Rock Identifier
Plume Agate (Silicon dioxide (SiO2))
gemstone

Plume Agate

Silicon dioxide (SiO2)

A translucent agate containing delicate three-dimensional feather- or plant-like plumes of mineral inclusions suspended in chalcedony.

Mohs hardness
6.5-7
Color
translucent to white base with red, pink, yellow, black or green plumes
Type
gemstone

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Overview

Plume agate is a variety of agate characterized by soft, feathery, three-dimensional inclusions that resemble plumes, feathers, or sprigs of vegetation suspended within translucent chalcedony. Unlike flat dendrites, true plumes have a billowy, branching structure that appears to float in the stone.

The plumes can be red, pink, yellow, white, black, or green depending on the mineral that formed them, often iron and manganese oxides. Each piece is unique, and well-formed plumes are highly prized by lapidaries.

Classic American plume agates come from Oregon and Texas localities.

Formation & geology

Plume agate forms when silica-rich solutions fill cavities in volcanic rock, while at the same time small amounts of metal-bearing minerals crystallize within the gel as it solidifies. These mineral growths develop the characteristic feathery, three-dimensional shapes before the chalcedony fully hardens around them.

The plumes are true inclusions distributed through the body of the stone, not surface staining. Iron oxides typically yield red, orange, or yellow plumes, while manganese produces black plumes.

Famous deposits include Graveyard Point and Priday in Oregon, and Woodward Ranch and the Big Bend area of Texas.

How to identify it

Look for translucent chalcedony containing soft, branching, feather-like inclusions that have visible depth when the stone is rotated, distinguishing plumes from flat, two-dimensional dendrites or moss inclusions.

The base is hard chalcedony with a waxy luster, conchoidal fracture, white streak, and hardness 6.5-7. Look-alikes include moss agate (more tangled, mossy filaments) and dendritic agate (flat, fern-like manganese dendrites on planes).

Plumes appear three-dimensional and feathery, while dendrites look painted onto a plane.

Uses & significance

Plume agate is a favorite lapidary material, cut into cabochons, slabs, and display pieces that showcase the suspended plumes. Cutting orientation is critical to capture the best plume view, so cut stones can carry significant value.

It has no industrial application and is purely ornamental and collectible. Fine Oregon and Texas plume agates are sought after by collectors.

In metaphysical use it is linked to growth and renewal because of its plant-like appearance, though this is symbolic rather than scientific.

Frequently asked questions

What is the difference between plume agate and dendritic agate?

Plume agate has three-dimensional, feathery inclusions floating in the stone, while dendritic agate has flat, fern-like dendrites on a plane.

What causes the plumes in plume agate?

They are inclusions of metal-bearing minerals, often iron and manganese oxides, that grew within the silica before it fully hardened.

Where does plume agate come from?

Classic sources include Graveyard Point and Priday in Oregon and Woodward Ranch in Texas.

Is plume agate good for jewelry?

Yes. At 6.5-7 Mohs it is durable, and its unique plumes make attractive cabochons and pendants.

Plume Agate identified by the community

Real specimens identified with Rock Identifier.

Chalcedony (Agate/Chert)AgateAgate (Chalcedony)AgateChalcedony (Agate)Chalcedony (Agate)Chalcedony (Common Agate)Agate (Moss or Plume Agate variety)Plume AgateAgate (Chert/Chalcedony)Chalcedony (Botryoidal Agate)Chalcedony (Agate/Chert)