{"pageNumber":"6216","pageRowStart":"155375","pageSize":"25","recordCount":184934,"records":[{"id":56412,"text":"wdrCA7212 - 1973 - Water resources data for California, 1972; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2012-06-13T01:01:47","indexId":"wdrCA7212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-72-1-2","title":"Water resources data for California, 1972; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley","docAbstract":"Surface-water records for the 1972 water year for California, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report, Records for a few pertinent gaging stations in bordering States also are included, The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of R. Stanley Lord and Lee R. Peterson, successive district chiefs. These data represent that portion of the National Water Data System collected by the Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA7212","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for California, 1972; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-72-1-2, 549 p., https://doi.org/10.3133/wdrCA7212.","productDescription":"549 p.","costCenters":[],"links":[{"id":181337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_72_1_2.jpg"},{"id":257430,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1972/ca-72/WDR-1972-vol2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Northern Great Basin;Central Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f774a","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":532593,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":56414,"text":"wdrCA722 - 1973 - Water resources data for California, 1972; Part 2: Water quality records","interactions":[],"lastModifiedDate":"2012-06-13T01:01:47","indexId":"wdrCA722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-72-2","title":"Water resources data for California, 1972; Part 2: Water quality records","docAbstract":"Water-resources data for the 1972 water year for California include records of data for the chemical and physical characteristics of surface and ground water. The distribution, type, and number of stations in each river or drainage basin are shown in figure 1. A few pertinent stations in bordering States are also included. The records were compiled by the Water Resources Division of the U.S. Geological Survey under the direction of R. Stanley Lord and Lee R. Peterson, successive district chiefs. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA722","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for California, 1972; Part 2: Water quality records: U.S. Geological Survey Water Data Report CA-72-2, 586 p., https://doi.org/10.3133/wdrCA722.","productDescription":"586 p.","costCenters":[],"links":[{"id":181431,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_72_2.jpg"},{"id":257431,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1972/ca-72/WDR-1972-wq.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7710","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":532595,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60682,"text":"mf532 - 1973 - Bottom features and processes related to drifting ice on the Arctic shelf, Alaska","interactions":[],"lastModifiedDate":"2023-04-05T18:43:11.86545","indexId":"mf532","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"532","title":"Bottom features and processes related to drifting ice on the Arctic shelf, Alaska","docAbstract":"

Early investigations of artic shelf regions led to the hypothesis that certain micro-relief forms are related to the action of grounded ice (for example, Rex, 1955). Since the introduction of side-scan sonar as a tool for ocean-floor surveys, a number of workers have described the occurrence of linear bottom features produced by grounded ice. Such features have been found on modern polar shelves (Skinner, 1971; Pelletier and Shearer, 1972; Kovacs, 1972; Reimnitz and Barnes, 1972; Brooks, 1973), and as relict features (Berkson and Clay, 1973; Belderson and Wilson, 1973; Belderson and others, 1973). Studies of core samples, high resolution seismic profiles, and diving observations indicate that the sediments of the Beaufort Sea Shelf are highly distorted by the action of grounding ice, and that the recurrence rate of gouging is very high. It has also become evident that grounding ice is contributing considerably to the sediment transport processes of modern Arctic shelves.

Sediments from similar environments exposed on the continents today should also contain the record of ice gouging and related processes. Thus it has become apparent that drifting ice is an important agent influencing the sedimentary structures and the sediment transport regime of Arctic shelves today and has been in the past. The diagrams presented here, with supporting evidence in the form of side-scan sonar records, and ice and bottom photos, demonstrate the most prevalent processes and types of bottom features observed on the continental shelf off northern Alaska. As the map shows, most of the shelf is affected by these processes today.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf532","usgsCitation":"Reimnitz, E., Barnes, P.W., and Alpha, T.R., 1973, Bottom features and processes related to drifting ice on the Arctic shelf, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 532, 1 Plate: 35.81 x 23.02 inches, https://doi.org/10.3133/mf532.","productDescription":"1 Plate: 35.81 x 23.02 inches","costCenters":[],"links":[{"id":415275,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0532/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182923,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0532/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -155,70 ], [ -155,71.5 ], [ -148,71.5 ], [ -148,70 ], [ -155,70 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db60290b","contributors":{"authors":[{"text":"Reimnitz, Erk","contributorId":17963,"corporation":false,"usgs":true,"family":"Reimnitz","given":"Erk","email":"","affiliations":[],"preferred":false,"id":264210,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barnes, Peter W.","contributorId":6042,"corporation":false,"usgs":true,"family":"Barnes","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":264209,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Alpha, Tau Rho","contributorId":63371,"corporation":false,"usgs":true,"family":"Alpha","given":"Tau","email":"","middleInitial":"Rho","affiliations":[],"preferred":false,"id":264211,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":5747,"text":"pp803 - 1973 - X-ray mineralogy of the Parachute Creek Member, Green River Formation, in the northern Piceance Creek basin, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:54","indexId":"pp803","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"803","title":"X-ray mineralogy of the Parachute Creek Member, Green River Formation, in the northern Piceance Creek basin, Colorado","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp803","usgsCitation":"Brobst, D.A., and Tucker, J.D., 1973, X-ray mineralogy of the Parachute Creek Member, Green River Formation, in the northern Piceance Creek basin, Colorado: U.S. Geological Survey Professional Paper 803, 53 p., https://doi.org/10.3133/pp803.","productDescription":"53 p.","costCenters":[],"links":[{"id":118062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0803/report-thumb.jpg"},{"id":32325,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0803/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de643","contributors":{"authors":[{"text":"Brobst, Donald Albert","contributorId":36117,"corporation":false,"usgs":true,"family":"Brobst","given":"Donald","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":151514,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tucker, Jerry D.","contributorId":38984,"corporation":false,"usgs":true,"family":"Tucker","given":"Jerry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":151515,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":40881,"text":"ofr73170 - 1973 - Preliminary geologic map of the Calf Creek Quadrangle, Campbell County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"ofr73170","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-170","title":"Preliminary geologic map of the Calf Creek Quadrangle, Campbell County, Wyoming","language":"ENGLISH","doi":"10.3133/ofr73170","usgsCitation":"McKay, E.J., and Mapel, W.J., 1973, Preliminary geologic map of the Calf Creek Quadrangle, Campbell County, Wyoming: U.S. Geological Survey Open-File Report 73-170, 1 map :photocopy ;58 x 42 cm. +coal sections (1 sheet : photocopy ; x cm.), https://doi.org/10.3133/ofr73170.","productDescription":"1 map :photocopy ;58 x 42 cm. +coal sections (1 sheet : photocopy ; x cm.)","costCenters":[],"links":[{"id":106551,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8767.htm","linkFileType":{"id":5,"text":"html"},"description":"8767"},{"id":173589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98337,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0170/plate-1.pdf","size":"4461","linkFileType":{"id":1,"text":"pdf"}},{"id":98338,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0170/plate-2.pdf","size":"4178","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bc47","contributors":{"authors":[{"text":"McKay, E. J.","contributorId":57040,"corporation":false,"usgs":true,"family":"McKay","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":224108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mapel, W. J.","contributorId":92225,"corporation":false,"usgs":true,"family":"Mapel","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":224109,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":56436,"text":"wdrAZ722 - 1973 - Water resources data for Arizona, water year 1972","interactions":[],"lastModifiedDate":"2012-02-02T00:12:20","indexId":"wdrAZ722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AZ-72-2","title":"Water resources data for Arizona, water year 1972","language":"ENGLISH","doi":"10.3133/wdrAZ722","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for Arizona, water year 1972: U.S. Geological Survey Water Data Report AZ-72-2, 166 p., https://doi.org/10.3133/wdrAZ722.","productDescription":"166 p.","costCenters":[],"links":[{"id":184718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7843","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":532617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63919,"text":"gp869 - 1973 - Aeromagnetic map of the Hamburg quadrangle, New London and Middlesex Counties, Connecticut","interactions":[],"lastModifiedDate":"2022-08-16T18:53:09.831402","indexId":"gp869","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"869","title":"Aeromagnetic map of the Hamburg quadrangle, New London and Middlesex Counties, Connecticut","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp869","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Aeromagnetic map of the Hamburg quadrangle, New London and Middlesex Counties, Connecticut: U.S. Geological Survey Geophysical Investigations Map 869, Report: 1 p.; 1 Plate: 20.04 × 30.36 inches, https://doi.org/10.3133/gp869.","productDescription":"Report: 1 p.; 1 Plate: 20.04 × 30.36 inches","costCenters":[],"links":[{"id":250246,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0869/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250245,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0869/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0869/report-thumb.jpg"},{"id":405209,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6222.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Connecticut","county":"Middlesex County, New London County","otherGeospatial":"Hamburg quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -72.375,\n 41.375\n ],\n [\n -72.25,\n 41.375\n ],\n [\n -72.25,\n 41.5\n ],\n [\n -72.375,\n 41.5\n ],\n [\n -72.375,\n 41.375\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69612b","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":533388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3105,"text":"wsp2094 - 1973 - Quality of surface waters of the United States, 1968, Parts 4 and 5, St. Lawrence River basin and Hudson Bay and upper Mississippi River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp2094","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2094","title":"Quality of surface waters of the United States, 1968, Parts 4 and 5, St. Lawrence River basin and Hudson Bay and upper Mississippi River basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2094","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Quality of surface waters of the United States, 1968, Parts 4 and 5, St. Lawrence River basin and Hudson Bay and upper Mississippi River basins: U.S. Geological Survey Water Supply Paper 2094, x, 293 p. ; 23 cm., https://doi.org/10.3133/wsp2094.","productDescription":"x, 293 p. ; 23 cm.","costCenters":[],"links":[{"id":139347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2094/report-thumb.jpg"},{"id":30017,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2094/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db65193d","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":528082,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23751,"text":"ofr741064 - 1973 - Preliminary investigation of land subsidence in the Sacramento Valley, California","interactions":[],"lastModifiedDate":"2025-07-25T17:07:11.89918","indexId":"ofr741064","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"74-1064","title":"Preliminary investigation of land subsidence in the Sacramento Valley, California","docAbstract":"Although a number of agencies have made leveling surveys in Sacramento Valley and a valleywide network of first- and second-order control exists, few areas have sufficient control for determining whether land subsidence has occurred and if so, how much, within the time span of vertical control. Available data suggest that 0.2 to 0.9 foot (0.06 to 0.3 m) of subsidence probably has occurred from 1935-42 to 1964 in an extensive agricultural area of heavy ground-water pumping between Zamora and Davis, and that as much as 2 feet (0.6 m) of subsidence has occurred in at least two areas of pumping overdraft--east of Zamora, and west of Arbuckle. \r\n\r\nA comparison of maps showing long-term water-level decline and average annual ground-water pumpage indicates several other areas of probable subsidence. In six general areas--northwest of Sacramento; northeast of Sacramento; southeast of Yuba City; 10 miles (16 km) north of Willows; 20 miles (32 km) north of Willows; and especially in the Arbuckle area,ground-water declines have quite probably produced significant subsidence. In two areas of most intensive pumping, no long-term water-level declines have occurred, and no subsidence is indicated.\r\n\r\nIf problems of land subsidence are of concern in Sacramento Valley, and if estimates of historic subsidence or subsidence potential are needed, serious consideration should be given to a field program of basic-data collection. Second-order leveling along a few carefully selected lines of existing control, and the installation and operation of two or three compaction recorders in areas of continuing water-level decline, would provide helpful data for estimating .past and future subsidence.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741064","issn":"0094-9140","usgsCitation":"Lofgren, B.E., and Ireland, R.L., 1973, Preliminary investigation of land subsidence in the Sacramento Valley, California: U.S. Geological Survey Open-File Report 74-1064, Report: 32 p.; 4 Figures: 17.20 x 22.10 inches or smaller, https://doi.org/10.3133/ofr741064.","productDescription":"Report: 32 p.; 4 Figures: 17.20 x 22.10 inches or smaller","costCenters":[],"links":[{"id":492916,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1974/1064/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":492915,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1974/1064/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":492914,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1974/1064/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":492913,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1974/1064/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":52984,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/1064/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391027,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52091.htm"},{"id":156134,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/1064/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sacramento Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.5,\n 38.5\n ],\n [\n -121.1667,\n 38.5\n ],\n [\n -121.1667,\n 40.5833\n ],\n [\n -122.5,\n 40.5833\n ],\n [\n -122.5,\n 38.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669e77","contributors":{"authors":[{"text":"Lofgren, B. E.","contributorId":42579,"corporation":false,"usgs":true,"family":"Lofgren","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":190653,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ireland, R. 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No abstract available.

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Water is defined in terms of its chemical composition and dominant physical properties, such as expansion on freezing and high surface tension. Water on the earth is about 97 percent in the seas, 2 percent in glacier ice, principally Greenland and Antarctica. Man is left with less than 1 percent as liquid fresh water to sustain his needs. This is possible under good management because water moves cyclically. Conjunctive use of surface and ground water is advocated, as is reuse of wastewater. Water needs for domestic and light industrial use can be reasonably forecast for planning purposes. Heavy-industry needs must be determined on a site-by-site basis.

\n

The units commonly used by hydrologists with respect to quantities and quality of water are denned; their significance in water management is outlined, and metric-english equivalents are given for many. A glossary of terms concludes the report which is intended as a reference work for use by planners and managers.

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Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-6","title":"Geology and quality of water in the Modesto-Merced area, San Joaquin Valley, California, with a brief section on hydrology","docAbstract":"

The Modesto-Merced area includes about 1,800 square miles on the northeast side of the San Joaquin Valley. The physiographic units in the area are (1) Sierra Nevada, (2) dissected uplands, (3) low alluvial plains and fans, (4) river flood plains and channels, and (5) overflow lands.

Geologic units consist of consolidated rocks and unconsolidated deposits. The dominant structure of the geologic units is that of a homocline, which reflects the southwestward-tilted fault block of the Sierra Nevada. The consolidated rocks include: (1) basement complex (pre-Tertiary), (2) marine sandstone and shale (Cretaceous), (3) Ione Formation and other sedimentary rocks (Eocene), (4) Valley Springs Formation (late? Miocene), and (5) the Mehrten Formation (Miocene and Pliocene). In the eastern part of the area, the consolidated rocks generally yield small quantities of water to wells except for the Mehrten Formation which is an important aquifer.

The unconsolidated deposits include: (1) continental deposits (Pliocene and Pleistocene?), (2) lacustrine and marsh deposits (Pleistocene), (3) older alluvium (Pleistocene and Holocene?), (4) younger alluvium (Holocene), and (5) flood-basin deposits (Holocene). The continental deposits and older alluvium are the main water-yielding units in the unconsolidated deposits. The lacustrine and marsh deposits (E-clay) and the flood-basin deposits yield little water to wells, and the younger alluvium in most places probably yields only moderate quantities of water to wells.

There are three ground-water bodies in the Modesto-Merced area: (1) the unconfined water body, (2) the confined water body, and (3) the water body in consolidated rocks. The unconfined water body occurs in the unconsolidated deposits above and east of the E-clay, except in the western and southern parts of the area where clay lenses occur and semiconfined conditions exist. The confined water body occurs in the unconsolidated deposits below the E-clay and extends downward to the base of fresh water. The water body in consolidated rocks occurs under both perched and confined conditions.

Ground-water movement in the unconfined and the confined water bodies is generally westward toward the valley trough. In the unconfined water body, the water also moves toward the major rivers, and toward pumping depressions at Modesto and near El Nido. Because of the higher head in the unconfined water body, water slowly moves from it through the E-clay to the underlying confined water body.

Surface water is used extensively for irrigation in most of the study area; consequently, shallow water in the unconfined water body has to be controlled by pumping. Nevertheless, water levels near Modesto declined about 6 feet between 1958 and 1962, for the most part during the dry years 1959-61. Near El Nido, water levels declined about 70 feet between 1942 and 1967. In the confined water body, water levels were high in the winter and spring and low in the summer and fall, reflecting irrigation practices. In the southwestern part of the area, water levels in the confined water body declined about 14 feet from 1962 to 1968 and rose slightly after 1968, whereas in the northwestern part water levels remained fairly constant.

Water from the upper reaches of the Stanislaus, Tuolumne, Merced, and Chowchilla Rivers is calcium bicarbonate in chemical type and is of excellent quality. As those rivers cross the valley floor, their water quality is generally degraded by return flows from irrigated land, and in the Tuolumne River by saline water discharged from abandoned gas wells. Average dissolvedsolids content in the major rivers, as indicated by chemical analyses, do not exceed 400 mg/1 (milligrams per liter) except in the San Joaquin River where average dissolved-solids content has not exceeded 1,050 mg/l.

Water from minor streams in the area is bicarbonate in chemical type with dissolved-solids content ranging from 56 mg/1 to about 350 mg/l.

Although chloride-type fresh ground water occurs in the unconfined and confined water bodies and in the water body in consolidated rocks, most of the fresh ground water is a bicarbonate type that has a dissolved-solids content of less than 500 mg/l.

Water having dissolved solids in excess of about 2,000 mg/1 is considered to be saline. Saline water extends below the base of fresh water to the basement complex and, except in the extreme eastern part, underlies most of the study area. Saline water also occurs as lenses above the base of fresh water in the unconfined and confined water bodies.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri736","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Page, R.W., and Balding, G.O., 1973, Geology and quality of water in the Modesto-Merced area, San Joaquin Valley, California, with a brief section on hydrology: U.S. Geological Survey Water-Resources Investigations Report 73-6, v, 85 p., https://doi.org/10.3133/wri736.","productDescription":"v, 85 p.","costCenters":[],"links":[{"id":367180,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0006/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0006/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -121.5,\n 37\n ],\n [\n -120,\n 37\n ],\n [\n -120,\n 38\n ],\n [\n -121.5,\n 38\n ],\n [\n -121.5,\n 37\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6842bf","contributors":{"authors":[{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balding, Gary O.","contributorId":25210,"corporation":false,"usgs":true,"family":"Balding","given":"Gary","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":200747,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61690,"text":"gq1092 - 1973 - Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming","interactions":[{"subject":{"id":40824,"text":"ofr71250 - 1971 - Preliminary geologic map of the Clause Peak Quadrangle, Lincoln, Sublette, and Teton counties, Wyoming","indexId":"ofr71250","publicationYear":"1971","noYear":false,"title":"Preliminary geologic map of the Clause Peak Quadrangle, Lincoln, Sublette, and Teton counties, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":61690,"text":"gq1092 - 1973 - Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming","indexId":"gq1092","publicationYear":"1973","noYear":false,"title":"Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming"},"id":1}],"lastModifiedDate":"2022-09-29T19:32:43.982602","indexId":"gq1092","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1092","title":"Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq1092","usgsCitation":"Schroeder, M.L., 1973, Geologic map of the Clause Peak quadrangle, Lincoln, Sublette and Teton Counties, Wyoming: U.S. Geological Survey Geologic Quadrangle 1092, Report: 1 p.; 1 Plate: 33.57 x 32.58 inches, https://doi.org/10.3133/gq1092.","productDescription":"Report: 1 p.; 1 Plate: 33.57 x 32.58 inches","costCenters":[],"links":[{"id":107533,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10636.htm","linkFileType":{"id":5,"text":"html"},"description":"10636"},{"id":252569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1092/report-thumb.jpg"},{"id":247992,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1092/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Wyoming","county":"Lincoln County, Sublette County, Teton County","otherGeospatial":"Clause Peak quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -110.625,\n 43.125\n ],\n [\n -110.5,\n 43.125\n ],\n [\n -110.5,\n 43.25\n ],\n [\n -110.625,\n 43.25\n ],\n [\n -110.625,\n 43.125\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69cad8","contributors":{"authors":[{"text":"Schroeder, Marvin L.","contributorId":91104,"corporation":false,"usgs":true,"family":"Schroeder","given":"Marvin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":266240,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61827,"text":"gq1123 - 1973 - Geologic map of parts of the Vevay South and Vevay North quadrangles, north-central Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:35","indexId":"gq1123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1123","title":"Geologic map of parts of the Vevay South and Vevay North quadrangles, north-central Kentucky","language":"ENGLISH","doi":"10.3133/gq1123","usgsCitation":"Swadley, W.C., 1973, Geologic map of parts of the Vevay South and Vevay North quadrangles, north-central Kentucky: U.S. Geological Survey Geologic Quadrangle 1123, 1 map., https://doi.org/10.3133/gq1123.","productDescription":"1 map.","costCenters":[],"links":[{"id":107559,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10664.htm","linkFileType":{"id":5,"text":"html"},"description":"10664"},{"id":248118,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1123/report.pdf","size":"39","linkFileType":{"id":1,"text":"pdf"}},{"id":252861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1123/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.11749999999999,38.6175 ], [ -85.11749999999999,38.75 ], [ -85,38.75 ], [ -85,38.6175 ], [ -85.11749999999999,38.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a26b0","contributors":{"authors":[{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":266418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66194,"text":"i739 - 1973 - Geologic map of the Langrenus Quadrangle of the Moon","interactions":[],"lastModifiedDate":"2023-05-02T15:53:25.384589","indexId":"i739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"739","subseriesTitle":"MOON","title":"Geologic map of the Langrenus Quadrangle of the Moon","docAbstract":"

The Langrenus quadrangle is on the east limb of the lunar nearside, at the southeast margin of Mare Fecunditatis. The crater Langrenus, about 140 km in diameter, is the most prominent feature. Rugged terra materials, scattered by craters of various sizes and ages, occupy much of the east half of the map area, and smooth mare materials in the Fecunditatis basin dominate the west. Mare Spumans and other irregular maria in the northeast are part of a belt of such maria concentric with Mare Crisium, which is centered approximately 500 km north of the quadrangle.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i739","usgsCitation":"Hodges, C.A., 1973, Geologic map of the Langrenus Quadrangle of the Moon: U.S. Geological Survey IMAP 739, 1 map, https://doi.org/10.3133/i739.","productDescription":"1 map","costCenters":[],"links":[{"id":486690,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P1N2AWTQ","text":"USGS data release","linkHelpText":"Interactive Map: IMAP 739 - Geologic map of the Langrenus Quadrangle of the Moon"},{"id":439037,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P95VQQCK","text":"USGS data release","linkHelpText":"Geologic map of the Langrenus Quadrangle of the Moon"},{"id":187667,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101326,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0739/plate-1.pdf","size":"10959","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db697057","contributors":{"authors":[{"text":"Hodges, C. A.","contributorId":104495,"corporation":false,"usgs":true,"family":"Hodges","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":274139,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61825,"text":"gq1095 - 1973 - Geologic map of the Sanders quadrangle, north-central Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:35","indexId":"gq1095","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1095","title":"Geologic map of the Sanders quadrangle, north-central Kentucky","language":"ENGLISH","doi":"10.3133/gq1095","usgsCitation":"Swadley, W.C., 1973, Geologic map of the Sanders quadrangle, north-central Kentucky: U.S. Geological Survey Geologic Quadrangle 1095, 1 map., https://doi.org/10.3133/gq1095.","productDescription":"1 map.","costCenters":[],"links":[{"id":107535,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10639.htm","linkFileType":{"id":5,"text":"html"},"description":"10639"},{"id":248116,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1095/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":252859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1095/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85,38.6175 ], [ -85,38.75 ], [ -84.86749999999999,38.75 ], [ -84.86749999999999,38.6175 ], [ -85,38.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c020","contributors":{"authors":[{"text":"Swadley, W. C.","contributorId":46940,"corporation":false,"usgs":true,"family":"Swadley","given":"W.","middleInitial":"C.","affiliations":[],"preferred":false,"id":266416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41689,"text":"ofr73293 - 1973 - Aeromagnetic map of parts of the Kalispell and Cutbank 1° by 2° quadrangles, Montana","interactions":[],"lastModifiedDate":"2025-08-01T13:19:18.034921","indexId":"ofr73293","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-293","title":"Aeromagnetic map of parts of the Kalispell and Cutbank 1° by 2° quadrangles, Montana","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73293","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Aeromagnetic map of parts of the Kalispell and Cutbank 1° by 2° quadrangles, Montana: U.S. Geological Survey Open-File Report 73-293, 1 Plate: 37.32 × 24.92 inches, https://doi.org/10.3133/ofr73293.","productDescription":"1 Plate: 37.32 × 24.92 inches","costCenters":[],"links":[{"id":79410,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0293/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":400355,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8804.htm","linkFileType":{"id":5,"text":"html"}},{"id":173675,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","country":"United States","state":"Montana","otherGeospatial":"Kalispell and Cutbank 1° by 2° quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115,\n 48\n ],\n [\n -112.25,\n 48\n ],\n [\n -112.25,\n 49\n ],\n [\n -115,\n 49\n ],\n [\n -115,\n 48\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69764c","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":530569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":28913,"text":"wri7317 - 1973 - Availability of water from limestone and dolomite aquifers in southwest Ohio and the relation of water quality to the regional flow system","interactions":[],"lastModifiedDate":"2016-11-07T10:24:55","indexId":"wri7317","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-17","title":"Availability of water from limestone and dolomite aquifers in southwest Ohio and the relation of water quality to the regional flow system","docAbstract":"

The largest ground-water supplies from the 150 to 450-foot thick carbonate-rock aquifer in southwest Ohio are available in a 2,800 squaremile area on the crest and eastern flank of the Cincinnati arch. Well production in the high-yield area is mainly from the Newburg zone, a permeable stratum in the lower part of the Bass Island group. A ' structure contour map on the top of the Lockport Dolomite shows that the Newburg zone conforms to the configuration of the Cincinnati arch. The chemical quality of the water in the consolidated-rock aquifers is intimately related to the regional flow system, and undergoes a progressive change from a calcium bicarbonate-type in recharge areas to a calcium sulfate-type in areas of natural discharge.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Columbus, OH","doi":"10.3133/wri7317","usgsCitation":"Norris, S.E., and Fidler, R.E., 1973, Availability of water from limestone and dolomite aquifers in southwest Ohio and the relation of water quality to the regional flow system: U.S. Geological Survey Water-Resources Investigations Report 73-17, iv, 42 p., https://doi.org/10.3133/wri7317.","productDescription":"iv, 42 p.","numberOfPages":"49","costCenters":[{"id":513,"text":"Ohio Water Science Center","active":true,"usgs":true}],"links":[{"id":159123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330803,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0017/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Ohio","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.8089599609375,\n 40.730608477796636\n ],\n [\n -82.8094482421875,\n 40.70979201243495\n ],\n [\n -82.7215576171875,\n 38.556757147352215\n ],\n [\n -82.8424072265625,\n 38.58252615935333\n ],\n [\n -82.869873046875,\n 38.67264490154078\n ],\n [\n -82.869873046875,\n 38.7283759182398\n ],\n [\n -82.9083251953125,\n 38.758366935612784\n ],\n [\n -82.99072265625,\n 38.732661120482334\n ],\n [\n -83.0731201171875,\n 38.69408504756833\n ],\n [\n -83.133544921875,\n 38.646908247760706\n ],\n [\n -83.199462890625,\n 38.61687046392973\n ],\n [\n -83.29833984375,\n 38.59540719940386\n ],\n [\n -83.34228515625,\n 38.634036452919226\n ],\n [\n -83.4576416015625,\n 38.66406704456943\n ],\n [\n -83.5784912109375,\n 38.69408504756833\n ],\n [\n -83.638916015625,\n 38.655488159953\n ],\n [\n -83.64990234375,\n 38.62974534092597\n ],\n [\n -83.7322998046875,\n 38.64261790634527\n ],\n [\n -83.7762451171875,\n 38.655488159953\n ],\n [\n -83.84765625,\n 38.71551876930462\n ],\n [\n -83.935546875,\n 38.77549900381297\n ],\n [\n -84.0728759765625,\n 38.77121637244273\n ],\n [\n -84.1552734375,\n 38.788345355085625\n ],\n [\n -84.2156982421875,\n 38.80975079723835\n ],\n [\n -84.2376708984375,\n 38.86109762182888\n ],\n [\n -84.2706298828125,\n 38.94232097947902\n ],\n [\n -84.320068359375,\n 39.01491572891582\n ],\n [\n -84.39147949218749,\n 39.04051963289309\n ],\n [\n -84.473876953125,\n 39.027718840211605\n ],\n [\n -84.605712890625,\n 39.036252959636606\n ],\n [\n -84.6441650390625,\n 39.0831721934762\n ],\n [\n -84.70184326171875,\n 39.115144700901475\n ],\n [\n -84.72930908203125,\n 39.142842478062505\n ],\n [\n -84.7650146484375,\n 39.144972625112224\n ],\n [\n -84.7869873046875,\n 39.11727568585598\n ],\n [\n -84.81994628906249,\n 39.11088253765179\n ],\n [\n -84.8089599609375,\n 40.730608477796636\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d626","contributors":{"authors":[{"text":"Norris, Stanley Eugene","contributorId":24772,"corporation":false,"usgs":true,"family":"Norris","given":"Stanley","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":200609,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fidler, Richard E.","contributorId":86313,"corporation":false,"usgs":true,"family":"Fidler","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":200610,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ]}