[No. 62]. This exquisite crystal might well suggest a jewelled brooch or pendant of rare workmanship. It began its formation in a very high altitude, where the solid, hexagonal centre was formed, started to descend in plain hexagonal form, but was caught upwards by the rushing clouds, tossed about awhile, and then allowed to pass into a lower, warmer altitude where its elaborated branches were added.
[No. 63]. A high, frigid-altitude crystal, notable for its delicately traced centre design, and the six curious, apparently raised formations in the plainer spaces.
[No. 64]. Remarkable for its six beautiful prism-like rays, and central wheel-like structure.
[No. 65]. An exquisitely designed centre, with air inclusions strongly marked.
[No. 66]. This crystal has been formed of two sections, and must have encountered another broken crystal in its travels, with which it united, and from this its crystalline growth formed.
[No. 68]. An oddity. The air inclusions are very strongly marked and bring into sharp relief its rare central design.
[No. 69]. A local-storm type. These crystals are always loose and feathery in construction.
94. Old snow, re-crystallized
