No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha180","usgsCitation":"Hansen, A., 1967, Availability of ground water in the Cayce quadrangle, Jackson Purchase region, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 180, 1 Plate: 42.68 x 34.00 inches, https://doi.org/10.3133/ha180.","productDescription":"1 Plate: 42.68 x 34.00 inches","costCenters":[],"links":[{"id":190418,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89820,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/180/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413581,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15543.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Cayce quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -89.125,\n 36.5\n ],\n [\n -89.125,\n 36.625\n ],\n [\n -89,\n 36.625\n ],\n [\n -89,\n 36.5\n ],\n [\n -89.125,\n 36.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e375","contributors":{"authors":[{"text":"Hansen, Arnold J.","contributorId":33316,"corporation":false,"usgs":true,"family":"Hansen","given":"Arnold J.","affiliations":[],"preferred":false,"id":278067,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011610,"text":"70011610 - 1967 - Geomagnetic polarity epochs: Nunivak Island, Alaska","interactions":[],"lastModifiedDate":"2020-11-24T21:00:54.675165","indexId":"70011610","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1427,"text":"Earth and Planetary Science Letters","active":true,"publicationSubtype":{"id":10}},"title":"Geomagnetic polarity epochs: Nunivak Island, Alaska","docAbstract":"New paleomagnetic and potassium-argon dating measurements have been made of basalt flows from Nunivak Island, Alaska, with the following results. (1) The best estimate of the age of the Brunhes/Matuyama polarity epoch boundary is found to be 0.694 m.y. (2) The best estimate of the age of the Gauss/Gilbert boundary is 3.32 m.y. (3) Three normally magnetized flows with ages from 0.93 to 0.88 m.y. are in accord with previous estimates of the age and duration of the Jaramillo normal event. (4) One normally magnetized flow with an age of 1.65 ± 0.09 m.y. supplies additional evidence for the Gilsá normal event. (5) Two new normal events are identified within the Gilbert reversed epoch, the “Cochiti normal event” with an age of 3.7 m.y. and the “Nunivak normal event” with an age of 4.1 m.y.
In some microscopic inclusions (consisting of aqueous liquid and vapor) in minerals, freezing eliminates the vapor phase because of greater volume occupied by the resulting ice. When vapor fails to nucleate again on partial melting, the resulting negative pressure (hydrostatic tension) inside the inclusions permits the existence of ice I crystals under reversible, metastable equilibrium, at temperatures as high as +6.5°C and negative pressures possibly exceeding 1000 bars.
Large talus blocks litter the flat floor of Oceanographer Canyon at a depth of 1460 meters; they indicate down-axis mass transport of floor sediment at an unknown time and rate. From 1460 to 1310 meters the sidewall is covered by unconsolidated sediment lying at 35° to 40° from the horizontal. An outcrop of Pleistocene or younger sediment at 1460 meters is probably a remnant of a former fill.
No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings, South Dakota Academy of Science","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"South Dakota Academy of Science","usgsCitation":"Pettyjohn, W.A., and Randich, P.G., 1967, Hydrologic applications of lithofacies clastic-ratio maps, in Proceedings, South Dakota Academy of Science, p. 48-60.","productDescription":"13 p.","startPage":"48","endPage":"60","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":562,"text":"South Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":353065,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff5ed3e4b0da30c1bfddab","contributors":{"authors":[{"text":"Pettyjohn, Wayne A.","contributorId":20724,"corporation":false,"usgs":true,"family":"Pettyjohn","given":"Wayne","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":732353,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Randich, Phillip G.","contributorId":93071,"corporation":false,"usgs":true,"family":"Randich","given":"Phillip","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":732354,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011549,"text":"70011549 - 1967 - Theory of friction based on brittle fracture","interactions":[],"lastModifiedDate":"2020-11-24T21:35:31.108544","indexId":"70011549","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2171,"text":"Journal of Applied Physics","active":true,"publicationSubtype":{"id":10}},"title":"Theory of friction based on brittle fracture","docAbstract":"Now that the dust has settled it is possible to assess the long term effects of the Alaskan earthquake on March 27, both on the activities of man and on the wild life of the State.
The significant known hydrated borate mineral assemblages (principally of the western United States) in the system Na2O-CaO-MgO-B2O3-H2O are expressible in three ternary composition diagrams. Phase rule interpretation of the diagrams is consistent with observation, if the activity of H2O is generally considered to be determined by the geologic environment. The absence of conflicting tie-lines on a diagram indicates that the several mineral assemblages of the diagram were formed under relatively narrow ranges of temperature and pressure.
The known structural as well as empirical formulas for the minerals are listed, and the more recent (since 1960) crystal structure findings are discussed briefly.
Schematic Gibbs free energy-composition diagrams based on known solubility-temperature relations in the systems Na2B4O7-H2O and Na2B4O7-NaCl-H2O, are highly useful in the interpretation and prediction of the stability relations in these systems; in particular these diagrams indicate clearly that tincalconite, although geologically important, is everywhere a metastable phase. Crystal-chemical considerations indicate that the same thermodynamic and kinetic behavior observed in the Na2B4O7-H2O system will hold in the Ca2B6O11-H2O system. This conclusion is confirmed by the petrologic evidence.
The chemical relations among the mineral assemblages of a ternary diagram are expressed by a schematic “activity-activity” diagram. These activity-activity diagrams permit the tracing-out of the paragenetic sequences as a function of changing cation and H2O activities.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(67)90045-2","issn":"00167037","usgsCitation":"Christ, C., Truesdell, A., and Erd, R.C., 1967, Borate mineral assemblages in the system Na2O-CaO-MgO-B2O3-H2O: Geochimica et Cosmochimica Acta, v. 31, no. 3, p. 313-337, https://doi.org/10.1016/0016-7037(67)90045-2.","productDescription":"25 p.","startPage":"313","endPage":"337","numberOfPages":"25","costCenters":[],"links":[{"id":219664,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f210e4b0c8380cd4afb6","contributors":{"authors":[{"text":"Christ, C. L.","contributorId":53906,"corporation":false,"usgs":true,"family":"Christ","given":"C. L.","affiliations":[],"preferred":false,"id":357746,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address: TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":357745,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erd, Richard C.","contributorId":89899,"corporation":false,"usgs":true,"family":"Erd","given":"Richard","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":357747,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010040,"text":"70010040 - 1967 - Fractionation of rare-earth elements in allanite and monazite as related to geology of the Mt. Wheeler mine area, Nevada","interactions":[],"lastModifiedDate":"2024-03-07T16:17:24.475759","indexId":"70010040","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"Fractionation of rare-earth elements in allanite and monazite as related to geology of the Mt. Wheeler mine area, Nevada","docAbstract":"Rare-earth contents of 20 allanites and 13 monazites, accessory minerals from a restricted outcrop area of intrusive granitic rocks, are reported. A quantity called sigma (Σ), which is the sum of the atomic percentages of La, Ce and Pr, is used as an index of composition with respect to the rare-earth elements. Values of sigma vary from 61.3 to 80.9 at.% for these allanites and monazites, representing an appreciable range of composition in terms of the rare-earth elements.
Degree of fractionation of rare earths varies directly with CaO content of the granitic rocks, which in turn depends largely on proximity of limestone. Four xenoliths included in the study suggest that spotty mosaic equilibria are superimposed on the regional gradients and that locally the degree of fractionation of rare earths responds to whole rock composition over distances of a few yards or less.
The chemistry of the granitic rocks under study appears to be similar in some respects to that of alkalio rocks and carbonatites. Allanites from the most calcium-rich rocks show a pronounced concentration of the most basic rare earths, and whole-rock concentrations of such rare constituents as total cerium earths, Zr, F, Ti, Ba and Sr increase sympathetically with whole-rock calcium.
The explanation for the concentration gradients observed in this chemical system must involve assimilation more than magmatic differentiation.
The eucrite and howardite calcium-rich achondrites and many mesosiderites are considered as a coherent meteorite assemblage, their silicates consisting essentially of calciumpoor monoclinic and orthorhombic pyroxenes and calcium-rich plagioclase feldspar. The achondrites can be grouped according to their brecciated structure as follows: eucrites—unbrecciated and monomict brecciated achondrites; howardites—polymict brecciated achondrites. Many mesosiderites contain brecciated structures; they are distinguished from the achondrites by their large metallic fraction. The structure and composition of rock fragments in the breccias indicate a complicated sequence of events including magmatic differentiation, brecciation, recrystallization and refragmentation, and ejection from the parent body. Detailed mineralogical and chemical data suggest that the magmatic differentiation proceeded primarily by the separation of pyroxene from an ultrabasic parent material that had a much lower alkali content than ordinary chondrites. Magmatic crystallization took place in environments ranging from extrusive to deep-seated intrusive. Polymict breccias contain fragments with a wide variety of magmatic and recrystallization textures, which suggests that the breccias were formed either in very large or repeated fragmentation events. Monomict breccias contain fragments with a small range of similar magmatic textures, which suggests that these breccias were formed by small or single events. Petrographic evidence suggests that many of the breccias are impact breccias. Either in their original magmatic crystallization sites or in the sites of breccia accumulation, most of these meteorites apparently had a near-surface location prior to ejection from the parent body.
Evidence obtained from eucrites, howardites and mesosiderites forms an important part of our understanding of the early evolution of the surface regions of their parent body. Chemical and oxidation conditions were different from those presently found in the Earth's crust and upper mantle, but the necessary conditions may have been present in the early history of the Earth. A lunar origin for eucrites, howardites and mesosiderites is proposed, but an asteroidal origin can not be presently excluded.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(67)90112-3","issn":"00167037","usgsCitation":"Duke, M., and Silver, L.T., 1967, Petrology of eucrites, howardites and mesosiderites: Geochimica et Cosmochimica Acta, v. 31, no. 10, p. 1637-1665, https://doi.org/10.1016/0016-7037(67)90112-3.","productDescription":"29 p.","startPage":"1637","endPage":"1665","costCenters":[],"links":[{"id":218650,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7830e4b0c8380cd78668","contributors":{"authors":[{"text":"Duke, M.B.","contributorId":106630,"corporation":false,"usgs":true,"family":"Duke","given":"M.B.","email":"","affiliations":[],"preferred":false,"id":359144,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Silver, L. T.","contributorId":46968,"corporation":false,"usgs":true,"family":"Silver","given":"L.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":359143,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011499,"text":"70011499 - 1967 - The fractionation of nickel between olivine and augite as a geothermometer","interactions":[],"lastModifiedDate":"2020-11-24T22:05:58.863265","indexId":"70011499","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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 fractionation of nickel between olivine and augite as a geothermometer","docAbstract":"The coexisting olivine, clinopyroxene and glass of five samples collected from the Makaopuhi lava lake in Hawaii, at temperatures ranging from 1050 to 1160°C were analysed for nickel with an electron probe microanalyser. The results strongly suggest that the distribution of nickel between these three phase pairs well obeys the thermodynamic partition law, and that under favourable conditions, the distribution coefficients permit the estimation of the crystallisation temperature within an accuracy of 10–20°C.
It is concluded that the application of the Makaopuhi data to plutonic and to other volcanic rocks should be carried out with caution because the effect of pressure and the changing composition of the phases upon the numerical values of the distribution coefficients is not known quantitatively.
","language":"English","publisher":"Elsevier","doi":"10.1016/S0016-7037(67)80036-X","issn":"00167037","usgsCitation":"Hakli, T., and Wright, T.L., 1967, The fractionation of nickel between olivine and augite as a geothermometer: Geochimica et Cosmochimica Acta, v. 31, no. 5, p. 877-884, https://doi.org/10.1016/S0016-7037(67)80036-X.","productDescription":"8 p.","startPage":"877","endPage":"884","numberOfPages":"8","costCenters":[],"links":[{"id":221176,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bac28e4b08c986b3232e6","contributors":{"authors":[{"text":"Hakli, T.A.","contributorId":87689,"corporation":false,"usgs":true,"family":"Hakli","given":"T.A.","email":"","affiliations":[],"preferred":false,"id":361268,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wright, T. L.","contributorId":11188,"corporation":false,"usgs":true,"family":"Wright","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":361267,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011500,"text":"70011500 - 1967 - Water resources: A global problem with local roots","interactions":[],"lastModifiedDate":"2023-10-20T14:50:04.321968","indexId":"70011500","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1565,"text":"Environmental Science & Technology","onlineIssn":"1520-5851","printIssn":"0013-936X","active":true,"publicationSubtype":{"id":10}},"title":"Water resources: A global problem with local roots","docAbstract":"No abstract available.
","language":"English","publisher":"American Chemical Society","doi":"10.1021/es60007a609","issn":"0013936X","usgsCitation":"Nace, R.L., 1967, Water resources: A global problem with local roots: Environmental Science & Technology, v. 1, no. 7, p. 550-551, https://doi.org/10.1021/es60007a609.","productDescription":"2 p.","startPage":"550","endPage":"551","costCenters":[],"links":[{"id":221177,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Earth","volume":"1","issue":"7","noUsgsAuthors":false,"publicationDate":"2004-08-12","publicationStatus":"PW","scienceBaseUri":"505bcc6ee4b08c986b32db35","contributors":{"authors":[{"text":"Nace, R. L.","contributorId":11332,"corporation":false,"usgs":true,"family":"Nace","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":361269,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1013734,"text":"1013734 - 1967 - An unusual case of fish disease caused by Ophyroglena sp","interactions":[],"lastModifiedDate":"2023-11-08T23:00:30.707835","indexId":"1013734","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1140,"text":"Bulletin of the Wildlife Disease Association","active":true,"publicationSubtype":{"id":10}},"title":"An unusual case of fish disease caused by Ophyroglena sp","docAbstract":"No abstract available.
","language":"English","publisher":"Wildlife Disease Association","doi":"10.7589/0090-3558-3.3.111","usgsCitation":"Hoffman, G.L., 1967, An unusual case of fish disease caused by Ophyroglena sp: Bulletin of the Wildlife Disease Association, v. 3, no. 3, p. 111-112, https://doi.org/10.7589/0090-3558-3.3.111.","productDescription":"2 p.","startPage":"111","endPage":"112","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":130036,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68410b","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":319161,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010546,"text":"70010546 - 1967 - Comparison of Macedon and Darwin glass","interactions":[],"lastModifiedDate":"2024-03-07T16:28:00.801608","indexId":"70010546","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","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":"Comparison of Macedon and Darwin glass","docAbstract":"Chemical analyses are presented for major and minor elements in two specimens of natural glass reported from Macedon, Victoria, and are compared with new analyses of glass from Mt. Darwin, Tasmania. One specimen of Macedon glass is dark, the other light; both are spongy with relatively large cavities of size uncommon in Darwin glass. Some of the new analyses of Darwin glass extend considerably the compositional range previously reported for Mg, Ni and Co. The chemical composition of Macedon glass cannot be distinguished from that of Darwin glass for any of twenty-five elements investigated. It appears possible that the two specimens of glass reported from Macedon may represent either two mislabelled pieces of Darwin glass, or else a separate natural occurrence of Darwin glass 560 km north of Mt. Darwin.
","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(67)90108-1","issn":"00167037","usgsCitation":"Chapman, D., Keil, K., and Annell, C., 1967, Comparison of Macedon and Darwin glass: Geochimica et Cosmochimica Acta, v. 31, no. 10, p. 1595-1603, https://doi.org/10.1016/0016-7037(67)90108-1.","productDescription":"9 p.","startPage":"1595","endPage":"1603","costCenters":[],"links":[{"id":218652,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"31","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f843e4b0c8380cd4cfa3","contributors":{"authors":[{"text":"Chapman, D.R.","contributorId":93621,"corporation":false,"usgs":true,"family":"Chapman","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":359148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Keil, Klaus","contributorId":55955,"corporation":false,"usgs":true,"family":"Keil","given":"Klaus","email":"","affiliations":[],"preferred":false,"id":359146,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Annell, C.","contributorId":61150,"corporation":false,"usgs":true,"family":"Annell","given":"C.","affiliations":[],"preferred":false,"id":359147,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70046372,"text":"70046372 - 1967 - Serial publications commonly cited in technical bibliographies of the United States Geological Survey","interactions":[],"lastModifiedDate":"2013-07-08T12:49:35","indexId":"70046372","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Serial publications commonly cited in technical bibliographies of the United States Geological Survey","docAbstract":"This compilation is a listing of the serial publications cited in the following publications of the United States Geological Survey: Geophysical Abstracts, Abstracts of North American Geology, Bibliography of North American Geology, and Bibliography of Hydrology of the United States. A supplement of publications added since the main list was compiled begins on page 83. New journals cited in Geophysical . Abstracts are listed in each monthly issue. Serial publications cited in each annual bibliography are listed in that volume.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70046372","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Serial publications commonly cited in technical bibliographies of the United States Geological Survey (1967 edition), 93 p., https://doi.org/10.3133/70046372.","productDescription":"93 p.","numberOfPages":"96","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":274617,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70046372/report.pdf"},{"id":273561,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70046372/report-thumb.jpg"}],"edition":"1967 edition","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b6f56ce4b0097a7158e5f2","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535544,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70046378,"text":"70046378 - 1967 - The Amazon, measuring a mighty river","interactions":[],"lastModifiedDate":"2013-07-08T12:46:58","indexId":"70046378","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"The Amazon, measuring a mighty river","docAbstract":"The Amazon, the world's largest river, discharges enough water into the sea each day to provide fresh water to the City of New York for over 9 years. Its flow accounts for about 15 percent of all the fresh water discharged into the oceans by all the rivers of the world. By comparison, the Amazon's flow is over 4 times that of the Congo River, the world's second largest river. And it is 10 times that of the Mississippi, the largest river on the North American Continent.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, DC","doi":"10.3133/70046378","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, The Amazon, measuring a mighty river, 16 p., https://doi.org/10.3133/70046378.","productDescription":"16 p.","numberOfPages":"16","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":273572,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70046378/report-thumb.jpg"},{"id":274613,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70046378/report.pdf"}],"country":"Brazil","otherGeospatial":"Amazon River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -60.89,-4.55 ], [ -60.89,0.71 ], [ -49.99,0.71 ], [ -49.99,-4.55 ], [ -60.89,-4.55 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b6f56de4b0097a7158e5ff","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535548,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":34623,"text":"b1163D - 1967 - Geology of the Taunton quadrangle, Bristol and Plymouth Counties, Massachusetts","interactions":[],"lastModifiedDate":"2023-03-23T22:08:57.607713","indexId":"b1163D","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1163","chapter":"D","title":"Geology of the Taunton quadrangle, Bristol and Plymouth Counties, Massachusetts","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1163D","usgsCitation":"Hartshorn, J.H., 1967, Geology of the Taunton quadrangle, Bristol and Plymouth Counties, Massachusetts: U.S. Geological Survey Bulletin 1163, Report: 67 p.; 1 Plate: 25.95 x 26.85 inches, https://doi.org/10.3133/b1163D.","productDescription":"Report: 67 p.; 1 Plate: 25.95 x 26.85 inches","costCenters":[],"links":[{"id":167559,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1163d/report-thumb.jpg"},{"id":96531,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1163d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":96530,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1163d/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109448,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20926.htm","linkFileType":{"id":5,"text":"html"},"description":"20926"}],"country":"United States","state":"Massachusetts","county":"Bristol County, Plymouth County","otherGeospatial":"Taunton quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -71.125,\n 42\n ],\n [\n -71.125,\n 41.875\n ],\n [\n -71,\n 41.875\n ],\n [\n -71,\n 42\n ],\n [\n -71.125,\n 42\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acbe4b07f02db67e3a8","contributors":{"authors":[{"text":"Hartshorn, Joseph H.","contributorId":89862,"corporation":false,"usgs":true,"family":"Hartshorn","given":"Joseph","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":213283,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011609,"text":"70011609 - 1967 - Altithermal timberline advance in Western United States","interactions":[],"lastModifiedDate":"2020-11-24T21:06:15.306226","indexId":"70011609","displayToPublicDate":"1967-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2840,"text":"Nature","active":true,"publicationSubtype":{"id":10}},"title":"Altithermal timberline advance in Western United States","docAbstract":"A combination of radiocarbon dating and counting of annual rings of the remains of trees has been used to establish the time of retreat of forests from sub-alpine mountains in California and Nevada. The information obtained can serve as a palaeoclimatic indicator.