Schenk v. City of Ann Arbor

163 N.W. 109, 196 Mich. 75, 1917 Mich. LEXIS 753
CourtMichigan Supreme Court
DecidedMay 31, 1917
DocketDocket No. 137
StatusPublished
Cited by24 cases

This text of 163 N.W. 109 (Schenk v. City of Ann Arbor) is published on Counsel Stack Legal Research, covering Michigan Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Schenk v. City of Ann Arbor, 163 N.W. 109, 196 Mich. 75, 1917 Mich. LEXIS 753 (Mich. 1917).

Opinions

Ostrander, J.

The demand of the inhabitants of the city of Ann Arbor for water for domestic and other purposes exceeds 3,000,000 gallons daily. The municipality owns and operates the water plant supplying water to the inhabitants. Its present used sources of supply are wells, some springs, and the Huron river, which flows through the city. It is dissatisfied with the quantity and the quality of water thus available for the use of the city and its citizens. The charter of the city in terms grants the power to purchase, erect, and maintain grounds and buildings, within or not exceeding three miles outside of the limits of the city, for waterworks. Act No. 331, Local Acts of 1889, as amended by Act No. 658, Local Acts of 1907. South, and some three miles distant from the city, is a considerable tract of marsh land, underlying which is a large bed of water-bearing gravel, within easy reach of the surface of the ground, and there are also two other beds of gravel lower down, one 80 and the other 140 feet below the surface, each of them containing water. Underlying this region, the formations are so distributed, to use the language of a witness:

“That there is a slope for the underground water from the western part of Washtenaw towards Lake Erie, and what is true of this region is true all the way from Hillsdale county northerly to the headwaters of the Huron river up in Oakland county, so that the area that lies between the western part of Washtenaw county and the Steere farm has a slope to the southeast, a general slope to the southeast, and a general [77]*77drainage to the southeast, and a general underground flowage to the southeast. This is the natural result of the conditions prior to the deposition of the glacial deposits. * * * The gravel deposits are very homogeneous. There is a great deal of fine marl, with clay in it. Traversing this are beds of gravel and sand that we find exposed, and these are found at various levels. These gravel deposits are in the neighborhood of 200 feet thick; in Lodi township they exceed 250 feet; and in the vicinity of the Steere farm they exceed 1,350 feet. Because of the great thickness of the gravel deposits there are running through these deposits at various levels various channels, so that in sinking wells it is not a difficult matter in this region to obtain a considerable supply of water, so that there are hardly any farmers in this neighborhood, I gather, who were unsuccessful in obtaining water; if not within a few feet of the surface, they could by going deeper. * * * The contributing area would come in through these western townships of the county — from Dexter, Lima, and Freedom townships, and part of Sylvan and the townships to the west. They would contribute to this underground water, the natural flow of this area in this way, and this is demonstrable from the records of the wells I have obtained through the intervening area.”

As early as the year 1910 attention was directed to this possible source of. a water supply for the city, and in the year 1912 and thereafter tests were made to determine the quantity of water procurable. There were a number of small wells upon the marsh from which water was flowing. Other wells were driven, five 8-inch wells, and later another 8-inch and a 12-inch well, being, put down by the city, to an average depth of about 30 feet. As many as 715,000 gallons of water flowed freely from the first five 8-inch wells, and from seven wells the daily flow was 866,200 gallons, a quantity which was materially increased by the use of a pump. In the year 1915 the city constructed upon the land a well 16 feet in diameter, from which it pumped water from May 1.2th until July 5th, the pumping being [78]*78fairly continuous, day and night, although for various reasons, pumping was for short periods of time interrupted. The result was from 3,700,000 to 3,800,000 gallons of water daily. The pumping lowered the water in the well from a point above the level of the ground to within three feet of the bottom of the well. At some time, before or after the tests were begun, the city bought and owns 130 acres of the land, including that upon which the test wells were constructed. Upon this land it desires to erect a costly pumping station, pump the water therefrom, force it to the city, and distribute it to the inhabitants.

It is the theory of the city, which its testimony, and especially its opinion evidence, tends to support, that it' can for an indefinite period take from the wells upon this land a quantity of water, approximating 4,000,000 gallons daily, without lowering the head of the underground water, or the water table, more than it was lowered during the tests it has conducted. It is its theory, also supported by its opinion evidence, that the water in the water-bearing gravel reached by its wells does not, by its presence in the earth, by sepage or percolation, affect agriculture upon or over or near to the particular tract of land; that it is from rains, and not from percolation or seepage from the subterranean body of water, that agriculture is supplied with required moisture.

The plaintiff, and, it appears, other land-owners, upon the marsh and on higher land, contend, and offer testimony to support the contention, that as a result of the pumping operations wells in the vicinity have gone dry, flowing wells upon the marsh have ceased to flow or flow a diminished quantity of water, and that the agricultural productiveness and value of land for a half mile in every direction from the large well of the city will be unfavorably affected by continued pumping of water from the city’s property. The testimony [79]*79for the plaintiff tends to prove that, when the city be-; gan to pump water from the large well, the water in, plaintiff’s well, 200 rods north and west from the city1 well, was 4 feet deep, and lowered at the rate of about a foot a week during the first two weeks, and thereafter an inch a day for a week, and then one-half inch a day, until there was no water left in the well. When the pumping ceased, the water returned at the rate of oné-half inch a day, and at the time of the hearing there were 40 inches of water in the well. While the pumping was continued, plaintiff was obliged to get water from a neighbor and to draw water in a tank from the county ditch for his stock. Upon another farm of 284 acres, east and across the road from the plaintiff’s, farm, were two wells, one dug at the house and one at| the barn, and two flowing wells in the fields for the use of stock. The well at the house had been dug more than 50 years, and had always furnished sufficient^ water for domestic use. The water in this well was lowered during the pumping, so that no water could be pumped from it, and after the pumping ceased the water in the well did not return. The well at the barn was affected in a similar way. The flowing wells upon this farm were about three-quarters of a mile north and west of the large well put down by the city. From| one of them the water ceased to flow at all, and from the other only a small quantity ran away, and at the. time of the hearing the flow of water had returned, in one well not at all and in the other only in reduced quantity. Upon another farm south of plaintiff’s land, and west of the land owned by the city, was a flowing well, a mile from the large well owned by the city. It was a 8-inch well, and before the pumping began had flowed a stream of water two-thirds the size of the¡ pipe. The flow was almost entirely cut off while the, pumping was carried on, and after it ceased about one-half of the original flow returned.

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Cite This Page — Counsel Stack

Bluebook (online)
163 N.W. 109, 196 Mich. 75, 1917 Mich. LEXIS 753, Counsel Stack Legal Research, https://law.counselstack.com/opinion/schenk-v-city-of-ann-arbor-mich-1917.