This specimen features a fine example of Faden Quartz, a distinct growth formation characterized by its visible white thread-like "faden" running through the crystal structure. Originating from high-altitude alpine clefts in northern Pakistan, this formation reflects episodic crystal growth interrupted by tectonic movement—an interplay of stress and recovery uniquely recorded within the quartz itself.
The piece exhibits excellent clarity, sharp crystal edges, and an elegant, elongated formation. Mounted on an acrylic base, it offers a stable, gallery-style presentation that highlights the internal faden line and the specimen’s natural symmetry.
Faden Quartz with visible central thread-like inclusion
Excellent optical clarity with well-formed, flattened tabular crystals
Composed of silicon dioxide (SiO₂) with typical alpine vein genesis
Formed under tectonic stress, indicative of dynamic geological environments
Approximate dimensions: 7 x 6 x 2 cm
Sourced from alpine cleft zones in northern Pakistan
Mounted on a minimalist acrylic base for unobstructed viewing
An exceptional addition for collectors interested in structural mineralogy, crystallographic phenomena, or alpine quartz varieties with visual and geological significance.
