{"pageNumber":"2288","pageRowStart":"57175","pageSize":"25","recordCount":68867,"records":[{"id":29739,"text":"wri7874 - 1978 - Preliminary evaluation of the water-supply potential of the spring-river system in the Weeki Wachee area and the Lower Withlacoochee River, west-central Florida","interactions":[],"lastModifiedDate":"2013-08-12T12:16:09","indexId":"wri7874","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-74","title":"Preliminary evaluation of the water-supply potential of the spring-river system in the Weeki Wachee area and the Lower Withlacoochee River, west-central Florida","docAbstract":"Coastal springs and seeps, including Rainbow Springs, a tributary of Withlacoochee River, discharge as much as a billion gallons of water per day to low-lying coastal swamps and estuarine marshes along the Guld Coast of Citrus and Hernando Counties, Florida. Although Weeki Wachee Spring has long been regarded as an obvious source of freshwater supply, long-term diversion of large volumes of water from Weeki Wachee River will cause encroachment of brackish water throughout the residential canals in the lower reach of the river to about 4.4 miles below Weeki Wachee Spring. Weeki Wachee Spring is analogous to a flowering well tapping an artesian aquifer. Flow characteristics of Withlacoochee River and Rainbow Springs indicate that about 600 cubic feet per second is available on a perennial basis, disregarding the downstream requirements for control of saltwater encroachment. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri7874","usgsCitation":"Sinclair, W.C., 1978, Preliminary evaluation of the water-supply potential of the spring-river system in the Weeki Wachee area and the Lower Withlacoochee River, west-central Florida: U.S. Geological Survey Water-Resources Investigations Report 78-74, iv, 40 p. :ill., maps ;26 cm., https://doi.org/10.3133/wri7874.","productDescription":"iv, 40 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":160458,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0074/report-thumb.jpg"},{"id":276466,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0074/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c37f","contributors":{"authors":[{"text":"Sinclair, William C.","contributorId":14798,"corporation":false,"usgs":true,"family":"Sinclair","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":202039,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29175,"text":"wri797 - 1978 - A preliminary appraisal of the impact of agriculture on ground-water availability in southwest Georgia","interactions":[],"lastModifiedDate":"2023-02-17T21:12:44.134681","indexId":"wri797","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"79-7","title":"A preliminary appraisal of the impact of agriculture on ground-water availability in southwest Georgia","docAbstract":"<p>Irrigated acreage in the study area in southwest Georgia increased from 130,000 acres in 1976 to 261,000 in 1977. Acreage irrigated entirely by ground water increased 85 percent for the same period. The largest quantity of ground water used for irrigation was in the Dougherty Plain district, where 92 percent of supplemental irrigation water comes from wells. In the Tifton Upland district, ground water is the source for only 16 percent of the irrigation water used. The major ground-water reservoir supplying the irrigation water is the principal artesian aquifer.</p><p>The Dougherty Plain, because of the gently rolling land surface and large fields, is suitable for the use of large self-propelled center-pivot irrigation systems requiring 1,200 to 1,500 gallons per minute. The installed pump capacity of the irrigation systems in the Dougherty Plain using ground water was 1.8 billion gallons per day in 1977. The total amount of water pumped for irrigation in the Dougherty Plain in 1977 was more than 42 billion gallons, 30 billion gallons more than in 1976. This quantity could be considerably higher in 1978 as preparations were being made to irrigate more than 214,000 acres during the 1978 growing season.</p><p>There were no concentrations of selected organic compounds or trace metals used in agricultural chemicals above the recommended limits for public consumption in water analyzed from 19 wells. However, concentrations of total nitrite plus nitrate ranged from 0.3 to 7.8 milligrams per liter in wells in the Dougherty Plain, and this could indicate that the downward percolation of water through sandy soils has carried soluble nitrate, a byproduct of fertilizer, into the ground-water reservoir.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri797","collaboration":"Prepared in cooperation with the Georgia Department of Natural Resources","usgsCitation":"Pollard, L., Grantham, R., and Blanchard, H., 1978, A preliminary appraisal of the impact of agriculture on ground-water availability in southwest Georgia: U.S. Geological Survey Water-Resources Investigations Report 79-7, Report: v, 22 p.; 4 Plates: 35.12 x 28.88 inches or smaller, https://doi.org/10.3133/wri797.","productDescription":"Report: v, 22 p.; 4 Plates: 35.12 x 28.88 inches or smaller","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":413192,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1979/0007/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413190,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1979/0007/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413191,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1979/0007/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413189,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1979/0007/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413188,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0007/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159369,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0007/report-thumb.jpg"}],"country":"United States","state":"Georgia","otherGeospatial":"Dougherty 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,{"id":29699,"text":"wri7942 - 1978 - Water-table map of Walworth County, Wisconsin","interactions":[],"lastModifiedDate":"2019-07-26T10:11:49","indexId":"wri7942","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"79-42","title":"Water-table map of Walworth County, Wisconsin","docAbstract":"<p>A map of the water table in Walworth County in southeastern Wisconsin was prepared using water levels from nearly 600 wells. The work was done as a cooperative project between the U.S. Geological Survey, the University of Wisconsin-Extension, Geological and Natural History Survey, and the Southeastern Wisconsin Regional Planning Commission. The map (scale 1:100 ,000) shows the altitude of the water table in increments of 20 feet, with supplemental 10-foot contours. The altitude ranges from less than 780 feet along parts of the eastern border of the county to more than 1,000 feet in a small area near the central part of the county. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7942","usgsCitation":"Sherrill, M.G., and Erickson, J.R., 1978, Water-table map of Walworth County, Wisconsin: U.S. Geological Survey Water-Resources Investigations Report 79-42, 1 Plate: 25.07 x 20.53 inches, https://doi.org/10.3133/wri7942.","productDescription":"1 Plate: 25.07 x 20.53 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":159506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1979/0042/report-thumb.jpg"},{"id":365974,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1979/0042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Walworth County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.5413,42.8445],[-88.3044,42.8444],[-88.3027,42.6134],[-88.3016,42.4979],[-88.4099,42.4977],[-88.5047,42.4981],[-88.6288,42.4985],[-88.6737,42.4977],[-88.7059,42.4972],[-88.7719,42.4957],[-88.7737,42.4958],[-88.774,42.5855],[-88.7744,42.6728],[-88.7753,42.7587],[-88.7757,42.8455],[-88.66,42.8453],[-88.5413,42.8445]]]},\"properties\":{\"name\":\"Walworth\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4ccd","contributors":{"authors":[{"text":"Sherrill, Marvin G.","contributorId":91469,"corporation":false,"usgs":true,"family":"Sherrill","given":"Marvin","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":201973,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Erickson, John R.","contributorId":76365,"corporation":false,"usgs":true,"family":"Erickson","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":201972,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19933,"text":"ofr78457 - 1978 - Hydrologic data for urban studies in the Austin, Texas metropolitan area, 1976","interactions":[],"lastModifiedDate":"2026-02-04T19:05:27.00182","indexId":"ofr78457","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-457","title":"Hydrologic data for urban studies in the Austin, Texas metropolitan area, 1976","docAbstract":"<p>Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. Studies are now in progress in Austin, Dallas and Dallas County, Fort Worth, Houston, and San Antonio.</p><p>The Geological Survey, in cooperation with the Texas Department of Water Resources, began hydrologic studies in the Austin urban area in 1954. In cooperation with the city of Austin, the program was expanded in 1975 to include additional streamflow and rainfall gaging stations, and the collection of water-quality data. The objectives of the Austin urban hydrology study are as follows:1. To determine, on the basis of historical data and hydrologic analyses, the magnitude and frequency of flood peaks and flood volume.; 2. To determine the effect of urban development on flood peaks and volume.; 3. To ascertain the variation in water quality for different seasons from selected basins of varying urban development.</p><p>This report presents the basic hydrologic data collected in the Austin urban area for the 1976 water year (Oct. 1, 1976 to Sept. 30, 1976). To facilitate the pubication and distribution of this report at the earliest feasible time, certain material has been included that does not conform to the formal publication standards of the U.S. Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78457","collaboration":"Prepared in cooperation with the City of Austin and the Texas Department of Water Resources","usgsCitation":"Maderak, M.L., Gordon, J., and Mitchell, R., 1978, Hydrologic data for urban studies in the Austin, Texas metropolitan area, 1976: U.S. Geological Survey Open-File Report 78-457, 263 p., https://doi.org/10.3133/ofr78457.","productDescription":"263 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":153349,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0457/report-thumb.jpg"},{"id":499541,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0457/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"Austin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db683257","contributors":{"authors":[{"text":"Maderak, Marion L.","contributorId":103248,"corporation":false,"usgs":true,"family":"Maderak","given":"Marion","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":181760,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gordon, J.D.","contributorId":26684,"corporation":false,"usgs":true,"family":"Gordon","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":181758,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mitchell, R.N.","contributorId":94301,"corporation":false,"usgs":true,"family":"Mitchell","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":181759,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40764,"text":"ofr78887 - 1978 - Degraded ground water in Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:10:54","indexId":"ofr78887","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-887","title":"Degraded ground water in Connecticut","language":"ENGLISH","doi":"10.3133/ofr78887","usgsCitation":"Rolston, J.L., Grossman, I., Handman, E., and Potterton, R., 1978, Degraded ground water in Connecticut: U.S. Geological Survey Open-File Report 78-887, 1 map., https://doi.org/10.3133/ofr78887.","productDescription":"1 map.","costCenters":[],"links":[{"id":170917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db672373","contributors":{"authors":[{"text":"Rolston, James L.","contributorId":102549,"corporation":false,"usgs":true,"family":"Rolston","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":223910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grossman, I.G.","contributorId":52574,"corporation":false,"usgs":true,"family":"Grossman","given":"I.G.","email":"","affiliations":[],"preferred":false,"id":223907,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Handman, E. H.","contributorId":63407,"corporation":false,"usgs":true,"family":"Handman","given":"E.","middleInitial":"H.","affiliations":[],"preferred":false,"id":223908,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Potterton, R.S. Jr.","contributorId":94370,"corporation":false,"usgs":true,"family":"Potterton","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":223909,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":60739,"text":"mf981C - 1978 - Surface water quality and built-up areas in Connecticut","interactions":[],"lastModifiedDate":"2025-03-21T15:38:26.640951","indexId":"mf981C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"981","chapter":"C","title":"Surface water quality and built-up areas in Connecticut","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf981C","usgsCitation":"Rolston, J., Banach, F., and Handman, E., 1978, Surface water quality and built-up areas in Connecticut: U.S. Geological Survey Miscellaneous Field Studies Map 981, 1 Plate: 58.89 x 43.97 inches, https://doi.org/10.3133/mf981C.","productDescription":"1 Plate: 58.89 x 43.97 inches","costCenters":[],"links":[{"id":182851,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0981-C/report-thumb.jpg"},{"id":483639,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0981-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"125000","country":"United States","state":"Connecticut","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.75,41 ], [ -73.75,42.05 ], [ -71.75,42.05 ], [ -71.75,41 ], [ -73.75,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6981f0","contributors":{"authors":[{"text":"Rolston, J.L.","contributorId":86766,"corporation":false,"usgs":true,"family":"Rolston","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":264323,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Banach, F.S.","contributorId":85659,"corporation":false,"usgs":true,"family":"Banach","given":"F.S.","email":"","affiliations":[],"preferred":false,"id":264322,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Handman, E. H.","contributorId":63407,"corporation":false,"usgs":true,"family":"Handman","given":"E.","middleInitial":"H.","affiliations":[],"preferred":false,"id":264321,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":27767,"text":"wri78104 - 1978 - Geohydrology of the northern Louisiana salt-dome basin pertinent to the storage of radioactive wastes; a progress report","interactions":[],"lastModifiedDate":"2012-02-02T00:08:26","indexId":"wri78104","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-104","title":"Geohydrology of the northern Louisiana salt-dome basin pertinent to the storage of radioactive wastes; a progress report","docAbstract":"Salt domes in northern Louisiana are being considered as possible storage sites for nuclear wastes. The domes are in an area that received regional sedimentation through early Tertiary (Eocene) time with lesser amounts of Quaternary deposits. The Cretaceous-Tertiary accumulation is a few thousand feet thick; the major sands are regional aquifers that extend far beyond the boundaries of the salt-dome basin. Because of multiple aquifers, structural deformation, and variations in the hydraulic characteristics of cap rock, the ground-water hydrology around a salt dome may be highly complex. The Sparta Sand is the most productive and heavily used regional aquifer. It is either penetrated by or overlies most of the domes. A fluid entering the Sparta flow system would move toward one of the pumping centers, all at or near municipalities that pump from the Sparta. Movement could be toward surface drainage where local geologic and hydrologic conditions permit leakage to the surface or to a surficial aquifer. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri78104","usgsCitation":"Hosman, R., 1978, Geohydrology of the northern Louisiana salt-dome basin pertinent to the storage of radioactive wastes; a progress report: U.S. Geological Survey Water-Resources Investigations Report 78-104, v, 27 p., [10] leaves of plates :ill. (some fold.), maps (some fold.) ;28 cm., https://doi.org/10.3133/wri78104.","productDescription":"v, 27 p., [10] leaves of plates :ill. (some fold.), maps (some fold.) ;28 cm.","costCenters":[],"links":[{"id":157991,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8841","contributors":{"authors":[{"text":"Hosman, R. L.","contributorId":42978,"corporation":false,"usgs":true,"family":"Hosman","given":"R.","middleInitial":"L.","affiliations":[],"preferred":false,"id":198663,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":17930,"text":"ofr78970 - 1978 - Potential potable-water supplies in Redwood National Park, California","interactions":[],"lastModifiedDate":"2026-02-04T17:03:16.690376","indexId":"ofr78970","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-970","title":"Potential potable-water supplies in Redwood National Park, California","docAbstract":"<p>An evaluation was made of the potential for potable-water supplies at 13 sites in or near Redwood National Park, Calif. The National Park Service is planning for the development of visitor facilities at these sites. At some sites, the report recommends using surface-water diversions. At other sites, locations are given for test-well drilling or springs are recommended for development. Chemical analyses of water are given for selected surface-water supplies and for some existing wells and springs. The chemical quality of the water is suitable at most of the sites, although concentrations of iron and chloride are excessively high in some areas.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78970","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Akers, J.P., 1978, Potential potable-water supplies in Redwood National Park, California: U.S. Geological Survey Open-File Report 78-970, iv, 26 p., https://doi.org/10.3133/ofr78970.","productDescription":"iv, 26 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":150083,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0970/report-thumb.jpg"},{"id":499513,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0970/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Redwood National 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,{"id":7483,"text":"ofr78578 - 1978 - Report on laboratory testing of shallow sediments, Middle Atlantic Outer Continental Shelf","interactions":[],"lastModifiedDate":"2026-02-19T18:27:58.608694","indexId":"ofr78578","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-578","title":"Report on laboratory testing of shallow sediments, Middle Atlantic Outer Continental Shelf","docAbstract":"<p>This report contains the results of geotechnical engineering testing on cores taken by the U.S. Geological Survey to evaluate the characteristics of the sea floor within the Baltimore Canyon Trough area. The coring took place in September, 1977 aboard the R/V ANNANDALE. During the cruise (AN-01-77), 20 vibracores were taken at 17 stations across the Continental Shelf off the coast of New Jersey (Figure 1). Table 1 shows the station locations, the water depths at each station, and the core lengths.&nbsp;</p><p>The objective of the study was to obtain a set of representative index properties as well as strength and compressibility data on sediments from across the shelf in the Baltimore Canyon Trough area. It was anticipated that these data, although of a reconnaissance rather than a site-specific nature, would provide a useful indication of the engineering properties of these sediments. Ultimately, these data may be used for preliminary design applications and the assessment of potential hazards. In this report, the results are presented without any interpretation. An overall evaluation of all data collected during the study, including those contained in this report, presently is underway.&nbsp;</p><p>Users of this report should be cautioned not to take these test results out of context. Two factors must be borne in mind. The first is that these tests were done on somewhat disturbed samples compared with those obtained through high-quality sampling programs onshore. Much disturbance is inevitable offshore but the significance of the disturbance on these test results has not yet been evaluated. The second factor is that these data are only part of the total set available from this project. A complete analysis of all data may lead to conclusions that are different from those based on this set of data only.</p><p>The tests reported herein were performed by Geotechnical Engineers Inc., 1017 Main Street, Winchester, Massachusetts 01890, under Contract 14-08-0001-16232 of the U.S. Geological Survey. Richard Brown and Charles Osgood performed the engineering properties tests. Sally A. Wood of the U.S. Geological Survey handled the transfer of vibracores between the U.S. Geological Survey and Geotechnical Engineers Inc. and, also, assisted in the preparation of this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78578","usgsCitation":"LaGatta, D.P., Dalenberg, K., Knebel, H., and Sangrey, D., 1978, Report on laboratory testing of shallow sediments, Middle Atlantic Outer Continental Shelf: U.S. Geological Survey Open-File Report 78-578, vi, 249 p. :ill., map ;28 cm.; (255 p. - PGS), https://doi.org/10.3133/ofr78578.","productDescription":"vi, 249 p.","costCenters":[],"links":[{"id":500216,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0578/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140438,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0578/report-thumb.jpg"}],"otherGeospatial":"Middle Atlantic Outer Continental Shelf","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a59e4b07f02db62fe36","contributors":{"authors":[{"text":"LaGatta, Daniel P.","contributorId":21158,"corporation":false,"usgs":true,"family":"LaGatta","given":"Daniel","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":155825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dalenberg, Karl","contributorId":29416,"corporation":false,"usgs":true,"family":"Dalenberg","given":"Karl","email":"","affiliations":[],"preferred":false,"id":155826,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knebel, H.J.","contributorId":79092,"corporation":false,"usgs":true,"family":"Knebel","given":"H.J.","affiliations":[],"preferred":false,"id":155828,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sangrey, D.A.","contributorId":47364,"corporation":false,"usgs":true,"family":"Sangrey","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":155827,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":20986,"text":"ofr79215 - 1978 - Flood-plain delineation for Occoquan River, Wolf Run, Sandy Run, Elk Horn Run, Giles Run, Kanes Creek, Racoon Creek, and Thompson Creek, Fairfax County, Virginia","interactions":[],"lastModifiedDate":"2026-01-08T19:16:47.89453","indexId":"ofr79215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"79-215","title":"Flood-plain delineation for Occoquan River, Wolf Run, Sandy Run, Elk Horn Run, Giles Run, Kanes Creek, Racoon Creek, and Thompson Creek, Fairfax County, Virginia","docAbstract":"<p>Water-surface profiles of the 25-year and 100-year floods and maps on which the 25-, 50-, and 100-year flood boundaries are delineated for streams in southwestern Fairfax County tributary to the Occoquan River, that part of the Occoquan River within Fairfax County and those streams on Mason Neck tributary to the Potomac River are presented in this report.</p><p>The techniques used in the computation of the flood profiles and delineation of flood boundaries are presented, and specific hydraulic problems encountered within the study area are also included.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr79215","usgsCitation":"Soule, P.L., 1978, Flood-plain delineation for Occoquan River, Wolf Run, Sandy Run, Elk Horn Run, Giles Run, Kanes Creek, Racoon Creek, and Thompson Creek, Fairfax County, Virginia: U.S. Geological Survey Open-File Report 79-215, v, 118 p., https://doi.org/10.3133/ofr79215.","productDescription":"v, 118 p.","costCenters":[],"links":[{"id":154372,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1979/0215/report-thumb.jpg"},{"id":498432,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1979/0215/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Virginia","county":"Fairfax 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,{"id":55167,"text":"wdrHI771 - 1978 - Water resources data for Hawaii and other Pacific areas, water year 1977: Volume 1. Hawaii","interactions":[],"lastModifiedDate":"2025-12-04T14:34:49.583024","indexId":"wdrHI771","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"HI-77-1","title":"Water resources data for Hawaii and other Pacific areas, water year 1977: Volume 1. Hawaii","docAbstract":"<p>Volume 1 of water resources data for the 1977 water year for Hawaii and other Pacific Areas consist of records of stage, discharge, and water quality of streams; and water levels and water quality in wells and springs. This report contains discharge records for 114 gaging stations; water quality for 10 gaging stations, 102 partial-record flow stations and 155 wells; and water levels for 25 observation wells. Also included are 108 crest-stage partial-record stations and 20 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State, Federal, and other agencies in Hawaii.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrHI771","collaboration":"Prepared in cooperation with the State of Hawaii and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Water resources data for Hawaii and other Pacific areas, water year 1977: Volume 1. Hawaii: U.S. Geological Survey Water Data Report HI-77-1, x, 348 p., https://doi.org/10.3133/wdrHI771.","productDescription":"x, 348 p.","costCenters":[],"links":[{"id":497041,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1977/hi-77-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173977,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1977/hi-77-1/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f71e2","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":532270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44539,"text":"wri7860 - 1978 - Maps showing ground-water conditions in the Willcox area, Cochise and Graham Counties, Arizona - 1975","interactions":[],"lastModifiedDate":"2026-03-27T17:19:07.758944","indexId":"wri7860","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"78-60","title":"Maps showing ground-water conditions in the Willcox area, Cochise and Graham Counties, Arizona - 1975","docAbstract":"The Willcox area includes about 1,500 square miles in southeastern Arizona. The main use of ground water is for irrigation. For 1954-75, the estimated ground-water pumpage exceeded 100,000 acre-feet per year, and for 1967-75, ground-water pumpage averaged about 300,000 acre-feet per year. Ground-water withdrawals have resulted in general water-level declines in most of the developed part of the area. Information shown on the maps includes change in water level (1963-75), irrigated area, depth to water, well depth, altitude of the water level, and distribution of dissolved solids and fluoride. Hydrographs of water levels in selected wells and a table of historical pumpage are included also. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7860","usgsCitation":"Mann, L.J., White, N.D., and Wilson, R.P., 1978, Maps showing ground-water conditions in the Willcox area, Cochise and Graham Counties, Arizona - 1975: U.S. Geological Survey Water-Resources Investigations Report 78-60, 3 maps ; 86 x 81 cm.; Scale ca. 1:130,000., https://doi.org/10.3133/wri7860.","productDescription":"3 Sheets: 34.11 x 38.77 inches or smaller","costCenters":[],"links":[{"id":501732,"rank":3,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/wri/1978/0060/sheet-2.pdf","text":"Sheet 2","linkFileType":{"id":1,"text":"pdf"}},{"id":501731,"rank":2,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/wri/1978/0060/sheet-1.pdf","text":"Sheet 1","linkFileType":{"id":1,"text":"pdf"}},{"id":501733,"rank":4,"type":{"id":26,"text":"Sheet"},"url":"https://pubs.usgs.gov/wri/1978/0060/sheet-3.pdf","text":"Sheet 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Larry J.","contributorId":48531,"corporation":false,"usgs":true,"family":"Mann","given":"Larry","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229964,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, Natalie D.","contributorId":97064,"corporation":false,"usgs":true,"family":"White","given":"Natalie","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":229965,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wilson, R. P.","contributorId":37672,"corporation":false,"usgs":true,"family":"Wilson","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":229963,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70112348,"text":"70112348 - 1978 - Hydrological applications of Landsat imagery used in the study of the 1973 Indus River flood, Pakistan","interactions":[],"lastModifiedDate":"2017-01-18T15:11:13","indexId":"70112348","displayToPublicDate":"1990-06-12T15:50:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2529,"text":"Journal of the American Water Resources Association","active":true,"publicationSubtype":{"id":10}},"title":"Hydrological applications of Landsat imagery used in the study of the 1973 Indus River flood, Pakistan","docAbstract":"<p>During August and September 1973, the Indus River Valley of Pakistan experienced one of the largest floods on record, resulting in damages to homes, businesses, public works, and crops amounting to millions of rupees. Tremendous areas of lowlands were inundated along the Indus River and major tributaries. Landsat data made it possible to easily measure the extent of flooding, totaling about 20,000 km<sup>2</sup> within an area of about 400,000 km<sup>2</sup> south from the Punjab to the Arabian Sea.</p><p>The Indus River data were used to continue experimentation in the development of rapid, accurate, and inexpensive optical techniques of flood mapping by satellite begun in 1973 for the Mississipi River floods. The research work on the Indus River not resulted in the development of more effective procedures for optical processing of flood data and synoptically depicting flooding, but also provided potentially valuable ancillary information concerning the hydrology of much of the Indus River Basin.</p>","language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","doi":"10.1111/j.1752-1688.1978.tb02165.x","usgsCitation":"Deutsch, M., and Ruggles, F., 1978, Hydrological applications of Landsat imagery used in the study of the 1973 Indus River flood, Pakistan: Journal of the American Water Resources Association, v. 14, no. 2, p. 261-274, https://doi.org/10.1111/j.1752-1688.1978.tb02165.x.","productDescription":"14 p.","startPage":"261","endPage":"274","numberOfPages":"14","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288558,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288557,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.1752-1688.1978.tb02165.x"}],"country":"Pakistan","otherGeospatial":"Indus River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 67.42,23.99 ], [ 67.42,35.54 ], [ 73.59,35.54 ], [ 73.59,23.99 ], [ 67.42,23.99 ] ] ] } } ] }","volume":"14","issue":"2","noUsgsAuthors":false,"publicationDate":"2007-06-08","publicationStatus":"PW","scienceBaseUri":"539acc03e4b0e83db6d08f63","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":494697,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ruggles, F.H. Jr.","contributorId":75822,"corporation":false,"usgs":true,"family":"Ruggles","given":"F.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":494698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70112342,"text":"70112342 - 1978 - Flood damage assessment using computer-assisted analysis of color infrared photography","interactions":[],"lastModifiedDate":"2017-01-18T15:11:58","indexId":"70112342","displayToPublicDate":"1990-06-12T15:38:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2456,"text":"Journal of Soil and Water Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Flood damage assessment using computer-assisted analysis of color infrared photography","docAbstract":"<p>Use of digitized aerial photographs for flood damage assessment in agriculture is new and largely untested. However, under flooding circumstances similar to the 1975 Red River Valley flood, computer-assisted techniques can be extremely useful, especially if detailed crop damage estimates are needed within a relatively short period of time.</p><p>Airphoto interpretation techniques, manual or computer-assisted, are not intended to replace conventional ground survey and sampling procedures. But their use should be considered a valuable addition to the tools currently available for assessing agricultural flood damage.</p>","language":"English","publisher":"Soil Conservation Society of America","publisherLocation":"Ankeny, IA","usgsCitation":"Anderson, W.H., 1978, Flood damage assessment using computer-assisted analysis of color infrared photography: Journal of Soil and Water Conservation, v. 33, no. 6, p. 283-286.","productDescription":"4 p.","startPage":"283","endPage":"286","numberOfPages":"4","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288554,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbfce4b0e83db6d08f31","contributors":{"authors":[{"text":"Anderson, William H.","contributorId":9678,"corporation":false,"usgs":true,"family":"Anderson","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":494694,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70098474,"text":"70098474 - 1978 - UTM grid declination and mil equivalents for center of quadrangle, coterminous United States","interactions":[],"lastModifiedDate":"2014-04-09T15:21:29","indexId":"70098474","displayToPublicDate":"1980-01-01T16:02:51","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"UTM grid declination and mil equivalents for center of quadrangle, coterminous United States","docAbstract":"The grid declination and mil equivalents for, the center of a quadrangle are tabulated for the four standard quadrangle map series listed above.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70098474","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, UTM grid declination and mil equivalents for center of quadrangle, coterminous United States, 49 p., https://doi.org/10.3133/70098474.","productDescription":"49 p.","numberOfPages":"55","costCenters":[{"id":587,"text":"Topographic Division","active":false,"usgs":true}],"links":[{"id":284191,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70098474.jpg"},{"id":286064,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70098474/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535595d6e4b0120853e8c2c9","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":535641,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70161980,"text":"70161980 - 1978 - Simulation model of <i>Cryptomonas ovata</i> population dynamics in southern Kootenay Lake, British Columbia","interactions":[],"lastModifiedDate":"2016-07-27T10:53:41","indexId":"70161980","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1458,"text":"Ecological Modelling","active":true,"publicationSubtype":{"id":10}},"title":"Simulation model of <i>Cryptomonas ovata</i> population dynamics in southern Kootenay Lake, British Columbia","docAbstract":"<div>A one-dimensional transient model is developed to simulate observed population dynamics of a small flagellate (<i>Cryptomonas ovata</i>) in southern Kootenay Lake, B.C., during a 1-year period (1 June 1974-31 May 1975). The model considers advective displacement of&nbsp;<i>C. ovata</i>&nbsp;as water flows from its southern entrance into the lake and moves northward toward sampling sites. Specific growth rate is computed from an experimentally determined function of mean irradiance, water temperature, and nutrient (ammonium and phosphate) concentration in the upper 10 m of the water column. Cell losses are assumed to result from zooplankton grazing and inhibition due to presence of the blue-green alga&nbsp;<i>Anabaena</i>.</div>\n<div>The model simulates well the timing and magnitude of all observed population changes and, more importantly, it gives insight into the important mechanisms which regulate population density of&nbsp;<i>C. ovata</i>&nbsp;in this natural system.</div>","language":"English","publisher":"Elsevier","doi":"10.1016/0304-3800(78)90004-2","usgsCitation":"Cloern, J.E., 1978, Simulation model of <i>Cryptomonas ovata</i> population dynamics in southern Kootenay Lake, British Columbia: Ecological Modelling, v. 4, no. 2, https://doi.org/10.1016/0304-3800(78)90004-2.","productDescription":"17 p.","endPage":"133","numberOfPages":"149","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":552,"text":"San Francisco Bay-Delta","active":false,"usgs":true},{"id":5079,"text":"Pacific Regional Director's Office","active":true,"usgs":true}],"links":[{"id":314140,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada","state":"British Columbia","otherGeospatial":"Lake Kootenay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.99066162109375,\n              49.20503726723141\n            ],\n            [\n              -116.99066162109375,\n              50.17162093714734\n            ],\n            [\n              -116.597900390625,\n              50.17162093714734\n            ],\n            [\n              -116.597900390625,\n              49.20503726723141\n            ],\n            [\n              -116.99066162109375,\n              49.20503726723141\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5694e051e4b039675d005e6a","contributors":{"authors":[{"text":"Cloern, James E. 0000-0002-5880-6862 jecloern@usgs.gov","orcid":"https://orcid.org/0000-0002-5880-6862","contributorId":1488,"corporation":false,"usgs":true,"family":"Cloern","given":"James","email":"jecloern@usgs.gov","middleInitial":"E.","affiliations":[{"id":438,"text":"National Research Program - Western Branch","active":true,"usgs":true},{"id":37277,"text":"WMA - Earth System Processes Division","active":true,"usgs":true}],"preferred":true,"id":588248,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70181772,"text":"70181772 - 1978 - Implications of water management and Lake Oahe for the spawning success of coolwater fishes","interactions":[],"lastModifiedDate":"2017-02-13T15:27:23","indexId":"70181772","displayToPublicDate":"1979-01-01T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":717,"text":"American Fisheries Society Special Publication","active":true,"publicationSubtype":{"id":10}},"title":"Implications of water management and Lake Oahe for the spawning success of coolwater fishes","docAbstract":"<p>No&nbsp;abstract available</p>","language":"English","publisher":"American Fisheries Society","usgsCitation":"Nelson, W., 1978, Implications of water management and Lake Oahe for the spawning success of coolwater fishes: American Fisheries Society Special Publication, v. 11, p. 154-158.","productDescription":"5 p. ","startPage":"154","endPage":"158","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":335283,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58a2d3c4e4b0c82512869a44","contributors":{"authors":[{"text":"Nelson, W.R.","contributorId":178924,"corporation":false,"usgs":false,"family":"Nelson","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":668456,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28720,"text":"wri7768 - 1978 - Water-resources setting, Martin County, Florida","interactions":[],"lastModifiedDate":"2022-01-04T17:28:01.388554","indexId":"wri7768","displayToPublicDate":"1978-12-31T21:30:00","publicationYear":"1978","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":"77-68","title":"Water-resources setting, Martin County, Florida","docAbstract":"This report describes some basic principles of hydrology as they apply to Martin County, Florida. The major land features are described first, then the hydrologic cycle and surface-water and ground-water resource. Specific problems associated with population growth and the county 's development, such as saltwater intrusion and water use, are cited and sections have been included to deal with these problems. The report is intended to provide a background on the water resource of Martin County to those who do not have the time nor the need to delve deeply into the county 's hydrologic conditions or its water-management problems. It is freely illustrated and uses a minimum of text to explain the illustrations. General data on the water resources of the county are given, but few specific basic data are presented. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7768","collaboration":"Prepared in cooperation with South Florida Water Management District and the Board of Commissioners, Martin County","usgsCitation":"Miller, R.A., 1978, Water-resources setting, Martin County, Florida: U.S. Geological Survey Water-Resources Investigations Report 77-68, 37 p., https://doi.org/10.3133/wri7768.","productDescription":"37 p.","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":392057,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0068/wri7768.pdf","text":"Report","size":"774 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":159415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0068/coverthb.jpg"}],"country":"United States","state":"Florida","county":"Martin County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-80.2812,27.2053],[-80.266,27.1963],[-80.2735,27.19],[-80.273,27.1877],[-80.2695,27.188],[-80.2673,27.1854],[-80.2628,27.1682],[-80.2575,27.1572],[-80.2528,27.1628],[-80.26,27.1675],[-80.2594,27.17],[-80.2569,27.1672],[-80.2533,27.1682],[-80.2596,27.1772],[-80.2595,27.1882],[-80.2619,27.1927],[-80.2569,27.2025],[-80.2172,27.2051],[-80.2092,27.1962],[-80.2097,27.1875],[-80.2041,27.1824],[-80.1967,27.1793],[-80.1933,27.1628],[-80.1977,27.1544],[-80.1944,27.1511],[-80.1953,27.1464],[-80.1928,27.1469],[-80.1942,27.1519],[-80.192,27.1626],[-80.1788,27.1609],[-80.1717,27.1547],[-80.1617,27.139],[-80.1513,27.1273],[-80.1514,27.1217],[-80.1406,27.1056],[-80.1397,27.11],[-80.1425,27.1175],[-80.1495,27.1293],[-80.1517,27.1294],[-80.1775,27.1636],[-80.1617,27.1647],[-80.1556,27.1582],[-80.1438,27.1297],[-80.1399,27.1144],[-80.1224,27.0836],[-80.1061,27.0495],[-80.095,27.0215],[-80.0879,26.9918],[-80.0807,26.9715],[-80.082,26.9708],[-80.0896,26.9871],[-80.0936,27.0064],[-80.1092,27.045],[-80.1197,27.0589],[-80.1214,27.0578],[-80.1203,27.0533],[-80.1089,27.0356],[-80.1064,27.0222],[-80.0938,27.0007],[-80.0915,26.9907],[-80.0926,26.9888],[-80.0899,26.9804],[-80.0865,26.9774],[-80.086,26.9708],[-80.1096,26.9709],[-80.1132,26.9762],[-80.1121,26.9801],[-80.1137,26.9754],[-80.1115,26.9715],[-80.1251,26.9699],[-80.1263,26.9732],[-80.1307,26.9749],[-80.1312,26.9735],[-80.1276,26.9724],[-80.1288,26.9704],[-80.1346,26.9751],[-80.1357,26.9737],[-80.1271,26.9687],[-80.1268,26.9657],[-80.1226,26.9632],[-80.121,26.9562],[-80.1228,26.9557],[-80.1255,26.9636],[-80.1349,26.9713],[-80.142,26.9711],[-80.1421,26.9564],[-80.3766,26.9588],[-80.4179,26.9574],[-80.8855,26.9586],[-80.6777,27.1212],[-80.6779,27.206],[-80.2856,27.2062],[-80.2854,27.2107],[-80.2839,27.2066],[-80.2812,27.2053]]],[[[-80.2272,27.2518],[-80.2211,27.2535],[-80.2207,27.2521],[-80.2273,27.25],[-80.2234,27.2462],[-80.2236,27.2429],[-80.2156,27.2305],[-80.213,27.2301],[-80.2097,27.2203],[-80.2,27.2041],[-80.1944,27.2064],[-80.1987,27.2014],[-80.1911,27.1896],[-80.1867,27.1883],[-80.1856,27.1787],[-80.1891,27.1737],[-80.1919,27.1744],[-80.1925,27.1814],[-80.2014,27.193],[-80.2033,27.2006],[-80.2135,27.2175],[-80.2253,27.2199],[-80.2428,27.2139],[-80.2561,27.215],[-80.2592,27.2125],[-80.2581,27.2103],[-80.2611,27.2028],[-80.2656,27.2117],[-80.278,27.2158],[-80.2809,27.2274],[-80.292,27.2364],[-80.2925,27.2402],[-80.3048,27.2433],[-80.2907,27.241],[-80.2849,27.2329],[-80.2846,27.2638],[-80.2332,27.2629],[-80.2272,27.2518]]],[[[-80.1951,27.2546],[-80.1619,27.1942],[-80.1529,27.1699],[-80.1546,27.1688],[-80.1692,27.1717],[-80.1703,27.1811],[-80.1619,27.1855],[-80.1661,27.1994],[-80.1722,27.2067],[-80.1757,27.2046],[-80.1799,27.2057],[-80.1834,27.2097],[-80.1886,27.2078],[-80.1846,27.2111],[-80.1837,27.2156],[-80.1853,27.2285],[-80.1897,27.2342],[-80.1979,27.2392],[-80.1967,27.2414],[-80.1925,27.2419],[-80.1926,27.2451],[-80.197,27.247],[-80.1999,27.2533],[-80.2031,27.2545],[-80.2097,27.2523],[-80.2113,27.2549],[-80.2105,27.263],[-80.1994,27.263],[-80.1951,27.2546]]],[[[-80.1802,27.1836],[-80.1794,27.1808],[-80.1808,27.1808],[-80.1802,27.1836]]],[[[-80.1851,27.1733],[-80.1858,27.1712],[-80.1869,27.1735],[-80.1851,27.1733]]],[[[-80.1719,27.1776],[-80.173,27.1743],[-80.1741,27.1785],[-80.1719,27.1776]]]]},\"properties\":{\"name\":\"Martin\",\"state\":\"FL\"}}]}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c7e4b07f02db5410b2","contributors":{"authors":[{"text":"Miller, R. Adam","contributorId":21540,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"Adam","affiliations":[],"preferred":false,"id":200285,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207277,"text":"70207277 - 1978 - Oxygen isotope composition of subglacially precipitated calcite: Possible paleoclimatic implications","interactions":[],"lastModifiedDate":"2019-12-16T06:44:31","indexId":"70207277","displayToPublicDate":"1978-12-31T15:28:58","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Oxygen isotope composition of subglacially precipitated calcite: Possible paleoclimatic implications","docAbstract":"<p><span>Isotopic analyses of subglacially precipitated calcite from near a modern temperate glacier show that the δ</span><sup>18</sup><span>O (=&nbsp;</span><sup>18</sup><span>O/&nbsp;</span><sup>16</sup><span>O relative to standard mean ocean water) of the calcite records the δ</span><sup>18</sup><span>O of the ice from that glacier. It may therefore be possible to determine the δ</span><sup>18</sup><span>O of Pleistocene ice sheets on the basis of isotopic analyses of calcite formed under that ancient ice. This, in turn, would allow estimation of the δ</span><sup>18</sup><span>O of Pleistocene oceans and correction of the paleotemperature scale based on foraminiferal oxygen isotopic analyses. Copyright&nbsp;</span></p>","language":"English","publisher":"Science ","doi":"10.1126/science.200.4347.1267","issn":" 00368075","usgsCitation":"Hanshaw, B., and Hallet, B., 1978, Oxygen isotope composition of subglacially precipitated calcite: Possible paleoclimatic implications: Science, v. 200, no. 4347, p. 1267-1270, https://doi.org/10.1126/science.200.4347.1267.","productDescription":"4 p. ","startPage":"1267","endPage":"1270","costCenters":[],"links":[{"id":370284,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"200","issue":"4347","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hanshaw, B.B.","contributorId":25928,"corporation":false,"usgs":true,"family":"Hanshaw","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":777523,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hallet, B.","contributorId":221246,"corporation":false,"usgs":false,"family":"Hallet","given":"B.","affiliations":[],"preferred":false,"id":777524,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70205827,"text":"70205827 - 1978 - Studies of trace metals in the waters and sediments of Badfish Creek and Lake Wingra, near Madison, Wisconsin : Technical completion report","interactions":[],"lastModifiedDate":"2019-10-07T13:05:18","indexId":"70205827","displayToPublicDate":"1978-12-31T12:57:09","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"seriesTitle":{"id":414,"text":"Technical Report","active":false,"publicationSubtype":{"id":9}},"seriesNumber":"78-07","title":"Studies of trace metals in the waters and sediments of Badfish Creek and Lake Wingra, near Madison, Wisconsin : Technical completion report","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Water Resources Center, University of Wisconsin","usgsCitation":"Delfino, J.J., Degelow, M.A., and Imbrigiotta, T., 1978, Studies of trace metals in the waters and sediments of Badfish Creek and Lake Wingra, near Madison, Wisconsin : Technical completion report: Technical Report 78-07.","costCenters":[],"links":[{"id":368055,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wisconsin","city":"Madison","otherGeospatial":"Badfish Creek, Lake Wingra","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.43600654602051,\n              43.04831801310415\n            ],\n            [\n              -89.40038681030272,\n              43.04831801310415\n            ],\n            [\n              -89.40038681030272,\n              43.06261723675984\n            ],\n            [\n              -89.43600654602051,\n              43.06261723675984\n            ],\n            [\n              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,{"id":70188833,"text":"70188833 - 1978 - A paleolimnological comparison of Burntside and Shagawa Lakes, northeastern Minnesota","interactions":[],"lastModifiedDate":"2017-06-26T10:00:51","indexId":"70188833","displayToPublicDate":"1978-12-31T00:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":5436,"text":"Ecological Research Series","active":true,"publicationSubtype":{"id":1}},"seriesNumber":"EPA-600/3-78-004 ","title":"A paleolimnological comparison of Burntside and Shagawa Lakes, northeastern Minnesota","docAbstract":"<p>The paleolimnological records of Burntside and Shagawa Lakes in northeastern Minnesota reveal that these two adjacent lakes have been limnologically distinct for many years prior to the late 19th century activities of white men that polluted Shagawa Lake. Although both lakes occur within the same vegetation type and share much of their water, the diatom stratigraphy of their bottom sediments indicates that Burntside Lake was less productive in its natural state than Shagawa Lake. The causes for this natural difference are not clearly known, but differences in relative size of drainage area and in bedrock geology may he responsible. </p><p>Intensive white settlement around Shagawa Lake beginning in 1866 supplied nutrients that increased its productivity and finally supported the massive blooms of blue-green algae that characterize culturally eutrophic lakes. Burntside Lake was spared such intensive eutrophication, but its diatom record shows that nutrients derived from shoreside recreational cabins and related construction activity are increasing the lake's productivity. </p><p>The results of this study show that paleolimnological studies may provide better comparative information for lake rehabilitation programs than do biological and chemical analyses of contemporary unpolluted water bodies. </p>","language":"English","publisher":"Environmental Protection Agency","usgsCitation":"Bradbury, J.P., and Waddington, J., 1978, A paleolimnological comparison of Burntside and Shagawa Lakes, northeastern Minnesota: Ecological Research Series EPA-600/3-78-004 , x, 51 p.","productDescription":"x, 51 p.","costCenters":[],"links":[{"id":342855,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","county":"St. Louis County","otherGeospatial":"Burntside Lake, 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,{"id":70170196,"text":"70170196 - 1978 - Status of projects in Minnesota fiscal year 1978","interactions":[],"lastModifiedDate":"2018-02-14T11:24:07","indexId":"70170196","displayToPublicDate":"1978-12-01T12:30:00","publicationYear":"1978","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Status of projects in Minnesota fiscal year 1978","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/70170196","usgsCitation":"Adolphson, D.G., and Jannis, J.A., 1978, Status of projects in Minnesota fiscal year 1978, 101 p., https://doi.org/10.3133/70170196.","productDescription":"101 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":626365,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jannis, J. A.","contributorId":30091,"corporation":false,"usgs":true,"family":"Jannis","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":626366,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70156358,"text":"70156358 - 1978 - Wood River mining district, Idaho - intrusion-related lead-silver deposits derived from country rock source","interactions":[],"lastModifiedDate":"2015-08-20T14:27:05","indexId":"70156358","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Wood River mining district, Idaho - intrusion-related lead-silver deposits derived from country rock source","docAbstract":"<p>Lead-silver deposits in the Wood River mining district occur in shear zones in hornfelsed argillite of the Devonian Milligen Formation near granitic plutons and under the Wood River thrust fault. The principal ore minerals are argentiferous galena and sphalerite; siderite is the principal gangue. The &delta;<sup>34</sup>S values of the sulfide minerals range from +2.2 to +15.0 permil, indicating that the sulfur had a shallow crustal source. &Delta;<sup>34</sup>S values between sphalerite and galena range from +2.3 to +3.4 permil, corresponding to sulfur isotope temperatures between 280&deg; and 182 &deg;C. Hydrothermal barite has a&nbsp;&delta;<sup>34</sup>S of +13.2 permil. Lead isotope ratios are radiogenic, also pointing to a shallow crustal source. Quartz gangue has &delta;<sup>18</sup>O of +16.4 permil and a calculated &delta;<sup>18</sup>O<sub>H20</sub> at 270&deg;C of +8.4 permil. This value is reasonable for a hydrothermal fluid that had reached equilibrium with the argillite country rock. The siderite gangue has&nbsp;&delta;<sup>18</sup>O and&nbsp;&delta;<sup>13</sup>C values of +14.0 and -5.5 permil, respectively. Fluid inclusions have homogenization temperatures of 244&deg;-307&deg;C and average 270&deg;C. Freezing-stage measurements ranged from -1.85 to -2.8&deg;C, suggesting salinities of 3.2 to 4.8 weight percent. The &delta;D values of inclusion fluid in ore and gangue minerals are -110 to -120 permil. The geology, isotope, and fluid-inclusion data are consistent with a model of hydrothermal systems of meteoric water in faulted and shattered Paleozoic rocks near plutonic masses. This environment permitted deep circulation of the hydrothermal fluids, which dissolved the metals and sulfur from the Paleozoic host rocks and deposited ore in favorable beds or structures under the regional Wood River thrust fault.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Hall, W.E., Rye, R.O., and Doe, B.R., 1978, Wood River mining district, Idaho - intrusion-related lead-silver deposits derived from country rock source: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 579-592.","productDescription":"14 p.","startPage":"579","endPage":"592","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":306999,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":306998,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Idaho","county":"Blaine County","city":"Hailey, Bellevue","otherGeospatial":"Wood River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.52629089355469,\n              43.3616313239934\n            ],\n            [\n              -114.52629089355469,\n              43.76514352427404\n            ],\n            [\n              -114.04907226562499,\n              43.76514352427404\n            ],\n            [\n              -114.04907226562499,\n              43.3616313239934\n            ],\n            [\n              -114.52629089355469,\n              43.3616313239934\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d6fa38e4b0518e3546bc5f","contributors":{"authors":[{"text":"Hall, Wayne E.","contributorId":89955,"corporation":false,"usgs":true,"family":"Hall","given":"Wayne","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":568845,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rye, Robert O. rrye@usgs.gov","contributorId":1486,"corporation":false,"usgs":true,"family":"Rye","given":"Robert","email":"rrye@usgs.gov","middleInitial":"O.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":568846,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Doe, Bruce R.","contributorId":87554,"corporation":false,"usgs":true,"family":"Doe","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":568847,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70156426,"text":"70156426 - 1978 - Late Miocene mollusks from the Queen Charlotte Islands, British Columbia, Canada","interactions":[],"lastModifiedDate":"2015-08-21T10:52:33","indexId":"70156426","displayToPublicDate":"1978-11-30T18:00:00","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Late Miocene mollusks from the Queen Charlotte Islands, British Columbia, Canada","docAbstract":"<p>A fauna of bivalve mollusks, scattered gastropods, and an echinoid from exposures of the Skonun Formation in the northeastern part of Graham Island is indicative of an early late Miocene age and correlation with the provincial Wishkahan Stage. The molluscan assemblages are from the upper 600 of the 1800-m-thick marine and nonmarine formation, which appears to be entirely of late Miocene age. The Skonun Formation is the strandline fa.cies of marginal marine and nonmarine deposits of the northwestern part of the Queen Charlotte basin, a Nieogene embayment paralleling the modern mainland coast. The molluscan fauna and associated lignite beds are known from a few widely scattered outcrops; they are indicative of alternating marine and nonmarine to brackish-water environments in the upper part of the formation. The Skonun fauna occurs near the northern boundary of the Pacific Northwest Neogene molluscan province. It is the only marine Neogene molluscan fauna known from the British Columbia coast. The fauna has strong taxonomic ties with the fauna of the Empire Formation of southwestern Oregon and has several species in common with the upper Miocene of the Lituya district, southeastern Alaska, implying that these three faunas are coeval.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Arlington, VA","usgsCitation":"Addicott, W.O., 1978, Late Miocene mollusks from the Queen Charlotte Islands, British Columbia, Canada: Journal of Research of the U.S. Geological Survey, v. 6, no. 5, p. 677-689.","productDescription":"13 p.","startPage":"677","endPage":"689","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":307118,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307111,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1978/vol6issue5/report.pdf","text":"Report","size":"31.11 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"Canada","otherGeospatial":"Queen Charlotte Islands, Graham Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -133.22296142578125,\n              53.1237017988457\n            ],\n            [\n              -133.22296142578125,\n              54.27645123048291\n            ],\n            [\n              -131.81396484375,\n              54.27645123048291\n            ],\n            [\n              -131.81396484375,\n              53.1237017988457\n            ],\n            [\n              -133.22296142578125,\n              53.1237017988457\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"6","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55d84bb9e4b0518e3546f01a","contributors":{"authors":[{"text":"Addicott, Warren O.","contributorId":80668,"corporation":false,"usgs":true,"family":"Addicott","given":"Warren","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":569135,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70199553,"text":"70199553 - 1978 - Model aids planners in predicting rising ground-water levels in San Bernardino, California","interactions":[],"lastModifiedDate":"2018-09-20T15:49:02","indexId":"70199553","displayToPublicDate":"1978-11-01T15:48:16","publicationYear":"1978","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3825,"text":"Groundwater","active":true,"publicationSubtype":{"id":10}},"title":"Model aids planners in predicting rising ground-water levels in San Bernardino, California","docAbstract":"<p>The city of San Bernardino is in a semiarid inland valley about 60 miles (100 kilometers) east of Los Angeles. The southern part of the city is traversed by the San Jacinto fault. Adjacent to the upgradient (northeast) side of the fault is a 10 square mile (26 square kilometers) area which contains a zone in the alluvial ground‐water basin that formerly was under artesian pressure and consisted of swampy lands with a history of flowing wells, springs, and ground‐water discharge to Warm Creek.</p><p>Since about 1945, water levels have declined more than 100 feet (30 meters), and the swampy lands have dried up and are now highly urbanized. Basin replenishment by artificial recharge of imported northern California water at the base of the San Bernardino Mountains may cause ground‐water levels to rise again in the area that was formerly swampy land. If this should happen, building foundations and basements could be subjected to structural damage and flooding by renewed flowing of unplugged artesian wells.</p><p>The U.S. Geological Survey, in cooperation with the San Bernardino Valley Municipal Water District, is developing a two‐layer digital model to aid in predicting the rate and extent of the rise in water levels. The solution to the mathematical equations used in the model was approximated numerically by the Galerkin finite‐element method. The water district desires to evaluate water management alternatives, such as varying location, distribution, amounts of recharge, and pumping centers, to avoid excessive water level rises that could indicate an overfilling of the basin and could cause damage.</p>","language":"English","doi":"10.1111/j.1745-6584.1978.tb03257.x","usgsCitation":"Hardt, W.F., and Hutchinson, C.B., 1978, Model aids planners in predicting rising ground-water levels in San Bernardino, California: Groundwater, v. 16, no. 6, p. 424-431, https://doi.org/10.1111/j.1745-6584.1978.tb03257.x.","productDescription":"8 p.","startPage":"424","endPage":"431","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":357576,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"San Berndardino","volume":"16","issue":"6","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Hardt, William F.","contributorId":70013,"corporation":false,"usgs":true,"family":"Hardt","given":"William","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":745839,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hutchinson, C. B.","contributorId":94655,"corporation":false,"usgs":true,"family":"Hutchinson","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":745840,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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