{"pageNumber":"2540","pageRowStart":"63475","pageSize":"25","recordCount":68805,"records":[{"id":52452,"text":"ofr6535 - 1965 - A progress report on the Malaga Bend Experimental Salinity Alleviation Project, Eddy County, New Mexico","interactions":[],"lastModifiedDate":"2017-04-07T10:48:17","indexId":"ofr6535","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-35","title":"A progress report on the Malaga Bend Experimental Salinity Alleviation Project, Eddy County, New Mexico","docAbstract":"At Malaga Bend on the Pecos River in Eddy County, New Mexico, a brine aquifer about 1950 feet below the stream channel has a pressure head about 10 feet above the river bed. This aquifer normally discharges about 430 tons of dissolved minerals daily into the river of which about 370 tons was sodium chloride. \r\n\r\nThe Malaga Bend Experimental Salinity Alleviation Project, authorized by the U.S. Congress in 1958, Public Law 85-333,is an attempt to determine if the salinity content of the Pecos River below Malaga Bend can be decreased by reducing the inflow of saline water into the river at Malaga Bend by pumping from the brine aquifer. \r\n\r\nConstruction for the project was supervised by the Bureau of Reclamation, and the collection of data and its interpretation were the responsibility cooperatively of the U. S. Geological Survey and the Pecos River Commission.","language":"ENGLISH","doi":"10.3133/ofr6535","usgsCitation":"Cox, E., and Havens, J., 1965, A progress report on the Malaga Bend Experimental Salinity Alleviation Project, Eddy County, New Mexico: U.S. Geological Survey Open-File Report 65-35, 92 p., https://doi.org/10.3133/ofr6535.","productDescription":"92 p.","costCenters":[],"links":[{"id":179274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0035/report-thumb.jpg"},{"id":86878,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0035/plate-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":86879,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0035/plate-2.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":86883,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0035/plate-6.pdf","text":"Figure 9","linkFileType":{"id":1,"text":"pdf"}},{"id":86880,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0035/plate-3.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}},{"id":86881,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0035/plate-4.pdf","text":"Figure 7","linkFileType":{"id":1,"text":"pdf"}},{"id":86882,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0035/plate-5.pdf","text":"Figure 8","linkFileType":{"id":1,"text":"pdf"}},{"id":86885,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0035/plate-8.pdf","text":"Figure 11","linkFileType":{"id":1,"text":"pdf"}},{"id":86884,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0035/plate-7.pdf","text":"Figure 10","linkFileType":{"id":1,"text":"pdf"}},{"id":86886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d1e","contributors":{"authors":[{"text":"Cox, E.R.","contributorId":6094,"corporation":false,"usgs":true,"family":"Cox","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":245366,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Havens, J.S.","contributorId":12043,"corporation":false,"usgs":true,"family":"Havens","given":"J.S.","email":"","affiliations":[],"preferred":false,"id":245367,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2068,"text":"wsp1817B - 1965 - Identification and measurement of chlorinated organic pesticides in water by electron-capture gas chromatography","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp1817B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1817","chapter":"B","title":"Identification and measurement of chlorinated organic pesticides in water by electron-capture gas chromatography","docAbstract":"Pesticides, in minute quantities, may affect the regimen of streams, and because they may concentrate in sediments, aquatic organisms, and edible aquatic foods, their detection and their measurement in the parts-per-trillion range are considered essential. \r\n\r\nIn 1964 the U.S. Geological Survey at Menlo Park, Calif., began research on methods for monitoring pesticides in water. Two systems were selected--electron-capture gas chromatography and microcoulometric-titration gas chromatography. Studies on these systems are now in progress. This report provides current information on the development and application of an electron-capture gas chromatographic procedure. This method is a convenient and extremely sensitive procedure for the detection and measurement of organic pesticides having high electron affinities, notably the chlorinated organic pesticides. The electron-affinity detector is extremely sensitive to these substances but it is not as sensitive to many other compounds. By this method, the chlorinated organic pesticide may be determined on a sample of convenient size in concentrations as low as the parts-per-trillion range. To insure greater accuracy in the identifications, the pesticides reported were separated and identified by their retention times on two different types of gas chromatographic columns.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1817B","usgsCitation":"Lamar, W.L., Goerlitz, D.F., and Law, L., 1965, Identification and measurement of chlorinated organic pesticides in water by electron-capture gas chromatography: U.S. Geological Survey Water Supply Paper 1817, iii, 12 p. ;24 cm., https://doi.org/10.3133/wsp1817B.","productDescription":"iii, 12 p. ;24 cm.","costCenters":[],"links":[{"id":138437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1817b/report-thumb.jpg"},{"id":27621,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1817b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5faacb","contributors":{"authors":[{"text":"Lamar, William L.","contributorId":15592,"corporation":false,"usgs":true,"family":"Lamar","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144630,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goerlitz, Donald F.","contributorId":10780,"corporation":false,"usgs":true,"family":"Goerlitz","given":"Donald","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Law, LeRoy M.","contributorId":44899,"corporation":false,"usgs":true,"family":"Law","given":"LeRoy M.","affiliations":[],"preferred":false,"id":144631,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1812,"text":"wsp1763 - 1965 - Water resources of the Pascagoula area, Mississippi","interactions":[{"subject":{"id":56147,"text":"ofr5950 - 1959 - Water resources of the Pascagoula area, Mississippi--Progress report","indexId":"ofr5950","publicationYear":"1959","noYear":false,"title":"Water resources of the Pascagoula area, Mississippi--Progress report"},"predicate":"SUPERSEDED_BY","object":{"id":1812,"text":"wsp1763 - 1965 - Water resources of the Pascagoula area, Mississippi","indexId":"wsp1763","publicationYear":"1965","noYear":false,"title":"Water resources of the Pascagoula area, Mississippi"},"id":1}],"lastModifiedDate":"2022-03-22T18:52:56.479653","indexId":"wsp1763","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1763","title":"Water resources of the Pascagoula area, Mississippi","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1763","usgsCitation":"Harvey, E.J., Golden, H.G., and Jeffery, H.O., 1965, Water resources of the Pascagoula area, Mississippi: U.S. Geological Survey Water Supply Paper 1763, Report: vii, 135 p.; 16 Plates: 32.00 × 56.00 inches or smaller, https://doi.org/10.3133/wsp1763.","productDescription":"Report: vii, 135 p.; 16 Plates: 32.00 × 56.00 inches or smaller","costCenters":[],"links":[{"id":27003,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1763/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27002,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26991,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26990,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26989,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26988,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26987,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137174,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1763/report-thumb.jpg"},{"id":26996,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27000,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26999,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26997,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26995,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26994,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397413,"rank":19,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24940.htm"},{"id":26998,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27001,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26993,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26992,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1763/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Mississippi","otherGeospatial":"Pascagoula area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.393,\n 30.317\n ],\n [\n -88.885,\n 30.317\n ],\n [\n -88.885,\n 31\n ],\n [\n -88.393,\n 31\n ],\n [\n -88.393,\n 30.317\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602ba5","contributors":{"authors":[{"text":"Harvey, Edward Joseph","contributorId":32131,"corporation":false,"usgs":true,"family":"Harvey","given":"Edward","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":144195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Golden, Harold G.","contributorId":103244,"corporation":false,"usgs":true,"family":"Golden","given":"Harold","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144197,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jeffery, H. O.","contributorId":38132,"corporation":false,"usgs":true,"family":"Jeffery","given":"H.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":144196,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68421,"text":"ha189 - 1965 - Calcium, sodium, sulfate, and chloride in stream water of the western conterminous United States to 1957","interactions":[],"lastModifiedDate":"2017-02-21T10:28:05","indexId":"ha189","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"189","title":"Calcium, sodium, sulfate, and chloride in stream water of the western conterminous United States to 1957","docAbstract":"

This Hydrologic Atlas shows concentrations of calcium, sodium (or sodium plus potassium), sulfate, and chloride in stream water of 11 of the Western States, regardless of the sources from which the mineral constituents came. The maps are, in a sense, a historical summary, showing concentrations observed to 1956 and reported in published references. Data on chemical quality of stream water has been obtained at various times and at various places; for no single year does the record even approach complete coverage of the area shown on the maps. It was necessary, therefore, to combine the records of many years in order to achieve this summary.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha189","usgsCitation":"Feth, J.H., 1965, Calcium, sodium, sulfate, and chloride in stream water of the western conterminous United States to 1957: U.S. Geological Survey Hydrologic Atlas 189, 4 Plates: 37.50 x 45.00 inches or smaller, https://doi.org/10.3133/ha189.","productDescription":"4 Plates: 37.50 x 45.00 inches or smaller","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":188996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89944,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/189/plate-1.pdf","text":"Plate 1: Concentrations of calcium in stream water","size":"9.67 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":89945,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/189/plate-2.pdf","text":"Plate 2: Concentrations of sodium in stream water","size":"7.93 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":89946,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/189/plate-3.pdf","text":"Plate 3: Concentrations of sulfate in stream water","size":"7.13 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":89947,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/189/plate-4.pdf","text":"Plate 4: Concentrations of chloride in stream water","size":"7.12 MB","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2500000","country":"United States","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -122.75802,\n 49.002357\n ],\n [\n -122.821631,\n 48.941369\n ],\n [\n -122.673472,\n 48.733082\n ],\n [\n -122.535803,\n 48.776128\n ],\n [\n -122.425271,\n 48.599522\n ],\n [\n -122.534719,\n 48.574246\n ],\n [\n 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Frederick","affiliations":[],"preferred":false,"id":278188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68422,"text":"ha199 - 1965 - Preliminary map of the conterminous United States showing depth to and quality of shallowest ground water containing more than 1,000 parts per million dissolved solids","interactions":[{"subject":{"id":52382,"text":"ofr644 - 1964 - A reconnaissance of saline ground water in California","indexId":"ofr644","publicationYear":"1964","noYear":false,"title":"A reconnaissance of saline ground water in California"},"predicate":"SUPERSEDED_BY","object":{"id":68422,"text":"ha199 - 1965 - Preliminary map of the conterminous United States showing depth to and quality of shallowest ground water containing more than 1,000 parts per million dissolved solids","indexId":"ha199","publicationYear":"1965","noYear":false,"title":"Preliminary map of the conterminous United States showing depth to and quality of shallowest ground water containing more than 1,000 parts per million dissolved solids"},"id":1}],"lastModifiedDate":"2018-03-08T12:34:25","indexId":"ha199","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"199","title":"Preliminary map of the conterminous United States showing depth to and quality of shallowest ground water containing more than 1,000 parts per million dissolved solids","docAbstract":"

In this atlas, mineralized ground water is viewed presently as a source of water in some areas, but in much of the country as a source for future development. Mineralized water underlies large areas of the country, and its importance will grow as present supplies of fresh water are appropriated and developed. The potential uses fall in two main categories: (1) direct use in industrial processes, such as cooling, or for irrigation, where a moderate mineral content may not be a disadvantage; and (2) use after demineralization or dilution to whatever degree may be required by the intended user. It is clearly more efficient to produce and process water of moderate mineralization at points of use, where available in adequate amounts, than it is to process ocean water and pump it many miles from the sea.

\n

The Geological Survey, as a part of its responsibility to describe the water resources of the United States, has surveyed the known occurrences of mineralized ground water in the conterminous United States. The results are shown on the maps (sheets 1 and 2).

\n

This atlas was prepared to meet needs for information on the distribution and availability of mineralized water as expressed by Government agencies, private industries, and consultants. The maps are one step in providing an inventory of mineralized water of the Nation and will serve as a planning guide for further investigations and for development. They are necessarily generalized in many places owing to the complexity of the occurrence of the mineralized water, lack of detailed information for parts of the nation, and the difficulties inherent in attempts to put three-dimensional information on maps.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha199","usgsCitation":"Feth, J.H., 1965, Preliminary map of the conterminous United States showing depth to and quality of shallowest ground water containing more than 1,000 parts per million dissolved solids: U.S. Geological Survey Hydrologic Atlas 199, Document: 31 p.; 2 Plates: 63.17 x 40.84 inches and 63.06 x 40.83 inches, https://doi.org/10.3133/ha199.","productDescription":"Document: 31 p.; 2 Plates: 63.17 x 40.84 inches and 63.06 x 40.83 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true},{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":264331,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/199/plate-2.pdf","text":"Sheet 2: Chemical types of water","size":"11.51 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":264330,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/199/plate-1.pdf","text":"Sheet 1: Depth and distribution of mineralized water","size":"18.04 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":89948,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/199/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186609,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/199/report-thumb.jpg"}],"scale":"3000000","country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969e0","contributors":{"authors":[{"text":"Feth, John Henry Frederick","contributorId":37310,"corporation":false,"usgs":true,"family":"Feth","given":"John","email":"","middleInitial":"Henry Frederick","affiliations":[],"preferred":false,"id":278189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1810,"text":"wsp1697 - 1965 - Geology and ground water of the Tualatin Valley, Oregon","interactions":[{"subject":{"id":14012,"text":"ofr5559 - 1956 - Preliminary report on the ground-water resources of the Tualatin Valley, Oregon","indexId":"ofr5559","publicationYear":"1956","noYear":false,"title":"Preliminary report on the ground-water resources of the Tualatin Valley, Oregon"},"predicate":"SUPERSEDED_BY","object":{"id":1810,"text":"wsp1697 - 1965 - Geology and ground water of the Tualatin Valley, Oregon","indexId":"wsp1697","publicationYear":"1965","noYear":false,"title":"Geology and ground water of the Tualatin Valley, Oregon"},"id":1}],"lastModifiedDate":"2017-02-03T13:40:41","indexId":"wsp1697","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1697","title":"Geology and ground water of the Tualatin Valley, Oregon","docAbstract":"The Tualatin Valley proper consists of broad valley plains, ranging in altitude from 100 to 300 feet, and the lower mountain slopes of the drainage basin of the Tualatin River, a tributary of the Willamette River in northwestern Oregon. The valley is almost entirely farmed. Its population is increasing rapidly, partly because of the expansion of metropolitan Portland. \r\n\r\nStructurally, the bedrock of the basin is a saucer-shaped syncline almost bisected lengthwise by a ridge. The bedrock basin has been partly filled by alluvium, which underlies the valley plains. \r\n\r\nGround water occurs in the Columbia River basalt, a lava unit that forms the top several hundred feet of the bedrock, and also in the zones of fine sand in the upper part of the alluvial fill. It occurs under unconfined, confined, and perched conditions. Graphs of the observed water levels in wells show that the ground water is replenished each year by precipitation. The graphs show also that the amount and time of recharge vary in different aquifers and for different modes of ground-water occurrence. The shallower alluvial aquifers are refilled each year to a level where further infiltration recharge is retarded and water drains away as surface runoff. No occurrences of undue depletion of the ground water by pumping are known. The facts indicate that there is a great quantity of additional water available for future development. The ground water is developed for use by some spring works and by thousands of wells, most of which are of small yield. Improvements are now being made in the design of the wells in basalt and in the use of sand or gravel envelopes for wells penetrating the fine-sand aquifers. \r\n\r\nThe ground water in the basalt and the valley fill is in general of good quality, only slightly or moderately hard and of low salinity. Saline and mineralized water is present in the rocks of Tertiary age below the Columbia River basalt. Under certain structural and stratigraphic conditions this water of poor quality contaminates the fresh-water aquifers. \r\n\r\nDetailed hydrologic and geologic conditions are presented in 5 tables, 7 pictures, and 17 graphic figures and plates.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1697","usgsCitation":"Hart, D.H., and Newcomb, R.C., 1965, Geology and ground water of the Tualatin Valley, Oregon: U.S. Geological Survey Water Supply Paper 1697, v, 172 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1697.","productDescription":"v, 172 p. :ill., maps ;24 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":26969,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1697/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26970,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1697/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26971,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1697/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26972,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1697/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1697/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db68618e","contributors":{"authors":[{"text":"Hart, D. H.","contributorId":16811,"corporation":false,"usgs":true,"family":"Hart","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newcomb, R. C.","contributorId":77907,"corporation":false,"usgs":true,"family":"Newcomb","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144193,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":98,"text":"wsp1782 - 1965 - Ground-water levels in the United States, 1958-62, Northeastern states","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1782","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1782","title":"Ground-water levels in the United States, 1958-62, Northeastern states","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1782","usgsCitation":"Hackett, O.M., 1965, Ground-water levels in the United States, 1958-62, Northeastern states: U.S. Geological Survey Water Supply Paper 1782, v, 252 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1782.","productDescription":"v, 252 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136216,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1782/report-thumb.jpg"},{"id":24704,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1782/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675c1","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":141926,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1195,"text":"wsp1759B - 1965 - Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota","interactions":[{"subject":{"id":52316,"text":"ofr6324 - 1963 - Water resources in the vicinity of municipalities on the Western Mesabi Iron Range, northeastern Minnesota","indexId":"ofr6324","publicationYear":"1963","noYear":false,"title":"Water resources in the vicinity of municipalities on the Western Mesabi Iron Range, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":1195,"text":"wsp1759B - 1965 - Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota","indexId":"wsp1759B","publicationYear":"1965","noYear":false,"chapter":"B","title":"Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota"},"id":1}],"lastModifiedDate":"2016-05-06T10:48:02","indexId":"wsp1759B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1759","chapter":"B","title":"Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota","docAbstract":"

Additional supplies of water are available near the municipalities on the western Mesabi Iron Range. Potential yields from both ground-water and surface-water sources are good. The most productive aquifers for ground-water supplies are the Biwabik Iron-Formation and the stratified glacial drift. Areas of stratified drift believed to have good water potential have been outlined. The most abundant surface-water supplies in the area of this report are from the Mississippi River and its tributaries.

\n

The ground water is generally hard and has a high concentration of iron and manganese. The surface water is generally high in iron and is colored. Analyses of water from many sources are included.

\n

Data from many wells and test holes are given as are flow data for two discharge stations.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1759B","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Cotter, R.D., Young, H.L., Petri, L.R., and Prior, C.H., 1965, Water resources in the vicinity of municipalities on the western Mesabi Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 1759, Document: iv, 24 p.; Plate: 23 x 23 inches, https://doi.org/10.3133/wsp1759B.","productDescription":"Document: iv, 24 p.; Plate: 23 x 23 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":137954,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1759b/report-thumb.jpg"},{"id":26064,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1759b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26065,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1759b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.591667,\n 47.279167\n ],\n [\n -93.591667,\n 47.175\n ],\n [\n -93.5,\n 47.175\n ],\n [\n -93.5,\n 47.279167\n ],\n [\n -93.591667,\n 47.279167\n ]\n ]\n ]\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -93.45,\n 47.341667\n ],\n [\n -93.358333,\n 47.341667\n ],\n [\n -93.358333,\n 47.33333333\n ],\n [\n -93.216667,\n 47.33333333\n ],\n [\n -93.216667,\n 47.275\n ],\n [\n -93.358333,\n 47.275\n ],\n [\n -93.358333,\n 47.25\n ],\n [\n -93.45,\n 47.25\n ],\n [\n -93.45,\n 47.341667\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648597","contributors":{"authors":[{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143342,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143339,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petri, L. R.","contributorId":48944,"corporation":false,"usgs":true,"family":"Petri","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143340,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prior, C. H.","contributorId":57827,"corporation":false,"usgs":true,"family":"Prior","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143341,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1193,"text":"wsp1759F - 1965 - Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","interactions":[{"subject":{"id":52314,"text":"ofr6322 - 1963 - Water resources in the vicinity of municipalities on the Eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","indexId":"ofr6322","publicationYear":"1963","noYear":false,"title":"Water resources in the vicinity of municipalities on the Eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":1193,"text":"wsp1759F - 1965 - Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","indexId":"wsp1759F","publicationYear":"1965","noYear":false,"chapter":"F","title":"Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota"},"id":1}],"lastModifiedDate":"2021-11-02T21:27:50.468028","indexId":"wsp1759F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1759","chapter":"F","title":"Water resources in the vicinity of municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range, northeastern Minnesota","docAbstract":"

Additional supplies of water are available near the municipalities on the eastern Mesabi Iron Range and the Vermilion Iron Range. On the eastern Mesabi Range the potential for additional development of both ground-water and surface-water supplies are good, and on the Vermilion Range the best potential for development is from surface-water resources.

\n

The most productive aquifers in the area of this report are the Biwabik Iron-Formation and the stratified glacial drift; Bast of Colby Lake the Biwabik Iron-Formation is not an important aquifer, and it is entirely absent on the Vermilion Range. Also, on the Vermilion Range the glacial drift is generally too thin to yield the quantities of water found on the Mesabi Range.

\n

Surface-water supplies in the area of this report are good. An extensive network of river systems and many lakes form a large untapped potential supply. Records of flow from eight gaging stations are presented as are data from many wells and test holes.

\n

Ground water commonly has a high concentration of iron and manganese and is hard. Surface water generally has a high concentration of iron and is colored. Analyses of water from many sources are included.

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Additional supplies of water are available near the municipalities or the west-central Mesabi Iron Range. The largest sources are the ground-water aquifers in the Biwabik Iron-Formation and the stratified glacial drift. Areas of stratified drift that probably have good water potential have been outlined. Surface-water supplies are negligible in the eastern part of this area but increase toward the west. Flow records from one gaging station, results of discharge measurements at two miscellaneous sites, and data from many wells and test holes are presented.

\n

Most of the ground water is hard and has a high concentration of iron and manganese. The surface water generally has a high concentration of. iron and is colored. Analyses of water from many sources are .shown.

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Additional supplies of water are available near the municipalities on the central Mesabi Iron Range. Ground water presents the greatest potential yield, and most of the productive aquifers are in the Biwabik Iron-Formation and the stratified glacial drift. /k single body of ice-contact stratified drift underlies parts of all but one of the five municipality areas mapped. Surface-water supplies are generally inadequate. The Two River system in the eastern part of the area of this report offers some possibilities. Flow data from one discharge station and one miscellaneous gaging site are presented.

\n

Analyses of water from many sources are presented as are data from many wells and test holes. Ground water commonly has a concentration of high iron and manganese and is hard. Surface water generally has a high concentration of iron and is colored.

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D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143346,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143343,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petri, L. R.","contributorId":48944,"corporation":false,"usgs":true,"family":"Petri","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143344,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prior, C. 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It ranks high among the more awesome gorges of North America.\r\n\r\nMany great western canyons are as well remembered for their brightly colored walls as for their airy depths. Not so the Black Canyon. Though it is assuredly not black, the dark-gray tones of its walls and the hazy shadows of its gloomy depths join together to make its name well deserved. Its name conveys an impression, not a picture.\r\n\r\nAfter the first emotional impact of the canyon, the same questions come to the minds of most reflective viewers and in about the following order: How deep is the Black Canyon, how wide, how does it compare with other canyons, what are the rocks, how did it form, and how long did it take? Several western canyons exceed the Black Canyon in overall size. Some are longer; some are deeper; some are narrower; and a few have walls as steep. But no other canyon in North American combines the depth, narrowness, sheerness, and somber countenance of the Black Canyon.\r\n\r\nIn many places the Black Canyon is as deep as it is wide. Between The Narrows and Chasm View in the Black Canyon of the Gunnison National Monument (fig. 15) it is much deeper than wide. Average depth in the monument is about 2,000 feet, ranging from a maximum of about 2,700 feet, north of Warner Point (which also is the greatest depth anywhere in the canyon), to a minimum of about 1,750 feet at The Narrows. The stretch of canyon between Pulpit Rock and Chasm View, including The Narrows, though the shallowest in the monument, is also the narrowest, has some of the steepest walls, and is, therefore, among the most impressive segments of the canyon (fig. 3).\r\n\r\nProfiles of several well-known western canyons are shown in figure 1. Deepest of these by far is Hells Canyon of the Snake, on the Idaho-Oregon border. Clearly, it dwarfs the Black Canyon in the immensity of its void, though its flaring walls lack the alarming verticality of the Black Canyon. Arizona's Grand Canyon of the Colorado is acknowledged as the greatest of them all; it is not as deep as Hells Canyon, but it is wider, longer, more rugged, and far more colorful. Its depth is two to three times that of the Black Canyon. Zion Canyon, Utah, combines depth, sheerness, serenity, and color in a chasm that ranges from capacious to extremely narrow. Its Narrows have a depth-to-width ratio unmatched by any other major American canyon.\r\n\r\nCalifornia's Yosemite Valley, in a setting of sylvan verdure, is unique among the gorges shown in profile in figure 1 in being the only glacial trough; its monolithic walls bear witness to the abrasive power of moving ice. Few cliffs in the world match the splendor of its El Capitan. Lodore Canyon, on the Green River in Dinosaur National Monument, Colorado, is best known, perhaps, for its noisy splashy rapids, first made famous by John Wesley Powell. Lodore Canyon also features towering cliffs of deep-red quartzite. Grand Canyon of the Yellowstone River, Wyoming, is noted for its great waterfalls, dashing river, and bright coloration. The Royal Gorge of the Arkansas River, Colorado, features the 'world's highest suspension bridge'.\r\n\r\nThe profiles shown in figure 1 afford some basis for comparing one canyon with another. They cannot abstract in two dimensions the overall impression that each canyon makes. Color, vegetation, outcrop habit, vantage point, season of year, length of visit - even the roar of the river or lack thereof - all contribute to this highly personal effect.\r\n\r\nFor a river of its size, the Gunnison has an unusually steep gradient through the Black Canyon. The river falls about 2,150 feet from the head of the canyon at Sapinero to the mouth at its junction with North Fork - a distance of about 50 miles and an average rate of fall of about 43 feet per mile. By comparison, the Green ","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/b1191","usgsCitation":"Hansen, W.R., 1965, The Black Canyon of the Gunnison: Today and Yesterday: U.S. Geological Survey Bulletin 1191, vii, 76 p., https://doi.org/10.3133/b1191.","productDescription":"vii, 76 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":92844,"rank":299,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1191/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1191/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db6828eb","contributors":{"authors":[{"text":"Hansen, Wallace R.","contributorId":90273,"corporation":false,"usgs":true,"family":"Hansen","given":"Wallace","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":213253,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":183,"text":"wsp1642 - 1965 - Quality of surface waters of the United States, 1959, Parts 3 & 4, Ohio River Basin and St. Lawrence River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1642","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1642","title":"Quality of surface waters of the United States, 1959, Parts 3 & 4, Ohio River Basin and St. Lawrence River Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1642","usgsCitation":"Love, S.K., 1965, Quality of surface waters of the United States, 1959, Parts 3 & 4, Ohio River Basin and St. Lawrence River Basin: U.S. Geological Survey Water Supply Paper 1642, x, 303 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1642.","productDescription":"x, 303 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":136327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1642/report-thumb.jpg"},{"id":24794,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1642/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651cb1","contributors":{"authors":[{"text":"Love, S. 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Additional supplies of water are available near the municipalities on the east-central Mesabi Iron Range. Both ground water and surface water offer good potential supplies. For the ground-water supplies, the most productive aquifers are the Biwabik Iron Formation and the stratified glacial drift. Surface-water supplies are variable. Streams in the western part of the report area are too small to yield supplies of importance, but lakes are a good potential supply. Eveleth and Gilbert are the only towns presently utilizing this source. In the eastern part of the area of this report, the Pike and Embarrass Rivers offer good potential supplies. Flow records from two gaging stations are presented as are data from many wells and test holes. Surface water generally has a high concentration of iron and is colored. Most ground water has a high concentration of iron and manganese and is hard. Analyses of water from many sources are presented.

","language":"English","publisher":"U.S. Government Publishing Office","publisherLocation":"Washington, DC","doi":"10.3133/wsp1759E","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Cotter, R.D., Young, H.L., Petri, L.R., and Prior, C.H., 1965, Water resources in the vicinity of municipalities on the east-central Mesabi Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 1759, Document: iv, 23 p.; Plate: 28.00 x 27.25 inches, https://doi.org/10.3133/wsp1759E.","productDescription":"Document: iv, 23 p.; Plate: 28.00 x 27.25 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":137956,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1759e/report-thumb.jpg"},{"id":26068,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1759e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1759e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -92.6,\n 47.583333\n ],\n [\n -92.6,\n 47.491667\n ],\n [\n -92.583333,\n 47.491667\n ],\n [\n -92.583333,\n 47.391667\n ],\n [\n -92.491667,\n 47.391667\n ],\n [\n -92.491667,\n 47.441667\n ],\n [\n -92.375,\n 47.441667\n ],\n [\n -92.375,\n 47.5\n ],\n [\n -92.3,\n 47.5\n ],\n [\n -92.3,\n 47.558333\n ],\n [\n -92.458333,\n 47.558333\n ],\n [\n -92.458333,\n 47.5\n ],\n [\n -92.491667,\n 47.5\n ],\n [\n -92.491667,\n 47.491667\n ],\n [\n -92.508333,\n 47.491667\n ],\n [\n -92.508333,\n 47.583333\n ],\n [\n -92.6,\n 47.583333\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f08db","contributors":{"authors":[{"text":"Cotter, R. D.","contributorId":89874,"corporation":false,"usgs":true,"family":"Cotter","given":"R.","email":"","middleInitial":"D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, H. L.","contributorId":23922,"corporation":false,"usgs":true,"family":"Young","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143347,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Petri, L. R.","contributorId":48944,"corporation":false,"usgs":true,"family":"Petri","given":"L.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143348,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Prior, C. 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Print. Off.,","doi":"10.3133/wsp1641","usgsCitation":"Love, S.K., 1965, Quality of surface waters of the United States, 1959, Parts 1 & 2, North Atlantic slope basins and South Atlantic slope and eastern Gulf of Mexico Basins: U.S. Geological Survey Water Supply Paper 1641, xi, 460 p. :map ; 24 cm., https://doi.org/10.3133/wsp1641.","productDescription":"xi, 460 p. :map ; 24 cm.","costCenters":[],"links":[{"id":136924,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1641/report-thumb.jpg"},{"id":26556,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1641/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651b64","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":143766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1458,"text":"wsp1790B - 1965 - Summary of floods in the United States during 1960","interactions":[],"lastModifiedDate":"2017-09-06T16:10:09","indexId":"wsp1790B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1790","chapter":"B","title":"Summary of floods in the United States during 1960","docAbstract":"

This report describes the most outstanding floods in the United States during 1960. No major floods occurred during the year, although two floods caused severe damage the first in March and April in eastern Nebraska and adjacent areas, and the second in September in Puerto Rico.

Unseasonal rains in mid-March caused extensive flooding in north-central Florida. Several thousand persons were evacuated from their homes, and damage to homes, roads, and crops was extensive.

The most widespread flooding ever known in Nebraska occurred late in March and early in April as a result of rapid melting of a heavy snow cover. Most of the flood damage, estimated at about $3 million, was to roads and bridges. The flood area extended into South Dakota, Iowa, Kansas, Missouri, and Wisconsin.

Snowmelt in April supplemented by rains and later heavy rains in early May caused severe flooding in northern Wisconsin and in Michigan Upper Peninsula.

The most destructive flood of the year was in eastern Puerto Rico as the result of hurricane Donna. More than one hundred persons died, and considerably more than one hundred persons were injured; property damage was f.bout $7 million. Hurricane Donna also caused severe flooding as it passed over Florida and along the Atlantic coastline.

In addition to these floods mentioned, 31 others of lesser magnitude were significant enough to report in this annual summary.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1790B","collaboration":"Prepared in cooperation with Federal, State, and local agencies","usgsCitation":"Rostvedt, J., 1965, Summary of floods in the United States during 1960: U.S. Geological Survey Water Supply Paper 1790, vi, 147 p., https://doi.org/10.3133/wsp1790B.","productDescription":"vi, 147 p.","numberOfPages":"150","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":26550,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1790b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1790b/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699277","contributors":{"authors":[{"text":"Rostvedt, J.O.","contributorId":24757,"corporation":false,"usgs":true,"family":"Rostvedt","given":"J.O.","email":"","affiliations":[],"preferred":false,"id":143748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52481,"text":"ofr65102 - 1965 - Depth to water measurements in wells in the alluvium of the Arkansas River valley between Little Rock, Arkansas, and the Mississippi River: Vol. I, Arkansas County; Vol. II, Desha County; Vol. III, Jefferson and Lincoln Counties; and Vol. IV, Lonoke, Pulaski, and Saline Counties","interactions":[],"lastModifiedDate":"2012-02-02T00:11:27","indexId":"ofr65102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-102","title":"Depth to water measurements in wells in the alluvium of the Arkansas River valley between Little Rock, Arkansas, and the Mississippi River: Vol. I, Arkansas County; Vol. II, Desha County; Vol. III, Jefferson and Lincoln Counties; and Vol. IV, Lonoke, Pulaski, and Saline Counties","language":"ENGLISH","doi":"10.3133/ofr65102","usgsCitation":"May, J., Yanchosek, J., Bedinger, M.S., and Emmett, L.F., 1965, Depth to water measurements in wells in the alluvium of the Arkansas River valley between Little Rock, Arkansas, and the Mississippi River: Vol. I, Arkansas County; Vol. II, Desha County; Vol. III, Jefferson and Lincoln Counties; and Vol. IV, Lonoke, Pulaski, and Saline Counties: U.S. Geological Survey Open-File Report 65-102, 197 p., https://doi.org/10.3133/ofr65102.","productDescription":"197 p.","costCenters":[],"links":[{"id":179710,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab1e4b07f02db66deef","contributors":{"authors":[{"text":"May, J.R.","contributorId":67158,"corporation":false,"usgs":true,"family":"May","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":245418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yanchosek, J.J.","contributorId":57146,"corporation":false,"usgs":true,"family":"Yanchosek","given":"J.J.","affiliations":[],"preferred":false,"id":245416,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":245417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Emmett, L. F.","contributorId":43332,"corporation":false,"usgs":true,"family":"Emmett","given":"L.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":245415,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1328,"text":"wsp1809S - 1965 - Suitability of irrigation water and changes in ground-water quality in the Lompoc subarea of the Santa Ynez River Basin, Santa Barbara County, California","interactions":[],"lastModifiedDate":"2015-02-19T08:59:47","indexId":"wsp1809S","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"1809","chapter":"S","title":"Suitability of irrigation water and changes in ground-water quality in the Lompoc subarea of the Santa Ynez River Basin, Santa Barbara County, California","docAbstract":"

Analyses of water samples collected since 1934 from some of the irrigation wells in the Lompoc subarea of the Santa Ynes River valley have shown a gradual deterioration in the chemical quality of the water.

\n

Most of the ground water pumped in the subarea has a dissolved-solids contents ranging from about 700 to about 2,000 parts per million, of which sulfate and chloride are the predominant constituents.  Suitability of the water for irrigation is variable and is dependent principally on \"potential salinity\" of the water, soil permeability, and type of crop.

\n

Changes in water quality are not consistent throughout the subarea.  No doubt the chloride concentration increases as a result of both the recycling irrigation water and inflow of high-chloride low-sulfate connate water from the consolidated Tertiary rocks.  The influence of recycled irrigation water is indicated by increase concentrations of chloride and sulfate in a ratio of 1:2.  Inflow of high-chloride low-sulfate connate water is indicated by increased chloride concentration correlated with little or no change in sulfate concentration.  Peak chloride concentrations in three local areas are probably the result of the inflow of connate water.  Furthermore, ground-water gradients in each of the local areas are favorable for inflow from the consolidated rocks.

","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1809S","usgsCitation":"Evenson, R.E., 1965, Suitability of irrigation water and changes in ground-water quality in the Lompoc subarea of the Santa Ynez River Basin, Santa Barbara County, California: U.S. Geological Survey Water Supply Paper 1809, iii, 20 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1809S.","productDescription":"iii, 20 p. :ill., maps ;24 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":26380,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809s/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26381,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809s/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26382,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1809s/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26383,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1809s/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1809s/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db6998a2","contributors":{"authors":[{"text":"Evenson, R. E.","contributorId":19933,"corporation":false,"usgs":true,"family":"Evenson","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143570,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68648,"text":"ha198 - 1965 - Water resources of the Appalachian region, Pennsylvania to Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:13:39","indexId":"ha198","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"198","title":"Water resources of the Appalachian region, Pennsylvania to Alabama","language":"ENGLISH","doi":"10.3133/ha198","usgsCitation":"Schneider, W.J., 1965, Water resources of the Appalachian region, Pennsylvania to Alabama: U.S. Geological Survey Hydrologic Atlas 198, 11 maps :col. ;each sheet 59 x 76 cm. in folder 30 x 24 cm., https://doi.org/10.3133/ha198.","productDescription":"11 maps :col. ;each sheet 59 x 76 cm. in folder 30 x 24 cm.","costCenters":[],"links":[{"id":252277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/198/report-thumb.jpg"},{"id":251464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/198/report.pdf","size":"47714","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49b1e4b07f02db5c92b7","contributors":{"authors":[{"text":"Schneider, William J.","contributorId":47349,"corporation":false,"usgs":true,"family":"Schneider","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278635,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15688,"text":"ofr65138 - 1965 - The validity of geologic projection, a successful example: the Straight Creek Tunnel pilot bore, Colorado","interactions":[{"subject":{"id":15688,"text":"ofr65138 - 1965 - The validity of geologic projection, a successful example: the Straight Creek Tunnel pilot bore, Colorado","indexId":"ofr65138","publicationYear":"1965","noYear":false,"title":"The validity of geologic projection, a successful example: the Straight Creek Tunnel pilot bore, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":25017,"text":"pp815 - 1974 - Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado","indexId":"pp815","publicationYear":"1974","noYear":false,"title":"Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado"},"id":1}],"supersededBy":{"id":25017,"text":"pp815 - 1974 - Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado","indexId":"pp815","publicationYear":"1974","noYear":false,"title":"Engineering geologic, geophysical, hydrologic, and rock-mechanics investigations of the Straight Creek Tunnel site and pilot bore, Colorado"},"lastModifiedDate":"2018-09-10T09:59:50","indexId":"ofr65138","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-138","title":"The validity of geologic projection, a successful example: the Straight Creek Tunnel pilot bore, Colorado","docAbstract":"

Projection of details of surface geology to depth prior to construction has met with only limited success in many tunneling operations. in the Straight Creek Tunnel pilot bore good results were obtained by making predictions of the extent and kinds but not the exact locations of conditions that could be expected at tunnel level based on a statistical study of surface features.

Successful predictions were made regarding percentages of rock types, linear feet of faulted and sheared rocks, and attitudes of foliation and fractures, including faults and joints. Predicted rock loads and final swell pressures in gouge and altered rocks agreed well with actual measurements. Ground water flows were encountered in expected amounts, but criteria for estimations proved to be unsound.

Estimates were made of the amount of temporary support, footage of exploratory feeler holes, and amounts of grouting and provided a sound basis for estimating total tunneling coats.

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