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1971 - Aeromagnetic map of the Mansfield Quadrangle, Norfolk and Bristol counties, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:10:56","indexId":"gp773","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"773","title":"Aeromagnetic map of the Mansfield Quadrangle, Norfolk and Bristol counties, Massachusetts","language":"ENGLISH","doi":"10.3133/gp773","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Aeromagnetic map of the Mansfield Quadrangle, Norfolk and Bristol counties, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 773, 1 map., https://doi.org/10.3133/gp773.","productDescription":"1 map.","costCenters":[],"links":[{"id":250186,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0773/report.pdf","size":"39","linkFileType":{"id":1,"text":"pdf"}},{"id":250187,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0773/plate-1.pdf","size":"3473","linkFileType":{"id":1,"text":"pdf"}},{"id":253659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0773/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.25,42 ], [ -71.25,42.1175 ], [ -71.11749999999999,42.1175 ], [ -71.11749999999999,42 ], [ -71.25,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691e4e","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":533359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":63835,"text":"gp747 - 1971 - Aeromagnetic map of the South Boston Quadrangle, Halifax County, Virginia, and Person and Granville counties, North Carolina","interactions":[],"lastModifiedDate":"2012-02-10T00:10:55","indexId":"gp747","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"747","title":"Aeromagnetic map of the South Boston Quadrangle, Halifax County, Virginia, and Person and Granville counties, North Carolina","language":"ENGLISH","doi":"10.3133/gp747","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Aeromagnetic map of the South Boston Quadrangle, Halifax County, Virginia, and Person and Granville counties, North Carolina: U.S. Geological Survey Geophysical Investigations Map 747, 1 map., https://doi.org/10.3133/gp747.","productDescription":"1 map.","costCenters":[],"links":[{"id":105376,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6102.htm","linkFileType":{"id":5,"text":"html"},"description":"6102"},{"id":186918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79,36.5 ], [ -79,36.75 ], [ -78.75,36.75 ], [ -78.75,36.5 ], [ -79,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aeee4b07f02db6911da","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":533304,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":24817,"text":"ofr71320 - 1971 - Ground-water reconnaissance of selected sites in Rocky Mountain National Park and Shadow Mountain National Recreation area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"ofr71320","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-320","title":"Ground-water reconnaissance of selected sites in Rocky Mountain National Park and Shadow Mountain National Recreation area, Colorado","docAbstract":"An evaluation of the ground-water supply potential at 30 sites within the Rocky Mountain National Park and Shadow Mountain National Recreation Area was made by the U.S. Geological Survey in 1967 and 1968. The work consisted of a geohydrologic reconnaissance, well inventory, and test drilling. \r\n\r\nThe study sites are underlain by. Precambrian crystalline rocks, Tertiary sediments, or Quaternary glacial and alluvial deposits. The crystalline rocks are generally poor aquifers; however, some wells intercepting fractures may yield as much as 10 gallons per minute from wells 100 to 200 feet deep. Wells drilled in Tertiary sandstones to a depth of 50 to 500 feet may supply 1 to 50 gallons per minute. Wells drilled in unconsolidated glacial and alluvial deposits of Quaternary age yield the largest supplies of ground water in the Rocky Mountain National Park. These deposits commonly can supply 5 to 100 gallons per minute to wells.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division, Colorado District,","doi":"10.3133/ofr71320","issn":"0094-9140","usgsCitation":"Welder, F., 1971, Ground-water reconnaissance of selected sites in Rocky Mountain National Park and Shadow Mountain National Recreation area, Colorado: U.S. Geological Survey Open-File Report 71-320, iii, 16 p. :maps ;27 cm., https://doi.org/10.3133/ofr71320.","productDescription":"iii, 16 p. :maps ;27 cm.","costCenters":[],"links":[{"id":156916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0320/report-thumb.jpg"},{"id":53825,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0320/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0320/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667186","contributors":{"authors":[{"text":"Welder, F.A.","contributorId":104878,"corporation":false,"usgs":true,"family":"Welder","given":"F.A.","email":"","affiliations":[],"preferred":false,"id":192618,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2596,"text":"wsp2020 - 1971 - Subsurface waste disposal by means of wells - A selective annotated bibliography","interactions":[],"lastModifiedDate":"2018-03-21T15:48:04","indexId":"wsp2020","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"2020","title":"Subsurface waste disposal by means of wells - A selective annotated bibliography","docAbstract":"Subsurface waste disposal by means of wells is the practice of using drilled wells to inject unwanted substances into underground rock formations. The use of wells for this purpose is not a new idea. As long ago as the end of the last century, it was common practice to drill wells for the express purpose of draining swamps and small lakes to reclaim the land for agricultural purposes. A few decades later in the 1920's and 1930's many oil companies began using injection wells to dispose of oil-field brines and to repressurize oil reservoirs. During World War II, the Atomic Energy Commission began using injection wells to dispose of certain types of radioactive wastes. More recently, injection wells have been drilled to dispose of a variety of byproducts of industrial processes. The number of such wells has increased rapidly since Congress passed the Clean Streams Act of 1966, which restricted the discharge of waste into surface waters.
Many scientists and public officials question the propriety of using the term \"disposal\" when referring to the underground injection of wastes. Their reasons are that underground injection is not, as many advocates claim, \"a complete and final answer\" to the waste-disposal problem. Rather, it is merely a process wherein the injected wastes are committed to the subsurface with uncertainty as to their ultimate fate or limits of confinement. In effect, the wastes, undiminished and unchanged, are removed from the custody of man and placed in the custody of nature.
Although the concept of waste-injection wells is relatively simple, the effects of waste injection can be very complex, particularly when dealing with the exotic and complex components of some industrial wastes. Besides the physical forces of injection, there are many varied interactions between the injected wastes and the materials within the injection zone. Because these changes occur out of sight in the subsurface, they are difficult to assess and not generally understood. In addition, the various aspects of the problem involve a wide spectrum of science and engineering. Hence, articles published on the subject are widely dispersed in the technical and scientific literature.
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Bay and Upper Mississippi River basins and Missouri River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"wsp2013","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"2013","title":"Quality of surface waters of the United States, 1967, Parts 5 and 6, Hudson Bay and Upper Mississippi River basins and Missouri River basin","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp2013","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Quality of surface waters of the United States, 1967, Parts 5 and 6, Hudson Bay and Upper Mississippi River basins and Missouri River basin: U.S. Geological Survey Water Supply Paper 2013, xiii, 585 p. ;23 cm., https://doi.org/10.3133/wsp2013.","productDescription":"xiii, 585 p. ;23 cm.","costCenters":[],"links":[{"id":139268,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2013/report-thumb.jpg"},{"id":30015,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2013/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db65197c","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":528080,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43561,"text":"ofr71142 - 1971 - Geologic reconnaissance map of the Chris Mountain and Pagosa Springs quadrangles, Archuleta County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:11:03","indexId":"ofr71142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-142","title":"Geologic reconnaissance map of the Chris Mountain and Pagosa Springs quadrangles, Archuleta County, Colorado","language":"ENGLISH","doi":"10.3133/ofr71142","usgsCitation":"Hail, W., 1971, Geologic reconnaissance map of the Chris Mountain and Pagosa Springs quadrangles, Archuleta County, Colorado: U.S. Geological Survey Open-File Report 71-142, 1 map, https://doi.org/10.3133/ofr71142.","productDescription":"1 map","costCenters":[],"links":[{"id":106503,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8596.htm","linkFileType":{"id":5,"text":"html"},"description":"8596"},{"id":169333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81191,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0142/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688473","contributors":{"authors":[{"text":"Hail, W. J. Jr.","contributorId":35332,"corporation":false,"usgs":true,"family":"Hail","given":"W. 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This report presents an analysis of the problem of making continuous accurate current-meter measurements in this channel where the flow regime is changing constantly in response to tidal action. Gaging-system requirements are delineated, and a brief description is given of the several applicable techniques that have been developed by others. None of these techniques provides the accuracies required for the flowmeter calibration. A new system is described--one which has been assembled and tested in prototype and which will provide the matrix of data needed for accurate continuous current-meter measurements. \r\n\r\nAnalysis of a large quantity of data on the velocity distribution in the channel of the Sacramento River at Chipps Island shows that adequate definition of the velocity can be made during the dominant flow periods--that is, at times other than slack-water periods--by use of current meters suspended at elevations 0.2 and 0.8 of the depth below the water surface. However, additional velocity surveys will be necessary to determine whether or not small systematic corrections need be applied during periods of rapidly changing flow. \r\n\r\nIn the proposed system all gaged parameters, including velocities, depths, position in the stream, and related times, are monitored continuously as a boat moves across the river on the selected cross section. Data are recorded photographically and transferred later onto punchcards for computer processing. \r\n\r\nComputer programs have been written to permit computation of instantaneous discharges at any selected time interval throughout the period of the current meter measurement program. It is anticipated that current-meter traverses will be made at intervals of about one-half hour over periods of several days. Capability of performance for protracted periods was, consequently, one of the important elements in system design. \r\n\r\nAnalysis of error sources in the proposed system indicates that errors in individual computed discharges can be kept smaller than 1.5 percent if the expected precision in all measured parameters is maintained.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1869G","usgsCitation":"Smith, W., 1971, Techniques and equipment required for precise stream gaging in tide-affected fresh-water reaches of the Sacramento River, California: U.S. Geological Survey Water Supply Paper 1869, vi, 46 p. ;24 cm., https://doi.org/10.3133/wsp1869G.","productDescription":"vi, 46 p. ;24 cm.","costCenters":[],"links":[{"id":139024,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1869g/report-thumb.jpg"},{"id":29101,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1869g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29102,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1869g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a321","contributors":{"authors":[{"text":"Smith, Winchell","contributorId":20311,"corporation":false,"usgs":true,"family":"Smith","given":"Winchell","email":"","affiliations":[],"preferred":false,"id":145658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25049,"text":"pp735 - 1971 - Chemistry of Kilauea and Mauna Loa lava in space and time","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"pp735","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"735","title":"Chemistry of Kilauea and Mauna Loa lava in space and time","language":"ENGLISH","publisher":"U.S. Govt. 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This report presents data obtained during the first 13 years of the proposed 20-year study. \r\n\r\nFor the period of record 1954-66, runoff from grazed watersheds has averaged about 33 acre-feet per square mile per year. Runoff from ungrazed watersheds averaged from 71 to 76 percent of that from grazed watersheds. During the last 6 years of the period, however, ungrazed watersheds produced 69 to 71 percent as much runoff as grazed watersheds. The sediment yield frown grazed watersheds during the same period was about 3 acre-feet per square mile per year. Sediment yield from ungrazed watersheds ranged from 51 to 75 percent of that from grazed watersheds and averaged 66 percent. The largest change in these relations occurred about 2 years after livestock were excluded from certain watersheds. The causative factors for changes in the runoff and sediment yield relations are not entirely clear. At the end of 13 years, a significant change had occurred in the amount of bare soil and rock. in the ground-cover index, and in the litter and moss on the grazed watersheds. These items remained essentially unchanged on ungrazed watersheds. The changes in ground-cover factors were not of large magnitude and did not occur at the same rate as the changes in runoff and sediment yield. A large part of the difference appears to have been caused by a change in the structure of surface soil. which was brought about by the elimination of trampling by livestock. \r\n\r\nDeer mice were the most common rodent present on the experimental watersheds, but even their population was not great enough to affect the composition of range vegetation. Deer mice populations remained comparable on grazed and ungrazed watersheds during the study. Other rodents were not present in sufficient numbers to allow their comparison on grazed and ungrazed range. Desert cottontail rabbits and black-tailed jackrabbits were more plentiful in ungrazed watersheds but were not present in large enough numbers to affect range vegetation.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1532D","usgsCitation":"Lusby, G.C., and Knipe, O., 1971, Effects of Grazing on the Hydrology and Biology of the Badger Wash Basin in Western Colorado, 1953-66: U.S. Geological Survey Water Supply Paper 1532, v, 90 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1532D.","productDescription":"v, 90 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":109968,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24708.htm","linkFileType":{"id":5,"text":"html"},"description":"24708"},{"id":138202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532d/report-thumb.jpg"},{"id":27799,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1532d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27800,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db5460de","contributors":{"authors":[{"text":"Lusby, Gregg C.","contributorId":68290,"corporation":false,"usgs":true,"family":"Lusby","given":"Gregg","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144778,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knipe, O.D.","contributorId":90158,"corporation":false,"usgs":true,"family":"Knipe","given":"O.D.","email":"","affiliations":[],"preferred":false,"id":144779,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3081,"text":"wsp1908 - 1971 - Surface water supply of the United States 1961–65: Part 3. Ohio River Basin; Volume 2. Ohio River Basin From Kanawha River to Louisville, Kentucky","interactions":[],"lastModifiedDate":"2021-10-27T19:29:28.502923","indexId":"wsp1908","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1908","title":"Surface water supply of the United States 1961–65: Part 3. Ohio River Basin; Volume 2. Ohio River Basin From Kanawha River to Louisville, Kentucky","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1908","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Surface water supply of the United States 1961–65: Part 3. Ohio River Basin; Volume 2. Ohio River Basin From Kanawha River to Louisville, Kentucky: U.S. Geological Survey Water Supply Paper 1908, Report: viii, 581 p.; 1 Plate: 24.50 × 25.50 inches, https://doi.org/10.3133/wsp1908.","productDescription":"Report: viii, 581 p.; 1 Plate: 24.50 × 25.50 inches","costCenters":[],"links":[{"id":138625,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1908/report-thumb.jpg"},{"id":29956,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1908/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391030,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25133.htm"},{"id":29955,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1908/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kentucy, Ohio, West Virginia","otherGeospatial":"Ohio River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.9,\n 36.2670\n ],\n [\n -79.65,\n 36.2670\n ],\n [\n -79.65,\n 40.737\n ],\n [\n -85.9,\n 40.737\n ],\n [\n -85.9,\n 36.2670\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6941e9","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":528062,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3164,"text":"wsp1937 - 1971 - Surface water supply of the United States, 1960-65, Part 16, Hawaii and other Pacific areas","interactions":[],"lastModifiedDate":"2022-10-27T21:32:45.124558","indexId":"wsp1937","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1937","title":"Surface water supply of the United States, 1960-65, Part 16, Hawaii and other Pacific areas","docAbstract":"No abstract available.
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