Nature Notes From Crater Lake
Volume 18, 1952
The Use of the Wheeler Creek
Pinnacles by Nesting Birds
By Donald S. Farner, Assistant Park Naturalist

The Pinnacles of Sand Creek and Wheeler
Creek have long been of interest to geologists because of their
contribution to our knowledge of the pumice-scoria flows which descended
the southern slope of Mount Mazama prior to its collapse. These
Pinnacles are the results of the most intense fumarolic activity in the
Park (Williams, 1942:8990). In this activity pumice and scoria were
hardened in vertical columns by ascending gasses. The present form of
the Pinnacles is the result of the modification of these original
columns by wind and water erosion. Some of the Pinnacles are actually
hollow and are sometimes referred to as "fossil gas vents."
Curiously little attention has been
given to the fact that the pinnacles are of some ornithologic interest.
Frequently they are used by birds as song perches in the same manner as
dead trees are used. Of even greater interest, however, is the use of
small cavities in some of the Pinnacles as nesting cavities. There are
at present records of the use of such cavities by three species of
birds. On June 26, 1952, I saw a pair of Mountain Chickadees, Parus
gambeli Ridgway, carrying material into one of these cavities.
Although I was unable to be certain, it appeared that the material was
items of food indicating that the eggs had already been hatched. On the
same day Park Naturalist Harry C. Parker and I observed a pair of
Mountain Bluebirds, Sialia currucoides Bechstein, entering
repeatedly an opening in one of the Pinnacles. At the time, we could not
feel certain that nesting activity was in progress. However, on July 29
I saw a female enter the same opening and on August 4, saw both male and
female carrying insects into the cavity. In the vicinity were two
juvenile bluebirds apparently completely independent of the adults. They
were catching insects on the wing. It would appear quite possible that
these juvenile birds were from the first brood with which the
observations of June 26 could be associated, whereas the food-carrying
observed on August 4, was doubtless in conjunction with the rearing of
the second brood.
On July 19, 1952, I discovered a pair
of Violet-green Swallows,
Tachycineta thalassina (Swainson), carrying food into a cavity in
the Wheeler Creek Pinnacles. The young could be seen and heard plainly.
Although Violet-green Swallows have been observed (Farner, 1952:74)
rather frequently in Wheeler Creek Canyon and elsewhere in the Park,
this is actually the first breeding record.
It should be noted that both the
bluebirds and chickadees normally nest in cavities in tree trunks. The
Pinnacles thereby constitute a curious, although understandable,
substitute for tree trunks.
It is further of interest to note that
Rough-winged Swallows,
Stelgidopteryx ruficollis (Vieillot), have also been known to breed
in Wheeler Creek Canyon (Farner, 1952:75). However, it appears that
holes in the cliffs, rather than holes in the Pinnacles, are used.
References
Farner, Donald S. 1952. The Birds of
Crater Lake National Park.
University of Kansas Press. ix + 190 pp.
Williams, Howell 1942. The Geology
of Crater Lake National Park, Oregon. Carnegie Institution of
Washington Publication 540. vi + 162 pp.