Radich v. Fredrickson

10 P.2d 352, 139 Or. 378, 1932 Ore. LEXIS 159
CourtOregon Supreme Court
DecidedFebruary 25, 1932
StatusPublished
Cited by9 cases

This text of 10 P.2d 352 (Radich v. Fredrickson) 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
Radich v. Fredrickson, 10 P.2d 352, 139 Or. 378, 1932 Ore. LEXIS 159 (Or. 1932).

Opinion

*379 ROSSMAN, J.

Before stating the issues awaiting decision it seems desirable to describe the location in dispute. As the waters of the Columbia river reach Tenas Illihee island they divide themselves into two parts and thus form two channels. The waters which flow to the right as they pass on their way to sea constitute the main channel of the Columbia river. With that channel we are not concerned. Those which flow to the left take their course in what is known as the Clifton channel. It is this channel with which we are, in part, concerned. About a mile below Clifton in the Clifton channel is the commencement point or towhead of what is known as Cottonwood drift. A drift is an expanse of water over which gill net fishermen drift their nets. (For a description of a gill net see Monroe v. Withycombe, 84 Or. 328, 331 (165 P. 227). Salmon swim against the current and gill themselves in the meshes of the gill nets which drift downstream with the ebbing tide. The nets used by the plaintiffs are approximately 1,200 feet long and are placed in the water at right angles to the shore line at the towhead. The plaintiffs’ witnesses testified that Cottonwood drift extended from the towhead downstream two and one-half miles. Since the defendant Fredrickson contends that the drift extended only one mile below the towhead, and that it was impossible to drift a 1,200-foot net below that point, we shall now describe the waterways below the towhead.

To the left of Clifton channel at the towhead is the mainland. To the right is Tenas Illihee island. When *380 the nets have drifted approximately one mile below the towhead a. point is reached where Clifton channel divides itself into two courses. Quinn’s island is the body of land which splits the channel. The fork which extends to the right is a continuation of Cottonwood drift, according to the plaintiffs’ witnesses. With the left fork we are not concerned. It may help one to obtain a mental picture of the surroundings to suggest that the two forks and the main channel out of which they have emerged assume the form of the letter Y, with' Quinn’s island filling the area between the two forks. Beyond the right fork, which is approximately 6,000 feet in length, is a wide, deep expanse of water which eventually leads into the main channel of the Columbia river. The waters in the stem of the Y over which the nets drift are amply wide and deep to accommodate them, but when the nets reach the above mentioned division point a different condition is encountered. The right fork which pursues a course almost due north is bounded on the east by a continuation of Tenas Illihee island, on the left by Quinn’s island, and is approximately 1,400 feet wide. Only the water in the easterly 550 feet of this fork is sufficiently deep at low tide to accommodate gill nets. All of the remainder of this channel is no deeper than five feet at low tide. Beyond this right fork is the expanse of water above mentioned which is of ample depth to suit the needs of gill net fishermen, and in it, according to the plaintiffs’ witnesses, the nets drift for a distance of 1,000 feet more when the end of Cottonwood drift is reached. A few feet beyond this point is the towhead of Castura drift. The defendant Fredrickson constructed the fish trap (for a description of such a device see Monroe v. Withycombe, 84 Or. 328, 331 (165 P. 227)) in the portion of the channel where the *381 deep water is only 550 feet wide. It extended from the shore of Tenas Illihee island ont into the channel for a distance of 300 feet. The water in its vicinity is about'30 feet deep at low tide.

The defendant Fredrickson contends: (1) that Cottonwood drift extends no farther than the point where Clifton channel is divided into two forks by Quinn’s island; (2) that since the nets used by the plaintiffs are at least 1,200 feet long, it is impossible to employ them advantageously in the right fork which contains deep water for a width of only 550 feet; (3) that since the' plaintiffs, in order to use Cottonwood drift ■with safety for their nets, remove from it snags and other debris, this circumstance proves that it is unsuited to the needs of gill net fishermen if left in its natural condition; (4) that since: (a) the gill net fishermen who employ Cottonwood drift apportion among themselves the cost of keeping the channel clear of snags, (b) have adopted a practice of starting from the towhead in numerical order determined by allotment, and (c) prevent those who do not submit to the foregoing from using Cottonwood drift (according to the defendants’ contention), they are guilty of inequitable conduct which denies them recourse to a chancellor; and (5) that the plaintiffs as gill net fishermen are entitled to ho rights superior to those of the defendant which will warrant the relief which the plaintiffs seek.

The decision of the first of the above issues requires a study of the evidence. We have examined all of it with care. The plaintiffs presented ten commercial fishermen, each of whom testified that he possessed a practical knowledge of and had had several years’ experience with gill net fishing. One of these swore that for 44 years he had drifted gill nets along Cottonwood drift. Another testified that he had done *382 so for 21 years. Each of them, as well as several of the others, used nets 1,200 feet long and 12 feet deep. All of the plaintiffs’ witnesses described the course of Cottonwood drift as starting at the towhead about one mile below Clifton, proceeding down Clifton channel and through the right fork of that channel as it takes its course between Quinn’s and Tenas Illihee islands to the Castura towhead. The defendants offered the testimony of seven witnesses, each of whom had observed gill net fishermen drifting their nets along Cottonwood drift, and each of whom testified that the fishermen removed their nets from the water as they approached the point where the channel is divided into two forks by Quinn’s island. A circumstance which we believe strongly corroborates the plaintiffs’ witnesses is the fact that those who use Cottonwood drift have adopted the aforementioned practice of removing from the bed of the channel snags and other objects which would interfere with their nets. Manifestly, the plaintiffs would not remove that material from the right fork unless they drifted their nets through there. All of the plaintiffs’ witnesses testified that they regarded the drift as a valuable one. One of them thus described its desirability: “One of the best on the river.” Another thus: “It is considered one of the best drifts.” And another: “It is one of the best drifts we got.” The findings of the circuit judge who heard the witnesses and who participated in two test drifts along the challenged part of the course, found that Cottonwood drift extended through and beyond this right fork of Clifton channel. Having bestowed upon the testimony careful attention, we are of the same opinion.

The defendant Fredrickson, after contending that it would be impossible for the plaintiffs’ nets, 1,200 *383 feet long, to catch any fish while drifting through that portion of the right fork where the water is deep for a width of only 550 feet, submits that her trap, therefore, has deprived the plaintiffs of nothing of value.

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Bluebook (online)
10 P.2d 352, 139 Or. 378, 1932 Ore. LEXIS 159, Counsel Stack Legal Research, https://law.counselstack.com/opinion/radich-v-fredrickson-or-1932.