174 M. Delesse on Gilobuliferous Rocks. 
The calcareous include pisolites, the priapolites of Castres, the 
kupstein of the Loess, ete. ere are also the ferruginous, con- 
traction while the mass within was ina pasty state. Such cavi- 
1 of the cavities. Hence the cavities must have been ” f 
during the state of partial fusion, before the crystallization © 
these minerals took place. sei 
rom the characters. of the cavities and their surfaces, wie 
water while the globules were still in a liquid state. It might 
objected to this view that normal and abnormal globules often 
occur together. Still the presence of water is altogether proba 
