{"pageNumber":"5696","pageRowStart":"142375","pageSize":"25","recordCount":165635,"records":[{"id":19925,"text":"ofr71195 - 1971 - Analyses of samples and preliminary geologic summary of barite- silver-base metal deposits near Glacier Creek, Skagway B-4 quadrangle, southeastern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:07:43","indexId":"ofr71195","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":"71-195","title":"Analyses of samples and preliminary geologic summary of barite- silver-base metal deposits near Glacier Creek, Skagway B-4 quadrangle, southeastern Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr71195","usgsCitation":"MacKevett, E., 1971, Analyses of samples and preliminary geologic summary of barite- silver-base metal deposits near Glacier Creek, Skagway B-4 quadrangle, southeastern Alaska: U.S. Geological Survey Open-File Report 71-195, 1 v. (various pagings) :ill. ;28 cm.; 8 p., https://doi.org/10.3133/ofr71195.","productDescription":"1 v. (various pagings) :ill. ;28 cm.; 8 p.","costCenters":[],"links":[{"id":153077,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0195/report-thumb.jpg"},{"id":49434,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0195/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680e28","contributors":{"authors":[{"text":"MacKevett, E.M. Jr.","contributorId":58613,"corporation":false,"usgs":true,"family":"MacKevett","given":"E.M.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":181746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20472,"text":"ofr71226 - 1971 - Microearthquake activity in the vicinity of Wooded Island, Hanford region, Washington","interactions":[],"lastModifiedDate":"2026-04-30T15:07:00.264259","indexId":"ofr71226","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":"71-226","title":"Microearthquake activity in the vicinity of Wooded Island, Hanford region, Washington","docAbstract":"<p>The U.S. Geological Survey (U.S.G.S.) began to monitor microearthquake activity in the region of the Atomic Energy Commission's Hanford Reservation in south-central Washington in March 1969. The Division of Reactor Development and Technology (DRDT), of the Atomic Energy Commission (AEC), supported the operation of a network of 6 (later 7) short-period, high-gain seismograph stations (Figure 1) through June 1970. Then the Chemical Processing Division (CPD) of the AEC assumed support of the original 7-station network and added 9 additional stations (Figure 1). Some preliminary results from the 7-station network covering the period 23 March 1969 to 31 December 1969 were released in the U.S.G.S. open-file4report \"Geologic Investigation of Faulting in the Hanford Region, Washington\", by James W. Bingham, Clark J. Landquist, and Elmer H. Baltz. Preliminary reports on the results from the seismograph network for 1970 have been submitted to the AEC. This report covers a specific zone of microearthquake activity located near Wooded Island in the Columbia River, which flows along the east side of the Hanford Reservation (Figure 1). The data cover the period 23 March 1969 to 28 February 1971.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71226","usgsCitation":"Pitt, A., 1971, Microearthquake activity in the vicinity of Wooded Island, Hanford region, Washington: U.S. Geological Survey Open-File Report 71-226, 23 leaves :ill., maps ;28 cm.; 24 p., https://doi.org/10.3133/ofr71226.","productDescription":"23 p.","costCenters":[],"links":[{"id":503674,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0226/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":152143,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0226/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Hanford region, Wooded 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,{"id":47934,"text":"ofr71144 - 1971 - Annual compilation and analysis of hydrologic data for Pin Oak Creek, Trinity River basin, Texas, 1969","interactions":[],"lastModifiedDate":"2021-09-15T19:49:48.727327","indexId":"ofr71144","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":"71-144","title":"Annual compilation and analysis of hydrologic data for Pin Oak Creek, Trinity River basin, Texas, 1969","docAbstract":"<p>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.</p><p>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.</p><p>Hydrologic investigations of these small watersheds were begun by the U.S. Geological Survey in 1951 and are now being made in 12 areas (fig. 1). These studies are being made in cooperation with the Texas Water Development Board, the Soil Conservation Service, the San Antonio River Authority, the city of Dallas, and the Tarrant County Water Control and Improvement District No. 1. The 12 study areas were chosen to sample watersheds having different rainfall, topography, geology, and soils. In five of the study areas (North, Little Elm, Mukewater, North Elm-Little Pond, and Pin Oak Creeks), streamflow and rainfall records were collected prior to construction of the floodwater-retarding structures, thus affording the opportunity for analyses of the conditions \"before and after\" development. Structures have now been built in three of these study areas. A summary of the development of the floodwater-retarding structures on each study area as of September 30, 1969, is shown in table 1.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71144","collaboration":"Prepared in cooperation with the Texas Water Development Board","usgsCitation":"Hampton, B., and Myers, D., 1971, Annual compilation and analysis of hydrologic data for Pin Oak Creek, Trinity River basin, Texas, 1969: U.S. Geological Survey Open-File Report 71-144, iii, 28 p., https://doi.org/10.3133/ofr71144.","productDescription":"iii, 28 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":389294,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0144/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0144/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Pin Oak Creek, Trinity River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.90765380859375,\n              31.344254455668054\n            ],\n            [\n              -96.12487792968749,\n              31.344254455668054\n            ],\n            [\n              -96.12487792968749,\n              31.891550612684366\n            ],\n            [\n              -96.90765380859375,\n              31.891550612684366\n            ],\n            [\n              -96.90765380859375,\n              31.344254455668054\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bbb4","contributors":{"authors":[{"text":"Hampton, B.B.","contributorId":43362,"corporation":false,"usgs":true,"family":"Hampton","given":"B.B.","email":"","affiliations":[],"preferred":false,"id":236547,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Myers, D.R.","contributorId":104534,"corporation":false,"usgs":true,"family":"Myers","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":236548,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38935,"text":"pp434F - 1971 - A flood-frequency relation based on regional record maxima","interactions":[],"lastModifiedDate":"2012-02-02T00:10:17","indexId":"pp434F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"434","chapter":"F","title":"A flood-frequency relation based on regional record maxima","language":"ENGLISH","doi":"10.3133/pp434F","usgsCitation":"Carrigan, P., 1971, A flood-frequency relation based on regional record maxima: U.S. Geological Survey Professional Paper 434, 21 p., https://doi.org/10.3133/pp434F.","productDescription":"21 p.","costCenters":[],"links":[{"id":120519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0434f/report-thumb.jpg"},{"id":65978,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0434f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec54","contributors":{"authors":[{"text":"Carrigan, P.H. Jr.","contributorId":21935,"corporation":false,"usgs":true,"family":"Carrigan","given":"P.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":220693,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47948,"text":"ofr71183 - 1971 - Estimated subsidence in the Chino-Riverside and Bunker Hill-Yucaipa areas in Southern California for a postulated water-level lowering, 1965-2015","interactions":[],"lastModifiedDate":"2017-03-08T13:52:55","indexId":"ofr71183","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":"71-183","title":"Estimated subsidence in the Chino-Riverside and Bunker Hill-Yucaipa areas in Southern California for a postulated water-level lowering, 1965-2015","docAbstract":"<p>One of the alternate plans for water utilization being considered by the California Department of Water Resources in the Chino-Riverside and Bunker Hill-Yucaipa areas in southern California involves partial mining of ground water during the period 1965-2015, and consequent substantial lowering of water levels. The Department wants to know whether land subsidence would be a problem as a result of the postulated lowering. To answer this question, to the extent that leveling control permits, the present study has been made at the request of and in cooperation with the State of California.</p><p>At a few locations in the Chino-Riverside and Bunker Hill-Yucaipa areas, comparable water-level decline and subsidence data are available from which rough estimates can be made of subsidence that would occur as a result of the postulated lowering from 1965 to 2015. Limited leveling control, and apparent discrepancies in the data, preclude accurate determination of amounts of subsidence caused by historic water-level decline.</p><p>Based on 1965-2015 water-level changes postulated by the California Department of Water Resources and on available subsidence/head decline ratios, as much as 6 feet of subsidence might occur northeast of the San Jacinto fault between Loma Linda and San Bernardino, in an area of more than 350 feet of projected water-level decline. Also, as much as 1.5 feet of subsidence might occur in the vicinity of Ontario.</p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71183","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Lofgren, B.E., 1971, Estimated subsidence in the Chino-Riverside and Bunker Hill-Yucaipa areas in Southern California for a postulated water-level lowering, 1965-2015: U.S. Geological Survey Open-File Report 71-183, 20 p., https://doi.org/10.3133/ofr71183.","productDescription":"20 p.","costCenters":[],"links":[{"id":335781,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0183/report.pdf","text":"Report","size":"12.08 Mb","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":169444,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0183/report-thumb.jpg"}],"country":"United States","state":"California","county":"Riverside County, San Bernadino County","otherGeospatial":"Bunker Hill-Yucaipa area, Chino-Riverside area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.8,\n              34.25\n            ],\n            [\n              -117.8,\n              34.25\n            ],\n            [\n              -117.8,\n              33.7\n            ],\n            [\n              -116.8,\n              33.7\n            ],\n            [\n              -116.8,\n              34.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcd08","contributors":{"authors":[{"text":"Lofgren, Ben Elder","contributorId":52973,"corporation":false,"usgs":true,"family":"Lofgren","given":"Ben","email":"","middleInitial":"Elder","affiliations":[],"preferred":false,"id":236568,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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