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Two volumes: Part 1, Data summary; Part 2, Basic data","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59c22cb5e4b091459a61b748","contributors":{"authors":[{"text":"Brennan, Robert","contributorId":105695,"corporation":false,"usgs":true,"family":"Brennan","given":"Robert","email":"","affiliations":[],"preferred":false,"id":710797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grozier, Richard Ural","contributorId":75806,"corporation":false,"usgs":true,"family":"Grozier","given":"Richard","email":"","middleInitial":"Ural","affiliations":[],"preferred":false,"id":710798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42597,"text":"ofr76698 - 1976 - Residual magnetic intensity map, Coso Hot Springs, California","interactions":[],"lastModifiedDate":"2023-04-27T18:55:43.389545","indexId":"ofr76698","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"76-698","title":"Residual magnetic intensity map, Coso Hot Springs, California","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76698","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Residual magnetic intensity map, Coso Hot Springs, California: U.S. Geological Survey Open-File Report 76-698, 1 Plate: 33.75 x 34.76 inches, https://doi.org/10.3133/ofr76698.","productDescription":"1 Plate: 33.75 x 34.76 inches","costCenters":[],"links":[{"id":168323,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":416451,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15401.htm","linkFileType":{"id":5,"text":"html"}},{"id":80367,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0698/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"California","otherGeospatial":"Coso Hot Springs","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -118.041,\n 36.25\n ],\n [\n -118.041,\n 35.813\n ],\n [\n -117.481,\n 35.813\n ],\n [\n -117.481,\n 36.25\n ],\n [\n -118.041,\n 36.25\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b9d6","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":530931,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":10772,"text":"ofr76600 - 1976 - Change in methylene blue active substances and chloride levels in streams in Suffolk County, New York, 1961-1976","interactions":[],"lastModifiedDate":"2023-01-24T19:26:10.143426","indexId":"ofr76600","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"76-600","title":"Change in methylene blue active substances and chloride levels in streams in Suffolk County, New York, 1961-1976","docAbstract":"Since 1961, concentrations of methylene blue active substances and chloride were measured in samples collected at 67 sampling stations on 44 streams in Suffolk County, Long Island, New York. Changes in the concentrations of these constituents and calculated chloride/methylene blue active substances ratios are reported. Although many factors--the 1962 to 1966 drought, urbanization, change in detergent formulation, and the 1971 Suffolk County detergent ban--make specific interpretation of the data difficult, it appears that the quality of water in streams and, consequently, that part of the upper glacial aquifer supplying water to the streams, is improving in terms of the concentration of methylene blue active substances.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76600","collaboration":"Prepared in cooperation with the Suffolk County Department of Environmental Control and the Suffolk County Water Authority","usgsCitation":"Ragone, S.E., Guerrera, A.A., and Flipse, W., 1976, Change in methylene blue active substances and chloride levels in streams in Suffolk County, New York, 1961-1976: U.S. Geological Survey Open-File Report 76-600, 65 p., https://doi.org/10.3133/ofr76600.","productDescription":"65 p.","costCenters":[],"links":[{"id":412284,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0600/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143533,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0600/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Suffolk County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6dbd","contributors":{"authors":[{"text":"Ragone, Stephen E.","contributorId":74374,"corporation":false,"usgs":true,"family":"Ragone","given":"Stephen","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":161940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guerrera, August A.","contributorId":35321,"corporation":false,"usgs":true,"family":"Guerrera","given":"August","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":161938,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flipse, W.J. Jr.","contributorId":98733,"corporation":false,"usgs":true,"family":"Flipse","given":"W.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":161939,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":21182,"text":"ofr76428 - 1976 - Conditions in the deeper parts of the hot spring systems of Yellowstone National Park, Wyoming","interactions":[],"lastModifiedDate":"2022-09-13T18:28:43.808532","indexId":"ofr76428","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"76-428","title":"Conditions in the deeper parts of the hot spring systems of Yellowstone National Park, Wyoming","docAbstract":"Yellowstone thermal areas are scattered over an area of nearly 50 x 60 kilometers (Fig. 1) and contain waters of diverse compositions. This has lead to the implicit assumption that Yellowstone consisted of discrete hydrothermal systems (e.g., Fournier and Truesdell, 1970). It is the purpose of this paper to suggest that these systems may be separate only near the surface and that there may exist at depth a large, relatively homogeneous body of water at 340 to 370°C containing about 1,000 ppm NaCl. This deep thermal water flows upwards losing steam into the near-surface geyser and hot spring systems where it undergoes variable amounts of dilution with cold meteoric water, reaction with rocks, and further steam loss to produce all of the hot spring waters of the Park. The evidence for these conclusions is from the application of chemical and isotopic geothermometers, from relationships between the chloride concentrations and subsurface heat contents of thermal waters, from the chemical and isotopic compositions of the waters, and from geophysical evidence.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76428","usgsCitation":"Truesdell, A.H., and Fournier, R.O., 1976, Conditions in the deeper parts of the hot spring systems of Yellowstone National Park, Wyoming: U.S. Geological Survey Open-File Report 76-428, 22 p., https://doi.org/10.3133/ofr76428.","productDescription":"22 p.","costCenters":[],"links":[{"id":153050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0428/report-thumb.jpg"},{"id":406615,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0428/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Yellowstone National Park","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -111.04705810546874,\n 44.1526518281754\n ],\n [\n -109.99786376953125,\n 44.1526518281754\n ],\n [\n -109.99786376953125,\n 44.88506649401471\n ],\n [\n -111.04705810546874,\n 44.88506649401471\n ],\n [\n -111.04705810546874,\n 44.1526518281754\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b14e4b07f02db6a47bc","contributors":{"authors":[{"text":"Truesdell, Alfred Hemingway","contributorId":106137,"corporation":false,"usgs":true,"family":"Truesdell","given":"Alfred","email":"","middleInitial":"Hemingway","affiliations":[],"preferred":false,"id":183986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fournier, Robert O.","contributorId":73202,"corporation":false,"usgs":true,"family":"Fournier","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":183985,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14344,"text":"ofr75650 - 1976 - A method for estimating magnitude and frequency of floods in Montana","interactions":[{"subject":{"id":40731,"text":"ofr6722 - 1967 - Magnitude and frequency of floods from drainage areas less than 100 square miles in Montana","indexId":"ofr6722","publicationYear":"1967","noYear":false,"title":"Magnitude and frequency of floods from drainage areas less than 100 square miles in Montana"},"predicate":"SUPERSEDED_BY","object":{"id":14344,"text":"ofr75650 - 1976 - A method for estimating magnitude and frequency of floods in Montana","indexId":"ofr75650","publicationYear":"1976","noYear":false,"title":"A method for estimating magnitude and frequency of floods in Montana"},"id":1}],"lastModifiedDate":"2023-08-30T18:52:08.189433","indexId":"ofr75650","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"75-650","title":"A method for estimating magnitude and frequency of floods in Montana","docAbstract":"This report provides methods for estimating flood characteristics at most natural flow sites on rural streams in Montana. It also contains significant flood data and related information for many gaged sites on Montana streams. Frequency curves are provided for 442 gaged sites as defined by log-Pearson Type III analysis. To allow estimates at ungaged sites, mathematical equations relate the 2-, 5-, 10-, 25-, 50-, and 100-year flood magnitudes to basin characteristics. Drainage area, main channel slope, and mean annual precipitation were found to be the most significant estimating variables. Equations presented are limited to use on streams with drainage areas from about 0.1 to 2,600 square miles (0.3 to 6,700 square kilometres), with slope from about 5 to 1,200 feet per mile (1.5 to 366 metres per kilometre), and with precipitation from 10 to 100 inches (250 to 2,500 millimetres). \r\n\r\nNomographs provide a simple graphical means of solving the estimating relations, and illustrative examples are presented.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75650","usgsCitation":"Johnson, M.V., and Omang, R.J., 1976, A method for estimating magnitude and frequency of floods in Montana: U.S. Geological Survey Open-File Report 75-650, Report: iv, 35 p.; 3 Plates: 21.08 x 22.74 inches or smaller, https://doi.org/10.3133/ofr75650.","productDescription":"Report: iv, 35 p.; 3 Plates: 21.08 x 22.74 inches or smaller","costCenters":[],"links":[{"id":420320,"rank":6,"type":{"id":36,"text":"NGMDB Index 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae137","contributors":{"authors":[{"text":"Johnson, M. V.","contributorId":95476,"corporation":false,"usgs":true,"family":"Johnson","given":"M.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":169294,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":169293,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":14195,"text":"ofr76152 - 1976 - Audio-magnetotelluric data log, station location map, and telluric profile data for the Elko Hot Springs Known Geothermal Resource Area (KGRA), Nevada","interactions":[],"lastModifiedDate":"2024-06-25T17:51:44.339312","indexId":"ofr76152","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"76-152","title":"Audio-magnetotelluric data log, station location map, and telluric profile data for the Elko Hot Springs Known Geothermal Resource Area (KGRA), Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76152","usgsCitation":"Hoover, D.B., Brougham, G.W., and Clark, J., 1976, Audio-magnetotelluric data log, station location map, and telluric profile data for the Elko Hot Springs Known Geothermal Resource Area (KGRA), Nevada: U.S. Geological Survey Open-File Report 76-152, 7 p., https://doi.org/10.3133/ofr76152.","productDescription":"7 p.","costCenters":[],"links":[{"id":145688,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6682e3","contributors":{"authors":[{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":169057,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brougham, Gary W.","contributorId":108122,"corporation":false,"usgs":true,"family":"Brougham","given":"Gary","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":169058,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Clark, John","contributorId":34145,"corporation":false,"usgs":true,"family":"Clark","given":"John","affiliations":[],"preferred":false,"id":169056,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":42222,"text":"ofr76280 - 1976 - Bouguer gravity map of Moscow, Idaho-Pullman, Washington area","interactions":[],"lastModifiedDate":"2023-03-02T22:49:52.26203","indexId":"ofr76280","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"76-280","title":"Bouguer gravity map of Moscow, Idaho-Pullman, Washington area","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76280","usgsCitation":"Gregory, D.I., and Jackson, D.B., 1976, Bouguer gravity map of Moscow, Idaho-Pullman, Washington area: U.S. Geological Survey Open-File Report 76-280, 1 Plate: 27.09 x 25.48 inches, https://doi.org/10.3133/ofr76280.","productDescription":"1 Plate: 27.09 x 25.48 inches","costCenters":[],"links":[{"id":168559,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413635,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15286.htm","linkFileType":{"id":5,"text":"html"}},{"id":79980,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0280/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Washington","city":"Moscow, Pullman","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.375,\n 46.875\n ],\n [\n -117.375,\n 46.6\n ],\n [\n -116.875,\n 46.6\n ],\n [\n -116.875,\n 46.875\n ],\n [\n -117.375,\n 46.875\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fce98","contributors":{"authors":[{"text":"Gregory, Daniel I.","contributorId":98723,"corporation":false,"usgs":true,"family":"Gregory","given":"Daniel","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":226119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackson, Dallas B.","contributorId":19947,"corporation":false,"usgs":true,"family":"Jackson","given":"Dallas","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":226118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13587,"text":"ofr7682 - 1976 - Geohydrology and water supply, Shemya Island, Alaska","interactions":[],"lastModifiedDate":"2023-03-23T19:53:59.589517","indexId":"ofr7682","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"76-82","title":"Geohydrology and water supply, Shemya Island, Alaska","docAbstract":"Sheyma Island, Alaska, was occupied as a military base in 1942. Since that time, potable water has been supplied by streams, lakes, wells, and in the late 1950's, a gallery system. The island is a low-lying, wave-cut platform composed of pyroclastic and volcanic rocks with some intrusives. Bedrock is overlain by thin glacial deposits. Most of the island 's present surface is relatively thick peat deposits. On the southern and western sides of the island active sand dunes are present. Ground-water supplies are limited by the dense bedrock; only a small amount of water penetrates into fracture systems. Most ground-water movement is in the overlying glacial and peat deposits. Ground water moves generally from north to south across the island. Currently water supplies are drawn from the gallery system which is capable of providing about 200,000 gallons per day. An emergency water supply is available from two wells. Additional supplies could be developed by either adding to the existing gallery or constructing an additional gallery near the present gallery system. The chemical quality of water analyzed from the gallery well generally approximates that of surface water on the island. None of the constituents in samples from streams, lakes, or ground water, except the August 27, 1970, analysis for Lower Lake, exceed the recommended limits for drinking water (Environmental Protection Agency, 1973).
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7682","usgsCitation":"Feulner, A.J., Zenone, C., and Reed, K.M., 1976, Geohydrology and water supply, Shemya Island, Alaska: U.S. Geological Survey Open-File Report 76-82, 1 Plate: 30.42 x 26.07 inches, https://doi.org/10.3133/ofr7682.","productDescription":"1 Plate: 30.42 x 26.07 inches","costCenters":[],"links":[{"id":147076,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414654,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15435.htm","linkFileType":{"id":5,"text":"html"}},{"id":42105,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0082/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Shemya Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 174.05425444829967,\n 52.750148768881076\n ],\n [\n 174.05425444829967,\n 52.70189105722818\n ],\n [\n 174.15968017055042,\n 52.70189105722818\n ],\n [\n 174.15968017055042,\n 52.750148768881076\n ],\n [\n 174.05425444829967,\n 52.750148768881076\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b2f","contributors":{"authors":[{"text":"Feulner, Alvin John","contributorId":32169,"corporation":false,"usgs":true,"family":"Feulner","given":"Alvin","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":168069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zenone, Chester","contributorId":8094,"corporation":false,"usgs":true,"family":"Zenone","given":"Chester","email":"","affiliations":[],"preferred":false,"id":168068,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, K. M.","contributorId":93888,"corporation":false,"usgs":true,"family":"Reed","given":"K.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":168070,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":43449,"text":"ofr76130 - 1976 - Land use and land cover map for Cartersville, Georgia","interactions":[],"lastModifiedDate":"2024-02-06T22:32:01.072407","indexId":"ofr76130","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","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":"76-130","title":"Land use and land cover map for Cartersville, Georgia","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76130","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover map for Cartersville, Georgia: U.S. Geological Survey Open-File Report 76-130, 1 Plate, https://doi.org/10.3133/ofr76130.","productDescription":"1 Plate","costCenters":[],"links":[{"id":120487,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_76_130.gif"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae503","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":531176,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14555,"text":"ofr75434 - 1975 - Relation of water level and fish availability to wood stork reproduction in the southern Everglades, Florida","interactions":[],"lastModifiedDate":"2022-01-04T17:13:41.741677","indexId":"ofr75434","displayToPublicDate":"2022-01-03T22:10:00","publicationYear":"1975","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":"75-434","title":"Relation of water level and fish availability to wood stork reproduction in the southern Everglades, Florida","docAbstract":"The wood stork is a species of colonial wading bird in the Everglades that is most sensitive to changes in the availability of food. Previous studies have shown that the initiation and success of wood stork nesting depends on high densities of fish concentrated in ponds and other catchment basins during the dry season. The extreme dependence of the wood stork on the cyclic hydrologic regime of the southern Florida wetlands makes it an indicator of the well-being and ecological stability of the Everglades. \r\n\r\nThe wood stork has declined in numbers over the last 25 years. One reason for the decline in wood stork population was the change in the hydrologic regimen of the Everglades which affected the feeding habitat and the food production. \r\n\r\nThe fish on which the wood stork feeds increase in density during the dry season as water levels fall. In the Everglades marsh, densities were highest in front of the drying edge of surface water at a depth of about 0.3 m. Dry-season densities were greatest when a drought occurred the previous year. \r\n\r\nHistorically wood stork nesting success was associated with high summer water levels, high rates of surface-water discharge and high rates of drying. Before the closure of the south side of Conservation Area 3 in 1962, years of successful and unsuccessful nesting were characterized by different patterns of drying. These patterns changed after 1962 and generally the predictability of successful nesting breaks down thereafter. Only two nesting years after 1962 were successful and in only one of these was the drying rate similar to years of successful nesting before 1962. Two other potentially successful years failed after 1962. This suggests that further changes in the hydrobiological relations occurred within the Everglades after 1962. \r\n\r\nLack of successful nesting after 1962 can be attributed in large part to late colony formation and the interruption of nesting by winter rainfall. In this period (1962-72), colonies formed earlier in years of high early drying rates than in years of low early drying rates. Delay of colony formation is ultimately the result of inability to attain a suitable nutritional state since food supply is the primary factor in the initiation of nesting. Many of the complex food associations of the wood stork remain to be explained.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr75434","collaboration":"Prepared in cooperation with the U.S. National Park Service","usgsCitation":"Kushlan, J.A., Ogden, J.C., and Higer, A.L., 1975, Relation of water level and fish availability to wood stork reproduction in the southern Everglades, Florida: U.S. Geological Survey Open-File Report 75-434, 56 p., https://doi.org/10.3133/ofr75434.","productDescription":"56 p.","startPage":"1","endPage":"56","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":994,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0434/ofr75434.pdf","text":"Report","size":"1.71 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR 75-434"},{"id":146621,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0434/coverthb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"Everglades","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.1834716796875,\n 25.11544539706194\n ],\n [\n -80.584716796875,\n 25.11544539706194\n ],\n [\n -80.584716796875,\n 25.928407032694118\n ],\n [\n -81.1834716796875,\n 25.928407032694118\n ],\n [\n -81.1834716796875,\n 25.11544539706194\n ]\n ]\n ]\n }\n }\n ]\n}","contact":"Caribbean-Florida Water Science Center
U.S. Geological Survey
3321 College Avenue
Davie, FL 33314
Water from California streams has been analyzed for concentrations of selected chemical constituents since the early 1950's. This summary includes about 1,200 water years of data from 88 sampling sites on 66 streams.
Results of this summary show that about 80 percent of the sites had a mean dissolved-solids concentration of 400 milligrams per litre or less. All the sites that had mean concentrations ranging from 601 to 800 milligrams per litre were in either the South Coastal or Central Coastal subregions.
Results of regression analysis between specific conductance and calcium, magnesium, sodium, bicarbonate, dissolved solids, and hardness usually indicated a high percentage of explained variance. Other constituents, such as potassium, sulfate, chloride, and particularly nitrate, were not as frequently highly associated with specific conductance.
At sites where the water discharge was highly regulated, the variation in specific conductance that was explained as a function of discharge ranged from 0 to more than 90 percent. Whereas at the unregulated sites, the explained variance ranged from 50 to more than 90 percent.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58c12664e4b014cc3a3d3541","contributors":{"authors":[{"text":"Irwin, George A.","contributorId":35363,"corporation":false,"usgs":true,"family":"Irwin","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":681204,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lemons, Michael","contributorId":24390,"corporation":false,"usgs":true,"family":"Lemons","given":"Michael","email":"","affiliations":[],"preferred":false,"id":681205,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70184367,"text":"70184367 - 1975 - Descriptions and chemical analyses for selected wells in the Tehama-Colusa Canal Service Area, Sacramento Valley, California","interactions":[],"lastModifiedDate":"2017-03-09T13:46:41","indexId":"70184367","displayToPublicDate":"1999-12-26T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Descriptions and chemical analyses for selected wells in the Tehama-Colusa Canal Service Area, Sacramento Valley, California","docAbstract":"The Tehama-Colusa Canal Service Area is in the northwestern part of the Sacramento Valley, in parts of Yolo, Colusa, Glenn, and Tehama Counties. The area includes 450 square miles (1,160 square kilometres). The boundaries are: West, the eastern slopes of the Coast Ranges; north, Elder Creek; northeast, the Sacramento River and the Glenn-Colusa Canal; east and southeast, the Colusa Basin Drainage Canal; and south, Oat Creek.
Between April and July 1974, 393 wells were selectively canvassed and between August and October 1974, water samples were collected for chemical analysis from 222 wells of the 393 wells canvassed. Field determinations of alkalinity, conductance, pH, and temperature were made on the site at the time of sampling. The samples were then field prepared for shipment and analysis for individual constituents at the Geological Survey Central Laboratory, Salt Lake City, Utah. Descriptive data for water wells are listed in table 1, chemical data in tables 2 and 3, and the location of these wells is shown on maps 1-28.
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