Morton v. Oregon Short Line Ry. Co.

87 P. 151, 48 Or. 444, 1906 Ore. LEXIS 112
CourtOregon Supreme Court
DecidedOctober 23, 1906
StatusPublished
Cited by15 cases

This text of 87 P. 151 (Morton v. Oregon Short Line Ry. Co.) is published on Counsel Stack Legal Research, covering Oregon Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Morton v. Oregon Short Line Ry. Co., 87 P. 151, 48 Or. 444, 1906 Ore. LEXIS 112 (Or. 1906).

Opinion

Mr. Justice Moore

delivered the opinion of the court.

The transcript shows that the plaintiff is the owner of the real property mentioned, and that Ms land borders on the west bank of the Snake River. The township referred to was surveyed in 1874, and the field notes thereof, a copy of which was offered in evidence, show that the left bank of the river, as meandered, then intersected the south boundary of section 33 at a point 68.35 chains west of the southwest corner of that section, and extended northwesterly by a curved line to a point west, but near the center, of section 33; thence, by a similar line northeasterly, to a point east of the northeast corner of that section; thence westerly and northerly by a curved line to a point west of, but near the center of, section 28; and thence northeasterly to a point 2.80 chains east of the northeast corner of the latter section. A sketch of the margin of the river as indicated will disclose that when the government survey was made, the stream flowed around a peninsula over which the boundary between sections 28 and 33 extended. The defendant, in 1883, constructed its railroad from Huntington, Oregon, southerly through the premises hereinbefore described, and also through adjoining land on the south, now owned by H. M. Plummer. The defendant offered in evidence a blue print of the locus in quo, reduced to a scale of 400 feet to the inch, which indicates the original course of the river as meandered, the line of the railway as constructed, and other data. It .appears from tMs plat that the railroad was built about 14 rods west of the meander line, at the bend near the center of section 28, and about 52 rods west thereof at the curve near the middle of section 33. An extraordinary freshet in Snake River in 1894 cut across the base of the peninsula a new channel, which extends northeasterly over what theretofore had been a meadow. Prior to such change, a large part of the river below the peninsula flowed in a channel that separated plaintiff’s land from Datey Island, east of Ms [447]*447premises; but, after such flood, the greater volume of water flowed east of that island. Immediately north of section 33, but south of Datey Island, the change in the channel of Snake Eiver formed a large sand bar, constituting an island, the surface of which was above the ordinary stage of water. The bar is separated from the left bank of the river by a narrow channel which extends northerly, and is also severed from Datey Island by a broader channel that extends northwesterly; the waters of which unite and flow by plaintiff’s premises.

The freshet adverted to and the annual floods in the river have washed away the left bank of the stream in sections 28 and 33, nearly to the east line of the right of way of the railroad, and, to prevent further injury therefrom, the defendant placed several hundred car loads of rock along the margin of the river; and in 1903, with Plummer’s consent, it built,, where the swale had been, five jetties that extend from the bank down stream at an acute angle with the thread thereof. These obstructions were made by driving parallel rows of piling about 12 feet apart, and filling the intervening space with brush and rock. The lower jetty is about 215 feet long, and extends nearly across the channel west of the sand bar at the head thereof. The other jetties are from 50 to 75 feet in length. Another extraordinary freshet in 1904 caused the bank of plaintiff’s land, for a distance of about half a mile, to be washed away to the depth of 100 feet or more, whereupon he instituted this suit, and, at the trial, offered testimony tending to show that the lower jetty ■ prevented the water from flowing in the channel west of the sand bar, thereby permitting the current in the channel between the bar and Datey Island to flow nearly at right angles against his bank, damaging it; that the closing of the channel west of the sand bar caused sediment to be deposited, shoaling the channel east of his land, and preventing him from operating, by force of the current, a ferry boat which he maintained for his own use from his premises to Datey Island, a part of which he held by lease from year to year, and another part thereof was claimed by his son as a homestead where cattle were pastured in which he had an interest; and that if the lower [448]*448jetty be maintained the diminution of water in the channel will prevent the subirrigation of his land, which is arid, and will also prevent the water in the channel north of the sand bar to cut into a swale on his premises, thereby forming a new course through his land and creating an island.

The testimony relating to the injury which it is claimed will result to plaintiff’s land by the maintenance of the lower jetty, though given by persons living in the vicinity of his premises, who are acquainted therewith, know the character of the soil, and the effect thereon of freshets in the river, consists of the opinions of several witnesses, and it is possible that the disastrous consequences which they predict may not eventuate. It was stipulated that three civil engineers who were employed by the defendant would, if present, testify that in the early spring of 1905, they made accurate measurements of the left bank of the river through the plaintiff’s premises, setting-stakes along the margin of the stream, and that returning to his land in the latter part of July, after the annual freshet had subsided, they found that no part of the bank had been washed away during that season, but that the water in the river in 1905 was not as high as it was the preceding year. The foregoing is deemed a fair statement of the material facts involved, and, based thereon, the question to be determined is whether or not the jetties can legally be maintained where they are built. The defendant’s counsel insist that the river having suddenly changed its channel in 1904, thereby endangering the railroad» track, their client, to protect its property, was authorized to restore the flow of the stream to its original bed, and hence the decree should be affirmed.

1. It has been held that the person across whose land a freshet in a natural stream suddenly causes a new channel to be formed may, within a reasonable time, restore the flow of water to its original bed: Farnham, Waters, § 491; Mathewson v. Hoffman, 77 Mich. 420 (43 N. W. 879, 6 L. R. A. 349).

2. It will be remembered that the defendant built the jetties into the river from the bank of Plummer’s land with his consent, and, as he is a riparian proprietor on the new channel, the [449]*449railway company, as Ms licensee, secured such right to change the flow of the current as he possessed: Slater v. Fox, 5 Hun, 544.

3. An examination of the blue prMt referred to shows that the upper jetty is built nearly half a mile behrw the original meander line of the river where it commenced to cut the new channel, and as the barriers complained of do not force the water around the peninsula, they were evidently constructed to prevent injury to the railroad grade by deflecting the current. Instead, therefore, of attempting to restore the stream to its ancient channel, the defendant, by building the jetties, has in fact recognized the new way as the true water course, and tried to confine it to the bed as at first made.

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Cite This Page — Counsel Stack

Bluebook (online)
87 P. 151, 48 Or. 444, 1906 Ore. LEXIS 112, Counsel Stack Legal Research, https://law.counselstack.com/opinion/morton-v-oregon-short-line-ry-co-or-1906.