Hostname: page-component-cd9895bd7-p9bg8 Total loading time: 0 Render date: 2024-12-26T05:21:00.112Z Has data issue: false hasContentIssue false

Glaciological Literature

Published online by Cambridge University Press:  30 January 2017

Rights & Permissions [Opens in a new window]

Abstract

Type
Other
Copyright
Copyright © International Glaciological Society 1951

This biannual list of glaciological literature aims to cover the scientific aspects of snow and ice in all parts of the world Attention is drawn to the bibliographies in each number of the Polar Record (Cambridge), which aim to cover the significant work dealing with expeditions, research, equipment and conditions of living in the Polar regions. Both journals, however, deal with Polar literature having specific glaciological interest and with general matters of a practical nature such as snowcraft.

Readers will greatly assist the Editor by notifying him of their own, or any other, publication of glaciological interest.

References

Aichele, H. Frostgefährdete Gebiete in der Baar, ein kleinklimatische Geländekartierung. Erdkunde, Bd. 5, Ht. 1, p. 703. [Topographical surroundings of three frost-hollows in south-west Baden.]Google Scholar
Alimen, Henriette. Les formations glaciaires et fluvio-glaciaires de la feuille de Tarbes. Comptes Rendus hebdomadaires des Séances de l’Academie des Sciences (Paris), Tom. 227, 1948, p. 14042. [Glacial deposits of the Adour valley in south-west France.]Google Scholar
Alimen, Henriette. La biogeographic et les glaciations aux diverses époques géologiques Compte Rendu sommaire des Séances de la Société de Biogéographie, 26 Année, Nos. 228–39, 1949, p. 6373.Google Scholar
Aliverti, G. Sui coni di ghiaccio del Lys. Geofisica Pura e Applicata, Vol. 18, 1950, p. 19297. [Ice cones on the Lys Glacier.]Google Scholar
Arnold, J. R. Libby, W. F. Radiocarbon dates. Science, Vol. 113, No. 2927, 1951, p. 11120. [Dates of wood, peat, etc. including material in glacial deposits based on a new value for the radiocarbon half-life.]CrossRefGoogle ScholarPubMed
Asselberghs, E. Caractères glaciaires des couches de base du Système de Karroo dans la vallée de Kwango. Bulletin, Société Belge de Géologie, de Paleontologic et d’Hydrologie, Tom. 56, Nase. 1–2, 1947, p. 5862.Google Scholar
[Avalanches.] Vorläufige Zusammenstellung der Lawinenschäden un Winter 1950/51. Schweizerische Zeitschrift für Forstwesen, Jahrg. 102, No. 4, 1951, p. 22728. [The 1951 Swiss avalanches; preliminary statement]Google Scholar
Bates, Charles C. Lill, Gordon G. Current naval research in land and sea ice. Transactions American Geophysical Union, Vol. 35, No. 2, 1950, p. 27881. [Reviews some recent work and states plans for future.]Google Scholar
Behrmann, Walter. Albrecht Penck. Petermann: Geographische Mitteilungen, 92 Jahrg., 3/4, Quartaisheft, 1948, p.19093. [Obituary.]Google Scholar
Biörslö, Nils. Israndstudier i sodra Bohuslän. Sverige: Geologiska Undersiikning, Avhandlingar ach Uppsatser, Ser. C., No. 504, Årsbok 43, No. 2, 1949, 351 p., illus., maps, tables, diagrs. [Determination of positions of marginal deposits in southern Bohuslän, west Sweden; reconstruction of progress of ice melting by study of retreat of ice front. English summary.]Google Scholar
Black, Robert F. Permafrost. Taask, P. D., ed. Applied sedimentation. New York, John Wiley and Sons, [c1950], p. 24775, map, diagrs. [Comprehensive summary of available literature on extent, nature and origin of permafrost in northern hemisphere, and on engineering problems caused by it.]Google Scholar
Boch, S. G. Yeshche veskal’ko zamechaniy o prirode snegovoy erozii. [Some further remarks on the nature of snow erosion.] Izvestiya Vsesoyuznogo Geograficheskago Obshchestva [News of the.All-Union Geographical Society] (Leningrad), Tom 80, No. 6, 1948, p. 60911. [Geomorphological action of snow patches observed in polar Ural in 5946.]Google Scholar
Boettcher, P. The avalanche catastrophe in the Alps, 19–21 January 1951. Weather, Vol. 6, No. 4, 1951, p. 10507, illus. [Brief account of weather conditions.]CrossRefGoogle Scholar
Bonacina, L. C. W. Snowfall in the British Isles during the decade 1936 to 1445. British Rainfall, 1948, Part 3, p. 20812. [Third historical survey; severe snowstorm in northern and eastern England, January 1940, was bordered in western England by an extensive and destructive ice storm.]Google Scholar
Brooks, C. E. P. Post-glacial climatic changes in the light of recent glaciological research. Geografuka Annaler, Årg. 31, Ht. 1–4, 1949, p.2124. [The importance of the “polar front.”]Google Scholar
Brooks, C. E. P. Oceans through the ages. Marine Observer, Vol. 21, No. 152, 1951, p. 10310. [Development of the ocean basins in relation to Precambrian, Permo-Carboniferous and Pleistocene glaciations; holds that present period is an interglacial one.]Google Scholar
Brouwer, A. De glacigene landschapstypen in Nederland. Tijdschrift van het Koninklijk Nederíandsch Aardrijkskundig Genootzchap, Deel 67, No. 1, 1950, p. 2032. [Northern part of the Riss II glacial stage in Holland exhibits typical old ground moraine landscape; south of river Vecht well developed push moraines occur.]Google Scholar
Bryan, Kirk. The erroneous use of Tjaelr as the equivalent of perennially frozen ground. Journal of Geology, Vol. 59, No. 1, 1951, p. 6971.Google Scholar
Büdel, Julius. Die räumliche und seitliche Gliederung des Eiszeitklimas. The Naturwissenscrtaften, 36 Jahrg., Ht. 4, 1949, p. 10512; Ht. 5, 1949, p.133–39. [Reconstructs height of snow-line in last glaciation, climatic vegetation zones of Europe, and thereby type of landscape.]Google Scholar
Cahen, L. À propos de formations éoliennes périglaciaires de la Série de Murashya. Bulletin de la Société Belge de Géologie, de Paléontologie et d’Hydrologie, Tom. 56, 1947, p.915.Google Scholar
Carlston, Charles W. Pleistocene history of coastal Alabama. Bulletin of the Geological Society of America, Vol. 61, No. 10, 1450, p. 111930.Google Scholar
Champion, D. L. Ablation in the Scottish Highlands. Meteorological Magazine, Vol. 79, No. 940, 1950, p. 29295. [Observations in the Cairngorms, July, 1949, showed that melting and not evaporation was the chief cause of ablation.]Google Scholar
Colbertaldo, D. di. Nuove osservazioni sui ghiacciai del Canin e del Montasio. Universo, An. 26, No. 2, 1948, p. 16685. [Description of two small transitional types of glaciers in the karst region of the western Julian Alps.]Google Scholar
Corte, A. E. La expedicion Britanica-sueca-norvega (1949–1952). Boletin de Esiudio Geograficos (Universidad Nacional de Cuyo), Vol. 1, No. 4, 1949, p.3744 Google Scholar
von Cbeutzburg, N. Erich Drygalsha und die deutsche Geographie. Erdkunde, Bd. 3, Ht. 2/3, 1949, p. 6568. [Obituary.] Caoca, K. Die Entwicklung der firhneeräummsschinen für Strassen in den Jahren 1949/50. Strasse und Autobahn, 1950, Ht. 10, p. 8–14. [Recent developments in snow clearance apparatus.]Google Scholar
David, A. Irrigations et glaciologie [à propos du bassin de la Durance.] Revue de Géographie Alpine (Grenoble), Vol. 39, Fase 2, 1951, p. 31723. [Decrease of ice reserves for irrigation.]CrossRefGoogle Scholar
Dewey, E. S. Late-glacial and post-glacial pollen diagrams from Maine. American Journal of Science, Vol. 249, No. 3, 1951, p. 177207. [A tundra climate preceded the post-glacial forest advance and corresponds with the late, glacial phase of Northern Europe.]Google Scholar
Defant, A. Konvektion und Eishereitschaft in polaren Schelfmeeren. Geografiska Anneler, Årg. 31, Ht. 1–4, 1949, p. 2535. [Effect of convection on ice formation in the northern seas.]Google Scholar
Ekhart, E. Das Temperaturfeld der Alpen und seine Jahresperiode. Geografiska Annaler, Årg. 32, Ht. 1–2, 1950, p. 136.Google Scholar
Evers, W. Die morpologisch-tektonischen Ursachen der diluvialen Vereisung Norddeutschlands. Deutsche Geographische Blauer (Bremen), Bd. 45, Ht. 1–2, 1949, p. 724. [Morphological and tectonic causes of the Pleistocene ice sheets in north Germany.]Google Scholar
[Expeditlons.] Polar Record, Vol. 5, No. 40, 1950, p. 589620. [Brief account of many expeditions to Polar regions including Juneau Ice Field Project, 1948; Durham University Expeditions to Iceland, 1948 and 1949; Oxford University Expedition to North East Land (Nordauatlandet); Oceanographical Investigations at Point Barrow, Alaska, 1949.]Google Scholar
Eythórsson, Jón. Temperature variations in Iceland. Geografiska Anneler, Årg. 31, Ht. 1–4, 1949, p. 3655. [Temperature variations since 1871, precipitation and glacial recession.]Google Scholar
Fels, Edwin. Erich von Drygalski, 9.2.1865–10.1.1949. Die Erde, Ht. 1, 1949, p. 6672. [Obituary and bibliography of writings.]Google Scholar
Fiels, Edwin. Die Alpen und die Eiszeit. Die Erde, 1949–50, Ht. 3–4, p. 26772. [Truth concerning ice erosion in the Alps probably lies between extreme views, the present morphology being partly pre-glacial.]Google Scholar
Flint, Richard Foster. Pleistocene drainage diversions in South Dakota. Geografiska Annaler, Årg. 31, Ht. 1–4, 1949. p. 5674. [Main changes from former to present drainage system in Missouri basin occurred in Kansan (second) glaciation.]Google Scholar
Flint, Richard Foster. Highland centers of former glacial outflow in northeastern North America. Bulletin of the Geological Society of America, Vol. 62, No. 1, 1991, p. 2138. [Local glaciers at high levels probably preceded the general ice sheets in north-eastern North America.]Google Scholar
Flint, Richard Foster Dating late-Pleistocene events by means of radiocarbon. Nature. Vol. 167, No. 4256, 1951, p. 83336.CrossRefGoogle ScholarPubMed
Flint, Richard Foster Deevey, Edward S. (Jr.). Radiocarbon dating of late-Pleistocene events. American Journal of Science, Vol. 249, No 4. 1951, p. 257300.Google Scholar
Glaister, R. M. Avalanche of the Glacier du Tour. Weather, Vol. 5, No. 4, 1950, p. 13839.Google Scholar
[Glaciological Methods.] Proceedings of the 1947 conference on snow and ice. Canada.National Research Council, Associate Committee on Soil and Snow Mechanics, Technical Memorandum No. 10, 1947, [ii], 35 + [9] pages. [Conference held in Ottawa 17–18 September 1947 under the joint auspices of the Associate Committees on Soil and Snow Mechanics and on Geodesy and Geophysics.]Google Scholar
Godwin, H. Comments on radiocarbon dating for samples from the British Isles. American Journal of Science, Vol. 249, No. 4, 1951, p. 30107. [Reviews value of this method for Quaternary research; some results confirm previous estimates of age, others are discordant.]Google Scholar
Gordon, Seton. Snow flora of the Scottish hills. Nature, Vol. 165, No. 4187, 1950, p. 13234. [Many details of the Scottish snow beds and summer conditions; flora following the snow.]Google Scholar
Grierson, John. Air whaler. London, Sampson Low, Marston & Co., Ltd., 1949. xii, 243 p., illus., maps, 22 cm. 18s. [Voyage of floating factory Beleena, Antarctic season 1946–47, with special reference to work by aircraft under author's command; includes sea ice distribution maps.]Google Scholar
Groissmayr, Fritz Béla. Die Einflussnahme der Wintertemperatur in Oat-Island aufjene des darauffolgenden Sommers. Polarforschung, Jahrg. 17, Bd, 2, Ht, 1/2, 1947, p. 16364. [Attempt to correlate some winter temperatures with those of following summers.]Google Scholar
Groissmayr, Fritz Béla. Die gewaltige Temperaturkompensation im Dezember: Barents-Seeregion und Weisses Meer mit Turkestan, Polarforsckung, Jahrg. 17, Bd. 2, Ht. 1/2, 1947, p. 149. [Two tables showing comparative temperatures of Tashkent and Sörvaranger, 1881–1940, and Arkhangelsk and Tashkent, 1884–1936.]Google Scholar
Guichonvrt, P. La catastrophe du Glacier du Tour. Revue de Géographie Alpine (Grenoble), Vol. 38, Fasc. 1, 1950, p. 198201. [Cause of the avalanche attributed to sudden temperature changes after hot summers.]Google Scholar
Gvlnchidze, N.M. Snezhnyye laviny i bor’ba s nimi. [Snow avalanches and the struggle against them.] Priroda [Nature] (Moscow), No. 11, 1948, p. 8082. [Work done in the Caucasus and Kol'ski Poluostrov.]Google Scholar
Hansen, H. P. Postglacial forests along the Alaska Highway in British Columbia. Proceedings of the American Philosophical Society, Vol. 94, No. 5, 1950, p. 41121 [Pollen analysis of peat sections from bogs and muskegs along the Alaska Highway.]Google Scholar
Hennig, R. Die Erwátmung der Arktis. Wetter und Klima. Bd. 2, Ht. 1/2, 1949, p. 4955.Google Scholar
Herrmann, R. Das Durchbcuehstal der Weser zwischen Holzminden und Bodenwerder. Geoldgisches Jahrbuch, Bd. 65, 1950, p. 61120.Google Scholar
Hobbs, William Herbert. New interpretation of the deposits of the Pleistocene continental glaciers. Papers of the Michigan Academy of Science, Arts and Leiters, Vol, 32, 1946 [pub. 1948], p. 18793. [Shows in tabular form the principal contrasts between Alpine and Continental glaciers.]Google Scholar
Hoppe, Gunnar. Några exempel på glacifluvial dränertng från det inre Norrbotten. Geografiska Anneler Årg. 32, Ht. 1–2, 1951, p. 3759.Google Scholar
Horberg, L. Intersecting minor ridges and periglacial features in the Lake Agassiz basin, North Dakota. Journal of Geology, Vol. 59, No. 1, 1951, p. 118. [Suggests ridges representing frozen-ground structures formed during retreat of the late Wisconsin ice.]Google Scholar
[Icebergs.] Southern ice reports during the year 1948. Marine Observer, Vol. 59, No. 144, 1949. p. 120.Google Scholar
[Japan. Central Meteorological Observatory.] The climatographic allas of Japan. Second Series, Climatography of snow and ice. Tokyo, Central Meteorological Observatory, 1949. Maps.Google Scholar
Jayet, A. Sur la surgissement et la ségrégation de matériaux erratiques profonds dans la moraine transversale du Glacier de Valsorey (Valais, Suisse). Archives des Sciences (Genève), Vol. 2, Fasc. 3, 1949, p. 53133. [Doubts the fluviatile or lacustrine origin of gravels near this glacier.]Google Scholar
Joerg, W. L. G. Erich von Drygalski. Geographical Review, Vol. 40, No. 3, 1950, p. 48991. [Obituary.]Google Scholar
Kirwan, L. P., and others. Glaciers and climatology; Hans W: son Ahlmann's contribution. By L. P. Kirwan, C. Mason Mannerfelt, C. G. Rossby and V. Schytt. Geografiska Annaler, Årg. 31, Ht. 1–4, 1949, p. 1520. Google Scholar
Kirwan, L. P. An international expedition to Antarctica. Geographical Magazine, Vol. 22, No. 7, 1949, p. 28088, illus., map. [Norwegian-British-Swedish Expedition to Dronning Maud Land, 1949–52; programme and preparations.]Google Scholar
Klein, George, J. Canadian survey of physical characteristics of snow-covers. Geografiska Annaler, Årg 31, Ht. 1–4, 1949, p. 10624. [Instruments and methods.]Google Scholar
Klute, Fritz. Rekonstruktion des Klimas der letzten Eiszeit in Mitteleuropa auf Grund morphologischer und pflanzen-geographischer Tatsachen. Geographische Rundschau, Jahrg. 1, No. 3, 1949, p. 8189; No. 4, 1949, p.121–26, maps.Google Scholar
Köhler, H. On evaporation from snow surfaces. Arkiv för Geofysik, Bd. 1, No. 8, 1950, p. 15985. (Equations and data.]Google Scholar
Köhler, H. On the problem of condensation in the atmosphere. Nova Acta Regis Societatis Scientiarun Upsaliensis, Ser. W, Vol 14, No. 9, 1950, p. 176. [Investigation of new ideas and new deductions from author's earlier investigations.Google Scholar
Lafargue, C. On the freezing of droplets of water and of aqueous solutions. Centenary Proceedings of the Royal Meteorological Society, 1950, p. 6163. [The freezing of droplets at –41° C. seems to be a molecular property of water and may not be caused by a freezing nucleus.]Google Scholar
Lagunov, I.L Redkaya po obifiyu snega aima 1946/47 g. na Kaznachatke [An uncommonly snowy winter in 1946–47 in Kamchatka]. Priroda [Nature] (Leningrad), No. 9, 1948, p. 95. [Two and a half times normal snowfall in southeastern Kamchatka.]Google Scholar
Lamb, H. H. Ablation in the Scottish Highlands. Meteorological Magazine, Vol. 80, No. 944, 1951, p. 58. [Letter.]Google Scholar
Lamont, Arthur H. Ice conditions over Hudson Bay and related weather phenomena. Bulletin American Meteorological Society, Vol. 30, No. 8, 1949, p. 28889. [Nature and extent of sea ice; observed weather in relation to ice conditions.]Google Scholar
Lawrence, Donald B. Lawrence, Elizabeth G. Some glaciers of southeastern Alaska. Mazama (Portland, Oregon),Vol. 31, No. 13. 1949,.p. 2430. [Deals inter alla with the advance of the Taku Glacier.]Google Scholar
Van Leckwijk, W. Macar, P. Phénomènes pseudo-tectoniques la plupart d’origine périglaciaire dans les dépôts sablograveleux dits “ONX” et les terrasses fluviales de la région liégeoise. Memories de la Société Géologique de Belgique, Torne 73, Fasc. 1, 1949–50, 78 p. [Description of pertglacial phenomena in the Liége district.]Google Scholar
Leighly, J. On contimttality and glaciation. Geografiska Annaler, Årg. 31, Ht. 1–4, 1949, p. 13345. [Influence of an ice sheet on anticyclonic flow and consequent extension of the ice sheet.]Google Scholar
Leighton, Morris M. Willman, H. B. Loess formations of the Mississippi Valley. Journal of Geology, Vol. 58, No. 6, 1950, p. 599623 Google Scholar
Lemée, Georges Böubdiek, Franck. Une flore pollinique tempérée incluse dans les moraines dites würmiennes d’Armoy près de Thonon (Haute-Savoie) Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences, Tom. 230, No. 26, 1950, p.231354.Google Scholar
Lend, E. Neuere gletscherkundliche Forschungen im nordöstlichen Sibirien. Mitteitungen der Geographischen Gesellschaft Wien, Bd. 90, Ht. 1–12, 1948, p. 11214. [Review of recent Russian glaciological work in north-east Siberia.]Google Scholar
Leopold, Luna B. Pleistocene climate in New Mexico. American Journal of Science, Vol. 249, No. 2, 1951, p. 15268. [Postulate that snow lines are controlled by summer temperatures is applied to the ice age temperature in New Mexico.]Google Scholar
Lawis, W. Vaughhan. Glacial movement by rotational slipping. Geografiska Annaler, Årg. 31, Ht. 1–4, 1949, p. 14658.Google Scholar
Löfquist, Bertil. Lifting force and bearing capacity of an ice sheet. Canada. National Research Council. Technical Translation TT–164, 1951, 27 pages. [Translation of paper by author in Teknisk Tidsknft (Stockholm), No. 25, 1944.]Google Scholar
Luolam, F. H. The structure of shower clouds. Nature, Vol. 167, No. 4242, 1951, p. 25456. [Not essential that presence of the crystals is necessary for rain production]Google Scholar
Ludlam, F. H. Wexler, R. The growth of ice particles in cumulonimbus. Weather, Vol. 5, No. 7, 1950, p. 262. [Letter.]Google Scholar
Lucbon, Maurice Jeremine, Elisabeth. Sur la confirmation de la présence d’un Précambrien d’origine glaciaire en Normandie (Manche), Comptes Rendus Hebdomadaires des Séances de l’Académie des Sciences, Tom. 230, No. 18, 1950. p.154950 Google Scholar
Lysgaara, Leo. On the present climatic variation. Centenary Proceedings of the Royal Meteorological Society, 1450, p. 206210. [Rise of temperature and decline of pressure in northern hemisphere.]Google Scholar
McFarlane, W. T., and others. Glacier survey in Banff and Jasper National Parks, 1949, by McFarlane, W. T. R. V., Blair Ozga, W. J. Canadian Alpine Journal, Vol. 33, 1950, p. 12026. Report on five glaciers; records kept annually since 1945 by Alpine Club of Canada.]Google Scholar
Manley, Gordon. The snowhne in Britain. Geografiska Annaler, Årg. 31, Ht. 5–4, 1949, p. 17993. [Theoretical glaciation level on Ben Nevis has risen some 90 m. since the period 1884–1903]Google Scholar
Manley, Gordon. The range of variation of the British climate. Geographical Journal, Vol. 117, No. 1, 1951, p. 4368. [Range and possible trend of variation in British climate as deduced from fluctuations in historic and prehistoric times.]Google Scholar
Mannerfelt, Carl M:son. Marginal drainage channels as indicators of the gradients of Quatemary ice caps. Geografiska Annaler, Årg. 31, Ht. 1–4, 1949, p. 19499.Google Scholar
Maran, Josef. Vliv ledovfrch dob na faunu Europy. Sbarnfk Ceskoslovenské spolecnostiZemépisné, Vol. 52, Part 2, 1947. p. 4146, and Part 3, 1947, p. 96–103. (The influence of the glacial period on the fauna of Europe.]Google Scholar
Mawson, Sir Douolas. The Elatina glaciation: a third occurrence of glaciation evidenced in the Adelaide system. Transactions of the Royal Society of South Australia, Vol. 73, Pt. 1, 1949, p. 11721. [A fading phase of the Late-Proterozoic glaciation.]Google Scholar
Meinardus, Wilhelm. Erich von Drygalski. Petermann Geographische Mitteilungen, Jahrg. 93, Ht. 4, 1949, p. 17780. [Obituary.]Google Scholar
Mercanton, P.-L. L’aceroisement du grain du glacier. Actes de la Société Helvétique des Sciences Naturelles (Lausanne), 1949, p. 12223. [Accords with Seligman's findings in certain glaciers and awaits general confirmation.]Google Scholar
Mercanton, P.-L. Conférence de météorologie et de glaciologie alpine. Die Alpen, [Bd.] 26, [Ht.] 11, 1950, p. 215.[Conference held at Milan and Turin, 1950.]Google Scholar
Mercanton, P.-L. Examen de quelques formules pour la prédetermination de l’épaisseur du glacier, á l’occasion de sondages recent,. Geaftsica Pura e Applicata. Vol. 18, 1950, p. 17074.Google Scholar
Miller, Maynard Malcolm. Alaskan glacier studies, 1946. American Alpine Journal, Vol. 6, No. 3, Issue 20, 1947, p. 33943, illus.Google Scholar
Miller, Maynard Malcolm. 1948 season of the Juneau Ice Field research project. American Alpine Journal, Vol. 7, No. 2, Issue 22, 1949, p. 18591, illus. [First season of field work.]Google Scholar
Miller, Maynard M. Preliminary report of field operations. The Juneau Ice Field Research Project, 1949 season. New York: American Geographical Society, Jan. 20, 1950. 37 pages, Maps, diagrs., 5 Appendixes. (Mimeographed.)Google Scholar
Mitchell, G. F. Two inter-glacial deposits in south-east Ireland. Proceedings of the Royal Irish Academy, Vol. 52, Sec. B, No. 1, 1948, p. 114. [Description of Ardcavan and Kilbeg deposits with notes on their ages.]Google Scholar
Morawetz, S. Zur Frage der Eiserosion. Mitteilungen der Geographischen Gesellschaft Wien, Bd. 91, Ht. 1–6, 1949, p. 1420. [Methods of deciding extent of glacial erosion by measuring quantity of transported deposits.]Google Scholar
Muchnik, V. M. Nekotoryye sluchai obrazovaniya snezhnykh agregatov. [Some cases in which snowflake aggregates have been formed]. Priroda [Nature] (Leningrad), No. 9, 1950, p. 5455. [Examination of ways in which snow crystals combine to form conglomerate masses in the air.]Google Scholar
Nichols, Robert L. Miller, Maynard M. Glacial geology of Ameghino Valley, Lago Argentino, Patagonia. Geographical Review, Vol. 41, No. 2, 1951, p. 27494. [Oscillations of the Ameghino glaciers from the maximum “Wisconsin” advance until today.]Google Scholar
Nilsson, E. The pluvials of East Africa: an attempt to correlate Pleistocene changes of climate. Geografiska Annaler, Årg. 31, Ht. 1–4, 1949, p. 20411. [Includes table correlating the main Pleistocene climatic phases in many parts of the world.]Google Scholar
Penck, Albrecht. Sechzig Jahre Eiszeitforschung. The Erde. Zeitschrift der Gesellschaft für Erdkunde zu Berlin, 1949, Ht. 1, p. 511. [Autobiography.]Google Scholar
Pleshkova, T. T. Al’bedo zemnykh obrazovaniy [Albedo of formations on the earth's surface]. Priroda [Nature] (Leningrad), No. 10, 1948, p. 4449. [Techniques used and results obtained in measuring albedo of various surfaces, including snow and sea ice; work of both Russian and foreign scientists.]Google Scholar
Putnam, W. L. Snow Conditions II: Fresh and powder snow avalanches. Appalachia, Vol. 16, No. 8, (Magazine No. 110) 1950, p. 17175.Google Scholar
Quervain, M. de. Zur Entstehung der Lawinen. Leben und Umwelt. Jahrg. 7, Ht. 6, 1951, p. 22131. [Avalanche types and recent research.]Google Scholar
Rafside, J. D. Some post-glacial climatic changes in Canterbury [N.Z.] and their effect on soil formation. Transactions of the Royal Society of New Zealand, Vol. 77, Pt. 1, 1948, p. 15371. [During the 7th and 13th centuries temperature was at least 2° C. warmer than now.]Google Scholar
Rakovec, Ivan. The valley of the Vrata during the Pleistocene Period and the development of the Perienik waterfall. (In Slovene with English summary). Geografiski Vestnik (Ljubliana) Vol. 20–21, 1948–9. p. 25167. [Glacier action is evident in this part of Carniola. (Slovenia)].Google Scholar
Ray, Louis L. Kirk Bryan. Geographical Review, Vol. 41, No. 1, 1951, p. 16566. [Obituary.]Google Scholar
Richards, H. G. Postglacial marine submergence of arctic North America with special reference to the Mackenzie Delta. Proceedings of the American Philosophical Society, Vol. 94, No. 1, 1950, p. 3137. [Delta region may have been submerged Soo ft. or more during late glacial time, so that sea level may have extended as far as Great Slave Lake.]Google Scholar
Rosendahl, Halvor. Albrecht Penck. Norsk Geografisk Tidsskrsft, Bd. 12, Ht. 2, 1949 p. 5760. [Obituary.]Google Scholar
Ruegc, Werner. La glaciation de la parte meridional de Is Cordillera Blanca. Informaciones y Memories de la Sociedad de Ingenieros del Peru, Vol. 1, No. 3, 1950, p. 17072. [Reply to “Die Vergletscherung in der Südhälfte der Cordillera Blanca (Peru)” by Hans Kinzl, Zeitschrift für Gletscherkunde und Glazialgeologie, Bd. 1, Heft 1, 1949, p. 1–28.]Google Scholar
Schwarzbach, Martin. Das Klima der Vorzeit. Stuttgart, Ferdinand Enke, 1950. viii, 211 pages, illus. [An introduction to pakeoclimatology.]Google Scholar
Schytt, Valter. Refreezing of the melt-water on the surface of glacier ice. Geografiska Annaler, Årg. 31, Ht. 1–4, 1949, p. 22227. [This adventitious ice layer, different in texture to glacier ice, gives valuable information about temperatures at the start of the ablation season.]Google Scholar
Seligman, Gerald. Research on glacier flow: an historical outline. Geografiska Annaler, Årg. 31, Ht. 1–4, 1949, p. 22838. [Sixteenth century to modern times.]Google Scholar
Sestoft, I. A geophysical theory of the Ice Ages. Union Géodésique et Géophysique Internationale. Huitième Assemblée Générale, Oslo, Norvège, Aunt 1948. Procès-Verbaux des séances de l’Association de Météorologie. Il. Mémoires et Discussions, No. 33, p. 16569. [Concludes inter alia that the present age is post-glacial, not interglacial.]Google Scholar
Sharp, Robert P. Status report of glaciological work on the Seward Ice Field, Yukon Territory. American Alpine Journal, Vol. 7, No. 2, Issue 22, 1949, p. 17883. [Project “Snow Cornice,” 1948.]Google Scholar
Sharp, Robert P. Glacial-meteorological investigations in Swedish Lappland. Arctic, Vol. 3, No. 2, 1950, p. 11316. [Review of recent work (Geografiska Annaler Årg. 30 and 35) by Dr. C. Wallin on the Kårsa Glacier.]Google Scholar
Sharp, Robert P. Glacial history of Wolf Creek, St. Elias Range, Canada. Journal of Geology, Vol. 59, No. 2, 1951, p. 97117. [Review of glaciation and glacierization in an area some 55 miles north of Mt. Logan.]Google Scholar
Sigafoos, R. S. Hopkins, D. M. Frost-heaved tussocks in Massachusetts. American Journal of Science, Vol. 249, No. 4, 1951, p. 31217.Google Scholar
Soule, Floyd M. Arctic ice drift and the Humboldt Current. Science, Vol. 112, No. 2898, 1950, p. 6162. [Disputes Boone's contention (Science, Vol. 110, 1949, p. 642) that heavy ice seasons in north Atlantic produce abnormalities in the Humboldt Current three years later.]Google Scholar
Sourbier, Messines du. Note sur l’éboulement du Glacier du Tour (Haute-Savoie) 14 Août 1949. Mémoires et Travaux de la Société Hydrologique de France, Vol. 1, 1950, p. 5660. [Detailed account of slide of the glacier; probable causes.]Google Scholar
Suter, K. Die eiszeitliche Vergletscherung des Nordapennines. VierteIjdhrsschrift des Naturforschenden Gesellschaft in Zürich, Jahrg. 95, Ht. 3, 1950, p. 22541. [The northern Apennines were only affected by the Würm glaciation according to the evidence of moraines and cirques.]Google Scholar
Synge, F. M. The glacial deposits around Trim, Co. Meath. Proceedings of the Royal Irish Academy, Vol. 53, Sec. B, No. 10, 1951, p. 99110. [Recession of last ice sheet north-westerly with one main halt or re-advance; speed 250–425 ft. a year.]Google Scholar
Thoral, M. Bourdier, F. Sur le mode de formation et l’âge des alluvions dites préglaciaires aux environs de Lyon. Comptes Rendus hebdomadaires des Séances de l’Académie des Sciences (Paria), Tom. 229, 1949, p. 102224.Google Scholar
Thorarinsson, Sigurdur. Some tephrochronological contributions to the volcanology and glaciology of Iceland. Geografiska Annaler, Årg. 31, Ht. 1–4, 1949, p. 23956. [Chronology by the various interstratified volcanic ash layers.]Google Scholar
Troll, Carl. Die Tagung der Deutschen Quartür-Vereinigung im Alpenvorland, September 1950. Erdkunde, Bd. 5, Ht. 1, 1950, p. 8587. [Account of meetings of Deutsche Quartür-Vereinigung, September 1950.]Google Scholar
Trdnov, M. V. Ob ustoychivosti lednikov [On the stability of glaciers]. Izvestiya Vsesoyuanogo Geograflcheskogo Obshchestva [News of the All-Union Geographical Society] (Leningrad), Tom 80, No. 5, 1948, p. 47688. [Factors influencing changes in size and character of glaciers; based chiefly on work done in Altay.]Google Scholar
Vaudaux, L. Les avalanches des ao et 21 janvier 1951 dans les alpes suisses, autrichiennes et italiennes. Revue de Géographie Alpine (Grenoble), Vol. 39, Fasc. 2, 1951, p. 28192. [Description of avalanches and conditioning factors of depth and character of snow cover, temperature and wind.]Google Scholar
Veyret, Paul. Visite aux Glaciers Alpins. Revue de Geographie Alpine (Grenoble), Vol. 39, Fasc. 1, 1951, p. 18992. [Journey of glacier investigation by Société Hydrotechnique de France.]Google Scholar
Viret, J. Une contribution à l’histoire des glaciations alpines, la faune de loess durci de Saint-Vallier (Drtime). Revue de Geographie de Lyon, Vol. 23, No. 4, 1948, p. 2272.Google Scholar
Wallen, C. C. Recent variations in the general circulation as related to glacier retreat in northern Scandinavia. Geofisica Pura e Applicata, Vol. 18, 1950, p. 17578.Google Scholar
Weichert, W. Die Schneedecke im Rheinischen Schiefer-Gebirge und ihre synoptisch-meteorologischen Bedingungen. Decheniana (Bonn), Bd. 104,1950, p. 10344. [Average number of days with snow cover increases by 10 or 11 days, and mean maximum depth of cover by 5 cm., for each 100 m. rise.)Google Scholar
Welters, R. Nachweis der Günz Eiszeit und der Günz-Mindel-Wármezwischenzeit am Niederrhein (Vorlaüfige Mitteilung) Geologisches Jahrbuch, Bd. 65, 1950, p. 76972.Google Scholar
Wiklander, L. Mineralogical composition of Quatemary Swedish clays. Nature, Vol. 166, No. 4215, 1950, p. 27778. [These clays not “rock flour” from granite, gneiss, etc., since they consist lÅrgely of illite.]Google Scholar
Willett, H. C. Temperature trends of the past century. Centenary Proceedings of the Royal Meteorological Society, 1959, p. 195206. [The trend is upward since about 1885 and is most pronounced in higher middle and polar latitudes of the northern hemisphere, but negative in those of the southern.))Google Scholar
Wiseman, J. D. H. Geology of the deep-sea floor. Nature, Vol. 164, No. 4173, 1949, p. 68284. [Summary of six papers presented to the British Association, Newcastle-upon-Tyne, September 1949; includes chronology and recording processes of Pleistocene climatology.]Google Scholar
Woldstedt, P. Das Vereisungsgebiet der Britischen Inseln und seine Beziehungen zum festlilndischen Pleistoziin. Geologisches Jahrbuch, Bd. 65, 1950, p. 62140.Google Scholar
Woldstedt, P. Norddeutschland und angrenzende Gebiete im Eiszeitalter. Stuttgart, K. F. Koehler Verlag, 1950. xii, 464 pages, maps, diagra. [Geomorphological development and character of area from the Netherlands to central Poland In Pleistocene and Recent times.]Google Scholar
Yardley, D. H. Frost-thrusting in the Northwest Territories. Journal of Geology, Vol. 59, No. 1, 1951, p. 6569. [Frost-thrust blocks date since the area was last covered by glaciers, and frost-thrusting is occurring now.]Google Scholar
Zenari, S. Un esempio di “Cattura glaciale” in Cadore. Anti del XIV Congresso Geografico Italian tenuto a Bologna 8 al 12 Aprile 1947, p.35254. [Example of “glacial capture” in the Venetian Alps causing the lower part of the glacier to flow in a different channel from the upper.]Google Scholar
Zeuner, F. E. Dating the past by radioactive carbon. Nature, Vol. 166, No. 4227, 1950, p. 75657. [The principles, method and scope of this process.]Google Scholar
Zonneveld, J. L. S. Over de noordelijke inslag in enkele Nederlandse sedimenten. Tijdschrift van het Konink. Nederlandsch Aadrijkskundig Genootschap (Amsterdam), Vol. 65, 1948, p. 2638. [Certain mineral sediments in Holland may come from the Rhine and not from a Scandinavian glacier as once thought.]Google Scholar