King v. Muller

67 A. 380, 73 N.J. Eq. 32, 3 Buchanan 32, 1907 N.J. Ch. LEXIS 57
CourtNew Jersey Court of Chancery
DecidedJune 27, 1907
StatusPublished
Cited by3 cases

This text of 67 A. 380 (King v. Muller) is published on Counsel Stack Legal Research, covering New Jersey Court of Chancery primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
King v. Muller, 67 A. 380, 73 N.J. Eq. 32, 3 Buchanan 32, 1907 N.J. Ch. LEXIS 57 (N.J. Ct. App. 1907).

Opinion

Pitney, Advisory Master.

The questions involved in this cause are important and have been argued on each side with great ability and industry.

The case is developed by bill, answer and affidavits and exhibits on each side. ■

The original order, with restraint, in the cause was made on the 15th day of September, 1906, and the parties seem to have been sufficiently industrious in collecting ex parte affidavits on each side and producing records, maps, &c., so that at the hearing it was not suggested that the case could be seriously changed by a final hearing.

[34]*34The complainants5 - bill sets forth title to certain lands, and on its presentation there was exhibited record evidence of such title. The defendant, by his answer, formally denied the title, but set up none on his part adverse thereto, and at the hearing I understood counsel for the defendant to substantially admit the title as asserted by the complainants, and to rest his case on other grounds.

The object of the bill is to restrain the defendant from navigating, with a passenger power boat, a certain channel or canal about thirty feet in width and three thousand feet in length, created by the complainants in a shallow arm or bay of Lake Hopatcong, and leading from what may be termed the main body of the lake to a point in the most southeasterly portion of its waters, including the arm, near Hopatcong station, on the Delaware, Lackawanna and Western railroad.

Lake Hopatcong is a -natural lake enlarged by a dam or dams built at various times across its outlet, by which its waters have been raised until it has attained its present size. It is quite irregular in shape, but much longer than it is wide, and in its deeper portions so deep as to indicate what is sustained by tradition that there was in its central portion at one time a natural lake. It lies just to the west of the high mountain ridge, which at that point divides the watersheds of the Delaware and the Raritan rivers at the southerly end of the lake, and those of the Delaware and the Rockaway rivers on the north end of it.

The lake is fed at its upper end by a small brook, and its outlet is the Musconetcong river, leading to the Delaware river.

A short distance south of its natural outlet there is a natural depression, or pass, in this high mountain ridge at an elevation of about nine hundred and ten feet above the sea, and about fifteen or twenty feet below the level of the lake when it is full, which is nine hundred and twenty-six feet above tide level. Through this pass the Morris canal was located and built about the year 1830-1831. By building a navigable feeder from the natural outlet of the lake along that level to the level of this pass the water of the lake is let into a level of the canal at that point, which is about fifteen feet lower than the level of the lake at high water, and from thence the water may be turned, [35]*35and in point of fact is turned each way in the canal to the waters of the Delaware on the west and to the Hudson on the east.

When the canal was laid out and built, a dam, called the “Bandolph dam,” already existed at the outlet of the lake, and was used to drive a forge.

The name of that place was Brooklyn, and the pond itself was known as “Brooklyn pond,” or, as expressed in the charter of the canal company, the “Great pond,” as well as “Lake Hopatcong.”

The canal company, by its charter, was obliged to file in the clerk’s office of the various counties through which it passed maps showing the amount and description of the lands intended to be taken or flowed by it in that county.

The map showing the land to be taken in the neighborhood of Lake Hopatcong is still in existence, in the clerk’s office of Morris county, and was used, by consent, at the hearing. That map shows the extent of the flow at the time the company made its survey, and the extent to which the flow of the land around the lake was to be increased by its dam. It showed a very little increase of flowage in any direction. Its importance in this connection is that it shows that at what was then the most southerly part of the lake and about five-eighths of a mile southeast of the outlet, there was a causeway by the water’s edge over which passed a mountain road running along the easterly side of the lake, and around what was then the southwesterly end of the lake to the outlet at Brooklyn. The remains of that causeway are still in existence, as shown by the map made for the purpose of this hearing, and proven by abundance of affidavits and not disputed by anyone on the part of the defendant. South of that causeway the canal company’s map shows no flowage, and the canal company did not claim that it desired to acquire the right to flow south of that causeway.

The well-known object of the canal company was to create ■a reservoir for the storage of water to be used in the operation of its canal during the dry season.

The evidence shows that in point of fact there was no flowage ■at that time south of that causeway. But there was a swamp .about three thousand feet long and from two hundred to five [36]*36hundred feet wide, called the “cedar” or “spruce” swamp, leading in a southerly direction from this causeway and at right angles to the general course of the lake and river, and reaching- to the very edge of the pass or depression in the mountain before mentioned.

Immediately to the south of this swamp the land begins to fall off in a southerly direction toward the headwaters of a branch of the Raritan river, and a small stream rose there leading- down ultimately to that river. No stream or brooklet was running through this swamp.

Later on, and in or about the year 1836, the canal company, finding the storage furnished by the dam and lake, as completed in or about 1830, not sufficient to supply its boats in dry seasons in August and September, raised the dam several feet higher. This raising was proven by one of the old witnesses in this case called by the defendant. The result of this raising was that the causeway before mentioned was flooded with water in the spring of the year and produced the litigation reported in the case of Seward v. Morris Canal and Banking Co., 23 N. J. Law (3 Zab.) 219. (That cause related to land at the northerly end of the lake and was tried twice. The first trial resulted in a verdict for the defendant and was set aside by the supreme court, as against the weight of the evidence. On the second trial a verdict was rendered for the plaintiff, which was sustained by the court on a rule to show cause, as reported, where the reporter has reversed the position of the counsel.)

With the flooding of the causeway before mentioned at the south end the whole cedar swamp was flooded, and the apparent area of the lake increased, and it is laid out on the maps as being an extension or arm of the lake running to the southward.

The road, which formerly crossed the causeway and led to and from Brooklyn, was abandoned at that point, and a substitute road was constructed around this arm and along the southerly bank of it, and so on northwardly to the outlet.

The water stood, according to the evidence, between the trees of this arm, or bay, about three feet deep at high water, but the [37]*37trees were so thick that it was scarcely navigable, even by small rowboats.

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Bluebook (online)
67 A. 380, 73 N.J. Eq. 32, 3 Buchanan 32, 1907 N.J. Ch. LEXIS 57, Counsel Stack Legal Research, https://law.counselstack.com/opinion/king-v-muller-njch-1907.