Gray v. Reclamation District No. 1500

163 P. 1024, 174 Cal. 622, 1917 Cal. LEXIS 845
CourtCalifornia Supreme Court
DecidedMarch 14, 1917
DocketSac. No. 2555.
StatusPublished
Cited by113 cases

This text of 163 P. 1024 (Gray v. Reclamation District No. 1500) 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
Gray v. Reclamation District No. 1500, 163 P. 1024, 174 Cal. 622, 1917 Cal. LEXIS 845 (Cal. 1917).

Opinion

HENSHAW, J.

Above the confluence of Feather River with Sacramento River lies a vast Y-shaped tract of land. Much of this land is swamp and overflowed land of the char-: acter contemplated by the Arkansas Act, and title to it passed to the state of California by virtue of that act. Defendant Reclamation District No. 1500, organized for the purpose of reclaiming the portion of this land within its boundaries, was proceeding with the work of levee construction when, at the instance of these plaintiffs, who for general purposes may be described as owners of land within the same triangle, lying to the north and east of the lands of the Reclamation District, and fronting upon Feather River, the work was stopped by a prohibitory injunction of the trial court. Still further, a mandatory injunction was decreed, by which the defendant Reclamation District was ordered to destroy the levees which already it had constructed.

The district is the same district, the work the same work, the law of the creation of the district the same law, that were considered in Reclamation District No. 1500 v. Superior Court, 171 Cal. 672, [154 Pac. 845].

*626 The geological and topographical conditions concerning these lands and others similarly situated have been the subject of frequent exposition by this and other courts. For a general review of these facts reference may be made to Kimball v. Reclamation etc. Comm., 45 Cal. 344; Hagar v. Yolo County, 47 Cal. 222; Dean v. Davis, 51 Cal. 406; North Bloomfield G. M. Co. v. Keyser, 58 Cal. 315; People v. Gold Run D. & M. Co., 66 Cal. 138, [56 Am. Rep. 80, 4 Pac. 1152] ; Lamb v. Reclamation Dist., 73 Cal. 125, [2 Am. St. Rep. 775, 14 Pac. 625] ; McDaniel v. Cummings, 83 Cal. 515, [8 L. R. A. 575, 23 Pac. 795]; Gray v. McWilliams, 98 Cal. 157, [35 Am. St. Rep. 163, 21 L. R. A. 593, 32 Pac. 976]; People v. Russ, 132 Cal. 102, [64 Pae. 111]; People v. Sacramento Drainage Dist., 155 Cal. 373, [103 Pac. 207]; Woodruff v. North Bloomfield G. M. Co., 18 Fed. 761; North Bloomfield G. M. Co. v. United States, 88 Fed. 664, [32 C. C. A. 84]; Hagar v. Reclamation Dist., 111 U. S. 701, [28 L. Ed. 569, 4 Sup. Ct. Rep. 663], Summarizing for the convenient consideration of the questions here presented, those conditions are the following: The Sacramento River and its principal tributaries, rising in the Sierra Nevada Mountains, flow with high gradients on to the low-lying lands of the Sacramento Valley. It is declared that anciently this valley was a shallow arm of the sea, and has been reclaimed from the ocean by the soils carried down by the rivers and deposited in it. This valley is still low land, and upon entering it the high gradient of the Sacramento River necessarily drops off to a very low one, with a corresponding arrest of current and carrying capacity. Fed by the heavy rains and the melting snows of the mountains, the onrush of these waters overflows the banks of the river and the waters themselves spread out over vast areas of these low-lying lands. Under the well-known principle of physics that the capacity of water to carry foreign matter in suspension is dependent upon the velocity of the water, and that the instant the velocity is checked the saturated water begins to deposit a portion of the matter held in suspension, the following conditions resulted: By the checking of the flow of the Sacramento River and its tributaries at its banks and edges and by the gradual deposit on top of these banks as the flood waters passed over them in slow-moving sheets, the banks themselves and very consider *627 able tracts of land upon either side were raised to a height greater than that of the lower lands beyond.

Thus the rivers themselves came to move along the center of ridges of their own construction. These ridges were highest in immediate proximity to the rivers and sloped gradually downward to the lowest plane of the valley. As the flood waters poured out of the rivers they found their way into these vast areas of lower lands lying on either side of them. These low areas came to be known as “basins,” and were bounded upon the river side by the high lands constituting its banks, and upon the opposite side by no well-defined boundary, but only by the natural and gradual rise of the land above the possibility of flooding. So both as to the higher lands near to the river and to the higher lands opposite, their condition was that of susceptibility to occasional and unexpected flooding, depending in any year upon the quantity of water which the river, called upon and unable to carry in its natural bed, cast out over the surrounding country. Thus as to such lands a man’s farm might escape flooding for ten years and be flooded on the eleventh. But the lower lying areas were subject to regular recurrent annual floods. We have spoken of these vast areas of low-lying lands as basins. Such is the designation which has been given them by hydraulic engineers. There are several of them. Following down the course of the Sacramento River there is, to the east, first, the Butte Basin, separated from the Sutter Basin by a slight elevation of the land caused by the proximity of the Sutter or Marysville Buttes and by the embankment or ridge built up, as we have heretofore described, by Butte Creek. Next the Sutter Basin, in which are the lands of defendants, subject to overflow both by the waters of the Sacramento River and of the Feather River. Below Sutter Basin and still upon the east side of the river is the American Basin near the junction of the American River with the Sacramento, and finally below this the Sacramento Basin, containing within it the city of Sacramento itself. Upon the west side of the river and opposite Butte Basin and Sutter Basin lies the Colusa Basin, and below that and separated therefrom by Knight’s Landing Ridge, itself the ancient high bank of Cache Creek, which subsequently abandoned its former course into the river and turned southward, is Yolo Basin. At all times there flow into these basins *628 minor streams usually known as creeks, which upon the east of the river commonly have their sources in the foothills of the Sierra Nevada Mountains, and to the west of the river in the Coast Range Mountains. They gather up as well,' of course, the surface waters coming from the rainfall upon the lands themselves. But both these elements of supply are insignificant as compared with the vast volumes of wafer delivered into these basins from the Sacramento River. The general characteristics of all these basins are similar. The river poured its excess waters into them in low places and breaks through the banks, known as sloughs, and over the banks themselves in sheets. These sloughs had well-defined channels as they cut through the higher lands of the river banks, which channels feathered out into nothingness as the sloughs poured their waters into the vast flat area of the basins’ low lands.

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Bluebook (online)
163 P. 1024, 174 Cal. 622, 1917 Cal. LEXIS 845, Counsel Stack Legal Research, https://law.counselstack.com/opinion/gray-v-reclamation-district-no-1500-cal-1917.