History of Linn County Iowa: From Its Earliest Settlement to the Present Time [1911]Brewer, Luther Albertus
History
History of Linn County Iowa: From Its Earliest Settlement to the Present Time [1911]
Brewer, Luther Albertus
Linn County (Iowa) -- Biography; Linn County (Iowa) -- History; Registers of births, etc. -- Iowa -- Linn County
For a succession of geologic ages our county, in common with eastern
Iowa, seems to have remained dry land, for no deposits of the sea are
found upon it. On both sides of the continent mountain ranges of Alpine
height were uplifted, and during the immeasurable years worn down,
grain by grain, to flat and featureless plains. But no deformations are
recorded in our county history and the lands seems to have remained so
low that little erosion was possible. We are permitted to conceive that
over our savannas in Mesozoic times there roamed monstrous reptiles of
strange shapes, such as are known to have existed in adjacent states.
In the later ages of this era it is not impossible that during the
great submergence which brought the Cretaceous sea over the Great
Plains from the Arctic to the Gulf, including western Iowa, our area
also may have been inundated and huge swimming reptiles such as are
found in the deposits of Kansas and Nebraska may have disported
themselves where now our rich farm lands lie open to the sun, while in
the air featherless cold-blooded creatures larger than any bird winged
their way on leathery pinions.
[Illustration: THE ASTOR HOUSE Erected by John Young in 1839, Looking
South The Second House in Cedar Rapids COURTESY CARROLL'S HISTORY]
During the millions of years which are included in the Tertiary ages
Linn county was undoubtedly dry land. On our grass lands pastured a
succession of strange and uncouth mammals evolving into higher and
higher forms. Among these denizens of the county were probably herds of
pig-like creatures, three toed horses little bigger than foxes, and
ancestral monkeys swarming in the trees, for such are known to have
existed in other states. But these chapters in the history of the
county can not be written from any local records.
THE GLACIAL EPOCH
The warm climate of Tertiary times changed slowly to one of arctic
cold. The winters lengthened and the summers becoming ever cooler and
yet cooler failed at last to melt the winter snows. Vast sheets of
glacial ice, such as that which shrouds Greenland today, covered much
of the continent. The geologic panorama thus presents our area as
buried beneath one after another of slow-moving glaciers hundreds of
feet thick. The proofs of their existence are found in almost every
cutting which goes below the soil. Any quarry will show the rock deeply
rotted and pitted by long preglacial decay. Here and there upon its
surface will be found remnants of the deep red residual clays, the
subsoils of preglacial times. Upon these clays formed from the decaying
rock rest stony clays in which clay, sand, and stones faceted as only
glacier ice can facet, are mingled pell-mell together, as only glacier
ice can mingle. Occasionally is found the unmistakable track of the
glacier left on the underlying rock scraped smooth and marked with
parallel scorings, as at the north end of the cut of the Chicago,
Milwaukee & St. Paul Railway at Linn Junction.
Public-domain text, read in full here on John Shaqi.
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