{"pageNumber":"5911","pageRowStart":"147750","pageSize":"25","recordCount":165658,"records":[{"id":40252,"text":"ofr6698 - 1966 - Complete Bouguer gravity anomaly map of the San Francisco Mountains vicinity, Beaver and Millard Counties, Utah","interactions":[],"lastModifiedDate":"2022-09-13T18:12:12.325832","indexId":"ofr6698","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-98","title":"Complete Bouguer gravity anomaly map of the San Francisco Mountains vicinity, Beaver and Millard Counties, Utah","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6698","usgsCitation":"Peterson, D.L., 1966, Complete Bouguer gravity anomaly map of the San Francisco Mountains vicinity, Beaver and Millard Counties, Utah: U.S. Geological Survey Open-File Report 66-98, 1 Plate: 29.79 × 44.99 inches, https://doi.org/10.3133/ofr6698.","productDescription":"1 Plate: 29.79 × 44.99 inches","costCenters":[],"links":[{"id":173207,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":406610,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8145.htm","linkFileType":{"id":5,"text":"html"}},{"id":71327,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0098/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Utah","county":"Beaver County, Millard County","otherGeospatial":"San Francisco Mountains vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.5,\n              38.25\n            ],\n            [\n              -113,\n              38.25\n            ],\n            [\n              -113,\n              38.75\n            ],\n            [\n              -113.5,\n              38.75\n            ],\n            [\n              -113.5,\n              38.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a830f","contributors":{"authors":[{"text":"Peterson, Donald L.","contributorId":28597,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":223177,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41757,"text":"ofr66103 - 1966 - Aeromagnetic map of parts of Rockland, Watersmeet, Greenland, Ontonagon, and Iron Counties, Michigan, and Vilas and Forest Counties, Wisconsin","interactions":[{"subject":{"id":41757,"text":"ofr66103 - 1966 - Aeromagnetic map of parts of Rockland, Watersmeet, Greenland, Ontonagon, and Iron Counties, Michigan, and Vilas and Forest Counties, Wisconsin","indexId":"ofr66103","publicationYear":"1966","noYear":false,"title":"Aeromagnetic map of parts of Rockland, Watersmeet, Greenland, Ontonagon, and Iron Counties, Michigan, and Vilas and Forest Counties, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":63808,"text":"gp831 - 1972 - Aeromagnetic map of the Watersmeet region, Ontonagon and Gogebic Counties, Michigan, and Vilas County, Wisconsin","indexId":"gp831","publicationYear":"1972","noYear":false,"title":"Aeromagnetic map of the Watersmeet region, Ontonagon and Gogebic Counties, Michigan, and Vilas County, Wisconsin"},"id":1}],"supersededBy":{"id":63808,"text":"gp831 - 1972 - Aeromagnetic map of the Watersmeet region, Ontonagon and Gogebic Counties, Michigan, and Vilas County, Wisconsin","indexId":"gp831","publicationYear":"1972","noYear":false,"title":"Aeromagnetic map of the Watersmeet region, Ontonagon and Gogebic Counties, Michigan, and Vilas County, Wisconsin"},"lastModifiedDate":"2019-08-20T10:15:06","indexId":"ofr66103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-103","title":"Aeromagnetic map of parts of Rockland, Watersmeet, Greenland, Ontonagon, and Iron Counties, Michigan, and Vilas and Forest Counties, Wisconsin","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr66103","usgsCitation":"Philbin, P.W., and McCaslin, W.E., 1966, Aeromagnetic map of parts of Rockland, Watersmeet, Greenland, Ontonagon, and Iron Counties, Michigan, and Vilas and Forest Counties, Wisconsin: U.S. Geological Survey Open-File Report 66-103, 1 Plate: 26.90 x 58.43 inches, https://doi.org/10.3133/ofr66103.","productDescription":"1 Plate: 26.90 x 58.43 inches","costCenters":[],"links":[{"id":176771,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0103/report-thumb.jpg"},{"id":366706,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1966/0103/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697660","contributors":{"authors":[{"text":"Philbin, P. W.","contributorId":25915,"corporation":false,"usgs":true,"family":"Philbin","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":225485,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCaslin, W. E.","contributorId":37002,"corporation":false,"usgs":true,"family":"McCaslin","given":"W.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":225486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38794,"text":"pp560B - 1966 - Geology of the Arabian Peninsula - Yemen","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp560B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"560","chapter":"B","title":"Geology of the Arabian Peninsula - Yemen","language":"ENGLISH","doi":"10.3133/pp560B","usgsCitation":"Geukens, F., 1966, Geology of the Arabian Peninsula - Yemen: U.S. Geological Survey Professional Paper 560, p. B1-B23, https://doi.org/10.3133/pp560B.","productDescription":"p. B1-B23","costCenters":[],"links":[{"id":113240,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0560b/report.pdf","size":"9257","linkFileType":{"id":1,"text":"pdf"}},{"id":173513,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0560b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68358a","contributors":{"authors":[{"text":"Geukens, F.","contributorId":49032,"corporation":false,"usgs":true,"family":"Geukens","given":"F.","email":"","affiliations":[],"preferred":false,"id":220456,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33866,"text":"b1222C - 1966 - Geology and mineral deposits of the Powell River area, Claiborne and Union Counties, Tennessee","interactions":[{"subject":{"id":55517,"text":"ofr4553 - 1945 - Areal and economic geology of the Powell River area, Claiborne and Union Counties, Tennessee","indexId":"ofr4553","publicationYear":"1945","noYear":false,"title":"Areal and economic geology of the Powell River area, Claiborne and Union Counties, Tennessee"},"predicate":"SUPERSEDED_BY","object":{"id":33866,"text":"b1222C - 1966 - Geology and mineral deposits of the Powell River area, Claiborne and Union Counties, Tennessee","indexId":"b1222C","publicationYear":"1966","noYear":false,"chapter":"C","title":"Geology and mineral deposits of the Powell River area, Claiborne and Union Counties, Tennessee"},"id":1}],"lastModifiedDate":"2022-03-30T19:45:03.823726","indexId":"b1222C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1222","chapter":"C","title":"Geology and mineral deposits of the Powell River area, Claiborne and Union Counties, Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1222C","usgsCitation":"Brokaw, A.L., Rodgers, J., Kent, D.F., Laurence, R.A., and Behre, C.H., 1966, Geology and mineral deposits of the Powell River area, Claiborne and Union Counties, Tennessee: U.S. Geological Survey Bulletin 1222, Report: iii, 56 p.; 4 Plates: 33.04 × 20.33 inches or smaller, https://doi.org/10.3133/b1222C.","productDescription":"Report: iii, 56 p.; 4 Plates: 33.04 × 20.33 inches or smaller","costCenters":[],"links":[{"id":397894,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21294.htm"},{"id":96171,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1222c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96170,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1222c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96169,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1222c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96168,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1222c/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1222c/report-thumb.jpg"},{"id":96172,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1222c/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Tennessee","county":"Claiborne County, Union County","otherGeospatial":"Powell River area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.881,\n              36.346\n            ],\n            [\n              -83.619,\n              36.346\n            ],\n            [\n              -83.619,\n              36.53\n            ],\n            [\n              -83.8881,\n              36.53\n            ],\n            [\n              -83.881,\n              36.346\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46bc","contributors":{"authors":[{"text":"Brokaw, Arnold Leslie","contributorId":11205,"corporation":false,"usgs":true,"family":"Brokaw","given":"Arnold","email":"","middleInitial":"Leslie","affiliations":[],"preferred":false,"id":212074,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rodgers, John","contributorId":74436,"corporation":false,"usgs":true,"family":"Rodgers","given":"John","affiliations":[],"preferred":false,"id":212078,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kent, D. F.","contributorId":48232,"corporation":false,"usgs":true,"family":"Kent","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":212076,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Laurence, Robert A.","contributorId":34981,"corporation":false,"usgs":true,"family":"Laurence","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":212075,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Behre, C. H. Jr.","contributorId":68366,"corporation":false,"usgs":true,"family":"Behre","given":"C.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":212077,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":47027,"text":"ofr6656 - 1966 - Geologic map of the Molalla-Salem Slope area, Oregon","interactions":[{"subject":{"id":47027,"text":"ofr6656 - 1966 - Geologic map of the Molalla-Salem Slope area, Oregon","indexId":"ofr6656","publicationYear":"1966","noYear":false,"title":"Geologic map of the Molalla-Salem Slope area, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":1791,"text":"wsp1997 - 1972 - Geology and ground water of the Molalla-Salem slope area, northern Willamette Valley, Oregon","indexId":"wsp1997","publicationYear":"1972","noYear":false,"title":"Geology and ground water of the Molalla-Salem slope area, northern Willamette Valley, Oregon"},"id":1}],"supersededBy":{"id":1791,"text":"wsp1997 - 1972 - Geology and ground water of the Molalla-Salem slope area, northern Willamette Valley, Oregon","indexId":"wsp1997","publicationYear":"1972","noYear":false,"title":"Geology and ground water of the Molalla-Salem slope area, northern Willamette Valley, Oregon"},"lastModifiedDate":"2012-02-02T00:10:46","indexId":"ofr6656","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-56","title":"Geologic map of the Molalla-Salem Slope area, Oregon","language":"ENGLISH","doi":"10.3133/ofr6656","usgsCitation":"Hampton, E.R., 1966, Geologic map of the Molalla-Salem Slope area, Oregon: U.S. Geological Survey Open-File Report 66-56, 1 map., https://doi.org/10.3133/ofr6656.","productDescription":"1 map.","costCenters":[],"links":[{"id":170677,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968f8","contributors":{"authors":[{"text":"Hampton, E. R.","contributorId":57038,"corporation":false,"usgs":true,"family":"Hampton","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":234514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39027,"text":"pp341E - 1966 - Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil","interactions":[{"subject":{"id":46618,"text":"ofr61126 - 1961 - Geologic map of the Rio Piracicaba quadrangle, Minas Gerais, Brazil","indexId":"ofr61126","publicationYear":"1961","noYear":false,"title":"Geologic map of the Rio Piracicaba quadrangle, Minas Gerais, Brazil"},"predicate":"SUPERSEDED_BY","object":{"id":39027,"text":"pp341E - 1966 - Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil","indexId":"pp341E","publicationYear":"1966","noYear":false,"chapter":"E","title":"Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil"},"id":1},{"subject":{"id":47028,"text":"ofr61125 - 1961 - Geologic map of the Monlevade quadrangle, Minas Gerais, Brazil","indexId":"ofr61125","publicationYear":"1961","noYear":false,"title":"Geologic map of the Monlevade quadrangle, Minas Gerais, Brazil"},"predicate":"SUPERSEDED_BY","object":{"id":39027,"text":"pp341E - 1966 - Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil","indexId":"pp341E","publicationYear":"1966","noYear":false,"chapter":"E","title":"Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil"},"id":2},{"subject":{"id":47154,"text":"ofr61124 - 1961 - Geologic map and sections of the Andrade mine, Monlevade quadrangle, Minas Gerais, Brazil","indexId":"ofr61124","publicationYear":"1961","noYear":false,"title":"Geologic map and sections of the Andrade mine, Monlevade quadrangle, Minas Gerais, Brazil"},"predicate":"SUPERSEDED_BY","object":{"id":39027,"text":"pp341E - 1966 - Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil","indexId":"pp341E","publicationYear":"1966","noYear":false,"chapter":"E","title":"Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil"},"id":3}],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp341E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"341","chapter":"E","title":"Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and mineral resources of parts of Minas Gerais, Brazil","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp341E","usgsCitation":"Reeves, R., 1966, Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil: U.S. Geological Survey Professional Paper 341, p. E1-E58, https://doi.org/10.3133/pp341E.","productDescription":"p. E1-E58","costCenters":[],"links":[{"id":120531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0341e/report-thumb.jpg"},{"id":66169,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66170,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341e/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66171,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66172,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66173,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341e/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66174,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341e/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66175,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341e/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66176,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0341e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46ff","contributors":{"authors":[{"text":"Reeves, R.G.","contributorId":61890,"corporation":false,"usgs":true,"family":"Reeves","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":220825,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64175,"text":"gp549 - 1966 - Aeromagnetic map of the Bangor quadrangle, New Jersey and Pennsylvania","interactions":[],"lastModifiedDate":"2025-04-29T18:58:23.587948","indexId":"gp549","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"549","title":"Aeromagnetic map of the Bangor quadrangle, New Jersey and Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp549","usgsCitation":"Boynton, G.R., Pittillo, D., and Zandle, G.L., 1966, Aeromagnetic map of the Bangor quadrangle, New Jersey and Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 549, 1 Plate: 22.40 x 26.65 inches, https://doi.org/10.3133/gp549.","productDescription":"1 Plate: 22.40 x 26.65 inches","costCenters":[],"links":[{"id":254142,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0549/report-thumb.jpg"},{"id":250686,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0549/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250685,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0549/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":485164,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3503.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"New Jersey, Pennsylvania","otherGeospatial":"Bangor quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -75.25,\n              40.875\n            ],\n            [\n              -75.25,\n              40.75\n            ],\n            [\n              -75.125,\n              40.75\n            ],\n            [\n              -75.125,\n              40.875\n            ],\n            [\n              -75.25,\n              40.875\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697260","contributors":{"authors":[{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pittillo, D.R.","contributorId":91179,"corporation":false,"usgs":true,"family":"Pittillo","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":270125,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270123,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38849,"text":"pp543D - 1966 - Geologic effects of the March 1964 earthquake and associated seismic sea waves on Kodiak and nearby islands, Alaska","interactions":[],"lastModifiedDate":"2022-02-17T19:34:30.778879","indexId":"pp543D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"543","chapter":"D","title":"Geologic effects of the March 1964 earthquake and associated seismic sea waves on Kodiak and nearby islands, Alaska","docAbstract":"Kodiak Island and the nearby islands constitute a mountainous landmass with an aggregate area of 4,900 square miles that lies at the western border of the Gulf of Alaska and from 20 to 40 miles off the Alaskan mainland. Igneous and metamorphic rocks underlie most of the area except for a narrow belt of moderately to poorly indurated rocks bordering the Gulf of Alaska coast and local accumulations of unconsolidated alluvial and marine deposits along the streams and coast. The area is relatively undeveloped and is sparsely inhabited. About 4,800 of the 5,700 permanent residents in the area live in the city of Kodiak or at the Kodiak Naval Station.\n\nThe great earthquake, which occurred on March 27, 1964, at 5:36 p.m. Alaska standard time (March 28,1964, 0336 Greenwich mean time), and had a Richter magnitude of 8.4-8.5, was the most severe earthquake felt on Kodiak Island and its nearby islands in modern times. Although the epicenter lies in Prince William Sound 250 miles northeast of Kodiak—the principal city of the area—the areal distribution of the thousands of aftershocks that followed it, the local tectonic deformation, and the estimated source area of the subsequent seismic sea wave, all suggest that the Kodiak group of islands lay immediately adjacent to, and northwest of, the focal region from which the elastic seismic energy was radiated. The duration of strong ground motion in the area was estimated at 2½ minutes. Locally, the tremors were preceded by sounds audible to the human ear and were reportedly accompanied in several places by visible ground waves.\n\nIntensity and felt duration of the shocks during the main earthquake and aftershock sequence varied markedly within the area and were strongly influenced by the local geologic environment. Estimated Mercalli intensities in most areas underlain by unconsolidated Quaternary deposits ranged from VIII to as high as IX. In contrast, intensities in areas of upper Tertiary rock ranged from VII to VIII, and in areas of relatively well indurated lower Tertiary and Mesozoic rocks, from VI to VII.\n\nLocal subsidence of as much as 10 feet was widespread in noncohesive granular deposits through compaction, flow, and sliding that resulted from vibratory loading during the earthquake. This phenomenon, which was largely restricted to saturated beach and alluvial deposits or artificial fill, was locally accompanied by extensive cracking of the ground and attendant ejection of water and water-sediment mixtures.\n\nNumerous landslides, including a wide variety of rockfalls, rockslides, and flows along steep slopes, were triggered by the long-duration horizontal and vertical accelerations during the earthquake. The landslides are most numerous in a narrow belt along the southeast coast of Kodiak Island and the nearby offshore islands. Their abundance appears to be related to an area underlain predominantly by Tertiary rocks.\n\nTemporary and permanent changes of level occurred after the earthquake in some wells, lakes, and streams throughout the area; ice was cracked, and the salinity of a few wells increased. Permanent change of water level at some localities appears to be related to readjustments of fracture porosity by earthquake-induced movements of bedrock blocks. Increased salinity of wells in coastal areas resulted from encroachment of seawater into aquifiers after subsidence during the earthquake, and to flooding of watersheds by seismic sea waves.\n\nVertical displacements, both downward and upward, occurred throughout the area as a result of crustal warping along a northeast-trending axis. Most of Kodiak and all of Afognak, Shuyak, and adjacent islands are within a regional zone of subsidence whose trough plunges gently northeastward and approximately coincides with the mountainous backbone of Kodiak Island. Subsidence in excess of 6 feet occurred throughout the northern part of the zone-a maximum subsidence of 6½ feet having occurred on Marmot and, eastern Afognak Islands. Southeast of the axis of tectonic tilting, uplift of at least 2lh feet occurred in a narrow zone that includes most of the southeasterly capes of Kodiak Island, the southeastern half of Sitkalidak Island, and Sitkinak Island. The uplift is inferred to extend offshore over much or all of the continental shelf adjacent to the Kodiak group of islands. Within the affected area, tectonic subsidence, which was locally augmented by surficial subsidence of unconsolidated. deposits, caused widespread inundation of shorelines and attendant damage to intertidal organisms, nearshore terrestrial vegetation, and salmon-spawning areas.\n\nThe most devastating effect of the earthquake on Kodiak Island and nearby islands resulted from seismic sea waves that probably originated along a linear zone of differential uplift in the Gulf of Alaska. A train of at least seven seismic sea waves, having initial periods of 50–55 minutes, struck along all the southeast coast of the island group from 38 to 63 minutes after the earthquake. The southeast shores were repeatedly washed by destructive waves having runup heights along exposed coasts of perhaps as much as 40 feet above existing tide level, and of 8–20 feet along protected shores. Runup heights of the waves were much less on the northwest and southwest sides of the islands, and no wave damage was incurred there. Locally, high-velocity currents that accompanied the waves caused intense erosion and redistribution of unconsolidated natural and artificial shore deposits and of shallow sea-floor deposits.\n\nThe Alaska earthquake was the greatest natural catastrophe to befall the Kodiak Island area in historic time. The combination of seismic shock and the earthquake-related tectonic deformation and seismic sea waves took 18 lives, destroyed property worth about $45 million, and resulted in estimated losses of income to the fishing industry of an additional $5 million.\n\nMost of the damage and all of the loss of life were directly attributable to the seismic sea waves that crippled the city of Kodiak, wiped out the village of Kaguyak, and destroyed most of the village of Old Harbor and parts of the villages of Afognak and Uzinki. Bridges and segments of the highways in the vicinity of the city of Kodiak were washed out, and parts of the Kodiak Naval Station were inundated and damaged. Especially serious to all the damaged communities was the loss of fishing boats, seafood processing plants, and other waterfront installations, which had been the mainstay of the economy.\n\nAdditional heavy losses resulted from the combined regional tectonic and local surficial subsidence that occurred during the earthquake. Widespread shoreline flooding by high tides necessitated raising, protecting, or removing many installations otherwise undamaged by the earthquake or waves.\n\nStructural damage attributable to seismic shock during the earthquake was relatively light and was restricted to areas underlain by saturated unconsolidated deposits. The chief structural failure in the area as a result of shaking was the collapse of part of a cannery built on saturated beach deposits that were partially liquefied during the earthquake. Minor structural damage resulted from differential settlement and cracking of the ground on natural granular deposits and artificial fills. The overwhelming majority of structures are constructed on indurated bedrock; none of these sustained damage other than small losses resulting from shifting about and breakage of their contents.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Regional effects (Professional Paper 543)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp543D","usgsCitation":"Plafker, G., and Kachadoorian, R., 1966, Geologic effects of the March 1964 earthquake and associated seismic sea waves on Kodiak and nearby islands, Alaska: U.S. Geological Survey Professional Paper 543, vi, 46 p., https://doi.org/10.3133/pp543D.","productDescription":"vi, 46 p.","numberOfPages":"58","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":277742,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/pp543D.gif"},{"id":65810,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543d/pp543d_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":396126,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99029.htm"},{"id":277741,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543d/index.html"}],"country":"United States","state":"Alaska","otherGeospatial":"Afognak Island, Kodiak Island, Marmot Island, Rasberry Island, Shuyak Island, Sitkalidak Island, Sitkinak Island, Spruce Island, Tugidak Island, Uganik Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155,\n              56.3778\n            ],\n            [\n              -151.6917,\n              56.3778\n            ],\n            [\n              -151.6917,\n              58.6444\n            ],\n            [\n              -155,\n              58.6444\n            ],\n            [\n              -155,\n              56.3778\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a633d","contributors":{"authors":[{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":220538,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kachadoorian, Reuben","contributorId":24336,"corporation":false,"usgs":true,"family":"Kachadoorian","given":"Reuben","email":"","affiliations":[],"preferred":false,"id":220539,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2447,"text":"wsp1683 - 1966 - Magnitude and frequency of floods in the United States: Part 9. Colorado River Basin","interactions":[],"lastModifiedDate":"2022-01-25T22:14:55.973665","indexId":"wsp1683","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1683","title":"Magnitude and frequency of floods in the United States: Part 9. Colorado River Basin","docAbstract":"<p>This report outlines methods by which the magnitude and frequency of expected floods of any recurrence interval from 1.1 to 50 years can be determined at most points in the Colorado River basin.</p><p>Composite frequency curves were drawn showing the relation of the mean annual flood to floods having recurrence intervals from 1.1 to 50 years. Other curves express the relation of the mean annual flood to basin characteristics. In the northern part of the basin (north of about lat 37° N.) both drainage area and mean altitude were important factors influencing the magnitude of the mean annual flood. Only drainage area was used as an independent variable in the southern part of the basin.</p><p>By combining data from the composite frequency curves and curves showing the relation of the mean annual flood to basin characteristics, flood-frequency curves can be drawn for streams in the report area not materially affected by regulation or diversion within the range and recurrence interval defined by base data.</p><p>Some of the larger streams in the basin do not lend themselves to regional analysis. These streams are given special treatment in this report. Owing to the paucity of streamflow data, flood-frequency relations are not defined in some of the more arid parts of the report area. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C","doi":"10.3133/wsp1683","usgsCitation":"Patterson, J.L., and Somers, W., 1966, Magnitude and frequency of floods in the United States: Part 9. Colorado River Basin: U.S. Geological Survey Water Supply Paper 1683, Report: xvii, 475 p.; Plate: 29.50 x 44.45 inches, https://doi.org/10.3133/wsp1683.","productDescription":"Report: xvii, 475 p.; Plate: 29.50 x 44.45 inches","numberOfPages":"491","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":394849,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24892.htm"},{"id":28521,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1683/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1683/report-thumb.jpg"},{"id":28520,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1683/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, California, Colorado, Nevada, Nevada, Utah, Wyoming","otherGeospatial":"Colorado River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115,\n              31.329\n            ],\n            [\n              -105.833,\n              31.329\n            ],\n            [\n              -105.833,\n              43.417\n            ],\n            [\n              -115,\n              43.417\n            ],\n            [\n              -115,\n              31.329\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495a4","contributors":{"authors":[{"text":"Patterson, James L.","contributorId":17593,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145219,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Somers, William P.","contributorId":47346,"corporation":false,"usgs":true,"family":"Somers","given":"William P.","affiliations":[],"preferred":false,"id":145220,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22776,"text":"ofr6619 - 1966 - Progress report on analog model construction, Orange County, California","interactions":[],"lastModifiedDate":"2013-05-22T15:03:30","indexId":"ofr6619","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-19","title":"Progress report on analog model construction, Orange County, California","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division,","doi":"10.3133/ofr6619","issn":"0094-9140","usgsCitation":"Cordes, E.H., Wall, J.R., and Moreland, J.A., 1966, Progress report on analog model construction, Orange County, California: U.S. Geological Survey Open-File Report 66-19, 49 p. ill., maps ;27 cm., https://doi.org/10.3133/ofr6619.","productDescription":"49 p. ill., maps ;27 cm.","costCenters":[],"links":[{"id":155915,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1966/0019/report-thumb.jpg"},{"id":272567,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0019/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65def1","contributors":{"authors":[{"text":"Cordes, E. H.","contributorId":49002,"corporation":false,"usgs":true,"family":"Cordes","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":188857,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wall, J. R.","contributorId":59863,"corporation":false,"usgs":true,"family":"Wall","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":188858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moreland, Joe A.","contributorId":48171,"corporation":false,"usgs":true,"family":"Moreland","given":"Joe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":188856,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":32793,"text":"pp352G - 1966 - Channel and hillslope processes in a semiarid area, New Mexico","interactions":[],"lastModifiedDate":"2017-03-27T16:52:06","indexId":"pp352G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"352","chapter":"G","title":"Channel and hillslope processes in a semiarid area, New Mexico","docAbstract":"<p>Ephemeral washes having drainage areas from a few acres to 5 square miles are shown by actual measurement to be accumulating sediment on the streambed. This aggradation is not apparent to the eye but is clearly shown in 7 years of annual remeasurement.</p><p>A similar aggradation was in progress in the same area some 3000 years ago as evidenced by an alluvial terrace later dissected by the present channel system. At that time as well as at present, aggradation occurred even in tributary areas draining a few acres. Colluvial accumulations merge with channel deposits and blanket the valleys and tributary basins even up to a few hundred feet of the drainage divides. </p><p>The present study concerned the amounts of sediment produced by different erosion processes in various physiographic positions in the drainage basins. Measurements show that by far the largest sediment source is sheet erosion operating on the small percentage of basin area near the basin divides. </p><p>Mass movement, gully head extension, and channel enlargement are presently small contributors of sediment compared with sheet erosion on unrilled slopes. As in previous studies, not all of the erosion products could be accounted for by accumulations on colluvial slopes and on beds of channels. The discrepancies are attributed primarily to sediment carried completely out of the basins studied and presumably deposited somewhere downstream.</p><p>Aggradation of alluvial valleys of 5 square miles area and smaller both in the present epicycle, and in prehistorical but post-glacial times in this locality, cannot be attributed to gullying or rill extension in the headwater tributaries but to sheet erosion of the most upstream margins of the basins.</p><p>Studies of rainfall characteristics of the 7 years of measurement compared with previous years in the 100-year record do not provide a clear-out difference which would account for the presently observed aggradation of channels. Longer period of measurement of erosion and sedimentation will be necessary to identify what precipitation parameters govern whether the channels aggrade or degrade. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Erosion and sedimentation in a semiarid environment (Professional Paper 352)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp352G","usgsCitation":"Leopold, L.B., Emmett, W.W., and Myrick, R.M., 1966, Channel and hillslope processes in a semiarid area, New Mexico: U.S. Geological Survey Professional Paper 352, iv, 57 p., https://doi.org/10.3133/pp352G.","productDescription":"iv, 57 p.","startPage":"193","endPage":"249","costCenters":[],"links":[{"id":119886,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0352g/report-thumb.jpg"},{"id":60773,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0352g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e648b","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":209184,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":209185,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Myrick, Robert M.","contributorId":24345,"corporation":false,"usgs":true,"family":"Myrick","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":209183,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38866,"text":"pp495B - 1966 - Paleozoic formations in the Wind River Basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp495B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"495","chapter":"B","title":"Paleozoic formations in the Wind River Basin, Wyoming","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology of the Wind River Basin, central Wyoming","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp495B","usgsCitation":"Keefer, W.R., and Van Lieu, J., 1966, Paleozoic formations in the Wind River Basin, Wyoming: U.S. Geological Survey Professional Paper 495, p. B1-B60, https://doi.org/10.3133/pp495B.","productDescription":"p. B1-B60","costCenters":[],"links":[{"id":104475,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4506.htm","linkFileType":{"id":5,"text":"html"},"description":"4506"},{"id":120289,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0495b/report-thumb.jpg"},{"id":65844,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0495b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65845,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0495b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65846,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0495b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65847,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0495b/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65848,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0495b/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65849,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0495b/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0495b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689f56","contributors":{"authors":[{"text":"Keefer, W. R.","contributorId":21538,"corporation":false,"usgs":true,"family":"Keefer","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":220576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Lieu, J. A.","contributorId":21203,"corporation":false,"usgs":true,"family":"Van Lieu","given":"J. A.","affiliations":[],"preferred":false,"id":220575,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32733,"text":"pp462I - 1966 - Summary of alluvial channel data from flume experiments, 1956-61","interactions":[],"lastModifiedDate":"2012-02-02T00:09:10","indexId":"pp462I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"462","chapter":"I","title":"Summary of alluvial channel data from flume experiments, 1956-61","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Sediment transport in alluvial channels, 1963-65","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp462I","usgsCitation":"Guy, H., Simons, D., and Richardson, E., 1966, Summary of alluvial channel data from flume experiments, 1956-61: U.S. Geological Survey Professional Paper 462, p. I1-I96, https://doi.org/10.3133/pp462I.","productDescription":"p. I1-I96","costCenters":[],"links":[{"id":119242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0462i/report-thumb.jpg"},{"id":60655,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0462i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699396","contributors":{"authors":[{"text":"Guy, H.P.","contributorId":73571,"corporation":false,"usgs":true,"family":"Guy","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":209055,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simons, D.B.","contributorId":50501,"corporation":false,"usgs":true,"family":"Simons","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":209054,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Richardson, E.V.","contributorId":105697,"corporation":false,"usgs":true,"family":"Richardson","given":"E.V.","email":"","affiliations":[],"preferred":false,"id":209056,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":52537,"text":"ofr6640 - 1966 - Principal facts for gravity stations in Safford and San Simon Valleys, Arizona","interactions":[{"subject":{"id":52537,"text":"ofr6640 - 1966 - Principal facts for gravity stations in Safford and San Simon Valleys, Arizona","indexId":"ofr6640","publicationYear":"1966","noYear":false,"title":"Principal facts for gravity stations in Safford and San Simon Valleys, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":70043129,"text":"70043129 - 1972 - Principal facts for gravity stations in Safford and San Simon Valleys, Arizona","indexId":"70043129","publicationYear":"1972","noYear":false,"title":"Principal facts for gravity stations in Safford and San Simon Valleys, Arizona"},"id":1}],"supersededBy":{"id":70043129,"text":"70043129 - 1972 - Principal facts for gravity stations in Safford and San Simon Valleys, Arizona","indexId":"70043129","publicationYear":"1972","noYear":false,"title":"Principal facts for gravity stations in Safford and San Simon Valleys, Arizona"},"lastModifiedDate":"2013-02-05T14:15:08","indexId":"ofr6640","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-40","title":"Principal facts for gravity stations in Safford and San Simon Valleys, Arizona","language":"ENGLISH","doi":"10.3133/ofr6640","usgsCitation":"Eaton, G.P., and Timmons, C., 1966, Principal facts for gravity stations in Safford and San Simon Valleys, Arizona: U.S. Geological Survey Open-File Report 66-40, 55 p., https://doi.org/10.3133/ofr6640.","productDescription":"55 p.","costCenters":[],"links":[{"id":173861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db667f5c","contributors":{"authors":[{"text":"Eaton, G. P.","contributorId":86334,"corporation":false,"usgs":true,"family":"Eaton","given":"G.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":245515,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Timmons, C.E.","contributorId":77586,"corporation":false,"usgs":true,"family":"Timmons","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":245514,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42921,"text":"ofr66129 - 1966 - Interim report on water for industrial development in south-central Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:10:27","indexId":"ofr66129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-129","title":"Interim report on water for industrial development in south-central Mississippi","language":"ENGLISH","doi":"10.3133/ofr66129","usgsCitation":"Taylor, R., Humphreys, C., and Shattles, D., 1966, Interim report on water for industrial development in south-central Mississippi: U.S. Geological Survey Open-File Report 66-129, 25 p., https://doi.org/10.3133/ofr66129.","productDescription":"25 p.","costCenters":[],"links":[{"id":173078,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0963","contributors":{"authors":[{"text":"Taylor, R.E.","contributorId":29836,"corporation":false,"usgs":true,"family":"Taylor","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":227410,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Humphreys, C.P. Jr.","contributorId":67956,"corporation":false,"usgs":true,"family":"Humphreys","given":"C.P.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":227411,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Shattles, D.E.","contributorId":23204,"corporation":false,"usgs":true,"family":"Shattles","given":"D.E.","affiliations":[],"preferred":false,"id":227409,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3666,"text":"cir531 - 1966 - The promise of precise borehole gravimetry in petroleum exploration and exploitation","interactions":[],"lastModifiedDate":"2017-08-27T17:57:39","indexId":"cir531","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"531","title":"The promise of precise borehole gravimetry in petroleum exploration and exploitation","docAbstract":"This report provides comprehensive information on the geology, geohydrology, and mineral resources of Boone and Winnebago Counties for use in resource-based land-use planning and development. Data on the composition, thickness, and regional distribution of glacial drift and bedrock materials were used to construct maps of: geologic materials to a depth of 20 ft; bedrock topography; drift thickness; major terrains; and glacial drift aquifers. Because contamination of aquifers is a serious concern in some areas of the two counties, a major focus of this study is on interpreting data critical to the selection of suitable areas for municipal waste disposal and prevention of contamination from existing municipal landfills and septic systems. Interpretive maps accompanying the text: (1) rate geological sequences on their capacity to protect aquifers and surface water from contamination by land burial of municipal wastes, septic system disposal, and surface spreading of wastes and agricultural chemicals; (2) geologic sequences on their suitability for general construction; and (3) delineate resources of sand, gravel, peat, and dolomite. Areas in which aquifer contamination from waste disposal and other land-use practices is most likely to occur are those in which sand and gravel and/or permeable creviced bedrock are at or near the surface. Areas having the lowest contamination potential are underlain by thick (20 ft or more) deposits of fine-grained glacial till. Areas most favorable for general construction are well-drained locations in major river valleys and terrace outwash plains; areas least favorable for construction are scattered throughout both counties on poorly drained land having low bearing capacities and on uplands and slopes in northwestern Winnebago County where the drift is thin over the bedrock. Extensive deposits of sand and gravel occur in the major bedrock valleys. Dolomite deposits underlie all the uplands of Winnebago County and most of Boone County, but extraction costs are prohibitive where overburden is thick. High-grade dolomite with relatively thin overburden is found in eastern Winnebago County and southwestern Boone County. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir531","usgsCitation":"McCulloh, T.H., 1966, The promise of precise borehole gravimetry in petroleum exploration and exploitation: U.S. Geological Survey Circular 531, iii, 12 p. :illus. ;27 cm., https://doi.org/10.3133/cir531.","productDescription":"iii, 12 p. :illus. ;27 cm.","costCenters":[],"links":[{"id":123916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1966/0531/report-thumb.jpg"},{"id":30706,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1966/0531/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641ae6","contributors":{"authors":[{"text":"McCulloh, Thane Hubert","contributorId":101625,"corporation":false,"usgs":true,"family":"McCulloh","given":"Thane","email":"","middleInitial":"Hubert","affiliations":[],"preferred":false,"id":147367,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2425,"text":"wsp1815 - 1966 - Gunpowder Falls, Maryland : uses of a water resource today and tomorrow","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1815","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1815","title":"Gunpowder Falls, Maryland : uses of a water resource today and tomorrow","language":"ENGLISH","publisher":"U. S,. Govt. Print. Off.,","doi":"10.3133/wsp1815","usgsCitation":"O’Bryan, D., and McAvoy, R.L., 1966, Gunpowder Falls, Maryland : uses of a water resource today and tomorrow: U.S. Geological Survey Water Supply Paper 1815, v, 90 p. :illus., maps. ;24 cm., https://doi.org/10.3133/wsp1815.","productDescription":"v, 90 p. :illus., maps. ;24 cm.","costCenters":[],"links":[{"id":139047,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1815/report-thumb.jpg"},{"id":28444,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1815/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a1ba","contributors":{"authors":[{"text":"O’Bryan, Deric","contributorId":15179,"corporation":false,"usgs":true,"family":"O’Bryan","given":"Deric","email":"","affiliations":[],"preferred":false,"id":145178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McAvoy, Russell Lonnie","contributorId":17595,"corporation":false,"usgs":true,"family":"McAvoy","given":"Russell","email":"","middleInitial":"Lonnie","affiliations":[],"preferred":false,"id":145179,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22740,"text":"ofr6615 - 1966 - Prospects for obtaining a water supply in the Fall River entrance area of Rocky Mountain National Park, Colorado, November 9, 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:08:05","indexId":"ofr6615","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-15","title":"Prospects for obtaining a water supply in the Fall River entrance area of Rocky Mountain National Park, Colorado, November 9, 1964","language":"ENGLISH","publisher":"U.S. Dept. of the Interior Geological Survey, Water Resources Division,","doi":"10.3133/ofr6615","issn":"0094-9140","usgsCitation":"Coffin, D.L., and Jenkins, E.J., 1966, Prospects for obtaining a water supply in the Fall River entrance area of Rocky Mountain National Park, Colorado, November 9, 1964: U.S. Geological Survey Open-File Report 66-15, 21 leaves :ill., maps ;29 cm., https://doi.org/10.3133/ofr6615.","productDescription":"21 leaves :ill., maps ;29 cm.","costCenters":[],"links":[{"id":155652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a149","contributors":{"authors":[{"text":"Coffin, Donald L.","contributorId":90696,"corporation":false,"usgs":true,"family":"Coffin","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":188799,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jenkins, Edward J.","contributorId":39821,"corporation":false,"usgs":true,"family":"Jenkins","given":"Edward","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":188798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2348,"text":"wsp1819H - 1966 - Fluvial sediment and chemical quality of water in the Little Blue River basin, Nebraska and Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1819H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1819","chapter":"H","title":"Fluvial sediment and chemical quality of water in the Little Blue River basin, Nebraska and Kansas","docAbstract":"The Little Blue River drains about 3,37)0 square miles in south-central Nebraska and north-central Kansas. The uppermost bedrock in the basin is limestone and shale of Permian age and sandstone, shale, and limestone of Cretaceous age. Bedrock is exposed in many places in the lower one-third of the basin but elsewhere is buried beneath a thin to thick mantle of younger sediments, mostly of Quaternary age. These younger sediments are largely fluvial and eolian deposits but also include some glacial till. Consisting in large part of sand and gravel, the fluvial deposits are an important source of ground-water supplies throughout much of the upper two-thirds of the basin. Loess, an eolian deposit of clayey silt, is by far the most widespread surficial deposit. The climate is continental. Temperatures ranging from -38 ? F to 118 ? F have been recorded in the basin. Average annual precipitation as low as 10.31 and as high as 49.32 inches has been recorded. During most years in the period 1956-62, when nearly all the water-quality data were obtained, annual precipitation and annual runoff were greater than normal. Flow-duration data indicate, however, that the flow distribution for the period was near normal. The Little Blue River has the same suspended-sediment characteristics as nearly all unregulated streams in the Great Plains--a wide range in concentrations, low concentrations during low-flow periods, and high concentrations during almost all periods of significant overland runoff. The maximum instantaneous concentration normally occurs many hours before maximum water discharge during any given rise in stage; the maximum daily mean concentration during any given year normally occurs at a moderate stream stage, not during a major flood. \r\n\r\nSuspended-sediment data for Little Blue River near Deweese, Nebr., which receives drainage from the upstream third of the basin, approximately, show that during the 1!}57-61 water years concentrations of 100 ppm (parts per million) or less prevailed about 42 percent of the time and concentrations of 1,000 ppm or less prevailed about 85 percent of the time. Observed concentrations ranged from 2 to 21,000 ppm: daily mean concentrations ranged from 2 to 13,800 ppm.\r\n\r\nThe discharge-weighted suspended-sediment concentration was computed as about 2,800 ppm at Little Blue River near Deweese, about 3,300 ppm near Fairbury (Endicott), and about 3,000 ppm at Waterville. These stations receive drainage from about one-third, two-thirds, and nearly all the basin, respectively. Water-utilization problems resulting from high concentrations are not significant in the basin ; use of water from the Little Blue River is quantitatively negligible. Concentrations and, consequently, discharges of sediment are greater at a given water discharge on a rising stage than at the same discharge on the falling stage of the same runoff event. Also, a wide range in sediment discharge occurs at similar water discharges during different runoff events. Daily sediment discharges at Little Blue River near Deweese ranged from about 1,400 to 16,000 tons at daily mean water discharges of about 500 cfs (cubic feet per second) and from almost 7,500 to 28,000 tons at water discharges of about 1,000 cfs. \r\n\r\nThe estimated long-term sediment discharge at Little Blue River near Deweese is about 400,000 tons per year: near Fairbury, about 1,200,000 tons per year: and at Waterville, about 1.900,000 tons per year. The high sediment discharge from the downstream part of the basin is due to greater precipitation and runoff--not to higher concentrations of suspended sediment--in the downstream parts of the basin. \r\n\r\nNearly all the suspended sediment is silt and clay. The streambed material is mainly medium sand to gravel. The median particle size of bed material observed was about 0.73 mm near Deweese and about 0.77 mm near Fairbury. A few computations of total sediment discharge of Little Blue River near Deweese indicate that suspended-sedim","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1819H","usgsCitation":"Mundorff, J.C., and Waddell, K., 1966, Fluvial sediment and chemical quality of water in the Little Blue River basin, Nebraska and Kansas: U.S. Geological Survey Water Supply Paper 1819, v, 45 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1819H.","productDescription":"v, 45 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137766,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819h/report-thumb.jpg"},{"id":28270,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de61f","contributors":{"authors":[{"text":"Mundorff, J. C.","contributorId":63374,"corporation":false,"usgs":true,"family":"Mundorff","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145059,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waddell, K.M.","contributorId":59009,"corporation":false,"usgs":true,"family":"Waddell","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":145058,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":40714,"text":"ofr66152 - 1966 - Records of selected wells, springs, test holes, materials tests, and chemical analyses of water in the lower Merrimack River basin, New Hampshire","interactions":[],"lastModifiedDate":"2012-02-02T00:10:50","indexId":"ofr66152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"66-152","title":"Records of selected wells, springs, test holes, materials tests, and chemical analyses of water in the lower Merrimack River basin, New Hampshire","language":"ENGLISH","doi":"10.3133/ofr66152","usgsCitation":"Weigle, J., and Kranes, R., 1966, Records of selected wells, springs, test holes, materials tests, and chemical analyses of water in the lower Merrimack River basin, New Hampshire: U.S. Geological Survey Open-File Report 66-152, 44 p., https://doi.org/10.3133/ofr66152.","productDescription":"44 p.","costCenters":[],"links":[{"id":171204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63570d","contributors":{"authors":[{"text":"Weigle, J.M.","contributorId":20400,"corporation":false,"usgs":true,"family":"Weigle","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":223841,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kranes, Richard","contributorId":23811,"corporation":false,"usgs":true,"family":"Kranes","given":"Richard","email":"","affiliations":[],"preferred":false,"id":223842,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68604,"text":"ha209 - 1966 - Floods in Steger Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:12","indexId":"ha209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"209","title":"Floods in Steger Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha209","usgsCitation":"Allen, H., 1966, Floods in Steger Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 209, 1 col. map ;58 x 44 cm., on sheet 88 x 134 cm., https://doi.org/10.3133/ha209.","productDescription":"1 col. map ;58 x 44 cm., on sheet 88 x 134 cm.","costCenters":[],"links":[{"id":190204,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90265,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/209/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.75,41.3675 ], [ -87.75,41.5 ], [ -87.61749999999999,41.5 ], [ -87.61749999999999,41.3675 ], [ -87.75,41.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d91","contributors":{"authors":[{"text":"Allen, Howard E.","contributorId":17274,"corporation":false,"usgs":true,"family":"Allen","given":"Howard E.","affiliations":[],"preferred":false,"id":278558,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32628,"text":"pp543A - 1966 - Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska","interactions":[{"subject":{"id":32628,"text":"pp543A - 1966 - Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska","indexId":"pp543A","publicationYear":"1966","noYear":false,"chapter":"A","title":"Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska"},"predicate":"IS_PART_OF","object":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"id":1}],"isPartOf":{"id":70048225,"text":"pp543 - 1966 - The Alaska earthquake, March 27, 1964: regional effects","indexId":"pp543","publicationYear":"1966","noYear":false,"title":"The Alaska earthquake, March 27, 1964: regional effects"},"lastModifiedDate":"2022-06-28T19:38:48.241938","indexId":"pp543A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"543","chapter":"A","title":"Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska","docAbstract":"The March 27, 1964, earthquake dislodged slides from nine deltas in Kenai Lake, south-central Alaska. Sliding removed protruding parts of deltas-often the youngest parts-and steepened delta fronts, increasing the chances of further sliding. Fathograms show that debris from large slides spread widely over the lake floor, some reaching the toe of the opposite shore; at one place debris traveled 5,000 feet over the horizontal lake floor.\n\nSlides generated two kinds of local waves: a backfill and far-shore wave. Backfill waves were formed by water that rushed toward the delta to fill the void left by the sinking slide mass, overtopped the slide scrap, and came ashore over the delta. Some backfill waves had runup heights of 30 feet and ran inland more than 300 feet, uprooting and breaking off large trees. Far-shore waves hit the shore opposite the slides. They were formed by slide debris that crossed the lake floor and forced water ahead of it, which then ran up the opposite slope, burst above the lake surface, and struck the shore. One far-shore wave had a runup height of 72 feet.\n\nKenai Lake was tilted and seiched; a power spectrum analysis of a limnogram shows a wave having the period of the calculated uninodal seiche (36 minutes) and several shorter period waves. In constricted and shallow reaches, waves caused by seiching had 20- and 30-foot runup heights.\n\nDeep lateral spreading of sediments toward delta margins displaced deeply driven railroad-bridge piles, and set up stress fields in the surface sediments which resulted in the formation of many shear and some tension fractures on the surface of two deltas.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Regional effects (Professional Paper 543)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp543A","usgsCitation":"McCulloch, D.S., 1966, Slide-induced waves, seiching and ground fracturing caused by the earthquake of March 27, 1964 at Kenai Lake, Alaska: U.S. Geological Survey Professional Paper 543, Report: vi, 41 p.; 2 Plates: 49.5 x 17.5 inches and 20.9 x 16.87 inches, https://doi.org/10.3133/pp543A.","productDescription":"Report: vi, 41 p.; 2 Plates: 49.5 x 17.5 inches and 20.9 x 16.87 inches","numberOfPages":"49","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":402630,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4590.htm","linkFileType":{"id":5,"text":"html"}},{"id":277653,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0543a/index.html"},{"id":60502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0543a/pp543a_text.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60501,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0543a/pp543a_plate2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60500,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0543a/pp543a_plate1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0543a/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Kenai Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -149.835071,60.335719 ], [ -149.835071,60.494895 ], [ -149.346197,60.494895 ], [ -149.346197,60.335719 ], [ -149.835071,60.335719 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee60a","contributors":{"authors":[{"text":"McCulloch, David S. dmccullo@usgs.gov","contributorId":3100,"corporation":false,"usgs":true,"family":"McCulloch","given":"David","email":"dmccullo@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":208818,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63242,"text":"gq523 - 1966 - Geologic map of the Edmonton quadrangle, Metcalfe County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gq523","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"523","title":"Geologic map of the Edmonton quadrangle, Metcalfe County, Kentucky","language":"ENGLISH","doi":"10.3133/gq523","usgsCitation":"Cattermole, J.M., 1966, Geologic map of the Edmonton quadrangle, Metcalfe County, Kentucky: U.S. Geological Survey Geologic Quadrangle 523, 1 map :col. ;77 x 88 cm., https://doi.org/10.3133/gq523.","productDescription":"1 map :col. ;77 x 88 cm.","costCenters":[],"links":[{"id":103253,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1839.htm","linkFileType":{"id":5,"text":"html"},"description":"1839"},{"id":249356,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0523/report.pdf","size":"39","linkFileType":{"id":1,"text":"pdf"}},{"id":252672,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0523/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.61749999999999,36.8675 ], [ -85.61749999999999,37 ], [ -85.5,37 ], [ -85.5,36.8675 ], [ -85.61749999999999,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699ead","contributors":{"authors":[{"text":"Cattermole, John Mark","contributorId":88746,"corporation":false,"usgs":true,"family":"Cattermole","given":"John","email":"","middleInitial":"Mark","affiliations":[],"preferred":false,"id":268545,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2669,"text":"wsp1819J - 1966 - Special sediment investigations Mississippi River at St. Louis, Missouri, 1961-63","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1819J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1819","chapter":"J","title":"Special sediment investigations Mississippi River at St. Louis, Missouri, 1961-63","docAbstract":"Four sets of comprehensive hydraulic and sediment data were obtained during 1961-63 for the Mississippi River at St. Louis at ranges of mean velocity from 3.3 to 5.6 feet per second, of mean depth from 22 to 37 feet, of width from 1,570 to 1,670 feet, of mean water-surface slope from 0.000054 to 0.000109, and of suspended-sediment concentration from 314 to 928 parts per million. The suspended sediment consisted of 9-46 percent sand, 30-46 percent silt, and 20-56 percent clay. The median size of bed material was about 0.42 millimeter for three sets of measurements and about 0.18 millimeter for the other set. A dune bed form was present during all four data-collection periods. Data obtained on consecutive days indicate that the turbulence constant can be computed from either streamflow-measurement notes or from vertical-velocity profiles. Constants computed from streamflow-measurement notes averaged 0.34, and those from vertical-velocity profiles averaged 0.35. The coefficients of vertical distribution of concentration for selected size ranges of suspended sands (expressed as z1, the slope, of the line relating the logarithms of concentration and a depth parameter) plotted against corresponding fall velocities indicate that on the average, the z1's are proportional to about the 0.7 power of the fall velocity. The data also indicate that the relation of z1 to fall velocity may vary with the mean velocity of flow.","language":"ENGLISH","publisher":"U.S. Geological Survey ;","doi":"10.3133/wsp1819J","usgsCitation":"Scott, C.H., and Stephens, H.D., 1966, Special sediment investigations Mississippi River at St. Louis, Missouri, 1961-63: U.S. Geological Survey Water Supply Paper 1819, iii, 35 p. :ill., maps (1 fold. in pocket) ;24 cm., https://doi.org/10.3133/wsp1819J.","productDescription":"iii, 35 p. :ill., maps (1 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":138251,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1819j/report-thumb.jpg"},{"id":29017,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29018,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819j/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29019,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1819j/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29020,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1819j/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb82a","contributors":{"authors":[{"text":"Scott, Cloyd H.","contributorId":106871,"corporation":false,"usgs":true,"family":"Scott","given":"Cloyd","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145584,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, Howard D.","contributorId":47347,"corporation":false,"usgs":true,"family":"Stephens","given":"Howard","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":145583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16612,"text":"ofr69321 - 1966 - Geologic evaluation of radar imagery, Caliente and Temblor Ranges, southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr69321","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1966","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"69-321","title":"Geologic evaluation of radar imagery, Caliente and Temblor Ranges, southern California","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr69321","usgsCitation":"Wolfe, E.W., 1966, Geologic evaluation of radar imagery, Caliente and Temblor Ranges, southern California: U.S. Geological Survey Open-File Report 69-321, 9 p. :maps ;29 cm., https://doi.org/10.3133/ofr69321.","productDescription":"9 p. :maps ;29 cm.","costCenters":[],"links":[{"id":150421,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6204","contributors":{"authors":[{"text":"Wolfe, Edward W.","contributorId":79878,"corporation":false,"usgs":true,"family":"Wolfe","given":"Edward","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":173151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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