Nature Notes From Crater Lake
Volume 5, No. 2, August 1932
Columnar Structure in Our Lavas
By E. L. Clark, Ranger Naturalist
Many of our visitors have wondered if
the elongated columns of rock that are observed in various parts of our
Park are petrified logs, i.e. logs that were neatly arranged in piles
and bundles, then turned to rock by some unknown and uncanny process. It
is found in our lava flows and dikes, and is due to the regular
development of prismatic joints that break up the rock mass into
parallel columns, the sides of which are characteristically five or six
in number. This rock phenomenon is known as columnar structure. While
most of the columns will portray a rough and irregular hexagonal
outline, many of them will have the sixth side so depressed and small
that it is entirely eliminated.
This structure is variously portrayed
in our Park. It may be observed at the following localities within the
Rim Area: (1) the upper exposed portions of the andesite dike about two
hundred yards west of the foot of the Lake Trail; (2) in a small area
some forty feet above the Lake and fifty yards west of the dike just
mentioned; (3) the Devil's Woodpile some seven hundred yards west of the
foot of the Lake Trail (this feature is observed on the lake excursions
under the guidance of some member of our Naturalist Staff); (4) parts of
the dike known as the Devils' Backbone; (5) near the base of the great
dacite flow that forms Llao Rock; (6) the constriction at the base of
the bowl portion of the Wineglass; and (7) in the lava flow on the
inside of the Rim below Kerr Notch. Near the crest of the steep portion
of the grade over Vidae Ridge, and facing Sun Creek Valley some
six-tenths of a mile southwest of the Sun Creek crossing another
exposure of columnar lava may be observed. Here the lava has been poured
onto a trifaceous agglomerate (a chaotic assemblage of coarse volcanic
ashes and cinders). The attitude of the lava readily suggests its direct
relations to the former mountain.