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,{"id":56139,"text":"ofr5897 - 1958 - Plugging by air entrainment in artificial-recharge tests","interactions":[{"subject":{"id":56139,"text":"ofr5897 - 1958 - Plugging by air entrainment in artificial-recharge tests","indexId":"ofr5897","publicationYear":"1958","noYear":false,"title":"Plugging by air entrainment in artificial-recharge tests"},"predicate":"SUPERSEDED_BY","object":{"id":2724,"text":"wsp1615F - 1963 - Problems in artificial recharge through wells in the Grand Prairie region, Arkansas","indexId":"wsp1615F","publicationYear":"1963","noYear":false,"chapter":"F","title":"Problems in artificial recharge through wells in the Grand Prairie region, Arkansas"},"id":1}],"supersededBy":{"id":2724,"text":"wsp1615F - 1963 - Problems in artificial recharge through wells in the Grand Prairie region, Arkansas","indexId":"wsp1615F","publicationYear":"1963","noYear":false,"title":"Problems in artificial recharge through wells in the Grand Prairie region, Arkansas"},"lastModifiedDate":"2012-02-02T00:12:11","indexId":"ofr5897","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-97","title":"Plugging by air entrainment in artificial-recharge tests","language":"ENGLISH","doi":"10.3133/ofr5897","usgsCitation":"Sniegocki, R., 1958, Plugging by air entrainment in artificial-recharge tests: U.S. Geological Survey Open-File Report 58-97, 12 p., 1 fig., https://doi.org/10.3133/ofr5897.","productDescription":"12 p., 1 fig.","costCenters":[],"links":[{"id":185389,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e7ce","contributors":{"authors":[{"text":"Sniegocki, R. T.","contributorId":38546,"corporation":false,"usgs":true,"family":"Sniegocki","given":"R. T.","affiliations":[],"preferred":false,"id":254813,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56107,"text":"ofr5844 - 1958 - Bear River hydrometric data, tri-State investigations, 1956","interactions":[],"lastModifiedDate":"2013-08-01T15:16:50","indexId":"ofr5844","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-44","title":"Bear River hydrometric data, tri-State investigations, 1956","language":"ENGLISH","doi":"10.3133/ofr5844","usgsCitation":"Harris, A., and Jibson, W., 1958, Bear River hydrometric data, tri-State investigations, 1956: U.S. Geological Survey Open-File Report 58-44, 81 p., 4 figs., https://doi.org/10.3133/ofr5844.","productDescription":"81 p., 4 figs.","costCenters":[],"links":[{"id":181696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":275862,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1958/0044/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63dce8","contributors":{"authors":[{"text":"Harris, A.B.","contributorId":92290,"corporation":false,"usgs":true,"family":"Harris","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":254772,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jibson, W.N.","contributorId":27928,"corporation":false,"usgs":true,"family":"Jibson","given":"W.N.","email":"","affiliations":[],"preferred":false,"id":254771,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":23002,"text":"ofr5836 - 1958 - Water levels in observation wells in Santa Barbara County, California, in 1957","interactions":[],"lastModifiedDate":"2012-02-02T00:07:51","indexId":"ofr5836","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-36","title":"Water levels in observation wells in Santa Barbara County, California, in 1957","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr5836","issn":"0094-9140","usgsCitation":"Evenson, R.E., 1958, Water levels in observation wells in Santa Barbara County, California, in 1957: U.S. Geological Survey Open-File Report 58-36, 46 p. ill., maps ;27 cm., https://doi.org/10.3133/ofr5836.","productDescription":"46 p. ill., maps ;27 cm.","costCenters":[],"links":[{"id":153777,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1958/0036/report-thumb.jpg"},{"id":52391,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1958/0036/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9df6","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":189265,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13527,"text":"ofr5835 - 1958 - Geology of part of the Fanny Peak quadrangle, Wyoming-South Dakota","interactions":[{"subject":{"id":13527,"text":"ofr5835 - 1958 - Geology of part of the Fanny Peak quadrangle, Wyoming-South Dakota","indexId":"ofr5835","publicationYear":"1958","noYear":false,"title":"Geology of part of the Fanny Peak quadrangle, Wyoming-South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":33830,"text":"b1063I - 1963 - Geology of the Fanny Peak quadrangle, Wyoming-South Dakota","indexId":"b1063I","publicationYear":"1963","noYear":false,"chapter":"I","title":"Geology of the Fanny Peak quadrangle, Wyoming-South Dakota"},"id":1}],"supersededBy":{"id":33830,"text":"b1063I - 1963 - Geology of the Fanny Peak quadrangle, Wyoming-South Dakota","indexId":"b1063I","publicationYear":"1963","noYear":false,"title":"Geology of the Fanny Peak quadrangle, Wyoming-South Dakota"},"lastModifiedDate":"2025-09-30T15:43:33.691744","indexId":"ofr5835","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-35","title":"Geology of part of the Fanny Peak quadrangle, Wyoming-South Dakota","docAbstract":"<p>The Fanny Peak quadrangle is located on the west flank of the Black Hills. The exposed strata total over 4000 feet in thickness and range in age from Mississippian to late Cretaceous. Local surficial Cenozoic deposits are common.</p><p>The upper 200 to 300 feet of the Minnelusa formation is a breccia whose origin is attributed to removal of anhydrite by ground water and consequent collapse of the overlying strata. Crude bedding indicates uniform collapse; breccia pipes result from more intensive brecciation. The anhydrite probably occurred as lenses at different levels. 3recciation started after the Black Hills were uplifted and the Minnelusa was breached. Calcium sulphate in spring waters attests to present removal of anhydrite.</p><p>The Minnekahta limestone exhibits secondary structures attributed to gravity sliding. Cascade folds and slip sheets with displacements of not more than 30 feet developed in exposed beds whose dip is more than 30 degrees. Numerous intraformational folds and faults formed when beds within the limestone slid over each other. Shortening of the Ninnekahta limestone of about 200 feet per mile is estimated.</p><p>Four monoclines and associated structural terraces are interpreted as reflecting six fault blocks at depth with minimum displacement of 6000 feet. The intersecting Fanny Peak and Black Hills monoclines represent lines of major deformation. 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,{"id":14562,"text":"ofr5857 - 1958 - Periodic heat flow in a stratified medium with application to permafrost problems","interactions":[{"subject":{"id":14562,"text":"ofr5857 - 1958 - Periodic heat flow in a stratified medium with application to permafrost problems","indexId":"ofr5857","publicationYear":"1958","noYear":false,"title":"Periodic heat flow in a stratified medium with application to permafrost problems"},"predicate":"SUPERSEDED_BY","object":{"id":47389,"text":"b1083C - 1959 - Dissipation of the temperature effect of drilling a well in Arctic Alaska","indexId":"b1083C","publicationYear":"1959","noYear":false,"chapter":"C","title":"Dissipation of the temperature effect of drilling a well in Arctic Alaska"},"id":1}],"supersededBy":{"id":47389,"text":"b1083C - 1959 - Dissipation of the temperature effect of drilling a well in Arctic Alaska","indexId":"b1083C","publicationYear":"1959","noYear":false,"title":"Dissipation of the temperature effect of drilling a well in Arctic Alaska"},"lastModifiedDate":"2024-07-15T18:34:29.601987","indexId":"ofr5857","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-57","title":"Periodic heat flow in a stratified medium with application to permafrost problems","docAbstract":"<p>Solutions to the Fourier heat equation for quasi-steady periodic flow in a stratified semi-infinite medium can be obtained readily by standard methods. The results have wide application to studies of earth-temperature variations induced by diurnal, annual, and other periodic variations in ground surface temperature. Much of the previous work on this subject has been interpreted with reference to the solution for the homogeneous case; and this can be seriously in error when applied to stratified earth materials.</p><p>One application of the theory is to the important problem of determining the minimum thickness of gravel fill required to maintain the material on which it rests (the subgrade) in a perennially frozen state in permafrost areas. The results indicate that the required fill thickness is quite sensitive to the thermal properties of the subgrade. If a thin layer of material with low thermal contact coefficient, such as spruce logs, is placed between the fill and subgrade, the thickness of fill required to maintain undisturbed permafrost can be greatly reduced.</p><p>The thermal properties of the soil beneath the layer supporting plant growth can exercise an important influence on the temperature in that layer. This effect, which cannot be explained by studies of the ground surface and the surficial layer, is likely to have important application to plant ecology in the Arctic.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5857","usgsCitation":"Lachenbruch, A.H., 1958, Periodic heat flow in a stratified medium with application to permafrost problems: U.S. Geological Survey Open-File Report 58-57, 67 p., https://doi.org/10.3133/ofr5857.","productDescription":"67 p.","costCenters":[],"links":[{"id":431070,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1958/0057/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146274,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1958/0057/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6885f5","contributors":{"authors":[{"text":"Lachenbruch, Arthur H.","contributorId":27850,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"Arthur","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":169652,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14596,"text":"ofr5860 - 1958 - Rate for flood insurance","interactions":[],"lastModifiedDate":"2024-06-24T18:18:38.017275","indexId":"ofr5860","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-60","title":"Rate for flood insurance","docAbstract":"<p>Soon after the 1951 floods on the Kansas and lower Missouri Rivers, President Truman submitted to Congress (82d Cong., 1st sess., 1951) a proposal for a national flood insurance fund. Although the proposal was not acted upon by the 82d Congree, there was considerable discussion of it in the press and in the technical literature. Among the latter were papers by Langbein (1953), Foster (1954), and by the Insurance Executive Association (1952). The paper by Langbein discussed flood insurance as a means of promoting wise use of the flood plain. Foster's paper reviewed his work for the Insurance Executive Association without, however, reaching any independent decision as to the workability of hydrologic techniques in an insurance program. The report of the Insurance Executive Association presented mainly the industries viewpoint that flood insurance is not feasible. It is interesting to note, however, that in a recent report McGuinness (1957), of the Allstate Insurance Co., says \"This position has been taken without recourse to actuarial or statistical methods which might be used to fit an insurance company's underwriting retentions to the exposures it would meet.\"&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5860","usgsCitation":"Langbein, W.B., 1958, Rate for flood insurance: U.S. Geological Survey Open-File Report 58-60, 20 p., https://doi.org/10.3133/ofr5860.","productDescription":"20 p.","costCenters":[],"links":[{"id":148236,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1958/0060/report-thumb.jpg"},{"id":430462,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1958/0060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649313","contributors":{"authors":[{"text":"Langbein, Walter Basil","contributorId":40581,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter","email":"","middleInitial":"Basil","affiliations":[],"preferred":false,"id":169711,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56128,"text":"ofr5874 - 1958 - Chemical quality of surface waters of South Dakota, with special reference to selenium, boron, and fluoride","interactions":[],"lastModifiedDate":"2012-02-02T00:12:04","indexId":"ofr5874","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1958","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":"58-74","title":"Chemical quality of surface waters of South Dakota, with special reference to selenium, boron, and fluoride","language":"ENGLISH","doi":"10.3133/ofr5874","usgsCitation":"Petri, L.R., 1958, Chemical quality of surface waters of South Dakota, with special reference to selenium, boron, and fluoride: U.S. Geological Survey Open-File Report 58-74, 150 p., 2 figs., 1 pl., https://doi.org/10.3133/ofr5874.","productDescription":"150 p., 2 figs., 1 pl.","costCenters":[],"links":[{"id":180843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3865","contributors":{"authors":[{"text":"Petri, L. R.","contributorId":48944,"corporation":false,"usgs":true,"family":"Petri","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":254798,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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