Ozark-Mahoning Co. v. State

37 N.W.2d 488, 76 N.D. 464, 1949 N.D. LEXIS 67
CourtNorth Dakota Supreme Court
DecidedApril 26, 1949
DocketFile 7112
StatusPublished
Cited by14 cases

This text of 37 N.W.2d 488 (Ozark-Mahoning Co. v. State) is published on Counsel Stack Legal Research, covering North Dakota Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Ozark-Mahoning Co. v. State, 37 N.W.2d 488, 76 N.D. 464, 1949 N.D. LEXIS 67 (N.D. 1949).

Opinion

Nuessle, Ch. J.

This is a statutory action, see Chapter 32, Rev Code ND 1943, to quiet title to the bed of Grenora Lake No. 2, hereinafter referred to as Grenora Lake. The case was tried to the court. The court found for the plaintiff. Judgment was entered accordingly whereupon the State, the defendant herein, perfected the instant appeal and demands a trial de novo.

Grenora Lake is one of a chain of lakes in Divide County in the northwestern corner of North Dakota. These lakes lie along a depression that probably was a part of the pre-glacial valley of either the Missouri River or the Yellowstone River when those streams emptied into Hudson Bay. The lake is of irregular shape with an area of a little more than a square mile. Its waters are malodorous and are unfit for use by man, beast, fish or fowl, though aquatic birds sometimes rest on its surface. Its bed is level and consists of a permanent solid body of sodium sulphate varying in thickness from two to eighty feet with an average thickness of twelve feet and containing an estimated eleven million tons of sodium sulphate. The lake is nearly surrounded by a quagmiry mud flat .of a character such as to make access to it difficult. No vegetation grows in it nor are there any trees or brush around it. It lies in a little valley or pocket wholly surrounded by hills and has neither inlet nor outlet. Its waters are derived from precipitation, from run-off from the hills and from numerous springs flowing from its bed as well as out of the mud flat. The water, as it flows from some of these springs, is clear and potable but that from others is somewhat impregnated with sodium sulphate. Ordinarily evaporation is greater than the sum of the waters from the various sources above mentioned. Through the course of thousands of years the mineral content of the spring-water has been deposited thus forming the bed of sodium sulphate. In the spring of the year when the run-off is heavy or when there is exceptional precipation the water level may reach a height of as much as a foot or two above the bed of the lake. In times of drouth or late in the summer season the surface water is greatly diminished *467 so that there are only occasional pools here and there, while other parts of the lake are covered with a slushy saturated solution of sodium sulphate and mud, varying from an inch to a foot in depth.

North Dakota was admitted to the Union as a state in 1889. At that time the public domain in the northwestern part of North Dakota had not been surveyed. That portion thereof wherein G-renora Lake lies was surveyed in June 1898 and this survey was approved by the Surveyor General in 1899. The lake was meandered. The fractional portions of the surrounding sections (Section 4, Township 159, 103, and Sections 28, 29, 32, 33, and 34, Township 160, 103) created by the meander lines were designated as lots and numbered in the manner usually followed by surveyors in such cases. Thereafter these lots were patented and ultimately the plaintiff purchased them from the patentees or their grantees, acquiring all but two. The patents contained no mineral or other reservations or restrictions. As owner of the lots plaintiff, as a riparian owner, now claims title to practically all of the bed of the lake. The state on the other hand denies this claim and asserts ownership in itself on the ground that the lake was navigable when North Dakota was admitted to the Union, when the survey by the government was made, and when the patents through which the plaintiff derives its title were issued.

There are many cases in the books dealing with the questions the answers to which are vital to the determination of the instant case. The case of United States v. Oregon, 295 US 1, 79 L ed 1267, 55 S Ct 610, decided April 1, 1935, in an exhaustive opinion states the rules which determine many of the questions here involved. In that case the court said that,

“Upon the admission of a state to the Union, the title of the United States to lands underlying navigable waters within the state passes to it, as incident to the transfer to the state of local sovereignty, and is subject only to the paramount power of the United States to control such waters for purposes of navigation in interstate and foreign commerce.”

Consistent with what is there said we have held to the same effect. See Roberts v. Taylor, 47 ND 146, 181 NW 622; State *468 v. Loy, 74 ND 182, 22 NW2d 668; State v. Brace, 76 ND 314, 36 NW2d 330 and cases cited. The Oregon case further holds that if waters in a state are not navigable in fact at the time of its creation the title of the United States to lands underlying them remains unaffected and whether such waters are navigable is a federal question to be determined according to the law and usage recognized in the federal courts.

We have heretofore stated the salient facts established by the record respecting Grenora Lake at the present time. There is nothing in the record to indicate that there is any particular difference between the general character and condition of the lake now and its character and condition when the state was admitted into the Union or at the time when the survey was made in 1898 and the meander lines about it were run by the surveyors. The lake has neither inlet nor outlet. Its bed is solid and practically level throughout its whole extent. The annual increment to the deposit of the mineral 'in its bed must have been insignificant throughout the centuries. It cannot he believed that the thickness of the sodium sulphate deposit has increased to any appreciable extent during the time since the state was admitted into the Union. There is no evidence that any use ever has been or could he made of the waters of the lake either for pleasure or for profit, for travel, or for trade. No boats were used thereon. The water at all times has been of such a character that it was not habitable for fish. Neither the lake nor its surroundings are suitable for any purposes of pleasure. It is true that aquatic birds sometimes rested on its surface and there is evidence that hunters occasionally shot waterfowl that flew to or from the lake, hut this was an infrequent occurrence. On these facts, measured by the federal rule as to navigability it is certain that the lake was not navigable in fact at the time of the admission of the state into the Union or at the time the lands abutting on its meander lines were patented. See United States v. Oregon (US) supra, and the numerous authorities cited therein. Accordingly the title to the land under the waters of Lake Grenora did not pass to the State of North Dakota when it was admitted into the Union, hut remained in the United States subject t.o such disposition *469 as the latter might see fit to make of it. And while the test as to navigability applied in North Dakota is not as narrow as that in the federal courts, nevertheless, considering the record in the light of the tests determining navigability heretofore adopted and applied by our own court, we can come to no other conclusion than that the lake is not now and was not navigable either at the time North Dakota was admitted into the Union or at the time when the land surrounding the lake was patented by the United States. See Brignall v. Hannah, 34 ND 174, 157 NW 1042; Roberts v. Taylor, 47 ND 146, 181 NW 622, supra; State v. Brace, 76 ND 314, 36 NW2d 330, supra.

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Bluebook (online)
37 N.W.2d 488, 76 N.D. 464, 1949 N.D. LEXIS 67, Counsel Stack Legal Research, https://law.counselstack.com/opinion/ozark-mahoning-co-v-state-nd-1949.