Snow cornice

A snow cornice forms by wind blowing snow over sharp terrain breaks (e.g. the crest of the mountain) where it attaches and builds out horizontally.

This build-up is most common on the steeper and leeward sides of mountains.

[2] When a cornice collapses, it breaks in from the cornice to the top of the peak; even being on the snow on top of rock exposes the alpinist to hazard in this situation.

The best practice in mountaineering is to stay far enough back from the edge so as not to be able to see the drop, as an approximate metric of exposure.

Cornices are particularly vulnerable to collapse during periods of high solar irradiance.