Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions
Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions
Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions
Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions
Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions
Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions
Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions
Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions
Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions
Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions

Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions

Precio de venta$250.00

Dimensions: 39.9 mm x 18.7 mm x 8.7 mm

This raw, unpolished Larimar specimen showcases the mineral’s signature soft blue-green coloration with natural matrix inclusions and earthy tones. Mined in the Dominican Republic, the only known source of Larimar, this piece highlights the stone's volcanic origin and unique geological features. The visible striations and matrix patterns add to its authenticity and raw charm, making it a perfect addition for collectors, educators, or those drawn to the natural beauty of untouched minerals. With a substantial weight of 83.69g and dimensions of 57.4 x 58.2 x 24.4mm, this piece stands as a testament to Larimar’s tranquil aesthetic and organic beauty.

 

Cantidad:

Unraveling the Beauty and Rarity of this Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions

Larimar, a rare gem exclusive to the Dominican Republic, embodies the serenity of the ocean with its dreamy blue-green hues. This raw specimen boasts unpolished natural beauty, enhanced by its earthy matrix and volcanic inclusions. Its uniqueness lies in the harmonious interplay of mineral colors and textures, making it a sought-after piece for collectors and admirers of Earth's geological wonders.

Additional Information about this Raw Larimar Specimen 83.69g with Earthy Matrix Inclusions

  • Very good (VG)
  • Dominican Republic
  • Triclinic
  • Primarily formed during hydrothermal activity in the Tertiary period
  • Occurs in cavities within basalt flows