Minton v. Steele

28 S.W. 746, 125 Mo. 181, 1894 Mo. LEXIS 379
CourtSupreme Court of Missouri
DecidedNovember 26, 1894
StatusPublished
Cited by22 cases

This text of 28 S.W. 746 (Minton v. Steele) 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
Minton v. Steele, 28 S.W. 746, 125 Mo. 181, 1894 Mo. LEXIS 379 (Mo. 1894).

Opinion

Barclay, J.

Plaintiff sued the original defendants in ejectment, December 20, 1890, to recover possession of a piece of land in Holt county.

The petition follows the statutory form (R. S. 1889, sec. 4631); but proceeds further to show the nature of plaintiff’s claim to possession. It alleges that plaintiff owns a tract of land adjoining that in controversy. It particularly describes both tracts, and charges that plaintiff’s claim to possession of the latter tract is based on the fact that it is an accretion to the former, which originally abutted upon the Missouri river.

The defendants answered by a general denial.

The cause was tried before Judge Anthony with the aid of a jury.

[188]*188On the plaintiff’s side, testimony was given tending to prove the following facts:

Plaintiff is the owner of land near the Missouri river in Holt county. The tract fronted on the shore for a considerable distance at the time the title passed from the United States government, by patent in 1849. The official survey, on which the entry of the first purchaser was based, represented the river as bounding the land on the west. So it then did, according to all accounts. The river pursued a semicircular course at that point, the effect of which was to give the river line the general shape of a crescent, with the points turned westward. The main land now owned by plaintiff was then near the center of that particular bend or inlet of the stream.

The land of the defendant, Mr. Hinekle, was further north, near the top of the bend.

Since the original survey and settlement of the several tracts now owned by plaintiff and Mr. Hinekle respectively, a large formation of land has taken place in front of them. The old river bend is now completely filled with land, comprising a tract of several hundred acres, extending from the old river line westward to the present bank, more than a mile distant.

The river now follows (or, rather, did follow at the last reports in this record) an irregular, but somewhat semicircular course. The outer side.of the curve was, at last accounts, toward the Kansas side.

The territory involved in this case may be generally described as a strip fronting for some sixteen hundred fee ton the river, and running thence a little northeast to the undisputed Minton estate on the old river bank. The strip is located near the center of a larger tract, all of which is said to have been formed by alluvial deposits in the old river bend.

[189]*189The defendant, Mr. Hinckle, admitted possession of the greater part of the tract, but denied plaintiff’s right thereto.

At the outset of the case, Mr. Steele, a tenant of Mr. Hinckle, was also a defendant; but as he moved away pending the proceedings, the cause was dismissed as to him in the circuit court.

The defendant offered evidence tending to negative plaintiff’s case at several points, and also intended to support a claim for the same property as an accretion upon the defendant’s estate, which lay near the head of the original bend. •

Under instructions to be again mentioned, the jury found for plaintiff for the strip of land sued for, and for damages and monthly rents. The latter items of the verdict were, however, remitted by the plaintiff, leaving the recovery and judgment standing for possession of the property only, and for costs.

From that judgment defendant appealed, after following the usual course to obtain a review.

The defendant’s counsel have advanced several assignments of error.

1. It is first urged that plaintiff should have been forced to a nonsuit by the instruction, which defendant asked, declaring that plaintiff had failed to make out a case. This contention is founded on the idea that the evidence shows that the new- river bank at the place in question, was not formed by gradual accretion.

It is claimed by defendant that a great part of the tract in suit consists of a large sand bar or island in the river, formed while one channel yet ran in front of plaintiff’s land and separated it from the island or bar; and that afterward, when the channel filled and was replaced by solid ground, the river shifted to the western channel, suddenly.

[190]*190The questions, which might arise on the facts just stated, we need not go into at this time. They certainly do not require discussion in connection with defendant’s instruction in the nature of a demurrer to the evidence. Por, on the plaintiff’s side, there was abundant testimony that the disputed land was formed by gradual and impreceptible alluvial deposit upon plaintiff’s original property, if so, he had a proprietary right to the possession, as hereafter more fully indicated.

Where there is substantial evidence to support the plaintiff’s case, the questions of its credibility and weight are for the trial jury and court, in an action of ejectment, such as that now in hand.

2. Defendant complains of the second instruction given for plaintiff, in which, among other things, it is said that if a large part of plaintiff’s original tract on the river bank, as described on the government survey, was first cut away toward the east, and if the jury find “that lands were made back to and against said lands where such other lands- were washed away, then, although a slough may remain against the bank of said river where the washing away of said land ceased, still the plaintiff would be entitled to all his old original lines and corners; and if accretions were by said riveformed against said old lines, after the same were so made back to his said land, then the plaintiff would be entitled to all said accretions, the same as though the original lines of his said lands had never been washed away or changed by said river,” etc.

None of the evidence tended to show that plaintiff’s whole estate on the river bank had been washed away by the movement of the river eastward. Only part of his land was thus swallowed up. Plaintiff still remained proprietor of a large tract on the bank. So that when, afterward, the river receded, and in course [191]*191of time restored what it had formerly taken, to such an extent as to replace the entire land within the lines of the original government survey, and of the description in the patent to plaintiff’s predecessors in title, plaintiff was entitled to reclaim the increase, to the extent of his original possession, even though a slough remained for a time on a part of the land, within the limits of the plaintiff’s former estate.

Whether that claim should properly rest upon the force of the original title, or be referred to the general law of accretion, we are not required to investigate. Under other instructions the jury found as a fact that the accretions in the old bend did not begin at the defendant’s land on the north, and extend in a southeasterly course until opposite plaintiff’s property on the main land.

Other instructions presented squarely the issue whether the accretion in suit was formed upon, and extended from, the land of plaintiff or from that of defendant; and on that issue the jury found - for the plaintiff.

There was evidence to support that finding, and we discover no error prejudicial to defendant in the language of the second instruction, above quoted, as applied to the case before the court.

3.

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Bluebook (online)
28 S.W. 746, 125 Mo. 181, 1894 Mo. LEXIS 379, Counsel Stack Legal Research, https://law.counselstack.com/opinion/minton-v-steele-mo-1894.