{"pageNumber":"6341","pageRowStart":"158500","pageSize":"25","recordCount":184689,"records":[{"id":48073,"text":"ofr72328 - 1971 - Annual compilation and analysis of hydrologic data for Honey Creek, Trinity River Basin, Texas, 1969","interactions":[],"lastModifiedDate":"2016-08-23T14:31:39","indexId":"ofr72328","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"72-328","title":"Annual compilation and analysis of hydrologic data for Honey Creek, Trinity River Basin, Texas, 1969","docAbstract":"

The U.S. Soil Conservation Service is actively engaged in the installation of flood and soil erosion reducing measures in Texas under the authority of ''The Flood Control Act of 1936 and 1944\" and ''Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. The Soil Conservation Service has found a total of approximately 3,500 floodwater-retarding structures to be physically and economically feasible in Texas. As of September 30, 1969, 1,355 of these structures had been built.

This watershed-development program will have varying but important effects on the natural surface- and ground-water resources of river basins, especially where a large number of the floodwater-retarding structures are built. Basic hydrologic data under natural and developed conditions are needed to appraise the effects of the structures on the yield and mode of occurrence of runoff .

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr72328","collaboration":"Prepared in cooperation with the Texas Water Development Board and the Soil Conservation Service","usgsCitation":"Sansom, J., 1971, Annual compilation and analysis of hydrologic data for Honey Creek, Trinity River Basin, Texas, 1969: U.S. Geological Survey Open-File Report 72-328, v, 85 p., https://doi.org/10.3133/ofr72328.","productDescription":"v, 85 p.","numberOfPages":"90","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327724,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr72328.JPG"},{"id":287735,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0328/report.pdf"}],"country":"United States","state":"Texas","otherGeospatial":"Honey Creek, Trinity River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.91,29.4 ], [ -98.91,33.81 ], [ -94.36,33.81 ], [ -94.36,29.4 ], [ -98.91,29.4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bc60","contributors":{"authors":[{"text":"Sansom, J.N.","contributorId":14391,"corporation":false,"usgs":true,"family":"Sansom","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":236772,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48081,"text":"ofr72374 - 1971 - Gallagher Creek flood of July 30, 1971, Meridian, Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"ofr72374","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"72-374","title":"Gallagher Creek flood of July 30, 1971, Meridian, Mississippi","language":"ENGLISH","doi":"10.3133/ofr72374","usgsCitation":"Tate, C.H., 1971, Gallagher Creek flood of July 30, 1971, Meridian, Mississippi: U.S. Geological Survey Open-File Report 72-374, 4 p., 2 folded leaves of plates : ill., map ; 28 cm., https://doi.org/10.3133/ofr72374.","productDescription":"4 p., 2 folded leaves of plates : ill., map ; 28 cm.","costCenters":[],"links":[{"id":161943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b143c","contributors":{"authors":[{"text":"Tate, Charles H.","contributorId":17282,"corporation":false,"usgs":true,"family":"Tate","given":"Charles","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":236782,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":48082,"text":"ofr72375 - 1971 - Techniques for assessing water resource potentials in the developing countries: with emphasis on streamflow, erosion and sediment transport, water movement in unsaturated soils, ground water, and remote sensing in hydrologic applications","interactions":[],"lastModifiedDate":"2014-06-17T14:26:17","indexId":"ofr72375","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"72-375","title":"Techniques for assessing water resource potentials in the developing countries: with emphasis on streamflow, erosion and sediment transport, water movement in unsaturated soils, ground water, and remote sensing in hydrologic applications","docAbstract":"

Hydrologic instrumentation and methodology for assessing water-resource potentials have originated largely in the developed countries of the temperature zone. The developing countries lie largely in the tropic zone, which contains the full gamut of the earth's climatic environments, including most of those of the temperate zone. For this reason, most hydrologic techniques have world-wide applicability.

\n
\n

Techniques for assessing water-resource potentials for the high priority goals of economic growth are well established in the developing countries--but much more are well established in the developing countries--but much more so in some than in other. Conventional techniques for measurement and evaluation of basic hydrologic parameters are now well-understood in the developing countries and are generally adequate for their current needs and those of the immediate future. Institutional and economic constraints, however, inhibit growth of sustained programs of hydrologic data collection and application of the data to problems in engineering technology.

\n
\n

Computer-based technology, including processing of hydrologic data and mathematical modelling of hydrologic parameters i also well-begun in many developing countries and has much wider potential application. In some developing counties, however, there is a tendency to look on the computer as a panacea for deficiencies in basic hydrologic data collection programs. This fallacy must be discouraged, as the computer is a tool and not a \"magic box.\" There is no real substitute for sound programs of basic data collection.

\n
\n

Nuclear and isotopic techniques are being used increasingly in the developed countries in the measurement and evaluation of virtually all hydrologic parameter in which conventional techniques have been used traditionally. Even in the developed countries, however, many hydrologists are not using nuclear techniques, simply because they lack knowledge of the principles involved and of the potential benefits. Nuclear methodology in hydrologic applications is generally more complex than the conventional and hence requires a high level of technical expertise for effective use. Application of nuclear techniques to hydrologic problems in the developing countries is likely to be marginal for some years to come, owing to the higher costs involved and expertise required. Nuclear techniques, however, would seem to have particular promise in studies of water movement in unsaturated soils and of erosion and sedimentation where conventional techniques are inadequate, inefficient and in some cases costly.

\n
\n

Remote sensing offers great promise for synoptic evaluations of water resources and hydrologic processes, including the transient phenomena of the hydrologic cycle. Remote sensing is not, however, a panacea for deficiencies in hydrologic data programs in the developing countries. Rather it is a means for extending and augmenting on-the-ground observations ans surveys (ground truth) to evaluated water resources and hydrologic processes on a regionall or even continental scale.

\n
\n

With respect to economic growth goals in developing countries, there are few identifiable gaps in existing hydrologic instrumentation and methodology insofar as appraisal, development and management of available water resources are concerned. What is needed is acceleration of institutional development and professional motivation toward more effective use of existing and proven methodology. Moreover, much sophisticated methodology can be applied effectively in the developing countries only when adequate levels of indigenous scientific skills have been reached and supportive institutional frameworks are evolved to viability.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72375","usgsCitation":"Taylor, G.C., 1971, Techniques for assessing water resource potentials in the developing countries: with emphasis on streamflow, erosion and sediment transport, water movement in unsaturated soils, ground water, and remote sensing in hydrologic applications: U.S. Geological Survey Open-File Report 72-375, 70 p., https://doi.org/10.3133/ofr72375.","productDescription":"70 p.","numberOfPages":"72","costCenters":[],"links":[{"id":285999,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0375/report.pdf"},{"id":285998,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0375/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa274","contributors":{"authors":[{"text":"Taylor, George C. Jr.","contributorId":22767,"corporation":false,"usgs":true,"family":"Taylor","given":"George","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":236783,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47917,"text":"ofr7139 - 1971 - Chemical quality of ground water in the Dos Palos-Kettleman City area, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2024-05-24T21:00:22.894001","indexId":"ofr7139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-39","title":"Chemical quality of ground water in the Dos Palos-Kettleman City area, San Joaquin Valley, California","docAbstract":"

The Dos Palos-Kettleman City area of this report includes approximately 1,350 square miles on the central-western side of the San Joaquin Valley, California. Large-scale farming operations in the area have used ground water as the major source of irrigation water for nearly three quarters of a century. In 1968, completion of the San Luis Canal part of the California Aqueduct, made surface water available to farmers. In time the widespread use of this imported water may cause chemical-quality changes in the native ground water. To document conditions prior to any possible changes, 361 samples of ground water were taken before deliveries of surface water were begun. The data will serve as a base to which future investigations can be compared. To establish any trends, the results were compared to earlier chemical data for the area. The results indicated that only minor changes in chemical quality had occurred between 1951 and 1968.

Water from an upper water-bearing zone is markedly different from water in a lower water-bearing zone. Water in the upper zone is of various chemical types, and the concentration of dissolved solids increases from east to west across the area.

Water in the lower zone is a sodium sulfate type and is fairly consistent throughout the zone.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7139","collaboration":"Prepared in cooperation with the California Department of Water Resources U.S. Bureau of Reclamation, and Westlands Water District","usgsCitation":"Bertoldi, G., 1971, Chemical quality of ground water in the Dos Palos-Kettleman City area, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 71-39, 45 p., https://doi.org/10.3133/ofr7139.","productDescription":"45 p.","costCenters":[],"links":[{"id":429283,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0039/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162914,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0039/report-thumb.jpg"}],"country":"United States","state":"California","city":"Dos Palos, Kettleman City","otherGeospatial":"San Joaquin Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -120.68923886927595,\n 36.99619474770276\n ],\n [\n -120.68923886927595,\n 35.97967811304345\n ],\n [\n -119.91146897398625,\n 35.97967811304345\n ],\n [\n -119.91146897398625,\n 36.99619474770276\n ],\n [\n -120.68923886927595,\n 36.99619474770276\n ]\n ]\n ],\n \"type\": \"Polygon\"\n },\n \"id\": 0\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e399e","contributors":{"authors":[{"text":"Bertoldi, G.L.","contributorId":11605,"corporation":false,"usgs":true,"family":"Bertoldi","given":"G.L.","affiliations":[],"preferred":false,"id":236526,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47916,"text":"ofr7118 - 1971 - Preliminary catalog of pictures taken on the lunar surface during the Apollo 15 mission","interactions":[{"subject":{"id":47916,"text":"ofr7118 - 1971 - Preliminary catalog of pictures taken on the lunar surface during the Apollo 15 mission","indexId":"ofr7118","publicationYear":"1971","noYear":false,"title":"Preliminary catalog of pictures taken on the lunar surface during the Apollo 15 mission"},"predicate":"SUPERSEDED_BY","object":{"id":70042577,"text":"70042577 - 1972 - Preliminary geologic investigation of the Apollo 15 landing site","indexId":"70042577","publicationYear":"1972","noYear":false,"title":"Preliminary geologic investigation of the Apollo 15 landing site"},"id":1}],"supersededBy":{"id":70042577,"text":"70042577 - 1972 - Preliminary geologic investigation of the Apollo 15 landing site","indexId":"70042577","publicationYear":"1972","noYear":false,"title":"Preliminary geologic investigation of the Apollo 15 landing site"},"lastModifiedDate":"2014-07-14T10:04:39","indexId":"ofr7118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-18","title":"Preliminary catalog of pictures taken on the lunar surface during the Apollo 15 mission","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr7118","usgsCitation":"Baston, R., Larson, K., Reed, V.S., Rennilson, J.J., Sutton, R.L., Tyner, R., Ulrich, G., and Wolfe, E., 1971, Preliminary catalog of pictures taken on the lunar surface during the Apollo 15 mission: U.S. Geological Survey Open-File Report 71-18, 61 p., https://doi.org/10.3133/ofr7118.","productDescription":"61 p.","numberOfPages":"61","costCenters":[],"links":[{"id":162831,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c7b8","contributors":{"authors":[{"text":"Baston, R.M.","contributorId":72840,"corporation":false,"usgs":true,"family":"Baston","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":236522,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Larson, K.B.","contributorId":55410,"corporation":false,"usgs":true,"family":"Larson","given":"K.B.","email":"","affiliations":[],"preferred":false,"id":236519,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Reed, V. S.","contributorId":58255,"corporation":false,"usgs":true,"family":"Reed","given":"V.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":236521,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rennilson, J. J.","contributorId":107336,"corporation":false,"usgs":true,"family":"Rennilson","given":"J.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":236525,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Sutton, R. L.","contributorId":24364,"corporation":false,"usgs":true,"family":"Sutton","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":236518,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Tyner, R.L.","contributorId":75505,"corporation":false,"usgs":true,"family":"Tyner","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":236523,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ulrich, G. E.","contributorId":88737,"corporation":false,"usgs":true,"family":"Ulrich","given":"G. E.","affiliations":[],"preferred":false,"id":236524,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Wolfe, E.W.","contributorId":57470,"corporation":false,"usgs":true,"family":"Wolfe","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":236520,"contributorType":{"id":1,"text":"Authors"},"rank":8}]}} ,{"id":47920,"text":"ofr7147 - 1971 - Water temperatures of California streams, Sacramento basin subregion","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"ofr7147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-47","title":"Water temperatures of California streams, Sacramento basin subregion","language":"ENGLISH","doi":"10.3133/ofr7147","usgsCitation":"Blodgett, J.C., 1971, Water temperatures of California streams, Sacramento basin subregion: U.S. Geological Survey Open-File Report 71-47, 161 p. : maps ; 27 cm., https://doi.org/10.3133/ofr7147.","productDescription":"161 p. : maps ; 27 cm.","costCenters":[],"links":[{"id":162917,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd1e1","contributors":{"authors":[{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":236529,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47921,"text":"ofr7148 - 1971 - Water temperatures of California streams, San Francisco Bay subregion","interactions":[],"lastModifiedDate":"2014-05-29T06:49:27","indexId":"ofr7148","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-48","title":"Water temperatures of California streams, San Francisco Bay subregion","docAbstract":"

A summary of water-temperature records is presented for data collected through September 1968 in the San Francisco Bay Subregion of California. This report is one of a series covering the 11 hydrologic subregions of the State and includes data for 87 stream sites.

\n
\n

Water temperatures, in degrees Celsius, are summarized by months, years, and for the period of record. A description is included to identify each station where data were collected. A tolerance interval analysis indicated that 99 percent of the point water-temperature observations, determined either with thermograph probes or hand-held thermometers, should be ±0.6°C of the mean water temperature at the 95-percent confidence level. The probable total error ranges from ±0.8°C for periodic data to ±1.4°C for thermograph data.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr7148","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Blodgett, J.C., 1971, Water temperatures of California streams, San Francisco Bay subregion: U.S. Geological Survey Open-File Report 71-48, iv, 53 p., https://doi.org/10.3133/ofr7148.","productDescription":"iv, 53 p.","numberOfPages":"58","costCenters":[],"links":[{"id":287728,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287727,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0048/report.pdf"}],"country":"United States","state":"California","otherGeospatial":"San Francisco Bay","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.0,37.0 ], [ -124.0,40.0 ], [ -121.0,40.0 ], [ -121.0,37.0 ], [ -124.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd204","contributors":{"authors":[{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":236530,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47923,"text":"ofr7176 - 1971 - Estimating magnitude and frequency of floods in Wisconsin","interactions":[],"lastModifiedDate":"2015-10-13T11:43:21","indexId":"ofr7176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-76","title":"Estimating magnitude and frequency of floods in Wisconsin","docAbstract":"

This report provides methods for estimating flood characteristics at most sites where flood information may be needed for planning and design and summatizes the significant flood data and related information available on Wisconsin streams. Individual equations are presented for estimating flood discharges for selected recurrence intervals up to a 25-year flood for drainage areas 0.5 square miles and larger, a 50-year flood for drainage areas 20 square miles and larger, and a 100-year flood for drainage areas 50 square miles and larger. A ratio method is used for estimating a 50-year flood for drainage areas 0.5 to 20 square miles. The equations were defined from multiple-regression analysis of flood peak records and basin characteristics for 119 continuous-record gaging stations and 114 crest-stage partial-record stations in Wisconsin and adjoining States. Of the severai basin characteristics used in this study, only drainage area, main-channel slope, lake and marsh area, and areal factors were found to be statistically significant at the 99 percent effectiveness level for all flood frequencies. Solution of a hypothetical problem is given for using the flood-frequency equations. Graphs are presented for solution of flood discharges on regulated streams where the formulas are not applicable. Flood-frequency characteristics, 2-year flood to 100-year flood, and drainage basin characteristics for stations used in the multiple regression are presented in the appendices of this report.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7176","collaboration":"Prepared in cooperation with the State of Wisconsin Department of Transportation Division of Highways","usgsCitation":"Conger, D.H., 1971, Estimating magnitude and frequency of floods in Wisconsin: U.S. Geological Survey Open-File Report 71-76, v, 200 p., https://doi.org/10.3133/ofr7176.","productDescription":"v, 200 p.","numberOfPages":"210","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":162919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0076/report-thumb.jpg"},{"id":84727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0076/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc9cb","contributors":{"authors":[{"text":"Conger, Duane H.","contributorId":90731,"corporation":false,"usgs":true,"family":"Conger","given":"Duane","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":236532,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47924,"text":"ofr7181 - 1971 - Thermal study of the Missouri River in North Dakota using infrared imagery","interactions":[],"lastModifiedDate":"2018-02-16T14:18:37","indexId":"ofr7181","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-81","title":"Thermal study of the Missouri River in North Dakota using infrared imagery","docAbstract":"

Studies of infrared imagery obtained from aircraft at 305- to 1,524- meter altitudes indicate the feasibility of monitoring thermal changes attributable to the operation of thermal-electric plants and storage reservoirs, as well as natural phenomena such as tributary inflow and ground-water seeps, in large rivers. No identifiable sources of ground-water inflow below t he surface of the river could be found in the imagery. The thermal patterns from the generating plants and the major tri butary inflow are readily apparent in imagery obtained from an altitude of 305 meters. Though the patterns are generally discernible in the imagery from 1,067-meter and 1,524-meter altitudes, there is not sufficient ground resolution to make any but the most general qualitative analyses. The quality of the imagery varied with land-water temperature relations as well as with instrument properties.

\n

Portions of the tape-recorded imagery were processed in a color-coded quantization to enhance the displays and to attach quantitative significance to the data. Apparent radiant temperature computations from the 305-meter imagery were generally within l° Celsius of ground-truth data.

\n

The study indicates a marked decrease in water temperature in the Missouri River prior to early fall and a moderate increase in temperature in late fall because of the Lake Sakakawea impoundment. At the present time, thermal additions generated by the powerplants have little effect on the temperature regimen of the Missouri River at high rates of river discharge.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7181","collaboration":"Prepared in cooperation with the National Aeronautics and Space Administration (NASA).","usgsCitation":"Crosby, O., 1971, Thermal study of the Missouri River in North Dakota using infrared imagery: U.S. Geological Survey Open-File Report 71-81, iv, 46 p., https://doi.org/10.3133/ofr7181.","productDescription":"iv, 46 p.","numberOfPages":"54","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":162920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr7181.jpg"},{"id":311193,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0081/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"North Dakota","otherGeospatial":"Missouri River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -101.71142578125,\n 46.803819640791566\n ],\n [\n -101.71142578125,\n 47.58393661978137\n ],\n [\n -100.469970703125,\n 47.58393661978137\n ],\n [\n -100.469970703125,\n 46.803819640791566\n ],\n [\n -101.71142578125,\n 46.803819640791566\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a56e4b07f02db62db40","contributors":{"authors":[{"text":"Crosby, Orlo A.","contributorId":6065,"corporation":false,"usgs":true,"family":"Crosby","given":"Orlo A.","affiliations":[],"preferred":false,"id":236533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68106,"text":"ha388 - 1971 - Floods on selected reaches of Elk Creek, Douglas County, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:26:10","indexId":"ha388","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"388","title":"Floods on selected reaches of Elk Creek, Douglas County, Oregon","language":"ENGLISH","doi":"10.3133/ha388","usgsCitation":"Oster, E.A., 1971, Floods on selected reaches of Elk Creek, Douglas County, Oregon: U.S. Geological Survey Hydrologic Atlas 388, 1 map., https://doi.org/10.3133/ha388.","productDescription":"1 map.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":186608,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89376,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/388/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123.41666666666667,43.583333333333336 ], [ -123.41666666666667,43.666666666666664 ], [ -123.16666666666667,43.666666666666664 ], [ -123.16666666666667,43.583333333333336 ], [ -123.41666666666667,43.583333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df7d8","contributors":{"authors":[{"text":"Oster, E. 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Y., in which large amounts of ground water are used, mostly for public supply. Ground water, pumped from local aquifers, by privately owned water-supply companies, supplied the water needs of about 750,000 of the nearly 2 million residents of the county in 1967; the balance was supplied by New York City from surface sources outside the county in upstate New York. \r\n\r\nThe county's aquifers consist of sand and gravel of Late Cretaceous and of Pleistocene ages, and the aquifers comprise a wedge-shaped ground-water reservoir lying on a southeastward-sloping floor of Precambrian(?) bedrock. Beds of clay and silt generally confine water in the deeper parts of the reservoir; water in the deeper aquifers ranges from poorly confined to well confined. Wisconsin-age glacial deposits in the uppermost part of the reservoir contain ground water under water-table conditions. \r\n\r\nGround water pumpage averaged about 60 mgd (million gallons per day) in Queens County from about 1900 to 1967. Much of the water was used in adjacent Kings County, another borough of New York City, prior to 1950. The large ground-water withdrawal has resulted in a wide-spread and still-growing cone of depression in the water table, reflecting a loss of about 61 billion gallons of fresh water from storage. Significant drawdown of the water table probably began with rapid urbanization of Queens County in the 1920's. The county has been extensively paved, and storm and sanitary sewers divert water, which formerly entered the ground, to tidewater north and south of the county. Natural recharge to the aquifers has been reduced to about one half of the preurban rate and is below the withdrawal rate. Ground-water levels have declined more than 40. feet from the earliest-known levels, in 1903, to 1967, and the water table is below sea level in much of the county. \r\n\r\nThe aquifers are being contaminated by the movement of salty ground water toward the deepest parts of the cone of depression in central Queens County. Contamination of ground water is probably also occurring from leaking sewers and from pollutants leaking downward from the land surface. Thermal pollution of the ground water has occurred locally where ground water pumped for cooling uses is returned, with elevated temperatures, to the source aquifer through recharge wells. \r\n\r\nThe quality of ground water in Queens County in 1967 was generally satisfactory for public-supply and most industrial uses. However, the rate and distribution of ground-water withdrawals in the county are leading to greater decline of the water table and to increasing contamination of the aquifers. No 'safe limit' on pumpage can be set for the county because limits on the effects of pumping have not been established. A safe limit, at the present stage of urbanization, could range from considerably less than the current average 60 mgd to considerably more over a wide-range of pumping effects and acceptable water quality. However, continued removal of fresh water from storage and deterioration of water quality reduces the value of the county's aquifers, not only for current supply, but also for additional supply to the county and other parts of New York City in times of drought or other emergency.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp01A","usgsCitation":"Soren, J., 1971, Ground-water and geohydrologic conditions in Queens County, Long Island, New York: U.S. Geological Survey Water Supply Paper 2001, iv, 39 p. :2 fold. col. maps (in pocket) ;23 cm., https://doi.org/10.3133/wsp01A.","productDescription":"iv, 39 p. :2 fold. col. maps (in pocket) ;23 cm.","costCenters":[],"links":[{"id":138958,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2001a/report-thumb.jpg"},{"id":247239,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2001a/plate-1.pdf","size":"5369","linkFileType":{"id":1,"text":"pdf"}},{"id":247240,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2001a/plate-2.pdf","size":"3255","linkFileType":{"id":1,"text":"pdf"}},{"id":29138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2001a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d491","contributors":{"authors":[{"text":"Soren, Julian","contributorId":54184,"corporation":false,"usgs":true,"family":"Soren","given":"Julian","email":"","affiliations":[],"preferred":false,"id":145677,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":47956,"text":"ofr71206 - 1971 - Drilling and testing of well 69, Fort Wingate Army Depot, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"ofr71206","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-206","title":"Drilling and testing of well 69, Fort Wingate Army Depot, McKinley County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr71206","usgsCitation":"Mercer, J.W., and Lappala, E.G., 1971, Drilling and testing of well 69, Fort Wingate Army Depot, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 71-206, 41 p. ill., map ; 29 cm., https://doi.org/10.3133/ofr71206.","productDescription":"41 p. ill., map ; 29 cm.","costCenters":[],"links":[{"id":170189,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0206/report-thumb.jpg"},{"id":84763,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0206/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84764,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0206/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84765,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0206/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84766,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0206/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84767,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0206/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633c05","contributors":{"authors":[{"text":"Mercer, Jerry W.","contributorId":32534,"corporation":false,"usgs":true,"family":"Mercer","given":"Jerry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":236580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lappala, Eric G.","contributorId":23182,"corporation":false,"usgs":true,"family":"Lappala","given":"Eric","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":236579,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63349,"text":"gq894 - 1971 - Geologic map of the Kaiser Peak quadrangle, central Sierra Nevada, California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:59","indexId":"gq894","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"894","title":"Geologic map of the Kaiser Peak quadrangle, central Sierra Nevada, California","language":"ENGLISH","doi":"10.3133/gq894","usgsCitation":"Bateman, P.C., Lockwood, J.P., and Lydon, P.A., 1971, Geologic map of the Kaiser Peak quadrangle, central Sierra Nevada, California: U.S. Geological Survey Geologic Quadrangle 894, 1 map., https://doi.org/10.3133/gq894.","productDescription":"1 map.","costCenters":[],"links":[{"id":101813,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_33.htm","linkFileType":{"id":5,"text":"html"},"description":"33"},{"id":249451,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0894/report.pdf","size":"318","linkFileType":{"id":1,"text":"pdf"}},{"id":252933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0894/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.25,37.25 ], [ -119.25,37.5 ], [ -119,37.5 ], [ -119,37.25 ], [ -119.25,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69758f","contributors":{"authors":[{"text":"Bateman, Paul Charles","contributorId":54586,"corporation":false,"usgs":true,"family":"Bateman","given":"Paul","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":268711,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lockwood, John P. 0000-0002-6562-0222","orcid":"https://orcid.org/0000-0002-6562-0222","contributorId":30976,"corporation":false,"usgs":true,"family":"Lockwood","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":268710,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lydon, Philip A.","contributorId":12112,"corporation":false,"usgs":true,"family":"Lydon","given":"Philip","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":268709,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68087,"text":"ha455 - 1971 - Glacier dammed lakes and outburst floods in Alaska","interactions":[],"lastModifiedDate":"2021-11-08T19:49:31.386944","indexId":"ha455","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"455","title":"Glacier dammed lakes and outburst floods in Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha455","usgsCitation":"Post, A., and Mayo, L., 1971, Glacier dammed lakes and outburst floods in Alaska: U.S. Geological Survey Hydrologic Atlas 455, Report: 10 p.; 3 Plates: 54.50 × 30.00 inches or smaller, https://doi.org/10.3133/ha455.","productDescription":"Report: 10 p.; 3 Plates: 54.50 × 30.00 inches or smaller","costCenters":[],"links":[{"id":91814,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/455/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91816,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/455/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91815,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/455/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/455/report-thumb.jpg"},{"id":391474,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15841.htm"},{"id":89347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/455/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -154,55.5 ], [ -154,64 ], [ -129.5,64 ], [ -129.5,55.5 ], [ -154,55.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679bca","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":277620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayo, L.R.","contributorId":21541,"corporation":false,"usgs":true,"family":"Mayo","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":277619,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":47950,"text":"ofr71185 - 1971 - Preliminary results of time-of-travel measurements on Wind/Bighorn River from Boysen Dam to Greybull, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"ofr71185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-185","title":"Preliminary results of time-of-travel measurements on Wind/Bighorn River from Boysen Dam to Greybull, Wyoming","language":"ENGLISH","doi":"10.3133/ofr71185","usgsCitation":"Lowham, H.W., and Wilson, J.F., 1971, Preliminary results of time-of-travel measurements on Wind/Bighorn River from Boysen Dam to Greybull, Wyoming: U.S. Geological Survey Open-File Report 71-185, 7 p.: map ; 27 cm., https://doi.org/10.3133/ofr71185.","productDescription":"7 p.: map ; 27 cm.","costCenters":[],"links":[{"id":170120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0185/report-thumb.jpg"},{"id":84744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0185/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66aad3","contributors":{"authors":[{"text":"Lowham, Hugh W.","contributorId":17483,"corporation":false,"usgs":true,"family":"Lowham","given":"Hugh","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":236570,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, James F. 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J.","affiliations":[],"preferred":false,"id":276060,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63302,"text":"gq852 - 1971 - Geologic map of the Park City East quadrangle, Summit and Wasatch Counties, Utah","interactions":[{"subject":{"id":47220,"text":"ofr6924 - 1969 - Geologic map of the Park City East Quadrangle, Summit and Wasatch Counties, Utah","indexId":"ofr6924","publicationYear":"1969","noYear":false,"title":"Geologic map of the Park City East Quadrangle, Summit and Wasatch Counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":63302,"text":"gq852 - 1971 - Geologic map of the Park City East quadrangle, Summit and Wasatch Counties, Utah","indexId":"gq852","publicationYear":"1971","noYear":false,"title":"Geologic map of the Park City East quadrangle, Summit and Wasatch Counties, Utah"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq852","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"852","title":"Geologic map of the Park City East quadrangle, Summit and Wasatch Counties, Utah","language":"ENGLISH","doi":"10.3133/gq852","usgsCitation":"Bromfield, C.S., and Crittenden, M., 1971, Geologic map of the Park City East quadrangle, Summit and Wasatch Counties, Utah: U.S. Geological Survey Geologic Quadrangle 852, 1 map :col. ;58 x 44 cm., on sheet 85 x 84 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq852.","productDescription":"1 map :col. ;58 x 44 cm., on sheet 85 x 84 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":103568,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2154.htm","linkFileType":{"id":5,"text":"html"},"description":"2154"},{"id":249406,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0852/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":252805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0852/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.5,40.6175 ], [ -111.5,40.75 ], [ -111.36749999999999,40.75 ], [ -111.36749999999999,40.6175 ], [ -111.5,40.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691fcf","contributors":{"authors":[{"text":"Bromfield, Calvin Stanton","contributorId":12048,"corporation":false,"usgs":true,"family":"Bromfield","given":"Calvin","email":"","middleInitial":"Stanton","affiliations":[],"preferred":false,"id":268636,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crittenden, Max D.","contributorId":43404,"corporation":false,"usgs":true,"family":"Crittenden","given":"Max D.","affiliations":[],"preferred":false,"id":268637,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63763,"text":"gp754 - 1971 - Aeromagnetic map and interpretation of the Salton Sea geothermal area, California","interactions":[],"lastModifiedDate":"2025-07-07T17:39:15.30804","indexId":"gp754","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"754","title":"Aeromagnetic map and interpretation of the Salton Sea geothermal area, California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp754","usgsCitation":"Griscom, A., and Muffler, L., 1971, Aeromagnetic map and interpretation of the Salton Sea geothermal area, California: U.S. Geological Survey Geophysical Investigations Map 754, 1 Plate: 49.97 x 34.44 inches, https://doi.org/10.3133/gp754.","productDescription":"1 Plate: 49.97 x 34.44 inches","costCenters":[],"links":[{"id":253460,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0754/report-thumb.jpg"},{"id":249946,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0754/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249945,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0754/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":491755,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6109.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"62500","country":"United States","state":"California","otherGeospatial":"Salton Sea geothermal area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -115.25,\n 33.0833\n ],\n [\n -115.25,\n 33.4167\n ],\n [\n -116,\n 33.4167\n ],\n [\n -116,\n 33.0833\n ],\n [\n -115.25,\n 33.0833\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db6983ff","contributors":{"authors":[{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":269536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Muffler, L.J.P.","contributorId":63383,"corporation":false,"usgs":true,"family":"Muffler","given":"L.J.P.","affiliations":[],"preferred":false,"id":269537,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42087,"text":"ofr71291 - 1971 - Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho","interactions":[{"subject":{"id":42087,"text":"ofr71291 - 1971 - Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho","indexId":"ofr71291","publicationYear":"1971","noYear":false,"title":"Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"id":1}],"supersededBy":{"id":64046,"text":"gp919 - 1978 - Aeromagnetic map of Idaho","indexId":"gp919","publicationYear":"1978","noYear":false,"title":"Aeromagnetic map of Idaho"},"lastModifiedDate":"2022-06-06T19:51:44.388865","indexId":"ofr71291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-291","title":"Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71291","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Aeromagnetic map of the Challis, May, Lone Pine Peak, and Doublespring quadrangles, east-central Idaho: U.S. Geological Survey Open-File Report 71-291, 1 Plate: 29.41 x 42.51 inches, https://doi.org/10.3133/ofr71291.","productDescription":"1 Plate: 29.41 x 42.51 inches","costCenters":[],"links":[{"id":175557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0291/report-thumb.jpg"},{"id":401700,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0291/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Idaho","otherGeospatial":"Challis Quadrangle, Doublespring Quadrangle, Lone Pine Peak Quadrangle, May Quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.8895263671875,\n 44.209772586984485\n ],\n [\n -113.7579345703125,\n 44.209772586984485\n ],\n [\n -113.7579345703125,\n 44.67646564865964\n ],\n [\n -114.8895263671875,\n 44.67646564865964\n ],\n [\n -114.8895263671875,\n 44.209772586984485\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db69704b","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":530820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":64807,"text":"i615 - 1971 - Geologic map of the Orocovis Quadrangle, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-10T00:10:56","indexId":"i615","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"615","subseriesTitle":"NONE","title":"Geologic map of the Orocovis Quadrangle, Puerto Rico","language":"ENGLISH","doi":"10.3133/i615","usgsCitation":"Briggs, R.P., 1971, Geologic map of the Orocovis Quadrangle, Puerto Rico: U.S. Geological Survey IMAP 615, 1 map., https://doi.org/10.3133/i615.","productDescription":"1 map.","costCenters":[],"links":[{"id":106869,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9406.htm","linkFileType":{"id":5,"text":"html"},"description":"9406"},{"id":186993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91441,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0615/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -66.5,18.1175 ], [ -66.5,18.25 ], [ -66.36749999999999,18.25 ], [ -66.36749999999999,18.1175 ], [ -66.5,18.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af6e4b07f02db692f9e","contributors":{"authors":[{"text":"Briggs, R. P.","contributorId":47797,"corporation":false,"usgs":true,"family":"Briggs","given":"R.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":272188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15717,"text":"ofr71242 - 1971 - Geology and economic potential for chromite in the Zhob Valley ultramafic rock complex, Hindubagh, Quetta division, West Pakistan","interactions":[],"lastModifiedDate":"2012-02-02T00:07:07","indexId":"ofr71242","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-242","title":"Geology and economic potential for chromite in the Zhob Valley ultramafic rock complex, Hindubagh, Quetta division, West Pakistan","docAbstract":"The ultramafic rocks making up the Zhob Valley igneous complex have yielded small amounts of metallurgical-grade chromite since the early part of the century. From 1968-1970 a cooperative study undertaken by the Geological Survey of Pakistan and the U. S. Geological Survey, under the auspices of the Government of Pakistan and the Agency for International Development, evaluated the chromite potential of the Zhob Valley area and provided data for effective exploration. \r\n\r\nThe Jung Tor Ghar ultramafic rock mass, covering an area of about 45 square miles, is a thrust-fault block completely surrounded and underlain (?) by sedimentary rocks as young as Late Cretaceous in age. The igneous rocks were thrust from the northwest along an east-trending, north-dipping fault in Late Cretaceous or Paleocene time and were peneplaned, dissected, and deeply laterized by mid-Eocene time. \r\n\r\nThe ultramafic rocks consist of interlayered harzburgite and dunite and a cross-cutting dunite here called transgressive dunite. Layered structure passes without discernible deviation from the interlayered harzburgite-dunite through the transgressive dunite. The lowest rocks in the mass, composed mainly of transgressive dunite, grade upward into the interlayered rock about 3,000 feet above the fault block base. The upper transgressive dunites tend to form interconnecting linear networks and probably a few pipe-like structures. The transgressive dunite is thought to have formed by action of water derived from the underlying sedimentary rocks; the water heated by the hot ultramafic rock (at the time of emplacement) altered the pyroxene to olivine and talc, and, with lowering temperature, to serpentine. Other interpretations are possible. \r\n\r\nVirtually all the chromite in the Jung Tor Ghar lies in or immediately above the masses of transgressive dunite. This fact provides a key to chromite exploration: The most favorable zone for prospecting lies in the vicinity of the upper contacts of the transgressive dunite masses where they. are flatly dipping; if the transgressive dunite masses are steeply dipping or pipe-like, the chromite tends to be more centrally located. \r\n\r\nThe Jung Tor Ghar is believed to contain enough unmined chromite at practical minable depths to equal or exceed that mined to date but the individual deposits are likely to be small.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr71242","usgsCitation":"Rossman, D.L., Ahmad, Z., and Rahman, H., 1971, Geology and economic potential for chromite in the Zhob Valley ultramafic rock complex, Hindubagh, Quetta division, West Pakistan: U.S. Geological Survey Open-File Report 71-242, ii, 63 leaves :ill., maps ;27 cm., https://doi.org/10.3133/ofr71242.","productDescription":"ii, 63 leaves :ill., maps ;27 cm.","costCenters":[],"links":[{"id":148462,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0242/report-thumb.jpg"},{"id":44731,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0242/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44732,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0242/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44733,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0242/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a28e","contributors":{"authors":[{"text":"Rossman, Darwin L.","contributorId":94663,"corporation":false,"usgs":true,"family":"Rossman","given":"Darwin","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":171595,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ahmad, Zaki","contributorId":85205,"corporation":false,"usgs":true,"family":"Ahmad","given":"Zaki","email":"","affiliations":[],"preferred":false,"id":171594,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rahman, Hamidur","contributorId":51757,"corporation":false,"usgs":true,"family":"Rahman","given":"Hamidur","email":"","affiliations":[],"preferred":false,"id":171593,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":12635,"text":"ofr7129 - 1971 - Total-count gamma radiation map of the Bopolu quadrangle, Liberia","interactions":[{"subject":{"id":12635,"text":"ofr7129 - 1971 - Total-count gamma radiation map of the Bopolu quadrangle, Liberia","indexId":"ofr7129","publicationYear":"1971","noYear":false,"title":"Total-count gamma radiation map of the Bopolu quadrangle, Liberia"},"predicate":"SUPERSEDED_BY","object":{"id":64727,"text":"i772C - 1974 - Total-count gamma radiation map of the Bopolu Quadrangle, Liberia","indexId":"i772C","publicationYear":"1974","noYear":false,"chapter":"C","title":"Total-count gamma radiation map of the Bopolu Quadrangle, Liberia"},"id":1}],"supersededBy":{"id":64727,"text":"i772C - 1974 - Total-count gamma radiation map of the Bopolu Quadrangle, Liberia","indexId":"i772C","publicationYear":"1974","noYear":false,"title":"Total-count gamma radiation map of the Bopolu Quadrangle, Liberia"},"lastModifiedDate":"2012-02-02T00:06:27","indexId":"ofr7129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"71-29","title":"Total-count gamma radiation map of the Bopolu quadrangle, Liberia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7129","usgsCitation":"Behrendt, J.C., and Wotorson, C.S., 1971, Total-count gamma radiation map of the Bopolu quadrangle, Liberia: U.S. Geological Survey Open-File Report 71-29, 5 leaves :maps ;27 cm.; 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