Bastian v. Nebeker

163 P. 1092, 49 Utah 390, 1916 Utah LEXIS 133
CourtUtah Supreme Court
DecidedDecember 27, 1916
DocketNo. 2898
StatusPublished
Cited by13 cases

This text of 163 P. 1092 (Bastian v. Nebeker) 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
Bastian v. Nebeker, 163 P. 1092, 49 Utah 390, 1916 Utah LEXIS 133 (Utah 1916).

Opinions

McCARTY, J.

(after stating tbe facts as above).

TJje first question presented by the appeal is, Did the court err in its findings of fact wherein it held that 84-J per cent, of the water flowing from the wells is developed water that did not, before the wells were constructed, come to the surface of the earth through the orifices and subterranean channels from which issues and flows the spring and seepage water of King's Meadows?

The court, in effect, found, and there is an abundance of evidence to support the finding, that the waters from the wells and the normal flow of the springs and seeps came from the same source and are supplied by the same underground reservoir or body of water. In fact no other conclusion is permissible from the evidence, considered, as it must be, in its entirety. Counsel for respondent concede this. In their printed brief they say:

‘ ‘ There is no question made by us, # * * but what the operation of the wells did interfere with the water of some of the springs to the extent of taking therefrom a small percentage of the water.”

The court, before the trial was concluded, suspended proceedings and made an order that:

‘ ‘ The water in dispute be measured on the 21st day of June, 1912, and that immediately after such measurements that the wells be plugged so as to prevent any waters flowing therefrom; that five days later, to wit, June 26th, the waters flowing in said basin be measured; that on July 1, 1912, the waters flowing from said basin be again measured, and immediately after such measurement that the wells be turned loose so that the water may flow therefrom; that on July 11, 1912, the waters from the wells and springs be measured separately; that on July 21, 1912, the said waters flowing from said wells and springs be measured separately, and that the wells be then plugged so as to prevent any water from flowing therefrom; that said measurements be continued each [398]*398and every month thereafter in the same manner * * * until final trial of this cause.’ ’

The court appointed J. Oscar Anderson, a civil engineer, “as the agent of the court to make such measurements.” Anderson, in pursuance of the order, made measurements as therein directed to and including July 1, 1912, and thereafter made measurements every ten days, instead of every five days, to and including January 21, 1913. The flow of the water from the spring, as shown by the several measure^ merits, also the flow from the wells when unplugged, was as follows:

Well Spring

Water. Water.

June 21 (wells unplugged).453 .263

June 26 (wells plugged). .336

July 1 (wells plugged). .336

July 11 .440 .263

July 21 (wells plugged).. .338

August 1 .438 .263

August 11 (wells plugged). .335

August 21 .438 .249

Sept. 1 (wells plugged).•. .365

Sept. 11 .439 .293

Sept. 21 (wells plugged). .352

Oct. 1 .540 .30

Oct. 11 (wells plugged). .364

Oct. 21 .■.452 .293

Nov. 1 (wells plugged). .388

Nov. 11 .439 .291

Nov. 21 (wells plugged). • .365

Jan. 1 (wells plugged). .394

Jan. 21 .'... .452 .313

The decimals indicate fractions of a second foot.

The result of the measurements made by Anderson in pursuance of the court’s order shows that when the wells are permitted to flow continuously for a period of ten days only, there is a substantial reduction in the flow of water from the springs. To what extent a continuous and uninterrupted flow from the wells would affect the springs in the course of a few months or a year is a matter of conjecture only.

[399]*3991 It is settled law in this jurisdiction that where a party goes upon a stream at or near its source, the waters of which have been appropriated, and are being nsed by others for beneficial purposes, and intercepts or taps a subterranean flow or body of water and diverts any substantial flow therefrom which he claims to be developed water, the burden is upon him to show by satisfactory proof that the water so intercepted and diverted is “developed water.” Mountain Lake Min. Co. v. Midway Irr. Co., 47 Utah 346, 149 Pac. 929. And where, as in the case at bar, it is shown by indisputable evidence that the water claimed to be developed water is drawn from the same underground flow or body of water that wholly or partially feeds and supplies the springs from which the prior appropriator obtains his water, the subsequent appropriator, the party claiming to have developed water, should be required to show by clear, positive, and convincing evidence, that the water claimed by him is developed water. Mountain Lake Min. Co. v. Midway Irr. Co., supra, and cases there cited.

2 The evidence in this case, as the record now stands, regarding the effect that a continuous and uninterrupted flow of the wells would eventually have upon the flow of water from the springs is, as stated, a matter for conjecture and theory only. The plaintiff, therefore, did not support his claim that 84 7/8 per cent, of the water flowing .from the wells is, as found by the court, developed water, by that quantum of evidence required in eases of this kind. The proof on this pont, as the record now stands, furnishes as sound a basis for concluding that a continuous, unimpeded flow of water from the wells, for a considerable period of time, would materially reduce the flow of the springs below, the lowest point shown by the measurements made by Anderson, if it did not entirely dry up the springs, as it does for concluding that it would not reduce the flow of the spring water below what it was when the measurements were made. The court therefore erred in making the finding of fact last referred to.

[400]*4003 [399]*399The trial court, by appointing some person, familiar with the rules for measuring water, to measure the water [400]*400flowing from the spring and seeps at intervals for a reasonable length of time while the wells are plugged and then make measurements at intervals for a considerable length of time when the wells are flowing at their full capacity, ought to be able to determine approximately the amount of developed water, if any, that flows from the wells. Should the trial court on retrying the ease make an order that further •measurements and tests be made to determine the amount of developed water, if any, produced by the wells, the entire expense of such measurements and tests shoulá be borne by the plaintiff, because, as stated, the burden is on him to show by clear and convincing evidence that the water claimed by him is developed water.

4 The evidence shows that plaintiff’s trench or drain ditch situated just west of and in close proximity to the natural water channel where the same passes through King’s Meadow intercepts and carries to plaintiff’s reservoir a substantial flow of seepage water. This seepage water is tributary to the main stream used by the Nebekers, and the court erred in not awarding and decreeing it to them.

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Bluebook (online)
163 P. 1092, 49 Utah 390, 1916 Utah LEXIS 133, Counsel Stack Legal Research, https://law.counselstack.com/opinion/bastian-v-nebeker-utah-1916.