EARTH SURFACE PROCESSES AND LANDFORMS, VOL 22, 703 (1997)

1997 by John Wiley & Sons, Ltd.

ERRATUM

SUBGLACIAL PRESERVATION OF VALLEY MORPHOLOGY AT AMUNDSENISEN, WESTERN DRONNING

MAUD LAND, ANTARCTICA

J. O. NÄSLUND

Department of Physical Geography, Stockholm University, S-106 91, Stockholm, Sweden

Figure 4 did not reproduce well in the final printing, for which the publishers apologise.

Figure 4. The subglacial valley system at Amundsenisen which was mapped in more detail, shown with a 2× vertical exaggeration andcontour interval of 25m. The bed surface has been corrected for the ice surface topography. Data on bed and ice sheet topography werecollected with a spacing of 500m or less along the profiles, shown by the dotted lines on the upper ice surface. The general valleymorphology indicates that the valley was formed by erosion by a wet-based local mountain glacier. This site is used for a comparative

calculation of basal temperature for discussing where, on a local scale, preservation of landforms may occur