Nature Notes From Crater Lake
Vol. 14, No. 1, September, 1948
The Retreat of Mount Mazama Glaciers
By William Kinsley

Glaciers once covered most of Mount
Mazama and the country around its base. Howel Williams points out that
during the stage of maximum glaciation, ice covered all but the highest
pinnacles of the cascade divide.
The tremendous glaciers on the slopes
of Mount Mazama have left scars in the form of U-shaped valleys. On the
southern side of Crater Lake one can see Kerr, Sun, and Munson Valleys;
all have the characteristic U-shape caused by moving rivers of ice. Here
is mute testimony that large glaciers moved down the slopes of Mount
Mazama, carving and gouging material from the sides of the valley. That
material was ground into rounded boulders and fine sand; when the
glaciers melted, the ground-up material was dropped in place forming
glacial till.
Today the climate has changed to a
point where only in the higher altitudes do the mountain peaks produce
their rivers of moving ice. The geographers tell us that the average
temperature of the world has been increasing is not known. Exactly what
brings about this increase is not known. A decrease in temperature did
occur over one million years ago that gave much of the land surface of
our earth a coating of ice in the form of glaciers. This is called the
Pleistocene Epoch or "Ice Age". In many recently glaciated areas of the
world geologists have found evidence that there were four periods during
the Ice Age when the glaciers dominated these areas, and three periods
between when the glaciers were all but extinct. The cause of these
cycles of fluctuation must have been caused by widespread temperature
variations on the earth. They may have been due to a variation in the
heat intensity from the sun, or perhaps a change of the axis inclination
of our earth. Either of these changes could have been enough to produce
far reaching temperature effects on the surface of the earth.
Wallace Atwood Jr. studied the layers
of glacial till that are interbedded with Mount Mazama lavas. He found
many more deposits of glacial till than could be accounted for by these
climatic cycles. Some other major cause must be sought for the retreats
which dropped these additional layers.
Throughout much of the Ice Age, Mount
Mazama was building itself. Tremendous eruptions of molten material were
ejected from the top or sides of Mount Mazama and flowed down the
slopes, cooling in the sharp, cool air. Other times great cinder showers
with pumice or volcanic ash fell back on the slopes, adding their
material in the building process. There must have been times when great
ice flows rested on the slopes when these molten lavas or cinder showers
came forth, and the picture of explosive steam clouds and rushing waters
issuing from the glaciers is one of appalling clearness. The melted
waters rushed down the canyons below the glaciers, carrying with them
large trees and boulders, dropping their load only when the momentum of
the flood died away. Quite often the glaciers were completely melted
away when volcanic activity persisted long enough. Surely then, there
were times when the glaciers disappeared due to volcanic activity of
Mount Mazama and not due to any climatic change in the region.
Thus the retreat of Mount Mazama
glaciers was governed by both climatic and volcanic conditions. Material
dropped from retreating glaciers gives, as yet, no hint as to which
influence caused the retreat. If the geologist can ascertain the rate at
which these glaciers melted, he may have the fundamental answer to this
problem. Volcanic action upon the glaciers will produce fast retreats,
while climatic temperature increase will give rise to slow retreats.
Somewhere the answers lie in the rocks around Crater Lake.