The Weinberg Co. v. Bixby

196 P. 25, 185 Cal. 87, 1921 Cal. LEXIS 525
CourtCalifornia Supreme Court
DecidedFebruary 15, 1921
DocketL. A. No. 5707.
StatusPublished
Cited by32 cases

This text of 196 P. 25 (The Weinberg Co. v. Bixby) is published on Counsel Stack Legal Research, covering California Supreme Court primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
The Weinberg Co. v. Bixby, 196 P. 25, 185 Cal. 87, 1921 Cal. LEXIS 525 (Cal. 1921).

Opinions

SLOANE, J.

This appeal is from a verdict and judgment awarding damages for alleged wrongful diversion of the flood waters of the Los Angeles River upon plaintiff’s lands.

The Pacific Electric Company, a railway corporation, the Dominguez Estate Company, a private corporation, and George H. Bixby and Amelia M. Bixby, who are husband and wife, were joined as parties defendant.

The Pacific Electric Company was exonerated from liability by the jury, and verdict and judgment were against the other defendants, appellants here, as joint tort-feasors.

The defendant Dominguez Estate Company was the owner of farming lands on the westerly banks of the river and defendant George H. Bixby, and later his wife, the defendant Amelia M. Bixby, was the owner of farming lands on the easterly side of the river at and in the vicinity of the place where the alleged wrongful diversion and interference with the river channel occurred. The Pacific Electric Company was the owner of a right of way and an electric railroad with embankments and trestles across the river valley, and particularly of a trestle which it had constructed over the natural channel of the Los Angeles River above and in the immediate vicinity of the diversion works charged to the other defendants.

It is alleged in the complaint that the location and construction of the railroad embankments and trestle were such as to concentrate the waters of the river in time of floods at this point and that the other defendants by the construction of embankments from this trestle downstream and along and on each side of the river-bed, and by dredging and deepening the channel of the stream between such embankments, so increased the current and flow of the river as to silt up and fill the natural bed of the stream below, thereby causing the waters to spread to each side, and that, in order to relieve this condition of overflow, they thereafter *91 cut an opening in the easterly embankment above the silted fill, thereby turning the current of the river from its former and natural course into a new channel, and that in recurring floods covering a period of two or three years great volumes of water were thus turned into this new channel and flowed down and across plaintiff’s lands below, cutting, eroding, and silting them to the damage of plaintiffs.

For an intelligent understanding of the points involved on this appeal it is necessary to describe generally the topography of the country forming the watershed of the Los Angeles River. The river with its various tributaries has its source in the Sierra Madre Mountain range lying to the north of the city of Los Angeles. These branches converge in the northerly part of the city where a comparatively narrow pass exists between the highlands. From this point the river runs in a generally southerly direction through a constantly widening plain and empties into the ocean between the cities of Long Beach and San Pedro. For several miles above its outlet the river bottom is near the sea level and has a very moderate slope toward the south. To the east of the watershed of the Los Angeles River is another watershed having its source in the same mountain range and draining its waters into what is known as the San Gabriel River. Toward the ocean the course of this stream is through a valley which widens out and merges on the west into the territory through which the Los Angeles River flows. The outlet of the San Gabriel River into the ocean through a period of its history has been east of the city of Long Beach and beyond the mesa lands in the vicinity of that city. The result is that in time of excessive floods the whole territory through which the two rivers flow, for a distance of some miles back from the coast, becomes a vast lake, the waters of the two streams commingling and moving toward the ocean with a very moderate current, which, of course, is accelerated in the deeper channels where the water is accustomed to run when the rivers are within their banks. At such times of overflow the higher body of land in the vicinity of Long Beach and extending back from the coast three or four miles stands above the flood waters as an island, and serves to separate the outlets to the ocean of the two rivers. At the northwesterly end of this body of mesa land a point juts out into the valley near the place where *92 the defendants constructed their dikes or embankments, and also forms an abutment for the southeasterly end of the railroad trestle of the Pacific Electric Company. The line of road of the Electric Company extends from this point in a northwesterly direction across the river bottom to a. projecting point of mesa lands on the opposite side called the Dominguez hills. The valley above and below these points immediately widens, both to the east and the west, but more particularly on the eastern and northern side where it extends toward the San Gabriel watershed.

The construction of the Electric Company’s railroad across this space from hill to hill, which is frequently called the Narrows, consists of an embankment several feet in height, intersected by a number of trestles or bridges at places of natural depression in the floor of the valley. The principal trestle is the one at the southeasterly end. This is about one thousand feet in length, consisting of stringers and rails, resting upon bents composed of piles driven into the ground, and braced with cross-timbers. The bents were placed about twenty feet apart and at right angles with the track.

The main channel of the Los Angeles River passes under this trestle in a slightly southwesterly direction at this point. At the time of and prior to the events upon which this action is based, the natural bed or channel of the river was a shallow erosion through the comparatively level floor of the valley not generally exceeding two or three feet in depth, and from one to two hundred feet wide. Nearly every winter season the flow of the waters greatly exceeds the capacity of this channel and spreads over the adjacent land, and occasionally there occur floods which cover the valley from mesa to mesa, with only infrequent spots of slightly higher land appearing above the surface.

The railroad embankments and trestles referred to were constructed by the Pacific Electric Company in the year 1901. The diking and dredging along the river channel by others of the defendants occurred in the fall and spring of 1912-13. This latter work originated with the Dominguez Estate Company. It owned lands bordering the westerly bank of the river, and was also in some way interested in a subsidiary company that was maintaining a cement water ditch which extended under this trestle from the north on the westerly side of the river. The construction of a line *93 of embankment along the west bank of the river and the deepening of the eroded channel, from a point some distance north of the trestle, was designed to protect their lands and this water ditch from overflow of the flood waters. In extending this work south from the trestle it was necessary to carry it over lands belonging to the defendant George H. Bixby.

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Bluebook (online)
196 P. 25, 185 Cal. 87, 1921 Cal. LEXIS 525, Counsel Stack Legal Research, https://law.counselstack.com/opinion/the-weinberg-co-v-bixby-cal-1921.