{"pageNumber":"7214","pageRowStart":"180325","pageSize":"25","recordCount":184635,"records":[{"id":32400,"text":"wl105 - 1938 - The Federal Aid to Wildlife Restoration Act","interactions":[],"lastModifiedDate":"2012-02-02T00:16:00","indexId":"wl105","displayToPublicDate":"1970-01-01T12:30:00","publicationYear":"1938","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":"105","title":"The Federal Aid to Wildlife Restoration Act","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Day, A., 1938, The Federal Aid to Wildlife Restoration Act: Wildlife Leaflet 105, 4 p.","productDescription":"4 p.","costCenters":[],"links":[{"id":112357,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015006161924?urlappend=%3Bseq=57"},{"id":204197,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba72ae4b08c986b3213d3","contributors":{"authors":[{"text":"Day, A.M.","contributorId":7406,"corporation":false,"usgs":true,"family":"Day","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":208514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32399,"text":"wl104 - 1938 - The status of wildlife research: 1937.","interactions":[],"lastModifiedDate":"2012-02-02T00:16:00","indexId":"wl104","displayToPublicDate":"1970-01-01T12:29:00","publicationYear":"1938","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":"104","title":"The status of wildlife research: 1937.","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"McAtee, W., 1938, The status of wildlife research: 1937.: Wildlife Leaflet 104, 30 p.","productDescription":"30 p.","costCenters":[],"links":[{"id":112356,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015006161924?urlappend=%3Bseq=27"},{"id":204196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb077e4b08c986b324e92","contributors":{"authors":[{"text":"McAtee, W.L.","contributorId":95176,"corporation":false,"usgs":true,"family":"McAtee","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":208513,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212847,"text":"70212847 - 1938 - The significance and nature of the cone of depression in ground-water bodies","interactions":[],"lastModifiedDate":"2020-08-31T14:57:33.866613","indexId":"70212847","displayToPublicDate":"1938-12-01T09:54:52","publicationYear":"1938","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 significance and nature of the cone of depression in ground-water bodies","docAbstract":"<p><span>In nature the hydraulic system in an aquifer is in balance; the discharge is equal to the recharge and the water table or other piezometric surface is more or less fixed in position. Discharge by wells is a new discharge superimposed on the previous system. Before a new equilibrium can be established water levels must fall throughout the aquifer to an extent sufficient to reduce the natural discharge or increase the recharge by an amount equal to the amount discharged by the well. Until this new equilibrium is established water must be withdrawnfrom storage in the aquifer and conversely the new equilibrium cannot be established until an amount of water is withdrawn from storage by the well sufficient to depress the piezometric surface enough to change the recharge or natural discharge the proper amount. The depression of the piezometric surface is called the cone of depression.The characteristics of the cone of depression in an idealized aquifer of infinite areal extent are considered mathematically. Time is an essential variable in the description of this cone. The time rate of lateral growth of the cone is independent of the rate of discharge by the well and depends only on the physical characteristics of the aquifer. The cone must grow laterally much more rapidly in artesian aquifers than it does in nonartesian. The characteristics of the cone in actual aquifers are then considered. In finely porous artesian aquifers the cone appears to be much like the cone in the ideal aquifer. The cone in non-artesian aquifers must be somewhat warped. The theory out-lined implies that well discharge from extensive water-table aquifers must be a draft on storage in the aquifer for many generations.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.33.8.889","usgsCitation":"Theis, C.V., 1938, The significance and nature of the cone of depression in ground-water bodies: Economic Geology, v. 33, no. 8, p. 889-902, https://doi.org/10.2113/gsecongeo.33.8.889.","productDescription":"4 p.","startPage":"889","endPage":"902","costCenters":[],"links":[{"id":378033,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"8","noUsgsAuthors":false,"publicationDate":"1938-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Theis, Charles V.","contributorId":48080,"corporation":false,"usgs":true,"family":"Theis","given":"Charles","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":797699,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207439,"text":"70207439 - 1938 - Sulphate minerals of the Comstock Lode, Nevada","interactions":[],"lastModifiedDate":"2019-12-19T11:35:37","indexId":"70207439","displayToPublicDate":"1938-11-01T11:30:27","publicationYear":"1938","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":"Sulphate minerals of the Comstock Lode, Nevada","docAbstract":"<p><span>Seventeen representative samples of supergene sulphates from old workings on the Comstock Lode are described. They range from simple minerals such as gypsum and epsomite to complex aggregates of four or more distinct species. All are well known species except a mineral of the copper (chalcanthite) or magnesium sulphate pentahydrate group, with about half the magnesium replaced by copper, zinc, ferrous iron, and manganese. Four new analyses of Comstock Lode mine waters are given. © 1938 Society of Economic Geologists, Inc.</span></p>","language":"English","publisher":"Society of Economic Geologists ","doi":"10.2113/gsecongeo.33.7.749","issn":"03610128","usgsCitation":"Milton, C., and Johnston, W.D., 1938, Sulphate minerals of the Comstock Lode, Nevada: Economic Geology, v. 33, no. 7, p. 749-771, https://doi.org/10.2113/gsecongeo.33.7.749.","productDescription":"23 p. 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,{"id":70211631,"text":"70211631 - 1938 - Dolomite and jasperoid in the Metaline District, northeastern Washington","interactions":[],"lastModifiedDate":"2020-08-05T16:22:02.125663","indexId":"70211631","displayToPublicDate":"1938-11-01T11:12:34","publicationYear":"1938","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":"Dolomite and jasperoid in the Metaline District, northeastern Washington","docAbstract":"<p><span>The replacement ore bodies of the Metaline zinc-lead district, in northeastern Washington are limited to the greatly disturbed fault block through which the Pend Oreille River flows and are associated with the major faults but are not in them. They are mostly near the top of the Metaline limestone, of Middle Cambrian age, and below black Ordovician slate. The ores are generally in jasperoid and are surrounded by a shell of crystalline dolomite. Outside of the dolomite is a shell of coarse-grained calcite that in places was deposited along solution channels long distances from known ore bodies. Jasperoid, crystalline dolomite, and, to a less extent, coarse-grained calcite are therefore favorable but not infallible signs of the presence of ore nearby. The Metaline limestone was dolomitized regionally before the ore was introduced, and this early dolomitization is independent of the ore.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.33.7.709","usgsCitation":"Park, C., 1938, Dolomite and jasperoid in the Metaline District, northeastern Washington: Economic Geology, v. 33, no. 7, p. 709-729, https://doi.org/10.2113/gsecongeo.33.7.709.","productDescription":"21 p.","startPage":"709","endPage":"729","costCenters":[],"links":[{"id":377044,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Metaline District","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -117.52349853515625,\n              48.60113322190171\n            ],\n            [\n              -117.21725463867186,\n              48.60113322190171\n            ],\n            [\n              -117.21725463867186,\n              48.996438064932285\n            ],\n            [\n              -117.52349853515625,\n              48.996438064932285\n            ],\n            [\n              -117.52349853515625,\n              48.60113322190171\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"33","issue":"7","noUsgsAuthors":false,"publicationDate":"1938-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Park, Charles Frederick","contributorId":236987,"corporation":false,"usgs":false,"family":"Park","given":"Charles Frederick","affiliations":[],"preferred":false,"id":794874,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220004,"text":"70220004 - 1938 - Mediterranean sediments and pleistocene sea levels","interactions":[],"lastModifiedDate":"2021-04-16T17:35:51.395758","indexId":"70220004","displayToPublicDate":"1938-10-21T12:29:56","publicationYear":"1938","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Mediterranean sediments and pleistocene sea levels","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"AAAS","doi":"10.1126/science.88.2286.376","usgsCitation":"Bradley, W., 1938, Mediterranean sediments and pleistocene sea levels: Science, v. 88, no. 2286, p. 376-379, https://doi.org/10.1126/science.88.2286.376.","productDescription":"4 p.","startPage":"376","endPage":"379","costCenters":[],"links":[{"id":385168,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"2286","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bradley, W.H.","contributorId":220222,"corporation":false,"usgs":false,"family":"Bradley","given":"W.H.","email":"","affiliations":[],"preferred":false,"id":814425,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38040,"text":"38040 - 1938 - Two home-made traps for English sparrows","interactions":[],"lastModifiedDate":"2014-07-21T11:48:41","indexId":"38040","displayToPublicDate":"1938-10-01T11:47:57","publicationYear":"1938","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":"121","title":"Two home-made traps for English sparrows","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","collaboration":"Prepared in the Section of Food Habits, Division of Wildlife Research.","usgsCitation":"U.S. Bureau of Biological Survey, 1938, Two home-made traps for English sparrows: Wildlife Leaflet 121, 6 p.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":290564,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd79d3e4b0b2908510d13d","contributors":{"authors":[{"text":"U.S. Bureau of Biological Survey","contributorId":128079,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Biological Survey","id":529813,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38039,"text":"38039 - 1938 - Botulism, a recurring hazard to waterfowl: with notes on recent outbreaks in the United States and Canada, and Australia","interactions":[],"lastModifiedDate":"2014-07-21T11:45:35","indexId":"38039","displayToPublicDate":"1938-09-01T11:45:05","publicationYear":"1938","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":"120","title":"Botulism, a recurring hazard to waterfowl: with notes on recent outbreaks in the United States and Canada, and Australia","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Kalmbach, E., 1938, Botulism, a recurring hazard to waterfowl: with notes on recent outbreaks in the United States and Canada, and Australia: Wildlife Leaflet 120, 8 p.","productDescription":"8 p.","numberOfPages":"8","costCenters":[],"links":[{"id":290563,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4fbee4b0b290850f2e5a","contributors":{"authors":[{"text":"Kalmbach, E.R.","contributorId":21610,"corporation":false,"usgs":true,"family":"Kalmbach","given":"E.R.","email":"","affiliations":[],"preferred":false,"id":218766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38038,"text":"38038 - 1938 - The coordination of mosquito control with wildlife conservation","interactions":[],"lastModifiedDate":"2014-07-21T11:42:01","indexId":"38038","displayToPublicDate":"1938-09-01T11:41:27","publicationYear":"1938","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":"119","title":"The coordination of mosquito control with wildlife conservation","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Cottam, C., 1938, The coordination of mosquito control with wildlife conservation: Wildlife Leaflet 119, 6 p.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":290561,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7788e4b0b2908510b99d","contributors":{"authors":[{"text":"Cottam, Clarence","contributorId":41490,"corporation":false,"usgs":true,"family":"Cottam","given":"Clarence","email":"","affiliations":[],"preferred":false,"id":218765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206679,"text":"70206679 - 1938 - Volcanic activity at Magnet Cove, Arkansas","interactions":[],"lastModifiedDate":"2019-11-16T17:18:18","indexId":"70206679","displayToPublicDate":"1938-08-31T17:10:52","publicationYear":"1938","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":"Volcanic activity at Magnet Cove, Arkansas","docAbstract":"<p><span>The igneous rocks and the minerals of Magnet Cove, Arkansas, have long interested geologists and mineralogists, but in much of the area rock‐exposures are so sparse that many of the geologic, relations have remained obscure. However, recent prospecting and the mining of titanium ores have uncovered rocks that throw new light on the geology of the region. The regional rocks of the area are sandstones, slates, and novaculite of Paleozoic age. They were folded and underwent metamorphism in late Paleozoic time. In Cretaceous time they were intruded by a series of igneous rocks. ©1938. American Geophysical Union. All Rights Reserved.</span></p>","language":"English ","publisher":"American Geophysical Union","doi":"10.1029/TR019i001p00263-2","issn":"00028606","usgsCitation":"Ross, C.S., 1938, Volcanic activity at Magnet Cove, Arkansas: Eos, Transactions, American Geophysical Union, v. 19, no. 1, p. 263-264, https://doi.org/10.1029/TR019i001p00263-2.","productDescription":"2 p.","startPage":"263","endPage":"264","costCenters":[],"links":[{"id":369264,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"Arkansas ","county":"Hot Spring","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-92.6691,34.414],[-92.6696,34.4072],[-92.6694,34.3922],[-92.6723,34.2686],[-92.6737,34.239],[-92.6765,34.239],[-92.6774,34.1499],[-92.794,34.151],[-92.8406,34.1539],[-92.8667,34.155],[-92.8767,34.1559],[-92.8867,34.1558],[-92.9222,34.1564],[-92.9361,34.1572],[-92.9517,34.1576],[-92.9644,34.1579],[-92.9917,34.159],[-92.9956,34.1595],[-92.9994,34.1594],[-93.0239,34.1601],[-93.0261,34.1606],[-93.03,34.1587],[-93.0311,34.1569],[-93.0333,34.155],[-93.0355,34.1546],[-93.04,34.1591],[-93.0417,34.1618],[-93.0429,34.1718],[-93.043,34.1772],[-93.0414,34.1818],[-93.0387,34.1868],[-93.0365,34.1918],[-93.0343,34.195],[-93.031,34.1969],[-93.0299,34.1982],[-93.0294,34.2005],[-93.0261,34.2015],[-93.0278,34.206],[-93.0268,34.2105],[-93.0307,34.2128],[-93.0346,34.2155],[-93.0346,34.2173],[-93.0302,34.2196],[-93.0302,34.221],[-93.0386,34.2213],[-93.0397,34.2227],[-93.0381,34.2263],[-93.0337,34.2296],[-93.0332,34.2337],[-93.0349,34.2368],[-93.0471,34.2367],[-93.0499,34.2353],[-93.0566,34.2375],[-93.0721,34.2351],[-93.0771,34.2364],[-93.0782,34.2351],[-93.081,34.2351],[-93.0799,34.2391],[-93.0822,34.2396],[-93.0849,34.2377],[-93.0843,34.2355],[-93.091,34.2372],[-93.0911,34.2409],[-93.0911,34.2418],[-93.095,34.2449],[-93.1167,34.2452],[-93.164,34.247],[-93.1829,34.2468],[-93.199,34.2471],[-93.1983,34.2771],[-93.2078,34.277],[-93.2223,34.2777],[-93.2339,34.2781],[-93.3196,34.2794],[-93.3502,34.2799],[-93.3524,34.2799],[-93.3569,34.2803],[-93.3562,34.3385],[-93.4074,34.3397],[-93.4071,34.3838],[-93.4074,34.397],[-93.4018,34.3966],[-93.3879,34.3968],[-93.3533,34.3962],[-93.3361,34.396],[-92.9885,34.3895],[-92.9501,34.3898],[-92.948,34.4489],[-92.9452,34.4489],[-92.9436,34.4489],[-92.9135,34.4482],[-92.9136,34.5055],[-92.7937,34.5036],[-92.7384,34.5031],[-92.7393,34.4735],[-92.6986,34.4733],[-92.6874,34.4734],[-92.6852,34.4693],[-92.6856,34.4584],[-92.6856,34.4539],[-92.6855,34.4471],[-92.6855,34.4453],[-92.6864,34.4143],[-92.6691,34.414]]]},\"properties\":{\"name\":\"Hot Spring\",\"state\":\"AR\"}}]}","volume":"19","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Ross, C. S.","contributorId":18337,"corporation":false,"usgs":true,"family":"Ross","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":775354,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206635,"text":"70206635 - 1938 - Igneous activity in the Comstock District, Nevada","interactions":[],"lastModifiedDate":"2024-09-24T17:54:41.442648","indexId":"70206635","displayToPublicDate":"1938-08-31T12:12:15","publicationYear":"1938","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}},"displayTitle":"Igneous activity in the Comstock District, Nevada","title":"Igneous activity in the Comstock District, Nevada","docAbstract":"<p><span>The oldest igneous rocks in the Comstock District are amphibolites probably derived from basalts and of Triassic age. These are intruded by pre‐Tertiary quartz monzonlte and by granodiorite of Sierran facies, the latter not being exposed on the surface but found on mine‐dumps. Igneous activity recorded mainly in volcanic rocks was almost continuous throughout the Tertiary. Its products, in order of age, were as follows: Eocene—Rhyolitic flows aggregating a few hundred feet in thickness: One intrusive plug of rhyolite occurs. Eocene or Miocene—Hornblende‐auglte andesite intrusive into the rhyolite, type locality American Ravine. ©1938. American Geophysical Union. All Rights Reserved.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i001p00262-1","issn":"00028606","usgsCitation":"Calkins, F.C., 1938, Igneous activity in the Comstock District, Nevada: Eos, Transactions, American Geophysical Union, v. 19, no. 1, p. 262-262, https://doi.org/10.1029/TR019i001p00262-1.","productDescription":"1 p.","startPage":"262","endPage":"262","costCenters":[],"links":[{"id":369206,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70207440,"text":"70207440 - 1938 - Diabase dikes of the Franklin Furnace, New Jersey, quadrangle","interactions":[],"lastModifiedDate":"2019-12-19T11:39:58","indexId":"70207440","displayToPublicDate":"1938-08-31T11:36:06","publicationYear":"1938","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":"Diabase dikes of the Franklin Furnace, New Jersey, quadrangle","docAbstract":"<p><span>Two of the numerous small dikes mapped on the areal geology sheet of the Franklin Furnace Folio (U.S. Geological Survey 161) as “Mostly basic, including nepheline tinguaite, leucite tinguaite, and camptonite” of post‐Ordovician age, have been found to be quite distinct from these alkalic rocks, and the two dikes in question are indistinguishable from the Triassic diabase found elsewhere in New Jersey and adjoining States. The association of diabase with highly alkalic rocks has been observed and commented on by numerous writers. There is evidence pointing to the post‐Triassic age of the Beemerville alkaline rocks, and a possible correlation with a volcanic ash of Cretaceous age found by Stephenson and Carter at Haddonfield, New Jersey, near Camden, in 1936. ©1938. American Geophysical Union. All Rights Reserved.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i001p00264-1","issn":" 00028606","usgsCitation":"Milton, C., 1938, Diabase dikes of the Franklin Furnace, New Jersey, quadrangle: Eos, Transactions, American Geophysical Union, v. 19, no. 1, p. 264-264, https://doi.org/10.1029/TR019i001p00264-1.","productDescription":"1 p. ","startPage":"264","endPage":"264","costCenters":[],"links":[{"id":370484,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States ","state":"New Jersey ","otherGeospatial":"Franklin Furnace, New Jersey, quadrangle","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-74.3677,41.2033],[-74.4886,41.0988],[-74.4996,41.0889],[-74.5026,41.0857],[-74.5203,41.0716],[-74.5301,41.063],[-74.5356,41.058],[-74.5465,41.0485],[-74.5477,41.0467],[-74.549,41.0457],[-74.5976,41.0031],[-74.5994,41.0017],[-74.6013,40.9999],[-74.6031,40.9985],[-74.6043,40.9972],[-74.6074,40.9949],[-74.611,40.9922],[-74.6414,40.9627],[-74.6426,40.9618],[-74.6426,40.959],[-74.6407,40.9563],[-74.6389,40.9549],[-74.6365,40.9527],[-74.6359,40.9518],[-74.6353,40.9495],[-74.6353,40.9477],[-74.6353,40.9463],[-74.6352,40.9454],[-74.6371,40.9409],[-74.6401,40.9373],[-74.6407,40.9368],[-74.6413,40.9363],[-74.6498,40.9318],[-74.651,40.9309],[-74.6523,40.93],[-74.6529,40.9291],[-74.6541,40.9268],[-74.6528,40.9245],[-74.6522,40.9236],[-74.6528,40.9214],[-74.6535,40.9209],[-74.6547,40.9205],[-74.6571,40.92],[-74.6577,40.92],[-74.6589,40.9195],[-74.662,40.9173],[-74.6638,40.9159],[-74.6735,40.9114],[-74.6905,40.9068],[-74.6978,40.9045],[-74.7051,40.8991],[-74.7106,40.8995],[-74.7124,40.9018],[-74.7136,40.9049],[-74.7148,40.9086],[-74.7191,40.9122],[-74.7252,40.9149],[-74.7301,40.9144],[-74.7343,40.9162],[-74.7355,40.9181],[-74.7386,40.919],[-74.7422,40.9189],[-74.7471,40.9158],[-74.7507,40.9144],[-74.7556,40.9126],[-74.7598,40.9126],[-74.7684,40.9112],[-74.827,40.9632],[-74.8416,40.9772],[-74.8655,41.0003],[-74.8716,41.0057],[-74.8734,41.0071],[-74.8802,41.0134],[-74.8863,41.0198],[-74.8894,41.0229],[-74.9016,41.0338],[-74.939,41.069],[-74.9408,41.0709],[-74.9525,41.0812],[-74.9659,41.0939],[-74.9658,41.0953],[-74.9664,41.0967],[-74.9676,41.0971],[-74.9702,41.0966],[-74.9719,41.096],[-74.9727,41.0957],[-74.975,41.0941],[-74.9768,41.0926],[-74.98,41.091],[-74.983,41.0893],[-74.9854,41.0888],[-74.988,41.0885],[-74.9899,41.0888],[-74.9911,41.0901],[-74.9915,41.0915],[-74.9915,41.0926],[-74.9909,41.0935],[-74.989,41.0962],[-74.9886,41.097],[-74.9867,41.1002],[-74.9837,41.1056],[-74.9807,41.1084],[-74.9775,41.111],[-74.9771,41.1114],[-74.9758,41.112],[-74.9728,41.1136],[-74.9716,41.1136],[-74.9697,41.1138],[-74.9667,41.114],[-74.9652,41.1144],[-74.9624,41.1157],[-74.9594,41.118],[-74.9564,41.1192],[-74.9556,41.1197],[-74.9521,41.1216],[-74.9495,41.1231],[-74.9485,41.1244],[-74.9471,41.1258],[-74.9465,41.1277],[-74.9442,41.1294],[-74.943,41.1303],[-74.9406,41.1312],[-74.9381,41.1317],[-74.9346,41.1333],[-74.9302,41.1353],[-74.9242,41.139],[-74.9196,41.1416],[-74.915,41.1458],[-74.9108,41.15],[-74.9084,41.1526],[-74.905,41.1568],[-74.9017,41.1626],[-74.8999,41.1658],[-74.8985,41.1675],[-74.8972,41.1697],[-74.8957,41.1713],[-74.8935,41.1729],[-74.8916,41.1741],[-74.8884,41.1758],[-74.8853,41.179],[-74.8834,41.1812],[-74.8829,41.1819],[-74.8814,41.1844],[-74.8805,41.1861],[-74.8799,41.1881],[-74.8788,41.1904],[-74.8775,41.1931],[-74.8744,41.1977],[-74.8714,41.2022],[-74.8688,41.2062],[-74.8672,41.2086],[-74.8648,41.2118],[-74.8629,41.214],[-74.8621,41.2149],[-74.8613,41.2162],[-74.8598,41.2193],[-74.8593,41.2216],[-74.8599,41.2233],[-74.8605,41.224],[-74.8612,41.2249],[-74.8636,41.2272],[-74.8657,41.2294],[-74.8662,41.2322],[-74.8661,41.2335],[-74.8629,41.237],[-74.8618,41.239],[-74.8612,41.2417],[-74.86,41.244],[-74.8594,41.2459],[-74.8571,41.2483],[-74.8551,41.2506],[-74.852,41.2523],[-74.8497,41.2531],[-74.8461,41.2559],[-74.8442,41.2594],[-74.8442,41.2604],[-74.8436,41.2631],[-74.843,41.2658],[-74.8418,41.269],[-74.8402,41.2709],[-74.8392,41.2729],[-74.8389,41.2752],[-74.8376,41.2779],[-74.8358,41.2799],[-74.8338,41.2823],[-74.8319,41.2851],[-74.8299,41.2877],[-74.828,41.29],[-74.8254,41.2922],[-74.8223,41.2943],[-74.8218,41.2946],[-74.8193,41.2958],[-74.8163,41.2976],[-74.8126,41.2999],[-74.8077,41.3027],[-74.8017,41.3063],[-74.796,41.3088],[-74.7945,41.3103],[-74.7937,41.3109],[-74.7932,41.3117],[-74.7925,41.3127],[-74.7925,41.3145],[-74.7931,41.3159],[-74.7944,41.3172],[-74.795,41.3186],[-74.7949,41.3207],[-74.7937,41.3219],[-74.7925,41.3228],[-74.79,41.3237],[-74.787,41.324],[-74.7846,41.3244],[-74.7802,41.3243],[-74.7764,41.325],[-74.7754,41.3253],[-74.773,41.3259],[-74.7697,41.3269],[-74.767,41.3283],[-74.7651,41.33],[-74.7633,41.3331],[-74.7619,41.3362],[-74.7602,41.3391],[-74.7581,41.3411],[-74.7571,41.3422],[-74.7537,41.3442],[-74.7506,41.3455],[-74.7461,41.3464],[-74.742,41.3471],[-74.7396,41.3473],[-74.7364,41.3475],[-74.7322,41.3469],[-74.7278,41.3469],[-74.7247,41.3473],[-74.7211,41.3485],[-74.7161,41.3502],[-74.7113,41.3519],[-74.7062,41.3532],[-74.7052,41.3536],[-74.7019,41.3549],[-74.6955,41.3576],[-74.6492,41.3359],[-74.605,41.3152],[-74.5363,41.284],[-74.4101,41.2248],[-74.3831,41.2111],[-74.3677,41.2033]]]},\"properties\":{\"name\":\"Sussex\",\"state\":\"NJ\"}}]}","volume":"19","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Milton, C.","contributorId":221243,"corporation":false,"usgs":false,"family":"Milton","given":"C.","email":"","affiliations":[],"preferred":false,"id":778045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212725,"text":"70212725 - 1938 - Role of physical chemistry in stratigraphic problems","interactions":[],"lastModifiedDate":"2020-08-26T18:59:03.354272","indexId":"70212725","displayToPublicDate":"1938-08-26T13:45:35","publicationYear":"1938","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":"Role of physical chemistry in stratigraphic problems","docAbstract":"<p><span>Stratigraphy is concerned mainly with the genesis and interpretation of stratified rocks, which include some of wide extent and of great scientific as well as economic interest that are largely of chemical rather than of detrital origin. Chemical agencies have been recognized to some extent in genetic studies of these rocks, but little work has been done approaching in maturity the type of study now given to the genesis of igneous rocks and of ores, in which physical chemistry plays so important a part.A plea is presented to geologists with training in physical chemistry to interest themselves in stratigraphic problems that involve the use of this science. Examples cited are the phosphate beds and bedded cherts of the Phosphoria formation in Idaho and adjacent States and the potash-bearing Salado halite of the Permian basin in New Mexico and Texas. The interplay of ions in the solutions from which these formations were derived must have been controlled by such conditions as temperature, pressure, degree of concentration, and the like. Possibly laboratory study would enable us to reproduce these conditions and results and thus better interpret the geologic history of the times when these formations were built.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.32.5.533","usgsCitation":"Mansfield, G., 1938, Role of physical chemistry in stratigraphic problems: Economic Geology, v. 32, no. 5, p. 335-549, https://doi.org/10.2113/gsecongeo.32.5.533.","productDescription":"27 p.","startPage":"335","endPage":"549","costCenters":[],"links":[{"id":377907,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"5","noUsgsAuthors":false,"publicationDate":"1937-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Mansfield, George R.","contributorId":76186,"corporation":false,"usgs":true,"family":"Mansfield","given":"George R.","affiliations":[],"preferred":false,"id":797363,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212724,"text":"70212724 - 1938 - Precipitation and vegetation","interactions":[],"lastModifiedDate":"2020-08-26T18:42:42.168712","indexId":"70212724","displayToPublicDate":"1938-08-26T13:42:11","publicationYear":"1938","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":"Precipitation and vegetation","docAbstract":"<p><span>As time marches on, historians are usually quite faithful in recording the activities of man, and it will usually be found that Mother Nature is even more meticulous in reflecting and preserving her experiences, more especially with regard to climate and vegetation. Just how much the activities of man have done to modify the natural conditions of a virgin country may in some respects always remain a question. There is however, no longer the slightest doubt about the influence civilization may have had on the climate—which is none at all! And it is the purpose of the present paper to introduce a few trustworthy witnesses in support of the hypothesis that the activities of man have also been ineffective with respect to noteworthy changes in the general aspect of the native vegetation, outside the ranch‐fences of the West.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i002p00604","usgsCitation":"Woolley, R., and Alter, J., 1938, Precipitation and vegetation: Eos, Transactions, American Geophysical Union, v. 19, no. 2, p. 804-807, https://doi.org/10.1029/TR019i002p00604.","productDescription":"4 p.","startPage":"804","endPage":"807","costCenters":[],"links":[{"id":377903,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Woolley, Ralf R.","contributorId":45301,"corporation":false,"usgs":true,"family":"Woolley","given":"Ralf R.","affiliations":[],"preferred":false,"id":797361,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alter, J.C.","contributorId":239605,"corporation":false,"usgs":false,"family":"Alter","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":797362,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212723,"text":"70212723 - 1938 - A recording evaporimeter","interactions":[],"lastModifiedDate":"2020-08-26T18:20:55.614369","indexId":"70212723","displayToPublicDate":"1938-08-26T13:13:11","publicationYear":"1938","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 recording evaporimeter","docAbstract":"<p>The instrument herein described was originally designed and built to record the evaporation‐loss from a standard Weather Bureau pan for use in a study of the variation of flow in Santa Ana River. Valuable suggestions were made by various members of the Water Resources Branch of the Geological Survey in Southern California, and financial assistance for construction was given by F. C. Ebert and H. C. Troxell of the same organization. The typing of the paper and some of the drafting were done by Works Progress Administration help.</p><p>The original instrument was damaged by flood‐waters in 1934, while in operation at Baldwin Park, California. It was then redesigned and constructed of stainless materials and installed on the campus of the San Bernardino Valley Junior College. The Weather Bureau pan was replaced by a thermally insulated pan. The damping unit was added at this time by the present writers. The evaporimeter was placed in regular operation on October 30, 1937, in a study of the relative magnitudes of the various energy‐components associated with solar and sky radiation and with evaporation from water‐surfaces, from damp soil, and from plants.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i002p00609","usgsCitation":"Oliver, J., and Cummings, N., 1938, A recording evaporimeter: Eos, Transactions, American Geophysical Union, v. 19, no. 2, p. 609-612, https://doi.org/10.1029/TR019i002p00609.","productDescription":"4 p.","startPage":"609","endPage":"612","costCenters":[],"links":[{"id":377902,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Oliver, J.","contributorId":167156,"corporation":false,"usgs":false,"family":"Oliver","given":"J.","affiliations":[],"preferred":false,"id":797359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, N.W.","contributorId":239604,"corporation":false,"usgs":false,"family":"Cummings","given":"N.W.","email":"","affiliations":[],"preferred":false,"id":797360,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212722,"text":"70212722 - 1938 - Ground‐water for air‐conditioning on Long Island, New York","interactions":[],"lastModifiedDate":"2020-08-26T18:02:47.291952","indexId":"70212722","displayToPublicDate":"1938-08-26T12:52:04","publicationYear":"1938","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":"Ground‐water for air‐conditioning on Long Island, New York","docAbstract":"<p><span>During the last five years ground‐water has been more and more extensively used for air‐conditioning on Long Island, New York. The wide‐spread occurrence of highly permeable water‐bearing material and the relatively small cost of installation and operation of a ground‐water, air‐conditioning system has resulted in many such installations by theaters, restaurants, stores, and other establishments. Many companies likewise have taken advantage of these favorable factors and are utilizing low‐temperature ground‐water for cooling purposes in the manufacture of ice. This new use of ground‐water has considerably increased the draft in the western end of Long Island where there had already been so much over‐development that the watertable was below sea‐level in an area of more than 40 square miles. In 1933 the State Legislature, recognizing the seriousness of this over‐development, passed a law requiring that the approval, of the State Water Power and Control Commission be secured before constructing a well with a capacity greater than 100,000 gallons a day. Since the passage of the law the‐policy of the Commission has been to require water pumped from new‐wells for cooling purposes to be returned to the ground. This requirement has resulted in the construction of many recharge‐wells (locally called diffusion‐wells) through which the warm water is returned to the ground.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i001p00412","usgsCitation":"Leggette, R., and Brashears, M., 1938, Ground‐water for air‐conditioning on Long Island, New York: Eos, Transactions, American Geophysical Union, v. 19, no. 1, p. 412-418, https://doi.org/10.1029/TR019i001p00412.","productDescription":"7 p.","startPage":"412","endPage":"418","costCenters":[],"links":[{"id":377901,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -74.04922485351562,\n              40.564937785967224\n            ],\n            [\n              -73.80752563476562,\n              40.564937785967224\n            ],\n            [\n              -73.80752563476562,\n              40.77430186363723\n            ],\n            [\n              -74.04922485351562,\n              40.77430186363723\n            ],\n            [\n              -74.04922485351562,\n              40.564937785967224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"19","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":797357,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brashears, M.L. Jr.","contributorId":23212,"corporation":false,"usgs":true,"family":"Brashears","given":"M.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":797358,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212721,"text":"70212721 - 1938 - Some mineral deposits of Glacier Bay and vicinity, Alaska","interactions":[],"lastModifiedDate":"2020-08-26T17:43:08.598011","indexId":"70212721","displayToPublicDate":"1938-08-26T12:39:43","publicationYear":"1938","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":"Some mineral deposits of Glacier Bay and vicinity, Alaska","docAbstract":"<p><span>Prospecting in the Glacier Bay National Monument has been confined so far to granitic rocks near contacts with Paleozoic sediments, which they intrude.Near Reid Glacier thin veins, a few of which are traceable for about 300 feet both horizontaliy and vertically, trend northerly and carry sphalerite, galena, and pyrite. Gold was panned from some of the better looking material.Near Sandy Cove, 30 miles away, more irregular, but locally thicker, veins appear to carry only pyrite. Here pyrite also occurs along the contact between the granitic rocks and the intruded limestone.Sparse ore minerals have been seen at other places in and near the monument. As yet, no large mineral deposits have been found there, but many miles of igneous contacts have not been prospected. In southeastern Alaska, as elsewhere, such contacts are considered favorable places in which to search for mineral deposits.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.33.1.52","usgsCitation":"Reed, J., 1938, Some mineral deposits of Glacier Bay and vicinity, Alaska: Economic Geology, v. 33, no. 1, p. 53-78, https://doi.org/10.2113/gsecongeo.33.1.52.","productDescription":"29 p.","startPage":"53","endPage":"78","costCenters":[],"links":[{"id":377900,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Glacier Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -139.46044921875,\n              55.85064987433714\n            ],\n            [\n              -131.484375,\n              55.85064987433714\n            ],\n            [\n              -131.484375,\n              59.77852198502987\n            ],\n            [\n              -139.46044921875,\n              59.77852198502987\n            ],\n            [\n              -139.46044921875,\n              55.85064987433714\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"33","issue":"1","noUsgsAuthors":false,"publicationDate":"1938-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Reed, John Calvin","contributorId":10769,"corporation":false,"usgs":true,"family":"Reed","given":"John Calvin","affiliations":[],"preferred":false,"id":797356,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70212720,"text":"70212720 - 1938 - Block diagrams","interactions":[],"lastModifiedDate":"2020-08-26T17:37:56.568717","indexId":"70212720","displayToPublicDate":"1938-08-26T12:29:29","publicationYear":"1938","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":"Block diagrams","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.33.1.107","usgsCitation":"Johnston, W.D., and Nolan, B.T., 1938, Block diagrams: Economic Geology, v. 33, no. 1, p. 107-108, https://doi.org/10.2113/gsecongeo.33.1.107.","productDescription":"2 p.","startPage":"107","endPage":"108","costCenters":[],"links":[{"id":377896,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationDate":"1938-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Johnston, W. D. Jr.","contributorId":27193,"corporation":false,"usgs":true,"family":"Johnston","given":"W.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":797350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nolan, B. Thomas 0000-0002-6945-9659","orcid":"https://orcid.org/0000-0002-6945-9659","contributorId":8905,"corporation":false,"usgs":true,"family":"Nolan","given":"B.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":true,"id":797351,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70212718,"text":"70212718 - 1938 - Effect of a sea-level canal on the ground-water level of Florida","interactions":[],"lastModifiedDate":"2020-08-26T17:18:35.013879","indexId":"70212718","displayToPublicDate":"1938-08-26T12:07:34","publicationYear":"1938","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":"Effect of a sea-level canal on the ground-water level of Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.33.1.87","usgsCitation":"Thompson, D.G., Meinzer, O.E., and Stringfield, V.T., 1938, Effect of a sea-level canal on the ground-water level of Florida: Economic Geology, v. 33, no. 1, p. 87-107, https://doi.org/10.2113/gsecongeo.33.1.87.","productDescription":"21 p.","startPage":"87","endPage":"107","costCenters":[],"links":[{"id":377893,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"1","noUsgsAuthors":false,"publicationDate":"1938-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Thompson, David Grosh","contributorId":19141,"corporation":false,"usgs":true,"family":"Thompson","given":"David","email":"","middleInitial":"Grosh","affiliations":[],"preferred":false,"id":797347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meinzer, Oscar Edward","contributorId":12020,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"Edward","affiliations":[],"preferred":false,"id":797348,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stringfield, V. T.","contributorId":72369,"corporation":false,"usgs":true,"family":"Stringfield","given":"V.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":797349,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70212717,"text":"70212717 - 1938 - Evaporation and runoff from snow in the Alpine Zone of our western mountains","interactions":[],"lastModifiedDate":"2020-08-26T17:06:53.405337","indexId":"70212717","displayToPublicDate":"1938-08-26T11:52:30","publicationYear":"1938","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":"Evaporation and runoff from snow in the Alpine Zone of our western mountains","docAbstract":"<p><span>In this informal paper the processes of snow‐wastage at high altitudes were discussed and a number of slides illustrating&nbsp;</span><span>suncups</span><span>&nbsp;and&nbsp;</span><span>sunpits</span><span>&nbsp;in different stages of development were shown. It was stressed that these features are peculiar to the region above the timber‐line, which biologists term the Alpine, or Arctic‐Alpine, Zone. That regions is, as a matter of fact, primarily and fundamentally a physiographic zone distinct from all other physiographic zones at lower levels by reason of an unusual combination of climatic, hydrologic, and geologic factors.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR019i002p00662-1","usgsCitation":"Matthes, F.E., 1938, Evaporation and runoff from snow in the Alpine Zone of our western mountains: Eos, Transactions, American Geophysical Union, v. 19, no. 2, https://doi.org/10.1029/TR019i002p00662-1.","productDescription":"1p.","startPage":"662","costCenters":[],"links":[{"id":377892,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Matthes, Francois E.","contributorId":97963,"corporation":false,"usgs":true,"family":"Matthes","given":"Francois","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":797346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211633,"text":"70211633 - 1938 - Manganese deposits of the Drum Mountains, Utah","interactions":[],"lastModifiedDate":"2020-08-05T16:38:05.799424","indexId":"70211633","displayToPublicDate":"1938-08-01T11:31:43","publicationYear":"1938","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":"Manganese deposits of the Drum Mountains, Utah","docAbstract":"<p><span>More than 15,000 tons of manganese ore has been produced from small deposits in the Drum Mountains in west-central Utah. Lenses of rhodochrosite, now largely weathered near the surface to manganese oxides, lie parallel to the bedding of Cambrian dolomites and shales near faults that are nearly normal to bedding. Two varieties of rhodochrosite, one fine-grained, dark-gray or black, and massive, the other coarser-grained, pink, and generally occurring in veinlets in the gray variety, are present. The gray contains less MnCO&nbsp;</span><sub>3</sub><span>&nbsp;and FeCO&nbsp;</span><sub>3</sub><span>&nbsp;, but more CaCO&nbsp;</span><sub>3</sub><span>&nbsp;and MgCO&nbsp;</span><sub>3</sub><span>&nbsp;than the pink variety. The deposits are interpreted as bodies that replaced favorable dolomite or limestone beds. The gray rhodochrosite first replaced the dolomite or limestone; the pink variety later formed veinlets in the gray rhodochrosite and replaced it to a small extent.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.33.5.508","usgsCitation":"Callaghan, E., 1938, Manganese deposits of the Drum Mountains, Utah: Economic Geology, v. 33, no. 5, p. 508-521, https://doi.org/10.2113/gsecongeo.33.5.508.","productDescription":"14 p.","startPage":"508","endPage":"521","costCenters":[],"links":[{"id":377046,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Drum Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.18389892578125,\n              39.444147324430396\n            ],\n            [\n              -112.87696838378906,\n              39.444147324430396\n            ],\n            [\n              -112.87696838378906,\n              39.6437675734185\n            ],\n            [\n              -113.18389892578125,\n              39.6437675734185\n            ],\n            [\n              -113.18389892578125,\n              39.444147324430396\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"33","issue":"5","noUsgsAuthors":false,"publicationDate":"1938-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Callaghan, Eugene","contributorId":79855,"corporation":false,"usgs":true,"family":"Callaghan","given":"Eugene","email":"","affiliations":[],"preferred":false,"id":794876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211630,"text":"70211630 - 1938 - Potash in the Permian Salt Basin","interactions":[],"lastModifiedDate":"2020-08-05T16:10:28.13344","indexId":"70211630","displayToPublicDate":"1938-08-01T11:04:33","publicationYear":"1938","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1986,"text":"Industrial and Engineering Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Potash in the Permian Salt Basin","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ie50344a005","usgsCitation":"Smith, H.I., 1938, Potash in the Permian Salt Basin: Industrial and Engineering Chemistry, v. 30, no. 8 p., p. 854-860, https://doi.org/10.1021/ie50344a005.","productDescription":"7 p.","startPage":"854","endPage":"860","costCenters":[],"links":[{"id":377043,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico, Texas","otherGeospatial":"Permian Salt Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.64453124999999,\n              31.109388560814963\n            ],\n            [\n              -100.0634765625,\n              31.109388560814963\n            ],\n            [\n              -100.0634765625,\n              34.615126683462194\n            ],\n            [\n              -105.64453124999999,\n              34.615126683462194\n            ],\n            [\n              -105.64453124999999,\n              31.109388560814963\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"30","issue":"8 p.","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, H. I.","contributorId":236986,"corporation":false,"usgs":false,"family":"Smith","given":"H.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":794873,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211629,"text":"70211629 - 1938 - The origin of the iron ore deposits in the Bull Valley and Iron Springs districts, Utah","interactions":[],"lastModifiedDate":"2020-08-05T16:00:58.018442","indexId":"70211629","displayToPublicDate":"1938-08-01T10:54:10","publicationYear":"1938","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 origin of the iron ore deposits in the Bull Valley and Iron Springs districts, Utah","docAbstract":"<p><span>A summary of the geology of the Bull Valley district, southwestern Utah, and a description of the occurrence of the magnetite and hematite deposits is given, as well as brief descriptions of the ore pits at Iron Mountain and Desert Mound 20 miles to the northeast, in which deposits formed under similar geologic conditions have been developed. Neither the ores nor the country rock show the features characteristic of contact-metamorphic deposits. The following explanation of the origin of the deposits is offered. During the intrusion of monzonite porphyry stocks, the hoods and overlying rock were fractured, causing a sudden release of pressure and liberating FeCl&nbsp;</span><sub>3</sub><span>&nbsp;and H&nbsp;</span><sub>2</sub><span>&nbsp;O gas from the stocks which were still at high temperature. These gases found ready egress to the surface along tension fissures without appreciably heating the country rock. They deposited magnetite and hematite in the fissures and replaced the contiguous fractured limestone. The period of gas emanation was brief and the hydrothermal stage probably evolved during the later magmatic history never reached this area. The deposits were formed under a cover of less than 5,000 feet.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.33.5.477","usgsCitation":"Wells, F.G., 1938, The origin of the iron ore deposits in the Bull Valley and Iron Springs districts, Utah: Economic Geology, v. 33, no. 5, p. 477-507, https://doi.org/10.2113/gsecongeo.33.5.477.","productDescription":"31 p.","startPage":"477","endPage":"507","costCenters":[],"links":[{"id":377040,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Bull Valley, Iron Springs","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.92822265625,\n              37.19533058280065\n            ],\n            [\n              -113.07952880859375,\n              37.19533058280065\n            ],\n            [\n              -113.07952880859375,\n              37.89002800137122\n            ],\n            [\n              -113.92822265625,\n              37.89002800137122\n            ],\n            [\n              -113.92822265625,\n              37.19533058280065\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"33","issue":"5","noUsgsAuthors":false,"publicationDate":"1938-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Wells, Francis Gerritt","contributorId":38628,"corporation":false,"usgs":true,"family":"Wells","given":"Francis","email":"","middleInitial":"Gerritt","affiliations":[],"preferred":false,"id":794872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70160865,"text":"70160865 - 1938 - Records of the drilled wells of the island of Oahu, Hawaii","interactions":[],"lastModifiedDate":"2016-01-06T08:56:21","indexId":"70160865","displayToPublicDate":"1938-08-01T10:30:00","publicationYear":"1938","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"4","title":"Records of the drilled wells of the island of Oahu, Hawaii","docAbstract":"<p>The description, location, log and meter tests of all the drilled wells on Oahu are given herein as of March 1 1938. Except for the discharges of plantation wells, which are published on pages 275 to 322 of Bulletin 1, head, chloride, and discharge records are listed only to the close of 1934, the date when this report was compiled. All head measurements and salt determinations made by the U.S. Geological Survey since 1934 will be found in the annual U.S. Geological Survey Water-Supply Papers entitled &ldquo;Water levels and artesian pressure in observation wells in the United States.&rdquo; Records of wells in the district of Honolulu are currently printed in the biennial reports of the Board of Water Supply, Honolulu. Most of the records of the plantation wells have been furnished by the owners.<br />Plate 2 shows the location of the wells, whether they are sealed, and whether the log is known. The static level or head of a well is the height above mean sea level to which the water will rise when all flow from the well is shut off. In the nonartesian wells the static level is the level of the water table of the basal zone of saturation in the basalts of the Koolau and Waianae volcanic series. Many of the wells are subartesian; that is, the water stands in the well above the level at which it was first encountered but does not overflow.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Honolulu, Oahu","collaboration":"Prepared in cooperation with the Geological Survey, United States Department of Interior","usgsCitation":"Stearns, H.T., and Vaksvik, K.N., 1938, Records of the drilled wells of the island of Oahu, Hawaii: Bulletin 4, 213 p.","productDescription":"213 p.","endPage":"213","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":221,"text":"Division of Hydrography","active":false,"usgs":true}],"links":[{"id":313174,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70160865.JPG"},{"id":313173,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/misc/stearns/Bulletin_4.pdf","size":"15.1 MB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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