The magnitude 5.2 (mb) northern Kentucky earthquake of July 27, 1980, at 18:52:21.8 UTC, located at 38.17N, 83.91W with a depth of 8 km (as determined by the National Earthquake Information Service), was particularly notable for the widespread damage it did, especially to older chimneys. Investigators from several different organizations were in the field shortly after the earthquake recording aftershocks and checking intensities. The data from postal intensity surveys and field personnel are still coming in, and it will be some time before it is all evaluated and analyzed. This preliminary list of the results of our own field investigations is being produced now in order that the information we gathered may be combined with that of other researchers for analysis.
Our investigation, conducted from July 28 to August 3, was designed to delineate the areal distribution of the intensities and to document the amount and type of damage in the epicentral region. Tentative intensities have been assigned to these reports and they have been plotted in figure 1. However, as more information becomes available from other investigators, some of these values may be changed and other locations may be added. Therefore no attempt has been made to contour the data. A maximum Modified Mercalli intensity of VII was assigned to Maysville, Ky., approximately 50 km north of the epicenter, based on the concentrated chimney and other types of building damage there. Elsewhere, similar but scattered chimney damage has been assigned intensity VI.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801242","usgsCitation":"Hopper, M.G., and Reagor, B.G., 1980, Field survey of intensity for the earthquake of July 27, 1980, Sharpsburg, Kentucky: U.S. Geological Survey Open-File Report 80-1242, 31 p., https://doi.org/10.3133/ofr801242.","productDescription":"31 p.","costCenters":[],"links":[{"id":426085,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1242/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142904,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1242/report-thumb.jpg"}],"country":"United States","state":"Kentucky","city":"Sharpsburg","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -83.94432382381211,\n 38.212285759691355\n ],\n [\n -83.94432382381211,\n 38.19556213355173\n ],\n [\n -83.91274325321169,\n 38.19556213355173\n ],\n [\n -83.91274325321169,\n 38.212285759691355\n ],\n [\n -83.94432382381211,\n 38.212285759691355\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5453","contributors":{"authors":[{"text":"Hopper, Margaret G. hopper@usgs.gov","contributorId":2227,"corporation":false,"usgs":true,"family":"Hopper","given":"Margaret","email":"hopper@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":159941,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reagor, B. Glen","contributorId":27038,"corporation":false,"usgs":true,"family":"Reagor","given":"B.","email":"","middleInitial":"Glen","affiliations":[],"preferred":false,"id":159942,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":21846,"text":"ofr80799 - 1980 - Grade and tonnage data used to construct models for the Regional Alaskan Mineral Resources Assessment Program","interactions":[],"lastModifiedDate":"2012-02-02T00:07:42","indexId":"ofr80799","displayToPublicDate":"1994-01-01T00:00:00","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":"80-799","title":"Grade and tonnage data used to construct models for the Regional Alaskan Mineral Resources Assessment Program","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr80799","issn":"0566-8174","usgsCitation":"Singer, D., Menzie, W., DeYoung, J., Sander, M., and Lott, A., 1980, Grade and tonnage data used to construct models for the Regional Alaskan Mineral Resources Assessment Program: U.S. Geological Survey Open-File Report 80-799, 59 p. ;27 cm., https://doi.org/10.3133/ofr80799.","productDescription":"59 p. ;27 cm.","costCenters":[],"links":[{"id":153180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0799/report-thumb.jpg"},{"id":51330,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0799/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49df","contributors":{"authors":[{"text":"Singer, D.A.","contributorId":69128,"corporation":false,"usgs":true,"family":"Singer","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":185946,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Menzie, W. D.","contributorId":52916,"corporation":false,"usgs":true,"family":"Menzie","given":"W. D.","affiliations":[],"preferred":false,"id":185945,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeYoung, J.H. Jr.","contributorId":86367,"corporation":false,"usgs":true,"family":"DeYoung","given":"J.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":185948,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Sander, M.","contributorId":74773,"corporation":false,"usgs":true,"family":"Sander","given":"M.","email":"","affiliations":[],"preferred":false,"id":185947,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lott, A.","contributorId":107721,"corporation":false,"usgs":true,"family":"Lott","given":"A.","email":"","affiliations":[],"preferred":false,"id":185949,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":60226,"text":"mf1213 - 1980 - Distribution of salt structures in the Gulf of Mexico map and descriptive text","interactions":[],"lastModifiedDate":"2025-04-29T17:07:52.16796","indexId":"mf1213","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1213","title":"Distribution of salt structures in the Gulf of Mexico map and descriptive text","docAbstract":"Slender diapiric stocks, broad massifs, anticlinal masses, low-relief swells, and pillowy lobes of Middle to Upper Jurassic salt (Viniegra, 1971; Kirkland and Gerhard, 1971; Imlay, 1980) dominate the structural fabric of large parts of the continental margins and deep basin of the Gulf of Mexico (sht. 1, A). These structures, known collectively as \"salt domes,\" are almost exclusively features of the terrigenous elastic margins of the northern and southwestern Gulf and the central Sigsbee Plain (sht. 2, A). Some salt structures may be present in the East Mexico Slope province of the western gulf, but they are difficult to distinguish from diapiric and nondiapiric shale anticlines, which are the dominant structures on this margin. Except for some piercement domes and nonpiercement uplifts in the northern Florida shelf region and in the eastern Golfo de Campeche, salt structures are not known in the extensive carbonate platform provinces off western Florida and the Yucatan Peninsula. The accompanying compilation from seismic-reflection data documents the distribution of Gulf of Mexico salt features and helps to define boundaries of structural provinces formed mainly, or in part, by tectonic movement of salt.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1213","usgsCitation":"Martin, R.G., 1980, Distribution of salt structures in the Gulf of Mexico map and descriptive text: U.S. Geological Survey Miscellaneous Field Studies Map 1213, Report: 8 p.; 2 Plates: 40.57 x 51.58 inches and 43.99 x 47.58 inches, https://doi.org/10.3133/mf1213.","productDescription":"Report: 8 p.; 2 Plates: 40.57 x 51.58 inches and 43.99 x 47.58 inches","costCenters":[],"links":[{"id":485151,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mf/1213/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":183110,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1213/report-thumb.jpg"},{"id":483645,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1213/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":483646,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1213/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"otherGeospatial":"Gulf of Mexico","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -100,17 ], [ -100,32 ], [ -78,32 ], [ -78,17 ], [ -100,17 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63f5d7","contributors":{"authors":[{"text":"Martin, R. G.","contributorId":100431,"corporation":false,"usgs":true,"family":"Martin","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":263347,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":23061,"text":"ofr80917 - 1980 - Helicopter airborne electromagnetic survey (using the Dighem II system) of parts of the Lake City caldera, Hinsdale County, Colorado","interactions":[],"lastModifiedDate":"2021-10-20T21:11:17.47653","indexId":"ofr80917","displayToPublicDate":"1994-01-01T00:00:00","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":"80-917","title":"Helicopter airborne electromagnetic survey (using the Dighem II system) of parts of the Lake City caldera, Hinsdale County, Colorado","docAbstract":"The data presented herein is from an airborne electromagnetic-resistivity-survey conducted by Dighem Limited of Toronto Canada for the U.S. Geological Survey. The area surveyed is located in the western San Juan Mountains near Lake City, Colorado. The general area covered is between 37°45' and 38° latitude north and 107°15' and 107°35' longitude west. The survey flying was confined to nine valleys which surround the Lake City caldera. Four blocks were surveyed from October 22 to October 27, 1979 for a total of 535 line - kilometers. The survey was flown as part of a mineral appraisal study conducted in cooperation with Bureau of Land Management (BLM). The survey was done to detect massive mineralization, mainly copper, and to locate conductive faults that may be suitable sites for uranium mineralization.
To be useful, airborne electromagnetic measurements must be made within a few hundred feet of the surface. The area that was flown is so rugged that a helicopter rather than a fixed-wing aircraft was used.
Fraser and Dvorak summarize the data of the survey areas as follows: in the east and south, the ground resistivities varied over a broad range—, from 20 to 1000 ohm-m. The western and northern parts of the area were characterized by resistivities mostly in the 300 to 1000 ohm-m range. Several weak to moderate EM anomalies were located that may warrant ground follow-up work.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr80917","issn":"0094-9140","usgsCitation":"Fraser, D., and Dvorak, Z., 1980, Helicopter airborne electromagnetic survey (using the Dighem II system) of parts of the Lake City caldera, Hinsdale County, Colorado: U.S. Geological Survey Open-File Report 80-917, Report: 31 p.; 8 Plates: 24.19 x 42.36 inches or smaller, https://doi.org/10.3133/ofr80917.","productDescription":"Report: 31 p.; 8 Plates: 24.19 x 42.36 inches or smaller","costCenters":[],"links":[{"id":364330,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0917/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364329,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0917/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364328,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0917/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390708,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11825.htm"},{"id":364331,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0917/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364332,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0917/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52432,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0917/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364334,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0917/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364333,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0917/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":155639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0917/report-thumb.jpg"},{"id":364327,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0917/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","county":"Hinsdale County","otherGeospatial":"Lake City caldera","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107.507,\n 37.874\n ],\n [\n -107.25,\n 37.874\n ],\n [\n -107.25,\n 38.078\n ],\n [\n -107.507,\n 38.078\n ],\n [\n -107.507,\n 37.874\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635dec","contributors":{"authors":[{"text":"Fraser, D.C.","contributorId":35732,"corporation":false,"usgs":true,"family":"Fraser","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":189368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dvorak, Z.","contributorId":57487,"corporation":false,"usgs":true,"family":"Dvorak","given":"Z.","email":"","affiliations":[],"preferred":false,"id":189369,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55116,"text":"wdrWY792 - 1980 - Water resources data, Wyoming, water year 1979: Volume 2. Green River basin, Bear River basin, and Snake River basin","interactions":[],"lastModifiedDate":"2025-07-28T17:06:18.839359","indexId":"wdrWY792","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"WY-79-2","title":"Water resources data, Wyoming, water year 1979: Volume 2. Green River basin, Bear River basin, and Snake River basin","docAbstract":"Water resources data for the 1979 water year for Wyoming consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of wells. Volume 2 of this report contains discharge records for 62 gaging stations; stage and contents for 5 lakes and reservoirs; water quality for 39 gaging stations and 30 ungaged stations; and water levels for 8 observation wells. Also included are 25 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Wyoming.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWY792","collaboration":"Prepared in cooperation with the State of Wyoming and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data, Wyoming, water year 1979: Volume 2. 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Missouri River Basin","interactions":[],"lastModifiedDate":"2025-07-21T14:11:30.674051","indexId":"wdrWY791","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"WY-79-1","title":"Water resources data, Wyoming, water year 1979: Volume 1. Missouri River Basin","docAbstract":"Water resources data for the 1979 water year for Wyoming consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of wells. Volume 1 of this report contains discharge records for 166 gaging stations; stage only records for 1 lake; stage and contents for 11 lakes and reservoirs; water quality for 116 gaging stations, 101 ungaged stations, 70 wells and springs; and water levels for 36 observation wells. Also included are 75 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. This data represents that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Wyoming.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWY791","collaboration":"Prepared in cooperation with the State of Wyoming and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data, Wyoming, water year 1979: Volume 1. 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Green River basin, Bear River basin, and Snake River basin","interactions":[],"lastModifiedDate":"2025-07-21T14:14:50.357987","indexId":"wdrWY782","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"WY-78-2","title":"Water resources data, Wyoming, water year 1978: Volume 2. Green River basin, Bear River basin, and Snake River basin","docAbstract":"Water resources data for the 1978 water year for Wyoming consists of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of wells. Volume 2 of this report contains discharge records for 62 gaging stations; stage and contents for 5 lakes and reservoirs; water quality for 43 gaging stations, 19 ungaged stations, and 75 wells and springs; and water levels for 8 observation wells. Also included are 24 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Wyoming.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWY782","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1980, Water resources data, Wyoming, water year 1978: Volume 2. 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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1204C","usgsCitation":"Griscom, A., 1980, Maps showing aeromagnetic survey and interpretation of the Virgin Mountains Instant Study Area Clark County, Nevada: U.S. Geological Survey Miscellaneous Field Studies Map 1204, 32.08 x 34.47 inches, https://doi.org/10.3133/mf1204C.","productDescription":"32.08 x 34.47 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":183359,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1204C.PNG"},{"id":327246,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1204-C/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Nevada","otherGeospatial":"Virgin Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.25,36.5 ], [ -114.25,36.666666666666664 ], [ -114,36.666666666666664 ], [ -114,36.5 ], [ -114.25,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6045c5","contributors":{"authors":[{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":262320,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43223,"text":"ofr801200 - 1980 - Geophysical, lithologic, and water-quality data from El Mirage Dry Lake, San Bernardino County, California","interactions":[],"lastModifiedDate":"2022-02-02T21:11:04.271649","indexId":"ofr801200","displayToPublicDate":"1994-01-01T00:00:00","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":"80-1200","title":"Geophysical, lithologic, and water-quality data from El Mirage Dry Lake, San Bernardino County, California","docAbstract":"No abstract available.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80238","usgsCitation":"Gunn, M., Hayashida, B., and Lee, W., 1980, 1979 annual index of current earthquake literature: U.S. Geological Survey Open-File Report 80-238, 320 p., https://doi.org/10.3133/ofr80238.","productDescription":"320 p.","costCenters":[],"links":[{"id":408717,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0238/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":151962,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0238/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4912e4b0b290850eedbf","contributors":{"authors":[{"text":"Gunn, M.L.","contributorId":16036,"corporation":false,"usgs":true,"family":"Gunn","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":180455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hayashida, B.S.","contributorId":42212,"corporation":false,"usgs":true,"family":"Hayashida","given":"B.S.","email":"","affiliations":[],"preferred":false,"id":180456,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lee, William Hung Kan","contributorId":83502,"corporation":false,"usgs":true,"family":"Lee","given":"William Hung Kan","affiliations":[],"preferred":false,"id":180457,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19107,"text":"ofr80759 - 1980 - Flood magnitude and frequency of small streams in Indiana: Preliminary estimating equations","interactions":[],"lastModifiedDate":"2022-08-09T15:48:08.503051","indexId":"ofr80759","displayToPublicDate":"1994-01-01T00:00:00","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":"80-759","title":"Flood magnitude and frequency of small streams in Indiana: Preliminary estimating equations","docAbstract":"This interim report presents preliminary estimating equations developed for the ongoing study, \"Flood Frequency of Small Streams in Indiana.\" The equations were developed by the multiple-regression technique from data collected at 57 crest-stage-gage and 15 rainfall-runoff sites in the study and from 133 streamflow stations in Indiana and 11 in eastern Illinois. Peak discharge was used as the dependent variable, and basin characteristics were used as the independent variables in the analysis. Drainage area and precipitation were the most significant basin characteristics.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e70bc","contributors":{"authors":[{"text":"Gold, Robert L.","contributorId":78324,"corporation":false,"usgs":true,"family":"Gold","given":"Robert L.","affiliations":[],"preferred":false,"id":180316,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6441,"text":"pp1132 - 1980 - Recent vegetation changes along the Colorado River between Glen Canyon Dam and Lake Mead, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:55","indexId":"pp1132","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1132","title":"Recent vegetation changes along the Colorado River between Glen Canyon Dam and Lake Mead, Arizona","docAbstract":"Vegetation changes in the canyon of the Colorado River between Glen Canyon Dam and Lake Mead were studied by comparing photographs taken prior to completion of Glen Canyon Dam in 1963 with photographs taken afterwards at the same sites. In general, the older pictures show an absence of riparian plants along the banks of the river. The newer photographs of each pair were taken in 1972 through 1976 and reveal an increased density of many plant species. Exotic species, such as saltcedar and camel-thorn, and native riparian plants such as sandbar willow, arrowweed, desert broom and cattail, now form a new riparian community along much of the channel of the Colorado River between Glen Canyon Dam and Lake Mead. The matched photographs also reveal that changes have occurred in the amount of sand and silt deposited along the banks. Detailed maps are presented showing distribution of 25 plant species along the reach of the Colorado River studied. Data showing changes in the hydrologic regime since completion of Glen Canyon Dam are presented. (Kosco-USGS)","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1132","usgsCitation":"Turner, R.M., and Karpiscak, M.M., 1980, Recent vegetation changes along the Colorado River between Glen Canyon Dam and Lake Mead, Arizona: U.S. Geological Survey Professional Paper 1132, 125 p.; plates in pocket, https://doi.org/10.3133/pp1132.","productDescription":"125 p.; plates in pocket","costCenters":[],"links":[{"id":104556,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4730.htm","linkFileType":{"id":5,"text":"html"},"description":"4730"},{"id":121543,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1132/report-thumb.jpg"},{"id":33851,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1132/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33852,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1132/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33853,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1132/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33854,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1132/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a75e4b07f02db644bab","contributors":{"authors":[{"text":"Turner, Raymond Marriner","contributorId":20319,"corporation":false,"usgs":true,"family":"Turner","given":"Raymond","email":"","middleInitial":"Marriner","affiliations":[],"preferred":false,"id":152726,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Karpiscak, Martin M.","contributorId":106107,"corporation":false,"usgs":true,"family":"Karpiscak","given":"Martin","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":152727,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":6193,"text":"pp1174 - 1980 - The Lewis thrust fault and related structures in the Disturbed Belt, northwestern Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"pp1174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1980","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":"1174","title":"The Lewis thrust fault and related structures in the Disturbed Belt, northwestern Montana","docAbstract":"The classical Lewis thrust fault in Glacier National Park has now been mapped 125 km south of the park to Steamboat Mountain, where the trace dies out in folded middle Paleozoic rocks. The known length of the fault is 452 km, extending northward from Steamboat Mountain to a point 225 km into Canada, where the fault also dies out in Paleozoic rocks. \r\n\r\nAt the south end, the surface expression of the Lewis thrust begins in a shear zone in folded Mississippian rocks. To the north, the thrust progressively cuts downsection into Proterozoic Y (Belt) rocks near Glacier National Park. \r\n\r\nDisplacement on the Lewis plate increases northward from approximately 3 km on an easterly trending hinge line at the West Fork of the Sun River to a postulated 65 km at the southern edge of the park, where the stratigraphic throw is about 6,500 m. Present data indicate the thrust formed during very late Paleocene to very early Eocene time. \r\n\r\nThe Lewis thrust and related structures, the Hoadley thrust and the Continental Divide syncline, probably formed concurrently under the same stress field. The northern limit of the trace of the Hoadley thrust is within the lower portion of the Lewis plate, about 28 km north of where the Lewis thrust develops, and the Hoadley extends for at least 125 km to the south. Displacement of the Hoadley increases southward from about 1 km at the hinge line to an inferred 70 km near its known southern extent. If our inference is correct, the Hoadley is nearly the southern mirror image of the Lewis to the north. The Continental Divide syncline, a doubly plunging, broad, northerly trending open fold that is about 120 km long, is a major fold within the Lewis plate.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp1174","usgsCitation":"Mudge, M.R., and Earhart, R.L., 1980, The Lewis thrust fault and related structures in the Disturbed Belt, northwestern Montana: U.S. Geological Survey Professional Paper 1174, 18 p., https://doi.org/10.3133/pp1174.","productDescription":"18 p.","costCenters":[],"links":[{"id":121960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1174/report-thumb.jpg"},{"id":33348,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1174/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b087","contributors":{"authors":[{"text":"Mudge, Melville Rhodes","contributorId":77119,"corporation":false,"usgs":true,"family":"Mudge","given":"Melville","email":"","middleInitial":"Rhodes","affiliations":[],"preferred":false,"id":152273,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Earhart, Robert L.","contributorId":74729,"corporation":false,"usgs":true,"family":"Earhart","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":152272,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":8511,"text":"ofr80981 - 1980 - Hole-to-surface resistivity measurements at Salt Valley, Utah","interactions":[],"lastModifiedDate":"2022-07-18T21:50:10.338216","indexId":"ofr80981","displayToPublicDate":"1994-01-01T00:00:00","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":"80-981","title":"Hole-to-surface resistivity measurements at Salt Valley, Utah","docAbstract":"Evaporites are an important potential medium for the storage of radioactive wastes. In order to ascertain the viability of a proposed waste isolation site, it is necessary to study its geology without extensive drilling that might destroy its structural integrity. Hole-to-surface and hole-to-hole geophysical measurements can be useful in supplementing geologic data obtained from a few drill holes and can be used to aid the interpretation of surface geophysical measurements. The study presented in this paper was conducted at Salt Valley, Utah to test the feasibility of using hole-to-surface direct-current resistivity measurements to detect geologic inhomogeneities in evaporites. These measurements show the following:
(1) It is feasible to make hole-to-surface resistivity measurements over evaporites. However, near-surface steel casing can make it difficult to quantitatively analyze the field data with present interpretation techniques. Future investigations should include theoretical studies to solve interpretation problems when steel casing is in the hole and the mud is a high-conductivity brine.
(2) A comparison of measurements made from the three different source drill holes shows that the halite acts as an electrical insulator and most of the current emitted from the source is contained in the caprock.
(3) A comparison of measurements made parallel and perpendicular to the valley walls shows that there are more variations in the halitecaprock interface perpendicular than parallel to the axis of the Salt Valley anticline.
(4) Structurally complex interbeds within the salt may cause differences in the current distribution measured at the surface from current sources buried at different depths.
(5) Total field mapping would be more useful than the single-component data that were collected in this study.