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Worsley, P. An evaluation of the attempt to date the recession of Tunsbergdalsbreen, southern Norway, by lichenometry. Geografiska Annaler, Vol. 55A, Nos. 3-4, 1973, p. 137–41. [Critical comment on paper by D. N. Mottershead and White., I. D, ibid., Vol. 54A, No. 2, 1972, p. 47–52.]Google Scholar

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Are, F. E. ed. Ozera kriolitozony Sibiri [Lakes of the permafrost zone of Siberia]. Novosibirsk, Izdatel’stvo “Nauka”, 1974. 159 p. [Formation and characteristics.]Google Scholar

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Cramptonc., B. Studies of vegetation, landform and permafrost in the Mackenzie valley: landscape survey in the upper and central Mackenzie valley.Canada. Task Force on Northern Oil Development. Environmental-Social Committee, Northern Pipelines. Report No. 73-8, 1973, 67 p. [Landscape of upper and central reaches of Mackenzie River valley mapped, using air photographs and ground inspection.]Google Scholar

Faheyb., D., Thompson, R.D., ed. Research in polar and alpine geomorphology. Proceedings: 3rd Guelph symposium on Geomorphology, 1973. Norwich, University of East Anglia, Geo Abstracts Ltd.; Guelph, Ontario, University of Guelph, Dept. of Geography, “Geomorphology Symposium”, [’1973]. [x], 206 p. (University of Guelph, Dept. of Geography, Geographical Publication No. 3.) [Includes the following papers: Ives, J.D., “Arctic and alpine geomorphology—a review of current outlook and notable gaps in knowledge, p. 1-10; Black, R.F., “Cryomorphic processes and micro-relief features, Victoria Land, Antarctica”, p. 11-24; Brown, R.J.E. “Ground ice as an initiator of landforms in permafrost regions”, p. 25-42; Rampton., V. N, “The influence of ground ice and thermokarst upon the geomorphology of the Mackenzie-Beaufort region”, p 43-59; Kerfoot., D. E, “Thermokarst features produced by man-made disturbances to the tundra terrain”, p. 60-72; Tallman, A.E., “Resistivity methodology for permafrost delineation”, p. 73-83; Johnson., J. P, “Some problems in the study of rock glaciers”, p. 84-94; Gardner., J. S, “The nature of talus shift on alpine talus slopes: an example from the Canadian Rocky Mountains”, p. 95-106; Gray., J. T, “Geomorphic effects of avalanches and rock-falls on steep mountain slopes in the central Yukon Territory”, p. 101-17; McCann, S.B.,Cogley., J. G, “The geomorphic significance of fluvial activity at high latitudes”, p. 118-35; Miller., M. M, “Entropy and self-regulation of glaciers in the Arctic”, p. 136-58; Goldthwait, R.P., “Till deposition versus glacial erosion”, p. 159-66; Calkin%., P. E, “Glacial processes in the ice-free valleys of southern Victoria Land, Antarctica”, p. 167- 86; C. Holdsworth, “Ice deformation and moraine formation at the margin of an ice cap adjacent to a proglaciallake”, p. 187– 99.]Google Scholar

French, H. M. Active thermokarst processes, eastern Banks Island, western Canadian Arctic. Canadian Journal of Earth Sciences, Vol. II, No. 6, 1974, p. 785–94. [Describes features in this area of continuous permafrost, remarking on numerous ground ice slumps in area west of Johnson Point.]Google Scholar

Fukuda, M. Inoue, M. Tōdo no dōteki seishitsu ni tsuile. I [On the dynamic moduli of frozen soils. I]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 31, 1973, p. 245–59. [Measurement of velocities of compressive and shear waves through frozen soil under different temperature and moisture conditions. English summary, p. 259.]Google Scholar

Gell, A. A contact between massive ice and wedge ice, Tuktoyaktuk coast, District of Mackenzie (107C). Project 680047. Canada. Geological Survey. Paper 74-1, Pt. B, 1974, p. 245–46. [Petrologic characteristics of massive and wedge ice are described to aid recognition of ice type from limited core samples or from poor exposure.]Google Scholar

Halstead, C. A. Soil freeze-thaw recording in the southern uplands of Scotland. Weather, Vol. 29, No. 7, 1974, p. 261–65. [Measurement of soil temperatures in the Lowther Hills.]Google Scholar

Hannell, F. G. The thickness of the active layer on some of Canada’s Arctic slopes. Geografiska Annaler, Vol. 55A, Nos. 3-4, 1973, p. 177–84. [Presents results of sub-surface temperature measurements down to a depth of 1 m, made near south-west coast of Devon Island, and discusses implications of these.]Google Scholar

Hartman, C. W., CARLSON, R. F. Water balance of a small lake in a permafrost region. Fairbanks, Alaska, University of Alaska. Institute of Water Resources, 1973. iv, 23 p. (Report No. IWR-42.) [By pumping water from the lake, it was possible to study the dynamics of the active layer surrounding the lake and to determine the amount of ground water recharge and interconnection with other lakes in area.]Google Scholar

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Howarth, P. J. Film and filter combinations for the study of the periglacial landscape of the high Arctic. (In White, D., ed. Resources satellites and remote airborne sensing for Canada. Proceedings of the first Canadian symposium on remote sensing, Ottawa, February 1972. Vol. 2. Ottawa, Dept. of Energy, Mines and Resources. Canada Centre for Remote Sensing, 1972, p. 379–86.) [Assesses results of vertical air photography using four film and filter combinations in Resolute Bay area, Cornwallis Island, N.W.T.]Google Scholar

Hunter, J. A. Seismic up.hole wavefront experiments in permafrost, Schefferville, Quebec. Project 730006. Canada. Geological Survey. Paper 74-1, Pt. B, 1974, p. 83–86. [Describes tests to determine seismic velocity section circumjacent to bore holes and relates velocities with existing geology and temperature information.]Google Scholar

Hunter, J. A. Seismic velocity measurements in permafrost, Fox Tunnel, Fairbanks, Alaska. Project 730006. Canada. Geological Survey. Paper 74-1, Pt. B, 1974, p. 89–90. [Trend towards higher seismic velocities with increasing ice content in silts was evident.]Google Scholar

Hunter, J. A. A shallow seismic experiment—Beaufort Sea, March 1974. Project 730006. Canada. Geological Survey. Paper 74-1, Pt. B, 1974, p. 87–88. [Attempt to detect sub-sea bottom permafrost in presence of thick ice cover (2 m).]Google Scholar

Hunter, J. A., Mereur., F. Computer model studies of seismic reflection coefficients for the base of the permafrost layer. Project 730006.Canada. Geological Survey. Paper 74-1, Pt. B, 1974, p. 95–96. [Study undertaken to determine relative effects of various physical parameters on reflection coefficients.]Google Scholar

Hunter, J. A. and others. Mapping the occurrence of sub-sea bottom permafrost in the Beaufort Sea by shallow refraction techniques. Project 730006, [by] Hunter., J. A,Good, R.L. and Hobson, G.D..Canada. Geological Survey, Paper 74-1, Pt. B, 1974, p. 91–94. [Permafrost detected below sea bottom in Mackenzie Delta– Beaufort Sea area, but detailed extent unknown.]Google Scholar

Johnston, G. H., Ladanyi, B. Field tests of deep power-installed screw anchors in permafrost. Canadian Geotechnical Journal, Vol. 11, No. 3, 1974, p. 348–58. [Evaluates creep behaviour and load capacity of anchors of various diameters embedded in frozen stratified silts and clays containing ice at 0.3° C.]Google Scholar

Kay, B. D. Specific heats of components of frozen soil. Research agreement 1135-D13-4-199/72. Canada. Geological Survey. Paper 74-1, Pt. B, 1974, p. 203. [Measured over temperature range −70° C to + 30° C.]Google Scholar

Kinosita[i.e. Kinosiuta],, S. Tōdo no ichijiku asshuku kriipu [Creep property of frozen soil]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 31, 1973, p. 261 –69. [Describes and discusses laboratory experiments. English summary, p. 269.] Google Scholar

Kinosita[i.e. Kinoshita],, S., SUZUKI, Y. Shiberia Vakūtsuku noeikyū tōdo chōsa [Researches on permafrost at Yakutsk, Siberia]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 31, 1973, p. 271–77. [Some observations made in August 1972 in north-eastern Siberia. English summary, p. 276–77.]Google Scholar

Mackay, J. R. Measurement of upward freezing above permafrost with a self-positioning thermistor probe. Project 680047. Canada. Geological Survey. Paper 74-1, Pt. B, 1974,p.250–51. [Satisfactory results obtained.]Google Scholar

Mackay, J. R. Reticulate ice veins in permafrost, northern Canada. Canadian Geotechnical Journal, Vol. 11, No. 2, 1974, p. 230–37. [Field observations suggest veins grew in vertical and horizontal shrinkage cracks in a semi-enclosed freezing system, rather than from the upward migration of water in an open system. Discusses this in relation to engineering problems.]Google Scholar

Mackay, J. R., Lavkulich, L. M. Ionic and oxygen isotopic fractionation in permafrost growth. Project 680047 Canada. Geological Survey. Paper 74-1, Pt. B, 1974, p. 255–56. [Shows that fractionation profiles may be helpful in interpreting history of permafrost sites.] Google Scholar

Mathieu, D., Petiot, R. Essai d’une typologie des dépōts périglaciaires de versants dans le Jura bisontin. Revue de Géomorphologie Dynamique, 22^e An., No. 4, 1973, p. 179–87. [Presents attempt to classify different types of periglacial slope deposits.]Google Scholar

Orama, R. Värmeisolering på finska vägar och flygfält. Frost i Jord, No. 6, 1972, p. 5–17. [Discusses principally use of polystyrenes for thermal insulation in roads and airfields in Finland. English summary, p. 16–17.]Google Scholar

Penner, E. Uplift forces on foundations in frost heaving soils. Canadian Geotechnical Journal, Vol. 11, No. 3, 1974, p. 323–38. [Unit adfreeze strengths and maximum uplift forces were highest for steel columns, followed by concrete and wood; the lowest values were for a block concrete wall. Unit adfreeze strengths were highest for small diameter columns, and lowest for large columns.]Google Scholar

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Sinha, A. Electromagnetic sounding in permafrost regions. Project 730004. Canada. Geological Survey. Paper 74-1, Pt. B, 1974, p. 109–10. [Theoretical study.]Google Scholar

Solbraa, K. Barkens bestandighet i veifundamenter. Laboratorieforsøk. Frost i Jord, No. 6, 1972, p. 25–31. [Presents results of experiments designed to show correlations between rate of bark decomposition and temperature, water content and concentration of gaseous O₂ and C0₂ in bark from various trees intended for use as frost protection layers in road construction.]Google Scholar

Svensson, H. Distribution and chronology of relict polygon patterns on the Laholm plain, the Swedish west coast. Geogrofiska Annaler, Vol. 55A, Nos. 3-4, 1973, p. 159–75. [Presents results of air photography studies.] Google Scholar

Svensson, H. Isfȧilt, “naledi”, i Cherskiybergen. Svensk Geografisk Arsbok, Arg. 49, 1973, p.225–27. [Observations of icings in Khrebet Cherskogo, Yakutskaya A.S.S.R., made during the second International Permafrost Conference in 1973.]Google Scholar

Tarnocai, C. The use of remote sensing techniques to study peatland and vegetation types, organic soils and permafrost in the boreal region of Manitoba. (In White, D., ed. Resources satellites and remote airborne sensing for Canada. Proceedings of the first Canc dian symposium on remote sensing, Ottatta, February 1972. Vol. 1. Ottawa, Dept. of Energy, Mines and Resources. Canada Centre for Remote Sensing, 1972, p. 287–92.) [Detectable differences were found in multispectral response patterns obtained from several kinds of photographs of various terrain types. Area of permafrost decreased at rate of 1% per year over 25-year period studies.]Google Scholar

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Whalley, W. B. Rock glaciers and their formation as part of a glacier debris-transport system. University of Reading. Dept. of Geography. Geographical Papers, No. 24, 1974, [i], 60 p. [Describes and discusses rock glaciers and suggests hypothesis of their formation and the mechanics of their flow.]Google Scholar

Yosida, Z. [i.e. Yoshida, J.] ’Tōjōryoku ni tsuite no rirontcki kōsatsu [A theoretical study on the heaving force of freezing soil]. Teion-kagaku: Low Temperature Science, Ser. A, [No.] 31, 1973, p. 231–44. [English summary, p. 242–44.]Google Scholar

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Bader, M. and others. The production of sub-micron ice fragments by water droplets freezing in free fall or on accretion upon an ice surface, by Bader, M.,Gloster, J.,Brownscombe, J.L.,Goldsmith, P. Quarterly Journal of the Royal Meteorological Society, Vol. 100, No. 425, 1974, p. 420–26. [Experiments show not enough particles are produced in free fall to explain nucleus concentration in some clouds, but number ejected during riming can help to explain this.]Google Scholar

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