{"pageNumber":"5913","pageRowStart":"147800","pageSize":"25","recordCount":165658,"records":[{"id":32779,"text":"pp440W - 1966 - Chemistry of the iron-rich sedimentary rocks","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"pp440W","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"440","chapter":"W","title":"Chemistry of the iron-rich sedimentary rocks","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Data of geochemistry","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp440W","usgsCitation":"James, H.L., 1966, Chemistry of the iron-rich sedimentary rocks: U.S. Geological Survey Professional Paper 440, p. W1-W61, https://doi.org/10.3133/pp440W.","productDescription":"p. W1-W61","costCenters":[],"links":[{"id":119280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0440w/report-thumb.jpg"},{"id":60722,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0440w/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e31f9","contributors":{"authors":[{"text":"James, H. L.","contributorId":96732,"corporation":false,"usgs":true,"family":"James","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":209143,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2306,"text":"wsp1822 - 1966 - Selected techniques in water resources investigations, 1965","interactions":[],"lastModifiedDate":"2017-09-06T15:33:12","indexId":"wsp1822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1822","title":"Selected techniques in water resources investigations, 1965","docAbstract":"<p>Increasing world activity in water-resources development has created an interest in techniques for conducting investigations in the field. In the United States, the Geological Survey has the responsibility for extensive and intensive hydrologic studies, and the Survey places considerable emphasis on discovering better ways to carry out its responsibility. For many years, the dominant interest in field techniques has been \"in house,\" but the emerging world interest has led to a need for published accounts of this progress. In 1963 the Geological Survey published \"Selected Techniques in Water Resources Investigations\" (Water-Supply Paper 1669-Z) as part of the series \"Contributions to the Hydrology of the United States.\"</p><p>The report was so favorably received that successive volumes are planned, of which this is the first. The present report contains 25 papers that represent new ideas being tested or applied in the hydrologic field program of the Geological Survey. These ideas range from a proposed system for monitoring fluvial sediment to how to construct stream-gaging wells from steel oil drums. The original papers have been revised and edited by the compilers, but the ideas presented are those of the authors. The general description of the bubble gage on page 2 has been given by the compilers as supplementary information.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1822","usgsCitation":"1966, Selected techniques in water resources investigations, 1965: U.S. Geological Survey Water Supply Paper 1822, iii, 117 p., https://doi.org/10.3133/wsp1822.","productDescription":"iii, 117 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":137715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1822/report-thumb.jpg"},{"id":28129,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1822/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f830d","contributors":{"compilers":[{"text":"Mesnier, Glennon N.","contributorId":67488,"corporation":false,"usgs":true,"family":"Mesnier","given":"Glennon","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":709724,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Chase, Edith B.","contributorId":11192,"corporation":false,"usgs":true,"family":"Chase","given":"Edith","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":709725,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}}
,{"id":2007,"text":"wsp1869B - 1966 - Effect of vertical motion on current meters","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1869B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1869","chapter":"B","title":"Effect of vertical motion on current meters","docAbstract":"The effect of vertical motion on the performance of current meters at various stream velocities was evaluated to determine whether accurate discharge measurements can be made from a bobbing boat. \r\n\r\nThree types of current meters--Ott, Price, and vane types--were tested under conditions simulating a bobbing boat. A known frequency and amplitude of vertical motion were imparted to the current meter, and the related effect on the measured stream velocity was determined. One test of the Price meter was made under actual conditions, using a boat and standard measuring gear. The results of the test under actual conditions verified those obtained by simulating the vertical movements of a boat. \r\n\r\nThe tests show that for stream velocities below 2.5 feet per second the accuracy of all three meters is significantly affected when the meters are subjected to certain conditions of vertical motion that can occur during actual field operations. Both the rate of vertical motion and the frequency of vertical oscillation affect the registration of the meter. \r\n\r\nThe results of these tests, presented in the form of graphs and tables, can be used as a guide to determine whether wind and stream flow are within an acceptable range for a reliable discharge measurement from a boat.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1869B","usgsCitation":"Kallio, N.A., 1966, Effect of vertical motion on current meters: U.S. Geological Survey Water Supply Paper 1869, iv, 20 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1869B.","productDescription":"iv, 20 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138395,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1869b/report-thumb.jpg"},{"id":27452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1869b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625434","contributors":{"authors":[{"text":"Kallio, Nicholas A.","contributorId":15992,"corporation":false,"usgs":true,"family":"Kallio","given":"Nicholas","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2313,"text":"wsp1819A - 1966 - Utilization of ground water in the Santa Maria Valley area, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1819A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1819","chapter":"A","title":"Utilization of ground water in the Santa Maria Valley area, California","docAbstract":"Overdraft in the Santa Maria Valley ground-water basin since about 1946 has resulted in a significant decline in water levels throughout the basin as ground water has been removed from storage. In 1959 approximately 2,200,000 acre-feet of ground water was in storage above sea level in the ground-water reservoir. Estimates of storage depletion are not consistent with estimates of groundwater recharge and discharge. The natural perennial yield of the basin probably is about 50.000 acre-feet, on the basis of estimated recharge and natural discharge. The augmented perennial yield probably is about 70,000 acre-feet and includes 21,200 acre-feet of water per year released at Twitchell Dam. Storage depletion, not estimated in the seaward ends of the aquifers, will result as the fresh watersea water interface moves landward in response to the continuing decrease in hydraulic gradient in the aquifer system. \r\n\r\nEvidence of sea-water intrusion into the basin has not been observed, but limited sea-water encroachment may have occurred at the offshore ends of the aquifers. Additional observation wells will be necessary to provide supplemental data to insure that hydraulic heads and gradients in the deeper aquifers are properly monitored.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1819A","usgsCitation":"Miller, G., and Evenson, R.E., 1966, Utilization of ground water in the Santa Maria Valley area, California: U.S. Geological Survey Water Supply Paper 1819, iii, 24 p. :ill. ;24 cm. + plate folded in pocket., https://doi.org/10.3133/wsp1819A.","productDescription":"iii, 24 p. :ill. ;24 cm. + plate folded in pocket.","costCenters":[],"links":[{"id":137738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819a/report-thumb.jpg"},{"id":28143,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28144,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602d5e","contributors":{"authors":[{"text":"Miller, G.A.","contributorId":107671,"corporation":false,"usgs":true,"family":"Miller","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":144995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144994,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2261,"text":"wsp1805 - 1966 - Ground water in Huerfano County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1805","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1805","title":"Ground water in Huerfano County, Colorado","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1805","usgsCitation":"McLaughlin, T.G., 1966, Ground water in Huerfano County, Colorado: U.S. Geological Survey Water Supply Paper 1805, v, 91 p. :illus., maps (8 fold. (3 col.)) ;24 cm., https://doi.org/10.3133/wsp1805.","productDescription":"v, 91 p. :illus., maps (8 fold. (3 col.)) ;24 cm.","costCenters":[],"links":[{"id":137571,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1805/report-thumb.jpg"},{"id":247196,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-1_sheet_1.pdf","size":"11698","linkFileType":{"id":1,"text":"pdf"}},{"id":247197,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-1_sheet_2.pdf","size":"10035","linkFileType":{"id":1,"text":"pdf"}},{"id":28046,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28047,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28048,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28049,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28050,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28051,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1805/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28052,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1805/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db6e","contributors":{"authors":[{"text":"McLaughlin, Thad Gerald","contributorId":48941,"corporation":false,"usgs":true,"family":"McLaughlin","given":"Thad","email":"","middleInitial":"Gerald","affiliations":[],"preferred":false,"id":144913,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2192,"text":"wsp1823 - 1966 - Sedimentation and chemical quality of surface water in the Heart River drainage basin, North Dakota","interactions":[],"lastModifiedDate":"2018-03-12T15:33:39","indexId":"wsp1823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1823","title":"Sedimentation and chemical quality of surface water in the Heart River drainage basin, North Dakota","docAbstract":"<p>The Heart River drainage basin of southwestern North Dakota comprises an area of 3,365 square miles and lies within the Missouri Plateau of the Great Plains province. Streamflow of the Heart River and its tributaries during 1949-58 was directly proportional to .the drainage area. After the construction of Heart Butte Dam in 1949 and Dickinson Dam in 1950, the mean annual streamflow near Mandan was decreased an estimated 10 percent by irrigation, evaporation from the two reservoirs, and municipal use. </p><p>Processes that contribute sediment to the Heart River are mass wasting, advancement of valley heads, and sheet, lateral stream, and gully erosion. In general, glacial deposits, terraces, and bars of Quaternary age are sources of sand and larger sediment, and the rocks of Tertiary age are sources of clay, silt. and sand. The average annual suspended-sediment discharges near Mandan were estimated to be 1,300,000 tons for 1945-49 and 710,000 tons for 1970-58. </p><p>The percentage composition of ions in water of the Heart River, based on average concentrations in equivalents per million for selected ranges of streamflow, changes with flow and from station to station. During extremely low flows the water contains a large percentage of sodium and about equal percentages of bicarbonate and .sulfate, and during extremely high flows the water contains a large percentage of calcium plus magnesium and bicarbonate. The concentrations, in parts per million, of most of the ions vary inversely with flow. </p><p>The water in the reservoirs--Edward Arthur Patterson Lake and Lake Tschida--during normal or above-normal runoff is of suitable quality for public use. Generally, because of medium or high salinity hazards, the successful long-term use of Heart River water for irrigation will depend on a moderate amount of leaching, adequate drainage, ,and the growing of crops that have moderate or good salt tolerance.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1823","usgsCitation":"Maderak, M.L., 1966, Sedimentation and chemical quality of surface water in the Heart River drainage basin, North Dakota: U.S. Geological Survey Water Supply Paper 1823, Report: v, 42 p.; Plate: 18.48 x 12.99 inches, https://doi.org/10.3133/wsp1823.","productDescription":"Report: v, 42 p.; Plate: 18.48 x 12.99 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":247119,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1823/plate-1.pdf","size":"1078","linkFileType":{"id":1,"text":"pdf"}},{"id":138275,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1823/report-thumb.jpg"},{"id":27833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1823/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbcd0","contributors":{"authors":[{"text":"Maderak, Marion L.","contributorId":103248,"corporation":false,"usgs":true,"family":"Maderak","given":"Marion","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":185,"text":"wsp1645 - 1966 - Quality of surface waters of the United States, 1959, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1645","title":"Quality of surface waters of the United States, 1959, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1645","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Quality of surface waters of the United States, 1959, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1645, xv, 524 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1645.","productDescription":"xv, 524 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136329,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1645/report-thumb.jpg"},{"id":24796,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1645/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651aeb","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":527220,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2070,"text":"wsp1817A - 1966 - Organic acids in naturally colored surface waters","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1817A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1817","chapter":"A","title":"Organic acids in naturally colored surface waters","docAbstract":"Most of the organic matter in naturally colored surface waters consists of a mixture of carboxylic acids or salts of these acids. Many of the acids color the water yellow to brown; however, not all of the acids are colored. These acids range from simple to complex, but predominantly they are nonvolatile polymeric carboxylic acids. \r\n\r\nThe organic acids were recovered from the water by two techniques: continuous liquid-liquid extraction with n-butanol and vacuum evaporation at 50?C (centigrade). The isolated acids were studied by techniques of gas, paper, and column chromatography and infrared spectroscopy. \r\n\r\nAbout 10 percent of the acids recovered were volatile or could be made volatile for gas chromatographic analysis. Approximately 30 of these carboxylic acids were isolated, and 13 of them were individually identified. The predominant part of the total acids could not be made volatile for gas chromatographic analysis. Infrared examination of many column chromatographic fractions indicated that these nonvolatile substances are primarily polymeric hydroxy carboxylic acids having aromatic and olefinic unsaturation. The evidence suggests that some of these acids result from polymerization in aqueous solution. Elemental analysis of the sodium fusion products disclosed the absence of nitrogen, sulfur, and halogens.","language":"ENGLISH","publisher":"U.S. G.P.O,","doi":"10.3133/wsp1817A","usgsCitation":"Lamar, W.L., and Goerlitz, D., 1966, Organic acids in naturally colored surface waters: U.S. Geological Survey Water Supply Paper 1817, iii, 17 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1817A.","productDescription":"iii, 17 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":138439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1817a/report-thumb.jpg"},{"id":27623,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1817a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cde4b07f02db544b7a","contributors":{"authors":[{"text":"Lamar, William L.","contributorId":15592,"corporation":false,"usgs":true,"family":"Lamar","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144634,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":144633,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22476,"text":"ofr666 - 1966 - Extent and frequency of inundation of flood plain in vicinity of Princeton, New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:08:08","indexId":"ofr666","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-6","title":"Extent and frequency of inundation of flood plain in vicinity of Princeton, New Jersey","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr666","issn":"0094-9140","usgsCitation":"Bettendorf, J., 1966, Extent and frequency of inundation of flood plain in vicinity of Princeton, New Jersey: U.S. Geological Survey Open-File Report 66-6, 36 p. ill., map ;28 cm., https://doi.org/10.3133/ofr666.","productDescription":"36 p. ill., map ;28 cm.","costCenters":[],"links":[{"id":156447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a06e4b07f02db5f8b7d","contributors":{"authors":[{"text":"Bettendorf, J.A.","contributorId":9686,"corporation":false,"usgs":true,"family":"Bettendorf","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":188323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2175,"text":"wsp1807 - 1966 - Ground-water resources of Sheridan County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1807","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1807","title":"Ground-water resources of Sheridan County, Wyoming","docAbstract":"Sheridan County is in the north-central part of Wyoming and is an area of about 2,500 square miles. The western part of the county is in the Bighorn Mountains, and the eastern part is in the Powder River structural basin. Principal streams are the Powder and Tongue Rivers, which are part of the Yellowstone River system. The climate is semiarid, and the mean annual precipitation at Sheridan is about 16 inches. \r\n\r\nRocks of Precambrian age are exposed in the central part of the Bighorn Mountains, and successively younger rocks are exposed eastward. Rocks of Tertiary age, which are the most widespread, are exposed throughout a large part of the Powder River structural basin. Deposits of Quaternary age underlie the flood plains and terraces along the larger streams, particularly in the western part of the basin. \r\n\r\nAquifers of pre-Tertiary age are exposed in the western part of the county, but they dip steeply and are deeply buried just a few miles east of their outcrop. Aquifers that might yield large supplies of water include the Bighorn Dolomite, Madison Limestone, Amsden Formation, and Tensleep Sandstone. The Flathead Sandstone, Sundance Formation, Morrison Formation, Cloverly Formation,. Newcastle Sandstone, Frontier Formation, Parkman Sandstone, Bearpaw Shale, .and Lance Formation may yield small or, under favorable conditions, moderate supplies of water. \r\n\r\nFew wells tap aquifers of pre-Tertiary age, and these are restricted to the outcrop area. The meager data available indicate that the water from the Lance Formation, Bearpaw Shale, Parkman Sandstone, Tensleep Sandstone and Amsden Formation, and Flathead Standstone is of suitable quality for domestic or stock purposes, and that water from the Tensleep Sandstone and Amsden Formation and the Flathead Sandstone is of good quality for irrigation. Samples could not be obtained from other aquifers of pre-Tertiary age; so the quality of water in these aquifers could not be determined. \r\n\r\nAdequate supplies of ground water for stock or domestic use can be developed throughout much of the report area from the Fort Union and Wasatch Formations of Tertiary age; larger supplies might be obtained from the coarse-grained sandstone facies of the Wasatch Formation near Moncreiffe Ridge. Four aquifer tests were made at wells tapping formations of Tertiary age, and the coefficients of permeability determined ranged from 2.5 to 7.9 gallons per day per square foot. The depths to which wells must be drilled to penetrate an aquifer differ within relatively short distances because of the lenticularity of the aquifers. Water in aquifers of Tertiary age may occur under water-table, artesian, or a combination of artesian and gas-lift conditions. \r\n\r\nWater from the Fort Union is usable for domestic purposes, but the iron and dissolved-solids content impair the quality at some localities. Water from the Fort Union Formation is not recommended for irrigation because of sodium and bicarbonate content. The water is regarded as good to fair for stock use. Water from the Wasatch Formation generally contains dissolved solids in excess of the suggested domestic standards, but this water is usable in the absence of other supplies. The development of irrigation supplies from the Wasatch Formation may be possible in some areas, but the water quality should be carefully checked. Water of good to very poor quality for stock supplies is obtained, depending upon the location. Hydrogen sulfide, commonly present in water of the Fort Union and Wasatch Formations, becomes an objectionable characteristic when the water is used for human consumption. \r\n\r\nDeposits of Quaternary age generally yield small to moderate supplies of water to wells. Two pumping tests were conducted, and the coefficients of permeability of the aquifers tested were 380 and 1,100 gallons per day per square foot. Usable supplies of ground water can be developed from the deposits of Quaternary age, principally along the valleys of perennial strea","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1807","usgsCitation":"Lowry, M.E., and Cummings, T.R., 1966, Ground-water resources of Sheridan County, Wyoming: U.S. Geological Survey Water Supply Paper 1807, iv, 77 p. :illus., maps (1 fold. col. in pocket) ;24 cm., https://doi.org/10.3133/wsp1807.","productDescription":"iv, 77 p. :illus., maps (1 fold. col. in pocket) ;24 cm.","costCenters":[],"links":[{"id":138198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1807/report-thumb.jpg"},{"id":27788,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1807/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1807/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d694","contributors":{"authors":[{"text":"Lowry, Marlin E.","contributorId":52552,"corporation":false,"usgs":true,"family":"Lowry","given":"Marlin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144773,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. Ray","contributorId":20722,"corporation":false,"usgs":true,"family":"Cummings","given":"T.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":144772,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52525,"text":"ofr667 - 1966 - A progress report on the test-well drilling program in the west part of Antelope Valley, California","interactions":[],"lastModifiedDate":"2018-01-04T11:37:27","indexId":"ofr667","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-7","title":"A progress report on the test-well drilling program in the west part of Antelope Valley, California","docAbstract":"<p>This progress report presents the results of a test-well drilling program undertaken by the Antelope Valley-East Kern Water Agency and the U.S. Geological Survey in the western part of Antelope Valley, Calif. </p><p>Eight test wells were drilled by the rotary method, and electric and lithologic logs were made of each well. </p><p>A water-level-contour map was drawn, based on water-level measurements in the test wells and other wells. On the basis of data from these wells, the Neenach and Randsburg-Mojave faults were located. The concealed trace of another fault, north of the Randsburg-Mojave fault, was postulated from water-level data. </p><p>This progress report considers the feasibility of utilizing a part of the Antelope Valley ground-water basin as a natural water-storage reservoir. The West Antelope ground-water subunit could probably be used as a large-volume holdover storage reservoir. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr667","collaboration":"Prepared in cooperation with the Antelope Valley-East Kern Water Agency","usgsCitation":"Bloyd, R., 1966, A progress report on the test-well drilling program in the west part of Antelope Valley, California: U.S. Geological Survey Open-File Report 66-7, Report: 20 p.; 1 Plate: 44.12 x 34.54 inches, https://doi.org/10.3133/ofr667.","productDescription":"Report: 20 p.; 1 Plate: 44.12 x 34.54 inches","costCenters":[],"links":[{"id":177834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0007/report-thumb.jpg"},{"id":86946,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0007/plate-1.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":350296,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0007/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Antelope Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.8,\n              34.6\n            ],\n            [\n              -118.2,\n              34.6\n            ],\n            [\n              -118.2,\n              35\n            ],\n            [\n              -118.8,\n              35\n            ],\n            [\n              -118.8,\n              34.6\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d02","contributors":{"authors":[{"text":"Bloyd, R. M. Jr.","contributorId":73243,"corporation":false,"usgs":true,"family":"Bloyd","given":"R. M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":245496,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2190,"text":"wsp1809U - 1966 - Reconnaissance of the geology and ground-water resources in the Aurora area, St. Louis county, Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T09:59:15","indexId":"wsp1809U","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1809","chapter":"U","title":"Reconnaissance of the geology and ground-water resources in the Aurora area, St. Louis county, Minnesota","docAbstract":"<p>The Aurora area is a glaciated upland of drift-mantled slopes, channels, swamps, and glacial-lake plains. It covers about 24 square miles of the eastern part of the Mesabi Iron Range in northeastern Minnesota. A deep narrow channel along the Embarrass River, the principal outlet of a former large glacial lake north of the Embarrass Mountains, lies partly within the area.</p>\n<p>The deposits in the report area consist of bedrock and unconsolidated glacial drift. The 'bedrock belongs to the Animikie Group of late Preeambrian age and consists of taconite (an iron-rich silicate rock) in the northern part and slightly metamorphosed argillite in the middle and southern parts. Bedrock is exposed only in the open-pit iron mines. Large quantities of ground water are pumped from porous and permeable ore zones in the St. James Mine. Small quantities of ground water are obtainable from openings along bedding planes and fractures in the argillite. Unconsolidated deposits consisting of till and water-laid glacial and alluvial materials mantle the bedrock to depths ranging from about 20 feet in the north-central part of the Aurora area to more than 300 feet near the Embarrass River. Thick deposits of sand and gravel in the Embarrass channel are capable of yielding large quantites of water. At places along the Partridge River glaeiofluvial deposits (glacial sediments deposited in running water) could yield moderate to large quantities of water. Sandy to bouldery till yields small quantities of water to domestic wells.</p>\n<p>Well yields in the Aurora area range from less than 5 gpm (gallons per minute) to about 250 gpm from a well tapping an ore body. The specific capacity of wells penetrating ore zones ranges from about 7 gpm per foot of drawdown to 25 gpm per foot of drawdown. Although no attempt has been made to develop a high-yield well in the sand and gravel deposits of the Embarrass channel, more than 5,000 gpm is pumped from sumps which collect water from these deposits in the Embarrass mine. Most domestic wells yield about 5 gpm and are drilled and finished in sand or gravel in either the bouldery till or glaciofluvial deposits.</p>\n<p>Ground water from the unconsolidated deposits is hard and commonly contains large, undesirable amounts of iron and manganese. Water from the 'bedrock aquifers contains less iron and manganese than does water from the unconsolidated deposits.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1809U","collaboration":"Prepared in cooperation with the Department of Iron Range Resources and Rehabilitaion","usgsCitation":"Maclay, R.W., 1966, Reconnaissance of the geology and ground-water resources in the Aurora area, St. Louis county, Minnesota: U.S. Geological Survey Water Supply Paper 1809, Document: 20 p.; Plate: 24.0 x 19.5 inches, https://doi.org/10.3133/wsp1809U.","productDescription":"Document: 20 p.; Plate: 24.0 x 19.5 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":138265,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809u/report-thumb.jpg"},{"id":27830,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809u/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27831,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809u/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","county":"St. Louis County","city":"Aurora","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -92.308333,\n              47.545833\n            ],\n            [\n              -92.308333,\n              47.483333\n            ],\n            [\n              -92.166667,\n              47.483333\n            ],\n            [\n              -92.166667,\n              47.545833\n            ],\n            [\n              -92.308333,\n              47.545833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a64e4b07f02db637b63","contributors":{"authors":[{"text":"Maclay, Robert W.","contributorId":13210,"corporation":false,"usgs":true,"family":"Maclay","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144798,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":191,"text":"wsp1950 - 1966 - Quality of surface waters of the United States, 1963, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1950","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"1950","title":"Quality of surface waters of the United States, 1963, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1950","usgsCitation":"Love, S.K., 1966, Quality of surface waters of the United States, 1963, Parts 7 and 8, lower Mississippi River basin and western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1950, xii, 635 p. ;23 cm., https://doi.org/10.3133/wsp1950.","productDescription":"xii, 635 p. ;23 cm.","costCenters":[],"links":[{"id":136096,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1950/report-thumb.jpg"},{"id":24802,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1950/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651a8a","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64173,"text":"gp553 - 1966 - Aeromagnetic map of parts of the Lambertville, Lumberville, and Stockton quadrangles, New Jersey and Pennsylvania","interactions":[],"lastModifiedDate":"2025-04-29T19:20:36.628353","indexId":"gp553","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"553","title":"Aeromagnetic map of parts of the Lambertville, Lumberville, and Stockton quadrangles, New Jersey and Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp553","usgsCitation":"Boynton, G.R., Pittillo, D., and Zandle, G.L., 1966, Aeromagnetic map of parts of the Lambertville, Lumberville, and Stockton quadrangles, New Jersey and Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 553, 1 Plate: 31.73 x 42.40 inches, https://doi.org/10.3133/gp553.","productDescription":"1 Plate: 31.73 x 42.40 inches","costCenters":[],"links":[{"id":485167,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3508.htm","linkFileType":{"id":5,"text":"html"}},{"id":254140,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0553/report-thumb.jpg"},{"id":250682,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0553/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250681,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0553/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"New Jersey, Pennsylvania","otherGeospatial":"Lambertville, Lumberville, and Stockton quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.08333,\n              40.5\n            ],\n            [\n              -75.08333,\n              40.25\n            ],\n            [\n              -74.875,\n              40.25\n            ],\n            [\n              -74.875,\n              40.5\n            ],\n            [\n              -75.08333,\n              40.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697549","contributors":{"authors":[{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pittillo, D.R.","contributorId":91179,"corporation":false,"usgs":true,"family":"Pittillo","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":270120,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270118,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43716,"text":"ofr6633 - 1966 - Geologic maps of Tierra Redonda Mountain and Bradley quadrangles, Monterey and San Luis Obispo Counties, California","interactions":[{"subject":{"id":43716,"text":"ofr6633 - 1966 - Geologic maps of Tierra Redonda Mountain and Bradley quadrangles, Monterey and San Luis Obispo Counties, California","indexId":"ofr6633","publicationYear":"1966","noYear":false,"title":"Geologic maps of Tierra Redonda Mountain and Bradley quadrangles, Monterey and San Luis Obispo Counties, California"},"predicate":"SUPERSEDED_BY","object":{"id":34277,"text":"b1255 - 1968 - Geology of the Tierra Redonda Mountain and Bradley quadrangles, Monterey and San Luis Obispo Counties, California","indexId":"b1255","publicationYear":"1968","noYear":false,"title":"Geology of the Tierra Redonda Mountain and Bradley quadrangles, Monterey and San Luis Obispo Counties, California"},"id":1}],"supersededBy":{"id":34277,"text":"b1255 - 1968 - Geology of the Tierra Redonda Mountain and Bradley quadrangles, Monterey and San Luis Obispo Counties, California","indexId":"b1255","publicationYear":"1968","noYear":false,"title":"Geology of the Tierra Redonda Mountain and Bradley quadrangles, Monterey and San Luis Obispo Counties, California"},"lastModifiedDate":"2012-02-02T00:04:57","indexId":"ofr6633","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"66-33","title":"Geologic maps of Tierra Redonda Mountain and Bradley quadrangles, Monterey and San Luis Obispo Counties, California","language":"ENGLISH","doi":"10.3133/ofr6633","usgsCitation":"Durham, D., 1966, Geologic maps of Tierra Redonda Mountain and Bradley quadrangles, Monterey and San Luis Obispo Counties, California: U.S. Geological Survey Open-File Report 66-33, 2 maps, https://doi.org/10.3133/ofr6633.","productDescription":"2 maps","costCenters":[],"links":[{"id":106375,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8135.htm","linkFileType":{"id":5,"text":"html"},"description":"8135"},{"id":134804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68860f","contributors":{"authors":[{"text":"Durham, David L.","contributorId":61417,"corporation":false,"usgs":true,"family":"Durham","given":"David L.","affiliations":[],"preferred":false,"id":228600,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62663,"text":"gq550 - 1966 - Geologic map of the Albany quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2012-02-10T00:11:01","indexId":"gq550","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","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":"550","title":"Geologic map of the Albany quadrangle, Kentucky-Tennessee","language":"ENGLISH","doi":"10.3133/gq550","usgsCitation":"Lewis, R., and Thaden, R.E., 1966, Geologic map of the Albany quadrangle, Kentucky-Tennessee: U.S. Geological Survey Geologic Quadrangle 550, 1 map :col. ;77 x 92 cm., https://doi.org/10.3133/gq550.","productDescription":"1 map :col. ;77 x 92 cm.","costCenters":[],"links":[{"id":103278,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1864.htm","linkFileType":{"id":5,"text":"html"},"description":"1864"},{"id":248821,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0550/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":254214,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0550/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.25,36.6175 ], [ -85.25,36.75 ], [ -85.11749999999999,36.75 ], [ -85.11749999999999,36.6175 ], [ -85.25,36.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2591","contributors":{"authors":[{"text":"Lewis, Richard Quintin","contributorId":91097,"corporation":false,"usgs":true,"family":"Lewis","given":"Richard Quintin","affiliations":[],"preferred":false,"id":267690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thaden, Robert E.","contributorId":75502,"corporation":false,"usgs":true,"family":"Thaden","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":267689,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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