IIR, the Mt. St. Helens 1980 eruption mechanism was the slow build-up of a steep slope of very weak rock, while various earthquakes (associated with deep magma movements) jiggled the whole mountain. The little glaciers on top were, at best, along for the ride when the "final" 'quake turned the unstable slope into a big landslide. Which landslide also "uncorked the champagne bottle" for the main eruption.