K\Pl.ANATIt)X OK PLATK X. 



Biiula Meteorite. 



The plioto<i:ra])li shows the front of tlie meteorite, the 

 wliite cross iiulicatiiior the point from which the lines 

 of crustal flow radiate. The area between A and B 

 shows the " tertiary " ci'iist, formed just befoi-e the 

 stone reached the ground. The rest of the surface is 

 invested with secondary crust. About three-tiftlis 

 natural size. 



