The Church of Sancta Sophia, Constantinople: A Study of Byzantine BuildingLethaby, W. R. (William Richard)
Religion
The Church of Sancta Sophia, Constantinople: A Study of Byzantine Building
Lethaby, W. R. (William Richard)
Ayasofya Müzesi
_Marmor Iassense._--The “Iassian, with slanting veins of blood-red
on livid white,” was used for the phiale. Corsi identifies this with
Porta Santa, but Porta Santa, Garofalo says, came from Chios, and this
conclusion we believe is now accepted. Garofalo thought Iassian to be
the same as the Carian marble mentioned by Porphyrogenitus in his _Life
of Basil the Macedonian_, and says it was quarried on the island quite
close to the coast of Caria. A “stone mingled with streaks of red” is
also mentioned by Paulus as brought from “the Lydian Creek.” Possibly
the port of Iassus is again intended. The ordinary Lapis Lydius was a
black touchstone. The “rosy cipollino,” in which wide bands of deep
red alternate with white, used in the panelling of the aisles does not
seem to be mentioned specifically by Paulus; unless this is the Iassian
marble to which his words would very well apply. A variety of rosy
cipollino, the splendidly figured red and white marble, is obtained in
Laconia.
_Marmor Numidicum._--“The stone, nurtured in the hills of the Moors,
crocus colour glittering like gold,” is the beautiful warm yellow
African marble from Semittu Colonia, about fifty miles from Tunis, so
highly prized by the Romans, and now called giallo antico. It is used
in S. Sophia in the sectile work.
_Marmor Celticum._--“The product of the Celtic crags, like milk poured
on a flesh of glittering black,” has been identified as the Bianco e
Nero Antico, quarried in the Pyrenees.[357] The black marble with white
streaks, which occurs in some of the panels in the nave, is probably
the one to which the poet refers.
_Onychites._--“The precious onyx” mentioned by the poet is the
alabastrites or onychites of the ancients. It is the oriental alabaster
(aragonite) used in the horizontal bands of the nave, and some of the
panels. It is a translucent, fibrous stalagmite formation, generally
of a clear honey-colour. Some of the varieties are strongly veined
with white, and others are much darker. Large ancient quarries of this
Egyptian alabaster have been discovered on the east bank of the Nile.
Paulus appears to make no mention of the dusky black with dull golden
veins used in the bema apse, which closely resembles the “Porto Venere”
quarried at Spezzia.
Public-domain text, read in full here on John Shaqi.
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