The Arizona sentinel., 1905-01-18
The GREAT COLORADO RIVER

The great Colorado river is the largest
stream, both in drainage area and discharge.
that lies wholly within the arid portion OF
the United States. 1t is formed by the juno
tion of the Greer and Grand rivers, rising in
Colorado and Wyoming respectively, in re-
gionS of great precipitation, mainly IN the
form of snow. Only small percentage of the
water yielded by the basin of the Colorado
has as vet been utilized for irrigation, and
practically none for any other purposes. The
obstacles are many. Through most of its
course this river and its tributaries flow at
the bottom of profound canyons, from which
1t Is impossible to divert them upon irrigablc
lands. The river cmergeS from its canyon a
short distance above the Necdles-the cross
ing of the Santa Fc Pacific railroad-and has
q series of valleys which between this point
and the Mexican line aggregate about 5O0,(NO
acres. IN this region the waters arc heavily
laden with sediment, which is IL serious OBJ
stacle 10 their diversion The grade of the
river is so fat that Il diversion canal taken
out ut the rivers bed must have so slight q
a fall and so low a velocity that il would
quickly fill with sediment from the river.
For the same reason a canal must be very
long in order TO command any considerable
area of land in the river valley.
TWO AND QUARTER BILLION GALLONS A
MINUTE.
Measurements of the flow near Yuma show
that the river sometimes discharges Il mini
mum of about 5000 cubic feet Per second Its
maximum discharge is unknown, but pToba-
bly, exceeds onc-half million cubic feet per
second. AS the river is supplied mainly by
melting SHOWS, its season of high water cu-
inmates in June, and the low water season is
in the winter. when its sources are frozen.
The river is naviGated more or less from its
mouth to the Needles by flat-bottom, stern
wheel boats which sometimes even ascend to
the mouth of Virgin river. Its navigation,
however, is so difficult and precariouS as to
make IL almost useless. At low water the
channel is so broad, shallow and changeablc
that boats arc continually running aground.
sometimes being nearly a week in advancing
ten fifteen miles. In times OF high water
the swift current greatly impairS navigation.
Wh9eVer wagon transportation is possible,
this is preferred TO the river.
The chief obstacle to the utilization of the
waters of this basin are: First, the great
fiuctuation in discharge; second, the paucity
of land that can be reached by them: third,
the large quantity of sediment making i'm
practicable any diversion on small scale.
A comprehensive project Is here presented,
which, if upon investigation, is found i'm
practicable will largely remove all of these
difficulties, and will also greatly improve
navigation at all seasons Of the year.
The development of the mineral resources,
in which this country is rich, is greatly ham
rered by the great cost of power and the lack
of transportation, both important requisites
for the mining industry. The proposed plan
Will completely solve both problems.
sUBTRoPICAL CLIMATE.
All of the land that can be irrigated from
the lower Colorado may be regarded as hav-
ing n semi-tropical climate, where the grow
year rOund-the requirements for wafer, how
ever, being greater in the summer season than
in the winter. 1t is here assumed that the
maximum use in July will be twice as great
as the minimum requirements in January;
and that Il stream with the maximum flow of
two cubic feet per second i'll July, furnishing
about 1000 acre-fcct per annum, Will supply
200 acres Of land.
1t is probable that with proper regulation
the Colorado river will be able TO furnish Il
continuous stream of water for Industrial
IL
in winter TO 10000 cubic feet per second in
summer in years OF smallest discharge, al
lowing the great floods of wet years to sweep
to the sea as at present. This will be Sufli-
cicnt to irrigate 2.000,0G0 acres of Hand, and is
so far in excess of the requirements below the
Grand Canyon that no restriction need to be
put upon storage and diversion of waters
from the tributaries of the Colorado.
4 considerable portion of the valleys of the
lower Colorado consists of sandy flood plains
subject to occasional foundations, and rough,
gravelly foothills with soil unSuitabl for cul-
tivation. There are also considerable areas
Of sand dunes, and some tracts rendered bar
rem by alka!i. All these it is proposed to re-
claim by impounding upon them the silt
which annually passes down the Colorado
river.
SERIES OF DAMS.
The general plan here proposed is the pro-
vision of II series of reservoirs on the Colo
RADIO river by the construction of high dams
at numerous points where the topography is
favorable and where the possible storage is
large. All of these dams will be provided
with large SluicewayS through the base, in
order that the stored waters may be entirely
drawn off, together with their load of silt,
whenever il is found desirable to do so. The
reservoirs will serve as settling basins for Sed-
iment The dams will also be utilized 10
raise the waters into canals, for the double
purpose of enclosing more irrigable lands by
such canals and of giving them q velocity
sufficient to carry Il large amount OF Sedl ment
in suspension until it can be deposited upon
I'm al q civ
will depend largely upon the character ofthe
soil, and will be the highest permissible with
out involving destructive erosion. The fall OF
the Colorado river is so slight that reSer-
VoiTs Of enormous capacity may he construct
ed without involving dams OF impracticable
height. At any time, by opening the Sluice-
ways of the reservoir, the current of the river
will quickly cut a channel through the de-
posted sediment from the upper end of the
reservoir to the sluice gates; this being the
longest dimension and deepest part of the
reservoir will in all cases form an important
part of this storage capacity, and to this eX-
tent every reservoir can be permanently kept
clear of sediment without expense. With
this exception. each reservoir is expected to
gradually fill; when this occurs ii Is proposed
to draw down the surface of the reservoir
permanently 20 to 40 feet, and to convert all
of the reservoir site except the river channel
into irrigated farming land and, if necessary.
construct another reservoir for storage puT-
poses higher up on the stream. This policy
viii greatly increase the arabic area. 1t will
then ne practicable, whenever desired, tC
close the siuiceS and iHundate all of the agri.
cultural land in each filed reservoir and thus
fertilze it, as Is naturally done by the river
Nile for the valley. This is done artiticially
in some parts of Europe and Africa. With
the deep, alluvial soil, Semi-trOpical climate
arid atmosphere, abundant water supply
and the possibility of fertiiizing the fields
every year without expense. it is believed
that such regions can be farmCd the year
round, and several crops taken off annually
an acreage production being TINS attained
entirely without precedent in history.