temperature. The theory is, however, confirmed by the results obtained
by workers on the subject of mineralogical synthesis, who have shown
that the material which has been produced at high temperatures has the
specific gravity and other physical properties of the mineral
anhydrite.

It was formerly supposed that plaster prepared by baking at a
temperature above 300 degrees loses completely its power of setting.
Later observations, however, as those of Landrin, negative this view.
Between 300 degrees and 400 degrees Landrin obtained plasters setting
almost instantaneously when mixed with a small amount of water. When
the temperature employed approached 400 degrees, the set plaster was
softer, but the setting still took place quickly. These observations
appear to show that the change to anhydrite is a very gradual process
at temperatures below a red heat.

Reference has been made to the differences in (1) time of setting of
plaster and (2) in hardness of the resulting material. Both of these
properties are affected by the mode of baking. The hardest material is
frequently obtained from the quick-setting plasters, but for certain
purposes this rapidity in setting is of great practical inconvenience.
Thus the moulder in pottery work must have leisure to fill in every
detail of a design often complicated and intricate before the material
with which he is working becomes intractable. Thus for many of the
more refined purposes to which plaster is applied, extreme hardness in
the set plaster is of less vital importance than a convenient period
of setting. On the other hand, plasters which set very slowly give as
a rule too soft a material, as well as being inconvenient in use.
Plasters which hit off the happy medium are alone suitable for the
work of the potter. The finer varieties of plaster prepared especially