The Wichita city eagle. [volume] (Wichita, Kan.) 1872-1883, 1874-07-16
SOUTHWESTERN KANSAS.

/ SOUTHWESTERN KANSAS.
The land of green meadows, clear
streams. fertile soil, healthful climate,
and almost continual sunshine, South
western Kansas. properly speaking,
consists of about fifteen counties, whose
territory is watered and drained BY the
Arkansas River and its tributaries,
the Little Arkansas. the twOW alnuts,
Pawnee, Minnesota, Medicine Lodge,
Cimarron and their hundreds of tri-
butaries. 1t a country 100 miles north
and south by $50 east and west. Being
but recently opened to settlements to
the prc-emptor and hOmesteader. the
settlement of a portion of il. especially
of Sedgwick. Harvey, Reno, Barbour,
Sumner. Cowley and Butler counties
has been wonderfully rapid. To this
country thousands of longing eyes are
turned, not only from the older states,
but from some portions of Europe.
These people who contemplate coming
to the west. and to this, the choicest
portion of it. are ANXIOUS 10 know
more Of the particulars, more of the
striking characteristics of the great
river, its tributaries, and valleys, that
] nav i0l uttdutc pdsb DCth SCI wv" II
! BY the gcograplcr and writer rs unin-
habitable. To newspapers of this val
! lev. and to the letters of friends alone.
can these people. who desire to come
among us, look for information. To
! this end is this article compiled.
Ii is a fact well known to the gov
crnmcn;, as TO all observing western
men. that the really valuable lands be-
/ longing 10 the general government arc
now limited and that the remaining
lands are rapidly being transferred to
| private hands-the homesteader, pre-
emptor and settler of the west. Out
side of the Indian territory there re-
mains but a limited supply of really
good agricultural lands in all the west,
! the choicest of which, for climate, soil.
! and health, are to be found in the great
valley of the Arkansas, in the counties
named above.
THE ARKANSAS RIVER
is little less than 1000 miles in length,
being one of the longest and swiftest
running streams upon the continent.
Rising in Colorado territory, longitude
one hundred and six and Onc-half de-
grecs west Of Greenwich. and latitude
thirty-ninc and onc-half degrees north,
receiving its waters from rivulets and
springs that are fed by the melting of
the eternal SHOWS of the snowy range
which rears its rugged, lofty and snow
crowned peaks $50 miles west of and
5000 feet above the base of the Rocky
mountains, it flows completely around
the south peak, surges and sparkles at
the base Of Mount Lincoln and rushes
out through a canyon in Pixies Peak
range into the valley of estern Colora-
do and Oh eastward. 1t enters Kansas
seventy-five miles north of the south
line of the state, runs due cast 40 miles,
DIVORCES scventy-tivc miles northeast,
then angles to the Southeast, forming
what is known as the Great Bend,
thence a little south of east through
Kansas, the Indian territory and the
state of Arkansas, cmptying into the
Mississippi midway between Memphis
and Vicksburg. The Arkansas is
broad and shallow stream. with many
islands, low but well defined banks,
varying from four to ten feet in height.
The most remarkable features are that
although draining a country, before
reaching Kansas, larger than all New
England, and although it carries the
melting SHOWS in June, July and Au-
gust of many thousand square miles, it
never overfows its banks, but its wa
of the stream, working great benefit
to the soil of the valley for miles upon
each side. The fact is the bed of the
stream throughout its source in Kan
sas is composed of sand and gravel, as
also the subsoil of the adjacent lands
The superabundant water spreads it.
self through his subsoil, instead of
overlooking the country, as would be
the case if the subsoil of the wide val
levs was clay. SO completely does the
porus subsoll drink up this water that
most of the year 1t is easily fordable
with teams, and there has been times
when, in the western portion of the
state. the river bed would go dry, al
though water could be obtained three
or four inches below the surface, where
in reality the river was flowing in the
gravel. The river at Wichita is about
| 800 feet wide, at Hutchinson, forty
miles further up, it is 900 feet wide.
TIE VALLEY AND SOIL.
The richest and most desirable por-
ton of the valley lies between the
Great Bend and the point where the
river enters in the Indian territory. in
which area are the counties of Reno,
Harvey. Sedgwick, Sumner, COwley
and Batter. TO describe perfectly the
lands, streams. towns and productions
of these counties would require more
facile and forcibie pen than we WELD.
The valley proper or bottom is from
ten to twenty miles in width. The
higher lands upon either side are a kind
of second bottom. or low rolling prai-
rics. with lust enough undulation or
swell to carry off the extra rain falls
The soil Of the valley proper, which is
also marked by gentle swells, is chief
ly Il sandy loan, made up of such min
cral clements as have been washed
from the Rocky mountains by the attri-
ton of ages. 1t is a marked feature of
this soil that il contains q much larger
proportion of mineral matter than the
prairie soils of Illinois and Iowa, which
are chiefly vegetable mould. For this
reason our valley will improve by cul-
tivation. To those accustomed to
murky soil, there appears to be in
places in this valley too much sand, but
the experience of our farmers is direct
" the opposite. Read what the editor
of the 1merican IgricnitmiSt. who vi
sitcd this valley in April of this year,
has to say:
The soil is Il deep black loan. rest
ing on a lighter colored subsoil con-
sisting of loan. clay and gravel, both
soil and subsoil being SO porus that
surface water readily passes through
them. and in 10 case is there any diff
Guilty experienced in crossing with
horses and wagons or stock. any water
courses or beds of streams. Teams NAV
be driven across springs or creek bot
toms fearlessly, without danger of mir
ing. This porosity of the soil. while
il renders it capable of being plOwed or
worked Immediately after the heaviest
rains, at the same lime keeps is con-
stantly moist from evaporation below,
and protects il from drouth. Within
six hours of the cessation of a rain in
which Judge AT least three inches of
water fell. ! saw farmers breaking sod
and cultivating the young corn. The
crops of corn, oats. rye. spring and fall
wheat. potatoes and garden vegetables.
which saw growing, both on new and
old breakings, in various localities in
the valley. arc equal to any that have
ever seen elsewhere. during many
years experience. know of no part
of the country, possessing a more at
tractive soil for the farmer than this"
STOCK.
This is the natural home for cattle.
From early spring until the middle of
October or the first of November the
herds of farmers and stock raiser'S
wander lcisurely through the green
nutritious grasses that brush their
sides in open meadows that are bound
L., 1r,.nr,.i,,nr fnt AMI ,,rnInci,,1r tho;,.