Hardy v. Beaver County Irr. Co.

234 P. 524, 65 Utah 28, 1924 Utah LEXIS 2
CourtUtah Supreme Court
DecidedDecember 27, 1924
DocketNo. 3459.
StatusPublished
Cited by12 cases

This text of 234 P. 524 (Hardy v. Beaver County Irr. Co.) 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
Hardy v. Beaver County Irr. Co., 234 P. 524, 65 Utah 28, 1924 Utah LEXIS 2 (Utah 1924).

Opinions

IVERSON, District Judge.

This appeal involves a general adjudication of water rights on that segment of the Beaver river extending from the lower end of what is commonly known as the “Beaver Valley” to a point approximately 14 miles below the town of Milford. The testimony is very voluminous, but for the purpose of this opinion it will suffice to make a statement of the following facts, which are established by the record:

From the Beaver Valley the river flows through a canyon approximately 7 miles in length from the lower end of which it traverses a tract of land owned by the appellant, comprising approximately 15,000 acres, commonly referred to in the testimony as the “Milford Project,” and flows thence through a tract of lowland, bordering the river channel on either side, some 5 miles in length, referred to in the testimony as the “Milford Bottoms”; thence through a series of hills a distance of several miles, from which it emerges into what is commonly known as the “Beaver Bottoms,” a valley varying from 1 to 2 miles in width and from 10 to 15 miles in length. Until it reaches Beaver Bottoms, the river is generally confined to a single and more or less well-defined channel, but there it divides into two channels, one of which extends along the west and the other along, the east side of the valley, in more or less well-defined courses, until they reach the land of those of the respondents whose farms are situated some 7 or 8 miles from the upper end of the valley, where the identity of the channels is lost in numerous swails and depressions.;

At the upper end of the canyon which has been mentioned, the appellant has constructed a dam, commonly known as the “Rocky Ford Dam,” and has thereby created a reservoir covering the channel of the river having an impounding capacity of approximately 28,000 acre-feet.

*31 Near tbe lower end of tbe canyon, tbe Minersville Reservoir & Irrigation Company, tbe original appropriation of wbicb antedates those of tbe respondents, bas its point of diversion from tbe river. At tbe time of construction of tbe reservoir, appellant acquired all tbe rights of tbe Minersville Reservoir & Irrigation Company in tbe river, subject to an interest reserved by such company of 7,500 acre-feet.

The river bas its principal source of supply in tbe Tusbar range of mountains, although tbe record shows' that at times, during the latter part of tbe winter and early spring, there is a considerable contribution to tbe stream of water which accumulates from the melting snow in tbe Milford Valley and from the mountain rang-es wbicb flank the valley on either side.

As is usual in mountain streams, there is a wide variance in tbe volume of water wbicb flow's in tbe river at different seasons of the year, the flood or high water usually commencing about tbe middle of May and lasting until tbe latter part of June or first of July, while during tbe summer season and early fall, comprising tbe months of July, August, and September, the flow of tbe stream recedes to such an extent that there is rarely, except at times of unusually heavy rainfall, more than a few second-feet of water in tbe stream at tbe Minersville point of diversion in excess of that diverted and used by tbe appropriators from tbe stream in tbe Beaver Valley. After irrigation ceases in tbe Beaver Valley, there is a substantial flow of water in tbe segment of tbe river under consideration, except when it is impounded in tbe reservoir constructed by tbe appellant, which usually continues during the late fall and winter months, until about tbe middle of March, when ordinarily there is another season when the river, in the Milford and Beaver Bottoms, is dry, due to tbe use of the water by the upper appropriators, wbicb lasts until tbe commencement of tbe succeeding high-water season. The aggregate run-off of tbe river at the lower end of tbe Beaver Valley, over tbe annual 'period, varies greatly in different years, depending upon tbe season, receding to approximately 18,000 acre-feet in some years and increasing to approximately 46,000 acre-feet in others.

*32 In former years, before the flood waters of the stream, were diverted to any great extent for irrigation in the Beaver Valley or impounded in the reservoir constructed by the appellant, most of the land in the Milford and Beaver Bottoms appears to have been more or less inundated during the high-water season, as well as at times during the winter season, and seemingly more of an effort was made by the owners of land on both the Milford and Beaver Bottoms, by the construction of dams and dikes, to divert the water away from rather than to and upon their land for the purpose of irrigation. However, it appears that prior to the construction of the appellant’s reservoir, in the years 1913 and 1914, the average run-off of the stream in the Milford Valley had been materially decreased by diversion in the upper valley and that of the Minersville Reservoir & Irrigation Company, and a number of respondents — mainly the original plaintiffs, in the action — by means of dams constructed in the river channels and in the swails into which the water overflowed during the flood season, and also in a number of instances by means of ditches, had been accustomed to divert water from the river to and upon their land for the purpose of irrigating their crops consisting principally of wild hay, gra'in and alfalfa. It appears from the evidence, however, that their irrigation systems for the most part were and still are extremely crude and inefficient, and that little, if anything, has been done by any of the respondents in the way of leveling, cross-ditching, and otherwise preparing their land for reasonably efficient irrigation.

Owing to the diversion of all the water in the stream by the upper appropriators during the low-water season, in July, August, and September, the appropriators from the river on the Milford and Beaver Bottoms Were accustomed to irrigate their crops once during the latter part of March or early in April, when there was water available for the purpose, and again during the season of flood flow, giving them, one or at most two, irrigations, as the condition of the crop required. By means of such irrigations, they were enabled to mature their grain crops and raise two crops of alfalfa or one crop *33 of bay and a crop, of alfalfa seed. While tbe respondents allege in tbeir pleadings that it was also their custom to use the water which flowed in the river during the winter for irrigation’ purposes, the evidence fails to show, with any degree of certainty, that there was any general use of the water in that manner or that such water as was used during the winter season accomplished any beneficial result.

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Cite This Page — Counsel Stack

Bluebook (online)
234 P. 524, 65 Utah 28, 1924 Utah LEXIS 2, Counsel Stack Legal Research, https://law.counselstack.com/opinion/hardy-v-beaver-county-irr-co-utah-1924.