mineral

Blue Agate (Dyed Chalcedony)

Silicon Dioxide (SiO2)

Hardness: 6.5–7 on Mohs scale; Color: Intense blue with lighter banding; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None; Specific Gravity: 2.58–2.64

Hardness: 6
Color: Intense blue with lighter banding
Luster: Waxy to vitreous

Identified April 22, 2026More mineral →

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Physical properties

Hardness: 6.5–7 on Mohs scale; Color: Intense blue with lighter banding; Luster: Waxy to vitreous; Crystal structure: Trigonal (microcrystalline); Cleavage: None; Specific Gravity: 2.58–2.64

Formation & geological history

Agates form in the cavities of volcanic rocks or ancient lavas. While the chalcedony itself is millions of years old, the vibrant uniform blue in many small tumbled stones is typically achieved through modern dyeing techniques because natural blue agate is rare and usually pale grayish-blue.

Uses & applications

Used primarily for jewelry (cabochons, beads), decorative ornaments, collection, and in alternative healing practices as a 'soothing stone'.

Geological facts

Naturally occurring blue agate, such as Blue Lace Agate, features delicate white banding. Most solid, vibrant blue agates on the market are dyed to enhance their visual appeal, taking advantage of the mineral's porous nature.

Field identification & locations

Identify in the field by its conchoidal fracture, waxy luster, and hardness (it will scratch glass). Tumbled specimens like this one are common in gift shops and mineral kits. Natural versions are famously found in Brazil, Uruguay, and Namibia.

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