Image from the Biodiversity Heritage Library.
Contributed by Yale Peabody Museum of Natural History.
| www.biodiversitylibrary.org
Transcription
Santa Barbara, Monday Feb 14
Raining hard this morning and all the steam
mudde in flord.
We leare at 11.30 A.M. to go to Palo Alto
or Stanford University. Got to Ramona Hotel
at 10.15 P.M.
At San Luis Obispo the railway climbs
from about sea-level to over 1000 feet, and soon
one begins to see highly metamorphic rocks --
layers of serpentine and volcanic ones -- and they
continue for a long distance to the north. Evi-
dently these are the San Franciscan series of
Jurassic times. The hills are not high here, not-
ally less than 2000 feet.
South of Obispo the railway goes along the
sea-shore, but northwards one goes inland and follows
for a long time a river that flows into Monterey Bay,
or this valley to the south of San Miguel one
sees fine alluvial terraces.