The Wichita city eagle. [volume] (Wichita, Kan.) 1872-1883, 1874-01-22
SOUTHWESTERN KANSAS.
THE ARKANSAS VALLEY.
The Land Of Sunshine, Streams and
Natural Meadows.

: The Land Of Sunshine, Streams and
} Natural Meadows.
T Its Settlements, Towns and People.
A Fertile Soil and Genial Climate
The land of green meadows, clear
streams, fertile soil, hcalthful climate
+ and almost continual sunshine, South.
western Kansas. properly speaking
consists of about fifteen counties, whose
territory is watered and drained by the
Great Arkansas River and its tributa
, rics, the Little Arkansas. the two Wal.
nuts, Pawnee, Minnesota, Medicine Lod.
ge, Cimarron and their hundreds of: ri-
, butaries. It's a country 100 miles north
and south by $50 east and west. Being
but recently opened to settlements to
the pre-emptor and homesteader, the
settlement of a portion of il. especially
of Sedgwick. Harvey, Reno. barbour
Sumner. Cowley and Butler countic,
, has been wonderfully rapid. TO this
country thousands Of longing eyes arc
turned, not only from the older states,
, but from some portions of Europe.
These people who contemplate coming
" tHc Wcst, anu ~ tllls. the ClOlCcst
portion Of it. are anxious to know
more of the particulars, more of the
striking characteristics Of the great
river, its tributaries, and valleys, that
have for decades past been set down
by the geographcr and writer as unin-
habitable. To newspapers of this val
ley, and to ~ letters of friends alone,
can these people. who desire to come
among us, look for information. To
this end is this article compiled.
1t is fact well known to the gov
crnment, as 10 all observing western
men, that the neatly valuable lands be-
longing to the general government are
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 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 ard swiftest
running streams upon the continent.
Rising in Colorado territory, longitude
one hundred and six and onc-helf de-
grecs west of Greenwich, and latitude
tbirty-nine and one-half degrees north.
receiving its waters from rivulets and
springs that arc fed by the melting of
the eternal SHOWS of the snowy range
which rcars its rugged, lofty and snow
crowned peaks $50 miles west o: 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 estcrn Colora-
do and on eastward. 1t enters Kansas
seventy-!iye miles north of the south
line of the state, runs due cast 40 miles.
DIVORCES seventy-five miles northeast.
then angles to the Southeast, forming
what is known as the Great Bend,
thence 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 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 ovcrflows its banks, but its wa
tiers are curiously kept within the bed
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
,as i composed of sand and gravel, as
also the subsoil of the adjacent lands.
The superintendent water spreads it.
self through his subsoiI, instead of
overflowing the country, as would be
the case if the subsoil of the wide val
lcys was clay. So completely does the
porus subsoil drink up this water that
most of the year it 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 i'm the
gravel. The river at Wichita is about
| 300 feet wide. at Hutchinson, forty
miles further up, it is |, 600 feet wide.
THE 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, Scdgwick, Sumner. Cowley
and Butler. To describe perfectly the
lands, streams, towns and productions
of these counties would require more
facile and forciblc pen than we WELD.
The valley proper or bottom is from
ten to twenty miles in width. The
higher lands upon either side arc kind
of second bottom, or low rolling prai-
rics, with just enough undulation or
swell TO carry of the extra rain falls.
The soil of the valley proper, which is
also marked by gentle swells, is chief
ly a sandy loan, made up of such min |
cral elements as have been washed
from the Rocky mountains by the attri- |
ton of ages. 1t is marked feature of |
this soil that il contains 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 a |
murky soil. there appears to be in
places in this valley too much sand, but !
the experience of our farmers is direct |
ly the opposite. Read what the editor
of the american Agriculturist. who Vi |
sitcd this valley in April of this year,
has to saw
The soil is deep black loan, rest
ing Oh 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, aud 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 may
be driven across springs or creek bot
toms fearlessly, without danger Of mir
ing. This porosity of the soil, while
it 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 q rain i'm
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 10 part
of the country. possessing n more at
tractive soil for the farmer than this"
STOCK.
This is the natural home for cattle.
From early spring until the middle of