Johnson v. Phillips Petroleum Co.

257 S.W.2d 813, 1953 Tex. App. LEXIS 2391
CourtCourt of Appeals of Texas
DecidedFebruary 2, 1953
Docket6276
StatusPublished
Cited by5 cases

This text of 257 S.W.2d 813 (Johnson v. Phillips Petroleum Co.) is published on Counsel Stack Legal Research, covering Court of Appeals of Texas primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Johnson v. Phillips Petroleum Co., 257 S.W.2d 813, 1953 Tex. App. LEXIS 2391 (Tex. Ct. App. 1953).

Opinion

MARTIN, Justice.

Appellant, Neil R. Johnson, is the owner of the North half of the North half of Section 64, Block 46, H & TC Ry. Co. Survey, Hutchinson. County, Texas. Appellee, Phillips Petroleum Company is lessee under an oil and gas lease on this tract of land, a' riparian survey on the Canadian riveri Appellant, the State of Texas, is the owner of the river bed of the Canadian river adjoining said Section 64 and executed an oil and gas lease to appellee, J. M. Pluber Corporation, which lease is in question in this cause as to the boundaries thereof. The respective parties will be known as Johnson, Phillips, Huber and the State.

Johnson presents two points of error on this appeal. His first point alleges the trial court erred in refusing to submit to the jury the issue of the present location of the south bank of the Canadian river "in the vicinity of and where said bank touches Block 46, H & TC Ry. Co. Survey and in dismissing the jury and finding as a matter of law the location of said bank. His second point asserts the court erred in dismissing the jury and holding as a matter of law that the J. M. Huber Corporation’s State lease of a portion of the bed of the Candadian river covers the full width of the river bed north of the present bank where it cuts across Block 46, H & TC Ry. Co. Survey.

Under the points raised by all parties only two issues are involved on this appeal. The first issue to be determined is the correct location of the south bank of the Canadian river. The second issue is whether the State oil and gas- lease to Huber extends to the banks of the Canadian river.

Upon the first issue, the State, Pluber and Phillips assert that the trial court correctly fixed the south bank of the Canadian river at the gradient boundary of the river under- the principles detailed in State of Oklahoma v. State of Texas, 260 U.S. 606, 43 S.Ct. 221, 67 L.Ed. 428. Upon the second issue, the State, as appellant, contends that the State lease to Huber does not extend to the banks of the Canadian river but is bounded by the original lines of survey.

The first issue to be determined in the cause is whether the rules followed in Oklahoma v. Texas, supra,, outlined in an article entitled “The Gradient Boundary,” define a proper method for ascertaining the south bank of the Canadian river. The evidence describing the Red River basin as shown in Oklahoma v. Texas, supra, and the detailed evidence in this cause describing the basin of the Canadian river will not be set forth herein but such evidence, when compared, reveals that the Canadian river basin is practically an exact duplicate of the Red River basin described on page 634 of 260 U.S., on page 225 of 43 S.Ct. in Oklahoma v. Texas, supra. Since *815 the two river beds are identical, the rules for establishing the gradient boundary define the correct, method .of ascertaining the south bank' of the Canadian river at issue in this cause.

Arthur A.' Stiles was one'of the Commissioners appointed by the Supreme Court of the United States to fix the boundary line along the Red River in Oklahoma vl Texas, supra, and the method Stiles and the' Commissioners used in fixing such boundary is clearly described in Vol. 30, Texas Law Review, 305. Stiles entitles his article detailing thé rules for locating a river bank such ás here in issue, “The Gradient Boundary,” and the quotations hereinafter are from such : article. The first and essential step in locating the boundary of the river here in issue is finding what Stiles defines as the “lowest qualified bank.” This bank is .an accretion bank and not a cut bank. ’ After the correct bank has been found a midpoint is “located midway between the lower level of the flowing water that'just reaches the bank and the higher level of, it that just does not overtop the bank.” In this cause, the midpoint a-s established on the lowest qualified bank was 1.4 feet above the level of the flowing water that just reached the bank. “The surface of the flowing water in the river is the datum plane from which the gradient boundary is located upon the ground.” The gradient of the flowing water in the Canadian river, its rate of fall per foot in traveling to the sea, was established at .00106 feet per foot. With these elements established a plane was run from the above midpoint at 1.4 feet on the qualified bank parallel 'with the surface of the flowing water, and the point where such plane touched the' south bank of the river established the gradient boundary line at such' point. “The gradient boundary is located upon the ground exclusively with a level, not.with a transit, compass, chain, or stadia. After it is located and marked, the line may. be meandered in the usual way with the usual instruments.” This boundary line follows the surface of the flowing water in the river. “When .the surface of the flowing water in the river and the elevation of the ...boundary coincide, the bpundary is on the ground at the feather edge of the water, and stakes driven there will mark the .perfect gradient and the perfect boundary.. Hence the name, ‘gradient boundary.’ ”

An examination of the record in the cause here at issue- .reveals that the principles set forth.for determining the gradient boundary were applied in detail to the Canadian River Bed.- Further, the .boundary line of the river was checked as to elevation ..with the surface of the flowing water of’ the river. The principles for establishing the gradient boundary were the correct method of locating the banks of the Canadian river under the ruling of Oklahoma v.' Texas, supra. . Since- the gradient boundary principles were the only correct rules for establishing the boundary of the Canadian river and there was no disputed issue of fact as to the correctness or incorrectness of the application of such rules, there was no evidence of any boundary other than that so established. Therefore, the trial court correctly withdrew the cause from the consideration of the jury and fixed the south bank- of the Canadian river along the gradient boundary shown in the record. State of Oklahoma v. State of Texas, supra; Diversion Lake Club v. Heath, 126 Tex. 129, 86 S.W.2d 441, 446; Motl v. Boyd, 116 Tex. 82, 286 S.W. 458, 467; State v. R. E. Janes Gravel Co., Inc., Tex.Civ.App., 175 S.W.2d 739, 742; Maufrais v. State, 142 Tex. 559, 180 S.W.2d 144.

As to the second point in issue on this appeal concerning the boundaries of the oil and gas lease executed by the State of Texas to J. M. Huber Corporation, the following are the pertinent facts necessary ■to determine the issue: The State admits that the -locative survey on the ground by George Spiller as to Block 46 and establishing the corners of Surveys 60 and 69, was a true meander of the banks of the Canadian river. On March 2, 1919, field notes were prepared covering the Canadian River-Bed Survey No., 4, pursuant to an application theretofore filed by Lulu Ker-micle covering a tract in the Canadian River Bed adjacent to Section 64. On May 7, 1919, an oil and gas permit was issued to'.Lulu Kermicle, pursuant to her *816 application, which permit described the land and contained the statement: “Thence down, the river with is meanders.” ' This permit was relinquished in 1920.

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Bluebook (online)
257 S.W.2d 813, 1953 Tex. App. LEXIS 2391, Counsel Stack Legal Research, https://law.counselstack.com/opinion/johnson-v-phillips-petroleum-co-texapp-1953.