Adkisson v. Starr

260 S.W.2d 956, 222 Ark. 331
CourtSupreme Court of Arkansas
DecidedOctober 19, 1953
Docket5-132
StatusPublished
Cited by7 cases

This text of 260 S.W.2d 956 (Adkisson v. Starr) is published on Counsel Stack Legal Research, covering Supreme Court of Arkansas primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Adkisson v. Starr, 260 S.W.2d 956, 222 Ark. 331 (Ark. 1953).

Opinion

George Rose Smith, J.

This is a suit between adjoining riparian landowners to obtain a division of about 1,200 acres of land that was formed by accretion as the channel of the Arkansas River gradually shifted westward. The appellants, defendants below, and their predecessors in title have long owned riparian land (referred to as the Adkisson place) in Section 13, Township 3 North, Range 14 West. The appellee and his predecessors have owned the adjoining farm to the south, known as the Rector place and lying in Sections 24, 25, and 36. The recession of the river over a period of more than fifty years exposed the lands now in dispute, which lie directly west of the original farms. The chancellor divided the new land by extending the common boundary (the south line of Section 13, which is also the north line of Section 24) due west across the area in controversy. The appellants contend that all the disputed acreage became their property by accretion, or, if it did not, that they have acquired title by adverse possession.

The voluminous record gives a pretty complete history of the shifting of the river in this vicinity. When the United States finished its survey in 1856 the river flowed southward through the four sections mentioned above, so that each section was then fractional. Apparently the river had long occupied this bed, for on the east its bank was so high that it is sometimes called a bluff.

The next survey, made in 1900, shows that the river had begun to move westward. This plat reveals an extensive sandbar on the east side of the river in Sections 13 and 24, indicating that the river’s movement to the west began in those sections. According to this survey Palarm Creek, which is an important factor in this litigation, came down from the northeast, crossed the sandbar, and emptied into the river at about the center of Section 13, which is part of the Adkisson place.

As this segment of the river continued to shift to the west Palarm Creek did not extend its channel in a direct line to reach the river. Instead, at some time not fixed by the proof the creek turned southward in Section 13 and flowed parallel to the river for two or three miles before joining the river some miles below the original mouth of the creek. In so paralleling the larger stream the creek for the most part followed the old river bed, but in doing so it left a strip of accreted land between the creek bed and the bluff bank on the east. The lands now in dispute comprise a long Y-shaped peninsula bounded on the north by the Adkisson place, on the west by the Arkansas River, and on the east by Palarm Creek, with the Rector place lying on the east side of the creek in the lower three of the sections mentioned.

As a preliminary matter a jurisdictional question was raised in the oral argument, although it is not urged 'in the briefs. All the land actually in dispute lies in Faulkner County, since in this vicinity the line between that county and Pulaski County runs down the river to the mouth of Palarm Creek and thence up that creek, with the land between the two streams being a part of Faulkner County. Act 59 of 1875, Adjourned Session. Although part of the disputed land lay in Pulaski County before the river shifted to the west, the rule is that a boundary line defined by a watercourse follows a gradual change in the course of the stream, though the boundary is not affected by a sudden avulsion. DeLoney v. State, 88 Ark. 311, 115 S. W. 138.

Nevertheless we think the Pulaski Chancery Court had jurisdiction, for the complaint also asked the court to apportion the narrow band of accretion lying between Palarm Creek and the bluff bank. That strip is east of the creek and is therefore in Pulaski County. It happens that the defendants concede the plaintiff’s title to this strip, and perhaps the defendants could have disclaimed ownership of the Pulaski County land and insisted that the real controversy be tried in Faulkner County. But the defendants acquiesced in the plaintiff’s choice of the forum, and the decree has the effect of awarding the Pulaski County land to the appellee. It follows that the suit involves the title to land in both counties; so the venue may be laid in either county. Ark. Stats., 1947, § 27-601.

On the merits the appellants first contend that the disputed acreage accreted entirely to their land in Section 13. This argument is based on the fact that the original Rector place lay entirely east of Palarm Creek and is now separated by that stream from the land in controversy. The Adkisson place, on the other hand, lay on both sides of the creek to the north, and it is therefore argued that the appellants ’ ownership extended southward and westward as the recession of the river built up land between the two watercourses.

This identical argument was rejected in Dowdle v. Wheeler, 76 Ark. 529, 89 S. W. 1002, 113 Am. St. Rep. 106. There, as here, a river had slowly shifted away from adjoining littoral properties, and later on a smaller stream occupied the old river bed and blocked Mrs. Wheeler’s access to the accretion that lay in front of her property. In upholding Mrs. Wheeler’s title we stressed the fact that a narrow strip of the accretion lay between her property and the creek. “This goes to show that there was a deposit against the shore line before the waters of the river receded, that this process continued until the bed of the river rose to the level of the creek’s bed, and that then, as the waters of the river receded, the flow from the creek prevented further deposits in its extended channel, and established a permanent channel along the old bed of the river.”

On its material facts this case cannot be distinguished from that one. The 1900 plat shows that Palarm Creek then entered the river in Section 13, but a sandbar had already begun to build up along the shore of the Rector place. Witness after witness confirmed the existence of accreted land between the creek’s new bed and the old bluff bank. Aerial photographs put the matter wholly beyond controversy. We can think of no reasonable theory to account for this physical situation except that advanced in the DeLoney case, to the effect that the river first left a shelf of accretion against the appellee’s property and that later Palarm Creek turned southward and established a new channel on that shelf. It is necessarily true that the new channel was bounded on both sides by accretions already a part of Rector place, and for that reason all later accretions to the west also became a part of the appellee’s property.

A much more difficult question is presented by the appellants’ proof of adverse possession. Except in rare seasons of extreme drought Palarm Creek is a formidable barrier that cannot be conveniently crossed without a boat. Hence the appellee has been cut off almost continuously from his part of the land in dispute, the only access having been from the Adkisson place to the north. Hence about the only dominion that has been exercised over the newly formed acreage has been that of the appellants and their predecessors. We agree with the chancellor, however, in thinking that the proof does not show sufficient acts of ownership to work an investiture of title in the appellants.

The claim of adverse possession rests mainly upon the assertion that the owners of the Adkisson place have long maintained a fence on their side of Palarm Creek.

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Bluebook (online)
260 S.W.2d 956, 222 Ark. 331, Counsel Stack Legal Research, https://law.counselstack.com/opinion/adkisson-v-starr-ark-1953.