Nature Notes From Crater Lake
Volume 3, No. 3, September 1930
The Devil's Backbone
By Robert L. Myers
On the western slope of Mount Mazama is
a jagged ridge of rock, the mute product of the original Mount Mazama,
and the object of a fascinating story.
Mount Mazama has been gradually built
up by the outpouring of lava from the crater, and its slops. Beneath it
once lay a heated body of rock, ever waiting for the chance to come to
the surface. Occasionally this mass became unusually restive, and once
the mountain could no longer withstand its attacks. Long cracks formed
down the slopes of the old volcano. The eager lava quickly filled them,
- the first stage in the formation of the Devil's Backbone was over.
The lava cooled, ages passed, and the
mountain lay dormant. No longer did lava flow down its summit. Instead,
glaciers carved its slopes, and gradually wore them down. The wind, the
ice, and the rain have all attacked the lava which filled the crack; but
more resistant, the newer lava has steadily resisted, and today stands
out from the Rim, clearly perceptible from the Lodge.