Haack v. San Fernando Mission Land Co.

HENSHAW, J.

In an action to quiet title brought by plaintiffs against defendants, the real controversy was over the boundary line between their respective land holdings. Plaintiffs prevailed in their contention as to the location of this boundary line and defendants have appealed. The call in the deed to plaintiffs’ land which gives rise to this controversy is “the center line of said Pacoima Creek or wash as the same existed on the fourteenth day of June, 1882.” It is conceded that plaintiffs own the land to the east of that line wherever it may be located. The word " wash ’ ’ employed in the description belongs neither to the terminology of geology nor of law. It is, however, a word in popular usage in the southern part of the state and as used is quite capable of definition. The streams in the southern part of the state rising in the mountains flow through narrow and often deep channels with sharp grades until they debouch on to the level lands below. They are torrential in character, carrying great quantities of water during the heavy rains in winter and becoming partially or wholly dry during the rainless season. At times, cloudbursts or long-continued heavy rains in the mountains cause these streams to overflow their banks in the valley lands below and flood the neighboring country. In the torrential season these streams bring down from the mountains, and for centuries have brought down, boulders, smaller Stones, gravel, and sand, and as the velocity of the waters so

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moving and carrying these earthy matters is arrested upon entering the plains, they begin, under familiar laws, to deposit, first, the heavy boulders- at and near the mouth of the canyon, or mountain passes, down which they have descended; next the smaller rocks, next the gravel, and finally the sands. Naturally, the greatest of these deposits is below and near to the canyon mouth, and they spread out fan-wise, lessening in depth and thickness until finally they feather out into nothingness. Geologically, the whole area of land thus affected, being built up of these deposits, is known as the “cone” of the stream. The “wash,” though bearing relation to the cone, is not synonymous with it. As these conditions of increased winter flow occur every year, and as each year is brought down and deposited debris of the character described, it results in creating upon the lower reaches of the stream always at the point where the waters first flow on to the level land, and at times in other parts of the river bottom, rocky, gravelly, and sandy stretches of waste lands, desolate to the eye and nourishing little or no vegetation; in brief, a tiny desert. It is this sandy, rocky, gravelly, boulder bestrewn part of the river bottom which is known as the wash. The wash is not, of course, coterminous with the cone. It frequently happens that in the lapse of centuries the outer portions of the cone have accumulated sufficient humus to create a fertile and fruitful soil raised above the danger of ordinary flooding. Through the wash the waters of the stream find their way. Under the conditions outlined it is quite apparent that the channel of the stream will move about in this wash. An impediment at the head of the old channel may cause a diversion; an obstruction at the lower part of the old channel will cause its rapid filling with debris, and so in time force the stream to leave it and make for itself a new way. Frequently, then, the channel of the stream shifts in the wash, and sometimes for no small distances a well-defined channel is entirely lost, the waters wandering over the surface of the wash in small rivulets, seeping through the gravels, and coming together within banks and boundaries at some lower point. Usually, however, somewhere through the wash runs a well-defined channel.