Canada Glacier where it meets Lake Fryxell. This is a cold base glacier with its base frozen onto the underlying rock. Cold base glaciers flow much more plastically and with less erosion than wet base glaciers found in temperate climates.
- Filename
- STNMTZ_20051122_RAW14755.tif
- Copyright
- ©2006 George Steinmetz
- Image Size
- 6144x4089 / 71.9MB
- www.georgesteinmetz.com
- Contained in galleries
- Antarctica
