VIIL CONTENTS. 
CHAPTER IV. 
Ocoya Creek Depot Camp—Ocoya creek to the Tejon—Tejon Depot Camp. 
Ocoya creek.—Rounded hills.—Fossils.—Charcoal and pumice-stone in the strata.—Hills between camp and the Posuncula | 
river. —Bottom-land of Posuncula river.—Swamp or Shallow pond.—Rounded hills on the west side of the Tulare valley.— | 
. Sandstone and fossils of Ocoya creek.—Selenite.—Shark’s teeth on the hills.—Ocoya creek to the Tejon.—Steep slopes of 
the hills Fa river.—Terrace.— Fossil stems —Conglomerate.—Terraces.—Light argillaceous soil.—Tertiary 
hills.—Drift at Tejon creek.—Tejon.—Sierra Nevada.—Depot camp. —Soil of the Tejon.—Oak openings—Indian reser- 
I udin of the soil by Indians.—Gra m itis of the Tejon valley. 
CHAPTER V. 
Tejon to San Amedio—Cañada de las Uvas. 
Reported existence of silver. — Entrance to the Cañada de las Uvas.—Sandstone strata, probably Tertiary —Miocene fossils.— 
Contorted strata. — Upraised sandstone strata.—Oak trees and acorns.—Mountain sheep.— Granite and gneiss.—Ruins of 
u forge. ias tpe of Br —Fir trees.—Granite of the ravine.—Large masses of antimony ore.—Outcrops of the 
vein. —Gossan.—Gyps co an of the vein.—View from the top of the mountain.—Coast mountains.—Dry lake or 
E in. pnm to € Die e las Uvas.—Section of sandstone strata. — Mountain sheep.— Deer. —Cañada de las Uvas.— 
Dr.ft from the Pass in the E —Sandstone filled with fossil shells.—Granite and metamorphic rocks.—Oak trees.— 
war, bears.—Open valley. P unsuper ti —Dry lake covered with salt. ee bear. —Granite and erupted rock. —Up- 
strata of sandstone.— d hills.—Erupted rocks in dykes:—Section of sandstone strata.—Fossil stems of 
c. silicified. —Ridges of white وس‎ at the summit of the pass. pm ore.—Tertiary strata. 
CHAPTER VI. 
Tejon to the Great Basin and Pass of San Francisquito—Pass of San Francisquito to the Mojave 
river. 
'Tejon Pass.—Granitic and metamorphic rocks. 一 Slope of the basin.— Yucca trees.—Tertiary.—Lost mountains.—Spring.— 
Porphyry.—Spring resorted to by Indians.- -Horns of the mountain sheep. —Dry lake-bed of clay.—Granite forming lost 
mountains.—Transverse chain of mountains, forming the southern boundary ot the basin.—Pass of San Francisquito.— 
Upraised strata, brecciated.—Volcanic rocks and obsidian in the strata.—Foot hills of sedimentary rocks.—Antelope. — 
Granite.—Lake Elizabeth.—View from the summit of the Pass.—Granitic and metamorphic rocks —Upraised ar OE 
probably Tertiary.—Talcose and auriferous slates.—Gold.—San Francisquito Pass to the Mojave river.—Cow ETT 
Hornblende and mica slate.— Hills of oa ee uo valleys.—Slope of the Great Basin. —Plants. Haro 
river.— Granite and metamorphic rocks.—Alluvi 
CHAPTER VI. 
Mojave River, by qe tetas s Pass, to San Fernando and Los Angeles.—Los u n to San 
Bernardino.—Cajon Puss. 
Mojave T: Williamson's Pass.— Granite.—Johnson's river.—Copper ore.—Inclined strata of sandstone. — Cottonwood 
Vise upted rocks and agate.—Cow camp.—Rounded hills. —Breccia of volcanic rocks. —Erupted dyke of porphyry.— 
Grani = ds summit of Williamson's Pass.—Trap dyke.—Vein of copper ore.— White granite.—Sandstones and con- 
gl urge upraised. — Bluff of sandstone. —Graphic syenite.—Iron ore. —Metamorphic rocks.—Low hills of sandstone.— 
San Francisquito rancho.—Alluvium of the Santa Clara.—Sandstone.—San Fernando Pass.— Tertiary fossils —Fig trees 
ngeles.—Bitumen springs.— Vineyards and wine.—San Gabriel.—Road to San Bernardino.—-San al 
mons — Soil and climate of the valley.— Productions.— Hot springs.— Analysis of the deposit from the springs. —B 
hot water. Pis of the nn camp.—Soil containing salt.—Cajon Pass. —Upraised strata of sandstone, MENU 
'Tertiary.—Granite.— Limestone.— Vegetation. 
CHAPTER VIII. 
San Bernardino to the Colorado desert.— Colorado desert to Carrizo Creek and Warner's valley. 
San Bernardino or San Gorgoño Pass.— Salt on the borders of the Santa Anna.—Weaver’s rancho. er 200% Gorgoño 
meuntain. —Granitic and ee toe rocks.—Hocks cut by driving sand. —Prevailing wind. —Metamorphic rocks. — - 
