Image from the Biodiversity Heritage Library.
Contributed by Museum of Vertebrate Zoology, University of California, Berkeley.
| www.biodiversitylibrary.org
Transcription
creosote desert and lava fields
until get to Newberry Springs
which is just into the edge
of Saltbush scrub. Post New
berry Springs Hwy 40 is in the
flood plain. Creosote is restric-
ted to the flanks of the mount-
ains to the SE of Newberry springs.
Fort Lady Rd goes up into some
higher elev mountains with Pinon
or juniper (can't tell). At Hector Rd
seem to rise out of flood plain and
back into creosote with a triplex. The
flood plane is gone, or more narrower. The
plane is cut off (ended) by the Mtus N
and NE of a crater. Hwy 40 is in the
lowland still, but there is no more
Atriplex. There is a dry (Bristol) lake
S.E. of the crater. The slopes from Hwy
40 to Bristol Lake are covered with low
status creosote. E and N of Bristol
Lake are broad bajadas. Going
E, the bajada peaks & then it dropped
into a broad NS valley. As 40 crosses
the flank of Bristol mountains, plant
diversity increases with grasses, shrubs,
and some Atriplex. These areas are,