Rowley Mine Arizona Chrysocolla Cabochon Polished Copper Mineral Gemstone Cab Southwestern Lapidary

A beautiful polished Chrysocolla cabochon sourced from the historic Rowley Mine in Arizona, showcasing the vivid copper-rich mineralization and striking Southwestern colors that have made Arizona chrysocolla world renowned among lapidary artists and mineral collectors.

Located in Arizona's historic mining region, the Rowley Mine is known for producing visually stunning copper minerals featuring rich blues, greens, turquoise tones, and complex matrix patterns formed through the oxidation of copper-bearing deposits. Material from this region has long been prized for both jewelry use and collector lapidary work due to its vibrant coloration and unique natural patterns.

This polished cabochon displays the smooth domed finish and dimensional color contrast sought after by collectors, jewelers, and lapidary enthusiasts alike. Chrysocolla from Arizona is especially admired because of its association with some of the most legendary copper mining districts in the American Southwest.

Features

• Genuine Rowley Mine Arizona Chrysocolla
• Polished cabochon finish
• Copper-rich blue and green coloration
• Natural mineral matrix patterns
• Excellent display and jewelry potential

Perfect For

• Lapidary collections
• Jewelry making
• Southwestern mineral collections
• Arizona mining memorabilia
• Copper mineral enthusiasts
• Wire wrapping and custom silversmith work
• Museum and educational displays

Arizona chrysocolla remains one of the most recognizable and collectible copper-associated minerals in the world due to its vivid natural beauty and strong connection to historic American mining regions.

Measurements & Weight

• Dimensions: 54 x 18 x 4 mm
• Weight: 9.8g / 49.4 carats

Condition

Please review all photos carefully for overall condition, polish quality, natural inclusions, matrix features, and color characteristics, as they are considered part of the description. Natural chrysocolla commonly displays inherent fractures, matrix variation, and mineral inclusions formed during geological growth.