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Seraphinite: The Silver-Feathered Green Chlorite

By Digital Towns Crystals ยท Last reviewed October 8, 2026

Short answer: seraphinite is a trade name for dense, fine-grained clinochlore, a magnesium iron aluminum member of the chlorite group, whose dark green body carries silvery, feather-shaped flashes that move as the stone turns. It is very soft, Mohs 2 to 2.5, with one perfect cleavage, so it scratches and chips easily. Commercial material comes from eastern Siberia. Buy it for the shimmer, and treat it like a polished soft stone rather than a tumbler-tough pocket stone.

Why is it called seraphinite?

The name is pure marketing with a pleasant logic. Gemdat explains that seraphinite was named after the seraphim, the highest order of angels, because the chatoyant fibers in the stone look like feathers. The mineral underneath has a far plainer name. Clinochlore comes, according to Webmineral, from the Greek klino, "oblique", and chloros, "green", a nod to its monoclinic crystals and usual color.

That two-name situation matters when you research or buy. Mineral databases list clinochlore and treat seraphinite as a variety or trade name. Minerals.net marks seraphinite as a less commonly used name: a trade name for clinochlore polished with feathery chatoyancy, used as a minor gemstone. A dealer who labels a piece "seraphinite (clinochlore)" is being precise; one who calls it a rare angel mineral is selling a story.

What is seraphinite made of?

Clinochlore is a sheet silicate, built like a stack of mica-style layers with a hydroxide layer sandwiched between them. That layered structure explains almost everything about how seraphinite behaves: the softness, the pearly luster and the way thin flakes peel.

Property Clinochlore (seraphinite)
Formula (Mg,Fe)5Al(Si3Al)O10(OH)8
Group Chlorite group, phyllosilicate
Crystal system Monoclinic
Mohs hardness 2 to 2.5
Specific gravity 2.55 to 2.75 (mineral); 2.60 to 3.02 (gem tables)
Cleavage Perfect on {001}
Luster Vitreous to pearly
Refractive index 1.571 to 1.597
Tenacity Thin flakes flexible, not elastic

Clinochlore is the magnesium-rich end of a series with chamosite, the iron-rich end. Minerals.net notes that the two are difficult to tell apart, with clinochlore usually softer, lighter and more transparent. It also lists a striking cousin: kammererite, a chromium-rich clinochlore that runs pink to deep crimson, prized by collectors from the Kop Krom mine in Erzurum, Turkey. So the same mineral that makes dark green seraphinite can, with a little chromium, turn raspberry red.

Where does the feathery shimmer come from?

Seraphinite's flash is chatoyancy, the same family of optical effect that gives tiger's eye its moving band. Light reflects off many parallel, finely layered or fibrous structures at once, and the reflections add up into a bright band that slides across the surface as the angle changes. Gemdat describes a dark green to gray body with a silvery, feathery shimmer caused by mica inclusions.

What makes seraphinite different from tiger's eye is the geometry. Tiger's eye has straight, parallel fibers, so its band is straight. In seraphinite the platy grains are arranged in curving, branching sprays, so each spray lights up on its own and the stone shows feathers, fans and wing shapes instead of a single stripe. Rotate a polished piece under one lamp and individual feathers switch on and off. For the physics in more depth, see the chatoyancy guide.

The practical lesson: the effect depends entirely on cut orientation and polish. A slab cut across the feather sprays shows a lot of silver; one cut parallel to them can look flat and dull. That is why two pieces of the same rough can look like different stones.

How does clinochlore form, and where is seraphinite found?

Chlorite minerals are products of low-grade alteration. Geology.com describes chlorite as a group of common sheet silicates that form during the early stages of metamorphism, usually at temperatures under a few hundred degrees and within a few miles of the surface. Webmineral lists clinochlore's environment as contact, hydrothermal and regional metamorphism of mafic minerals. Minerals.net puts it more bluntly: clinochlore is always an alteration mineral.

In other words, seraphinite is what iron and magnesium silicates turn into when warm water works through them. Most clinochlore ends up as a dull green smear in schist or as matrix under showier crystals. Only a few deposits produce massive, coherent material with the feathered structure intact.

Among the noteworthy clinochlore localities Minerals.net names, the first is the Korshunovskoye mine at Zheleznogorsk, Russia, an iron-ore district in eastern Siberia. Seraphinite in the trade is sold as Russian material. Other classic clinochlore localities include the Fee Glacier in Switzerland, the Zillertal in Austria and Val Malenco in Italy, but these are known for crystals and specimens, not ornamental seraphinite. For more Siberian material, see the Russia origins guide.

How do you tell seraphinite from look-alikes?

Seraphinite is distinctive when the feathers are good, but green, soft, shimmery stones are easy to mix up in a tumbled bin.

Stone What it is Mohs How it differs
Seraphinite Clinochlore (chlorite group) 2 to 2.5 Dark green with silver feathers; flakes are flexible but do not spring back
Fuchsite Chromium-bearing muscovite mica 2 to 3 Brighter grass to emerald green, glittery flakes, flakes are elastic
Green aventurine Quartz with green mica flakes about 7 Hard; scattered sparkle rather than feathers
Generic chlorite schist Mixed chlorite rock 2 to 3 Dull, flaky, no organized shimmer

The elasticity test is the classic mineralogy trick. Minerals.net notes that muscovite and other micas are more elastic than chlorites: bend a thin mica flake and it springs back, bend a chlorite flake and it stays bent. You will not perform this on a finished cabochon, but rough pieces often have loose edge flakes you can test.

Fuchsite is the most common confusion. Geology.com on fuchsite describes it as a green muscovite colored by chromium substituting for aluminum, hardness 2 to 3, with green flakes that shed onto the streak plate. Fuchsite reads brighter and more yellow or emerald green, with sparkle from countless flat scales, while seraphinite is darker, bottle to forest green, with organized silver feathers. Do not rely on a scratch test here: plain muscovite, KAl2(Si3Al)O10(OH,F)2 in Webmineral's muscovite data, rates 2 to 2.5, the same as clinochlore.

Geology.com also cautions that chlorite minerals are hard to separate from each other in hand specimen, and that detailed optical, chemical or X-ray analysis is usually needed to name a particular chlorite. For seraphinite that rarely matters, because the trade name describes the look, but it is a reason to be skeptical of very confident claims on cheap unlabeled green rocks.

How should you care for seraphinite?

At 2 to 2.5 Mohs, seraphinite is about as hard as a fingernail. Household dust contains quartz grains that rate 7, so even wiping a polished face with a dry cloth can leave fine scratches over time. With a perfect cleavage, a knock on a hard surface can also lift a flake from an edge.

  • Dust with a soft brush or a blower, not a cloth.
  • Store each piece in its own soft pouch, away from quartz points and tumbled stones.
  • Do not tumble it with other stones or carry it loose in a pocket with keys or coins.
  • Avoid ultrasonic and steam cleaners, and do not soak it. Water can work into the cleavage, and any resin used to stabilize a carving may not tolerate it.
  • For jewelry, choose pendants and earrings over rings and bracelets.

Seraphinite in crystal traditions

In crystal traditions, seraphinite is associated with angels and with spiritual lightness, an idea that follows directly from its feather-like shimmer and its name. These are cultural associations, not mineral properties.

Choosing seraphinite: what to look for

Good seraphinite is about the feathers. Hold the piece under a single light and rotate it slowly. The best material has dense, bright, well-defined silver feathers across most of the surface and a deep, even green body. Lesser pieces show patchy shimmer, gray or brownish areas, or a dull face because the cut runs the wrong way across the sprays.

Check the polish closely in photos. Because the stone is so soft, many cheap pieces show fine scratches, orange-peel texture or rounded, worn edges. Gemdat's contributed photos of cut seraphinite run from about 1.92 to 59.99 carats, which reflects how it is usually sold: cabochons, small carvings and polished freeforms, not faceted gems.

  • Seraphinite: a small polished piece at an entry price, a practical way to see the feather effect in hand before paying for a larger carving.
  • Fuchsite (Rough/Unpolished): raw chromium mica. Put it beside seraphinite to compare bright, glittery mica flakes with the darker, feathered chlorite.
  • Ruby in Fuchsite Tumbles: medium tumbles of green fuchsite with red corundum, the other soft green mica stone sellers often shelve beside seraphinite.
  • Ruby in Fuchsite spheres: spheres including a 47.5 mm piece, useful for seeing how a soft green mica rock takes a large polish.

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Frequently asked questions

Is seraphinite a real mineral?

Seraphinite is a trade name, not a separate species. The mineral is clinochlore, a member of the chlorite group with the formula (Mg,Fe)5Al(Si3Al)O10(OH)8. Seraphinite describes massive clinochlore that shows silvery, feather-shaped chatoyancy when polished.

How hard is seraphinite?

Very soft. Clinochlore rates 2 to 2.5 on the Mohs scale, about the same as a fingernail, and it has one perfect cleavage. It scratches from ordinary dust and chips if knocked, so store it separately and dust it with a soft brush.

Can seraphinite get wet?

A brief splash will not dissolve it, but soaking is a poor idea. Water can work into the perfect cleavage, and some carvings are stabilized with resin that may not tolerate long immersion. Clean it with a soft dry brush and keep it out of ultrasonic and steam cleaners.

Where does seraphinite come from?

Commercial seraphinite is Russian material from eastern Siberia. Minerals.net lists the Korshunovskoye mine at Zheleznogorsk, Russia, as a noteworthy clinochlore locality. Clinochlore crystals also come from the Alps and elsewhere, but these do not show the feathered ornamental form.

What is the difference between seraphinite and fuchsite?

Both are soft green sheet silicates. Seraphinite is clinochlore, a chlorite, with darker green color and organized silver feathers. Fuchsite is a chromium-bearing muscovite mica, brighter green and glittery. Mica flakes spring back when bent; chlorite flakes stay bent.

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