
Mineral
Blue Chalcedony
Chalcedony (a cryptocrystalline variety of Quartz - SiO₂)
Hardness: 7 (Mohs scale) for quartz, varies slightly for chalcedony varieties. Color: Typically light blue to bluish-gray, but can range from colorless to white, gray, and other pastel shades. Luster: Waxy to vitreous (glassy).…
- Luster
- Waxy to vitreous (glassy)
Identified More mineral →
Identify your own rocks.
Get a report just like this from any photo, free.
Physical properties
Hardness: 7 (Mohs scale) for quartz, varies slightly for chalcedony varieties. Color: Typically light blue to bluish-gray, but can range from colorless to white, gray, and other pastel shades. Luster: Waxy to vitreous (glassy). Crystal Structure: Cryptocrystalline (microscopic crystals that are not visibly discernable). Cleavage: None. Specific Gravity: 2.58 - 2.64.
Formation & geological history
Blue Chalcedony forms from the slow deposition of silica-rich water in cavities and fissures within existing rocks. It's often found in volcanic rocks (like basalts and andesites) and sedimentary environments where silica-rich fluids permeate. The precise blue color is often attributed to the presence of micro-inclusions, possibly of certain minerals or very fine scattering of light due to its microstructure. Geological age can vary widely depending on the specific deposit, ranging from relatively recent to millions of years old.
Uses & applications
Blue Chalcedony is primarily used as a gemstone in jewelry (cabochons, beads, carvings) and for ornamental objects. It is also collected by mineral enthusiasts.
Geological facts
Blue Chalcedony, particularly varieties like 'Blue Lace Agate,' are popular in lapidary arts and for ornamental purposes. It's often associated with tranquility, communication, and calm in metaphysical beliefs.
Field identification & locations
In the field, you can identify Blue Chalcedony by its characteristic waxy luster, often light blue to grayish-blue color, and its translucent to opaque appearance. It typically forms in botryoidal, mammillary, or stalactitic habits, or as massive fillings. Its hardness of 6.5-7 can be tested by scratching glass. Common locations include Namibia, Turkey, Brazil, the United States (California, Oregon), and some parts of India. When collecting, look for pieces with good color saturation and a pleasing shape. Tumbled specimens like the one shown are often found in rock shops and metaphysical stores.
More like this
Other mineral specimens
Sandstone (with potential mineral staining/concretions)
Arenite (SiO2 based)
sedimentary
Epidote
Epidote | Ca2(Al2,Fe3+)(SiO4)(Si2O7)O(OH)
metamorphic
Nephrite Jade
Nephrite
Mineral/Rock
Banded Gneiss (River Rock/Pebble)
Gneiss (specifically a banded variety often found as a river rock)
Metamorphic Rock
Green Apatite on Albite
Fluorapatite [Ca5(PO4)3F] on Albite [Na(AlSi3O8)]
mineral
Epidote
Epidote - Ca2(Al2,Fe3+)3(SiO4)3(OH)
mineral