The various subterranean changes which have acted upon the coal-fields
during the course of unnumbered ages have not only raised or sunk, but
frequently dislocated, contorted, ruptured, or broken them up in a most
extraordinary manner. In the coal-field near Mons, in Belgium, for
instance, a vast lateral pressure has curved the strata again and again,
and even folded them four or five times into zigzag bendings, so that on
sinking a shaft the same continuous layer of coal is cut through several
times.
[Illustration: SECTION OF COAL-FIELD SOUTH OF MALMESBURY.]
1. Old red sandstone.
2. Mountain limestone.
3. Millstone grit.
4. Coal seams.
5. Coarse sandstone.
6. New red sandstone.
7. Lias.
8. Inferior oolite.
9. Great oolite.
10. Corn brash and
forest marl.
Frequently a concave form has been the result of these terrestrial
revolutions, and hence coal-fields are often called coal-basins. Thus,
in the coal-field south of Malmesbury, the strata appear to dip from the
surface, and rise again to it after attaining a certain depth, so that a
section of them suggests the idea of a boat or basin.
Very commonly one portion of a continuous stratum or series of strata
has been broken away from the rest, and has been displaced, either by
elevation or depression, or shifting on one side, for various distances.
The amount of displacement is sometimes only a few inches, and at other
times several hundred fathoms, and the extent may be twenty yards or
twenty miles.
We may easily conceive the difficulties which these disruptions
frequently throw in the way of the miner, who in following what he
considers a valuable seam of coal is suddenly stopped by coming in
contact with a fault, a trouble, or a slip, as these phenomena are
expressively called, and finds the coal shifted several yards above or
below, or even completely lost. On the other hand, the miner, thus
provokingly stopped in his labours, must not forget that it is perhaps
owing to the very shifts he complains of that the outcrop of the coal
has occurred at all in his neighbourhood, and that the coal is workable
throughout a very large portion of the district in which he is
interested.
Public-domain text, read in full here on John Shaqi.
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