Beach Rambles in Search of Seaside Pebbles and Crystals: With Some Observations on the Origin of the Diamond and Other Precious StonesFrancis, John George
Science
Beach Rambles in Search of Seaside Pebbles and Crystals: With Some Observations on the Origin of the Diamond and Other Precious Stones
Now, I think this argument a very strong one; in fact, although simple,
almost unanswerable. For no _plant_ dwells thus in a house. We have the
plant itself, but nothing more; and if this be not capable, and I hold it
to be incapable, of sustaining the most vehement mineralizing process in
the crucible of Nature, its history must be a brief one, and excepting in
the dark “lithographs” of the coal-measures, its memory must pass away. I
have already allowed an exceptionable case in favour of the _conifers_,
which, be it observed, nowise resemble anything portrayed in siliceous
pebbles, and it is remarkable how much this class of plants predominates
in the COAL.
I have always been suspicious of what are called “vegetable
petrifactions.” I examined those at Tivoli, near Rome, in the year 1845,
and I made up my mind that they are simple _incrustations_. In like
manner, many of the buildings at Pæstum are constructed with a kind
of “travertine” taken from the bed of a neighbouring river, and which
rapidly incrusts any solid objects submitted to the action of its waters.
But the truth is, the vegetable pipe or “straw” remains for a while,
owing to the silex which entered into its composition while the plant
was growing. After some years the _straw_ decays, and there is a hole or
depression in that part of the pillar or pediment. On the other hand, a
calcareous “menstruum,” imbibing silex and iron, hardens into a substance
which, like the best mortar or cement used in building, will sometimes
outlast even the blocks of limestone or oolite which it was put to bind
together.
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