It was one of many days in a mediocre winter. The base was lean, it had snowed a good 10 centimetres overnight with a lot of wind. Nobody wanted to go freeriding in the area, nor did they want to go on a longer tour. The situation report spoke of a combined drift and old snow problem, danger level Considerable. The old snow problem had been in the text section of the bulletin every day for weeks, a kind of background noise to the season. The fresh drift snow was much more present in our minds that day. We considered a variant with a short ascent from the lift to a longer descent over flat, comfortable alpine terrain.
The only critical point was a short, somewhat steeper slope area at the very beginning of the descent: bordered on the left by a few tufts of grass and stones peeking out, the top 15 meters perhaps 30-32° steep, then quickly becoming significantly flatter. We stood together at the top and discussed whether it would be better to go around the outside and cross to the next flat section with some pushing. On the other hand, it was really only the first few meters that were a little steeper. And going over the flat section with a bit of momentum would definitely be the more pleasant option. We agreed: at most, the first turn would take off the little bound drift snow on the surface, but even if it did - that shouldn't be a problem in this terrain.
One of my two touring colleagues set off on the descent while we watched him from the entrance. A few quick turns and he was down on the flat, the snow even looked pretty good. We watched as he crossed the flat section - whether it would work out without pushing? - and got ready to leave.
My colleague was just past the next crest, maybe 300m away, when a crack opened up at the top of the entry slope. The slope seemed to detach as a whole, initially without breaking into smaller slabs. A few seconds later, the slope next to ours also broke away, and a few more seconds later the one next to it. In the meantime, our colleague was standing much further down on another crest - long outside the danger zone. Our position at the start was not at risk either. The avalanche didn't travel far thanks to the flat terrain, but the avalanche edge was around 150m long. The trigger point was probably in the first flat section in one of the many places with little snow. The break continued flat up the slope until the terrain became steep enough for a descent.
The steeper slope at the beginning was borderline that day, according to Munter, but not completely beyond good and evil. And if we had bypassed the slope and crossed directly into the flat section - a "permitted", not even borderline, variant according to Munter? Of course, I'll never know, but I suspect we would have triggered the avalanche anyway.