{"pageNumber":"2653","pageRowStart":"66300","pageSize":"25","recordCount":68824,"records":[{"id":3735,"text":"cir292 - 1953 - Water-power resources of Crystal River, Colorado","interactions":[],"lastModifiedDate":"2017-05-19T18:24:59","indexId":"cir292","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"292","title":"Water-power resources of Crystal River, Colorado","docAbstract":"The Crystal River drains the western slope of the Elk Mountains, a relatively small range in the southern Rocky Mountain province, and flows into the Roaring Fork 13 miles southeast of Glenwood Springs, Colo. The lower 7 miles of the valley is cultivated, but upstream from this stretch the valley is narrow and is used mainly for summer grazing and recreation. Above the mouth of Thompson Creek, numerous dam sites are available, but the narrow valley and steep gradient do not favor storage for regulation of streamflow. The potential power from the natural flow of the stream in an average year is estimated to be 4,750 kilowatts for 95 percent of the time; 5,102 kw for 90 percent of the time; 10,570 kw for 50 percent of the time; and 36,940 kw at mean flow. Using the regulated flow resulting from the utilization of reservoirs at Marble and Redstone, the potential power is estimated to be 26,510 kw for 90 percent of the time and 27,810 kw for 50 percent of the time.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir292","usgsCitation":"Lawrence, F.F., 1953, Water-power resources of Crystal River, Colorado: U.S. Geological Survey Circular 292, 17 p. :ill., col. map ;27 cm., https://doi.org/10.3133/cir292.","productDescription":"17 p. :ill., col. map ;27 cm.","costCenters":[],"links":[{"id":30796,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1953/0292/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1953/0292/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e734a","contributors":{"authors":[{"text":"Lawrence, Fred Forrest","contributorId":93034,"corporation":false,"usgs":true,"family":"Lawrence","given":"Fred","email":"","middleInitial":"Forrest","affiliations":[],"preferred":false,"id":147505,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3224,"text":"cir200 - 1953 - Annotated bibliography of U.S. Geological Survey reports on water-power resources, including floods and droughts","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"200","title":"Annotated bibliography of U.S. Geological Survey reports on water-power resources, including floods and droughts","language":"ENGLISH","publisher":"[U.S. Geological Survey],","doi":"10.3133/cir200","usgsCitation":"Young, L.L., and Jones, B.E., 1953, Annotated bibliography of U.S. Geological Survey reports on water-power resources, including floods and droughts: U.S. Geological Survey Circular 200, 32 p. ;27 cm., https://doi.org/10.3133/cir200.","productDescription":"32 p. ;27 cm.","costCenters":[],"links":[{"id":117324,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1953/0200/report-thumb.jpg"},{"id":30217,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1953/0200/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf9f","contributors":{"authors":[{"text":"Young, Loyd L.","contributorId":14805,"corporation":false,"usgs":true,"family":"Young","given":"Loyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Benjamin Earl","contributorId":69961,"corporation":false,"usgs":true,"family":"Jones","given":"Benjamin","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":146467,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":16436,"text":"ofr53278 - 1953 - Additional Field Methods Used in Geochemical Prospecting by the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:07:09","indexId":"ofr53278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-278","title":"Additional Field Methods Used in Geochemical Prospecting by the U.S. Geological Survey","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr53278","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Additional Field Methods Used in Geochemical Prospecting by the U.S. Geological Survey: U.S. Geological Survey Open-File Report 53-278, 42 p., https://doi.org/10.3133/ofr53278.","productDescription":"42 p.","costCenters":[],"links":[{"id":148330,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1953/0278/report-thumb.jpg"},{"id":45415,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1953/0278/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699be0","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":22829,"text":"ofr5350 - 1953 - Memorandum on ground-water irrigation in Mitchell County, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"ofr5350","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1953","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":"53-50","title":"Memorandum on ground-water irrigation in Mitchell County, Texas","language":"ENGLISH","publisher":"Texas Board of Water Engineers,","doi":"10.3133/ofr5350","issn":"0094-9140","usgsCitation":"Dale, O.C., and Broadhurst, W.L., 1953, Memorandum on ground-water irrigation in Mitchell County, Texas: U.S. Geological Survey Open-File Report 53-50, 21 p, https://doi.org/10.3133/ofr5350.","productDescription":"21 p","costCenters":[],"links":[{"id":156946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ce4b07f02db613dcf","contributors":{"authors":[{"text":"Dale, Oscar C.","contributorId":46124,"corporation":false,"usgs":true,"family":"Dale","given":"Oscar","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":188952,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broadhurst, William Leslie","contributorId":95513,"corporation":false,"usgs":true,"family":"Broadhurst","given":"William","email":"","middleInitial":"Leslie","affiliations":[],"preferred":false,"id":188953,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70207421,"text":"70207421 - 1953 - Iron deposits of the congonhas district, minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2019-12-19T09:49:30","indexId":"70207421","displayToPublicDate":"1953-12-01T09:47:16","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Iron deposits of the congonhas district, minas Gerais, Brazil","docAbstract":"

Various origins have been proposed for the itabirite and associated hematite ores of Minas Gerais, Brazil. The U.S. Geological Survey, in cooperation with the Brazilian Departamento Nacional da Produqao Mineral, has undertaken a comprehensive program of mapping of these Precambrian deposits, which bear many similarities to other Precambrian iron formations. Itabirite is a finely laminated quartz-iron oxide rock with more or less dolomite, corresponding to James's oxide facies. It occurs principally in the middle group of the Minas series-a eugeosynclinal assemblage of quartzite, schist, chemical precipitates, graywacke, and volcanic rocks. Iron and silica were precipitated rhythmically in a shallow restricted basin under somewhat acid conditions that inhibited the precipitation of carbonates. Erosion of moderately deformed rocks of the Minas series furnished sediments for the overlying conglomeratic Itacolumi series. Severe post-Itacolumi deformation folded and thrust-faulted rocks of both series; the accompanying regional metamorphism recrystallized the chert and iron oxide to quartz, specular hematite, and minor amounts of magnetite. Ultramafic intrusions antedate this diastrophism; granodiorites and various basic dike rocks are younger. Hydrothermal replacement of breccia zones in itabirite and of dolomitic beds associated with the iron formation produced high-grade specular hematite ore nearly free of impurities. The areal distribution of the deposits indicates that the solutions followed fault zones. Heated meteoric water may have been responsible for the replacement, as minerals of obvious magmatic origin are absent. Since early Tertiary time the area has been uplifted several thousand feet. Leaching and cementation related to the present surface have modified both the iron formation and the hematite deposits, giving rise to various types of commercial ore. © 1953 Society of Economic Geologists, Inc.

","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.48.8.639","issn":"03610128","usgsCitation":"Guild, P.W., 1953, Iron deposits of the congonhas district, minas Gerais, Brazil: Economic Geology, v. 48, no. 8, p. 639-676, https://doi.org/10.2113/gsecongeo.48.8.639.","productDescription":"38 p. ","startPage":"639","endPage":"676","costCenters":[],"links":[{"id":370466,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil ","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-57.62513,-30.21629],[-56.2909,-28.85276],[-55.16229,-27.88192],[-54.49073,-27.47476],[-53.64874,-26.92347],[-53.62835,-26.12487],[-54.13005,-25.54764],[-54.62529,-25.73926],[-54.42895,-25.16218],[-54.29348,-24.5708],[-54.29296,-24.02101],[-54.65283,-23.83958],[-55.0279,-24.00127],[-55.40075,-23.95694],[-55.51764,-23.572],[-55.61068,-22.65562],[-55.79796,-22.35693],[-56.47332,-22.0863],[-56.88151,-22.28215],[-57.93716,-22.09018],[-57.87067,-20.73269],[-58.16639,-20.1767],[-57.8538,-19.97],[-57.95,-19.4],[-57.67601,-18.96184],[-57.49837,-18.17419],[-57.73456,-17.55247],[-58.2808,-17.27171],[-58.38806,-16.87711],[-58.24122,-16.29957],[-60.15839,-16.25828],[-60.54297,-15.09391],[-60.25115,-15.07722],[-60.26433,-14.64598],[-60.4592,-14.35401],[-60.5033,-13.77595],[-61.08412,-13.47938],[-61.7132,-13.4892],[-62.12708,-13.19878],[-62.80306,-13.00065],[-63.1965,-12.62703],[-64.31635,-12.46198],[-65.40228,-11.56627],[-65.3219,-10.89587],[-65.44484,-10.51145],[-65.33844,-9.76199],[-66.64691,-9.93133],[-67.1738,-10.30681],[-68.04819,-10.71206],[-68.27125,-11.01452],[-68.78616,-11.03638],[-69.52968,-10.95173],[-70.09375,-11.12397],[-70.54869,-11.00915],[-70.48189,-9.49012],[-71.30241,-10.07944],[-72.18489,-10.0536],[-72.56303,-9.52019],[-73.22671,-9.46221],[-73.01538,-9.03283],[-73.57106,-8.42445],[-73.98724,-7.52383],[-73.7234,-7.341],[-73.72449,-6.9186],[-73.12003,-6.62993],[-73.21971,-6.08919],[-72.96451,-5.74125],[-72.89193,-5.27456],[-71.74841,-4.59398],[-70.92884,-4.40159],[-70.79477,-4.25126],[-69.89364,-4.29819],[-69.4441,-1.55629],[-69.42049,-1.12262],[-69.57707,-0.54999],[-70.02066,-0.18516],[-70.01557,0.54141],[-69.4524,0.70616],[-69.25243,0.60265],[-69.21864,0.98568],[-69.8046,1.08908],[-69.81697,1.71481],[-67.86857,1.69246],[-67.53781,2.03716],[-67.26,1.72],[-67.06505,1.13011],[-66.87633,1.25336],[-66.32577,0.72445],[-65.54827,0.78925],[-65.35471,1.09528],[-64.61101,1.32873],[-64.19931,1.49285],[-64.08309,1.91637],[-63.36879,2.2009],[-63.42287,2.41107],[-64.27,2.49701],[-64.40883,3.12679],[-64.36849,3.79721],[-64.81606,4.05645],[-64.62866,4.14848],[-63.88834,4.02053],[-63.0932,3.77057],[-62.80453,4.00697],[-62.08543,4.16212],[-60.96689,4.53647],[-60.60118,4.9181],[-60.73357,5.20028],[-60.21368,5.24449],[-59.98096,5.01406],[-60.111,4.57497],[-59.76741,4.4235],[-59.53804,3.9588],[-59.81541,3.6065],[-59.97452,2.75523],[-59.71855,2.24963],[-59.64604,1.78689],[-59.03086,1.3177],[-58.54001,1.26809],[-58.42948,1.46394],[-58.11345,1.5072],[-57.66097,1.68258],[-57.33582,1.94854],[-56.7827,1.86371],[-56.53939,1.89952],[-55.9957,1.81767],[-55.9056,2.022],[-56.07334,2.22079],[-55.97332,2.51036],[-55.56976,2.42151],[-55.09759,2.52375],[-54.52475,2.31185],[-54.08806,2.10556],[-53.77852,2.3767],[-53.55484,2.3349],[-53.41847,2.05339],[-52.93966,2.12486],[-52.55642,2.50471],[-52.24934,3.24109],[-51.6578,4.15623],[-51.31715,4.20349],[-51.06977,3.6504],[-50.50888,1.90156],[-49.97408,1.73648],[-49.9471,1.04619],[-50.69925,0.22298],[-50.38821,-0.07844],[-48.62057,-0.23549],[-48.5845,-1.23781],[-47.82496,-0.58162],[-46.56658,-0.94103],[-44.9057,-1.55174],[-44.41762,-2.13775],[-44.58159,-2.69131],[-43.41879,-2.38311],[-41.47266,-2.91202],[-39.97867,-2.87305],[-38.50038,-3.70065],[-37.22325,-4.82095],[-36.45294,-5.1094],[-35.5978,-5.1495],[-35.23539,-5.46494],[-34.89603,-6.73819],[-34.72999,-7.34322],[-35.12821,-8.9964],[-35.63697,-9.64928],[-37.04652,-11.04072],[-37.68361,-12.17119],[-38.42388,-13.03812],[-38.67389,-13.05765],[-38.95328,-13.79337],[-38.8823,-15.66705],[-39.16109,-17.20841],[-39.26734,-17.86775],[-39.58352,-18.2623],[-39.76082,-19.59911],[-40.77474,-20.90451],[-40.94476,-21.93732],[-41.75416,-22.37068],[-41.98828,-22.97007],[-43.0747,-22.96769],[-44.64781,-23.35196],[-45.35214,-23.79684],[-46.47209,-24.08897],[-47.64897,-24.8852],[-48.49546,-25.87702],[-48.641,-26.6237],[-48.47474,-27.17591],[-48.66152,-28.18613],[-48.88846,-28.67412],[-49.58733,-29.22447],[-50.69687,-30.98447],[-51.57623,-31.7777],[-52.25608,-32.24537],[-52.7121,-33.19658],[-53.37366,-33.76838],[-53.65054,-33.202],[-53.20959,-32.72767],[-53.78795,-32.04724],[-54.57245,-31.49451],[-55.60151,-30.85388],[-55.97324,-30.88308],[-56.97603,-30.10969],[-57.62513,-30.21629]]]},\"properties\":{\"name\":\"Brazil\"}}]}","volume":"48","issue":"8","noUsgsAuthors":false,"publicationDate":"1953-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Guild, P. W.","contributorId":39039,"corporation":false,"usgs":true,"family":"Guild","given":"P.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":777952,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70217838,"text":"70217838 - 1953 - Discussion of “the efficiency of depth‐integrating suspended‐sediment sampling”","interactions":[],"lastModifiedDate":"2021-02-05T18:09:08.018871","indexId":"70217838","displayToPublicDate":"1953-10-31T12:04:21","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Discussion of “the efficiency of depth‐integrating suspended‐sediment sampling”","docAbstract":"

The author has developed equations and approximate curves to express the percentage of the total sediment discharge that is carried in suspension above the lowest point reached by the nozzle of a depth‐integrating sediment sampler. He assumes that bed load and suspended load are defined by the equations in a paper by H. A. Einstein [The bed‐load function for sediment transportation in open‐channel flows, U.S. Dept. Agric., Tech. Bull. 1026, 1950]. The percentage is termed the efficiency of sampling.

In a vertical strip of unit width, the suspended‐sediment discharge discussed by the author' in effect the product of the mean concentration of the depth‐integrated sample, the water discharge in that portion of the depth above the lowest nozzle position, and a factor for converting the result into desired units, such as tons per day. In contrast, the common operating practice is to compute the suspended‐sediment load as the product of the measured concentration, the total water discharge, and the conversion factor. The difference in computed suspended‐sediment discharge by the two methods is sometimes appreciable as, for example, in the wide, shallow streams that drain the sandhills of Nebraska.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR034i005p00796","usgsCitation":"Kreiss, R.F., Colby, B.R., and Chien, N., 1953, Discussion of “the efficiency of depth‐integrating suspended‐sediment sampling”: Eos, Transactions, American Geophysical Union, p. 796-797, https://doi.org/10.1029/TR034i005p00796.","productDescription":"2 p.","startPage":"796","endPage":"797","costCenters":[],"links":[{"id":383055,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Kreiss, R. F.","contributorId":248792,"corporation":false,"usgs":false,"family":"Kreiss","given":"R.","email":"","middleInitial":"F.","affiliations":[{"id":6605,"text":"USGS","active":true,"usgs":false}],"preferred":false,"id":809872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colby, B. R.","contributorId":59776,"corporation":false,"usgs":true,"family":"Colby","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":809873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chien, Ning","contributorId":248793,"corporation":false,"usgs":false,"family":"Chien","given":"Ning","email":"","affiliations":[],"preferred":false,"id":809874,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221520,"text":"70221520 - 1953 - The influence of ground‐water storage on the runoff in the San Bernardino and eastern San Gabriel Mountains of Southern California","interactions":[],"lastModifiedDate":"2021-06-21T17:20:02.129427","indexId":"70221520","displayToPublicDate":"1953-08-01T12:14:16","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The influence of ground‐water storage on the runoff in the San Bernardino and eastern San Gabriel Mountains of Southern California","docAbstract":"

The steep and rugged mountains of Southern California contain considerable ground‐water storage. A large portion of the runoff is seepage from this storage The variations in runoff distribution depend on the geology, physiography, and soil cover of these mountain areas.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR034i004p00552","usgsCitation":"Troxell, H., 1953, The influence of ground‐water storage on the runoff in the San Bernardino and eastern San Gabriel Mountains of Southern California: Eos, Transactions, American Geophysical Union, v. 34, no. 4, p. 552-562, https://doi.org/10.1029/TR034i004p00552.","productDescription":"11 p.","startPage":"552","endPage":"562","costCenters":[],"links":[{"id":386615,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"San Gabriel Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.8173828125,\n 32.55144352864431\n ],\n [\n -115.48828124999999,\n 32.55144352864431\n ],\n [\n -115.48828124999999,\n 33.87953701355924\n ],\n [\n -116.6748046875,\n 34.15272698011818\n ],\n [\n -117.8173828125,\n 33.87953701355924\n ],\n [\n -117.8173828125,\n 32.55144352864431\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"34","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Troxell, Harold C.","contributorId":243566,"corporation":false,"usgs":false,"family":"Troxell","given":"Harold C.","affiliations":[],"preferred":false,"id":817923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221518,"text":"70221518 - 1953 - Volumes And weights of pyroclastic material, lava, and water erupted by Paricutin volcano, Michoacan, Mexico","interactions":[],"lastModifiedDate":"2021-06-21T17:03:58.256912","indexId":"70221518","displayToPublicDate":"1953-08-01T11:56:36","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Volumes And weights of pyroclastic material, lava, and water erupted by Paricutin volcano, Michoacan, Mexico","docAbstract":"

Estimates of the weights of pyroclastic material and lava erupted by Parícutin Volcano from early 1943 to early 1952 have given a pyroclastic weight of some 2230 million metric tons and a lava weight of about 1330 million metric tons, making a total of 3560 million metric tons of solids. The weight of pyroclastic material ranged from a maximum daily average of more than 10 million metric tons in the first two weeks of eruption to a minimum of some 65,000 metric tons in 1951. The weight of lava ranged from a maximum daily average of about 650,000 metric tons in 1943 to a minimum of some 170,000 metric tons in the second half of 1950.

The only period for which an estimate of the average daily weight of water vapor expelled by the Volcano could be made was the spring of 1945, when some 13,000 metric tons of water were expelled through the crater daily, besides some 500 metric tons contained in the lava extruded concurrently. Since the weight of pyroclastic material and lava erupted by Parícutin in the spring and summer of 1945 is estimated to have averaged about 1.2 million metric tons a day, the water expelled at that time amounted to about 1.1 pct of the total weight of material erupted. If the proportion of water had been nearly constant throughout the active life of the Volcano, the total weight of water would have amounted to some 39 million metric tons.

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR034i004p00603","usgsCitation":"Fries, C., 1953, Volumes And weights of pyroclastic material, lava, and water erupted by Paricutin volcano, Michoacan, Mexico: Eos, Transactions, American Geophysical Union, v. 34, no. 4, p. 603-616, https://doi.org/10.1029/TR034i004p00603.","productDescription":"14 p.","startPage":"603","endPage":"616","costCenters":[],"links":[{"id":386613,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","state":"Michoacan","otherGeospatial":"Paricutin volcano","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102.41180419921875,\n 19.687849316424483\n ],\n [\n -102.25250244140624,\n 19.687849316424483\n ],\n [\n -102.25250244140624,\n 19.830017252151734\n ],\n [\n -102.41180419921875,\n 19.830017252151734\n ],\n [\n -102.41180419921875,\n 19.687849316424483\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"34","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Fries, Carl Jr.","contributorId":86396,"corporation":false,"usgs":true,"family":"Fries","given":"Carl","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":817920,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221519,"text":"70221519 - 1953 - Pumping from wells on the floor of the Sevier Desert, Utah","interactions":[],"lastModifiedDate":"2021-06-21T17:12:34.015216","indexId":"70221519","displayToPublicDate":"1953-02-01T12:05:46","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Pumping from wells on the floor of the Sevier Desert, Utah","docAbstract":"

Data collected at the Topaz Relocation Center provide an excellent record of the development and subsequent disappearance of a cone of depression caused by pumping. This Center occupied temporarily an area of natural ground‐water discharge on the floor of the Sevier Desert in west‐central Utah. Water for a population of 6500 was pumped from artesian wells which tapped aquifers of sand. Overlying these sand beds are lake‐bed sediments too impermeable to yield water to wells, but apparently permeable enough to permit slow upward movement of water from the artesian aquifers. The water table is near the surface, and there is natural discharge by evapotranspiration, accumulation of “alkali” in the soil, and a need for drainage of irrigated lands. The wells were abandoned when the Relocation Center was closed, apparently because these handicaps were so great that the ground water could not be used profitably for irrigation. 

","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR034i001p00074","usgsCitation":"Nelson, W., and Thomas, H., 1953, Pumping from wells on the floor of the Sevier Desert, Utah: Eos, Transactions, American Geophysical Union, v. 34, no. 1, p. 74-84, https://doi.org/10.1029/TR034i001p00074.","productDescription":"11 p.","startPage":"74","endPage":"84","costCenters":[],"links":[{"id":386614,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Sevier Desert","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.0380859375,\n 37.79676317682161\n ],\n [\n -112.1044921875,\n 37.79676317682161\n ],\n [\n -112.1044921875,\n 40.463666324587685\n ],\n [\n -114.0380859375,\n 40.463666324587685\n ],\n [\n -114.0380859375,\n 37.79676317682161\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"34","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Nelson, W.B.","contributorId":30282,"corporation":false,"usgs":true,"family":"Nelson","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":817921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, H.E.","contributorId":243568,"corporation":false,"usgs":false,"family":"Thomas","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":817922,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70265922,"text":"70265922 - 1953 - Reconnaissance of the Missouri River pumping units between Garrison Dam and Bismarck, North Dakota","interactions":[],"lastModifiedDate":"2025-04-21T17:58:53.451703","indexId":"70265922","displayToPublicDate":"1953-01-01T13:48:46","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Reconnaissance of the Missouri River pumping units between Garrison Dam and Bismarck, North Dakota","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70265922","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Reconnaissance of the Missouri River pumping units between Garrison Dam and Bismarck, North Dakota, https://doi.org/10.3133/70265922.","costCenters":[],"links":[{"id":484787,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":933998,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70228616,"text":"70228616 - 1953 - High Plains, or Llano Estacado, Texas-New Mexico","interactions":[],"lastModifiedDate":"2022-02-14T18:29:00.632682","indexId":"70228616","displayToPublicDate":"1953-01-01T13:28:43","publicationYear":"1953","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"High Plains, or Llano Estacado, Texas-New Mexico","docAbstract":"

No abstract available.

","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The physical and economic foundation of natural resources; Volume 4: Subsurface facilities of water management and patterns of supply, type area studies","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Interior and Insular Affairs Committee, House of Representatives, United States Congress","usgsCitation":"Gaum, C.H., 1953, High Plains, or Llano Estacado, Texas-New Mexico, chap. of The physical and economic foundation of natural resources; Volume 4: Subsurface facilities of water management and patterns of supply, type area studies, p. 94-104.","productDescription":"11 p.","startPage":"94","endPage":"104","costCenters":[],"links":[{"id":395905,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico, Texas","otherGeospatial":"Llano Estacado","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gaum, Carl H.","contributorId":278598,"corporation":false,"usgs":true,"family":"Gaum","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":834834,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70095722,"text":"tei197 - 1953 - Reconnaissance for radioactive deposits in the Fairbanks and Livengood Quadrangles, east-central Alaska, 1949","interactions":[],"lastModifiedDate":"2014-06-05T13:59:24","indexId":"tei197","displayToPublicDate":"1953-01-01T11:35:00","publicationYear":"1953","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":"197","title":"Reconnaissance for radioactive deposits in the Fairbanks and Livengood Quadrangles, east-central Alaska, 1949","docAbstract":"

Several mines and prospects in the Fairbanks and Livengood quadrangles, east-central Alaska, were examined for the possible presence of radioactive materials in the summer of 1949. Also tested were pre-Cambrian and Paleozoic metamorphic and sedimentary rocks crossed by the Elliott Highway, which extends from Fox, near Fairbanks, northward about 70 miles to the town of Livengood. None of the lodes tested exhibited radioactivity in excess of 0.003 percent equivalent uranium, although nuggets consisting chiefly of native bismuth and containing as much as 0.1 percent equivalent uranium had been found previously in a placer on Fish Creek several miles below the reported bismuth-bearing lode on Melba Creek. The greatest radioactivity found in the rocks along the Elliott Highway was in an iron-stained schist of pre-Cambrian age and in carbonaceous shale of Middle Devonian or Carboniferous age. Respective samples of these rocks contain 0.003 and 0.004 percent equivalent uranium. A possible local bedrock source for a euxenite-polycrase mineral found in a placer concentrate containing about 0.04 percent equivalent uranium was sought in the watershed of Goodluck Creek, near Livengood. The bedrock source of this mineral could not be located; it is believed that the source could be outside of the Goodluck watershed, as drainage changes in the area during Quaternary time might well have introduced gravels from nearby areas.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei197","collaboration":"This report concerns work done on behalf of the Division of Raw materials of the U.S. Atomic Energy Commission","usgsCitation":"Wedow, H., Stevens, J., and Tolbert, G., 1953, Reconnaissance for radioactive deposits in the Fairbanks and Livengood Quadrangles, east-central Alaska, 1949: U.S. Geological Survey Trace Elements Investigations 197, Report: 13 p.; 1 Plate: 15.14 x 19.35 inches, https://doi.org/10.3133/tei197.","productDescription":"Report: 13 p.; 1 Plate: 15.14 x 19.35 inches","numberOfPages":"14","temporalStart":"1949-01-01","temporalEnd":"1949-12-31","costCenters":[],"links":[{"id":283648,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei197.jpg"},{"id":285616,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0197/figure-1.pdf"},{"id":285617,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0197/report.pdf"}],"country":"United States","state":"Alaska","otherGeospatial":"Fairbanks Quadrangle;Livengood Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -149.5,64.5 ], [ -149.5,66.0 ], [ -147.0,66.0 ], [ -147.0,64.5 ], [ -149.5,64.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559531e4b0120853e8c18c","contributors":{"authors":[{"text":"Wedow, H. Jr.","contributorId":6369,"corporation":false,"usgs":true,"family":"Wedow","given":"H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":491388,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stevens, J.M.","contributorId":49851,"corporation":false,"usgs":true,"family":"Stevens","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":491390,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tolbert, G.E.","contributorId":33759,"corporation":false,"usgs":true,"family":"Tolbert","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":491389,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":71159,"text":"tei51 - 1953 - Uranium deposits at Shinarump Mesa and some adjacent areas in the Temple Mountain district, Emery County, Utah","interactions":[],"lastModifiedDate":"2014-06-03T09:14:55","indexId":"tei51","displayToPublicDate":"1953-01-01T11:01:00","publicationYear":"1953","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":"51","title":"Uranium deposits at Shinarump Mesa and some adjacent areas in the Temple Mountain district, Emery County, Utah","docAbstract":"

Deposits of uraniferous hydrocarbons are associated with carnotite in the Shinarump conglomerate of Triassic age at Shinarump Mesa and adjacent areas of the Temple Mountain district in the San Rafael Swell of Emery County, Utah. The irregular ore bodies of carnotite-bearing sandstone are genetically related to lenticular uraniferous ore bodies containing disseminated asphaltitic and humic hydrocarbon in permeable sandstones and were localized indirectly by sedimentary controls. Nearly non-uraniferous bitumen commonly permeates the sandstones in the Shinarump conglomerate and the underlying Moekopi formation in the area. The ore deposits at Temple Mountain have been altered locally by hydrothermal solutions, and in other deposits throughout the area carnotite has been transported by ground and surface water.

\n
\n

Uraniferous asphaltite is thought to be the non-volatile residue of an original weakly uraniferous crude oil that migrated into the San Rafael anticline; the ore metals concentrated in the asphaltite as the oil was devolatilized and polymerized. Carnotite is thought to have formed from the asphaltite by ground water leaching.

\n
\n

It is concluded that additional study of the genesis of the asphaltitic uranium ores in the San Rafael Swell, of the processes by which the hydrocarbons interact and are modified (such as heat, polymerization, and hydrogenation under the influence of alpha-ray bombardment), of petroleum source beds, and of volcanic intrusive rocks of Tertiary age are of fundamental importance in the continuing study of the uranium deposits on the Colorado Plateau.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei51","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Wyant, D., 1953, Uranium deposits at Shinarump Mesa and some adjacent areas in the Temple Mountain district, Emery County, Utah: U.S. Geological Survey Trace Elements Investigations 51, Report: 91 p.; 3 Plates: 30.44 x 20.69 inches and smaller, https://doi.org/10.3133/tei51.","productDescription":"Report: 91 p.; 3 Plates: 30.44 x 20.69 inches and smaller","numberOfPages":"95","costCenters":[],"links":[{"id":284500,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0051/plate-5.pdf"},{"id":284498,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0051/plate-3.pdf"},{"id":284499,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0051/plate-4.pdf"},{"id":284501,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0051/report.pdf"},{"id":283474,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei51.jpg"}],"country":"United States","state":"Utah","county":"Emery County","otherGeospatial":"Temple Mountain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.307,38.4992 ], [ -111.307,39.7076 ], [ -109.9878,39.7076 ], [ -109.9878,38.4992 ], [ -111.307,38.4992 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"535595d6e4b0120853e8c2cd","contributors":{"authors":[{"text":"Wyant, Donald G.","contributorId":75950,"corporation":false,"usgs":true,"family":"Wyant","given":"Donald G.","affiliations":[],"preferred":false,"id":283745,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011093,"text":"70011093 - 1953 - Water","interactions":[],"lastModifiedDate":"2012-03-12T17:18:27","indexId":"70011093","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Water","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00032700","usgsCitation":"Love, S.K., and Thatcher, L.L., 1953, Water: Analytical Chemistry, v. 25, no. 1, p. 65-74.","startPage":"65","endPage":"74","numberOfPages":"10","costCenters":[],"links":[{"id":221349,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bc3fee4b08c986b32b44e","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":360265,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thatcher, L. L.","contributorId":23271,"corporation":false,"usgs":true,"family":"Thatcher","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360264,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":39721,"text":"pp257A - 1953 - Lake Bonneville: Geology of northern Utah Valley, Utah","interactions":[{"subject":{"id":52055,"text":"ofr49117 - 1949 - Statement on the hydrology of pre-Pleistocene (?) aquifers, from a chapter on water resources to be included in a Geological Survey report on the geology of North Utah Valley","indexId":"ofr49117","publicationYear":"1949","noYear":false,"title":"Statement on the hydrology of pre-Pleistocene (?) aquifers, from a chapter on water resources to be included in a Geological Survey report on the geology of North Utah Valley"},"predicate":"SUPERSEDED_BY","object":{"id":39721,"text":"pp257A - 1953 - Lake Bonneville: Geology of northern Utah Valley, Utah","indexId":"pp257A","publicationYear":"1953","noYear":false,"chapter":"A","title":"Lake Bonneville: Geology of northern Utah Valley, Utah"},"id":1}],"lastModifiedDate":"2022-11-22T15:28:33.251107","indexId":"pp257A","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"257","chapter":"A","title":"Lake Bonneville: Geology of northern Utah Valley, Utah","docAbstract":"

Lake Bonneville was a vast Pleistocene lake that covered 20,000 square miles in northwestern Utah and had a maximum depth of about 1,000 feet. It was a body of water comparable in size to modern Lake Michigan.

Surveys of the unconsolidated deposits in the Lake Bonneville basin utilize the same methods used in studies of hard rocks, namely: separation of the deposits into mappable units and contacts between formations; observations of lateral and vertical changes in lithology; and plotting of these data on the map.

","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp257A","usgsCitation":"Hunt, C.B., Varnes, H., and Thomas, H.E., 1953, Lake Bonneville: Geology of northern Utah Valley, Utah: U.S. Geological Survey Professional Paper 257, Report: v, 99 p.; 4 Plates, https://doi.org/10.3133/pp257A.","productDescription":"Report: v, 99 p.; 4 Plates","numberOfPages":"109","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":409532,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409531,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409530,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":409529,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0257a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0257a/report-thumb.jpg"},{"id":67485,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0257a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Northern Utah Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b42ff","contributors":{"authors":[{"text":"Hunt, C. B.","contributorId":42573,"corporation":false,"usgs":true,"family":"Hunt","given":"C.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":222036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Varnes, H.D.","contributorId":38631,"corporation":false,"usgs":true,"family":"Varnes","given":"H.D.","email":"","affiliations":[],"preferred":false,"id":222035,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":222034,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2450,"text":"wsp1137E - 1953 - Floods of 1950 in southwestern Oregon and northwestern California","interactions":[],"lastModifiedDate":"2023-03-23T19:00:20.210453","indexId":"wsp1137E","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"1137","chapter":"E","title":"Floods of 1950 in southwestern Oregon and northwestern California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1137E","usgsCitation":"Paulsen, C.G., 1953, Floods of 1950 in southwestern Oregon and northwestern California: U.S. Geological Survey Water Supply Paper 1137, Report: vi, 61 p.; 1 Plate: 17.50 x 36.00 inches, https://doi.org/10.3133/wsp1137E.","productDescription":"Report: vi, 61 p.; 1 Plate: 17.50 x 36.00 inches","startPage":"413","endPage":"503","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":414641,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24229.htm","linkFileType":{"id":5,"text":"html"}},{"id":28525,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1137e/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28526,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1137e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138130,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1137e/report-thumb.jpg"}],"country":"United States","state":"California, Oregon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -124.5,\n 45.367\n ],\n [\n -124.5,\n 40.4670\n ],\n [\n -121.5,\n 40.4670\n ],\n [\n -121.5,\n 45.367\n ],\n [\n -124.5,\n 45.367\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0d83","contributors":{"authors":[{"text":"Paulsen, C. G.","contributorId":96239,"corporation":false,"usgs":true,"family":"Paulsen","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":145223,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2507,"text":"wsp1136 - 1953 - Native and contaminated ground waters in the Long Beach-Santa Ana area, California","interactions":[],"lastModifiedDate":"2023-03-15T20:15:14.575742","indexId":"wsp1136","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"1136","title":"Native and contaminated ground waters in the Long Beach-Santa Ana area, California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1136","usgsCitation":"Piper, A., and Garrett, A.A., 1953, Native and contaminated ground waters in the Long Beach-Santa Ana area, California: U.S. Geological Survey Water Supply Paper 1136, Report: ix, 320 p.; 19 Plates: 20.00 x 15.50 inches or smaller, https://doi.org/10.3133/wsp1136.","productDescription":"Report: ix, 320 p.; 19 Plates: 20.00 x 15.50 inches or smaller","costCenters":[],"links":[{"id":28641,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28640,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28639,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28658,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1136/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414254,"rank":22,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24224.htm","linkFileType":{"id":5,"text":"html"}},{"id":28657,"rank":21,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28656,"rank":20,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138888,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1136/report-thumb.jpg"},{"id":28655,"rank":19,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28654,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28653,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28652,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28651,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28650,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28649,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28648,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28647,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28646,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28645,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28644,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28643,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28642,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","city":"Long Beach, Santa Ana","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.292,\n 33.602\n ],\n [\n -117.698,\n 33.602\n ],\n [\n -117.698,\n 34.031\n ],\n [\n -118.292,\n 34.031\n ],\n [\n -118.292,\n 33.602\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698311","contributors":{"authors":[{"text":"Piper, Arthur M.","contributorId":65060,"corporation":false,"usgs":true,"family":"Piper","given":"Arthur M.","affiliations":[],"preferred":false,"id":145310,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrett, A. A.","contributorId":44901,"corporation":false,"usgs":true,"family":"Garrett","given":"A.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":2140,"text":"wsp1228 - 1953 - Geology and water resources of Smith Valley, Lyon and Douglas Counties, Nevada","interactions":[],"lastModifiedDate":"2023-03-23T21:31:36.397394","indexId":"wsp1228","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"1228","title":"Geology and water resources of Smith Valley, Lyon and Douglas Counties, Nevada","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1228","usgsCitation":"Loeltz, O.J., and Eakin, T., 1953, Geology and water resources of Smith Valley, Lyon and Douglas Counties, Nevada: U.S. Geological Survey Water Supply Paper 1228, Report; iv, 89 p.; 3 Plates: 14.00 x 26.57 inches or smaller, https://doi.org/10.3133/wsp1228.","productDescription":"Report; iv, 89 p.; 3 Plates: 14.00 x 26.57 inches or smaller","costCenters":[],"links":[{"id":414665,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24284.htm","linkFileType":{"id":5,"text":"html"}},{"id":27743,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1228/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27742,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1228/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27741,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1228/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27740,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1228/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137794,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1228/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Douglas County, Lyon County","otherGeospatial":"Smith Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119.433,\n 39\n ],\n [\n -119.433,\n 38.733\n ],\n [\n -119.283,\n 38.733\n ],\n [\n -119.283,\n 39\n ],\n [\n -119.433,\n 39\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db684126","contributors":{"authors":[{"text":"Loeltz, Omar J.","contributorId":86312,"corporation":false,"usgs":true,"family":"Loeltz","given":"Omar","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":144729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eakin, Thomas E.","contributorId":95449,"corporation":false,"usgs":true,"family":"Eakin","given":"Thomas E.","affiliations":[],"preferred":false,"id":144730,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1285,"text":"wsp1190 - 1953 - Ground-water conditions in artesian aquifers in Brown County, Wisconsin","interactions":[],"lastModifiedDate":"2023-04-11T19:43:34.619708","indexId":"wsp1190","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"1190","title":"Ground-water conditions in artesian aquifers in Brown County, Wisconsin","docAbstract":"The principal water-bearing rocks underlying Brown County, Wis., are thick sandstone units of Cambrian and Ordovician age. Other aquifers include limestone and dolomite of Ordovician age, dolomite of Silurian age, and sands and gravel of Pleistocene and Recent age. Underlying the water-bearing formations are crystalline rocks of pre-Cambrian age which contain little or no water. \r\n\r\nGround water is the source of all public and most private and industrial supplies in. the county. Several of the large industries use large quantities of surface water also. Most of the water is pumped from wells that penetrate the Cambrian sandstones where the water occurs under artesian conditions. From 1886, when the first deep well was drilled, to 1949, the pumpage in the county increased to an average of about 5 million gallons a day (mgd) in 1939 and to about 10 mgd in 1949.\r\n\r\nThe piezometric level, which was about 100 feet above the land surface in 1886, was about 300 feet below the land surface in 1949. About 200 feet of this decline took place after 1938. The water-level-measurement program begun in 1946 shows that yearly fluctuations of water levels in observation wells range from less than 1 foot to about 90 feet, the fluctuations being larger at the center of the heavily pumped area. The highest water levels occur in the winter or spring and the lowest in the summer near the end of the season of maximum withdrawal. Coefficients of transmissibility and storage for the sandstones were obtained by making controlled pumping tests at Green Bay and De Pere. The coefficients were verified by comparing computed water-level declines and rates of withdrawal with actual ones. The computed values were within I0 percent of the actual values. \r\n\r\nProbable declines of water levels by 1960 were computed, using the same coefficients of transmissibility and storage, and assuming three different conditions of pumping. The additional decline in water level will be 15 to 150 feet in the center of the pumped area, depending upon the amount of increased pumping and its distribution relative to the present pumped area and to the recharge area. \r\n\r\nThe water from the sandstones is a hard calcium magnesium bicarbonate water. Further work is needed to determine whether there is danger of contamination by salt water which occurs down the dip in the same formations. It is concluded that the rate of withdrawal from the area can be increased to 15 mgd by 1960 without dangerously lowering water levels, provided that new wells are properly spaced. In order to avoid expressive lowering of water levels, it is recommended that new wells be located west of Green Bay toward the recharge area. \r\n\r\nA detailed study has not been made of shallow aquifers in the county. Further work should be done to evaluate the possibilities of auxiliary supplies from the limestone of the Platteville formation or from the Niagara dolomite. \r\n\r\nConservation should be practice.4 by all users of ground water to avoid waste resulting in lower water levels and higher pumping costs.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1190","usgsCitation":"Drescher, W.J., 1953, Ground-water conditions in artesian aquifers in Brown County, Wisconsin: U.S. Geological Survey Water Supply Paper 1190, Report: iv, 49 p.; 7 Plates: 20.00 x 9.00 inches or smaller, https://doi.org/10.3133/wsp1190.","productDescription":"Report: iv, 49 p.; 7 Plates: 20.00 x 9.00 inches or smaller","numberOfPages":"53","costCenters":[],"links":[{"id":415594,"rank":10,"type":{"id":36,"text":"NGMDB Index 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States","state":"Wisconsin","county":"Brown County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-87.9887,44.6778],[-87.9888,44.6728],[-87.9901,44.6719],[-87.9907,44.6719],[-87.9914,44.6719],[-87.9932,44.6751],[-87.9939,44.6751],[-87.9952,44.6751],[-87.9958,44.6747],[-87.9971,44.6719],[-87.9991,44.672],[-88.0029,44.6738],[-88.0061,44.6743],[-88.0067,44.6739],[-88.0074,44.6734],[-88.008,44.673],[-88.0074,44.6716],[-88.0062,44.6702],[-88.0005,44.6679],[-87.9998,44.6674],[-87.9998,44.6665],[-88.0005,44.6651],[-88.0012,44.6647],[-88.0018,44.6647],[-88.0075,44.6679],[-88.0082,44.6679],[-88.0088,44.6675],[-88.0082,44.6638],[-88.009,44.6575],[-88.0099,44.6461],[-88.0106,44.6456],[-88.0112,44.6456],[-88.0144,44.6466],[-88.0151,44.6466],[-88.0151,44.6457],[-88.0145,44.6429],[-88.0145,44.642],[-88.0191,44.6352],[-88.0185,44.6343],[-88.0153,44.6338],[-88.0147,44.6334],[-88.0117,44.6251],[-88.0074,44.6141],[-88.0068,44.6132],[-88.0004,44.6118],[-87.9941,44.6067],[-87.9816,44.5947],[-87.9797,44.5933],[-87.979,44.5924],[-87.9798,44.5878],[-87.9805,44.5828],[-87.9818,44.5824],[-87.983,44.5892],[-87.9848,44.591],[-87.9861,44.5943],[-87.9898,44.6002],[-88.0012,44.6077],[-88.0082,44.61],[-88.0088,44.61],[-88.0101,44.61],[-88.0107,44.6105],[-88.0107,44.6119],[-88.0136,44.6228],[-88.0149,44.6238],[-88.0155,44.6247],[-88.0162,44.6247],[-88.0168,44.6247],[-88.0175,44.6234],[-88.0182,44.6188],[-88.0178,44.6092],[-88.0187,44.5974],[-88.0188,44.5946],[-88.0207,44.5937],[-88.0214,44.5924],[-88.0214,44.5901],[-88.019,44.585],[-88.0204,44.5782],[-88.0191,44.5782],[-88.0185,44.5759],[-88.0173,44.5745],[-88.0179,44.5732],[-88.0192,44.5723],[-88.0211,44.5737],[-88.0217,44.5755],[-88.0237,44.5755],[-88.0269,44.5746],[-88.0365,44.577],[-88.039,44.5766],[-88.0462,44.5726],[-88.0468,44.5717],[-88.0475,44.5694],[-88.0476,44.5658],[-88.0451,44.5644],[-88.0425,44.5639],[-88.0406,44.5648],[-88.0399,44.5675],[-88.0386,44.5684],[-88.0335,44.5665],[-88.0284,44.5637],[-88.0259,44.5614],[-88.0234,44.56],[-88.0234,44.5591],[-88.0247,44.5582],[-88.0266,44.5573],[-88.0286,44.5569],[-88.0337,44.5583],[-88.0349,44.5583],[-88.0356,44.5574],[-88.0356,44.5565],[-88.0287,44.5514],[-88.0255,44.5495],[-88.0249,44.5486],[-88.0249,44.5477],[-88.0249,44.5463],[-88.0218,44.5445],[-88.0212,44.5436],[-88.0212,44.5427],[-88.0218,44.5422],[-88.027,44.5391],[-88.0264,44.5386],[-88.0245,44.5386],[-88.0226,44.5386],[-88.02,44.5399],[-88.018,44.5435],[-88.0167,44.544],[-88.0154,44.5435],[-88.0142,44.5417],[-88.0116,44.5407],[-88.0046,44.5393],[-87.9925,44.5337],[-87.9811,44.5303],[-87.9664,44.5284],[-87.9504,44.5277],[-87.9401,44.529],[-87.9343,44.5316],[-87.931,44.5348],[-87.927,44.5416],[-87.9244,44.5429],[-87.9171,44.5529],[-87.9105,44.5605],[-87.9079,44.5628],[-87.9053,44.5664],[-87.9052,44.5682],[-87.9045,44.571],[-87.9031,44.575],[-87.905,44.5755],[-87.9095,44.576],[-87.914,44.5743],[-87.916,44.5743],[-87.9172,44.5752],[-87.9172,44.5761],[-87.9094,44.5797],[-87.9036,44.5819],[-87.8964,44.5864],[-87.8918,44.5918],[-87.886,44.5963],[-87.8839,44.6026],[-87.8813,44.6049],[-87.8741,44.6085],[-87.8695,44.6139],[-87.861,44.6188],[-87.8585,44.6192],[-87.8565,44.6187],[-87.8527,44.6178],[-87.8495,44.6173],[-87.8463,44.6177],[-87.8262,44.6284],[-87.8177,44.6338],[-87.8131,44.636],[-87.806,44.6373],[-87.7919,44.638],[-87.7823,44.6374],[-87.7732,44.6396],[-87.7706,44.6414],[-87.7654,44.645],[-87.7628,44.6477],[-87.7643,44.5888],[-87.7646,44.5017],[-87.7655,44.4146],[-87.7665,44.3271],[-87.8879,44.3277],[-87.888,44.2402],[-87.9238,44.2402],[-88.0099,44.2407],[-88.0431,44.2411],[-88.1317,44.2411],[-88.163,44.2414],[-88.193,44.2421],[-88.1919,44.3288],[-88.1921,44.3871],[-88.1921,44.4167],[-88.1918,44.5016],[-88.1908,44.5864],[-88.2203,44.5858],[-88.2453,44.5846],[-88.2446,44.6239],[-88.2432,44.664],[-88.2528,44.6641],[-88.2525,44.6846],[-88.2435,44.6845],[-88.2287,44.6844],[-88.2289,44.6725],[-88.1833,44.6734],[-88.1312,44.677],[-88.0092,44.6775],[-87.9887,44.6778]]]},\"properties\":{\"name\":\"Brown\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d1fd","contributors":{"authors":[{"text":"Drescher, William James","contributorId":95448,"corporation":false,"usgs":true,"family":"Drescher","given":"William","email":"","middleInitial":"James","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000163,"text":"1000163 - 1953 - The movement of tagged lake trout in Lake Superior, 1950-52","interactions":[],"lastModifiedDate":"2012-02-02T00:04:33","indexId":"1000163","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"The movement of tagged lake trout in Lake Superior, 1950-52","docAbstract":"A total of 733 native lake trout was tagged at two widely separated localities in Lake Superior; subsequent recaptures numbered 155 fish (21.1 percent) during the year following marking. In October 1950, 116 large lake trout (average total length, 27.3 inches) were tagged near Keweenaw Point, Michigan. Fifteen (12.9 percent) were recovered during the first year at points as far west as the Gooseberry River, Minnesota (190 miles), north to the Slate Islands, Ontario (95 miles), and east to Grand Marais, Michigan (100 miles). Nine fish (7.8 percent) were recovered during the second year after marking. Returns from 617 tagged lake trout of smaller size (average length 18.2 inches) released in the Apostle Island region of Wisconsin during the period June 12 to August 6, 1951, numbered 140 (22.7 percent) during the first year. Of these fish, 90 percent were recaptured within a radius of 50 miles of the points of release. Seventy-six percent were caught in Wisconsin, 14 percent in Minnesota, and 9 percent in Michigan waters. The fish retaken in Michigan had moved 120 to 255 miles between the time of release and recapture, traveling as far wast as Grand Marais. Lake trout recaptured at distances of more than 50 miles from the tagging locality were of larger average size than marked fish caught within this radius.\r\nThe four types of tages used in the marking of lake trout in the Apostle Island region, together with the number tagged and percentage recovered during the first year were as follows: 103 aluminum lower-jaw tags (used only on fish less than 17 inches in length when marked)-10.7 percent; 200 monel upper-jaw tags-14 percent; 162 streamer tags-19.8 percent; and 152 Peterson tags-45.4 percent. Obviously lake trout marked with the Peterson tag, with the discs and ends of the pin projecting from each side near the point of maximum girth, were more vulnerable to the fishery than were fish marked with other tags. The recoveries of marked fish show that Lake Superior lake trout-particularly fish of large size-may move many miles and freely cross political boundaries; and that the rate of harvest is moderately high for a fish with a life history as long as that of the lake trout.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Transactions of the American Fisheries Society","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Eschmeyer, P.H., Daly, R., and Erkkila, L.F., 1953, The movement of tagged lake trout in Lake Superior, 1950-52: Transactions of the American Fisheries Society, v. 82, p. 68-77.","productDescription":"p. 68-77","startPage":"68","endPage":"77","numberOfPages":"9","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4732","contributors":{"authors":[{"text":"Eschmeyer, Paul H.","contributorId":86719,"corporation":false,"usgs":true,"family":"Eschmeyer","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308169,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daly, Russell","contributorId":97857,"corporation":false,"usgs":true,"family":"Daly","given":"Russell","email":"","affiliations":[],"preferred":false,"id":308171,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erkkila, Leo F.","contributorId":92197,"corporation":false,"usgs":true,"family":"Erkkila","given":"Leo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308170,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000221,"text":"1000221 - 1953 - Trout fishing in Michigan waters of Lake Superior, 1952","interactions":[],"lastModifiedDate":"2012-02-02T00:04:35","indexId":"1000221","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3560,"text":"The Fisherman","active":true,"publicationSubtype":{"id":10}},"title":"Trout fishing in Michigan waters of Lake Superior, 1952","docAbstract":"This article has been prepared to present the results of recently completed statistical studies on the fishery in the State of Michigan waters of the lake. The tabulations of production of lake trout and the estimates of levels of fishing pressure and abundance in the various statistical districts have been based on the monthly reports submitted by commercial operators to the Michigan Department of Conservation and turned over to the U.S. Fish and Wildlife Service for statistical analysis. To be sure, trends indicated by these statistics may not hold exactly for other areas of the lake. Conditions in Michigan are nonetheless of primary importance since during the last 25 years that state has accounted for nearly half of the entire Lake Superior trout production and for more than 70 percent of the take in U.S. waters.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"The Fisherman","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Hile, R., 1953, Trout fishing in Michigan waters of Lake Superior, 1952: The Fisherman, v. 21, no. 5, p. 7, 11-12, 14.","productDescription":"p. 7, 11-12, 14","startPage":"7, 11","endPage":"12, 14","numberOfPages":"5","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132937,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0651","contributors":{"authors":[{"text":"Hile, Ralph","contributorId":48510,"corporation":false,"usgs":true,"family":"Hile","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":308247,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000178,"text":"1000178 - 1953 - Fluctuations in the fisheries of State of Michigan waters of Green Bay","interactions":[],"lastModifiedDate":"2016-02-15T13:22:01","indexId":"1000178","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1664,"text":"Fishery Bulletin of the U.S. Fish and Wildlife Service","active":true,"publicationSubtype":{"id":10}},"title":"Fluctuations in the fisheries of State of Michigan waters of Green Bay","docAbstract":"

Green Bay, traditionally a major center of production, has assumed in recent years a position of overwhelming dominance in the commercial fisheries of the State of Michigan waters of Lake Michigan. Within the 4-year period 1945-1948 the commercial take in State of Michigan waters of Green Bay increased from 3,317,000 pounds in 1945 to 7,909,000 pounds in 1948, and it was 7,782,000 poinds in 1949. At the same time the percentage contribution of Green Bay to the State total for Lake Michigan rose each year, increasing from 36.5 in 1945 to 65.4 in 1949. The tremendous upswing in commercial production in Green Bay can be attributed to the abnormally high abundance of three important species--the lake whitefish (Coregonus clupeaformis), the lake herring or shallowwater cisco (Coregonus [=Leucichthys] artedii), and the walleye or yellow pikeperch (Stizostedion v. vitreum)--and to a marked rise in fishing intensity.

","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin of the U.S. Fish and Wildlife Service","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hile, R., Lunger, G.F., and Buettner, H.J., 1953, Fluctuations in the fisheries of State of Michigan waters of Green Bay: Fishery Bulletin of the U.S. Fish and Wildlife Service, v. 54, no. 75, p. 1-34.","productDescription":"p. 1-34","startPage":"1","endPage":"34","numberOfPages":"33","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131765,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"54","issue":"75","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aed3d","contributors":{"authors":[{"text":"Hile, Ralph","contributorId":48510,"corporation":false,"usgs":true,"family":"Hile","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":308196,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lunger, George F.","contributorId":11550,"corporation":false,"usgs":true,"family":"Lunger","given":"George","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308195,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Buettner, Howard J.","contributorId":82247,"corporation":false,"usgs":true,"family":"Buettner","given":"Howard","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":308197,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1000323,"text":"1000323 - 1953 - Movement of parasitic-phase sea lampreys in Lakes Huron and Michigan","interactions":[],"lastModifiedDate":"2016-02-15T11:49:13","indexId":"1000323","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Movement of parasitic-phase sea lampreys in Lakes Huron and Michigan","docAbstract":"

A program of tagging was carrie dout in the waters of northern Lake Huron during the fall and winter of 1951-52 in order to supplement the small amount of information available on movement of sea lampreys during their parasitic phase. A total of 219 parasitic-phase sea lampreys were tagged and released at three localities. Of this number 38 or 17.2 percent were recovered. One tag was recovered near North Manitou Island, Lake Michigan. The remaining 37 were take in Lake Huron or in streams tributary to that lake. The dispersal of tagged lampreys throughout Lake Huron was wide. Five marked individuals were taken in the southern part of the lake over 150 miles from the point of tagging; 4 of these 5 were captured in Canadian waters. The marked lampreys exhibited no distinct pattern of migration other than a tendency toward a general southeasterly movement in Lake Huron.

","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1952)82[123:MOPSLI]2.0.CO;2","usgsCitation":"Smith, B.R., and Elliott, O.R., 1953, Movement of parasitic-phase sea lampreys in Lakes Huron and Michigan: Transactions of the American Fisheries Society, v. 82, no. 1, p. 123-128, https://doi.org/10.1577/1548-8659(1952)82[123:MOPSLI]2.0.CO;2.","productDescription":"6 p.","startPage":"123","endPage":"128","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128614,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4814","contributors":{"authors":[{"text":"Smith, Bernard R.","contributorId":38924,"corporation":false,"usgs":true,"family":"Smith","given":"Bernard","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308390,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Elliott, Oliver R.","contributorId":11549,"corporation":false,"usgs":true,"family":"Elliott","given":"Oliver","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308389,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1000150,"text":"1000150 - 1953 - Movement of tagged lake trout in Lake Superior, 1950-1952","interactions":[],"lastModifiedDate":"2012-02-02T00:04:34","indexId":"1000150","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3560,"text":"The Fisherman","active":true,"publicationSubtype":{"id":10}},"title":"Movement of tagged lake trout in Lake Superior, 1950-1952","docAbstract":"A total of 733 native lake trout was tagged at two widely separated localities in Lake Superior; subsequent recaptures numbered 155 fish (21.1 percent) during the year following marking. In October 1950, 116 large lake trout (average total length, 27.3 inches) were tagged near Keweenaw Point, Michigan. Fifteen (12.9 percent) were recovered during the first year at points as far west as the Gooseberry River, Minnesota (190 miles), north to the Slate Islands, Ontario (95 miles), and east to Grand Marais, Michigan (100 miles). Nine fish (7.8 percent) were recovered during the second year after marking. Returns from 617 tagged lake trout of smaller size released in the Apostle Island region of Wisconsin during the period June 12 to August 6, 1951, numbered 140 (22.7 percent) during the first year. Of these fish, 90 percent were recaptured within a radius of 50 miles of the point of release. Seventy-six percent were caught in Wisconsin, 14 percent in Minnesota, and 9 percent in Michigan waters. The fish retaken in Michigan had moved 120 to 255 miles between the time of release and recapture, traveling as far east as Grand Marais. Lake trout recaptured at distances of more than 50 miles from the tagging locality were of larger average size than marked fish caught within this radius.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"The Fisherman","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Eschmeyer, P.H., Daly, R., and Erkkila, L.F., 1953, Movement of tagged lake trout in Lake Superior, 1950-1952: The Fisherman, v. 21, no. 3.","productDescription":"p. 4, 11","startPage":"4, 11","numberOfPages":"-4","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4816","contributors":{"authors":[{"text":"Eschmeyer, Paul H.","contributorId":86719,"corporation":false,"usgs":true,"family":"Eschmeyer","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daly, Russell","contributorId":97857,"corporation":false,"usgs":true,"family":"Daly","given":"Russell","email":"","affiliations":[],"preferred":false,"id":308150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erkkila, Leo F.","contributorId":92197,"corporation":false,"usgs":true,"family":"Erkkila","given":"Leo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308149,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70046375,"text":"70046375 - 1953 - Abbreviations used in publications of the United States Geological Survey","interactions":[],"lastModifiedDate":"2013-07-08T12:48:15","indexId":"70046375","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Abbreviations used in publications of the United States Geological Survey","docAbstract":"The use of abbreviations in publications of the Geological Survey is determined by several forces working in different directions. Pulling in the direction of greater condensation and the freer use of abbreviations and symbols is the desire to achieve greater economy in publications. Working in the opposite direction is the desire to have the publications used more conveniently by an increasingly heterogeneous public.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/70046375","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1953, Abbreviations used in publications of the United States Geological Survey, 9 p., https://doi.org/10.3133/70046375.","productDescription":"9 p.","numberOfPages":"11","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274615,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70046375/report.pdf"},{"id":273567,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70046375/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b6f562e4b0097a7158e57b","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535546,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}