Rock Identifier
Hag Stone (Flint with natural hole) (Silicon Dioxide (SiO2) - Nodular Chert / Flint) — sedimentary
sedimentary

Hag Stone (Flint with natural hole)

Silicon Dioxide (SiO2) - Nodular Chert / Flint

Hardness of 7 on the Mohs scale, waxy to dull luster, conchoidal fracture, grayish-blue to brown color with a chalky outer cortex and a naturally eroded hole through the center.

Identified More sedimentary
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Physical properties

Hardness of 7 on the Mohs scale, waxy to dull luster, conchoidal fracture, grayish-blue to brown color with a chalky outer cortex and a naturally eroded hole through the center.

Formation & geological history

Formed in Cretaceous chalk deposits from the accumulation of microscopic silica-rich sponge spicules and radiolarians. The hole is created through long-term water erosion, wave action, or the decay of an ancient organism trapped in the nodule.

Uses & applications

Historically used as protective amulets in folklore to ward off evil spirits and bad dreams. Also collected by rockhounds, used in natural crafts, and made into pendants.

Geological facts

Hag stones (also known as adder stones, witch stones, or holey stones) have a rich history in Celtic and European folklore. Legend holds that looking through the hole allows a person to see the fairy realm or reveal hidden truths.

Field identification & locations

Easily identified by a naturally occurring hole worn entirely through a hard flint or chert matrix. Commonly found along UK beaches, northern European coasts, and chalk beds.