Karlsson, T. ed. Proceedings, the second international conference on port and ocean engineering under Arctic conditions. University of Iceland. Dept. of Engineering and Science. Reykjavík, Iceland. August 27–30, 1973. [Reykjavík, University of Iceland, 1974.] viii. 801 p. [Includes the following papers: D. Bajzak, “A remote sensing program in sea ice and current studies”, p. 3–21; Ashton, G. D.,DenHartog, S. L.,Hanamoto, B. “Icebreaking by tow on the Mississippi River with mv Renee G”, p. 63–79; Edwards, R. Y.,German, J. G.,Lawrence, R. G. A “Comparative model tests of the icebreaker performance of two Canadian Coast Guard icebreakers”, p. 80–99;Legerer, F. J. “Design Strategy for ice navigation”, p. 101–14; Mäkinen, K. “Ship model testing in ice. Possibilmes and reliability”, p. 115–37;Lewis, J. W.,Ehrlieh, N. A. andLecourt, E. J. “Development of a craft capable of preparing an ice free channel through solid iee cover”, p. 138–61; Bárðarson, H. R. “Icing of ships”, p. 185–202;Lewis, E. L. “Arcticfjord flushing”, p. 233 37;Walker, H. J. “Changes occurring in the oceanic portion of the Colville River delta, Alaska during spring flooding”. p. 266–73; Hirayama, K.,Schwarz, J. andWu, H. C. “Model technique for the investigation of ice forces on structures”, p. 332–44; Sundararajan, C. andReddy, D. V. “Stochastic analysis of ice-structure interaction”, p. 345–53; Holdsvvorth, G.,Traetteberg, A. “The deformation of an Arctic ice island”, p. 419–40;Murty, T. S.,Barber, F. G. “An assessment of ice transport in the Hudson Bay region”, p. 441–50;Mills, D. A. “Ridges and rafted ire on Lake Melville”, p. 451–72;Nemec, A. O.,Mills, D. A.,Langford, C. J. andJesseau, S. L. “Lake Melville ice investigation, Labrador”, p. 472–89;Parmerter, R. R. “Dimensionless strength parameters for floating ice sheets”, p. 490–501;Benedict, C. P. “Underwater profiling of icebergs”, p. 601–07;Chari, T. R. andAllen, J. H. “Iceberg grounding problems in the North Atlantic”, p. 608–16;Croasdale, K. R. “The movement of Arctic landfast ice; its measurement and influence on offshore drilling”, p. 617–36;Dehn, W. S. andHughes, F. D. “Sea ice versus Arctic operations in the Alaskan area”, p. 637–58; English, J. andDempster, R. T. “Underwater laboratory in sub-Arctic waters”, p. 659–70; P. Jumppanen, “Ice thermal loads against walls of water reservoirs”, p. 679–702.]Google Scholar

Hofmann, W. Die Internationale Glaziologische Grönland-Expedition (EGIG). 1. Das Forschungsprojekt und seine Ausführung. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2. 1973, p. 239–52 [Describes conception, foundation and research programmes of the Expédition Glaciologique Internationale au Groenland from its beginnings to the second expedition in 1967–68.]Google Scholar

Ives, J. D. Barry, R. G. ed. Arctic and alpine environments. London, Methucn, [^e1974]. xviii, 999 p., 49 plates. [Articles relevant to glaciology are listed separately.]Google Scholar

Langway, C. C. Ice core storage facility. Antarctic Journal of the United States, Vol. 9, No. 6.1974. p. 322–24. [Describes briefly storage of cores by the U.S. Army Cold Regions Research and Engineering Laboratory at their facilities in New Hampshire.]Google Scholar

Mukai, T. Mukai, S. Temperature and motion of the grains in interplanetary space. Publications of the Astronomical Society of Japan, Vol. 25, No. 4,1973, p. 481–88. [Equilibrium temperatures of interplanetary iee grains deduced. Radiation pressure is less than gravitational force for all sizes.]Google Scholar

Williams, R. S., Environmental studies of Iceland wilh ERTS-1 imagery, by Williams, R. S. [and 8 Others]. Proceedings of the ninth International Symposium on Remote Sensing of Environment … 1974. … Ann Arbor, Center for Remote Sensing Information and Analysis, Willow Run Laboratories, Environmental Research Institute of Michigan, Vol. 1, [1974]. p. 31–81. [Use of ERTS imagery is particularly valuable in studying geophysical phenomena of Iceland, including aspects of glaciology.]Google Scholar

Blincow, D. W. Dominey, S. C. A portable profiling snow gauge. Proceedings of the Western Snow Conference, 42nd annual meeting.1974, p. 53–57. [Describes gauge, and discusses results from field studies.]Google Scholar

Chudoblak, W. J., Radar remote sensors for iee thickness and soil moisture measurements, by Chudobiak, W. J. [and 6 Others]. (In Thompson, G. E. ed. The applications of remote sensing and benefits to Canada. Proceedings [of the] second Canadian symposium on remote sensing, University af Guelph, Guelph, Ontario, Canada. April 29–May 1,1974. Vol. 2. Ottawa, Canadian Remote Sensing Society,1974, p. 417–24.) [Fresh and saline ice. Five systems having very high-range resolution capabilities described.]Google Scholar

Goodman, D. J., Wire strainmeters on ice, [by] Goodman, D. J. Allan, A. J.,Bilham, R. G. Nature, Vol. 255, No. 5503,1975, p. 45–46. [Deseription of instrument for recording strain continuously and its use on sea ice and a glacier.]CrossRefGoogle Scholar

KovÁcs, G. MolnÁr, G. Determination of snow water equivalent and snowmelt water by thickness of snow cover data. Hydrological Sciences Bulletin, Vol. 19, No. 4,1974, p. 435–47. [New method derived.]Google Scholar

Meteor, R. E. Leader burst communication. Proceedings of the Western Snow Conference, 42nd annual meeting,1974, p. 29–36. [Discusses application of technique to remote data collection, such as hydrological and meteorological data.]Google Scholar

Schreck, R. I., A simple, airborne, ice particle collector, [by] Schreck, R. I.,Touienhoofd, V.,Knight, C. A. Journal of Applied Meteorology, Vol. 13, No. 8,1974, p. 949–50. [Device for collecting particles in cold silicone oil and bringing them back to the laboratory.]2.0.CO;2>CrossRefGoogle Scholar

Veillette, J. Helicopter portable drill for high Arctic programs. Project 730019. Canada. Geological Survey, Paper 75–1, Pt. A,1975, p. 427–29. [Describes drill for permafrost coring.]Google Scholar

Veillette, J. Modified CRREL ice coring augers. Project 730019. Canada. Geological Survey, Paper 75–1, Pt. A,1975, p. 425–26. [Describes modification for use in permafrost, which provides additional storage room for cuttings and permits longer core run.]Google Scholar

Watanabe, Z. Kongöeki ni yoru sekisetsu hakuhen no tsukurikata [A method of making thin sections of deposited snow by mixed solution]. Seppyö, Vol. 36, No. 3,1974, p. 91–95. [Solutions of caprylic and capric acids and methyl cinnamate and of caprylic acid and ethyl cinnamate used at temperatures, respectively, of −8 to −10° C and −10 to −12° C. English summary, p. 94–95]Google Scholar

Addison, J. R. Electrical properties of saline ice at 1 kHz down to −150° C. Journal of Applied Physics, Vol. 46, No. 2,1975, p. 513–22. [Laboratory measurements on artificial sea ice and comparison with earlier work on pure and doped ice.]CrossRefGoogle Scholar

Anderson, B. J. Nucleation and epitaxial growth of ice crystals from the vapor. Dissertation Abstracts International, B, Vol. 35, No. 9,1975, p. 4580-B. [Experiments on growth of ice on covellite and AgI single crystals. Differences attributed to inherited strain which can also affect habit of snow crystals. Abstract of Ph.D. thesis, University of Nevada, Reno,1974. University Microfilms order no. 75-5307].Google Scholar

Browell, E. V. UV optical constants of water and ammonia ices. Dissertation Abstracts International, B, Vol. 35, No. 8,1975, p. 4105–B. [Determination from 1610 Å to 3200 Å for amorphous and Ih ice; 1925 Å to 3200 Å for amorphous ammonia ice. Abstract of Ph.D. thesis, University of Florida,1974. University Microfilms order no. 75-3478.]CrossRefGoogle Scholar

Carras, J. N. Macklin, W. C. Air bubbles in accreted ice. Quarterly Journal of the Royal Meteorological Society, Vol. 101, No. 427,1975, p. 127–46. [Theory of formation of air bubbles in accreted ice and comparison with experiments.]CrossRefGoogle Scholar

Carras, J. N. Macklin, W. C. The opacity of accreted ice. Quarterly Journal of the Royal Meteorological Society, Vol. 101, No. 428,1975, p. 203–06. [Method of measurement described. Also suitable lor studying air bubble structures of hailstones.]CrossRefGoogle Scholar

Davis, C. I. The ice-nucleating characteristics of various silver-iodide aerosols. Dissertation Abstracts International, B, Vol. 35, No. 7,1975, p.4374-B–75-B. [Experiments in cloud seeding in Wyoming and their relation to cloud chamber tests. Abstract of Ph.D. thesis, University of Wyoming,1974. University Microfilms order no. 74-23689.]Google Scholar

Doolittle, J. B. Vali, G. Heterogeneous freezing nucleation in electric fields. Journal of the Atmospheric Sciences, Vol. 32, No. 2,1975, p. 375–79. [Experiments using AgI and organic nuclei show no effect oi electric field up to 6 kV cm⁻¹.]2.0.CO;2>CrossRefGoogle Scholar

Evrard, G., Influence de la température sur le comportement diélectrique des émulsions de glace dans le domaine des ondes kilométriques, note Evrard,, de G.,Lagourette, B. et Montfort., J.-P. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences, Sér. B, Tom. 279, No. 19,1974, p. 491–93. [Measurements of dielectric dispersion of ice emulsions from 0 to −60° C.]Google Scholar

Falciglia, F., Positronium formation in ice, [by] Falciglia, F.,Iaci, G.,LoSavio, M.,Turrisi, E. Applied Physics, Vol. 5, No. 2,1974, p. 179–80. [Broadening of narrow component in γ-annihilation distribution curve for positrons in ice attributed to Bloch slates.]CrossRefGoogle Scholar

Gibson, R. A. Wright, P. G. Dielectric Pippard plots for ferroelectric transitions in certain solid solutions, including impure ice. Journal of the Physics and Chemistry of Solids, Vol. 36, No. 4,1975. p. 321–24. [Application of the theory to data for the 100 K transition in F-doped ice used to predict field dependence ot transition temperature.]CrossRefGoogle Scholar

Hale, B. N. Molecular, P. L. M Plumber model for ice clusters in a supersaturated vapor. Journal of Chemical Physics, Vol. 61, No. 10,1974, p. 4012–19. [Theory of ice Ih embryos shows this structure less stable than clathrate-like clusters.]CrossRefGoogle Scholar

Hale, B. N. On, P. L. M Plumber nucleation phenomena 1: a molecular model. Journal of the Atmospheric Sciences, Vol. 31, No. 6,1974, p. 1615–21. [Molecular model of cluster nucleation in supersaturated vapour.]2.0.CO;2>CrossRefGoogle Scholar

Jones, D. R. H Determination of the kinetics of ice-brine interfaces from the shapes of migrating droplets. Journal of Crystal Growth, Vol. 26, No. 1,1974, p. 177–79. [Elongation of layer droplets migrating under a temperature gradient used to deduce kinetic solidification at the ice-droplet interface.]CrossRefGoogle Scholar

Kelland, S. B. Twenty-vertex model on a triangular lattice. Australian Journal of Physics, Vol. 27, No. 6,1974, p. 813–29. [Solution of a theoretical model connected with the ice polarization problem.]CrossRefGoogle Scholar

King, W. D. Freezing rate of water droplets. Journal of the Atmospheric Sciences, Vol. 32, No. 2,1975, p. 403–08. [Theory developed and compared with experiments.]2.0.CO;2>CrossRefGoogle Scholar

Kiselev, V. F., Poverkhnostnyye yavleniya na granitse led-gaz i led-tverdoye telo [Surface phenomena at the ice-gas and ice-solid interfaces]. [by] Kiselev, V. F.,Kvlividze, V. I.,Kurzayev, A. B. (In Tsytovich, N. A., ed. Vtoraya Mezhdunarodnaya Konferentsiya po Merzotovedeniyu. Doklady i soobshchemya. [Edited by]Tsytovich, N. A.,A, B. Savel’yev,Votyakov, I. N. Vyp. 4. Yakutsk, Yakutskoye Knizhnoye Izdalel’stvo,1973, p. 199–202.) [Review of liquid-like layer on ice surface.]Google Scholar

Kobayashi, T. VLS [vapour–liquid–solid] growth on ice surfaces treated with AgI-NH₄I. Journal of Crystal Growth, Vol. 26, No, 1,1974, p. 6–12. [Formation of terraces on basal plane and later growth rate of steps observed and discussed.]CrossRefGoogle Scholar

Lamy, P. L. Interaction of interplanetary dust grains with the solar radiation field. Astronomy and Astrophysics, Vol. 35, No. 2,1974, p. 197–207. [Investigation of this interaction for, among others, ice spheres.]Google Scholar

Mehrer, H. Theory of tracer diffusion in the Wurtzite structure with applications to hexagonal ice. Zeitschrift für Physik B, Vol. 20, No. 3,1975, p. 281–88. [Theory of diffusion by vacancy mechanism.]CrossRefGoogle Scholar

Meschi, D. J. Searcy, A. W. Kinetics of dissociative vaporization reactions. High Temperature Science, Vol. 6, No. 3,1974, p. 221–36. [Theory of evaporation from solids developed and compared with data on ice and NaCl.]Google Scholar

Miloshev, G. N. Todorova, S. V. Adsorption effect on the appearance of the primary water product in the atmosphere. Doklady Bolgarskoy Akademii Nauk, Tom. 26, No. 11.1973, p. 1481–84. [Adsorption increases temperature at which ice crystals form by sublimation.]Google Scholar

Nevskiy, A. S. Malysheva, A. I. vliyanii sposoba barbotazha vanny na teploobmen pri plavlenii l’da [Effect of the manner of bath bubbling on the heat transfer in ice melting]. Inzhenerno-Fizicheskiy Zhurnal, Tom 28, No. 1,1975, p. 141–43. [Experiments on ice cylinders in water and NaCl solutions.]Google Scholar

Olinger, B. Halleck, P. M. Compression and bonding of ice VII and an empirical linear expression for the isothermal compression of solids. Journal of Chemical Physics, Vol. 62, No. 1,1975, p. 94–99. [Measurement of density from 3–8 GPa and 298 K.]CrossRefGoogle Scholar

Onuki, A., First-order phase transition with a moving boundary. II. Theory of ice formation, [by] Onuki, A.,Shibuya, Y.,Kozaki, S. Journal of Law Temperature Physics, Vol. 15, Nos. 1–2,1974, p. 161–68. [Exact solution of differential equation for moving boundary found and applied to ice freezing from water.]CrossRefGoogle Scholar

Passarelli, R. E., Ice nucleation in a supercooled cloud by CuI–3AgI and AgI aerosols, [by] Passarelli, R. E.,Chessin, H.,Vonnegut, B. Journal of Applied Meteorology, Vol. 13, No. 8,1974, p. 946–48. [Experiments on numbers of active nuclei produced.]2.0.CO;2>CrossRefGoogle Scholar

Rosinski, J. Nagamoto, C. T. Silver halides and iodine monobromide systems as freezing nuclei. Journal of Applied Meteorology, Vol. 13, No. 7,1974, p. 778–82. [Experimental study of enhancement of ice nucleability by exchange of I ions on surface of AgI.]2.0.CO;2>CrossRefGoogle Scholar

Ryan, B. F., The densities and growth rates of ice crystals between −5 C and −9 C, [by] Ryan, B. F.,Wishart, E. R.,Holroyd, E. W. III. Journal of the Atmospheric Sciences, Vol. 31, No. 8,1974, p. 2136–41. [Measurements and comparison with theory.]2.0.CO;2>CrossRefGoogle Scholar

Rye, P. J. Macklin, W. C. Crystal size in accreted ice. Quarterly Journal of the Royal Meteorological Society, Vol. 101, No. 428,1975, p. 207–15. [Measurement of preferred orientation and dimensions of ice crystals resulting from freezing supercooled droplets on ice substrates.]CrossRefGoogle Scholar

Shipman, L. L. Scheraga, H. A. Computation of the intermolecular vibrational modes of a tetrahedral water pentamer at the core of an ice-like water cluster. Journal of Physical Chemistry, Vol. 79, No. 4,1975, p. 380–83. [Calculations reported and compared with infra-red and neutron scattering spectra of ice Ih.]CrossRefGoogle Scholar

SmedskjÆr, L. Trumpy, G. Temperature dependence of the narrow component for positronium in ice. Applied Physics, Vol. 5, No. 1,1974, p. 49–52. [Interpretation of results in terms of delocalized and localized positronium ice, the latter possibly trapped by L-defects.]CrossRefGoogle Scholar

Stephen, T. Freezing potentials and electrical conductivities of LiF, LiCl, and amine group ices. Dissertation Abstracts International, B, Vol. 35, No. 5,1974, p. 2379-B. [Measurement and interpretation. Abstract of Ph.D. thesis, Saint Louis University,1974. University Microfilms order no. 74-24146.]Google Scholar

Stillinger, F. H. Lemberg, H. L. Symmetry breaking in water molecule interactions. Journal of Chemical Physics, Vol. 62, No. 4,1975, p. 1340–46. [Discusses how dipole-dipole forces between water molecules at large separation cause a change in symmetry as they approach.]CrossRefGoogle Scholar

Sullivan, D. E. Deutch, J. M. Molecular theory of dielectric relaxation. Journal of Chemical Physics, Vol. 62, No. 6,1975, p. 2130–38. [New theory of frequency-dependent dielectric permittivity in terms of a dipole “memory function“.]CrossRefGoogle Scholar

Tatibouet, J., Influence de la déformation plastique sur les propriétés ultrasonores de la glace I_h , [par]Tatibouet, J.,Vassoille, R.,Perez, J.,Gobin, P. F. Journal de Physique, Tom. 36, No. 1,1975, p. 69–73. [Measurement of attenuation and velocity of ultrasonic waves in ice single crystals after plastic deformation and during annealing.]CrossRefGoogle Scholar

Vasconcellos, K. F. Beech, J. Development of blow-holes in the ice–water–carbon dioxide system. Journal of Crystal Growth, Vol. 28, No. 1,1975, p. 85–92. [Formation of blow-holes considered in relation to solute profile. Effect of freezing rate.]CrossRefGoogle Scholar

Venkatesh, C. G., Amorphous solid water: an X-ray diffraction study, [by] Venkatesh, C. G.,Rice, S. A.,Narten, A. H. Science, Vol. 186, No. 4167,1974, p. 927–28. [O atom pair correlation function determined for amorphous ice deposited at 10 K.]CrossRefGoogle Scholar

Whitworth, R. W. Charged dislocations in ionic crystals. Advances in Physics, Vol. 24, No. 2,1975, p. 203–304. [Revies. Includes section on charged dislocations in ice, p. 291–93.]CrossRefGoogle Scholar

Ambach, W. Jochum, O. Zur Dispersion im offenen Gerinne: Einfluss von Randzonen bei Gletscherbächen. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2,1973, p. 181–88. [Discusses perturbation by boundary layers at margin of glacial streams when measuring discharge with tracers.]Google Scholar

Arkel Van, N. A. Die gegenwärtige Vergletscherung des Ararat. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2,1973, p. 89–103. [Results of survey of ice cover of Mt Ararat made in summer1966. Presents map, description and selection of photographs for future comparisons.]Google Scholar

Barkov, N. I., Izotopnyy khimicheskiy sostav materikovogo l’da v rayone stantsii Mirnyy [Isotopic chemical composition of continental ice in the Mirny station region]. [by] Barkov, N. I.,Polyakoy, V. A. Yu.Seletskiy, V.,Yakubovskiy, A. V.,Isayev, N. V. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 89,1974, p. 19–23.Google Scholar

Dean, W. W. Maclure Glacier. California. A contribution to the International Hydrological Decade. Proceedings of the Western Snow Conference. 42nd annual meeting,1974, p. 1–8. [Presents six years’ data from mass balance studies of this small (0.17 km²) glacier in the Sierra Nevada, altitude 3 600–3 800 m.]Google Scholar

Dewart, G., Analysis of the Byrd station strain net, Antarctica, by Dewart, G.,Whillans, I. M.,Brecher, H. H. Ohio State University. Institute of Polar Studies. Report No. 48,1974, iv l, 49 p. [Presents results of field investigations relating to study of glacier flow.]Google Scholar

Elachi, C. Brown, W. E. Imaging and sounding of ice fields with airborne coherent radars. Journal of Geophysical Research, Vol. 80, No. 8,1975, p. 1113–19. [Presents recent results from radar imagery of glaciers in south-eastern Alaska, imagery of coastal and sea ice in northern Alaska and Beaufort Sea, and sounding of layered continental ice in Greenland.]CrossRefGoogle Scholar

Finsterwalder, RÜdiger, Rentsch, H. Das Verhalten der bayerischen Gletscher in den letzten zwei Jahrzehnten. Erläuterungen zu den Gletscherstandskarten für die Jahre 1949(50)–1959–1970(71). Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9. Ht. 1–2,1973, p. 59–72, 5 maps [in end-pocket]. [The five small glaciers of the German part of the Alps were surveyed in these three years and documented in maps, scale 1: 5 000. Behaviour of glaciers during this period is discussed.]Google Scholar

Gloersen, P., Microwave maps of the polar ice of the Earth, [by] Gloersen, P.,Wilheit, T. T.,Chang, T. C.,Nordberg, W.,Campbell, W. J. Bulletin of the American Meteorological Society, Vol. 55, No. 12,1974, p. 1442–48. [By using scanning microwave radiometer at wavelength 1.55 cm on Nimbus-5 satellite, three different views of each pole were obtained at monthly intervals from December 1972 to January1973, Results analysed and discussed.]2.0.CO;2>CrossRefGoogle Scholar

Govorukha, L. S., Radiolokatsionnoye zondirovaniye lednikovogo pokrova o. King-Dzhordzh (Vaterloo) [Radio-echo sounding of the King George Island (Waterloo) ice sheet]. [by] Govorukha, L. S.,Chudakov, V. I.,Shalygin, A. M. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 89,1974, p. 15–18.Google Scholar

Hambrey, M. J. Oxygen isotope studies at Charles Rabots Bre, Okstindan, northern Norway. Geografiska Annaler, Vol. 56A, Nos. 3–4,1974, p. 147–58. [Evaluates usefulness of oxygen isotope analysis in elucidating problems concerning flow and structure of this glacier.]CrossRefGoogle Scholar

Harrison, A. E. Mt. Baker, Washington. Coleman Glacier survey. Description and coordinates of programmetric control stations. [Seattle], Washington, University of Washington. College of Engineering. Dept. of Electrical Engineering,1974. 49 p. (Technical Report No. 181.) [Results summarized in table and maps; descriptions and data for each station are given individually.]Google Scholar

Hattersley-Smith, G. Present Arctic ice cover. (In Ives, J. D.,Barry, R. G. ed. Arctic and alpine environments. London, Methuen, [^e1974], p. 195–223.) [Surveys current state of knowledge of Arctic glaciers and their behaviour.]Google Scholar

Hughes, T. J. Is the west Antarctic ice sheet disintegrating? ISCAP Bulletin (University of Maine at Orono), No. 3,1974, iv, 93 p. [Study of unstable Ross Sea glacial episodes; mechanisms that may control rate and extent of disintegration.]Google Scholar

Iken, A. Srhwankungen der Oberflächengeschwindigkeit des White Ciacier, Axel Heiberg Island im Zusammenhang mit Schwankungen der Wasserführung von Gletscherbächen und des Wasserdruckes in Gletschermühlen. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2,1973, p. 207–19. [Results of field work relating variations of surface velocity of glacier to variations of discharge of subglacial streams and of water pressure in moulins.]Google Scholar

Krenke, A. N. Zony l’doobrazovaniya na lednikakh [Zones of ice formation on a glacier]. Geofizicheskiy Byulleten’, No. 25.1973, p. 44–56. [Classification of glaciers and formation of firn.]Google Scholar

Krimmel, R. M. Tangborn, W. V. South Cascade Glacier: the moderating effect of glaciers on runoff. Proceedings of the Western Snow Conference, 42nd annual meeting,1974, p. 9–13. [Applies results obtained from this glacier, 1965–73, to illustrate mechanisms by which glaciers moderate stream flow.]Google Scholar

Lichti-Federovich, S. Pollen analysis of ice core samples from the Devon Island Ice Cap. Project 690064. Canada. Geological Survey. Paper 75–1, Pt. A,1975. p. 441–44. [Spectra from all levels were dominated by pollen from distant sources.]Google Scholar

LiestØl, O. Glaciological work in 1973 . Norsk Polarinstitutt. Årbok 1973 [pub. 1975], p. 181–92. [Mainly mass-balance studies on four glaciers in Norway and two in Spitsbergen.]Google Scholar

Loijens, H. S. Streamflow formation in the Mistaya River basin, Rocky Mountains, Canada. Proceedings of the Western Snow Conference, 42nd annual meeting,1974, p. 86–95. [Discusses influence of glacier melt.]Google Scholar

Mokievsky-Zubok, O. Analysis of mass balance values and their accuracy fir Sentinel Glacier, British Columbia, Canada. Ottawa, Environment Canada. Inland Waters Directorate. Water Resources Branch,1974. v, 4 p. (Scientific Series, No.31.) [Method 1 based on determination of difference between measured winter and summer balances compared with method 2 based on difference between volume of remaining snow cover and ice and firn ablation. Latter more accurate.]Google Scholar

Mokievsky-Zubok, O. Determination of the mass balance on Sentinel Glacier, British Columbia, Canada. Ottawa, Environment Canada. Inland Waters Directorate. Water Resources Branch,1973. v, 39 p. (Scientific Series, No. 30.) [Two surface methods compared for entire glacier; terrestrial photogrammetry for tongue.Between 1966 and1971, four years with positive and two years with negative mass balantes. Total loss exceeded gain by 28 cm of water for entire surface.]Google Scholar

Mokievsky-Zubok, O. Study of Sentinel Glacier, British Columbia, Canada within the International Hydrological Decade program. Procedures and techniques. Ottawa. Environment Canada. Inland Waters Directorate. Water Resources Branch,1973. vii, 31 p. (Technical Bulletin No. 77.) [General description of field work on this glacier, situated in maritime climate and subject to high winter precipitation.]Google Scholar

Ostrem, G. Present alpine ice cover, (In Ives, J. D.,Barry, R. G. ed. Arctic and alpine environments. London. Methuen, [^e1974], p. 225–50.) [Conceptual discussion of alpine glaciers together with consideration of past and present conditions and interrelated aspects such as regional glaciation levels and snow-lines.]Google Scholar

Patzelt, G. Die neuzeitlichen Gletscherschwankungen in der Venedigergruppe (Hohe Tauern. Oslalpen). Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2,1973, p. 5–57. [Discusses glacier fluctuations from A.D. 1500 to present day.]Google Scholar

Peterson, J. A., Recession of snow and ice fields of Irian Java. Republic of Indonesia, by Peterson, J. A.,Hope, G. S.,Mitton, R. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2,1973. p. 74–87. [Discusses retreat of tropical ice masses during last 50 years, and compares behaviour of and factors affecting glaciers of New Guinea to those of the Andes and Africa.]Google Scholar

Ross Ice Shelf Project. Ross Ice Shelf Project (RISP) science plan. First edition (final draft). Prepared by Ross Ice Shelf Project steering group. Lincoln, Nebraska, University of Nebraska—Lincoln. Ross Ice Shelf Project,1974. viii, 91 p. [Describes project, objectives of which are to investigate conditions in ice shelf, in water beneath ice, and in sediments and bedrock on sea bottom, and to interpret from data past history and present conditions in this part of Antarctica.]Google Scholar

Rutford, R. H. Coordination of ice core drilling. Antarctic Journal of the United Slates, Vol. 9, No. 6, 1974 p. 325–26. [Describes activities of the Polar Ice Core Office (PICO), established in March 1974 at the University of Nebraska, Lincoln.]Google Scholar

Savatyugin, L. M. O. “samooblamyvanii” shel’fovykh lednikov Antarktidy [On “self-calving” of Antarctic shelf ice]. Informatsionnyy Byulleten’ Sovetskoy Antarktkheskoy Ekspeditsii, No. 89,1974, p. 24–26. [Based on theory of N. Reeh.]Google Scholar

Schulz, E. F. Harvesting glacier ice. Proceedings of the Western Snow Conference, 42nd annual meeting,1974, p. 73–85. [Discusses icebergs as a source of fresh water.]Google Scholar

Sokolov, D. P. Otsenka velichiny stoka talykh vod s lednikovykh obnazheniy lednika Fedchenko [Estimate of size of flow of melt water from the ice slopes of Lednik Fedchenko]. Vestnik Leningradskogo Universiteta. Seriya Geologiya i Geografiya,1974, Vyp. 3, p. 103–07. [Melting occurs particularly from lower part of glacier tongue. English summary, p. 107.]Google Scholar

StØyva, J. Breboka. Handbok i brevandring. Oslo, Grøndahl & Sons,1974. 99 p. [Handbook for climbing on glaciers.]Google Scholar

Williams, L. D. Computer simulation of glacier mass balance throughout an ablation season. Proceedings of the Western Snow Conference, 42nd ammal meeting.1974, p. 23–28. [Programme described predicts arcal distribution of snow water equivalent for each day of ablation season.]Google Scholar

Yeskin, L. I. O svyazi teplovogo rezhima vod i srokov stanovleniya pripaya v rayone Yuzhnykh Orkneyskikh ostrovov [On the relation between water temperature and times of fast ice formation in the South Orkney Islands region]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 89,1974, p. 59–61.Google Scholar

Zotikov, I. A., Stok materikovogo l’da Antarktidy i formirovaniye donnykh antarkticheskikh vod [Continental ice discharge of Antarctica and the formation of Antarctic bottom water]. [by] Zotikov, I. A.,Ivanov, Yu. A,Barbash, V. R. Okeanologiya, Tom. 14, Vyp. 4,1974. p. 607–13. [English summary, p. 613.]Google Scholar

Bajzak, D. Thermal mapping of water envelopes surrounding icebergs. (In Thompson, G. E. ed. The application of remote sensing and benefits to Canada. Proceedings [of the] second Canadian symposium on remote sensing, University of Guelph, Guelph, Ontario, Canada, April 29–May 1, 1974. Vol. 2. Ottawa, Canadian Remote Sensing Society,1974, p. 574–79.) [Information gathered on melt water and movement of icebergs, using large-scale thermal imagery.]Google Scholar

Barash, M. S. Granitsa plavuchikh l’dov v severnoy Atlantike v verkhnem pleystotsene [The limit of floating ice in the North Atlantic in ihe Upper Pleistocene]. Okeanologiya, Tom 14, Vyp. 5.1974, p. 846–51. [Evidence from foraminifera in sediments indicates extent of ice sheet. English summary, p. 851.]Google Scholar

Bondarev, E. A., K postroyeniyu modeli vskrytiya bol’shikh rek [On the construction of a model of break-up on big rivers]. [by] Bondarev, E. A.,Kolmogorov, A. V.,Fayko, L. I. Meteorologiya i Gidrologiya,1974, No. 5, p. 99–101.Google Scholar

Bushuyev, A. V., Atlas ledovykh obrazovaniy [Atlas of ice formations]. [by] Bushuyev, A. V.,Volkov, N. A.,Loshchilov, V. S. Leningrad. Gidrometroizdat,1974. 139 p. [Glossary in Russian and English and annotated photographs of sea-ice forms, preceded by short account of processes of formation, deformation and melting.]Google Scholar

Buynitskiy, V. K. H. Organicheskaya zhizn’ v morskom l’du [Organic life in sea ice]. Vestnik Leningradskogo Universiteta. Seriya Geologiya i Geografiya, 1974. Vyp. 3, p. 76–81. [Algae studied in fast ice in Mirny harbour and Alasheyev Bay. English summary, p. 80.]Google Scholar

Cherepanov, N. V. Kozlovskiy, A. M. Vliyaniye strukturnoy neodnorodnosti morskogo antarkticheskogo l’da na yego prochnost’ [Influence of the structural heterogeneity of Antarctic sea ice on its strength]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Kkspeditsii, No. 89,1974, p, 67–71. [Study of fast ice.]Google Scholar

Cox, G. F. N. Brine drainage in sodium chloride ice. Dissertation Abstracts international, B, Vol. 35, No. 4,1974, p. 1749-B–50-B. [Laboratory study of brine drainage using radioactive sodium and comparison with theory. Abstract of Ph.D. thesis, Dartmouth College,1974, University Microfilms order no. 74-23090.]Google Scholar

Cutfield, S. K. Hydrological aspects of Lake Vanda, Wright Valley, Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 17, No. 3,1974, p. 645–57. [Discusses results obtained from simultaneous measurements of lake-ice thickness and density, and ice surface ablation made weekly for almost 12 months. Water inflow from Onyx River and lake level were also recorded at regular intervals.]CrossRefGoogle Scholar

Dunbar, Moira, Lowry, R. T. Remote sensing of sea ice in Nares Strait and the Arctic Ocean, March 1973. (In Thompson, G. E.,ed. The application of remote sensing and benefits to Canada. Proceedings [of the] second Canadian symposium on remote sensing, University of Guelph, Guelph, Ontario, Canada, April 29–May 1, 1974. Vol. 2. Ottawa, Canadian Remote Sensing Society,1974, p. 407–15.) [Presents preliminary interpretaron of this multisensor exercise.]Google Scholar

Fitch, J. L. Jones, L. G. Artificial ice islands could cut Arctic costs. Oil and Gas Journal, 11 November1974, p 173–81. [Discusses construction, maintenance and use for protecting off-shore drilling and production equipment from ice and waves. Island could be built on fast ice and ice added until it becomes grounded on sea bed.]Google Scholar

Gordon, A. L. Taylor, H. W. Seasonal change of Antarctic sea ice cover. Science, Vol. 187, No. 4174,1975, p. 346–47. [Winter expansion of sea ice and subsequent retreat in summer may be linked with wind stress acting on Southern Ocean in conjunction with heat exchange in open water regions within ice fields.]CrossRefGoogle ScholarPubMed

HÄllfors, G. Niemi, Å A Chrysochromulina (Haptophyceae) bloom under the ice in the Tvärminne archipelago, southern coast of Finland. Memoranda Societalis pro Fauna el Flora Fennica, 50,1974, p. 89–104. [Observed March 1974 on under-surface of sea ice. Main component, Chrysochromulina Birgeri, described as new species.]Google Scholar

Hirayama, K.-I An investigation of ice forces on vertical structures. Dissertation Abstracts International, B, Vol. 35,No. 4,1974, p. 1678–B. [Model studies. Abstract of Ph.D. thesis, University of Iowa, 1974. University Microfilms order no. 74-21902.]Google Scholar

Hutter, K. Floating sea ice plates and the significance of the dependence of the Poisson ratio on brine content. Proceedings of the Royal Society of London, Ser. A, Vol. 343, No. 1632,1975, p. 85–108. [Influence of temperature profile in ice plates calculated. Results show dependence of Poisson’s ratio on microstructure to be negligible.]Google Scholar

Kivisild, H. R., Salvage of heavy construction equipment by a floating ice bridge, [by] Kivisild, H. R.,Rose, G. D.,Masterson, D. M. Canadian Geotechnical Journal, Vol. 12, No. 1.1975, p. 58–69. [Discusses design criteria and procedures required to build ice bridge across which equipment could be moved in winter from grounded barge in James Bay to land.]CrossRefGoogle Scholar

Langleben, M. P. Pounder, E. R. On the air drag of an Arctic ice floe. Geophysical Research Letters, Vol. 2, No. 1,1975, p. 15–18. [Estimation of appropriate drag coefficient for any given type of ice surface possible; forecasting still presents difficulties.]CrossRefGoogle Scholar

LAViolette, P. E. Diachok, O. I. The use of APT satellite imagery in a subarctic airborne oceanographic survey. Arctic, Vol. 27, No. 4,1974, p. 306–09. [Ice and cloud conditions over the Greenland Sea.]CrossRefGoogle Scholar

Legen’kay, A. P., Rezul’taty izmereniy temperatury ledyanogo ostrova dreyfuyushchey stantsii SP-19 [Results of temperature measurements on ice island drifting station SP-19]. [By] Legen’kov, A. P.,Chugin, I. V.,Yermin, N. N. Okeanologiya, Tom 14, Vyp. 4,1974, p. 619–22. [Measurements made from May 1971 to April 1972.]Google Scholar

Mackay, D. K. LØken, O. H. Arctic hydrology. (In Ives, J. D.,Barry, R. G. ed. Arctic and alpine environments. London, Methuen, [³1974], p. 111–32.) [Includes river and lake ice conditions and effect of permafrost on groundwater.]Google Scholar

Masterson, D. M. Floating ice sheets. Northern Engineer, Vol. 6, No. 3,1974, p. 11’18. [Presents simple method for estimating stresses and deflections beneath long-term loads on floating ice sheets.]Google Scholar

Meeks, D. C., A study of microwave emission properties of sea ice—AIDJEX 1972, by Meeks, D. C.,Ramseier, R. O.,Campbell, W. J. Proceedings of the ninth International Symposium on Remote Sensing of Environment … 1974. … Ann Arbor, Center for Remote Sensing Information and Analysis, Willow Run Laboratories, Environmental Research Institute of Michigan, Vol. 1, [1974]. p. 307–22. [Comparative study of surface-based 13.4 GHz passive microwave measurements shows distinct decreasing microwave emissions for first-year, transitional and multi-year sea ice types,]Google Scholar

Murzin, A. I. Opredeleniye informatsionnoy svyazi mezhdu polyami davleniya atmosfery i dreyfom l’da v arkticheskikh moryakh (na primere morva Laptevykh) [Determination of information relationship between atmospheric pressure fields and ice drift in Arctic seas (for example the Laptev Sea)]. Meteoralogiya i Gidrologiya,1974, No. 5, p. 74–79. [Possibility of using entropic ratio in estimating optimum scales of atmospheric processes affecting formation of drifting ice discussed. English abstract, p. 79.]Google Scholar

Nalimov, YU. V Timerev, A. A. Velichiny al’bedo snezhno-ledyanogo pokrova v nizov’yakh 1 ust’yakh arkticheskikh rek [Albedo values of snow and ice cover in lower course and mouth regions of Arctic rivers]. Meteoralogiya i Gidrologiya,1974, No. 5, p. 64–68.Google Scholar

Neshyba, S. BadaN-Dangon, A. On ocean current induced by a prograding ice pack. Geophysical Research Letters, Vol. 1, No. 8,1974, p. 351–54. [Presents model illustrating theory, and applies to Bering Sea shelf during freeze-up.]CrossRefGoogle Scholar

Olenicoff, S. M. Soviet laboratory for sea ice research. Arctic Bulletin, Vol. 1, No. 5, [1975], p. 208–17. [Describes equipment and research in progress in the ice research laboratory of the Arkticheskiy i Antarktieheskiy Nauehno-Issledovatel’skiy Institut, Leningrad.]Google Scholar

Osterkamp, T. E. Frazil ice nucleation mechanisms. University of Alaska. Geophysical Institute. Report Series UAG R-230,1975, ii 1., 13 1. [Reviews mechanisms, generalizes mass exchange process proposed by Osterkamp and others (Journal of the Atmospheric Sciences, Vol. 31, No. 5,1974, p. 1464–65) and shows that only mass exchange and secondary nucleation can account for frazil-ice formation in streams and rivers.]Google Scholar

Parashar, S. K., Investigation of radar discrimination of sea ice, [by] Parashar, S. K.,Biggs, A. W.,Fung, A. K.,Moore, R. K. Proceedings of the ninth International Symposium on Remote Sensing of Environment … 1974. .. Ann Arbor, Center for Remote Sensing Information and Analysis, Willow Run Laboratories, Environmental Research Institute of Michigan, Vol. I, [1974], p. 323–32. [Combining a 400 MHz and a 13.3 GHz system gave satisfactory discrimination between sea-ice types and thicknesses when used during April off Point Barrow, Alaska.]Google Scholar

Piotrovich, V. V. Vliyaniye deyatel’nosti cheloveka na tolshchinu snezhnogo l’da na vodokhranilishchakh [The influence of man’s activities on the thickness of slush-agglomera ted ice on reservoirs). Meteorologiya i Gidrologiya, 1974, No. 7, p. 83–86.Google Scholar

Reimnitz, E., Influence of grounding ice on the Arctic shelf of Alaska, [by] Reimnitz, E.,Barnes, P.,Forgatsch, T.,Rodeick, C. Marine Geology, Vol. 13, No. 5,1972, p. 323–34. [Describes Alaska’s Beaufort Sea shelf; much of bottom roughness of this reflects action of grounded ice.]CrossRefGoogle Scholar

Romanov, A. A. Ob osnovnykh osobennostyakh raspredel eniya l’dov v moryakh, omyvayushchikh vostochnuyu Anta rktidy [The main features of ice distribution in seas off eastern Antarctica]. informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 89,1974, p. 62–66. [Calculations of speed and direction of ice drift.]Google Scholar

Rothrock, D. A. The steady drift of an incompressible Arctic ice cover. Journal of Geophysical Research, Vol. 80, No. 3,1975, p. 387–97. [Calculated by assuming ice is incompressible and inviscid. Realistic flow patterns conforming to geometry of basin were obtained.]CrossRefGoogle Scholar

Shearer, J. Blasco, S. Further observations of the scouring phenomena in the Beaufort Sea. Project 700092. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 483–93. [Describes observations on sea bottom scours and discusses characteristics of sea ice causing them.]Google Scholar

Streten, N. A. Large-scale sea ice features in the western Arctic basin and the Bering Sea as viewed by the NOAA-2 satellite. Arctic and Alpille Research, Vol. 6, No. 4,1974, p. 333–45’ [VHRR data in both visible and infra-red channels were used for mapping sea ice distribution. Principal problem was high frequency of cloudy days.]CrossRefGoogle Scholar

Tsang, G. Ice piling on lakeshores with special reference to the occurrences On Lake Simcoe in spring of 1973. Burlington, Ontario, Environment Canada. Inland Waters Directorate. Canada Centre for Inland waters,1974. vii, 12 p . (Scientific Series, No. 35.) [Discusses structure of ice pile, formation, meteorological conditions under which piling may occur, dynamic analysis of factors affecting piling, and proposed method of avoiding piling damage to shoreline structures .]Google Scholar

Uzuner, M. S. Hydraulics and mechanics of river ice jams. Dissertation Abstracts Intenational, B, Vol. 34, No. 4,1975, p. 1679–B. [Analytic model developed. Includes experiments on compress ive strength. Abstract of Ph.D. thesis, University of Iowa, 1974. University Microfilms order no. 74–2 1947.]Google Scholar

Vinje, T . E Sea ice and drift speed observations in 1973. Norsk Polarinstitutt. Årbok 1973 [pub. 1975], p. 197–202. [Monthly maps showing region between Greenland and Novaya Zemlya, based mainly on American satellite pictures .]Google Scholar

Volkov, N. A. Bushuyev, A. V. ed. Nomenklatura morskikh l’dov. Uslovnyye oboznacheniya dlya ledovykh kart [Nomenclature of sea ice. Conventional signs for ice maps]. Leningrad, Gidrometeoizdat, 1974. [86] p. [Includes Russian- English and English- Russian terms.] Google Scholar

Aartolahti, T. Ring ridge hummocky moraines in northern Finland. Fennia, 134,1974, 22 p. [Form, composition, structure, age and location studied. Appear to be dead-ice formations, being laid down as ice sheet melted.]Google Scholar

Agrell, H. Glaciation and deglaciation in the Sommen-Åsunden region, southeastern Sweden. Bulletin of the Geological Institutions of the University of Uppsala, New Series, Vol. 4, Nos. 1–8,1972, p. 125–87. [Deals with Quaternary ice movements and till distribution, features left by Baltic ice, morphology, stratigraphy and distribution of glacio-fluvial deposits, and periglacial deposits.]Google Scholar

Andrews, J. T. Cainozoic glaciations and crustal movements of the Arctic. (In Ives, J. D.,Barry, R. G. ed. Arctic and alpine environments. London, Methuen, [^e1974], p. 277–317.) [Deals with number and timing of events since Tertiary, presenting a detailed treatment of events for the Wisconsin stage. Discusses response of Arctic regions to giacio-isostatic and euslatic movements.]Google Scholar

Andrews, J. T.,Multiple tills, radiometric ages, and assessment of the Wisconsin glaciation in eastern Baffin Island, N.W.T., Canada: a progress report, [by] Andrews, J. T.,Szabo, B. J.,Isherwood, W. Arctic and Alpine Research, Vol, 7, No. 1,1975, p. 39–59.CrossRefGoogle Scholar

BergstrÖm, E. Den prerecenta lokalglaciationens utbredningshistoria inom Skanderna. Stockholms Universitet. Naturgeografiska Institutionen. Forskningsrapport 16,1973, vii, 214 p, [History of local glaciation in Norwegian and north Swedish mountains before post-glacial climatic optimum in 8100 B.P. English summary, p. 193–204.]Google Scholar

Blake, W. Glacial geological investigations in northwestern Greenland. Project 670031. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 435–39. [Study of glacial and marine deposits on Saunders Ø and Carey Ø er, with some conclusions on glacial history of these islands.]Google Scholar

Boulton, G. S. Dent, D. L. The nature and rates of post-depositional changes in recently deposited till from south-east Iceland. Geografiska Annaler, Vol. 56A, Nos. 3–4,1974, p. 121–34. [Observations at retreating frontal margin of Breioamerkurjökull,]CrossRefGoogle Scholar

Boulton, G. S., Subglacial shearing and crushing, and the role of water pressures in tills from southeast Iceland, by Boulton, G. S.,Dent, D. L.,Morris, E. M. Geografiska Annaler, Vol, 56A, Nos. 3–4,1974, p. 135–45. [Observations at retreating frontal margin of Breioamerkurjökull.]CrossRefGoogle Scholar

Calder, N. Arithmetic of ice ages. Nature, Vol. 252, No. 5480,1974, p. 216–18. [Suggests ice age began 5000 years ago and will end t 19000 years from now.]CrossRefGoogle Scholar

Carrara, P. E. The ice-cored moraines of Akudnirmuit Glacier, Cumberland Peninsula, Baffin Island N.W. T ., Canada. Arctic and Alpine Research, Vol. 7, No. 1,1975, p. 61–67. [Describes and dates these four moraines and discusses their significance.]CrossRefGoogle Scholar

Chappell, J. Relationships between sealevels, ¹⁸O variations and orbital perturbations, during the past 250,000 years.’ Nature, Vol. 252, No. 5480, 1974., p. 199–202. [Sea-level changes are synchronous with processional changes in solar radiation when orbital eccentricity is large. Oxygen-isotope variations in deep-sea cores correspond in timing but not in amplitude, reflecting changing isotopic composition of Pleistocene ice sheets.] CrossRefGoogle Scholar

Croot, D. G. The morphology and evolution of an esker in Spitsbergen. Norsk Polarinstitutt. Årbok 1973 [pub. 1975], p. 237–39. [Conditions at Battyebreen, Dicksondalen, in 1973 compared with air photographs from 1966 and 1969.]Google Scholar

Dvuvillier, A. Les glaciations géologiques, le paléornagndtisme et le probleme des neutrinos solaires. Bulletin de la Société Royale des Sciences de Liége, An. 43, Nos. 1–2,1974, p. 35–39. [Suggestion that thermal neutrinos cause palaeomagnetic inversions and glaciations.],Google Scholar

Delepau, P. -C Essai sur la formation et I’évolution du lac d’Annecy. Jalonnement du glacier Beaufort-Roseland vers Annecy. Revve de Géographie Alpine, Tom. 63, Ease. 3,1974, p. 38–93- [Some observations on the glacial geology and Quaternary glaciation of this area of France.]Google Scholar

Derbyshire, E. The bathymetry of Jökulsárlón, south-east Iceland. Geographical Journal, Vol. 140,pt. 2,1974, p. 269–74. [Presents results of bathymetric survey of largest proglacial lake of Breioamerkurjökull in form of chart of ice-free part of lake in July 1970.] CrossRefGoogle Scholar

Dionne, J.-C The eastward transport of erratics in James Bay area, Quebec. Revue de Géographie de Montréal.Vol, 28, No. 4,1974, p- 453–57. [Criticizes Lee’s theory that erratics were transported by glaciers with an eastward flow.]Google Scholar

Dredoe, I. Surficial geology, Sept Iles-Cap Chat. Project 710083. Canada. Geological Survey. Paper 75–1, pt. A,1975, p. 401. [Observations in this area north of St. Lawrence River give indication of direction of flow of early ice mass.]Google Scholar

Drozdowski, E. Geneza Basenu Grudziądzkicgn w świetle osadów i form glacjalntych [Genesis of the, Grudziądz basin in the light of its deposits and glacial forms], Prace Geograficzne, Nr. 104 ,1974, 139 p. [Lower part of the Wisla (Vistula) valley, Poland. English p. summary 129–36.]Google Scholar

Dubois, J-M Phases et formes de déglaciation du bassin du Bury, Estrie, Québec. Revue de Géographie de Montréal,Vol. 28, No. 4,1974, p. 389–406. [Discusses nature of ground, till, and processes of downwasting.] Google Scholar

Dubois, J -M Le quaternaire de la côte nord de l’estuaire maritime du Saint-Laurent. Convention de recherche 1135-D13–4–1/74. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 403–05. [Study of landforms suggest direction of flow of Quaternary ice sheet in this area.]Google Scholar

Fillon, R. H. Geomorphology and glacial history of Hamilton Bank, Labrador Shelf. Project 730076. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 167–69. [Freshness and distribution of relict glacial landforms, markedly end moraines, suggest entire bank was glaciated during late Wisconsin.]Google Scholar

Fliri, F. Der zentralalpine Bänderton von Schabs (Südtirol). zeitschrift für Gletscherkunde und Glazialgeologie. Bd. 9, Ht. 1–2,1973, p. 231–35. [Discusses these Quaternary sediments in relation to chronology of glaciation in the Alps.]Google Scholar

Frakes, L. A.,Late Paleozoic glaciation: part VI, Asia, [by] Frakes, L. A.,Kemp, E. M.].Crowell, J. C. Geological Society of America. Bulletin, Vol. 86, No. 4,1975, p, 454–64. [Late Palaeozoic deposits known only in peninsular India; possible deposits rafted by shore ice in Siberia.]2.0.CO;2>CrossRefGoogle Scholar

Galon, R. ed. Scientific results of the Polish geographical expedition to Vatnajökull (Iceland), 1968. A collection of reports by the research groups. Geographia Polonica, Vol. 26,1973, 312 p. +maps [in separate folder]. [Expedition devoted mainly to glacial geology. Contents; R. Galon and J. Szupryczyński, “The polish geographical expedition to Vatnajökull (Iceland) June 5 to September 7,1968, p. 5–14;Galon, R. “Geomorphological and geological analysis of the proglacial area of Skeidarárjökull. Central section” . p. 15–56;Bogacki, M. “Geomorphological and geological analysis of the proglacial area of Skeidárarjökull. Central western and eastern sections”, p. 57–88;Klimek, K. “Geomorphological and geological analysis of the proglacial area of the Skeidarárjökull. Extreme eastern and extreme western sections, p. 89–113;Jewtuchowicz, S. “The present-day marginal zone of Skeidarárjökull”, p. 115–37; Galon, A synthetic description of deposits and landforms observed on the proglacial area of Skeidarárjökull. Conclusions w ith regard to the age of the deposits and the way in which deglaciation is proceeding”, p. 139–5°; j “Report on the photogrammetric surveys made by the Polish expedition in 1968 on the forefield of the Skeidarárjökull”, p. 151 55; G. Wójcik, “The results of the meteorological investigations on the forefield of Skeidarárjökull”. p. 157–83; G. Wójcik, “Glaciological studies on the Skeidarárjökull”, P- 209–54 Churski, “Hydrographic features of the proglacial area of Skeidarárjökull”, p. 209–54; S.Kozarski Szupryczynski, J. “Glacial forms and deposits in the Sidujökull deglaciation area”, p. 255–311.Google Scholar

Gangloff, P. Les structures cylindriques et I’évolution géomorphologiquc d’une plage tardiglaciaire á Saint- Jérôme, Quebec. Revve de Geographie de Montréal, Vol. 28, No. 4,1974, p. 357–73. [Describes structures and how they were formed, possibly 10 300 years B.P.]Google Scholar

Genes, A. N. Glacial geology of Stord Island, Norway. Dissertation Abstracts International. B, Vol. 35, No. 3,1974, p. 1295-B-96-B. [Studies made to determine chronology and extent of Pleistocene glaciation in Bergen district. Abstract of Ph.D. thesis, Syracuse University, 1973. University Microfilms order no. 74–17576.]Google Scholar

Grant, D. R. Surficial geology of northern Cape Breton Island. Project 700056. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 407–08. [Great variety of glacial materials and landforms present in this part of Nova Scotia.]Google Scholar

Grogger, P. K. Glaciation of the high Uintas primitive area, Utah, with emphasis on the northern slope. Dissertation Abstracts International, B, Vol. 35, No. 3,1974, P. 1296–B 97–B. [Four glacial advances identified during Pleistocene Abstract of Ph.D. thesis University of Utah 1974. University Microfilms order no. 74–20781.]Google Scholar

Gustavson, T. C. Sedimentation on, gravel outwash fans, Makspina Glacier foreland, Alaska, Journal of Sedi- maryl etrology. Vol. 44. No. 2,1974, p. 374–815. [Observations on two large melt-water streams in order to understand sedimentary processes active on braided outwash fans.Google Scholar

Hastenrath, S. On the Pleistocene glaciation of the Cordillera de Talamanca, Costa Rica. Zeitschrift für Gletscherkunde und Glazialgeologie Bd. 9, Ht. 1–2 1973, p., 105–21. [Suggests Pleistocene snow line at 3500 m. Describes moraines and periglacial phenomena, and discusses course of Pleistocene glaciation.] Google Scholar

Heuberger, H. Alpine Quaternary glaciation. (In Ives, J. D.,Barry, R. G.ed. Arctic and alpine environments. London Methuen [^e1974] , p.319–38.) [Reviews current knowledge, comparing Alps and Rocky Mountains and mentioning problems concerning interior Alps. Lists post-glacial glacier advances since 9000 B.P.]Google Scholar

Hillaire-marcel, C. La deglacia tion a u nord-oues t de Montreal: donnees radiochronologiques et faits stra tigraphiques. graphiques. Revue de Geographie de Montréal, Vol. 28, No . 4,1974, p. 407–17. [Discusses course of events in this area following Wisconsin glaciation.]Google Scholar

Holtedahl, O. Noen glas ifluviale isrand-avsetninger I den sydlige del av Glomma-vassdragnets (nåvrerende) dreneringsomrade. Med en d el berggeologisk-morfologiske data fra de nordlige Øyere n-trakter. Norges Geologiske Undersokelse, Nr. 306, 1974, 85 p. [Discusses glacio-Auvial marginal deposits in southern part of present drainage area of Glomma river system, southern Norway, and presents data on geology and morphology of northern Øyeren district. English abstract, p. 1.]Google Scholar

[ICELAND: GLACIAL GEOLOGY.]University of Sheffield earth sciences expedition to Iceland (Solheimajokull). 21st June-30th July, 1973. [Sheffield], University of Sheffield, Dept. of Geology, 1974. 74 leaves. [Mostly geology and glacial geology in south Iceland.]Google Scholar

Ives, J. D., Growth and decay of the Laurentide ice sheet and comparisons with Fenno-Scandinavia, [by] Ives, J. D.,Andrews, J. T.,Barry, R. G.. Naturwissenschoflen,] a hrg. 62, Ht. 3, 19 75, p. 118–2 5 [Outlines early work and reviews field data for La brador-Ungava and Baffin Island in a climatological context. Proposes alternative model and compares with Fenno-Scandinavia.]CrossRefGoogle Scholar

Kennett, J. P. Shackleton, N. J. Laurentide ice sheet meltwater recorded in Gulf of Mexico deep-sea cores. Science, Vol. 188, No. 4184,1975, p. 147–50 . [Evidence shows major influx of iso topically light glacial melt water occurred during late Wisconsin via Mississippi River li’om ice sheet 2000km north.]CrossRefGoogle ScholarPubMed

Kneussl, W. H ohlenbarenknochen aus der Tischoferhohle (Kaisertal bei Kufstein-Nordtirol) mit ¹⁴C-Methode altersbes timmt. Zeitschrift für Gletscherbnde und Glazialgeologie, Bd. 9, Ht. 1–2,1973, p. 237–38. [^I4C dating of cave bear’s bone shows age of 27 875 ± 485 years B.P., further evidence of ice-free valley during Wlirm interstadial.]Google Scholar

KrzemiŃskl, T. Geneza mlodoplejstoceńskiej rzeźby glacjalnej w dorzeczu środkowej Warty [The formation of glacial relief during the upper Pleistocene in the basin of the middle Warta]. Acta Geographica Lodziellsia, Nr. 33,1974, p. 1–167. [Describes effects of Quaternary deglaciation in this area of Poland. French p. summary 151–67.]Google Scholar

Lacercrantz, C.-L Om den glaciala erosion en i Kilpisjärvi sjöbäcken. Terra, Vol. 86. No. 4. 1974 p 175–80 [study of glacial erosion in basin of lake in north-western Finnish Lapland, based on soundings made in 1938–39 and on recent maps. English abstract, p. 175.]Google Scholar

Lortie, G. Direction d’écoulement des glaciers du pléistocéne des cantons de l’est, Québec. Project 740094. Canada Geological Survey Paper 75–1, Pt. A.1975, p. 415–16. [Presents preliminary findings from this st udy of Quaternary glacier flow in a limited area of Quebec.]Google Scholar

Mclaren, P. Under-ice diving observations in the coastal environments of southeast Melville and western Byam. Martin islands. Project 730020. Canada. Geological Survey. Paper 75–1, Pt. A.1975, p. 475–77. [Study of bottom environments, including effects of ice such as scouring and “scour moraines”.]Google Scholar

Mahaney, W. C. ed Quaternary environments: proceedings of a symposium. First York University Symposium on Quaternary Research 1974. Toronto, York University. Atkinson College, 1974. vii, 318 p. (Geographical Monographs, No. 5.) [Includes the following papers: Terasmae, J., “An evaluation of methods used for reconstruction of Quaternary environments”, p. 5–32;Miller, M. M.,Anderson, J. H. “Out-of-phase Holocene climatic trends in the maritime and continental sectors of the Alaska-Canada Boundary Range”, p. 33–58;Nielsen, E. “A mid-Wisconsinan glacio-marine deposit from Nova Scotia”, p. 59–60;Madole, R. F. “Quaternary research methodologies applied to delimiting natural hazards in mountainous Colorado”, p . 79–98; Coates, D. R.,Kirkland, J. T. “Application of glacial models for large-scale terrain derangements”, p. 99–136; Cadwell, D. H., “Jökulhlaup lakes on existing glaciers as an aid to interpretation in Pleistocene stratigraphy”, p. 137–52;Kiver, E. P. “Holocene glaciation in the Wallowa Mountains, Oregon”, p. 169–95;Mahaney, W. C. “Soil stratigraphy and genesis of neoglacial deposits in the Arapaho and Henderson cirques, central Colorado Front Range”, p. 197–240;Pettapiece, W. W.,Zoltai, S. C. “Soil environments in the western Canadian subarctic”, p. 279–92;Jones, V. K. “Late-neoglacial regimes of an inland cirque glacier and their paleoc1imatic implications”, p. 293–94;Williams, J. “Simulation of the atmospheric circulation with glacial period boundary conditions: moisture balance of the earth-atmosphere system”, p. 295–310.]Google Scholar

Masurel, Y. Aspects morphologiques de l’Ile d’Axel Heiberg (Arctique canadien septentrional). Revue de Géographie Alpille, Tom. 62, Fasc. 3,1974, p. 369–80. [Describes glaciological work, with emphasis on glacial geology, carried out by McGill University in this area, mentioning Baby, White and Thompon glaciers.]CrossRefGoogle Scholar

Piper, D. J. W Upper Cenozoic glacial history south of the Grand Banks of Newfoundland. Canadian Journal of Earth Sciences, Vol. 12, No. 3,1975, p. 503–08. [Study to determine history of ice rafting in this area.]CrossRefGoogle Scholar

Plumet, P. L’archéologie et le relévement glacio-isostatique de la région de Poste-de-Ia-Baleine, Nouveau Québec. Revue de Géographie de Montréal, Vol. 28, No. 4,1974, p. 443–47. [Compares archaeological with geomorphological data obtained from two estimates relating to rate of glacio-isostatic uplift in this area.]Google Scholar

Porter, S. C. Glaciation limit in New Zealand’s Southern Alps Arctic and Alpine Research, Vol. 7, No. 1,1975, p. 33–37 [Regional survey made of glaciation limit to obtain information on altitudinal distribution of glaciers. Data provide insight into relative significance of topographic and climatic controls on present glacier distribution.]CrossRefGoogle Scholar

Reimnitz, E., Strudel scour: a unique Arctic marine geologic phenomenon, [by] Reimmtz, E.,Rodeick, C. A.,Wolf, S. C. Journal of Sedimentary Petrology, Vol. 44, No. 2. 1974. p. 409–20 [Various methods used to study scour features in sea bottom caused by fresh-water flooding of Beaufort Sea ice by northern Alaskan rivers in spring melt followed by draining or overflow through holes and cracks in ice producing depressions in underlying sediments.]Google Scholar

Rondot, J L’épisode glaciaire de Saint-Narcisse dans Charlevoix, Québec1. Revue de Géographie de Montréal, Vol. 28, No. 4,1974, p. 375–88. [Study of moraines and extensive glacial deposits, probably formed over 12000 years B.P.]Google Scholar

Rukhina, YE. V O spornykh voprosakh pokrovno-lednikovoy i driftovoy teorii [On the vexed question of ice cover and ice drift theory]. Vestnik Leningradskogo Universiteta. Seriya Geologiya i Geografiya, 1974, Vyp. 3, p. 56–61. [Geological evidence favours arguments supporting theory of continental glaciation. English p. summary 61.]Google Scholar

Ryder, J. M. Quaternary geology-terrain inventory, Lytton map-area, British Columbia (92 I/SW). Project 740066. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 419–20. [General observations of glacial geology.]Google Scholar

SchlÜchter, C. Die Gliederung der letzteiszeitlichen Ablagerungen in Aartal südlich von Bern (Schweiz). Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2,1973, p. 123–41. [Presents reconstruction of Würm glaciation from investigations of deposits in the Aar river valley.]Google Scholar

Schubert, C. Valastro, S. Late Pleistocene glaciation of Páramo de La Culata, north-central Venezuelan Andes. Geologische Rundschau, Bd. 63, Ht. 2,1974, p. 516–38. [Describes glacial features and discusses age of formation.]CrossRefGoogle Scholar

Shilts, W. Mcdonald, B. C. Dispersal of clasts and trace elements in the Windsor esker, southern Quebec. Project 690095. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 495–99. [Detailed description.]Google Scholar

Sindre, E. Ice movement in the Vossestrand-Vikafjell area, western Norway. Norges Geologiske Undersokelse, Nr. 311, Bulletin 25,1974, p. 25–34. [Stone counting of till and analysis of glacial striae used to determine Quaternary ice movement directions.]Google Scholar

Sollid, J. L. SØRBEL, L. Younger Dryas ice-marginal deposits in Trøndelag, central Norway. Norsk Geografisk Tidsskrift, Bd. 29, Ht. I,1975, p. 1–9. [Deposits mapped on basis of morphological studies and analysis of air photographs.]CrossRefGoogle Scholar

Stalker, A. M. The large interdrift bedrock blocks of the Canadian prairies . Project 740089. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 421–22. [Preliminary results of study of blocks lying between till and other drift in attempt to explain their origin.]Google Scholar

Stuiver, M.,Erroneous date for Chilean glacial advance, [by] Stuiver,, M.,Mercer, J. H.,Moreno, H. R. Science, Vol. 188, No. 4183,1975, p. 73–74. [Comments on date suggested by Mercer and Laugenie, ibid., Vol. 182, No. 4116,1973, p. 1017–19.]CrossRefGoogle ScholarPubMed

Valadas, B. Veyret, Y. Quelques aspects des modelés d’origine glaciaire, périglaciaire et nivale sur les confins méridonaux de la Margeride. Revue de Géomorphologie Dynamique, 23^e An., No. 4,1974, p. 163–77. [One ancient a nd one more recent glaciation identified in this region of France, but absolute chronology not yet possible.]Google Scholar

Waltt, R. B. Late Pleistocene alpine glaciers and the Cordilleran ice sheet at Washington Pass, North Cascade Range, Washington. Arctic and Alpine Research, Vol. 7, No. 1,1975, p. 25–32. [Presents observations on glacial erosion and striated erratics in this area and discusses post-glaciation ice sheets.]Google Scholar

Walcott, R. I. Craig, B. G. Uplift studies, southeastern Hudson Bay. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 455–56. [Rate of emergence of land during last few thousand years deduced from study of marine shells.]Google Scholar

Webb, P. N. Derivation of the older moraines in Beacon Valley, Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 17, No. 3,1974, p. 723–28. [Comments upon paper by Link letter, Bockheim and Ugolini, ibid., Vol. 16, No. I,1973, p. 90–108. Reply by these authors, p. 727–28.]CrossRefGoogle Scholar

Worsley, P. Some observations on lake ice-push features, Grasvatn, northern Scandinavia. Norsk Geografisk Tidsskrift, Bd. 29, Ht. I,1975, p. 11–19. [Artificial lowering of lake revealed features considered to have been formed by wind-powered ice-floes.]CrossRefGoogle Scholar

Afanasenko, V. YE, Gidrogeologicheskiye usloviya Selennyakhskoy nalozhennoy vpadiny i sopredel’nykh s ney gornykhs ney gornykh sooruzheniy [Hydrological conditions of Selennyakh superimposed depression and adjacent mountain structures] . [By] Afanasenko, V. Ye.,Romanovskiy, N. N.,Koreysha, M. M. Merzlotnyye Issledovanrya, Vyp. 14,1974, p. 91–104. [Permafrost conditions and underground water system in Yakutskaya A.S.S.R.]Google Scholar

Aguirre-PUENTE, J., Frost heaving and the classification of soils in accordance with their frost susceptibility, by Aguirre-Puente, J.,Dupas, A.,Philippe, A. Frost i jord, Nr. 14,1974, p. 41–47. [Translated from the original French in Bulletin de Liaison des Laboratoires des Ponts et Chaussées, No. 68, 1973.]Google Scholar

Alekseyev, V. P. Naledi Sibiri i dal’nego vostoka [Naleds of Siberia and the far east]. Sibirskiy Geograficheskiy Sbornik, [No .] 8,1974, p. 5–68. [General survey of naleds in Siberia, including the eastern region. English abstract, p. 278.]Google Scholar

Apostolopoulos, C., Theoretical investigation of some possible frost-resistant pavement constructions in relation to their thermal properties, by Apostolopoulos, C.,Kuhle, H.,Schneider, W. Frost i jord, Nr. 12,1973, p. 37–43. [Constructions considered, in descending order of frost resistance, were those with non-load bearing and load bearing insulations, conventional full-depth asphalt constructions. Text also in German, p. 29–35.]Google Scholar

Arkhangelov, A. A. Shaposhnikova, YE. A Priblizhennaya otsenka paleomerzlolnykh usloviy formire- vaniya nizhnepleystotsenovykh otlozheniy vostochnoy chasti Primorskoy nizmenncsti [Approximate estimalion of palaeo-permafrost conditions of formation of lower Pleistocene deposits in the eastern Primorskiy lowland]. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 76–80. [Yakutskaya A.S.S.R.]Google Scholar

Barsch, D. Refraktionsseismische Bestimmung der Obergrenze des gefrorenen Schuttkörpers in verschiedenen Blockgletschern Graubündens, Schweizer Alpen. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2,1973, p. 143–67. [Describes seismometric method for determining upper boundary of frozen debris core in rock glaciers and presents some results and conclusions in relation to conditions in the Swiss Alps.]Google Scholar

Bikd, J. B. Geomorphic processes in the Arctic. (In Ives, J. D.,Barry, R. G. ed. Arctic and alpine environments. London, Methuen, [^e1974], p. 703–20.) [Reviews processes affecting polar landscapes, referring to periglacial features.]Google Scholar

Boydell, A. N., Terrain inventory and land classification, Boothia Peninsula and northern Keewatin. Project 740074, [by] Boydell, A. N.,Drabinsky, K. A.,Nelterville, J. A. Canada. Geological Survey. Paper 75–1 pt- A,1975, p. 393–95. [Includes study of characteristics of permafrost terrain and distribution of ground ice with respect to sediment types.]Google Scholar

Boykov, C. A. Prodol’noye elektroprofilirovaniye po dnishcham vodotokov v tselyakh kartirovaniya talykh i merzlykh porod [Mapping of taliks and permanently frozen rocks in the bottoms of river valleys by means of electrical profiling]. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 163–66.Google Scholar

Brown, R. J. E Kupsch, W. ed. Permafrost terminology. Canada. National Research Council. Associate Committee on Geotechnical Research. Technical Memorandum No. 111,1974, 62 p. (NRCC 14374.) [Defines common terms.]Google Scholar

Cailleux, A. Une naled’ d’embouchure á Poste-de-la-Baleine. nouveau Québec. Revue de Géographie de Montréal, Vol. 28, No. 4,1974, p. 458–60. [Describes naled, which may be one of the first to be described in North America.]Google Scholar

Chizhova, N. 1. Geokhimiya prirodnykh vod Yano-Omoloyskogo mezhdurech’ya [Geochemistry of natural waters of the Yana-Omoloy interfluve], Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 109–15. [Permafrost area of Yakutskaya A.S.S.R.]Google Scholar

Crampton, G. B. Linear-patterned slopes in the discontinuous permafrost zone of the central Mackenzie River valley. Arctic, Vol. 27, No. 4,1974, p. 265–72. [Discusses effect of aspect of slope on occurrence and depth of permafrost.]CrossRefGoogle Scholar

Dionne, J .-C Cryosols avec triage sur rivage et fond de lacs, Québec central subarctique. Revue de Géographie de Montréal, Vol. 28, No. 4,1974, p. 333–42. [Describes and discusses formation of patterned ground in the Lake Le Grand area.]Google Scholar

Feroyvik, F. Frostsikre gulv på grunnen. Frost i jord, Nr. 14,1974, p. 49–57. [Discusses development of simple frost-protected foundations for practical use, based on computer calculations for normally heated family houses in four Norwegian towns. English p. summary 57.]Google Scholar

French, H. M. Pingo investigations and terrain disturbance studies. Banks Island, District of Franklin. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 459–64. [Several pingos were sectioned and examined. Gullying as result of off-road vehicle movement was studied.]Google Scholar

Frivik, P.-E Termisk analyse av frost i jord. Del i. Elementer og prinsipper. Frost i jord, Nr. 9,1973, p. 21–26. [Discusses decisive factors and principles involved in thermal analysis of frost in soils with reference to frost protected constructions. English p. summary 25–26.]Google Scholar

Fyrhake, L. Samband mellan tjälning och rörelser hos grundmurar i småhus; inverkan av markisolering med mineralull. Statens Institut för Byggnadsforskning. Rapport. R20:1973, [1973,] [iv], 26 p. [Discusses correlation between frost heave and movements in the foundation walls of houses and effect of ground insulalion using mineral wool. English summary, p, iii–iv,]Google Scholar

Gandahl, R. Styrencellplast i väg. Frost i jord, Nr. 10,1973, p. 5–12, [Presents results of field tests of polystyrene foam as road insulating material. English summary, p 11–12.]Google Scholar

Garagulya, L. S., Osnovnyye zadachi merzlotnykh issledovaniy dlya proyektirovaniya i stroitel’stva gazoprovodov v rayonakh kraynego severa [Main problems of permafrost investigations for gas pipe projection and construction in regions of the far north]. [by] Garagulya, L. S.,F, N. Poltev [and]Spiridonov, V. V. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 3–11. [General outline of problems.]Google Scholar

Gatto, L. W. Anderson, D. M. Alaskan thermokarst terrain and possible Martian analog. Science, Vol. 188, No. 4185,1975, p. 255–57, [Terrain recognized on ERTS-i imagery was formed by degrading permafrost in manner similar to one of processes postulated for development of Martian fretted terrain.]CrossRefGoogle ScholarPubMed

Gell, A. Tension-crack ice, icing-mound ice, Tuktoyakluk coast. District of Mackenzie (107°C). Canada. Geological Survey. Paper 75–1, Pt. A,1975, p, 465–66. [Discusses tension-crack ice which forms in cracks produced by mechanical rupture of overburden when pingos grow, and icing-mound ice formed by injection of water from depth into base of active layer.]Google Scholar

Gill, D. Influence of white spruce trees on permafrost-table microtopography, Mackenzie River delta. Canadian .Journal of Earth Sciences, Vol. 12, No. 2,1975, p. 263—72. [Permafrost table is depressed in conical shape surrounding stem of each tree.]CrossRefGoogle Scholar

Govorukha, L. S. Ob intensivnosti soliflyuktsii na o. King-Dzhordzh (Vaterloo) [Intensity of solifluction on King George Island (Waterloo)]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 89,1974, p, 10–14.Google Scholar

Gundersen, P. Frostisolering av rørgrofter. Frost i jord, Nr. 13,1974, p. 37–47. [Discusses insulation of trenches for service pipes. English summary, p 47.]Google Scholar

Haeberli, W. Die Basis-Temperatur der winterlichen Schneedecke als möglicher Indikator für die Verbreitung von Permafrost in den Alpen. Zeitsckrihrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2, 1973- P- 221–27. [Suggests that bottom temperature of winter snow cover could be used as indicator of distribution of permafrost in the Alps.]Google Scholar

Hansen, P. B. Frostbeskyttelse av eksisterende veger med toppisoleringsmetoden. Frost i jord. Nr. 9,1973, p. 7–19. [Describes frost protection of existing roads using boards of insulating material of high compressive strength placed directly on road with thin layer of asphaltic gravel on top of the boards. In p. English 15 19.] Google Scholar

Heidmann, L. J. An investigation into the causes and prevention of frost heaving of forest tree seedlings. Dissertation Abstracts International. B, Vol. 35, No. 3,1974, P. 1143-B. [Frost heaving was reduced by ploughing with and without addition of chemicals; survival was better on ploughed plus chemical plots. Abstract of ph.D). thesis, University of Arizona, 1974. University Microfilms order no. 74–20256.]Google Scholar

Hershfield, D. M. The frequency of freeze-thaw cycles. Journal of Applied Meteorology, Vol. 13, No. 3,1974, p. 348–54. [Data from 1300 climatic summaries used to construct map for United States showing annual frequency of freeze-thaw cycles.]2.0.CO;2>CrossRefGoogle Scholar

Isaacs, R. M. Geotechnical studies of permafrost in the Fort Good Hope-Norman Wells region N.W.F. Canada. Task Force on Northern Oil Development. Environmental-Social Committee, Northern Pipelines. Report No. 74–16, 1974 iv, 212 p. [Presence of considerable ice in all terrain types discussed with reference to thermal behaviour in relation to pipeline and associated constructions.]Google Scholar

Ivashenko, I. N. Vrachev, V. V. Vliyaniye moroznogo issusheniya na deformiruyemost’ merzlykh gruntov pri trekhosnom szhatii [Influence of frost drying in deformation of frozen soils under triaxial pressure], Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 204–08.Google Scholar

Ives, J. D. Permafrost. (In Ives, J. D.,Barry, R. G. ed. Arctic and alpine environments. London, Methuen, [^e1974], p. 157–94.) [Survey of current knowledge.]Google Scholar

Janson, L.-E. Undersokning av frysrisken för vattenledningar ovanför tjälgransen. Frost i jord, Nr. 14,1974, p, 59–67. [Tests on water mains show foundation depths can be reduced if high quality frost insulation is used. English summary, p 67.]Google Scholar

Johansen, Ø. Beregningsmelode for varmeledningsevnen av fuktige og frosne jordater. Del 2. frost i jord Nr. 10,1973, p. 13—28) +[4] p. [Describes method for calculation of thermal conductivity of damp and frozen soils. English summary, p 25–28.]Google Scholar

Kinosita, S.[i,e. Kinoshita],. Water migration in the soil during frost heaving. Frost ford. Nr. 11,1973, p. 37–40. [Presents equation for calculation of water migration, based on experiments in Hokkaido.]Google Scholar

Knutson, Å. Praktisk bruk av bark i vegbygging. Frost i jord, Nr. 10,1973, p, 29–44. [Results of held and laboratory work in Norway on use of bark as frost accumulating road base. Water in bark must freeze belore Host can penetrate into sub-soil. English summary, p 39–44.]Google Scholar

Kondkat’yeva, K. A. K voprosu o sledakh promerzaniya i ottaivamya v nizhnechetvertichnykh otloznemyakh basseyna r. Khromy [On freezing and thawing traces in lower Quaternary deposits of the Khroma river basin]. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 67–75. [Yakutskaya A.S.S.R.]Google Scholar

Kondrat’yeva, K. A. Novyye dannyye ob obnazhenii Mus-Khaya na r. Yane [New data on the Mus-Khaya outcrop on the Yana river]. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 56–66. [Veins of ice in lake-alluvial deposits along river banks in Yakutskaya A.S.S.R.]Google Scholar

Korsunskiy, M. B., Determination of temperature and depth of frost penetration in pavements and subgrades, by Korsunskiy, M. B.,Gayvoronskiy, V. N.,Rossovskiy, P. D. Frost i jord, Nr. 13,1974, p. 49–52. [Presents results of tests on road with asphalt surface.]Google Scholar

Korsunskiy, M. B., Moisture content and frost heaving of highway subgradc soils, by Korsunskiy, M. B.,Gayvoronskiy, V. N.,Rossovskiy, P. D. Frost i jord, Nr. 12,1973, p. 13–16. [Results of investigations on test road.]Google Scholar

Kudryavtsev, V. A., Vliyaniye fizicheskikh i strukturnoadsorbtsionnykh kharakteristik gruntov na protsess sublimatsii I’da v nikh [Influence of physical and structural-adsorptional characteristics of soils on the ice sublimation process in them]. [by] Kudryavtsev, V. A.,Yershov, Ye. D,Gurov, V. V.,Kuchukov, Ye. Z,Akimov, Yu. P Merzlotnyye Issledovaniya, Vyp. 14,1974, P- 24–21Google Scholar

Kudryavtsev, V. A., Zakonomernosti formirovaniya sezonno- i mnugolctnemerzlykh gornykh porod V rayone Srednego Priangar’ya [Regularities of seasonal and perennial permafrost development in the middle Angara river region], |By]Kudryavtsev, V. A.,Maksimova, L. N.,Boyarskiy, O. G.,Dubrovin, V. A.,Zabolotskaya, M. I. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 22–34 [Irkulskaya Oblast.']Google Scholar

Luk’yanov, V. S. Application of hydraulic analogue method to investigation of physical processes in soils. Frost i jord. Nr. 11,1973, p. 11–14. [Method used for analysing thermal and filtration processes in soils in connection with construction work in permafrost environments.]Google Scholar

Mmcdonald, G. N. Snow and ice and the transAlaska pipeline. Proceedings of the Western Snow Conference, 42nd annual meeting,1974, p. 103–05. [Very general outline of problems of constructing pipeline over peimafrost, icings and naleds, and effects on ecology.]Google Scholar

Mackay, J. R. Freezing processes at the bottom of permafrost, Tuktoyaktuk Peninsula area, District of Mackenzie (107C). Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 471–74. [Thermal and physical conditions that have produced ground ice now found in continuous permafrost were studied by examining thin [less than 50 m) permafrost now growing for the first time.]Google Scholar

Mackay, J. R. Relict ice wedges, pelly Island N.W.T. (107 C/12). Canada. Geological Survey. Paper 75–1, Pt. A, p. 469–70. [Description, with suggestion of age.]Google Scholar

Mackay, J. R. Mathews, W. H. Movement of sorted stripes, the Cinder Gone, Garibaldi Park, B.C., Canada. Arctic and Alpine Research, Vol. 6, No. 4,1974, p. 347–59- [Examines frost heave, displacement by needle ice, surface wash and drag from snow creep. Growth and ablation of needle ice down-slope movement.]CrossRefGoogle Scholar

McRobekts, E. C. Field observations of thawing in soils. Canadian Geotechnical Journal, Vol. 12, No. 1 1975. P.126–30. [Considers case histories indicating thaw interface proceeds as predicted by simple model. Investigate deviations and compares calculated and measured rates of thaw.]CrossRefGoogle Scholar

McRoberts, E. C. Some aspects of a simple secondary creep model for deformations in permafrost slopes Canadian Geotechnical Journal. Vol. 12, No. 1,1975, p. 98–105. [Introduces flow law for ice into model and that significant creep deformations can occur in frozen slopes. Suggests secondary creep in ice-rich sous may be faster than in ice alone.]CrossRefGoogle Scholar

McRoberts, E. C. Morgenstern, N. R. pore water expulsion during freezing. Canadian Geotechnical Journal, Vol. 12, No. 1,1975, p, 130–41. [Reviews this phenomenon and confirmation by laboratory tests. Discusses implications.]CrossRefGoogle Scholar

McRoberts, E. C. Nixon, J. F. Reticulate ice veins in permafrost, northern Canada: discussion. Geotechnical Journal, Vol. 12, No. 1,1975, p, 159–62. [Comments upon article by J. R. No. 2,1974, p. 230–37. Reply by Mackay, p. 163–65.CrossRefGoogle Scholar

Makeyev, O. V. ed. Pochvennyy kriogenez. K 10 mezhdunarodnomu kongressu pochvovedov. Moskva 1974 [Soil cryogenesis. For the 10th international congress of soil science. Moscow. 1974]. Mockaoy, lzdatel’stvo “Nauka”, 1074 244 p. [Collected papers on genesis, geography and regimes of cryogenic soils and problems of increasing their fertility.]Google Scholar

Melamet’, V. G. Medvedev, A. V. Ob optimal’nykh usloviyakh segregatsionnogo l’doobrazovaniya v tonkodispersnykh gornykh gorodakh [On the optimum conditions of scgregational ice-forming in finely dispersed rocks], Merzlotnyye Issledovamya, Vyp. 14,1974, p. 12–21.Google Scholar

Melent’vev, V. S. Vertikal’naya yaruchnost' verkhncy gidrodinamich eskoy zony i oblasti rasprostraneniya ostrovnoy i preryvistoy mnogole tney merzloty (na primere Aldano-Chul’manskogo rayona) [Vertical subdivisions of the upper hydrodynamic zone and regions of insular and fragmental permafrost (e.g. in the Aldan-Ghul’man region)]. Merziotnyye lssledovaniya, Vyp. 14,1974, p. 159–62. [Yakutskaya A.S.S.R.]Google Scholar

Melent’vev, V. S. Naumov, M. S. Landshaftnoye deshifrirova niye noveyshikh razryvnykh narusheniy v tseiyakh merzlotno-gidrogeologicheskikh nablyudeniy (na primere uglenosnykh rayonov yuzhnoy Yakutii) [Landscape interpretation of new dislocations with a break in continuity in permafrost hydrogeological studies (e.g. in the south Yakutiya coal-bearing region)]. Merzlotnyye Issledovalliya, Vyp. 14,1974, p. 137–40.Google Scholar

Mel’nikov, P. I. Tolstikhin, N. I. ed. Obshcheye merzlotovedeniye [General permafrost study]. Novosibirsk, Izdatel’stvo “Na uka”, 1974. 291 p. [Surveys research during last thirty years.]Google Scholar

Önalp, A. A study of the mechanism of frost heave and stabilization by the use of deflocculating agents. Frost i jord, Nr. 11,1973, p. 15–30. [Concludes that sodium tripolyphosphate may be regarded as suitable stabilizing agent for frost susceptible soils.Google Scholar

Ospennikov, YE. N Trush, N. I. L’ distost’ alasnykh i ozero-allyuvial’nykh otlozheniy Yano-Omoloyskogo mezhdurech’ya i metodika yeye polevogo opredeleniya [Ice content of alas and lake-alluvial deposits of the Yana-Omoloy interfluve and field methods for determining it]. Merziotnyye Issledovaniya, Vyp. 14,1974, p. 35–42. [Yakutskaya A.S.S.R.]Google Scholar

Pavlov, A. V. Olovin, B. A. Iskusstvennoye ottaivaniye merzlykh porod teplom solnechnoy radiatsii pri razrabotke rossypey [Artificial thawing of frozen ground by warm solar radiation during milling of placer deposits]. Novosibirsk, Izdatel’stvo “Nauka”, 1974. 182 p. [Presents methods of thawing frozen ground and protection of rocks from freezing, based on studies in Yakutskaya A.S.S.R.]Google Scholar

PÈwÈ, T. L. Second International Conference on Permafrost—northeast Siberia. Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 9, Ht. 1–2,1973, p . 253–60. [Detailed account of field trips made after the conference, which was held 15–28 July 1973.]Google Scholar

Piotrovskiv, M . V Problema reshetchatykh struktur i svyazi s nimi merzlotno-gidrogeologicheskikh usloviy [The problem of latticed structures and their connection with perma frost-hydrogeologi cal conditions]. Merz lotnyye lssledo vaniya, Vyp. 14,1974, p. 126–36.Google Scholar

Pissart, A. Banks Island N.W.T.: pingos, wind action, periglacial structures. Proj ect 640004. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 479–81.. [Brief description of recent findings in this area.]Google Scholar

Popov, A. I. ed. Problemy kriolitologii. Vyp. 4 [Problems of cryolithology. Vyp. 4]. Moscow, Izdatel’stvo Moskovskogo Universiteta, 1974. 253 p. [Articles on theoretical, methodological and regional problems of cryolithology, with examples from the U.S.S.R.]Google Scholar

Price, L. W., Origin a nd significance of wet spots on scraped surfaces in the high Arctic. Arctic, Vol. 27, No. 4,1974, p. 304–06. [Describes development and discusses cause of wet spots occurring on polygonal ground cleared for camp sites and air strips.]CrossRefGoogle Scholar

Pyshchev, N. F., Kraschetu glubiny promerzaniya pochY [Calculation of soil freezing depth]. [by] Pyshchev, N. F.,Mel’nikov, B. N.,Vostretsov, O. K. Meteorologiya Gidrologiya,1974, No. 6, p. 85–89.Google Scholar

Refsdal, G. The use of thermal insulating materials in highway engineering. Results from Norwegian tes troads. Frost i jord, Nr. 9,1973, p. 27–39. [Discusses use of insulating boards made of polystyrene or polyurethane.]Google Scholar

Retzer, J. L. Alpine soils. (In Ives, J. D.,Barry, R. G. ed. Arctic and alpine environments. London, Methuen, [^c1974], p. 771–802.) [Brief mention of occurrence of permafrost.)Google Scholar

Rieger, S. Arctic soils. (In Ives, J. D.,Barry, R. G. ed. Arctic and alpine environments. London, Methuen, [^e1974], p. 749–69.) [Deals with types of soils, their uses and classification, mentioning features caused by low temperatures.]Google Scholar

Romanovskiy, N. N., Naled’ “ozero Gusinoye” [The naled of Ozera Gusinoye]. [by] Romanovskiy, N. N., Afanasenko, Ye. V,Koreysha, M. M. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 1O5–08. [Measures naled and records changes since 1939. Yakulskaya A.S.S.R .]Google Scholar

Schmidt, W. Opportunities for the use of rigid polyurethane foams in roadbuilding to effect savings in frost blanket gravel. Frost i jord, Nr. 12,1973, p. 9–12. [Compares advantages and disadvantages of methods of applying foams.]Google Scholar

Schmidt, W. Result’s of insulating a highway test section with rigid polyurethane foams. Frost i jord Nr. 12, 1973 p. 5–7 [Discusses briefly water absorption, insulating behaviour and load-bearing capacity.]Google Scholar

Scotter, G. W. Permafrost profiles in the continental divide region of Alberta and British Columbia Arctic Alpine Research, Vol. 7, No. 1,1975, P. 93“95. [Only the second report of permafrost from this region. Observed Summer 1970.]CrossRefGoogle Scholar

SÉguin, M. K. État des recherches sur le pergèlisol dans la partie centrale de la fosse du Labrador, Quèbec subarctique. Revue de Gèographie de Montreal, Vol. 28, No. 4,1974, p. 343–56. [Discusses applied research on discontinuous permafrost, with particular reference to work at Schefferville.]Google Scholar

Shakhunyants, G. M. Soviet experience in handling harmful frost-heaving effects on railways. Frost i jord, Nr. 11,1973, p. 5–9. [Discusses use of plastic foams.]Google Scholar

Shusherina, YE. P. Soprotivleniye merzlykh dispersnykh porod i I’da razryvu v oblasti nizkikh temperatur (do - 60°C) [Resistance of froz en dispersed rocks and ice to a fracture in regions of low temperature (to –60°C)] Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 179–89.Google Scholar

Shusherina, YE. P, Novyye dannyye po mekanicheskim svoystvam merzlykh gruntov pri nizkikh temperatur (do —550°C) [New data on the mechanical properties of frozen rocks at low temperatures (to —550°C)]. [By] Shusherina, Ye. P,Vrachev, V. V.,Ivashenko, I. N. Merzlotnyye I ssledovaniya, Vyp. 14,1974, p. 190–95..Google Scholar

Sinha, A. K. Electromagnetic sounding over layered permafrost terrain. Project 730004. Canada. Geological Survey. Paper 75–1, Pt. A,1975, p. 149–51. [Describes theoretical studies to solve problem of determining electrical constants of a two-layer medium.]Google Scholar

Storr, D. Fergoson, H. L. On the ambiguity of Bow en ratios over freezing and melting surfaces. Journal of Applied Meteorology, Vol. 13, No. 4,1974, p. 509–11.. [Draws attention to two different definitions ofratio and favours that which excludes the melt (freezing) term.]2.0.CO;2>CrossRefGoogle Scholar

Takashl, T., Tsuchi no ryōketsu-bōchō-ritsu ni oyobosu ryōketsu-sokudo, yūkō-ōryoku no eikyo ni kansuru kenkyū [Experimental study on the inAuence of freezing speed upon frost heave ratio of soil under constant effective stress]. [By Takashi, T.,Masuda, M.,Yamamoto, H. Seppyō, Vol. 36, No. 2,1974, p. 49–68. [Presents empirical formula for this and proposes mechanical pump model of freezing surface to explain it. English summary, p 67–68.]Google Scholar

Tarnocai, C. Thie, J. Permafrost and remote sensing. (In Thompson, C. E.ed. The applications of remote sensing and benefits to Canada. Proceedings [of the] second Canadian symposium on remote sensing, University of Guelph, Guelph, Ontario, Canada, April 29-May 1, 1974. Vol. 2. Ottawa, Canadian Remote Sensing Society,1974, p. 437–47.) [Various techniques compared; air photography, especially colour infra-red, was particularly accurate.]Google Scholar

Thompson, M. Lime stabilization offrost-susceptible soils. Frost i jord, Nr. 10,1973, p. 45–52. [Study of freezethaw durability of lime-treated soils with reference to highway construction.]Google Scholar

Thue, J. V. Om utforming av grunne fundamenter. Frost i jord, Nr. 13,1974, p. 5–21. [Describes research on thermal design of shallow foundations to be used in conditions such as exist in Norway. English summary, p 20–21.]Google Scholar

Tolstlkhin, O. N. Naledi i podzemnyye vody severo-vostoka SSSR [Naleds and underground waters of north-eastcrn U.S.S.R.]. Novosibirsk, Izdatel’stvo “Nauka”, 1974. 164 p. [Comprehensive study, including formation and distribution of naleds, and the hydrological and permafrost conditions in this area.]Google Scholar

Tomirdlaro, S. V., Fiziko-geograficheskaya obstanovka i osobennosti formirovaniya lessovo-ledovogo pokrova na ravinakh severo-vostoka Azii [Physico-geographic environment and features of formation of the loess-glacial covering of the plains of north-eastern Asia]. [by] Tomidiaro, S. V.,Ryabchun, V. K.,Ivanets, B. S. Geologiya i Geojizika, 1974, No. 7, p. 47–61. [Ice veins and polygons observed. English summary, p 61.]Google Scholar

Trush, N. I. Nistratova, T . A Sostav i svoystva alasnykh otlozheniy Yano-Indigirskogo mezhdurech’ya [Composition and properties of alas deposits of the Yana-Indigirka interAuve]. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 43–55. [Yakutskaya A.S.S.R.]Google Scholar

Ugollni, F. C. Ice-rafted sediments as a cause of some thermokarst lakes in the Noatak River delta, Alaska. Science, Vol. 188, No. 4183,1975, p. 51 – 53. [Evidence suggests sediments, which exist as sheets of mud, change albedo and thermal regime of soil, inducing development of thermokarst and leading to formation of ponds and lakes.]CrossRefGoogle Scholar

Vasil’yev, Y. M. Factors affecting the heaving of subgrade soils at freezing. Frost i jord, Nr. 12,1973, p. 17–18. [Lists factors and classifies soils according to susceptibility to heaving.]Google Scholar

Volkova, V. P. Nekotoryye osobennosti solevogo stoka v oblastyakh sploshnogo rasprostraneniya mnogoletnemerzlykh porod [Some peculiarities of salt run-off in regions of continuous permafrost]. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 116–25.. [Surface and underground waters in Yakutskaya A.S.S.R.]Google Scholar

Watson, E. Watson, S. Remains of pingos in the Cletwr basin, southwest Wales. Geograjiska Annaler, Vol. 56A, Nos. 3–4,1974, p. 213–25. [Relationship to topography and superficial d eposits similar to those of open-system pingos of central Alaska and southern Yukon; on this basis, attempt is made to reconstruct permafrost and hydrological conditions in which Cletwr pingos developed.]CrossRefGoogle Scholar

Yershov, YE. D, Kraschetnoy skheme prognoza razvitiya protsessa moroznogo issusheniya dispersnykh gornykh porod [Calculation for forecasting developments of frost drying processes of dispersed rocks] . [By] Yershov, Ye. D,Gurov, V. V.,Komarov, I. A.,Akimov, Yu. P,Kuchukov, Ye. Z Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 222–29.Google Scholar

Zamolotchikova, S. A. Pucheniye i osadka porod sloya sezonnogo ottaivaniya na Leno-Vilyuyskom vodorazdele [Heaving and settlement of the seasonally frozen layer of rocks in the Lena-Vilyuy divide]. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 148–53. [Thermokarst topogra phy, particularly frost mounds and alases, in Yakutskaya A.S.S.R.]Google Scholar

Zamolotchikova, S. A. Smirnova, V. N . T emperatury i sezonnoye ottaivaniye porod na Leno-Vilyu yskom vodorazdele [Temperature and seasonal thawing of rocks in the Lena-Vilyuy divide] . Merzlotnyye I ssledo vaniya, Vyp. 14,1974, p. 141 – 47. [Ya kutskaya A.S.S.R.]Google Scholar

Zestkova, T. N. Vlazhnost’ mineral’nykh prosloyek i agregatov merzlykh gruntov [Water content in frozen soil mineral bands and aggregates]. Merzlotnyye Issledovaniya, Vyp. 14,1974, p. 196–203.Google Scholar

Zoltai, S. C. Pettapiece, W. W. Tree distribution on perennially frozen earth hummocks. Arctic and Alpine Research, Vol. 6, No. 4,1974, p. 403–11. [Trees grow mainly on sides of hummocks or in troughs between, leaning away from the hummocks as result of severe and repeated ground heaving.]CrossRefGoogle Scholar

Zoltai, S. C. Tarnocai, C. Perennially frozen peatlands in the wes tern Arctic and subarctic of Canada. Canadian Journal of Earth Sciences, Vol. 12, No. 1,1975, p. 28–43. [Describes main types and relates occurrence to climatic zonation.]CrossRefGoogle Scholar

Battan, L. J. Doppler radar observations of a hailstorm. Journal of Applied Meteorology, Vol. 14, No, 1 1975 p. 98–108. [Results interpreted in terms of hailstone growth in updraughts.]2.0.CO;2>CrossRefGoogle Scholar

Dansgaard, W., Climatic changes, Norsemen and modern man, [by] Dansgaard, W.,Johnsen, S. J.,Rech, N.,Gundestrup, N.,Clausen, H. B.,Hammer, C. U. Nature, Vol, 255, No. 5503,1975, p. 24–28. [Use of isotope data from a core on Crest of Greenland ice sheet to deduce climatic record and deduce evidence on present fluctuations.]CrossRefGoogle Scholar

Held, I. M. suarez, M. J. Simple albedo feedback models of the icês, Tellus, Vol. 26, No. 6.1974, p. 613–29. [Analysis of simple models of albedo feedback mechanism and its effect on global climate.] CrossRefGoogle Scholar

Henmi, T. Secondary ice particle production from rimed ice. Dissertation Abstracts International B, Vol. 35, No. 61974, p. 2830-B. [Study of riming shows number of secondary particles too small to account for ice particle concentrations in clouds, but evaporation of rimed particles could. Abstract of Ph.D, thesis Colorado State University, 1974. University Microfilms rder no. 74–27949.]Google Scholar

Hobbs, P V, The dimensions and aggregation of ice crystals in natural clouds, [by] Hobbs, P. V.,Chang, S.,Locatclli, J. D. Journal of Geophysical Research, Vol. 79, No. 15,1974, p. 2199–206. [Study on particles collected in clouds and ground stations in Cascade Mountains.]CrossRefGoogle Scholar

Jouzel, J., Ètude isotopique de forage á grèle du 19 août 1971 dans la règion de Clermont-Ferrand, par J. Jouzel, L. Merlivat avec la collaboration de P. Admiral. Journal de Recherches Atmospheriques, Tom. 7 3, 1973? P- ¹67–74. [Analysis of deuterium and tritium in hailstones.]Google Scholar

Locatfill, J. D. HOBBS, P. V. Fall speeds and masses of solid precipitation particles. Journal of Geophysical Kesearch, Vol. 79, No. 15,1974, p. 2185–97. [Measurements for various sorts of natural particles with particular attention to effects of riming and aggregation.]Google Scholar

Loewe, F. Über Änderungcn des Luftdrucks während der Eiszcit. Zeitscherift für Gletscherkunde mid Glazialgeologie, Bd. 9. Ht, 1–2,1973, p. 229–30. [During changes in amount of ice on land, air pressure at original sea-level changes. Uptake of air by growth of glacier ice and by cooling ocean diminishes mass of atmosphere and average global air pressure. Presents examples.]Google Scholar

Macklin, W. C. Rye, P. J. Crystallographic orientation distributions in accreted ice. Journal of the Atmospheric Sciences, Vol. 31, No. 3,1974, p. 849–52. [Distribution of c-axes measured for wide range of air and deposition temperatures. Results can be used to infer growth environment of hail.]2.0.CO;2>CrossRefGoogle Scholar

Mossop, S. C. Hallett, J. Ice crystal concentration in cumulus clouds: influence of the drop spectrum. Science, Vol. 186, No. 4164,1974, p. 632–34. [Cloud chamber experiments on secondary ice crystals thrown off when supercooled droplets freeze on a moving target.]CrossRefGoogle ScholarPubMed

Pontikis, C., Germination des cristaux de glace dans I’air atmosphirique, par C. Pontikis, A. Rigaud et C. Rebotifx. Annates de Chimie, I om. 9, Nos. 4–6, 1974. p. 393–99. [Nucleation discussed in terms of observations of tee crystal growth in the atmosphere. Includes data on effect or electric field English abstract P- 393- Discussion, p. 399.]Google Scholar

Prodi, F. Chlorides in natural and artificial hailstones. Journal of Applied Meteorology, Vol. 14, No. 1, 1975 p. 120–24. [Technique described. Results show chlorides are distributed through lattice, but segregate to grain boundaries during storage near o°C.]2.0.CO;2>CrossRefGoogle Scholar

Schnell, R. C. Biogenie sources of atmospheric ice nuclei. Dissertation Abstracts International, B, Vol. 35, No. 6, ’1974, P. 2947–B. [Freezing nuclei formed from leaf litter, phytoplankton in sea-water and other biogenic sources Can account for large proportion of observed nuclei. Abstract of Ph.D. thesis, University of Wyoming, 1974 University Microlilms order no. 74–23704.]Google Scholar

Williams, J. H., Simulation of the atmospheric circulation using the NGAR global circulation model with ice age boundary conditions, [by] Williams, J. H.,Barry, R. G.,Washington, W. M. Journal of Applied Meteorology, Vol. 13, No. 3,1974, p. 305–17. [Boundary conditions used represent those of present and of Würm/Wisconsin glacial maximum about 20 000 years ago for January and July.]2.0.CO;2>CrossRefGoogle Scholar

Adams, E. S. Uptake by brook trout of lead and hydrocarbons from snowmobile exhaust: I. Field study. II. Lead and hydrocarbon content of snow after snowmobiling. III. Laboratory study. IV. Stamina tests Dissertation Abstracts International, B, Vol. 35, No. 4,1974, p. 1980–B. [No abstract for part II received. Abstract of Ph.D. thesis, University of New Hampshire, 1974. University Microfilms order no. 74–21088.]Google Scholar

Akitaya, E. Chōsa kādo ni yoru nad are jōhō no seiri [Statistics of avalanche accidents in Japan (1918–74) by the use of ha nd-sorting edge-punched cards]. Seppyō, Vol. 36, No. 3,1974, p. 96–103.. [Presents some facts and figures. English summary, p 102–03.]Google Scholar

Alford, D. Snow. (In I ves, J. D.,Barry, R. G. ed. Arctic and alpine environments. London, Methuen, [^e1974], p. 85–110.) [Deals wi th snow as a climatic factor.]Google Scholar

Allen, L. E. A sub-alpine snowmelt runoff model. Dissertation Abstracts rntemational, B, Vol. 35, No. 5,1974, p. 2 173-B. [Desc ribes development of digital computer model for simulat ing daily watershed run-off. Abstract of Ph.D. thesis, Uni versity of Wyoming, 1974. University Micro films order no. 74–23680.]Google Scholar

Benson, C. S., Physical cha racteristics of sea sona l snow cover in northern Alaska, by Benson, C. S.,Holmgren, B.,Trabant, D.,Weller, G. Proceedings oJ the Western Snow Co/yerence, 42nd annual meeting,1974, p. 58–63. [Describes na ture and behaviour of snow cover in this a rea.]Google Scholar

Draeger, W. C. Lauer, D. T. Area l extent of snow in fores ted regions: a practical estima tion technique using ERT S-I d a ta . Proceedings oJ the ninth i nternational Sy mposiulIl on Remote Sensing of Environment . . 1974 . Ann Arbor, Center for Remote Sensing Informa tion and Analysis, Willow Run La boratories, Environmental Research Institute of Michigan, Vol. I, [1974], p. 333–39. [Use in stream-flow forecasting verified.] Google Scholar

Evans, W. E. Progress in measuring snow cover from ERTS imagery. Proceedings of the Western Snow Conference, 42nd annual meeting,1974, p. 37–45. [Discusses some problems including errors arising from snow-covered areas which esca pe detec tion for several reasons.]Google Scholar

Fowler, W. B. T hermal conductivity- bas is of a potential method for d e termining in situ snow density. Proceedings of the Western Snow ConJerence, 42nd annua l meeting,1974, p. 44 – 52. [Describes technique and discusses accuracy.] Google Scholar

Gary, H . L. Snow accumulation and melt along borders of a strip cut in New Mexico. U.S. D ept oJ Agriculture. Forest Service . R esearch Note RM-279,1974, 8 p. [Presen ts results of two-year survey along sunny a nd shady borders of east- west 60 ft (18 m) wide clearing on south slope of spruce for est.]Google Scholar

Good, W. Ortung Lawinenverschutteter: optima ler Einsatz von Sender-Empfa nger-Sys temen . Les Alpes. Bulletin Mensuel du Club Alpin Suisse, 1975, No. I, p. 13–14. [Outlines principles of efficient sea rch for people overwhelmed by avalanches.]Google Scholar

Good, W. Zum heu t igen Stand d el' Ortung Lawinen verschutteter. Les Alpes. Bulletin Mensuel du Club A/pin Suisse, 1974, No. 12, p. 322–24. [Discusses choice of d e tectors for finding vic tims of avala nches, mentioning features of different makes .]Google Scholar

Good, W. R. Some effec ts of spring snowmelt runoff on aqua tic invertebrate populations in a high mountain stream. Dissertation Abstracts i nternational, B, Vol. 35, No. 5,1974, p. 2145–B. [Run-off a t 3000 m in Wyoming began in mid-May and reached peak in la te June. Abstract of Ph.D. thesis, University of Wyoming, 1974. Uni versity Microfilms order no. 74–23692.]Google Scholar

Goodrich, L. E. A one-dimensional numerical model for geothermal problems. Canada. National Research Council. Division of Building Research. T echnical Paper No. 421,1974, [36] p . [Model is programmed to allow flexibility in choice of thermal parameters and initi al and boundary conditions, and provision is made for build-up and decay of seasonal snow cover on ground surface.]Google Scholar

Hoham, R . W. Optimum tempera tures and tempera ture ranges for growth of snow algae. Arctic and Alpine Research, Vol. 7, No. 1,1975, p. 13–24.. [Describes la bora tory studies. Species tha t do not g row a bove 100 C and have optimum growth a t lower temperatures a re cl assified as true snow a lgae.] CrossRefGoogle Scholar

Hourcade, B. Le ramassage de la neige en haute vallee du Djadj-e-Roud (Elbourz central, Ira n). ReVile de Geographie Alpine, Tom. 63, Fasc. I,1975, p. 147–49. [Commerce in snow in Iran, where it was once coll ected from the mounta ins and tra nsported to Tehran, is now d ying out.]CrossRefGoogle Scholar

Ives, J. D., Development of methodologyfor evaluation and prediction of avalanche hazard in the Sanfuan mountain Area of southhwestem Colorado, [by] Ives, F. D.,Harrison, F. C.,Armstrang, R. L. Boulder, Colora do, University of Colorado. Institute of Arctic and Alpine Research, 19 73. [viii], 122 p . (INSTAAR-14–06–7155–2.) [Study of rela tionship between terrain, clima te and snow stratigraphy.]Google Scholar

JernelÖv, A. Wallin, T.. Air-borne mercury fall-out on snow around five Swedish chlor-alkali plants. Atmospheric Environment, Vol. 7, No. 2,1973, p. 209–14. [Only small fraction of total amount is deposited locall y.]CrossRefGoogle ScholarPubMed

Kol, E. Eurola, S. Red snow algae from Spitsbergen. Astarte, Vol. 7, No. 2,1974, p. 61–66. [Twelve Arctic- alpine species, three of them new to Spitsbergen, recorded in ten localities.]Google Scholar

Kolomyts, E. G. Kristallomorfologiya i metamorfizm snezhnoy tolshchi (k teorii strukturnogo snegovedeniya) [Crystallomorphology and metamorphism of snow cover (theory of snow structure)]. Sibirskiy Geograjicheskiy Sborniik, [No.] 8,1974, p. 69–144. [Describes theoretical and field studies. English abstract, p . 278.]Google Scholar

Korolev, A. I. Nablyudeniya za dvizheniyem laviny [Avalanche movement observations]. Meteorologiya I Gidrologiya, 1974, No. 5, p. 107–08. [Discusses vari a tions in snow friction in different parts of avalanche.]Google Scholar

Lang, H. Davidson, G. Beitrag zum Problem del' klima tischen Schneegren ze. Verhandlllngen der Schweizerischen N aturforschenden Gesellschaft, 1973, p. 158–60. [Contribution to the problem of the climatic snow line, with reference to results obtained at Weissfluhjoch.]Google Scholar

Larson, F. R., Using aerial measurements of forest overstory and topography to estimate peak snowpack, [by] Larson, F. R.,Ffo lliott, P. F.,Moessner, K.E U.S. Dept. of Agriculture. Forest Service. Research Note RM-267,1974, 4 p. [Wher e slope steepness and aspect vary, and several forest overstory size and density classes are mixed, only topogra phic a ttributes need be measured.]Google Scholar

LemmelÄ, R. Kuusisto, E. Evaporation from snow cover. Hydrological Sciences Bulletin, Vol. 19, No. 4,1974, p. 541–48. [Discusses dependence on climatic factors. Mean evaporation in daytime (0700–1900 h) was 0.26 mm and during night 0.03 mm during 107 d ays between Februa ry and April in southern Finland .] Google Scholar

Lorch, W. Méthodes modernes pour éviter le mort sous l'avalanche. Les Alpes. BulletinMensuel du Club Alpin Suisse, 1974, No. 12, p. 325–[29]. [Discusses choice of d etectors for finding avalanche victims, listing features of various makes.]Google Scholar

Lowndes, C. A. S., An assessment of the usefuln ess of some snow predictors, by Lowndes, C.A.S,Beynon, A.,Hawson, C. l. Meteorological Maga z ine, Vol. 103, No. 1229,1974, p. 341–58. [Probability of snow obtained for different values of four predictors, based on observations made at stations in Wales and West Midlands of England.]Google Scholar

Mackay, J. R. Mackay, D. K. Snow cover and ground temperature, Garry Island N.W.T. Arctic, Vol. 27, No. 4,1974, p. 287–96. [Discusses insulating effect of snow for 1968–73 period.]CrossRefGoogle Scholar

Martinelli, M. Snow ava la nche sites; their identification and evaluation. V.S. Dept. oJ Agriculture. Forest Service. Agriculture Information Bulletin 360,1974,27 p . [Describes, with many illustra tions, ava lanche-prone areas and how to estimate frequency and intensity. Presents check-list for field observers to help evaluate evidence.] Google Scholar

Nord, M. Taesler, R. Snotackets densitet och massa i Sverige. Statens Institutfor Byggnadsforsknillg. Rapport, R2 I:1973, [1973,] [iv], 124 p. [Density and weight of snow cover in Sweden, using data from 1909–25 and 193 1–60. English abstract, pii i- iv.]Google Scholar

Onodera, H. Hokkaidō shiretoko-hantō ni o keru nadare-taiseki chi no tokuchō [The dirt cone deposition of an avalanche on Shire toko peninsul a, Hokkaido]. Seppy6, Vol. 36, No. 2,1974, p. 69–72. [Describes cone, which was observed on 26 July 1970 a nd was composed of snow under a 10–15 cm layer of rocks and clods. English summary, p 72.]Google Scholar

Parry, J. T. X-band radar in terrain analysis und er summer and winter conditions. (In Thompson, G. E. ed. The applications of remote sensing and benefits to Canada. Proceedings [of the] second Canadian symposium 011 remote sensing, University ofCuelph, Cue/ph, Ontario, Canada, April 29- May 1, 1974. Vol. 2. Ottawa, Canadian Remote Sensing Society, 1974, p. 471–85.) [Describes advantages of SLAR systems. Tested over snow cover up to 40 cm d epth.]Google Scholar

Parry, J.T Grey, B. The use of composite minimum brightness charts in the ma pping and interpretation of snow in Quebec-Labrador. (In Thompson, G. E.ed. The application of remote sensing alld benefits to Canada. Proceedings [of the] second Canadian symposium on remote sensing, University of Cue/ph, Guelj)h, Olltario, Canada, April 29 - May 1, 1974. Vol. 1. Ottawa, Ca nadian Remote Sensing Society,1974, p. 165–84.) [Presents results of investigation of areal ex tent and temporal variation of snow cover in this area from early March to late July.]Google Scholar

Peak, G. W. An ice melt formula. Proceedings oJ the Western Snow COIiference, 42nd annual meeting, 1974, p. 64–72. [Discusses application to snow melt run-off.]Google Scholar

Pearson, T. Simulating runoff to the Hungry Horse reservoir of western Montana. Proceedings of the Westem Snow COliferellce, 42nd annual meeting, 1974, p. 96–102. [Shows that major basin with large snow-melt component can be reconstituted on annual basis with good results, and basin model can be used for planning Rood control, stream-Row forecasting, etc.]Google Scholar

Peel, D. A. Organochlorine residues in Antarctic snow. N ature, Vol. 254, No. 5498, 1975, p. 324–25. [Samples from previous 5–10 yr accumulation a nalysed for DDT; results s uggest concentration of DDT in atmosphere may not be as high as thought.]Google Scholar

Quervaln De, M. R. Die Berucksichtigung der Lawinenhaufigkeit in del' Lawinengefa hre nkarte. Eine grundsatzliche Betrachtung. Winterbericht des Eidgerzossischen Institutes Jilr Sclmee- Imd Lawineliforschllllg, Nr. 37,1974, p. 157–62. [Proposals discussed for prepa ration of map showing likelihood of avalanches and most suitable scheme to adopt based on fa ctors such as pressu re, time and location .]Google Scholar

Quervaln De, M. R. Eine internationale Lawinenklassifikation. Z eitsclzriflfijr Cletscherkul1de wld Cla zialgeologie, Bd. 9, Ht. 1–2,1973, p. 189–206. [Presents German version of proposals of the working group of the International Commission of Snow and Ice (see Hydrological Sciences Bulletill, Vol. 18, No. 4,1973, p. 391 – 402) for a valanche classification.]Google Scholar

Rickerd, J. P. Earth quakes, traffic vibrations, skiers- what triggers an avalanche ? Science Dimension, Vol. 7, No. I,1975, p. 22–27. [Outlines work of the Di vision of Building R esearch, National Research Council of Canada, investigating characteristics of a valanches and ava lanche defence methods. T ext in English and French .]Google Scholar

Ricq-debouard, M. Interpre tation de mesures chimiques et physico-chimiques sur des ea ux de fusion de neige et de glace. ZeitschriftJiir Gletscherkullde Illld Glaz ialgeologie, Bd. 9, Ht. 1–2,1973, p. 169–80. [Presents results of analysing melt waters.]Google Scholar

Roten, M. A propos de chutes de neige sale en Suisse centrale (mars (973). Revue de Geographie Alpine, Tom. 62, Fasc. 3,1974, p. 315–25. [Discusses grey colo ur of snowfall on 13 a nd 14 March 1973 due to dust.] CrossRefGoogle Scholar

Saeki, M., Mitsumata ōnadare hassei-seki chi no rinkyo chosa [Investigation of condition of forest on site of origin of large avala nche in Mitsuma taJ. [By] Saeki, M.,Watanabe, S.,Umeyama, D.,Kawai, E. Seppyō, Vol. 36, No. 2,1974, p. 73–78. [Avalanche occurred in 1918 and there ha ve been heavy snowfalls since then. Growth of trees is poor on upper ha lf of slope. English summary, p 78.]Google Scholar

Salto, S. Setsugai taisaku to shiteno heitanchi ni okeru nanameue [Slant planting for reducing snow damage on Rat ground] . Seppyô, Vol. 36, No. 4,1974, p. 137–40. [Suggests method of planting trees to reduce damage by snow. E nglish summa ry, p. 140.]Google Scholar

Shul'ts, V. L. Suslov, V. F. ed. Glyatsiologiya Sredney Azii (s nezhnyy pokrov i ledniki) [Glaciology of Central Asia (snow cover and glaciers)]. Srednea z iaticheskiy Regiollal'nyy Naucllllo-Issledo vatel'skiy Cidrometeorologicheskiy IlI stitut. Trudy, Vyp. 9(90),1973, 128 p. [Ten a rti cles dealing with snow cover in mounta inous areas, hydrometeorological glacier regimes and melt water Row.]Google Scholar

Slaughter, C. W., Snow accumulation for Arctic freshwater supplies, [by] Slaughter, C. W.,Melior, M.,Sellmann, P. V.,Brown, J.,Brown, R. Arctic Builetin, Vol. I, No. 5, [1975] p 218–24. [Discusses use of fences for snow drift accumula tion to increase amount of snow available for fresh water.]Google Scholar

Slaymaker, H. O. Alphine hydrology. (In Ives, J. D.,Barry, R. G. ed. Arctic alld alpine environmellts. London, Methuen, [Cl 974], p. 133–58.) [Includes effects of snow accumulation and snow melt, and contrasts Arctic and a lpine hydrology.]Google Scholar

Sofiyan, A. P. Mazur, A. I. Veroyatnosti raschet vysoty snezhnogo pokrova s uchetom territori al'noy neravnomernosti zalega niya [Probability calculation of snow cover d epth taking into account areal nonuniformity of deposits]. M eteorologiya i Gidrologiya, 1974, No.5,p. 80–8S. [English summary, p 84.]Google Scholar

tabler, R. D. New engineering criteria for snow fence systems. Tratlsportation Research Record 506,1974, p. 65–78. [Summarizes factors contributing to success of snow fences specially constructed along new section of road in Wyoming.]Google Scholar

Vinje, T. E. On the small scale features of temperature and wind profiles nea r a snow surface. Norsk Polarillstitult. Arbok 1973 [pub. 1975], p. 27–39.• [Vertical extension ofzig-zag form found to be markedly reduced with decreasing roughness of underlying surface.]Google Scholar

Willlams, G. P. Surface heat losses from heated pavements during snow melting tests. Canada. JVational Research Council. Division of Building R esearch. T echnical Paper 10 • 427,1975, [36] p. [Presents observations, analysis and res ults of tests carried out during three winter seasons on elec trically heated concrete slab instrumented to measure heat in-puts and losses during and between snowfalls.]Google Scholar

Young, G. J. A stratified sampling design for snow surveys based on terra in shape. Proceedings of the Westertl Snow Conference, 42nd annual meeting,1974, p. 15–22. [Spatial distribution of snow-pack at cnd of winter may be mapped by this method.]Google Scholar