{"pageNumber":"6819","pageRowStart":"170450","pageSize":"25","recordCount":184743,"records":[{"id":52118,"text":"ofr60101 - 1960 - Ground-water inventory for 1959, Edwards Air Force Base, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr60101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-101","title":"Ground-water inventory for 1959, Edwards Air Force Base, California","language":"ENGLISH","doi":"10.3133/ofr60101","usgsCitation":"Moyle, W.R., 1960, Ground-water inventory for 1959, Edwards Air Force Base, California: U.S. Geological Survey Open-File Report 60-101, 35 p., https://doi.org/10.3133/ofr60101.","productDescription":"35 p.","costCenters":[],"links":[{"id":178012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698659","contributors":{"authors":[{"text":"Moyle, W. R. Jr.","contributorId":85938,"corporation":false,"usgs":true,"family":"Moyle","given":"W.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":244833,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52117,"text":"ofr60100 - 1960 - A plan for the practical management of the water resources in an alluvial valley","interactions":[],"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr60100","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-100","title":"A plan for the practical management of the water resources in an alluvial valley","language":"ENGLISH","doi":"10.3133/ofr60100","usgsCitation":"Moulder, E.A., 1960, A plan for the practical management of the water resources in an alluvial valley: U.S. Geological Survey Open-File Report 60-100, 7 p., https://doi.org/10.3133/ofr60100.","productDescription":"7 p.","costCenters":[],"links":[{"id":178011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab772","contributors":{"authors":[{"text":"Moulder, E. A.","contributorId":78719,"corporation":false,"usgs":true,"family":"Moulder","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":244832,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52109,"text":"ofr6081 - 1960 - Glacier observations, Glacier National Park, Montana, 1959","interactions":[],"lastModifiedDate":"2012-02-02T00:11:32","indexId":"ofr6081","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-81","title":"Glacier observations, Glacier National Park, Montana, 1959","language":"ENGLISH","doi":"10.3133/ofr6081","usgsCitation":"Johnson, A., 1960, Glacier observations, Glacier National Park, Montana, 1959: U.S. Geological Survey Open-File Report 60-81, 23 p., https://doi.org/10.3133/ofr6081.","productDescription":"23 p.","costCenters":[],"links":[{"id":178492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac3e4b07f02db678779","contributors":{"authors":[{"text":"Johnson, Arthur","contributorId":76720,"corporation":false,"usgs":true,"family":"Johnson","given":"Arthur","affiliations":[],"preferred":false,"id":244812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2153,"text":"wsp1485 - 1960 - Quality of surface waters for irrigation, western United States, 1956","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1485","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1485","title":"Quality of surface waters for irrigation, western United States, 1956","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1485","usgsCitation":"Love, S.K., 1960, Quality of surface waters for irrigation, western United States, 1956: U.S. Geological Survey Water Supply Paper 1485, viii, 185 p. :ill, map ;25 cm., https://doi.org/10.3133/wsp1485.","productDescription":"viii, 185 p. :ill, map ;25 cm.","costCenters":[],"links":[{"id":137845,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1485/report-thumb.jpg"},{"id":27763,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1485/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651db1","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3938,"text":"cir436 - 1960 - Preliminary report on ground water in the Salmon Falls area, Twin Falls County, Idaho","interactions":[],"lastModifiedDate":"2013-07-24T14:28:49","indexId":"cir436","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"436","title":"Preliminary report on ground water in the Salmon Falls area, Twin Falls County, Idaho","docAbstract":"The Salmon Falls area contains about 80,000 acres of irrigable land, of which about 30,000 acres receives some water from the distribution system of Salmon River Canal Co., Ltd. This system utilizes virtually all the available surface water.  A substantial amount of surface water, estimated to be about 70,000 acre-feet annually, is lost by leakage from the reservoir and the distribution system. Some of this water could be salvaged by lining sections of the canal where excessive losses occur. Ground water has not been extensively developed in the area, but some successful irrigation wells furnished supplemental irrigation water. Recharge to the area is from precipitation on the area, seepage from peripheral streams, seepage losses from the reservoir and canal system, irrigation seepage, and ground-water underflow. Ground water leaves the area by undertow to the north and northwest, and eventually reaches the Snake River. The total mount of underflow from the area was estimated by three different methods to be 17,000, 100,000, and 170,000 acre-feet per year. The preliminary estimate of 100,000 acre-feet was derived by the inventory of recharge and is probably more accurate than the other two methods.  Calculations, based on estimates of transmissibility computed from specific capacities of wells, suggest that there may be some channels or conduits of higher than average transmissibility through which a large part of the undertow leaves the area, Possibly 25 percent of the ground-water outflow could be intercepted by wells. However, in part of the area the depth to water may be excessive for economic development.  Chemical analyses of 25 samples of ground water indicate that most of the water sampled is suitable for irrigation. The samples found least suitable were of water occurring at shallow depth, south and east of Hollister.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir436","usgsCitation":"Fowler, K.H., 1960, Preliminary report on ground water in the Salmon Falls area, Twin Falls County, Idaho: U.S. Geological Survey Circular 436, Document: iii, 17 p.; 1 Map: 14.22 x 15.24 inches, https://doi.org/10.3133/cir436.","productDescription":"Document: iii, 17 p.; 1 Map: 14.22 x 15.24 inches","numberOfPages":"21","costCenters":[],"links":[{"id":124626,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0436/report-thumb.jpg"},{"id":31023,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0436/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271073,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0436/plate-1.pdf"}],"country":"United States","state":"Idaho","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.04,41.99 ], [ -115.04,42.9 ], [ -114.0,42.9 ], [ -114.0,41.99 ], [ -115.04,41.99 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e11e","contributors":{"authors":[{"text":"Fowler, Kenneth H.","contributorId":23930,"corporation":false,"usgs":true,"family":"Fowler","given":"Kenneth","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":147861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4177,"text":"cir431 - 1960 - Wetland and water supply","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"cir431","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"431","title":"Wetland and water supply","docAbstract":"The Geological Survey has received numerous inquiries about the effects of proposed changes in the wetland environment. The nature of the inquiries suggests a general confusion in the public mind as to wetland values and an increasing concern by the public with the need for facts as a basis for sound decisions when public action is required. \r\n\r\nPerhaps the largest gap in our knowledge is in regard to the role played by the wetland in the natural water scheme. Specialists in such fields as agriculture and conservation have studied the wetland in relation to its special uses and values for farming and as a habitat for fish and wildlife. However, except as studied incidentally by these specialists, the role of the wetland with respect to water has been largely neglected. This facet of the wetland problem is of direct concern to the Geological Survey. \r\n\r\nWe commonly speak of water in terms of its place in the hydrologic environment---as, for example, surface water or ground water. These terms imply that water can be neatly pigeonholed. With respect to the wetland environment nothing can be further from the truth. In fact, one objective of this discussion is to demonstrate that for the wetland environment surface water, ground water, and soil water cannot be separated realistically, but are closely interrelated and must be studied together. It should be noted that this statement holds true for the hydrologic environment in general, and that the wetland environment is by no means unique in this respect. Our second and principal objective is to identify some of the problems that must be studied in order to clarify the role of the wetland in relation to water supply. \r\n\r\nWe have chosen to approach these objectives by briefly describing one area for which we have some information, and by using this example to point out some of the problems that need study. First, however, let us define what we, as geohydrologists, mean by wetland and briefly consider wetland classifications. \r\n\r\nFor our purpose wetlands are land areas that are covered with shallow water or subjected to intermittent flooding and subsequent slow drainage, and which generally are characterized by an accumulation of organic matter hereafter termed \u001Cswamp deposits.' These wetlands may be classified in a number of different ways depending on the purpose of the classifier. For example, the Fish and Wildlife Service classifies wetlands into 20 different types based on water quality (fresh or salty), drainage, and vegetation. At the risk of some oversimplification we might consider 4 types of wetland from the standpoint of hydrology: (1) fresh-water swamps in which the swamp deposits are underlain by glacial till or bedrock; (2)fresh-water swamps in which the swamp deposits are underlain by marine or lacustrine clay and silt; (3) fresh-water swamps in which the swamp deposits are underlain by glacial outwash or alluvium consisting mostly of sand or sand and gravel; and (4) salt .marshes and salt meadows. The three fresh-water types of wetland are of interest with respect to water supply, and of these, the type in which swamp deposits are underlain by glacial outwash is of particular interest in New England. \r\n\r\nIn the Ipswich River basin above the Geological Survey gaging station at South Middleton, Mass., is an area of 44 square miles which forms the headwaters section of the basin. The relief of the area is low. About half the area consists of hills mostly underlain by bedrock but mantled by a thin layer of glacial till. The other half consists Of lowlands---including swamps, low terraces and plains---underlain by glacial outwash, Swampland, used hereafter as a synonym for wetland, forms about a fourth of the area. Some of the swamps occupy depressions in the till blanket and are situated at somewhat higher levels than the lowlands. The largest swamps, however, border the Ipswich River and its tributaries. Here the swamp deposits, which consist of muck and peat mixed with s","language":"ENGLISH","publisher":"[U.S. Geological Survey],","doi":"10.3133/cir431","usgsCitation":"Baker, J.A., 1960, Wetland and water supply: U.S. Geological Survey Circular 431, 3 p. ;27 cm., https://doi.org/10.3133/cir431.","productDescription":"3 p. ;27 cm.","costCenters":[],"links":[{"id":117878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0431/report-thumb.jpg"},{"id":31289,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0431/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db545334","contributors":{"authors":[{"text":"Baker, John Augustus","contributorId":48159,"corporation":false,"usgs":true,"family":"Baker","given":"John","email":"","middleInitial":"Augustus","affiliations":[],"preferred":false,"id":148348,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4183,"text":"cir421 - 1960 - Sediment discharge and stream power--A preliminary announcement","interactions":[],"lastModifiedDate":"2018-01-02T20:28:44","indexId":"cir421","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"421","title":"Sediment discharge and stream power--A preliminary announcement","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir421","usgsCitation":"Bagnold, R.A., 1960, Sediment discharge and stream power--A preliminary announcement: U.S. Geological Survey Circular 421, 23 p. :diagrs. ;26 cm., https://doi.org/10.3133/cir421.","productDescription":"23 p. :diagrs. ;26 cm.","costCenters":[],"links":[{"id":118237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0421/report-thumb.jpg"},{"id":31294,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0421/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc059","contributors":{"authors":[{"text":"Bagnold, Ralph A.","contributorId":78724,"corporation":false,"usgs":true,"family":"Bagnold","given":"Ralph","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":148355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3565,"text":"cir429 - 1960 - Water-resources summary for southern California, 1959","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir429","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"429","title":"Water-resources summary for southern California, 1959","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir429","usgsCitation":"Peterson, W.C., 1960, Water-resources summary for southern California, 1959: U.S. Geological Survey Circular 429, iii, 10 p. :ill., maps ;27 cm., https://doi.org/10.3133/cir429.","productDescription":"iii, 10 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":117709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0429/report-thumb.jpg"},{"id":30593,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0429/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4db6","contributors":{"authors":[{"text":"Peterson, William C.","contributorId":54970,"corporation":false,"usgs":true,"family":"Peterson","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":147165,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64324,"text":"gp238 - 1960 - Aeromagnetic map of the Langhorne quadrangle, Bucks County, Pennsylvania","interactions":[],"lastModifiedDate":"2021-12-06T22:49:15.652741","indexId":"gp238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"238","title":"Aeromagnetic map of the Langhorne quadrangle, Bucks County, Pennsylvania","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp238","usgsCitation":"Bromery, R.W., Henderson, J.R., and Zandle, G.L., 1960, Aeromagnetic map of the Langhorne quadrangle, Bucks County, Pennsylvania: U.S. Geological Survey Geophysical Investigations Map 238, 1 Plate: 22.82 × 27.69 inches, https://doi.org/10.3133/gp238.","productDescription":"1 Plate: 22.82 × 27.69 inches","costCenters":[],"links":[{"id":392540,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3160.htm"},{"id":251715,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0238/report-thumb.jpg"},{"id":250967,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0238/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250966,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0238/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Pennsylvania","county":"Bucks County","otherGeospatial":"Langhorne quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75,40.125 ], [ -75,40.25 ], [ -74.875,40.25 ], [ -74.875,40.125 ], [ -75,40.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b50b","contributors":{"authors":[{"text":"Bromery, Randolph Wilson","contributorId":22746,"corporation":false,"usgs":true,"family":"Bromery","given":"Randolph","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":270574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Henderson, J. R. Jr.","contributorId":88802,"corporation":false,"usgs":true,"family":"Henderson","given":"J.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270576,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270575,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":178,"text":"wsp1450 - 1960 - Quality of surface waters of the United States, 1956. Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1450","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1450","title":"Quality of surface waters of the United States, 1956. Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1450","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1960, Quality of surface waters of the United States, 1956. Parts 1-4, North Atlantic slope basins to St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1450, xv, 603 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1450.","productDescription":"xv, 603 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137361,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1450/report-thumb.jpg"},{"id":24789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1450/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651d4f","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":527218,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":180,"text":"wsp1520 - 1960 - Quality of surface waters of the United States, 1957, Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1520","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1520","title":"Quality of surface waters of the United States, 1957, Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1520","usgsCitation":"Love, S.K., 1960, Quality of surface waters of the United States, 1957, Parts 1-4, North Atlantic slope basins to St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1520, xvi, 641 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1520.","productDescription":"xvi, 641 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1520/report-thumb.jpg"},{"id":24791,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1520/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651cd9","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142051,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2951,"text":"wsp1553 - 1960 - Surface water supply of the United States, 1958, Part 2-A, South Atlantic slope basins, James River to Savannah River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"wsp1553","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1553","title":"Surface water supply of the United States, 1958, Part 2-A, South Atlantic slope basins, James River to Savannah River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1553","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1958, Part 2-A, South Atlantic slope basins, James River to Savannah River: U.S. Geological Survey Water Supply Paper 1553, viii, 273 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1553.","productDescription":"viii, 273 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":139149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1553/report-thumb.jpg"},{"id":29660,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1553/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69607e","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146037,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3817,"text":"cir434 - 1960 - Progress report on use of water by riparian vegetation, Cottonwood Wash, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"cir434","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"434","title":"Progress report on use of water by riparian vegetation, Cottonwood Wash, Arizona","docAbstract":"Measurements of streamflow, ground-water levels, and meterological data obtained in a 4.1-mile reach of the flood plain of Cottonwood Wash, Mohave County, Ariz., define the use of water by riparian vegetation in that part of the stream valley. The computed evapotranspiration loss during the growing season of 1959 was 175 acre-feet, which represented about 33 percent of the water that entered the reach. The maximum rate of loss during the season was slightly more than 8 acre-feet per week, or about 60 percent of the inflow. \r\n\r\nThe project reach is divided into two parts: An upstream subreach of 2.6 miles and a downstream subreach of 1.5 miles. Seasonal losses in the upstream and downstream subreaches were 75 and 100 acre-feet respectively. Losses in the shorter downstream subreach were larger because of the greater plant population. \r\n\r\nDuring the summer of 1960 the vegetation in the lower subreach will be chemically defoliated as a part of the experiment to determine the savings in water losses that can be effected by modifying riparian vegetation. Tests on chemical defoliants indicate that a single spraying eliminates the leaves on cottonwood trees for 7 or 8 days and that no permanent damage results.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir434","usgsCitation":"Hendricks, E.L., Kam, W., and Bowie, J.E., 1960, Progress report on use of water by riparian vegetation, Cottonwood Wash, Arizona: U.S. Geological Survey Circular 434, iii, 11 p. :ill., map ;27 cm., https://doi.org/10.3133/cir434.","productDescription":"iii, 11 p. :ill., map ;27 cm.","costCenters":[],"links":[{"id":124664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0434/report-thumb.jpg"},{"id":30887,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0434/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6493f4","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":147660,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kam, William","contributorId":85159,"corporation":false,"usgs":true,"family":"Kam","given":"William","email":"","affiliations":[],"preferred":false,"id":147661,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bowie, James E.","contributorId":29393,"corporation":false,"usgs":true,"family":"Bowie","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":147659,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2711,"text":"wsp1479 - 1960 - Geohydrologic evaluation of streamflow records in the Big Wood River basin, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1479","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1479","title":"Geohydrologic evaluation of streamflow records in the Big Wood River basin, Idaho","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1479","usgsCitation":"Smith, R.O., 1960, Geohydrologic evaluation of streamflow records in the Big Wood River basin, Idaho: U.S. Geological Survey Water Supply Paper 1479, v, 68 p. :maps (2 fold. col. in pocket) diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1479.","productDescription":"v, 68 p. :maps (2 fold. col. in pocket) diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":139062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1479/report-thumb.jpg"},{"id":29090,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1479/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29091,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1479/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29092,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1479/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8efe","contributors":{"authors":[{"text":"Smith, Rex Onis","contributorId":93889,"corporation":false,"usgs":true,"family":"Smith","given":"Rex","email":"","middleInitial":"Onis","affiliations":[],"preferred":false,"id":145647,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3783,"text":"cir424 - 1960 - Ground-water supplies in shale and sandstone in Fairfax, Loudoun, and Prince William Counties, Virginia","interactions":[],"lastModifiedDate":"2018-01-02T20:38:28","indexId":"cir424","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"424","title":"Ground-water supplies in shale and sandstone in Fairfax, Loudoun, and Prince William Counties, Virginia","docAbstract":"The Triassic rocks of northern Virginia may be a potential source of moderately large supplies of ground water for municipal end industrial use if the performance of two deep wells drilled at the site of the new Dulles International Airport is a criterion. These two wells produced 327 and 600 gpm (gallons per minute) from depths of 860-and 955 feet in sedimentary rocks in an immediate area where the previous maximum depth reported was 180 feet and the maximum yield 12 gpm. \r\n\r\nChemical analyses of the water indicates that it is extremely hard--533 and 500 ppm (parts per million) in the two wells--and would require treatment to be satisfactory for domestic and some industrial uses. However, water of better quality may be present at greater depths, and it may be possible to case off the more highly mineralized water. Further exploration and sampling of water from various depths will be necessary for efficient development of the Triassic groundwater reservoir.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir424","usgsCitation":"Johnston, P.M., 1960, Ground-water supplies in shale and sandstone in Fairfax, Loudoun, and Prince William Counties, Virginia: U.S. Geological Survey Circular 424, iv, 7 p. :map, tables. ;27cm., https://doi.org/10.3133/cir424.","productDescription":"iv, 7 p. :map, tables. ;27cm.","costCenters":[],"links":[{"id":30855,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0424/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0424/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a463","contributors":{"authors":[{"text":"Johnston, Paul McKelvey","contributorId":8828,"corporation":false,"usgs":true,"family":"Johnston","given":"Paul","email":"","middleInitial":"McKelvey","affiliations":[],"preferred":false,"id":147591,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2154,"text":"wsp1524 - 1960 - Quality of surface water for irrigation, western United States, 1957","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1524","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1524","title":"Quality of surface water for irrigation, western United States, 1957","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1524","usgsCitation":"Love, S.K., 1960, Quality of surface water for irrigation, western United States, 1957: U.S. Geological Survey Water Supply Paper 1524, viii, 183 p., [1] folded leaf of plates :ill., map ;25 cm., https://doi.org/10.3133/wsp1524.","productDescription":"viii, 183 p., [1] folded leaf of plates :ill., map ;25 cm.","costCenters":[],"links":[{"id":137846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1524/report-thumb.jpg"},{"id":27764,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1524/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db654cf7","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144749,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1760,"text":"wsp1482 - 1960 - Geology and ground-water resources of the Gallatin Valley, Gallatin County, Montana","interactions":[],"lastModifiedDate":"2022-01-05T22:16:46.657229","indexId":"wsp1482","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1482","title":"Geology and ground-water resources of the Gallatin Valley, Gallatin County, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1482","usgsCitation":"Hackett, O.M., Visher, F.N., McMurtrey, R.G., Steinhilber, W.L., Stermitz, F., Boner, F.C., and Krieger, R.A., 1960, Geology and ground-water resources of the Gallatin Valley, Gallatin County, Montana: U.S. Geological Survey Water Supply Paper 1482, Report: viii, 282 p.; 11 Plates: 38.00 × 38.93 inches or smaller, https://doi.org/10.3133/wsp1482.","productDescription":"Report: viii, 282 p.; 11 Plates: 38.00 × 38.93 inches or smaller","costCenters":[],"links":[{"id":26869,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26867,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26862,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26873,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1482/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138441,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1482/report-thumb.jpg"},{"id":26872,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26871,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26870,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26868,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26866,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26865,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26864,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26863,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1482/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393942,"rank":14,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24425.htm"}],"country":"United States","state":"Montana","county":"Gallatin County","otherGeospatial":"Gallatin Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.5,\n              45.5\n            ],\n            [\n              -110.918,\n              45.5\n            ],\n            [\n              -110.918,\n              46.0210\n            ],\n            [\n              -111.5,\n              46.0210\n            ],\n            [\n              -111.5,\n              45.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6856a7","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":144097,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Visher, F. N.","contributorId":52554,"corporation":false,"usgs":true,"family":"Visher","given":"F.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":144098,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"McMurtrey, R. G.","contributorId":36913,"corporation":false,"usgs":true,"family":"McMurtrey","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144096,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Steinhilber, W. L.","contributorId":79456,"corporation":false,"usgs":true,"family":"Steinhilber","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144099,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stermitz, Frank","contributorId":15175,"corporation":false,"usgs":true,"family":"Stermitz","given":"Frank","email":"","affiliations":[],"preferred":false,"id":144094,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Boner, F. C.","contributorId":32136,"corporation":false,"usgs":true,"family":"Boner","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144095,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Krieger, R. A.","contributorId":11202,"corporation":false,"usgs":true,"family":"Krieger","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144093,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":1624,"text":"wsp1637 - 1960 - Surface water supply of the United States, 1959, Part 13, Snake River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp1637","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1637","title":"Surface water supply of the United States, 1959, Part 13, Snake River Basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp1637","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1959, Part 13, Snake River Basin: U.S. Geological Survey Water Supply Paper 1637, 271 p. :tables. ;23 cm., https://doi.org/10.3133/wsp1637.","productDescription":"271 p. :tables. ;23 cm.","costCenters":[],"links":[{"id":137187,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1637/report-thumb.jpg"},{"id":26689,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1637/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6943cd","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":143906,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1797,"text":"wsp1488 - 1960 - The geology and ground-water resources of Calcasieu Parish, Louisiana","interactions":[],"lastModifiedDate":"2022-02-09T20:24:07.378165","indexId":"wsp1488","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1488","title":"The geology and ground-water resources of Calcasieu Parish, Louisiana","docAbstract":"<p>Large quantities of fresh ground water are available in Calcasieu Parish. Fresh water is present in sand of Recent, Pleistocene, Pliocene, and Miocene ages, although locally only small supplies for rural or stock use can be obtained from the shallow sand lenses of Recent and Pleistocene ages. The principal fresh-water-bearing sands are the '200-foot,' '500-foot,' and '700-foot' sands of the Chicot aquifer of Pleistocene age, from which 105 million gallons is pumped daily. A yield of as much as 4,500 gpm (gallons per minute) has been obtained from a single well. The sands are typical of the Chicot aquifer throughout southwestern Louisiana in that generally they grade from fine sand at the top to coarse sand and gravel at the base of the aquifer. The coefficient of permeability of the principal sands in Calcasieu Parish ranges from 660 to about 2,000 gpd (gallons per day) per square foot and averages 1,200 gpd per square foot. The permeability of the sands generally varies with textural changes. The maximum depth of occurrence of fresh ground water in Calcasieu Parish ranges from about 700 feet to 2,500 feet below mean sea level; locally, however, where the sands overlie structures associated with oil fields, the maximum depth is less than 300 feet. Pumping has caused water levels to decline, at varying rates, in all the sands. In the '200-foot' sand they are declining at a rate of about 2 feet per year. In the industrial district of Calcasieu Parish, levels in the '500-foot' sand are declining at a rate of about 5 feet per year, and in the '700-foot' sand at a rate of about 3.5 feet per year. Salt-water contamination is accompanying the water-level decline in the '700-foot' sand in the central part of the parish. Quality-of-water data indicate that water from wells screened in the Chicot aquifer generally is suitable for some uses without treatment but would require treatment to be satisfactory for other uses. The temperature of the water ranges from 70° to 79°F. The lenticular sands of Pliocene and Miocene ages have not been used as a source of fresh ground water in Calcasieu Parish; however, north of the Houston River these formations contain fresh water, and the water contained in these formations in other parts of southwestern Louisiana is known to be soft and suitable for most purposes.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1488","usgsCitation":"Harder, A., 1960, The geology and ground-water resources of Calcasieu Parish, Louisiana: U.S. Geological Survey Water Supply Paper 1488, Report: vi, 102 p.; 9 Plates: 28.00 × 21.86 inches or smaller, https://doi.org/10.3133/wsp1488.","productDescription":"Report: vi, 102 p.; 9 Plates: 28.00 × 21.86 inches or 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,{"id":14281,"text":"ofr6079 - 1960 - Preliminary textures and mineral associations in the ultramafic zone of the Stillwater complex, Montana","interactions":[{"subject":{"id":14281,"text":"ofr6079 - 1960 - Preliminary textures and mineral associations in the ultramafic zone of the Stillwater complex, Montana","indexId":"ofr6079","publicationYear":"1960","noYear":false,"title":"Preliminary textures and mineral associations in the ultramafic zone of the Stillwater complex, Montana"},"predicate":"SUPERSEDED_BY","object":{"id":6052,"text":"pp358 - 1961 - Primary textures and mineral associations in the ultramafic zone of the Stillwater complex, Montana","indexId":"pp358","publicationYear":"1961","noYear":false,"title":"Primary textures and mineral associations in the ultramafic zone of the Stillwater complex, Montana"},"id":1}],"supersededBy":{"id":6052,"text":"pp358 - 1961 - Primary textures and mineral associations in the ultramafic zone of the Stillwater complex, Montana","indexId":"pp358","publicationYear":"1961","noYear":false,"title":"Primary textures and mineral associations in the ultramafic zone of the Stillwater complex, Montana"},"lastModifiedDate":"2025-06-04T15:42:53.850211","indexId":"ofr6079","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-79","title":"Preliminary textures and mineral associations in the ultramafic zone of the Stillwater complex, Montana","docAbstract":"<p>This paper presents some results of work done between 1951 and 1955 as a part of a comprehensive investigation of the stratigraphy, geochemistry, and petrography of the Ultramafic zone of the Stillwater complex by the U. S. Geological Survey. Detailed mapping of the chromite deposits of the complex was done between 1939 and 1943, under the supervision of J. W. Peoples. Reports of this work, and geologic maps of most of the complex, have been published: Peoples and Howland (1940); Wimmler (1948); Howland, Garrels, and Jones (1949); Peoples, Howland, Jones, and Flint (1954); Jackson, Howland, Peoples, and Jones (1954); Howland (1955); Jones, Peoples, and Howland (in press). The present investigation has called for additional mapping and study of many problems which had to be bypassed because of the pressure of wartime urgency. I spent a total of about 15 months in the field during the summers of 1951 through 1955; P. R. Vail assisted in the field work in 1952 and 1953, and R. L. 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