No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1679","usgsCitation":"Patterson, J.L., 1966, Magnitude and frequency of floods in the United States: Part 6-A. Missouri River basin above Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1679, Report: xix, 471 p. 1 Plate: 36.00 × 23.22 inches, https://doi.org/10.3133/wsp1679.","productDescription":"Report: xix, 471 p. 1 Plate: 36.00 × 23.22 inches","costCenters":[],"links":[{"id":394847,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24888.htm"},{"id":28514,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1679/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28513,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1679/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138108,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1679/report-thumb.jpg"}],"country":"United States","state":"Minnesota, Montana, Nebraska, North Dakota, Iowa. South Dakota","otherGeospatial":"Missouri River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.667,\n 42\n ],\n [\n -95.333,\n 42\n ],\n [\n -95.333,\n 49.5\n ],\n [\n -113.667,\n 49.5\n ],\n [\n -113.667,\n 42\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495f9","contributors":{"authors":[{"text":"Patterson, James L.","contributorId":17593,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145214,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1813,"text":"wsp1819F - 1966 - Recharge studies on the High Plains in northern Lea County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1819F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1819","chapter":"F","title":"Recharge studies on the High Plains in northern Lea County, New Mexico","docAbstract":"The area described in this report is that part of the southern High Plains principally within northern Lea County, N. Mex. ; it comprises about 1,400,000 acres. Hydrologic boundaries isolate the main aquifer of the area, the Ogallala Formation, from outside sources of natural recharge other than precipitation on the area. Natural recharge to this aquifer from the 15-inch average annual precipitation for the period 1949-60 is estimated to be about 95,000 acre-ft (acre-feet) which is between the 59,000 and 118,000 acre-ft a year obtained from the This estimate (1934) of ? to 1 inch a year. About one-sixth of the water pumped for irrigation, or an average of about 23,000 acre-ft a year in the period \r\n1949-60, returns to the aquifer. The estimated long-term (1939-60) average \r\nannual recharge to the aquifer is about 77,000 acre-ft. \r\n\r\nDischarge from the aquifer is by pumping and underflow from the area. Gross pumpage averaged about 151,000 acre-ft a year in the period 1949-60. Underflow from the area is estimated to have been about 36,000 acre-ft a year. Thus, the estimated average annual discharge from the aquifer was about 187,000 acre-ft a year, and this exceeded recharge by about 69,000 acre-ft a year. This overdraft is reflected in a general net decline of the water table of 10 ft in the period 1950-60 and net declines of as much as 30 feet in local areas. \r\n\r\nData obtained during this study indicate that about 100,000 acre-ft of water collects in closed depressions on the surface of the High Plains in years when precipitation is normal. Studies of water losses from ponds in selected depressions indicate that between 20 and 80 percent of this loss recharges the groundwater body and the balance is lost to evapotranspiration, principally evaporation. Artificial recharge facilities constructed in the depressions could put at least 50,000 acre-ft of water underground annually that otherwise would be lost to evaporation. Recharging through pits or spreading ponds would cost less per unit volume of water than recharge through wells.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1819F","usgsCitation":"Havens, J., 1966, Recharge studies on the High Plains in northern Lea County, New Mexico: U.S. Geological Survey Water Supply Paper 1819, vii, 52 p. :ill., maps ;24 cm. + plates folded in pocket., https://doi.org/10.3133/wsp1819F.","productDescription":"vii, 52 p. :ill., maps ;24 cm. + plates folded in pocket.","costCenters":[],"links":[{"id":137175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819f/report-thumb.jpg"},{"id":27004,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27005,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27006,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27007,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819f/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27008,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629844","contributors":{"authors":[{"text":"Havens, John S.","contributorId":13949,"corporation":false,"usgs":true,"family":"Havens","given":"John S.","affiliations":[],"preferred":false,"id":144198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57737,"text":"ofr66159 - 1966 - Ground water in the Cimarron River basin: New Mexico, Colorado, Kansas, and Oklahoma","interactions":[],"lastModifiedDate":"2022-10-05T21:23:01.391973","indexId":"ofr66159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-159","title":"Ground water in the Cimarron River basin: New Mexico, Colorado, Kansas, and Oklahoma","docAbstract":"This report on ground water in the Cimarron River basin was prepared by the Water Resources Division of the U.S. Geological Survey at the request of the U.S. Corps of Engineers, Tulsa District, for inclusion in the Corps' overall report on the water resources of the basin. The report is an updating of the Cimarron Basin part of the report on the Arkansas, White, and Red River basins (Lohman and Burtis, 1953a) and includes more recently published data, as well as unpublished data in the files of the Geological Survey. These data are compiled by district offices of the Geological Survey in each State in cooperation with State and local agencies and with other Federal agencies. No new data were collected as a part of this investigation. The report is primarily a map presentation, and the text is intended mainly to clarify and supplement the maps and to make them more understandable and usable. The report also presents some of the ground-water problems--both present and potential--and suggests some partial solutions. As the maps and text are of necessity highly generalized, the reader is referred to the more detailed reports for more precise information.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr66159","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Ground water in the Cimarron River basin: New Mexico, Colorado, Kansas, and Oklahoma: U.S. Geological Survey Open-File Report 66-159, Report: iii, 51 p.; 5 Plates: 35.62 × 21.82 inches or smaller, https://doi.org/10.3133/ofr66159.","productDescription":"Report: iii, 51 p.; 5 Plates: 35.62 × 21.82 inches or smaller","costCenters":[],"links":[{"id":185413,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0159/report-thumb.jpg"},{"id":100617,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0159/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":100616,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0159/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":100615,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0159/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":100614,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0159/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":100613,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0159/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":100612,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0159/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":408005,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52093.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Colorado, Kansas, New Mexico, Oklahoma","otherGeospatial":"Cimarron River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.1333,\n 35.55\n ],\n [\n -96.2833,\n 35.55\n ],\n [\n -96.2833,\n 37.8792\n ],\n [\n -104.1333,\n 37.8792\n ],\n [\n -104.1333,\n 35.55\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d797","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":533180,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1892,"text":"wsp1696D - 1966 - Quantitative determination of tritium in natural waters","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1696D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1696","chapter":"D","title":"Quantitative determination of tritium in natural waters","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1696D","usgsCitation":"Hoffman, C., and Stewart, G., 1966, Quantitative determination of tritium in natural waters: U.S. Geological Survey Water Supply Paper 1696, iii, 18 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1696D.","productDescription":"iii, 18 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":138402,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1696d/report-thumb.jpg"},{"id":27181,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1696d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ee3","contributors":{"authors":[{"text":"Hoffman, C.M.","contributorId":77128,"corporation":false,"usgs":true,"family":"Hoffman","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":144322,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stewart, G.L.","contributorId":31374,"corporation":false,"usgs":true,"family":"Stewart","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":144321,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":185,"text":"wsp1645 - 1966 - Quality of surface waters of the United States, 1959, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1645","title":"Quality of surface waters of the United States, 1959, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1645","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Quality of surface waters of the United States, 1959, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1645, xv, 524 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1645.","productDescription":"xv, 524 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1645/report-thumb.jpg"},{"id":24796,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1645/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651aeb","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":527220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":191,"text":"wsp1950 - 1966 - Quality of surface waters of the United States, 1963, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1950","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1950","title":"Quality of surface waters of the United States, 1963, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1950","usgsCitation":"Love, S.K., 1966, Quality of surface waters of the United States, 1963, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1950, xii, 635 p. ;23 cm., https://doi.org/10.3133/wsp1950.","productDescription":"xii, 635 p. ;23 cm.","costCenters":[],"links":[{"id":136096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1950/report-thumb.jpg"},{"id":24802,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1950/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651a8a","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5711,"text":"pp498A - 1966 - Hydrochemical facies and ground-water flow patterns in northern part of Atlantic Coastal Plain","interactions":[],"lastModifiedDate":"2017-06-05T21:55:49","indexId":"pp498A","displayToPublicDate":"1991-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"498","chapter":"A","title":"Hydrochemical facies and ground-water flow patterns in northern part of Atlantic Coastal Plain","docAbstract":"The part of the Atlantic Coastal Plain that extends from New Jersey through Virginia was selected as a suitable field model in which to study the relationships between geology, hydrology, and chemical character of ground water. The ground-water flow pattern is the principal hydrologic control on the chemical character of the water. Within the Coastal Plain sediments, the proportions of clay, glauconitic sand, and calcareous material are the principal lithologic controls over the chemistry of the water.
\nA subsurface body of salt water extends from southern New Jersey through southern Virginia and occupies the deposits deeper than about 500 feet below land surface in the eastern part of the Coastal Plain. The position of its top is determined by the relative head, which in turn is influenced by topography, drainage density, and the thickness and permeability of the Coastal Plain sediments.
\nHydrochemical facies is a term used in this paper to denote the diagnostic chemical aspect of ground-water solutions occurring in hydrologic systems. The facies reflect the response of chemical processes operating within the lithologic framework and also the pattern of flow of the water. The distribution of these facies is shown in trilinear diagrams and isometric fence diagrams and on maps showing isopleths of chemical constituents within certain formations. The occurrence of the various facies within one formation or within a group of formations of uniform mineralogy indicates that the ground-water flow through the aquifer system modifies the distribution of the facies.
\nFlow patterns of fresh ground water shown on maps and in cross sections have been deduced from available water-level data. These patterns are controlled by the distribution of the higher landmasses and by the depth to either bedrock or to the salt-water interface. The mapping of hydrochemical facies shows that at shallow depths within the Coastal Plain (less than about 200 ft) the calcium-magnesium cation facies generally predominates. The bicarbonate anion facies occurs within more of the shallow Coastal Plain sediments than does the sulfate or the chloride facies. In deeper formations, the sodium chloride character predominates. The lower dissolved-solids content of the ground water in New Jersey indicates less upward vertical leakage than in Maryland and Virginia, where the shallow formations contain solutions of higher concentration.
","largerWorkTitle":"Hydrology of aquifer systems","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp498A","usgsCitation":"Back, W., 1966, Hydrochemical facies and ground-water flow patterns in northern part of Atlantic Coastal Plain: U.S. Geological Survey Professional Paper 498, Report: iv, 42 p.; 1 Plate: 54.00 x 41.50 inches, https://doi.org/10.3133/pp498A.","productDescription":"Report: iv, 42 p.; 1 Plate: 54.00 x 41.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":32282,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0498a/plate-1.pdf","text":"Plate 1","size":"7.25 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":118160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0498a/report-thumb.jpg"},{"id":104479,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4513.htm","linkFileType":{"id":5,"text":"html"},"description":"4513"},{"id":32283,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0498a/report.pdf","text":"Report","size":"5.06 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Delaware, Maryland, New Jersey, Pennsylvania, Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.03662109375,\n 41.50857729743935\n ],\n [\n -73.80615234375,\n 40.94671366508002\n ],\n [\n -73.89404296875,\n 40.41349604970198\n ],\n [\n -74.1357421875,\n 39.487084981687495\n ],\n [\n -74.6630859375,\n 38.8225909761771\n ],\n [\n -75.234375,\n 37.70120736474139\n ],\n [\n -75.6298828125,\n 37.00255267215955\n ],\n [\n -75.69580078125,\n 36.527294814546245\n ],\n [\n -80.33203125,\n 36.63316209558658\n ],\n [\n -79.16748046874999,\n 37.56199695314352\n ],\n [\n -78.046875,\n 38.75408327579141\n ],\n [\n -77.62939453125,\n 39.52099229357195\n ],\n [\n -77.05810546875,\n 40.094882122321174\n ],\n [\n -76.31103515625,\n 40.697299008636755\n ],\n [\n -75.6298828125,\n 41.36031866306708\n ],\n [\n -75.03662109375,\n 41.50857729743935\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628ed5","contributors":{"authors":[{"text":"Back, William","contributorId":59007,"corporation":false,"usgs":true,"family":"Back","given":"William","email":"","affiliations":[],"preferred":false,"id":151470,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70112260,"text":"70112260 - 1966 - Water resources in the Everglades","interactions":[],"lastModifiedDate":"2017-03-27T13:43:28","indexId":"70112260","displayToPublicDate":"1990-06-12T10:29:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3052,"text":"Photogrammetric Engineering and Remote Sensing","active":true,"publicationSubtype":{"id":10}},"title":"Water resources in the Everglades","docAbstract":"Aerial photography is playing an important role in the evaluation of the water resources of the almost-inaccessible 1,400 square miles of Everglades in southern Florida. Color, infrared, and panchromatic photographs show salient features that permit evaluation of the overall water resources picture. The fresh water-salt water interface, drainage patterns, ecologic changes resulting from flood and drought, quantities of flow, and other hydrologic features are easily observed or measured from the photographs. Such data permit areal extension of very limited point observations of water resources data, and will assist in providing the necessary guidelines for decisions in water management in the Everglades.
","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Schneider, W.J., 1966, Water resources in the Everglades: Photogrammetric Engineering and Remote Sensing, v. 32, no. 6, p. 958-965.","productDescription":"8 p.","startPage":"958","endPage":"965","numberOfPages":"8","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288452,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.5212,24.85 ], [ -81.5212,25.8918 ], [ -80.3887,25.8918 ], [ -80.3887,24.85 ], [ -81.5212,24.85 ] ] ] } } ] }","volume":"32","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc61e4b0e83db6d0907f","contributors":{"authors":[{"text":"Schneider, William J.","contributorId":47349,"corporation":false,"usgs":true,"family":"Schneider","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":494588,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70112258,"text":"70112258 - 1966 - Water and the Everglades","interactions":[],"lastModifiedDate":"2017-03-27T13:46:14","indexId":"70112258","displayToPublicDate":"1990-06-12T10:17:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2825,"text":"Natural History","active":true,"publicationSubtype":{"id":10}},"title":"Water and the Everglades","docAbstract":"This fundamental element, whether profuse or scarce, rules the life and character of Florida's great park. But water, like living space, is a resource that civilization demands in ever increasing quantities. Examined here are the economics of water use by Florida's east coast cities and its effects on Everglades ecology.
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Dakota\",\"nation\":\"USA \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5620ce6ae4b06217fc478add","contributors":{"authors":[{"text":"Crosby, Orlo A.","contributorId":6065,"corporation":false,"usgs":true,"family":"Crosby","given":"Orlo A.","affiliations":[],"preferred":false,"id":577601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70173975,"text":"70173975 - 1966 - Selected flow characteristics of streams in the Willamette River Basin, Oregon","interactions":[],"lastModifiedDate":"2016-06-21T14:07:14","indexId":"70173975","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Selected flow characteristics of streams in the Willamette River Basin, Oregon","docAbstract":"Flow-duration, annual low-flow, and annual high-flow tables through September 30, 1963, are given in this report for 110 stream-gaging stations in the Willamette and Sandy River basins. These tables summarize the basic data needed to define the streamflow characteristics at the gaging stations. The content of each of the three summary tables is described, and techniques for preparing flow-duration curves, low-flow frequency curves, and high-flow frequency curves are explained.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/70173975","usgsCitation":"Swift, C.H., 1966, Selected flow characteristics of streams in the Willamette River Basin, Oregon: Open-File Report, 177 p., https://doi.org/10.3133/70173975.","productDescription":"177 p.","numberOfPages":"181","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":324025,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70173975.jpg"},{"id":324138,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70173975/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon","otherGeospatial":"Willamette River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -123.585205078125,\n 43.30919109985686\n ],\n [\n -123.585205078125,\n 45.775186183521036\n ],\n [\n -121.40991210937499,\n 45.775186183521036\n ],\n [\n -121.40991210937499,\n 43.30919109985686\n ],\n [\n -123.585205078125,\n 43.30919109985686\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913e7e4b07657d19ff265","contributors":{"authors":[{"text":"Swift, C. H. III","contributorId":43624,"corporation":false,"usgs":true,"family":"Swift","given":"C.","suffix":"III","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":639897,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70210055,"text":"70210055 - 1966 - Insecticide contaminations in wetland habitats and their effects on fish- eating birds","interactions":[],"lastModifiedDate":"2020-05-12T17:56:10.93947","indexId":"70210055","displayToPublicDate":"1966-12-31T12:48:33","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2163,"text":"Journal of Applied Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Insecticide contaminations in wetland habitats and their effects on fish- eating birds","docAbstract":"An unusual mortality of fish-eating birds occurred at the Tule Lake National Wildlife Refuge in California between 1960 and 1962. Over 1100 dead birds of ten species were found during that period. Investigations of the mortality indicated that birds died as a result of their exposure to toxaphene, which was applied to adjoining agricultural areas, transported to the refuge in waste irrigation water, and accumulated in fish eaten by the birds. Toxaphene was used in agriculture for only 3 years, 1958-60, and by 1962 residues were no longer found in the marsh habitat. However, results also showed that a potentially hazardous contamination of DDT and its metabolites was present in the birds and the environment. Studies were, therefore, continued to determine the food-chain relationships of DDT in marsh ecosystems, and the effects of the insecticide on birds. Sampling for insecticide residues was undertaken at four waterfowl refuges, each representing a somewhat different set of environmental conditions. DDT residues in water at each refuge were found to be relatively low, but filtered samples showed that residues in suspended material were 10 000 to 20 000 times as great as those in the filtrate. Much of the suspended material was organic matter, which is an important source of energy for the ecosystems. In environments with invertebrates, DDT residues were relatively low in sediments and high in fish, while residues in vegetation were highest where invertebrates were absent. Results suggest that organic materials and invertebrates can be important factors in determining the fate and involvement of insecticides in aquatic environments. Studies of the movements, exposure to pesticides, productivity, and longevity of individuals in three nesting colonies of White Pelicans were begun in 1962 to depict the relationships of pesticides to a migratory population of birds dependent upon wetland habitats. To date there is no evidence that the exposure of pelicans to DDT is influencing the population dynamics of the birds.
","language":"English","publisher":"Blackwell Scientific ","doi":"10.2307/2401446","usgsCitation":"Keith, J.O., 1966, Insecticide contaminations in wetland habitats and their effects on fish- eating birds: Journal of Applied Ecology, v. 3, no. Suppl, p. 71-85, https://doi.org/10.2307/2401446.","productDescription":"15 p.","startPage":"71","endPage":"85","costCenters":[],"links":[{"id":374701,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California, Oregon","otherGeospatial":"Tule Lake Basin, Upper Klamath National Wildlife Refuge ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.58843994140625,\n 41.81431422987254\n ],\n [\n -121.37832641601561,\n 41.81431422987254\n ],\n [\n -121.37832641601561,\n 41.98246303636425\n ],\n [\n -121.58843994140625,\n 41.98246303636425\n ],\n [\n -121.58843994140625,\n 41.81431422987254\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.10205078125,\n 42.407234661551875\n ],\n [\n -121.8878173828125,\n 42.407234661551875\n ],\n [\n -121.8878173828125,\n 42.77423534479349\n ],\n [\n -122.10205078125,\n 42.77423534479349\n ],\n [\n -122.10205078125,\n 42.407234661551875\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"3","issue":"Suppl","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Keith, James O.","contributorId":76039,"corporation":false,"usgs":true,"family":"Keith","given":"James","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":788938,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70206947,"text":"70206947 - 1966 - Hydration of natural glass and formation of perlite","interactions":[],"lastModifiedDate":"2019-12-02T07:01:07","indexId":"70206947","displayToPublicDate":"1966-12-31T09:13:43","publicationYear":"1966","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":" Hydration of natural glass and formation of perlite","docAbstract":"The hydration rate of rhyolitic glass has been determined at temperatures ranging from 5° C to 100° C. The relationship between the depth of hydration, x, and time, t is x2 = kt; k varies from 0.4 μ2/103 years at 5° C to 104 μ2/103 years at 100° C; k is independent of the water pressure from a few hundredths of a centimeter to 1 atm. water pressure. The activation energy of hydration is about 20 kcal/mole. The determined hydration rates are consistent with the observation that perlite commonly forms by the hydration of shattered rhyolitic glass, either during the late cooling of a deposit or after the deposit has cooled to a surficial temperature.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1966)77[323:HONGAF]2.0.CO;2","issn":"00167606","usgsCitation":"Friedman, I., Smith, R., and Long, W., 1966, Hydration of natural glass and formation of perlite: Geological Society of America Bulletin, v. 77, no. 3, p. 323-328, https://doi.org/10.1130/0016-7606(1966)77[323:HONGAF]2.0.CO;2.","productDescription":"6 p. ","startPage":"323","endPage":"328","costCenters":[],"links":[{"id":369776,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"77","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Friedman, I.","contributorId":95596,"corporation":false,"usgs":true,"family":"Friedman","given":"I.","email":"","affiliations":[],"preferred":false,"id":776351,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, R.L.","contributorId":47422,"corporation":false,"usgs":true,"family":"Smith","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":776352,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Long, W.D.","contributorId":82845,"corporation":false,"usgs":true,"family":"Long","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":776353,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70219934,"text":"70219934 - 1966 - Tropical lakes, copropel, and oil shale","interactions":[],"lastModifiedDate":"2021-04-16T12:23:10.823743","indexId":"70219934","displayToPublicDate":"1966-12-31T07:19:20","publicationYear":"1966","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":"Tropical lakes, copropel, and oil shale","docAbstract":"During a long-continued study of the lacustrine beds of the Eocene Green River Formation, I have tried to interpret past events from observation of present-day processes. After a search of some 40 years, four lakes have been found that are producing a kind of organic ooze judged to be a modern analogue of the precursors of rich oil shale. Two of the lakes are in central Africa and two are in Florida. All four are shallow. The ooze in all four is predominantly algal, entirely in the form of minute fecal pellets, and does not decay in warm, wet, oxidizing environments.
Several of the most unusual, mummified microorganisms found in the oil shale of the Green River are illustrated as testament to the inference that the Eocene organic oozes also were resistant to decay.
Studies to determine why these algal oozes do not decay are in progress, but as yet no satisfactory explanation is available. The ooze from Mud Lake, Florida, contains very few living bacteria but a great many bacterial spores, suggesting some active inhibitor. Gentle and slow anaerobic decay takes place in the ooze 1 foot or more below the mud-water interface.
The algal ooze accumulates slowly. That at a depth of 3 feet below the mud-water interface has a C14 age of 2280 ± 200 years. If compacted, this 3-foot layer would amount to a layer only about 0.5 inch thick.
The air-dried algal mud (from Mud Lake) looks much like oil shale and has a C-H ratio essentially like that of the organic matter in oil shale. The oxygen of the mud, however, is roughly 5 times as high as in oil shale. The calorific value of dried Mud Lake algal ooze is about 6600 cal/g, whereas the organic matter from Green River oil shale averages about 9500 cal/g.
Analyses show that the dried algal ooze from Mud Lake contains small quantities of higher fatty acids (C12–C34), with C16 being dominant. It also contains some unsaturated fatty acids and about 0.3 per cent of n-alkanes, predominantly odd carbons, with C29 being dominant. A few qualitative analyses show that carotenoid pigments and terpenes are also present.
A possible source of hydrocarbons is the long branched side chain of the chlorophyll molecule. Small crustaceans liberate this in the form of phytol, which, by dehydration, can go over into a series of saturated and unsaturated hydrocarbons, including phytanc and pristane, both of which are common in Green River oil shale. Search for other precursors of hydrocarbons continues.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1966)77[1333:TLCAOS]2.0.CO;2","usgsCitation":"Bradley, W., 1966, Tropical lakes, copropel, and oil shale: GSA Bulletin, v. 77, no. 12, p. 1333-1337, https://doi.org/10.1130/0016-7606(1966)77[1333:TLCAOS]2.0.CO;2.","productDescription":"5 p.","startPage":"1333","endPage":"1337","costCenters":[],"links":[{"id":385151,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"77","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bradley, W.H.","contributorId":220222,"corporation":false,"usgs":false,"family":"Bradley","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":814404,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5210183,"text":"5210183 - 1966 - Pesticide residues in the ecosystem","interactions":[],"lastModifiedDate":"2023-05-19T16:19:07.242799","indexId":"5210183","displayToPublicDate":"1966-12-31T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"8","title":"Pesticide residues in the ecosystem","docAbstract":"Pesticide residues have become a component of nearly all living organisms. Nearly all California birds and fish collected in a 1963 pesticide survey contained residues. Discovery of DDT and metabolites in Antarctic animals in 1964 pushed the distribution of pesticides to the remotest portions of the globe. Exchange of pesticides in the aquatic world progresses rapidly, even in the quiet waters of a pond. Any segment of the ecosystem–marshland, pond, forest, or field–receives pesticides of varied amounts and kinds at irregular and unknown intervals. Phytoplankton communities are an important food base in aquatic environments whose productivity can be affected by rather small exposure to pesticides. Degradation and loss of chlorinated hydrocarbon pesticides from the ecosystem has been shown to proceed slowly. Pesticide-tolerant or resistant populations of fish and possibly other cold-blooded vertebrates have been shown to exist in areas of the south long subjected to pesticide treatments.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Pesticides and their effects on soils and water","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"American Society of Agronomy and Soil Science Society of America, Inc","publisherLocation":"Madison, Wisconsin","doi":"10.2134/asaspecpub8.c11","usgsCitation":"Dustman, E.H., and Stickel, L.F., 1966, Pesticide residues in the ecosystem, chap. of Pesticides and their effects on soils and water, p. 109-121, https://doi.org/10.2134/asaspecpub8.c11.","productDescription":"13 p.","startPage":"109","endPage":"121","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200435,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2015-10-26","publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688356","contributors":{"editors":[{"text":"Breth, S.","contributorId":113091,"corporation":false,"usgs":true,"family":"Breth","given":"S.","email":"","affiliations":[],"preferred":false,"id":506098,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Dustman, E. H.","contributorId":12579,"corporation":false,"usgs":true,"family":"Dustman","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":327926,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stickel, Lucille F.","contributorId":76598,"corporation":false,"usgs":true,"family":"Stickel","given":"Lucille","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":327927,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221256,"text":"70221256 - 1966 - Development of permeability and storage in the tertiary limestones of the southeastern states, USA","interactions":[],"lastModifiedDate":"2021-06-09T14:23:08.197702","indexId":"70221256","displayToPublicDate":"1966-12-01T12:33:20","publicationYear":"1966","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":"Development of permeability and storage in the tertiary limestones of the southeastern states, USA","docAbstract":"Permeability and storage characteristics in the Tertiary limestone system of southern United States have developed progressively but non-uniformly as circulation of water and solution in the limestone have changed during the geologic and hydrologic history.
The limestone formations, predominantly of Eocene age and subordinated of Oligocene and Miocene age, are widespread at and beneath the surface. They commonly dip gently seaward and are covered in coastal areas by Miocene to Recent clays and sands. Sinkholes and other karst features are common, but topographic relief is generally not great.
Circulation of water under water-table conditions when the limestone was exposed to meteoric weathering, before middle Miocene time, resulted in development of secondary permeability as solution channels in near-surface parts of the limestone, Marine deposition of middle and late Miocene clays and later emergence converted part of the water-table circulation system to the present great artesian system. Later, Pleistocene changes in sea level caused changed in places where water discharged, which in turn caused changes in rates of circulation and changes in rates and positions of solution of limestone. Both present and past circulation of water have contributed to changes in permeability and storage of this limestone system.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666609493494","usgsCitation":"LeGrand, H.E., and Stringfield, V.T., 1966, Development of permeability and storage in the tertiary limestones of the southeastern states, USA: International Association of Scientific Hydrology - Bulletin , v. 11, no. 4, p. 61-73, https://doi.org/10.1080/02626666609493494.","productDescription":"13 p.","startPage":"61","endPage":"73","costCenters":[],"links":[{"id":480349,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666609493494","text":"Publisher Index Page"},{"id":386302,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Southeastern United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.1748046875,\n 25.085598897064752\n ],\n [\n -73.2568359375,\n 25.085598897064752\n ],\n [\n -73.2568359375,\n 36.42128244364947\n ],\n [\n -83.75976562499999,\n 36.421282443649496\n ],\n [\n -94.1748046875,\n 36.42128244364947\n ],\n [\n -94.1748046875,\n 25.085598897064752\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"11","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"LeGrand, H. E.","contributorId":54571,"corporation":false,"usgs":true,"family":"LeGrand","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":817175,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stringfield, V. T.","contributorId":72369,"corporation":false,"usgs":true,"family":"Stringfield","given":"V.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":817176,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010674,"text":"70010674 - 1966 - Deep layer of sediments in Alpine Lake in the tropical mid-Pacific","interactions":[],"lastModifiedDate":"2026-02-09T23:05:38.550285","indexId":"70010674","displayToPublicDate":"1966-11-04T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Deep layer of sediments in Alpine Lake in the tropical mid-Pacific","docAbstract":"Sediments from a unique high-altitude lake on Hawaii indicate ash falls and other airborne and waterborne materials for a period estimated to extend into the Pleistocene.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.154.3749.647","issn":"00368075","usgsCitation":"Woodcock, A., Rubin, M., and Duce, R., 1966, Deep layer of sediments in Alpine Lake in the tropical mid-Pacific: Science, v. 154, no. 3749, p. 647-648, https://doi.org/10.1126/science.154.3749.647.","productDescription":"2 p.","startPage":"647","endPage":"648","costCenters":[],"links":[{"id":219400,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Alpine Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -155.6312883187875,\n 19.94113454424118\n ],\n [\n -155.6312883187875,\n 19.766294755854474\n ],\n [\n -155.359556527811,\n 19.766294755854474\n ],\n [\n -155.359556527811,\n 19.94113454424118\n ],\n [\n -155.6312883187875,\n 19.94113454424118\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"154","issue":"3749","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fe25e4b0c8380cd4eb46","contributors":{"authors":[{"text":"Woodcock, A.H.","contributorId":39515,"corporation":false,"usgs":true,"family":"Woodcock","given":"A.H.","email":"","affiliations":[],"preferred":false,"id":359402,"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":359403,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Duce, R.A.","contributorId":91236,"corporation":false,"usgs":true,"family":"Duce","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":359404,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221251,"text":"70221251 - 1966 - Use of analog model to predict streamflow depletion, big and little Blue River basin, Nebraska","interactions":[],"lastModifiedDate":"2021-06-08T16:50:02.742396","indexId":"70221251","displayToPublicDate":"1966-10-01T11:44:40","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Use of analog model to predict streamflow depletion, big and little Blue River basin, Nebraska","docAbstract":"The States of Nebraska and Kansas are negotiating a compact for apportionment of the waters of the Big and Little Blue Rivers. So that the negotiating officials could allocate the water equitably, the amount of streamflow depletion caused by ground‐water withdrawals upgradient from the State line needed to be determined. At the request of the Nebraska officials, the U. S. Geological Survey constructed an electric analog model which could be used to determine the amount of streamflow depletion expected to occur in the next 60 years. The model simulates hydraulic conditions in an area of 7,400 square miles which includes the entire area drained by the Big and Little Blue Rivers in Nebraska. The trans‐missibility of the aquifer (Pleistocene in age) ranges from less than 1,000 to as much as 300,000 gallons per day per foot, and the storage coefficient averages about 0.20. The transmissibility values are based on examination of test‐ hole samples from more than 400 test holes in and adjacent to the basin. Analysis of the model indicates that predicted maximum ground‐water withdrawals between 1962 and 2022 will not deplete the base flow of the Big or Little Blue Rivers by more than 5 percent.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1966.tb01610.x","usgsCitation":"Emery, P.A., 1966, Use of analog model to predict streamflow depletion, big and little Blue River basin, Nebraska: Groundwater, v. 4, no. 4, p. 13-19, https://doi.org/10.1111/j.1745-6584.1966.tb01610.x.","productDescription":"7 p.","startPage":"13","endPage":"19","costCenters":[],"links":[{"id":386298,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nebraska","otherGeospatial":"Blue River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -99.66796875,\n 39.9434364619742\n ],\n [\n -95.4052734375,\n 39.9434364619742\n ],\n [\n -95.4052734375,\n 41.705728515237524\n ],\n [\n -99.66796875,\n 41.705728515237524\n ],\n [\n -99.66796875,\n 39.9434364619742\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"4","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Emery, P. A.","contributorId":49392,"corporation":false,"usgs":true,"family":"Emery","given":"P.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":817170,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221250,"text":"70221250 - 1966 - Ground-water levels and trends May-July 1966 (Abstracted from U. S. Geological Survey “Water Resources Review”)","interactions":[],"lastModifiedDate":"2021-06-09T14:47:10.026473","indexId":"70221250","displayToPublicDate":"1966-10-01T11:39:37","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Ground-water levels and trends May-July 1966 (Abstracted from U. S. Geological Survey “Water Resources Review”)","docAbstract":"No abstract available.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1966.tb01616.x","usgsCitation":"Payne, F.N., 1966, Ground-water levels and trends May-July 1966 (Abstracted from U. S. Geological Survey “Water Resources Review”): Groundwater, v. 4, no. 4, p. 55-55, https://doi.org/10.1111/j.1745-6584.1966.tb01616.x.","productDescription":"1 p.","startPage":"55","endPage":"55","costCenters":[],"links":[{"id":386297,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Payne, Faith N.","contributorId":104875,"corporation":false,"usgs":true,"family":"Payne","given":"Faith","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":817169,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221249,"text":"70221249 - 1966 - Frequency distribution of dissolved solids in ground water","interactions":[],"lastModifiedDate":"2021-06-08T15:36:41.288843","indexId":"70221249","displayToPublicDate":"1966-10-01T10:31:06","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Frequency distribution of dissolved solids in ground water","docAbstract":"The frequency distribution of dissolved‐solids content of ground waters in geologically and climatologically homogeneous terrane units commonly approximates a log‐normal distribution. A graphic logarithmic transformation is de‐scribed which permits rapid calculation of approximate values for the mean, standard deviation, and coefficient of variation. Statistical parameters calculated by this method show good agreement with known physical conditions in the terranes studied and are precise enough for use as a mea‐sure of variability of quality of ground waters for national planning purposes.
","language":"English","publisher":"NGWA The Groundwater Association","doi":"10.1111/j.1745-6584.1966.tb01609.x","usgsCitation":"Davis, G., 1966, Frequency distribution of dissolved solids in ground water: Groundwater, v. 4, no. 4, p. 5-12, https://doi.org/10.1111/j.1745-6584.1966.tb01609.x.","productDescription":"8 p.","startPage":"5","endPage":"12","costCenters":[],"links":[{"id":386296,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Davis, G.H.","contributorId":258184,"corporation":false,"usgs":false,"family":"Davis","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":817168,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}