A statistical analysis is made of the sequences of annual tree ring widths and indices. The expected value of growth during any year is shown to be proportional to the standard deviation of the growth, so that the coefficient of variation is a measure of the sensitivity of the growth of a tree. Tree ring data were found to be non-randomly distributed in time. The large values of serial correlation indicated that the non-randomness cannot be attributed entirely to climatic factors. Correlogram and power spectrum analyses applied to a sequence of tree ring indices for a pinyon pine showed that the data were generated by an autoregressive process. The statistical parameter measuring the sensitivity or complacency of growth is used to derive a growth function.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666209493254","usgsCitation":"Matalas, N., 1962, Statistical properties of tree ring data: International Association of Scientific Hydrology - Bulletin , v. 7, no. 2, p. 39-47, https://doi.org/10.1080/02626666209493254.","productDescription":"9 p.","startPage":"39","endPage":"47","costCenters":[],"links":[{"id":480373,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666209493254","text":"Publisher Index Page"},{"id":385948,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Matalas, N.C.","contributorId":25173,"corporation":false,"usgs":true,"family":"Matalas","given":"N.C.","affiliations":[],"preferred":false,"id":816460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220776,"text":"70220776 - 1962 - Use of thermometry in hydrogeologic studies of glacial deposits at Worthington, Minnesota","interactions":[],"lastModifiedDate":"2021-05-25T17:37:15.261452","indexId":"70220776","displayToPublicDate":"1962-06-01T12:32:22","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Use of thermometry in hydrogeologic studies of glacial deposits at Worthington, Minnesota","docAbstract":"Precise measurements of fluctuations of ground-water temperature based on monthly readings in shallow glacial-outwash aquifers may be used to study ground-water movement and recharge. An increase in storage in the shallow basin of Okabena Lake, Worthington, Minnesota, permits the water to cover a much larger area and probably increases the opportunity for infiltration of lake water into aquifers connected with the lake. In a shallow artesian aquifer confined by relatively impervious glacial till, water moves toward the land surface in response to steep temperature gradients in the winter, and cool water descends to the aquifer when the upward temperature gradient is lowered or eliminated. Thermometry may also be used in hydrogeologic studies of limestone terrane.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[1305:UOTIHS]2.0.CO;2","usgsCitation":"Schneider, R., 1962, Use of thermometry in hydrogeologic studies of glacial deposits at Worthington, Minnesota: Geological Society of America Bulletin, v. 73, no. 10, p. 1305-1308, https://doi.org/10.1130/0016-7606(1962)73[1305:UOTIHS]2.0.CO;2.","productDescription":"4 p.","startPage":"1305","endPage":"1308","costCenters":[],"links":[{"id":385947,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Worthington","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.78979492187499,\n 43.600284023536325\n ],\n [\n -95.350341796875,\n 43.600284023536325\n ],\n [\n -95.350341796875,\n 43.72744458647464\n ],\n [\n -95.78979492187499,\n 43.72744458647464\n ],\n [\n -95.78979492187499,\n 43.600284023536325\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schneider, R.J.","contributorId":97283,"corporation":false,"usgs":true,"family":"Schneider","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":816459,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220768,"text":"70220768 - 1962 - Limiting parameters in the magnetic interpretation of a geologic structure","interactions":[],"lastModifiedDate":"2021-05-25T17:13:30.803418","indexId":"70220768","displayToPublicDate":"1962-06-01T12:07:16","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Limiting parameters in the magnetic interpretation of a geologic structure","docAbstract":"A prominent aeromagnetic anomaly in Randolph County, Indiana, suggests the existence of a dikelike structure within the Precambrian basement rocks. Because of the ambiguity inherent in magnetic interpretation, a unique solution for the parameters involved (depth of burial, geometric configuration, and magnetic susceptibility of the mass producing the anomaly) is impossible. However, if one of the parameters is known it is sometimes possible to indicate a range of plausible values for each of the remaining parameters. The depth to the surface of the Precambrian rocks in Randolph County is known from drill-hole data to be about 3,000 ft. As the depth of burial is known, limits need be set only on the thickness, angle of dip, and susceptibility contrast of the assumed dike. These limits are determined by a graphical method. Theoretical anomalies over the postulated dike are computed for different dike thicknesses, angles of dip, and susceptibility contrasts. The computed profiles are then fitted to an observed magnetic profile flown at right angles to the trend of the feature. Numerical values for the \"goodness of fit\" are calculated by using the statistical method of sums of squares. Two plots, one of the index of goodness of fit and the other of susceptibility as functions of dip angle and dike thickness, are made to show graphically the interdependence of the variables and the plausible range of each. The contoured plots of the goodness of fit and the susceptibility contrast show that the range of best fit is between dip angles of 30 and 60 degrees and dike thickness of 1,000 to over 4,000 ft. The contoured plot of the susceptibility contrast, translated into percentage of magnetite, shows this parameter to be independent of the dip angle, varying only with thickness.
","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1439104","usgsCitation":"Andreasen, G.E., and Zietz, I., 1962, Limiting parameters in the magnetic interpretation of a geologic structure: Geophysics, v. 27, no. 6, p. 807-814, https://doi.org/10.1190/1.1439104.","productDescription":"8 p.","startPage":"807","endPage":"814","costCenters":[],"links":[{"id":385945,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Indiana","otherGeospatial":"Randolph County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -85.23056030273438,\n 40.01499435375046\n ],\n [\n -84.79934692382812,\n 40.01499435375046\n ],\n [\n -84.79934692382812,\n 40.310948849735\n ],\n [\n -85.23056030273438,\n 40.310948849735\n ],\n [\n -85.23056030273438,\n 40.01499435375046\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"27","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Andreasen, G. E.","contributorId":105315,"corporation":false,"usgs":true,"family":"Andreasen","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":816456,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zietz, I.","contributorId":59937,"corporation":false,"usgs":true,"family":"Zietz","given":"I.","email":"","affiliations":[],"preferred":false,"id":816457,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220759,"text":"70220759 - 1962 - The distribution of tritium fallout in precipitation over North America","interactions":[],"lastModifiedDate":"2021-05-25T16:41:45.677086","indexId":"70220759","displayToPublicDate":"1962-06-01T11:38:37","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5334,"text":"International Association of Scientific Hydrology - Bulletin ","onlineIssn":"2150-3435","printIssn":"0262-6667","active":false,"publicationSubtype":{"id":10}},"title":"The distribution of tritium fallout in precipitation over North America","docAbstract":"In 1958 the U.S. Geological Survey and the U.S. Weather Bureau jointly conducted a study of tritium fallout distribution over the continental United States, Alaska, and Puerto Rico. The observation period extended from early April to late July in most areas. While this was insufficient to cover the decay side of the curve, it was sufficiently long to establish general trends of tritium activity contours. Tritium activities were found to be maximum in the north central part of the country and minimum in coastal areas. The tritium activities show an inverse correlation with chloride concentrations in precipitation. Tritium activities in precipitation appear to be influenced by several “low altitude effects” particularly in storms of brief duration. Ground level tritium activity measurements are not directly representative of tritium in cloud moisture because of these effects.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666209493255","usgsCitation":"Thatcher, L.L., 1962, The distribution of tritium fallout in precipitation over North America: International Association of Scientific Hydrology - Bulletin , v. 7, no. 2, p. 48-58, https://doi.org/10.1080/02626666209493255.","productDescription":"11 p.","startPage":"48","endPage":"58","costCenters":[],"links":[{"id":480374,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1080/02626666209493255","text":"Publisher Index Page"},{"id":385943,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Thatcher, L. L.","contributorId":23271,"corporation":false,"usgs":true,"family":"Thatcher","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220758,"text":"70220758 - 1962 - Aeromagnetic and gravity studies of theprecambrian in northeastern New Mexico","interactions":[],"lastModifiedDate":"2021-05-25T16:34:19.133489","indexId":"70220758","displayToPublicDate":"1962-06-01T11:30:09","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Aeromagnetic and gravity studies of theprecambrian in northeastern New Mexico","docAbstract":"A contour map of the Precambrian surface for a part of northeastern New Mexico has been prepared from aeromagnetic, gravity, and drill-hole data. The area extends approximately from the Colorado border south to latitude34° N., and from the foothills of the Sangre de Cristo Mountains east to longitude 104° W. Thirty-seven depths to Precambrian rocks were computed from aeromagnetic anomalies. Regional gravityanomalies were generally not suitable for quantitative analysis, but the gravity highs correlated with known areas ofbasement highs, providing a basis for contouring in areas of meager depth control. Drill-hole data provided 61depths to basement in and near the survey area. The contouring along the east edge of the Sangre de Cristo Mountainswas guided by exposures of Precambrian rocks. A principal feature of the contour map is the Sierre Grande Arch, a basement highland that trends southwestacross the area to the northwest part of Guadalupe County. Major depressions are outlined west of Vegas Junction, northeast of Santa Rosa, and north and northeast of Las Vegas. The largest of these, the Las Vegas basin, occupiesmore than 1,000 square miles and may be more than 10,000 ft deep Copyright.
","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.3301595","usgsCitation":"Andreasen, G.E., Kane, M.F., and Zietz, I., 1962, Aeromagnetic and gravity studies of theprecambrian in northeastern New Mexico: Geophysics, v. 27, no. 3, p. 343-358, https://doi.org/10.1190/1.3301595.","productDescription":"16 p.","startPage":"343","endPage":"358","costCenters":[],"links":[{"id":385942,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"northeastern New Mexico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.0400390625,\n 34.66935854524543\n ],\n [\n -102.98583984374999,\n 34.66935854524543\n ],\n [\n -102.98583984374999,\n 36.96744946416934\n ],\n [\n -106.0400390625,\n 36.96744946416934\n ],\n [\n -106.0400390625,\n 34.66935854524543\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"27","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Andreasen, G. E.","contributorId":105315,"corporation":false,"usgs":true,"family":"Andreasen","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":816451,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kane, M. F.","contributorId":45708,"corporation":false,"usgs":true,"family":"Kane","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":816452,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zietz, I.","contributorId":59937,"corporation":false,"usgs":true,"family":"Zietz","given":"I.","email":"","affiliations":[],"preferred":false,"id":816453,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70220754,"text":"70220754 - 1962 - Progress report on an international decade for hydrology","interactions":[],"lastModifiedDate":"2021-05-25T16:28:24.653044","indexId":"70220754","displayToPublicDate":"1962-06-01T11:25:20","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"title":"Progress report on an international decade for hydrology","docAbstract":"As reported in the Transactions of March 1961 (p. 96), the ad hoc Panel on Hydrology convened to report on ways of stimulating research in scientific hydrology, recommended a program of international cooperation in hydrology—more specifically a plan for an ‘International Decade for Hydrology,’ as drawn for the Panel by R. L. Nace. The proposal for an international program in scientific hydrology was submitted to the Council of the International Association of Scientific Hydrology (IASH), meeting at Athens during October 1961, and was explained to them by Nace. The proposal was endorsed in principle by the country representatives who were present, and further endorsement is being requested of national committees not represented at Athens. The report of the ad hoc Panel on International Cooperation in Hydrology will be published in a forthcoming Bulletin of the International Association of Scientific Hydrology.
","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR043i001p00009","usgsCitation":"Langbein, W.B., 1962, Progress report on an international decade for hydrology, v. 42, no. 1, p. 9-9, https://doi.org/10.1029/TR043i001p00009.","productDescription":"1 p.","startPage":"9","endPage":"9","costCenters":[],"links":[{"id":385941,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"42","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":816450,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220753,"text":"70220753 - 1962 - Paleozoic seas of central Idaho","interactions":[],"lastModifiedDate":"2021-05-26T12:04:10.351447","indexId":"70220753","displayToPublicDate":"1962-06-01T11:19:39","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Paleozoic seas of central Idaho","docAbstract":"Some recent paleogeographic maps indicate that central Idaho was part of a major geosyncline throughout Paleozoic time. This concept, apparently based on thick marine accumulations far apart on the margins of the region, is inconsistent with field data. Within the area of the Idaho batholith, Permian(?) volcanic rocks rest either on batholithic rocks or on the Belt Series. The Belt Series rocks have furnished the xenoliths in the batholith. To the west upper Paleozoic and Mesozoic strata are invaded. Along the eastern margin, south of lat. 45°, thick Paleozoic strata are intruded by the batholith. These locally exceed 30,000 feet in thickness and thin eastward. They have many variations. Those close to the batholith, especially those high in the sequence, are regarded as of near-shore origin. The Paleozoic strata in southeastern Idaho, more than 17,000 feet thick, are broadly similar except that Cambrian strata there are thicker and more widespread. The part of central Idaho north of the vicinity of lat. 45° has no known Paleozoic strata. Northern Idaho has only a few outcrops of beds of Cambrian age. The differences in thickness and character between Paleozoic strata in south-central and southeastern Idaho and those in western Montana and Wyoming (less than 7500 feet thick) suggest a hinge line near the eastern boundary between Idaho and Montana with a shelf to the east and a trough to the west. In south-central Idaho this trough had a maximum width of 90 miles and a western shore roughly at the east margin of the batholith. This trough wedged out northward a little beyond lat. 45°. Thus the area of the present Idaho batholith has been a positive block since Precambrian time, comparable to but apparently of longer duration than the geanticline in northern Nevada. Any invasion of the positive block in Idaho by marine waters during the Paleozoic was local and brief, except perhaps along the western border. Uncertain correlations within the area of the batholith leave open the possibility of some deposition there early in Paleozoic time.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[769:PSOCI]2.0.CO;2","usgsCitation":"Ross, C.P., 1962, Paleozoic seas of central Idaho: Geological Society of America Bulletin, v. 73, no. 6, p. 769-793, https://doi.org/10.1130/0016-7606(1962)73[769:PSOCI]2.0.CO;2.","productDescription":"25 p.","startPage":"769","endPage":"793","costCenters":[],"links":[{"id":385940,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"western-central Idaho","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -117.24609374999999,\n 43.26120612479979\n ],\n [\n -114.5654296875,\n 43.26120612479979\n ],\n [\n -114.5654296875,\n 45.398449976304086\n ],\n [\n -117.24609374999999,\n 45.398449976304086\n ],\n [\n -117.24609374999999,\n 43.26120612479979\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Ross, Clyde P.","contributorId":10473,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":816449,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220746,"text":"70220746 - 1962 - Magnetic anomalies and magnetizations of the Biwabik iron-formation, Mesabi area, Minnesota","interactions":[],"lastModifiedDate":"2021-05-25T15:49:46.095599","indexId":"70220746","displayToPublicDate":"1962-06-01T10:44:49","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Magnetic anomalies and magnetizations of the Biwabik iron-formation, Mesabi area, Minnesota","docAbstract":"In a study of the relationship of magnetic anomalies to the magnetite content and structure of layered Precambrian iron-formations, the effective induced and remanent magnetizations of the Biwabik iron-formation were determined by analyses of aeromagnetic anomalies recorded 1,000 ft above the Biwabik in areas of known geology. The induced magnetization along the layers is relatively insignificant because the formation is almost perpendicular to the earth's magnetic field. For the relatively unmetamorphosed iron-formation of the Main Mesabi district, the dominant magnetization was found to be across the layers, about 0.012 gauss, and most likely induced. For the strongly metamorphosed iron-formation of the East Mesabi district, the dominant magnetization was found to be along the layers, about 0.100 gauss, and remanent. These values are used as bases for explaining aeromagnetic anomalies from correlatives of the Biwabik iron-formation in the Gunflint, Cuyuna, and Gogebic districts.
","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1439073","usgsCitation":"Bath, G.D., 1962, Magnetic anomalies and magnetizations of the Biwabik iron-formation, Mesabi area, Minnesota: Geophysics, v. 27, no. 5, p. 627-650, https://doi.org/10.1190/1.1439073.","productDescription":"24 p.","startPage":"627","endPage":"650","costCenters":[],"links":[{"id":385939,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"north-central Minnesota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.47119140625,\n 47.32393057095941\n ],\n [\n -92.373046875,\n 47.32393057095941\n ],\n [\n -92.373046875,\n 48.96579381461063\n ],\n [\n -95.47119140625,\n 48.96579381461063\n ],\n [\n -95.47119140625,\n 47.32393057095941\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"27","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bath, G. D.","contributorId":71968,"corporation":false,"usgs":true,"family":"Bath","given":"G.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":816448,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220742,"text":"70220742 - 1962 - Analysis of present geomagnetic field for comparison with paleomagnetic results","interactions":[],"lastModifiedDate":"2021-05-25T15:39:48.18603","indexId":"70220742","displayToPublicDate":"1962-06-01T10:35:33","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2310,"text":"Journal of Geomagnetism & Geoelectricity","active":true,"publicationSubtype":{"id":10}},"title":"Analysis of present geomagnetic field for comparison with paleomagnetic results","docAbstract":"Both the dipole and nondipole components of the present geomagnetic field are analyzed by calculating the orientation of hypothetical geocentric dipoles which, if acting alone, would produce the present geomagnetic field as observed at points on a grid covering the earth at 10° intervals. The dispersion in direction of these virtual geomagnetic poles due to the nondipole component of thee geomagnetic field (1) is larger in the southern hemisphere than in the northern; (2) increases with increase in latitude; (3) at all latitudes is of the same order of magnitude as the dispersion due to a wobble of several tens of degrees of the main geocentric dipole; (4) is anomalously small over a region of continental dimensions in the central Pacific ocean. The parameters describing these variations of poles are transformed to parameters describing variations of the geomagnetic field for comparison with paleomagnetic data.
","language":"English","publisher":"Society of Geomagnetism and Earth, Planetary and Space Sciences","doi":"10.5636/jgg.13.101","usgsCitation":"Cox, A., 1962, Analysis of present geomagnetic field for comparison with paleomagnetic results: Journal of Geomagnetism & Geoelectricity, v. 13, no. 3-4, p. 101-112, https://doi.org/10.5636/jgg.13.101.","productDescription":"12 p.","startPage":"101","endPage":"112","costCenters":[],"links":[{"id":494171,"rank":0,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.5636/jgg.13.101","text":"Publisher Index Page"},{"id":385938,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"3-4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cox, Allan","contributorId":89949,"corporation":false,"usgs":true,"family":"Cox","given":"Allan","email":"","affiliations":[],"preferred":false,"id":816447,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220738,"text":"70220738 - 1962 - Erosion on miniature pediments in badlands national monument, South Dakota","interactions":[],"lastModifiedDate":"2021-05-25T15:33:32.646653","indexId":"70220738","displayToPublicDate":"1962-06-01T10:28:22","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Erosion on miniature pediments in badlands national monument, South Dakota","docAbstract":"Measurements of erosion on miniature pediments in Badlands National Monument, South Dakota, show that during almost eight years, the pediments were lowered by sheetwash. The adjacent hillslopes have retreated leaving a belt of newly formed pediment from 6 to 12 cm wide at their bases. The hillslopes are rough and relatively permeable; the miniature pediments are smooth and less permeable. Calculations based on the Manning equation suggest that the velocity of overland flow on the pediments may be of the same magnitude as that on the hillslopes. The decrease in roughness from hillslope to pediment compensates for the decrease in slope angle. The pediments are swept free of debris and are regraded by a more effective utilization of runoff energy.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[719:EOMPIB]2.0.CO;2","usgsCitation":"Schumm, S.A., 1962, Erosion on miniature pediments in badlands national monument, South Dakota: Bulletin of the Geological Society of America, v. 73, no. 6, p. 719-724, https://doi.org/10.1130/0016-7606(1962)73[719:EOMPIB]2.0.CO;2.","productDescription":"6 p.","startPage":"719","endPage":"724","costCenters":[],"links":[{"id":385937,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota","otherGeospatial":"Badlands National Monument","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.22753906249999,\n 43.205175817237304\n ],\n [\n -101.151123046875,\n 43.205175817237304\n ],\n [\n -101.151123046875,\n 44.24519901522129\n ],\n [\n -103.22753906249999,\n 44.24519901522129\n ],\n [\n -103.22753906249999,\n 43.205175817237304\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schumm, S. A.","contributorId":71957,"corporation":false,"usgs":true,"family":"Schumm","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":816446,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220667,"text":"70220667 - 1962 - Tertiary landslides, northwestern South Dakota and Southeastern Montana","interactions":[],"lastModifiedDate":"2021-05-24T14:06:04.607035","indexId":"70220667","displayToPublicDate":"1962-06-01T08:59:58","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5935,"text":"Bulletin of the Geological Society of America","active":true,"publicationSubtype":{"id":10}},"title":"Tertiary landslides, northwestern South Dakota and Southeastern Montana","docAbstract":"Landslide blocks of latest Oligocene or earliest Miocene age are preserved at several localities in northwestern South Dakota and southeastern Montana. These tilted blocks contain Late Cretaceous to late Oligocene rocks and are unconformably overlain by nearly horizontal strata of the Arikaree Formation of Miocene age. Undisturbed rocks of late Oligocene age were completely stripped from the area by pre-Arikaree erosion. More than 100 landslide blocks are preserved in the Slim Buttes, Harding County, South Dakota. Some of the blocks are several miles long, 600 feet wide, and contain a thickness of 300 feet or more of relatively unbroken or unjumbled strata which have been displaced downward as much as 250 feet. The strike of the tilted blocks is about N. 60° W., and the dip of the bedding in the blocks at most places is to the southwest and ranges from a few to more than 60°. Most of the rock in the blocks consists of coarse arkosic sandstone, tuffaceous siltstone, claystone, and thick beds of bentonite of the Chadron and Brule formations of Oligocene age. In a few places, small sections of the underlying Paleocene strata are tilted. The blocks formed along northwest-trendingpre-Arikaree valley walls and escarpments. The major joint system of underlying rocks apparently controlled the orientation of the slides, and the dip of these older rocks facilitated the downward and outward movement of the landslide blocks. The Short Pine Hills, Harding County, South Dakota, and the Long Pine Hills, Carter County, Montana, contain numerous landslide blocks that are similar in orientation and geologic setting to those of the Slim Buttes. In contrast, the Finger Buttes of Carter County, Montana, contain landslide blocks that strike about N. 70° E. and dip to the southeast. This lack of parallelism with blocks of nearby areas is apparently due to the lack of a well-developed joint system in underlying rocks of this area. The presence of the complete sequence of Oligocene rocks in the downdropped blocks indicates that before pre-Arikaree erosion the area was covered by 500 feet or more of beds of the Chadron and Brule formations. These landslide blocks show that the time interval represented by the unconformity at the base of the Arikaree Formation was of relatively short duration.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[725:TLNSDA]2.0.CO;2","usgsCitation":"Gill, J.R., 1962, Tertiary landslides, northwestern South Dakota and Southeastern Montana: Bulletin of the Geological Society of America, v. 73, no. 6, p. 725-735, https://doi.org/10.1130/0016-7606(1962)73[725:TLNSDA]2.0.CO;2.","productDescription":"11 p.","startPage":"725","endPage":"735","costCenters":[],"links":[{"id":385898,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"South Dakota, Montana","otherGeospatial":"southeastern Montana, northwestern South Dakota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.04052734375,\n 45.93587062119052\n ],\n [\n -107.46826171874999,\n 45.89000815866184\n ],\n [\n -107.42431640625,\n 44.98034238084973\n ],\n [\n -101.7333984375,\n 45.058001435398275\n ],\n [\n -101.75537109375,\n 45.9511496866914\n ],\n [\n -104.04052734375,\n 45.93587062119052\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Gill, J. R.","contributorId":8125,"corporation":false,"usgs":true,"family":"Gill","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":816357,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014486,"text":"1014486 - 1962 - Experimental propagation of lymphocystis disease of fishes","interactions":[],"lastModifiedDate":"2026-03-16T15:12:27.861627","indexId":"1014486","displayToPublicDate":"1962-05-28T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3696,"text":"Virology","active":true,"publicationSubtype":{"id":10}},"title":"Experimental propagation of lymphocystis disease of fishes","docAbstract":"The agent of lymphocystis disease has been propagated under laboratory conditions for more than 2 years. Although several hatchery-propagated centrarchids are susceptible, the bluegill (Lepomis macrochirus) is the host of choice because it is most easily maintained. At 12.5° the disease was transmitted by implantation and by injection, but there was no evidence of fish-to-fish spread, nor seasonal change in host susceptibility. The infective agent was clearly demonstrated to be filterable (Millipore HA). It retained infectivity in storage at −20° for almost two years, and its viability after desiccation was confirmed. These facts support its postulated viral nature. The virus was glycerol- and ether-sensitive and did not induce formation of giant lymphocystis cells in monolayer cultures of bluegill ovary cells.
","language":"English","publisher":"Elsevier","doi":"10.1016/0042-6822(62)90011-9","usgsCitation":"Wolf, K., 1962, Experimental propagation of lymphocystis disease of fishes: Virology, v. 18, no. 2, p. 249-256, https://doi.org/10.1016/0042-6822(62)90011-9.","productDescription":"8 p.","startPage":"249","endPage":"256","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131730,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"18","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db60244f","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":320453,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70209343,"text":"70209343 - 1962 - Mechanics of a small landslide block, Wattener Lizum, Austria","interactions":[],"lastModifiedDate":"2020-04-03T14:03:23.960525","indexId":"70209343","displayToPublicDate":"1962-04-01T11:49:05","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Mechanics of a small landslide block, Wattener Lizum, Austria","docAbstract":"A small landslide block left a trail about 81 meters long on an 11½-degree slope in the Tuxer Voralpen, Austria. The movement is explained in terms of fluid pressure mechanics; hypothetically, the requisite pore pressure was caused by the loading of contiguous saturated segments of the slide path during rapid sliding.
","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1962)73[1277:MOASLB]2.0.CO;2","usgsCitation":"Brew, D.A., 1962, Mechanics of a small landslide block, Wattener Lizum, Austria: GSA Bulletin, v. 73, no. 10, p. 1277-1280, https://doi.org/10.1130/0016-7606(1962)73[1277:MOASLB]2.0.CO;2.","productDescription":"4 p.","startPage":"1277","endPage":"1280","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":373711,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Austria","otherGeospatial":"Wattener Lizum","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[16.97967,48.1235],[16.90375,47.71487],[16.34058,47.7129],[16.53427,47.49617],[16.2023,46.85239],[16.01166,46.68361],[15.13709,46.6587],[14.63247,46.43182],[13.80648,46.50931],[12.37649,46.76756],[12.15309,47.11539],[11.16483,46.94158],[11.04856,46.75136],[10.4427,46.89355],[9.93245,46.92073],[9.47997,47.10281],[9.63293,47.3476],[9.59423,47.52506],[9.89607,47.5802],[10.40208,47.30249],[10.5445,47.5664],[11.42641,47.52377],[12.14136,47.70308],[12.62076,47.67239],[12.93263,47.46765],[13.02585,47.63758],[12.8841,48.28915],[13.24336,48.41611],[13.59595,48.87717],[14.3389,48.55531],[14.90145,48.9644],[15.25342,49.03907],[16.02965,48.7339],[16.49928,48.78581],[16.96029,48.59698],[16.87998,48.47001],[16.97967,48.1235]]]},\"properties\":{\"name\":\"Austria\"}}]}","volume":"73","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brew, David A. dbrew@usgs.gov","contributorId":3244,"corporation":false,"usgs":true,"family":"Brew","given":"David","email":"dbrew@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":786216,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000378,"text":"1000378 - 1962 - Temperature correction in conductivity measurements","interactions":[],"lastModifiedDate":"2025-05-01T15:42:14.299821","indexId":"1000378","displayToPublicDate":"1962-04-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2620,"text":"Limnology and Oceanography","active":true,"publicationSubtype":{"id":10}},"title":"Temperature correction in conductivity measurements","docAbstract":"Electrical conductivity has been widely used in freshwater research but usual methods employed by limnologists for converting measurements to conductance at a given temperature have not given uniformly accurate results. The temperature coefficient used to adjust conductivity of natural waters to a given temperature varies depending on the kinds and concentrations of electrolytes, the temperature at the time of measurement, and the temperature to which measurements are being adjusted. The temperature coefficient was found to differ for various lake and stream waters, and showed seasonal changes. High precision can be obtained only by determining temperature coefficients for each water studied. Mean temperature coefficients are given for various temperature ranges that may be used where less precision is required.","language":"English","publisher":"Association for the Sciences of Limnology and Oceanography","doi":"10.4319/lo.1962.7.3.0330","usgsCitation":"Smith, S.H., 1962, Temperature correction in conductivity measurements: Limnology and Oceanography, v. 7, no. 3, p. 330-334, https://doi.org/10.4319/lo.1962.7.3.0330.","productDescription":"5 p.","startPage":"330","endPage":"334","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":486857,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.4319/lo.1962.7.3.0330","text":"Publisher Index Page"},{"id":133095,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"3","noUsgsAuthors":false,"publicationDate":"2003-12-22","publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685741","contributors":{"authors":[{"text":"Smith, Stanford H.","contributorId":86711,"corporation":false,"usgs":true,"family":"Smith","given":"Stanford","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308482,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014146,"text":"1014146 - 1962 - Established eurythermic line of fish cells in vitro","interactions":[],"lastModifiedDate":"2026-02-25T16:54:58.079982","indexId":"1014146","displayToPublicDate":"1962-03-23T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Established eurythermic line of fish cells in vitro","docAbstract":"An established line of fish cells has been propagated in vitro for 21 months and 48 subcultivations. Important characteristics of the cells are described.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3508.1065","usgsCitation":"Wolf, K., and Quimby, M.C., 1962, Established eurythermic line of fish cells in vitro: Science, v. 135, no. 3508, p. 1065-1066.","productDescription":"2 p.","startPage":"1065","endPage":"1066","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131542,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"3508","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdddb","contributors":{"authors":[{"text":"Wolf, K.","contributorId":16344,"corporation":false,"usgs":true,"family":"Wolf","given":"K.","email":"","affiliations":[],"preferred":false,"id":319862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Quimby, M. C.","contributorId":14334,"corporation":false,"usgs":true,"family":"Quimby","given":"M.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":319861,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010570,"text":"70010570 - 1962 - Glass electrodes sensitive to divalent cations","interactions":[],"lastModifiedDate":"2026-02-25T16:37:12.820953","indexId":"70010570","displayToPublicDate":"1962-03-23T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Glass electrodes sensitive to divalent cations","docAbstract":"Glass electrodes suitable for measurement of divalent cations have been made and tested. Empirical and theoretical electrode equations have been presented to describe electrode behavior in a variety of aqueous solutions. Most electrodes show response interpretable as showing nearly ideal solid-solution behavior of the cations in the glass surface. The electrodes should be useful in the measurement of divalent-cation activities in natural waters and biological fluids, and useful in general analytical chemistry.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3508.1045","issn":"00368075","usgsCitation":"Garrels, R., Sato, M., Thompson, M., and Truesdell, A., 1962, Glass electrodes sensitive to divalent cations: Ion exchange models for new electrode glasses simplify analyses for calcium and other ions: Science, v. 135, no. 3508, p. 1045-1048.","productDescription":"4 p.","startPage":"1045","endPage":"1048","costCenters":[],"links":[{"id":218972,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"3508","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2929e4b0c8380cd5a6f7","contributors":{"authors":[{"text":"Garrels, R.M.","contributorId":88804,"corporation":false,"usgs":true,"family":"Garrels","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":359195,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sato, M.","contributorId":50201,"corporation":false,"usgs":true,"family":"Sato","given":"M.","email":"","affiliations":[],"preferred":false,"id":359193,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Thompson, M.E.","contributorId":98794,"corporation":false,"usgs":true,"family":"Thompson","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":359196,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address: TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":359194,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010568,"text":"70010568 - 1962 - Hydrology","interactions":[],"lastModifiedDate":"2026-02-25T16:58:59.570241","indexId":"70010568","displayToPublicDate":"1962-03-02T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology","docAbstract":"An understanding of water in relation to earth processes requires the collaboration of many disciplines.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3505.699","issn":"00368075","usgsCitation":"Hendricks, E.L., 1962, Hydrology: Science, v. 135, no. 3505, p. 699-705.","productDescription":"7 p.","startPage":"699","endPage":"705","costCenters":[],"links":[{"id":218970,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"135","issue":"3505","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a36b2e4b0c8380cd6091d","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220772,"text":"70220772 - 1962 - Correlation of the Carrizo Sand in Arkansas and adjacent states","interactions":[],"lastModifiedDate":"2021-05-25T17:25:38.428381","indexId":"70220772","displayToPublicDate":"1962-03-01T12:21:40","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Correlation of the Carrizo Sand in Arkansas and adjacent states","docAbstract":"The Carrizo Sand (Eocene), the basal unit of the Claiborne Group, can be recognized in the subsurface throughout much of southeastern Arkansas and is correlated with the Carrizo Sand of Louisiana and the Meridian Sand Member of the Tallahatta Formation of Mississippi. The term Carrizo Sand is appropriate for use in Arkansas, as the stratigraphic terminology most workers apply to the Claiborne Group in Arkansas conforms with the terminology of Louisiana. A surface exposure of the Carrizo Sand in Arkansas is lithologically identical with described exposures of the Carrizo in northwestern Louisiana.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[389:COTCSI]2.0.CO;2","usgsCitation":"Hosman, R., 1962, Correlation of the Carrizo Sand in Arkansas and adjacent states: Geological Society of America Bulletin, v. 73, no. 3, p. 389-394, https://doi.org/10.1130/0016-7606(1962)73[389:COTCSI]2.0.CO;2.","productDescription":"6 p.","startPage":"389","endPage":"394","costCenters":[],"links":[{"id":385946,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arkansas, Louisiana, Mississippi, Tennessee","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -94.52636718749999,\n 29.19053283229458\n ],\n [\n -88.24218749999999,\n 29.19053283229458\n ],\n [\n -88.24218749999999,\n 36.63316209558658\n ],\n [\n -94.52636718749999,\n 36.63316209558658\n ],\n [\n -94.52636718749999,\n 29.19053283229458\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Hosman, R. L.","contributorId":42978,"corporation":false,"usgs":true,"family":"Hosman","given":"R.","middleInitial":"L.","affiliations":[],"preferred":false,"id":816458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010811,"text":"70010811 - 1962 - Preliminary geologic report on the 1961 U.S. expedition to Bellingshausen Sea, Antarctica","interactions":[],"lastModifiedDate":"2026-02-25T17:10:03.874934","indexId":"70010811","displayToPublicDate":"1962-02-23T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Preliminary geologic report on the 1961 U.S. expedition to Bellingshausen Sea, Antarctica","docAbstract":"Five areas of outcrop were examined along 120 miles of the coast of the Bellingshausen Sea east of the Thurston Peninsula. Hornblende quartz diorite is the principal rock in the area and occurs in a body of batholithic dimensions. The quartz diorite contains inclusions of older granulitic rock and is cut by mafic dikes. An island in Paradise Harbor on the Palmer Peninsula was also examined briefly.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3504.671","issn":"00368075","usgsCitation":"Drake, A.A., 1962, Preliminary geologic report on the 1961 U.S. expedition to Bellingshausen Sea, Antarctica: Science, v. 135, no. 3504, p. 671-672.","productDescription":"2 p.","startPage":"671","endPage":"672","costCenters":[],"links":[{"id":218738,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Bellingshausen Sea, Antarctica","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -69.39594402462191,\n -66.071280772103\n ],\n [\n -90.1472833271104,\n -66.071280772103\n ],\n [\n -90.1472833271104,\n -73.22555094647112\n ],\n [\n -69.39594402462191,\n -73.22555094647112\n ],\n [\n -69.39594402462191,\n -66.071280772103\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"135","issue":"3504","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8775e4b0c8380cd7d388","contributors":{"authors":[{"text":"Drake, Avery A. Jr.","contributorId":81090,"corporation":false,"usgs":true,"family":"Drake","given":"Avery","suffix":"Jr.","middleInitial":"A.","affiliations":[],"preferred":false,"id":359702,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70238052,"text":"70238052 - 1962 - Browsing habits of white-tailed deer in the western Gulf Region","interactions":[],"lastModifiedDate":"2022-11-07T19:57:52.792816","indexId":"70238052","displayToPublicDate":"1962-02-01T13:41:54","publicationYear":"1962","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Browsing habits of white-tailed deer in the western Gulf Region","docAbstract":"No abstract available.
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","language":"English","publisher":"American Water Resources Association","publisherLocation":"Herndon, VA","usgsCitation":"Scott, C., and Skinner, J.V., 1962, Valve position indicator for P-46 sampler: Water Resources Bulletin, v. February, p. 9-10.","productDescription":"2 p.","startPage":"9","endPage":"10","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":321725,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"February","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57481e3ee4b07e28b664dc1d","contributors":{"authors":[{"text":"Scott, C.H.","contributorId":101634,"corporation":false,"usgs":true,"family":"Scott","given":"C.H.","email":"","affiliations":[],"preferred":false,"id":630418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Skinner, J. V.","contributorId":32504,"corporation":false,"usgs":true,"family":"Skinner","given":"J.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":630419,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70176600,"text":"70176600 - 1962 - Phenol contamination of an artesian aquifer at Alma, Michigan, 1962","interactions":[],"lastModifiedDate":"2016-09-22T14:14:24","indexId":"70176600","displayToPublicDate":"1962-01-30T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5209,"text":"Proceedings of the Society for Water Treatment and Examination","active":true,"publicationSubtype":{"id":10}},"title":"Phenol contamination of an artesian aquifer at Alma, Michigan, 1962","docAbstract":"No abstract available.
","language":"English","publisher":"Society for Water Treatment and Examination","publisherLocation":"Sutton, England","usgsCitation":"Deutsch, M., 1962, Phenol contamination of an artesian aquifer at Alma, Michigan, 1962: Proceedings of the Society for Water Treatment and Examination, v. 11, p. 94-100.","startPage":"94","endPage":"100","numberOfPages":"7","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":328867,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","city":"Alma","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -84.72656249999999,\n 43.33791397478761\n ],\n [\n -84.72656249999999,\n 43.415522593099915\n ],\n [\n -84.60090637207031,\n 43.415522593099915\n ],\n [\n -84.60090637207031,\n 43.33791397478761\n ],\n [\n -84.72656249999999,\n 43.33791397478761\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcff4e4b0824b2d17619c","contributors":{"authors":[{"text":"Deutsch, Morris","contributorId":69119,"corporation":false,"usgs":true,"family":"Deutsch","given":"Morris","email":"","affiliations":[],"preferred":false,"id":649338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207936,"text":"70207936 - 1962 - Lava tree molds of the September 1961 eruption, Kilauea Volcano, Hawaii","interactions":[],"lastModifiedDate":"2020-01-20T14:16:14","indexId":"70207936","displayToPublicDate":"1962-01-20T14:04:33","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Lava tree molds of the September 1961 eruption, Kilauea Volcano, Hawaii","docAbstract":"Well-developed lava tree molds were formed during the September 1961 eruption along the east rift zone of Kilauea Volcano. The upright molds were produced where fluid lava, flowing through dense tropical forest, became chilled against the larger trees and tree ferns and later drained away. Where the lava ponded temporarily in a structural valley, tree molds more than 14 feet high mark the high level attained by the flow.
","language":"English","publisher":"GSA","doi":"10.1130/0016-7606(1962)73[1153:LTMOTS]2.0.CO;2","usgsCitation":"Moore, J.G., and Richter, D., 1962, Lava tree molds of the September 1961 eruption, Kilauea Volcano, Hawaii: GSA Bulletin, v. 73, no. 9, p. 1153-1158, https://doi.org/10.1130/0016-7606(1962)73[1153:LTMOTS]2.0.CO;2.","productDescription":"6 p.","startPage":"1153","endPage":"1158","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":371388,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Hawaii","otherGeospatial":"East rift zone","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -155.2532958984375,\n 19.197053439464852\n ],\n [\n -154.8028564453125,\n 19.197053439464852\n ],\n [\n -154.8028564453125,\n 19.51319789966427\n ],\n [\n -155.2532958984375,\n 19.51319789966427\n ],\n [\n -155.2532958984375,\n 19.197053439464852\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Moore, James G. 0000-0002-7543-2401 jmoore@usgs.gov","orcid":"https://orcid.org/0000-0002-7543-2401","contributorId":2892,"corporation":false,"usgs":true,"family":"Moore","given":"James","email":"jmoore@usgs.gov","middleInitial":"G.","affiliations":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":779824,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richter, D.H.","contributorId":43325,"corporation":false,"usgs":true,"family":"Richter","given":"D.H.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":779825,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010743,"text":"70010743 - 1962 - Metallic spherules in tektites from Isabela, Philippine Islands","interactions":[],"lastModifiedDate":"2026-02-25T17:20:30.675416","indexId":"70010743","displayToPublicDate":"1962-01-12T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Metallic spherules in tektites from Isabela, Philippine Islands","docAbstract":"Iron-nickel spherules, as much as 0.5 mm in diameter, have been found completely embedded in some philippinites. The spherules consist mainly of kamacite with unidentified pink inclusions. The meteoritic origin of these spherules seems reasonable, suggesting that the tektites containing them were formed by asteroidal or meteoritic impact.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.135.3498.97","issn":"00368075","usgsCitation":"Chao, E.C., Adler, I., Dwornik, E., and Littler, J., 1962, Metallic spherules in tektites from Isabela, Philippine Islands: Science, v. 135, no. 3498, p. 97-98.","productDescription":"2 p.","startPage":"97","endPage":"98","costCenters":[],"links":[{"id":219636,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Philippines","otherGeospatial":"Isabela","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 121.8321580263597,\n 17.61561971503707\n ],\n [\n 121.8321580263597,\n 16.98428859480572\n ],\n [\n 122.52219426023623,\n 16.98428859480572\n ],\n [\n 122.52219426023623,\n 17.61561971503707\n ],\n [\n 121.8321580263597,\n 17.61561971503707\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"135","issue":"3498","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a54dbe4b0c8380cd6d071","contributors":{"authors":[{"text":"Chao, E. C. T.","contributorId":96713,"corporation":false,"usgs":true,"family":"Chao","given":"E.","email":"","middleInitial":"C. T.","affiliations":[],"preferred":false,"id":359547,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adler, I.","contributorId":13371,"corporation":false,"usgs":true,"family":"Adler","given":"I.","email":"","affiliations":[],"preferred":false,"id":359545,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dwornik, E.J.","contributorId":99128,"corporation":false,"usgs":true,"family":"Dwornik","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":359548,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Littler, J.","contributorId":40724,"corporation":false,"usgs":true,"family":"Littler","given":"J.","email":"","affiliations":[],"preferred":false,"id":359546,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}