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Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

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Copyright © International Glaciological Society 1970

This is a selected list of glaciological literature on the scientific study of snow and ice and of their effects on the earth; for the literature on polar expeditions, and also on the “applied” aspects of glaciology, such as snow-ploughs, readers should consult the bibliographies in each issue of the Polar Record. For Russian material the system of transliteration used is that agreed by the U.S. Board on Geographic Names and the Permanent Commitee 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 i interest. It should be noted that the Society does not necessarily hold copies of the items in this list, and also that the Society does not possess facilities for microfilming or photocopying.

References

Conferences

Shchukina,O. VE. Chetvertyy obshchesoyuznyy glyatsiologicheskiy simpozium [Fourth all-Union glaciological symposium].Vestnik Moskovskogo Unwersiteta, Ser. 5. God 24, No, 3, 1969, p. 12223. I Report of symposium held in northern Caucasus al “El'brus”, 21 September-5 October 1968.]Google Scholar

General Glaciology

Bryazgin, N.N. Koptev., A. P. O spektral'nom al'bedo snczhno-ledyanogo pokrova [Spectral albedo of a snow or ice surface], Probiemy Arktiki i Antarktiki Vyp. 31, 1969, p. 7983.Google Scholar
Fliri, F. ed. [Alpcnkundliche Studien, l.J Festschrift für Hans Kinzl zum siebzigsten Geburtstag Veröffentlichungen der Universität Innsbruck, 1, 1968, xi, 160 p. [Papers include: Fliri, F., “Beiträge zur Hydrologie und Glaziologie der Cordillera Bianca (Peru)”, p. 2552; Heuberger, H., “Die Ötztalmündung (Inntal, Tirol)”, P. 53–90; H. Heuberger and H. Penz, “Verzeichnis der wissenschaftlichen Arbeiten von Univ.-Prof. Dr Hans Kinzl”, p. 149156.]Google Scholar
Hoinkes, H.C. Raimund von Klebeisberg, 14.1a.1886 6.6.1067. Jahrbuch der Bayerischen Akademie der Wissenschajten 1968, p. 21220. [Obituary.]Google Scholar
Kattekfel'D G. N., Frolov, P. M. O sushchestvovanii vody na Lune [On the existence of water on the moon], Izvestiya Vsesoyuznago Geograficheskogo Obshchestva, Tom 101, Vyp. 3, 1969, p. 26064. [Discussion of possibility of ice, water and water vapour on the moon.]Google Scholar

Glaciological Instruments and Methods

Berdnikov, V.V. Kotyukov,, V. A. Opyt primeneniya geofizicheskikh metodov pri izuchenii reliktovykh merzlolnykh obrazovamy [The use of geophysical methods for studying relict frozen ground formationsl Izvestiya Akademii Nook SSSR, Seriya Geograjicheskaya, 1969. No. 5, p. 10917. Bogokodskiy, V.V. Fizkheskiye melody issledovaniya lednikov·(Physical methods of investigating glaciers] Leningrad Gidrometeorologichcskoye Izdatel'stvo, 1968.214 p. [Book summarizing basic principles of gravimetric, seismic, and radar techniques used in glaciology. English summary.]Google Scholar
Evans, S. Smith, B.M.E. A radio echo equipment for depth sounding in polar ice sheets. Journal of Scientific Instruments (Journal of Physics, E), Ser, a, Vol. 2, No. 2, 1969. p. 13136. [Discusses need for depth-sounding in glaciers, ice sheets, and ice shelves, and describes v.h.f. radar, designed specifically to produce continuous profiles of ice depth. Practical problems and results.]CrossRefGoogle Scholar
Gluck,, S. _ Épaisseur du Glacier Blanc (massif de I’Oisans) dans sa partie supérieure. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 268, Sér. D, No. 12, 1969. p. 158385. [Seismic reflexion technique used to determine glacier thickness in accumulation area of this French glacier.]Google Scholar
Nelsln, D.E. Radar sounding of glaciers in the Icefield Ranges. (In Bushnell, V.C., Ragle, R.H. ed. Icefeld Ranges Research Project. Scientific results. Vol. 1. New York, American Geographical Society; Montreal, Arctic Institute of North America, 1969, p. 107.) [Successful use of technique in divide region of ice field.]Google Scholar

Physics of Ice

Aknason, B. Equilibrium constant for the fractionation of deuterium between ice and water. Journal of Physical Chemistry, Vol. 73, No. 10, 1969, p. 349194. [Accurate experimental determination.]CrossRefGoogle Scholar
Bailey, W.A. Measuring heat losses through common greenhouse covering materials under different test conditions, [by] Bailey, W.A., Liu, R.C., Klueter, H.H., Krizek, D.T. (In Ho, C.Y., Taylor, R.E. ed. Thermal conductivity. Proceedings of the eighth conference held at Purdue University, West Lafayette Indiana October 7–10, 1968. New York, Plenum Press, 1969>. p. 94148.) [Experiments show that ice or snow cover over the glass increases heat transmittance.]Google Scholar
Bennett, J.E. Trapped electrons produced by deposition of alkali-metal atoms on ice at 77°K. Part III. Invariance of electron spin resonance spectra with metal cation, by Bennett, J.E., Mile, B., Thomas, A.. Journal of the Chemical Society, Sect. A. 1969, [No.] 10, p. 150205. [Identical e.s.r. spectra result from deposition of Li, K, Na, Rb or Cs, so the cation is not involved in the trap.]CrossRefGoogle Scholar
Bertie, J.E. Absorptivity of ice I in the range 4 000–30 cm.-1 [by] Bertie, J.E., Labbé, H.J., Whalley, E. Journal of Chemical Physics, Vol. 50, No. 10, 1969. p. 450120. [Measurements and interpretation.]CrossRefGoogle Scholar
Bhadra, T.C Effects of physical stimulii, aeratign [sic], preheating, electric field on the supercooling and nucleation of water droplets. Indian Journal of Physics, Vol. 42, No. 8, 1968, p. 47485. [Study of time to freeze droplets under various conditions. Shock waves had no effect, contrary to results for bulk water ]Google Scholar
Bhadra, T. C. Induction of freezing of bulk samples of supercooled water by physical stimulii. Indian Journal of Physics,Vol. 42. No. a. 1968. p. 91102. [Experiments on effect of air content and of mechanical or electrical stimuli.]Google Scholar
Bhadra, T.C. On the feasibility of inducing cavitation in hailstones and supercooled water by low-intensity shock wave. Indian Journal of Physics,Vol. 42. Xo. to. 1968. p. 60309. [No effect produced by ultrasonic waves on ice. Results used to discuss theory of hailstone break-up.]Google Scholar
Blair, D.N. Davis, B. L. Aging of silver iodide-sodium iodide generator effluent in moist dry air. Journal of Applied Meteorology. Vol. 8, No 4. 1969. p. 55155. [Effect of storage of aerosol panicles on their efficiency as ice nuclei.]2.0.CO;2>CrossRefGoogle Scholar
Box, H.C. Hydroxyl radicals of X-irradiated single crystals of ice, [by] Box, H.C., Lilga, K.T., Budzinski, E.E., Deer, R. Journal of Chemical Physics,Vol. 50. No. 12, 1969, p. 542223. [Leiter. Electron spin resonance study at low temperatures.]CrossRefGoogle Scholar
Chiu, S.-Y Experiniental study of the ice-making operation in the inversion desalination freezing process, [by]Chiu, S.-Y, Fan, L.-T, Akins, R.G.. Industrial und Engineering Chemistry. Process Design and Development. Vol. 8, No 3. 1969. p. 34756. [Experimental study of shape of ice crystals formed.]CrossRefGoogle Scholar
Cross, J.D. Speare., P. A. Electrical aspects of the evaporation of ice. British Journal of Applied Physics (Journal of Physics. D). Ser. 2,Vol. 2. No. 7. 1969. p. 102125. I Electrical charge due to evaporation of polycrystalline ice in vacuo found to be very small. Scanning electron microscopy suggests earlier results may be due to particles breaking off.]CrossRefGoogle Scholar
Davis,, B. L., Blair,, D. N. Role of substrate strain in ice nucleation. Journal of Geophysical Research. Vol. 74. No. 18. 1969. p. 457180. [Deformed AgI. CuS and AI2,SiO3 (OH)4 were much more efficient ice nuclei than undeformed specimens.]CrossRefGoogle Scholar
Dean, P. Remarks on the vibrations of disordered systems. Journal of the Physical Society of Japan,Vol. 26. Supplement, 1968 [pub. 1969]. p. 2024. [Includes a discussion of vibrations of ice Ih on basis of two-dimensional theoretical model.]Google Scholar
Dillard, D.S. Timmc.rhaus., K. D. Low temperature conductivity of selected dielectric crystalline solids. (In Ho, C.Y-, Taylor, R.E. ed. Thermal conductivity. Proceedings of the eighth conference held at Purdue university. West Lafayette, Indiana, October 7–10. 1963. New York, Plenum Press. 1969. p. 94968.) [Includes results for ice from 80 to 273 K.]Google Scholar
Dilorenzo, J. Kaplan, V. M.Phase transformations in doped ice: concentration effect m frozen ferrous solutions. Chemical Physics Letters,Vol. 3. No. 4, 1969. p. 21618. [Mössbaucr studies of effect of Sn4+ and Eu3+ ions on ice with Fe ++ ions in solution.]CrossRefGoogle Scholar
Engelhardt,, H. Detection of single collisions of fast neutrons by nucleation of Tyndall Bowers in ice, [by] Engelhardt,, H., Müller-Krumbhaar., H., Bullemer, B., Riehl, N. Journal of Applied Physics. Vol. 40, No. 13, 1969 [pub. 19701, p. 530811. [Method of growing good single crystals of ice and of using them to detect neutrons by the nucleation of Tyndall flowers.]CrossRefGoogle Scholar
Fukuda, A. Higashi., A. X-ray diffraction topographic studies of dislocations in natural large ice single crystals. Japanese Journal of Applied Physics,Vol. 8. No. 8. 1969. p. 99399. [Study of shape and Burgers vectors of dislocations in glacier ice from Mendenhall Glacier, Alaska.]CrossRefGoogle Scholar
Gitlin, S.N. Lin., S.-S. Dynamic nucleation of the ice phase in supercooled water. Journal of Applied Physics. Vol. 40, No 12. 1969. p. 470167. [Experiments which show that cavitation is a necessary but not a sufficient condition for dynamic nucleation of ice in supercooled water.]CrossRefGoogle Scholar
Gold,, L. W. Crack formation in ice during creep, Scripta Metallurgica. Vol. 3. No. 6, 1969. p. 36770. [Correlation between density of cracks and creep deformation in columnar ice.]CrossRefGoogle Scholar
Haring, O.K. Slow neutron inelastic scattering study of light water and ice. Journal of Chemical Physics. Vol. 50. No. 12. 1969. p. 527996. [Study analysed to give proton motions in ice.]CrossRefGoogle Scholar
Hase, H. Kevan,, L. Paramagnetic relaxation of radiation-produced electrons in annealed glassy and polycrystalline alkaline ices. Journal of Physical Chemistry. Vol. 73. No. 10. 1969. p. 329093. [Measurements show spin-spin relaxation time depends on annealing while spin-lattice does nol. Explanation in terms of trap sites.CrossRefGoogle Scholar
Higashi, A. Hikiage hoo ni yoru hyōlankcsshō no seisaku (dai 2 hō)—X-sen topogurafu ni yoru ten-i no kansatsu [Growth of large single crystals of ice from water (2)—X-ray diffraction topographie observations ofdislocations]. [By]Higashi, A., Oguro, M., Fukuda, A. Ōyō Butsuri. [Vol.] 38, [No.] 6. 1969. p. 56773. [Observations interpreted in terms of mechanism of growth. English summary.]Google Scholar
Isono, K. Iwai, K. Growth mode of ice crystals in air at low pressure. Nature. Vol. 223. No. 5211. 1969. p. 114950. [At low pressure ice crystals formed on solid nuclei are quasi-spherical with facets. Importance of these observations in study of noctilucent. and nacreous clouds.]CrossRefGoogle Scholar
Kamb, W.B. Structural studies of the high-pressure forms of ice. Transections of the American Crystallography Association. Vol. 5. 1969. p. 6180. [Review of knowledge of high-pressure forms of ice.]Google Scholar
Krausz, A. S. A rate theory of strain relaxation. Materials Science and Engineering. Vol. 4. No. 4, 1969. p. 19397.[Theory of strain relaxation in belter agreement with dislocation velocity measurements. Results compared with data on strain relaxation in ice.]CrossRefGoogle Scholar
Krausz, P.N. Salomon, R.E. Solubility of hydrogen chloride in ice. Journal of Physical Chemistry. Vol. 73. No. 8, 1969. p. 268083. [Determination from diffusion of HC1 into pure ice.Google Scholar
Lavrov, V. V. Osnovnyye zakonomernosti deformirovaniya l'da [Main principles in ice deformation]. Problemy Arktiki i Antarktiki. Vyp. 28, 1968. p. 4245.Google Scholar
Lyashchenko, A.K. Malenkov, G.G. Rentgenograficheskoye izuchemye sistemy ftorid ammoniya led [X-ray diffraction study of the ammonium fluoride-ice system]. Zhumal Strukturnoy Khimii. Tom 10. No. 4, 1969, p. 72425. [Determination of phase diagram and of lattice constant variations with concentration of dissolved NH4F in ice.]Google Scholar
Macklin, W.C Payne, G.S The spreading of accreted droplets. Quarterly Journal of the Royal Meteorological Society. Vol. 95. No. 40b, 1969, p. 72430. [Measurement of amount of spreading of supercooled droplets accreting on an ice surface.]CrossRefGoogle Scholar
Mayoral, J.R. Isaka, H. Action glaçogène l'eau. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 269, Sér. B, No. 3, 169, p. 14548. [Evidence that phloroglucinols act as sublimation agents below water super-saturation.]Google Scholar
Miller, S.L. Clathrate hydrates of air in Antarctic ice. Science,Vol. 165. No. 3892. 1969. p. 48990 [Calculations show these should form at pressure corresponding to 800 m depth. This explains gas bubble disappearance in cores at 1 200 m.]CrossRefGoogle ScholarPubMed
Nakahara, V. Phonon spectrum and thermal neutron scattering in light water ice. Journal of nuclear Science and Technology (Tokyo),Vol. 5. No. 12, 1968. p. 63542. [Calculation of phonon spectrum and thermal neutron scattering law.]CrossRefGoogle Scholar
Odencrantz, F.K Freezing of water droplets: nucleation efficiency at temperatures above -5 C. Journal of Applied Meteorology. Vol. 8. No. 3, 1969. p. 32225. [Laboratory studies show efficiency depends strong on experimental conditions.]2.0.CO;2>CrossRefGoogle Scholar
Orem, M.W. Adamson, A. W. Physical adsorption of vapor on ice. II. n-Alkalies. Journal of Colloid and Interface Science, Vol. 31,. No. 2,. 1969. p. 27886. [Adsorption isotherms of simple non-polar hydrocarbon vapours on ice.]CrossRefGoogle Scholar
Pelah, I. Rum., S. L, Conductivity and Mössbauer measurements in doped ice. Journal of Chemical Physics, Vol. 51, No. 1,1969,. p. 38387. [Conductance anomalies in ice with Sn4+ ions at same temperature as Mössbaucr anomalies.]CrossRefGoogle Scholar
Ryan, B.F. The growth of ice parallel to the basal plane in supercooled water and supercooled meta fluoride solutions. Journal of Crystal Growth. Vol. 5, No 4. 1969, p. 28488. [Measxurements of dendritic growth rates.]CrossRefGoogle Scholar
Smith-johannsen,, R.I. Ice crystal agglomeration: T formation. Jounral of the Atmospheric Sciences Vol. 26, No. 3, 1969, p. 53234. [Agglomerates collected from laboratory ice clouds frequently had T shape. Possible explanations discussed.]2.0.CO;2>CrossRefGoogle Scholar
Stein, G.D Angular and wavelength dependence of the light scattered from a cloud of particles formed by homogeneous nucleation. Journal of Chemical Physics. Vol. 51 No. 3., 1969. p. 93842. I Experiments using laser light to study light scattering from ice particles formed via condensation by homogeneous nucleation ]CrossRefGoogle Scholar
Stow, C.D [tie charging of ice surfaces by natural ice particles. Quarterly Journal of the. Royal Meteorological Society, Vol. 95, No. 406, 1969, p. 797800. [Letter commenting on paper by Scott, W.D, Hobbs, P.V. ibid.,Vol. 94. No. 402. 1968.p. 510–22, with reply by authors p. 799800.]CrossRefGoogle Scholar
Wardman, P. Sediion., W A. Electron spin resonance studies of radicals condensed from irradiated water vapor: reactions of the radicals. Canadian Journal of Chemistry, Vol. 47, No. 12, 1969, p. 214954. [Studies in both H2O and D2O condensed after irradiation at 77 K.]CrossRefGoogle Scholar
Wardman, P. Sedbon, W.A. Electron spin resonance studies of radicals condensed from irradiated water vapor: paramagnetic relaxation of trapped electrons in ice. Canadian Journal of Chemistry, Vol 47 No 12, 1969. p. 215560. [Studies in both H2O and D2.O condensed after irradiation at 77 K]CrossRefGoogle Scholar
Weertman, J. Dislocation climb theory of steady-state creep. Transactions of American Society for Metals. Vol 61.No. 4. 1968. p. 68194, [Critical review of high temperature creep theories. Includes hitherto unpublished data on creep of polycrystalline H2O and D2.O ice.]Google Scholar
Weisweiler., W. Bemerkungen zur Bildung der Eisdendriten. Zetsdtrifi für Meteorologie. Bd. 21. Ht 3–4 1969, p. 10812. [Conditions of growth of different shapes of ice dendrites (snow crystals) from the vapour, Theory depending on vapour pressure difference between water and ice ]Google Scholar
Whalley, E. Change of high-frequency permittivity at an orientational order disorder transformation: a method of detecting very slow transformations. Journal of Chemical Physics. Vol. 51, No 1 1969, p 47172. Letter Measurement of high-frequency permittivity used to detect presence of ice III-IX phase change ]CrossRefGoogle Scholar
WöRZ,, O Cole., R. H. Dielectric properties of ice I. Journal of Chemical Physics, Vol. 51, No. 4 1969 p. 154650. [Measurements from o° to -80 C. Deviations from Arrhenius rate equation below 50°C]CrossRefGoogle Scholar
Zatsepina, G.N. K voprosu o mekhanizme dvizheniya ionov H3O+I OH-vo l’du I vode [On the question of the movement of H2O+ and OH- ions in ice and water]. Zhumal Strukturnoy Khimii, Tom 10, No 2. 1969. p. 211147. [Discussion of ionic mobility in ice assuming H3O+ moves along voids and OH moves along hexagonal framework in ice.]Google Scholar

Land Ice. Glaciers. Ice Shelves

Ambach, W. Ein Beitrag zur Kenntnis des Wärmehaushaltes des grönländischen Inlandeises. Polarforschung Bd. 6. Jahrg. 38, Nr. 1–2 1968 [pub. 1969], p. 20711. [Measurement of nearly balanced heat budget in May-July on Greenland ice sheet. English abstract.]Google Scholar
Andkrton, P.W. Structural geology of a glacier confluence. Kaskawulsh Glacier. Yukon Territory Canada Dissertations Abstracts. B. Vol. 28, No 9. 1968. p. 3747.B. [Strain-rate measurements and fabric studies. Abstract of dissertation submitted to Ohio State University, 1967. Microfilm order (University Microfilms. Ann Arbor, Mich.. L.S.A.Î no. 68-2945.]Google Scholar
Bailey, j.T. Evans, S. Radio echo-sounding on the Brunt Ice Shelf. British Antarctic Survey Bulletin No 17, 1968, p. 112. [Analysis of records obtained on a journey from Halley Bay to a sub-station in Coats Land, 300 km to the south.]Google Scholar
Bondarev, L.G. Orozgozhoyev, B.O. Basseyny pravykh pritikov r. Sary-Dzhaz mezhdu usfyami rek Ak-Shiyrak i Kuylyu (vklyuchaya basseyn Kuylyu) [The basin of right-hand tributaries of the river Sary-Dzhaz to the mouth of the rivers Ak-Shiyrak and Kuyly (including the river Kuylyu basin], Katalog lednikov SSSR [Catalogue of glaciers of the U.S.S.R.]. Tom 14, Vyp. 2. Chast' 7. Leningrad, Gidrometeorolo-gicheskoye Izdatel stvo. 1969. 58 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 including the Terskey Alatau. The Tom and Vyp. numbers correspond with those of Resursy poverkhnostnykh vod SSSR (Surface water resources of the U.S.S.R.].]Google Scholar
Bull, C.B. Marangunic, B. Glaciological effects of debris slide on Sherman Glacier. (In [U.S.] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C., National Academy of Sciences, 1968, p. 30917. (Publication 1603.)) [Earthquake-induced debris, about 1.3 m thick and covering third of ablation area, prevents melting of underlying ice and has thus changed regime of Sherman Glacier, Alaska, since 1964.]Google Scholar
Campbell, P.I. Glacier surveys in British Columbia, by Campbell, P.I., Reid, I.A, Shastal, J. Canada. Department of Energy, Mines and Resources. Inland Waters Branch. Water Survey of Canada. Report Series No. 5. 1969. v, 18 p., maps [in folder at back]. [Studies of volume changes of Sentinel, Sphinx, Nadahini. Kokanee and Bugaboo Glaciers.)Google Scholar
Cherkaksov, P.A. Yerasov, N.V. Reki Tcntek, Rgayty. Katalog lednikov SSSR [Catabgue of glaciers of the U.S.S.R.], Tom 13, Vyp. 2, Chast' 7. Leningrad, Gidrometeorologicheskoye Izdatel'stvo, 1969. 82 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 the Dzhungarskiy Alatau. The Tom and Vyp. numbers correspond with those of Resursy poverkhnostnykh nod SSSR [Surface water resources of the U.S.S.R.].]Google Scholar
Cronk, C. Glaciological investigations near the ice sheet margin, Wilkes station, Antarctica. Dissertations Abstracts·, B, Vol. 29, No. 3, 1968, p. 1066-B. [Pit and stake measurements, ice temperature and movement measurements and their analysis. Abstract of dissertation submitted to Ohio State University, 1968. Microfilm order (University Microfilms, Ann Arbor, Mich., U.S.A.) no. 68-12826.]Google Scholar
Davvdov, L.K. Krupneyshiye ledniki Sredney Azii—Ledniki Fedchenko i Zeravshanskiy. Rezultaty meteorologicheskikh i gidrologicheskikh issledovaniy [The biggest glaciers of Central Asia—Lednik Fedchenko and Lednik Zeravshanskiy. Results of meteorological and hydrological studies]. [Leningrad], Izdatel'stvo Leningradskogo Universiteta, 1967. 263 p. [Results of I.G.Y. studies on these glaciers.]Google Scholar
Denisov,, YE. P., Niikol'skaya,, V. V. Poxdnclednikov'ye v basseyen Amura [Modern glacicrization in the Amur basin]. Izvestiya Vsesoyuznogo Geograficheskogo Obshechestva, Tom 100, Vyp. 2, 1968, p. 13235. [Description of small glaciers in this region of U.S.S.R.]Google Scholar
Dort, W jr.,. Firn-ice relationships, Sandy Glacier, southern Victoria Land, Antarctica, by Dort, W jr.,, Roots, E.F, Derbyshire, E. Geografiska Annaler, Vol. 51A, No. 3, 1969, p. 10411. [Pit studies through alternate layers of ice and sand and interpretation.]Google Scholar
Fashchevskiy, B.V. O lednikovom pilaniî rek Gornogo Altaya [On the glacial streams of the Altay mountains]. Izoestiya Vsesoyuznogo Geograficheskogo Obshchestva, Tom 101, Vyp. 4, 1969, p. 36569. [Hydrographs oi glacial streams and their causes.].Google Scholar
Field, W.O. The effect of previous earthquakes on glaciers. {In | U.S.] National Research Council. Division oi Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C., National Academy of Sciences, 1968, 252-65. (Publication 1603.)) [Discusses different responses of Alaskan glaciers to 1899, 1958 and 1964 earthquakes, as well as other smaller earthquakes.]Google Scholar
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Flohn, H Zum Klima und Wasserhaushalt des Hindukuschs und der benachbarten Hochgebirge. Erdkunde. Bd. 23, Ht. 3, 1969, p. 20515. [Precipitation and run-otf in Hindu Kush and neighbouring mountains; includes discussion of contribution from glaciers and snow melt. English summary, p. 205.]CrossRefGoogle Scholar
Giessino,, Y. Trcdje etappe av Dronning Maud Land traversen. Norsk Polarinstitutt. Arbok, 1967 [pub. 1969]. p. 23337. [Third part of traverse of Dronning Maud Land ("Plateau" station to lat. 78° 42' S., long. 6° 52’ W.) in 1967–68 as part of U.S. Antarctic Research Program. English summary.]Google Scholar
Govorukha,, L. S. Otkryt novyy lednikovyy rayon [A new glacial region has been discovered]. Prtroda, 1969, No. 7, p. 6365. [Many glaciers found in 1967 in north-east Taymyr, U.S.S.R.]Google Scholar
Hamilton, W.L. Microparticle deposition on polar ice sheets. Ohio State University. Institute of Polar Studies. Report No. 29, 1969, vii, 77 p. (Study of micro-particle deposition in Antarctic and Greenland ice sheets and variations in size, concentration and kind of particle.]Google Scholar
Johnson, N.M. Ragle, R.H. Analysis of flow characteristics of Allen II slide from aerial photographs. (In [U S] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydúrology. Part A. Washington, D.C., National Academy of Sciences, 1968. p. 36973- (Publication 1603.)) [Some principles of flow mechanics illustrated by Allen II rock slide, Allen Glacier, and by other rock slides resulting from 1964 Alaska earthquake.]Google Scholar
Kjartansson,, G. Steinsholtshlaupiö 15. Janaúar 1967. NatturufrsMngurinn, Arg. 37, Ht. 3–4, 1967 [pub. 1968]. p 12069. [Jökullhtaup which began as rock slide at Steinsholt, south Iceland, in 1967. English summary.]Google Scholar
Koblents,, YA. P. O dvizhenii lednika v rayone Mirnogo [Glacier movement in the region of Mirny]. Informatsionnyy Byulleten' Souetskoy Antarktklteskoy Ekspeditsii, No. 70, 1968, p. 3235.Google Scholar
Konovalov, V.G. Rol* ablyatsii v obshchem byudzhete veshchestva i cvolyutsii gornogo lednika [Role of ablation in the budget and evolution of mountain glaciers]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva,Tom 101, Vyp. 4, 1969, p. 296305. [Discussion of importance of ablation in determining mass balance of glaciers.]Google Scholar
Kotlyakovv, M. Snezhnyy pokrov zemli i ledniki [Snow cover of the earth and glaciers]. Leningrad,Gidrometeorologicheskoye Izdatel'stvo, 1968. 479 p. [Interrelationship.]Google Scholar
Kupetskiy, V.N. O tendentsii sovremennogo morskogo i nazemnogo oledeneniya v svyazi s solnechnoy aktivnost'yu [The tendency of present sea and land glaciation in connexion with solar activity]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva,Tom 101, Vyp. 5, 1969, p. 42832.Google Scholar
LaChapelle, E.R The character of snow avalanching induced by the Alaska earthquake. (In [U.S I National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A Washington, D.C., National Academy of Sciences, 1968, p. 35561 (Publication 1603.)) [Reviews technical aspects of snow avalanche formation influenced by 1064 'earthquake.]Google Scholar
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Marangunic, C. Bull, C.B.B. The landslide on the Sherman Glacier. (In [U.S.] National Research Council. Division ol Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C., National Academy of Sciences, 1968. p. 38394. (Publication 1603)) [Detailed description of physical features and sliding mechanism of debris slide, induced by 1664 Alaska earthquake and now covering third of ablation area of glacier.]Google Scholar
Marcus, M.G. Effects on glacier-dammed lakes in the Chugach and Kenai Mountains. {In [U S ] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C., National Academy of Sciences. 1968. p 3204.7 (Publication 1603.)) [No appreciable response observed after Alaska earthquake, 1964.]Google Scholar
Markin, V. Λ. Teplovoy balans, usloviya yego formirovaniya i ablyatsiya lednikov o. Zapadnyy Shpitsbergen v 1965 [Heat balance, the conditions of formation and ablation of glaciers in Vestspitsbergen in 1965] Problemy Arktiki·i Antarktiki, Vyp. 29, 1968, p. 8088.Google Scholar
Nye, J.F. The advance and retreat of glaciers. Weather,Vol. 24. No. 12, 1969,p. 50112. [Text of sixth Margary Lecture summarizing relation between weather and climate and glaciers.]CrossRefGoogle Scholar
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[SOVIET CENTRAL. ASIA: GLACIOLOGY.] Teplovoy i vodnyy rez.him lednikov Kazakhslana [Heal and water regime of the glaciers of Kazakhstan]. Akademiya. Nauk Kazakhshoy SSR. Sektor Fizicheskoy Geografii. Glyatsiologicheskiyc issledovaniya v Kazakhstane [Academy of Sciences of the Kazakh S.S.R. Sector of Physical Geography. Glaciological investigations in Kazakhstan}. Vyp. 8. Alma-Ata, Izdatel'stvo “Nauka” Kazakhskoy SSR, 10,69. 160 P-[Contains the following papers, all in Russian with English summaries: N. N. Pal'gov, “Hydrologie balance of the glacio-nival landscape (as represented by the Maloalmatinka glacio-nival bell)”, p. 516; Ye. N. Vilesov, “Contemporary glacierization of the Kazakhstan Altay”, p. 1727; K. G. Makarevich, “Regime and budget problems of the Berel'sk glaciers in the Altay”, p. 2840; K. G. Makarevich and others. “Electrical sounding of the Lednik Korzhenevskiy, its run-off and mass balance”, by K. G. Makarevich, I. Ya. Fedulov and S. A. Borovinskiy, p. 4150; G. A. Rakhimzhanova and T. Ya. Denisova. “Weather characteristics of the basic forms of atmospheric circulation during the warm season in the Zailiyskiy Alatau glaciers”, p. 5157; P. A. Sudakov and G. A. Tokmagambetov, “Preliminary data on distribution of precipitation and snow reserves in the nival-glacial zone in the south-eastern part of the Chiliko-Keminskiy mountain complex”. p. 5868; P. A. Sudakov and V. A. Chekhonadskaya, “Quantitative assessment of the total annual précipitation in the Zailiyskiy Alatau”, p. 6974; P- A. Sudakov and others, “Snow accumulation on the glaciers of the Zailiyskiy Alatau range”, by P. A. Sudakov, G. A. Tokmagambetov and V. A. Chekhonadskaya. p. 7586; G. A. Tokmagambetov and P. A. Sudakov, “Structure of the firn-ice layer in the accumulation region of glaciers in the south-eastern part of the Chiliko-Keminskiy mountain complex”, p. 8790; P. A. Cherkasov, “Basic features of contemporary glacierization of the Biyon and Aksu river basins in the Dzhungarskiy Alatau”, p. 91108; V. A. Chekhonadskaya and others. “On the question of the distribution of atmospheric precipitation in the Dzhungarskiy Alatau”, by V. A. Chekhonadskaya, N. V. Yerasov and R. S. Bekten'yarov, p. 109- 13; V. A. Chekhonadskaya. “Ice melting and run-off from glaciers of the rivers Aksu and Biyon in the Dzhungarskiy Alatau”, p. 11423; A. P. Voloshina, “Investigation of heal balance in the firn area of Lednik Tsentral'nyy Tuyuksu”, p. 124 40; N. N. Pal'gov. “The firn line as an index of the hydrological regime of glaciers”, p. 14148; K. G. Makarevich and P. F. Shabonov, “Ice ablation and run-off from the Maloalmatinka glaciers during the period 1963 67”, p. 14957.]Google Scholar
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Thompson, R.D. Glaciological research on Mt. Ruapehu. .New Zealand Geographical Society Record. No. 45. 1968. p. 68. [Aims of a project to measure meteorological and mass balance quantities on the. Whakapapanui Glacier, North Island. New Zealand. |Google Scholar
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Tuthill, S.J. Earthquake-triggered rock avalanches and glacial stagnation in south central Alaska. (In [U.S.] National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.G.. National Academy of Sciences. 1968, p. 36208. (Publication 1603.)) [Discusses rock avalanche slides, resulting from 1964 earthquake, on to four glaciers (Sherman, Slide, Martin River, Schwan) which will affect regime of these glaciers.]Google Scholar
Tuthill, S.J., Postearthquake studies at Sherman and Sheridan glaciers, by Tuthill, S.J., Field, W.O., Clayton, L. {In [U.S.J National Research Council. Division of Earth Sciences. Committee on the Alaska Earthquake. The great Alaska earthquake; hydrology. Part A. Washington, D.C, National Academy of Sciences, 1968, p. 31828. (Publication 1603.)) [Predictions of future glaciological and ecological behaviour of Sherman Glacier, as a result of earthquake-induced rock avalanche of 1964, compared with unaffected Sheridan Glacier.]Google Scholar
Vilesov,, YE. N. Khonin, R.V. Basseyny levykh pritokov r. Ili ot ust'ya r. Kurty do ust'ya r, Turgen’ [Basins of the left tributaries of the river Ili from the mouth of the Kurty to the mouth of the Turgen']. Katalog lednikov SSSR [Catalogue of glaciers of the U.S.S.R.]. Tom 13, Vyp. 2, Chast' 1. Leningrad, Gidro-meteorologicheskoye Izdatel'stvo, 1967. 79 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 the basin of Ozero Balkhash. The Tom and Vyp. numbers correspond with those of Resursy poverkhnoslnykh vod SSSR [Surface wetter resources of the U. S.S.R.}.]Google Scholar
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Icebergs. Sea, River and Lake Ice

Antonov,, V S Ledovyy rezhim ust'ycvoy oblasti r. Leny v yestestvennom i zaregulirovannom sostoyanii [Natural and controlled ice regime of the mouth of the river Lena]. Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva,Tom 101, Vyp. 3, 1969. p. 20109.Google Scholar
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Heinsheimer, J.J. ¿QUC cantidad de hielo flota en los mares? Boletin del Servicio de Hidrografia Naual (Buenos Aires), Vol 4. No. 2. 1967 [pub. 1968], p. 21523. [Estimate of total volume of sea ice and of icebergs floating in the sea. English and German summaries.]Google Scholar
Hoshiai, T. Shōwa-kichi ni okeru kaihyōka no kororofiru-a ryō to kankvō-jōken no kisetsu-henka [Seasonal variation of chlorophyll-a and hydrological conditions under sea ice at “Syowa” station Antarctica] Nankyoku Shiryō: Antarctic Record. No. 35. 1969. p. 5267. [Study of conditions under sea ice including marked effect of thaw water. English abstract.]Google Scholar
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Tunnell, G. A Synoptic ice maps of the Meteorological Office. Journal of the Institute of Navigation. Vol 21 No. 4. 1968. p. 43947- [Describes preparation every 10 days of maps showing distribution of ice in Arctic Basin and areas adjacent to North Atlantic Ocean.]CrossRefGoogle Scholar
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Voyevodin, V.A. Mironov., L. V. Opyt opredeleniya tolshchiny plavuchikh l'dov pri pomoshchi stereofoto-grammctrichcskoy obrabotki aerosnimkov [Attempt to determine the thickness of floating ice with stereo air photographs]. Okeanologiya,Tom 8. Vyp. 2. 1968, p. 32736. [Measurement of height above water and computation of total thickness.]Google Scholar
Yeskin, L.I. Morskiye I'dy Yuzhnogo Okeana [Sea ice of the Southern Ocean]. Problemy·Arktiki i Antarktiki. Vyp. 31, 1969. p. 2430. [General characteristics, especially in Mirny region.]Google Scholar
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Glacial Geology

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Corbel,, ]. Recherches sur l'inlandsis quaternaire en Norvège septentrionale. Tramsø Museums Skrifter, Vol. 7, Ht. 6, 1968, p. 7595. [Study of Quaternary ice sheet in northern Norway. Norwegian summary.] CURRY, R. R. Holocene climatic and glacial history of the central Sierra Nevada, California. Geological Society of America. Special Paper No. 123, 1969, p. 147. [Chronology of climatic fluctuations based on fluctuations of mean snowfall.]Google Scholar
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Hamilton, T.D. Glacial geology of the lower Alatna valley, Brooks Range, Alaska. Geological Society of America. Special Paper No. 123, i960, p. 181223. [Interpretation of evidence of multiple glaciations oldest of which is thought to be Illinoian in age.]Google Scholar
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Hult, J. Some aspects of the shore formations on lake Lylykkäänjärvi, Finland. Fennia, 97, No. 5, 1968 [1967–68 on cover], 22 p. [Ice ramparts on south-western and north-western shores formed by ice-push.]Google Scholar
Ives, J.D. Buckley, J.T. Glacial geomorphology of Remote Peninsula, Baffin Island, N.W.T.. Canada. Arctic and Alpine Research, Vol. 1, No. 2, 1969. p. 8395. [Physiography described (high mountains, coastal uplands, glacial troughs, coastal lowlands) and used to interpret glacial geomorphology, especially significance of moraines. Probable appearance during Pleistocene discussed.]CrossRefGoogle Scholar
Jones, J A A The truth about ice-shove or the origins of certain “ice-shove” features on the lakeshores of central Labrador-Ungava. Geographical Articles (Cambridge). No. 11, 1968, p. 4.7-54. [Reviews and discusses work on lake-shore ice damage.]Google Scholar
King, C.A.M., Buckley, J.T. Geomorphological investigations in west-central Baffin Island, N.W.T.,Canada. Arctic and Alpine. Research, Vol. 1, No. 2, 1969. p. 10519. [Presents details of glacial, glacio-fluvial, and periglacial forms of west coast region, between Eqe Bay and Foley Island. Comments on icings on edge of coastal flats.CrossRefGoogle Scholar
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Krinsley, D.H Recognition of pre-Pleistocenc glacial environments. Bulletin of the American Association of Petroleum Geologists, Vol. 53, No. 3, 1969, p. 727. [Abstract only. Survey of methods of identification.] Lauer, W. Die Glaziallandschaft des südchilcnischen Seengebietes.Acta Geograplnca, 20, 1968, p. 21530. [Glacial geology of lake district in south Chile. Field-work in 1956–58 and 1966.]Google Scholar
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Wright, H.E.jr Quaternary geology and climate. Vol. 16. of the Proceedings of the V11 Congress of the International Association for Quaternary Research. Washington, D.C., [U.S.] National Academy of Sciences, 1969, ix, 162 p. [Includes the following papers: Picard, K.E., “Pleistocene tectonics and glaciation in Schleswig-Holstein, Germany”, p. 6771; Gerasimov, I.P., “Degradation of the last European ice sheet”, p. 7278; Chebotareva, N.S., “Recession of the last glaciation in northeastern European USSR”, p. 7983; Strelkov, S.A., “Main events in the evolution of relief in northern Eurasia and their tentative correlation with those in North America”, p. 8488; F. M. Synge, “The Wurm ice limit in the west of Ireland”, p. 8993; Dreimanis, A., Vagners, U.J., “Lithologie relation of till to bedrock”, p. 9398; Bayroek, L.A., “Incomplete continental glacial record of Alberta, Canada”, p. 99103; N. W. Rutter. “A Late-Pleistocene glacial advance. Bow River Valley, Alberta, Canada”, p. 10409; IX S. Simone» and Brown, D.A., “Uses of satellite-borne radar to study Antarctic ice conditions”, p. 11015; J· Demek, “Importance of slope deposits in the study of landscape development”, p. 13033.]Google Scholar
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Frost action on Rocks and Soil. Frozen Ground, Permafrost

Black, R.K. Climatically significant fossil periglacial phenomena in northcentral United States. Biuletyn Peryglacjalny, No. 20, 1969, p. 23538. [Discussion of which periglacial phenomena are of most use in interpreting palaeoclimates.]Google Scholar
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Meteorological and Climatological Glaciology

Budvko, M. I. On the causes of climate variations. Meddelanden frân Sveriges Meteorologiska och Hydrologiska Institut. Ser. B. Nr. 28, 1968. p. 613. [Discussion of phenomena and their possible causes. Importance of volcanic activity.]Google Scholar
Davitaya, F. F. Atmospheric dust content as a Factor affecting glaciation and climatic change. Annals of the Association of American Geographers. Vol. 59. No. 3. 1969. p. 55260. [Evidence Brenn solar radiation records and from samples of firn from glaciers that atmospheric dust is increasing and effect of this on albedo and hence mass balance.]CrossRefGoogle Scholar
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Snow

Benson, C.S. The seasonal snow cover of Arctic Alaska. Arctic Institute of Worth America. Research Paper No. 51,1969, vi, 86 p. [Studies of physical properties of surface layer of seasonal snow and physical processes occurring in, above, and below it are described and discussed.]Google Scholar
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Higuchi, K.. Nihon ni okeru sekkei no hyōgagaku-teki kenkyü |Glaciological studies on permanent snow-patches formed in gulleys in Japan]. Seppyō, [Vol.] 30. [No.] 6. 1968. p. 195207. [Review of previous observations of permanent snow-patches in Japan. English abstract.]Google Scholar
Jayaweeka, K. Cottis, O.L.F. R, E. Fall velocities of plate-like and columnar ice crystals. Quarterly Journal of the. Royal Meteorological Society,Vol. 95. No. 406. 1969, p. 70309. [Model experiments used to provide data for theoretical calculation of ice crystal terminal fall velocities.!CrossRefGoogle Scholar
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Lisignoli, C.A., Observaciones sobre la relación entre la durez a v la densidad de la nieve en el Antärtico. [by] Lisignoli, C.A., Dalinger, R.E., Machado, E. Contribución del institute Antartico Argentina. No. 92, 1967, 13 p. [Reports results on relation between hardness (i.e. resistance to penetration) and density of snow from 9 pits on Filchncr lee Shelf, Antarctica.]Google Scholar
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