Mount Diablo Mill & Mining Co. v. Callison

17 F. Cas. 918, 5 Sawy. 439, 1879 U.S. App. LEXIS 2044
CourtU.S. Circuit Court for the District of Nevada
DecidedMarch 19, 1879
StatusPublished
Cited by19 cases

This text of 17 F. Cas. 918 (Mount Diablo Mill & Mining Co. v. Callison) is published on Counsel Stack Legal Research, covering U.S. Circuit Court for the District of Nevada primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Mount Diablo Mill & Mining Co. v. Callison, 17 F. Cas. 918, 5 Sawy. 439, 1879 U.S. App. LEXIS 2044 (circtdnv 1879).

Opinion

BY THE COURT (HILLYER, District Judge).

This is an action to recover posses[919]*919sion of a mining claim situated in tlie Columbus mining district, Esmeralda county, Nevada. Tie complaint alleges ownership of fourteen hundred feet of a certain quartz lode, called the Dinero lode, seven hundred feet easterly and seven hundred feet westerly from the Dinero location monument, “together with one hundred feet of surface on each side of said fourteen hundred feet of said lode,” with all the dips, spurs, etc.; and also all that portion of the Dinero, and of all other lodes or veins, the top or apex of which lies within such surface lines, and end planes drawn north and south through points seven hundred feet east and west from a stake marked “Centre Mount Diablo Claim.”

The trial has been by the court, a jury having been waived by a written stipulation of counsel. There has been a somewhat extended oral argument, and, in addition, a very full discussion of all the points in briefs. The point most discussed is as to the lateral boundaries of the Mount Diablo lode; the plaintiff contending that the Mount Diablo, Dinero and Callison, or “Mountain Boy” claims, are all on one and the same vein or lode, and the defendants that the Callison is a lode distinct from every other in that district. By agreement of parties, three scientific mining experts only were examined on each side. For the plaintiff, W. S. Keyes, Carl Davis and Dr. Blatchley are of opinion that the said claims are on one single lode. For the defendants, C. A. Luckhart, Professor W. F. Stewart and Charles F. Hoffman are of opinion that the Callison is a separate lode. All of these experts are men of large and practical experience in mining. Each one has examined the mining region now. in question with care, and has, under oath, stated the facts upon which he bases his opinion. If the court is not now fully informed, such result is not due to the failure of the parties on either side to present their ease thoroughly, but to the inherent difficulties to be found in the questions brought forward for decision.

We proceed now to a consideration of the first question, stated, namely, whether the Mount Diablo and Callison claims are on the same or separate lodes. We find at the point where the claim in controversy is located a metalliferous belt, or zone, or district, extending east and west some two miles in length, the width of which has not, so far as appears in this case, been accurately ascertained. Scattered over this belt or zone, a dark rock stained with iron and manganese is seen, called by all the witnesses croppings. Booking west, from the Mount Diablo claim, the general course of the metalliferous region can be seen marked by these black croppings for about two miles. Along this line a great many claims have been located; in some cases several claims being parallel, or nearly so.

Describing this belt of country at the point where the claim in dispute lies, the experts tell us, that they find on the south of the Peru claim, and perhaps coming into that claim, a rock in place which they call variously, silieious, or stratified, or unaltered clay slate. (The Peru is a claim belonging to the plaintiff which lies immediately south of the Mount Diablo. Then follow, going north, the Mount Diablo, the Dinero, and lastly, the Mountain Boy, which covers on the surface nearly the same ground as the Dinero.)

Going north from the Peru; that is, across the belt, the experts find a i’ock which the plaintiff’s witnesses name clay - slate, and which they insist, notwithstanding some alterations in color and texture, extends from the stratified slate on the south to a belt of greenstone found about two hundred feet north of the Callison claim, or some eight hundred feet from the Peru south line. This rock is, according to the plaintiff’s experts, for the most part a decomposed clay state. In many places, and especially near ore bodies, it is white, and without signs of stratification; in other places it becomes a hard and highly silieious rock of a dark brown color, also unstratified, but always, in their opinion, clay slate more or less altered and decomposed, and all a part of the Mount Diablo lode. On the other hand, the experts of the defendants name this prevailing rock in the Mount Diablo,- Dinero and Calli-son claims, felsite porphyry and decomposed felsite porphyry; the former being the dark brown, and the latter the white clay slate of the plaintiff’s witnesses.

. Except in the names they give the rocks, and that they differ as to the presence of feldspar crystals therein, the witnesses on both sides agree in their description of such rocks as to color, texture and position.

The stratified slate on the south is barren, as is the greenstone to the north. Throughout this belt the ■ ore bodies, the pay ores, have occurred quite irregularly, unless we except the Callison ore body, to be considered further on. The-main tunnel of the Mount Diablo followed; -for two or three hundred feet, a crack .or fissure which Mr. Keyes at first took to be the fissure up through which the metals came to impregnate the neighboring rocks; but later concluded was a rent made after the: deposition of the metals.

Along the line'.of this tunnel, for the first two hundred .feet, the paying ores of the Mount Diablo have chiefly been found. From a point at the foot of an incline (No. 2) sunk from this ’tunnel, which point is near the center of the- Mount Diablo claim, a drift, called the “connecting drift,” has been run north two hundred and thirty feet to the Callison upper/incline and ore body. At a distance of one hundred and fifteen feet from the foot of this incline there is encountered in the drift a belt of rock, called, by some of the witnesses, the “black dyke,” which is from twenty-two to thirty feet in thickness. By whatever ñamé called, clay, slate or porphyry, it is in every exterior quality presented to the sight or touch a different rock from that [920]*920adjoining it on each side. About two hundred and fifty feet east of this, in the “blue drift,” run from the foot of incline No. 3, a dyke of . similar rock is found at a- depth considerably greater than in the connecting drift, and appearing, from its position and physical properties, to be the same black dyke found in the connecting drift. This dyke, the defendants claim, is the hanging wall of the Mount Diablo lode. Assuming it to be continuous between the points exposed in the two drifts, it has a course east and west corresponding to the gene™.! course of the ore channels' in the Mount Diablo and Callison claims. Going on north in the connecting drift from this dyke, we pass through some decomposed felsite porphyry or slate, some quartz and other rocks, not in place, just under the ravine which runs between the Mount Diablo and the Callison claims, and at ninety feet north of the dyke come to a stratum of dark, hard, flinty rock, which is about six feet thick; lying upon this next comes about fifteen feet of defendants’ decomposed felspathic porphyry, or plaintiff’s clay slate, which defendants call their foot-wall. Then comes the Callison ore body, from two to six feet thick, followed by a hanging wall of the white decomposed barren rock, extending on one hundred feet or more to belts of porphyry, greenstone and serpentine. From the Mount Diablo tunnel to the “black dyke,” assays taken by Mr. Keyes every ten feet show from sixty-four dollars and ten cents, in one place twenty feet north of the tunnel, to three dollars and seventy-seven cents silver.

The black dyke is practically barren, though traces of silver are shown by some assays.

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Bluebook (online)
17 F. Cas. 918, 5 Sawy. 439, 1879 U.S. App. LEXIS 2044, Counsel Stack Legal Research, https://law.counselstack.com/opinion/mount-diablo-mill-mining-co-v-callison-circtdnv-1879.