A narrow gravity minimum anomaly of amplitude 30 mgals indicates that northern Owens Valley, California, a narrow fault-bounded trough or graben filled with Cenozoic clastic deposits to a depth of as much as 8,000 ft. Seismic-refraction measurements support this conclusion. Aeromagnetic and gravity measurements define a small, dense, and magnetic body buried by the valley fill of northern Owens Valley.
","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1439021","usgsCitation":"Pakiser, L.C., and Kane, M.F., 1962, Geophysical study of Cenozoic geologic structures of northern Owens Valley, California: Geophysics, v. 27, no. 3, p. 334-342, https://doi.org/10.1190/1.1439021.","productDescription":"9 p.","startPage":"334","endPage":"342","costCenters":[],"links":[{"id":385884,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Owens Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -118.71826171875,\n 38.151837403006766\n ],\n [\n -119.267578125,\n 38.14319750166766\n ],\n [\n -118.905029296875,\n 37.64903402157866\n ],\n [\n -118.63037109375,\n 37.142803443716836\n ],\n [\n -118.20190429687501,\n 36.19109202182454\n ],\n [\n -117.75146484375,\n 35.505400093441324\n ],\n [\n -117.00439453125,\n 35.66622234103479\n ],\n [\n -117.454833984375,\n 36.2354121683998\n ],\n [\n -117.98217773437499,\n 36.86204269508728\n ],\n [\n -118.05908203124999,\n 37.45741810262938\n ],\n [\n -118.41064453125,\n 37.84015683604136\n ],\n [\n -118.71826171875,\n 38.151837403006766\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"27","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pakiser, L. C.","contributorId":83512,"corporation":false,"usgs":true,"family":"Pakiser","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":816310,"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":816311,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220652,"text":"70220652 - 1962 - Stability relations of the ferruginous biotite, annite","interactions":[],"lastModifiedDate":"2021-05-24T11:54:17.595358","indexId":"70220652","displayToPublicDate":"1962-12-31T06:49:51","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Stability relations of the ferruginous biotite, annite","docAbstract":"Annite, KFe3AISi3O10(OH)2 a member of the iron biotites and the ferrous analogue of phlogopite, has been synthesized and its phase relations have been determined as functions of temperature, fugacity of oxygen (fo2), and total pressure (Ptotal≈PH2O+PH2). A method for controlling fo2at high total pressures is described, and data for the 'oxygen buffers' used are given. Buffers range from quartz+iron+fayalite assemblages (low fo2) to magnetite-hematite assemblages (high fo2). Optical properties and unit-cell dimensions of synthetic annites depend on the conditions of synthesis.By recalculating published analyses of natural iron-rich biotites it can be shown that one cannot assume a constant hydrogen content for such biotites. Oxidation may have occurred by drying at 115°C. Octahedral occupancy therefore cannot be calculated from such data.Phase relations of annite are presented in 2,070 and 1,035 bar sections. Depending on fo2-T values annite was found to decompose to one of the following assemblages: hematite+ sanidine, magnetite+sanidine, fayalite+leucite+kalsilite, iron+sanidine. All decompositions are dehydration and redox reactions and are sensitive to changes in fH20 and fo2 (or fH20 and fH2). At 2, 070 bars total pressure annite+magnetite+sanidine can coexist between 425°C and 825° C, depending upon the magnitude of fo2.In the presence of quartz the stability field of annite is more restricted. Phase equilibria in the system KAlSiO4-SiO2-Fe-O2-H2 have been summarized schematically.Wherever possible, thermodynamic extrapolations are made to test the internal consistency of the data. Enthalpies of formation are calculated for both annite and phlogopite. Ranges of fo2 values in nature as well as mechanisms for changes in fo2 are investigated. It is useful to distinguish between assemblages which are internally buffered with respect to fo2changes and those which are not buffered. The applications of individual reactions involving annite to specific geologic problems are discussed with respect to igneous, metamorphic, and sedimentary rocks.
","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/3.1.82","usgsCitation":"Eugster, H., and Wones, D.R., 1962, Stability relations of the ferruginous biotite, annite: Journal of Petrology, v. 3, no. 1, p. 82-125, https://doi.org/10.1093/petrology/3.1.82.","productDescription":"44 p.","startPage":"82","endPage":"125","costCenters":[],"links":[{"id":385878,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Eugster, H.P.","contributorId":99992,"corporation":false,"usgs":true,"family":"Eugster","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":816302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wones, D. R.","contributorId":104079,"corporation":false,"usgs":true,"family":"Wones","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":816303,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220650,"text":"70220650 - 1962 - Simple X-Y translation stage and indexing mechanism","interactions":[],"lastModifiedDate":"2021-05-24T11:41:13.016627","indexId":"70220650","displayToPublicDate":"1962-12-31T06:36:46","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3276,"text":"Review of Scientific Instruments","active":true,"publicationSubtype":{"id":10}},"title":"Simple X-Y translation stage and indexing mechanism","docAbstract":"No abstract available.
","language":"English","publisher":"American Institute of Physics","doi":"10.1063/1.1746580","usgsCitation":"Adler, I., and Massoni, C.J., 1962, Simple X-Y translation stage and indexing mechanism: Review of Scientific Instruments, v. 33, no. 3, p. 247-247, https://doi.org/10.1063/1.1746580.","productDescription":"1 p.","startPage":"247","endPage":"247","costCenters":[],"links":[{"id":385876,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"33","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Adler, I.","contributorId":13371,"corporation":false,"usgs":true,"family":"Adler","given":"I.","email":"","affiliations":[],"preferred":false,"id":816298,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Massoni, C. J.","contributorId":29082,"corporation":false,"usgs":true,"family":"Massoni","given":"C.","middleInitial":"J.","affiliations":[],"preferred":false,"id":816299,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70197633,"text":"70197633 - 1962 - Field Trip 2: San Francisco to Monterey via California Highways 1, 5, 17 and connecting routes","interactions":[],"lastModifiedDate":"2018-06-14T09:24:45","indexId":"70197633","displayToPublicDate":"1962-12-31T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"181","title":"Field Trip 2: San Francisco to Monterey via California Highways 1, 5, 17 and connecting routes","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geologic guide to the gas and oil fields of northern California: California Division of Mines and Geology Bulletin 181","language":"English","publisher":"California Division of Mines and Geology","usgsCitation":"Brabb, E.E., Bowen, O., and Hart, E., 1962, Field Trip 2: San Francisco to Monterey via California Highways 1, 5, 17 and connecting routes, chap. of Geologic guide to the gas and oil fields of northern California: California Division of Mines and Geology Bulletin 181, p. 381-390.","productDescription":"10 p.","startPage":"381","endPage":"390","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355043,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Brabb, E. E.","contributorId":43780,"corporation":false,"usgs":true,"family":"Brabb","given":"E.","middleInitial":"E.","affiliations":[],"preferred":false,"id":737996,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowen, O.E. Jr.","contributorId":49859,"corporation":false,"usgs":true,"family":"Bowen","given":"O.E.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":737997,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hart, E.W.","contributorId":205626,"corporation":false,"usgs":false,"family":"Hart","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":737998,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70197635,"text":"70197635 - 1962 - Geology of the northern Santa Cruz Mountains, California","interactions":[],"lastModifiedDate":"2018-06-14T09:45:12","indexId":"70197635","displayToPublicDate":"1962-12-31T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Geology of the northern Santa Cruz Mountains, California","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Geologic guide to the oil and gas fields of northern California: California Division Mines and Geology Bulletin 181","language":"English","publisher":"California Division Mines and Geology","usgsCitation":"Cummings, J., Touring, R., and Brabb, E.E., 1962, Geology of the northern Santa Cruz Mountains, California, chap. of Geologic guide to the oil and gas fields of northern California: California Division Mines and Geology Bulletin 181, p. 179-220.","productDescription":"42 p.","startPage":"179","endPage":"220","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Cummings, J.C.","contributorId":205630,"corporation":false,"usgs":false,"family":"Cummings","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":738000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Touring, R.M.","contributorId":205631,"corporation":false,"usgs":false,"family":"Touring","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":738001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brabb, E. E.","contributorId":43780,"corporation":false,"usgs":true,"family":"Brabb","given":"E.","middleInitial":"E.","affiliations":[],"preferred":false,"id":738002,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70220057,"text":"70220057 - 1962 - Temperature of crystallization of pyrrhotite and sphalerite from the Highland-Surprise Mine, Coeur d'Alene district, Idaho","interactions":[],"lastModifiedDate":"2021-04-19T12:17:15.714621","indexId":"70220057","displayToPublicDate":"1962-12-01T15:30:39","publicationYear":"1962","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":"Temperature of crystallization of pyrrhotite and sphalerite from the Highland-Surprise Mine, Coeur d'Alene district, Idaho","docAbstract":"The ore bodies of the Highland-Surprise Mine are replacements along shear zones in quartzose slate, quartzite, and phyllite of the Prichard Formation of the Belt series (Precambrian). Pyrite, arsenopyrite, pyrrhotite, sphalerite, chalcopyrite, and galena are the chief metallic minerals and were probably deposited in that order. Temperatures of formation were estimated for pyrrhotite-pyrite and sphalerite-pyrrhotite assemblages contained in the steeply dipping vein system. Measurements on 62 pyrrhotites indicate a range in temperature of crystallization between 370 degrees and 492 degrees C. (no correction required for confining pressures <2000 bars below 670 degrees C.), and measurements on 14 sphalerites indicate crystallization temperatures between 375 degrees and 460 degrees C. (uncorrected for confining pressure). No systematic temperature gradients were recognized. Minor elements in 23 pyrrhotite, 8 pyrite, 13 sphalerite, and 2 galena samples were determined. Partition ratios of Ni and Co in pyrrhotite-pyrite and sphalerite-pyrrhotite pairs are erratic. This suggests a dis-equilibrium distribution of these elements between the phases of each mineral pair and/or b) crystallization of the mineral pairs under different physical conditions.
","language":"English","publisher":"American Geological institute","doi":"10.2113/gsecongeo.57.8.1163","usgsCitation":"Arnold, R., Coleman, R.G., and Fryklund, V.C., 1962, Temperature of crystallization of pyrrhotite and sphalerite from the Highland-Surprise Mine, Coeur d'Alene district, Idaho: Economic Geology, v. 57, no. 8, p. 1163-1174, https://doi.org/10.2113/gsecongeo.57.8.1163.","productDescription":"12 p.","startPage":"1163","endPage":"1174","costCenters":[],"links":[{"id":385184,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","county":"Shoshone County","otherGeospatial":"Highland-Surprise Mine","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -116.89453125,\n 46.9502622421856\n ],\n [\n -115.48828125000001,\n 46.9502622421856\n ],\n [\n -115.48828125000001,\n 48.951366470947725\n ],\n [\n -116.89453125,\n 48.951366470947725\n ],\n [\n -116.89453125,\n 46.9502622421856\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"57","issue":"8","noUsgsAuthors":false,"publicationDate":"1962-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Arnold, R.","contributorId":94785,"corporation":false,"usgs":true,"family":"Arnold","given":"R.","email":"","affiliations":[],"preferred":false,"id":814466,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coleman, R. G.","contributorId":75170,"corporation":false,"usgs":true,"family":"Coleman","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":814467,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fryklund, Verne Charles Jr.","contributorId":104886,"corporation":false,"usgs":true,"family":"Fryklund","given":"Verne","suffix":"Jr.","email":"","middleInitial":"Charles","affiliations":[],"preferred":false,"id":814468,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70220792,"text":"70220792 - 1962 - Hornblendes formed during progressive metamorphism of amphibolites, northwest Adirondack Mountains, New York","interactions":[],"lastModifiedDate":"2021-05-25T18:22:16.308949","indexId":"70220792","displayToPublicDate":"1962-12-01T13:17:36","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":"Hornblendes formed during progressive metamorphism of amphibolites, northwest Adirondack Mountains, New York","docAbstract":"Hornblendes in amphibolite interlayers in the paragneiss of the northwest Adirondack Mountains undergo systematic changes in color, composition, and density during progressive metamorphism from almandine-amphibolite to hornblende-granulite facies. In contrast, indices of refraction of the hornblendes remain about constant. In the almandine-amphibolite facies the amphibolite layers have the bulk composition of a saturated basalt and consist of bluish-green hornblende, andesine, and quartz. As these layers are traced into the hornblende-granulite facies, their composition undergoes a progressive change to that of an olivine basalt with brownish-green hornblende, clinopyroxene and orthopyroxene, and calcic andesine as major constituents. Compositional changes in the hornblendes with increasing grade of metamorphism include increases in Ti, Na, K, Cr, V, and Sc. Decreases occur in the amounts of Mn, Zn, OH + F + Cl, and in the ratios Fe2O3/FeO and Fe/Mg. Density of the hornblendes increases from 3.260 to 3.278 with the increasing grade of metamorphism. These changes in the hornblendes with increasing T and P, although well denned, are less pronounced than those measured in biotites and garnets of the enclosing paragneiss. Large variations in the physical and chemical properties of hornblendes in metamafic rocks reconstituted above the epidote-amphibolite facies appear to be induced principally by critical changes in the bulk composition of the total rock, and not by the regional gradients in T, P, or by changes in kind, or composition, of the coexisting minerals.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[1499:HFDPMO]2.0.CO;2","usgsCitation":"Engel, A., and Engel, C., 1962, Hornblendes formed during progressive metamorphism of amphibolites, northwest Adirondack Mountains, New York: Geological Society of America Bulletin, v. 73, no. 12, p. 1499-1514, https://doi.org/10.1130/0016-7606(1962)73[1499:HFDPMO]2.0.CO;2.","productDescription":"16 p.","startPage":"1499","endPage":"1514","costCenters":[],"links":[{"id":385954,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Anirondack Mountains","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -75.34423828125001,\n 42.88401467044255\n ],\n [\n -73.399658203125,\n 42.88401467044255\n ],\n [\n -73.399658203125,\n 44.941473354802504\n ],\n [\n -75.34423828125001,\n 44.941473354802504\n ],\n [\n -75.34423828125001,\n 42.88401467044255\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Engel, A.E.J.","contributorId":241621,"corporation":false,"usgs":false,"family":"Engel","given":"A.E.J.","affiliations":[],"preferred":false,"id":816469,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engel, C.G.","contributorId":18489,"corporation":false,"usgs":true,"family":"Engel","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":816470,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010493,"text":"70010493 - 1962 - Early postglacial beavers in southeastern New England","interactions":[],"lastModifiedDate":"2026-02-24T16:55:43.88458","indexId":"70010493","displayToPublicDate":"1962-11-23T00:00:00","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":"Early postglacial beavers in southeastern New England","docAbstract":"Wood cut by Castor canadensis(?) has been found at or near the base of five peat deposits studied in open exposure. Beavers apparently entered the region about 12,000 years ago and rapidly occupied most low-lying places. Many existing bogs may be the result of early dams. The disturbance of pond sediments by beavers probably affects pollen stratigraphy. Charred wood in early beaver structures indicates forest fires and the possibility that the climate was drier than it is today.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.138.3543.906","issn":"00368075","usgsCitation":"Kaye, C.A., 1962, Early postglacial beavers in southeastern New England: Science, v. 138, no. 3543, p. 906-907.","productDescription":"2 p.","startPage":"906","endPage":"907","costCenters":[],"links":[{"id":219376,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"southeastern New England","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -74.78255117878962,\n 43.39411172743712\n ],\n [\n -74.78255117878962,\n 40.76451052187403\n ],\n [\n -70.33358859479547,\n 40.76451052187403\n ],\n [\n -70.33358859479547,\n 43.39411172743712\n ],\n [\n -74.78255117878962,\n 43.39411172743712\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"138","issue":"3543","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a048fe4b0c8380cd50a64","contributors":{"authors":[{"text":"Kaye, C. A.","contributorId":6003,"corporation":false,"usgs":true,"family":"Kaye","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359054,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220788,"text":"70220788 - 1962 - Tuscaloosa formation in Tennessee","interactions":[],"lastModifiedDate":"2021-05-25T18:15:12.552445","indexId":"70220788","displayToPublicDate":"1962-11-01T13:10:39","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":"Tuscaloosa formation in Tennessee","docAbstract":"Late Cretaceous Tuscaloosa Formation occurs as discontinuous remnants that cap many of the ridges in the Western Highland Rim. Typically the formation consists of well-rounded, poorly sorted chert gravel which is trimodal in size distribution. The gravel fraction (mode 15 to 40+ mm) consists of Devonian and Mississippian chert and a small percentage of sandstone pebbles. The medium sand fraction (mode 0.5 mm) consists mainly of angular to well-rounded chert grains developed by attrition during transport. Well-rounded and frosted quartz grains also are present. The fine fraction (mode 0.15 mm) consists of clay, authi-genic (?) mica, and quartz. At its eastern limit the Tuscaloosa is locally well sorted and contains quartz pebbles and a large proportion of quartz sand. Also present in the same area are well-sorted, heavy-mineral-bearing sands and bimodal (0.04, 0.2 mm) siltstone, which contains sand-sized pellet aggregates and fragmentary plant fossils. The finest fraction (less than 0.044 mm) of both eastern and western facies of the Tuscaloosa consists of 60-80 per cent quartz, 5-30 per cent kaolin, and 5-30 per cent montmorillonite, all of which are present in Devonian and Mississippian bedrock. Minor exotic constituents include volcanic(?) glass and heavy minerals. The Mississippian chert gravel in the Tuscaloosa is of local origin, but the Devonian chert was transported from a western source. Other components from a western source are sandstone pebbles and frosted sand grains, both of which probably were derived from Cambrian or Ordovician formations that cropped out on the Pascola arch, an eastward-sloping extension of the Ozark dome. Quartz pebbles, heavy minerals, and some of the angular quartz sand present at the eastern edge of the Tuscaloosa may have been derived from Pennsylvanian sandstone and conglomerates that cropped out north and south of the Pascola arch. Most of the Tuscaloosa Formation is believed to be of nonmarine origin, deposited on the eastward-sloping flank of the Pascola arch. The eastern facies of the Tuscaloosa is believed to be partly marine in origin, the exotic components having been swept in by longshore currents. During deposition of the Tuscaloosa, the Ozark dome and the Cincinnati arch were connected by the Pascola arch, which is now deeply buried beneath the Mississippi Embayment, At that time the Pascola arch stood structurally about 3000 feet higher than at present, and its structural shape and dimensions were comparable to the present Nashville dome. During deposition of the Tuscaloosa the Nashville dome was structurally about 1000 feet lower than at present, and its crest probably was submerged beneath the sea.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[1365:TFIT]2.0.CO;2","usgsCitation":"Marcher, M., and Stearns, R.G., 1962, Tuscaloosa formation in Tennessee: Geological Society of America Bulletin, v. 73, no. 11, p. 1365-1386, https://doi.org/10.1130/0016-7606(1962)73[1365:TFIT]2.0.CO;2.","productDescription":"22 p.","startPage":"1365","endPage":"1386","costCenters":[],"links":[{"id":385953,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Tennessee","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.82421875,\n 35.11990857099681\n ],\n [\n -82.52929687499999,\n 35.11990857099681\n ],\n [\n -82.52929687499999,\n 36.5978891330702\n ],\n [\n -89.82421875,\n 36.5978891330702\n ],\n [\n -89.82421875,\n 35.11990857099681\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Marcher, M.V.","contributorId":9267,"corporation":false,"usgs":true,"family":"Marcher","given":"M.V.","affiliations":[],"preferred":false,"id":816467,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stearns, R. G.","contributorId":95859,"corporation":false,"usgs":true,"family":"Stearns","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":816468,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220787,"text":"70220787 - 1962 - Flume studies of the transport of pebbles and cobbles on a sand bed","interactions":[],"lastModifiedDate":"2021-05-25T18:06:23.791591","indexId":"70220787","displayToPublicDate":"1962-11-01T13:03:05","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":"Flume studies of the transport of pebbles and cobbles on a sand bed","docAbstract":"During experiments on sediment transport and resistance to flow with a uniform 0.33-mm sand, data were recorded on the movement of individual rocks having intermediate diameters from about 0.1 to 0.5 foot. The experiments were conducted in a flume 2 feet wide by 60 feet long and for most runs, depth was held constant at 0.5 foot. The experiments showed that rocks on the sand bed moved downstream consistently only if the flow was in the upper regime - that is, only if the bed forms were plane bed, standing waves, or antidunes. The rocks moved at velocities that were approximately half the average velocity of the water. On all bed forms in the lower flow regime (ripples, ripples superimposed upon dunes, and dunes), the rocks moved upstream and down into the bed. That is, the rocks moved into a scour pocket that formed at the upstream side of the rock. The movement upstream and down into the bed is limited by and approximately equal to the distance below the original rock position of the minimum bed elevation plus approximately half the rock diameter. The data indicate that cross-bedded sand deposits formed by the ripple or dune phases of transport would contain few, if any, pebbles or cobbles. Because the flow, in at least the downstream reaches, of most rivers is in the lower regime, the upstream movement and scour into the bed demonstrated in these experiments is an important factor in the sorting process.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[1431:FSOTTO]2.0.CO;2","usgsCitation":"Fahnestock, R.K., and Haushild, W., 1962, Flume studies of the transport of pebbles and cobbles on a sand bed: Geological Society of America Bulletin, v. 73, no. 11, p. 1431-1436, https://doi.org/10.1130/0016-7606(1962)73[1431:FSOTTO]2.0.CO;2.","productDescription":"6 p.","startPage":"1431","endPage":"1436","costCenters":[],"links":[{"id":480371,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://hdl.handle.net/10217/196127","text":"External Repository"},{"id":385952,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fahnestock, Robert K.","contributorId":100381,"corporation":false,"usgs":true,"family":"Fahnestock","given":"Robert","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":816465,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":816466,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220656,"text":"70220656 - 1962 - Studies of fluid inclusions I: Low temperature application of a dual-purpose freezing and heating stage","interactions":[],"lastModifiedDate":"2021-05-24T12:29:26.087514","indexId":"70220656","displayToPublicDate":"1962-11-01T07:26:21","publicationYear":"1962","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":"Studies of fluid inclusions I: Low temperature application of a dual-purpose freezing and heating stage","docAbstract":"The design and operation of a microscope freezing stage developed for use at magnifications up to 500X are described. It makes possible studies of low-temperature phase changes such as the freezing of a saline water phase, and hence an estimate of the total salt concentration, in fluid inclusions as small as 10 microns (10-6 milligram in weight). The crystal or polished mineral plate containing the inclusions is viewed while immersed in a thermostated heat exchange medium (acetone) circulating rapidly in order to minimize thermal gradients. The stage permits easy operation at temperatures down to -35° C, with electrical control to ±0.05° C, and to much lower temperatures with manual control. With substitution of silicone oil for acetone, the same stage can be used for heating experiments up to +250° C. Calibration points in the low range indicate the accuracy of freezing temperature determinations on optimum material to be better than ±0.1° C. The low relief of ice crystals in water solution places considerable importance on sample selection, preparation, and lighting. As a result of almost ubiquitous and drastic supercooling (meta-stability), -35° C is inadequate to freeze most inclusions. Holding at -78.5° C (acetone + solid CO 2) for thirty minutes is generally adequate, although a few samples require extended immersion in liquid nitrogen at -196° C to cause freezing of even a part of their inclusions. Such extensive supercooling is not possible with most surface waters owing to the presence of abundant extraneous solid nuclei for the crystallization of ice.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.57.7.1045","usgsCitation":"Roedder, E., 1962, Studies of fluid inclusions I: Low temperature application of a dual-purpose freezing and heating stage: Economic Geology, v. 57, no. 1, p. 1045-1061, https://doi.org/10.2113/gsecongeo.57.7.1045.","productDescription":"17 p.","startPage":"1045","endPage":"1061","costCenters":[],"links":[{"id":385882,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"1","noUsgsAuthors":false,"publicationDate":"1962-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Roedder, E.","contributorId":100986,"corporation":false,"usgs":true,"family":"Roedder","given":"E.","affiliations":[],"preferred":false,"id":816308,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220655,"text":"70220655 - 1962 - Observations on the pyrite deposits of the huelva district, Spain, and their relation to volcanism","interactions":[],"lastModifiedDate":"2021-05-24T12:19:51.371943","indexId":"70220655","displayToPublicDate":"1962-11-01T07:13:42","publicationYear":"1962","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":"Observations on the pyrite deposits of the huelva district, Spain, and their relation to volcanism","docAbstract":"The felsitic porphyritic rocks that occur with Lower Carboniferous shale or slate in the Huelva district, Spain, were examined at the Rio Tinto, Tharsis, and La Zarza mines. Most of the bodies of porphyry are not intrusive into the shale, but instead consist of rhyolite flows overlain by variable thicknesses of coarse and fine pyroclastic rhyolite. These lie conformably beneath the shale. The pyroclastic beds are the ore horizon, and the ore bodies are confined to this stratigraphic zone. Various modes of formation have been postulated for the ore bodies of the Huelva district. The apparent limitation of ore to one strati-graphic horizon for more than 100 kilometers seems to favor a modified syngenetic origin with metallic elements derived from volcanic emanations.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.57.7.1071","usgsCitation":"Kinkel, A., 1962, Observations on the pyrite deposits of the huelva district, Spain, and their relation to volcanism: Economic Geology, v. 57, no. 7, p. 1071-1080, https://doi.org/10.2113/gsecongeo.57.7.1071.","productDescription":"10 p.","startPage":"1071","endPage":"1080","costCenters":[],"links":[{"id":385881,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Spain","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -9.140625,\n 41.77131167976407\n ],\n [\n -8.349609375,\n 42.22851735620852\n ],\n [\n -7.998046875,\n 42.00032514831621\n ],\n [\n -6.50390625,\n 41.96765920367816\n ],\n [\n -6.240234374999999,\n 41.50857729743935\n ],\n [\n -6.85546875,\n 40.91351257612758\n ],\n [\n -6.85546875,\n 39.977120098439634\n ],\n [\n -7.250976562499999,\n 39.639537564366684\n ],\n [\n -7.163085937499999,\n 39.095962936305476\n ],\n [\n -7.250976562499999,\n 38.47939467327645\n ],\n [\n -7.338867187500001,\n 37.75334401310656\n ],\n [\n -7.3828125,\n 37.19533058280065\n ],\n [\n -5.8447265625,\n 35.92464453144099\n ],\n [\n -1.9775390625,\n 36.80928470205937\n ],\n [\n -0.8349609375,\n 37.71859032558816\n ],\n [\n 0.3076171875,\n 38.788345355085625\n ],\n [\n 3.4716796874999996,\n 42.06560675405716\n ],\n [\n 2.98828125,\n 42.52069952914966\n ],\n [\n 0.8349609375,\n 42.8115217450979\n ],\n [\n -1.9335937499999998,\n 43.48481212891603\n ],\n [\n -7.646484374999999,\n 43.739352079154706\n ],\n [\n -8.173828125,\n 43.644025847699496\n ],\n [\n -9.31640625,\n 43.004647127794435\n ],\n [\n -9.140625,\n 41.77131167976407\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"57","issue":"7","noUsgsAuthors":false,"publicationDate":"1962-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Kinkel, A.R. Jr.","contributorId":87200,"corporation":false,"usgs":true,"family":"Kinkel","given":"A.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":816307,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220654,"text":"70220654 - 1962 - The ore knob massive sulfide copper deposit, North Carolina: An example of recrystallized ore","interactions":[],"lastModifiedDate":"2021-05-24T12:12:24.891787","indexId":"70220654","displayToPublicDate":"1962-11-01T07:08:21","publicationYear":"1962","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 ore knob massive sulfide copper deposit, North Carolina: An example of recrystallized ore","docAbstract":"Massive and disseminated pyrrhotite-chalcopyrite-pyrite ore replaced a fault zone in Precambrian Carolina Gneiss of Keith (1). Closely following sulfide deposition, vein sulfides and silicates in the wall rock were recrystallized under a rising temperature gradient to coarse-grained unoriented aggregates that contain late pyrite porphyroblasts in pyrrhotite. Boudinage, dilation, and flow structures are common.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.57.7.1116","usgsCitation":"Kinkel, A., 1962, The ore knob massive sulfide copper deposit, North Carolina: An example of recrystallized ore: Economic Geology, v. 57, no. 7, p. 1116-1121, https://doi.org/10.2113/gsecongeo.57.7.1116.","productDescription":"6 p.","startPage":"1116","endPage":"1121","costCenters":[],"links":[{"id":385880,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"North Carolina","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.6943359375,\n 36.56260003738545\n ],\n [\n -83.8037109375,\n 35.567980458012094\n ],\n [\n -84.5947265625,\n 35.06597313798418\n ],\n [\n -81.03515625,\n 35.209721645221386\n ],\n [\n -80.8154296875,\n 34.84987503195418\n ],\n [\n -79.5849609375,\n 34.813803317113155\n ],\n [\n -78.486328125,\n 33.87041555094183\n ],\n [\n -78.0029296875,\n 33.87041555094183\n ],\n [\n -76.5087890625,\n 34.88593094075317\n ],\n [\n -75.76171875,\n 35.67514743608467\n ],\n [\n -75.849609375,\n 36.491973470593685\n ],\n [\n -81.6943359375,\n 36.56260003738545\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"57","issue":"7","noUsgsAuthors":false,"publicationDate":"1962-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Kinkel, A.R. Jr.","contributorId":87200,"corporation":false,"usgs":true,"family":"Kinkel","given":"A.R.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":816306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220653,"text":"70220653 - 1962 - Trace element distribution in the searchlight, Nevada quartz monzonite stock","interactions":[],"lastModifiedDate":"2021-05-24T12:04:48.097911","indexId":"70220653","displayToPublicDate":"1962-11-01T07:01:09","publicationYear":"1962","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":"Trace element distribution in the searchlight, Nevada quartz monzonite stock","docAbstract":"Gold, silver, copper, and lead-bearing veins, non-radially zoned, occur just beyond the southern and western margins of the Searchlight, Nevada, quartz monzonite stock. Seven samples of the quartz monzonite and purified individual constituent minerals of the rock, representing apophyses and marginal and interior parts of the intrusive mass, were analyzed petrographically and spectrographically. A semiquantitative total-energy spectrographic method proved satisfactory for Cu, Pb, Ni, Co, Ga, Mo, Mn, Ti, V, Cr, Sr, and Zr, but too insensitive for Zn, Ag, and Au. A synthetic silicate base was used for preparation of standards and working curves. The modal trace element content of unaltered (hypothetical) quartz monzonite samples was determined from the trace element content of the purified minerals. Ferromagnesian minerals contain concentrations of Cu, Pb, Ni, Co, Mn, and Cr. Felsic minerals are low in these but high in Sr and Ga. Cu appears to have been partly released during chloritization of the mafic minerals. Ni, Cr, Zr show little difference between the unaltered (hypothetical) and actual rock. Ga, V, Mn, Sr are in lesser quantities in the altered rock. Pb and Cu also show a loss, especially nearest largest Pb and Cu producers. Pb, Cu, V occur in the spatially related veins, but Sr or Ga have not been reported to date. Pb/Cu in unaltered rock compared to altered rock is 1.6/1; past mining production ratio of Pb/Cu is 2.6/1. While further work is needed, the trace element pattern suggests a possible means of identifying a \"productive\" intrusive body.
","language":"English","publisher":"Society for Economic Geologist","doi":"10.2113/gsecongeo.57.7.1062","usgsCitation":"Shrivastava, J., and Proctor, P., 1962, Trace element distribution in the searchlight, Nevada quartz monzonite stock: Economic Geology, v. 57, no. 7, p. 1062-1070, https://doi.org/10.2113/gsecongeo.57.7.1062.","productDescription":"9 p.","startPage":"1062","endPage":"1070","costCenters":[],"links":[{"id":385879,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"7","noUsgsAuthors":false,"publicationDate":"1962-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Shrivastava, J.N.","contributorId":258272,"corporation":false,"usgs":false,"family":"Shrivastava","given":"J.N.","email":"","affiliations":[],"preferred":false,"id":816304,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Proctor, P.D.","contributorId":45391,"corporation":false,"usgs":true,"family":"Proctor","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":816305,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010717,"text":"70010717 - 1962 - Pollen sequence at Kirchner Marsh, Minnesota","interactions":[],"lastModifiedDate":"2026-02-24T17:10:57.723005","indexId":"70010717","displayToPublicDate":"1962-10-26T00:00:00","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":"Pollen sequence at Kirchner Marsh, Minnesota","docAbstract":"A pollen diagram from Kirchner Marsh, southeastern Minnesota, records a continuous vegetation sequence from the time of Late Wisconsin ice retreat from the region. The late-glacial and early postglacial portions of the diagram are correlated with a radiocarbon-dated diagram from Madelia, Minnesota. Both diagrams show a series of maxima of pollen types in the early postglacial that suggest a significant climatic change at that time. The Kirchner diagram, in addition, shows high percentages of nonarboreal pollen later in the postglacial that indicate an advance of prairie elements into the area between 7200 and 5000 years ago.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.138.3539.526","issn":"00368075","usgsCitation":"Winter, T.C., 1962, Pollen sequence at Kirchner Marsh, Minnesota: Science, v. 138, no. 3539, p. 526-528.","productDescription":"3 p.","startPage":"526","endPage":"528","costCenters":[],"links":[{"id":219551,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Kirchner Marsh, southeastern Minnesota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -94.5353613530863,\n 44.9862199607831\n ],\n [\n -94.5353613530863,\n 43.480942652159\n ],\n [\n -91.20989848000198,\n 43.480942652159\n ],\n [\n -91.19183277165098,\n 43.93030288730306\n ],\n [\n -91.5563212737562,\n 44.08932263212808\n ],\n [\n -91.79670775565427,\n 44.35187146621146\n ],\n [\n -93.10837332847433,\n 44.916917148974335\n ],\n [\n -94.5353613530863,\n 44.9862199607831\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"138","issue":"3539","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7cd5e4b0c8380cd79be1","contributors":{"authors":[{"text":"Winter, T. C.","contributorId":23485,"corporation":false,"usgs":true,"family":"Winter","given":"T.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":359483,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37740,"text":"37740 - 1962 - 1962 address list of refuge managers","interactions":[],"lastModifiedDate":"2014-07-24T13:20:49","indexId":"37740","displayToPublicDate":"1962-10-01T13:20:06","publicationYear":"1962","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":"448","title":"1962 address list of refuge managers","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in Branch of Wildlife Refuge.","usgsCitation":"U.S. Fish and Wildlife Service, 1962, 1962 address list of refuge managers: Wildlife Leaflet 448, 9 p.","productDescription":"9 p.","numberOfPages":"9","temporalStart":"1962-01-01","temporalEnd":"1962-12-31","costCenters":[],"links":[{"id":290931,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd085e4b0824b2d1763ee","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529691,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1003296,"text":"1003296 - 1962 - Evaluation of some heparinized capillaries for microhematocrit determinations of warm-water fishes","interactions":[],"lastModifiedDate":"2025-08-01T15:39:53.140727","indexId":"1003296","displayToPublicDate":"1962-10-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"Evaluation of some heparinized capillaries for microhematocrit determinations of warm-water fishes","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1962)24[188:EOSHCF]2.0.CO;2","usgsCitation":"Mairs, D., and Kennedy, T., 1962, Evaluation of some heparinized capillaries for microhematocrit determinations of warm-water fishes: Progressive Fish-Culturist, v. 24, no. 4, p. 188-189, https://doi.org/10.1577/1548-8659(1962)24[188:EOSHCF]2.0.CO;2.","productDescription":"2 p.","startPage":"188","endPage":"189","costCenters":[{"id":606,"text":"Upper Midwest Environmental Sciences Center","active":true,"usgs":true}],"links":[{"id":131317,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a09e4b07f02db5fab53","contributors":{"authors":[{"text":"Mairs, D.F.","contributorId":40936,"corporation":false,"usgs":true,"family":"Mairs","given":"D.F.","affiliations":[],"preferred":false,"id":313084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kennedy, T.E.","contributorId":101604,"corporation":false,"usgs":true,"family":"Kennedy","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":313085,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1014051,"text":"1014051 - 1962 - A new medium for isolation and presumptive identification of Aeromonas salmonicida","interactions":[],"lastModifiedDate":"2025-08-01T15:44:09.701885","indexId":"1014051","displayToPublicDate":"1962-10-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"A new medium for isolation and presumptive identification of Aeromonas salmonicida","docAbstract":"No abstract available.
","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1962)24[184:ANMFIA]2.0.CO;2","usgsCitation":"Bullock, G.L., 1962, A new medium for isolation and presumptive identification of Aeromonas salmonicida: Progressive Fish-Culturist, v. 24, no. 4, p. 184-184, https://doi.org/10.1577/1548-8659(1962)24[184:ANMFIA]2.0.CO;2.","productDescription":"1 p.","startPage":"184","endPage":"184","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131456,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abc03","contributors":{"authors":[{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319688,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010742,"text":"70010742 - 1962 - Unit-cell dimensions of natural and synthetic scapolites","interactions":[],"lastModifiedDate":"2026-02-25T16:11:49.104366","indexId":"70010742","displayToPublicDate":"1962-09-14T00:00:00","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":"Unit-cell dimensions of natural and synthetic scapolites","docAbstract":"In natural scapolites the cell dimension a shows a regular increase from marialite to meionite composition, while c remains constant. Both a and c of synthetic meionite are larger than the corresponding dimensions of synthetic marialite. The cell volume of both natural and synthetic scapolites is a nearly linear function of composition. Variations in cell dimensions of scapolites may be caused by differences in structural state similar to those in plagioclase feldspars.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.137.3533.853","issn":"00368075","usgsCitation":"Eugster, H., Prostka, H., and Appleman, D., 1962, Unit-cell dimensions of natural and synthetic scapolites: Science, v. 137, no. 3533, p. 853-854.","productDescription":"2 p.","startPage":"853","endPage":"854","costCenters":[],"links":[{"id":219635,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"137","issue":"3533","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbc89e4b08c986b328cbb","contributors":{"authors":[{"text":"Eugster, H.P.","contributorId":99992,"corporation":false,"usgs":true,"family":"Eugster","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":359544,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Prostka, H.J.","contributorId":31369,"corporation":false,"usgs":true,"family":"Prostka","given":"H.J.","affiliations":[],"preferred":false,"id":359542,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Appleman, D.E.","contributorId":44909,"corporation":false,"usgs":true,"family":"Appleman","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":359543,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010551,"text":"70010551 - 1962 - Contamination of vegetation by tetraethyl lead","interactions":[],"lastModifiedDate":"2026-02-25T16:22:06.938996","indexId":"70010551","displayToPublicDate":"1962-09-07T00:00:00","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":"Contamination of vegetation by tetraethyl lead","docAbstract":"Tetraethyl lead is a normal constituent of vegetation growing along our highways. Washed grass near Denver contained 3000 ppm (in ash) near major intersections and > 50 ppm for 500 feet downwind. Vegetables grown within 25 feet of a road in upstate New York and western Maryland averaged 80 to 115 ppm.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.137.3532.765","issn":"00368075","usgsCitation":"Cannon, H., and Bowles, J., 1962, Contamination of vegetation by tetraethyl lead: Science, v. 137, no. 3532, p. 765-766.","productDescription":"2 p.","startPage":"765","endPage":"766","costCenters":[],"links":[{"id":218960,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryland, New York","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.02326150069752,\n 45.222679457328326\n ],\n [\n -76.02326150069752,\n 43.72150362077252\n ],\n [\n -73.42565560121596,\n 43.72150362077252\n ],\n [\n -73.42565560121596,\n 45.222679457328326\n ],\n [\n -76.02326150069752,\n 45.222679457328326\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n },\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -79.50848433661743,\n 39.73002227276692\n ],\n [\n -79.50848433661743,\n 39.24767569481017\n ],\n [\n -78.75074335528438,\n 39.49974212117189\n ],\n [\n -78.16783640696123,\n 39.52976508302085\n ],\n [\n -77.73404571575558,\n 39.24767569481017\n ],\n [\n -77.73404571575558,\n 39.73002227276692\n ],\n [\n -79.50848433661743,\n 39.73002227276692\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"137","issue":"3532","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059fa49e4b0c8380cd4da09","contributors":{"authors":[{"text":"Cannon, H.L.","contributorId":43416,"corporation":false,"usgs":true,"family":"Cannon","given":"H.L.","email":"","affiliations":[],"preferred":false,"id":359157,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bowles, J.M.","contributorId":33314,"corporation":false,"usgs":true,"family":"Bowles","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":359156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":37738,"text":"37738 - 1962 - Big game inventory for 1961","interactions":[],"lastModifiedDate":"2014-07-22T13:36:41","indexId":"37738","displayToPublicDate":"1962-09-01T13:36:04","publicationYear":"1962","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":"446","title":"Big game inventory for 1961","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in Bird and Mammal Laboratories, Branch of Wildlife Research.","usgsCitation":"U.S. Branch of Wildlife Research, 1962, Big game inventory for 1961 (Revises Wildlife Leaflet 342 (1952).): Wildlife Leaflet 446, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290720,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet 342 (1952).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd085e4b0824b2d1763f0","contributors":{"authors":[{"text":"U.S. Branch of Wildlife Research","contributorId":127903,"corporation":true,"usgs":false,"organization":"U.S. Branch of Wildlife Research","id":529690,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220783,"text":"70220783 - 1962 - Late cretaceous and subsequent structural development of the northern Mississippi Embayment area","interactions":[],"lastModifiedDate":"2021-05-25T18:01:14.190725","indexId":"70220783","displayToPublicDate":"1962-09-01T12:57:06","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":"Late cretaceous and subsequent structural development of the northern Mississippi Embayment area","docAbstract":"During early Late Cretaceous the area of the northern Mississippi Embayment was occupied by a structural and topographic dome standing nearly 1000 feet above sea level. Rocks as old as Cambrian were exposed on its crest. Downwarping of the dome, which commenced in Late Cretaceous time, resulted in the development of the Mississippi Embayment syncline, now filled with sediments of Cretaceous, Paleocene, and Eocene age. The flanks of the Mississippi Embayment syncline slope uniformly about 30 feet per mile. Most of the bending occurred near the synclinal axis, which generally follows the present course of the Mississippi River. Faults cutting the Paleozoic basement and, in some areas, extending upward into the overlying younger rocks resulted from superposition of the narrow synclinal bend across the now-buried structural high. Adjustment also probably occurred by faulting of Paleozoic rocks along the Tennessee River, where the eastern flank of the syncline was bent downward. As a result of structural movements during the Cretaceous and later periods, the old dome has been depressed beneath the Mississippi Embayment and now forms the Pascola arch connecting the Ozark and Nashville domes.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[1387:LCASSD]2.0.CO;2","usgsCitation":"Stearns, R., and Marcher, M.V., 1962, Late cretaceous and subsequent structural development of the northern Mississippi Embayment area: Geological Society of America Bulletin, v. 73, no. 11, p. 1387-1394, https://doi.org/10.1130/0016-7606(1962)73[1387:LCASSD]2.0.CO;2.","productDescription":"8 p.","startPage":"1387","endPage":"1394","costCenters":[],"links":[{"id":385951,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"MIssissippi","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -91.7138671875,\n 29.99300228455108\n ],\n [\n -87.978515625,\n 29.99300228455108\n ],\n [\n -87.978515625,\n 35.71083783530009\n ],\n [\n -91.7138671875,\n 35.71083783530009\n ],\n [\n -91.7138671875,\n 29.99300228455108\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"73","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stearns, Richard G.","contributorId":258557,"corporation":false,"usgs":false,"family":"Stearns","given":"Richard G.","affiliations":[],"preferred":false,"id":816463,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":816464,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70220782,"text":"70220782 - 1962 - Remanent magnetism as a contributor to some aeromagnetic anomalies","interactions":[],"lastModifiedDate":"2021-05-25T17:54:36.232087","indexId":"70220782","displayToPublicDate":"1962-09-01T12:51:11","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":"Remanent magnetism as a contributor to some aeromagnetic anomalies","docAbstract":"An investigation of some aeromagnetic anomalies in north-central Montana shows that remanent magnetization is the dominant factor in anomalies over some rocks and a contributing factor in anomalies over others. In volcanic rocks, remanence is commonly south-seeking down and has an intensity approximately ten times the induced intensity of magnetization. Remanence is shown to be the dominating factor in anomalies over volcanic rocks by the agreement between the profiles of an observed anomaly over a volcanic rock body and an anomaly calculated from remanence data for the same body. In intrusive rocks, the remanence is north-seeking down and comparable in intensity to the induced intensity of magnetization. That remanence also contributes to the anomalies over some intrusive rocks is shown by the agreement between the profiles of an observed anomaly over an intrusive body and an anomaly calculated from the resultant of induced and remanent magnetizations. A consistent relationship between the axis of the anomaly, or direction between the anomaly high and low, and the horizontal direction of magnetization suggests that the direction of the anomaly axis can be used to indicate the horizontal direction of magnetization in this area.
","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1439024","usgsCitation":"Books, K.G., 1962, Remanent magnetism as a contributor to some aeromagnetic anomalies: Geophysics, v. 27, no. 3, p. 359-375, https://doi.org/10.1190/1.1439024.","productDescription":"17 p.","startPage":"359","endPage":"375","costCenters":[],"links":[{"id":385950,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Books, K. G.","contributorId":99129,"corporation":false,"usgs":true,"family":"Books","given":"K.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":816462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220778,"text":"70220778 - 1962 - Perspective on problems of hydrogeology","interactions":[],"lastModifiedDate":"2021-05-25T17:48:19.016446","indexId":"70220778","displayToPublicDate":"1962-09-01T12:43:52","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":"Perspective on problems of hydrogeology","docAbstract":"A trend toward increasing use of test drilling and subsurface exploration is resulting in a decreasing reliance on human experience in coping with problems in hydrogeology. Application of \"observation and inference\" and discreet abstraction of readily available data will solve more problems than is now realized.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1962)73[1147:POPOH]2.0.CO;2","usgsCitation":"LeGrand, H.E., 1962, Perspective on problems of hydrogeology: Geological Society of America Bulletin, v. 73, no. 9, p. 1147-1152, https://doi.org/10.1130/0016-7606(1962)73[1147:POPOH]2.0.CO;2.","productDescription":"6 p.","startPage":"1147","endPage":"1152","costCenters":[],"links":[{"id":385949,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"73","issue":"9","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"LeGrand, H. E.","contributorId":54571,"corporation":false,"usgs":true,"family":"LeGrand","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":816461,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70220657,"text":"70220657 - 1962 - The origin of jasperoid in limestone","interactions":[],"lastModifiedDate":"2021-05-24T12:37:43.054398","indexId":"70220657","displayToPublicDate":"1962-09-01T07:33:31","publicationYear":"1962","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 jasperoid in limestone","docAbstract":"The name jasperoid has been applied to rocks that consist mainly of silica and that have formed by replacement. This paper considers only those jasperoids formed by replacement of limestone. Major problems involved in the origin of such jasperoid include: source of the silica; nature of solutions that dissolve, transport, and precipitate silica; and the mechanism of replacement of limestone by silica. The answers to these problems are of practical as well as scientific interest because many jasperoid bodies are closely related to mineralization. Silica may be derived from: juvenile silica of magmatic origin; silica leached from underlying rocks by hydrothermal solutions; silica locally derived from enclosing rocks by circulating solutions; and silica carried downward in ground water from the weathering of overlying rocks. The nature and the concentration of other substances in solutions influence,in a complex manner, the ability of these solutions to dissolve, transport, and precipitate silica. Nevertheless, the following generalizations can be made. The solubility and rate of solution of silica in water at moderate pressure increase slowly with temperature up to 200 degrees C.; from 200 degrees to 360 degrees C. they increase rapidly; above 360 degrees C. solubility is pressure dependent, increasing steadily at high pressure and decreasing slightly at moderate pressure due to the formation of a vapor phase. The pH has slight effect on the ionic solubility of silica in the range from pH 1 to ph 9 at low temperature. The effect of other components on the solubility of silica is probably subordinate to that of temperature above 200 degrees C., but becomes increasingly important as the temperature falls below that point. Most jasperoid bodies form by both replacement and silica deposition in voids, with replacement dominant during the early phase, and precipitation dominant during later phases. Replacement of limestone by silica is favored by relatively low temperature acid solutions, and the presence of CO 2 . As limestone dissolves, Ca ions are released to promote the precipitation of colloidal silica. Acid solutions then diffuse through this gelatinous film to continue dissolving limestone behind it; the Ca ions diffusing outward cause the precipitation of more colloidal silica at the solution-gel interface. As the gel mass ages, it shrinks, hardens, and ruptures. More silica is then deposited in the fractures. Eventually the gel crystallizes to a dense mass of aphanitic quartz and chalcedony, with shrinkage cracks and vugs filled or coated with younger coarse-grained quartz and other minerals that have been deposited directly from solution. The theory that relatively low temperature favors the formation of jasperoid replacement bodies in carbonate rocks, and high temperature inhibits their formation, offers an explanation for the gap that is observed in some districts between contact metasomatic lime silicates and siliceous replacement of limestone. This gap is characterized by the lack of any reaction between limestone and silica-bearing solutions moving through it.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.57.6.861","usgsCitation":"Lovering, T., 1962, The origin of jasperoid in limestone: Economic Geology, v. 57, no. 6, p. 861-889, https://doi.org/10.2113/gsecongeo.57.6.861.","productDescription":"29 p.","startPage":"861","endPage":"889","costCenters":[],"links":[{"id":385883,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"57","issue":"6","noUsgsAuthors":false,"publicationDate":"1962-09-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Lovering, T.G.","contributorId":91098,"corporation":false,"usgs":true,"family":"Lovering","given":"T.G.","email":"","affiliations":[],"preferred":false,"id":816309,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}