"Industry and nature have made the state of Iowa a creditor. Her soil has always been solvent and her system of farming does not tend to pauperize. She is a constant seller and therefore wants the evidence of the transaction to be unimpeachable. She has more school teachers than any other state except the Empire state and only three and six-tenths per cent of her population are illiterates. The state of Iowa has yielded the greatest dividends on her educational investments. She has become illustrious on account of her enlightenment. She has progressed further from 'primitive indifferent tissue' than the land even of Darwin himself, and in her escape from protoplasm and prejudice she is practically out of danger. Marked out in the beginning by the hand of God, bounded on the east and west by the two great rivers of the continent, purified and stimulated by the snows of winter, blessed with copious rainfall in the growing season, with generous soil and stately forests interspersed, no wonder that the dusky aborigines exclaimed when they crossed the Father of Waters, 'Iowa, this is the place!' Not only did the red men give our state its beautiful and poetic name, but Indian nomenclature runs like a romance throughout the counties and communities. What infinite meaning, what tokens of joy and sadness, of triumph and of tears, of valor and of vanquishment, of life and love and song there may be in these weird, strange words that name to-day so many of our towns and streams and counties: Allamakee, Chickasaw, Dakota City, Sioux, Pocahontas, Winneshiek, Keosauqua, Sac, Winnebago, Tama, Nodawa, Competine, Chariton, Comanche, Cherokee, Waukon, Muchakinock, Washta, Monona, Waupeton, Onawa, Keota, Waudina, Ioka, Ottumwa, Oneska, Waukee, Waucoma, Nishnabotna, Keokuk, Decorah, Wapello, Muscatine, Maquoketa, Mahaska, Ocheyedan, Mississippi, Appanoose, Missouri, Quasqueton, Anamosa, Poweshiek, Pottawattamie, Osceola, Oskaloosa, Wapsipinicon.
"Ere long some westland genius, moved by the mystic inspiration of the rich and wondrous heritage of Iowa nativity, may sing the song of our legends and traditions, may voice in verse the wondrous story of his illustrious state. Maybe somewhere among the humble homes where blood and bone and brain grow pure and strong, where simple food with frugal ways feeds wondering minds and drives them craving into nature's secrets and her songs—somewhere along the settler's pathway or by the Indian trail where now the country churchyards grown with uncut grasses hide the forms of sturdy ancestors sleeping all in peaceful ignorance of wayward sons or wondrous progeny—somewhere where rising sun beholds the peasantry at early toil and leaves them in the mystic twilight ere their tasks are done, where odors of the corn and new-mown hay and vine-clad hedges by the shadowy roadside linger long into the night-time, as a sweet and sacred balm for tired hearts—somewhere, sometime the song of Iowa shall rise and live, and it will not omit the thought of that gifted son who said: 'Iowa, the affections of her people, like the rivers of her borders, flow to an inseparable union.'"
[CHAPTER V]
The Geology of Linn County
BY WILLIAM HARMON NORTON, PROFESSOR OF GEOLOGY IN CORNELL COLLEGE
It is said that a certain county in Kentucky, underlain by limestone, always goes democratic; while a county adjacent, underlain by sandstone, is as invariably republican. Certain it is that a deal of politics, economics, and history depends at last analysis more or less upon the processes past and present which belong to geology and physiography. The rocks, the minerals they contain, and the water they store, the hills and valleys into which they have been carved, and the soils to which they weather, largely control the industries, locate the cities, and outcrop even in the social, intellectual, and moral life of the people. The metropolis of Linn county, for example, owes its name and place to the rapids of the Cedar, and the rapids find ultimate cause in the fact that some millions of years ago nature stopped laying a softer rock upon the ocean bed and deposited upon it one of more resistant texture. In the eastern part of the county the Chicago & Northwestern Railway runs for very good and sufficient reasons where once rested the edge of a long tongue of glacial ice, and west of Cedar Rapids its route is determined by the course taken by the turbid floods issuing from the melting glaciers. The streets of Mount Vernon and several of the main highways of the county do not lie with the points of the compass but follow the direction of flow of ancient ice-streams. The distribution of forest and prairie is due to geologic causes. The values of farm lands are markedly affected by the same influences, and we can even point out a little area which differs from its surroundings in its inhabitants and in their literacy, language, architecture, manners, and morals, primarily because it belongs to what geologists classify as the deeply dissected loess-covered Kansan drift sheet.
The inductive history of Linn county, reasoned out from what we have learned of the lie of the land, the shapes of hills and valleys, the soils and subsoils, and the underlying rocks, is a wonderfully long one. The first chapter that has been opened to inspection in the geologic record of our area is that of the deepest rocks probed by the first deep well drilled at Cedar Rapids. At a depth of 2,150 feet from the surface—1,417 feet below the level of the sea—the drill encountered a hard red siliceous rock which may be taken as the equivalent of the Sioux Quartzite, which comes to the surface at Sioux Falls, South Dakota, and at Baraboo, Wisconsin. This well known building stone is used in a number of the business blocks and private residences of Cedar Rapids, as for example in the old office building of the Republican. Belonging to the Algonkian, an era so remote that its age must be reckoned in scores if not in hundreds of millions of years, the quartzite at the bottom of the deep well tells of time inconceivably remote when Linn county was part of a wide sea floor on which red sands were washed to and fro and finally laid to rest in thick deposits of sandstone. Tilted and folded and hardened by pressure, the Algonkian rocks were uplifted from the sea to form dry land of mountainous heights. After the lapse of ages the old land sunk beneath the sea, and again and again with intervals of uplift and subaerial erosion there were laid upon it sea muds, impure limestones, and thick sandstones during a long succession of geologic aeons. Samples of these deposits can be seen in the well drillings preserved in the Y. M. C. A. at Cedar Rapids and in the collections of Cornell College. For many millions of years Linn county was thus sometimes land and sometimes sea, but neither land nor sea was tenanted by aught but the humblest of living creatures. These ancient deposits concern us because they are the aqueducts by which artesian waters of purest quality are brought to our doors from their sources far to the northward in other states.
