Some years ago the senior author, in collaboration with Norah Dowell Stearns, undertook to make a monthly inventory of the water‐supply of the Pomperaug River Basin, in Connecticut, from a study of data obtained by A. J. Ellis from 1913 to 1916. For this purpose approximate determinations or estimates were made of the ground‐water runoff, that is, of the part of the daily discharge of the river that consisted of water derived from the zone of saturation by effluent seepage. The determinations or estimates were essentially based on the assumption that after a week of fair weather the storm‐water was all discharged and that until the next rain the runoff was essentially all ground‐water (U.S. Geol, Surv. Water‐Supply Paper 597, pp. 107–116 and pi. 19, 1929). In the discussion of the methods and results of this investigation, the following statement was made (Water‐Supply Paper 597, pp. 145–146):
“In this investigation the estimates of ground‐water runoff were based on the discharge of the Pomperaug at Bennetts Bridge—that is, on the discharge during the periods between rains, when there was virtually no direct runoff left in the stream‐system. Much better results could be obtained by basing the estimates on periods beginning as soon after rains as all of the direct runoff has reached the streams. With this method the ground‐water runoff during any particular day would be the total runoff minus the decrease in stream‐storage. The decrease in stream‐storage could be estimated by maintaining gages at several points on the trunk‐stream and on selected tributaries and making surveys of the stream‐system showing the approximate water‐areas of different parts of the system at different gage‐heights.”
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00415","usgsCitation":"Meinzer, O.E., Cady, R., Leggette, R., and Fishel, V., 1936, The channel‐storage method of determining effluent seepage: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 415-418, https://doi.org/10.1029/TR017i002p00415.","productDescription":"4 p.","startPage":"415","endPage":"418","costCenters":[],"links":[{"id":378141,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, Oscar E.","contributorId":83436,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":797950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cady, R.C.","contributorId":44905,"corporation":false,"usgs":true,"family":"Cady","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":797951,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":797952,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":797953,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70213000,"text":"70213000 - 1936 - Several methods of studying fluctuations of ground‐water levels","interactions":[],"lastModifiedDate":"2020-09-03T17:03:47.454516","indexId":"70213000","displayToPublicDate":"1936-09-03T11:58:47","publicationYear":"1936","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":"Several methods of studying fluctuations of ground‐water levels","docAbstract":"As a result of increased interest in ground‐water conditions in recent years, records of water‐levels in wells are now being collected in many places in the United States for the primary purpose of determining the relation of precipitation and other natural factors to fluctuations in water‐level. In the past, records of ground‐water levels have been collected chiefly in connection with intensive investigations in areas where the water‐levels were affected by artificial withdrawals and it has not been generally possible to correlate water‐level fluctuations closely with natural factors. It now appears probable that certain methods of studying water‐level fluctuations may be utilized advantageously in areas unaffected by heavy artificial withdrawals, but these methods generally do not yield satisfactory results in areas where there is considerable pumping or artesian flow. Three such methods are presented in this paper. The methods have not been given intensive study and their practical use is therefore not yet fully known. It is hoped that their application will be further investigated. Illustrations of the methods have been taken from records of ground‐water levels in the Platte River Valley, Nebraska, collected by the United States Geological Survey in cooperation with the Conservation and Survey Division of the University of Nebraska.
","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00400","usgsCitation":"Wenzel, L., 1936, Several methods of studying fluctuations of ground‐water levels: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 400-405, https://doi.org/10.1029/TR017i002p00400.","productDescription":"6 p.","startPage":"400","endPage":"405","costCenters":[],"links":[{"id":378140,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wenzel, Leland K.","contributorId":46077,"corporation":false,"usgs":true,"family":"Wenzel","given":"Leland K.","affiliations":[],"preferred":false,"id":797949,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212999,"text":"70212999 - 1936 - Introduction: Some problems relating to fluctuations of ground‐water level","interactions":[],"lastModifiedDate":"2020-09-03T16:51:13.584707","indexId":"70212999","displayToPublicDate":"1936-09-03T11:34:28","publicationYear":"1936","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":"Introduction: Some problems relating to fluctuations of ground‐water level","docAbstract":"When the program for the meeting of the Section of Hydrology a year ago was in preparation, it was suggested that a symposium be presented on the subject of the effects of the recent drought on ground‐water levels. The proposal was not carried out largely because at that time not enough accurate information on the subject was yet available. It has, however, seemed that this year a worth‐while group of papers could be developed on the broader subject of fluctuations of ground‐water levels.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00337","usgsCitation":"Thompson, D.G., 1936, Introduction: Some problems relating to fluctuations of ground‐water level: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 337-341, https://doi.org/10.1029/TR017i002p00337.","productDescription":"5 p.","startPage":"337","endPage":"341","costCenters":[],"links":[{"id":378139,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, D. G.","contributorId":95050,"corporation":false,"usgs":true,"family":"Thompson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":797948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212977,"text":"70212977 - 1936 - Suspended matter in several small streams","interactions":[],"lastModifiedDate":"2020-09-02T16:22:43.22912","indexId":"70212977","displayToPublicDate":"1936-09-02T11:11:29","publicationYear":"1936","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":"Suspended matter in several small streams","docAbstract":"The measurement of the loads of suspended matter carried past 34 gaging‐stations located on streams in eight regional projects of the Soil Conservation Service has required greater precision in the measurement of discharge and a more intensive program for the collection of samples of suspended matter than has been found necessary by the Geological Survey in making similar measurements on the larger streams on which measurements have been made in the past. It was found early in the work that much the greater part of the annual load of suspended matter was carried in a relatively few days of high water for almost all the streams on which measurements were made. In order that these loads might be determined with reasonable accuracy it was found necessary to collect samples every hour and occasionally every half‐hour on rising and rapidly changing stages during floods. Some floods occurring at night were missed in part or entirely because the resident observer did not realize that a flood was in progress. Twenty‐four‐hour sampling programs, together with the aid of electric‐alarm systems at some stations, have made possible the collection of an adequate number of samples during most floods.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00447","usgsCitation":"Love, S.K., 1936, Suspended matter in several small streams: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 447-452, https://doi.org/10.1029/TR017i002p00447.","productDescription":"6 p.","startPage":"447","endPage":"452","costCenters":[],"links":[{"id":378112,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Love, Samuel K.","contributorId":77845,"corporation":false,"usgs":true,"family":"Love","given":"Samuel","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":797879,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212920,"text":"70212920 - 1936 - Fluctuations of ground‐water levels in Utah","interactions":[],"lastModifiedDate":"2020-09-01T19:39:53.339645","indexId":"70212920","displayToPublicDate":"1936-09-01T14:35:39","publicationYear":"1936","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":"Fluctuations of ground‐water levels in Utah","docAbstract":"Long‐time continuous records of the fluctuations of ground‐water levels have been obtained at relatively few locations in the United States. Among the few available records for Utah that extend continuously over a period of a year or more are those made in the Jordan River and Ogden valleys by the United States Geological Survey in cooperation with Salt Lake City and Ogden. A few of the records of water‐levels, with records of stream‐flow and precipitation, are shown in Figure 1. Most of these records were begun during 1931 or 1932. A State‐wide program of well‐observations was begun during the summer of 1935 and is now in progress, the work being done by the Geological Survey in cooperation with the Utah State Engineer.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00378","usgsCitation":"Taylor, G., 1936, Fluctuations of ground‐water levels in Utah: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 378-382, https://doi.org/10.1029/TR017i002p00378.","productDescription":"5 p.","startPage":"378","endPage":"382","costCenters":[],"links":[{"id":378070,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":797814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212919,"text":"70212919 - 1936 - Movement of ground‐water","interactions":[],"lastModifiedDate":"2020-09-01T19:31:16.766349","indexId":"70212919","displayToPublicDate":"1936-09-01T14:20:38","publicationYear":"1936","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":"Movement of ground‐water","docAbstract":"The movement of water through formations having capillary openings is generally laminar and obeys Darcy's law, at least down to very low gradients. About 1000 samples tested in the laboratory of the United States Geological Survey have coefficients of permeability ranging from 0.001 to 90,000, indicating probable velocities ranging from a fraction of a foot to a few miles in a year. The Thiem field‐method gives promising results for determining permeability. Movement through sub‐capillary openings is important but poorly understood; molecular attraction of the water offers great resistance to movement or compression.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00478","usgsCitation":"Meinzer, O.E., 1936, Movement of ground‐water: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 478-479, https://doi.org/10.1029/TR017i002p00478.","productDescription":"2 p.","startPage":"478","endPage":"479","costCenters":[],"links":[{"id":378069,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":797813,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212918,"text":"70212918 - 1936 - Review of the work of W. J. McGee on ground‐water levels","interactions":[],"lastModifiedDate":"2020-09-01T19:16:38.83257","indexId":"70212918","displayToPublicDate":"1936-09-01T14:09:18","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3879,"text":"Eos, Earth and Space Science News","active":true,"publicationSubtype":{"id":10}},"title":"Review of the work of W. J. McGee on ground‐water levels","docAbstract":"W J McGee was a scientist of broad‐interests, large vision, and unbounded enthusiasm for science and its application to human welfare. He was one of the earliest champions of the conservation of our natural resources. He rose from humble origin, by rigorous self‐discipline, to outstanding national leadership. He was absorbed by zeal for service to mankind. His life had a heroic quality, as is well portrayed in the sympathetic and interesting memoir by F. H. Knowlton (Geol. Soc Amer. Bull., v. 24, pp. 18–29, 1913).
","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00386","usgsCitation":"Meinzer, O.E., 1936, Review of the work of W. J. McGee on ground‐water levels: Eos, Earth and Space Science News, v. 17, no. 2, p. 386-390, https://doi.org/10.1029/TR017i002p00386.","productDescription":"5 p.","startPage":"386","endPage":"390","costCenters":[],"links":[{"id":378068,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Meinzer, O. E.","contributorId":10020,"corporation":false,"usgs":true,"family":"Meinzer","given":"O.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":797812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212917,"text":"70212917 - 1936 - Long‐time records of ground‐water levels on Long Island, New York","interactions":[],"lastModifiedDate":"2020-09-01T19:01:42.655018","indexId":"70212917","displayToPublicDate":"1936-09-01T13:55:50","publicationYear":"1936","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":"Long‐time records of ground‐water levels on Long Island, New York","docAbstract":"As early at 1851 the need for information as to the position of the water‐table was recognized by workers on Long Island. In that year water‐level measurements were made in about 32 domestic wells in the southern part of Kings and Queens counties, New York (W. J. McAlpine, Report made to the water committee of the common council of the City of Brooklyn on supplying the City with water, p. 113, Brooklyn, I. Van Anden, 1852). Although specific water‐level data are given in this report, it has not been possible to determine the exact locations of the old wells that were measured, or the months during which measurements were made.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00341","usgsCitation":"Leggette, R., 1936, Long‐time records of ground‐water levels on Long Island, New York: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 341-344, https://doi.org/10.1029/TR017i002p00341.","productDescription":"4 p.","startPage":"341","endPage":"344","costCenters":[],"links":[{"id":378067,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":797811,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212916,"text":"70212916 - 1936 - Report of the committee on chemistry of natural waters, 1935–36","interactions":[],"lastModifiedDate":"2020-09-01T18:27:02.107194","indexId":"70212916","displayToPublicDate":"1936-09-01T13:21:15","publicationYear":"1936","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":"Report of the committee on chemistry of natural waters, 1935–36","docAbstract":"The membership of this Committee was not changed during the past year.
A publication has appeared during the year giving the analytical data assembled for and used as a basis for Bulletin 40 of the Department of Public Works, California. This new publication, printed as 40‐A, is entitled “Detailed analyses showing qualities of irrigation‐waters.” Analyses are given for both surface‐ and ground‐waters.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00335","usgsCitation":"Howard, C.S., 1936, Report of the committee on chemistry of natural waters, 1935–36: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 335-336, https://doi.org/10.1029/TR017i002p00335.","productDescription":"2 p.","startPage":"335","endPage":"336","costCenters":[],"links":[{"id":378066,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":797810,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212914,"text":"70212914 - 1936 - Report of the Committee on Underground Waters, 1935–36","interactions":[],"lastModifiedDate":"2020-09-01T17:53:58.343522","indexId":"70212914","displayToPublicDate":"1936-09-01T12:51:48","publicationYear":"1936","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":"Report of the Committee on Underground Waters, 1935–36","docAbstract":"Interest in problems of ground‐water hydrology continues unabated. As proof of this statement it is only necessary to state that of 57 papers listed for presentation at the present annual meeting of the Section of Hydrology and of the Pacific Coast meeting of the Section on January 31 and February 1, 26 papers, or 45 per cent, related to some phase of ground‐water hydrology. In this connection, attention may be called especially to the papers on ground‐water presented at the Pacific Coast meeting and published in the present Transactions.
At this early point in his report, the Chairman should state that at about the time he usually takes the preliminary steps in compiling data for his annual report, his official duties somewhat unexpectedly took him to field‐work in New Mexico and Colorado. Without the usual office facilities it has not been possible for him to make all desired contacts, and the present report of current ground‐water studies is necessarily somewhat incomplete.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00326","usgsCitation":"Thompson, D., 1936, Report of the Committee on Underground Waters, 1935–36: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 326-329, https://doi.org/10.1029/TR017i002p00326.","productDescription":"4 p.","startPage":"326","endPage":"329","costCenters":[],"links":[{"id":378064,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, David G.","contributorId":8443,"corporation":false,"usgs":true,"family":"Thompson","given":"David G.","affiliations":[],"preferred":false,"id":797808,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212913,"text":"70212913 - 1936 - The relation of the drought of 1934 to ground‐water supplies in the James and Sheyenne River‐Basins of North And South Dakota","interactions":[],"lastModifiedDate":"2020-09-01T17:50:24.555566","indexId":"70212913","displayToPublicDate":"1936-09-01T12:44:06","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The relation of the drought of 1934 to ground‐water supplies in the James and Sheyenne River‐Basins of North And South Dakota","docAbstract":"The water‐shortage caused by the drought of 1934 in the Middle West drew nation‐wide attention to the lack of adequate information on the relation of precipitation to water‐supplies. The shortage was especially severe in the Dakotas because precipitation had been below normal in North Dakota since 1930 and in South Dakota since 1931. Many wells and springs failed, numerous streams ceased to flow, and levels of water in lakes and ponds declined until some of them became completely dry. Many of the inhabitants felt great concern lest the water‐supplies of the area had been permanently depleted.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00366","usgsCitation":"Sayre, A., 1936, The relation of the drought of 1934 to ground‐water supplies in the James and Sheyenne River‐Basins of North And South Dakota: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 366-370, https://doi.org/10.1029/TR017i002p00366.","productDescription":"5 p.","startPage":"366","endPage":"370","costCenters":[],"links":[{"id":378063,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":797807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212909,"text":"70212909 - 1936 - United States Geological Survey records of suspended and dissolved matter in surface‐waters","interactions":[],"lastModifiedDate":"2020-09-01T17:02:06.154396","indexId":"70212909","displayToPublicDate":"1936-09-01T11:59:21","publicationYear":"1936","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":"United States Geological Survey records of suspended and dissolved matter in surface‐waters","docAbstract":"Although the widest‐known and most conspicuous task of the United States Geological Survey with reference to surface‐waters has been the measurement of discharge, attention has always been given to the suspended and dissolved matter carried in them. From 1902 to 1909 the Survey published about 20 reports on the quality of surface‐waters. These reports dealt largely with stream‐pollution and its prevention, subjects that have not been included in the work of the Geological Survey since the Public Health Service began investigations of them in 1913.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00444","usgsCitation":"Grover, N., 1936, United States Geological Survey records of suspended and dissolved matter in surface‐waters: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 444-446, https://doi.org/10.1029/TR017i002p00444.","productDescription":"3 p.","startPage":"444","endPage":"446","costCenters":[],"links":[{"id":378060,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Grover, N.C.","contributorId":65453,"corporation":false,"usgs":true,"family":"Grover","given":"N.C.","email":"","affiliations":[],"preferred":false,"id":797804,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212908,"text":"70212908 - 1936 - Suspended matter in the Colorado River, 1925–1935","interactions":[],"lastModifiedDate":"2020-09-01T16:56:32.719768","indexId":"70212908","displayToPublicDate":"1936-09-01T11:54:01","publicationYear":"1936","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":"Suspended matter in the Colorado River, 1925–1935","docAbstract":"The rugged topography of a great part of the Colorado River Basin is a significant factor in determining the quantity of water and suspended matter carried by the River. The mountainous regions of Colorado and Wyoming contribute a large part of the flow of the River, whereas the central part of the Basin, cut by deep gorges and canyons, contributes a large part of the suspended matter carried by the River.
The discharge of the Colorado River as measured near Cisco, Utah, with a drainage‐area of 24,100 square miles is slightly greater than the discharge of the largest tributary, the Green River, measured near Greenriver, Utah, with a drainage‐area of 40,600 square miles. The Green, however, carries a considerably larger load of suspended matter. Two other tributaries, the San Juan and Little Colorado rivers, each with a drainage‐area of about 25,000 square miles, carry large loads of suspended matter in proportion to their discharge. For example, the Little Colorado River in the summer of 1931 contributed less than 10 per cent of the flow of the main river at Grand Canyon, but the Little Colorado carried about 10,000,000 tons of suspended matter during this period and the main river had about 25,000,000 tons for the same period.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00446","usgsCitation":"Howard, C.S., 1936, Suspended matter in the Colorado River, 1925–1935: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 446-447, https://doi.org/10.1029/TR017i002p00446.","productDescription":"2 p.","startPage":"446","endPage":"447","costCenters":[],"links":[{"id":378059,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":797803,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212906,"text":"70212906 - 1936 - An interpretation of water‐table fluctuations at four wells in Southern California","interactions":[],"lastModifiedDate":"2020-09-01T16:52:57.644276","indexId":"70212906","displayToPublicDate":"1936-09-01T11:48:52","publicationYear":"1936","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":"An interpretation of water‐table fluctuations at four wells in Southern California","docAbstract":"The urban and agricultural development in most areas of southern California have depended on the underground water‐resources of which more and more use has been made. It has been estimated that in the South Coastal Basin during the summer 90 per cent of the water‐supply for irrigation and other purposes developed locally is obtained from underground sources [see 1 of “References” at end of paper]. Because of the economic importance of this resource, measurements of the depth of water‐level are made regularly at hundreds of wells in the area to obtain knowledge of the draw‐down and replenishment.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00371","usgsCitation":"Ebert, F.C., 1936, An interpretation of water‐table fluctuations at four wells in Southern California: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 371-378, https://doi.org/10.1029/TR017i002p00371.","productDescription":"8 p.","startPage":"371","endPage":"378","costCenters":[],"links":[{"id":378058,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Ebert, Fred Charles","contributorId":36114,"corporation":false,"usgs":true,"family":"Ebert","given":"Fred","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":797802,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212904,"text":"70212904 - 1936 - The recovery of ground‐water levels in Nebraska in 1935","interactions":[],"lastModifiedDate":"2020-09-01T16:34:50.863548","indexId":"70212904","displayToPublicDate":"1936-09-01T11:22:30","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"The recovery of ground‐water levels in Nebraska in 1935","docAbstract":"A program of water‐level measurements in about 350 wells scattered throughout Nebraska was begun in 1934 by the United States Geological Survey in cooperation with the Conservation and Survey Division of the University of Nebraska (see L. K. Wenzel, A state‐wide program of periodic measurements of ground‐water level in Nebraska, Trans. Amer. Geophys. Union, 16th annual meeting, pp. 495–498, 1935). Included in this program were about 60 wells in the Platte River Valley on which periodic measurements were started in 1930. Observations on the 350 wells were continued in 1935 at about monthly intervals and the measurements collected are now being prepared for publication as a paper of the Nebraska Geological Survey.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00370","usgsCitation":"Wenzel, L., 1936, The recovery of ground‐water levels in Nebraska in 1935: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 370-371, https://doi.org/10.1029/TR017i002p00370.","productDescription":"2 p.","startPage":"370","endPage":"371","costCenters":[],"links":[{"id":378056,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Wenzel, Leland K.","contributorId":46077,"corporation":false,"usgs":true,"family":"Wenzel","given":"Leland K.","affiliations":[],"preferred":false,"id":797800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212790,"text":"70212790 - 1936 - Dissolved mineral matter in surface‐waters","interactions":[],"lastModifiedDate":"2020-08-27T20:14:50.548999","indexId":"70212790","displayToPublicDate":"1936-08-27T15:13:50","publicationYear":"1936","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":"Dissolved mineral matter in surface‐waters","docAbstract":"The only unpublished comprehensive Geological Survey records of dissolved matter in surface‐waters are the results obtained in the study of the Colorado River and its tributaries since 1930. The records are mainly analyses of 10‐day composites of daily samples, although there are several analyses of spot‐samples from some streams in the basin and about 4000 single determinations of chloride or sulphate in daily samples.
The need for a large number of analyses is shown by the fact that during the period 1925–35 the quantity of dissolved solids in 10‐day composites from the Colorado River at Grand Canyon ranged from 226 parts per million for June 11–20, 1929, to 1889 parts per million for. September 21–30, 1934. A series of analyses covering a whole year might be misleading. The weighted averages for the different years ranged from 491 parts per million for the year ending September 30, 1928, to 960 for the year ending September 30, 1934.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00452","usgsCitation":"Collins, W.D., 1936, Dissolved mineral matter in surface‐waters: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 252-253, https://doi.org/10.1029/TR017i002p00452.","productDescription":"2 p.","startPage":"252","endPage":"253","costCenters":[],"links":[{"id":377964,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Collins, W. D.","contributorId":37713,"corporation":false,"usgs":true,"family":"Collins","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":797463,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010856,"text":"70010856 - 1936 - Volumetric determination of sulfate in water: The barium chromate method","interactions":[],"lastModifiedDate":"2020-12-10T20:36:17.388539","indexId":"70010856","displayToPublicDate":"1936-01-01T00:00:00","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1982,"text":"Industrial And Engineering Chemistry Analytical Edition","active":true,"publicationSubtype":{"id":10}},"title":"Volumetric determination of sulfate in water: The barium chromate method","docAbstract":"No abstract available.
","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac50101a015","usgsCitation":"Foster, M., 1936, Volumetric determination of sulfate in water: The barium chromate method: Industrial And Engineering Chemistry Analytical Edition, v. 8, no. 3, p. 195-196, https://doi.org/10.1021/ac50101a015.","productDescription":"2 p.","startPage":"195","endPage":"196","numberOfPages":"2","costCenters":[],"links":[{"id":218816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505bc368e4b08c986b32b168","contributors":{"authors":[{"text":"Foster, Margaret D.","contributorId":97958,"corporation":false,"usgs":true,"family":"Foster","given":"Margaret D.","affiliations":[],"preferred":false,"id":359793,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70006901,"text":"70006901 - 1935 - The protozoan diseases of hatchery fish","interactions":[],"lastModifiedDate":"2015-12-21T08:02:42","indexId":"70006901","displayToPublicDate":"2012-01-01T12:21:54","publicationYear":"1935","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"The protozoan diseases of hatchery fish","docAbstract":"Following the somewhat bleak picture painted in the consideration of the bacterial diseases of hatchery fish in the last number of The Progressive Fish Culturist, it is a relief to turn to another large group of fish diseases caused by small, single-celled parasitic animals known as the protozoa. To the hatcheryman, the protozoan diseases of fish are just as important as the bacterial diseases for they are equally destructive if allowed to run unchecked. The protozoan diseases are just as common as those caused by bacteria, particularly at those hatcheries which depend upon lakes or streams for their water supplies. However, a very cheery point of difference exists between these two groups of diseases—the protozoan diseases are easier to recognize and, for the most part, they are exceedingly easy to eradicate. To the hatcheryman who has struggled day and night for weeks in an attempt to combat an epidemic wherein he is rewarded immediately by the satisfying sight of a complete recovery of his infected fish as the direct result of his labors.","language":"English","publisher":"Taylor & Francis","publisherLocation":"Philadelphia, PA","doi":"10.1577/1548-8640(1935)26[1:TPDOHF]2.0.CO;2","usgsCitation":"Fish, F.F., 1935, The protozoan diseases of hatchery fish: Progressive Fish-Culturist, v. 2, no. 6, p. 1-4, https://doi.org/10.1577/1548-8640(1935)26[1:TPDOHF]2.0.CO;2.","productDescription":"4 p.","startPage":"1","endPage":"4","numberOfPages":"4","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":258353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":258341,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1577/1548-8640(1935)26[1:TPDOHF]2.0.CO;2","linkFileType":{"id":5,"text":"html"}}],"volume":"2","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baed7e4b08c986b32439e","contributors":{"authors":[{"text":"Fish, F. F.","contributorId":82572,"corporation":false,"usgs":true,"family":"Fish","given":"F.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":355430,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70175578,"text":"70175578 - 1935 - Ground water in the southern High Plains","interactions":[],"lastModifiedDate":"2016-08-17T11:20:40","indexId":"70175578","displayToPublicDate":"2000-07-12T10:30:00","publicationYear":"1935","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Ground water in the southern High Plains","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lawrence, KS","usgsCitation":"Theis, C., Burleigh, H.P., and Waite, H., 1935, Ground water in the southern High Plains, Report: 4 p.","productDescription":"Report: 4 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326647,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58acfe4b03bcb0104bbab","contributors":{"authors":[{"text":"Theis, C.V.","contributorId":101641,"corporation":false,"usgs":true,"family":"Theis","given":"C.V.","email":"","affiliations":[],"preferred":false,"id":645745,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burleigh, H. P.","contributorId":173752,"corporation":false,"usgs":false,"family":"Burleigh","given":"H.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":645746,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waite, H.A.","contributorId":58336,"corporation":false,"usgs":true,"family":"Waite","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":645747,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":478,"text":"wsp742 - 1935 - Surface water supply of the United States, 1933, Part II, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp742","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"742","title":"Surface water supply of the United States, 1933, Part II, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp742","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1933, Part II, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 742, vii, 206 p. ;23 cm., https://doi.org/10.3133/wsp742.","productDescription":"vii, 206 p. ;23 cm.","costCenters":[],"links":[{"id":137420,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0742/report-thumb.jpg"},{"id":25041,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0742/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697822","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527450,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4607,"text":"wsp748 - 1935 - Surface water supply of the United States, 1933, Part VIII, Western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"wsp748","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"748","title":"Surface water supply of the United States, 1933, Part VIII, Western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp748","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1933, Part VIII, Western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 748, vi, 180 p. ;23 cm., https://doi.org/10.3133/wsp748.","productDescription":"vi, 180 p. ;23 cm.","costCenters":[],"links":[{"id":139595,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0748/report-thumb.jpg"},{"id":31664,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0748/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6977e2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1592,"text":"wsp751 - 1935 - Surface water supply of the United States, 1933 : Part 11. Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"751","title":"Surface water supply of the United States, 1933 : Part 11. Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp751","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1933 : Part 11. Pacific slope basins in California: U.S. Geological Survey Water Supply Paper 751, xi, 376 p. :ill. ;23 cm., https://doi.org/10.3133/wsp751.","productDescription":"xi, 376 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0751/report-thumb.jpg"},{"id":26657,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0751/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697839","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527955,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1598,"text":"wsp769 - 1935 - Surface water supply of the United States, 1934 : Part 12. North Pacific slope basins : C. Pacific slope basins in Oregon and Lower Columbia River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp769","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"769","title":"Surface water supply of the United States, 1934 : Part 12. North Pacific slope basins : C. Pacific slope basins in Oregon and Lower Columbia River Basin","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp769","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1934 : Part 12. North Pacific slope basins : C. Pacific slope basins in Oregon and Lower Columbia River Basin: U.S. Geological Survey Water Supply Paper 769, vi, 165 p. :ill. ;23 cm., https://doi.org/10.3133/wsp769.","productDescription":"vi, 165 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0769/report-thumb.jpg"},{"id":26663,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0769/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6961ef","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527961,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":480,"text":"wsp745 - 1935 - Surface water supply of the United States, 1933, Part V, Hudson Bay and upper Mississippi River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp745","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"745","title":"Surface water supply of the United States, 1933, Part V, Hudson Bay and upper Mississippi River basin","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp745","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1935, Surface water supply of the United States, 1933, Part V, Hudson Bay and upper Mississippi River basin: U.S. Geological Survey Water Supply Paper 745, vii, 220 p. ;23 cm., https://doi.org/10.3133/wsp745.","productDescription":"vii, 220 p. ;23 cm.","costCenters":[],"links":[{"id":136642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0745/report-thumb.jpg"},{"id":25043,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0745/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697813","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527452,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":487,"text":"wsp761 - 1935 - Surface water supply of the United States, 1934, Part VI, Missouri River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp761","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1935","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":"761","title":"Surface water supply of the United States, 1934, Part VI, Missouri River basin","language":"ENGLISH","publisher":"U.S. Govt. 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