In reply to Rampikino:
Have not read the document as it doesn't open in my computer, but i thought about vertical Abalakovs before, and my conclusion was that in waterfall ice it'd be weaker, as ice tends to form in vertical columns that end up fusing together to give the impression of a continuous sheet of ice. By doing vertical abalakovs you'd be weakening said columns, and depend on the strength of the bonding between them.
No idea what the result would be on Alpine or Glacial ice. I'll keep trying to download the document to find out about the results.