Hostname: page-component-cd9895bd7-7cvxr Total loading time: 0 Render date: 2024-12-26T06:10:14.941Z Has data issue: false hasContentIssue false
  • English
  • Français

Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

Rights & Permissions [Opens in a new window]

Abstract

An abstract is not available for this content. As you have access to this content, full HTML content is provided on this page. A PDF of this content is also available in through the ‘Save PDF’ action button.
Type
Other
Information
Journal of Glaciology , Volume 7 , Issue 49 , 1968 , pp. 135 - 145
Copyright
Copyright © International Glaciological Society 1968

This is a selected list of glaciological literature ou the scientific study of snow and ice and of their effects on the earth; for the literature on polar expeditions, and also on the “applied” aspects of glaciology. such as snow ploughs, readers should consult the bibliographies in each issue of the Polar Record. For Russian material the system of transliteration used is that agreed by the U.S. Board on Geographic Names and the Permanent Committee on Geographical Names for British Official Use in 1947. Readers can greatly assist by sending reprints of their publications to the Society, or by informing Dr J. W. Glen of publications of glaciological interest. It should be noted that the Society does not necessarily hold copies of the items in this list, and also that the Society does not possess facilities for microfilming or photocopying.

References

General Glaciology

Bull, C. [B. B.] Antarctic glaciology. Geotimes, Vol. 11, No. 4, 1966, p. 22–23. [Review of progress since beginning of I.G.Y.]Google Scholar
[Conferences.] Proceedings of the, first international symposium on water desalination. Washington, D.C. October 3–9, 1965. Washington, D.C., U.S. Department of the Interior. Office of Saline Water, [c 1967]. 3 vols.: 632 p., 830 p., 792 p. $3.25. [Full text of papers with summaries in French, Russian and Spanish. Includes the following papers: C. Jaccard. “Electrical properties of ice”, Vol. 1, p. 224–39; V. A. Klyachko, “Research in the field of water desalination”, Vol. 1, p. 331–38; A. J. Barduhn, “The freezing process for water conversion in the United States”, Vol. 2, p. 641–58; G. Bozza, G. Dassù [and] G. Giambclli, “On the freezing process”, Vol. 2, p. 751–67; A. Peled, “Operation of the freeze desalination plant at Eilat, Israel”, Vol. 3. p. 1–10; J. W. Pike, “The direct contact controlled crystal desalination process”, Vol. 3, p. 173–88; D. J. Sandell, Jr., and C. A. Johnson, “Direct freeze-wash separation process”, Vol. 3, p. 625–50.1Google Scholar
[Glaciology Arctic.] Glaciology in the Arctic, [by] Glaciology Panel, Committee on Polar Research, . Transactions. American Geophysical Union, Vol. 48, No. 2, 1967, p. 759–67. [Includes reports on sea ice (volume. condition and dynamics), glaciers, seasonal snow cover, frozen ground and Quaternary chronology.]CrossRefGoogle Scholar
Jaworowski, Z. Temporal and geographical distribution of radium D (lead-210). Nature, Vol. 212, No. 5065, 1966, p. 886–89. [Concentration in snow and ice fluctuates and is greater in Arctic than temperate regions.]CrossRefGoogle ScholarPubMed
McLeod, I. R. Glaciological observations in Enderby, Kemp, and Mac.Robertson [sic] Lands, Antarctica. ANARE Interim Reports. Series A (IV). Glaciology. Publication No. 90, 1967, 48p. [Snow and ice features, and topography of the ice sheet in 1958, 1959 and 1961 are described, also sea ice formation in 1958 and 1959.]Google Scholar
Meier, M. F. Why study glaciers? In the context of water resources. Transactions. American Geophysical Union, Vol. 48, No. 2, 1967, p. 798–802. [Major problems in an understanding of the hydrology of snow and ice.]Google Scholar
O’Leary, B. T. The presence of ice in the Venus atmosphere as inferred from a halo effect. Astrophysical Journal, Vol. 146, No. 3, 1966, p. 754–66. [Evidence for existence of ice crystals at top of clouds in Venus atmosphere.]CrossRefGoogle Scholar
O’Leary, B. T. Rea, D. G. Mars: influence of topography on formation of temporary bright patches. Science, Vol. 155, No. 3760, 1967, p. 317–19. [Bright patches may be CO2 in depressions rather than ice on mountains.]CrossRefGoogle ScholarPubMed
Oulianoff, N. De quelques termes employés dans la littérature glaciologique. Actes de la Société Helvétique des Sciences Naturelles, 1966, p. 137–39.Google Scholar
Ragle, R. H. Icefield Ranges Research Project, St. Elias Mountains, Yukon, 1966. Arctic, Vol. 20, No. 1, 1967, p. 49–53. [Study of Kaskawulsh Glacier medial moraine; morphological analysis of streams on a glacier; rock glacier studies; cation content of snow and ice in the area of the divide station; snow and ice sampling for analysis of 120Pb; and Steele Glacier observations.]CrossRefGoogle Scholar
Sekyra, J. Glacial geology and cryogeology of the Dronning Maud Land-East Antarctica (the Schirmacher Oasis-the Wohlthat Massif). Casopis pro Mineralogii a Geologii (Prague), [Vol.] 11, No. 2, 1966, F. 209–16.Google Scholar
Tolstikov, Ye. I., ed. Atlas Antarkliki . Moscow. Leningrad, Glavnoye Upravleniye Geodezii i Kartografii, 1966. xxiii, 225 p., maps. 60 cm. [Distribution of natural phenomena over whole area, and by regions.]Google Scholar
Vendrov, S. L., and others. Grigoriy Aleksandrovich Avsyuk (k 60-lctno so dnya rozhdeniya) , [by] S. L. Vendrov [and 13 others]. Izvestiya Akademii Nauk SSSR. Seriya Geograficheskaya , 1967, No. 2, p. 152–53. [Tribute and biography.]Google Scholar
Wilhelm, F. Hydrologie, Claziologie. Braunschweig, Georg Westermann Verlag, [c 1966]. 144 p. (Das Geographische Seminar.) [Includes sections on underground water, springs, rivers and seas, chemical properties of water, and glaciers (description, behaviour, and properties).]Google Scholar

Glaciological Instruments and Methods

Bauer, A. Utilisation de la photographie aérienne en glaciologie. (In Chevallier, R., ed. Phodographie aérienne. panorama intertechnique. Paris, Gauthier-Villars, 1965, p. 65–68.) [Review of use of aerial photographs in glaciology.]Google Scholar
Beaumont, R. T. Mt. Hood pressure pillow snow gage. Proceedings of the Western Snow Conference, 33rd annual meeting, 1965, p. 29–35. [Description of device for measuring water equivalent.]Google Scholar
Bertle, F. A. Snow compaction method for the analysis of runoff from rain on snow. Proceedings of the Western Snow Conference, 33rd annual meeting, 1965, p. 11–18. [Method of computation described.]Google Scholar
Bogorodskiy, V. V. Fedorov, B. A. Radiolokatsiya lednikov . Zhurnal Tekhnicheskoy Fiziki , Torn 37, Vyp. 4, 1967, p. 781–88. [Use during Soviet Antarctic Expedition near Mirny. English translation in Soviet Physics-Technical Physics, Vol. 12, No. 4. 1967, p. 561–66.]Google Scholar
Bonneval, M. Mesure de la direction et de la vitesse d’écoulement d’un glacier par photogrammetrie. (In Chevallier, R., ed. Photographie aérienne, panorama intertechnique. Paris, Gauthier-Villars, 1965, p. 69–72.) [Description of method of determining glacier velocity by aerial photogrammetry.]Google Scholar
Bugayev, Yu. G. Opyt rabot s radiodal’nomerami v Antarktide . Geodeziya i Kartografiya , No. 4, 1966, p. 10–14. [Use of this instrument under extreme conditions without loss of accuracy.]Google Scholar
Clough, J. W. Bentley, C. R. Electromagnetic sounding of glacial and shelf ice. Antarctic journal of the U.S., Vol. 2, No. 4, 1967, p. 119–20. [Soundings of ice thickness in five areas in Antarctica during the 1966–67 field season. Two complete systems were used.]Google Scholar
Crozaz, G., and others. Artificial radioactivity reference horizons in Greenland firn, by G. Crozaz, C. C. Langway. Jr., and E. Picciotto. Earth and Planetary Science Letters, Vol. 1, No. 1, 1966, p. 42–48. [Object was to investigate total a-activity in firn layers and to determine whether artificial nuclide variations exist which could be used to measure snow accumulation rates.]CrossRefGoogle Scholar
Dansgaard, W., and others. The Si32 fallout in Scandinavia: a new method for ice dating, by W. Dansgaard, H. B. Clausen and A. Aarkrog. Tellus, Vol. 18, Nos. 2–3, 1966, p. 187–91. [Measurements on snow and old glacier ice in Jotunheimen, Norway, in 1962 show 32Si as usable element for dating ice up to 2 000–3 000 years old.]CrossRefGoogle Scholar
Grant, L. O., and others. Application of radar to snow surveying, by L. O. Grant, J. D. Marwitz and C. W. Thompson. Proceedings of the Western Snow Conference, 33rd annual meeting, 1965, p. 42–48. [Discussion of methods of using radar to study falling snow.]Google Scholar
Jaccard, C. Four-point method for measuring the volume and surface conductivities of a thin sample.,Zeitschrifl für angewandte Mathcrnalik and Physik, Vol. 17, Fase. 6, 1966, p. 657–63. [Details of method suitable for application to ice.]CrossRefGoogle Scholar
Lambert, G., and others. Possibilities of using lead 210 as an atmospheric tracer, by G. Lambert, B. Ardouin, M. Nezami and G. Polian. Tellus, Vol. 18, Nos. 2–3, 1966, p. 421–26. [Use to date seasonal layers in snow.]CrossRefGoogle Scholar
Lorius, C., and others. Sur une méthode gravimétrique simplifiée de détermination de l’épaisseur de glace en bordure de l’Antarctique. [par] C. Lorius, G. Rouillon et F. Helly. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 264, No. 3, 1967, p. 266–69. [Description of simple gravimetric method for determining ice thickness at edge of ice sheet and comparison of depths so found with depths found by drilling at Cap André Prudhomme, Terre Adélie.]Google Scholar
Meier, M. F., and others. Multispectral sensing tests at South Cascade Glacier, Washington, by M. F. Meier, R. H. Alexander and W. J. Campbell. Proceedings of the fourth symposium on remote sensing of environment… 1966… University of Michigan (Ann Arbor, Willow Run Laboratories, Institute of Science and Technology, University of Michigan), 1966, p. 145–59. [Correlative meteorological and photometric measurements were made on the ground; detailed glaciological information was available from past studies.]Google Scholar
Penton, V. E. Robertson, A. C. Experience with the pressure pillow as a snow measuring device. Water Resources Research, Vol. 3, No. 2, 1967, p. 405–08. [Useful for seasonal measurements; unreliable for short time-period variations.]CrossRefGoogle Scholar
Pettengill, D. Ice auger. U.S. Geological Survey. Water Supply Paper No. 1822, 1966, p. 53–54. [Description of powered auger suitable for drilling holes through river ice up to 0.5 m thick.]Google Scholar
Rinker, J. N., and others. Radio ice-sounding techniques, by J. N. Rinker, S. Evans and G. de Q. Robin. Proceedings of the fourth symposium on remote sensing of environment… 1966… University of Michigan (Ann Arbor. Willow Run Iaboratories, Institute of Science and Technology, University of Michigan), 1966, p. 793–800. [Evaluation of two VHF-band radar systems for measuring ice thickness and contouring bedrock profile of ice-rock interface, Greenland ice sheet, 1964.]Google Scholar
Shannon, W. G. Electronic methods of snow surveying. Soil Conservation, Vol. 23, No. 5, 1966, p. 107–09. [Continuous recording of snowfall, air temperature and water equivalent.]Google Scholar

Physics of Ice

Adamson, A. W. Surface of very cold ice is nonpolar. Chemical and Engineering News, Vol. 44, No. 18, 1966, p. 50. [Adsorption of Na at 78°K implies ice is non-polar at surface.]Google Scholar
Al-Naimy, B. S., and others. An electron spin resonance study of the radiolysis and the photolysis of frozen ammonia-water systems, by B. S. Al-Naimy, P. N. Moorthy and J. J. Weiss. Journal of Physical Chemistry, Vol. 70, No. 11, 1966, p. 3654–60. [Identification of NH2 radical as formed by γ-irradiation. Study of its production.]CrossRefGoogle Scholar
Arias, D., and others. Electrical properties of ice doped with NH3, [by] D. Arias, L. Levi and L. Lubart. Transactions of the Faraday Society, Vol. 62, No. 523, 1966, p. 1955–62. [Dielectric constant and conductivity as function of temperature and NH3 concentration.]CrossRefGoogle Scholar
Barnaal, D. E. Lowe, I. J. Experimental free-induction-decay shapes and theoretical second moments for hydrogen in hexagonal ice. Journal of Chemical Physics, Vol. 46, No. 12, 1967, p. 4800–09. [Good agreement with model of nuclear magnetic resonance line shape which assumes that high-frequency proton tunnelling does not take place along the hydrogen bonds.]CrossRefGoogle Scholar
Berendsen, H. J. C. Water structure in biological systems. Federation Proceedings. Federation of American Societies for Experimental Biology, Vol. 25, No. 3, Pt. 1, 1966, p. 971–76. [Discussion of structure of H2O in biomolecular systems. Includes suggestion about ice nucleating ability of many steroid hormones.]Google ScholarPubMed
Blinc, R. Hadži, D. Deuteron quadrupole coupling and hydrogen bonding in crystals. Nature, Vol. 212, No. 5068, 1966, p. 1307–09. [Use of deuteron magnetic resonance to study hydrogen bonds in, among other things. ice.]CrossRefGoogle Scholar
Bogorodskiy, V. V. Khokhlov, G. P. Akusticheskiyc kharakteristiki l’da, nakhodyashchegosya pod staticheskim davleniyem . Akusticheskiy.Zhurnal , Tom 13, Vyp. 1, 1967, p. 18–22. [Velocity of sound in columnar polycrystalline ice up to 500 bar. Main effect attributed to recrystallization of ice. English translation in Soviet Physics—Acoustics, Vol. 13, No. 1, 1967, p. 14–17.]Google Scholar
Brill, R. Tippe, A. Gitterparameter von Eis I bei tiefen Temperaturen. Acta Crystallographiea, Vol. 23, No. 3, 1967, p. 343–45. [Accurate determination of lattice parameters of hexagonal ice, 15°-200°K. English summary.]CrossRefGoogle Scholar
Campbell, E. S., and others. Interpretation of the energy of hydrogen bonding; permanent multiple contribution to the energy of ice as a function of the arrangement of hydrogens, [by] E. S. Campbell, G. Gelertner, H. Heinen and V. R. G. Moorti. Journal of Chemical Physics, Vol. 46, No. 7, 1967, p. 2690–707, [Review of present knowledge of hydrogen bond and of hydrogen positions in ice and calculation of energy variation for different hydrogen arrangements.]CrossRefGoogle Scholar
De Micheli, S. M. de Licenblat, A. R. Ice whiskers grown in subsaturated atmospheres. Journal of the Atmospheric Sciences, Vol. 24, No. 3, 1967, p. 312–15. [Appearance of whiskers during evaporation of ice crystals.]2.0.CO;2>CrossRefGoogle Scholar
Grant, N. H. The biological role of ice. Discovery, Vol. 27, No. 8, 1966, p. 26–30. [Implications of discovery that some biochemical reactions are faster in ice.]Google Scholar
Grant, N. H. Alburn, H. E. Acceleration of enzyme reactions in ice. Nature, Vol. 212, No. 5058, 1966, p. 194. [Reactions faster in ice at −23°C than in water at +1°C.]CrossRefGoogle ScholarPubMed
Gunter, T. E. Electron paramagnetic resonance studies of the radiolysis of H2O in the solid state. Journal of Chemical Physics, Vol. 46, No. 10, 1967, p. 3818–29. [Study of OH radical in ice after electron irradiation at 77°K.]CrossRefGoogle Scholar
Hall, P. G. Tompkins, F. C. Dielectric relaxation in water adsorbed on ionic crystals. Journal of the Chemical Society, Sect. A, 1966, No. 1, p. 36–40. [Study of dielectric loss of ILO adsorbed on CaF2, MgO, KCl and Ag1. Discussion of extent to which adsorbed layers are ordered and ice-like.]CrossRefGoogle Scholar
James, D. W. Solidification kinetics of ice determined by the thermal wave technique. (In Peiser, H. S., ed. Crystal growth. Proceedings of an international conference on crystal growth, Boston, 20–24 June 1966. Oxford, etc., Pergamon Press, [1967], p. 767–73.) [Application to ice of method of determining kinetics of freezing normal to basal plane.]Google Scholar
Jones, S. J. Softening of ice crystals by dissolved fluoride ions. Physics Letters, Vol 25A, No. 5, 1967, p. 366–67. [At c. −70°C small amounts of HF considerably reduce stress in constant strain-rate tests and increase the creep rate.]CrossRefGoogle Scholar
Kikuchi, K. On the positive electrification of snow crystals in the process of their melting (III).-(IV). Journal of the Meteorological Society of Japan, Ser. 2, Vol. 43, No. 6, 1965, p. 343–50; p. 351–58. [(III): relation between bubble concentration in ice and charge generation during melting confirmed experimentally. (IV): during melting of bubbly ice, droplets seen to burst from surface carried negative charge.]Google Scholar
Kim, D.-Y. Schmidt, V. H. Semiclassical theory of proton transport in ice. Canadian Journal of Physics, Vol. 45, No. 4, 1967, p. 1507–16. [Calculation of mobility of protons in ice which agrees well with electrical conductivity experiments.]CrossRefGoogle Scholar
Koros, R. M., and others. The sticking probability of water on ice, [by] R. M. Koros, J. M. Deckers, R. P. Andreas and M. Boudart. Chemical Engineering Science, Vol. 21, No. 10, 1966, p. 941–50. [Beam of water vapour molecules impinges on ice target and number sticking found.]CrossRefGoogle Scholar
Krausz, A. S., and others. Tubular ice crystals, by A. S. Krauss, B. Harron and G. G. Litvan. Nature, Vol. 215, No. 5098, 1967, p. 271–73.CrossRefGoogle Scholar
Kröger, F. A. The chemistry of imperfect crystals. Amsterdam, North-Holland Publishing Co., 1964. xvi, 1039 p. [Ch. 18, “Special cases of disorder”, has section 18.2, p. 750–67, devoted to ice.]Google Scholar
Levi, L. Kobayashi, T. Ice filaments grown in a gradient of vapour pressure. Journal of the Meteorological Society ofjapan, Ser. 2, Vol. 45, No. 4, 1967. p. 315–25. [Study of the filaments which form when ice crystals, nucleated on fine threads, grow upwards and sublimate underneath, leaving a Filament between crystals and thread.]CrossRefGoogle Scholar
Levi, L. Milman, O. Freezing potential of electrolytic solutions. Journal of the Atmospheric Sciences, Vol. 23. No. 2, 1966, p. 182–86. [Experimental study for NH3 and NaCI solutions.]2.0.CO;2>CrossRefGoogle Scholar
Lieb, E. H. Exact solution of the F model of an antiferroelectric. Physical Review Letters, Vol. 18, No. 24, 1967. p. 1046–48. [Exact solution of phase transition and electrical properties of antiferroelectric structure similar to that of ice.]CrossRefGoogle Scholar
Lieb, E. H. Exact solution of the problem of the entropy of two-dimensional ice. Physical Review Letters, Vol. 18, No. 17, 1967, p. 692–94. [Entropy of two-dimensional square lattice obeying Bernal-Fowler rules found to be k In (4/3)3/1 per molecule.]CrossRefGoogle Scholar
Lieb, E. H. Exact solution of the two-dimensional Slater KDP model of a ferroelectric. Physical Review Letters, Vol. 19, No. 3, 1967, p. 508–10. [Exact solution of phase transition and electrical properties of ferroelectric structure similar to that of ice.]CrossRefGoogle Scholar
Lindenmeyer, C. S. Chalmers, B. Growth rate of ice dendrites in aqueous solutions. Journal of Chemical Physics, Vol. 45, No. 8, 1966, p. 2807–08. [Measurement of free and substrate growth rates as function of supercooling and solute concentration.]CrossRefGoogle Scholar
Lindenmeyer, C. S. Chalmers, B. Morphology of ice dendrites. Journal of Chemical Physics, Vol. 45, No. 8, 1966, p. 2804–06. [Direction of dendrites growing in supercooled pure water, aqueous solution and on substrates.]CrossRefGoogle Scholar
Maybank, J. Barthakur, N. N. The growth and destruction of ice filaments in an electric field. Nature. Vol. 216, No. 5110, 1967, p. 50–52. [Letter. Study of filament-like ice crystals growing near a freezing water drop and their modification by an electric field.]CrossRefGoogle Scholar
Morachevskiy, B. G. Ob aktivnosti chastits Ag J v kachestve l’doobrazuyushchikh yader . Izvestiya Akademii.Nauk SSSR. Atmosfery I Okeana , Tom 3, No. 1, 1967, p. 105–07. [If the isotope 131I is used in the Ag1 it does not act as nucleus. English translation in Izvestiya. Academy of Sciences, U.S.S.R. Atmospheric and Oceanic Physics, Vol. 3, No. 1, 1967, p. 59–60.]Google Scholar
Parungo, F. P. Lodge, J. P. jr. Amino acids as ice nucleators. Journal of the Atmospheric Sciences, Vol. 24. No. 3, 1967, p. 274–77. [Difference between optically active and inactive forms. Thermodynamic explanation.]2.0.CO;2>CrossRefGoogle Scholar
Parungo, F. P. Lodge, J. P. jr. Molecular structure and ice nucleation of some organics. Journal of the Atmospheric Sciences, Vol. 22, No. 3, 1965, p. 309–13. [Nucleating ability found to vary with potential strength of hydrogen bond between hydroxyl or carboxyl group and H2O molecule.]2.0.CO;2>CrossRefGoogle Scholar
Pinatti, D. Mascarenhas, S. Electrical currents produced during the solidification of water (Costa Ribeiro effect). Journal of Applied Physics, Vol. 38, No. 6, 1967, p. 2648–52. [Description of apparatus in which freezing or melting rate can be controlled and associated current measured. Results quoted. Importance for thunderstorm electricity discussed.]CrossRefGoogle Scholar
Pruppacher, H. R. On the growth of ice in aqueous solutions contained in capillaries. eitschriftfür.Nataforschung, Bd. 22A, Ht. 6, 1967, p. 895–901. [Observations of variation of dendritic growth rate with various dissolved monovalent ions.]Google Scholar
Qureshi, M. M. Maybank, J. Further tests on the ice nucleation potential of meteoritic material. Nature, Vol. 211, No. 5048, 1966, p. 508–09. [Laboratory tests.]CrossRefGoogle Scholar
Ramseier, R. O. Self-diffusion of tritium in natural and synthetic ice monocrystals. Journal of Applied Physics, Vol. 38, No. 6, 1967, p. 553–56. [Measurement both parallel and perpendicular to c-axis from −2.5° to −35.9°C. Interpretation as due to vacancy diffusion of H2O molecules.]CrossRefGoogle Scholar
Riehl, N. Protonic mobility and its importance for biological systems. Transactions of the New rork Academy of Sciences, Ser. 2, Vol. 27, No. 7, 1965, p. 772–81. [Discussion of proton motion along hydrogen bonds, particularly in ice. Also published in Phillips, G. O., ed. Energy transfer in radiation processes. Chemical, physical and biological aspects. Proceedings of the international symposium held at Cardiff, January, 1965. Amsterdam, Elsevier, 1966, p. 95–104.]CrossRefGoogle Scholar
Roedder, E. Metastable superheated ice in liquid-water inclusions under high negative pressure. Science, Vol. 155, No. 3768, 1967, p. 1413–57. [Retention of ice up to +6.5°C in liquid inclusions in minerals with negative pressure of c. 1000 bar.]CrossRefGoogle ScholarPubMed
Roulleau, M. Poc, M.-M. Electrocongelation des brouillards surfondus. Comptes Rendas Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 264, No. 21, 1967, p. 1480–83. [Strong electric field causes freezing of supercooled mist droplets.]Google Scholar
Shreve, R. L. Migration of air bubbles, vapor figures and brine pockets in ice under a temperature gradient. Journal of Geophysical Research, Vol. 72, No. 16, 1967, p. 4093–100. [Theory, and comparison with reported experiments.]CrossRefGoogle Scholar
Soules, J. A. Improved sophomore experiment to measure latent heat of fusion. American Journal of Physics, Vol. 35, No. 1, 1967, p. 23–26. [Two forms of teaching experiment to determine latent heat of fusion of ice.]CrossRefGoogle Scholar
Starr, J. R. Mason, B. J. The melting of small ice spheres and cones. Quarterly Journal of the Royal Meteorological Society, Vol. 92, No. 394, 1966, p. 500–09. [Times of complete melting in airstreams of controlled temperature, humidity and velocity measured and compared with theory.]Google Scholar
Sutherland, Bill. Exact solution of a two-dimensional model for hydrogen-bonded crystals. Physical Review Letters, Vol. 19, No. 3, 1967, p. 103–04. [Solution of two-dimensional ice lattice in electric field.]CrossRefGoogle Scholar
Tippe, A. Zum Piezoeffekte bei Eis I. Naturwissenschaften, 54. Jahrg., Ht. 3, 1967, p. 68–69. [Explanation of effect observed by A. Deubner, R. Heise and K. Wenzel, ibid., 47. Jahrg., Ht. 24, 1960, p. 600–01, as not due to piezoelectricity.]CrossRefGoogle Scholar
Weissmann, M., and others. On the hydrogen bond in an ice-like structure, [by] M. Weissmann, L. Blum and N. V. Cohan. Chemical Physics Letters, Vol. 1, No. 3, 1967, p. 95–98. [Comparison of various methods of calculating hydrogen-bond energy between water molecules in ice.]CrossRefGoogle Scholar
Williamson, R. B. Chalmers, B. Morphology of ice solidified in undercooled water. (In Peiser, H. S., ed. Crystal growth. Proceedings of an international conference on crystal growth, Boston, 20–24 June 1966. Oxford, etc. Pergamon Press, [c 1967], p. 739–43.) [Study of shapes of crystals formed at different supercooling and explanation.]Google Scholar
Yosida, Z. Kōri no kesshō no hyómen kōzō. I. Kesshō teimen no kōzō, keiri no kesshō no heikōkei . Teion-kagaku , Ser. A, Vol. 24, 1966, p. 1–18. [Theory of equilibrium form of ice surface. English extended summary p. 14–18.]Google Scholar
Zhitnikov, R. A. Kolesnikov, N. V. Teoreticheskoye rassmotreniye matrichnykh sdvigov rasshchepleniy sverkhtonkoy struktury dlya atomov Cu, Ag i Au, stabilizirovannykh v polyarnoy matritse (ILO) . Fizika Tverdogo Tela , Tom 9, Vyp. 1, 1967, p. 162–66. [Results for Ag and Au in good agreement with theory. English translation in Soviet Physics-Solid State, Vol. 9, No. 1, 1967, p. 121–24]Google Scholar
Zimbrick, J. Kevan, L. Evidence for trapped dielectrons in ice. Journal of the American Chemical Society, Vol. 89, No. 10, 1967, p. 2483–84. [Letter. After high y-irradiation electron resonance studies suggest two electrons can be trapped in the same OH− vacancy.]CrossRefGoogle Scholar

Land Ice Glaciers. Ice shelves

Adamson, R. G. Cavaney, R. J. Volcanic debris-layers near Mount Melbourne, northern Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967, p. 418–21. [Description of layers in Campbell Glacier.]CrossRefGoogle Scholar
Bayrock, L. A. Catastrophic advance of the Steele Glacier, Yukon, Canada. Alberta University. Boreal Institute. Occasional Publication No. 3, 1967, 35 p. [Report of survey, 20–23 August 1966. Maximum rate of flow was 46 ft (14 m) per 24 h mainly by slipping at the base. At the toe, most of the motion could be accounted for by shearing along the base.]Google Scholar
Behrendt, J. C., and others. Geophysical reconnaissance in the Pensacola Mountains, by J. C. Behrendt, J. R. Henderson and L. J. Meister. Antarctic Journal of the U.S., Vol. 1, No. 4, 1966, p. 125–26. [Helicopter survey made during 1965–66 austral summer included seismic reflection. gravity and aeromagnetic studies.]Google Scholar
Beitzel, J. E. Bentley, C. R. Geophysical investigations in Marie Byrd Land. Antarctic Journal of the U.S., Vol. 2, No. 4, 1967, p. 95–97. [Measurements of ice thickness, required for reduction of gravity data as well as for glaciological purposes.]Google Scholar
Bowman, G. C. Directional characteristics of ionosende interference patterns from the Filchner Ice Shelf. AVCO Corporation, AVCO Space Sÿslems Division, Wilmington, Mass., Contract NSF-C403, Antarctic Research and Data Analysis, Scientific Report 24, AVSSD-0224–66-CR, 1966, 34 p. [Use of apparatus intended to study ionosphere to find depth of ice shelf and dielectric constant of its ice.]Google Scholar
Brecher, H. H. Measurements of ice-surface movement by aerial triangulation. Antarctic Journal of the U.S., Vol. 2, No. 4, 1967, p. 123. [Variation of accumulation along line of markers was strikingly similar during two time intcrvals]Google Scholar
Browne-Cooper, P. J., and others. Probable local seismicity at Wilkes, Antarctica, [by] P. J. Browne-Cooper, G. R. Small and R. Whitworth. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967, p. 443–45. [Includes seismic records attributed to “ice-quakes”.]CrossRefGoogle Scholar
Crozaz, G. Langway, C. C. jr. Dating Greenland firn-ice cores with Ph-210. Earth and Planetary Science Letters, Vol. 1, No. 4, 1966, p. 194–96. [Method applied to depth profile of North Greenland ice sheet.]CrossRefGoogle Scholar
Einarsson, E. H. Sudurbrún Mÿrdalsjökuls viò Gvendarfell. Breytingar sioustu 100 ár 0. fl. Jökull, [Vol.] 3, Ár 16, 1966, p. 216–18. [Variations of the southern margin of Mÿrdalsjökull at Gvendarfell. Between about 1870 and about 189n the glacier margin advanced, but from then until 1966 it was on the whole retreating.]CrossRefGoogle Scholar
Einarsson, T. Physical aspects of sub-glacial eruptions. Jökull, [Vol.] 3, Ár 16, 1966, p. 167–74.CrossRefGoogle Scholar
Evison, F. E. Note on the aseismicity of Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967, p. 479–83. [Suggests that scarcity of earthquakes is dues to thickening of ice sheet.]CrossRefGoogle Scholar
Gluck, S. Détermination du lit rocheux sous la Mer de Glace par séismique-réflexion. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. D, Tom. 264, No. 19, 1967, p. 2272–75. [Seismic study of bed of Mer de Glace, France.]Google Scholar
Goncharov, E. P. Hydrofneteorological observatory on the Fed”cenko glacier. WMO Bulletin, Vol. 16, No. 1, 1967, p. 20–23. [Early history of glacier and construction of observatory at side of glacier in 1932, described. Brief outline of results of research.]Google Scholar
Gow, A. J. Antarctic glaciological studies. Antarctic Journal of the U.S., Vol. 2, No. 4, 1967, p. 121–22. [Investigations of the composition, structure, and mass balance of the Koettlitz Glacier.]Google Scholar
Heine, A. J. The McMurdo Ice Shelf, Antarctica: a preliminary report. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967, p. 474–78. [Ice movement and strain, density profiles and accumulation rates.]CrossRefGoogle Scholar
Holdsworth, G. Investigation of Meserve Glacier. Antarctic Journal of the U.S., Vol. 2, No. 4, 1967, p. 123–24. [Determining conditions of ice flow at base of glacier. Micrometeorological investigations were continued both on moraine and glacier surface.]Google Scholar
Kazanskiy, A. B. Temperaturnoye pole lednikov . Geojlzicheskiy Byuíleten’ , No. 17, 1966, p. 25–32. [Theoretical determination. Emphasis on temperature near bed.]Google Scholar
Kotlyakov, V. M. Opyt podscheta zapasov vody akkumulirovannoy v gornykh lednikakh Sovetskogo Soyuza . lzvest ya Akademii Nauk SSSR. Seriya Geograflcheskaya , 1966, No. 3, p. 43–48.Google Scholar
Lazarev, G. E., and others. Podlednyy rel’yef shel’fovogo lednika Shekltona po dannym geofizicheskikh issledovaniy . Izvestya Akademii Nauk SSSR, Fitika Zemli , 1965, No. 9, p. 44–53. [Gravity, seismic. hydrological and echo-sounding data compared. English translation in Izveslya. Academy of Sciences, U.S.S.R. Physics of the Solid Earth, 1965, No. 9 [pub. 1966], p. 607–12.]Google Scholar
Liestøl, O. Storbreen glacier in Jotunheimen, Norway. Norsk Polarinstitpzt. Skrifter, Nr. 141, 1967, 63 p. [Review of work, 1949–65, including accumulation, ablation, mass balance, and surface speed.]Google Scholar
Oettli, M. Un monde glaciaire sous l’équateur: le Ruwenzori. Les Alpes. Revue du Club Alpin Suisse, 43e An., 3e Trimestre, 1967, p. 162–65. [General description.]Google Scholar
Østrem, G. A new glacier map of Erdalsbreen/Vesledalsbreen: a part of the,Josledalsbreen ice-cap. Oslo, Norges Vassdragsog Elektrisitetsvesen, Hydrologisk Avdeling, 1967. 2 p., map [1: 20 000]. [Copies available from Hydrologisk Avdeling, Vassdragsvesenet, Postboks 5091 Mj, Oslo 3. Norway.]Google Scholar
Østrem, G., and others. Glacio-hydrology, discharge and sediment transport in the Decade Glacier area, Baffin Island, N.W.T., by G. Østrero, C. W. Bridge and W. F. Rannie. Geografiska Annaler, Vol. 49A, Nos. 2–4, 1967, p. 268–82. [Mass balance studies were initiated in 1965; the 1965 budget was slightly positive.]Google Scholar
Outcalt, S. I. MacPhail, D. D. A survey of neoglaciation in the Front Range of Colorado. Unidersîtr of Colorado Studies. Series in Earth Sciences, No. 4, 1965, 124 p. [Investigations of glacier net budget and regional climatic variation reveal curious metabolic characteristics of Front Range glaciers.]Google Scholar
Risk, G. P. Hochstein, M. P. Subsurface measurements on the McMurdo Ice Shelf, Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967, p. 484–97. [Measurement of ice melting rate at bottom and of density and temperature profiles]CrossRefGoogle Scholar
Ritchie, W. Note on the retreat of Reintindbre glacier (Frostisen). Norsk Geografisk Tidsskrift, Bd. 21, Ht. 2, 1967–68, [pub.] 1967, p. 143–44. [Comparison of surveys of front in 1906, 1934 and 1963.]Google Scholar
Robin, G. de Q. Surface topography of ice sheets. Nature, Vol. 215, No. 5105, 1967, p. 1029–32. [Refinement of theory of relation between surface slope and depth of flowing ice sheets.]CrossRefGoogle Scholar
Schytt, V. A study of ablation gradient . Geografiska Annaler, Vol. 49a, Nos. 2–4, 1967, p. 327–32. [Observations show that there is no clear relation between ablation gradient and latitude but that the ablation gradient is strongly dependent upon the degree of continentality.]CrossRefGoogle Scholar
Suyetova, I. A. The dimensions of Antarctica. Polar Record, Vol. 13, No. 84, 1966, p. 344–47. [Analysis of modern data on area, mean elevation of ice and rock, thickness and volume of ice sheet and ice budget.]CrossRefGoogle Scholar
Thorarinsson, S. The age of the maximum postglacial advance of Hagafellsjökul eystri (a tephrochronological study). Jökull, [Vol.] 3, Ár 16, 1966, p. 207–10. [Between A.D. 850 and 900, glacier smaller than or maximally as large as in 1929; about 1670, glacier reached its 1939 position; 1708, extension of the glacier the same as in 1929 or 1939; glacier is now stagnant or receding.]CrossRefGoogle Scholar
Tronov, M. V. Ledniki i klimat . Leningrad. Gidrometeorologicheskoye Izdatel’stvo [Hydrological and Meteorological Publishing Flouse], 1966. 407 p. [Glacial climatic regions and interactions between glaciers and climate.]Google Scholar
Vinogradov, O. N., and others., ed. Rukovodstvo po sostavleniyu kataloga lednikov SSSR , [edited by] Vinogradov, O. N. Krenke, A. N. Oganovskiy, P. N.. Leningrad, Gidrometcorologicheskoye Izdatel’stvo [Hydrological and Meteorological Publishing House], 1966. 154 p. [Detailed instructions for compilation of major reference work.]Google Scholar
Vivian, R. Mallon, R. Fiches des glaciers français. Le glacier d’Argentière. Reme de Géographie Alpine, Tom. 55, Ease. 3, 1967, p. 579–82.CrossRefGoogle Scholar
Vivian, R. Mallon, R. Fiches des glaciers français. Le glacier du Tour. Revue de Géographie Alpine, Tom. 55, Fast 3, 1967, p. 583–86.CrossRefGoogle Scholar

Icebergs. Sea, River and Lake Ice

Adams, W. P. Shaw, J. B. Studies of ice cover on Knob Lake, New Quebec. Cahiers de Géographie de Québec, 11e An., No. 2, 1967, p. 88–96. [Systematic observations of lake ice cover in the vicinity of Schefferville, Quebec.]CrossRefGoogle Scholar
Bell, R. A. I. Lake Miers, south Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 10. No. 2, 1967, p. 540–56. [Includes study of lake ice and ablation phenomena on its surface.]CrossRefGoogle Scholar
Berdennikov, V. P. Fizicheskiye kharakteristiki l’da zatorov i zazhorov . Trudy Gosodarstvennogo Gidrologicheskogo Instituta , Vyp. 129, 1965, p. 19–43. [Studies on ice in two rivers, including mechanical tests. English translation in Soviet Hydrology. Selected Papers, 1965, No. 4, p. 384–402]Google Scholar
Bogorodskiy, V. V. Galkin, E. I, Issledovaniye vnutrennego treniya plastin I’da so sloyetn pri izgibnykh kolebaniyakh . Akusticheskiy Zhurnal . Tom 12, Vyp. 4, 1966, p. 411–15. [Investigations on slabs frozen in a tank of water in the laboratory. English translation in Soviet Physics-Acoustics, Vol. 12, No. 4, 1967, p. 360–63.]Google Scholar
Bradle, R. A. Slar imagery for sea ice studies. Photogrammetric Engineering, Vol. 33, No. 7, 1967, p. 763–66. [Use of side-looking airborne radar for study of sea ice under bad weather conditions or darkness.]Google Scholar
Bradley, J. Palmer, D. F. Ice-cored moraines and ice diapirs, Lake Miers, Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967. p. 599–623. [Discussion of mechanism of formation of these “moraines” in the lake ice over this lake.]CrossRefGoogle Scholar
Bukina, L. A. Raspredeleniye po razmeram kristallov vnutrivodnogo l’da v turbulentnom potoke . Izvestiya Akademii Nauk SSSR. Fizika Atmosfery i Okeana , Tom 3, No. 1, 1967, p. 58–68. [Experimental determination. English translation in Izvestáya. Academy of Sciences, U.S.S.R. Atmospheric and Oceanic Physics, Vol. 3, No. 1, 1967, p. 31–36.]Google Scholar
Buynitskiy, V. Kh. Nekotoryye zakonomernosti raspredeleniya i formirovaniya dreyfuyushchikh morskikh l’dov v Antarktike . Trudy Sovetskoy Antarkticheskoy Ekspeditsii , Tom 44, 1965, p. 27–34– [Sea-ice limits and zones of differing ice conditions from Prinsesse Astrid Kyst to Shackleton Ice Shelf, 1961–62]Google Scholar
Buynitskiy, V. Kh. O vliyanii diatomovykh vodorosley na stroyeniye i prochnost’ morskikh l’dov . Trudy Sovetskoy Antarkticheskoy Ekspeditsii , Tom 44, 1965, p. 83–88. [Experiments on samples of shore ice.]Google Scholar
Buynitskiy, V. Kh Dmitrash, Zh. A. Novey dannyye po fizike morskikh l’dov Antarktiki . Trudy Sovetskoy Antarkticheskoy Ekspeditsii , Tom 44. 1965. p. 44–82– [Brine content, density, strength and elastic modulus of sea ice.]Google Scholar
Groen, P. The waters of the sea. Princeton, N. J., London, etc., D. Van Nostrand and Co. Ltd., 1967. 328 p. (Chapter on “Ice in the seas” includes: icebergs, ice islands, ground ice, formation, thawing and gravity of sea ice, thickness of polar ice, the “Great Ice Barrier”, and ice drift.)Google Scholar
Hunkins, K. Inertial oscillations of Fletcher’s Ice Island (T-3). Journal of Geophysical Research, Vol. 72, No. 4.1967, p. 1165–74. [Circular motion interpreted as inertial oscillations due to change of wind stress.]CrossRefGoogle Scholar
Kagan, B. A. O vertikal’nom profile skorosti prilivnogo techeniya v more, pokrytom l’dom . Izvestiya Akademii JVauk SSSR. Fizika Atrnosfery i Okeana , Tom 3, No. 1, 1967. p. 69–77. [Equations for profile of tidal current velocity in ice-covered sea. English translation in Izvestiva. Academy of Sciences, U.S.S.R. Atmospheric and Oceanic Physics, Vol. 3, No. 1. 1967 p. 37–41.]Google Scholar
Kagan, B. A. Trekhmernaya model’ prilivnogo potoka v more. pokrytom l’donv . Izvestiya Akademii Arauk SSSR. Fizika Atnlosfery i Okeana , Tom 3. No. 5. 1967. p. 526–36. [Equations set up and used to deduce charts of tidal characteristics in Sea of Okhotsk. English abstract.]Google Scholar
Kerr, A. D. On plates sealing an incompressible liquid. International Journal of Mechanical Sciences, Vol. 8, No. 4, 1966. p. 295–304. [Mathematical study of problem of bearing capacity of ice floes on which melt water has partially refrozen.]CrossRefGoogle Scholar
Nikolayev, S. Ye. Ledoissledovatel’skiye raboty . Trudy Sovetskoy Antarkticheskoy Ekspeditsii , Tom 51, 1967, p. 101–07. [Experiments on mechanical properties of floating ice carried out off Mirny, 1963.]Google Scholar
Ofuya, A. O. Reynolds, A. J. Laboratory simulation of waves in an ice floe. Journal of Geophysical Research. Vol. 72, No. 14, 1967, p. 3567–83. [Use of model with thin polyethylene sheets floating on water to simulate sea ice.]CrossRefGoogle Scholar
Romanov, I. P. Raspredeleniye l’dov i aysbergov v pribrezhnykh vodakh Antarktidy v navigatsiyu 1964 g. . Trudy Sovetskoy Antarkticheskoy Ekspeditsii , Tom 51, 1967, p. 184–89. [Floating ice observed by Soviet parties, long. 10°–100°E.]Google Scholar
Stonehouse, B. Occurrence and effects of open water in McMurdo Sound, Antarctica. during winter and early spring. Polar Record, Vol, 13, No. 87, 1967, p. 775–78.CrossRefGoogle Scholar
Tsurikov, V. L. O formirovanii ionnogo sostava i solennosti morskogo l’da . Okeanologiya , Tom 5, Vyp. 3, 1965, p. 463–72. [Results of experiments on freezing sea-water and NaCl solution.]Google Scholar
Wilson, J. Tuzo- Are the structures of the Caribbean and Scotia Arc regions analogous to ice rafting? Earth and Planetary Science Letters, Vol. 1, No. 5, 1966, p. 335–38. [Analogy between thrust structures in young sea ice and structure of island arcs.]CrossRefGoogle Scholar
Yeskin, L. I. Ledovyye nablyudeniya . Trudy Sovetskoy Antarkticheskoy Ekspeditsii . Tom 51, 1967. p. 92–100. [Sea ice observations off coast of Antarctica, long. 10°–100°E., 1962–63.]Google Scholar
Zakharov, V. F. Nekotoryye osobennosti raschetnogo dreyfa l’da v more Laptevykh . Problemy Arktiki i Antarkliki . Vyp. 23, 1966, p. 45–46. [Mean drift calculated from air pressure pattern over many years.]Google Scholar
Zdanovich, V. G. Sharikov, Yu. D. Nekotoryye voprosy opredeleniya dreyfa l’dov s primeneniyem aerofotos”yemki . Problemy Arkliki i Antarktiki , Vyp. 21, 1965, p. 81–88. [Improved method suggested.]Google Scholar

Glacial Geology

Brown, M. J. F., and others. A new radiocarbon date for Wales, by M. J. F. Brown, L D. Ellis-Gruffydd, H. D. Foster, D. J. Unwin. Nature, Vol. 213, No. 5082, 1967, p. 1220–21. [Results in new views on southern limit of Würm ice in Irish Sea basin.]CrossRefGoogle Scholar
Corbel, J. Zones hypoglaciaires et hyperglaciaires lors du maximum des inlandsis quaternaires arctiques. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. D. Tom. 263, No. 16, 1966. p. 1055–57. [Study of Arctic Quaternary ice sheets shows region of strong glacierization on one side and of arid, periglacial region on the other.]Google Scholar
Dahl, R. Senglaciala ackumulationsformer och glaciationsförh$llanden i Narvik- Skjomenomradet, Norge. Norsk Geograftsk Tidsskrift, Bd. 21, Ht. 3, 1967–68, [pub.] 1967, p. 157–241. [Late-glacial accumulation forms and glaciation in the Narvik-Skjomen district, Norway, are described and discussed.]CrossRefGoogle Scholar
Dauvillier, A. Sur le rôle de l’activité solaire et des migrations polaires dans l’origine et l’évolution de la vie terrestre. Comptes Rendue Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. B, Tom. 263, No. 10. 1966, p. 660–63. [Eocambrian glaciation due to low level of atmospheric oxygen; subsequent glaciations to reduction of solar activity.]Google Scholar
Denton, G. H. Stuiver, M. Neoglacial chronology, northeastern St. Elias Mountains, Canada. American,Journal of Science, Vol. 264, No. 8, 1966, p. 577–99. [Donjek and Kaskawulsh Glaciers, from 12 500 b.p. to present.]CrossRefGoogle Scholar
Derbyshire, E. Discussion on the glacial map of Tasmania. Australian Journal of Science, Vol. 29, No. 4, 1966. p. 102–03. [Report of discussion during ANZAAS meeting in Hobart concerning new glacial map and problems of Tasmanian glaciation.]Google Scholar
Einarsson, T. Late- and post-glacial rise in Iceland and sub-crustal viscosity., Jökull, [Vol.] 3, Ár 16, 1966. p. 157–66. [Subcrustal viscosity for Iceland is one order of magnitude less than that for Scandinavia (Einarsson, 1953).]CrossRefGoogle Scholar
Flinn, D. The ice front in the North Sea. Nature, Vol. 215, No. 5106, 1967, p. 1151–54. [Belt of deeps suggests that at last glacial maximum Norwegian ice did not cross North Sea.]CrossRefGoogle Scholar
Gabert-Delay, J. Moraines, terrasses et glacis dc versant du bassin de Laragne. Revue de Géographie Alpine, Tom. 55, Fasc. 3, 1967, p. 521–48. [Study of moraines and other geomorphological features of this region of southern France.]CrossRefGoogle Scholar
Gage, M. Accordant and discordant glacial sequences. Geological Society of America. Special Papers, No. 84, 1965. p. 393–414. [Contrast between accordant and discordant histories illustrates the “topographic” element in Flint’s “solar-topographic” generalization of the causes of glaciations.]CrossRefGoogle Scholar
Gage, M. The climate of New Zealand during cool phases of the Pleistocene. In Pleistocene and post-Pleistocene climatic variations in the Pacific area. Honolulu, Bishop Museum Press, 1966, p. 83–94. [Willett’s (1950) estimate of 3 500 ft (1 000 m) average lowering of snow line is still regarded as reasonable for the last glaciation, but may not be applicable to earlier glaciations.]Google Scholar
Grindley, G. W. The geomorphology of the Miller Range, Transantarctic Mountains, with notes on the glacial history and neotectonics of East Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967, p. 557–98 CrossRefGoogle Scholar
Heuberger, H. GletschergeschichtIiche Unterstwhungen in den Zentralalpen zwischen Sellrain- und Ötztal. Innsbruck. Universitätsverlag Wagner, 1966. 127 p., map [in end-pocket]. (Wissenschaftliche Alpenvereinshefte. Ht. 20.) [Analysis of glacial geological features and interpretation for this region of the Austrian Alps.]Google Scholar
Hoppe, G. Case studies of degIaciation patterns. Geogratska Avaler, Vol. 49a, Nos. 2–4, 1967, p. 204–12. [Describes two cases of rather complicated patterns of deglaciation and ice movements.]Google Scholar
Kaiser, K. Probleme und Ergebnisse der Quartärforschung in den Rocky Mountains (i.w.S.) und angrenzenden Gebieten. Zeitschrift far Geomorphologie, Neue Folge, Bd. 10, Ht. 3, 1966, p. 264–302. [Discussion of present and Pleistocene snow line in Rocky Mountains and climatic implications. French and English summaries.]Google Scholar
Krayner, N. P. S.S. Kutorga o drevnem oledenenii AI’p . Izvestiya Akademii Nauk SSSR. Seriya Geograficheskaya , 1966, No. 6, p. 66–74. [Work of pioneer Russian investigator published 1840–58.]Google Scholar
Laverdière, C. Le vocabulaire de la géomorphologie glaciaire, III. Cahiers de Géographie de Québec, 11e An., No. 2, 1967, p. 102–07.CrossRefGoogle Scholar
Lewis, C. A. The Breconshire end-moraine. Nature, Vol. 212, No. 5070, 1966, p. 1559–61. [Discussion of limits of ice during last glaciation.]CrossRefGoogle Scholar
McCulloch, D. Hopkins, D. Evidence for an early Recent warm interval in northwestern Alaska. Geological Society of America. Bulletin, Vol. 77, No. 10, 1966, p. 1089–107. [Radiocarbon dating of warm period 10 000–8 300 b.p]CrossRefGoogle Scholar
Mitchell, G. F. Orme, A. R. The Pleistocene deposits of the Isles of Scilly. Quarterly Journal of the Geological Society of London, Vol. 123, No. 489, Pt. 1, 1967, p. 59–92. [Existence of till and outwash gravel along the northern margin of the Scilly Isles. The sequence is compared with similar deposits in the south of England and Ireland.]Google Scholar
Mölder, K. Über die Entstehung des inneren Salpausselkä zwischen Jaala und Saimaa. Bulletin de la Commission Géologique de Finlande, Tom. 38, No. 222, 1966, p. 75–92. [Description of conditions which gave rise to this esker.]Google Scholar
Nichols, R. L. Geomorphology of Antarctica. (In Tedrow, J. C. F., ed. Antarctic soils and soil forming processes. Washington, D.C., American Geophysical Union, 1966, p. 1–46. (Antarctic Research Series, Vol. 8.)) [Includes glacial and periglacial geomorphology.]Google Scholar
Oen Ing Soen. Geomorphological observations on Sermersôq. A contribution to the geomorphology of S. Greenland. Meddelelser om Grønland, Bd. 179, Nr. 5, 1965, 41 p. [Four erosion surfaces recognized and related to three cycles of erosion interrupted by two glacial stages.]Google Scholar
Peacock, J. D. West Highland morainic features aligned in the direction of ice flow. Scottish Journal of Geology, Vol. 3, Pt. 2, 5967, p. 372–73. [Surface features of glacial deposit aligned by overriding ice.]CrossRefGoogle Scholar
Peterson, J. A. Glaciation of the Frenchman’s Cap, National Park. Papers and Proceedings of the Royal Society of Tasmania, Vol. 100, 1966, p. 117–29. [Study of glacial landlbrms suggests an independent system of cirque and valley glaciers during the last Pleistocene glaciation of this part of Tasmania.]CrossRefGoogle Scholar
Portmann, J.-P. Recherches géo-glaciologiques. Les Alpes, 43e An., 3e Trimestre, 1967, p. 190–91. [Necessity of recording geographical features, e.g. nature of rocks incorporated in glacier and periglacial features.]Google Scholar
Shackleton, N. Oxygen isotope analyses and Pleistocene temperatures re-assessed. Nature, Vol. 215, No. 5096. 1967, p. 15–17. [Changes in oxygen isotope composition are said to correspond with the extraction of large amounts of water from the oceans during glacial periods and the recirculation of this water during periods when glaciers were at their present levels.]CrossRefGoogle Scholar
Shotton, F. W. Age of the Irish Sea glaciation of the Midlands. Nature, Vol. 215, No. 5108, 1967, p. 1366. [Letter. Ice advance in central England dated as late Würm.]CrossRefGoogle Scholar
Shotton, F. W. The problems and contributions of methods of absolute dating within the Pleistocene period. Quarterly Journal of the Geological Society of London, Vol. 122, No. 488, Pt. 4, 1966, [pub.] 1967, p. 357–83. [Radiocarbon dates now indicate that the Würm glaciation in the northern hemisphere had two stadia of approximately equal importance.]CrossRefGoogle Scholar
Souchez, R. A. Le recul des verrous-gradins et les rapports glaciaire-périglaciaire en Antarctique. Revue de Géomorphologie Dynamique, An. 17, No. 2, 1967, p. 49–54. [Study of glacial erosion by outlet glaciers in south Victoria Land and in western Sor-Rondane mountains, Dronning Maud Land. Relation between periglacial processes and glacial erosion.]Google Scholar
Souchez, R. A. Réflexions sur l’évolution des versants sous climat froid. Revue de Géographie Physique et de Géologie Dynamique, Sér. 2, Vol. 8, Fasc. 4, 1966, p. 317–34. [Discussion of evolution of slopes in a cold climate.]Google Scholar
Souchez, R. A. Sur les mécanismes de l’érosion en Antarctique. Bulletin de la Société Belge d’Études Géographiques, Tom. 35, No. 1, 1966, p. 25–34. [Stresses idea of glacial erosion under ice falls of distributary glaciers.]Google Scholar
Szupryczyński, J. Przebieg deglatjacji na obszarze pólnocnego Spitsbergenu w rejonie fiordu Bock. Przeglqd Geograficzny, Tom 38, Zeszyt 3, 1966, p. 407–28. [The course of deglaciation in north Vestspitsbcrgcn in the Bock Fjord region. Extended summaries in Russian and English.]Google Scholar

Frost Action on Rocks and Soil. Frozen Ground. Permafrost

Anderson, D. W., and others. Frost phenomena on Mars, by D. W. Anderson, E. S. Gaffney and P. F. Low. Science, Vol. 155, No. 3760, 1967, p. 319–22. [Suggests frost phenomena are not to be expected on Mars without strongly deliquescent soils.]CrossRefGoogle Scholar
Baulin, V. V. Moshchnost’ merzlykh tolshch kak odin iz pokazateley tektonicheskogo stroyeniya rayona . Geologcaa i Geoprzika , 1966, No. 1, p. 53–62. [Correlation between permafrost thickness and tectonic movement in west Siberian plain. English translation: Canada. Defence Research Board. Translation T464R, 1966.]Google Scholar
Black, R. F. Ice-wedge casts of Wisconsin. Transactions of the Wisconsin Academy of Sciences, Arts and Letters, Vol. 54, 1965, p. 187–222. [Description of these features and their locations, discussion of mode and time of formation and their palaeoclimatological significance.]Google Scholar
Black, R. F. Bowser, C. J. Patterned ground studies in Victoria Land. Antarctic Journal of the U.S., Vol. 2, No. 4, 1967, p. 116–18. [Studies to define the environment of sand and ice wedges and to determine their rate of growth for dating of various surfaces.]Google Scholar
Brown, R. J. E. Comparison of permafrost conditions in Canada and the USSR. Polar Record, Vol. 13, No. 87. 1967, p. 741–51. [Despite the disparity in knowledge of permafrost conditions in the two countries, it is clear that significant differences do exist.]CrossRefGoogle Scholar
Cailleux, A. Actions du vent et du froid entre le Yukon et Anchorage, Alaska. Geografiska Annaler, Vol. 49a, Nos. 2–4, 1967, p. 145–54. [Observations on the influence of wind and frost action, made during the INQUA field trip in Alaska in 1965, reported, discussed and compared with examples from other areas.]CrossRefGoogle Scholar
Chambers, M. J. G. Investigations of patterned ground at Signy Island, South Orkney Islands. III. Miniature patterns, frost heaving and general conclusions. British Antarctic Survey Bulletin, No. 12, 1967, p. 1–22. [Experiments on development of these features.]Google Scholar
Couvreur, G. Les formations périglaciaires du Haut Atlas central marocain. Revue de Géographie de Maroc, No. 10, 1966, p. 47–50. [Quaternary and present periglacial processes described. Importance of aspect and nature of rocks.]Google Scholar
Dahl, R. Block fields and other weathering forms in the Narvik mountains. Geografska Annuler, Vol. 48a, No. 4, 1966, p. 224–27. [Reply to criticism by Ives, ibid., Vol. 48a, No. 4, p. 220–23.]CrossRefGoogle Scholar
Danilova, N. S. Obrazovaniye tonkikh ledyanykh zhil i psevdomorfoz no nim v peschanom allyuvii del’ty r. Leny . Vestnik Moskovskogo Universiteta. Seriya 5 , God 21, [No.] 6, 1966, p. 108–11.Google Scholar
Dikinov, Kh. Zh. Raschet glubiny promerzaniya pochvy, pokrytoy snegosn, po zadannoy temperature vozdukha . Izvestiya Akademii Nauk SSSR. Fizika Atmosfery i Okeana , Tom 3, No. 6, 1967, p. 602–10. [Numerical solution of equations. Results compared with observations. English summary.]Google Scholar
Dylik, J. Solifluxion, congelifluxion and related slope processes. Geografiska Annuler, Vol. 49a, Nos. 2–4, 1967. p. 167–77.CrossRefGoogle Scholar
Dylik, J. Traces fossiles de l’évolution descendante des polygones des fentes de gel. Tijdschrift van het koninklijk Nederlandsch Aardrijkskundig Genootschap, Deel 83, No. 3, 1966, p. 227–37. [Discussion of what can be learnt by studying fossil frost-wedge polygons.]Google Scholar
Everett, K. R. Mass-wasting in the Tasersiaq area, West Greenland. Meddelelser ove Gronland, Bd. 165, Nr. 5, 1967, 31 p. [Description of geology and geomorphology of this area marginal to Sukkertoppen Iskappe with special emphasis on mass-wasting processes including solifluction and slumping.]Google Scholar
[Frozen Ground: Canada.] Permafrost in Canada. Canada. Geological Survey. Dept. of Energy, Mines and Resources. Map 1246A, 1967. [Scale 1: 7 603 200.] 50 c. [Shows extent of continuous and discontinuous permafrost zones and occurrence of permafrost at high elevations, with other data. Explanatory notes on definition of permafrost, distribution and occurrence, physical factors influencing permafrost and a bibliography of source information are printed on the map.]Google Scholar
Gabert-Delay, J. L’importance des déformations quaternaires et du modelé cryonival würmien dans les paysages du bas Rhône et de la basse Durance. Méditerranée. Revue Géographique des Pays Méditerranéens, 8e An., No. 2, 1967, p. 87–107. [Importance of Quaternary deformations and periglacial processes in the Würm period in landform development of this region of southern France.]Google Scholar
Hoekstra, P. Conductance of frozen bentonite suspensions. Proceedings. Soil Science Society of America, Vol. 29, No. 5, 1965, p. 519–22. [Evidence for films of unfrozen water on clay particles in frozen soil.]CrossRefGoogle Scholar
Holdgate, M. W., and others. A preliminary investigation of the soils of Signy Island, South Orkney Islands, by M. W. Holdgate, S. E. Allen and M. J. G. Chambers. British Antarctic Survey Bulletin, No. 12, 1967, p. 53–71. [Mechanical break-down of rock by frost action is proceeding rapidly and solifluction processes are influencing the upper layers of the ground on a large scale.]Google Scholar
Ives, J. D. Block fields, associated weathering forms on mountain tops and the nunatak hypothesis. Geografuka Annaler, Vol. 48a, No. 4, 1966, p. 220–23. [Criticism of paper by Dahl, ibid., Vol. 48a, No. 2, 1966, p. 55–85.1CrossRefGoogle Scholar
Juusela, T. Some results of field observations on the frost phenomenon on peat soil. Journal of Hydrology (Amsterdam), Vol. 5, No, 3, 1967, p. 269–78. [Measurement of frost depth and moisture content throughout the winter.]CrossRefGoogle Scholar
Klyuyev, Ye. V. Proyavleniye termokarsta na doe morya Laptevykh . Problemy Arktiki i Antarktiki , Vyp. 23, 1966, p. 26–32.Google Scholar
Lewin, J. Fossil ice wedges in Hampshire. Nature, Vol. 211, No. 5050, 1966, p. 728. [Description of forms and suggested date.]CrossRefGoogle Scholar
Liestøl, O. Lokalt omráde med permafrost i Gudbrandsdalen. Norsk Polarinstitutt. Årbok, 1965 [pub. 1966], p. 129–33. [Small local permafrost area discovered near Otta in Gudbrandsdalen, central Norway, in 1965. English summary.]Google Scholar
McCraw, J. D. Some surface features of McMurdo Sound region, Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 10, No. 2, 1967, p. 394–417. [Description of rock weathering, debris movement, glacial and fluvioglacial deposits, and patterned ground.]CrossRefGoogle Scholar
Mackay, J. R. Permafrost depths, lower Mackenzie Valley, Northwest Territories. Arctic, Vol. 20, No. 1, 1967, p. 21–26. [Measurements at 7 new sites and discussion.]CrossRefGoogle Scholar
McManus, J. An ice-wedge and associated phenomena in the Lower Limestone series of Fife. Scottish Journal of Geology, Vol. 2, No. 3, 1966, p. 259–64. [Description of fossil ice wedge.]CrossRefGoogle Scholar
Rougerie, M. G. Filiation de sols figurés au Spitzberg nord-occidental. Bulletin de l’ Association de Géographes Français, No. 346–47, 1966, p. 32–40. [Study of possible relationship between different forms of frost action on superficial deposits at Kvadehuken, Vestspitsbergen.]CrossRefGoogle Scholar
Shmelev, L. M. Proiskhozhdeniye plastovykh zalezhey podzemnogo Pda v nizov’yakh r. Yeniseya . Izuestiya Akademii Nauk SSSR. Seriya Geografcheskaya , 1967, No. 2, p. 108–15.Google Scholar
Tedrow, J. C. F. Polar desert soils. Proceedings. Soil Science Society of America, Vol. 30, No. 3, 1966, p. 985–87. [Review of physical conditions in high Arctic, resulting soils and patterned ground.]CrossRefGoogle Scholar
Tedrow, J. C. F. Ugolini, F. C. Antarctic soils. (In Tedrow, J. C. F., ed. Antarctic soils and soil forming processes. Washington, D.C., American Geophysical Union, 1966, p. 161–77. (Antarctic Research Series, Vol. 8.)) [Description of weathering processes and resulting soil types.]CrossRefGoogle Scholar
Tolstikhin, O. N. Pritok vody of naledey v basseyne r. Indigirki . Meteorologiya i Gidrologiya , 1966, No. 9, p. 17–22. [Observations of volume of run-off from giant ice-mounds.]Google Scholar
Williams, P. J. Downslope soil movement at a sub-arctic location with regard to variations with depth. Canadian Geotechnical Journal, Vol. 3, No. 4, 1966, p. 191–203. [Soil movements resulting from solifluction were investigated at Schefferville, P.Q., variation of movement with depth below surface being specially considered.]CrossRefGoogle Scholar

Meteorological and Climatological Glaciology

Browning, K. A. Hailstones breaking in mid-air. Weather, Vol. 22, No. 8, 1967, p. 331–34. [A small but significant proportion of hailstones may break up in mid-air by natural causes.]CrossRefGoogle Scholar
Hitschfeld, W. Stauder, M. The temperature of hailstones. Journal of the Atmospheric Sciences, Vol. 24, No. 3, 1967, p. 293–97. [Theoretical study shows hailstones ‘o rum in radius may be c. 12 deg colder than surrounding air.]2.0.CO;2>CrossRefGoogle Scholar
Knollenberg, R. G. Urea as an ice nucleant for supercooled clouds. Journal of the Atmospheric Sciences, Vol. 23, No. 2, 1966, p. 197–201. [Laboratory and field tests.]2.0.CO;2>CrossRefGoogle Scholar
Kupetskiy, V. N. O prichinakh teplovoy asimmetrii Antarktiki . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva , Tom 98, Vyp. 2, 1966, p. 130–37. [Discusses cause of asymmetry of Antarctic ice sheet and surrounding oceans,]Google Scholar
Sansom, H. W. A possible effect of lightning on hail. Weather, Vol. 21, No. 9, 1966, p. 315. [Evidence for hailstone softening by shock wave from lightning flash.]CrossRefGoogle Scholar
Starr, J. R. Mason, B. J. The capture of airborne particles by water drops and simulated snow crystals. Quarterly Journal of the Royal Meteorological Society, Vol. 92, No. 394, 1966, p. 490–99. [Experiments with paper models of snow crystals on capture of pollen grains.]CrossRefGoogle Scholar
Weyant, W. S. The Antarctic climate. (In Tedrow, J. C. F. ed. Antarctic soils and soil forming processes. Washington, D.C., American Geophysical Union, 1966, p. 47–59. (Antarctic Research Series, Vol. 8.)) [General description of three broad climatic zones.]Google Scholar
Whitehurst, C. A. A survey of research efforts in heat transfer through frost formation. ASHRAE Journal (New York), Vol. 8, No. 10, 1966, p. 50–55. [Survey of abstracts and paraphrases. Recommendations for future research.]Google Scholar

Snow

Isono, K., and others. A physical study of solid precipitation from convective clouds over the sea: part I, by K. Isono, M. Komabayashi and T. Takahashi. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 44, No. 3, 1966, p. 178–84. [Deuterium content of snow crystals with respect to crystal shapes and their relation to origins of the water vapour of snowfall.]Google Scholar
Isono, K., and others. A physical study of solid precipitation from convective clouds over the sea: part II, by K. Isono, M. Komabayashi, T. Takahashi and T. Tanaka. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 44, No. 4, 1966, p. 258–26. [Relation between ice nucleus concentration and precipitation.]Google Scholar
Isono, K., and others. A physical study of solid precipitation from convective clouds over the sea: part III, by K. Isono, M. Komabayashi [and] T. Takahashi.,Journal of the Meteorological Society of Japan, Ser. 2, Vol. 44, No. 4, 1966, p. 227–33. [Measurement of electric charge of snow crystals.]Google Scholar
Isono, K., and others. A physical study of solid precipitation from convective clouds over the sea: part IV, by K. Isono, M. Komabayashi, T. Takahashi and T. Gonda. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 44, No. 6, 1966, p. 308–19. [Importance of giant sea salt nuclei in formation of solid precipitation.]Google Scholar
Kaisergruber, F. Eine merkwürdige Schneeform (“Schneerollen”). Wetter and Leben, Bd. 17, Ht. 3–4, 1965, p. 67–68. [Description of curious toroidal form.]Google Scholar
Magono, C. Kikuchi, K. On the positive electrification of snow crystals in the process of their melting (II). Journal of the Meteorological Society of Japan, Ser. 2, Vol. 43, No. 6, 1966, p. 331–42. [Measurement of charge on snow crystals in process of melting.]Google Scholar
Magono, C. Nakamura, T. Aerodynamic studies of falling snowflakes. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 43, No. 3, 1965, p. 139–47 [Simultaneous observations of fall velocity, size and mass.]Google Scholar
Martinelli, M. jr. Avalanche technology and research: recent accomplishments and future prospects. Weatherwise, Vol. 19, No. 6, 1966, p. 270–71. [Including current avalanche control and forecasting techniques.]CrossRefGoogle Scholar
Ōura, H. Kobayashi, D. Sektsetsu no ryūdo bumpu no motomekata ni tsuite . Teion-kagaku , Ser. A, Vol. 24, 1966, p. 139–57. [Determination from microphotographs of cross-sections of snow cover. English extended summary p. 155–57.]Google Scholar
Pitman, D. Zuckerman, B. Effective thermal conductivity of snow at −88°, −27°, and −5°C. Journal of Applied Physics, Vol. 38, No. 6, 1967, p. 2698–99. [Measurements of conductivity of “snow” made from dendritic frost crystals with density from 0.1 to 0.6 g cm−3. Comparison with previous work and theory.]CrossRefGoogle Scholar
Rakita, S. A. Vliyaniye rastitel’nosti na perenos i otlozheniye snega v gorakh basseyna Kolymy . Vestnik Moskovskogo Universiteta. Seriya 5 , God 21, [No.] 3, 1966, p. 103–07.Google Scholar
Roch, A. Fraser, C. How to estimate avalanche danger. Alpine Journal, Vol. 72, No. 314, 1967, p. 87–94.Google Scholar
Stow, C. D. The generation of electricity by blowing snow. Weather, Vol. 23, No. 9, 1967, p. 371–77. [Three types of interaction, all involving the temperature-gradient effect, are primarily responsible for the observed electrification.]CrossRefGoogle Scholar
Thom, H. C. S. Distribution of maximum annual water equivalent of snow on the ground. Monthly Weather Review, Vol. 94, No. 4, 1966, p. 265–71. [Study of statistical distribution.]2.3.CO;2>CrossRefGoogle Scholar
Tushinskiy, G. K., and others. Karta lavinoopasnykh rayonov SSSR . Vestnik Moskovskogo Universiteta. Seriya 5 , God 22, [No.] 1, 1967, p. 3–14.Google Scholar
Wilken, G. C. Snow accumulation in a manzanita brush field. Water Resources Research, Vol. 3, No. 2, 1967, p. 409–22. [Study of how snow accumulates in areas of Sierra Nevada, U.S.A., covered by this shrub.]CrossRefGoogle Scholar
Zanin, G. V. Snezhnye melioratsii i geomorfologicheskiye protsessy . Izvestiya Akademii Nauk SSSR. Seriya Geograficheskaya , 1966, No. 3, p. 49–51.Google Scholar