Jeremejevite

Jeremejevite is a very popular mineral composed of aluminium borate. ^[1]

Jeremejevite: Quick Facts and Characteristics

Some quick facts for Jeremejevite:

• Transparency: Jeremejevite is transparent.
• Crystallography: In terms of crystallography, jeremejevite is hexagonal.
• Luster: In terms of luster, jeremejevite is vitreous (glassy).
• Streak: Jeremejevite streaks white.
• Hardness: Jeremejevite's hardness ranges from 6.5 to 7.5 on the Moh's scale.
• Specific Gravity: Jeremejevite's specific gravity ranges from 3.28 to 3.31.

Jeremejevite: Background and Summary

Jeremejevite is a rare mineral that was first discovered in 1883 in the Adun-Chilon Mountains of Siberia. It was named after Pavel V. Jeremejev, a Russian mineralogist who first identified the mineral. Jeremejevite is a complex aluminum borate mineral with the chemical formula Al6B5O15(F,OH)3. It is usually found in pegmatite veins and granite rocks, and its color ranges from colorless to pale blue, yellow, green, or brown.

One of the most distinctive features of jeremejevite is its crystal structure. The mineral forms elongated, hexagonal prisms with tapered ends, and the crystals are often transparent and highly lustrous. The prisms can reach up to several centimeters in length, and they are usually terminated by a pyramidal face. The crystals are often twinned and can be mistaken for other hexagonal minerals such as aquamarine, beryl, or topaz. However, jeremejevite has a higher specific gravity and a different crystal structure than these minerals.

Jeremejevite is a rare and valuable gemstone that is sought after by collectors and jewelry designers. Its rarity and unique crystal structure make it an attractive option for those who want to own a piece of the Earth's natural beauty. However, due to its scarcity, jeremejevite is not widely available on the market, and its price can be quite high. The gemstone is often cut into faceted gems, cabochons, or beads, and it is usually set in high-end jewelry pieces.

Jeremejevite has also been used in scientific research to study the properties of minerals and the Earth's geology. Its crystal structure and chemical composition have been analyzed using X-ray diffraction, electron microscopy, and other techniques, providing valuable insights into the formation and evolution of minerals in the Earth's crust.