Image from the Biodiversity Heritage Library.
Contributed by Museum of Vertebrate Zoology, University of California, Berkeley.
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Transcription
JESimpson, 1958
29.
1000 ± ft., 2 mi. n.e. Tinajas de los Papagos, Sierra del Pincate, Sonora
March 24, 1938, continued
the palos verdes, mesquite, and iron-wood of the
wash contrasts with the adjacent lava fields. Here
two miles to the northeast the creosote entirely
dominates the cinder fields; near Papago tanks,
however, creosote tho heavy is associated with some
saquero, much ochotillo, cholla, palo verde, mesquite, etc.
After putting up our specimens (Dr. Benson helped
me.) we broke camp, and drove (accompanied by Mr. Lenon
and his Plymouth coupe) six and a half miles to:
850 ft., Paso McDougal, Pinacate Region, Sonora
Here we made camp at base of Sierra Hornaday.
Set out 50 mousetraps along the face of " " ;
37 mousetraps in sand-grass at base of " " ;
50 live traps after dark within few hundred yards" ".
March 25, 1958
Along the east face of Sierra Hornaday caught
9 Peromyscus eremicus (5♂+4♀; put up two: 69♀,70♂);.
2 Peromyscus crinitus (71♂and 75♀), and one Perognathus
intermedius (but its skull was badly broken; also the tail of one
was in a trap). In the sand and grass caught 15 Dipodomys
merriami (100♂+5♀; see 730and 740) and one Perognathus
pencillatus (720). Cheek-pouch contents of latter and the
kangaroo rats saved.
Sierra Hornaday, unlike the majority of the peaks
and ranges of the near vicinity?, is not lava at all;
it is composed of mazonite and granite mostly
(granite-like but without quartz)