{"pageNumber":"5600","pageRowStart":"139975","pageSize":"25","recordCount":184776,"records":[{"id":27342,"text":"wri8049 - 1980 - Reconnaissance snow survey of the National Petroleum Reserve in Alaska, April-May 1979","interactions":[],"lastModifiedDate":"2019-07-09T13:00:59","indexId":"wri8049","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-49","title":"Reconnaissance snow survey of the National Petroleum Reserve in Alaska, April-May 1979","docAbstract":"Moderately low snowfall and an early and abrupt spring thaw resulted in removal of most of the snow cover from the National Petroleum Reserve in Alaska (NPRA) before the snow survey of April 30 through May 2, 1979. Logistical problems and lack of snow permitted sampling at only seven sites. The average snow depth (0.263 meter) was approximately 60% of that measured in the 1977 and 1978 surveys. Snow density in 1979 averaged 337 kilograms per cubic meter and water equivalent averaged 0.088 meter. These two values are about 110% and 70%, respectively, of values for those characteristics in 1977-78. The average temperature of -5.2 Celsius at the base of the snowpack was about 6 Celsius higher than in the previous surveys. Extensive recent slab avalanche activity was noted in the Brooks Range. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8049","usgsCitation":"Glude, W.J., and Sloan, C.E., 1980, Reconnaissance snow survey of the National Petroleum Reserve in Alaska, April-May 1979: U.S. Geological Survey Water-Resources Investigations Report 80-49, iii, 13 p. , https://doi.org/10.3133/wri8049.","productDescription":"iii, 13 p. ","costCenters":[],"links":[{"id":365384,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0049/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158875,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0049/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"National Petroleum Reserve","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -158.84033203125,\n              68.47186403726954\n            ],\n            [\n              -149.4140625,\n              68.47186403726954\n            ],\n            [\n              -149.4140625,\n              71.335983102213\n            ],\n            [\n              -158.84033203125,\n              71.335983102213\n            ],\n            [\n              -158.84033203125,\n              68.47186403726954\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67c2cd","contributors":{"authors":[{"text":"Glude, William J.","contributorId":60684,"corporation":false,"usgs":true,"family":"Glude","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":197947,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sloan, Charles E.","contributorId":74364,"corporation":false,"usgs":true,"family":"Sloan","given":"Charles","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":197948,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8113,"text":"ofr801290 - 1980 - Selected administrative, land, and resource data for Known Geothermal Resources Areas in Arizona, California, Idaho, Nevada, Oregon, and Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr801290","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1290","title":"Selected administrative, land, and resource data for Known Geothermal Resources Areas in Arizona, California, Idaho, Nevada, Oregon, and Washington","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801290","usgsCitation":"Burkhardt, H., Brook, C., and Smith, F., 1980, Selected administrative, land, and resource data for Known Geothermal Resources Areas in Arizona, California, Idaho, Nevada, Oregon, and Washington: U.S. Geological Survey Open-File Report 80-1290, i, 29 p. ;28 cm., https://doi.org/10.3133/ofr801290.","productDescription":"i, 29 p. ;28 cm.","costCenters":[],"links":[{"id":140629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1290/report-thumb.jpg"},{"id":35718,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1290/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa787","contributors":{"authors":[{"text":"Burkhardt, H.E.","contributorId":69974,"corporation":false,"usgs":true,"family":"Burkhardt","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":157170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brook, C.A.","contributorId":82699,"corporation":false,"usgs":true,"family":"Brook","given":"C.A.","email":"","affiliations":[],"preferred":false,"id":157171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, F.W.","contributorId":27445,"corporation":false,"usgs":true,"family":"Smith","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":157169,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":7371,"text":"ofr802010 - 1980 - Overconsolidated surficial sediment on the Beaufort Sea shelf","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr802010","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-2010","title":"Overconsolidated surficial sediment on the Beaufort Sea shelf","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr802010","usgsCitation":"Reimnitz, E., Kempema, E., Ross, R., and Minkler, P., 1980, Overconsolidated surficial sediment on the Beaufort Sea shelf: U.S. Geological Survey Open-File Report 80-2010, 37 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr802010.","productDescription":"37 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140388,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/2010/report-thumb.jpg"},{"id":34770,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/2010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a30b","contributors":{"authors":[{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":155442,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kempema, Edward","contributorId":49353,"corporation":false,"usgs":true,"family":"Kempema","given":"Edward","email":"","affiliations":[],"preferred":false,"id":155444,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, Robin","contributorId":36547,"corporation":false,"usgs":true,"family":"Ross","given":"Robin","email":"","affiliations":[],"preferred":false,"id":155443,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Minkler, Peter","contributorId":8846,"corporation":false,"usgs":true,"family":"Minkler","given":"Peter","email":"","affiliations":[],"preferred":false,"id":155441,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":7370,"text":"ofr801226 - 1980 - Overburden geochemistry of the U.S. Bureau of Land Management experimental coal mining reclamation site at Ojo Encino, Northeast McKinley County, San Juan Basin, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr801226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1226","title":"Overburden geochemistry of the U.S. Bureau of Land Management experimental coal mining reclamation site at Ojo Encino, Northeast McKinley County, San Juan Basin, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801226","usgsCitation":"Hinkley, T.K., Herring, J., Smith, K., and Boerngen, J., 1980, Overburden geochemistry of the U.S. Bureau of Land Management experimental coal mining reclamation site at Ojo Encino, Northeast McKinley County, San Juan Basin, New Mexico: U.S. Geological Survey Open-File Report 80-1226, 21 p.  ;28 cm., https://doi.org/10.3133/ofr801226.","productDescription":"21 p.  ;28 cm.","costCenters":[],"links":[{"id":140387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1226/report-thumb.jpg"},{"id":112896,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1226/report.pdf","size":"701","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a3f0","contributors":{"authors":[{"text":"Hinkley, Todd K. 0000-0001-8507-6271 thinkley@usgs.gov","orcid":"https://orcid.org/0000-0001-8507-6271","contributorId":1497,"corporation":false,"usgs":true,"family":"Hinkley","given":"Todd","email":"thinkley@usgs.gov","middleInitial":"K.","affiliations":[{"id":211,"text":"Crustal Geophysics and Geochemistry Science Center","active":true,"usgs":true}],"preferred":true,"id":155437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herring, J. R.","contributorId":43348,"corporation":false,"usgs":true,"family":"Herring","given":"J. R.","affiliations":[],"preferred":false,"id":155439,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, K. S. 0000-0001-8547-9804","orcid":"https://orcid.org/0000-0001-8547-9804","contributorId":47779,"corporation":false,"usgs":true,"family":"Smith","given":"K. S.","affiliations":[],"preferred":false,"id":155440,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boerngen, J.G.","contributorId":28974,"corporation":false,"usgs":true,"family":"Boerngen","given":"J.G.","affiliations":[],"preferred":false,"id":155438,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":48495,"text":"ofr80396 - 1980 - Spectrographic and chemical analyses of whole-rock and insoluble-residue samples, Rolla 1 degrees by 2 degrees quadrangle, Missouri; drill hole No. 63","interactions":[],"lastModifiedDate":"2012-02-02T00:10:08","indexId":"ofr80396","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-396","title":"Spectrographic and chemical analyses of whole-rock and insoluble-residue samples, Rolla 1 degrees by 2 degrees quadrangle, Missouri; drill hole No. 63","language":"ENGLISH","doi":"10.3133/ofr80396","usgsCitation":"Mosier, E.L., Arbogast, B., and McDanal, S., 1980, Spectrographic and chemical analyses of whole-rock and insoluble-residue samples, Rolla 1 degrees by 2 degrees quadrangle, Missouri; drill hole No. 63: U.S. Geological Survey Open-File Report 80-396, 25 p.; 27 cm., https://doi.org/10.3133/ofr80396.","productDescription":"25 p.; 27 cm.","costCenters":[],"links":[{"id":162239,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4f19","contributors":{"authors":[{"text":"Mosier, E. L.","contributorId":71537,"corporation":false,"usgs":true,"family":"Mosier","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":237626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Arbogast, B. F.","contributorId":60623,"corporation":false,"usgs":true,"family":"Arbogast","given":"B. F.","affiliations":[],"preferred":false,"id":237625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McDanal, S.K.","contributorId":108078,"corporation":false,"usgs":true,"family":"McDanal","given":"S.K.","email":"","affiliations":[],"preferred":false,"id":237627,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":6116,"text":"pp1156 - 1980 - Patterns and trends of land use and land cover on Atlantic and Gulf Coast barrier islands","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"pp1156","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1156","title":"Patterns and trends of land use and land cover on Atlantic and Gulf Coast barrier islands","language":"ENGLISH","publisher":"Geological Survey (U.S.)","doi":"10.3133/pp1156","usgsCitation":"Lins, H.F., 1980, Patterns and trends of land use and land cover on Atlantic and Gulf Coast barrier islands: U.S. Geological Survey Professional Paper 1156, viii, 164 p., https://doi.org/10.3133/pp1156.","productDescription":"viii, 164 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":117283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1156/report-thumb.jpg"},{"id":33173,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1156/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688aec","contributors":{"authors":[{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":152146,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8256,"text":"ofr801297 - 1980 - Working notes on current-meter deployment, recovery, maintenance, and data processing for San Francisco Bay","interactions":[],"lastModifiedDate":"2016-07-27T10:41:30","indexId":"ofr801297","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-1297","title":"Working notes on current-meter deployment, recovery, maintenance, and data processing for San Francisco Bay","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr801297","usgsCitation":"Cheng, R.T., and Gartner, J.W., 1980, Working notes on current-meter deployment, recovery, maintenance, and data processing for San Francisco Bay: U.S. Geological Survey Open-File Report 80-1297, 71 p. ;27 cm., https://doi.org/10.3133/ofr801297.","productDescription":"71 p. ;27 cm.","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":140071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1297/report-thumb.jpg"},{"id":35872,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1297/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae02","contributors":{"authors":[{"text":"Cheng, Ralph T.","contributorId":69134,"corporation":false,"usgs":true,"family":"Cheng","given":"Ralph","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":157436,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gartner, Jeffrey W.","contributorId":77524,"corporation":false,"usgs":true,"family":"Gartner","given":"Jeffrey","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157437,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28066,"text":"wri8076 - 1980 - Simulation of water-quality data at selected stream sites in the Missouri River Basin, Montana","interactions":[],"lastModifiedDate":"2018-11-14T10:15:59","indexId":"wri8076","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-76","title":"Simulation of water-quality data at selected stream sites in the Missouri River Basin, Montana","docAbstract":"<p>Modification of sampling programs at some water-quality stations in the Missouri River basin in Montana has eliminated the means by which solute loads have been directly obtained in past years. To compensate for this loss, water-quality and streamflow data were statistically analyzed and solute loads were simulated using computer techniques.</p><p>Functional relationships existing between specific conductance and solute concentration for monthly samples were used to develop linear regression models. The models were then used to simulate daily solute concentrations using daily specific conductance as the independent variable. Once simulated, the solute concentrations, in milligrams per liter, were transformed into daily solute loads, in tons, using mean daily streamflow records.</p><p>Computer output was formatted into tables listing simulated mean monthly solute concentrations, in milligrams per liter, and the monthly and annual solute loads, in tons, for water years 1975-78.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8076","usgsCitation":"Knapton, J.R., and Jacobson, M., 1980, Simulation of water-quality data at selected stream sites in the Missouri River Basin, Montana: U.S. Geological Survey Water-Resources Investigations Report 80-76, iv, 30 p., https://doi.org/10.3133/wri8076.","productDescription":"iv, 30 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,{"id":68006,"text":"ha631 - 1980 - Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Daphne-Point Clear quadrangles, Alabama","interactions":[],"lastModifiedDate":"2022-10-07T20:07:17.867974","indexId":"ha631","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"631","title":"Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Daphne-Point Clear quadrangles, Alabama","docAbstract":"<p>Shown on a topographic map are floodmark elevations and approximate areas flooded by Hurricane Frederic tides of September 12-13, 1979, along the eastern shore of Mobile Bay generally from Daphne, Alabama, southward through Fairhope and Point Clear to Mullet Point, Alabama. Buildings and sewalls were damaged by flooding and tidal waves in the vicinity of Fairhope, Alabama. Most fishing piers along the shore were either destroyed or severely damaged. From Fairhope southward, many homes and other buildings, including the Grand Hotel complex at Great Point Clear, were severely damaged. Storm-tide frequency and records of annual maximum tides at Mobile, Alabama, since 1772, are presented. Offshore winds reached about 160 miles per hour. A wind-velocity of about 145 miles per hour was recorded near Dauphin Island, Alabama.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha631","usgsCitation":"Scott, J.C., and Bohman, L.R., 1980, Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Daphne-Point Clear quadrangles, Alabama: U.S. Geological Survey Hydrologic Atlas 631, 1 Plate: 25.90 × 40.74 inches, https://doi.org/10.3133/ha631.","productDescription":"1 Plate: 25.90 × 40.74 inches","costCenters":[],"links":[{"id":408124,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16029.htm","linkFileType":{"id":5,"text":"html"}},{"id":89250,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/631/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188386,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Alabama","otherGeospatial":"Daphne and Point Clear quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.958,\n              30.417\n            ],\n            [\n              -87.875,\n              30.417\n            ],\n            [\n              -87.875,\n              30.625\n            ],\n            [\n              -87.958,\n              30.625\n            ],\n            [\n              -87.958,\n              30.417\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6960af","contributors":{"authors":[{"text":"Scott, John C.","contributorId":21963,"corporation":false,"usgs":true,"family":"Scott","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bohman, Larry R. lrbohman@usgs.gov","contributorId":4769,"corporation":false,"usgs":true,"family":"Bohman","given":"Larry","email":"lrbohman@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":277491,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9358,"text":"ofr8060 - 1980 - Preliminary catalog of seismicity prior to the Guatemala earthquake of February 4, 1976, from the area between Guatemala City and Lake Atitlan, March 4, 1975 - February 4, 1976","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr8060","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-60","title":"Preliminary catalog of seismicity prior to the Guatemala earthquake of February 4, 1976, from the area between Guatemala City and Lake Atitlan, March 4, 1975 - February 4, 1976","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8060","usgsCitation":"Harlow, D.H., and White, R., 1980, Preliminary catalog of seismicity prior to the Guatemala earthquake of February 4, 1976, from the area between Guatemala City and Lake Atitlan, March 4, 1975 - February 4, 1976: U.S. Geological Survey Open-File Report 80-60, [ii], 27 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr8060.","productDescription":"[ii], 27 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":140855,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0060/report-thumb.jpg"},{"id":37070,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c79d","contributors":{"authors":[{"text":"Harlow, David H.","contributorId":15198,"corporation":false,"usgs":true,"family":"Harlow","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159539,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, R.A.","contributorId":21953,"corporation":false,"usgs":true,"family":"White","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":159540,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68004,"text":"ha633 - 1980 - Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Bon Secour Bay quadrangle, Alabama","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"ha633","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"633","title":"Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Bon Secour Bay quadrangle, Alabama","docAbstract":"Shown on the Bon Secour Bay map are floodmark elevations and approximate areas flooded by Hurricane Frederic tides of September 12-13, 1979, along the shore of Bon Secour Bay, generally from Weeks Bay southward to Gasque, Alabama. Most homes along the northern shore of Bon Secour Bay were severely damaged by floodwater and tidal waves. Damage to homes along the southern shore was not as great. Storm-tide frequency and records of annual maximum tides at Mobile, Ala., since 1772, are presented. Offshore winds reached about 160 miles per hour. A wind-velocity of about 145 miles per hour was recorded near Dauphin Island, Ala. (USGS)","language":"ENGLISH","doi":"10.3133/ha633","usgsCitation":"Scott, J.C., and Bohman, L.R., 1980, Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Bon Secour Bay quadrangle, Alabama: U.S. Geological Survey Hydrologic Atlas 633, 1 map :col. ;58 x 50 cm., https://doi.org/10.3133/ha633.","productDescription":"1 map :col. ;58 x 50 cm.","costCenters":[],"links":[{"id":188384,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89248,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/633/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.86749999999999,30.25 ], [ -87.86749999999999,30.3675 ], [ -87.75,30.3675 ], [ -87.75,30.25 ], [ -87.86749999999999,30.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a50f","contributors":{"authors":[{"text":"Scott, John C.","contributorId":21963,"corporation":false,"usgs":true,"family":"Scott","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277488,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bohman, Larry R. lrbohman@usgs.gov","contributorId":4769,"corporation":false,"usgs":true,"family":"Bohman","given":"Larry","email":"lrbohman@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":277487,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28230,"text":"wri8044 - 1980 - Evaluation of selected dam-break flood-wave models by using field data","interactions":[],"lastModifiedDate":"2012-02-02T00:08:50","indexId":"wri8044","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-44","title":"Evaluation of selected dam-break flood-wave models by using field data","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division, Gulf Coast Hydroscience Center, National Space Technology Laboratories,","doi":"10.3133/wri8044","usgsCitation":"Land, L.F., 1980, Evaluation of selected dam-break flood-wave models by using field data: U.S. Geological Survey Water-Resources Investigations Report 80-44, vi, 54 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8044.","productDescription":"vi, 54 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123233,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0044/report-thumb.jpg"},{"id":57061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fab79","contributors":{"authors":[{"text":"Land, Larry F.","contributorId":60612,"corporation":false,"usgs":true,"family":"Land","given":"Larry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199431,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69453,"text":"gp937 - 1980 - Aeromagnetic map of part of the southeastern United States","interactions":[],"lastModifiedDate":"2012-02-10T00:11:33","indexId":"gp937","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"937","title":"Aeromagnetic map of part of the southeastern United States","language":"ENGLISH","doi":"10.3133/gp937","usgsCitation":"Zietz, I., and Gilbert, F.P., 1980, Aeromagnetic map of part of the southeastern United States: U.S. Geological Survey Geophysical Investigations Map 937, -, https://doi.org/10.3133/gp937.","productDescription":"-","costCenters":[],"links":[{"id":251513,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0937/report.pdf","size":"22","linkFileType":{"id":1,"text":"pdf"}},{"id":251514,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0937/plate-1.pdf","size":"4327","linkFileType":{"id":1,"text":"pdf"}},{"id":252461,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0937/report-thumb.jpg"}],"scale":"2000000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88,40 ], [ -88,75 ], [ -75,75 ], [ -75,40 ], [ -88,40 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697865","contributors":{"authors":[{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":280457,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilbert, F. P.","contributorId":53033,"corporation":false,"usgs":true,"family":"Gilbert","given":"F.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":280456,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66986,"text":"i1129 - 1980 - Geologic map and structure sections of the Cokeville 30-minute Quadrangle, Lincoln and Sublette counties Wyoming","interactions":[{"subject":{"id":47114,"text":"ofr76597 - 1976 - Geologic map of the Cokeville 30-minute Quadrangle, Lincoln and Sublette counties, Wyoming","indexId":"ofr76597","publicationYear":"1976","noYear":false,"title":"Geologic map of the Cokeville 30-minute Quadrangle, Lincoln and Sublette counties, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":66986,"text":"i1129 - 1980 - Geologic map and structure sections of the Cokeville 30-minute Quadrangle, Lincoln and Sublette counties Wyoming","indexId":"i1129","publicationYear":"1980","noYear":false,"title":"Geologic map and structure sections of the Cokeville 30-minute Quadrangle, Lincoln and Sublette counties Wyoming"},"id":1}],"lastModifiedDate":"2012-02-10T00:11:10","indexId":"i1129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1129","subseriesTitle":"NONE","title":"Geologic map and structure sections of the Cokeville 30-minute Quadrangle, Lincoln and Sublette counties Wyoming","language":"ENGLISH","doi":"10.3133/i1129","usgsCitation":"Rubey, W., Oriel, S., and Tracey, J.I., 1980, Geologic map and structure sections of the Cokeville 30-minute Quadrangle, Lincoln and Sublette counties Wyoming: U.S. Geological Survey IMAP 1129, 1 map : col. ;88 x 66 cm. +13 structure sections on sheet 125 x 80 cm., https://doi.org/10.3133/i1129.","productDescription":"1 map : col. ;88 x 66 cm. +13 structure sections on sheet 125 x 80 cm.","costCenters":[],"links":[{"id":106612,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8980.htm","linkFileType":{"id":5,"text":"html"},"description":"8980"},{"id":189981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111,42 ], [ -111,42.5 ], [ -110.5,42.5 ], [ -110.5,42 ], [ -111,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671fd0","contributors":{"authors":[{"text":"Rubey, W.W.","contributorId":6426,"corporation":false,"usgs":true,"family":"Rubey","given":"W.W.","affiliations":[],"preferred":false,"id":275411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oriel, S.S.","contributorId":42591,"corporation":false,"usgs":true,"family":"Oriel","given":"S.S.","affiliations":[],"preferred":false,"id":275413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tracey, J. I.","contributorId":35718,"corporation":false,"usgs":true,"family":"Tracey","given":"J.","middleInitial":"I.","affiliations":[],"preferred":false,"id":275412,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":67652,"text":"l200 - 1980 - Land use and land cover, 1973-76, Waco, Texas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"l200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"200","title":"Land use and land cover, 1973-76, Waco, Texas","language":"ENGLISH","doi":"10.3133/l200","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Land use and land cover, 1973-76, Waco, Texas: U.S. Geological Survey Land Use and Land Cover 200, -, https://doi.org/10.3133/l200.","productDescription":"-","costCenters":[],"links":[{"id":185724,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260959,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/200/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98,31 ], [ -98,32 ], [ -96,32 ], [ -96,31 ], [ -98,31 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae463","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":534398,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68007,"text":"ha635 - 1980 - Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Gulf Shores quadrangle, Alabama","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"ha635","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"635","title":"Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Gulf Shores quadrangle, Alabama","docAbstract":"Shown on the Gulf Shores topographic map are floodmark elevations and approximate areas flooded by Hurricane Frederic tides of September 12-13, 1979, along the shores of the Gulf of Mexico, Oyster Bay, and the Bon Secour River, in Alabama. Most beachfront homes in the Gulf Shores area and most homes fronting on Little Lagoon in western Gulf Shores were either destroyed or heavily damaged. All beachfront motels were severly damaged. Damage to homes and other buildings in the Oyster Bay-Bon Secour area was not as great. Storm-tide frequency and records of annual maximum tides at Mobile, Ala., since 1772, are presented. Offshore winds reached about 160 miles per hour. A wind-velocity of about 145 miles per hour was recorded near Dauphin Island, Ala. (USGS)","language":"ENGLISH","doi":"10.3133/ha635","usgsCitation":"Scott, J.C., and Bohman, L.R., 1980, Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Gulf Shores quadrangle, Alabama: U.S. Geological Survey Hydrologic Atlas 635, 1 map :col. ;65 x 50 cm., https://doi.org/10.3133/ha635.","productDescription":"1 map :col. ;65 x 50 cm.","costCenters":[],"links":[{"id":188387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89251,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/635/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.75,30.25 ], [ -87.75,30.3675 ], [ -87.61749999999999,30.3675 ], [ -87.61749999999999,30.25 ], [ -87.75,30.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629e3d","contributors":{"authors":[{"text":"Scott, John C.","contributorId":21963,"corporation":false,"usgs":true,"family":"Scott","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277494,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bohman, Larry R. lrbohman@usgs.gov","contributorId":4769,"corporation":false,"usgs":true,"family":"Bohman","given":"Larry","email":"lrbohman@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":277493,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":67639,"text":"l170 - 1980 - Land use and land cover, 1974-75, Wolf Point, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:29","indexId":"l170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":321,"text":"Land Use and Land Cover","code":"L","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"170","title":"Land use and land cover, 1974-75, Wolf Point, Montana","language":"ENGLISH","doi":"10.3133/l170","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Land use and land cover, 1974-75, Wolf Point, Montana: U.S. Geological Survey Land Use and Land Cover 170, -, https://doi.org/10.3133/l170.","productDescription":"-","costCenters":[],"links":[{"id":186530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260944,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/l/170/plate-1.pdf"}],"scale":"1","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106,48 ], [ -106,48.5 ], [ -105,48.5 ], [ -105,48 ], [ -106,48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae294","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":534385,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27894,"text":"wri812 - 1980 - Temperature and solute-transport simulation in streamflow using a Lagrangian reference frame","interactions":[],"lastModifiedDate":"2018-11-02T10:26:27","indexId":"wri812","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"81-2","title":"Temperature and solute-transport simulation in streamflow using a Lagrangian reference frame","docAbstract":"<p>A computer program for simulating one-dimensional, unsteady temperature and solute transport in a river has been developed and documented for general use. The solution approach to the convective-diffusion equation uses a moving reference frame (Lagrangian) which greatly simplifies the mathematics of the solution procedure and dramatically reduces errors caused by numerical dispersion. The solution procedure has the further advantages, relative to conventional Eulerian solution schemes, of being easy to understand in the physical sense, of being extremely stable numerically, and of providing an accounting system which is very useful for model calibration.</p><p>The model documentation is presented as a series of four programs of increasing complexity. The conservative transport model can be used to route a single conservative substance, such as dye, through a reach of a river. The simplified temperature model is used to predict water temperature in rivers, either with or without thermal loading, when few meteorological data are available. Only equilibrium temperature and windspeed are required. It is suggested that air temperature can be used to approximate equilibrium temperature. The complete temperature model is highly accurate but requires rather complete meteorological data. Finally, the 10-parameter model can be used to route as many as 10 interacting constituents through a river reach. The mathematical description of the interaction between the constituents, which does not need to be linear, is generally up to the user to supply. An example problem is solved for a three-parameter system involving temperature, dissolved oxygen, and biochemical oxygen demand.</p><p>For simplicity, all models are developed and presented assuming steady non-uniform flow. Generalization of the models to allow unsteady flow is extremely simple, involving the addition of no more than 18 cards to the program deck. The report is concluded by describing this generalization for any of the models. Before using the models with unsteady flow, a flow model must be used to calculate and store the necessary flow data at each cross section and time step. Such a flow model is available and documented.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri812","usgsCitation":"Jobson, H.E., 1980, Temperature and solute-transport simulation in streamflow using a Lagrangian reference frame: U.S. Geological Survey Water-Resources Investigations Report 81-2, ix, 165 p., https://doi.org/10.3133/wri812.","productDescription":"ix, 165 p.","costCenters":[],"links":[{"id":359109,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0002/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0002/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685762","contributors":{"authors":[{"text":"Jobson, Harvey E.","contributorId":27032,"corporation":false,"usgs":true,"family":"Jobson","given":"Harvey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28248,"text":"wri8078 - 1980 - Water-quality monitoring of three major tributaries to the Chesapeake Bay: Interim data report","interactions":[],"lastModifiedDate":"2017-07-12T14:11:31","indexId":"wri8078","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-78","title":"Water-quality monitoring of three major tributaries to the Chesapeake Bay: Interim data report","docAbstract":"<p>The U.S. Geological Survey is monitoring the water quality of three major tributaries to Chesapeake Bay at their fall lines to obtain estimates of constituent inputs potentially available to the bay. The monitoring sites are: Susquehanna River at Conowingo, Md.; Potomac River at Washington, D.C.; and James River at Cartersville, Va. Water-quality data collected from October 1978 to April 1980 are presented in tables. Concentrations of major ions, nutrient and carbon species, metals, pesticides, suspended sediment, and other selected constituents are presented for a range of flows. The mean, standard deviation, minimum, maximum, and median values for each constituent were determined by standard methods and are presented for each sampling station. Bivariate linear regressions were run for all constituents versus streamf low, specific conductance, and suspended sediment. Those relationships exhibiting coefficients of determination (R ) greater than 0.50 are tabulated.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8078","usgsCitation":"Lang, D.J., and Grason, D., 1980, Water-quality monitoring of three major tributaries to the Chesapeake Bay: Interim data report: U.S. Geological Survey Water-Resources Investigations Report 80-78, x, 66 p., https://doi.org/10.3133/wri8078.","productDescription":"x, 66 p.","numberOfPages":"79","costCenters":[],"links":[{"id":159213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0078/report-thumb.jpg"},{"id":343735,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0078/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"James River, Potomac River, Susquehanna River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80,\n              37\n            ],\n            [\n              -75,\n              37\n            ],\n            [\n              -75,\n              42\n            ],\n            [\n              -80,\n              42\n            ],\n            [\n              -80,\n              37\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fa8f6","contributors":{"authors":[{"text":"Lang, David J.","contributorId":36548,"corporation":false,"usgs":true,"family":"Lang","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grason, David","contributorId":29819,"corporation":false,"usgs":true,"family":"Grason","given":"David","email":"","affiliations":[],"preferred":false,"id":199467,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28356,"text":"wri8093 - 1980 - Investigation of artificial recharge of aquifers in Nebraska","interactions":[],"lastModifiedDate":"2024-07-30T14:26:01.843492","indexId":"wri8093","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-93","title":"Investigation of artificial recharge of aquifers in Nebraska","docAbstract":"<p>Large withdrawals of ground water for irrigation are causing progressive declines of ground-water levels in some areas of Nebraska. An investigation was conducted to determine the technical feasibility of artificially recharging aquifers through wells and through surface spreading by means of impoundments, pits, and canals. Information gained from a literature search and from preliminary tests was used to design several artificial-recharge experiments. The experiments showed that large quantities of water can be recharged through wells and by surface spreading if conditions are favorable.</p><p>In the well experiments, about 0.5 billion gallons of water from an aquifer recharged by the Platte River was transported 3 miles by pipeline and recharged through a well into a Pleistocene sand and gravel aquifer near Aurora where ground-water levels are declining. The recharge rate was about 730 gallons per minute during two tests of 6 and 8 months duration. The rise in ground-water levels due to recharge extended more than a mile from the recharge well in both tests.</p><p>The pattern of ground-water-level buildup during the 8-month test was similar to that during the 6-month test. Two-thirds of the way through the test the rate of water-level buildup in the recharge well increased greatly because casing failure allowed a large amount of sediment to enter the well.</p><p>Although the chemical quality of the recharge water was markedly different from that of the native aquifer water, no evidence of clogging due to chemical reaction was detected; also, there was no evidence of clogging due to air entrainment or bacterial growth. Evaluation of water-level changes in the recharge well and in observation wells during the 6-month test indicated some clogging of the aquifer in the immediate vicinity of the recharge well due to a small amount (0.04 milligram per liter) of fine sediment in the recharge water. Analysis of water-level buildup in the recharge well during the 6-month test indicated that recharge could have continued at a rate of about 700 gallons per minute for several years before rehabilitation of the recharge well would have been necessary.</p><p>In surface-spreading experiments, the maximum sustained infiltration rates from a 24-foot-diameter ring infiltrometer set in loess at the well-recharge site near Aurora were about 0.5 foot per day during a 140day test. The recharge water caused water levels in a perched zone of saturation at depths between 36 and 38 feet to rise 15 feet, to within 21 feet of the surface, indicating that if the test had continued or if the impoundment area had been larger, the water level in the perched zone of saturation might have risen to the surface thereby reducing the infiltration rate.</p><p>The maximum sustained infiltration rate from a similar experiment in the Sand Hills near Tryon was 11 feet per day. Perching layers also retarded downward infiltration and caused lateral movement of water in the subsurface at this site.</p><p>Infiltration rates from re-use pits near the Aurora site ranged from 0.01 to 1.60 feet per day, indicating that the permeability of the subsurface material is extremely variable and that perching layers probably are absent in some areas.</p><p>Flow measurements in an irrigation canal excavated in loess near Farwell indicate an infiltration rate of 0.36 foot per day from a 2.7mile reach.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8093","collaboration":"Prepared in cooperation with the Old West Regional Commission; the Nebraska Resources Center, Institute of Agriculture and Natural Resources, The University of Nebraska-Lincoln and the Nebraska Natural Resources Commission","usgsCitation":"Lichtler, W.F., Stannard, D.I., and Kouma, E., 1980, Investigation of artificial recharge of aquifers in Nebraska: U.S. Geological Survey 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,{"id":68005,"text":"ha630 - 1980 - Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Bridgehead quadrangle, Alabama","interactions":[],"lastModifiedDate":"2012-02-10T00:11:16","indexId":"ha630","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"630","title":"Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Bridgehead quadrangle, Alabama","docAbstract":"Shown on a topographic map are floodmark elevations and approximate areas flooded by Hurricane Frederic tides of September 12-13, 1979, along the Mobile Causeway (U.S. Highway 90) from the Tensaw River to Spanish Fort, Alabama, and the eastern shore of Mobile Bay in the vicinity of Spanish Fort. Most buildings and business establishments along Mobile Causeway were completely destroyed, and the remaining buildings were severly damaged by flooding. Storm-tide frequency and records of annual maximum tides at Mobile, Alabama, since 1772, are presented. Offshore winds reached about 160 miles per hour. A wind-velocity of about 145 miles per hour was recorded near Dauphin Island, Alabama. (USGS)","language":"ENGLISH","doi":"10.3133/ha630","usgsCitation":"Scott, J.C., and Bohman, L.R., 1980, Hurricane Frederic tidal floods of September 12-13, 1979, along the Gulf Coast, Bridgehead quadrangle, Alabama: U.S. Geological Survey Hydrologic Atlas 630, 1 map : col. ;58 x 50 cm., https://doi.org/10.3133/ha630.","productDescription":"1 map : col. ;58 x 50 cm.","costCenters":[],"links":[{"id":188385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89249,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/630/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88,30.6175 ], [ -88,30.75 ], [ -87.86749999999999,30.75 ], [ -87.86749999999999,30.6175 ], [ -88,30.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a47a","contributors":{"authors":[{"text":"Scott, John C.","contributorId":21963,"corporation":false,"usgs":true,"family":"Scott","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277490,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bohman, Larry R. lrbohman@usgs.gov","contributorId":4769,"corporation":false,"usgs":true,"family":"Bohman","given":"Larry","email":"lrbohman@usgs.gov","middleInitial":"R.","affiliations":[],"preferred":true,"id":277489,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3746,"text":"cir814 - 1980 - Isolation of uranium mill tailings and their component radionuclides from the biosphere; some earth science perspectives","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir814","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"814","title":"Isolation of uranium mill tailings and their component radionuclides from the biosphere; some earth science perspectives","docAbstract":"Uranium mining and milling is an expanding activity in the. Western United States. Although the milling process yields a uranium concentrate, the large volume of tailings remaining contains about 85 percent of the radioactivity originally associated with the ore. By virtue of the physical and chemical processing of the ore and the redistribution of the contained radionuclides at the Earth's surface, these tailings constitute a technologically enhanced source of natural radiation exposure. Sources of potential human radiation exposure from uranium mill tailings include the emanation of radon gas, the transport of particles by wind and water, and the transport of soluble radionuclides, seeping from disposal areas, by ground water. Due to the 77,000 year half-life of thorium-230, the parent of radium-226, the environmental effects associated with radionuclides contained in these railings must be conceived of within the framework of geologic processes operating over geologic time. The magnitude of erosion of cover materials and tailings and the extent of geochemical mobilization of the contained radionuclides to the atmosphere and hydrosphere should be considered in the evaluation of the potential, long-term consequences of all proposed uranium mill tailings management plans.","language":"ENGLISH","publisher":"Dept. of the Interior, Geological Survey,","doi":"10.3133/cir814","usgsCitation":"Landa, E., 1980, Isolation of uranium mill tailings and their component radionuclides from the biosphere; some earth science perspectives: U.S. Geological Survey Circular 814, iii, 32 p. :ill., map ;26 cm., https://doi.org/10.3133/cir814.","productDescription":"iii, 32 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":124670,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1980/0814/report-thumb.jpg"},{"id":30808,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1980/0814/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db660e2e","contributors":{"authors":[{"text":"Landa, Edward","contributorId":100368,"corporation":false,"usgs":true,"family":"Landa","given":"Edward","affiliations":[],"preferred":false,"id":147523,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67988,"text":"ha619 - 1980 - Columbia Glacier, Alaska: Recent ice loss and its relationship to seasonal terminal embayments, thinning, and glacial flow","interactions":[{"subject":{"id":40361,"text":"ofr791265 - 1979 - Columbia Glacier, Alaska: Recent ice loss and its relationship to seasonal terminal embayments, thinning, and glacier flow","indexId":"ofr791265","publicationYear":"1979","noYear":false,"title":"Columbia Glacier, Alaska: Recent ice loss and its relationship to seasonal terminal embayments, thinning, and glacier flow"},"predicate":"SUPERSEDED_BY","object":{"id":67988,"text":"ha619 - 1980 - Columbia Glacier, Alaska: Recent ice loss and its relationship to seasonal terminal embayments, thinning, and glacial flow","indexId":"ha619","publicationYear":"1980","noYear":false,"title":"Columbia Glacier, Alaska: Recent ice loss and its relationship to seasonal terminal embayments, thinning, and glacial flow"},"id":1}],"lastModifiedDate":"2022-01-21T21:39:50.03072","indexId":"ha619","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"619","title":"Columbia Glacier, Alaska: Recent ice loss and its relationship to seasonal terminal embayments, thinning, and glacial flow","docAbstract":"<p>In 1974 the U.S. Geological Survey began an intensive investigation of the stability of Columbia Glacier, a calving tidewater glacier terminating in Columbia Bay, near Valdez, Alaska. Aerial photographs taken in 1957 and a sequence of photographs taken at about 2-month intervals since 1976, when analyzed photogrammetrically, provided detailed data on changes in Columbia Glacier's thickness, flow rate, and terminal position. Annual embayments in the glacier 's terminus form during the summer-autumn season in most years; the size of embayments appears to be related to (1) the thickness of the glacier, and (2) the position and nature of subglacial freshwater discharge. Embayments have apparently increased in size in recent years; the largest embayments yet observed formed in 1975, 1976, 1977, and 1978. From April 1, 1977, to April 1, 1978, the total volume of ice calved was about 1.0 cubic kilometer. By January 1979 the glacier front had retreated from Heather Island. Glacier flow varies seasonally and synchronously in the lower 17 kilometers of the glacier; large accelerations occur near the terminus in response to embayment formation. Daily speed within 5 kilometers of the terminus increased from about 1.9 meters per day between 1963 and 1968 to about 2.7 meters per day between 1977 and 1978. In the lowest 15 kilometers, the glacier surface was lowered about 9 meters between 1957 and 1974, and about 13 meters between 1974 and 1978. Columbia Glacier is being reduced in mass due, in part, to recent losses caused by large embayments forming annually. If such reduction continues it will result in a drastic retreat.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha619","usgsCitation":"Sikonia, W., and Post, A., 1980, Columbia Glacier, Alaska: Recent ice loss and its relationship to seasonal terminal embayments, thinning, and glacial flow: U.S. Geological Survey Hydrologic Atlas 619, 3 Plates: 33.50 × 41.18 inches or smaller, https://doi.org/10.3133/ha619.","productDescription":"3 Plates: 33.50 × 41.18 inches or smaller","costCenters":[],"links":[{"id":394726,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16015.htm"},{"id":89230,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/619/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89229,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/619/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89228,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/619/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","country":"United States","state":"Alaska","otherGeospatial":"Columbia Glacier","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147.30056762695312,\n              60.99974987461457\n            ],\n            [\n              -146.78009033203125,\n              60.99974987461457\n            ],\n            [\n              -146.78009033203125,\n              61.390143658580335\n            ],\n            [\n              -147.30056762695312,\n              61.390143658580335\n            ],\n            [\n              -147.30056762695312,\n              60.99974987461457\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae79d","contributors":{"authors":[{"text":"Sikonia, W. G.","contributorId":23946,"corporation":false,"usgs":true,"family":"Sikonia","given":"W. G.","affiliations":[],"preferred":false,"id":277458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":277459,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28059,"text":"wri8048 - 1980 - Distribution of nitrate in the unsaturated zone, Highland-East Highlands area, San Bernardino County, California","interactions":[],"lastModifiedDate":"2013-03-19T10:51:27","indexId":"wri8048","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-48","title":"Distribution of nitrate in the unsaturated zone, Highland-East Highlands area, San Bernardino County, California","docAbstract":"Nitrogen in the unsaturated soil zone in the Highland-East Highlands area of San Bernardino County, Calif., has been suspected as the source of nitrate in water from wells. Plans to recharge the local aquifers with imported surface water would raise the water table and intercept that nitrogen. This study was made to describe the distribution of inorganic nitrogen and other chemical constituents and nitrogen-using bacteria in the unsaturated zone, to relate nitrogen occurrences, in a general way, to present and historical land use, and to attempt to predict nitrogen concentrations in ground water after recharge. Some generalized correlations between nitrogen occurrence and land use were observed. In 11 of 13 test holes, the maximum nitrate-nitrogen (NO<sub>3</sub><sup>-</sup>-N) concentrations occurred within 10 feet of the surface, suggesting that the major source of nitrogen is from the surface at these sites. Test holes were ranked according to maximum NO<sub>3</sub><sup>-</sup>-N in the top 10 feet, total NO<sub>3</sub><sup>-</sup>-N in the top 10 feet, and total NO<sub>3</sub><sup>-</sup>-N in the top 40 feet. In all three rankings, the top seven test holes were the same--five in or near present or historical agricultural areas (primarily citrus groves), one in a feedlot, and one adjacent to an abandoned sewage-treatment plant. Two test holes in historically uninhabited areas ranked lowest. The control test hole  in an uninhabited area ranked high in geometric mean of ammonium-nitrogen concentration (NH<sub>4</sub><sup>+</sup>-N), suggesting that present in freshly weathered granite. The geometric means of NH<sub>4</sub><sup>+</sup>-N concentrations in six of eight citrus-related test holes were significantly lower than in the control hole, suggesting that irrigation in citrus groves may have created conditions favoring nitrification of the primary NH<sub>4</sub><sup>+</sup>-N. Rank correlation analyses between various measurements in test holes showed that high NO<sub>3</sub><sup>-</sup>-N concentrations tend to occur with high specific conductance and chloride concentrations in soil extracts. If recharge is carried out as planned, assuming complete mixing of the recharge water and interstitial pore water in the top 20 feet of the saturated zone, NO<sub>3</sub><sup>-</sup>-N concentrations in water at the top of the saturated zone may exceed 10 milligrams per liter in seven areas studied. Concentrations could reach as high as 66 milligrams per liter in the worst case projected. The highest concentrations may be found in three areas that are now, or were recently, citrus groves.","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8048","collaboration":"Prepared in cooperation with the San Bernardino Valley Municipal Water District","usgsCitation":"Klein, J.M., and Bradford, W.L., 1980, Distribution of nitrate in the unsaturated zone, Highland-East Highlands area, San Bernardino County, California: U.S. Geological Survey Water-Resources Investigations Report 80-48, v, 70 p., https://doi.org/10.3133/wri8048.","productDescription":"v, 70 p.","numberOfPages":"78","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":157990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri8048.png"},{"id":269696,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0048/WRIR80-48.pdf"}],"country":"United States","state":"California","city":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.8026,33.871 ], [ -117.8026,35.8093 ], [ -114.1308,35.8093 ], [ -114.1308,33.871 ], [ -117.8026,33.871 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db64096a","contributors":{"authors":[{"text":"Klein, John M.","contributorId":27036,"corporation":false,"usgs":true,"family":"Klein","given":"John","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":199149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradford, Wesley L.","contributorId":95451,"corporation":false,"usgs":true,"family":"Bradford","given":"Wesley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":199150,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27903,"text":"wri8026 - 1980 - Geology and ground water in north-central Santa Cruz County, California","interactions":[],"lastModifiedDate":"2019-07-09T12:38:02","indexId":"wri8026","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"80-26","title":"Geology and ground water in north-central Santa Cruz County, California","docAbstract":"North-central Santa Cruz County is underlain mainly by folded sedimentary rocks of Tertiary and Cretaceous age that have been highly fractured by movements in the San Andreas fault system. Ground water is stored in fractures within shale and mudstone formations and in intergranular pore spaces within fine- to very fine-grained sandstone and siltstone formations. Fewer than 10% of the wells yield more than 15 gallons of water per minute. The water in most wells is moderately hard to very hard, is generally of a sodium bicarbonate or calcium bicarbonate type, and commonly has excessive concentrations of iron or manganese. Of the many geologic units in the study area, only the Purisima Formation of Pliocene age has the potential to sustain well yields greater than 100 gallons per minute. (USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri8026","usgsCitation":"Johnson, M.J., 1980, Geology and ground water in north-central Santa Cruz County, California: U.S. Geological Survey Water-Resources Investigations Report 80-26, iv, 33 p. , https://doi.org/10.3133/wri8026.","productDescription":"iv, 33 p. ","costCenters":[],"links":[{"id":158642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1980/0026/report-thumb.jpg"},{"id":365383,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1980/0026/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Santa Cruz County","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684788","contributors":{"authors":[{"text":"Johnson, Michael J. johnsonm@usgs.gov","contributorId":2282,"corporation":false,"usgs":true,"family":"Johnson","given":"Michael","email":"johnsonm@usgs.gov","middleInitial":"J.","affiliations":[{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":198875,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}