{"pageNumber":"6503","pageRowStart":"162550","pageSize":"25","recordCount":184904,"records":[{"id":2823,"text":"wsp1672 - 1968 - Magnitude and frequency of floods in the United States; part 1-B. North Atlantic slope basins, New York to York River","interactions":[],"lastModifiedDate":"2022-01-07T20:34:53.772695","indexId":"wsp1672","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1672","title":"Magnitude and frequency of floods in the United States; part 1-B. North Atlantic slope basins, New York to York River","docAbstract":"<p>Flood magnitude-frequency relation applicable to streams in the North Atlantic slope basins, New York to York River, Va., are presented in this report. &nbsp;The relations are based on flood data collected at 487 gaging stations having&nbsp;5 or more years of record not materially affected by regulation. For sites on most streams, the magnitude of a flood of any given frequency between 1.1 and 50&nbsp;years can be determined from two curves - one expressing the relation between&nbsp;the mean annual flood and size of draining basin and the other expressing the&nbsp;ratio to the mean annual flood of floods of other recurrence intervals. For New&nbsp;Jersey streams, an adjustment to the mean annual flood is based on the percentage&nbsp;of surface area covered by lakes and swamps in the basin.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1672","usgsCitation":"Tice, R.H., 1968, Magnitude and frequency of floods in the United States; part 1-B. North Atlantic slope basins, New York to York River: U.S. Geological Survey Water Supply Paper 1672, Report: xvii, 585 p.; Plate: 29.23 x 37.19 inches, https://doi.org/10.3133/wsp1672.","productDescription":"Report: xvii, 585 p.; Plate: 29.23 x 37.19 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":138743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1672/report-thumb.jpg"},{"id":29382,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1672/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29381,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1672/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":110006,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24881.htm","linkFileType":{"id":5,"text":"html"},"description":"24881"}],"country":"United States","state":"Delaware, Maryland, New Jersey, New York, Pennsylvania, Virginia, West Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.4970703125,\n              36.84446074079564\n            ],\n            [\n              -79.4970703125,\n              43.75522505306928\n            ],\n            [\n              -73.388671875,\n              43.75522505306928\n            ],\n            [\n              -73.388671875,\n              36.84446074079564\n            ],\n            [\n              -79.4970703125,\n              36.84446074079564\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495ad","contributors":{"authors":[{"text":"Tice, Richard H.","contributorId":13601,"corporation":false,"usgs":true,"family":"Tice","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145857,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2671,"text":"wsp1798E - 1968 - Sedimentation in the Piru Creek watershed, southern California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1798E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1798","chapter":"E","title":"Sedimentation in the Piru Creek watershed, southern California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1798E","usgsCitation":"Scott, K.M., Ritter, J.R., and Knott, J.M., 1968, Sedimentation in the Piru Creek watershed, southern California: U.S. Geological Survey Water Supply Paper 1798, vi, 48 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1798E.","productDescription":"vi, 48 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1798e/report-thumb.jpg"},{"id":29022,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1798e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fbc55","contributors":{"authors":[{"text":"Scott, Kevin M.","contributorId":88331,"corporation":false,"usgs":true,"family":"Scott","given":"Kevin","email":"","middleInitial":"M.","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":false,"id":145588,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ritter, John R.","contributorId":75508,"corporation":false,"usgs":true,"family":"Ritter","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145586,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knott, J. M.","contributorId":77909,"corporation":false,"usgs":true,"family":"Knott","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":145587,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2620,"text":"wsp1775 - 1968 - Hydrologic characteristics and sustained yield of principal ground-water units, Potowomut-Wickford area, Rhode Island","interactions":[{"subject":{"id":52067,"text":"ofr603 - 1960 - Ground-water conditions in the Hunt River basin, Rhode Island-April 1960","indexId":"ofr603","publicationYear":"1960","noYear":false,"title":"Ground-water conditions in the Hunt River basin, Rhode Island-April 1960"},"predicate":"SUPERSEDED_BY","object":{"id":2620,"text":"wsp1775 - 1968 - Hydrologic characteristics and sustained yield of principal ground-water units, Potowomut-Wickford area, Rhode Island","indexId":"wsp1775","publicationYear":"1968","noYear":false,"title":"Hydrologic characteristics and sustained yield of principal ground-water units, Potowomut-Wickford area, Rhode Island"},"id":1}],"lastModifiedDate":"2023-03-14T19:57:42.874774","indexId":"wsp1775","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1775","title":"Hydrologic characteristics and sustained yield of principal ground-water units, Potowomut-Wickford area, Rhode Island","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"English","doi":"10.3133/wsp1775","usgsCitation":"Rsenshein, J.S., Gonthier, J.B., and Allen, W., 1968, Hydrologic characteristics and sustained yield of principal ground-water units, Potowomut-Wickford area, Rhode Island: U.S. Geological Survey Water Supply Paper 1775, Report: iv, 38 p.; 5 Plates: 50.00 x 36.00 inches, https://doi.org/10.3133/wsp1775.","productDescription":"Report: iv, 38 p.; 5 Plates: 50.00 x 36.00 inches","costCenters":[],"links":[{"id":414123,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24952.htm","linkFileType":{"id":5,"text":"html"}},{"id":28932,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1775/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28931,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1775/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28930,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1775/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28929,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1775/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28934,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1775/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28933,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1775/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138145,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1775/report-thumb.jpg"}],"country":"United States","state":"Rhode Island","otherGeospatial":"Potowomut-Wickford area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.397,\n              41.69\n            ],\n            [\n              -71.562,\n              41.69\n            ],\n            [\n              -71.562,\n              41.509\n            ],\n            [\n              -71.397,\n              41.509\n            ],\n            [\n              -71.397,\n              41.69\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683706","contributors":{"authors":[{"text":"Rsenshein, J. S.","contributorId":49338,"corporation":false,"usgs":true,"family":"Rsenshein","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gonthier, Joseph B.","contributorId":74350,"corporation":false,"usgs":true,"family":"Gonthier","given":"Joseph","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":145511,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Allen, William B.","contributorId":22321,"corporation":false,"usgs":true,"family":"Allen","given":"William B.","affiliations":[],"preferred":false,"id":145509,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2616,"text":"wsp1663C - 1968 - Ground-water resources of the Acu Valley, Rio Grande Norte, Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1663C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1663","chapter":"C","title":"Ground-water resources of the Acu Valley, Rio Grande Norte, Brazil","docAbstract":"The Acu Valley is the lower part of the Rio Piranhas valley in the northwestern part of the State of Rio Grande do Norte, Brazil. It begins where the Rio Piranhas leaves the crystalline Precambrian rocks to flow across the outcrop of sedimentary rocks. The area considered in this report extends northward for about 45 kilometers; it is terminated arbitrarily where encroachment by sea water has contaminated the aquifer and imparted a disagreeable saline taste to the water in it. The boundary was not determined in the field, however, for lack of special equipment. Part of the extensive uplands on either side of the valley are included. This makes the total area approximately 2,500 square kilometers. The largest town, Acu, had a population of about 8,000 in 1960. \r\n\r\nThe area is considered to be part of the Drought Polygon of northeast Brazil because the precipitation, although averaging 448 millimeters annually at Acu, varies widely from year to year and often is deficient for many months. The precipitation has been supplemented by use of irrigation wells, but irrigated agriculture is not yet far advanced, and the quantities of water used in irrigation are small. \r\n\r\nGeologically, the area consists of basement crystalline rocks (Precambrian), a wedge of sedimentary rocks thickening northward (Cretaceous), and alluvial sediments constituting a narrow band in the bottom of the valley (Alluvium and terrace deposits). The crystalline rocks contain water mainly in fractures and, in general, are impermeable. The sedimentary rocks of Cretaceous age comprise two units: a thick but fine-grained sandstone grading upward into siltstone and shale (Acu Sandstone), and limestone and dolomite with an included shale zone (Jandaira Limestone). The sandstone especially and the limestone to a lesser degree are ground-water reservoirs of large capacity. The limestone has been tapped at several places, but the sandstone and its contained water are practically untested and, hence, imperfectly understood. \r\n\r\nThe alluvium of the first terrace is the aquifer supplying most of the ground water being used in the area. Wells in the alluvium yield as much as S0,000 liters per hour. Larger yields probably could be obtained from wells designated to take full advantage of the aquifer. There are in the valley about 300 dug wells which are used for irrigation. Half of these are equipped with pumps and engines. The rest, together with about 500 drive-point wells, are equipped with manual or windmill-driven pumps. In addition to irrigation, the water is used in homes and for cattle. The quantities of water currently used in irrigation are relatively small, both per hectare and in the area as a whole, but .this will probably increase substantially when intensive irrigation becomes a reality. The annual pumpage from the alluvium, nearly constant since 1959, was about 2.5 million cubic meters in 1964, which is only about 90 cubic meters from each hectare-meter of saturated alluvium. This amount would lower the water table about 1 meter in 11 years, if there were no recharge. Actually, no such decline is likely to occur, because the recharge from precipitation alone is estimated to be more than enough to replace the water currently being pumped. \r\n\r\nChemical analyses of eight samples show that the ground water in the alluvium is acceptable for most uses. The water in the Acu Sandstone and Jandazra Limestone is more mineralized than that in the alluvium and at some places, at least, is not acceptable for human consumption. The available chemical data on this water, however, are not adequate to judge fully the quality of the water in these formations. \r\n\r\nIt is estimated that about .'22 million cubic meters of water would be needed annually if irrigation were extended to all the bottom land, which totals about 25,000 hectares. This amount is only one-fourth to one-half the estimated recharge from precipitation alone. The present rate of application of water is very low ","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1663C","usgsCitation":"Rodis, H.G., and de Castro Araujo, J.M., 1968, Ground-water resources of the Acu Valley, Rio Grande Norte, Brazil: U.S. Geological Survey Water Supply Paper 1663, iv, 34 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1663C.","productDescription":"iv, 34 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1663c/report-thumb.jpg"},{"id":28907,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1663c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28908,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1663c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d564","contributors":{"authors":[{"text":"Rodis, Harry G.","contributorId":25141,"corporation":false,"usgs":true,"family":"Rodis","given":"Harry","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145500,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"de Castro Araujo, Jonas Maria.","contributorId":72648,"corporation":false,"usgs":true,"family":"de Castro Araujo","given":"Jonas","email":"","middleInitial":"Maria.","affiliations":[],"preferred":false,"id":145501,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2589,"text":"wsp1852 - 1968 - Water resources of King County, Washington","interactions":[],"lastModifiedDate":"2023-01-03T21:32:56.352719","indexId":"wsp1852","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1852","title":"Water resources of King County, Washington","docAbstract":"<p>Although the total supply of water in King County is large, water problems are inevitable because of the large and rapidly expanding population. The county contains a third of the 3 million people in Washington, most of the population being concentrated in the Seattle metropolitan area. </p><p>King County includes parts of two major physiographic features: the western area is part of the Puget Sound Lowland, and the eastern area is part of the Cascade Range. In these two areas, the terrain, weather, and natural resources (including water) contrast markedly. </p><p>Average annual precipitation in the county is about 80 inches, ranging from about 30 inches near Puget Sound to more than 150 inches in parts of the Cascades. Annual evapotranspiration is estimated to range from 15 to 24 inches. </p><p>Average annual runoff ranges from about 15 inches in the lowlands to more than 100 inches in the mountains. Most of the streamflow is in the major basins of the county--the Green-Duwamish, Lake Washington, and Snoqualmie basins. The largest of these is the Snoqualmie River basin (693 square miles), where average annual runoff during the period 1931-60 was about 79 inches. During the same period, annual runoff in the Lake Washington basin ( 607 square miles) averaged about 32 inches, and in the Green-Duwamish River basin (483 square miles), about 46 inches. Seasonal runoff is generally characterized by several high-flow periods in the winter, medium flows in the spring, and sustained low flows in the summer and fall. </p><p>When floods occur in the county they come almost exclusively between October and March. The threat of flood damage is greatest on the flood plaits of the larger rivers, but in the Green-Duwamish Valley the threat was greatly reduced with the completion of Howard A. Hanson Dam in 1962. In the Snoqualmie River basin, where no such dam exists, the potential damage from a major flood increases each year as additional land is developed in the Snoqualmie Valley. </p><p>Only moderate amounts of sediment are transported by most streams in the county, except during short periods of heavy rain in the winter. The temperature and chemical quality of surface waters are well suited to the requirements of fisheries and for municipal, industrial, and domestic supplies. Little treatment is needed for most uses of surface water, except where the water is subject to pollution. </p><p>Most recoverable ground water in the county occurs in the Puget Sound Lowland, where great volumes of unconsolidated sedimentary deposits were left by the continental glaciers of the Pleistocene Epoch. Bedrock, most of which is in the Cascade Range, contains very little ground water. Numerous springs, largely undeveloped, occur in several parts of the county. </p><p>Most of the ground water is of good to excellent quality except for excessive iron, which in some places may require treatment of the water before it is suitable for domestic or industrial use. </p><p>Excluding water used for hydroelectric-power, recreation, and fisheries, more than 80 percent of the water used in the county is provided by municipal-supply systems. Each of the major river basins includes municipal watersheds that provide large supplies of excellent water. By the 1980's, more than 90 percent of the county's population will probably be served by the Seattle municipal supply. With full development, Seattle's water system would have a capacity sufficient to supply more than 2 million people with 300 gallons per person per day. Most industrial and commercial establishments in the county obtain water from public supply systems. </p><p>The most serious water problem in the county at present (1965) is the threat of pollution in the densely populated areas. The immediate threat in the Seattle area is being reduced by the sewage-treatment program of the Municipality of Metropolitan Seattle, which will eliminate the discharge of waste into Lake Washington. Expected increases in population and industry will introduce new problems that will require additional planning to assure adequate water quality for fisheries, recreation, and other uses.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1852","usgsCitation":"Richardson, D., Bingham, J., Madison, R.J., and Williams, R., 1968, Water resources of King County, Washington: U.S. Geological Survey Water Supply Paper 1852, Report: v, 74 p.; 2 Plates: 20.00 x 22.80 inches and 20.00 x 19.24 inches, https://doi.org/10.3133/wsp1852.","productDescription":"Report: v, 74 p.; 2 Plates: 20.00 x 22.80 inches and 20.00 x 19.24 inches","costCenters":[],"links":[{"id":411295,"rank":5,"type":{"id":36,"text":"NGMDB Index 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Donald","contributorId":68288,"corporation":false,"usgs":true,"family":"Richardson","given":"Donald","email":"","affiliations":[],"preferred":false,"id":145452,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, J.W.","contributorId":35295,"corporation":false,"usgs":true,"family":"Bingham","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":145451,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Madison, R. J.","contributorId":84734,"corporation":false,"usgs":true,"family":"Madison","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":145453,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Williams, R.","contributorId":7686,"corporation":false,"usgs":true,"family":"Williams","given":"R.","affiliations":[],"preferred":false,"id":145450,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2494,"text":"wsp1859E - 1968 - Hydrology of Crater, East and Davis Lakes, Oregon; with section on Chemistry of the Lakes","interactions":[],"lastModifiedDate":"2017-02-03T13:43:14","indexId":"wsp1859E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1859","chapter":"E","title":"Hydrology of Crater, East and Davis Lakes, Oregon; with section on Chemistry of the Lakes","docAbstract":"Crater, East, and Davis Lakes are small bodies of fresh water that occupy topographically closed basins in Holocene volcanic terrane. Because the annual water supply exceeds annual evaporation, water must be lost by seepage from each lake. The seepage rates vary widely both in volume and in percentage of the total water supply. Crater Lake loses about 89 cfs (cubic feet per second), equivalent to about 72 percent of its average annual supply. East Lake loses about 2.3 cfs, or about 44 percent of its estimated supply. Davis Lake seepage varies greatly with lake level, but the average loss is about 150 cfs, more than 90 percent of its total supply. The destination of the seepage loss is not definitely known for any of the lakes. \r\n\r\nAn approximate water budget was computed for stationary level for each lake, by using estimates 'by the writer to supplement the hydrologic data available. The three lake waters are dilute. Crater Lake contains about 80 ppm, (parts per million) of dissolved solids---mostly silica, sodium, and bicarbonate, and lesser amounts of calcium, sulfate, and chloride. Much of the dissolved-solids content of Crater Lake---especially the sulfate and chloride---may be related to fumarole and thermal-spring activity that presumably followed the collapse of Mount Mazama. Although Grater Lake loses an estimated 7,000 tons of its 1.5million-ton salt content each year by leakage, the chemical character of the lake did not change appreciably between 1912 and 1964. East Lake contains 200 ppm of dissolved solids, which includes major proportions of calcium, sodium, bicarbonate, and sulfate, but almost no chloride. The lake apparently receives much of its dissolved solids from subsurface thermal springs. Annual solute loss from East Lake by leakage is about 450 tons, or 3 percent of the lake's 15,000-ton estimated solute content. Davis Lake contains only 48 ppm of dissolved solids, much of which is silica and bicarbonate; chloride is almost completely absent. Approximate physical and hydrologic data for the lakes are summarized in the following table.\r\n\r\n[Table]","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1859E","usgsCitation":"Phillips, K.N., and Van Denburgh, A.S., 1968, Hydrology of Crater, East and Davis Lakes, Oregon; with section on Chemistry of the Lakes: U.S. Geological Survey Water Supply Paper 1859, iv, 60 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1859E.","productDescription":"iv, 60 p. :ill. ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":138755,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859e/report-thumb.jpg"},{"id":28614,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604971","contributors":{"authors":[{"text":"Phillips, Kenneth N.","contributorId":34105,"corporation":false,"usgs":true,"family":"Phillips","given":"Kenneth","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":145287,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Denburgh, A. S.","contributorId":23928,"corporation":false,"usgs":true,"family":"Van Denburgh","given":"A.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":145286,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2448,"text":"wsp1859G - 1968 - Storage requirements for Arkansas streams","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1859G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1859","chapter":"G","title":"Storage requirements for Arkansas streams","docAbstract":"The supply of good-quality surface water in Arkansas is abundant. owing to seasonal and annual variability of streamflow, however, storage must be provided to insure dependable year-round supplies in most of the State. Storage requirements for draft rates that are as much as 60 percent of the mean annual flow at 49 continuous-record gaging stations can be obtained from tabular data in this report. \r\n\r\nThrough regional analyses of streamflow data, the State was divided into three regions. Draft-storage diagrams for each region provide a means of estimating storage requirements for sites on streams where data are scant, provided the drainage area, the mean annual flow, and the low-flow index are known. These data are tabulated for 53 gaging stations used in the analyses and for 132 partial-record sites where only base-flow measurements have been made. Mean annual flow can be determined for any stream whose drainage lies within the State by using the runoff map in this report. Low-flow indices can be estimated by correlating base flows, determined from several discharge measurements, with concurrent flows at nearby continuous-record gaging stations, whose low-flow indices have been determined.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1859G","usgsCitation":"Patterson, J.L., 1968, Storage requirements for Arkansas streams: U.S. Geological Survey Water Supply Paper 1859, 36 p. :ill. (1 col.) ;24 cm., https://doi.org/10.3133/wsp1859G.","productDescription":"36 p. :ill. (1 col.) ;24 cm.","costCenters":[],"links":[{"id":138128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1859g/report-thumb.jpg"},{"id":28522,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1859g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28523,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1859g/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4244","contributors":{"authors":[{"text":"Patterson, James Lee","contributorId":24329,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"Lee","affiliations":[],"preferred":false,"id":145221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2444,"text":"wsp1678 - 1968 - Magnitude and frequency of floods in the United States, part 5. Hudson Bay and Upper Mississippi River Basins","interactions":[],"lastModifiedDate":"2022-02-04T19:42:49.140794","indexId":"wsp1678","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1678","title":"Magnitude and frequency of floods in the United States, part 5. Hudson Bay and Upper Mississippi River Basins","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1678","usgsCitation":"Patterson, J.L., and Gamble, C.R., 1968, Magnitude and frequency of floods in the United States, part 5. Hudson Bay and Upper Mississippi River Basins: U.S. Geological Survey Water Supply Paper 1678, xix, 546 p., https://doi.org/10.3133/wsp1678.","productDescription":"xix, 546 p.","costCenters":[],"links":[{"id":28515,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1678/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138124,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1678/report-thumb.jpg"},{"id":395471,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24887.htm"}],"country":"United States","otherGeospatial":"Hudson Bay and upper Mississippi River basins","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -101.6015625,\n              38.34165619279595\n            ],\n            [\n              -85.341796875,\n              38.34165619279595\n            ],\n            [\n              -85.341796875,\n              49.03786794532644\n            ],\n            [\n              -101.6015625,\n              49.03786794532644\n            ],\n            [\n              -101.6015625,\n              38.34165619279595\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6495eb","contributors":{"authors":[{"text":"Patterson, James L.","contributorId":17593,"corporation":false,"usgs":true,"family":"Patterson","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145216,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gamble, Charles R.","contributorId":6822,"corporation":false,"usgs":true,"family":"Gamble","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145215,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3271,"text":"cir596 - 1968 - Preliminary results of geological, geochemical, and geophysical studies in part of the Virginia City quadrangle, Nevada","interactions":[],"lastModifiedDate":"2017-08-27T17:52:09","indexId":"cir596","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"596","title":"Preliminary results of geological, geochemical, and geophysical studies in part of the Virginia City quadrangle, Nevada","docAbstract":"Geological, geochemical, and geophysical studies in the Comstock Lode district and adjoining parts of the Virginia Range near Virginia City, Nev., have resulted in recognition of two geophysical anomalies and several geochemical anomalies in an area north of Virginia City. The geophysical anomalies were found during an induced-polarization survey carried out to aid in tracing the Comstock fault, the principal structure localizing the bonanza silver-gold deposits of the Comstock Lode district, in an area of intensely altered rock and alluvial cover about 5 miles north of Virginia City. Geochemical anomalies showing mercury in excess of 5 ppm (parts per million) were found in altered rocks along the Cornstock fault near Cornwall Knob about 5 miles north of Virginia City and in the Washington Hill area, 6 miles farther north.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir596","usgsCitation":"Whitebread, D.H., and Hoover, D.B., 1968, Preliminary results of geological, geochemical, and geophysical studies in part of the Virginia City quadrangle, Nevada: U.S. Geological Survey Circular 596, iii, 20 p. :illus., maps. ;26 cm., https://doi.org/10.3133/cir596.","productDescription":"iii, 20 p. :illus., maps. ;26 cm.","costCenters":[],"links":[{"id":30265,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0596/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0596/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b309","contributors":{"authors":[{"text":"Whitebread, Donald Harvey","contributorId":11582,"corporation":false,"usgs":true,"family":"Whitebread","given":"Donald","email":"","middleInitial":"Harvey","affiliations":[],"preferred":false,"id":146553,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":146554,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2341,"text":"wsp1854 - 1968 - Ground-water hydrology of the Sevier Desert, Utah","interactions":[],"lastModifiedDate":"2017-09-04T17:15:01","indexId":"wsp1854","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1854","title":"Ground-water hydrology of the Sevier Desert, Utah","docAbstract":"<p>The Sevier Desert, as used in this report, comprises the main part of the Sevier Desert, the Tintic Valley, and the southeastern part of the Old River Bed. It covers an area of about 3,000 square miles and occupies a large basin in the eastern part of the Basin and Range physiographic province.</p><p>Large alluvial fans extend from the mountain fronts into the basin where they interfinger with eolian and lacustrine deposits and with fluvial deposits of the Sevier River. These unconsolidated deposits form a multiaquifer artesian system that is more than 1,000 feet thick and that extends from near the area of main recharge along the east side of the basin to Sevier Lake.</p><p>Most of the recharge to the ground-water reservoir results from water entering alluvial fans as percolation from streams, irrigation ditches, and irrigated fields. Another important source may be water in the limestone, quartzite, and other consolidated rocks in the mountains that border the basin. Leakage from the Central Utah Canal is a major source of recharge to the water-table aquifer.</p><p>Flowing wells are common in the central lowland part of the Sevier Desert, but as a result of below-normal precipitation and an increase in withdrawals from wells during 1950-64, the area of flowing wells has decreased. The quantity of ground water being wasted from flowing wells is not more than a few hundred acre-feet a year.</p><p>The amount of water discharged by withdrawal from wells has increased nearly 15 times since 1950 (from 2,000 acre-feet in 1950 to 30,000 acre-feet in 1964). As a result of this increasing withdrawal, the water levels in observation wells have declined 4 feet in areas of small withdrawals to more than 7 feet near centers of pumping for public supplies and irrigation.</p><p>An estimated 135,000-175,000 acre-feet of ground water is consumed by evapotranspiration each year in the 440,000 acres of desert that mainly support phreatophytes. This rate of discharge has changed little since 1950. The consumptive waste of ground water by undesirable phreatophytes, principally saltcedar and pickleweed, was not a serious problem in 1964 but could become a serious problem in the near future if saltcedar is permitted to spread.</p><p>Water levels in wells changed little during 1935-40. During 1941-50, however, water levels rose in response to the general above-normal precipitation during 1939-47. During 1950-64 water levels declined, partly in response to below-normal precipitation and partly in response to an increase in pumping from irrigation wells. Although the period 1961-63 was one of above-normal precipitation, water levels continued the overall decline that was started in 1950. The decline, therefore, probably is due to increased pumping.</p><p>The amount of water that could be obtained from storage if the piezometric surface in the artesian aquifer were lowered 20 feet is estimated to be 120,006 acre-feet. The specific capacities of wells used for irrigation and public supply range from 5 to 215 gallons per minute per foot of drawdown. Specific capacities generally decrease with increasing distances away from the edge of the basin.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1854","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Mower, R.W., and Feltis, R., 1968, Ground-water hydrology of the Sevier Desert, Utah: U.S. Geological Survey Water Supply Paper 1854, Report: v, 75 p.; 7 Plates: 30.00 in. x 24.82 in. or smaller, https://doi.org/10.3133/wsp1854.","productDescription":"Report: v, 75 p.; 7 Plates: 30.00 in. x 24.82 in. or smaller","numberOfPages":"88","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":28244,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1854/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of the Sevier Desert, Utah, showing areas of phreatophyte growth in 1963"},{"id":138337,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1854/report-thumb.jpg"},{"id":28238,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1854/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of the Sevier Desert, Utah, showing location of selected wells and hydrogeochemical data"},{"id":28241,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1854/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of the Sevier Desert, Utah, showing average annual precipitation (1931-60) and recharge areas along the north and east edges"},{"id":28242,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1854/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of the Sevier Desert, Utah, showing areas of artesian flow during 1935 and March 1964 and water-level contours in the upper artesian and unconfined aquifers in March 1964"},{"id":28243,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1854/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of the Sevier Desert, Utah, showing total dissolved solids in water from wells finished in the artesian aquifers, springs, and streams"},{"id":28239,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1854/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Generalized geologic map of the Sevier Desert and adjacent mountains, Utah"},{"id":28240,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1854/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Geologic section across the Sevier Desert, Utah, showing generalized stratigraphy and lithology and selected parts from an electrical log from an oil test"},{"id":28245,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1854/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Desert","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6682c2","contributors":{"authors":[{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145048,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":145049,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3289,"text":"cir548 - 1968 - Reports and maps of the Geological Survey released only in the open files, 1967","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir548","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"548","title":"Reports and maps of the Geological Survey released only in the open files, 1967","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir548","usgsCitation":"Weld, B., Griffin, M.S., and Brett, G.W., 1968, Reports and maps of the Geological Survey released only in the open files, 1967: U.S. Geological Survey Circular 548, 21 p. ;27 cm., https://doi.org/10.3133/cir548.","productDescription":"21 p. ;27 cm.","costCenters":[],"links":[{"id":117575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1968/0548/report-thumb.jpg"},{"id":30285,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1968/0548/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f422","contributors":{"authors":[{"text":"Weld, Betsy A.","contributorId":68714,"corporation":false,"usgs":true,"family":"Weld","given":"Betsy A.","affiliations":[],"preferred":false,"id":146599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griffin, Margaret S.","contributorId":101252,"corporation":false,"usgs":true,"family":"Griffin","given":"Margaret","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":146600,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brett, George W.","contributorId":58622,"corporation":false,"usgs":true,"family":"Brett","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":146598,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":13091,"text":"ofr6858 - 1968 - Metallic mineral resources map of the Skagway Quadrangle, Alaska","interactions":[{"subject":{"id":13091,"text":"ofr6858 - 1968 - Metallic mineral resources map of the Skagway Quadrangle, Alaska","indexId":"ofr6858","publicationYear":"1968","noYear":false,"title":"Metallic mineral resources map of the Skagway Quadrangle, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":59238,"text":"mf424 - 1972 - Metallic mineral resources map of the Skagway Quadrangle, Alaska","indexId":"mf424","publicationYear":"1972","noYear":false,"title":"Metallic mineral resources map of the Skagway Quadrangle, Alaska"},"id":1}],"supersededBy":{"id":59238,"text":"mf424 - 1972 - Metallic mineral resources map of the Skagway Quadrangle, Alaska","indexId":"mf424","publicationYear":"1972","noYear":false,"title":"Metallic mineral resources map of the Skagway Quadrangle, Alaska"},"lastModifiedDate":"2023-12-08T18:58:07.273207","indexId":"ofr6858","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"68-58","title":"Metallic mineral resources map of the Skagway Quadrangle, Alaska","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6858","usgsCitation":"1968, Metallic mineral resources map of the Skagway Quadrangle, Alaska: U.S. Geological Survey Open-File Report 68-58, Report: 4 p.; 1 Plate: 29.67 x 23.41 inches, https://doi.org/10.3133/ofr6858.","productDescription":"Report: 4 p.; 1 Plate: 29.67 x 23.41 inches","costCenters":[],"links":[{"id":423356,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1968/0058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":423355,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1968/0058/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146137,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1968/0058/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Skagway Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -135,\n              60\n            ],\n            [\n              -138,\n              60\n            ],\n            [\n              -138,\n              59\n            ],\n            [\n              -135,\n              59\n            ],\n            [\n              -135,\n              60\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4fe4b07f02db6284fa","contributors":{"compilers":[{"text":"Cobb, Edward H.","contributorId":64689,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward H.","affiliations":[],"preferred":false,"id":889900,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":2257,"text":"wsp1855 - 1968 - Ground-water levels in the United States, 1961-65, southwestern States","interactions":[],"lastModifiedDate":"2024-01-31T21:32:21.660914","indexId":"wsp1855","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1968","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":"1855","title":"Ground-water levels in the United States, 1961-65, southwestern States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1855","usgsCitation":"McGuinness, C.L., 1968, Ground-water levels in the United States, 1961-65, southwestern States: U.S. Geological Survey Water Supply Paper 1855, v, 125 p., https://doi.org/10.3133/wsp1855.","productDescription":"v, 125 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