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,{"id":47150,"text":"ofr6566 - 1965 - Geologic map and sections for the Columbia Basin Irrigation Project area, Washington","interactions":[{"subject":{"id":47150,"text":"ofr6566 - 1965 - Geologic map and sections for the Columbia Basin Irrigation Project area, Washington","indexId":"ofr6566","publicationYear":"1965","noYear":false,"title":"Geologic map and sections for the Columbia Basin Irrigation Project area, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":66013,"text":"i589 - 1971 - Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington","indexId":"i589","publicationYear":"1971","noYear":false,"title":"Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington"},"id":1}],"supersededBy":{"id":66013,"text":"i589 - 1971 - Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington","indexId":"i589","publicationYear":"1971","noYear":false,"title":"Geologic map and sections of parts of Grant, Adams, and Franklin Counties, Washington"},"lastModifiedDate":"2012-02-02T00:10:56","indexId":"ofr6566","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"65-66","title":"Geologic map and sections for the Columbia Basin Irrigation Project area, Washington","language":"ENGLISH","doi":"10.3133/ofr6566","usgsCitation":"Grolier, M.J., and Bingham, J., 1965, Geologic map and sections for the Columbia Basin Irrigation Project area, Washington: U.S. Geological Survey Open-File Report 65-66, 1 map on two sheets., https://doi.org/10.3133/ofr6566.","productDescription":"1 map on two sheets.","costCenters":[],"links":[{"id":167894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a48e3","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":234713,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, J.W.","contributorId":35295,"corporation":false,"usgs":true,"family":"Bingham","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":234712,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1129,"text":"wsp1498I - 1965 - Total bed-material discharge in alluvial channels","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1498I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1498","chapter":"I","title":"Total bed-material discharge in alluvial channels","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Studies in flow in alluvial channels","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/wsp1498I","usgsCitation":"Chang, F.M., Simons, D., and Richardson, E., 1965, Total bed-material discharge in alluvial channels: U.S. Geological Survey Water Supply Paper 1498, v, 23 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1498I.","productDescription":"v, 23 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137928,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1498i/report-thumb.jpg"},{"id":25907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1498i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629af0","contributors":{"authors":[{"text":"Chang, Fred M.","contributorId":87913,"corporation":false,"usgs":true,"family":"Chang","given":"Fred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":143224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simons, D.B.","contributorId":50501,"corporation":false,"usgs":true,"family":"Simons","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":143223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richardson, E.V.","contributorId":105697,"corporation":false,"usgs":true,"family":"Richardson","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":143225,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68487,"text":"ha140 - 1965 - Water-table, surface-drainage, and engineering soils map of the Frederica area, Delaware","interactions":[],"lastModifiedDate":"2012-02-10T00:11:31","indexId":"ha140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"140","title":"Water-table, surface-drainage, and engineering soils map of the Frederica area, Delaware","language":"ENGLISH","doi":"10.3133/ha140","usgsCitation":"Davis, C.F., Boggess, D.H., and Coskery, O.J., 1965, Water-table, surface-drainage, and engineering soils map of the Frederica area, Delaware: U.S. Geological Survey Hydrologic Atlas 140, 1 map :col. ;on sheet 76 x 96 cm., https://doi.org/10.3133/ha140.","productDescription":"1 map :col. ;on sheet 76 x 96 cm.","costCenters":[],"links":[{"id":185494,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90040,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/140/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.5,39 ], [ -75.5,39.1175 ], [ -75.33333333333333,39.1175 ], [ -75.33333333333333,39 ], [ -75.5,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4cf7","contributors":{"authors":[{"text":"Davis, Christian F.","contributorId":84004,"corporation":false,"usgs":true,"family":"Davis","given":"Christian","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":278312,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278311,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coskery, O. J.","contributorId":8440,"corporation":false,"usgs":true,"family":"Coskery","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278310,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68484,"text":"ha157 - 1965 - Availability of ground water in the Symsonia quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"ha157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"157","title":"Availability of ground water in the Symsonia quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/ha157","usgsCitation":"Davis, R.W., 1965, Availability of ground water in the Symsonia quadrangle, Kentucky: U.S. Geological Survey Hydrologic Atlas 157, col. map ;99 x 120 cm., https://doi.org/10.3133/ha157.","productDescription":"col. map ;99 x 120 cm.","costCenters":[],"links":[{"id":188725,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90037,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/157/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.61749999999999,36.8675 ], [ -88.61749999999999,37 ], [ -88.5,37 ], [ -88.5,36.8675 ], [ -88.61749999999999,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8d8","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":278305,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1839,"text":"wsp1667D - 1965 - Reduction and complexing of manganese gallic acids","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1667D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1667","chapter":"D","title":"Reduction and complexing of manganese gallic acids","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1667D","usgsCitation":"Hem, J.D., 1965, Reduction and complexing of manganese gallic acids: U.S. Geological Survey Water Supply Paper 1667, iii, 28 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1667D.","productDescription":"iii, 28 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1667d/report-thumb.jpg"},{"id":27044,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1667d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db635256","contributors":{"authors":[{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":144236,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1159,"text":"wsp1795 - 1965 - Water resources of the Humboldt River Valley near Winnemucca, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1795","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1795","title":"Water resources of the Humboldt River Valley near Winnemucca, Nevada","docAbstract":"This report, resulting from studies made by the U.S. Geological Survey as part of the interagency Humboldt River Research Project, describes the qualitative and quantitative relations among the components of the hydrologic system in the Winnemucca Reach of the Humboldt River valley. The area studied includes the segment of the Humboldt River valley between the Comus and Rose Creek gaging stations. It is almost entirely in Humboldt County in north-central Nevada, and is about 200 miles downstream from the headwaters of the Humboldt River. \r\n\r\nAgriculture is the major economic activity in the area. Inasmuch as the valley lowlands receive an average of about 8 inches of precipitation per year and because the rate of evaporation from free-water surfaces is about six times the average annual precipitation, all crops in the area (largely forage crops) are irrigated. About 85 percent of the cultivated land is irrigated with Humboldt River water; the remainder is irrigated from about 20 irrigation wells. \r\n\r\nThe consolidated rocks of the uplifted fault-block mountains are largely barriers to the movement of ground water and form ground-water and surface-water divides. Unconsolidated deposits of late Tertiary and Quaternary age underlie the valley lowlands to a maximum depth of about 5,000 feet. These deposits are in hydraulic continuity with the Humboldt River and store and transmit most of the economically recoverable ground water. Included in the valley fill is a highly permeable sand and gravel deposit having a maximum thickness of about 90-100 feet; it underlies the flood plain and bordering terraces throughout most of the project area. This deposit is almost completely saturated and contains about 500,000 acre-feet of ground water in storage. The Humboldt River is the source of 90-95 percent of the surface-water inflow to the area. In water years 1949-62 the average annual streamflow at the Comus gaging station at the upstream margin of the area was 172,100 acre-feet; outflow at the Rose Creek gaging station averaged about 155,400 acre-feet. Accordingly, the measured loss of Humboldt River streamflow averaged nearly 17,000 acre-feet per year. Most of this water was transpired by phreatophytes and crops, evaporated from free-water surfaces, and evaporated from bare soil. \r\n\r\nInasmuch as practically no tributary streamflow normally discharges into the river in the Winnemucca reach and because pumpage is virtually negligible during the nonirrigation season, gains and losses of streamflow during most of the year reflect the close interrelation of the Humboldt River and the groundwater reservoir. An estimated average of about 14,000 acre-feet per year of ground-water underflow moves toward the Humboldt River from tributary areas. Much of this water discharges into the Humboldt River; hovever, some evaporates or is transpired before reaching the river. \r\n\r\nMore than 65 percent of the average annual flow of the river horn-ally occurs in April, May, and June owing to the spring runoff. The stage of the river generally rises rapidly during these months causing water to move from the river to the ground-water reservoir. Furthermore, the period of high streamflow normally coincides with the irrigation season, and much of the excess irrigation water diverted from the river percolates downward to the zone of saturation. \r\n\r\nThe net measured loss of streamflow in April-June, which averaged about 24,000 acre-feet in water years 1949-62, was about 7,000 acre-feet more than the average annual loss. The estimated net average annual increase of ground water in storage during these months in this period was on the order of 10,000 acre-feet. Following the spring runoff and the irrigation season, normally in July, some of the ground water stored in the flood-plain deposits during the spring runoff begins to discharge into the river. In addition, ground-water inflow from tributary areas again begins to discharge into the river. \r\n\r\nExperiments utilizin","language":"ENGLISH","publisher":"U. S. Govt. Print. 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Introduction and summary"},{"id":33024,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0441/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Upper Colorado River Basin showing the distribution of hydrologic units and chemical quality of surface water"},{"id":33025,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0441/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Upper Colorado River Basin showing the distribution of hydrologic units and the quality of water from representative wells and springs principally in river alluvium"},{"id":33026,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0441/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Grand division, Upper Colorado River basin, showing average annual precipitation and evaporation, key streamflow-gaging stations, and coefficients of variation of annual runoff"},{"id":464260,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4436.htm","text":"Surface-water resources of the Grand division","linkFileType":{"id":5,"text":"html"}},{"id":464261,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4437.htm","text":"Surface-water resources of the Green division","linkFileType":{"id":5,"text":"html"}},{"id":464262,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4438.htm","text":"Surface-water resources of the San Juan division","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Arizona, Colorado, Idaho, New Mexico, Utah, Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.2917,\n              35.5456\n            ],\n            [\n              -105.625,\n              35.5456\n            ],\n            [\n              -105.625,\n              43.45\n            ],\n            [\n              -112.2917,\n              43.45\n            ],\n            [\n              -112.2917,\n              35.5456\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f3e4b07f02db5efc81","contributors":{"authors":[{"text":"Iorns, William Vaughn","contributorId":53793,"corporation":false,"usgs":true,"family":"Iorns","given":"William","email":"","middleInitial":"Vaughn","affiliations":[],"preferred":false,"id":152015,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hembree, Charles Herbert","contributorId":63784,"corporation":false,"usgs":true,"family":"Hembree","given":"Charles","email":"","middleInitial":"Herbert","affiliations":[],"preferred":false,"id":152016,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oakland, Godfrey L.","contributorId":18760,"corporation":false,"usgs":true,"family":"Oakland","given":"Godfrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":152014,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3158,"text":"wsp1819B - 1965 - Predicted hydrologic effects of pumping from the Lichterman Well Field in the Memphis Area, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"wsp1819B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1819","chapter":"B","title":"Predicted hydrologic effects of pumping from the Lichterman Well Field in the Memphis Area, Tennessee","docAbstract":"The Lichterman well field is scheduled to go into operation early in 1965 to supplement the municipal water-supply system for the city of Memphis, Tenn. Although the initial rate of withdrawal from the well field will be about 8 mgd (million gallons per day), the ultimate design capacity of the field is 20 mgd. A study of sand samples, drillers' logs, and geophysical logs collected during preliminary test drilling at the site for the Lichterman well field was used as a basis for defining three zones of sand favorable for the construction of high-capacity (1,000 gallons per minute or more) water wells. The three zones occur in the '500-foot' sand and are here designated (in descending order) as zone A, zone B, and zone C. The depth to the top of these zones below land surface has the following ranges: zone A, 125 to 225 feet; zone B, 200 to 350 feet; and zone C, 700 to 775 feet. Zones A and B range from 0 to 100 feet in thickness, and zone C ranges from 10 to 100 feet in thickness. Within the well field proper these zones are expected to react to the stress of pumping as separate hydrologic units, but outside the well field the three zones are expected to react as a single hydrologic unit. \r\n\r\nThe '500-foot' sand in the Germantown-Collierville area is recharged chiefly by precipitation on the outcrop area of the sand to the east, but the evidence indicates that additional recharge is entering the aquifer from the Wolf River. In spite of this additional recharge, water levels in the '500-foot' sand are declining at an average rate of about two-thirds of a foot per year, owing to municipal and industrial pumpage in the Memphis area. However, this decline is not expected to alter the excellent quality of the water in the '500-foot' sand at the site of the Lichterman well field. \r\n\r\nPumping in the Lichterman well field will create a cone of depression in the free-water (piezometric) surface of the '500-foot' sand. The decline in water levels will be directly proportional to the rate of pumping and inversely proportional to the distance from the well field. The resultant changes in hydraulic gradients will alter the direction of ground-water movement in the vicinity of the well field and increase the rate of movement toward the well field from areas of recharge. The lowering of water levels might also accelerate locally the changeover from artesian conditions to semiartesian or water-table conditions in the '500-foot' sand. \r\n\r\nWithin the well field proper, water levels are expected to fluctuate as individual wells are turned on and off to accommodate the demand for water. The presence of clay beds in the aquifer will tend to limit the specific capacity of individual production wells, but could serve to limit interference between wells if adjacent wells are screened in different sections of the aquifer. Interference between wells might also be lessened by pumping those wells having the highest specific capacities for the longest periods of time.","language":"ENGLISH","doi":"10.3133/wsp1819B","usgsCitation":"Nyman, D.J., 1965, Predicted hydrologic effects of pumping from the Lichterman Well Field in the Memphis Area, Tennessee: U.S. Geological Survey Water Supply Paper 1819, 26 p. , https://doi.org/10.3133/wsp1819B.","productDescription":"26 p. ","costCenters":[],"links":[{"id":138860,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819b/report-thumb.jpg"},{"id":30106,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30107,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e99e","contributors":{"authors":[{"text":"Nyman, Dale J.","contributorId":28584,"corporation":false,"usgs":true,"family":"Nyman","given":"Dale","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":146347,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3286,"text":"cir498 - 1965 - Reports and maps of the Geological Survey released only in the open files, 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir498","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"498","title":"Reports and maps of the Geological Survey released only in the open files, 1964","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir498","usgsCitation":"Weld, B., Griffin, M.S., and Brett, G.W., 1965, Reports and maps of the Geological Survey released only in the open files, 1964: U.S. Geological Survey Circular 498, 16 p. ;26 cm., https://doi.org/10.3133/cir498.","productDescription":"16 p. ;26 cm.","costCenters":[],"links":[{"id":120935,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0498/report-thumb.jpg"},{"id":30282,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0498/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f3f3","contributors":{"authors":[{"text":"Weld, Betsy A.","contributorId":68714,"corporation":false,"usgs":true,"family":"Weld","given":"Betsy A.","affiliations":[],"preferred":false,"id":146590,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griffin, Margaret S.","contributorId":101252,"corporation":false,"usgs":true,"family":"Griffin","given":"Margaret","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":146591,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brett, George W.","contributorId":58622,"corporation":false,"usgs":true,"family":"Brett","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":146589,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3984,"text":"cir512 - 1965 - Index of surface-water records to December 31, 1963--Part 12, Pacific slope basins in Washington and upper Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir512","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"512","title":"Index of surface-water records to December 31, 1963--Part 12, Pacific slope basins in Washington and upper Columbia River basin","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir512","usgsCitation":"Eisenhuth, H., 1965, Index of surface-water records to December 31, 1963--Part 12, Pacific slope basins in Washington and upper Columbia River basin: U.S. Geological Survey Circular 512, 39 p. :ill., map ;26 cm., https://doi.org/10.3133/cir512.","productDescription":"39 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":122517,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1965/0512/report-thumb.jpg"},{"id":31069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1965/0512/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3137","contributors":{"authors":[{"text":"Eisenhuth, H.P.","contributorId":38140,"corporation":false,"usgs":true,"family":"Eisenhuth","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":147949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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