[Antarctic Regions: Glaciology.] U.S. Antarctic activities: long-range projection, 1965–70. Part 1. Scientific plans. Antarctic Journal of the U.S., Vol. 1, No. 3, 1966, p. 79–83. [Including the major future glaciological programmes.]Google Scholar

Miller, M. M. Prouty, C. E. A field institute concept in the glaciological sciences. Proceedings of the 16th Alaskan Science Conference, College, Alaska, August 29-September 1, 1965, 1966, p. 97–103. [Description of Summer Institute of Glaciological Sciences, its activities, aims and achievements.]Google Scholar

[Soviet Central Asia: Glaciology.] Akademiya Nauk Kazakhskoy SSR. Sektor Fizicheskoy Geografti. Glyatsiologicheskiye issledooaniya e Kazakhstan . Vyp. 6. Alma-Ata, Izdatel’stvo “Nauka” Kazakhskoy SSR [Publishing House “Nauka” of the Kazakh S.S.R.], 1966. 140 p. [Continuation of five volumes published 1961–65. Contains the following papers, all in Russian with English summaries: P. A. Cherkasov, “Main features of recent glaciation of the Dzhungar Alatau eastern part”, p. 5–28; P. A. Cherkasov and N. V. Yerasov, “Recent glaciation of the Rgayty river basin in the Dzhungar Alatau range”, p. 29–49; P. A. Cherkasov and V. A. Zenkova, “Glacial ablation of the basin Aganakty Tentek in the Dzhungar Alatau range”, p. 50–68; K. Sh. Diyarova and L. P. Koneva, “Weather and radiation conditions in the Dzhungar Alatau range glacial zone”, p. 69–81; K. G. Makarevich, “Static [i.e. mass] balance of some small glaciers in the Zailiysky Alatau”, p. 82–92; N. N. Pal’gov, “Characteristics of some interconnections in the hydrological regime of one of the central Tuyuksu glacier[s]”, p. 93–111; L. N. Filatova, “On influence of versant altitude and orientation on the time of snow cover deposition (by the example of the Malaya Almatinka river basin)”, p. 112–22; L S. Sosedov and I. V. Severskiy, “Influence of avalanches on run-off formation in the Zailiysky Alatau midmountain zone”, p. 123–32; T. Ya. Denisova, “Accumulated radiation in the Zailiysky Alatau range Alpine zone”, p. 133–39.]Google Scholar

Whitmore, G. D. Southard, R. B. Topographic mapping in Antarctica by the U.S. Geological Survey. Antarctic Journal of the U.S., Vol. 1, No, 2, 1966, p. 40–50.Google Scholar

Anderson, E. Computer model for forecasting runoff from melting snow.Proceedings of the Eastern Snow Conference, 22nd annual meeting, 1965, p. 50–70. [Reports method and results.]Google Scholar

[Conferences.] Symposium on the heat exchange at snow and ice surfaces, 26 October 1962. Canada. National Research Council. Associate Committee on Soil and Snow Mechanics. Technical Memorandum No. 78, 1963, ii, 82 p. [Papers on energy exchange and instruments for measuring it.]Google Scholar

Lambert, G., and others. Corrélations entre le depôt de plomb 210 dans l’Antarctique et l’activité solaire, par G. Lambert, M. Nezami et J. Labeyrie. Compres Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 260, No. 2, 1965, p. 619–22. [Found that concentration of zoPb in Antarctic snow passes through maximum after each period of maximum solar activity.]Google Scholar

Winston, W. A comprehensive procedure for evaluating snow ablation. Proceedings of the Eastern Snow Conference, 22nd annual meeting, 1965, p. 71–113. [Empirical method for evaluating ablation from meteorological data.]Google Scholar

Brivati, J. A., and others. Electron spin resonance studies of the hydroxyl radical in γ-irradiated ice, by J. A. Brivati, M. C. R. Symons, D. J. A. Tilling, H. W. Wardale, and D. O. Williams. Chemical Communications, 1965, No. 17, p. 402–03. [Results and brief interpretation.]Google Scholar

Coulson, C. A. Eisenberg, D. Interactions of H₂O molecules in ice. I. The dipole moment of an H₂O molecule in ice.—II. Interaction energies of H₂O molecules in ice. Proceedings of the Royal Society, Ser. A. Vol. 291, No. 1427, 1965, p. 445–53; p. 454–59; [I: calculation of field arising from 85 nearest neighbours and hence of dipole moment of molecule itself. 11: calculation for hexagonal and cubic ice.]Google Scholar

Dibdin, G. H. New structure in the electron spin resonance spectrum of y-irradiated single crystals of ice. Nature, Vol. 209, No. 5021, 1966, p. 394–95. [Letter. Results at 77° K. interpreted as evidence that OH ion defects in ice are on normal oxygen sites.]Google Scholar

Evans, L. F. Ice nucleation by proteins and surface films. Nature, Vol. 211, No. 5046, 1966, p. 281–82. [Pepsin, egg albumen, and a whole range of long-chain filins do not promote ice nucleation.]Google Scholar

Kamb, W. B. Overlap interaction of water molecules. Journal of Chemical Physics, Vol. 43, No. 11, 1965, p. 3917–24. [Calculations and comparison with properties of ice VII and ice II. Discussion of stability of ice VII at very high pressures.]Google Scholar

Knight, C. A. Knight, N. C. “Negative” crystals in ice: a method for growth. Science, Vol. 150, No. 3705, 1965, p. 1819–21. [Made by inserting hypodermic needle and connecting to vacuum. Study of habit as function of temperature and growth rate.]Google Scholar

Lavrov, V. V. K probleme mekhanicheskikh svoystv l’da . Problemy Arktiki i Antarktiki , Vyp. 21, 1965, p. 60–65. [Ways to avoid difficulties arising from scaling up of results obtained from small samples.]Google Scholar

Macklin, W. C. Ryan, B. F. Habits of ice grown in supercooled water and aqueous solutions. Philosophical Magazine, Eighth Ser., Vol. 14, No. 130, 1966, p. 847–60. [Observations of deviations from basal plane in the growth of dendrites with increasing supercooling. Explanation proposed.]Google Scholar

Montefinale, A. C Papée, H. M. Nucleation of ice by some porous particles. Zeitschrift für angewandte Mathematik and Physik, Vol. 16, Fasc. 6, 1965, p. 740–45. [Effect of absorbed water and of desorption of gas on nucleating properties of kaolin, silica gel and alumina.]CrossRefGoogle Scholar

Muguruma, J. Pairs of spiral etch pits in ice crystals. Nature, Vol. 208, No. 5006, 1965, p. 180–81. [Letter. Observation of phenomenon when etching (0001) surface and two possible explanations.]Google Scholar

Muguruma, J., and others. Void formation by non-basal glide in ice single crystals, by J. Muguruma, S. Mae and A. Higashi. Philosophical Magazine, Eighth Ser., Vol. 13, No. 123, 1966, p. 625–29. [Results of tensile tests of ice crystals with tensile axis perpendicular to c-axis.]Google Scholar

Vali, G. Stansbury, E. J. Time-dependent characteristics of the heterogeneous nucleation of ice. Canadian Journal of Physics, Vol. 44, No. 3, 1966, p. 477–502. [Study of nucleation of drops as function of temperature and time and interpretation.]Google Scholar

Vonnegut, B. Latham, J. Electrification of frost deposits. Quarterly Journal of the Royal Meteorological Society, Vol. 91, No. 389, 1965, p. 369–74. [Letters. Question from Vonnegut concerning Latham’s statement (ibid., Vol. 90, No. 386, 1964, p. 486) that there is no evidence that convective processes could generate sufficient charge to explain thunderstorms and reply by Latham.]Google Scholar

Wyllie, G. Kinetic theory and transport in ice and water. (In Fogg, G. E., ed. The state and movement of water in living organisms. Symposia of the Society for Experimental Biology, No. 19, 1965, p. 33–54.) [Review article. Includes discussion of similarities and differences between diffusion, heat transfer and electrical transport in water and ice.]Google Scholar

Ashwell, I. Y. Drummond Glacier, Rocky Mountains in Alberta. Annual Report. British Schools Exploring Society, 1964–65, p. 89–90. [Account of work by Dept. of Geography, University of Alberta, on contribution of glacier melt water to flow of upper Red Deer River.]Google Scholar

Brecher, H. H. Measurements of ice surface movement by aerial triangulation. Antarctic Journal of the U.S., Vol. 1, No. 4, 5966, p. 139. [Comparison with the accumulation figures from the stratigraphie studies indicated that the latter underestimated the accumulation by 4 to 28 per cent.]Google Scholar

Burgos, F. O., and others. Tareas glaciologicas en la campaña Enero-Febrero de 1964, [by] F. O. Burgos, S. M. Olivares, B. S. Ratto, D. Rossetti [and] S. Shinjo. Instituto Nacional del Hielo Continental Patagónico. Publicación (Buenos Aires), No. 7, 1964, p. 3–13.Google Scholar

Dolgushin, L. D. Regional’nyye problem, oledeneniya po issledovaniyam na Urale, v Tsentral’noy Azii i Antarktide . Moscow, Akademiya Nauk SSSR. Institut Geografii [Academy of Sciences of the U.S.S.R. Geographical Institute], 1963. 55 p. [Dissertation.]Google Scholar

Gliozzi, J. Size-distribution analysis of microparticles in two Antarctic firn cores. Journal of Geophysical Research, Vol. 71, No. 8, 1966, p. 1993–98. [Variation with depth described and analysed.]Google Scholar

Gow, A. J. Glaciological studies in Antarctica. Antarctic Journal of the U.S., Vol. 1, No. 4, 1966, p. 140. [Brief report.]Google Scholar

Hamilton, W. L. Bull, C. [B. B.] A comparison of the dust flux in the upper atmosphere and on the polar ice sheets. Journal of Geophysical Research, Vol. 71, No. 10, 1966, p. 2679–83. [Letter. Particles in ice cores show concentration that suggests most of upper atmosphere flux arrives at surface.]Google Scholar

[Iceland: Ice caps.] Vatnajökull-the biggest glacier in Europe, Iceland Review, Vol. 3, No. 3, 1965, p. 24–29.Google Scholar

Izrael’, Yu. A., and others. O soderzhanii tritiya v lednikakh . Doklady Akademii Nauk SSSR , Tom 156, No. 1, 1964, p. 72–73. [Results of tritium sampling on Lednik Fedchenko.]Google Scholar

Kehle, R. O. Deformation of the Ross Ice Shelf, Antarctica. Geological Society of America. Bulletin, Vol. 75, No. 4, 1964, p. 259–86. [Study of structural features of Camp Michigan area on north-east margin of Ross Ice Shelf. Attempt made to extend data obtained from ice to study of rock faults.]Google Scholar

Kennett, P. Reconnaissance gravity and magnetic surveys of part of the Larsen Ice Shelf and adjacent mainland. British Antarctic Survey Bulletin, No. 8, 1966, p. 49–62. [Results give the sub-ice topography of much of the east coast of Graham Land.]Google Scholar

Larsson, R. A. Notes on ice-velocity data from observations on Mikkaglaciären, 1895–1962. Geografiska Annaler, Vol. 48A, No. 1, 1966, p. 40–42. [Ice-movement observations from 1895 to 1962, especially from the aspect of decrease in velocity. Different methods used for point-marking are examined and a new method is described.]Google Scholar

Liestøl, O. Bremâlinger i Norge 1964. Norsk Polarinstitutt. Årbek, 1964 [pub. 1966], p. 155–64. [Regime measurements on nine glaciers in Norway in 1964; detailed data on Storbreen and Hardangerjokulen. Ice front fluctuations for 13 glaciers. English summary.]Google Scholar

Lliboutry, L. Bottom temperatures and basal low-velocity layer in an ice sheet. Journal of Geophysical Research, Vol. 71, No. 10, 1966, p. 2535–43. [Suggestion that layer of low seismic wave velocity found in Antarctica may consist of temperate pure ice, not cold ice with morainal material.]Google Scholar

Magnani, M. Über mexikanische Gletscher. Polarforschung, Bd. 5, Jahrg. 34, Ht. 1–2, 1964 [pub. 1965] p. 275–78. [Discussion of present glaciers in Mexico and their extension in the Pleistocene.]Google Scholar

Maksimov, Ye. V. Oledeneniye basseynov severnoy i yuzhnoy Shamsi v Kirgizskom Alatau . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva , Tom 95, Vyp. 5, 1963, p. 420–29. [General description of 29 glaciers in this region.]Google Scholar

Oelsner, C. Ergebnisse von Gravimetermessungen im Kingsbay-Gebiet (Westspitzbergen). Petermanns Geographische Mitteilungen, Jahrg. 110, 2. Quartalsht., 1966, p. 111–16. [Gravimetric measurements for the determination of ice thickness carried out on glaciers in Kongsfjorden, Vestspitsbergen. Ice thicknesses of more than 200 m. were recorded.]Google Scholar

Picciotto, E. E. Kane, H. S. Glaciological studies on the South Pole-Queen Maud Land traverse. II. Antarctic Journal of the U.S., Vol. 1, No. 4, 1966, p. 132. [Report of intensive glaciological programme.]Google Scholar

Picciotto, E. E. Wilgain, S. Radioaktivitätsmessungen zur Bestimmung der Firnrücklagen eines Alpengletschers. Die Naturwissenschaften, Jahrg. 52, Ht. 7, 1965, p. 154. [Connection between atomic bomb tests and the beta activity of the firn layers.]Google Scholar

Reed, J. C. jr. Rate of ice movement and estimated ice thickness in part of the Teton Glacier, Grand Teton National Park, Wyoming. U.S. Geological Survey. Professional Paper 525-B, 1965, p. 137–41.Google Scholar

Schulze, O. Die Eisverhältnisse an der Prawda-Küste während der VI sowjetischen Antarktisexpedition 1961/1962. Abhandlungen des Meteorologischen Dienstes der Deutschen Demokratischen Republik, Bd. 10, Nr. 75, 1965, p. 19–35. [Ice thickness measurements obtained from Mirny station on coastal region of Davis Sea, May 1961 January 1962.]Google Scholar

Schytt, V. Notes on glaciological activities in Kebnekaise, Sweden, during 1965. Geografiska Annaler, Vol. 48a, No. 1, 1966, p. 43–50. [Mass balance studies on Storglaciären, and variations of the extent of Swedish glaciers.]Google Scholar

Sellevoll, M. A. Kloster, K. Seismic measurements on the glacier Hardangerjøkulen, western Norway. Norsk Polarintitutt., Årbok, 1964 [pub. 1966], p. 87–91. [Field work in s 963.]Google Scholar

Shimizu, H. Wakahama, G. Kasukaurushu hyōga (Kanada) genryùiki ni okeru sekisetsu chōsa . Teion-kagaku , Ser. A, Vol. 23, 1965, p. 137–56. [Measurements of properties and dating of layers in 15 m. pit. English summary.]Google Scholar

Stenborg, T. Some observations of differential ice-movements on Mikkaglaciären. Geografiska Annaler, Vol. 48a, No. 1, 1966, p. 32–39. [Measurements of movement vectors show a relatively large lateral component of glacier movement in the lee of a sharp bend on the eastern margin.]Google Scholar

Taylor, L. D. Glaciological studies on the South Pole traverse, 1962–1963. Ohio State University. Institute of Polar Studies. Report No. 17, 1965, iv, [24] leaves. [Measurements of accumulation, temperature, density and hardness of firn at 25 stations between South Pole and Queen Maud Mountains.]Google Scholar

Vivian, R. La catastrophe du glacier Allalin. Revue de Géographie Alpine, Torn. 54, Fasc. 1, 1966. p. 97–112. [Description of condition of glacier which led to portion of snout breaking away, and of measurements made subsequently.]CrossRefGoogle Scholar

Voigt, U. Die Arbeiten der Überwinterungsgruppe der Deutschen Spitzbergen-Expedition 5964/65. Petermanns Geographische Mitteilungen, Jahrg. 110, 1. Quartalsht., 106. p. 43. [Motion of glaciers, mapping of 61 glacier fronts in Kongsfjorden, meteorology, etc.]Google Scholar

Yablokov, A. A. Aksuyskiye ledniki . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva , Tom 95, Vyp. 5, 1963, p. 452–54. [General description of glaciers in Turkistan.]Google Scholar

Zotikov, I. A. O temperaturakh v tolshche lednikov Antarktidy . (In Antarktika. Doklady Komissii, 1963 . Moscow, Izdatel’stvo Akademii Nauk SSSR [Publishing House of the Academy of Sciences of the U.S.S.R.], 1964, p. 61–105. [Analysis of glacier temperature due to heat conduction and ice movement in simple model.]Google Scholar

Apollonio, S. Chlorophyll in Arctic sea ice. Arctic, Vol. 18, No. 2, 1965, p. 118–22. [Measurements under various depths of sea ice.]Google Scholar

Arnell, S. Dunbar, Moira, comp. A bibliography on ice in navigable waters in Canada, 1945–64. Compiled in the Defence Research Board under the auspices of the Working Group on Ice in Navigable Waters…. Ottawa, National Research Council of Canada, 1964. [viii], 64 p. (N.R.C. 8503.)Google Scholar

Baranov, G. I. O fiziko-mekhanicheskikh svoystvakh morskogo antarkticheskogo l’da . Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii , No. 54, 1965. p. 43–46.Google Scholar

Black, W. A. Cartographic techniques for mapping sea ice. Cartographer, Vol. 2, No. 1, 1965, p. 9–13. [Methods used to present results of aerial surveys of Gulf of St. Lawrence.]Google Scholar

Bukina, L. A. O koeffitsiyente teplootdachi kristallov vnutrivodnogo Pda diskoobraznoy formy . Izvestiya Akademii Nauk SSSR. Seriya Geofizicheskaya , 1963, No. 7, p. 1131–39. [Derivation of formula for heat emission coefficient from empirical data on rate of growth. English translation in Bulletin of the Academy of Sciences of the U.S.S.R Geophysical Series, 1963, No. 7, p. 689–93.]Google Scholar

Ganton, J. H. Milne, A. R. Temperature- and wind-dependent ambient noise under midwinter pack ice. Journal of the Acoustical Society of America, Vol. 38, No. 3, 1965, p. 406–11. [Measurement of noise reveals two sources, cracking due to thermal stresses and wind effects.]Google Scholar

Harrison, J. D. Measurement of brine droplet migration in ice. Journal of Applied Physics, Vol. 36, No. 12, 1965, p. 3811–15. [Observations of velocity and changes of size and shape of droplets of NaCI, KF, and KI through ice from –6° to 0° C.]Google Scholar

Izraileva, N. I. Krasil’nikov, V. N. Otrazheniye izgibnykh vole torosami . Akusticheskiy Zhurnal , Tom 10, No. 3, 1964, p. 301–08. [Theoretical analysis of reflection of waves by sea-ice hummocks. English translation in Soviet Physics-Acoustics, Vol. 10, No. 3, 1965, p. 256–61.]Google Scholar

Koslowski, G. Über den Zusammenhang zwischen Grosswetterlagen and Eisbildung im Finnischen Meerbusen. Deutsche Hydrographische. eitschrift, Jahrg. 17, Ht. 6, 1964, p. 273–85. [Discussion of connection between general weather situation and the growth of ice in the Gulf of Finland. English and French summaries.]Google Scholar

Kuz’min, P. P. Issledovaniya i raschety ledovykh yavleniy na rekakh i vodokhranilishchakh . Trudy Gosudarstuennogo Gidrologitheskogo Instituta , Vyp. 129, 1965, 80 p. [Aspects of behaviour of ice on inland waters.]Google Scholar

Lewis, E. L., and others. Frozen sea research, by E. L. Lewis, P. H. Bridge, R. W. Mackay, R. W. Sawler and B. Trudel. Bedford Institute of Oceanography. Third Annual Report, 1964, p. 6–7. [Canada. Account of work in 1964 at Bedford, N.S., Cambridge Bay, N.W.T. and Victoria, B.C.]Google Scholar

Lieske, B. J. Net radiation over fast sea ice during spring breakup at Pt. Barrow, Alaska. Proceedings of the fifteenth Alaskan Science Conference, College, Alaska, August 31-September 4, 1964, 1965, p. 52–60. [Importance of different factors in deterioration of sea ice.]Google Scholar

Likens, G. E. Ragotzkie, R. A. Vertical water motions in a small ice-covered lake. Journal of Geophysical Research, Vol. 70, No. 10, 1965, p. 2333–44. [Earlier measurements discussed theoretically.]Google Scholar

Mackay, D. K. Break-up on the Mackenzie River and its delta, 1964. Geographical Bulletin (Ottawa), Vol. 7, No. 2, 1965, p. 117–28. [Aerial and ground observations.]Google Scholar

Maksimov, I. V. O prichinakh vnezapnogo obloma shel’fovykh lednikov Antarktidy . Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii , No. 54, 1965, p. 29–32. [Icebergs may be calved as a result of a wave originated by a cyclone.]Google Scholar

Müller, W. “Seegfrörni” in Zürich. Wetter und Leben, Bd. 15, Ht. 5–6, 1963, p. 107–09. [Discussion of conditions in 1963 which caused the Zürcher See to freeze over for the first time since 1929.1Google Scholar

Oliver, D. R. A limnological investigation of a large Arctic lake, Nettilling Lake, Baffin Island. Arctic, Vol. 57, No. 2, 1964, p. 69–83. [Includes details of lake ice.]Google Scholar

Ono, N. Kaihyō no netsu no seishitsu no kenkyū. I. Usu i tōhyō no netsu dendōritsu no sokutei.—II. Fukinshitsuna hyōsō no no atai o motomeru. Teion-kagaku , Ser. A, Vol. 23, 1965, p. 167–76; p. 177–83. [English summaries.]Google Scholar

Predoehl, M. C. Spano, A. F. Airborne albedo measurements over the Ross Sea, October-November 1962. Monthly Weather Review, Vol. 93, No. 11, 1965, p. 687–96. [Includes values for sea ice.]Google Scholar

Stepanov, V. N. O vozmozhnosti i tselesoobraznosti unichtozheniya arkticheskikh Pdov . Problemy Severa , Vyp. 7, 1963, p. 188–22. [Discusses whether Arctic sea ice would reappear if destroyed and what effects would be. English translation: Problems of the. North, No. 7, 1964, p. 129–33 (National Research Council of Canada).]Google Scholar

Sytinskiy, A. D. Tripol’nikov, V. P. Nekotoryye rezul’taty issledovaniy yestestvennykh kolebaniy ledyanykh poley tsentral’noy Arktiki . Izvestiya Akademii Nauk SSSR, Seriya Geofizicheskaya , 1964, No. 4, p. 615–21. [Seismological observations. Discussion of importance of various kinds of vibrations. English translation in Bulletin of the Academy of Sciences of the U.S.S.R. Geophysical Series, 1964, No. 4, p. 370–741Google Scholar

Tabata, T. Fujino, K. Kaihyō no rikigaku no seishitsu no kenkyū. VIII . Teion-kagaku , Ser. A, Vol. 23, 1965, p. 157–66. [Results of cantilever beam tests on shore-fast ice in situ. English summary.]Google Scholar

Williams, G. P. Correlating freeze-up and break-up with weather conditions. Canadian Ceotechnical Journal, Vol. 2, No. 4, 1965, p. 313–26. [The results of studies, and usefulness of these relationships for a small fresh-water lake.]Google Scholar

Bennett, R. G. Glacial lake overflow channels, south Svartisen. Norsk Polarinstitutt. Arbok, 1964 [pub. 1966],p. 236–39. [Nordland, north Norway. Field work during Cambridge expeditions 1959–64.]Google Scholar

Craig, B. G. Notes on moraines and radiocarbon dates in northwest Baffin Island, Melville Peninsula, and northeast District of Keewatin. Canada. Geological Survey, Paper 65–20, 1965, [iii], 7 p.Google Scholar

Crandell, D. R. Miller, R. D. Post-hypsithermal glacier advances at Mount Rainier, Washington. U.S. Geological Survey. Professional Paper 501-D, 1964, p. D110–14. [Volcanic ash layers and tree ring data used to date advances 3500-2000 B.F.]Google Scholar

Derbyshire, E., and others. A glacial map of Tasmania, by E. Derbyshire, M. R. Banks, J. L. Davies and J. N. Jennings. Royal Society of Tasmania. Special Publication No. 2, 1965, 11 p., map. [A summary of present knowledge of the glacial features of Tasmania.]Google Scholar

Dort, W. jr. Antarctic cirques and glaciated valleys. Antarctic Journal of the U.S., Vol. 1, No. 4, 1966, p. 137–38. [Studies conducted at 48 different locations, and highly informative aerial observations. The purpose was for comparison with temperate region types.]Google Scholar

Gillberg, M. A statistical study of till from Sweden. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 87, Pt. 1, No. 520, 1965, p. 84–108. [Study of particle size distribution and weight distribution. Suggests method may be useful in developing theories of transport and deposition.]Google Scholar

Gjessing, J. Deglaciation of southeast and east-central south Norway. Norsk Geografisk Tidsskrift, Bd. 20, Ht. 5, 1965–66, [pub.] 1966, p. 133–49. [A short survey of the deglaciation, stressing the glacio-fluvial activity.]Google Scholar

Holmes, G. W. Lewis, C. R. Quaternary geology of the Mount Chamberlin area, Brooks Range, Alaska. U.S. Geological Survey. Bulletin 1201-B, 1965, 32 p. [Includes glacial deposits and frozen ground features.]Google Scholar

Kuc, M. Deglaciation of Treskelen- I’reskelodden in Hornsund, Vestspitsbergen, as shown by vegetation. Studio Geologica Polonica (Warszawa), Vol. 11, 1964, p. 197–205. [Field work in 1958. Succession of plant communities during retreat of glacier 1890–1958. Polish summary.]Google Scholar

Lliboutry, L. Idées actuelles concernant les grandes glaciations. Bulletin de l’Association Française pour l’Étude du Quaternaire, No. 3–4, 1965, p. 257–65. [The great glaciations occur as a result of auto-oscillations in the atmosphere of the oceans and the inland ice systems.]Google Scholar

Lundqvist, J. Glacial geology in northeastern Newfoundland. Geologiska Fdreningens i Stockholm Förhandlingar, Vol. 87, Pt. 3, No. 522, 1965, p. 285–306. [Field work in 1962.1Google Scholar

Mattsson, Å. Fynd av stromatolitkalk utanför Svartisen i Norge. Swath Geografisk. Årsbok, Årg. 41, 1965, p. 177–78. [Observations of stromatolitic lime crust on rock newly free of ice, Osterdalsisen, north Norway.]Google Scholar

Michot, J. Souchez, R. La composition minéralogique des moraines, preuve de l’érosion glaciaire régressive en Antarctique. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 261, No. 20, 1965, p. 4155–58.Google Scholar

Miller, M. M. Prather, B. W. Teleconnection problems in the glaciation of the Himalaya and of the north Pacific Coast Ranges. Proceedings of the sixteenth Alaskan Science Conference, College, Alaska, August 29—September 1, 1965, 1966, p. 167–75. [In the Himalaya glaciers advanced recently close to their Pleistocene extent. This may be due to tectonic changes.]Google Scholar

Thomas, C. W. Late Pleistocene and recent climates as inferred from ocean bottom cores. Proceedings of the fifteenth Alaskan Science Conference, College, Alaska, August 31-September 4, 1964, 1965, p. 73–82. [In high latitudes present climate is warmest since Wisconsin maximum; evidence for lack of bipolar synchronism.]Google Scholar

Warren, C. R. Wright Valley: conjectural volcanoes. Science, Vol. 149, No. 3684, 1965, p. 658. [Suggests features in this region of Antarctica are due to catastrophic flooding caused by melting of ice by volcanic eruption west of Wright Valley.]Google Scholar

Anderson, G. S. Hussey, K. M. Preliminary investigation of thermokarst development on the North Slope, Alaska. Proceedings of the Iowa Academy of Science, Vol. 70, 1963, p. 306–20. [Observations of development and discussion of conditions.]Google Scholar

Baranov, I. Y. Printsipy geokriologieheskogo (merzlotnogo) rayonirovaniya oblasti mnogoletnmerzlykh gornykh porod . Moscow, Izdatel’stvo “Nauka” [Publishing House “Nauka”], 1965. 150 p. [Basis for classification of permafrost types.]Google Scholar

Bennett, R. G. Periglacial features of the Østerdalsisen outwash plain, Svartisen. Norsk Polarinstituti., Årbok, 1964 [pub. 1966], p. 233–36. [Nordland, north Norway. Field work during Cambridge expeditions in 1957–64.]Google Scholar

Bottinelli, A. M., and others. Contribucion al conocimiento de la poblacion en la zona periglaciaria del Lago Argentino, [by] A. M. Bottinelli, S. E. Cipolla, M. S. Gándola, A. M. Leis [and] E. Membrado. Instituto Nacional del Hielo Continental Patagónico. Publicación (Buenos Aires), No. 7, 1964, p. 14–41.Google Scholar

Dionne, J. C. Formes de cryoturbation fossiles dans le sud-est du Québec. Cahiers de Géographie de Québec, 10e An., No. 19, 1966, p. 89–100. [About 60 ice-wedges were observed in unconsolidated late Pleistocene and lower Holocene deposits. These forms indicate the existence of a periglacial climate during the late Wisconsin between 12,500 and 10,000Google Scholar

Freden, S. Mechanism of frost heave and its relation to heat flow. Proceedings of the sixth International Conference on Soil Mechanics and Foundation Engineering, Montreal, Sept. 8–15, 1965, Vol. 1, Div. 1–2,1965, p. 41–45. [Theory which indicates that rate of frost heave is approximately proportional to temperature gradient.]Google Scholar

Johnston, G. H. Brown, R. Jr. E. Occurrence of permafrost at an Arctic lake. Nature, Vol. 211, No. 1052, 1966, p. 952–53. [Ground temperature measurements indicate that the thermal effect of the lake extends for some distance beyond its perimeter.]Google Scholar

Popov, A. I., ed. Podzemnyy led . Moscow, Izdatel’stvo Moskovskogo Universiteta [Publishing House of Moscow University], 1965. 217 p. [Soviet papers presented at seventh meeting of INQUA, 1965.]Google Scholar

Ragg, J. M. Bibby, J. S. Frost weathering and solifluction products in southern Scotland. Geografiska Annaler, Vol. 48a, No. 1, 1966, p. 12–23. [Extent of detritus due to intensive frost weathering found to be much greater than was hitherto supposed.]Google Scholar

Raup, H. M. The structure and development of turf hummocks in the Mesters Vig district, northeast Greenland. Meddelelser om Grønland, Bd. 166, Nr. 3, 1965, 112 p. [Field work in 1956–58 and 1960.]Google Scholar

Romanovskiy, N. N. O temperaturnom rezhime merzlykh tolshch nebol’shoy moshchnosti, podstilayemykh vodonosnymi sloyami . Vestnik Moskovskaga Universiteta. Seriya 4. Geologia , 1965, No. 3, p. 53–58.Google Scholar

Vyalov, S. S. Yermakov, V. F. Novyy metod opredeleniya dlitel’noy prochnosti merzlykh gruntov . Merzlotnyye Issledovaniya (Moscow University), Vyp. 3. 1966, p. 229–41. [Suggests use of stress relaxation tests.]Google Scholar

Wiegand, G. Fossile Pingos in Mitteleuropa. Würzóurger Geographische Arbeiten, Ht. 16, 1965, 152 p.[Symmetrical filled-in cavities found in central Europe were formed by collapse of pingos at end of Ice Age.]Google Scholar

Williams, J. R. Ground water in permafrost regions; an annotated bibliography. U.S. Geological Survey. Water Supply Paper 1792, 1965, 294 p. [Includes brief summary of frozen ground research.]Google Scholar

Williams, L. Regionalization of freeze-thaw activity. Annals of the Association of American Geographers, Vol. 54.No. 4, 1964, p. 597–611. [Compares with distribution of precipitation, vegetation and soils.]Google Scholar

Yong, R. N. Soil suction effects on partial soil freezing. Highway Research Record, No. 68, 1965, p. 31–42. [Measurement of relation between soil suction and quantity of water remaining unfrozen.]Google Scholar

Gotaas, Y. Benson, C. S. The effect of suspended ice crystals on radiative cooling. Journal of Applied Meteorology, Vol. 4, No 4, 1965, p. 446–53. [Experiments during very cold ice fogs show radiative cooling from ice crystals in the air to be important.]Google Scholar

Holroyd, E. W. A suggested origin of conical graupel. Journal of Applied Meteorology, Vol. 3, No. 5, 1964, p. 633–36. [Laboratory examination of samples and radiosonde studies suggest conical graupel forms from needle-shaped ice crystals.]Google Scholar

Latham, J. Miller, A. H. The role of ice specimen geometry and impact velocity in the Reynolds-Brook theory of thunderstorm electrification. Journal of the Atmospheric Sciences, Vol. 22, No. 5, 1965, p. 505–08. [Experiments on ice spheres rotated in streams of snow crystals show that charge acquired increases markedly with impact velocity and surface irregularity. Implications for thunderstorm electrification discussed.]Google Scholar

Macklin, W. C. List, R. Comments on the “general heat and mass exchange of spherical hailstones”. Journal of the Atmospheric Sciences, Vol. 21, No. 2, 1964, p. 227–28. [Comments by Macklin on earlier work by List and others with reply by List.]Google Scholar

Munn, R. E. Descriptive micrometeorology. New York and London, Academic Press, 1966. xiv, 245 p. (Advances in Geophysics. Supplement 1.) [Includes chapter on “The air over snow and ice surfaces”, p. 133–42.]Google Scholar

Nagel, J. F. Formung and Bildung von Graupel and Hagel. Berichle des Deutschen Wetterdienstes, Bd. 12, Ht. 91, 1963, p. 129–31. [Fall experiments show graupel forms in conical shape with apex down, but may be subsequently rotated. English abstract.]Google Scholar

Picca, R. Conduction de la chaleur à l’intérieur d’un grêlon sphérique. Journal de Recherches Atmosphériques, Tom. 1, No. 1, 1964, p. 51–53. [Measurement of temperature inside artificial hailstone while warming. English abstract.]Google Scholar

Picca, R. Mazzaschi, J. Le réchauffement d’une sphère de glace. Journal de Recherches Atmosphériques, Tom. 1, No. 1, 1964, p. 45–49. [Measurements of surface heat transfer coefficient for artificial hailstone. English abstract.]Google Scholar

Rogers, R. R. Tripp, B. R. Some radar measurements of turbulence in snow. Journal of Applied Meteorology, Vol. 3, No. 5, 1964, p. 603–10. [Use of Doppler spectrum of reflections from snow to determine turbulent structure of wind.]Google Scholar

Thomann, H. Determination of the size of ice crystals formed during condensation of water in wind tunnels and of their effect on boundary layers. Flygtekniska Försölesanstalten. Meddelanden (Stockholm), No. 101, 1964, 80 p.Google Scholar

Zander, R. Spectral scattering properties of ice clouds and hoarfrost. Journal of Geophysical Research, Vol. 71, No. 2, 1966, p. 575–78. [Measurement in the infrared.]Google Scholar

Akitaya, E. Shimozarame setsu no kenkyū. I . Teion-kagaku , Ser. A, Vol. 23, 1965, p. 67–74. [Laboratory study of growth of depth hoar in snow. English summary.]Google Scholar

Cooper, C. F. Snow cover measurement. Photograrnmetric Engineering, Vol. 31, No. 4, 1965, p. 611–19.[Practicality of using photogrammetry to determine the volume of snow on an area.]Google Scholar

Endo, Y. Yuki nadare hassen kikō no kōsa . Teion-kagaku , Ser. A, Vol. 23, 1965, p. 75–86. [Theoretical study of conditions of avalanche release on a concave surface. English summary.]Google Scholar

Engelmann, R. J. Perkins, R. W. Snow and rain washout coefficients for process plant radioiodine vapour. Nature, Vol. 211, No. 5044, 1966, p. 61–62. [Letter. Experiments show amount of iodine vapour captured from the atmosphere by rain and snow.]Google Scholar

Herman, J. R. Radio noise by Antarctic blizzards. Journal of Geomagnetism and Geoelectricity, Vol. 16, No. 2, 1964, p. 152–60. [Spectral power distribution from 50 kc./sec. to 20 Mc./sec.]Google Scholar

Kinosita, S. Sekisetsu he no ensui no oshikomi . Teion-kagaku , Ser. A, Vol. 23, 1965, p. 17–37. [Variation of behaviour of snow with angle of cone and speed of intrusion. English summary.]Google Scholar

Klyukin, N. K. Nekotoryye voprosy melioratsii klimata putem vozdeystviya na snezhnyy pokrov . Problemy Severa , Vyp. 7, 1963, p. 65–84 [Discusses methods of increasing accumulation and increasing or decreasing snow melt. English translation: Problems of the North, No. 7, 1964, p. 67–90 (National Research Council of Canada)]Google Scholar

McKay, G. A. Relationships between snow survey and climatological measurements for the Canadian Great Plains. Proceedings of the Western Snow Conference, 32nd annual meeting, 1964, [pub.] 1964, p. 9–19. [Measurements at climatological stations can be used to predict snow cover conditions on nearby snow courses. Discussion p. 19.]Google Scholar

Magono, C. Kikuchi, K. On the positive electrification of snow crystals in the process of their melting. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 41, No. 5, 1963, p. 270–77. [Experiments and discussion in terms of observed electric field during snowfall.]Google Scholar

Mellor, M. Snow mechanics. Applied Mechanics Reviews, Vol. 19, No. 5, 1966, p. 379–89. [General account.]Google Scholar

Osokin, I. M. Khimicheskiy sostav snezhnogo pokrova na territorii SSSR . Izvestjya Akademii Nauk SSSR. Seriya Geograflcheskaya , 1963, No. 3, p. 26–34. [Review e]’ Soviet literature and results of detailed studies in Transbaykalya.]Google Scholar

Oura, H. Kobayashi, D. Sekisetsu no ko ni taisuru sanren; kyúshia keisii sokuteihô shian . Teionkagaku , Ser. A, Vol. 23. 1965, p. 87–98. [Results show deviations from Lambert’s law near the surface.]Google Scholar

Poggi, A. L’évolution de la neige déposée á moyenne altitude. La Houille Blanche, 20e An., Nos. 4–5, 1965, p. 3–40. [Report of the results of four years of operation of a laboratory set up at Col de Porte in October 1959.]Google Scholar

Poulton, H. J. James Edward Church: bibliography of a snow scientist. Nevada University. Bibliographical Series No. 4, 1964, 35 p. [Includes some biographical material.]Google Scholar

Pupkov, V. N. Formation, distribution. and variation of snow cover on the Asiatic territory of the U.S.S.R. Soviet Hydrology. Selected Papers. 1964, No. 5, p. 514–21.Google Scholar

Salm, B. Anlage zur Untersuchung dynamischer Wirkungen von bewegtem Schnee. Zeitschrift für angewandte Mathematik und Physik, Vol. 15, Fasc. 4, 1964, p. 357–75. [Description of an installation to observe and measure artifically released masses of snow sliding over an inclined plane and especially the impact pressure on an obstacle. Also published as Mitteilungen des Eidgenössischen Institutes für Schnee- und Lawinenforschung, No. 21, 1964.]Google Scholar

Schulz, L. Ober die Ursachen von Schneereichen und Schneearmen Wintern im Harz. Meteorologische Rundschau, Bd. 18, Ht. 3, 1965, p. 91–92. [Data for 73 winters analysed for correlations between snowfall and temperature deviations.]Google Scholar

Shimizu, H. “Long prism” crystals observed in the precipitation in Antarctica. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 41, No. 5, 1963, p. 304–05. [Results of studies of snow crystal shapes at “Byrd” station, Antarctica.]Google Scholar

Tillotson, J. G. Attenuation of sound over snow-covered fields. Journal of the Acoustical Society of America, Vol. 39, No. 1, 1966, p. 175–73. [Letter. Measurements of characteristic impedance and complex propagation constant.]Google Scholar

[Union Géodésique et Géophysique Internationale.] Union de Géodésie et Géophysique Internationale. Association Internationale d’Hydrologie Scientifique. Commission pour la Neige el la Glace. Division Neige Saisonnière et Avalanches. Symposium international sur les aspects scientifiques des avalanches de neige, 5–10 avril 1965, Davos, Suisse. Gentbrugge, Association Internationale d’Hydrologie Scientifique, 1966. 424 p. (Publication No. 69 de l’Association Internationale d’Hydrologie Scientifique.) Bel. fr. 300. [”Organisation”, p. 5–10; H. Hoinkes, Presidential address, p. 11–13; M. R. de Quervain, “Problems of avalanche research”, p. 15–22; A. Poggi and J. Plas, “Conditions météorologiques critiques pour le déclenchement des avalanches”, p. 25–34; V. N. Akkuratov, “Meteorological conditions of avalanche formation in the Khibiny”, p. 35–42;J. Martinet, “Snow cover density changes in an experimental watershed”, p. 43–52; V. M. Kotlyakov and M. Ya. Plain, “The influence of drifting on snow distribution in the mountains and its role in the formation of avalanches”, p. 53–60; T. Zingg, “Relation between weather situation, snow metamorphism and avalanche activity”, p. 61–64; W. Ambach and F. Howorka, “Avalanche activity and free water content of snow at Obergurgl (1980m. a.s.l., spring 1962)”, p. 65–72; M. I. Iveronova, “The hydrological role of snow avalanches”, p. 73–77; I. S. Sosedov and I. V. Severskiy, “On hydrological role of snow avalanches in the northern slope of the Zailiysky Alatau”, p. 78–85; A. Roch, “Les variations de la resistance de la neige”, p. 86–99; M. Mellor and J. H. Smith, “Strength studies on snow”, p. 100–13; S. N. Kartashov, “Mechanical properties of snow and firn”, p. 114–18; R. O. Ramseier and G. W. Sander, “Sintering of snow as a function of temperature”, p. 119–27; M. Mellor, “Some optical properties of snow”, p. 128–40; R. Haefeli, “Considérations sur la pente critique et la coefficient de pression au repos de la couverture de neige”, p. 141–53; M. R. de Quervain, “Measurements on the pressure at rest in a horizontal snow cover”, p. 154–59; G. E. H. Ballard and R. W. McGaw, “A theory of snow failure”, p. 160–69; C. Jaccard, “Stabilité des plaques de neige”. p. 170–81; A. Roch, “Les déclenchements d’avalanches”, p. 182–95; Yu D. Moskalev, “On the mechanism of the formation of wet snow avalanches”, p. 196–98; B. Salm, “Contribution to avalanche dynamics”, p. 199–214; M. Shoda, “An experimental study on dynamics cf avalanches snow”, p. 215–29d; H. R. in der Gand and M. Zupanèic, “Snow gliding and avalanches”, p. 230–42; H. Frutiger, “Behaviour of avalanches in areas controlled by supporting structures”, p. 243–50; C. C. Bradley, “The snow resisto-graph and slab avalanche investigations”, p. 255–60; E. [R.] LaChapelle and R. M. Stillman, “The control of snow metamorphism by chemical agents”, p. 261–66; L. H. Nobles, “Slush avalanches in northern Greenland and the classification of rapid mass movements”, p. 267–72; B. Cottman, “A wet snow avalanche on a slope of 12 degrees”, p. 273–75; C. F. Capello, “Contributions de l’Institut Italien de Géographie Alpine à l’étude des neiges saisonnières et des avalanches”, p. 276–82; G. K. Tushinskiy, “Major trends in the study of avalanche danger in the U.S.S.R.”, p. 283–85; V. Kozlik, “La couche dc neige et sa mesure au-dessus dc la zone forestière (dans la région des avalanches)”, p. 286–93; K. Chomicz, “Les avalanches dans les montagnes de Tatra. Méthodes de mesures”, p. 294–303; B. Morales, “The Huascaràn avalanche in the Santa valley, Peru”, p. 304–15; R. Haefeli, “Note sur la classification, le mécanisme et le contrôle des avalanches de glace et des crues glaciaires extraordinaires”, p. 316–25; W. O. Field, “Avalanches caused by the Alaska earthquake of March 1964”, p. 326–31; M. Kahn, “Considérations préliminaires sur la répartition chronologique des avalanches de neige”, p. 332–40; R. T. Beaumont, “Evaluation of the Mt. Hood pressure pillow snow gage and application to forecasting avalanche hazard”, p. 341–49; E. [R.] LaChapelle, “Avalanche forecasting—a modern synthesis”, p. 350–56; Kh. D. Peev, “Geomorphic activity of snow avalanches”, p. 357–68; L. de Crécy, “Statistique et prévision d’avalanches”, p. 369–74; A. Fukui, “The classification of snow avalanches in Japan”, p. 377–81; G. K. Tushinskiy, “Avalanche classification, and rhythms in snow cover and glaciation of the northern hemisphere in historical times”, p. 382–93; K. S. Lossev, “Genetic classification of avalanches”, p. 394–96; M. Vanni, “Pour une classification géographique des avalanches”, p. 397–407; K. Chomicz, “Essai d’une classification des avalanches”, p. 408–09; M. R. de Quervain, “On avalanche classification: a further contribution”, p. 410–17; M. R. de Quervain, “Conclusions drawn from the Symposium”, p. 421.]Google Scholar