{"pageNumber":"2434","pageRowStart":"60825","pageSize":"25","recordCount":68807,"records":[{"id":56318,"text":"wdrMI712 - 1972 - Water resources data for Michigan, water year 1971; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2017-07-12T14:37:55","indexId":"wdrMI712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MI-71-2","title":"Water resources data for Michigan, water year 1971; Part 2, Water quality records","docAbstract":"<p>Water resources data for the 1971 water year for Michigan include records of data for the chemical and physical characteristics of surface and ground waters. Data on the quality of surface water (chemical, temperature, and sediment) were collected from designated sampling sites at predetermined intervals such as once-daily, weekly, monthly or less frequently, and at some sites data were recorded on punched paper tape at 60-minute intervals. Records are given for 371 sampling stations, of which 41 are continuous-record stations, 24 are partial-record stations, and 306 are miscellaneous sites. Records of chemical analyses also are given for 260 ground-water sites. Locations of surface-water quality stations are shown in Figures 3 and 4. The records were collected by the Water Resources Division of the U.S. Geological Survey under the direction of T. R. Cummings, district chief, and John J. Molloy, district chief, Water Resources Division, Columbus, Ohio. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Michigan.</p><p>The Geological Survey has published records of chemical quality, water temperatures, and sediment since 1941 in an annual series of water-supply papers entitled, \"Quality of Surface Waters of the United States.\" Beginning with the 1964 water year, water-quality records have been released by the Geological Survey in annual reports on a State-boundary basis. These reports are for limited distribution and are designed primarily for rapid release of data shortly after the end of the water year. These records will be published later in Geological Survey water-supply papers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMI712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Michigan, water year 1971; Part 2, Water quality records: U.S. Geological Survey Water Data Report MI-71-2, v, 145 p., https://doi.org/10.3133/wdrMI712.","productDescription":"v, 145 p.","numberOfPages":"156","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":343742,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/mi-71-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/mi-71-2/report-thumb.jpg"}],"country":"United 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,{"id":63960,"text":"gp758 - 1972 - Aeromagnetic map of the Bradshaw Mountains and vicinity, Yavapai County, Arizona","interactions":[],"lastModifiedDate":"2025-07-07T18:53:19.449137","indexId":"gp758","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"758","title":"Aeromagnetic map of the Bradshaw Mountains and vicinity, Yavapai County, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp758","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Aeromagnetic map of the Bradshaw Mountains and vicinity, Yavapai County, Arizona: U.S. Geological Survey Geophysical Investigations Map 758, 1 Plate: 52.13 x 33.83 inches, https://doi.org/10.3133/gp758.","productDescription":"1 Plate: 52.13 x 33.83 inches","costCenters":[],"links":[{"id":491759,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6113.htm","linkFileType":{"id":5,"text":"html"}},{"id":253809,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0758/report-thumb.jpg"},{"id":250323,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0758/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250322,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0758/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Arizona","county":"Yavapai County","otherGeospatial":"Bradshaw Mountains and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.75,\n              34.425\n            ],\n            [\n              -112.75,\n              34\n            ],\n            [\n              -112,\n              34\n            ],\n            [\n              -112,\n              34.425\n            ],\n            [\n              -112.75,\n              34.425\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db697118","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533429,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42179,"text":"ofr72383 - 1972 - Aeromagnetic data from SW Naval Petroleum Reserve, Alaska","interactions":[],"lastModifiedDate":"2022-05-18T20:24:36.304734","indexId":"ofr72383","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-383","title":"Aeromagnetic data from SW Naval Petroleum Reserve, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72383","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Aeromagnetic data from SW Naval Petroleum Reserve, Alaska: U.S. Geological Survey Open-File Report 72-383, 4 Plates: 50.00 × 34.00 inches or smaller, https://doi.org/10.3133/ofr72383.","productDescription":"4 Plates: 50.00 × 34.00 inches or smaller","costCenters":[],"links":[{"id":172340,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98811,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0383/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":98812,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0383/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":98813,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0383/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":98814,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0383/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400781,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8715.htm"}],"country":"United States","state":"Alaska","otherGeospatial":"SW Naval Petroleum Reserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -161.833,\n              68\n            ],\n            [\n              -155.667,\n              68\n            ],\n            [\n              -155.667,\n              69.5\n            ],\n            [\n              -161.833,\n              69.5\n            ],\n            [\n              -161.833,\n              68\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698492","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530886,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63880,"text":"gp838 - 1972 - Aeromagnetic map of the Morenci-Monticello area, southeastern Arizona and southwestern New Mexico","interactions":[{"subject":{"id":41740,"text":"ofr70337 - 1970 - Aeromagnetic map of the Morenci-Monticello area, southeastern Arizona and southwestern New Mexico","indexId":"ofr70337","publicationYear":"1970","noYear":false,"title":"Aeromagnetic map of the Morenci-Monticello area, southeastern Arizona and southwestern New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":63880,"text":"gp838 - 1972 - Aeromagnetic map of the Morenci-Monticello area, southeastern Arizona and southwestern New Mexico","indexId":"gp838","publicationYear":"1972","noYear":false,"title":"Aeromagnetic map of the Morenci-Monticello area, southeastern Arizona and southwestern New Mexico"},"id":1}],"lastModifiedDate":"2025-07-09T16:14:38.866877","indexId":"gp838","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"838","title":"Aeromagnetic map of the Morenci-Monticello area, southeastern Arizona and southwestern New Mexico","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp838","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Aeromagnetic map of the Morenci-Monticello area, southeastern Arizona and southwestern New Mexico: U.S. Geological Survey Geophysical Investigations Map 838, 1 Plate: 35.23 x 16.50 inches, https://doi.org/10.3133/gp838.","productDescription":"1 Plate: 35.23 x 16.50 inches","costCenters":[],"links":[{"id":491906,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6191.htm","linkFileType":{"id":5,"text":"html"}},{"id":253649,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0838/report-thumb.jpg"},{"id":250167,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0838/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250166,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0838/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Arizona, New Mexico","otherGeospatial":"Morenci-Monticello area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.5,\n              33.75\n            ],\n            [\n              -109.5,\n              33\n            ],\n            [\n              -107.25,\n              33\n            ],\n            [\n              -107.25,\n              33.75\n            ],\n            [\n              -109.5,\n              33.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d86","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":533349,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14137,"text":"ofr74220 - 1972 - Water resources of the Potomac River basin in West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:43","indexId":"ofr74220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"74-220","title":"Water resources of the Potomac River basin in West Virginia","language":"ENGLISH","publisher":"s.n.],","doi":"10.3133/ofr74220","usgsCitation":"Hobba, W., Friel, E.A., and Chisholm, J.L., 1972, Water resources of the Potomac River basin in West Virginia: U.S. Geological Survey Open-File Report 74-220, 1 v. (various pagings) :ill., maps (1 folded, col.) ;28 cm.; (232 p., 3 sheets - PGS), https://doi.org/10.3133/ofr74220.","productDescription":"1 v. (various pagings) :ill., maps (1 folded, col.) ;28 cm.; (232 p., 3 sheets - PGS)","costCenters":[],"links":[{"id":145426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0220/report-thumb.jpg"},{"id":42779,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0220/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42780,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0220/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42781,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0220/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42782,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5ef657","contributors":{"authors":[{"text":"Hobba, W.A.","contributorId":24781,"corporation":false,"usgs":true,"family":"Hobba","given":"W.A.","affiliations":[],"preferred":false,"id":168983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friel, Eugene A.","contributorId":36144,"corporation":false,"usgs":true,"family":"Friel","given":"Eugene","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":168984,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chisholm, James L.","contributorId":77911,"corporation":false,"usgs":true,"family":"Chisholm","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":168985,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":13750,"text":"ofr72395 - 1972 - Documentation and environment of the Apollo 16 samples a preliminary report","interactions":[],"lastModifiedDate":"2013-01-27T17:24:06","indexId":"ofr72395","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-395","title":"Documentation and environment of the Apollo 16 samples a preliminary report","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72395","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Documentation and environment of the Apollo 16 samples a preliminary report: U.S. Geological Survey Open-File Report 72-395, 252 p. :ill. (some folded), folded maps ;27 cm., https://doi.org/10.3133/ofr72395.","productDescription":"252 p. :ill. (some folded), folded maps ;27 cm.","costCenters":[],"links":[{"id":146562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d7cf","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528947,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24790,"text":"ofr72440 - 1972 - Test observation well near Almira, Washington: description and preliminary results","interactions":[],"lastModifiedDate":"2014-05-29T07:25:47","indexId":"ofr72440","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-440","title":"Test observation well near Almira, Washington: description and preliminary results","docAbstract":"<p>A 750-foot test-observation well drilled bear Almira, Wash., is one of several drilled to date (1971) in selected areas if the State. The test wells provide information on ground-water conditions where large-scale pumping from wells is rapidly increasing or ids expected to increase, but where data available from existing wells are incomplete and fail to provide adequate guidance for management of the area;s ground-water resources.</p>\n<br>\n<p>The upper 60 feet of the Almira well has a 10-inch casing below this depth the well is uncased in basalt. Four major aquifer zones are penetrated by the well. Geophysical logging during drilling provided data on hole diameter, water resistivity (mineralization) and temperature, and natural radiation of the rock units. These data supplemented the driller's log as a basis for final selection of the aquifers to be monitored. Two pumping tests showed that (1) when the well was 546 feet deep and was pumped at a rate of about 510 gpm (gallons per minute) for 9 1/2 hours, the specific capacity was 92 gpm per foot of drawndown; and (2) at the final 750-foot depth, with all four aquifers contributing water and the well being pumped at a rate of 525 gpm for 24 hours, the specific capacity was 96 gpm per foot of drawdown. Water from the well when drilled to its final depth of 750 feet is slightly warmer and somewhat more mineralized than when the well was only 546 feet deep.</p>\n<br>\n<p>Four piezometer pipes were installed in the well so that\neach reflected the head in a specific aquifer zone that is\nhydraulically isolated from the other aquifer zones by cement\nseals. The maximum difference in water levels between the\nuppermost and lowermost aquifers after the zones were isolated\nwas 180 feet; the difference may increase somewhat as the\nheads in the aquifers continue to adjust after isolation.\nAn access pipe also was provided for an instrument to measure\nthe geothermal gradient.</p>\n<br>\n<p>The data that have been obtained from the test-observation\nwell and that which will be available from it in the\nfuture are expected to provide invaluable guidance for management of the ground-water resources.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tacoma, WA","doi":"10.3133/ofr72440","issn":"0094-9140","collaboration":"Prepared in cooperation with the State of Washington Department of Ecology","usgsCitation":"Walters, K., 1972, Test observation well near Almira, Washington: description and preliminary results: U.S. Geological Survey Open-File Report 72-440, iii, 20 p., https://doi.org/10.3133/ofr72440.","productDescription":"iii, 20 p.","numberOfPages":"23","costCenters":[],"links":[{"id":287748,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287747,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0440/report.pdf"}],"country":"United States","state":"Washington","city":"Almira","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.0,46.5 ], [ -119.0,48.0 ], [ 117.0,48.0 ], [ 117.0,46.5 ], [ -119.0,46.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684c1b","contributors":{"authors":[{"text":"Walters, Kenneth L.","contributorId":104099,"corporation":false,"usgs":true,"family":"Walters","given":"Kenneth L.","affiliations":[],"preferred":false,"id":192570,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16226,"text":"ofr72376 - 1972 - Potential ground-water resources of the upper John Day River Valley, Grant County, Oregon","interactions":[],"lastModifiedDate":"2025-07-30T21:00:23.779044","indexId":"ofr72376","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-376","title":"Potential ground-water resources of the upper John Day River Valley, Grant County, Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72376","usgsCitation":"Thayer, T.P., 1972, Potential ground-water resources of the upper John Day River Valley, Grant County, Oregon: U.S. Geological Survey Open-File Report 72-376, Report: 8 p.; 3 Plates: 28.03 x 12.16 inches or smaller, https://doi.org/10.3133/ofr72376.","productDescription":"Report: 8 p.; 3 Plates: 28.03 x 12.16 inches or smaller","costCenters":[],"links":[{"id":45150,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0376/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45152,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0376/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":493220,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8714.htm","linkFileType":{"id":5,"text":"html"}},{"id":45151,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0376/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45153,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0376/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149346,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0376/report-thumb.jpg"}],"country":"United States","state":"Oregon","county":"Grant County","otherGeospatial":"upper John Day River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -118.96,\n              44.5\n            ],\n            [\n              -118.96,\n              44.364\n            ],\n            [\n              -118.557,\n              44.364\n            ],\n            [\n              -118.557,\n              44.5\n            ],\n            [\n              -118.96,\n              44.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db6831d2","contributors":{"authors":[{"text":"Thayer, Thomas Prence","contributorId":18371,"corporation":false,"usgs":true,"family":"Thayer","given":"Thomas","email":"","middleInitial":"Prence","affiliations":[],"preferred":false,"id":172452,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22333,"text":"ofr727 - 1972 - Water resources of the Kenai-Soldotna area, Alaska","interactions":[],"lastModifiedDate":"2020-02-25T14:33:04","indexId":"ofr727","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-7","title":"Water resources of the Kenai-Soldotna area, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr727","issn":"0094-9140","usgsCitation":"Anderson, G.S., and Jones, S.H., 1972, Water resources of the Kenai-Soldotna area, Alaska: U.S. Geological Survey Open-File Report 72-7, Report: 81 p.; 2 Plates: 19.01 x 21.13 inches and 19.77 x 21.43 inches, https://doi.org/10.3133/ofr727.","productDescription":"Report: 81 p.; 2 Plates: 19.01 x 21.13 inches and 19.77 x 21.43 inches","costCenters":[],"links":[{"id":51741,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0007/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0007/report-thumb.jpg"},{"id":51742,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0007/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":51743,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Kenai-Soldotna area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -151.4520263671875,\n              60.28613138228136\n            ],\n            [\n              -149.8974609375,\n              60.4165643862813\n            ],\n            [\n              -149.8974609375,\n              60.91441435497479\n            ],\n            [\n              -150.325927734375,\n              61.079544234557304\n            ],\n            [\n              -151.534423828125,\n              60.79402357411143\n            ],\n            [\n              -151.4520263671875,\n              60.28613138228136\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0522","contributors":{"authors":[{"text":"Anderson, G. S.","contributorId":81928,"corporation":false,"usgs":true,"family":"Anderson","given":"G.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":188056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, S. H.","contributorId":68759,"corporation":false,"usgs":true,"family":"Jones","given":"S.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":188055,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22342,"text":"ofr728 - 1972 - Surface water in Duval and Nassau Counties, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:07:51","indexId":"ofr728","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-8","title":"Surface water in Duval and Nassau Counties, Florida","language":"ENGLISH","publisher":"United States Department of the Interior, Geological Survey,","doi":"10.3133/ofr728","issn":"0094-9140","usgsCitation":"Anderson, W., 1972, Surface water in Duval and Nassau Counties, Florida: U.S. Geological Survey Open-File Report 72-8, 64 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr728.","productDescription":"64 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":153609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ee1b","contributors":{"authors":[{"text":"Anderson, Warren","contributorId":7712,"corporation":false,"usgs":true,"family":"Anderson","given":"Warren","affiliations":[],"preferred":false,"id":188071,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38769,"text":"pp585A - 1972 - Hydrologic investigations of prairie potholes in North Dakota, 1959-68","interactions":[],"lastModifiedDate":"2023-01-06T19:52:07.682963","indexId":"pp585A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"585","chapter":"A","title":"Hydrologic investigations of prairie potholes in North Dakota, 1959-68","docAbstract":"<p>A prairie pothole is a depression in the prau1e, capable of storing water, that is the result of glacial processes. Years ago, there were many hundreds of thousands of prairie potholes in the North-Central United States, but large numbers of them have been drained for agricultural use. This report is limited to studies of prairie potholes in the eastern part of the glaciated northern Great Plains region in North Dakota-a rolling upland area covered with glacial drift, called the Coteau du Missouri. Potholes are wetlands that are the primary breeding area of migratory waterfowl in the United States. If production of waterfowl is to continue, suitable wetlands must be maintained, and even new wetlands created to offset those destroyed for agricultural use. The initial stage of the Garrison Diversion Unit calls for a normal annual diversion from Garrison Reservoir of 60,000 acre-feet of water for this purpose. </p><p>Many prairie potholes contain large amounts of emergent aquatic vegetatjon known as hydrophytes. Determining the loss of water by transpiration from emergent hydrophytes was one of the major objectives of the present study of the hydrology of prairie potholes. Other hydrologic factors were studied later, but the first part of the study was devoted almost exclusively to the determination of evaporation and transpiration losses at groups of potholes in Ward, Stutsman, and Dickey Counties. The mass-transfer method was used, and by determining the variation in the mass-transfer coefficient throughout a season, the losses by evaporation and transpiration were determined separately. Separate determinations were accomplished by relating the emergent height and the moisture content of the hydrophytes to the rate of transpiration, as determined by the mass-transfer coefficient. </p><p>Seasonal evaporation from the study potholes clear of vegetation was found to very nearly equal the generalized evaporation values published by the U.S. Weather Bureau. The effect of hydrophytes in potholes was twofold: their presence reduced evaporation from the water surfaces; and, at the height of the growing season, their transpiration rate, added to the reduced evaporation rate, frequently was greater than the evaporation rate from potholes clear of vegetation. </p><p>Net seepage outflow from potholes was generally very small-less than 0.01 foot per day per unit of water surface. This rate of seepage was not insignificant, however, because it often amounted to more than one-fourth of the total seasonal .loss of water from a pothole. </p><p>The source of water supplying the evapotranspiration losses was primarily precipitation on the water surface of a pothole pond. Augmenting this supply was basin inflowoverland flow, flow in channels, and seepage inflow. Of these, overland flow was estimated to have been the largest by far; direct observations were not possible. Basin inflow was very erratic; it depended on combinations of events, such as antecedent soil moisture and rainfall intensity, or depth of snow at time of melting and concurrent rainfall. The occurrences of these combinations were such that, for a given season (October-March or April-September), the total basin inflow generally showed little relation to total precipitation. The greatest inflows were associated with late snowmelt flowing over frozen ground. </p><p>Following the evapotranspiration study, the effects of ground-water movement were investigated. All the study potholes were located in areas of glacial till in order to reduce the effect of seepage in the mass-transfer computations. Accordingly, ground-water movement was not a major factor in the water budget of the study potholes; however, it could be, in potholes located in areas of outwash sands and gravels, and in potholes in glacial till with only temporary ponds. Also, the direction of ground-water movement has a controlling effect on the water quality of a pothole pond. Where there is no seepage outflow or overflow, there is no mechanism for the removal of dissolved solids brought to the pond by basin inflow. Such potholes are saline-some even more so than sea water. Conversely, potholes that receive no seepage inflow generally contain fresh water and are usually not permanent. All conditions between these two extremes were found. </p><p>The permanence of water in a pothole (the extent to which the water body is permanent) and its quality were found to have a direct and significant relation to the species of vegetation that grows under those conditions. In fact, the species of vegetation are excellent indicators of water quality and permanence, and the report contains a table listing the common species used as indicators and the conditions that they indicate.&nbsp;</p><p>Many other facets of the hydrology of prairie potholes were investigated to ensure that no major factor was ignored, and the investigation results are described briefly. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp585A","usgsCitation":"1972, Hydrologic investigations of prairie potholes in North Dakota, 1959-68: U.S. Geological Survey Professional Paper 585, Report: x, 102 p.; 3 Plates: 33.74 x 32.74 inches or smaller, https://doi.org/10.3133/pp585A.","productDescription":"Report: x, 102 p.; 3 Plates: 33.74 x 32.74 inches or smaller","numberOfPages":"114","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science 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,{"id":2510,"text":"wsp2009B - 1972 - Hydrologic interpretations based on infrared imagery of Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp2009B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"2009","chapter":"B","title":"Hydrologic interpretations based on infrared imagery of Long Island, New York","docAbstract":"Six remote-sensing flights over Long Island's north and south shores were made during the period July 13, 1967, to February 25, 1970. Infrared imagery in the 8- to 14-micrometer range was obtained; results varied from poor to excellent in quality. \r\n\r\nThe ability of the RS 7 and Reconofax IV imagers to discern thermal contrasts of as little .as 1 ? to 2?C (Celsius) permitted identification of areas of heavy ground-water discharge. These areas were concentrated primarily along the eroded headlands of the north shore and in the lower reaches of watercourses draining into Great South Bay. Only a few highly localized examples of direct ground-water discharge into the embankments ,along Long Island's south shore were detected in the imagery. \r\n\r\nThermal loading emanating from a powerplant near Oceanside is shown to be quickly dissipated in Middle Bay. Specific examples show that infrared imagery may ,also be used to identify circulation patterns, ice cover, changes in stream-temperature regimen, and the location of sewer outfalls. Optimal time for the collection of infrared imagery for hydrologic studies on Long Island is in summer and in winter, when surface-water thermal differences are relatively large.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2009B","usgsCitation":"Pluhowski, E.J., 1972, Hydrologic interpretations based on infrared imagery of Long Island, New York: U.S. Geological Survey Water Supply Paper 2009, iv B 1-B 20 p. :illus. ;24 cm., https://doi.org/10.3133/wsp2009B.","productDescription":"iv B 1-B 20 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2009b/report-thumb.jpg"},{"id":28663,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2009b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606a7b","contributors":{"authors":[{"text":"Pluhowski, Edward J.","contributorId":87911,"corporation":false,"usgs":true,"family":"Pluhowski","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145315,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38771,"text":"pp585C - 1972 - Ground-water hydrology of prairie potholes in North Dakota","interactions":[],"lastModifiedDate":"2018-03-16T14:10:14","indexId":"pp585C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"585","chapter":"C","title":"Ground-water hydrology of prairie potholes in North Dakota","docAbstract":"<p>Prairie potholes (sloughs) are water-holding depressions of glacial origin in the prairies of the Northern United States and southern Canada. Water is supplied to the potholes by precipitation on the water surface, basin runoff, and seepage inflow of ground water. Depleticn of pothole water results from evapotranspiration, overflow, and seepage outflow. Since potholes generally do not overflow, seepage outflow is the principal way in which dissolved salts can be removed. Salinity of pothole water is therefore a good indication of the seepage balance. Net seepage outflow results in fresh to brackish waters that constitute ephemeral to semipermanent ponds, whereas net seepage inflow results in brackish to saline waters that constitute semipermanent to permanent ponds. </p><p>Because the water table in the glacial deposits is continuous with the water surface in prairie potholes, the watertable gradient is adjusted to the water-surface elevation of the potholes. In cross section the water table is represented by a nearly straight line which connects potholes. The configuration of the water table around a pothole determines the direction of ground-water flow with respect to the pothole. Ground water flows toward the pothole if the adjacent water table is higher than the pothole water surface and flows away from the pothole if the adjacent water table is lower than the pothole water surface. </p><p>Prairie potholes were studied in North Dakota on the Coteau du Missouri, an area of stagnation moraine. About 90 percent of the glacial drift on the Coteau du Missouri is glacial till, and the remainder is largely glacial outwash and lake sediments. Ground-water movement in glacial till is controlled by its lithology and structure. This till, being a poorly sorted, largely unstratified mixture of clay, silt, sand, and gravel, is not highly permeable, so ground water moves most readily along the joints. Because joints in glacial till are most numerous near the land surface (owing to weathering effects), the most active ground-water flow systems are shallow and localized in the vicinity of potholes. As a result, local ground-water flow systems have a noticeable effect on pothole hydrology, particularly the salinity</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of prairie potholes in North Dakota","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp585C","usgsCitation":"Sloan, C.E., 1972, Ground-water hydrology of prairie potholes in North Dakota: U.S. Geological Survey Professional Paper 585, Report: vi, 28 p.; 2 Plates, https://doi.org/10.3133/pp585C.","productDescription":"Report: vi, 28 p.; 2 Plates","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":65643,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0585c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65644,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0585c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65645,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0585c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":104523,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4627.htm","linkFileType":{"id":5,"text":"html"},"description":"4627"},{"id":120412,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0585c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dbf8","contributors":{"authors":[{"text":"Sloan, C. E.","contributorId":59037,"corporation":false,"usgs":true,"family":"Sloan","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":220425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38772,"text":"pp585D - 1972 - Vegetation of prairie potholes, North Dakota, in relation to quality of water and other environmental factors","interactions":[],"lastModifiedDate":"2018-03-16T14:06:00","indexId":"pp585D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"585","chapter":"D","title":"Vegetation of prairie potholes, North Dakota, in relation to quality of water and other environmental factors","docAbstract":"<p>Measurements of specific conductance provide an adequate indication of the average salinity of surface waters in natural ponds and lakes of the northern .prairie region. Yearly and seasonal variations in specific conductance were much greater in brackish and subsaline wetlands than in fresh-water areas. The principal vegetational types. Land-use practices of varying brackish to saline wetlands were sulfates and chlorides of sodium and magnesium. In less saline waters, carbonate and bicarbonate salts of calcium and potassium were of greater importance, but as salinity increased, the proportion of these compounds decreased rapidly.</p><p>A major environmental factor controlling the establishment of marsh and aquatic vegetation is the permanence of surface water. Permanence is a measure of the extent to which surface water persists at a given site. Varying degrees of water permanence during the growing season led to the establishment of distinct vegetational types, which were differentiated primarily on the 'basis of community structure or life form of the dominant vegetation.</p><p>Salinity of surface waters was closely correlated with differences in species composition of plant communities found in the principal vegetational types. Land-use practices of varying degrees of intensity also had a secondary influence on species composition. Since an unstable water chemistry is characteristic of most prairie ponds and lakes, it is more reliable to use the plant communities as indicators of average salinity than to use single measurements of specific conductance.</p><p>Characteristic species of wetland vegetational types occupied the central deeper parts of pond and lake basins or occurred as concentric peripheral bands. The wetland vegetational types are wetland low-prairie, wet-meadow, shallow-marsh emergent, deep-marsh emergent, fen emergent, submerged and floating, natural drawdown, cropland drawdown, and cropland tillage vegetation. Combinations of species (plant associations) within these vegetational types were placed in one of six salinity categories designated as fresh, slightly brackish, moderately brackish, brackish, subsaline, and saline. Salt tolerance apparently varied greatly among the various marsh and aquatic plants since the num'ber of species represented in moderately brackish&nbsp;to saline communities decreased markedly with increased salinity of the surface water environment. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of prairie potholes in North Dakota","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp585D","usgsCitation":"Stewart, R.E., and Kantrud, H., 1972, Vegetation of prairie potholes, North Dakota, in relation to quality of water and other environmental factors: U.S. Geological Survey Professional Paper 585, 35 p., https://doi.org/10.3133/pp585D.","productDescription":"35 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":480,"text":"Northern Prairie Wildlife Research Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":22019,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0585d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170479,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0585d/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db6025cb","contributors":{"authors":[{"text":"Stewart, R. E.","contributorId":93426,"corporation":false,"usgs":true,"family":"Stewart","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":220427,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kantrud, H.A.","contributorId":28553,"corporation":false,"usgs":true,"family":"Kantrud","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":220426,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56317,"text":"wdrMI711 - 1972 - Water resources data for Michigan, water year 1971; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2017-07-12T14:35:07","indexId":"wdrMI711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MI-71-1","title":"Water resources data for Michigan, water year 1971; Part 1, Surface water records","docAbstract":"<p>Surface-water records for the 1971 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Michigan 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 T. R. Cummings, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Michigan. </p><p>Records of discharge and stage of streams, and contents and stage of lakes or reservoirs are published in a series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Through September 30, 1960, these water-supply papers were in an annual series and since then are in a 5-year series. 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 Michigan were contained in Part 4 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.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMI711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Michigan, water year 1971; Part 1, Surface water records: U.S. Geological Survey Water Data Report MI-71-1, ix, 271 p., https://doi.org/10.3133/wdrMI711.","productDescription":"ix, 271 p.","numberOfPages":"286","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":343741,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/mi-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/mi-71-1/report-thumb.jpg"}],"country":"United 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,{"id":39583,"text":"pp800C - 1972 - Geological Survey research 1972, Chapter C","interactions":[],"lastModifiedDate":"2023-09-27T21:12:22.126609","indexId":"pp800C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"800","chapter":"C","title":"Geological Survey research 1972, Chapter C","docAbstract":"<p>This collection of 37 short papers is the second published chapter of \"Geological Survey Research 1972.\" The papers report on scientific and economic results of current work by members of the Conservation, Geologic, and Water Resources Divisions of the U.S. Geological Survey.</p><p>Chapter A, to be published later in the year, will present a summary of significant results of work done ~n fiscal year 1972, together with lists of investigations in progress, cooperating agencies, and Geological Survey offices.</p><p>\"Geological Survey Research 1972\" is the thirteenth volume of the annual series Geological Survey Research. The twelve volumes already published are listed below, with their series designations.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp800C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Geological Survey research 1972, Chapter C: U.S. Geological Survey Professional Paper 800, v, 283 p., https://doi.org/10.3133/pp800C.","productDescription":"v, 283 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":421294,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31369.htm","linkFileType":{"id":5,"text":"html"}},{"id":67167,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0800c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119829,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0800c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee92a","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529921,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48022,"text":"ofr7297 - 1972 - Ground-water outflow, San Timoteo-Smiley Heights area, upper Santa Ana Valley, southern California, 1927 through 1968","interactions":[],"lastModifiedDate":"2022-09-16T19:31:03.070135","indexId":"ofr7297","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-97","title":"Ground-water outflow, San Timoteo-Smiley Heights area, upper Santa Ana Valley, southern California, 1927 through 1968","docAbstract":"The San Timoteo-Smiley Heights area is in the upper Santa Ana Valley, San Bernardino and Riverside Counties, Calif., where the Yucaipa and San Timoteo-Beaumont ground-water basins border Bunker .Hill basin on the south between the San Jacinto and San Andreas faults. The area is broken by numerous faults, the topography is rough, and in a large part of the area few wells had been drilled prior to 196S. \r\n\r\nThe alluvial deposits, which constitute the aquifers in the area, range in thickness from 0 where they lap onto exposed bedrock hills to about 1,000 feet. Beneath the southern part of the area near the San Jacinto fault the total thickness of alluvial and lacustrine deposits may be as much as 6,000 feet. \r\n\r\nThe purpose of this study was to estimate ground-water outflow by an indirect method not involving balancing of the hydrologic budget. For this purpose it was necessary to estimate the permeability of the aquifer materials, the average annual hydraulic gradient, and the cross-sectional area through which the flow occurs; these values were estimated for five segments along a line of section between the San Jacinto fault and Crafton Hills. \r\n\r\nTo provide data for the outflow estimates, several miles of reflection and refraction seismic traverses were made along and across the outflow section. Nineteen deep and shallow test holes were drilled; one of the deep test holes and several existing wells were pumped to obtain data on aquifer permeability.\r\n\r\nThe estimated average permeabilities of the aquifer materials range from 5 gallons per day per square foot for the lower part of the San Timoteo beds of Frick (1921) and 40 gallons per day per square foot for the older alluvium to 220 gallons per day per square foot for the upper part of the San Timoteo beds. \r\n\r\nThe estimated outflow in 1927 was 8,150 acre-feet. By 1967 the estimated total outflow was 5,350 acre-feet, a reduction of approximately 34 percent. During the 12-year period 1956 through 1967, however, the annual outflow decline has been considerably less than the average for the 41-year period 1927 through 1967, and the decline as of 1968 was probably about 30-35 acre-feet per year.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7297","usgsCitation":"Dutcher, L., and Fenzel, F., 1972, Ground-water outflow, San Timoteo-Smiley Heights area, upper Santa Ana Valley, southern California, 1927 through 1968: U.S. Geological Survey Open-File Report 72-97, Report: ii, 30 p.; 2 Plates: 35.22 × 22.43 inches and 33.72 × 22.76 inches, https://doi.org/10.3133/ofr7297.","productDescription":"Report: ii, 30 p.; 2 Plates: 35.22 × 22.43 inches and 33.72 × 22.76 inches","costCenters":[],"links":[{"id":110340,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52161.htm","linkFileType":{"id":5,"text":"html"},"description":"52161"},{"id":84797,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0097/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84796,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0097/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84795,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0097/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":161751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0097/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Timoteo-Smiley Heights area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.2431,\n              33.9756\n            ],\n            [\n              -117.0681,\n              33.9756\n            ],\n            [\n              -117.0681,\n              34.0778\n            ],\n            [\n              -117.2431,\n              34.0778\n            ],\n            [\n              -117.2431,\n              33.9756\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66741d","contributors":{"authors":[{"text":"Dutcher, L.C.","contributorId":42191,"corporation":false,"usgs":true,"family":"Dutcher","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":236685,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fenzel, F. W.","contributorId":94742,"corporation":false,"usgs":true,"family":"Fenzel","given":"F. W.","affiliations":[],"preferred":false,"id":236686,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2514,"text":"wsp2025 - 1972 - Glossary of selected terms useful in studies of the mechanics of aquifer systems and land subsidence due to fluid withdrawal","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp2025","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"2025","title":"Glossary of selected terms useful in studies of the mechanics of aquifer systems and land subsidence due to fluid withdrawal","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2025","usgsCitation":"Poland, J.F., Lofgren, B.E., and Riley, F.S., 1972, Glossary of selected terms useful in studies of the mechanics of aquifer systems and land subsidence due to fluid withdrawal: U.S. Geological Survey Water Supply Paper 2025, iv, 9 p. ;24 cm., https://doi.org/10.3133/wsp2025.","productDescription":"iv, 9 p. ;24 cm.","costCenters":[],"links":[{"id":138792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2025/report-thumb.jpg"},{"id":28696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2025/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abee4b07f02db67473a","contributors":{"authors":[{"text":"Poland, J. F.","contributorId":64223,"corporation":false,"usgs":true,"family":"Poland","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145323,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lofgren, B. E.","contributorId":42579,"corporation":false,"usgs":true,"family":"Lofgren","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":145322,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Riley, Francis S.","contributorId":93028,"corporation":false,"usgs":true,"family":"Riley","given":"Francis","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145324,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56755,"text":"wdrMS711 - 1972 - Water resources data for Mississippi, water year 1971","interactions":[],"lastModifiedDate":"2025-08-28T14:25:18.228863","indexId":"wdrMS711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MS-71-1","title":"Water resources data for Mississippi, water year 1971","docAbstract":"<p>Water resources data for the 1971 water year for Mississippi including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, and records of water-quality data on the chemical and physical characteristics of surface water, are given in this report. In Part 1, records are included for 71 gaging stations of which 67 are streamflow discharge stations, and 4 are reservoir or lake stations; also are included records for 27 low-flow partial-record stations, 143 crest-stage partial-record stations, and 91 miscellaneous sites. Locations of gaging stations are shown in Figure 1. In Part 2, data on the quality of surface water (chemical and temperature) were collected from designated sampling sites at pre-determined intervals such as monthly, or less frequently, and at one site data were recorded on punched paper tape at 60-minute intervals. Records are given for 55 sampling stations of which 5 are continuous record stations, 26 are partial-record stations, and 3 are miscellaneous sites. Locations of water-quality stations are shown in Figure 1. A few pertinent stations (not included above) in bordering States are also included in this report. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of L. E. Carroon, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Mississippi. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMS711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Mississippi, water year 1971: U.S. Geological Survey Water Data Report MS-71-1, vii, 180 p., https://doi.org/10.3133/wdrMS711.","productDescription":"vii, 180 p.","costCenters":[],"links":[{"id":494996,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/ms-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175273,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/ms-71-1/report-thumb.jpg"}],"country":"United 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,{"id":38736,"text":"pp627F - 1972 - Summary of the hydrologic situation on Long Island, New York, as a guide to water-management alternatives","interactions":[],"lastModifiedDate":"2025-04-15T19:41:42.123747","indexId":"pp627F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"627","chapter":"F","title":"Summary of the hydrologic situation on Long Island, New York, as a guide to water-management alternatives","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology and some effects of urbanization on Long Island, New York (Professional Paper 627)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp627F","usgsCitation":"Franke, O., and McClymonds, N.E., 1972, Summary of the hydrologic situation on Long Island, New York, as a guide to water-management alternatives: U.S. Geological Survey Professional Paper 627, 58 p., https://doi.org/10.3133/pp627F.","productDescription":"58 p.","costCenters":[],"links":[{"id":65598,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0627f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119578,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0627f/report-thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.82194273612976,\n              41.07786507528178\n            ],\n            [\n              -72.20943503836517,\n              41.2154243330921\n            ],\n            [\n              -73.59610391993449,\n              40.940017333637996\n            ],\n            [\n              -73.79358198591106,\n              40.79824207303625\n            ],\n            [\n              -73.86178655629323,\n              40.79599717030078\n            ],\n            [\n              -73.9096568448226,\n              40.794714334653065\n            ],\n            [\n              -73.93592195888237,\n              40.77675203289462\n            ],\n            [\n              -73.9668470125343,\n              40.739849931946566\n            ],\n            [\n              -73.97531962997304,\n              40.70999238292043\n            ],\n            [\n              -74.00624468362446,\n              40.699073376332024\n            ],\n            [\n              -74.02446081111779,\n              40.67819382271807\n            ],\n            [\n              -74.05199681779393,\n              40.62451943874552\n            ],\n            [\n              -74.00158426558416,\n              40.54988209243214\n            ],\n            [\n              -73.92660160125092,\n              40.526379869031246\n            ],\n            [\n              -73.0763843222474,\n              40.624838818992174\n            ],\n            [\n              -72.36934591632716,\n              40.86170639680046\n            ],\n            [\n              -71.84784461657901,\n              41.0482487530538\n            ],\n            [\n              -71.82194273612976,\n              41.07786507528178\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6980ed","contributors":{"authors":[{"text":"Franke, O.L.","contributorId":57082,"corporation":false,"usgs":true,"family":"Franke","given":"O.L.","affiliations":[],"preferred":false,"id":220366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McClymonds, N. E.","contributorId":94653,"corporation":false,"usgs":true,"family":"McClymonds","given":"N.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":220367,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56750,"text":"wdrWA711 - 1972 - Water resources data for Washington, water year 1971; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2022-12-27T17:57:48.379983","indexId":"wdrWA711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WA-71-1","title":"Water resources data for Washington, water year 1971; Part 1, Surface water records","docAbstract":"<p>Surface-water records for the 1971 water year for Washington, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report and their locations shown in figures 1, 2. Records for a few pertinent gaging stations in bordering States also are included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of L. B. Laird, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA711","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Washington, water year 1971; Part 1, Surface water records: U.S. Geological Survey Water Data Report WA-71-1, xiv, 427 p., https://doi.org/10.3133/wdrWA711.","productDescription":"xiv, 427 p.","costCenters":[],"links":[{"id":411073,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/wa-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175193,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/wa-71-1/report-thumb.jpg"}],"country":"United 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,{"id":56739,"text":"wdrNY711 - 1972 - Water resources data for New York water year 1971; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2020-12-14T23:24:32.38053","indexId":"wdrNY711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NY-71-1","title":"Water resources data for New York water year 1971; Part 1, Surface water records","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for New York water year 1971; Part 1, Surface water records: U.S. Geological Survey Water Data Report NY-71-1, ix, 311 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,{"id":41657,"text":"ofr72387 - 1972 - Aeromagnetic map of parts of the Richfield and Cedar City 1° by 2° quadrangles, Utah","interactions":[],"lastModifiedDate":"2021-11-18T21:22:34.549789","indexId":"ofr72387","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-387","title":"Aeromagnetic map of parts of the Richfield and Cedar City 1° by 2° quadrangles, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72387","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Aeromagnetic map of parts of the Richfield and Cedar City 1° by 2° quadrangles, Utah: U.S. Geological Survey Open-File Report 72-387, 1 Plate: 30.90 × 36.53 inches, https://doi.org/10.3133/ofr72387.","productDescription":"1 Plate: 30.90 × 36.53 inches","costCenters":[],"links":[{"id":175546,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":391892,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8719.htm"},{"id":79374,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0387/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Nevada","otherGeospatial":"Richfield and Cedar City 1° by 2° quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114,\n              37\n            ],\n            [\n              -112.625,\n              37\n            ],\n            [\n              -112.625,\n              38.5\n            ],\n            [\n              -114,\n              38.5\n            ],\n            [\n              -114,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69748d","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530546,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2638,"text":"wsp1873C - 1972 - Physical, chemical, and biological aspects of the Duwamish River Estuary, King County, Washington, 1963-67","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1873C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1873","chapter":"C","title":"Physical, chemical, and biological aspects of the Duwamish River Estuary, King County, Washington, 1963-67","docAbstract":"This report describes the significant results to 1967 of a comprehensive study that began in 1963 to evaluate what changes take place in an estuary as the loads .of raw and partially treated industrial and municipal wastes are replaced by effluent from a secondary treatment plant. The study area is the Duwamish River estuary, about 18.3 river kilometers long. At mean sea level the estuary has a water-surface area of about 1 square mile and a mean width of 440 feet. At the lowest and highest recorded tides, the volume of the estuary is about 205 and 592 million cubic feet, respectively. The estuary is well stratified (salt-wedge type) at fresh-water inflows greater than 1,000 cfs \r\n(cubic feet per second), but when inflow rates are less than 1,000 cfs the lower 5.6 kilometers of the estuary grades into the partly mixed type. The crosschannel salinity distribution is uniform for a given location and depth. Salinity migration is controlled by tides and fresh-water inflow. At fresh-water inflow rates greater than 1,000 cfs, water in the upper 8.4 kilometers of the estuary is always fresh regardless of tide. At inflow rates less than 600 cfs and tide heights greater than 10 feet; some salinity has been detected 16.1 kilometers above the mouth of the estuary. Studies using a fluorescent dye show that virtually no downward mixing into the salt wedge occurs; soluble pollutants introduced at the upper end of the estuary stay in the surface layer (5-15 ft thick). On the basis of dye studies when fresh-water inflow is less than 400 cfs, it is estimated that less than 10 percent of a pollutant will remain in the estuary a minimum of 7 days. Longitudinal dispersion coefficients for the surface layer have been determined to be on the order of 100-400 square feet per second. \r\n\r\nFour water-quality stations automatically monitor DO (dissolved oxygen), water temperature, pH, and specific conductance; at one station solar radiation also is measured. DO concentration in the surface layer decreases almost linearly in a downstream direction. Minimum DO concentration in the surface layer is usually greater than 4 rag/1 (milligrams per liter). The smallest DO values are consistently recorded in the bottom layer at the station 7.7 kilometers above the mouth; monthly means of less than 3 mg/1 of DO have occurred at this point. Manual sampling shows that the DO sag in the bottom layer oscillates between 7.7 and 10.4 kilometers above the mouth of the estuary. Multiple-regression analysis shows that the surface DO content can be estimated from the fresh-water inflow and water temperature. Tidal exchange and fresh-water inflow indirectly control the bottom DO content. Information available from previous studies failed to indicate a progressive decrease in DO content during the period 1949-56, but data from the present study suggest a slight general decrease in the annual minimum DO concentrations in both the upper and lower layers. Average nitrate concentration in fresh water at station 16.2 has increased progressively since 1964, by amounts greater than those which can be attributed to the Renton Treatment Plant, 4.3 kilometers upstream from station 16.2. \r\n\r\nThe BOD (biochemical oxygen demand) in both surface and bottom layers is generally less than 4 rag/1 of oxygen, but values greater than 6 rag/1 have been measured during a period of phytoplankton bloom. Phytoplankton blooms can occur during periods of minimum tidal exchange and fresh-water inflows of less than 300 cfs if solar radiation and water temperature are optimum. Nutrients (nitrogen and phosphorus compounds) do not control the occurrence of a bloom, because sufficient quantities of these nutrients are always present. Nutrients in the treated effluent may increase the biomass of the bloom. Trace-element studies have not defined any role that these elements may play in algal growth. \r\nThe inflowing fresh water contains principally calcium and bicarbonate and \r\nhas a dissolved-solids content ra","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1873C","usgsCitation":"Santos, J.F., and Stoner, J., 1972, Physical, chemical, and biological aspects of the Duwamish River Estuary, King County, Washington, 1963-67: U.S. Geological Survey Water Supply Paper 1873, vi, 74 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1873C.","productDescription":"vi, 74 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138728,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1873c/report-thumb.jpg"},{"id":28957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1873c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ac0","contributors":{"authors":[{"text":"Santos, John F.","contributorId":21530,"corporation":false,"usgs":true,"family":"Santos","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":145542,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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