{"pageNumber":"2395","pageRowStart":"59850","pageSize":"25","recordCount":68839,"records":[{"id":41726,"text":"ofr74128 - 1974 - Aeromagnetic map of parts of the Chiricahua Peak and Portal quadrangles, Cochise County, Arizona","interactions":[],"lastModifiedDate":"2021-12-28T20:18:35.939335","indexId":"ofr74128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-128","title":"Aeromagnetic map of parts of the Chiricahua Peak and Portal quadrangles, Cochise County, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74128","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Aeromagnetic map of parts of the Chiricahua Peak and Portal quadrangles, Cochise County, Arizona: U.S. Geological Survey Open-File Report 74-128, 1 Plate: 20.90 × 31.94 inches, https://doi.org/10.3133/ofr74128.","productDescription":"1 Plate: 20.90 × 31.94 inches","costCenters":[],"links":[{"id":168264,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393540,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15001.htm"},{"id":79438,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0128/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Arizona","county":"Cochise County","otherGeospatial":"Chiricahua Peak and Portal quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.417,\n              31.733\n            ],\n            [\n              -109.167,\n              31.733\n            ],\n            [\n              -109.167,\n              32\n            ],\n            [\n              -109.417,\n              32\n            ],\n            [\n              -109.417,\n              31.733\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6976ca","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530589,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26707,"text":"wri7342 - 1974 - Flood profiles and inundated areas along the Lower Nisqually River, Washington","interactions":[],"lastModifiedDate":"2018-11-02T14:08:49","indexId":"wri7342","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-42","title":"Flood profiles and inundated areas along the Lower Nisqually River, Washington","docAbstract":"<p>Nisqually River flood profiles, covering the reach from near the river mouth to river mile 6.4, were developed in a 2-year field study (1970-72) as part of a continuing program with the State of Washington Department of Ecology. The main channel of the reach will convey without overflow discharges as large as about 21,000 cubic feet per second, which have a 6-year recurrence interval. The banks in some areas will be overtopped at 25,500 cubic feet per second, which has a 13-year recurrence interval. The areas where overbank flooding will first occur, and water-surface profiles of a 3.4-year and 100-year flood were determined for six flood-profile stations. The largest flood for which data are available was that of December 1933; the approximate area that would be presently inundated by such a flood is shown. Alder and La Grande Reservoirs can reduce the magnitude of lower annual flood peaks downstream to some extent, but insufficient data are available to predict their effects on very large floods.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7342","usgsCitation":"Cummans, J., 1974, Flood profiles and inundated areas along the Lower Nisqually River, Washington: U.S. Geological Survey Water-Resources Investigations Report 73-42, iii, 9 p., https://doi.org/10.3133/wri7342.","productDescription":"iii, 9 p.","costCenters":[],"links":[{"id":158369,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":" https://pubs.usgs.gov/wri/1973/0042/report-thumb.jpg"},{"id":359120,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Lower Nisqually River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.67,\n              47.0833\n            ],\n            [\n              -122.7083,\n              47.0833\n            ],\n            [\n              -122.7083,\n              47.0417\n            ],\n            [\n              -122.67,\n              47.0417\n            ],\n            [\n              -122.67,\n              47.0833\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eeb50","contributors":{"authors":[{"text":"Cummans, J. E.","contributorId":24767,"corporation":false,"usgs":true,"family":"Cummans","given":"J. E.","affiliations":[],"preferred":false,"id":196859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68266,"text":"ha510 - 1974 - Reconnaissance investigation of ground water in the Rio Grande drainage basin, with special emphasis on saline ground-water resources","interactions":[],"lastModifiedDate":"2022-12-28T20:57:01.97667","indexId":"ha510","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"510","title":"Reconnaissance investigation of ground water in the Rio Grande drainage basin, with special emphasis on saline ground-water resources","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha510","usgsCitation":"Kelly, T.E., 1974, Reconnaissance investigation of ground water in the Rio Grande drainage basin, with special emphasis on saline ground-water resources: U.S. Geological Survey Hydrologic Atlas 510, 4 Plates: 57.00 x 41.96 inches or smaller, https://doi.org/10.3133/ha510.","productDescription":"4 Plates: 57.00 x 41.96 inches or smaller","costCenters":[],"links":[{"id":411143,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15900.htm","linkFileType":{"id":5,"text":"html"}},{"id":89668,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/510/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89667,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/510/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188472,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89669,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/510/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89670,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/510/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2500000","country":"United States","state":"Colorado, Kansas, New Mexico, Oklahoma, Texas","otherGeospatial":"Rio Grande basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.5,\n              38\n            ],\n            [\n              -108.5,\n              26\n            ],\n            [\n              -97.5,\n              26\n            ],\n            [\n              -97.5,\n              38\n            ],\n            [\n              -108.5,\n              38\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63ebe4","contributors":{"authors":[{"text":"Kelly, T. E.","contributorId":63824,"corporation":false,"usgs":true,"family":"Kelly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":277934,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27916,"text":"wri744 - 1974 - Availability of ground water in the Blackstone River area Rhode Island and Massachusetts","interactions":[],"lastModifiedDate":"2013-12-13T15:44:16","indexId":"wri744","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-4","title":"Availability of ground water in the Blackstone River area Rhode Island and Massachusetts","docAbstract":"The Blackstone River study area covers 83 square miles of northern Rhode Island and 5 square miles of adjacent Massachusetts (fig. 1). It includes parts of the Blackstone, Moshassuck, and Tenmile River basins, and a coastal area that drains to the brackish Seekonk and Providence Rivers. In Rhode Island, all or parts of the suburban towns of Cumberland, Lincoln, North Smithfield, and Smithfield and all or parts of the cities of Central Falls, East Povidence, Pawtucket, Providence, and Woonsocket are within the study area. Also included are parts of the towns Attleboro and North Attleborough in Massachusetts. In 1970, total population was about 240,000, which was equivalent to about one-fourth of the total population of Rhode Island. Fresh water usage in 1970 by public-supply systems and self-supplied industry was about 33 mgd (million gallons per day), which was equal to 22 percent of total fresh water use in Rhode Island for all purposes except generation of electric power (fig. 2). Anticipated increases in population and per capita water requirements are likely to cause the demand for water to more than double within the next 50 years. A significant part of this demand can be met from wells that tap the principal streams. This aquifer yielded an average of 10 mgd in 1970 and is capable of sustaining a much higher yield. The primary objectives of the study were to determine and map the saturated thickness and transmissivity of the stratified-drift aquifer and to assess the potential sustained yield of those parts of the aquifer favorable for large-scale development of water. A secondary objective was to describe ground-water quality and to evaluate the impact of induced infiltration of polluted stream water on the quality of native ground water. This report is based on analysis of drillers' records of more than 700 wells and borings which include 462 lithologic logs; 35 specific-capacity determinations; 12 aquifer tests, including detailed tests at two sites to determine streambed infiltration rates; chemical analyses of 92 ground-water and 15 stream-water samples; and geologic mapping. Selected base data are published in a separate (Johnston and Dickerman, in press). The authors are indebted to well drillers, especially American Drilling and Boring Company, R.E. Chapman Company, and Layne New England Company, for making their records available; to the water departments of the towns of Cumberland and Lincoln, for allowing aquifer tests of their well fields; to the Rhode Island Department of Health, for providing data on water quality and use; and to many other federal, state, and municipal agencies, companies, and individuals who supplied information. Their contributions are gratefully acknowledged.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri744","collaboration":"Prepared in cooperation with Rhode Island Water Resources Board","usgsCitation":"Johnston, H.E., and Dickerman, D.C., 1974, Availability of ground water in the Blackstone River area Rhode Island and Massachusetts: U.S. Geological Survey Water-Resources Investigations Report 74-4, 2 Plates: 41.74 x 50.88 and 41.40 x 50.46 inches, https://doi.org/10.3133/wri744.","productDescription":"2 Plates: 41.74 x 50.88 and 41.40 x 50.46 inches","costCenters":[],"links":[{"id":158655,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0004/report-thumb.jpg"},{"id":279495,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0004/plate-2.pdf"},{"id":279494,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0004/plate-1.pdf"}],"country":"United States","state":"Massachusetts;Rhode Island","otherGeospatial":"Blackstone River Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.566667,41.75 ], [ -71.566667,42.0 ], [ -71.333333,42.0 ], [ -71.333333,41.75 ], [ -71.566667,41.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660474","contributors":{"authors":[{"text":"Johnston, Herbert E.","contributorId":16392,"corporation":false,"usgs":true,"family":"Johnston","given":"Herbert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":198894,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickerman, David C.","contributorId":41047,"corporation":false,"usgs":true,"family":"Dickerman","given":"David","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":198895,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27917,"text":"wri7418 - 1974 - Availability of ground water in the Branch River basin; Providence County, Rhode Island","interactions":[],"lastModifiedDate":"2015-12-03T12:43:06","indexId":"wri7418","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-18","title":"Availability of ground water in the Branch River basin; Providence County, Rhode Island","docAbstract":"<p>Stratified glacial drift consisting largely of sand and gravel constitutes the only aquifer capable of supporting continuous yields of 100 gpm (6.3 1/s) or more to individual wells. The aquifer covers about a third of the 79 mi 2 (205 km2) study area, occurring mainly in stream valleys that are less than a mi le wide. Its saturated thickness is commonly 40 to 60ft (12 to 18 m); its transmissivity is commonly 5,000 to 8,000 ft 2/day (460 to 740m2 /day). The aquifer is hydraulically connected to streams that cross it and much of the water from heavily pumped wells will consist of infiltration induced from them. Potential sustained yield from most parts of the aquifer is limited chiefly by the rate at which infiltration can be induced from streams or low streamflow, whichever is smaller. Ground-water withdrawals deplete streamflow; and if large-scale development of ground water is not carefully planned and managed, periods of no streamflow may result during dry weather. Potential sustained yield varies with the scheme of well development, and is evaluated for selected areas by mathematically simulating pumping from assumed schemes of well Is in models of the stream-aquifer system. Results indicate that sustained yields of 5.5, 3.4, 1.6, and 1.3 mgd (0.24, 0.15, 0.07, and 0.06 m3 /s) can be obtained from the stratified-drift aquifer near Slatersville, Oakland, Harrisville, and Chepachet, respectively. Pumping at these rates will not cause streams to go dry, if the water is returned to streams near points of withdrawal. A larger ground-water yield can be obtained, if periods of no streamflow along reaches of principal streams are acceptable. Inorganic chemical quality of water in the stream-aquifer system is suitable for most purposes; the water is soft, slightly acidic, and generally contains less than 100 milligrams per litre of dissolved sol ids. Continued good quality ground water depends on maintenance of good quality of water in streams, because much of the water pumped from wells will be infiltrated from streams.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7418","collaboration":"Prepared in cooperation with the Rhode Island Water Resources Board","usgsCitation":"Johnston, H., and Dickerman, D., 1974, Availability of ground water in the Branch River basin; Providence County, Rhode Island: U.S. Geological Survey Water-Resources Investigations Report 74-18, Report: v, 39 p.; 1 Plate: 34.54 x 39.14 inches, https://doi.org/10.3133/wri7418.","productDescription":"Report: v, 39 p.; 1 Plate: 34.54 x 39.14 inches","numberOfPages":"46","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":158656,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri7418.jpg"},{"id":311731,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0018/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":311732,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0018/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Rhode Island","county":"Providence County","otherGeospatial":"Branch River","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-71.4983,42.0169],[-71.4266,42.0187],[-71.3797,42.0191],[-71.3806,41.985],[-71.3817,41.9427],[-71.3824,41.8915],[-71.3386,41.8983],[-71.3373,41.8937],[-71.3386,41.891],[-71.3398,41.8874],[-71.3392,41.8824],[-71.3368,41.8733],[-71.3356,41.8678],[-71.3337,41.861],[-71.3331,41.8574],[-71.3337,41.8538],[-71.3356,41.8497],[-71.3387,41.8429],[-71.3393,41.841],[-71.3387,41.8392],[-71.3381,41.8374],[-71.3369,41.8351],[-71.3369,41.8329],[-71.3387,41.8302],[-71.3406,41.8279],[-71.3437,41.8242],[-71.3437,41.8211],[-71.3443,41.8174],[-71.3425,41.8129],[-71.3406,41.8093],[-71.3406,41.8056],[-71.3406,41.8029],[-71.3406,41.7997],[-71.3394,41.797],[-71.3376,41.7952],[-71.3345,41.7925],[-71.3314,41.7897],[-71.3302,41.7865],[-71.329,41.7838],[-71.3271,41.7811],[-71.3259,41.7793],[-71.318,41.7759],[-71.3518,41.7534],[-71.3537,41.7502],[-71.3604,41.7493],[-71.3604,41.7566],[-71.3635,41.7625],[-71.3684,41.7638],[-71.3715,41.767],[-71.3672,41.7761],[-71.3696,41.7829],[-71.3727,41.7911],[-71.377,41.7993],[-71.3868,41.807],[-71.388,41.8083],[-71.3862,41.8147],[-71.3812,41.8224],[-71.3744,41.8324],[-71.3701,41.8401],[-71.3695,41.8474],[-71.3689,41.8533],[-71.375,41.8583],[-71.3806,41.8506],[-71.3812,41.8469],[-71.3824,41.8429],[-71.3825,41.8392],[-71.3855,41.8356],[-71.388,41.8306],[-71.393,41.8179],[-71.3966,41.8174],[-71.4028,41.8197],[-71.4047,41.8179],[-71.3985,41.8065],[-71.3967,41.8025],[-71.393,41.7997],[-71.3887,41.7984],[-71.3856,41.7952],[-71.3838,41.7929],[-71.3844,41.7902],[-71.3887,41.787],[-71.3893,41.782],[-71.3881,41.7752],[-71.3863,41.7689],[-71.385,41.7639],[-71.3857,41.7607],[-71.3881,41.7634],[-71.3924,41.7666],[-71.3979,41.7711],[-71.3998,41.7707],[-71.4016,41.768],[-71.409,41.7671],[-71.4146,41.7648],[-71.4177,41.7639],[-71.4207,41.7648],[-71.4244,41.7607],[-71.4306,41.7603],[-71.4343,41.7607],[-71.4373,41.7598],[-71.4392,41.7575],[-71.441,41.7539],[-71.4417,41.7525],[-71.4435,41.7516],[-71.446,41.7498],[-71.446,41.748],[-71.4447,41.7421],[-71.4472,41.7394],[-71.4521,41.7358],[-71.4583,41.7308],[-71.6102,41.7275],[-71.7904,41.7232],[-71.7937,41.8154],[-71.7963,41.9184],[-71.7968,41.9376],[-71.7971,41.9588],[-71.7979,42.0089],[-71.6681,42.0122],[-71.5588,42.0153],[-71.5366,42.0159],[-71.4983,42.0169]]]},\"properties\":{\"name\":\"Providence\",\"state\":\"RI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e241","contributors":{"authors":[{"text":"Johnston, H.E.","contributorId":27070,"corporation":false,"usgs":true,"family":"Johnston","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":198896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dickerman, D.C.","contributorId":48601,"corporation":false,"usgs":true,"family":"Dickerman","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":198897,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68537,"text":"ha538 - 1974 - Ground-water conditions in the Franklin area, southeastern Virginia","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha538","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"538","title":"Ground-water conditions in the Franklin area, southeastern Virginia","language":"ENGLISH","doi":"10.3133/ha538","usgsCitation":"Brown, G.A., and Cosner, O.J., 1974, Ground-water conditions in the Franklin area, southeastern Virginia: U.S. Geological Survey Hydrologic Atlas 538, 2 col. maps ;45 x 59 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha538.","productDescription":"2 col. maps ;45 x 59 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":186124,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90149,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/538/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90150,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/538/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90151,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/538/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96.5,36.5 ], [ -96.5,37 ], [ -77.25,37 ], [ -77.25,36.5 ], [ -96.5,36.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d207","contributors":{"authors":[{"text":"Brown, G. Allen","contributorId":39460,"corporation":false,"usgs":true,"family":"Brown","given":"G.","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":278418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cosner, O. J.","contributorId":19587,"corporation":false,"usgs":true,"family":"Cosner","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278417,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42043,"text":"ofr741102 - 1974 - Aeromagnetic map of eastern half of the Beaver quadrangle, northeastern Alaska","interactions":[],"lastModifiedDate":"2022-08-01T20:10:01.397291","indexId":"ofr741102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-1102","title":"Aeromagnetic map of eastern half of the Beaver quadrangle, northeastern Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741102","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Aeromagnetic map of eastern half of the Beaver quadrangle, northeastern Alaska: U.S. Geological Survey Open-File Report 74-1102, 1 Plate: 25.26 x 25.86 inches, https://doi.org/10.3133/ofr741102.","productDescription":"1 Plate: 25.26 x 25.86 inches","costCenters":[],"links":[{"id":136582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79795,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1102/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"},"description":"Plate"},{"id":404600,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8857.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Alaska","otherGeospatial":"Beaver quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147,\n              66\n            ],\n            [\n              -148,\n              66\n            ],\n            [\n              -148,\n              67\n            ],\n            [\n              -147,\n              67\n            ],\n            [\n              -147,\n              66\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697e20","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530793,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56320,"text":"wdrMI731 - 1974 - Water resources data for Michigan, water year 1973; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2017-07-12T14:44:18","indexId":"wdrMI731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MI-73-1","title":"Water resources data for Michigan, water year 1973; Part 1, Surface water records","docAbstract":"<p>Surface-water records for the 1973 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Michigan are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of T.R. Cummings, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and Federal agencies in Michigan. </p><p>Records of discharge and stage of streams, and contents and stage of lakes or reservoirs are published in a series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States\". Through September 30, 1960, these water-supply papers were in an annual series and since then are in a 5-year series. Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Michigan are contained in Part 4 of that series. </p><p>Beginning with the 1961 water year, streamflow records and related data have been released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports is limited and primarily for local needs.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMI731","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Water resources data for Michigan, water year 1973; Part 1, Surface water records: U.S. Geological Survey Water Data Report MI-73-1, viii, 249 p., https://doi.org/10.3133/wdrMI731.","productDescription":"viii, 249 p.","numberOfPages":"262","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":343745,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1973/mi-73-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":180733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1973/mi-73-1/report-thumb.jpg"}],"country":"United 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,{"id":28989,"text":"wri7345 - 1974 - Base and thickness of the Post-Eocene continental deposits in the Sacramento Valley, California","interactions":[],"lastModifiedDate":"2018-10-29T13:43:43","indexId":"wri7345","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"73-45","title":"Base and thickness of the Post-Eocene continental deposits in the Sacramento Valley, California","docAbstract":"<p>The Sacramento Valley, which forms most of the northern one-third of the Central Valley, is a broad structural trough. The study area comprises the valley floor and some of the foothills of the Sierra Nevada and the Coast Ranges, a total area of about 6,000 square miles.</p><p>Beneath most places in the valley, the base of the post-Eocene continental deposits is equivalent to the base of the Tehama Formation of Pliocene age, which in some places at least may be of late Oligocene and early Miocene age. The deposits consist of intercalated beds of gravel, sand, silt, clay, tuff, conglomerate, sandstone, siltstone, and claystone. And beneath large areas along the eastern side of the valley the deposits consist of basaltic and andesitic mudflows, tuff, tuff breccias, volcanic sandstones and conglomerates, and sand and gravel, as well as overlying nonvolcanic sediments. They contain most of the fresh ground water in the valley.</p><p>The structure of the base of the continental deposits is that of a large northward-trending syncline whose trend is interrupted only by the Sutter Buttes. In the subsurface, faulting has occurred mostly within the basal part of the deposits. Beneath the northeastern part of the valley, along the Chico monocline, faulting has occurred through probably the total thickness of the deposits.</p><p>The deposits range in thickness from zero near the margins of the valley to about 3,500 feet beneath the south-central part of the valley. The thickest sections occur along the axis of the syncline, but near Sutter Buttes the deposits are thinner than at any other locale near the central part of the valley.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7345","usgsCitation":"Page, R.W., 1974, Base and thickness of the Post-Eocene continental deposits in the Sacramento Valley, California: U.S. Geological Survey Water-Resources Investigations Report 73-45, iii, 16 p., https://doi.org/10.3133/wri7345.","productDescription":"iii, 16 p.","costCenters":[],"links":[{"id":439031,"rank":3,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9XQ1CQF","text":"USGS data release","linkHelpText":"Digital subsurface data from previously published maps of the base and thickness of post-Eocene continental deposits in the Sacramento Valley, California"},{"id":158885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0045/report-thumb.jpg"},{"id":358896,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1973/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Sacramento Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.904052734375,\n              38.013476231041935\n            ],\n            [\n              -120.70678710937499,\n              38.013476231041935\n            ],\n            [\n              -120.70678710937499,\n              40.64730356252251\n            ],\n            [\n              -122.904052734375,\n              40.64730356252251\n            ],\n            [\n              -122.904052734375,\n              38.013476231041935\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6492b6","contributors":{"authors":[{"text":"Page, R. W.","contributorId":17215,"corporation":false,"usgs":true,"family":"Page","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":200745,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69532,"text":"hu58 - 1974 - Hydrologic Unit Map -- 1974, Caribbean region","interactions":[],"lastModifiedDate":"2012-02-02T00:13:21","indexId":"hu58","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"58","subseriesTitle":"Caribbean region 1974","title":"Hydrologic Unit Map -- 1974, Caribbean region","language":"ENGLISH","doi":"10.3133/hu58","isbn":"060776807X","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Hydrologic Unit Map -- 1974, Caribbean region: U.S. Geological Survey Hydrologic Unit 58, 1 map : col. 39 x 122 cm. fold. in envelope 30 x 24 cm.; Reprint 1990; An overprint of the 1:240,000-scale base map. Shows location and names of all cities and towns and most of the smaller settlements and railroads in black; water features in blue; hydrologic boundaries and codes in red. No contours. Sheet 42 by 58 inches. 1952 base., https://doi.org/10.3133/hu58.","productDescription":"1 map : col. 39 x 122 cm. fold. in envelope 30 x 24 cm.; Reprint 1990; An overprint of the 1:240,000-scale base map. Shows location and names of all cities and towns and most of the smaller settlements and railroads in black; water features in blue; hydrologic boundaries and codes in red. No contours. Sheet 42 by 58 inches. 1952 base.","costCenters":[],"links":[{"id":251558,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/hu/58/report.pdf","size":"21","linkFileType":{"id":1,"text":"pdf"}},{"id":251559,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/hu/58/plate-1.pdf","size":"7896","linkFileType":{"id":1,"text":"pdf"}},{"id":252482,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/hu/58/report-thumb.jpg"}],"scale":"240000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2de4b07f02db614559","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534622,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41696,"text":"ofr7414 - 1974 - Aeromagnetic map of parts of the Pittsburgh and Cumberland 1° by 2° quadrangles, Pennsylvania","interactions":[],"lastModifiedDate":"2021-09-14T21:09:29.734747","indexId":"ofr7414","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-14","title":"Aeromagnetic map of parts of the Pittsburgh and Cumberland 1° by 2° quadrangles, Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7414","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Aeromagnetic map of parts of the Pittsburgh and Cumberland 1° by 2° quadrangles, Pennsylvania: U.S. Geological Survey Open-File Report 74-14, 1 Plate: 30.49 × 37.06 inches, https://doi.org/10.3133/ofr7414.","productDescription":"1 Plate: 30.49 × 37.06 inches","costCenters":[],"links":[{"id":176505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79416,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0014/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":389241,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15005.htm"}],"scale":"250000","country":"United States","state":"Pennsylvania","otherGeospatial":"Cumberland quadrangle, Pittsburg quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -78.0,\n              39.75\n            ],\n            [\n              -79,\n              39.75\n            ],\n            [\n              -79,\n              41.0\n            ],\n            [\n              -78.0,\n              41.0\n            ],\n            [\n              -78.0,\n              39.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6974ee","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530575,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66736,"text":"i845F - 1974 - Chemical quality of ground water for public supply in the Phoenix area, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:03","indexId":"i845F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"845","subseriesTitle":"NONE","chapter":"F","title":"Chemical quality of ground water for public supply in the Phoenix area, Arizona","language":"ENGLISH","doi":"10.3133/i845F","usgsCitation":"Osterkamp, W.R., 1974, Chemical quality of ground water for public supply in the Phoenix area, Arizona: U.S. Geological Survey IMAP 845, 1 map., https://doi.org/10.3133/i845F.","productDescription":"1 map.","costCenters":[],"links":[{"id":255463,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0845f/plate-1.pdf","size":"18249","linkFileType":{"id":1,"text":"pdf"}},{"id":256049,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0845f/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":256050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0845f/report-thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113,32.75 ], [ -113,33.75 ], [ -111,33.75 ], [ -111,32.75 ], [ -113,32.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3d0d","contributors":{"authors":[{"text":"Osterkamp, W. R.","contributorId":46044,"corporation":false,"usgs":true,"family":"Osterkamp","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":274993,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68394,"text":"ha506 - 1974 - Hydrology and water resources of the Deerfield River basin, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:11:27","indexId":"ha506","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"506","title":"Hydrology and water resources of the Deerfield River basin, Massachusetts","language":"ENGLISH","doi":"10.3133/ha506","usgsCitation":"Gay, F.B., Toler, L., and Hansen, B.P., 1974, Hydrology and water resources of the Deerfield River basin, Massachusetts: U.S. Geological Survey Hydrologic Atlas 506, 8 col. maps on 2 sheets ;113 x 87 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha506.","productDescription":"8 col. maps on 2 sheets ;113 x 87 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":185700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89894,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/506/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89895,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/506/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,41.08416666666667 ], [ -77.5,41.166666666666664 ], [ -77.36749999999999,41.166666666666664 ], [ -77.36749999999999,41.08416666666667 ], [ -77.5,41.08416666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604d08","contributors":{"authors":[{"text":"Gay, Frederick B.","contributorId":102052,"corporation":false,"usgs":true,"family":"Gay","given":"Frederick","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":278143,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Toler, L.G.","contributorId":98710,"corporation":false,"usgs":true,"family":"Toler","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":278142,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hansen, Bruce P.","contributorId":90727,"corporation":false,"usgs":true,"family":"Hansen","given":"Bruce","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":278141,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":28648,"text":"wri7429 - 1974 - Preconstruction assessment of biological quality of the Chena and Little Chena Rivers in the vicinity of the Chena Lakes Flood Control Project near Fairbanks, Alaska","interactions":[],"lastModifiedDate":"2019-11-25T14:14:27","indexId":"wri7429","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-29","title":"Preconstruction assessment of biological quality of the Chena and Little Chena Rivers in the vicinity of the Chena Lakes Flood Control Project near Fairbanks, Alaska","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7429","usgsCitation":"McCoy, G.A., 1974, Preconstruction assessment of biological quality of the Chena and Little Chena Rivers in the vicinity of the Chena Lakes Flood Control Project near Fairbanks, Alaska: U.S. Geological Survey Water-Resources Investigations Report 74-29, 84 p. , https://doi.org/10.3133/wri7429.","productDescription":"84 p. ","costCenters":[],"links":[{"id":158294,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0029/report-thumb.jpg"},{"id":369561,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0029/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","city":"Fairbanks","otherGeospatial":"Chena, Little Chena Rivers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -147.98583984375,\n              64.7747105865518\n            ],\n            [\n              -147.60269165039062,\n              64.7747105865518\n            ],\n            [\n              -147.60269165039062,\n              64.86819106223713\n            ],\n            [\n              -147.98583984375,\n              64.86819106223713\n            ],\n            [\n              -147.98583984375,\n              64.7747105865518\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db680478","contributors":{"authors":[{"text":"McCoy, George A.","contributorId":20300,"corporation":false,"usgs":true,"family":"McCoy","given":"George","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200169,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68594,"text":"ha526 - 1974 - Water resources of the Lower Minnesota River Watershed, south-central Minnesota","interactions":[],"lastModifiedDate":"2018-03-05T10:18:10","indexId":"ha526","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"526","title":"Water resources of the Lower Minnesota River Watershed, south-central Minnesota","docAbstract":"<p>The lower Minnesota River watershed, an area of 2,005 square miles, is fairly flat west of the Minnesota River, but rises to a hilly ridge along the east side of the watershed. Most of the area is covered by ground moraine cut deeply by the Minnesota River and less deeply by its tributaries. Surface drainage is toward the Minnesota River at the northeast corner of the watershed. The configuration of the water table, generally between 10 and 50 feet below land surface, is a subdued replica of the land surface. Shallow ground water moves generally toward local streams and then into the Minnesota River.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Mounds View, MN","doi":"10.3133/ha526","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources Division of Waters, Soils, and Minerals","usgsCitation":"Anderson, H., Farrell, D., and Broussard, W., 1974, Water resources of the Lower Minnesota River Watershed, south-central Minnesota: U.S. Geological Survey Hydrologic Atlas 526, 3 Plates: 37.00 x 38.00 inches or smaller, https://doi.org/10.3133/ha526.","productDescription":"3 Plates: 37.00 x 38.00 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f04e8","contributors":{"authors":[{"text":"Anderson, H.W.","contributorId":78016,"corporation":false,"usgs":true,"family":"Anderson","given":"H.W.","email":"","affiliations":[],"preferred":false,"id":278544,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Farrell, D.F.","contributorId":91163,"corporation":false,"usgs":true,"family":"Farrell","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":278545,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Broussard, W.L.","contributorId":35334,"corporation":false,"usgs":true,"family":"Broussard","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":278543,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14386,"text":"ofr74113 - 1974 - Analog-model studies of ground-water hydrology in the Houston District, Texas","interactions":[],"lastModifiedDate":"2016-08-10T16:05:38","indexId":"ofr74113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-113","title":"Analog-model studies of ground-water hydrology in the Houston District, Texas","docAbstract":"<p>The major water-bearing units in the Houston district are the Chicot and the Evangeline aquifers. The Chicot aquifer overlies the Evangeline aquifer, which is underlain by the Burkeville confining layer. Both aquifers consist of unconsolidated and discontinuous layers of sand and clay that dip toward the Gulf of Mexico. Heavy pumping of fresh water has caused large declines in the altitudes of the potentiometric surfaces in both aquifers and has created large cones of depression around Houston. The declines have caused compaction of clay layers, which has resulted in land surface subsidence and the movement of saline ground water toward the centers of the cones of depression. An electric analog model was used to study the hydrologic system and to simulate the declines in the altitudes of the potentiometric surfaces for several alternative plans of ground-water development. The results indicate that the largest part. of the pumped water comes from storage in the water-table part of the Chicot aquifer. Vertical leakage from the aquifers and water derived from the compaction of clay layers in the aquifers are also large sources of the water being pumped. The response of the system, as observed on the model, indicates that development of additional ground-water supplies from the water-table part of the Chicot aquifer north of Houston would result in a minimum decline of the altitudes of the potentiometric surfaces. Total withdrawals of about 1,000 million gallons (5.8 million cubic meters) per day may be possible without seriously, increasing subsidence or salt-water encroachment. Analyses of the recovery of water levels indicate that both land-surface subsidence and salt-water encroachment could be reduced by artificially recharging the artesian part of the aquifer.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74113","usgsCitation":"Jorgensen, D.G., 1974, Analog-model studies of ground-water hydrology in the Houston District, Texas: U.S. Geological Survey Open-File Report 74-113, Report: x, 86 p.; 33 Plates, https://doi.org/10.3133/ofr74113.","productDescription":"Report: x, 86 p.; 33 Plates","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":95252,"rank":417,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-18.pdf","size":"2911","linkFileType":{"id":1,"text":"pdf"}},{"id":95253,"rank":418,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-19.pdf","size":"3452","linkFileType":{"id":1,"text":"pdf"}},{"id":95254,"rank":419,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-20.pdf","size":"3790","linkFileType":{"id":1,"text":"pdf"}},{"id":95255,"rank":420,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-21.pdf","size":"2695","linkFileType":{"id":1,"text":"pdf"}},{"id":95256,"rank":421,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-22.pdf","size":"1868","linkFileType":{"id":1,"text":"pdf"}},{"id":95257,"rank":422,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-23.pdf","size":"1740","linkFileType":{"id":1,"text":"pdf"}},{"id":95258,"rank":423,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-24.pdf","size":"2007","linkFileType":{"id":1,"text":"pdf"}},{"id":95259,"rank":424,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-25.pdf","size":"1731","linkFileType":{"id":1,"text":"pdf"}},{"id":95260,"rank":425,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-26.pdf","size":"3503","linkFileType":{"id":1,"text":"pdf"}},{"id":95261,"rank":426,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-27.pdf","size":"2932","linkFileType":{"id":1,"text":"pdf"}},{"id":95262,"rank":427,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-28.pdf","size":"3048","linkFileType":{"id":1,"text":"pdf"}},{"id":95263,"rank":428,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-29.pdf","size":"3884","linkFileType":{"id":1,"text":"pdf"}},{"id":95264,"rank":429,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-30.pdf","size":"3176","linkFileType":{"id":1,"text":"pdf"}},{"id":95265,"rank":430,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-31.pdf","size":"3093","linkFileType":{"id":1,"text":"pdf"}},{"id":95266,"rank":431,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-32.pdf","size":"3280","linkFileType":{"id":1,"text":"pdf"}},{"id":95267,"rank":432,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-33.pdf","size":"1261","linkFileType":{"id":1,"text":"pdf"}},{"id":95235,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-01.pdf","size":"9012","linkFileType":{"id":1,"text":"pdf"}},{"id":95236,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-02.pdf","size":"4740","linkFileType":{"id":1,"text":"pdf"}},{"id":95237,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-03.pdf","size":"3451","linkFileType":{"id":1,"text":"pdf"}},{"id":95238,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-04.pdf","size":"2351","linkFileType":{"id":1,"text":"pdf"}},{"id":95239,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-05.pdf","size":"2992","linkFileType":{"id":1,"text":"pdf"}},{"id":95234,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0113/report.pdf","size":"26972","linkFileType":{"id":1,"text":"pdf"}},{"id":95240,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-06.pdf","size":"3022","linkFileType":{"id":1,"text":"pdf"}},{"id":148804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0113/report-thumb.jpg"},{"id":95241,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-07.pdf","size":"2938","linkFileType":{"id":1,"text":"pdf"}},{"id":95242,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-08.pdf","size":"3099","linkFileType":{"id":1,"text":"pdf"}},{"id":95243,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-09.pdf","size":"3491","linkFileType":{"id":1,"text":"pdf"}},{"id":95244,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-10.pdf","size":"3185","linkFileType":{"id":1,"text":"pdf"}},{"id":95245,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-11.pdf","size":"3569","linkFileType":{"id":1,"text":"pdf"}},{"id":95246,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-12.pdf","size":"3311","linkFileType":{"id":1,"text":"pdf"}},{"id":95247,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0113/plate-13.p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Donald G.","contributorId":19537,"corporation":false,"usgs":true,"family":"Jorgensen","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":169367,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2673,"text":"wsp2031 - 1974 - Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp2031","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"2031","title":"Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York","docAbstract":"An investigation of recharge basins on Long Island was made by the U.S. Geological Survey in cooperation with the New York State Department of Environmental Conservation, Nassau County Department of Public Works, Suffolk County Department of Environmental Control, and Suffolk County Water Authority. The major objectives of the study were to (1) catalog basic physical data on the recharge basins in use on Long Island, (2) measure quality and quantity of precipitation and inflow, (3) measure infiltration rates at selected recharge basins, and (4) evaluate regional effects of recharge basins on the hydrologic system of Long Island. The area of study consists of Nassau and Suffolk Counties -- about 1,370 square miles -- in eastern Long Island, N.Y. \r\n\r\nRecharge basins, numbering more than 2,100 on Long Island in 1969, are open pits in moderately to highly permeable sand and gravel deposits. These pits are used to dispose of storm runoff from residential, industrial, and commercial areas, and from highways, by infiltration of the water through the bottom and sides of the basins. \r\n\r\nThe hydrology of three recharge basins on Long Island -- Westbury, Syosset, and Deer Park basins -- was studied. The precipitation-inflow relation showed that the average percentages of precipitation flowing into each basin were roughly equivalent to the average percentages of impervious areas in the total drainage areas of the basins. Average percentages of precipitation flowing into the basins as direct runoff were 12 percent at the Westbury basin, 10 percent at the Syosset basin, and 7 percent at the Deer Park basin. Numerous open-bottomed storm-water catch basins at Syosset and Deer Park reduced the proportion of inflow to those basins, as compared with the Westbury basin, which has only a few open-bottomed catch basins. \r\n\r\nInflow hydrographs for each basin typify the usual urban runoff hydrograph -- steeply rising and falling limbs, sharp peaks, and short time bases. Unit hydrographs for the Westbury and the Syosset basins are not expected to change; however, the unit hydrograph for the Deer Park basin is expected to broaden somewhat as a result of additional future house construction within the drainage area. \r\n\r\nInfiltration rates averaged 0.9 fph (feet per hour) for 63 storms between July 1967 and May 1970 at the Westbury recharge basin, 0.8 fph for 22 storms from July 1969 to September 1970 at the Syosset recharge basin, and 0.2 fph for 24 storms from March to September 1970 at the Deer Park recharge basin. Low infiltration rates at Deer Park resulted mainly from (1) a high percentage of eroded silt, clay, and organic debris washed in from construction sites in the drainage area, which partly filled the interstices of the natural deposits, and (2) a lack of a well-developed plant-root system on the floor of the younger basin, which would have kept the soil zone more permeable. \r\n\r\nThe apparent rate of movement of storm water through the unsaturated zone below each basin averaged 5.5 fph at Westbury, 3.7 fph at Syosset, and 3.1 fph at Deer Park. The rates of movement for storms during the warm months (April through October) were slightly higher than average, probably because the recharging water was warmer than it was during the rest of the year, and therefore, was slightly less viscous.\r\n\r\nOn the average, a 1-inch rainfall resulted in a peak rise of the water table directly below each basin of 0.5 foot; a 2-inch rainfall resulted in a peak rise of about 2 feet. The mound commonly dissipated within 1 to 4 days at Westbury, 7 days to more than 15 days at Syosset, and 1 to 3 days at Deer Park, depending on the magnitude of the peak buildup. \r\n\r\nAverage annual ground-water recharge was estimated to be 6.4 acre-feet at the Westbury recharge basin, 10.3 acre-feet at the Syosset recharge basin, and 29.6 acre-feet at the Deer Park recharge basin. \r\n\r\nChemical composition of precipitation at Westbury, Syosset, and Deer Park drainage areas was similar: ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2031","usgsCitation":"Seaburn, G., and Aronson, D.A., 1974, Influence of recharge basins on the hydrology of Nassau and Suffolk Counties, Long Island, New York: U.S. Geological Survey Water Supply Paper 2031, vi, 66 p. :ill. (1 fold. in pocket) ;23 cm., https://doi.org/10.3133/wsp2031.","productDescription":"vi, 66 p. :ill. (1 fold. in pocket) ;23 cm.","costCenters":[],"links":[{"id":138260,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2031/report-thumb.jpg"},{"id":247234,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2031/plate-1.pdf","size":"1142","linkFileType":{"id":1,"text":"pdf"}},{"id":29023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2031/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ede49","contributors":{"authors":[{"text":"Seaburn, G.E.","contributorId":42193,"corporation":false,"usgs":true,"family":"Seaburn","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":145593,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aronson, D. 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,{"id":4037,"text":"cir703 - 1974 - Water demands for expanding energy development","interactions":[],"lastModifiedDate":"2017-07-07T08:59:49","indexId":"cir703","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"703","title":"Water demands for expanding energy development","docAbstract":"<p>Water is used in producing energy for mining and reclamation of mined lands, onsite processing, transportation, refining, and conversion of fuels to other forms of energy. In the East, South, Midwest, and along the seacoasts, most water problems are related to pollution rather than to water supply. West of about the 100th meridian, however, runoff is generally less than potential diversions, and energy industries must compete with other water users. Water demands for extraction of coal, oil shale, uranium, and oil and gas are modest, although large quantities of water are used in secondary recovery operations for oil. The only significant use of water for energy transportation, aside from in-stream navigation use, is for slurry lines. Substantial quantities of water are required in the retorting and the disposal of spent oil shale. The conversion of coal to synthetic gas or oil or to electric power and the generation of electric power with nuclear energy require large quantities of water, mostly for cooling. Withdrawals for cooling of thermal-electric plants is by far the largest category of water use in energy industry, totaling about 170 billion gallons (644 million m3) per day in 1970. Water availability will dictate the location and design of energy-conversion facilities, especially in water deficient areas of the West.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/cir703","usgsCitation":"Davis, G.H., and Wood, L., 1974, Water demands for expanding energy development: U.S. Geological Survey Circular 703, iv, 14 p. :ill. ;26 cm., https://doi.org/10.3133/cir703.","productDescription":"iv, 14 p. :ill. ;26 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true},{"id":532,"text":"Pennsylvania Water Science 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,{"id":43976,"text":"ofr74323 - 1974 - Hardness of ground water on north coast of Long Island Sound, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:10:29","indexId":"ofr74323","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-323","title":"Hardness of ground water on north coast of Long Island Sound, Connecticut","language":"ENGLISH","doi":"10.3133/ofr74323","usgsCitation":"Melvin, R., and Haeni, F., 1974, Hardness of ground water on north coast of Long Island Sound, Connecticut: U.S. Geological Survey Open-File Report 74-323, 1 map, https://doi.org/10.3133/ofr74323.","productDescription":"1 map","costCenters":[],"links":[{"id":173754,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":99121,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0323/plate-1.pdf","size":"14540","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641091","contributors":{"authors":[{"text":"Melvin, R.L.","contributorId":50497,"corporation":false,"usgs":true,"family":"Melvin","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":228928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haeni, F.P.","contributorId":87105,"corporation":false,"usgs":true,"family":"Haeni","given":"F.P.","affiliations":[],"preferred":false,"id":228929,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44067,"text":"ofr74366 - 1974 - Water resources of the Rock River watershed, southwestern Minnesota","interactions":[{"subject":{"id":44067,"text":"ofr74366 - 1974 - Water resources of the Rock River watershed, southwestern Minnesota","indexId":"ofr74366","publicationYear":"1974","noYear":false,"title":"Water resources of the Rock River watershed, southwestern Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":68654,"text":"ha555 - 1976 - Water resources of the Rock River watershed, southwestern Minnesota","indexId":"ha555","publicationYear":"1976","noYear":false,"title":"Water resources of the Rock River watershed, southwestern Minnesota"},"id":1}],"supersededBy":{"id":68654,"text":"ha555 - 1976 - Water resources of the Rock River watershed, southwestern Minnesota","indexId":"ha555","publicationYear":"1976","noYear":false,"title":"Water resources of the Rock River watershed, southwestern Minnesota"},"lastModifiedDate":"2012-02-02T00:10:31","indexId":"ofr74366","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-366","title":"Water resources of the Rock River watershed, southwestern Minnesota","language":"ENGLISH","doi":"10.3133/ofr74366","issn":"ma","usgsCitation":"Anderson, H.W., Broussard, W., Farrell, D., and Felsheim, P., 1974, Water resources of the Rock River watershed, southwestern Minnesota: U.S. Geological Survey Open-File Report 74-366, 1 map on 3 sheets, https://doi.org/10.3133/ofr74366.","productDescription":"1 map on 3 sheets","costCenters":[],"links":[{"id":173576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f038a","contributors":{"authors":[{"text":"Anderson, H. W. Jr.","contributorId":11187,"corporation":false,"usgs":true,"family":"Anderson","given":"H.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":229101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broussard, W.L.","contributorId":35334,"corporation":false,"usgs":true,"family":"Broussard","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":229102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Farrell, D.F.","contributorId":91163,"corporation":false,"usgs":true,"family":"Farrell","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":229104,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Felsheim, P.E.","contributorId":39395,"corporation":false,"usgs":true,"family":"Felsheim","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":229103,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":68372,"text":"ha442 - 1974 - Ground water in Finney County, southwestern Kansas","interactions":[],"lastModifiedDate":"2017-02-13T16:43:04","indexId":"ha442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"442","title":"Ground water in Finney County, southwestern Kansas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha442","usgsCitation":"Gutentag, E.D., Lobmeyer, D., McGovern, H., and Long, W., 1974, Ground water in Finney County, southwestern Kansas: U.S. Geological Survey Hydrologic Atlas 442, Maps: 3 Sheets, 35.0 x 34.0 inches or smaller; Color and Pattern Guide: 4 Sheets, 8.0 x 10.6 inches , https://doi.org/10.3133/ha442.","productDescription":"Maps: 3 Sheets, 35.0 x 34.0 inches or smaller; Color and Pattern Guide: 4 Sheets, 8.0 x 10.6 inches ","costCenters":[],"links":[{"id":185799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89861,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/442/plate-5.pdf","text":"Color and Pattern Guide: Sheet 2 of 4","linkFileType":{"id":1,"text":"pdf"}},{"id":89862,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/442/plate-6.pdf","text":"Color and Pattern Guide: Sheet 3 of 4","linkFileType":{"id":1,"text":"pdf"}},{"id":89860,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/442/plate-4.pdf","text":"Color and Pattern Guide: Sheet 1 of 4","linkFileType":{"id":1,"text":"pdf"}},{"id":89863,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/442/plate-7.pdf","text":"Color and Pattern Guide: Sheet 4 of 4","linkFileType":{"id":1,"text":"pdf"}},{"id":89857,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/442/plate-1.pdf","text":"Sheet 1 of 3","linkFileType":{"id":1,"text":"pdf"}},{"id":89858,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/442/plate-2.pdf","text":"Sheet 2 of 3","linkFileType":{"id":1,"text":"pdf"}},{"id":89859,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/442/plate-3.pdf","text":"Sheet 3 of 3","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Kansas","county":"Finney County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-100.6845,38.2627],[-100.2447,38.2606],[-100.2265,38.2609],[-100.2269,38.0007],[-100.6638,38.0005],[-100.6641,37.8296],[-100.6507,37.8285],[-100.6526,37.7364],[-101.0904,37.737],[-101.0895,37.8281],[-101.103,37.8297],[-101.1037,38.2636],[-100.6845,38.2627]]]},\"properties\":{\"name\":\"Finney\",\"state\":\"KS\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66db50","contributors":{"authors":[{"text":"Gutentag, Edwin D.","contributorId":76287,"corporation":false,"usgs":true,"family":"Gutentag","given":"Edwin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":278107,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lobmeyer, D.H.","contributorId":106502,"corporation":false,"usgs":true,"family":"Lobmeyer","given":"D.H.","affiliations":[],"preferred":false,"id":668480,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McGovern, H.E.","contributorId":85600,"corporation":false,"usgs":true,"family":"McGovern","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":668481,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Long, W.A.","contributorId":46619,"corporation":false,"usgs":true,"family":"Long","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":668482,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":48246,"text":"ofr741072 - 1974 - Availability of ground water for the U.S. Navy well field near Florida City, Dade County, Florida","interactions":[],"lastModifiedDate":"2025-04-25T15:58:31.027959","indexId":"ofr741072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-1072","title":"Availability of ground water for the U.S. Navy well field near Florida City, Dade County, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741072","usgsCitation":"Availability of ground water for the U.S. Navy well field near Florida City, Dade County, Florida; 1974; OFR; 74-1072; Meyer, Frederick W.","productDescription":"50 p.","costCenters":[],"links":[{"id":172060,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":4029,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/1072/ofr-fl-74014.pdf","text":"Report","size":"1.68 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.08605391503532,\n              25.929807618584235\n            ],\n            [\n              -80.75843989851955,\n              25.929807618584235\n            ],\n            [\n              -80.75843989851955,\n              25.199350614801148\n            ],\n            [\n              -80.08605391503532,\n              25.199350614801148\n            ],\n            [\n              -80.08605391503532,\n              25.929807618584235\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"1974-10-01","noUsgsAuthors":false,"publicationDate":"1974-10-01","publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667e08","contributors":{"authors":[{"text":"Meyer, Frederick W.","contributorId":39373,"corporation":false,"usgs":true,"family":"Meyer","given":"Frederick","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":237034,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42635,"text":"ofr741113 - 1974 - Residual magnetic intensity map of the southern Raft River area, Cassia County, Idaho","interactions":[],"lastModifiedDate":"2025-08-01T17:10:08.464423","indexId":"ofr741113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-1113","title":"Residual magnetic intensity map of the southern Raft River area, Cassia County, Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr741113","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Residual magnetic intensity map of the southern Raft River area, Cassia County, Idaho: U.S. Geological Survey Open-File Report 74-1113, 1 Plate: 36.00 x 63.00 inches, https://doi.org/10.3133/ofr741113.","productDescription":"1 Plate: 36.00 x 63.00 inches","costCenters":[],"links":[{"id":493356,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8863.htm","linkFileType":{"id":5,"text":"html"}},{"id":98921,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/1113/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172439,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","country":"United States","state":"Idaho","county":"Cassia County","otherGeospatial":"southern Raft River area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -113.472,\n              42.292\n            ],\n            [\n              -113.472,\n              42\n            ],\n            [\n              -113.25,\n              42\n            ],\n            [\n              -113.25,\n              42.292\n            ],\n            [\n              -113.472,\n              42.292\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b9cc","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530936,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":12711,"text":"ofr74198 - 1974 - Hydraulic analysis of floodflows in Butte Basin at State Highway 162, Glenn and Butte counties, California","interactions":[],"lastModifiedDate":"2017-06-18T21:53:43","indexId":"ofr74198","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","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":"74-198","title":"Hydraulic analysis of floodflows in Butte Basin at State Highway 162, Glenn and Butte counties, California","docAbstract":"Inundation of State Highway 162 across Butte Basin at the latitude of Butte City results from overland floodflow from the Sacramento River and flooding on Butte Creek. Flooding of Butte Basin from the Sacramento River will occur whenever flow in the main channel at Butte City exceeds 90,000 cubic feet per second (2550 cubic metres per second), a discharge with a recurrence interval of about 3 years. The distribution of floodflow across the basin is not uniform. During the flood of January 24, 1970, 84 percent of the total discharge resulted from overland flow from the Sacramento River and 16 percent from flooding on Butte Creek. \r\n\r\nWhen flooding in Butte Basin is severe enough to affect State Highway 162, overflow across the road first occurs between bridges 11-21 and 11-22. The construction of bridges or culverts at two locations between bridges 11-21 and 11-22 would increase the period of time that the road is usable. \r\n\r\nAnalysis of the present roadway, bridge geometry, and ground elevations adjacent to the roadway indicates that backwater is less than 0.6 foot (0.2 metre) for flows of the magnitude experienced during the flood of January 24, 1970. The concurrent maximum velocity of flow at the bridges is 6.8 feet per second (2.1 metres per second). Part of the backwater is caused by ground elevations adjacent to the roadway that are, at many locations, higher than the road crown. \r\n\r\nIf the roadway embankment were raised to prevent overtopping by a flood equivalent to that of January 24, 1970, without increasing the capacity or number of the bridges, backwater greater than 0.5 foot (0.2 metre) would result upstream from 6 of the 15 bridges on State Highway 162, and velocities would be excessive. Additional bridge openings to discharge a total of 37,800 cubic feet per second (1070 cubic metres per second) would be required for at least six locations if backwater and velocity were to be kept to levels similar to those observed for present conditions. \r\n\r\nDuring the flood of November 12, 1973, water-surface elevations recorded in several of the overflow channels of Butte Creek were higher than those observed during the January 1970 flood even though the discharge was less. The higher water-surface elevations in 1973 probably resulted from vegetal growth in the channels and consequent reduction in the capacity of the channel to carry floodflows.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr74198","usgsCitation":"Blodgett, J.C., and Stiehr, P.L., 1974, Hydraulic analysis of floodflows in Butte Basin at State Highway 162, Glenn and Butte counties, California: U.S. Geological Survey Open-File Report 74-198, vii, 48 p. :ill., maps (some folded) ;27 cm.; (63 p. - PGS), https://doi.org/10.3133/ofr74198.","productDescription":"vii, 48 p. :ill., maps (some folded) ;27 cm.; (63 p. - PGS)","costCenters":[],"links":[{"id":144790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1974/0198/report-thumb.jpg"},{"id":41125,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1974/0198/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41126,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1974/0198/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a50e4b07f02db6295f8","contributors":{"authors":[{"text":"Blodgett, J. C.","contributorId":32154,"corporation":false,"usgs":true,"family":"Blodgett","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":166582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stiehr, Patrick Lenard","contributorId":79480,"corporation":false,"usgs":true,"family":"Stiehr","given":"Patrick","email":"","middleInitial":"Lenard","affiliations":[],"preferred":false,"id":166583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69534,"text":"hu12 - 1974 - Hydrologic Unit Map -- 1974, Idaho","interactions":[],"lastModifiedDate":"2018-12-10T14:14:44","indexId":"hu12","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1974","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"12","subseriesTitle":"Idaho 1974","title":"Hydrologic Unit Map -- 1974, Idaho","docAbstract":"<p>This map and accompanying table show Hydrologic Units that are basically hydrographic in nature. The Cataloging Units shown will supplant the Cataloging Units previously used by the U.S. Geological Survey in its Catalog of Information on Water Data (1966-72). The previous U.S. Geological Survey Catalog-Indexing System was by map number and letter, such as 49M. The boundaries as shown have been adapted from \"The Catalog of Information on Water Data\" (1972), \"Water Resources Regions and Subregions for the National Assessment of Water and Related Land Resources\" by the U.S. Water Resources Council (1970), \"River Basins of the United States\" by the U.S. Soil Conservation Service (1963, 1970), \"River Basin Maps Showing Hydrologic Stations\" by the Inter-Agency Committee on Water Resources, Subcommittee on Hydrology (1961), and State planning maps.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu12","isbn":"607767707","collaboration":"Prepared in cooperation with the U.S. Water Resources Council","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1974, Hydrologic Unit Map -- 1974, Idaho: U.S. Geological Survey Hydrologic Unit 12, 42.80 x 67.48 inches, https://doi.org/10.3133/hu12.","productDescription":"42.80 x 67.48 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