Nature Notes From Crater Lake
Volume 29, 1998
A Natural History of My
Refugium: Seven Summers in Crater Lake National Park (1)
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. |
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.
|
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.
|
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.