Specimen at a glance
| Mineral | Quartz |
|---|---|
| Chemistry | SiO2 |
| Mohs hardness | 7 |
| Crystal system | Trigonal |
| Locality | New Jersey |
| Form | Raw / rough |
| You receive | The exact specimen pictured |
About this specimen
Quartz (silicon dioxide, SiO₂) is the second most common mineral in Earth’s crust, but its crystal habit varies dramatically depending on where and how it forms. This specimen comes from New Jersey, a state famous among mineral collectors for its basalt trap-rock quarries around Paterson and the Watchung Mountains, where quartz grew alongside zeolites like stilbite and prehnite in gas cavities left behind by cooling lava, and from pegmatites elsewhere in the state that produced larger, blockier crystal habits.
This piece shows the crystal habit typical of New Jersey’s classic localities — sites that have been actively collected since the 1800s and remain well known in mineralogical literature. At Mohs hardness 7, quartz holds up well to regular handling; wipe clean with a soft, dry cloth.
An affordable way to add a genuine New Jersey locality piece to a regional or quartz-focused collection.
Inside the Quartz Crystal
One mineral species, a thousand looks — quartz is the shape-shifter of the mineral world.
The story: Quartz is the second most abundant mineral in Earth’s crust, and it crystallizes in nearly every rock-forming environment on the planet — which is exactly why it shows up in this shop as clear points, milky clusters, smoky towers, ghostly phantoms, and druzy-crusted matrix, all built from the same simple formula.
Why collectors chase it: Because one species covers this much ground: a single collection can hold a dozen genuinely different-looking quartz pieces without ever repeating a mineral. Phantom growth lines, smoky color zoning, and druzy crusts each record a different chapter of how that particular crystal grew.
Care: Quartz shrugs off scratches and most chemicals at Mohs 7, but avoid sudden temperature swings (a hot dishwasher after a cold shelf can crack a large piece) and clean with a soft, dry cloth.
Quartz: the science
- Every natural quartz crystal has a six-sided prism capped by a point, the same trigonal geometry whether it is a thumbnail or a meter long.
- Quartz is piezoelectric: squeeze it and it produces a tiny voltage. That property is why quartz keeps time in watches and electronics.
- At Mohs 7 it scratches glass and steel, which is why quartz sand is the main abrasive in nature and why quartz outlasts almost everything on a beach.
Go deeper
Want the full story on quartz: how it forms, how to identify it, and what makes a great specimen?
Questions about this piece
What is quartz?
Quartz is crystalline silicon dioxide and one of the most common minerals in Earth’s crust. Clear, well-formed points and clusters grow in open cavities and veins where silica-rich fluids had room and time to crystallize.
Where was it found?
This piece comes from New Jersey. We list a locality whenever it is known, because where a mineral formed is part of its story and its value.
How hard is it, and how should I care for it?
It rates 7 on the Mohs scale. Quartz is Mohs 7 and very durable. Dust with a soft brush or rinse in lukewarm water and air dry. Avoid knocking points together and avoid sudden temperature changes.
Is this the exact piece I will receive?
Yes. This listing was photographed individually, and you receive the exact piece shown in the photos.
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