Looking for genuine Healing Crystals, natural Tumblestones, Jewellery, Meteorites (Space rocks) and Fossils? Look no further than My Lost Gems. Our extensive collection of nature’s hidden treasures is carefully selected for high quality and authenticity, and each item comes with a certificate of authentication. We offer a unique “buy what you see” shopping experience. With new products constantly being added, My Lost Gems is your go-to source for one-of-a-kind hidden gems. Shop now and discover the wonders of the earth.

FREE UK DELIVERY - Save up to 60%

Hackmanite

Hackmanite is a variety of the mineral sodalite, belonging to the feldspathoid group of minerals. What sets hackmanite apart is its unique ability to exhibit tenebrescence, a phenomenon where the mineral’s color changes when exposed to ultraviolet (UV) light. In the case of hackmanite, exposure to UV light often induces a striking transformation from a pale or colorless appearance to shades of pink, violet, or lavender.

The name “Hackmanite” is derived from the Finnish mineralogist Victor Axel Hackman, who extensively studied the mineral. The tenebrescent property of hackmanite is reversible; upon prolonged exposure to daylight or heat, the altered color fades gradually.

Hackmanite is typically found in sodalite-rich rocks, often associated with other minerals such as lazurite, nosean, and hauyne. It can be discovered in various geological settings, including alkaline igneous rocks and metamorphic environments.

Beyond its geological significance, hackmanite is highly valued for its unique optical properties. Gem-quality hackmanite, particularly those displaying strong tenebrescence, is sought after by collectors and lapidaries. The changing colors under UV light make hackmanite an intriguing and aesthetically appealing mineral.

As with any mineral, the availability, color-changing intensity, and other characteristics of hackmanite specimens may vary. For accurate and detailed information, it is advisable to consult current mineralogical references and geological literature.