{"pageNumber":"7153","pageRowStart":"178800","pageSize":"25","recordCount":184733,"records":[{"id":5220102,"text":"5220102 - 1946 - The source of animals moving into a depopulated area","interactions":[],"lastModifiedDate":"2025-03-06T16:35:33.27772","indexId":"5220102","displayToPublicDate":"1946-11-25T00:00:00","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2373,"text":"Journal of Mammalogy","onlineIssn":"1545-1542","printIssn":"0022-2372","active":true,"publicationSubtype":{"id":10}},"title":"The source of animals moving into a depopulated area","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Oxford Academic","doi":"10.2307/1375337","usgsCitation":"Stickel, L.F., 1946, The source of animals moving into a depopulated area: Journal of Mammalogy, v. 27, no. 4, p. 301-307, https://doi.org/10.2307/1375337.","productDescription":"7 p.","startPage":"301","endPage":"307","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":198067,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland","otherGeospatial":"Patuxent Research Refuge","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -76.81153328582378,\n              39.08394929404287\n            ],\n            [\n              -76.81153328582378,\n              39.00458548002837\n            ],\n            [\n              -76.73065304265401,\n              39.00458548002837\n            ],\n            [\n              -76.73065304265401,\n              39.08394929404287\n            ],\n            [\n              -76.81153328582378,\n              39.08394929404287\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"27","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db63646f","contributors":{"authors":[{"text":"Stickel, Lucille F.","contributorId":76598,"corporation":false,"usgs":true,"family":"Stickel","given":"Lucille","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":331335,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70219996,"text":"70219996 - 1946 - Influenza B in 1945-46","interactions":[],"lastModifiedDate":"2021-04-16T17:14:25.062015","indexId":"70219996","displayToPublicDate":"1946-11-02T12:05:54","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2595,"text":"Lancet","active":true,"publicationSubtype":{"id":10}},"title":"Influenza B in 1945-46","docAbstract":"<p>No abstract&nbsp; available.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/S0140-6736(46)90085-2","usgsCitation":"Dudgeon, J., Camb, M., Stuart-Harris, C., Andrews, C., Glover, R., and Bradley, W., 1946, Influenza B in 1945-46: Lancet, https://doi.org/10.1016/S0140-6736(46)90085-2.","costCenters":[],"links":[{"id":385166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Dudgeon, J.A.","contributorId":257506,"corporation":false,"usgs":false,"family":"Dudgeon","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":814417,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Camb, M.A.","contributorId":257507,"corporation":false,"usgs":false,"family":"Camb","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":814418,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stuart-Harris, C.H.","contributorId":257508,"corporation":false,"usgs":false,"family":"Stuart-Harris","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":814419,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Andrews, C.H.","contributorId":257510,"corporation":false,"usgs":false,"family":"Andrews","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":814420,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Glover, R.E.","contributorId":81169,"corporation":false,"usgs":true,"family":"Glover","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":814421,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Bradley, W.H.","contributorId":220222,"corporation":false,"usgs":false,"family":"Bradley","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":814422,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":70222083,"text":"70222083 - 1946 - Preliminary report on the stratigraphy and structure of the Kurupa, Colville, and Oolamnagavik Rivers, Alaska","interactions":[],"lastModifiedDate":"2022-05-31T20:24:01.910966","indexId":"70222083","displayToPublicDate":"1946-11-01T16:27:50","publicationYear":"1946","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"1","subseriesTitle":"Preliminary Report","title":"Preliminary report on the stratigraphy and structure of the Kurupa, Colville, and Oolamnagavik Rivers, Alaska","docAbstract":"<p>U. S. Geological Survey Party No. 4 covered the area between 68° 30' and 69° 08' N. latitude and between 154° and 155°20' W. longitude during the period May 18 to September 2. Traverses were confined mainly to the valleys of the Kurupa, Colville, and Oolamnagavik Rivers inasmuch as very little rock is exposed in the interstream areas. This report is limited to the Colville River valley area between the Kura and Killik Rivers, and to a stratigraphic section exposed. on the Kurupa 7-12 miles south of the Colville.</p><p>A final report will be prepared by April 1, 1947, on the total area and will include discussions of the stratigraphy and structure of Upper Cretaceous formations A through D on the Oolamnagavik and Kurupa, the stratigraphy of Formation D on the Colville, and the Lower Cretaceous and Triassic rocks. Separation and identification of heavy minerals from the sandstones and conglomerates, binocular and petrographic microscope examinations of specimens, identification of megafossils, and separation and identification of microfossils, if any, will be undertaken. Detailed examination of all aerial photos will be made to trace out structures and formations in the adjacent areas to the east, north, and west. It seems probable that close correlation between this area, the Killik River area, and Maybe Creek area will be possible by extrapolating field and aerial photo data. It is possible also to trace structures and some formation westward from the Kurupa River.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70222083","usgsCitation":"Chapman, R., and Thurrell, R.F., 1946, Preliminary report on the stratigraphy and structure of the Kurupa, Colville, and Oolamnagavik Rivers, Alaska: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 1, Report: 11 p.; 2 Plates: 51.68 x 36.09 inches and 9.71 x 31.29 inches, https://doi.org/10.3133/70222083.","productDescription":"Report: 11 p.; 2 Plates: 51.68 x 36.09 inches and 9.71 x 31.29 inches","costCenters":[],"links":[{"id":401382,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70222083/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401383,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70222083/figure-1.pdf","text":"Figure 1","linkFileType":{"id":1,"text":"pdf"}},{"id":401384,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/unnumbered/70222083/figure-2.pdf","text":"Figure 2","linkFileType":{"id":1,"text":"pdf"}},{"id":396834,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70222083/report-thumb.jpg"},{"id":387245,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_74562.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Kurupa, Colville, and Oolamnagavik Rivers","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -155.25,\n              68.8333\n            ],\n            [\n              -153.8333,\n              68.8333\n            ],\n            [\n              -153.8333,\n              69.1667\n            ],\n            [\n              -155.25,\n              69.1667\n            ],\n            [\n              -155.25,\n              68.8333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Chapman, Robert M.","contributorId":81888,"corporation":false,"usgs":true,"family":"Chapman","given":"Robert M.","affiliations":[],"preferred":false,"id":837411,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thurrell, R. F. Jr.","contributorId":43024,"corporation":false,"usgs":true,"family":"Thurrell","given":"R.","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":837412,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70220484,"text":"70220484 - 1946 - Structural control of ore deposition at Kasaan Peninsula, southeastern Alaska","interactions":[],"lastModifiedDate":"2021-05-16T15:41:42.249065","indexId":"70220484","displayToPublicDate":"1946-10-31T10:35:21","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"title":"Structural control of ore deposition at Kasaan Peninsula, southeastern Alaska","docAbstract":"<p><span>Copper‐bearing magnetite deposits and associated copper deposits&nbsp;</span><span class=\"ScopusTermHighlight\">at</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Kasaan</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Peninsula</span><span>, Prince of Wales Island,&nbsp;</span><span class=\"ScopusTermHighlight\">southeastern</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Alaska</span><span>, have been known for many years and have been mined to some extent for their copper content.&nbsp;</span><span class=\"ScopusTermHighlight\">At</span><span>&nbsp;the beginning of World War II, the development of war industries in the Pacific northwest focused attention on the deposits as possible sources of iron&nbsp;</span><span class=\"ScopusTermHighlight\">ore</span><span>. From 1942 through 1944 the United States Geological Survey made detailed studies of most of the&nbsp;</span><span class=\"ScopusTermHighlight\">ore</span><span>&nbsp;deposits and&nbsp;</span><span class=\"ScopusTermHighlight\">at</span><span>&nbsp;a few of the more promising localities diamond‐drilling operations were carried on by the United States Bureau of Mines. The deposits are for the most part small and irregular but of relatively high grade. The chief&nbsp;</span><span class=\"ScopusTermHighlight\">ore</span><span>&nbsp;minerals are magnetite, pyrite, and chalcopyrite, and the gangue consists largely of skarn minerals, including garnet, epidote, diopside, and hornblende. The deposits are presumably of pyrometasomatic origin, but whereas deposits of this type are commonly replacement bodies in limestone,&nbsp;</span><span class=\"ScopusTermHighlight\">at</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Kasaan</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Peninsula</span><span>&nbsp;limestone seemingly was a poor host rock for the&nbsp;</span><span class=\"ScopusTermHighlight\">ore.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i005p00712","usgsCitation":"Warner, L., and Goddard, E.N., 1946, Structural control of ore deposition at Kasaan Peninsula, southeastern Alaska, v. 27, no. 5, p. 712-712, https://doi.org/10.1029/TR027i005p00712.","productDescription":"1 p.","startPage":"712","endPage":"712","costCenters":[],"links":[{"id":385662,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Alaska","otherGeospatial":"Kasaan  Penninsula","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -132.5775146484375,\n              55.42277902267131\n            ],\n            [\n              -132.0721435546875,\n              55.42277902267131\n            ],\n            [\n              -132.0721435546875,\n              55.67138928829547\n            ],\n            [\n              -132.5775146484375,\n              55.67138928829547\n            ],\n            [\n              -132.5775146484375,\n              55.42277902267131\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"27","issue":"5","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Warner, L.A.","contributorId":99611,"corporation":false,"usgs":true,"family":"Warner","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":815730,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goddard, E. N.","contributorId":77158,"corporation":false,"usgs":true,"family":"Goddard","given":"E.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":815731,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215042,"text":"70215042 - 1946 - A portable differential thermal analysis unit for bauxite exploration","interactions":[],"lastModifiedDate":"2020-10-06T18:49:46.321638","indexId":"70215042","displayToPublicDate":"1946-10-06T13:30:32","publicationYear":"1946","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":"A portable differential thermal analysis unit for bauxite exploration","docAbstract":"<p><span>A small differential thermal analysis unit that embodies the fundamental features of larger laboratory models is designed for field exploration for bauxite and related materials. The apparatus, requiring only a source of electrical power, combines portability with ease of operation and rapid analysis. The portable unit is suitable for quantitative work and has been successfully applied in bauxite exploration on the island of Hispaniola.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.41.1.64","usgsCitation":"Hendricks, S.B., and Nelson, R.A., 1946, A portable differential thermal analysis unit for bauxite exploration: Economic Geology, v. 41, no. 1, p. 64-76, https://doi.org/10.2113/gsecongeo.41.1.64.","productDescription":"13 p.","startPage":"64","endPage":"76","costCenters":[],"links":[{"id":379099,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"1","noUsgsAuthors":false,"publicationDate":"1946-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hendricks, S. B.","contributorId":50202,"corporation":false,"usgs":true,"family":"Hendricks","given":"S.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":800618,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, R. A.","contributorId":96727,"corporation":false,"usgs":true,"family":"Nelson","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":800619,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215040,"text":"70215040 - 1946 - Contribution to the petrography of Haleakala Volcano, Hawaii ","interactions":[],"lastModifiedDate":"2020-10-06T17:52:56.057828","indexId":"70215040","displayToPublicDate":"1946-10-06T12:43:26","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Contribution to the petrography of Haleakala Volcano, Hawaii ","docAbstract":"<p><span>The volcanic rocks of Haleakala Volcano comprise, from oldest to youngest, the Honomanu, Kula, and Hana volcanic series. The Honomanu volcanic series consists largely of olivine basalt, with less abundant basalt and picrite-basalt containing large phenocrysts of olivine. In the Kula and Hana volcanic series there are some basalts and olivine basalts, but the characteristic rocks are andesites and picrite-basalt containing abundant phenocrysts of augite as well as olivine. New chemical analyses of six specimens of Kula lavas are given. Five are andesites, and one a picrite-basalt. Each of the six rocks is described in detail. A variation diagram for Haleakala rocks illustrates the alkalic character of the series.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1946)57[115:CTTPOH]2.0.CO;2","usgsCitation":"Macdonald, G.A., and Powers, H.A., 1946, Contribution to the petrography of Haleakala Volcano, Hawaii : GSA Bulletin, v. 57, no. 1, p. 115-124, https://doi.org/10.1130/0016-7606(1946)57[115:CTTPOH]2.0.CO;2.","productDescription":"10 p.","startPage":"115","endPage":"124","costCenters":[],"links":[{"id":379098,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"Haleakala Volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.2200927734375,\n              18.641040231399984\n            ],\n            [\n              -154.7479248046875,\n              18.641040231399984\n            ],\n            [\n              -154.7479248046875,\n              20.452749362534945\n            ],\n            [\n              -156.2200927734375,\n              20.452749362534945\n            ],\n            [\n              -156.2200927734375,\n              18.641040231399984\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"57","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Macdonald, G. A.","contributorId":86824,"corporation":false,"usgs":true,"family":"Macdonald","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":800616,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Powers, H. A.","contributorId":116601,"corporation":false,"usgs":true,"family":"Powers","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":800617,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215038,"text":"70215038 - 1946 - Quartz crystal in Brazil","interactions":[],"lastModifiedDate":"2020-10-06T21:15:22.849686","indexId":"70215038","displayToPublicDate":"1946-10-06T12:34:58","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Quartz crystal in Brazil","docAbstract":"<p>The peak production of Brazilian quartz crystal was reached in 1943 when 2411 metric tons were exported. Minas Gerais, Goiaz, and Bahia are the principal producing states. Minor quantities are obtained from Espirito Santo and Northeastern Brazil.</p><p>Primary veins and pegmatites yield secondary deposits of eluvial, colluvial, and alluvial origin. The veins range in form from tabular or lenticular bodies, pipes, and pockets to composite lodes and bedded masses. The mineralogy is simple; accessory minerals are few and rare. A small proportion of clear crystals, occurring in vein masses of milky quartz, furnishes the commercial product. Filling, rather than replacement, is believed to be the dominant emplacement process. Pegmatites yield a little commercial quartz. Both residual (eluvial) and water-laid (alluvial) quartz deposits are economically important.</p><p>Crystals range up to 40 metric tons in weight; those of 1 to 5 tons occur in many deposits. Quartz from every locality studied is twinned on both the Brazil and Dauphiné laws. Phantoms are abundant.</p><p>Field studies reveal little difference between the final quartz from some pegmatites and that from veins. It is inferred that the veins may grade into pegmatites at depth and that both are products of the same mineralogenic epoch. Present evidence does not justify a closer dating for the formation of the veins and pegmatites than the early Paleozoic.</p><p>There are few large quartz mines in Brazil. The impressive quartz production during the war years came from many small, scattered workings. Mining methods are primitive, and mechanization was feasible in relatively few areas. The ratio of mine-clean crystal to the total quantity of excavated material varies between 1:1000 and 1:100,000, with an over-all average for the best mines of the order of 1:10,000. Cost of mining ranges from $2 to $10 a kilogram. The average export value during 1944 was $12.50 per kilogram.</p><p>The potential reserves of quartz crystal in Brazil are large, but actual or visual reserves in known districts are small. Future production capacity will be determined by economic factors.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1946)57[601:QCIB]2.0.CO;2","usgsCitation":"Johnston, W.D., and Butler, R., 1946, Quartz crystal in Brazil: GSA Bulletin, v. 57, no. 7, p. 601-650, https://doi.org/10.1130/0016-7606(1946)57[601:QCIB]2.0.CO;2.","productDescription":"50 p.","startPage":"601","endPage":"650","costCenters":[],"links":[{"id":379097,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-57.62513,-30.21629],[-56.2909,-28.85276],[-55.16229,-27.88192],[-54.49073,-27.47476],[-53.64874,-26.92347],[-53.62835,-26.12487],[-54.13005,-25.54764],[-54.62529,-25.73926],[-54.42895,-25.16218],[-54.29348,-24.5708],[-54.29296,-24.02101],[-54.65283,-23.83958],[-55.0279,-24.00127],[-55.40075,-23.95694],[-55.51764,-23.572],[-55.61068,-22.65562],[-55.79796,-22.35693],[-56.47332,-22.0863],[-56.88151,-22.28215],[-57.93716,-22.09018],[-57.87067,-20.73269],[-58.16639,-20.1767],[-57.8538,-19.97],[-57.95,-19.4],[-57.67601,-18.96184],[-57.49837,-18.17419],[-57.73456,-17.55247],[-58.2808,-17.27171],[-58.38806,-16.87711],[-58.24122,-16.29957],[-60.15839,-16.25828],[-60.54297,-15.09391],[-60.25115,-15.07722],[-60.26433,-14.64598],[-60.4592,-14.35401],[-60.5033,-13.77595],[-61.08412,-13.47938],[-61.7132,-13.4892],[-62.12708,-13.19878],[-62.80306,-13.00065],[-63.1965,-12.62703],[-64.31635,-12.46198],[-65.40228,-11.56627],[-65.3219,-10.89587],[-65.44484,-10.51145],[-65.33844,-9.76199],[-66.64691,-9.93133],[-67.1738,-10.30681],[-68.04819,-10.71206],[-68.27125,-11.01452],[-68.78616,-11.03638],[-69.52968,-10.95173],[-70.09375,-11.12397],[-70.54869,-11.00915],[-70.48189,-9.49012],[-71.30241,-10.07944],[-72.18489,-10.0536],[-72.56303,-9.52019],[-73.22671,-9.46221],[-73.01538,-9.03283],[-73.57106,-8.42445],[-73.98724,-7.52383],[-73.7234,-7.341],[-73.72449,-6.9186],[-73.12003,-6.62993],[-73.21971,-6.08919],[-72.96451,-5.74125],[-72.89193,-5.27456],[-71.74841,-4.59398],[-70.92884,-4.40159],[-70.79477,-4.25126],[-69.89364,-4.29819],[-69.4441,-1.55629],[-69.42049,-1.12262],[-69.57707,-0.54999],[-70.02066,-0.18516],[-70.01557,0.54141],[-69.4524,0.70616],[-69.25243,0.60265],[-69.21864,0.98568],[-69.8046,1.08908],[-69.81697,1.71481],[-67.86857,1.69246],[-67.53781,2.03716],[-67.26,1.72],[-67.06505,1.13011],[-66.87633,1.25336],[-66.32577,0.72445],[-65.54827,0.78925],[-65.35471,1.09528],[-64.61101,1.32873],[-64.19931,1.49285],[-64.08309,1.91637],[-63.36879,2.2009],[-63.42287,2.41107],[-64.27,2.49701],[-64.40883,3.12679],[-64.36849,3.79721],[-64.81606,4.05645],[-64.62866,4.14848],[-63.88834,4.02053],[-63.0932,3.77057],[-62.80453,4.00697],[-62.08543,4.16212],[-60.96689,4.53647],[-60.60118,4.9181],[-60.73357,5.20028],[-60.21368,5.24449],[-59.98096,5.01406],[-60.111,4.57497],[-59.76741,4.4235],[-59.53804,3.9588],[-59.81541,3.6065],[-59.97452,2.75523],[-59.71855,2.24963],[-59.64604,1.78689],[-59.03086,1.3177],[-58.54001,1.26809],[-58.42948,1.46394],[-58.11345,1.5072],[-57.66097,1.68258],[-57.33582,1.94854],[-56.7827,1.86371],[-56.53939,1.89952],[-55.9957,1.81767],[-55.9056,2.022],[-56.07334,2.22079],[-55.97332,2.51036],[-55.56976,2.42151],[-55.09759,2.52375],[-54.52475,2.31185],[-54.08806,2.10556],[-53.77852,2.3767],[-53.55484,2.3349],[-53.41847,2.05339],[-52.93966,2.12486],[-52.55642,2.50471],[-52.24934,3.24109],[-51.6578,4.15623],[-51.31715,4.20349],[-51.06977,3.6504],[-50.50888,1.90156],[-49.97408,1.73648],[-49.9471,1.04619],[-50.69925,0.22298],[-50.38821,-0.07844],[-48.62057,-0.23549],[-48.5845,-1.23781],[-47.82496,-0.58162],[-46.56658,-0.94103],[-44.9057,-1.55174],[-44.41762,-2.13775],[-44.58159,-2.69131],[-43.41879,-2.38311],[-41.47266,-2.91202],[-39.97867,-2.87305],[-38.50038,-3.70065],[-37.22325,-4.82095],[-36.45294,-5.1094],[-35.5978,-5.1495],[-35.23539,-5.46494],[-34.89603,-6.73819],[-34.72999,-7.34322],[-35.12821,-8.9964],[-35.63697,-9.64928],[-37.04652,-11.04072],[-37.68361,-12.17119],[-38.42388,-13.03812],[-38.67389,-13.05765],[-38.95328,-13.79337],[-38.8823,-15.66705],[-39.16109,-17.20841],[-39.26734,-17.86775],[-39.58352,-18.2623],[-39.76082,-19.59911],[-40.77474,-20.90451],[-40.94476,-21.93732],[-41.75416,-22.37068],[-41.98828,-22.97007],[-43.0747,-22.96769],[-44.64781,-23.35196],[-45.35214,-23.79684],[-46.47209,-24.08897],[-47.64897,-24.8852],[-48.49546,-25.87702],[-48.641,-26.6237],[-48.47474,-27.17591],[-48.66152,-28.18613],[-48.88846,-28.67412],[-49.58733,-29.22447],[-50.69687,-30.98447],[-51.57623,-31.7777],[-52.25608,-32.24537],[-52.7121,-33.19658],[-53.37366,-33.76838],[-53.65054,-33.202],[-53.20959,-32.72767],[-53.78795,-32.04724],[-54.57245,-31.49451],[-55.60151,-30.85388],[-55.97324,-30.88308],[-56.97603,-30.10969],[-57.62513,-30.21629]]]},\"properties\":{\"name\":\"Brazil\"}}]}","volume":"57","issue":"7","noUsgsAuthors":false,"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":800614,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, R.D.","contributorId":242663,"corporation":false,"usgs":false,"family":"Butler","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":800615,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215037,"text":"70215037 - 1946 - Notes on determining the effective distance to a line of recharge","interactions":[],"lastModifiedDate":"2020-10-06T17:31:34.027294","indexId":"70215037","displayToPublicDate":"1946-10-06T12:13:09","publicationYear":"1946","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":"Notes on determining the effective distance to a line of recharge","docAbstract":"<p><span>Increasing emphasis has been given in recent years to the installation of wells in sand and gravel deposits along perennial streams. Under favorable conditions water enters the aquifer from the adjacent stream so that the safe yield is not limited by recharge from local precipitation [see “References” at end of paper, Jeffords, 1946]. Some of the installations tested, however, have not been successful. At times the preliminary investigations have been inadequate, and often quantitative hydrologic techniques have been applied without adequate consideration of the existing local conditions.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i006p00854","usgsCitation":"Kazmann, R., 1946, Notes on determining the effective distance to a line of recharge: Eos, Transactions, American Geophysical Union, v. 27, no. 6, p. 854-859, https://doi.org/10.1029/TR027i006p00854.","productDescription":"6 p.","startPage":"854","endPage":"859","costCenters":[],"links":[{"id":379096,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Kazmann, R.G.","contributorId":242662,"corporation":false,"usgs":false,"family":"Kazmann","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":800613,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215036,"text":"70215036 - 1946 - Activity of Parícutin volcano from April 12 to May 3, 1946","interactions":[],"lastModifiedDate":"2020-10-06T17:11:41.236949","indexId":"70215036","displayToPublicDate":"1946-10-06T12:04:17","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Activity of Parícutin volcano from April 12 to May 3, 1946","docAbstract":"<p><span>The activity of Parícutin varied greatly during the period April 12 to May 3. The strong eruptive activity that began in mid‐March, marked on March 17 by the formation of a new boca with a short‐lived volcancito and by external changes in the form of the cone, continued until April 18, The period April 12–18 was marked by bomb‐showers and explosive blasts at the rate of ten to 15 a minute, mostly from the south vent of the double crater. Most of the bombs fell into the north crater and on the north flank of the cone. From April 19 to 26 the activity was, in general, very weak, and little ash and few bombs were projected beyond the rim of the cone, Explosions were very rare, and the weak vapor column from the Volcano was accompanied by a dull surf‐like roar. Most of the vapor emerged from a small vent near the center of the divide between the two coalescing craters. A heavy ash column, at times approaching in intensity that of 1943, emerged from the Volcano from April 27 to 29. The ash was erupted from both the north and south vents of the crater, though the south vent is believed to have contributed the most. From April 30 to May 3 the activity was again very weak, and only a feeble column rose above the cone.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i003p00410","usgsCitation":"Kennedy, G.C., 1946, Activity of Parícutin volcano from April 12 to May 3, 1946: Eos, Transactions, American Geophysical Union, v. 27, no. 3, p. 410-411, https://doi.org/10.1029/TR027i003p00410.","productDescription":"2 p.","startPage":"410","endPage":"411","costCenters":[],"links":[{"id":379095,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Mexico","state":"Michoacan","otherGeospatial":"Parícutin volcano","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.535400390625,\n              19.17111285978146\n            ],\n            [\n              -102.0355224609375,\n              19.17111285978146\n            ],\n            [\n              -102.0355224609375,\n              19.694314241825747\n            ],\n            [\n              -102.535400390625,\n              19.694314241825747\n            ],\n            [\n              -102.535400390625,\n              19.17111285978146\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"27","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kennedy, George C.","contributorId":19201,"corporation":false,"usgs":true,"family":"Kennedy","given":"George","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":800612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215034,"text":"70215034 - 1946 - Hydrology in relation to economic geology","interactions":[],"lastModifiedDate":"2020-10-06T16:58:00.704592","indexId":"70215034","displayToPublicDate":"1946-10-06T11:54:36","publicationYear":"1946","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":"Hydrology in relation to economic geology","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.41.1.1","usgsCitation":"Meinzer, O.E., 1946, Hydrology in relation to economic geology: Economic Geology, v. 41, no. 1, p. 1-12, https://doi.org/10.2113/gsecongeo.41.1.1.","productDescription":"12 p.","startPage":"1","endPage":"12","costCenters":[],"links":[{"id":379094,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"1","noUsgsAuthors":false,"publicationDate":"1946-01-01","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":800611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215033,"text":"70215033 - 1946 - Veterans' retraining program in geology","interactions":[],"lastModifiedDate":"2021-01-28T21:21:07.044307","indexId":"70215033","displayToPublicDate":"1946-10-06T11:39:16","publicationYear":"1946","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":"Veterans' retraining program in geology","docAbstract":"<p>No&nbsp; abstract available.</p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.41.1.86","usgsCitation":"Bradley, W.H., 1946, Veterans' retraining program in geology: Economic Geology, v. 41, no. 1, p. 86-87, https://doi.org/10.2113/gsecongeo.41.1.86.","productDescription":"2 p.","startPage":"86","endPage":"87","costCenters":[],"links":[{"id":379092,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"41","issue":"1","noUsgsAuthors":false,"publicationDate":"1946-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Bradley, Wilmont H.","contributorId":80173,"corporation":false,"usgs":true,"family":"Bradley","given":"Wilmont","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":809309,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215032,"text":"70215032 - 1946 - Radial flow in a leaky artesian aquifer","interactions":[],"lastModifiedDate":"2020-10-06T16:32:20.844552","indexId":"70215032","displayToPublicDate":"1946-10-06T11:23:15","publicationYear":"1946","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":"Radial flow in a leaky artesian aquifer","docAbstract":"<p><span>A partial differential equation is set up for radial flow in an elastic artesian aquifer into which there is vertical leakage in proportion to the drawdown. This differential equation is integrated to obtain two steady state solutions, one for the case of a well in an infinite aquifer, and the other for the case where the head is maintained constant along an outer boundary concentric with the well. In the second case, the solution of the non‐steady state is also obtained for flow towards a well discharging at a steady rate, the initial state being one of uniform head distribution. A table and some curves are given for one set of assumed values of three of the parameters of the system.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00198","usgsCitation":"Jacob, C.E., 1946, Radial flow in a leaky artesian aquifer: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 198-208, https://doi.org/10.1029/TR027i002p00198.","productDescription":"11 p.","startPage":"198","endPage":"208","costCenters":[],"links":[{"id":379089,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":800609,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215031,"text":"70215031 - 1946 - The glacial anticyclone theory examined in the light of recent meteorological data from Greenland—Part I","interactions":[],"lastModifiedDate":"2020-10-06T16:21:18.116529","indexId":"70215031","displayToPublicDate":"1946-10-06T11:03:21","publicationYear":"1946","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 glacial anticyclone theory examined in the light of recent meteorological data from Greenland—Part I","docAbstract":"<p>The glacial anticyclone theory, which William H. Hobbs propounded in 1910, is today still the only definitely formulated theory concerning the atmospheric movements that take place over an ice sheet of large extent. It stands chiefly on deductive grounds and contains several features that to climatologists as well as to glaciologists have always seemed questionable. Aside from the need of its verification for scientific reasons, there is now also urgent practical need for reliable information about the weather conditions that prevail over the ice sheet of Greenland, for Greenland lies athwart several of the great air routes of the future. In this paper, accordingly, the glacial anticyclone theory is first analyzed and then confronted with the facts of observation that are now at hand, especially those reported from the fixed meteorological stations which were maintained in the interior of Greenland during the 1930s.</p><p>In this, the first part of the paper, the meteorological data from the Eismitte station of the German Wegener Expedition are reviewed. The second part will cover the areological data of that expedition and the similar material from the other ice‐cap stations. The conclusions reached are that there is no evidence of a virtually permanent “glacial anticyclone” centered over the Greenland ice sheet. On the contrary, there is consistent evidence from all parts of Greenland that the weather over the ice sheet is controlled by alternating cyclonic and anticyclonic movements. Cyclonic activity is most intense in southern Greenland and weakest in northern Greenland. The entire ice sheet is supplied with snow brought by rising maritime air masses, not by air descending from the upper troposphere. Aviators need not expect so much as a fifty‐fifty chance of meeting with good weather on flights across central Greenland, except for a few weeks in midsummer.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i003p00324","usgsCitation":"Matthes, F.E., 1946, The glacial anticyclone theory examined in the light of recent meteorological data from Greenland—Part I: Eos, Transactions, American Geophysical Union, v. 27, no. 3, p. 324-341, https://doi.org/10.1029/TR027i003p00324.","productDescription":"18 p.","startPage":"324","endPage":"341","costCenters":[],"links":[{"id":379087,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Greenland","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-46.76379,82.62796],[-43.40644,83.22516],[-39.89753,83.18018],[-38.62214,83.54905],[-35.08787,83.64513],[-27.10046,83.51966],[-20.84539,82.72669],[-22.69182,82.34165],[-26.51753,82.29765],[-31.9,82.2],[-31.39646,82.02154],[-27.85666,82.13178],[-24.84448,81.78697],[-22.90328,82.09317],[-22.07175,81.73449],[-23.16961,81.15271],[-20.62363,81.52462],[-15.76818,81.91245],[-12.77018,81.71885],[-12.20855,81.29154],[-16.28533,80.58004],[-16.85,80.35],[-20.04624,80.17708],[-17.73035,80.12912],[-18.9,79.4],[-19.70499,78.75128],[-19.67353,77.63859],[-18.47285,76.98565],[-20.03503,76.94434],[-21.67944,76.62795],[-19.83407,76.09808],[-19.59896,75.24838],[-20.66818,75.15585],[-19.37281,74.29561],[-21.59422,74.22382],[-20.43454,73.81713],[-20.76234,73.46436],[-22.17221,73.30955],[-23.56593,73.30663],[-22.31311,72.62928],[-22.29954,72.18409],[-24.27834,72.59788],[-24.79296,72.3302],[-23.44296,72.08016],[-22.13281,71.46898],[-21.75356,70.66369],[-23.53603,70.471],[-24.30702,70.85649],[-25.54341,71.43094],[-25.20135,70.75226],[-26.36276,70.22646],[-23.72742,70.18401],[-22.34902,70.12946],[-25.02927,69.2588],[-27.74737,68.47046],[-30.67371,68.12503],[-31.77665,68.12078],[-32.81105,67.73547],[-34.20196,66.67974],[-36.35284,65.9789],[-37.04378,65.93768],[-38.37505,65.69213],[-39.81222,65.45848],[-40.66899,64.83997],[-40.68281,64.13902],[-41.1887,63.48246],[-42.81938,62.68233],[-42.41666,61.90093],[-42.86619,61.07404],[-43.3784,60.09772],[-44.7875,60.03676],[-46.26364,60.85328],[-48.26294,60.85843],[-49.23308,61.40681],[-49.90039,62.38336],[-51.63325,63.62691],[-52.14014,64.27842],[-52.27659,65.1767],[-53.66166,66.09957],[-53.30161,66.8365],[-53.96911,67.18899],[-52.9804,68.35759],[-51.47536,68.72958],[-51.08041,69.14781],[-50.87122,69.9291],[-52.01358,69.57492],[-52.55792,69.42616],[-53.45629,69.28363],[-54.68336,69.61003],[-54.75001,70.28932],[-54.35884,70.82131],[-53.43131,70.83576],[-51.39014,70.56978],[-53.10937,71.20485],[-54.00422,71.54719],[-55,71.40654],[-55.83468,71.65444],[-54.71819,72.58625],[-55.32634,72.95861],[-56.12003,73.64977],[-57.32363,74.71026],[-58.59679,75.09861],[-58.58516,75.51727],[-61.26861,76.10238],[-63.39165,76.1752],[-66.06427,76.13486],[-68.50438,76.06141],[-69.66485,76.37975],[-71.40257,77.00857],[-68.77671,77.32312],[-66.76397,77.37595],[-71.04293,77.63595],[-73.297,78.04419],[-73.15938,78.43271],[-69.37345,78.91388],[-65.7107,79.39436],[-65.3239,79.75814],[-68.02298,80.11721],[-67.15129,80.51582],[-63.68925,81.21396],[-62.23444,81.3211],[-62.65116,81.77042],[-60.28249,82.03363],[-57.20744,82.19074],[-54.13442,82.19962],[-53.04328,81.88833],[-50.39061,82.43883],[-48.00386,82.06481],[-46.59984,81.98595],[-44.523,81.6607],[-46.9007,82.19979],[-46.76379,82.62796]]]},\"properties\":{\"name\":\"Greenland\"}}]}","volume":"27","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":800604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215000,"text":"70215000 - 1946 - Report of committee on Glaciers, 1945","interactions":[],"lastModifiedDate":"2021-02-05T19:50:50.795727","indexId":"70215000","displayToPublicDate":"1946-10-05T14:16:50","publicationYear":"1946","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, 1945","docAbstract":"<p><span>To Preston P. Macy, Superintendent of Olympic National Park, the Committee is indebted for the first data on the recession of the Blue Glacier, one of the major ice streams on Mount Olympus. Annual measurements to its terminus were begun in 1938, the year in which Olympic National Park was established, and such measurements, MACY states, will be continued in future years, circumstances permitting. Thus one more sizable glacier is added to the list of ice bodies in the western United States whose variations in length and volume in response to current climatic fluctuations are being observed from year to year.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00219","usgsCitation":"Matthes, F., 1946, Report of committee on Glaciers, 1945: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 219-233, https://doi.org/10.1029/TR027i002p00219.","productDescription":"15 p.","startPage":"219","endPage":"233","costCenters":[],"links":[{"id":379068,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Matthes, Francois E.","contributorId":240914,"corporation":false,"usgs":false,"family":"Matthes","given":"Francois E.","affiliations":[],"preferred":false,"id":800517,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214998,"text":"70214998 - 1946 - Appendix A—Report of the subcommittee on permeability","interactions":[],"lastModifiedDate":"2020-10-05T19:16:32.873158","indexId":"70214998","displayToPublicDate":"1946-10-05T13:58:53","publicationYear":"1946","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":"Appendix A—Report of the subcommittee on permeability","docAbstract":"<p><span>The Subcommittee on Permeability of the Permanent Research Committee on Ground Water of the Section of Hydrology, was organized in 1943 to provide for the open discussion of the terminology relating to permeability with a view toward the elimination of conflicting usages and the clarification and standardization of acceptable terms. Confusion had arisen not only in the units of measurement but also in the notation and nomenclature of permeability. It seemed desirable to have general agreement particularly in regard to the names of the different physical parameters in common use and their symbols.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00245","usgsCitation":"Jacob, C.E., 1946, Appendix A—Report of the subcommittee on permeability: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 245-256, https://doi.org/10.1029/TR027i002p00245.","productDescription":"12  p.","startPage":"245","endPage":"256","costCenters":[],"links":[{"id":379066,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":800516,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214997,"text":"70214997 - 1946 - Appendix B—Notes on the permeability coefficient and its units","interactions":[],"lastModifiedDate":"2020-10-05T18:58:32.033392","indexId":"70214997","displayToPublicDate":"1946-10-05T13:51:45","publicationYear":"1946","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":"Appendix B—Notes on the permeability coefficient and its units","docAbstract":"<p><span>In the development of terms and units for a new science such as ground‐water hydrology, which is based on physics, it would seem fitting to adopt the terminology that has become standard in other branches of physics such as heat and electricity. Darcy's law has its counterpart in similar laws in the other branches of physics.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00256","usgsCitation":"Fishel, V., 1946, Appendix B—Notes on the permeability coefficient and its units: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 256-269, https://doi.org/10.1029/TR027i002p00256.","productDescription":"4 p.","startPage":"256","endPage":"269","costCenters":[],"links":[{"id":379065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Fishel, V.C.","contributorId":6126,"corporation":false,"usgs":true,"family":"Fishel","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":800515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214996,"text":"70214996 - 1946 - Appendix D—Notes on Darcy's law and permeability","interactions":[],"lastModifiedDate":"2020-10-05T18:46:28.96217","indexId":"70214996","displayToPublicDate":"1946-10-05T13:32:23","publicationYear":"1946","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":"Appendix D—Notes on Darcy's law and permeability","docAbstract":"<p><span>In any effort to establish nomenclature relating to the flow of fluids through porous media it would seem well first to consider the history of the development of our concepts and of the terms or expressions involved. Only in this way can precedent rightfully be honored and at the same time duplicating expressions be eliminated and the remaining more useful terms clarified. Then, proceeding with a foresight lined up with recent advances, we may hope to anticipate the needs of the future.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00265","usgsCitation":"Jacob, C.E., 1946, Appendix D—Notes on Darcy's law and permeability: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 265-673, https://doi.org/10.1029/TR027i002p00265.","productDescription":"9 p.","startPage":"265","endPage":"673","costCenters":[],"links":[{"id":379064,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":800514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214995,"text":"70214995 - 1946 - Appendix E—List of current publications concerning ground water","interactions":[],"lastModifiedDate":"2020-10-05T18:31:59.032967","indexId":"70214995","displayToPublicDate":"1946-10-05T13:17:18","publicationYear":"1946","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":"Appendix E—List of current publications concerning ground water","docAbstract":"<p>Alexander, W. H., Jr., Broadhurst, W. L., and White, W. N., Progress report on ground water In the High Plains in Texas, Tex. State Bd. Water Engrs., 12 pp., 7 tigs. (mimeogranhedl May 1944.</p><p>Ashley, George H.,and Graham, Jack B., Groundwater investigations in Pennsylvania Pa. Dep. Internal Affairs, Monthly Bull., v. 13, pp. 10–13 and 28, 1945.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00274","usgsCitation":"Berdan, J.M., 1946, Appendix E—List of current publications concerning ground water: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 274-278, https://doi.org/10.1029/TR027i002p00274.","productDescription":"5 p.","startPage":"274","endPage":"278","costCenters":[],"links":[{"id":379063,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Berdan, Jean M.","contributorId":34140,"corporation":false,"usgs":true,"family":"Berdan","given":"Jean","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":800513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214994,"text":"70214994 - 1946 - Report of Committee on Ground Water—1944–1945","interactions":[],"lastModifiedDate":"2020-10-05T18:16:42.707377","indexId":"70214994","displayToPublicDate":"1946-10-05T13:07:31","publicationYear":"1946","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 Ground Water—1944–1945","docAbstract":"<p>Because of war‐imposed responsibilities of most agencies and individuals this year, no new programs were undertaken by the Committee, but the work of the Subcommittee on Permeability was continued, and a substantial progress report by C. E. Jacob, Acting Chairman, and by members of this Subcommittee follows this report as Appendices A to D.</p><p>Following a suggestion by Max Suter, copies of this year's Committee report were sent to each member prior to publication and it is planned to follow this procedure in the future.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i002p00236","usgsCitation":"Lohman, S.W., 1946, Report of Committee on Ground Water—1944–1945: Eos, Transactions, American Geophysical Union, v. 27, no. 2, p. 236-245, https://doi.org/10.1029/TR027i002p00236.","productDescription":"10 p.","startPage":"236","endPage":"245","costCenters":[],"links":[{"id":379062,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Lohman, S. W.","contributorId":45318,"corporation":false,"usgs":true,"family":"Lohman","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":800512,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214993,"text":"70214993 - 1946 - Great Salt Lake: A selected bibliography with annotations","interactions":[],"lastModifiedDate":"2021-04-06T13:38:12.529337","indexId":"70214993","displayToPublicDate":"1946-10-05T12:57:09","publicationYear":"1946","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":"Great Salt Lake: A selected bibliography with annotations","docAbstract":"<p>Explorers began to push into the vast uncharted areas of the West in 1804, when Captains Lewis and Clarke ascended the Missouri River, crossed the Rocky Mountains into the headwaters of the Columbia River, and followed that stream to the Pacific Ocean. The honor of being the first white man to see Great Salt Lake is claimed for a number of explorers and trappers who visited the region in the twenties and thirties of the Nineteenth Century. Among these were Etienne Provot and James Bridger, who were in the region in 1824–25, each quite unaware of the other's activities and discoveries.</p><p>In 1833 Captain B. L. E. Bonneville dispatched a party from his camp at Green River, Wyoming, for the purpose of exploring Great Salt Lake. This party attempted to make a circuit of the lake, chart its outline, and trap all the streams en route, but the attempt was abandoned because the great barren salt plains west of the lake were so hazardous that the party was in grave danger of perishing.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i001p00103","usgsCitation":"Marsell, R.E., 1946, Great Salt Lake: A selected bibliography with annotations: Eos, Transactions, American Geophysical Union, v. 27, no. 1, p. 103-107, https://doi.org/10.1029/TR027i001p00103.","productDescription":"5 p.","startPage":"103","endPage":"107","costCenters":[],"links":[{"id":379061,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.258056640625,\n              40.613952441166596\n            ],\n            [\n              -111.8353271484375,\n              40.613952441166596\n            ],\n            [\n              -111.8353271484375,\n              41.78769700539063\n            ],\n            [\n              -113.258056640625,\n              41.78769700539063\n            ],\n            [\n              -113.258056640625,\n              40.613952441166596\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"27","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Marsell, Ray E.","contributorId":60204,"corporation":false,"usgs":true,"family":"Marsell","given":"Ray","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":800511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70214992,"text":"70214992 - 1946 - Discussion of “Forecasting stream‐flow of the Salt River, Arizona”","interactions":[],"lastModifiedDate":"2020-10-05T17:56:28.220078","indexId":"70214992","displayToPublicDate":"1946-10-05T12:44:13","publicationYear":"1946","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Discussion of “Forecasting stream‐flow of the Salt River, Arizona”","docAbstract":"<p>Matthew I. Rorabaugh (U.S. Geological Survey, Louisville, Kentucky, August 27, 1945)—In regions where snow is not a factor there is some advantage in making forecasts based on the effects of travel time and base flow. However, the runoff which results from precipitation during the period of forecast usually constitutes a substantial portion of the flow in many streams, and accordingly these predictions may be highly speculative.</p><p>The authors state that on March 1 an average of 52 per cent of the winter flow of Parker Creek has passed the gaging station on that creek while only 36 per cent of the winter flow of the Salt River has reached Roosevelt Reservoir. The forecast is based on this lag, which would approximate 16 per cent of the winter flow of the Salt River or about 25 per cent of the flow during March to May. In giving reasons for the lag the authors minimize the effect of accumulated snow, because less than 15 per cent of the Salt River Basin is thought to have accumulated snow. It may be, however, that the snow on this portion of the basin is the principal reason for the lag. The snow cover accumulates at high altitudes, where precipitation is heaviest and temperatures lowest. As losses will be proportionally less in these low‐temperature areas than in the remainder of the basin, it follows that storage of 25 per cent of the flow could result from snow accumulation on less than 15 per cent of the basin.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i003p00441","usgsCitation":"Rorabaugh, M.I., 1946, Discussion of “Forecasting stream‐flow of the Salt River, Arizona”: Eos, Transactions, American Geophysical Union, v. 27, no. 3, p. 441-443, https://doi.org/10.1029/TR027i003p00441.","productDescription":"3 p.","startPage":"441","endPage":"443","costCenters":[],"links":[{"id":379060,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Rorabaugh, M. I.","contributorId":28221,"corporation":false,"usgs":true,"family":"Rorabaugh","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":800510,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214991,"text":"70214991 - 1946 - Report of Committee on Runoff—1944–1945","interactions":[],"lastModifiedDate":"2020-10-05T17:41:15.472723","indexId":"70214991","displayToPublicDate":"1946-10-05T12:31:55","publicationYear":"1946","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—1944–1945","docAbstract":"<p>The membership of the committee has been selected to afford good representation of geographic sections and of organizations engaged in runoff research. Some new members were added during the year in order to strengthen the representation of the committee in certain phases of runoff research. Norbert H. Leupold submitted his resignation in April because his work is no longer directly related to runoff‐research.</p><p>At the beginning of the year members of the committee met to discuss its setup and plans for the future. The committee has two subcommittees, one dealing with floods and the other with subsurface‐flow. The question was considered whether progress might be facilitated by the addition of one or more additional committees dealing with logical classifications of the subject of runoff. The confusion in nomenclature and terminology relating to runoff was discussed,but it was thought that the present time was not fitting for comprehensive consideration of standardization. It was considered important that the writer of a paper dealing with runoff should make clear the usage of terms he follows In his paper. It was emphasized that there is still an important need for better understanding or liaison between groups dealing with the influence of land use on stream‐flow and those dealing with control and development of streams.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i001p00121","usgsCitation":"Davenport, R.W., 1946, Report of Committee on Runoff—1944–1945: Eos, Transactions, American Geophysical Union, v. 27, no. 1, p. 121-123, https://doi.org/10.1029/TR027i001p00121.","productDescription":"3 p.","startPage":"121","endPage":"123","costCenters":[],"links":[{"id":379054,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Davenport, R. W.","contributorId":41798,"corporation":false,"usgs":true,"family":"Davenport","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":800509,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214990,"text":"70214990 - 1946 - Report of the Research Committee on Runoff, 1945–46","interactions":[],"lastModifiedDate":"2020-10-05T17:31:33.542479","indexId":"70214990","displayToPublicDate":"1946-10-05T12:23:07","publicationYear":"1946","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 Research Committee on Runoff, 1945–46","docAbstract":"<p>The variety of usage and even the confusion in the nomenclature and terminology of some fields of hydrology have been often remarked. The Committee on Runoff conceived the idea that it would be profitable to consider some of the terms which are especially pertinent to the field of runoff. That consideration was the principal Committee project of the past year and is featured in this report.</p><p>The Chairman sent a letter to the members of the Committee that was planned to draw out a symposium of opinions on the subject. A good starting point seemed to be the classification of water on the Earth. Meinzer's well‐known classification was given: atmospheric water, surface water, and subsurface or subterranean water. Comments were solicited.</p>","publisher":"American Geophysical Union","doi":"10.1029/TR027i006p00876","usgsCitation":"Davenport, R.W., 1946, Report of the Research Committee on Runoff, 1945–46: Eos, Transactions, American Geophysical Union, v. 27, no. 6, p. 876-878, https://doi.org/10.1029/TR027i006p00876.","productDescription":"3 p.","startPage":"876","endPage":"878","costCenters":[],"links":[{"id":379053,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"6","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Davenport, R. W.","contributorId":41798,"corporation":false,"usgs":true,"family":"Davenport","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":800508,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70214988,"text":"70214988 - 1946 - A generalized graphical method for evaluating formation constants and summarizing well‐field history","interactions":[],"lastModifiedDate":"2020-10-05T17:18:02.929995","indexId":"70214988","displayToPublicDate":"1946-10-05T12:13:43","publicationYear":"1946","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 generalized graphical method for evaluating formation constants and summarizing well‐field history","docAbstract":"<p><span>The capacities of a water‐bearing formation to transmit water under a hydraulic gradient and to yield water from storage when the water table or artesian pressure declines, are generally expressed, respectively, in terms of a coefficient of transmissibility and a coefficient of storage. Determinations of these two constants are almost always involved in quantitative studies of ground‐water problems.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i004p00526","usgsCitation":"Cooper, H., and Jacob, C.E., 1946, A generalized graphical method for evaluating formation constants and summarizing well‐field history: Eos, Transactions, American Geophysical Union, v. 27, no. 4, p. 526-534, https://doi.org/10.1029/TR027i004p00526.","productDescription":"9 p.","startPage":"526","endPage":"534","costCenters":[],"links":[{"id":379052,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Cooper, H.H.","contributorId":62573,"corporation":false,"usgs":true,"family":"Cooper","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":800505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jacob, C. E.","contributorId":64504,"corporation":false,"usgs":true,"family":"Jacob","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":800506,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70214987,"text":"70214987 - 1946 - Activities in tectonics of Research Committee of American Association of Petroleum Geologists","interactions":[],"lastModifiedDate":"2020-10-05T17:05:27.363002","indexId":"70214987","displayToPublicDate":"1946-10-05T11:56:53","publicationYear":"1946","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":"Activities in tectonics of Research Committee of American Association of Petroleum Geologists","docAbstract":"<p><span>During 1945 and 1946, the Research Committee of the American Association of Petroleum Geologists, under the chairmanship of Shepard W. Lowman, has been engaged in “a reconnaissance survey of research in petroleum geology and allied sciences with explicit reference to exploration” in order “to formulate a comprehensive research program which the American Association of Petroleum Geologists may adopt as its recommendation for that research most needed to improve our ability to find oil” [see “References” at end of report, Lowman, 1945]. In order to make this survey, the field was divided among a number of subcommittees, including a Subcommittee on Tectonics, of which the writer was chairman. Preliminary reports, discussing the research possibilities in the various fields covered by the subcommittees, were submitted in January, 1946, and concrete recommendations were formulated by the Research Committee at the Chicago meeting of the Association in April 1946 [Lowman, 1946]. Final reports of the subcommittees will be published later in 1946 in the Bulletin of the American Association of Petroleum Geologists.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR027i005p00713","usgsCitation":"King, P., 1946, Activities in tectonics of Research Committee of American Association of Petroleum Geologists: Eos, Transactions, American Geophysical Union, v. 27, no. 5, p. 713-714, https://doi.org/10.1029/TR027i005p00713.","productDescription":"2 p.","startPage":"713","endPage":"714","costCenters":[],"links":[{"id":379051,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"5","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"King, P.B.","contributorId":221242,"corporation":false,"usgs":false,"family":"King","given":"P.B.","email":"","affiliations":[],"preferred":false,"id":800504,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}