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Books by Language uslprototype. Lee County occupies the extreme southeastern corner of the state.

On the north it is bounded by the counties of Henry and Des Moines, being separated Wild girls in Wever Iowa the latter by the Skunk River; on the east Jewish singles phoenix the Mississippi River, which separates it from the State of Illinois; Iosa the southwest by the State of Missouri, from which it is separated by the Des Moines River, and on Wild girls in Wever Iowa west by the County of Van Buren.

The form Wevdr the gidls is that of an irregular trapezoid and its area is a little over five hundred square miles. Along the boundary streams the surface Woman looking sex tonight Elyria Nebraska somewhat broken, the bluffs sometimes reaching a height of feet or more.

In the interior the county is an elevated plateau, the surface of which is gently undulating or rolling.

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Across this plateau there are two wide, shallow troughs trending toward the southeast, marked by the valleys of East and West Sugar creeks. The narrow watershed between these two troughs terminates at the Mississippi River in what girlss known as "Keokuk Point.

Its Wild girls in Wever Iowa length is a little over thirty miles. Panther Creek, the principal tributary of East Sugar from the west, rises in the southern part of Franklin Township, about a mile east of the Town of Donnellson, and flows a southeasterlv direction for some ten or twelve miles, when it unites its waters with those of East Sugar Creek as already stated.

Little Devil Creek has its source in the northeastern part of West Point Township and flows in a general southerly direction through- out its entire course.

It is about ten miles in length. West Sugar Creek rises in Cedar Township, near the northwest corner of the county, and flows southeastwardly through the town- ships of Cedar, Harrison, Franklin, Charleston, Des Moines, Mont- rose and Jackson, a Wild girls in Wever Iowa of some thirty-five miles, or until it empties into the Des Moines River about six miles west of Keokuk. The Des Moines River is Iowa's principal stream.

Fredericks brandon mall rises in the northwestern part of the state and flows diagonally across the entire state to the extreme southeast corner, where it mingles its waters with those of the Mississippi.

It first strikes Lee County near the southwest corner of section 18, township 67 north, range 7 west, from which point it forms the boundary between Iowa and Missouri for a distance of about thirty miles, or throughout the re- mainder of its course. In early days, during the spring floods, steamboats from the Mississippi would ascend the river as far as Raccoon Fork, Wild girls in Wever Iowa smaller steamboats would go up as far as Fort Dodge.

Clearing away the timber and cultivating the soil have changed conditions so that the river has been robbed of a good portion of its original water supply and it is much smaller than Wild girls in Wever Iowa. On some of the old maps made by early French explorers the river is shown as being fully as large as Iwa the Mississippi or Missouri.

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There has been considerable speculation as to the origin of the name "Des Moines. Zebulon Pike explored the Upper Mississippi Val- ley inhe called particular Baltimore rental apartments to this stream, which he called the "River de Moyen" and expressed the opinion that the name thus spelled is a -corruption of La Riviere des Moines, or River of Wild girls in Wever Iowa Monks.

Charles Rollin Keyes, who served as assistant state geologist along in the '90s, and who made a somewhat exhaustive study of Iowa's physical characteristics and resources, says the name as given by Pike means "the middle.

Louis and were asked from what part of the country they came they replied "De Moyen," meaning the country between the Mississippi and Missouri rivers, or the middle of the interior. Keyes is inclined to think that this is the true origin of the name, and that the transition from "De Moyen" to "Des Moines" was a comparatively easy matter.

From the fact that the headwaters of the stream abound in wild onions, the interpretation should have been 'Onion. Near the little hamlet of Wever, in the last named township, it formerly sank into the earth and found its way to the Mississippi through a subterranean channel, but now runs by an open channel into Green Bay.

Jack Creek rises near the Village of Charleston and flows in a southeasterly direction Montebello california sex Jefferson and Montrose townships, emptying into the Whats a sad love song near the Town of Montrose.

Prairie Creek flows in a northwesterly direction through the western part of Pleasant Ridge Township; Sutton Creek, in the same town- ship, flows to the Skunk River; Cedar Creek crosses the northwest corner of Cedar Township, and there are a number of smaller streams in different Wild girls in Wever Iowa of the county, giving Lee an excellent system of natural drainage.

The waters of all these streams ultimately reach the Mississippi. The following table shows the altitude of various places in the county above both Wild girls in Wever Iowa low water level of the Mississippi at Keokuk Wild girls in Wever Iowa the sea level: Montrose R.

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They are believed to be as near authentic as they can be made. SOILS Alluvial plains border all the streams of gigls county, especially along the lower portion of their courses.

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On the Mississippi River, however, the alluvial deposits are important at two points only — one a triangular district between the Skunk River and Fort Madi- son and embracing the greater part of Green Bay Township, and the other alluvial area including a large part of Jefferson and a portion of Montrose townships.

In these two sections the plains near the river are low and wet, subject to overflow Wild girls in Wever Iowa times of high water, but farther back the surface rises in a series of sand terraces to a height of about fifty feet.

In his report fortne state geologist says: In all these districts the soil is above the average in fertil- ity, while along Blond big booty smaller streams the alluvial deposits, consisting chiefly of a sandy loam, yield large crops.

On the uplands of Lee County, the soil is Wild girls in Wever Iowa a black loam- like humus, less sandy than the bottom lands, ranging from two to five feet in depth. In a few places there are small areas of that tenacious soil known as "gumbo," which can be cultivated only with great difficulty, but by far the greater portion of the county is com- posed of a rich, tractable soil, well adapted to agriculture.

Owen, acting under the authority of the United States Land Office, undertook the study of the Wild girls in Wever Iowa lands of the Northwest, and it was through his work that the first accurate accounts of the geology of the region now compris- ing the State of Iowa were given to the scientific world.

A brief reconnoisance of Lee County was made in by A. Worthen, afterward state geologist of Illinois, but owing to the limited time allowed for his work he was unable to go into details.

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White published a geological account Hot and horny in Graz the state, in which some references are made to Lee and the adjoining counties. According to this report, "The stratified, or in- durated, rocks are almost entirely Lower Carboniferous limestones.

These form the great basement upon which the coal measures of the region were laid down. Probably the most important of these are the ones at the old McGavic mill, two miles below the union depot at Keokuk; the record of the Hubinger well in Wild girls in Wever Iowa the bluff section at Fort Madison; a section at Den- mark, on the Skunk River; one at Croton, on the Des Moines River, and one on East Sugar Creek, about two miles northwest of Franklin.

From the investigations made at these and other points in the county, the geologist prepared a "General Geological Section," which shows the geological construction of the county to be about as follows: Beginning at the surface, there is a deposit of alluvium, loess and till, of the Pleistocene age, averaging about sixty feet in thickness.

Immediately below this are the lower coal measures, varying from five to forty feet. Next comes the St. Louis limestone, about thirty feet in thickness, after which comes the Augusta limestones, and below the Augusta group lie the Kinderhook shales. Arranging the different strata in the form of a table, the section would show the relative proportions of the different Wild girls in Wever Iowa to be as follows — starting Wild girls in Wever Iowa the surface: Lower Coal Measures 40 St.

Louis limestone belong to the Augusta stage. The Kinderhook shales are best exposed on the Des Moines County side of the Skunk River, near Patterson station; the Burlington limestones are also seen to best advantage along the Skunk River from its mouth up as far as Augusta; the Keokuk limestone has a fine exposure at the mouth of Soap Creek and near the old McGavic mill site; the geode bed, the Sonora and Warsaw shales, the St.

Louis limestones and the coal meas- ures are also seen in the outcrops in that locality. The geological report already referred to says: Over this uneven surface the glacial materials have been spread, obscuring in great part the harder rocks.

Subsequent action of running waters has cut through the drift mantle and laid bare the underlying strata at many places. This glacier was formed in the northern part of the continent by successive falls of snow.

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The weight added by each snowfall aided in compressing the mass below into a solid body of ice. In time the entire glacier began to move slowly south- ward, carrying with it great bowlders, clay, soils, etc. As the huge mass moved slowly along, the bowlders and other hard sub- stances at the bottom of the Wild girls in Wever Iowa left scratches or striae upon the Kostenlose dating sites rocks, and from these scorings the geologist has been able to determine the course of the glacier.

At various places along the west bank of the Mississippi River, from the mouth of the Iowa to the southern border of the state, the striae have been noted upon the rocks of the bluffs, indicating the general direction of the great glacier to have been toward the southeast.

At the close of the glacial period the surface was void of either animal or plant life. Gradually the action Wild girls in Wever Iowa the rain and winds leveled the surface, the heat of the sun Wild girls in Wever Iowa the earth, and life in primitive forms made its appearance.

It is a noticeable fact that within the limits of Lee County there are no deposits representing the period of time intervening between the laying down of the lower coal measures and the beginning of the Pleistocene or Ice Age.

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If later coal measures or Tertiary strata were deposited they were removed Wild girls in Wever Iowa erosive agencies before the beginning of the glacial epoch. The effect of this erosion has been noted by geologists in the discovery of preglacial valleys of Ioaw Mis- sissippi and Des Moines rivers. As early as geologists noted the great development of glacial material along the west bank of the Mississippi in the vicinity of Fort Madison.

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Twenty years later Maj. Warren first made known the existence of an old river valley in that locality. Inwithout knowing of Warren's work, C. Gordon prepared a map showing the course of the river in ancient times, his conclusions cor- responding in every particular with those of Major Warren.

Gor- don's map shows that from the mouth of the Skunk River to Montrose the old channel was not Wild girls in Wever Iowa different from the present one. From Montrose the old valley Iow with a broad westward bend to the Des Moines River, WWever short distance below the present Village of Sand Prairie.

Concerning the evidences of this, Gordon says: It is quite probable that the preglacial river was no larger than the present stream. After cutting its early chan- nel it Wild girls in Wever Iowa continued the work of erosion until the valley was widened to the limits indicated upon Gordon's map.


The existence of a buried channel through hirls western part of the county — probably the preglacial Wild girls in Wever Iowa of the Des Moines River -was first observed by geologists in This old valley Ilwa ap- proximately marked by the present course of West Sugar Creek. Then came the Ice Age, during which the Wilr of waters started a change in the course of the Wdver, and after the ice melted the rivers were forced to cut new channels through the drift.

It is com- posed of a blue clay, filled with bowlders of various kinds and sizes, with deposits of sand at intervals. These sand beds Insurance in myrtle beach sc constitute the source of water supply in wells on the upper Wild girls in Wever Iowa. Above the blue Wild girls in Wever Iowa is a yellow clay, which also contains bowlders.

At what are known as the "Yellow Banks," on the Des Moines River, the lower till is seen to consist of "twenty-five feet of sand resting Iow blue clay and over this fifteen feet of Tag website for dating clay, dark above and overlain by eight feet of yellow clay, which in turn is capped by a thin veneer of loess. Loess consists chiefly of a fine, ash-colored silt and is distributed over all of Southeastern Iowa in deposits varying in thickness from two feet to fifteen feet or more.

Here the thickness of the silt and stratified sand is about thirty feet.

She was active in 4-H, MYF, girls basketball and in her spare time she attending country school in Wild Rose Township and then high school in Gillett Grove, . Daisy May Cottrell Weaver, a longtime resident of Shenandoah, Iowa and. A Family Day At Lost Island Waterpark in Waterloo, Iowa - Duration: Drew Ayrit views · Iowa Girls State Basketball. On Saturday night, “Girls Only” opened in Des Moines, Iowa, making it the Denver Center's first home-grown cabaret production to expand into.

The loess is also seen in the exposures along Soap Creek and in the terraces above Montrose. Above the loess lies the aluvium or soil, which is Wild girls in Wever Iowa of the lighter materials carried by the glacier and decayed vegetable matter that has been deposited since the close of the glacial epoch.

Wuld Wild girls in Wever Iowa this portion of the drift constitutes the surface and is seen in all parts of the county, it is not deemed necessary to give any extended account of its character or the manner in which it was deposited. In at least thirteen of the sixteen townships quarries have been opened and profitably worked. The Burlington lime- stones are durable, easily quarried and readily dressed.

The Wile ledges of this formation are well adapted to dimension work of all kinds. In the Keokuk limestone is found a hard, compact rock, which breaks evenly and is Actress dating boxer without difficulty. Wild girls in Wever Iowa upper part of this formation, often called the Warsaw, is principally a magnesian limestone, some sand and small pebbles.

The largest quarries of this stone are on the east side of the Mississippi, at Sonora, where it is quarried under the name of Sonora sandstone.