Johnson v. McMahan

15 S.W.2d 1023, 118 Tex. 633
CourtTexas Supreme Court
DecidedJanuary 22, 1930
DocketNo. 5250.
StatusPublished
Cited by10 cases

This text of 15 S.W.2d 1023 (Johnson v. McMahan) is published on Counsel Stack Legal Research, covering Texas Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Johnson v. McMahan, 15 S.W.2d 1023, 118 Tex. 633 (Tex. 1930).

Opinion

Mr. Presiding Judge SHORT

delivered the opinion of the Commission of Appeals, Section B.

The following statement and questions based thereon from the Court of Civil Appeals for the Seventh District have been filed with the Supreme Court and referred to this Section of the Commission for disposition:

This appeal is prosecuted from a judgment in the District Court of Dickens County, perpetuating, after a hearing on the merits, a temporary injunction theretofore granted, restraining W. A. Johnson and W. P. T. Smith, the Appellants, from draining a lake located on Johnson’s land into what is known as Hackberry Draw, which crosses the farm on the land of Appellee, Mrs. O. C. McMahon.

The record shows that W. A. Johnson owns the S. W. J/\ of Survey No. 297 and a strip of land extending along the west side of Survey No. 284 from its northwest corner to Hackberry Draw. That W. P. T. Smith owns all of the west J2 of Survey No. 284 except the strip thereof owned by Johnson; that the Appellee owns the S. 105 acres of the S. E. % of Survey No. 284 and the N. 60 acres of the N. W. J4 of the Survey No. 259, which two tracts constitute one body of land. Survey No. 259 is immediately south of Survey No. 284, and No. 284 is immediately south of Survey No. 297. That Dry Lake covers approximately 160 acres of land, 120 acres of which is in the N. W. % of Survey No. 297; that the land is 2.7 feet deep in the center, is a natural basin into which the water falling on eight or ten square miles of territory lying north, northeast and northwest of the lake drains; that water stands in the lake from one-third to one-half of the time and on several occasions it has remained full for many consecutive months; that when the lake overflows from excessive rains, the overflow passes out near the southeast corner and meanders through a natural depression on the east part of the northwest quarter of Survey No. 284 and reaches Hackberry Draw and through it flows onto and over the land of Appellee. Hackberry Draw is some eleven miles in length, runs in a southeasterly direction, crosses Survey No. 296, which is immediately west of Survey No. 297, runs over the S. W. % of Survey No. 284 and enters Appellee’s land on the west, spreads out over *638 her farm and finally flows into Dockum Creek. Dockum Creek roughly parallels the course of Hackberry Draw to near the point of their confluence. Hackberry Draw is a drain or depression through which water flows, but is dry except while it is raining and immediately thereafter. Its width across Appellee’s land varies from 100 feet to 60 feet and it is about 2y2 feet deep in the center with a natural slope to either side. It runs down in a few hours after a rain and many of the farmers through whose land it passes cultivate the land in the draw, plow across it and grow farm products therein, as the soil is sub-irrigated and very productive. During excessive rains Dockum Creek occasionally overflows into Hackberry Draw and said overflows into Dry Lake and on the north and east of- said lake there are other natural ponds or basins that overflow into Dry Lake; but, independent of such overflow water, Dry Lake is a natural basin into which the rainfall on some eight or ten square miles of territory, drains. The soil in Dry Lake is sub-irrigated, fertile and would be susceptible of cultivation and very productive, if drained.

W. A. Johnson was digging, and if he had not been enjoined, would have completed a ditch from the southwest part of Dry Lake on his S. W. °f Survey No. 297 to and along his strip of land on the west side of Survey No. 284 to where it would empty into Hackberry Draw. The length of the ditch if completed, would be 4,434 feet and its average depth 8 or 9 feet with a width of 6 feet at the bottom and 10 feet at the top. The natural drainage for the lake when it overflows is about one-half mile east of the proposed ditch. The proposed ditch would drain the water from Dry Lake and empty it into Hackberry Draw and thence onto some of the cultivated lands of the Appellee. It would materially increase the amount of water that flows over Appellee’s land under natural conditions, cause water to flow over her land that would not do so without the ditch, would cause the water to flow longer and stand longer on her land than it would without the ditch and increase the acreage overflowed under natural conditions; all of which would result in injury to -Appellee’s cultivated lands, wash away the soil, damage her crop and destroy her alfalfa field.

W. A. Johnson had never sought Appellee’s permission to drain the lake into Hackberry Draw, but he pleaded and testified that he intended to put a flood gate in the ditch for the purpose of holding the water in the lake until the water from natural rainfall and other sources passed out of Hackberry Draw.

*639 We attach hereto a map used before this Court in the oral argument by counsel for both Appellants and Appellee.

Appellants insist that they are not prohibited by Articles 7589, 7589a and 7590, R. C. S., from draining Dry Lake by the proposed ditch into Hackberry Draw and are not liable for damages that will be sustained by Appellee on account of the increased flow to which Appellee’s land will be subjected, so long as Appellants are guilty of no negligence.

In as much as the decision of the case requires a construction of said articles of the statutes and a determination of the legal liability of Appellants for the damage that will be inflicted on Appellee, we deem it advisable to certify to your Honorable Court for decision, the following questions:

“1. Is the Appellant, W. A. Johnson, prohibited by said statutes, or either of them, from draining said lake, by means of the ditch, into Hackberry Draw, which is a natural drain?

2. Is W. A. Johnson liable for the damages that will result to Appellee by the increased acreage overflowed by the water drained from the lake by the proposed ditch?”

We think both questions propounded should be answered in the negative. The map attached to the certificates shows Dockum Creek and Hackberry Draw to be well defined water courses running parallel with each other, in a general way, having their origin at the foot of the plains and forming a junction to the south of the lands mentioned in the certificate. Dry Lake, so called, is in the watershed of and to the east of Hackberry Draw. Dockum Creek lies west of Hackberry Draw. The depression in the lands of the Appellant, Johnson, designated as Dry Lake, covers from 120 to 150 acres of his quarter section, the deepest part of which depression is 2 feet and 7 inches. The surface and flood water flowing across this land would naturally empty into the water course, designated upon the map as Hackberry Draw, shown to be a well-defined channel having its origin at the foot of the plains and running to its junction with Dockum Creek for a distance of about 11 miles. It is shown that Dockum Creek contains a stream of flowing water the year around, but that Hackberry Draw only has water in it when a sufficient amount of rainfall has occurred to concentrate from its water-shed an amount of water sufficient to create a flow. In times of flood the natural banks of Hackberry Draw overflow occasionally, but unless the flood waters are unusually large, its natural banks are sufficient to confine the waters between them.

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Bluebook (online)
15 S.W.2d 1023, 118 Tex. 633, Counsel Stack Legal Research, https://law.counselstack.com/opinion/johnson-v-mcmahan-tex-1930.