{"pageNumber":"7215","pageRowStart":"180350","pageSize":"25","recordCount":184651,"records":[{"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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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"568ba5dee4b0e7594ee776c1","contributors":{"authors":[{"text":"Stearns, Harold T.","contributorId":65831,"corporation":false,"usgs":true,"family":"Stearns","given":"Harold","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":584087,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vaksvik, Knute N.","contributorId":151030,"corporation":false,"usgs":false,"family":"Vaksvik","given":"Knute","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":584088,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38051,"text":"38051 - 1938 - Cultural and other methods for the control of injurious wildlife","interactions":[],"lastModifiedDate":"2014-07-21T12:54:59","indexId":"38051","displayToPublicDate":"1938-06-01T12:54:31","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":"115","title":"Cultural and other methods for the control of injurious wildlife","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Spencer, D.A., 1938, Cultural and other methods for the control of injurious wildlife: Wildlife Leaflet 115, 6 p.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":290575,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb30e4b0824b2d178d2a","contributors":{"authors":[{"text":"Spencer, Donald A.","contributorId":49712,"corporation":false,"usgs":true,"family":"Spencer","given":"Donald","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":218788,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38036,"text":"38036 - 1938 - Protecting orchard trees from deer","interactions":[],"lastModifiedDate":"2014-07-21T11:39:31","indexId":"38036","displayToPublicDate":"1938-06-01T11:38:49","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":"117","title":"Protecting orchard trees from deer","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Mills, E., 1938, Protecting orchard trees from deer: Wildlife Leaflet 117, 5 p.","productDescription":"5 p.","numberOfPages":"5","costCenters":[],"links":[{"id":290560,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd6e6de4b0b29085105c8d","contributors":{"authors":[{"text":"Mills, E.M.","contributorId":78651,"corporation":false,"usgs":true,"family":"Mills","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":218763,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211632,"text":"70211632 - 1938 - Outlook for further ore discoveries in the Little Hatchet Mountains, New Mexico","interactions":[],"lastModifiedDate":"2020-08-05T16:29:00.490516","indexId":"70211632","displayToPublicDate":"1938-06-01T11:24:55","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":"Outlook for further ore discoveries in the Little Hatchet Mountains, New Mexico","docAbstract":"<p><span>The Little Hatchet Mountains contain two mining districts, the Eureka silver-lead-zinc district and the Sylvanite gold district, the deposits of each being associated with a mass of monzonite that intrudes Lower Cretaceous sediments. The same formations crop out in both districts, having been duplicated by a large post-ore fault, and the two monzonite masses and their accompanying mineralized zones lie at essentially the same stratigraphic position in the two fault blocks. The deposits of the Eureka district are mesothermal whereas those of the Sylvanite district are hypothermal, but the two groups are mineralogically similar in many respects.As the two monzonite exposures are several miles apart, the natural inference is that there are two separate intrusions. Contrary to this inference, the evidence of structure, mineralogy, and petrology indicates that the two monzonite masses are faulted parts of the same body and that the mineralized areas of the Eureka and Sylvanite districts were originally continuous and zonally related, the original igneous mass having been a flat-lying sill-like streamer, 7 miles or more long, that was bordered by a contact-metamorphic halo and that formed the core of a zone of mineralization.The economic implications of this interpretation are three-fold: (1) the mineralized zone is limited in thickness and is restricted, like a bedded deposit, to a particular sedimentary horizon; (2) the area between the Eureka and Sylvanite districts, hitherto considered barren, should contain mineralized ground at variable depths below the surface; and (3) the deposits change along the trend of the zone from the gold deposits of the one district to the silver-bearing base-metal deposits of the other. In structure and size the deposits in the hidden parts of the mineralized zone probably are similar to those already known. Under the alternative interpretation that the two districts are separate centers of activity, the outlook for future successful prospecting depends upon the depths at which the underlying Paleozoic limestones lie and the possibility of large deposits having been formed in them.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.33.4.365","usgsCitation":"Lasky, S.G., 1938, Outlook for further ore discoveries in the Little Hatchet Mountains, New Mexico: Economic Geology, v. 33, no. 4, p. 365-389, https://doi.org/10.2113/gsecongeo.33.4.365.","productDescription":"25 p.","startPage":"365","endPage":"389","costCenters":[],"links":[{"id":377045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Little Hatchet Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.56414794921875,\n              31.726999082308968\n            ],\n            [\n              -108.37257385253905,\n              31.726999082308968\n            ],\n            [\n              -108.37257385253905,\n              31.962648655655887\n            ],\n            [\n              -108.56414794921875,\n              31.962648655655887\n            ],\n            [\n              -108.56414794921875,\n              31.726999082308968\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"33","issue":"4","noUsgsAuthors":false,"publicationDate":"1938-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lasky, Samuel Grossman","contributorId":35380,"corporation":false,"usgs":true,"family":"Lasky","given":"Samuel","email":"","middleInitial":"Grossman","affiliations":[],"preferred":false,"id":794875,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32429,"text":"32429 - 1938 - Care of rabbits during warm weather","interactions":[],"lastModifiedDate":"2014-07-22T15:50:05","indexId":"32429","displayToPublicDate":"1938-05-01T15:49:21","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":"114","title":"Care of rabbits during warm weather","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Templeton, G.S., 1938, Care of rabbits during warm weather: Wildlife Leaflet 114, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290734,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb30e4b0824b2d178d2c","contributors":{"authors":[{"text":"Templeton, George S.","contributorId":22252,"corporation":false,"usgs":true,"family":"Templeton","given":"George","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":208539,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32428,"text":"32428 - 1938 - European and American methods of rat control","interactions":[],"lastModifiedDate":"2014-07-22T15:14:29","indexId":"32428","displayToPublicDate":"1938-05-01T15:13:48","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":"113","title":"European and American methods of rat control","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Mills, E., 1938, European and American methods of rat control: Wildlife Leaflet 113, 6 p.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":290730,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb30e4b0824b2d178d2e","contributors":{"authors":[{"text":"Mills, E.M.","contributorId":78651,"corporation":false,"usgs":true,"family":"Mills","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":208538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32423,"text":"32423 - 1938 - History and significance of American wildlife","interactions":[],"lastModifiedDate":"2014-07-22T13:59:23","indexId":"32423","displayToPublicDate":"1938-03-01T13:58:48","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":"108","title":"History and significance of American wildlife","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Sheldon, H.P., 1938, History and significance of American wildlife: Wildlife Leaflet 108, 8 p.","productDescription":"8 p.","numberOfPages":"8","costCenters":[],"links":[{"id":290726,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb30e4b0824b2d178d30","contributors":{"authors":[{"text":"Sheldon, Harold P.","contributorId":38477,"corporation":false,"usgs":true,"family":"Sheldon","given":"Harold","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":208534,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32422,"text":"32422 - 1938 - Planning for wildlife management: an outline","interactions":[],"lastModifiedDate":"2014-07-22T13:54:39","indexId":"32422","displayToPublicDate":"1938-03-01T13:53:59","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":"107","title":"Planning for wildlife management: an outline","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","collaboration":"Prepared in the Section of Wildlife Surveys, Division of Wildlife Research.","usgsCitation":"U.S. Division Of Wildlife Research, 1938, Planning for wildlife management: an outline: Wildlife Leaflet 107, 5 p.","productDescription":"5 p.","numberOfPages":"5","costCenters":[],"links":[{"id":290725,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb30e4b0824b2d178d32","contributors":{"authors":[{"text":"U.S. Division Of Wildlife Research","contributorId":128226,"corporation":true,"usgs":false,"organization":"U.S. Division Of Wildlife Research","id":529375,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70206430,"text":"70206430 - 1938 - The future of paleontology","interactions":[],"lastModifiedDate":"2019-11-02T19:23:33","indexId":"70206430","displayToPublicDate":"1938-01-01T19:19:06","publicationYear":"1938","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2711,"text":"Memoir of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"displayTitle":"The future of paleontology","title":"The future of paleontology","docAbstract":"<p>No abstract available.</p>","language":"English ","publisher":"Elsevier ","doi":"10.1130/GSAB-49-359","issn":" 00167606","usgsCitation":"Cushman, J., 1938, The future of paleontology: Memoir of the Geological Society of America, v. 49, no. 3, p. 359-366, https://doi.org/10.1130/GSAB-49-359.","productDescription":"8 p. ","startPage":"359","endPage":"366","costCenters":[],"links":[{"id":368908,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"49","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cushman, Joseph A.","contributorId":77200,"corporation":false,"usgs":true,"family":"Cushman","given":"Joseph A.","affiliations":[],"preferred":false,"id":774516,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32426,"text":"32426 - 1938 - The waterfowl situation: 1937-38","interactions":[],"lastModifiedDate":"2014-07-22T14:11:04","indexId":"32426","displayToPublicDate":"1938-01-01T14:09:56","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":"111","title":"The waterfowl situation: 1937-38","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","collaboration":"Prepared in the Section of Distribution and Migration of Birds, Division of Wildlife Research.","usgsCitation":"U.S. Bureau of Biological Survey, 1938, The waterfowl situation: 1937-38: Wildlife Leaflet 111, 10 p.","productDescription":"10 p.","numberOfPages":"10","temporalStart":"1937-01-01","temporalEnd":"1938-01-01","costCenters":[],"links":[{"id":290729,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb30e4b0824b2d178d34","contributors":{"authors":[{"text":"U.S. Bureau of Biological Survey","contributorId":128079,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Biological Survey","id":529376,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32425,"text":"32425 - 1938 - Status of eelgrass (Zostera marina) on the north Atlantic coast, February 1938.","interactions":[],"lastModifiedDate":"2014-07-22T14:07:54","indexId":"32425","displayToPublicDate":"1938-01-01T14:07:22","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":"110","title":"Status of eelgrass (Zostera marina) on the north Atlantic coast, February 1938.","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of Agriculture","publisherLocation":"Washington, D.C.","usgsCitation":"Cottam, C., 1938, Status of eelgrass (Zostera marina) on the north Atlantic coast, February 1938.: Wildlife Leaflet 110, 7 p.","productDescription":"7 p.","numberOfPages":"7","costCenters":[],"links":[{"id":290728,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffdb34e4b0824b2d178d36","contributors":{"authors":[{"text":"Cottam, Clarence","contributorId":41490,"corporation":false,"usgs":true,"family":"Cottam","given":"Clarence","email":"","affiliations":[],"preferred":false,"id":208536,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}