320 PROCEEDINGS OF THE AMERICAN ACADEMY. 



b: (5276) = (6lT). This scalenohedron was recorded by Moesz 84 

 on crystals from Korosmezo, Hungary. The form which is referable 

 to normal series N 4 falls at the intersection of a number of well marked 

 secondary zones. It should be ranked as probable. 



The following scalenohedrons have been recorded in the zone 

 fragment between the limits (1232) = (211) and (0221) = (111): 



S t\ f: J: 9: V: t: t\ ui mi 



<P 



Form ?211 955 533 322 755 433 544 655 988 111 



1 



Referred to N4 this zone fragment is very incomplete and contains 

 the extra form §. 



mi (1-16 -17 -9) = (988). This form, appointed out by Irby, was 

 substituted by Zippe 85 for (1453) = (322) in Levy's 86 figure of a 

 Derbyshire occurrence. Irby favors discarding the figure of Levy 

 on the ground that the zonal relations shown in the drawing do not 

 conform to the indices assigned. The form must be regarded as 

 doubtful. 



Zone 5 — Scalenohedrons of the Zone [0221 : 1120] = [111 : 101] 



Symbol - • 



This portion of the zone [lOTl : 0221 : 1120] can be developed as a 

 whole without splitting: 



ip._ i)'_ ni_ n^ pi_ q_ ti ri_ f: o_ 



Form 111 434 323 535 212 313 11-3-11 414 515 101 



Symbol 1 f § § 2 3 x 3 l 4 5^ 



v-l J i I 1 2 f 34co 



N 3 " i I I 1 • 2 (f) 3 (4) co 



Referred to N3 this zone fragment is nearly complete and contains 

 the extra forms ^ and 5. 



84 Moesz, G., Fold.'Kozlony, 27, 495 (1897). 



85 Zippe, loc. cit., Fig. 15. 



86 Levy, A., Description d'une collection des mineraux formee par M. 

 Heuland, London, Fig. 122 (1837). 



