George T. Houston, III and Ruth H. Jarvis Baker v. United States Gypsum Company, a Corporation

569 F.2d 880, 1978 U.S. App. LEXIS 12135
CourtCourt of Appeals for the Fifth Circuit
DecidedMarch 16, 1978
Docket76-2988
StatusPublished
Cited by3 cases

This text of 569 F.2d 880 (George T. Houston, III and Ruth H. Jarvis Baker v. United States Gypsum Company, a Corporation) is published on Counsel Stack Legal Research, covering Court of Appeals for the Fifth Circuit primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
George T. Houston, III and Ruth H. Jarvis Baker v. United States Gypsum Company, a Corporation, 569 F.2d 880, 1978 U.S. App. LEXIS 12135 (5th Cir. 1978).

Opinion

COLEMAN, Circuit Judge.

What happens when an unstoppable force collides with an immovable object? In this case the unstoppable force is the never ending, often shifting, accretive processes of the Mississippi River. The immovable object is the boundary line of privately owned land in the bed of the river. 1 After an extended Bench trial, which accumulated a voluminous record, judgment went for the owner of the river bed. This appeal followed. We affirm the Judgment of the District Court as to the riparian ownership of the tract in dispute. We vacate the remand on the issue of adverse possession.

The facts are not in dispute. The parties agree that the common law of Mississippi governs the outcome. The question is, what does the common law of Mississippi require in such a situation?

We begin with “Stack Island” in the Mississippi River, so identified in the original 1826 United States Land Survey (platted as “Island No. 94” by the government in 1881). The government patented the island to a private purchaser in 1888. As successors in the chain of title, the Houstons have owned the island since 1934. The island, and the accretions at issue, are on the west side of the main river channel, across the channel from the dry land owned by Gypsum on the east bank. Consequently, the island and its accretions do not interfere with Gypsum’s access to the main channel.

Since 1950 Gypsum has owned a tract of land in Issaquena County on the east bank of, and riparian to, the main channel. The 1950 conveyance to Gypsum included “all accretions and batture lands adjoining or any way connected with above described land . . . and any islands located between the above described lands [and] the Louisiana-Mississippi state line”. 2

Gypsum lays no claim to Stack Island accretions situated north of its boundary line as extended from the river bank westerly across the river to the middle or thread of the stream of the old river. Gypsum says, however, that when the Stack Island accretions advanced downriver and crossed that north (extended) line, the dry land thereafter accreting became its property.

It is shown by the evidence that over a period of many years, particularly from *882 1913 to 1925, the Mississippi River by its meanderings and avulsive actions developed the following situation:

(a) The Louisiana-Mississippi state line became permanently fixed west of Stack Island near the Louisiana shore along the line described in the Bill of Complaint as shown by various exhibits to the testimony of Mr. Austin Smith, river expert;

(b) All lands which had formerly once developed as accretions southward from Stack Island before 1925, and all remnants of any accretions from the Mississippi mainland west of the navigation channel prior to 1925 were wiped out and washed away by the river in a gradual process of erosion;

(c) After 1913, the main channel of the River has constantly remained east of Stack Island (and its downstream extensions), that is, between Stack Island as extended and the Mississippi mainland shore;

(d) After 1925, Stack Island proper, which remained intact, began a completely new process of building up southward, downstream, on the west side of the main channel which separated the island and its lengthwise accretions from the Mississippi riparian mainland;

(e) The southward growth of Stack Island west of the main channel continued downstream considerably beyond the westward extension of the north line of the Gypsum property on the Mississippi shore;

(f) No part of Stack Island as extended after 1925 formed between the main channel and the Mississippi riparian shore. Its total growth as now constituted is southward from the island and on the west side of the main channel;

(g) By 1950, Stack Island had grown southward downstream west of the main channel so as to include virtually all of the land here in controversy;

(h) The identity and unity of Stack Island as extended has been officially recognized and maintained by U. S. Government navigation and hydrographic maps designating the entire growth as Stack Island;

(i) The downriver extension of Stack Island west of the navigation channel has not blocked or excluded Gypsum or any other riparian owner on the Mississippi shore (east bank) from access to the river channel;

(j) Gypsum lands have riparian access to the river channel for the entire length of the Gypsum property.

The respective rights of adjacent riparian owners have collided.

The Houstons contend that they own the Stack Island accretions, regardless of how far south they may run, so long as they do not cross into the territory of another sovereignty.

Gypsum responds that when the accretions 3 crossed its northern boundary, as extended westerly from the east bank, the dry land so created passed out of the ownership of the Houstons and became its property. The District Court agreed.

The Applicable Law

It has been held that “The right of accretion to an Island in the river cannot be extended lengthwise of the river as to exclude riparian properties above or below such island from access to the river”, City of St. Louis v. Rutz, 138 U.S. 226, 11 S.Ct. 337, 34 L.Ed. 941 (1891). In the present case, however, the downstream accretions to Stack Island do not affect Gypsum’s access to the main channel of the Mississippi.

In City of St. Louis v. Rutz, supra, it was further held:

It is laid down by all the authorities, that, if an island or dry land forms upon that part of the bed of a river which is owned in fee by the ripárian proprietor, the same is the property of such riparian proprietor. He retains the title to the land previously owned by him with the new deposits thereon. *883 138 U.S. at 245, 11 S.Ct. at 344. In the Fifth Circuit, in a Texas case, it has been said that “[I]f an island arises in navigable inland waters ... it belongs to the owner of the bed of the water”, Humble Oil and Refining Co. v. Sun Oil Co., 5 Cir. 1951, 190 F.2d 191, 196. 4

Compared to the present litigation these cases are not factually squarely in point because we are not dealing with an island recently formed but with the accretions to an island which has been there all the time. We think, however, that we should not minimize the significance of the Rutz language to the effect that if “dry land forms upon that part of the bed of a river which is owned in fee by the riparian proprietor . he retains title to the land previously owned by him with the deposits thereon (emphasis added)”.

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Bluebook (online)
569 F.2d 880, 1978 U.S. App. LEXIS 12135, Counsel Stack Legal Research, https://law.counselstack.com/opinion/george-t-houston-iii-and-ruth-h-jarvis-baker-v-united-states-gypsum-ca5-1978.