Nature Notes From Crater Lake
Volume 6, No. 2, July 1933
How Fast is the Rim
Retreating?
By Earl W. Count
Immediately behind the group in the
photograph stand three trees close together. But today they are gone.
The stump of one now projects over the rim of the funnel-like
amphitheater immediately east of the Information Bureau. According to
Judge Steel, the present U. S. Commissioner and affectionately called
"The Father of Crater Lake", who gave the party on that day in 1907,
there was at that time ten feet more of rim, as well as the now vanished
three trees.
At the head of this amphitheater the
rim area itself is depressed, so that melting snow from the rim drains
off over the amphitheater-shaped rim slope. The concentration of this
water into several streamlets affords those frequent landslides at this
time which attract the attention of visitors and cause them to lean out
over the parapet at the Sinnott Memorial. So works the relentless
erosive forces of Nature gradually accomplishing the recession of the
rim of Crater Lake. Undoubtedly it is this unevenness in the
distribution of morainal material over the rim area that accounts for
the formation of the amphitheater in the first place. In the course of
the ages to come, probably such amphitheaters as this will father the
development of steep, V-shaped valleys converging upon a shallower
"Crater Lake"; and that lake of the future will occupy but the center of
a much broader, shallower basin-valley than the rugged precipices of
Crater Lake now enclose.