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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Copyright © International Glaciological Society 1973

This is a selected list of glaciological literature on the scientific study of snow and ice and of their effects on the Earth; for the literature on polar expeditions, and also on the “applied” aspects of glaciology, such as snow ploughs, readers should consult the bibliographies in each issue of Recent Polar Literature. For Russian material the system of transliteration used is that agreed by the U.S. Board on Geographic Names and the Permanent Committee on Geographical Names for British Official Use in 1947. Readers can greatly assist by sending reprints of their publications to the Society, or by informing Dr J. W. Glen of publications of glaciological interest. It should be noted that the Society does not necessarily hold copies of the items in this list, and also that the Society does not possess facilities for microfilming or photocopying.

References

General Glaciology

Bentley, C. R., and others. The International Antarctic Glaciological Project standardization document, by Bentley, C. R., Budd, W. F., Kotlyakov, V. M., Lorius, C. and Q. Robin, G. de. Polar Record, Vol. 16, No. 101, 1972, p. 34964. [Sets out agreed standards for various studies so that different national groups may produce readily comparable results.]Google Scholar
Müller, F., and others. International Geographical Union. Field tour Ea2: Arctic Archipelago I. 22nd International Geographical Congress. Miscellaneous papers, [by] F. Müller and members of the expedition. Axel Heiberg Island Research Reports, McGill University, Montreal, 1972, iv, 56 p. [Contains the following papers: Müller, F., “Climatological research on Axel Heiberg Island”, p. 1–3 ; Ohmura, A., “Some climatological notes on the expedition area”, p. 5–13; Braithwaite, R., “Statistical modelling of the thermal interaction of ice masses with the atmosphere”, p. 15–18; Young, G. J., “Snow sampling at the end of winter, Wolf River basin”, p. 19–23; Young, G. J., “White Glacier mass balance”, p. 25–30; Iken, A., “Velocity variations of the White Glacier”, p. 31–38; Maag, H. U., “Ice-dammed lakes on Axel Heiberg Island, with special reference to the geomorphological effect of the outflowing lake water”, p. 39–48; Caflisch, T., “Limnological investigations on Colour and Phantom lakes”, p. 49–56.]Google Scholar
Savel’yev, B. A. Fizika, khimiya i stroyeniye prirodnykh l’dov i merzlykh gornykh porod [Physics, chemistry and structure of natural ice and frozen rocks]. Moscow, Izdatel’stvo Moskovskogo Universiteta, 1971. 506 p.Google Scholar
Simonov, I. M. Oazisy vostochnoy Antarktidy [Oases of eastern Antarctica]. Leningrad, Gidrometeorologicheskoye Izdatel’stvo, 1971. 176 p. [Study of formation, landscape, climate and natural history of oases along the coast from Dronning Maud Land to Wilkes Land.]Google Scholar
Tronov, M. V., ed. Glyatsiologiya Altaya [Glaciology of the Allay]. Vyp. 6. Tomsk, Izdatel’stvo Tomskogo Universiteta, 1970. 288 p. [Twenty-one articles: no English abstracts.]Google Scholar
Tuhinskiy, G. K., ed. Inzhenernaya glyatsiologiya [Engineering glaciology]. Moscow, Izdatel’stvo Moskovskogo Universiteta, 1971. 208 p. [Textbook based on course in Moscow State University. First part describes relevant mechanical properties of snow and ice; second part introduces many applications of glaciology.]Google Scholar
Zamoruyev, V. V. Rezul’taty glyatsiologicheskikh nablyudeniy na stantsii Bellinsgauzen v 1968 g. [Results of glaciological observations at “Bellingshausen” station in 1968]. Trudy Sovetskoy Antarkticheskoy Ekspeditsii, Tom 55, 1972, p. 13544.Google Scholar

Glaciological Instruments and methods

Boutron, C. Concentration of dilute solutions at p.p.b. level by non-boiling evaporation in quartz and teflon. Analytica Chimica Acta, Vol. 61, No. 1, 1972, p. 14043. [Method for preconcentration of dilute ionic solutions in the presence of acids developed to allow flame spectrometry of Antarctic snow samples.]Google Scholar
Jollymore, P. G. A portable digital sounding system for Arctic use. International Hydrographic Review, Vol. 48, No. 2, 1971, p. 3542. [Describes a light-weight digital echo sounder for water depth determination through ice.]Google Scholar
Lesca, C. Metodo generalizzato per la determinazione di variazioni volumetriche con impiego della fotogrammetria e del calcolatore elettronico. Bollettino del Comitato Glaciologico Italiano, Ser. 2, No. 19, 1971, p. 28198. [Application to glaciology discussed.]Google Scholar
Vickers, R. S., and Rose, G. C. Short pulse radar measurements of layered ice and snow. (In 4th annual earth resources program review. Vol. 3. U.S. Geological Survey programs. Presented at the Manned Spacecraft Center, Houston, Texas, January 17 to 21, 1972. Houston, Texas, NASA Manned Spacecraft Center, 1972, p. 67-167-20.) [Describes development of a high resolution system for the remote measurement of layer thickness, designed for eventual incorporation into light-weight aircraft.]Google Scholar

Physics of Ice

Aburakawa, H., and Yosida, Z. Sekisetsu oyobi kōri no teishūha Yangu-ritsu sokutei-yō rensei-furiko [A double pendulum used for the determination of low frequency Young’s modulus of snow and ice]. Teion-kagaku: Low Temperature Science, Ser. A. [No.] 29, 1971, p. 3749. [Measurement of Young’s modulus of snow and commercial ice down to 2.2 Hz. English summary, p. 4749.]Google Scholar
Auvert, G., and others. Low entropy form of ice I h obtained from a linear step growth model, [by] Auvert, G., Bullemer, B. and Kahane, A.. Solid State Communications, Vol. 11, No. 8, 1972, p. 103134. [Linear growth, molecule by molecule, in the basal plane leads to non-equilibrium configurational entropy.]Google Scholar
Azouni, M. Effets d’une membrane sur la progression d’un front de glace dans l’eau. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. C, Tom. 275, No. 3, 1972, p. 15557. [Effect of a semipermeable membrane on rate of freezing of water.]Google Scholar
Bales, B. L., and Kevan, L. Role of fluoride ion in irradiated aqueous systems. Journal of Chemical Physics, Vol. 57, No. 4, 1972, p. 181314. [Suggests that F can serve as a hole trap in irradiated ice doped with KF or NH4F.]Google Scholar
Bantysh, L. A., and others. Vliyaniye vneshnego magnitnogo polya na skorost’ kristallizatsii vody i strukturu obrazuyushchegosya l’da [Effect of an external magnetic field on the rate of water crystallization and structure of the resulting ice]. [By] Bantysh, L. A., Popovskiy, V. G., Lazarenko, B. R., Kreponosova, A. N.. Elektronnaya Obrabotka Materialov, 1972, No. 2, p. 5458. [Both crystallization rate and structure are affected.]Google Scholar
Barchet, W. R., and Corrin, M. L. Water vapor adsorption by pure silver iodide above ice saturation. Journal of Physical Chemistry, Vol. 76, No. 16, 1972, p. 228085. [Evidence for liquid-like adsorbate-vapour interface prior to nucleation. Classical nucleation theory is inadequate to explain these data.]Google Scholar
Blom, B. E. Desalination by high-pressure solidification of water to ice IV [sic ]. Dissertation Abstracts International, B, Vol. 32, No. 6, 1972, p. 3875-B. [Direct formation of ice VI from saline solutions by pressure used to show feasibility of desalination in this way. Second part of Ph.D. thesis, Clarkson College of Technology, 1971. University Microfilms order no. 72–1727.]Google Scholar
Bodhaine, B. A. The effects of ammonia on the electrification of freezing and splashing water drops. Tellus, Vol. 24, No. 5, 1972, p. 47380. [Water drops containing NaCl and/or (NH4)2CO3 were cooled and then fell on ice target. Charge deposited was measured and sign could be varied by control of impurities.]Google Scholar
Bogorodskiy, V. V., and Khokhlov, G. P. Mezhdusloynaya polyarizatsiya vo l’du, soderzhashchem vklyucheniya NaCl [Interlayer polarization in ice containing sodium chloride inclusions]. Trudy Arkticheskogo i Antarkticheskogo Nauchno-1ssledovatel’skogo Instituta, Tom 295, 1970, p. 10307. [Measurements of electrical permittivity with and without blocking electrodes.]Google Scholar
Bogorodskiy, V. V., and Khokhlov, G. P. Vliyaniye nekotorykh solevykh komponent i ikh sostava na elektricheskiye svoystva l’da [Effect of some salt components and their composition on the electrical properties of ice]. Trudy Arkticheskogo i Antarkticheskogo Nauchno-1ssledovatel’ skogo Instituta, Tom 295, 1970, p. 8995. [Study of effect of KCl, NaCl and MgCl2 on electrical properties of ice.]Google Scholar
Bryan, J. B., and Curnutte, B. A normal coordinate analysis based on the local structure of liquid water. Journal of Molecular Spectroscopy, Vol. 41, No. 3, 1972, p. 51233. [Includes calculation of far infrared frequencies for ice in good agreement with measured peaks.]Google Scholar
Chatterton, P. A., and Cross, J. D. Early stages of the growth of ice in the air at low pressure. Nature, Physical Science, Vol. 236, No. 67, 1972, p. 9192. [Ice formed by condensing low-pressure water vapour at 160 K is not crystalline.]Google Scholar
Duval, P. Fluage et recristallisation dynamique de la glace polycristalline. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. D, Tom. 275, No. 3, 1972, p. 33739. [Tertiary creep of randomly oriented polycrystalline ice and of strongly textured Antarctic ice studied for periods of several weeks.]Google Scholar
Edmonds, D. T., and Zussman, A. Pure quadrupole resonance of 17O in ice. Physics Letters, Vol. 41A, No. 2, 1972, p. 16769. [Effect observed in ice enriched in 17O and the quadrupole coupling constant observed is very different from that in isolated H2O molecule due to hydrogen bonding.]Google Scholar
Falciglia, F., and others. Magnetic quenching of orthopositronium in ice, [by] Falciglia, F., Iaci, G., Lo Savio, M. and Turrisi, E.. Lettere al Nuovo Cimento della Società Italiana di Fisica, Vol. 5, No. 3, 1972, p. 30204. [Discusses how to resolve differences between observed and calculated values of this quantity.]Google Scholar
Faure, P., and Kahane, A. Modéle dynamique polaire de la glace Ih rnonocristalline. (In Nusimovici, M. A., ed. Phonons. Comptes rendus de la conférence internationale, Rennes, France, 1971. Paris, Flammarion Sciences, [c1971], p. 24347.) [Model of ice with locally oriented regions which fluctuate rapidly.]Google Scholar
Floyd, G. R., and Prince, R. H. Production of ionized water clusters by electron bombardment of ice. Nature, Physical Science, Vol. 240, No. 97, 1972, p. 1112. [Bombardment in high vacuum at 153 and 193 K produced H+(H2O)n clusters with 3 ⩽ n ⩽ 8 while bombardment at 77 K produced nothing.]Google Scholar
Franks, F., ed. Water: a comprehensive treatise. Vol. 1. The physics and physical chemistry of water. New York, London, Plenum Press, 1972. xx, 596 p. [Contains chapters on “The properties of ice”, by Franks, F., p. 11549; “Nuclear magnetic resonance studies on water and ice”, by Glasel, J. A., p. 215–54.]Google Scholar
Friedrichs, H. A., and others. Zur Auflösung eines Kristalls in der eigenen Schmelze, Friedrichs, von II. A., Jauer, H. und Knacke, O.. Zeitschrift für Metallkunde, Bd. 63, Ht. 4, 1972, p. 16972. [Theory for melting of crystal in its own well-stirred melt derived, and model experiments on ice performed.]Google Scholar
Glasser, M. L., and others. Analytic properties of the free energy for the “ice” models, [by] Glasser, M. L. and Abraham, D. B. and Lieb, E. H.. Journal of Mathematical Physics, Vol. 13, No. 6, 1972, p. 887900. [Theoretical calculation of free energy of 2-dimensional square lattice obeying Bernal-Fowler rules.]Google Scholar
Gobush, Jr.,W., and Hoeve, C. A. J. Calculation of the dielectric correlation factor of cubic ice. Journal of Chemical Physics, Vol. 57, No. 8, 1972, p. 341621. [Method for estimation of factor entering into theoretical calculation of entropy of cubic ice.]Google Scholar
Gold, L. W. The process of failure of columnar-grained ice. Philosophical Magazine, Eighth Ser., Vol. 26, No. 2, 1972, p. 31128. [Study of cracks forming during compressive creep.]Google Scholar
Gough, S. R. Comment on the microwave “dielectric constant” of ice. Journal of Applied Physics, Vol. 43, No. 10, 1972, p. 4251. [Points out that values obtained by Perry, J. W. and Straiton, A. W., ibid., Vol. 43, No. 2, 1972, p. 731–33, are inconsistent with other experiments.]Google Scholar
Gough, S. R. A low temperature dielectric cell and the permittivity of hexagonal ice to 2 K. Canadian Journal of Chemistry, Vol. 50, No. 18, 1972, p. 304651. [Measurement of high-frequency permittivity from 2 to 270 K.]Google Scholar
Gow, A. J., and Williamson, T. C. Linear compressibility of ice. Journal of Geophysical Research, Vol. 77, No. 32, 1972, p. 634852. [New technique at relatively low pressures (less than 0.5 kbar) described.]Google Scholar
Gränicher, H. NMR investigations of ice crystals. I. Proton magnetic resonance in ice. (In Blinc, R., ed. Pulsed magnetic and optical resonance. Proceedings of the Ampère International Summer School II, Basko polje, 2–13 September 1971. Ljubljana, Institut “Jozef Stefan”, 1972, p. 22331.) [Review of past work and what can be deduced from it.]Google Scholar
Greenberg, J. M. Absorption and emission of radiation by nonspherical particles. Journal of Colloid and Interface Science, Vol. 39, No. 3, 1972, p. 51319. [Absorption and emission cross-sections of very small particles depend on their shapes even when the Rayleigh approximation is valid. Detailed application to infra-red absorption spectrum of ice.]Google Scholar
Gritsay, V. A., and others. Adgeziya l’da k nekotorym plastikam [Adhesion of ice to some plastics]. [By] Gritsay, V. A., Nechipor, A. I., Shvayshteyn, Z. I., Kamenetskiy, I. Ya.. (In Borisenkov, Ye. P., ed. Teoreticheskiye i eksperimental’nyye issledovaniya usloviy obledeneniya sudor. Leningrad, Gidrometeorologicheskoye Izdatel’stvo, 1971, p. 14649.) [Adhesion force of ice to 10 plastics less than to steel or aluminium, and increases with decreasing temperature.]Google Scholar
Gross, G. W. Solute interference effects in freezing potentials of dilute electrolytes. (In Jellinek, H. H. G., ed. Water structure at the water–polymer interface. Proceedings of a symposium held on March 30 and April 1, 1971, at the 161st .National Meeting of the American Chemical Society. New York, London, Plenum Press, 1971, p. 10625.) [Observations of charge separation phenomena during freezing and of interference effects between different solute species.]Google Scholar
Hahne, E. W. P., and Grigull, U. Regelation of ice. Problem of heat conduction. International Journal of Heat and Mass Transfer, Vol. 15, No. 5, 1972, p. 105766. [Experiments on penetration of wires of various conductivity and diameter through ice. Theory agrees well with results.]Google Scholar
Hanley, T. O’D. Freezing potentials in potassium fluoride solutions at constant growth rate. Dissertation Abstracts International, B, Vol. 33, No. 3, 1972, p. 1250-B. [Measurement of freezing potentials and their interpretation. Abstract of Ph.D. thesis, St. Louis University, 1971. University Microfilms order no. 72–23945.]Google Scholar
Helmreich, D. Molecular forces of heavy and light ice. (In Nusimovici, M. A., ed. Phonons. Comptes rendus de la conférence internationale, Rennes, France, 1971. Paris, Flammarion Sciences, [c 1971], p. 27983.) [Deduction of variation of intermolecular force constants with temperature and pressure.]Google Scholar
Jones, D. R. H., and Chadwick, G. A. Experimental measurement of the solid-liquid interfacial energies of transparent materials. Philosophical Magazine, Eighth Ser., Vol. 22, No. 176, 1970, p. 291300. [Includes ice–water interfacial energy.]Google Scholar
Jones, D. R. H., and Chadwick, G. A. An expression for the free energy of fusion in the homogeneous nucleation of solid from pure melts. Philosophical Magazine, Eighth Ser., Vol. 24, No. 190, 1971, p. 99598. [Includes correction to ice–water interfacial energy as determined from homogeneous nucleation.]Google Scholar
Kawabata, K., and others. Shoulder of optical absorption spectrum of the trapped electron in gamma-irradiated crystalline ice, [by] Kawabata, K., Okabe, S. and Taniguchi, S.. Journal of Chemical Physics, Vol. 57, No. 7, 1972, p. 285556. [Precise measurements suggest at least two components in the spectrum.]Google Scholar
Krause, P. M. Conduction mechanisms in pure and doped hexagonal ice. Dissertation Abstracts International, B, Vol. 33, No. 3, 1972, p. 1250-B51-B. [Measurements on pure ice and ice doped with KCl and HCl, 50 Hz to 20 kHz, −100° C to 0° C. Abstract of Ph.D. thesis, St. Louis University, 1970. University Microfilms order no. 72–24043.]Google Scholar
Lebedev, D. P., and Andreyev, Ye. F. Optimal’nyye usloviya desublimatsii l’da v vakuume i zavisimost’ ot nikh ρ i λ l’da [Optimum conditions of ice de-sublimation in vacuo and dependence of ρ and λ of ice on these conditions]. Inzhenemo-Fizicheskiy Zhurnal, Tom 23, No. 1, 1972, p. 3341. [Visual and photographic observations of ice deposition process from vapour. Form of interface, its density and thermal conductivity at different vapour pressures. English summary, p. 40.]Google Scholar
Maeno, N. Enka-kariumu-hyō no yūden bunsan. III. Kōnōdo-hyō no yūden bunsan [The dielectric dispersion of KCl ice. III. The dielectric dispersion of high-concentration ice]. Teion-kagaku : Low Temperature Science, Ser. A, [No.] 29, 1971, p. 110. [Above concentration of 10−2M, two dielectric dispersions are observed, that at high frequencies showing a single relaxation process. English summary, p. 10.]Google Scholar
Rahman, A., and Stillinger, F. H. Proton distribution in ice and the Kirkwood correlation factor. Journal of Chemical Physics, Vol. 57, No. 9, 1972, p. 400917. [Correlation due to Bernal–Fowler rules calculated for ice Ih and ice Ic. Consequent value of effective dipole moment of water molecule in ice is 2.92 D.]Google Scholar
Rasmussen, D. H., and Mackenzie, A. P. Effect of solute on ice–solution interfacial free energy; calculation from measured homogeneous nucleation temperatures. (In Jellinek, H. H. G., ed. Water structure at the water–polymer interface. Proceedings of a symposium held on March 30 and April 1, 1971, at the 161st National Meeting of the American Chemical Society. New York, London, Plenum Press, 1971, p. 12645.) [Measurements for a number of solutions.]Google Scholar
Reischel, M. T. Ice whiskers. Weather, Vol. 27, No. 10, 1972, p. 42330. [Discusses reports of whisker growth on ice, and whiskers’ possible properties, origin and significance.]Google Scholar
Renker, B. Lattice dynamics of D2O-ice Ih. (In Nusimovici, M. A., ed. Phonons. Comptes rendus de la conférence internationale, Rennes, France, 1971. Paris, Flammarion Sciences, [c 1971], p. 16770.) [Phonon dispersion curves measured by inelastic neutron scattering at 90 K.]Google Scholar
Rozental’, O. M. Voprosy obrazovaniya l’da v vode i rastvorakh. 111. Zarozhdeniye l’da pri radiolize vody [Problem of the formation of ice in water and solutions. III. Formation of ice during radiolysis of water]. Zhurnal Fizicheskoy Khimii, Tom 46, Vyp. 4, 1972, p. 97172. [Increase in number of dissociated molecules when water is irradiated with γ rays assists ice nucleation in supercooled water. English translation in Russian Journal of Physical Chemistry, Vol. 46, No. 4, 1972, p. 559–60.]Google Scholar
Schmidt, V. H. NMR investigations of ice crystals. 11. Deuteron spin-lattice relaxation in D2O ice. (In Blinc, R., ed. Pulsed magnetic and optical resonance. Proceedings of the Ampère International Summer School II, Basko polje, 2–13 September 1971. Ljubljana, Institut “Jozef Stefan”, 1972, p. 23237.) [Two pairs of lines observed at −80° C which broaden, and one pair vanish, on heating to −8° C. Interpreted as showing deuterons move by vacancy, not Bjerrum defect, diffusion.]Google Scholar
Shio, H., and Magono, C. Frictional electrification of polycrystalline and single ice crystals. Journal of the Meteorological Society of Japan, Vol. 50, No. 3, 1972, p. 15965. [Concludes that polycrystalline ice is always electrified positively when rubbed with single crystal ice.]Google Scholar
Spengler, J. D., and Gokhale, N. R. Freezing of freely suspended, supercooled water drops in a large vertical wind tunnel. Journal of Applied Meteorology, Vol. 11, No. 7, 1972, p. 110107. [Description of tunnel and observation of behaviour of large drops as they freeze.]Google Scholar
Suzuki, S. Asshuku henkei de shōjiru kōtino saikesshō [Recrystallization of compressed ice]. Teion-kagaku: Low Temperature Science, Ser. A. [No.] 29, 1971, p. 1128. [Observation of recrystallization phenomena in compressed ice bicrystals. English summary, p. 28.]Google Scholar
Villain, J. The 3-dimensional eight vertex model and the proton–proton correlation functions in ice. Solid Stale Communications, Vol. 10, No. 10, 1972, p. 96770. [Theoretical study of statistics of protons in ice as compared with two-dimensional model.]Google Scholar
Vodovskiy, A. L. Eksperimental’noye opredeleniye davleniya pri rashirenii l’da [Experimental determination of pressure when ice expands]. Gidrotekhnicheskoye Stroitel’stvo, 1972, No. 8, p. 4647.Google Scholar
Von Hippel, A. R., and others. Dielectric and mechanical response of ice Ih single crystals and its interpretation, by A. [R.] Hippel, Von, Mykolajewycz, R., Runck, A. H. and Westphal, W. B.. Journal of Chemical Physics, Vol. 57, No. 6, 1972, p. 2560–71. [Interpretation of the seven dielectric relaxation spectra found in ice Ih crystals using data on HF-doped crystals. Mechanical relaxation attributed to different process.]Google Scholar
Weithase, M., and others. Proton spin relaxation in hexagonal ice. 11. The T1ρ minimum, [ by] Weithase, M., Noack, F. and Schütz, J. von. Zeitschrift für Physik, Bd. 246, Ht. 1, 1971, p. 9196. [Measurement of this relaxation time shows minimum at low field strengths and allows determination of proton correlation time.]Google Scholar
Zadumkin, S. N., and Khokonov, Kh. B. Akusticheskiy effekt pri kristallizatsii vody [Acoustic effect during the crystallization of water]. Trudy Vysokogornogo Geofizicheskogo Instituta, No. 17, 1970, p. 25559. [Ferroelectric detectors used to sense acoustic emission during freezing of water and melting of ice.]Google Scholar
Zweerink, G. L. The thermal accommodation coefficients of helium, neon and argon on surfaces. Dissertation Abstracts International, B, Vol. 32, No. 12, Pt. 1, 1972, p. 6966-B. [Measurements on ice surfaces at 77 K. Abstract of Ph.D. thesis, University of Missouri, Rolla, 1971. University Microfilms order no. 72-18195.]Google Scholar

Land Ice. Glaciers. Ice Shelves

Ambach, W. Zur Schätzung der Eis-Nettoablation im Randgebiet des grönländischen Inlandeises. Polarforschung, 42. Jahrg., Nr. 1, 1972, p. 1823. [Relation between net ablation and height above sea-level.]Google Scholar
Barnakova, G. M., and Rototayeva, O. V. Basseyn r. Surkhob mezhdu ust’yami rek Obikhingoy i Muksu [Basin of the river Surkhob between the mouths of the Obikhingoy and Muksu rivers]. Katalog lednikov SSSR [Catalogue of glcciers of the U.S.S.R.]. Tom 14, Vyp. 3, Chast’ 6. Leningrad, Gidrometeorologicheskoye Izdatel’stvo, 1971. 90 p. [Part of the I.H.D. catalogue of glaciers of the U.S.S.R. giving details of what is known of the glaciers in this part of Central Asia (Amu-Dar’ya). The Tom and Vyp. numbers correspond with those of Resursy poverkhnostnykh vod SSSR [Surface water resources of the U.S.S.R.].]Google Scholar
Belloni, S. Ricerche di laboratorio sulle precipitazioni occulte e sui parametri che le determinano. Bollettino del Comitato Glaciologico Italiano, Ser. 2, No. 19, 1971, p. 299309. [Discusses the effect of condensation from the air (hidden precipitation) on the hydraulic balance of a glacier and describes a method of measuring this. Discussion, p. 309.]Google Scholar
Benson, C. S., and others. Glaciers, , [by] Benson, C. [S.], Harrison, W. [D.], Raymond, C. [F.], Meier, M. [F.], Shreve, R. [L.] and Weller, G.. Eos. Transactions. American Geophysical Union, Vol. 53, No. 3, 1972, p. 24853. [Summarizes U.S. studies conducted in North American and Antarctic glacier basins since 1965 as part of the International Hydrological Decade.]Google Scholar
Bentley, C. R. Seismic-wave velocities in anisotropic ice: a comparison of measured and calculated values in and around the deep drill hole at Byrd station, Antarctica. Journal of Geophysical Research, Vol. 77, No. 23, 1972, p. 440620. [Results of ultrasonic (28 kHz) velocity measurements carried out at depth of 1550 m in 1969–70.]Google Scholar
Berry, M. V. On deducing the form of surfaces from their diffracted echoes. Journal of Physics, A, Vol. 5, No. 2, 1972, p. 27291. [Theoretical explanation.]Google Scholar
Björnsson, H. Bægisárjökull, north-Iceland. Results of glaciological investigations 1967–1968. Part I. Mass balance and general meteorology. Jökull, Ár 21, 1971, [pub. 1972], p. 123. [Investigation of the water balance of a glacier-fed drainage area along with general meteorological and energy budget measurements on the glacier. Icelandic summary, p. 22–23.]Google Scholar
Boulton, G. S., and Vivian, R. Underneath the glaciers. Geographical Magazine, Vol. 45, No. 4, 1973, p. 31116. [Describes study of processes taking place beneath glaciers, with reference to activities in the subglacial laboratory beneath Glacier d’Argentière in France and to the behaviour of jökulhlaups in Iceland.]Google Scholar
Brewer, T. A two-year mass-balance study of the Rusty Glacier, 1968–1969. (In Bushnell, V. C., and Ragle, R. H., ed. Icefield Ranges Research Project. Scientific results. Vol. 3. New York, American Geographical Society; Montreal, Arctic Institute of North America, 1972, p. 7582.) [Summary of results.]Google Scholar
Broscoe, A. J. Some aspects of the geomorphology of meltwater streams, Steele Glacier terminus. (In Bushnell, V. C., and Ragle, R. H., ed. Icefield Ranges Research Project. Scientific results. Vol. 3. New York, American Geographical Society; Montreal, Arctic Institute of North America, 1972, p. 4751.) [Study of two channels flowing from Steele Glacier.]Google Scholar
Bucher, P., and Stauffer, B. Bore hole isotope studies at Byrd station, Antarctica. Antarctic Journal of the United States, Vol. 7, No. 4, 1972, p. 11011. [Describes sampling technique, 1971–72.]Google Scholar
Bushnell, V. C., and Ragle, R. H., ed. Icefield Ranges Research Project. Scientific results. Vol. 3. New York, American Geographical Society; Montreal, Arctic Institute of North America, 1972. ix, 261 p. [Some articles have been published previously; the others are listed separately.]Google Scholar
Capello, C. F. Il rilievo stereofotogrammetrico del ghiacciaio della Brenva. Bollettino del Ccmitato Glaciologico Italiano, Ser. 2, No. 19, 1971, p. 1730. [Describes stereophotogrammetric survey of this glacier in the Monte Bianco massif.]Google Scholar
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Icebergs. Sea, River and Lake Ice

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Klimovich, V. M. Kharakteristika torosov v pripaye [Characteristics of hummocks in fast ice]. Meteorologiya i Gidrologiya, 1972, No. 5, p. 8087. [Mathematical analysis. English abstract, p. 87.]Google Scholar
Kovacs, A., and Mellor, M. Investigation of ice islands in Babbage Bight. (In Canada. Dept. of Public Works. Engineering Programs Branch. Beaufort Sea storm. September 13–16 1970. Investigation of effects in the Mackenzie Delta region. [Ottawa], Dept. of Public Works, 1971, iv, [36] leaves.) [Presents findings on the geometry and structure of two grounded ice islands and information on the local bathymetry and sea ice cover.]Google Scholar
Kuzenkova, L. O. Izmeneniye solenosto vody pri obrazovanii l’da v melkovodnykh moryakh [Salinity variation of water during ice formation in shallow seas]. Meteorologiya i Gidrologiya, 1972, No. 5, p. 7579. [Method described takes into account the increase in salinity due to variation in the volume of water during ice formation. English abstract, p. 79.]Google Scholar
Kuznetsov, I. M., and Timerev, A. A. Izmeneniye al’bedo l’da v zavisimosti ot sostoyaniya yego poverkhnosti po izmereniyam s samoleta [Albedo changes in ice depending on its surface condition according to air observation]. Problemy Arktiki i Antarktiki, Vyp. 40, 1972, p. 7177. [Sea ice.]Google Scholar
Langleben, M. P. A study of the roughness parameters of sea ice from wind profiles. Journal of Geophysical Research, Vol. 77, No. 30, 1972, p. 593544. [Reports results of measurements of wind speed at five heights in geometric progression to a maximum of 4 m made in the Beaufort Sea for a three-week period in spring 1971 at the junction of two ice floes of differing surface morphology.]Google Scholar
Lebedev, A. A., and Uralov, N. S. O vozmozhnosti primeneniya sovremennykh teoreticheskikh skhem dlya rascheta vetrovogo dreyfa ledovoy kromki v yugo-vostochnoy chasti Barentseva morya [On the application of recent theoretical methods in calculating wind drift of the ice edge in the south-east part of the Barents Sea]. Gosudarstvennyy Okeanologicheskiy Institut. Leningradskoye Otdeleniye. Trudy, Vyp. 110, 1972, p. 13847.Google Scholar
Legen’kov, A. P., and Romanov, M. A. O podvizhkakh l’da v Arkticheskom basseyne [The shearing of drifting ice in the Arctic Basin]. Okeanologiya, 1972, No. 4, p. 61724. [Very slow and chaotic movement. English abstract, p. 624.]Google Scholar
Likhomanov, V. A., and Kheysin, D. Ye. Eksperimental’noye issledovaniye udara tverdogo tela o led [Experimental investigation of solid body impact on ice]. Problemy Arktiki i Antarktiki, Vyp. 38, 1971, p. 10511. [Experiments on fresh-water lake ice 1967–69.]Google Scholar
Lorrain, R. D., and Souchez, R. A. Sorption as a factor in the transport of major cations by meltwaters from an alpine glacier. Quaternary Research, Vol. 2, No. 2, 1972, p. 25356. [Results show that in melt water from the Glacier de Moiry, Switzerland, sorption of suspended sediments can be a significant factor in chemical transport.]Google Scholar
Losev, S. M. K metodike izucheniya prilivo-otlivnogo dreyfa l’da v pribrezhnoy zone s primeneniyem aerofotos”yemki [Methods of studying tidal ice drift in the coastal zone by aerial photography]. Problemy Arktiki i Antarktiki, Vyp. 40, 1972, p. 12427.Google Scholar
Loshchilov, V. S., and Voyevodin, V. A. Opredeleniye elementov dreyfa ledyanogo pokrova i peremeshcheniya kromki l’dov s pomoshchyu samoletnoy radiolokatsionnoy stantsii bokovogo obzora “Toros” [Determination of the drift elements of ice cover and ice edge movements by means of the airborne side-looking radar “Toros”]. Problemy Arktiki i Antarktiki, Vyp. 40, 1972, p. 2330. [Barents Sea.]Google Scholar
McClain, E. P. Special displays of satellite infrared data for sea ice monitoring. (In 4th annual earth resources program review. Vol. 4. National Oceanic and Atmospheric Administration programs and U.S. Naval Research Laboratory programs. Presented at the Manned Spacecraft Center, Houston, Texas, January 17 to 21, 1972. Houston, Texas, NASA Manned Spacecraft Center, 1972, p. 87-187-11.) [Describes sea ice surveillance by satellites, stressing importance of infra-red imagery.]Google Scholar
McDougall, H. The ice seekers. Canadian Geographical Journal, Vol. 85, No. 3, 1972, p. 8089. [Describes air reconnaissance and remote sensing techniques used to observe sea ice in the Canadian Arctic by the Atmospheric Environment Service of the Department of the Environment.]Google Scholar
Macintosh, N. A. Life cycle of Antarctic krill in relation to ice and water conditions. Discovery Reports, Vol. 35, 1972, p. 194. [ Includes section on sea ice limits, one aim being to improve on existing maps of these.]Google Scholar
Martin, S. Ice stalactites and the desalination of sea ice. Naval Research Reviews, Vol. 25, No. 9, 1972, p. 1726. [Discusses observations and formation of large ice stalactites (0.5–6.0 m in length) growing beneath Arctic and Antarctic pack ice, and their relation to the desalination of ice.]Google Scholar
Mills, D. A. On waves in a sea ice cover. Horace Lamb Centre for Oceanographical Research. School of Physical Sciences, Flinders University of South Australia. Research Paper No. 53, 1972, iii, [123] p. [Study of waves generated oil an ice-covered sea by travelling forcing effects.]Google Scholar
Mock, S. J., and others. Spatial aspects of pressure ridge statistics, [by] Mock, S. J., Hartwell, A. D. and Hibler III, W. D.. Journal of Geophysical Research, Vol. 77, No. 30, 1972, p. 594553. [Examined by a census of directional characteristics of all ridges in each of three small areas in the Arctic Basin.]Google Scholar
Mordasova, N. V., and Fedosov, M. V. ü soderzhanii khlorofilla i feofitina v vode i l’dakh Barentseva morya [On the chlorophyll and pheophytin content of the water and ice of the Barents Sea]. Trudy Vsesoyuznogo Nauchno-Issledovatel’skogo Instituta Morskogo Rybnogo Khozyaystva i Okeanografii, Tom 75, 1972, p. 8087. [English summary, p. 87.]Google Scholar
Oradovskiy, S. G. Izucheniye biogennogo khimicheskogo sostava l’dov Barentseva morya [Study of the composition of nutrients in the ice of the Barents Sea]. Trudy Vsesoyuznogo .Nauchno-lssledovatel’skogo Instituta Morskogo Rybnogo Khozyaystva i Okeanografii, Torn 75, 1972, p. 6573. [Results of analysis of mineral nutrients occurring at the drift ice edge, in ice, snow on ice floes, newly fallen snow and sea-water. English summary, p. 73.]Google Scholar
Oradovskiy, S. G., and Filonov, A. Ye. Nekotoryye dannyye po khimii l’dov i prilednykh vod severnogo Kaspiya [Certain data on the chemistry of ice and near-ice waters of the Caspian Sea]. Trudy Vsesoyuznogo Nauchno-Issledovatel’skogo Instituta Morskogo Rybnogo Khozyaystva i Okeanografii, Tom 75, 1972, p. 7479. [Analysis of mineral nutrients occurring at the ice edge, in the ice and in sea-water, which contribute to the photosynthesis of plants in the area. English summary, p. 79.]Google Scholar
Palmer, M. D., and Izatt, J. B. Lake movements with partial ice cover. Limnology and Oceanography, Vol. 17, No. 3, 1972, p. 40309. [Current meter data obtained every 10 min under a winter ice sheet on Lake Erie in 11 m of water at a depth of 3 m from the bottom. Results discussed.]Google Scholar
Parmentier, F. C. Picture of the month. Spring ice migration near Newfoundland. Monthly Weather Review, Vol. 100, No. 9, 1972, p. 69091. [Sequence of ESSA 8 photographs, showing changes in the ice along the north and east coasts of Newfoundland, 3–31 May 1972.]Google Scholar
Parmerter, R. R., and Coon, M. D. Model of pressure ridge formation in sea ice. Journal of Geophysical Research, Vol. 77, No. 33, 1972, p. 656575. [Presents a kinematic model of pressure-ridge formation in which the lateral and vertical motion of ice blocks is combined with a force balance and breaking stress calculation.]Google Scholar
Ruddiman, W. F., and Glover, L. K. Vertical mixing of ice-rafted volcanic ash in North Atlantic sediments. Geological Society of America. Bulletin, Vol. 83, No. 9, 1972, p. 281735. [Study of vertical mixing of silicic bubble-wall sand-sized volcanic shards, which are too big to be distributed by wind and so must be ice-rafted.)Google Scholar
Scott, W. D., and Levin, Z. Open channels in sea ice (leads) as ion sources. Science, Vol. 177, No. 4047, 1972, p. 42526. [Field experiments suggest that leads act as sources of atmospheric ions.]Google Scholar
Sinotin, V. I. Zatoroobrazovatel’nyye protsessy i ikh regulirovaniye v tselyakh bor’by s navodneniyami [Jamming processes and their regulation in the fight against flooding]. Gidrotekhnicheskoye Stroitel’stvo, 1972, No. 8, p. 2224. [Control of ice jams on Russian rivers, 1969–71.]Google Scholar
Smith, S. D. Wind stress and turbulence over a flat ice floe. Journal of Geophysical Research, Vol. 77, No. 21, 1972, p. 3886901. [Study of ice movement and pressure. Average drag coefficient is the same as that of the sea surface and about half that of moderately rough ice.]Google Scholar
Tabata, T. Hokkaidō-engan no ryūhyōya no yugami no sokutei [Measurements of strain of ice field off the [Okhotsk Sea] coast of Hokkaido]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971,p. 199211. [Marked effect of space and time. English summary, p. 211.]Google Scholar
Toksubayev, A. I. Razvitiye pripaya v pribrezhnoy zone zaliva Alasheyeva [Fast ice development in the coastal zone of Alasheyev Bight]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 83, 1972, p. 1216. [Near “Molodezhnaya” station, 1970.]Google Scholar
Urick, R. J. The noise of melting icebergs. Journal of the Acoustical Society of America, Vol. 50, No. 1, Pt. 1, 1971, p. 33741. [Noise may be caused by the explosion of tiny air bubbles entrapped in ice under pressure and released as melting occurs, or, at deep depths, by implosion of the cavities by inrushing water. Other factors are probably involved.]Google Scholar
Volkov, N. A., ed. Issledovaniye ledovogo rezhima Arkticheskikh morey i metody prognozov i raschetov [Study of the ice regime of Arctic seas and methods of forecasting and calculating]. Trudy Arkticheskogo i Antarkticheskogo Nauchno-Issledovatel’skogo Instituta, Tom 303, 1971, 211 p.Google Scholar
Weeks, W. F., and Assur, A. Fracture of lake and sea ice. (In Liebowitz, H., ed. Fracture: an advanced treatise. Vol. 7. New York and London, Academic Press, 1972, p. 879978.) [Chapter reviewing structure of ice and ice sheets and their fracture.]Google Scholar
Wilheit, T., and others. Aircraft measurements of microwave emission from Arctic sea ice, [by] Wilheit, T. and Nordberg, W., Blinn, J., Campbell, W. [J.] and Edgerton, A.. Remote Sensing of Environment, Vol. 2, No. 3, 1972, p. 12939. [The expected contrast in emissivities between ice and water was observed in all 8 wave-lengths tested (0.51 to 2.81 cm), and different forms of ice exhibited strong contrasts in emissivity; the more emissive ice is identified as more recent than the less emissive ice.]Google Scholar

Glacial geology

Anderson, J. B. Nearshore glacial-marine deposition from modern sediments of the Weddell Sea. .Nature, Physical Science, Vol. 240, No. 104, 1972, p. 18992. [Contrasting glacial and oceanographic conditions are reflected in the present sedimentologic and faunal distributions.]Google Scholar
Andrews, J. T. Recent and fossil growth rates of marine bivalves, Canadian Arctic, and Late-Quaternary Arctic marine environments. Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 11, No. 3, 1972, p. 15776. [Present-day growth rates of marine bivalves in Arctic and sub-Arctic waters were examined and results related to growth rates in fossil bivalves, and thus to Quaternary marine conditions.]Google Scholar
Andrews, J. T., and Miller, G. H. The Quarternary [sic] history of northern Cumberland Peninsula, east Baffin Island, N.W.T. Part 10. Radiocarbon date list. Arctic and Alpine Research, Vol. 4, No. 3, 1972, p. 26177. [Fifty-two radiocarbon dates are reported and sites, material and significance of deposits are discussed.]Google Scholar
Bardin, V. I., and Sudakova, N. G. Litologicheskiye osobennosti raznovozrastnykh moren v gorakh Zemli Korolevy Mod [Lithology of moraines of different ages in the mountains of Dronning Maud Land]. Informatsionnyy Byulleten’ Sovetskoy Antarkticheskoy Ekspeditsii, No. 83, 1972, p. 2530. [Study of moraines in Wohlthat Massivet, near Insel mountains.]Google Scholar
Barrett, P. J. Late Paleozoic glacial valley at Alligator Peak, southern Victoria Land, Antarctica. New Zealand Journal of Geology and Geophysics, Vol. 15, No. 2, 1972, p. 26268. [Describes geology and probable genesis of this valley, found in 1970–71.]Google Scholar
Behling, R. E. Pedological development on moraines of the Meserve Glacier, Antarctica. Dissertation Abstracts International, B, Vol. 32, No. 11, 1972, p. 6471-B72-B. [Sequence of glacial events suggested. Abstract of Ph.D. thesis, Ohio State University in cooperation with Miami (Ohio) University, 1971. University Microfilms order no 72-15173.]Google Scholar
Bergersen, O. F., and Garnes, K. Ice movements and till stratigraphy in the Gudbrandsdal area. Preliminary results. Norsk Geografisk Tidsskrift, Bd. 26, Ht. 1–2, 1972, p. 116. [Presents evidence suggesting that sub-till sediments in this area of Norway were deposited during an interstadial period before the last interglacial maximum.]Google Scholar
Birkeland, P. W. Late Quaternary eustatic sea-level changes along the Malibu coast, Los Angeles County, California. Journal of Geology, Vol. 80, No. 4, 1972, p. 43248. [Study of geomorphic features and marine and associated stream deposits.]Google Scholar
Borns, H. W., jr., and others. Mawson tillite, Victoria Land, east Antarctica: reinvestigation continued, [by] Borns, Jr., H. W., and Hall, B. A., Ball, H. W., Brooks., H. K. Antarctic Journal of the United States, Vol. 7, No. 4, 1972, p. 10607. [Origin and age of tillite studied by means of fossil remains.]Google Scholar
Boulton, G. S. Modern Arctic glaciers as depositional models for former ice sheets. Journal of the Geological Society (London), Vol. 128, Pt. 4, 1972, p. 36193. [Sedimentary sequences currently forming at the margins of Spitsbergen glaciers are identical in thickness and detail to many Pleistocene and earlier glacigenic sequences, and provide a more accurate model for the reconstruction of the structural characteristics 01 ancient ice margins than existing simple models. Discussion, p. 38893.]Google Scholar
Burrows, C. J. Post-Otiran moraines in Canterbury. Comment. New Zealand Journal of Geology and Geophysics, Vol. 15, No. 2, 1972, p. 29699. [Doubts that one of the samples from the Macauley site, described by Grant-Taylor and Rafter, ibid., Vol. 14, No. 2, 1971, p. 364402, records a glacial event. Further comment by A. C. Beck, p. 299.]Google Scholar
Carr, A. P. The unquiet landscape. Tide marks on the sands of time. Geographical Magazine, Vol. 45, No, 3, 1972, p. 20711. [Explains the types of changes of relative sea-level (tectonic, isostatic, eustatic) and discusses their implications.]Google Scholar
Church, M., and Ryder, J. M. Paraglacial sedimentation: a consideration of fluvial processes conditioned by glaciation. Geological Society of America. Bulletin, Vol. 83, No. 10, 1972, p. 305971. [Defines the term “paraglacial” and describes examples of paraglacial denudation and sedimentation from Baffin Island and British Columbia.]Google Scholar
Crowell, J. C., and Frakes, L. A. Late Paleozoic glaciation: part 5, Karroo Basin, South Africa. Geological Society of America. Bulletin, Vol. 83, No. 10, 1972, p. 2887912. [Representative exposures and stratigraphic sections from various regions were examined and are described and interpreted.]Google Scholar
Daniel, E. Some ridges formed in the open crevasses of a melting ice sheet in northern Sweden. Geologiska Föreningens i Stockholm Förhandlingar, Vol. 94, Pt. 3, No. 550, 1972, p. 45963. [Ridges thought to have been formed through accumulation of till or the sedimentation of glacio-fluvial material in open crevasses of a thin ice sheet.]Google Scholar
Derbyshire, E. Pleistocene glaciation of Tasmania: review and speculations. Australian Geographical Studies, Vol. 10, No. 1, 1971, p. 7994. [Detailed discussion of evidence.]Google Scholar
Derbyshire, E. A synoptic approach to the atmospheric circulation of the last glacial maximum in southeastern Australia. Palaeogeography, Palaeoclimatology, Palaeoecology, Vol. 10, Nos. 2–3, 1971, p. 10324. [The general circulation presents a simpler synoptic pattern in the middle latitudes of the southern hemisphere compared with the northern, so, in the last pleniglacial, it remained simpler and probably underwent a much smaller degree of change.]Google Scholar
Derbyshire, E., and Peterson, J. A. On the status and correlation of Pleistocene glacial episodes in south-eastern Australia. Search, Vol. 2, No. 8, 1971, p. 28588. [Present knowledge suggests that there is no evidence for more than one Pleistocene glaciation in Australia.]Google Scholar
Dilke, F. W. W., and Gough, D. O. The solar spoon. Nature, Vol. 240, No. 5379, 1972, p. 26264, 29394. [Suggests overstability causes the Sun’s core to mix every few hundred million years, inducing ice ages and temporarily depressing the solar neutrino flux.]CrossRefGoogle Scholar
Dingle, R. V. Buried tunnel valleys off the Northumberland coast, western North Sea. Geologie en Mijnbouw, Vol. 50, No. 5, 1971, p. 67986. [Concludes that hollows on north-western side of Dogger Bank were excavated by subglacial streams near the edge of the Weichselian ice sheet, which deposited the Dogger Bank moraine.]Google Scholar
Edelman, N. Meandrande glacialrännor. Terra, Vol. 84, No. 3, 1972, p. 10407. [Meandering channels on roches moutonnées are explained as the results of ice scouring in joints. English abstract, p. 104.]Google Scholar
Embleton, C., ed. Glaciers and glacial erosion. London and Basingstoke, Macmillan, [c 1972]. 287 p. (Geographical Readings.) [A selection of significant contributions to this aspect of glacial geomorphology published between 1842 and 1965.]Google Scholar
Fleck, R. J., and others. Chronology of late Pliocene and early Pleistocene glacial and magnetic events in southern Argentina, [by] Fleck, R. J., Mercer, J. H., Nairn, A. E. M. and Peterson., D. N. Earth and Planetary Science Letters, Vol. 16, No. 1, 1972, p. 1522. [Till interbedded with lava indicates at least four separate incursions of ice, the earliest prior to 2.06 million years ago.]Google Scholar
Fullerton, D. S. The Indian Castle glacial readvance in the Mohawk lowland, New York, and its regional implications (parts I and II). Dissertation Abstracts International, B, Vol. 32, No. 11, 1972, p. 6474-B. [Abstract of Ph.D. thesis, Princeton University, 1971. University Microfilms order no. 72-13741.]Google Scholar
Glückert, G., and Kontturi, O. On esker formations in Nousiainen, sw-Finland. Bulletin of the Geological Society of Finland, No. 44, Pt. 1, 1972, p. 17. [Reports investigation of the occurrence, material and genesis of radial and transverse esker-like glacio-fluvial formations.]Google Scholar
Goldthwait, R. P., ed. Till: a symposium. [Columbus], Ohio, Ohio State University Press, [c 1971]. xii, 402 p. [Some of the papers presented at the regional (North-Central) meetings of the Geological Society of America in Columbus, Ohio, on 15 and 16 May 1969.]Google Scholar
Grimmel, E. Geomorphologische Untersuchungen in der nordöstlichen Lüneburger Heide. Hamburger Geographische Studien, Ht. 27, 1971, [viii], 57 p. [Reviews earlier theories on the glaciogeomorphic development of this area and, on the basis of these, presents some alternative suggestions.]Google Scholar
Helm, D. G. Succession and sedimentation of glacigenic deposits at Hendre, Anglesey. Geological Journal (Liverpool), Vol. 7, Pt. 2, 1971, p. 27198. [Presents results of detailed investigation into fluvio-glacial sediments forming part of the Quaternary superficial deposits of Anglesey, North Wales.]Google Scholar
Hughes, O. L. Surficial geology of northern Yukon Territory and northwestern District of Mackenzie, Northwest Territories. Canada. Geological Survey. Paper 69-36, 1972, v, 11 p. [Includes discussion of extent and stages of Laurentide glaciation.]Google Scholar
Jaatinen, S. Preglaciala bergskittlar i åländsk rapakivi. Terra, Vol. 84, No. 3, 1972, p. 14351. [Describes appearance and discusses formation of pre-glacial potholes in the granite of the Ahvenanmaa (Åland) islands, Gulf of Bothnia. Suggests how they could have been preserved during glaciation. English summary, p. 150–51.]Google Scholar
Jackson, J. G., jr. Physical property and dynamic compressibility analysis of a glacial lake deposit. Dissertation Abstracts International, B, Vol. 32, No. 11, 1972, p. 6388-B. [Abstract of Ph.D. thesis, University of Michigan, 1971. University Microfilms order no. 72-14903.]Google Scholar
Jewtuchowicz, S. Glacjalne problemy plojstocenu a badania lodowców współczesnych [Some problems on Pleistocene glaciation as related to investigations on present-day glaciers]. Przegląd Geograficzny, Tom 44, Zeszyt 2, 1972, p. 195232. [Observations on dead ice, drainage of glaciers, and mode of glaciation, with examples from Arctic regions. Russian summary, p. 225–26, English summary, p. 227–32.]Google Scholar
Johansson, H. G. Moraine ridges and till stratigraphy in Västerbotten, northern Sweden. Sveriges Geologiska Undersökning, Avhandlingar och Uppsatser, Ser. C, Nr. 673, Årsbok 66, Nr. 4, 1972, 50 p. [Investigations show considerable variety in morphology, structure and texture of these ridges, and it is suggested that they are related to bedrock knobs.]Google Scholar
John, B. S. A late Weichselian kame terrace at Mullock Bridge, Pembrokeshire. Proceedings of the Geologists’ Association, Vol. 83, Pt. 2, 1972, p. 21329. [Probably formed during retreat of the Irish Sea ice at the end of the last glaciation of this area.]Google Scholar
Jungerius, P. D., and Wiggers, A. J. The effects of selective erosion by overland flow on the ice-pushed ridges of Uelsen (county Bentheim, Germany). Geologie en Mijnbouw, Vol. 50, No. 3, 1971, p. 42528. [Brief description and suggested formation.]Google Scholar
Kälin, M. Glaciology, No. 4. The active push moraine of the Thompson Glacier, Axel Heiberg Island, Canadian .Arctic Archipelago. Axel Heiberg Island Research Reports, McGill University, Montreal, 1971, iv, 68 p. [Detailed description of this representative example of the push moraines of the Canadian High Arctic.]Google Scholar
Kidson, C., and Haynes, J. R. Glaciation in the Somerset levels: the evidence of the Burtle Beds. Nature, Vol. 239, No. 5372, 1972, p. 39092. [Suggests that these sands and gravels are of marine origin, not glacial.]Google Scholar
Kvasov, D. D. Postulate einer Eiszeit-Theorie. Eiszeitalter und Gegenwart, Bd. 22, 1971, p. 17887. [Theory of cause of ice ages, based on importance of fluctuations in sea-level, and circulation, thermal and ice regime of the oceans.]Google Scholar
McDonald, B. C., and Vincent, J. S. Fluvial sedimentary structures formed experimentally in a pipe, and their implications for interpretation of subglacial sedimentary environments. Canada. Geological Survey. Paper 72-27, 1972, vi, 30 p. [Describes experiments and discusses factors affecting deposition of sediments of glacier tunnels, extending relationships to processes of esker sedimentation.]Google Scholar
Mansikkaniemi, H. Saven peittämä harju Paimionjokilaaksossa [A clay-covered esker in the Paimionjoki valley]. Terra, Vol. 84, No. 3, 1972, p. 10814. [Describes an esker covered by varved clay, and suggests it was deposited in deep water at the mouth of a stream flowing within or on the continental ice. English summary, p. 114.]Google Scholar
Mayewski, P. A. Glacial geology near McMurdo Sound and comparison with the central Transantarctic Mountains. Antarctic Journal of the United States, Vol. 7, No. 4, 1972, p. 10306. [Presents results of 1970–71 and 1971–72 seasons, with particularly interest in the so-called Sirius Formation.]Google Scholar
Mercer, J. H. The lower boundary of the Holocene. Quaternary Research, Vol. 2, No. 1, 1972, p. 1524. [Plea for a globally relevant definition, not merely one based on a European climatic sequence.]Google Scholar
Miller, J. W., jr. Variations in New York drumlins. Annals of the Association of American Geographers, Vol. 62, No. 3, 1972, p. 41823. [Describes and discusses significance of differences between drumlins in three east-to-west belts in west-central New York State.]Google Scholar
Möller, J. J., and Sollid, J. L. Deglaciation chronology of Lofoten–Vesterålen–Ofoten, north Norway. Norsk Geografisk Tidsskrift, Bd. 26, Ht. 3, 1972, p. 10133. [Seven stages in ice recession traced from study of regional shore displacement.]Google Scholar
Niemelä, J. Die quartäre Stratigraphie von Tonablagerungen und der Rückzug des Inlandeises zwischen Helsinki und Hämeenlinna in Südfinnland. Finland. Geological Suvey. Bulletin 253, 1971, 79 p. [Observations on the effects and movement of the Quaternary ice sheet in this pari of Finland.]Google Scholar
Nogami, M. Andesu-sanmyaku ni okeru genzai oyobi hyōki no sessen-kōdo no bunpu kara mita hyōki no kikō [The climate of the [last] glacial period as seen in the distribution of snow-line heights in the present day and the glacial period in the Andes range]. Dai-yonki Kenkyū: Quaternary Research, Vol. 11, No. 2, 1972, p. 7181. [English abstract, p. 71.]Google Scholar
Okko, M. Jäätikon häviämistapa Toisen Salpausselän Lammilla [Deglaciation in the Second Salpausselkä ice-marginal belt at Lammi]. Terra, Vol. 84, No. 3, 1972, p. 11523. [South Finland. English summary, p. 123].Google Scholar
Parmuzin, Yu. P. Genezis kamov [The origin of kames]. Vestnik Moskovskogo Universiteta, Ser. 5, 27 God, No. 3, 1972, p. 4349. [New theory. English summary, p. 49.]Google Scholar
Peterson, J. A., and Hope, G. S. Lower limit and maximum age for the last major advance of the Carstensz glaciers, West Irian. Nature, Vol. 240, No. 5375, 1972, p. 3637. [Discusses implications of finding that a major advance took place with a glacier reaching 3 500 m less than 11 300 years ago and extending to 1 700 m less than 10 000 years ago, with a length of about 15 km. Western New Guinea.]Google Scholar
Pheasant, D. R. The glacial chronology and glacio-isostasy of the Narpaing–Quajon fiord area, Cumberland Fiord area, Baffin Island. Dissertation Abstracts International, B, Vol. 32, No. 12,Pt. 1, 1972, p. 7118-B. [Abstract of Ph.D. thesis, University of Colorado, 1971. University Microfilms order no. 72-17295.]Google Scholar
Price, R. J., and Sugden, D. E., comp. Polar geomorphology. London, Institute of British Geographers, 1972. v, 215 p. (Institute of British Geographers. Special Publication No. 4.) [Contains the following papers: G. S. Boulton, “The role of thermal régime in glacial sedimentation”, p. 1–19; R. Hope, H. Lister and R. Whitehouse, “The wear of sandstone by cold, sliding ice”, p. 21–31; S. Funder, “Deglaciation of the Scoresby Sund fjord region, north-east Greenland”, p. 33–42 ; D. J. Drewry, “The contribution of radio echo sounding to the investigation of Cenozoic tectonics and glaciation in Antarctica”, p. 43–57; W. E. LeMasurier, “Volcanic record of Antarctic glacial history: implications with regard to Cenozoic sea levels”, p. 59–74; B. S. John, “Evidence from the South Shetland Islands towards a glacial history of west Antarctica”, p. 75–92; E. Derbyshire, “Tors, rock weathering and climate in southern Victoria Land, Antarctica”, p. 93–105; B. A. Kennedy and M. A. Melton, “Valley asymmetry and slope forms of a permafrost area in the Northwest Territories, Canada”, p. 107–21; D. Gill, “Modification of levee morphology by erosion in the Mackenzie River delta, Northwest Territories, Canada”, p. 123–38; P. J. Howarth and J. G. Bones, “Relationships between process and geometrical form on high Arctic debris slopes, south-west Devon Island, Canada”, p. 139–53; C. Harris, “Processes of soil movement in turf-banked solifluction lobes, Okstindan, northern Norway”, p. 155–74; S. B. McCann and R. J. Carlisle, “The nature of the ice-foot on the beaches of Radstock Bay, south-west Devon Island, N.W.T., Canada”, p. 175–86; D. I. Smith, “The solution of limestone in an Arctic environment”, p. 187–200; J. G. Cogley, “Processes of solution in an Arctic limestone terrain”, p. 201–11.]Google Scholar
Romanovskiy, N. N., and others. Kaynozoyskiye otlozheniya mezhgornoy Uyandinskoy vpadiny i ikh kriogennoye stroyeniye [Cainozoic beds of the Uyandina lowland and their cryogenic structure]. [By] Romanovskiy, N. N., Kaplina, T. N., Kondrat’yeva, K. A., Rybakova, N. O., Pirumova., L. G. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 8095. [Yano-Indigirka interfluve, Yakutskaya A.S.S.R.]Google Scholar
Rutter, N. W. Geomorphology and multiple glaciation in the area of Banff, Alberta. Canada. Geological Survey. Bulletin 206, 1972, [x], 54 p. [Describes glacial deposits and outlines sequence of events of Pleistocene glaciation, with reference to present-day processes of erosion and deposition.]Google Scholar
Saint-Onge, D.-A. Sequence of glacial lakes in north-central Alberta. Canada. Geological Survey. Bulletin 213, 1972, ix, 16 p. [Evidence suggests that deglaciation was rapid in this area and that vegetation took hold shortly afterwards or even on top of the debris-covered ice. Periglacial processes were probably not important in shaping the landscape.]Google Scholar
Savage, N. M. Soft-sediment glacial grooving of Dwyka age in South Africa. Journal of Sedimentary Petrology, Vol. 42, No. 2, 1972, p. 30708. [Presents evidence to show that grooves previously described as glacial striations in sandstone are soft-sediment grooves in a thin veneer of periglacial sandstone.]Google Scholar
Schaffel, S. Reconstruction of late-glacial and post-glacial events in Long Island Sound, New York. Dissertation Abstracts International, B, Vol. 32, No. 11, 1972, p. 6479-B. [Information from analyses of pollen, diatoms and sediments from cores. Abstract of Ph.D. thesis, New York University, 1971. University Microfilms order no. 72-13399.]Google Scholar
Sharp, R. P. Pleistocene glaciation, Bridgeport basin, California. Geological Society of America. Bulletin, Vol. 83, No. 8, 1972, p. 223360. [Conclusions drawn from detailed investigation and mapping of deposits.]Google Scholar
Shaw, J. Sedimentation in the ice-contact environment, with examples from Shropshire (England). Sedimentology, Vol. 18, Nos. 12, 1972, p. 2362. [Describes and interprets internal structure of landforms at three sites in the Shrewsbury area.]Google Scholar
Siedlecka, A., and Roberts, D. A late Precambrian tilloid from Varangerhalvøya—evidence of both glaciation and subaqueous mass movement. Norsk Geologisk Tidsskrift, Vol. 52, No. 2, 1972, p. 13541. [Although some features suggest that subaqueous mass movement was responsible for deposition, other criteria do not exclude a glacial affinity, and these are discussed along with evidence from other Precambrian regions.]Google Scholar
Sinn, P. Zur Ausdehnung der Donau-Vergletscherung im schwäbischen Alpenvorland. Eiszeitalter und Gegenwart, Bd. 22, 1971, p. 18891. [Suggests that the Donau glaciation in Schwaben, West Germany, was not as extensive as previously thought.]Google Scholar
Soyez, D. Geomorfologisk kartering av nordvästra Dalarna jämte försök till värdering av terrängformerna för naturvårdssyften. Stockholms Universitet. Naturgeografiska Institutionen. Forskningsrapport 11, 1971, vii, 130 leaves+errata slip. [Geomorphological mapping of north-western Dalarna, Sweden, by air photo interpretation. Several landforms are described and their genesis discussed. English summary, 1. 109–12.]Google Scholar
Strömberg, B. Glacial striae in southern Hinlopenstretet and Kong Karls Land, Svalbard. Geograjiska Annaler, Vol. 54a, No. 2, 1972, p. 5365. [Presence or absence of glacial striae enable conclusions to be made about previous glaciations.]Google Scholar
Strömberg, B. Isrecessionen i området kring Ålands hav. Stockholms Universitet. Naturgeografiska Institutionen. Forskningsrapport 10, 1971, [171] leaves + errata slip. [Discusses Quaternary deglaciation of the area around the Ahvenanmaa (Åland) islands, Gulf of Bothnia, on the basis of investigations of varves and glacial striae on the islands and in north-eastern Uppland, Sweden. English summary, 1. 142–47.]Google Scholar
Ten Brink, N. W. Holocene deleveling and glacial history between Søndre Strømfjord and the Greenland ice sheet, west Greenland. Dissertation Abstracts International, B, Vol. 32, No. 11, 1972, p. 6479-B80-B [Discusses sequence of events. Abstract of Ph.D. thesis, University of Washington, 1972. University Microfilms order no. 72-15151.]Google Scholar
Trompette, R. Présence, dans le bassin voltaïen, de deux glaciations distinctes à la limite Précambrien supérieur–Cambrien. Incidences sur l’interprétation chronostratigraphique des séries de bordure du craton ouest-africain. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Sér. D, Tom. 275, No. 10, 1972, p. 102730. [Evidence from stratigraphic studies.]Google Scholar
Walcott, R. I. Past sea levels, eustasy and deformation of the Earth. Quaternary Research, Vol. 2, No. 1, 1972, p. 114. [Discussion.]Google Scholar
Weber, W. M. Correlation of Pleistocene glaciation in the Bitterroot Range, Montana, with fluctuations of glacial Lake Missoula. Dissertation Abstracts International, B, Vol. 32, No. 5, 1971, p. 2804-B05-B. [Reports evidence of three major Pleistocene glaciations and nine cycles of Lake Missoula. Abstract of Ph.D. thesis, University of Washington, 1971. University Microfilms order no. 71-28490.]Google Scholar
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Winterhalter, B. On the geology of the Bothnian Sea, an epeiric sea that has undergone Pleistocene glaciation. Finland. Geological Survey. Bulletin 258, 1972, 66 p. [Study of the glacial morphology of the sea bottom.]Google Scholar
Zamoruyev, V. V. Osobennosti chetvertichnogo oledeneniya khrebta Kodar [Peculiarities of Quaternary glaciation of the Kodar mountain range]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 104, Vyp. 5, 1972, p. 38588.Google Scholar

Frost Action on Rocks and Soil. Frozen Ground. Permafrost

Aartolahti, T. Dyynien routahalkeamista ja routahalkeamapolygoneista [Frost cracks and frost-crack polygons on dunes in Finland]. Terra, Vol. 84, No. 3, 1972, p. 12430. [Study of three localities. English summary, p. 13031.]Google Scholar
Afanasenko, V. Ye. Nekotoryye osobennosti vodonosnykh dolinnykh talikov zapadnykh otrogov Zolotogo khrebta [Some features of water-bearing tabetisols of the western arm of the Zolotoy mountain range]. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 15363. [Unfrozen layers in permafrost in the northern part of the Anadyr depression, Kamchatskaya Oblast’.]Google Scholar
Anderson, D. M., and others. An Antarctic analog of Martian permafrost terrain, [by] Anderson, D. M. and Gatto, L. W., Ugolini., F. C. Antarctic Journal of the United States, Vol. 7, No. 4, 1972, p. 11416. [Study of Beacon Valley, southern Victoria Land.]Google Scholar
Bogdanets, Yu. I. O vliyanii rastitel’nogo pokrova na tempy ottaivaniya merzlykh porod [On the influence of vegetation cover on the speed at which frozen rocks thaw]. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 22326. [Thawing of the active layer at Salekhard, Omskaya Oblast’.]Google Scholar
Boyarskiy, O. G., and Maksimova, L. N. O “pereletkakh” i kratkovremenno sushchestvuyushchikh mnogoletnemerzlykh prodakh [On intergelisols and temporarily frozen rocks]. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 19397. [Study showing connection between climatic variations and length of existence of temporarily frozen layers, Patomskoye Nagor’ye, Irkutskaya Oblast’.]Google Scholar
Brochu, M. Une nouvelle forme périglaciaire: les cavités emboitées de l’argile (éxtremité nord-est du lac Hazen, île d’Ellesmère). Polarforschung, 42. Jahrg., Nr. 1, 1972, p. 3134. [Describes double cavities (8–25 cm diameter and 15–57 cm depth) found in clay and suggests how periglacial conditions may cause their development.]Google Scholar
Cailleux, A. Fentes minces et dépôts chimiques secondaires en Iakoutie et au nord de Moscou. Biuletyn Peryglacjalny, No. 21, 1972, p. 2131. [Periglacial features.]Google Scholar
Cary, J. W., and Mayland, H. F. Salt and water movement in unsaturated frozen soil. Soil Science Society of America. Proceedings, Vol. 36, No. 4, 1972, p. 54955. [Evaluates relative effects of possible transport systems and suggests appropriate flow equations.]Google Scholar
Danilova, N. S. Nekotoryye osobennosti kriogennogo stroyeniya drevnego poymennogo allyuviya krupnykh rek zapadnoy Yakutii [Some features of the cryogenic structure of ancient flood-plain alluvium of the large rivers of western Yakutiya]. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 12936.Google Scholar
Dubikov, G. N. Vozmozhnyye osadki pri protaivanii mnogoletnemerzlykh rykhlykh otlozheniy Zapadnoy Sibiri [Possible settlement following thawing of permanently frozen friable deposits in Western Siberia]. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 22022. [Study of depth of thawing as aid to construction in permafrost areas.]Google Scholar
Fahey, B. D. A quantitative analysis of freeze-thaw cycles, frost heave cycles, and frost penetration in the Front Range of the Rocky Mountains, Colorado. Dissertation Abstracts International, B, Vol. 32, No. 12, Pt. 1, 1972, p. 7106-B, [Abstract of Ph.D. thesis, University of Colorado, 1971. University Microfilms order no. 72-17257.]Google Scholar
Fukuda, M. Ganseki-nai no mizu no ryōketsu—yūkai ni tsuite (johō) [Freezing-thawing process of water in pore space of rocks (preliminary report)]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 22529. [By measuring elastic wave velocity and electrical resistance of porous rocks, both of which change suddenly when water in the rock freezes, it was found that water in the rocks usually froze at −4° C, depending on the water content and the porosity of the rocks. English summary, p. 229.]Google Scholar
Garagulya, L. S., and others. O formirovanii mnogoletnemerzlykh porod v usloviyakh poymy nizhnego Yeniseya (rayon g. Dudinki) [On formation of permafrost in the floodlands of the lower course of the Yenisey (Dudinka region)]. [By] Garagulya, L. S., Gordeyeva, G. I., Poltev, N. F., Smirnov, V. V., Bogolyubov., A. N. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 2733. [Three types of permafrost distinguished.]Google Scholar
Garagulya, L. S., and others. Vliyaniye geologo-geograficheskikh faktorov na temperaturnyy rezhim porod sloya sezonnogo protaivaniya v severnoy chasti Yano-Indigirskogo mezhdurech’ya [Influence of geological and geographical factors on the temperature regime of rocks of the seasonally thawing layer in the Yano-Indigirka interfluve]. [By] Garagulya, L. S., Kudryatsev, V. A., Kondrat’yeva, K. A., Maksimova., L. N. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 5979. [Yakutskaya A.S.S.R.]Google Scholar
Gavrilov, A. V. Nekotoryye osobennosti kartograficheskogo isobrazheniya na merzlotnykh kartakh masshtabov 1 : 200000 i 1 : 500000 [Some features of cartographic representation on maps showing permafrost on scales of 1 : 200000 and 1 : 500000]. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 23744. [Selection and representation of permafrost, geological and hydrological features on Soviet maps.]Google Scholar
Harris, A. R. Infiltration rate as affected by soil freezing under three cover types. Soil Science Society of America. Proceedings, Vol. 36, No. 3, 1972, p. 48992. [Restricted infiltration in frozen soil may cause spring floods; a coniferous plantation contributed more surface run-off during snow melt and rain than did deciduous forest or abandoned fields.]Google Scholar
James, P. The unquiet landscape. Land under refrigeration. Geographical Magazine, Vol. 44, No. 12, 1972, p. 85357. [Periglacial phenomena.]Google Scholar
Kaplina, T. N. Kriogennoye stroyeniye otlozheniy krutykh sklonov v surovykh merzlotnykh usloviyakh [Cryogenic structure of steep slope deposits in severe permafrost conditions]. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 10513. [Selennyakh valley, Yakutskaya A.S.S.R.]Google Scholar
Kaplina, T. N., and others. Proyavleniye noveyshikh tektonicheskikh dvizheniy v kriogennom stroyenii epigeneticheski promerzshikh porod [The appearance of new tectonic movements in the cryogenic structure of epigenetically frozen rocks]. [By] Kaplina, T. N., Kondrat’yeva, K. A., Romanovskiy., N. N. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 96104. [Yano-Indigirka interfluve, Yakutskaya A.S.S.R.]Google Scholar
Kinosita, S., and others. Ryōjō to chiki-suii to no kankei. III [Relation between water level and frost heaving. III]. [By] Kinosita, S., Suzuki, Y., Horiguchi, K. [and] Tanuma., K. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 24556. [Observations of frost heaving in two water-resistant basins, one containing sandy clayish loam and the other containing clay. English summary, p. 25556.]Google Scholar
Klitten, K., and Oleson, O. B. Geoelektriske resistivitetsmålinger ved permafrostundersøgelser i Holsteinsborg, Grønland. Grønlands Geologiske Undersøgelse. Rapport Nr. 47, 1972, 24 p. [Geoelectrical soundings indicated higher resistivity in areas with supposed permafrost. English summary, p. 2223.]Google Scholar
Lougeay, R. Patterns of surface temperature in the alpine/periglacial environment as determined by radiometric measurements. (In Bushnell, V. C., and Ragle, R. H., ed. Icefield Ranges Research Project. Scientific results. Vol. 3. New York, American Geographical Society; Montreal, Arctic Institute of North America, 1972, p. 16376.) [Describes observations conducted in the St. Elias Mountains to determine some aspects of the applicability of thermal remote sensing in this type of environment.]Google Scholar
Mackay, J. R. Offshore permafrost and ground ice, southern Beaufort Sea, Canada. Canadian Journal of Earth Sciences, Vol. 9, No. 11, 1972, p. 155061. [Discusses distribution and origin. Permafrost in thermal equilibrium with negative sea bottom temperatures may be distinguished from that not in equilibrium with either positive or negative sea bottom temperatures.]Google Scholar
Mackay, J. R. The world of underground ice. Annals of the Association of American Geographers, Vol. 62, No. 1, 1972, p. 122. [Detailed description of the various forms illustrated by examples from N.W.T., Canada.]Google Scholar
Mackay, J. R., and others. Relic Pleistocene permafrost, western Arctic, Canada, [by] Mackay, J. R. Rampton, V. N. [and] Fyles., J. G. Science, Vol. 176, No. 4041, 1972, p. 132123. [Icy layers and interbedded frozen sediments along the Arctic coastal plain of north-western Canada have been subjected to glacial deformation. Radiocarbon dates indicate that this took place more than 40000 years ago.]Google Scholar
McSaveney, E. R., and McSaveney, M. J. Ancient ice wedges in Wright Valley, Antarctica. Antarctic Journal of the United States, Vol. 7, No. 4, 1972, p. 10203. [Describes three complete ice wedge sections along the south bank of Onyx River.]Google Scholar
Morris, E. C., and others. Mars analog studies in Wright and Victoria valleys, Antarctica, [by] Morris, E. C. and Holt, H. E., Mutch, T. A., Lindsay., J. F Antarctic Journal of the United States, Vol. 7, No. 4, 1972, p. 11314. [Photographs of geomorphic features caused by cold and wind in these valleys will be compared with photographs returned from the “Viking” Mars mission in 1976.]Google Scholar
Nakano, Y., and others. Ultrasonic velocities of the dilatational and shear waves in frozen soils, [by] Nakano, Y Martin III, R. J. and Smith., M. Water Resources Research, Vol. 8, No. 4, 1972, p. 102430. [Shear wave velocity tended to decrease with ascending temperature, but the effect was greater on the dilatational velocity.]Google Scholar
Nogawa, K., and others. Tokachi Heiya ni okeru kōki kyōsekisei no shūhyōka genshō to sono sōjun (1) [On the late Pleistocene periglacial phenomena and their stratigraphical positions in the Tokachi plain, [Hokkaido] (1)]. [By] Nogawa, K., Kosaka, T. and Matsui., M. Dai-yonki Kenkyū: Quaternary Research, Vol. 11, No. 1, 1972, p. 113. [Five distinct phases from the Quaternary glaciation were recognized. English abstract, p. 1.]Google Scholar
Penner, E. Soil moisture redistribution by ice lensing in freezing soils. Canada. National Research Council. Division of Building Research. Technical Paper No. 371, 1972, [20] p. [Review of present knowledge. Reprinted from the proceedings of the 17th annual meeting of the Canadian Society of Soil Science, held at Lethbridge, Alberta, 4–8 July 1971, p. 4462.]Google Scholar
Piirola, J. Pohjois-Suomen kuviomaista [Patterned ground in northern Finland]. Terra, Vol. 84, No. 3, 1972, p. 13242. [Observations in Finnish Lapland. English summary, p. 14142.]Google Scholar
Potter, N., jr. Ice-cored rock glacier, Galena Creek, northern Absaroka Mountains, Wyoming. Geological Society of America. Bulletin, Vol. 83, No. 10, 1972, p. 302557. [Describes features, considers origin of surficial features, infers internal composition from pit studies and from mechanisms by which ice and debris are supplied to it, and examines problem of mass balance of both ice and debris.]Google Scholar
Pustovoytov, N. D. Sezonno-merzlotnyye pochvy i ikh melioratsiya [Seasonally frozen soils and their improvement]. Moscow, Izdatel’stvo “Nauka”, 1971. 231 p. [Detailed study of seasonally frozen soils, particularly in Soviet Far East, with indications of their potential value.]Google Scholar
Rampton, V. N., and Mackay, J. R. Massive ice and icy sediments throughout the Tuktoyaktuk peninsula, Richards Island, and nearby areas, District of Mackenzie. Canada. Geological Survey. Paper 71-21, 1971, vi, 16 p. [Describes extent of these features and where examples that are easily accessible for examination may be found.]Google Scholar
Romanovskiy, N. N. Vliyaniye temperaturnogo rezhima gornykh porod na morozoboynoye treshchinoobrazovaniye i razvitiye poligonal’no-zhil’nykh form [Influence of the temperature regime of rocks on frost cleft jointing and development of polygon veined forms]. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 16492.Google Scholar
Romanovskiy, N. N., and others. Merzlotnyye i gidrogeologicheskiye osobennosti rayona Deputatskogo rudnogo uzla (Permafrost and hydrogeological features of the Deputatskiy ore region]. [By] Romanovskiy, N. N., Kondrat’yeva, K. A., Kudryavtsev, V. A., Afanasenko, V. Ye., Volkova., V. P. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 3458. [Yano-Indigirka interfluve, Yakutskaya A.S.S.R.]Google Scholar
Seppälä, M. Location, morphology and orientation of inland dunes in northern Sweden. Geografiska Annaler, Vol. 54A, No. 2, 1972, p. 85104. [Ancient wind directions may be deduced from an aerial study of these periglacial features.]Google Scholar
Tanuma, K. Dannetsuzai maisetsu ga ryōketsu shinkō ni oyobosu eikyō. II [Effect of thermal insulating on frost penetration. II]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 23944. [Though the effect of thermal insulators was evident, the relative effectiveness of their various depths and thicknesses was not clear. English summary, p. 244.]Google Scholar
Tanuma, K. Ryōjō no sai no suibun idō to chichū netsu ryūryō no suketei [Measurements of water displacement and heat flow during frost heaving]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 23137. [Presents results of a study of the heat balance in a soil layer between 20 and 100 cm depth for a given time interval. English summary, p. 23637.]Google Scholar
Tomirdiaro, S. V. Podzemnoye oledeneniye Vostochnoy Sibiri [Eastern Siberia’s underground glaciation]. Priroda, 1972, No. 7, p. 8491. [Describes occurrence of permafrost in the lowlands.]Google Scholar
Tricart, J., and others. Cônes rocheux, pédiments, glacis, par Tricart, J., Raynal, R., Besançon., J. Annales de Géographie, 81 e An., No. 443, 1972, p. 124. [Discusses terminology and formation of these features.]Google Scholar
Ugolini, F. C., and Anderson, D. M. Ionic migration in frozen Antarctic soil. Antarctic Journal of the United States, Vol. 7, No. 4, 1972, p. 11213. [Evidence suggests that ionic migration takes place, assisted by liquid films of water surrounding the minerals.]Google Scholar
Volkova, V. P., and Romanovskiy, N. N. Nekotoryye osobennosti khimicheskogo sostava podzemnykh l’dov Uyandinskoy vpadiny i prilegayushchikh chastey Selennyakhskogo khrebta [Some features of the chemical composition of underground ice in the Uyandina lowland and adjoining parts of the Selennyakh mountain range]. Merzlotnyye Issledovaniya, Vyp. 10, 1970, p. 11428. [Yano-Indigirka interfluve, Yakutskaya A.S.S.R.]Google Scholar
Watson, E. Pingos of Cardiganshire and the latest ice limit. Nature, Vol. 236, No. 5346, 1972, p. 34344. [Contribution to argument about the extent of the most recent glaciation in south-west Wales.]Google Scholar
Webb, R. Vegetation cover on Icelandic thúfur. Acta Botanica Islandica, 1, 1972, p. 5160. [Describes development of thúfur, defined as vegetation-covered mineral-cored mounds, with diameter 0.5–2.0 m and height 0.25–0.5 m, created by frost action.]Google Scholar

Meteorological and Climatological Glaciology

Barry, R. G. The summer flux-divergence of atmospheric water over the Queen Elizabeth Islands, N.W.T. McGill University. Dept. of Meteorology. Arctic Meteorology Research Group. Publication in Meteorology No. 104, 1972, 24 p. [Includes examination of possible relationship between atmospheric moisture conditions and present distribution of snow and ice.]Google Scholar
Charlton, R. B., and List, R. Hail size distributions and accumulation zones. Journal of the Atmospheric Sciences, Vol. 29, No. 6, 1972, p. 118293. [Theory of growth of hail in a cloud.]Google Scholar
Friedman, I., and Smith, G. I. Deuterium content of snow as an index to winter climate in the Sierra Nevada area. Science, Vol. 176, No. 4036, 1972, p. 79093. [Higher snowfall in 1968–69 had depleted D content. This is associated with changed air-mass trajectory.]Google Scholar
Ishikawa, N. Tōki ni okeru bonchi-reikyaku no kansoku [Observations of basin cooling in winter]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 11523. [Meteorological measurements at two stations in Teshio mountainous region, north Hokkaido, one on mountain top, the other in a basin, show lower station to have lower temperatures. Reasons discussed. English summary, p. 12223.]Google Scholar
Kikuchi, K. Sintering phenomenon of frozen cloud particles observed at Syowa station, Antarctica. Journal of the Meteorological Society of Japan, Vol. 50, No. 2, 1972, p. 13135. [Measurement of the rate of growth of the ice neck between sintered frozen cloud particles led to the conclusion that sintering was caused by volume diffusion and plastic or viscous flow as well as evaporation-condensation.]Google Scholar
Kline, D. B. Measurements of ice nucleus and associated chloride particle concentrations at Mauna Loa Observatory. Journal of Applied Meteorology, Vol. 11, No. 4, 1972, p. 68487. [Measurements show pronounced relation to flow regime of atmosphere.]Google Scholar
McCormick, G. Estimation of design freezing indices. Transportation Engineering Journal of ASCE. Proceedings of the American Society of Civil Engineers, Vol. 97, No. TE3, 1971, p. 40109. [An estimate was obtained for places in Alberta, Saskatchewan and Manitoba, based on mean annual temperature.]Google Scholar
Mason, B. J. The physics of the thunderstorm. Proceedings of the Royal Society of London, Ser. A, Vol. 237, No. 1571, 1972, p. 43366. [Discusses mechanisms by which electric charge may be generated and separated within clouds, including melting of snow, freezing of supercooled droplets and collisions between ice crystals and water droplets.]Google Scholar
Mizuno, Y. Shimo no kesshō hōi [Crystallographic orientations of hoarfrost crystals]. Teion-kagaku : Low Temperature Science, Ser. A, [No.] 29, 1971, p. 2936, 2 plates. [X-ray Laue photographs used to determine crystal orientations of hoarfrost crystals of various shapes on cold-room pipes. English summary, p. 3536.]Google Scholar
Moran, J. M. An analysis of periglacial climatic indicators of late Glacial time in North America. Dissertation Abstracts International, B, Vol. 32, No. 12, Pt. 1, 1972, p. 7231-B. [Winters were probably milder than at present and summers cooler. Abstract of Ph.D. thesis, University of Wisconsin, 1972. University Microfilms order no. 72-15373.]Google Scholar
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Snow

Aburakawa, H., and Magono, C. Temperature dependency of crystallographic orientation of spatial branches of snow crystals. Journal of the Meteorological Society of Japan, Vol. 50, No. 3, 1972, p. 16669. [Presents evidence to show that the angle of spatial branches to the basal ice plate is not only determined by the lattice misfit of ice crystals, but is affected by temperature.]Google Scholar
Ageta, Y. Nankyoku no shamen-kakō-fūiki ni okeru sasutsurugi ya dorifuto no shokō ni tsuite [Some aspects of ablation of sastrugi and drifts in the area subjected to katabatic winds in Antarctica]. Nankyoku Shiryō: Antarctic Record, No. 43, 1972, p. 819. [Seasonal variations. English summary, p. 89.]Google Scholar
Akitaya, E., and Kawada, K. Shamen sekisetsu no kyodō no kenkyū. II—hen-i, yugami, teimen suberi [Studies of the behaviour of snow cover on slopes. II—displacements, strains, glides]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 13549. [English summary, p. 14749.]Google Scholar
Akitaya, E., and Kawada, K. Yōtei-san ni okeru seppō no deburi chōsa [Studies ot the debris of an avalanche on Mt. Yōtei, 1970]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 27175.Google Scholar
Ambach, W., and Denoth, A. Frequenzganz und Relaxationszeiten der Dielektrizitätskonstante von Schneeproben nach dem Modell von Cole-Cole. Acta Physica Austriaca, Bd. 35, Ht. 3, 1972, p. 24961. [Dielectric behaviour of dry, wet, new and old snows. New snow has a range of relaxation times; old snow follows a single relaxation spectrum. D.C. conductivity predominates below 50 kHz.]Google Scholar
Barica, J., and Armstrong, F. A. J. Contribution by snow to the nutrient budget of some small northwest Ontario lakes. Limnology and Oceanography, Vol. 16,No. 6, 1971, p. 89199. [61%–92% of nutrients came from snowfall and the remainder from lake water by seepage through ice and refreezing.]Google Scholar
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Bones, J. Meltwater runoff within talus cones on Devon Island, N.W.T., Canada. Canadian Geographer, Vol. 16, No. 1, 1972, p. 6975. [Attempt to monitor pattern and rates of flow.]Google Scholar
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Brown, C. B., and others. Slab avalanching and the state of stress in fallen snow, [by] Brown, C. B., Evans, R. J. and LaChapelle., E. R. Journal of Geophysical Research, Vol. 77, No. 24, 1972, p. 457080. [The initial state of stress in fallen snow is calculated by considering incremental gravity loading of the accreting snow slab, corresponding, in nature, to conditions for soft-slab avalanches in newly fallen snow.]Google Scholar
Chernikin, Ye. M. Rol’ kukhty v zhizni taygy [Effect of clumps of snow on branches on life of the taiga]. Priroda, 1971, No. 11, p. 12223. [Discusses damage to trees and effect on food supply of animals.]Google Scholar
Dickinson, W. T., and Whiteley, H. R. A sampling scheme for shallow snowpacks. Hydrological Sciences Bulletin, Vol. 17, No. 3, 1972, p. 24758. [A criterion for selecting a scheme is expressed in terms of the standard error of the mean water equivalent as a function of the means, variance, and sample sizes of snow depth and density.]Google Scholar
Dyunin, A. K., ed. Zheleznyye dorogi v slozhnykh fiziko-geograficheskikh usloviyakh [Railways in complicated physical and geographical conditions]. Trudy Novosibirskogo Instituta Inzhenerov Zheleznodorozhnogo Transporta, Vyp. 115, 1970, 161 p. [Thirteen articles on methods of controlling snow-drifts and avalanches.]Google Scholar
Eggleston, K. O., and others. Hybrid computer simulation of the accumulation and melt processes in a snowpack, by K. O. Eggleston, E. K. Israelsen and J. P. Riley, Logan, Utah, Utah State University. College of Engineering. Utah Water Research Laboratory, 1971. x, 77 p. [First phase of an investigation to develop an operational simulation model of the point snow melt process based on a time increment of one day or less.]Google Scholar
Enz, R. W. Proposed system for Arizona. Telemetry of mountain snowpack and related data. Phoenix, Arizona, U.S. Dept. of Agriculture. Soil Conservation Service, 1972. [10] p. [Outline of proposals.]Google Scholar
Federer, B. Abschwachung von Schockwellen in der Schneedecke. Wissenschaftliche Verhandlungen der Schweizerischen Naturforschenden Gesellschaft, 151. Jahresversammlung in Freiburg, 1971, p. 14649. [Suggests that in snow cover there is a definite critical layer (possibly at 30 cm) which has a diminishing effect on the expected shock from sonic booms.]Google Scholar
Fujino, K. Sekisetsu-naibu ni okeru yūsetsusui no ryūkasokudo no sokutei. II—shamen-sekisetsu-nai de no yūsetsusui no idō [Measurement of flow-down speed of melt water in snow cover. II—flow of melt water in snow cover on a slope]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 15158. [Speed and path studied by means of NaCl solution as a tracer, detected by pre-set electrodes. Results discussed. English summary, p. 158.]Google Scholar
Galbally, I., and Allison, I. Ozone fluxes over snow surfaces. Journal of Geophysical Research, Vol. 77, No. 21, 1972, p. 394649. [Old snow surfaces have an ozone destruction rate which is much slower than that for a soil or vegetation rate. More complicated ozone exchange processes are observed above fresh snow surfaces.]Google Scholar
Giorgi, M., and others. Misura della temperatura superficiale di un manto nevoso mediante radiometro all’infrarossa, [by] Giorgi, M., Colacino, M., Vivona., F. M. Bollettino del Camitato Glaciologico Italiano, Ser. 2, No. 19, 1971, p. 24150. [Describes method and results of measuring snow temperature with an infra-red radiometer in the Val Formazza. Discussion, p. 24950.]Google Scholar
Harris, S. A. Three modifications to produce more accurate measurements of snowfall and evapotranspiration. Canadian Geographer, Vol. 16, No. 3, 1972, p. 27177. [Describes field experiments in Alberta on a cross-section across a valley with north- and south-facing slopes, a burn area and a pine forest.]Google Scholar
Hopkins, J. S. A study of snowmelt floods in a mountainous catchment using limited meteorological data. Meteorological Magazine, Vol. 101, No. 1201, 1972, p. 22128. [Twenty years’ daily maximum temperatures at the lower end of the catchment were analysed to derive plausible critical sequences of daily maximum temperature which were then applied to run-off/temperature relationships derived from observed snow melt discharges.]Google Scholar
Huzioka, T., and others. Seppō kansoku jikken shitsu jikken syamen no sesshitsu chōsa hōkoku. V (Shōwa 45–46 nen, fuyu) [Report of investigations of snow character at the avalanche research station, Toikanbetsu, northern Hokkaido. V (1970–71)]. [By] Huzioka, T., Shimizu, H., Akitaya, E., Narita, H. and Kawada., K. Teion-kagaku: Low Temperature Science, Ser. A, [Supplement to No.] 29, Shiryō Shū: Data Report, 1971, p. 2127.Google Scholar
Huzioka, T., and others. Shamen sekisetsu no kyodō no kenkyū. I—sekisetsu-nai no yugami, wai sokudo [Studies of the behaviour of snow cover on slopes. I—strains and strain-rates]. [By] Huzioka, T., Shimizu, H., Akitaya, E., Narita, H. [and] Kawada., K. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 12534. [English summary, p. 13334.]Google Scholar
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Kikuchi, K. On snow crystals with small raindrops. Journal of the Meteorological Society of Japan, Vol. 50, No. 2, 1972, p. 14244. [Describes appearance of these snow crystals which are associated with small raindrops and were observed at “Syowa” station, Antarctica.]Google Scholar
Kobayashi, D., and others. Teshio chihō sanchi no seppi chosa. II [Observations of cornices in Teshio mountainous district. II]. [By] Kobayashi, D., Ishikawa, N., Nishio, F., Naruse, R., Kobayashi, S. [and] Ishida., T. Teionkagaku : Low Temperature Science, Ser. A, [No.] 29, 1971, p. 10314. [The effect of snow drifting on the development of a cornice, the growth and deformation of a cornice, and the distribution of cornices in relation to prevailing winds were studied. English summary, p. 11314.]Google Scholar
Kobayashi, S. Jifubuki ni okeru setsumen no hajō-moyō no seisei to undō [Development and movement of wavy features on the snow surface during snow drifting]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 8192.] Classifies and describes microreliefs formed during drifting by depositional and/or erosional patterns. English summary, p. 92.]Google Scholar
Kojima, K. Sapporo-shi no heichi sekisetsu no ondo. I. 1963–64–1968–69 nen no sekisetsu danmen sokutei shiryō yori [Snow cover temperatures on the plain in Sapporo. I. From the data of pit-wall observations of snow cover in Sapporo, 1963–64–1968–69]. Teion-kagaku: Low Temperature Science, Ser. A, [Supplement to No.] 29, Shiryō Shū: Data Report, 1971, p. 1520.Google Scholar
Kojima, K., and others. Moshiri no koryūiki ni okeru yūsetsu, ryūshitsu oyobi netsu-shūshi no kenkyū. II [Studies of snow melt, run-off, and heat balance in a small drainage area in Moshiri, Hokkaido. II]. [By] Kojima, K., Kobayashi, D., Aburakawa, H., Naruse, R., Ishimoto, K., Ishikawa, N. [and] Takahashi., S. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 15976. [Particular attention was paid to the difference between melting rates at the highest (547 m) and the lowest (290 m) sites. English summary, p. 17576.]Google Scholar
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Leaf, C. F., and Kovner, J. L. Sampling requirements for areal water equivalent estimates in forested subalpine watersheds. Water Resources Research, Vol. 8, No. 3, 1972, p. 71316. [Sampling zones should be stratified by elevation, the sampling in each zone being proportional, and sampling points should be widely spaced over each zone.]Google Scholar
Lee, C. W. On the crystallographic orientation of spatial branches on natural polycrystalline snow crystals. Journal of the Meteorological Society of Japan, Vol. 50, No. 3, 1972, p. 17180. [Angles between spatial branches were mostly about 70°; other small maxima occurred near 56° and 39°.]Google Scholar
Narita, H. Sekisetsu no hihvō-menseki no sokutei. II [Measurement of the specific surface of deposited snow. II]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 6979. [Method described and results presented for new snow, granular snow and hoar. English summary, p. 7879.]Google Scholar
Parkin, D. W., and Phillips, D. R. Particulate matter in Antarctic snow. Geophysical Journal of the Royal Astronomical Society, Vol. 27, No. 1, 1972, p. 1522. [Description of dust particles settled out of melt water from a 30-year-old site at the base of the ice cliff at Halley Bay. Details of the sampling technique are given.]Google Scholar
Rossi, G. Apporto dei manto nevoso al deflussi superficiali del torrente Lumiei. Bollettino del Comitato Glaciologico Italiano, Ser. 2, No. 19, 1971, p. 21539. [During 1965–71, 48% of the snow cover of the Lumiei river basin (a medium-altitude catchment basin free of glaciers or permanent snow-fields) yielded melt water.]Google Scholar
Runich, A. V. Metod rascheta davleniya lavinnogo potoka na prepyatstviye [A method for calculating the pressure of an avalanche flow upon an obstacle]. Meteorologiya i Gidrologiya, 1972, No. 5, p. 6974. [English abstract, p. 74.]Google Scholar
Runich, A. V., ed. Rasprostraneniye i rezhim lavin na territorii SSSR. (Kratkiy katalog izvestnykh svedeniy) [Distribution and regimes of avalanches in the territory of the U.S.S.R. (Short catalogue of known information)]. Leningrad, Gidrometeorologicheskoye lzdatel’stvo, 1970. 92 p. [Nineteen regions.]Google Scholar
Schmidt, R. A., jr. Sublimation of wind-transported snow—a model. U.S. Dept. of Agriculture. Forest Service. Research Paper RM-90, 1972, [ii], 24 p. [Sublimation from blowing snow is estimated from the balance of heat and mass transfer on a volume of air and non-uniform ice particles.]Google Scholar
Tushinskiy, G. K., ed. Voprosy prikladnoy glyatsiologii. Snezhnyye laviny i seli [Questions of applied glaciology. Snow avalanches and mud avalanches]. Informatsionnyy Sbornik o Rabotakh po Mezhdunarodnomu Geofizicheskomu Godu, No. 15, 1970, 167 p. [Includes the following papers: I. R. Zaitov and V. I. Kravtsova, “Issledovaniye vozmozhnostey deshifrirovaniya vysokogornogo landshafta pri s”yemke v razlichnykh zonakh spektra [The interpretation of mountainous landscapes from photographs in various zones of the spectrum]”, p. 7–14; V. I. Kravtsova and N. A. Raspolozhenskiy, “Izucheniye spektral’noy yarkosti ob”yektov vysokogornogo lavinno-lednikovogo landshafta [Study of the spectral luminance of objects of an avalanche and glacier landscape]”, p. 15–24; R. A. Alekseyev and I. R. Zaitov, “O vozmozhnosti primeneniya s”yemki v infrakrasnoy zone spektra pri izuchenii vysokogornogo landshafta [On the possibility of using photographs in the infra-red zone of the spectrum in the study of mountain landscapes]”, p. 25–33; K. V. Akif’yeva, V. I. Kravtsova and V. I. Turmanina, “Krupnomasshtabnyye kompleksnyye issledovaniya lavinnykh konusov kak ob”yekta deshifrirovaniya na tsvetograficheskikh materialakh [Large-scale complex research of avalanche cones as the object of interpretation in colour photography]”, p. 34–69; V. I. Turmanina, “Priyemy fitoindikatsiy pri glyatsiologicheskikh issledovaniyakh [Methods of using phyto-indicators in glaciology]”, p. 70–77; S. M. Myagkov, “Nekotoryye perspektivy izucheniya vidimykh granits lavinoopasnykh zon [Prospects of the study of visible limits of regions where there is danger of avalanches]”, p. 78–93; N. L. Kondakova, “Snezhnost’ gornykh rayonov SSSR i voprosy lavinnoy opasnosti [Snow cover in mountain regions of the U.S.S.R. and problems of danger from avalanches]”, p. 94–112; N. A. Volodicheva, “Snezhnyy pokrov Kamchatki [The snow cover of Kamchatka]”, p. 113–31: K. M. Shanshiyev, “Snezhnyy pokrov i vozmozhnosti organizatsii zimnego otdykha v tsentral’noy chasti Vostochnykh Karpat [Snow cover and the possibility of organizing winter holidays in the central part of the eastern Carpathians]”, p. 132–42; V. Ya. Farber, “Opyt aktivnogo vozdeystviya na snezhnyy pokrov s tsel’yu predotvrashcheniya vnezapnogo skhoda lavin [Experience of using ballistic methods on snow covering as a warning of unexpected avalanches]”, p. 143–50; Yu. F. Knizhnikov, “Sovremennyye sposoby opredeleniya poverkhnostnoy skorosti dvizheniya l’da v lednike [Present-day methods of determining the surface speed of ice movement in a glacier]”, p. 150–65.]Google Scholar
Tusima, K. Ondo ni yoru sekisetsu no kōdo henka [Hardness of snow as dependent on its temperature]. Teionkagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 5155. [Quantitative examination of relationship between hardness of snow and temperature. English summary, p. 5455.]Google Scholar
Tusima, K. Taisekisa-hō ni yoru sekisetsu gansui-ryōkei no shisaku [Trial measurements of the free water content of deposited snow by the volume difference method]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 29, 1971, p. 5767. [Describes method, using dilatometer. English summary, p. 6667.]Google Scholar
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Errata

Vol. 12, No. 64, p. 153. In the eighteenth entry the second author’s name should read Murty, Ramana., Bh. V. Google Scholar
Vol. 12, No. 64, p. 154. In the thirteenth entry the title of the paper should read “… in the eastern Canadian Arctic”.Google Scholar
Vol. 12, No. 64, p. 163. In the tenth entry the name Kaplinat should read Kaplina.Google Scholar