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1 item @ $25.00  

Schorl intergrowth with Quartz

#DL63837

Schorl intergrowth with Quartz

#DL63837
Availability
Sold
Size
11 x 8 x 5 cm - Cabinet 
Formula
NaFe2+3Al6(BO3)3Si6O18(OH)4 (RRUFF)
Locality
Midnight Owl mine, Yavapai Co., Arizona, United States
Tagged
pegmatite mineral

This specimen is illustrated on page 185, Fig. 12-6a of London's book called "Pegmatites".

This specimen of Schorl tourmaline exhibits the intergrowth with Quartz much like Quartz -Microcline graphite granite. One of the interesting features of Schorl in pegmatites is the nucleation of tourmaline along the contact zone of pegmatite with the wall-rock. At this contact tourmaline begins to grow rapidly toward the center of the pegmatite and perpendicular to the wall. Tourmaline is a cyclosilicate and crystallizes like a spiral outward from that original point of nucleation with the wall. All crystals of Schorl will compete for the boron in solution and rapid crystallization produces divergent crystals.

Illustrated in London's book "Pegmatites"

Schorl

Formula
NaFe2+3Al6(BO3)3Si6O18(OH)4 
Crystal System
Trigonal 
Crystal Habit
Acicular, Prismatic, Striated 
Cleavage
Indistinct, None, None 
Luster
Vitreous (Glassy) 
Color
black, brownish black, greenish black, bluish black 
Streak
brown 
Class
Trigonal - Ditrigonal Pyramidal 
Fracture
Brittle - Conchoidal 
Hardness
7.5 

Data courtesy of Webmineral.

Collection
Dr. David London Collection
Special Info
Illustrated in London's book "Pegmatites"
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