Thoughts on a Pebble, or, A First Lesson in Geology — John Shaqi
Thoughts on a Pebble, or, A First Lesson in GeologyMantell, Gideon Algernon
Science
Thoughts on a Pebble, or, A First Lesson in Geology
Mantell, Gideon Algernon
Geology -- Juvenile literature
The surface exposed by the division of the pebble, is an oblique
vertical section of the petrified zoophyte. It shows a central canal
filled with bluish-grey flint (_Plate II, c_), in a mass traversed by
tubes or channels, which possess considerable beauty and variety of
colour from an impregnation of iron.[L] A transverse section (see
_Lign. 14._ fig. 1) would, of course, have a central spot, with rays
proceeding thence to the circumference, as in the oblique fracture
(_Plate I, c_).[M]
[L] Specimens of this kind form beautiful objects when polished, and
are mounted as brooches by the lapidaries of Brighton, Bognor, and
the Isle of Wight, who term them petrified sea-animal flowers. Mr. G.
Fowlstone (4, Victoria Arcade) of Ryde, has many splendid examples, and
also agates and jaspers, the genuine productions of the Island.
[M] Note VII. _Isle of Wight Pebbles._
[Sidenote: CHOANITES KONIGI.]
The form of the original zoophyte when living, must have been that of
an inverted cone or funnel, (hence the scientific name _Choanite_ or
funnel-like,) with a long cylindrical digestive cavity in the centre,
from which tubes ramified through every part of the mass. It was
attached to a rock, stone, or shell, by root-like fibres which spread
out from its base; and its soft body was strengthened, as is the case
in many sponges and animals of a similar nature, by numerous siliceous
spines or spicula, which are often found in the flint and chalk (see
_Lign. 10._ fig. 5).[N]
[N] Note VIII. _Zoophytes of the Chalk._
[Illustration: Lign. 14:--Choanites _Konigi_: from
the Chalk.
Fig. 1.--A transverse section.
2.--Upper portion of the body.
3.--Vertical section, like the pebble, Pl. II. p. 41.
4.--A flint, enclosing a Choanite, which is exposed on the
upper surface.
5.--Various forms of siliceous spines of Choanites and other
analogous bodies; magnified slightly.
(See '_Medals of Creation_,' p. 264.)
]
The _Choanites_ must have swarmed in the Chalk ocean, for in some of
the strata almost every flint exhibits traces of these zoophytes.[O]
[O] The shingle at Brighton and Bognor in Sussex, and in various
localities in the Isle of Wight, abounds in specimens more or less
perfect. I would inform my fair readers who may visit these places, and
be inclined to purchase a brooch, in illustration of these "_Thoughts
on a Pebble_," that by far the greater number of the so-called
Brighton and Isle of Wight moss-agates, jaspers, &c., sold by the
lapidaries and jewellers, are of German or Scotch origin; and that the
_false-emeralds_, and _aquamarines_, are water-worn fragments of common
green glass bottles!
[Sidenote: CORALS IN CHALK.]
[Illustration: Lign. 15:--Branch of Coral on the
Pebble.
Fig. 1.--A portion magnified.
2.--A fragment represented as when alive.
_a, a_, Two polypes collapsed.
_b, b_, Two polypes with their tentacula extended.
]
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