r.lM'A ,MKTKn|;ri'K__.ANI)Ki;S(i\ AM> MINdAYK 



51 



The twt) jiortioiis iiu'iisiu'e res|)ectively H^ inches X 7 inches 

 X 3 inches (fi'ont to back) and (J^ inches X 5^ inclies X 3 

 indies ('rcchnoloo'ical Miiseiuii portion). 



The spccitic uraxitv is .S.25. 



M iiTiisi-tijiii- ( 'liiirnch-rs. — The stone is rathei' t'l'iahU", and (lie 

 section prepared is nnduly tliick. Tlie only constituents 

 identifiable under the microscope are anoi'tliite, hypei'sthene, 

 clironiite and specks of nickel -iron. The sti-ucture is 

 holocrystalline ; thei'e is no sign of chondrules. 



( 'licitili-dl r/iiii-iirtrrs. — Analysis yielded tlie following figures: 



100.22 



