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LIBRARY
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THE LIBRARY

THE UNIVERSITY
OF CALIFORNIA

IRRIGATION STATISTICS

TERRITORY OF UTAH,

WITH MATTERS RELATIVE THERETO.

COMPILED AND PKEPARKD FOR

IRRIGATION CONGRESS

TO BE IIKLD AT

LAKE CITY, UTAH, SEPTEMBER is.

BY CHARLES L STEVENSON,

SECRETARY OF UTAH STATISTICS COMMITTEE.

SALT LAKK i r,

IRRIGATION STATISTICS

WITH MATTERS RELATIVE THERETO.

COMPILED AND PREPARED FOR

THE IRRIGATION CONGRESS.

TO BE HELD AT

SALT LAKE CITY, UTAH, SEPTEMBER 15, 16, 17, 1891.

BY CHARLES L. STEVENSON

SECRETARY OF UTAH STATISTICS COMMITTEE.

SALT LAKE CITY, UTAH.
1891.

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To His Excellency Arthur L. Thomas, Governor of Utah ; Col.

J. W. Donnellan, Chairman of Utah Delegation, Irrigation

Congress:

The Committee on Statistics present herewith their report
concerning irrigation in Utah and matters relative thereto. In
the absence of a Territorial Engineer or other officer where full
information can be had, as in other States, your committee have
been obliged to adopt the following course:

First. By availing themselves of the very complete machinery
of the Mormon Church, as it is the most complete repository of
local data, and to which end the Church authorities have given
every possible ara, circulars of inquiry embracing the questions,
deemed most desirable, were forwarded to every President of
Stakes and Bishop of Wards throughout the Territory.

Second. Somewhat similar notes of inquiry, but much more
in detail, embracing thirty-two questions, ha/e likewise been sent
to every county assessor, county surveyor, and Committee
Delegate from Utah.

Third. Special letters to Utah Delegates from Scientific
Societies and to Departments at Washington.

Fourth. To private individuals and companies who are
owners or have been engaged in the construction of important
canal and storage works in the Territory, and

Fifth. The obtaining of all literature, maps, and public
documents pertaining to irrigation in Utah.

The number of letters thus sent was four hundred and
seventy-three.

By this method it was believed that so many checks would
be had upon the returns as to eliminate many of the sources of
error and wide differences of statement had in previous investiga-
tions. In this respect the result has been quite satisfactory, and
the amount of valuable data collected very large.

The Committee began their investigations the first week in
August, but owing to. circumstances beyond their control, and
several vexatious delays, the returns only began to come in by
September, so that it was not until September 6th that the work
of collating could be commenced.

Owing to the then short time at our disposal it was found
impracticable to carry out the original intentions and very
reluctantly we were forced to leave out some two-thirds of the
data collected. Much of this was quite valuable reading and of
great interest to Utah. It will be seen that the whole book has
been prepared and printed inside of eiglt days.* These facts are
mentioned so that our sins of omission and commission may be
condoned, and the few errors that have crept in be accounted for

Necessarily any book of statistics is a work mainly of com-
pilation, hence we desire to here extend the thanks of the Com-
mittee to all who have so willingly imparted information.
Especially are we indebted to Hon. John T. Caine, U. S. Con-
gressional Delegate; Professor Marcus E. Jones, U. S. Treasury
Expert; R. J. Hinton, Expert of U. S. Agricultural Department;
P. E. Newell, Expert U. S. Interior Department; General A. W.
Greely, Chief Signal Officer, War Department; Major J. W.
Powell and G. K. Gilbert, of Geological Survey; Joseph Lipman,
Territorial Statistician; O. J. Hollister, Statistican; the Territor-
ial and Church officers, and U. S. Senator Hon. Wm. M. Stewart.

As a fact that may be overlooked, we would remind the
Utah delegation that at the last session of our Legislature a
memorial was addressed to the U. S. Congress petitioning it to
enact into law, Senate Title 326, "A bill ceding, upon condition,
public lands to the State of California and other existing States,
and to the eventual States to be formed out of the existing
Territories, in aid of the irrigation of dry and arid lands/' 'In
this memorial the Legislature says:

"We believe that such a law will greatly aid the important
work of reclamatoin of vast tracts of land now useless, and
would add to the population, wealth, and grandeur of this
country's western domain." We have endeavored to obtain a
copy of this bill, but unsuccessfully up to date.

Regretting that the time will not permit rendering more
complete work, we remain.

Respectrully Yours,

JESSE W. FOX, JR., Chairman,
CHARLES L. STEVENSON, Secretary,

Statistics Committee, Utah Delegation to Irrigation Congress.

Salt Lake City, Utah, Sept. 14, 1891.

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OP THE

Territory of Utati,

WITH MATTERS REL \TIVE THERETO.

MAIN PHYSICAL FEATURES.

'TAH is situated between the parallels of 37 and 42 degrees
north latitude, and the meridians of 109 and 114 degrees
west of Greenwich. It is on the same parallels as
Colorado, Kansas, Missouri, Southern Illinois, Kentucky, Vir-
ginia, Spain, Italy, Greece, Turkey, and Corea. Utah belongs
to the great plateau of the Rocky Mountains, its valleys being
elevated from 2,700 to 7,000 feet above the sea, while its moun-
tain peaks reach a height of 12,000 to 13,500 feet above the sea.
One-half of the Territory is on the western side of the Wasatch
Mountains, and within what is called the great basin. This
basin occupies western Utah, nearly all of Nevada, and parts of
California, Oregon, and Idaho. It has no outlet, the drainage
being toward two great depressions where there are salt lakes,
one on the western side under the Sierra Nevada Mountains,
and the other, under the base of the Wasatch Mountains, called
Great Salt Lake. There are many other minor lakes that receive
the drainage of small areas which do not" now flow into either of
these depressions, but once they all flowed into one or other of
them. These lakes have no outlet, and the water that flows into
them evaporates by the heat of the sun. The average elevation

of the great basin is from 4,200 to 5,500 feet above the sea.
Most of the inhabited portion of Utah lies at the western base of
the Wasatch Mountains and on the eastern side of the Great
Basin. The eastern half of Utah and a small portion of the
southern part lies on the eastern side of the Wasatch Mountains
and belongs to the drainage of the Colorado River and its trib-
utaries. Its valleys range from 2,700 on the south to 7,000
feet on the north. In the former, figs, almonds, cotton, and
delicate fruits are raised, while in the latter only small grain and
potatoes are grown.

The Wasatch Mountains enter the Territory on the north at
about the middle, extend nearly due south until near the southern
boundary, where they turn to the westward and pass out into
Nevada, forming in Utah the letter "J." The Wasatch are not,
however, the rim of the Great Basin. They are cut through by
all the larger streams which flow to the westward, but they are
the chief sources of the water supply. About twenty miles east
of the Wasatch and parallel with them runs the rim of the Great
Basin, a low, broad, and well-rounded range called the Coal
Range, which has an average elevation of 7,000 to 8,000 feet
above the sea, and encloses between it and the Wasatch some
very fertile valleys, such as Ogden, Weber, Sanpete, Provo, and
Sevier. At the upper (southern) end of Sevier Valley the Coal
Range joins the Wasatch, or rather the Wasatch fades into the
Coal Range, and turns westward into Nevada. West of the
Wasatch and about 15 miles from them runs the Oquirrh range
parallel with them. About the same distance west from the
Oquirrh and parallel with it is the Aqui range, and so on, with
jnore or less regularity to the western boundary, extend parallel
ranges. These mountains reach a height of 8,000 to 11,000 feet
above the sea, rising out of what was once the bed of the Great
Salt Lake. These ranges run from the northern boundary of
the Territory nearly to the southern, as far as the rim of the
basin. They have the peculiarity of running along for 30
miles or thereabouts, and then sinking beneath the plain, only
to reappear as another range a few miles further on. .These

interrupted ranges do not, therefore, prevent easy communication
with any parts of western Utah, and they also enclose between
them many beautiful valleys, which would be garden spots if
there were sufficient water flowing from the mountains to irrigate
them. The Oquirrh, Aqui, and Lakeside mountains run through
Great Salt Lake, forming those ranges of islands which add

much to the picturesqueness of the lake.

•

DRAINAGE SYSTEMS.

As stated, the Wasatch rise over a mile above the valleys,
run from north to south through the Territory, a little west of
the middle, until they reach Iron County, where they turn to the
southwest and into Nevada. Their average height will not fall
far below 10,000 feet above the sea. Neatly east of Salt Lake
City, the Uintahs, still loftier than the Wasatch, abut on them
and run eastward until they pass out of the Territory. These
are so close to the northern edges of Utah that we get little
benefit from them, while to the south of them is an Indian reser-
vation embracing the greater part of the arable lands. Nearly
due east of Utah Lake and about forty miles from the Wasatch,
the coal range starts from the Uintahs and runs southward par-
allel with the Wasatch for 160 miles when it joins them at
Panguitch Lake. These three ranges form the watershed of
Utah, the coal range and Uintahs forming the rim of the Great
Basin, while the Wasatch perform a similar part below Pan-
guitch. The Wasatch and Uintahs are narrow, lofty and rugged,
while the coal range is younger, lower and broad. The Wasatch
reach their culmination near Salt Lake City, and, aided by Great
Salt Lake, give the greatest water supply in the Territory. The
streams from this source irrigate the bulk of the cultivated area
of Utah.

The eastern part of the Territory is drained by the Rio
Colorado and its tributaries; the western part, by streams that
head in the Wasatch and the high plateaus of the central part, and
find their way into the salinas and desert sands of the Great
Basin. Thus we have the Rio Colorado drainage area, and

the Desert drainage area; the former about two-fifths, the
latter about three-fifths of the total area.

GREAT SALT LAKE DRAINAGE SYSTEM. — Three rivers enter
Great Salt Lake, namely, the Bear, the Weber and the Jordan,
and upon their water will ultimately depend the major part of
the agriculture of Utah. They rise close together in the west-
ern end of. the Uintah Mountains, and cut through the Wasatch.
Bear River flows northward, now in Utah, now in Wyoming, and
into Idaho as far as Soda Springs. Here it bends round
like a fish hook and returns on a more westerly line. Re-
entering Utah in Cache Valley, it passes thence by a short canyon
to its delta plain on the northeastern border of Great Salt Lake.
Its principal tributaries are received in Idaho and Cache Valley.
Utah occupies the central position in the arid region, and there-
fore the details of irrigation in this Territory possess more than
ordinary interest, from the fact that they represent conditions in-
termediate between those of the north and south, the east and
the west. Besides this the irrigation methods and systems have
been developed by men of English-speaking origin, who, unaided by
capital or previous experience, have introduced methods of their
own, and, taught by repeated failures, finally achieved success.

IRRIGABLE LANDS.

In Utah Territory agriculture is dependent upon irrigation.
To this statement there are some small exceptions. In the more
elevated regions there are tracts of meadow land from which
small crops of hay can be taken; such lands being at higher al-
titudes need less moisture, and at the same time receive a greater
amount of rainfall because of the altitude. But these meadows
have been, often are, and in future will be, still more improved by
irrigation. Again, on the belt of country lying between Great
Salt Lake and the Wasatch Mountains, the local rainfall is much
greater than the general rainfall of the region. The water
evaporated from the lake is carried by the westerly winds to the
adjacent mountains on the east and again condensed, and the
rainfall thus produced extends somewhat beyond the area oc-

cupied by the mountains, so that the foothills and contiguous
bench lands receive a modicum of this special supply. In some
seasons this additional supply is enough to water the lands for
remunerative agriculture, but the crops grown will usually be
very small, and they will be subject to seasons of extreme
drought, when all agriculture will result in failure. Most of
these lands can be irrigated, and doubtless will be, from a con-
sideration of the facts already stated, namely, that crops, will
thereby be greatly increased and immunity from drought
secured.

In order to determine the amount of irrigable land in
Utah, it was necessary to determine the areas to which the larger
streams can be taken by proper engineering skill, and the amount
wnich the smaller streams can serve. In the latter it was neces-
sary to determine first the amount of land which a given
amount or unit of water would supply, and then the volume of
water running in the streams; the product of these factors giv-
ing the extent of the irrigable lands. A continuous flow of one
cubic foot of water per second was taken as the unit, and after
careful- consideration it was assumed that this unit of water will
serve from 80 to 100 acres of land. Usually the computations
have been made on the basis of 100 acres. The unit was deter-
mined in the most practical way — from the experience of the
farmers of Utah, who have been practicing agriculture for the
past thirty years. Many of the farmers will not admit that so
great a tract can be cultivated by this unit. In the early history
of irrigation in this country the lands were over- supplied with
water, but experience has shown that irrigation is most success-
ful when the least amount of water is used necessary to a vigor-
ous growth of the crops; that is, a greater yield is obtained by
avoiding both scanty and excessive watering; but the tendency to
over-water the lands is corrected only by extended experience.
A. great many of the waterways are so rudely constructed that
much waste ensues. As irrigating methods are improved this
wastage 'will be avoided; so in assuming that a cubic foot of
water will irrigate an average of 100 acres of land, it is at the

same time assumed that only the necessary amount of water will
be used, and that the waterways will eventually be so constructed
that the waste now almost universal will be prevented.

The recent returns to the committee show an average waste
of 70 per cent.

In determining the volume of water flowing in the streams,
great accuracy has not been attained. For this purpose it would
be necessary to make continuous daily, or even hourly, observa-
tions for a series of years on each stream.

Having determined from the operations of irrigation in
Utah that one cubic foot per second of water will irrigate from
80 to 100 acres of land, and having determined the volume of
water or number of cubic feet per second flowing in the several
streams of Utah by the most thorough methods available under
the circumstances, it appears that within the Territory the
amount of land which it is possible to redeem by this method in-
cluding that already under irrigation, is about 3600 square miles,
or 2,304,000 acres. . Of course this amount does not lie in a con-
tinuous body, but is scattered in small tracts along the water
courses. Utah has an area of 84,970 square miles, or 52,001,600
acres. That is, 4.23 per cent, of the lands under consideration
can be cultivated by utilizing all the available streams during
the irrigating season. Previous estimates of the total arable-
irrigable lands of the Territory have been as follows:

Church authorities, 2,525,403 acres.

Powell (not entire) .... 1,447,920 "

Hollister, 3,000,000 "

Jones, 2,000,000 "

In addition to the streams considered in this statement
there are numerous small streams on the mountain sides, scattered
throughout the Territory — springs which do not feed permanent
streams; and if their waters are used for irrigation, the extent
of irrigable land will be slightly increased; to what exact amount
cannot be stated, but the difference will be so small a$ not to
materially affect the general statement, and doubtless these

springs can be used in another way and to a better purpose, as
will hereafter appear.

This statement of the facts relating to the irrigable lands of
Utah will serve to give a clear conception of the extent and con-
dition of the irrigable lands throughout the arid region. Such
as can be redeemed are scattered along the water courses, and
are in general the lowest lands of the several districts to which
they belong.

Whatever conditions future developments may bring about,
the present water supply in Utah Territory is surface. It depends
entirely upon the fall of snow in the winter, and to a slight
degree upon the rainfall during the spring and fall months As
a consequence the character of the water supply is found in the
mountain streams. The fall of snow in the mountains is incom-
parably greater than in the valleys, and it lasts much longer, for
the reason thai the cold is much severer.

The snow packs in the ravines until almost as hard and solid
as stones. The solidifying is materially assisted by what are
termed "January thaws," the result of a marked relaxation in the
severity of the weather, which generally occurs during the month
of January. This temporary relaxation is invariably followed by
a renewal of the rigor of winter, when the snow which has
settled and become packed by the thaw, freezes until it is almost a
solid mass of ice. The snow is the source of all streams in Utah
save the little running water that comes through rains.

The volume of these streams depends entirely upon the
season of the year. During the winter months the supply is very
small, for the reason that the quantity of melting snow is at its
minimum and the cold has a tendency to stay the flow .With the
disappearance of winter and the increased warmth of the sun the
snow begins to melt, the volume of water increases and con-
tinues to grow until puny and tiny streams are swollen into rush-
ing torrents, sometimes causing great damage from the over-
flowing of their banks. The water supply attains its maximum
height between the 10th and 20th of the month of June. This
statement may be given the force that attaches to a rule almost,

if not entirely, without exception. The solidifying and freezing of
the snow in winter, as above stated, makes certain the tenure of
the water supply that would otherwise be both uncertain and
disastrous ; it prevents the too rapid melting, that would other-
wise result in absolutely uncontrollable torrents for a period,
and thus makes the streams available for agricultural purposes.

The experience of Utah farmers as to the best methods for
increasing and controlling the water supply would be valuable
only to people surrounded by similar country with like elementary
conditions existing. The introduction of genuine artesian wells
and utilization of the sub-flow may considerably increase the
irrigable acreage. Experiments, sufficiently thorough to demon-
strate the success that would attend the digging or boring of
such wells in Utah, have not been made. The best opinions,
however, are that the geological conditions existing in Utah are
peculiarly favorable to their introduction and successful develop-
ment.

The Territory, or rather its habitable portion, is com-
posed of valleys, mountains and canyons, with some lakes. The
melting snow on mountain and in valley which fails to find its
way into some of the streams must sink and collect somewhere,
and there is a well-founded belief, which can easily be verified,
that beneath these valleys are subterranean lakes that would feed
with a never-failing supply of water innumerable artesian wells.
To increase the supply by other means would be to increase the
fall of snow, a thing humanity is not yet prepared to base a cal-
culation upon. Preserving methods are, however, more prac-
ticable, and nature has done her best to make that task as light as
possible. The outlet for all the streams is into the valleys. The
streams come from the canyons high above the valleys, and the
supply can be preserved or saved by the construction of reser-
voirs or by dams. In case the latter method was adopted, it
would simply be necessary to select the most suitable place in
season and place a dam across the ravine.

The work would be more or less expensive as the stream was
large or small and the canyon wide or narrow, but in every can-

yon suitable points abound, and as the future development of
Utah largely depends on her permanent and increased water sup-
ply, her people will be forced to resort to damming the
streams within their natural confines in the ravines. To what
extent this idea carried out, would save the water that yearly runs to
waste, the word "waste" b£ing used here with the knowledge that
every drop of water is in valuable in a country, where agriculture de-
pends upon irrigation, it is absolutely impossible to form even an
estimate, and for several reasons : First, the volume of the stream
differs every day in the year, and one year from another.
Second, it would require a measurement of the streams and a
knowledge of the amount consumed in irrigation and in local
evaporation, which would increase with increased distributing
canals and ditches.

It may be safe to state, however, that if complete and
thorough methods of saving were introduced, all the laad in the
Territory, if it could be reached, could be well and thoroughly
irrigated; this, too, without resorting to artesian wells, so vast
is the amount of water that runs to waste during the winter,
spring and early summer months.

As now ascertained the average first cost oE water right in
Utah, $10.55 per acre, is noticeably great, being largely due to
the manner in which the ditches and canals are made. Nearly
all are laid out and constructed by farmers of ordinary education,
without the use of surveying instruments. As a consequence,
few of the more important works laid out in this manner have
proved serviceable without great changes, involving in many
instances the reconstruction of almost the entire system. The
perseverance shown in many of these cases is remarkable.

On the other hand, the annual cost of 91 cents per acre is re-
markably low, from the fact that farmers have done all the work of
cleaning and making the small annual repairs necessary after the
canals and ditches were in successful operation. It should be noted,
however, that the maintenance is, as a general thing, comparatively
poor, and that the main canals and ditches receive only enough
labor to keep the water flowing. It undoubtedly would be far

Ifi

more economical to spend a larger sum annually, and thus save
much water which is lost through evaporation and seepage, due
to the poor condition of the channel. The changes now being
made in the construction of permanent works, scientifically
built, Awhile they may not materially reduce the cost, will insure a
stability of construction and maintenance which heretofore has
been as variable as the rainfall.

The use of flowing wells for the irrigation of gardens,
orchards and vineyards is such a matter of interest and import-
ance, that at the time of making the agricultural census the
enumerators obtained the number of artesian wells owned by each
farmer. The total number of these is 2,524. Of this number,
facts concerning the depth, cost, flow and other matters of
interest have been obtained from the owners regarding 897
wells. The average depth of these is 145.54 feet, and the aver-
age cost is $77.00 per well, the average cost per foot in depth
being 53 cents. The diameter of these wells ranged from one
and a quarter to four inches, or, in a few cases, to six inches or
more, the average being from one and three-quarters to two and
one-half inches. The average amount of water discharged by
these wells was 26.37 gallons per minute, equivalent to 0.059
cubic feet per second, or second feet, as is the common term.

Most of these wells were used for domestic supply and
watering stock, 48.49 per cent, being employed in irrigation,
watering on an average 4.74 acres per well,thus making the average
cost of irrigation from the successful flowing wells $16.37 per
acre. It has already been shown that the average cost of water
right from canals or ditches was $10.55 per acre.

From the preceding figures the1 average duty of water from
these flowing wells has been ascertained to be one second foot to
80.3 acres, an amount which could doubtless be increased if the
farmers considered it feasible to store part of- the water which
flows daily during the non-irrigating season.

These flowing wells are confined mostly to the lower parts of
the valleys along the foot of the Wasatch mountains and to the
lacustrine deposits from the great body of fresh water which

1 7

formerly filled these valleys, and which has been named Lake
Bonneville. The wells are made by drilling and by driving pipe
through the sands and clays until some pervious water-bearing
layer is reached. Along the eastern shores of Great Salt Lake
and Utah Lake these wells are particularly numerous, but they
gradually decrease in number and discharge as the higher ground
is reached. The depth as a rule ranges from 30 feet on the
lowest ground up to 400 feet or more nearer the edge of the valley.
The Utah Bureau of Statistics has only recently been organized,
and it is impossible to give any idea of the extent, character and
cost of the artificial means introduced jn the Territory for the
utilization and distribution of the water supply. As to the
flumes for mining and railroad purposes it is impossible to give
even an estimate. Very little is necessary for railroad purposes,
and where water is not otherwise naturally available, wells are
utilized and form the. almost exclusive supply. It is sufficient
with regard to mining, as flumes are used in this case to carry
off water from the lower workings of the mines. There is no
hydraulic mining carried on in any part of Utah, for which
reason supply flumes, save for reduction works, concentrators^
leaching purposes and milling, are unnecessary. It is not in-
frequently the case that the water out of the mines is more than
enough to run the mills.

As heretofore stated, the increase and decrease in the water
supply depends entirely upon the fall of snow in the winter and,
in an unimportant degree, upon the fall of rain in the fall, spring
and early summer months. A very noteworthy fact, attested on
the best authority, is that for a period of years there has been a
steady increase in the water supply. It has been thought by
many that the claim of increased water has been more imaginary
than real. The claim, however, has been verified by
measurements made in Great Salt Lake, which is the reservoir
for many of the largest mountain streams, including the Jordan,
which is the outlet of Utah Lake, the Bear River, the Ogden,
Weber, Logan, and Blacksmith Fork, and innumerable smaller
streams.

The lake has a shore line of 350 miles, and since 1856 the
water has increased 14 feet in depth; though not at present quite
that much ; and Great Salt Lake, depending as it does entirely
upon the inflowing of mountain streams and that amount of
water which is not consumed by agricultural utilization, shows
beyond question that there has been a marked increase in the
water supply.

This rise in the body of the water of the lake has taken
place, it must be remembered, during a period when there was
a rapid increase in the demand for water for agricultural
purposes.

Where irrigation ha's been applied for a few years there has
been a perceptible decrease in the amount of water necessary to
irrigate the land properly. The decrease is placed at about 25
per cent.

The value of irrigated land depends entirely on its location,
not only in the Territory, but in a precinct or county, and upon
the character of the soil, which often differs materially from land
adjoining it and enjoying the same water advantages. In earlier
days all persons interested in digging a canal would turn out and
keep on working under the direction of a person chosen by them-
selves. Later, laws were passed on the subject, and will be found
by reference to the statutes of the Territory, which will give the
fullest attainable information as to water rights and conditions
in the Territory.

Grants, of course, were given to municipal and canal cor-
porations, counties, and districts, but these also are set forth in
the statutes.

One of the most important of the class under consideration
in the Territory was the construction of a canal to supply Salt
Lake City with water. The city was bonded for the purpose, and
the canal was commenced in December of 1879, and finished in
the fall of 1881.

Its length is something over 27 miles, and its source is the
Jordan River, a short distance below the point where Utah Lake
has its outlet into the Jordan. The canal is 20 feet wide at the

bottom, the depth being 5 feet, sufficient to carry 3| feet of
water.

Four other canals have been constructed in the valley of the
Jordan, all about of the same capacity, and built about the same
time. These canals, owing to inferior construction in vogue at
that period, do not furnish more than 60 per cent, of the water
entering their heads. The total length being 132 miles, covering
about 44,000 acres.

As a contrast, the great Bear River Canal, which enters the
north end of Salt Lake Valley, is a good illustration of the more
modern system of scientific construction, and also shows what
may be done by successfully damming a large river.

BEAR RIVER CANAL COMPANY.

The big irrigating enterprise of the Bear River Canal Com-
pany has been mentioned before, and also the appropriation of
Bear Lake as a reservoir by the company. The latter step for-
ever assures the supply. The headworks for the canals are in
Bear River Canyon. A canal of 1,000 second cubic feet capacity
is taken out on each side of the river. That on the left bank is
carried down along the base of the mountains, about forty miles
to Utah Hot Springs. In this vicinity a branch is led off toward
the lake, where, around Plain City, there is a large body of warm,
sandy, rich land. The main canal goes on to Ogden. There,
exchanged with the users of Weber River water, the latter is said
to be taken out high up in Weber Canyon and carried out upon
the sand ridge south of Ogden.

The canal on the right bank, where it reaches the valley
plain, strikes up the valley diagonally three miles to near the
Toponce Ranch, where it is carried over the Malad, here 100 feet
below its banks, on an iron viaduct costing $30,000. Thence it
is led around the northeastern edge of the valley past Point
Lookout and the Walker Ranch, toward Blue Creek, about forty
miles. Soon after reaching the plateau it throws off one branch
which goes down near Bear River, past Corinne, to the lake,
about 30 miles. It throws off a second branch west of the Malad,

which runs southward to near Little Mountain, and then west-
ward to the main canal.

The area of lands which will be tributary to these canals is
some 20'),000 acres. The soil is extremely fertile, and the lands
most favorably located.

The Canal Company offer these lands for sale at $25 to $35
an acre, which includes $10 for perpetual right to one cubic foot
of water per second for each 80 acres. The yearly rental or
maintainance tax it is proposed to put at $1.50 or $2.00 an acre
of land watered. The irrigating works were planned by eminent
engineers; the canal owners have water power and city (Ogden)
water works to look after, which will compel them to maintain
the works in good repair. The water may be depended upon
absolutely.

This work of the Bear River Canal Company, though less
than one-third completed, is by far the most important irrigation
work yet undertaken in this Territory.

DUCHESNE AND STBAWBERRY RIVER CANAL CO.

There is now a very elaborate and extensive project, well
under way, to take out a portion of the waters of the Straw-
berry and Duchesne Rivers and irrigate 200,000 acres of the
most fertile lands. Much of this now lies within the Indian
Reserve, but which it is believed will be set off. As this enter-
prise will form the subject of a separate paper by one of the
delegates (Mr. A. D. Ferron, C. E.) reference is made thereto.

NORTH POINT CONSOLIDATED CANAL.

This is also a canal of quite recent construction (1891). It
adds 14| miles to the system now west of the Jordan River. Of
the whole length, nearly one quarter, has a bottom width of 50
feet, the remainder varying from 20 to 15 feet. The fall is very
slight, 0.7 feet to the mile. The estimated capacity is 93 cubic
feet to the second. The soils are such that two-thirds of a
second foot, it is stated, will irrigate 100 acres, or a total of about
14,000 acres.

SWAN LAKE RESERVOIR AND CANAL COMPANY.

This is another comparatively recent enterprise and has for
its object the utilization of the waters of the Sevier River. It
consists of a reservoir covering an area of 70 square miles fed
by the river and located in the central portion of Millard County,
five miles west of the Union Pacific railroad, fifteen miles north-
east of Sevier Lake or Sink, and 170 miles south of Salt Lake
City.

This large reservoir of over 40,000 acres, as may be supposed,
is very largely natural, and consists of a number of lake basins
which are appropriated by the work of construction, such changes
being made as were necessary to adapt them to the requirements
of the reservoir.

The continued action of the river current has built up walls
or natural levees which rise to a height above the surrounding
country like the levees of the Mississippi and other streams. The
company in constructing their reservoir have repaired the natural
walls, built strong dykes across channels, cut ditches and canals,
built dams and flumes. The entire plant is of such a character
it can be enlarged and improved indefinitely.

There are at present over 200,000 acres of level fertile and
irrigable land lying under the reservoir supply. There has
already been completed about 15 miles of canal. A townsite and
buildings for employers and laborers has been laid out, some
20,000 shade trees planted a rod apart and along also several
of the streets.

The reservoir, or more appropriately lake, when full will
hold about three and one half billion cubic feet, or 200,000 acre
feet. In May, 1891, when the river had its rise, the flow over
the waste dam was 30,000 miners' inches. The hrigable land has
an underlie of clay a few feet below surface, which will materially
lessen the amount of water required for irigation. The company
expect to irrigate 75,000 acres.

OQUIRRH WATER AND LAND COMPANY.

This company has for its object the lowering of the Jordan
River at the outlet and below Utah lake. The present river

bed is much higher than the bottom of the lake and acts as a
bar to the lowering thereof and to the obtaining of a large supply
of water that now cannot be utilized and which when so utilized
will be restored in the winter. Such a lowering will also admit
of a better regulation of the rise and fall of the lake. This low-
ering of the outlet will permit the irrigation of possibly some
25,000 acres, and by storing in the Provo River this can be still
further augmented.

In cities the municipal corporations control the waters,
water-masters being appointed to regulate the division of the
water.

For regulation of water rights see Utah statutes of 1880,
page 36 ; for acts relating to Salt Lake City Canal, see same
pages 55 and 85; for law relating to irrigating companies, see
Utah statutes of 1884, page 127, laws of 1890, pp. 12, 21, and
142.

PRINCIPAL IRRIGATION STREAMS.

As concerns the Great Salt Lake drainage system it has been
shown that the three principal rivers are the Bear, the Weber
and the Jordan.

The mean annual flow of Bear River, where it enters Salt
Lake Valley, is about 5,000 cubic feet per second. Its delta-
plain^ contains about 214 square miles of unsurpassable soil,
upon which the Bear River Canal Company has diverted 2,000
second-cubic feet of water through upward of 100 miles of canals
at a cost of nearly $2,000,000. The soil is rich and ideally
adapted to irrigation, having a gentle fall, being smooth as a
floor, and well and deeply drained by the Bear and Malad rivers.

As if to forever bar a water famine in North Salt Lake Valley,
nature has provided a natural reservoir in Bear Lake, situated
near Bear River and connected with the river by a narrow out-
let, high up in the mountains. The lake has an area of 150
square miles, and can be raised ten feet by a dam thrown across
the outlet at small expense. Thus enough water can be stored
during two-thirds of the year to flow, in connection with
the current, 5,000 feet per second during the other third

of the year. Bear River itself can be turned into the lake
by a short canal from above, and upon its upper tributaries, on
the northern slope of the Uintah Range, there are many
glacial lakes which can be made use of for impounding water.
The Weber River runs in a general northwesterly course
from the Uintah Mountains to Great Salt Lake, entering the
latter at the middle of its eastern shore. The Ogden is its only
important tributary. Its delta-plain comprises about 2-'0 square
miles of farming land.

The Jordan River is the outlet of Utah Lake, and runs
northward, entering Great Salt Lake at its southeastern angle. On
the right it receives anumber of large tributaries from the Wasatch.
The largest tributary of Utah Lake is Provo or Tunpanogas River,
which rises near the souice of the Weber and Bear, in the Uintah
Mountains. Minor tributaries of Utah Lake are American Fork,
Spanish Fork, Hobble Creek, Payson Creek, Salt Creek, etc. On
all the tributaries of Utah Lake there are about 320 square
miles of irrigable land ; and in the Jordan Valley, below Utah
Lake, inclusive of Bountiful and Centerville, there are about 250
square miles. In addition the water can be carried around the
point of the Oquirrh Range on the southern shore of Great
Salt Lake, and be used to water 50 square miles of Tooele
Valley.

Utah Lake is a natural reservoir, 145 square miles in surface
area. With suitable headworks its volume can be controlled, and
the entire charge be concentrated in the season of irrigation.
The mean volume of the outlet is about 1,000 second-cubic feet,
but one-fourth of this must be assigned to watering lands on the
tributaries of the lake and to evaporation, leaving a perennial
flow of 750 second-cubic feet, which if concentrated into four
months would irrigate for that period, 350 square miles.

There is thus water enough forever assured to irrigate every
acre of the eastern border of Great Salt Lake Basin, from Nephi
on the south to Bear River canyon on the north, a distance, as
traveled, of about 180 miles. This fringe of the desert, between the
Wasatch and Great Salt Lake, and between the Wasatch and Utah

Lake, is, in location, resources, climate, fertility, potentially, the
glory of the earth. It is easily the garden spot of Utah. Every
acre of land is intrinsically worth $100, although it ranges in
prices all the way from $5 to $225 per acre. The average, away
from the suburbs of larger towns, is perhaps, $50 per acre. Al-
together, about 7,590 secand-cubic feet of water perennially
flows into Great Salt Lake.

SEVIER LAKE DRAINAGE BASIN. — According to the accom-
plished geologists of the United States Geological Survey, which
this sketch follows, the Wasatch ends with Mount Nebo, which
overhangs Nephi. The elevated lands southward these gentlemen
term the high plateaus, divided by great longitudinal faults into
three ranges, each made up of different members, as the Sanpete,
the Pahvant, the Tushar, and the Markagunt, facing the Great
Basin; and the Wasatch, the Fish Lake, the Awapa, and the
Aquarius, east of Grass Valley. The Pahvant and the Tushar,
says Captain Button, present a curious admixture of plateau
and sierra, but the others are true tables, made and kept so by
the lavas which cap them and successfully resist erosion.

The Wasatch plateau is east of Sanpete Valley, above which
it rises a whole mile. The San Pitch River is the largest tribu-
tary of the Sevier. In 1890 the farmers of Gunnision dammed
the San Pitch River a few miles southwesterly of the town of
Manti; by this they have funished a reservoir with capacity of
26'),()00,000 cubic feet, or 6,000 acre feet. Powell gives the
capacity of this stream at 60 second-feet. This reservoir is in-
tended only as a storage basin, but is good evidence in showing
the tendency of the people to increase their cultivable acreage
in the most practical way. The whole cost had not eoualled $4,000.

Probably upward of a hundred square miles are served by
the small streams of southwestern Utah, as at Levan, Scipio,
Holden, Fillmore, Oak City, Kanosh, Beaver, Paragoonah, Cedar
City, Pinto, Hebron, etc. In this region the water is insufficient
to supply the arable land, but it can be largely increased by stor-
age, without doubt.

COLORADO RIVER DRAINAGE. — Of the Rio Colorado drainage

system, the main channel is the river Colorado and its proper
continuation, the Green River. The principal tributaries of
these streams from the east are the White, the Grand and the
San Juan, the White entering the Green, the Grand uniting with
the Green to form the Colorado, and the San Juan entering
the latter about 125 miles from the confluence of the Grand and
the Gr^en. The tributaries from the west are the Virgin, the
Kanab, the Paria, the Escalante, the Fremont, the San Rafael,
the Price, the Minnie Maud, the Uintah. or Du Chesne and the
Ashley Fork.

The climate is extremely arid, the elevation between 2,500
and 11,500 feet, giving great range in the temperature. The
limit of successful (hay) farming is about 7,000 feet. Aside
from the Uintah- White basin, which contains more than half of
the irrigable land of the entire district, and which is an Indian
Reserve, the lands are generally of terraces or benches, or in re-
stricted valleys between the higher courses of the streams and
their canyons, and are from 4,500 to 6,000 feet in altitude. The
Price, the Uintah or Du Chesne, the Green and the Grand have
plenty of water, but, excepting the Uintah, the land upon which
their waters can be diverted is very limited. On the Virgin,
which is far south and low in altitude, there are thirty to fifty
square miles. In the entire district there may be a thousand
square miles of irrigable arable land.

METHODS OF IRRIGATION.

As will be seen there are only a few square miles in Utah
that do not require irrigation. The system of cultivating the soil
in Utah is to start canals at the mouth of the canyons, where
dams are built. These canals are run from the canyons out
upon the more level laud of the valleys and there subdivided into
branch canals, and these again divided into laterals leading to every
farm so long 'as there is water to be distributed. Each farmer
has canals leading from the main one to every field, and gener-
ally along the whole length of the upper side of each field. Each
field has little furrows, a foot or more apart, and parallel with each

other, running either lengthwise or crosswise or diagonally across
as the slope of the land requires. Into these furrows the water is
turned, one or more at a time, as the quantity of water permits,
until it has flowed nearly to the other end, when it is turned into
the next furrows, and so on until all are watered.

This is the usual custom, but where the soil is made of clay
this method is not so good and another is used. This method
is to throw up little embankments six inches high around separ-
ate plats of land that are of uniform level, and turn the water in
until the plat is full to the top, when the water is drawn off to
the next lower plat and so on to the end. This enables the water
to soak in more and so does thfc crop more good, but where the
soil is porous, as is generally the case, it is not so good a method,
as it wastes water. Each farm generally has the right to use the
water so many hours once a week or once in 10, 12 or 14 days,
as the particular valley and the time of the year require. The
crops are supposed to get a good soaking at every watering. The
amount of land that each person can cultivate depends upon the
quantity of water right that he owns. The method of dividing
the water depends upon the intelligence of the far ners; in some
places it is very crude, in others it is thorough. In few places is
any one entitled to a certain number of cubic feet per second.
Generally each man has a right to such a portion of the water
in a certain stream or river; if the season is a" dry one he gets
less water, and if it is a wet one he gets plenty. He must govern
the quantity of crops put in by what he thinks will be the water
supply for the season.

The method of dividing the water is to put in a dam at the
head of the canal on the stream, with a partition in it separating
the proper share for the canal, the rest being allowed to flow
down the channel of the stream. The same method is used in
the canal where people have certain shares in the stream at every
new canal. Where the rights of people are based on a certain
number of cubic feet per second, or miners' inches, there is a
gate put in at every dam and lowered into the water till the water
reaches a mark six inches above the bottom of the gate. This

gate is raised or lowered as the quantity of water requires to
keep the water on that point on the gate. The length and width
of the space below the gate are multiplied together, and the pro-
duct is called so many miners' inches ; generally 48 of these are
considered to be equal to one cubic foot per second. This method
is correct where there is no back water below the darn to inter-
fere with the fall of the water. The partition is then put in at
the proper place to give the owners their due share of water.
This division is kept up until there is no water to distribute.
Those people who have a secondary right get what is left after
the primary rights are filled. The irrigation season generally
begins in May or the first of June, and ends in August, and is
about 120 days long. The amount of land that one cubic foot
of water can irrigate, ranges from 35 acres in the very hot and
sandy country in the south, to 150 acres in the higher valleys.
The average is about one cubic foot to 100 acres. The future
growth in agriculture depends upon the storage of water in
reservoirs, and above all in the economical use of the water we
have. Subsoil irrigation is another great hope of Utah. By
this many times the present cultivated area can be reclaimed, and
as before stated, by a proper use of the underground sources.

SOIL AND CLIMATE.

As before stated, Salt Lake is in latitude 40 degrees 46
minutes north, and longitude 111 degrees 54 minutes west, and
is near the isotherm of 52 degrees. In latitude we are in line
with northern Missouri, Peoria, Illinois; Columbus, Pittsburg,
Reading, and Staten Island; and can raise all kinds of fruits
except oranges, etc., and even these we can raise in Southern Utah.
Every kind of tree growing north of Virginia will thrive herein the
open air. There are now growing in Salt Lake City the follow-
ing: sycamore,basswood, locust, honey locust, ailantus, cottonwood,
balm of gilead, lombardy, soft and hard maple, box elder, walnut,
chestnut, white ash, white and roch elm, mulberry, butternut,
larch, pines, spruces, firs, oaks, peach, plum, apricot, apple, etc.

Since our winter is only about six weeks long, the spring is

quite early; the farmers frequently plow in February, and sow
their small grain. Our latest frost averages April 8th, so that
the most delicate plants are safe after that. Our earliest frost
comes about September 26, so that all our crops have ample time
to mature.

During the season of 1890, crops were raised by irrigation
on 396,000 acres, say about three-fourths of one per cent.
About 85 per cent, of the cultivated areas required irrigation, the
remaining 15 per cent, being "dry farmed."

The average size of the portions of farms under cultivation
was 40 acres. The average first cost of the water right is
$10.55 per acre, and the average first cost of preparing the soil
for cultivation, including the purchase price of land is $16.10
per acre. The average present value of the irrigated land of the
Territory, including improvements etc., is reported at $84.25 per
acre, showing an apparent profit, less cost of improvements of
$57.60 per acre.

The average of the estimated value placed by the farmer up-
on this water right is $^J6.84 this is the price which the water
rights,wherever transferable without the land, have usually brought
or would probably bring in the various localities, the value of
these rights being dependant largely upon the probabilities of
the owner receiving the amount of water claimed.

A TYPICAL CASE.

The following statement, based on actual experience, and
made by one of the most intelligent farmers in Utah, shows the
prime cost of settlement; what he has done and what may be
done with a typical farm of forty acres, well irrigated land and
properly handled:

EXPENDITURE.

First cost 40 acres of land and water right, $40 per acre, $1,600.00
One mile of fence (4 wire) - - - 140.00

Dwelling house, complete, 600.00

Stable, barn and sheds, - - 260.00

Clearing, plowing and harrowing 40 acres, - 150.00

100 shade trees, .... . 15.00

200 fruit trees, $30.00

10 acres planted to alfalfa and seed, 20.00

20 acres wheat and seed, • 30.00

4 acres of potatoes, seed and planting, 20.00

5 acres of oats, - - 10.00
Water rental, - - 80.00

Total, $2,955.00

FIRST YEAR'S RETURNS, HARVESTED.

800 bushels of wheat, 60 cents per bushel, $ 480.00

1,200 bushels of potatoes, 50 cents per bushel, - 600.00

250 bushels of oats, $1.00 per bushel, 250.00

10 acres of alfalfa and seed (J return), - 150.00

Total, - $1,480.00

The above shows a net earning of 50 per cent., or one-half
the total amount invested, for the first year's work.

RAINFALL AND HUMIDITY.

For ease of comprehension Utah may best be divided into
three divisions: The moist counties, whose rainfall exceeds 12
inches per annum; the dry counties, with a rainfall of 6 to 12
inches; and the hot counties, with a slight rainfall and great heat.

The moist counties are Cache, Box Elder, Rich, Morgan,
Weber,Davis, Summit, Salt Lake, Utah, Wasatch, Uintah, San-
pete, Sevier and parts of Emery, Garfield, Piute and San Juan.

The dry counties areTooele, Juab, Millard, Beaver, Iron and
parts of others.

The hot counties are Washington, Kane, and parts of San
Juan, Piute and Garfjeld.

General Greely, Chief Signal Officer of the United States
has most thoughtfully sent through Governor Thomas advance
sheets (galley proofs) giving complete tables and graphical charts
of the rainfall and temperature. The former dating from 1856,
the latter from 1850. Whether the observations as to rainfall
made prior to the establishment of the signal office here, 1874,
are reliable, is very doubtful — they increase the annual average
verv materiallv.

No other data more forcibly shows the arid nature of Utah,
and it is only to be regretted that we have not yet established
points of observations in the Wasatch and Uintah ranges that
we might have a better knowledge of the annual precipitation in
the locality from which our irrigation supply is obtained.

Temperature also cuts quite a figure, for a "late spring" and
cool summer, even with a lesser and late snowfall, gives better
and more equable results from the irrigation standpoint, as wit-
ness this "season" of 1891.

In Salt Lake Valley, 40 per cent, of the rainfall occurs in
the spring, 9 in the summer, 25 in the fall, and 26 in the
winter. Winter begins about January 1st and lasts six weeks.
In latitude 40 degrees there should be on general principles 30
inches in a year.

Over the United States, east of the one hundredth meridian
west of Greenwich, the average rainfall is 40 inches, 60 per cent,
of which is at once thrown off in the river discharge.

The meterological records do not indicate that the climate is
growing moister; but Rush Lake rolls its blue waves over what
was a meadow 20 years ago, and Great Salt Lake has at least ten
feet of brine where wagons were driven to and fro in 1863.

Increased humidity has followed the settlement and cultivation
of the Mississippi valley prairies, and it is not unlikely that it is
doing so in Utah, although there is not sufficient data as yet to
determine in what degree.

The mean-air pressure at Salt Lake City is 25.63 inches;
water boils at 204.3 degrees. The prevailing winds are from the
north-northwest, and the most windy months are March, July,
August and September. The mean velocity ot the winds during the
entire year is 5£ miles an hour. On the ocean it is 18; at Liverpool
it is 13; at Toronto, 9; at Philadelphia, 11. The climate of Utah
on the whole is not unlike that of northwestern Texas and New
Mexico, and is agreeable except for a month or so in winter, and
then the temperature seldom falls to zero or snow to a greater
depth than a foot; and it soon melts away, although it sometimes
affords a few days' sleighing. The spring opens early in March.

Means...

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MONTHLY AND ANNUAL PRECIPITATION AT SALT LAKE CITY, UTAH, FROM RETURNS
U. S. SIGNAL OFFICE, WAR DEPARTMENT.

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The following gives the average annual precipitation at
prominent points north, east, south and west of Salt Lake City:

STATION.

DURATION OF
OBSERVATIONS.

AVERAGE ANNUAL
PRECIPITATION.

Kelton, ------
Ogden, --. - -

12 years.
21
10
3
9
3

6.10 inches.
13.46
13.74
6.53
17.41
5.18

Fort Duchesne,
Fort Douglass, -
Deep Creek, - - - -

UNITED STATES LAND OFFICE RETURNS,

No. of acres entered under the Desert Land Laws, 694,176.76
No. of acres on which final papers have issued

under Desert Land Laws, 135,340.32

No. of acres entered under the Timber Culture Laws, 179,118.35
No. of acres entered under the Homestead Laws, 1,293,750.00
No. of acres on which Cash Certificates have issued, 375,791.25
No of acres entered under all the land laws, - 2,542,836.36
Estimated No. of acres of surveyed land still sub-
ject to entry, under the public land laws, 6,919,840.00
Estimated No. of acres of unsurveyed land subject

to entry, - 26,88',),853.00

ESTIMATED NUMBER OF ACRES OF LAND IN EACH COUNTY
SUBJECT TO ENTRY.

NO.

COUNTY.

ACRES SURVEYED.

ACRES UNSURVEYED.

Beaver, -

335,160

1,700,000

Box Elder, - -

483,316

1,906,960

Cache . - -

90,740

95,668

Davis, - - - -

9,367

700,000

Emery, - - -

448,165

2,300,000

Garfield, - - -

214,500

2,30<>,000

Iron, - - - -

58-2,250

1,920,000

Juab, - - - -

707,920

1,500,000

Kane, ...

377,580

1,610,000

Millard, - - -

1,191,590

2,500,000

Morgan, - - -

51,080

500,000

Piute, - - - -

220,880

1,380,000

Rich, - ...

289,8«0

7,000

Salt Lake, - -

2,700

130,000

San pete, - - -

122,680

860,000

Sevier, ...

211,100

1,460,000

Summit, - - -

217,500

1,000,000

Tooele, - - -

769,220

2,500,000

Uintah, -

150,540

1, (544,000

Utah, .....

182,677

1,000,000

Wasatch, - -

62,155

207,000

Washington, -

188,340

1,000,000

Weber, - - -

8,500

290,519

Total, - - -

6,919,840

26,882,853

DUTY OF WATER.

0
As there does not appear to be a clear understanding by

most people of many of the terms used in connection with irri-
gation, the following, defining the meaning of such expressions
and giving the comparative values used, it was deemed would be
useful. Irrigation water is measured generally by the cubic
foot, by the gallon or by miners inches.

The "duty of water" means the area of land upon which a
.definite volume of water, applied during a given period, will suc-
cessfully raise crops. Thus the average duty in Utah of one
cubic foot per second, during a period of 120 days, is 100 acres.

One cubic foot per second is called a "second-foot." The "acre-
foot" is the equivalent of one acre covered one foot deep or
43,560 cubic feet. The miners inch is a variable quantity de-
pending upon the head above the one inch orifice of discharge.
It varies from a four inch head to a six inch head, and is not a
commendable unit of measure. Thus there are 50 miners inches
to a cubic foot per second, California measurement, and about -JO
miners inches Colorado measurement. One cubic foot contains
7£ U. S. gallons of 231 cubic inches.

CUBIC FEET.

] cubic foot peT second equals 2 acre feet in 24 hours.

" 60 " " 30 days.
" 130 " " 3 months.

" 170 " " 1 year.

" " " " 7.5 gallons per second.

" 449 " " minute.
" " " 50 California inches.

" 38.4 Colorado

CALIFORNIA INCHES.

ICO California inches equals 4 acre feet in 24 hours.

1 " foot 6 "
" 120 " feet 30 days.
" 360 " " 3 months.
" 14-iQ " " 1 year.

" " "15 gallons per second.

" 900 " minute.

" " 77 Colorado inches.

" % " " 2 Cubic feet per second.

COLORADO INCHES.

100 Colorado inches equals 5^ acre feet in 24 hours.

1 " foot in 4.2 "
"155 " feet in 1 month.
" 465 " " 3 months.
" 1,860 " " 1 year.
" " 19.50 gallons per second.

"1,170 " minute.

" " 2.6 cubic feet per second.

" 130 California inches.

The terms as applied to wells such as "artesian positive"
means one from which the water rises above the surface.

"Artesian negative" is one in which the water does not rise
above the surface.

"Phreatic water" (signifying ground water), is that nearer
the surface and derived from absorption, and is a name given
in a general way to all species of wells that arc supplied from
the "ground water."

SYNOPSIS OF UTAH LAWS RELATIVE TO
IRRIGATION.

Whenever the public necessity requires it> the county court
may organize the county, or a part of it, into an irrigation dis-
trict, and the land holders therein may use the water brought into
the district according to their respective needs, provided they pay
and perform their proportion of the necessary expense and labor.
They may, on due notice, elect trustees, a secretary, and a
treasurer.

The trustees shall locate the ditches and estimate all costs
and report to the county court. If the report be approved by a
two-thirds vote, a tax shall be assessed and the ditch constructed.

The trustees have general supervision of the construction,
maintenance, and regulation of the ditches; they may hold
such personal property as is necessary to the performance of
their duties; may sue and be sued, and may have appraised and
sell any unclaimed lands that are to be benefited, and apply the
proceeds to the construction of the ditches.

Lakes and ponds may be used as reservoirs, provided they
are not raised so as to injure settlers upon their banks.

In case of inundation or other sudden emergency, the trus-
tees may take measures for protection.

Property and money in the hands of trustees to be used on
the ditches is exempt from taxation.

Ditches have the right of way, a proper compensation having
been paid.

Any person injuring a ditch or any of its appurtenances, is
liable in damages and to a fine and imprisonment.

The district is liable for damage caused by the breakage of
a ditch.

The rate of tax at any election subsequent to the first may
be determined by a majority vote, and the tax thus assessed shall

be a lien upon the taxpayer's interest in the ditch and a right to
use the water.

By act of February 20, 1880, the selectmen of the several
counties are made water commissioners, who have a kind of su-
perior jurisdiction of the water rights in their respective coun-
ties.

They determine claims relative to the use of water, oversee,,
either personally or by agents-, its distribution and determine
questions of right of way, etc.

They also issue certificates showing the extent of water
rights.

A person first taking water from any source of
supply, or having the open, peaceable, and continuous use of
the water for seven years, has a primary right therein to the
extent of the reasonable use thereof.

Whenever persons having the primary right use the
water for a part of the year only, the person appropriating it for
the balance of the year acquires a secondary right.

The person appropriating the surplus above the average of
seven years also acquires a secondary right.

Water rights may be measured in inches or by fractional
parts of the whole supply. Water rights may pertain to the land
or may be personal property, as the owner may elect, and a
change of place shall not affect the right to use the water; but
no change of place shall be made to the injury of another owner
without ju t compensation Neglect for seven years to use water,,
or keep in repair the means of conveying it, is regarded as an
abandonment of the right.

Water rights are exempt from taxation, except for the pur-
pose of regulating the use of the rights, but the increased value
of the land may be regarded in making the assessments.

Surplus water must be returned to the natural channel, and
any person wasting it is liable to have his supply shut off, and to
pay damages to any person injured.

Any person using water lawfully appropriated to another, or
diverting the flow of water lawfully distributed, or injuring any
dam, ditch, etc., is guilty of a misdemeanor.

V( henever the supply is not sufficient for all purposes, the
use for domestic purposes and for irrigating purposes takes pre-
cedence in that order.

Corporations may be formed under general laws for dis-
tributing water to their stockholders.

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