{"pageNumber":"1856","pageRowStart":"46375","pageSize":"25","recordCount":46593,"records":[{"id":52982,"text":"ofr50101 - 1950 - Second progress report on the cooperative investigation of springs and stream flow in the Tecolote Tunnel area of Santa Barbara County, California","interactions":[],"lastModifiedDate":"2014-05-15T07:15:42","indexId":"ofr50101","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"50-101","title":"Second progress report on the cooperative investigation of springs and stream flow in the Tecolote Tunnel area of Santa Barbara County, California","docAbstract":"<p>This report represents the second of a series of progress reports giving the results of discharge measurements made at more than 100 locations in the Santa Ynez Mountains from the Refugio Canyon on the west to the San Marcos Pass and Painted Cave area on the east. The flow in all the developed springs and headwater streams within this area, here designated as the Tecolote Tunnel Area of the purpose of this report, is generally measured monthly. The primary purpose of this second progress report is to make available to the public all factual data regarding the flow at these locations obtained since the preparation of the first progress report, issued in May 1949. </p>\n<br>\nNear the mid-point of this area the Bureau of Reclamation and the Santa Barbara County Water Agency proposed a tunnel, known as Tecolote Tunnel, for the purpose of diverting a portion of the runoff of the Santa Ynez River drainage area into water-deficient Santa Barbara and the coastal areas to the east and west, Because the water users of the mountain springs in the Tecolote Tunnel Area are somewhat apprehensive as to the influence this tunnel may have on their present water supply, the Santa Barbara Water Agency has requested the Geological Survey to obtain records of flow in their springs at frequent and regular intervals. During the current fiscal year these observations have been made as a result of a cooperative agreement between the Geological Survey and the Santa Barbara County Water Agency whereby each paid half the cost of the investigation. During the previous fiscal year all the costs to the Geological Survey in obtaining these observations were completely reimbursed by the Bureau of Reclamation.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr50101","collaboration":"Prepared in cooperation with the Santa Barbara County Water Agency","usgsCitation":"Troxell, H.C., and Burgess, C., 1950, Second progress report on the cooperative investigation of springs and stream flow in the Tecolote Tunnel area of Santa Barbara County, California: U.S. Geological Survey Open-File Report 50-101, 156 p., https://doi.org/10.3133/ofr50101.","productDescription":"156 p.","numberOfPages":"159","costCenters":[],"links":[{"id":287187,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0101/report.pdf"},{"id":287188,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1950/0101/report-thumb.jpg"}],"scale":"50000","country":"United States","state":"California","county":"Santa Barbara County","otherGeospatial":"Tecolote Tunnel","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.083333,34.25 ], [ -120.083333,34.616667 ], [ -119.45,34.616667 ], [ -119.45,34.25 ], [ -120.083333,34.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc336","contributors":{"authors":[{"text":"Troxell, Harold C.","contributorId":33354,"corporation":false,"usgs":true,"family":"Troxell","given":"Harold","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":246325,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burgess, C.E.","contributorId":64329,"corporation":false,"usgs":true,"family":"Burgess","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":246326,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":50920,"text":"ofr5052 - 1950 - Geologic interpretations of seismic data, relocation of Route 116, Stations 7-135 in Cheshire, Mass.","interactions":[],"lastModifiedDate":"2014-05-15T06:59:49","indexId":"ofr5052","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"50-52","title":"Geologic interpretations of seismic data, relocation of Route 116, Stations 7-135 in Cheshire, Mass.","docAbstract":"Three segments of the proposed relocation of Route 116, stations 7 to 135, in Cheshire, Mass. require shallow cuts. For the purpose of obtaining information on the depths to bedrock, and on the nature of the overlaying materials, seismic and geologic studies were made of the segments in October 1949. The work was done as part of the cooperative program of the Massachusetts Department of Public Works and the United States Department of the Interior, Geological Survey. On seismic transverse was made between stations 7 and 15, 1 between stations 80 and 82, 3 between stations 85 and 90, and 4 between stations 125 and 135.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boston, MA","doi":"10.3133/ofr5052","usgsCitation":"Willard, M., and Linehan, D., 1950, Geologic interpretations of seismic data, relocation of Route 116, Stations 7-135 in Cheshire, Mass.: U.S. Geological Survey Open-File Report 50-52, 4 p., https://doi.org/10.3133/ofr5052.","productDescription":"4 p.","numberOfPages":"9","costCenters":[],"links":[{"id":287183,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0052/report.pdf"},{"id":287184,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1950/0052/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Cheshire","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.212153,42.510932 ], [ -73.212153,42.606173 ], [ -73.080344,42.606173 ], [ -73.080344,42.510932 ], [ -73.212153,42.510932 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a50a7","contributors":{"authors":[{"text":"Willard, Max E.","contributorId":104147,"corporation":false,"usgs":true,"family":"Willard","given":"Max E.","affiliations":[],"preferred":false,"id":242621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":242620,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3532,"text":"cir89 - 1950 - Coal resources of New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir89","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"89","title":"Coal resources of New Mexico","docAbstract":"A study of water quality degradation due to brine contamination was made in an area of about 1,700 sq mi in east-central Oklahoma. The study area coincides in part with the outcrop of the Vamoosa-Ada aquifer of Pennsylvanian age. Water samples collected from 180 wells completed in the Vamoosa-Ada aquifer and at 167 sites from streams draining the Vamoosa-Ada aquifer show scattered occurrences of water quality degradation by brine. Degradation of water quality by brine is indicated where: (1) chloride concentration is &gt; or = to 400 mg/L; (2) bromide concentration is &gt; or = 2 mg/L; (3) the ratio of sodium plus chloride to dissolved solids is &gt; or = 0.64. Ratios of secondary importance that also indicate water quality degradation by brine in the area are: (1) a ratio of lithium to bromide &lt; or = 0.01, when the chloride concentration is &gt; or = 400 mg/L; (2) a sodium/chloride ratio of about 0.46; (3) a sodium/bromide ratio of about 92; and (4) a bromide/chloride ratio of about 0.0048. Values for bromide, lithium, strontium, dissolved solids, calcium, magnesium, sodium, chloride, and sulfate concentrations were subjected to analysis of variance based on use of the index values in partition data sets. The analysis of variance showed the significance of the indexes for all constituents except sulfate. The two most reliable brine indicators are chloride and bromide. Statistically, chloride is a slightly more reliable index than bromide. The developed indexes can be used to indicate water quality degradation by brine. Accuracy is improved if both indexes are used. When geophysical logs from 133 pairs of oil and gas wells were analyzed, data from 5 pairs of wells indicated a possible rise in the interface between fresh water and salt water in the Vamoosa-Ada aquifer. Therefore , any rise of the interface is local rather than regional. The criteria developed in this study indicate that brine has degraded water quality at 63 sites on streams draining the Vamoosa-Ada aquifer, at 15 water wells completed in the Vamoosa-Ada aquifer, and at 5 oil and gas wells penetrating the Vamoosa-Ada aquifer. (Author 's abstract)","language":"ENGLISH","publisher":"[Interior Duplicating Section],","doi":"10.3133/cir89","usgsCitation":"Read, C.B., Duffner, R.T., Wood, G., and Zapp, A., 1950, Coal resources of New Mexico: U.S. Geological Survey Circular 89, ii, 24 p. :fold. map, tables. ;27 cm., https://doi.org/10.3133/cir89.","productDescription":"ii, 24 p. :fold. map, tables. ;27 cm.","costCenters":[],"links":[{"id":123345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1950/0089/report-thumb.jpg"},{"id":30546,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1950/0089/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30547,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1950/0089/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4804e4b07f02db4ceff3","contributors":{"authors":[{"text":"Read, Charles Brian","contributorId":68716,"corporation":false,"usgs":true,"family":"Read","given":"Charles","email":"","middleInitial":"Brian","affiliations":[],"preferred":false,"id":147108,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duffner, R. T.","contributorId":66243,"corporation":false,"usgs":true,"family":"Duffner","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":147107,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wood, G. H.","contributorId":106096,"corporation":false,"usgs":true,"family":"Wood","given":"G. H.","affiliations":[],"preferred":false,"id":147109,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Zapp, A.D.","contributorId":51280,"corporation":false,"usgs":true,"family":"Zapp","given":"A.D.","affiliations":[],"preferred":false,"id":147106,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":3936,"text":"cir74 - 1950 - A glossary of uranium- and thorium-bearing minerals","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir74","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"74","title":"A glossary of uranium- and thorium-bearing minerals","docAbstract":"During 1980, an estimated 121 million gallons of water per day was pumped in a 26-county area in east-central Georgia from sand aquifers of Paleocene and Late Cretaceous age. Maximum withdrawals were at the kaolin mining and processing centers in Twiggs, Wilkinson, and Washington Counties, where water levels have declined as much as 50 ft since 1944-50. In the southern two-thirds of the study area, water levels have shown little, if any, change. Declining water levels and increasing competition for groundwater have caused concern over the adequacy of groundwater supplies. This report defines the areal extent and describes the geohydrology of the Paleocene-Upper Cretaceous aquifers of east-central Georgia, and evaluates the effects of man on the groundwater flow system. Geohydrologic data from four test wells indicate that the aquifers consist of alternating layers of sand and clay that are largely of deltaic origin. In the northern third of the study area, the confining unit between the Dublin and Midville aquifer systems is absent and the aquifer systems combine to form the Dublin-Midville aquifer system. The aquifer systems range in thickness from 80 to 645 ft and their transmissivities range from 800 to 39,000 sq ft/day. The hydraulic conductivity ranges from 15 to 530 ft/day. Wells yield as much as 3,400 gpm (gallons per minute). Chemical analyses of water from 49 wells indicate that water from both aquifer systems is of good quality except in the central part of the study area, where iron concentrations are as high as 6,700 micrograms/L and exceed the 300 micrograms/L recommended limit for drinking water. The principal recharge to the aquifer systems is from precipitation that occurs within and adjacent to the outcrop areas. The principal discharge is to streams in the outcrop area. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir74","usgsCitation":"Frondel, J.W., and Fleischer, M., 1950, A glossary of uranium- and thorium-bearing minerals: U.S. Geological Survey Circular 74, 20 p. ;27 cm., https://doi.org/10.3133/cir74.","productDescription":"20 p. ;27 cm.","costCenters":[],"links":[{"id":123799,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1950/0074/report-thumb.jpg"},{"id":31021,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1950/0074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae59e","contributors":{"authors":[{"text":"Frondel, Judith Weiss","contributorId":55810,"corporation":false,"usgs":true,"family":"Frondel","given":"Judith","email":"","middleInitial":"Weiss","affiliations":[],"preferred":false,"id":147856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fleischer, Michael","contributorId":65835,"corporation":false,"usgs":true,"family":"Fleischer","given":"Michael","email":"","affiliations":[],"preferred":false,"id":147857,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3767,"text":"cir71 - 1950 - Techniques used in mine-water problems of the east Tennessee zinc district","interactions":[],"lastModifiedDate":"2012-02-02T00:05:32","indexId":"cir71","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"71","title":"Techniques used in mine-water problems of the east Tennessee zinc district","docAbstract":"A study of ground water as related to mining in cavernous limestones and dolomites in eastern Tennessee was made in 1946 by the U. S. Geological Survey. Surface and subsurface mapping indicated the geologic control of underground channels. Several methods of tracing water were tried and new techniques in using these methods evolved from the work. Rainfall data, when correlated with ground-water volumes and velocities, gave much information as to expected pumping volumes for any period. The use of fluorescent dye for tracing the flow of the water is described and other methods are discussed briefly. Four examples, each from a different mine, are discussed in detail and some remedies for the problems are suggested.","language":"ENGLISH","publisher":"[U.S. Geological Survey],","doi":"10.3133/cir71","usgsCitation":"Kent, D.F., 1950, Techniques used in mine-water problems of the east Tennessee zinc district: U.S. Geological Survey Circular 71, 9 p. :ill. ;27 cm., https://doi.org/10.3133/cir71.","productDescription":"9 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":122062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1950/0071/report-thumb.jpg"},{"id":30832,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1950/0071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685a8a","contributors":{"authors":[{"text":"Kent, Deane Frederick","contributorId":42083,"corporation":false,"usgs":true,"family":"Kent","given":"Deane","email":"","middleInitial":"Frederick","affiliations":[],"preferred":false,"id":147567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4188,"text":"cir94 - 1950 - Coal resources of the United States, A progress report, November 1, 1950","interactions":[],"lastModifiedDate":"2018-03-14T14:10:40","indexId":"cir94","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"94","title":"Coal resources of the United States, A progress report, November 1, 1950","docAbstract":"<p>Interest in the quantity and quality of the coal reserves of the United States has increased greatly since the end of World War II, principally because of the growing realization that the ultimate reserves of petroleum and natural gas, although largely undefined, still. have finite limits. With the greatly increased use of petroleum and natural gas, it has become further apparent that the reserves of these two fuels, whatever their ultimate limits may prove to be, are being consumed at a rate far surpassing that anticipated a few years ago. At some time in the future, therefore, the contribution of coal to the total production of energy in this country must inevitably be enlarged to include some of the needs now served by petroleum and natural gas. </p><p>Although coal-bearing rocks cover 14 percent of the total area of the United States (fig. 1) and contain enormous reserves, it is equally apparent that reserves of coal also have limits. In the extensively mined sections in the East it is already increasingly difficult to locate new areas containing thick beds of high-rank and high-quality coal to replace areas that have been mined out. Furthermore, a considerable part of the total reserves of the United States consists of coal of lignite and subbituminous ranks and coal contained in thin beds that can be mined only with great difficulty and expense. At the present time, therefore, the depletion of reserves of high-rank and high-quality coal, particularly the Eastern coal that is suitable for the manufacture of metallurgical coke, is a more serious problem than the percentage depletion of the total coal reserves. </p><p>Recognizing the need for more detailed estimates of coal reserves than those that have been available in the past, the U. S. Geological Survey is now preparing a reappraisal of the coal reserves of the United States in which primary emphasis is placed on the amounts of coal in separate categories according to rank,thickness of coal, and thickness of overburden. Many of the state geological surveys in coal-producing areas are also preparing new appraisals of coal reserves. The increasing volume of geologic data available on the occurrence of coal and the detailed and careful methods now employed in calculating reserves should ultimately provide a more reliable estimate for the coal reserves of the United States than has been obtainable previously, although much additional work remains to be done.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/cir94","usgsCitation":"Averitt, P., and Berryhill, L.R., 1950, Coal resources of the United States, A progress report, November 1, 1950: U.S. Geological Survey Circular 94, ii, 33 p., https://doi.org/10.3133/cir94.","productDescription":"ii, 33 p.","costCenters":[],"links":[{"id":31302,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1950/0094/report.pdf","text":"Report","size":"3.76 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":120879,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1950/0094/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6aedef","contributors":{"authors":[{"text":"Averitt, Paul","contributorId":12464,"corporation":false,"usgs":true,"family":"Averitt","given":"Paul","email":"","affiliations":[],"preferred":false,"id":148368,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berryhill, Louise R.","contributorId":37727,"corporation":false,"usgs":true,"family":"Berryhill","given":"Louise","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148369,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1064,"text":"wsp1070 - 1950 - Public water supplies in southern Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:36:08","indexId":"wsp1070","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","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":"1070","title":"Public water supplies in southern Texas","docAbstract":"<p>This report gives a summarized description of the public water supplies in 42 counties of southern Texas, extending from the Rio Grande northward to the northern boundaries of Kinney, Uvalde, Bandera, Kendall, and Hays Counties and eastward to the eastern boundaries of Caldwell, Gonzales, DeWitt, Victoria, and Calhoun Counties. It gives the available data as follows for each of the 114 communities: Population of the community; name of the official from whom the information was obtained; ownership of water works, whether private or municipal; source of supply, whether ground or surface water; the amount of water consumed; the facilities for storage; the number of customers served; the character of the chemical and sanitary treatment, if any; and chemical analyses of the water. Where ground water is used, the following information also is given: Records of wells, including drillers' logs; character of the pumping equipment; yield of the wells and records of water levels, where they are available.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1070","usgsCitation":"Broadhurst, W., Sundstrom, R., and Rowley, J., 1950, Public water supplies in southern Texas: U.S. Geological Survey Water Supply Paper 1070, vi, 114 p., https://doi.org/10.3133/wsp1070.","productDescription":"vi, 114 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":138102,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1070/report-thumb.jpg"},{"id":25743,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1070/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bc22","contributors":{"authors":[{"text":"Broadhurst, W. L.","contributorId":55414,"corporation":false,"usgs":true,"family":"Broadhurst","given":"W. L.","affiliations":[],"preferred":false,"id":143116,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sundstrom, R.W.","contributorId":103657,"corporation":false,"usgs":true,"family":"Sundstrom","given":"R.W.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":143117,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rowley, J.H.","contributorId":54968,"corporation":false,"usgs":true,"family":"Rowley","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":143115,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":35854,"text":"b964B - 1950 - Mineral resources of Colombia (other than petroleum)","interactions":[],"lastModifiedDate":"2017-06-10T11:41:02","indexId":"b964B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"964","chapter":"B","title":"Mineral resources of Colombia (other than petroleum)","docAbstract":"The following report summarizes data acquired during 1942-45, in Colombia, by geologists and engineers of the Foreign Economic Administration, with whom the United States Geological Survey cooperated. Twenty-nine mineral commodities are considered, but the data for five of them are scant because they were of no interest to FEA personnel. Petroleum is not considered. Preliminary to a review of individual mineral commodities, resumes are given of the general geography and geology of Colombia and of the country's mining laws. The principal mineral commodities, besides petroleum, produced in Colombia are (1) emeralds, gold, platinum, and silver, mainly for export, and (2) barite, cement, clay, coal, gypsum, salt, sand and gravel, silica, and stone, mainly for the domestic market. A large number of other mineral commodities are known in \"raw\" prospects, some of which may eventually become productive. Their distribution and apparent potentialities, as of 1945, are given. Factors unfavorable to mining are the ruggedness of the terrain, the scarcity of outcrops, and the very high transportation costs.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/b964B","collaboration":"Prepared in cooperation with the Foreign Economic Administration","usgsCitation":"Singewald, Q.D., 1950, Mineral resources of Colombia (other than petroleum): U.S. Geological Survey Bulletin 964, Report: viii, p. 53-204; 9 Plates: 14.64 x 13.3 inches or smaller, https://doi.org/10.3133/b964B.","productDescription":"Report: viii, p. 53-204; 9 Plates: 14.64 x 13.3 inches or smaller","numberOfPages":"161","temporalStart":"1942-01-01","temporalEnd":"1945-01-01","costCenters":[],"links":[{"id":266388,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964b/plate-7.pdf"},{"id":266389,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964b/plate-8.pdf"},{"id":266386,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964b/plate-5.pdf"},{"id":266387,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964b/plate-6.pdf"},{"id":266394,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964b/plate-13.pdf"},{"id":266391,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964b/plate-11.pdf"},{"id":266393,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964b/plate-10.pdf"},{"id":266390,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964b/plate-9.pdf"},{"id":266392,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/0964b/plate-12.pdf"},{"id":63813,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0964b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165575,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0964b/report-thumb.jpg"}],"country":"Colombia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.74,-4.23 ], [ -81.74,13.4 ], [ -66.85,13.4 ], [ -66.85,-4.23 ], [ -81.74,-4.23 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b08e4b07f02db69b5c0","contributors":{"authors":[{"text":"Singewald, Quentin Dreyer","contributorId":87115,"corporation":false,"usgs":true,"family":"Singewald","given":"Quentin","email":"","middleInitial":"Dreyer","affiliations":[],"preferred":false,"id":215336,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69200,"text":"coal5 - 1950 - The Fire Clay and Whitesburg coals in the Hyden quadrangle, Leslie, Clay, and Perry Counties, Kentucky","interactions":[],"lastModifiedDate":"2018-11-30T14:30:31","indexId":"coal5","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":309,"text":"Coal Map","code":"COAL","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"5","title":"The Fire Clay and Whitesburg coals in the Hyden quadrangle, Leslie, Clay, and Perry Counties, Kentucky","docAbstract":"<p>This preliminary report on the coal in the Hyden quadrangle, Kentucky, presents data on two of the principal commercial coals.&nbsp; The Fire Clay is the most valuable commercial coal in the quadrangle, and locally the Whitesburg bed is of minable thickness.&nbsp; Special emphasis has been placed on determining the thickness, extent, composition, and structure of these beds, and on obtaining an accurate estimate of the coal reserves.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/coal5","usgsCitation":"Johnston, J.E., and Heck, W.A., 1950, The Fire Clay and Whitesburg coals in the Hyden quadrangle, Leslie, Clay, and Perry Counties, Kentucky: U.S. Geological Survey Coal Map 5, 31.88 x 36.15 inches, https://doi.org/10.3133/coal5.","productDescription":"31.88 x 36.15 inches","costCenters":[],"links":[{"id":359839,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/coal/005/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":188181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/coal/005/report-thumb.jpg"}],"scale":"62500","country":"United States","state":"Kentucky","county":"Clay County, Leslie County, Perry County","otherGeospatial":"Hyden Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.5,37 ], [ -83.5,37.25 ], [ -83.25,37.25 ], [ -83.25,37 ], [ -83.5,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c82d","contributors":{"authors":[{"text":"Johnston, John Edward","contributorId":27946,"corporation":false,"usgs":true,"family":"Johnston","given":"John","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":279806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heck, W. A.","contributorId":207808,"corporation":false,"usgs":false,"family":"Heck","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":279807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":52932,"text":"ofr5054 - 1950 - Ground-water data collected in the Missouri River basin units in Kansas during 1948","interactions":[],"lastModifiedDate":"2018-10-30T09:33:05","indexId":"ofr5054","displayToPublicDate":"1993-12-31T00:00:00","publicationYear":"1950","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":"50-54","title":"Ground-water data collected in the Missouri River basin units in Kansas during 1948","docAbstract":"<p>Ground-water studies in the Missouri River Basin were begun by the U.S. Geological Survey during the fall of 1945 as a part of the program for development of the resources of the basin by the U.S. Bureau of Reclamation and other Federal agencies. The studies of the ground-water resources in the part of Kansas that lies within the basin have been coordinated with the cooperative program of ground-water studies already being carried on in Kansas by the Federal Geological Survey and the Kansas State Geological Survey with the cooperation of the Division of Sanitation of the Kansas State Board of health and the Division of Water Resources of the Kansas State Board of Agriculture.</p><p>Areas in which ground-water data have been collected under the Missouri Basin program include the Almena Unit in Norton and Phillips Counties; the Bostwick Unit in Jewell, Republic, and Cloud Counties; the Cedar Bluff Unit in Ellis and Trego Counties; the Glen Elder Unit in Mitchell County; the Kanopolis Unit in McPherson and Saline Counties; the Kirwin Unit in Phillips, Smith, and Osborne Counties; the St. Francis Unit in Cheyenne County; the Webster Unit in Osborne County; and the Wilson Unit in Lincoln County.</p><p>Most of the ground-water data presented in this report were collected during 1948. Most of the data collected in these areas prior to the end of 1947 were presented in a report mimeographed in September 1948. This report and the previous report are the first two of a series of annual reports on ground-water studies in the Missouri Basin units in Kansas. These reports are a means of more promptly releasing for administrative use the data collected each year. Data for a given area that are included in the annual reports will be assembled later in a report on the geology and hydrology of that area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5054","collaboration":"Compiled in cooperation with the State Geological Survey of Kansas, the Division of Sanitation of the Kansas State Board of Health, and the Division of Water Resources of the Kansas State Board of Agriculture.","usgsCitation":"Berry, D.W., 1950, Ground-water data collected in the Missouri River basin units in Kansas during 1948: U.S. Geological Survey Open-File Report 50-54, iv, 84 p., https://doi.org/10.3133/ofr5054.","productDescription":"iv, 84 p.","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":358926,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0054/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174908,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1950/0054/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Missouri River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.030029296875,\n              38.44498466889473\n            ],\n            [\n              -97.415771484375,\n              38.44498466889473\n            ],\n            [\n              -97.415771484375,\n              40.002371935876475\n            ],\n            [\n              -102.030029296875,\n              40.002371935876475\n            ],\n            [\n              -102.030029296875,\n              38.44498466889473\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cfe7","contributors":{"authors":[{"text":"Berry, Delmar W.","contributorId":25107,"corporation":false,"usgs":true,"family":"Berry","given":"Delmar","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":511498,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70222238,"text":"70222238 - 1950 - Preliminary report on selected sections of Lisburne Limestone, Brooks Range, Alaska","interactions":[],"lastModifiedDate":"2022-05-31T22:09:22.569709","indexId":"70222238","displayToPublicDate":"1950-11-01T16:24:31","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"31","subseriesTitle":"Preliminary Report","title":"Preliminary report on selected sections of Lisburne Limestone, Brooks Range, Alaska","docAbstract":"<p>Location: - This report describes sections of the Lisburne limestone studied in the foothills and northern mountains of the Brooks Range, Alaska. The area covered extends along the front of the range from Sagavanirktok Lake (68°28' N. - 149°25' W.) west to the head of the Kukpowruk River (68°25' N. - 162°40' W.). The southernmost point in the area is at the head of Alapah Creek (68°11' N. - 150°40' W.) and the northernmost point is on Lisburne Ridge just west of the Etivluk River (68°36' N. - 156°40' W.).</p><p>Field work was done by the authors at Sagavanirktok Lake, Kanayut Lake, Alapah Creek, the Anaktuvuk and Tiglukpuk Creek, and Chandler Lake. Brief visits were made to the Lisburne Ridge just north and west of the junction of the Nigu and Etivluk Rivers and to outcrops of Lisburne limestone along the Kiligwa River (68°30' N. - 158°35' W.). Data from other areas included in this report were collected by other field parties of the U. S. Geological Survey. A. L. Bowsher, Sr. .and J. T. Dutro, Jr. studied the Lisburne limestone at Kanayut Lake, Nanushuk Lake, and Itkillik Lake in 1949<sup>1</sup>/ .W. W. Patton, Jr. and Irving L. Tailleur described the Lisburne limestone exposed in the northern Brooks Range along the Kiruktagiak River <sup>2</sup>/ and the Okokmilage River <sup>3</sup>/ in1949, and I. L. Tailleur and Bion H. Kent have supplied data on the Etivluk-Kiligwa Rivers area from their field work of 1950 <sup>4</sup>/. R. M. Chapman, G. D. Eberlein, and C. D. Reynolds measured sections of Lisburne limestone at Kurupa Lake and on the east fork of the Etivluk River in 1950 <sup>5</sup>/. E. G. Sable and M. D. Mangus measured the section on Iligluruk Creek near the head of the Kokolik River in 1950 <sup>6</sup>/,, and Chapman end Sable measured the section at the head of the Kukpowrok River in 1949 <sup>7</sup>/.<br></p><p><br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70222238","usgsCitation":"Brosge, W.P., and Reiser, H.N., 1950, Preliminary report on selected sections of Lisburne Limestone, Brooks Range, Alaska: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 31, Report: 18 p.; 4 Plate: 44.73 x 25.47 inches or smaller; 5 Figures: 13.52 x 6.91 inches or smaller, https://doi.org/10.3133/70222238.","productDescription":"Report: 18 p.; 4 Plate: 44.73 x 25.47 inches or smaller; 5 Figures: 13.52 x 6.91 inches or smaller","costCenters":[],"links":[{"id":401495,"rank":12,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70222238/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":401494,"rank":11,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70222238/figure-4.pdf","text":"Figure 4","linkFileType":{"id":1,"text":"pdf"}},{"id":401493,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70222238/figure-3.pdf","text":"Figure 3","linkFileType":{"id":1,"text":"pdf"}},{"id":401492,"rank":9,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70222238/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":401491,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70222238/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":401490,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222238/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401489,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222238/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401488,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222238/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401487,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222238/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401486,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70222238/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":387346,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74580.htm","linkFileType":{"id":5,"text":"html"}},{"id":396881,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70222238/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Brooks Range, Lisburne Limestone","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -153,\n              68.2333\n            ],\n            [\n              -149.3333,\n              68.2333\n            ],\n            [\n              -149.3333,\n              68.5667\n            ],\n            [\n              -153,\n              68.5667\n            ],\n            [\n              -153,\n              68.2333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brosge, William P.","contributorId":287895,"corporation":false,"usgs":false,"family":"Brosge","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":837489,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reiser, Hillard N.","contributorId":189303,"corporation":false,"usgs":true,"family":"Reiser","given":"Hillard","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":837490,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215453,"text":"70215453 - 1950 - Discussion of “Annual floods and the partial duration flood series”","interactions":[],"lastModifiedDate":"2020-10-20T17:08:50.078713","indexId":"70215453","displayToPublicDate":"1950-10-20T11:55:22","publicationYear":"1950","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 “Annual floods and the partial duration flood series”","docAbstract":"<p>The writer is interested in finding from this paper a similar idea which he had in mind when engaging in a statistical study of hydrologic data, a part of the Highway Drainage Research Project being carried out in the Department of Civil Engineering, the University of Illinois. However, a complete presentation of the study will be reserved for future publications, and only fragments of thought are discussed here.</p><p>In treating hydrologic data for the study of their frequency of recurrence, two phases of study are generally met. One is the frequency of recurrence for the observed distributions, and the other is the corresponding frequency of recurrence for the theoretical distributions of best‐fit. The former is usually required for the purpose of plotting observed data, and hence is called the “plotting positions,” a term used by Foster [1934, p. 1217]. The latter is treated by the mathematical theory of probability, and generally serves as a theoretical interpretation of the observed phenomena.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR031i006p00939","usgsCitation":"Chow, V.T., and Langbein, W.B., 1950, Discussion of “Annual floods and the partial duration flood series”: Eos, Transactions, American Geophysical Union, v. 31, no. 6, p. 393-941, https://doi.org/10.1029/TR031i006p00939.","productDescription":"3 p.","startPage":"393","endPage":"941","costCenters":[],"links":[{"id":379551,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Chow, Ven Te","contributorId":243424,"corporation":false,"usgs":false,"family":"Chow","given":"Ven","email":"","middleInitial":"Te","affiliations":[],"preferred":false,"id":802229,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":802230,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215345,"text":"70215345 - 1950 - Activity Of Paricutin Volcano From August 1, 1948 to June 30, 1949","interactions":[],"lastModifiedDate":"2020-10-15T19:25:28.244133","indexId":"70215345","displayToPublicDate":"1950-10-15T14:19:28","publicationYear":"1950","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":"Activity Of Paricutin Volcano From August 1, 1948 to June 30, 1949","docAbstract":"<p><span>The present brief summary of activity at Paricutin Volcano, State of Michoacán, Mexico, follows the pattern of the last report on this volcano published in these&nbsp;</span><span>Transactions</span><span>&nbsp;late in 1948 [Wilcox and Gutierrez, 1948]. Anticipating the end of his two‐year period of observation at Parícutin in December 1948, Wilcox instructed the junior author, a native Tarascan from the town of San Juan Parangaricutiro, now destroyed, in the processes of keeping detailed diagrammatic records of eruptive activity, of making weather observations, and of outlining the monthly advance of the new lava. On Wilcox's departure the senior author, who had closely followed the series of studies at Paricutin and had frequently visited the Volcano from June 1943 onward, took up the task‐of watching over Paricutin and preparing reports on its activity. During the first six months of 1949 he spent 11 days at the Volcano on the following dates: January 25–28, March 29–April 1, and May 18–20. On these visits he checked the elevations of the chief points on the rim of tie cone, using an alidade at known stations, and in addition followed the growth of the lava‐vent mound, variations in the form of the interior of the crater, and any other features that showed change. Further, he discussed with the junior author, the Volcano's activity during the periods between visits and assembled the observational data for formal presentation.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR031i003p00406","usgsCitation":"Fries, C., and Gutierrez, C., 1950, Activity Of Paricutin Volcano From August 1, 1948 to June 30, 1949: Eos, Transactions, American Geophysical Union, v. 31, no. 3, p. 406-418, https://doi.org/10.1029/TR031i003p00406.","productDescription":"13p.","startPage":"406","endPage":"418","costCenters":[],"links":[{"id":379427,"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              -102.45849609375,\n              19.264479800497103\n            ],\n            [\n              -102.16735839843749,\n              19.264479800497103\n            ],\n            [\n              -102.16735839843749,\n              19.590844152960923\n            ],\n            [\n              -102.45849609375,\n              19.590844152960923\n            ],\n            [\n              -102.45849609375,\n              19.264479800497103\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"31","issue":"3","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":801832,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gutierrez, Celedonio","contributorId":243225,"corporation":false,"usgs":false,"family":"Gutierrez","given":"Celedonio","email":"","affiliations":[],"preferred":false,"id":801833,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":5223177,"text":"5223177 - 1950 - Populations and home range relationships of the box turtle, Terrapene c. carolina (Linnaeus)","interactions":[],"lastModifiedDate":"2023-10-11T16:57:40.046154","indexId":"5223177","displayToPublicDate":"1950-10-01T12:18:19","publicationYear":"1950","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1459,"text":"Ecological Monographs","active":true,"publicationSubtype":{"id":10}},"title":"Populations and home range relationships of the box turtle, Terrapene c. carolina (Linnaeus)","docAbstract":"SUMMARY:  A population study of the box turtle (Terrapene c. carolina Linnaeus) was made during the years 1944 to 1947 at the Patuxent Research Refuge, Maryland.      A thirty acre area in well drained bottomland forest on the flood plain of the Patuxent River was selected for intensive study.  Similarly forested land extended in all directions from the study plot.      Markers were established at eighty-three foot intervals over the study plot for reference in recording locality data.  Individuals were marked by filing notches in the marginal scutes according to a code system.  There were 2109 collections of study area turtles.      Records of collecting sites and turtle behavior showed that in the bottomlands habitat cover is utilized extensively during the day as well as at night. Turtles not actively moving about are almost always found in or around brush piles, heaps of debris, and tangles of vines and briars. Gully banks and woods openings are used for sunning. Turtles are occasionally found in the mud or water of the gullies.      The commonest type of night retreat is a cavity constructed by the turtle in leaves, debris, or earth. These cavities, termed 'forms,' may be used only once, but are sometimes used repeatedly, often at intervals of several days or more. Different turtles sometimes use the same form on successive nights.      Weather conditions most favorable to turtle activity are high humidity, warm sunny days, and frequent rains. The most unfavorable influences are low temperatures and drought. On most summer days there are some active turtles but individual turtles are not active every day. Periods of activity are alternated with periods of quiet even in favorable weather. This behavior is most pronounced in early spring and late fall when inactive days are often more numerous than active ones.      Adult turtles occupy specific home ranges which they maintain from year to year. The turtles living in the study plot retained their ranges even through a flood that completely covered the area.      Maximum home range diameters were determined by measurements of the mapped ranges of individual turtles. The average range of adult males was 330 feet, adult females 370 feet. The difference between male and female ranges was not statistically significant.      There was no evidence of defense of territory.  Ranges of turtles of all ages and both sexes overlapped grossly. Turtles were frequently found near each other and no antagonistic behavior was observed.      A trail-laying device was developed in order to follow individual travel routes. The trailer consists of a light weight housing fastened to the turtle's back. It contains a spool of white thread that unwinds as the turtle moves, thus marking its exact route.      Turtles selected for this more detailed study were followed with trailers for a total of 456 turtle days. Maps illustrating their travels are shown. Normal movements within the home range are characterized by, (1) turns, doublings, detours, and criss-crossing paths completely covering the area, (2) interspersion of fairly direct traverses of the home range, (3) frequently repeated travels over certain paths or routes.      Trailer records and mapped collection records both show that the maximum limits of the home range are ordinarily reached within a few days or weeks. This general procedure is varied by some turtles to include intensive coverage of only one portion of the range at a time.      Some turtles have two home ranges and travel between them at infrequent intervals. One turtle showing this behavior was followed with a trailer for 161 days during 1946 and 1947.      Trips outside the home range are made by some turtles. These include egg laying trips by females as well as trips of unexplained nature made by both males and females. Turtles from other areas occasionally occur as transients in the study plot.      The size of the population was estimated on the basis of collections during on","language":"English","publisher":"Ecological Society of America","doi":"10.2307/1943570","usgsCitation":"Stickel, L.F., 1950, Populations and home range relationships of the box turtle, Terrapene c. carolina (Linnaeus): Ecological Monographs, v. 20, no. 4, p. 351-378, https://doi.org/10.2307/1943570.","productDescription":"28 p.","startPage":"351","endPage":"378","numberOfPages":"28","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":199905,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"20","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69689c","contributors":{"authors":[{"text":"Stickel, Lucille F.","contributorId":76598,"corporation":false,"usgs":true,"family":"Stickel","given":"Lucille","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":338054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71144,"text":"tei108 - 1950 - A preliminary report on methods of determining the age of Colorado plateau carnotite","interactions":[],"lastModifiedDate":"2014-03-25T08:34:21","indexId":"tei108","displayToPublicDate":"1950-03-06T12:36:00","publicationYear":"1950","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":"108","title":"A preliminary report on methods of determining the age of Colorado plateau carnotite","docAbstract":"Four methods of dating Colorado Plateau carnotite have been examined and evaluated: mineralogic methods, radioactive-equilibrium methods, lead-uranium-ratio methods, and lead-isotope methods. The data on 12 high-grade samples, from a suite of 50 representative carnotite ores, are presented.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/tei108","usgsCitation":"Stieff, L.R., Girhard, M., and Stern, T.W., 1950, A preliminary report on methods of determining the age of Colorado plateau carnotite: U.S. Geological Survey Trace Elements Investigations 108, v, 126 p., https://doi.org/10.3133/tei108.","productDescription":"v, 126 p.","costCenters":[],"links":[{"id":284507,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0108/report.pdf"},{"id":283420,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei108.png"}],"country":"United States","state":"Colorado","otherGeospatial":"Colorado Plateau","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.36,33.6 ], [ -114.36,40.27 ], [ -106.92,40.27 ], [ -106.92,33.6 ], [ -114.36,33.6 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4a51e4b0b290850efb38","contributors":{"authors":[{"text":"Stieff, Lorin Rollins","contributorId":46509,"corporation":false,"usgs":true,"family":"Stieff","given":"Lorin","email":"","middleInitial":"Rollins","affiliations":[],"preferred":false,"id":283720,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Girhard, M.N.","contributorId":80142,"corporation":false,"usgs":true,"family":"Girhard","given":"M.N.","email":"","affiliations":[],"preferred":false,"id":283721,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stern, T. W.","contributorId":36122,"corporation":false,"usgs":true,"family":"Stern","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":283719,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70243784,"text":"70243784 - 1950 - Canada geese of the Mississippi flyway with special reference to an Illinois flock","interactions":[],"lastModifiedDate":"2023-05-19T15:47:04.938662","indexId":"70243784","displayToPublicDate":"1950-03-01T09:52:57","publicationYear":"1950","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":14436,"text":"Bulletin of the Illinois Natural History Survey","active":false,"publicationSubtype":{"id":10}},"title":"Canada geese of the Mississippi flyway with special reference to an Illinois flock","docAbstract":"<p><span>This Canada goose study is based on data from three primary sources : data collected at Horseshoe Lake, Alexander County, Illinois ; surveys by the authors on the distribution, habitat, and behavior of the population elsewhere in the Mississippi flyway ; and banding records of the Jack Miner Bird Sanctuary, Kingsville, Ontario. Data from other sources have been used as indicated in the text.</span></p>","language":"English","publisher":"Illinois Natural History Survey","doi":"10.21900/j.inhs.v25.184","usgsCitation":"Hanson, H.C., and Smith, R.H., 1950, Canada geese of the Mississippi flyway with special reference to an Illinois flock: Bulletin of the Illinois Natural History Survey, v. 25, no. 3, p. 67-210, https://doi.org/10.21900/j.inhs.v25.184.","productDescription":"144 p.","startPage":"67","endPage":"210","costCenters":[],"links":[{"id":480440,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.21900/j.inhs.v25.184","text":"Publisher Index Page"},{"id":417250,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Illinois","otherGeospatial":"Horseshoe Lake Game Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -90.14237612234776,\n              38.72469471493051\n            ],\n            [\n              -90.14237612234776,\n              38.64672855001197\n            ],\n            [\n              -90.0556040162737,\n              38.64672855001197\n            ],\n            [\n              -90.0556040162737,\n              38.72469471493051\n            ],\n            [\n              -90.14237612234776,\n              38.72469471493051\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"25","issue":"3","noUsgsAuthors":false,"publicationDate":"1950-03-31","publicationStatus":"PW","contributors":{"authors":[{"text":"Hanson, Harold C.","contributorId":305583,"corporation":false,"usgs":false,"family":"Hanson","given":"Harold","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":873244,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Robert H.","contributorId":305584,"corporation":false,"usgs":true,"family":"Smith","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":873245,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72045,"text":"tem128 - 1950 - Report of factual data obtained during examination of Copper King shaft, Black Hawk Claim No. 1, Larimer County, Colorado","interactions":[],"lastModifiedDate":"2014-02-28T13:51:22","indexId":"tem128","displayToPublicDate":"1950-01-10T13:07:00","publicationYear":"1950","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"128","title":"Report of factual data obtained during examination of Copper King shaft, Black Hawk Claim No. 1, Larimer County, Colorado","docAbstract":"No abstract available","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem128","usgsCitation":"Granger, H., and King, R., 1950, Report of factual data obtained during examination of Copper King shaft, Black Hawk Claim No. 1, Larimer County, Colorado: U.S. Geological Survey Trace Elements Memorandum 128, 8 p., https://doi.org/10.3133/tem128.","productDescription":"8 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":279184,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0128/report-thumb.jpg"},{"id":282977,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0128/report.pdf"}],"country":"United States","state":"Colorado","county":"Larimer County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -105.518789,40.836282 ], [ -105.518789,40.852449 ], [ -105.471840,40.852449 ], [ -105.471840,40.836282 ], [ -105.518789,40.836282 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"528c96bae4b0c629af44ddfe","contributors":{"authors":[{"text":"Granger, Harry C.","contributorId":67992,"corporation":false,"usgs":true,"family":"Granger","given":"Harry C.","affiliations":[],"preferred":false,"id":285039,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"King, R.U.","contributorId":7692,"corporation":false,"usgs":true,"family":"King","given":"R.U.","email":"","affiliations":[],"preferred":false,"id":285038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70104152,"text":"ofr5046B - 1950 - Geologic interpretation of seismic data relocation Route 1, cut, Stations 34-52, Copper Mine Road area and northern portion of Ballard Estate in Topsfield, Mass.","interactions":[],"lastModifiedDate":"2014-05-15T08:59:30","indexId":"ofr5046B","displayToPublicDate":"1950-01-01T14:56:00","publicationYear":"1950","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":"50-46","chapter":"B","title":"Geologic interpretation of seismic data relocation Route 1, cut, Stations 34-52, Copper Mine Road area and northern portion of Ballard Estate in Topsfield, Mass.","docAbstract":"Relocation of the Newburyport Turnpike, Route 1, in Topsfield, Mass., will require a long relatively deep cut between stations 34 and 52. In order to obtain preliminary information on the depths to bedrock and on the nature of the subsurface materials at this site, reconnaissance seismic work was performed in October 1949. Because this reconnaissance work indicated that bedrock might be relatively near the surface over an extensive area where cuttings were to be made, a more detailed seismic study of the area was made in November 1949. The results of both the reconnaissance and detailed seismic work are included in this report. The work was done as part of a cooperative program of the Massachusetts Department of Public Works and the U.S. Geological Survey.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5046B","usgsCitation":"May, J.E., and Linehan, D., 1950, Geologic interpretation of seismic data relocation Route 1, cut, Stations 34-52, Copper Mine Road area and northern portion of Ballard Estate in Topsfield, Mass.: U.S. Geological Survey Open-File Report 50-46, 5 p., https://doi.org/10.3133/ofr5046B.","productDescription":"5 p.","numberOfPages":"10","costCenters":[],"links":[{"id":287202,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0046-B/report.pdf"},{"id":287207,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1950/0046-B/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Topsfield","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -70.985293,42.599707 ], [ -70.985293,42.673091 ], [ -70.894833,42.673091 ], [ -70.894833,42.599707 ], [ -70.985293,42.599707 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5375e204e4b010920bbded93","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":493576,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":493575,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70104151,"text":"ofr5046A - 1950 - Geologic interpretation of seismic data relocation Route 2, Littleton Road grade separation stations 243-252 in Harvard, Mass.","interactions":[],"lastModifiedDate":"2014-05-15T06:54:35","indexId":"ofr5046A","displayToPublicDate":"1950-01-01T14:48:00","publicationYear":"1950","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":"50-46","chapter":"A","title":"Geologic interpretation of seismic data relocation Route 2, Littleton Road grade separation stations 243-252 in Harvard, Mass.","docAbstract":"<p>During parts of June and July 1949 nine seismic traverses were made at this site. Upon preliminary office development, the velocity data for some of these traverses were though to be inadequate and it was recommended that these lines be re-surveyed. Later surveys (March 1950), however, of nearby sites indicated that the original data were reliable and that a re-survey was unnecessary.</p>\n<br>\n<p>The work was done as part of a cooperative program of the Massachusetts Department of Public Works and the United States Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5046A","usgsCitation":"May, J.E., and Linehan, D., 1950, Geologic interpretation of seismic data relocation Route 2, Littleton Road grade separation stations 243-252 in Harvard, Mass.: U.S. Geological Survey Open-File Report 50-46, 4 p., https://doi.org/10.3133/ofr5046A.","productDescription":"4 p.","numberOfPages":"7","costCenters":[],"links":[{"id":287181,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0046-A/report.pdf"},{"id":287182,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1950/0046-A/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Harvard","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.635397,42.447486 ], [ -71.635397,42.550424 ], [ -71.529753,42.550424 ], [ -71.529753,42.447486 ], [ -71.635397,42.447486 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5375e204e4b010920bbded9d","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":493574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":493573,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70104145,"text":"ofr5043D - 1950 - Geologic interpretations of seismic data relocation Routes 15 and 20 in Sturbridge, Mass.","interactions":[],"lastModifiedDate":"2014-05-15T06:35:56","indexId":"ofr5043D","displayToPublicDate":"1950-01-01T14:06:00","publicationYear":"1950","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":"50-43","chapter":"D","title":"Geologic interpretations of seismic data relocation Routes 15 and 20 in Sturbridge, Mass.","docAbstract":"<p>The proposed improvements at the junction of Routes 15 and 20, Sturbridge, Massachusetts, requires a cut of considerable magnitude for the relocation of east-bound Route 20 between stations 158 and 167. Geologic and seismic studies were made of the site for the purpose of determining the position of the bedrock surface, the kinds of material to be excavated, and the relationships of these materials to each other.</p>\n<br>\n<p>The work was performed in November 1949 as a part of a cooperative program of the Massachusetts Department of Public Works and the United States Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boston, MA","doi":"10.3133/ofr5043D","usgsCitation":"May, J.E., and Linehan, D., 1950, Geologic interpretations of seismic data relocation Routes 15 and 20 in Sturbridge, Mass.: U.S. Geological Survey Open-File Report 50-43, 3 p., https://doi.org/10.3133/ofr5043D.","productDescription":"3 p.","numberOfPages":"6","costCenters":[],"links":[{"id":287175,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0043-D/report.pdf"},{"id":287176,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1950/0043-D/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Sturbridge","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.135687,42.028723 ], [ -72.135687,42.174597 ], [ -72.02387,42.174597 ], [ -72.02387,42.028723 ], [ -72.135687,42.028723 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5375e206e4b010920bbdedad","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":493550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":493549,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70104142,"text":"ofr5043A - 1950 - Geologic interpretations of seismic data Route 128 (Northern Circumferential Highway) cut, and Hopkins Street grade separation stations 1-18 in Wakefield, Mass.","interactions":[],"lastModifiedDate":"2014-05-15T06:28:20","indexId":"ofr5043A","displayToPublicDate":"1950-01-01T13:23:00","publicationYear":"1950","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":"50-43","chapter":"A","title":"Geologic interpretations of seismic data Route 128 (Northern Circumferential Highway) cut, and Hopkins Street grade separation stations 1-18 in Wakefield, Mass.","docAbstract":"<p>The completion of a segment of the Northern Circumferential Highway, Route 126, in Wakefield, Mass., requires an underpass bridge at Hopkins Street, Station 5+50. The plan of the project shows approximately 1800 feet if approach cuts between stations 1 and 18. In October 1945 a preliminary seismic study was made of a segment of this cut between stations 6+50 and 13+30. Four profiles were made at this time and a report was submitted by Newton E. Chute and Rev. Daniel Linhan (file report of January 15). This work showed a relatively shallow (in general, 6 to 12 feet in depth) somewhat irregular bedrock surface between stations 6+50 and 13+50. That data indicated that much of this segment of the cut will be in bedrock. In order to obtain more complete data for the preparation of detailed estimates on the amount of bedrock to be excavated for this segment of the cut, and also to obtain sufficient data for the unexplored segment of the cut, 21 additional seismic traverses were made in September 1949. The present report contains only the results obtained from this later work.</p>\n<br>\n<p>The work was performed as a part of a cooperative program of the Massachusetts Department of Public Works and the United States Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5043A","usgsCitation":"May, J.E., and Lineham, D., 1950, Geologic interpretations of seismic data Route 128 (Northern Circumferential Highway) cut, and Hopkins Street grade separation stations 1-18 in Wakefield, Mass.: U.S. Geological Survey Open-File Report 50-43, 4 p., https://doi.org/10.3133/ofr5043A.","productDescription":"4 p.","numberOfPages":"8","costCenters":[],"links":[{"id":287173,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0043-A/report.pdf"},{"id":287174,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1950/0043-A/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Wakefield","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.101045,42.471428 ], [ -71.101045,42.530895 ], [ -71.035296,42.530895 ], [ -71.035296,42.471428 ], [ -71.101045,42.471428 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5375e205e4b010920bbdeda8","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":493543,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lineham, Daniel","contributorId":99474,"corporation":false,"usgs":true,"family":"Lineham","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":493544,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70104140,"text":"ofr5042B - 1950 - Geologic interpretation of seismic data relocation Route 1, stations 150-155 in Danvers, Mass.","interactions":[],"lastModifiedDate":"2014-05-15T06:23:32","indexId":"ofr5042B","displayToPublicDate":"1950-01-01T13:10:00","publicationYear":"1950","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":"50-42","chapter":"B","title":"Geologic interpretation of seismic data relocation Route 1, stations 150-155 in Danvers, Mass.","docAbstract":"At this site the reconstruction of Route 1 requires a deep excavation through a high, east-west elongated hill. In order to obtain subsurface information that would be of aid in selecting the most suitable location for this deep cut through the hill, geologic and seismic studies were made in October 1949. The work was done as part of a cooperative program of the Massachusetts Department of Public Works and the United States Geological Survey.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5042B","usgsCitation":"May, J.E., and Linehan, D., 1950, Geologic interpretation of seismic data relocation Route 1, stations 150-155 in Danvers, Mass.: U.S. Geological Survey Open-File Report 50-42, 2 p., https://doi.org/10.3133/ofr5042B.","productDescription":"2 p.","numberOfPages":"5","costCenters":[],"links":[{"id":287171,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0042-B/report.pdf"},{"id":287172,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1950/0042-B/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Danvers","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.002683,42.540335 ], [ -71.002683,42.613052 ], [ -70.907922,42.613052 ], [ -70.907922,42.540335 ], [ -71.002683,42.540335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5375e204e4b010920bbded98","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":493542,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":493541,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70102219,"text":"ofr5043C - 1950 - Geologic interpretation of seismic data relocation of Route 2, Shelburne Falls in Shelburne, Mass.","interactions":[],"lastModifiedDate":"2014-04-25T07:45:33","indexId":"ofr5043C","displayToPublicDate":"1950-01-01T12:55:00","publicationYear":"1950","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":"50-43","chapter":"C","title":"Geologic interpretation of seismic data relocation of Route 2, Shelburne Falls in Shelburne, Mass.","docAbstract":"<p>In June 1945 a seismic study was made for the projected Halligan Avenue out, stations 364-374, Route 2 relocation in Shelburne, Mass. Nine profiles were run at this time and a report on this work was submitted by James E. Maynard and Rev. Daniel Linehan (file report of July 1945). As a result of a consultation with the State Engineers in August 1948, the proposed center-line of the road was relocated so as to be in a more favorable position. This new location is shown as alternate center-line number 2 on the plan of the seismic transverses. A cut approximately 1600 feet long is planned between stations 364 and 380. The approximate maximum depths of the cut are:</p>\n<br>\n<p>17 feet at station 365</p>\n<p>24 \" \" \" 368+50</p>\n<p>23 \" \" \" 371+50</p>\n<p>12 \" \" \" 372+50</p>\n<p>8 \" \" \" 375+00</p>\n<br>\n<p>Between stations 375+80 and 379+50 the depth of the cut gradually decreases from 8 feet to 0 feet. In order to obtain additional information on subsurface conditions at this site, especially along the segment of the relocated center-line where cuts are to be the deepest, a supplementary program of seismic studies was undertaken.</p>\n<br>\n<p>The work was done in October 1948 as a part of a cooperative program of the Massachusetts Department of Public Works and the United States Geological Survey.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boston, MA","doi":"10.3133/ofr5043C","usgsCitation":"May, J.E., and Linehan, D., 1950, Geologic interpretation of seismic data relocation of Route 2, Shelburne Falls in Shelburne, Mass.: U.S. Geological Survey Open-File Report 50-43, 4 p., https://doi.org/10.3133/ofr5043C.","productDescription":"4 p.","numberOfPages":"7","costCenters":[],"links":[{"id":286572,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":286571,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0043-C/report.pdf"}],"country":"United States","state":"Massachusetts","city":"Shelburne","otherGeospatial":"Shelburne Falls","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -72.740697,42.552891 ], [ -72.740697,42.645265 ], [ -72.632962,42.645265 ], [ -72.632962,42.552891 ], [ -72.740697,42.552891 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355943ee4b0120853e8bfae","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":492856,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":492855,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70101778,"text":"ofr5043B - 1950 - Geologic interpretation of seismic data relocation route 1: proposed cut at stations 127-135 in Danvers, Mass.","interactions":[],"lastModifiedDate":"2014-04-25T07:40:54","indexId":"ofr5043B","displayToPublicDate":"1950-01-01T11:55:00","publicationYear":"1950","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":"50-43","chapter":"B","title":"Geologic interpretation of seismic data relocation route 1: proposed cut at stations 127-135 in Danvers, Mass.","docAbstract":"The layout for the reconstruction of the Newburyport Turnpike (Route 1) proposed cit at stations 127-135, in Danvers, Mass., shows a deep cut through the western end of a hill between stations 127 and 135. Because of the depth of this cut seismic work was done at the site in September 1949. The work constitutes part of the cooperative program of the Department of Public Works and the United States Geological Survey.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5043B","collaboration":"Cooperative Geologic Project","usgsCitation":"May, J.E., and Linehan, D., 1950, Geologic interpretation of seismic data relocation route 1: proposed cut at stations 127-135 in Danvers, Mass.: U.S. Geological Survey Open-File Report 50-43, 2 p., https://doi.org/10.3133/ofr5043B.","productDescription":"2 p.","numberOfPages":"5","costCenters":[],"links":[{"id":286569,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":286568,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1950/0043-B/report.pdf"}],"country":"United States","state":"Massachusetts","city":"Danvers","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.002683,42.540335 ], [ -71.002683,42.613052 ], [ -70.907922,42.613052 ], [ -70.907922,42.540335 ], [ -71.002683,42.540335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355943ee4b0120853e8bfb0","contributors":{"authors":[{"text":"May, James E.","contributorId":85255,"corporation":false,"usgs":true,"family":"May","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":492752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":492751,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70217159,"text":"ofr49130 - 1950 - Geologic interpretation of seismic data grade separation, proposed Route 102 and Route 7 in Stockbridge, Massachusetts","interactions":[],"lastModifiedDate":"2021-01-26T20:40:42.462173","indexId":"ofr49130","displayToPublicDate":"1949-01-01T11:07:26","publicationYear":"1950","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":"49-130","title":"Geologic interpretation of seismic data grade separation, proposed Route 102 and Route 7 in Stockbridge, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr49130","usgsCitation":"Maynard, J.E., and Linehan, D., 1950, Geologic interpretation of seismic data grade separation, proposed Route 102 and Route 7 in Stockbridge, Massachusetts: U.S. Geological Survey Open-File Report 49-130, Report: 2 p.; 1 Plate: 8.86 x 7.06 inches, https://doi.org/10.3133/ofr49130.","productDescription":"Report: 2 p.; 1 Plate: 8.86 x 7.06 inches","costCenters":[],"links":[{"id":382622,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1949/0130/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382621,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1949/0130/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":382005,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1949/0130/report-thumb.jpg"}],"country":"United States","state":"Massachussetts","city":"Stockbridge","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Maynard, James E.","contributorId":247500,"corporation":false,"usgs":true,"family":"Maynard","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":true,"id":807788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Linehan, Daniel","contributorId":36998,"corporation":false,"usgs":true,"family":"Linehan","given":"Daniel","email":"","affiliations":[],"preferred":false,"id":807789,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}