{"pageNumber":"6695","pageRowStart":"167350","pageSize":"25","recordCount":184617,"records":[{"id":1013637,"text":"1013637 - 1964 - Crystal formation in furunculosis agar","interactions":[],"lastModifiedDate":"2016-01-06T08:47:02","indexId":"1013637","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Crystal formation in furunculosis agar","docAbstract":"<p>SINCE ITS&nbsp;INTRODUCTION SOME MONTHS AGO, FURUNCULOSIS AGAR has been employed in the diagnosis of suspect furunculosis and also as a general purpose medium. During our work with this medium we have noticed discrete \"colonies,\" of crystalline material, which very closely resemble microbial colonies. These crystal colonies are compact and appear on both the surface and subsurface; they occur in inoculated slants and plates incubated for long periods (2 to 3 weeks), as well as in uninoculated stored medium. As the crystal colonies could be confusing to workers using this medium, we decided to attempt to identify them and also to determine whether storage conditions and different lots of medium affect crystal formation.</p>","language":"English","publisher":"Bureau of Fisheries, U.S. Department of Commerce","doi":"10.1577/1548-8659(1964)26[25:CFIFA]2.0.CO;2","usgsCitation":"Bullock, G.L., and Ross, A.J., 1964, Crystal formation in furunculosis agar: Progressive Fish-Culturist, v. 26, no. 1, p. 25-26, https://doi.org/10.1577/1548-8659(1964)26[25:CFIFA]2.0.CO;2.","productDescription":"2 p.","startPage":"25","endPage":"26","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true},{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":132302,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ecbc","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":318931,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ross, A. J.","contributorId":105267,"corporation":false,"usgs":true,"family":"Ross","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":318932,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1014052,"text":"1014052 - 1964 - Pseudomonadales as fish pathogens","interactions":[],"lastModifiedDate":"2012-02-02T00:04:22","indexId":"1014052","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1385,"text":"Developments in Industrial Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Pseudomonadales as fish pathogens","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Developments in Industrial Microbiology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"143a/FH","usgsCitation":"Bullock, G.L., 1964, Pseudomonadales as fish pathogens: Developments in Industrial Microbiology, v. 5, p. 101-108.","productDescription":"p. 101-108","startPage":"101","endPage":"108","numberOfPages":"8","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131457,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db651509","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":85343,"text":"85343 - 1964 - Adventuresome waterfowl","interactions":[],"lastModifiedDate":"2012-02-02T00:04:03","indexId":"85343","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Adventuresome waterfowl","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Waterfowl tomorrow","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","publisherLocation":"Washington, DC","usgsCitation":"Mendall, H.L., and Nelson, H., 1964, Adventuresome waterfowl, chap. <i>of</i> Waterfowl tomorrow, p. 305-311 [770 pp.].","productDescription":"p. 305-311 [770 pp.]","costCenters":[{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":128709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698ec3","contributors":{"editors":[{"text":"Linduska, J.P.","contributorId":64308,"corporation":false,"usgs":true,"family":"Linduska","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":504426,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Mendall, H. L.","contributorId":29352,"corporation":false,"usgs":true,"family":"Mendall","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":295936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, H.K.","contributorId":21489,"corporation":false,"usgs":true,"family":"Nelson","given":"H.K.","email":"","affiliations":[],"preferred":false,"id":295935,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000316,"text":"1000316 - 1964 - Age, growth, sex ratio, and maturity of the whitefish in central Green Bay and adjacent waters of Lake Michigan","interactions":[],"lastModifiedDate":"2016-02-25T15:28:23","indexId":"1000316","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1664,"text":"Fishery Bulletin of the U.S. Fish and Wildlife Service","active":true,"publicationSubtype":{"id":10}},"title":"Age, growth, sex ratio, and maturity of the whitefish in central Green Bay and adjacent waters of Lake Michigan","docAbstract":"<p>This study is based on 1,023 whitefish, Coregonus clupeaformis (Mitchill)--819 in seven samples from five localitites in central Green Bay in 1948-49 and 1851-52 and 204 in a single 1948 collection from northwestern Lake Michigan proper. Records of age indicated unusual strength for only one year class--1943 which strongly dominated the 1948 sample from Lake Michigan and the 1949 sample from Green Bay and was well represented in the 1948 collection from green Bay. Collection of 1951-52 without exception were dominated by age group III. Length distributions of samples varied widely according to the age composition. Among fish more than 2 years old, the length distributions of age groups overlapped broadly. Several 1-inch intervals included fish of four age groups. The length-weight relation varied considerably among central Green Bay samples, but differences among localitites were nearly equalled by the year-to-year difference at a single locality. Lake Michigan whitefish were generally lighter than those from Green Bay. Weight increased to the 3.386 power of length in Green Bay (combined samples) and the 3.359 power in Lake Michigan. Growth in length, calculated by direct proportion from diameter measurements of growth fields on scales, differed among localities in central Green Bay and between samples of different years at a single locality. If permanent locality differences exist they are not large and can be obscured by the evident annual fluctuations of growth. The grand average calculated length of Green Bay whitefish (combined collections) exceeded that of Lake Michigan fish in all years of life. The advantage was greatest (2.2 inches) at 3 years (calculated lengths of 16.0 inches and 13.8 inches) and subsequently declined to 0.5 inch at 9 years (lengths of 24.6 and 24.1 inches). Both groups reached the minimum legal length of 17 inches during the fourth growing season. Green Bay whitefish also had the larger calculated weights. The advantage reached 9.3 ounces in 3 years (calculated weights of 22.4 and 13.1 ounces). In years of life 4-9, the weight advantage over Lake Michigan fish ranged from 8.7 ounces, (seventh year; weights of 74.4 and 65.7 ounces) to 12.2 ounces (ninth year; weights of 96.2 and 84.0 ounces). Comparison of growth of whitefish at four localities in northern Lake Michigan indicates that fastest growth is in central Green Bay and slowest near the Fox Islands. Growth is intermediate and similar in northwestern Lake Michigan proper and sorthern Green Bay. Youngest mature male whitefish in green Bay belonged to age group II and youngest mature females to age group III. All IV-group fish were mature. Shortest mature males were at 14.5-14.9 inches and shortest mature females at 16.5-16.9 inches. All males longer than 17.9 inches and all females longer than 18.4 inches were mature.</p>","language":"English","usgsCitation":"Mraz, D., 1964, Age, growth, sex ratio, and maturity of the whitefish in central Green Bay and adjacent waters of Lake Michigan: Fishery Bulletin of the U.S. Fish and Wildlife Service, v. 63, no. 3, p. 619-634.","productDescription":"16 p.","startPage":"619","endPage":"634","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"63","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db68925b","contributors":{"authors":[{"text":"Mraz, Donald","contributorId":21502,"corporation":false,"usgs":true,"family":"Mraz","given":"Donald","email":"","affiliations":[],"preferred":false,"id":308379,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014137,"text":"1014137 - 1964 - Remarks on some facets of epizootiology of bacterial fish diseases","interactions":[],"lastModifiedDate":"2012-02-02T00:04:30","indexId":"1014137","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1385,"text":"Developments in Industrial Microbiology","active":true,"publicationSubtype":{"id":10}},"title":"Remarks on some facets of epizootiology of bacterial fish diseases","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Developments in Industrial Microbiology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"143b/FH","usgsCitation":"Snieszko, S.F., 1964, Remarks on some facets of epizootiology of bacterial fish diseases: Developments in Industrial Microbiology, v. 5, p. 97-100.","productDescription":"p. 97-100","startPage":"97","endPage":"100","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634432","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319851,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014138,"text":"1014138 - 1964 - Selected topics on bacterial fish diseases","interactions":[],"lastModifiedDate":"2012-02-02T00:04:30","indexId":"1014138","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1164,"text":"Canadian Fish Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Selected topics on bacterial fish diseases","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Canadian Fish Culturist","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"144/FH","usgsCitation":"Snieszko, S.F., 1964, Selected topics on bacterial fish diseases: Canadian Fish Culturist, v. 32, p. 19-24.","productDescription":"p. 19-24","startPage":"19","endPage":"24","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132254,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a01e4b07f02db5f8004","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":81404,"text":"81404 - 1964 - Parasites of freshwater fishes IV, Miscellaneous, The anchor worm (Lernaea cyprinacea) and related species","interactions":[],"lastModifiedDate":"2012-02-02T00:15:00","indexId":"81404","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"575","title":"Parasites of freshwater fishes IV, Miscellaneous, The anchor worm (Lernaea cyprinacea) and related species","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"703/FH","usgsCitation":"Putz, R., and Bowen, J., 1964, Parasites of freshwater fishes IV, Miscellaneous, The anchor worm (Lernaea cyprinacea) and related species: Fishery Leaflet 575, 4 p.","productDescription":"4 p.","startPage":"0","endPage":"4","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":199058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689237","contributors":{"authors":[{"text":"Putz, R.E.","contributorId":42543,"corporation":false,"usgs":true,"family":"Putz","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":295330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowen, J.T.","contributorId":67946,"corporation":false,"usgs":true,"family":"Bowen","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":295331,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":81393,"text":"81393 - 1964 - Basic list of publications in English on fish diseases and parasites","interactions":[],"lastModifiedDate":"2012-02-02T00:14:59","indexId":"81393","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"570","title":"Basic list of publications in English on fish diseases and parasites","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"670/FH","usgsCitation":"Snieszko, S.F., Hoffman, G.L., and Wolf, K., 1964, Basic list of publications in English on fish diseases and parasites: Fishery Leaflet 570, 4 p.","productDescription":"4 p.","startPage":"0","endPage":"4","numberOfPages":"4","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":92143,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015005852226?urlappend=%3Bseq=261"},{"id":199053,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485f2","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":295324,"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":295326,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":295325,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175640,"text":"70175640 - 1964 - Records of precipitation, aquifer head, and ground-water recharge to the Edwards and associated limestones, San Antonio area, Texas, 1963","interactions":[],"lastModifiedDate":"2016-08-17T14:12:09","indexId":"70175640","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"6","title":"Records of precipitation, aquifer head, and ground-water recharge to the Edwards and associated limestones, San Antonio area, Texas, 1963","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Garza, S., 1964, Records of precipitation, aquifer head, and ground-water recharge to the Edwards and associated limestones, San Antonio area, Texas, 1963: Edwards Underground Water District Bulletin 6, 7 p.","productDescription":"7 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326726,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58b56e4b03bcb0104bc3f","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":645907,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2233,"text":"wsp1779C - 1964 - Chemical quality of surface water in the West Branch Susquehanna River basin, Pennsylvania","interactions":[],"lastModifiedDate":"2023-03-22T18:45:31.751873","indexId":"wsp1779C","displayToPublicDate":"1964-01-01T00:00:00","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":"C","title":"Chemical quality of surface water in the West Branch Susquehanna River basin, Pennsylvania","docAbstract":"<p>The West Branch Susquehanna River is 228 miles long and drains 6,913 square miles of mountainous area in central Pennsylvania. Much of this area is forestcovered wilderness, part of which is reserved as State game land. Wild animals, such as deer, bear, turkey and grouse, are sheltered there, and many streams contain trout and other game fish. This helps to make the region one of the best hunting and fishing areas in Pennsylvania. The Congress has approved Federal funds for the construction of several reservoirs to prevent flooding of the main river and several of its tributaries. Water stored behind the dams will not be withdrawn below a minimum level designated as conservation pools. These pools will be available for recreation. Several headwater streams, such as Clearfield, Moshannon, and at times Sinnemahoning Creek, that carry drainage from coal mines are acid and contain high concentrations of dissolved solids, especially sulfates. These streams acidify the West Branch Susquehanna River downstream as far as Jersey Shore. One of the most influential tributaries affecting the quality of the West Branch Susquehanna River after they merge is Bald Eagle Creek. Bald Eagle Creek enters the main river downstream from Lock Haven which is approximately 100 river miles from the river's source. Because of its alkaline properties, water of Bald Eagle Creek can neutralize acidic water. Many streams draining small areas and several draining large areas such as Pine Creek, Lycoming Creek, and Loyalsock Creek are clear nearly neutral water low in dissolved solids whose pH is about 7.0 most of the time. These streams have a diluting and neutralizing effect on the quality of the West Branch Susquehanna River, so that from Williamsport downstream the river water is rarely acid, and for most of the time it is of good chemical quality.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1779C","usgsCitation":"McCarren, E.F., 1964, Chemical quality of surface water in the West Branch Susquehanna River basin, Pennsylvania: U.S. Geological Survey Water Supply Paper 1779, Report; iv, 40 p.; 1 Plate: 21.00 x 16.62 inches, https://doi.org/10.3133/wsp1779C.","productDescription":"Report; iv, 40 p.; 1 Plate: 21.00 x 16.62 inches","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":27992,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414560,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24956.htm","linkFileType":{"id":5,"text":"html"}},{"id":27991,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137748,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779c/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Susquehanna River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -78.667,\n              41.75\n            ],\n            [\n              -78.667,\n              40.583\n            ],\n            [\n              -76.25,\n              40.583\n            ],\n            [\n              -76.25,\n              41.75\n            ],\n            [\n              -78.667,\n              41.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3b11","contributors":{"authors":[{"text":"McCarren, Edward F.","contributorId":106472,"corporation":false,"usgs":true,"family":"McCarren","given":"Edward","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144863,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2511,"text":"wsp1768 - 1964 - Hydrology of the Babylon-Islip area, Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2023-03-14T20:23:08.28216","indexId":"wsp1768","displayToPublicDate":"1964-01-01T00:00:00","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":"1768","title":"Hydrology of the Babylon-Islip area, Suffolk County, Long Island, New York","docAbstract":"The report area comprises 270 square miles, and includes most of the Towns of Babylon and Islip, and parts of the Towns of Huntington, Smithtown, and Brookhaven, in southwestern Suffolk County, New York. \r\n\r\nAlmost all the water used in the area is obtained from wells screened in permeable zones of the ground-water reservoir which consists of unconsolidated deposits of gravel, sand, silt, and clay as much as 1,800 feet thick. The ground-water reservoir contains three principal aquifers. From the surface down these are (a) surficial deposits of sand and gravel of Pleistocene age, (b) sands of the Magothy (?) Formation of Cretaceous age, and (c) the Lloyd Sand Member of the Raritan Formation of Cretaceous age. At present only the upper two aquifers are tapped by wells. Natural replenishment of the ground-water reservoir in the area takes place entirely by infiltration of precipitation and averages about 215 mgd (million gallons per day). Average ground-water runoff to streams above tidewater is 114 mgd, and it is estimated that an additional 54 mgd is discharged into tidal reaches of streams. Ground-water evapotranspiration is computed to be about 10 mgd and submarine outflow from the area is estimated to be 18 mgd. The average streamflow of the area above tidewater is 120 mgd. Because of the permeable soils and low relief, direct runoff is only about 5 percent of the average streamflow. Streams are perennial along their middle and lower reaches and exhibit well-sustained low flows. Flooding rarely occurs although continued urbanization may result in minor flooding problems as additional storm sewers are constructed. \r\n\r\nWater in most of the area is generally of good quality; however, it may be contaminated locally. Some streams and parts of the water-table aquifer contain low concentrations of synthetic detergents and other dissolved constituents from domestic and industrial wastes. Salty water occurs in parts of the water-table aquifer in the area under and bordering Great South Bay and under the barrier beaches. Present information, however, indicates that submarine outflow in the artesian aquifers is sufficient to maintain the fresh water-salt water interface some distance seaward of the barrier beaches. \r\n\r\nGround-water withdrawals in 1960 averaged 39 mgd, most of which was returned to the ground through cesspools, leaching beds, and recharge wells; pumpage did not appreciably affect the natural water balance of the groundwater reservoir. If withdrawals continue to be artificially recharged, pumpage can be increased at least fivefold before consumptive losses materially reduce ground-water levels. However, if the area were completely sewered in the future, an adequate supply of ground water for a substantially increased population could not be obtained without (a) reducing the amount of ground water in storage in the reservoir or (b) recharging treated-sewage effluent.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1768","usgsCitation":"Pluhowski, E.J., and Kantrowitz, I.H., 1964, Hydrology of the Babylon-Islip area, Suffolk County, Long Island, New York: U.S. Geological Survey Water Supply Paper 1768, Report: v, 119 p.; 8 Plates: 30.00 x 32.00 inches or smaller, https://doi.org/10.3133/wsp1768.","productDescription":"Report: v, 119 p.; 8 Plates: 30.00 x 32.00 inches or smaller","costCenters":[],"links":[{"id":28672,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1768/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28671,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28670,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28669,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28668,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28667,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28666,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28665,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28664,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1768/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138711,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1768/report-thumb.jpg"},{"id":414130,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24946.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"New York","county":"Suffolk County","otherGeospatial":"Babylon-Islip area, Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.479,\n              40.883\n            ],\n            [\n              -73.479,\n              40.604\n            ],\n            [\n              -73,\n              40.604\n            ],\n            [\n              -73,\n              40.883\n            ],\n            [\n              -73.479,\n              40.883\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601ef4","contributors":{"authors":[{"text":"Pluhowski, Edward J.","contributorId":87911,"corporation":false,"usgs":true,"family":"Pluhowski","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145316,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kantrowitz, Irwin H.","contributorId":93472,"corporation":false,"usgs":true,"family":"Kantrowitz","given":"Irwin","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145317,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185667,"text":"70185667 - 1964 - [Book review] Politics and water resources","interactions":[],"lastModifiedDate":"2017-03-27T12:55:04","indexId":"70185667","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"[Book review] Politics and water resources","docAbstract":"<p>Arizona is a state in which development has proceeded sufficiently rapidly relative to the available water supply that its water problems are as acute as those of nearly any other state in the Union. Owing to the fact that, in the past, the principal use of water was for irrigation, and that the areas where the water has been utilized were geographically separated from the mountain zones where the water originated, surface water resources were developed fairly early in the state’s history.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.144.3617.402-b","usgsCitation":"Leopold, L.B., 1964, [Book review] Politics and water resources: Science, v. 144, no. 3617, p. 402-403, https://doi.org/10.1126/science.144.3617.402-b.","productDescription":"2 p.","startPage":"402","endPage":"403","costCenters":[],"links":[{"id":338376,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","volume":"144","issue":"3617","publicComments":"This is a review of \"<u>The Politics of Water in Arizona</u>. Dean E. Mann. University of Arizona Press, Tucson, 1963. xviii + 317 pp. Illus.\"","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da2540e4b0543bf7fda881","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2353,"text":"wsp1600 - 1964 - Geology and ground-water conditions of Clark County, Washington, with a description of a major alluvial aquifer along the Columbia River","interactions":[],"lastModifiedDate":"2023-03-23T21:07:44.77317","indexId":"wsp1600","displayToPublicDate":"1964-01-01T00:00:00","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":"1600","title":"Geology and ground-water conditions of Clark County, Washington, with a description of a major alluvial aquifer along the Columbia River","docAbstract":"<p>This report presents the results of an investigation of the ground-water resources of the populated parts of Clark County. Yields adequate for irrigation can be obtained from wells inmost farmed areas in Clark County, Wash. The total available supply is sufficient for all foreseeable irrigation developments. In a few local areas aquifers are fine-grained, and yields of individual wells are low. An enormous ground-water supply is available from a major alluvial aquifer underlying the flood plain of the Columbia River in the vicinity of Vancouver, Camas, and Washougal, where the aquifer is recharged, in part, by infiltration from the river. Yields of individual wells are large, ranging to as much as 4,000 gpm (gallons per minute). Clark County lies along the western flank of the Cascade Range. in the structural lowland (Willamette-Puget trough) between those mountains and the Coast Ranges to the west. The area covered by the report includes the urban, the suburban, and most of the agricultural lands in the county. These lands lie on a Series of nearly fiat plains and benches which rise steplike from the level of the Columbia River (a few feet above sea level) to about 800 feet above sea level. Clark County is-drained by the Columbia River (the trunk stream of the Pacific Northwest) and its tributaries. The Columbia River forms the southern and western boundaries of the county. Although the climate of the county is considered to be humid, the precipitation ranging from about 37 to more than 110 inches annually in various parts of the county, the unequal seasonal distribution (about 1.5 inches total for ;July and August in the agricultural area) makes irrigation highly desirable for most .crops and essential for some specialized crops. Consolidated rocks of Eocene to Miocene age, chiefly volcanic lava flows and pyroclastics but including some sedimentary strata, crop out in the foothills of the Cascades in the eastern part of the county and underlie the younger, unconsolidated rocks in the lowlands to the west At most places small to moderate quantities of water can be obtained from fractures in the older consolidated rocks. However, in the populated parts of the county, these rocks generally are overlain by considerable thicknesses of more permeable materials, and few wells have been drilled in them. Springs and dug wells yield an ample domestic supply at a number of outlying farms in the foothills. The younger (Pliocene to Recent) unconsolidated materials were deposited chiefly by streams in the basin formed by downwarping of the older rocks. However, some lake deposits and glacial drift also are included. The oldest unit of this group, the lower member of the Troutdale formation of Pliocene age, consists chiefly of clay, silt, and fine sand but includes lenses of coarser sand and, rarely, gravel. The maximum known thickness of the lower member of the Troutdale formation is about 660 feet. This unit is not a good aquifer because most of the strata are fine grained. However, at a few places drilled wells have penetrated lenses of coarser grained materials in these deposits and have obtained small to moderate amounts of water from them. The upper member of the Troutdale formation consists almost entirely of lightly to moderately cemented gravel, of which the most striking feature is the presence of a considerable percentage of quartzite pebbles. The average thickness of the upper member of the Troutdale may originally have been 300 to 400 feet. The member crops out over considerable areas in the county and, where conditions of topography and exposure are optimum, has beer very deeply weathered. It is suggested that the upper member of the Troutdale formation may prove to be of early Pleistocene age.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1600","usgsCitation":"Mundorff, M.J., 1964, Geology and ground-water conditions of Clark County, Washington, with a description of a major alluvial aquifer along the Columbia River: U.S. Geological Survey Water Supply Paper 1600, Report: vi, 268 p.; 3 Plates: 35.00 x 50.19 inches or smaller, https://doi.org/10.3133/wsp1600.","productDescription":"Report: vi, 268 p.; 3 Plates: 35.00 x 50.19 inches or smaller","costCenters":[],"links":[{"id":28281,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1600/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28280,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1600/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28279,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1600/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414663,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24789.htm","linkFileType":{"id":5,"text":"html"}},{"id":28282,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1600/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137781,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1600/report-thumb.jpg"}],"country":"United States","state":"Washington","county":"Clark 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Maurice John","contributorId":41404,"corporation":false,"usgs":true,"family":"Mundorff","given":"Maurice","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":145066,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2970,"text":"wsp1698 - 1964 - Ground-water resources and geology of northern and western Crook County, Wyoming, with a section on the chemical quality of the ground water","interactions":[],"lastModifiedDate":"2026-01-23T16:42:24.706514","indexId":"wsp1698","displayToPublicDate":"1964-01-01T00:00:00","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":"1698","title":"Ground-water resources and geology of northern and western Crook County, Wyoming, with a section on the chemical quality of the ground water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1698","usgsCitation":"Whitcomb, H.A., Morris, D.A., and Langford, R.H., 1964, Ground-water resources and geology of northern and western Crook County, Wyoming, with a section on the chemical quality of the ground water: U.S. Geological Survey Water Supply Paper 1698, Report: v, 92 p.; 2 Plates: 22.50 x 17.50 inches and 39.00 x 41.50 inches, https://doi.org/10.3133/wsp1698.","productDescription":"Report: v, 92 p.; 2 Plates: 22.50 x 17.50 inches and 39.00 x 41.50 inches","costCenters":[],"links":[{"id":422302,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24903.htm","linkFileType":{"id":5,"text":"html"}},{"id":29706,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1698/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29705,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1698/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29707,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1698/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139274,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1698/report-thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Crook County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.05869314135387,\n              44.680054743731034\n            ],\n            [\n              -104.05486809016973,\n              44.99604278399539\n            ],\n            [\n              -105.08954443542197,\n              44.99604278399539\n            ],\n            [\n              -105.09145696101382,\n              44.87961376782616\n            ],\n            [\n              -105.07615675627818,\n              44.878258553546004\n            ],\n            [\n              -105.07424423068589,\n              44.78874383711761\n            ],\n            [\n              -105.08954443542197,\n              44.7860290994428\n            ],\n            [\n              -105.08380536354262,\n              44.17608275825614\n            ],\n            [\n              -104.48900990444203,\n              44.178826027141696\n            ],\n            [\n              -104.52726041628155,\n              44.67189518750155\n            ],\n            [\n              -104.05869314135387,\n              44.680054743731034\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db666fe3","contributors":{"authors":[{"text":"Whitcomb, Harold A.","contributorId":102868,"corporation":false,"usgs":true,"family":"Whitcomb","given":"Harold","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146068,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morris, D. A.","contributorId":56204,"corporation":false,"usgs":true,"family":"Morris","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146067,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langford, Russell H.","contributorId":48950,"corporation":false,"usgs":true,"family":"Langford","given":"Russell","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":887270,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","interactions":[{"subject":{"id":33633,"text":"b1160D - 1964 - A microfauna from the Coker formation, Alabama","indexId":"b1160D","publicationYear":"1964","noYear":false,"chapter":"D","title":"A microfauna from the Coker formation, Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":1},{"subject":{"id":33769,"text":"b1160B - 1964 - Petrology of pre-Selma strata from core holes in western Alabama","indexId":"b1160B","publicationYear":"1964","noYear":false,"chapter":"B","title":"Petrology of pre-Selma strata from core holes in western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":2},{"subject":{"id":34057,"text":"b1160F - 1964 - General remarks on the pre-Selma Cretaceous strata of western Alabama","indexId":"b1160F","publicationYear":"1964","noYear":false,"chapter":"F","title":"General remarks on the pre-Selma Cretaceous strata of western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":3},{"subject":{"id":34940,"text":"b1160E - 1964 - A preliminary report on the pollen and spores of the pre-Selma Upper Cretaceous strata of western Alabama","indexId":"b1160E","publicationYear":"1964","noYear":false,"chapter":"E","title":"A preliminary report on the pollen and spores of the pre-Selma Upper Cretaceous strata of western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":4},{"subject":{"id":35282,"text":"b1160A - 1964 - General description of cores of pre-Selma Cretaceous strata in western Alabama","indexId":"b1160A","publicationYear":"1964","noYear":false,"chapter":"A","title":"General description of cores of pre-Selma Cretaceous strata in western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":5},{"subject":{"id":35920,"text":"b1160C - 1964 - Pre-Selma larger invertebrate fossils from well core samples in western Alabama","indexId":"b1160C","publicationYear":"1964","noYear":false,"chapter":"C","title":"Pre-Selma larger invertebrate fossils from well core samples in western Alabama"},"predicate":"IS_PART_OF","object":{"id":70168893,"text":"b1160 - 1964 - Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","indexId":"b1160","publicationYear":"1964","noYear":false,"title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama"},"id":6}],"lastModifiedDate":"2016-03-07T13:39:25","indexId":"b1160","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1160","title":"Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama","docAbstract":"<p>In 1954 four core holes were drilled in the pre-Selma Cretaceous strata of the Alabama Coastal Plain in order to get unweathered samples within a few miles of the outcrops. During the next few years several specialists studied the cores, and their reports are published as consecutive parts of this bulletin.</p>\n<p>Watson H. Monroe, who spent many years studying the Coastal Plain strata in Alabama and Mississippi, conceived and supervised the drilling and planned the later studies. His earlier published report (W. H. Monroe, 1955, Cores of pre-Selma Cretaceous rocks in the outcrop area in western Alabama: Gulf Coast Geol. Societies Trans., v. 5, p. 11-37) contains a brief description of the stratigraphy, together with logs and other information regarding the core holes, and he has provided the introductory chapter to this bulletin. Richard E. Bergenback studied the petrology of the cores, which included finding the distribution of grain sizes, determining the mineralogy of the grains and the matrix of the sediments, and having X-Ray identifications made of the clay minerals. Norman F. Sohl studied the mollusks and other large fossils obtained from the cores and compared them with other faunal suites collected in Alaban1a and Texas. Esther R. Applin studied the sparse microfauna, comparing it with faunas obtained from deep wells downdip in Georgia, Alabama, and Mississippi and with outcrop samples fron1 Texas, and has described a new species of Foraminifera. Estella B. Leopold and Helen M. Pakiser obtained a large pollen and spore assemblage by digesting carbonaceous layers of some of the cores in acid; this flora includes much new material, which is not described here.</p>\n<p>The Bergenback, Sohl, and Applin reports discuss the probable environment in which the sediments accumulated. Louis C. Conant, who spent several years studying and mapping these sediments, has written a summary chapter integrating some of the surface and subsurface information.</p>\n<p>Quarter-cuts of the cores belonging to the U.S. National Museum have been deposited on indefinite loan with the Alabama Geological Survey at University, Ala., and with the Shell Oil Co. at Jackson, Miss. They are available there for inspection and study.</p>","language":"English","publisher":"U.S. G.P.O.","doi":"10.3133/b1160","usgsCitation":"Monroe, W.H., Bergenback, R.E., Sohl, N.F., Applin, E.R., Leopold, E.B., Pakiser, H.M., and Conant, L.C., 1964, Studies of pre-Selma Cretaceous core samples from the outcrop area in western Alabama: U.S. Geological Survey Bulletin 1160, Report: ix, 108 p.; Plate: 17 x 22.25 inches, https://doi.org/10.3133/b1160.","productDescription":"Report: ix, 108 p.; Plate: 17 x 22.25 inches","numberOfPages":"162","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":318661,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/b1160.jpg"},{"id":318660,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1160a/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":318659,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1160/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56deb472e4b015c306fb8a78","contributors":{"authors":[{"text":"Monroe, Watson Hiner","contributorId":93020,"corporation":false,"usgs":true,"family":"Monroe","given":"Watson","email":"","middleInitial":"Hiner","affiliations":[],"preferred":false,"id":622087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergenback, Richard E.","contributorId":65897,"corporation":false,"usgs":true,"family":"Bergenback","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":622088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sohl, Norman F.","contributorId":27906,"corporation":false,"usgs":true,"family":"Sohl","given":"Norman","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":622089,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Applin, Esther R.","contributorId":40974,"corporation":false,"usgs":true,"family":"Applin","given":"Esther","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":622090,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Leopold, Estella B.","contributorId":30979,"corporation":false,"usgs":true,"family":"Leopold","given":"Estella","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":622091,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pakiser, Helen M.","contributorId":167378,"corporation":false,"usgs":false,"family":"Pakiser","given":"Helen","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":622092,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Conant, Louis C.","contributorId":83921,"corporation":false,"usgs":true,"family":"Conant","given":"Louis","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":622093,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":2404,"text":"wsp1749 - 1964 - Geology and ground-water resources of Nobles County, and part of Jackson County, Minnesota","interactions":[],"lastModifiedDate":"2023-04-11T18:27:13.54031","indexId":"wsp1749","displayToPublicDate":"1964-01-01T00:00:00","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":"1749","title":"Geology and ground-water resources of Nobles County, and part of Jackson County, Minnesota","docAbstract":"<p>The area described in this report is in southwestern Minnesota, about 130 miles southwest of Minneapolis and St. Paul. It includes; Nobles County and the western tier of townships in Jackson County, a total of 864 square miles. Worthington, the Nobles County seat, is the largest city in the area, having a population of 9,015 persons (1960 census). Farming is the leading occupation, and food processing is the major industry. Critical water shortages have occurred in several parts of the area.</p>\n<p>The climate is characterized by mild, subhumid summers and relatively long, severe winters. Mean monthly temperatures range from 15.1 &deg;F in January to 73.3 &deg;F in July. The mean annual precipitation is 26.75 inches.</p>\n<p>The crest of the Coteau des Prairies, a broad highland belt, traverses Nobles County from northwest to southeast. Three glacial end moraines and their associated ground moraines trend south to southeast across the area. Altitudes range from about 1,820 feet on the crest of the coteau in the northwestern part of the area to about 1,390 feet above mean sea level in the Jack and Okabena Creek valleys in the northeast.</p>\n<p>The Mississippi-Missouri River drainage divide crosses the area from north to east. The Gary outer end moraine trends southeast through central Nobles County. East of this moraine the land is poorly drained and contains numerous lakes and swamps; west of this moraine the land is well drained and contains few, if any, undrained depressions.</p>\n<p>Within the area, granite and Sioux Quartzite of Precambrian age are overlain by Cretaceous strata, except locally in the northeast and northwest parts of the area where the quartzite is directly overlain by glacial drift. The Cretaceous strata are composed of interbedded shale, siltstone, and sandstone. The surface of the area is composed of Pleistocene deposits of glacial drift and some thin, patchy deposits of Recent age. Bedrock is not known to crop out in the area. The drift ranges in thickness from about 150 feet in the southwest and northeast corners to about 500 feet on the highest part of the Coteau des Prairies.</p>\n<p>The Precambrian granite is not a source of ground water in this area. The Sioux Quartzite yields moderate supplies in adjacent counties to the north and west, but because of its sporadic occurrence it does not constitute an important water source in this area. The Cretaceous sandstone units are a secondary source of ground water and yield adequate supplies 'to at least 24 farm wells, which range in depth from 283 to 586 feet below land surface.</p>\n<p>The primary source of ground water in the Nobles-Jackson County area is the glacial drift. Buried outwash deposits supply water to 7 of the 10 municipalities and to most of the farms in the area. Two Worthington city wells, completed in a buried outwash deposit underlying East Okabena dry lake bed, were tested for short periods at 500 gallons per minute. The estimated coefficient of transmissibility for the aquifer at one of the wells was 70,000 gpd (gallons per day) per ft.</p>\n<p>The buried outwash deposits may occur anywhere within the drift from about 15 feet below land surface to bedrock which is as much as 500 feet below land surface. The outwash ranges from a fraction of a foot to more than 25 feet in thickness where permeable; below the water table it generally will supply ample quantities of water to properly constructed wells.</p>\n<p>Surflcial outwash deposits fill the valley bottoms and form the terrace deposits associated with the present-day drainage channels. The thicker, more extensive, and continuous deposits occur in the proglacial stream channels that drained the fronts of the ice sheets rather than in those channels that now drain the backs of the moraines. The surflcial outwash deposits generally are made up of sand, gravel and some silt and clay, and range in thickness from 0 to more than 60 feet; they range in width from a few feet in the narrow tributaries to about one mile in the larger stream valleys.</p>\n<p>Four municipalities and many farms obtain part or all of their water supplies from surficial outwash. An Adrian municipal well, completed in this source, was pumped at a rate of 400 gpm. At the confluence of two streams which drain Ocheda Lake in southeastern Nobles County, the sand and gravel section is more than 60 feet thick in places. Results of a pumping test here showed an average coefficient of transmissibility of 150,000 gpd per ft. Coefficients of transmissibility may be as much as 500,000 gdp per ft in the thickest part of the deposit if the permeability of the sand and gravel is uniform.</p>\n<p>Recharge to the surflcial outwash deposits is relatively rapid; it is slower to the buried outwash deposits where the descending water must percolate through till of low permeability before entering the aquifers.</p>\n<p>The quality of water in the Precambrian crystalline rocks, the Cretaceous strata, and the buried Pleistocene aquifers is poor. Chemical analyses of 22 water samples showed that dissolved solids ranged from 1,100 ppm (parts per million) to 3,050 ppm. Water from the surficial outwash deposits is good by comparison; dissolved solids in water from these aquifers ranged from 425 to 870 ppm.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1749","collaboration":"Prepared in cooperation with the Division of Waters, Minnesota Department of Conservation, and the city of Worthington","usgsCitation":"Norvitch, R.F., 1964, Geology and ground-water resources of Nobles County, and part of Jackson County, Minnesota: U.S. Geological Survey Water Supply Paper 1749, Document: iv, 70 p.; 5 Plates: 23.0 x 23.5 inches or smaller, https://doi.org/10.3133/wsp1749.","productDescription":"Document: iv, 70 p.; 5 Plates: 23.0 x 23.5 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":28402,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1749/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28399,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1749/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28404,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1749/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":415582,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24926.htm","linkFileType":{"id":5,"text":"html"}},{"id":28403,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1749/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28400,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1749/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139050,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1749/report-thumb.jpg"},{"id":28401,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1749/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"Jackson County, Nobles County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.051,\n              43.847\n            ],\n            [\n              -96.051,\n              43.5\n            ],\n            [\n              -95.336,\n              43.5\n            ],\n            [\n              -95.336,\n              43.847\n            ],\n            [\n              -96.051,\n              43.847\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685a7f","contributors":{"authors":[{"text":"Norvitch, Ralph F.","contributorId":65456,"corporation":false,"usgs":true,"family":"Norvitch","given":"Ralph","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68480,"text":"ha112 - 1964 - Availability of ground water in the Lynn Grove quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:50:13.724412","indexId":"ha112","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"112","title":"Availability of ground water in the Lynn Grove quadrangle, Kentucky-Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha112","usgsCitation":"Davis, R.W., 1964, Availability of ground water in the Lynn Grove quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 112, 1 Plate: 47.50 x 32.50 inches, https://doi.org/10.3133/ha112.","productDescription":"1 Plate: 47.50 x 32.50 inches","costCenters":[],"links":[{"id":188021,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413586,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15468.htm","linkFileType":{"id":5,"text":"html"}},{"id":90033,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/112/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Lynn Grove quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.5,\n              36.5\n            ],\n            [\n              -88.5,\n              36.625\n            ],\n            [\n              -88.375,\n              36.625\n            ],\n            [\n              -88.375,\n              36.5\n            ],\n            [\n              -88.5,\n              36.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d936","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":278301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":34971,"text":"b1178 - 1964 - Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska","interactions":[{"subject":{"id":14707,"text":"ofr6189 - 1961 - Structure and stratigraphy of the Pybus-Gambier area, Alaska","indexId":"ofr6189","publicationYear":"1961","noYear":false,"title":"Structure and stratigraphy of the Pybus-Gambier area, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":34971,"text":"b1178 - 1964 - Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska","indexId":"b1178","publicationYear":"1964","noYear":false,"title":"Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska"},"id":1}],"lastModifiedDate":"2023-03-17T18:40:35.707136","indexId":"b1178","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1178","title":"Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1178","usgsCitation":"Loney, R.A., 1964, Stratigraphy and petrography of the Pybus-Gambier area, Admiralty Island, Alaska: U.S. Geological Survey Bulletin 1178, Report: vi, 103 p.; 2 Plates: 35.50 x 21.00 inches and 31.50 x 19.25 inches, https://doi.org/10.3133/b1178.","productDescription":"Report: vi, 103 p.; 2 Plates: 35.50 x 21.00 inches and 31.50 x 19.25 inches","costCenters":[],"links":[{"id":109464,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20944.htm","linkFileType":{"id":5,"text":"html"},"description":"20944"},{"id":62920,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1178/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62919,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1178/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62921,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1178/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164863,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1178/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Admiralty Island, Pybus-Gambier area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -134.333,\n              57.5\n            ],\n            [\n              -134.333,\n              57.25\n            ],\n            [\n              -133.667,\n              57.25\n            ],\n            [\n              -133.667,\n              57.5\n            ],\n            [\n              -134.333,\n              57.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b33","contributors":{"authors":[{"text":"Loney, R. A.","contributorId":90757,"corporation":false,"usgs":true,"family":"Loney","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":213911,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1007574,"text":"1007574 - 1964 - 1,1' diacetyl-1,1'-dihydro-4,4' bipyridine and the yellow and colorless modifications of 1,1'-diacetyl-1,1',4,4'-tetrahydro-4,4' bipyridine","interactions":[],"lastModifiedDate":"2013-02-23T21:58:33","indexId":"1007574","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2408,"text":"Journal of Organic Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"1,1' diacetyl-1,1'-dihydro-4,4' bipyridine and the yellow and colorless modifications of 1,1'-diacetyl-1,1',4,4'-tetrahydro-4,4' bipyridine","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Organic Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"American Chemical Society","doi":"10.1021/jo01031a016","usgsCitation":"Nielsen, A., Moore, D.W., Muha, G., and Highberg, K., 1964, 1,1' diacetyl-1,1'-dihydro-4,4' bipyridine and the yellow and colorless modifications of 1,1'-diacetyl-1,1',4,4'-tetrahydro-4,4' bipyridine: Journal of Organic Chemistry, v. 29, no. 8, p. 2175-2179, https://doi.org/10.1021/jo01031a016.","startPage":"2175","endPage":"2179","numberOfPages":"5","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":268064,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1021/jo01031a016"},{"id":130194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"8","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e55e","contributors":{"authors":[{"text":"Nielsen, A.T.","contributorId":62551,"corporation":false,"usgs":true,"family":"Nielsen","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":315650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, D. W.","contributorId":93431,"corporation":false,"usgs":true,"family":"Moore","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":315653,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muha, G.M.","contributorId":78687,"corporation":false,"usgs":true,"family":"Muha","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":315651,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Highberg, K.","contributorId":90673,"corporation":false,"usgs":true,"family":"Highberg","given":"K.","email":"","affiliations":[],"preferred":false,"id":315652,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":81377,"text":"81377 - 1964 - The true pikes","interactions":[],"lastModifiedDate":"2023-04-05T16:44:37.895882","indexId":"81377","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"569","title":"The true pikes","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Karvelis, E.G., 1964, The true pikes: Fishery Leaflet 569, 11 p.","productDescription":"11 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198084,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92142,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://spo.nmfs.noaa.gov/content/true-pikes-0","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db6349a1","contributors":{"authors":[{"text":"Karvelis, Ernest G.","contributorId":55547,"corporation":false,"usgs":true,"family":"Karvelis","given":"Ernest","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":295307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2000008,"text":"2000008 - 1964 - Lake Michigan chemical data, 1954-55, 1960-61","interactions":[],"lastModifiedDate":"2012-02-02T00:14:59","indexId":"2000008","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":17,"text":"Data Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"6","title":"Lake Michigan chemical data, 1954-55, 1960-61","docAbstract":"This report presents without interpretation methods used in and the results of chemical analyses, and supplemental observations of temperatures at depth, transparency, and meteorological conditions for Lake Michigan in 1954, 1955, 1960, and 1961.","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Beeton, A.M., and Moffett, J.W., 1964, Lake Michigan chemical data, 1954-55, 1960-61: Data Report 6, 102 p.","productDescription":"102 p.","startPage":"0","endPage":"102","numberOfPages":"102","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4339","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":324918,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moffett, James W.","contributorId":94245,"corporation":false,"usgs":true,"family":"Moffett","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":324917,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046789,"text":"70046789 - 1964 - Classes of land-surface form in the United States","interactions":[],"lastModifiedDate":"2013-07-08T13:35:00","indexId":"70046789","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Classes of land-surface form in the United States","docAbstract":"This digital dataset describes classes of land-surface form in the conterminous United States.  The source of the data is the map of land-surface form in the 1970 National Atlas of the United States, pages 62-63, which was adapted from Edwin H. Hammond, \"Classes of land surface form in the forty-eight states, U.S.A,\" Annals of the Assoc. of Am. Geographers, v.54, no. 1, 1964, map supp. no. 1, 1:5,000,000.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The national atlas of the United States of America","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70046789","usgsCitation":"Hammond, E., 1964, Classes of land-surface form in the United States (1.0), Datatset, https://doi.org/10.3133/70046789.","productDescription":"Datatset","onlineOnly":"Y","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274677,"type":{"id":16,"text":"Metadata"},"url":"https://water.usgs.gov/GIS/metadata/usgswrd/XML/na70_landfrm.xml"},{"id":274684,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.889969,22.863141 ], [ -127.889969,51.606088 ], [ -65.349827,51.606088 ], [ -65.349827,22.863141 ], [ -127.889969,22.863141 ] ] ] } } ] }","edition":"1.0","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dbdf69e4b0f81004b77ce8","contributors":{"authors":[{"text":"Hammond, Edwin","contributorId":100719,"corporation":false,"usgs":true,"family":"Hammond","given":"Edwin","email":"","affiliations":[],"preferred":false,"id":480257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000274,"text":"1000274 - 1964 - A horizontal sampler for collection of water samples near the bottom","interactions":[],"lastModifiedDate":"2013-01-28T12:31:27","indexId":"1000274","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"A horizontal sampler for collection of water samples near the bottom","docAbstract":"The need to obtain adequate water samples immediately above a lake bottom or at a precisely defined depth is not new. The problem is of particular concern in a large  section  of  central  Lake  Erie, where dissolved oxygen concentration may be reduced to 1 ppm or less in the hypolimnion and where the metalimnion frequently extends to or within 30 or 60 cm of the bottom (Becton 1963; Cam 1962).It is impossible to sample the hypolimnrtic waters satisfactorily with the usual Nanscn, Kemmerer, and Frautschy bottles (Carr 1962). Although the 500-ml sampler described here was designed, constructed, and used extensively and successfully to meet the particular problem in Lake Erie, it should be equally useful in a varirty of situations.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Limnology and Oceanography","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.4319/lo.1964.9.4.0595","collaboration":"Out-of-print","usgsCitation":"Joeris, L.S., 1964, A horizontal sampler for collection of water samples near the bottom: Limnology and Oceanography, v. 9, no. 4, p. 595-598, https://doi.org/10.4319/lo.1964.9.4.0595.","productDescription":"p. 595-598","startPage":"595","endPage":"598","numberOfPages":"3","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266600,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.4319/lo.1964.9.4.0595"}],"volume":"9","issue":"4","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae44c","contributors":{"authors":[{"text":"Joeris, Leonard S.","contributorId":104430,"corporation":false,"usgs":true,"family":"Joeris","given":"Leonard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":308322,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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