Kerley v. Wolfe

84 N.W.2d 748, 349 Mich. 350, 1957 Mich. LEXIS 347
CourtMichigan Supreme Court
DecidedSeptember 4, 1957
DocketDocket 46, Calendar 47,139
StatusPublished
Cited by17 cases

This text of 84 N.W.2d 748 (Kerley v. Wolfe) 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
Kerley v. Wolfe, 84 N.W.2d 748, 349 Mich. 350, 1957 Mich. LEXIS 347 (Mich. 1957).

Opinion

Black, J.

Inland Lake Narrin occupies the greater portion of the northeast quarter of section 23, plus smaller portions of adjacent sections 13 and 24, of Oakland county’s G-roveland township. It is shaped like a summer squash, with the bulbous and deeper part situated in sections 23 and 24 and the shallower neck extending northeasterly into section 13 as far as 2 highways. One of the highways extends north-south and touches the lake at northeast-ernmost or stem end. The other extends in a general northeast-southwest direction and borders a short distance along the northernmost part of the neck.

Plaintiffs and defendants own contiguous acreage in section 13. The respective premises so owned by the contending parties is covered in part by the extremely shallow waters of the described neck of the lake. At one point defendants’ premises extend, upland to fast land, entirely across the neck and at this point they have erected a fence designed to prevent passage of rowboats and other small craft from the upper end of the lake (where plaintiffs’ premises are situated) into the main body thereof. Plaintiffs, claiming that they are riparian proprietors with right of boating and fishing between their part of the shore and the larger portion of the lake, filed this bill to abate the fence and enjoin its maintenance.

We have described the physical situation as it appears from exhibit 25 in the case, * and present *353 proprietorship • as it appears from the proofs. The principal question — aside from jurisdiction of equity — is whether the lake ever did extend to plaintiffs’ premises in such manner as to provide their predecessors, and plaintiffs in turn, with riparian rights as claimed. In such regard defendants insist that the vicinity of dispute was never anything more than swamp or marsh and that it is nonnavigable both in fact and law. A secondary question is whether, assuming plaintiffs’ said premises did at one time border on Lake Narrin with then accruing riparian rights, nature has not long since changed the character of the bed of the lake so that such rights are now extinct.

The issues so made were tried in detail. Dr. Donald MacLachlan, a professor of geology and principal witness for defendants, testifying from personal examination of the area in question, said:

“I would call the area between the 2 fences marsh. A marsh is a low-lying, wet, soggy tract of land. It’s described as land usually, wholly, or partially covered with shallow water. There are certain characteristics which are part of a complete definition of marsh; one of the characteristics is that the water covering the marsh be relatively shallow. The entire marsh may exist in a discontinuous body of water. If it exists in a continuous body, the level of the water in this body may be the same or may be at a different level. Another characteristic is the character of the plant life. I think the plant life characteristic of a marsh can best be described by giving the general nature of the forming of the marsh. Most marshes are formed from water in a *354 body or depression in which there is water, and formed by filling np this depression from a condition of open water to what is typically a marsh condition. If the original body of water is fairly deep, then usually the beginning of the filling process is accomplished. Detrital material; sand, mud, and silt is washed in from the land. After the body becomes sufficiently shallow, then the plants begin to grow on the bottom, and when the plants begin to grow and begin to add in the fill, at first when the water is still relatively deep and the area still may be considered something other than a marsh, the plants are primarily floating forms of life and gradually, when dying, settle to the bottom of the lake, or pond, or what is going to be a marsh, and tend to build up the bottom of the area. Shortly following that, water lilies begin growing, and as they die, more and more vegetation accumulates and keeps getting more and more shallow. Ultimately sometimes, you have a floating bog, I mean a floating mass of vegetation, and as the lake becomes nearer filled the later part of the filling being done by vegetation, sedges begin to take hold and they are followed in turn by shrubs, and these in turn are followed by spruce and tamarack. Water in a marsh may occur in disconnected bodies of water or you can call it accluded water.”

He testified further, with reference to the secondary question noted above:

“It is entirely possible that the lake proper, at one time, covered the area depicted in plaintiffs’ exhibit 25, an 1872 atlas. I could logically draw that conclusion from the tree line and the hard land line and the floor covered with muck and decayed vegetation. If you had some old residents who came in here and so testified, I would be in no position to doubt their word. I see no evidence of the wash of sand from the process of waves having affected the area towards Kerley’s. There is a very strong indication of the process of filling to the decay of vegetation. That’s why, when you even wade up by Kerley’s, *355 there is clear water down a little ways, and then there is soft substance that’s largely decayed vegetation. There may come a time when you couldn’t row a boat over that area if that process continued over a period of time. That same process occurs generally in the shallow portions of our inland lakes. To a lesser extent it occurs in the bottom of the deep portions of these lakes. There is an enclosement of vegetation toward the bottom of the lake. In the center of Narrin lake you would expect to find an accumulation of sediment on the bottom of that lake by reason of the valuation of depth, [but] its importance becomes minimized.” *

The chancellor, in a painstakingly prepared opinion, analyzed the testimony of each witness. She came to conclusion that “this area is part of Narrin lake and that as a result thereof, plaintiff (plaintiffs) is entitled to riparian rights.” Decree accordingly passed for plaintiffs. Defendants appeal.

First: At conclusion of the proofs the chancellor obtained a small boat and, in company of the court stenographer, rowed over the entire vicinity of dispute. Her log of the voyage fairly records all essential details. It is quite consistent with testimony and finding that the waters extending from plaintiffs’ premises to the deeper part of the lake were and are navigable in fact by small boats and canoes; that the upper as well as lower end of the lake as delineated on exhibit 25 was and is in regular use for boating and fishing purposes; that there is 18 inches of boatable water in the shallowest part of the disputed area in the driest time of year; that *356

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Bluebook (online)
84 N.W.2d 748, 349 Mich. 350, 1957 Mich. LEXIS 347, Counsel Stack Legal Research, https://law.counselstack.com/opinion/kerley-v-wolfe-mich-1957.