Bird, J. B The physiography of Arctic Canada, with special reference to the area south of Parry Channel. Baltimore. Johns Hopkins Press, 1967. xix, 336 p., map [in end-pocket]. [Canada north of 60° N. (except Yukon Territory).[Includes sections on present-day distribution of glaciers, permafrost, periglacial mass movement and patterned ground, the role of snow and of sea, river and glacier ice, and on waning of Quaternary ice sheet.]Google Scholar

Davies, J. L Landforms of cold climates. Cambridge, Mass., and London, The M.I.T. Press, Massachusetts Institute of Technology, [^e1969]. xvi, 200 p., illus. (An Introduction to Systematic Geomorphology, Vol. 3.)Google Scholar

Fukuta, N, Ice nucleation in the Venus atmosphere, by Fukuta, N.,Wang, T.-L., Libby, W.F. Journal of the Atmospheric Sciences, Vol. 26, No. 5, Pt. 2, 1969, p 142–45. [Laboratory tests of ice nuclei with CO₂, present and deductions about ice in Venus atmosphere.]2.0.CO;2>CrossRefGoogle Scholar

Kick, W Alexander von Humboldts Wirken für die Hochgebirgsforschung in Asien, besonders über die Brüder Schlagintweit. Petermanns Geographische Mitteilungen, 113. Jahrg., 2. Quartalsht., 1969, p 89–99. [History of Humboldt's interest in exploration and the consequent glaciological work of the Schlagintweit brothers. English summary.]Google Scholar

Kobayashi, T Kitahara, T Sukēto-rinku no hyōshitsu-chōsa [Studies on the properties of ice in skating rinks]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 26, 1968, p 297–314. [Measurements of surface temperature and indentation hardness. English summary, p. 313.]Google Scholar

Crozaz, G Fission products in Antarctic snow, an additional reference level in January 1965. Earth and Planetary Science Letters, Vol. 6, No. 1, 1969, p 6–8. [Discusses occurrence of recent artificial radio-activity levels, used to date snow accumulation rates in Antarctica.]Google Scholar

Evans, S, Glacier sounding in the polar regions: a symposium. Geographical Journal, Vol. 135, Pt. 4, 1969, p 547–63, plates. [Contains the following papers: S. Evans, “The VHF radio echo technique”, p. 547–48; P. Gudmandsen, “Airborne radio echo sounding of the Greenland ice sheet”, p. 548–51. Swithinbank, C. [W. M.], “Airborne radio echo sounding by the British Antarctic Survey”, p. 551–53; Hattersley-Smith, G. “Results of radio echo sounding in northern Ellesmere Island, 1966”, p. 553–57; Robin, G. de Q , “Long-range, radio echo flights over the Antarctic ice sheet”, p. 557–59; discussion,p. 559–63]CrossRefGoogle Scholar

Murozumi, M, Chemical concentrations of pollutant lead aerosols, terrestrial dusts, and sea salts in Greenland and Antarctic snow slrata, [by] Murozumi, M,Chow, T.J,Patterson, C Geochimiea et Cosmochimica Acta. Vol, 33, No. 10, 1969, p, 1247–94. [Observations and possible archaeological significance.]Google Scholar

Allen, L.C Kollman, P. A A theory of anomalous water. Science, Vol. 167, No. 3924, 1970, p 1443–54. [Theory of anomalous water as a structure related to ice Ic as graphite is to diamond.]Google Scholar

Anderson, B. J,, Influence of methyl 2-cyanoacrylate monomer on the habit of ice crystals grown from the vapor, by Anderson, B.J,Sutkoff, J.D,Hallett, J Journal of the Atmospheric Sciences, Vol. 26, No. 4, 1969, p 673–74. [Ice crystals in presence of this substance grow from the vapour as thin fibres parallel to the c-axis.]Google Scholar

Angell, C. A Sake, E. J Vitreous water: identification and characterization. Science, Vol. 168, No. 3928, 1970, p 280–81. [Review of experimental evidence for a glass transition in ice and discussion of its peculiarities.]Google Scholar

Barak, A Dagan, G An analytical investigation of the flow in the saturated zone of ice counterwashers. A[merlcan] I[nstitute of] Ch[emical] E[ngineers] Journal, Vol. 16, No. 1, 1970, p 9–17. [Theoretical study of flow of brine through an ice bed.]Google Scholar

Bascom, W. D,, Ice adhesion to hydrophibic and hydrophobic surfaces, [by] Bascom, W.D,Cottington, R.L,Singleterry, C.R Journal of Adhesion, Vol. 1, October 1969, p 246–63. [Study of adhesional shear strength and of structure of ice near the surface.].Google Scholar

Bates, J. B,, Dynamics of some lattice models of polywater, [by] Bates, J.B,Lippincott, E.R,Mikawa, Y,Jakobsen, R.J Journal of Chemical Physics, Vol. 52, No. 7, 1970, p 3731–39. [Calculations give excellent agreement with infra-red and Raman data. Model consists of two-dimensional network of water molecules.]Google Scholar

Botsaris, G. D,, Crystallization. Part III. Data concerning particular system and product, by Botsaris, G.D Industrial and Engineering Chemistry, Vol. 61, No. 12, 1969, p 65–79. [Review of papers published 1967-69. Has separate section on the crystallization aspects of ice.]Google Scholar

Brian, P. L. T,, Transport of heat and mass between liquids and spherical particles in an agitated tank, [by] Brian, P .L. T,Hales, H.B,Sherwood, T.K A[merican] I[nstitute of] Ch[emical] E[ngineers] Journal, Vol. 15, No. 5, 1969, p 727–33. [Data for heat transfer from water to melting ice spheres.]Google Scholar

Castellion, G. A,, Polywater: methods for identifying polywater columns and evidence for ordered growth, [by] Castellion, G.A,Grabar, D.G,Hession, J,Burkhard, H Science, Vol. 167, No. 3919, 1970, p 865–68. [Refractive index measurements give rapid indication of polywater formation and indicate it is initially ordered.]Google Scholar

Corbató, C. E Thermal diffusivity and conductivity of glacier ice. Eos (Transactions. American Geophysical Union), Vol. 50, No. 4, 1969, p 142. [Abstract only. Measurements at Wilkes station, Antarctica, reinterpreted allowing for solar radiation.]Google Scholar

Delsemme, A. H Wenger, A Super dense water ice. Science, Vol. 167, No. 3914, 1970, p 44–45. [Below 100 K ice deposited from the vapour at low temperatures had a density of 2.32 ± 0.15 g cm^-3,]Google Scholar

Domian, H. A. Bolling, G. F. Continuous solidification pores. Metals and Materials, Vol. 3, No. 10, 1969, p 394–95. [Letter, Includes observation of effect of supersaturation of gas on growth of gas pores in ice frozen from water.]Google Scholar

Edwards, G. R,, Two-dimensional phase changes in water absorbed on ice-nucleating substrates, [by] Edwards, G.R,Evans, L. F,Zipper, A.F Transactions of the Faraday Society, Vol. 66, No. 5, Pt. 1, 1970, p 230–34. [Study of ordered ice-like state on some substrates at low temperatures.]Google Scholar

Elsele, I, Temperature dependence of photocurrent in y-irradiated alkaline ice. Location of energy levels of trapped electrons, [by] Eisele, I,Lapple, R,Kevan, L Journal of the American Chemical Society, Vol. 91, No. 23, 1969, p 6504–05. [Letter. Dependence from 4 to 77 K and above 77 K shows nature of transition and presence ofshallow traps.]Google Scholar

Fletcher, N. H Active sites and ice crystal nucleation. Journal of the Atmospheric Sciences, Vol. 26, No. 6, 1969, p 1266–71. [Suggests active sites are re-entrant corners or jogs in growth steps. Theory for nucleation by spherical particle with conical pit.]Google Scholar

Fletcher, N. H The chemical physics of ice. Cambridge, University Press, 1970. xi, 271 p. (Cambridge Monographs on Physics.) [Monograph describing recent developments in knowledge of structure and defects of ice and the resulting physical properties.]Google Scholar

Fukuta, N Experimental studies on the growth of small ice crystals. Journal of the Atmospheric Sciences, Vol. 26, No. 3, 1969, p 522–31. [Fall velocities and growth rates of freely falling ice crystals in a nucleated supercooled fog. Modification of theory required to explain results.Google Scholar

Haridasan, T. M Govindarajan, J Lattice dynamics of hexagonal ice. Chemical Physics Letters, Vol. 4, No. 1, 1969, p 11–12. [Deduced on basis of clastic constants. Normal mode frequencies agree with experiment.]Google Scholar

Harriott, P The growth of ice crystals in a stirred tank. A[meriean] I[nstitute of] Ch[emical] E[ngineers] Journal. Vol. 13, No. 4, 1967, p 755–59. [Rate of growth of crystals growing in water or sodium chloride solution compared with rate predicted from heat-transfer theory.)Google Scholar

Hase, H Kevan, L EPR studies on trapped species produced by tritium 00DF; particles in alkaline and acid ices at 77° K. Journal of Chemical Physics, Vol. 52, No. 6, 1970, p 3183–88. [Comparison with results for y-irradiated ice.]Google Scholar

Huffman, P. J Thuksby, W. R.jr Light scattering by crystals. Journal of the Atmospheric Sciences, Vol. 26,No. 5, Pt. a, 1969, p 1073–77. [Measurement for microscopic ice crystals in laboratory cold chamber.]2.0.CO;2>CrossRefGoogle Scholar

Hunter, L. M,, Low-energy electron reflection spectrometry for thin films of n-hexane, benzene, and ice at 77° K, [by] Hunter, L.M,Lewis, D,Hamill, W.H journal of Chemical Physics, Vol. 52, No. 4, 1970, p 1733–39. [Measurement and interpretation.]Google Scholar

Jancso, G, Vapour pressure of H₂ ¹⁸O ice (I) (— 17° to o°) and H₂ ^l8O water (o° to 16°), [by] Jancso, G,Pupezin, J,Van Hook, W. A. Nature, Vol. 225, No. 5234, 1970, p.723. [Letter. Experiments which disagree with previous data.]Google Scholar

Knacke, R. F,, Infrared spectra of highly reddened stars: a search for interstellar ice grains, by Knacke, R.F,Cudaback, D.D,Gaustad, J.E Astrophysical Journal, Vol. 158, No. 1, Pt. 1, 1969, p 151–60. [Absence of absorption bands implies that interstellar grains contain very little ice.]Google Scholar

Kubarev, S. I Shedrin, M. I A model calculation of protonic mobility in ice. International Journal of Quantum Chemistry, Vol. 3, No. 6, 1969, p 893–901. [Theory based on strong coupling between protons and phonons gives results in qualitative agreement with experiment.]Google Scholar

Kurtin, S. L,, “Polywater": a hydrosol? [By] Kurtin, S.L,Mead, C.A,Mueller, W.A,Kurtin, B.C,Wolf, E.D Science, Vol. 167, No. 3926, 1970, p 1720–22. [Suggestion that anomalous water owes its properties to dispersed particulate matter not to a polymeric form of water.]Google Scholar

Layton, R. G Fletcher, N. H Comments on “Ice nucleation behavior of silver iodide smokes containing a soluble component”. Journal of the Atmospheric Sciences, Vol. 26, No. 4, 1969, p. 774–75. [Comments by Layton on paper by Fletcher, ibid., Vol. 25,No. 6, 1968, p 1058–60, and reply by Fletcher.]Google Scholar

Layton, R. G Steger, J Nucleation of ice on silver iodide. Journal of the Atmospheric Sciences, Vol. 26, No. 3, 1969, p 518–21. [Study of supercoolings required for condensation and deposition.]Google Scholar

Leiohly, H. P.jr Penetrating punch. Metals and Materials, Vol. 4, No. 2, 1970, p 49. [Letter. Observation that grape juice and “ginger ale” will separate ice crystals from each other.]Google Scholar

Levi, L Different interpretations of the growth rates of ice dendrites in supercooled water. Journal of Chemical Physics, Vol. 52, No. 7, 1970, p 3854–55. [Letter. Discussion of results found by Pruppacher and by Macklin and Ryan.]Google Scholar

Linnett, J. W Structure of polywater. Science, Vol. 167, No. 3926, 1970, p 1719–20. [Discusses possible structures for high density concentrate of anomalous water.]Google Scholar

Lippincott, E. R,, Polywater, [by]Lippincott, E.R,Stromberg, R.R,Grant, W.H,Cessac, G.L Science, Vol. 164, No. 3887, 1969, p 1482–87. [Infra-red and Raman spectra suggest very strong OHO bond with H midway between two O. Possible structures lor polywater discussed.]Google Scholar

Mal'tsev, V. A Nekrasov, L I. K voprosu o vysshey perekisi vodoroda i zamorozhennykh radikalakh. XIII. Elektronograhcheskoye issledovaniye amorfnogo l'da, sistem H₂O₂ - H₂O i perekisno-radikal'nykh kondensatov [Higher H₂O₂ and frozen free radicals. XIII. Electron diffraction study of amorphous ice, the H₂O₂ H₂O system and peroxy free radical condensates]. Zhuntal Fizicheskoy Khimii, Tom. 43, Vyp. 5, 1969. p. 1153–58. [Temperature of crystallization of amorphous ice with no cubic ice found to be — 115°C English translation in Russian Journal of Physical Chemistry, Vol. 43, No. 5, 1969, p. 641–45.]Google Scholar

Miksch, E. S Solidification of ice dendrites in flowing supercooled water. Transactions of the Metallurgical Society of AIME, Vol. 245, No. 9, 1969, p 2069–72. [Effect of convection on morphology and growth rate of ice dendrites.]Google Scholar

Muguruma, J. Effects of surface condition on the mechanical properties of ice crystals. British Journal of Applied Physics (Journal of Physics, D), Ser. 2, Vol. 2, No. 11, 1969, p 1517–25. [Large difference in properties of chemically and mechanically polished ice single crystals.]Google Scholar

Odpencrantz, F. K An apparent confirmation of the transient nature of whiskers on ice crystals. Journal of the Atmospheric Sciences, Vol. 27, No. 1, 1970, p 167–68. [Formvar replicas show whisker remnants.]Google Scholar

Owe-bero, T. G Gaukler, T A. Electrification experiments with Agi in the system: water vapor, liquid water and ice. Journal of the Atmospheric Sciences, Vol. 26, No. 4, 1969, p 675–83. [Measurement of charge on AgI particles in air currents as sorption, freezing and melting lake place.]Google Scholar

Plumb, R. C Chemical principles exemplified. The snowmaking machines. Journal of Chemical Education, Vol. 47, No. 3, 1970, p. 176. [Draws attention to thermodynamics involved in snowmaking machines using compressed air and water.]Google Scholar

Renker, B Phonon dispersion in D₂O-ice. Physics Letters A, Vol. 30, No. 9, 1969, p 493–94. [Neutron inelastic scattering study. Dispersion curves along [1120| and [l010] compared with Forslind's theory.]Google Scholar

Rousseau, D. L Porto, S. P. S Polywater: polymer or artifact? Science, Vol. 167, No. 3926, 1970, p 1715–19. [Analysis of samples prepared in same way as other “polywater” samples shows high concentration of impurities.]Google Scholar

Sakabe, Y, Dielectric dispersion of NaOH-doped ice at low temperatures, [by] Sakabe, Y,Ida, M,Kawada, S Journal of the Physical Society of Japan, Vol. 28, No. 1, 1970, p. 265. [By using purer water than before, dielectric constant found which is consistent with phase transition at ~60 K.]Google Scholar

Takahashi, T Electric potential of liquid water on an ice surface. Journal of the Atmospheric Sciences, Vol. 26, No. 6, 1969, p 1253–58. [Theoretical and experimental study. Discussion of implications for hailstone electrification and charging of melting snow.]2.0.CO;2>CrossRefGoogle Scholar

Takahashi, T Electric potential of a rubbed ice surface. Journal of the Atmospheric Sciences, Vol. 26, No. 6, 1969, p 1259–65. [Theoretical and experimental study of electric potential of ice surface rubbed by single crystal piece of ice.]Google Scholar

Tiller, W. A Migration of a liquid zone through a solid. Journal of Crystal Growth, Vol. 6, No. 1, 1969, p 77–85. [Analysis of data on migration of a droplet of aqueous solution through ice in a temperature gradient.]Google Scholar

Tseng, P. K Ritby, S. L Some further results on the concentration dependence of tin (IV) isomer shifts in ice. Chinese Journal of Physics (Taipei), Vol. 7, No. 1, 1969, p 50–52. [Study of effect of adding KF, or HCI in addition to HF, or of changing the ratio of KCl to HCl. Isomer shifts depend on type and concentration of anions, but not on different calions.]Google Scholar

Vanier, C. R Tien, C Free convection melting of ice spheres. A[merkan] I[nstitute of] Ch[emical] E[ngineers] Journal, Vol. 16, No. 1, 1970, p 76–82. [Experimental study of melting of ice spheres in water.]Google Scholar

Weisweiler, W Messung der lachstumsgeschwindigkeit lamellarer Eiskristallc gezüchtet am Tauspicgel. Zeitschrift für Meteorologie, Bd. 20, Ht. 11–12, 1968, p 327–36. [Study of nucleation and growth of lamellar ice crystals growing on a dew-point mirror. English summary.]Google Scholar

Weisweiler, W Wachstum lamellarer Eiskristalle unter instationären Züchlungsbedingungen auf einem Tauspiegel. Zeitschrift für Meteorologie, Bd. 20, Ht. 11–12, 1968, p.337–43. [Study of growth and evaporation of lamellar ice crystals of a dew-point mirror under controlled supersaturation and air flow velocity. English summary.]Google Scholar

Whalley, E Labbé, H. J. Optical spectra of orientationally disordered crystals. III. Infrared spectra of the sound waves. Journal of Chemical Physics, Vol. 51, No. 7, 1969, p 3120–27. [Theory of light absorption by translational vibrations in such crystals compared with measurements on ice.]Google Scholar

Williams, P. J Melting point behaviour of glacier ice. Nature, Vol. 220, No. 5168, 1968, p 689. [Comment on letter having same title by Radd, F.J,Oertle, D.H, ibid., Vol. 218, No. 5148, 1968, p 1242.]Google Scholar

Yen, YIN-CHAO. On the effect of density inversion on natural convection in a melted water layer. Chemical Engineering Progress Symposium Series, Vol. 65, No. 92, 1969, p 245–53. [Study of convective heal transfer in water above and below melting ice cylinder.]Google Scholar

Zweerink, G. R Roach, D. V Thermal accommodation coefficients of helium, neon and argon on an ice surface. Surface Science, Vol. 19, No. 1, 1970, p 249–54. [Determination at 77 K and 216 K.]Google Scholar

Ambach, W, Dcutcrium-Gehalt des Wassers im Gletseherabfluss,Von Ambach, W,Eisner, H,Moser, H,Stichler, W Naturwissenschaften, Bd. 57, Ht. 2, 1970, p 86. [Diurnal and long-period variations in deuterium content of stream below Kessel wand ferner, Austria.]CrossRefGoogle Scholar

Ambach, W, Untersuchung von charakteristischen Pollenspektren in Akkumulationsgebiet eines Alpengletschers (Kesselwandferner, (Etztaler Alpen, (Esterreich,Von Ambach, W,Bortenschlager, S,Eisner, H Pollen et Spores, Vol. 11, No. 1, 1969, p 65–72. [High content of Picea pollen in those summers which have maximum flowering of Picea. English and French summaries.]Google Scholar

Andersen, E Report of the geodetic, geophysic, and photogrammetric work at the west coast region of Greenland executed by the Danish Geodetic Institute in connection with the ice-cap work of E.G.I.G. Meddelelser om Grønland, Bd. 173, Nr. 4, 1969, 14 p. [Gives connection between northern terminal of E.G.I.G. network on ice sheet and Danish first order triangulation on west coast. Includes topographic map on scale 1: 50 000 of glacier Kangerdlugssûp sermerssua.]Google Scholar

Andrews, J. T Webber, P. J Lichenometry to evaluate changes in glacial mass budgets: as illustrated from north-central Baffin Island, N.W.T. Arctic and Alpine Research, Vol. 1, No. 3, 1969, p 181–94. [Lichen studies used to define ice margins from A.D. 1650 and hence glacier changes.JGoogle Scholar

Baker, P. E,, Volcanic activity at Deception Island in 1967 and 1969, by Baker, P.E,Davies, T.G,Roobol, M.J Nature, Vol. 224, No. 5219, 1969, p 553–60. [Eruptions, apparently associated with the caldera fault zone, have created a new island and a new 5 km fissure. Rift in overlying glacier released flood of water.]Google Scholar

Colbeck, S. C Evans, R. J Experimental studies related to the mechanics of glacier flow. Trends in Engineering, Vol. 21, No. 2, 1969, p 8–14. [Field experiments on Blue Glacier, Washington, U.S.A., including study of strain-rates in crevasse fields and creep tests on glacier ice at o° C]Google Scholar

Fedorov, B. A Radiolokatsionnyye issledovaniya lednikovogo pokrova Antarktidy [Radar studies of the Antarctic ice sheet]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 49, 1969, p 213–38. [Survey of Soviet and other work.]Google Scholar

Gerke, K Barometrische Höhenbestimmungen auf dem grönländischen Inlandeis bei der Internationalen Glaziologischcn Grönlandexpedition (EGIG) 1959. Meddelelser om Grønland, Bd. 173, Nr. 8, 1969, 77 p. [Barometric levellings on Greenland ice sheet, 1959. English and French summaries.]Google Scholar

Liestøl, O. Bremålinger i 1967. Norsk Polarinstitutt. Årbok, 1967 [pub. 1969], p. 183–90. [Mass balance measurements on four glaciers and front variations of thirteen glaciers in Norway. English ahslract.]Google Scholar

Mikhaliov, V. I The character of ice formation on Spitsbergen glaciers. Norsk Polarinstituti. Årbok, 1967 [pub. 1969], p. 129–38. [General description of glacier faciès as determined by Sovetskoy Shpitsbergenskoy Ekspeditsiya 1965 and 1966.]Google Scholar

Neave, K. G Savage, J. C Icequakes on the Athabasca Glacier. Journal of Geophysical Research, Vol. 75, No. 8, 1970, p 1351–62. [All seismic events appear to originate from extensional faulting near glacier surface.]Google Scholar

Neave, K. G Savage, J. C Seismic activity in the Athabasca Glacier. £oj ( Transactions. American Geophysical Union), Vol. 50, No. 4, 1969, p 236. [Abstract only. Seismic method of locating newly formed crevasses.]Google Scholar

Quervain, M DE. Schneekundliche Arbeiten der Internationalen Glaziologischen Grönlandexpedilion (Nivo-logie). Meddelelser om Grønland, Bd. 177, Nr. 4, 1969, 283 p. [Accumulation, temperature and metamorphosis studies on the snow and firn of Greenland. Appendices by Brandenberger, F,Reinwarth, O,Renaud, A,Schneider, R. English abstract.]Google Scholar

Schneider, H. J Minapin—Gletscher und Menschen im NW-Karakorum. Die Erde, 100. Jahrg., Ht. a-4, 1969, p 266–86, map. [Description of 1: 50000 map prepared by terrestrial photogrammetry. Advance and retreat of Minapin Glacier since 1889. Velocity measurements in 1959. English summary.]Google Scholar

Vivian, R Alphonse, P-H Fiches des glaciers français. Les glaciers de Chasseforêt. Revue de Géographie Alpine, Tom. 58, Fasc, 1, 1970, p 237–40. [Summary of knowledge of these glaciers.]Google Scholar

Vivian, R Chinal, M Fiches des glaciers français. Le glacier du Chardon. Revue de Géographie Alpine, Tom. 58, Fasc, 1, 1970, p 233–35. [Summary of knowledge of this glacier.]Google Scholar

Vorndran, G Untersuchungen zur Aktivität der Gletscher, dargestellt an Beispielen aus der Silvrettagruppe. Schriften des Geographischen Instituts der Universität Kiel, Bd. 29, Ht. 1, 1968, 129 p. [Study of changes in ice thickness and area of glaciers in this region of Switzerland and Austria and their dependence on glacier type. French and English summaries.]Google Scholar

Weiss, R. F,, Compositional variations in gases in temperate glaciers, by Weiss, R.F,Bucher, P,Oeschger, H,Craig, H Eos (Transactions. American Geophysical Union), Vol. 50, No. 4, 1969, p 142. [Abstract only. Analysis of entrapped air from Jungfraujoch, Switzerland.]Google Scholar

Addison, J. R Electrical relaxation in saline ice. Journal of Applied Physics, Vol. 41, No. 1, 1970, p 54–63. [Frequency dispersion of dielectric coefficient used to determine spectrum of relaxation times which is interpreted in terms of properties of ice and brine.]Google Scholar

Buzuyev, A.YA Shesterikov, N. P. Zavisimost' sredney tolshchiny pripaynogo l'da ot torosistosti [Relation between mean thickness of fast ice and hummockiness]. Prohlemy Arktiki i Antarktiki, Vyp. 32, 1969, p 30–36.Google Scholar

Dean, C. H Wave recording in a field of pack ice: a comparison of three independent methods. (In Symposium on Antarctic oceanography, Santiago, Chile, 13-16 September 1166. Cambridge, Scott Polar Research Institute for Scientific Committee on Antarctic Research, 1968, p 222–23.) [Three categories of independent systems for measuring ocean waves defined.]Google Scholar

Gorbunov, YU. A Timokhov, L. A K issledovaniyu dinamiki 1'dov [Investigation of ice dynamics]. Izvestiya Akademii Nauk SSSR. Fizika Atmosfery i Okeana, Tom 4, No. 10, 1968, p 1086–91. [Numerical values of various indices of ice dynamics and relationships between them. English translation in Izvestiya. Academy of Sciences, U.S.S.R. Atmospheric and Oceanic Physics, Vol. 4, No. 10, 1968 [pub. 1969J, p. 623–26.]Google Scholar

Gushchenkov, YE, M. K metodike prognoza srokov dostizheniya I'dom tolshchiny 20-25 cm [Method of forecasting time taken for ice to grow to a thickness of 20-25 cm]. Prohlemy Arktiki i Antarktiki, Vyp. 32, 1969, p 45–51. [Floating ice.]Google Scholar

Ingram, R. G, Pilot study of ice drift in the Gulf of St. Lawrence, [by] Ingram, R. G.,Johannessen, O.M,Pounder, E.R Journal of Geophysical Research, Vol. 74, No. 23, 1969, p. 5453–59. [Observations and comparison with theoretical calculations.]Google Scholar

Karlsson, P Hugleiòingar um hafís. Timurit Verkfreeôingafélags īslands, Ārg, 53, Ht. 2–3, 1968, p 17–25. [Distribution and movement of floating ice in Arctic Ocean.]Google Scholar

Kutschale, H Arctic hydroacoustics. Arctic, Vol. 22, No. 3, 1969, p 346–64. [Includes effect of sea ice on background noise and on propagation of underwater sound.]Google Scholar

Lake, R. A,, Brine drainage during sea ice growth and vertical circulation in the underlying water, [by] Lake, R.A,Lewis, E.L,Walker, E.R Eos (Transactions. American Geophysical Union), Vol. 50, No. 2, 1969, p 63. [Abstract only.]Google Scholar

Lock, G. S. H, A study of one-dimensional ice formation with particular reference to periodic growth and decay, by Lock, G .S. H,Gunderson, J.R,Quon, D,Donnelly, J.K International Journal of Heat and Mass Transfer, Vol. 12, No. 11, 1969, p 1343–52. [Experiments compared with theoretical predictions.]Google Scholar

Paige, R. A Stalactite growth beneath sea ice. Science, Vol. 167, No. 3915, 1970, p 171–72. [Hollow tapering inverted cones found extending beneath sea ice in McMurdo Sound, Antarctica.]Google Scholar

Pitts, J Black icebergs, 2. Antarktiese Bulletin, No. 26, 1968, p 40. [Further comments on this phenomenon, quoting Sir Alister Hardy on R.R.S. Discovery in Antarctic waters, 1925-27. For “Black icebergs, [1]”, see below, Van der Merwe, A.]Google Scholar

Untersteiner, N Sea ice and heat budget. Arctic, Vol. 22, No. 3, 1969, p 195–99. [Survey of progress in understanding properties of sea ice and conditions for its development.]Google Scholar

Van der merwe, A. Black icebergs. Antarktiese Bulletin, No. 25, 1968, p 30–31. [Comments by author and Sir Vivian Fuchs and Dr Swithinbank, C .W. M (in letter to author) on this phenomenon, reported in Antarctic waters, 1967. For continuation, see above, Pitts, J.]Google Scholar

Vinje, T. E Sea ice conditions in Svalbard in 1967. Norsk Polarinstitull. Arbok, 1967 [pub. 1969], p. 194–96. [Area charts for each month and discussion.]Google Scholar

Black, R. F Geology, especially geomorphology, of northern Alaska. Arctic, Vol. 22, No. 3, 1969, p 283–99. [Survey of present knowledge particularly that due to Naval Arctic Research Laboratory work.]Google Scholar

Bray, J. R Glaciation and solar activity since the fifth century B.C. and the solar cycle. Nature, Vol. 220, No. 5168, 1968, p 672–74. [Evidence for a 2 600 year solar cycle.]Google Scholar

Clark, R A contribution to glacial studies of the Malham Tarn area. Field Studies, Vol. 2, No. 4, 1967.479–91. [Late-glacial and post-glacial landforms.]Google Scholar

Dansgaard, W Taubek, H Glacier oxygen-18 content and Pleistocene ocean temperatures. Science, Vol. 166, No. 3904, 1969, p 499–502. [^l80 content of ice in ice sheets during glacial maximum could account for observed changes in marine deposits.]Google Scholar

Emiliani, C Interglacial high sea levels and the control of Greenland ice by the precession of the equinoxes. Science, Vol. 166, No. 3912, 1969, p 1503–04. [Correlation between ages of high sea-level and coincidence of perihelion with northern summer solstice suggests considerable melting of Greenland ice during interglacial periods was climatically controlled.]Google Scholar

Gillberg, G A great till section on Kinnekule, Sweden, W Geologiska Föreningens i Stockholm Förhandlingar, Vol 91, Pt. 3, No. 538, 1969, p 313–42. [Discussion of depositional processes and factors which caused variations in them.]Google Scholar

Horai, K. I. Effect of past climatic change on the thermal field of the Earth. Earth and Planetary Science Letters, Vol. 6, No. 1, 1969, p 39–42. [Corrections to heat flow due to glaciation.]Google Scholar

Howarth, P. J Price, R. J The proglacial lakes of Breiòamerkurjökull and Fjallsjökull, Iceland. Geographical Journal, Vol. 135, Pt. 4, 1969, p 573–81, plates. [Study of these lakes, the formation of icebergs in them, and discussion of their origin.]Google Scholar

Jones, J. G Intraglacial volcanoes of the Laugarvatn region, south-west Iceland—I. Quarterly Journal of the Geological Society of London, Vol. 124, No. 495, Pt. 3, 1969 [for 1968], p. 197–211. [Shape and structure of these volcanoes attributed to their having formed within bodies of melt water in an ice sheet, discussion by Walker, G .P. L,Early, K.R,Sabine, P.A, p. 211.]Google Scholar

King, C. A M. Glacial geomorphology and chronology of Henry Kater Peninsula, east Baffin Island, N.W.T. Arctic and Alpine Research, Vol. 1, No. 3, 1969, p 195–212. [Deglaciation stages and study of moraines.]Google Scholar

Koopmans, B. N Staueeer, P Glacial phenomena on Mount Kinabalu, Sabah. Malaysia. Borneo Region. Geological Survey. Bulletin 8, 1967, p 25–35, plates. [Evidence that this mountain was capped by ice fields in the Pleistocene; at least two valley glaciers developed.]Google Scholar

Macneill, R. H Dates relating to the dating of the last major ice sheet in Nova Scotia. Maritime Sediments, Vol. 5, No. I, 1969, p 3. [Dating of three samples, two relating to beginning and one to end of ice advance.]Google Scholar

Malaurie, J Thèmes de recherche géomorphologique dans le nord-ouest du Groenland. Centre de Recherches et Documentation Cartographiques et Géographiques. Mémoires et Documents (Paris), Numero hors série, 1968, 495 p. [Study of geomorphology of parts of Thule district, north-west Greenland. Sections on frost-shaltering, geomorphology of Inglefield Land and Washington Land, talus slopes and effect of running water on sandy slopes.]Google Scholar

Nichols, R. I. Geomorphology of Inglefield Land, North Greenland. Mtddelelser om Grönland, Bd. 188, Nr. ι,. 1969) 109 p. [Study of geomorphology, mainly glacial and periglacial, of this area of north-west Greenland.]Google Scholar

Péchoux, P.-Y. Traces d'activité glaciaire dans les montagnes de Grèce centrale. Revue de Géographie Alpine,. Tom. 58, Fasc. 1, 1970, p 211–24. [Observations of small cirques in central Greece giving evidence of glaciation in the late Quaternary. English abstract.]Google Scholar

Ray, L. L Glacial erratics and the problem of glaciation in northeast Kentucky and southeast Ohio—a review and suggestion. U.S. Geological Survey. Professional Paper 650-D, 1969, p 0195–99. [Mode of transportation not adequately explained. Possibly Nebraskan ice advanced further than at present thought.]Google Scholar

White, W. A Erosion of cirques. Journal of Geology, Vol. 78, No. 1, 1970, p 123–26. [Suggests that cirques form by deepening through glacial erosion of floors rather than by headward sapping of walls.JGoogle Scholar

Benedict, J. B Microfabric of patterned ground. Arctic and Alpine Research, Vol. 1, No. 1, 1969, p 45–48. [Sand grain orientation studied. Possible use in reconstructing soil movement.]Google Scholar

Black, R, F. Slopes in southwestern Wisconsin, U.S.A., periglacial or temperate? Biuletyn Peryglacjalrty, No. 18, 1969, p 69–82. [Present temperate climate sufficient to explain most features.]Google Scholar

Brown, J Soil properties developed on the complex tundra relief of northern Alaska. Biuletyn Peryglacjalny, No. 18, 1969, p 153–67. [Study of soils, surface relief and near-surface lithology above permafrost near Barrow, Alaska.]Google Scholar

Churska, Z The development of the Drwęca valley slopes in the late-glacial period. Biuletyn Peryglacjalny, No. 18, 1969, p 423–34. [Periglacial deposits and processes which formed them in this region of Poland.]Google Scholar

Demek, J Cryogene processes and the development of cryoplanation terraces. Biuletyn Peryglacjalny, No. 18, 1969, p 115–25. [Significance of different processes at different stages of terrace development.]Google Scholar

Dylik, J Slope development under periglacial conditions in the Lódź region. Biuletyn Peryglacjalny, No. 18,1969, p. 381–410. [Excursion notes on this part of Poland.]Google Scholar

Ivanov, N. S Teplo- i massoperenos v merzlykh gomykk porodakh [Heat and mass transport in frozen soils]. Moscow, Izdatel'stvo “Nauka”, 1969. 240 p. [Theoretical study,]Google Scholar

Jahn, A Some problems concerning slope development in the Sudeles. Biuletyn Peryglacjalny, No. 18, 1969, p 331–48. [Excursion notes including periglacial effects.]Google Scholar

Kar, N. R Studies on the geomorphic characteristics and development of slopes in the periglacial zones of Sikkim and Darjeeling Himalayas. Biuletyn Peryglacjalny, No. 18, 1969, p 43–67. [Field studies and deduction of mechanisms of slope development.]Google Scholar

Katasonov, E, M. The typical features of cryogenic eluvium on slopes. Biuletyn Peryglacjalny, No. 18, 1969, p 11–14. [Study of comminution and deformation of deposits in situ by freezing of water within them.]Google Scholar

Kinosita, S, Kitami ni okeru tōjō kansoku (Shōwa 42-43 nen tōki), tsuketari dochūsui-idō no kikō oyobi tōchaku tō j ō no teionshitsu jikken [Measurement of frost heave in Kitami (1967-68), including low temperature chamber experiments on the mechanism of movement, temperature profile and heaving lorce]. [By] Kinosita, S,Horiguchi, K,Tanuma, K,Ōno, T Teion-kagaku : Low Temperature Science, Scr. A, [No.] 26, 1968, p 363–81. [English summary, p. 381.]Google Scholar

Lyczewska, J Sédiments et processus quaternaires du versant crétacé de la vallée de la Basse-Nida (partie méridionale delà Pologne centrale). Biuletyn Peryglacjalny, No. 18, 1969, p 195–208. [Study of sediments and periglacial processes which formed them in this part of Poland.]Google Scholar

Macar, P Actions périglacîaires et évolution des pentes en Belgique. Biuletyn Peryglacjalny, No. 18, 1969, p 137–52. [Study of fossil periglacial forms in Belgium.]Google Scholar

Owens, I. F Causes and rates of soil creep in the Chilton Valley, Cass, New Zealand. Arctic and Alpine Research, Vol. 1, No. 3, 1969, p 213–20. [Frost action shown to be main cause. Rates measured.]Google Scholar

PÉCSI, M. Genetic classification of slope sediments. Biuletyn Peryglacjalny, No. 18, 1969, p 15–27. [Suggests classification, including periglacial slope sediments.]Google Scholar

PÉwÉ, T. L ed. The periglacial environment, past and present. Montreal, McGill-Queen's University Press [and] Arctic Institute of North America, 1969. ix, 487 p. [Book containing the following papers: Péwé, T. L., “The periglacial environment”, p. 1–9; Brown, R .J. E, “Factors influencing discontinuous permafrost in Canada”, p. 11–53; Popov, A.I, “Underground ice in the Quaternary deposits of the Yana-Indigirka lowland as a genetic and stratigraphie indicator”, p. 55–64; Rapp, A,Annersten, L, “Permafrost and tundra polygons in northern Sweden”, p. 65–91;,Brown, J, “Soils of the Okpilak river region, Alaska”, p. 93–128; Rudberg, S, “Distribution of small-scale periglacial and glacial geomorphological features on Axel Heiberg Island, Northwest Territories, Canada”, p. 129–59; Lorenzo, J. L, “Minor periglacial phenomena among the high volcanoes of Mexico”, p. 161–75; Marr, J. W, “Cyclical change in a patterned-ground ecosystem, Thule, Greenland”, p. 177–201; Lundqvist, J, “Earth and ice mounds: a terminological discussion”, p. 203–15; Bellair, P, “Soil stripes and polygonal ground in the subantarctic islands of Crozct and Kerguelen”, p. 217–22; Reger, R.D,Péwé, T. L, “Lichcnometric dating in the central Alaska Range”, p. 223–47; Weidick, A, “Investigations of the Holocene deposits around Jakobshavns Isbrae, West Greenland”, p. 249–62; Markov, K.K, “The Pleistocene history of Antarctica”, p. 263–69; Harris, S.A, “Isostatic recovery near glacier-ice margins; some evidence from Waterloo, Ontario, Canada”, p. 271–83; Cailleux, A, “Quaternary periglacial wind-worn sand grains in USSR”, p. 285–301; Journaux, A and others, “Distribution, source, and age of the loess on the plain of Caen, Normandy, France”, by Λ. Journaux, Helluin, M,Lautridou, J.P,Pellerin, J, p. 303–20; Mullenders, W,Gullentops, F, “The age of the pingos of Belgium”, p. 321–35; Macar, P, “A peculiar type of fossil ice fissure”, p. 337–46;Ménorval, E. B. de, “Periglacial phenomena recently observed in the terraces of the Seine southeast of Bonnières, France”, p. 347–50; Gruhn, R,Bryan, A.L, “Fossil ice wedge polygons in southeast Essex, England”, p. 351–63; Dylik, J, “Slope development affected by frost fissures and thermal erosion”, p. 365–86; Ford, T.D, “Dolomite tors and sandfilled sink holes in the Carboniferous limestone of Derbyshire, England”, p. 387–97; Williams, R .G. B, “Permafrost and temperature conditions in England during the last glacial period”, p. 399–41; West, K. G, “Stratigraphy of periglacial features in East Anglia and adjacent areas”, p. 411–15; Bigarella, J. J and others, “Processes and environments of the Brazilian Quaternary”, by Bigarella, J.J,Mousinho, M.R,Silva, J. X. da, p. 417–87. Reviewed on p. 408–09.]Google Scholar

Raynal, R Mutations en cours dans la morphogénèse périglaciaire au Nord-Ouest du Spitsberg (région du Kongsfjord). Biuletyn Peryglacjalny, No. 18, 1969, p 83–88. [Study of” slope evolution and of detailed forms on level ground in Spitsbergen.]Google Scholar

Rohdenburg, H Observations concerning Lateglacial [sic] slope-dynamics in Central Europe. Biuleiyn Peryglacjalny, No. 18, 1969, p 89–94. [Inference of amount of periglacial development that took place in this period.]Google Scholar

Starkel, L. L'évolution des versants des Carpates à flysch au (Quaternaire. Biuleiyn Peryglacjalny, No. 18, 1969, p 349–79. [Excursion notes including periglacial effects.]Google Scholar

Tolstikhin, O. N Piguzova, V. M ed. Naledi Sibiri [Icings of Siberia]. Moscow, Izdatel'stvo “Nauka”, 1969. 208 p. [Collected papers on many aspects.]Google Scholar

Velitchko, A. A. Milieu géologique et géomorphologique de la zone périglaciaire de la Plaine Est-Européenne. Biuletyn Peryglacjalny, No. 18, 1969, p 183–93. [General description of the geology and geomorphology of the periglacial zone of the east European plain.]Google Scholar

Washbukn, A. L Patterned ground in the Meslers Vig district, northeast Greenland. Biuletyn Peryglacjalny, No. 18, 1969, p 259–330. [Detailed study of patterned ground and discussion of origin.]Google Scholar

Watson, E The slope deposits in the Nant lago valley, near Cader Idris, Wales. Biuleiyn Peryglacjalny, No. 18, 1969, p 95–113. [Interpretation as due to solifluetion and slope wash.]Google Scholar

Auer, A. H.jr,, Observations of ice crystal and ice nuclei concentrations in stable cap clouds, [by] Auer, A.H.Jr,Veal, D.L,Marwitz, J.D Journal of the Atmospheric Sciences, Vol. 26, No. 6, 1969, p 1342–43. [Measurements show temperature dependence of ratio of crystals to nuclei.]Google Scholar

Bailey, I. H,, Isotopic composition of hailstones, by Bailey, I.H,Hulston, J.R,Macklin, W.C,Stewart, J.R Journal of the Atmospheric Sciences, Vol. 26, No. 4, 1969, p 689–94. [Theory of isotopic fractionation in hailstones and analyses of accreted ice which confirm the predictions.]Google Scholar

Burrows, D. A Robertson, CE Comments on “ice multiplication in clouds”. Journal of the Atmospheric Sciences, Vol. 26, No. 6, 1969, p 1340–41. [Comments on paper by Hobbs, P.V, ibid., Vol. 26, No. 2, 1969, P· 315-18]Google Scholar

Morgan, G. M.jr Prodi, F. Λ laboratory observation of hailstone “lobe” formation following the termination of spongy growth by accretion. Journal of Applied Meteorology, Vol. 8, No. 5, 1969, p 840–42. [Possibility that observed lobes are due to protuberances caused by volume change of freezing water inside a spongy ice mass frozen from the outside.]Google Scholar

Rosinski, J Kerrigan, T. C The role of aerosol particles in the formation of raindrops and hailstones in severe thunderstorms. Journal of the Atmospheric Sciences, Vol. 26, No. 4, 1969, p 695–714. [Study of collected hailstones to determine nature of nucleation process.]Google Scholar

Ruskin, R. E Multiplication of ice embryos by ice-whisker shedding. Science, Vol. 166. No. 3907, 1969, p 906. [Possibility of ice whiskers as formed on evaporating ice forming in cloud conditions and shedding as ice embryos.]Google Scholar

Schuepp, P. H List, R Influence of molecular properties of the fluid on simulation of the total heat and mass transfer of solid precipitation particles. Journal of Applied Meteorology, Vol. 8. No. 5, 1969, p 743–46. [Measurements of heat transfer from solid lo water used as model experiment to indicate roughness effect on heat and mass transfer of spherical hailstones.]Google Scholar

Devine, J. C The “snowburst” of 14 March 1969 at Fort Huachuca, Arizona. Weatherwise, Vol. 22, No. 6, 1968, p 236–39. [Meteorological conditions which led to exceptionally cold spell with heavy snow close to Mexican border.]Google Scholar

Fujino, K Sekisetsu naibu de no yūselsu-sui no ryūka sokudo no sokutei, I [Measurement of flowing down speed of melt water in a snow cover, I]. Teion-kagaku; Low Temperature Science, Ser. A. [No.] 26, 1968, p 87–100. [NaC] used as a tracer to measure penetration of melt water. English summary, p. 100.]Google Scholar

Kikuchi, K Mitrayama, M Kyokuchi sōbiyō mōhi, nunoji no chakusetsu genshō [Snow deposition on fur and cloth used in the polar regions]. Nankyaku Shiryō: Antarctic Record, [No.] 36, 1970, p 78–84. [Study at “Syowa” station on thirteen kinds of fur and cloth of amount of snow and hoar frost deposited. English abstract.]Google Scholar

Lauscher, F Eine Analyse von Schneehöhen der Slowakei. Wetter und lieben, Jahrg. 22,, Ht. 1–2, 1970, p 9–12. [Data on average maximum and monthly snow depths in Slovakia analysed and compared with similar data for Austria. English summary.]Google Scholar

Mayr, E Wartburg, B Über die Bodentemperatur unter- schneefreier und schneebedeckter Oberfläche. Wetter und Leben, Jahrg. 22,, Ht. 1–2, 1970, p 21–24. [Effect of snow cover on soil temperature measurements. English summary.]Google Scholar

Peterle, T. J DDT in Antarctic snow. Nature, Vol. 224, No. 5219, 1969, p 020. [Measurement in snow at “Plateau” station and deduction of possible total amount of DDT in Antarctic snow.]Google Scholar

Seppänen, M. Average depth of snow in undulating land in Finland. Geophysica, Vol. 9, No. 4, 1967, p 277–86. [Covers period 1952-63. Also published in Hydrologisen Toimiston Tiedonantoja, 27.]Google Scholar

Shimizu, H Shamen sekisetsu no naibu-hizumi, I [Study on internal strain of snow cover on a slope, I]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 26, 1968. p. 143–68, [Direct observation of strain. English summary, p. 166–68.]Google Scholar

Wakahama, G Sekisetsu-nai ni okeru yūsetsu-sui no idō, III suiro ryūka sokudo himaku ryūka sokudo [Infiltration of melt water into snow cover, III—flowing down speed of melt water in a snow cover]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 26, 1968, p 77–86. [Measurement of speed of penetration of melt water by two different processes. English summary, p. 85–86.]Google Scholar

Wakahama, G, Daisetsu-san no sekkei chōsa (dai 3 nendo) [Studies of firn on Mt Daisetsu in summer (third year)]. [By] Wakahama, G,Endo, Y,Yamada, T,Ushiki, H,Naruse, R Teion-kagaku; Low Temperature Science, Ser. A, [No.] 26, 1968, p 215–29. [Results in 1966 of measurements on snow patches in Hokkaido, Japan. English summary, p. 227.]Google Scholar

Wakahama, G, Sekisetsu-nai ni okeru yōsetsu-sui no idō, II [Infiltration of melt water into snow cover, II], [By]Wakahama, G,Nakamura, T,Endo, Y Teion-kaguku; Low Temperature Science, Ser. A, [No.] 26, 1968, p 53–75. [Measurement of water content in each layer of a snow cover. English summary, p. 73–75.]Google Scholar

Wisdom, H. L Atmospheric dust records in permanent snowfields: implications to marine sedimentation. Geological Society of America. Bulletin, Vol. 80, No. 5, 1969, p 761–82. [Analyses of samples from Antarctic and Greenland and five temperate glaciers and discussion of significance.]Google Scholar