Weight per
Cubic Foot
Number of
Cubic Feet
per Ton of
2000 lb.
Antimony417.504.79
Sulphide285.007.01
Arsenical Pyrites371.875.37
Barium Sulphate278.127.19
Calcium:
Fluorite198.7510.06
Gypsum145.6213.73
Calcite169.3711.80
Copper552.503.62
Calcopyrite262.507.61
Bornite321.876.21
Malachite247.508.04
Azurite237.508.42
Chrysocolla132.5015.09
Iron (Cast)450.004.44
Magnetite315.626.33
Hematite306.256.53
Limonite237.508.42
Pyrite312.506.40
Carbonate240.628.31
Lead710.622.81
Galena 468.754.27
Carbonate 406.874.81
Manganese Oxide268.756.18
Rhodonite221.259.04
Magnesite187.5010.66
Dolomite178.1211.23
Quartz165.6212.07
Quicksilver849.752.35
Cinnabar531.253.76
Sulphur127.1215.74
Tin459.004.35
Oxide418.754.77
Zinc437.504.57
Blende253.127.90
Carbonate273.127.32
Silicate215.629.28
Andesite165.6212.07
Granite162.6212.30
Diabase181.2511.03
Diorite171.8711.63
Slates165.6212.07
Sandstones162.5012.30
Rhyolite156.2512.80

The specific gravity of any particular mineral has a considerable range, and a medium has been taken. The possible error is inconsequential for the purpose of these calculations.

For example, a representative gold ore may contain in the main 96% quartz, and 4% iron pyrite, and the weight of the ore may be deduced as follows:—

Quartz,96% × 12.07 = 11.58
Iron Pyrite,4% × 6.40 = .25
11.83 cubic feet per ton.

Most engineers, to compensate porosity, would allow twelve to thirteen cubic feet per ton.

CLASSIFICATION OF ORE IN SIGHT.

The risk in estimates of the average value of standing ore is dependent largely upon how far values disclosed by sampling are assumed to penetrate beyond the tested face, and this depends upon the geological character of the deposit. From theoretical grounds and experience, it is known that such values will have some extension, and the assumption of any given distance is a calculation of risk. The multiplication of development openings results in an increase of sampling points available and lessens the hazards. The frequency of such openings varies in different portions of every mine, and thus there are inequalities of risk. It is therefore customary in giving estimates of standing ore to classify the ore according to the degree of risk assumed, either by stating the number of sides exposed or by other phrases. Much discussion and ink have been devoted to trying to define what risk may be taken in such matters, that is in reality how far values may be assumed to penetrate into the unbroken ore. Still more has been consumed in attempts to coin terms and make classifications which will indicate what ratio of hazard has been taken in stating quantities and values.

The old terms "ore in sight" and "profit in sight" have been of late years subject to much malediction on the part of engineers because these expressions have been so badly abused by the charlatans of mining in attempts to cover the flights of their imaginations. A large part of Volume X of the "Institution of Mining and Metallurgy" has been devoted to heaping infamy on these terms, yet not only have they preserved their places in professional nomenclature, but nothing has been found to supersede them.

Some general term is required in daily practice to cover the whole field of visible ore, and if the phrase "ore in sight" be defined, it will be easier to teach the laymen its proper use than to abolish it. In fact, the substitutes are becoming abused as much as the originals ever were. All convincing expressions will be misused by somebody.

The legitimate direction of reform has been to divide the general term of "ore in sight" into classes, and give them names which will indicate the variable amount of risk of continuity in different parts of the mine. As the frequency of sample points, and consequently the risk of continuity, will depend upon the detail with which the mine is cut into blocks by the development openings, and upon the number of sides of such blocks which are accessible, most classifications of the degree of risk of continuity have been defined in terms of the number of sides exposed in the blocks. Many phrases have been coined to express such classifications; those most currently used are the following:—