Volume XXIX - 1998
A Natural History of My Refugium: Seven Summers in Crater Lake National Park1
By John K. Simmons
It was 6 a.m. and cloudy on the gray spring morning when we flew
from Ashland's airport in a small four-passenger plane. We rose above
the clouds at 5,000 feet and in short order headed east into the
breaking dawn. The sky grew lighter and ever so colorful as the sun
began to rise. Within a half hour I could see the gray stillness of
Crater Lake as the dawn's light bounced down the caldera walls. I always
knew Wizard Island was supposed to be a nearly perfect cinder cone, but
as we circled high above the lake, we were able to see just how
perfectly it was shaped because the snow traces radiated down
along its slopes, just like the spokes of a wheel. By 7:00 we landed
back in Ashland, where the town was just awakening to another gray,
dreary morning. But we were not drowsy and feeling under a burden of
dark clouds, having just experienced a sunrise flight over Crater
Lake!
Golden mantled ground squirrel. Drawing by Mike
Cook, 1992.
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I enjoyed many days hiking and camping during my employment at the
park. We discovered many differing habitats, and even climbed Mount
Thielson, the peak that towers over Diamond Lake. Though we came to
expect golden mantled ground squirrels (Citellus lateralis) along
the rim of Crater Lake,2 we were surprised to see one at the
very top of Thielson, begging for a handout!
Anywhere I went within the park, I would be greeted by some form of
wildlife. Once, while walking along the base of a talus slope near Park
Headquarters, I came across a doe and her fawn. In their attempt to
avoid me, they could not run away because of the big, blocky boulders
they had to cross. So they just walked away. One animal often heard, but
rarely seen, is the pika (Ochotona princeps). I often heard them
along the caldera walls as I hiked down the Cleetwood trail to the
lake's edge. The first one I ever saw was also the only one that I was
able to photograph! It is these little lagamorphs that I miss on my
treks in Olympic National Park since they never populated the isolated
Olympic Peninsula.
I have had the unique opportunity to "talk" with some of the spotted
owls (Strix occidentalis caurina) living within the boundaries of
Crater Lake National Park. During my first year as a ranger, I read
through the preliminary reports of spotted owl surveys conducted in the
park in 1976. Since I had been involved with a spotted owl survey for
the Forest Service prior to working at Crater Lake, I was eager to help
with work in the park. Even though it was late in the summer of 1977, we
were able to locate the owls seen the year before and find a couple of
new locations. More surveys followed the next year, along with some
predictions for where these birds might be found in the future. Not
until 1992 were more in depth surveys conducted, but they found owls in
the predicted locations!3
One of my favorite places to visit is Anderson Falls. Not many
visitors know about it, or how to get there, because there are no formal
trails leading to this spectacular feature.4 One can almost
melt into the scenery there, where wildflowers wave at your knees. Upon
the cliff above these falls are onions (Allium validum) that grow
nearly up to your waist! And are they ever tasty...and strong! I admit
that I ate a couple, and then progressed to taste those powerful bulbs
the rest of that day and even through breakfast the next day!
Wild onion.
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A fellow employee and I once got trapped in a hail storm near
Anderson Falls. We found refuge in a small cave along the cliff, but
knew that we had to get back to Rim Village. After running back to Rim
Drive, a visitor picked us up and took us to the lodge. There were quite
a line of cars headed down the mountain, since those visitors did not
want to stay around to weather the storm. Very shortly after we reached
the lodge, however, the rain stopped. We were the only ones left on the
rim, it seemed, and then the clouds began to lift. As if we were the
only ones who were meant to see, a rainbow formed and arched low over
the lake. It moved across the water to the other side as the storm
clouds headed eastward, and washed the rim wall with its colors.
Crater Lake itself seems to have many colors, textures, and moods
that change frequently. Though the lake seems to be ever constant,
staying the same year after year, one has only to spend a day along its
edge to know differently. Some visitors stay for only an hour or two,
and of course fail to appreciate the subtle and dramatic changes that
take place.
The water is not blue, nor gray, but is crystal clear. Sunlight
penetrates the water, some of which is reflected, but most is refracted
or bent by the water molecules in the lake. White light from the sun is
a blend of all visible wavelengths and penetrates Crater Lake's surface.
Most of the reds and yellows are absorbed in the first few feet of
water. The greens that are often seen along the lake's edge and around
Wizard Island reach down further, but become absorbed at relatively
shallow depth. Blues reach the deepest, with these wavelengths being
scattered and bent. Much of that blue light is reflected toward us. This
provides that deep blue as we gaze at the lake. The color of Crater Lake
at any one time is influenced by the intensity of sunlight, cloud cover,
and suspended particles in the water.
Clark's nutcracker. Drawing by L. Howard Crawford,
1936.
Sometimes the clouds pour into the caldera, much like water from the
spout of a pitcher, reminding one of the witches cauldron in
Shakespeare's Macbeth. The differences in air pressure and
temperatures between the caldera and surrounding mountain slopes, often
cause clouds to rise or descend. On one occasion, when the clouds poured
into the caldera, they descended along the lake surface but left the rim
walls and Wizard Island's conical peak poking out of the blanket.
Although park employees knew this was a rare event, some visitors were
puzzled and subsequently complained because they came to see the
lake, not a bunch of clouds! If only they could understand how
special this event was, they might have joined in the excitement.
Along much of the rim you can observe the survival struggle of
whitebark pine (Pinus albicaulis). Their growth is limited by the
slope, aspect, direction and strength of winds or storms, availability
of water, and the Clark's nutcracker (Nucifraga columbiana). The
resinous cones are sealed to protect the seeds from most predators, but
the Clark's nutcracker (as its name implies) can break open these cones.
It is as though this bird has just the right tool to pick the lock on
this safe of seeds. They cache the seeds for their winter food supply,
which is usually located along a ridge top where winter winds scour the
snow. The bird does not always find its caches, so this eventually
results in another crop of whitebark pines! Ornithologists believe that
the tree and bird co-evolved, for the tree depends upon the bird to
plant its seeds.
Ernest G. Moll, in his collection of poems about Crater Lake, wrote
of the whitebark pine:
On this torn ridge he rooted, proud and free,
Battling the wild earth-forces for control;
Life granted not his dream of beauty, so he,
Majestically dying, reached his goal.
Sundew. Drawing by Walter Rivers, 1948.
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Crater Lake is also where I began to learn many of my wildflowers.
The glacier lilies (Erythronium grandiflorum) that sprout along
the Rim Drive are one of the first flowers to come up through the snow
in early summer. Adorning the south facing and drier talus rock slopes
are the pasque flowers (Anemone occidentalis). As the flowers
fade, the stems grow high above the rocks, pushing the pom pom-like
seedheads into the wind. This allows seeds to be dispersed more
easily.
Sphagnum Bog, a marshy area along the western boundary of the park,
hosts several insectivorous plants such as two species of sundew
(Drosera anglica and D. rotundifolia) and the butterwort
(Pinguicula vulgaris).5 Tiny insects get stuck on the
Sundew surface of their leaves or showy parts and are "digested"
right there. This gives the plants a source of nitrogen, a substance not
found in high supply around boggy areas. I hiked out there to find the
sundews and photograph them, but not until later did I realize I had
butterworts among the sundews in my pictures! A somewhat similar area is
Thousand Springs, an area south of Sphagnum Bog, where I found the aster
fleabane (Erigeron peregrinus var. callianthemus), arrowleaf
groundsel (Senecio triangularis), and two species of bog orchids
(Habenaria dilatata and H. stricta).
Beargrass (Xerophyllum tenax) was not to be found in Crater
Lake National Park, or so I had read in a wildflower book.6
Being rather curious about this plant, I asked Ron Mastrogiuseppe. He
answered that it had recently been located, but would not say where.
Over the course of that summer, though, Ron gave me two hints about its
location. One was "pre- Mazama landscape" and the other was "refugium."
I had heard of a refuge, but not refugium. The latter word appeared in a
geologist's dictionary, with the definition being "a place that had been
protected in some way from a climactic event."
After some study, I approached Ron with some possibilities for where
beargrass might be found. He smiled and sent me out to locate the plants
in early September. In an area only 40 feet or so square, along a small
rocky ridge, I found some withered stalks!7 Charlie Bacon,
whose work has substantially changed our understanding of the park's
geological story, told me later that there were no refugia -- that is to
say, protected areas within what is now the park when Mazama's climactic
eruption took place 7,700 years ago.8 He figured that birds
had deposited the seeds. Even so, it is fascinating to consider the
possibility of such a refugium.
Although the park may not have been a refuge for life at the time of
the big eruption, it certainly is now. When things become too hectic, I
return for a visit to Crater Lake and it rejuvenates me. Crater Lake
seems like home after spending seven summers of my life there, a place
where one can relax and feel like they belong. That feeling has
persisted for two decades in Crater Lake National Park, my refugium.
Notes
1 Edited from an interpretive slide program presented at
a symposium entitled Crater Lake National Park: Still Beautiful at
90, on May 16, 1992.
2 See Roger Brandt's article on this topic in the 1993
volume of Nature Notes from Crater Lake.
3 See Lori Stonum's article on spotted owl survey in the
1993 issue of Nature Notes.
4 It is, however, less than a half mile from the East
Rim Drive.
5 More detail about Sphagnum Bog can be found in the
article by Jean Danielson and Steve Mark which appeared in the 1994
volume of Nature Notes.
6 See Elizabeth L. Horn, Wildflowers 1: The
Cascades. Beaverton: The Touchstone Press, 1972 (p. 58).
7 This occurred in 1978. See Mastrogiuseppe's article on
pp. 12-14 in the 1994 issue of Nature Notes.
8 New evidence refutes Bacon's position, but more study
of Sphagnum Bog is needed.
John Simmons began his career as a park naturalist at Crater
Lake and is presently stationed at Canyonlands National Park.
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