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,{"id":64460,"text":"gp190 - 1959 - Aeromagnetic and geologic map of the Santa Clara quadrangle and part of the St. Regis quadrangle, Franklin County, New York","interactions":[],"lastModifiedDate":"2022-04-11T20:52:24.633217","indexId":"gp190","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"190","title":"Aeromagnetic and geologic map of the Santa Clara quadrangle and part of the St. Regis quadrangle, Franklin County, New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp190","usgsCitation":"Balsley, J.R., and Buddington, A.F., 1959, Aeromagnetic and geologic map of the Santa Clara quadrangle and part of the St. Regis quadrangle, Franklin County, New York: U.S. Geological Survey Geophysical Investigations Map 190, Report: 1 p.; 1 Plate: 24.33 × 28.81 inches, https://doi.org/10.3133/gp190.","productDescription":"Report: 1 p.; 1 Plate: 24.33 × 28.81 inches","costCenters":[],"links":[{"id":392522,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3107.htm"},{"id":251212,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0190/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":251213,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0190/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":252001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0190/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"New York","county":"Franklin County","otherGeospatial":"Santa Clara quadrangle, St. Regis quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.5,44.4167 ], [ -74.5,44.75 ], [ -74.25,44.75 ], [ -74.25,44.4167 ], [ -74.5,44.4167 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db6989ad","contributors":{"authors":[{"text":"Balsley, J. R. Jr.","contributorId":79535,"corporation":false,"usgs":true,"family":"Balsley","given":"J.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270972,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buddington, A. F.","contributorId":40211,"corporation":false,"usgs":true,"family":"Buddington","given":"A.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":270971,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36290,"text":"b1028N - 1959 - Some effects of recent volcanic ash falls, with especial reference to Alaska","interactions":[],"lastModifiedDate":"2022-12-28T22:01:54.507238","indexId":"b1028N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1028","chapter":"N","title":"Some effects of recent volcanic ash falls, with especial reference to Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1028N","usgsCitation":"Wilcox, R.E., 1959, Some effects of recent volcanic ash falls, with especial reference to Alaska: U.S. Geological Survey Bulletin 1028, 68 p., https://doi.org/10.3133/b1028N.","productDescription":"68 p.","startPage":"409","endPage":"476","costCenters":[],"links":[{"id":411151,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20600.htm","linkFileType":{"id":5,"text":"html"}},{"id":165159,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1028n/report-thumb.jpg"},{"id":93823,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1028n/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Russia, United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -148,\n              62\n            ],\n            [\n              -179.9,\n              62\n            ],\n            [\n              -179.9,\n              51\n            ],\n            [\n              -148,\n              51\n            ],\n            [\n              -148,\n              62\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              179.9,\n              62\n            ],\n            [\n              172,\n              62\n            ],\n            [\n              172,\n              51\n            ],\n            [\n              179.9,\n              51\n            ],\n            [\n              179.9,\n              62\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e93a9","contributors":{"authors":[{"text":"Wilcox, Ray E.","contributorId":63074,"corporation":false,"usgs":true,"family":"Wilcox","given":"Ray","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":216078,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2030,"text":"wsp1475A - 1959 - Hydrologic data, Wind River and Fifteen Mile Creek basins, Wyoming, 1947-54","interactions":[],"lastModifiedDate":"2023-01-17T21:00:21.670922","indexId":"wsp1475A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1475","chapter":"A","title":"Hydrologic data, Wind River and Fifteen Mile Creek basins, Wyoming, 1947-54","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475A","usgsCitation":"King, N.J., 1959, Hydrologic data, Wind River and Fifteen Mile Creek basins, Wyoming, 1947-54: U.S. Geological Survey Water Supply Paper 1475, Report: iv, 44 p.; 3 Plates: 14.40 x 21.24 inches or smaller, https://doi.org/10.3133/wsp1475A.","productDescription":"Report: iv, 44 p.; 3 Plates: 14.40 x 21.24 inches or smaller","costCenters":[],"links":[{"id":411995,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24405.htm","linkFileType":{"id":5,"text":"html"}},{"id":27506,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27505,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27504,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27503,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137647,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475a/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Wind River and Fifteen Mile Creek basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110,\n              43.917\n            ],\n            [\n              -110,\n              42.25\n            ],\n            [\n              -107.25,\n              42.25\n            ],\n            [\n              -107.25,\n              43.917\n            ],\n            [\n              -110,\n              43.917\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607160","contributors":{"authors":[{"text":"King, Norman Julius","contributorId":57048,"corporation":false,"usgs":true,"family":"King","given":"Norman","email":"","middleInitial":"Julius","affiliations":[],"preferred":false,"id":144553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56161,"text":"ofr5976 - 1959 - Surface waters of Illinois River basin in Arkansas and Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:12:10","indexId":"ofr5976","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-76","title":"Surface waters of Illinois River basin in Arkansas and Oklahoma","docAbstract":"The estimated runoff from the Illinois River basin of 1,660 square miles has averaged 1,160,000 acre-feet per year during the water years 1938-56, equivalent to an average annual runoff depth of 13.1 inches. About 47 percent of the streamflow is contributed from drainage in Arkansas, where an average of 550,000 acre-ft per year runs off from 755 square miles, 45.5 percent of the total drainage area.\r\nThe streamflow is highly variable. Twenty-two years of record for Illinois River near Tahlequah, Okla., shows a variation in runoff for the water year 1945 in comparison with 1954 in a ratio of almost 10 to 1. Runoff in 1927 may have exceeded that of 1945, according to records for White River at Beaver, Ark., the drainage basin just east of the Illinois River basin. Variation in daily discharge is suggested by a frequency analysis of low flows at the gaging station near Tahlequah, Okla. The mean flow at that site is 901 cfs (cubic feet per second), the median daily flow is 350 cfs, and the lowest 30-day mean flow in a year probably will be less than 130 cfs half of the time and less than 20 cfs every 10 years on the average.\r\n\r\nThe higher runoff tends to occur in the spring months, March to May, a 3-month period that, on the average, accounts for almost half of the annual flow. High runoff may occur during any month in the year, but in general, the streamflow is the lowest in the summer. The mean monthly flow of Illinois River near Tahlequah, Okla., for September is about 11 percent of that for May. Records show that there is flow throughout the year in Illinois River and its principal tributaries Osage Creek, Flint Creek and Barren Fork.\r\n\r\nThe high variability in streamflow in this region requires the development of storage by impoundment if maximum utilization of the available water supplies is to be attained. For example, a 120-day average low flow of 22 cfs occurred in 1954 at Illinois River near Tahlequah, Okla. To have maintained the flow at 350 cfs, the median daily flow during the 19-year base period, an impoundment at that site would have required a usable storage of 185,000 acre-ft to satisfy this demand during the drought years 1954-1956.\r\n\r\nThe surface waters of the Illinois River basin are excellent quality being suitable for municipal, agriculture and most industrial uses. The average concentration of the dissolved mineral content is about 105 ppm (parts per million) and the hardness about 85 ppm. The water is slightly alkaline, having a range of pH values from 7.2 to 8.0.\r\n\r\nThis report gives the estimated average discharge at gaging stations and approximations of average discharge at the State line for 3 sub-basins during the 19-year period October 1937 to September 1956, used as a base period in this report. Duration-of-flow data for various percentages of the time are shown for the period of observed record at the gaging stations; similar data are estimated for the selected base period. Storage requirements to sustain flow during the recent drought years are given for 3 stations. The streamflow records in the basin are presented on a monthly and annual basis through September 1957; provisional records for 3 stations are included through July 1958 for correlation purposes. Results of discharge measurements are given for miscellaneous sites where low-flow observations have been made.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr5976","usgsCitation":"Laine, L., 1959, Surface waters of Illinois River basin in Arkansas and Oklahoma: U.S. Geological Survey Open-File Report 59-76, 65 p., 13 figs., https://doi.org/10.3133/ofr5976.","productDescription":"65 p., 13 figs.","costCenters":[],"links":[{"id":184636,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6912cd","contributors":{"authors":[{"text":"Laine, L.L.","contributorId":100464,"corporation":false,"usgs":true,"family":"Laine","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":254854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56145,"text":"ofr5948 - 1959 - Geology of the USGS and Ranier Tunnel areas, Nevada Test Site","interactions":[],"lastModifiedDate":"2012-02-02T00:12:11","indexId":"ofr5948","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-48","title":"Geology of the USGS and Ranier Tunnel areas, Nevada Test Site","language":"ENGLISH","doi":"10.3133/ofr5948","usgsCitation":"Hansen, W.R., and Lemke, R.W., 1959, Geology of the USGS and Ranier Tunnel areas, Nevada Test Site: U.S. Geological Survey Open-File Report 59-48, 111 p., 8 figs., 7 tables, https://doi.org/10.3133/ofr5948.","productDescription":"111 p., 8 figs., 7 tables","costCenters":[],"links":[{"id":184439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca61","contributors":{"authors":[{"text":"Hansen, W. R.","contributorId":59378,"corporation":false,"usgs":true,"family":"Hansen","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":254821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lemke, R. W.","contributorId":92319,"corporation":false,"usgs":true,"family":"Lemke","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":254822,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56144,"text":"ofr5942 - 1959 - Low-flow analysis of Pearl River at Jackson, Mississippi","interactions":[{"subject":{"id":56144,"text":"ofr5942 - 1959 - Low-flow analysis of Pearl River at Jackson, Mississippi","indexId":"ofr5942","publicationYear":"1959","noYear":false,"title":"Low-flow analysis of Pearl River at Jackson, Mississippi"},"predicate":"SUPERSEDED_BY","object":{"id":2081,"text":"wsp1899M - 1972 - Geohydrologic summary of the Pearl River basin, Mississippi and Louisiana","indexId":"wsp1899M","publicationYear":"1972","noYear":false,"chapter":"M","title":"Geohydrologic summary of the Pearl River basin, Mississippi and Louisiana"},"id":1}],"supersededBy":{"id":2081,"text":"wsp1899M - 1972 - Geohydrologic summary of the Pearl River basin, Mississippi and Louisiana","indexId":"wsp1899M","publicationYear":"1972","noYear":false,"title":"Geohydrologic summary of the Pearl River basin, Mississippi and Louisiana"},"lastModifiedDate":"2012-02-02T00:12:11","indexId":"ofr5942","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-42","title":"Low-flow analysis of Pearl River at Jackson, Mississippi","language":"ENGLISH","doi":"10.3133/ofr5942","usgsCitation":"Golden, H.G., 1959, Low-flow analysis of Pearl River at Jackson, Mississippi: U.S. Geological Survey Open-File Report 59-42, 6 p., 3 charts, https://doi.org/10.3133/ofr5942.","productDescription":"6 p., 3 charts","costCenters":[],"links":[{"id":184438,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644a26","contributors":{"authors":[{"text":"Golden, H. G.","contributorId":56280,"corporation":false,"usgs":true,"family":"Golden","given":"H.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":254820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":4757,"text":"wsp1473_ed1 - 1959 - Study and interpretation of the chemical characteristics of natural water","interactions":[],"lastModifiedDate":"2019-11-25T11:55:33","indexId":"wsp1473_ed1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1473","title":"Study and interpretation of the chemical characteristics of natural water","docAbstract":"<p>The chemical composition of natural water is derived from many different sources of solutes, including gases and aerosols from the atmosphere, weathering and erosion of rocks and soil, solution or precipitation reactions occurring below the land surface, and cultural effects resulting from activities of man. Some of the processes of solution or precipitation of minerals can be closely evaluated by means of principles of chemical equilibrium including the law of mass action and the Nernst equation. Other processes are irreversible and require consideration of reaction mechanisms and rates. The chemical composition of the crustal rocks of the earth and the composition of the ocean and the atmosphere are significant in evaluating sources of solutes in natural fresh water.</p>\n<p>The ways in which solutes are taken up or precipitated and the amounts present in solution are influenced by many environmental factors, especially climate, structure and position: of rock strata, and biochemical effects associated with life cycles of plants and animals, both microscopic and macroscopic. Taken all together and in application with the further influence of the general circulation of all water in the hydrologic cycle, the chemical principles and environmental factors form a basis for the developing science of natural-water chemistry.</p>\n<p>Fundamental data used in the determination of water quality are obtained by the chemical analysis of water samples in the laboratory or onsite sensing of chemical properties in the field. Sampling is complicated by changes in composition of moving water and the effects of particulate suspended material. Most of the constituents determined are reported in gravimetric units, usually milligrams per liter or milliequivalents per liter.</p>\n<p>More than 60 constituents and properties are included in water analyses frequently enough to provide a basis for consideration of the sources from which each is generally derived, most probable forms of elements and ions in solution, solubility controls, expected concentration ranges and other chemical factors. Concentrations of elements that are commonly present in amounts less than a few tens of micrograms per liter cannot always be easily explained, but present information suggests many are controlled by solubility of hydroxide or carbonate or by sorption on solid particles.</p>\n<p>Chemical analyses may be grouped and statistically evaluated by averages, frequency distributions, or ion correlations to summarize large volumes of data. Graphing of analyses or of groups of analyses aids in showing chemical relationships among waters, probable sources of solutes, areal water-quality regimen, and water-resources evaluation. Graphs may show water type based on chemical composition, relationships among ions, or groups of ions in individual waters or&nbsp;many waters considered simultaneously. The relationships of water quality to hydrologic parameters, such as stream discharge rate or ground-water flow patterns, can be shown by mathematical equations, graphs, and maps.</p>\n<p>About 75 water analyses selected from the literature are tabulated to illustrate the relationships described, and some of these, along with many others that are not tabulated, are also utilized in demonstrating graphing and mapping techniques.</p>\n<p>Relationships of water composition to source rock type are illustrated by graphs of some of the tabulated analyses. Activities of man may modify water composition extensively through direct effects of pollution and indirect results of water development, such as intrusion of sea water in ground-water aquifiers.</p>\n<p>Water-quality standards for domestic, agricultural, and industrial use have been published by various agencies. Irrigation project requirements for water quality are particularly intricate.</p>\n<p>Fundamental knowledge of processes that control natural water composition is required for rational management of water quality.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wsp1473_ed1","usgsCitation":"Hem, J.D., 1959, Study and interpretation of the chemical characteristics of natural water (1st edition): U.S. Geological Survey Water Supply Paper 1473, Report: ix, 269 p.; 2 Plates: 7.24 x 10.39 inches and 19.01 x 7.21 inches, https://doi.org/10.3133/wsp1473_ed1.","productDescription":"Report: ix, 269 p.; 2 Plates: 7.24 x 10.39 inches and 19.01 x 7.21 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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,{"id":2674,"text":"wsp1542A - 1959 - Flow-duration curves","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1542A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1542","chapter":"A","title":"Flow-duration curves","docAbstract":"The flow-duration curve is a cumulative frequency curve that shows the percent of time specified discharges were equaled or exceeded during a given period. It combines in one curve the flow characteristics of a stream throughout the range of discharge, without regard to the sequence of occurrence. If the period upon which the curve is based represents the long-term flow of a stream, the curve may be used to predict the distribution of future flows for water- power, water-supply, and pollution studies. \r\n\r\nThis report shows that differences in geology affect the low-flow ends of flow-duration curves of streams in adjacent basins. Thus, duration curves are useful in appraising the geologic characteristics of drainage basins. \r\n\r\nA method for adjusting flow-duration curves of short periods to represent long-term conditions is presented. The adjustment is made by correlating the records of a short-term station with those of a long-term station.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1542A","usgsCitation":"Searcy, J.K., 1959, Flow-duration curves: U.S. Geological Survey Water Supply Paper 1542, iv, 33 p. :ill. ;24 cm.; Reprinted 1963, https://doi.org/10.3133/wsp1542A.","productDescription":"iv, 33 p. :ill. ;24 cm.; Reprinted 1963","costCenters":[],"links":[{"id":138261,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1542a/report-thumb.jpg"},{"id":29024,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1542a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de861","contributors":{"authors":[{"text":"Searcy, James Kincheon","contributorId":54175,"corporation":false,"usgs":true,"family":"Searcy","given":"James","email":"","middleInitial":"Kincheon","affiliations":[],"preferred":false,"id":145594,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2012,"text":"wsp1468 - 1959 - Geology and ground-water resources of Clay County, Nebraska","interactions":[{"subject":{"id":51835,"text":"ofr5579 - 1955 - Hydrology of Clay County, Nebraska, with special reference to recharge","indexId":"ofr5579","publicationYear":"1955","noYear":false,"title":"Hydrology of Clay County, Nebraska, with special reference to recharge"},"predicate":"SUPERSEDED_BY","object":{"id":2012,"text":"wsp1468 - 1959 - Geology and ground-water resources of Clay County, Nebraska","indexId":"wsp1468","publicationYear":"1959","noYear":false,"title":"Geology and ground-water resources of Clay County, Nebraska"},"id":1}],"lastModifiedDate":"2022-02-17T19:58:29.014942","indexId":"wsp1468","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1468","title":"Geology and ground-water resources of Clay County, Nebraska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1468","usgsCitation":"Keech, C.F., Dreeszen, V., and Rainwater, F.H., 1959, Geology and ground-water resources of Clay County, Nebraska: U.S. Geological Survey Water Supply Paper 1468, Report: vi, 157 p.; 4 Plates: 17.50 × 14.62 inches or smaller, https://doi.org/10.3133/wsp1468.","productDescription":"Report: vi, 157 p.; 4 Plates: 17.50 × 14.62 inches or smaller","costCenters":[],"links":[{"id":27466,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1468/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27465,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1468/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27468,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1468/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27467,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1468/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109947,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24400.htm","linkFileType":{"id":5,"text":"html"},"description":"24400"},{"id":27464,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1468/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137580,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1468/report-thumb.jpg"}],"country":"United States","state":"Nebraska","county":"Clay County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-97.8245,40.6985],[-97.826,40.6105],[-97.8256,40.5243],[-97.8246,40.4367],[-97.8236,40.3505],[-97.9371,40.3506],[-98.0493,40.352],[-98.2744,40.3507],[-98.278,40.3512],[-98.2798,40.524],[-98.2797,40.5277],[-98.2799,40.5699],[-98.2797,40.5794],[-98.2796,40.6107],[-98.278,40.6987],[-97.9385,40.6981],[-97.8245,40.6985]]]},\"properties\":{\"name\":\"Clay\",\"state\":\"NE\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685d52","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":144527,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dreeszen, V. H.","contributorId":8825,"corporation":false,"usgs":true,"family":"Dreeszen","given":"V. H.","affiliations":[],"preferred":false,"id":144525,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rainwater, F. H.","contributorId":41402,"corporation":false,"usgs":true,"family":"Rainwater","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144526,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3067,"text":"wsp1445 - 1959 - Surface water supply of the United States, 1956, Part XI, Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:37","indexId":"wsp1445","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1445","title":"Surface water supply of the United States, 1956, Part XI, Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1445","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1959, Surface water supply of the United States, 1956, Part XI, Pacific slope basins in California: U.S. Geological Survey Water Supply Paper 1445, xii, 601 p. ;23 cm., https://doi.org/10.3133/wsp1445.","productDescription":"xii, 601 p. ;23 cm.","costCenters":[],"links":[{"id":139439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1445/report-thumb.jpg"},{"id":29925,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1445/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696102","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528055,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70056313,"text":"tem1096 - 1959 - Preliminary geologic map of the Circle Cliffs 1 NE quadrangle, Garfield County, Utah","interactions":[],"lastModifiedDate":"2014-03-04T14:34:22","indexId":"tem1096","displayToPublicDate":"1979-01-30T10:17:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1096","title":"Preliminary geologic map of the Circle Cliffs 1 NE quadrangle, Garfield County, Utah","docAbstract":"No abstract available","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem1096","collaboration":"Prepared in cooperation the the U.S. Commission on Atomic Energy","usgsCitation":"Davidson, E., and Cadigan, R., 1959, Preliminary geologic map of the Circle Cliffs 1 NE quadrangle, Garfield County, Utah: U.S. Geological Survey Trace Elements Memorandum 1096, Report: 1 p.; Plate: 31.18 inches x 42.20 inches, https://doi.org/10.3133/tem1096.","productDescription":"Report: 1 p.; Plate: 31.18 inches x 42.20 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":279161,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/1096/report-thumb.jpg"},{"id":283349,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/1096/plate-1.pdf"},{"id":283350,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/1096/report.pdf"}],"country":"United States","state":"Utah","county":"Garfield County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.1250,37.8750 ], [ -111.1250,38.0000 ], [ -111.0000,38.0000 ], [ -111.0000,37.8750 ], [ -111.1250,37.8750 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"528c96b6e4b0c629af44dddc","contributors":{"authors":[{"text":"Davidson, Edward S.","contributorId":75843,"corporation":false,"usgs":true,"family":"Davidson","given":"Edward S.","affiliations":[],"preferred":false,"id":486517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cadigan, Robert A.","contributorId":93514,"corporation":false,"usgs":true,"family":"Cadigan","given":"Robert A.","affiliations":[],"preferred":false,"id":486518,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70207364,"text":"70207364 - 1959 - Re-evaluation of the salt chronology of several Great Basin lakes: A discussion","interactions":[],"lastModifiedDate":"2019-12-19T08:05:02","indexId":"70207364","displayToPublicDate":"1959-12-31T11:51:40","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Re-evaluation of the salt chronology of several Great Basin lakes: A discussion","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1959)70[637:ROTSCO]2.0.CO;2","issn":"00167606","usgsCitation":"Feth, J.H., 1959, Re-evaluation of the salt chronology of several Great Basin lakes: A discussion: Geological Society of America Bulletin, v. 70, no. 5, p. 637-640, https://doi.org/10.1130/0016-7606(1959)70[637:ROTSCO]2.0.CO;2.","productDescription":"4 p. ","startPage":"637","endPage":"640","costCenters":[],"links":[{"id":370406,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States, Canada","otherGeospatial":"Great Lakes basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.900390625,\n              40.97989806962013\n            ],\n            [\n              -75.498046875,\n              40.97989806962013\n            ],\n            [\n              -75.498046875,\n              49.26780455063753\n            ],\n            [\n              -92.900390625,\n              49.26780455063753\n            ],\n            [\n              -92.900390625,\n              40.97989806962013\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"70","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206630,"text":"70206630 - 1959 - Upper ordovician (?) and upper silurian formations of the northern Klamath Mountains, California","interactions":[],"lastModifiedDate":"2019-11-14T07:59:20","indexId":"70206630","displayToPublicDate":"1959-12-31T07:50:48","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Upper ordovician (?) and upper silurian formations of the northern Klamath Mountains, California","title":"Upper ordovician (?) and upper silurian formations of the northern Klamath Mountains, California","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English ","doi":"10.1130/0016-7606(1959)70[645:UOAUSF]2.0.CO;2","issn":"00167606","usgsCitation":"Wells, F.G., Walker, G., and Merriam, C., 1959, Upper ordovician (?) and upper silurian formations of the northern Klamath Mountains, California: Geological Society of America Bulletin, v. 70 , no. 5, p. 645-650 , https://doi.org/10.1130/0016-7606(1959)70[645:UOAUSF]2.0.CO;2.","productDescription":"6 p. 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,{"id":37548,"text":"ssrw42 - 1959 - Mourning dove management units: A progress report","interactions":[],"lastModifiedDate":"2022-12-02T15:48:40.072773","indexId":"ssrw42","displayToPublicDate":"1959-12-31T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"42","title":"Mourning dove management units: A progress report","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Kiel, W.H., 1959, Mourning dove management units: A progress report: Special Scientific Report  - Wildlife 42, iv, 24 p.","productDescription":"iv, 24 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Jr.","contributorId":100449,"corporation":false,"usgs":true,"family":"Kiel","given":"William","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":218239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197729,"text":"70197729 - 1959 - K-feldspar content of Jurassic and Cretaceous graywackes of northern Coast Ranges and Sacramento Valley, California","interactions":[],"lastModifiedDate":"2023-02-01T14:38:56.550016","indexId":"70197729","displayToPublicDate":"1959-12-31T00:00:00","publicationYear":"1959","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":"K-feldspar content of Jurassic and Cretaceous graywackes of northern Coast Ranges and Sacramento Valley, California","docAbstract":"<div id=\"115644527\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Graywackes of Late Jurassic to Late Cretaceous age are the predominant rocks in the northern Coast Ranges and the western Sacramento Valley provinces in California. These graywackes are similar in appearance, but their content of K-feldspar, which can be readily estimated after selective staining, differs widely. Study of several hundred specimens indicates that K-feldspar content is helpful in correlating or distinguishing these rocks, and sheds light on the geologic history of western California.</p><p>In the Sacramento Valley a conformable sequence of Knoxville (Upper Jurassic), Shasta (Lower Cretaceous), and Upper Cretaceous rocks progressively increases in average K-feldspar content with decreasing age. Graywackes of the Franciscan formation, lying in the Coast Ranges farther west, generally contain no K-feldspar, although some contain a trace, and a few of more uncertain affiliation contain large amounts. Another belt of graywackes, west of the Franciscan formation and paralleling the Pacific shore, contains nearly as much K-feldspar as the Upper Cretaceous rocks of the Sacramento Valley, and most of these rocks are probably of middle Cretaceous age.</p><p>The writers attribute the increase of K-feldspar with decreasing age of the rocks of the Sacramento Valley to changes in the source area, which is believed to be the Klamath Mountains and the Sierra Nevada. The changes include an increase in proportion of granitic rocks to others as the areas were stripped, and more abundant K-feldspar in the younger granitic rocks. The high K-feldspar content in the middle Cretaceous rocks of the coastal belt suggests that the rocks were deposited in the same basin as the Sacramento Valley rocks.</p></div>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/0BDA5F54-16BD-11D7-8645000102C1865D","usgsCitation":"Bailey, E.H., and Irwin, W.P., 1959, K-feldspar content of Jurassic and Cretaceous graywackes of northern Coast Ranges and Sacramento Valley, California: American Association of Petroleum Geologists Bulletin, v. 43, no. 12, p. 2797-2809, https://doi.org/10.1306/0BDA5F54-16BD-11D7-8645000102C1865D.","productDescription":"13 p.","startPage":"2797","endPage":"2809","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355158,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Coast Ranges, Sacramento Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -124.3589017191801,\n              40.455701586167095\n            ],\n            [\n              -124.3589017191801,\n              38.971511643076354\n            ],\n            [\n              -122.52733835266014,\n              38.971511643076354\n            ],\n            [\n              -122.52733835266014,\n              40.455701586167095\n            ],\n            [\n              -124.3589017191801,\n              40.455701586167095\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"43","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bailey, Edgar Herbert","contributorId":85179,"corporation":false,"usgs":true,"family":"Bailey","given":"Edgar","email":"","middleInitial":"Herbert","affiliations":[],"preferred":false,"id":738313,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Irwin, William Porter","contributorId":85648,"corporation":false,"usgs":true,"family":"Irwin","given":"William","email":"","middleInitial":"Porter","affiliations":[],"preferred":false,"id":738314,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010688,"text":"70010688 - 1959 - Age of marginal Wisconsin drift at Corry, northwestern Pennsylvania","interactions":[],"lastModifiedDate":"2026-02-27T15:22:26.019651","indexId":"70010688","displayToPublicDate":"1959-12-25T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Age of marginal Wisconsin drift at Corry, northwestern Pennsylvania","docAbstract":"Marl began to accumulate about 14,000 years ago, as determined by radiocarbon dating, in a pond in a kettle hole in Kent drift at Corry, Pa., 9 miles inside the Wisconsin drift margin. This radiocarbon age represents the minimum time since the disappearance of the ice from Corry and confirms an assignment of Cary age to the drift.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.130.3391.1760.a","issn":"00368075","usgsCitation":"Droste, J., Rubin, M., and White, G.W., 1959, Age of marginal Wisconsin drift at Corry, northwestern Pennsylvania: Science, v. 130, no. 3391, p. 1760-1760, https://doi.org/10.1126/science.130.3391.1760.a.","productDescription":"1 p.","startPage":"1760","endPage":"1760","costCenters":[],"links":[{"id":219408,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Pennsylvania","city":"Corry","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -79.68200482460028,\n              41.947621733403906\n            ],\n            [\n              -79.68200482460028,\n              41.904127695039165\n            ],\n            [\n              -79.60218635375541,\n              41.904127695039165\n            ],\n            [\n              -79.60218635375541,\n              41.947621733403906\n            ],\n            [\n              -79.68200482460028,\n              41.947621733403906\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"130","issue":"3391","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e8efe4b0c8380cd47fb8","contributors":{"authors":[{"text":"Droste, J.B.","contributorId":98463,"corporation":false,"usgs":true,"family":"Droste","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":359432,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rubin, M.","contributorId":88079,"corporation":false,"usgs":true,"family":"Rubin","given":"M.","email":"","affiliations":[],"preferred":false,"id":359431,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, G. W.","contributorId":62293,"corporation":false,"usgs":true,"family":"White","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70207256,"text":"70207256 - 1959 - Peneconcordant uranium deposit: A proposed term","interactions":[],"lastModifiedDate":"2020-06-01T20:02:16.284558","indexId":"70207256","displayToPublicDate":"1959-12-13T13:25:59","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Peneconcordant uranium deposit: A proposed term","docAbstract":"<p><span>The term peneconcordant is proposed to describe the form of the numerous and highly productive U deposits in sedimentary rocks of the Colorado Plateau, Wyoming, the Dakotas, and Texas. Peneconcordant U deposits are tabular, lenticular, or irregularly-shaped masses of widely differing size that are, in general, concordant to the gross sedimentary structures of the enclosing rock but that in detail cut across sedimentary structures. They differ from vein deposits in that they do not occupy or follow fractures or shear zones in the sedimentary rocks. Furthermore, they are not coextensive with a specific lithologic unit, such as U-bearing marine black shale. The many terms now used to describe these U deposits are based variously on petrographic, mineralogic, geographic, and genetic considerations; none is satisfactory for describing all these deposits having a common and distinctive form. Furthermore, some of the terms are ambiguous and have been commonly used to group together deposits having distinctly different forms. The term peneconcordant U deposit clearly sets apart a widespread and important type of U deposit that has a common and distinctive form, namely, nearly concordant to the bedding of the host rock. The meaning of the term is self-evident, and the term is readily applicable to field usage.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.54.5.944","usgsCitation":"Finch, W., 1959, Peneconcordant uranium deposit: A proposed term: Economic Geology, v. 54, p. 944-946, https://doi.org/10.2113/gsecongeo.54.5.944.","productDescription":"3 p.","startPage":"944","endPage":"946","costCenters":[],"links":[{"id":370263,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","noUsgsAuthors":false,"publicationDate":"1959-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Finch, W.I.","contributorId":75919,"corporation":false,"usgs":true,"family":"Finch","given":"W.I.","email":"","affiliations":[],"preferred":false,"id":777473,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206770,"text":"70206770 - 1959 - Paleozoic and mesozoic fossils in a thick stratigraphic section in the eastern Sierra Nevada, California","interactions":[],"lastModifiedDate":"2019-11-21T13:15:24","indexId":"70206770","displayToPublicDate":"1959-11-21T13:15:01","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Paleozoic and mesozoic fossils in a thick stratigraphic section in the eastern Sierra Nevada, California","docAbstract":"<p>A thick section of metamorphosed Paleozoic and Mesozoic rocks is exposed in two roof pend- ants, one each in the Mount Morrison and Devils Postpile quadrangles in the eastern Sierra Nevada near Mammoth Lakes, Cali- fornia (Fig. 1). In the course of geologic mapping in these quadrangles by the U. S. Geo- logical Survey in co-operation with the California Division of Mines, fossils of Ordovician, Pennsylvanian, Permian(P), and Early Jurassic ages were collected from weakly metamorphosed parts of the pendants. Detailed map- ping in the Mount Morrison quadrangle has been completed by Rinehart and Ross, and a report on this area is in preparation. Similar mapping in the Devils Postpile quadrangle by Rinehart and Huber is in progress. In the part of the Devils Postpile quadrangle not yet covered in the present study, the contacts shown on the map (Fig. 1) are after Erwin (1934). Because diagnostic fossils are extremely rare in the metamorphic rocks of the Sierra Nevada, these fossils are considered important enough to merit this short note prior to completion of the detailed mapping in the Devils Postpile quadrangle and the publication of more comprehensive reports on the two quadrangles</p>","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1959)70[941:PAMFIA]2.0.CO;2","usgsCitation":"Huber, N., 1959, Paleozoic and mesozoic fossils in a thick stratigraphic section in the eastern Sierra Nevada, California: GSA Bulletin, v. 70, no. 7, p. 141-146, https://doi.org/10.1130/0016-7606(1959)70[941:PAMFIA]2.0.CO;2.","productDescription":"6 p.","startPage":"141","endPage":"146","onlineOnly":"Y","costCenters":[],"links":[{"id":369391,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Mammoth Lakes Region","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.15,\n              37.45\n            ],\n            [\n              -118.45,\n              37.45\n            ],\n            [\n              -118.45,\n              37.30\n            ],\n            [\n              -119.15,\n              37.30\n            ],\n            [\n              -119.15,\n              37.45\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"70","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Huber, N.K.","contributorId":73610,"corporation":false,"usgs":true,"family":"Huber","given":"N.K.","affiliations":[],"preferred":false,"id":775719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206769,"text":"70206769 - 1959 - Some aspects of the origin of the Ironwood iron-formation of Michigan and Wisconsin ","interactions":[],"lastModifiedDate":"2019-11-21T11:50:28","indexId":"70206769","displayToPublicDate":"1959-11-21T11:41:35","publicationYear":"1959","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Some aspects of the origin of the Ironwood iron-formation of Michigan and Wisconsin ","docAbstract":"<p><span>The Ironwood iron-formation of the Gogebic Range of Michigan and Wisconsin is made up of several rock types, each of which is characterized by a different iron-rich mineral: hematite, magnetite, pyrite, iron carbonate, or iron silicate (minnesotaite, stilpnomelane). Where the Ironwood iron-formation is relatively unaltered the Plymouth, Norrie, and Anvil members consist of wavy-bedded magnetite and silicate-rich rocks, whereas the Yale and Pence members consist of even-bedded carbonate, silicate, magnetite, and pyrite-rich rocks. These rock types represent primary facies of the iron-formation that were deposited under differing physical and chemical conditions during a period of continuous iron-rich sedimentation. Animikie sedimentation in the Gogebic district began with the deposition of sandstone and dolomitic limestone in a shallow sea advancing over a low-lying land mass of lower Precambrian granite and green-stone. Continued advance of the sea, with effective separation of clastic material near shore, permitted the dominantly chemical sedimentation of the iron- formation in somewhat deeper water. The development of an off-shore basin with partially restricted circulation would have facilitated such deposition. Minor fluctuations in the physical and chemical conditions within the depositional environment are reflected in the differing facies of the iron-formation. Deposition of the iron and silica-rich chemical sediments was terminated by increased tectonism and the deposition of the thick sequence of slates and graywackes of the Tyler formation.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.54.1.82","usgsCitation":"Huber, N., 1959, Some aspects of the origin of the Ironwood iron-formation of Michigan and Wisconsin : Economic Geology, v. 54, no. 1, p. 82-118, https://doi.org/10.2113/gsecongeo.54.1.82.","productDescription":"37 p.","startPage":"82","endPage":"118","costCenters":[],"links":[{"id":369389,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan, Wisconsin","otherGeospatial":"The Gogebic Range of Michigan and Wisconsin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.209228515625,\n              45.01918507438176\n            ],\n            [\n              -87.637939453125,\n              44.83249999349062\n            ],\n            [\n              -85.682373046875,\n              47.19717795172789\n            ],\n            [\n              -85.660400390625,\n              48.42191010942875\n            ],\n            [\n              -93.18603515624999,\n              48.334343174592014\n            ],\n            [\n              -93.42773437499999,\n              46.5286346952717\n            ],\n            [\n              -88.209228515625,\n              45.01918507438176\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"54","issue":"1","noUsgsAuthors":false,"publicationDate":"1959-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Huber, N.K.","contributorId":73610,"corporation":false,"usgs":true,"family":"Huber","given":"N.K.","affiliations":[],"preferred":false,"id":775718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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