CHAP. 57. (17.)—CRETACEOUS EARTHS USED FOR SCOURING CLOTH.
CIMOLIAN EARTH; NINE REMEDIES. SARDINIAN EARTH. UMBRIAN
EARTH. SAXUM.
Of cretaceous[1] earths there are several varieties; and among
them, two kinds of Cimolian earth, employed in medicine, the
one white and the other inclining to the tint of purpurissum.[2]
Both kinds, moistened with vinegar, have the effect of dispersing
tumours and arresting defluxions. They are curative
also of inflammatory swellings and imposthumes of the parotid
glands; and, applied topically, they are good for affections of
the spleen and pustules on the body. With the addition of
aphronitrum,[3] oil of cypros,[4] and vinegar, they reduce
swellings of the feet, care being taken to apply the lotion in
the sun, and at the end of six hours to wash it off with salt
and water. In combination with wax and oil of cypros,
Cimolian earth is good for swellings of the testes.
Cretaceous earths, too, are of a cooling tendency, and,
applied to the body in the form of a liniment, they act as a
check upon excessive perspiration: taken with wine, in the
bath, they remove pimples on the body. The most esteemed
of all these earths is that of Thessaly: it is found also in the
vicinity of Bubon[5] in Lycia.
Cimolian earth is used also for another purpose, that of
scouring cloth. As to the kind which is brought from Sardinia,
and is known as "sarda," it is used for white tissues
only, and is never employed for coloured cloths. Indeed, this
last is held in the lowest estimation of all the Cimolian earths;
whereas, that of Umbria is more highly esteemed, as also the
kind generally known as "saxum."[6] It is a property of
this last to increase in weight[7] by maceration, and it is by
weight that it is usually sold, Sardinian earth being sold by
measure. Umbrian earth is only used for giving lustre to
cloths.
It will not be deemed out of place to give some further
account here of this process, there being still in existence the
Metilian Law, relative to fullers; an enactment which C.
Flaminius and L. Æmilius, in their censorship,[8] had passed by
the people,[9] so attentive to everything were our ancestors.
The following then is the method employed in preparing
cloth: it is first washed in an infusion of Sardinian earth, and
is then exposed to a fumigation with sulphur. This done, it is
scoured[10] with Cimolian earth, when the cloth has been found
to be of a genuine colour; it being very soon detected when it
has been coloured with spurious materials, by its turning
black and the colours becoming dispersed[11] by the action of the
sulphur. Where the colours are genuine and rich, they are
softened by the application of Cimolian earth; which brightens
and freshens them also when they have been rendered sombre
by the action of the sulphur. Saxum is better for white tissues,
after the application of sulphur, but to coloured cloths it is
highly injurious.[12] In Greece they use Tymphæan[13] gypsum in
place of Cimolian earth.
1. Cimolian earth, known in modern chemistry as Cimolite, is not a cretaceous earth, but an aluminous silicate, still found in the island of
Kimoli, or Argentiera, one of the Cyclades; See B. iv. c. 23. Tournefort
describes it as a white chalk, very heavy, tasteless, and dissolving in
water. It is found also at Alexandrowsk in Russia.
2. See Chapter 25 of this Book.
3. See B. xxxi. c. 46.
4. See B. xii. c. 51.
5. See B. v. c. 28.
6. Beckmann thinks that this may have been our common chalk.
Vol. II. p. 105.
7. This seems to be the meaning of "crescit in macerando."
8. A.U.C. 535, it is supposed.
9. As a plebiscitum.
10. "Desquamatur." This is most probably the meaning of the word,
though Beckmann observes "that it was undoubtedly a term of art, which
cannot be further explained, because we are unacquainted with the operation
to which it alludes."—Vol II. p. 104. Bohn's Edition.
11. " Funditur sulphure." The meaning of these words is very doubtful.
Beckmann proposes to read "offenditur," but he is not supported
by any of the MSS. He has evidently mistaken the meaning of the
whole passage.
12. Probably because it was too calcareous, Beckmann thinks.
13. See B. iv. c. 3, and B. xxxvi. c. 59.