the arch between rock and water,
making a novel and beautiful effect.

Under ordinary weather conditions the fall strikes on flat-topped slabs,
forming a kind of ledge about two-thirds of the way down from the top,
and as the fall sways back and forth with great variety of motions
among these flat-topped pillars, kissing and plashing notes as well as
thunder-like detonations are produced, like those of the Yosemite Fall,
though on a smaller scale.

The rainbows of the Veil, or rather the spray- and foam-bows, are
superb, because the waters are dashed among angular blocks of granite
at the foot, producing abundance of spray of the best quality for iris
effects, and also for a luxuriant growth of grass and maiden-hair on
the side of the talus, which lower down is planted with oak, laurel
and willows.

General Features Of The Valley

On the other side of the Valley, almost immediately opposite the Bridal
Veil, there is another fine fall, considerably wider than the Veil when
the snow is melting fast and more than 1000 feet in height, measured
from the brow of the cliff where it first springs out into the air to
the head of the rocky talus on which it strikes and is broken up into
ragged cascades. It is called the Ribbon Fall or Virgin's Tears. During
the spring floods it is a magnificent object, but the suffocating blasts
of spray that fill the recess in the wall which it occupies prevent a
near approach. In autumn, however when its feeble current falls in a
shower, it may then pass for tears with the sentimental onlooker fresh
from a visit to the Bridal Veil.

Just beyond this glorious flood the El Capitan Rock, regarded by many as
the most sublime feature of the Valley, is seen through the pine groves,
standing forward beyond the general line of the wall in most imposing
grandeur, a type of permanence. It is 3300 feet high, a plain, severely
simple, glacier-sculptured face of granite, the end of one of the most
compact and enduring of the mountain ridges, unrivaled in height and
breadth and flawless strength.

Across the Valley from here, next to the Bridal Veil, are the
picturesque Cathedral Rocks, nearly 2700 feet high, making a noble
display of fine yet massive sculpture. They are closely related to El
Capitan, having been eroded from the same mountain ridge by the great
Yosemite Glacier when the Valley was in process of formation.

Next to the Cathedral Rocks on the south side towers the Sentinel Rock
t