No abstract available.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i001p00257-2","usgsCitation":"Goddard, E.N., 1936, Mode of intrusion of pre‐Cambrian granites in Central Boulder County, Colorado: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 257-257, https://doi.org/10.1029/TR017i001p00257-2.","productDescription":"1 p.","startPage":"257","endPage":"257","costCenters":[],"links":[{"id":378138,"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":"Goddard, Edwin N.","contributorId":103305,"corporation":false,"usgs":true,"family":"Goddard","given":"Edwin","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":797947,"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":70212921,"text":"70212921 - 1936 - A source of heat‐energy in crystallization of granodiorite magma, and some related problems of volcanism","interactions":[],"lastModifiedDate":"2020-09-01T19:48:06.368551","indexId":"70212921","displayToPublicDate":"1936-09-01T14:40:35","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":"A source of heat‐energy in crystallization of granodiorite magma, and some related problems of volcanism","docAbstract":"Evidence obtained from thin sections, polished sections, and chemical analyses of granodiorite porphyries from the Ouray District of Colorado show that during crystallization of the granodiorite magma a number of shifts occurred in the equilibrium between the oxides of iron. These changes are reflected in processes of mineralization associated with the magma. The geologic setting of the igneous bodies and episodes of fissuring connected with the mineralization indicate that relief of pressure was the primary cause of the shifts in equilibrium. The iron occurring in the crystallized products and in the residual magmatic liquids is changed from its low to its high state of oxidation and thus provides an internal and potential source of heat‐energy in crystallizing magmas. The transformation of the potential energy into neat is shown to occur both as an episodic process, interrupting the normal course of igneous metamorphism and mineralization near the magma bodies, and also as a more or less continuous process in the production of primary subalkaline magmas. The energy‐transformation is so controlled by crystal fractionation within the magma‐hood that it provides a mechanism by which magma bodies are enabled to rise in the Earth's crust by selective fusion of salic material.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i001p00236","usgsCitation":"Burbank, W.S., 1936, A source of heat‐energy in crystallization of granodiorite magma, and some related problems of volcanism: Eos, Transactions, American Geophysical Union, v. 17, no. 1, p. 236-255, https://doi.org/10.1029/TR017i001p00236.","productDescription":"20 p.","startPage":"236","endPage":"255","costCenters":[],"links":[{"id":378072,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Burbank, W. S.","contributorId":38197,"corporation":false,"usgs":true,"family":"Burbank","given":"W.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":797815,"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":70212915,"text":"70212915 - 1936 - Report of Committee on Glaciers, 1935–36","interactions":[],"lastModifiedDate":"2020-09-01T18:02:46.862774","indexId":"70212915","displayToPublicDate":"1936-09-01T13:00:14","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 Committee on Glaciers, 1935–36","docAbstract":"The membership of the Committee remains the same as stated in the Transactions of the 15th Annual Meeting, except that Kenneth N. Phillips has taken the place of Carl P. Richards, as representative of the Mazamas, of Portland, Oregon.
The Committee submits the following report on the variations of glaciers in the continental United States and Alaska for 1935 or, more precisely, for the 12‐month period from the autumn of 1934 to the autumn of 1935.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00286","usgsCitation":"Matthes, F.E., 1936, Report of Committee on Glaciers, 1935–36: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 286-294, https://doi.org/10.1029/TR017i002p00286.","productDescription":"9 p.","startPage":"286","endPage":"294","costCenters":[],"links":[{"id":378065,"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":"Matthes, Francois E.","contributorId":97963,"corporation":false,"usgs":true,"family":"Matthes","given":"Francois","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":797809,"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":70212912,"text":"70212912 - 1936 - Volcanological boron compounds","interactions":[],"lastModifiedDate":"2020-09-01T17:22:16.247538","indexId":"70212912","displayToPublicDate":"1936-09-01T12:18:46","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":"Volcanological boron compounds","docAbstract":"I wish to present what evidence we have as to the geochemistry of boron minerals as related to volcanological processes, or, in other words, what are the volcanological boron compounds?
Volcanological processes, considered only as they apply to this question, may be grouped for present convenience as follows: (1) Extrusion of volcanic rocks; (2) volcanic exhalations including fumaroles and solfataras; (3) hot springs.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i001p00234","usgsCitation":"American Geophysical Union, 1936, Volcanological boron compounds: Eos, Transactions, American Geophysical Union, v. 17, no. 1, p. 234-235, https://doi.org/10.1029/TR017i001p00234.","productDescription":"2 p.","startPage":"234","endPage":"235","costCenters":[],"links":[{"id":378062,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW"} ,{"id":70212910,"text":"70212910 - 1936 - Decline of artesian head in west‐central South Dakota","interactions":[],"lastModifiedDate":"2020-09-01T17:15:56.262022","indexId":"70212910","displayToPublicDate":"1936-09-01T12:02:45","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":"Decline of artesian head in west‐central South Dakota","docAbstract":"During the summer of 1935 the United States Geological Survey, in cooperation with the South Dakota Geological Survey, made a field‐study and report of the artesian conditions in the west‐central part of South Dakota. This study covered the semiarid plains‐region between the Black Hills uplift and the Missouri River, in which the Pierre shale is at or very near the surface. One of the important facts brought out by this study was the large decline in artesian head since development of the artesian basin began in the early 1890's.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00363","usgsCitation":"Robinson, T.W., 1936, Decline of artesian head in west‐central South Dakota: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 363-366, https://doi.org/10.1029/TR017i002p00363.","productDescription":"4 p.","startPage":"363","endPage":"366","costCenters":[],"links":[{"id":378061,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","otherGeospatial":"West Central South Dakota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.590087890625,\n 43.389081939117496\n ],\n [\n -99.228515625,\n 43.389081939117496\n ],\n [\n -99.228515625,\n 44.55916341529182\n ],\n [\n -103.590087890625,\n 44.55916341529182\n ],\n [\n -103.590087890625,\n 43.389081939117496\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"17","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Robinson, Thomas William","contributorId":31736,"corporation":false,"usgs":true,"family":"Robinson","given":"Thomas","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":797805,"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":70212905,"text":"70212905 - 1936 - Extension of normals by precipitation‐data and by comparison with another stream","interactions":[],"lastModifiedDate":"2020-09-01T16:42:07.361027","indexId":"70212905","displayToPublicDate":"1936-09-01T11:35:45","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":"Extension of normals by precipitation‐data and by comparison with another stream","docAbstract":"The factors affecting relationship between precipitation and consequent runoff are multitudinous and their interrelation is exceedingly complex. They vary widely from time to time and place to place. Basic data are meager and the weight to be given to any single factor is usually uncertain. Runoff‐characteristics of drainage‐areas within the same region will frequently be quite dissimilar. Under these circumstances no one should hope to answer conclusively paragraph V(a) of the questionnaire submitted January 4, 1935 by the Conference.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR017i002p00542","usgsCitation":"Parker, G.L., 1936, Extension of normals by precipitation‐data and by comparison with another stream: Eos, Transactions, American Geophysical Union, v. 17, no. 2, p. 542-543, https://doi.org/10.1029/TR017i002p00542.","productDescription":"2 p.","startPage":"542","endPage":"543","costCenters":[],"links":[{"id":378057,"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":"Parker, G. L.","contributorId":73566,"corporation":false,"usgs":true,"family":"Parker","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":797801,"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":70212789,"text":"70212789 - 1936 - Hydrothermal leaching in the Virginia mining district, New Mexico","interactions":[],"lastModifiedDate":"2020-08-27T20:01:05.226531","indexId":"70212789","displayToPublicDate":"1936-08-27T14:55:53","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Hydrothermal leaching in the Virginia mining district, New Mexico","docAbstract":"The tourmaline-copper deposits of the Virginia mining district, New Mexico, lie along veins that were plugged and reopened repeatedly during the process of mineral deposition. At some time between the second and third stages of deposition the solutions removed calcite, sericite, and chlorite from interstitial and included fragments of altered wall-rock in the veins and thereby produced honeycombed box-works of first- and second-stage minerals, chiefly specularite, quartz, and chalcopyrite, on the walls of which minerals of later stages were deposited. It is suggested that the leaching solutions may have been acid and that the leaching was done by the fresh solutions of the third stage before their acidity was neutralized through reactions along their channelways. A mechanism is suggested to account for their presence at places previously traversed by alkaline or neutral solutions.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.31.2.156","usgsCitation":"Lasky, S.G., 1936, Hydrothermal leaching in the Virginia mining district, New Mexico: Economic Geology, v. 31, no. 2, p. 156-169, https://doi.org/10.2113/gsecongeo.31.2.156.","productDescription":"14 p.","startPage":"156","endPage":"169","costCenters":[],"links":[{"id":377963,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Virginia Mining District","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -108.984375,\n 31.840232667909365\n ],\n [\n -108.577880859375,\n 31.840232667909365\n ],\n [\n -108.577880859375,\n 32.30106302536928\n ],\n [\n -108.984375,\n 32.30106302536928\n ],\n [\n -108.984375,\n 31.840232667909365\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"31","issue":"2","noUsgsAuthors":false,"publicationDate":"1936-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lasky, Samuel Grossman","contributorId":35380,"corporation":false,"usgs":true,"family":"Lasky","given":"Samuel","email":"","middleInitial":"Grossman","affiliations":[],"preferred":false,"id":797462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212788,"text":"70212788 - 1936 - Cinnabar deposits in southwestern Arkansas","interactions":[],"lastModifiedDate":"2020-08-27T19:51:25.914539","indexId":"70212788","displayToPublicDate":"1936-08-27T14:43:54","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Cinnabar deposits in southwestern Arkansas","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.31.3.314","usgsCitation":"Reed, J., 1936, Cinnabar deposits in southwestern Arkansas: Economic Geology, v. 31, p. 314-317, https://doi.org/10.2113/gsecongeo.31.3.314.","productDescription":"4 p.","startPage":"314","endPage":"317","costCenters":[],"links":[{"id":377962,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","noUsgsAuthors":false,"publicationDate":"1936-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Reed, John Calvin","contributorId":10769,"corporation":false,"usgs":true,"family":"Reed","given":"John Calvin","affiliations":[],"preferred":false,"id":797461,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212787,"text":"70212787 - 1936 - Nodular, orbicular, and banded chromite in northern California","interactions":[],"lastModifiedDate":"2020-08-27T19:37:06.426388","indexId":"70212787","displayToPublicDate":"1936-08-27T14:30:34","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Nodular, orbicular, and banded chromite in northern California","docAbstract":"IN I930 Mr. A. F. Duggleby gave me a specimen of orbicular chromite from the Octopus claim, in Siskiyou County, Calif., showing two generations of chromite, one older than the associated olivine and one younger. In November, I93I, I examined briefly a number of deposits in northern California, in search for chromite showing similar and related textures. Some of the more unusual and genetically significant occurrences are described in this paper.
Most of the chromite localities here described are in Siskiyou County, northern California. Localities I and 2 are in the Seiad Quadrangle, where a belt of chromite-bearing dunite, striking northwest, extends from McGuffy Creek, near Scott Bar, into Oregon. Other deposits are in southern Siskiyou, Shasta, and Trinity Counties.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.31.4.417","usgsCitation":"Johnston, W.D., 1936, Nodular, orbicular, and banded chromite in northern California: Economic Geology, v. 31, no. 4, p. 417-427, https://doi.org/10.2113/gsecongeo.31.4.417.","productDescription":"11 p.","startPage":"417","endPage":"427","costCenters":[],"links":[{"id":377961,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"4","noUsgsAuthors":false,"publicationDate":"1936-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Johnston, W. D. Jr.","contributorId":27193,"corporation":false,"usgs":true,"family":"Johnston","given":"W.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":797460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32473,"text":"32473 - 1936 - Suggestions on trapping coyotes and wolves in Alaska","interactions":[],"lastModifiedDate":"2014-07-24T11:52:44","indexId":"32473","displayToPublicDate":"1936-08-01T11:52:11","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"62","title":"Suggestions on trapping coyotes and wolves in Alaska","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Gubser, H.H., 1936, Suggestions on trapping coyotes and wolves in Alaska: Wildlife Leaflet 62, 6 p.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":290906,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb66e4b0824b2d178dfa","contributors":{"authors":[{"text":"Gubser, Harlan H.","contributorId":89451,"corporation":false,"usgs":true,"family":"Gubser","given":"Harlan","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":208562,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70212848,"text":"70212848 - 1936 - Copper deposits of the southern Appalachian region; discussion","interactions":[],"lastModifiedDate":"2020-08-31T15:59:29.297363","indexId":"70212848","displayToPublicDate":"1936-06-01T10:51:56","publicationYear":"1936","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Copper deposits of the southern Appalachian region; discussion","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.31.4.428","usgsCitation":"Ross, C.S., 1936, Copper deposits of the southern Appalachian region; discussion: Economic Geology, v. 31, no. 4, p. 428-432, https://doi.org/10.2113/gsecongeo.31.4.428.","productDescription":"5 p.","startPage":"428","endPage":"432","costCenters":[],"links":[{"id":378035,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Georgia, North Carolina, South Carolina, Tennessee, Virginia, West Virginia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -78.211669921875,\n 38.453588708941375\n ],\n [\n -80.936279296875,\n 37.75334401310656\n ],\n [\n -84.0234375,\n 36.09349937380574\n ],\n [\n -84.990234375,\n 35.003003395276714\n ],\n [\n -83.924560546875,\n 34.17090836352573\n ],\n [\n -82.342529296875,\n 34.93097858831627\n ],\n [\n -80.277099609375,\n 36.527294814546245\n ],\n [\n -77.71728515624999,\n 38.25543637637947\n ],\n [\n -78.211669921875,\n 38.453588708941375\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"31","issue":"4","noUsgsAuthors":false,"publicationDate":"1936-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Ross, Clarence Samuel","contributorId":28647,"corporation":false,"usgs":true,"family":"Ross","given":"Clarence","email":"","middleInitial":"Samuel","affiliations":[],"preferred":false,"id":797700,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":32463,"text":"32463 - 1936 - Raising guinea pigs","interactions":[],"lastModifiedDate":"2014-07-24T13:09:16","indexId":"32463","displayToPublicDate":"1936-04-01T13:08:31","publicationYear":"1936","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"52","title":"Raising guinea pigs","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","collaboration":"Prepared in Section of Fur Resources, Division of Wildlife Research.","usgsCitation":"U.S. Bureau of Biological Survey, 1936, Raising guinea pigs: Wildlife Leaflet 52, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290927,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb67e4b0824b2d178dfc","contributors":{"authors":[{"text":"U.S. Bureau of Biological Survey","contributorId":128079,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Biological Survey","id":529383,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}