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Volume 1 - Issue 10 - 1951

Contents

Page 1 of 2

Reviews

Research Article

  • Instruments and Methods: Englacial Investigations Related to Core Drilling on the Upper Taku Glacier, Alaska

  • Maynard M. Miller
  • Published online by Cambridge University Press:
    30 January 2017, pp. 579-580
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Other

  • Conclusion of Volume 1, Journal of Glaciology

  • Published online by Cambridge University Press:
    30 January 2017, p. 594
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Correspondence

  • The Formation of Forbes’s Bands

  • Joel E. Fisher
  • Published online by Cambridge University Press:
    30 January 2017, pp. 580-581
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Research Article

  • The Glaciers of Jostedalsbreen

  • R. Finsterwalder
  • Published online by Cambridge University Press:
    30 January 2017, pp. 557-558
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Other

  • Glaciological Literature

  • Published online by Cambridge University Press:
    30 January 2017, pp. 590-594
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  • Glacier Fluctuation in the Swiss Alps, 1950*

  • Published online by Cambridge University Press:
    30 January 2017, p. 558
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Letter

  • Melting versus Evaporation in the Sierra Nevada, California

  • Robert P. Sharp
  • Published online by Cambridge University Press:
    30 January 2017, p. 583
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Correction

  • Erratum

  • Published online by Cambridge University Press:
    30 January 2017, p. 594
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Research Article

  • Glacier Movement in North-East Greenland, 1949: With a Note on Some Subglacial Observations

  • W. R. B. Battle
  • Published online by Cambridge University Press:
    30 January 2017, pp. 559-563
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  • Work on the Fröya Gletscher, N.E. Greenland, appears to substantiate the evidence already brought forward for the irregular flow of glaciers over short periods. It appears possible to correlate the daily temperature regime with the flow of some “polar glaciers.” The distribution of thrust planes seems to have no noticeable effect on the flow. It is suggested that Block-Schollen movement may underlie the jerky motion of some of even the slower moving glaciers. A subglacial stream bed on the Skille Gletscher was explored from the snout for a distance of 500 m. It is estimated that at the farthest point the ice was 76 m. thick. There appears to be good observational evidence for de Martonne’s theory of medial moraines extending to the bed of the glacier.

Other

  • Fluctuations of the Italian Glaciers, 1950

  • Manfredo Vanni
  • Published online by Cambridge University Press:
    30 January 2017, p. 563
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Research Article

  • Early Discoverers: VI

  • Robert Hooke
  • Published online by Cambridge University Press:
    30 January 2017, pp. 576-577
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  • The Effect of the Altitude of the firn area on a Glacier’s Response to Temperature Variations

  • G. S. Callendar
  • Published online by Cambridge University Press:
    30 January 2017, pp. 573-576
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Reviews

Correspondence

  • [No Title]

  • R. Haefeli
  • Published online by Cambridge University Press:
    30 January 2017, pp. 581-582
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  • The Cameron Glacier, New Zealand

  • Maxwell Gage
  • Published online by Cambridge University Press:
    30 January 2017, p. 583
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Research Article

  • The Crystallization of Ice

  • P. G. Owston
  • Published online by Cambridge University Press:
    30 January 2017, pp. 571-573
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Reviews

Page 1 of 2