A continuation of the volcanics of the early Cascade Range in Washington, accretionary lapilli, like volcanic “hail stones” made of concentric rings of ash around an ash core, are common clasts in the Ohanapecosh Formation.
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A continuation of the volcanics of the early Cascade Range in Washington, accretionary lapilli, like volcanic “hail stones” made of concentric rings of ash around an ash core, are common clasts in the Ohanapecosh Formation.