The Geologic Story of Mount Rainier: A look at the geologic past of one of America's most scenic volcanoesCrandell, Dwight R. (Dwight Raymond)
Science
The Geologic Story of Mount Rainier: A look at the geologic past of one of America's most scenic volcanoes
Crandell, Dwight R. (Dwight Raymond)
Geology -- Washington (State) -- Rainier, Mount; Rainier, Mount (Wash.)
Some time during these eruptions, hot volcanic bombs and rock fragments
were thrown out of Mount Rainier’s crater and fell onto surrounding
areas of snow and ice. Wholesale melting resulted, and floods descended
the east flank of the volcano carrying millions of tons of ash, newly
erupted rock debris, and breadcrust bombs. Breadcrust bombs seem to be
solid rock, but if you would break one open, you would find that the
inside is hollow or is filled with a spongy mass of black glass. Their
outer surfaces are cracked like the crust of a loaf of hard-crusted
bread (fig. 9), so we call them breadcrust bombs. They originated as
blobs of soft, red-hot lava which were thrown out of the volcano’s
crater. As the masses arched through the air, they quickly chilled on
the outside, and a hardened skin formed around the still hot and plastic
core. As their outsides cooled, gas pressure in their hot interiors
caused the bombs to expand slightly and their solidified outer skin to
crack. When they struck the ground, many of the bombs became flattened
on one side, but they were still plastic and sticky enough to remain
whole.
Bombs can be found in two deposits that form the south bank of the White
River about half a mile downstream from the White River campground. The
deposits are mudflows caused by the mixing of hot rock debris with the
water from melted snow and ice. As the mudflows moved down the valley
floor they must have resembled flowing masses of wet concrete.
Mount Rainier erupted several times between about 2,500 and 2,000 years
ago. During one of the first eruptions, a mass of hot ash, rock
fragments, and breadcrust bombs avalanched down the side of the volcano
and buried the floor of the South Puyallup River valley. Although this
hot mass flowed like a wet mudflow, the temperature of the rock debris
was above 600°F. Thus, if any water had been present, it would have been
in the form of steam. You can see the resulting deposit in cuts along
the West Side Road on both sides of the bridge across the South Puyallup
River. Innumerable bombs have rolled from the cuts into the ditches
beside the road. A charcoal log found in the deposit had a radiocarbon
age of about 2,500 years.
[Illustration: A large breadcrust bomb enclosed in a mudflow deposit
that consists of a mixture of volcanic ash and rock fragments. The
outcrop is on the south bank of the White River about half a mile
downstream from the White River campground. (Fig. 9)]
Public-domain text, read in full here on John Shaqi.
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