Rock Identifier

Carey Plume Agate Identification Guide

How to identify Carey Plume Agate by its feathery mineral plumes in translucent chalcedony, and tell it from moss and dendritic agates.

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Carey Plume Agate Identification Guide

What Carey Plume Agate Looks Like

Carey Plume Agate is a prized plume agate from the Carey Ranch area of Oregon. It is a translucent chalcedony (microcrystalline quartz) hosting delicate, three-dimensional plume inclusions that resemble feathers, smoke, or coral suspended in the stone.

  • Color: plumes are typically red, pink, golden, orange, or black set in a clear-to-milky or pale-blue background.
  • Luster: waxy to vitreous.
  • Transparency: translucent body so the plumes show through.
  • Texture: branching, billowing 3-D mineral growths (often iron/manganese oxides), distinct from flat dendrites.

Step-by-Step Field-ID Checklist

  1. Confirm it is chalcedony: waxy luster, conchoidal fracture, no crystal faces, very hard.
  2. Backlight the stone: genuine plume agate shows the plumes floating in three dimensions inside translucent chalcedony.
  3. Examine the inclusions: look for soft, feathery, billowing forms rooted to a point — not flat tree-like patterns.
  4. Hardness test: scratches glass easily (Mohs ~6.5–7).
  5. Check for the host material context: Oregon plume agates form in volcanic (rhyolite/tuff) host rock seams and nodules.

Key Diagnostic Tests

  • Mohs hardness: about 6.5–7; will scratch glass and steel.
  • Streak: white.
  • Fracture: conchoidal, with sharp edges.
  • Cleavage: none.
  • Acid: no reaction (silica, not carbonate) — separates it instantly from any carbonate look-alike.
  • Density: ~2.6 g/cm³.

Common Look-Alikes

  • Moss agate: inclusions form irregular mossy or web-like masses, not organized feathery plumes anchored to a base.
  • Dendritic agate: inclusions are flat, fern- or tree-like manganese dendrites grown along a plane, not 3-D plumes.
  • Other Oregon plume agates (e.g., Graveyard Point, Priday): very similar; provenance and plume color/style distinguish them, but all share the same plume structure.
  • Glass imitations: show bubbles, swirl, and lack the natural rooted-plume geometry.

Where Carey Plume Agate Is Found

The namesake material comes from the Carey Ranch / central and southeastern Oregon high desert, occurring in seams and nodules within volcanic tuffs and rhyolite. It is a collector and lapidary favorite, often cut into cabochons that frame the plumes.

Frequently asked questions

What is Carey Plume Agate?

It is a translucent chalcedony from the Carey area of Oregon containing feathery, three-dimensional mineral plumes — usually iron/manganese oxides — that look like smoke or coral suspended inside the stone.

How is plume agate different from dendritic agate?

Plume agate inclusions are billowing, three-dimensional, feather-like growths rooted to a point, while dendritic agate has flat, fern- or tree-shaped manganese patterns grown along a single plane.

How can you tell real Carey Plume Agate from glass?

Real plume agate is hard (scratches glass), shows a waxy conchoidal fracture, and contains natural rooted plumes. Glass imitations show bubbles, mold swirl, and uniform color.

Is Carey Plume Agate valuable?

Yes among collectors and lapidaries; well-defined colorful plumes in clean translucent chalcedony command premium prices, especially as finished cabochons.