About 2,000 years ago lava poured down the southern flank of Mount St. Helens in streams. As the lava flowed the outer edges of the lava stream cooled forming a hardened crust which insulated the molten lava beneath. This allowed the lava to remain hot and fluid encased in this “lava tube” and continued flowing months during the eruption. The end result was the creation of this spectacular 13,042 foot long lava tube. This formation is especially unusual at Mount St. Helens as this type of volcano usually erupts lava of a much thicker consistency which tends to block flow and build up pressure resulting in explosive eruptions like the blast of 1980. |
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