{"pageNumber":"2523","pageRowStart":"63050","pageSize":"25","recordCount":68788,"records":[{"id":70047174,"text":"70047174 - 1966 - A study of some effects of urbanization on storm runoff from a small watershed","interactions":[{"subject":{"id":52538,"text":"ofr6641 - 1966 - Some effects of urbanization on storm runoff, Waller Creek, Austin, Texas, 1955-62","indexId":"ofr6641","publicationYear":"1966","noYear":false,"title":"Some effects of urbanization on storm runoff, Waller Creek, Austin, Texas, 1955-62"},"predicate":"SUPERSEDED_BY","object":{"id":70047174,"text":"70047174 - 1966 - A study of some effects of urbanization on storm runoff from a small watershed","indexId":"70047174","publicationYear":"1966","noYear":false,"title":"A study of some effects of urbanization on storm runoff from a small watershed"},"id":1}],"lastModifiedDate":"2013-07-23T14:29:46","indexId":"70047174","displayToPublicDate":"2013-01-01T14:16:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":280,"text":"Report","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"23","title":"A study of some effects of urbanization on storm runoff from a small watershed","docAbstract":"The evaluation of the effects of urbanization on the runoff characteristics of a small watershed is a problem that can be studied by either a short-range or a long-range investigation. Because the long-range type of investigation would require several years for hydrologic data accumulation, it cannot provide any immediate information on the changes in watershed behavior arising as a result of urbanization. A short-range investigation, however, based on synthetic evaluation of present data would provide immediate answers. It is in the realm of this short-range objective that this study of a small urban watershed is directed.","language":"English","publisher":"Texas Water Development Board","publisherLocation":"Austin, TX","collaboration":"Prepared in the Center for Research in Water Resources at the University of Texas in cooperation with the Texas Water Development Board","usgsCitation":"Espey, W.H., Morgan, C.W., and Masch, F.D., 1966, A study of some effects of urbanization on storm runoff from a small watershed: Report 23, xiv, 110 p.","productDescription":"xiv, 110 p.","numberOfPages":"122","costCenters":[],"links":[{"id":275315,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047174.png"},{"id":275313,"type":{"id":11,"text":"Document"},"url":"https://www.twdb.state.tx.us/publications/reports/numbered_reports/doc/R23/R23.pdf"}],"country":"United States","state":"Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.6,25.8 ], [ -106.6,36.5 ], [ -93.5,36.5 ], [ -93.5,25.8 ], [ -106.6,25.8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51efa5f0e4b0b09fbe58f179","contributors":{"authors":[{"text":"Espey, William Howard Jr.","contributorId":102361,"corporation":false,"usgs":true,"family":"Espey","given":"William","suffix":"Jr.","email":"","middleInitial":"Howard","affiliations":[],"preferred":false,"id":481227,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morgan, Carl W.","contributorId":58924,"corporation":false,"usgs":true,"family":"Morgan","given":"Carl","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":481226,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Masch, Frank D.","contributorId":19456,"corporation":false,"usgs":true,"family":"Masch","given":"Frank","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":481225,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70047641,"text":"70047641 - 1966 - Water Resources of Rapides Parish, Louisiana","interactions":[],"lastModifiedDate":"2013-08-16T09:33:10","indexId":"70047641","displayToPublicDate":"2013-01-01T09:26:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":144,"text":"Water Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"8","title":"Water Resources of Rapides Parish, Louisiana","language":"English","publisher":"Louisiana Geological Survey","publisherLocation":"Baton Rouge, LA","collaboration":"Prepared in cooperation with the U.S. Geological Survey","usgsCitation":"Newcome, R., and Sloss, R., 1966, Water Resources of Rapides Parish, Louisiana: Water Resources Bulletin 8, ix, 104 p.","productDescription":"ix, 104 p.","costCenters":[],"links":[{"id":276670,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Louisiana","county":"Rapides Parish","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -92.981464,30.889193 ], [ -92.981464,31.517594 ], [ -92.07239,31.517594 ], [ -92.07239,30.889193 ], [ -92.981464,30.889193 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520f49e9e4b0fc50304bc525","contributors":{"authors":[{"text":"Newcome, Roy","contributorId":14796,"corporation":false,"usgs":true,"family":"Newcome","given":"Roy","affiliations":[],"preferred":false,"id":482614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sloss, Raymond","contributorId":59323,"corporation":false,"usgs":true,"family":"Sloss","given":"Raymond","email":"","affiliations":[],"preferred":false,"id":482615,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70038368,"text":"70038368 - 1966 - Hydrogeologic data in the Quinebaug River basin, Connecticut","interactions":[],"lastModifiedDate":"2014-04-09T14:02:24","indexId":"70038368","displayToPublicDate":"2012-05-06T17:29:00","publicationYear":"1966","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":"9","title":"Hydrogeologic data in the Quinebaug River basin, Connecticut","docAbstract":"This report presents hydrologic and geologic data collected by the U.S. Geological Survey during an investigation of water resources in the Quinebaug River basin of Connecticut in cooperation with the Connecticut Water Resources Commission. The Quinebaug River basin occupies about 425 square miles in the northeastern part of the State, including the towns of Brooklyn, Griswold, Killingly, Plainfield, Pomfret, Putnam, Sterling, and Thompson, and parts of Canterbury, Hampton, Lisbon, North Stonington, Preston, Voluntown, and Woodstock. A companion interpretive report evaluating the water resources of the basin will be published as Connecticut Water Resources Bulletin 8. The data on the following pages serve to document and supplement that report, and should be especially useful in planning the development of water resources at specific localities.","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Connecticut Water Resources Commission","usgsCitation":"Thomas, C.E., Randall, A.D., and Thomas, M.P., 1966, Hydrogeologic data in the Quinebaug River basin, Connecticut: Connecticut Water Resources Bulletin 9, Report: 84 p.; 1 Plate: 30.39 x 53.70 inches.","productDescription":"Report: 84 p.; 1 Plate: 30.39 x 53.70 inches","numberOfPages":"86","costCenters":[],"links":[{"id":286027,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70038368/report-thumb.jpg"}],"scale":"48000","country":"United States","state":"Connecticut","otherGeospatial":"Quinebaug River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.166667,41.466667 ], [ -72.166667,42.041667 ], [ 71.766667,42.041667 ], [ 71.766667,41.466667 ], [ -72.166667,41.466667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a33c0e4b0c8380cd5f233","contributors":{"authors":[{"text":"Thomas, Chester E. Jr.","contributorId":37182,"corporation":false,"usgs":true,"family":"Thomas","given":"Chester","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463985,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randall, Allan D. arandall@usgs.gov","contributorId":1168,"corporation":false,"usgs":true,"family":"Randall","given":"Allan","email":"arandall@usgs.gov","middleInitial":"D.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":463984,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463986,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70038367,"text":"70038367 - 1966 - Water resources inventory of Connecticut Part 1: Quinebaug River basin","interactions":[],"lastModifiedDate":"2014-03-28T09:52:58","indexId":"70038367","displayToPublicDate":"2012-05-06T16:53:00","publicationYear":"1966","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":"8","title":"Water resources inventory of Connecticut Part 1: Quinebaug River basin","docAbstract":"The Quinebaug River basin is blessed with a relatively abundant supply of water of generally good quality which is derived from precipitation that has fallen on the basin. Annual precipitation has ranged from about 30 to 67 inches and has averaged about 45 inches over a 44-year period. Approximately 21 inches of water are returned to the atmosphere each year by evaporation and transpiration; the remainder of the annual precipitation either flows overland to streams or percolates downward to the water table and ultimately flows out of the basin in the Quinebaug River. During the autumn and winter months precipitation normally is sufficient to cause a substantial increase in the amount of water stored underground and in surface reservoirs within the basin, whereas in the summer most of the precipitation is lost through evaporation and transpiration, resulting in sharply reduced streamflow and lowered ground-water levels.","language":"English","publisher":"Connecticut Water Resources Commission","collaboration":"Prepared in cooperation with the Connecticut Water Resources Commission","usgsCitation":"Randall, A.D., Thomas, M.P., Thomas, C.E., and Baker, J.A., 1966, Water resources inventory of Connecticut Part 1: Quinebaug River basin: Connecticut Water Resources Bulletin 8, v, 102 p.; Plate A: 30.96 x 55.54 inches; Plate B: 30.56 x 55.83 inches; Plate C: 30.11 x 56.07 inches; Plate D: 29.28 x 54.36 inches.","productDescription":"v, 102 p.; Plate A: 30.96 x 55.54 inches; Plate B: 30.56 x 55.83 inches; Plate C: 30.11 x 56.07 inches; Plate D: 29.28 x 54.36 inches","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":258833,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ctwrb/0008/report.pdf","size":"8463","linkFileType":{"id":1,"text":"pdf"}},{"id":258834,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ctwrb/0008/report-thumb.jpg"},{"id":258829,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ctwrb/0008/plate-a.pdf","size":"5415","linkFileType":{"id":1,"text":"pdf"}},{"id":258830,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ctwrb/0008/plate-b.pdf","size":"5727","linkFileType":{"id":1,"text":"pdf"}},{"id":258831,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ctwrb/0008/plate-c.pdf","size":"5463","linkFileType":{"id":1,"text":"pdf"}},{"id":258832,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ctwrb/0008/plate-d.pdf","size":"5509","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Connecticut","otherGeospatial":"Quinebaug River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.11749999999999,41.46666666666667 ], [ -72.11749999999999,42.034166666666664 ], [ -71.76666666666667,42.034166666666664 ], [ -71.76666666666667,41.46666666666667 ], [ -72.11749999999999,41.46666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bcb77e4b08c986b32d67b","contributors":{"authors":[{"text":"Randall, Allan D. arandall@usgs.gov","contributorId":1168,"corporation":false,"usgs":true,"family":"Randall","given":"Allan","email":"arandall@usgs.gov","middleInitial":"D.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":463980,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Mendall P.","contributorId":104314,"corporation":false,"usgs":true,"family":"Thomas","given":"Mendall","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":463983,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, Chester E. Jr.","contributorId":37182,"corporation":false,"usgs":true,"family":"Thomas","given":"Chester","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":463981,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Baker, John A.","contributorId":90815,"corporation":false,"usgs":true,"family":"Baker","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":463982,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70039091,"text":"70039091 - 1966 - Systems for monitoring and digitally recording water-quality parameters","interactions":[],"lastModifiedDate":"2012-07-19T01:01:48","indexId":"70039091","displayToPublicDate":"2012-01-01T09:06:35","publicationYear":"1966","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":"Systems for monitoring and digitally recording water-quality parameters","docAbstract":"Digital recording of water-quality parameters is a link in the automated data collection and processing system of the U.S. Geological Survey. The monitoring and digital recording systems adopted by the Geological Survey, while punching all measurements on a standard paper tape, provide a choice of compatible components to construct a system to meet specific physical problems and data needs. As many as 10 parameters can be recorded by an Instrument, with the only limiting criterion being that measurements are expressed as electrical signals.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/70039091","collaboration":"Other Contributors: Honeywell, Inc.","usgsCitation":"Smoot, G.F., and Blakey, J.F., 1966, Systems for monitoring and digitally recording water-quality parameters: Open-File Report, 14 p., https://doi.org/10.3133/70039091.","productDescription":"14 p.","numberOfPages":"16","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":261298,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039091/report.pdf"},{"id":261299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039091/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba378e4b08c986b31fcf7","contributors":{"authors":[{"text":"Smoot, George F.","contributorId":34116,"corporation":false,"usgs":true,"family":"Smoot","given":"George","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":465605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blakey, James F.","contributorId":65550,"corporation":false,"usgs":true,"family":"Blakey","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":465606,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046323,"text":"wdrNM651 - 1966 - Water resources data for New Mexico, water year 1965; Part 1. Surface water records","interactions":[],"lastModifiedDate":"2013-07-08T10:51:57","indexId":"wdrNM651","displayToPublicDate":"2012-01-01T00:00:00","publicationYear":"1966","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-65-1","title":"Water resources data for New Mexico, water year 1965; Part 1. Surface water records","docAbstract":"The surface-water records for the 1965 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of New Mexico are given in this report. For convenience there are also Included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of W. E. Hale, District Chief, Water Resources Division. This report is the fifth In a series presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams 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. Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in New Mexico were contained in Parts 7, 8 and 9 of that series. Beginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5~year intervals. These 5-year water-supply papers will show daily discharge and will be compi led On the same geographical areas previously used for the annual series; however, some of the 14 parts of conterminous United States will be further subdivided.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Santa Fe, NM","doi":"10.3133/wdrNM651","collaboration":"Prepared in cooperation with the State of New Mexico and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Water resources data for New Mexico, water year 1965; Part 1. Surface water records: U.S. Geological Survey Water Data Report NM-65-1, 275 p., https://doi.org/10.3133/wdrNM651.","productDescription":"275 p.","costCenters":[],"links":[{"id":273452,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":274521,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1965/nm-65/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":"51b300e9e4b01368e589e414","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":535533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220147,"text":"5220147 - 1966 - Recent tests on waterchestnut control","interactions":[],"lastModifiedDate":"2012-02-02T00:14:36","indexId":"5220147","displayToPublicDate":"2010-06-16T12:17:35","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3171,"text":"Proceedings of the Northeastern Weed Control Conference","active":true,"publicationSubtype":{"id":10}},"title":"Recent tests on waterchestnut control","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Proceedings of the Northeastern Weed Control Conference","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Steenis, J., and Stotts, V.D., 1966, Recent tests on waterchestnut control: Proceedings of the Northeastern Weed Control Conference, v. 20, p. 476-479.","productDescription":"476-479","startPage":"476","endPage":"479","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":194327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6449ba","contributors":{"authors":[{"text":"Steenis, J.H.","contributorId":73694,"corporation":false,"usgs":true,"family":"Steenis","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":331403,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stotts, Vernon D.","contributorId":86724,"corporation":false,"usgs":false,"family":"Stotts","given":"Vernon","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":331404,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5220076,"text":"5220076 - 1966 - A method of shipping live larvae of Simulium vittatum long distances (Diptera: Simuliidae)","interactions":[],"lastModifiedDate":"2023-02-21T17:36:57.1659","indexId":"5220076","displayToPublicDate":"2010-06-16T12:17:35","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":798,"text":"Annals of the Entomological Society of America","active":true,"publicationSubtype":{"id":10}},"displayTitle":"A method of shipping live larvae of <i>Simulium vittatum</i> long distances (Diptera: Simuliidae)","title":"A method of shipping live larvae of Simulium vittatum long distances (Diptera: Simuliidae)","docAbstract":"<p><span>During studies on the biology and ecology of black flies (Simuliidae) at the Seney National Wildlife Refuge, Seney, Michigan, and at the Patuxent Wildlife Research Center, Laurel, Maryland, larvae of 3 species of black fly (</span><i>Simulium vittatum</i><span>&nbsp;Zetterstedt,&nbsp;</span><i>S. aureum</i><span>&nbsp;Fries, and&nbsp;</span><i>S. decorum</i><span>&nbsp;Walker) were collected and transported for distances of up to 50 miles in nonagitated jars of water. In each case the water used to transport the larvae was removed from the waterway where the particular larvae were taken. However, on numerous occasions it was found that larvae could not be kept alive in nonagitated water jars for more than 6 hr.</span></p>","language":"English","publisher":"Oxford University Press","doi":"10.1093/aesa/59.4.866","usgsCitation":"Tarshis, I., 1966, A method of shipping live larvae of Simulium vittatum long distances (Diptera: Simuliidae): Annals of the Entomological Society of America, v. 59, no. 4, p. 866-867, https://doi.org/10.1093/aesa/59.4.866.","productDescription":"2 p.","startPage":"866","endPage":"867","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193473,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"59","issue":"4","noUsgsAuthors":false,"publicationDate":"1966-07-01","publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae01e","contributors":{"authors":[{"text":"Tarshis, I.B.","contributorId":83625,"corporation":false,"usgs":true,"family":"Tarshis","given":"I.B.","email":"","affiliations":[],"preferred":false,"id":331298,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220435,"text":"5220435 - 1966 - Fall food habits of ducks near Santee Refuge, South Carolina","interactions":[],"lastModifiedDate":"2020-05-13T19:48:59.404526","indexId":"5220435","displayToPublicDate":"2010-06-16T12:17:35","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"Fall food habits of ducks near Santee Refuge, South Carolina","docAbstract":"<p>During the 1961 waterfowl hunting season, 360 stomachs of 10 duck species were collected from hunters near the Santee National Wildlife Refuge, Lake Marion, South Carolina. Based on percentage of total volume, 20 of the most important foods are listed. The six most important duck species in the kill were: mallard (<i>Anas platyrhynchos</i>), wood duck (<i>Aix sponsa</i>), widgeon (<i>Mareca americam</i>), pintail (<i>Anas acuta</i>) , black duck (<i>Anas rubripes</i>) , and green-winged teal (<i>Anas carolinensis</i>). Six plant species made up 5 percent or more of the total volume of food items found in the stomachs of all ducks. Only seeds of oaks (<i>Quercus</i> sp.), corn, sweet gum (<i>Liquidambar Styraciflua</i>), and buttonbush (<i>Cephalanthus occidentalis</i>) were consumed. Some seed, but mostly the vegetative portions of hydrochloa (<i>Hydrochloa carolinensis</i>) and only the vegetative portions of southern rice cutgrass (<i>Leersia hexandra</i>) were taken. The more important game ducks concentrated on the refuge farmlands when water levels were below 72 feet mean sea level (msl). When levels reached 75 feet msl, natural foods became available, ducks dispersed from refuge areas, and hunting success increased greatly.</p>","largerWorkTitle":"","language":"English","publisher":"Wiley","doi":"10.2307/3798750","usgsCitation":"McGilvrey, F., 1966, Fall food habits of ducks near Santee Refuge, South Carolina: Journal of Wildlife Management, v. 30, no. 3, p. 577-580, https://doi.org/10.2307/3798750.","productDescription":"4 p.","startPage":"577","endPage":"580","numberOfPages":"4","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Carolina","otherGeospatial":"Lake Marion, Bluff Unit of Santee National Wildlife Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.48858642578125,\n              33.520789053588494\n            ],\n            [\n              -80.41374206542969,\n              33.520789053588494\n            ],\n            [\n              -80.41374206542969,\n              33.578014746143985\n            ],\n            [\n              -80.48858642578125,\n              33.578014746143985\n            ],\n            [\n              -80.48858642578125,\n              33.520789053588494\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7bc7","contributors":{"authors":[{"text":"McGilvrey, Frank B.","contributorId":14908,"corporation":false,"usgs":true,"family":"McGilvrey","given":"Frank B.","affiliations":[],"preferred":false,"id":331807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5230095,"text":"5230095 - 1966 - Problems in aerial surveys of waterfowl in eastern Canada","interactions":[],"lastModifiedDate":"2012-02-02T00:15:22","indexId":"5230095","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"93","title":"Problems in aerial surveys of waterfowl in eastern Canada","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Chamberlain, E., and Kaczynski, C., 1966, Problems in aerial surveys of waterfowl in eastern Canada: Special Scientific Report  - Wildlife 93, 21.","productDescription":"21","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":112121,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486769?urlappend=%3Bseq=629"},{"id":202638,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660a45","contributors":{"authors":[{"text":"Chamberlain, E.B.","contributorId":46149,"corporation":false,"usgs":true,"family":"Chamberlain","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":343492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kaczynski, C.F.","contributorId":76804,"corporation":false,"usgs":true,"family":"Kaczynski","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":343493,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5210184,"text":"5210184 - 1966 - Monitoring wildlife for pesticide content","interactions":[],"lastModifiedDate":"2018-04-06T14:10:15","indexId":"5210184","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1966","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesTitle":{"id":5675,"text":"National Academy of Sciences NRC Publication","active":true,"publicationSubtype":{"id":19}},"seriesNumber":"1402","title":"Monitoring wildlife for pesticide content","docAbstract":"<p>In May 1963, the President's Science Advisory Committee issued a report entitled&nbsp;<i>Use of Pesticides</i>.<sup>17</sup>&nbsp; the President already had requested the responsible federal agencies to implement the recommendations in the report. One of these recommendations was to provide for the development and coordination of a pesticide-monitoring program conducted on a continuing basis, by federal agencies to obtain timely systematic data on pesticide residues in the environment.</p><p>Many people re engaged in research to learn the quantities of pesticide that may be hazardous. Yet there is concern that hazardous quantities may accumulate before the difficult task of evaluation can be completed. The President's report on environmental pollution<sup>12</sup> expresses the view that the soils and waters of the world cannot indefinitely provide a vast dumping ground to absorb and render harmless all human wastes. Chlorinated hydrocarbon pesticides are only one of these kinds of pollutants, yet they are particularly important because they persist long in the environment and accumulate in the tissues of animals.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Scientific aspects of pest control: A symposium arranged and conducted by the National Academy of Sciences, National Research Council","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Scientific aspects of pest control","conferenceDate":"Washington, D.C.","conferenceLocation":"February 1-3, 1966","language":"English","publisher":"National Academy of Sciences; National Research Council","publisherLocation":"Washington, DC.","usgsCitation":"Dustman, E.H., 1966, Monitoring wildlife for pesticide content, <i>in</i> Scientific aspects of pest control: A symposium arranged and conducted by the National Academy of Sciences, National Research Council, February 1-3, 1966, Washington, D.C., p. 343-351.","productDescription":"9 p.","startPage":"343","endPage":"351","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200436,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db698ffd","contributors":{"authors":[{"text":"Dustman, E. H.","contributorId":12579,"corporation":false,"usgs":true,"family":"Dustman","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":327928,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70197603,"text":"70197603 - 1966 - Summary of hydrologic and physical properties of rock and soil materials, as analyzed by the hydrologic laboratory of the U.S. Geological Survey, 1948-60","interactions":[],"lastModifiedDate":"2022-05-25T19:08:32.837128","indexId":"70197603","displayToPublicDate":"1999-11-28T00:00:00","publicationYear":"1966","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":"Summary of hydrologic and physical properties of rock and soil materials, as analyzed by the hydrologic laboratory of the U.S. Geological Survey, 1948-60","docAbstract":"<p>The Hydrologic Laboratory was established in 1948 to serve as the central laboratory for the Ground Water Branch, Water Resources Division, of the U.S. Geological Survey. During the period it has been in existence, numerous samples of rock and soil materials have been analyzed. Analysis data on samples from 42 states and for the period 1948 through 1960 are summarized.</p><p>The data are presented in a form to allow an easy comparison of the physical and hydrologic properties of many sedimentary, igneous, and metamorphic rock and soil materials. Sedimentary rocks, the principal water-bearing rocks, are discussed in more detail.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70197603","usgsCitation":"Morris, D.A., and Johnson, A., 1966, Summary of hydrologic and physical properties of rock and soil materials, as analyzed by the hydrologic laboratory of the U.S. Geological Survey, 1948-60: Open-File Report, vi, 60 p., https://doi.org/10.3133/70197603.","productDescription":"vi, 60 p.","costCenters":[],"links":[{"id":401068,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70197603/report.pdf"},{"id":354998,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70197603/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Morris, D. A.","contributorId":56204,"corporation":false,"usgs":true,"family":"Morris","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":737880,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, A.I.","contributorId":82676,"corporation":false,"usgs":true,"family":"Johnson","given":"A.I.","email":"","affiliations":[],"preferred":false,"id":737881,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70195987,"text":"70195987 - 1966 - Geohydrologic use of lithofacies maps in glaciated areas","interactions":[],"lastModifiedDate":"2018-03-12T15:50:52","indexId":"70195987","displayToPublicDate":"1996-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3722,"text":"Water Resources Research","onlineIssn":"1944-7973","printIssn":"0043-1397","active":true,"publicationSubtype":{"id":10}},"title":"Geohydrologic use of lithofacies maps in glaciated areas","docAbstract":"<p><span>Subsurface conditions may differ considerably from conditions indicated by surficial geologic maps, particularly in glaciated areas. Therefore, it is advantageous to use a series of lithofacies maps as a sequence of overlays plotted on transparent paper. Such maps permit direct visual determination of the lithology and areal extent of aquifers and indicate areas of possible stream losses or gains. They indicate areas and boundaries of confining layers and, in some places, they may be used to delineate areas of water-table and artesian conditions. They are especially useful in determining buried channels in glaciated areas. The porosity of rock units making up an aquifer may be plotted on a lithofacies map, and the product of the volume of each lithologic type and the porosity provides an estimate of the total water in storage. In addition, if the water-bearing properties are known, the quantity of water moving through an aquifer and the amount available to wells may be determined. Lithofacies maps also aid in the explanation of complex changes in water quality.</span></p>","language":"English","publisher":"AGU","doi":"10.1029/WR002i004p00679","usgsCitation":"Pettyjohn, W.A., and Randich, P., 1966, Geohydrologic use of lithofacies maps in glaciated areas: Water Resources Research, v. 2, no. 4, p. 679-689, https://doi.org/10.1029/WR002i004p00679.","productDescription":"11 p.","startPage":"679","endPage":"689","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352417,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationDate":"2010-07-09","publicationStatus":"PW","scienceBaseUri":"5aff5fabe4b0da30c1bfddc3","contributors":{"authors":[{"text":"Pettyjohn, Wayne A.","contributorId":20724,"corporation":false,"usgs":true,"family":"Pettyjohn","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":730818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randich, P.G.","contributorId":69953,"corporation":false,"usgs":true,"family":"Randich","given":"P.G.","affiliations":[],"preferred":false,"id":730819,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38850,"text":"pp543E - 1966 - Effects of the earthquake of March 27, 1964, in the Copper River Basin area, Alaska","interactions":[{"subject":{"id":38850,"text":"pp543E - 1966 - Effects of the earthquake of March 27, 1964, in the Copper River Basin area, Alaska","indexId":"pp543E","publicationYear":"1966","noYear":false,"chapter":"E","title":"Effects of the earthquake of March 27, 1964, in the Copper River Basin area, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"id":1}],"isPartOf":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"lastModifiedDate":"2022-01-31T20:57:58.244609","indexId":"pp543E","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"543","chapter":"E","title":"Effects of the earthquake of March 27, 1964, in the Copper River Basin area, Alaska","docAbstract":"The Copper River Basin area is in south-central Alaska and covers 17,800 square miles. It includes most of the Copper River Basin and parts of the surrounding Alaska Range and the Talkeetna, Chugach, and Wrangell Mountains.\n\nOn March 27, 1964, shortly after 5:36 p.m. Alaska standard time, a great earthquake having a Richter magnitude of about 8.5 struck south-central Alaska. Computations by the U.S. Coast and Geodetic Survey place the epicenter of the main shock at lat 61.1° N. and long 147.7° W., and the hypocenter, or actual point of origin, from 20 to 50 kilometers below the surface. The epicenter is near the western shore of Unakwik Inlet in northern Prince William Sound; it is 30 miles from the closest point within the area of study and 180 miles from the farthest point.\n\nReleveling data obtained in 1964 after the earthquake indicates that broad areas of south-central Alaska were warped by uplift and subsidence. The configuration of these areas generally parallels the trend of the major tectonic elements of the region. Presumably a large part of this change took place during and immediately after the 1964 earthquake.\n\nThe water level in several wells in the area lowered appreciably, and the water in many became turbid; generally, however, within a few days after the earthquake the water level returned to normal and the suspended sediment settled out. Newspaper reports that the Copper River was completely dammed and Tazlina Lake drained proved erroneous.\n\nThe ice on most lakes was cracked, especially around the margins of the lakes where floating ice broke free from the ice frozen to the shore. Ice on Tazlina, Klutina, and Tonsina Lakes was intensely fractured by waves generated by sublacustrine landslides off the fronts of deltas. These waves stranded large blocks of ice above water level along the shores. River ice was generally cracked in the southern half of the area and was locally cracked in the northern half.\n\nIn the area of study, the majority of the ground cracks occurred within a radius of 100 miles from the epicenter of the earthquake. Ground cracks formed in flood plains of rivers, in deltas, and along the toes of alluvial fans. They also occurred locally in low terraces adjacent to flood plains, in highway and other fill material, along the margins of lakes, along the faces of steep slopes of river bluffs and hillsides, and in areas cleared of vegetation for several years.\n\nThe ground cracks were restricted to areas underlain by unconsolidated deposits where one or more of the following conditions existed: (1) permafrost was absent or deep lying, (2) the ground-water table was near the surface, (3) bedrock was relatively deep lying, and (4) slopes were steep. Because the earthquake occurred in March, seasonal frost was present throughout the area.\n\nDespite the diversity of local conditions, the origin of most of the ground cracks can be explained by the following mechanisms: (1) lateral extension, caused by materials moving toward an unconfined face such as a lakeshore, river bluff, hillside, or terrace escarpment; (2) horizontal compaction, caused by repeated alternate compression and dilation (in the horizontal direction) of materials in flat-lying areas where there are no unconfined faces; (3) differential vertical compaction, caused by the shaking of materials that vary laterally in thickness or character; and (4) combinations of the above.\n\nSnowslides, avalanches, and rockslides were restricted to the mountainous areas surrounding the Copper River Basin. They were especially numerous in the Chugach Mountains which are closest to the epicenter of the earthquake. The large amount of snow and rock debris that has cascaded onto the icefield and glaciers of these mountains, and, probably even more important, the overall disturbance to the ice field will affect the regimen of the glaciers.\n\nMost of the damage to manmade structures occurred in the southern half of the area, and, primarily because of the sparsity of population and manmade structures, property damage was not great and no lives were lost.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: regional effects (Professional Paper 543)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp543E","usgsCitation":"Ferrians, O.J., 1966, Effects of the earthquake of March 27, 1964, in the Copper River Basin area, Alaska: U.S. Geological Survey Professional Paper 543, v, 28 p., https://doi.org/10.3133/pp543E.","productDescription":"v, 28 p.","numberOfPages":"36","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":395184,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99030.htm"},{"id":277744,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543e/index.html"},{"id":65811,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543e/pp543e_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":120235,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0543e/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Copper River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -147.5,61.0 ], [ -147.5,63.0 ], [ -144.0,63.0 ], [ -144.0,61.0 ], [ -147.5,61.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61028f","contributors":{"authors":[{"text":"Ferrians, Oscar J. Jr.","contributorId":42952,"corporation":false,"usgs":true,"family":"Ferrians","given":"Oscar","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":220540,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32612,"text":"pp544B - 1966 - Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska","interactions":[{"subject":{"id":32612,"text":"pp544B - 1966 - Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska","indexId":"pp544B","publicationYear":"1966","noYear":false,"chapter":"B","title":"Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048246,"text":"pp544 - 1966 - The Alaska earthquake, March 27, 1964: effects on hydrologic regimen","indexId":"pp544","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on hydrologic regimen"},"id":1}],"isPartOf":{"id":70048246,"text":"pp544 - 1966 - The Alaska earthquake, March 27, 1964: effects on hydrologic regimen","indexId":"pp544","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on hydrologic regimen"},"lastModifiedDate":"2022-01-31T21:02:54.236706","indexId":"pp544B","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"544","chapter":"B","title":"Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska","docAbstract":"The Anchorage hydrologic system was greatly affected by the seismic shock. Immediate but temporary effects included increased stream discharge, seiche action on lakes, and fluctuations in ground-water levels. Generally, ground-water levels were residually lowered after the initial period of fluctuation. This lowering is attributed either to changes in the discharge zones offshore or to a change in the permeability of the aquifers by seismically induced strain. Water supplies were disrupted temporarily by snowslides on streams and by sanding or turbidity in wells. Salt-water encroachment to wells on Fire Island seems to have increased. The approximate 3.7-foot lowering of land level and the diminished artesian head may permit further salt-water encroachment. Increased pore pressure in the Pleistocene Bootlegger Cove Clay led to liquefaction in silt and sand lenses that contributed to the disastrous bluff landslides. Measurements after the earthquake indicate that most pore pressures are declining, whereas some remain high or are increasing. Subsidence in the area was caused principally by tectonic readjustment, but differential compaction within the Bootlegger Cove Clay contributed to subsidences estimated to be as much as 0.6 foot beneath Anchorage.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Effects on the hydrologic regimen (Professional Paper 544)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp544B","usgsCitation":"Waller, R., 1966, Effects of the March 1964 Alaska earthquake on the hydrology of the Anchorage area, Alaska: U.S. Geological Survey Professional Paper 544, Report: 18 p.; 1 Plate: 37.13 x 41.12 inches, https://doi.org/10.3133/pp544B.","productDescription":"Report: 18 p.; 1 Plate: 37.13 x 41.12 inches","numberOfPages":"18","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":119428,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0544b/report-thumb.jpg"},{"id":277808,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0544b/pp544b_text.pdf"},{"id":277809,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0544b/pp544b_plate1.pdf"},{"id":277810,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0544b/index.html"},{"id":395185,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4594.htm"}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -150.2863,60.7338 ], [ -150.2863,61.4839 ], [ -148.46,61.4839 ], [ -148.46,60.7338 ], [ -150.2863,60.7338 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c890","contributors":{"authors":[{"text":"Waller, Roger M.","contributorId":90353,"corporation":false,"usgs":true,"family":"Waller","given":"Roger M.","affiliations":[],"preferred":false,"id":208793,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32676,"text":"pp542C - 1966 - Effects of the earthquake of March 27, 1964, at Valdez, Alaska","interactions":[{"subject":{"id":32676,"text":"pp542C - 1966 - Effects of the earthquake of March 27, 1964, at Valdez, Alaska","indexId":"pp542C","publicationYear":"1966","noYear":false,"chapter":"C","title":"Effects of the earthquake of March 27, 1964, at Valdez, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"id":1}],"isPartOf":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"lastModifiedDate":"2022-04-28T19:29:26.11427","indexId":"pp542C","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"542","chapter":"C","title":"Effects of the earthquake of March 27, 1964, at Valdez, Alaska","docAbstract":"<p>Valdez is situated on the seaward edge of a large outwash delta composed of a thick section of saturated silty sand and gravel. The earthquake of March 27, 1964, triggered a massive submarine slide, involving approximately 98 million cubic yards of material that destroyed the harbor facilities and nearshore installations. Waves generated by the slide and subsequent strong seiches did additional damage in the downtown area. Stresses generated by the seismic shocks and the slide developed an extensive system of fissures throughout the unconsolidated deposits at the head of the fiord. These fissures plus the shocks caused structural damage to many of the buildings in Valdez and destroyed the sewer and water systems. Removal of support from the face of the delta by submarine sliding allowed some of the material to move seaward and caused parts of the shore area to subside below high-tide level.</p>\n</br>\n<p>A site for relocating the town of Valdez has been designated. It is situated on the Mineral Creek fan--an area underlain by coarse alluvial gravel. This relocation site is protected from sea waves by a series of bedrock ridges and islands that also provide a resistant buttress retaining and protecting the toe of the fan from danger of sliding or slumping. The absence of evidence of ground breakage on the Mineral Creek fan indicates that the coarse subsoils at the relocation site react favorably under seismic conditions.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Effects on communities (Professional Paper 542)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp542C","usgsCitation":"Coulter, H.W., and Migliaccio, R.R., 1966, Effects of the earthquake of March 27, 1964, at Valdez, Alaska: U.S. Geological Survey Professional Paper 542, Report: viii, 36 p.; 3 Plates: 38.5 x 23.76 inches or smaller, https://doi.org/10.3133/pp542C.","productDescription":"Report: viii, 36 p.; 3 Plates: 38.5 x 23.76 inches or smaller","numberOfPages":"46","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":399841,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4585.htm"},{"id":60587,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0542c/pp542c_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60586,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0542c/pp542c_plate3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60585,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0542c/pp542c_plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60584,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0542c/pp542c_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119322,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0542c/report-thumb.jpg"},{"id":104503,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0542c/index.html","linkFileType":{"id":5,"text":"html"},"description":"4585"}],"scale":"6000","country":"United States","state":"Alaska","city":"Valdez","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -146.425549,61.07992 ], [ -146.425549,61.15779 ], [ -146.213554,61.15779 ], [ -146.213554,61.07992 ], [ -146.425549,61.07992 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610344","contributors":{"authors":[{"text":"Coulter, Henry Welty","contributorId":85872,"corporation":false,"usgs":true,"family":"Coulter","given":"Henry","email":"","middleInitial":"Welty","affiliations":[],"preferred":false,"id":208908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Migliaccio, Ralph R.","contributorId":22667,"corporation":false,"usgs":true,"family":"Migliaccio","given":"Ralph","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":208907,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32677,"text":"pp542D - 1966 - Effects of the earthquake of March 27, 1964, in the Homer area, Alaska","interactions":[{"subject":{"id":32677,"text":"pp542D - 1966 - Effects of the earthquake of March 27, 1964, in the Homer area, Alaska","indexId":"pp542D","publicationYear":"1966","noYear":false,"chapter":"D","title":"Effects of the earthquake of March 27, 1964, in the Homer area, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"id":1}],"isPartOf":{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","indexId":"pp542","publicationYear":"1969","noYear":false,"title":"The Alaska earthquake, March 27, 1964: Effects on communities"},"lastModifiedDate":"2022-06-06T20:19:16.156352","indexId":"pp542D","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"542","chapter":"D","title":"Effects of the earthquake of March 27, 1964, in the Homer area, Alaska","docAbstract":"<p>The March 27, 1964, earthquake shook the Homer area for about 3 minutes. Land effects consisted of a 2- to 6-foot subsidence of the mainland and Homer Spit, one earthflow at the mouth of a canyon, several landslides on the Homer escarpment and along the sea bluffs, and minor fissuring of the ground, principally at the edges of bluffs and on Homer Spit. Hydrologic effects consisted of at least one and possibly two submarine landslides at the end of the spit, seiche waves in Kachemak Bay, ice breakage on Beluga Lake, sanding of wells, and a temporary loss of water in some wells.</p>\n</br>\n<p>Seismic damage to the community was light in comparison with that of other communities closer to the epicenter. One submarine landslide, however, took out most of the harbor breakwater. The greatest damage was due to the subsidence of the spit, both tectonically (2–3 ft) and by differential compaction or lateral spreading (an additional 1–4 ft). Higher tides now flood much of the spit. The harbor and dock had to be replaced, and buildings on the end of the spit had to be elevated. Protection works for other buildings and the highway were needed. These works included application of fill to raise the highway and parts of the spit above high tides. Reconstruction costs and disaster loans totaled about $2½ million, but this amount includes added improvement costs over preexisting values.</p>\n</br>\n<p>Homer Spit in particular and the Homer area in general rank as areas where precautions must be taken in selecting building sites. The hazards of landslides, earthflows, compaction and submarine slumping—all of which might be triggered by an earthquake—should be considered in site selection.</p>\n</br>\n<p>In plan, Homer Spit resembles a scimitar with its curving blade pointed seaward. It is about 4 miles long and as much as 1,500 feet wide. The spit is composed largely of gravel intermixed with some sand.</p>\n</br>\n<p>After the earthquake and the resulting tectonic subsidence and compaction, much of the spit was below high-tide levels and consequently flooded periodically. The entire beach face has retreated. Much of the material eroded from the beach has been redeposited to form a new storm or frontal berm, locally migrating around buildings and covering roads. Beach recession of 10–15 feet is probably the overall average; maximum recession 1 year after the earthquake was 56 feet along one limited section of the distal end of the spit.</p>\n</br>\n<p>Subsidence of the mainland has caused accelerated erosion of the beaches and headlands that have been—and are—source areas for the material deposited on Homer Spit. The resulting increased supply of gravel and sand probably will cause the spit to widen gradually on the Cook Inlet side. Similarly, the new frontal berm will probably grow to a height sufficient to prevent overtopping by all but the larger storm swashes. The nature of shore processes on the spit has not been materially altered by subsidence, but the rates of erosion and deposition have been accelerated. The lasting effect of subsidence (excluding flooding) will be enlargement of the beach on the Cook Inlet side and gradual wasting of the beach on the bay side of the spit.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Effects on communities (Professional Paper 542)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp542D","usgsCitation":"Waller, R., and Stanley, K.W., 1966, Effects of the earthquake of March 27, 1964, in the Homer area, Alaska: U.S. Geological Survey Professional Paper 542, Report: vi, 28 p.; Plate: 18.00 × 18.83 inches, https://doi.org/10.3133/pp542D.","productDescription":"Report: vi, 28 p.; Plate: 18.00 × 18.83 inches","numberOfPages":"36","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":60589,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0542d/pp542d_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399848,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4586.htm"},{"id":60588,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0542d/pp542d_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0542d/report-thumb.jpg"}],"scale":"2400","country":"United States","state":"Alaska","city":"Homer","otherGeospatial":"Homer Spit","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -151.655037,59.598268 ], [ -151.655037,59.681295 ], [ -151.403995,59.681295 ], [ -151.403995,59.598268 ], [ -151.655037,59.598268 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db6106cc","contributors":{"authors":[{"text":"Waller, Roger M.","contributorId":90353,"corporation":false,"usgs":true,"family":"Waller","given":"Roger M.","affiliations":[],"preferred":false,"id":208910,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stanley, Kirk W.","contributorId":8900,"corporation":false,"usgs":true,"family":"Stanley","given":"Kirk","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":208909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38819,"text":"pp544A - 1966 - Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska","interactions":[{"subject":{"id":38819,"text":"pp544A - 1966 - Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska","indexId":"pp544A","publicationYear":"1966","noYear":false,"chapter":"A","title":"Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska"},"predicate":"IS_PART_OF","object":{"id":70048246,"text":"pp544 - 1966 - The Alaska earthquake, March 27, 1964: effects on hydrologic regimen","indexId":"pp544","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on hydrologic regimen"},"id":1}],"isPartOf":{"id":70048246,"text":"pp544 - 1966 - The Alaska earthquake, March 27, 1964: effects on hydrologic regimen","indexId":"pp544","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on hydrologic regimen"},"lastModifiedDate":"2022-02-15T20:52:49.535943","indexId":"pp544A","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"544","chapter":"A","title":"Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska","docAbstract":"The earthquake of March 27, 1964, greatly affected the hydrology of Alaska and many other parts of the world. Its far-reaching effects were recorded as water-level fluctuations in gages operated on water wells and streams. The close-in effects were even more striking, however; sediment-laden ground water erupted at the surface, and even ice-covered lakes and streams responded by seiching. Lake and river ice was broken for distances of 450 miles from the epicenter by seismic shock and seiche action. The surging action temporarily dewatered some lakes. Fissuring of streambeds and lakeshores, in particular, caused a loss of water, and hydrologic recovery took weeks in some places. Landslides and snow avalanches temporarily blocked streams and diverted some permanently. The only stream or lake structures damaged were a tunnel intake and two earthen dams. The winter conditions-low stages of water and the extensive ice cover on lakes and streams-at the time of the earthquake greatly reduced the damaging potential. Ground water was drastically affected mostly in unconsolidated aquifers for at least 160 miles from the epicenter. Within 100 miles of the epicenter, vast quantities of sediment-laden water were ejected in most of the flood plains of the glaciofluvial valleys. A shallow water table and confinement by frost seemed to be requirements for the ejections, which were commonly associated with cratering and subsidence of the unconsolidated material. Subsidence was also common near the disastrous submarine landslides, and was probably caused by loss of water pressure and by lateral spreading of sediments. Effects on ground water in bedrock were not determinable because of lack of data and accessibility, particularly within 50 miles of the epicenter. Deep aquifers in unconsolidated sediments, which in most areas are under high hydrostatic pressure, were also greatly affected. Postearthquake water levels for a year were compared with long-term prequake levels to show permanent changes in an aquifer system. At Anchorage and in parts of the kenai Peninsula, artesian-pressure levels dropped as much as 15 feet. These lower pressures were probably caused either by grain rearrangement which increased the porosity within the aquifer or by a displacement of material that allowed water to discharge more freely at the submarine terminus of the aquifer. Seismically induced pressure on ground water was instrumental in causing most of the disastrous slides. Water quality was not changed except for temporary increases in turbidity in wells and streams. The sediment load in streams during the April spring run-off appeared to be greatly increased over previous years.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Effects on the hydrologic regimen (Professional Paper 544)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp544A","usgsCitation":"Waller, R., 1966, Effects of the March 1964 Alaska earthquake on the hydrology of south-central Alaska: U.S. Geological Survey Professional Paper 544, 28 p., https://doi.org/10.3133/pp544A.","productDescription":"28 p.","numberOfPages":"28","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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,{"id":38787,"text":"pp550B - 1966 - Geological Survey research 1966, Chapter B","interactions":[],"lastModifiedDate":"2025-08-25T20:26:52.136612","indexId":"pp550B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"550","chapter":"B","title":"Geological Survey research 1966, Chapter B","docAbstract":"<p>This collection of 43 short papers is the first published chapter of 'Geological Survey Research 1966.' The papers report on scientific and economic results of current work by members of the Conservation, Geologic, Topographic, and Water Resources Divisions of the U.S. Geological Survey. Chapter A, to be published later in the year, will present a summary of significant results of work done during fiscal year 1966, together with lists of investigations in progress, reports published, cooperating agencies, and Geological Survey offices. 'Geological Survey Research 1966' is the seventh volume of the annual series Geological Survey Research. The six volumes already published are listed below, with their series designations. Geological Survey Research 1960-Prof. Paper 400 Geological Survey Research 1961-Prof. Paper 424 Geological Survey Research 1962-Prof. Paper 450 Geological Survey Research 1963-Prof. Paper 475 Geological Survey Research 1964-Prof. Paper 501 Geological Survey Research 1965-Prof. Paper 525</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey Research 1966","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp550B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Geological Survey research 1966, Chapter B: U.S. Geological Survey Professional Paper 550, v, 227 p., https://doi.org/10.3133/pp550B.","productDescription":"v, 227 p.","numberOfPages":"234","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":170056,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0550b/report-thumb.jpg"},{"id":403306,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27597.htm","text":"Unconformity between gneissic granodiorite and overlying Yavapai series (older Precambrian), central Arizona","linkFileType":{"id":5,"text":"html"}},{"id":65660,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0550b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":494814,"rank":17,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27611.htm","text":"Uranium-lead and potassium-argon ages of parts of the Amargosa thrust complex, Death Valley, California","linkFileType":{"id":5,"text":"html"}},{"id":494812,"rank":15,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27609.htm","text":"Trona in the Wilkins Peak Member of the Green River Formation, southwestern Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":494810,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27607.htm","text":"Structural control of wind gaps and water gaps and of stream capture in the Stroudsberg area, Pennsylvania and New Jersey","linkFileType":{"id":5,"text":"html"}},{"id":494808,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27605.htm","text":"Stratigraphic relations of Upper Cretaceous rocks, Lamont - Bairoil area, south-central Wyoming","linkFileType":{"id":5,"text":"html"}},{"id":494807,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27604.htm","text":"Tertiary extrusive volcanic rocks in Middle Park, Grand County, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":494804,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27601.htm","text":"Domes in the Atlantic Coastal Plain east of Trenton, New Jersey","linkFileType":{"id":5,"text":"html"}},{"id":494815,"rank":18,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27612.htm","text":"Distribution and geologic structure of Triassic rocks in the Bay of Fundy and the northeastern part of the Gulf of Maine","linkFileType":{"id":5,"text":"html"}},{"id":494802,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27599.htm","text":"Cattle Creek anticline, a salt diapir near Glenwood Springs, Colorado","linkFileType":{"id":5,"text":"html"}},{"id":494803,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27600.htm","text":"Devonian stratigraphy of the Confusion Range, west-central Utah","linkFileType":{"id":5,"text":"html"}},{"id":494801,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27598.htm","text":"Tectonic movement in the Grapevine area, Kern County, California","linkFileType":{"id":5,"text":"html"}},{"id":494813,"rank":16,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27610.htm","text":"Pre-Wisconsin glacial deposits in northern Kentucky","linkFileType":{"id":5,"text":"html"}},{"id":494811,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27608.htm","text":"Phosphate deposits in the basal beds of the Maquoketa Shale near Dubuque, Iowa","linkFileType":{"id":5,"text":"html"}},{"id":494809,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27606.htm","text":"Milnor Channel, an ice-marginal course of the Sheyenne River, North Dakota","linkFileType":{"id":5,"text":"html"}},{"id":494806,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27603.htm","text":"Stratigraphic significance of Tertiary fossils from the Orca Group in the Prince William Sound region, Alaska","linkFileType":{"id":5,"text":"html"}},{"id":494805,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_27602.htm","text":"Graptolite-bearing Silurian rocks of the Houlton - Smyrna Mills area, Aroostook County, Maine","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688037","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":529883,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33129,"text":"b1234 - 1966 - Bibliography of North American geology, 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"b1234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1234","title":"Bibliography of North American geology, 1964","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1234","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1966, Bibliography of North American geology, 1964: U.S. Geological Survey Bulletin 1234, 944 p, https://doi.org/10.3133/b1234.","productDescription":"944 p","costCenters":[],"links":[{"id":247374,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1234/report.pdf","size":"45083","linkFileType":{"id":1,"text":"pdf"}},{"id":251821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1234/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629913","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":529455,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32628,"text":"pp543A - 1966 - Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska","interactions":[{"subject":{"id":32628,"text":"pp543A - 1966 - Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska","indexId":"pp543A","publicationYear":"1966","noYear":false,"chapter":"A","title":"Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"id":1}],"isPartOf":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"lastModifiedDate":"2022-06-28T19:38:48.241938","indexId":"pp543A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"543","chapter":"A","title":"Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska","docAbstract":"The March 27, 1964, earthquake dislodged slides from nine deltas in Kenai Lake, south-central Alaska. Sliding removed protruding parts of deltas-often the youngest parts-and steepened delta fronts, increasing the chances of further sliding. Fathograms show that debris from large slides spread widely over the lake floor, some reaching the toe of the opposite shore; at one place debris traveled 5,000 feet over the horizontal lake floor.\n\nSlides generated two kinds of local waves: a backfill and far-shore wave. Backfill waves were formed by water that rushed toward the delta to fill the void left by the sinking slide mass, overtopped the slide scrap, and came ashore over the delta. Some backfill waves had runup heights of 30 feet and ran inland more than 300 feet, uprooting and breaking off large trees. Far-shore waves hit the shore opposite the slides. They were formed by slide debris that crossed the lake floor and forced water ahead of it, which then ran up the opposite slope, burst above the lake surface, and struck the shore. One far-shore wave had a runup height of 72 feet.\n\nKenai Lake was tilted and seiched; a power spectrum analysis of a limnogram shows a wave having the period of the calculated uninodal seiche (36 minutes) and several shorter period waves. In constricted and shallow reaches, waves caused by seiching had 20- and 30-foot runup heights.\n\nDeep lateral spreading of sediments toward delta margins displaced deeply driven railroad-bridge piles, and set up stress fields in the surface sediments which resulted in the formation of many shear and some tension fractures on the surface of two deltas.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Regional effects (Professional Paper 543)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp543A","usgsCitation":"McCulloch, D.S., 1966, Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska: U.S. Geological Survey Professional Paper 543, Report: vi, 41 p.; 2 Plates: 49.5 x 17.5 inches and 20.9 x 16.87 inches, https://doi.org/10.3133/pp543A.","productDescription":"Report: vi, 41 p.; 2 Plates: 49.5 x 17.5 inches and 20.9 x 16.87 inches","numberOfPages":"49","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":402630,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4590.htm","linkFileType":{"id":5,"text":"html"}},{"id":277653,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543a/index.html"},{"id":60502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543a/pp543a_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60501,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0543a/pp543a_plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60500,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0543a/pp543a_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0543a/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kenai Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -149.835071,60.335719 ], [ -149.835071,60.494895 ], [ -149.346197,60.494895 ], [ -149.346197,60.335719 ], [ -149.835071,60.335719 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee60a","contributors":{"authors":[{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":208818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39123,"text":"pp272G - 1966 - Evaporation study in a humid region, Lake Michie, North Carolina","interactions":[],"lastModifiedDate":"2017-01-11T11:33:34","indexId":"pp272G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"272","chapter":"G","title":"Evaporation study in a humid region, Lake Michie, North Carolina","docAbstract":"The mass-transfer and water-budget techniques of calibrating a reservoir for evaporation were evaluated through a study of Lake Michie, N.C. The techniques appear adequate for estimation of lake evaporation and net seepage in humid regions where lake storage is affected by streamflow and ground-water seepage, under conditions no more adverse than those affecting Lake Michie.\r\n\r\nThe analysis of 25 months of mass-transfer and water-budget data collected at Lake Michie indicates pronounced seasonal variation in both evaporation and seepage.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Studies of evaporation","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp272G","usgsCitation":"Turner, J., 1966, Evaporation study in a humid region, Lake Michie, North Carolina: U.S. Geological Survey Professional Paper 272, p. 137-150, https://doi.org/10.3133/pp272G.","productDescription":"p. 137-150","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":66611,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0272g/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122162,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0272g/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Lake Michie","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.95015716552734,\n              36.092389668927595\n            ],\n            [\n              -78.95015716552734,\n              36.216856162150144\n            ],\n            [\n              -78.73867034912108,\n              36.216856162150144\n            ],\n            [\n              -78.73867034912108,\n              36.092389668927595\n            ],\n            [\n              -78.95015716552734,\n              36.092389668927595\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6119e2","contributors":{"authors":[{"text":"Turner, J.F. Jr.","contributorId":88399,"corporation":false,"usgs":true,"family":"Turner","given":"J.F.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":220997,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37659,"text":"tp3 - 1966 - Observations on the marine cladoceran Penilia avirostris in northwestern Atlantic waters","interactions":[],"lastModifiedDate":"2012-02-02T00:09:57","indexId":"tp3","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":89,"text":"Technical Paper","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"3","title":"Observations on the marine cladoceran Penilia avirostris in northwestern Atlantic waters","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Croce, N.D., 1966, Observations on the marine cladoceran Penilia avirostris in northwestern Atlantic waters: Technical Paper 3, 37 p. : ill. ; 26 cm.","productDescription":"37 p. : ill. ; 26 cm.","costCenters":[],"links":[{"id":164821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696417","contributors":{"authors":[{"text":"Croce, Norberto Della","contributorId":61483,"corporation":false,"usgs":true,"family":"Croce","given":"Norberto","email":"","middleInitial":"Della","affiliations":[],"preferred":false,"id":218424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":40714,"text":"ofr66152 - 1966 - Records of selected wells, springs, test holes, materials tests, and chemical analyses of water in the lower Merrimack River basin, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:10:50","indexId":"ofr66152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-152","title":"Records of selected wells, springs, test holes, materials tests, and chemical analyses of water in the lower Merrimack River basin, New Hampshire","language":"ENGLISH","doi":"10.3133/ofr66152","usgsCitation":"Weigle, J., and Kranes, R., 1966, Records of selected wells, springs, test holes, materials tests, and chemical analyses of water in the lower Merrimack River basin, New Hampshire: U.S. Geological Survey Open-File Report 66-152, 44 p., https://doi.org/10.3133/ofr66152.","productDescription":"44 p.","costCenters":[],"links":[{"id":171204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63570d","contributors":{"authors":[{"text":"Weigle, J.M.","contributorId":20400,"corporation":false,"usgs":true,"family":"Weigle","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":223841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kranes, Richard","contributorId":23811,"corporation":false,"usgs":true,"family":"Kranes","given":"Richard","email":"","affiliations":[],"preferred":false,"id":223842,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40711,"text":"ofr66157 - 1966 - Effect of treated effluent diversion on Yahara River flow, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-13T12:32:32","indexId":"ofr66157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-157","title":"Effect of treated effluent diversion on Yahara River flow, Wisconsin","docAbstract":"<p>Before December 1958 the treated sewage effluent from the Madison, Wisconsin, metropolitan area was discharged into the Yahara River at the north end of Lake Waubesa, which is upstream from the USGS gaging station on the Yahara River near McFarland, Wis. Since December 1958 the effluent has been diverted southward from the sewage treatment plant into Badfish Creek and enters the lower reach of Yahara River, thus byrpassing the gaging station. The purpose of this report is to demonstrate the effect that this diversion seems to have on the flow of the Yahara River near McFarland. Indirectly, it also demonstrates the effect on streamflow of withdrawing ground water for use in the Madison metropolitan area since the treated effluent is primarily the major portion of the used ground water.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr66157","usgsCitation":"Young, K., 1966, Effect of treated effluent diversion on Yahara River flow, Wisconsin: U.S. Geological Survey Open-File Report 66-157, 23 p., https://doi.org/10.3133/ofr66157.","productDescription":"23 p.","numberOfPages":"23","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":98243,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0157/report.pdf","size":"1509","linkFileType":{"id":1,"text":"pdf"}},{"id":171098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0157/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","otherGeospatial":"Yahara River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.36965942382812,\n              43.3101903843356\n            ],\n            [\n              -89.55230712890624,\n              43.17814279946058\n            ],\n            [\n              -89.65805053710938,\n              43.08995208151042\n            ],\n            [\n              -89.44244384765625,\n              42.943355168255806\n            ],\n            [\n              -89.25979614257812,\n              42.898100636939276\n            ],\n            [\n              -89.22821044921875,\n              42.819580715795915\n            ],\n            [\n              -89.15817260742188,\n              42.78129125156277\n            ],\n            [\n              -89.11148071289062,\n              42.78431496548022\n            ],\n            [\n              -89.07852172851562,\n              42.790361950280925\n            ],\n            [\n              -89.0716552734375,\n              42.81353658623225\n            ],\n            [\n              -89.0936279296875,\n              42.89105805581562\n            ],\n            [\n              -89.17739868164062,\n              42.99761672705504\n            ],\n            [\n              -89.32159423828125,\n              43.17513839170044\n            ],\n            [\n              -89.36141967773438,\n              43.26020603533185\n            ],\n            [\n              -89.36965942382812,\n              43.3101903843356\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62543f","contributors":{"authors":[{"text":"Young, K.B.","contributorId":77997,"corporation":false,"usgs":true,"family":"Young","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":223836,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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