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The Story of the Rocks
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THERE
was a timehundreds of million of years agowhen
the flat top of Starved Rock was but a spot in the sandy bottom
of an oceanan ocean that covered most of the Middle West!
The Exposed Coal
Seam at Buffalo Rock
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The waters of that ocean had gradually
invaded most of the land, creeping in stealthily its some
places and in others with the force and power of a mighty
torrent. The high Ozark Mountains of Missouri kept their
heads above the water,, but few indeed were the other spots
left unsubmerged in this vast area. This ocean deposited
a layer of clean white sand now called Saint Peter Sandstone.
Ages later the waters receded, then returned and once again
retreated in their never-ending battle with the land
For
a timeperhaps a hundred thousand
years or moreplants took root and flourished in the
soft sands. The climate was tropical, warm, and sultry
all the year round. Great fern-like trees sprang up; mosses
as high as a mans waist grew in their shade. But
this was not for long. The seas returned, depositing their
layer, of sand over this luxuriant vegetation, forcing
it into compact lavers, from a foot tot eighteen inches
thick. As more sand settled ins these layers of vegetation
its the many years that followed, they turned into coal. |
Rock Layers that
Tell... |
The pre-historic ocean that deposited
the sand entered the valley many times. Some idea of the
number of times it covered the site of Starved lock can
be gained by counting the various strata of the rock and
its surrounding cliffs.
Only
a million years agoa comparatively
recent period as geologists measure timethe earth
grew steadily colder. This change did not take place abruptly,
but over a period of many thousand years. It began to snow
during the winters. Each year it snowed more, and the snow
stayed longer. Then came the first great glacier, pressing
clown from the frozen north, a mountain of ice that extended
as far as the eye could seehad there been men or
animals to see it. After several thousand years this glacier
began to melt, and its icy waters loured down the valley
of the Illinois River.
Several such glaciers moved down from
the north, covering Starved Rock with sheets of ice several
hundred feet thick. When they melted their waters flowed
down the valley, cutting through the softer parts of the
sandstone and leaving the harder portions to form the fantastic
shapes we now see in the park. |
Even the canyons were cut by
the rush of glacial waters as they tossed and churned on
their way to the Gulf of Mexico. Each spring the waters
spread out over the plains, then cut their way back to
the river. Heavy rains and thawing winter snows also contributed
to the torrents that washed away the rocks. Waterfalls
were formed where hard, cemented layers of stone gave way
to soft sand that was easily washed away. The process has
not ceased. The little rivulets that now flow in the canyons
imperceptibly but constantly wear away the rock over which
they flow.
The many caves in the bluffs were formed
by streams of water that forced their way under the rock,
undermining the cliffs. The over-hanging rocks fell when
their supports had been washed away, leaving caves that
provided shelters for the earliest inhabitants of the valley.
Most of these caves are small, but one, Council Cave, is
large enough to permit a thousand persons to stand beneath
its sheltering roof.
The ancestor of the Illinois River that carried
the torrents of glacial waters was more than a mile wide
and extended from bluff to bluff. At one time it covered
the broad flood-plain on the northern shore; now it is
a small stream, occupying only a small portion of its former
bed. Once, in its early days, it was strong enough to send
its eddies between the rock and the bluff, carving out
tine valleys that separate Starved Rock from the bluffs. |
...the Story of the
Rocks.
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The trees and flowers that thrive in
tire park are all native to Illinois. The oldest trees
in the park are white pines, reminders of a day when once
these towering giants were lords of the soil. Oaks, maples,
elms, and many other species now predominate where once
the pines were most common. Bushes of all kind, known in
Illinois thrive ]it the moist sandy earth. Ferns with great
broad fronds cling to rocky ledges where even a bird could
not rest. The forest floor is covered with wild flowers
of all the varied hues of the rainbow. The delicately shaded
columbine with its red and white flowers may he seen in
any canyon and along any of tit, wooded paths. The foxglove,
too, grows in profusion. Protected from drought by the
porous sandstone which ever yields it, moisture to plants,
these and a thousand other flowers bloom at Starved Rock
every year.
Where now the squirrel scampers to bury
its food, once roamed more ferocious animals in search
of their prey. Wildcats, bear, and wolves had their hiding
places in these words. Buffaloes and deer were the first
citizens of this state of nature. Along the waterfront
and in the swamps were the mounds of muskrats and the darns
of beavers. These, however, are long gone. The Indians
hunted them and reduced their numbers and the steady push
of the first settlers drove them to the farther west. Only
those animals titan can live in friendship with man have
survived.
Frenchmen visiting the Illinois valley
in tire seventeenth century mentioned the brilliantly colored paroquets that
lived lure at that time. Today these are no longer seen,
but the little wren is still merry with song and the cardinal
is a spot of red in the tree. The red-winged blackbird,
the scarlet tanager, the canary, and the blue-jay lend
their colors to the bird-life in which the park abounds. |
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