This
image, from the Beartooth Plateau of southcentral Montana, shows a granitic
boulder detached, but not removed, from its bed. Strongly developed
joint sets trending approximately vertically and horizontally are obvious
in the image. A less well developed set of joints trending diagonally
across the photo has loosened the clast, so only gravity holds it in place.
Ice moving towards the camera may have allowed meltwater to freeze to both
the clast and the glacier bed on the down-ice (low-pressure) side of the
obstruction. Continued flow had apparently begun to pull the rock
free, but stopped short of complete removal. This process provides
clasts to the glacier bed to accomplish abrasion.
Thumbnail, photo, and annotated photo copyright W.
W. Locke, 1998; all rights reserved.