{"pageNumber":"1800","pageRowStart":"44975","pageSize":"25","recordCount":46619,"records":[{"id":3829,"text":"cir642 - 1971 - Streamflow, sediment-transport, and water-temperature characteristics of the three small watersheds in the Alsea River basin, Oregon","interactions":[],"lastModifiedDate":"2022-11-29T21:12:54.994564","indexId":"cir642","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"642","title":"Streamflow, sediment-transport, and water-temperature characteristics of the three small watersheds in the Alsea River basin, Oregon","docAbstract":"<p>Data collected during the prelogging period 1959-65 indicate an average annual runoff for Needle Branch and Deer and Flynn Creeks of 74.2, 75.1, and 77.7 inches, respectively. The measured precipitation at Flynn Creek of 92.9 inches was 5 inches less than at either Needle Branch or Deer Creek. Unit flood runoff during the prelogging period was found to be lowest on Flynn Creek and highest on Needle Branch. On Needle Branch, there appear to be two distinct low-flow patterns, one for a saturated and one for an unsaturated soil condition. The average annual sediment yield was highest on Flynn Creek, 321 tons per square mile, and lowest on Needle Branch, 166 tons per square mile. Maximum water temperatures were 62°F on Flynn Creek and 61°F on Needle Branch and Deer Creek.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir642","usgsCitation":"Harris, D.D., and Williams, R.C., 1971, Streamflow, sediment-transport, and water-temperature characteristics of the three small watersheds in the Alsea River basin, Oregon: U.S. Geological Survey Circular 642, v, 21 p., https://doi.org/10.3133/cir642.","productDescription":"v, 21 p.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":30900,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1971/0642/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409822,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23957.htm","linkFileType":{"id":5,"text":"html"}},{"id":124366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1971/0642/report-thumb.jpg"}],"country":"United States","state":"Oregon","otherGeospatial":"Alsea River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -123.833,\n              44.572\n            ],\n            [\n              -123.833,\n              44.528\n            ],\n            [\n              -123.9,\n              44.528\n            ],\n            [\n              -123.9,\n              44.572\n            ],\n            [\n              -123.833,\n              44.572\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4cc6","contributors":{"authors":[{"text":"Harris, David Dell","contributorId":24338,"corporation":false,"usgs":true,"family":"Harris","given":"David","email":"","middleInitial":"Dell","affiliations":[],"preferred":false,"id":147689,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Robert Charles","contributorId":35306,"corporation":false,"usgs":true,"family":"Williams","given":"Robert","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":147690,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4017,"text":"cir643 - 1971 - Reconnaissance of selected minor elements in surface waters of the United States, October 1970","interactions":[],"lastModifiedDate":"2018-02-16T16:17:21","indexId":"cir643","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"643","title":"Reconnaissance of selected minor elements in surface waters of the United States, October 1970","docAbstract":"<p>A nationwide reconnaissance of selected minor elements in water resources of the 50 States and Puerto Rico was made by the U.S. Geological Survey in cooperation with the U.S. Bureau of Sport Fisheries and Wildlife during autumn, 1970. Initiated in response to the growing need for data on minor elements in water, including toxic metals, the synoptic survey provides an up-to-date baseline of such data largely for dry-weather flows of streams that are sources of municipal and industrial water for the Nation's metropolitan areas.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir643","collaboration":"Prepared in cooperation with the U.S. Bureau of Sport Fisheries and Wildlife","usgsCitation":"Durum, W.H., Hem, J.D., and Heidel, S.G., 1971, Reconnaissance of selected minor elements in surface waters of the United States, October 1970: U.S. Geological Survey Circular 643, vi, 49 p., https://doi.org/10.3133/cir643.","productDescription":"vi, 49 p.","numberOfPages":"28","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science 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H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":147990,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hem, John David","contributorId":42577,"corporation":false,"usgs":true,"family":"Hem","given":"John","email":"","middleInitial":"David","affiliations":[],"preferred":false,"id":147989,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heidel, Sumner Griggs","contributorId":97082,"corporation":false,"usgs":true,"family":"Heidel","given":"Sumner","email":"","middleInitial":"Griggs","affiliations":[],"preferred":false,"id":147991,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4068,"text":"cir460D - 1971 - The national hydrologic bench-mark network","interactions":[],"lastModifiedDate":"2012-02-02T00:05:27","indexId":"cir460D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"460","chapter":"D","title":"The national hydrologic bench-mark network","docAbstract":"The United States is undergoing a dramatic growth of population and demands on its natural resources. The effects are widespread and often produce significant alterations of the environment. The hydrologic bench-mark network was established to provide data on stream basins which are little affected by these changes. The network is made up of selected stream basins which are not expected to be significantly altered by man. Data obtained from these basins can be used to document natural changes in hydrologic characteristics with time, to provide a better understanding of the hydrologic structure of natural basins, and to provide a comparative base for studying the effects of man on the hydrologic environment. \r\n\r\nThere are 57 bench-mark basins in 37 States. These basins are in areas having a wide variety of climate and topography. The bench-mark basins and the types of data collected in the basins are described.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir460D","usgsCitation":"Cobb, E.D., and Biesecker, J., 1971, The national hydrologic bench-mark network: U.S. Geological Survey Circular 460, iv, 38 p. :ill., map ;26 cm., https://doi.org/10.3133/cir460D.","productDescription":"iv, 38 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":120873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1971/0460d/report-thumb.jpg"},{"id":31163,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1971/0460d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a064","contributors":{"authors":[{"text":"Cobb, Ernest D.","contributorId":25139,"corporation":false,"usgs":true,"family":"Cobb","given":"Ernest","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":148114,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Biesecker, J.E.","contributorId":103257,"corporation":false,"usgs":true,"family":"Biesecker","given":"J.E.","affiliations":[],"preferred":false,"id":148115,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6236,"text":"pp701A - 1971 - Hydrology of two small river basins in Pennsylvania before urbanization, with a section on observation of stream fauna","interactions":[],"lastModifiedDate":"2017-07-07T09:08:31","indexId":"pp701A","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":"701","chapter":"A","title":"Hydrology of two small river basins in Pennsylvania before urbanization, with a section on observation of stream fauna","docAbstract":"<p>Basic data on water quantity, chemical quality, and suspended sediment are tabulated to record the conditions existing in two basins near Philadelphia, each about 32 square miles in area. The basins in 1970 are agricultural land for the most part, but urban and industrial development is imminent as the Philadelphia metropolitan area expands. Hopefully, as changes caused by urbanization occur in future years, data published herein will be useful as a base for comparison. </p><p>Pickering Creek basin has a higher population than the upper East Branch Brandywine Creek basin. The two are comparable in discharge characteristics and in shapes and sizes of channels, but the Pickering Creek basin is producing a considerably larger suspended-sediment load. Also the effects of urbanization are discernible in some chemical parameters. </p><p>During the study, a small subbasin, one-half square mile in area, was converted from agricultural use to an industrial park. This change resulted in a marked increase in sulfates, nitrates, chlorides, and dissolved solids in the streamflow. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp701A","usgsCitation":"Miller, R.A., Troxell, J., Leopold, L.B., Patrick, R., and Grant, R.R., 1971, Hydrology of two small river basins in Pennsylvania before urbanization, with a section on observation of stream fauna: U.S. Geological Survey Professional Paper 701, iv, 57 p., https://doi.org/10.3133/pp701A.","productDescription":"iv, 57 p.","numberOfPages":"68","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":117927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0701a/report-thumb.jpg"},{"id":33442,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0701a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Upper East Branch Brandywine Creek, Pickering Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -75.89355468749999,\n              39.96870074491696\n            ],\n            [\n              -75.45135498046875,\n              39.96870074491696\n            ],\n            [\n              -75.45135498046875,\n              40.16418235037417\n            ],\n            [\n              -75.89355468749999,\n              40.16418235037417\n            ],\n            [\n              -75.89355468749999,\n              39.96870074491696\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc7cc","contributors":{"authors":[{"text":"Miller, R. Adam","contributorId":21540,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"Adam","affiliations":[],"preferred":false,"id":152357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Troxell, John","contributorId":83517,"corporation":false,"usgs":true,"family":"Troxell","given":"John","email":"","affiliations":[],"preferred":false,"id":152359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":152360,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Patrick, Ruth","contributorId":95055,"corporation":false,"usgs":true,"family":"Patrick","given":"Ruth","email":"","affiliations":[],"preferred":false,"id":152361,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Grant, Robert R. Jr.","contributorId":75524,"corporation":false,"usgs":true,"family":"Grant","given":"Robert","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152358,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":4253,"text":"cir647 - 1971 - Classification of public lands valuable for geothermal steam and associated geothermal resources","interactions":[],"lastModifiedDate":"2012-02-02T00:05:37","indexId":"cir647","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"647","title":"Classification of public lands valuable for geothermal steam and associated geothermal resources","docAbstract":"The Organic Act of 1879 (43 U.S.C. 31) that established the U.S. Geological Survey provided, among other things, for the classification of the public lands and for the examination of the geological structure, mineral sources, and products of the national domain. In order to provide uniform executive action in classifying public lands, standards for determining which lands are valuable for mineral resources, for example, leasable mineral lands, or for other products are prepared by the U.S. Geological Survey. This report presents the classification standards for determining which Federal lands are classifiable as geothermal steam and associated geothermal resources lands under the Geothermal Steam Act of 1970 (84 Star. 1566). \r\n\r\nThe concept of a geothermal resources province is established for classification of lands for the purpose of retention in Federal ownership of rights to geothermal resources upon disposal of Federal lands. A geothermal resources province is defined as an area in which higher than normal temperatures are likely to occur with depth and in which there is a reasonable possibility of finding reservoir rocks that will yield steam or heated fluids to wells. \r\n\r\nThe determination of a 'known geothermal resources area' is made after careful evaluation of the available geologic, geochemical, and geophysical data and any evidence derived from nearby discoveries, competitive interests, and other indicia. The initial classification required by the Geothermal Steam Act of 1970 is presented.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir647","usgsCitation":"Godwin, L.H., Haigler, L.B., Rioux, R., White, D., Muffler, L., and Wayland, R.G., 1971, Classification of public lands valuable for geothermal steam and associated geothermal resources: U.S. Geological Survey Circular 647, iii, 18 p. :maps ;26 cm., https://doi.org/10.3133/cir647.","productDescription":"iii, 18 p. :maps ;26 cm.","costCenters":[],"links":[{"id":122505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1971/0647/report-thumb.jpg"},{"id":31366,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1971/0647/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b46fa","contributors":{"authors":[{"text":"Godwin, Larry H.","contributorId":57446,"corporation":false,"usgs":true,"family":"Godwin","given":"Larry","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":148571,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haigler, L. B.","contributorId":71533,"corporation":false,"usgs":true,"family":"Haigler","given":"L.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":148572,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rioux, R.L.","contributorId":36541,"corporation":false,"usgs":true,"family":"Rioux","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":148569,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"White, D. E.","contributorId":20729,"corporation":false,"usgs":false,"family":"White","given":"D. E.","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":148568,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Muffler, L.J.","contributorId":54188,"corporation":false,"usgs":true,"family":"Muffler","given":"L.J.","affiliations":[],"preferred":false,"id":148570,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Wayland, R. G.","contributorId":12027,"corporation":false,"usgs":true,"family":"Wayland","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":148567,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":6197,"text":"pp715A - 1971 - Combined Ice and Water Balances of Gulkana and Wolverine Glaciers, Alaska, and South Cascade Glacier, Washington, 1965 and 1966 Hydrologic Years","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"pp715A","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":"715","chapter":"A","title":"Combined Ice and Water Balances of Gulkana and Wolverine Glaciers, Alaska, and South Cascade Glacier, Washington, 1965 and 1966 Hydrologic Years","docAbstract":"Glaciers occur in northwestern North America between lat 37 deg and 69 deg N. in two major mountain systems. The Pacific Mountain System, near the west coast, receives large amounts of precipitation, has very mild temperatures, and contains perhaps 90 percent of the glacier ice. The Rocky Mountain or Eastern System, on the other hand, receives nearly an order of magnitude less precipitation, has temperatures that range from subpolar to subtropic, and contains glaciers that are much smaller in both size and total area.\r\n\r\nAs a contribution to the International Hydrological Decade program on combined balances at selected glaciers, the U.S. Geological Survey is conducting studies of ice and water balance on four glaciers in the Pacific Mountain System: Wolverine and Gulkana Glaciers in Alaska, South Cascade Glacier in Washington, and Maclure Glacier in California. Similar data are being collected by other organizations at five glaciers in western Canada, including two in the Rocky Mountain System, and at one glacier in the Rocky Mountain System in northern Alaska.\r\n\r\nGulkana, Wolverine, South Cascade, and Maclure Glaciers have dissimilar mass balances, and each is fairly representative of the glaciers for its particular region. Gulkana Glacier (lat 63 deg 15' N., Alaska Range, Alaska) normally has an equilibrium line at an altitude of 1,800 m (meters), an activity index of about 6 mm/m (millimeters per meter), a winter balance of about 1.0 m, and an annual exchange of about 2.2 m. (Balance values are given in terms of water-equivalent measure; the winter balance of 1 m, for example, indicates a volume of ice equal in mass to a volume of water 1 m in depth covering the area of the glacier.) The normal approximate parameters for the other glaciers studied are as follows: Wolverine Glacier (lat 60 deg 24' N., Kenai Mountains, Alaska) - equilibrium-line altitude 1,200 m, activity index 9 mm/m, winter balance 2.5 m, and annual exchange 5.5 m; South Cascade Glacier (lat 48 deg 22' N., North Cascades, Wash.) - equilibrium-line altitude 1,900 m, activity index 17 mm/m, winter balance 3.1 m, and annual exchange 6.6 m; and Maclure Glacier (lat 37 deg 45' N., Sierra Nevada, Calif.) - equilibrium-line altitude 3,600 m, activity index 23 mm/m, winter balance 2.3 m, and annual exchange 4.6 m.\r\n\r\nMass balances of these four glaciers and their drainage basins are measured annually by standard glaciological techniques. In addition, the hydrologic balance is calculated using streamflow and precipitation measurements. Combining these independent measurements results in fairly well defined values of water and ice balance for the glaciers and drainage basins. A revision of the standard International Hydrological Decade mass-balance system permits combination of annual and stratigraphic terms.\r\n\r\nThe annual balance of South Cascade Glacier at the end of the 1965 hydrologic year was slightly positive (+0.07 m averaged over the glacier), but continued ablation and deficient accumulation in October 1965 resulted in slightly negative net balances for both the glacier and the drainage basin. Factors tending to produce this near-zero balance were the above-average late-winter balance (3.48 m) and the numerous summer snowfalls. Ice ablation averaged about 39 mm of water per day during the main melt season. Runoff during the summer ablation season was lower than the 1958-64 average.\r\n\r\nThe South Cascade Glacier annual balance in 1966 (-0.94 m) was considerably more negative mainly owing to the deficient winter snowpack (the late-winter balance was only 2.52 m) and the warm dry summer. Ice ablation averaged about 44 mm of water per day during the melt season. The loss in storage of this and other glaciers in the North Cascades increased the runoff of many valley streams by approximately 50 percent during August and September.\r\n\r\nThe 1966 Gulkana Glacier annual balance was slightly positive (+0.06 m); on the basis of past observations and the rapid terminus ret","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/pp715A","collaboration":"A contribution to the International Hydrological Decade","usgsCitation":"Meier, M.F., Tangborn, W.V., Mayo, L.R., and Post, A., 1971, Combined Ice and Water Balances of Gulkana and Wolverine Glaciers, Alaska, and South Cascade Glacier, Washington, 1965 and 1966 Hydrologic Years: U.S. Geological Survey Professional Paper 715, 22 p., https://doi.org/10.3133/pp715A.","productDescription":"22 p.","temporalStart":"1964-10-01","temporalEnd":"1966-09-30","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":140787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0715a/report-thumb.jpg"},{"id":12506,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/715-A/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":33352,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33353,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33354,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33355,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33356,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33357,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0715a/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33358,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0715a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae731","contributors":{"authors":[{"text":"Meier, Mark Frederick","contributorId":30982,"corporation":false,"usgs":true,"family":"Meier","given":"Mark","email":"","middleInitial":"Frederick","affiliations":[],"preferred":false,"id":152278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tangborn, Wendell V.","contributorId":32152,"corporation":false,"usgs":true,"family":"Tangborn","given":"Wendell","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":152279,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mayo, Lawrence R.","contributorId":98344,"corporation":false,"usgs":true,"family":"Mayo","given":"Lawrence","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152281,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":152280,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":4319,"text":"cir663 - 1971 - Index of surface-water records to September 30, 1970: Part 13. - Snake River basin","interactions":[{"subject":{"id":3997,"text":"cir583 - 1968 - Index of surface-water records to September 30, 1967: Part 13. - Snake River basin","indexId":"cir583","publicationYear":"1968","noYear":false,"title":"Index of surface-water records to September 30, 1967: Part 13. - Snake River basin"},"predicate":"SUPERSEDED_BY","object":{"id":4319,"text":"cir663 - 1971 - Index of surface-water records to September 30, 1970: Part 13. - Snake River basin","indexId":"cir663","publicationYear":"1971","noYear":false,"title":"Index of surface-water records to September 30, 1970: Part 13. - Snake River basin"},"id":1}],"lastModifiedDate":"2017-02-21T17:12:31","indexId":"cir663","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"663","title":"Index of surface-water records to September 30, 1970: Part 13. - Snake River basin","docAbstract":"<p>This report lists the streamflow and reservoir stations in the Snake River basin for which records have been or are to be published in reports of the Geological Survey for periods through September 30, 1970. It supersedes Geological Survey Circular 583. It was updated by personnel of the Data Response Unit, Water Resources Division, Geological Survey. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir663","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Index of surface-water records to September 30, 1970: Part 13. - Snake River basin: U.S. Geological Survey Circular 663, 29 p., https://doi.org/10.3133/cir663.","productDescription":"29 p.","numberOfPages":"34","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":31429,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1971/0663/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122508,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1971/0663/report-thumb.jpg"}],"country":"United States","state":"Idaho, Nevada, Oregon, Utah, Washington, Wyoming","otherGeospatial":"Snake River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.76269531249999,\n              47.17477833929903\n            ],\n            [\n              -117.48779296875,\n              47.42808726171425\n            ],\n            [\n              -118.76220703125001,\n              47.32393057095941\n            ],\n            [\n              -119.42138671875,\n              46.830133640447386\n            ],\n            [\n              -119.35546875000001,\n              46.30140615437332\n            ],\n            [\n              -118.85009765625,\n              46.13417004624326\n            ],\n            [\n              -119.02587890624999,\n              45.598665689820635\n            ],\n            [\n              -119.70703125,\n              45.120052841530544\n            ],\n            [\n              -119.94873046875,\n              44.33956524809713\n            ],\n            [\n              -117.31201171875001,\n              42.08191667830631\n            ],\n            [\n              -115.53222656249999,\n              41.72213058512578\n            ],\n            [\n              -114.49951171875,\n              41.393294288784865\n            ],\n            [\n              -113.00537109375,\n              41.82045509614034\n            ],\n            [\n              -112.17041015625,\n              41.85319643776675\n            ],\n            [\n              -111.57714843749999,\n              42.50450285299051\n            ],\n            [\n              -110.89599609375,\n              42.47209690919285\n            ],\n            [\n              -110.302734375,\n              42.32606244456202\n            ],\n            [\n              -109.9072265625,\n              42.87596410238256\n            ],\n            [\n              -110.25878906249999,\n              44.276671273775186\n            ],\n            [\n              -111.37939453125,\n              44.87144275016589\n            ],\n            [\n              -112.08251953125,\n              44.94924926661153\n            ],\n            [\n              -113.92822265625,\n              45.82879925192134\n            ],\n            [\n              -114.23583984374999,\n              46.31658418182218\n            ],\n            [\n              -114.32373046875,\n              46.694667307773116\n            ],\n            [\n              -114.7412109375,\n              46.92025531537451\n            ],\n            [\n              -116.27929687499999,\n              47.249406957888446\n            ],\n            [\n              -116.76269531249999,\n              47.17477833929903\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f8e4b07f02db5f2c2e","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":528181,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4665,"text":"twri05A2 - 1971 - Determination of minor elements in water by emission spectroscopy","interactions":[],"lastModifiedDate":"2021-05-28T18:22:21.899438","indexId":"twri05A2","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"05-A2","title":"Determination of minor elements in water by emission spectroscopy","docAbstract":"With the emission spectrograph, the analyst is able to determine many minor elements simultaneously in water samples. Spectrographic methods differ chiefly in techniques of preconcentrating the elements. For waters with dissolved solids of less than 1,000 milligrams per liter, the method of evaporating to dryness and determining the elements in the dried residue is sensitive, precise, and reasonably accurate. The lower limits of detection vary with the quantity of dissolved solids. Twenty-four elements are determined by this method.\r\nFor waters with more than 1,000 milligrams per liter of dissolved solids, it is necessary to separate the minor elements from the major constituents before spectrographically determining the former, in order to achieve adequate lower limits of detection. Such procedures generally require more time than the residue method. In the first of two such procedures given, 21 of the metallic elements are precipitated with thioacetamide prior to spectrographic determination. In an alternate procedure, 18 elements are precipitated quantitatively with complexing reagents 8-hydroxyquinoline, tannic acid, and thioanlide. This method is faster than the thioacetamide method, but at the sacrifice of some elements. A Fortran IV computer program for processing densitometric data is given in the section 'Computer Program.'","language":"English","publisher":"U.S. Govt. Print. Off., For sale by the Superintendent of Documents,","doi":"10.3133/twri05A2","usgsCitation":"Barnett, P.R., and Mallory, E.C., 1971, Determination of minor elements in water by emission spectroscopy: U.S. Geological Survey Techniques of Water-Resources Investigations 05-A2, v, 31 p., https://doi.org/10.3133/twri05A2.","productDescription":"v, 31 p.","costCenters":[{"id":452,"text":"National Water Quality Laboratory","active":true,"usgs":true}],"links":[{"id":139511,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":191,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri5a2/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675a4","contributors":{"authors":[{"text":"Barnett, Paul R.","contributorId":29801,"corporation":false,"usgs":true,"family":"Barnett","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":149587,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mallory, E. C.","contributorId":90700,"corporation":false,"usgs":true,"family":"Mallory","given":"E.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":149588,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5839,"text":"pp732A - 1971 - Channel movement of meandering Indiana streams","interactions":[],"lastModifiedDate":"2016-05-13T10:41:13","indexId":"pp732A","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":"732","chapter":"A","title":"Channel movement of meandering Indiana streams","docAbstract":"<p>The process of channel movement in a meander system involves rotation and translation of meander loops and an increasing path length. The amount of path-length increase is directly proportional to the impulse supplied by discharge and is inversely proportional to the silt-clay percentage of the material composing the channel perimeter.</p>\n<p>Comparable paths have been obtained by standardizing measurements with a sine-generated curve and a moving reference axis. Analysis of previous investigations and time-of-travel data indicates that the discharge effective in channel formation consists of the range beginning just higher than the average and continuing throughout all higher discharges. Of six field sites investigated, three meander systems had path-length increases of sufficient magnitude to correlate with above-average discharge volume, one had no discernible change over a 30-year period, and two had changes which were too small for correlation owing to the short period of time covered by the available data.</p>\n<p>Because of the consistency of yearly above-average discharge volumes, it was possible to develop a general relation between path-length increase per thousand cubic-feet-per-second-days per square mile of drainage area above average discharge and the width-depth ratio of the channel. Little progress was made toward defining relationships for rotation and translation.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp732A","collaboration":"State of Indiana Department of  Natural Resources","usgsCitation":"Daniel, J.F., 1971, Channel movement of meandering Indiana streams: U.S. Geological Survey Professional Paper 732, 17 p., https://doi.org/10.3133/pp732A.","productDescription":"17 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":32598,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0732a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0732a/report-thumb.jpg"}],"country":"United 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,{"id":4720,"text":"twri03B1 - 1971 - Aquifer-test design, observation, and data analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"twri03B1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"03-B1","title":"Aquifer-test design, observation, and data analysis","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/twri03B1","issn":"0565-596X","usgsCitation":"Stallman, R., 1971, Aquifer-test design, observation, and data analysis: U.S. Geological Survey Techniques of Water-Resources Investigations 03-B1, v, 26 p. :ill. ;26 cm. Reprinted in 1983., https://doi.org/10.3133/twri03B1.","productDescription":"v, 26 p. :ill. ;26 cm. Reprinted in 1983.","costCenters":[],"links":[{"id":139091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":348,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri3-b1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679e8d","contributors":{"authors":[{"text":"Stallman, Robert W.","contributorId":32903,"corporation":false,"usgs":true,"family":"Stallman","given":"Robert W.","affiliations":[],"preferred":false,"id":149676,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2179,"text":"wsp1532D - 1971 - Effects of Grazing on the Hydrology and Biology of the Badger Wash Basin in Western Colorado, 1953-66","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1532D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1532","chapter":"D","title":"Effects of Grazing on the Hydrology and Biology of the Badger Wash Basin in Western Colorado, 1953-66","docAbstract":"An intensive study of the effect of grazing on the hydrologic and biotic characteristics of small drainage basins on the Colorado Plateau was begun in the fall of 1953. This report presents data obtained during the first 13 years of the proposed 20-year study. \r\n\r\nFor the period of record 1954-66, runoff from grazed watersheds has averaged about 33 acre-feet per square mile per year. Runoff from ungrazed watersheds averaged from 71 to 76 percent of that from grazed watersheds. During the last 6 years of the period, however, ungrazed watersheds produced 69 to 71 percent as much runoff as grazed watersheds. The sediment yield frown grazed watersheds during the same period was about 3 acre-feet per square mile per year. Sediment yield from ungrazed watersheds ranged from 51 to 75 percent of that from grazed watersheds and averaged 66 percent. The largest change in these relations occurred about 2 years after livestock were excluded from certain watersheds. The causative factors for changes in the runoff and sediment yield relations are not entirely clear. At the end of 13 years, a significant change had occurred in the amount of bare soil and rock. in the ground-cover index, and in the litter and moss on the grazed watersheds. These items remained essentially unchanged on ungrazed watersheds. The changes in ground-cover factors were not of large magnitude and did not occur at the same rate as the changes in runoff and sediment yield. A large part of the difference appears to have been caused by a change in the structure of surface soil. which was brought about by the elimination of trampling by livestock. \r\n\r\nDeer mice were the most common rodent present on the experimental watersheds, but even their population was not great enough to affect the composition of range vegetation. Deer mice populations remained comparable on grazed and ungrazed watersheds during the study. Other rodents were not present in sufficient numbers to allow their comparison on grazed and ungrazed range. Desert cottontail rabbits and black-tailed jackrabbits were more plentiful in ungrazed watersheds but were not present in large enough numbers to affect range vegetation.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1532D","usgsCitation":"Lusby, G.C., and Knipe, O., 1971, Effects of Grazing on the Hydrology and Biology of the Badger Wash Basin in Western Colorado, 1953-66: U.S. Geological Survey Water Supply Paper 1532, v, 90 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1532D.","productDescription":"v, 90 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":109968,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24708.htm","linkFileType":{"id":5,"text":"html"},"description":"24708"},{"id":138202,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532d/report-thumb.jpg"},{"id":27799,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1532d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27800,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cfe4b07f02db5460de","contributors":{"authors":[{"text":"Lusby, Gregg C.","contributorId":68290,"corporation":false,"usgs":true,"family":"Lusby","given":"Gregg","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144778,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knipe, O.D.","contributorId":90158,"corporation":false,"usgs":true,"family":"Knipe","given":"O.D.","email":"","affiliations":[],"preferred":false,"id":144779,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1339,"text":"wsp1893 - 1971 - Potential development and recharge of ground water in Mill Creek Valley, Butler and Hamilton Counties, Ohio, based on analog model analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp1893","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1893","title":"Potential development and recharge of ground water in Mill Creek Valley, Butler and Hamilton Counties, Ohio, based on analog model analysis","docAbstract":"Mill Creek valley is part of the greater Cincinnati industrial area in southwestern Ohio. In 1964, nearly 30 percent of the water supply in the study area of about 27 square miles was obtained from wells in the glacial-outwash aquifer underlying the valley. Ground-water demand has increased steadily since the late 1800's, and excessive pumpage during the years of World War II caused water levels to decline to critical levels. Natural recharge to the aquifer, from precipitation, is about 8.5 mgd (million gallons per day). In 1964, the total water use was about 30 mgd, of which 8.1 mgd was obtained from wells in Mill Creek valley, and the remainder was imported from outside the basin. With rapid industrial expansion and population growth, demand for ground water is continuing to increase. By the year 2000 ground-water pumpage is expected to exceed 25 mgd. \r\n\r\nAt a public hearing before the Ohio Water Commission in 1961, artificial recharge of the aquifer through injection wells was proposed as a possible solution to the Mill Creek valley water-supply problem. The present study attempts to determine the feasibility of injection-well recharge systems in the Mill Creek valley. \r\n\r\nAlthough basically simple, the hydrologic system in Mill Creek valley is complex in detail and is difficult to evaluate using conventional quantitative methods. Because of this complexity, an electric analog model was used to test specific development plans. \r\n\r\nThree hypothetical pumping plans were developed by projecting past pumpage data to the years 1980 and 2000. Various combinations of injection wells were tested on the model under different hypothetical conditions of pumpage. Based on analog model analysis, from three to eight inject-ion wells, with an approximate input of 2 mgd each, would reverse the trend in declining groundwater levels and provide adequate water to meet anticipated future demands.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1893","usgsCitation":"Fidler, R.E., 1971, Potential development and recharge of ground water in Mill Creek Valley, Butler and Hamilton Counties, Ohio, based on analog model analysis: U.S. Geological Survey Water Supply Paper 1893, iv, 37 p. :illus., maps. ;23 cm., https://doi.org/10.3133/wsp1893.","productDescription":"iv, 37 p. :illus., maps. ;23 cm.","costCenters":[],"links":[{"id":110030,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25110.htm","linkFileType":{"id":5,"text":"html"},"description":"25110"},{"id":137426,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1893/report-thumb.jpg"},{"id":26399,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1893/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26400,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1893/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26401,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1893/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26402,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1893/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26403,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1893/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6838f1","contributors":{"authors":[{"text":"Fidler, Richard E.","contributorId":86313,"corporation":false,"usgs":true,"family":"Fidler","given":"Richard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143591,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47952,"text":"ofr71193 - 1971 - Geohydrologic sections, Cache Valley, Utah and Idaho","interactions":[],"lastModifiedDate":"2017-09-04T12:23:14","indexId":"ofr71193","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":"71-193","title":"Geohydrologic sections, Cache Valley, Utah and Idaho","docAbstract":"<p>This report was prepared as a part of a study of the ground-water resources of Cache Valley, Utah and Idaho. The study by the U.S. Geo- logical Survey was made during 1967-70 in cooperation with the Utah Department of Natural Resources, Division of Water Rights. The U.S. Bureau of Reclamation and the U.S. Soil Conservation Service cooperated by providing services; and counties, cities, irrigation districts, and some local organizations and businesses in both Utah and Idaho cooperated financially through the Utah Department of Natural Resources. In addition to this report, results of the study are presented in a basic-data release (McGreevy and Bjorklund, 1970) and in an interpretive report in preparation.</p><p>Geologic and hydrologic data are combined and presented on a series of cross sections. Geologic contacts and faults or fault zones are based on indicated well logs, on the geologic map in the interpretive report (in preparation) , and on gravity data by Peterson and Oriel (1970).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr71193","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"McGreevy, L.J., and Bjorklund, L., 1971, Geohydrologic sections, Cache Valley, Utah and Idaho: U.S. Geological Survey Open-File Report 71-193, Report: 9 p.; 13 Figures: 28.17 in. x 12.86 in. or smaller; 2 Plates: 7.62 in. x 18.16 in. and 16.09 in. x 15.66 in., https://doi.org/10.3133/ofr71193.","productDescription":"Report: 9 p.; 13 Figures: 28.17 in. x 12.86 in. or smaller; 2 Plates: 7.62 in. x 18.16 in. and 16.09 in. x 15.66 in.","numberOfPages":"11","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":84756,"rank":409,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-10.pdf","text":"Figure 10","linkFileType":{"id":1,"text":"pdf"}},{"id":84757,"rank":410,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-11.pdf","text":"Figure 11","linkFileType":{"id":1,"text":"pdf"}},{"id":84758,"rank":411,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-12.pdf","text":"Figure 13","linkFileType":{"id":1,"text":"pdf"}},{"id":84759,"rank":412,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-13.pdf","text":"Figure 14","linkFileType":{"id":1,"text":"pdf"}},{"id":84760,"rank":413,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-14.pdf","text":"Figure 15","linkFileType":{"id":1,"text":"pdf"}},{"id":84761,"rank":414,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-15.pdf","text":"Figure 16","linkFileType":{"id":1,"text":"pdf"}},{"id":84762,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0193/report.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Report, including Figures 7, 8, and 12"},{"id":170185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0193/report-thumb.jpg"},{"id":84747,"rank":400,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-01.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":84752,"rank":405,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-06.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":84753,"rank":406,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-07.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":84754,"rank":407,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-08.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}},{"id":84755,"rank":408,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-09.pdf","text":"Figure 9","linkFileType":{"id":1,"text":"pdf"}},{"id":84748,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-02.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Cache Valley, Utah and Idaho, showing locaitons of sections."},{"id":84749,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-03.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Explanation of figures"},{"id":84750,"rank":403,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-04.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":84751,"rank":404,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1971/0193/plate-05.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho, Utah","otherGeospatial":"Cache Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8ec8","contributors":{"authors":[{"text":"McGreevy, L. J.","contributorId":108124,"corporation":false,"usgs":true,"family":"McGreevy","given":"L.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":236575,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bjorklund, L.J.","contributorId":14035,"corporation":false,"usgs":true,"family":"Bjorklund","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":236574,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":47966,"text":"ofr71232 - 1971 - Annual compilation and analysis of hydrologic data for Escondido Creek, San Antonio River basin, Texas, 1969","interactions":[],"lastModifiedDate":"2017-06-14T16:24:09","indexId":"ofr71232","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":"71-232","title":"Annual compilation and analysis of hydrologic data for Escondido Creek, San Antonio River basin, Texas, 1969","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71232","usgsCitation":"Reddy, D., 1971, Annual compilation and analysis of hydrologic data for Escondido Creek, San Antonio River basin, Texas, 1969: U.S. Geological Survey Open-File Report 71-232, 62 p., https://doi.org/10.3133/ofr71232.","productDescription":"62 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":170090,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bc07","contributors":{"authors":[{"text":"Reddy, D.R.","contributorId":14027,"corporation":false,"usgs":true,"family":"Reddy","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":236597,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47967,"text":"ofr71234 - 1971 - Effects of roadway and pond construction on sediment yield near Harrisburg, Pennsylvania","interactions":[],"lastModifiedDate":"2016-10-21T10:58:14","indexId":"ofr71234","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":"71-234","title":"Effects of roadway and pond construction on sediment yield near Harrisburg, Pennsylvania","docAbstract":"<p>This report shows the effects that the construction of half a mile of one-lane roadway during June, July, and August 1970 and construction of a 5-acre pond during August and September 1970, had on sediment concentrations and sediment discharge of a stream draining an area of 0.76 square mile. The effects of the construction are shown by comparing the data collected from the affected basin with data collected from a similar adjacent basin, unaffected by construction.</p><p>During the pond construction, base-flow sediment concentrations increased from the expected 6 mg/1 (milligrams per liter) to an average of 35 mg/l. Sediment discharge during June through December 1970 attributable to the construction was 55 tons, two-thirds of the amount normally expected during a year.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/ofr71234","usgsCitation":"Reed, L.A., 1971, Effects of roadway and pond construction on sediment yield near Harrisburg, Pennsylvania: U.S. Geological Survey Open-File Report 71-234, iii, 14 p., https://doi.org/10.3133/ofr71234.","productDescription":"iii, 14 p.","numberOfPages":"21","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":170091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":330312,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0234/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","city":"Harrisburg","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.99785232543945,\n              40.28725188869884\n            ],\n            [\n              -76.99785232543945,\n              40.315726511613626\n            ],\n            [\n              -76.94609642028809,\n              40.315726511613626\n            ],\n            [\n              -76.94609642028809,\n              40.28725188869884\n            ],\n            [\n              -76.99785232543945,\n              40.28725188869884\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611982","contributors":{"authors":[{"text":"Reed, Lloyd A.","contributorId":79861,"corporation":false,"usgs":true,"family":"Reed","given":"Lloyd","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":236598,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47970,"text":"ofr71240 - 1971 - Annual compilation and analysis of hydrologic data for urban studies in the Austin, Texas metropolitan area, 1969","interactions":[],"lastModifiedDate":"2017-06-14T16:10:20","indexId":"ofr71240","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":"71-240","title":"Annual compilation and analysis of hydrologic data for urban studies in the Austin, Texas metropolitan area, 1969","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71240","usgsCitation":"Robbins, W., 1971, Annual compilation and analysis of hydrologic data for urban studies in the Austin, Texas metropolitan area, 1969: U.S. Geological Survey Open-File Report 71-240, 46 p., https://doi.org/10.3133/ofr71240.","productDescription":"46 p.","costCenters":[],"links":[{"id":170094,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Texas","city":"Austin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              29.991812888666043\n            ],\n            [\n              -97.38006591796874,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              30.615459280672667\n            ],\n            [\n              -98.09280395507812,\n              29.991812888666043\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bc7c","contributors":{"authors":[{"text":"Robbins, W.D.","contributorId":72852,"corporation":false,"usgs":true,"family":"Robbins","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":236601,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47910,"text":"ofr715 - 1971 - Electrical analog model study of water in the Yabucoa Valley, Puerto Rico; Phase 1, collecting preliminary data and assembling available data","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"ofr715","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":"71-5","title":"Electrical analog model study of water in the Yabucoa Valley, Puerto Rico; Phase 1, collecting preliminary data and assembling available data","language":"ENGLISH","doi":"10.3133/ofr715","usgsCitation":"Anders, R.B., 1971, Electrical analog model study of water in the Yabucoa Valley, Puerto Rico; Phase 1, collecting preliminary data and assembling available data: U.S. Geological Survey Open-File Report 71-5, 47 p. ill., maps ; 27 cm., https://doi.org/10.3133/ofr715.","productDescription":"47 p. ill., maps ; 27 cm.","costCenters":[],"links":[{"id":162825,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607293","contributors":{"authors":[{"text":"Anders, Robert B.","contributorId":44125,"corporation":false,"usgs":true,"family":"Anders","given":"Robert","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":236507,"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":"<p>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.</p><p>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.</p><p>Water in the lower zone is a sodium sulfate type and is fairly consistent throughout the zone. </p>","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":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":"<p>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.</p> \n<br>\n<p>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 &plusmn;0.6&deg;C of the mean water temperature at the 95-percent confidence level. The probable total error ranges from &plusmn;0.8&deg;C for periodic data to &plusmn;1.4&deg;C for thermograph data.</p>","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":"<p>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.</p>","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 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,{"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":"<p>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.</p>\n<p>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&deg; Celsius of ground-truth data.</p>\n<p>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.</p>","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":48005,"text":"ofr7211 - 1971 - Data for wells in the Modesto-Merced area, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2020-01-21T11:58:28","indexId":"ofr7211","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":"72-11","title":"Data for wells in the Modesto-Merced area, San Joaquin Valley, California","docAbstract":"<p>The Modesto-Merced area is in the northeastern part of the San Joaquin Valley. The area includes about 1,800 square miles that lie in the eastern portions of Merced and Stanislaus Counties. Specifically the boundaries are: North, the Stanislaus River; south, the Merced-Madera County line; east, the Merced-Mariposa and the Stanislaus-Tuolumne County lines; west, the San Joaquin River.</p><p>Between September 1970 and May 1971, 859 wells were selectively canvassed in the area. The resulting data are on file in the U.S. Geological Survey office at 2800 Cottage Way, Sacramento, Calif. Selected well data are tabulated in table 1, and the location of these wells is shown on maps 1-65. Selected chemical analyses are shown in table 2. Table 3 is a listing of the well numbers of all wells canvassed in the area by the U.S. Geological Survey through April 1971. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7211","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Balding, G.O., and Page, R.W., 1971, Data for wells in the Modesto-Merced area, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 72-11, iv, 122 p., https://doi.org/10.3133/ofr7211.","productDescription":"iv, 122 p.","costCenters":[],"links":[{"id":161984,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0011/report-thumb.jpg"},{"id":371414,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"San Joaquin Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db615a3d","contributors":{"authors":[{"text":"Balding, Gary O.","contributorId":25210,"corporation":false,"usgs":true,"family":"Balding","given":"Gary","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":236663,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":236662,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":49023,"text":"ofr7186 - 1971 - Electric analog model study of water in the Guayama area, Puerto Rico; Phase 1, Assembling data for the analog model","interactions":[],"lastModifiedDate":"2012-02-02T00:10:40","indexId":"ofr7186","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":"71-86","title":"Electric analog model study of water in the Guayama area, Puerto Rico; Phase 1, Assembling data for the analog model","language":"ENGLISH","doi":"10.3133/ofr7186","usgsCitation":"Diaz, J., 1971, Electric analog model study of water in the Guayama area, Puerto Rico; Phase 1, Assembling data for the analog model: U.S. Geological Survey Open-File Report 71-86, 68 p., https://doi.org/10.3133/ofr7186.","productDescription":"68 p.","costCenters":[],"links":[{"id":172987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60edf4","contributors":{"authors":[{"text":"Diaz, J.R.","contributorId":81170,"corporation":false,"usgs":true,"family":"Diaz","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":238852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":"<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>","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":47985,"text":"ofr71302 - 1971 - Compilation of hydrologic data, Honey Creek, Trinity River basin, Texas, 1968","interactions":[],"lastModifiedDate":"2021-12-23T17:02:37.554188","indexId":"ofr71302","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":"71-302","title":"Compilation of hydrologic data, Honey Creek, Trinity River basin, Texas, 1968","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71302","collaboration":"Prepared in cooperation with Texas Water Development Board and Soil Conservation Service","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1971, Compilation of hydrologic data, Honey Creek, Trinity River basin, Texas, 1968: U.S. Geological Survey Open-File Report 71-302, iv, 78 p., https://doi.org/10.3133/ofr71302.","productDescription":"iv, 78 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":393373,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0302/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":162679,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0302/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Honey Creek","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6a9e7f","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":531773,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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