V. Geological and
Biological Information on Crater Lake Area
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F. Other Natural Resources
1. Forests
and Plant Life
It should not be presumed from the
foregoing discussion that Crater Lake is a sterile expanse, encompassing only
barren desert terrain, remnants of rugged volcanic cones, and high, impenetrable
lava cliffs and precipices. Actually, a soil of great fertility has been created
from the volcanic lava of the Cascades through the processes of time and
weathering, permitting a profusion of forests and wildflowers. One approaches
Crater Lake National Park through the lowlands outside the boundary where
forests of ponderosa and lodgepole pine alternate with junipers, sagebrush, and
antelope bitterbrush--an environment characteristic of the Great Basin desert
which it adjoins on the east. Passing through this more arid zone onto the lower
elevations of Mazama, one finds several varieties of pine (ponderosa, sugar) and
fir (white, Douglas), as well as western hemlock, western yew, dogwood, and
assorted bushes. The park's forests are unusual because of the heavy growth of
fine virgin trees that have been undisturbed by man except for the removal of
diseased members. On the higher slopes of Mount Mazama western white pine and
lodgepole are slowly establishing themselves in thick growths. Still higher
points introduce mountain hemlocks, red fir, and subalpine fir, but only
whitebark pines grow on the high, windblown rim. Over the edge, sparse strips of
vegetation descend to the lake in the lee of protecting rock ledges.
At least 570 species of flowering plants and ferns also thrive in the park,
ranging from lichen at Palisade Point to the wildflowers of Castle Crest and
Munson Meadows to the stunted vegetation of the Pumice Desert and Wizard Island.
Water is supplied by springs outside the caldera on the west and southwest
slopes, enabling dripping mossy cliffs, bogs, and lush meadows to proliferate.
The blooming season here is short, however, from July 1 to mid-September at the
latest.
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