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,{"id":1097,"text":"wsp1669S - 1964 - Yearly variations in runoff for the conterminous United States, 1931-1960","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1669S","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"S","title":"Yearly variations in runoff for the conterminous United States, 1931-1960","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1669S","usgsCitation":"Busby, M., 1964, Yearly variations in runoff for the conterminous United States, 1931-1960: U.S. Geological Survey Water Supply Paper 1669, iii, 49 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1669S.","productDescription":"iii, 49 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669s/report-thumb.jpg"},{"id":25827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669s/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de56d","contributors":{"authors":[{"text":"Busby, Mark W.","contributorId":83099,"corporation":false,"usgs":true,"family":"Busby","given":"Mark W.","affiliations":[],"preferred":false,"id":143172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":229,"text":"wsp1613C - 1964 - Sea water in coastal aquifers","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1613C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1613","chapter":"C","title":"Sea water in coastal aquifers","docAbstract":"Investigations in the coastal part of the Biscayne aquifer, a highly productive aquifer of limestone and sand in the Miami area, Florida, show that the salt-water front is dynamically stable as much as 8 miles seaward of the position computed according to the Ghyben-Herzberg principle. This discrepancy results, at least in part, from the fact that the salt water in the Biscayne aquifer is not static, as explanations of the dynamic balance commonly assume. Cross sections showing lines of equal fresh-water potential indicate that during periods of heavy recharge, the fresh-water head is high enough to cause the fresh water, the salt water, and the zone of diffusion between them to move seaward. When the fresh-water head is low, salt water in the lower part of the aquifer intrudes inland, but some of the diluted sea water in the zone of diffusion continues to flow seaward. Thus, salt water circulates inland from the floor of the sea through the lower part of the aquifer becoming progressively diluted with fresh water to a line along which there is no horizontal component of flow, after which it moves upward and returns to the sea. \r\n\r\nThis cyclic flow is demonstrated by a flow net which is constructed by the use of horizontal gradients determined from the low-head equipotential diagram. The flow net shows that about seven-eights of the total discharge at the shoreline originates as fresh water in inland parts of the aquifer. The remaining one-eighth represents a return of sea water entering the aquifer through the floor of the sea.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1613C","usgsCitation":"Cooper, H.H., 1964, Sea water in coastal aquifers: U.S. Geological Survey Water Supply Paper 1613, v, 84 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1613C.","productDescription":"v, 84 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":137491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1613c/report-thumb.jpg"},{"id":24839,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1613c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4814e4b07f02db4dab60","contributors":{"authors":[{"text":"Cooper, Hilton H.","contributorId":106867,"corporation":false,"usgs":true,"family":"Cooper","given":"Hilton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":142102,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":932,"text":"wsp1779G - 1964 - Geology and ground-water resources of Bradley, Calhoun, and Ouachita Counties, Arkansas","interactions":[],"lastModifiedDate":"2013-11-05T14:26:47","indexId":"wsp1779G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"G","title":"Geology and ground-water resources of Bradley, Calhoun, and Ouachita Counties, Arkansas","language":"ENGLISH","publisher":"U. S. Government Printing Office,","doi":"10.3133/wsp1779G","usgsCitation":"Albin, D.R., 1964, Geology and ground-water resources of Bradley, Calhoun, and Ouachita Counties, Arkansas: U.S. Geological Survey Water Supply Paper 1779, iv, 32 p. :ill., maps (6 fold. in pocket) ;24 cm., https://doi.org/10.3133/wsp1779G.","productDescription":"iv, 32 p. :ill., maps (6 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":246954,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779g/plate-7.pdf","size":"1337","linkFileType":{"id":1,"text":"pdf"}},{"id":276513,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779g/plate-1.pdf"},{"id":276514,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779g/plate-4.pdf"},{"id":276515,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779g/plate-5.pdf"},{"id":276516,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779g/plate-6.pdf"},{"id":277938,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779g/report-thumb.jpg"},{"id":278835,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779g/plate-3.pdf"},{"id":278833,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779g/report.pdf"},{"id":278834,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779g/plate-2.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685bb3","contributors":{"authors":[{"text":"Albin, Donald R.","contributorId":67486,"corporation":false,"usgs":true,"family":"Albin","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":142876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1307,"text":"wsp1779L - 1964 - Discharge ratings for streams at submerged section controls","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1779L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"L","title":"Discharge ratings for streams at submerged section controls","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1779L","usgsCitation":"Eisenlohr, W.S., 1964, Discharge ratings for streams at submerged section controls: U.S. Geological Survey Water Supply Paper 1779, iii, 32 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1779L.","productDescription":"iii, 32 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137889,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779l/report-thumb.jpg"},{"id":26340,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26341,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a98a","contributors":{"authors":[{"text":"Eisenlohr, William Stewart","contributorId":36533,"corporation":false,"usgs":true,"family":"Eisenlohr","given":"William","email":"","middleInitial":"Stewart","affiliations":[],"preferred":false,"id":143536,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1338,"text":"wsp1809E - 1964 - Galleries and their use for development of shallow ground-water supplies, with special reference to Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1809E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1809","chapter":"E","title":"Galleries and their use for development of shallow ground-water supplies, with special reference to Alaska","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809E","usgsCitation":"Feulner, A.J., 1964, Galleries and their use for development of shallow ground-water supplies, with special reference to Alaska: U.S. Geological Survey Water Supply Paper 1809, v, 16 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1809E.","productDescription":"v, 16 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809e/report-thumb.jpg"},{"id":26398,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1449","contributors":{"authors":[{"text":"Feulner, Alvin J.","contributorId":49775,"corporation":false,"usgs":true,"family":"Feulner","given":"Alvin","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":143590,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1021,"text":"wsp1536I - 1964 - Methods of determining permeability, transmissibility and drawdown","interactions":[{"subject":{"id":51650,"text":"ofr5480 - 1954 - The \"slug test\" for estimating transmissibility","indexId":"ofr5480","publicationYear":"1954","noYear":false,"title":"The \"slug test\" for estimating transmissibility"},"predicate":"SUPERSEDED_BY","object":{"id":1021,"text":"wsp1536I - 1964 - Methods of determining permeability, transmissibility and drawdown","indexId":"wsp1536I","publicationYear":"1964","noYear":false,"chapter":"I","title":"Methods of determining permeability, transmissibility and drawdown"},"id":1},{"subject":{"id":51779,"text":"ofr54310 - 1954 - Estimating transmissibility from specific capacity","indexId":"ofr54310","publicationYear":"1954","noYear":false,"title":"Estimating transmissibility from specific capacity"},"predicate":"SUPERSEDED_BY","object":{"id":1021,"text":"wsp1536I - 1964 - Methods of determining permeability, transmissibility and drawdown","indexId":"wsp1536I","publicationYear":"1964","noYear":false,"chapter":"I","title":"Methods of determining permeability, transmissibility and drawdown"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1536I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1536","chapter":"I","title":"Methods of determining permeability, transmissibility and drawdown","docAbstract":"If the Theis graphical method is used for determining the hydraulic constants of an aquifer under water-table conditions, the observed drawdowns should be corrected for the decrease in saturated thickness. This is especially true if the drawdown is a large fraction of the original saturated thickness, for then the computed coefficient of permeability is highly inaccurate if based on observed, rather than corrected, water levels. Wenzel's limiting formula, a modification of the Theis graphical method, is useful where u=r2s/4Tt is less than about 0.01. However, a shorter procedure for determination of the coefficient of transmissibility, as well as the coefficient of storage, consists of plotting the values of the corrected drawdowns against the values of the logarithm of r. \r\n\r\nWenzel (1942) suggested that observation wells be situated on lines that extend upgradient and downgradient from the pumped well. However, a detailed analysis of aquifer-test results indicates that such a restriction is unnecessary. The gradient method for determining permeability should yield the same results as the Thies method. The former, when applied for a distance within the range of applicability of the latter, is merely a duplication of effort or, at best, a crude check. Because of the limitations of accuracy in plotting, the gradient method is much less satisfactory. That Wenzel (1942) obtained identical results from the two methods is regarded as a coincidence. \r\n\r\nFailure to take into consideration the fact that the pumped well does not tap the full thickness of the aquifer leads to an apparent coefficient of permeability that is much too low, especially if the aquifer consists of stratified sediments. The average coefficient of permeability computed from uncorrected drawdowns may be only a little more than half of the true value.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1536I","usgsCitation":"Bentall, R., 1964, Methods of determining permeability, transmissibility and drawdown: U.S. Geological Survey Water Supply Paper 1536, vi, 99 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1536I.","productDescription":"vi, 99 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1536i/report-thumb.jpg"},{"id":25635,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1536i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62bcc6","contributors":{"authors":[{"text":"Bentall, Ray","contributorId":78711,"corporation":false,"usgs":true,"family":"Bentall","given":"Ray","email":"","affiliations":[],"preferred":false,"id":143040,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1004,"text":"wsp1669V - 1964 - Ground water in the lower Arkansas River valley, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1669V","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"V","title":"Ground water in the lower Arkansas River valley, Arkansas","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1669V","usgsCitation":"Bedinger, M.S., and Jeffery, H., 1964, Ground water in the lower Arkansas River valley, Arkansas: U.S. Geological Survey Water Supply Paper 1669, iii, 17 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1669V.","productDescription":"iii, 17 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":136147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669v/report-thumb.jpg"},{"id":25575,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669v/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25576,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669v/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25577,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669v/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25578,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669v/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25579,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669v/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25580,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669v/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25581,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669v/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d765","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":143003,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jeffery, H. G.","contributorId":74353,"corporation":false,"usgs":true,"family":"Jeffery","given":"H. G.","affiliations":[],"preferred":false,"id":143004,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1023,"text":"wsp1669U - 1964 - Ground-water resources of Waupaca County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-02T13:05:28","indexId":"wsp1669U","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"U","title":"Ground-water resources of Waupaca County, Wisconsin","docAbstract":"<p>Waupaca County is in east-central Wisconsin. No serious ground-water problems existed in 1960 except in a few localities where crystalline rock is near land surface or is covered by nearly impermeable till. The use of ground water for irrigation has not appreciably affected ground-water levels.</p>\n<p>The county is covered by Pleistocene till, glaciolacustrine (lake), glaciofluvial (stream), and eolian (wind) deposits. In the northern three-quarters of the county these deposits overlie Precambrian crystalline rocks; in the remainder, they overlie sandstone of Cambrian age and, to a minor extent, dolomite of the Prairie du Chien Group of Ordovician age. The deposits of Pleistocene age, particularly outwash, are the principal sources of ground water except in those areas where the saturated thickness is slight or the permeability low. The sandstone of Cambrian age is an important aquifer in the southeastern part of the county. The crystalline rocks of Precambrian age yield little water except from fractures, joints, and weathered zones, and they are a source of water only in areas where better aquifers are absent.</p>\n<p>Ground water in Waupaca County occurs under both water-table and artesian conditions. The source of this ground water is precipitation that falls on the county and percolates downward to the zone of saturation. Regional movement of ground water is to the Wolf River. In most of the county the direction of movement is eastward or southeastward, except in the southeastern corner of the county, where the movement is westward.</p>\n<p>&nbsp;Water-level fluctuations reflect the variations of ground-water storage or artesian pressure in response to variations in recharge and discharge. Declining water levels from 1956 to 1959 reflect a period of below-normal precipitation, and rising water levels in late 1959 and 1960 reflect above-normal precipitation. Average precipitation, runoff, and evapotranspiration in 1959 are estimated to be 1,000, 400, and 600 mgd (million gallons per day) respectively. Pumpage in the county was estimated to be about 4 mgd in 1959, and about half of this amount was used for public supplies.</p>\n<p>A pumping test of a well in outwash deposits near Waupaca indicated that at that point the coefficient of transmissibility is about 100,000 gpd (gallons per day) per ft, the permeability is about 1,000 gpd per sq ft, the coefficient of storage is about 0.2, and the specific capacity is 41 gpm (gallons per minute) per ft of drawdown. These hydraulic characteristics are probably in the same order of magnitude as the characteristics of outwash deposits in the county in general.</p>\n<p>The water from wells in Waupaca County, although hard and generally containing iron, is good for most purposes.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1962","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1669U","collaboration":"Prepared in cooperation with the Wisconsin Geological and Natural History Survey, University of Wisconsin","usgsCitation":"Berkstresser, C., 1964, Ground-water resources of Waupaca County, Wisconsin: U.S. Geological Survey Water Supply Paper 1669, Report: iv, 38 p.; 7 Plates: 32.00 x 34.06 inches or smaller, https://doi.org/10.3133/wsp1669U.","productDescription":"Report: iv, 38 p.; 7 Plates: 32.00 x 34.06 inches or smaller","numberOfPages":"42","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":137935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1669u/report-thumb.jpg"},{"id":25641,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25642,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25643,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25644,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25645,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25646,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25647,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1669u/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25648,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1669u/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Waupaca County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.6062,44.5903],[-88.6152,44.5903],[-88.7371,44.5906],[-88.7368,44.5021],[-88.7365,44.4164],[-88.7381,44.3307],[-88.7397,44.2432],[-88.7658,44.2434],[-88.8609,44.2425],[-88.8871,44.2426],[-88.9821,44.243],[-89.007,44.2426],[-89.104,44.243],[-89.1288,44.243],[-89.2245,44.2433],[-89.2242,44.3308],[-89.2238,44.4174],[-89.2235,44.504],[-89.2231,44.5916],[-89.2234,44.6814],[-88.982,44.6798],[-88.8587,44.6797],[-88.7367,44.6791],[-88.6051,44.6783],[-88.6062,44.5903]]]},\"properties\":{\"name\":\"Waupaca\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d523","contributors":{"authors":[{"text":"Berkstresser, Charles F.","contributorId":33697,"corporation":false,"usgs":true,"family":"Berkstresser","given":"Charles F.","affiliations":[],"preferred":false,"id":143042,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2821,"text":"wsp1779M - 1964 - Historical floods in New England","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1779M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1779","chapter":"M","title":"Historical floods in New England","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey ;","doi":"10.3133/wsp1779M","isbn":"pbk","usgsCitation":"Thomson, M., Cannon, W., Thomas, M.P., and Hayes, S., 1964, Historical floods in New England: U.S. Geological Survey Water Supply Paper 1779, iv, 105 p. ;24 cm., https://doi.org/10.3133/wsp1779M.","productDescription":"iv, 105 p. ;24 cm.","costCenters":[],"links":[{"id":138741,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779m/report-thumb.jpg"},{"id":29379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62eac3","contributors":{"authors":[{"text":"Thomson, M.T.","contributorId":99961,"corporation":false,"usgs":true,"family":"Thomson","given":"M.T.","email":"","affiliations":[],"preferred":false,"id":145854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cannon, W.B.","contributorId":45695,"corporation":false,"usgs":true,"family":"Cannon","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":145852,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, M. P.","contributorId":62574,"corporation":false,"usgs":true,"family":"Thomas","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":145853,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hayes, S.S.","contributorId":33303,"corporation":false,"usgs":true,"family":"Hayes","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":145851,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1845,"text":"wsp1700 - 1964 - Geochemistry of natural waters of the Blue Grass region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1700","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1700","title":"Geochemistry of natural waters of the Blue Grass region, Kentucky","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1700","usgsCitation":"Hendrickson, G.E., and Krieger, R.A., 1964, Geochemistry of natural waters of the Blue Grass region, Kentucky: U.S. Geological Survey Water Supply Paper 1700, vii, 135 p. :illus., maps (1 col.) diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1700.","productDescription":"vii, 135 p. :illus., maps (1 col.) diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":138527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1700/report-thumb.jpg"},{"id":27059,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1700/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27060,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1700/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27051,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1700/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27052,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1700/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27053,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1700/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27054,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1700/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27055,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1700/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27056,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1700/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27057,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1700/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27058,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1700/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a72c","contributors":{"authors":[{"text":"Hendrickson, G. E.","contributorId":99958,"corporation":false,"usgs":true,"family":"Hendrickson","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krieger, Robert A.","contributorId":99954,"corporation":false,"usgs":true,"family":"Krieger","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144243,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1952,"text":"wsp1689 - 1964 - Magnitude and frequency of floods in the United States: Part 14. Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2022-01-25T21:53:44.628933","indexId":"wsp1689","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1689","title":"Magnitude and frequency of floods in the United States: Part 14. Pacific slope basins in Oregon and lower Columbia River basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1689","usgsCitation":"Hulsing, H., and Kallio, N.A., 1964, Magnitude and frequency of floods in the United States: Part 14. Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1689, Report: xiii, 319 p.; 5 Plates: 11.00 × 22.25 inches or smaller, https://doi.org/10.3133/wsp1689.","productDescription":"Report: xiii, 319 p.; 5 Plates: 11.00 × 22.25 inches or smaller","costCenters":[],"links":[{"id":394846,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24898.htm"},{"id":27292,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1689/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27291,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27290,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27289,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27288,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27287,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1689/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138533,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1689/report-thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"lower Columbia River basin, Pacific slope basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -124.564,\n              42\n            ],\n            [\n              -118,\n              42\n            ],\n            [\n              -118,\n              46.667\n            ],\n            [\n              -124.564,\n              46.667\n            ],\n            [\n              -124.564,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649599","contributors":{"authors":[{"text":"Hulsing, Harry","contributorId":62200,"corporation":false,"usgs":true,"family":"Hulsing","given":"Harry","email":"","affiliations":[],"preferred":false,"id":144425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kallio, N. A.","contributorId":42833,"corporation":false,"usgs":true,"family":"Kallio","given":"N.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144424,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":57732,"text":"ofr64169 - 1964 - Ground-water levels in observation wells in Oklahoma, 1961-62","interactions":[],"lastModifiedDate":"2018-11-16T09:34:27","indexId":"ofr64169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-169","title":"Ground-water levels in observation wells in Oklahoma, 1961-62","docAbstract":"<p>The investigation of the ground-water resources of Oklahoma by the U. S. Geological Survey in cooperation with the Oklahoma Water Resources Board includes a continuing program to collect records of water levels in selected observation wells on a systematic basis. These water-level records: (1) provide an index to available ground-water supplies; (2) facilitate the prediction of trends in water levels that will indicate likely changes in storage; (3) aid in the prediction of the base flow of streams; (4) provide information for use in basic research; (5) provide long-term continuous records of fluctuations of water levels in representative wells; and (6) serve as a framework to which other types of hydrologic data may be related.</p><p>Prior to 1956, measurements of water levels in observation wells in Oklahoma were included in water-supply papers published annually by the U. S. Geological Survey (table 1). Beginning with the 1956 calendar year, however, Geological Survey water-level reports will contain only records of a selected network of observation wells, and will be published at 5-year intervals. The first of this series, for the 1956-59 period, was published in 1962.</p><p>This report has been prepared primarily to present water-level records of wells not included in the Federal network. However, for the sake of completeness it includes water-level records of Federal wells that either have been or will be published in Water-Supply Papers since 1955. This report, which contains water-level records for the 2-year period (1961-62), is the second of a series presenting water-level records for all permanent observation wells in Oklahoma. 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