This Specimen has been sold.
Large, 14.5" Free-Standing, Polished Carnelian Agate - 56 Lbs
This is a large and gorgeous, hand polished piece of carnelian agate collected from Madagascar. This beautiful piece features fiery hues of red and oranges with large pockets of quartz. The base has been cut flat so it can be displayed without the use of a stand. It measures 14.5" tall and weighs just over 56 lbs.
About Carnelian
Carnelian is a semi-precious variety of chalcedony that features an orange or orange-red coloration. Its name is believed to come from the Latin word carneus, meaning 'flesh colored'. The reddish color is caused by iron oxide impurities in the silica that makes up the chalcedony. Carnelian is one of the oldest known gemstones. It was widely used in ancient Rome to make insignias and seals for imprinting on letters or important documents because hot wax does not stick to carnelian.
Carnelian is a semi-precious variety of chalcedony that features an orange or orange-red coloration. Its name is believed to come from the Latin word carneus, meaning 'flesh colored'. The reddish color is caused by iron oxide impurities in the silica that makes up the chalcedony. Carnelian is one of the oldest known gemstones. It was widely used in ancient Rome to make insignias and seals for imprinting on letters or important documents because hot wax does not stick to carnelian.
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
Chalcedony var. Carnelian Agate
LOCATION
Madagascar
SIZE
14.5 x 8.6 x 8", weighs just over 56 lbs
CATEGORY
SUB CATEGORY
ITEM
#168309