Nature Notes From Crater Lake
Volume 12, October 1946
Editorial: An Appraisement
By Dr. C. G. Ruhle, Editor
Undoubtedly most people are initially
attracted to Crater Lake National Park by the extraordinary beauty of
the lake. This is expressed particularly in its Parriah blue color,
which is not exceeded in brilliance, depth, and intensity by other
bodies of water and which contrasts with a landscape especially suitable
for its delineation and emphasis. From favorable sites on its singular
setting on the truncated summit of a volcano, is presented an expansive
outlook of dense forests, pumice waste lands, dark ranges, and high,
solitary peaks.
The lake and its immediate surroundings
form an infinite combination of pleasurable sense impressions arising
from the symmetry and harmony of color, form, pattern, and sound, each
acquiring significance by the intimacy of association together. The
steep, variegated crater walls center attention on the lake and furnish
a frame to delimit the picture and enhance its charms. The graceful
green clusters of mountain hemlocks, themselves of exceptional charm,
accent sharply the ultramarine color, and while acquiring emphasis by
projection against it, act as effective borders for vistas of the lake.
Cloud patterns cast moving shadows on the lake, and the varying light
affects changes in the reflections of the enclosing cliffs. Countless
wind flurries sweep across the basin and stir ripples of wavelets in
sharply defined paths, as if created by jets of air.
To complete the picture, put in this
framework a magnificent abandon of colorful wildflowers, open, park-like
stands of Hudsonian forests, gnarled and wind-tortured veteran trees,
desperately clinging to existence or succumbent to the vicissitudes of
their home, tortuous rocks fashioned in the furnace of a volcano, and a
benign salubrity of climate resulting from a combination of the
crispness of the mountains and a suavity of the nearby Pacific shores.
In winter all these are wrapped with or
completely buried under a score or more feet of snow, that softens the
forms and imparts an enchanting aspect to the landscape. This is the
paradise for the skier, but just as many come to see what great change
winter has wrought, in the beauty of the lake and its surroundings.
Sublimity, power, and orderly operation
are expressed in this creation. As practically all who come are
impressed by its beauty, so few are uninfluenced by the significance of
its story of origin as acquaintance grows. In this instance, one deals
with the evolution of a landscape by age-long operation of forces
generated from the power and energy of the inner earth. Although the
visual beauty is enough in itself, it gather significance and emphasis
only as the story of its genesis and structure are apparent. Crater Lake
focuses attention on the realities of a landscape.
Not only Mount Mazama, the decapitated
volcano now marked by Crater Lake, but also a vast area of some 200,000
square miles around it was built up by repeated flows of lava. The walls
of the lake reveal how the mountain was built up layer on layer of
volcanic ash, lava, or wash of streams and glaciers. Sometimes the
mountain was quiet; forests and flowery meadows covered its mass, while
tumultuous streams slowly were washing away its bulk. At times it was
the mother of snowfields and glaciers, at times it glowed with Vulcan's
fire. Later, through collapse or explosion, the top gave way to form the
tremendous caldera whose layers have edges that give evidence of recent
breaking increasingly to widen the opening.
Of chief scientific interest is an
accounting for the presence of this lake of overwhelming depth and
beauty on the very summit of an unusual mountain. What are the
interesting geological and dynamics of the volcano? What connects the
beauty of the scenic features and the story of their origin? Why is the
water so blue and so pure? How does one account for the presence of
freshness of this lake at all, since it has no inlet and no known
outlet? What is the origin, nature, and distribution of the flora and
fauna of the region and how have they been influenced by the signal
environment in which they are found?
The amounts of rain and snow that are
added year by year are adequate to account for the filing of the caldera
to its present height with water. Seepage, lack of suspended material
washed in by rain, and the nature of the basin are such that the lake
possesses marvelous clarity and beauty. Only in a region in which all of
these local peculiar qualities are concatenate could a Crater Lake be
possible.