completely covered with thick, furry mosses, and the white fall shines
against the green like a silver
instrument in a
velvet case. Here
come the Gabriel lads and lassies from the
commonplace orange groves,
to make love and gather ferns and dabble away their hot holidays in
the cool pool. They are
fortunate in
finding so fresh a
retreat so
near their homes. It is the Yosemite of San Gabriel. The walls,
though not of the true Yosemite type either in form or
sculpture, rise
to a
height of nearly two thousand feet. Ferns are
abundant on all
the rocks within reach of the spray, and
picturesque maples and
sycamores spread a
grateful shade over a rich profusion of wild
flowers that grow among the
boulders, from the edge of the pool a mile
or more down the dell-like bottom of the
valley, the whole forming a
charming little poem of wildness--the vestibule of these shaggy
mountain temples.
The foot of the fall is about a thousand feet above the level of the
sea, and here climbing begins. I made my way out of the
valley on the
west side, followed the ridge that forms the
western rim of the Eaton
Basin to the
summit of one of the
principal peaks,
thence crossed the
middle of the basin, forcing a way over its many
subordinate ridges,
and out over the eastern rim, and from first to last during three days
spent in this
excursion, I had to
contend with the richest, most
self-possessed and uncompromising chaparral I have every enjoyed since
first my mountaineering began.
For a hundred feet or so the
ascent was
practicable only by means of
bosses of the club moss that clings to the rock. Above this the ridge
is weathered away to a
slender knife-edge for a distance of two or
three hundred yards, and
thence to the
summit it is a bristly mane of
chaparral. Here and there small
openings occur, commanding grand
views of the
valley and beyond to the ocean. These are favorite
outlooks and resting places for bears, wolves, and wildcats. In the
densest places I came upon woodrat villages whose huts were from four
to eight feet high, built in the same style of
architecture as those
of the muskrats.
The day was nearly done. I reached the
summit and I had time to make
only a hasty
survey of the topography of the wild basin now outspread
maplike beneath, and to drink in the rare
loveliness of the sunlight
before hastening down in search of water. Pushing through another
mile of chaparral, I emerged into one of the most beautiful parklike
groves of live oak I ever saw. The ground beneath was planted only
with aspidiums and brier roses. At the foot of the grove I came to
the dry
channel of one of the
tributary streams, but, following it
down a short distance, I descried a few specimens of the scarlet
mimulus; and I was
assured that water was near. I found about a
bucketful in a
granite bowl, but it was full of leaves and beetles,
making a sort of brown coffee that could be rendered
available only by
filtering it through sand and
charcoal. This I
resolved to do in case
the night came on before I found better. Following the
channel a mile
farther down to its confluence with another, larger
tributary, I found
a lot of
boulder pools, clear as
crystal, and brimming full, linked
together by little glistening currents just strong enough to sing.
Flowers in full bloom adorned the banks, lilies ten feet high, and
luxuriant ferns arching over one another in
lavishabundance, while a
noble old live oak spread its
rugged boughs over all, forming one of
the most perfect and most secluded of Nature's gardens. Here I
camped, making my bed on smooth cobblestones.
Next morning, pushing up the
channel of a
tributary that takes its
rise on Mount San Antonio, I passed many lovely gardens watered by
oozing currentlets, every one of which had lilies in them in the full
pomp of bloom, and a rich growth of ferns,
chiefly woodwardias and
aspidiums and maidenhairs; but toward the base of the mountain the
channel was dry, and the chaparral closed over from bank to bank, so
that I was compelled to creep more than a mile on hands and knees.
In one spot I found an
opening in the
thorny sky where I could stand
erect, and on the further side of the
opening discovered a small pool.
"Now, HERE," I said, "I must be careful in creeping, for the birds of
the
neighborhood come here to drink, and the rattlesnakes come here to
catch them." I then began to cast my eye along the
channel, perhaps
instinctively feeling a snaky
atmosphere, and finally discovered one
rattler between my feet. But there was a
bashful look in his eye, and
a withdrawing, deprecating kink in his neck that showed
plainly as
words could tell that he would not strike, and only wished to be let
alone. I
therefore passed on, lifting my foot a little higher than
usual, and left him to enjoy his life in this his own home.
My next camp was near the heart of the basin, at the head of a grand
system of cascades from ten to two hundred feet high, one following
the other in close
succession and making a total
descent of nearly
seventeen hundred feet. The rocks above me leaned over in a
threatening way and were full of seams, making the camp a very unsafe
one during an earthquake.
Next day the chaparral, in ascending the eastern rim of the basin,
was, if possible, denser and more
stubbornly bayoneted than ever. I
followed bear trails, where in some places I found tufts of their hair
that had been pulled out in squeezing a way through; but there was
much of a very interesting
character that far overpaid all my pains.
Most of the plants are
identical with those of the Sierra, but there
are quite a number of Mexican
species. One coniferous tree was all I
found. This is a
spruce of a
species new to me, Douglasii
macrocarpa.[14]
My last camp was down at the narrow, notched bottom of a dry
channel,
the only open way for the life in the
neighborhood. I
therefore lay
between two fires, built to fence out snakes and wolves.
From the
summit of the eastern rim I had a
glorious view of the
valleyout to the ocean, which would require a whole book for its
description. My bread gave out a day before reaching the settlements,
but I felt all the fresher and clearer for the fast.
XII
Nevada Farms[15]
To the farmer who comes to this thirsty land from beneath rainy skies,
Nevada seems one vast desert, all sage and sand, hopelessly
irredeemable now and forever. And this, under present conditions, is
severely true. For
notwithstanding it has gardens, grainfields, and
hayfields
generouslyproductive, these compared with the arid
stretches of
valley and plain, as
beheld in general views from the
mountain tops, are mere specks lying inconspicuously here and there,
in out-of-the-way places, often thirty or forty miles apart.
In leafy regions,
blessed with
copious rains, we learn to
measure the
productivecapacity of the soil by its natural
vegetation. But this
rule is almost
wholly inapplicable here, for,
notwithstanding its
savage nakedness,
scarce at all veiled by a sparse growth of sage and
linosyris[16], the desert soil of the Great Basin is as rich in the
elements that in rainy regions rise and ripen into food as that of any
other State in the Union. The rocks of its numerous mountain ranges
have been
thoroughly crushed and ground by glaciers, thrashed and
vitalized by the sun, and sifted and outspread in lake basins by
powerful torrents that attended the breaking-up of the glacial period,
as if in every way Nature had been making haste to prepare the land
for the husbandman. Soil,
climate, topographical conditions, all that
the most
exacting could demand, are present, but one thing, water, is
wanting. The present
rainfall would be
wholly inadequate for
agriculture, even if it were advantageously distributed over the
lowlands, while in fact the greater
portion is poured out on the
heights in sudden and
violent thundershowers called "cloud-bursts,"
the waters of which are fruitlessly swallowed up in sandy gulches and
deltas a few minutes after their first
boisterous appearance. The
principal mountain chains, trending nearly north and south, parallel
with the Sierra and the Wahsatch, receive a good deal of snow during
winter, but no great masses are stored up as fountains for large
perennial streams
capable of irrigating
considerable areas. Most of
it is melted before the end of May and absorbed by moraines and
gravelly taluses, which send forth small rills that slip quietly down
the upper canyons through narrow strips of
flowery verdure, most of
them sinking and vanishing before they reach the base of their
fountain ranges. Perhaps not one in ten of the whole number flow out
into the open plains, not a single drop reaches the sea, and only a
few are large enough to
irrigate more than one farm of
moderate size.
It is upon these small outflowing rills that most of the Nevada
ranches are located, lying countersunk beneath the general level, just