The Economic Aspect of GeologyLeith, C. K. (Charles Kenneth)
Science
The Economic Aspect of Geology
Leith, C. K. (Charles Kenneth)
Geology, Economic
Nevertheless, the mineral industry has become second only to agriculture
in its capital value and in its earning capacity. In this industry it is
hardly possible to arrive at valuations as securely based as in many
other industries, but the elements of hazard are not so hopeless of
measurement as might be supposed. The great mineral and financial
organizations do not depend on mere guesses, but use well-tried methods.
If the general investor were to give more attention to these methods he
would doubtless save himself money, and the mineral industry would be
rid of a great incumbrance of parasites who live on the credulity of the
public. To anyone familiar with the mineral field, it is often
surprising to see the rashness with which a conservative business man,
who would not think of entering another industrial field without close
study of all the factors in the situation, will invest in minerals
without using ordinary methods of analysis of values.
In the following account of valuation of minerals in the ground, and the
closely related subject, taxation of such minerals, the attempt is made
to state some of the principles briefly and simply with a view to making
them intelligible to the layman. Values beyond the mine are concerned
with so many factors of a non-geologic nature that they are not here
discussed.
VALUATION AND TAXATION OF MINES
INTRINSIC AND EXTRINSIC FACTORS IN VALUATION
It is essential to recognize at the outset that the value of a mineral
deposit, like the value of any other commercial material, comprises two
main elements; an intrinsic element based on the qualities of the
material itself, and an extrinsic element based on its availability and
the nature of the demands for it. The two elements may not be sharply
separated, and neither exists without the other. A mineral deposit in
easy reach of a populous community, which has sufficiently advanced
methods and requirements to use it, may have high value; an exactly
similar deposit, if far removed from points of consumption, handicapped
by transportation, or available only to people without developed methods
for its use, may have little or no value. Intrinsically the deposits are
alike; but extrinsically they are far different, and their values are
correspondingly unlike. Even two adjacent properties, differently
managed and controlled, and with different relations to markets, may
have somewhat different values depending on the use made of them. The
value of a deposit may vary from year to year with changes in demand for
its output, or with changes in metallurgical and other processes which
make its use possible. Minerals of small bulk and high value, as for
instance gold, platinum, and diamonds, have a nearly standard value
related to their intrinsic properties, because they can be transported
so easily to any part of the world. On the other hand, materials of
large bulk and low unit value, such as coal, iron ore, and clay, may
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