How can crevasses be detected in alpine solo tours?

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Discussion Overview

The discussion revolves around the detection of crevasses during alpine solo tours, particularly focusing on methods to differentiate between solid ice and crevasses that are covered by snow. Participants explore various detection technologies and the challenges associated with them, as well as the importance of understanding snow formation and crevasse patterns.

Discussion Character

  • Exploratory
  • Technical explanation
  • Debate/contested

Main Points Raised

  • One participant suggests using a detector that can differentiate between solid subsoil and crevasses, potentially utilizing radar signals similar to those used by satellites.
  • Another participant mentions that crevasses can be identified with experience and knowledge of snow formation, implying that detection devices may not be necessary.
  • Concerns are raised about the practicality of carrying heavy radio and radar detection devices during tours.
  • A participant shares insights from a conversation with a researcher, indicating that current detection methods are unreliable due to signal attenuation and interference, with some success in identifying crevasses post-passage through image processing of radiograms.
  • There is a discussion about the predictability of crevasses based on topological features, suggesting that experienced individuals may be able to navigate safely without advanced technology.
  • Another participant emphasizes the importance of supervised instruction and exposure to learn how to identify crevasses effectively.

Areas of Agreement / Disagreement

Participants express differing views on the necessity and effectiveness of detection devices versus experiential knowledge in identifying crevasses. There is no consensus on the best approach to safely navigate areas with potential crevasses.

Contextual Notes

Limitations include the unreliability of current detection methods, the need for further research into effective technologies, and the challenges of understanding snow's structural characteristics.

Anton Alice
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Hello there,

I want to do a alpine solo tour at the beginning of april.
Crevasses, which are covert by snow are very insidious. This is why solo tours are more of a gambling game.
The basic idea is: Using a detector which can make a differentiation between a solid subsoil of ice, and a crevasse.

For example Satellites use radar signals, to measure the thickness of ice plateaus by use of reflection at material boundaries. In my case, I only want a binary information: Can I take a step or not?

Do you have an idea how that differentiation can be accomplished?
I mean there should always be some difference between the scan of a solid subsoil and of a hollow underground. The question is, how to make that difference maximally distinctive.Which kind of signal is most appropriate for that? Also radars?
 
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You are exactly right that crevasses can be rather insidious. They are not really that difficult to identify or predict. Being well acquainted with snow and the formation of crevasses is also very helpful. If you have access to a typicall mountaineering group such as the Mountaineers or Mazamas they they would be more than to lead some trips for education. Alternatively one could study a book like "Freedom of the Hills."

What sort of trip are you planning? Radio and Radar type detection devices are much heavier than I would want to carry very far in the snow.
 
Ketch22 said:
Radio and Radar type detection devices are much heavier than I would want to carry very far in the snow.
Yes, that imagination was rather utopic. I planned a trip to Switzerland, Berner Oberland (the Eiger is also in that region).
For me as a student such a guided tour is not affordable. But I found another mountain (in that same region) which has a smaller (due to global warming), bypassable glacier. Still dangerous...
Nevertheless, its an interesting topic, and I will come back to that after the exams.
Ketch22 said:
They are not really that difficult to identify or predict.
With Portable masers (lasers at 500MHz) that would be a cakewalk, if they existed.
But I spoke to one of the persons, who wrote the paper, that @Nidum has posted, and he told me, that actually the detection is very unreliable, because the signal energy is so badly attenuated, and there are a lot of disturbing factors. What this research group has achieved, is to detect some crevasses, after passing them completely with the antennas. They show up in the radiogram as hyperbolas. Then this hyperbola has to be identified via image processing.

Predicting them by eye is sometimes impossible:



But if someone has a feeling for it, one certainly can predict the route of it with regard to the topology. For example, it is better to rest in a trough, than at a zenith, like the guy in the video did.
 
Anton, it is great to hear that a considered mind is prevailing. There is a possibly a few misunderstanding from my short post. The groups that I referred to are very low cost clubs. Also many schools have outdoor activity clubs that are part of the student union. It should not be very hard to locate one of these. The trips are ususally very economical and provide a good base exposure.
The Book is a very extent training book and is readily available online. Just search "Mountaineering, Freedom of the Hills"
With some study and a bit of exposure it is not too hard to start identifying crevasses. They are almost always in a pattern on the hills and are somewhat predictable. The challenging part is in understanding the structural characteristics of snow. Many ( if not most) of them are just walked over via the snow that is bridging the gap. Being able to identify a viable bridge made of snow is somewhat tricky. Again it is a much better place for supervised instruction.

Hope your trip comes together well. Anytime spent out on a tour like that is well worth it
 

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