125 



but they may nevertheless be grouped rather naturally round 

 two types. 



Type 1 comprises Winther' s principal form from Tu top 

 Agdlerkofia, and also the well developed crystals by Flink 

 designated as «rhodonite-like» from Range rd luar suk. They 



Fig. 8. Schizolite. 



are of a rather well-marked shape always lengthened after the 

 è-axis, and also often flattened after a{lOO). The most com- 

 mon combination is given in figure 8. 



Here are found a{lOO}, è{010), c{00l}, i¥{lTo}, n{\Q\], 

 and r{l02}. The faces M and Ъ are often of about the same 



Fis. 9. Schizolite. 



size, but they do not, however, appear symmetrical, as the 

 angle, formed by ^*{oio} with a{lOO} is 21V2° larger than the 

 angle between Ж(110} and «{lOO}. Besides these faces 

 m{ll0} and o{530) may more rarely be found, as shown in 

 figure 9. 



