Giovinetto, M. B. Results of glaciological research in Antarctica. U.S. Antarctic Projects Officer. Bulletin, Vol. 4. No. 7, 1933, p. 2–7. [Summary of recent advances in knowledge.]Google Scholar

Lorius, C. Terre Adélie. Campagne d’été 1961–1962. Glaciologie. Territoire des Terres Australes et Antarctiques Françaises. Expéditions Polaires Françaises (Missions Paul-Emile Victor), Publication No. 241, 1963, 109 p. [Results of 1961–62 field season in Terre Adélie including positions and elevations of markers, mean annual temperature, accumulation, coastal regression, electrical conductivity measurements on melted snow, firn and ice. English and Russian summaries.]Google Scholar

Nangeront, G. Vanni, M. The activities of the Italian Glaciological Committee on the occasion of the International Geophysical Year. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 8e An., No. 3, 1963, p. 97–100 Google Scholar

Østrem, G. Comparative crystallographic studies on ice from ice-cored moraines, snow-banks, and glaciers. Geografska Annaler, Vol. 45, No. 4, 1963, p. 210–40. [Detailed and fully illustrated account of ice crystal sizes in different snow and ice deposits.]Google Scholar

Pal’gov, N. N. (ed.) Mezhdunarodnyy Geofrzicheskiy God. Glyatsiologicheskiye issledovaniya v period MGG:, Zailiyskiy i Kirgizskiy Alatau, Allay . Vyp. 4. Alma-Ata, Izdatel’stvo Akademii Nauk Kazakhskoy SSR [Publishing House of the Academy of Sciences of the Kazakh S.S.R.], 1964. 168 p. [Fourth of series of publications of I.G.Y. results of which first three were entitled Zailiyskiy i Dzhungarskiy Alatau. Contains following papers, all in Russian with English summaries: N. N. Pal’gov, “Glaciers of Kazakhstan and their main regime features”, p. 5–27; N. N. Pal’gov, “On discharge of thawing waters from firn field of mountain glaciers”, p. 28–43; Ye. N. Vilesov, “The change of heat content of the active layer of glacier ice”, p. 44–53; K. G. Makarevich, “New glaciological studies in glaciers in the. Talgar basin of the Zailiyskiy Alatau”, p. 54–70; K. G. Makarevich, “Problems of the regime of the left Talgar glaciers”, p. 71–82; T. Ya. Tkachyk, “Direct radiation in the Zailiyskiy Alatau range mountainous zone”, p. 83–90; R. G. Golovkova, Yu. S. Dyukareva, and N. D. Yegorova, “Comparative characteristics of meteorological and actinometric indicts at glaciers on the upper Malaya Almatinka and Talgar rivers”, p. 91–104; R. G. Golovkova, K. Sh. Diyarova, and N. D Yegorova, “Main ablation factors of the Lednik Shokal’skogo in the Zailiyskiy Alatau range”, p. 105–10; N. D. Yegorova, “Meteorological conditions of the glacierized zone in the Zailiyskiy Alamo range”, p. 111–25; N. Ya. Barvenko, “Some features of glacial movement regime of the Maloalmatinskaya group of glaciers in the Zailiyskiy Alatau range”, p. 126–42; V. V. Zamoruyev, “Geomorphological observations on the Berel’skiy Lednik during the summer of 1960”, p. 143–49; Ye. V. Maksimov, “Results of glaciological observations in the western part of the northern slopes of Kirgizskiy Alatau”, p. 150–61; G. A. Tokmagambetov and V. N. Goluber, “The texture and structure of buried ice in the moraines of the Maloalmatinskaya glaciers”, p. 162–67.]Google Scholar

Robin, G. de Q. Glaciology. Endeavour, Vol. 23, No. 89, 1964, p.102–07. [Description of the development of study of ice as a plastic material.]Google Scholar

Streten, N. A. Some peculiarities of ice formation in MacRobertson Land. Australian MeteorologicalMagazine, No. 37, 1962, p. 29–34. [Rift in Amery Ice Shelf, inland mountain top “ice boulders” and formation of large open water pool in winter sea ice.]Google Scholar

Taljaard, J. J. Advances in knowledge of Antarctic topography, ice and meteorology since 1955. South Africa. Weather Bureau. News Letter, No.161, 1962, p. 131–37.Google Scholar

Beaumont, R. T. Work, R. A. Snow sampling results from three samplers. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 8e An., No. 4, 1963, p. 74–78. [Tests of two new designs and the Federal Snow Sampler.]CrossRefGoogle Scholar

Bonnema, D. J. Jagsneeumetcrs op Antarktika. South Africa. Weather Bureau. News Letter, No. 164, 1962, p. 178–79. [History of drift-snow meters and details of meter used on second South African Antarctic Expedition, 1961.]Google Scholar

Breuck, W. de. Un appareil pour découper ley carottes de sondage dans la glace.Bruxelles, Presses Universitaires de Bruxelles, 1962. 4 leaves. [Description of simple apparatus for cutting firn and ice cores from drillings.]Google Scholar

Schwerdtfeger, P. An analogue computer for solving growth problems of floating ice. Gerlands Beiträge zur Geophysik, Bd. 73, Ht. 1, 1964, p. 44–52. [Electrical device to predict ice thickness from surface temperature data.]Google Scholar

Schwerdtfeger, P. Measurement of conducted flow of heat in a sea ice cover. Nature, Vol. 200, No. 4908, 1963, p. 769. [Method of measurement.]Google Scholar

Barthakur, N. Maybank, J. Anomalous behaviour of some amino-acids as ice nucleators. Nature, Vol. 200, No. 4909, 1963, p. 866–68. [Experiments and discussion of mechanism.]Google Scholar

Bowden, F. P. Tabor, D. The friction and lubrication of solids. Part II. Oxford, Clarendon Press, 1964. xx, 544 p. [Ch. 8, p. 128–48, on friction, adhesion and deformation properties of ice and solid krypton; ch. g, p. 149–58, on friction of ski on snow and ice.]Google Scholar

Fukuta, N. Ice nucleation by metaldehydc. Nature, Vol. 199, No. 4892, 1963, p. 475–76.Google Scholar

Kuroiwa, D. Internal friction of ice. Contributions from the Institute of Low Temperature Science (Sapporo), Ser. A, No. 18, 1964, p. 1–62. [Paper in three parts: (1) the internal friction of H₂O and D₂O ice, and the influence of chemical impurities on mechanical damping, p. 1–37; (2) the grain boundary internal friction of ice, p. 38–48; (3) the internal friction of natural glacier ice, p. 49–62.]Google Scholar

Latham, J. Charge transfer associated with temperature gradients in ice. Nature, Vol. 200, No. 4911, 1963, p. 1087. [Test of theory. Deviations shown to be due to surface effects.]Google Scholar

Latham, J. Charge transfer associated with temperature gradients in ice crystals grown in a diffusion chamber. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 385, 1964, p. 266–74. [Experiments on charge acquired during growth and on contact between ice crystals at different temperatures.]Google Scholar

List, R. Zur Thermodynamik von Schwammeisansätzen an langsam rotierenden Zylindern. Winterbericht des Eidgenössischen Institutes für Schnee- und Lawinenforschung, Nr. 25, 1962, p. 105–09. [Study of the accretion of ice on slowly rotating cylinders. Also published as Eidgenössische Kommission zum Studium der Hagelbildung und Hagelabwehr Wissenschaftliche Mitteilungen, Nr. 42, 1963.]Google Scholar

Matthews, J. B. Mason, B. J. Electrification accompanying melting of ice and snow. Quarterly Journal of the Royal Meteorological Society, Vol. 89, No. 381, 1963, p. 376–80.Google Scholar

Mossop, S. C. Atmospheric ice nuclei. Zeitschrift für angewandte Mathematik und Physik, Vol. 14, Fasc. 5, 1963, p. 456–86. [Review article. 147 literature references. French summary.]CrossRefGoogle Scholar

Townsend, A. A. Natural convection in water over an ice surface. Quarterly Journal of the Royal Meteorological Society, Vol. 90, No. 385, 1964, p. 248–59.Google Scholar

Avsyux, G. A. Iskusstvennoye usileniye tayniya gornykh lednikov . Priroda , 1963, No. 7, p. 61–66. [Methods used in Central Asia.]Google Scholar

Bondarev, L. G. Ocherki po oledeneniyu massiva Ak-Shiyrak . Frunze, Izdatel’stvo Akademii Nauk Kirgizskoy SSR [Publishing House of the Academy of Sciences of the Kirgiz S.S.R.], 1963. 202 p. [Discussion of basis of I.G.Y. results.]Google Scholar

Buynitskiy, V. Kh. Shel’fovyye l’dy Antarktiki, ikh morfologiya, vnutrennyaya struktura i proiskhozhdeniye . Vestnik Leningradskogo Universiteta , No. 18, 1963, p. 82–101. [General discussion, with list of essential facts about 55 ice shelves.]Google Scholar

Chang, F. K. Seismic wave studies in northwest Marie Byrd Land, Antarctica. Bulletin of the Seismological Society of America, Vol. 54, No. 1, 1964, p. 51–65. [Relation between seismic wave velocity and other physical properties of ice and snow.]CrossRefGoogle Scholar

Epstein, S., and others. Oxygen-isotope ratios in Antarctic snow, firn and ice, by S. Epstein R. P. Sharp I. Goddard. Journal of Geology, Vol. 71, No. 6, 1963, p. 698–720. [O-isotope ratios in snow as a technique for measuring annual accumulation, and as a reflection of climatic changes in Antarctica.]Google Scholar

Eythórsson, J. Brúarjökull hlaupinn. Jökull, Ár 13, No. 3, 1963, p. 19–21. [Re-advance since 1890 of the eastern half of the margin by about 9 km. while western half had only advanced about 3 km. English summary.]Google Scholar

Eythórsson, J. Variation of Iceland glaciers 1931–1960. Jökuil, Ár 13, No. 3, 1963, p. 31–33. [General recession.]CrossRefGoogle Scholar

Georgii, H.-W. Der Spurenstoffgehalt des Gletschereises. Polarforschung, Bd. 5, Jahrg. 32, Ht. 1–2, 1962 [pub. 1963], p. 140–44. [The concentration of ions in glacier ice from Hintereisferner (Austria) is much less than in new precipitation whereas in ice from Axel Heiberg Island it is not. This is explained by the mechanism of formation of glacier grains.]Google Scholar

Giovinetto, M. B. Behrendt, J. C. The area of ice shelves in Antarctica. Polar Record, Vol. 12, No. 77, 1964, p. 171–73. [Discussion of differences between estimates by I. A. Suyetova and Giovinetto.]Google Scholar

Glen, J. W. Glaciers. Times Science Review, Spring, 1964, p. 12–14. [General review of present knowledge.]Google Scholar

Gonfiantini, R., and others. Geographical variations of oxygen–18/oxygen–16 ratio in surface snow and ice from Queen Maud Land, Antarctica, by R. Gonfiantini V. Togliatti E. Tongiorgi W. de Breuck E. Picciotto. Nature, Vol. 197, No. 4872, 1963, p. 1096–98.Google Scholar

Hattersley-Smith, G. Serson, H. Stratified water of a glacial lake in northern Ellesmere Island. Arctic, Vol. 17, No. 2, 1964, p.108–11. [Saline water near the bottom of the lake seems to have been sea-water trapped by the advancing glacier.]Google Scholar

Joubert, J.-L. Stratigraphie de la glace tempérée à l’aide de la teneur en eau liquide. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 257, No. 23, 1963, p. 3638–39. [Liquid-water content of cores from a temperate glacier show a periodic variation corresponding to the annual layering.]Google Scholar

Kapitsa, A. P. Moshchnost’ lednikovogo pokrova tsentral’nykh rayonov vostochnoy Antarktidy . Geofizicheskiy Byulleten’ , No. 13, 1963, p. 57–64. [Completed results for traverse “Komsomol’skaya”-South Pole made in 1959; earlier results for other traverses also given.]Google Scholar

Konovalov, V. G. Iskusstvennoye usileniye tayaniya snega i l’da v gorakh . Izvestiya Vsesoyuznogo Geograficheskogo Obshchestva , Tom 95, Vyp. 4, 1963, p. 330–38. [Disadvantages of scattering dark material on glaciers.]Google Scholar

Kopanev, I. D. Rol’ meteorologicheskikh usloviy v formirovanii snezhno-ledyanoy poverkhnosti Antarktidy . Problem, Arktiki i Antarktiki , Vyp. 14, 1963, p. 47–52. [Discussion of factors affecting accumulation.]Google Scholar

Koreysha, M. M. Sovremennoye oledeneniye Khrebta Suntar-Khayata . Rezul’laty Issledovaniy _po Programme Mezhdunarodnogo Geofizicheskogo Goda. Glyatsiologiya. IX Razdel Programm, MCC , No. 11, 1963, 98 p. [Results of field studies, 1956–59, in this range in Yakutskaya A.S.S.R.]Google Scholar

Liestøl, O. Noen resultater av bremålinger i Norge 1962. Norsk Polarinstitutt. Årbok, 1962 [pub. 1963], p. 187–90. [Glacier regime measurements in Norway, 1962; mainly Storbreen, Jotunheimcn.]Google Scholar

Mrkos, A. Opredeleniyc osadkov kosmicheskoy pyli na poverkhnosti lednikovogo shchita vostochnoy Antarktidy . Informatsionnyy Buuleeten’ Sovetskoy Antarktichesku, Ekspeditsii , No. 32, 1962, p. 38. [Analysis of filtered residue of snow melt.]Google Scholar

Peguy, C.-P. Observations glaciologiques dans le Massif des Grandes Rousses (France). Biuletyn Peryglacjalny ((Łódź), Nr. 11, 1962, p. 279–86. [Description or work including changes in glaciers and mass balance for the Glacier de Saint-Sorlin and the Glacier de Sarennes.]Google Scholar

Picciotto, E. Wilgain, S. Fission productsinAntarctic snow: a reference level for measuring accumulation. Journal of Geophysical Research, Vol. 68, No. 21, 1963, p. 5965–72. [Observations of sharp rise in β activity and ⁹⁰Sr in 1955 snow.]Google Scholar

Pillewizer, W. Vergletscherung und Schneegrenze in Hochasien. Petermanns Geographische Mitteilungen, Jahrg. 106, Quartalsheft 3, 1962, p. 186–87.Google Scholar

Renaud, A. Analyse climatique des variations de longueur des glaciers de Pizol et Sardona (Suisse). Bulletin de la Société Vaudoise des Sciences Naturelles, Vol. 68, Fasc. 5, No. 310, 1963, p. 195–204. [Study of causes of variations of these Swiss glaciers.]Google Scholar

Renaud, A. Quel est l’âge des glaciers? Les Alpes. Revue du Club Alpin Suisse, 40e An., 2e trimestre, 1964, p. 149–53. [The complexity of determining the true ages of glacier cover throughout the world.]Google Scholar

Ronca, L. B. Minimum length of time of frigid conditions in Antarctica as determined by thermoluminescence. American Journal of Science, Vol. 262, No. 6, 1964, p. 767–81.Google Scholar

Schytt, V. Fredrik Enquist, 1885–1963. Some comments on his glacier photographs of 1910. Ceograftska Annalen, Vol. 45, No. 4. 1963, p. 299–302. [The recession from 1910 to 1962 of Isfallsglaciären is well illustrated with photographs.]Google Scholar

Schytt, V., and others. Notes on glaciological activities in Kebnekaise, Sweden—1963, [by] V. Schytt S. Jonson P. Gederstrand. Geogrrfska Annalen, Vol. 45, No. 4, 1963, p. 292–99. [Mass balance studies on Storglaciären during 1963. Glacier retreat studied by levelled profiles. Variations of the extent of Swedish glaciers: field work 1963.]Google Scholar

Stone, K. H. Alaskan ice-dammed lakes. Annals of the Association of American Geographers, Vol. 53, No. 3, 1963, p. 332–49. [53 lakes in south-east Alaska and adjacent parts of Canada, described.]Google Scholar

Vallon, M. Contribution à l’étude structurographique de la glace froide de haute latitude. Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences (Paris), Tom. 257, No. 25, 1963, p. 3988–91. [Crystallography and structure of ice domes in front of the glaciers and of glacier ice from Kongsbreen, Vestspitsbergen.]Google Scholar

Wölcken, K. Seismische Eisdickenmessungen auf Nowaja Semlja 1932/33. Polarforschung, Bd. 5, Jahrg.31, Ht. 1–2, 1961 [pub. 1963], p. 87–91. [Seismic measurements of thickness of ice on Novaya Zemlya, 1932–33. English summary.]Google Scholar

Dunbar, Moira Wittman, W. I. Some features of ice movement in the Arctic Basin. (In Proceedings of the Arctic Basin Symposium, Hershey, Pa., October 1962 [pub. 1963], p. 90–108.)Google Scholar

Kheysin, D. Ye. Rasprostraneniyc dlinnykh gravitatsionnykh voln v more, pokrytom melkobitom l’dom . Problemy Arktiki i Antarktiki , Vyp. 14, 1963, p. 61–66.Google Scholar

Kusunoki, K. Ono, N. Ice conditions in Lützow-Holm Bay, Antarctica 1956–59, presented on the basis of photo-interpretation. Contributions from the Institute of Low Temperature Science (Sapporo), Ser. A. No. 19, 1964, p. 1–21. [Sea-ice conditions in the bay are studied on the basis of shipboard observations and air photos.]Google Scholar

Lunde, T. Sea ice in the Svalbard region 1957–1962. Norsk Polarinstitult. Årbok, 1962 [pub. 1963], p. 24–34 Google Scholar

Orvig, S. Energy exchange, air-ice-water. (In Proceedings of the Arctic Basin Symposium, Hershey, Pa., October 1962 [pub. 1963], p. 231–43.) [General discussion of problem of heat balance determination for Arctic Ocean.]Google Scholar

Roberts, B. B. Armstrong, T. E. Proposed new terms and definitions of sea ice for the use of submariners. Polar Record, Vol. 12, No. 77, 1964, p. 197–98.Google Scholar

Turanov, I. M. Rezul’taty nablyudeniy nad staivaniyem l’da v Bukhte Dikson v 1957 g. . Trudy Arkticheskogo i Antarkticheskogo Nauchno-Issledovatel’skogo Instituta , Tom 248, 1963, p. 37–41. [Observation of experimental area of 100 m.² of sea ice.]Google Scholar

Untersteiner, N. Ice budget of the Arctic Ocean. (In Proceedings of the Arctic Basin Symposium, Hershey, Pa., October 1962 [pub. 1963], p. 219–30.) [General discussion of mass and heat budget of sea ice. Discussion by W. I. Wittman, p. 227–30.]Google Scholar

Untersteiner, N. Sommerfeld, R. Supercooled water and the bottom topography of floating ice. Journal of Geophysical Research, Vol. 69, No. 6, 1964, p. 1057–62. [Experiments to verify presence of supercooled water under tabular icebergs in Arctic Ocean.]Google Scholar

Vowinckel, E. Ice transport in the East Greenland current and its causes. Arctic, Vol. 17, No. 2, 1964, p. 111–19. [Ice is transported (a) by ocean currents, and (b) by wind.]Google Scholar

Wellman, H. W. Wilson, A. T. Salts on sea ice in McMurdo Sound, Antarctica. Nature, Vol. 200, No. 4905, 1963, p. 462–63. [Explanation in terms of freezing of sea-water percolating through cold snow.]Google Scholar

Andrews, J. T. The cross-valley moraines of north-central Baffin Island: a quantitative analysis. Geographical Bulletin (Ottawa), No. 20, 1963, p. 82–129. [Re-examination of hypothesis of their genesis.]Google Scholar

Andrews, J. T. Cross-valley moraines of the Rimrock and Isortoq river valleys, Baffin Island, N.W.T.—a descriptive analysis. Geographical Bulletin (Ottawa), No. 19, 1963, p. 49–77.Google Scholar

Andrews, J. T. Sim, V. W. Examination of the carbonate contents of the drift in the area of Foxe Basin, N.W.T. Geographical Bulletin (Ottawa), No. 21, 1964, P. 44–53. [Evidence that the eastward movement of ice across the island was followed by a later westward flow.]Google Scholar

Broecker, W. S. Radiocarbon ages of Antarctic materials. Polar Record, Vol. II, No. 73, 1963, p. 472–73. [Warning on systematic error in ¹⁴C dating of material from cold oceans.]Google Scholar

Cardenas, A. L. El glaciarismo Pleistoceno en las cabeceras del Chama. Revista Geográfica (Universidad de los Andes. Instituto de Geografía. Mérida, Venezuela), Vol. 3, No. 8, 1961–62, p. 173–94. [Account of the Pleistocene glacierization in the Chama valley, Venezuela.]Google Scholar

Dahl, R. Shifting ice culmination, alternating ice covering and ambulant refuge organisms? A discussion of the question of ice-free areas in Scandinavia during the last Ice Age. Geografiska Annaler, Vol. 45, Nos. 2–3, 1963, p. 122–38.Google Scholar

Davies, W. E. Glacial geology of northern Greenland. Polarforschung, Bd. 5, Jahrg. 31, Ht. 1–2, 1961 [pub. 1963], p. 94–103. [Field-work by U.S. Air Force Cambridge Research Laboratories, 1956–60. German summary.]Google Scholar

Heinzelin, J. D. E. Carte des extensions glaciaires du Ruwenzori (versant congolais). Biuletyn Peryglacjalny (Łódź), Nr. II, 1962, p. 133–39. [Project for mapping former ice limits on the Congolese side of Ruwenzori. General description of moraines and periglacial phenomena.]Google Scholar

Hollin, J. T. Origin of ice ages: an ice shelf theory for Pleistocene glaciation. Nature, Vol. 202, No, 4937, 1964, P. 1099–1100. [Discussion of A. T. Wilson’s paper with same title in Nature, Vol. 201, No. 4915, 1964, P. 147–49, on the effects of instability of the Antarctic Ice Sheet.]Google Scholar

Huang, P’ei-hua. Kuan-yü ch’ang-chiang yi-nan ti-ch’ü ping-ch’uan yi-chi wen-t’i . Kexue Tongbao (K’o-hsiüeh T’ung-pao) , 1963, No.10, p. 29–33. [Reply to criticisms by T’sao and others, ibid., 1963, No. 3, p. 29–30, and by Wu and others, ibid., 1963, No. 6, p. 31–35, of author’s view that glaciers did not occur in this area.]Google Scholar

Ives, J. D. Deglaciation and land emergence in north-eastern Foxe Basin. Geographical Bulletin (Ottawa), No. 21, 1964, p. 54–65. [Glaciation and deglaciation of the Baffin Island-Foxe Basin area, and the regional significance of the results.]Google Scholar

Ives, J. D. Field problems in determining the maximum extent of Pleistocene glaciation along the eastern Canadian seaboard—a geographer’s point of view. (In Löve, Á. Löve, D., ed. North Atlantic biota and their history. Oxford, Pergamon Press, 1963, p. 337–54.)Google Scholar

Lee, H. A. Method of deglaciation, age of submergence and rate of uplift west and east of Hudson Bay, Canada. Biuleyn Peryglacjalny (Łódź), Nr. 11, 1962, P. 239–45.Google Scholar

Liestøl, O. Et senglacialt breframstøt ved Hardangerjøkulen. Norsk Polarinstitult. Årbok, 1962 [pub. 1963], p. 132–39. [Study of moraine ridges, north-west Hardangervidda, south Norway, indicating glacier advance in late glacial time. English summary.]Google Scholar

Linton, D. L. The forms of glacial erosion. Institute of British Geographers. Publication No. 33, Transactions and Papers, 1963, p. 1–28. [Presidential address surveying various forms of glacial erosion.]Google Scholar

Linton, D. L. Glacial erosion on soft-rock outcrops in central Scotland. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 247–57. [Description of features attributable to glacial action and discussion of enormous effect of glacial erosion in this area.]Google Scholar

Louis, H. Die vom Grundrelief bedingten Typen glazialer Erosionslandschaften. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 259–70. [General discussion of mountain landforms of glacial erosion and variations arising from differences of pre-glacial relief.]Google Scholar

Mackay, J. R. Mathews, W. II. The role of permafrost in ice-thrusting. Journal of Geology, Vol. 72, No. 3, 1964, p. 378–80. [Discussion of paper by W. O. Kupsch (“Ice thrust wedges in western Canada”, Journal of Geology, Vol. 70, No. 5, 1962, p. 582–94) and conclusion that permafrost assists formation of ice-thrust ridges or Stauchmoränen.]Google Scholar

Norris, S. E. Permeability of glacial till. U.S. Geological Survey. Professional Paper 450-E, No. 224, 1963, p. 150–51.Google Scholar

Norrman, J. O. Lake Vättern. Investigations on shore and bottom morphology. Geografiska Annater, Vol. 46, Nos. 1–2, 1964, p. 1–238. [Very full account, including ice recession in the Quaternary, hydrology and present-day ice conditions.]Google Scholar

Østrem, C. Ice-cored moraines in the Kebnekajse area. Biuleyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 271–78. [Observations of ice-cored moraines and investigation into nature of ice which is not glacier ice in origin.]Google Scholar

Paschinger, H. Glazialmorphologische Studien in der Neumarkter Passlandschaft. Mitteilungen des Naturwissenschaftlichen Vereins für Steiermark, Bd. 93, Sonderband, 1963, p. 63–72. [Glacial geomorphology of the country to the south-east of the Seetaler Alpen, Austria.]Google Scholar

Paschinger, V. Beziehungen zwischen einigen Formelementen und den Kleinschwankungen von Alpengletschern. Denkschriften der Österreichischen Akademie der Wissenschaften. Mathematisch-naturwissenschaftliche Klasse, 110. Bd., 4. Abh., 1963, 56 p. [Connexion between certain regional influences and minor fluctuations of alpine glaciers. Posthumous republication.]Google Scholar

Chao-Yüan, Ts’ao and others Kuan-yü chung-kuo ping-ch’i ho chien-ping-ch’i wen-t’i . Kexue Tongbao (k’o-hsüeh T’ung-pao) , 1963, No. 3, p. 29–30. [Criticism of paper by Huang (ibid., 1963, No. 1, P. 34–39) on presence of Pleistocene glaciers in China.]Google Scholar

Hsi-Hao, Wu and others. Tui “Chung-kuo ti-ssu-chi ch’i-hou yen-pien ti t’an-t’ao” yi-wen ti t’ao-lun . Kexue Tongbao (K’o-hsüeh T’ung-pao) , 1963, No. 6, p. 33–35. [Criticism of paper by Huang (ibid., 1963, No. 1, p. 34–39) on presence of Pleistocene glaciers in China.]Google Scholar

Yevteyev, S. A. Geologicheskaya deyatel’nost lednikovogo pokrova vostochnoy Antarktidy . Geofizicheskiy Byulleten’ , No. 12, 1962, p. 61–68. [Discussion of geomorphological effects of Antarctic Ice Sheet.]Google Scholar

Alexandre, J. Phénomènes périglaciaires dans le Basoutoland et le Drakensberg du Natal. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 11–13. [Description of current and former periglacial processes in Basutoland and neighbouring regions of Natal.]Google Scholar

Andrews, J. T. So-called “vallons de gelivation” in central Labrador-Ungava. Biuletyn Pesyglacjalny (Łódź), Nr. 12, 1963, p. 137–43. [These valleys were formed at least before the last glacial period but have been modified during the end of the deglaciation of the area.]Google Scholar

Brunnschweiler, D. The periglacial realm in North America during the Wisconsin glaciation. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 15–27. [Discussion of evidence for existence of frost action in the non-glaciated parts of North America.]Google Scholar

Brunnschweiler, D. Der pleistozäne Periglazialbereich in Nordamerika. Zeitschrift für Geomorphologie, Neue Folge, Bd. 8, Ht. 2, 1964, p. 223–31. [Frozen soils, polygons, etc., and climatic-morphological order in North America during the Wisconsin Ice Age.]Google Scholar

Corte, A. E. Blanca, B. Relationship between four ground patterns, structure of the active layer, and type and distribution of ice in the permafrost. Biulelyn Peryglacjalny (Łódź), Nr. 12, 1963, p. 7–90. [Correlation between surface pattern, grain size and structure of the active layer, and type and distribution of ground ice.]Google Scholar

Dylik, J. Problèmes périglaciaires de Hongrie. Biuletyn Peryglacjalny (Łódź), Nr. 12, 1963, p. 91–109.Google Scholar

Herz, K. Ergebnisse mikromorphologischer Untersuchungen im Kingsbay-Gebiet (Westspitzbergen). Petermanns Geographische Mitteilungen, Jahrg. 108, Quartalsheft 1–2, 1964, p. 45–53. [Investigations of patterned ground in Vestspitsbergen.]Google Scholar

Johnston, G. H., and others. Permafrost investigations at Thompson, Manitoba; terrain studies, by G. H. Johnston R. J. E. Brown D. N. Pickersgill. Canada. National Research Council. Division of Building Research. Technical Paper No. 158, 1963, [139]p.Google Scholar

Kachurin, S. P. Thermokarst within the territory of the U.S.S.R. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 49–55. [General description and discussion of origin.]Google Scholar

Kar, N. R. Investigations on a piedmont drift deposit in the foot-hills of the eastern Himalayas and its glacial and periglacial significance. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 211–28. [Description of enormous deposits in the Himalayan foot-hills attributed to solifluction.]Google Scholar

Koziejowa, U. Denudaeja stoków w rocznym cyklu klimatycznym [Erosion of slopes during the climatic cycle of a year]. Acta Geographica Universitatis Lodziensis (Łódź), No. 16, 1963, p. 7–56. [Work carried out on the Plateau of Łódź indicates that the most active periods occur when snow melts and when summer begins.]Google Scholar

Ksandr, J. Über die glaziale und periglaziale Problematik in der Tschechoslowakei. Biuletyn Peryglacjalny (Łódź.), Nr. 11, 1962, p. 229–37. [Description of glacial and periglacial phenomena in Czechoslovakia.]Google Scholar

Nir, D. Indices de gelivation récente et pléistocène en Israël. Biuletyn Peryglacjalny (Łódź), Nr. 12, 1963, p. 161–64. [Fossil and present frost action in Israel.]Google Scholar

Péwé, T. L. Ice wedges in permafrost, lower Yukon River area near Galena, Alaska. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 65–76. [Description of these ice wedges and their structure, discussion of origin.]Google Scholar

Pissart, A. Des replats de cryoturbation au Pays de Galles, une variété géante de sols en guirlandes. Biuletyn Peryglacjalny (Łódź), Nr. 12, 1963, p. 119–35. [In central Wales very prominent benches or terraces exist. It is thought that these are of periglacial origin.]Google Scholar

Popov, A. I. Periglacial phenomena and the laws of their distribution in the U.S.S.R. Biuletyn Pesyglacjalny (Łódź), Nr. 11, 1962, p. 77–83. [Geographical variations described.]Google Scholar

Rapp, A. Kärkevagge. Some recordings of mass-movements in the northern Scandinavian mountains. Biuletyn Peyglacjalny (Łódź), Nr. 11, 1962, p. 287–309. [Field evidence of movement on slopes under periglacial conditions.]Google Scholar

Rudberg, S. A report on some field observations concerning periglacial geomorphology and mass movement on slopes in Sweden. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 311–23.Google Scholar

Smith, H. T. U. Periglacial frost features and related phenomena in the United States. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 325–42. [General survey.]Google Scholar

Tedrow, J. C. F. Morphological evidence of frost action in Arctic soils. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 343–52.Google Scholar

Tidten, G. Ungewöhnliche Steinblock-Migrationen unter besonderen Bedingungen bei Bjönahamn, Eisfjord, Spitzbergen. Polarforschung, Bd. 5, Jahrg. 32, Ht. 1–2, 1962 [pub. 1963], p. 155–58. [Observation of remarkable boulder migrations below chffs of Tempelberg near Bjonahamn, Vestspitsbergen and attempted explanation.]Google Scholar

Vaumas, E. de. Phénomènes périglaciaires à Chypre et formation des glacis en période froide. Reme de Géomorphologie Dynamique, An. 14e, Nos. 4–5–6, 1963, p. 70–80. [Description of the periglacial formation in Cyprus before, during and after the maximum glaciation during the Riss and Würm periods.]Google Scholar

Waters, E. S. Altiplanation terraces and slope development in Vest-Spitsbergen and south-west England. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 89–101. [Comparison of landforms in Vestspitsbergen and England suggests periglacial origin for these features.]Google Scholar

Wiche, K. Le périglaciaire dans le Karakorum de l’ouest. Biuletyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 103–10. [Description of Pleistocene and current periglacial phenomena in west Karakoram.]Google Scholar

Williams, P. J. Quantitative investigations of soil movements in frozen ground phenomena. Biulelyn Peryglacjalny (Łódź), Nr. 11, 1962, p. 353–62. [Discussion of past work and presentation of a new method of determining sub-surface movements.]Google Scholar

Browning, K. A. The growth of large hail within a steady updraught. Quarterly Journal of the Royal Meteorological Society, Vol. 89, No. 382, 1963, p. 490–506.Google Scholar

Browning, K. A., and others. The density and structure of hailstones, by K. A. Browning F. H. Ludlam W. C. Macklin. Quarterly Journal of the Royal Meteorological Society, Vol. 89, No. 379, 1963, p. 75–84 Google Scholar

MacDowall, J. Tribble, D. T. Radiation observations. (In SirBrunt, D., ed. The Royal Society International Geophysical year Antarctic Expedition. Halley Bay, Coats Land, Falkland Islands Dependencies 1955–59. Vol. 3. Seismology, Meteorology. London, Royal Society, 1962, p. 111–60.) [Measurement of radiation balance at Halley Bay.]Google Scholar

Skeib, G. Einige Bemerkungen über Orographie und Witterung der Drygalski-Insel. Polarforschung, Bd. 5, Jahrg. 32, Ht. 1–2, 1962 [pub. 1963], p.132–35. [Observations of surface altitudes, temperature and wind for the ice cap on Drygalski Island, Antarctica.]Google Scholar

Gams, I. Snežišča v Julijskih Alpah . Geografski Zbornik, [Vol.] 6, 1961, p. 241–69. [Description of different types of snowfield in the Julian Alps and of meteorological factors of importance. English summary.]Google Scholar

Hoinkes, H. C. Lang, H. Winterschneedecke und Gebietsniederschlag 1957/58 und 1958/59 im Bereich des Hintereis- und Kesselwandferners (Ötztaler Alpen). Archiv für Meteorologie, Geophysik und Bioklimatologie, Ser. B, Bd. 11, Ht. 4, 1962, p. 424–46. [Comparison of five different methods of determining winter precipitation in this glacierized basin.]Google Scholar

Klyukin, N. K. Nekotoryye voprosy melioratsii klimata putem vozdeystviya na snezhnyy pokrov . Problemy Severa , Vyp. 7, 1963, p. 65–84. [Situations in north Siberia in which both hastening and retarding disappearance of snow may have helpful effects.]Google Scholar

La Grange, J. J. Rammsonde measurements for determining the density of snow. South Africa. Weather Bureau. News Letter, No. 167, 1963, p. 25–28.Google Scholar

Lied, N. T. Notes on sastrugi and snow dune observations, A.N.A.R.E. satellite station, Vestfold Hills, 1961. Australian Meteorological Magazine, No. 40, 1963, p. 35–46. [Analysis of factors affecting sastrugi and dunes.]Google Scholar

Magono, C. Sakurai, K. On the electric charge on drifting snow pellets. Journal of the Meteorological Society of Japan, Ser. 2, Vol. 41, No. 4, 1963, p. 211–17. [Measurement of electrical potential near surface of snow cover while drifting was occurring, used to deduce charge on drifting snow particles.]Google Scholar

Morandini, G. Ten years’ observations on snow in Italy 1951/52–1960/61. Bulletin de l’Association Internationale d’Hydrologie Scientifique, 8e An., No. 3, 1963, p. 101–08.Google Scholar

Picciotto, E., and others. Rate of accumulation of snow at the South Pole as determined by radioactive measurements, by E. Picciotto G. Crozaz W. de Breuck. Nature, Vol. 203, No. 4943, 1964, p. 393–94.Google Scholar

Šifrer, M. Snežišča v Kamniških Alpah . Geografski Zbomik, [Vol.] 6, 1961, p. 271–86. [Systematic survey of snowfields in Kamnik Alps and comparison with state in 1874–76. English summary.]Google Scholar