Hanson v. Salt Lake City

205 P.2d 255, 115 Utah 404, 1949 Utah LEXIS 143
CourtUtah Supreme Court
DecidedApril 16, 1949
DocketNo. 7112.
StatusPublished
Cited by17 cases

This text of 205 P.2d 255 (Hanson v. Salt Lake City) 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
Hanson v. Salt Lake City, 205 P.2d 255, 115 Utah 404, 1949 Utah LEXIS 143 (Utah 1949).

Opinions

WADE, Justice.

Plaintiff, Orson Hanson, respondent here, brought this action against defendant, Salt Lake City, appellant here, for injunctive relief and money damages. He claims that as a result of the city drilling a large well and pumping large quantities of water therefrom during the summer *405 of 1934 in the neighborhood of his artesian well, the flow of water therefrom was greatly reduced so that without the aid of a pump on his well it would not supply sufficient water to satisfy his culinary and irrigation requirements as it had previously done, and that to supply his needs he installed a pump on his well. He asked as damages the cost of installing the pump, cost of operating it, and that the city be enjoined from pumping water from its well. The court refused to grant injunctive relief but did award him the damages which he asked in the sum of $295.10, which includes a substantial amount of interest.

The plaintiff is the owner of about 24 acres of land located at about 5200 South and 1700 East, according to Salt Lake County numbering system, southeast of Salt Lake City. It is an “L” shaped piece of property, facing a county road called Spring Lane on the north, and Highland Drive on the east.

This well is the only source of culinary water for plaintiff’s home; it was drilled in 1921. Prior thereto, there was another well only 60 feet deep which went dry shortly before this one was drilled. These two wells have supplied the culinary water for that home for 40 years prior to the time of the trial, in May, 1947. The first of these two wells was drilled after 1903. The present well is 260 feet deep, and until the city commenced pumping in August, 1934, it had always supplied about 50 gallons of water per minute, which was ample to supply the culinary needs of the home and water for the chickens and livestock and the dairy and to irrigate some land.

A three inch pipe brings the well water above the surface of the ground. From there a horizontal pipe extends about 7 feet in which the size of the pipe is reduced to 1 inch, from which the water flows into a 30 gallon barrel. From the barrel the water is piped on a downward slope a distance of about 25 feet through a 3 inch pipe into a ram, which uses the fall of the water from the barrel to *406 lift some of it about 32 feet into a tank. The water used to lift this water into the tank escapes into a ditch through which it runs onto the lands of others and sometimes is used for irrigation but is not thereafter used by plaintiff. The water is piped from the tank to plaintiff’s house, barn, chicken coops and stock watering trough. There is a valve on the well through which the well water may be turned into the dairy house and used for cooling purposes and onto the lawn around plaintiff’s house.

The summer of 1934 was an extremely dry one. In order to obtain irrigation water which it was obligated to supply to certain farmers, the city sank a large well on the banks of its canal at a point about 6000 South and 2100 East and about 1% miles southeast from plaintiff’s well. This well was drilled to a depth of 500 feet, and was perforated so that it would drain the water from all the various depths where water was encountered. It was on higher ground than plaintiff’s well and required a pump to bring the water to the surface. The city installed an electric pump thereon and commenced to pump on August 21, 1934, and continued to operate, with the exception of short intermittent periods, until October 17th of that year. It was also operated some in the summers of 1935 and 1936, but plaintiff’s evidence was positive that the pumping only interfered with his flow during 1934. When the pump was operating it produced a flow of from 2 cubic feet per second to 10.24 c. f. s.; usually it produced around 8 c. f. s. Shortly after the city commenced operating its pumps, the flow of water from plaintiff’s well decreased from 50 to about 4 gallons per minute. This quantity was insufficient to operate plaintiff’s ram and supply the water necessary for the other purposes for which he had used it in the past. He thereupon installed an electric pump on his well.

The court found that the operation of the city pump on its well reduced the flow in plaintiff’s well from 50 gallons to 4 gallons per minute. And, further, that such flow was insufficient to operate his ram or supply his needs for irri *407 gation culinary purposes. It refused to enjoin the city from operating its pump but awarded plaintiff damages as stated above. From this award the city appeals. It contends that in pumping water from this well it violated no right of the plaintiff.

The evidence is undisputed that both of these wells tap a large interconnected subterranean or artesian water basin. It indicates that this basin exists in the pervious strata or layers under the surface of the earth at various depths, and covers an irregular area from north to south of about 12 miles and from east to west of about 6 miles. This basin is sealed by impervious strata on the east, south and west but to the north it has an outlet into the Great Salt Lake. The water in question enters the basin from the east at the foot of the Wasatch mountain range. West of the Wasatch range fault line there is another fault line running generally from the south to the north which breaks the strata through which this water courses through which some of the water escapes to the surface as springs. About 6000 wells have been drilled into this basin, in some of which the pressure is sufficient to cause the water to flow naturally to the surface and in others, pumps are required. Part of these wells were drilled prior to 1934 and others have been drilled since.

Generally, each well has a tendency to lower the static head pressure, or the height to which the water will naturally rise, of all the wells, in the basin. But since pressure is required to force the water through the strata of per-vious materials and the movement of the water is slow, the direct effect of one well upon another cannot be traced for more than a distance of two and a half miles and then only where there are no natural interferences between the two wells in the artesian basin. Each well is said to have a cone of influence, or that within a circular shaped area around the well, in the absence of natural interference, each well tends to directly effect the static head pressure, of all other wells within a distance in some cases as far from *408 the well as two and one half miles. The closer the wells are together the greater the effect one has on the other, and where one well is upstream, or the course of the movement of the waters of the basin is from it toward the other well, the upper well in the flow of the waters has a greater effect and effects the other for a greater distance away than where the conditions are reversed. There also may be pockets in the basin or natural interferences in the flow of the water from one to the other, so that two wells might be relatively close to each other without either exerting any appreciable effect on the other.

Data was introduced in evidence by both parties of the effect the pumping from the city well had upon the flow and the static head pressure of plaintiff’s well, and a number of expert witnesses gave testimony on that question.

Free access — add to your briefcase to read the full text and ask questions with AI

Related

Rocky Ford v. Kents Lake
2019 UT 31 (Utah Supreme Court, 2019)
Salt Lake City v. Silver Fork Pipeline Corp.
2000 UT 3 (Utah Supreme Court, 2000)
F. Arthur Stone & Sons v. Gibson
630 P.2d 1164 (Supreme Court of Kansas, 1981)
Fairfield Irrigation Company v. White
416 P.2d 641 (Utah Supreme Court, 1966)
Current Creek Irrigation Co. v. Andrews
344 P.2d 528 (Utah Supreme Court, 1959)
N. M. Long & Co. v. Cannon-Papanikolas Construction Co.
343 P.2d 1100 (Utah Supreme Court, 1959)
Bullock v. Tracy
294 P.2d 707 (Utah Supreme Court, 1956)
Little Cottonwood Water Co. v. Sandy City
258 P.2d 440 (Utah Supreme Court, 1953)
FAIRFIELD IRRIGATION CO. v. CARSON Et Ux.
247 P.2d 1004 (Utah Supreme Court, 1952)
McNaughton v. Eaton
242 P.2d 570 (Utah Supreme Court, 1952)

Cite This Page — Counsel Stack

Bluebook (online)
205 P.2d 255, 115 Utah 404, 1949 Utah LEXIS 143, Counsel Stack Legal Research, https://law.counselstack.com/opinion/hanson-v-salt-lake-city-utah-1949.