Analyses of samples G-1 and W-1 made since 1962 are collected and \"best values\" for many elements are suggested.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(65)90005-0","issn":"00167037","usgsCitation":"Fleischer, M., 1965, Summary of new data on rock samples G-1 and w-1, 1962-1965: Geochimica et Cosmochimica Acta, v. 29, no. 12, p. 1263-1283, https://doi.org/10.1016/0016-7037(65)90005-0.","productDescription":"21 p.","startPage":"1263","endPage":"1283","numberOfPages":"21","costCenters":[],"links":[{"id":218723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9e9be4b08c986b31e000","contributors":{"authors":[{"text":"Fleischer, M.","contributorId":84069,"corporation":false,"usgs":true,"family":"Fleischer","given":"M.","email":"","affiliations":[],"preferred":false,"id":358940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70009989,"text":"70009989 - 1965 - Alkali content of alpine ultramafic rocks","interactions":[],"lastModifiedDate":"2020-11-24T00:39:56.572868","indexId":"70009989","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Alkali content of alpine ultramafic rocks","docAbstract":"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.
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.
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.
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.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1199B","usgsCitation":"Conant, L.C., 1965, Bauxite and kaolin deposits of Mississippi, exclusive of the Tippah-Benton district: U.S. Geological Survey Bulletin 1199, Report: v, 70 p.; 5 Plates: 18.50 × 39.50 inches or smaller, https://doi.org/10.3133/b1199B.","productDescription":"Report: v, 70 p.; 5 Plates: 18.50 × 39.50 inches or smaller","costCenters":[],"links":[{"id":109490,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20971.htm","linkFileType":{"id":5,"text":"html"},"description":"20971"},{"id":61974,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1199b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61973,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1199b/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61972,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1199b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61971,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1199b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61970,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1199b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61969,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1199b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163961,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1199b/report-thumb.jpg"}],"country":"United States","state":"Mississippi","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -89.219,\n 34.432\n ],\n [\n -89.219,\n 34.396\n ],\n [\n -89.169,\n 34.396\n ],\n [\n -89.169,\n 34.432\n ],\n [\n -89.219,\n 34.432\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e157","contributors":{"authors":[{"text":"Conant, Louis C.","contributorId":83921,"corporation":false,"usgs":true,"family":"Conant","given":"Louis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":212385,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010598,"text":"70010598 - 1965 - Water analysis","interactions":[],"lastModifiedDate":"2023-03-20T16:01:05.594468","indexId":"70010598","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Water analysis","docAbstract":"No abstract available.
","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60224a016","usgsCitation":"Skougstad, M.W., and Fishman, M., 1965, Water analysis: Analytical Chemistry, v. 37, no. 5, p. 232-260, https://doi.org/10.1021/ac60224a016.","productDescription":"29 p.","startPage":"232","endPage":"260","costCenters":[],"links":[{"id":219097,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"5","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505bc795e4b08c986b32c509","contributors":{"authors":[{"text":"Skougstad, Marvin W.","contributorId":65064,"corporation":false,"usgs":true,"family":"Skougstad","given":"Marvin","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359243,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fishman, Marvin J.","contributorId":87110,"corporation":false,"usgs":true,"family":"Fishman","given":"Marvin J.","affiliations":[],"preferred":false,"id":866865,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1001399,"text":"1001399 - 1965 - Regrouping of family members of the white-fronted goose (Anser albifrons) after individual release","interactions":[],"lastModifiedDate":"2023-11-04T00:09:54.021051","indexId":"1001399","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1054,"text":"Bird-Banding","active":true,"publicationSubtype":{"id":10}},"title":"Regrouping of family members of the white-fronted goose (Anser albifrons) after individual release","docAbstract":"No abstract available.
","language":"English","publisher":"Association of Field Ornithologists","doi":"10.2307/4511184","usgsCitation":"Miller, H., and Dzubin, A., 1965, Regrouping of family members of the white-fronted goose (Anser albifrons) after individual release: Bird-Banding, v. 36, no. 3, p. 184-191, https://doi.org/10.2307/4511184.","productDescription":"8 p.","startPage":"184","endPage":"191","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128805,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"36","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db634d2f","contributors":{"authors":[{"text":"Miller, H.","contributorId":57009,"corporation":false,"usgs":true,"family":"Miller","given":"H.","affiliations":[],"preferred":false,"id":310973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dzubin, Alexander","contributorId":35673,"corporation":false,"usgs":true,"family":"Dzubin","given":"Alexander","email":"","affiliations":[],"preferred":false,"id":310972,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14173,"text":"ofr6573 - 1965 - Preliminary materials map, Massachusetts portion, Berlin quadrangle, New York-Massachusetts-Vermont","interactions":[],"lastModifiedDate":"2022-06-08T19:45:22.122861","indexId":"ofr6573","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"65-73","title":"Preliminary materials map, Massachusetts portion, Berlin quadrangle, New York-Massachusetts-Vermont","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6573","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts Department of Public Works and the United States Bureau of Public Roads","usgsCitation":"Holmes, G.W., 1965, Preliminary materials map, Massachusetts portion, Berlin quadrangle, New York-Massachusetts-Vermont: U.S. Geological Survey Open-File Report 65-73, Report: 3 p.; 1 Plate: 30.93 × 29.11 inches, https://doi.org/10.3133/ofr6573.","productDescription":"Report: 3 p.; 1 Plate: 30.93 × 29.11 inches","costCenters":[],"links":[{"id":42832,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0073/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0073/report-thumb.jpg"},{"id":397578,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8108.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Massachusetts, New York","otherGeospatial":"Berlin quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -73.283,\n 42.625\n ],\n [\n -73.25,\n 42.625\n ],\n [\n -73.25,\n 42.708\n ],\n [\n -73.283,\n 42.708\n ],\n [\n -73.283,\n 42.625\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cdf9","contributors":{"authors":[{"text":"Holmes, George William","contributorId":79107,"corporation":false,"usgs":true,"family":"Holmes","given":"George","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":169029,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":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":70010521,"text":"70010521 - 1965 - Eocene and miocene rocks off the northeastern coast of the United States","interactions":[],"lastModifiedDate":"2020-11-24T00:26:49.155915","indexId":"70010521","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":"Eocene and miocene rocks off the northeastern coast of the United States","docAbstract":"A grab sample from a depth of 1675 m at a point south of Cape Cod contains early Eocene planktonic Foraminifera and is correlated with the Globorotalia rex zone of Trinidad. The assemblage indicates a depth comparable to that existing today. Regional relations suggest that the Cretaceous and Eocene deposits deepen to the west toward New Jersey.
Two mollusk-bearing blocks dredged from the northern side of Georges Bank are correlative with the Miocene Yorktown Formation. Rocks from two other stations are probably Miocene. Benthonic Foraminifera in one sample indicate deposition in cool temperate waters of less than 60 m depth.
","language":"English","publisher":"Elsevier","doi":"10.1016/0011-7471(65)90815-6","issn":"00117471","usgsCitation":"Gibson, T., 1965, Eocene and miocene rocks off the northeastern coast of the United States: Deep-Sea Research and Oceanographic Abstracts, v. 12, no. 6, 8 p., https://doi.org/10.1016/0011-7471(65)90815-6.","productDescription":"8 p.","costCenters":[],"links":[{"id":219616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Cape Cod","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.784912109375,\n 41.50034959128928\n ],\n [\n -69.796142578125,\n 41.50034959128928\n ],\n [\n -69.796142578125,\n 42.13896840458089\n ],\n [\n -70.784912109375,\n 42.13896840458089\n ],\n [\n -70.784912109375,\n 41.50034959128928\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"12","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a09f7e4b0c8380cd5212b","contributors":{"authors":[{"text":"Gibson, T. G.","contributorId":103702,"corporation":false,"usgs":true,"family":"Gibson","given":"T. G.","affiliations":[],"preferred":false,"id":359104,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010522,"text":"70010522 - 1965 - Servo-amplifiers for ion current measurement in mass spectrometry","interactions":[],"lastModifiedDate":"2012-03-12T17:18:25","indexId":"70010522","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2448,"text":"Journal of Scientific Instruments","active":true,"publicationSubtype":{"id":10}},"title":"Servo-amplifiers for ion current measurement in mass spectrometry","docAbstract":"A servo-voltmeter can provide a useful alternative to the d.c. amplifier or vibrating reed electrometer for the accurate measurement of mass spectrometer ion currents, and has some advantages which recommend its use in certain applications. A generalized analysis based on servomechanism theory is presented as an aid for understanding the design criteria for this type of device. Two existing systems are described and their operation and performance are examined.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Scientific Instruments","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1088/0950-7671/42/6/305","issn":"09507671","usgsCitation":"Stacey, J.S., Russell, R., and Kollar, F., 1965, Servo-amplifiers for ion current measurement in mass spectrometry: Journal of Scientific Instruments, v. 42, no. 6, p. 390-394, https://doi.org/10.1088/0950-7671/42/6/305.","startPage":"390","endPage":"394","numberOfPages":"5","costCenters":[],"links":[{"id":204953,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1088/0950-7671/42/6/305"},{"id":219617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"6","noUsgsAuthors":false,"publicationDate":"2002-12-20","publicationStatus":"PW","scienceBaseUri":"505b8d6be4b08c986b3183c1","contributors":{"authors":[{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":359107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Russell, R.D.","contributorId":42349,"corporation":false,"usgs":true,"family":"Russell","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":359105,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kollar, F.","contributorId":50653,"corporation":false,"usgs":true,"family":"Kollar","given":"F.","email":"","affiliations":[],"preferred":false,"id":359106,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185670,"text":"70185670 - 1965 - Vigil Network sites: A sample of data for permanent filing","interactions":[],"lastModifiedDate":"2017-03-27T13:03:24","indexId":"70185670","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Vigil Network sites: A sample of data for permanent filing","docAbstract":"The Vigil Network consists of places where observations are made through time to record changes in landscape features over a long period. Resurveys will usually be made once each year or every few years and the period of observation, hopefully, will extend through and beyond the International Hydrological Decade.
Vigil Network sites will usually be chosen to represent some typical feature of a given landscape. In the example shown here, the feature is a small ephemeral channel in a basin of moderate relief underlain by silty sandstone typical of the surrounding area. Vigil sites are not protected from man's influence and indeed may be selected because of the possible or portending cultural influences. In this respect they differ from the Bench Mark Network whose purpose is to make precise observations of hydrologic factors in areas uninfluenced by and protected from man's use.
The factors which might be observed are many and varied. A few might be mentioned here, others are explained at length elsewhere (Miller and Leopold, 1963; Leopold, 1962). Streamchannel position, form, depth, and profile; vegetation in form of transects or quadrats; soil movement on slopes; rock movement on slopes or in channels. These and many more would yield valuable information on changes with time.
To assure permanence of initial field observations, including reference points, bench marks, and cross sections, brief descriptions, maps, and initial data should be filed identically in designated repositories where the data will be made available for inspection by any interested scientist. It is recommended that the designation of two such locations where records of the type here attached will be filed be taken up by the Coordinating Council of the International Hydrological Decade. In designating such repositories it should be recognized that there is no need for elaborate indexing. The main requirement is merely the maintenance of a simple file where the data are stored and can be inspected or copied by any scientist. There need be no special provision for lending or reproduction services.
The present document is an example showing what data, maps, and descriptions should be included in those permanent files at the two repositories. The material in these repositories should be sufficient to permit someone in the indefinite future to find and remeasure the same features described now. Thus the scientific value of the original surveys increases with time, - provided that the descriptions are sufficient to allow a person to find with assurance the original feature in the field.
It must be visualized that a permanent repository must economize in space. Thus, as the example here shows, the filed material is not all of the original field notes but a summary, brief but descriptive.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666509493401","usgsCitation":"Leopold, L.B., and Emmett, W.W., 1965, Vigil Network sites: A sample of data for permanent filing: International Association of Scientific Hydrology - Bulletin , v. 10, no. 3, p. 12-21, https://doi.org/10.1080/02626666509493401.","productDescription":"10 p.","startPage":"12","endPage":"21","costCenters":[],"links":[{"id":480681,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666509493401","text":"Publisher Index Page"},{"id":338379,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da253fe4b0543bf7fda87d","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":686309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170549,"text":"70170549 - 1965 - Instructions for use of BM-54 and BM-60 bed-material samplers for the collection of samples to be analyzed for organic substances","interactions":[],"lastModifiedDate":"2018-03-05T12:24:49","indexId":"70170549","displayToPublicDate":"1964-05-01T11:15:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":66,"text":"Report","active":false,"publicationSubtype":{"id":1}},"title":"Instructions for use of BM-54 and BM-60 bed-material samplers for the collection of samples to be analyzed for organic substances","docAbstract":"No abstract available.
","language":"English","publisher":"Federal Interagency Sedimentation Project","publisherLocation":"Vicksburg, MS","usgsCitation":"Colby, V., 1965, Instructions for use of BM-54 and BM-60 bed-material samplers for the collection of samples to be analyzed for organic substances: Report, 3 p.","productDescription":"3 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320505,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571f3fbee4b071321fe56a44","contributors":{"authors":[{"text":"Colby, V.C.","contributorId":168886,"corporation":false,"usgs":false,"family":"Colby","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":627589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70217562,"text":"wdrMDDE642 - 1964 - Water quality records in Maryland and Delaware, water year 1964","interactions":[],"lastModifiedDate":"2021-01-22T19:14:49.762449","indexId":"wdrMDDE642","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MD-DE-64-2","displayTitle":"Water Quality Records in Maryland and Delaware, Water Year 1964","title":"Water quality records in Maryland and Delaware, water year 1964","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE642","usgsCitation":"U.S. Geological Survey, 1964, Water quality records in Maryland and Delaware, water year 1964: U.S. Geological Survey Water Data Report MD-DE-64-2, 69 p., https://doi.org/10.3133/wdrMDDE642.","productDescription":"69 p.","costCenters":[{"id":41514,"text":"Maryland-Delaware-District of Columbia Water Science Center","active":true,"usgs":true}],"links":[{"id":382350,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1964/md-de-64-2/wdrMDDE642.pdf","text":"Report","size":"24.3 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Water Data Report MD-DE-64-2"},{"id":382349,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1964/md-de-64-2/wdrMDDE642_coverthb.jpg"}],"country":"United States","state":"Delaware, 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\"}}]}","contact":"","noUsgsAuthors":false,"publicationStatus":"PW"} ,{"id":70197584,"text":"70197584 - 1964 - Subdivision of the San Lorenzo Formation (Eocene and Oligocene) west-central California","interactions":[],"lastModifiedDate":"2023-02-01T14:31:27.84101","indexId":"70197584","displayToPublicDate":"2018-06-12T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Subdivision of the San Lorenzo Formation (Eocene and Oligocene) west-central California","docAbstract":"The San Lorenzo Formation was for many years considered synonymous with Oligocene Series. The formation name was extended, incorrectly in most cases, to rocks as far north as British Columbia and as far south as southern California. The formation in its type area was never adequately studied, resulting in fallacious concepts of its faunas and erroneous correlations.
The San Lorenzo Formation has been subdivided into the Twobar Shale Member of Narizian (late Eocene) age and Rices Mudstone Member of Rufugian and Zemorrian (Eocene and Oligocene) age. Faunas and lithology suggest that the older member was deposited slowly in a bathyal, open-sea environment, whereas the Rices Mudstone Member seems to have been deposited rapidly in a restricted basin. Glauconite at the contact of the members suggests a stratigraphic break in the depositional sequence.
Most, perhaps all, of the so-called characteristic San Lorenzo mollusks are from the upper (Zemorrian) part of the Rices Mudstone Member, or from the overlying Vaqueros Sandstone. The \"transitional sandstone\" of Arnold is Vaqueros, not San Lorenzo.
Subdivision of the San Lorenzo Formation and the discovery of glauconitic marker beds provide additional stratigraphic control in an oil province characterized by poor exposures.
","language":"English","publisher":"American Association of Petroleum Geologists","publisherLocation":"Tulsa, OK","doi":"10.1306/BC743D21-16BE-11D7-8645000102C1865D","usgsCitation":"Brabb, E.E., 1964, Subdivision of the San Lorenzo Formation (Eocene and Oligocene) west-central California: American Association of Petroleum Geologists Bulletin, v. 48, no. 5, p. 670-679, https://doi.org/10.1306/BC743D21-16BE-11D7-8645000102C1865D.","productDescription":"10 p.","startPage":"670","endPage":"679","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":354982,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Lorenzo Formation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -122.45677512208947,\n 37.38122044720332\n ],\n [\n -122.45677512208947,\n 36.95089653986274\n ],\n [\n -121.96980337303017,\n 36.95089653986274\n ],\n [\n -121.96980337303017,\n 37.38122044720332\n ],\n [\n -122.45677512208947,\n 37.38122044720332\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"48","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brabb, Earl E.","contributorId":8545,"corporation":false,"usgs":true,"family":"Brabb","given":"Earl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":737846,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70179736,"text":"70179736 - 1964 - Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part II: Technical report","interactions":[],"lastModifiedDate":"2017-09-06T17:19:54","indexId":"70179736","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"3-II","title":"Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part II: Technical report","docAbstract":"During the 1960 and 1961 water years an annual load of about 2 million tons of dissolved minerals was contributed to the Great Salt Lake area by surficial sources. Almost 60 percent of this load was sodium and chloride. Of the six units contributing to the lake area, three - the Bear River, the Jordan River, and the unit comprising drains and sewage canals – contributed about three-fourths of the runoff and of the load. The water type of these tributaries ranged from bicarbonate in the headwaters to sulfate and chloride near the mouths; the dissolved-solids concentrations were higher in the downstream reaches than in the headwaters.
","language":"English","publisher":"Utah Geological and Minerological Society","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with The College of Mines and Mineral Industries, University of Utah, Salt Lake City, Utah","usgsCitation":"Hahl, D.C., and Langford, R., 1964, Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part II: Technical report: Utah Geological and Mineralogical Survey Water-Resources Bulletin 3-II, 40 p.","productDescription":"40 p.","numberOfPages":"44","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333226,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345530,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179734","text":"Part I: Selected hydrologic data"},{"id":345529,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-3part2.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.2305908203125,\n 40.59727063442024\n ],\n [\n -113.2305908203125,\n 41.795888098191426\n ],\n [\n -111.81884765624999,\n 41.795888098191426\n ],\n [\n -111.81884765624999,\n 40.59727063442024\n ],\n [\n -113.2305908203125,\n 40.59727063442024\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d2","contributors":{"authors":[{"text":"Hahl, D. C.","contributorId":57436,"corporation":false,"usgs":true,"family":"Hahl","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":658475,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langford, R.H.","contributorId":59426,"corporation":false,"usgs":true,"family":"Langford","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":658476,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70180001,"text":"70180001 - 1964 - Developing a state water plan: Ground-water conditions in Utah, spring of 1964","interactions":[],"lastModifiedDate":"2017-01-23T11:29:18","indexId":"70180001","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"2","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1964","docAbstract":"This report is the first in a series of annual reports which will describe ground-water conditions in Utah. It was prepared cooperatively by the U.S. Geological Survey and the Utah Water and Power Board and was designed to provide the data for interested parties, such as legislators, administrators, and planners to keep abreast of changing ground-water conditions in the state. Because this report is the first of the series, it necessarily includes certain background and descriptive information which gives a broad general picture of ground-water conditions. Subsequent reports will discuss only changes that have taken place during the previous year.
Many of the data used in the preparation of the report were collected by the Geological Survey in cooperation with the Utah State Engineer during past and continuing programs. The well-location map and some statistical information about numbers of wells in the State were prepared by digital computer from the Utah Resources Information System, University of Utah, utilizing records which were compiled largely from the files of the Utah State Engineer. R.E. Marsell, geological consultant to the Utah Water and Power Board, first suggested that this report be prepared.
","language":"English","publisher":"Utah Water and Power Board","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Arnow, T., Butler, R., Mower, R.W., Gates, J., Cordova, R., Carpenter, C., Bjorklund, L., Feltis, R., Robinson, G., and Sandberg, G.W., 1964, Developing a state water plan: Ground-water conditions in Utah, spring of 1964: Cooperative Investigations Report 2, 104 p.","productDescription":"104 p.","numberOfPages":"208","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333666,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333665,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-201"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58863a15e4b0cad700058b71","contributors":{"authors":[{"text":"Arnow, Ted","contributorId":84733,"corporation":false,"usgs":true,"family":"Arnow","given":"Ted","affiliations":[],"preferred":false,"id":659661,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, R.G.","contributorId":60706,"corporation":false,"usgs":true,"family":"Butler","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":659662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659663,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gates, Joseph S.","contributorId":21647,"corporation":false,"usgs":true,"family":"Gates","given":"Joseph S.","affiliations":[],"preferred":false,"id":659664,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Cordova, R.M.","contributorId":77511,"corporation":false,"usgs":true,"family":"Cordova","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":659665,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Carpenter, C.H.","contributorId":69229,"corporation":false,"usgs":true,"family":"Carpenter","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":659666,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659667,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":659668,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Robinson, G.B.","contributorId":178487,"corporation":false,"usgs":true,"family":"Robinson","given":"G.B.","email":"","affiliations":[],"preferred":false,"id":659669,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659670,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}} ,{"id":70179723,"text":"70179723 - 1964 - Geology and ground-water resources of the Jordan Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-06T17:26:29","indexId":"70179723","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"7","title":"Geology and ground-water resources of the Jordan Valley, Utah","docAbstract":"The Jordan Valley occupies about 400 square miles in the central part of Salt Lake County in north-central Utah. Salt Lake City, the capital of Utah, is in the northeastern part of the valley. The valley is at the eastern margin of the Basin and range physiographic province, and it is bounded on the northeast, east, south, and west by mountain ranges. The valley is drained by the Jordan River which enters through a water gap in the mountains to the south, flows north, and empties into the Great Salt Lake, which forms the northwestern border of the valley.
","language":"English","publisher":"Utah Geological and Mineralogical Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Marine, I.W., and Price, D., 1964, Geology and ground-water resources of the Jordan Valley, Utah: Utah Geological and Mineralogical Survey Water-Resources Bulletin 7, 67 p.","productDescription":"67 p.","numberOfPages":"79","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333200,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333199,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179625","text":"Utah State Engineer Water Circular 1"},{"id":333198,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-7.pdf"}],"country":"United States","state":"Utah","otherGeospatial":"Jordan Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -112.22122192382812,\n 40.72540497175607\n ],\n [\n -112.10861206054688,\n 40.693134153308065\n ],\n [\n -112.13470458984375,\n 40.59935608796518\n ],\n [\n -112.08663940429688,\n 40.54093880017256\n ],\n [\n -112.09899902343749,\n 40.51901917108279\n ],\n [\n -112.07565307617186,\n 40.48873742102282\n ],\n [\n -112.03994750976562,\n 40.48455955508278\n ],\n [\n -111.98638916015625,\n 40.478292268560175\n ],\n [\n -111.95205688476562,\n 40.45321727150385\n ],\n [\n -111.93283081054688,\n 40.43126897044754\n ],\n [\n -111.87515258789062,\n 40.450082238680295\n ],\n [\n -111.88339233398438,\n 40.46889024168825\n ],\n [\n -111.8463134765625,\n 40.49709237269567\n ],\n [\n -111.81198120117188,\n 40.526326510744006\n ],\n [\n -111.78726196289061,\n 40.565981025008355\n ],\n [\n -111.785888671875,\n 40.608739823836984\n ],\n [\n -111.78176879882812,\n 40.61812224225511\n ],\n [\n -111.8023681640625,\n 40.65459689980922\n ],\n [\n -111.77078247070312,\n 40.68063802521456\n ],\n [\n -111.79000854492188,\n 40.713955826286046\n ],\n [\n -111.80923461914062,\n 40.73581157695217\n ],\n [\n -111.80923461914062,\n 40.74725696280421\n ],\n [\n -111.8353271484375,\n 40.773261878622634\n ],\n [\n -111.86279296875,\n 40.78885994449482\n ],\n [\n -111.87377929687499,\n 40.79717741518766\n ],\n [\n -111.8902587890625,\n 40.78885994449482\n ],\n [\n -111.90399169921874,\n 40.81380923056958\n ],\n [\n -111.88201904296875,\n 40.83563216247778\n ],\n [\n -111.86004638671875,\n 40.853293085675155\n ],\n [\n -112.13058471679686,\n 40.83251504043271\n ],\n [\n -112.12921142578125,\n 40.79925662005228\n ],\n [\n -112.16903686523436,\n 40.75245875985305\n ],\n [\n -112.18551635742186,\n 40.73893324113601\n ],\n [\n -112.22122192382812,\n 40.72540497175607\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d4","contributors":{"authors":[{"text":"Marine, I. Wendell","contributorId":49339,"corporation":false,"usgs":true,"family":"Marine","given":"I.","email":"","middleInitial":"Wendell","affiliations":[],"preferred":false,"id":658436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":658437,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70161770,"text":"70161770 - 1964 - Larval echinochasmus (trematoda: echinostomatidae) in rainbow trout, Salmo gairdneri","interactions":[],"lastModifiedDate":"2016-01-06T08:53:27","indexId":"70161770","displayToPublicDate":"2015-10-05T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"title":" Larval echinochasmus (trematoda: echinostomatidae) in rainbow trout, Salmo gairdneri","docAbstract":"No abstract available.
","language":"English","publisher":"Allen Press","doi":"10.2307/3275627","usgsCitation":"Uzmann, J., and Hayduk, S., 1964, Larval echinochasmus (trematoda: echinostomatidae) in rainbow trout, Salmo gairdneri: Journal of Parasitology, v. 50, no. 4, p. 586-586, https://doi.org/10.2307/3275627.","productDescription":"1 p.","startPage":"586","endPage":"586","numberOfPages":"1","costCenters":[],"links":[{"id":313880,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568e48c9e4b0e7a44bc41808","contributors":{"authors":[{"text":"Uzmann, J. R.","contributorId":38647,"corporation":false,"usgs":true,"family":"Uzmann","given":"J. R.","affiliations":[],"preferred":false,"id":587721,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayduk, S.H.","contributorId":151275,"corporation":false,"usgs":false,"family":"Hayduk","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":587722,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}