Churchill Co. v. Kingsbury

174 P. 329, 178 Cal. 554, 1918 Cal. LEXIS 520
CourtCalifornia Supreme Court
DecidedJuly 24, 1918
DocketSac. No. 2798. In Bank.
StatusPublished
Cited by12 cases

This text of 174 P. 329 (Churchill Co. v. Kingsbury) 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
Churchill Co. v. Kingsbury, 174 P. 329, 178 Cal. 554, 1918 Cal. LEXIS 520 (Cal. 1918).

Opinion

SLOSS, J.

This is a proceeding in mandamus, brought to compel the state surveyor-general to perform the acts preliminary to the issuance to petitioner of a patent for 5,120 acres of land in Siskiyou County. An alternative writ was *556 ordered. The material facts are admitted, either by answer or by stipulation.

On October 11, 1872, one Dorris made application under the law of 1868 (Stats. 1867-68, p. 507) for the land in question, as swamp and overflowed land. The county surveyor of Siskiyou County made a survey, and returned the same to the surveyor-general. On October 4, 1874, the register of the state land office issued to Dorris certificate of purchase No. 4185 for said land, as swamp and overflowed land. Dorris and his successors in interest have ever since been in possession of said property, and have paid all taxes levied and assessed against it. On October 11, 1917, the petitioner, as successor to the interest of Dorris, presented to the county treasurer the certificate of purchase, made tender of the amount due for the balance of principal and interest, and took the further steps required under the law to entitle it to demand a patent. The tender and demand having been refused, this proceeding followed.

The land lies at the edge of Little Klamath Lake, a navigable body of water about eighteen miles long and half as wide, lying partly in California and partly in Oregon. Little Klamath Lake has no outlet and no separate watershed. It receives its main supply of water from Upper Klamath Lake, which is in Oregon. Prom Upper Klamath Lake water flows to Little Klamath Lake through a branch of the Klamath River. There is but a slight fall in the channel between the two lakes, and water flows through it to Little Klamath Lake only when the water in Upper Klamath Lake is high. In ordinary seasons the water in Little Klamath Lake reaches its maximum height about the month of April in each year. During the summer months the water level gradually falls, reaching its lowest point from August to November. Ordinarily, the difference between the high and the low water levels of Little Klamath Lake is about three feet. The land in question is part of a wide strip which, in ordinary seasons, is covered during the period of high water to a depth of about three feet, and is uncovered when the water is at its lowest stage, the latter condition continuing, usually, during the months of September and October. The strip which includes the tract in controversy slopes gently toward the center of the lake. At its inner edge there is an abrupt break or drop to a depth varying from four to seven feet. This break marks *557 the edge or hank of the lake at low water. There is, also, a distinct rise of several feet at the outer border of the strip. The land thus annually uncovered is fertile and susceptible of cultivation without further reclamation than such as would be necessary to exclude the water of the lake from it. Klamath River itself, as. well as Little Klamath Lake, is navigable. A survey of the region was made under the authority of the United States in August, 1872. In making that survey a meander line was run along the ordinary high-water line of the lake and marked upon the land. No land was surveyed or lines run north or west of said meander line (i. e., below said high-water line), and no survey has ever been made by the United States of the lands (including those in controversy) beyond said meander line.

Whether the lands in question were swamp and overflowed lands, passing to the state by grant from the United States, or were lands lying under the waters of a navigable lake, belonging to the state by virtue of her sovereignty, the petitioner concedes that no right of purchase was vested in Dorris by the certificate, under the law as it stood when the certificate was issued. The statute then in force did not authorize the sale of swamp and overflowed land until six months “after the same has been segregated by authority of the United States.” (Pol. Code, sec. 3441; Garfield v. Wilson, 74 Cal. 175, [15 Pac. 620]; Wren v. Mangan, 88 Cal. 274, [26 Pac. 100]; Polk v. Sleeper, 143 Cal. 70, [76 Pac. 819].) The pleadings and the stipulation of the parties show that there had been no segregation of the land below the meander line. So, likewise, the certificate of purchase was invalid if the land described in it was sovereign land of the state, there being at the time no law authorizing the sale of any such land, except tide-lands. (Edwards v. Rolley, 96 Cal. 408, [31 Am. St. Rep. 234, 31 Pac. 267].)

The petitioner relies upon the terms of the act of March 24, 1893, providing for the sale of lands uncovered by the recession or drainage of the waters of inland lakes and unsegregated swamp and overflowed lands. (Stats. 1893, p. 341.) This act, which, with its amendments, has been incorporated into the Political Code (sec. 3493m et seq., contains a provision validating certificates of purchase theretofore made for any lands as swamp and overflowed lands which belonged to any of the classes offered for sale by the act. The peti *558 tioner claims, accordingly, that its certificate, although unauthorized by law at the date of its issue, was confirmed and made valid for all purposes by the statute just mentioned. Since the act authorizes the sale both of sovereign lands and of unsegregated swamp and overflowed lands, it might not be necessary for the petitioner to maintain that the lands in question fall within one of these classes rather than the other. It does, however, take the stand that the land is, in fact, sovereign land of the state, and in this, we think, it is clearly right.

Since the decision of the supreme court of the United States in Pollard's Lessee v. Hagan, 3 How. 212, 229, [11 L. Ed. 565], there has never been any question of these propositions, there laid down: “First, the shores of navigable waters, and the soils under them, were not granted by the constitution to the United States, but were reserved to the states respectively. Secondly, the new states have the same rights, sovereignty, and jurisdiction over the subject as the original states.” In England the only waters regarded as navigable are those in which the tide ebbs and flows. The different conditions prevailing in this country have, however, led to the adoption of the broader rule that “all waters are deemed navigable which are really so.” (Barney v. Keokuk, 94 U. S. 324, 336, [24 L. Ed. 224].) The title of the state extends not only to the land underlying that part of a navigable stream or body of water over which navigation may be conducted, but extends to the entire bed, and in particular to the land which is covered and uncovered by the ordinary rise and fall of the tide, stream, or lake. (Barney v. Keokuk, supra; McManus v. Carmichael, 3 Iowa, 1.) The agreed facts in this case show that the land in controversy is a part of the bed of Little Klamath Lake, a navigable body of water. During the greater part of the year, in ordinary seasons, the land is covered by the waters of the lake. It is uncovered only at times of low water.

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Bluebook (online)
174 P. 329, 178 Cal. 554, 1918 Cal. LEXIS 520, Counsel Stack Legal Research, https://law.counselstack.com/opinion/churchill-co-v-kingsbury-cal-1918.