Ground‐water dams are recognized in the unconsolidated sediments of two intermontane valleys in southwestern Utah. Parowan Valley is about 30 miles long and has a general northeasterly trend; Cedar City Valley lies west and south of Parowan Valley, is somewhat larger, and has a more nearly north‐south trend. Great accumulations of boulders, gravel, sand, and clay have been brought into both valleys by the streams that drain the surrounding highlands, and the valleys have become topographic basins whose lowest parts are occupied by lakes or dry alkali flats, rimmed on all sides with the alluvial fans and cones that have been formed by the streams tributary to the valleys. Ground‐water occurs principally in these unconsolidated sediments, and in both valleys a large proportion of the irrigated lands is dependent upon water pumped from wells.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00775","usgsCitation":"Thomas, H.E., 1941, Ground‐water dams created by faulting of alluvial sediments in the hurricane fault‐zone, Utah: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 775-778, https://doi.org/10.1029/TR022i003p00775.","productDescription":"4 p.","startPage":"775","endPage":"778","costCenters":[],"links":[{"id":378469,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.0380859375,\n 36.98500309285596\n ],\n [\n -112.35717773437499,\n 36.98500309285596\n ],\n [\n -112.35717773437499,\n 38.603993275591684\n ],\n [\n -114.0380859375,\n 38.603993275591684\n ],\n [\n -114.0380859375,\n 36.98500309285596\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":798932,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213274,"text":"70213274 - 1941 - Report of committee on glaciers, 1940–41","interactions":[],"lastModifiedDate":"2020-09-17T13:42:09.991041","indexId":"70213274","displayToPublicDate":"1941-09-16T13:58:51","publicationYear":"1941","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, 1940–41","docAbstract":"The personnel of the Committee is now as follows: Harry Fielding Reid, Professor Emeritus of Geology, Johns Hopkins University, 608 Cathedral Street, Baltimore, Maryland; William H. Hobbs, Professor Emeritus of Geology, University of Michigan, Ann Arbor, Michigan; Lawrence Martin, Chief of the Division of Maps, Library of Congress, Washington, D.C.; J. E. Church, Professor of Meteorology, Agricultural Experiment Station, University of Nevada, Reno, Nevada; Wm. Osgood Field, Jr., Explorer, 18 West Twelfth Street, New York, New York; Oliver Kehrlein, Chairman, Committee on Glacier Studies of Sierra Club, 1050 Mills Tower, 220 Bush Street, San Francisco, California; Kenneth N. Phillips, Associate Hydraulic Engineer, Water Resources Branch, United States Geological Survey, Chairman, Research Committee of the Mazamas, 606 Post‐Office Building, Portland, Oregon; William S. Cooper, Professor of Botany, University of Minnesota, Minneapolis, Minnesota; Gerald Fitzgerald, Senior Topographic Engineer, Alaska Branch, United States Geological Survey, Washington, D.C.; Laurence M. Gould, Professor of Geology, Carleton College, Northfield, Minnesota; Dr. Max Demorest, Department of Geology, Yale University, New Haven, Connecticut; François E. Matthes (Chairman), Senior Geologist, Section of Glacial Geology, United States Geological Survey, Washington, D.C.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p01006","usgsCitation":"Matthes, F.E., 1941, Report of committee on glaciers, 1940–41: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 1006-1011, https://doi.org/10.1029/TR022i003p01006.","productDescription":"6 p.","startPage":"1006","endPage":"1011","costCenters":[],"links":[{"id":378468,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","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":798931,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213273,"text":"70213273 - 1941 - Report of committee on runoff, 1940–41","interactions":[],"lastModifiedDate":"2021-04-06T15:54:18.543956","indexId":"70213273","displayToPublicDate":"1941-09-16T13:33:35","publicationYear":"1941","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 runoff, 1940–41","docAbstract":"The Committee members are the same as last year, namely: H. K. Barrows; Merrill Bernard; E. S. Cullings; R. S. Goodridge; G. A. Hathaway; Joseph Jacobs; F. T. Havis; H. S. Riesbol; Waldo E. Smith; F. F. Snyder; and H. G. Wilm.
During the year one addition was made, namely, AURELIO BENASSINI of Mexico City and associated with the Mexican Government. One of Mr. Benassini's associates, Mr. Quintero, was appointed on Mr. Bernard's Rainfall Committee, and in view of the fact that we have common hydrologic problems with Mexico, it seems desirable to have representatives of the Mexican Government on both the Rainfall and the Runoff Committees.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p01014","usgsCitation":"Hoyt, W.G., 1941, Report of committee on runoff, 1940–41: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 1014-1015, https://doi.org/10.1029/TR022i003p01014.","productDescription":"2 p.","startPage":"1014","endPage":"1015","costCenters":[],"links":[{"id":378464,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hoyt, W. G.","contributorId":38547,"corporation":false,"usgs":true,"family":"Hoyt","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":798927,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213271,"text":"70213271 - 1941 - The possibility of seiemic measurement of the rotation of the Earth's core","interactions":[],"lastModifiedDate":"2020-09-16T18:32:37.577055","indexId":"70213271","displayToPublicDate":"1941-09-16T13:22:41","publicationYear":"1941","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 possibility of seiemic measurement of the rotation of the Earth's core","docAbstract":"The calculations of Inglis show that the rate of transfer of angular momentum to the Earth's (liquid) core may be small enough to permit the axis of rotation of the core to lag about 2° behind that of the rock‐mantle in the precessional motion of the Earth. The travel‐time of P′ would be altered by about one‐fifth of a second, which is too small to be detected by a single observation made with even the best instrument, but can be brought out statistically when we have accumulated about three thousand clear measurements, on sensitive vertical‐component seismographs, of the P′‐waves from accurately located earthquakes.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i002p00387","usgsCitation":"Blake, A., 1941, The possibility of seiemic measurement of the rotation of the Earth's core: Eos, Transactions, American Geophysical Union, v. 22, no. 2, p. 387-392, https://doi.org/10.1029/TR022i002p00387.","productDescription":"6 p.","startPage":"387","endPage":"392","costCenters":[],"links":[{"id":378463,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Blake, Archie","contributorId":240766,"corporation":false,"usgs":false,"family":"Blake","given":"Archie","email":"","affiliations":[],"preferred":false,"id":798926,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213270,"text":"70213270 - 1941 - Factors producing a nine‐year decline in ground‐water levels in Scott County, Kansas","interactions":[],"lastModifiedDate":"2020-09-17T13:48:51.812102","indexId":"70213270","displayToPublicDate":"1941-09-16T13:18:28","publicationYear":"1941","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":"Factors producing a nine‐year decline in ground‐water levels in Scott County, Kansas","docAbstract":"In the south‐central part of Scott County, Kansas, there is an area of shallow water‐table in which the ground‐water levels have declined steadily since 1932 (Fig. 1). In this area water has been withdrawn from wells for irrigation in increasing amounts during the last decade and the precipitation has been considerably below normal for the last seven years. Thus, the problem of interpreting the downward trend of the water‐table has been complicated by the presence of two competent causes.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00772","usgsCitation":"Waite, H.A., 1941, Factors producing a nine‐year decline in ground‐water levels in Scott County, Kansas: Eos, Transactions, American Geophysical Union, v. 22, no. 3, p. 772-775, https://doi.org/10.1029/TR022i003p00772.","productDescription":"4 p.","startPage":"772","endPage":"775","costCenters":[],"links":[{"id":378462,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas","county":"Scott County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-100.6882,38.7037],[-100.6845,38.2627],[-101.1037,38.2636],[-101.1254,38.264],[-101.1293,38.7001],[-100.8168,38.7032],[-100.6882,38.7037]]]},\"properties\":{\"name\":\"Scott\",\"state\":\"KS\"}}]}","volume":"22","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Waite, H. A.","contributorId":173753,"corporation":false,"usgs":false,"family":"Waite","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":798925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213269,"text":"70213269 - 1941 - Factors influencing runoff during the flood of December, 1937, in northern California","interactions":[],"lastModifiedDate":"2020-09-17T13:50:56.499789","indexId":"70213269","displayToPublicDate":"1941-09-16T12:28:00","publicationYear":"1941","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":"Factors influencing runoff during the flood of December, 1937, in northern California","docAbstract":"Engineers and hydrologists engaged on flood‐problems throughout much of the United States east of the Rocky Mountains must deal to a considerable extent with wide‐spread storms covering thousands of square miles. The gradations of meteorologic conditions as regard both area and time are relatively homogeneous during such storm‐events and are affected but moderately by orographical influences. Under such conditions similar storm‐characteristics prevail over vast areas. True, precipitation decreases toward the boundaries of such major storm‐areas, and locally precipitation‐rates may greatly exceed the average. Often, however, drainage‐basin after drainage‐basin will yield comparable depths of flood‐runoff. The storms of March, 1936, which resulted in the simultaneous occurrence of floods throughout all of the northeastern part of the United States from Ohio and Virginia to Maine and the storm of January, 1937, which embraced all of the 200,000 square miles comprising the Ohio River drainage are typical of major Eastern disturbances. The storm of December, 1937, in the Sacramento and San Joaquin valleys is used herein to illustrate what may be called a typical major California disturbance, and it is this storm and resulting flood that I wish to consider in some detail and also to make such comparisons and contrasts with Eastern floods as seem to be of general interest.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i001p00124","usgsCitation":"Boyt, W., 1941, Factors influencing runoff during the flood of December, 1937, in northern California: Eos, Transactions, American Geophysical Union, v. 22, no. 1, p. 124-129, https://doi.org/10.1029/TR022i001p00124.","productDescription":"6 p.","startPage":"124","endPage":"129","costCenters":[],"links":[{"id":378461,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -124.134521484375,\n 37.47485808497102\n ],\n [\n -120.498046875,\n 37.47485808497102\n ],\n [\n -120.498046875,\n 40.18726672309203\n ],\n [\n -124.134521484375,\n 40.18726672309203\n ],\n [\n -124.134521484375,\n 37.47485808497102\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"22","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Boyt, W.G.","contributorId":240765,"corporation":false,"usgs":false,"family":"Boyt","given":"W.G.","email":"","affiliations":[],"preferred":false,"id":798924,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213268,"text":"70213268 - 1941 - Report of committee on the chemistry of natural waters, 1840–41","interactions":[],"lastModifiedDate":"2020-09-17T13:52:06.202075","indexId":"70213268","displayToPublicDate":"1941-09-16T12:17:59","publicationYear":"1941","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 the chemistry of natural waters, 1840–41","docAbstract":"The membership of the Committee during the past year was as follows: I. A. Dennison. Bureau of Standards; C. S. Scofield, Department of Agriculture; D. G. Thompson, Geological Survey; T. G. Thompson, University of Washington, Seattle, Washington; and C. S. Howard, United States Geological Survey, Washington, D.C. (Chairman).
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i003p00901-1","usgsCitation":"Howard, C.S., 1941, Report of committee on the chemistry of natural waters, 1840–41: Eos, Transactions, American Geophysical Union, v. 22, no. 3, https://doi.org/10.1029/TR022i003p00901-1.","productDescription":"1 p.","startPage":"901","costCenters":[],"links":[{"id":378460,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"3","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":798923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213267,"text":"70213267 - 1941 - Magnetic studies by the Geophysical Section of the United States Geological Survey","interactions":[],"lastModifiedDate":"2020-09-16T17:05:51.805795","indexId":"70213267","displayToPublicDate":"1941-09-16T11:57:32","publicationYear":"1941","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":"Magnetic studies by the Geophysical Section of the United States Geological Survey","docAbstract":"Continued progress has been made in magnetic surveys over large sectional areas by G. R. MacCarthy. Beginning in Florida south of the Okeefenokee Swamp, magnetic traverses were measured and continued through the southern part of Georgia. The most northerly traverses crossed regions where they contacted the crystallines near the surface of the ground. All traverses were run in an east‐west direction. It is planned to continue the magnetic relief‐map described in the Transactions of 1939 of the American Geophysical Union by adding to it this portion of the State of Georgia.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR022i002p00460","usgsCitation":"Lee, F., 1941, Magnetic studies by the Geophysical Section of the United States Geological Survey: Eos, Transactions, American Geophysical Union, v. 22, no. 2, p. 460-462, https://doi.org/10.1029/TR022i002p00460.","productDescription":"3 p.","startPage":"460","endPage":"462","costCenters":[],"links":[{"id":378454,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"22","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Lee, F.W.","contributorId":240764,"corporation":false,"usgs":false,"family":"Lee","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":798922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213120,"text":"70213120 - 1941 - The quicksilver deposits of the Terlingua region, Texas","interactions":[],"lastModifiedDate":"2020-09-09T20:23:23.184757","indexId":"70213120","displayToPublicDate":"1941-09-09T15:17:34","publicationYear":"1941","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":"The quicksilver deposits of the Terlingua region, Texas","docAbstract":"Texas is second among quicksilver-producing States because of the Terlingua region, in the Big Bend of the Rio Grande. This region contains Cretaceous strata, largely calcareous, which grade upward into Tertiary volcanics, locally without break. The strata are cut by numerous intrusions, largely alkalic, and are extensively folded and faulted.Many of the lodes are near the base of the impervious Del Rio clay, some at higher horizons, and a few in intrusive masses. The solutions penetrated only along open passageways, such as major fractures or joints in zones of tension, and, especially at horizons above the Del Rio, in fractures related to fault zones.The quicksilver is believed to have been brought in by alkali sulphide solutions. Most other constituents that may once have been present in the solutions had been separated earlier. Precipitation resulted largely from mingling with groundwater. The comparatively low temperature and pressure at the shallow levels where groundwater was present aided the precipitation. As the then-existing zone of groundwater circulation has since been partly exposed by erosion, the lodes are necessarily rather close to the present surface. The gangue minerals, particularly the calcite, are believed to have been derived mainly from the sedimentary rocks with some addition of material from deep sources. The relation of the widespread bitumen to genesis is puzzling here, as in many other quicksilver deposits. Weathering is of slight economic importance. Many minerals that resemble supergene products, including the quicksilver chlorides, are thought to have resulted here from original deposition within the zone of vadose water.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.36.2.115","usgsCitation":"Ross, C.P., 1941, The quicksilver deposits of the Terlingua region, Texas: Economic Geology, v. 36, no. 2, p. 115-142, https://doi.org/10.2113/gsecongeo.36.2.115.","productDescription":"28 p.","startPage":"115","endPage":"142","costCenters":[],"links":[{"id":378287,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Terlingua Region","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.2108154296875,\n 29.463514026304715\n ],\n [\n -104.12841796875,\n 29.38217507514529\n ],\n [\n -104.0130615234375,\n 29.31514119318728\n ],\n [\n -103.7933349609375,\n 29.27202470909843\n ],\n [\n -103.71093749999999,\n 29.19532826709913\n ],\n [\n -103.5736083984375,\n 29.161755515328824\n ],\n [\n -103.46923828124999,\n 29.080175989623203\n ],\n [\n -103.3099365234375,\n 29.017748018496047\n ],\n [\n -103.1231689453125,\n 29.00333620017934\n ],\n [\n -103.0133056640625,\n 29.137768254983335\n ],\n [\n -102.9254150390625,\n 29.23847708592805\n ],\n [\n -102.864990234375,\n 29.3678143847754\n ],\n [\n -102.799072265625,\n 29.544787796199465\n ],\n [\n -102.6947021484375,\n 29.750070930806785\n ],\n [\n -104.2108154296875,\n 29.7453016622136\n ],\n [\n -104.2108154296875,\n 29.463514026304715\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"36","issue":"2","noUsgsAuthors":false,"publicationDate":"1941-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Ross, Clyde P.","contributorId":10473,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":798285,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213118,"text":"70213118 - 1941 - Discussion and communications: \"Band\", \"Layer,\" and some kindred terms","interactions":[],"lastModifiedDate":"2020-09-09T20:17:18.625621","indexId":"70213118","displayToPublicDate":"1941-09-09T15:15:39","publicationYear":"1941","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":"Discussion and communications: \"Band\", \"Layer,\" and some kindred terms","docAbstract":"No abstract available.
","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.36.3.345","usgsCitation":"Calkins, F., 1941, Discussion and communications: \"Band\", \"Layer,\" and some kindred terms: Economic Geology, v. 39, no. 3, p. 345-349, https://doi.org/10.2113/gsecongeo.36.3.345.","productDescription":"5 p.","startPage":"345","endPage":"349","costCenters":[],"links":[{"id":378284,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"3","noUsgsAuthors":false,"publicationDate":"1941-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Calkins, Frank C.","contributorId":62263,"corporation":false,"usgs":true,"family":"Calkins","given":"Frank C.","affiliations":[],"preferred":false,"id":798283,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70213117,"text":"70213117 - 1941 - Comments on the origin and major structural control of igneous rocks and related mineral deposits","interactions":[],"lastModifiedDate":"2020-09-09T20:14:16.966586","indexId":"70213117","displayToPublicDate":"1941-09-09T15:08:51","publicationYear":"1941","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":"Comments on the origin and major structural control of igneous rocks and related mineral deposits","docAbstract":"No abstract available.
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1941 - Directions for destroying crawfishes","interactions":[],"lastModifiedDate":"2014-07-21T09:10:53","indexId":"37994","displayToPublicDate":"1941-05-01T09:10:26","publicationYear":"1941","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":"190","title":"Directions for destroying crawfishes","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Prepared in the Division of Predator and Rodent Control.","usgsCitation":"U.S. Fish and Wildlife Service, 1941, Directions for destroying crawfishes: Wildlife Leaflet 190, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290518,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5525e4b0b290850f6287","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529798,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37993,"text":"37993 - 1941 - Publications on the selection and care of furs","interactions":[],"lastModifiedDate":"2014-07-21T09:08:37","indexId":"37993","displayToPublicDate":"1941-05-01T09:08:12","publicationYear":"1941","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":"189","title":"Publications on the selection and care of furs","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Fish and Wildlife Service, 1941, Publications on the selection and care of furs: Wildlife Leaflet 189, 1 p.","productDescription":"1 p.","numberOfPages":"1","costCenters":[],"links":[{"id":290517,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6e87e4b0b29085105d6a","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529797,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37992,"text":"37992 - 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