This report concerns the progress in remote sensing during the period 1972–1976. Remote sensing has been variously defined but is basically the art or science of telling something about an object without touching it.
\nDuring the past four years, the major research thrusts have been in three areas:
\n\n(1) computer-assisted enhancement and interpretation systems;
\n\n(2) earth science applications of Landsat data;
\n\n(3) and investigations of the usefulness of observations of luminescence, thermal infrared, and microwave energies.
Based on the data sales at the EROS Data Center, the largest users of the Landsat data are industrial companies, followed by government agencies (both national and foreign), and academic institutions.
\nThermal surveys from aircraft have become largely operational, however, significant research is being undertaken in the field of thermal modeling and analysis of high altitude images. Microwave research is increasing rapidly and programs are being developed for satellite observations. Microwave research is concentrating on oil spill detection, soil moisture measurement, and observations of ice distributions. Luminescence investigations offer promise for becoming a quantitative method of assessing vegetation stress and pollutant concentrations.
","language":"English","publisher":"Elsevier","doi":"10.1016/0031-8663(76)90013-2","issn":"00318663","usgsCitation":"Fischer, W.A., Hemphill, W.R., and Kover, A., 1976, Progress in remote sensing (1972-1976): Photogrammetria, v. 32, no. 2, p. 33-72, https://doi.org/10.1016/0031-8663(76)90013-2.","productDescription":"40 p.","startPage":"33","endPage":"72","numberOfPages":"40","temporalStart":"1972-01-01","temporalEnd":"1976-12-31","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":269814,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-8663(76)90013-2"},{"id":221493,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"32","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a8e67e4b0c8380cd7f191","contributors":{"authors":[{"text":"Fischer, W. A.","contributorId":91571,"corporation":false,"usgs":true,"family":"Fischer","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359885,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hemphill, W. R.","contributorId":19525,"corporation":false,"usgs":true,"family":"Hemphill","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359883,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kover, Allan","contributorId":24094,"corporation":false,"usgs":true,"family":"Kover","given":"Allan","affiliations":[],"preferred":false,"id":359884,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1007780,"text":"1007780 - 1976 - Capturing and marking howler monkeys for field behavioral studies","interactions":[],"lastModifiedDate":"2025-07-17T15:23:10.650303","indexId":"1007780","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3118,"text":"Primates","active":true,"publicationSubtype":{"id":10}},"title":"Capturing and marking howler monkeys for field behavioral studies","docAbstract":"Methods for capturing and marking howler monkeys for ecological studies are discussed. Systems for capturing and handling animals are compared. A dart with liquid Sernylan for capture and Sernylan or Ketamine as a holding drug was preferred to darts using powdered succinylcholine chloride (SCC) and ether. The effectiveness of both Sernylan and SCC is compared and dosages are given for Sernylan in howler monkeys and SCC for howlers and capuchins. The advantages of Ketamine over ether as a holding drug are discussed. Animals can be marked with leg-bands, collars, and freeze-branding.
","language":"English","publisher":"Springer","doi":"10.1007/BF02382910","usgsCitation":"Scott, N., Scott, A., and Malmgren, L., 1976, Capturing and marking howler monkeys for field behavioral studies: Primates, v. 17, p. 527-533, https://doi.org/10.1007/BF02382910.","productDescription":"7 p.","startPage":"527","endPage":"533","numberOfPages":"7","costCenters":[{"id":651,"text":"Western Ecological Research Center","active":true,"usgs":true}],"links":[{"id":129769,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"17","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5f37","contributors":{"authors":[{"text":"Scott, N.J. Jr.","contributorId":8407,"corporation":false,"usgs":true,"family":"Scott","given":"N.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":316017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, A.F.","contributorId":20284,"corporation":false,"usgs":true,"family":"Scott","given":"A.F.","email":"","affiliations":[],"preferred":false,"id":316018,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Malmgren, L.A.","contributorId":21495,"corporation":false,"usgs":true,"family":"Malmgren","given":"L.A.","email":"","affiliations":[],"preferred":false,"id":316019,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010045,"text":"70010045 - 1976 - Distribution of small channels on the Martian surface","interactions":[],"lastModifiedDate":"2025-02-28T16:44:58.760113","indexId":"70010045","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1963,"text":"Icarus","active":true,"publicationSubtype":{"id":10}},"title":"Distribution of small channels on the Martian surface","docAbstract":"The distribution of small channels on Mars has been mapped from Mariner 9 images, at the 1:5 000 000 scale, by the author. The small channels referred to here are small valleys ranging in width from the resolution limit of the Mariner 9 wide-angle images (???1 km) to about 10 km. The greatest density of small band occurs in dark cratered terrain. This dark zone forms a broad subequatorial band around the planet. The observed distribution may be the result of decreased small-channel visibility in bright areas due to obscuration by a high albedo dust or sediment mantle. Crater densities within two small-channel segments show crater size-frequency distributions consistent with those of the oldest of the heavily cratered plains units. Such crater densities coupled with the almost exclusive occurrence of small channels in old cratered terrain and the generally degraded appearance of small channels in the high-resolution images (???100 m) imply a major episode of small-channel formation early in Martian geologic history. ?? 1976.","language":"English","publisher":"Elsevier","doi":"10.1016/0019-1035(76)90182-2","issn":"00191035","usgsCitation":"Pieri, D., 1976, Distribution of small channels on the Martian surface: Icarus, v. 27, no. 1, p. 25-50, https://doi.org/10.1016/0019-1035(76)90182-2.","productDescription":"26 p.","startPage":"25","endPage":"50","numberOfPages":"26","costCenters":[],"links":[{"id":218696,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a0301e4b0c8380cd502cb","contributors":{"authors":[{"text":"Pieri, D.","contributorId":80814,"corporation":false,"usgs":true,"family":"Pieri","given":"D.","email":"","affiliations":[],"preferred":false,"id":357766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010999,"text":"70010999 - 1976 - Interactive computer programs for petrologic modeling with extended Q-mode factor analysis","interactions":[],"lastModifiedDate":"2013-01-21T16:12:50","indexId":"70010999","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"Interactive computer programs for petrologic modeling with extended Q-mode factor analysis","docAbstract":"An extended form of Q-mode factor analysis may be used if the row-sums of the data matrix are constant and can be helpful especially in developing and testing petrologic-mixing models for igneous systems. The first step is to represent the sample compositions as unit vectors in M-dimensional space and then to project them into space of fewer dimensions (m) as determined to be appropriate from a factor-variance diagram. Compositions thought to be those of possible end-members in the petrologic system then are represented as vectors in the M-dimensional space and projected into the same space as the sample vectors. If these vectors remain close to unity in length after projection, the corresponding compositions can serve as end-member compositions for the model. After m suitable end-member compositions have been identified, each sample composition is expressed as a mixture of the end-members by computation of the composition loadings. The interactive computer programs presented are useful in these procedures because of the trial-and-error nature of the modeling procedures. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(76)90039-X","issn":"00983004","usgsCitation":"Miesch, A., 1976, Interactive computer programs for petrologic modeling with extended Q-mode factor analysis: Computers & Geosciences, v. 2, no. 4, p. 439-492, https://doi.org/10.1016/0098-3004(76)90039-X.","startPage":"439","endPage":"492","numberOfPages":"54","costCenters":[],"links":[{"id":221561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266212,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(76)90039-X"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3cd5e4b0c8380cd630a6","contributors":{"authors":[{"text":"Miesch, A.T.","contributorId":88726,"corporation":false,"usgs":true,"family":"Miesch","given":"A.T.","affiliations":[],"preferred":false,"id":360059,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010350,"text":"70010350 - 1976 - The national coal-resources data system of the U.S. geological survey","interactions":[],"lastModifiedDate":"2013-01-21T16:09:12","indexId":"70010350","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1315,"text":"Computers & Geosciences","printIssn":"0098-3004","active":true,"publicationSubtype":{"id":10}},"title":"The national coal-resources data system of the U.S. geological survey","docAbstract":"The National Coal Resources Data System (NCRDS) was designed by the U.S. Geological Survey (USGS) to meet the increasing demands for rapid retrieval of information on coal location, quantity, quality, and accessibility. An interactive conversational query system devised by the USGS retrieves information from the data bank through a standard computer terminal. The system is being developed in two phases. Phase I, which currently is available on a limited basis, contains published areal resource and chemical data. The primary objective of this phase is to retrieve, calculate, and tabulate coal-resource data by area on a local, regional, or national scale. Factors available for retrieval include: state, county, quadrangle, township, coal field, coal bed, formation, geologic age, source and reliability of data, and coal-bed rank, thickness, overburden, and tonnage, or any combinations of variables. In addition, the chemical data items include individual values for proximate and ultimate analyses, BTU value, and several other physical and chemical tests. Information will be validated and deleted or updated as needed. Phase II is being developed to store, retrieve, and manipulate basic point source coal data (e.g., field observations, drill-hole logs), including geodetic location; bed thickness; depth of burial; moisture; ash; sulfur; major-, minor-, and trace-element content; heat value; and characteristics of overburden, roof rocks, and floor rocks. The computer system may be used to generate interactively structure-contour or isoline maps of the physical and chemical characteristics of a coal bed or to calculate coal resources. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Computers and Geosciences","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1016/0098-3004(76)90062-5","issn":"00983004","usgsCitation":"Carter, M., 1976, The national coal-resources data system of the U.S. geological survey: Computers & Geosciences, v. 2, no. 3, p. 331-340, https://doi.org/10.1016/0098-3004(76)90062-5.","startPage":"331","endPage":"340","numberOfPages":"10","costCenters":[],"links":[{"id":219366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266209,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0098-3004(76)90062-5"}],"volume":"2","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505badf8e4b08c986b323e95","contributors":{"authors":[{"text":"Carter, M.D.","contributorId":31382,"corporation":false,"usgs":true,"family":"Carter","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":358697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011165,"text":"70011165 - 1976 - Automation in photogrammetry: Recent developments and applications (1972-1976)","interactions":[],"lastModifiedDate":"2013-03-20T19:51:32","indexId":"70011165","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3050,"text":"Photogrammetria","active":true,"publicationSubtype":{"id":10}},"title":"Automation in photogrammetry: Recent developments and applications (1972-1976)","docAbstract":"An overview of recent developments in the automation of photogrammetry in various countries is presented. Conclusions regarding automated photogrammetry reached at the 1972 Congress in Ottawa are reviewed first as a background for examining the developments of 1972-1976. Applications are described for each country reporting significant developments. Among fifteen conclusions listed are statements concerning: the widespread practice of equipping existing stereoplotters with simple digitizers; the growing tendency to use minicomputers on-line with stereoplotters; the optimization of production of digital terrain models by progressive sampling in stereomodels; the potential of digitization of a photogrammetric model by density correlation on epipolar lines; the capabilities and economic aspects of advanced systems which permit simultaneous production of orthophotos, contours, and digital terrain models; the economy of off-line orthophoto systems; applications of digital image processing; automation by optical techniques; applications of sensors other than photographic imagery, and the role of photogrammetric phases in a completely automated cartographic system. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Photogrammetria","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1016/0031-8663(76)90008-9","issn":"00318663","usgsCitation":"Thompson, M., and Mikhail, E., 1976, Automation in photogrammetry: Recent developments and applications (1972-1976): Photogrammetria, v. 32, no. 4, p. 111-145, https://doi.org/10.1016/0031-8663(76)90008-9.","startPage":"111","endPage":"145","numberOfPages":"35","costCenters":[],"links":[{"id":221091,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":269815,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-8663(76)90008-9"}],"volume":"32","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059eefbe4b0c8380cd4a0a6","contributors":{"authors":[{"text":"Thompson, M.M.","contributorId":78876,"corporation":false,"usgs":true,"family":"Thompson","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":360434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mikhail, E.M.","contributorId":74515,"corporation":false,"usgs":true,"family":"Mikhail","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":360433,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70009808,"text":"70009808 - 1976 - The dissolution of calcite in CO2-saturated solutions at 25°C and 1 atmosphere total pressure","interactions":[],"lastModifiedDate":"2018-03-21T15:10:39","indexId":"70009808","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"The dissolution of calcite in CO2-saturated solutions at 25°C and 1 atmosphere total pressure","docAbstract":"The dissolution of Iceland spar in CO2-saturated solutions at 25°C and 1 atm total pressure has been followed by measurement of pH as a function of time. Surface concentrations of reactant and product species have been calculated from bulk fluid data using mass transport theory and a model that accounts for homogeneous reactions in the bulk fluid. The surface concentrations are found to be close to bulk solution values. This indicates that calcite dissolution under the experimental conditions is controlled by the kinetics of surface reaction. The rate of calcite dissolution follows an empirical second order relation with respect to calcium and hydrogen ion from near the initial condition (pH 3.91) to approximately pH 5.9. Beyond pH 5.9 the rate of surface reaction is greatly reduced and higher reaction orders are observed. Calculations show that the rate of calcite dissolution in natural environments may be influenced by both transport and surface-reaction processes. In the absence of inhibition, relatively short times should be sufficient to establish equilibrium.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(76)90176-9","issn":"00167037","usgsCitation":"Plummer, N., and Wigley, T., 1976, The dissolution of calcite in CO2-saturated solutions at 25°C and 1 atmosphere total pressure: Geochimica et Cosmochimica Acta, v. 40, no. 2, p. 191-202, https://doi.org/10.1016/0016-7037(76)90176-9.","productDescription":"12 p.","startPage":"191","endPage":"202","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":218907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505baac7e4b08c986b3229e1","contributors":{"authors":[{"text":"Plummer, Niel 0000-0002-4020-1013 nplummer@usgs.gov","orcid":"https://orcid.org/0000-0002-4020-1013","contributorId":190100,"corporation":false,"usgs":true,"family":"Plummer","given":"Niel","email":"nplummer@usgs.gov","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":357196,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wigley, T.M.L.","contributorId":56788,"corporation":false,"usgs":true,"family":"Wigley","given":"T.M.L.","email":"","affiliations":[],"preferred":false,"id":357195,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011156,"text":"70011156 - 1976 - Qal’eh hasan ali maars, central Iran","interactions":[],"lastModifiedDate":"2023-08-31T15:27:51.8006","indexId":"70011156","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"Qal’eh hasan ali maars, central Iran","docAbstract":"A group of craters 120 km southeast of Kerman, the largest 1200 m across and 300 m deep, are typical maars, excavated depression with rims of bedded pyroclastic debris. Most of the crater rims are composed entirely of country rock clasts, but the largest crater yields tephrite, composed of phenocrysts of phlogopite, clinopyroxene, and olivine in a groundmass of anorthoclase, analcime, hauyne, clinopyroxene and magnetite, and a cumulate of phlogopite and clinopyroxene with highly potassic glass. The occurrence of hauyne as a ground mass mineral is a rare or unique feature. The maar field lies in the projection to the south of the Nayband fault and, with some flows near that fault, represents a province of Quaternary alkali basalt volcanism.
","language":"English","publisher":"Springer","doi":"10.1007/BF02597000","usgsCitation":"Milton, D., 1976, Qal’eh hasan ali maars, central Iran: Bulletin Volcanologique, v. 40, no. 3, p. 201-208, https://doi.org/10.1007/BF02597000.","productDescription":"8 p.","startPage":"201","endPage":"208","numberOfPages":"8","costCenters":[],"links":[{"id":220962,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Iran","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 57.5,\n 29.5\n ],\n [\n 57.5,\n 29.333\n ],\n [\n 57.666,\n 29.333\n ],\n [\n 57.666,\n 29.5\n ],\n [\n 57.5,\n 29.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"40","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a9072e4b0c8380cd7fd45","contributors":{"authors":[{"text":"Milton, D.J.","contributorId":44121,"corporation":false,"usgs":true,"family":"Milton","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":360418,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1003755,"text":"1003755 - 1976 - An outbreak of erysipelas in eared grebes (Podiceps nigricollis)","interactions":[],"lastModifiedDate":"2018-02-27T10:13:14","indexId":"1003755","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2507,"text":"Journal of Wildlife Diseases","active":true,"publicationSubtype":{"id":10}},"displayTitle":"An outbreak of erysipelas in eared grebes (Podiceps nigricollis)","title":"An outbreak of erysipelas in eared grebes (Podiceps nigricollis)","docAbstract":"An outbreak of erysipelas killed an estimated 5,000 aquatic birds on Great Salt Lake (Utah) in late November, 1975. Although several thousand ducks and gulls were using the lake, at least 99 percent of the victims were eared grebes. A hypothetical explanation for the selective mortality is offered.
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At the level of the clearest water, in the mid-depth regions, the turbidity distribution primarily reflects the pattern of productivity in the surface waters. This suggests that the ‘background’ turbidity level in the oceans is largely a function of biogenic fallout. The bottom waters of the western Atlantic generally exhibit large increases in turbidity. The most intense benthic nepheloid layers are in the southwestern Argentine basin and northern North American basin; the lowest bottom water turbidity in the western Atlantic is in the equatorial regions. Both the Argentine and North American basin bottom waters appear to derive their high turbidity largely from local resuspension of terrigenous input in these basins. In contrast to the west, the eastern Atlantic basins show very low turbidities with the exception of three regions: the Mediterranean outflow area, the Cape basin, and the West European basin.
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This uplift extends at least 150 kilometers west-northwestward along the San Andreas Fault from Cajon to Maricopa, southward from the San Andreas into the northern Transverse Ranges, and eastward from Lebec into and including much of western Mojave block. It seems to have grown spasmodically eastward from a center near the junction of the San Andreas and Garlock faults and has occurred largely within an area that has remained virtually aseismic since at least 1932. Although much of this area has been characterized by crustal mobility since at least the turn the century, the described uplift seems to be an unusually large and probably unique event superimposed the existing pattern of continuing deformation.
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1976 - A note on the effect of fault gouge thickness on fault stability","interactions":[],"lastModifiedDate":"2013-01-18T13:31:41","indexId":"70010253","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2071,"text":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","active":true,"publicationSubtype":{"id":10}},"title":"A note on the effect of fault gouge thickness on fault stability","docAbstract":"At low confining pressure, sliding on saw cuts in granite is stable but at high pressure it is unstable. The pressure at which the transition takes place increases if the thickness of the crushed material between the sliding surfaces is increased. This experimental result suggests that on natural faults the stability of sliding may be affected by the width of the fault zone. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0148-9062(76)90226-6","issn":"01489062","usgsCitation":"Byerlee, J., and Summers, R., 1976, A note on the effect of fault gouge thickness on fault stability: International Journal of Rock Mechanics and Mining Sciences & Geomechanics Abstracts, v. 13, no. 1, p. 35-36, https://doi.org/10.1016/0148-9062(76)90226-6.","productDescription":"p.35-36","startPage":"35","endPage":"36","numberOfPages":"2","costCenters":[],"links":[{"id":265952,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0148-9062(76)90226-6"},{"id":219675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"13","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e4c3e4b0c8380cd468ee","contributors":{"authors":[{"text":"Byerlee, J.","contributorId":105838,"corporation":false,"usgs":true,"family":"Byerlee","given":"J.","affiliations":[],"preferred":false,"id":358459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Summers, R.","contributorId":65483,"corporation":false,"usgs":true,"family":"Summers","given":"R.","email":"","affiliations":[],"preferred":false,"id":358458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70010265,"text":"70010265 - 1976 - Foraminiferal biostratigraphy of the shelf edge: a key to late Quaternary paleoenvironments","interactions":[],"lastModifiedDate":"2013-02-19T16:19:21","indexId":"70010265","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Foraminiferal biostratigraphy of the shelf edge: a key to late Quaternary paleoenvironments","docAbstract":"Foraminiferal assemblages in eight piston cores from West Flower Garden Bank at the edge of the Texas continental shelf contain a nearly complete record of late Quaternary paleoclimatic and geologic events. The faunas are divisible into three distinct successive biofacies on the basis of both planktonic and benthic foraminifers: the basal Inflata Facies accumulated in cool shallow waters during late Pleistocene glaciation; the middle Crassaformis Facies represents a deepening sea that had warming surface waters; the upper Cultrata Facies is characteristic of the Holocene outer-shelf environment. Sea level was at -73 m and -53 m at the end of deposition of the Inflata and Crassaformis Facies, respectively. The biostratigraphic events at West Flower Garden Bank can be accurately correlated with those recorded in the middle and inner shelf and in deep-sea cores. The sequence of late Quaternary sea level and paleotemperature changes in the northern Gulf of Mexico can thereby be reconstructed. Eventually, this knowledge can be integrated with similar data from the shelf edge in other parts of the world to help bridge the gap between the known Quaternary record of the deep sea and that of the continents. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Palaeogeography, Palaeoclimatology, Palaeoecology","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(76)90040-7","issn":"00310182","usgsCitation":"Poag, C.W., and Sidner, B., 1976, Foraminiferal biostratigraphy of the shelf edge: a key to late Quaternary paleoenvironments: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 19, no. 1, p. 17-37, https://doi.org/10.1016/0031-0182(76)90040-7.","startPage":"17","endPage":"37","numberOfPages":"21","costCenters":[],"links":[{"id":267788,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1016/0031-0182(76)90040-7"},{"id":218711,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"19","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a1309e4b0c8380cd544c2","contributors":{"authors":[{"text":"Poag, C. Wylie","contributorId":52714,"corporation":false,"usgs":true,"family":"Poag","given":"C.","email":"","middleInitial":"Wylie","affiliations":[],"preferred":false,"id":358478,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sidner, B.R.","contributorId":57590,"corporation":false,"usgs":true,"family":"Sidner","given":"B.R.","email":"","affiliations":[],"preferred":false,"id":358479,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011134,"text":"70011134 - 1976 - Alternate drop pulse polarography","interactions":[],"lastModifiedDate":"2023-03-16T16:59:39.477689","indexId":"70011134","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Alternate drop pulse polarography","docAbstract":"The new technique of alternate drop pulse polarography is presented. An experimental evaluation of alternate drop pulse polarography shows complete compensation of the capacitative background due to drop expansion. The capillary response phenomenon was studied in the absence of faradaic reaction and the capillary response current was found to depend on the pulse width to the -0.72 power. Increased signal-to-noise ratios were obtained using alternate drop pulse polarography at shorter drop times.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60366a002","usgsCitation":"Christie, J.H., Jackson, L.L., and Osteryoung, R.A., 1976, Alternate drop pulse polarography: Analytical Chemistry, v. 48, no. 2, p. 242-247, https://doi.org/10.1021/ac60366a002.","productDescription":"6 p.","startPage":"242","endPage":"247","numberOfPages":"6","costCenters":[],"links":[{"id":220745,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"48","issue":"2","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059e97ce4b0c8380cd482f9","contributors":{"authors":[{"text":"Christie, J. H.","contributorId":74402,"corporation":false,"usgs":true,"family":"Christie","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":360371,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackson, Larry L.","contributorId":18790,"corporation":false,"usgs":true,"family":"Jackson","given":"Larry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":360370,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Osteryoung, R. A.","contributorId":12185,"corporation":false,"usgs":true,"family":"Osteryoung","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360369,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70011133,"text":"70011133 - 1976 - Oroville earthquakes: Normal faulting in the Sierra Nevada foothills","interactions":[],"lastModifiedDate":"2026-01-21T16:20:22.256023","indexId":"70011133","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Oroville earthquakes: Normal faulting in the Sierra Nevada foothills","docAbstract":"Aftershocks of the Oroville, California, earthquake of 1 August 1975 define a 16- by 12-kilometer fault plane striking north-south and dipping 60 degrees to the west to a depth of 10 kilometers. Focal mechanisms from P-wave first motions indicate normal faulting with the western, Great Valley side downdropped relative to the Sierra Nevada block. The northward projection of the fault plane passes beneath Oroville Dam and crops out under the reservoir.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.192.4234.72","issn":"00368075","usgsCitation":"Bufe, C., Lester, F., Lahr, K., Lahr, J., Seekins, L.C., and Hanks, T.C., 1976, Oroville earthquakes: Normal faulting in the Sierra Nevada foothills: Science, v. 192, no. 4234, p. 72-74, https://doi.org/10.1126/science.192.4234.72.","productDescription":"3 p.","startPage":"72","endPage":"74","costCenters":[],"links":[{"id":220691,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Oroville","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -121.84478686570523,\n 39.729207337221794\n ],\n [\n -121.84478686570523,\n 39.206896214987836\n ],\n [\n -120.65753121366123,\n 39.206896214987836\n ],\n [\n -120.65753121366123,\n 39.729207337221794\n ],\n [\n -121.84478686570523,\n 39.729207337221794\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"192","issue":"4234","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7125e4b0c8380cd764ac","contributors":{"authors":[{"text":"Bufe, C. G.","contributorId":79443,"corporation":false,"usgs":true,"family":"Bufe","given":"C. G.","affiliations":[],"preferred":false,"id":360367,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lester, F.W.","contributorId":10767,"corporation":false,"usgs":true,"family":"Lester","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":360363,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lahr, K.M.","contributorId":72126,"corporation":false,"usgs":true,"family":"Lahr","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":360366,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lahr, J.C.","contributorId":34892,"corporation":false,"usgs":true,"family":"Lahr","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":360364,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Seekins, L. C.","contributorId":99561,"corporation":false,"usgs":true,"family":"Seekins","given":"L.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":360368,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Hanks, Thomas C.","contributorId":35763,"corporation":false,"usgs":true,"family":"Hanks","given":"Thomas","middleInitial":"C.","affiliations":[],"preferred":false,"id":360365,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":70011024,"text":"70011024 - 1976 - Observations of eruption clouds from Sakura-zima volcano, Kyushu, Japan from Skylab 4","interactions":[],"lastModifiedDate":"2012-03-12T17:19:05","indexId":"70011024","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2499,"text":"Journal of Volcanology and Geothermal Research","active":true,"publicationSubtype":{"id":10}},"title":"Observations of eruption clouds from Sakura-zima volcano, Kyushu, Japan from Skylab 4","docAbstract":"Hasselblad and Nikon stereographic photographs taken from Skylab between 9 June 1973 and 1 February 1974 give synoptic plan views of several entire eruption clouds emanating from Sakura-zima volcano in Kagoshima Bay, Kyushu, Japan. Analytical plots of these stereographic pairs, studied in combination with meteorological data, indicate that the eruption clouds did not penetrate the tropopause and thus did not create a stratospheric dust veil of long residence time. A horizontal eddy diffusivity of the order of 106 cm2 s-1 and a vertical eddy diffusivity of the order of 105 cm2 s-1 were calculated from the observed plume dimensions and from available meteorological data. These observations are the first, direct evidence that explosive eruption at an estimated energy level of about 1018 ergs per paroxysm may be too small under atmospheric conditions similar to those prevailing over Sakura-zima for volcanic effluents to penetrate low-level tropospheric temperature inversions and, consequently, the tropopause over northern middle latitudes. Maximum elevation of the volcanic clouds was determined to be 3.4 km. The cumulative thermal energy release in the rise of volcanic plumes for 385 observed explosive eruptions was estimated to be 1020 to 1021 ergs (1013 to 1014 J), but the entire thermal energy release associated with pyroclastic activity may be of the order of 2.5 ?? 1022 ergs (2.5 ?? 1015 J). Estimation of the kinetic energy component of explosive eruptions via satellite observation and meteorological consideration of eruption clouds is thus useful in volcanology as an alternative technique to confirm the kinetic energy estimates made by ground-based geological and geophysical methods, and to aid in construction of physical models of potential and historical tephra-fallout sectors with implications for volcano-hazard prediction. ?? 1976.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Volcanology and Geothermal Research","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"03770273","usgsCitation":"Friedman, J.D., Heiken, G., Randerson, D., and McKay, D., 1976, Observations of eruption clouds from Sakura-zima volcano, Kyushu, Japan from Skylab 4: Journal of Volcanology and Geothermal Research, v. 1, no. 4, p. 305-329.","startPage":"305","endPage":"329","numberOfPages":"25","costCenters":[],"links":[{"id":221790,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"1","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a6a91e4b0c8380cd74242","contributors":{"authors":[{"text":"Friedman, J. 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The sample is digested with HF—HCl—H2O2; the final solution for analysis is in 10 % (v/v) HCl. Copper and zinc are determined directly by aspirating the solution into an air—acetylene flame. A separate aliquot of the solution is used for determination of lead; lead is extracted into TOPO-MIBK from the acidic solution in the presence of iodide and ascorbic acid. For a 0.50-g sample, the limits of determination are 10–2000 p.p.m. for Cu and Zn, and 5–5000 p.p.m. for Pb. As much as 40 % Fe or Ca. and 10 % Al, Mg, or Mn in the sample do not interfere. The proposed method can be applied to the determination of copper, zinc, and lead in a wide range of geological materials including iron- and manganese-rich, calcareous and carbonate samples.
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","language":"English","publisher":"Ducks Unlimited","usgsCitation":"Friend, M., 1976, Combating waterfowl diseases: Ducks Unlimited, v. 40, no. 3, p. 44-46.","productDescription":"3 p.","startPage":"44","endPage":"46","costCenters":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"links":[{"id":129472,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"40","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae72a","contributors":{"authors":[{"text":"Friend, Milton 0000-0002-2882-3629","orcid":"https://orcid.org/0000-0002-2882-3629","contributorId":31332,"corporation":false,"usgs":true,"family":"Friend","given":"Milton","email":"","affiliations":[{"id":456,"text":"National Wildlife Health Center","active":true,"usgs":true}],"preferred":true,"id":314188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1000276,"text":"1000276 - 1976 - Allantoinase in the marine polychaete Eudistylia vancouveri","interactions":[],"lastModifiedDate":"2013-02-04T14:45:43","indexId":"1000276","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1606,"text":"Experientia","active":true,"publicationSubtype":{"id":10}},"title":"Allantoinase in the marine polychaete Eudistylia vancouveri","docAbstract":"Allantoinase, an enzyme in the purine-urea cycle, was found in Eudistylia vancouveri (Polychaeta). The enzyme had a pH optimum at 7.6. The Km was 0.012 M allantoin, and the Arrhenius energy of activation was 12.6 to 14.6 kcal/mol.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Experientia","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"Elsevier","publisherLocation":"Amsterdam, Netherlands","doi":"10.1007/BF01937383","collaboration":"Out-of-print","usgsCitation":"Passino, D., and Brown, G., 1976, Allantoinase in the marine polychaete Eudistylia vancouveri: Experientia, v. 32, no. 11, p. 1376-1377, https://doi.org/10.1007/BF01937383.","productDescription":"2 p.","startPage":"1376","endPage":"1377","numberOfPages":"2","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266957,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1007/BF01937383"}],"volume":"32","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687e14","contributors":{"authors":[{"text":"Passino, Dora R. M.","contributorId":29345,"corporation":false,"usgs":true,"family":"Passino","given":"Dora R. M.","affiliations":[],"preferred":false,"id":308324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, G.W. Jr.","contributorId":102827,"corporation":false,"usgs":true,"family":"Brown","given":"G.W.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":308325,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70190974,"text":"70190974 - 1976 - Salt-load computations - Colorado River, Cameo, Colorado, to Cisco, Utah","interactions":[],"lastModifiedDate":"2017-09-20T12:06:45","indexId":"70190974","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Salt-load computations - Colorado River, Cameo, Colorado, to Cisco, Utah","docAbstract":"No abstract available.
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Two volumes: Part 1, Data summary; Part 2, Basic data","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59c22cb5e4b091459a61b748","contributors":{"authors":[{"text":"Brennan, Robert","contributorId":105695,"corporation":false,"usgs":true,"family":"Brennan","given":"Robert","email":"","affiliations":[],"preferred":false,"id":710797,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grozier, Richard Ural","contributorId":75806,"corporation":false,"usgs":true,"family":"Grozier","given":"Richard","email":"","middleInitial":"Ural","affiliations":[],"preferred":false,"id":710798,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170233,"text":"70170233 - 1976 - The San Francisco cow; did she or didn’t she?","interactions":[],"lastModifiedDate":"2016-04-12T15:28:01","indexId":"70170233","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"The San Francisco cow; did she or didn’t she?","docAbstract":"No one has suggested that Mr. Shafter's nameless cow was the cause of the 1906 earthquake, but she has been the source of as persistent a rumor as Mrs. Murphy's Chicago cow. Since 1906, \"the cow that fell in the crack\" has been a favorite subject of humorous speculation. large earthquakes have always produced large exaggerations, and, although it is difficult to exaggerate the terror humans feel in an earthquake, many scientists have said that much of what witnesses said they witnessed they did not witness at all. Huge, gaping cracks that legend says open and close in the earth, swallowing whole cities, are among those earthquake features that just aren't featured in earthquakes. True, soil may \"snap open and shut,\" but most earth scientists do not think that the cracks are wide enough or deep enough to accommodate houses.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Hill, M., 1976, The San Francisco cow; did she or didn’t she?: Earthquake Information Bulletin (USGS), v. 8, no. 3, p. 19-23.","productDescription":"5 p.","startPage":"19","endPage":"23","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319995,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"570e1c37e4b0ef3b7ca24c49","contributors":{"authors":[{"text":"Hill, M.","contributorId":12635,"corporation":false,"usgs":true,"family":"Hill","given":"M.","affiliations":[],"preferred":false,"id":626561,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70190976,"text":"70190976 - 1976 - Water-resources investigations of the U.S. Geological Survey in selected coal-energy areas of Utah","interactions":[],"lastModifiedDate":"2017-09-19T15:32:20","indexId":"70190976","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Water-resources investigations of the U.S. Geological Survey in selected coal-energy areas of Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/70190976","collaboration":"Prepared in cooperation with the Utah Division of Water Rights and the U.S. Bureau of Land Management","usgsCitation":"Waddell, K.M., 1976, Water-resources investigations of the U.S. Geological Survey in selected coal-energy areas of Utah: Open-File Report, 21 p., https://doi.org/10.3133/70190976.","productDescription":"21 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345891,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59c22cb5e4b091459a61b740","contributors":{"authors":[{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":710800,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70188398,"text":"70188398 - 1976 - Radiocarbon dates from Alaska, Yukon Territory, and British Columbia","interactions":[],"lastModifiedDate":"2017-06-07T16:02:28","indexId":"70188398","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"Radiocarbon dates from Alaska, Yukon Territory, and British Columbia","docAbstract":"No abstract available.
","language":"English","publisher":"University of Alaska Institute of Marine Sciences","usgsCitation":"Wilson, F.H., and Young, M.S., 1976, Radiocarbon dates from Alaska, Yukon Territory, and British Columbia, iii, 64 p.","productDescription":"iii, 64 p.","costCenters":[{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"links":[{"id":342280,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Canada, United States","state":"Alaska, British Columbia, Yukon Territory","publicComments":"IMS Report R76-6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59391117e4b0764e6c5e8df6","contributors":{"authors":[{"text":"Wilson, Frederic H. 0000-0003-1761-6437 fwilson@usgs.gov","orcid":"https://orcid.org/0000-0003-1761-6437","contributorId":67174,"corporation":false,"usgs":true,"family":"Wilson","given":"Frederic","email":"fwilson@usgs.gov","middleInitial":"H.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true},{"id":114,"text":"Alaska Science Center","active":true,"usgs":true}],"preferred":true,"id":697554,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Young, M. Springer","contributorId":177178,"corporation":false,"usgs":false,"family":"Young","given":"M.","email":"","middleInitial":"Springer","affiliations":[],"preferred":false,"id":697555,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70170235,"text":"70170235 - 1976 - The sound of an earthquake","interactions":[],"lastModifiedDate":"2016-04-12T15:36:05","indexId":"70170235","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1435,"text":"Earthquake Information Bulletin (USGS)","active":true,"publicationSubtype":{"id":10}},"title":"The sound of an earthquake","docAbstract":"Historical accounts of earthquakes often include references to sounds which accompany earthquakes.
","language":"English","publisher":"U.S Geological Survey","usgsCitation":"Hill, D., 1976, The sound of an earthquake: Earthquake Information Bulletin (USGS), v. 8, no. 3, p. 15-18.","productDescription":"4 p.","startPage":"15","endPage":"18","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":319998,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"8","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"570e1c38e4b0ef3b7ca24c50","contributors":{"authors":[{"text":"Hill, D.P.","contributorId":27432,"corporation":false,"usgs":true,"family":"Hill","given":"D.P.","email":"","affiliations":[],"preferred":false,"id":626563,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}