Hostname: page-component-78c5997874-94fs2 Total loading time: 0 Render date: 2024-11-10T08:00:19.326Z 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 5 , Issue 42 , 1965 , pp. 883 - 891
Copyright
Copyright © International Glaciological Society 1965

This is a selected list of glaciological literature on 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

Crary, A. P. Recent U.S. scientific research in Antarctic– Part I. Activities and preliminary findings of field programs during austral summer 1963–64. Transactions. American Geophysical Union, Vol. 45, No. 4, 1964, p. 719–26; 1G Bulletin (Washington, D.C.), No. 88, 1964, p. 15–22. [Glaciological research by various U.S. bodies in Antarctica described, p. 725–26.]Google Scholar
Grötzbach, E. Hillebrandt, A. Von. Die rezente und eiszeitliche Vergletscherung im mittleren Khwāja Muhammad-Gebirge. (In Münchner Hindukvsch-Kundfahrt 1963. Verlatf, wissenschaftliche und bergsteigerische Ergebnisse. München, Akademischen Sektion München des Deutschen Alpenvereins, 1964, p. 26–31.) [General description, also periglacial phenomena of the recent and Ice Age glacierizations in the central Khwāja Muhammad ranges.]Google Scholar
Grosval’d, M. G. Sukhodrovskiy, V. L. Some results of glaciological investigations on the territory of the U.S.S.R. according to the I.G.ϒ. program. Translations of various articles appearing in Opisareiye ob’yektou glyatsiologicheskikkh rsledavaniy, provedennykh po programme Mezhdunarodnoga Geofizicheskago Goda na territorii Sovietskogo Soyuza (Description of subjects of glaciological investigations conducted on the territory of the Soviet Union under the I.G.Y. program), Moscow, 1938, p. 4–18, 19–41, 42–56, 139–160. Washington, D.C., U.S. Department of Commerce, 1960. 60 p.Google Scholar
Haefeli, R. Kommentar, Spezifikation und Ergänzungen zum generellen Arbeitsprogramm von 25. September 1963 für die 2. Expedition 1966. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 9e An., No. 3, 1964, p. 5–11. [Aims, supplies, budget etc. and programme of work from 25 Sept. 1963 for 2nd international glaciological expedition to Greenland 1966.]Google Scholar
Hofmann, W. Richard Finsterwalder und die Alpenvereinskartographie. Jahrbuch des Österreichischen Alpenvereins, Bd. 89, 1964, p. 132–37. [Description of Finsterwalder’s many–sided interests and work in the mountains.]Google Scholar
Lorius, C. Contribution à la connaissance de l’Antarctique: glaciologie en Terre Adélie (1956–1959), Année Géophysique Internationale. Participation Française, Sér. 9, Fasc. 1, 1964, 101 p. [Analysis of glaciological observations in Terre Adélie 1956–59 during French I.G.Y. expeditions.]Google Scholar
SirPriestley, R. E., and others, ed. Antarctic research: a review of British scientific achievement in Antarctica. Edited by SirPriestley, R. [E.] Adie, R. J. Robin, G. de Q.. London, Butterworths, 1964. xii, 360 p. [Contents include: Sir R. [E.] Priestley, “The background”, p. 1–15; Sir V. [E.] Fuchs, “Polar travel”, p. 16–27; D. L. Linton, “Landscape evolution”, p. 85–99; G. de Q. Robin and R. J. Adie, “The ice cover”, p. 100–17; R. J. Adie, “Geological history”, p. 118–62; G. de Q. Robin, “International co–operation and geophysics”, p. 254–64; H. H. Lamb, “Circulation of the atmosphere”, p, 265–77; H. H, Lamb, “The climate”, p. 278–91; G. E. R. Deacon, “The Southern Ocean”, p. 292–307; J, A. Heap, “Pack ice”, p. 308–17.]Google Scholar
Roberts, B. B. Gazetteer of the British Antarctic Territory, South Georgia and the South Sandwich Islands. First supplement to first edition. London, H.M. Stationery Office, 1964. 4 p. [196 new names with alterations and corrections.]Google Scholar
Rutsch, R. F. Grindelwald, Wiege der experimentellen Gletscherforschung. Les Alpes. Revue du Club Alpin Suisse, 38e An., 1er Trimestre. 1962, p. 49–50.Google Scholar
Ya-Feng, Shih Tzu-Hsiu, Chi Scientists study Mount Shisha Pangma. China Reconstructs, Vol. 14, No. 3, 1965, p. 19–23. [One of the centres of present glaciation in the Himalaya.]Google Scholar
Troll, C. Richard Finsterwalders Lebenswerk und die geographische Hochgebirgsforschung. Allgemeine Vermessungsnachrichten, Jahrg. 71, Ht.11, 1964, p. 398–404. [Account of Richard Finsterwalder’s work and his geographical researches in the high mountains of the world.]Google Scholar
Yoshida, A. Suzuki, T. Map compilation for coastal region between 37° and 45° E. Antarctic Record (Tokyo), No. 23, 1964. p. 32–41. [Compilation of 8 colour maps scale 1:250,000 of “Lützow–Holm Bay” and “Prince Olav Coast”, Dronning Maud Land. In Japanese with English abstract and captions.]Google Scholar

Glaciological Instruments and Methods

Bogorodskiy, V. V. Sovremennyye fizicheskiye sposoby izmereniya tolshchiny morskikh l’dov . Okeanologiya , Tom 3, Vyp. 4, 1963, p. 720–30. [Electric, ultrasonic and electromagnetic close-contact methods; seismic-acoustic and electromagnetic remote methods discussed and compared.]Google Scholar
Buck, B. M. Ice drilling in Fletcher’s Ice Island (T–3) with a portable mechanical drill. Arctic, Vol. 18, No. 1, 1965, p. 51–54.CrossRefGoogle Scholar
Cheremnykh, G. D. Novoye v izmerenii skorostey dvizheniya l’da v poverkhnostnykh chastyakh lednikov po materialam aeros”yemki . Geodeziya i Aerofotos”yemka, No. 5, 1962, p. 111–15. [Discussion of techniques and accuracy. English translation, Geodesy and Aerophotography, No. 5, 1962 [pub. 1963], p. 342–44.]Google Scholar
Konovalov, V. G. A method of measuring ablation of a glacier. Soviet Hydrology. Selected Papers, 1963, No. 2, p. 201–04. [Method based on collecting melt water from sample area.]Google Scholar
Langway, C. C. jr., and others. Sampling Polar ice for radiocarbon dating, [by] C. C. Langway, Jr., Hans Oeschger, Bernhard Alder [and] André Renaud., Nature, Vol. 206, No. 4983, 1965, p. 500–01. [Letter. Joint research by U.S. Cold Regions Research and Engineering Laboratory, Swiss Gletscherkommission and Universität Bern, using a highly sensitive low-level counting device.]Google Scholar
McLerran, J. H. Airborne crevasse detection. Proceedings of the third symposium on remote sensing of environment, 14, 15, 16 October 1964 (Ann Arbor, University of Michigan. Institute of Science and Technology), 1965, p. 801–02. [Feasibility of aerial detection of snow-bridged crevasses by infrared sensing.]Google Scholar
McLerran, J. H. Infrared sea ice reconnaissance. Proceedings of the third symposium on remote sensing of environment, 14, 15, 16 October 1964 (Ann Arbor, University of Michigan. Institute of Science and Technology), 1965, p. 789–99. [Interpretation of illustrations of infra-red images of sea ice; applications and limitations discussed briefly.]Google Scholar
Nezami, M., and others. Mesure du taux d’accumulation de la neige au bord du continent antarctique par la méthode du plomb 210, par M. Nezami, G. Lambert, C. Lorius et J. Labeyrie. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 259, No. 19, 1964, p. 3319–22. [Measurement of rate of accumulation of snow in Terre Adélie by means of 210Pb.]Google Scholar
Rinker, J. N. Radio echo sounding and strain rate measurement in the ice sheet of north-west Greenland: 1964. Polar Record, Vol. 12, No. 79, 1965, p. 403–05. [Results of measurements briefly reported. Future use of ice depth determination by radar discussed.]Google Scholar
Savel’yev, B. A. Rukovodstvo po izucheniyu suoystv l’da . Moscow, Izdatel’stvo Moskovskoga Universiteta [Publishing House of Moscow University], 1963. 198 p. [Properties of ice and how to determine them in laboratory and field.]Google Scholar
Shvayshteyn, Z. I. Poluprovnikovyy solemer dlya izmereniya solenosti morskogo l’da . Problemy Arktiki i Antarktiki , Vyp. 15, 1964, p. 85–87.Google Scholar

Physics of Ice

Barnes, G. T., and others. Ice forming activity and the surface properties of nucleating materials, [by] G. T. Barnes, U. Katz and R. Sänger., Zeitschrift für angewandte Mathematik and Physik, Vol. 13, Fasc. 1, 1962, p. 76–80. [Theoretical study of physics of nucleation.]Google Scholar
Bennett, J. E., and others. Electron spin resonance spectra of hydrated electrons prepared by reaction of atomic sodium with ice at 77° K, [by] J. E. Bennett, B. Mile [and] A. Thomas., Nature, Vol. 201, No. 4922, 1964, p. 919–20. [Letter. Results allow state of this defect in ice to be analysed.]Google Scholar
Bertie, J. E. Whalley, E. Infrared spectra of ices Ih and Ic in the range 4000 to 350 cm–1’. Journal of Chemical Physics, Vol. 40, No. 6, 1964, p. 1637–45. [Observations and discussion. No detectable difference between hexagonal and cubic ice.]Google Scholar
Bertie, J. E. Whalley, E. Infrared spectra of ices II, III and V in the. range 4000 to 350 cm–1’. Journal of Chemical Physics, Vol. 40, No. 6, 1964, p. 1646–59. [Observations and interpretation in terms of structure.]Google Scholar
Bertie, J. E., and others. Transformations of ice II, ice III, and ice V at atmospheric pressure, [by] J. E. Bertie, L. D. Calvert and E. Whalley. Journal of Chemical Physics, Vol. 38, No. 4, 1963, p, 840–46. [All these high-pressure phases transform first to cubic ice on heating from liquid nitrogen temperature.]Google Scholar
Bigg, E. K. Miles, G. T. The results of large-scale measurements of natural ice nuclei. Journal of the Atmospheric Sciences, Vol. 21, No. 4, 1964, p. 396–403. [Australian data used to show probable extra-terrestrial source of many nuclei.]Google Scholar
Blicks, H., and others. Zur Verteilung von Fremdsubstanzen in Eis-Einkristallen, von H. Blicks, H. Egger and N. Riehl. Physik der kondensierten Materie, Bd. 2, Ht. 5, 1964, p. 419–22. [Study of radial distribution of HF and NH4F in ice grown from dilute solutions.]Google Scholar
Camp, P. R. Barter, C. F. An electrical effect un the growth of ice crystals. Nature. Vol. 200, No. 4904, 1963, p. 350–51. [Letter. Presence of electric field affects grain size and shape of ice frozen from water.]Google Scholar
Camp, P. R. Barter, C. F. Rate of growth of ice at an aluminium-water interface. Nature, Vol. 206, No. 4983, 1965, p. 495–97. [Letter. At least two different modes of growth occurred depending on the amount of supercooling and the manner of nucleation.]Google Scholar
Child, W. C. jr. Thermodynamic functions for metastable ice structures I and II. Journal of Physical Chemistry, Vol. 68, No. 7, 1964, p. 1834–38. [Reanalysis of data on free energies.]Google Scholar
Dean, J. W. Timmerhaus, K. D. Thermal conductivity of solid H2O and D2O at low temperatures. Advances in Cryogenic Engineering, Vol. 8, 1962, p. 263–67. [Measurements at liquid hydrogen and liquid nitrogen temperatures.]Google Scholar
Dengel, O. Riehl, N. Diffusion von Protonen (Tritonen) in Eiskristallen. Physik der kondensierten Materie, Bd. 1, Ht. 3, 1963, p. 191–96. [Diffusion of 3H in ice measured. Activation energy consistent with that for dielectric and mechanical relaxation.]Google Scholar
Dengel, O., and others. Ferroelectric behaviour of ice, [by] O. Dengel, U. Eckener, H. Plitz and N. Riehl. Physics Letters, Vol. 9, No. 4, 1964, p. 291–94. [Ferroelectricity observed below 100°K. provided water from which ice was made was not extremely pure.]CrossRefGoogle Scholar
DiMarzio, E. A. Stillinger, F. H. jr. Residual entropy of ice. Journal of Chemical Physics, Vol. 40, No. 6, 1964, p. 1577–81. [Calculation.]Google Scholar
Dinger, J. E. Electrification accompanying melting of ice and snow. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 384, 1964, p. 208–09. [Correspondence relating to use of artificially made snow arising out of article by J. B. Matthews and B. J. Mason, ibid., Vol. 89, No. 381, 1963, p. 376–80. Reply by Mason and Matthews, p. 208–09.]Google Scholar
Dooley, D. Observations on the deformation of ice at low stresses. Ohio State University Institute of Polar Studies. Report No. 12, 1964, [ii, 16] p. [Single crystals and polycrystalline ice.]Google Scholar
Eisenberg, D. Coulson, C. A. Energy of formation of D-defects in ice. Nature, Vol. 199, No. 4891, 1963, p. 368–69. [Comparison of total energies of formation of D- and X-defects.]Google Scholar
Giguère, P. A. Arraudeau, J. P. Spectres d’absorption de trois formes allotropiques de la glace dans l’infrarouge lointain. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 257, No. 10, 1963, p. 1692–94. [Similarities in far infrared absorption spectra of vitreous, cubic and hexagonal ice.]Google Scholar
Gränicher, C. Properties and lattice imperfections of ice crystals and the behaviour of H2O–HF solid solutions. Physik der kondensierten Materie, Bd. 1, Ht. 1, 1963, p. 1–12. [A review article dealing with electrical, acoustic and nuclear magnetic resonance properties of ice and their interpretation.]Google Scholar
Haas, C. On diffusion, relaxation and defects in ice. Physics Letters, Vol. 3, No. 3, 1962, p. 126–28. [Suggests mechanism for electrical and mechanical relaxation and diffusion of oxygen in ice.]Google Scholar
Harrison, J. D. Solute transpiration pores in ice. Journal of Applied Physics, Vol. 36, No. 1, 1965, p. 326–27. [Letter. Observation of pores developed when freezing solutions and theory of their formation.]Google Scholar
Hayes, C. E. Webb, W. W. Dislocations in ice. Science, Vol. 147, No. 3653, 1965, p. 44–45. [X-ray diffraction topography shows Burgers vectors of slip dislocations to have <1120>directions.]Google Scholar
Heinmets, F. Blum, R. Conductivity measurements on pure ice. Transactions of the Faraday Society, Vol. 59, No. 5, 1963, p. 1141–46. [Results give activation energy of 24.2 kcal. for proton transfer.]Google Scholar
Higashi, A., and others. Plastic yielding in ice single crystals, [by] A. Higashi, S. Koinuma and S. Mae. Japanese Journal of Applied Physics, Vol. 3, No. 10, 1964. p. 610–16. [Constant strain-rate tests. No work hardening found. Activation energy consistent with Johnston’s dislocation theory.]Google Scholar
Hollins, G. T. Configurational statistics and the dielectric constant of ice. Proceedings of the Physical Society, Vol. 84, Pt. 6, 1964, p. 1001–16. [Theoretical study.]Google Scholar
Itagaki, K. SeIf-diffusion in single crystals of ice. journal of the Physical Society ofjapan, Vol. 19, No. 6, 1964, p. 1081. [Measurements of activation energy and of D 0. Time variation found and discussed. No anisotropy observed.]Google Scholar
Jaccard, C. Thermodynamics of irreversible processes applied to ice. Physik der kondensierten Materie, Bd. 3, Ht. 2, 1964, p. 99–118. [Calculation of entropy production and resulting thermoelectric effects.]Google Scholar
Jaccard, C. Thermoelectric effects in ice crystals. I. Theory of the steady state. Physik der kondensierten Materie, Bd. 1, Ht. 2, 1963, p. 143–51. [Theory starting from equations for ice defects.]Google Scholar
Jackson, J. A. Rabideau, S. W. Deuteron magnetic resonance in polycrystalline heavy ice (D2O). Journal of Chemical Physics, Vol. 41. No.12, 1964, p. 4008. [Letter. Measurements reported and discussed.]Google Scholar
Joss, J. List, R. Zur Radarrückstrahlung von Eis-Wasser-Germischen. Zeitschrift für angewandte Mathematik und Physik, Vol. 14, Fasc. 4, 1963, p. 377–80. [Radar experiments on back-scattering of spherical ice particle.]Google Scholar
Kamb, W. B. Ice II: a proton-ordered form of ice. Acta C.ryslallographica, Vol. 17, Pt, 11, 1964, p. 1437–49. [X-ray structure determination and discussion.]Google Scholar
Kamb, W. B. Davis, B. L. Ice VII, the densest form of ice. Proceedings of the National Academy of Sciences of the United States of America, Vol. 52, No. 6, 1964, p. 1433–39. X-ray structure determination shows ice VII to have body–centred cubic structure.]Google Scholar
Kevan, L., and others. Formation of electrons and of atomic hydrogen in y-irradiated ice, by L. Kevan, P. N. Moorthy and J. J. Weiss. Nature, Vol. 199, No. 4894, 1963, p. 689–90.Google Scholar
Larsson, K. E. Dahlborg, U. Some vibrational properties of solid and liquid H2O and D2O derived from differential cross-section measurements. Journal of Nuclear Energy, Parts A and B, Vol. 16, No. 2, 1962, p. 81–89. [Neutron measurements used to deduce phonon frequency spectra.]Google Scholar
Latham, J. The electrification of freezing water drops. Quarterly Journal of the Royal Meteorological Society, Vol, 90, No. 384, 1964, p. 209–11. [Correspondence arising out of article by D. G. Evans and W. C. A. Hutchinson, ibid., Vol. 89, No. 381, 1963, p. 370–75. Reply by W. C. A. Hutchinson, p. 211.]Google Scholar
Levi, L., and others. Electrical conductivity and dissociation constants in ice doped with HF and NH, in different ratios, by L. Levi, O. Milman and E. Suraski. Transactions of the Faraday Society, Vol. 59, No. 9, 1963, p. 2064–75. [Measurements suggest lower conductivity and ion mobilities in purr ice than previously assumed.]Google Scholar
Levi, L., and others. Thermal etching on ice crystals, by L. Levi, S. M. de De Michcli and L. Lubart. Physica Status Solidi, Vol. 4, No. 1, 1964, p. 63–70. [Facets found in pure ice but not ice doped with NaCI.]CrossRefGoogle Scholar
McMillan, J. A. Los, S. C. Vitreous ice: irreversible transformations during warm-up. Nature, Vol. 206, No. 4986, 1965, p. 807–07. [Observation of glass transformation and of change to cubic and finally hexagonal ice and measurement of heats of transformation.]Google Scholar
Magnan, D. Kahane, A. Conductivité de la glace aux basses températures. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 256, No. 26, 1963, p. 5539–41. [Electrical conductivity measurements at −80° to −120°C. and high fields indicate a space-charge-limited proton current.]Google Scholar
Onsager, L. Runnels, L. K. Mechanism for self-diffusion in ice. Proceedings of the National Academy of Sciences of the United States of America, Vol. 50, No. 2, 1963, p. 208–10. [Evidence for interstitial molecule mechanism.]Google Scholar
Pascalar, H. G. Sakamoto, R. T. Microwave radiometric measurements of ice and water. Proceedings of the third symposium on remote sensing of environment, 14, 15, 16 October 1964 (Ann Arbor, University of Michigan. Institute of Science and Technology), 1965, p. 803–11. [Description of an experiment of ice measurements with a passive microwave radiometer, equipment used and data obtained. Possible utility of microwave radiometry in various ice applications is indicated.]Google Scholar
Pistorius, C. W. T., and others. Melting curve of ice VII to 200 kbar, [by] C. W. T. Pistorius, M. C. Pistorius, J. P. Blakey and L. J. Admiraal. Journal of Chemical Physics, Vol. 38, No. 3, 1963, p. 600–02. [Follows melting curve up to 442°C.]Google Scholar
Rabideau, S. W. Jackson, J. A. Low temperature observation of oxygen–17 NMR in H2O, D2O, and eutectic solutions. Journal of Chemical Physics, Vol. 41, No. 11, 1964, p. 3405–07. [No signals observed in pure solids.]CrossRefGoogle Scholar
Sano, I., and others. Adsorption studies on the mechanism of ice nucleation, [by] I Sano, N. Fukuta, Y. Kojima [and] T. Murai. Journal of the Meteorological Society of japan, Ser. 2, Vol. 41, No. 4, 1963, p. 189–96. [Relation between adsorption measurements and nucleation.]Google Scholar
Sitharamarao, D. N. Duncan, J. F. Molecular excitation of water by y-irradiation. journal of Physical Chemistry, Vol. 67, No. 10, 1963, p. 2126–32. [Study of thermoluminescence and fluorescence of y-irradiated ice.]Google Scholar
Taylor, M. J. Whalley, E. Raman spectra of ices Ih, Ic, II, III, and V. Journal of Chemical Physics, Vol. 40, No. 6, 1964, p. 1660–64. [Observations and discussion.]Google Scholar
Townsend, A. A. Natural convection in water over an ice surface. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 385, 1964, p. 248–59; Vol. 91, No. 388, 1965, p. 243–45. [Laboratory observation of motions set up in water with upper surface at 25°C. and bottom surface of ice. Discussion printed in later issue.]Google Scholar
Waldstein, P., and others. Nuclear magnetic resonance of single crystals of D2O ice, by P. Waldstein, S. W. Rabideau and J. A. Jackson. Journal of Chemical Physics, Vol. 41, No. 11, 1964, p. 3407–11. [Measurements of deuteron magnetic resonance used to estimate hydrogen-bond energies.]CrossRefGoogle Scholar

Land ice. Glaciers. Ice shelves

Aitkenhead, N. Ice calderas. British Antarctic Survey Bulletin, Vol. 1, No. 5, 1965, p. 63–64. [Letter. Suggestions regarding nomenclature; see also Stokes, J., below.]Google Scholar
Aliverti, G. Glaciologia. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 11, Pt. 1, 1962, [pub.] 1964, supplement, 50 p. [Account of glaciers, their structure and flow, and of current theories.]Google Scholar
Andrews, J. T. Webber, P. J. A lichenometrical study of the northwestern margin of the Barnes Ice Cap: a geomorphological technique. Geographical Bulletin (Ottawa), No. 22, 1964, p. 80–104. [Use to date moraines back to 1680.]Google Scholar
Angino, E. E., and others. Ionic content of Antarctic ice samples, by E. E. Angino, K. B. Armitage and J. C. Tash. Polar Record, Vol. 12, No. 79, 1965, p. 407–09. [Results of analysis of chemical composition of samples of glacier ice, melt water and lake water.]Google Scholar
Ardus, D. A. Morphology and regime of the Brunt Ice Shelf and the adjacent inland ice, 1960–61. British Antarctic Survey Bulletin, No. 5, 1965, p. 13–42. [At present the glacierization of the area appears to be in equilibrium. Precipitation is discussed.]Google Scholar
Astori, V. Togliatti, G. II rilievo areofotogrammetrico del Ghiacciaio Pian di Neve. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 11, Pt. 1, 1962, [pub.] 1964, p. 33–50. [Survey, plotting and drawing of map, scale 1:5,000, of Ghiacciaio Pian di Neve in the massif of Adamello.]Google Scholar
Bardin, V. I. Oledeneniye Zemli Korolevy Mod . Rezul’toy Issledovaniy po Programme Mezhdunarodnogo Ceofizicheskogo Goda. Glyatsiologiya. IX Razdel Programmy MGG , No. 13, 1964, p. 19–25.Google Scholar
Black, R. F., and others. Saline discharge from Taylor Glacier, Victoria Land, Antarctica, [by] R. F. Black, M. L. Jackson and T. E. Berg. Journal of Geology, Vol. 73, No. 1, 1965, p. 175–81. [Analysis and discussion of origin.]Google Scholar
Buynitskiy, V. Kh. Dvizhenlye i balans massy shel’fovykh l’dov Antarktiki . Vestnik Leningradskogo Universiteta , 1964, No. 6, p. 57–70.Google Scholar
Carabelli, E. Esplorazione geofisica al Ghiacciaio del Careser. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 11, Pt. 1, 1962, [pub.] 1964, p. 61–68. [Geophysical examination of Ghiacciaio del Careser, including exploration of ice thickness.]Google Scholar
Carabelli, E. Misure sismiche di spessore del Ghiacciaio del Pian di Neve (Adamello). Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 11, Pt. 1, 1962, [pub.] 1964, p. 51–60. [Seismic measurements of ice depth of Ghiacciaio Pian di Neve.]Google Scholar
Chizhov, O. P. Pitaniye osadkami i tayaniye lednikovykh pokrovov severo-vostochnoy Atlantiki v sovremennykh klimaticheskikh usloviyakh . Rezul’taty Issledovaniy po Programme Mezhdunarodnogo Geofizicheskogo Goda. Glyatsiologiya. IX Razdel Programmy MGG , No. 13, 1964, p. 30–38. [Mass balance of glaciers in Svalbard, Novaya Zemlya, Zemlya Frantsa-Iosifa and Severnaya Zemlya.]Google Scholar
Chuchkalov, B. S. The causes for movements of the Medvezhiy glacier. Soviet Hydrology. Selected Papers, 1963, No. 5, p. 522–24. [Report of sudden advance and its explanation.]Google Scholar
Corbel, J. Ladurie, E. Le R. Datation au C14 d’une moraine du Mont Blanc. Revue de Géographie Alpine, Vol. 51, No. 1, 1963, p. 173–75. [Results imply seventeenth century advance.]Google Scholar
Crary, A. P. Results of United States traverses in East Antarctica, 1958–1961. IGϒ Glaciological Report (New York), No. 7, 1963, xiv, 144 p. [Elevations and deduced ice flow, ice thickness, accumulation, in sector between Ross Ice Shelf and long. 120° E.]Google Scholar
Dolgushin, L. D., and others. Nedavneye nastupleniye Lednika Medvezh’yego . Priroda , 1963, No. 11, p. 85–92. [Enormous occasional speed of flow is thought to be due to decrease of bottom friction when the temperature rises above 0°C. English translation: Canada. Defence Research Board. Report No. T409 R, 1964.]Google Scholar
Dubrovin, L. I. Konovalov, G. V. Zavisimost’ snegonakopleniya of rel’yefa v rayon stantsii Lazarev . Informatsionnyy Byullelen’ Sovetskoy Antarklicheskov Ekspeditsii , No. 45, 1964, p. 29–32. [Local variations in snow accumulation.]Google Scholar
Freeberne, M. Glacial meltwater resources in China. Geographical Journal, Vol. 131, Pt. 1, 1965, p. 57–60. [Sinkiang is the major region in which the Chinese are attempting to harness the great glacial resources.]CrossRefGoogle Scholar
Gavrilova, M. K. Radiatsionnyy i teplovoy balans tayaniya severnogo polushariya . Rezul’taty Issledovaniy po Programme Mezhdunarodnogo Geoflzicheskogo Goda. Glyatsiologiya. IX Razdel Programmy MGG , No. 13, 1964, p. 97–105. [Summary of LG.Y. results.]Google Scholar
Gili-Borghet, A. Il Ghiacciaio del Belvedere e gli studi compiuti sino all’ anno 1957. Bolletlino del Comitato Glaciologico Italian, 2 Ser., No. 10, Pt. 1, 1961, [pub.] 1963, p. 33–64. [History of Ghiacciaio del Belvedere, Switzerland.]Google Scholar
Golubev, G. N. Regulation of melt water by glaciers. Soviet Hydrology. Selected Papers, 1963, No. 5, p. 498–501. [Study of relation between ablation and stream flow in Tien Shan.]Google Scholar
Govorukha, L. S. Mikhalenko, P. Ya. Sovremennoye otstupaniye lednikovogo pokrova Zemli FrantsaIosifa i kolebaniya beregovoy linii yeye ostrovov . Problemy Arktiki i Antarkiiki , Vyp. 15, 1964, p. 81–84.Google Scholar
Harrison, D. A. A reconnaissance glacier and geomorphological survey of the Duart Lake area, Bruce Mountains, Baffin Island, N.W.T. Geographical Bulletin (Ottawa), No. 22, 1964, p. 57–71. [Suvey of glacier snouts in this area; comparison of recent glacierization with that of other countries.]Google Scholar
Heinsheimer, G. J. Die Temperaturabhängigkeit der Wasserführung schmelzwassergenährter Flüsse. Archiv für Meteorologie, Geophysik und Bioklimatologie, Ser. B, Bd. 13, Ht. 3, 1964, p. 404–13. [On the ice-covered area of Patagonia a precipitation of 7,000–8,000 mm. was recorded. The waters of the rivers Leona and Santa Cruz originated here. and the paper deals with the forecasting of their consequent stream flow.]CrossRefGoogle Scholar
Hofmann, W. Die geodätischr Lagemessung über das grönländische Inlandeis der Internationalen Glaziologischen Grönland-Expedition (EGIG) 1959. Meddelelser om Crosland, Bd. 173, Nr. 6, 1964, 144 p. [A basis for the determination of movement and strain rate of the ice in two big profiles over the Greenland Ice. Sheet by precise measurement of fixed points.]Google Scholar
Kamb, W. B. Glacier geophysics. Science, Vo. 146, No. 3642, 1964, p. 353–65. [General review.]Google Scholar
Kapitsa, A. P. Priroda tsentral’noy Antarktidy . Priroda , 1964, No. 9, p. 46–56. [Soviet traverse “Vostok”-”Molodezhnaya”, 1964.]Google Scholar
Kick, W. Dorrer, E. Photogrammetrische Gletschermessungen in Norwegen. Allgemneine Vermessungsnachrichlen, Jahrg. 71, Ht. 11, 1964, p. 422–32. [Photogrammetric glacier measurements in Norway, particularly the fluctuation of Tunsbergsdalsbreen, with a map of the glacier showing states in 1937 and 1961.]Google Scholar
Kondrat’yev, O. K. Gamburtsev, A. G. Seysmicheskiye issledovaniya v pribrezhnoy chasti Vostochnoy Antarktidy . Moscow, lzciatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.), 1963. 188 p.Google Scholar
Koryakin, V. S. Osobennosti morfologii i evolyutsii sovremennogo oledeneniya Novoy Zemli i sosednikh lcdnikovykh rayonov . Rezul’taty Issledovaniy po Programme Mezhdunarodnogo Ceoftzicheskogo Goda. Glyatsiologiya. IX Razdel Programme MGG , No. 13, 1964, p. 39–43.Google Scholar
Kotlyakov, V. M. O sootnoshenii mezhdu vypadayushchimi osadkami i ikh akkumulyatsiyey na antarkticheskom lednikovom pokrove . Rezul’taty Issledovaniy po Programme Mezhdunarodnogo Geofizicheskogo Goda. Glyatsiologiya. IX Razdel Programmy MGG , No. 13, 1964, p. 12–18.Google Scholar
Mälzer, H. Das Nivellement über das grönländische Inlandeis der Internationalen Glaziologischen Grönland-Expedition 1959. Meddelelser om Grønland, Bd. 173, Nr. 7, 1964, 122 p. [About 700 km. was geometrically levelled from the western shore of central Greenland across the inland ice.]Google Scholar
Noble, H. M. Glaciological observations at Admiralty Bay, King George Island, in 1957–58. British Antarctic Survey Bulletin, No. 5, 1965, p. 1–11. [A tidal glacier (Stenhouse Glacier) and a small cirque glacier (Flagstaff Glacier). Tentative budgets are suggested and a few general conclusions.]Google Scholar
Østrem, G. Glacio-hydrological investigations in Norway. Journal of Hydrology, Vol. 2, No. 2, 1964, p. 101–15. [Accumulation, ablation, glacier action as long–term reservoirs, relation between melting and summer temperature, new mapping of glacierized areas in Norway. Also published as Norges Vassdrags- og Elektrisitetsvesen. Meddelelse fra Hydrologisk Avdeling, No. 13, 1964.]Google Scholar
Péguy, C.-P. Le Glacier de Saint-Sorlin (Massif des Grandes-Rousses): évolution générale. Problèmes et types de bilan. Bulletin de l’Association de Géographes Français, No. 311–12, 1963, p. 49–60. [Regime study of Glacier de Saint-Sorlin, France.]Google Scholar
Pytte, R. Østrem, G., ed. Glasio-hydrologiske undersokelser i Norge 1964, [av] O. Frøystein, V. Karlen, O. Liestøl, R. Pytte, 0g G. Østrem. Norges Vassdrags- 0 g Elektrisitetsvesen. Meddelelse fra Hydrologisk Avdeling, No. 14, 1965, p. 1–92, maps [in folder at back]. [Mass balance studies of many Norwegian glaciers, various special investigations, including correlation between air temperature and discharge, ablation studies, dusting glacier surfaces to facilitate mapping.]Google Scholar
Sagar, R. B. Meteorological and glaciological observations on the Gilman Glacier, northern Ellesmere Island, 1961. Geographical Bulletin (Ottawa), No. 22, 1964, p. 13–56. [Observations in the névé area indicate that an early summer snowfall, or a small negative deviation in temperature, or both, can critically affect the Gilman Glacier economy.]Google Scholar
Schwerdtfeger, P. Effect of polarization on the albedo. Nature, Vol. 202, No. 4935, 1964, p. 894. [Observations on Antarctic snow surfaces.]Google Scholar
Shul’ts, V. L. On the question of the expediency of artificial intensification of the melting of snow in the mountains of central Asia. Soviet Hydrology. Selected Papers, 1963, No. 3, p. 275–78. [Calculations to show uselessness of blackening glacier surface to increase run-off.]Google Scholar
Shul’ts, V. L., ed. Lednik Fedchenko. Tom 2. Tashkent, Izdatel’stvo Akademii Nauk Uzbekskoy SSR [Publishing House of the Academy of Sciences of the Uzbekskaya S.S.R.], 1962. 598 p. [Analysis of I.G.ϒ. studies on this glacier in the Pamir. English summary.]Google Scholar
Slupetzky, H. Slupetzky, W. Ergebnisse der Gletschermessungen in der Granatspitz- und westlichen Glocknergruppe in den Jahren 1961/63. Mitteilungen der Österreichischen Geographischen Gesellschaft, Bd. 106, Ht. 2, 1964, p. 231–35. [Data on glacier variations.]Google Scholar
Slupetzky, W. Slupetzky, H. Die Veränderungen des Sonnblick-, Ödenwinkel und Unteren Riffelkeeses in den Jahren 1960–1962. Wetter und Leben, Jahrg. 15, Ht. 3–4, 1963, p. 60–72. [Start of glaciological programme reported. Variations for 1960–61 and 1961–62 discussed in detail.]Google Scholar
Stokes, J. Ice calderas. British Antarctic Survey Bulletin, Vol. 1, No. 5, 1965, p. 63. [Letter. Suggestions regarding nomenclature; see also Aitkenhead, N., above.]Google Scholar
Tonini, D. II Ghiacciaio del Calderone del Gran Sasso d’Italia. Bollettino del Comitato Glaciologico Italiano, 2 Ser., No. 10, Pt. 1, 1961, [pub.] 1963, p. 71–135. [Summary of studies carried out since 1929 and study of topographical features and variations of glacier.]Google Scholar
Tonini, D. Recherches et mesures executées dans la zone glacier de la Marmolada. Bollettino del Comitato Glaciologico Italian, 2 Ser., No. 10, Pt. 1, 1961, [pub.] 1963, p. 11–18. [Depth and temperature of snow, radiation of sun and topographical surveys of the glacier.]Google Scholar
Tsukernik, V. B., and others. Seysmicheskiye i gravimetricheskiye issledovaniya na Zapadnom Shel’fovom Lednike v Antarktide . Izvestiya a Akademii Nauk SSSR. Seriya Geofizicheskaya , 1963, No. 6, p. 907–21. [Queen Mary Land.]Google Scholar
Visintini, G. de. Rilievo sismico a riflessione sul Ghiacciaio del Belvedere (Monte Rosa). Bollettino del Comitato Glaciologico Italian, 2 Ser., No. 10, Pt. 1, 1961, [pub.] 1963, p. 65–70. [Depth measurements on Ghiacciaio del Belvedere, Switzerland.]Google Scholar
Voigt, U. Die Bewegung der Gletscherzunge des Kongsvegen (Kingsbay, Westspitzbergen). Petermann Ceographische Mitteilungen, Jahrg. 109, 1 Quartalsheft, 1965, p. 1–8. [A movement of 4 m. a day was recorded from the main tongue of Koogsvegcn. Strain-rates and time variations were studied.]Google Scholar
Ward, W. H. A pilot study of recent fluctuations of glaciers. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 10e An., No. 1, 1965, p. 100–01.Google Scholar
Zanon, G. Sui ghiacciai di Suphelle e di Nigard (Jostedalsbreen). Bollettino del Comitato Glaciologico Italian, 2 Ser., No. 11, Pt. 1, 1962, [pub.] 1964, p. 9–30.Google Scholar
Zanon, G. La tournée glaciologica 1962 al Pelvoux. Bolletlino del Comitato Glaciologico Italian, 2 Ser., No. 11, Pt. 1, 1961, [pub.] 1963, p. 19–29. [Glaciological tour in Pelvoux alps, south-east France.]Google Scholar

Icebergs. Sea, river and lake ice

Goedecke, E. Über die Eisverhältnisse auf den Grossen Seen. Der Seewart, Bd. 22, Ht. 1, 1961, p. 31–44. [Ice distribution in the Great Lakes.]Google Scholar
Heap, J. A. Some characteristics of the winter ice cover of Lake Michigan 1962–63. University of Michigan. Institute of Science and Technology. Great Lakes Research Division. Publication No. 10, 1963, p. 216–18.Google Scholar
Heap, J. A. Winter ice cover in the Great Lakes. University of Michigan. Institute of Science and Technology. Great Lakes Research Division. Special Report No. 18, 1963, ii, 25 leaves.Google Scholar
Nutt, D. C. Coachman, L. K. A note on ice island WH–5. Arctic, Vol. 16, No. 3, 1963, p. 204–06. [Break-up and drift of “ice island” from Ward Hunt Ice Shelf, in Arctic basin and Nares Channel.]Google Scholar
Panzarini, R. N. Nomenclatura del hielo en el mar. Instituto Antártico Argentina. Publicación No. 10, 1963, 104 p. [Illustrated sea ice glossary. Includes other language equivalents of terms used.]Google Scholar
Savel’yev, B. A. Stroyeniye, sostav i svoystva ledyanogo pokrova morskikh i presnykh vodoyemov . Moscow, Izdatel’stvo Moskovskogo Universiteta [Publishing House of Moscow University], 1963. 541 p. [Includes porosity, thermal properties, elasticity and strength.]Google Scholar
Schumann, W. Physikalische Untersuchungen am Eibsee bei Garmisch-Partenkirchen. Mitteilungen der Geographischen Gesellschaft München, Bd. 50, 1965, p. 77–108. [Investigations of ice conditions, and observations covering a period of 50 winters, revealed that the Ice-coating of the Eibsee is marked by a very strict seasonal rhythm.]Google Scholar

Glacial Geology

Ahmad, F. Ahmad, N. The age of the Gondwana glaciation. Proceedings of the National Institute of Sciences of India, Pt. A, Vol. 28, No. 1, 1962, p. 16–56. [Evidence against very extensive Gondwanaland ice age.]Google Scholar
Bakker, J. P. A forgotten factor in the interpretation of glacial stairways. (An old question: new problems.) Zeitschrift für Geomorphologie, Neue Folge, Bd. 9, Ht. 1, 1965, p. 18–34. [Discussion on, and explanation of three different types of stairways.]Google Scholar
Bellair, P., and others. Un échantillon de moraine interne du Glacier de l’Astrolabe (Terre Adélie) par P. Bellair, J. Tourenq et S. Vernhet. Revue de Géographie Physique et de Géologie Dynamique, Sér. 2, Vol. 6, Fasc. 2, 1964, p. 115–21. [Study of a sample of morainic material recovered from a large iceberg broken in many fragments.]Google Scholar
Bray, J. R. Chronology of a small glacier in eastern British Columbia, Canada. Science, Vol. 14.4, No. 3616, 1964, p. 287–88.Google Scholar
Bray, J. R. Forest growth and glacier chronology in north-west North America in relation to solar activity. Nature, Vol. 205, No. 4970, 1965, p. 440–43. [Correlation between sunspot activity and glacial retreat.]Google Scholar
Brown, A. S. Nasmith, H. The glaciation of the Queen Charlotte Islands. Canadian Field-Naturalist, Vol. 76, No. 4, 1962, p. 209–19.Google Scholar
Brown, E. H. Glacial and periglacial landscapes in Poland. Geography: Journal of the Geographical Association (Sheffield), Vol. 50, Pt. 1, No. 226, 1965, p. 31–44.Google Scholar
Calkin, P. E. Geomorphology and glacial geology of the Victoria Valley system, southern Victoria Land, Antarctica. Ohio State University. Institute of Polar Studies. Report No. 10, 1964, xii, [102] p.Google Scholar
Calkin, P. E. Glacial geology of the Mount Gran area, southern Victoria Land, Antarctica. Geological Society of America. Bulletin, Vol. 75, No. 10, 1964, p. 1031–36. [At least two major glaciations are represented in this area. Ablation phenomena immediately adjacent to the glacier fronts suggest recent recession.]Google Scholar
Clayton, K. M. Glacial erosion in the Finger Lakes region (New York State, U.S.A.). Zeitschrift für Geomorphologie, Neue Folge, Bd. 9, Ht. 1, 1965, p. 50–62. [Shows that the ice movement was concentrated along the valleys of the main area of the Allegheny plateau.]Google Scholar
Colinvaux, P. A. Origin of ice ages: pollen evidence from Arctic Alaska. Science, Vol. 145, No. 3633, 1964, p. 707–08. [Evidence against Arctic Ocean having been ice-free 11,000 yr. ago.]Google Scholar
Corbel, J. Glaciers et climates dans le Massif du Mont-Blanc. Revue de Géographie Alpine, Vol. 51, No. 2, 1963, p. 321–60. [Reconstruction of fluctuations of glaciers and climate back to Würm maximum.]Google Scholar
Downie, C. Glaciations of Mount Kilimanjaro, north-east Tanganyika. Geological Society of America. Bulletin, Vol. 75, No. 1, 1964, p. 1–16. [Six glacial episodes recognized.]Google Scholar
Haserodt, K. Riesengletschertöpfe am Nordausgang des Kalkhochalpen-Durchbruchstals der Salzach bei Golling (Salzburg). Mitteilungen der Geographischen Gesellschaft München, Bd. 50, 1965, p. 161–73. [Subglacial pot-holes near Salzburg (Austria) are larger than similar forms known up to now in the northern limestone Alps.]Google Scholar
Holmes, G. W. Andersen, B. G. Glacial chronology of Ullsfjord, northern Norway. U.S. Geological Survey. Professional Paper 475–D, Art. 154, 1964, p. D159–63. [Quaternary features of Ullsfjord record late glacial fluctuations of the Fennoscandian ice sheet and of local alpine glaciers.]Google Scholar
Ives, J. D., and others. Fluvioglacial erosion near Knob Lake, central Quebec-Labrador, Canada, [by] J. D. Ives, R. P. Kirby [and] E. Derbyshire. Geological Society of America. Bulletin, Vol. 75, No. 9, 1964, p. 917–25. [Criticism by Ives and Kirby of classification of drainage forms proposed by Derbyshire in his article of same title, ibid., Vol. 73, No. 9, 1962, p. 1111–26, with reply (p. 923) by Derbyshire.]Google Scholar
Kjartansson, G. Ísaldarlok og eldfjöll á Kili. Náttúrufræðingurinn , Àrg. 34, Ht. 1, 1964, p. 9–38. [Course of deglaciation in Kjölur area, central Iceland. Influence of various glacial stages on formation of volcanoes in area. English summary.]Google Scholar
MacClintock, P. Dreimanis, A. Reorientation of till fabric by overriding glacier in the St. Lawrence valley. American Journal of Science, Vol. 262, No. 1, 1964, p. 133–42.Google Scholar
Mathews, W. H. Sediment transport from Athabasca Glacier, Alberta. [Union Géodésique et Géophysique Internationale.] Association Internationale d’Hydrologie Scientifique. Assemblée générale de Berkeley de l’UGGI, 19–8–31–8 1963. Erosion continentale, précipitations, hydrométrie, humidité du sol, 1964, p. 155–65.Google Scholar
Østrem, G. Ice crystals from an ice-cored moraine on Baffin Island, N.W.T. Geographical Bulletin (Ottawa), No. 22, 1964, p. 72–79. [Crystals on the surface larger than those of the buried ice, indicating that the latter have not developed from the surface ice.]Google Scholar
Østrem, G. Problems of dating ice-cored moraines. Geografiska Annoter, Vol. 47A, No. 1, 1965, p. 1–38. [Conditions under which ‘14C and pollen analysis methods are valid.]Google Scholar
Reed, B., and others. Some aspects of drumlin geometry, by B. Reed, C. J. Galvin, Jr., and J. P. Miller. American Journal of Science, Vol. 260, No. 3, 1962, p. 200–10. [Comparison of geometrical properties of drumlins located in three different regions of United States.]Google Scholar
Scheidegger, A. E. A theory of varve formation. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 10e An., No. 1, 1965, p. 68–73. [Under the premise that the thickness of varves is directly proportional to the sedimentation rate, a theory is proposed which relates varve thickness with the time of deposition after the retreat of the ice.]Google Scholar
Shnitnikov, A. V. O nekotorykh zakonomernostyakh razvitiya oledeneniya Antarktidy . Rezul’taty Issledovaniy po Programme Mezhdunarodnogo Geofizicheskogo Goda. Glyatsiologiya. IX Razdel Programmy MGG , No. 13, 1964, p. 49–56.Google Scholar
Yevteyev, S. A. Geologicheskaya deyatel’nost’ lednikovogo pokrova Vostochnoy Antarktidy . Rezul’tay Issledovaniy po Programme Mezhdunarodnogo Geofizicheskogo Goda. Glyalsiologiya. IX Razdel Programmy MGG , No. 12, 1964, 120 p.Google Scholar
Yevteyev, S. A. Osnovnyye etapy razvitiya oledeneniya yuzhnogo polushariya v chetvertichnom periode . Rezul’taty Issledovaniy po Programme Mezhdunarodnogo Geofizicheskogo Goda. Glyatsiologiya. IX Razdel Programmy MGG , No. 13, 1964, p. 7–11 Google Scholar
Yevteyev, S. A. Lazukov, G. I. Rol’ glyatsioizostazii v dvizheniyakh zemnoy kory oblastey sovremennogo i drevnego oledeneniy . Izvestiya Akademii Nauk SSSR. Serfiya Geogrqfuheskaya , 1964, No. 2, p. 24–36. [Critical examination of evidence.]Google Scholar

Frost action on rocks and soil. Frozen ground. Permafrost

Brochu, M. Essai de définition des grandes zones périglaciaires du Globe. Zeitschrift für Geomorphologie, Neue Folge, Bd. 8, Ht. 1, 1964, p. 32–39. [Attempt to make a synthetic definition of the periglacial zones of the world.]Google Scholar
Brown, R. J. E. Permafrost investigations on the Mackenzie Highway in Alberta and Mackenzie District. Canada. National Research Council. Division of Building Research. Technical Paper No. 175, 1964, 67 p.Google Scholar
Brown, R. J. E. Some observations on the influence of climatic and terrain features on permafrost at Norman Wells, N.W.T., Canada. Canadian Journal of Earth Sciences, Vol. 2, February 1965, p. 15–31.Google Scholar
Day, J. H. Rice, H. M. The characteristics of some permafrost soils in the Mackenzie Valley, N.W.T. Arctic, Vol. 17, No. 4, 1964, p. 223–36. [Description and constitution of 8 profiles, methods of investigation, landforms and soils.]Google Scholar
Foster, H. L. Holmes, G. W. A large transitional rock glacier in the Johnson River area, Alaska Range. U.S. Geological Survey. Professional Paper 525–B, 1965, p. B112–16. [The rock glacier is an end member of an unbroken series of ice-related features and merges up-valley with an ice-cored moraine and an ice glacier in the cirque.]Google Scholar
Grötzbach, E. Beobachtungen an Blockströmen im afghanischen Hindukusch und in den Ostalpen. Mitteilungen der Geographischen Gesellschaft München, Bd. 50, 1965, p. 175–201. [Differentiation between rock tongues as remnants of active ice glaciers and rock glaciers which originated as independent accumulations of rocks and debris interspersed by recent ice.]Google Scholar
Hoekstra, P. Chamberlain, E. Electro-osmosis in frozen soil. Nature, Vol. 203, No. 4952, 1964, p. 1406–07. [Letter. Measurement of movement of water through frozen soil under electric field.]Google Scholar
Johnston, G. H. Brown, R. J. E. Some observations on permafrost distribution at a lake in the Mackenzie Delta, N.W.T., Canada. Arctic, Vol. 17, No. 3, 1964, p. 162–75. [Thawing effect of the lake is confined to the ground below it, but ground temperatures measured inland indicate that the thermal effect of the lake extends some distance beyond its perimeter. Also published as Canada. National Research Council. Division of Building Research. Research Paper No. 233, 1964.]Google Scholar
Johnston, G. H. Brown, R. J. E. Stratigraphy of the Mackenzie River Delta, Northwest Territories, Canada. Geological Society of America. Bulletin, Vol. 76, No. 1, 1965, p. 103–11. [Results of an investigation to determine the distribution of permafrost under and adjacent to a small lake in the delta near the new townsite of Inuvik. Also published as Canada. National Research Council. Division of Building Research. Research Paper No. 235, 1965.]Google Scholar
Rathjens, C. Ein Beitrag zur Frage der Solifluktionsgrcnzc in den Cebirgen Vorderasiens. Zeitschrift für Geomorphologie, Neue Folge, Bd. 9, Ht. 1, 1965, p. 35–49. [Researches in the Afghan Hindu Kush indicate that the region influenced by solifluction is broader in a dry climate.]Google Scholar
Shvetsov, P. F. Merzlyye sloi zemnvye ikh rasprostraneniye i znacheniye . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1963. 102 p. [Review of present state of knowledge.]Google Scholar
Vel’mina, N. A. Vtyurin, B. I., ed. Geokriologicheskiye usloviya zapadnoy Sibiri, ϒakutii i Chukotki . Moscow, Izdatel’stvo “Nauka” [Publishing House “Nauka”], 1964. 140 p. [Papers on frozen ground and associated phenomena.]Google Scholar
Vtyurin, B. I. Kriogennoye stroyeniye chetverlichnykh otlozheniy na primere Anadyrskoy nizmennosti . Moscow, Izdatel’stvo “Nauka” [Publishing House “Nauka”], 5964. 152 p. [Features of frozen ground in this region.]Google Scholar
Williams, P. J. Experimental determination of apparent specific heats of frozen soils. Géotechnique, Vol. 14, No. 2, 1964, p. 133–42. [Also published as Canada. National Research Council. Division of Building Research. Research Paper No. 226, 1964.]Google Scholar
Williams, R. B. G. Permafrost in England during the last glacial period, Nature, Vol. 205, No. 4978, 1965, p. 1304–05. [Letter. Evidence that permafrost existed mainly in eastern England and also in south-west Wales but was largely absent in south-west England.]Google Scholar

Meteorological and Climatological Glaciology

Arnold, K. C. MacKay, D. K. Different methods of calculating mean daily temperatures, their effects on degree-day totals in the high Arctic and their significance to glaciology. Geographical Bulletin (Ottawa), No. 21, 1964, p. 123–29.Google Scholar
Astapovich, I. S. Ledyanyye meteority . Priroda , 1964, No. 5, p. 84–85. [Analysis of meteorite and appeal in footnote by K. P. Florenskiy for information on any others that are found.]Google Scholar
Fliri, F. Zur Witterungsklimatologie sommerlicher Schneefälle in den Alpen. Wetter und Leben, Jahrg. 16, Ht. 1–2, 1964, p. 1–11. [Based on observations of precipitation on the Säntis. It is shown that summer snowfalls are caused by meridional circulation in connection with disturbances travelling west to east.]Google Scholar
Havens, J. M. Climatological notes from Axel Heiberg Island, N.W.T., Canada. Arctic, Vol. 17, No. 4, 1964, p. 261–63. [Includes the cooling effect of a glacier terminus on the lower atmosphere.]Google Scholar
Jiusto, J. E. Rogers, R. R. Seeding whiteouts in Greenland. Research Trends, Cornell Aeronautical Laboratory, Vol. 9, No. 1, 1961, p. 5–7.Google Scholar
Kosiba, A. Loewe, F. Meteorological observations in the Tasersiaq area, southwest Greenland, during summer, 1963. Ohio State University. Institute of Polar Studies. Report No. 11, 1964, [vi, 59] p. [General account of meteorological observations and particular study of wind. Influence on snow and ice accumulation on Sukkertoppen ice cap discussed.]Google Scholar
McVehil, G. E. Wind and temperature profiles near the ground in stable stratification. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 384, 1964, p. 136–46. [Antarctic and U.S.A. data compared. Surface stress and heat flux deduced.]Google Scholar

Snow

[Austria: Snow.] Der Schnee in Österreich im Zeitraum 1901–1950. Beitrage zur Hydrographie Österreichs, Ht. 34, 1962, 174 p., maps.Google Scholar
Bergen, J. D. Swanson, R. H. Evaporation from a winter snow cover in the Rocky Mountain forest zone. Proceedings of the Western Snow Conference, 32nd annual meeting, 1964, [pub.] 1964, p. 52–57. [Quantitative results.]Google Scholar
Coulianos, C.-C. Johnels, A. G. Note on the subnivcan environment of small mammals. Arkiv for. zoologi, Ser. 2, Bd. 15, No. 24, 1962, p. 363–70. [Observations on biological importance of snow cover from central Sweden.]Google Scholar
[France: Institutions.] Institut Français pour l’Étude de la Neige au Parc national de la Vanoise. Les Alpes. Revue du Club Alpin Suisse, 40e An., 3e Trimestre, 1964, p. 74–75. [Institute for study of snow in all aspects in course of construction in Parc national de la Vanoise.]Google Scholar
Herman, J. R. On the electrical properties of blowing snow. Annales de Géophysique, Tom. 20, No. 3, 1964, p. 235–41. [Deduced from radio noise.]Google Scholar
Judson, A. Relative importance of weather factors creating slab avalanches in Colorado. Proceedings of the Western Snow Conference, 32nd annual meeting, 1964, [pub.] 1964, p. 60–67.Google Scholar
Onufriyenko, L. G. Losses of snowmelt on slopes. Soviet Hydrology. Selected Papers, 1964, No. 1, p. 55–61. [Observations on effect of slope on run-off.]Google Scholar
Power, B. A., and others. Snow crystal forms and riming effects as related to snowfall density and general storm conditions, [by] B. A. Power, P. W. Summers [and] J. D’Avignon. Journal of the Atmospheric Sciences, Vol. 21, No. 3, 1964, p. 300–05. [Relationship found between new-snow density and crystal form.]Google Scholar
Uttinger, H. Die Dauer der Schneedecke in Zürich. Archiv für Meteorologie, Geophysik und Bioklimatologie, Ser. B, Bd. 12, Ht. 3–4, 1963, p. 404–21. [Number of days with snow cover at Zürich, Switzerland, since winter 1880–81.]Google Scholar