{"pageNumber":"5970","pageRowStart":"149225","pageSize":"25","recordCount":165658,"records":[{"id":70009990,"text":"70009990 - 1965 - Glass electrode determination of sodium in closed basin waters","interactions":[],"lastModifiedDate":"2020-11-24T13:25:10.296594","indexId":"70009990","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Glass electrode determination of sodium in closed basin waters","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id6\" class=\"abstract author\"><div id=\"aep-abstract-sec-id7\"><p>Because of its direct relation to total dissolved solids content, sodium concentration is the most useful single hydrochemical parameter of closed basin waters in the western United States. Therefore, it is advantageous to have a rapid method for sodium determination which could be readily adapted to field use. Accordingly, thirty waters of highly variable concentration and anionic composition from the western Great Basin have been analyzed with a sodium-sensitive glass electrode. Na<sup>+</sup><span>&nbsp;</span>values ranged from 10 to 130,000 ppm in waters containing from 102 to 401,000 ppm total dissolved solids. The electrode values were compared with conventional sodium determinations; results differed by as much as 11 per cent, although over two-thirds were within 5 per cent. No significant relation was found between the glass electrode and conventional method differences and the total dissolved solids or sodium concentration. The comparative accuracy of electrode and conventional procedures was checked, employing solutions of known sodium concentration. It was concluded that for the analysis of sodium in natural waters the glass electrode method offers results comparable in accuracy to those obtained by conventional methods, but with increased simplicity, and therefore the possibility of rapid, accurate field measurements.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(65)90066-9","issn":"00167037","usgsCitation":"Truesdell, A., Jones, B., and Van Denburgh, A.S., 1965, Glass electrode determination of sodium in closed basin waters: Geochimica et Cosmochimica Acta, v. 29, no. 6, p. 725-736, https://doi.org/10.1016/0016-7037(65)90066-9.","productDescription":"12 p.","startPage":"725","endPage":"736","numberOfPages":"12","costCenters":[],"links":[{"id":218617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2928e4b0c8380cd5a6f4","contributors":{"authors":[{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":357604,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, B.F.","contributorId":52156,"corporation":false,"usgs":true,"family":"Jones","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":357603,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":357602,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70009989,"text":"70009989 - 1965 - Alkali content of alpine ultramafic rocks","interactions":[],"lastModifiedDate":"2020-11-24T00:39:56.572868","indexId":"70009989","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Alkali content of alpine ultramafic rocks","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"aep-abstract-id5\" class=\"abstract author\"><div id=\"aep-abstract-sec-id6\"><p>The lower limit of abundance of sodium and potassium in ultramafic rocks is less than the threshold amount detectable by conventional analytical methods. By a dilutionaddition modification of the flame-spectrophotometric method, sodium and potassium have been determined in 40 specimens of alpine ultramafic rocks. Samples represent six regions in the United States and one in Australia, and include dunite, peridotite, pyroxenite, and their variably serpentinized and metamorphosed derivatives.</p><p>The median value found for Na<sub>2</sub>O is 0.004 per cent, and the range of Na<sub>2</sub>O is 0.001–0.19. The median value for K<sub>2</sub>O is 0.0034 per cent and the range is 0.001–0.031 per cent. Alkali concentrations are below 0.01 per cent Na<sub>2</sub>O in 28 samples and below 0.01 per cent K<sub>2</sub>O in 35.</p><p>Derivation of basalt magma from upper-mantle material similar to such ultramafic rocks, as has been postulated, is precluded by the relative amounts of sodium and potassium, which are from 200 to 600 times more abundant in basalt than in the ultramafic rocks. Similar factors apply to a number of other elements. No reasonable process could produce such concentrations in, for example, tens of thousands of cubic miles of uniform tholeiitic basalt. The ultramafic rocks might have originated either as magmatic crystal precipitates or as mantle residues left after fusion and removal of basaltic magma. Injection of ultramafic rocks to exposed positions is tectonic rather than magmatic.</p></div></div></div>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(65)90062-1","issn":"00167037","usgsCitation":"Hamilton, W., and Mountjoy, W., 1965, Alkali content of alpine ultramafic rocks: Geochimica et Cosmochimica Acta, v. 29, no. 6, p. 661-671, https://doi.org/10.1016/0016-7037(65)90062-1.","productDescription":"11 p.","startPage":"661","endPage":"671","numberOfPages":"11","costCenters":[],"links":[{"id":218616,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e966e4b0c8380cd48251","contributors":{"authors":[{"text":"Hamilton, W.","contributorId":46683,"corporation":false,"usgs":true,"family":"Hamilton","given":"W.","email":"","affiliations":[],"preferred":false,"id":357600,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mountjoy, W.","contributorId":65122,"corporation":false,"usgs":true,"family":"Mountjoy","given":"W.","email":"","affiliations":[],"preferred":false,"id":357601,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":34683,"text":"b1202B - 1965 - Regional structure of the southeast Missouri and Illinois-Kentucky mineral districts","interactions":[],"lastModifiedDate":"2023-03-16T21:13:14.671067","indexId":"b1202B","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"1202","chapter":"B","title":"Regional structure of the southeast Missouri and Illinois-Kentucky mineral districts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1202B","usgsCitation":"Heyl, A.V., Brock, M.R., Jolly, J.L., and Wells, C.E., 1965, Regional structure of the southeast Missouri and Illinois-Kentucky mineral districts: U.S. Geological Survey Bulletin 1202, Report: iii, 20 p.; 3 Plates: 38.00 x 21.70 inches, https://doi.org/10.3133/b1202B.","productDescription":"Report: iii, 20 p.; 3 Plates: 38.00 x 21.70 inches","costCenters":[],"links":[{"id":414306,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_19254.htm","linkFileType":{"id":5,"text":"html"}},{"id":62553,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1202b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62552,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62551,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62550,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1202b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165873,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1202b/report-thumb.jpg"}],"country":"United States","state":"Illinois, Kentucky, Missouri","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88,\n              39\n            ],\n            [\n              -92,\n              39\n            ],\n            [\n              -92,\n              37\n            ],\n            [\n              -88,\n              37\n            ],\n            [\n              -88,\n              39\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c460","contributors":{"authors":[{"text":"Heyl, Allen Van","contributorId":91078,"corporation":false,"usgs":true,"family":"Heyl","given":"Allen","email":"","middleInitial":"Van","affiliations":[],"preferred":false,"id":213396,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brock, M. R.","contributorId":96230,"corporation":false,"usgs":true,"family":"Brock","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":213398,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jolly, J. L.","contributorId":89200,"corporation":false,"usgs":true,"family":"Jolly","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":213395,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wells, C. E.","contributorId":92729,"corporation":false,"usgs":true,"family":"Wells","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":213397,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1000112,"text":"1000112 - 1965 - Food of lake trout in Lake Superior","interactions":[],"lastModifiedDate":"2016-02-25T11:07:17","indexId":"1000112","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Food of lake trout in Lake Superior","docAbstract":"<p>Stomachs were examined from 1,492 lake trout and 83 siscowets collected from Lake Superior. Data are given on the food of lake trout of legal size (17 inches or longer) by year, season, and depth of water, and on the relation between food and size among smaller lake trout. Fish contributed 96.7 to 99.9 per cent of the total volume of food in the annual samples. Ciscoes (Coregonus spp.) were most common (52.2 to 87.5 per cent of the volume) in 1950 to 1953 and American smelt ranked first (65.6 per cent of the volume) in 1963. Cottids were in 8.9 to 12.3 per cent of the stomachs in 1950 to 1953 but in only 4.3 per cent in 1963. Insects ranked second to fish in occurrence (9.6 per cent for the combined samples) and crustaceans followed at 3.9 per cent. The greatest seasonal changes in the food of lake trout were among fish caught at 35 fathoms and shallower. The occurrence of Coregonus increased from 34.6 per cent in February-March to 71.1 per cent in October-December. Smelt were in 76.9 per cent of the stomachs in February-March but in only 2.2 per cent in October-December. Cottids, Mysis relicta, and insects were most common in the July-September collections. Lake trout taken at depths greater than 35 fathoms had eaten a higher percentage of Cottidae and Coregonus than had those captured in shallower water. Smelt, ninespine sticklebacks, Mysis, and insects were more frequent in stomachs of lake trout from less than 35 fathoms. Crustaceans comprised more than 70 per cent of the total volume of food for 4.0- to 7.9-inch lake trout but their importance decreased as the lake trout grew larger. Pontoporeia affinis was the most common in the stomachs of 4.0- to 6.9-inch lake trout and Mysis held first rank at 7.0 to 12.9 inches. Ostracods were important only to 4.0- to 4.9-inch lake trout. As the lake trout became larger, the importance of fish grew from 4.4-per cent occurrence at 5.0 to 5.9 inches to 93.9 per cent at 16.0 to 16.9 inches. Smelt were most commonly eaten by undersize (less than 17 inches) lake trout.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1965)94[169:FOLTIL]2.0.CO;2","usgsCitation":"Dryer, W.R., Erkkila, L.F., and Tetzloff, C.L., 1965, Food of lake trout in Lake Superior: Transactions of the American Fisheries Society, v. 94, no. 2, p. 169-176, https://doi.org/10.1577/1548-8659(1965)94[169:FOLTIL]2.0.CO;2.","productDescription":"8 p.","startPage":"169","endPage":"176","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":480682,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"http://hdl.handle.net/2027.42/141203","text":"External Repository"},{"id":132749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae686","contributors":{"authors":[{"text":"Dryer, William R.","contributorId":71921,"corporation":false,"usgs":true,"family":"Dryer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erkkila, Leo F.","contributorId":92197,"corporation":false,"usgs":true,"family":"Erkkila","given":"Leo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308096,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tetzloff, Clifford L.","contributorId":84710,"corporation":false,"usgs":true,"family":"Tetzloff","given":"Clifford","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308095,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1000291,"text":"1000291 - 1965 - Movements of hatchery-reared lake trout in Lake Superior","interactions":[],"lastModifiedDate":"2016-02-25T10:45:56","indexId":"1000291","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2543,"text":"Journal of the Fisheries Research Board of Canada","active":true,"publicationSubtype":{"id":10}},"title":"Movements of hatchery-reared lake trout in Lake Superior","docAbstract":"<p>The history of stocking of lake trout (Salvelinus namaycush) in the Great Lakes is reviewed. The study of movements is based on capture of 24,275 fin-clipped lake trout taken in experimental gill nets and trawls and commercial gill nets. Yearling lake trout planted from shore dispersed to 15-fath (27-m) depths in 3A? hr. Most fish remained within 2 miles (3.2 km) of the planting site 2 months, but within 4 months some fish had moved as much as 17 miles (27 km). The highest abundance of planted lake trout was in areas 2-4 miles (3.2-6.4 km) from the planting site even 3 years after release. Distance moved and size of fish were not correlated. Dispersal of lake trout begins at planting and probably continues until the fish are mature. Most movement was eastward in southern Lake Superior and followed the counterclockwise surface currents. Movement is most rapid in areas of strong currents and slowest in areas of weak currents or eddies. Movement to areas west of the Keweenaw Peninsula was insignificant from plantings in Keweenaw Bay and nil from other plantings farther east. Lake trout planted in the eastern third of the lake dispersed more randomly than those planted farther west. Few fish moved farther offshore than the 50-fath (91-m) contour. Lake trout planted in Canadian waters made insignificant contributions to populations in US waters.</p>","language":"English","publisher":"NRC Research Press","doi":"10.1139/f65-093","usgsCitation":"Pycha, R.L., Dryer, W.R., and King, G.R., 1965, Movements of hatchery-reared lake trout in Lake Superior: Journal of the Fisheries Research Board of Canada, v. 22, no. 4, p. 999-1024, https://doi.org/10.1139/f65-093.","productDescription":"26 p.","startPage":"999","endPage":"1024","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63ee14","contributors":{"authors":[{"text":"Pycha, Richard L.","contributorId":17175,"corporation":false,"usgs":true,"family":"Pycha","given":"Richard","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dryer, William R.","contributorId":71921,"corporation":false,"usgs":true,"family":"Dryer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308347,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"King, George R.","contributorId":74721,"corporation":false,"usgs":true,"family":"King","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308348,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1718,"text":"wsp1809I - 1965 - Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61","interactions":[],"lastModifiedDate":"2023-03-13T20:10:12.868331","indexId":"wsp1809I","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"I","title":"Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61","docAbstract":"<p>Artesian water pressure in the deep sandstone aquifer continued to decline throughout most of the Milwaukee-Waukesha area, Wisconsin between 1950 and 1961. Areas of greatest water-level decline were in northeast Waukesha County and in northwest Milwaukee County. The chief cause of the decline was continued heavy pumpage. The major aquifers of southeastern Wisconsin are the Niagara aquifer, which is primarily Niagara Dolomite of Silurian age, and the sandstone aquifer, which consists of sandstones of Cambrian and Ordovician ages. Locally, the glacial sands and gravels ,of Pleistocene age also are important aquifers. In the Milwaukee-Waukesha area, the sandstone aquifer is completely artesian, confined above by the Maquoketa Shale. The Niagara aquifer is generally unconfined. Pumpage from the sandstone aquifer in the Milwaukee-Waukesha area de- creased from about 23.3 million gallons per day in 1950 to about 20.9 million gallons per day in 1961. The principal reason for decreased pumpage was sub- stitution of surface-water supply from Lake Michigan. Between 1950 and 1961, the water-level changes in wells in the sandstone aquifer ranged from plus 10 feet at Town of Lake to minus 98 feet in northwest Milwaukee. Except for a small area near Town of Lake, water levels in wells in the Milwaukee-Waukesha area were lower in 1961 than in 1950. Water-level changes were directly related to the pumpage pattern and pump- age changes. Increased pumpage at Waukesha and in northwest Milwaukee and continued heavy pumpage at Wauwatosa caused widespread water-level declines in northeast Waukesha County and in northwest Milwaukee County. Locally, decreased pumpage at West Milwaukee allowed limited recovery of water levels since 1957. Estimates of pumpage through the year 1975 indicate a pumpage decrease in the middle 1960's, followed by an increase in the late 1960's and early 1970's. Additional conversion to surface-water supply in Milwaukee County will account for most pumpage decreases. Increased pumpage is most likely in Waukesha County where the population is expanding rapidly and an adequate surface-water supply is not readily accessible. The westward shift of the pumpage pattern may cause an additional water-level decline of about 50 feet at Waukesha but will permit water levels to recover about 100 feet at West Allis by 1975. Partial or complete conversion to surface-water supplies by municipalities that depend entirely on water from the sandstone aquifer would allow greater use of the sandstone aquifer by isolated suburban developments and industries.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809I","collaboration":"Prepared in cooperation with the University of Wisconsin, Geological and Natural History Survey","usgsCitation":"Green, J.H., and Hutchinson, R.D., 1965, Ground-water pumpage and water-level changes in the Milwaukee-Waukesha area, Wisconsin, 1950-61: U.S. Geological Survey Water Supply Paper 1809, Report: iii, 19 p. ; 2 Plates: 19.50 x 24.00 inches and 18.50 x 24.00 inches, https://doi.org/10.3133/wsp1809I.","productDescription":"Report: iii, 19 p. ; 2 Plates: 19.50 x 24.00 inches and 18.50 x 24.00 inches","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":26806,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136940,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809i/report-thumb.jpg"},{"id":26805,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26804,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414041,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25008.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Wisconsin","city":"Milwaukee, Waukesha","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -88.82011978710044,\n              43.6048598948214\n            ],\n            [\n              -88.82011978710044,\n              42.619688745253114\n            ],\n            [\n              -87.76500461016991,\n              42.619688745253114\n            ],\n            [\n              -87.76500461016991,\n              43.6048598948214\n            ],\n            [\n              -88.82011978710044,\n              43.6048598948214\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6673ff","contributors":{"authors":[{"text":"Green, J. H.","contributorId":43312,"corporation":false,"usgs":true,"family":"Green","given":"J.","email":"","middleInitial":"H.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":144010,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, R. D.","contributorId":99112,"corporation":false,"usgs":true,"family":"Hutchinson","given":"R.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":144011,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70176114,"text":"70176114 - 1965 - Surface water records of Texas, 1964","interactions":[],"lastModifiedDate":"2017-04-19T10:37:54","indexId":"70176114","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5196,"text":"Water Data Report","active":true,"publicationSubtype":{"id":6}},"title":"Surface water records of Texas, 1964","docAbstract":"<p>The surface-water records for the 1964 water year for gaging stations, partial-record stations, miscellaneous sites, and base-flow studies within the State of Texas are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U. S. Geological Survey, under the direction of Trigg Twichell, district chief, Water Resources Division. </p><p>Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water supply papers, entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Texas were contained in Parts 7 and 8 of that series. </p><p>Beginning with the 1961 water year, streamflow records and related data have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports is limited and primarily for local needs. Records will be published in Geological Survey water-supply papers at 5-year intervals.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70176114","collaboration":"Prepared in cooperation with the Texas Water Commission, Pecos River Commission, Sabine River Compact Administration, City of Dallas, City of Houston, U.S. Army Corps of Engineers, U.S. Soil Conservation Service, U.S. Public Health Service, and U.S. Bureau of Reclamation","usgsCitation":"U.S. Geological Survey, 1965, Surface water records of Texas, 1964: Water Data Report, xiv, 479 p., https://doi.org/10.3133/70176114.","productDescription":"xiv, 479 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":1000089,"text":"1000089 - 1965 - Length-weight relationship of northern pike, Esox lucius, from East Harbor, Ohio","interactions":[],"lastModifiedDate":"2016-02-25T11:11:27","indexId":"1000089","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Length-weight relationship of northern pike, Esox lucius, from East Harbor, Ohio","docAbstract":"<p>The northern pike is one of Ohio's largest game fish but is well known to comparatively few anglers. Large numbers of the big fish spawn in the Ohio marshes adjacent to Lake Erie. Movements related to spawning reach a peak in late March or early April. Later the spawning population disperses and is seldom represented in catches by experimental gear or by anglers. The short period of availability was used to obtain life history information in March of 1951 through 1953. No comprehensive length-weight data for this species have previously been published from this area. East Harbor is a sandspit pond separated from Lake Erie by a large sand bar. Waters and fish populations of the harbor and lake can mix freely through a permanent connecting channel. The larger part of the 850 surface acres of the harbor is normally less than 8 feet deep. The male northern pike averaged 20.5 inches in length and ranged from 13.5 to 28.5 inches. The conspicuously larger females averaged 26.0 inches and ranged from 15.5 to 37.5 inches.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1965)94[404:LRONPE]2.0.CO;2","usgsCitation":"Brown, E.H., and Clark, C.F., 1965, Length-weight relationship of northern pike, Esox lucius, from East Harbor, Ohio: Transactions of the American Fisheries Society, v. 94, no. 4, p. 404-405, https://doi.org/10.1577/1548-8659(1965)94[404:LRONPE]2.0.CO;2.","productDescription":"2 p.","startPage":"404","endPage":"405","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6108","contributors":{"authors":[{"text":"Brown, Edward H. Jr.","contributorId":33251,"corporation":false,"usgs":true,"family":"Brown","given":"Edward","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308058,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clark, Clarence F.","contributorId":99101,"corporation":false,"usgs":true,"family":"Clark","given":"Clarence","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308059,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14173,"text":"ofr6573 - 1965 - Preliminary materials map, Massachusetts portion, Berlin quadrangle, New York-Massachusetts-Vermont","interactions":[],"lastModifiedDate":"2022-06-08T19:45:22.122861","indexId":"ofr6573","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"65-73","title":"Preliminary materials map, Massachusetts portion, Berlin quadrangle, New York-Massachusetts-Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6573","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts Department of Public Works and the United States Bureau of Public Roads","usgsCitation":"Holmes, G.W., 1965, Preliminary materials map, Massachusetts portion, Berlin quadrangle, New York-Massachusetts-Vermont: U.S. Geological Survey Open-File Report 65-73, Report: 3 p.; 1 Plate: 30.93 × 29.11 inches, https://doi.org/10.3133/ofr6573.","productDescription":"Report: 3 p.; 1 Plate: 30.93 × 29.11 inches","costCenters":[],"links":[{"id":42832,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0073/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144671,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0073/report-thumb.jpg"},{"id":397578,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8108.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Massachusetts, New York","otherGeospatial":"Berlin quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.283,\n              42.625\n            ],\n            [\n              -73.25,\n              42.625\n            ],\n            [\n              -73.25,\n              42.708\n            ],\n            [\n              -73.283,\n              42.708\n            ],\n            [\n              -73.283,\n              42.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cdf9","contributors":{"authors":[{"text":"Holmes, George William","contributorId":79107,"corporation":false,"usgs":true,"family":"Holmes","given":"George","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":169029,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70009988,"text":"70009988 - 1965 - Age and metamorphism of some massive sulfide deposits in Virginia, North Carolina and Tennessee","interactions":[],"lastModifiedDate":"2020-11-24T13:28:02.415799","indexId":"70009988","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Age and metamorphism of some massive sulfide deposits in Virginia, North Carolina and Tennessee","docAbstract":"<p>Isotopic ages of vein and wall-rock samples have been determined on five massive sulflde deposits of the southern Appalachians. Vein mineral ages of about 1100 m.y. indicate that some ore bodies formed at least as early as the Grenville metamorphism, and probably soon after the formation of the enclosing gneiss and schist. Present textures of the ore were formed during subsequent metamorphic periods at about 450 m.y. and 300 to 330 m.y. ago.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(65)90065-7","issn":"00167037","usgsCitation":"Kinkel, A., Thomas, H., Marvin, R.F., and Walthall, F., 1965, Age and metamorphism of some massive sulfide deposits in Virginia, North Carolina and Tennessee: Geochimica et Cosmochimica Acta, v. 29, no. 6, p. 717-724, https://doi.org/10.1016/0016-7037(65)90065-7.","productDescription":"8 p.","startPage":"717","endPage":"724","numberOfPages":"8","costCenters":[],"links":[{"id":218615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina, Tennessee, 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,{"id":70171153,"text":"70171153 - 1965 - Field application methods for recovery of the selective lampricide, 3-trifluoromethyl-4-nitrophenol","interactions":[],"lastModifiedDate":"2016-05-24T09:56:22","indexId":"70171153","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Field application methods for recovery of the selective lampricide, 3-trifluoromethyl-4-nitrophenol","docAbstract":"<p>Colorimetric methods are described for the detection of residues of the selective lampricide, 3-trifluoromethyl-4-nitrophenol (TFM), in natural waters and fish tissues. Solvent extraction and anion exchange were used to separate and concentrate the lampricide, and to reduce high background colors which often interfere with the determinations. Data from the Pentwater and Muskegon Rivers (Michigan) showed an exponential rate of disappearance of TFM from the water immediately after treatments to eradicate larvae of the sea lamprey (<i>Petromyzon marinus</i>). No TFM was recovered from fish exposed in their natural environment to low levels of the lampricide during treatment; residues were recovered, however, from fish exposed to high concentrations in the laboratory.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 8th Conference on Great Lakes Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"8th Conference on Great Lakes Research","conferenceDate":"March 29-30","conferenceLocation":"Ann Arbor, MI","language":"English","publisher":"University of Michigan","usgsCitation":"Billy, T.J., Daniels, S.L., Kempe, L.L., and Beeton, A.M., 1965, Field application methods for recovery of the selective lampricide, 3-trifluoromethyl-4-nitrophenol, <i>in</i> Proceedings of the 8th Conference on Great Lakes Research, Ann Arbor, MI, March 29-30, p. 17-24.","productDescription":"8 p.","startPage":"17","endPage":"24","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321589,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d6505e4b07e28b6683e7b","contributors":{"authors":[{"text":"Billy, Thomas J.","contributorId":76853,"corporation":false,"usgs":true,"family":"Billy","given":"Thomas","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daniels, Stacy L.","contributorId":105821,"corporation":false,"usgs":true,"family":"Daniels","given":"Stacy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630122,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kempe, Lloyd L.","contributorId":55117,"corporation":false,"usgs":true,"family":"Kempe","given":"Lloyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630123,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630124,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70171212,"text":"70171212 - 1965 - Relative toxicities of similar formulations of pyrethrum and rotenone to fish and immature stoneflies","interactions":[],"lastModifiedDate":"2016-06-20T11:06:46","indexId":"70171212","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5079,"text":"Pyrethrum Post","active":true,"publicationSubtype":{"id":10}},"title":"Relative toxicities of similar formulations of pyrethrum and rotenone to fish and immature stoneflies","docAbstract":"<p><span>The insecticidal properties of rotenone and pyrethrum have been known for many years. Both toxicants have long histories of extensive use for control of a variety of insect pests. Rotenone has been also employed as a management tool by fishery biologists to rehabilitate fishing waters, and its toxicity to fish in a number of ecological situations is well established. Pyrethrum's toxicity to fish is less well known.</span></p>","language":"English","publisher":"Pyrethrum Bureau","publisherLocation":"Nakuru, Kenya","usgsCitation":"Bridges, W., and Cope, O., 1965, Relative toxicities of similar formulations of pyrethrum and rotenone to fish and immature stoneflies: Pyrethrum Post, v. 8, no. 1, p. 3-5.","productDescription":"3 p.","startPage":"3","endPage":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":323976,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"576913e6e4b07657d19ff253","contributors":{"authors":[{"text":"Bridges, W.R.","contributorId":38097,"corporation":false,"usgs":true,"family":"Bridges","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":630279,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cope, O.B.","contributorId":23193,"corporation":false,"usgs":true,"family":"Cope","given":"O.B.","email":"","affiliations":[],"preferred":false,"id":630280,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2968,"text":"wsp1788 - 1965 - Ground-water resources and geology of Niobrara County, Wyoming, with a section on chemical quality of the ground water","interactions":[],"lastModifiedDate":"2023-11-01T19:43:02.446947","indexId":"wsp1788","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"1788","title":"Ground-water resources and geology of Niobrara County, Wyoming, with a section on chemical quality of the ground water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1788","usgsCitation":"Whitcomb, H.A., and Cummings, T.R., 1965, Ground-water resources and geology of Niobrara County, Wyoming, with a section on chemical quality of the ground water: U.S. Geological Survey Water Supply Paper 1788, Report: v, 101 p.; 3 Plates: 27.50 x 35.70 inches, https://doi.org/10.3133/wsp1788.","productDescription":"Report: v, 101 p.; 3 Plates: 27.50 x 35.70 inches","costCenters":[],"links":[{"id":110018,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24976.htm","linkFileType":{"id":5,"text":"html"},"description":"24976"},{"id":29702,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1788/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29701,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1788/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29700,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1788/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29703,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1788/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139272,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1788/report-thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Niobrara County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-104.0542,43.5037],[-104.0541,43.4827],[-104.0539,43.4772],[-104.054,43.4677],[-104.0541,43.4535],[-104.0536,43.4221],[-104.0536,43.3893],[-104.0533,43.2973],[-104.0531,43.2122],[-104.053,43.1976],[-104.0536,43.1284],[-104.0534,43.0028],[-104.0527,43.0028],[-104.0527,43.0014],[-104.0528,42.9334],[-104.0525,42.6128],[-104.1247,42.6113],[-104.3598,42.6117],[-104.4777,42.6104],[-104.5967,42.6104],[-104.616,42.6105],[-104.6516,42.61],[-104.7133,42.6098],[-104.8323,42.6114],[-104.8915,42.6105],[-104.8941,42.6915],[-104.8992,42.8704],[-104.9014,43.0738],[-104.9019,43.1175],[-104.9019,43.1321],[-104.9018,43.2732],[-104.9009,43.3633],[-104.9002,43.3933],[-104.8996,43.4488],[-104.9001,43.478],[-104.8991,43.5008],[-104.8372,43.5011],[-104.7968,43.5015],[-104.7785,43.5015],[-104.7374,43.5019],[-104.6155,43.502],[-104.5966,43.5019],[-104.5764,43.5019],[-104.3572,43.5028],[-104.1431,43.5036],[-104.0824,43.5036],[-104.0542,43.5037]]]},\"properties\":{\"name\":\"Niobrara\",\"state\":\"WY\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a95e4b07f02db659b74","contributors":{"authors":[{"text":"Whitcomb, Harold A.","contributorId":102868,"corporation":false,"usgs":true,"family":"Whitcomb","given":"Harold","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146063,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. Ray","contributorId":20722,"corporation":false,"usgs":true,"family":"Cummings","given":"T.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":887313,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68244,"text":"ha125 - 1965 - Availability of ground water in the Lynnville quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:53:30.559684","indexId":"ha125","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"125","title":"Availability of ground water in the Lynnville quadrangle, Kentucky-Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha125","usgsCitation":"Lambert, T.W., 1965, Availability of ground water in the Lynnville quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 125, 1 Plate: 47.50 x 33.50 inches, https://doi.org/10.3133/ha125.","productDescription":"1 Plate: 47.50 x 33.50 inches","costCenters":[],"links":[{"id":189572,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413587,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15482.htm","linkFileType":{"id":5,"text":"html"}},{"id":89624,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/125/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Lynnville quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.625,\n              36.5\n            ],\n            [\n              -88.625,\n              36.625\n            ],\n            [\n              -88.5,\n              36.625\n            ],\n            [\n              -88.5,\n              36.5\n            ],\n            [\n              -88.625,\n              36.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d945","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277901,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5964,"text":"pp484 - 1965 - Geomorphology of the Shenandoah Valley, Virginia and West Virginia, and origin of the residual ore deposits","interactions":[],"lastModifiedDate":"2023-04-11T19:23:30.357282","indexId":"pp484","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"484","title":"Geomorphology of the Shenandoah Valley, Virginia and West Virginia, and origin of the residual ore deposits","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp484","usgsCitation":"Hack, J.T., 1965, Geomorphology of the Shenandoah Valley, Virginia and West Virginia, and origin of the residual ore deposits: U.S. Geological Survey Professional Paper 484, Report: iv, 84 p.; 3 Plates: 24.96 x 33.44 inches or smaller, https://doi.org/10.3133/pp484.","productDescription":"Report: iv, 84 p.; 3 Plates: 24.96 x 33.44 inches or smaller","costCenters":[],"links":[{"id":415590,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4488.htm","linkFileType":{"id":5,"text":"html"}},{"id":112656,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0484/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":112655,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0484/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":112658,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0484/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":112657,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0484/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140350,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0484/report-thumb.jpg"}],"country":"United States","state":"Virginia, West Virginia","otherGeospatial":"Shenandoah Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -79.3189,\n              39.6217\n            ],\n            [\n              -79.3189,\n              37.8864\n            ],\n            [\n              -77.7392,\n              37.8864\n            ],\n            [\n              -77.7392,\n              39.6217\n            ],\n            [\n              -79.3189,\n              39.6217\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4a3","contributors":{"authors":[{"text":"Hack, John Tilton","contributorId":76279,"corporation":false,"usgs":true,"family":"Hack","given":"John","email":"","middleInitial":"Tilton","affiliations":[],"preferred":false,"id":151885,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64241,"text":"gp509 - 1965 - Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont","interactions":[{"subject":{"id":44227,"text":"ofr6110 - 1961 - Total intensity aeromagnetic map of parts of Bolton, Whitehall, Glens Falls, and Fort Ann quadrangles, New York","indexId":"ofr6110","publicationYear":"1961","noYear":false,"title":"Total intensity aeromagnetic map of parts of Bolton, Whitehall, Glens Falls, and Fort Ann quadrangles, New York"},"predicate":"SUPERSEDED_BY","object":{"id":64241,"text":"gp509 - 1965 - Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont","indexId":"gp509","publicationYear":"1965","noYear":false,"title":"Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont"},"id":1}],"lastModifiedDate":"2025-04-28T17:13:30.023397","indexId":"gp509","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"509","title":"Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp509","usgsCitation":"Balsley, J.R., and Bromery, R.W., 1965, Aeromagnetic map of parts of the Bolton Landing, Glens Falls, and Whitehall quadrangles, Warren and Washington Counties, New York and Rutland County, Vermont: U.S. Geological Survey Geophysical Investigations Map 509, Report: 1 p.; 1 Plate: 22.31 x 34.57 inches, https://doi.org/10.3133/gp509.","productDescription":"Report: 1 p.; 1 Plate: 22.31 x 34.57 inches","costCenters":[],"links":[{"id":254280,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0509/report-thumb.jpg"},{"id":250809,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0509/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250808,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0509/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414488,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3460.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"62500","country":"United States","state":"New York, Vermont","county":"Rutland County, Warren County, Washington County","otherGeospatial":"Bolton Landing, Glens Falls, and Whitehall quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.75,\n              43.333\n            ],\n            [\n              -73.75,\n              43.75\n            ],\n            [\n              -73.3667,\n              43.75\n            ],\n            [\n              -73.3667,\n              43.333\n            ],\n            [\n              -73.75,\n              43.333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697670","contributors":{"authors":[{"text":"Balsley, James R.","contributorId":10010,"corporation":false,"usgs":true,"family":"Balsley","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270291,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bromery, R. W.","contributorId":11676,"corporation":false,"usgs":true,"family":"Bromery","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":270292,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":64149,"text":"gp546 - 1965 - Aeromagnetic map of the Uncasville quadrangle and part of the New London quadrangle, New London County, Connecticut","interactions":[],"lastModifiedDate":"2023-03-21T20:06:33.503288","indexId":"gp546","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"546","title":"Aeromagnetic map of the Uncasville quadrangle and part of the New London quadrangle, New London County, Connecticut","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp546","usgsCitation":"Boynton, G.R., and Smith, C.W., 1965, Aeromagnetic map of the Uncasville quadrangle and part of the New London quadrangle, New London County, Connecticut: U.S. Geological Survey Geophysical Investigations Map 546, Report: 1 p.; 1 Plate: 22.05 x 40.97 inches, https://doi.org/10.3133/gp546.","productDescription":"Report: 1 p.; 1 Plate: 22.05 x 40.97 inches","costCenters":[],"links":[{"id":414494,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3500.htm","linkFileType":{"id":5,"text":"html"}},{"id":254117,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0546/report-thumb.jpg"},{"id":250636,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0546/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250635,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0546/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Connecticut","county":"New London County","otherGeospatial":"New London quadrangle, Uncasville quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.125,\n              41.3028\n            ],\n            [\n              -72.125,\n              41.5\n            ],\n            [\n              -72,\n              41.5\n            ],\n            [\n              -72,\n              41.3028\n            ],\n            [\n              -72.125,\n              41.3028\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68baad","contributors":{"authors":[{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, C. W.","contributorId":57457,"corporation":false,"usgs":true,"family":"Smith","given":"C.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":270055,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68242,"text":"ha160 - 1965 - Availability of ground water in the Kentucky part of the Rushing Creek quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:46:02.159683","indexId":"ha160","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"160","title":"Availability of ground water in the Kentucky part of the Rushing Creek quadrangle, Kentucky-Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha160","usgsCitation":"Lambert, T.W., 1965, Availability of ground water in the Kentucky part of the Rushing Creek quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 160, 1 Plate: 47.50 x 34.50 inches, https://doi.org/10.3133/ha160.","productDescription":"1 Plate: 47.50 x 34.50 inches","costCenters":[],"links":[{"id":189570,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413585,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15521.htm","linkFileType":{"id":5,"text":"html"}},{"id":89622,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/160/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Rushing Creek quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.125,\n              36.625\n            ],\n            [\n              -88.125,\n              36.75\n            ],\n            [\n              -88,\n              36.75\n            ],\n            [\n              -88,\n              36.625\n            ],\n            [\n              -88.125,\n              36.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db6608f4","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277899,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68248,"text":"ha162 - 1965 - Availability of ground water in the Water Valley quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:56:42.836243","indexId":"ha162","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"162","title":"Availability of ground water in the Water Valley quadrangle, Kentucky-Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha162","usgsCitation":"Lambert, T.W., 1965, Availability of ground water in the Water Valley quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 162, 1 Plate: 47.50 x 35.50 inches, https://doi.org/10.3133/ha162.","productDescription":"1 Plate: 47.50 x 35.50 inches","costCenters":[],"links":[{"id":189576,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413588,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15523.htm","linkFileType":{"id":5,"text":"html"}},{"id":89629,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/162/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Water Valley quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.875,\n              36.5\n            ],\n            [\n              -88.875,\n              36.625\n            ],\n            [\n              -88.75,\n              36.625\n            ],\n            [\n              -88.75,\n              36.5\n            ],\n            [\n              -88.875,\n              36.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8db","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185670,"text":"70185670 - 1965 - Vigil Network sites: A sample of data for permanent filing","interactions":[],"lastModifiedDate":"2017-03-27T13:03:24","indexId":"70185670","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"Vigil Network sites: A sample of data for permanent filing","docAbstract":"<p>The Vigil Network consists of places where observations are made through time to record changes in landscape features over a long period. Resurveys will usually be made once each year or every few years and the period of observation, hopefully, will extend through and beyond the International Hydrological Decade.</p><p>Vigil Network sites will usually be chosen to represent some typical feature of a given landscape. In the example shown here, the feature is a small ephemeral channel in a basin of moderate relief underlain by silty sandstone typical of the surrounding area. Vigil sites are not protected from man's influence and indeed may be selected because of the possible or portending cultural influences. In this respect they differ from the Bench Mark Network whose purpose is to make precise observations of hydrologic factors in areas uninfluenced by and protected from man's use.</p><p>The factors which might be observed are many and varied. A few might be mentioned here, others are explained at length elsewhere (Miller and Leopold, 1963; Leopold, 1962). Streamchannel position, form, depth, and profile; vegetation in form of transects or quadrats; soil movement on slopes; rock movement on slopes or in channels. These and many more would yield valuable information on changes with time.</p><p>To assure permanence of initial field observations, including reference points, bench marks, and cross sections, brief descriptions, maps, and initial data should be filed identically in designated repositories where the data will be made available for inspection by any interested scientist. It is recommended that the designation of two such locations where records of the type here attached will be filed be taken up by the Coordinating Council of the International Hydrological Decade. In designating such repositories it should be recognized that there is no need for elaborate indexing. The main requirement is merely the maintenance of a simple file where the data are stored and can be inspected or copied by any scientist. There need be no special provision for lending or reproduction services.</p><p>The present document is an example showing what data, maps, and descriptions should be included in those permanent files at the two repositories. The material in these repositories should be sufficient to permit someone in the indefinite future to find and remeasure the same features described now. Thus the scientific value of the original surveys increases with time, - provided that the descriptions are sufficient to allow a person to find with assurance the original feature in the field.</p><p>It must be visualized that a permanent repository must economize in space. Thus, as the example here shows, the filed material is not all of the original field notes but a summary, brief but descriptive.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666509493401","usgsCitation":"Leopold, L.B., and Emmett, W.W., 1965, Vigil Network sites: A sample of data for permanent filing: International Association of Scientific Hydrology - Bulletin , v. 10, no. 3, p. 12-21, https://doi.org/10.1080/02626666509493401.","productDescription":"10 p.","startPage":"12","endPage":"21","costCenters":[],"links":[{"id":480681,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666509493401","text":"Publisher Index Page"},{"id":338379,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"10","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da253fe4b0543bf7fda87d","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686308,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":686309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2902,"text":"wsp1809L - 1965 - Reconnaissance of the ground-water resources in parts of Larimer, Logan, Morgan, Sedgwick, and Weld Counties, Colorado, with a section on the chemical quality of the water","interactions":[],"lastModifiedDate":"2023-11-01T21:23:13.44938","indexId":"wsp1809L","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"L","title":"Reconnaissance of the ground-water resources in parts of Larimer, Logan, Morgan, Sedgwick, and Weld Counties, Colorado, with a section on the chemical quality of the water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1809L","usgsCitation":"Weist, W., and Brennan, R., 1965, Reconnaissance of the ground-water resources in parts of Larimer, Logan, Morgan, Sedgwick, and Weld Counties, Colorado, with a section on the chemical quality of the water: U.S. Geological Survey Water Supply Paper 1809, Report; iv, 24 p.; 1 Plate: 37.50 x 16.00 inches, https://doi.org/10.3133/wsp1809L.","productDescription":"Report; iv, 24 p.; 1 Plate: 37.50 x 16.00 inches","costCenters":[],"links":[{"id":422318,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25011.htm","linkFileType":{"id":5,"text":"html"}},{"id":29581,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29582,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809l/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138383,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809l/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Larimer County, Logan County, Morgan County, Sedgwick County, Weld County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -102.425,\n              41\n            ],\n            [\n              -105.17,\n              41\n            ],\n            [\n              -105.17,\n              40.282\n            ],\n            [\n              -102.425,\n              40.282\n            ],\n            [\n              -102.425,\n              41\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636d2d","contributors":{"authors":[{"text":"Weist, William G.","contributorId":21526,"corporation":false,"usgs":true,"family":"Weist","given":"William G.","affiliations":[],"preferred":false,"id":145983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brennan, Robert","contributorId":105695,"corporation":false,"usgs":true,"family":"Brennan","given":"Robert","email":"","affiliations":[],"preferred":false,"id":887318,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2897,"text":"wsp1811 - 1965 - Hydrology of the Little Plover River basin, Portage County, Wisconsin, and the effects of water resource development","interactions":[],"lastModifiedDate":"2023-04-13T20:54:27.826245","indexId":"wsp1811","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","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":"1811","title":"Hydrology of the Little Plover River basin, Portage County, Wisconsin, and the effects of water resource development","docAbstract":"<p>The Little Plover River basin is in the sand-plain area of central Wisconsin. The basin and the surrounding sand-plain area provide a good fish and wildlife habitat and is a popular locale for sport fishing. Good yields may be obtained in the area from irrigated crops, and the irrigated acreage has been increasing rapidly in recent years. Sportsmen and conservationists are concerned about the effects of increased development of the water resources on the streams as trout habitat. In the past, many political and legal conflicts among water users have arisen from erroneous opinions as to the behavior of water. Many of these conflicts would be diminished or eliminated if the participants were cognizant of fundamental hydrologic principles. </p><p>This study was made to demonstrate the extent and nature of the interrelation of ground water and surface water and the fundamental hydrologic principles governing water movement. The study was also made to determine the hydrologic changes that might occur following development, to provide information that might be used as a basis for planning water development, and for drafting legislation that recognizes the relation between ground water and surface water. </p><p>Water has been developed in the Little Plover River basin for industry, for domestic and stock supplies, and for irrigation. Irrigated acreage is increasing in the area, and the use of water for irrigation may alter the hydrology of the basin somewhat. About 4,000-4,500 acres of land within the basin, or 50-60 percent of the basin area, is suitable for irrigated farming, but probably no more than 2,500 acres will be under irrigation in any one year, unless present crop-rotation practices are changed. </p><p>Most of the Little Plover River basin is underlain by from 40 to 100 feet of glacial outwash consisting of highly permeable sand and gravel. The glacial outwash is the main aquifer in the area and is capable of yielding large quantities of water to wells. An aquifer test in the area indicated that the coefficient of transmissibility of the glacial outwash is about 140,000 gallons per day per foot. The specific yield of the outwash is about 20 percent, as determined from water-level and streamfiow data. Morainal deposits occur locally with the glacial outwash. These deposits transmit water readily and do not form barriers to ground water in the outwash. Relatively impermeable crystalline rocks underlie the glacial deposits, and a sandstone ridge of low permeability impedes the movement of ground water from the basin by underflow. </p><p>The glacial outwash and morainal deposits are recharged by infiltration of 9-10 inches of the 31 inches of precipitation that falls on the area in an average year. If it is not withdrawn by wells for consumptive use or by phreatophytes, water that infiltrates the sand and gravel discharges later into the Little Plover River. This ground-water discharge constitutes 90-95 percent of the total flow of the Little Plover River. </p><p>Annual evapotranspiration varies considerably, but generally ranges from 2 to 8 inches less than the potential evapotranspiration of 24 inches. Consumptive use of irrigation water averages about 4 inches per year. Most of the water pumped from wells otherwise would be discharged to the stream, and consumptive use of irrigation water will deplete streamflow by the amount of evapotranspiration. </p><p>Pumping wells have little effect on the water level in the highly permeable sand and gravel. Significant interference between wells would occur only if large capacity wells were within a few tens of feet of each other. </p><p>Ground water and surface water are closely interrelated in the sand-plain area and ground-water withdrawals near the Little Plover River may cause a measurable streamflow depletion. In a test, a well that was pumping about 1,120 gpm (gallons per minute) and that was 300 feet from the stream derived about 30 percent of its flow from the stream after 3 days of pumping. </p><p>For this study, the effects of increased ground-water development were evaluated from a hypothetical development schedule, for which it was assumed that 500 acres were irrigated the first year and that an additional 50 acres were irrigated in each succeeding year for 10 years. It also was assumed that the average annual consumptive-use requirement for irrigation water would be one- third of an acre-foot per acre. Calculations indicate that the maximum monthly rate of depletion due to the consumptive use of 4 inches of ground water per year on 500 acres would be about 0.4 cfs (cubic feet per second) the first year and 0.5 cfs after 10 years of pumping. Other computations indicate that the maximum monthly rate of depletion due to irrigating 500 acres the first year and 50 additional acres each year for 10 years would be about 0.8 cfs. Maximum depletion would occur during the summer months, concurrent with the irrigation withdrawals. </p><p>Because of the close interrelation between ground and surface water, surface- water withdrawals will cause an increased inflow of ground water to the stream and a decline in ground-water levels near the stream. These effects were demonstrated by pumping from the stream. After 29 hours of pumping, a depletion of 1,120 gpm at a site 7,000 feet downstream was about 200 gpm less than the diversion at the pump. Most of the 200 gpm was supplied from the stream-banks, and ground-water levels near the stream declined as much as 0.3 foot. Computations indicated that ground-water inflow, following a streamflow diver- sion that lowered the stage 0.15 foot, would be 0.14 cfs after 5 days and 0.06 cfs after 30 days. </p><p>The demonstration of the quantitative relation between ground water and surface water, as given by this study, should provide a sound basis for planning water development to minimize conflicts of interest. The demonstrations also should provide a basis for drafting legislation that recognizes the interrelation of ground water and surface water. </p><p>Because the geology and the hydrology are relatively uniform throughout the sand plains, many of the methods and hydrologic values determined for this detailed study of the Little Plover River basin may be applied to other basins in the sand-plain area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1811","collaboration":"Prepared in cooperation with the Wisconsin Conservation Department and the University of Wisconsin Geological and Natural History Survey","usgsCitation":"Weeks, E.P., Erickson, D.W., and Holt, C.L., 1965, Hydrology of the Little Plover River basin, Portage County, Wisconsin, and the effects of water resource development: U.S. Geological Survey Water Supply Paper 1811, Report: v, 78 p.; 6 Plates: 21.00 x 18.01 inches or smaller, https://doi.org/10.3133/wsp1811.","productDescription":"Report: v, 78 p.; 6 Plates: 21.00 x 18.01 inches or smaller","numberOfPages":"85","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":415734,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25017.htm","linkFileType":{"id":5,"text":"html"}},{"id":29561,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29559,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29558,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29562,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29560,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29563,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1811/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138378,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1811/report-thumb.jpg"},{"id":29557,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1811/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Portage County","otherGeospatial":"Little Plover River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -89.589,\n              44.554\n            ],\n            [\n              -89.589,\n              44.404\n            ],\n            [\n              -89.367,\n              44.404\n            ],\n            [\n              -89.367,\n              44.554\n            ],\n            [\n              -89.589,\n              44.554\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdc0c","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":145973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, Donald W.","contributorId":34900,"corporation":false,"usgs":true,"family":"Erickson","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145974,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holt, Charles Lee Roy Jr.","contributorId":77913,"corporation":false,"usgs":true,"family":"Holt","given":"Charles","suffix":"Jr.","email":"","middleInitial":"Lee Roy","affiliations":[],"preferred":false,"id":145975,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":81356,"text":"81356 - 1965 - Distribution of fishes in U. S. streams tributary to Lake Superior","interactions":[],"lastModifiedDate":"2016-02-25T10:52:08","indexId":"81356","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"516","title":"Distribution of fishes in U. S. streams tributary to Lake Superior","docAbstract":"<p>Experimental sea lamprey control by the Bureau of Commercial Fisheries on Lake Superior streams provided many new distributional records of the fish fauna. Seventy-one species were recorded from 175 streams. Specimens were collected at the electromechanical barriers, with electric shockers, with fyke nets, and during chemical treatment of streams. Maps showing stream records of each species are presented.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Moore, H.H., and Braem, R.A., 1965, Distribution of fishes in U. S. streams tributary to Lake Superior: Special Scientific Report - Fisheries 516, 61 p.","productDescription":"61 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101759,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015045826339?urlappend=%3Bseq=193"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63bfbf","contributors":{"authors":[{"text":"Moore, Harry H.","contributorId":48670,"corporation":false,"usgs":true,"family":"Moore","given":"Harry","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":295282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Braem, Robert A.","contributorId":34858,"corporation":false,"usgs":true,"family":"Braem","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":295281,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70174082,"text":"70174082 - 1965 - The water story in Central Iowa","interactions":[],"lastModifiedDate":"2016-06-27T14:45:29","indexId":"70174082","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5106,"text":"Iowa Geological Survey Water Atlas","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"The water story in Central Iowa","docAbstract":"<p>\"The general welfare of the people of the state of Iowa requires that the water resources of the state be put to beneficial use to the fullest extent of which they are capable.\" &nbsp;This can be achieved only by a knowledge and understanding of the water resources - their use, their source, their quality, their availability, and the demands place upon them. &nbsp;To provide such knowledge and understanding, the United States Geological Survey in cooperation with the Iowa Geological Survey produced this report on the utilization and availability of water in central Iowa.</p>\n<p>This report contains information on the past, present, and future statues of central Iowa;s water; information that can be used by the regional developer, the resource planner and manager, and other informed persons whose opinions and sound judgements are required in making decisions toward efficient development, management, use, and conservation of water. &nbsp;It gives an over-all view of the area's water resources and is aimed at guiding the people of central Iowa to the best available sources of water.</p>","language":"English","publisher":"Iowa Geological Survey","usgsCitation":"Twenter, F.R., and Coble, R.W., 1965, The water story in Central Iowa: Iowa Geological Survey Water Atlas 1, viii, 89 p.","productDescription":"viii, 89 p.","numberOfPages":"95","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":324446,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":324445,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://s-iihr34.iihr.uiowa.edu/publications/publications?category=Water-Supply-Bulletins"}],"country":"United States","state":"Iowa","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-93.972,42.5566],[-93.8563,42.557],[-93.7367,42.5568],[-93.6191,42.5565],[-93.5002,42.557],[-93.3819,42.557],[-93.2637,42.5564],[-93.1473,42.5561],[-93.0284,42.5562],[-92.9101,42.5557],[-92.7925,42.556],[-92.6755,42.5558],[-92.5553,42.555],[-92.5552,42.4695],[-92.5353,42.4694],[-92.5353,42.2972],[-92.6531,42.2971],[-92.7697,42.2964],[-92.7687,42.2101],[-92.7672,42.1234],[-92.7662,42.0348],[-92.7671,41.9494],[-92.7674,41.8618],[-92.7683,41.776],[-92.768,41.6879],[-92.7683,41.6007],[-92.7567,41.6011],[-92.7564,41.509],[-92.8729,41.5082],[-92.9894,41.5083],[-93.1047,41.5078],[-93.2181,41.5076],[-93.3304,41.5074],[-93.3304,41.4906],[-93.3347,41.4888],[-93.339,41.4833],[-93.3414,41.481],[-93.3445,41.481],[-93.347,41.4815],[-93.3488,41.4833],[-93.3531,41.4947],[-93.3561,41.4965],[-93.3586,41.4965],[-93.3598,41.4947],[-93.3611,41.4879],[-93.3641,41.4861],[-93.3703,41.4852],[-93.3733,41.4856],[-93.3745,41.4874],[-93.3764,41.4902],[-93.3776,41.492],[-93.3801,41.4929],[-93.3862,41.4929],[-93.3893,41.492],[-93.3935,41.4879],[-93.3978,41.4856],[-93.4021,41.4856],[-93.4052,41.4866],[-93.4058,41.4884],[-93.4052,41.4897],[-93.4015,41.492],[-93.3991,41.4938],[-93.3991,41.4961],[-93.4003,41.4988],[-93.4027,41.5002],[-93.407,41.4993],[-93.4113,41.4943],[-93.4162,41.4916],[-93.4199,41.4911],[-93.423,41.4925],[-93.4236,41.4943],[-93.4224,41.4961],[-93.4174,41.4997],[-93.4162,41.502],[-93.4162,41.5047],[-93.4174,41.507],[-93.4217,41.5084],[-93.426,41.5075],[-93.4346,41.502],[-93.4407,41.5025],[-93.4432,41.5038],[-93.4414,41.5061],[-93.4456,41.5061],[-93.5615,41.5102],[-93.6774,41.511],[-93.7927,41.5108],[-93.8773,41.5024],[-93.9006,41.5014],[-94.0159,41.5019],[-94.1299,41.5028],[-94.2427,41.5031],[-94.2419,41.5993],[-94.2812,41.6],[-94.281,41.6871],[-94.2813,41.7757],[-94.2811,41.8624],[-94.1671,41.8626],[-94.1652,41.8626],[-94.166,41.9493],[-94.1656,42.0347],[-94.1665,42.1228],[-94.1649,42.1519],[-94.1673,42.2091],[-94.2843,42.2089],[-94.3989,42.2086],[-94.3982,42.2954],[-94.3975,42.3835],[-94.3974,42.4721],[-94.4434,42.4718],[-94.4445,42.5572],[-94.4457,42.644],[-94.3279,42.6435],[-94.2101,42.6437],[-94.0942,42.6438],[-93.9714,42.6434],[-93.972,42.5566]]]},\"properties\":{\"name\":\"Boone\",\"state\":\"IA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57724e36e4b07657d1a819df","contributors":{"authors":[{"text":"Twenter, F. 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