State v. Cain

236 A.2d 501, 126 Vt. 463, 1967 Vt. LEXIS 222
CourtSupreme Court of Vermont
DecidedOctober 3, 1967
Docket391
StatusPublished
Cited by15 cases

This text of 236 A.2d 501 (State v. Cain) is published on Counsel Stack Legal Research, covering Supreme Court of Vermont primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
State v. Cain, 236 A.2d 501, 126 Vt. 463, 1967 Vt. LEXIS 222 (Vt. 1967).

Opinion

Smith, J.

The defendants own a tract of land in the Town of Colchester, bounded westerly by Lake Champlain, near to where the water of the Winooski River flows into the lake. In the latter part of 1966, the defendants started to place land fill, in the form of a dike, in that portion of the lake immediately in front of their shore property, with the intention of filling in behind the dike and creating usable land adjacent to the present usable land area owned by them.

*465 The State of Vermont brought an action in the Chittenden County Court of Chancery, alleging that the land fill of the defendants was being placed in the public waters of the State, and seeking an injunction preventing the defendants from proceeding with their operation.

In its complaint, the State stated that the public waters involved were those of Lake Champlain, meaning the waters “beyond and below the low water line thereof.” Upon hearing below, the parties agreed that there was only one material question for the determination of the Chancellor, and such question is set forth in No. 4 of the Findings of Fact: “The parties are in agreement, and the Court finds, that the only material question for the Court’s determination is the fixing from a physical standpoint of the ‘ordinary low water mark’ of Lake Champlain, since this mark, under McBurney v. Young, 67 Vt. 574 [32 A. 492, 29 L.R.A. 539], is the boundary line between the public lands underlying the lake and the riparian lands of the defendants.”

The record below establishes that almost the entire evidence of both parties was directed toward defining and establishing the “ordinary low water mark” of Lake Champlain. The Chancellor did not adopt the definition or the physical “average low water mark” advocated by either party. Proceeding on a computation of his own devising, the Chancellor found the “average of the lowest levels reached by Lake Champlain” to be 93.417 feet above mean sea level. (F. 9.)

The concluding finding of the Chancellor was that he “was unable to find that the defendants have placed any land fill in the public waters of the state (i.e., Lake Champlain) or are threatening to do so, or that they have committed, or threaten to commit, trespass or public nuisance upon lands of the State.”

In its appeal here, the State has briefed its exception .to Finding 9, on the ground that the Chancellor did not find the “average low water mark” of the lake, the question for determination, by his finding of the “average of the lowest levels reached by Lake Champlain,” as well as to the negative finding (F. 10) that the defendants had placed no fill in public waters, or trespassed upon lands of the State.

But the real relief here sought by the State is a remand of the whole cause for a new hearing on the ground that the key question in the cause was never reached by the parties, or the Chancellor, in the hearing below. The key question that should have been considered, now alleges the State, is the right of the public to use the overlying waters of Lake Champlain, regardless of the ownership of the bed of the lake under such waters.

*466 We first turn to the exceptions of the State to the Findings of Fact to ascertain if this cause must be remanded in any event before considering the other relief here sought by the appellant.

The Chancellor did not, at least in so many words, ever determine the sole question for his determination below, which was the “fixing from a physical standpoint, of the ‘ordinary low water mark’ of Lake Champlain.” He did determine the average of the lowest levels reached by Lake Champlain in a 37-year period was 93.417 fee.t above mean sea level. This figure was computed by taking the lowest water level reached by the lake in each year, and dividing the figure reached by the 37. It should be noted that drought years were not included in the computations of the Chancellor, or in those of either party.

The defendants contended that ordinary low water mark meant the lowest elevation point to which the lake had receded during the years examined (excluding drought years) and submitted a figure of 92.60 as the average low water mark of the lake.

The State contended that the term “ordinary low water mark” meant the low water level representing the arithmetic mean or average of all the daily water level readings below the mean lake level, as recorded over a period of years. The record discloses that this method of computation is the one used by both the State of New York, and the Commissioner of Water Resources for the State of Vermont in determining the ordinary low water level of Lake Champlain. The Chancellor found that in the use of this method of computation the ordinary low water level of the lake would be 94.32 feet above mean sea level; a point higher than the toe elevation of the dike of the defendants which the Chancellor found to be 93.75 feet above sea level.

In employing the phrase “ordinary low water mark” in McBurney v. Young, supra, this Court did not explicitly define the term used. The Supreme Judicial Court of Massachusetts was called upon to define this term in East Boston Co. v. Commonwealth, 203 Mass. 68, 89 N.E. 236, at p. 237. While the factual question before the Massachusetts court was as to the meaning of “ordinary low water mark” as applied to land abutting on salt water, we believe it to be equally applicable to the question presented here.

“The quoted words suggest at once a distinction between the line indicated and absolute low-water mark, or extreme low-water mark. The language is ‘ordinary’ low-water mark, which seems to imply that there is some recognized line to which the tide *467 usually ebbs. But the evidence shows that this is not the fact. The line of low water, like the line of the high water, is gradually and constantly changing from day to day in different parts of the month, and in different parts of the year, from the highest spring tides to the lowest neap tides. If the distinction intended is between the extreme low-water mark and the ordinary or common line of low water, having reference to all times, and all seasons, the only way of reaching a correct result is to take the average of the low tides, which gives us the line of mean low water.”

The opinion also states that the word “ordinary” when applied to a high or low water mark, has generally been used in the sense of average in the courts of this country, and of England.

Lake Champlain is not subject to tidal action as in the case of the sea, but the evidence in the record below is undisputed that there is an almost daily variation in the level of the lake, and the reasoning above given is applicable. The Chancellor, in selecting the intermittent lowest levels over the 37-year period, ignored the ordinary mean low water mark in favor of the extraordinary low water levels, excluding drought years. This was in error.

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Bluebook (online)
236 A.2d 501, 126 Vt. 463, 1967 Vt. LEXIS 222, Counsel Stack Legal Research, https://law.counselstack.com/opinion/state-v-cain-vt-1967.