Salt Lake City v. Gardner

114 P. 147, 39 Utah 30, 1911 Utah LEXIS 27
CourtUtah Supreme Court
DecidedFebruary 1, 1911
DocketNo. 2135
StatusPublished
Cited by23 cases

This text of 114 P. 147 (Salt Lake City v. Gardner) is published on Counsel Stack Legal Research, covering Utah Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Salt Lake City v. Gardner, 114 P. 147, 39 Utah 30, 1911 Utah LEXIS 27 (Utah 1911).

Opinions

FRICK, C. J.

This action was instituted pursuant to section 1288x14, Comp. Laws 1907, to determine the right of respondents to-[32]*32appropriate a specific quantity of water from Utah Lake. In September, 1905, pursuant to section 1288x6, respondents duly made and filed with, the state engineer their application to appropriate forty cubic feet of water per second of time from said lake. Appellants, pursuant to section 1288x9, duly protested said application, which protest the state engineer overruled and allowed respondents’ application, whereupon appellants brought this action to determine respondents’ rights to appropriate any of the waters of said lake as aforesaid.

Utah Lake is a rather shallow body of water which varies in depth from a few inches near the shore line to thirteen feet at its deepest part. The water covers an area of about ninety-three thousand acres, or approximately one hundred and fifty square miles. The lake is the lowest part of a drainage basin comprising an area of about three thousand square miles. The sole outlet of the lake is Jordan Eiver with its source in the extreme north end of the lake, and thence flows in a northerly direction emptying into the Great Salt Lake. In the year 1882, each on¿ of the plaintiffs, as separate corporations, and each in its own right and behalf, constructed certain canals into which they diverted a certain quantity of the water flowing from the Jordan Eiver or Utah Lake and devoted such to a useful and beneficial purpose. The combined capacity of the canals aforesaid amounted to a flow of eight hundred and twenty-eight cubic feet per second. In addition to the foregoing corporations, other parties, had also appropriated certain quantities of water from said lake in the manner aforesaid, and whose rights were prior to appellants’, amounting to a flow of about one hundred and seventy-six cubic feet per second. In diverting the water, and for the purpose of obtaining a more regular as well as a more continuous flow from the lake into- the Jordan Eiver at its source, appellants caused a certain dam to be constructed at the point where the water of the lake flowed into’ the Jordan Eiver, and in that way impounded the water in the lake, and thus, in certain seasons of the year, caused the water to rise and stand at a higher level. In [33]*33doing this, tbe water in the lake was caused to overflow some of the lower lands surrounding the lake, to which the landowners objected and insisted that the dam be removed or lowered. In 1885 a compromise was effected, and it was agreed between the water users and the landowners that the dam might be maintained at a certain height, which was fixed at three feet three and one-half inches above low-water mark, which point was designated “compromise point.” This point is precisely three feet three and one-half inches above the bottom of Jordan Eiver at the point where the water of the lake enters that stream.

It will thus be seen that, when the water in the lake rose so that it reached compromise point, the water users had to permit the water to flow into and through the Jordan Eiver unmolested, and, when the water fell so that it was three feet three and one-half inches below compromise point, the water users could obtain no water by natural flow from the lake at the intakes of their canals, which were some distance north from the source of the Jordan Eiver and along said stream.

In view of the foregoing conditions, the lake water flowed somewhat irregularly and in varying quantities into the Jordan Eiver, and from that stream into the diverting canals of the plaintiffs. The varying quantities so flowing were determined by a series of measurements, from which the following results were obtained, namely: When the water in the lake stands at one foot above compromise point, the natural flow from the lake into the river is eight hundred cubic feet per second; when' the water is only six inches above that point, the flow is six hundred and twenty-five feet per second; when the water stands at compromise point, the flow is reduced to five hundred and five feet per second; when it is six inches below that point, the flow is four hundred and ten feet per second, and at two feet below; it is one hundred and eighty-seven feet per second, while at three feet below the flow is but eighty-two and a fraction cubic feet per second. As a matter of course, when the water fell below the bottom [34]*34of tbe Jordan Kiver there was no natural flow at all. For the purpose of overcoming the difficulty arising from the foregoing variation in the flow, and to obtain a regular flow of water from the lake into their diverting canals, plaintiffs, in 1902, installed a pumping plant at the point where the lake empties into the Jordan Kiver, to which plant they have added from time to time after 1902 so that when this case was tried appellants had seven pumps installed with a combined theoretical pumping capacity of seven hundred cubic feet per second.

From various measurements that were made, it was also made to appear from the record that from 1887 to 1900 the water fluctuated in Utah Lake from being eleven inches above compromise point, the highest point reached, in June, 1893, to three feet one inch below that point, the lowest, in October, 1900. During the term of years aforsaid there were only four years when the water rose above compromise point, namely, 1893, 1894, 1896, and 1897; and two years, to-wit, 1890 and 1899, when the water reached, but did not go above, compromise point; while in all the years it fell below that point during a large portion of each year. The average of all the measurements, as near as we can Ob'lain it from the record, that the water fell below compromise point each year during the years aforesaid, was probably about eleven inches; while the average of all the measurements that the water rose above that point was about five inches. The water, however, was above compromise point but a short time in each year. In one year it was above that point for about sixty days; while in the other years the time did not exceed thirty days, which was during the high-water season.

It is important to bear in mind that from the foregoing measurements, which are not disputed by any one, there was no time, so far as the record shows, when the natural state of the water in Utah Lake was such as would permit a natural flow into Jordan Kiver and from thence into the diverting ditches of appellants of the quantity of water claimed by them, namely, eight hundred and twenty-eight cubic feet [35]*35per second. Tbe highest amount that would thus flow was during parts of the months of June and July, 1893, and May, 1897, at which times, however, less than eight hundred second feet would flow into the Jordan Eiver. During two other months the flow of water was slightly in excess of six hundred feet, and during eleven months more the flow was between five hundred and six hundred feet, while during all the remainder of the time between December, 1887, and December, 1900, covering the whole period of the measurements, the flow was less than five hundred cubic feet per second into the Jordan Eiver from the lake. Moreover, taking the period from 1893 to 1906, during which time an attempt was made to show the quantity of water that appellants diverted from their ditches and actually applied to a useful and beneficial purpose, the clear weight of the evidence is to the effect that appellants did not at any time take or use water in the amount allowed them in the decree by the trial court.

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Bluebook (online)
114 P. 147, 39 Utah 30, 1911 Utah LEXIS 27, Counsel Stack Legal Research, https://law.counselstack.com/opinion/salt-lake-city-v-gardner-utah-1911.