Dear Carissa,
Eruptions began at Mount Saint Helens about 40,000 years ago. The deposits are air-fall tephra and pyroclastic flows, the type of material produced by explosive eruptions. One pumiceous tephra deposit produced during this episode had a volume as great as any subsequent tephra eruption at Mount Saint Helens. I think it would qualify as a big eruption.
A recent paper suggests that eruptions at Mount Saint Helens began as long ago as 80,000 years. Berger and Busacca (1995) dated a loess (wind-blown slit-sized material) deposit just below a tephra layer in eastern Washington that is known to be from Mount Saint Helens. The loess is about 80,000 years old. The tephra is thought to be slightly younger.
For more details about the eruptive history of Mount Saint Helens visit the Mount Saint Helens page in VolcanoWorld.
Steve Mattox, University of North Dakota
Sources of Information:
Berger, G., and Busacca, AJ., 1995, Thermoluminescence dating of late
Pleistocene loess and tephra from eastern Washington and southern Oregon
and implications for the eruptive history of Mount St. Helens: Journal of
Geophysical Research, v. 100, p. 22,361-22,374.
Mullineaux, D.R., and Crandell, D.R., 1981, The eruptive history of Mount St. Helens, in Lipman, P.W., and Mullineaux, D.R., (eds.), The 1980 eruptions of Mount St. Helens, Washington, U.S. Geological Survey Professional Paper 1250, p. 3-15.
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