Canada -- Description and travel; United States -- Description and travel
The Valley is a Government Park, which also includes the watershed of
the streams flowing into it. Originally it was the home of the Digger
Indians, a tribe of Shoshonés, and a rather low type, of whom a few
still survive. It was first seen by white men in 1851, when a
detachment of troops pursuing these Indians came unexpectedly upon it.
The attractions soon became widely known, and visitors were numerous,
especially after the opening of the Pacific Railways. Entering the
Valley, the most striking object is its northwestern buttress, the
ponderous cliff El Capitan, rising thirty-three hundred feet, at a
very narrow part, its majestic form dominating the view. There are two
vertical mountain walls almost at right angles, these enormous bare
precipices facing west and south. On the opposite side, forming the
other portal, rise the imposing Cathedral Rocks, adjoined by the two
slender Cathedral Spires of splintered granite, nearly three thousand
feet high. Over these rocks on their western side pours the Bridal
Veil Fall, about seventy feet wide, and descending vertically six
hundred and thirty feet. As the winds often make the foaming column
flutter like a white veil, its title has been appropriately given.
Adjoining El Capitan descends the Ribbon Fall, or the Virgin's Tears,
falling two thousand feet, but losing much of its waters as the summer
advances. Eastward of El Capitan are the peaks called the Three
Brothers, the highest also named the Eagle Peak, rising three thousand
feet. To the eastward of this peak and in a recess near the centre of
the Valley are the Yosemite Falls, one of the highest waterfalls in
the world. Yosemite Creek, which comes over the brink with a breadth
of thirty-five feet, descends twenty-five hundred feet in three leaps.
It pours down a vertical wall, the Upper Fall descending nearly
fifteen hundred feet without a break, the column of water swaying as
the winds blow with marvellous grace of motion, the eddying mists
fading into light summer clouds above. The Middle Fall is a series of
cascades descending over six hundred feet, and the Lower Fall is four
hundred feet high. This is one of the grandest features of the Valley,
but its vigor, too, dwindles as the season advances. There is a high
and splendid ice cone formed at the foot of the Upper Fall in the
winter. Alongside, upon a projection called Yosemite Point, at over
thirty-two hundred feet elevation, is given one of the best views of
the famous Valley.
Public-domain text, read in full here on John Shaqi.
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