Gloucester County is in the southwestern part of New Jersey, below Camden, and is a part of the Lower Delaware River Valley. This area is attracting new industry and has shown a population increase of about 47 percent from 1950 to 1960, mostly urban. With the economic growth of the county, the availability and quality of water become increasingly important.
The county is in the Coastal Plain of New Jersey. It is underlain by unconsolidated sands and clays of Quaternary, Tertiary, and Cretaceous age. The Raritan and Magothy Formations constitute the most important aquifers and yield more than 95 percent of the water pumped by the public water systems in the county. These formations are capable of yielding 1,400 gpm (gallons per minute) or more to large diameter wells. High yielding wells generally can be drilled anywhere in the county, although the formations are deeper toward the Atlantic Ocean. The Cohansey Sand, second most important aquifer, yields up to 800 gpm or more from large diameter wells. This aquifer is present only in the sparsely populated southeastern half of the county. The Wenonah Formation and Mount Laurel Sand are capable of yielding 100 to 200 gpm in certain areas.
The overall chemical quality of the naturally occurring ground water is good. The water generally meets the U.S. Public Health Service's (1962) suggested limit for dissolved solids; however, in some areas, the water carries objectionable amounts of iron and nitrate in solution and has a low pH. Contamination of ground water by salt-water encroachment or by pollution from industrial activity or organic waste in densely populated areas should be prevented. The quality rather than the quantity of water may be the important factor in future ground-water developments.
The 21 public water systems in Gloucester County pumped about 1.3 billion gallons of water during 1948 and some 2.7 billion gallons during 1959. This is slightly more than a hundred percent increase in pumpage in 12 year s. The average per capita public water supply consumption in 1959 was approximately 75 gallons per day.
This report includes a summary of the history of the present installations, groundwater conditions, quality and availability of water, and potential future yield for the 2 public water systems in Gloucester County.
","language":"English","publisher":"State of New Jersey Department of Conservation and Economic Development, Division of Water Policy and Supply","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the State of New Jersey","usgsCitation":"Hardt, W.F., 1963, Public water supplies in Gloucester County, New Jersey: New Jersey Division of Water Policy and Supply Water Resources Circular 9, vii, 55 p.","productDescription":"vii, 55 p.","numberOfPages":"64","costCenters":[],"links":[{"id":284195,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":286049,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70095403/report.pdf"}],"country":"United States","state":"New Jersey","county":"Gloucester County","otherGeospatial":"Lower Delaware River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.42875,39.514802 ], [ -75.42875,39.888317 ], [ 74.877189,39.888317 ], [ 74.877189,39.514802 ], [ -75.42875,39.514802 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355952ee4b0120853e8c16f","contributors":{"authors":[{"text":"Hardt, William F.","contributorId":70013,"corporation":false,"usgs":true,"family":"Hardt","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":491187,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221092,"text":"70221092 - 1963 - Some aspects of sampling salty ground water in coastal aquifers","interactions":[],"lastModifiedDate":"2021-06-01T19:38:26.940939","indexId":"70221092","displayToPublicDate":"1963-01-01T14:34:40","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Some aspects of sampling salty ground water in coastal aquifers","docAbstract":"Investigations of the fluctuations of chloride content in wells that tap the zone of diffusion between fresh and salt water show that the salty well water behaves erratically when the well is pumped. Frequently, a static distribution of chloride content that ranges from less than 1,000 ppm at the top to more than 10,000 ppm at the bottom is present in the open‐hole part of a well. When the well is pumped, the discharge water tends to come from the upper part of the open hole because less energy is expended by removal of low‐density water from this region than by removal of high‐density water from the lower part of the open hole. Where the permeability of strata in the deep part of the open hole is greater than that in the shallow part, the tendency for natural selection of the less dense, shallow water is suppressed, and practically all the water in the blend comes from the deep part. As a result of this complex interrelation of hydraulics, distribution and density of the salt water, and permeability, the depth at which the pumped water enters the well bore is indeterminate. This deficiency leads to the use of multiple‐depth‐bottle, windshield‐wiper, and electrical‐conductivity sampling techniques for collection of data used in constructing maps and cross sections that show the areal‐depth relations of salt water in the Biscayne aquifer of the Miami area, Florida.
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1963.tb01903.x","usgsCitation":"Kohout, F., and Hoy, N., 1963, Some aspects of sampling salty ground water in coastal aquifers: Groundwater, v. 1, no. 1, p. 28-43, https://doi.org/10.1111/j.1745-6584.1963.tb01903.x.","productDescription":"16 p.","startPage":"28","endPage":"43","costCenters":[],"links":[{"id":386072,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Kohout, F. A.","contributorId":103979,"corporation":false,"usgs":true,"family":"Kohout","given":"F. A.","affiliations":[],"preferred":false,"id":816732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoy, N.D.","contributorId":15618,"corporation":false,"usgs":true,"family":"Hoy","given":"N.D.","email":"","affiliations":[],"preferred":false,"id":816733,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221066,"text":"70221066 - 1963 - The atomic ratios of natural ferruginous biotites with reference to 'the stability relations of the ferruginous biotite, annite'","interactions":[],"lastModifiedDate":"2021-06-01T16:49:03.824921","indexId":"70221066","displayToPublicDate":"1963-01-01T11:45:56","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"The atomic ratios of natural ferruginous biotites with reference to 'the stability relations of the ferruginous biotite, annite'","docAbstract":"The atomic ratios given by Eugster and Wones (1962) for analyses of high FeO-low MgO micas cited by Foster (1960) are in error. The recalculated atomic ratios herein presented show that only three of the thirteen have low (OH+F), and only one has characteristics that may possibly be due to loss of water during determination. None of the analyses exhibit characteristics suggestive of oxidation of iron and loss of H, as in progression towards oxyannite.
The average recalculated octahedral occupancy is 2.69, not 2.91 as in the previous calculation.
The differences between atomic ratios calculated on the basis ot determined H2O+ and F and those calculated on the basis of the theoretical O10 (OH)2 content are not great enough to change the essential compositional character of these micas as interpreted by Foster (1960). However, they do affect significantly the calculated octahedral occupancy.
","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/4.2.302","usgsCitation":"Foster, M.D., Wones, D.R., and Eugster, H., 1963, The atomic ratios of natural ferruginous biotites with reference to 'the stability relations of the ferruginous biotite, annite': Journal of Petrology, v. 4, no. 2, p. 302-306, https://doi.org/10.1093/petrology/4.2.302.","productDescription":"5 p.","startPage":"302","endPage":"306","costCenters":[],"links":[{"id":386038,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Foster, Margaret D.","contributorId":21141,"corporation":false,"usgs":true,"family":"Foster","given":"Margaret","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":816682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wones, David R.","contributorId":47455,"corporation":false,"usgs":true,"family":"Wones","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":816683,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Eugster, H.P.","contributorId":99992,"corporation":false,"usgs":true,"family":"Eugster","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":816684,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70209095,"text":"70209095 - 1963 - Preliminary report on the water resources of Kohala Mountain and Mauna Kea, Hawaii","interactions":[],"lastModifiedDate":"2020-03-16T10:35:26","indexId":"70209095","displayToPublicDate":"1963-01-01T11:35:09","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5942,"text":"Circular","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"C14","title":"Preliminary report on the water resources of Kohala Mountain and Mauna Kea, Hawaii","docAbstract":"No abstract available.
","language":"English","publisher":"State of Hawaii","publisherLocation":"Honolulu, Hawaii","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Division of Water and Land Development, Department of Land and Natural Resources","usgsCitation":"Davis, D.A., and Yamanaga, G., 1963, Preliminary report on the water resources of Kohala Mountain and Mauna Kea, Hawaii: Circular C14, vi, 44 p.","productDescription":"vi, 44 p.","costCenters":[],"links":[{"id":373285,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Kohala Mountain, Mauna Kea","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.7964324951172,\n 20.033999524160667\n ],\n [\n -155.57395935058594,\n 20.033999524160667\n ],\n [\n -155.57395935058594,\n 20.209689679623374\n ],\n [\n -155.7964324951172,\n 20.209689679623374\n ],\n [\n -155.7964324951172,\n 20.033999524160667\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.64193725585938,\n 19.711768236041355\n ],\n [\n -155.3404998779297,\n 19.711768236041355\n ],\n [\n -155.3404998779297,\n 19.930104752803004\n ],\n [\n -155.64193725585938,\n 19.930104752803004\n ],\n [\n -155.64193725585938,\n 19.711768236041355\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Davis, Dan A.","contributorId":81188,"corporation":false,"usgs":true,"family":"Davis","given":"Dan","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":784917,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yamanaga, George","contributorId":57117,"corporation":false,"usgs":true,"family":"Yamanaga","given":"George","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":784918,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70263266,"text":"wdrCA632 - 1963 - Surface water records of California, 1963; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2025-02-14T15:46:09.61915","indexId":"wdrCA632","displayToPublicDate":"1963-01-01T10:45:35","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-63-2","title":"Surface water records of California, 1963; Volume 2: Northern Great Basin and Central Valley","docAbstract":"The surface-water records for the 1963 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of California are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Walter Hofmann, district engineer. Surface Water Branch.
Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in California were contained in parts 9, 10, and 11 of that series.
Beginning with the 1961 water year, streamflow records and related data are being released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic data reports is limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas Previously used for the annual series; however, some of the 14 Parts of conterminous United States will be further subdivided.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrCA632","collaboration":"Prepared in cooperation with the State of California and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1963, Surface water records of California, 1963; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-63-2, xiii, 465-938 p., https://doi.org/10.3133/wdrCA632.","productDescription":"xiii, 465-938 p.","costCenters":[],"links":[{"id":482108,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1963/ca-63-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":482107,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1963/ca-63-2/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Central Valley, Northern Great 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp15361","usgsCitation":"Theis, C.V., Brown, R.H., and Meyer, R.R., 1963, Estimating the transmissibility of aquifers from the specific capacity of wells: U.S. Geological Survey Water Supply Paper 1536, 10 p., https://doi.org/10.3133/wsp15361.","productDescription":"10 p.","startPage":"331","endPage":"340","costCenters":[],"links":[{"id":356127,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1536i/report.pdf"},{"id":356238,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Theis, Charles V.","contributorId":48080,"corporation":false,"usgs":true,"family":"Theis","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":741488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, Russell H.","contributorId":106151,"corporation":false,"usgs":true,"family":"Brown","given":"Russell","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":741489,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Meyer, R. R.","contributorId":20725,"corporation":false,"usgs":true,"family":"Meyer","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":741490,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70195915,"text":"70195915 - 1963 - Late Pleistocene glacial drainage in the Devils Lake Region, North Dakota","interactions":[],"lastModifiedDate":"2018-03-07T16:17:10","indexId":"70195915","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"Late Pleistocene glacial drainage in the Devils Lake Region, North Dakota","docAbstract":"The Devils Lake region of northeastern North Dakota is covered with glacial drift deposited by the Leeds lobe of the Mankato Substage of the Wisconsin Stage of the Pleistocene and is underlain by Pierre Shale of Cretaceous age. Associated with the Sheyenne River, which flows through the southern part of the region in a deep trench, are many stream terraces, spillways, deposits of ice-contact stratified drift, and eroded ground-moraine areas. Six stages of drainage have been established to which these various features can be assigned. In the first two stages the features formed as melt water drained to the glacial James River south of the region and as the ice front stood at and later retreated from the site of the Heimdal moraine, a recessional moraine of the Leeds lobe. The later stages occurred after the valley of the Sheyenne River was free of ice and after glacial Lake Souris northwest of the region drained down the valley to glacial Lake Agassiz in the eastern part of the state. Features originating during the four later stages are largely related to the deposition of the North Viking moraine (another, more northern, recessional moraine of the Leeds lobe) and subsequent retreat of the ice from the moraine. Discharge from the local Devils and Stump lakes and from glacial Lake Souris also were of considerable importance in the genesis of many features.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[859:LPGDIT]2.0.CO;2","usgsCitation":"Aronow, S., 1963, Late Pleistocene glacial drainage in the Devils Lake Region, North Dakota: GSA Bulletin, v. 74, no. 7, p. 859-874, https://doi.org/10.1130/0016-7606(1963)74[859:LPGDIT]2.0.CO;2.","productDescription":"16 p.","startPage":"859","endPage":"874","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352309,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Dakota","otherGeospatial":"Devils Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -99.25,\n 47.75\n ],\n [\n -98.25,\n 47.75\n ],\n [\n -98.25,\n 48\n ],\n [\n -99.25,\n 48\n ],\n [\n -99.25,\n 47.75\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"74","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6264e4b0da30c1bfde80","contributors":{"authors":[{"text":"Aronow, Saul","contributorId":59509,"corporation":false,"usgs":true,"family":"Aronow","given":"Saul","email":"","affiliations":[],"preferred":false,"id":730482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2600,"text":"wsp1539V - 1963 - Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water","interactions":[],"lastModifiedDate":"2023-11-01T21:34:49.498797","indexId":"wsp1539V","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"1539","chapter":"V","title":"Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539V","usgsCitation":"Robinove, C.J., Berry, D.W., and Connor, J.G., 1963, Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 44 p.; 2 Plates: 25.00 x 42.75 inches and 27.00 x 11.88 inches, https://doi.org/10.3133/wsp1539V.","productDescription":"Report: iv, 44 p.; 2 Plates: 25.00 x 42.75 inches and 27.00 x 11.88 inches","costCenters":[],"links":[{"id":422319,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24743.htm","linkFileType":{"id":5,"text":"html"}},{"id":28882,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539v/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28881,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539v/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28880,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539v/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138893,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539v/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Bear River Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110.8033,\n 42.221\n ],\n [\n -111.048,\n 42.221\n ],\n [\n -111.048,\n 41\n ],\n [\n -110.8033,\n 41\n ],\n [\n -110.8033,\n 42.221\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66035d","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":145473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, Delmar W.","contributorId":25107,"corporation":false,"usgs":true,"family":"Berry","given":"Delmar","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145472,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Connor, John G.","contributorId":34489,"corporation":false,"usgs":true,"family":"Connor","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":887319,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":23,"text":"wsp1738 - 1963 - Compilation of records of surface waters of the United States, October 1950 to September 1960; Part 14. Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2023-10-31T18:57:46.240092","indexId":"wsp1738","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"1738","title":"Compilation of records of surface waters of the United States, October 1950 to September 1960; Part 14. Pacific slope basins in Oregon and lower Columbia River basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1738","usgsCitation":"Hendricks, E.L., Phillips, K.N., and Veatch, F.M., 1963, Compilation of records of surface waters of the United States, October 1950 to September 1960; Part 14. Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1738, Report: xi, 327 p.; 1 Plate: 22.00 x 26.50 inches, https://doi.org/10.3133/wsp1738.","productDescription":"Report: xi, 327 p.; 1 Plate: 22.00 x 26.50 inches","costCenters":[],"links":[{"id":422297,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24922.htm","linkFileType":{"id":5,"text":"html"}},{"id":24636,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1738/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24635,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1738/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137547,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1738/report-thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.29995400606613,\n 46.89602197924074\n ],\n [\n -124.05841651446201,\n 46.74913966177681\n ],\n [\n -124.53147247564391,\n 41.36227985029197\n ],\n [\n -122.50227705219493,\n 41.81684742741416\n ],\n [\n -120.14970701275175,\n 43.59789521537286\n ],\n [\n -117.18739538704797,\n 44.9711058195835\n ],\n [\n -117.29995400606613,\n 46.89602197924074\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9915","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":141826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phillips, K. N.","contributorId":36806,"corporation":false,"usgs":true,"family":"Phillips","given":"K.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":887257,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Veatch, F. M.","contributorId":97484,"corporation":false,"usgs":true,"family":"Veatch","given":"F.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":887258,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1149,"text":"wsp1669C - 1963 - Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water","interactions":[{"subject":{"id":52076,"text":"ofr6029 - 1960 - A preliminary report of the geology and ground-water resources of Upper Black Earth Creek Basin, Wisconsin, with a section on surface water","indexId":"ofr6029","publicationYear":"1960","noYear":false,"title":"A preliminary report of the geology and ground-water resources of Upper Black Earth Creek Basin, Wisconsin, with a section on surface water"},"predicate":"SUPERSEDED_BY","object":{"id":1149,"text":"wsp1669C - 1963 - Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water","indexId":"wsp1669C","publicationYear":"1963","noYear":false,"chapter":"C","title":"Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water"},"id":1}],"lastModifiedDate":"2023-11-27T21:46:12.820397","indexId":"wsp1669C","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"1669","chapter":"C","title":"Hydrology of upper Black Earth Creek basin, Wisconsin, with a section on surface water","docAbstract":"The upper Black Earth Creek drainage basin has an area of 46 square miles and is in Dane County in south-central Wisconsin. The oldest rock exposed in the valley walls is the sandstone of Late Cambrian age. Dolomite of the Prairie du Chien Group of Ordovician age overlies the sandstone and forms the. resistant cap on the hills. The St. Peter Sandstone, Platteville and Decorah Formations, and Galena Dolomite, all Ordovician in age, form a narrow belt along the southern boundary of the area. Outwash and alluvium of Pleistocene and Recent age fill the valleys. The eastern half of the area was glaciated and is covered with till. The sandstone of Late Cambrian age and the sand and gravel of the outwash deposits are hydraulically connected. Ground water occurs under unconfined (water-table) conditions in the western unglaciated part of the basin and under artesian conditions beneath the till locally in the eastern part. The source of most of the ground water is direct infiltration of precipitation; however, some ground water enters the area as underflow from the south. About 7 inches of the 30 inches of average annual precipitation recharges the ground-water reservoir. The ground water generally moves toward Black Earth Creek where it is discharged. Some ground water moves out of the basin as underflow beneath the valley of Black Earth Creek, and some is discharged by evapotranspiration or is withdrawn by pumping from wells. Water levels in shallow nonartesian wells respond rapidly to precipitation. The effect of precipitation on water levels in artesian wells is slower and more subdued. Water levels are generally highest in spring and lowest in fall and winter. The flow of upper Black Earth Creek is derived mostly from ground-water discharge, except during short periods of and immediately after precipitation when most of the flow is derived from surface runoff. The runoff from upper Black Earth Creek basin decreased from an average of 8.72 inches per square mile of drainage area in 1955 to 5.55 inches in 1958; the decrease reflects the generally decreasing precipitation and declining water levels in the basin during that period. On July 10, 1958, the discharge from the basin was 0.367 cubic feet per second per square mile, and the greatest discharge was 0.84 cubic feet per second per square mile from the southwest subbasin. The ground water has an average temperature of about 50°F. It is a calcium magnesium bicarbonate type water and is very hard.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa19c","contributors":{"authors":[{"text":"Swindel, George Washington","contributorId":82684,"corporation":false,"usgs":true,"family":"Swindel","given":"George","email":"","middleInitial":"Washington","affiliations":[],"preferred":false,"id":145784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, M.R.","contributorId":13603,"corporation":false,"usgs":true,"family":"Williams","given":"M.R.","email":"","affiliations":[],"preferred":false,"id":145783,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Geurin, James Walter","contributorId":102060,"corporation":false,"usgs":true,"family":"Geurin","given":"James","email":"","middleInitial":"Walter","affiliations":[],"preferred":false,"id":145785,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baldwin, H. L.","contributorId":104032,"corporation":false,"usgs":true,"family":"Baldwin","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":889263,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1079,"text":"wsp1619D - 1963 - Ground-water resources of the coastal sand-dune area north of Coos Bay, Oregon","interactions":[{"subject":{"id":22590,"text":"ofr5618 - 1956 - Ground-water resources of the sand-dune area north of Coos Bay, Oregon","indexId":"ofr5618","publicationYear":"1956","noYear":false,"title":"Ground-water resources of the sand-dune area north of Coos Bay, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":1079,"text":"wsp1619D - 1963 - Ground-water resources of the coastal sand-dune area north of Coos Bay, Oregon","indexId":"wsp1619D","publicationYear":"1963","noYear":false,"chapter":"D","title":"Ground-water resources of the coastal sand-dune area north of Coos Bay, Oregon"},"id":1}],"lastModifiedDate":"2023-03-24T19:41:14.513066","indexId":"wsp1619D","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","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":"1619","chapter":"D","title":"Ground-water resources of the coastal sand-dune area north of Coos Bay, Oregon","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619D","usgsCitation":"Brown, S., and Newcomb, R.C., 1963, Ground-water resources of the coastal sand-dune area north of Coos Bay, Oregon: U.S. Geological Survey Water Supply Paper 1619, Report; iv, 32 p.; 2 Plates: 15.00 x 24.25 inches and 19.00 x 10.00 inches, https://doi.org/10.3133/wsp1619D.","productDescription":"Report; iv, 32 p.; 2 Plates: 15.00 x 24.25 inches and 19.00 x 10.00 inches","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":137097,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619d/report-thumb.jpg"},{"id":25791,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25790,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25789,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1619d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414726,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24818.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Oregon","city":"Coos Bay","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.367,\n 43.632\n ],\n [\n -124.367,\n 43.333\n ],\n [\n -124.123,\n 43.333\n ],\n [\n -124.123,\n 43.632\n ],\n [\n -124.367,\n 43.632\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65ac40","contributors":{"authors":[{"text":"Brown, S. G.","contributorId":46914,"corporation":false,"usgs":true,"family":"Brown","given":"S. G.","affiliations":[],"preferred":false,"id":143142,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newcomb, R. C.","contributorId":77907,"corporation":false,"usgs":true,"family":"Newcomb","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":143143,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000140,"text":"1000140 - 1963 - Age and growth of the whitefish in Lake Superior","interactions":[],"lastModifiedDate":"2013-02-04T11:54:57","indexId":"1000140","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Age and growth of the whitefish in Lake Superior","docAbstract":"The average annual commercial production of whitefish in the U.S. waters of Lake Superior dropped from 2,194,000 pounds in 1879-1908 to 504,000 pounds in 1911-59. The modern production, though far below the earlier, has accounted for more than 10 percent of the total value of the fishery in all but one of the last 20 years. Data are given on growth rate, age and year-class composition, size distribution, and length-weight relation of 1,800 fish collected in 1957-59 at Bayfield, Wis., and Marquette, Whitefish Point, and Dollar Settlement, Mich. Studies of the body-scale relation, sex ratio, and age and size at maturity were limited to fish collected at Bayfield. The age composition and mean age varied widely by port and year of capture. Oldest fish were those of the 1957 Bayfield samples which were dominated by age group VII and averaged 5.5 years old. The youngest were from Whitefish Point in 1959; age-group III was dominant, and the mean age was 3.2 years. The evidence on the strength of year classes was not clear-cut, but it was obvious that fluctuations in stocks of different areas were largely independent. The percentage of legal-size fish (17 inches or longer) in age groups ranged widely; only 8.6 percent of the V group were legal in the 1957 Bayfield collections, whereas 100 percent of fish of the same age were legal in the 1957-59 collections from Whitefish Point. The weight of whitefish in the combined samples increased as the 3.2408 power of the length. The growth rate from the fastest to the slowest growing stocks ranked as follows: Whitefish Point; Dollar Settlement and Marquette (fish from the two ports reversed ranks after 3 years); Bayfield. The major differences in growth in length among the various stocks occurred during the first years of life. Beyond the fifth year the annual increments were nearly the same in all stocks. The whitefish from Whitefish Point, Dollar Settlement, and Marquette are among the fastest growing in the Great Lakes. The differences among the Lake Superior stocks in age and year-class composition, and in growth rate offer convincing evidence that populations of different areas are entirely independent. The sexes were almost equally represented (51.5 percent males) in the combined Bayfield samples, but males were scarce in age groups older than VIII. Whitefish from Bayfield shorter than 14.5 inches were immature and those larger than 17.4 inches were mature. The youngest mature fish belonged to age-group V,and all older than the VII group were mature.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Dryer, W.R., 1963, Age and growth of the whitefish in Lake Superior: Fishery Bulletin, v. 63, no. 1, p. 77-95.","productDescription":"19 p.","startPage":"77","endPage":"95","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266925,"type":{"id":11,"text":"Document"},"url":"https://fishbull.noaa.gov/63-1/dryer.pdf"}],"volume":"63","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6896d5","contributors":{"authors":[{"text":"Dryer, William R.","contributorId":71921,"corporation":false,"usgs":true,"family":"Dryer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308130,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000476,"text":"1000476 - 1963 - The movements of walleyes tagged as yearlings in Lake Erie","interactions":[],"lastModifiedDate":"2016-02-29T10:15:47","indexId":"1000476","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"The movements of walleyes tagged as yearlings in Lake Erie","docAbstract":"A total of 3,998 yearling walleyes, Stizostedion vitreum vitreum (Mitchill), were captured, tagged, and released along the south shore of western Lake Erie to determine their movements and their dispersal from a known nursery area. Four hundred ninety-nine recoveries were made over a period of 3 years. Tagged walleyes traveled primarily north toward the islands in the Western Basin during their first year of liberation, and in succeeding years moved progressively toward the extreme western end of the lake. Some walleyes were recaptured within 6 months in the Detroit River, Lake St. Clair, the St. Clair River, and southern Lake Huron, and the percentage of fish recaptured in these waters north of Lake Erie increased annually. Movement eastward into the Central and Eastern Basins of the lake appeared negligible. The greatest distance traveled by a marked walleye was 236 miles. The average distance traveled by all tagged fish was 25 miles.
","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1963)92[414:TMOWTA]2.0.CO;2","usgsCitation":"Wolfert, D.R., 1963, The movements of walleyes tagged as yearlings in Lake Erie: Transactions of the American Fisheries Society, v. 92, no. 4, p. 414-420, https://doi.org/10.1577/1548-8659(1963)92[414:TMOWTA]2.0.CO;2.","productDescription":"7 p.","startPage":"414","endPage":"420","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132839,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4956","contributors":{"authors":[{"text":"Wolfert, David R.","contributorId":49305,"corporation":false,"usgs":true,"family":"Wolfert","given":"David","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000471,"text":"1000471 - 1963 - Food of the bloater, Coregonus hoyi, in Lake Michigan","interactions":[],"lastModifiedDate":"2016-02-29T10:28:56","indexId":"1000471","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Food of the bloater, Coregonus hoyi, in Lake Michigan","docAbstract":"Stomachs were examined from 1,469 Lake Michigan bloaters, Coregonus [Leucichthys] hoyi, greater than 7 inches long which contained identifiable food. An additional 461 ciscoes less than 7 inches long were incorporated into the study; these latter fish were not positively identified, but most of them undoubtedly were bloaters. The specimens were caught in bottom nets except for 49, all less than 6 inches long, taken in midwater trawls. Lake Michigan bloaters under 7 inches long depend heavily on zooplankton. Those larger than 7 inches feed predominantly on Pontoporeia affinis and Mysis relicta, although fish of the 7.0- to 7.9-inch size range commonly eat zooplankton, expecially in shallower water. Generally, Mysis becomes more important, and Pontoporeia less so, as the depth increases and as the season progresses from spring to fall. Incidence of Pontoporeia increases and that of Mysis declines as the fish size increases. Other food items, in decreasing order of importance, are fingernail clams, midges (all stages of development), fish eggs, ostracods, and miscellaneous adult and immature insects other than midges.
","language":"English","doi":"10.1577/1548-8659(1963)92[245:FOTBCH]2.0.CO;2","usgsCitation":"Wells, L., and Beeton, A.M., 1963, Food of the bloater, Coregonus hoyi, in Lake Michigan: Transactions of the American Fisheries Society, v. 92, no. 3, p. 245-255, https://doi.org/10.1577/1548-8659(1963)92[245:FOTBCH]2.0.CO;2.","productDescription":"11 p.","startPage":"245","endPage":"255","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133681,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"92","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de4f2","contributors":{"authors":[{"text":"Wells, LaRue","contributorId":75476,"corporation":false,"usgs":true,"family":"Wells","given":"LaRue","email":"","affiliations":[],"preferred":false,"id":308593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":308594,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4091,"text":"cir478 - 1963 - Floods in Wyoming, magnitude and frequency","interactions":[],"lastModifiedDate":"2023-04-27T19:49:17.622715","indexId":"cir478","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"478","title":"Floods in Wyoming, magnitude and frequency","docAbstract":"This report contains the results of four separate flood-frequency analyses designated A, B, C, and D. Analysis A is for the portion of Wyoming east of the Continental Divide. Analysis B applies to the portion of Wyoming in Part 9, as designated in streamflow reports entitled \"Surface Water Supply of the United Stated\" published by the U.S. Geological Survey, and was extracted fro.m an unpublished study by W. P. Somers in 1959. Analysis C applies to Part 10 and was extracted from Circutar 457 (Berwick, 1962). Analysis D applies to Part 13 and was extracted from a report by C. A. Thomas, H. C. Broom, and J. E. Cummans (1963).
Methods described in this report can be used to estimate the magnitude of a flood of any selected recurrence interval between 1.1 and 50 years for any unregulated stream in Wyoming, gaged or ungaged, within the scope of the data. Flood-frequency relations are not defined for a large part of the North Platte River basin in south-central Wyoming because of insufficient data.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir478","collaboration":"Prepared in cooperation with Wyoming State Highway Department","usgsCitation":"Carter, J.R., and Green, A.R., 1963, Floods in Wyoming, magnitude and frequency: U.S. Geological Survey Circular 478, Report: iv, 27 p.; 2 Plates: 9.36 x 12.59 and 9.18 x 12.67 inches, https://doi.org/10.3133/cir478.","productDescription":"Report: iv, 27 p.; 2 Plates: 9.36 x 12.59 and 9.18 x 12.67 inches","numberOfPages":"32","costCenters":[],"links":[{"id":416456,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23527.htm","linkFileType":{"id":5,"text":"html"}},{"id":31192,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0478/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271068,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0478/plate-1.pdf"},{"id":271069,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0478/plate-2.pdf"},{"id":124473,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0478/report-thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0569,40.9947 ], [ -111.0569,45.0059 ], [ -104.0522,45.0059 ], [ -104.0522,40.9947 ], [ -111.0569,40.9947 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699af5","contributors":{"authors":[{"text":"Carter, J. R.","contributorId":23128,"corporation":false,"usgs":true,"family":"Carter","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148173,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, A. Rice","contributorId":31731,"corporation":false,"usgs":true,"family":"Green","given":"A.","email":"","middleInitial":"Rice","affiliations":[],"preferred":false,"id":148174,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":7000056,"text":"7000056 - 1963 - A primer on ground water","interactions":[],"lastModifiedDate":"2017-06-10T11:40:17","indexId":"7000056","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"A primer on ground water","docAbstract":"Most of us don't have to look for water. We grew up either in big cities where there was a public water supply, or in small towns or on farms where the water came from wells. But there are some people to whom finding a new supply of water is vitally important.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/7000056","usgsCitation":"Baldwin, H., and McGuinness, C.L., 1963, A primer on ground water (1990 reprint): General Interest Publication, iii, 26 p., https://doi.org/10.3133/7000056.","productDescription":"iii, 26 p.","numberOfPages":"31","costCenters":[],"links":[{"id":261219,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/7000056/report.pdf"},{"id":261220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/7000056/report-thumb.jpg"}],"edition":"1990 reprint","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9ad0","contributors":{"authors":[{"text":"Baldwin, Helene L.","contributorId":34622,"corporation":false,"usgs":true,"family":"Baldwin","given":"Helene L.","affiliations":[],"preferred":false,"id":344031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McGuinness, C. L.","contributorId":20313,"corporation":false,"usgs":true,"family":"McGuinness","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":344030,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2000028,"text":"2000028 - 1963 - The use of alkalinity and conductivity measurements to estimate concentrations of 3-trifluormethyl-4-nitrophenol required for treating lamprey streams","interactions":[],"lastModifiedDate":"2012-02-02T00:14:56","indexId":"2000028","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"7","title":"The use of alkalinity and conductivity measurements to estimate concentrations of 3-trifluormethyl-4-nitrophenol required for treating lamprey streams","docAbstract":"A method has been devised to estimate the minimum concentration of TFM that will kill sea lampreys and the maximum that will not kill fish. It is based on the relation of these concentrations to the alkalinity and the conductivity of various waters. Pretreatment bioassays will continue to be required for precise determination of treatment concentrations, but the estimates made possible by the method will permit a great reduction in the number of bioassays on a single stream.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Kanayama, R.K., 1963, The use of alkalinity and conductivity measurements to estimate concentrations of 3-trifluormethyl-4-nitrophenol required for treating lamprey streams: Technical Report 7, 10 p.","productDescription":"10 p.","startPage":"0","endPage":"10","numberOfPages":"10","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198774,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92068,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr07.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4efc","contributors":{"authors":[{"text":"Kanayama, Richard K.","contributorId":102974,"corporation":false,"usgs":true,"family":"Kanayama","given":"Richard","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":324951,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2000007,"text":"2000007 - 1963 - Limnological survey of Lake Erie 1959 and 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:14:59","indexId":"2000007","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"6","title":"Limnological survey of Lake Erie 1959 and 1960","docAbstract":"Federal, provincial, state, and university organizations participated in cooperative limnological surveys of Lake Erie in September 1959 and August 1960 to determine the extent and severity of the low dissolved-oxygen content of the hypolimnetic waters. Observations were restricted to the central basin in 1959, but were lake-wide in 1960. Approximately 70 percent of the bottom waters of the central basin had a serious oxygen deficiency during both years. Data were obtained also on the distribution of temperature, transparency, specific conductance, pH, and phenolphthalein and total alkalinity. The distributions of the chemical values are discussed in terms of their relationships to each other, and to thermal stratification, river outflow, lake morphometry, and lake currents.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Beeton, A.M., 1963, Limnological survey of Lake Erie 1959 and 1960: Technical Report 6, 32 p.","productDescription":"32 p.","startPage":"0","endPage":"32","numberOfPages":"32","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92067,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr06.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9d92","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":324916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014271,"text":"1014271 - 1963 - Two new Gyrodactylus (Trematoda: Monogenea) from cyprinid fishes with synopsis of those found on North American fishes","interactions":[],"lastModifiedDate":"2025-05-01T15:05:00.807077","indexId":"1014271","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2414,"text":"Journal of Parasitology","active":true,"publicationSubtype":{"id":10}},"title":"Two new Gyrodactylus (Trematoda: Monogenea) from cyprinid fishes with synopsis of those found on North American fishes","docAbstract":"Gyrodactylus atratuli from the blacknose dace (Rhinichthys atratulus) and the pearl dace (Semotilus margarita) is compared with known species of Gyrodactylus from North American fishes and described as a new species. Gyrodactylus margaritae from the pearl dace (Semotilus margarita) is compared with known species of Gyrodactylus from North American fishes and described as a new species. The average number of G. atratuli per blacknose dace in the natural habitat is 7.8 (1 to 32) and in the laboratory at the same water temperature after 55 days in captivity, 5.4 (0 to 11). G. atratuli and G. margaritae fail to live and reproduce on fish kept in nonrunning water at between 19 and 26 C in laboratory aquaria, but will live and reproduce in running spring water at 12 C in laboratory aquaria. An illustrated synopsis with a comparative table of measurements of known North American Gyrodactylus and a list of the species with brief reference to their differentiating characteristics are given.
","language":"English","publisher":"American Society of Parasitologists","doi":"10.2307/3275760","usgsCitation":"Putz, R., and Hoffman, G.L., 1963, Two new Gyrodactylus (Trematoda: Monogenea) from cyprinid fishes with synopsis of those found on North American fishes: Journal of Parasitology, v. 49, no. 4, p. 559-566, https://doi.org/10.2307/3275760.","productDescription":"8 p.","startPage":"559","endPage":"566","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":487911,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.2307/3275760","text":"Publisher Index Page"},{"id":130867,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a48e4b07f02db6239f5","contributors":{"authors":[{"text":"Putz, R.E.","contributorId":42543,"corporation":false,"usgs":true,"family":"Putz","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":320087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320088,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70171156,"text":"70171156 - 1963 - Quantitation of microorganic compounds in waters of the Great Lakes by adsorption on activated carbon","interactions":[],"lastModifiedDate":"2016-05-24T10:12:08","indexId":"70171156","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Quantitation of microorganic compounds in waters of the Great Lakes by adsorption on activated carbon","docAbstract":"Microorganic compounds in waters of Lakes Michigan and Huron have been sampled by adsorption on activated carbon in filters installed aboard the M/V Cisco and at the Hammond Bay Laboratory of the U.S. Bureau of Commercial Fisheries. The organic compounds were eluted from the carbon according to techniques developed at the U.S. Public Health Service. On the assumption that chloroform eluates represent less polar compounds from industrial sources and alcohol eluates the more polar varieties of natural origin, plots of chloroform eluates against alcohol eluates appear to be useful in judging water qualities. Based upon these criteria, the data in this paper indicate that both the waters of northern Lake Michigan and of Lake Huron, in the vicinity of Hammond Bay, Michigan, are relatively free from pollution. The limnetic waters of Lake Michigan showed a particularly high ratio of alcohol to chloroform eluates. Data for monthly samples indicated that this ratio fluctuated seasonally. The periodicity of the fluctuations was similar to those of lake levels and water temperatures.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 6th Conference on Great Lakes Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"6th Conference on Great Lakes Research","conferenceDate":"June 13-15, 1963","conferenceLocation":"Ann Arbor, MI","language":"English","publisher":"University of Michigan","usgsCitation":"Daniels, S.L., Kempe, L.L., Graham, E.S., and Beeton, A.M., 1963, Quantitation of microorganic compounds in waters of the Great Lakes by adsorption on activated carbon, in Proceedings of the 6th Conference on Great Lakes Research, Ann Arbor, MI, June 13-15, 1963, p. 118-123.","productDescription":"6 p.","startPage":"118","endPage":"123","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321594,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d6635e4b07e28b6684cbe","contributors":{"authors":[{"text":"Daniels, Stacy L.","contributorId":105821,"corporation":false,"usgs":true,"family":"Daniels","given":"Stacy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kempe, Lloyd L.","contributorId":55117,"corporation":false,"usgs":true,"family":"Kempe","given":"Lloyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630131,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Graham, E. S.","contributorId":169582,"corporation":false,"usgs":false,"family":"Graham","given":"E.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":630132,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630133,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70171157,"text":"70171157 - 1963 - The movement, heterogeneity, and rate of exploitation of walleyes in northern Green Bay, Lake Michigan, as determined by tagging","interactions":[],"lastModifiedDate":"2016-05-24T10:26:29","indexId":"70171157","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"The movement, heterogeneity, and rate of exploitation of walleyes in northern Green Bay, Lake Michigan, as determined by tagging","docAbstract":"The Michigan waters of northern Green Bay are an important center for commercial and sport fishing. This 400-square-mile area has supported a commercial fishery for many years but the development of the intensive sport fishery is more recent, mostly since World War II. The commercial fishery is based on several species, whereas anglers are particularly interested in the walleye, Stizostedion v. vitreum. Broad objectives of tagging studies initiated in September 1957 were to obtain information on the heterogeneity, movement, and exploitation of the walleye population of northern Green Bay. The statistical data on the commercial fishery are very sound but other information on the Green Bay walleye has been sketchy.
","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the North Atlantic Fish Marking Symposium","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"North Atlantic Fish Marking Symposium","conferenceDate":"May 1961","conferenceLocation":"Woods Hole, MA","language":"English","publisher":"International Commission for the Northwest Atlantic Fisheries","usgsCitation":"Crowe, W.R., Karvelis, E.G., and Joeris, L.S., 1963, The movement, heterogeneity, and rate of exploitation of walleyes in northern Green Bay, Lake Michigan, as determined by tagging, in Proceedings of the North Atlantic Fish Marking Symposium, Woods Hole, MA, May 1961, p. 38-41.","productDescription":"4 p.","startPage":"38","endPage":"41","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321595,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d6663e4b07e28b6684fb0","contributors":{"authors":[{"text":"Crowe, Walter R.","contributorId":38673,"corporation":false,"usgs":true,"family":"Crowe","given":"Walter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":630134,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karvelis, Ernest G.","contributorId":55547,"corporation":false,"usgs":true,"family":"Karvelis","given":"Ernest","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":630135,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Joeris, Leonard S.","contributorId":104430,"corporation":false,"usgs":true,"family":"Joeris","given":"Leonard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":630136,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}