{"pageNumber":"1847","pageRowStart":"46150","pageSize":"25","recordCount":46603,"records":[{"id":61395,"text":"mf41 - 1955 - Preliminary geologic map of the Paris-Bloomington vanadium area, Bear Lake County, Idaho","interactions":[],"lastModifiedDate":"2018-10-12T13:17:09","indexId":"mf41","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"41","title":"Preliminary geologic map of the Paris-Bloomington vanadium area, Bear Lake County, Idaho","docAbstract":"<p>The Permian Phosphoria formation in the vicinity of the towns of Paris and Bloomington, Bear Lake County, Idaho, contains large tannages of vanadiferous mudstone and phosphorite.&nbsp; The area underlain by these rocks was mapped in 1943 as a guide to the exploration of the vanadiferous zone then being conducted by the Wyodak Coal and Manufacturing Company, agent for the Metals Reserve Company.&nbsp; Pending publication of the full data acquired during these studies, the geologic maps are made available here in preliminary form as an aid to any who contemplate mining in the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf41","usgsCitation":"McKelvey, V., and Strobell, J., 1955, Preliminary geologic map of the Paris-Bloomington vanadium area, Bear Lake County, Idaho: U.S. Geological Survey Miscellaneous Field Studies Map 41, 4 Plates: 39.02 x 39.73 inches or smaller, https://doi.org/10.3133/mf41.","productDescription":"4 Plates: 39.02 x 39.73 inches or smaller","costCenters":[],"links":[{"id":183468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0041/report-thumb.jpg"},{"id":358338,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358339,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0041/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358340,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0041/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358341,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0041/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2000","country":"United States","state":"Idaho","county":"Bear Lake County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.48333333333333,42.13472222222222 ], [ -111.48333333333333,42.28444444444444 ], [ -111.35,42.28444444444444 ], [ -111.35,42.13472222222222 ], [ -111.48333333333333,42.13472222222222 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ae5c","contributors":{"authors":[{"text":"McKelvey, V.E.","contributorId":85161,"corporation":false,"usgs":true,"family":"McKelvey","given":"V.E.","email":"","affiliations":[],"preferred":false,"id":265573,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Strobell, J.D. Jr.","contributorId":22823,"corporation":false,"usgs":true,"family":"Strobell","given":"J.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":265572,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51836,"text":"ofr5580 - 1955 - Water levels in observation wells in Nebraska during 1954","interactions":[],"lastModifiedDate":"2015-10-22T11:19:45","indexId":"ofr5580","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-80","title":"Water levels in observation wells in Nebraska during 1954","docAbstract":"<p>The observation well program, begun in 1934 in cooperation with the Conservation and Survey Division, University of Nebraska, was continued during 1954. &nbsp;The United States Geological Survey began a series of ground-water investigations in Nebraska during the fall of 1945, as part of the program for development of the Missouri River basin. &nbsp;These 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,{"id":51838,"text":"ofr5585 - 1955 - Ground-water hydraulics - A summary of lectures presented by John G. Ferris at short courses conducted by the Ground Water Branch, part 1, Theory","interactions":[],"lastModifiedDate":"2015-10-08T11:42:40","indexId":"ofr5585","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-85","title":"Ground-water hydraulics - A summary of lectures presented by John G. Ferris at short courses conducted by the Ground Water Branch, part 1, Theory","docAbstract":"<p>The objective of the Ground Water Branch is to evaluate the occurrence, availability, and quality of ground water. &nbsp;The science of ground-water hydrology is applied toward attaining that goal. &nbsp;Although many ground-water investigations are of a qualitative nature, quantitative studies are necessarily an integral component of the complete evaluation of occurrence and availability. &nbsp;The worth of an aquifer as a fully developed source of water depends largely on two inherent characteristics: its ability to store, and its ability to transmit water. &nbsp;Furthermore, quantitative knowledge of these characteristics facilitates measurement of hydrologic entities such as recharge, leakage, evapotranspiration, etc. &nbsp;It is recognized that these two characteristics, referred to as the coefficients of storage and transmissibility, generally provide the very foundation on which quantitative studies are constructed. &nbsp;Within the science of ground-water hydrology, ground-water hydraulics methods are applied to determine these constats from field data.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5585","usgsCitation":"Knowles, D., 1955, Ground-water hydraulics - A summary of lectures presented by John G. Ferris at short courses conducted by the Ground Water Branch, part 1, Theory: U.S. Geological Survey Open-File Report 55-85, vi, 105 p., https://doi.org/10.3133/ofr5585.","productDescription":"vi, 105 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":275882,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0085/report.pdf"},{"id":177862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1955/0085/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db668dad","contributors":{"authors":[{"text":"Knowles, D.B.","contributorId":83898,"corporation":false,"usgs":true,"family":"Knowles","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":244369,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71583,"text":"tei559 - 1955 - Reconnaissance for uranium in asphalt-bearing rocks in the western states","interactions":[],"lastModifiedDate":"2015-10-20T12:59:44","indexId":"tei559","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"559","title":"Reconnaissance for uranium in asphalt-bearing rocks in the western states","docAbstract":"<p>An appraisal of asphalt-bearing rocks as potential sources of uranium was made during 1953 and 1954 by examining deposits in 45 areas in California, Utah, Wyoming, Montana, New Mexico, Texas, Oklahoma, and Missouri.&nbsp; A total of 202 samples from these areas was analyzed for uranium. The oldest rocks sampled are Ordovician in age, and the youngest are Recent. Although none of the deposits are of value at this time as a source of uranium, some of the deposits may constitute a low grade uranium resource whose recovery will depend upon the primary use to which the asphalt is placed.</p>\n<p>Significant amounts of uranium in the ash of the extracted oil were found in samples from 7 of the 45 areas examined. These areas are Chalone Creek, McKittrick, Edna, and Los Alamos areas, California: Vernal area, Utah; Sulphur area, Oklahoma; and the Ellis area, Missouri. The average uranium content of samples from these seven areas ranges: from 0.028 to 0.376 percent in the ash of the extracted oil. &nbsp;All except the Chalone Creek area contain large estimated reserves of asphalt-bearing rock, ranging from 15,000,000 to almost 2,000,000,000 tons.&nbsp; The average uranium content of samples from 13 additional areas ranges from 0.020 to 0.068 percent in the ash of the extracted oil. &nbsp;Many of these areas contain very large reserves of asphalt-bearing rocks.</p>\n<p>Evaluation of field data indicates that naturally occurring asphalts with a relatively high uranium content probably originated in, or migrated through, rocks that contain more than average amounts of uranium. It is believed that some of the uranium was present as an original constituent of the oil but that some uranium may have been introduced during migration of the oil.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei559","usgsCitation":"Hail, W.J., 1955, Reconnaissance for uranium in asphalt-bearing rocks in the western states: U.S. Geological Survey Trace Elements Investigations 559, 49 p., https://doi.org/10.3133/tei559.","productDescription":"49 p.","numberOfPages":"50","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":90857,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/559/report.pdf","text":"Report","size":"14.55 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":185933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/559/report-thumb.jpg"}],"country":"United States","state":"California, Missouri, Montana, New Mexico, Oklahoma, Texas, Utah, Wyoming","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-119.789798,34.05726],[-119.5667,34.053452],[-119.795938,33.962929],[-119.916216,34.058351],[-119.789798,34.05726]]],[[[-118.524531,32.895488],[-118.573522,32.969183],[-118.369984,32.839273],[-118.524531,32.895488]]],[[[-118.500212,33.449592],[-118.32446,33.348782],[-118.593969,33.467198],[-118.500212,33.449592]]],[[[-122.289533,42.007764],[-120.001058,41.995139],[-120.001014,38.999574],[-114.633013,35.002085],[-114.139534,34.295844],[-114.401352,34.111652],[-114.5403,33.580615],[-114.701732,33.408388],[-114.707896,33.097432],[-114.502871,33.011153],[-114.468971,32.845155],[-114.612697,32.734516],[-117.118868,32.534706],[-117.50565,33.334063],[-118.088896,33.729817],[-118.428407,33.774715],[-118.519514,34.027509],[-119.159554,34.119653],[-119.616862,34.420995],[-120.441975,34.451512],[-120.608355,34.556656],[-120.644311,35.139616],[-120.873046,35.225688],[-120.884757,35.430196],[-121.851967,36.277831],[-121.932508,36.559935],[-121.788278,36.803994],[-121.880167,36.950151],[-122.140578,36.97495],[-122.419113,37.24147],[-122.511983,37.77113],[-122.425942,37.810979],[-122.168449,37.504143],[-122.144396,37.581866],[-122.385908,37.908136],[-122.301804,38.105142],[-122.484411,38.11496],[-122.492474,37.82484],[-122.972378,38.020247],[-123.103706,38.415541],[-123.725367,38.917438],[-123.851714,39.832041],[-124.373599,40.392923],[-124.063076,41.439579],[-124.23972,41.7708],[-124.203402,41.940964],[-122.289533,42.007764]]],[[[-89.545006,36.336809],[-89.703511,36.243412],[-89.615128,36.113816],[-89.733095,36.000608],[-90.368718,35.995812],[-90.075934,36.281485],[-90.157136,36.484317],[-94.617919,36.499414],[-94.431822,35.397652],[-94.485528,33.663388],[-94.386086,33.544923],[-94.070395,33.574561],[-94.0427,32.056012],[-93.523248,31.037842],[-93.765822,30.333318],[-93.702436,30.112721],[-93.922744,29.818808],[-93.852868,29.675885],[-94.731047,29.369141],[-94.532348,29.5178],[-94.767246,29.525523],[-94.724616,29.774766],[-94.965963,29.70033],[-94.894234,29.338],[-95.16525,29.113566],[-94.73132,29.338066],[-94.803695,29.279237],[-96.341617,28.417334],[-95.983106,28.641942],[-96.221784,28.580364],[-96.287942,28.683164],[-96.473694,28.57324],[-96.664534,28.696904],[-96.481836,28.407844],[-96.790235,28.383926],[-96.898123,28.152881],[-97.21535,28.076575],[-97.040618,28.028708],[-97.183455,27.833231],[-97.354614,27.849572],[-97.296598,27.613947],[-97.399398,27.344735],[-97.640111,27.270943],[-97.485149,27.250841],[-97.552325,26.867633],[-97.145567,25.971132],[-97.36542,25.849826],[-99.110855,26.426278],[-99.452316,27.062669],[-99.556812,27.614336],[-99.841708,27.766464],[-100.280518,28.267969],[-100.785521,29.228137],[-101.441059,29.753451],[-102.341033,29.869305],[-102.698347,29.695591],[-102.944911,29.18882],[-103.227801,28.991532],[-104.46652,29.609296],[-104.924796,30.604832],[-106.158218,31.438885],[-106.381039,31.73211],[-108.208394,31.783599],[-108.208573,31.333395],[-109.050044,31.332502],[-109.045272,36.968871],[-94.625224,36.998672],[-94.605734,39.122204],[-95.082714,39.516712],[-94.876344,39.806894],[-95.382957,40.027112],[-95.731179,40.525436],[-95.64184,40.584234],[-91.625161,40.5435],[-91.452458,40.375501],[-91.510322,40.127994],[-91.369953,39.745042],[-90.721593,39.23273],[-90.653164,38.916141],[-90.113327,38.849306],[-90.370819,38.333554],[-90.322353,38.181593],[-89.516685,37.692762],[-89.438275,37.161287],[-89.102879,36.9697],[-89.202607,36.601576],[-89.343753,36.630991],[-89.429311,36.481875],[-89.55264,36.577178],[-89.545006,36.336809]]],[[[-111.048974,44.474072],[-111.323669,44.724474],[-111.50494,44.635746],[-111.469185,44.552044],[-112.258665,44.569516],[-112.387389,44.448058],[-112.749011,44.491233],[-112.844859,44.358221],[-113.134824,44.752763],[-113.455071,44.865424],[-113.802955,45.592631],[-114.015633,45.696127],[-114.345019,45.459916],[-114.559038,45.565706],[-114.422963,45.855381],[-114.527096,46.146218],[-114.322912,46.642938],[-114.76689,46.696901],[-115.294785,47.220914],[-115.731348,47.433381],[-115.72377,47.696671],[-116.049153,47.999923],[-116.049193,49.000912],[-104.048736,48.999877],[-104.053097,41.018045],[-109.050076,41.000659],[-109.045223,36.999084],[-114.0506,37.000396],[-114.041723,41.99372],[-111.046689,42.001567],[-111.048974,44.474072]]],[[[-97.240849,26.411504],[-97.383531,26.875521],[-97.366771,27.333276],[-96.946988,28.026522],[-96.403206,28.371475],[-96.929053,27.99044],[-97.276091,27.472145],[-97.370731,26.909706],[-97.161471,26.088705],[-97.240849,26.411504]]]]},\"properties\":{\"name\":\"California\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db643f9a","contributors":{"authors":[{"text":"Hail, William James Jr.","contributorId":95933,"corporation":false,"usgs":true,"family":"Hail","given":"William","suffix":"Jr.","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":284430,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51855,"text":"ofr55120 - 1955 - Basic data of the 1946-47 study of the ground-water resources of Brevard County, Florida","interactions":[],"lastModifiedDate":"2014-07-14T10:11:19","indexId":"ofr55120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-120","title":"Basic data of the 1946-47 study of the ground-water resources of Brevard County, Florida","docAbstract":"A reconnaissance investigation of the ground-water resources of Brevard County was made in 1946-47 by the United States Geological Survey in cooperation with the Florida Geological Survey. The following tables of well records and illustrations were compiled from data collected during that investigation.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr55120","usgsCitation":"Neill, R.M., 1955, Basic data of the 1946-47 study of the ground-water resources of Brevard County, Florida: U.S. Geological Survey Open-File Report 55-120, 21 p., https://doi.org/10.3133/ofr55120.","productDescription":"21 p.","numberOfPages":"21","costCenters":[],"links":[{"id":289856,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289855,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0120/report.pdf"}],"country":"United States","state":"Florida","county":"Brevard County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.9871,27.8221 ], [ -80.9871,28.7914 ], [ -80.4464,28.7914 ], [ -80.4464,27.8221 ], [ -80.9871,27.8221 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640c66","contributors":{"authors":[{"text":"Neill, Robert M.","contributorId":18682,"corporation":false,"usgs":true,"family":"Neill","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":244396,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2433,"text":"wsp1255 - 1955 - Water resources of southeastern Florida, with special reference to the geology and ground water of the Miami area","interactions":[],"lastModifiedDate":"2024-02-22T23:08:50.440875","indexId":"wsp1255","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1255","title":"Water resources of southeastern Florida, with special reference to the geology and ground water of the Miami area","docAbstract":"<p>The circulation of water, in any form, from the surface of the earth to the atmosphere and back again is called the hydrologic cycle. A comprehensive study of the water resources of any area must, therefore, include data on the climate of the area.</p><p>The humid subtropical climate of southeastern Florida is characterized by relatively high temperatures, alternating semi-annual wet and dry seasons, and usually light but persistent winds.</p><p>The recurrence of drought in an area having relatively large rainfall such as southeastern Florida indicates that the agencies that remove water are especially effective. Two of the most important of the agencies associated with climate are evaporation and transpiration, or \"evapotranspiration\". Evaporation losses from permanent water areas are believed to average between about 40 and 45 inches per year. Over land areas indirect methods must be used to determine losses by evapotranspiration; necessarily, these values are not precise.</p><p>Because of their importance in the occurrence and movement of both surface and ground waters, detailed studies were made of the geology and geomorphology of southern Florida.</p><p>As a result of widespread crustal movements, southern Florida emerged from the sea in late Pliocene time and probably was slightly tilted to the west. At the beginning of the Pleistocene the continent emerged still farther as a result of the lowering of sea level attending the first widespread glaciation. During this epoch, southern Florida may have stood several hundred feet above sea level.</p><p>During the interglacial ages the sea repeatedly flooded southern Florida. The marine members of the Fort Thompson formation in the Lake Okeechobee-Everglades depression and the Caloosahatchee River Valley apparently are the deposits of these interglacial invasions by the sea. The fresh-water marls, sands, and organic deposits of the Fort Thompson formation appear to have accumulated during glacial ages when sea level was low and the area was a land surface partly occupied by fresh-water lakes and marshes. Elsewhere in southern Florida the deposits are mainly marine limestones and sandy terrace deposits.</p><p>The Pliocene surface upon which these Pleistocene sediments were deposited was highest to the north and west of the present Everglades and Kissimmee River basin, and it sloped gently to the south, southeast, and east. On this slightly sloping floor, alternately submerged and emerged, the later materials were built; these materials modified by wind, rain, and surface and ground waters, have largely determined the present topographic and ecologic character of southern Florida.</p><p>The most important aquifer in southern Florida, and the one in which most of the wells are developed, is the Biscayne aquifer. It is composed of parts of the Tamiami formation (Miocene), Caloosahatchee marl (Pliocene), Fort Thompson formation, Anastasia formation, Key Largo limestone, Miami oolite, and Pamlico sand (Pleistocene). In some parts of southern Florida, the Pamlico sand and the Anastasia formation are not a part of the Biscayne aquifer; however, they are utilized in the development of small water supplies. Most of the Caloosahatchee marl and the Fort Thompson formation in the Lake Okeechobee area is of very low permeability. In the northern Everglades their less permeable parts contain highly mineralized waters, which appear to have been trapped since the invasions by the Pleistocene seas. These waters have been modified by dilution with fresh ground water and by chemical reactions with surrounding materials.</p><p>Sea-level fluctuations, starting at the close of the Pliocene with the highest levels and progressing toward the Recent with successively lower levels, have built a series of nearly flat marine terrances abutting against one another much like a series of broad stearsteps. Erosion and solution have defaced and, in places, have obliterated the original surficial forms of these old sea bottoms, shores, and shoreline features, but their remnants today are widespread and, in some places, are easily recognizable.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1255","collaboration":"Prepared in cooperation with the Florida Geological Survey, Dade County, cities of Miami and Miami Beach, and other agencies","usgsCitation":"Parker, G., Ferguson, G., and Love, S.K., 1955, Water resources of southeastern Florida, with special reference to the geology and ground water of the Miami area: U.S. Geological Survey Water Supply Paper 1255, Report: xxv, 965 p.; 24 Plates: 19.50 x 30.25 inches or smaller, https://doi.org/10.3133/wsp1255.","productDescription":"Report: xxv, 965 p.; 24 Plates: 19.50 x 30.25 inches or smaller","costCenters":[],"links":[{"id":425904,"rank":28,"type":{"id":36,"text":"NGMDB Index 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    ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0656","contributors":{"authors":[{"text":"Parker, Garald G.","contributorId":106880,"corporation":false,"usgs":true,"family":"Parker","given":"Garald G.","affiliations":[],"preferred":false,"id":145191,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferguson, G.E.","contributorId":62575,"corporation":false,"usgs":true,"family":"Ferguson","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":145190,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":145189,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71616,"text":"tei595 - 1955 - On the air-scattering of gamma rays from thick uranium sources","interactions":[],"lastModifiedDate":"2014-05-23T16:01:33","indexId":"tei595","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"595","title":"On the air-scattering of gamma rays from thick uranium sources","docAbstract":"<p>Semiquantative interpretation of data from airborne radioactivity surveying requires detailed knowledge of air-scattered gamma-ray intensity at considerable air distances from natural, thick uranium sources. Based on the concept of an elementary source of infinite\nthickness rather than on the classical point source, semi-empirical\nexpressions, are developed for measured gamma-radiation intensities from\n. the two extreme types of natural, thick uranium sources, the elementary\n(point) and t-he broad (semi-infinite) source. These expressions agree\nboth with extensive experimental data and with the form and structure\nof theory.</p>\n<br>\n<p>Theoretical computations based on published solutions of the\nBoltzmann equation for ga.m.ma-ray transport in one medium agree closely\nwith experimental measurements. The calculated value for primary,\nscattered,  and total intensities from thick uranium sources show that\nat considerable air distances the scattered intensities are more than\nhalf of the total intensities for energies above 0.4 Mev and become\nconsiderably more than half as the lower limit of detector energy\nresponse is decreased below 0.4 Mev.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei595","collaboration":"This report concerns work done on behalf of the Division of Research of the U.S. Atomic Energy Commission","usgsCitation":"Sakakura, A.Y., 1955, On the air-scattering of gamma rays from thick uranium sources: U.S. Geological Survey Trace Elements Investigations 595, 99 p., https://doi.org/10.3133/tei595.","productDescription":"99 p.","numberOfPages":"100","costCenters":[],"links":[{"id":284162,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei595.jpg"},{"id":285962,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0595/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691b75","contributors":{"authors":[{"text":"Sakakura, Arthur Y.","contributorId":54117,"corporation":false,"usgs":true,"family":"Sakakura","given":"Arthur","email":"","middleInitial":"Y.","affiliations":[],"preferred":false,"id":284482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51817,"text":"ofr5535 - 1955 - Statement on ground water in Connecticut","interactions":[],"lastModifiedDate":"2014-07-09T13:43:34","indexId":"ofr5535","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-35","title":"Statement on ground water in Connecticut","docAbstract":"Connecticut has a supply of ground water, most of it of good quality, which is largely undeveloped, and much of which would lend itself to industrial and other uses. Ground water is available in small quantities in nearly all parts of the State, and in moderate to large quantities in many areas, chiefly along the major stream. However, specific and detailed information on the ground water is available in report form for relatively few specific localities and areas. Definitive investigations of the occurrence, general availability, quality, and quality of ground water in Connecticut are being made under cooperative agreements between the State Water Commission and the U.S. Geological Survey; and some progress has been made. Generalized information of a reconnaissance nature is shown on plate 1, which gives areas of estimated moderate to large yields, delineated on the basis of currently available data, and shows the locations of wells for which records are given in tables 1 and 2. Some specific information on particular areas is available in the open files of the agencies cooperating in the investigations.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5535","collaboration":"Prepared in cooperation with the Connecticut State Water Commission","usgsCitation":"Cushman, R., 1955, Statement on ground water in Connecticut: U.S. Geological Survey Open-File Report 55-35, 6 p., https://doi.org/10.3133/ofr5535.","productDescription":"6 p.","numberOfPages":"11","costCenters":[],"links":[{"id":289665,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289664,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0035/report.pdf"}],"country":"United States","state":"Connecticut","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.8321,40.9851 ], [ -73.8321,42.2013 ], [ -71.4,42.2013 ], [ -71.4,40.9851 ], [ -73.8321,40.9851 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb2a8","contributors":{"authors":[{"text":"Cushman, R.V.","contributorId":28220,"corporation":false,"usgs":true,"family":"Cushman","given":"R.V.","email":"","affiliations":[],"preferred":false,"id":244340,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22611,"text":"ofr5521 - 1955 - Data on water wells in Coyote, Cronise, Soda, and Silver Lake Valleys, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:50","indexId":"ofr5521","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-21","title":"Data on water wells in Coyote, Cronise, Soda, and Silver Lake Valleys, San Bernardino County, California","language":"ENGLISH","publisher":"United States Department of the Interior, Geological Survey, Ground Water Branch,","doi":"10.3133/ofr5521","issn":"0094-9140","usgsCitation":"Burnham, W., 1955, Data on water wells in Coyote, Cronise, Soda, and Silver Lake Valleys, San Bernardino County, California: U.S. Geological Survey Open-File Report 55-21, 48 p, https://doi.org/10.3133/ofr5521.","productDescription":"48 p","costCenters":[],"links":[{"id":153813,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1955/0021/report-thumb.jpg"},{"id":52081,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1955/0021/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52082,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac5e4b07f02db679d77","contributors":{"authors":[{"text":"Burnham, W.L.","contributorId":58668,"corporation":false,"usgs":true,"family":"Burnham","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":188564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15759,"text":"ofr55158 - 1955 - Geochemical exploration for antimony in southeastern Alaska","interactions":[{"subject":{"id":15759,"text":"ofr55158 - 1955 - Geochemical exploration for antimony in southeastern Alaska","indexId":"ofr55158","publicationYear":"1955","noYear":false,"title":"Geochemical exploration for antimony in southeastern Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":35717,"text":"b1024H - 1957 - A geochemical exploration for antimony in southeastern Alaska","indexId":"b1024H","publicationYear":"1957","noYear":false,"chapter":"H","title":"A geochemical exploration for antimony in southeastern Alaska"},"id":1}],"supersededBy":{"id":35717,"text":"b1024H - 1957 - A geochemical exploration for antimony in southeastern Alaska","indexId":"b1024H","publicationYear":"1957","noYear":false,"title":"A geochemical exploration for antimony in southeastern Alaska"},"lastModifiedDate":"2023-07-14T19:06:24.911348","indexId":"ofr55158","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-158","title":"Geochemical exploration for antimony in southeastern Alaska","docAbstract":"<p>Preliminary geochemical prospecting by the Geological Survey was carried out in 1952 in muskeg-covered ground at Caamano Point, Cleveland Peninsula, Alaska, in an effort to delimit areas of stibnite concentrations. It was conducted to aid, if possible, a prospecting project of the Defense Minerals Exploration. Samples were collected from soil and decomposed limestone-and-schist bedrock at depths ranging from 18 inches to 60 inches, by means of a pipe with an interior plunger.</p><p>Initial sampling was followed by detailed sampling of the areas where the antimony content of the soils consistently averaged more than 300 ppm. These Areas of major soil concentrations were prospected by surface trenching and percussion drilling to depths of 20 feet which proved the existence of stibnite ore. Next a shaft and drifts made in the most favorable area proved disseminated stibnite ore to depths of 60 feet.</p><p>This geochemical work of soil sampling to indicate hidden ore bodies in a typical Alaskan muskeg area is believed to be the first application in Alaska of such techniques in active ore exploration. The results show the economic feasibility of such exploration as a first step in extending the known boundaries of mineralized areas, and in directing initial exploration toward the most favorable areas of near-surface ore bodies.</p><p>Data are presented to help establish values of soil content of antimony that may be considered as normal in this type of geologic terrain.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr55158","usgsCitation":"Sainsbury, C., 1955, Geochemical exploration for antimony in southeastern Alaska: U.S. Geological Survey Open-File Report 55-158, Report: 28 p.; 4 Plates: 19.61 x 29.88 inches or smaller, https://doi.org/10.3133/ofr55158.","productDescription":"Report: 28 p.; 4 Plates: 19.61 x 29.88 inches or 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C.L.","contributorId":99968,"corporation":false,"usgs":true,"family":"Sainsbury","given":"C.L.","email":"","affiliations":[],"preferred":false,"id":171657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51822,"text":"ofr5548 - 1955 - Flood of May 27-28, 1954, in Panola and Lafayette Counties, Mississippi","interactions":[],"lastModifiedDate":"2014-07-09T13:53:50","indexId":"ofr5548","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-48","title":"Flood of May 27-28, 1954, in Panola and Lafayette Counties, Mississippi","docAbstract":"<p>As a result of heavy rains during the late afternoon and night of May 27, 1954, record-breaking floods occurred on small streams in Panola and Lafayette Counties. All flooding was in rural areas, and no loss of life was reported. The Agriculture Stabilization Committees at Sardis and at Oxford estimated the crop and soil losses in Panola county as $400,000, and in Lafayette County as $25,000. The total damage to county roads and State highways was estimated to be in excess of $25,000.</p>\n<br/>\n<p>The purpose of this report is to present rainfall information and more detailed runoff data than are found in the regular Water Supply Papers. The report contains a summary of peak discharges at 10 miscellaneous sites and a detailed record of discharge at the gaging station Clear Creek near Oxford, Miss.</p>\n<br/>\n<p>Field investigation incident to this report were conducted by members of the District Office, U.S. Geological Survey, Jackson, Miss., I. E. Anderson, District Engineer.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Jackson, MS","doi":"10.3133/ofr5548","usgsCitation":"Goines, W., 1955, Flood of May 27-28, 1954, in Panola and Lafayette Counties, Mississippi: U.S. Geological Survey Open-File Report 55-48, 13 p., https://doi.org/10.3133/ofr5548.","productDescription":"13 p.","numberOfPages":"13","costCenters":[],"links":[{"id":289672,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289671,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0048/report.pdf"}],"country":"United States","state":"Mississippi","county":"Lafayette County;Panola County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.0508,34.0487 ], [ -90.0508,34.5204 ], [ -89.4473,34.5204 ], [ -89.4473,34.0487 ], [ -90.0508,34.0487 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5df976","contributors":{"authors":[{"text":"Goines, W.H.","contributorId":95088,"corporation":false,"usgs":true,"family":"Goines","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":244346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51828,"text":"ofr5563 - 1955 - Ground-water conditions between Oracle and Oracle Junction, Pinal County, Arizona","interactions":[],"lastModifiedDate":"2014-07-09T14:00:45","indexId":"ofr5563","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-63","title":"Ground-water conditions between Oracle and Oracle Junction, Pinal County, Arizona","docAbstract":"<p>The development of the San Manuel copper prospect has greatly increased traffic along State Highway 77. Considerable interest in commercial possibilities along that road has resulted in a request by the Arizona State Land Department for information about the ground-water conditions between Oracle and Oracle Junction. This request came too late for information to be included in a recently completed memorandum report on the occurrence of ground water in the vicinity of Oracle, released in February 1955. These data are presented as a supplement to that report to minimized duplication of statements about the general geologic and hydrologic conditions. The necessary well data and sample descriptions that were not included in the Oracle report are shown in tables 3 and 4.</p>\n<br/>\n<p>The area discussed in this supplement comprises parts of Tps. 9 and 10 S., Rs. 13, 14, and 15 E., and includes about 90 square miles (fig. 3). The eastern portion overlaps part of the area covered by the earlier report.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tucson, AZ","doi":"10.3133/ofr5563","collaboration":"A supplement to \"Memorandum on geology and ground-water resources in the vicinity of Oracle, Pinal County, Arizona.\" Prepared in cooperation with Arizona State Land Department, Roger Ernst, Commissioner","usgsCitation":"Heindl, L., 1955, Ground-water conditions between Oracle and Oracle Junction, Pinal County, Arizona: U.S. Geological Survey Open-File Report 55-63, 4 p., https://doi.org/10.3133/ofr5563.","productDescription":"4 p.","numberOfPages":"8","costCenters":[],"links":[{"id":289676,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":289675,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0063/report.pdf"}],"country":"United States","state":"Arizona","county":"Pinal County","city":"Oracle;Oracle Junction","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.975151,32.539636 ], [ -110.975151,32.651248 ], [ -110.740825,32.651248 ], [ -110.740825,32.539636 ], [ -110.975151,32.539636 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d300","contributors":{"authors":[{"text":"Heindl, L.A.","contributorId":52150,"corporation":false,"usgs":true,"family":"Heindl","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":244353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51827,"text":"ofr5557 - 1955 - Water supplies for irrigation in the Northeast","interactions":[],"lastModifiedDate":"2015-10-22T11:17:33","indexId":"ofr5557","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-57","title":"Water supplies for irrigation in the Northeast","docAbstract":"<p>The subject of this paper as given on the program is \"Water Supplies for Irrigation in the Northeast.\" &nbsp;Both surface-water and ground-water resources are discussed, although with somewhat differing approaches. &nbsp;First we discuss the use of streamflow data in estimating the surface-water supplies available for irrigation use. &nbsp;Then we treat some of the hydrologic factors that bear on the uses of ground-water for irrigation in the New England-New York region.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5557","usgsCitation":"Hardison, C., and Hackett, O.M., 1955, Water supplies for irrigation in the Northeast: U.S. Geological Survey Open-File Report 55-57, 19 p., https://doi.org/10.3133/ofr5557.","productDescription":"19 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":177333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr5557.jpg"},{"id":310414,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Connecticut, Maine, Massachusetts, New Hampshire, New York, Rhode Island, 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M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":244352,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51826,"text":"ofr5556 - 1955 - Data on wells and test borings in the Slocum quadrangle, Rhode Island","interactions":[],"lastModifiedDate":"2021-01-21T19:21:03.800973","indexId":"ofr5556","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-56","title":"Data on wells and test borings in the Slocum quadrangle, Rhode Island","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5556","usgsCitation":"Hahn, G., 1955, Data on wells and test borings in the Slocum quadrangle, Rhode Island: U.S. Geological Survey Open-File Report 55-56, Report: 36 p.; 1 Plate: 7.24 x 9.04 inches, https://doi.org/10.3133/ofr5556.","productDescription":"Report: 36 p.; 1 Plate: 7.24 x 9.04 inches","costCenters":[],"links":[{"id":382399,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1955/0056/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382398,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0056/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177332,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1955/0056/report-thumb.jpg"}],"country":"United States","state":"Rhode Island","otherGeospatial":"Slocum quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.61749999999999,41.5 ], [ -71.61749999999999,41.6175 ], [ -71.5,41.6175 ], [ -71.5,41.5 ], [ -71.61749999999999,41.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bd2d","contributors":{"authors":[{"text":"Hahn, G.W.","contributorId":49235,"corporation":false,"usgs":true,"family":"Hahn","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":244350,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48491,"text":"ofr80340 - 1955 - Annual peak discharges from small drainage areas in Montana through September 1979","interactions":[],"lastModifiedDate":"2012-02-02T00:10:06","indexId":"ofr80340","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"80-340","title":"Annual peak discharges from small drainage areas in Montana through September 1979","docAbstract":"Annual peak stage and discharge data have been collected and tabulated for crest-stage gaging sites in Montana. The crest-stage program was begun in July 1955 to investigate the magnitude and frequency of floods from small drainage areas. The program has expanded from 45 crest-stage gaging stations initially to 173 stations maintained in 1979. Data in the report are tabulated for the period of record. (USGS)","language":"ENGLISH","doi":"10.3133/ofr80340","usgsCitation":"Omang, R.J., Parrett, C., and Hull, J.A., 1955, Annual peak discharges from small drainage areas in Montana through September 1979: U.S. Geological Survey Open-File Report 80-340, 120 p. : maps ; 27 cm.; 2 over-size sheets, https://doi.org/10.3133/ofr80340.","productDescription":"120 p. : maps ; 27 cm.; 2 over-size sheets","costCenters":[],"links":[{"id":162043,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bb52","contributors":{"authors":[{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":237613,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parrett, C.","contributorId":43400,"corporation":false,"usgs":true,"family":"Parrett","given":"C.","email":"","affiliations":[],"preferred":false,"id":237615,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hull, J. A.","contributorId":39345,"corporation":false,"usgs":true,"family":"Hull","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":237614,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2845,"text":"wsp1298 - 1955 - Reconnaissance of geology and ground water in the lower Grand River valley, South Dakota, with a section on Chemical quality of the ground water","interactions":[],"lastModifiedDate":"2016-04-05T09:11:18","indexId":"wsp1298","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1298","title":"Reconnaissance of geology and ground water in the lower Grand River valley, South Dakota, with a section on Chemical quality of the ground water","docAbstract":"<p>The area described in this report is the flood plain of the Grand River and the bordering benchlands in Perkins and Corson Counties, S. Dak., from a point about 6 miles west of the town of Shadehill to the confluence of the Grand and Missouri Rivers near Mobridge.</p>\n<p>The exposed bedrock formations include the Pierre shale, the Fox Hills sandstone, and the Hell Creek formation of Late Cretaceous age, and-the Ludlow member of the Fort Union formation of Tertiary (Paleocene) age. Some stringers of the Cannonball formation probably interfinger with beds of the Ludlow member but none of the former was identified during the field investigations. The Pierre shale is exposed from the mouth of the Grand River to approximately the center of the area. Although a few wells in the area obtain water from this formation, it is not generally considered to be a source of supply. The Fox Hills sandstone, the Hell Creek formation, and the Ludlow member of the Fort Union formation are exposed successively upstream and, where saturated, yield small to moderate quantities of water to wells.</p>\n<p>Unconsolidated deposits of silt, sand, and gravel occur in several physiographic positions; they underlie the high benchland on both sides of the river, the poorly defined terraces along the river, and the flood plain throughout its entire length. Possibly all these unconsolidated deposits are water bearing; however, where the deposits on the benchland and in the terraces are dissected by streams, they probably contain little or no water.</p>\n<p>The average depth to ground water along the lower Grand River valley is about 17 feet. Probably, the flow of ground water in the bottom lands is nearly parallel to and slightly toward the surface stream. The measurements of the water level in observation wells for the period 1946-48 indicate that the fluctuations of the water table are small.</p>\n<p>The results of analyses of 13 samples of ground water from the alluvium and the Hell Creek formation show that the suitability of the ground water for use varies because of the considerable range in mineralization and composition. Dissolved solids ranged from 343 to 4,250 parts per million (ppm), hardness from 11 to 1,130 ppm, and percentage of sodium from 25 to 98. Concentrations of some of the individual constituents exceed standards of the United States Public Health Service. The water is moderately hard and contains undesirable amounts of iron and moderate to large amounts of dissolved solids. In general, the water quality ranges from excellent to unsuitable for irrigation use. The result of the mixing of the ground water with recharge water from Shadehill Reservoir cannot be predicted on the basis of available data.</p>\n<p>The geologic and hydrologic data in this report were obtained from earlier reports and from field observations during the period 1946-48. The report includes a geologic map and tabulated well records.</p>","language":"English","publisher":"U.S. Government Print Office","publisherLocation":"Washington, DC","doi":"10.3133/wsp1298","usgsCitation":"Tychsen, P.C., Vorhis, R., and Jochens, E.R., 1955, Reconnaissance of geology and ground water in the lower Grand River valley, South Dakota, with a section on Chemical quality of the ground water: U.S. Geological Survey Water Supply Paper 1298, Report: iv, 33 p.; 2 Plates: 30.00 x 18.15 inches and 27.50 x 9.69 inches, https://doi.org/10.3133/wsp1298.","productDescription":"Report: iv, 33 p.; 2 Plates: 30.00 x 18.15 inches and 27.50 x 9.69 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":138696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1298/report-thumb.jpg"},{"id":29415,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1298/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29416,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1298/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29417,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1298/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Dakota","otherGeospatial":"Grand River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.23876953125,\n              45.336701909968106\n            ],\n            [\n              -102.23876953125,\n              45.73685954736049\n            ],\n            [\n              -100.30517578125,\n              45.73685954736049\n            ],\n            [\n              -100.30517578125,\n              45.336701909968106\n            ],\n            [\n              -102.23876953125,\n              45.336701909968106\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c389","contributors":{"authors":[{"text":"Tychsen, Paul C.","contributorId":82683,"corporation":false,"usgs":true,"family":"Tychsen","given":"Paul","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vorhis, R.C.","contributorId":32512,"corporation":false,"usgs":true,"family":"Vorhis","given":"R.C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":145894,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jochens, Eugene R.","contributorId":55804,"corporation":false,"usgs":true,"family":"Jochens","given":"Eugene","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145895,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40065,"text":"ofr55103 - 1955 - Data on Fountain Creek project, Colorado Springs, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:10:36","indexId":"ofr55103","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-103","title":"Data on Fountain Creek project, Colorado Springs, Colorado","language":"ENGLISH","doi":"10.3133/ofr55103","usgsCitation":"McLaughlin, T.G., 1955, Data on Fountain Creek project, Colorado Springs, Colorado: U.S. Geological Survey Open-File Report 55-103, 1 map., https://doi.org/10.3133/ofr55103.","productDescription":"1 map.","costCenters":[],"links":[{"id":172869,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c878","contributors":{"authors":[{"text":"McLaughlin, Thad G.","contributorId":95548,"corporation":false,"usgs":true,"family":"McLaughlin","given":"Thad","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":222932,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1162,"text":"wsp1357 - 1955 - Computations of total sediment discharge, Niobrara River near Cody, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1357","title":"Computations of total sediment discharge, Niobrara River near Cody, Nebraska","docAbstract":"A natural chute in the Niobrara River near Cody, Nebr., constricts the flow of the river except at high stages to a narrow channel in which the turbulence is sufficient to suspend nearly the total sediment discharge. Because much of the flow originates in the sandhills area of Nebraska, the water discharge and sediment discharge are relatively uniform. \r\n\r\nSediment discharges based on depth-integrated samples at a contracted section in the chute and on streamflow records at a recording gage about 1,900 feet upstream are available for the period from April 1948 to September 1953 but are not given directly as continuous records in this report. Sediment measurements have been made periodically near the gage and at other nearby relatively unconfined sections of the stream for comparison with measurements at the contracted section. \r\n\r\nSediment discharge at these relatively unconfined sections was computed from formulas for comparison with measured sediment discharges at the contracted section. A form of the Du Boys formula gave computed tonnages of sediment that were unsatisfactory. Sediment discharges as computed from the Schoklitsch formula agreed well with measured sediment discharges that were low, but they were much too low at measured sediment discharges that were higher. The Straub formula gave computed discharges, presumably of bed material, that were several times larger than measured discharges of sediment coarser than 0.125 millimeter. All three of these formulas gave computed sediment discharges that increased with water discharges much less rapidly than the measured discharges of sediment coarser than 0.125 millimeter. \r\n\r\nThe Einstein procedure when applied to a reach that included 10 defined cross sections gave much better agreement between computed sediment discharge and measured sediment discharge than did anyone of the three other formulas that were used. This procedure does not compute the discharge of sediment that is too small to be found in the stream bed in appreciable quantities. Hence, total sediment discharges were obtained by adding computed discharges of sediment larger than 0.125 millimeter to measured discharges of sediment smaller than 0.125 millimeter. The size distributions of the computed sediment discharge compared poorly with the size distributions of sediment discharge at the contracted section. Ten sediment discharges computed from the Einstein procedure as applied to a single section averaged several times the measured sediment discharge for the contracted section and gave size distributions that were unsatisfactory.\r\n\r\nThe Einstein procedure was modified to compute total sediment discharge at an alluvial section from readily measurable field data. The modified procedure uses measurements of bed-material particle sizes, suspended-sediment concentrations and particle sizes from depth-integrated samples, streamflow, and water temperatures. Computations of total sediment discharge were made by using this modified procedure, some for the section at the gaging station and some for each of two other relatively unconfined sections. The size distributions of the computed and the measured sediment discharges agreed reasonably well. Major advantages of this modified procedure include applicability to a single section rather than to a reach of channel, use of measured velocity instead of water-surface slope, use of depth-integrated samples, and apparently fair accuracy for computing both total sediment discharge and approximate size distribution of the sediment. Because of these advantages this modified procedure is being further studied to increase its accuracy, to simplify the required computations, and to define its limitations. \r\n\r\nIn the development of the modified procedure, some relationships concerning theories of sediment transport were reviewed and checked against field data. Vertical distributions of suspended sediment at relatively unconfined sections did not agree well with theoretical dist","language":"ENGLISH","publisher":"U.S. Geological Survey ; for sale by U.S. G.P.O.,","doi":"10.3133/wsp1357","isbn":"pbk","usgsCitation":"Colby, B.R., and Hembree, C., 1955, Computations of total sediment discharge, Niobrara River near Cody, Nebraska: U.S. Geological Survey Water Supply Paper 1357, vii, 187 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1357.","productDescription":"vii, 187 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1357/report-thumb.jpg"},{"id":25989,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25990,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25991,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25992,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25993,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25994,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25995,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25996,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1357/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6392","contributors":{"authors":[{"text":"Colby, Bruce R.","contributorId":59775,"corporation":false,"usgs":true,"family":"Colby","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hembree, C. H.","contributorId":106866,"corporation":false,"usgs":true,"family":"Hembree","given":"C. H.","affiliations":[],"preferred":false,"id":143283,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48707,"text":"ofr81332 - 1955 - Annual peak discharges from small drainage areas in Montana through September 1980","interactions":[],"lastModifiedDate":"2012-02-02T00:10:22","indexId":"ofr81332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"81-332","title":"Annual peak discharges from small drainage areas in Montana through September 1980","docAbstract":"Annual peak stage and discharge data have been collected and tabulated for crest-stage gaging sites in Montana. The crest-stage program was begun in July 1955 to investigate the magnitude and frequency of floods from small drainage areas. The program has expanded from 45 crest-stage gaging stations initially to 172 stations maintained in 1980. Data in the report are tabulated for the period of record. (USGS)","language":"ENGLISH","doi":"10.3133/ofr81332","usgsCitation":"Omang, R.J., Parrett, C., and Hull, J.A., 1955, Annual peak discharges from small drainage areas in Montana through September 1980: U.S. Geological Survey Open-File Report 81-332, 118 p., illus. incl. sketch maps, 1981. 2 over-size sheets, https://doi.org/10.3133/ofr81332.","productDescription":"118 p., illus. incl. sketch maps, 1981. 2 over-size sheets","costCenters":[],"links":[{"id":170576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0332/report-thumb.jpg"},{"id":20121,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0332/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20122,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0332/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":85500,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0332/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db680d39","contributors":{"authors":[{"text":"Omang, R. J.","contributorId":31365,"corporation":false,"usgs":true,"family":"Omang","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":238076,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parrett, Charles","contributorId":9635,"corporation":false,"usgs":true,"family":"Parrett","given":"Charles","email":"","affiliations":[],"preferred":false,"id":238075,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hull, J. A.","contributorId":39345,"corporation":false,"usgs":true,"family":"Hull","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":238077,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4152,"text":"cir363 - 1955 - Coal reserves of the Pittsburgh (No. 8) bed in Belmont County, Ohio","interactions":[],"lastModifiedDate":"2022-01-27T22:30:09.132527","indexId":"cir363","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"363","title":"Coal reserves of the Pittsburgh (No. 8) bed in Belmont County, Ohio","docAbstract":"Remaining coal reserves totaling 1,929 million tons have been appraised in the Pittsburgh (No. 8) coal bed in Belmont County, Ohio. Of these, 508 million tons are classified as measured and 1,421 million tons are classified as indicated. All the coal has less than 1,000 feet of overburden, and most of it is of high volatile A bituminous rank. \r\n\r\nThis estimate is based on field work by the United States Geological Survey, supplemented by data from the fries of the Ohio Geological Survey and from mine and drill-hole records provided by mining companies.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir363","usgsCitation":"Berryhill, H., 1955, Coal reserves of the Pittsburgh (No. 8) bed in Belmont County, Ohio: U.S. Geological Survey Circular 363, iv, 11 p., https://doi.org/10.3133/cir363.","productDescription":"iv, 11 p.","costCenters":[],"links":[{"id":395026,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23702.htm"},{"id":31258,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1955/0363/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122498,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1955/0363/report-thumb.jpg"}],"country":"United States","state":"Ohio","county":"Belmont County","otherGeospatial":"Pittsburgh (No. 8) bed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.224,\n              39.841\n            ],\n            [\n              -80.7,\n              39.841\n            ],\n            [\n              -80.7,\n              40.167\n            ],\n            [\n              -81.224,\n              40.167\n            ],\n            [\n              -81.224,\n              39.841\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ace4b07f02db5c6b05","contributors":{"authors":[{"text":"Berryhill, Henry L.","contributorId":83107,"corporation":false,"usgs":true,"family":"Berryhill","given":"Henry L.","affiliations":[],"preferred":false,"id":148298,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23398,"text":"ofr5571 - 1955 - Quality of water of the Colorado River, 1925-40","interactions":[{"subject":{"id":51134,"text":"ofr5276 - 1952 - Quality of Colorado River water","indexId":"ofr5276","publicationYear":"1952","noYear":false,"title":"Quality of Colorado River water"},"predicate":"SUPERSEDED_BY","object":{"id":23398,"text":"ofr5571 - 1955 - Quality of water of the Colorado River, 1925-40","indexId":"ofr5571","publicationYear":"1955","noYear":false,"title":"Quality of water of the Colorado River, 1925-40"},"id":1}],"lastModifiedDate":"2017-09-07T12:39:44","indexId":"ofr5571","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-71","title":"Quality of water of the Colorado River, 1925-40","docAbstract":"<p>The study of the quality of water of the Colorado River and its tributaries has been a continuing one since 1925. The data so obtained have been useful in the planning and construction of dams and reservoirs, the utilization of the water within the basin, and in planning the economy of areas outside of the basin, partially or wholly dependent on the diversion or importation of water from the Colorado River or its tributaries. Much chemical quality data of the Colorado River and its tributaries collected during the period from 1925 to 1940 have not been published in detail. </p><p>The purpose of this report is to make available for consultation and ready reference those previously unpublished data collected for the period 1925 to 1940, mainly between 1930 and 1940. Included among these data are many detailed chemical analyses of composites of daily samples and single samples of the Colorado River and its main tributaries and less detailed analyses of many other samples. In a few instances, for continuity of the record, analyses are included that have been published in Survey reports. Discussions of the quality of water of the Colorado River basin either in published reports or in mimeograph form are available; therefore, this report will include only tabulated data. </p><p>Data obtained for the period 1925 to 1930 for the most part were published in three Geological Survey Water-Supply Papers, 596-B, 636-A, and 638-D, all out of print. Summary data for the streams in the Colorado River basin for the period 1925 to 1943 were published in U.S. Geological Survey Water-Supply Paper 970, \"Quality of surface waters of the United States, 1943\". These summaries consist mainly of annual weighted averages of chemical analyses, dissolved-solids loads, and extremes of dissolved solids and hardness. Analyses of samples from Lake Mead are available in a series of reports, \"Lake Mead Density Currents Investigations\", by the Bureau of Reclamation /1937 -1940, Vols. I and ll; 1940 -1946; Vol. III/. Data on the suspended sediment in the Colorado River for the period 1925-1941 were published in 1947, in U.S. Geological Survey Water -Supply Paper 998. Since 1940 results of water-quality investigations in the Colorado River basin have been published in the annual U.S. Geological Survey reports, \"Quality of surface waters of the United States\". </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ofr5571","issn":"0094-9140","usgsCitation":"Howard, C.S., 1955, Quality of water of the Colorado River, 1925-40: U.S. Geological Survey Open-File Report 55-71, i, 103 p., https://doi.org/10.3133/ofr5571.","productDescription":"i, 103 p.","numberOfPages":"106","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":113004,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0071/report.pdf","size":"6521","linkFileType":{"id":1,"text":"pdf"}},{"id":156938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1955/0071/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Colorado River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db6516c6","contributors":{"authors":[{"text":"Howard, Charles S.","contributorId":15990,"corporation":false,"usgs":true,"family":"Howard","given":"Charles","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":190040,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23721,"text":"ofr5596 - 1955 - Records of wells, water levels, and quality of ground water in the Sammamish Lake area, King County, Washington","interactions":[],"lastModifiedDate":"2015-10-22T12:48:39","indexId":"ofr5596","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-96","title":"Records of wells, water levels, and quality of ground water in the Sammamish Lake area, King County, Washington","docAbstract":"<p>This report, one of a series on the ground-water resources of the State of Washington, contains well records and other data collected during the course of an investigation in the Sammamish Lake area immediately east of Seattle, King County, Washington. &nbsp;Most of these investigations are conducted in cooperation with the State of Washington, Department of Conservation and Development, Division of Water Resources. &nbsp;However, a few investigations, including the one in the Sammamish Lake area, have been made entirely with Federal funds. &nbsp;A similar investigation is now being made in the area to the west, including the city of Seattle and metropolitan areas to the north and south. &nbsp;It is planned that results of teh two investigations will be combined into a single comprehencive report. &nbsp;In order that the data collected can be made available sooner, this report as been prepared with only a brief explanatory and descriptive text.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5596","issn":"0094-9140","usgsCitation":"Liesch, B.A., 1955, Records of wells, water levels, and quality of ground water in the Sammamish Lake area, King County, Washington: U.S. Geological Survey Open-File Report 55-96, Report: iii, 193 p.; Plate: 10.21 x 7.94 inches, https://doi.org/10.3133/ofr5596.","productDescription":"Report: iii, 193 p.; Plate: 10.21 x 7.94 inches","numberOfPages":"197","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":157237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr5596.jpg"},{"id":310473,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0096/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310474,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1955/0096/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","county":"King County","otherGeospatial":"Sammamish Lake","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-122.4525,47.5039],[-122.4596,47.4967],[-122.4606,47.4867],[-122.4338,47.4665],[-122.4438,47.4533],[-122.44,47.4491],[-122.4397,47.4361],[-122.43,47.4219],[-122.4394,47.4176],[-122.437,47.4072],[-122.4254,47.4018],[-122.3949,47.3992],[-122.3737,47.3883],[-122.3993,47.382],[-122.4365,47.3664],[-122.4433,47.3618],[-122.4541,47.344],[-122.4643,47.3436],[-122.4767,47.3518],[-122.4728,47.3619],[-122.4636,47.3742],[-122.4544,47.3706],[-122.4318,47.3888],[-122.4376,47.3933],[-122.439,47.4058],[-122.4619,47.4011],[-122.4667,47.3925],[-122.4619,47.3908],[-122.4524,47.395],[-122.4478,47.3874],[-122.4517,47.3839],[-122.4725,47.3872],[-122.4844,47.3803],[-122.4913,47.3325],[-122.5041,47.3309],[-122.5203,47.3345],[-122.527,47.3427],[-122.5279,47.3509],[-122.5152,47.3779],[-122.5275,47.3972],[-122.512,47.4219],[-122.5132,47.4529],[-122.4957,47.4767],[-122.4814,47.4827],[-122.4754,47.5108],[-122.4525,47.5039]]],[[[-121.1216,47.782],[-121.1059,47.7646],[-121.0904,47.7587],[-121.0923,47.7494],[-121.0788,47.738],[-121.0867,47.7246],[-121.0706,47.7178],[-121.0664,47.7086],[-121.0711,47.7049],[-121.0892,47.7039],[-121.0905,47.6933],[-121.1026,47.6919],[-121.124,47.6816],[-121.1266,47.6738],[-121.1224,47.6609],[-121.1331,47.6503],[-121.1242,47.6297],[-121.1154,47.6228],[-121.1153,47.6177],[-121.122,47.6108],[-121.1105,47.6017],[-121.1111,47.5961],[-121.1553,47.5936],[-121.1733,47.5811],[-121.1673,47.5775],[-121.1799,47.5655],[-121.2268,47.5634],[-121.2334,47.5564],[-121.2333,47.5436],[-121.2446,47.5329],[-121.2572,47.5241],[-121.2746,47.5249],[-121.2886,47.5152],[-121.2885,47.5065],[-121.2964,47.5005],[-121.2983,47.488],[-121.365,47.4637],[-121.3848,47.4457],[-121.384,47.4328],[-121.3947,47.4332],[-121.4038,47.4193],[-121.4253,47.4196],[-121.4204,47.4086],[-121.4343,47.3998],[-121.4268,47.3861],[-121.4409,47.3869],[-121.4433,47.3736],[-121.4594,47.3757],[-121.4653,47.3665],[-121.4597,47.3527],[-121.4355,47.3414],[-121.4307,47.3281],[-121.4444,47.3092],[-121.4337,47.306],[-121.4302,47.2928],[-121.422,47.2859],[-121.378,47.2862],[-121.3653,47.2904],[-121.3405,47.2823],[-121.3308,47.2552],[-121.3387,47.2469],[-121.3547,47.2413],[-121.3645,47.2238],[-121.3383,47.2162],[-121.3197,47.2153],[-121.3027,47.1966],[-121.3138,47.1704],[-121.2969,47.1521],[-121.2968,47.1429],[-121.306,47.1364],[-121.334,47.1339],[-121.3654,47.1425],[-121.3893,47.135],[-121.3918,47.1276],[-121.4011,47.123],[-121.405,47.1124],[-121.3962,47.1055],[-121.4035,47.1009],[-121.4001,47.0959],[-121.3801,47.0928],[-121.374,47.0869],[-121.3812,47.0813],[-121.4047,47.0931],[-121.4432,47.0855],[-121.4869,47.1146],[-121.5237,47.1249],[-121.5782,47.1185],[-121.5869,47.1207],[-121.6146,47.1444],[-121.6321,47.153],[-121.6621,47.1559],[-121.6774,47.1503],[-121.7194,47.1513],[-121.7436,47.1626],[-121.7549,47.1615],[-121.7751,47.1719],[-121.7911,47.174],[-121.8109,47.1624],[-121.8121,47.1578],[-121.8307,47.1525],[-121.8352,47.1461],[-121.8412,47.1446],[-121.8974,47.1565],[-121.9259,47.1465],[-121.9304,47.1405],[-121.9458,47.1418],[-121.9498,47.1449],[-121.9501,47.1546],[-121.9849,47.1629],[-121.9944,47.1706],[-122.0004,47.1687],[-122.0152,47.1764],[-122.0518,47.1718],[-122.0661,47.1864],[-122.0964,47.1971],[-122.1162,47.217],[-122.1123,47.2208],[-122.1191,47.2248],[-122.1241,47.2385],[-122.1349,47.2435],[-122.1378,47.254],[-122.1446,47.2576],[-122.3309,47.258],[-122.3337,47.2635],[-122.416,47.3198],[-122.3937,47.3278],[-122.3805,47.3265],[-122.3707,47.3346],[-122.3374,47.3414],[-122.324,47.3523],[-122.3259,47.3928],[-122.3303,47.4025],[-122.3491,47.4176],[-122.3544,47.4411],[-122.3818,47.4503],[-122.3682,47.4592],[-122.3698,47.4688],[-122.3617,47.4852],[-122.3877,47.5033],[-122.3979,47.5161],[-122.3942,47.5246],[-122.4006,47.5295],[-122.3961,47.5359],[-122.3998,47.5541],[-122.4104,47.5693],[-122.4199,47.575],[-122.386,47.5953],[-122.3713,47.5843],[-122.3633,47.585],[-122.3592,47.5744],[-122.3575,47.5897],[-122.3478,47.5903],[-122.3461,47.5747],[-122.3433,47.5744],[-122.3431,47.5931],[-122.3374,47.5999],[-122.3417,47.6066],[-122.3781,47.6266],[-122.3782,47.6316],[-122.3792,47.6273],[-122.3814,47.6331],[-122.3828,47.6258],[-122.3839,47.6308],[-122.3958,47.6308],[-122.4111,47.6377],[-122.4171,47.6424],[-122.4205,47.6525],[-122.4339,47.6608],[-122.4092,47.6714],[-122.4039,47.6653],[-122.3675,47.6553],[-122.388,47.6651],[-122.4019,47.6664],[-122.4105,47.676],[-122.4037,47.6899],[-122.4057,47.6944],[-122.3824,47.7071],[-122.3736,47.7278],[-122.3824,47.747],[-122.3806,47.7592],[-122.3937,47.7709],[-122.3952,47.7778],[-121.972,47.776],[-121.1216,47.782]]]]},\"properties\":{\"name\":\"King\",\"state\":\"WA\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a60e4b07f02db6354e8","contributors":{"authors":[{"text":"Liesch, Bruce A.","contributorId":71208,"corporation":false,"usgs":true,"family":"Liesch","given":"Bruce","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":190603,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51839,"text":"ofr5586 - 1955 - Open-file Appendix: Tables on basic data on geology and ground water of the Inyokern Naval Ordinance Test Station and vicinity, California","interactions":[],"lastModifiedDate":"2013-08-19T14:39:50","indexId":"ofr5586","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-86","title":"Open-file Appendix: Tables on basic data on geology and ground water of the Inyokern Naval Ordinance Test Station and vicinity, California","language":"ENGLISH","doi":"10.3133/ofr5586","usgsCitation":"Kunkel, F., Chase, G., and Hiltgen, W., 1955, Open-file Appendix: Tables on basic data on geology and ground water of the Inyokern Naval Ordinance Test Station and vicinity, California: U.S. Geological Survey Open-File Report 55-86, 115 p., 1 plate, https://doi.org/10.3133/ofr5586.","productDescription":"115 p., 1 plate","costCenters":[],"links":[{"id":178704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af1e4b07f02db691865","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":244371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chase, G.H.","contributorId":68391,"corporation":false,"usgs":true,"family":"Chase","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":244372,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hiltgen, W.J.","contributorId":8929,"corporation":false,"usgs":true,"family":"Hiltgen","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":244370,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2784,"text":"wsp1295 - 1955 - Chemical quality of surface waters in Devils Lake basin, North Dakota","interactions":[],"lastModifiedDate":"2018-03-16T13:46:22","indexId":"wsp1295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1295","title":"Chemical quality of surface waters in Devils Lake basin, North Dakota","docAbstract":"Devils Lake basin, a closed basin in northeastern North Dakota, covers about 3,900 square miles of land, the topography of which is morainal and of glacial origin. In this basin lies a chain of waterways, which begins with the Sweetwater group and extends successively through Mauvais Coulee, Devils Lake, East Bay Devils Lake, and East Devils Lake, to Stump Lake. In former years when lake levels were high, Mauvais Coulee drained the Sweetwater group and discharged considerable water into Devils Lake. Converging coulees also transported excess water to Stump Lake. For at least 70 years prior to 1941, Mauvais Coulee flowed only intermittently, and the levels of major lakes in this region gradually declined. Devils Lake, for example, covered an area of about 90,000 acres in 1867 but had shrunk to approximately 6,500 acres by 1941. Plans to restore the recreational appeal of Devils Lake propose the dilution and eventual displacement of the brackish lake water by fresh water that would be diverted from the Missouri River. Freshening of the lake water would permit restocking Devils Lake with fish. \r\n\r\nDevils and Stump Lake have irregular outlines and numerous windings and have been described as lying in the valley of a preglacial river, the main stem and tributaries of which are partly filled with drift. Prominent morainal hills along the south shore of Devils Lake contrast sharply with level farmland to the north. The mean annual temperature of Devils Lake basin ranges between 36 ? and 42 ? F. Summer temperatures above 100 ? F and winter temperatures below -30 ? Fare not uncommon. The annual precipitation for 77 years at the city of Devils Lake averaged 17.5 inches. Usually, from 75 to 80 percent of the precipitation in the basin falls during the growing season, April to September. \r\n\r\nFrom 1867 to 1941 the net fall of the water surface of Devils Lake was about 38 feet. By 1951 the surface had risen fully 14 feet from its lowest altitude, 1,400.9 feet. Since 1951, the level has fallen slowly. Hydrologic changes that may have caused Devils Lake to alter from a very large, moderately deep lake of fresh water to a small, shallow body of brackish water are discussed and evaluated on the basis of scanty information. During several years of average precipitation, temperature, and evaporation, Devils Lake and lakes upstream should receive nearly a quarter of an inch of runoff annually from the drainage area of about 3,000 square miles. Approximately 55 square miles of tributary area would be required to maintain each square mile of lake surface. However, runoff, expressed as percentage of the average, differs greatly from year to year. The amount of runoff retained in upstream lakes also Varies greatly. For these two reasons, annual inflow to Devils Lake is extremely variable. \r\n\r\nBecause many waterways in this basin have no surface outlets at normal stages, runoff collects in depressions, is concentrated by evaporation, and forms saline or alkaline lakes. The chemical and physical properties of the lake waters vary chiefly with changes in lake stage and volume of inflow. Scattered records from 1899 to 1923 and more comprehensive data from 1948 to 1952 show a range of salt concentration from 6,130 to 25,000 parts per million (ppm) in the water of Devils Lake. Although concentration has varied, the chemical composition of the dissolved solids has not changed appreciably. Lake waters are more concentrated in the lower part of the basin, downstream from Devils Lake. For periods of record the salt concentration ranged from 14,932 to 62,000 ppm in East Devils Lake and from 19,000 to 106,000 ppm in east Stump Lake. \r\n\r\nCurrent and past tonnages of dissolved solids in Devils Lake, East Bay Devils Lake, East Devils Lake, and east and west Stump Lakes were computed from concentrations and from altitude-capacity curves for each lake. Neither the average rate of diversion of water to restore Devils Lake to a higher level nor the quality of the divert","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1295","usgsCitation":"Swenson, H., and Colby, B.R., 1955, Chemical quality of surface waters in Devils Lake basin, North Dakota: U.S. Geological Survey Water Supply Paper 1295, Report: v, 81 p.; Plate: 17.5 x 17.1 inches, https://doi.org/10.3133/wsp1295.","productDescription":"Report: v, 81 p.; Plate: 17.5 x 17.1 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":29259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1295/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1295/report-thumb.jpg"},{"id":29258,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1295/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e332f","contributors":{"authors":[{"text":"Swenson, Herbert","contributorId":54181,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","affiliations":[],"preferred":false,"id":145781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colby, Bruce R.","contributorId":59775,"corporation":false,"usgs":true,"family":"Colby","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145782,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24455,"text":"ofr55160 - 1955 - Records of wells and springs, water levels, and quality of ground water in central Pierce County, Washington","interactions":[],"lastModifiedDate":"2015-10-21T09:46:39","indexId":"ofr55160","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"55-160","title":"Records of wells and springs, water levels, and quality of ground water in central Pierce County, Washington","docAbstract":"<p>Location and Extent of Area</p>\n<p>The area covered by this report (fig. 1) includes the part of Pierce County, ~ash. that lies west of the foothills of the Cascade Mountains and east of the main waterway of Puget Sound, and extends from the county line on the north to the Nisqually River on the south.</p>\n<p>Purpose and Scope of Report</p>\n<p>This report presents basic information pertaining to the ground-water resources of the central Pierce County area which has been obtained by the United States Geological Survey since the beginning of the cooperative groundwater investigation in 1937. The data have been tabulated and prepared for release at this time so that they may be used by those concerned with the development and use of ground-water supplies in the area. A comprehensive report analyzing and interpreting the basic data is being prepared and will be released in the future.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr55160","collaboration":"Prepared in cooperation with the State of Washington Department of Conservation and Development Division of Water Resources","usgsCitation":"Sceva, J.E., and Wegner, D.E., 1955, Records of wells and springs, water levels, and quality of ground water in central Pierce County, Washington: U.S. Geological Survey Open-File Report 55-160, Report: iv, 261 p.; Plate: 8.7 x 8.0 inches, https://doi.org/10.3133/ofr55160.","productDescription":"Report: iv, 261 p.; Plate: 8.7 x 8.0 inches","numberOfPages":"264","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":157203,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/OFR55160.jpg"},{"id":310227,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1955/0160/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":310228,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1955/0160/plate-1.pdf","text":"Plate","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","county":"Pierce 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