Nature Notes From Crater Lake
Volume 1, No. 1, July 1928
Crater Lake
By Earl U. Homuth
In this, the first issue of the first volume of our "Nature Notes
from Crater Lake", it might be well to describe briefly that marvelous
feature which is known as Crater Lake, and to attempt, briefly, to
outline the theories as to its origin.
Crater Lake lies in the caldera of a once mighty mountain. The lake
is approximately six miles wide and slightly longer; is nearly 2000 feet
deep at the deepest sounding; is surrounded by cliffs varying from 500
to over 1800 feet in sheer height.
Many interesting features may be observed on the walls above the
lake; ancient valleys on a still more ancient mountain, filled with
lava, and then cut in cross-section to show in perfect clearness; broad
glacial valleys opening on the very brink of the caldera, indicating
again some points in the history of the original peak; cut edges of as
many as thirty successive lava flows and other points illustrating the
development of Mt. Mazama. Mazama is the name given to the mountain that
once stood here. Evidence that a peak did rise a full ten thousand feet
above the lake bottom, or a full seven thousand above the Rim, is
derived from four sources.
First, glacial evidence is clear, and the source of the glaciers have
been higher than the present rim, since there are no cirques, the cut
edges of moraines show at the rim, and the valleys are broad and
U-shaped at the very top.
Second, dikes stand out boldly on the inside of the walls, indicating
an angle toward an original peak. Fully ten of these can be counted.
Third, the slope of the flow of lava is downward, away from the rim
on every side, and the walls are largely the broken edges of these
flows, not coated over with other lava material.
Fourth, Wizard Island is a true crater rising to approximately eight
hundred feet above the water, or considering the depth of the lake, a
cone two thousand eight hundred feet from base to summit. Since the
action of a crater builds it up, and material was present to build up
this cone, then possibly a previous period of volcanic action could have
raised Mt. Mazama to a height where it could rival Mt. Shasta, Hood, and
others of our great volcanic peaks.
What became of Mt. Mazama will be discussed briefly in a future issue
of these notes.
