{"pageNumber":"1685","pageRowStart":"42100","pageSize":"25","recordCount":46619,"records":[{"id":1007443,"text":"1007443 - 1980 - Visitor use patterns in Yosemite National Park","interactions":[],"lastModifiedDate":"2024-05-15T11:17:20.056621","indexId":"1007443","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2486,"text":"Journal of Travel Research","active":true,"publicationSubtype":{"id":10}},"title":"Visitor use patterns in Yosemite National Park","docAbstract":"<p>After several years of dramatic increases, visitor use in Yosemite National Park has leveled off to an average of 2.4 million visits per year. Coincident with this decline in the growth rate, there have been some changes in visitation trends and patterns. Data collected in the park show that the average length of stay has decreased to less than 32 hours and that the average number of visitors per vehicle has dropped to slightly less than three.</p>","language":"English","publisher":"Sage Journals","doi":"10.1177/004728758001900203","usgsCitation":"van Wagtendonk, J., 1980, Visitor use patterns in Yosemite National Park: Journal of Travel Research, v. 19, no. 2, p. 12-17, https://doi.org/10.1177/004728758001900203.","productDescription":"6 p.","startPage":"12","endPage":"17","numberOfPages":"6","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":130019,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationDate":"1980-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdbb9","contributors":{"authors":[{"text":"van Wagtendonk, J. W.","contributorId":85111,"corporation":false,"usgs":true,"family":"van Wagtendonk","given":"J. W.","affiliations":[],"preferred":false,"id":315363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9276,"text":"ofr80218 - 1980 - Geohydrology of southwestern Kansas","interactions":[{"subject":{"id":9276,"text":"ofr80218 - 1980 - Geohydrology of southwestern Kansas","indexId":"ofr80218","publicationYear":"1980","noYear":false,"title":"Geohydrology of southwestern Kansas"},"predicate":"SUPERSEDED_BY","object":{"id":70046183,"text":"70046183 - 1981 - Geohydrology of southwestern Kansas","indexId":"70046183","publicationYear":"1981","noYear":false,"title":"Geohydrology of southwestern Kansas"},"id":1}],"supersededBy":{"id":70046183,"text":"70046183 - 1981 - Geohydrology of southwestern Kansas","indexId":"70046183","publicationYear":"1981","noYear":false,"title":"Geohydrology of southwestern Kansas"},"lastModifiedDate":"2022-07-05T13:52:38.731892","indexId":"ofr80218","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"80-218","title":"Geohydrology of southwestern Kansas","docAbstract":"<p>Southwestern Kansas is one of the principal areas of ground-water development for irrigation in the State, and many reports are available concerning ground-water conditions in the area. The purposes of this investigation were to consolidate and update data, to determine the extent and effects of irrigation development on the ground-water resource, to determine the chemical quality of the ground water in relation to irrigation use, to describe the general operation of the hydrologic system, and to identify problem areas where intensive quantitative studies will be needed by State and local agencies for planning and management of the resource. This study began in 1972 as part of a cooperative program of ground-water investigations between the Kansas Geological Survey and the U.S. Geological Survey. Support in this study was provided by the Division of Water Resources of the Kansas State Board of Agriculture and the Division of Environment of the Kansas Department of Health and Environment. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80218","collaboration":"Prepared in cooperation with the Kansas Geological Survey","usgsCitation":"Gutentag, E.D., Lobmeyer, D.H., and Slagle, S.E., 1980, Geohydrology of southwestern Kansas: U.S. Geological Survey Open-File Report 80-218, Report: 97 p.; 11 Plates: 31.40 x 27.20 inches or smaller, https://doi.org/10.3133/ofr80218.","productDescription":"Report: 97 p.; 11 Plates: 31.40 x 27.20 inches or smaller","costCenters":[],"links":[{"id":402936,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402933,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402930,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402928,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402927,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402926,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402932,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402935,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402931,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402929,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402934,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0218/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402925,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0218/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":140894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0218/report-thumb.jpg"}],"country":"United States","state":"Kansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.04376220703125,\n              37.004746084814784\n            ],\n            [\n              -100.04974365234375,\n              37.004746084814784\n            ],\n            [\n              -100.04974365234375,\n              38.47079371120379\n            ],\n            [\n              -102.04376220703125,\n              38.47079371120379\n            ],\n            [\n              -102.04376220703125,\n              37.004746084814784\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a23","contributors":{"authors":[{"text":"Gutentag, Edwin D.","contributorId":76287,"corporation":false,"usgs":true,"family":"Gutentag","given":"Edwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":159405,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lobmeyer, David H.","contributorId":85156,"corporation":false,"usgs":true,"family":"Lobmeyer","given":"David","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":159406,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Slagle, Steven E.","contributorId":35284,"corporation":false,"usgs":true,"family":"Slagle","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159404,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70158694,"text":"70158694 - 1980 - A selected bibliography: Remote sensing applications in wildlife management","interactions":[],"lastModifiedDate":"2022-04-05T13:45:30.093975","indexId":"70158694","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"A selected bibliography: Remote sensing applications in wildlife management","docAbstract":"<p>Citations of 165 selected technical reports, journal articles, and other publications on remote sensing applications for wildlife management are presented in a bibliography. These materials summarize developments in the use of remotely sensed data for wildlife habitat mapping, habitat inventory, habitat evaluation, and wildlife census. The bibliography contains selected citations published between 1947 and 1979.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sioux Fall, SD","doi":"10.3133/70158694","usgsCitation":"Carneggie, D.M., Ohlen, D.O., and Pettinger, L.R., 1980, A selected bibliography: Remote sensing applications in wildlife management, 30 p., https://doi.org/10.3133/70158694.","productDescription":"30 p.","numberOfPages":"36","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":309550,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70158694.JPG"},{"id":310258,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70158694/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56139f2fe4b0ba4884c60f80","contributors":{"authors":[{"text":"Carneggie, David M.","contributorId":62758,"corporation":false,"usgs":true,"family":"Carneggie","given":"David","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":576559,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ohlen, Donald O. ohlen@usgs.gov","contributorId":3779,"corporation":false,"usgs":true,"family":"Ohlen","given":"Donald","email":"ohlen@usgs.gov","middleInitial":"O.","affiliations":[],"preferred":true,"id":576560,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pettinger, Lawrence R.","contributorId":18274,"corporation":false,"usgs":true,"family":"Pettinger","given":"Lawrence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":576561,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012161,"text":"70012161 - 1980 - Hydraulic piston coring of late Neogene and Quaternary sections in the Caribbean and equatorial Pacific: Preliminary results of Deep Sea Drilling Project leg 68","interactions":[],"lastModifiedDate":"2024-01-04T12:23:07.044757","indexId":"70012161","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Hydraulic piston coring of late Neogene and Quaternary sections in the Caribbean and equatorial Pacific: Preliminary results of Deep Sea Drilling Project leg 68","docAbstract":"<div id=\"15191171\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Leg 68 of the Deep Sea Drilling Project used the newly developed Hydraulic Piston Corer (HPC) to recover two virtually continuous, undisturbed sections of late Neogene and Quaternary sediment. The sites are located in the western Caribbean (Site 502, 4 holes) and in the eastern equatorial Pacific (Site 503, 2 holes). The sediment of Site 502 is primarily foram-bearing nanno marl which accumulated at about 3 to 4 cm/thousand yr. The bottom of Site 502 (228.7 m) is ∼ 8 m.y. old. The sediment of Site 503 is primarily siliceous calcareous ooze which accumulated at about 2 to 3 cm/thousand yr. The bottom of Site 503 (235.0 m) is ∼ 8 m.y. old.</p><p>The magnetostratigraphy of both sites was determined on the R.V.<span>&nbsp;</span><i>Glomar Challenger</i><span>&nbsp;</span>with a long-core spinner magnetometer. All paleomagnetic boundaries through the Gilbert were identified in Site 502; most of them were identified in Site 503. The sediment at both sites shows a distinct cyclicity of calcium carbonate content. These relatively high accumulation rate, continuous, undisturbed HPC cores will enable a wide variety of high-resolution biostratigraphic, paleoclimatic, and paleoceanographic studies heretofore not feasible.</p></div>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1980)91<433:HPCOLN>2.0.CO;2","usgsCitation":"Prell, W., Gardner, J.V., Adelseck, C., Blechschmidt, G., Fleet, A.J., Keigwin, L.D., Kent, D.V., Ledbetter, M.T., Mann, U., Mayer, L., Reidel, W.R., Sancetta, C., Spariosu, D.J., and Zimmerman, H.B., 1980, Hydraulic piston coring of late Neogene and Quaternary sections in the Caribbean and equatorial Pacific: Preliminary results of Deep Sea Drilling Project leg 68: Geological Society of America Bulletin, v. 91, no. 7 pt 1, p. 433-444, https://doi.org/10.1130/0016-7606(1980)91<433:HPCOLN>2.0.CO;2.","productDescription":"12 p.","startPage":"433","endPage":"444","numberOfPages":"12","costCenters":[],"links":[{"id":489064,"rank":3,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.7916/d8m90k6f","text":"External Repository"},{"id":268110,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://academiccommons.columbia.edu/catalog/ac:143426"},{"id":222701,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"91","issue":"7 pt 1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a32f9e4b0c8380cd5ec08","contributors":{"authors":[{"text":"Prell, W.L.","contributorId":78092,"corporation":false,"usgs":true,"family":"Prell","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":362897,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gardner, James V.","contributorId":93035,"corporation":false,"usgs":true,"family":"Gardner","given":"James","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":362900,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adelseck, Charles","contributorId":17767,"corporation":false,"usgs":true,"family":"Adelseck","given":"Charles","email":"","affiliations":[],"preferred":false,"id":362889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blechschmidt, Gretchen","contributorId":87296,"corporation":false,"usgs":true,"family":"Blechschmidt","given":"Gretchen","email":"","affiliations":[],"preferred":false,"id":362898,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Fleet, Andrew J.","contributorId":63534,"corporation":false,"usgs":true,"family":"Fleet","given":"Andrew","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":362893,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Keigwin, Lloyd D.","contributorId":37476,"corporation":false,"usgs":true,"family":"Keigwin","given":"Lloyd","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":362892,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Kent, Dennis V.","contributorId":63951,"corporation":false,"usgs":true,"family":"Kent","given":"Dennis","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":362894,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Ledbetter, Michael T.","contributorId":87692,"corporation":false,"usgs":true,"family":"Ledbetter","given":"Michael","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":362899,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Mann, Ulrich","contributorId":22499,"corporation":false,"usgs":true,"family":"Mann","given":"Ulrich","email":"","affiliations":[],"preferred":false,"id":362891,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Mayer, Larry","contributorId":77936,"corporation":false,"usgs":true,"family":"Mayer","given":"Larry","affiliations":[],"preferred":false,"id":362896,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Reidel, William R.","contributorId":72131,"corporation":false,"usgs":true,"family":"Reidel","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":362895,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Sancetta, Constance","contributorId":12979,"corporation":false,"usgs":true,"family":"Sancetta","given":"Constance","email":"","affiliations":[],"preferred":false,"id":362888,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Spariosu, Dann J.","contributorId":10930,"corporation":false,"usgs":true,"family":"Spariosu","given":"Dann","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":362887,"contributorType":{"id":1,"text":"Authors"},"rank":13},{"text":"Zimmerman, Herman B.","contributorId":18111,"corporation":false,"usgs":true,"family":"Zimmerman","given":"Herman","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":362890,"contributorType":{"id":1,"text":"Authors"},"rank":14}]}}
,{"id":70012314,"text":"70012314 - 1980 - Arctic sea-ice variations from time-lapse passive microwave imagery","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70012314","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1072,"text":"Boundary-Layer Meteorology","active":true,"publicationSubtype":{"id":10}},"title":"Arctic sea-ice variations from time-lapse passive microwave imagery","docAbstract":"This paper presents: (1) a short historical review of the passive microwave research on sea ice which established the observational and theoretical base permitting the interpretation of the first passive microwave images of Earth obtained by the Nimbus-5 ESMR; (2) the construction of a time-lapse motion picture film of a 16-month set of serial ESMR images to aid in the formidable data analysis task; and (3) a few of the most significant findings resulting from an early analysis of these data, using selected ESMR images to illustrate these findings. ?? 1980 D. Reidel Publishing Co.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Boundary-Layer Meteorology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00117913","issn":"00068314","usgsCitation":"Campbell, W.J., Ramseier, R., Zwally, H., and Gloersen, P., 1980, Arctic sea-ice variations from time-lapse passive microwave imagery: Boundary-Layer Meteorology, v. 18, no. 1, p. 99-106, https://doi.org/10.1007/BF00117913.","startPage":"99","endPage":"106","numberOfPages":"8","costCenters":[],"links":[{"id":205168,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00117913"},{"id":221940,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ed56e4b0c8380cd4974a","contributors":{"authors":[{"text":"Campbell, W. J.","contributorId":8614,"corporation":false,"usgs":true,"family":"Campbell","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363251,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ramseier, R.O.","contributorId":98039,"corporation":false,"usgs":true,"family":"Ramseier","given":"R.O.","email":"","affiliations":[],"preferred":false,"id":363254,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zwally, H.J.","contributorId":33847,"corporation":false,"usgs":true,"family":"Zwally","given":"H.J.","email":"","affiliations":[],"preferred":false,"id":363252,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gloersen, P.","contributorId":55961,"corporation":false,"usgs":true,"family":"Gloersen","given":"P.","affiliations":[],"preferred":false,"id":363253,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012258,"text":"70012258 - 1980 - Morphology of Lonar Crater, India: Comparisons and implications","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70012258","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3570,"text":"The Moon and the Planets","active":true,"publicationSubtype":{"id":10}},"title":"Morphology of Lonar Crater, India: Comparisons and implications","docAbstract":"Lonar Crater is a young meteorite impact crater emplaced in Deccan basalt. Data from 5 drillholes, a gravity network, and field mapping are used to reconstruct its original dimensions, delineate the nature of the pre-impact target rocks, and interpret the emplacement mode of the ejecta. Our estimates of the pre-erosion dimensions are: average diameter of 1710 m; average rim height of 40 m (30-35 m of rim rock uplift, 5-10 m of ejected debris); depth of 230-245 m (from rim crest to crater floor). The crater's circularity index is 0.9 and is unlikely to have been lower in the past. There are minor irregularities in the original crater floor (present sediment-breccia boundary) possibly due to incipient rebound effects. A continuous ejecta blanket extends an average of 1410 m beyond the pre-erosion rim crest. In general, 'fresh' terrestrial craters, less than 10 km in diameter, have smaller depth/diameter and larger rim height/diameter ratios than their lunar counterparts. Both ratios are intermediate for Mercurian craters, suggesting that crater shape is gravity dependent, all else being equal. Lonar demonstrates that all else is not always equal. Its depth/diameter ratio is normal but, because of less rim rock uplift, its rim height/diameter ratio is much smaller than both 'fresh' terrestrial and lunar impact craters. The target rock column at Lonar consists of one or more layers of weathered, soft basalt capped by fresh, dense flows. Plastic deformation and/or compaction of this lower, incompetent material probably absorbed much of the energy normally available in the cratering process for rim rock uplift. A variety of features within the ejecta blanket and the immediately underlying substrate, plus the broad extent of the blanket boundaries, suggest that a fluidized debris surge was the dominant mechanism of ejecta transportation and deposition at Lonar. In these aspects, Lonar should be a good analog for the 'fluidized craters' of Mars. ?? 1980 D. Reidel Publishing Co.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"The Moon and the Planets","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Kluwer Academic Publishers","doi":"10.1007/BF00897591","issn":"01650807","usgsCitation":"Fudali, R., Milton, D., Fredriksson, K., and Dube, A., 1980, Morphology of Lonar Crater, India: Comparisons and implications: The Moon and the Planets, v. 23, no. 4, p. 493-515, https://doi.org/10.1007/BF00897591.","startPage":"493","endPage":"515","numberOfPages":"23","costCenters":[],"links":[{"id":205191,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF00897591"},{"id":222064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"23","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a5e52e4b0c8380cd7096a","contributors":{"authors":[{"text":"Fudali, R.F.","contributorId":26445,"corporation":false,"usgs":true,"family":"Fudali","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":363112,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Milton, D.J.","contributorId":44121,"corporation":false,"usgs":true,"family":"Milton","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":363113,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fredriksson, K.","contributorId":11328,"corporation":false,"usgs":true,"family":"Fredriksson","given":"K.","email":"","affiliations":[],"preferred":false,"id":363111,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dube, A.","contributorId":8615,"corporation":false,"usgs":true,"family":"Dube","given":"A.","email":"","affiliations":[],"preferred":false,"id":363110,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70012390,"text":"70012390 - 1980 - Implications of regional gravity for state of stress in the earth's crust and upper mantle","interactions":[],"lastModifiedDate":"2024-07-16T16:32:20.739665","indexId":"70012390","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":6453,"text":"Journal of Geophysical Research Solid Earth","active":true,"publicationSubtype":{"id":10}},"title":"Implications of regional gravity for state of stress in the earth's crust and upper mantle","docAbstract":"<p><span>Topography is maintained by stress differences within the earth. Depending on the distribution of the stress we classify the support as either local or regional compensation. In general, the stresses implied in a regional compensation scheme are an order of magnitude larger than those corresponding to local isostasy. Gravity anomalies, a measure of the earth's departure from hydrostatic equilibrium, can be used to distinguish between the two compensation mechanisms and thus to estimate the magnitude of deviatoric stress in the crust and upper mantle. Topography created at an oceanic ridge crest or in a major continental orogenic zone appears to be locally compensated. Such features were formed on weak crust incapable of maintaining stress differences much greater than the stress from the applied load. Oceanic volcanoes formed on an already cooled, thickened lithosphere are regionally supported with elastic stresses. Similarly, the broad topographic rise seaward of subduction zones is elastically supported as the lithosphere is bent near the plate margin. Although the implied stress is to some degree dependent on the rheological model assumed, the gravity anomalies and surface deformation produced by these features demonstrate that the upper 30–40 km of the oceanic lithosphere is capable of regionally supporting stress differences in the 100-MPa range. Given certain conditions of load emplacement, continental crust can also support loads regionally over 100-m.y. time scales, but the effects of erosion only allow an estimate of a lower bound on stress. Data from space probes indicate that the upper layers of other terrestrial planets also support topographic-induced stress differences in excess of 100 MPa.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/JB085iB11p06377","issn":"01480227","usgsCitation":"McNutt, M., 1980, Implications of regional gravity for state of stress in the earth's crust and upper mantle: Journal of Geophysical Research Solid Earth, v. 85, no. B11, p. 6377-6396, https://doi.org/10.1029/JB085iB11p06377.","productDescription":"20 p.","startPage":"6377","endPage":"6396","numberOfPages":"20","costCenters":[],"links":[{"id":222473,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"85","issue":"B11","noUsgsAuthors":false,"publicationDate":"2012-09-20","publicationStatus":"PW","scienceBaseUri":"505a3929e4b0c8380cd61811","contributors":{"authors":[{"text":"McNutt, M.","contributorId":64805,"corporation":false,"usgs":true,"family":"McNutt","given":"M.","email":"","affiliations":[],"preferred":false,"id":363431,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012196,"text":"70012196 - 1980 - Comparison of bed form variance spectra within a meander bend during flood and average discharge","interactions":[],"lastModifiedDate":"2024-05-23T00:48:57.127749","indexId":"70012196","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2450,"text":"Journal of Sedimentary Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Comparison of bed form variance spectra within a meander bend during flood and average discharge","docAbstract":"<div><div id=\"12457701\" class=\"article-section-wrapper js-article-section js-content-section  \" data-section-parent-id=\"0\"><p>Time series analysis of streambed elevation in a meander bend along the Congaree River was used to determine the changes in bed form population succeeding a 16-year flood event. Bed forms observed during the flood event had a significantly greater total height variance than bed forms observed at the same location one week later. Variance spectra were computed for a 595 m longitudinal profile. The data indicate that: a) the bed form variance for the flood record is significantly greater for all wavelengths from 5 to 30 m; b) no well-demarcated bed form classes were present during the survey times, pointing to the possible existence of a continuum of bed form sizes rather than well-defined classes; and c) bed forms produced by the flood discharge were rapidly altered as the stage returned toward average level.</p></div></div>","language":"English","publisher":"SEPM","doi":"10.1306/212F798C-2B24-11D7-8648000102C1865D","issn":"00224472","usgsCitation":"Levey, R., Kjerfve, B., and Getzen, R., 1980, Comparison of bed form variance spectra within a meander bend during flood and average discharge: Journal of Sedimentary Petrology, v. 50, no. 1, p. 149-155, https://doi.org/10.1306/212F798C-2B24-11D7-8648000102C1865D.","productDescription":"7 p.","startPage":"149","endPage":"155","numberOfPages":"7","costCenters":[],"links":[{"id":222186,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"50","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f852e4b0c8380cd4d00b","contributors":{"authors":[{"text":"Levey, R.A.","contributorId":34265,"corporation":false,"usgs":true,"family":"Levey","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":362969,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kjerfve, B.","contributorId":49110,"corporation":false,"usgs":true,"family":"Kjerfve","given":"B.","affiliations":[],"preferred":false,"id":362970,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Getzen, R.T.","contributorId":21281,"corporation":false,"usgs":true,"family":"Getzen","given":"R.T.","affiliations":[],"preferred":false,"id":362968,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012553,"text":"70012553 - 1980 - Computational methods for a three-dimensional model of the petroleum-discovery process","interactions":[],"lastModifiedDate":"2013-01-21T15:55:26","indexId":"70012553","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Computational methods for a three-dimensional model of the petroleum-discovery process","docAbstract":"A discovery-process model devised by Drew, Schuenemeyer, and Root can be used to predict the amount of petroleum to be discovered in a basin from some future level of exploratory effort: the predictions are based on historical drilling and discovery data. Because marginal costs of discovery and production are a function of field size, the model can be used to make estimates of future discoveries within deposit size classes. The modeling approach is a geometric one in which the area searched is a function of the size and shape of the targets being sought. A high correlation is assumed between the surface-projection area of the fields and the volume of petroleum. To predict how much oil remains to be found, the area searched must be computed, and the basin size and discovery efficiency must be estimated. The basin is assumed to be explored randomly rather than by pattern drilling. The model may be used to compute independent estimates of future oil at different depth intervals for a play involving multiple producing horizons. We have written FORTRAN computer programs that are used with Drew, Schuenemeyer, and Root's model to merge the discovery and drilling information and perform the necessary computations to estimate undiscovered petroleum. These program may be modified easily for the estimation of remaining quantities of commodities other than petroleum. ?? 1980.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(80)90013-8","issn":"00983004","usgsCitation":"Schuenemeyer, J., Bawiec, W., and Drew, L., 1980, Computational methods for a three-dimensional model of the petroleum-discovery process: Computers & Geosciences, v. 6, no. 4, p. 323-360, https://doi.org/10.1016/0098-3004(80)90013-8.","startPage":"323","endPage":"360","numberOfPages":"38","costCenters":[],"links":[{"id":266197,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(80)90013-8"},{"id":222147,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"6","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f951e4b0c8380cd4d56d","contributors":{"authors":[{"text":"Schuenemeyer, J.H.","contributorId":106094,"corporation":false,"usgs":true,"family":"Schuenemeyer","given":"J.H.","affiliations":[],"preferred":false,"id":363889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bawiec, W.J.","contributorId":71540,"corporation":false,"usgs":true,"family":"Bawiec","given":"W.J.","affiliations":[],"preferred":false,"id":363888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Drew, L.J.","contributorId":69157,"corporation":false,"usgs":true,"family":"Drew","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":363887,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70012434,"text":"70012434 - 1980 - Computer-composite mapping for geologists","interactions":[],"lastModifiedDate":"2012-03-12T17:19:04","indexId":"70012434","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1539,"text":"Environmental Geology","active":true,"publicationSubtype":{"id":10}},"title":"Computer-composite mapping for geologists","docAbstract":"A computer program for overlaying maps has been tested and evaluated as a means for producing geologic derivative maps. Four maps of the Sugar House Quadrangle, Utah, were combined, using the Multi-Scale Data Analysis and Mapping Program, in a single composite map that shows the relative stability of the land surface during earthquakes. Computer-composite mapping can provide geologists with a powerful analytical tool and a flexible graphic display technique. Digitized map units can be shown singly, grouped with different units from the same map, or combined with units from other source maps to produce composite maps. The mapping program permits the user to assign various values to the map units and to specify symbology for the final map. Because of its flexible storage, easy manipulation, and capabilities of graphic output, the composite-mapping technique can readily be applied to mapping projects in sedimentary and crystalline terranes, as well as to maps showing mineral resource potential. ?? 1980 Springer-Verlag New York Inc.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Environmental Geology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF02473490","issn":"09430105","usgsCitation":"van Driel, J., 1980, Computer-composite mapping for geologists: Environmental Geology, v. 3, no. 3, p. 151-157, https://doi.org/10.1007/BF02473490.","startPage":"151","endPage":"157","numberOfPages":"7","costCenters":[],"links":[{"id":205212,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF02473490"},{"id":222202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f96fe4b0c8380cd4d5ea","contributors":{"authors":[{"text":"van Driel, J.N.","contributorId":29959,"corporation":false,"usgs":true,"family":"van Driel","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":363571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012583,"text":"70012583 - 1980 - Radioactivity method","interactions":[],"lastModifiedDate":"2024-04-18T16:42:03.970695","indexId":"70012583","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Radioactivity method","docAbstract":"<p><span>Radioactivity measurements have played an important role in geophysics since about 1935, and they have increased in importance to the present. The most important areas of application have been in petroleum and uranium exploration. Radioactivity measurements have proved useful in geologic mapping, as well as in specialized applications such as reactor-site monitoring. The technological development of the method has reached a plateau, and the future of the method for some applications will depend upon development of more sophisticated data processing and interpretation.</span></p>","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1441059","issn":"00168033","usgsCitation":"Duval, J.S., 1980, Radioactivity method: Geophysics, v. 45, no. 11, p. 1690-1694, https://doi.org/10.1190/1.1441059.","productDescription":"5 p.","startPage":"1690","endPage":"1694","numberOfPages":"5","costCenters":[],"links":[{"id":221836,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"45","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a93c2e4b0c8380cd80feb","contributors":{"authors":[{"text":"Duval, J. S.","contributorId":15200,"corporation":false,"usgs":true,"family":"Duval","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":363974,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13364,"text":"ofr801029 - 1980 - Geophysical, lithologic, and water-quality data from Superior Dry Lake, San Bernardino County, California","interactions":[],"lastModifiedDate":"2023-03-24T18:16:57.114608","indexId":"ofr801029","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","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":"80-1029","title":"Geophysical, lithologic, and water-quality data from Superior Dry Lake, San Bernardino County, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801029","usgsCitation":"Dockter, R.D., 1980, Geophysical, lithologic, and water-quality data from Superior Dry Lake, San Bernardino County, California: U.S. Geological Survey Open-File Report 80-1029, 1 Plate: 27.54 x 24.86 inches, https://doi.org/10.3133/ofr801029.","productDescription":"1 Plate: 27.54 x 24.86 inches","costCenters":[],"links":[{"id":146974,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414713,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75333.htm","linkFileType":{"id":5,"text":"html"}},{"id":41789,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1029/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"San Bernardino County","otherGeospatial":"Superior Dry Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -117.1333,\n              35.2594\n            ],\n            [\n              -117.1333,\n              35.2197\n            ],\n            [\n              -117.0028,\n              35.2197\n            ],\n            [\n              -117.0028,\n              35.2594\n            ],\n            [\n              -117.1333,\n              35.2594\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b3b8","contributors":{"authors":[{"text":"Dockter, Roger D.","contributorId":81875,"corporation":false,"usgs":true,"family":"Dockter","given":"Roger","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":167684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70012404,"text":"70012404 - 1980 - A lead isotope study of mineralization in the Saudi Arabian Shield","interactions":[],"lastModifiedDate":"2012-03-12T17:19:01","indexId":"70012404","displayToPublicDate":"1980-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1336,"text":"Contributions to Mineralogy and Petrology","active":true,"publicationSubtype":{"id":10}},"title":"A lead isotope study of mineralization in the Saudi Arabian Shield","docAbstract":"New lead isotope data are presented for some late Precambrian and early Paleozoic vein and massive sulfide deposits in the Arabian Shield. Using the Stacey Kramers (1975) model for lead isotope evolution, isochron model ages range between 720 m.y. and 420 m.y. Most of the massive sulfide deposits in the region formed before 680 m.y. ago, during evolution of the shield. Vein type mineralization of higher lead content occurred during the Pan African event about 550 m.y. ago and continued through the Najd period of extensive faulting in the shield that ended about 530 m.y. ago. Late post-tectonic metamorphism may have been responsible for vein deposits that have model ages less than 500 m.y. Alternatively some of these younger model ages may be too low due to the mineralizing fluids acquiring radiogenic lead from appreciably older local crustal rocks at the time of ore formation. The low207Pb/204Pb ratios found for the deposits in the main part of the shield and for those in north-eastern Egypt, indicate that the Arabian craton was formed in an oceanic crustal environment during the late Precambrian. Involvement of older, upper-crustal material in the formation of the ore deposits in this part of the shield is precluded by their low207Pb/204Pb and208Pb/204Pb characteristics. In the eastern part of the shield, east of longitude 44??20???E towards the Al Amar-Idsas fault region, lead data are quite different. They exhibit a linear207Pb/204Pb-206Pb/204Pb relationship together with distinctly higher208Pb/204Pb characteristics. These data imply the existence of lower crustal rocks of early Proterozoic age that apparently have underthrust the shield rocks from the east. If most of the samples we have analyzed from this easterly region were mineralized 530 m.y. ago, then the age of the older continental rocks is 2,100??300 m.y. (2??). The presence of upper crustal rocks, possibly also of early Proterozoic age, is indicated by galena data from Hailan in South Yemen and also from near Muscat in Oman. These data are the first to indicate such old continental material in these regions. ?? 1980 Springer-Verlag.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Contributions to Mineralogy and Petrology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisherLocation":"Springer-Verlag","doi":"10.1007/BF01132003","issn":"00107999","usgsCitation":"Stacey, J.S., Doe, B.R., Roberts, R.J., Delevaux, M., and Gramlich, J.W., 1980, A lead isotope study of mineralization in the Saudi Arabian Shield: Contributions to Mineralogy and Petrology, v. 74, no. 2, p. 175-188, https://doi.org/10.1007/BF01132003.","startPage":"175","endPage":"188","numberOfPages":"14","costCenters":[],"links":[{"id":205282,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01132003"},{"id":222657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"74","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e435e4b0c8380cd464db","contributors":{"authors":[{"text":"Stacey, J. S.","contributorId":72785,"corporation":false,"usgs":true,"family":"Stacey","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":363463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doe, B. R.","contributorId":52173,"corporation":false,"usgs":true,"family":"Doe","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":363460,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roberts, R. J.","contributorId":58250,"corporation":false,"usgs":true,"family":"Roberts","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":363461,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Delevaux, M.H.","contributorId":27853,"corporation":false,"usgs":true,"family":"Delevaux","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":363459,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Gramlich, J. W.","contributorId":69967,"corporation":false,"usgs":false,"family":"Gramlich","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":363462,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70236599,"text":"70236599 - 1980 - Satellite image atlas of glaciers","interactions":[],"lastModifiedDate":"2022-09-12T17:02:34.116305","indexId":"70236599","displayToPublicDate":"1978-09-01T11:35:57","publicationYear":"1980","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesTitle":{"id":5644,"text":"IAHS Red Book","active":true,"publicationSubtype":{"id":19}},"seriesNumber":"126","title":"Satellite image atlas of glaciers","docAbstract":"<p>The US Geological Survey has initiated a project to prepare a satellite image atlas of glaciers with the cooperation of a number of US and international organizations. The atlas will include the geographical distribution of glaciers as well as topics of glaciology and related environmental phenomena using Landsat, NOAA and other satellite data. 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,{"id":57488,"text":"wdrMDDE781 - 1979 - Water resources data for Maryland and Delaware, water year 1978","interactions":[],"lastModifiedDate":"2021-01-22T19:30:19.560537","indexId":"wdrMDDE781","displayToPublicDate":"2021-01-22T14:45:00","publicationYear":"1979","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":"MD-DE-78-1","displayTitle":"Water Resources Data for Maryland and Delaware, Water Year 1978","title":"Water resources data for Maryland and Delaware, water year 1978","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMDDE781","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, Water resources data for Maryland and Delaware, water year 1978: U.S. Geological Survey Water Data Report MD-DE-78-1, 322 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 \"}}]}","contact":"<p><a href=\"https://pubs.er.usgs.gov/contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcdf8","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":533120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70180028,"text":"70180028 - 1979 - Developing a state water plan: Ground-water conditions in Utah, spring of 1979","interactions":[],"lastModifiedDate":"2017-01-23T13:08:35","indexId":"70180028","displayToPublicDate":"2017-01-01T00:00:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":110,"text":"Cooperative Investigations Report","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"18","title":"Developing a state water plan: Ground-water conditions in Utah, spring of 1979","docAbstract":"<p>This report is the sixteenth in a series of annual reports that describe ground-water conditions in Utah. Reports in this series, prepared cooperatively by the U.S. Geological Survey and the Utah Division of Water Resources, provide data to enable interested parties to keep abreast of changing ground-water conditions.</p><p>This report, like the others in the series, contains information on well construction, ground-water withdrawals, water-level changes, and related changes in precipitation and streamflow. Supplementary data such as graphs showing chemical quality of water and maps showing water-table configuration are included in reports of this series only for those years or areas for which applicable data are available and are important to a discussion of changing ground-water conditions.</p><p>This report includes individual discussions of selected major areas of ground-water withdrawal in the State for the calendar year 1978. Water-level fluctuations, however, are described for the period spring 1978 to spring 1979. Much of the data used in this report were collected by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Resources","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the State of Utah","usgsCitation":"Price, D., Jibson, W., Contratto, P., Mower, R.W., Steiger, J.I., Jensen, V., ReMillard, M.D., Emett, D.C., Sumison, C., Carroll, P., Neff, L., Sandberg, G.W., and Herbert, L.R., 1979, Developing a state water plan: Ground-water conditions in Utah, spring of 1979: Cooperative Investigations Report 18, vi, 68 p.","productDescription":"vi, 68 p.","numberOfPages":"76","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":333721,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":333720,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=50-1-186"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5887248be4b08aa8f945abf6","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":659892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jibson, W.N.","contributorId":27928,"corporation":false,"usgs":true,"family":"Jibson","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":659893,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Contratto, P. Kay","contributorId":15598,"corporation":false,"usgs":true,"family":"Contratto","given":"P. Kay","affiliations":[],"preferred":false,"id":659894,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659895,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Steiger, Judy I. jsteiger@usgs.gov","contributorId":3689,"corporation":false,"usgs":true,"family":"Steiger","given":"Judy","email":"jsteiger@usgs.gov","middleInitial":"I.","affiliations":[],"preferred":true,"id":659896,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Jensen, V.L.","contributorId":99034,"corporation":false,"usgs":true,"family":"Jensen","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":659897,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"ReMillard, M. D.","contributorId":38645,"corporation":false,"usgs":true,"family":"ReMillard","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":659898,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Emett, D. C.","contributorId":21213,"corporation":false,"usgs":true,"family":"Emett","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":659899,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Sumison, C.T.","contributorId":39057,"corporation":false,"usgs":true,"family":"Sumison","given":"C.T.","email":"","affiliations":[],"preferred":false,"id":659900,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Carroll, P.A.","contributorId":178594,"corporation":false,"usgs":false,"family":"Carroll","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":659901,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Neff, L.J.","contributorId":178596,"corporation":false,"usgs":false,"family":"Neff","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":659902,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Sandberg, G. W.","contributorId":55426,"corporation":false,"usgs":true,"family":"Sandberg","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":659903,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Herbert, L. R.","contributorId":39865,"corporation":false,"usgs":true,"family":"Herbert","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":659904,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":70159096,"text":"70159096 - 1979 - Preliminary geologic and geophysical data of the UE25a-3 exploratory drill hole, Nevada Test Site, Nevada","interactions":[],"lastModifiedDate":"2015-10-22T10:20:52","indexId":"70159096","displayToPublicDate":"2015-07-14T13:15:00","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Preliminary geologic and geophysical data of the UE25a-3 exploratory drill hole, Nevada Test Site, Nevada","docAbstract":"<p>The UE25a-3 drill hole, located in the Calico Hills area, southwestern part of the Nevada Test Site, was drilled as part of an effort to evaluate the Calico Hills area as a possible nuclear waste repository site. The purpose of the drill hole was to verify the existence of an intrusive crystalline body in the subsurface and to determine the stratigraphy, structure, and nature of fractures of the cored rocks. Cored samples were obtained for mineral, chemical, and material property analyses.</p>\n<p>Continuous cores were taken from 30.5 m (100ft) to total depth of 771.2 m (2,530.1 ft) of units J and I{?) (Late Mississippian age) of the Eleana Formation. The drill hole penetrated 416.1 m (1 ,365ft) of argillite, and 304.5 m (999ft) of thermally altered argillite of unit J, and 50.6 m (166ft) of marble of unit I(?). No crystalline rocks were intersected by the drill hole.</p>\n<p>Numerous high-angle faults and brecciated zones were intersected by the drill hole. The units cored were intensely fractured with fracture analysis of the core consisting of frequency of fractures, dips of fractures, open and closed (sealed) fractures and types of fracture sealing or coating material. Twenty-four hundred and thirty fractures, representing approximately 30 percent of the fractures present, indicate an average fracture frequency of 13.2 fractures per meter, predominantly high-angle dips with 66 percent of the fractures closed. Fractures in the argillite interval are sealed or coated predominantly with kaolinite, nacrite, and dickite. Calcite, chlorite, and magnetite are present in fractures in the altered argillite interval. Fractures in the marble interval are sealed or coated with calcite, dolomite, and ferruginous clay. The core index indicates that the lower half of the drilled interval is more competent than the upper half.</p>\n<p>Borehole geophysical logs were run by the Birdwell Division of Seismograph Service Corporation for geologic correlations and lithologic characterizations. The logs include: caliper, density, resistivity, spontaneous potential, Vibroseis, 3-D velocity, neutron, and gamma-ray logs. Lithologic boundaries and structures correlate to responses in the logs.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70159096","usgsCitation":"Maldonado, F., Muller, D.C., and Morrison, J., 1979, Preliminary geologic and geophysical data of the UE25a-3 exploratory drill hole, Nevada Test Site, Nevada, Report: iii, 43 p.; 1 Plate: 18.94 x 34.10 inches, https://doi.org/10.3133/70159096.","productDescription":"Report: iii, 43 p.; 1 Plate: 18.94 x 34.10 inches","numberOfPages":"48","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309924,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70159096.jpg"},{"id":310369,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70159096/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}},{"id":310368,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70159096/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","otherGeospatial":"Calico Hills","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.93847656250001,\n              37.01132594307015\n            ],\n            [\n              -114.85107421875,\n              35.36217605914681\n            ],\n            [\n              -114.268798828125,\n              35.44277092585766\n            ],\n            [\n              -114.3017578125,\n              37.09023980307208\n            ],\n            [\n              -114.32373046875,\n              37.87485339352928\n            ],\n            [\n              -114.444580078125,\n              38.25543637637947\n            ],\n            [\n              -114.70825195312501,\n              38.736946065676\n            ],\n            [\n              -117.8173828125,\n              38.71980474264239\n            ],\n            [\n              -118.68530273437501,\n              38.38472766885085\n            ],\n            [\n              -116.93847656250001,\n              37.01132594307015\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5620ce8fe4b06217fc478b08","contributors":{"authors":[{"text":"Maldonado, Florian fmaldona@usgs.gov","contributorId":805,"corporation":false,"usgs":true,"family":"Maldonado","given":"Florian","email":"fmaldona@usgs.gov","affiliations":[],"preferred":true,"id":577591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muller, D. C.","contributorId":75936,"corporation":false,"usgs":true,"family":"Muller","given":"D.","middleInitial":"C.","affiliations":[],"preferred":false,"id":577592,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morrison, J.N.","contributorId":95510,"corporation":false,"usgs":true,"family":"Morrison","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":577593,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039176,"text":"70039176 - 1979 - Land use statistics for West Virginia, Part I","interactions":[],"lastModifiedDate":"2012-07-24T01:01:47","indexId":"70039176","displayToPublicDate":"2012-01-01T14:36:33","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":249,"text":"Environmental Geology Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"18","title":"Land use statistics for West Virginia, Part I","docAbstract":"The West Virginia Geological and Economic Survey and the United States Geological Survey have completed a cooperative program to provide land-use and land-cover maps and data for the State. This program begins to satisfy a longstanding need for a consistent level of detail, standardization in categorization, and scale of compilation for land-use and land-cover maps and data. The statistical information contained in this Bulletin provides land-use acreage tabulations for the first 20 counties that have been completed. Statistics are being compiled for the remaining counties and will be published shortly. This information has been derived from the recently completed Land-Use Map of West Virginia (on open file at the West Virginia Geological and Economic Survey - Environmental Section). In addition to land-use acreage, we have also included land-use percent. All statistics throughout this Bulletin are in the same format for ease of comparison.","language":"English","publisher":"West Virginia Geological and Economic Survey","collaboration":"Permission to reproduce this report is granted if West Virginia Geological and Economic Survey is acknowledged.","usgsCitation":"Erwin, R.B., West Virginia Geological and Economic Survey, and Water Resources Division, U.S. Geological Survey, 1979, Land use statistics for West Virginia, Part I: Environmental Geology Bulletin 18, 25 p.","productDescription":"25 p.","costCenters":[],"links":[{"id":261332,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/othergov/70039176/report.pdf"},{"id":261333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/othergov/70039176/report-thumb.jpg"}],"country":"United States","state":"West Virginia","county":"Braxton;Calhoun;Clay;Doddridge;Gilmer;Harrison;Jackson;Lewis;Nicholas;Pendleton;Pleasants;Pocahontas;Ritchie;Roane;Tyler;Upshur;Webster;Wetzel;Wirt;Wood","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.66666666666667,37.166666666666664 ], [ -82.66666666666667,40.666666666666664 ], [ -77.66666666666667,40.666666666666664 ], [ -77.66666666666667,37.166666666666664 ], [ -82.66666666666667,37.166666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a439ee4b0c8380cd6649d","contributors":{"authors":[{"text":"Erwin, Robert B.","contributorId":33165,"corporation":false,"usgs":true,"family":"Erwin","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":465736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"West Virginia Geological and Economic Survey","contributorId":127943,"corporation":true,"usgs":false,"organization":"West Virginia Geological and Economic Survey","id":535224,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535225,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70039032,"text":"70039032 - 1979 - United States Geological Survey Yearbook, fiscal year 1978","interactions":[],"lastModifiedDate":"2017-03-08T16:45:01","indexId":"70039032","displayToPublicDate":"2012-01-01T11:39:03","publicationYear":"1979","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":392,"text":"Yearbook","active":false,"publicationSubtype":{"id":6}},"title":"United States Geological Survey Yearbook, fiscal year 1978","docAbstract":"Fiscal year 1978 saw the U.S. Geological Survey continuing to perform its basic historical missions of collecting, analyzing, and disseminating information about the Earth, its processes, and its water and mineral resources. Classifying Federal lands and supervising lessee mineral extraction operations on those lands were also major Survey concerns during the year. In addition, substantial progress was made in the exploration and assessment of the petroleum potential of the National Petroleum Reserve in Alaska, a recently assigned mission. These basic missions found expression in a wide range of program activities and interests as diverse as the sands of Mars and the volcanoes of Hawaii. Programs included assessment of numerous potential energy and mineral resources, study of earthquakes and other geologic hazards, appraisal of the magnitude and quality of the Nation's water resources, and supervision of lease operations on Federal lands. The Survey also was involved in developing data on land use and producing topographic, geologic, and hydrologic maps for public and private use. In cooperation with other Federal agencies, the Survey participated in studies under the U.S. Climate Program and continued its analysis of data received from the two Viking landers on the surface of Mars. On April 3, 1978, Dr. H. William Menard became the 10th Director of the U.S. Geological Survey. Dr. Menard, who, until his appointment, was Professor of Geology at the Scripps Institution of Oceanography, San Diego, Calif., brings to the Director's post the experience gained in a long and successful career as a marine geologist and oceanographer. He succeeds Dr. Vincent E. McKelvey, who continues with the Survey as a senior research scientist.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/70039032","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1979, United States Geological Survey Yearbook, fiscal year 1978: Yearbook, vi, 208 p., https://doi.org/10.3133/70039032.","productDescription":"vi, 208 p.","costCenters":[],"links":[{"id":261269,"rank":800,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70039032/report.pdf","text":"Report","size":"73.02 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":261270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70039032/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc90e4b08c986b328ce9","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":535201,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10735,"text":"ofr791654 - 1979 - Preliminary summary of the U.S. Geological Survey strong-motion records from the October 15, 1979 Imperial Valley earthquake","interactions":[],"lastModifiedDate":"2012-02-10T00:10:07","indexId":"ofr791654","displayToPublicDate":"2011-09-20T00:00:00","publicationYear":"1979","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":"79-1654","title":"Preliminary summary of the U.S. Geological Survey strong-motion records from the October 15, 1979 Imperial Valley earthquake","docAbstract":"This report summarizes the data from near-in strong-motion accelerograph stations operated by the U.S. Geological Survey in the Imperial Valley of California at the time of the October 15, 1979 Imperial Valley earthquake. The purpose of this report is to alert others as to the nature of the strong-motion data that is available from this event. In order to provide the information in a timely manner, the report has been limited to a summary of the data. A similar preliminary report of strong-motion data collected by the Office of Strong-Motion Studies of the California Division of Mines and Geology has already been issued. A more complete report of all of the strong ground motion data is contemplated. This will require the cooperation of all of the agencies in both the U.S. and Mexico that operate strong-motion instruments in the region. A report on the processing of the data from near-in stations is in preparation. The moderate-size (magnitude 6.4) October 15, 1979 Imperial Valley earthquake was instrumentally located on the Imperial fault approximately 25 km southeast of El Centro, California. This location is approximately the same as that of the 1940 Imperial Valley earthquake.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr791654","collaboration":"In cooperation with the National Science Foundation","usgsCitation":"Porcella, R.L., and Matthiesen, R., 1979, Preliminary summary of the U.S. Geological Survey strong-motion records from the October 15, 1979 Imperial Valley earthquake: U.S. Geological Survey Open-File Report 79-1654, ii, 41 p., https://doi.org/10.3133/ofr791654.","productDescription":"ii, 41 p.","onlineOnly":"Y","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":379,"text":"Menlo Park Science Center","active":false,"usgs":true}],"links":[{"id":116315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr_79_1654.gif"},{"id":94157,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1979/1654/","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"California","city":"El Centro","otherGeospatial":"Imperial Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.75,32.75 ], [ -115.75,33.25 ], [ -115.25,33.25 ], [ -115.25,32.75 ], [ -115.75,32.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db669df8","contributors":{"authors":[{"text":"Porcella, R. L.","contributorId":102869,"corporation":false,"usgs":true,"family":"Porcella","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161877,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Matthiesen, R.B.","contributorId":102907,"corporation":false,"usgs":true,"family":"Matthiesen","given":"R.B.","email":"","affiliations":[],"preferred":false,"id":161878,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5223032,"text":"5223032 - 1979 - Feeding ecology and development of juvenile black ducks in Maine","interactions":[],"lastModifiedDate":"2017-05-16T09:36:39","indexId":"5223032","displayToPublicDate":"2010-06-16T12:19:18","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Feeding ecology and development of juvenile black ducks in Maine","docAbstract":"<p><span>Data from 41 juvenile Black Ducks (<i>Anas rubripes</i>) collected in the Penobscot River valley of Maine from June through August 1974-76 were used to estimate the proportion of aquatic invertebrates in the prefledging diet and the allometric growth rates of the tarsi, flight muscles, and alimentary system. The proportion of aquatic invertebrates in the diet of downy and partially feathered juveniles averaged 88 and 91% of dry weight, but decreased to 43% for fully feathered young. The most important invertebrate food organisms for juvenile Black Ducks were asellid isopods, molluscs, nymphs of Ephemeroptera and Odonata, and larvae of Coleoptera, Trichoptera, and Diptera. A high proportion of invertebrates was consumed during the period of fastest absolute and relative growth. Estimation of allometric growth rates with the power formula (Y = a·$X_{b}$) showed that (1) the legs were relatively large at hatching and developed slowly; (2) the flight muscles, which were relatively small at hatching, grew slowly until the 4-week period preceding fledging, when they increased as the 4.75 power of body weight; and (3) growth of the liver and gizzard was approximately proportional to body weight. The data support Ricklefs' thesis that delayed functional maturity of the wings permits an increase in the overall growth rate of waterfowl.</span></p>","language":"English","publisher":"American Ornithological Society","usgsCitation":"Reinecke, K.J., 1979, Feeding ecology and development of juvenile black ducks in Maine: The Auk, v. 96, no. 4, p. 737-745.","productDescription":"9 p.","startPage":"737","endPage":"745","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198052,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":18181,"rank":300,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/4085660 "}],"volume":"96","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5d9d","contributors":{"authors":[{"text":"Reinecke, Kenneth J.","contributorId":87275,"corporation":false,"usgs":true,"family":"Reinecke","given":"Kenneth","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":337716,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220978,"text":"5220978 - 1979 - Multiple-factor influences upon feeding flight rates at wading bird colonies (Alias: Are flight-line counts useful?)","interactions":[],"lastModifiedDate":"2018-02-27T17:13:58","indexId":"5220978","displayToPublicDate":"2010-06-16T12:19:12","publicationYear":"1979","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Multiple-factor influences upon feeding flight rates at wading bird colonies (Alias: Are flight-line counts useful?)","docAbstract":"<p> The temporal patterns of feeding, resting, and reproductive behavior in colonial wading birds have been studied by a number of investigators (Recher and Recher 1972, King 1974, Capen 1978, Custer and Osborn 1978, Kushlan 1978) both on a short-term (daily) and long-term (annual) basis. In coastal marine environments, activities at colonies are influenced by tides (Recher and Recher 1972, Krebs 1974, Custer and Osborn 1978), time of day (Kushlan 1978) and phase of the nesting cycle (Kahl 1964).</p><p> The purpose of this paper is twofold: (1) to examine the effects of tide, time of day (physical factors), nesting phase, colony site, and spe cies identity (biological factors) on feeding flight rates at breeding col onies and, as a result of this, (2) to evaluate the usefulness of feeding flight counts as an index of the number of nests in the colony.</p><p> Earlier work suggests that the relationship between the number of in dividuals flying to and from the nesting colony may be quite consistent with nest numbers. Thus, by monitoring flights from remote locations, ob servers might obtain relatively accurate census data while minimizing time and disturbance at colonies. Recent concern for the deleterious impact of humans at waterbird colonies (Buckley and Buckley 1976, Ellison and Cleary 1978) underscores the need to investigate alternative census methods.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the 1979 conference of the colonial waterbird group","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"1979 conference of the colonial waterbird group","conferenceDate":"October 25-28, 1979","conferenceLocation":"Lafayette, LA","language":"English","publisher":"Waterbird Society","usgsCitation":"Erwin, R.M., and Ogden, J.C., 1979, Multiple-factor influences upon feeding flight rates at wading bird colonies (Alias: Are flight-line counts useful?), <i>in</i> Proceedings of the 1979 conference of the colonial waterbird group, v. 3, Lafayette, LA, October 25-28, 1979, p. 225-234.","productDescription":"10 p.","startPage":"225","endPage":"234","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":193421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":352101,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.jstor.org/stable/4626717"}],"volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b48c3","contributors":{"compilers":[{"text":"Southern, William E.","contributorId":68919,"corporation":false,"usgs":false,"family":"Southern","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":729781,"contributorType":{"id":3,"text":"Compilers"},"rank":1}],"authors":[{"text":"Erwin, R. Michael 0000-0003-2108-9502","orcid":"https://orcid.org/0000-0003-2108-9502","contributorId":57125,"corporation":false,"usgs":true,"family":"Erwin","given":"R.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":332799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ogden, John C.","contributorId":67895,"corporation":false,"usgs":true,"family":"Ogden","given":"John","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":332800,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5221464,"text":"5221464 - 1979 - Acute oral and percutaneous toxicity of pesticides to mallards: Correlations with mammalian toxicity data","interactions":[],"lastModifiedDate":"2020-05-12T14:40:53.627551","indexId":"5221464","displayToPublicDate":"2010-06-16T12:18:37","publicationYear":"1979","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3612,"text":"Toxicology and Applied Pharmacology","active":true,"publicationSubtype":{"id":10}},"title":"Acute oral and percutaneous toxicity of pesticides to mallards: Correlations with mammalian toxicity data","docAbstract":"<p><span>Acute oral (po) and 24-hr percutaneous (perc) LD50 values for 21 common pesticides (19 anticholinesterases, of which 18 were organophosphates, and one was a carbamate; one was an organochlorine central nervous system stimulant; and one was an organonitrogen pneumotoxicant) were determined in mallards (</span><i>Anas platyrhynchos</i><span>). Three of the pesticides tested were more toxic percutaneously than orally. An index to the percutaneous hazard of a pesticide, the dermal toxicity index (DTI = po LD50/perc LD50 × 100), was also calculated for each pesticide. These toxicity values in mallards were compared with toxicity data for rats from the literature. Significant positive correlations were found between log po and log percutaneous LD50 values in mallards (</span><i>r</i><span>&nbsp;= 0.65,&nbsp;</span><i>p</i><span>&nbsp;&lt; 0.01), between log po LD50 values in mallards and in rats (</span><i>r</i><span>&nbsp;= 0.71,&nbsp;</span><i>p</i><span>&nbsp;&lt; 0.01), and between log DTI values in mallards and in rats (</span><i>r</i><span>&nbsp;= 0.52,&nbsp;</span><i>p</i><span>&nbsp;&lt; 0.05). Percutaneous toxicity values were not significantly correlated between mallards and rats (</span><i>r</i><span>&nbsp;= 0.36,&nbsp;</span><i>p</i><span>&nbsp;&gt; 0.10). Variations in percutaneous methodologies are discussed with reference to interspecies variation in toxicity values. It is recommended that a mammalian DTI value approaching 30 be used as a guideline for the initiation of percutaneous toxicity studies in birds, when the po LD50 and/or projected percutaneous LD50 are less than expected field exposure levels.</span></p>","largerWorkTitle":"","language":"English","publisher":"Elsevier","doi":"10.1016/0041-008X(79)90515-5","usgsCitation":"Hudson, R.H., Haegele, M.A., and Tucker, R.K., 1979, Acute oral and percutaneous toxicity of pesticides to mallards: Correlations with mammalian toxicity data: Toxicology and Applied Pharmacology, v. 47, no. 3, p. 451-460, https://doi.org/10.1016/0041-008X(79)90515-5.","productDescription":"10 p.","startPage":"451","endPage":"460","numberOfPages":"10","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198372,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"47","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699c3c","contributors":{"authors":[{"text":"Hudson, R. H.","contributorId":29534,"corporation":false,"usgs":true,"family":"Hudson","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":333913,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haegele, M. A.","contributorId":107010,"corporation":false,"usgs":true,"family":"Haegele","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":333915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tucker, R. K.","contributorId":96383,"corporation":false,"usgs":true,"family":"Tucker","given":"R.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":333914,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":5211356,"text":"5211356 - 1979 - Seasonal occurrence and distribution of submerged aquatic macrophytes in the tidal Potomac River","interactions":[],"lastModifiedDate":"2019-07-29T12:00:34","indexId":"5211356","displayToPublicDate":"2009-06-09T09:23:19","publicationYear":"1979","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Seasonal occurrence and distribution of submerged aquatic macrophytes in the tidal Potomac River","docAbstract":"A systematic survey was conducted in the Tidal Potomac River in 1978 to determine the presence, abundance, and phenology of submersed aquatic macrophytes.  The survey covered 81.5 km of main river and 59.3 km of tributary on the Maryland shore.  Four regions were selected for the study: (1) Piscataway - Mattawoman Creek region (fresh-tidal river), (2) Nanjemoy Creek-Port Tobacco River region (transition zone), (3) Wicomico River region (estuary), and (4) St. Marys River region (estuary).  The Wicomico River region was subdivided into fresh tidal river, transition zone and estuary for purposes of date analysis.  Data were gathered by sampling each 15 m along transects running perpendicular to shore for a maximum distance of 300 m.  Modified oyster tongs were used to sample both plants and benthic soils from an outboard boat.  A total of 131 transects were established with a total of approximately 3500 grabs being taken per sampling period.  Sampling was initiated in the spring and repeated in the summer and fall.  Highest plant diversity and productivity were measured in the transition zone extending from Lower Cedar Point to beyond Maryland Point, a distance of approximately 30 km, and in the transition zone of the Wicomico River above Chaptico Bay.  Fresh tidal areas were devoid of plants.  The estuary had a sparse growth of horned pondweed (Zannichellia palustris) and widgeon grass (Ruppia maritima) in the spring: horned pondweed was not found in summer or fall.  Redhead grass (Potomageton perfoliatus) was the most abundant pondweed; it matured in early summer and died back in mid-to-late summer.  Wild celery (Vallisneria americana) and widgeon grass matured in early-to-late fall and were the most abundant plants during that period.  Data analysis is being finalized and a publication is in preparation.  This research will be continued over the next several seasons as part of the long term USGS effort on the Potomac","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Seminar on water quality in the tidal Potomac River, December 1978","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, Va.","usgsCitation":"Haramis, G., Carter, V., Gammon, P., and Hupp, C., 1979, Seasonal occurrence and distribution of submerged aquatic macrophytes in the tidal Potomac River, chap. <i>of</i> Seminar on water quality in the tidal Potomac River, December 1978.","productDescription":"21","startPage":"19 (abs)","numberOfPages":"21","costCenters":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true},{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200844,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685e32","contributors":{"authors":[{"text":"Haramis, G.M.","contributorId":101212,"corporation":false,"usgs":true,"family":"Haramis","given":"G.M.","email":"","affiliations":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"preferred":false,"id":330835,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carter, V.","contributorId":61115,"corporation":false,"usgs":true,"family":"Carter","given":"V.","email":"","affiliations":[],"preferred":false,"id":330833,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gammon, P.","contributorId":68861,"corporation":false,"usgs":true,"family":"Gammon","given":"P.","affiliations":[],"preferred":false,"id":330834,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hupp, C. 0000-0003-1853-9197","orcid":"https://orcid.org/0000-0003-1853-9197","contributorId":59150,"corporation":false,"usgs":true,"family":"Hupp","given":"C.","affiliations":[],"preferred":false,"id":330832,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":5210116,"text":"5210116 - 1979 - Bird communities associated with succession and management of lowland conifer forests","interactions":[],"lastModifiedDate":"2012-02-02T00:15:17","indexId":"5210116","displayToPublicDate":"2009-06-09T09:23:16","publicationYear":"1979","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Bird communities associated with succession and management of lowland conifer forests","docAbstract":"Data from published bird censuses were used to determine changes in avian communities in relation to plant succession, fire, type conversion, and timber management practices in lowland conifer forests in the northeastern United States.  With modifications in current logging practices, habitat for the bird species that nest in undisturbed stands can be provided.  Management guidelines are recommended.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Management of North Central and Northeastern Forests for Nongame Birds, Proceedings of the Workshop","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"North Central Forest Experiment Station, U.S. Forest Service","publisherLocation":"St. Paul, MN","collaboration":"  PDF on file: 2195_Dawson.pdf","usgsCitation":"Dawson, D., 1979, Bird communities associated with succession and management of lowland conifer forests, chap. <i>of</i> Management of North Central and Northeastern Forests for Nongame Birds, Proceedings of the Workshop, p. 120-131.","productDescription":"268","startPage":"120","endPage":"131","numberOfPages":"268","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":201184,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a28e4b07f02db611363","contributors":{"authors":[{"text":"Dawson, D.K. 0000-0001-7531-212X","orcid":"https://orcid.org/0000-0001-7531-212X","contributorId":94752,"corporation":false,"usgs":true,"family":"Dawson","given":"D.K.","affiliations":[],"preferred":false,"id":327810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}