{"pageNumber":"5512","pageRowStart":"137775","pageSize":"25","recordCount":165626,"records":[{"id":70047243,"text":"70047243 - 1974 - A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 3: Lake Walcott-Bonanza Lake area","interactions":[],"lastModifiedDate":"2013-07-26T10:18:59","indexId":"70047243","displayToPublicDate":"2013-01-01T10:07:00","publicationYear":"1974","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":"38","title":"A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 3: Lake Walcott-Bonanza Lake area","docAbstract":"Direct-current resistivity soundings and exploratory drilling suggest that the basalt of the Snake River Group is relatively thin in the area along the Snake River that is topographically suitable for pumping large quantities of ground water in exchange for surface water. The formations underlying the Snake River Group appear to have low permeability and probably would not yield large amounts of water. Previous studies have indicated that the southern edge of the Snake Plain aquifer extended to the Snake River. Data presented in this report implies that, in general, the southern boundary should, in fact, be several miles north of the river.","language":"English","publisher":"Idaho Department of Water Resources","publisherLocation":"Boise City, ID","collaboration":"Prepared by the United States Geological Survey in cooperation with the Idaho Department of Water Resources","usgsCitation":"Crosthwaite, E., 1974, A progress report on results of test drilling and ground-water investigations of the Snake Plain aquifer, southeastern Idaho: Part 3: Lake Walcott-Bonanza Lake area: Water Information Bulletin 38, iv, 25 p.","productDescription":"iv, 25 p.","numberOfPages":"30","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":275429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047243.png"},{"id":275426,"type":{"id":11,"text":"Document"},"url":"https://www.idwr.idaho.gov/WaterInformation/Publications/wib/wib38-lake_walcott-bonanza_lake.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":"51f39a62e4b0a32220222f56","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":481486,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047240,"text":"70047240 - 1974 - Application of digital modeling to the prediction of radioisotope migration in ground water","interactions":[],"lastModifiedDate":"2013-07-26T10:00:20","indexId":"70047240","displayToPublicDate":"2013-01-01T09:24:00","publicationYear":"1974","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Application of digital modeling to the prediction of radioisotope migration in ground water","docAbstract":"Recently developed numerical techniques have been adapted to the solution of transient radioactive solute migration problems in groundwater.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Isotope Techniques in Groundwater Hydrology","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"IAEA","usgsCitation":"Robertson, J., 1974, Application of digital modeling to the prediction of radioisotope migration in ground water, <i>in</i> Isotope Techniques in Groundwater Hydrology, v. 2, p. 451-478.","productDescription":"28 p.","startPage":"451","endPage":"478","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":275424,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":275423,"type":{"id":11,"text":"Document"},"url":"https://www-naweb.iaea.org/napc/ih/documents/IAEA%20Symposia/W-04%20Proc%20Symposium%201974%20Vol%20II%20Isotope%20Techniques%20in%20gw%20hydrology%201974.pdf"}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,41.99 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,41.99 ], [ -117.24,41.99 ] ] ] } } ] }","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51f39a64e4b0a32220222f69","contributors":{"authors":[{"text":"Robertson, J.B.","contributorId":85173,"corporation":false,"usgs":true,"family":"Robertson","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":481484,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70045954,"text":"70045954 - 1974 - Quality of water in the Red River alluvial aquifer, Shreveport, to the mouth of the Black River, Louisiana","interactions":[],"lastModifiedDate":"2013-07-08T10:48:55","indexId":"70045954","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Quality of water in the Red River alluvial aquifer, Shreveport, to the mouth of the Black River, Louisiana","docAbstract":"Chemical analyses of water samples from 296 wells in the Red River alluvial aquifer indicate that the ground water in the valley is generally hard (more than 120 milligrams per liter) and has a high iron concentration (greater than 6,000 micrograms per liter). The predominant ions found in the water were calcium and bicarbonate. However, in places in the vicinity of Natchitoches, saline water, probably from underlying formations, has infiltrated the aquifer and sodium and chloride are the principal constituents.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70045954","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the  U.S. Army Corps of Engineers","usgsCitation":"Ludwig, A.H., 1974, Quality of water in the Red River alluvial aquifer, Shreveport, to the mouth of the Black River, Louisiana: Open-File Report, ii, 7, A3, B3, C3, D2, E2, F2, G4, H4, I4, J2 p., https://doi.org/10.3133/70045954.","productDescription":"ii, 7, A3, B3, C3, D2, E2, F2, G4, H4, I4, J2 p.","startPage":"1","endPage":"J2","numberOfPages":"67","costCenters":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"links":[{"id":272263,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70045954/report-thumb.jpg"},{"id":274512,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-1.pdf"},{"id":274511,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70045954/report.pdf"},{"id":274513,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-2.pdf"},{"id":274514,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-3.pdf"},{"id":274515,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-4.pdf"},{"id":274516,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-5.pdf"},{"id":274517,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70045954/plate-6.pdf"}],"country":"United States","state":"Louisiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.0,28.93 ], [ -94.0,33.0 ], [ -88.82,33.0 ], [ -88.82,28.93 ], [ -94.0,28.93 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51dbdf73e4b0f81004b77da2","contributors":{"authors":[{"text":"Ludwig, A. H.","contributorId":63007,"corporation":false,"usgs":true,"family":"Ludwig","given":"A.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":478598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046284,"text":"70046284 - 1974 - Geology and ground-water resources of Gordon, Whitfield, and Murray Counties, Georgia","interactions":[{"subject":{"id":46059,"text":"ofr7179 - 1971 - Maps of Gordon, Whitfield, and Murray counties, Georgia, showing geology and location of wells and springs","indexId":"ofr7179","publicationYear":"1971","noYear":false,"title":"Maps of Gordon, Whitfield, and Murray counties, Georgia, showing geology and location of wells and springs"},"predicate":"SUPERSEDED_BY","object":{"id":70046284,"text":"70046284 - 1974 - Geology and ground-water resources of Gordon, Whitfield, and Murray Counties, Georgia","indexId":"70046284","publicationYear":"1974","noYear":false,"title":"Geology and ground-water resources of Gordon, Whitfield, and Murray Counties, 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,{"id":70042677,"text":"70042677 - 1974 - Analyses and economic potential of monazite in Liberia","interactions":[{"subject":{"id":15712,"text":"ofr69234 - 1969 - Preliminary spectrographic analyses of monazite from western Liberia","indexId":"ofr69234","publicationYear":"1969","noYear":false,"title":"Preliminary spectrographic analyses of monazite from western Liberia"},"predicate":"SUPERSEDED_BY","object":{"id":70042677,"text":"70042677 - 1974 - Analyses and economic potential of monazite in Liberia","indexId":"70042677","publicationYear":"1974","noYear":false,"title":"Analyses and economic potential of monazite in Liberia"},"id":1}],"lastModifiedDate":"2013-01-17T10:17:43","indexId":"70042677","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1974","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":"Analyses and economic potential of monazite in Liberia","docAbstract":"Eleven monazite samples from Liberia, including seven from beach sands, were analyzed by the X-ray fluorescence method. The monazite samples, containing only one-half percent impurities, were obtained by use of a hot Clerici-solution procedure for purification which was devised by the author. The percentage of the rare-earth elements in Liberian monazite concentrates does not differ greatly from that of monazite sands elsewhere in the world. The average of the 11 samples shows less praseodymium and neodymium than Russian and American monazites, but more cerium. Liberian coastal sands apparently contain sufficient reserves of monazite (and other heavy minerals of commerce) to encourage mining. A feasibility study of production and marketing of monazite from Liberian beach sands is recommended.","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":"Rosenblum, S., 1974, Analyses and economic potential of monazite in Liberia: Journal of Research of the U.S. Geological Survey, v. 2, no. 6, p. 689-692.","productDescription":"4 p.","startPage":"689","endPage":"692","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":265794,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265795,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue6/report.pdf"}],"country":"Liberia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -11.4742,4.3154 ], [ -11.4742,8.5 ], [ -7.3693,8.5 ], [ -7.3693,4.3154 ], [ -11.4742,4.3154 ] ] ] } } ] }","volume":"2","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f92b79e4b0727905955f3b","contributors":{"authors":[{"text":"Rosenblum, Sam","contributorId":60620,"corporation":false,"usgs":true,"family":"Rosenblum","given":"Sam","email":"","affiliations":[],"preferred":false,"id":472037,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042518,"text":"70042518 - 1974 - Structural framework of United States Atlantic outer continental shelf north of Cape Hatteras","interactions":[{"subject":{"id":17561,"text":"ofr73181 - 1973 - A preliminary report on U.S. Geological Survey geophysical studies of the northeastern United States Outer Continental Shelf","indexId":"ofr73181","publicationYear":"1973","noYear":false,"title":"A preliminary report on U.S. Geological Survey geophysical studies of the northeastern United States Outer Continental Shelf"},"predicate":"SUPERSEDED_BY","object":{"id":70042518,"text":"70042518 - 1974 - Structural framework of United States Atlantic outer continental shelf north of Cape Hatteras","indexId":"70042518","publicationYear":"1974","noYear":false,"title":"Structural framework of United States Atlantic outer continental shelf north of Cape Hatteras"},"id":1}],"lastModifiedDate":"2023-01-25T16:55:54.317347","indexId":"70042518","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1974","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":"Structural framework of United States Atlantic outer continental shelf north of Cape Hatteras","docAbstract":"<p><span>To assess the area’s hydrocarbon potential, regional geologic and geophysical studies are being conducted by the U.S. Geological Survey to determine the structural framework of the United States Atlantic outer continental shelf (AOCS) north of Cape Hatteras. Preliminary interpretations of geophysical data suggest that the buried ridge under the eastern edge of the AOCS in the Baltimore Canyon trough area is deeper and farther west than previously suspected. Although it is not observed under the seaward extension of the Cape Fear arch, this ridge can be traced from the south side of the Baltimore Canyon trough northeastward toward the eastern edge of the Georges Bank trough. In the Baltimore Canyon trough area, the ridge seems to be fault controlled and to form the eastern edge of a Mesozoic depocenter in which approximately 12 km of relatively undisturbed post-Paleozoic sediments accumulated. Below a depth of 6 km, rocks previously considered to be crystalline basement instead may be carbonate and/or evaporite sequences of Jurassic age or older which overlie an even deeper crystalline basement. More than 8 km of sediments are present beneath the continental shelf on Georges Bank. The preliminary regional geophysical studies indicate that thick marine sedimentary sections and geologic structures favorable for the accumulation of petroleum apparently exist under the AOCS off the northeastern part of the United States.</span></p>","language":"English","publisher":"American Association of Petroleum Geologists","publisherLocation":"Tulsa, OK","doi":"10.1306/83D91641-16C7-11D7-8645000102C1865D","usgsCitation":"Mattick, R., Foote, R.Q., Weaver, N.L., and Grim, M.S., 1974, Structural framework of United States Atlantic outer continental shelf north of Cape Hatteras: American Association of Petroleum Geologists Bulletin, v. 58, no. 6, p. 1179-1190, https://doi.org/10.1306/83D91641-16C7-11D7-8645000102C1865D.","productDescription":"12 p.","startPage":"1179","endPage":"1190","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":265528,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Atlantic outer continental shelf","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.0,25.0 ], [ -84.0,47.5 ], [ -60.0,47.5 ], [ -60.0,25.0 ], [ -84.0,25.0 ] ] ] } } ] }","volume":"58","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f7da2fe4b0faa3ef21ec50","contributors":{"authors":[{"text":"Mattick, R.E.","contributorId":85162,"corporation":false,"usgs":true,"family":"Mattick","given":"R.E.","affiliations":[],"preferred":false,"id":471683,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foote, R. Q.","contributorId":6871,"corporation":false,"usgs":true,"family":"Foote","given":"R.","email":"","middleInitial":"Q.","affiliations":[],"preferred":false,"id":471682,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weaver, N. L.","contributorId":86359,"corporation":false,"usgs":true,"family":"Weaver","given":"N.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":471684,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Grim, M. S.","contributorId":102884,"corporation":false,"usgs":true,"family":"Grim","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":471685,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70043691,"text":"70043691 - 1974 - Hydrologic Data from the Piceance Basin, Colorado","interactions":[{"subject":{"id":23031,"text":"ofr7371 - 1973 - Selected hydrologic data from the Piceance Basin, Colorado","indexId":"ofr7371","publicationYear":"1973","noYear":false,"title":"Selected hydrologic data from the Piceance Basin, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70043691,"text":"70043691 - 1974 - Hydrologic Data from the Piceance Basin, Colorado","indexId":"70043691","publicationYear":"1974","noYear":false,"title":"Hydrologic Data from the Piceance Basin, Colorado"},"id":1}],"lastModifiedDate":"2018-01-08T20:11:26","indexId":"70043691","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":245,"text":"Colorado Division of Water Resources Basic-Data Release","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"31","title":"Hydrologic Data from the Piceance Basin, Colorado","docAbstract":"<p>No abstract available.<br data-mce-bogus=\"1\"></p>","language":"English","publisher":"Colorado Department of Natural Resources","publisherLocation":"Denver, CO","collaboration":"Prepared by the U.S. Geological Survey, in cooperation with the Colorado Department of Natural Resources","usgsCitation":"Ficke, J.F., Weeks, J., and Welder, F.A., 1974, Hydrologic Data from the Piceance Basin, Colorado: Colorado Division of Water Resources Basic-Data Release 31, vii, 246 p.","productDescription":"vii, 246 p.","costCenters":[{"id":191,"text":"Colorado Water Science Center","active":true,"usgs":true}],"links":[{"id":267620,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0,37.0 ], [ -109.0,41.0 ], [ -102.0,41.0 ], [ -102.0,37.0 ], [ -109.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51235b83e4b0c9f2bfcf8d43","contributors":{"authors":[{"text":"Ficke, John F.","contributorId":86750,"corporation":false,"usgs":true,"family":"Ficke","given":"John","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":474089,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weeks, John B.","contributorId":36123,"corporation":false,"usgs":true,"family":"Weeks","given":"John B.","affiliations":[],"preferred":false,"id":474088,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Welder, Frank A.","contributorId":32173,"corporation":false,"usgs":true,"family":"Welder","given":"Frank","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":474087,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70043037,"text":"70043037 - 1974 - Apollo 11 voice transcript pertaining to the geology of the landing site","interactions":[{"subject":{"id":15835,"text":"ofr70287 - 1970 - Geologic transcript from Apollo 11 mission","indexId":"ofr70287","publicationYear":"1970","noYear":false,"title":"Geologic transcript from Apollo 11 mission"},"predicate":"SUPERSEDED_BY","object":{"id":70043037,"text":"70043037 - 1974 - Apollo 11 voice transcript pertaining to the geology of the landing site","indexId":"70043037","publicationYear":"1974","noYear":false,"title":"Apollo 11 voice transcript pertaining to the geology of the landing site"},"id":1}],"lastModifiedDate":"2013-01-31T13:00:29","indexId":"70043037","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":360,"text":"Final Report","active":false,"publicationSubtype":{"id":6}},"title":"Apollo 11 voice transcript pertaining to the geology of the landing site","docAbstract":"On July 20, 1969, America's Eagle touched down in southwestern Mare Tranquillitatis beginning man's firsthand exploration of the moon. This document is an edited record of the conversations between astronauts Neil Armstrong and Edwin \"Buzz\" Aldrin, Jr., at Tranquility Base, and Bruce McCandless at Mission Control in Houston during the approximately 22 hours spent on the lunar surface. It includes additional commentary during their return to Earth. It is a condensation hopefully of all the verbal data having geological significance. All discussions and observations documenting the lunar landscape, its geologic characteristics, the rocks and soils collected, and the photographic record are retained along with supplementary remarks essential to the continuity of events during the mission. We have deleted the words of mechanical housekeeping and engineering data, attempting not to lose the personal and philosophical aspects of this intensely human experience. The sources of this verbal transcript are the complete audio tapes recorded during the mission and the Technical Air-to-Ground Voice Transcription published by NASA. The voice record is listed chronologically given in days, hours, minutes, and seconds. These are the Ground Elapsed Times (GET) after launch from Kennedy Space Center which was 9:32 a.m. EDT on July 16, 1969. Figure 1 shows the vicinity of the landing site that was described, sampled, and photographed by the Apollo 11 crewmen.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043037","usgsCitation":"Bailey, N.G., and Ulrich, G., 1974, Apollo 11 voice transcript pertaining to the geology of the landing site: Final Report, 42 p., https://doi.org/10.3133/70043037.","productDescription":"42 p.","numberOfPages":"45","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":266844,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":266843,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a11/Apollo11VoiceTranscript-Geology.pdf"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"510ba075e4b0947afa3c8568","contributors":{"authors":[{"text":"Bailey, N. G.","contributorId":14408,"corporation":false,"usgs":true,"family":"Bailey","given":"N.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":472815,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ulrich, G. E.","contributorId":88737,"corporation":false,"usgs":true,"family":"Ulrich","given":"G. E.","affiliations":[],"preferred":false,"id":472816,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043778,"text":"70043778 - 1974 - Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah","interactions":[{"subject":{"id":16125,"text":"ofr74137 - 1974 - Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver counties, Utah","indexId":"ofr74137","publicationYear":"1974","noYear":false,"title":"Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043778,"text":"70043778 - 1974 - Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah","indexId":"70043778","publicationYear":"1974","noYear":false,"title":"Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah"},"id":1}],"lastModifiedDate":"2016-12-10T15:21:08","indexId":"70043778","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"47","title":"Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah","docAbstract":"The Wah Wah Valley drainage basin is an area of about 600 square miles (1,550 km<sup>2</sup>) in Millard and Beaver Counties in southwestern Utah. Surface-water supplies of the area are negligible--total runoff averages about 7,800 acre-feet (9.62 hm<sup>3</sup>) annually, all streams are ephemeral or intermittent, and surface storage is negligible. Evaporation and transpiration within the basin consume more than 97 percent of total annual precipitation. There is no surface outflow.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources, Division of Water Rights","usgsCitation":"Stephens, J.C., 1974, Hydrologic reconnaissance of the Wah Wah Valley drainage basin, Millard and Beaver Counties, Utah: Technical Publication 47, v, 53 p.","productDescription":"v, 53 p.","numberOfPages":"60","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267803,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331871,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-220"},{"id":267802,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w9200099.pdf"}],"country":"United States","state":"Utah","county":"Beaver County, Millard County","otherGeospatial":"Wah Wah Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.97766113281249,\n              38.14751758025121\n            ],\n            [\n              -113.97766113281249,\n              38.886757140695906\n            ],\n            [\n              -113.2470703125,\n              38.886757140695906\n            ],\n            [\n              -113.2470703125,\n              38.14751758025121\n            ],\n            [\n              -113.97766113281249,\n              38.14751758025121\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5124ad45e4b0b6328103b44e","contributors":{"authors":[{"text":"Stephens, Jerry C.","contributorId":81493,"corporation":false,"usgs":true,"family":"Stephens","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":474227,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042609,"text":"70042609 - 1974 - Geology and mineral deposits of Churchill County, Nevada","interactions":[{"subject":{"id":16546,"text":"ofr68329 - 1968 - Geology and mineral deposits of Churchill County, Nevada","indexId":"ofr68329","publicationYear":"1968","noYear":false,"title":"Geology and mineral deposits of Churchill County, Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":70042609,"text":"70042609 - 1974 - Geology and mineral deposits of Churchill County, Nevada","indexId":"70042609","publicationYear":"1974","noYear":false,"title":"Geology and mineral deposits of Churchill County, Nevada"},"id":1}],"lastModifiedDate":"2019-07-10T15:07:26","indexId":"70042609","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":268,"text":"NBMG Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"83","title":"Geology and mineral deposits of Churchill County, Nevada","docAbstract":"Churchill County, in west-central Nevada, is an area of varied topography and geology that has had a rather small total mineral production. The western part of the county is dominated by the broad low valley of the Carson Sink, which is underlain by deposits of Lake Lahontan. The bordering mountain ranges to the west and south are of low relief and underlain largely by Tertiary volcanic and sedimentary units. Pre-Tertiary rocks are extensively exposed east of the Carson Sink in the Stillwater Range, Clan Alpine Mountains, Augusta Mountains, and New Pass Mountains. The eastern valleys are underlain by Quaternary alluvial and lacustrine deposits contemporaneous with the western deposits of Lake Lahontan. The eastern mountain ranges are more rugged than the western ranges and have higher relief; the eastern valleys are generally narrower.","language":"English","publisher":"Nevada Bureau of Mines and Geology","publisherLocation":"Reno, NV","usgsCitation":"Willden, R., and Speed, R.C., 1974, Geology and mineral deposits of Churchill County, Nevada: NBMG Bulletin 83, vii, 95 p.","productDescription":"vii, 95 p.","startPage":"i","endPage":"95","numberOfPages":"102","costCenters":[{"id":234,"text":"Earthquake Hazards Program","active":true,"usgs":true},{"id":300,"text":"Geologic Hazards Science Center","active":true,"usgs":true}],"links":[{"id":265675,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265674,"type":{"id":1,"text":"Abstract"},"url":"https://www.nbmg.unr.edu/sales/davescans/bull83.pdf"}],"country":"United States","state":"Nevada","county":"Churchill County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.2261,39.0733 ], [ -119.2261,40.0026 ], [ -117.4613,40.0026 ], [ -117.4613,39.0733 ], [ -119.2261,39.0733 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f53707e4b0114312ab0216","contributors":{"authors":[{"text":"Willden, Ronald","contributorId":107368,"corporation":false,"usgs":true,"family":"Willden","given":"Ronald","affiliations":[],"preferred":false,"id":471925,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Speed, Robert C.","contributorId":69998,"corporation":false,"usgs":true,"family":"Speed","given":"Robert","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":471924,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038681,"text":"wdrCA7312 - 1974 - Water resources data for California, 1973; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley","interactions":[],"lastModifiedDate":"2012-06-13T01:01:48","indexId":"wdrCA7312","displayToPublicDate":"2012-06-04T10:44:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CA-73-1-2","title":"Water resources data for California, 1973; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley","docAbstract":"Surface-water records for the 1973 water year for California, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report, Records for a few pertinent gaging stations in bordering States also are included, The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Lee R. Peterson, district chief. These data represent that portion of the National Water Data System collected by the Geological Survey and cooperating State and Federal agencies in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrCA7312","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for California, 1973; Part 1: Surface water records; Volume 2: Northern Great Basin and Central Valley: U.S. Geological Survey Water Data Report CA-73-1-2, xiv, 523 p., https://doi.org/10.3133/wdrCA7312.","productDescription":"xiv, 523 p.","startPage":"511","endPage":"1033","costCenters":[],"links":[{"id":257515,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdr_CA_73_1_2.jpg"},{"id":257492,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1973/ca-73/WDR-1973-vol2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc957e4b08c986b32cce3","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":535194,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70038245,"text":"70038245 - 1974 - Water resources inventory of Connecticut Part 5: lower Housatonic River basin","interactions":[],"lastModifiedDate":"2014-06-26T15:00:35","indexId":"70038245","displayToPublicDate":"2012-04-22T14:28:00","publicationYear":"1974","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":"19","title":"Water resources inventory of Connecticut Part 5: lower Housatonic River basin","docAbstract":"<p>The 557 square miles of the lower Housatonic River basin in western Connecticut include the basins of two major tributaries, the Pomperaug and Naugatuck Rivers. Nearly all water is derived from precipitation, which averaged 47 inches per year during 1931-60, In this period an additional 570 billion gallons of water per year entered the basin in the main stem of the Housatonic River at Lake Lillinonah, and some water was imported by water-supply systems from outside the basin. Almost half the precipitation--21.6 inches--was lost from the basin by evapotranspiration. Except for small amounts exported, the remainder discharged as runoff and underflow into Long Island Sound.  </p>\n<br/>\n<p>Variations in streamflow at 6 long-term continuous-record gaging stations are summarized in standardized graphs and tables that can be used to estimate streamflow characteristics at other sites. For example, mean flow and two low-flow characteristics, the 7-day annual minimum flow for 2-year and 10-year recurrence intervals, have been determined for many partial-record stations throughout the basin.</p>\n<br/>\n<p>Of the 37 principal lakes, ponds, and reservoirs in the basin, 6 have usable storage of more than 1 billion gallons. The “maximum safe draft rate” (described in: “Storage of Water in Lakes and Reservoirs”) of the largest of these, Thomaston Reservoir near Thomaston, is 75.6 million gallons per day for the 10-year and 20-year recurrence intervals of annual lowest mean flow.</p>\n<br/>\n<p>Floods have occurred during every month, at one time or another. The two greatest floods on the Naugatuck River in historical time occurred 2 months apart in 1955. The larger, in August, had a peak of 106,000 cfs (cubic feet per second) at Beacon Falls. Since then, the likelihood of major floods has been considerably reduced by a program of flood control in the basin.</p>\n<br/>\n<p>Water can be obtained from three aquifers under-lying the basin-stratified drift, till, and bedrock. Stratified drift covers about 16 percent of the basin, mostly in valleys and lowlands, and its saturated part generally ranges in thickness from 10 feet in small valleys to 200 feet in the Housatonic River valley. Its transmissivity ranges from 0 to 47,000 ft<sup>2</sup>/day (feet shared per day). Till, deposited directly by glacial ice, forms a widespread but discontinuous mantle over bedrock in most upland areas and extends beneath stratified drift in lowlands; it ranges in thickness from 0 to 200 feet. The median value of 31 published determinations of hydraulic conductivity of till in southern New England is 0.67 ft/day and ranges from 0.013 to 29 ft/day. Crystalline bedrock underlies most of the basin and is composed principally of granite, gneiss, and schist. Sedimentary volcanic bedrock underlies only the Pomperaug River basin. Regardless of rock type, water is obtained mostly from fractures. </p>\n<br/>\n<p>Streambed deposits are significant features of the hydrogeologic system because they affect the amount of water from streams and lakes that can be induced to infiltrate aquifers. Based on field tests, characteristic values of vertical hydraulic conductivity of streambed deposits are 0.40 ft/day for fine-grained deposits and 14 ft/day for gravelly deposits.</p>\n<br/>\n<p>Ground-water supplies generally range in yield from several millions of gallons per day from large well fields to 1 gpm (gallons per minute) from single wells. Large supplies, with yields of 100 gpm or more from individual wells, are most commonly obtained from stratified drift. Yields to be expected from screened wells tapping this aquifer can be calculated by use of a series of graphs in conjunction with estimates of transmissivity and aquifer thickness.</p>\n<br/>\n<p>The yields of 14 principal ground-water reservoirs are estimated from aquifer characteristics and also from the amount of water that can be obtained from aquifer storage, from interception or runoff, and from infiltration of streamflow at low-flow conditions, using a hypothetical well-field arrangement for each reservoir. It is assumed that induced infiltration is restricted to an amount equal to the 7-day annual minimum stream-flow for a 2-year recurrence interval. Yields range from 1.4 to 15 mgd (million gallons per day) during periods of no recharge, and from 2.0 to 17 mgd during recharge periods.</p>\n<br/>\n<p>Small to moderate water supplies can be obtained from any of the aquifers under suitable conditions. For example, data from 294 wells in the basin indicate that yields of a few gallons per minute can be obtained from bedrock at most sites. The likelihood of obtaining an adequate domestic supply is slightly greater in granite than in schist and also is greater where the overburden is stratified drift rather than till.</p>\n<br/>\n<p>Chemical analyses of precipitation samples collected monthly from five stations in the basin during a 9-month period in 1966 show that rainfall is acidic and that sulfate is the dominant anion, probably because of industrial fumes and smoke within and near the basin.</p>\n<br/>\n<p>Where unaffected by man’s activities, water in the basin is generally low in dissolved-solids concentration, is of the calcium magnesium bicarbonate type, and is soft to moderately hard. In general, streamflow is less mineralized than ground water, particularly when it consists largely of direct runoff. However, streamflow becomes more highly mineralized during low-flow conditions, when most of it consists of more highly mineralized water discharged from aquifers. The median value of dissolved-solids concentration of water at 22 stream sites was 51 mg/1 (milligrams per liter) during high flow, and 68 mg/1 during low flow within the study period. Iron and manganese occur naturally in objectionable concentrations in parts of the basin, particularly in streams draining swamps and in water from bedrock containing iron and manganese-bearing minerals.</p>\n<br/>\n<p>Man’s activities have degraded the quality of water in streams in much of the basin, except in the Pomperaug subbasin. In the Naugatuck River basin, the degradation in quality is shown by wide and erratic changes in dissolved-solids concentration, excessive amounts of certain trace elements, a low dissolved oxygen content, and abnormally high temperatures. Ground water is degraded principally by induced infiltration of stream water containing chemical wastes, by wastes stored on the ground and by effluents from septic tanks.</p>\n<br/>\n<p>Below its confluence with the Naugatuck River, much of the Housatonic River and adjoining marshes, wetlands, and aquifers contain salt water. Measurements of specific conductance during low-flow conditions in 1969 indicate that the dissolved-solids concentration of water in the estuary ranged from 210 mg/1 near Twomile Island to 20,000 mg/1 near Long Island Sound.</p>\n<br/>\n<p>The quantity and quality of water in the basin are satisfactory for a wide variety of uses, and, with suitable treatment, the water may be used for most purposes. In 1967, the total amount of water used in the basin was about 194 billion gallons. About 90 percent of this was used for industrial purposes, and 95 percent of the industrial water was obtained from surface-water sources. In the same year, 17 municipal and private water-supply systems supplied water of satisfactory quality to about three-fourths of the population.</p>","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":"Wilson, W.E., Burke, E.L., and Thomas, C.E., 1974, Water resources inventory of Connecticut Part 5: lower Housatonic River basin: Connecticut Water Resources Bulletin 19, Report: viii, 79 p.; 6 Plates: 28.66 x 40.55 inches and smaller.","productDescription":"Report: viii, 79 p.; 6 Plates: 28.66 x 40.55 inches and smaller","numberOfPages":"85","costCenters":[],"links":[{"id":258805,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0019/report.pdf","size":"29327","linkFileType":{"id":1,"text":"pdf"}},{"id":258806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0019/report-thumb.jpg"},{"id":285980,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-a.pdf"},{"id":285981,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-b.pdf"},{"id":285982,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-c-1.pdf"},{"id":285983,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-c-2.pdf"},{"id":285984,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-c-3.pdf"},{"id":285985,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70038245/plate-d.pdf"}],"scale":"125000","country":"United States","state":"Connecticut","otherGeospatial":"Housatonic River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.333333,41.125 ], [ -73.333333,42.0 ], [ -72.9,42.0 ], [ -72.9,41.125 ], [ -73.333333,41.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb7be4b08c986b32d693","contributors":{"authors":[{"text":"Wilson, William E.","contributorId":46478,"corporation":false,"usgs":true,"family":"Wilson","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463728,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burke, Edward L.","contributorId":38398,"corporation":false,"usgs":true,"family":"Burke","given":"Edward","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":463727,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Chester E. 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,{"id":70007405,"text":"70007405 - 1974 - Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 6","interactions":[],"lastModifiedDate":"2021-09-15T12:15:02.769009","indexId":"70007405","displayToPublicDate":"2012-02-07T08:11:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 6","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70007405","usgsCitation":"U.S. Geological Survey, 1974, Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 6, https://doi.org/10.3133/70007405.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":204669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue6/report-thumb.jpg"},{"id":115854,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue6/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4015e4b0c8380cd64a72"}
,{"id":70007404,"text":"70007404 - 1974 - Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 5","interactions":[],"lastModifiedDate":"2022-04-20T19:40:32.129869","indexId":"70007404","displayToPublicDate":"2012-02-07T08:10:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 5","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70007404","usgsCitation":"U.S. Geological Survey, 1974, Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 5, 132 p., https://doi.org/10.3133/70007404.","productDescription":"132 p.","costCenters":[],"links":[{"id":115853,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue5/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399229,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31460.htm"},{"id":399228,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31459.htm"},{"id":399227,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31458.htm"},{"id":399226,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31457.htm"},{"id":399225,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31456.htm"},{"id":399224,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31455.htm"},{"id":399223,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31454.htm"},{"id":399222,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31453.htm"},{"id":399221,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31452.htm"},{"id":399220,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31451.htm"},{"id":204668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue5/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4014e4b0c8380cd64a69"}
,{"id":70007403,"text":"70007403 - 1974 - Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 4","interactions":[],"lastModifiedDate":"2022-04-20T21:46:19.64169","indexId":"70007403","displayToPublicDate":"2012-02-07T08:08:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 4","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70007403","usgsCitation":"U.S. Geological Survey, 1974, Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 4, 132 p., https://doi.org/10.3133/70007403.","productDescription":"132 p.","costCenters":[],"links":[{"id":399332,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93318.htm"},{"id":399217,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31447.htm"},{"id":115852,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue4/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":204667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue4/report-thumb.jpg"},{"id":399218,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31448.htm"},{"id":399219,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31449.htm"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4014e4b0c8380cd64a63"}
,{"id":70007402,"text":"70007402 - 1974 - Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 3","interactions":[],"lastModifiedDate":"2022-04-20T21:45:32.912549","indexId":"70007402","displayToPublicDate":"2012-02-07T08:07:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 3","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70007402","usgsCitation":"U.S. Geological Survey, 1974, Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 3, 132 p., https://doi.org/10.3133/70007402.","productDescription":"132 p.","costCenters":[],"links":[{"id":399331,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93320.htm"},{"id":399215,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31445.htm"},{"id":399214,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31444.htm"},{"id":204666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue3/report-thumb.jpg"},{"id":399213,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31443.htm"},{"id":399216,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31446.htm"},{"id":115851,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue3/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4013e4b0c8380cd64a5d"}
,{"id":70007401,"text":"70007401 - 1974 - Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 2","interactions":[],"lastModifiedDate":"2022-04-20T21:44:42.220668","indexId":"70007401","displayToPublicDate":"2012-02-07T08:06:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 2","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70007401","usgsCitation":"U.S. Geological Survey, 1974, Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 2, 132 p., https://doi.org/10.3133/70007401.","productDescription":"132 p.","costCenters":[],"links":[{"id":399330,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93319.htm"},{"id":204664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue2/report-thumb.jpg"},{"id":399208,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31438.htm"},{"id":399209,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31439.htm"},{"id":399210,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31440.htm"},{"id":399211,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31441.htm"},{"id":115850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399212,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31442.htm"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4013e4b0c8380cd64a5a"}
,{"id":70007400,"text":"70007400 - 1974 - Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 1","interactions":[],"lastModifiedDate":"2022-04-20T18:52:24.644207","indexId":"70007400","displayToPublicDate":"2012-02-07T08:04:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 1","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70007400","usgsCitation":"U.S. Geological Survey, 1974, Journal of Research of the U. S. Geological Survey, 1974, volume 2, issue 1, 138 p., https://doi.org/10.3133/70007400.","productDescription":"138 p.","costCenters":[],"links":[{"id":399207,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31432.htm"},{"id":399206,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31431.htm"},{"id":399205,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31430.htm"},{"id":399204,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31429.htm"},{"id":115849,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":204663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/journal/1974/vol2issue1/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a4012e4b0c8380cd64a57"}
,{"id":70039072,"text":"70039072 - 1974 - Tour guide: John Wesley Powell Federal Building","interactions":[],"lastModifiedDate":"2012-08-10T01:01:49","indexId":"70039072","displayToPublicDate":"2012-01-01T14:38:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"Tour guide: John Wesley Powell Federal Building","docAbstract":"Data from 5,594 samples collected from 1931 through 2006 were used to describe naturally occurring fluoride concentrations in freshwater aquifers in Louisiana. Statistical analyses were used to summarize fluoride concentrations in the aquifers.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039072","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Tour guide: John Wesley Powell Federal Building: General Information Product, 15 p., https://doi.org/10.3133/70039072.","productDescription":"15 p.","numberOfPages":"16","costCenters":[{"id":410,"text":"National Center","active":false,"usgs":true}],"links":[{"id":261291,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039072/report.pdf"},{"id":261292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039072/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Reston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.61666666666666,38.75 ], [ -77.61666666666666,39.11666666666667 ], [ -77.11666666666666,39.11666666666667 ], [ -77.11666666666666,38.75 ], [ -77.61666666666666,38.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb5a5e4b08c986b3267e6","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":535213,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039202,"text":"70039202 - 1974 - New activities at the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2017-05-19T18:47:24","indexId":"70039202","displayToPublicDate":"2012-01-01T11:41:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":362,"text":"General Information Product","active":false,"publicationSubtype":{"id":6}},"title":"New activities at the U.S. Geological Survey","docAbstract":"As the Nation's principal source of information about the configuration of the land surface, the composition and structure of the rocks at and beneath the surface, the distribution and character of its energy, mineral, and water resources, and the nature of natural geologic processes, the U. S. Geological Survey focuses its work on some of the Nation's most critical problems. As the Survey tackles new problems with new techniques, it is fully aware of the resource needs and environmental pressures of an expanding economy and growing population.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039202","usgsCitation":"McKelvey, V., 1974, New activities at the U.S. Geological Survey: General Information Product, 6 p. (11 columns), https://doi.org/10.3133/70039202.","productDescription":"6 p. (11 columns)","costCenters":[],"links":[{"id":261370,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039202/report.pdf"},{"id":261371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039202/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a654ee4b0c8380cd72b63","contributors":{"authors":[{"text":"McKelvey, Vincent E.","contributorId":106637,"corporation":false,"usgs":true,"family":"McKelvey","given":"Vincent E.","affiliations":[],"preferred":false,"id":465771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039200,"text":"70039200 - 1974 - Studying the Earth from space","interactions":[],"lastModifiedDate":"2017-05-19T18:48:11","indexId":"70039200","displayToPublicDate":"2012-01-01T11:17:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":363,"text":"General Interest Publication","active":false,"publicationSubtype":{"id":6}},"title":"Studying the Earth from space","docAbstract":"Pictures of the Earth's surface obtained from satellites are providing scientists with new tools to investigate tne Earth and its environment. A growing population and an everexpanding technology place demands on our natural resources. However, man can no longer treat his resources strictly according to immediate economic dictates; a balance must be struck between the short-term demands of technological and industrial development and the long-term effects on the environment. Intelligent development, management, and conservation of resources are goals that represent an unprecedented challenge in the acquisition and use of information.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039200","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Studying the Earth from space: General Interest Publication, 19 p., https://doi.org/10.3133/70039200.","productDescription":"19 p.","numberOfPages":"20","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":261366,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gip/70039200/report.pdf"},{"id":261367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gip/70039200/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b9ce9e4b08c986b31d515","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":535239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039544,"text":"70039544 - 1974 - Shore zone land use and land cover: Central Atlantic Regional Ecological Test Site","interactions":[],"lastModifiedDate":"2012-08-11T01:01:52","indexId":"70039544","displayToPublicDate":"2012-01-01T11:16:26","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":372,"text":"Natural Resources Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"8","title":"Shore zone land use and land cover: Central Atlantic Regional Ecological Test Site","docAbstract":"Anderson's 1972 United States Geological Survey classification in modified form was applied to the barrier-island coastline within the CARETS region. High-altitude, color-infrared photography of December, 1972, and January, 1973, served as the primary data base in this study. The CARETS shore zone studied was divided into six distinct geographical regions; area percentages for each class in the modified Anderson classification are presented. Similarities and differences between regions are discussed within the framework of man's modification of these landscapes. The results of this study are presented as a series of 19 maps of land-use categories. Recommendations are made for a remote-sensing system for monitoring the CARETS shore zone within the context of the dynamics of the landscapes studied.","language":"English","publisher":"National Park Service; U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/70039544","usgsCitation":"Dolan, R., Hayden, B., and Vincent, C., 1974, Shore zone land use and land cover: Central Atlantic Regional Ecological Test Site: Natural Resources Report 8, v, 50 p.; maps; 28 cm., https://doi.org/10.3133/70039544.","productDescription":"v, 50 p.; maps; 28 cm.","numberOfPages":"58","costCenters":[],"links":[{"id":261668,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039544/report.pdf"},{"id":261669,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039544/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8e83e4b08c986b3189af","contributors":{"authors":[{"text":"Dolan, R.","contributorId":44053,"corporation":false,"usgs":true,"family":"Dolan","given":"R.","email":"","affiliations":[],"preferred":false,"id":466454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayden, B.P.","contributorId":32049,"corporation":false,"usgs":true,"family":"Hayden","given":"B.P.","email":"","affiliations":[],"preferred":false,"id":466453,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Vincent, C.L.","contributorId":85849,"corporation":false,"usgs":true,"family":"Vincent","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":466455,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70040602,"text":"70040602 - 1974 - Ground-water resources, Allegheny River basin and part of the Lake Erie basin, New York","interactions":[],"lastModifiedDate":"2012-11-02T13:43:22","indexId":"70040602","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":241,"text":"Basin Planning Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"ARB-2","title":"Ground-water resources, Allegheny River basin and part of the Lake Erie basin, New York","language":"English","publisher":"New York State Department of Environmental Conservation","publisherLocation":"Albany, NY","usgsCitation":"Frimpter, M., 1974, Ground-water resources, Allegheny River basin and part of the Lake Erie basin, New York: Basin Planning Report ARB-2, 98 p.","productDescription":"98 p.","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262955,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.760000,40.480000 ], [ -79.760000,45.020000 ], [ -71.860000,45.020000 ], [ -71.860000,40.480000 ], [ -79.760000,40.480000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5094ebc6e4b0e5cfc2acdcd1","contributors":{"authors":[{"text":"Frimpter, M. H.","contributorId":34127,"corporation":false,"usgs":true,"family":"Frimpter","given":"M. H.","affiliations":[],"preferred":false,"id":468660,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70040712,"text":"70040712 - 1974 - Ground-water resources of the western Oswego River basin, New York","interactions":[],"lastModifiedDate":"2012-11-13T12:49:40","indexId":"70040712","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":241,"text":"Basin Planning Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"ORB-5","title":"Ground-water resources of the western Oswego River basin, New York","language":"English","publisher":"New York State Department of Environmental Conservation","publisherLocation":"Albany, NY","usgsCitation":"Crain, L., 1974, Ground-water resources of the western Oswego River basin, New York: Basin Planning Report ORB-5, 137 p.; 3 Plates in 4 Sheets.","productDescription":"137 p.; 3 Plates in 4 Sheets","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":263108,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.76,40.48 ], [ -79.76,45.02 ], [ -71.86,45.02 ], [ -71.86,40.48 ], [ -79.76,40.48 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50a3ba6ee4b0855e233c074e","contributors":{"authors":[{"text":"Crain, L.J.","contributorId":70829,"corporation":false,"usgs":true,"family":"Crain","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":468858,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70046328,"text":"wdrNM731 - 1974 - Water resources data for New Mexico, water year 1973; Part 1. Surface water records","interactions":[],"lastModifiedDate":"2013-07-08T10:54:41","indexId":"wdrNM731","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NM-73-1","title":"Water resources data for New Mexico, water year 1973; Part 1. Surface water records","docAbstract":"Surface-water records for the 1973 calendar year for New Mexico, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, are given in this report and their locations shown in figures 1, 2. Records for a 'few pertinent gaging stations in bordering States also are included. The records were collected and computed by the Water Resources Division of the US. Geological Survey under the direction of W. E. Hale, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in New Mexico. Through September 30, 1960, the records of discharge and stage of streams and canals and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water supply papers entitled \"Surface Water Supply of the United States\" Beginning with the 1961 water year, surface-water records have been released by the Geological Survey in annual reports on a State boundary basis. Distribution of these reports is limited; they are designed primarily for rapid release of data shortly after the end of the water year to meet local needs. The discharge and reservoir storage records for 1961-65 also are published in a Geological Survey water supply paper series entitled \"Surface Water Supply of the United States 1961-65.\" There will be a similar series of water-supply papers for the water years 1966-70.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Santa Fe, NM","doi":"10.3133/wdrNM731","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for New Mexico, water year 1973; Part 1. Surface water records: U.S. Geological Survey Water Data Report NM-73-1, 250 p., https://doi.org/10.3133/wdrNM731.","productDescription":"250 p.","costCenters":[],"links":[{"id":273457,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274526,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1973/nm-73/report.pdf"}],"country":"United States","state":"New Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.052,31.3322 ], [ -109.052,37.0003 ], [ -103.002,37.0003 ], [ -103.002,31.3322 ], [ -109.052,31.3322 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b300ebe4b01368e589e42f","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":535538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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