{"pageNumber":"5574","pageRowStart":"139325","pageSize":"25","recordCount":165626,"records":[{"id":70156917,"text":"70156917 - 1973 - Hydraulic tests in hole UAe-2, Amchitka Island, Alaska","interactions":[],"lastModifiedDate":"2019-11-12T16:14:59","indexId":"70156917","displayToPublicDate":"2015-09-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Hydraulic tests in hole UAe-2, Amchitka Island, Alaska","docAbstract":"<p>Inflatable straddle packers were used to isolate and test 19 intervals ranging from 56 to 747 meters (183 to 2,450 feet) each in hole UAe-2, Amchitka Island, Alaska. Packer seats were poor in part of the hole because of unstable wall conditions. Thus, some zones had to be tested several times. </p><p>The static water levels in the intervals tested ranged from 14.2 meters (46.6 feet) below land surface in the upper interval to 33.7 meters (110.6 feet) below land surface in one of the intervals near a depth of 1,500 meters (4,900 feet). </p><p>The specific capacity of the open hole from 83.5 to 1,980.6 meters (274 to 6,498 feet) was 3.26 cubic meters per day per meter (0.182 gallon per minute per foot) of drawdown after the hole had been jetted at an average rate of 763 cubic meters per day (140 gallons per minute) for about 41 hours. Transmissivity computed from the recovery of water level after jetting stopped was 2.97 cubic meters per day per meter (239.2 gallons per day per foot). </p><p>The relative specific capacities of isolated intervals ranged from 0.001 cubic meter per day per meter (less than 0.001 gallon per minute per foot) of drawdown to 2.765 cubic meters per day per meter (0.155 gallon per minute per foot) of drawdown.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70156917","usgsCitation":"Ballance, W.C., 1973, Hydraulic tests in hole UAe-2, Amchitka Island, Alaska, iii, 34 p., https://doi.org/10.3133/70156917.","productDescription":"iii, 34 p.","numberOfPages":"40","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308061,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70156917.PNG"},{"id":308542,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156917/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              178.584136963,\n              51.63677159243599\n            ],\n            [\n              178.592376709,\n              51.61290019118336\n            ],\n            [\n              179.21585083,\n              51.3254629443313\n            ],\n            [\n             179.508361816,\n              51.37520943448463\n            ],\n            [\n              179.057922363,\n              51.587309751245456\n            ],\n            [\n              178.628082275,\n              51.67936786087718\n            ],\n            [\n              178.584136963,\n              51.63677159243599\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f2a9b4e4b0dacf699ec6b5","contributors":{"authors":[{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571143,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5224973,"text":"5224973 - 1973 - Effect of salt on the response of birds to sucrose","interactions":[],"lastModifiedDate":"2025-07-09T17:11:06.972235","indexId":"5224973","displayToPublicDate":"2013-10-07T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3073,"text":"Physiological Psychology","active":true,"publicationSubtype":{"id":10}},"title":"Effect of salt on the response of birds to sucrose","docAbstract":"<p><span>The preference of male red-winged blackbirds for solutions of sucrose and sucrose with 0.03 M sodium chloride was tested, using a two-bottle choice test. Preliminary experiments demonstrated that the birds were indifferent to 0.03 M NaCl in water. Both control and experimental animals exhibited indifference to the solutions at the lowest concentration and aversion at the highest. The data suggest that the added sodium chloride makes the sucrose stimulus more discriminable.</span></p>","language":"English","publisher":"Springer Nature","doi":"10.3758/BF03326903","usgsCitation":"Rogers, J., and Maller, O., 1973, Effect of salt on the response of birds to sucrose: Physiological Psychology, v. 1, no. 2, p. 199-200, https://doi.org/10.3758/BF03326903.","productDescription":"2 p.","startPage":"199","endPage":"200","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":492039,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.3758/bf03326903","text":"Publisher Index Page"},{"id":202167,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"2","noUsgsAuthors":false,"publicationDate":"2013-10-07","publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625337","contributors":{"authors":[{"text":"Rogers, J.G. Jr.","contributorId":46651,"corporation":false,"usgs":true,"family":"Rogers","given":"J.G.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":343340,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maller, O.","contributorId":19271,"corporation":false,"usgs":true,"family":"Maller","given":"O.","email":"","affiliations":[],"preferred":false,"id":343339,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047584,"text":"70047584 - 1973 - Reconnaissance investigation of the ground-water resources of the Brazos River basin, Texas","interactions":[{"subject":{"id":52319,"text":"ofr6327 - 1963 - A reconnaissance of the ground-water resources of the Brazos River basin, Texas","indexId":"ofr6327","publicationYear":"1963","noYear":false,"title":"A reconnaissance of the ground-water resources of the Brazos River basin, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70047584,"text":"70047584 - 1973 - Reconnaissance investigation of the ground-water resources of the Brazos River basin, Texas","indexId":"70047584","publicationYear":"1973","noYear":false,"title":"Reconnaissance investigation of the ground-water resources of the Brazos River basin, Texas"},"id":1}],"lastModifiedDate":"2013-08-12T16:13:22","indexId":"70047584","displayToPublicDate":"2013-01-01T16:07:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"6310","title":"Reconnaissance investigation of the ground-water resources of the Brazos River basin, Texas","docAbstract":"The Brazos River Basin in Texas extends from the New Mexico State line southeastward to the Gulf of Mexico. The basin is about 600 miles long and ranges in width from 1 to 120 miles--an area of about 42,000 square miles, which includes all or parts of 69 counties. About 1,385,000 persons reside in the basin.","language":"English","publisher":"Texas Water Development Board","publisherLocation":"Austin, TX","collaboration":"Prepared by the U. S. Geological Survey in cooperation with the Texas Water Commission","usgsCitation":"Cronin, J., Follett, C., Shafer, G., and Rettman, P., 1973, Reconnaissance investigation of the ground-water resources of the Brazos River basin, Texas (Second Printing February 1974 by Texas Water Development Board): Bulletin 6310, 152 p.; 9 Figures; 1 Table; Maps: 11 Sheets.","productDescription":"152 p.; 9 Figures; 1 Table; Maps: 11 Sheets","costCenters":[],"links":[{"id":276557,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047584.PNG"},{"id":276556,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.state.tx.us/publications/reports/bulletins/doc/Bull.htm/B6310.asp"}],"country":"United States","state":"Texas","otherGeospatial":"Brazos River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0,28.8 ], [ -103.0,34.7167 ], [ -94.9833,34.7167 ], [ -94.9833,28.8 ], [ -103.0,28.8 ] ] ] } } ] }","edition":"Second Printing February 1974 by Texas Water Development Board","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03f9e4b0026c2bc11c75","contributors":{"authors":[{"text":"Cronin, J.G.","contributorId":47769,"corporation":false,"usgs":true,"family":"Cronin","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":482462,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Follett, C.R.","contributorId":14800,"corporation":false,"usgs":true,"family":"Follett","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":482460,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shafer, G.H.","contributorId":46604,"corporation":false,"usgs":true,"family":"Shafer","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":482461,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rettman, P.L.","contributorId":60663,"corporation":false,"usgs":true,"family":"Rettman","given":"P.L.","affiliations":[],"preferred":false,"id":482463,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70047488,"text":"70047488 - 1973 - Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida","interactions":[{"subject":{"id":24343,"text":"ofr71241 - 1971 - A preliminary evaluation of hydrologic conditions of the Lakeland Ridge area of Polk County, Florida","indexId":"ofr71241","publicationYear":"1971","noYear":false,"title":"A preliminary evaluation of hydrologic conditions of the Lakeland Ridge area of Polk County, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047488,"text":"70047488 - 1973 - Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida","indexId":"70047488","publicationYear":"1973","noYear":false,"title":"Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida"},"id":1}],"lastModifiedDate":"2017-09-13T17:59:54","indexId":"70047488","displayToPublicDate":"2013-01-01T15:31:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":283,"text":"Florida Bureau of Geology Report of Investigations","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"64","title":"Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida","docAbstract":"The Lakeland ridge area of this investigation covers about 300 square miles in northwest Polk County in central Florida. The growth of industry, phosphate mining, and citrus production as well as population growth during the last two decades has resulted in an increase in ground-water pumpage from about 11 billion gallons in 1950 to 27 billion gallons in 1970.","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by United States Geological Survey in cooperation with Southwest Florida Water Management District the City of Lakeland, Florida and the Bureau of Geology Florida Department of Natural Resources","usgsCitation":"Robertson, A.F., 1973, Hydrologic conditions in the Lakeland Ridge area of Polk County, Florida: Florida Bureau of Geology Report of Investigations 64, vii, 48 p.","productDescription":"vii, 48 p.","costCenters":[],"links":[{"id":276182,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047488.PNG"},{"id":276181,"type":{"id":11,"text":"Document"},"url":"https://ufdc.ufl.edu/UF00001251/00001/pdf?search=report+%3dinvestigations"}],"country":"United States","state":"Florida","county":"Polk County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.1062,27.6432 ], [ -82.1062,28.3619 ], [ -81.131,28.3619 ], [ -81.131,27.6432 ], [ -82.1062,27.6432 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5203a37ae4b02bdb1bc63fbc","contributors":{"authors":[{"text":"Robertson, Alton F.","contributorId":71177,"corporation":false,"usgs":true,"family":"Robertson","given":"Alton","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":482174,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047607,"text":"70047607 - 1973 - Ground-water resources of Coke County, Texas","interactions":[{"subject":{"id":47996,"text":"ofr71342 - 1971 - Ground-water resources of Coke County, Texas","indexId":"ofr71342","publicationYear":"1971","noYear":false,"title":"Ground-water resources of Coke County, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70047607,"text":"70047607 - 1973 - Ground-water resources of Coke County, Texas","indexId":"70047607","publicationYear":"1973","noYear":false,"title":"Ground-water resources of Coke County, Texas"},"id":1}],"lastModifiedDate":"2013-08-14T13:41:12","indexId":"70047607","displayToPublicDate":"2013-01-01T13:13:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":133,"text":"Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"166","title":"Ground-water resources of Coke County, Texas","docAbstract":"Coke County, located in semiarid west-central Texas, where large ranches, small farms, and oil production are the main bases of the economy, has a small supply of ground and surface water. Of the approximately 1,900 acre-feet of fresh to moderately saline ground water used in 1968, industry used 880 acre-feet, irrigation used 210 acre-feet, and domestic supply and livestock used 820 acre-feet. All of the water for municipal supply and some of the water for industry is obtained from surface-water reservoirs.","language":"English","publisher":"Texas Water Development Board","publisherLocation":"San Antonio, TX","collaboration":"This report was prepared by the U.S. Geological Survey under cooperative agreement with the Texas Water Development Board","usgsCitation":"Wilson, C.A., 1973, Ground-water resources of Coke County, Texas: Report 166, v, 87 p.","productDescription":"v, 87 p.","costCenters":[],"links":[{"id":276605,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047607.png"},{"id":276604,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.state.tx.us/publications/reports/numbered_reports/doc/R166/Report166.asp"}],"country":"United States","state":"Texas","county":"Coke County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100.8254,31.692 ], [ -100.8254,32.0856 ], [ -100.2344,32.0856 ], [ -100.2344,31.692 ], [ -100.8254,31.692 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520ca6e7e4b081fa6136d3ff","contributors":{"authors":[{"text":"Wilson, Clyde A.","contributorId":65464,"corporation":false,"usgs":true,"family":"Wilson","given":"Clyde","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":482515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047604,"text":"70047604 - 1973 - Ground-water resources of Wheeler and eastern Gray Counties, Texas","interactions":[{"subject":{"id":57747,"text":"ofr69333 - 1969 - Ground-water resources of Wheeler and eastern Gray Counties, Texas","indexId":"ofr69333","publicationYear":"1969","noYear":false,"title":"Ground-water resources of Wheeler and eastern Gray Counties, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70047604,"text":"70047604 - 1973 - Ground-water resources of Wheeler and eastern Gray Counties, Texas","indexId":"70047604","publicationYear":"1973","noYear":false,"title":"Ground-water resources of Wheeler and eastern Gray Counties, Texas"},"id":1}],"lastModifiedDate":"2013-08-14T12:54:54","indexId":"70047604","displayToPublicDate":"2013-01-01T11:15:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":133,"text":"Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"170","title":"Ground-water resources of Wheeler and eastern Gray Counties, Texas","docAbstract":"Wheeler and eastern Gray Counties are in the east·central part of the Texas Panhandle. The two counties are characterized by rolling to fairly rugged topography with many sand-dune areas and a well developed drainage system.","language":"English","publisher":"Texas Water Development Board","publisherLocation":"San Antonio, TX","collaboration":"This report was prepared by the U.S. Geological Survey under cooperative agreement with the Texas Waler Development Board","usgsCitation":"Maderak, M., 1973, Ground-water resources of Wheeler and eastern Gray Counties, Texas: Report 170, v, 66 p.","productDescription":"v, 66 p.","costCenters":[],"links":[{"id":276599,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047604.png"},{"id":276598,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.state.tx.us/publications/reports/numbered_reports/doc/R170/Report170.asp"}],"country":"United States","state":"Texas","county":"Wheeler County;Gray County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -101.0862,35.1817 ], [ -101.0862,35.6208 ], [ -100.0003,35.6208 ], [ -100.0003,35.1817 ], [ -101.0862,35.1817 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520ca6e8e4b081fa6136d406","contributors":{"authors":[{"text":"Maderak, M.L.","contributorId":41452,"corporation":false,"usgs":true,"family":"Maderak","given":"M.L.","affiliations":[],"preferred":false,"id":482509,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047603,"text":"70047603 - 1973 - Ground-water resources of Brazoria County, Texas","interactions":[{"subject":{"id":57139,"text":"ofr70377 - 1970 - Ground-water resources of Brazoria County, Texas","indexId":"ofr70377","publicationYear":"1970","noYear":false,"title":"Ground-water resources of Brazoria County, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":70047603,"text":"70047603 - 1973 - Ground-water resources of Brazoria County, Texas","indexId":"70047603","publicationYear":"1973","noYear":false,"title":"Ground-water resources of Brazoria County, Texas"},"id":1}],"lastModifiedDate":"2013-08-14T12:56:02","indexId":"70047603","displayToPublicDate":"2013-01-01T10:55:28","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":133,"text":"Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"163","title":"Ground-water resources of Brazoria County, Texas","docAbstract":"The Chicot and Evangeline aquifers are the only hydrologic units bearing fresh (less than 1,000 milligrams per liter dissolved solids) or slightly saline water (1,000-3,000 milligrams per liter dissolved solids in Brazoria County. These aquifers are composed of gravel, sand, silt, and clay of Pliocene, Pleistocene, and Holocene age.","language":"English","publisher":"Texas Water Development Board","publisherLocation":"San Antonio, TX","collaboration":"This report was prepared by the U.S. Geological Survey under cooperative agreement with the Texas Water Development Board; Reprinted by the Texas Department of Water Resources December 1982","usgsCitation":"Sandeen, W.M., and Wesselman, J.B., 1973, Ground-water resources of Brazoria County, Texas: Report 163, v, 64 p.","productDescription":"v, 64 p.","numberOfPages":"40","costCenters":[],"links":[{"id":276596,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047603.png"},{"id":276595,"type":{"id":15,"text":"Index Page"},"url":"https://www.twdb.state.tx.us/publications/reports/numbered_reports/doc/R163/report163.asp"}],"country":"United States","state":"Texas","county":"Brazoria County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.8721,28.8214 ], [ -95.8721,29.5991 ], [ -95.0561,29.5991 ], [ -95.0561,28.8214 ], [ -95.8721,28.8214 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520ca6e6e4b081fa6136d3f1","contributors":{"authors":[{"text":"Sandeen, William M.","contributorId":32533,"corporation":false,"usgs":true,"family":"Sandeen","given":"William","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":482507,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wesselman, John B.","contributorId":52154,"corporation":false,"usgs":true,"family":"Wesselman","given":"John","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":482508,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047245,"text":"70047245 - 1973 - Fluorite equilibria in thermal springs of the Snake River Basin, Idaho","interactions":[],"lastModifiedDate":"2015-08-25T15:31:18","indexId":"70047245","displayToPublicDate":"2013-01-01T10:40:58","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Fluorite equilibria in thermal springs of the Snake River Basin, Idaho","docAbstract":"<p>Some thermal water sources of the Snake River basin, Idaho, are near saturation with respect to fluorite. That mineral was identified by X-ray diffraction in precipitates induced in three water samples by adding sodium fluoride. The derived solubility product (K<sub>S0</sub>) for zero ionic strength was close to that calculated from Latimer's thermodynamic data (10<sup>-9.7 7</sup>). The relative ease of precipitation of fluorite from these water samples indicates that equilibrium with respect to fluorite may occur in some ground-water systems.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Research of the U.S. Geological Survey","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Roberson, C.E., and Schoen, R., 1973, Fluorite equilibria in thermal springs of the Snake River Basin, Idaho: Journal of Research of the U.S. Geological Survey, v. 1, no. 3, p. 367-370.","productDescription":"4 p.","startPage":"367","endPage":"370","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":275432,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":307459,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue3/report.pdf","text":"Report","size":"23.61 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.02636718749999,\n              42.00032514831621\n            ],\n            [\n              -117.02636718749999,\n              46.73986059969267\n            ],\n            [\n              -111.02783203125,\n              46.73986059969267\n            ],\n            [\n              -111.02783203125,\n              42.00032514831621\n            ],\n            [\n              -117.02636718749999,\n              42.00032514831621\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"1","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51f39a65e4b0a32220222f79","contributors":{"authors":[{"text":"Roberson, C. E.","contributorId":40190,"corporation":false,"usgs":true,"family":"Roberson","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":481489,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schoen, Robert","contributorId":22418,"corporation":false,"usgs":true,"family":"Schoen","given":"Robert","email":"","affiliations":[],"preferred":false,"id":481488,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047244,"text":"70047244 - 1973 - A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 1: Mud Lake Region, 1969-70 and Part 2: Observation Wells South of Arco and West of Aberdeen","interactions":[],"lastModifiedDate":"2013-07-26T10:37:43","indexId":"70047244","displayToPublicDate":"2013-01-01T10:25:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":301,"text":"Water Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"32","title":"A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 1: Mud Lake Region, 1969-70 and Part 2: Observation Wells South of Arco and West of Aberdeen","docAbstract":"The results of drilling test holes to depths of approximately 1,000 feet in the Mud Lake region show that a large part of the region is underlain by both sedimentary deposits and basalt flows. At some locations, predominantly sedimentary deposits were penetrated; at others, basalt flows predominated. The so-called Mud Lake-Market Lake barrier denotes a change in geology. From the vicinity of the barrier area, as described by Stearns, Crandall, and Steward (1938, p. 111), up the water-table gradient for at least a few tens of miles, the saturated geologic section consists predominantly of beds of sediments that are intercalated with numerous basalt flows. Downgradient from the barrier, sedimentary deposits are not common and practically all the water-bearing formations are basalt, at least to the depths explored so far. Thus, the barrier is a transition zone from a sedimentary-basaltic sequence to a basaltic sequence. The sedimentary-basaltic sequence forms a complex hydrologic system in which water occurs under water-table conditions in the upper few tens of feet of saturated material and under artesian conditions in the deeper material in the southwest part of the region. The well data indicate that southwest of the barrier, artesian pressures are not significant. Southwest of the barrier, few sedimentary deposits occur in the basalt section and, as described by Mundorff, Crosthwaite, and Kilburn (1964). ground water occurs in a manner typical of the Snake Plain aquifer. In several wells, artesian pressures are higher in the deeper formations than in the shallower ones, but the reverse was found in a few wells. The available data are not adequate to describe the water-bearing characteristics of the artesian aquifer nor the effects that pumping in one zone would have on adjacent zones. The water-table aquifer yields large quantities of water to irrigation wells.","language":"English","publisher":"Idaho Department of Water Administration","publisherLocation":"Boise City, ID","collaboration":"Prepared by the United States Geological Survey in cooperation with Idaho Department of Water Administration","usgsCitation":"Crosthwaite, E., 1973, A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 1: Mud Lake Region, 1969-70 and Part 2: Observation Wells South of Arco and West of Aberdeen: Water Information Bulletin 32, vii, 60 p.; Figures.","productDescription":"vii, 60 p.; Figures","numberOfPages":"73","costCenters":[],"links":[{"id":275431,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047244.png"},{"id":275430,"type":{"id":11,"text":"Document"},"url":"https://www.idwr.idaho.gov/WaterInformation/Publications/wib/wib32-mud_lake_arco_aberdeen.pdf"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake Plain Aquifer","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.0,42.0 ], [ -117.0,45.0 ], [ -111.0,45.0 ], [ -111.0,42.0 ], [ -117.0,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51f39a62e4b0a32220222f52","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":481487,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046308,"text":"70046308 - 1973 - Ground-water basic data for Griggs and Steele Counties, North Dakota","interactions":[],"lastModifiedDate":"2018-05-23T12:56:45","indexId":"70046308","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"64-2","title":"Ground-water basic data for Griggs and Steele Counties, North Dakota","docAbstract":"The objectives of the hydrologic investigation in Griggs and Steele Counties, N. Dak. (fig. 1) were to: (1) determine the location, extent, and nature of the major aquifers; (2) evaluate the occurrence and movement of ground water, including recharge and discharge; (3) estimate the quantities of water stored in the aquifers; (4) estimate the potential yields of wells tapping the major aquifers; and (5) determine the chemical quality of the ground water.","language":"English","publisher":"North Dakota Geological Survey","publisherLocation":"Grand Forks, ND","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the North Dakota Geological Survey, North Dakota State Water Commission, Griggs County Water Management District and the Steele County Water Management District; this report was also published as North Dakota County Ground-Water Studies 21-2","usgsCitation":"Downey, J.S., 1973, Ground-water basic data for Griggs and Steele Counties, North Dakota: Bulletin 64-2, ii, 468 p.","productDescription":"ii, 468 p.","numberOfPages":"470","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":273371,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046308.png"},{"id":273369,"type":{"id":11,"text":"Document"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-253/GriggsSteele_Part_2.pdf"},{"id":273370,"type":{"id":17,"text":"Plate"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-254/Griggs_and_Steele_Part2_Plates.pdf"}],"country":"United States","state":"North Dakota","county":"Griggs County, Steele County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.5019,47.2394 ], [ -98.5019,47.6742 ], [ -97.4505,47.6742 ], [ -97.4505,47.2394 ], [ -98.5019,47.2394 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b1bbd2e4b022a6a540f9cf","contributors":{"authors":[{"text":"Downey, Joe S.","contributorId":102454,"corporation":false,"usgs":true,"family":"Downey","given":"Joe","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":479434,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042557,"text":"70042557 - 1973 - Volcanic studies: Part E: Eratosthenian volcanism in Mare Imbrium: source of youngest lava flows","interactions":[],"lastModifiedDate":"2013-01-11T14:25:56","indexId":"70042557","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Volcanic studies: Part E: Eratosthenian volcanism in Mare Imbrium: source of youngest lava flows","docAbstract":"Orbital photographs taken at low-Sun illumination during both the Apollo 15 (ref. 30-14) and Apollo 17 missions have provided excellent data on the lava flows in the southwestern Mare Imbrium. These photographs have been used recently to present a detailed photogeologic evaluation of these flows and their role in mare volcanism of Eratosthenian age in the basin (ref. 30-15). Eruption of these flood basalts apparently took place in at least three major episodes with suggested dates of 3.0 &plusmn; 0.4 billion years (phase I), 2.7 &plusmn; 0.3 billion years (phase II), and 2.5 &plusmn; 0.3 billion years (phase III) using the mare age-dating method described by Soderblom and Lebofsky (ref. 30-16) and recent data by Soderblom and Boyce (ref. 30-17).","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Schaber, G.G., 1973, Volcanic studies: Part E: Eratosthenian volcanism in Mare Imbrium: source of youngest lava flows, chap. <i>of</i> Apollo 17 preliminary science report, p. 30-17-30-25.","productDescription":"9 p.","startPage":"30-17","endPage":"30-25","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265570,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265569,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a17/a17psr.html"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f1428be4b0c982afefa8db","contributors":{"authors":[{"text":"Schaber, Gerald G.","contributorId":12511,"corporation":false,"usgs":true,"family":"Schaber","given":"Gerald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":471810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042561,"text":"70042561 - 1973 - Crater studies: Part A: lunar crater morphometry","interactions":[],"lastModifiedDate":"2013-01-11T15:27:14","indexId":"70042561","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Crater studies: Part A: lunar crater morphometry","docAbstract":"Morphometry, the quantitative study of shape, complements the visual observation and photointerpretation in analyzing the most outstanding landforms of the Moon, its craters (refs. 32-1 and 32-2). All three of these interpretative tools, which were developed throughout the long history of telescopic lunar study preceding the Apollo Program, will continue to be applicable to crater analysis until detailed field work becomes possible. Although no large (>17.5 km diameter) craters were examined in situ on any of the Apollo landings, the photographs acquired from the command modules will markedly strengthen results of less direct investigations of the craters. For morphometry, the most useful materials are the orbital metric and panoramic photographs from the final three Apollo missions. These photographs permit preparation of contour maps, topographic profiles, and other numerical data that accurately portray for the first time the surface geometry of lunar craters of all sizes. Interpretations of craters no longer need be compromised by inadequate topographic data. In the pre-Apollo era, hypotheses for the genesis of lunar craters usually were constructed without any numerical descriptive data. Such speculations will have little credibility unless supported by accurate, quantitative data, especially those generated from Apollo orbital photographs. This paper presents a general study of the surface geometry of 25 far-side craters and a more detailed study of rim-crest evenness for 15 near-side and far-side craters. Analysis of this preliminary sample of Apollo 15 and 17 data, which includes craters between 1.5 and 275 km in diameter, suggests that most genetic interpretations of craters made from pre-Apollo topographic measurements may require no drastic revision. All measurements were made from topographic profiles generated on a stereoplotter at the Photogrammetric Unit of the U.S. Geological Survey, Center of Astrogeology, Flagstaff, Arizona.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report (NASA SP-330)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Pike, R.J., 1973, Crater studies: Part A: lunar crater morphometry, chap. <i>of</i> Apollo 17 preliminary science report (NASA SP-330), p. 32-1-32-7.","productDescription":"7 p.","startPage":"32-1","endPage":"32-7","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265575,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265576,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a17/a17psr.html"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f14273e4b0c982afefa87f","contributors":{"authors":[{"text":"Pike, Richard J. rpike@usgs.gov","contributorId":5753,"corporation":false,"usgs":true,"family":"Pike","given":"Richard","email":"rpike@usgs.gov","middleInitial":"J.","affiliations":[],"preferred":true,"id":471818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042560,"text":"70042560 - 1973 - Mare ridges and related studies: Part D: small structures of the Taurus-Littrow region","interactions":[],"lastModifiedDate":"2013-01-11T14:55:35","indexId":"70042560","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Mare ridges and related studies: Part D: small structures of the Taurus-Littrow region","docAbstract":"Apollo 17 permission geologic studies of the Taurus-Littrow region of the Moon revealed numerous small structures, in both mare and terra, having somewhat similar morphologies and variously resembling fault scarps, flow fronts, and mare ridges. Many of these features are too small to be identified on Lunar Orbiter IV photographs, which provided the most comprehensive, high-resolution coverage of this area before the later Apollo missions. The panoramic- and metric-camera photographs of Apollo 17 were taken at lower Sun angles than those of Apollo 15, which were used for the geologic mapping (refs. 31-40 and 31-41), and thus more clearly reveal fine details of texture and relief. In the illustrations of this part, several of these small structures are compared. It is concluded that they probably developed as lava extrusions from fractures and fissures; they cannot be easily explained by faulting.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report (NASA SP-330)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Scott, D.H., 1973, Mare ridges and related studies: Part D: small structures of the Taurus-Littrow region, chap. <i>of</i> Apollo 17 preliminary science report (NASA SP-330), p. 31-25-31-29.","productDescription":"5 p.","startPage":"31-25","endPage":"31-29","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265574,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265573,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a17/a17psr.html"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f1427ae4b0c982afefa893","contributors":{"authors":[{"text":"Scott, David H. 0000-0002-7925-7452 dscott@usgs.gov","orcid":"https://orcid.org/0000-0002-7925-7452","contributorId":14415,"corporation":false,"usgs":true,"family":"Scott","given":"David","email":"dscott@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":false,"id":471817,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042566,"text":"70042566 - 1973 - Remote sensing and photogrammetric studies: Part C: comparison between photogrammetric and bistatic-radar slope-frequency distributions","interactions":[],"lastModifiedDate":"2013-01-11T16:21:08","indexId":"70042566","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Remote sensing and photogrammetric studies: Part C: comparison between photogrammetric and bistatic-radar slope-frequency distributions","docAbstract":"Stereoscopic photographs taken by the metric and panoramic cameras can be used to obtain information on the roughness and slope-frequency distributions of lunar surfaces (see appendix to this part). Bistatic radar on board Apollo 14, 15, and 16 spacecraft may also be used to obtain information on lunar surface roughness at two wavelengths&mdash;13 cm (S-band) and 116 cm (VHF).","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report (NASA SP-330)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Moore, H., and Tyler, G., 1973, Remote sensing and photogrammetric studies: Part C: comparison between photogrammetric and bistatic-radar slope-frequency distributions, chap. <i>of</i> Apollo 17 preliminary science report (NASA SP-330), p. 33-17-33-26.","productDescription":"10 p.","startPage":"33-17","endPage":"33-26","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265582,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265581,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a17/a17psr.html"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f14282e4b0c982afefa8b4","contributors":{"authors":[{"text":"Moore, H. J.","contributorId":71962,"corporation":false,"usgs":true,"family":"Moore","given":"H. J.","affiliations":[],"preferred":false,"id":471830,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tyler, G.L.","contributorId":26297,"corporation":false,"usgs":true,"family":"Tyler","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":471829,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042541,"text":"70042541 - 1973 - Surface electrical properties experiment","interactions":[],"lastModifiedDate":"2013-01-11T11:37:29","indexId":"70042541","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Surface electrical properties experiment","docAbstract":"The surface electrical properties (SEP) experiment was used to explore the subsurface material of the Apollo 17 landing site by means of electromagnetic radiation. The experiment was designed to detect electrical layering, discrete scattering bodies, and the possible presence of water. From the analysis of the data, it was expected that values of the electrical properties (dielectric constant and loss tangent) of lunar material in situ would be obtained.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report (NASA SP-330)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"usgsCitation":"Simmons, G., Strangway, D., Annan, P., Baker, R.G., Bannister, L., Brown, R.E., Cooper, W., Cubley, D., deBettencourt, J., England, A.W., Groener, J., Kong, J., LaTorraca, G., Meyer, J., Nanda, V., Redman, D., Rossiter, J., Tsang, L., Urner, J., and Watts, R., 1973, Surface electrical properties experiment, chap. <i>of</i> Apollo 17 preliminary science report (NASA SP-330), p. 15-1-15-14.","productDescription":"14 p.","startPage":"15-1","endPage":"15-14","costCenters":[{"id":131,"text":"Astrogeology Science 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,{"id":70042574,"text":"70042574 - 1973 - Remote sensing and photogrammetric studies: Part D: repeatability of elevation measurements--Apollo photography","interactions":[],"lastModifiedDate":"2013-01-11T18:03:44","indexId":"70042574","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Remote sensing and photogrammetric studies: Part D: repeatability of elevation measurements--Apollo photography","docAbstract":"Stereoscopic photographs of the Moon taken by the metric and panoramic cameras on board the service module of Apollo spacecraft provide a source for quantitative data on lunar topography. The accuracy of the topographic data depends, in part, on the repeatability of elevation measurements. The repeatability depends on contrast in the stereoscopic image and is affected by many factors, such as photographic quality, the photogrammetric instrument used, and illumination conditions. For the Moon, illumination conditions are important so that repeatability of elevation measurements may be statistically related to Sun elevation angles, local slopes, and albedos of surfaces. We have examined the effect of Sun elevation angle on repeatability, using Apollo 15 photographs (Wu, unpublished data), and extended the results to slope-related effects.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report (NASA SP-330)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Wu, S.S., Schafer, F.J., Nakata, G.M., and Jordan, R., 1973, Remote sensing and photogrammetric studies: Part D: repeatability of elevation measurements--Apollo photography, chap. <i>of</i> Apollo 17 preliminary science report (NASA SP-330), p. 33-35-33-40.","productDescription":"6 p.","startPage":"33-35","endPage":"33-40","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265585,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a17/a17psr.html"},{"id":265586,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f14282e4b0c982afefa8b8","contributors":{"authors":[{"text":"Wu, Sherman S.C.","contributorId":33198,"corporation":false,"usgs":true,"family":"Wu","given":"Sherman","email":"","middleInitial":"S.C.","affiliations":[],"preferred":false,"id":471841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schafer, Francis J.","contributorId":60517,"corporation":false,"usgs":true,"family":"Schafer","given":"Francis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":471842,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nakata, Gary M.","contributorId":22224,"corporation":false,"usgs":true,"family":"Nakata","given":"Gary","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":471840,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jordan, Raymond","contributorId":91466,"corporation":false,"usgs":true,"family":"Jordan","given":"Raymond","email":"","affiliations":[],"preferred":false,"id":471843,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70042942,"text":"70042942 - 1973 - Geological literature on the San Joaquin Valley of California","interactions":[{"subject":{"id":14789,"text":"ofr68174 - 1968 - Geological literature on the San Joaquin Valley of California","indexId":"ofr68174","publicationYear":"1968","noYear":false,"title":"Geological literature on the San Joaquin Valley of California"},"predicate":"SUPERSEDED_BY","object":{"id":70042942,"text":"70042942 - 1973 - Geological literature on the San Joaquin Valley of California","indexId":"70042942","publicationYear":"1973","noYear":false,"title":"Geological literature on the San Joaquin Valley of California"},"id":1}],"lastModifiedDate":"2013-01-29T11:08:11","indexId":"70042942","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":4,"text":"Book"},"title":"Geological literature on the San Joaquin Valley of California","docAbstract":"The following list of references includes most of the geological literature on the San Joaquin Valley and vicinity in central California (see figure 1) published prior to January 1, 1973. The San Joaquin Valley comprises all or parts of 11 counties -- Alameda, Calaveras, Contra Costa, Fresno, Kern, Kings, Madera, Merced, San Joaquin, Stanislaus, and Tulare (figure 2). As a matter of convenient geographical classification the boundaries of the report area have been drawn along county lines, and to include San Benito and Santa Clara Counties on the west and Mariposa and Tuolumne Counties on the east. Therefore, this list of geological literature includes some publications on the Diablo and Temblor Ranges on the west, the Tehachapi Mountains and Mojave Desert on the south, and the Sierra Nevada Foothills and Mountains on the east.","language":"English","publisher":"AAPG","publisherLocation":"Tulsa, OK","usgsCitation":"Maher, J., Trollman, W., and Denman, J., 1973, Geological literature on the San Joaquin Valley of California, 582 p.","productDescription":"582 p.","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":266684,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/pacific/data/036/036001/1_ps0360001.htm"},{"id":266685,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.84,35.06 ], [ -121.84,38.17 ], [ -118.67,38.17 ], [ -118.67,35.06 ], [ -121.84,35.06 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd82e4b0d965cd9f232e","contributors":{"authors":[{"text":"Maher, J.C.","contributorId":98800,"corporation":false,"usgs":true,"family":"Maher","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":472641,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trollman, W.M.","contributorId":45597,"corporation":false,"usgs":true,"family":"Trollman","given":"W.M.","affiliations":[],"preferred":false,"id":472640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Denman, J.M.","contributorId":42084,"corporation":false,"usgs":true,"family":"Denman","given":"J.M.","affiliations":[],"preferred":false,"id":472639,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70042564,"text":"70042564 - 1973 - Remote sensing and photogrammetric studies: Part A: remote sensing of Mare Serenitatis","interactions":[],"lastModifiedDate":"2013-01-11T15:47:04","indexId":"70042564","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Remote sensing and photogrammetric studies: Part A: remote sensing of Mare Serenitatis","docAbstract":"Mare Serenitatis is a circular mare approximately 600 km  in diameter in the northeast quadrant of the lunar near side. It occupies an old multi-ringed basin (refs. 33-1 and 33-2) and is the site of a prominent mascon (ref. 33-3). A conspicuous dark annulus in this mare prompted subdivision of the mare materials into different stratigraphic units (refs. 33-2 and 33-4). A revised stratigraphic sequence for the southern part of Mare Serenitatis, based on photogeologic interpretation of Apollo 15 and 17 photographs, is summarized as follows after Howard et al.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report (NASA SP-330)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Thompson, T., Howard, K.A., Shorthill, R., Tyler, G., Zisk, S., Whitaker, E.A., Schaber, G.G., and Moore, H., 1973, Remote sensing and photogrammetric studies: Part A: remote sensing of Mare Serenitatis, chap. <i>of</i> Apollo 17 preliminary science report (NASA SP-330), p. 33-3-33-10.","productDescription":"8 p.","startPage":"33-3","endPage":"33-10","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265578,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265577,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a17/a17psr.html"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f14280e4b0c982afefa8ac","contributors":{"authors":[{"text":"Thompson, T.W.","contributorId":78736,"corporation":false,"usgs":true,"family":"Thompson","given":"T.W.","email":"","affiliations":[],"preferred":false,"id":471826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howard, K. A.","contributorId":48938,"corporation":false,"usgs":false,"family":"Howard","given":"K.","middleInitial":"A.","affiliations":[],"preferred":false,"id":471823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shorthill, R.W.","contributorId":20321,"corporation":false,"usgs":true,"family":"Shorthill","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":471819,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Tyler, G.L.","contributorId":26297,"corporation":false,"usgs":true,"family":"Tyler","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":471820,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Zisk, S.H.","contributorId":35311,"corporation":false,"usgs":true,"family":"Zisk","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":471821,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Whitaker, E. A.","contributorId":43086,"corporation":false,"usgs":true,"family":"Whitaker","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":471822,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Schaber, G. G.","contributorId":68300,"corporation":false,"usgs":true,"family":"Schaber","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":471824,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Moore, H. J.","contributorId":71962,"corporation":false,"usgs":true,"family":"Moore","given":"H. J.","affiliations":[],"preferred":false,"id":471825,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}}
,{"id":70042550,"text":"70042550 - 1973 - Stratigraphic studies: Part C: relative ages of some near-side mare units based on Apollo 17 metric photographs","interactions":[],"lastModifiedDate":"2013-01-11T13:13:56","indexId":"70042550","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Stratigraphic studies: Part C: relative ages of some near-side mare units based on Apollo 17 metric photographs","docAbstract":"The lunar maria formed at different times and in multiple stages of extrusion. An understanding of their evolution is essential in placing the Apollo samples in a regional context and in interpreting the regional geology of a vast part of the lunar surface.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report (NASA SP-330)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Boyce, J.M., and Dial, A.L., 1973, Stratigraphic studies: Part C: relative ages of some near-side mare units based on Apollo 17 metric photographs, chap. <i>of</i> Apollo 17 preliminary science report (NASA SP-330), p. 29-26-29-28.","productDescription":"3 p.","startPage":"29-26","endPage":"29-28","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265562,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265561,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a17/a17psr.html"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f14288e4b0c982afefa8cb","contributors":{"authors":[{"text":"Boyce, Joseph M.","contributorId":52963,"corporation":false,"usgs":true,"family":"Boyce","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":471800,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dial, Arthur L. Jr.","contributorId":32413,"corporation":false,"usgs":true,"family":"Dial","given":"Arthur","suffix":"Jr.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":471799,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042539,"text":"70042539 - 1973 - Preliminary geologic investigation of the Apollo 17 landing site","interactions":[],"lastModifiedDate":"2013-01-11T18:17:01","indexId":"70042539","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Preliminary geologic investigation of the Apollo 17 landing site","docAbstract":"The Apollo 17 lunar module (LM) landed on the flat floor of a deep valley that embays the mountainous highlands at the eastern rim of the Serenitatis basin. Serenitatis, the site of a pronounced mascon, is one of the major multi-ringed basins on the near side of the Moon. 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,{"id":70042543,"text":"70042543 - 1973 - Stratigraphic studies: Part A: basalt stratigraphy of southern Mare Serenitatis","interactions":[],"lastModifiedDate":"2013-01-11T12:44:22","indexId":"70042543","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Stratigraphic studies: Part A: basalt stratigraphy of southern Mare Serenitatis","docAbstract":"Mare Serenitatis has long been noted for its conspicuous dark border (fig. 29-1). The Apollo 17 metric photographs traverse this border in southern Mare Serenitatis and show clearly  superposition relationships among the mare and mare-related stratigraphic units. These photographs, together with full-Moon photographs, albedo measurements, and color information (table 29-I), provide the basis for a revised stratigraphic framework for these presumedly basaltic rocks (figs. 29-2 and 29-3). In contrast to most previous studies, we conclude that the darker units are older than lighter ones. Similar conclusions have been reached by Bryan and Adams (part C of sec. 30) and Boyce and Dial (part C of this section). The relatively light-colored central part of Mare Serenitatis is thought to represent the youngest basalt in the region; a very dark unit that includes the Apollo 17 landing site is one of the oldest.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report (NASA SP-330)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Howard, K.A., Carr, M.H., and Muehlberger, W., 1973, Stratigraphic studies: Part A: basalt stratigraphy of southern Mare Serenitatis, chap. <i>of</i> Apollo 17 preliminary science report (NASA SP-330), p. 29-1-29-12.","productDescription":"12 p.","startPage":"29-1","endPage":"29-12","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265555,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265554,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a17/a17psr.html"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f14287e4b0c982afefa8c3","contributors":{"authors":[{"text":"Howard, K. A.","contributorId":48938,"corporation":false,"usgs":false,"family":"Howard","given":"K.","middleInitial":"A.","affiliations":[],"preferred":false,"id":471790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carr, M. H.","contributorId":84727,"corporation":false,"usgs":true,"family":"Carr","given":"M.","email":"","middleInitial":"H.","affiliations":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"preferred":false,"id":471792,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Muehlberger, W.R.","contributorId":66732,"corporation":false,"usgs":true,"family":"Muehlberger","given":"W.R.","affiliations":[],"preferred":false,"id":471791,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70042551,"text":"70042551 - 1973 - Stratigraphic studies: Part D: geologic map of the northern Crisium region","interactions":[],"lastModifiedDate":"2013-01-11T13:38:45","indexId":"70042551","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"330","title":"Stratigraphic studies: Part D: geologic map of the northern Crisium region","docAbstract":"Apollo 17 metric photographs (fig. 29-26) provide the best available coverage for geologic interpretation of northern Mare Crisium and the northern Crisium basin. The area was covered previously by low-resolution telescopic and Lunar Orbiter IV photographs and by oblique, high-illumination, or low-resolution photographs from earlier Apollo missions. One region in particular, between Alhazen Crater and longitude 66&deg; E, had previously been covered very poorly. The Apollo 17 photographs provide excellent monoscopic (fig. 29-26) as well as stereoscopic viewing because of the favorably low Sun illuminations (15&deg; to 49&deg;). These new photographic data allow the geology of the basin, the mare, and other nearby terrains to be reevaluated. This reexamination together with data from continuing Moon-wide photogeologic studies and analyses of returned rocks from Apollo landing sites, has produced a simple evolutionary picture of the region, expressed by fewer map units and explained by fewer basic processes than previously thought necessary (refs. 29-35 and 29-45 to 29-48).","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 17 preliminary science report (NASA SP-330)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Wilhelms, D.E., 1973, Stratigraphic studies: Part D: geologic map of the northern Crisium region, chap. <i>of</i> Apollo 17 preliminary science report (NASA SP-330), p. 29-29-29-35.","productDescription":"7 p.","startPage":"29-29","endPage":"29-35","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":265564,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265563,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a17/a17psr.html"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f14289e4b0c982afefa8cf","contributors":{"authors":[{"text":"Wilhelms, Don E.","contributorId":28972,"corporation":false,"usgs":true,"family":"Wilhelms","given":"Don","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":471801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042626,"text":"70042626 - 1973 - Revised age and structural interpretations of Nuka Formation at Nuka Ridge, northwestern Alaska: Geologic notes","interactions":[{"subject":{"id":16203,"text":"ofr72372 - 1972 - Revised age and structural interpretations of the Nuka Formation at Nuka Ridge, northwestern Alaska","indexId":"ofr72372","publicationYear":"1972","noYear":false,"title":"Revised age and structural interpretations of the Nuka Formation at Nuka Ridge, northwestern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70042626,"text":"70042626 - 1973 - Revised age and structural interpretations of Nuka Formation at Nuka Ridge, northwestern Alaska: Geologic notes","indexId":"70042626","publicationYear":"1973","noYear":false,"title":"Revised age and structural interpretations of Nuka Formation at Nuka Ridge, northwestern Alaska: Geologic notes"},"id":1}],"lastModifiedDate":"2023-01-31T17:41:56.952336","indexId":"70042626","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Revised age and structural interpretations of Nuka Formation at Nuka Ridge, northwestern Alaska: Geologic notes","docAbstract":"New collections of foraminifers and macrofossils from Nuka Ridge, the type area of the enigmatic Nuka Formation, demonstrate that the type Nuka Formation is not a continuous stratigraphic sequence as originally described. Paleontologic evidence indicates the presence of a structurally repeated sequence at Nuka Ridge consisting of Upper Mississippian (Meramec and younger) strata overlain by Permian beds which, in turn, are succeeded by Triassic(?) and Cretaceous rocks. Mississippian calcareous mudstone and limestone units are correlated with the Lisburne Group; microcline-bearing arkose units with Mississippian and Permian macrofossils and microfossils represent the Nuka Formation; units of chert are inferred to be of Permian and Triassic age; and wacke at the top of the sequence resembles unnamed wacke assigned to the Cretaceous elsewhere. These new data and their interpretations indicate that the type section of the Nuka Formation is inadequate. The standard for the Nuka Formation is therefore referred to a newly measured section of the middle arkosic unit of the old section.","language":"English","publisher":"American Association of Petroleum Geologists","publisherLocation":"Tulsa, OK","doi":"10.1306/83D90EBC-16C7-11D7-8645000102C1865D","usgsCitation":"Tailleur, I., Mamet, B.L., and Dutro, J., 1973, Revised age and structural interpretations of Nuka Formation at Nuka Ridge, northwestern Alaska: Geologic notes: American Association of Petroleum Geologists Bulletin, v. 57, no. 7, p. 1348-1352, https://doi.org/10.1306/83D90EBC-16C7-11D7-8645000102C1865D.","productDescription":"5 p.","startPage":"1348","endPage":"1352","costCenters":[{"id":499,"text":"Office of National Petroleum Reserve in Alaska","active":false,"usgs":true}],"links":[{"id":265702,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Nuka Ridge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -159.81888947497808,\n              68.72624503225839\n            ],\n            [\n              -159.81888947497808,\n              68.23007744142308\n            ],\n            [\n              -158.38069909853127,\n              68.23007744142308\n            ],\n            [\n              -158.38069909853127,\n              68.72624503225839\n            ],\n            [\n              -159.81888947497808,\n              68.72624503225839\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"57","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f53710e4b0114312ab0241","contributors":{"authors":[{"text":"Tailleur, I.L.","contributorId":59027,"corporation":false,"usgs":true,"family":"Tailleur","given":"I.L.","email":"","affiliations":[],"preferred":false,"id":471940,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mamet, B. L.","contributorId":12886,"corporation":false,"usgs":true,"family":"Mamet","given":"B.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":471939,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dutro, J.T. Jr.","contributorId":8432,"corporation":false,"usgs":true,"family":"Dutro","given":"J.T.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":471941,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70038339,"text":"70038339 - 1973 - Hydrogeologic data for the Quinnipiac River basin, Connecticut","interactions":[{"subject":{"id":49321,"text":"ofr77662 - 1977 - Water resources inventory of Connecticut; Part 8, Quinnipiac River basin, Connecticut","indexId":"ofr77662","publicationYear":"1977","noYear":false,"title":"Water resources inventory of Connecticut; Part 8, Quinnipiac River basin, Connecticut"},"predicate":"SUPERSEDED_BY","object":{"id":70038339,"text":"70038339 - 1973 - Hydrogeologic data for the Quinnipiac River basin, Connecticut","indexId":"70038339","publicationYear":"1973","noYear":false,"title":"Hydrogeologic data for the Quinnipiac River basin, Connecticut"},"id":1}],"lastModifiedDate":"2014-04-09T14:19:40","indexId":"70038339","displayToPublicDate":"2012-05-01T09:45:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":108,"text":"Connecticut Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"26","title":"Hydrogeologic data for the Quinnipiac River basin, Connecticut","docAbstract":"This report contains geologic, ground-water, and quality-of-water data collected for the ground-water part of a water-resources inventory of the Quinnipiac River basin, Connecticut. The study was made by the U.S. Geological Survey in fiscal cooperation with the Connecticut Department of Environmental Protection. Collection sites for data used in the study are shown in plate A. A companion report interprets the ground-water, quality-of-water, and surfacewater data collected for the study (Connecticut Water Resources Bulletin No. 27, in parparation).\nThe Quinnipiac River basin~ as used in this report~ is a 360-square-mile\narea in south-central Connecticut drained principally by the Quinnipiac River\nand its tributaries and several smaller streams~ which drain directly to Long\nIsland Sound. (See front cover and plate A.) The study area includes all or\nparts of the following towns: Ansonia, Berlin, Bethany, Branford, Bristol,\nCheshire, Derby, Durham, East Haven, Farmington, Guilford, Hamden, Meriden,\nMiddlefield, Middletown, Milford, New Britain, New Haven, North Branford, North\nHaven, Orange, Plainville, Prospect, Southington, Wallingford, West Haven, Wolcott,\nand Woodbridge.\nData collected for this investigation from July 1969 to December 1971 were\nsupplemented by data collected during previous investigations. This report includes\nsome records of wells and test holes published in Connecticut Water\nResources Bulletin No. 5 and also includes some records used but not published\nin Connecticut Water Resources Bulletin No. 14.\nTable 5 contains old but previously unpublished analyses of water from wells\nin New Haven collected primarily from 1938 to 1949. Ownership of the sampled\nwells, as shown in table 1 and table 5, was determined at the time of the original\ninventory, and this information may now be outdated. Many of these wells\nhave been destroyed since they were last sampled and others, though still in\nexistence, are no longer in use.","language":"English","publisher":"Connecticut Department of Environmental Protection","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Department of Environmental Protection","usgsCitation":"Mazzaferro, D.L., 1973, Hydrogeologic data for the Quinnipiac River basin, Connecticut: Connecticut Water Resources Bulletin 26, Report: 54 p.; 1 Plate: 33.36 x 54.39 inches.","productDescription":"Report: 54 p.; 1 Plate: 33.36 x 54.39 inches","numberOfPages":"58","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":258817,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0026/report.pdf","size":"2919","linkFileType":{"id":1,"text":"pdf"}},{"id":258818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0026/report-thumb.jpg"},{"id":286038,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038339/plate-a.pdf"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Quinnipiac River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.083333,41.166667 ], [ -73.083333,41.708333 ], [ -72.666667,41.708333 ], [ -72.666667,41.166667 ], [ -73.083333,41.166667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a33b1e4b0c8380cd5f1b9","contributors":{"authors":[{"text":"Mazzaferro, David L.","contributorId":89539,"corporation":false,"usgs":true,"family":"Mazzaferro","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":463905,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70007399,"text":"70007399 - 1973 - Journal of Research of the U. S. Geological Survey, 1973, volume 1, issue 6","interactions":[],"lastModifiedDate":"2016-02-05T16:24:19","indexId":"70007399","displayToPublicDate":"2012-02-07T08:03:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Journal of Research of the U. S. Geological Survey, 1973, volume 1, issue 6","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70007399","usgsCitation":"U.S. Geological Survey, 1973, Journal of Research of the U. S. Geological Survey, 1973, volume 1, issue 6, https://doi.org/10.3133/70007399.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":204665,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue6/report-thumb.jpg"},{"id":115848,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1973/vol1issue6/report.pdf","size":"16.01 MB","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4011e4b0c8380cd64a4e"}
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