le Sugar and Yellow
Pines, Douglas Spruce, Libocedrus, and the Silver Firs, each a giant of
its kind, assembled together in one and the same forest, surpassing all
other coniferous forests in the world, both in the number of its species
and in the size and beauty of its trees. The winds flow in melody
through their colossal spires, and they are vocal everywhere with the
songs of birds and running water. Miles of fragrant ceanothus and
manzanita bushes bloom beneath them, and lily gardens and meadows, and
damp, ferny glens in endless variety of fragrance and color, compelling
the admiration of every observer. Sweeping on over ridge and valley,
these noble trees extend a continuous belt from end to end of the range,
only slightly interrupted by sheer-walled canons at intervals of about
fifteen and twenty miles. Here the great burly brown bears delight to
roam, harmonizing with the brown boles of the trees beneath which they
feed. Deer, also, dwell here, and find food and shelter in the ceanothus
tangles, with a multitude of smaller people. Above this region of
giants, the trees grow smaller until the utmost limit of the timber line
is reached on the stormy mountain-slopes at a height of from ten to
twelve thousand feet above the sea, where the Dwarf Pine is so lowly and
hard beset by storms and heavy snow, it is pressed into flat tangles,
over the tops of which we may easily walk. Below the main forest belt
the trees likewise diminish in size, frost and burning drought repressing
and blasting alike.

The rose-purple zone along the base of the range comprehends nearly all
the famous gold region of California. And here it was that miners from
every country under the sun assembled in a wild, torrent-like rush to
seek their fortunes. On the banks of every river, ravine, and gully they
have left their marks. Every gravel- and boulder-bed has been
desperately riddled over and over again. But in this region the pick and
shovel, once wielded with savage enthusiasm, have been laid away, and
only quartz-mining is now being carried on to any considerable extent.
The zone in general is made up of low, tawny, waving foot-hills,
roughened here and there with brush and trees, and outcropping masses of
slate, colored gray and red with lichens. The smaller masses of slate,
rising abruptly from the dry, grassy sod in leaning slabs, look like
ancient tombstones in a deserted burying-ground. In early spring, say
from February to April, the w