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Contributed by Museum of Vertebrate Zoology, University of California, Berkeley.
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Transcription
Journal
R.E. Johnson
1968
March 10 Peavine Mtn., Washoe Co., Nevada (cont.)
ridge has a small cluster of Jeffrey Pines on
it & a road running up it. On its left (west)
slope a large mine dump can be seen we
visited it but found no shaft. We returned
to the "big shaft" and headed south over the west
shoulder of the same hill we had circled on the
road earlier. This hill also has Jeffrey Pine
trees on it. John pointed out that W.D. Billings
had believed that Jeffrey Pine could only compete
with sagebrush & other surrounding vegetation on three
sites which were too poor for sagebrush. These hilltops
he believed to date back to the Pleistocene & to
have highly leached soils. These soils have a light
color & nothing grows on them except the Jeffrey
Pine, which is knarled & stunted. Presumably
the pine could grow on the surrounding better
soils were it not for the brush competition.
In the Pleistocene the Jeffrey Pine had
ancestors
occupied the whole area. At the present time
the dominant vegetation on most sites is Sagebrush,
Artemisia tridentata. Other species include: Ephedra
viridis; Horse brush, Tetradymia (glabata or canescens);
Desert Peach, Prunus andersoni (has spines), Gutierrezia
sarothrae; Onion, Allium parvum (now in bloom); a grass
Sitanion hystrix (6 inches tall, with leaves curling downward);
Great Basin Wild Rye, Elymus; Eriogonum (several species)
Bitterbrush, Purshia tridentata; Bitterroot, Lewisia