{"pageNumber":"609","pageRowStart":"15200","pageSize":"25","recordCount":16498,"records":[{"id":23396,"text":"ofr72169 - 1971 - Geology, hydrology, and water quality of the Tracy-Dos Palos area, San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2017-04-14T09:09:16","indexId":"ofr72169","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":"72-169","title":"Geology, hydrology, and water quality of the Tracy-Dos Palos area, San Joaquin Valley, California","docAbstract":"

The Tracy-Dos Palos area includes about 1,800 square miles on the northwest side of the San Joaquin Valley. The Tulare Formation of Pliocene and Pleistocene age, terrace deposits of Pleistocene age, and alluvium and flood-basin deposits of Pleistocene and Holocene age constitute the fresh ground-water reservoir Pre-Tertiary and Tertiary sedimentary and crystalline rocks, undifferentiated, underlie the valley and yield saline water.

Hydrologically most important, the Tulare Formation is divided into a lower water-bearing zone confined by the Corcoran Clay Member and an upper zone that is confined, semiconfined, and unconfined in different parts of the area. Alluvium and flood-basin deposits are included in the upper zone. Surficial alluvium and flood-basin deposits contain a shallow water-bearing zone. Lower zone wells were flowing in 1908, but subsequent irrigation development caused head declines and land subsidence. Overdraft in both zones ended in 1951 with import of surface water.

Bicarbonate water flows into the area from the Sierra Nevada and Diablo Range. Diablo Range water is higher in sulfate, chloride, and dissolved solids. Upper zone water averages between 400 and 1,200 mg/l (milligrams per liter) dissolved solids and water hardness generally exceeds 180 mg/l as calcium carbonate. Nitrate, fluoride, iron, and boron occur in excessive concentrations in water from some wells. Dissolved constituents in lower zone water generally are sodium chloride and sodium sulfate with higher dissolved solids concentration than water from the upper zone.

The foothills of the Diablo Range provide favorable conditions for artificial recharge, but shallow water problems plague about 50 percent of the area and artificial recharge is undesirable at this time.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72169","issn":"0094-9140","usgsCitation":"Hotchkiss, W.R., and Balding, G., 1971, Geology, hydrology, and water quality of the Tracy-Dos Palos area, San Joaquin Valley, California: U.S. Geological Survey Open-File Report 72-169, Report: viii, 107 p.; 3 Plates: 33.24 x 31.14 inches or smaller, https://doi.org/10.3133/ofr72169.","productDescription":"Report: viii, 107 p.; 3 Plates: 33.24 x 31.14 inches or smaller","costCenters":[],"links":[{"id":156308,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0169/report-thumb.jpg"},{"id":52697,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0169/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52698,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0169/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52699,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0169/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52700,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0169/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c64e","contributors":{"authors":[{"text":"Hotchkiss, W. R.","contributorId":61820,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":190037,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Balding, G. O.","contributorId":87135,"corporation":false,"usgs":true,"family":"Balding","given":"G. O.","affiliations":[],"preferred":false,"id":190038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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":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":68043,"text":"ha392 - 1971 - Availability and quality of ground water in the Medford area, Jackson County, Oregon","interactions":[],"lastModifiedDate":"2017-02-03T13:26:48","indexId":"ha392","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"392","title":"Availability and quality of ground water in the Medford area, Jackson County, Oregon","language":"ENGLISH","doi":"10.3133/ha392","usgsCitation":"Robison, J.H., 1971, Availability and quality of ground water in the Medford area, Jackson County, Oregon: U.S. Geological Survey Hydrologic Atlas 392, 1 map on two sheets., https://doi.org/10.3133/ha392.","productDescription":"1 map on two sheets.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":187738,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89297,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/392/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89296,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/392/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,42.20138888888889 ], [ -123,42.5 ], [ -122.75,42.5 ], [ -122.75,42.20138888888889 ], [ -123,42.20138888888889 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6671d6","contributors":{"authors":[{"text":"Robison, J. H.","contributorId":60183,"corporation":false,"usgs":true,"family":"Robison","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277555,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67983,"text":"ha423 - 1971 - Flood of January 1969 near Ventura, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:27","indexId":"ha423","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"423","title":"Flood of January 1969 near Ventura, California","language":"ENGLISH","doi":"10.3133/ha423","usgsCitation":"Singer, J.A., and Price, M., 1971, Flood of January 1969 near Ventura, California: U.S. Geological Survey Hydrologic Atlas 423, 1map :col. ;76 x 100 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/ha423.","productDescription":"1map :col. ;76 x 100 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":186279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89221,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/423/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.33416666666666,34.266666666666666 ], [ -119.33416666666666,34.5 ], [ -119.16666666666667,34.5 ], [ -119.16666666666667,34.266666666666666 ], [ -119.33416666666666,34.266666666666666 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eee22","contributors":{"authors":[{"text":"Singer, John A.","contributorId":48976,"corporation":false,"usgs":true,"family":"Singer","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, McGlone","contributorId":42964,"corporation":false,"usgs":true,"family":"Price","given":"McGlone","email":"","affiliations":[],"preferred":false,"id":277449,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68426,"text":"ha414 - 1971 - Floods in the Guayanilla-Yauco area, Puerto Rico","interactions":[{"subject":{"id":70203695,"text":"70203695 - 1969 - Floods in the Guayanilla-Yauco area, Puerto Rico","indexId":"70203695","publicationYear":"1969","noYear":false,"title":"Floods in the Guayanilla-Yauco area, Puerto Rico"},"predicate":"SUPERSEDED_BY","object":{"id":68426,"text":"ha414 - 1971 - Floods in the Guayanilla-Yauco area, Puerto Rico","indexId":"ha414","publicationYear":"1971","noYear":false,"title":"Floods in the Guayanilla-Yauco area, Puerto Rico"},"id":1}],"lastModifiedDate":"2024-05-29T20:13:09.553174","indexId":"ha414","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"414","title":"Floods in the Guayanilla-Yauco area, Puerto Rico","docAbstract":"

This report is a compilation of data pertaining to floods in Rios Guayanilla and Yauco and is based principally upon information obtained from residents in the study area. This information is a useful tool in making land-use and development decisions.

The Guayanilla and Yauco basins lie in the southwestern part of Puerto Rico. The streams flow southward from the rugged Cordillera Central and empty into Bahia de Guayanilla. The lower basins are devoted principally to the production of sugarcane and are subject to destructive floods. Details pertaining to basin features, flood frequency, flood profiles, and inundated areas are discussed by individual basins. All elevations given are in meters above mean sea level.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha414","collaboration":"Prepared in cooperation with the Commonwealth of Puerto Rico Department of Public Works","usgsCitation":"Fields, F.K., 1971, Floods in the Guayanilla-Yauco area, Puerto Rico: U.S. Geological Survey Hydrologic Atlas 414, 1 Plate: 43.57 x 36.94 inches, https://doi.org/10.3133/ha414.","productDescription":"1 Plate: 43.57 x 36.94 inches","costCenters":[],"links":[{"id":89951,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/414/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":429364,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15798.htm","linkFileType":{"id":5,"text":"html"}},{"id":186613,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/414/report-thumb.jpg"}],"scale":"20000","datum":"Mean Sea Level","country":"United States","state":"Puerto Rico","otherGeospatial":"Guayanilla-Yauco area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -66.875,\n 17.93333333\n ],\n [\n -66.75,\n 17.93333333\n ],\n [\n -66.75,\n 18.05833333\n ],\n [\n -66.875,\n 18.05833333\n ],\n [\n -66.875,\n 17.93333333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e116f","contributors":{"authors":[{"text":"Fields, Fred K.","contributorId":69981,"corporation":false,"usgs":true,"family":"Fields","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278193,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68427,"text":"ha382 - 1971 - Floods in Yabucoa area, Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha382","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"382","title":"Floods in Yabucoa area, Puerto Rico","language":"ENGLISH","doi":"10.3133/ha382","usgsCitation":"Fields, F.K., 1971, Floods in Yabucoa area, Puerto Rico: U.S. Geological Survey Hydrologic Atlas 382, 1 map., https://doi.org/10.3133/ha382.","productDescription":"1 map.","costCenters":[],"links":[{"id":186614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89952,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/382/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"20000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -65.91666666666667,18.034166666666668 ], [ -65.91666666666667,18.083333333333332 ], [ -65.78416666666666,18.083333333333332 ], [ -65.78416666666666,18.034166666666668 ], [ -65.91666666666667,18.034166666666668 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dde4b07f02db5e1fe6","contributors":{"authors":[{"text":"Fields, Fred K.","contributorId":69981,"corporation":false,"usgs":true,"family":"Fields","given":"Fred","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278194,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68432,"text":"ha422 - 1971 - Flood of January 1969 near Carpinteria, California","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha422","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"422","title":"Flood of January 1969 near Carpinteria, California","language":"ENGLISH","doi":"10.3133/ha422","usgsCitation":"Fenzel, F.W., and Price, M., 1971, Flood of January 1969 near Carpinteria, California: U.S. Geological Survey Hydrologic Atlas 422, 1 map., https://doi.org/10.3133/ha422.","productDescription":"1 map.","costCenters":[],"links":[{"id":186680,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89958,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/422/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.55,34.3675 ], [ -119.55,34.416666666666664 ], [ -119.46666666666667,34.416666666666664 ], [ -119.46666666666667,34.3675 ], [ -119.55,34.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eef16","contributors":{"authors":[{"text":"Fenzel, Frank Walker","contributorId":101326,"corporation":false,"usgs":true,"family":"Fenzel","given":"Frank","email":"","middleInitial":"Walker","affiliations":[],"preferred":false,"id":278201,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Price, McGlone","contributorId":42964,"corporation":false,"usgs":true,"family":"Price","given":"McGlone","email":"","affiliations":[],"preferred":false,"id":278200,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":67948,"text":"ha361 - 1971 - Floods in Huntley Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:13","indexId":"ha361","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"361","title":"Floods in Huntley Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha361","usgsCitation":"Walter, G.L., and Mycyk, R.T., 1971, Floods in Huntley Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 361, 1 col. map ;58 x 43 cm., on sheet 80 x 110 cm., https://doi.org/10.3133/ha361.","productDescription":"1 col. map ;58 x 43 cm., on sheet 80 x 110 cm.","costCenters":[],"links":[{"id":190323,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89159,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/361/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.5,42.1175 ], [ -88.5,42.25 ], [ -88.36749999999999,42.25 ], [ -88.36749999999999,42.1175 ], [ -88.5,42.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e70ee","contributors":{"authors":[{"text":"Walter, Gerald L.","contributorId":59880,"corporation":false,"usgs":true,"family":"Walter","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277375,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mycyk, Roman T.","contributorId":58331,"corporation":false,"usgs":true,"family":"Mycyk","given":"Roman","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":277374,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68087,"text":"ha455 - 1971 - Glacier dammed lakes and outburst floods in Alaska","interactions":[],"lastModifiedDate":"2021-11-08T19:49:31.386944","indexId":"ha455","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"455","title":"Glacier dammed lakes and outburst floods in Alaska","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha455","usgsCitation":"Post, A., and Mayo, L., 1971, Glacier dammed lakes and outburst floods in Alaska: U.S. Geological Survey Hydrologic Atlas 455, Report: 10 p.; 3 Plates: 54.50 × 30.00 inches or smaller, https://doi.org/10.3133/ha455.","productDescription":"Report: 10 p.; 3 Plates: 54.50 × 30.00 inches or smaller","costCenters":[],"links":[{"id":91814,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/455/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91816,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/455/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":91815,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/455/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":185806,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/455/report-thumb.jpg"},{"id":391474,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15841.htm"},{"id":89347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/455/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -154,55.5 ], [ -154,64 ], [ -129.5,64 ], [ -129.5,55.5 ], [ -154,55.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679bca","contributors":{"authors":[{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":277620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mayo, L.R.","contributorId":21541,"corporation":false,"usgs":true,"family":"Mayo","given":"L.R.","email":"","affiliations":[],"preferred":false,"id":277619,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68444,"text":"ha357 - 1971 - Hydrogeology of the Pine Ridge Indian Reservation, South Dakota","interactions":[],"lastModifiedDate":"2017-10-15T12:38:32","indexId":"ha357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"357","title":"Hydrogeology of the Pine Ridge Indian Reservation, South Dakota","docAbstract":"

An investigation of the geology and ground-water resources of the Pine Ridge Indian Reservation, South Dakota, was made at the request of the Bureau of Indian Affairs as part of the U.S. Department of the Interior's program for the development of the Missouri River basin.  The area of investigation (about 3,930 square miles) includes all the land within the original boundaries of the Reservation, except for that part of Bennett County south of the U.S. Highway 18, where there are only small tracts of Indian land.

\n

Emphasis in the study was placed on mapping major rock units and on determining their potential as sources of water for domestic and stock use.  The geologic map on sheet 1 shows the areal extent of the major rock units, and a summary of the stratigraphy and physical characteristics of the exposed geologic formations is given in the table on this sheet.

\n

The writers appreciate the cooperation of the personnel of the South Dakota State Geological Survey, who provided most of the well data for Bennett County, information about the stratigraphy and geology of selected areas, and copies of published and unpublished geologic maps.  (See map showing areas mapped prior to this investigation.) Also, they appreciate the cooperation of ranch owners and tenants, who permitted access to their lands, and the personnel of the Bureau of Indian affairs, who supplied soils mps and other data.

\n

Data on which this report is based, including logs of wells and test holes, chemical analyses of water and records of wells and springs, have been summarized by the authors in a basic-data report published jointly by the South Dakota Geological Survey and South Dakota Water Resources Commission (Water Resources Report 4, Basic hydrogeologic data - Pine Ridge Indian Reservation, South Dakota).  A selected bibliography of reports pertaining to the geology of the area has been included in the basic-data report.  This atlas will be more useful if studied in conjunction with a copy of the basic-data report.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha357","usgsCitation":"Ellis, M.J., and Adolphson, D.G., 1971, Hydrogeology of the Pine Ridge Indian Reservation, South Dakota: U.S. Geological Survey Hydrologic Atlas 357, 2 Plates: 54.25 x 33.00 inches and 35.50 x 32.00 inches, https://doi.org/10.3133/ha357.","productDescription":"2 Plates: 54.25 x 33.00 inches and 35.50 x 32.00 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":186220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha357.PNG"},{"id":89975,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/357/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89974,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/357/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","country":"United States","state":"South Dakota","otherGeospatial":"Pine Ridge Indian Reservation","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103,43 ], [ -103,43.75 ], [ -101.25,43.75 ], [ -101.25,43 ], [ -103,43 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db615063","contributors":{"authors":[{"text":"Ellis, M. J.","contributorId":27840,"corporation":false,"usgs":true,"family":"Ellis","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":278230,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68446,"text":"ha355 - 1971 - Hydrology of the Rosebud Indian Reservation, South Dakota","interactions":[],"lastModifiedDate":"2022-04-13T19:19:33.318147","indexId":"ha355","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"355","title":"Hydrology of the Rosebud Indian Reservation, South Dakota","docAbstract":"

An investigation of the geology and ground-water resources of the Rosebud Indian Reservation, South Dakota, was made at the request of the Bureau of Indian Affairs as part of the U.S. Department of Interior's program for the development of the Missouri River basin.  Originally, the Reservation included all of Mellette, Todd, and Tripp Counties; most of Gregory County, and a small part of Lyman County.  (See index map.)  However, of the 1,500 square miles of land now owned by individual Indians or by the Rosebud Sioux Tribe, nearly 95 percent is located in Mellette and Todd Counties.  Accordingly, the area of this investigation (about 2,700 square miles) was restricted to these two counties.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha355","usgsCitation":"Ellis, M.J., Ficken, J.H., and Adolphson, D.G., 1971, Hydrology of the Rosebud Indian Reservation, South Dakota: U.S. Geological Survey Hydrologic Atlas 355, 2 Plates: 35.0 x 50.0 inches, https://doi.org/10.3133/ha355.","productDescription":"2 Plates: 35.0 x 50.0 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":186198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha355.PNG"},{"id":89979,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/355/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89978,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/355/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398663,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15732.htm"}],"scale":"125000","country":"United States","state":"South Dakota","otherGeospatial":"Rosebud Indian Reservation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -101.225,\n 43\n ],\n [\n -100.199,\n 43\n ],\n [\n -100.199,\n 43.875\n ],\n [\n -101.225,\n 43.875\n ],\n [\n -101.225,\n 43\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca4b","contributors":{"authors":[{"text":"Ellis, M. 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This investigation is part of a statewide program to determine the location, extent, and nature of the ground-water reservoirs (aquifers); to evaluate the occurrence and movement of ground water within these aquifers, including the sources and areas of recharge and discharge; to estimate the potential yields of wells tapping the major aquifers; and to determine the chemical quality of the ground water.

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LOCATION AND EXTENT OF STUDY AREA

\n

The central Wisconsin River basin is the middle part of the entire Wisconsin River basin. The basin is about 5,050 square miles in area, and extends about 110 miles south from Merrill to Wisconsin Dells. The basin includes all or parts of the following counties: Adams, Clark, Columbia, Jackson, Juneau, Langlade, Lincoln, Marathon, Marquette, Monroe, Portage, Sauk, Taylor, Waushara, and Wood.

\n

PURPOSE AND SCOPE

\n

This study provides a background of hydrologic knowledge suitable for use by water-resource planners and managers, and it provides a framework for more detailed water-resource studies in the future. Specifically, the purposes of this report are to: (1) Describe the geologic and hydrologic environments of the central Wisconsin River basin. (2) Describe the water resources of the central Wisconsin River basin including their sources, uses, quality, interrelationships, availability, and behavior within the basin environment. Much of the information in this report has been generalized to allow presentation in the atlas format. Liberal use was made of available data from many sources and interpretations from published reports. Additional material was collected and analyzed to allow a balanced presentation on water resources and the physical environment. This study is part of an investigation of the water resources of the major river basins in Wisconsin. The completed basin studies and those being studied are shown on the cover envelope. The information in this report should be adequate for the broad aspects of planning water-resource development and management. However, individual problems and water needs will require more specific information than is given in this report.

\n

 

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