Notwithstanding the enthusiastic eagerness of tourists
to reach the crown of the Dome the views of the Valley
from this lofty standpoint are less striking than
from many other points comparatively low, chiefly on
account of the foreshortening effect produced by looking
down from so great a height. The North Dome is
dwarfed almost beyond recognition, the grand sculpture
of the Royal Arches is scarcely noticeable, and the
whole range of walls on both sides seem comparatively
low, especially when the Valley is flooded with noon
sunshine; while the Dome itself, the most sublime
feature of all the Yosemite views, is out of sight
beneath one’s feet. The view of Little Yosemite
Valley is very fine, though inferior to one obtained
from the base of the Starr King Cone, but the summit
landscapes towards Mounts Ritter, Lyell, Dana, Conness,
and the Merced Group, are very effective and complete.
No one has attempted to carry out Anderson’s
plan of making the Dome accessible. For my part
I should prefer leaving it in pure wildness, though,
after all, no great damage could be done by tramping
over it. The surface would be strewn with tin
cans and bottles, but the winter gales would blow
the rubbish away. Avalanches might strip off any
sort of stairway or ladder that might be built.
Blue jays and Clark’s crows have trodden the
Dome for many a day, and so have beetles and chipmunks,
and Tissiack would hardly be more “conquered”
or spoiled should man be added to her list of visitors.
His louder scream and heavier scrambling would not
stir a line of her countenance.
When the sublime ice-floods of the glacial period
poured down the flank of the Range over what is now
Yosemite Valley, they were compelled to break through
a dam of domes extending across from Mount Starr King
to North Dome; and as the period began to draw near
a close the shallowing ice-currents were divided and
the South Dome was, perhaps, the first to emerge,
burnished and shining like a mirror above the surface
of the icy sea; and though it has sustained the wear
and tear of the elements tens of thousands of years,
it yet remains a telling monument of the action of
the great glaciers that brought it to light. Its
entire surface is still covered with glacial hieroglyphics
whose interpretation is the reward of all who devoutly
study them.
Chapter 11
The Ancient Yosemite Glaciers:
How the Valley Was Formed
All California has been glaciated, the low plains
and valleys as well as the mountains. Traces
of an ice-sheet, thousands of feet in thickness, beneath
whose heavy folds the present landscapes have been
molded, may be found everywhere, though glaciers now
exist only among the peaks of the High Sierra.
No other mountain chain on this or any other of the
continents that I have seen is so rich as the Sierra
in bold, striking, well-preserved glacial monuments.
Indeed, every feature is more or less tellingly glacial.
Copyrights
The Yosemite from Project Gutenberg. Public domain.