
Herkimer Diamond
Silicon dioxide (SiO2)
Exceptionally clear, naturally double-terminated quartz crystals from Herkimer County, New York, prized for their diamond-like brilliance.
- Mohs hardness
- 7
- Color
- colorless and water-clear
- Type
- crystal
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Overview
Herkimer diamonds are not diamonds at all but exceptionally clear, brilliant double-terminated quartz crystals. They earned the name for their natural facets and water-clear sparkle that mimic cut gemstones.
They are named for Herkimer County, New York, where they occur in Cambrian dolostone. Their hallmark is that they grow with points (terminations) on both ends, free-floating in rock cavities, rather than attached to a matrix at one end.
Genuine Herkimer diamonds come specifically from this New York region, though similar double-terminated quartz from elsewhere is sometimes loosely (and incorrectly) sold under the name. They often contain interesting inclusions of water, carbon, or hydrocarbons.
Formation & geology
Herkimer diamonds formed in cavities (vugs) within a Cambrian dolostone roughly 500 million years old. Silica-rich solutions slowly crystallized inside these pockets, where the crystals could grow freely suspended in the cavity.
Because they grew unattached, they developed natural terminations on both ends and unusually clear, well-formed faces. The surrounding dolomite host and tarry hydrocarbon pockets sometimes produced inclusions of liquid water, bitumen, or carbon within the crystals.
The classic localities lie around Herkimer County, New York, especially near Middleville and Little Falls, where collectors break the crystals from the dolostone matrix. The defining "Herkimer" character comes from this specific geological setting.
How to identify it
Look for small, water-clear, doubly-terminated quartz crystals with naturally sharp, glassy facets and a stubby, brilliant form. The crystals are hard (Mohs 7) and scratch glass.
Key traits: points on both ends, exceptional clarity, and often internal inclusions (water bubbles, black anthraxolite/carbon specks, or rainbow fractures). Streak is white; no acid reaction.
Distinguish from real diamond by hardness (diamond is 10) and by the hexagonal quartz crystal habit. Many "Herkimer-style" crystals sold online are double-terminated quartz from other countries (e.g., China, Pakistan); only crystals from the Herkimer, New York area are true Herkimer diamonds. Glass imitations show bubbles and mold seams, not natural quartz faces.
Uses & significance
Herkimer diamonds are used in jewelry as natural, often unfaceted gems in pendants, rings, and earrings, prized for their built-in brilliance and clarity. Their double points make them attractive for wire-wrapped and artisan designs.
They are also popular collector and specimen crystals, valued for clarity, well-formed terminations, and interesting inclusions such as enhydros (water bubbles).
In metaphysical traditions they are associated with clarity, energy amplification, and attunement; these are spiritual beliefs rather than scientific facts. As durable quartz (hardness 7) they wear well, though the small natural crystals are often left in their raw form rather than cut.
Frequently asked questions
Are Herkimer diamonds real diamonds?
No. They are exceptionally clear, double-terminated quartz crystals; the name comes from their diamond-like sparkle and natural facets.
Why are they called Herkimer diamonds?
They are named for Herkimer County, New York, where these distinctive clear quartz crystals are found in Cambrian dolostone.
What makes Herkimer diamonds special?
They grow naturally double-terminated (pointed on both ends) and are unusually clear, often with water, carbon, or rainbow inclusions.
Is double-terminated quartz from China a real Herkimer diamond?
Not strictly. Only double-terminated quartz from the Herkimer, New York area is a true Herkimer diamond; other localities are similar but different.
Herkimer Diamond guides
In-depth guides for identifying, valuing, and understanding Herkimer Diamond.











