This visually striking specimen showcases a dynamic combination of vibrant amazonite, sharply formed smoky quartz, and contrasting black goethite, all set atop a solid feldspar matrix from the renowned Pikes Peak region of Colorado.
A dense spread of blocky amazonite crystals dominates the surface, displaying a rich, saturated blue-green color with classic Pikes Peak form. These crystals are well-developed and tightly clustered, creating a textured, layered landscape across the top of the specimen.
Emerging between the amazonite are multiple smoky quartz crystals, ranging from translucent gray to deeper smoky tones. Their glassy luster and defined terminations provide depth and contrast, drawing the eye across the piece.
What sets this specimen apart is the presence of goethite, appearing as dark, metallic, radiating aggregates perched among the amazonite and quartz. These sculptural formations introduce a bold visual contrast and add a layer of mineralogical rarity not commonly seen in standard amazonite–smoky quartz associations from this locality.
Size: 5.25” x 2.5” x 2.25”
Weight: 928 grams
This specimen originates from the Pikes Peak region of Colorado, one of the most iconic localities in the world for amazonite and smoky quartz formed within granitic pegmatites.
Pegmatites are coarse-grained igneous formations that crystallize slowly from mineral-rich fluids, allowing for the growth of large, well-formed crystals such as those seen here. These geological conditions are responsible for the exceptional structure of the quartz, as well as the bold coloration of the amazonite.
In recent years, much of the Pikes Peak collecting area has become privately owned, significantly limiting access to new material. As a result, specimens—particularly those collected from historically accessible or public areas—are becoming increasingly scarce and highly desirable among collectors.
The addition of goethite introduces a less commonly encountered mineral association in this region. Goethite typically forms as an iron oxide mineral in oxidizing environments and can appear as botryoidal or radiating aggregates, as seen here.
Specimens combining amazonite, smoky quartz, and well-defined goethite are notably less common, making this a more distinctive and conversation-worthy piece.
Specimens from the Pikes Peak region continue to appreciate in value due to increasing scarcity and limited access to productive collecting sites. With much of the area now privately owned, opportunities to obtain this already rare material are becoming more restricted.
As a result, well-composed pieces—especially those featuring strong amazonite color and defined smoky quartz crystals—are increasingly sought after by collectors. This specimen represents not only a visually compelling display piece, but also a meaningful addition to a collection focused on classic American mineral localities.
These types of specimens have already tripled in value since 2023.
Pieces that include additional, less common mineral associations—such as goethite—offer an added layer of rarity and differentiation. As access to collecting areas continues to decline and high-quality material becomes more limited, specimens that combine strong aesthetics with unique mineralogical features are positioned to remain especially desirable among collectors.
Rare pegmatite formation
Vibrant, saturated blue-green amazonite crystals
Sharply terminated smoky quartz crystals
Sculptural black goethite aggregates
Large, display-oriented specimen with strong surface coverage
From the highly collectible Pikes Peak pegmatite region
This specimen formed within a granitic pegmatite, a late-stage igneous environment that allows for the growth of large, well-formed crystals due to slow cooling and high concentrations of volatile elements.
Amazonite is a variety of microcline feldspar, colored by trace amounts of lead and water in its crystal structure. Smoky quartz forms alongside feldspar in these environments and derives its coloration from natural radiation exposure.
Goethite, an iron oxide mineral, forms under oxidizing conditions and often develops in radiating or fibrous aggregates. Its presence in this specimen reflects secondary mineralization processes that occurred after the initial pegmatite formation, adding complexity to the overall mineral assemblage.
Amazonite is often associated with harmony, communication, and emotional balance, while smoky quartz is traditionally linked to grounding and energetic protection. Goethite is believed to enhance introspection and inner strength, making this combination one that symbolically blends clarity, stability, and deep personal insight.
This visually striking specimen showcases a dynamic combination of vibrant amazonite, sharply formed smoky quartz, and contrasting black goethite, all set atop a solid feldspar matrix from the renowned Pikes Peak region of Colorado.
A dense spread of blocky amazonite crystals dominates the surface, displaying a rich, saturated blue-green color with classic Pikes Peak form. These crystals are well-developed and tightly clustered, creating a textured, layered landscape across the top of the specimen.
Emerging between the amazonite are multiple smoky quartz crystals, ranging from translucent gray to deeper smoky tones. Their glassy luster and defined terminations provide depth and contrast, drawing the eye across the piece.
What sets this specimen apart is the presence of goethite, appearing as dark, metallic, radiating aggregates perched among the amazonite and quartz. These sculptural formations introduce a bold visual contrast and add a layer of mineralogical rarity not commonly seen in standard amazonite–smoky quartz associations from this locality.
Size: 5.25” x 2.5” x 2.25”
Weight: 928 grams
This specimen originates from the Pikes Peak region of Colorado, one of the most iconic localities in the world for amazonite and smoky quartz formed within granitic pegmatites.
Pegmatites are coarse-grained igneous formations that crystallize slowly from mineral-rich fluids, allowing for the growth of large, well-formed crystals such as those seen here. These geological conditions are responsible for the exceptional structure of the quartz, as well as the bold coloration of the amazonite.
In recent years, much of the Pikes Peak collecting area has become privately owned, significantly limiting access to new material. As a result, specimens—particularly those collected from historically accessible or public areas—are becoming increasingly scarce and highly desirable among collectors.
The addition of goethite introduces a less commonly encountered mineral association in this region. Goethite typically forms as an iron oxide mineral in oxidizing environments and can appear as botryoidal or radiating aggregates, as seen here.
Specimens combining amazonite, smoky quartz, and well-defined goethite are notably less common, making this a more distinctive and conversation-worthy piece.
Specimens from the Pikes Peak region continue to appreciate in value due to increasing scarcity and limited access to productive collecting sites. With much of the area now privately owned, opportunities to obtain this already rare material are becoming more restricted.
As a result, well-composed pieces—especially those featuring strong amazonite color and defined smoky quartz crystals—are increasingly sought after by collectors. This specimen represents not only a visually compelling display piece, but also a meaningful addition to a collection focused on classic American mineral localities.
These types of specimens have already tripled in value since 2023.
Pieces that include additional, less common mineral associations—such as goethite—offer an added layer of rarity and differentiation. As access to collecting areas continues to decline and high-quality material becomes more limited, specimens that combine strong aesthetics with unique mineralogical features are positioned to remain especially desirable among collectors.
Rare pegmatite formation
Vibrant, saturated blue-green amazonite crystals
Sharply terminated smoky quartz crystals
Sculptural black goethite aggregates
Large, display-oriented specimen with strong surface coverage
From the highly collectible Pikes Peak pegmatite region
This specimen formed within a granitic pegmatite, a late-stage igneous environment that allows for the growth of large, well-formed crystals due to slow cooling and high concentrations of volatile elements.
Amazonite is a variety of microcline feldspar, colored by trace amounts of lead and water in its crystal structure. Smoky quartz forms alongside feldspar in these environments and derives its coloration from natural radiation exposure.
Goethite, an iron oxide mineral, forms under oxidizing conditions and often develops in radiating or fibrous aggregates. Its presence in this specimen reflects secondary mineralization processes that occurred after the initial pegmatite formation, adding complexity to the overall mineral assemblage.
Amazonite is often associated with harmony, communication, and emotional balance, while smoky quartz is traditionally linked to grounding and energetic protection. Goethite is believed to enhance introspection and inner strength, making this combination one that symbolically blends clarity, stability, and deep personal insight.
