The Botanists at Crater Lake National Park
by Elizabeth L. Horn
Kalmiopsis Volume 12, 2005 31
Early Interpreters and a Park Flora: F. Lyle Wynd
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F. Lyle Wynd high school graduation
photograph, 1923, from Eugene High School Yearbook.
Courtesy of Lane County Historical Museum, Eugene,
OR |
Wynd (1904-1987) spent his youth at Fort Klamath, only ten miles
from the Park’s boundary and became enthralled with Crater Lake. He was only 18
when he started working there as a ranger naturalist (Love 2002). Between 1923
and 1930 he collected extensively, and six years later he published the first
“Flora of Crater Lake National Park” (Wynd 1936), which listed 433 species (Zika
2003). He personally collected all but three of the listed specimens, indicating
his intimacy with the Park’s flora. His specimens became part of the University
of Oregon Herbarium (now housed at Oregon State University).
Wynd worked with C. Hart Merriam and was intrigued with the
concept of Life Zones, which recognized that plant and animal species occur in
latitudinal and altitudinal zones. Wynd went beyond finding and listing plants
to describe how plants grouped together in communities; thus expanding botanical
knowledge at CLNP to include habitats and vegetation patterns. He adapted
Merriam’s concept to describe three Life Zones in the Park. By increasing
elevation these were 1) the Transition Zone, indicated by ponderosa pine (Pinus
ponderosa) occurring mostly in the southeastern and northeastern corners of
the park and interspersed with moist canyons, open slopes and meadows; 2) the
Canadian Zone where forest cover is primarily lodgepole pine (P.
contorta) and western white pine (P.
monticola), from about 5,500 ft. elevation up to the Hudsonian Zone; and 3)
the Hudsonian Zone, which includes forests of mountain hemlock (Tsuga
mertensiana) and whitebark pine (Pinus
albicaulis) on ridges (Wynd 1941). Within the Canadian Zone, diversity is
contributed by environments such as streamsides, pumice flats (the Pumice
Desert), and islands (Wizard Island and Phantom Ship). Comparable variation in
the Hudsonian Zone is found in open pumice slopes around the rim, streamsides,
talus slopes, and wet areas.
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Herbarium sheet of Wynd’s
holotype for Ranunculus terrestris
collected at Red Blanket Creek, CLNP. Lyman
Benson annotated the specimen as Ranunulus
gormanii Greene in 1932. |