LOCATION AND NATURAL FEATURES.
JACKSON County (formerly Calhoun), was one of the thirty-three counties
organized by the first Territorial Legislature of Kansas, at its session in
1858, at the Shawnee Manual Labor School, in Johnson County. Calhoun County
embraced upwards of 1,140 square miles.
February 11, 1859, by act of the Territorial Legislature, the names of Calhoun
- suggestive of treason of the American nation - gave way to Jackson, in honor
of the President who boldly denounced nullification, and "by the Eternal"
declared "nation" constitutionally written with a big "N."
The lines of Brown, Jackson and Shawnee counties were changed by an act of
the Legislature of 1868, and the county-seat of Jackson County was thereby
permanently located at Holton.
The northwest portion of the county was government land; from Netawaka east in
the northeast part of the county, having for a southern boundary the line of
Straight Creek, was the land of the Kickapoos. Their diminished reserve is
now entirely within the limits of Brown County. The Delaware lands lay south
of the Kickapoo Reserve, in the east part of the county. In the southwest
part of the county was the Pottawatomie Reservation, now diminished to a tract
eleven by eleven miles, with an area of 121 square miles, leaving some 530
square miles of territory in the county available for settlement.
The Delaware lands were brought into market July, 1857, at a public sale held
at Osawkee, prior to which time settlements had been made on these lands, and
the appraisements were from $1.25 to $2 per acre, where the occupant had a
cabin and slight improvements on a quarter section. The Kickapoo Reservation
was purchased or granted as a subsidy to the Central Branch of the Union
Pacific Railroad in 1867, and settlement commenced on these lands in June of
that year.
The Diminished Pottawatomic Reserve has been long looked upon as a section
exceedingly fertile, and highly desirable for settlement, but since 1875,
there has been but little expectation that it would become a part of the
taxable domain of Jackson County, until at a somewhat distant period. State
Senator John S Hopkins, at Topeka, February 15, 1875, wrote to Frank A. Root,
then Editor of the Holton Express and News, as follows:
The prospect is good for the early selling out of the lands and removal of the
diminished reserve band of Pottawatomic Indians, located in the bowels of our
county. No fact will be left unpresented by those having the matter in hand,
showing the situation of our county - the demoralizing effects, both upon the
Indians and settlers, of the policy of surrounding a band of Indians by white
settlements, the willingness on the part of the reserve band to remove beyond
the whiteman's plow. Earnest work in the right direction is now being
performed.
The general surface of Jackson County is undulating: the rolling prairies
rising and falling in gentle swells; the elevation averaging about thirty feet
in a distance of a mile or more. These crestlines of motionless waves are
intersecting each other at every conceivable angle, which brings into view the
most extensive landscape, and shows the light green of the prairie grasses in
pleasing contrast with the dark green foliage of the forest trees of greater
or less size, which skirt the many streams of running water that pass through
the county. Of upland prairie there is 87 per cent, of bottom land 13 per
cent, of timber land 7 per cent. The average width of the creek bottom lands
is one mile, of timber belts one-half mile.
Lime and sandstone exist in large quantities. A most excellent whitish
magnesian limestone is found in different portions of the county, which though
easily worked when first quarried, becomes hard and exceedingly durable when
exposed to the air. The Linscott Bank building on the west side of the public
square at Holton, and the Campbell University building, furnish excellent
specimens of this choice material for public and private structures. To the
northeast and south of Holton, on the Elk and Barmer creeks, may be found the
best specimens of brick-clay, and large quantities of brick have been made
therefrom. Coal has been discovered in some parts of the county, but few
mines have as yet been opened; the thickness of the veins not warranting the
expense of excavating for it.
In the bottom lands the soil is a rich sandy loam; it is a heavier black soil
on the upland prairie, but it is all easily cultivated, and there are scarcely
any untillable lands in the county. The depths of soil varies from eighteen
inches to four feet. Stagnant pools, common to extensive bottoms along rivers
and near the mouth of large creeks, are unknown in this county, hence the easy
and rapid drainage of the soil, and the consequent fertility and the salubrity
of the atmosphere.
The supply of timber in Jackson County is hardly surpassed by that of any
county in the State, and its area is constantly on the increase caused by the
rapid diminution of prairie fires, and the very considerable culture of
prairie groves. The streams are so numerous that the distribution of timber
over the county is very well equalized; the traveler is hardly ever out of
sight of timber. Conspicuous among the native varieties are cottonwood, black
walnut, oak of the black, white, red, and burr varieties; hickory, elm,
hackberry, linden, sycamore, willow, and box-elder. The cultivated groves are
generally soft maple, cottonwood, elm, and black walnut.
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