This Specimen has been sold.
7.1" Quartz Geode Section on Metal Stand - Uruguay
This is a beautiful quartz geode section from the famous amethyst mines near Artigas, Uruguay. The "rind" has been polished to reveal the gorgeous banded agate that surrounds the quartz encrusted cavity.
The attached custom metal display stand makes for a very aesthetic display.
The attached custom metal display stand makes for a very aesthetic display.
About Uruguay Amethyst
Though Brazil produces a greater volume of amethyst, the material from the Artigas region of Uruguay is renowned for its exceptional depth of color and superb crystal quality. Uruguayan amethyst typically forms in dense basalt flows and develops into richly saturated, grape-purple crystals that are considered some of the finest in the world. Because we import our specimens directly from the mines, we’re able to offer outstanding prices on everything from dramatic geodes to premium clusters and collector-grade crystal formations.
Though Brazil produces a greater volume of amethyst, the material from the Artigas region of Uruguay is renowned for its exceptional depth of color and superb crystal quality. Uruguayan amethyst typically forms in dense basalt flows and develops into richly saturated, grape-purple crystals that are considered some of the finest in the world. Because we import our specimens directly from the mines, we’re able to offer outstanding prices on everything from dramatic geodes to premium clusters and collector-grade crystal formations.
About Agate
Agate is a variety of microcrystalline quartz (chalcedony) that displays translucence and, in some cases, banding. Agate primarily forms when silica-rich fluids fill pockets within rocks and/or fossils, depositing the silica along the walls of the rock. This process can result in banding patterns, as the compositions and impurities of these depositing fluids change over time. These banding patterns can either form as flat layers, creating linear patterns known as waterline agate, or as rounded layers, forming more common ring-like patterns. These patterns depend on the surfaces available for deposition.
Agate is a variety of microcrystalline quartz (chalcedony) that displays translucence and, in some cases, banding. Agate primarily forms when silica-rich fluids fill pockets within rocks and/or fossils, depositing the silica along the walls of the rock. This process can result in banding patterns, as the compositions and impurities of these depositing fluids change over time. These banding patterns can either form as flat layers, creating linear patterns known as waterline agate, or as rounded layers, forming more common ring-like patterns. These patterns depend on the surfaces available for deposition.
SPECIES
Quartz & Chalcedony var. Agate
LOCATION
Artigas, Uruguay
SIZE
7.1" tall, 2.7" wide, 9.9" tall on stand
CATEGORY
SUB CATEGORY
ITEM
#172083
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