","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1202B","usgsCitation":"Heyl, A.V., Brock, M.R., Jolly, J.L., and Wells, C.E., 1965, Regional structure of the southeast Missouri and Illinois-Kentucky mineral districts: U.S. Geological Survey Bulletin 1202, Report: iii, 20 p.; 3 Plates: 38.00 x 21.70 inches, https://doi.org/10.3133/b1202B.","productDescription":"Report: iii, 20 p.; 3 Plates: 38.00 x 21.70 inches","costCenters":[],"links":[{"id":414306,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19254.htm","linkFileType":{"id":5,"text":"html"}},{"id":62553,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1202b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62552,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62551,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62550,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165873,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1202b/report-thumb.jpg"}],"country":"United States","state":"Illinois, Kentucky, Missouri","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -88,\n 39\n ],\n [\n -92,\n 39\n ],\n [\n -92,\n 37\n ],\n [\n -88,\n 37\n ],\n [\n -88,\n 39\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c460","contributors":{"authors":[{"text":"Heyl, Allen Van","contributorId":91078,"corporation":false,"usgs":true,"family":"Heyl","given":"Allen","email":"","middleInitial":"Van","affiliations":[],"preferred":false,"id":213396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brock, M. R.","contributorId":96230,"corporation":false,"usgs":true,"family":"Brock","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":213398,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jolly, J. L.","contributorId":89200,"corporation":false,"usgs":true,"family":"Jolly","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":213395,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wells, C. E.","contributorId":92729,"corporation":false,"usgs":true,"family":"Wells","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":213397,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}