Fluorapophyllite Twin big Crystal with Stilbite Natural Mineral Specimen - image 1
Fluorapophyllite Twin big Crystal with Stilbite Natural Mineral Specimen - image 2
Fluorapophyllite Twin big Crystal with Stilbite Natural Mineral Specimen - image 3
Fluorapophyllite Twin big Crystal with Stilbite Natural Mineral Specimen - image 4
Fluorapophyllite Twin big Crystal with Stilbite Natural Mineral Specimen - image 5
Fluorapophyllite Twin big Crystal with Stilbite Natural Mineral Specimen - image 6
Fluorapophyllite Twin big Crystal with Stilbite Natural Mineral Specimen - image 7

Fluorapophyllite Twin big Crystal with Stilbite Natural Mineral Specimen

Unknown Owner
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Features: A typical Deccan Trap association specimen with strong, extremely glossy, crisp, well-formed, blocky, green and colourless Fluorapophyllite crystals (K).which are linked with extremely glossy, delicate peach coloured Stilbite-Ca "sheaves" A Chalcedony "core" may be seen in a tiny region on the back.The primar

Product details

SpeciesApophyllite
SizeCabinet
Dimensions13.0 x 11.0 cm
Weight720 grams
Added on10/28/2024
LocalityIndia, Maharashtra, Jalgaon District

Known provenance

DateCollectorAcquisition price
02/2026Unknown Owner$300.00
—Superb MineralsNot disclosed

Learn more

Apophyllite
Mineral guide
Learn about Apophyllite
glassy, fish-tail crystals; colorless to green. Great for display and provenance. Key sources: Deccan Traps (India), New Jersey; collecting value.
Apophyllite
Regional guide
Apophyllite from Jalgaon District, India
Jalgaon District is one of the great modern names in apophyllite collecting: a Deccan Trap basalt locality where glassy, geometric fluorapophyllite-(K) crystals emerge from dark volcanic rock with the kind of sculptural contrast collectors remember. The best pieces combine water-clear to mint-green apophyllite with peach stilbite, brown heulandite, sugary chalcedony, quartz crusts, celadonite-rich matrix, calcite, and, more rarely, powellite. The visual language is unmistakably Indian Deccan: bright vitreous faces, steep pyramidal terminations, pseudocubic outlines, and vug-shaped matrix plates that still read as sections of the original cavity.