{"pageNumber":"2333","pageRowStart":"58300","pageSize":"25","recordCount":68857,"records":[{"id":26349,"text":"wri7669 - 1976 - Availability and chemical characteristics of ground water in central La Plata County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri7669","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-69","title":"Availability and chemical characteristics of ground water in central La Plata County, Colorado","docAbstract":"The central part of La Plata County, Colo., has undergone rapid population growth in recent years. This growth has resulted in an increased demand for information for additional domestic, industrial, and municipal water supplies. A knowledge of the occurrence of ground water will permit a more efficient allocation of the resource. Aquifers in central La Plata County include: alluvium, Animas Formation of Quaternary and Tertiary age, Fruitland Formation, Pictured Cliffs Sandstone, three formations of the Mesa Verde Group, the Mancos Shale, Dakota Sandstone, Morrison Formation of Cretaceous and Jurassic age, and undifferentiated formations. Well yields generally are low, usually less than 25 gallons per minute. However, higher yields, 25 to 50 gallons per minute may be found locally in aquifers in the alluvium and the Animas Formation. The quality of water from the aquifers is dependent on rock type. Most of the water is a calcium bicarbonate type. However, aquifers that are predominantly fine-grained or contain interbeds of shale may contain sodium bicarbonate type water. The dissolution of minerals in the coal beds, which are present in the Mesa Verde Group and the Dakota Sandstone, can contribute high concentrations of iron, sulfate, and chloride to ground water. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri7669","usgsCitation":"Brogden, R., and Giles, T., 1976, Availability and chemical characteristics of ground water in central La Plata County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 76-69, 2 maps (1 col.) ;on sheet 82 x 95 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/wri7669.","productDescription":"2 maps (1 col.) ;on sheet 82 x 95 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":158459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":55145,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0069/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f34","contributors":{"authors":[{"text":"Brogden, R. E.","contributorId":43356,"corporation":false,"usgs":true,"family":"Brogden","given":"R. E.","affiliations":[],"preferred":false,"id":196228,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Giles, T.F.","contributorId":83096,"corporation":false,"usgs":true,"family":"Giles","given":"T.F.","email":"","affiliations":[],"preferred":false,"id":196229,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43568,"text":"ofr76114 - 1976 - Land use and land cover and associated maps for Santa Ana, Calif.","interactions":[],"lastModifiedDate":"2012-02-02T00:11:03","indexId":"ofr76114","displayToPublicDate":"1994-01-01T00:00:00","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":"76-114","title":"Land use and land cover and associated maps for Santa Ana, Calif.","language":"ENGLISH","doi":"10.3133/ofr76114","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Santa Ana, Calif.: U.S. Geological Survey Open-File Report 76-114, 5 maps., https://doi.org/10.3133/ofr76114.","productDescription":"5 maps.","costCenters":[],"links":[{"id":167848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af392","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":531243,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43571,"text":"ofr76112 - 1976 - Land use and land cover and associated maps for Scott City, Kans.","interactions":[],"lastModifiedDate":"2012-02-02T00:11:04","indexId":"ofr76112","displayToPublicDate":"1994-01-01T00:00:00","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":"76-112","title":"Land use and land cover and associated maps for Scott City, Kans.","language":"ENGLISH","doi":"10.3133/ofr76112","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Scott City, Kans.: U.S. Geological Survey Open-File Report 76-112, 5 maps., https://doi.org/10.3133/ofr76112.","productDescription":"5 maps.","costCenters":[],"links":[{"id":168460,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af5b0","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":531246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13692,"text":"ofr76353 - 1976 - Effect of deicing chemicals on the hydrologic environment in Massachusetts; evaluation of surface-water data collection","interactions":[],"lastModifiedDate":"2012-02-02T00:06:55","indexId":"ofr76353","displayToPublicDate":"1994-01-01T00:00:00","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":"76-353","title":"Effect of deicing chemicals on the hydrologic environment in Massachusetts; evaluation of surface-water data collection","language":"ENGLISH","publisher":"The Division,","doi":"10.3133/ofr76353","usgsCitation":"Frost, L., 1976, Effect of deicing chemicals on the hydrologic environment in Massachusetts; evaluation of surface-water data collection: U.S. Geological Survey Open-File Report 76-353, 34 leaves ;28 cm., https://doi.org/10.3133/ofr76353.","productDescription":"34 leaves ;28 cm.","costCenters":[],"links":[{"id":146625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625761","contributors":{"authors":[{"text":"Frost, L.R.","contributorId":96675,"corporation":false,"usgs":true,"family":"Frost","given":"L.R.","affiliations":[],"preferred":false,"id":168243,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26260,"text":"wri76118 - 1976 - Geohydrology of the Albin and La Grange areas, aoutheastern Wyoming","interactions":[],"lastModifiedDate":"2023-01-11T19:49:02.96036","indexId":"wri76118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-118","title":"Geohydrology of the Albin and La Grange areas, aoutheastern Wyoming","docAbstract":"<p>The Albin and La Grange areas in southeastern Wyoming are two adjoining different hydrologic areas. Since ground water is the only source of water for irrigation in the Albin area, 34 irrigation wells have been drilled since 1968 and developed in conjunction mostly with center-pivot sprinkler systems that in 1974 irrigated about 6,980 acres. Most irrigation wells are developed in channel deposits of the Ogallala Formation of late Miocene. Water levels in parts of these channel deposits have declined about 4 to 7 feet since pumping began in 1968. In the La Grange area, lands are irrigated by surface water, ground water or a combination of both. The best producing wells are those completed in both the Brule Formation of Oligocene age and the alluvium. Secondary porosity was located and elevated in the Brule using caliper logs, an Acoustic Borehole Televiewer and geophysical logs. From the spring of 1970 to the spring of 1974, hydrographs of wells in parts of the La Grange area show water-level rises of about 5 feet resulting from the net effect of surface-water recharge and groundwater pumpage. Throughout the La Grange area no significant annual water-table declines have occurred. It is unlikely that irrigation wells pumping near Horse Creek have caused significant direct streamflow depletion.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76118","usgsCitation":"Borchert, W.B., 1976, Geohydrology of the Albin and La Grange areas, aoutheastern Wyoming: U.S. Geological Survey Water-Resources Investigations Report 76-118, Report: v, 72 p.; 6 Plates: 33.00 x 27.25 inches or smaller, https://doi.org/10.3133/wri76118.","productDescription":"Report: v, 72 p.; 6 Plates: 33.00 x 27.25 inches or smaller","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":411732,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35026.htm","linkFileType":{"id":5,"text":"html"}},{"id":55066,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55065,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55062,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55061,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55067,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0118/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118958,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0118/report-thumb.jpg"},{"id":55063,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55064,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0118/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Albin and La Grande areas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -104.482,\n              41.565\n            ],\n            [\n              -104.482,\n              41.317\n            ],\n            [\n              -104.057,\n              41.317\n            ],\n            [\n              -104.057,\n              41.565\n            ],\n            [\n              -104.482,\n              41.565\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89dd","contributors":{"authors":[{"text":"Borchert, W. B.","contributorId":34965,"corporation":false,"usgs":true,"family":"Borchert","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":196076,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9872,"text":"ofr76547 - 1976 - Use of USGS earth-science products by county planning agencies in the San Francisco Bay region, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr76547","displayToPublicDate":"1994-01-01T00:00:00","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":"76-547","title":"Use of USGS earth-science products by county planning agencies in the San Francisco Bay region, California","docAbstract":"An inventory of the use of USGS products in selected planning studies, plans, ordinances, and other planning activities was made for eight counties in the San Francisco Bay region--a region of almost five million people. This inventory was designed to determine and document the use of the 87 earth-science information products prepared as a part of the San Francisco Bay Region Environment and Resources Planning Study (SFBRS). \r\n\r\nThe inventory showed that: (1) all eight counties had planning staffs who were very familiar with SFBRS products and had made frequent use of such products; (2) all eight counties had prepared planning documents which cite SFBRS products; (3) the types of planning applications most often indicated were: geologic hazards studies, seismic safety and public safety plan elements, general reference, and the preparation and review of environmental impact reports and statements; (4) over 90 percent of the 87 SFBRS products were used at least once, and nine of the products were used over 30 times each for various county planning activities; and (5) at least 85 other USGS products were also used for various county planning activities. \r\n\r\nAfter the inventory, selected county officials, employees, and consultants were interviewed and asked--among other things--to indicate any problems in the use of the SFBRS products, to suggest improvements, and to identify any needed or desired earth-science information. The responses showed that: (1) the scales commonly used for working maps were 1:62,500 or larger and for plan implementation were 1:24,000 or larger; (2) only one county had a geologist on its planning staff, although six others had the benefit of geotechnical services from private consulting firms, county engineering staffs, or the State Division of Mines and Geology; (3) seven of the eight counties expressed some problems in using the products, primarily because of their small scale or lack of detail; (4) all eight counties expected to continue to use the products and expressed a need or desire for additional earth-science, engineering, or other information; (5) all eight counties suggested specific improvements to future products, primarily larger scale or more detail and fewer technical or more interpretive products; and (6) all eight counties received educational, advisory, and review services from USGS personnel. Seventeen selected examples of the application of SFBRS products to various county planning activities are discussed and illustrated. These examples include four planning studies, seven plans, and two ordinances. From the inventory and responses to the interviews, it is concluded that the counties in the Bay region are very familiar with, have made frequent use of, and will continue to use SFBRS products for a wide range of county planning activities.\r\n\r\nSuggestions to ensure more effective use of earth-science information in the future include: (1) monitoring emerging critical issues and analyzing new state and federal laws and regulations so as to better anticipate and respond to county earth-science information needs; (2) creating a users advisory committee to help identify critical issues and user needs; (3) providing engineering interpretations and land- and water-use capability ratings to make earth-science information more readily usable; (4) giving priority to areas impacted by development so as to husband staff resources; (5) providing earth-science information at the larger scale and greater detail commonly used and needed by counties; (6) releasing earth-science information earlier and according to a formal distribution pattern; and (7) providing educational, advisory, and review services in connection with any earth-science information designed for planners and decisionmakers.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76547","usgsCitation":"Kockelman, W.J., 1976, Use of USGS earth-science products by county planning agencies in the San Francisco Bay region, California: U.S. Geological Survey Open-File Report 76-547, 186 leaves :ill., maps ;28 cm., https://doi.org/10.3133/ofr76547.","productDescription":"186 leaves :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0547/report-thumb.jpg"},{"id":37663,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0547/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699be7","contributors":{"authors":[{"text":"Kockelman, William J.","contributorId":34510,"corporation":false,"usgs":true,"family":"Kockelman","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":160436,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25921,"text":"wri7541 - 1976 - Ground water in the San Juan metropolitan area, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:31","indexId":"wri7541","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"75-41","title":"Ground water in the San Juan metropolitan area, Puerto Rico","docAbstract":"Ground water in the San Juan, Puerto Rico, area has played a declining role in water supply since the completion of the Lofza reservoir project in the early 1950's. Ground-water potential is limited because of the small size of the aquifers and susceptibility to seawater intrusion. Of the 30 million gallons per day about half is being used. Two water-bearing zones are present: an artesian aquifer, composed of the San Sebastian Formation and the lower Cibao Formation that yields an average of 244 gallons per minute to wells; and, a water-table aquifer composed of the upper Cibao Formation and the Aguada and Aymamon Limestones that yields an average of 515 gallons per minute to wells. Ground water is less mineralized inland and in the artesian aquifer. Mean concentrations of dissolved solids are 363 milligrams per liter for the artesian aquifer and 525 milligrams per liter for the water-table aquifer. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/wri7541","usgsCitation":"Anderson, H., 1976, Ground water in the San Juan metropolitan area, Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 75-41, vi, 34 p. :ill., maps ;28 cm. [PGS: 107 p.], https://doi.org/10.3133/wri7541.","productDescription":"vi, 34 p. :ill., maps ;28 cm. [PGS: 107 p.]","costCenters":[],"links":[{"id":121917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0041/report-thumb.jpg"},{"id":54679,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0041/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d8c8","contributors":{"authors":[{"text":"Anderson, H. R.","contributorId":67487,"corporation":false,"usgs":true,"family":"Anderson","given":"H. R.","affiliations":[],"preferred":false,"id":195484,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9059,"text":"ofr76869 - 1976 - Preliminary report on 1975 drilling of lignite in western North Dakota: Adams, Bowman, Dunn, Hettinger, McLean, Mercer, Oliver, Slope, and William counties","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr76869","displayToPublicDate":"1994-01-01T00:00:00","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":"76-869","title":"Preliminary report on 1975 drilling of lignite in western North Dakota: Adams, Bowman, Dunn, Hettinger, McLean, Mercer, Oliver, Slope, and William counties","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76869","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Preliminary report on 1975 drilling of lignite in western North Dakota: Adams, Bowman, Dunn, Hettinger, McLean, Mercer, Oliver, Slope, and William counties: U.S. Geological Survey Open-File Report 76-869, i, 144 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr76869.","productDescription":"i, 144 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141858,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cbc0","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":528892,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26922,"text":"wri7636 - 1976 - Sources of arsenic in streams tributary to Lake Crowley, California","interactions":[],"lastModifiedDate":"2018-11-15T11:57:48","indexId":"wri7636","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-36","title":"Sources of arsenic in streams tributary to Lake Crowley, California","docAbstract":"<p>Lake Crowley is the largest single source of water for the city of Los Angeles. More than 50 percent of the water entering the Los Angeles-Owens River aqueduct flows through Lake Crowley. Arsenic enters Lake Crowley primarily from hot springs in Long Valley.</p><p>Sixty percent of the arsenic discharged to Lake Crowley is from hot springs in Hot Creek Gorge. The hot-spring water containing about 1,000 micrograms per litre of arsenic blends with the water flowing in the creek and is usually diluted to a concentration of about 200 micrograms per litre; additional dilution occurs downstream.</p><p>About 75 percent of the arsenic in Hot Creek is discharged from only two springs. The remaining sources of arsenic in the gorge are poorly defined seepage and flow from numerous small springs.</p><p>Other sources of arsenic in Long Valley are from either high volume and low-arsenic concentration springs, such as the springs at Hot Creek Fish Hatchery, or high-concentration and low-volume springs, such as those found in the vicinity of the Alkali lakes. These other sources individually are small in comparison with the source in Hot Creek Gorge. It seems unlikely that arsenic from these sources could cause the arsenic concentration in Lake Crowley to exceed the Environmental&nbsp;Protection Agency's recommended criterion (limit) for a public water supply.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7636","usgsCitation":"Eccles, L.A., 1976, Sources of arsenic in streams tributary to Lake Crowley, California: U.S. Geological Survey Water-Resources Investigations Report 76-36, iv, 39 p., https://doi.org/10.3133/wri7636.","productDescription":"iv, 39 p.","costCenters":[],"links":[{"id":359455,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0036/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Lake Crowley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.13848876953125,\n              37.55328764595765\n            ],\n            [\n              -118.67431640625,\n              37.55328764595765\n            ],\n            [\n              -118.67431640625,\n              37.87160128507345\n            ],\n            [\n              -119.13848876953125,\n              37.87160128507345\n            ],\n            [\n              -119.13848876953125,\n              37.55328764595765\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e76b8","contributors":{"authors":[{"text":"Eccles, Lawrence A.","contributorId":90274,"corporation":false,"usgs":true,"family":"Eccles","given":"Lawrence","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":197250,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26963,"text":"wri7538 - 1976 - Hydrologic characteristics of lagoons at San Juan, Puerto Rico, during a January 1974 tidal cycle","interactions":[],"lastModifiedDate":"2012-02-02T00:08:23","indexId":"wri7538","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"75-38","title":"Hydrologic characteristics of lagoons at San Juan, Puerto Rico, during a January 1974 tidal cycle","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri7538","usgsCitation":"Ellis, S.R., and Gómez-Gómez, F., 1976, Hydrologic characteristics of lagoons at San Juan, Puerto Rico, during a January 1974 tidal cycle: U.S. Geological Survey Water-Resources Investigations Report 75-38, v, 45 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri7538.","productDescription":"v, 45 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118994,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0038/report-thumb.jpg"},{"id":55849,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0038/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db61164d","contributors":{"authors":[{"text":"Ellis, Sherman R.","contributorId":41010,"corporation":false,"usgs":true,"family":"Ellis","given":"Sherman","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":197325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gómez-Gómez, Fernando","contributorId":31366,"corporation":false,"usgs":true,"family":"Gómez-Gómez","given":"Fernando","affiliations":[],"preferred":false,"id":197324,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37138,"text":"rr79 - 1976 - Changes in the fish population of Lewis and Clark Lake, 1956-74, and their relation to water management and the environment","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"rr79","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":74,"text":"Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"79","title":"Changes in the fish population of Lewis and Clark Lake, 1956-74, and their relation to water management and the environment","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Walburg, C.H., 1976, Changes in the fish population of Lewis and Clark Lake, 1956-74, and their relation to water management and the environment: Research Report 79, iv, 34 p. : ill. ; 26 cm.","productDescription":"iv, 34 p. : ill. ; 26 cm.","costCenters":[],"links":[{"id":164623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e69fa","contributors":{"authors":[{"text":"Walburg, Charles H.","contributorId":30268,"corporation":false,"usgs":true,"family":"Walburg","given":"Charles","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":217547,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27009,"text":"wri76102 - 1976 - Estimating runoff volumes and flood hydrographs in the Colorado River Basin, southern Utah","interactions":[],"lastModifiedDate":"2018-03-30T16:00:30","indexId":"wri76102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-102","title":"Estimating runoff volumes and flood hydrographs in the Colorado River Basin, southern Utah","docAbstract":"<p>Hydrographs of 364 floods from 18 continuous-record gaging sites in the Colorado River basin in southern Utah were used to define a single relation of flood volume to peak discharge; the standard error of estimate of that relation . is 82 percent. Using the same data, a mean dimensionless hydrograph was pre-pared. Synthetic hydrographs may be derived for basins of 5 to 300 square miles (13 to 780 square kilometers) and flood peaks of 1 to 7,000 cubic feet per second<br>(0.03 to 200 cubic meters per second) using that mean dimensionless hydrograph. Design flood peaks may be estimated from other reports. A method is presented to estimate the reduction in culvert or bridge size resulting from use of storage above the structure. Reduction of structure capacity of 25 percent may be achieved by storing 4 percent of the total flood volume.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri76102","usgsCitation":"Eychaner, J.H., 1976, Estimating runoff volumes and flood hydrographs in the Colorado River Basin, southern Utah: U.S. Geological Survey Water-Resources Investigations Report 76-102, iv, 18 p., https://doi.org/10.3133/wri76102.","productDescription":"iv, 18 p.","numberOfPages":"27","costCenters":[],"links":[{"id":158741,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Colorado River Basin","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              -109,\n              37\n            ],\n            [\n              -109,\n              39.5\n            ],\n            [\n              -114,\n              39.5\n            ],\n            [\n              -114,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f86d","contributors":{"authors":[{"text":"Eychaner, James H.","contributorId":102050,"corporation":false,"usgs":true,"family":"Eychaner","given":"James","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":197402,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27023,"text":"wri7676 - 1976 - Geology and ground-water resources of Camden County, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:36","indexId":"wri7676","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-76","title":"Geology and ground-water resources of Camden County, New Jersey","docAbstract":"The major fresh water aquifers in Camden County, N. J., are in the unconsolidated sediments of Cretaceous and Tertiary age. The major aquifers are the sand and gravel units in the Potomac Group and the Raritan and Magothy Formations, the Cohansey Sand, the Wenonah Formation-Mount Laurel Sand, and the Englishtown Formation. The average ground-water use for Camden County was 68 million gallons per day for 1966. All of the major artesian aquifers have had potentiometric head declines due to ground-water withdrawals. The largest water-level decline occurred in the aquifer system in the Potomac Group and the Raritan and Magothy Formations. At Haddon Heights the potentiometric head declined over 110 feet from 1900 to 1968. In the aquifer in the Wenonah Formation-Mount Laurel Sand the potentiometric head declined 43 feet in about 60 years. The quality of ground water is generally good. In the southeastern portion of the county chloride concentrations in excess of 250 mg/liter occur in the Potomac-Raritan-Magothy aquifer system. The high chloride water has remained in the aquifer system from the time of deposition or has re-entered the system from the ocean after the changes in sea level. The greatest potential of future ground-water development is from the Cohansey Sand which is under water table conditions. It also may have the greatest possibility of local ground-water contamination. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri7676","usgsCitation":"Farlekas, G., Nemickas, B., and Gill, H., 1976, Geology and ground-water resources of Camden County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 76-76, xvii, 146 p. :ill., maps (some fold. in pocket) ;27 cm. --, https://doi.org/10.3133/wri7676.","productDescription":"xvii, 146 p. :ill., maps (some fold. in pocket) ;27 cm. --","costCenters":[],"links":[{"id":158562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60fc51","contributors":{"authors":[{"text":"Farlekas, G.M.","contributorId":67129,"corporation":false,"usgs":true,"family":"Farlekas","given":"G.M.","affiliations":[],"preferred":false,"id":197425,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nemickas, Bronius","contributorId":105733,"corporation":false,"usgs":true,"family":"Nemickas","given":"Bronius","email":"","affiliations":[],"preferred":false,"id":197426,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gill, H.E.","contributorId":24330,"corporation":false,"usgs":true,"family":"Gill","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":197424,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27040,"text":"wri7671 - 1976 - Mathematical model of the West Bolsa Ground-water Basin, San Benito County, California","interactions":[],"lastModifiedDate":"2019-07-17T13:51:27","indexId":"wri7671","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-71","title":"Mathematical model of the West Bolsa Ground-water Basin, San Benito County, California","docAbstract":"Simulation of the West Bolsa ground-water basin hydrology in California had provided values of basin recharge and discharge and nodally distributed values of transmissivity and storage coefficient. Average net recharge from April 1945 to March 1969 was 6.2 cubic feet per second and occurred as subsurace recharge and infiltration of rain and minor streamflow. Discharge from the basin during the same period was 8.1 cubic feet per second and occurred as pumping and leakage from confined parts of the basin. Values of transmissivity used in the model generally range from 3,300 to 20,000 feet squared per day. Values of storage coefficient used in the model range from 0.0005 to 0.10. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7671","usgsCitation":"Faye, R.E., 1976, Mathematical model of the West Bolsa Ground-water Basin, San Benito County, California: U.S. Geological Survey Water-Resources Investigations Report 76-71, v, 54 p. , https://doi.org/10.3133/wri7671.","productDescription":"v, 54 p. 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,{"id":27309,"text":"wri7612 - 1976 - Results of infiltration tests near Scott City, western Kansas","interactions":[],"lastModifiedDate":"2018-11-15T11:55:18","indexId":"wri7612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-12","title":"Results of infiltration tests near Scott City, western Kansas","docAbstract":"<p>Several types of ring infiltrometers were used to determine infiltration rates in loessial soil near Scott City, Kansas. Test results were evaluated for consistency, and were compared with infiltration rates in the underlying loess and with hydraulic conductivities in the unsaturated zone.</p><p>Average daily infiltration rates in the Richfield soil ranged from 3 to 5 feet or 0.9 to 1.5 m (metres) after 16 days using 22-inch or 560mm (millimetre) ring infiltrometers; 2.3 feet (0.7 m) after 68 days using a 10-inch (250-mm) ring infiltrometer; and from 1.3 to 2.2 feet (0.4 to 0.7 m) after 38 days using double-ring infiltrometers. By comparison, the average daily infiltration rate in the underlying Peoria Loess using a 10-inch (250-mm) ring infiltrometer was about 13 feet (4.0 m) after 7 days.</p><p>Tests using the double-ring infiltrometer, a paraffin seal in the 22-inch (560-mm) infiltrometer, and the measurement of flow through concentric areas of the soil core indicated that leakage of water between the infiltrometer wall and the soil was not significant. Lateral movement of the wetting front extended radially 4.7 feet (1.4 m) from the infiltrometer wall.</p><p>Laboratory tests of a soil core indicated that the lowest hydraulic conductivity was in the depth interval from 3.9 to 8.6 inches (99 to 218 mm). Soil in this interval, which coincides with the depth of cultivation, evidently limits the rate of infiltration.</p><p>Air-permeability tests in the unsaturated deposits gave a hydraulic conductivity of 0.2 foot per day (0.1 m/day) for the depth interval from 57 to 75 feet (17.0 to 23.0 m) as compared to a hydraulic conductivity of 1.9 feet per day (0.6 m/day) for the depth interval from 0 to 5 feet (0 to 1.5 m). A perched water table probably would occur above this interval during prolonged infiltration.</p><p>Infiltration rates determined from the different types of ring infiltrometers were not consistent, but the tests showed that substantial quantities of water could infiltrate the Richfield soil.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7612","usgsCitation":"Gillespie, J.B., and Hargadine, G., 1976, Results of infiltration tests near Scott City, western Kansas: U.S. Geological Survey Water-Resources Investigations Report 76-12, iv, 29 p., https://doi.org/10.3133/wri7612.","productDescription":"iv, 29 p.","costCenters":[],"links":[{"id":359453,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0012/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158585,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0012/report-thumb.jpg"}],"country":"United States","state":"Kansas","city":"Scott City","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -101.11953735351562,\n              38.240337375904566\n            ],\n            [\n              -100.70343017578125,\n              38.240337375904566\n            ],\n            [\n              -100.70343017578125,\n              38.65119833229951\n            ],\n            [\n              -101.11953735351562,\n              38.65119833229951\n            ],\n            [\n              -101.11953735351562,\n              38.240337375904566\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699fc8","contributors":{"authors":[{"text":"Gillespie, Joe B.","contributorId":21194,"corporation":false,"usgs":true,"family":"Gillespie","given":"Joe","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":197893,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hargadine, G.D.","contributorId":93927,"corporation":false,"usgs":true,"family":"Hargadine","given":"G.D.","email":"","affiliations":[],"preferred":false,"id":197894,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4529,"text":"cir729 - 1976 - Earthquake prediction; opportunity to avert disaster : a conference on earthquake warning and response held in San Francisco, California, on November 7, 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"cir729","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"729","title":"Earthquake prediction; opportunity to avert disaster : a conference on earthquake warning and response held in San Francisco, California, on November 7, 1975","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir729","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Earthquake prediction; opportunity to avert disaster : a conference on earthquake warning and response held in San Francisco, California, on November 7, 1975: U.S. Geological Survey Circular 729, v, 35 p. :ill. ;26 cm., https://doi.org/10.3133/cir729.","productDescription":"v, 35 p. :ill. ;26 cm.","costCenters":[],"links":[{"id":121547,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1976/0729/report-thumb.jpg"},{"id":31587,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1976/0729/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629785","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":528229,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27331,"text":"wri7677 - 1976 - Hydrologic effects of hypothetical earthquake-caused floods below Jackson Lake, northwestern Wyoming","interactions":[],"lastModifiedDate":"2019-07-17T09:41:18","indexId":"wri7677","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-77","title":"Hydrologic effects of hypothetical earthquake-caused floods below Jackson Lake, northwestern Wyoming","docAbstract":"Jackson Lake, located in Grand Teton National Park, Wyoming, is in an area of seismic instability. There is a possibility of flooding in the Snake River downstream from Jackson Lake Dam in the event of a severe earthquake. Hypothetical floods were routed 38 miles (61 kilometers) downstream from the dam for three cases: (1) Instantaneous destruction of the dam outlet structure, (2) instantaneous destruction of the entire dam, and (3) for waves overtopping the dam without failure of the dam. In each case, a full reservoir was assumed. Hydrographs for outflow from the reservoir for the two cases of dam failure were developed utilizing an accelerated discharge due to the travel of a negative wave through the reservoir, and Muskingum storage routing. For the case of waves overtopping the dam, a 10-foot (3-meter) wave was assumed to be propagated from the upstream end of the reservori. A multiple-linearization technique was used to route the flow through the reach. The model was calibrated from U.S. Geological Survey streamflow records. Most extensive flooding and largest water velocities would occur if the entire dam were destroyed; floods for the other two cases were smaller. An inundation map was prepared from channel conveyance curves and profiles of the water surface. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7677","usgsCitation":"Glass, W.R., Keefer, T., and Rankl, J., 1976, Hydrologic effects of hypothetical earthquake-caused floods below Jackson Lake, northwestern Wyoming: U.S. Geological Survey Water-Resources Investigations Report 76-77, Report: iv, 32 p.; 1 Plate: 32.04 x 49.21 inches, https://doi.org/10.3133/wri7677.","productDescription":"Report: iv, 32 p.; 1 Plate: 32.04 x 49.21 inches","costCenters":[],"links":[{"id":365652,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0077/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0077/report-thumb.jpg"},{"id":365651,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0077/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Jackson Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.77789306640625,\n              43.8008364060122\n            ],\n            [\n              -110.5389404296875,\n              43.8008364060122\n            ],\n            [\n              -110.5389404296875,\n              44.03232064275081\n            ],\n            [\n              -110.77789306640625,\n              44.03232064275081\n            ],\n            [\n              -110.77789306640625,\n              43.8008364060122\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606f9b","contributors":{"authors":[{"text":"Glass, W. R.","contributorId":97535,"corporation":false,"usgs":true,"family":"Glass","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":197929,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keefer, T.N.","contributorId":97943,"corporation":false,"usgs":true,"family":"Keefer","given":"T.N.","email":"","affiliations":[],"preferred":false,"id":197930,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rankl, J.G.","contributorId":107733,"corporation":false,"usgs":true,"family":"Rankl","given":"J.G.","affiliations":[],"preferred":false,"id":197931,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44682,"text":"wri767 - 1976 - The Sparta aquifer system in Mississippi","interactions":[],"lastModifiedDate":"2016-10-20T09:13:38","indexId":"wri767","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-7","title":"The Sparta aquifer system in Mississippi","docAbstract":"<p>A large amount of information is available on the aquifers of Mississippi. &nbsp;Reports resulting from various areal studies have described the ground-water resources of the areas concerned, but no reports dealing specifically with the entire Mississippi occurrence of individual aquifer systems have previously been prepared. &nbsp;A series of \"aquifer atlases\" was deemed the most effective way to describe the character, the potential, and the extent of development of the aquifers and thereby provide water managers with data needed for efficient utilization of available resources. &nbsp;This report on the Sparta aquifer system is the third in the series. &nbsp;Information on the aquifers was obtained in the cooperative programs of the U.S. Geological Survey with the Mississippi Board of Water Commissioners and other State and Federal agencies.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Jackson, Mississippi","doi":"10.3133/wri767","usgsCitation":"Newcome, R., 1976, The Sparta aquifer system in Mississippi: U.S. Geological Survey Water-Resources Investigations Report 76-7, 3 Plates: 41.79 x 42.02 inches or smaller, https://doi.org/10.3133/wri767.","productDescription":"3 Plates: 41.79 x 42.02 inches or 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,{"id":44562,"text":"wri7634 - 1976 - Maps showing ground-water conditions in the Ranegras plain and Butler valley areas, Yuma County, Arizona - 1975","interactions":[],"lastModifiedDate":"2019-07-16T11:56:19","indexId":"wri7634","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-34","title":"Maps showing ground-water conditions in the Ranegras plain and Butler valley areas, Yuma County, Arizona - 1975","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7634","usgsCitation":"Wilkins, D.W., and Webb, W., 1976, Maps showing ground-water conditions in the Ranegras plain and Butler valley areas, Yuma County, Arizona - 1975: U.S. Geological Survey Water-Resources Investigations Report 76-34, 3 Plates: 29.21 x 33.19 inches or smaller, https://doi.org/10.3133/wri7634.","productDescription":"3 Plates: 29.21 x 33.19 inches or smaller","costCenters":[],"links":[{"id":365600,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0034/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":134972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0034/report-thumb.jpg"},{"id":365602,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0034/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365601,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0034/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","country":"United States","state":"Arizona","county":"Yuma County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.16666666666667,33.5 ], [ -114.16666666666667,34.25 ], [ -113.41666666666667,34.25 ], [ -113.41666666666667,33.5 ], [ -114.16666666666667,33.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6059dd","contributors":{"authors":[{"text":"Wilkins, D. W.","contributorId":97471,"corporation":false,"usgs":true,"family":"Wilkins","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":229999,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Webb, W.C.","contributorId":38105,"corporation":false,"usgs":true,"family":"Webb","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":229998,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33532,"text":"b1450A - 1976 - Principles of the mineral resource classification system of the U.S. Bureau of Mines and U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:09:22","indexId":"b1450A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1450","chapter":"A","title":"Principles of the mineral resource classification system of the U.S. Bureau of Mines and U.S. Geological Survey","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1450A","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Principles of the mineral resource classification system of the U.S. Bureau of Mines and U.S. Geological Survey: U.S. Geological Survey Bulletin 1450, v, p. A1-A5, ill. ;24 cm., https://doi.org/10.3133/b1450A.","productDescription":"v, p. A1-A5, ill. ;24 cm.","costCenters":[],"links":[{"id":92307,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1450a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163028,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1450a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66705b","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":529487,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28712,"text":"wri7630 - 1976 - Occurrence of arsenic in the Dry Creek Basin, Sonoma County, California","interactions":[],"lastModifiedDate":"2018-11-02T10:23:56","indexId":"wri7630","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-30","title":"Occurrence of arsenic in the Dry Creek Basin, Sonoma County, California","docAbstract":"<p>A reconnaissance study was made of occurrence of arsenic in the Dry Creek basin in northern California where the U.S. Army Corps of Engineers proposes to construct Warm Springs Dam. The purpose of the study, made from August through November 1974, was to determine the extent of any potential arsenic problems that may affect Lake Sonoma which would form behind the dam. Samples of sediment, water, and biota were collected and analyzed for arsenic content.</p><p>Results of the study indicate that arsenic presents a potential problem only in the Little Warm Springs Creek area. Samples of the geothermal water from that area contained 140 micrograms of arsenic per litre of water--almost two and one-half times the maximum allowable concentration for drinking water. However, the contribution of arsenic to the proposed lake would be minimal because discharge of the geothermal water in the area is estimated to be only about 0.01 cubic foot per second (0.0003 cubic metre per second).</p><p>Analyses of limited numbers of biota samples indicated that there is no biomagnification of arsenic through the food chain. Concentrations of arsenic in fish and benthic invertebrates collected from water containing high levels of arsenic were similar to concentrations in samples collected from water with low arsenic content. Concentrations of arsenic on sediment were low throughout the project area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7630","usgsCitation":"Middelburg, R.F., 1976, Occurrence of arsenic in the Dry Creek Basin, Sonoma County, California: U.S. Geological Survey Water-Resources Investigations Report 76-30, iv, 17 p., https://doi.org/10.3133/wri7630.","productDescription":"iv, 17 p.","costCenters":[],"links":[{"id":359107,"rank":2,"type":{"id":11,"text":"Document"},"url":" https://pubs.usgs.gov/wri/1976/0030/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0030/report-thumb.jpg"}],"country":"United States","state":"California","county":"Sonoma County","otherGeospatial":"Dry Creek Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -123.3333,\n              38.59540719940386\n            ],\n            [\n              -122.75,\n              38.59540719940386\n            ],\n            [\n              -122.75,\n              38.94285503599089\n            ],\n            [\n              -123.3333,\n              38.94285503599089\n            ],\n            [\n              -123.3333,\n              38.59540719940386\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af6e4b07f02db69299b","contributors":{"authors":[{"text":"Middelburg, Robert F.","contributorId":35360,"corporation":false,"usgs":true,"family":"Middelburg","given":"Robert","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":200272,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7786,"text":"ofr76598 - 1976 - Ground-water levels in Wyoming, 1975","interactions":[],"lastModifiedDate":"2017-01-09T10:20:12","indexId":"ofr76598","displayToPublicDate":"1994-01-01T00:00:00","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":"76-598","title":"Ground-water levels in Wyoming, 1975","docAbstract":"<p>Ground-water levels are measured periodically in a network of about 260 observation wells in Wyoming to record changes in ground-water storage. The areas of water-level observation are mostly where ground water is used in large quantities for irrigation or municipal purposes. This report contains maps showing location of observation wells and water-level changes from 1975 to 1976. Well history, highest and lowest water levels , and hydrographs for most wells also are included in this report.</p><p>The program of ground-water observation is conducted by the U.S. Geological Survey in cooperation with the Wyoming State Engineer and the city of Cheyenne.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Cheyenne, WY","doi":"10.3133/ofr76598","collaboration":"Prepared in cooperation with the Wyoming State Engineer and the City of Cheyenne","usgsCitation":"Ballance, W.C., and Freudenthal, P.B., 1976, Ground-water levels in Wyoming, 1975: U.S. Geological Survey Open-File Report 76-598, v, 170 p., https://doi.org/10.3133/ofr76598.","productDescription":"v, 170 p.","numberOfPages":"174","costCenters":[],"links":[{"id":35273,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0598/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0598/report-thumb.jpg"}],"country":"United States","state":"Wyoming","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675ea","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":156597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Freudenthal, Pamela B.","contributorId":60641,"corporation":false,"usgs":true,"family":"Freudenthal","given":"Pamela","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":156596,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56327,"text":"wdrAL751 - 1976 - Water resources data for Alabama, water year 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:12:21","indexId":"wdrAL751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"AL-75-1","title":"Water resources data for Alabama, water year 1975","language":"ENGLISH","doi":"10.3133/wdrAL751","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for Alabama, water year 1975: U.S. Geological Survey Water Data Report AL-75-1, 391 p., https://doi.org/10.3133/wdrAL751.","productDescription":"391 p.","costCenters":[],"links":[{"id":184837,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7876","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":532510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55408,"text":"wdrLA761 - 1976 - Water resources data for Louisiana, water year 1976, volume 1. Central and northern Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:12:08","indexId":"wdrLA761","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","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":"LA-76-1","title":"Water resources data for Louisiana, water year 1976, volume 1. Central and northern Louisiana","language":"ENGLISH","doi":"10.3133/wdrLA761","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for Louisiana, water year 1976, volume 1. Central and northern Louisiana: U.S. Geological Survey Water Data Report LA-76-1, 463 p., https://doi.org/10.3133/wdrLA761.","productDescription":"463 p.","costCenters":[],"links":[{"id":180695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fbe4b07f02db5f4730","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":532338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17552,"text":"ofr76450 - 1976 - Preliminary report of coal drill-hole data and chemical analyses of coal beds in Campbell, Converse, and Sheridan Counties, Wyoming; and Big Horn, Richland, and Dawson Counties, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:07:12","indexId":"ofr76450","displayToPublicDate":"1994-01-01T00:00:00","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":"76-450","title":"Preliminary report of coal drill-hole data and chemical analyses of coal beds in Campbell, Converse, and Sheridan Counties, Wyoming; and Big Horn, Richland, and Dawson Counties, Montana","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76450","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Preliminary report of coal drill-hole data and chemical analyses of coal beds in Campbell, Converse, and Sheridan Counties, Wyoming; and Big Horn, Richland, and Dawson Counties, Montana: U.S. Geological Survey Open-File Report 76-450, 382 p. :ill. ;35 cm., https://doi.org/10.3133/ofr76450.","productDescription":"382 p. :ill. ;35 cm.","costCenters":[],"links":[{"id":149627,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0450/report-thumb.jpg"},{"id":46761,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0450/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a16d","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":529024,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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