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,{"id":23054,"text":"ofr78986 - 1978 - A magnesium correction for the Na-K-Ca chemical geothermometer","interactions":[],"lastModifiedDate":"2012-02-02T00:08:05","indexId":"ofr78986","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":"78-986","title":"A magnesium correction for the Na-K-Ca chemical geothermometer","docAbstract":"Graphs and equations have been devised to correct for the adverse effects of magnesium upon the Na-K-Ca geothermometer. Either the graphs or equations can be used to determine temperature corrections when given waters have Na-K-Ca calculated temperatures above 70? C and values of R less than 50, where R = {Mg/(Mg + Ca + K)} x 100 in equivalents. Waters with values of R greater than 50 probably come from relatively cool aquifers with temperatures about equal to the measured spring temperature, irrespective of much higher calculated Na-K-Ca temperatures.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78986","issn":"0094-9140","usgsCitation":"Fournier, R., and Potter, R., 1978, A magnesium correction for the Na-K-Ca chemical geothermometer: U.S. Geological Survey Open-File Report 78-986, 25 p. :ill. ;27 cm., https://doi.org/10.3133/ofr78986.","productDescription":"25 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":155568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0986/report-thumb.jpg"},{"id":52427,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0986/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae21a","contributors":{"authors":[{"text":"Fournier, R.O.","contributorId":73584,"corporation":false,"usgs":true,"family":"Fournier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":189358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Potter, Robert W.","contributorId":27045,"corporation":false,"usgs":true,"family":"Potter","given":"Robert W.","affiliations":[],"preferred":false,"id":189357,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19050,"text":"ofr781105 - 1978 - Geochemical survey of the western energy regions: fifth anual progress report, July 1978","interactions":[],"lastModifiedDate":"2012-02-02T00:07:31","indexId":"ofr781105","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":"78-1105","title":"Geochemical survey of the western energy regions: fifth anual progress report, July 1978","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr781105","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Geochemical survey of the western energy regions: fifth anual progress report, July 1978: U.S. Geological Survey Open-File Report 78-1105, xiv, 194 leaves :ill., maps ;28 cm.; (207 p. - PGS), https://doi.org/10.3133/ofr781105.","productDescription":"xiv, 194 leaves :ill., maps ;28 cm.; (207 p. - PGS)","costCenters":[],"links":[{"id":152007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/1105/report-thumb.jpg"},{"id":48485,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/1105/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6ab943","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":529047,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20271,"text":"ofr78959 - 1978 - Hydrologic information for land-use planning, Fairbanks vicinity, Alaska","interactions":[],"lastModifiedDate":"2021-12-17T22:40:18.314429","indexId":"ofr78959","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":"78-959","title":"Hydrologic information for land-use planning, Fairbanks vicinity, Alaska","docAbstract":"The flood plain on the Chena and Tanana Rivers near Fairbanks, Alaska, has abundant water in rivers and in an unconfined alluvial aquifer. The principal source of ground water is the Tanana River, from which ground water flows northwesterly to the Chena River. Transmissivity of the aquifer commonly exceed 100 ,000 sq ft. The shallow water table (less than 15 ft below land surface), high hydraulic conductivity of the sediments and cold soil give the flood plain a high susceptibility to pollution by onsite sewerage systems. The Environmental Protection Agency recommended maximum concentrations for drinking water may be exceeded in surface water for manganese and bacteria and in ground water for iron, manganese, and bacteria. Residents of the uplands obtain water principally from a widely-distributed fractured schist aquifer. The aquifer is recharged by local infiltration of precipitation and is drained by springs on the lower slopes and by ground-water flow to alluvial aquifers of the valleys. The annual base flow from basins in the uplands ranged from 3,000 to 100,000 gallons per acre; the smallest base flows occur in basins nearest the city of Fairbanks. The thick silt cover and great depth to the water table give much of the uplands a low susceptibility to pollution by onsite sewage disposal. Ground water is locally high in nitrate, arsenic, iron , and manganese. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78959","usgsCitation":"Nelson, G.L., 1978, Hydrologic information for land-use planning, Fairbanks vicinity, Alaska: U.S. Geological Survey Open-File Report 78-959, vi, 47 p., https://doi.org/10.3133/ofr78959.","productDescription":"vi, 47 p.","costCenters":[],"links":[{"id":152287,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":94448,"rank":800,"type":{"id":15,"text":"Index Page"},"url":"https://dggs.alaska.gov/pubs/id/11192"},{"id":393068,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14970.htm"}],"country":"United States","state":"Alaska","city":"Fairbanks","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -148.326416015625,\n              64.73429692356085\n            ],\n            [\n              -147.3211669921875,\n              64.73429692356085\n            ],\n            [\n              -147.3211669921875,\n              65.00026079026213\n            ],\n            [\n              -148.326416015625,\n              65.00026079026213\n            ],\n            [\n              -148.326416015625,\n              64.73429692356085\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606a25","contributors":{"authors":[{"text":"Nelson, Gordon L.","contributorId":55443,"corporation":false,"usgs":true,"family":"Nelson","given":"Gordon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":182362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20220,"text":"ofr78957 - 1978 - Reconnaissance of chemical quality of surface water and fluvial sediment in the Dirty Devil River basin, Utah","interactions":[{"subject":{"id":20220,"text":"ofr78957 - 1978 - Reconnaissance of chemical quality of surface water and fluvial sediment in the Dirty Devil River basin, Utah","indexId":"ofr78957","publicationYear":"1978","noYear":false,"title":"Reconnaissance of chemical quality of surface water and fluvial sediment in the Dirty Devil River basin, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70044040,"text":"70044040 - 1979 - Reconnaissance of chemical quality of surface water and fluvial sediment in the Dirty Devil River basin, Utah","indexId":"70044040","publicationYear":"1979","noYear":false,"title":"Reconnaissance of chemical quality of surface water and fluvial sediment in the Dirty Devil River basin, Utah"},"id":1}],"supersededBy":{"id":70044040,"text":"70044040 - 1979 - Reconnaissance of chemical quality of surface water and fluvial sediment in the Dirty Devil River basin, Utah","indexId":"70044040","publicationYear":"1979","noYear":false,"title":"Reconnaissance of chemical quality of surface water and fluvial sediment in the Dirty Devil River basin, Utah"},"lastModifiedDate":"2013-02-25T17:23:19","indexId":"ofr78957","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":"78-957","title":"Reconnaissance of chemical quality of surface water and fluvial sediment in the Dirty Devil River basin, Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr78957","usgsCitation":"Mundorff, J.C., 1978, Reconnaissance of chemical quality of surface water and fluvial sediment in the Dirty Devil River basin, Utah: U.S. Geological Survey Open-File Report 78-957, 162 p., 3 sheets :ill., maps ;27 cm., https://doi.org/10.3133/ofr78957.","productDescription":"162 p., 3 sheets :ill., maps ;27 cm.","costCenters":[],"links":[{"id":152089,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63e82f","contributors":{"authors":[{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":182270,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23143,"text":"ofr78751 - 1978 - Land use and land cover maps for Palo Alto, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr78751","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":"78-751","title":"Land use and land cover maps for Palo Alto, California","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr78751","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Land use and land cover maps for Palo Alto, California: U.S. Geological Survey Open-File Report 78-751, 1 map., https://doi.org/10.3133/ofr78751.","productDescription":"1 map.","costCenters":[],"links":[{"id":155598,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3bf","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":529119,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23133,"text":"ofr78748 - 1978 - Land use and land cover maps for Ano Nuevo, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:05","indexId":"ofr78748","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":"78-748","title":"Land use and land cover maps for Ano Nuevo, California","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr78748","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Land use and land cover maps for Ano Nuevo, California: U.S. Geological Survey Open-File Report 78-748, 1 map., https://doi.org/10.3133/ofr78748.","productDescription":"1 map.","costCenters":[],"links":[{"id":155708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae495","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":529109,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23142,"text":"ofr78754 - 1978 - Land use and land cover maps for Newark, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr78754","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":"78-754","title":"Land use and land cover maps for Newark, California","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr78754","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Land use and land cover maps for Newark, California: U.S. Geological Survey Open-File Report 78-754, 1 map., https://doi.org/10.3133/ofr78754.","productDescription":"1 map.","costCenters":[],"links":[{"id":155597,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae397","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":529118,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23148,"text":"ofr78749 - 1978 - Land use and land cover maps for San Leandro, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr78749","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":"78-749","title":"Land use and land cover maps for San Leandro, California","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr78749","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Land use and land cover maps for San Leandro, California: U.S. Geological Survey Open-File Report 78-749, 1 map., https://doi.org/10.3133/ofr78749.","productDescription":"1 map.","costCenters":[],"links":[{"id":157076,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae215","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":529124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26517,"text":"wri77127 - 1978 - Low-flow frequency of Georgia streams","interactions":[],"lastModifiedDate":"2019-06-18T15:37:36","indexId":"wri77127","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":"77-127","displayTitle":"Low-Flow Frequency of Georgia Streams","title":"Low-flow frequency of Georgia streams","docAbstract":"<p>This report contains analyses of low-flow data and tabulations of computed low-flow frequency for all stream sites in Georgia where suitable flow records have been collected. These include 134 continuous-record gaging stations and 102 partial-record gaging stations. Frequency records for gaging stations with short records have been adjusted where possible to more closely represent results that would have been obtained from longer records.</p><p>Variations in time and place of low-flow characteristics, per unit of drainage area, are demonstrated. Low flows for 7 consecutive days with a 10-year recurrence interval vary from 0 to more than 1.0 cubic feet per second per square mile [(ft<sup>3</sup>/s)/mi<sup>2</sup>]. In the Blue Ridge province in the northern part of the State, unit low flows range from 0.3 to 0.8 (ft<sup>3</sup>/s)/mi<sup>2</sup>; in the Valley and Ridge province in the northwest they range from 0.05 to 0.04 (ft<sup>3</sup>/s)/mi<sup>2</sup>; and in the Piedmont province they range from 0.1 to 1.1 (ft<sup>3</sup>/s)/mi<sup>2</sup>.</p><p>There is a contrast in unit rates of low flow between the upper zone of the Coastal Plain where most flows are high, and the lower zone where most flows are low. Flows in the upper zone are in the range of 0.1 to 1.1 (ft <sup>3</sup>/s)/mi<sup>2</sup>, but in the lower zone only the largest streams have appreciable flow during low-flow periods. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri77127","usgsCitation":"Carter, R., and Putnam, S., 1978, Low-flow frequency of Georgia streams: U.S. Geological Survey Water-Resources Investigations Report 77-127, xi, 104 p., https://doi.org/10.3133/wri77127.","productDescription":"xi, 104 p.","numberOfPages":"119","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":364428,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0127/report.pdf","text":"Report","size":"1 MB","linkFileType":{"id":1,"text":"pdf"},"description":"WRI 1977-127"},{"id":158438,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0127/report-thumb.jpg"}],"country":"United 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 \"}}]}","contact":"<p><a href=\"mailto:dc_ga@usgs.gov\" data-mce-href=\"mailto:dc_ga@usgs.gov\">Director</a>, <a href=\"https://www.usgs.gov/centers/sa-water\" data-mce-href=\"https://www.usgs.gov/centers/sa-water\">South Atlantic Water Science Center</a><br>U.S. Geological Survey<br>1770 Corporate Dr #500<br>Norcross, GA 30093</p>","tableOfContents":"<ul><li>Abstract</li><li>Introduction</li><li>Data compilation and analysis</li><li>Regional characteristics</li><li>Applications of low-flow frequency data</li><li>Presentation of low-flow characteristics of streams</li><li>Supplementary data</li><li>Selected references</li></ul>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648766","contributors":{"authors":[{"text":"Carter, R.F.","contributorId":101261,"corporation":false,"usgs":true,"family":"Carter","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":196529,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Putnam, S.A.","contributorId":12891,"corporation":false,"usgs":true,"family":"Putnam","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":196528,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24071,"text":"ofr78684 - 1978 - Hydrologic environment of the Silurian salt deposits in parts of Michigan, Ohio, and New York","interactions":[],"lastModifiedDate":"2016-11-07T10:05:18","indexId":"ofr78684","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":"78-684","title":"Hydrologic environment of the Silurian salt deposits in parts of Michigan, Ohio, and New York","docAbstract":"<p>The aggregate thickness of evaporites (salt, gypsum, and anhydrite) in the Silurian Salina sequence in Michigan exceeds 1200 feet in areas near the periphery of the Michigan basin, where the salt beds are less than 3000 feet below land surface. In northeast Ohio the aggregate thickness of salt beds is as much as 200 feet in places, and in western New York it is more than 500 feet, where th beds are less than 3000 feet deep. </p><p>The salt-bearing rocks dip regionally on the order of 50 feet per mile; those in Michigan dip toward the center of the Michigan basin, and those in Ohio and New York, in the Appalachian basin, dip generally southward. The rocks in both basins thicken downdip. Minor folds and faults occur in the salt-bearing rocks in all three states. Some of this defrmation has been attenuated or absorbed bo the salt beds. </p><p>Occuring near the middle of thick sedimentary sequences, the salt beds are bounded aboe and below by beds containing water having dissolved-solids concentrations several times that seawter. The brines occur commonly in discrete zones of high permeability at specific places in the stratigraphic sequence. </p><p>In northeast Ohio two prominent brine zones are recognized by the driller, the Devonian Oriskany Sandstone, or 'first water' zone, above the Salina Formation, and the Newburg or 'second water' zone below the Salina. In each aquifer there is a vertical component of hydraulic head, but little brine probably moves through the salt beds because their permeability is extremely low. Also, ther is little evidence of dissolution of the salt in areas distant from the outcrop, suggesting that if brine does move through the salt, movement is at a slow enough rate so that, in combination with the saturated or near-saturated condition of the water, it precludes significant dissolution. Principal brine movement is probably in the permeable zones in the direction of the hydraulic gradient. </p><p>Two areas in Michigan and one area each in Ohio and New York appear suitable for additional investigation of salt beds for purposes radioactive waste disposal. One of the Michigan areas is in the northern part of the southern peninsula, in Presque Isle and Alpena Counties; the other is in the southern part of the southern peninsula, in Oakland, Macomb, and St. Clair Counties (fig. 3). In northeast Ohio the area that appears to be suitable for investigation includes most of the eastern half of Lake County and extends eastward into Ashtabula County and southward into Geauga County. In western New York conditions may warrant additional investigation in Schuyler, Tompkins, and western Cortland Counties.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Columbus, OH","doi":"10.3133/ofr78684","issn":"0094-9140","usgsCitation":"Norris, S., 1978, Hydrologic environment of the Silurian salt deposits in parts of Michigan, Ohio, and New York: U.S. Geological Survey Open-File Report 78-684, iii, 31 p., https://doi.org/10.3133/ofr78684.","productDescription":"iii, 31 p.","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":157248,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330791,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0684/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606df8","contributors":{"authors":[{"text":"Norris, Stanley E.","contributorId":63844,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley E.","affiliations":[],"preferred":false,"id":191271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26271,"text":"wri7794 - 1978 - Preliminary water-quality characterization of lakes in Washington","interactions":[],"lastModifiedDate":"2018-11-15T12:01:19","indexId":"wri7794","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":"77-94","title":"Preliminary water-quality characterization of lakes in Washington","docAbstract":"<p>This report describes a method for comparing and characterizing lakes in Washington on the basis of water quality. The method can aid in selecting lakes for lake-restoration efforts. To simplify comparisons, a characteristic value (CV) was developed for each of 617 lakes in Washington using principal-component analysis. Three of 14 water-quality properties measured were used in this analysis because the principal component of the three properties accounted for 63 percent of the variance in the correlation matrix. The three properties were Secchi-disc visibility and concentrations of phosphorus and organic nitrogen. The significance of the derived CV's was evaluated by regression of chlorophyll a concentration against CV. The resulting standard error of estimate of +1.8 micrograms per liter of chlorophyll a indicated that the CV can be a useful index in assessing relative water-quality and trophic conditions among lakes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7794","usgsCitation":"Bortleson, G.C., 1978, Preliminary water-quality characterization of lakes in Washington: U.S. Geological Survey Water-Resources Investigations Report 77-94, iii, 31 p., https://doi.org/10.3133/wri7794.","productDescription":"iii, 31 p.","costCenters":[],"links":[{"id":359457,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0094/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0094/report-thumb.jpg"}],"country":"United 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,{"id":23141,"text":"ofr78755 - 1978 - Land use and land cover maps for Mountain View, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr78755","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":"78-755","title":"Land use and land cover maps for Mountain View, California","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr78755","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Land use and land cover maps for Mountain View, California: U.S. Geological Survey Open-File Report 78-755, 1 map., https://doi.org/10.3133/ofr78755.","productDescription":"1 map.","costCenters":[],"links":[{"id":155583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae365","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":529117,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23140,"text":"ofr78739 - 1978 - Land use and land cover maps for Montara Mountain, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr78739","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":"78-739","title":"Land use and land cover maps for Montara Mountain, California","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr78739","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Land use and land cover maps for Montara Mountain, California: U.S. Geological Survey Open-File Report 78-739, 1 map., https://doi.org/10.3133/ofr78739.","productDescription":"1 map.","costCenters":[],"links":[{"id":155582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae319","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":529116,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26058,"text":"wri7853 - 1978 - Bacteriological water quality of Tulpehocken Creek basin, Berks and Lebanon Counties, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-07T08:38:21","indexId":"wri7853","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":"78-53","title":"Bacteriological water quality of Tulpehocken Creek basin, Berks and Lebanon Counties, Pennsylvania","docAbstract":"<p>A four month intensive study of the bacteriological quality of water in the Tulpehocken Creek basin indicates that (1) the streams locally contain high densities of bacteria indicative of fecal contamination, (2) nonpoint waste sources, particularly livestock, are the dominant influence in the excessive bacteriological-indicator counts observed, and (3) retention time of water in the proposed Blue Marsh Lake is believed sufficient to reduce bacteria densities to acceptable levels except following intense rainfall and runoff events during normally low flow periods.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7853","usgsCitation":"Barker, J.L., 1978, Bacteriological water quality of Tulpehocken Creek basin, Berks and Lebanon Counties, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 78-53, iii, 25 p., https://doi.org/10.3133/wri7853.","productDescription":"iii, 25 p.","numberOfPages":"32","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":310276,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0053/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":158073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri7853.jpg"}],"country":"United States","state":"Pennsylvania","county":"Berks County, Lebanon County","otherGeospatial":"Tulpehocken Creek","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-75.89,40.6761],[-75.8005,40.6182],[-75.7796,40.6052],[-75.7701,40.5992],[-75.7677,40.5974],[-75.7498,40.5862],[-75.7402,40.5802],[-75.7188,40.5654],[-75.6956,40.5505],[-75.6849,40.544],[-75.6206,40.5023],[-75.5582,40.4641],[-75.5278,40.4464],[-75.5416,40.4299],[-75.5466,40.4245],[-75.5516,40.4182],[-75.5604,40.4066],[-75.5647,40.4021],[-75.5666,40.4003],[-75.5685,40.3976],[-75.5884,40.3748],[-75.5971,40.364],[-75.6034,40.355],[-75.6046,40.3533],[-75.6084,40.3483],[-75.6164,40.3407],[-75.6233,40.3322],[-75.6258,40.3295],[-75.6389,40.313],[-75.6457,40.3044],[-75.6488,40.3008],[-75.6501,40.299],[-75.66,40.2874],[-75.6644,40.2811],[-75.6681,40.2775],[-75.6744,40.269],[-75.6899,40.2502],[-75.6949,40.2444],[-75.6961,40.2426],[-75.6968,40.2417],[-75.6986,40.2408],[-75.7322,40.2231],[-75.7602,40.2085],[-75.7724,40.2028],[-75.7773,40.1997],[-75.8494,40.154],[-75.8604,40.1464],[-75.8757,40.1371],[-75.9017,40.1546],[-75.9172,40.1644],[-75.9385,40.1782],[-75.97,40.1995],[-75.9997,40.2189],[-76.0092,40.2249],[-76.0175,40.2304],[-76.0454,40.2489],[-76.0562,40.2558],[-76.0675,40.2627],[-76.0782,40.2688],[-76.0841,40.2729],[-76.0889,40.2761],[-76.0919,40.278],[-76.1139,40.2918],[-76.1514,40.3158],[-76.3134,40.2567],[-76.3219,40.2545],[-76.3442,40.252],[-76.3587,40.2503],[-76.3798,40.2473],[-76.4251,40.2414],[-76.4372,40.2387],[-76.4971,40.2188],[-76.4995,40.2179],[-76.5092,40.2153],[-76.5286,40.2091],[-76.5485,40.2029],[-76.5703,40.1963],[-76.5796,40.2213],[-76.5848,40.2345],[-76.6024,40.2781],[-76.6099,40.2981],[-76.614,40.3081],[-76.6263,40.3381],[-76.6404,40.3727],[-76.648,40.3923],[-76.6574,40.4173],[-76.6691,40.4477],[-76.6796,40.4754],[-76.6346,40.5005],[-76.6097,40.5144],[-76.5707,40.535],[-76.5549,40.5435],[-76.5353,40.5552],[-76.5257,40.5487],[-76.4538,40.5042],[-76.4412,40.4973],[-76.4231,40.4967],[-76.3988,40.5028],[-76.34,40.5154],[-76.3176,40.5161],[-76.3091,40.5161],[-76.2915,40.5168],[-76.2601,40.5174],[-76.2395,40.5213],[-76.2316,40.5244],[-76.2163,40.5288],[-76.1902,40.5357],[-76.1817,40.5357],[-76.1739,40.5369],[-76.1678,40.5396],[-76.158,40.5454],[-76.1494,40.5503],[-76.1305,40.556],[-76.122,40.5586],[-76.1135,40.5617],[-76.1019,40.5643],[-76.0929,40.5646],[-76.0825,40.5677],[-76.0764,40.5704],[-76.0696,40.578],[-76.0647,40.5793],[-76.0623,40.5784],[-76.0599,40.5761],[-76.0575,40.5747],[-76.0527,40.5746],[-76.0496,40.5769],[-76.0478,40.5791],[-76.0435,40.5809],[-76.0417,40.5799],[-76.0393,40.5776],[-76.0357,40.5758],[-76.0279,40.5743],[-76.0188,40.5733],[-76.0054,40.609],[-75.9957,40.6375],[-75.9475,40.655],[-75.9395,40.6581],[-75.9078,40.6695],[-75.89,40.6761]]]},\"properties\":{\"name\":\"Berks\",\"state\":\"PA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab16","contributors":{"authors":[{"text":"Barker, James L.","contributorId":53000,"corporation":false,"usgs":true,"family":"Barker","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":195728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23139,"text":"ofr78752 - 1978 - Land use and land cover maps for Mindego Hill, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:06","indexId":"ofr78752","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":"78-752","title":"Land use and land cover maps for Mindego Hill, California","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr78752","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Land use and land cover maps for Mindego Hill, California: U.S. Geological Survey Open-File Report 78-752, 1 map., https://doi.org/10.3133/ofr78752.","productDescription":"1 map.","costCenters":[],"links":[{"id":155581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae465","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":529115,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26284,"text":"wri7799 - 1978 - Water-quality investigation, Upper Santa Clara River Basin, California","interactions":[],"lastModifiedDate":"2019-07-23T11:54:07","indexId":"wri7799","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":"77-99","title":"Water-quality investigation, Upper Santa Clara River Basin, California","docAbstract":"Water-quality data are summarized for the upper Santa Clara River basin, California from studies beginning August 1974 through June 1976 and during past monitoring programs. Data were collected for nitrogen, phosphorus, total organic carbon, trace elements, detergents, and pesticide compounds. Because of the limited number of samples, the data are only an estimate of conditions that existed in the basin. Sampling was designed so that samples from each site would represent seasonal variations in discharge. Most constituents were fairly low in concentration near the headwaters at Ravenna and higher below the urban and agricultural area near Saugus. Mean specific conductance in the river ranged from 745 micromhos per centimeter at 25 deg C below the headwaters near Lang to 2,640 micromhos at the Los Angeles-Ventura County line. Results also indicate that discharge was not the single factor controlling the concentration variance for most constituents. Regression analyses indicated a high correlation between specific conductance and most major inorganic chemical constituents, and between specific conductance and discharge. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7799","usgsCitation":"Bowers, J.C., and Irwin, G.A., 1978, Water-quality investigation, Upper Santa Clara River Basin, California: U.S. Geological Survey Water-Resources Investigations Report 77-99, iv, 43 p., https://doi.org/10.3133/wri7799.","productDescription":"iv, 43 p.","costCenters":[],"links":[{"id":365862,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1977/0099/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1977/0099/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Upper Santa Clara River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e549d","contributors":{"authors":[{"text":"Bowers, James C. jcbowers@usgs.gov","contributorId":4185,"corporation":false,"usgs":true,"family":"Bowers","given":"James","email":"jcbowers@usgs.gov","middleInitial":"C.","affiliations":[],"preferred":true,"id":196112,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Irwin, G. A.","contributorId":35733,"corporation":false,"usgs":true,"family":"Irwin","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":196113,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26270,"text":"wri7864 - 1978 - Preferred and observed conditions for sockeye salmon in Ozette Lake and its tributaries, Clallam County, Washington","interactions":[],"lastModifiedDate":"2019-11-06T12:30:32","indexId":"wri7864","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":"78-64","title":"Preferred and observed conditions for sockeye salmon in Ozette Lake and its tributaries, Clallam County, Washington","docAbstract":"<p>Ozette River and Ozette Lake and its tributaries in Washington have many of the water-quality and stream-hydraulic characteristics that are generally supportive of good sockeye salmon production. Ozette Lake is a large, deep lake and a natural rearing area and for young sockeye. In the summer of 1976 water temperatures preferred for the growth of young sockeye (45-68 degrees Fahrenheit) occurred between about 200 feet of depth and the water surface, or generally in the zone of steep temperature gradient. Dissolved-oxygen concentrations in excess of 8.0 milligrams per liter at all depths throughout the year provided an adequate supply of oxygen for sockeye production. In comparison with eight other sockeye-producing lakes in Washington and Alaska, the concentrations of zooplankton in Ozette Lake appear adequate to support the rearing of sockeye salmon. In Big River and Umbrella Creek, tributaries to Ozette Lake, the streambed areas with gravels suitable for spawning were calculated to be about 39,000 and 31 ,000 square yards, respectively. If those areas were completely utilized they would accommodate about 13,000 and 10,000 spawning sockeye females, respectively. (Woodard-USGS)</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7864","usgsCitation":"Bortleson, G.C., and Dion, N.P., 1978, Preferred and observed conditions for sockeye salmon in Ozette Lake and its tributaries, Clallam County, Washington: U.S. Geological Survey Water-Resources Investigations Report 78-64, viii, 61 p., https://doi.org/10.3133/wri7864.","productDescription":"viii, 61 p.","costCenters":[],"links":[{"id":368977,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1978/0064/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157746,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0064/report-thumb.jpg"}],"country":"United States","state":"Washington","county":"Clallam 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Gilbert C.","contributorId":57472,"corporation":false,"usgs":true,"family":"Bortleson","given":"Gilbert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":196094,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dion, N. P.","contributorId":33302,"corporation":false,"usgs":true,"family":"Dion","given":"N.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":196093,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25495,"text":"wri7832 - 1978 - An evaluation of problems arising from acid mine drainage in the vicinity of Shasta Lake, Shasta County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"wri7832","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":"78-32","title":"An evaluation of problems arising from acid mine drainage in the vicinity of Shasta Lake, Shasta County, California","docAbstract":"Streams draining the mined areas of massive sulfide ore deposits in the Shasta Mining Districts of northern California are generally acidic and contain large concentrations of dissolved metals, including iron, copper, and zinc. The streams, including Flat, Little Backbone, Spring, West Squaw, Horse, and Zinc Creeks, discharge into Shasta Reservoir and the Sacramento River and have caused numerous fish kills. The sources of pollution are discharge from underground mines, streams that flow into open pits, and streams that flow through pyritic mine dumps where the oxidation of pyrite and other sulfide minerals results in the production of acid and the mobilization of metals. Suggested methods of treatment include the use of air and hydraulic seals in the mines, lime neutralization of mine effluent, channeling of runoff and mine effluent away from mine and tailing areas, and the grading and sealing of mine dumps. A comprehensive preabatement and postabatement program is recommended to evaluate the effects of any treatment method used. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri7832","usgsCitation":"Fuller, R.H., Shay, J.M., Ferreira, R.F., and Hoffman, R., 1978, An evaluation of problems arising from acid mine drainage in the vicinity of Shasta Lake, Shasta County, California: U.S. Geological Survey Water-Resources Investigations Report 78-32, iv, 39 p. :ill., maps ;27 cm., https://doi.org/10.3133/wri7832.","productDescription":"iv, 39 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":156920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68495d","contributors":{"authors":[{"text":"Fuller, Richard H.","contributorId":66236,"corporation":false,"usgs":true,"family":"Fuller","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":193927,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shay, J. M.","contributorId":98321,"corporation":false,"usgs":true,"family":"Shay","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193929,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ferreira, R. F.","contributorId":80690,"corporation":false,"usgs":true,"family":"Ferreira","given":"R.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":193928,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hoffman, R.J.","contributorId":38582,"corporation":false,"usgs":true,"family":"Hoffman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":193926,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":25396,"text":"wri78144 - 1978 - Annual summary of ground-water conditions in Arizona, spring 1977 to spring 1978","interactions":[],"lastModifiedDate":"2019-08-05T10:40:39","indexId":"wri78144","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":"78-144","title":"Annual summary of ground-water conditions in Arizona, spring 1977 to spring 1978","docAbstract":"The withdrawal of ground water was about 5.5 million acre-feet in Arizona in 1977. About 4.7 million acre-feet of ground water was used for the irrigation of crops in 1977. The Salt River Valley and the lower Santa Cruz basin are the largest agricultural areas in the State. For 1973-77, ground-water withdrawal in the two areas was about 8.1 and 5.1 million acre-feet, respectively, and, in general, water levels are declining. Other areas in which ground-water withdrawals have caused water-level declines are the Willcox, San Simon, upper Santa Cruz, Avra Valley, Gila Bend, Harquahala Plains, and McMullen Valley areas. Two small-scale maps of Arizona show (1) pumpage of ground water by areas and (2) the status of the ground-water inventory in the State. The main map, scale 1:500 ,000, shows potential well production, depth to water in selected wells in spring 1978, and change in water level in selected wells from 1973 to 1978. The brief text that accompanies the maps summarizes the current ground-water conditions in the State. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri78144","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Annual summary of ground-water conditions in Arizona, spring 1977 to spring 1978: U.S. Geological Survey Water-Resources Investigations Report 78-144, 2 Plates: 24.89 x 38.32 inches and 24.68 x 37.95 inches, https://doi.org/10.3133/wri78144.","productDescription":"2 Plates: 24.89 x 38.32 inches and 24.68 x 37.95 inches","costCenters":[],"links":[{"id":366202,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0144/plate2-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":366203,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0144/plate1-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":157535,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0144/report-thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.2578125,\n              31.27855085894653\n            ],\n            [\n              -108.8525390625,\n              31.27855085894653\n            ],\n            [\n              -108.8525390625,\n              36.98500309285596\n            ],\n            [\n              -114.2578125,\n              36.98500309285596\n            ],\n            [\n              -114.2578125,\n              31.27855085894653\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b857","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":529218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25121,"text":"cir776A - 1978 - Climate variation and its effects on our land and water : Part A, Earth science in climate research","interactions":[],"lastModifiedDate":"2018-10-23T18:10:03","indexId":"cir776A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"776","chapter":"A","title":"Climate variation and its effects on our land and water : Part A, Earth science in climate research","docAbstract":"To better coordinate information being generated by the U.S. Geological Survey, a workshop was convened near Denver, Colo., on December 7-9, 1976, to exchange ideas about research that is oriented toward climate, climate variation, and the effects of climate on the Nation 's land and water resources. This is the first circular of a three-part report resulting from that workshop. Hydrologic records provide information to the earth scientist about the responses of ground water, surface water, and glaciers to climatic change; geologic sequences provide evidence of earth-surface water, and glaciers to climatic change; geologic sequences provide evidence of earth-surface responses to climatic change; biological records yield information about the effects of climatic change on the Earth 's biota; archeological records tell us where and how man was able to live under changing climatic conditions; and historical records allow the specific effects of short-term changes in climate to be accurately documented. The interrelation between present and past geologic environments, various methods of study , and the span of time over which the results can be applied are shown in a table. (Woodard-USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, Geological Survey ;distributed by Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir776A","usgsCitation":"1978, Climate variation and its effects on our land and water : Part A, Earth science in climate research: U.S. Geological Survey Circular 776, 3 v. :ill., maps ;26 cm. --, https://doi.org/10.3133/cir776A.","productDescription":"3 v. :ill., maps ;26 cm. --","costCenters":[],"links":[{"id":54101,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0776a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0776a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de1f9","contributors":{"editors":[{"text":"Smith, George I.","contributorId":57096,"corporation":false,"usgs":true,"family":"Smith","given":"George I.","affiliations":[],"preferred":false,"id":749540,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":23135,"text":"ofr78747 - 1978 - Land use and land cover maps for Franklin Point, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:05","indexId":"ofr78747","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":"78-747","title":"Land use and land cover maps for Franklin Point, California","language":"ENGLISH","publisher":"The Survey,","doi":"10.3133/ofr78747","issn":"0094-9140","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1978, Land use and land cover maps for Franklin Point, California: U.S. Geological Survey Open-File Report 78-747, 1 map., https://doi.org/10.3133/ofr78747.","productDescription":"1 map.","costCenters":[],"links":[{"id":155710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae484","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":529111,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25122,"text":"cir776B - 1978 - Climate variation and its effects on our land and water : Part B, Current research by the Geological Survey","interactions":[],"lastModifiedDate":"2018-10-23T18:09:14","indexId":"cir776B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1978","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":"776","chapter":"B","title":"Climate variation and its effects on our land and water : Part B, Current research by the Geological Survey","docAbstract":"To better coordinate information being generated by the U.S. Geological Survey, a workshop was convened near Denver, Colo., on December 7-9, 1976, to exchange ideas about research that is oriented toward climate, climate variation, and the effects of climate on the Nation 's land and water resources. This is the first circular of a three-part report resulting from that workshop. Hydrologic records provide information to the earth scientist about the responses of ground water, surface water, and glaciers to climatic change; geologic sequences provide evidence of earth-surface water, and glaciers to climatic change; geologic sequences provide evidence of earth-surface responses to climatic change; biological records yield information about the effects of climatic change on the Earth 's biota; archeological records tell us where and how man was able to live under changing climatic conditions; and historical records allow the specific effects of short-term changes in climate to be accurately documented. The interrelation between present and past geologic environments, various methods of study , and the span of time over which the results can be applied are shown in a table. (Woodard-USGS)","language":"ENGLISH","publisher":"Dept. of the Interior, Geological Survey ;distributed by Branch of Distribution, U.S. Geological Survey,","doi":"10.3133/cir776B","usgsCitation":"1978, Climate variation and its effects on our land and water : Part B, Current research by the Geological Survey: U.S. Geological Survey Circular 776, 3 v. :ill., maps ;26 cm. --, https://doi.org/10.3133/cir776B.","productDescription":"3 v. :ill., maps ;26 cm. --","costCenters":[],"links":[{"id":54102,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1978/0776b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123897,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1978/0776b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de1d4","contributors":{"editors":[{"text":"Smith, George I.","contributorId":57096,"corporation":false,"usgs":true,"family":"Smith","given":"George I.","affiliations":[],"preferred":false,"id":749539,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}}
,{"id":26280,"text":"wri7898 - 1978 - The Tuscaloosa Aquifer system in Mississippi","interactions":[],"lastModifiedDate":"2019-07-23T15:28:47","indexId":"wri7898","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":"78-98","title":"The Tuscaloosa Aquifer system in Mississippi","docAbstract":"A three-sheet map report describes the Tuscaloosa aquifer system in Mississippi. The Tuscaloosa aquifer system, of Cretaceous age , is in the interconnected irregular sand and gravel beds in the Coker and Gordo Formations. The aquifer contains freshwater in an area of about 9,000 sq mi in northeastern Mississippi. Water produced from the aquifer by about 90 water systems and numerous industries in 1975 averaged about 47 Mgal/d. Regional water level declines have averaged less than two feet per year and the aquifer has a large potential for future development. The aquifer is used in some areas where the dissolved-solids concentration is more than 500 mg/L and where wells exceed 2,000 ft in depth. The most common problems in water supplies are excessive chloride and iron. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7898","usgsCitation":"Boswell, E.H., 1978, The Tuscaloosa Aquifer system in Mississippi: U.S. Geological Survey Water-Resources Investigations Report 78-98, 3 Plates: 41.89 x 32.41 inches or smaller, https://doi.org/10.3133/wri7898.","productDescription":"3 Plates: 41.89 x 32.41 inches or smaller","costCenters":[],"links":[{"id":158221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1978/0098/report-thumb.jpg"},{"id":365891,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0098/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365892,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0098/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365893,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1978/0098/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":" "}],"country":"United States","state":"Mississippi","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db6735df","contributors":{"authors":[{"text":"Boswell, E. H.","contributorId":38954,"corporation":false,"usgs":true,"family":"Boswell","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":196108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}