Hecker v. Bleish

37 S.W.2d 444, 327 Mo. 377, 1931 Mo. LEXIS 541
CourtSupreme Court of Missouri
DecidedMarch 31, 1931
StatusPublished
Cited by6 cases

This text of 37 S.W.2d 444 (Hecker v. Bleish) is published on Counsel Stack Legal Research, covering Supreme Court of Missouri primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Hecker v. Bleish, 37 S.W.2d 444, 327 Mo. 377, 1931 Mo. LEXIS 541 (Mo. 1931).

Opinions

This is an action in ejectment begun in the Circuit Court of Holt County in 1923. The cause was tried by the court without a jury. The record recites a waiver of a jury by the parties. Judgment was for plaintiff for possession of lands therein described, and defendants appealed. In an able opinion by SEDDON, C., in Division One of this court, adopted as the opinion of the court and reported in 319 Mo. 178, 3 S.W.2d 1008, the cause was reversed and remanded with specific directions to the trial court to ascertain and determine certain boundaries and to enter a corrected judgment for plaintiff in conformity with such finding, which order we hereinafter set out in full. *Page 380

For a proper approach to and disposition of the instant appeal, it is necessary that an understanding be had of the matters and issues involved and finally adjudicated and determined on the first appeal, and to that end we refer to the opinion by Commissioner SEDDON — the following quotations being excerpts therefrom:

"Plaintiff grounds his claim of title and right to possession of the land in controversy upon a patent from Holt County, conveying to him certain `lands of island formation.'

"Plaintiff claims that the land in controversy is a part of made or river-bed land which first formed as an island in the Missouri River, and that the island, by reason of accretions attaching thereto, gradually grew larger, and after a considerable time extended to the east shore line or high bank of the Missouri River, and thereby filled up and closed a channel of the Missouri River which had existed for some years between the island and the east shore line or high bank of the river. Defendants claim, and they sought to show, that no island ever formed or existed in the vicinity of the land in controversy, but that the land in controversy is, and always has been, a distinguishable and integral part of lands which had been owned in fee simple by defendants' predecessors in title since the issuance of a patent therefor by the State of Missouri in 1848 and which had been deeded to defendants, or that the land in controversy had accreted to defendants' deeded lands. Hence, the main issue tried was whether the land in controversy is of island or river-bed formation, or accretion thereto, or whether such land always was an integral, distinguishable and discernible part of defendants' deeded lands.

"The land in controversy, . . . is in the northwest quarter of Section 24, Township 63, Range 41, and embraces all of said quarter section, except a small triangular tract of land in the northeast corner of said quarter section of about one acre in area, to which triangular tract plaintiff apparently concedes in his brief, and conceded on the trial, he makes no claim to possession. This small triangular tract of approximately one acre is bounded on the north by the north line of Section 24, or the boundary line between Atchison and Holt counties, and on the east by the north-and-south center line of Section 24, and the hypotenuse of the triangle, extending from the northwest to the southeast, is variously denominated by the witnesses as the `high bank,' `left high erosion bank,' `east bank,' `old original bank,' and `old erosion bank,' of the Missouri River. But by whatever name it is called by the witnesses, the evidence tends to show that it marks the location of the extreme easterly shore line or bank to which the Missouri River had extended, or cut in, since the Government survey of 1839. . . . According to the testimony of many of the witnesses, the `old high bank' of the Missouri River, which separates or divides the land in controversy from the small triangular corner, *Page 381 is today quite distinguishable, or was at the time of the trial of this cause.

"Plaintiff's evidence tended to show that, about the year 1881, a sand bar or island formed in the bed or channel of the Missouri River, and on the Missouri side of the main river channel; that the island gradually grew larger; . . . that the main or larger channel of the Missouri River ran on the westerly side of the island, and another and smaller channel of the Missouri River ran on the easterly side of the island for several years, thereby separating the island from the `east high erosion bank' or east shore line of the river; that the waters of the easterly channel of the Missouri River flowed with a perceptible current between the island and the `east high erosion bank' until 1891, 1892 or 1893; . . . that thereafter the easterly channel of the Missouri River gradually filled with mud and sediment brought down from the hills and uplands by the Nishnabotna River and by two creeks, known as Rock and Mill creeks, and the sediment was discharged by those streams into the waters of the easterly channel of the Missouri River; that the sediment thus discharged into the waters of the easterly channel of the Missouri River was deposited against the northerly and easterly sides of the island; and that the island formation gradually grew larger and extended toward the east until it completely filled the easterly channel, and eventually became joined to the `old high erosion bank.'

"The trial court, in finding the issues for plaintiff, thereby found the fact to be that the land in controversy was not a part of the original land embraced in the Government survey of 1839, or accretion to such land, . . . and that the land in controversy was remade in the bed or channel of the Missouri River and took form as an island which sprang up in the river bed and which gradually enlarged, by reason of accretion or recession, so as eventually to become joined to the east high erosion bank of the river. Such being the fact as found by the trial court, defendants have no legal title to the land in controversy.

"The main issue tried below was wholly an issue of fact, viz., whether the land in controversy is land of island or river-bed formation and accretion thereto, or otherwise. An examination and analysis of the pleadings discloses, we think, that no equitable issue or defense was tendered by defendants sufficient to convert the action into one in equity, or to make the issue of fact aforesaid exclusively triable by a chancellor. The record indicates that the parties deemed the action, and the issue of fact arising therein, to be triable by a jury, for the recordrecites the waiver of a jury by agreement of the parties. . . . The action was tried by the court, sitting as a jury, without declarations of law asked or given, and without a request for written findings of fact, and the general finding and judgment of the trial court being supported by substantial evidence, such *Page 382 finding and judgment is conclusive upon this court, unless reversible error in the admission or rejection of evidence, or other procedural error, shall appear to have been committed by the trial court.

"The judgment below orders that plaintiff be restored to the premises, which are described in the judgment as `all land of island formation in the northwest quarter of Section 24, Township 63, of Range 41, same being the fractional northwest quarter ofSection 24, Township 63, of Range 41, containing 158.909 acres, more or less,' except two strips of lands, described by metes and bounds, reserved for a public road.

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Cite This Page — Counsel Stack

Bluebook (online)
37 S.W.2d 444, 327 Mo. 377, 1931 Mo. LEXIS 541, Counsel Stack Legal Research, https://law.counselstack.com/opinion/hecker-v-bleish-mo-1931.