{"pageNumber":"5785","pageRowStart":"144600","pageSize":"25","recordCount":165657,"records":[{"id":5220821,"text":"5220821 - 1969 - The killing efficiency of soft iron shot","interactions":[],"lastModifiedDate":"2012-02-02T00:14:58","indexId":"5220821","displayToPublicDate":"2010-06-16T12:17:28","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3638,"text":"Transactions of the North American Wildlife and Natural Resources Conference","active":true,"publicationSubtype":{"id":10}},"title":"The killing efficiency of soft iron shot","docAbstract":"A cooperative research effort between the ammunition industry and the Bureau of Sport Fisheries and Wildlife is aimed at finding a suitable non-toxic substitute for lead shot. A contract study by an independent research organization evaluated ways of coating or detoxifying lead shot or replacing it with another metal. As a result of that study, the only promising candidate is soft iron. Previous tests of hard iron shot had suggested that its killing effectiveness was poor at longer ranges due to the lower density. In addition, its hardness caused excessive damage to shotgun barrels.  A unique, automated shooting facility was constructed at the Patuxent Wildlife Research Center to test the killing effectiveness of soft iron shot under controlled conditions. Tethered game-farm mallards were transported across a shooting point in a manner simulating free flight. A microswitch triggered a mounted shotgun so that each shot was 'perfect.' A soft iron shot, in Number 4 size, was produced by the ammunition industry and loaded in 12-gauge shells to give optimum ballistic performance. Commercial loads of lead shot in both Number 4 and Number 6 size were used for comparison.  A total of 2,010 ducks were shot at ranges of 30 to 65 yards and at broadside and head-on angles in a statistically designed procedure. The following data were recorded for each duck: time until death, broken wing or leg bones, and number of embedded shot. Those ducks not killed outright were held for 10 days. From these data, ducks were categorized as 'probably bagged,' 'probably lost cripples,' or survivors.  The test revealed that the killing effectiveness of this soft iron shot was superior to its anticipated performance and close to that obtained with commercial lead loads containing an equal number of pellets. Bagging a duck, in terms of rapid death or broken wing, was primarily dependent on the probability of a shot striking that vital area, and therefore a function of range. There was no indication that iron shot would result in greater crippling loss.  Despite the apparent effectiveness of this iron shot, transition to its use in waterfowl hunting is not now possible. The sample used for this test was produced by a laboratory procedure that is unsuitable for manufacture. There is no process for producing soft iron shot in the quantities needed. Industry is doing its best to resolve this problem.  ","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the North American Wildlife and Natural Resources Conference","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","usgsCitation":"Andrews, R., and Longcore, J.R., 1969, The killing efficiency of soft iron shot: Transactions of the North American Wildlife and Natural Resources Conference, v. 34, p. 337-345.","productDescription":"337-345","startPage":"337","endPage":"345","numberOfPages":"9","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199398,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64b250","contributors":{"authors":[{"text":"Andrews, R.","contributorId":62662,"corporation":false,"usgs":true,"family":"Andrews","given":"R.","email":"","affiliations":[],"preferred":false,"id":332554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Longcore, J. R. 0000-0003-4898-5438","orcid":"https://orcid.org/0000-0003-4898-5438","contributorId":43835,"corporation":false,"usgs":true,"family":"Longcore","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":332553,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221265,"text":"5221265 - 1969 - Nationwide residues of organochlorine pesticides in wings of mallards and black ducks","interactions":[],"lastModifiedDate":"2018-02-12T11:52:48","indexId":"5221265","displayToPublicDate":"2010-06-16T12:17:28","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3038,"text":"Pesticides Monitoring Journal","onlineIssn":" 0031-615","printIssn":" 0031-615","active":true,"publicationSubtype":{"id":10}},"title":"Nationwide residues of organochlorine pesticides in wings of mallards and black ducks","docAbstract":"Nationwide monitoring of organochlorine pesticides in wings of more than 24,000 mallards and black ducks bagged during the1965 and 1966 hunting seasons showed DDE to be the predominant residue, followed in order by DDT, DDD, dieldrin, and heptachlor epoxide.  Residues were generally highest in wings from the Atlantic and Pacific Flyways, and lowest in the Central Flyway.  DDE was reported for every State and was notably high in wings from New Jersey, Massachusetts, Connecticut, Rhode Island, New York, Pennsylvania, Alabama, California, and Utah.  Dieldrin residues were prevalent in wings from Arkansas, Texas, Utah, California, and several Stales in the Atlantic Flyway.","language":"English","publisher":"Federal Committee on Pest Control","publisherLocation":"Washington, D.C.","issn":"0031-6156","usgsCitation":"Heath, R.G., 1969, Nationwide residues of organochlorine pesticides in wings of mallards and black ducks: Pesticides Monitoring Journal, v. 3, no. 2, p. 115-123.","productDescription":"9 p.","startPage":"115","endPage":"123","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193906,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269743,"type":{"id":11,"text":"Document"},"url":"https://biodiversitylibrary.org/page/26094085"}],"country":"United States","volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69832e","contributors":{"authors":[{"text":"Heath, Robert G.","contributorId":103719,"corporation":false,"usgs":true,"family":"Heath","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":333439,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5230026,"text":"5230026 - 1969 - The Breeding Bird Survey, 1967 and 1968","interactions":[],"lastModifiedDate":"2012-02-02T00:15:23","indexId":"5230026","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1969","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":"124","title":"The Breeding Bird Survey, 1967 and 1968","docAbstract":"In the Breeding Bird Survey of North America, cooperators ran 982 survey routes in 1967 and 1,174 in 1968. All States except Hawaii and all Canadian Provinces except Newfoundland were included. Roadside routes are selected at random within 1-degree blocks of latitude and longitude. Each 24 1/2-mile route, with 3-minute stops spaced half a mile apart, is driven by automobile. All birds heard or seen at the stops are recorded on special forms, and the data are transferred to magnetic tape for analysis. The average number of birds of each species per route is tabulated by State and Province, presenting for the first time a record of the comparative abundance of each species across the continent. The sample size is given for each species recorded. A sophisticated analysis program, here employed for the first time, is used to compute weighted mean values of the survey results for selected species at the State, stratum, regional, and continental level. The statistical significance of year-to-year changes at the 80, 90, 95, and 99 percent levels of probability are part of the computer output. An index for comparing populations of each species from year to year is established, with 1968 as the base year. Maps show the breeding range and comparative abundance of selected species.","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Robbins, C., and Van Velzen, W., 1969, The Breeding Bird Survey, 1967 and 1968: Special Scientific Report  - Wildlife 124, 107.","productDescription":"107","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":112125,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/coo.31924055486793?urlappend=%3Bseq=47"},{"id":202791,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627adf","contributors":{"authors":[{"text":"Robbins, C.S.","contributorId":53907,"corporation":false,"usgs":true,"family":"Robbins","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":343383,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Velzen, W.T.","contributorId":72080,"corporation":false,"usgs":true,"family":"Van Velzen","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":343384,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5211359,"text":"5211359 - 1969 - Statement","interactions":[],"lastModifiedDate":"2012-02-02T00:15:20","indexId":"5211359","displayToPublicDate":"2009-06-09T09:23:19","publicationYear":"1969","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Statement","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hearing before the Subcommittee on Fisheries and Wildlife Conservation of the Committee on Merchant Marine and Fisheries, U.S. House of Representatives, 91st Congress, on the recent outbreak of botulism in the Tulare Lake Basin of California's Joaquin Valley.  Serial No. 91-8","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","usgsCitation":"Herman, C.M., 1969, Statement, chap. <i>of</i> Hearing before the Subcommittee on Fisheries and Wildlife Conservation of the Committee on Merchant Marine and Fisheries, U.S. House of Representatives, 91st Congress, on the recent outbreak of botulism in the Tulare Lake Basin of California's Joaquin Valley.  Serial No. 91-8, p. 11-14.","productDescription":"33 ","startPage":"11","endPage":"14","numberOfPages":"33","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200847,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e474f","contributors":{"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":330838,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5210062,"text":"5210062 - 1969 - Blood protozoa of free-living birds","interactions":[],"lastModifiedDate":"2012-02-02T00:15:14","indexId":"5210062","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1969","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Blood protozoa of free-living birds","docAbstract":"Blood protozoa were first reported from wild birds in 1884. Since then numerous surveys throughout the world have demonstrated their presence in a wide variety of hosts and localities with continuing designations of new species. Taxonomic determinations include parasites in the genera Plasmodium, Haemoproteus, Leucocytozoon, Babesia, Lankesterella and Trypanosoma.  Transmission of Plasmodium by mosquitoes was demonstrated with a bird parasite before these insects were proven as vectors of human malaria. All the genera under consideration require an insect vector to complete their life-cycles and susceptible vectors have been demonstrated. Most experimental work on the blood protozoa of birds has been carried on with captive birds. An extensive volume of research has been conducted on Plasmodium because of its close similarity to malaria in man. Field studies that would provide information on the epizootiology of occurrence of these parasites in wild populations have been very limited, mainly confined to single blood film surveys. Such data are inadequate to provide an understanding of true prevalence or incidence or of factual knowledge of their impact on the wild population. Mechanisms for procuring such information are available in some cases and can be developed to fit other situations. Isodiagnosis, inoculation of blood from wild birds into susceptible captive hosts, has revealed a prevalence of over 60 % for Plasmodium in situations where microscope examination of single peripheral blood preparations yielded less than 1 %. Culture of bone marrow collected by biopsy demonstrates high prevalence of trypanosomes even when none are evident from microscopic examination of blood. Often preparations of tissues collected at necropsy reveal Leucocytozoon and Lankesterella when examination of peripheral blood gave no indication of infection. Methods developed by bird ringers provide techniques for obtaining repeat examinations of free-living birds that can yield further pertinent data. The use that has been made of these techniques, beyond the mere procurement of a single blood film, is reviewed from the standpoint of providing knowledge of the epizootiology of the blood protozoa of birds and their further potential is projected.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Diseases in free-living wild animals: the proceedings of a symposium held at the Zoological Society of London on 9 and 10 May 1968","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Academic Press","publisherLocation":"London","collaboration":"DLC OCLC  54304 ; NLM OCLC  38231442","usgsCitation":"Herman, C.M., 1969, Blood protozoa of free-living birds, chap. <i>of</i> Diseases in free-living wild animals: the proceedings of a symposium held at the Zoological Society of London on 9 and 10 May 1968, p. 177-193.","productDescription":"xxiv, 332","startPage":"177","endPage":"193","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201223,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db60769a","contributors":{"editors":[{"text":"McDiarmid, Archibald","contributorId":112080,"corporation":false,"usgs":true,"family":"McDiarmid","given":"Archibald","email":"","affiliations":[],"preferred":false,"id":505957,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Herman, C. M.","contributorId":101335,"corporation":false,"usgs":true,"family":"Herman","given":"C.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":327699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047559,"text":"70047559 - 1969 - Water resources investigation program for Rio Aconcagua Valley, Chile","interactions":[],"lastModifiedDate":"2026-01-30T20:14:29.119392","indexId":"70047559","displayToPublicDate":"2009-01-01T10:25:00","publicationYear":"1969","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":"Water resources investigation program for Rio Aconcagua Valley, Chile","docAbstract":"This report, prepared at the request of the Government of Chile under the auspices of the U. S. Agency for International Development (US AID), is based on a 2-month assignment (Oct. 22 to Dec. 31, 1969) of the author and outlines a program of water resources studies. The study program, if followed to its conclusion, will provide the basic hydrologic and hydrogeologic information and analysis essential for planning optimum future development and use of the water resources of the valley.","language":"English, Spanish","publisher":"U.S. Geological Survey","publisherLocation":"Santiago, Chile","doi":"10.3133/70047559","collaboration":"Prepared in cooperation with the Government of Chile","usgsCitation":"Moore, J.E., 1969, Water resources investigation program for Rio Aconcagua Valley, Chile: Open-File Report, iii, 59 p., https://doi.org/10.3133/70047559.","productDescription":"iii, 59 p.","numberOfPages":"66","costCenters":[],"links":[{"id":276365,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70047559/report-thumb.jpg"},{"id":277871,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70047559/report.pdf"}],"country":"Chile","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.9962,-34.0071 ], [ -71.9962,-31.8356 ], [ -69.9911,-31.8356 ], [ -69.9911,-34.0071 ], [ -71.9962,-34.0071 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a0404e4b0026c2bc11d26","contributors":{"authors":[{"text":"Moore, John Ezra","contributorId":93582,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"Ezra","affiliations":[],"preferred":false,"id":482400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039428,"text":"70039428 - 1969 - Activities and services of the U.S. Geological Survey, Denver area, Colorado","interactions":[],"lastModifiedDate":"2012-08-11T01:01:51","indexId":"70039428","displayToPublicDate":"2008-01-22T11:37:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Activities and services of the U.S. Geological Survey, Denver area, Colorado","docAbstract":"This booklet is a summary of the activities and services of the United States Geological Survey, written for people who have visited or plan to visit one or more of its offices in the Denver area as well as to provide general information about the Geological Survey and its work. Sources of additional information are listed on pages 42-43.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039428","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1969, Activities and services of the U.S. Geological Survey, Denver area, Colorado, 45 p., https://doi.org/10.3133/70039428.","productDescription":"45 p.","numberOfPages":"47","costCenters":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true}],"links":[{"id":261566,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039428/report.pdf"},{"id":261567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039428/report-thumb.jpg"}],"country":"United States","state":"Colorado","city":"Denver","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.11666666666666,39.61666666666667 ], [ -105.11666666666666,39.85 ], [ -1.0677777777777777,39.85 ], [ -1.0677777777777777,39.61666666666667 ], [ -105.11666666666666,39.61666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e6b1e4b0c8380cd475bb","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":535297,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010034,"text":"70010034 - 1969 - Discussion on the paper \"The origin of ultramafic and ultrabasic rocks\" by P.J. Wyllie","interactions":[],"lastModifiedDate":"2025-08-29T15:34:30.362335","indexId":"70010034","displayToPublicDate":"2003-04-09T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Discussion on the paper \"The origin of ultramafic and ultrabasic rocks\" by P.J. Wyllie","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(69)90021-3","issn":"00401951","usgsCitation":"Jackson, E.D., 1969, Discussion on the paper \"The origin of ultramafic and ultrabasic rocks\" by P.J. Wyllie: Tectonophysics, v. 7, no. 5-6, p. 517-518, https://doi.org/10.1016/0040-1951(69)90021-3.","productDescription":"2 p.","startPage":"517","endPage":"518","costCenters":[],"links":[{"id":219585,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"7","issue":"5-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0201e4b0c8380cd4fe40","contributors":{"authors":[{"text":"Jackson, Everett D.","contributorId":7289,"corporation":false,"usgs":true,"family":"Jackson","given":"Everett","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":357742,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6479,"text":"pp631 - 1969 - Analysis of a 24-Year photographic record of Nisqually glacier, Mount Rainier National Park, Washington","interactions":[],"lastModifiedDate":"2014-06-06T11:15:02","indexId":"pp631","displayToPublicDate":"2001-10-01T00:00:00","publicationYear":"1969","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":"631","title":"Analysis of a 24-Year photographic record of Nisqually glacier, Mount Rainier National Park, Washington","docAbstract":"<p>A systematic coverage of Nisqually Glacier by photographs taken from a network of stations on the ground was begun in 1942 to explore the value and limitations of such photographs as an aid in glacier study. Principles developed may be of value elsewhere, especially for the program 'Measurement of Glacier Variations on a World-Wide Basis' of the International Hydrological Decade.</p>\n<br>\n<p>Nisqually Glacier in Mount Rainier National Park, Wash., covers 2.5 square miles (6.5 square kilometers) (1961) and extends from an altitude of about 14,300 feet (4,400 meters) near the top of Mount Rainier down to 4,700 feet (1,400 meters), in a horizontal distance of 4.1 miles (6.6 kilometers).</p>\n<br>\n<p>Analyses were made of the annual photographs taken by the writer for 24 years from about 20 stations. A number of pictures taken sporadically from 1884 to 1941 by others were also available for use in the study. Where possible, the results obtained from photographs were compared with those from the available engineering surveys. Such detailed analysis of an extensive photographic coverage of a single glacier may be unique.</p>\n<br>\n<p>Photographs illustrating the retreat and advance of the glacier's west ice margin in a reach extending for about a mile (1.6 kilometers) downstream from Wilson Glacier show that, by 1965, most of the ice thickness lost in that area between 1890 and 1944 had been recovered. Withering of the stagnant valley tongue down glacier from the nunatak is portrayed, as is its spectacular reactivation in the 1960's by a vigorous advance of fresh ice. Some of the visible characteristics of advancing and receding termini are noted.</p>\n<br>\n<p>Annual values of the glacier's surface slope (5 to 10 degrees) at a cross profile were measured on photographs with respect to a projected vertical line identifiable in each picture. The results were found to average about 2 degrees less than those obtained from the 5-year topographic maps, but they are thought to be a little more accurate owing to lack of a sufficiently small contour interval on the maps for this special purpose.</p>\n<br>\n<p>Year-to-year variations in the surface slope and other characteristics from place to place along the glacier are portrayed by pictures to a degree not economically attainable by any other means.</p>\n<br>\n<p>Annual changes in the glacier's thickness at two locations were determined from photographs and found to agree well with the results of stadia surveys.</p>\n<br>\n<p>A summary of conclusions reached in regard to other data or features of the glacier that were illustrated by annual photographs follows:</p>\n<br>\n<p>1. Toward the end of the ablation season, position of the annual snowline ranged between altitudes of about 5,800 and 7,300 feet (1,750 and 2,250 meters). The altitude limits within which firn was observed on the glacier were about 6,000 and 7,300 feet (1,850 and 2,250 meters).</p>\n<br>\n<p>2. Sources from which debris reaches the glacier are evident.</p>\n<br>\n<p>3. Medial moraines and other persistent patterns sometimes overlooked in the field are more noticeable in photographs. Ice-cored moraines and patterns of multiple lateral moraines are visible.</p>\n<br>\n<p>4. The extent, severity, and nature of crevassing in an area reflect the dynamic condition of the glacier at that location.</p>\n<br>\n<p>5. Erosion has caused certain bedrock areas or features on canyon walls to become unrecognizable within less than 15 years.</p>\n<br>\n<p>6. Effects of the 1932 and 1955 outburst floods on the stream channel and trees for a mile (1.6 kilometers) or so below the glacier are shown in comparison with ordinary, lesser floods. Visible effects include degradation, widening and changes in configuration of the channel, formation of small terraces, removal of vegetation from the flood plain, and the deposition of huge boulders on the stream banks and flood plain.</p>\n<br>\n<p>Some photographic procedures recommended for use in a program of this type are described in the section on \"Recommended Photographic Procedures.\"</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington","doi":"10.3133/pp631","usgsCitation":"Veatch, F.M., 1969, Analysis of a 24-Year photographic record of Nisqually glacier, Mount Rainier National Park, Washington: U.S. Geological Survey Professional Paper 631, Report: iv, 52 p.; 1 Plate: 17.01 x 30.38 inches, https://doi.org/10.3133/pp631.","productDescription":"Report: iv, 52 p.; 1 Plate: 17.01 x 30.38 inches","numberOfPages":"56","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":288144,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp631.jpg"},{"id":33909,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0631/pdf/plate_1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33910,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0631/pdf/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":288143,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0631/"}],"country":"United States","state":"Washington","otherGeospatial":"Mount Rainier National Park","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.833333,46.75 ], [ -121.833333,46.916667 ], [ -121.666667,46.916667 ], [ -121.666667,46.75 ], [ -121.833333,46.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680afe","contributors":{"authors":[{"text":"Veatch, Fred M.","contributorId":46517,"corporation":false,"usgs":true,"family":"Veatch","given":"Fred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":152792,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5658,"text":"pp498D - 1969 - Chemical properties of ground water and their corrosion and encrustation effects on wells","interactions":[],"lastModifiedDate":"2017-03-15T13:09:06","indexId":"pp498D","displayToPublicDate":"1994-01-01T12:00:00","publicationYear":"1969","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":"498","chapter":"D","title":"Chemical properties of ground water and their corrosion and encrustation effects on wells","docAbstract":"<p>Well waters in Egypt, Nigeria, and West Pakistan were studied for their chemical properties and corrosive or encrusting behavior. From the chemical composition of the waters, reaction states with reference to equilibrium were tested for 29 possible coexisting oxides, carbonates, sulfides, and elements. Of the 29 solids considered, only calcite, CaCO<sub>3</sub>, and ferric hydroxide, Fe(OH)<sub>3</sub>, showed any correlation with the corrosiveness of the waters to mild steel (iron metal). All 39 of the waters tested were out of equilibrium with iron metal, but those waters in equilibrium or supersaturated with both calcite and ferric hydroxide were the least corrosive. Supersaturation with other solid phases apparently was unrelated to corrosion. </p><p>A number of solids may form surface deposits in wells and lead to decreased yields by fouling well intakes (screens and gravel packs) or increasing friction losses in casings. Calcite, CaCO<sub>3</sub>; ferric hydroxide, Fe(OH)<sub>3</sub>; magnetite, Fe<sub>3</sub>O<sub>4</sub>; siderite, FeCO<sub>3</sub>; hausmannite, Mn<sub>3</sub>0<sub>4</sub> (tetragonal); manganese spinel, Mn<sub>3</sub>O<sub>4</sub> (isometric); three iron sulfides mackinawite, FeS (tetragonal); greigite, Fe<sub>3</sub>S<sub>4</sub> (isometric); and smythite, Fe<sub>3</sub>S<sub>4</sub> (rhombohedral)-copper hydroxide, Co(OH)<sub>2</sub>; and manganese hydroxide, Mn(OH)<sub>2</sub>, were all at least tentatively identified in the deposits sampled. </p><p>Of geochemical interest is the demonstration that simple stable equilibrium models fail in nearly every case to predict compositions of water yielded by the wells studied. Only one stable phase (calcite) was found to exhibit behavior approximately predictable from stable equilibrium considerations. No other stable phase was found to behave as would be predicted from equilibrium considerations. All the solids found to precipitate (except calcite) are metastable in that they are not the least soluble phases possible in the systems studied. </p><p>In terms of metastable equilibrium, siderite and ferric hydroxide behave approximately as would be predicted from equilibrium considerations, but both are metastable and the presence of neither would be anticipated if only the most stable phases were considered. The behaviors of none of the other solids would be predictable from either stable or metastable equilibrium considerations. An unanswered problem raised by the study reported here is how, or by what paths, truly stable phases form if first precipitates are generally metastable.</p><p>The utility of the findings in well design and operation is in no way impaired by the general lack of equilibrium. Conditions leading to either corrosion (which is related to lack of supersaturation with protective phases), or encrustation (supersaturation&nbsp;with phases that were found to precipitate), or both, apparently can be identified. The application of the methods described can be of great importance in developing unexploited ground-water resources in that certain practical problems can be identified before extensive well construction and unnecessary well failure.</p>","largerWorkTitle":"Hydrology of aquifer systems","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/pp498D","collaboration":"Prepared in cooperation with the Governments of Nigeria, the United Arab Republic, and West Pakistan, under the auspices of the United States Agency for International Development Studies of well waters from Nigeria, Egypt, and Pakistan","usgsCitation":"Barnes, I., and Clarke, F., 1969, Chemical properties of ground water and their corrosion and encrustation effects on wells: U.S. Geological Survey Professional Paper 498, iv, p. D1-D58, https://doi.org/10.3133/pp498D.","productDescription":"iv, p. D1-D58","costCenters":[],"links":[{"id":32162,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0498d/report.pdf","text":"Report","size":"7.59 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":117859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0498d/report-thumb.jpg"}],"country":"Egypt, Nigeria, Pakistan","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[34.9226,29.50133],[34.64174,29.09942],[34.42655,28.34399],[34.15451,27.8233],[33.92136,27.6487],[33.58811,27.97136],[33.13676,28.41765],[32.42323,29.85108],[32.32046,29.76043],[32.73482,28.70523],[33.34876,27.69989],[34.10455,26.14227],[34.47387,25.59856],[34.79507,25.03375],[35.69241,23.92671],[35.49372,23.75237],[35.52598,23.10244],[36.69069,22.20485],[36.86623,22],[32.9,22],[29.02,22],[25,22],[25,25.6825],[25,29.23865],[24.70007,30.04419],[24.95762,30.6616],[24.80287,31.08929],[25.16482,31.56915],[26.49533,31.58568],[27.45762,31.32126],[28.45048,31.02577],[28.91353,30.87005],[29.68342,31.18686],[30.09503,31.4734],[30.97693,31.55586],[31.68796,31.4296],[31.96041,30.9336],[32.19247,31.26034],[32.99392,31.02407],[33.7734,30.96746],[34.26544,31.21936],[34.9226,29.50133]]],[[[8.50029,4.77198],[7.46211,4.41211],[7.0826,4.46469],[6.69807,4.24059],[5.89817,4.26245],[5.3628,4.88797],[5.03357,5.6118],[4.32561,6.27065],[3.57418,6.2583],[2.6917,6.25882],[2.74906,7.87073],[2.72379,8.50685],[2.91231,9.13761],[3.22035,9.44415],[3.70544,10.06321],[3.60007,10.33219],[3.79711,10.73475],[3.57222,11.32794],[3.61118,11.66017],[3.68063,12.5529],[3.96728,12.95611],[4.10795,13.53122],[4.36834,13.74748],[5.44306,13.86592],[6.44543,13.49277],[6.82044,13.11509],[7.33075,13.09804],[7.80467,13.34353],[9.01493,12.82666],[9.52493,12.8511],[10.11481,13.27725],[10.70103,13.24692],[10.98959,13.38732],[11.5278,13.32898],[12.30207,13.03719],[13.08399,13.59615],[13.3187,13.55636],[13.99535,12.46157],[14.18134,12.48366],[14.57718,12.08536],[14.46819,11.90475],[14.41538,11.57237],[13.57295,10.79857],[13.30868,10.16036],[13.1676,9.64063],[12.95547,9.41777],[12.75367,8.71776],[12.21887,8.30582],[12.06395,7.79981],[11.83931,7.39704],[11.74577,6.98138],[11.05879,6.64443],[10.49738,7.05536],[10.11828,7.03877],[9.52271,6.45348],[9.23316,6.44449],[8.75753,5.47967],[8.50029,4.77198]]],[[[75.15803,37.13303],[75.8969,36.66681],[76.19285,35.8984],[77.83745,35.49401],[76.87172,34.65354],[75.75706,34.50492],[74.2402,34.74889],[73.74995,34.3177],[74.10429,33.44147],[74.45156,32.7649],[75.25864,32.27111],[74.40593,31.69264],[74.42138,30.97981],[73.45064,29.97641],[72.82375,28.96159],[71.77767,27.91318],[70.6165,27.9892],[69.51439,26.94097],[70.16893,26.49187],[70.28287,25.72223],[70.8447,25.2151],[71.04324,24.35652],[68.8426,24.35913],[68.17665,23.69197],[67.44367,23.94484],[67.14544,24.66361],[66.37283,25.42514],[64.53041,25.23704],[62.9057,25.21841],[61.49736,25.07824],[61.87419,26.23997],[63.31663,26.75653],[63.2339,27.21705],[62.75543,27.37892],[62.72783,28.25964],[61.77187,28.69933],[61.36931,29.30328],[60.87425,29.82924],[62.54986,29.31857],[63.55026,29.46833],[64.148,29.34082],[64.35042,29.56003],[65.04686,29.47218],[66.34647,29.88794],[66.38146,30.7389],[66.93889,31.30491],[67.68339,31.30315],[67.79269,31.58293],[68.55693,31.71331],[68.92668,31.62019],[69.31776,31.90141],[69.26252,32.50194],[69.68715,33.1055],[70.32359,33.35853],[69.93054,34.02012],[70.8818,33.98886],[71.15677,34.34891],[71.11502,34.73313],[71.61308,35.1532],[71.49877,35.65056],[71.26235,36.07439],[71.84629,36.50994],[72.92002,36.72001],[74.06755,36.83618],[74.57589,37.02084],[75.15803,37.13303]]]]},\"properties\":{\"name\":\"Egypt\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3daa","contributors":{"authors":[{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":151379,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Clarke, Frank Eldridge","contributorId":107255,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank Eldridge","affiliations":[],"preferred":false,"id":151380,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048211,"text":"pp542 - 1969 - The Alaska earthquake, March 27, 1964: Effects on communities","interactions":[{"subject":{"id":6309,"text":"pp542G - 1969 - Effects of the earthquake of March 27, 1964, on various communities","indexId":"pp542G","publicationYear":"1969","noYear":false,"chapter":"G","title":"Effects of the earthquake of March 27, 1964, on various communities"},"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},{"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":2},{"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":3},{"subject":{"id":38844,"text":"pp542A - 1965 - Effects of the earthquake of March 27, 1964, at Anchorage, Alaska","indexId":"pp542A","publicationYear":"1965","noYear":false,"chapter":"A","title":"Effects of the earthquake of March 27, 1964, at Anchorage, 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":4},{"subject":{"id":38845,"text":"pp542B - 1965 - Effects of the earthquake of March 27, 1964, at Whittier, Alaska","indexId":"pp542B","publicationYear":"1965","noYear":false,"chapter":"B","title":"Effects of the earthquake of March 27, 1964, at Whittier, 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":5},{"subject":{"id":38846,"text":"pp542E - 1967 - Effects of the earthquake of March 27, 1964, at Seward, Alaska","indexId":"pp542E","publicationYear":"1967","noYear":false,"chapter":"E","title":"Effects of the earthquake of March 27, 1964, at Seward, 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":6},{"subject":{"id":38847,"text":"pp542F - 1967 - Effects of the earthquake of March 27, 1964 on the communities of Kodiak and nearby islands","indexId":"pp542F","publicationYear":"1967","noYear":false,"chapter":"F","title":"Effects of the earthquake of March 27, 1964 on the communities of Kodiak and nearby islands"},"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":7}],"lastModifiedDate":"2022-04-28T20:06:01.293026","indexId":"pp542","displayToPublicDate":"1994-01-01T09:41:00","publicationYear":"1969","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","title":"The Alaska earthquake, March 27, 1964: Effects on communities","docAbstract":"This is the second in a series of six reports that the U.S. Geological Survey published on the results of a comprehensive geologic study that began, as a reconnaissance survey, within 24 hours after the March 27, 1964, Magnitude 9.2 Great Alaska Earthquake and extended, as detailed investigations, through several field seasons. The 1964 Great Alaska earthquake was the largest earthquake in the U.S. since 1700. Professional Paper 542, in 7 parts, describes the effects of the earthquake on Alaskan communities.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/pp542","usgsCitation":"Hansen, W.R., Kachadoorian, R., Coulter, H., Migliaccio, R.R., Waller, R., Stanley, K.W., Lemke, R., Plafker, G., Eckel, E.B., and Mayo, L.R., 1969, The Alaska earthquake, March 27, 1964: Effects on communities: U.S. Geological Survey Professional Paper 542, 7 Chapters, https://doi.org/10.3133/pp542.","productDescription":"7 Chapters","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":277615,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp542.gif"},{"id":277613,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0542/"}],"country":"United States","state":"Alaska","city":"Anchorage, Homer, Kodiak, Seward, Valdez, Whittier","otherGeospatial":"Kenai Peninsula, Prince William Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -168,\n              52\n            ],\n            [\n              -130,\n              52\n            ],\n            [\n              -130,\n              66.5\n            ],\n            [\n              -168,\n              66.5\n            ],\n            [\n              -168,\n              52\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd76c7e4b0b2908510b1cf","contributors":{"authors":[{"text":"Hansen, Wallace R.","contributorId":90273,"corporation":false,"usgs":true,"family":"Hansen","given":"Wallace","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":484011,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kachadoorian, Reuben","contributorId":24336,"corporation":false,"usgs":true,"family":"Kachadoorian","given":"Reuben","email":"","affiliations":[],"preferred":false,"id":484007,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Coulter, Henry W.","contributorId":56967,"corporation":false,"usgs":true,"family":"Coulter","given":"Henry W.","affiliations":[],"preferred":false,"id":484009,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Migliaccio, Ralph R.","contributorId":22667,"corporation":false,"usgs":true,"family":"Migliaccio","given":"Ralph","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":484006,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Waller, Roger M.","contributorId":90353,"corporation":false,"usgs":true,"family":"Waller","given":"Roger M.","affiliations":[],"preferred":false,"id":484012,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Stanley, Kirk W.","contributorId":8900,"corporation":false,"usgs":true,"family":"Stanley","given":"Kirk","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":484005,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lemke, Richard W.","contributorId":59409,"corporation":false,"usgs":true,"family":"Lemke","given":"Richard W.","affiliations":[],"preferred":false,"id":484010,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":484004,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Eckel, Edwin B.","contributorId":26680,"corporation":false,"usgs":true,"family":"Eckel","given":"Edwin","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":484008,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Mayo, Lawrence R.","contributorId":98344,"corporation":false,"usgs":true,"family":"Mayo","given":"Lawrence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":484013,"contributorType":{"id":1,"text":"Authors"},"rank":10}]}}
,{"id":6309,"text":"pp542G - 1969 - Effects of the earthquake of March 27, 1964, on various communities","interactions":[{"subject":{"id":6309,"text":"pp542G - 1969 - Effects of the earthquake of March 27, 1964, on various communities","indexId":"pp542G","publicationYear":"1969","noYear":false,"chapter":"G","title":"Effects of the earthquake of March 27, 1964, on various communities"},"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":"2022-04-28T19:46:13.571561","indexId":"pp542G","displayToPublicDate":"1994-01-01T07:00:00","publicationYear":"1969","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":"G","title":"Effects of the earthquake of March 27, 1964, on various communities","docAbstract":"<p>The 1964 earthquake caused wide-spread damage to inhabited places throughout more than 60,000 square miles of south-central Alaska. This report describes damage to all communities in the area except Anchorage, Whittier, Homer, Valdez, Seward, the communities of the Kodiak group of islands, and communities in the Copper River Basin; these were discussed in previous chapters of the Geological Survey's series of reports on the earthquake. At the communities discussed herein, damage resulted primarily from sea waves of diverse origins, displacements of the land relative to sea level, and seismic shaking. Waves took all of the 31 lives lost at those communities; physical damage was primarily from the waves and vertical displacements of the land relative to sea level.</p>\n</br>\n<p>Destructive waves of local origin struck during or immediately after the earthquake throughout much of Prince William Sound, the southern Kenai Peninsula, and the shores of Kenai Lake. In Prince William Sound, waves demolished all but one home at the native village of Chenega, destroyed homesites at Point Nowell and Anderson Bay, and caused varying amounts of damage to waterfront facilities at Sawmill Bay, Latouche, Port Oceanic, Port Nellie Juan, Perry Island, and western Port Valdez. The local waves, which ran up as high as 70 feet above tide level at Chenega and more than 170 feet in several uninhabited parts of the Sound, took nearly all of the lives lost by drowning at these communities. Destructive local waves that devastated shores of Anderson Bay and adjacent parts of western Port Valdez probably were generated primarily by massive submarine slides of glacial and fluvioglacial deposits ; the origin of the waves that caused damage at most of the other communities and at extensive uninhabited segments of shoreline is not known. At these places the most probable generative mechanisms are: unidentified submarine slides of unconsolidated deposits, and (or) the horizontal tectonic displacements, of 20 to more than 60 feet, that occurred in the Prince William Sound region during the earthquake.</p>\n</br>\n<p>A train of long-period seismic sea waves that began about 20 minutes after the start of the earthquake inundated shores along the Gulf of Alaska coast to a maximum height of 35 feet above tide level. At the communities described, they virtually destroyed two logging camps at Whidbey Bay and Puget Bay on the south coast of the Kenai Peninsula, caused moderate damage to boat harbors and docks at Seldovia and Cordova, floated away some beach cabins in the Cordova area, and drowned two people, one at Point Whitshed near Cordora and one at the Cape Saint Elias Light Station. The seismic sea waves were generated by regional tectonic uplift of the sea floor on the Continental Shelf.</p>\n</br>\n<p>Vertical tectonic displacements of the land relative to sea level that accompanied the earthquake affected virtually all the coastal communities. Tectonic subsidence of 5 to 6 feet, augmented locally by surficial subsidence of unconsolidated deposits required either the relocation or raising of structures at Portage, Girdwood, and Hope on Turnagain Arm. Shoreline submergence resulting from about 3½ feet of tectonic subsidence at Seldovia necessitated raising all waterfront facilities and the airstrip above the level of high tides. On the other hand, tectonic uplift of the land in the Prince Williams Sound region required deepening of the small-boat harbors at Cordora and Tatitlek, dredging of the waterways in the Cordova area, and lengthening of some docks or piers at Cordova, the Cape Hinchinbrook Light Station, and in Sawmill Bay.</p>\n</br>\n<p>Significant structural damage from direct seismic shaking was largely confined to fluid containers and a pier facility near Kenai. Indirect damage from fissuring and differential settling of foundation mterials in the vicinity of the Cordova airfield mused damage to a building, underground utilities, an airfield fill, and the highway. Minor amounts of direct and indirect damage from seismic vibrations were sustained by most of the communities situated on unconsolidated deposits as far east as Yakutat, north to Fairbanks, and west to King Salmon. Except for a few cracked or toppled chimney, all the damage from shaking was confined to areas of thick, unconsolidated deposits. Foundation damage was almost entirely restricted to water-saturated unconsolidated deposits which, when liquefied by seismic shaking, could spread laterally toward free faces and (or) settle differentially through compaction.</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/pp542G","usgsCitation":"Plafker, G., Kachadoorian, R., Eckel, E.B., and Mayo, L.R., 1969, Effects of the earthquake of March 27, 1964, on various communities: U.S. Geological Survey Professional Paper 542, Report: vi, 50 p.; 2 Plates: 47 x 35 inches and 41.96 x 37 inches, https://doi.org/10.3133/pp542G.","productDescription":"Report: vi, 50 p.; 2 Plates: 47 x 35 inches and 41.96 x 37 inches","numberOfPages":"61","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. 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,{"id":62394,"text":"gq795 - 1969 - Geologic map of the Escabosa quadrangle, Bernalillo County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq795","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"795","title":"Geologic map of the Escabosa quadrangle, Bernalillo County, New Mexico","language":"ENGLISH","doi":"10.3133/gq795","usgsCitation":"Myers, D.A., 1969, Geologic map of the Escabosa quadrangle, Bernalillo County, New Mexico: U.S. Geological Survey Geologic Quadrangle 795, 1 map., https://doi.org/10.3133/gq795.","productDescription":"1 map.","costCenters":[],"links":[{"id":103511,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2097.htm","linkFileType":{"id":5,"text":"html"},"description":"2097"},{"id":248569,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0795/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":253713,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0795/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.36749999999999,34.8675 ], [ -106.36749999999999,35 ], [ -106.25,35 ], [ -106.25,34.8675 ], [ -106.36749999999999,34.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69992f","contributors":{"authors":[{"text":"Myers, Donald A.","contributorId":100906,"corporation":false,"usgs":true,"family":"Myers","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":267325,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68029,"text":"ha334 - 1969 - Ground-water resources of the St. James area, South-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T11:14:47","indexId":"ha334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"334","title":"Ground-water resources of the St. James area, South-central Minnesota","docAbstract":"<p>The purpose of this investigation was to evaluate the quality and quantity of the ground-water resources in the area of St. James, Minnesota. St. James is located in the center of Watonwan County in south-central Minnesota. The area is covered by a thick layer of glacial drift which is underlain by Cretaceous, Cambrian, and Precambrian rocks. St. James presently obtains its water supply from two aquifers. One is a Cretaceous sandstone 160 feet below the surface, in which two wells are completed. This aquifer yields abundant water but it is of poor quality and is expensive to treat. The second source, tapped by three municipal wells, is a surficial sand and gravel deposit less than 40 feet thick at the well field. This aquifer produces water of better quality, but its extent and capacity are not known. There are other wells in the area completed at depths ranging from 15 to 500 feet.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha334","collaboration":"Prepared in cooperation with the Minnesota Department of Conservation Division of Waters, Soils, and Mineral and the City of St. James, Minnesota","usgsCitation":"Ropes, L., 1969, Ground-water resources of the St. James area, South-central Minnesota: U.S. Geological Survey Hydrologic Atlas 334, Plate: 28.5 x 39.5 inches, https://doi.org/10.3133/ha334.","productDescription":"Plate: 28.5 x 39.5 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":185715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89273,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/334/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Minnesota","city":"St. James","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.71519470214844,\n              43.94636115619796\n            ],\n            [\n              -94.71519470214844,\n              44.09177709435134\n            ],\n            [\n              -94.52602386474608,\n              44.09177709435134\n            ],\n            [\n              -94.52602386474608,\n              43.94636115619796\n            ],\n            [\n              -94.71519470214844,\n              43.94636115619796\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a699","contributors":{"authors":[{"text":"Ropes, L.H.","contributorId":37824,"corporation":false,"usgs":true,"family":"Ropes","given":"L.H.","affiliations":[],"preferred":false,"id":277526,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5953,"text":"pp613C - 1969 - Early Pennsylvanian ammonoids from southern Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:56","indexId":"pp613C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"613","chapter":"C","title":"Early Pennsylvanian ammonoids from southern Nevada","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to paleontology, 1968","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp613C","usgsCitation":"Gordon, M., 1969, Early Pennsylvanian ammonoids from southern Nevada: U.S. Geological Survey Professional Paper 613, p. C1-C13, https://doi.org/10.3133/pp613C.","productDescription":"p. C1-C13","costCenters":[],"links":[{"id":121430,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0613c/report-thumb.jpg"},{"id":32841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0613c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c268","contributors":{"authors":[{"text":"Gordon, Mackenzie Jr.","contributorId":13225,"corporation":false,"usgs":true,"family":"Gordon","given":"Mackenzie","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":151864,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34201,"text":"b1274M - 1969 - Paleocene and lower Eocene units in the southern part of the Piceance Creek basin, Colorado","interactions":[],"lastModifiedDate":"2023-09-14T20:02:11.515338","indexId":"b1274M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"1274","chapter":"M","title":"Paleocene and lower Eocene units in the southern part of the Piceance Creek basin, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1274M","usgsCitation":"Donnell, J., 1969, Paleocene and lower Eocene units in the southern part of the Piceance Creek basin, Colorado: U.S. Geological Survey Bulletin 1274, iii, 18 p., https://doi.org/10.3133/b1274M.","productDescription":"iii, 18 p.","costCenters":[],"links":[{"id":420804,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92632.htm","linkFileType":{"id":5,"text":"html"}},{"id":163566,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1274m/report-thumb.jpg"},{"id":96278,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1274m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Piceance Creek basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -109.06,\n              40.3689\n            ],\n            [\n              -109.06,\n              38.8414\n            ],\n            [\n              -107.6986,\n              38.8414\n            ],\n            [\n              -107.6986,\n              40.3689\n            ],\n            [\n              -109.06,\n              40.3689\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d3b","contributors":{"authors":[{"text":"Donnell, John R.","contributorId":84330,"corporation":false,"usgs":true,"family":"Donnell","given":"John R.","affiliations":[],"preferred":false,"id":212603,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15362,"text":"ofr69197 - 1969 - Predicting the dye layer densities of color infrared transparencies","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr69197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"69-197","title":"Predicting the dye layer densities of color infrared transparencies","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69197","usgsCitation":"Pease, R.W., 1969, Predicting the dye layer densities of color infrared transparencies: U.S. Geological Survey Open-File Report 69-197, 33 p. ill. ;29 cm., https://doi.org/10.3133/ofr69197.","productDescription":"33 p. ill. ;29 cm.","costCenters":[],"links":[{"id":95297,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1969/0197/report.pdf","size":"1455","linkFileType":{"id":1,"text":"pdf"}},{"id":148578,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1969/0197/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e7ff","contributors":{"authors":[{"text":"Pease, Robert W.","contributorId":43760,"corporation":false,"usgs":true,"family":"Pease","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":171009,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39670,"text":"pp614E - 1969 - Distribution of thorium, uranium, and potassium in igneous rocks of the Boulder batholith region, Montana, and its bearing on radiogenic heat production and heat flow","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"pp614E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"614","chapter":"E","title":"Distribution of thorium, uranium, and potassium in igneous rocks of the Boulder batholith region, Montana, and its bearing on radiogenic heat production and heat flow","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1968","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp614E","usgsCitation":"Tilling, R., and Gottfried, D., 1969, Distribution of thorium, uranium, and potassium in igneous rocks of the Boulder batholith region, Montana, and its bearing on radiogenic heat production and heat flow: U.S. Geological Survey Professional Paper 614, p. E1-E29, https://doi.org/10.3133/pp614E.","productDescription":"p. E1-E29","costCenters":[],"links":[{"id":121898,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0614e/report-thumb.jpg"},{"id":67394,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0614e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f3c6","contributors":{"authors":[{"text":"Tilling, R.I. 0000-0003-4263-7221","orcid":"https://orcid.org/0000-0003-4263-7221","contributorId":98311,"corporation":false,"usgs":true,"family":"Tilling","given":"R.I.","affiliations":[],"preferred":false,"id":221949,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gottfried, David","contributorId":82295,"corporation":false,"usgs":true,"family":"Gottfried","given":"David","email":"","affiliations":[],"preferred":false,"id":221948,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6202,"text":"pp611 - 1969 - Foraminifera and stratigraphy of the upper part of the Pierre Shale and lower part of the Fox Hills Sandstone (Cretaceous), north-central South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:05:57","indexId":"pp611","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"611","title":"Foraminifera and stratigraphy of the upper part of the Pierre Shale and lower part of the Fox Hills Sandstone (Cretaceous), north-central South Dakota","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp611","usgsCitation":"Mello, J.F., 1969, Foraminifera and stratigraphy of the upper part of the Pierre Shale and lower part of the Fox Hills Sandstone (Cretaceous), north-central South Dakota: U.S. Geological Survey Professional Paper 611, 121 p., https://doi.org/10.3133/pp611.","productDescription":"121 p.","costCenters":[],"links":[{"id":121387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0611/report-thumb.jpg"},{"id":33378,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0611/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33379,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0611/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de42d","contributors":{"authors":[{"text":"Mello, James F.","contributorId":31384,"corporation":false,"usgs":true,"family":"Mello","given":"James","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":152293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":67233,"text":"i623 - 1969 - (ORB II-13 (25)) Geologic map of Apollo landing site 5, part of Maestlin G region Oceanus Procellarum","interactions":[],"lastModifiedDate":"2012-02-02T00:13:20","indexId":"i623","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"623","subseriesTitle":"MOON","title":"(ORB II-13 (25)) Geologic map of Apollo landing site 5, part of Maestlin G region Oceanus Procellarum","language":"ENGLISH","doi":"10.3133/i623","usgsCitation":"Titley, S., and Trask, N., 1969, (ORB II-13 (25)) Geologic map of Apollo landing site 5, part of Maestlin G region Oceanus Procellarum: U.S. Geological Survey IMAP 623, 1 map., https://doi.org/10.3133/i623.","productDescription":"1 map.","costCenters":[],"links":[{"id":189988,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101412,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0623/plate-1.pdf","size":"5711","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4905e4b0b290850eed13","contributors":{"authors":[{"text":"Titley, S.R.","contributorId":60602,"corporation":false,"usgs":true,"family":"Titley","given":"S.R.","affiliations":[],"preferred":false,"id":275826,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trask, N.J.","contributorId":31729,"corporation":false,"usgs":true,"family":"Trask","given":"N.J.","email":"","affiliations":[],"preferred":false,"id":275825,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":36127,"text":"b1289 - 1969 - Atomic-absorption methods of analysis useful in geochemical exploration","interactions":[],"lastModifiedDate":"2012-02-02T00:09:36","indexId":"b1289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1969","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":"1289","title":"Atomic-absorption methods of analysis useful in geochemical exploration","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1289","usgsCitation":"Ward, F.N., Nakagawa, H.M., Harms, T.F., and Van Sickle, G., 1969, Atomic-absorption methods of analysis useful in geochemical exploration: U.S. Geological Survey Bulletin 1289, 45 p, https://doi.org/10.3133/b1289.","productDescription":"45 p","costCenters":[],"links":[{"id":93778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1289/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1289/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6693d0","contributors":{"authors":[{"text":"Ward, Frederick Norville","contributorId":105698,"corporation":false,"usgs":true,"family":"Ward","given":"Frederick","email":"","middleInitial":"Norville","affiliations":[],"preferred":false,"id":215806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nakagawa, H. M.","contributorId":106475,"corporation":false,"usgs":true,"family":"Nakagawa","given":"H.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":215807,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Harms, T. F.","contributorId":76752,"corporation":false,"usgs":true,"family":"Harms","given":"T.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":215805,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Van Sickle, G.H.","contributorId":45295,"corporation":false,"usgs":true,"family":"Van Sickle","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":215804,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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