Hostname: page-component-78c5997874-v9fdk Total loading time: 0 Render date: 2024-11-10T09:44:30.949Z 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 8 , Issue 53 , 1969 , pp. 329 - 338
Copyright
Copyright © International Glaciological Society 1969

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

Conferences

Schram, K. Thams, J. C., ed. 9. Internationale Tagung für alpine Meteorologie in Brig und Zermatt 14–17. Sept. 1966. Veröffentlichungen der Schweizerischen Meteorologischen Zentralanstalt, Nr. 4, 1967. v, 366 p. [Proceedings of conference which included as one theme the relation between Alpine meteorology and glaciology. For relevant papers see elsewhere in this list.]Google Scholar
[Union Géodésique Et Géophysique Internationale.] Laien de Géodésie el Géophysique Internationale. Association Internationale d’Hydrologie Scientifique. Assemblée générale de Berne, 25 sept−7 oct. 1967. [Commission de Neiges et Glaces.] Rapports el discussions. Gentbrugge, Association Internationale d’Hydrologie Scientifique, 1968. 461 p. (Publication No. 79 de l’Association Internationale d’Hydrologie Scientifique.) Bel. fr. 500. [For details of papers see elsewhere in this list.]Google Scholar

General Glaciology

Avsyuk, G. A. Krenke, A. N. The beginning of the Soviet glaciological investigations in the IHI) programme. Union de Géodésie… Berne, 1967. Rapports el discussions, 1968, p. 292–99. [Report of progress in forming programme for International Hydrological Decade, and some early results.]Google Scholar
Bender, J. A. Snow and ice. Transactions. American Geophysical Union, Vol. 48, No. 2, 1967, p. 724–29. [Review of recent work]Google Scholar
Bostock, H. S. A catalogue of selected airphotographs. Canada. Geological Survey. Paper 67–48, 1968, iii, 163 p., map. [Description of aerial photographs of geomorphological phenomena in Canada. Includes many glaciological and glacial geological items.]Google Scholar
Haefeli, R. Research on snow, avalanches, ice and glaciers. (In Thams, J. C., ed. The development of geodesy and geophysics in Switzerland.… Zurich, Bcrichthaus, 1967, p. 72–83.) [General account of early and recent Swiss research.]Google Scholar
Hansen, J. E. Cheyney, H. Comments on the paper by D. G. Rea and B. T. O’Leary, “On the composition of the Venus clouds”. Journal of Geophysical Research, Vol. 73, No. 18, 1968, p. 6136–37. [Criticism of conclusion of paper, ibid., Vol. 73, No. 2, 1968, p. 665–75, that ice crystals. if they exist, must be submicron in diameter.]CrossRefGoogle Scholar
Hoinkes, H. C. Glaciology in the International Hydrological Decade. Union de Géodésie.… Berne, 1967. Rapports et discussions. 1968, p. 7–16. [Presidential address to Commission de Neiges et Glaces. Survey of glaciological programme of I.H.D.]Google Scholar
Mokhnach, D. O. O vozmozhnosti otsenki razmerov i mass ledyanogo yadra komety . Doklady.lkademii Nauk SSSR, Tom 180, No. 5, 1968, p. 1067–70. [Discussion of interpretation of optical observations in terms of photodissociation of molecules.]Google Scholar
Owen, T. Ice on Venus: can it exist? Science, Vol. 161, No. 3844, 1968, p. 915–16. [Arguments against existence of ice sheets on Venus and discussion of anomalous water content of Venus compared with Earth.]Google Scholar
Pollack, J. B. Sagan, C. The case for ice clouds on Venus., Journal of Geophysical Research, Vol. 73, No. 18. 1968, p. 5943–49. [Discussion of experimental evidence on reflectivity.]Google Scholar
Rea, D. G. O’Leary, B. T. On the composition of the Venus clouds. Journal of Geophysical Research. Vol. 73, No. 2, 1968, p. 665–75. [Spectroscopic evidence that ice crystals can only be present if they are submicron in size, which is not likely.]Google Scholar

Glaciological Instruments and Methods

Adams, W. P. A note on the pressure pillow method of snow measurement. McGill Sub-Arctic Research Laboratory. Research Paper No. 23, 1967, p. 94–97. [Describes method of use.]Google Scholar
Ambach, W., and others. Investigations of fission products in the accumulation area of an alpine glacier (Kcsselwandferner, Oetztal Alps), [by] W. Ambach, H. Eisner and F. A. Prantl. Union de Géodésie … Berne. 1967. Rapports et discussions, 1968. p. 117–25. [Studies show that 137Cs from nuclear tests remains within a Ern layer and so can be used for dating.]Google Scholar
Ambach, W., and others. Tritium content in the urn layers of an alpine glacier, [by] W. Ambach, H. Eisner and L. L. Thatcher. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 126–34. [Study of tritium from thermonuclear tests in Kesselwandferner, Austria. Results show that despite changes due to melt water, layers retain high tritium content. Use as tracer in run-off studies.]Google Scholar
Jaccard, C. Apparatus for growing large monocrystals of ice with radial refining. Zeitschrift für angewandte Mathematik und Physik, Vol. 18, Fasc. 5, 1967, p. 758–60. [Method of producing pure ice crystals or ice crystals doped with HF but otherwise pure.]Google Scholar
Jaccard, C. Automatic thin section analysis with the tomograph. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 345–51. [Description of apparatus which identifies optically the crystallographic orientation of ice at any point in a thin section, and by scanning can determine crystallite boundaries.]Google Scholar
Lorius, C., and others. Détermination des épaisseurs de glace par une méthode gravimétrique simplifiée, Terre Adélie, campagnes d’été 1964–65 et 1965–66, par C. Lorius, G. Rouillon, F. Helly. Expéditions Polaires Françaises, Missions Paul-Émile Victor, Publication No. 295, 1967, 35 p. [Description of simplified gravimetric method used to determine ice thickness and verified by direct boring. English and Russian summaries.]Google Scholar
Oeschger, H., and others. Radiocarbon dating of ice, by H. Oeschger, B. Alder, H. Loosli, C. C. Langway, Jr., and A. Renaud. Earth and Planetary Science Letters, Vol. 1, No. 2, 1966, p. 49–54. [Development of special counter to allow dating with 20–loo mg of carbon.]Google Scholar
Ueda, H. T. Garfield, D. E. Deep-core drilling program at Byrd station (1967–1968). Antarctic Journal of the United States, Vol. 3, No. 4, 5968, p. 111–12. [Report of drilling operations that penetrated Antarctic ice sheet.]Google Scholar
Walker, J. W., and others. Airborne radar soundings of the Greenland ice cap: flight 1, [by] J. W. Walker, D. C. Pearce, A. H. Zanella. Geological Society of America. Bulletin, Vol. 79, No. 11, 5968, p. 1639–46. [Feasibility of airborne radar for ice thickness measurements studied on basis of flight over Greenland.]Google Scholar

Physics of Ice

Barnes, P. Tabor, D. Plastic flow and pressure melting in the deformation of ice I. Union de Géodésie … Berne, 1967. Rapports el discussions, 1968, p. 303–15. [Marked drop in hardness °f lee very close to melting point attributed to pressure melting along grain boundaries. Experiments confirm this view and explain large grain size and loss of bubbles of such ice. Discussion, by E. R. LaChapelle, R. Haefeli, N. S. Stehle, P. V. Hobbs and J. F. Nye, p. 313–15.]Google Scholar
Bartlett, J. T. Readings, C. J. Some optical effects in deformed single crystals of ice. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 316–25. [Observation of stress-optical effects in crystals which have asymmetry, also of interference bands parallel to traces of basal planes, interpreted as evidence for non-basal glide.]Google Scholar
Bertie, J. E., and others. Far-infrared spectra of ice II, V and IX, by J. E. Bertie, H. J. Labbé and E. Whalley. Journal of Chemical Physics, Vol. 49, No. 2, 1968, p. 775–80. [Spectra obtained in range 360–20 cm−1. In ice II and IX the bands are sharp while in ice V they are broad confirming the disorder of ice V and order of ice II and IX.]Google Scholar
Bertie, J. E., and others. Infrared spectrum of ice VI in the range 4000–50 cm−1, [by] J. E. Bertie, H. J. Labbé and E. Whalley. Journal of Chemical Physics, Vol. 49, No. 5, 1968, p. 2141–44. [Spectrum showing that ice VI recovered at liquid-nitrogen temperature is orientationally disordered.]Google Scholar
Bullemer, B., and others. Conductivity of ice by a guarded potential probe method, [by] B. Bullemer, I. Eisele, H. Engelhardt, N. Riehl and P. Seige. Solid State Communications, Vol. 6, No. 9, 1968, p. 663–64. [Determination of bulk conductivity and activation energy.]Google Scholar
Colombino, P., and others. Positronium annihilation in water and ice down to −144° C by angular correlation measurements, [by] P. Colombino, B. Fiscella and L. Trossi. (In Stewart, A. T. Roelling, L. O., ed. Positron annihilation. Proceedings of the conference held at Wayne State University on July 27–29, 1965. New York, London, Academic Press, 1967, p. 353–56.) [Explanation of differences in terms of changes in number of hydrogen bonds in ice.]CrossRefGoogle Scholar
Cross, J. D. Thermoelectrets. (In Stickland, A. C., ed. Static electrification. Proceedings of the conference organized by the Institute of Physics and the Physical Society, Static Electrification Group, London, May 1967. London, Institute of Physics and Physical Society, 1967, p. 22–28. (Institute of Physics and Physical Society Conference Series, No. 4.)) [Results of measurements at −78°C on, among other things, ice. Effect attributed to impurities. Discussion by J. Hart, M. Block, W. G. Lawson and J. Latham, p. 27–28.]Google Scholar
Dantl, G. Die elastischen Moduln von Eis-Einkristallen. Physik der kondensierten Materie, Bd. 7, Ht. 5, 1968, p. 390–97. [Measurement of velocity of sound in ice single crystals from 0° to −140°C and deduction of elastic constants.]Google Scholar
Defrain, A., and others. Sur ies changements de phase dans les depôts de glace, d’acétamide, d’ortho-crésol et de phénol, obtenus par condensation de vapeur sur un support maintenu a basse température, par A. Defrain, N. T. Linh et J. Poulie. Journal de Chimie Physique et Physicochimie Biologique, Tom. 65, No. 9, 1968, p. 1510–18. [Study of vitreous phase formed by low temperature deposition by X-rays and differential thermal analysis. English summary.]Google Scholar
Fletcher, N. H. Surface structure of water and ice. II. A revised model. Philosophical Magazine, Eighth Ser., Vol. 18, No. 156, 1968, p. 1287–1300. [Theoretical study shows preferred orientation of water molecules at surface and resulting quasi-liquid layer which accounts for surface electrical conductivity.]Google Scholar
Gilra, N. K. Homogeneous nucleation temperature of supercooled water. Physics Letters, Vol. 28a, No. 1, 1968, p. 51–52. [Calculated value on various precrystallization theories and structure models agree with observed values.]Google Scholar
Glen, J. W. The importance of the hydrogen atom arrangement in determining how ice can deform plastically. Union de Géodésie… Berne, 1967. Rapports et discussion, 1968, p. 352–55. [Theory of movement of dislocations in ice. Movement of electrical point defects can limit dislocation movement. Discussion by]. T. Bartlett, C. J. Readings, P. Barnes and C. Jaccard, p- 354–55.]Google Scholar
Gokhale, N. R. Goold, J. jr. Droplet freezing by surface nucleation. Journal of Applied Meteorology, Vol. 7, No. 5, 1968, p. 870–74. [Laboratory study in which nucleating particles were sprinkled on supercooled drops.]Google Scholar
Haefeli, R., and others. Deformation of polycrystalline ice under combined uniaxial and hydrostatic pressure, by R. Haefeli, C. Jaccard and M. de Quervain. Union de Géodésie… Berne, 1967. Rapports el discussions, 1968, p. 341–44. [Effect of hydrostatic pressure is to increase creep rate at constant temperature, but to reduce creep rate at constant temperature-difference from melting point.]Google Scholar
Hobbs, P. V. Alkezweeny, A. J. The fragmentation of freezing water droplets in free fall. Journal of the Atmospheric Sciences, Vol. 25, No. 5, 1968, p. 881–88. [Laboratory experiments under conditions similar to those in natural clouds.]Google Scholar
Johnson, D. A. Hallett, J. Freezing and shattering of supercooled water drops. Quarterly Journal of the Royal Meteorological Society. Vol. 94, No. 402, 1968, p. 468–82. [Laboratory observations of conditions under which drops shatter on freezing.]CrossRefGoogle Scholar
Jones, S. J. Glen, J. W. The mechanical properties of single crystals of ice at low temperatures. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 326–40. [Results of tensile and compressive tests on pure and HF-doped ice single crystals down to −90°C. Discussion by C. Jaccard, p. 340.]Google Scholar
Julienne, P. S. Gary, L. P. Trapped electrons in ice. Molecular Crystals. Vol. 5, No. 1, 1968, p. 135–39. [Theoretical study of hydrated electron in ice. Model predicts trapping only in region of defect.]Google Scholar
Kamb, W. B. Prakash, A. Structure of ice III. Acta Crystallographica, Vol. B24, Pt. 10, 1968, p. 5317–27. [X-ray determination of structure of this phase; discussion of possible proton ordering.]Google Scholar
Ketcham, W. M. Hobbs, P. V. Step growth on ice during the freezing of pure water. Philosophical Magazine, Eighth Ser., Vol. 18. No. 153, 1968, p. 659–61. [Direct observation of steps on basal plane of ice growing in water.]Google Scholar
Kevan, L., and others. Optical absorption spectrum of trapped dielectrons in alkaline ice, [by] L. Kevan. D. R. Renneke and R. J. Friauf. Solid State Communications, Vol. 6. No. 7. 1968, p. 469–71. [At heavy y irradiation an optical absorption band appears that is interpreted as two electrons trapped on the same vacancy site.]Google Scholar
Knight, C. A. Growth of ice crystals after a method by Helmholtz. Natare, Vol. 220, No. 5162, 1968, p. 62–63. [Letter. Study of growth of ice in a vessel sealed under vacuum immersed in an open ice-water bath.]Google Scholar
Kormer, S. B., and others. Fazovoye prevrashcheniyc vody y led VII pri udarnom szhatii , Zhurnal Eksperimentalnoy i Teoreticheskoy Fiziki, Tom 54. Vyp. 6, 1968, p. 1640–45. [Optical observations of loss of transparency and diffuse scattering demonstrate existence of’ ice VII when shock waves above 20–40 kbar pass through water. English summary. English translation in Soviet Physics-JETP, Vol. 27, No. 6, 1968, [c1969], p. 879–81.]Google Scholar
Krause, A. S. A rate theory of dislocation mobility. Acta Metallurrgica, Vol. 16, No. 7, 1968, p. 897–902. [Theory of dislocation velocity applied to various substances including ice.]Google Scholar
Kuhns, I. E. The nucleation of water droplets at deep supercooling in different gaseous environments. Journal of the atmospheric Sciences. Vol. 25, No. 5, 1968, p. 878–80. [Experimental study of freezing temperature of supercooled droplets in different gases.]Google Scholar
Latham, J. The importance in atmospheric electricity of charge transfer associated with temperature gradients in ice. (In Stickland, A. C., ed. Static electrification. Proceedings of the conference organized by the Institute of Physics and the Physical Society, Static Electrification Group. London, May 1967. London, Institute of Physics and Physical Society, 5967, p. 44–55. (Institute of Physics and Physical Society Conference Series, No. 4.)) Review of work on thermoelectric effect in ice and its relevance to electrification processes in ice. Application to meteorological phenomena.]Google Scholar
Levi, L. Lubart, L. On the electric properties of ice doped with NH4F. Physik der kondensierten Materie. Bd. 7, Ht. 5, 1968. p. 368–71. [Measurement of dielectric constant and electric conductivity. Activation energy of 0.10 eV is not the same as that of pure ice.]Google Scholar
Mossop, S. C. Silver iodide as nucleus for water condensation and crystallization. Journal de Recherches Atmosphériques, Vol. 3, 1968. Nos. 5–2. p. 185–90. [At small supercoolings laboratory tests show ice-forming ability of aerosols of Agl and NaI depends on supersaturation in test cloud.]Google Scholar
O’Neil, J. R. Hydrogen and oxygen isotope fractionation between ice and water, Journal of Physical Chemistry. Vol. 72. No. 10. 1968, p. 3683–84. [Experimental determination of fractionation of D and 18O on freezing of water.]Google Scholar
Pistorius, C. W. F. T., and others. Phase diagrams of H2O and D2O at high pressures, by C. W. F. T. Pistorius, E. Rapoport and J. B. Clark. Journal of Chemical Physics, Vol. 48, No. 12. 5968. p. 5509–14. [Study of the phase boundaries between ice VI, ice VII and ice VIII and of melting curve of ice VII in H2O and D2O.]Google Scholar
Prask, H., and others. The frequency distribution of ice by neutron scattering, [by] H. Prask and H. Boutin and S. Yip. Developments in Applied Spectroscopy, Vol. 6, 1968, p. 265–76. [Determination of phonon frequency distribution and comparison with thermodynamic data.]Google Scholar
Rabideau, S. W., and others. Neutron diffraction study of ice polymorphs. I. Ice IX, [by] S. W. Rabideau, E. D. Finch, G. P. Arnold and A. L. Bowman. Journal of Chemical Physics, Vol. 49, No. 6, 1968, p. 2514–19. [Neutron diffraction verification of proton-ordered structure.]Google Scholar
Ruby, S. L., and others. Concentration dependence of tin (IV) isomer shifts in ice, [by] S. L. Ruby and P. K. Tseng and H.-S. Cheng and N. C. Li. Chemical Physics Letters, Vol. 2, No. 1, 1968, p. 39–41. [Mössbauer measurements on very rapidly frozen solutions of HF, HCl, HBr and SnCl4.]Google Scholar
Schweitzer, D. G. Origin of irreversibility from conventional equilibrium concepts. Physics Letters, Vol. 27A, No. 6, 1968, p. 402–04. [Discussion with water-ice equilibrium as specific example.]Google Scholar
Scott, W. D. Hobbs, P. V. The spectra of charging events due to the collision of natural ice particles with an ice surface. Quarterly Journal of the Royal Meteorological Society, Vol. 94, No. 402, 1968, p. 510–22. [Measurements in natural conditions of charges acquired.]Google Scholar
Taub, I. A. Eiben, K. Transient solvated electron, hydroxyl, and hydroperoxy radicals in pulse-irradiated crystalline ice. Journal of Chemical Physics, Vol. 49, No. 6, 1968, p. 2499–2513. [Optical and electron spin resonance studies used to study transient intermediates produced in ice by electron irradiation.]Google Scholar
Whalley, E. Structures of ice and water as investigated by infrared spectroscopy. Developments in Applied Spectroscopy, Vol. 6, 1968, p. 2776. [Review of infrared spectra of ice and water and their interpretation.]CrossRefGoogle Scholar
Zander, R. Additional details on the near-infrared reflectivity of laboratory ice crystals. Journal of Geophysical Research, Vol. 73, No. 20, 1968, p. 6581–84. [Additional information on experiments previously reported, ibid., Vol. 71, No. 2, 1966, p. 375–78.]Google Scholar

Land ice. Glaciers. Ice shelves

Ambach, W. Eisner, H. Klimatologische Interpretationen eines Firnpollenprofiles. Veröffentlichungen der Schweizerischen Meteorologischen, entralanstalt, Nr. 4, 1967, p. 25–31. [Determination of net annual accumulation from pollen profile and comparison with climatic elements in Vent. French and English summaries.]Google Scholar
Ambach, W., and others. The altitude effect on the isotopic composition of precipitation and glacier ice in the Alps, by W. Ambach, W. Dansgaard, H. Eisner and J. Moller. Telles, Vol. 20, No. 4, 1968, p. 595–600. [Study of effect in rain, snow and glacier ice.]CrossRefGoogle Scholar
Benson, C. S. Glaciological studies on Mount Wrangell, Alaska, 1961. Arctic, Vol. 21, No. 3, 1968, p. 127–52. [Results of snow pit studies in the caldera of this volcano. Surface velocity measurements of caldera rim.]Google Scholar
Black, R. F. Bowser, C. J. Salts and associated phenomena of the termini of the Hobbs and Taylor Glaciers, Victoria Land, Antarctica. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 226–38. [Study of these salt deposits, the origin of which is still unknown.]Google Scholar
Budd, W. The longitudinal velocity profile of large ice masses. Union de Géodésie… Berne, 1967. Rapports et discussions, p. 58–77. [A local ice cap at the edge of the Antarctic ice sheet has provided data which are analysed in terms of glacier flow theory. Discussion by W. S. B. Paterson, G. de Q. Robin, L. Lliboutry and J. W. Glen, p. 75–77.]Google Scholar
Clapp, J. L. Ice-flow studies on Roosevelt Island. Antarctic Journal of the United Stales, Vol. 3, No. 4, 1968, p. 114. [Brief account of work done.]Google Scholar
Clarke, G. K. C. Geophysical measurements on Kaskawulsh and Hubbard Glaciers, Yukon Territory. Arctic Institute of North America. Technical Paper No. 20, 1967, 36 p. [Depth measurements by gravity and seismic means; surface velocity measurements.]Google Scholar
Clausen, H. B., and others. Si32 dating of an alpine glacier, by H. B. Clausen and B. Buchmann [and] W. Ambach. Union de Géodésie… Berne, 1967. Rapports et discussions, 1968, p. 135–40. [Ice from snout of Hintereisferner, Austria, has 32Si activity one-fifth of that of neighbouring glacier of Kesselwand-ferner implying age of 1200 years for snout ice of Hintereisferner.]Google Scholar
Clough, J. W., and others. Ice-thickness investigations on SPQMLT III, by J. W. Clough, C. R. Bentley, and C. K. Poster. Antarctic Journal of the United States, Vol. 3, No. 4, 1968, p. 96–97. [Seismic and electromagnetic reflection measurements during traverse.]Google Scholar
Collins, I. F. Swithinbank, C. W. M. Rifts at the foot of Beardmore Glacier, Antarctica. Union de Géodésie… Berne, 1967. Rapports el discussions, 1968, p. 109–14. [Suggestion that rifts are not annual but a flow phenomenon. Discussion by J. F. Nye and W. H. Ward, p. 113–14.]Google Scholar
Dahl, R. The retreat of the Reintind glacier (Frostiren). Norsk Geografisk Tidsskrift, Bd. 22, Ht. 4, 1968, p. 271−73. [Report of measurements of the margin of Reintindbreen made in 1950 and 1951 and comparison with data for 1906, 1934 and 1963.]Google Scholar
Fireman, E. L. Studies of material in polar ice. Antarctic Journal of the United States, Vol. 3, No. 6, 1968, p. 250–52. [Collection and analysis of particulate material from Greenland ice sheet.]Google Scholar
Giovinetto, M. B. Zumberge, J. H. The ice regime of the eastern part of the Ross Ice Shelf drainage system. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 255–66. [Estimate of components of mass balance for this ice shelf suggests positive net balance for whole of Ross Ice Shelf and of Antarctic ice sheet. Discussion by M. F. Meier and G. dc Q. Robin, p. 265–661Google Scholar
Gow, A. J. Preliminary analysis of ice cores from Byrd station. Antarctic Journal of the United States, Vol. 3, No. 4, 1968. p. 113–14. [Study of cores from first boring to penetrate Antarctic ice sheet.]Google Scholar
Gow, A. J., and others. Antarctic ice sheet: preliminary results of first core hole to bedrock, [by] A. J. Gow, H. T. Ueda, D. E. Garfield. Science, Vol. 161, No. 3845, 1968. p. 1011–13. [Temperature and density measurements and study of ice cores for hole bored “Byrd” station.]Google Scholar
Hoinkes, H. C. Gletscherschwankung und * in den Alpen. Veröffentlichungen der Schweizerischen Meteorologischen, Zentralansfalt. Nr. 4, 1967, p. 9–24. [Discussion of relation between general weather situations and glacier mass balance.]Google Scholar
Hoinkes, H. C. Wendler, G. Die Berechmmg des Strahlungsanteiles an der Ablation im Gebiet des Hintereis- und Kesselwandferners (Otztaler Alpen) im Sommer 1958. Veröffentlichungen der Schweizerischen Meteorologischen.Zentralansklt, Nr. 4, 1967, p. 43–45. [Preliminary report of study of radiation contribution to ablation.]Google Scholar
Ives, J. D. Glacier terminal and lateral features in northeast Baffin Island: illustrations with descriptive notes. Geographical Bulletin (Ottawa), Vol. 9, No. 2, 1967, p. 106–14. [Photographs showing terminal and lateral sections of five glaciers with notes.]Google Scholar
Judson, S. Hollin, J. T. Testing for Antarctic surges. Antarctic Journal of the United States, Vol. 3, No. 5, 1968, p. 183–84. [Programme to test whether Wilson’s surge theory of ice ages is correct.]Google Scholar
Kick, W. Experiences in comparing geometric elements of glacier variations. Union de Géodésie. … Berne, 1967. Rapports et discussions, 1968, p. 173–81. [Statistical analysis of measurements of length variations and of ice level variations show much less dispersal for level variations. Discussion by J. W. Glen and J. F. Nye, p. 180–81.1Google Scholar
LaChapelle, E. R. Glaciers. Transactions. American Geophysical Union, Vol. 48, No. 2, 1967, p. 729–36. [Reviews recent work, including Arctic and Antarctic regions.]Google Scholar
Lang, H. Relations between glacier runoff and meteorological factors observed on and outside the glacier. Union de Géodésie… Berne, 1967. Rapforls et discussions, 1968, p. 429–39. [Study on the Grosser Aletschgictscher of run-off from whole glacier and from a small drainage basin on the ice surface. Discussion by H. Lister and M. de Quervain, p. 438–39.]Google Scholar
Lang, H. Über den Tagesgang im Gletscherabfluss. Veröffentlichungen der Schweizerischen Meteorologischen Zentralanstall, Nr. 4, 1967, p. 32–38. [Comparison between melt-water run-off from glacier and meteorological factors. French and English summaries.]Google Scholar
Langway, C. C. jr. Deep ice core study program; Greenland. Antarctic Journal of the United States, Vol. 3, No. 5, 1968, p. 184–85. [Report of tests being made on all the “Site 2” and “Camp Century” cores.]Google Scholar
Lliboutry, L. Théorie complète du glissement des glaciers, compte tenu du fluage transitoire. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 33–48. [Generalization of theory presented in Journal of Glaciology, Vol. 7, No. 49. 1968, p. 21–58, by using a computer to extend the range of variables and to include effects of transient creep, which can introduce some instability. Discussion by J. F. Nye, p. 48. English summary.]Google Scholar
Løken, O. H. Sagar, R. B. Mass balance observations on the Barnes Ice Cap, Baffin Island, Canada. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 282–91. [Measurements made 1964–66 indicate considerable asymmetry. Discussion by M. F. Meier, W. J. Campbell, O. Orheins and G. Hattersley-Smith, p. 290–91.]Google Scholar
Lorius, C. A physical and chemical study of the coastal ice sampled from a core drilling in Antarctica. Union de Géodésie…Berne, 1967. Rapports et discussions, 1968, p. 141–48. [Stable isotope content used to establish origin of ice at various depths; studies of ice crystals, gas bubbles and impurities in agreement with interpretation]Google Scholar
Macpherson, D. S. Krouse, H. R. O18/O16 ratios in snow and ice of the Hubbard and Kaskawulsh Glaciers. (In Stout, G. E., ed. Isotope techniques in the hydrologic cycle. Washington, D.C.. American Geophysical Union. 1967, p. 180–94. (Geophysical Monograph Series, No. 11.)) [Observations interpreted and compared with other work. Discussion by K. Itagaki and D. J. Brown, p. 594.]Google Scholar
McSaveney, Y. M. J. Gage, M. Ice flow measurements on Franz Josef Glacier. New Zealand. New Zealand Journal of Geology and Geophysics, Vol. 11, No. 3, 1968, p. 564–92. [Measurements of surface velocity near actively advancing glacier snout associated with kinematic wave.]CrossRefGoogle Scholar
Meier, M. F. Calculations of slip of Nisqually Glacier on its bed: no simple relation of sliding velocity to shear stress. Union de Géodésie … Berne, 1967. Rapports el discussions, 1968, p. 49–57. [Results of analysis of measurements made at given transverse profile of Nisqually Glacier over 22 years.]Google Scholar
Mellor, M. The Greenland mass balance; flux divergence considerations. Union de Géodésie… Berne. 1967. Rapports et discussions, 1968. p. 275–81. [Possibility of determining changes in ice thickness if accumulation and surface strain-rates are known is used to assess ice thickness variations of Greenland ice sheet.]Google Scholar
Mercer, J. H. Glaciers of the Antarctic. Antarctic Map Folio Series (New York, American Geographical Society), Folio 7, 1967, 10 p. [Maps of glaciers of surrounding islands and of Antarctica itself.]Google Scholar
Merlivat, L., and others. Etudes isotopiques en profondeur d’un glacier en Antarctique, [par] L. Merlivat, C. Lorius, M. Majzoub, G. Nief et E. Roth. (In Isotopes in hydrology. Proceedings of the symposium … Vienna, 14–18 November 1966. Vienna, International Atomic Energy Agency, 1967, p. 671–81.) [Analysis of deuterium concentration in ice from bore hole in Terre Adélie used to deduce flow patterns.]Google Scholar
Nielsen, L. E. Some hypotheses on surging glaciers. Geological Society of America. Bulletin, Vol. 79, No. 9, 1968, p. 1195–1201. [Theory of surging glaciers based on sliding on the bed and fluidized block flow.]Google Scholar
Paterson, W. S. B. A temperature profile through the Meighen Ice Cap, Arctic Canada. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 440–49. [Measurements on this essentially stagnant ice cap and interpretation in terms of mean annual temperature changes. Discussion by M. de Quervain, p. 449.]Google Scholar
Reed, J. C., in Observations on the Teton Glacier, Grand Teton National Park, Wyoming, 1965 and 1966. U.S. Geological Survey. Professional Paper 575–C, 1967, p. C154–C159. [Ice movement measurements, sounding of a moulin, front variations,]Google Scholar
Sara, W. A. Franz Josef and Fox Glaciers, 1951–1967. New Zealand journal of Geology and Geophysics, Vol. 11, N 11. 3, 1968, p. 768–80. [Movements of the snouts of these glaciers.]Google Scholar
Schonbächler, M. Beziehung zwischen Strahlungsbilar and Ablation des Aletschgletschers (vorläufige Ergebnisse). Veröffentlichungen der Schweizerischen Meleoro,a, schen Zentralanstalt, Nr. 4, 1967. p. 39–42. [Preliminary results of measurements of radiation balance and ablation. Discussion. p. 41–42.]Google Scholar
Schytt, V. Notes on glaciological activities in Kebnekaise, Sweden, during 1966 and 1967. Geografiska Annaler, Vol. 50A, No. 2, 1968, p. 111–20. [Report of mass-balance and temperature studies on Storglaciären, observations of variations of Swedish glaciers, and spot observations of mass balance on 6 other glaciers.]Google Scholar
[Soviet Central Asia: Glaciology.] Gidrologicheskiy rezhim lednikov . Akademiya Nook Kazakhskoy SSR. Sektor Fizicheskey Geograf[i. Clyaisiologicheskiye issledovaniya v Kazakhstane . Vyp. 7. Alma-Ata, Izdatel’stvo “Nauka” Kazakhskoy SSR, 1968. 156 p. [Contains the following papers, all in Russian with English summaries: R. G. Golovkova and others, “Meteorological conditions of ablation of glacier of southern exposure in the Zailiyskiy Alatau”, by R. G. Golovkova, T. Ya. Denisova and G. A. Rakhimzhanova, p. 5–31; R. G. Golovkova and G. A. Rakhimzhanova, “Heat and moisture exchange on Lednik Tsentral’nyy Tuyuksu”, p. 32–42; N. N. Palgov, “Hydrological definition of the glacial and nival landscape”. p. 43–59; P. A. Sudakov, “Dates of setting in of snow cover and its term of life in the glacial zone of Zailiyskiy Alatau”, p. 60–70; P. A. Sudakov and others, “Characteristic features of formation of solid sediments in the glacial zone of the Zailiyskiy Alatau”, by P. A. Sudakov, G. A. Tokmagambetov and P. F. Shabanov, p. 71–80; P. A. Sudakov and V. A. Zenkova, “Some regularities of the distribution of maximum snow cover in the glacial belt of the Zailiyskiy Alatau”, p. 81–86; P. A. Sudakov and G. A. Tokmagambetov, “Wind conditions and redistribution of snow and snow cover in the glacial zone of the Zailiyskiy Alatau”, p. 87–94; Ye. N. Vilesov and I. Ya. Fedulov, “Lednik Korzhenevskogo in the Zailiyskiy Alatau”, p. 95–103; K. G. Makarevich and I. Ya. Fedulov, “Initial data on the regime of Lednik Korzhenevskogo”, p. 104–16; P. A. Cherkasov, “Dependence of ablation on the height of location and on the orientation and the angle of inclination of glaciers of the Dzhungarskiy Alatau (from the example of the glaciers of the Tentek river basin)”, p. 117–37; P. A. Cherkasov and V. A. Chekhonadskaya, “Run-off from glaciers and its role in the nourishment of the rivers Tentek and Rgayty in the Dzhungarskiy Alatau range”, p. 138–45; N. V. Yerasov, “The volume of ice of the glaciers of the northern slopes of the Dzhungarskiy Alatau and method of its calculation (by way of discussion)”, p. 146–51.]Google Scholar
Swithinbank, C. W. M. Radio echo sounding of Antarctic glaciers from light aircraft. Union de Géodésie … Berne, 1967. Rapports el discussions, 1968, p. 405–14. [Report of soundings over the Antarctic Peninsula area. Successful over ice shelves and at high latitudes or in high terrain. Discussion by M. de Quervain, W. Ambach, C. B. B. Bull, J. F. Nye and J. Behrendt, p. 413–14]Google Scholar
Tangborn, W. V. Mass balances of some North Cascade glaciers as determined by hydrologic parameters. 1920–65. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 267–74. [Difference between stream flow in glacierized and non-glacierized basins used with precipitation data to deduce mass balance of glaciers of Thunder Creek drainage basin. Results compared with measurements on neighbouring South Cascade Glacier. Discussion by J. W. Glen, p. 274.]Google Scholar
Tonini, M. Rossi, G. Le glacier de la Marmolada; variations depuis 1951. Union de Géodésie… Berne. 1967. Rapports et discussions, 1968, p. 193–206. [Results of photogrammetric measurements of this Italian glacier. English abstract.]Google Scholar
Tsukernik, V. B., and others. Komplekanyye geofizicheskiye issledovaniya na zapadnom shel’fovom lednike . Trudy Souetskoy Antarkticheskoy Ekspeditsii, Tom 48, 1967, p. 79–96. [Seismic, magnetic and gravity studies to determine thickness and structure.]Google Scholar
Vanni, M. Les variations des glaciers italiens au cours des dix dernières années 1957–1966. Union de Géodésie… Berne, 1967. Rapports el discussions, 1968, p. 182–92. [During the last decade an increasing number of glacier fronts in Italy have become stationary. Discussion by A. Krenke, L. I.liboutry and M. de Quervain, p. 192. English abstract.]Google Scholar
Vivian, R. Jail, M. Fiches des glaciers français. Le glacier de la Grande Motte. Revue de Géographie Alpine, Tom. 57, Fasc. 1, 1969, p. 229–31. [General description.]Google Scholar
Weller, G. The annual heat energy transfer above and inside Antarctic blue ice. Union de Géodésie… Berne, 1967. Rapports et discussions, 1968, p. 417–28. [Measurements near Mawson.]Google Scholar
Zinger, Ye. M. Troitskiy, L. S. Sovetskiye glyatsiologicheskiye issledovaniya na Shpitsbergene v 1966 godu . Izvestiya Akademii Nauk SSSR. Seriya Geograficheskaya, 1967, No. 2, p. 157–59.Google Scholar

Icebergs. Sea, River and Lake Ice

Adams, W. P. Jones, J. A. A. Crystallography of ice on Knob Lake. McGill Sub-Arctic Research Laboratory. Research Paper No. 23, 1967, p. 108–17. [Results of pilot study, April 1966; lake near Schefferville, Quebec.]Google Scholar
Campbell, W. J. Synoptic temperature measurements of a glacier lake and its environment. Union de Géodésie… Berne, 1967. Rapports et discussions, 1968, p. 450–58. [Temperature measurements within a small lake at end of South Cascade Glacier, Washington State, U.S.A.]Google Scholar
Dingman, S. L., and others. The effects of thermal pollution on river ice conditions, by S. L. Dingman, W. F. Weeks and Y. C. Yen. Water Resources Research, Vol. 4, No. 2, 1968, p. 349–62. [Calculation of ice-free reach below such a site.]Google Scholar
Ferguson, H. L. A preliminary estimate of the ice-season energy balance for the Niagara River. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 13e An., No. 3, 1968, p. 41–58. [Estimate of various terms in energy balance and its use in ice forecasting.]Google Scholar
Gjessing, Y. T. On the relation between the meteorological conditions and the freezing of Lusterfjord. Norsk Geografuk Tidsskrift, Bd. 22, Ht. 3, 1968, p. 200–08. [Explanation of why this fjord freezes rapidly in mild weather but sometimes remains ice-free in very cold weather.]Google Scholar
Gyulai, Z. Jeszenszky, B. Wachstumsfiguren auf der freien Eisfläche eines kleinen Sees. Revue Roumaine de Physique, Tom. 13, No. 2, 1968, p. 159–61. [Study of geometrical figures on surface of lake ice and deductions about growth process.]Google Scholar
Langleben, M. P. The heat budget of a melting cover of sea ice. Union de Géodésie… Berne, 1967. Rapports et discussions, 1968, p. 151–60. [Measurements at Tanquary Fiord, Ellesmere Island, Canada, in spring and early summer. Discussion by G. P. Williams and E. R. LaChapelle, p. 159–60.]Google Scholar
Lindsay, D., and others. Ice islands, 1967, [by] D. Lindsay, W. Seifert, N. Anderson. Arctic, Vol. 21, No. 2, 1968, p. 103–06. [Movements observed for ice islands which broke away from Ward Hunt Ice Shelf in 1961–62.]Google Scholar
Makarevich, T. N., and others. Osenniye ledovyye yavleniya na rekakh severnogo kraya i vozmozhnosti ikh prognoza . Trudy Gosudarstvennogo Gidrologicheskogo Institute, Vyp. 138, 1967, p. 3–75. [Correlations with preceding weather in Pechora and Severnaya Dvina basins.]Google Scholar
Pounder, E. R. Langleben, M. P. Acoustic attenuation in sea ice. Union de Géodésie.… Berne, 1967. Rapports et discussions. 1968, p. 161–69. [Laboratory and field measurements in frequency range 10–500 kHz.]Google Scholar
Šinik-Labovic, N. Die atmosphärischen Ursachen von Donauhochwassern in Österreich während der kalten Jahreszeit. Welter und Leben, Jahrg. 20, Ht. 11–12, 1968, p. 243–49. [Study of meteorological conditions which lead to break-up of ice cover of the Danube and resulting floods.]Google Scholar
Spetzler, H. Anderson, D. L. The effect of temperature and partial melting on velocity arid attenuation in a simple binary system. Journal of Geophysical Research, Vol. 73, No. 18, 1968, p. 6051–60. [Study of propagation of sound waves through ice-salt mixtures with and without appreciable brine volumes.]Google Scholar

Glacial Geology

Andrews, J. T. Pattern and cause of variability of postglacial uplift and rate of uplift in Arctic Canada. Journal of Geology, Vol. 76, No. 4, 1968, p. 404–25. [Variability of uplift in Arctic Canada correlated with distance from ice margin and date of deglaciation.]Google Scholar
Andrews, J. T. King, C. A. M. Comparative till fabrics and till fabric variability in a till sheet and a drumlin: a small-scale study. Proceedings of the Yorkshire Geological Society, Vol. 36, Pt. 4, 1968, P. 435–61. [Study of fabric with attention to shape of pebbles. Discussion, p. 459–61.]Google Scholar
Bennett, R. G. Frost shatter and glacial erosion under the margins of Osterdalsisen, Svartisen. Norsk Geografirk Tidrskrift, Bd. 22, Ht. 3, 1968, p. 209–13. [Subglacial observations showed more debris was transported by the glacier in winter than in summer.]Google Scholar
Birman, J. H. Glacial reconnaissance in Turkey. Geological Society of America. Bulletin, Vol. 79, No. 8, 1968. p. 1009–26. [Evidence of glaciation in various parts of Turkey.]Google Scholar
Clayton, L. Late Pleistocene glaciations of the Waiau valleys, North Canterbury. New Zealand Journal of Geology and Geophysics, Vol. 11, No. 3, 1968, p. 753–67. [Glacial chronology of this area of New Zealand.]Google Scholar
Clayton, L. Freers, T. F., ed. Glacial geology of the Missouri Coteau and adjacent areas. North Dakota Geological Survey. Miscellaneous Series 30, 1967, v, 170 p. [Guidebook and papers for 18th annual field conference of Midwest Friends of the Pleistocene, south-central North Dakota, 19–21 May 1967. Includes following papers: L. Clayton, “Stagnant-glacier features of the Missouri Coteau in North Dakota”. p. 25–46; L. Clayton and J. A. Cherry, “Pleistocene superglacial and ice-walled lakes of west-central North America”, P. 47–52; C. F. Royse and E. Callender, “A preliminary report on sonie ice-walled-lake deposits (Pleistocene). Mountrail County, North Dakota”, p. 53–62; M. J. J. Bik, “On the periglacial origin of prairie mounds”, p. 83–94; W. A. Pettyjohn. “Dump ridges and collapsed sub-ice channels in Ward County. North Dakota”, p. 115–16; T. E. Kelly and F. Buturla, Jr., “Pleistocene diversion of streams in central North Dakota”, p. 117–21; W. A. Pettyjohn, “Multiple drift sheets in southwestern Ward County. North Dakota”, p. 123–29; J. P. Bluemle, “Multiple drifts in northeast North Dakota”, p. 133–36.]Google Scholar
Denton, G. H. Armstrong, R. L. Glacial geology and chronology of the McMurdo Sound region. Antarctic Journal of the United Slates, Vol. 3, No. 4, 1968, p. 99–101.Google Scholar
Derbyshire, E. Glacial map of N.W.-central Tasmania. Tasmania. Department of Mines. Geological Survey Record No. 6, 1968, 58 p., map [in folder at back]. A $0.50. [Description of this map and of the glacial morphology, sediments and stratigraphy of the area.]Google Scholar
Dionne, J.-C. Boucher, P. Levé des striures glaciaires le long de la Nationale 54–A (parc des Laurentides). Cahiers de Géographie de Québec, 11e An., No. 24. 1967, p. 574–76. [Survey of glacial striae in this part of Quebec.]Google Scholar
Foss, J. E. Rust, R. H. Soil genesis study of a lithologie discontinuity in glacial drift in western Wisconsin. Proceedings. Soil Science Society of America, Vol. 32, No. 3, 1968, p. 393–98. [Discontinuities dated at 30000 and 14000 years B.P.]Google Scholar
Gidon, M., and others. Sur la morphologie fluvio-glaciaire aux marges des glaciers Würmiens alpins: le dispositif moraine-chenal marginal, par M. Gidon, G. Montjuvent et E. Steinfàtt. Bulletin de l’Association Française pour l’Étude du Quaternaire, 5e An., No. 15, 5968, p. 125–49. [Complex terraces in this region of France interpreted as ice marginal features.]Google Scholar
Haefeli, R. Gedanken zum Problem der glazialen Erosion. Rock Mechanics and Engineering Geology: Felsmechanik und Ingenieurgeologie, Suppl. 4, 1968, p. 31–51. [Discussion of problems of glacial erosion and particularly overdeepening in light of recent developments in ice and rock mechanics.]Google Scholar
Harris, S. A. Till fabrics and speed of movement of the Arapahoe Glacier, Colorado. Professional Geographer, Vol, 20, No. 3, 5968, p. 195–98. [Measurement of amount of preferred orientation in newly deposited moraine near site where ice velocity is known. Strong correlation found.]Google Scholar
Holmes, G. W. Foster, H. L. Geology of the Johnson River area, Alaska. U.S. Geological Survey. Bulletin 1249, 1968, vi, 49 p., map [in folder at back]. [Includes sections on glacial geology and on frost action and mass movement.]Google Scholar
Ives, J. D. Late-Wisconsin events in Labrador-Ungava: an interim commentary. Canadian Geographer, Vol. 12, [No.] 3, 1968, p. 192–203. [Discussion of recent papers dealing with this subject.]Google Scholar
Laverdière, C. Dionne, J.-C. Une nouvelle forme glaciaire: les micro-bourrelets concentriques de plage. Cahiers de Géographie de Québec, 11e An., No. 24, 1967, p. 570–73. [Description of concentric beach microridges formed by the melting of lake ice trapped in beach deposits.]Google Scholar
Lister, H., and others. Laboratory experiments on abrasion of sandstones by ice, [by] H. Lister, A. Pendlington and J. Chorlton. Union de Géodésie … Berne, 1967. Rapports et discussions. 1968, p. 98–106. [Rate of abrasion as function of velocity and duration of test.]Google Scholar
McGinnis, L. D. Glacial crystal bending. Geological Society of America. Bulletin, Vol. 79, No. 6, 1968, p. 769–75. [Theory of glacial isostatic bending and marginal uplift.]Google Scholar
Mercer, J. H. Antarctic ice and Sangamon sea level. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 217–25. [Evidence that interglacial temperatures were 7–10° C higher in Antarctica than today. Implications of this for Antarctic ice shelves and Antarctic ice sheet; consequent sea-level changes. Discussion by C. B. B. Bull, J. T. Hollin and C. W. M. Swithinbank, p. 225.]Google Scholar
Nye, J. F. Martin, P. C. S. Glacial erosion. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 78–86. [Perfectly plastic glacier theory suggests that concave curvature of glacier bed cannot exceed a limiting value. Application to theory of glacial erosion of rock bars. Discussion by L. Lliboutry, E. R. LaChapelle, W. H. Ward and I. F. Collins, p. 83–86.]Google Scholar
Phrola, J. Die glazialen Oberflächenformen und die Entwicklung der Täler auf den Fjelden Marastotunturit und Viipustunturit in Finnisch-Lappland. Annales Academiae Scientiarum Fennicae, Ser. A, 3, Geologica-Geographica, Tom. 92; Publicationes Inslituti Geographici Universilatis Helsingiensis, No. 54, 1967, 115 p. [Glacial geology and valley formation in Marastotunturit and Viipustunturit mountains in Finnish Lapland. Field work in 1962, 1963, 1965 and 1966.]Google Scholar
Prest, V. K. Nomenclature of moraines and ice-flow features as applied to the glacial map of Canada. Canada. Geological Survey. Paper 67–57, 1968, v, 32 p. [Description of nomenclature adopted in preparing glacial map of Canada.]Google Scholar
Röthlisberger, H. Erosive processes which are likely to accentuate or reduce the bottom relief of valley glaciers. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 87–97. [Discussion of various processes involved in glacial erosion. Discussion by L. Lliboutry, p. 96–97.]Google Scholar
Schweizer, G. Der Formenschatz der Spät- und Postglazials in der Hohen Seealpen. Aktualgeomorphologische Studien im oberen Tinéetal. Zeitschrift für Geomorphologie, Supplementbd. 6, 1968, vii, 167 p. [Study of present-day and late- and post-glacial geomorphological processes in this region of the French Alps. French summary.]Google Scholar
Schytt, V., and others. The extent of the Würm glaciation in the European Arctic; a preliminary report about the Stockholm University Svalbard Expedition 1966, [by] V. Schytt, G. Hoppe, W. Blake, Jr., and M. G. Grosswald [i.e. M. G. Grosval’d]. Union de Géodésie… Berne, 1967. Rapports et discussions, 1968, p. 207–16. [Evidence from raised beaches in Svalbard for existence of thick ice sheet over Barents Sea. Discussion by N. A. Ostenso, O. H. Laken and R. F. Black. p. 216.]Google Scholar
Straw, A. A geomorphological appraisal of the deglaciation of an area between Hamilton and Guelph, southern Ontario. Canadian Geographer, Vol. 12, [No.] 3, 1968, p. 135–43. [Discussion of surface features and their relation to glacial deposits.]Google Scholar
Synge, F. M. The glaciation of west Mayo. Irish Geography, Vol. 5, No. 5, 1968, p. 372–86. [Study of this region of Ireland indicates that in last glaciation the highlands were not major centres of ice dispersal.]Google Scholar
Viers, G. La carte du relief glaciaire des Pyrénées. Feuille de Mont-Louis au 50000e (Pyrénées Orientales). Revue Géographiques des Pyrénées et du Sud-Ouest, Tom. 39, Fasc. 4, 1968, p. 429–34. 2 maps. [Presentation and description of maps showing glacial relief of this part of the French Pyrenees.]Google Scholar
Westgate, J. A. Linear sole markings in Pleistocene till. Geological Magazine, Vol. 105, No. 6, 1968, p. 501–05, 4 plates. [Description of current-produced sole markings in Pleistocene till deposits of Alberta, Canada, and their use as rapid indicator of local ice-flow directions.]Google Scholar
White, A. H. The glacial origin of Carboniferous conglomerates west of Barraba, New South Wales. Geological Society of America. Bulletin, Vol. 79, No. 6, 1968, p. 675–86. [Conglomerate considered to be a tillite formed as a moraine probably from Alpine type glaciation.]Google Scholar

Frost Action on Rocks and Soil. Frozen Ground. Permafrost

Blagbrough, J. W. Farkas, S. E. Rock glaciers in the San Mateo Mountains, south-central New Mexico. American Journal of Science, Vol. 266, No. 9, 1968, p. 812–23. [Description of these rock glaciers of Wisconsin age and discussion of their origin and development.]Google Scholar
Clark, G. M. Sorted patterned ground: new Appalachian localities south of the glacial border. Science, Vol., 161, No. 3839, 1968, p. 355–56. [Observation of stripes, nets and polygons in this area. Possible implications for palaeoclimate.]Google Scholar
Grave, N. A. Nekrasov, I. A., ed. Geokriologicheskiye usloviya Zabaykal’skogo Severa . Moscow, Izdatel’stvo “Nauka”, 1966. 216 p. [Permafrost in northern Chitinskaya Oblast’.]Google Scholar
Low, P. F., and others. Some thermodynamic relationships for soils at or below the freezing point. I. Freezing point depression and heat capacity, [by] P. F. Low, D. M. Anderson and P. Hoekstra. Water Resources Research, Vol. 4, No. 2, 1968, p. 379–94. [Derivation of equation and deduction of values.]Google Scholar
Morand, F., and others. Cryoturbation et solifluxion sur les versants d’une platiere en foret de Fontainebleau: le nord de la Malmontagne, par F. Morand, G. Rougerie, [et] O. Vaudene. Bulletin de l’Association Franfaise pour l’Étude du Quaternaire, 5e An., No. 15, 1968, p. 83–88. [Solifluxion deduced from movement of sandstone slabs.]Google Scholar
Popov, A. I. Merzlotnyye yavleniya a zemnoy kore (kriolitologáya) . Moscow, Izdatel’stvo Moskovskogo Universiteta, 1967. 304 p. [Textbook on permafrost.]Google Scholar
Romanovskiy, N. N. Chiznov, A. B. Voprosy vzaimosvyazi i vzaimodeystviya podzemnykh vod i merzlykh tolshch gornykh porod . Vestnik Moskoaskogo Universiteta, Ser. 4, 1967, No. 4, p. 22–36. [Physical processes of heat and mass exchange between frozen ground and ground water.]Google Scholar
Sheveleva, N. S. Khomichevskaya, L. S. Geokriologicheskiye usloviva yenisevskogo severa . Moscow, Izdatel’stvo “Nauka”, 1967. 127 p. [Characteristics of permafrost and associated land forms.]Google Scholar
Tak-Schneider, U. van den. Fossil frost fissures in the province of Jönköping, Sweden. Geografiska Annaler, Vol. 50a, No. 2, 1968, p. 109–10. [Description of observations.]Google Scholar
Tremblay, G. Glacitectonique dans la partie est de la région du lac Saint-Jean. Cahiers de Géographie de Québec, 11e An., No. 24, 1967, p. 563–66. [Study of periglacial features in this region of Quebec and deduction of climatic conditions during deglaciation.]Google Scholar

Meteorological and Climatological Glaciology

Berg, T. G. O. Gaukler, T. A. Exploratory studies of charged ice particles in natural clouds. Journal of Applied Meteorology, Vol. 7, No, 5, 1968, p. 952–55. [Apparatus for collecting and studying such particles and preliminary results.]Google Scholar
Briggs, G. A. Weather note. Hailstones, starfish. and daggers—spiked hail falls in Oak Ridge, Tennessee. Monthly Weather Review, Vol. 96, No. 10, 1968, p. 744–45. [Report of fall of unusually shaped hailstones.]2.0.CO;2>CrossRefGoogle Scholar
Browning, K. A., and others. The collection and analysis of freshly fallen hailstones, by K. A. Browning. J. Hallett. T. W. Harrold and D. [A.] Johnson. Journal of Applied Meteorology, Vol. 7. No. 4, 1968, p. 603–12. [Method of locating large hailstones for immediate collection and results of sectioning them.]Google Scholar
Davis, C. I. Steele, R. L. Performance characteristics of various artificial ice nuclei sources. Journal of Applied Meteorology, Vol. 7, No. 4, 1968, p. 667–73. [Results of field studies.]Google Scholar
Goyer, G. G. Plooster, M. N. On the role of shock waves and adiabatic cooling in the nucleation of ice crystals by the lightning discharge. Journal of the Atmospheric Sciences, Vol. 25, No. 5, 1968, 857–62. [Labora- tory study of supercooled cloud subjected to shock waves. Results suggest shock wave from lightning does not cause nucleation.]Google Scholar
Hoinkes, H. C., and others. Glacier mass budget and mesoscale weather in the Austrian Alps 1964 to 1966. by H. C. Hoinkes, F. Howarka and W. Schneider. Union de Géodésie … Berne, 1967. Rapports el discussions, 1968, p. 241–54. [Comparison between ablation phenomena on glaciers in two regions of Austria and the frequency of selected weather types during the ablation season. Discussion by H. Lister and J. C. Thams. p. 253–54.]Google Scholar
Knight, C. A. Knight, N. C. The final freezing of spongy ice: hailstone collection techniques and interpretations of structures. Journal of Applied Meteorology, Vol. 7, No. 5, 1968, p. 875–81. [Study of preservation of freezing structure by quenching balloons containing spongy ice in dry-ice-alcohol mixture.]Google Scholar
List, R. Parsons, D. F. Simulation of the total heat transfer of spherical hailstones. Heluelica Physica Acta. Vol. 41, Fasc. 6–7, 1968, p. 1016–20. [Introduction of an effective Nusselt number to explain how different icing conditions can produce similar ice and air bubble structures in hailstones.]Google Scholar
Morel, P., and others. The occurrence of icing on constant level balloons, by P. Morel, J. Fourrier and P. Sitbon. Journal of Applied Meteorology, Vol. 7, No. 4, 1968, p. 626–34. ‘Observation of ice loading and explanation as due to fall of large ice particles on top of balloon.]Google Scholar
Mossop, S. C., and others. Glaciation of a cumulus at approximately −4C, [by] S. C. Mossop, R. E. Ruskin and K. J. Heffernan. Journal of the Atmospheric Sciences, Vol. 25. No. 5, 1968. p. 889–99. [Observation on cloud showed many columnar crystals. more than expected number of ice nuclei.]Google Scholar
Peterson, M. P. Spillane, K. T. Oceans as a source of ice nuclei. Nature, Vol. 218, No. 5149., 1968, p. 864–65. [Experiments show that peptides in the ocean are not a source of natural ice nuclei.]Google Scholar
Radok, U., and others. Surface and subsurface meteorological conditions at Plateau Station. by U. Radok. P. Schwerdtfegcr and G. Weller. Antarctic Journal of the United States, Vol. 3. No. 6. 1968. p. 257–58. [Preliminary results of studies of snow temperature, snow heat flux. levelling of snow surface by sublimation-deposition, surface accumulation and snow drift.]Google Scholar
Streten, N. A. Wendler, G. Some observations of Alaskan glacier winds in midsummer. Arctic. Vol. 2 t. No. 2, 1968. p. 98–102. [Results of wind observations on Worthington and Castner Glaciers.]Google Scholar

Snow

Barnes, J. C. Bowley, C. J. Snow cover distribution as mapped from satellite photography, Water Resources Research, Vol. 4. No. 2, 1968, p. 257–71. [Maps of distribution in Missouri and upper Mississippi river basins.]Google Scholar
Bergen, J. D. Atmospheric humidity measurement near the snow surface. U.S. Forest Service Research Note RM-116, 1968, 4 p. [Technique for measuring humidity in first few cm above snow surface and some results obtained.]Google Scholar
Bergen, J. D. Some measurements of air permeability in a mountain snow cover. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 13e An., No, 3. 1968, p. 5–53. [Results of air permeability correlated with grain size and porosity.]Google Scholar
Bergen, J. D. Some observations on temperature profiles of a mountain snow cover. U.S. Forest Service Research Note RM-110, 1968, 7 p. [Measurements of profiles and discussion of how they vary.]Google Scholar
Cavazza, S. Variations de densité dans les parties supérieures et inférieures de la couche de neige (Calabre, Italic). Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 359–69. [Statistical analysis of 144 density measurements made on snow cover. Discussion of characteristics of density variations and extent to which measurements are representative. English abstract.]Google Scholar
Chitadze, V. S. Analytical method of the forecast of snow avalanches. Vergentlichungen der Schweizerischen Meteorologischen Zentralanstalt, Nr. 4, 1967, p. 46–50. [Description of analytical method used to predict avalanches.]Google Scholar
Hanappe, F., and others. Chimie des neiges antarctiques et taux de deposition de matière extraterrestre deuxième article, [par] F. Hanappe. M. Vosters. E. [E.] Picciotto. and [sic] S. Deutsch. Earth and Planetary Science Letters, Vol. 4, No. 6, 1968. p. 487–96, [New and lower estimate of deposition rate. English summary.]Google Scholar
Hansen, E. A. Ffolliott, P. F. Observations of snow accumulation and melt in demonstration cuttings of ponderosa pine in central Arizona. U.S. Forest Service Research Note RM-111, 1968, 12 p. [Study of effect on snow accumulation and run-off of strips cut through forest in various aspects.]Google Scholar
Hobbs, P. V. The metamorphism of dry snow at a uniform temperature. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 392–402. [Study of mechanisms by which strength and density of old, dry snow change; deduction that strength is governed by diffusion through the vapour phase, density by bulk diffusion through the solid. Discussion by 6 contributors, p. 400–02.]Google Scholar
Holtmeier, F.-K. Entgegnung zu; “Über ‘Schneeschliff’ in den Alpen” von Hans Turner. Wetter imd Leben, Jahrg. 20, Ht. 9–10, 1968, p. 201–05. [Comments on paper by Turner, ibid., Jahrg. 20, Ht. g to, 1968. p. 192–200, which discusses a point arising from an earlier article of Holtmeier’s on the damage to young trees caused by snow-laden wind.]Google Scholar
Jaffé, A. Über Bine Ursache frühsommerlicher Schneefalle in Talniederungen. Veröffèntlichungen der Schweizerischen Meteorologischen Zentralanstalt, Nr. 4, 1967, p. 150–54. [Meteorological explanation for snowfalls which occur in early summer in Alpine valleys. French and English summaries.]Google Scholar
Kuhn, W. Snow cylinders at Geltwil, Switzerland. Meteorological Magazine, Vol. 97, No. 1956, 1968, p. 350, 2 plates. [Short report of formation of hollow snow cylinders and meteorological conditions at the time.]Google Scholar
Kuroiwa, D. Liquid permeability of snow. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 380–91. [Studies of permeability of kerosene through natural and artificial snow and comparison with porosity.]Google Scholar
Leaf, C. F. Areal extent of snow cover in relation to streamllow in central Colorado. (In Proceedings. The International Hydrology Symposium, September 6–8, 1967. Fort Collins, Colorado, U.S.A. Fort Collins, Colorado, Colorado State University, 1968, Vol, 1, p. 157–64.) [Study of relation between snow depletion seen on aerial photographs and run-off.]Google Scholar
Megahan, W. F., and others. Net, allwave radiation as an index of natural snowmelt and snowmelt accelerated with albedo reducing materials, [by] W. F. Megahan, J. R. Meiman and B. C. Goodell. (In Proceedings. The International Hydrology Symposium, September 6–8, 1967, Fort Collins, Colorado, U.S.A. Fort Collins. Colorado. Colorado State University, 1968, Vol. s, p. 149–56.) [Field study of usefulness of net radiation as index of snow melt.]Google Scholar
Meiman, J. R. Slaughter, C. W. Long-chain alcohol suppression of snow evaporation. Proceedings of the American Society of Civil Engineers. Journal of the Hydraulics Division, Vol. 93, No. HY6, 1967, p. 271–79. [Laboratory studies of reduction of evaporation when emulsions of these substances are applied to snow surface.]Google Scholar
Meyer, L. Comparaison des caractéristiques de la couche de neige des deux hivers 1964–1965 et 1965–1966 au Col de Porte (Isère), France. Vereentlichurgera der Schweizerischen Meteorologischen Zentralanstalt, Nr. 4., 1967, p. 139–49. [Study of snow pack development over two winters.]Google Scholar
Moskalev, Yu. D. Problems of the forecasts ofsnow avalanches in the Tien-Shan. Veröíèratlichungen der.Schweizerischen Metecrologischen Zentralanstalt, Nr. 4, 1967. p. 51–59. [Description of difference of problem in Alps or Caucasus and Tien-Shan and of methods used.]Google Scholar
Pavlov, V. V. and others. Otsenka oslableniya y-izlucheniya of radioaktivnykh osadkov snezhnym pokrovom . Atomnaya Energiya. Tom 25, Vyp. 1, 1968, p. 66–67. [Letter. Estimates of effect of snow layers in reducing 137Cs γ-irradiation from the soil.]Google Scholar
Rogerson, R. J. Snow research at Knob Lake, winter 1965–1966. McGill Sub-Arctic Research Laboratory. Research Paper No. 23, 1967, p. 85–93. [Account of year’s activities, chiefly snow surveys; lake near Schefferville, Quebec.]Google Scholar
Rundle, A. S. Snow stratigraphy and accumulation (SPQMLT III). Antarctic Journal of the United Stales, Vol. 3, No. 4. 1968, p. 95–96. [Measurements during traverse.]Google Scholar
Salm, B. On nonuniform, steady flow of avalanching snow. Union de Géodésie … Berne, 1967. Rapports el discussions, 1968, p. 19–29. [Hydraulic theory used to develop theory of steady but turbulent flow of avalanche material. Discussion by A. Dyunin, p. 29.]Google Scholar
Smith, J. L., and others. Isotope snow gages for determining hydrologic characteristics of snowpacks, [by] J. L. Smith, D. W. Willen and M. S. Owens. (In Stout, G. E., ed. Isotope techniques in the hydrologic cycle. Washington, D.C.. American Geophysical Union, 1967, p. 11–21. (Geophysical Monograph Series, No. 11.)) [System for measuring snow density at small vertical intervals or for faster profiling at larger intervals. Discussion by 5 contributors. p. 20–21.]Google Scholar
Sneyers, R. L’épaisseur maximale de la couche de neige en Belgique. Veröffentlichungen der Schweizerischen Meteorologischen Zentralanstalt, Nr. 4, 1967, p. 124–31. [Statistical analysis of data on maximum snow depth in Belgium, German and English summaries.]Google Scholar
Turner, H. Über “Schneeschliff” in den Alpen. Wetter und Leben, Jahrg. 20, Ht. 9–10, 1968, p. 192–200. [Discussion of whether snow-laden wind has injurious effects on tree regeneration. English summary.]Google Scholar
Wakahama, G. The metamorphism of wet snow. Union de Géodésie … Berne, 1967. Rapports et discussions, 1968, p. 370–79. [Laboratory study of metamorphosis of snow in cold chamber at 0°C with differing amounts of added water and with and without added weight.]Google Scholar
Wishart, E. R. Electrical phenomena in snow drift. Antarctic Journal of the United States, Vol. 3, No. 6, 1968, p. 256–57. [Measurement of charge on drift particles.]Google Scholar
Younkin, R. J. Circulation patterns associated with heavy snowfall over the western United States. Monthly Weather Review, Vol. 96, No. 12, 1968, p. 851–53. [Relationship between circulation patterns and snowfall studied to improve forecasting.Google Scholar
Zingg, T. Die Niederschlags- und Lawinenverhältnisse im Frühwinter in den oberen Vispertälern. Veroffentlichunhen der Schweizerischen Meteorologischen Zentralanstalt, Nr. 4, 1967, p. 92–96. [Discussion of early winter precipitation in this Alpine valley and its effect on avalanche formation.]Google Scholar