The upper outcrops of the valley walls form spires and towers and hoodoo-like shapes. Talus looks like it will come sliding down at any moment, although no rock falls occurred the entire time we were in the cirque.
In order to make your way up the cirque valley, you either have to go off-trail and skirt the entire rock glacier (RG) on talus (not recommended or encouraged - or allowed? - by the Park Service), or you walk across several patches of firm to slightly slushy snow. Ski poles are something I would recommend. MOH and I had hiking poles, but we had taken the little ski-pole baskets off, and so our poles would sink into the snow. The poles would also get stuck occasionally in the rocks of the RG, and ski-pole-type baskets would have helped there, keeping the poles from going into gaps between the rocks.References:
Osborn, G., 1990. The Wheeler Peak cirque and glacier/rock glacier. Unpublished report prepared for the Great Basin Natural History Association. University of Calgary Dept. of Geology and Geophysics.
Osborn, G. and Bevis, K., 2001, Glaciation in the Great Basin of the Western United States: Quaternary Science Reviews 20, 1377-1410.
Osborn, G., 1990. The Wheeler Peak cirque and glacier/rock glacier. Unpublished report prepared for the Great Basin Natural History Association. University of Calgary Dept. of Geology and Geophysics.
Osborn, G. and Bevis, K., 2001, Glaciation in the Great Basin of the Western United States: Quaternary Science Reviews 20, 1377-1410.
3 comments:
Thanks so much for this travelogue!
rock glaciers are very cool but I notice that when climbing them they are much more massive then they look. Also, I've known of some very bad endings on scree - I suspect that's why you are told to avoid it.
Andrew, thanks for visiting, and I appreciate your kind comment.
Wayfarer, you seem quite familiar with rock glaciers, I know there are some way up north. I think they can especially seem quite massive when at over 10,000 feet!
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