{"pageNumber":"5665","pageRowStart":"141600","pageSize":"25","recordCount":165635,"records":[{"id":68300,"text":"ha461 - 1972 - Hydrogeologic characteristics of the valley-fill aquifer in the Arkansas River Valley, Bent County, Colorado","interactions":[],"lastModifiedDate":"2018-09-25T10:22:27","indexId":"ha461","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"461","title":"Hydrogeologic characteristics of the valley-fill aquifer in the Arkansas River Valley, Bent County, Colorado","docAbstract":"<p>The investigation on which this report is based is a part of a comprehensive evaluation of the water resources of the Arkansas River valley undertaken by the U.S. Geological Survey in cooperation with the Colorado Water Conservation Board and the Southeastern Colorado Water Conservancy District. The study reach extends 150 miles from Pueblo to the Kansas State line. The water-resources investigation of the stream aquifer system in the Arkansas River valley, which began in 1963, is being made to provide information about the water resources for planning, management, and administration of the supply. </p><p>The objectives of the investigation are to define the effects of present water use, to determine the relation between ground and surface water, and to evaluate the effects of proposed changes in water law and management. The major steps in the study are: (1) Inventory the water resources, (2) describe the hydrogeologic character of the aquifer, (3) document and evaluate the effects of development, (4) construct and verify models to aid in the evaluation of the hydrology, and (5) develop models to test water-management plans and to optimize water use. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha461","collaboration":"Prepared in cooperation with the Colorado Water Conservation Board and the Southeastern Colorado Water Conservancy District","usgsCitation":"Hurr, R.T., and Moore, J.E., 1972, Hydrogeologic characteristics of the valley-fill aquifer in the Arkansas River Valley, Bent County, Colorado: U.S. Geological Survey Hydrologic Atlas 461, 4 Plates: 40 x 33 inches or smaller, https://doi.org/10.3133/ha461.","productDescription":"4 Plates: 40 x 33 inches or smaller","costCenters":[],"links":[{"id":186622,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89735,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/461/plate-3.pdf","text":"Plate 3","size":"315 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":89736,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/461/plate-4.pdf","text":"Plate 4","size":"266 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 4"},{"id":89733,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/461/plate-1.pdf","text":"Plate 1","size":"4.85 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":89734,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/461/plate-2.pdf","text":"Plate 2","size":"4.71 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"}],"scale":"62500","country":"United States","state":"Colorado","county":"Bent County","otherGeospatial":"Arkansas River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.38333333333334,38 ], [ -103.38333333333334,38.166666666666664 ], [ -102.75,38.166666666666664 ], [ -102.75,38 ], [ -103.38333333333334,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628c24","contributors":{"authors":[{"text":"Hurr, R. Theodore","contributorId":27023,"corporation":false,"usgs":true,"family":"Hurr","given":"R.","email":"","middleInitial":"Theodore","affiliations":[],"preferred":false,"id":277989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, John E.","contributorId":33688,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":277990,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56749,"text":"wdrWA712 - 1972 - Water resources data for Washington, water year 1971; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2022-12-27T17:59:24.489336","indexId":"wdrWA712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"WA-71-2","title":"Water resources data for Washington, water year 1971; Part 2, Water quality records","docAbstract":"<p>Water resources data for the 1971 water year for Washington include records of data for the chemical and physical characteristics of surface water. Data on the quality of surface water (chemical, temperature, and sediment) were collected from designated sampling sites at predetermined intervals such as once daily, weekly, monthly or less frequently. Records are given for sampling stations of which are continuous record stations and are partial-record stations. A few pertinent stations (not included above) in bordering States are also included. The records were collected by the Water Resources Division of the U.S. Geological Survey under the direction of L. B. Laird, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Washington.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrWA712","collaboration":"Prepared in cooperation with the State of Washington and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Washington, water year 1971; Part 2, Water quality records: U.S. Geological Survey Water Data Report WA-71-2, viii, 256 p., https://doi.org/10.3133/wdrWA712.","productDescription":"viii, 256 p.","costCenters":[],"links":[{"id":411074,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/wa-71-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":175192,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/wa-71-2/report-thumb.jpg"}],"country":"United 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,{"id":1349,"text":"wsp1798I - 1972 - Fluvial sediment in Hocking River subwatershed 1 (North Branch Hunters Run), Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1798I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1798","chapter":"I","title":"Fluvial sediment in Hocking River subwatershed 1 (North Branch Hunters Run), Ohio","docAbstract":"From May 1956 to May 1962, Hocking River subwatershed 1 of Upper Hocking River Pilot Watershed had an average annual sediment yield from its contributing area of 0.94 square mile of 1,195 tons per square mile. Annual suspended-sediment yield at the outlet, expressed in tons per acre-foot of outflow, decreased from 0.45 in the 1957 water year to 0.10 in the 1962 water year, reflecting a decrease in sediment yield from the 1.04-squaremile drainage area above detention structure 1. ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1798I","usgsCitation":"Flint, R., 1972, Fluvial sediment in Hocking River subwatershed 1 (North Branch Hunters Run), Ohio: U.S. Geological Survey Water Supply Paper 1798, iv, 23 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1798I.","productDescription":"iv, 23 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":137540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1798i/report-thumb.jpg"},{"id":26424,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1798i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aea7d","contributors":{"authors":[{"text":"Flint, R.F.","contributorId":39761,"corporation":false,"usgs":true,"family":"Flint","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":143607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41118,"text":"ofr72352 - 1972 - Preliminary bedrock geologic map of the Yaquina and Toledo quadrangles, Oregon","interactions":[{"subject":{"id":41118,"text":"ofr72352 - 1972 - Preliminary bedrock geologic map of the Yaquina and Toledo quadrangles, Oregon","indexId":"ofr72352","publicationYear":"1972","noYear":false,"title":"Preliminary bedrock geologic map of the Yaquina and Toledo quadrangles, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":67459,"text":"i867 - 1976 - Geologic map of the Yaquina and Toledo quadrangles, Lincoln County, Oregon","indexId":"i867","publicationYear":"1976","noYear":false,"title":"Geologic map of the Yaquina and Toledo quadrangles, Lincoln County, Oregon"},"id":1}],"supersededBy":{"id":67459,"text":"i867 - 1976 - Geologic map of the Yaquina and Toledo quadrangles, Lincoln County, Oregon","indexId":"i867","publicationYear":"1976","noYear":false,"title":"Geologic map of the Yaquina and Toledo quadrangles, Lincoln County, Oregon"},"lastModifiedDate":"2012-02-02T00:11:10","indexId":"ofr72352","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-352","title":"Preliminary bedrock geologic map of the Yaquina and Toledo quadrangles, Oregon","language":"ENGLISH","doi":"10.3133/ofr72352","usgsCitation":"Snavely, P.D., MacLeod, N.S., and Wagner, H.C., 1972, Preliminary bedrock geologic map of the Yaquina and Toledo quadrangles, Oregon: U.S. Geological Survey Open-File Report 72-352, 1 map, https://doi.org/10.3133/ofr72352.","productDescription":"1 map","costCenters":[],"links":[{"id":106539,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8712.htm","linkFileType":{"id":5,"text":"html"},"description":"8712"},{"id":175444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"48000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c6b2","contributors":{"authors":[{"text":"Snavely, P. D. Jr.","contributorId":22770,"corporation":false,"usgs":true,"family":"Snavely","given":"P.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":224530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacLeod, N. S.","contributorId":55816,"corporation":false,"usgs":true,"family":"MacLeod","given":"N.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":224531,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wagner, H. C.","contributorId":95033,"corporation":false,"usgs":true,"family":"Wagner","given":"H.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":224532,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68312,"text":"ha377 - 1972 - Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas","interactions":[{"subject":{"id":55906,"text":"ofr69127 - 1969 - Water resources of Clay, Greene, Craighead and Poinsett Counties, Arkansas","indexId":"ofr69127","publicationYear":"1969","noYear":false,"title":"Water resources of Clay, Greene, Craighead and Poinsett Counties, Arkansas"},"predicate":"SUPERSEDED_BY","object":{"id":68312,"text":"ha377 - 1972 - Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas","indexId":"ha377","publicationYear":"1972","noYear":false,"title":"Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas"},"id":1}],"lastModifiedDate":"2019-08-23T12:57:37","indexId":"ha377","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"377","title":"Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas","docAbstract":"<p>Water is available in Clay, Greene, Craighead, and Poinsett Counties from ground-water and surface-water sources. However, ground water is more accessible in many places than surface water. Ground water is available from the alluvium, which covers all the area except Crowleys Ridge, and is also available from other formations below the alluvium.</p><p>Surface water is available from the Black and Cache Rivers west of Crowleys Ridge, and from the St/ Francis and Little Rivers, and from many ditches and laterals east of the ridge. Continuous water supplies are not available from streams on Crowleys Ridge, but additional surface-water supplies could be made available from reservoirs storage on the ridge. Average annual streamflow ranges from 1.2 cfs per sq mi (Cubic feet per second per square mile) in the western part of the four counties to 1.4 cfs per sq mi in the eastern part. Average annual precipitation is about 48 inches.</p><p>Use of water in the area for agriculture greatly exceeds all other used combined, and progressively greater amounts of water are being used for irrigation. In 1965, 111.4 mgd (million gallons per day) was used for irrigation of other crops. An additional 16.9 mgd was used by industry, municipalities, and others. Of these amounts, 180.1 mgd was ground water and 19.7 mgd was surface water, or a total of 199.8 mgd. More than 80 manufacturing firms, many of which are closely allied to agriculture, use moderate amounts of water, mostly from municipal supplies.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha377","collaboration":"Prepared in cooperation with the Arkansas Geological Commission","usgsCitation":"Hines, M.S., Plebuch, R.O., and Lamonds, A.G., 1972, Water resources of Clay, Greene, Craighead, and Poinsett Counties, Arkansas: U.S. Geological Survey Hydrologic Atlas 377, 2 Plates: 44.00 x 38.50 inches and 45.00 x 38.00 inches, https://doi.org/10.3133/ha377.","productDescription":"2 Plates: 44.00 x 38.50 inches and 45.00 x 38.00 inches","costCenters":[],"links":[{"id":366867,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/377/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185693,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/377/plate-1-thumb.jpg"},{"id":89760,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/377/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arkansas","county":"Clay County, Craighead County, Greene County, Poinsett County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91,35.5 ], [ -91,36.5 ], [ -90.5,36.5 ], [ -90.5,35.5 ], [ -91,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f08aa","contributors":{"authors":[{"text":"Hines, Marion S.","contributorId":29388,"corporation":false,"usgs":true,"family":"Hines","given":"Marion","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":278012,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plebuch, Raymond O.","contributorId":15177,"corporation":false,"usgs":true,"family":"Plebuch","given":"Raymond","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":278011,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lamonds, A. G.","contributorId":8450,"corporation":false,"usgs":true,"family":"Lamonds","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278010,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":45995,"text":"ofr72340 - 1972 - Flood of June 1972: Allegheny River near Limestone, New York","interactions":[],"lastModifiedDate":"2014-05-21T10:30:25","indexId":"ofr72340","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-340","title":"Flood of June 1972: Allegheny River near Limestone, New York","docAbstract":"<p>In June 1972, tropical storm Agnes caused sever flooding in Pennsylvania and southern New York. The flood, on many major streams were the highest known since the river valleys were settled. Maximum discharges were as much as twice the discharge of a 50-year flood. In southern New York, large areas in Corning, Elmire, Wellsville, Salamanca, and in many smaller communities were inundated to depths of several feet. Levels of all of the Finger Lakes were higher than any previously recorded, and extensive flooding of lakeside properties resulted.</p>\n<br>\n<p>The extent of flooding shown on the map was delineated by the U.S. Geological Survey from earlier photography and limited field survey.</p>\n<br>\n<p>The investigation was conducted in cooperation with the State of New York and the U.S. Army Corps of Engineers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72340","usgsCitation":"Schultz, G., Hladio, S., and Sherwood, D.A., 1972, Flood of June 1972: Allegheny River near Limestone, New York: U.S. Geological Survey Open-File Report 72-340, 1 Plate: 7.26 x 9.64 inches, https://doi.org/10.3133/ofr72340.","productDescription":"1 Plate: 7.26 x 9.64 inches","costCenters":[],"links":[{"id":287454,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287453,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0340/plate-1.pdf"}],"scale":"24000","country":"United States","state":"New York","city":"Limestone","otherGeospatial":"Allegheny River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78.75,42.0 ], [ -78.75,42.125 ], [ -78.625,42.125 ], [ -78.625,42.0 ], [ -78.75,42.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ef1","contributors":{"authors":[{"text":"Schultz, G.K.","contributorId":65823,"corporation":false,"usgs":true,"family":"Schultz","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":232426,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hladio, S.","contributorId":99530,"corporation":false,"usgs":true,"family":"Hladio","given":"S.","affiliations":[],"preferred":false,"id":232428,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sherwood, D. A.","contributorId":65824,"corporation":false,"usgs":true,"family":"Sherwood","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":232427,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":46045,"text":"ofr72426 - 1972 - Flood of June 1972: Chemung River at Big Flats, New York","interactions":[],"lastModifiedDate":"2018-03-26T15:40:31","indexId":"ofr72426","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-426","title":"Flood of June 1972: Chemung River at Big Flats, New York","docAbstract":"<p>In June 1972, tropical storm Agnes caused sever flooding in Pennsylvania and southern New York. The flood, on many major streams were the highest known since the river valleys were settled. Maximum discharges were as much as twice the discharge of a 50-year flood. In southern New York, large areas in Corning, Elmire, Wellsville, Salamanca, and in many smaller communities were inundated to depths of several feet. Levels of all of the Finger Lakes were higher than any previously recorded, and extensive flooding of lakeside properties resulted.</p>\n<br>\n<p>The extent of flooding shown on the map was delineated by the U.S. Geological Survey from earlier photography and limited field survey.</p>\n<br>\n<p>The investigation was conducted in cooperation with the State of New York and the U.S. Army Corps of Engineers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72426","usgsCitation":"Wagner, L., and Hamecher, P., 1972, Flood of June 1972: Chemung River at Big Flats, New York: U.S. Geological Survey Open-File Report 72-426, 1 Plate: 7.04 x 9.59 inches, https://doi.org/10.3133/ofr72426.","productDescription":"1 Plate: 7.04 x 9.59 inches","costCenters":[],"links":[{"id":287471,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0426/plate-1.pdf"},{"id":287472,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"New York","city":"Big Flats","otherGeospatial":"Chemung River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.0,42.125 ], [ -77.0,42.25 ], [ -76.875,42.25 ], [ -76.875,42.125 ], [ -77.0,42.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687e3f","contributors":{"authors":[{"text":"Wagner, L.A.","contributorId":12427,"corporation":false,"usgs":true,"family":"Wagner","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":232517,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamecher, P.H.","contributorId":57425,"corporation":false,"usgs":true,"family":"Hamecher","given":"P.H.","affiliations":[],"preferred":false,"id":232518,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46052,"text":"ofr72433 - 1972 - Flood of June 1972: Cohocton River at Campbell, New York","interactions":[],"lastModifiedDate":"2014-05-21T13:23:25","indexId":"ofr72433","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-433","title":"Flood of June 1972: Cohocton River at Campbell, New York","docAbstract":"<p>In June 1972, tropical storm Agnes caused sever flooding in Pennsylvania and southern New York. The flood, on many major streams were the highest known since the river valleys were settled. Maximum discharges were as much as twice the discharge of a 50-year flood. In southern New York, large areas in Corning, Elmire, Wellsville, Salamanca, and in many smaller communities were inundated to depths of several feet. Levels of all of the Finger Lakes were higher than any previously recorded, and extensive flooding of lakeside properties resulted.</p>\n<br>\n<p>The extent of flooding shown on the map was delineated by the U.S. Geological Survey from earlier photography and limited field survey.</p>\n<br>\n<p>The investigation was conducted in cooperation with the State of New York and the U.S. Army Corps of Engineers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72433","usgsCitation":"Wagner, L., and Hamecher, P., 1972, Flood of June 1972: Cohocton River at Campbell, New York: U.S. Geological Survey Open-File Report 72-433, 1 Plate: 7.07 x 9.92 inches, https://doi.org/10.3133/ofr72433.","productDescription":"1 Plate: 7.07 x 9.92 inches","costCenters":[],"links":[{"id":287489,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287488,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0433/plate-1.pdf"}],"scale":"24000","country":"United States","state":"New York","city":"Campbell","otherGeospatial":"Cohocton River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.25,42.125 ], [ -77.25,42.25 ], [ -77.125,42.25 ], [ -77.125,42.125 ], [ -77.25,42.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6416","contributors":{"authors":[{"text":"Wagner, L.A.","contributorId":12427,"corporation":false,"usgs":true,"family":"Wagner","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":232531,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hamecher, P.H.","contributorId":57425,"corporation":false,"usgs":true,"family":"Hamecher","given":"P.H.","affiliations":[],"preferred":false,"id":232532,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":950,"text":"wsp1939C - 1972 - Electrical-analog analysis of the hydrologic system, Tucson basin, southeastern Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1939C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1939","chapter":"C","title":"Electrical-analog analysis of the hydrologic system, Tucson basin, southeastern Arizona","docAbstract":"The water supply for the Tucson basin, Arizona, is derived entirely from ground water. The average annual pumpage for 1962-64 was about 165,000 acre-feet and was greater than the natural rate of ground-water recharge. Water-level declines of as much as 70 feet occurred from spring 1940 to spring 1965 as a result of the overdraft. \r\n\r\nAn electrical-analog model of the hydrologic system was constructed to provide a tool for determining the possible future effects of ground-water management schemes. Basic data required for the simulation of the hydrologic system in the model included periodic water-level measurements, determinations of transmissibility, and pumpage and recharge values. The model was analyzed using steady-state and storage-depletion techniques. The steady state analysis served to determine the average annual recharge to the hydrologic system and to verify the pattern of transmissibility. The steady-state analysis indicated that 97,000 acre-feet of water was entering and leaving the ground-water reservoir annually prior to extensive development. The storage-depletion analysis for 1940-64 was made to verify that the model was a valid analog of the hydrologic system and, therefore, could be used for the prediction of future water-level conditions. The storage-depletion analysis indicated areas where some of the basic-data values and (or) the conceptual design of the hydrologic system used in the model were in error. After all the hydrologic variables simulated in the model had been adjusted, the analog model reasonably simulated the historical field data. Based on the assumption that pumpage and recharge would continue at existing rates and locations, the model was then used to predict water-level conditions in spring 1985. The results of the projection indicate a maximum water-level decline of 140 feet for 1940-84. The predicted overall shapes of the cones of depression will remain about the same as in the historical period, except that a large amount of lateral development will take place in all the cones.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1939C","usgsCitation":"Anderson, T.W., 1972, Electrical-analog analysis of the hydrologic system, Tucson basin, southeastern Arizona: U.S. Geological Survey Water Supply Paper 1939, 1 portfolio (iv, p. illus.) ;24 cm., https://doi.org/10.3133/wsp1939C.","productDescription":"1 portfolio (iv, p. illus.) ;24 cm.","costCenters":[],"links":[{"id":110053,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25165.htm","linkFileType":{"id":5,"text":"html"},"description":"25165"},{"id":138058,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1939c/report-thumb.jpg"},{"id":25455,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1939c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25456,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1939c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25457,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1939c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25458,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1939c/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25459,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1939c/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25460,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1939c/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25461,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1939c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db606096","contributors":{"authors":[{"text":"Anderson, T. W.","contributorId":105686,"corporation":false,"usgs":true,"family":"Anderson","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":142906,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60938,"text":"mf449 - 1972 - Geologic map of the Mountain Top mercury deposit, southwestern Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:34","indexId":"mf449","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"449","title":"Geologic map of the Mountain Top mercury deposit, southwestern Alaska","language":"ENGLISH","doi":"10.3133/mf449","usgsCitation":"Sorg, D.H., and Estlund, M., 1972, Geologic map of the Mountain Top mercury deposit, southwestern Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 449, 1 map., https://doi.org/10.3133/mf449.","productDescription":"1 map.","costCenters":[],"links":[{"id":104108,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2878.htm","linkFileType":{"id":5,"text":"html"},"description":"2878"},{"id":179861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -159,61 ], [ -159,62 ], [ -156,62 ], [ -156,61 ], [ -159,61 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6965ad","contributors":{"authors":[{"text":"Sorg, D. H.","contributorId":63380,"corporation":false,"usgs":true,"family":"Sorg","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":264653,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Estlund, M.B.","contributorId":38575,"corporation":false,"usgs":true,"family":"Estlund","given":"M.B.","email":"","affiliations":[],"preferred":false,"id":264652,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62458,"text":"gq1000 - 1972 - Geologic map of the Upton quadrangle, central Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gq1000","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1000","title":"Geologic map of the Upton quadrangle, central Kentucky","language":"ENGLISH","doi":"10.3133/gq1000","usgsCitation":"Moore, F.R., 1972, Geologic map of the Upton quadrangle, central Kentucky: U.S. Geological Survey Geologic Quadrangle 1000, 1 map., https://doi.org/10.3133/gq1000.","productDescription":"1 map.","costCenters":[],"links":[{"id":103236,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1822.htm","linkFileType":{"id":5,"text":"html"},"description":"1822"},{"id":248624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1000/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":253851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1000/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86,37.3675 ], [ -86,37.5 ], [ -85.86749999999999,37.5 ], [ -85.86749999999999,37.3675 ], [ -86,37.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a238","contributors":{"authors":[{"text":"Moore, Frank R.","contributorId":54582,"corporation":false,"usgs":false,"family":"Moore","given":"Frank","email":"","middleInitial":"R.","affiliations":[{"id":12981,"text":"Department of Biological Sciences, University of Southern Mississippi","active":true,"usgs":false}],"preferred":false,"id":267402,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62589,"text":"gq993 - 1972 - Geologic map of the Whitmore quadrangle, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq993","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"993","title":"Geologic map of the Whitmore quadrangle, California","language":"ENGLISH","doi":"10.3133/gq993","usgsCitation":"Macdonald, G.A., and Lydon, P.A., 1972, Geologic map of the Whitmore quadrangle, California: U.S. Geological Survey Geologic Quadrangle 993, 1 map., https://doi.org/10.3133/gq993.","productDescription":"1 map.","costCenters":[],"links":[{"id":102003,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_378.htm","linkFileType":{"id":5,"text":"html"},"description":"378"},{"id":248749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0993/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":254059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0993/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122,40.5 ], [ -122,40.75 ], [ -121.75,40.75 ], [ -121.75,40.5 ], [ -122,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ef6","contributors":{"authors":[{"text":"Macdonald, Gordon Andrew","contributorId":25939,"corporation":false,"usgs":true,"family":"Macdonald","given":"Gordon","email":"","middleInitial":"Andrew","affiliations":[],"preferred":false,"id":267585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lydon, Philip A.","contributorId":12112,"corporation":false,"usgs":true,"family":"Lydon","given":"Philip","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":267584,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62976,"text":"gq1040 - 1972 - Geologic map of the Morgantown quadrangle, Butler and Warren Counties, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:44","indexId":"gq1040","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1040","title":"Geologic map of the Morgantown quadrangle, Butler and Warren Counties, Kentucky","language":"ENGLISH","doi":"10.3133/gq1040","usgsCitation":"Gildersleeve, B., 1972, Geologic map of the Morgantown quadrangle, Butler and Warren Counties, Kentucky: U.S. Geological Survey Geologic Quadrangle 1040, 1 map., https://doi.org/10.3133/gq1040.","productDescription":"1 map.","costCenters":[],"links":[{"id":107484,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10585.htm","linkFileType":{"id":5,"text":"html"},"description":"10585"},{"id":249114,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1040/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":252115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1040/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.75,37.1175 ], [ -86.75,37.25 ], [ -86.61749999999999,37.25 ], [ -86.61749999999999,37.1175 ], [ -86.75,37.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6967b0","contributors":{"authors":[{"text":"Gildersleeve, Benjamin","contributorId":14468,"corporation":false,"usgs":true,"family":"Gildersleeve","given":"Benjamin","email":"","affiliations":[],"preferred":false,"id":268125,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61378,"text":"mf359 - 1972 - Geologic map of the Carter Creek iron deposit, secs. 3, 9, and 10, T.8 S., R.7 W., Madison and Beaverhead Counties, Montana","interactions":[{"subject":{"id":40658,"text":"ofr6175 - 1961 - Carter Creek iron deposit, Madison and Beaverhead Counties, Montana","indexId":"ofr6175","publicationYear":"1961","noYear":false,"title":"Carter Creek iron deposit, Madison and Beaverhead Counties, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":61378,"text":"mf359 - 1972 - Geologic map of the Carter Creek iron deposit, secs. 3, 9, and 10, T.8 S., R.7 W., Madison and Beaverhead Counties, Montana","indexId":"mf359","publicationYear":"1972","noYear":false,"title":"Geologic map of the Carter Creek iron deposit, secs. 3, 9, and 10, T.8 S., R.7 W., Madison and Beaverhead Counties, Montana"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:42","indexId":"mf359","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"359","title":"Geologic map of the Carter Creek iron deposit, secs. 3, 9, and 10, T.8 S., R.7 W., Madison and Beaverhead Counties, Montana","language":"ENGLISH","doi":"10.3133/mf359","isbn":"0607797665","usgsCitation":"James, H.L., and Wier, K.L., 1972, Geologic map of the Carter Creek iron deposit, secs. 3, 9, and 10, T.8 S., R.7 W., Madison and Beaverhead Counties, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 359, 1 map., https://doi.org/10.3133/mf359.","productDescription":"1 map.","costCenters":[],"links":[{"id":104096,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2779.htm","linkFileType":{"id":5,"text":"html"},"description":"2779"},{"id":179723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"1","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.4675,45.13444444444444 ], [ -112.4675,45.166666666666664 ], [ -112.43333333333334,45.166666666666664 ], [ -112.43333333333334,45.13444444444444 ], [ -112.4675,45.13444444444444 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d2d3","contributors":{"authors":[{"text":"James, H. L.","contributorId":96732,"corporation":false,"usgs":true,"family":"James","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wier, K. L.","contributorId":106864,"corporation":false,"usgs":true,"family":"Wier","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265546,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62624,"text":"gq1037 - 1972 - Geologic map of the Falmouth quadrangle, Pendleton County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:12:49","indexId":"gq1037","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1037","title":"Geologic map of the Falmouth quadrangle, Pendleton County, Kentucky","language":"ENGLISH","doi":"10.3133/gq1037","usgsCitation":"Luft, S.J., 1972, Geologic map of the Falmouth quadrangle, Pendleton County, Kentucky: U.S. Geological Survey Geologic Quadrangle 1037, 1 map :col. ;58 x 45 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1037.","productDescription":"1 map :col. ;58 x 45 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107481,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10582.htm","linkFileType":{"id":5,"text":"html"},"description":"10582"},{"id":248783,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1037/report.pdf","size":"38","linkFileType":{"id":1,"text":"pdf"}},{"id":254176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1037/report-thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6991dd","contributors":{"authors":[{"text":"Luft, Stanley J.","contributorId":30634,"corporation":false,"usgs":true,"family":"Luft","given":"Stanley","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":267629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42865,"text":"ofr72354 - 1972 - Preliminary geologic map of the White Butte East Quadrangle, Hettinger County, North Dakota","interactions":[{"subject":{"id":42865,"text":"ofr72354 - 1972 - Preliminary geologic map of the White Butte East Quadrangle, Hettinger County, North Dakota","indexId":"ofr72354","publicationYear":"1972","noYear":false,"title":"Preliminary geologic map of the White Butte East Quadrangle, Hettinger County, North Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":69144,"text":"coal70 - 1975 - Geologic map and coal resources of the White Butte East quadrangle, Hettinger County, North Dakota","indexId":"coal70","publicationYear":"1975","noYear":false,"title":"Geologic map and coal resources of the White Butte East quadrangle, Hettinger County, North Dakota"},"id":1}],"supersededBy":{"id":69144,"text":"coal70 - 1975 - Geologic map and coal resources of the White Butte East quadrangle, Hettinger County, North Dakota","indexId":"coal70","publicationYear":"1975","noYear":false,"title":"Geologic map and coal resources of the White Butte East quadrangle, Hettinger County, North Dakota"},"lastModifiedDate":"2012-02-02T00:10:29","indexId":"ofr72354","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-354","title":"Preliminary geologic map of the White Butte East Quadrangle, Hettinger County, North Dakota","language":"ENGLISH","doi":"10.3133/ofr72354","usgsCitation":"Soward, K., 1972, Preliminary geologic map of the White Butte East Quadrangle, Hettinger County, North Dakota: U.S. Geological Survey Open-File Report 72-354, 1 map, https://doi.org/10.3133/ofr72354.","productDescription":"1 map","costCenters":[],"links":[{"id":173188,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679d4a","contributors":{"authors":[{"text":"Soward, K.S.","contributorId":20721,"corporation":false,"usgs":true,"family":"Soward","given":"K.S.","affiliations":[],"preferred":false,"id":227293,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56486,"text":"wdrCO711 - 1972 - Water resources data for Colorado, water year 1971; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2012-02-02T00:11:59","indexId":"wdrCO711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"CO-71-1","title":"Water resources data for Colorado, water year 1971; Part 1, Surface water records","language":"ENGLISH","doi":"10.3133/wdrCO711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Colorado, water year 1971; Part 1, Surface water records: U.S. Geological Survey Water Data Report CO-71-1, 425 p., https://doi.org/10.3133/wdrCO711.","productDescription":"425 p.","costCenters":[],"links":[{"id":181115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/co-71-1/report-thumb.jpg"},{"id":88133,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/co-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f75c7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532667,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16672,"text":"ofr72454 - 1972 - Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards","interactions":[],"lastModifiedDate":"2024-03-27T17:56:09.862376","indexId":"ofr72454","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-454","title":"Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards","docAbstract":"<p>A program to study the engineering geology of most of the larger Alaska coastal communities and to evaluate their earthquake and other geologic hazards was started promptly after the 1964 Alaska earthquake; this report is a product of that program. Field-study methods were largely reconnaissance, and thus the interpretations in the report are subject to revision as further information becomes available. The report provides broad guidelines for planners and engineers when considering geologic factors during preparation of land-use plans. The use of this information should lead to minimizing future loss of life and property, especially during major earthquakes.</p><p>Skagway was established in 1897 as a seaport near the head of Taiya Inlet fiord in the northern part of southeastern Alaska. Rugged mountains, steep-walled valleys, fiords, and numerous glaciers and icefields characterize the landscape of the area. Valley floors are narrow and most carry large streams, which end in tidewater deltas. Skagway is situated on the delta and lower valley floor of the Skagway River.</p><p>Glaciers became vastly enlarged during the Pleistocene Epoch and presumably covered the area at least several times. The last major deglaciation probably occurred about 10,000 years ago. Subsequently, there was minor expansion and then partial retreat of glaciers; land rebound because of glacial melting is still going on today.</p><p>Bedrock is composed predominantly of plutonic intrusive rocks, chiefly quartz diorite and granodiorite, some metamorphic rocks and a few dikes are present. Most bedrock is of Jurassic and Cretaceous age.</p><p>An assortment of surficial deposits of Quaternary age form the valley bottoms and locally part of the valley walls. Thick deposits of sand and gravel have accumulated as deltas at the heads of fiords and as alluvium in the main stream valleys; deposits may be as much as S8S feet thick at Skagway. Locally, thin deposits mantle some of the steep bedrock slopes and also form some moderately to gently sloping ground. Manmade fill covers much of the top of the delta and floor of the Skagway valley. The fill is composed chiefly of gravel and sand. Quarried blocks of granodiorite are used as riprap to face river dikes and on fill areas exposed to waves of Taiya Inlet.</p><p>The geologic structure of the area is imperfectly known. However, it appears that plutonic rocks intruded metamorphic rocks in Jurassic and Cretaceous time. Extensive faulting is strongly indicated by the strikingly linear or curvilinear pattern of fiords and many large and small valleys, but no major faults have been positively identified because of concealment by water or surficial deposits. Inferred faults include those coincident with the lower Skagway valley, Taiya Inlet-Taiya valley, and the Katzehin River delta-Upper Dewey Lake. Principal fault movements probably occurred in middle Tertiary time but some movement might have been in late Tertiary or possibly early Quaternary time. Local faults appear to join the Chilkat River fault, a segment of the important Denali fault system, one of the major tectonic elements of southeastern Alaska. One fault segment of this system shows evidence of movement within the last several hundred years. Southeastern Alaska's other major fault system is the active Fairweather-Queen Charlotte Islands fault system'near the coast of the Pacific Ocean. This fault system passes to within about 100 miles of Skagway. At its northwest end the fault system merges with the Chugach-St. Elias fault.</p><p>One hundred twenty-two earthquakes, some of them strong, have been felt or possibly felt at Skagway during the years 1898 through 1969. The closest large earthquake (magnitude about 8) causing some damage at Skagway occurred July 10, 1958. Its epicenter was about 100 miles to the southwest. Other earthquakes, as much as 150 miles away, also have caused slight to moderate damage. The closest instrumentally recorded earthquake (magnitude 6) had its epicenter about 30 miles to the west of Skagway.</p><p>Most earthquakes in southeastern Alaska have occurred southwest, west, or northwest of Skagway, near the coast of the Pacific Ocean. They appear to be related to movement along the Fairweather-Queen Charlotte Islands fault system or the Chugach-St. Elias fault. Most have had their epicenters offshore. Some earthquakes may be related to movement at depth along the Denali fault system.</p><p>The probability of destructive earthquakes at Skagway is unknown because the tectonics of the region have not been studied in detail. However, on the basis of the seismic record and limited tectonic evidence, we suggest that sometime in the future an earthquake of at least magnitude 6 probably will occur very close to the city, a magnitude 7 earthquake might occur in the general area, and an earthquake of magnitude 8 probably will occur at some distance to the southwest, west, or northwest.</p><p>Effects from nearby large earthquakes could cause extensive damage at Skagway. Nine principal effects are considered.</p><p>1. Surface&nbsp;displacement. Displacement of ground caused by fault movement would affect only structures built athwart the fault. However, a sudden tectonic uplift of land of as much as a few feet might affect a wide area and necessitate extensive dredging and wharf rebuilding. On the other hand, a subsidence of several feet would allow tidewater to reach inland and flood part of the harbor facilities and the business district.</p><p>2. Ground shaking. Because intensity of ground shaking during earthquakes largely depends on type and water content of the geologic material being shaken, the geologic materials are separated into three categories. Those considered susceptible to strongest shaking are grouped into category 1 (containing materials that are saturated, loose, and of medium- to fine-grain sizes); those of intermediate susceptibility in category 2; and those least susceptible to shaking in category 3.</p><p>3. Compaction of some medium-grained sediments during strong earthquake shaking could cause local settling of alluvial and deltaic surfaces. Also, some manmade fills near the harbor might undergo marked differential settling.</p><p>4. Liquefaction of saturated beds of uniform, fine sand commonly occurs during strong earthquakes. Few such beds, however, are positively identified at Skagway; some may occur within deltaic and alluvial deposits. If present, these beds might liquefy and cause local settling or trigger landslides.</p><p>5. Ejection of water-sediment mixtures from earthquake-induced fractures or from point sources, plus some associated ground subsidence, is common during major earthquakes where saturated sand and fine gravel deposits are confined beneath generally impermeable beds. Some alluvial and deltaic deposits at Skagway probably are susceptible to these processes. Locally, ejecta might cover roads and areas between buildings and fill low-lying areas. Associated ground fracturing might damage roadways, foundations of buildings, and other facilities.</p><p>6. Subaerial and subaqueous slides occur frequently during earthquakes. Saturated loose sediments on steep slopes are especially susceptible to sliding. During a major earthquake, surficial deposits forming such slopes along the southeast side of the Skagway valley probably would be subject to sliding or earthflowing on an extensive scale. Some sliding might extend onto the valley floor and damage or destroy buildings and part of the railroad. Rockfalls would be numerous and locally very large rockslides might occur.</p><p>Subaqueous sliding of the Skagway delta is potentially the most damaging of earthquake effects. Sliding may have occurred there during the earthquake of September 16, 1899; any future major earthquake close to the city would cause extensive sliding, possibly triggered in part by liquefaction. If shaking continued for several minutes, successive slides might progressively remove large portions of the delta and allow extensive land spreading and fracturing of Skagway River alluvium as much as several thousand feet landward from the shoreline.</p><p>7. Glacier surfaces commonly receive extensive snow avalanches and rockslides during seismic shaking. In the Skagway area, glaciers may be disrupted at their margins, and resulting blocked streams might form lakes in a few places. If these lakes drained suddenly, downstream areas would he flooded. No long-term effects, such as glacier expansion, are expected.</p><p>8. Ground- and surface-water levels often are affected during and after strong earthquake shaking. At Skagway, ground-water levels probably would be lowered, but there would be no permanent change in water quality. Earthquake-triggered landslides could dam the Skagway River; the sudden failure of the dams might cause severe flooding.</p><p>9. Waves generated by earthquakes include tsunamis, seiche waves, and waves caused by subaerial and submarine sliding and tectonic displacement of land. Damage in the Skagway area would depend on wave height, tidal stage, and warning time. Some waves triggered by subaerial and subaqueous slides have a strong possibility of reaching heights of as much as 60 feet--or possibly even higher. Tsunamis from the open ocean must travel 160 miles of fiords before reaching Skagway, which allows sufficient time for appraisal of expectable wave height and, if necessary, evacuation of the harbor area and other low-lying ground.</p><p>Geologic hazards other than those hazards associated with earthquakes include nonearthquake-induced subaerial and subaqueous slides, floods, and slow uplift (rebound) of land. Landslides of moderate size are known to have occurred from time to time during heavy rains such as those of September 1967. Subaqueous slides happen intermittently during the normal growth of deltas. Submarine cables on the floor of northern Taiya Inlet presumably were broken by such slides on September 10, 1927. Flooding by the Skagway River has inundated parts of the city many times, usually during heavy rains in the fall. Two floods were reported to have been caused by the sudden draining of glacier-dammed lakes. Dikes protect the city from many smaller floods, but heightening and broadening is needed to give full protection. Slow land uplift at Skagway, because of regional glacioisostatic rebound, averages 0.059 foot per year. On this basis, the shoreline theoretically shifted seaward 500 feet and the harbor shoaled 4.4 feet between 1897 and 1972.</p><p>It is recommended that future geologic study of the Skagway area include: detailed geologic mapping and collection of data on geologic materials, joints, faults, and slope stability; complete evaluation of earthquake probability and response of materials to shaking; and collection and evaluation of periodic soundings and sediment data from Skagway and Taiya deltas to assist in forecasting the stability of the delta front.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72454","usgsCitation":"Yehle, L.A., and Lemke, R.W., 1972, Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open-File Report 72-454, Report: iv, 108 p.; 4 Plates: 35.77 x 18.67 inches or smaller, https://doi.org/10.3133/ofr72454.","productDescription":"Report: iv, 108 p.; 4 Plates: 35.77 x 18.67 inches or smaller","costCenters":[],"links":[{"id":427161,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427160,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427159,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427158,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427153,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0454/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150379,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0454/report-thumb.jpg"}],"scale":"9600","country":"United States","state":"Alaska","city":"Skagway","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -135.3463249696411,\n              59.48810534833572\n            ],\n            [\n              -135.3463249696411,\n              59.40680330286153\n            ],\n            [\n              -135.22164285027563,\n              59.40680330286153\n            ],\n            [\n              -135.22164285027563,\n              59.48810534833572\n            ],\n            [\n              -135.3463249696411,\n              59.48810534833572\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6443d4","contributors":{"authors":[{"text":"Yehle, Lynn A. yehle@usgs.gov","contributorId":3794,"corporation":false,"usgs":true,"family":"Yehle","given":"Lynn","email":"yehle@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":173260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lemke, Richard Walter","contributorId":105280,"corporation":false,"usgs":true,"family":"Lemke","given":"Richard","email":"","middleInitial":"Walter","affiliations":[],"preferred":false,"id":173261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42925,"text":"ofr72242 - 1972 - Preliminary geologic map of the Loma Prieta-Mount Madonna area, Santa Clara and Santa Cruz counties, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:27","indexId":"ofr72242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-242","title":"Preliminary geologic map of the Loma Prieta-Mount Madonna area, Santa Clara and Santa Cruz counties, California","language":"ENGLISH","doi":"10.3133/ofr72242","usgsCitation":"McLaughlin, R.J., Simoni, T., Osbun, E., and Bauer, P., 1972, Preliminary geologic map of the Loma Prieta-Mount Madonna area, Santa Clara and Santa Cruz counties, California: U.S. Geological Survey Open-File Report 72-242, 1 map, https://doi.org/10.3133/ofr72242.","productDescription":"1 map","costCenters":[],"links":[{"id":173082,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":99011,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0242/plate-1.pdf","size":"13100","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67b141","contributors":{"authors":[{"text":"McLaughlin, R. J. 0000-0002-4390-2288","orcid":"https://orcid.org/0000-0002-4390-2288","contributorId":107271,"corporation":false,"usgs":true,"family":"McLaughlin","given":"R.","middleInitial":"J.","affiliations":[],"preferred":false,"id":227420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Simoni, T.R. Jr.","contributorId":34581,"corporation":false,"usgs":true,"family":"Simoni","given":"T.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":227418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Osbun, E.D.","contributorId":10091,"corporation":false,"usgs":true,"family":"Osbun","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":227417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bauer, P.G.","contributorId":50956,"corporation":false,"usgs":true,"family":"Bauer","given":"P.G.","email":"","affiliations":[],"preferred":false,"id":227419,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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,{"id":62393,"text":"gq1008 - 1972 - Geologic map of the Capilla Peak quadrangle, Torrance and Valencia Counties, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq1008","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1008","title":"Geologic map of the Capilla Peak quadrangle, Torrance and Valencia Counties, New Mexico","language":"ENGLISH","doi":"10.3133/gq1008","usgsCitation":"Myers, D.A., and McKay, E.J., 1972, Geologic map of the Capilla Peak quadrangle, Torrance and Valencia Counties, New Mexico: U.S. Geological Survey Geologic Quadrangle 1008, 1 map., https://doi.org/10.3133/gq1008.","productDescription":"1 map.","costCenters":[],"links":[{"id":107455,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10556.htm","linkFileType":{"id":5,"text":"html"},"description":"10556"},{"id":248568,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1008/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":253712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1008/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.5,34.6175 ], [ -106.5,34.75 ], [ -106.36749999999999,34.75 ], [ -106.36749999999999,34.6175 ], [ -106.5,34.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d358","contributors":{"authors":[{"text":"Myers, Donald A.","contributorId":100906,"corporation":false,"usgs":true,"family":"Myers","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":267324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKay, E. J.","contributorId":57040,"corporation":false,"usgs":true,"family":"McKay","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":267323,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63164,"text":"gq1012 - 1972 - Geologic map of the White Mountain Peak quadrangle, Mono County, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:43","indexId":"gq1012","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1012","title":"Geologic map of the White Mountain Peak quadrangle, Mono County, California","language":"ENGLISH","doi":"10.3133/gq1012","usgsCitation":"Crowder, D., and Sheridan, M.F., 1972, Geologic map of the White Mountain Peak quadrangle, Mono County, California: U.S. Geological Survey Geologic Quadrangle 1012, 1 map., https://doi.org/10.3133/gq1012.","productDescription":"1 map.","costCenters":[],"links":[{"id":101837,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_85.htm","linkFileType":{"id":5,"text":"html"},"description":"85"},{"id":179900,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.5,37.5 ], [ -118.5,37.75 ], [ -118.25,37.75 ], [ -118.25,37.5 ], [ -118.5,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689f61","contributors":{"authors":[{"text":"Crowder, D. F.","contributorId":57045,"corporation":false,"usgs":true,"family":"Crowder","given":"D. F.","affiliations":[],"preferred":false,"id":268431,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sheridan, Michael F.","contributorId":59413,"corporation":false,"usgs":true,"family":"Sheridan","given":"Michael","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":268432,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42866,"text":"ofr72355 - 1972 - Preliminary geologic map of the White Butte NE Quadrangle, Stark and Hettinger counties, North Dakota","interactions":[{"subject":{"id":42866,"text":"ofr72355 - 1972 - Preliminary geologic map of the White Butte NE Quadrangle, Stark and Hettinger counties, North Dakota","indexId":"ofr72355","publicationYear":"1972","noYear":false,"title":"Preliminary geologic map of the White Butte NE Quadrangle, Stark and Hettinger counties, North Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":69145,"text":"coal72 - 1975 - Geologic map and coal resources of the White Butte NE quadrangle, Stark and Hettinger Counties, North Dakota","indexId":"coal72","publicationYear":"1975","noYear":false,"title":"Geologic map and coal resources of the White Butte NE quadrangle, Stark and Hettinger Counties, North Dakota"},"id":1}],"supersededBy":{"id":69145,"text":"coal72 - 1975 - Geologic map and coal resources of the White Butte NE quadrangle, Stark and Hettinger Counties, North Dakota","indexId":"coal72","publicationYear":"1975","noYear":false,"title":"Geologic map and coal resources of the White Butte NE quadrangle, Stark and Hettinger Counties, North Dakota"},"lastModifiedDate":"2022-06-17T19:14:29.750909","indexId":"ofr72355","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-355","title":"Preliminary geologic map of the White Butte NE Quadrangle, Stark and Hettinger counties, North Dakota","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72355","usgsCitation":"Soward, K.S., 1972, Preliminary geologic map of the White Butte NE Quadrangle, Stark and Hettinger counties, North Dakota: U.S. Geological Survey Open-File Report 72-355, 1 Plate: 45.70 x 27.50 inches, https://doi.org/10.3133/ofr72355.","productDescription":"1 Plate: 45.70 x 27.50 inches","costCenters":[],"links":[{"id":173189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0355/report-thumb.jpg"},{"id":402353,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0355/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"North Dakota","county":"Hettinger County, Stark County","otherGeospatial":"White Butte NE Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.375,\n              46.625\n            ],\n            [\n              -102.25,\n              46.625\n            ],\n            [\n              -102.25,\n              46.75\n            ],\n            [\n              -102.375,\n              46.75\n            ],\n            [\n              -102.375,\n              46.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679d8c","contributors":{"authors":[{"text":"Soward, Kenneth S.","contributorId":39351,"corporation":false,"usgs":true,"family":"Soward","given":"Kenneth","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":227294,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63024,"text":"gq1004 - 1972 - Geologic map of the Ruedi quadrangle, Pitkin and Eagle Counties, Colorado","interactions":[],"lastModifiedDate":"2012-02-10T00:10:46","indexId":"gq1004","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1004","title":"Geologic map of the Ruedi quadrangle, Pitkin and Eagle Counties, Colorado","language":"ENGLISH","doi":"10.3133/gq1004","usgsCitation":"Freeman, V.L., 1972, Geologic map of the Ruedi quadrangle, Pitkin and Eagle Counties, Colorado: U.S. Geological Survey Geologic Quadrangle 1004, 1 map :col. ;58 x 45 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq1004.","productDescription":"1 map :col. ;58 x 45 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":107451,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_10552.htm","linkFileType":{"id":5,"text":"html"},"description":"10552"},{"id":249157,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/1004/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":252158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/1004/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.86749999999999,39.25 ], [ -106.86749999999999,39.3675 ], [ -106.75,39.3675 ], [ -106.75,39.25 ], [ -106.86749999999999,39.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68c090","contributors":{"authors":[{"text":"Freeman, Val L.","contributorId":40570,"corporation":false,"usgs":true,"family":"Freeman","given":"Val","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":268213,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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