This bulletin, which for convenience is to be published in eight parts, contains the results of all transit traverse* done In Missouri through 1937 by the Geological Survey, United States Department of the Interior, including those heretofore published. (See page X.) Each of the parts deals with one of eight sections into which the State has been divided for this purpose and which have been designated northeastern, northwestern, southeastern, southwestern, central, east-central, south-central, and west-central Missouri. In each part descriptions of the points for which geodetic positions have been determined are listed according to the quadrangles in which the points occur. Results of transit traverse other than that done by the Geological Survey have not been included.
Southeastern Missouri, as the term is used in this bulletin and as the subject of part 1 of the bulletin, is that section of the State lying south of latitude 38°00' and east of longitude 91°15'.
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A few miscellaneous measurements of streams In central Texas, between Del Rio and Austin, were made, by C. C. Babb of the Geological Survey in 1894, 1895, and 1896. In 1897 T. U. Taylor, professor of civil engineering at the University of Texas, at Austin, began a systematic study for the Geological Survey of as many of the principal streams as the limited funds would permit. In the same year the American section of the International Water Commission began collecting records of flow of the Rio Grande in Texas. Records for the Rio Grande and some of its tributaries from 1897 to 1913, inclusive, collected by that commission under the immediate direction of W. W. Follett, United States consulting engineer, are contained in Geological Survey Water-supply Paper 358. It was not until 1915, when the State Legislature appropriated funds for stream measurement investigations by the Texas Board of Water Engineers, that a substantial beginning toward the systematic collection of stream-flow records was made. The work has been continued and enlarged gradually so that records have been collected at about 230 stations in Texas. In September 1937 86 gaging stations were being maintained in Texas by the Geological Survey and the cooperating agencies. Many miscellaneous discharge measurements have been made at other points. The records collected by the Geological Survey from 1889 to 1937 are now scattered through more than 50 reports, many of which are out of print.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp850","usgsCitation":"Ellsworth, C., 1939, Summary of records of surface waters of Texas, 1898-1937: U.S. Geological Survey Water Supply Paper 850, vi, 154 p., https://doi.org/10.3133/wsp850.","productDescription":"vi, 154 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":26355,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0850/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0850/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698c7a","contributors":{"authors":[{"text":"Ellsworth, Clarence E.","contributorId":54575,"corporation":false,"usgs":true,"family":"Ellsworth","given":"Clarence E.","affiliations":[],"preferred":false,"id":143552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":42724,"text":"ofr391 - 1939 - Preliminary structure contour map of the Dunkirk-Chester region, Toole and Liberty Counties, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:05:03","indexId":"ofr391","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1939","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":"39-1","title":"Preliminary structure contour map of the Dunkirk-Chester region, Toole and Liberty Counties, Montana","language":"ENGLISH","doi":"10.3133/ofr391","usgsCitation":"Erdmann, C.E., 1939, Preliminary structure contour map of the Dunkirk-Chester region, Toole and Liberty Counties, Montana: U.S. Geological Survey Open-File Report 39-1, 1 map ;31 x 46 cm., on sheet 42 x 68 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/ofr391.","productDescription":"1 map ;31 x 46 cm., on sheet 42 x 68 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":135501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":98934,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1939/0001/plate-1.pdf","size":"14722","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aace4b07f02db66a585","contributors":{"authors":[{"text":"Erdmann, Charles Edgar","contributorId":16388,"corporation":false,"usgs":true,"family":"Erdmann","given":"Charles","email":"","middleInitial":"Edgar","affiliations":[],"preferred":false,"id":227004,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2270,"text":"wsp836D - 1939 - Ground water in the United States, a summary of ground-water conditions and resources, utilization of water from wells and springs, methods of scientific investigation, and literature relating to the subject","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp836D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1939","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":"836","chapter":"D","title":"Ground water in the United States, a summary of ground-water conditions and resources, utilization of water from wells and springs, methods of scientific investigation, and literature relating to the subject","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp836D","usgsCitation":"Meinzer, O.E., 1939, Ground water in the United States, a summary of ground-water conditions and resources, utilization of water from wells and springs, methods of scientific investigation, and literature relating to the subject: U.S. Geological Survey Water Supply Paper 836, v, p. 157-232 :ill., maps ;24 cm., https://doi.org/10.3133/wsp836D.","productDescription":"v, p. 157-232 :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137599,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0836d/report-thumb.jpg"},{"id":28059,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0836d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d816","contributors":{"authors":[{"text":"Meinzer, O. 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Four general methods of detecting salt-water leaks have been used. In the pumping method, samples taken at measured time intervals while the well is being pumped show by their progressive change in salinity if salt water is being drawn in. In the velocity method, which is suitable for use only in artesian wells, a current meter lowered into the well indicates the location of possible salt water leaks by determining the levels at which there are changes in the rate of upward movement of the water. In the sampler method a container lowered into the well brings up a sample from any depth desired for analysis of its chloride content. The electric conductivity method, for which special apparatus was designed, has been used successfully in the Winter Garden area and Kleberg County, Tex., and in Sarasota County, Fla. The procedure in this method was to lower a pair of insulated electrodes into the well and measure the resistance of the water between them with the Wheatstone bridge or, in waters low in chloride, to apply a direct current of low voltage and measure the current flowing between .the electrodes by means of a milliammeter. The installments showed a marked increase in the conductivity of the water as the electrodes passed from fresh to salt water in the well, leaving no doubt as to the location of the leaks.
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