Mines & Minerals

2 Colo. L. Rep. 467
CourtDepartment of Interior
DecidedFebruary 28, 1882
StatusPublished

This text of 2 Colo. L. Rep. 467 (Mines & Minerals) is published on Counsel Stack Legal Research, covering Department of Interior primary law. Counsel Stack provides free access to over 12 million legal documents including statutes, case law, regulations, and constitutions.

Bluebook
Mines & Minerals, 2 Colo. L. Rep. 467 (Del. 1882).

Opinion

Register and Receiver, Leadville, Colorado.

Gentlemen: I have examined the testimony taken before you at the hearing ordered by my predecessor, March 13, 1880, upon the protest of Robert Boraem, against the issue of a pat-tent to Neils Larson et al., for the Shamus O’Brien lode.

The affidavits in support of the protest raised the following points:

1. That the boundaries of the Shamus O’Brien location were not marked upon the ground. 2. That there was no discovery of a ledge or vein within the said claim, prior to location or application for patent. 3. That the plat of survey and notice of intention to apply for patent were not posted in a conspicuous place upon the claim. 4. That the certificate of location did not contain such a description of the claim as would serve to identify the same. 5. That the discovery shaft was not sunk to [468]*468a sufficient depth to show a vein or lode; and, 6. That such shaft is not located midway between the side lines of the claim; and a hearing was ordered to determine these questions.

The hearing of testimony was commenced before you August 10, 1880, and on the 7th of March, 1881, you rendered your j oint opinion “ that the protestant had failed to maintain- his allegations; that, therefore, the protest should be dismissed, and that patents should issue to applicants,” etc.

•At the hearing C. C. Davis, publisher of the Leadville Chronicle, testified that the notice of application for patent was published in the weekly edition of said paper from October 4th to December 6, 1879. The testimony shows that the plat of survey and the notice of intention to apply for patent were posted on the claim from October 3d to December 14, 1879.

During this period no adverse claim was filed against the Shamus O’Brien application, and it must be assumed that none existed. Boraem et al. appear as protestants merely, and a large amount of testimony has been taken to show that the applicants have failed to comply with the terms of the law.

The burden of proof is assumed by protestants.

Upon the first point of protest, I find that the testimony in support of the allegation is entirely negative in character, whereas the testimony introduced by the applicants for patent shows that the location upon the ground was regularly made, and that the stakes were so set that the lines thereof could be readily traced. Nyce, U. S. Deputy Mineral Surveyor, testifies that he surveyed the O’Brien claim in August and September, 1879, and found five of the six location stakes standing, to wit: Stakes 1, 2, 3, ⅞ and 6.

To the second and fifth points of objection, which will be considered together, the evidence is principally directed. At the date of the hearing the shaft had been sunk in the Shamus O’Brien claim to the depth of about 310 feet. The first 165 feet was through wash material, the succeeding iio feet was through porphyry, and at the depth of about 275 feet, what is styled by the witnesses for the applicants for patent as the “contact,” or “crevice” matter was reached.

Upon the finding as to the character of this contact matter depends the validity of the location.

This contact matter was discovered in the discovery shaft about the 15th of January, and upon a%says thereof, which it is [469]*469stated show the existence of mineral, the location was based, dated February 22, 1879.

The only assays of which any record was made, or which are evidenced by the certificate of the assayer, were made after the date of location; but from the evidence of Larson, one of the locators, Woodward and James, the assayers, are satisfied that numerous assays were made prior to location of the matter contained in the shaft, which showed that the same carried from 2 j4 to 13 ounces silver to the ton of ore. There is no legal obligation upon the locator to cause an assay to be made of the mineral which he claimed to have discovered within his location. Such assay is only an element of the proof to sustain the legality of the location.

Since the location, drifts have been run on this so-styled contact matter in an easterly direction over 100 feet, and in a westerly direction about 50 feet. These drifts show a substance of the same general character as that discovered in the shaft.

This contact matter consists of a clay material intermixed with a harder substance containing the mineral.

Admitting that this matter contains mineral to a small extent, the protestants urge that it is 'not a continuous body, and because it does not rest upon a foot-wall of limestone, as usually occurs at Leadville, the discovery in the Shamus O’Brien shaft is not of a vein or lode of quartz, or other rock in place, bearing gold, silver, etc.

It is shown .in this case that the contact or crevice referred to lays between two walls of solid rock.

The Courts have frequently passed upon the question as to what constitutes a vein or lode within the meaning of the mining law, and I quote the following judicial definitions:

In the Eureka case (4 Saw., 302) Judge Field decided: “These acts (of Congress) give no definition of the term (lode). They use it always in connection with the term vein. * * * The definition of a lode given by geologists is that of a fissure in the earth’s crust filled with mineral matter, or more accurately, as aggregations of mineral matter containing ores in fissures. (See Von Cotta’s Treatise on Ore Deposits, Prime’s Translation, 26). But miners used the term before geologists attempted to give it a definition. * * * Cinnabar is not found in any fissure of the earth’s crust, or in any lode as defined by geologists; yet the [470]*470acts of Congress' speak, as already seen, of lodes of quartz or rock in place, bearing cinnabar. Any definition of lode as there used, which did not embrace deposits of cinnabar, would be as defective as if it did not embrace deposits of gold and silver. The definition must apply to deposits of all the metals named, if it apply to deposits of any one of them. Those acts were not drawn by geologists or for geologists; they were not framed in the interests of science, and consequently with scientific accuracy in the use of terms. They were framed for the protection of miners in the claims which they had located and developed, and should receive such a construction as will carry out this purpose.”
“ It is difficult to give any definition of the term, as understood and used in the act of Congress, which will not be subject to criticism. A fissure in the earth’s crust, an opening in its rocks and strata made by some force of nature, in which the mineral is deposited, would seem to be essential to the definition of a lode, in the judgment of geologists. But to the practical miner, the fissure and wall are only of importance as indicating the boundaries within which he may look for and reasonably expect to find the ore he seeks. A continuous body of mineralized rock lying within any other well defined boundaries on the earth’s surface and under it, would equally constitute in his eyes a lode. We are of opinion, therefore, that the term as used in the acts of Congress is applicable to any zone or belt of mineralized rock lying within the boundaries clearly separating it from the neighboring rock!’

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Related

Eureka Consol. Min. Co. v. Richmond Min. Co.
8 F. Cas. 819 (U.S. Circuit Court for the District of Nevada, 1877)

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Bluebook (online)
2 Colo. L. Rep. 467, Counsel Stack Legal Research, https://law.counselstack.com/opinion/mines-minerals-deptinterior-1882.