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,{"id":47930,"text":"ofr71114 - 1970 - Crest-stage gaging stations in Oregon, a compilation of peak data collected from October 1952 to September 1970","interactions":[{"subject":{"id":47930,"text":"ofr71114 - 1970 - Crest-stage gaging stations in Oregon, a compilation of peak data collected from October 1952 to September 1970","indexId":"ofr71114","publicationYear":"1970","noYear":false,"title":"Crest-stage gaging stations in Oregon, a compilation of peak data collected from October 1952 to September 1970"},"predicate":"SUPERSEDED_BY","object":{"id":70047759,"text":"70047759 - 1974 - Crest-stage gaging stations in Oregon: a compilation of peak data collected from October 1952 to September 1974","indexId":"70047759","publicationYear":"1974","noYear":false,"title":"Crest-stage gaging stations in Oregon: a compilation of peak data collected from October 1952 to September 1974"},"id":1}],"supersededBy":{"id":70047759,"text":"70047759 - 1974 - Crest-stage gaging stations in Oregon: a compilation of peak data collected from October 1952 to September 1974","indexId":"70047759","publicationYear":"1974","noYear":false,"title":"Crest-stage gaging stations in Oregon: a compilation of peak data collected from October 1952 to September 1974"},"lastModifiedDate":"2013-08-20T10:58:43","indexId":"ofr71114","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"71-114","title":"Crest-stage gaging stations in Oregon, a compilation of peak data collected from October 1952 to September 1970","language":"ENGLISH","doi":"10.3133/ofr71114","usgsCitation":"Friday, J., 1970, Crest-stage gaging stations in Oregon, a compilation of peak data collected from October 1952 to September 1970: U.S. Geological Survey Open-File Report 71-114, 71 p. : map ; 27 cm., https://doi.org/10.3133/ofr71114.","productDescription":"71 p. : map ; 27 cm.","costCenters":[],"links":[{"id":162565,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6836a5","contributors":{"authors":[{"text":"Friday, John","contributorId":19160,"corporation":false,"usgs":true,"family":"Friday","given":"John","email":"","affiliations":[],"preferred":false,"id":236540,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56033,"text":"ofr70224 - 1970 - Supplement to the report \"A graphical summary of dissolved-oxygen data for the Delaware River estuary for water years 1965-69\"","interactions":[],"lastModifiedDate":"2012-02-02T00:11:47","indexId":"ofr70224","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-224","title":"Supplement to the report \"A graphical summary of dissolved-oxygen data for the Delaware River estuary for water years 1965-69\"","language":"ENGLISH","doi":"10.3133/ofr70224","usgsCitation":"Merk, C., 1970, Supplement to the report \"A graphical summary of dissolved-oxygen data for the Delaware River estuary for water years 1965-69\": U.S. Geological Survey Open-File Report 70-224, 3 p., 5 figs., https://doi.org/10.3133/ofr70224.","productDescription":"3 p., 5 figs.","costCenters":[],"links":[{"id":174724,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6985e1","contributors":{"authors":[{"text":"Merk, C.F.","contributorId":67517,"corporation":false,"usgs":true,"family":"Merk","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":254671,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55963,"text":"ofr7015 - 1970 - Basic data on the quantity of low flow in Barton Creek, Texas, July 6-8 and October 1-3, 1970","interactions":[],"lastModifiedDate":"2017-06-14T14:49:37","indexId":"ofr7015","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-15","title":"Basic data on the quantity of low flow in Barton Creek, Texas, July 6-8 and October 1-3, 1970","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7015","usgsCitation":"Baker, E.T., and Watson, J., 1970, Basic data on the quantity of low flow in Barton Creek, Texas, July 6-8 and October 1-3, 1970: U.S. Geological Survey Open-File Report 70-15, 12 p., https://doi.org/10.3133/ofr7015.","productDescription":"12 p.","costCenters":[],"links":[{"id":185346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641b86","contributors":{"authors":[{"text":"Baker, E. T. Jr.","contributorId":88366,"corporation":false,"usgs":true,"family":"Baker","given":"E.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":254565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Watson, J.A.","contributorId":98809,"corporation":false,"usgs":true,"family":"Watson","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":254566,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56028,"text":"ofr70212 - 1970 - Hydrogeologic data for the lower Arkansas River valley, Colorado","interactions":[{"subject":{"id":56028,"text":"ofr70212 - 1970 - Hydrogeologic data for the lower Arkansas River valley, Colorado","indexId":"ofr70212","publicationYear":"1970","noYear":false,"title":"Hydrogeologic data for the lower Arkansas River valley, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70047894,"text":"70047894 - 1970 - Hydrogeologic data for the Lower Arkansas River Valley, Colorado","indexId":"70047894","publicationYear":"1970","noYear":false,"title":"Hydrogeologic data for the Lower Arkansas River Valley, Colorado"},"id":1}],"supersededBy":{"id":70047894,"text":"70047894 - 1970 - Hydrogeologic data for the Lower Arkansas River Valley, Colorado","indexId":"70047894","publicationYear":"1970","noYear":false,"title":"Hydrogeologic data for the Lower Arkansas River Valley, Colorado"},"lastModifiedDate":"2013-08-29T10:43:18","indexId":"ofr70212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-212","title":"Hydrogeologic data for the lower Arkansas River valley, Colorado","language":"ENGLISH","doi":"10.3133/ofr70212","usgsCitation":"Major, T.J., Hurr, R., and Moore, J., 1970, Hydrogeologic data for the lower Arkansas River valley, Colorado: U.S. Geological Survey Open-File Report 70-212, 125 p., 5 figs., https://doi.org/10.3133/ofr70212.","productDescription":"125 p., 5 figs.","costCenters":[],"links":[{"id":181175,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db628a3b","contributors":{"authors":[{"text":"Major, T. J.","contributorId":18762,"corporation":false,"usgs":true,"family":"Major","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":254660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hurr, R. T.","contributorId":20713,"corporation":false,"usgs":true,"family":"Hurr","given":"R. T.","affiliations":[],"preferred":false,"id":254661,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, J.E.","contributorId":34927,"corporation":false,"usgs":true,"family":"Moore","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":254662,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56000,"text":"ofr70136 - 1970 - Summary of ground-water hydrological data in Michigan in 1969","interactions":[],"lastModifiedDate":"2017-07-12T10:30:30","indexId":"ofr70136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-136","title":"Summary of ground-water hydrological data in Michigan in 1969","docAbstract":"<p>The purpose of this report is to make available the records of ground-water levels in the principal aquifers of the State through 1969 and to compile other related data, such as records of groundwater pumpage, data on municipal, public and industrial water-supply facilities, and the effects of precipitation on ground-water levels. Records of water levels in areas of heavy pumpage, and in areas where changes are principally from natural influences, are illustrated or tabulated to allow comparison between these types of water-level fluctuations. The water levels and related data provide a day-to-day record for the evaluation of available ground-water supplies. The long-term records serve as a framework to which short-term records may be related.</p><p>This report is written for those persons, municipalities, industries, institutions, consultants, drillers, and hydrologists interested in the ground-water resources of the State.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70136","usgsCitation":"Giroux, P., and Huffman, G., 1970, Summary of ground-water hydrological data in Michigan in 1969: U.S. Geological Survey Open-File Report 70-136, vii, 101 p., https://doi.org/10.3133/ofr70136.","productDescription":"vii, 101 p.","numberOfPages":"113","costCenters":[{"id":382,"text":"Michigan Water Science 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,{"id":14020,"text":"ofr70155 - 1970 - Qualitative analysis of airborne magnetometer data: The Arabian Shield, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2026-01-06T15:42:16.443199","indexId":"ofr70155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-155","title":"Qualitative analysis of airborne magnetometer data: The Arabian Shield, Kingdom of Saudi Arabia","docAbstract":"<p>A qualitative analysis and interpretation of magnetic data obtained from airborne magnetometer and scintillometer surveys of the Precambrian Arabian Shield, Kingdom of Saudi Arabia, show that some rock units and geologic features exhibit characteristic magnetic expressions and anomalies. Circular to elliptical anomalies are attributed to younger intrusive or less commonly older masses, stocks, and plugs of granitic rocks. The linear anomalies may be expressions of faults, lineation trends, or dike swarms. Reconnaissance exploration for evidence of mineralization are recommended in the vicinity of some of these anomalies.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70155","usgsCitation":"Hase, D.H., 1970, Qualitative analysis of airborne magnetometer data: The Arabian Shield, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 70-155, Report: 44 p.; 1 Plate: 23.51 x 30.84 inches, https://doi.org/10.3133/ofr70155.","productDescription":"Report: 44 p.; 1 Plate: 23.51 x 30.84 inches","costCenters":[],"links":[{"id":498353,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0155/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":498352,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0155/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147206,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0155/report-thumb.jpg"}],"scale":"2000000","country":"Saudi Arabia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.1569003387927,\n              42.19240723701009\n            ],\n            [\n              -120.10749572008328,\n              38.838079005221346\n            ],\n            [\n              -114.92237135508793,\n              34.88069804889223\n            ],\n            [\n              -114.98297993586107,\n              31.350750228533002\n            ],\n            [\n              -108.86155573128843,\n              31.164630024551755\n            ],\n            [\n              -108.78553410798668,\n              37.13467902221349\n            ],\n            [\n              -113.85445865369462,\n              37.17625160026044\n            ],\n            [\n              -113.88260270021135,\n              42.186786176024185\n            ],\n            [\n              -120.1569003387927,\n              42.19240723701009\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              42.32738784712694,\n              15.512723400556823\n            ],\n            [\n              55.46938659113218,\n              19.579159163878117\n            ],\n            [\n              56.089387644546775,\n              21.93229208405711\n            ],\n            [\n              48.656849713663576,\n              28.702737353396188\n            ],\n            [\n              39.424873163889,\n              32.90306864705684\n            ],\n            [\n              33.20660131965218,\n              29.600711506057223\n            ],\n            [\n              42.32738784712694,\n              15.512723400556823\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","publicComments":"(IR)SA 110","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db65531d","contributors":{"authors":[{"text":"Hase, Donald H.","contributorId":15633,"corporation":false,"usgs":true,"family":"Hase","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":168803,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68096,"text":"ha371 - 1970 - Flood of March 1968 on the Sudbury, Assabet, and Concord Rivers, Massachusetts","interactions":[],"lastModifiedDate":"2021-12-17T20:52:07.682141","indexId":"ha371","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"371","title":"Flood of March 1968 on the Sudbury, Assabet, and Concord Rivers, Massachusetts","docAbstract":"<p><span>During a 3-day period from March 17 to 19, 1968, a total of 3 to 7 inches of rain fell on parts of eastern Massachusetts. This heavy rainfall, combined with the generally wet antecedent conditions of the spring season and some runoff from snowmelt, caused considerable flooding of the rivers in the area. Property damage in Massachusetts from the flood was reported by the New England Division, Corps of Engineers (1968) to be $28 million. Most of the damage occurred where construction, both industrial and domestic, had encroached upon the flood plains of the rivers.</span></p>\n<p><span>The Sudbury and Assabet Rivers join at Concord, Mass., to form the Concord River (see fig. 1). This three-river system, which is known locally as the &ldquo;SuAs-Co&rsquo;&rsquo; basin, drains an area of about 405 square miles.</span></p>\n<p><span>The purpose of this report, which is one of a series covering the major flooded rivers in eastern Massachusetts, is to show flood stages and areas inundated by the March 1968 flood, to compare the severity of this flood with past floods, and to show the frequency of floods of given magnitudes which may be expected in the future at gaging stations in the basins. These basic flood data, as compiled, will serve as a broad, sound basis to assist state and local planners in such measures as flood-plain zoning and flood containment and prevention.</span></p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha371","usgsCitation":"Petersen, R.G., Wood, G.K., and Gadoury, R.A., 1970, Flood of March 1968 on the Sudbury, Assabet, and Concord Rivers, Massachusetts: U.S. Geological Survey Hydrologic Atlas 371, 2 Plates: 47.00 x 40.50 inches, https://doi.org/10.3133/ha371.","productDescription":"2 Plates: 47.00 x 40.50 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":186307,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393058,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15750.htm"},{"id":91808,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/371/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91807,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/371/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"12000","country":"United States","state":"Massachusetts","otherGeospatial":"Assabet River, Concord River, Sudbury River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.631,\n              42.25\n            ],\n            [\n              -71.25,\n              42.25\n            ],\n            [\n              -71.25,\n              42.648\n            ],\n            [\n              -71.631,\n              42.648\n            ],\n            [\n              -71.631,\n              42.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eed14","contributors":{"authors":[{"text":"Petersen, Richard G.","contributorId":44232,"corporation":false,"usgs":true,"family":"Petersen","given":"Richard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, G. K.","contributorId":44235,"corporation":false,"usgs":true,"family":"Wood","given":"G.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":277637,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gadoury, Russell A.","contributorId":99542,"corporation":false,"usgs":true,"family":"Gadoury","given":"Russell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277638,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56055,"text":"ofr70303 - 1970 - A proposed streamflow-data program for Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:11:50","indexId":"ofr70303","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-303","title":"A proposed streamflow-data program for Illinois","language":"ENGLISH","doi":"10.3133/ofr70303","usgsCitation":"Sieber, C., 1970, A proposed streamflow-data program for Illinois: U.S. Geological Survey Open-File Report 70-303, 79 p., 8 figs., https://doi.org/10.3133/ofr70303.","productDescription":"79 p., 8 figs.","costCenters":[],"links":[{"id":174180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a69","contributors":{"authors":[{"text":"Sieber, C.R.","contributorId":95953,"corporation":false,"usgs":true,"family":"Sieber","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":254700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16772,"text":"ofr7071 - 1970 - Analyses of rock and stream-sediment samples from the Sumdum A-3 Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2024-02-16T20:32:55.944715","indexId":"ofr7071","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-71","title":"Analyses of rock and stream-sediment samples from the Sumdum A-3 Quadrangle, Alaska","docAbstract":"<p>Analytical data for 138 rock and 71 stream-sediment samples from the Sumdum A-3, 1:63,360 scale quadrangle are presented in this report, together with a statistical treatment of the data. The samples were collected in 1969 as part of the Heavy Metals Program of the U.S. Geological Survey.</p><p>The most comprehensive discussion of the geology of the study area is a report by A. F. Buddington and Theodore Chapin (1929). Known metalliferous lodes of the area are described and additional references to specific areas are given by Berg and Cobb (1967). Additional data is given in reports by Herbert and Race (1964) and Alaska Department of Mines (1950). Supplemental publications are being prepared on the general geology and mineral occurrences of the study area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7071","usgsCitation":"Clark, A.L., Brew, D.A., Grybeck, D.A., and Wehr, R., 1970, Analyses of rock and stream-sediment samples from the Sumdum A-3 Quadrangle, Alaska: U.S. Geological Survey Open-File Report 70-71, Report: 98 p.; 1 Plate: 19.22 x 25.97 inches, https://doi.org/10.3133/ofr7071.","productDescription":"Report: 98 p.; 1 Plate: 19.22 x 25.97 inches","costCenters":[],"links":[{"id":425759,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0071/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":425758,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149588,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0071/report-thumb.jpg"}],"scale":"63360","country":"United States","state":"Alaska","otherGeospatial":"Sumdum A-3 Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -133.1280067073484,\n              57.29310072436553\n            ],\n            [\n              -133.1280067073484,\n              56.78002256064593\n            ],\n            [\n              -132.1742424106991,\n              56.78002256064593\n            ],\n            [\n              -132.1742424106991,\n              57.29310072436553\n            ],\n            [\n              -133.1280067073484,\n              57.29310072436553\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6837ac","contributors":{"authors":[{"text":"Clark, Allen L.","contributorId":96258,"corporation":false,"usgs":true,"family":"Clark","given":"Allen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":173524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brew, David A. dbrew@usgs.gov","contributorId":3244,"corporation":false,"usgs":true,"family":"Brew","given":"David","email":"dbrew@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":173523,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grybeck, Donald A.","contributorId":73213,"corporation":false,"usgs":true,"family":"Grybeck","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":173522,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wehr, Raymond","contributorId":13241,"corporation":false,"usgs":true,"family":"Wehr","given":"Raymond","email":"","affiliations":[],"preferred":false,"id":173521,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":55972,"text":"ofr7049 - 1970 - Annual water-resources review, White Sands Missile Range, 1969--a basic data report","interactions":[],"lastModifiedDate":"2012-02-02T00:12:09","indexId":"ofr7049","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-49","title":"Annual water-resources review, White Sands Missile Range, 1969--a basic data report","language":"ENGLISH","doi":"10.3133/ofr7049","usgsCitation":"Busch, F., 1970, Annual water-resources review, White Sands Missile Range, 1969--a basic data report: U.S. Geological Survey Open-File Report 70-49, 41 p., 9 figs., https://doi.org/10.3133/ofr7049.","productDescription":"41 p., 9 figs.","costCenters":[],"links":[{"id":100422,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0049/report.pdf","size":"1523","linkFileType":{"id":1,"text":"pdf"}},{"id":181087,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0049/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b792","contributors":{"authors":[{"text":"Busch, F.E.","contributorId":41079,"corporation":false,"usgs":true,"family":"Busch","given":"F.E.","email":"","affiliations":[],"preferred":false,"id":254578,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":18204,"text":"ofr7034 - 1970 - Interim report on worldwide historic surface faulting","interactions":[],"lastModifiedDate":"2020-06-08T13:47:37.618507","indexId":"ofr7034","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-34","title":"Interim report on worldwide historic surface faulting","docAbstract":"<p>This interim report presents data on and interrelations between the parameters L (length of surface rupture), D (maximum surface displacement), and M (Richter magnitude of associated earthquake) for the main traces of historic surface faults that have been reported in the worldwide literature. Original descriptions of the individual fault-events published in English, French, German, or Spanish were used whenever possible, supplemented by translations of selected passages of reports published in Japanese and Chinese. For some events, original descriptions were not published in these languages and secondary sources were used. Although more than 100 fault-events have been reported in the literature, only those for which reliable data (in the judgement of the present writers) were available on at least two of the three parameters M, L, and D are included in this interim report and listed in table 1. Some fault-events have been omitted because the available reports contained significantly different data for the same event and the writers had insufficient basis for choosing between them.</p><p>This report was prepared to permit early release of part of the results of a more comprehensive study of historic surface faulting now under way, and to elicit suggestions and criticisms from users of the report. Comments are especially invited regarding the methods used in designating the fault type and in identifying the main fault.</p><p>The more comprehensive report will deal with subsidiary faults as well as main faults, will have detailed citations of the sources of information, and will discuss various additional aspects of faulting. It is anticipated that reliable data on a few more faults will be obtained, and it is hoped that comments from users of this interim report will permit improvement of the comprehensive report. Thus it is expected that the comprehensive report will contain modifications of the present data and will be of larger scope. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7034","usgsCitation":"Bonilla, M.G., and Buchanan, J.M., 1970, Interim report on worldwide historic surface faulting (Version 1.1): U.S. Geological Survey Open-File Report 70-34, ii, 32 p., https://doi.org/10.3133/ofr7034.","productDescription":"ii, 32 p.","costCenters":[],"links":[{"id":47569,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0034/report.pdf","text":"Version 1.0","linkFileType":{"id":1,"text":"pdf"}},{"id":150858,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0034/report-thumb.jpg"},{"id":375406,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/of/1970/of1611/","linkFileType":{"id":5,"text":"html"}},{"id":375405,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/of1611/of1611.pdf","text":"Version 1.1","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Version 1.1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0921","contributors":{"authors":[{"text":"Bonilla, Manuel G.","contributorId":74384,"corporation":false,"usgs":true,"family":"Bonilla","given":"Manuel","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":178700,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buchanan, Jane M.","contributorId":32543,"corporation":false,"usgs":true,"family":"Buchanan","given":"Jane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":178699,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56009,"text":"ofr70161 - 1970 - Basic data report No. 1, for magnitude and frequency of floods on small streams in Tennessee","interactions":[{"subject":{"id":56009,"text":"ofr70161 - 1970 - Basic data report No. 1, for magnitude and frequency of floods on small streams in Tennessee","indexId":"ofr70161","publicationYear":"1970","noYear":false,"title":"Basic data report No. 1, for magnitude and frequency of floods on small streams in Tennessee"},"predicate":"SUPERSEDED_BY","object":{"id":70047570,"text":"70047570 - 1975 - Peak stages and discharges on small streams in Tennessee, 1965-1975","indexId":"70047570","publicationYear":"1975","noYear":false,"title":"Peak stages and discharges on small streams in Tennessee, 1965-1975"},"id":1}],"supersededBy":{"id":70047570,"text":"70047570 - 1975 - Peak stages and discharges on small streams in Tennessee, 1965-1975","indexId":"70047570","publicationYear":"1975","noYear":false,"title":"Peak stages and discharges on small streams in Tennessee, 1965-1975"},"lastModifiedDate":"2013-08-12T11:32:12","indexId":"ofr70161","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-161","title":"Basic data report No. 1, for magnitude and frequency of floods on small streams in Tennessee","language":"ENGLISH","doi":"10.3133/ofr70161","collaboration":"This report was also published as Basic Data Report 1 of the Tennessee Department of Transportation","usgsCitation":"Hickenlooper, I., 1970, Basic data report No. 1, for magnitude and frequency of floods on small streams in Tennessee: U.S. Geological Survey Open-File Report 70-161, 52 p., 1 fig., https://doi.org/10.3133/ofr70161.","productDescription":"52 p., 1 fig.","costCenters":[],"links":[{"id":181688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640c49","contributors":{"authors":[{"text":"Hickenlooper, I.J.","contributorId":10872,"corporation":false,"usgs":true,"family":"Hickenlooper","given":"I.J.","affiliations":[],"preferred":false,"id":254636,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56056,"text":"ofr70305 - 1970 - A proposed streamflow-data program for Missouri","interactions":[],"lastModifiedDate":"2012-02-02T00:11:50","indexId":"ofr70305","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-305","title":"A proposed streamflow-data program for Missouri","language":"ENGLISH","doi":"10.3133/ofr70305","usgsCitation":"Skelton, J., and Homyk, A., 1970, A proposed streamflow-data program for Missouri: U.S. Geological Survey Open-File Report 70-305, 100 p., 6 figs., https://doi.org/10.3133/ofr70305.","productDescription":"100 p., 6 figs.","costCenters":[],"links":[{"id":174256,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8a11","contributors":{"authors":[{"text":"Skelton, John","contributorId":70392,"corporation":false,"usgs":true,"family":"Skelton","given":"John","email":"","affiliations":[],"preferred":false,"id":254701,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Homyk, Anthony","contributorId":83592,"corporation":false,"usgs":true,"family":"Homyk","given":"Anthony","email":"","affiliations":[],"preferred":false,"id":254702,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32614,"text":"pp545D - 1970 - Effects of the earthquake of March 27, 1964, on the Alaska Railroad","interactions":[{"subject":{"id":32614,"text":"pp545D - 1970 - Effects of the earthquake of March 27, 1964, on the Alaska Railroad","indexId":"pp545D","publicationYear":"1970","noYear":false,"chapter":"D","title":"Effects of the earthquake of March 27, 1964, on the Alaska Railroad"},"predicate":"IS_PART_OF","object":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"id":1}],"isPartOf":{"id":70048241,"text":"pp545 - 1967 - The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities","indexId":"pp545","publicationYear":"1967","noYear":false,"title":"The Alaska earthquake, March 27, 1964: effects on transportation, communications, and utilities"},"lastModifiedDate":"2022-02-15T20:33:33.73754","indexId":"pp545D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"545","chapter":"D","title":"Effects of the earthquake of March 27, 1964, on the Alaska Railroad","docAbstract":"In the 1964 Alaska earthquake, the federally owned Alaska Railroad sustained damage of more than $35 million: 54 percent of the cost for port facilities; 25 percent, roadbed and track; 9 percent, buildings and utilities; 7 percent, bridges and culverts; and 5 percent, landslide removal. Principal causes of damage were: (1) landslides, landslide-generated waves, and seismic sea waves that destroyed costly port facilities built on deltas; (2) regional tectonic subsidence that necessitated raising and armoring 22 miles of roadbed made susceptible to marine erosion; and (3), of greatest importance in terms of potential damage in seismically active areas, a general loss of strength experienced by wet waterlaid unconsolidated granular sediments (silt to coarse gravel) that allowed embankments to settle and enabled sediments to undergo fiowlike displacement toward topographic depressions, even in fiat-lying areas. The term “landspreading” is proposed for the lateral displacement and distension of mobilized sediments; landspreading appears to have resulted largely from liquefaction. Because mobilization is time dependent and its effects cumulative, the long duration of strong ground motion (timed as 3 to 4 minutes) along the southern 150 miles of the rail line made landspreading an important cause of damage. Sediments moved toward natural and manmade topographic depressions (stream valleys, gullies, drainage ditches, borrow pits, and lakes). Stream widths decreased, often about 20 inches but at some places by as much as 6.5 feet, and sediments moved upward beneath stream channels. Landspreading toward streams and even small drainage ditches crushed concrete and metal culverts. Bridge superstructures were compressed and failed by lateral buckling, or more commonly were driven into, through, or over bulkheads. Piles and piers were torn free of superstructures by moving sediments, crowded toward stream channels, and lifted in the center. The lifted piles arched the superstructures. Vertical pile displacement was independent of the depth of the pile penetration in the sediment and thus was due to vertical movement of the sediments, rather than to differential compaction. The fact that bridge piles were carried laterally without notable tilting suggests that mobilization exceeded pile depths, which averaged about 20 feet. Field observations, largely duplicated by vibrated sandbox models of stream channels, suggest that movement was distributed throughout the sediments, rather than restricted to finite failure surfaces. Landspreading generated stress that produced cracks in the ground surface adjacent to depressions. The distribution of this stress controlled the crack patterns: tension cracks parallel to straight or concave streambanks, shear cracks intersecting at 45° to 70° on convex banks where there was some component of radial spreading, and orthogonal cracks on the insides of tight meander bends or islands where spreading was omnidirectional. Ground cracks of these kinds commonly extended 500 feet, and occasionally about 1,000 feet, back from streams, which indicates that landspreading occurred over large areas. In areas of landspreading, highway and railroad embankments, pavements, and rails were pulled apart endways and were displaced laterally if they lay at an angle to the direction of sediment displacement. Sediment movement commonly skewed bridges that crossed streams obliquely. The maximum horizontal skew was 10 feet. Embankment settlement, nearly universal in areas of landspreading, also occurred in areas where there was no evidence for widespread loss of strength in the unconsolidated sediments. In the latter areas embankments themselves clearly caused the loss of bearing strength in the underlying sediment. In both areas, settlement was accompanied by the formation of ground cracks approximately parallel to the embankment in the adjacent sediments. Sediment-laden ground water was discharged from the cracks, and extreme local settlements (as much as 6 ft) were associated with large discharges. Landspreading was accompanied by transient horizontal displacement of the ground that pounded bridge ends with slight or considerable force. The deck of a 105-foot bridge was repeatedly arched up off its piles by transient compression. Bridges may also have developed high horizontal accelerations. One bridge deck, driven through its bulkhead, appears to have had an acceleration of at least 1.1 to 1.7 g; however, most evidence for high accelerations is ambiguous. Limited standard penetration data show that landspreading damage was not restricted to soft sediments. Some bridges were severely damaged by displacement of piles driven in sediments classified as compact and dense. Total thickness of unconsolidated sediments strongly controlled the degree of damage. In areas underlain by wet water-laid sediments the degree of damage to uniformly designed and built wooden railroad bridges shows a closer correlation with total sediment thickness at the bridge site than with the grain size of the material in which the piles were driven. Local geology and physiography largely controlled the kind, distribution, and severity of damage to the railroad. This relationship is so clear that maps of surficial geology and physiography of damaged areas of the rail belt show that only a few geologic-physiographic units serve to identify these areas: 1. Bedrock and glacial till on bedrock. No foundation displacements, but ground vibration increased toward the area of maximum strain-energy release. 2. Glacial outwash terraces. Landspreading and damage ranged from none where the water table was low and the terrace undissected to severe where the water table was near the surface and the terrace dissected by streams. 3. Inactive flood plains. Landspreading, ground cracking, flooding by ejected ground water, and damage were generally slight but increased to severe toward lower, wetter active flood plains or river channels. 4. Active flood plains. Landspreading, ground cracking, and flooding were nearly universal and were greater than on adjacent inactive flood plains. 5. Fan deltas. Radial downhill spreading and ground cracking were considerable near the lower edges of the fan deltas and were accompanied by ground-water discharge. Landslides were common from edges of deltas. Damage, landspreading, ground crack-ing, vibration, and flooding by ground water generally increased with (1) increasing thickness of unconsolidated sediments, (2) decreasing depth to the water table, (3) proximity to topographic depressions, and (4) proximity to the area of maximum strain-energy release.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"The Alaska earthquake, March 27, 1964: Effects on transportation, communications, and utilities (Professional Paper 545)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp545D","usgsCitation":"McCulloch, D.S., and Bonilla, M.G., 1970, Effects of the earthquake of March 27, 1964, on the Alaska Railroad: U.S. Geological Survey Professional Paper 545, Report: viii, 161 p.; 4 Plates: 42.15 inches x 12.39 inches or smaller, https://doi.org/10.3133/pp545D.","productDescription":"Report: viii, 161 p.; 4 Plates: 42.15 inches x 12.39 inches or smaller","numberOfPages":"173","additionalOnlineFiles":"Y","costCenters":[{"id":380,"text":"Menlo ParkCalif. Office-Earthquake Science Center","active":false,"usgs":true}],"links":[{"id":396000,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_99039.htm"},{"id":277819,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0545d/pp545d_plate4.pdf"},{"id":277818,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0545d/pp545d_plate3.pdf"},{"id":277817,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0545d/pp545d_plate2.pdf"},{"id":277816,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0545d/pp545d_plate1.pdf"},{"id":277815,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/pp/0545d/index.html"},{"id":277814,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0545d/pp545d_text.pdf"},{"id":121756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0545d/report-thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -150,\n              60\n            ],\n            [\n              -149.5,\n              60\n            ],\n            [\n              -149.5,\n              62\n            ],\n            [\n              -150,\n              62\n            ],\n            [\n              -150,\n              60\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db610609","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":208797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bonilla, Manuel G.","contributorId":74384,"corporation":false,"usgs":true,"family":"Bonilla","given":"Manuel","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":208798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1049,"text":"wsp1899C - 1970 - Sediment transport by streams in the Palouse River basin, Washington and Idaho, July 1961-June 1965","interactions":[],"lastModifiedDate":"2022-12-15T22:12:36.12682","indexId":"wsp1899C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"1899","chapter":"C","title":"Sediment transport by streams in the Palouse River basin, Washington and Idaho, July 1961-June 1965","docAbstract":"The Palouse River basin covers about 3,300 square miles in southeastern Washington and northwestern Idaho. The eastern part of the basin is composed of steptoes and foothills which are generally above an altitude of 2,600 feet; the central part is of moderate local relief and is mantled chiefly by thick loess deposits; and the western part is characterized by low relief and scabland topography and is underlain mostly by basalt. \r\n\r\nPrecipitation increases eastward across the study area. It ranges annually from 12 to 18 inches in the western part and from 14 to 23 inches in the central part, and it exceeds 40 inches in the eastern part. \r\n\r\nSurface runoff from the basin for the 4-year period of study (July 1961-June 1965) averaged 408,000 acre-feet per year, compared with 445,200 acre-feet per year for the 27-year period of record. The eastern part of the basin contributed about 55 percent of the total, whereas the central and western parts contributed 37 percent and 8 percent, respectively. Most sediment transport from the Palouse River basin and the highest sediment concentrations in streams occurred in the winter. Of the several storms during the study period, those of February 3-9, 1963, December 22-27, 1964, and January 27-February 4, 1965, accounted for 81 percent of the total 4-year suspended-sediment load; the storm of February 3-9, 1963, accounted for nearly one-half the total load. The discharge-weighted mean concentration of suspended sediment carried in the Palouse River past Hooper during the study period was 2,970 milligrams per liter. \r\n\r\nThe average annual sediment discharge of the Palouse River at its mouth was about 1,580,000 tons per year, and the estimated average annual sediment yield was 480 tons per square mile. The yield ranged from 5 tons per square mile from the western part of the basin to 2,100 tons per square mile from the central part. The high yield from the central part is attributed to a scarcity of vegetal cover, to the fine-grained loess soils, and to rapid runoff during winter storms. Sediment yield from the eastern part of the basin ranged from 460 to more than 1,000 tons per square mile.\r\n\r\nDuring high flow, silt particles make up the largest part of the suspended-sediment load, whereas during low flow, clay particles represent the greatest part. On the average, the suspended sediment transported by the Palouse River past Hooper contained 3 percent sand, 68 percent silt, and 29 percent clay. Unmeasured sediment discharge was estimated to have been 5 percent of the total sediment discharge. \r\n\r\nData collected during the 4-year period of study show that sediment loads were higher than those recorded by V. G. Kaiser during the longer period 1939-65. Whereas Kaiser's study showed an average annual soil loss of 9.6 million tons, the average annual loss during the recent study was 14.2 million tons. \r\n\r\nThe factor that has had the greatest effect on the increase of sediment yields is land use. Lands once covered and protected by natural vegetation have been extensively, cultivated, and much of the soil has become susceptible to erosion, particularly in areas mantled by loessal soils.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1899C","usgsCitation":"Boucher, P.R., 1970, Sediment transport by streams in the Palouse River basin, Washington and Idaho, July 1961-June 1965: U.S. Geological Survey Water Supply Paper 1899, Report: iv, 37 p.; 1 Plate: 26.50 × 24.50 inches, https://doi.org/10.3133/wsp1899C.","productDescription":"Report: iv, 37 p.; 1 Plate: 26.50 × 24.50 inches","costCenters":[],"links":[{"id":110035,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25118.htm","linkFileType":{"id":5,"text":"html"},"description":"25118"},{"id":137923,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1899c/report-thumb.jpg"},{"id":25713,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1899c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25714,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1899c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Washington","otherGeospatial":"Palouse River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.508,\n              47.483\n            ],\n            [\n              -118.322,\n              47.483\n            ],\n            [\n              -118.322,\n              46.517\n            ],\n            [\n              -116.508,\n              46.517\n            ],\n            [\n              -116.508,\n              47.483\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e9e4b07f02db5e94ca","contributors":{"authors":[{"text":"Boucher, P. 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,{"id":47933,"text":"ofr71122 - 1970 - A proposed streamflow data program for North Carolina","interactions":[],"lastModifiedDate":"2016-12-14T09:24:07","indexId":"ofr71122","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"71-122","title":"A proposed streamflow data program for North Carolina","language":"ENGLISH","doi":"10.3133/ofr71122","usgsCitation":"Goddard, G., Jackson, N., Hubbard, E., and Hinson, H., 1970, A proposed streamflow data program for North Carolina: U.S. Geological Survey Open-File Report 71-122, 113 p. ill., maps ; 28 cm., https://doi.org/10.3133/ofr71122.","productDescription":"113 p. ill., maps ; 28 cm.","costCenters":[{"id":13634,"text":"South Atlantic 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,{"id":55999,"text":"ofr70135 - 1970 - Summary of ground-water hydrological data in Michigan in 1968","interactions":[],"lastModifiedDate":"2017-07-12T10:31:57","indexId":"ofr70135","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-135","title":"Summary of ground-water hydrological data in Michigan in 1968","docAbstract":"<p>The purpose of this report is to make available the records of groundwater levels in the principal aquifers of the State through 1968 and to compile other related data, such as records of ground-water pumpage, data on municipal, public and industrial water-supply facilities, and the effects of precipitation on ground-water levels. Records of water levels in areas of heavy pumpage and in areas where changes are principally from natural influences are illustrated or tabulated to allow comparison between these types of water-level fluctuations. The water-levels and related data provide a day-to-day record for the evaluation of available ground-water supplies. The long-term records serve as a framework to which short-term records may be related.</p><p>This report is written for those persons, municipalities, industries, institutions, consultants, drillers and hydrologists interested in the groundwater resources of the State.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70135","usgsCitation":"Giroux, P., and Huffman, G., 1970, Summary of ground-water hydrological data in Michigan in 1968: U.S. Geological Survey Open-File Report 70-135, vii, 105 p., https://doi.org/10.3133/ofr70135.","productDescription":"vii, 105 p.","numberOfPages":"115","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":182180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0135/report-thumb.jpg"},{"id":343657,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0135/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":5720,"text":"pp655C - 1970 - Error analysis of streamflow data for an alluvial stream","interactions":[],"lastModifiedDate":"2012-02-02T00:05:49","indexId":"pp655C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"655","chapter":"C","title":"Error analysis of streamflow data for an alluvial stream","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp655C","usgsCitation":"Burkham, D., and Dawdy, D., 1970, Error analysis of streamflow data for an alluvial stream: U.S. Geological Survey Professional Paper 655, p. C1-C13, https://doi.org/10.3133/pp655C.","productDescription":"p. C1-C13","costCenters":[],"links":[{"id":118425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0655c/report-thumb.jpg"},{"id":32296,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0655c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdeaa","contributors":{"authors":[{"text":"Burkham, D. E.","contributorId":97073,"corporation":false,"usgs":true,"family":"Burkham","given":"D. E.","affiliations":[],"preferred":false,"id":151483,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dawdy, D.R.","contributorId":99956,"corporation":false,"usgs":true,"family":"Dawdy","given":"D.R.","affiliations":[],"preferred":false,"id":151484,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":16233,"text":"ofr70324 - 1970 - Geologic log and chemical data, diamond drill hole 1, Samrah, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2026-01-07T18:06:28.515395","indexId":"ofr70324","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-324","title":"Geologic log and chemical data, diamond drill hole 1, Samrah, Kingdom of Saudi Arabia","docAbstract":"<p>Diamond drill hole number 1 at the Samrah ancient mine, Kingdom of Saudi Arabia penetrated a series of mineralized fractures. Lead, zinc, and silver are the principal ore metals and galena and sphalerito are the ore minerals identified to date. Throughout the core there is a somewhat better correlation of silver with zinc than with lead.</p><p>The richest interval of core is in the main vein, 51-1/2 feet of core from 430 to 482 feet, and averages nearly 20 ounces of silver to the ton. Within this interval, 15 feet of core from 444 to 459 feet averages 60 ounces of silver to the ton. The richest single sample represents the five-foot interval from 454 to 459 feet and is reported to contain nearly 140 ounces of silver to the ton. All of these intervals contain recoverable quantities of lead and zinc and some contain a small amount of gold.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr70324","usgsCitation":"Theobald, P.K., Thompson, C., and Horn, H.D., 1970, Geologic log and chemical data, diamond drill hole 1, Samrah, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 70-324, Report: 61 p.;  4 Figures: 29.84 x 11.90 inches or smaller, https://doi.org/10.3133/ofr70324.","productDescription":"Report: 61 p.;  4 Figures: 29.84 x 11.90 inches or smaller","costCenters":[],"links":[{"id":148894,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0324/report-thumb.jpg"},{"id":498400,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1970/0324/figure-10.pdf","text":"Figure 10","linkFileType":{"id":1,"text":"pdf"}},{"id":498399,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1970/0324/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":498398,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1970/0324/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":498397,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1970/0324/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":498396,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0324/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Saudi Arabia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120.1569003387927,\n              42.19240723701009\n            ],\n            [\n              -120.10749572008328,\n              38.838079005221346\n            ],\n            [\n              -114.92237135508793,\n              34.88069804889223\n            ],\n            [\n              -114.98297993586107,\n              31.350750228533002\n            ],\n            [\n              -108.86155573128843,\n              31.164630024551755\n            ],\n            [\n              -108.78553410798668,\n              37.13467902221349\n            ],\n            [\n              -113.85445865369462,\n              37.17625160026044\n            ],\n            [\n              -113.88260270021135,\n              42.186786176024185\n            ],\n            [\n              -120.1569003387927,\n              42.19240723701009\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              42.32738784712694,\n              15.512723400556823\n            ],\n            [\n              55.46938659113218,\n              19.579159163878117\n            ],\n            [\n              56.089387644546775,\n              21.93229208405711\n            ],\n            [\n              48.656849713663576,\n              28.702737353396188\n            ],\n            [\n              39.424873163889,\n              32.90306864705684\n            ],\n            [\n              33.20660131965218,\n              29.600711506057223\n            ],\n            [\n              42.32738784712694,\n              15.512723400556823\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4f35","contributors":{"authors":[{"text":"Theobald, P. K. Jr.","contributorId":70398,"corporation":false,"usgs":true,"family":"Theobald","given":"P.","suffix":"Jr.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":172462,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, Charles E.","contributorId":35333,"corporation":false,"usgs":true,"family":"Thompson","given":"Charles E.","affiliations":[],"preferred":false,"id":172461,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Horn, Henry D.","contributorId":79492,"corporation":false,"usgs":true,"family":"Horn","given":"Henry","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":172463,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68309,"text":"ha376 - 1970 - Sediment yields of Wisconsin streams","interactions":[],"lastModifiedDate":"2015-10-06T07:48:35","indexId":"ha376","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"376","title":"Sediment yields of Wisconsin streams","docAbstract":"<p><span>Sediment in Wisconsin streams causes economic and engineering problems in water management and reduces the value of water for nearly all uses. Sediment produces problems such as reduced reservoir capacity, navigation hazards, increased cost of water treatment, property damage, temporary loss of farmland, destruction of feeding and nesting grounds of fish, and destruction of wildlife habitat. Sediment in water also reduces the aesthetic value of surface waters and is detrimental to the State's tourist and recreation industry.</span></p>\n<p><span>The yield of sediment from a drainage basin is subject to many environmental influences. Most sediment results from the weathering and erosion of soil and rock materials. Other factors such as rainfall intensity, runoff rate, topography, rock type, soil characteristics, vegetal cover, and land use also influence the rate of sediment production and movement. An understanding of the many parameters that influence sediment yield is a basic need for managing the State's water resources.</span></p>\n<p><span>The purpose of this report is to describe the magnitude and variability of sediment in Wisconsin streams, to relate sediment yields to the local environment, and to identify areas that need further study. The report is based on sediment data from 44 stream-gaging sites throughout the State. Determination of local areas of erosion and deposition are beyond the scope of the report.</span></p>\n<p>&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha376","usgsCitation":"Hindall, S.M., and Flint, R., 1970, Sediment yields of Wisconsin streams: U.S. Geological Survey Hydrologic Atlas 376, 1 Sheet: 35.50 x 35.00 inches, https://doi.org/10.3133/ha376.","productDescription":"1 Sheet: 35.50 x 35.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":185690,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89753,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/376/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United 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,{"id":12426,"text":"ofr702 - 1970 - A geochemical evaluation of the Ash Sha'ib mineral prospect, Asir quadrangle, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:33","indexId":"ofr702","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-2","title":"A geochemical evaluation of the Ash Sha'ib mineral prospect, Asir quadrangle, Kingdom of Saudi Arabia","docAbstract":"The mineralized zone at the remotely located Ash Sha'ib ancient mine contains only a small tonnage of moderately low grade sulfide- bearing rock. Based on present data the gross value of the deposit, with a value of $25.00 or more per ton, is $20,000,000. A belt of metasedimentary rocks, intruded by gabbro to the south and granite to the north, was the host for fissure vein-replacement type mineralization. Most of the mineralization is in a siliceous dolomite transected by fissures. The main sulfide mineral is sphalerite, but minor amounts of chalcopyrlte and argentlferous galena contribute to the value of the mineralized sections.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr702","usgsCitation":"Allcott, G.H., 1970, A geochemical evaluation of the Ash Sha'ib mineral prospect, Asir quadrangle, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 70-2, 38 p. ill. (some col.), col. maps ;28 cm., https://doi.org/10.3133/ofr702.","productDescription":"38 p. ill. (some col.), col. maps ;28 cm.","costCenters":[],"links":[{"id":144859,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1970/0002/report-thumb.jpg"},{"id":40664,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0002/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40665,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0002/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40666,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0002/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40667,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0002/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40668,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1970/0002/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":40669,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1970/0002/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae713","contributors":{"authors":[{"text":"Allcott, Glenn H.","contributorId":29422,"corporation":false,"usgs":true,"family":"Allcott","given":"Glenn","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":166120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56003,"text":"ofr70147 - 1970 - A proposed streamflow-data program for Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:12:07","indexId":"ofr70147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1970","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":"70-147","title":"A proposed streamflow-data program for Alabama","language":"ENGLISH","doi":"10.3133/ofr70147","usgsCitation":"Hains, C., 1970, A proposed streamflow-data program for Alabama: U.S. Geological Survey Open-File Report 70-147, 94 p., 4 figs., https://doi.org/10.3133/ofr70147.","productDescription":"94 p., 4 figs.","costCenters":[],"links":[{"id":181581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8aca","contributors":{"authors":[{"text":"Hains, C.F.","contributorId":55411,"corporation":false,"usgs":true,"family":"Hains","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":254629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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