Gregory v. Pershbaker

14 P. 401, 73 Cal. 109, 1887 Cal. LEXIS 613
CourtCalifornia Supreme Court
DecidedJuly 12, 1887
DocketNo. 12105
StatusPublished
Cited by10 cases

This text of 14 P. 401 (Gregory v. Pershbaker) 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
Gregory v. Pershbaker, 14 P. 401, 73 Cal. 109, 1887 Cal. LEXIS 613 (Cal. 1887).

Opinion

McKinstry, J.

1. It is contended by the defendant and the intervenor (respondents) that the mineral, if any, found in the land claimed by the plaintiffs herein constitutes a “lode ” within the meaning of the acts of Congress; that ledges or lodes can be located only in a manner entirely different from the mode adopted by plaintiffs’ predecessors; and therefore, however regular their surface location might have been as a location of a “placer claim,” it is invalid, because no placer exists within its limits.

Finding No. 51 of the court below is as follows:—

“ That in the year 1856 John Barrett, and others associated with him, discovered on the westerly bank of Little Butte Creek, on the southeast quarter of said section 13, a thin seam of gravel cropping out between an underlying bed of slate-rock and an overlying bed of lava-rock, and finding that the said seam of gravel was gold-bearing, located the same as and for a mining claim, under the name and designation of the Burch [112]*112and Barrett Claim, and thereupon commenced to work and develop their said claim by excavating a tunnel into the hill, following the course of the channel, and the said channel became thicker and better developed and more valuable as they pursued and explored the same into the hill, and showed that the said deposit was a well-developed channel, varying from a few inches to eight and ten feet in thickness, and from eight or ten to forty feet in breadth, with a well-defined bed and side walls of slate-rock, and capped by a thin stratum of clay, with an overlying body of lava-rock for hanging wall. Prior to the v"iar 1879, the said John Barrett, by mesne conveyances from his associates in said location, became sole owner of the said Burch and Barrett location, and in that year sold and conveyed the same to the intervener, the Magalia Gold Mining Company, a corporation duly formed and organized under the laws of the state of California, and the said intervener thereupon entered into and took, and thence hitherto has kept and held, and still holds, the possession, and has ever since continued the work of exploring and pursuing and working and mining the said gravel deposit in and along the said channel or bed, and had, in the spring of the year 1882, pursued,' and opened, and worked the said gravel channel or bed in said southeast quarter of said section 13, and in the direction of the said southwest quarter of said section, and had discovered that the said gold-bearing channel extended towards and probably into the said southwest quarter, and' that the' said southeast quarter of section 13 contained deposits of gold-bearing gravel in quantity sufficient, not only to pay for working and mining the same, but sufficient to render the said quarter-section of great value for mining purposes; that after the commencement of this action, the said Magalia Gold Mining Company projected and extended its tunnel mentioned in these findings into said southwest quarter of said section 13, following the said gold-bearing deposit [113]*113or channel; that said channel in its course inf descends or drops at an angle on an average o’ eight degrees; that the bed-rock of said channel its entire length, so far as worked, is composed of a formation, and upon that slate formation said gravel rests, and over said gravel is a formation of clay gouge overlapping said mineral deposit, and that above £ 'id clay seam is the lava which extends to the surface, and that the overlying lava-rock at the point where the said channel crosses the easterly line of the said southwest quarter aforesaid is about six hundred feet in thickness; that said gravel is of a hard nature, and in mining and extracting the same has to be detached from its position by the use of picks and gads, and when extracted is taken out to the surface and there washed, and in so washing gold is extracted therefrom; that neither gold nor any other mineral was discovered within the boundaries of said southwest quarter of said section 13 until the said tunnel of said Magalia company penetrated therein, as aforesaid; that said pay-streak of gravel and deposit does not crop out at any other place or places than the place where the same was discovered, as aforesaid; and that the same cannot be seen or reached without entering the works of the said Magalia Gold Mining Company, and following the trend and meanderings of said channel to the present face of the mineral deposit, except by sinking a shaft or running expensive tunnels other than those run, occupied, and used by the intervener therein.”

In support of their view, counsel cite the Eureka Vase, 4 Saw. 302, and other decisions following and referring to that. In the Eureka Vase, Mr. Justice Field of the Supreme Court of the United States said: “We are of opinion that the term [lode] as used in the acts of Congress is applicable to any zone or belt of mineralized rock lying within boundaries clearly separating it from the neighboring rock. It includes, to use the language [114]*114cited^P* counsel, ‘‘all deposits of mineral matter found y^Ma a mineralized zone or belt, coming from the ViPre source, impressed with the same forms, and appearing to have been created by the same processes.’”

This definition would not include a bed of gravel from which particles of gold may be washed. The words “mineralized rock” were evidently intended to qualify the last as well as the first sentence. That which in the Eureka Case was declared to be a “lode” was a zone of limestone, lying between a wall of quartz and a seam of clay or shale, the one having a dip of 45° and the other of 80°.

Section 2320 of the Revised Statutes of the United States, 1873-74, treats of “mining claims upon veins or lodes of quartz or other rock in place bearing gold”; section 2322, of veins, lodes, and ledges “the top or apex of which” lies inside of surface limes extended vertically downward.

In Soane’s, Newman, and Bafetti (by Valazquez), a “placer” is said to be “a place near the bank of a river where gold-dust is found.” In the last edition of Webster, which gives the meaning of the term as approved by usage in Mexico and California, it is defined,—“a gravelly place where gold is found, especially by the side of a river, or in the bed of a mountain torrent.” Whatever the origin of the subterranean channels containing gravel beds, they have long been known to exist in California, and they have been generally supposed to be, and generally spoken of, as the beds of ancient rivers in which the gravel was deposited by fluvial action, and which were either from their beginning subterranean, or upon which the superincumbent earth or rock has been hurled, by means of convulsion, caused by volcanic or other natural force. That the bed of gravel mentioned in -the findings, to the limited extent it has been prospected by the intervenor’s tunnel, “descends or drops on tan average of about eight degrees,” does not of itself [115]*115make the gravel deposit a lode with “a top or apex,” nor contradict the theory that the channel was the channel of a mountain stream or torrent.

The terms employed in the acts of Congress are used in the sense in which they are received by miners. (The Eureka Case, supra.) Moreover, by express enactment, “claims usually called placers” are declared to include all forms of deposit, “excepting veins of quartz or other rock in place.” (U. S. B. S., sec. 3229.)

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Cite This Page — Counsel Stack

Bluebook (online)
14 P. 401, 73 Cal. 109, 1887 Cal. LEXIS 613, Counsel Stack Legal Research, https://law.counselstack.com/opinion/gregory-v-pershbaker-cal-1887.