Quartz - Exceptional Water-Clear Focal Crystal with Anatase Inclusion

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A commanding Himalayan quartz crystal group from Pakistan, distinguished by exceptional clarity and luster, imposing crystal size, and an unusually balanced composition centered upon a magnificent dominant quartz crystal.

The specimen's defining feature is the large, vertically oriented focal quartz crystal, which rises dramatically from the center of the cluster. Exceptionally well proportioned, the crystal possesses a long prismatic body culminating in a sharply developed pyramidal termination. Its placement is particularly effective: the principal crystal occupies the visual center of the specimen and towers above the surrounding quartz, producing a strong, almost architectural silhouette.

The quality of the quartz is outstanding. Much of the main crystal is remarkably transparent and water-clear, allowing an unobstructed view through substantial portions of the prism. Broad faces exhibit superb glassy to mirror-bright vitreous luster, with crisp reflections emphasizing the crystal's geometry. Fine horizontal growth striations across the prism faces provide natural texture while preserving the exceptional transparency.

The termination is similarly impressive, consisting of large, well-developed faces that converge to a sharp apex. Within the upper portion of the main crystal are several small dark inclusions, including a particularly interesting anatase inclusion near the termination. This subtle mineralogical feature adds considerable interest to an otherwise extraordinarily clear crystal, providing a discreet internal accent without compromising the specimen's overall brilliance.

Surrounding the dominant crystal is a beautifully arranged assemblage of smaller transparent quartz points. Rather than competing with the centerpiece, these subsidiary crystals form a natural pedestal around it, creating both depth and visual balance. Particularly striking is the substantial laterally projecting quartz crystal extending outward from one side of the group. Its horizontal orientation provides an effective counterpoint to the strong vertical line of the main crystal and gives the entire specimen a more dynamic three-dimensional structure.

The surrounding crystals display similarly bright luster and good transparency, with numerous sharply defined terminations and intersecting growth orientations. Subtle internal veils, reflective fractures, minute dark inclusions, and occasional flashes of spectral color provide additional visual interest when the specimen is viewed under directional lighting.

A restrained amount of darker matrix remains beneath the quartz group, with pale to slightly greenish mineralization visible around portions of the base. This natural matrix provides useful contrast and geological context while remaining subordinate to the exceptionally transparent crystal architecture above it.