M. E. Wadsworth—Bishopville Meteorite. 35 
quartz. These glass inclusions are of various dimensions an 
many contain a small bubble. Some microlites were also seen. 
In the feldspar at one end of a section the enstatite was 
found in minute crystals extending outward from a center 
forming stellate or rosette-like forms. The structure is like 
that observed in terrestrial rocks in minerals formed from 
alteration or solution. This apparently might have been pro- 
duced in this case, either by the rapid crystallization of enstatite 
material of a liquid feldspathic mass, or by secondary alteration 
through water action on the rock itself. The absence of any 
other signs of alteration, except in the ferruginous materials, 
seems to negative the latter supposition. The ferruginous 
ene these masses are like olivine, they are referred to that 
n 
This stone in its mineralogical composition, its structure, 
bubble-bearing glass-inclusions, and microlites is like terrestrial 
