The glass itself is in all cases remarkable for the number of minute
bubbles contained in it; in some of the lamps these bubbles are so
numerous that the material is barely to be classed as transparent. In
colour the glass varies from a pronounced bottle-green to an amber
tint; it is more rarely of a greyish white. The size of many of the
lamps and bowls must have necessitated the use of large melting-pots as
well as considerable skill in blowing and manipulation. The irregular
form so often to be observed in both lamps and vases is more likely to
be the result of a partial collapse during the melting on of the
enamels, than of any defect in the original piece as it came from the
glass-blower’s hands.
In composition, to judge from the analysis of a fragment of a Cairene
lamp made by Dr. Linke of Vienna (Schmoranz, p. 42), this Saracenic
glass is essentially a normal soda-lime silicate with 69 per cent. of
silica, 15·4 per cent. of alkali, and 8·6 per cent. of lime, thus far
resembling the ordinary Roman type. The specimen examined, however,
contained in addition to the lime as much as 4 per cent. of magnesia.
As Dr. Linke points out, the presence of this last base would hinder
the complete fluidity of the glass in the pots and make it difficult to
get rid of the bubbles. But whether the presence of this earth in a
single specimen is in itself sufficient to prove the non-Egyptian
origin of these lamps as a class is another question. The fact that
nearly one per cent. of manganese was found in this glass is of
interest, as it shows that some attempt had been made to ‘cleanse’ the
metal.
As regards the enamels on this Saracenic glass, we find that, with one
important exception, they resemble generally in composition and
character those employed at a later date by the Chinese in the
decoration of their porcelain[109]—we have a readily fusible flux
containing much lead coloured by various metallic oxides. The opaque
red is given by oxide of iron, the green by oxide of copper, and the
yellow by antimonic acid. The presence of this last substance is of
interest: Dr. Percy found antimony in the glaze of Assyrian bricks, and
I have taken for granted that it is the source of the yellow in the
primitive glass of Egypt. The opaque colours, including the white, are
probably produced by the addition of a little oxide of tin to the flux;
Dr. Linke, however, does not seem to have found that metal in his
analysis.
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