Provenite

Planggenstock

Natural outcropUnknownDraft data

46.6306° N, 8.4733° E · ± 1 km

Rock crystal and Smoky quartz from Uri, Switzerland, with photos of specimens from this locality.

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Minerals found here

Rock crystal at Planggenstock

Exceptionally clear, very large Alpine-cleft crystals, accompanied by pink fluorite.

Formula
SiO₂
Morphology
Large crystals and crystal groups grown in an Alpine cleft
Typical size
Crystal groups up to 300 kg; the central crystal of the 2005 find is 107 cm long
Color / luster
Clear; crystals from the cleft floor can show greenish, cloudy patches from chlorite grains
Associated minerals
Smoky quartzfluorite (pink)chloriteadularia
History
Opened on 21 September 2005 after eleven years of exploratory digging; the find was bought by the Natural History Museum Bern in 2010 and has been on show there since 2011. The crystals later inspired modern gem-carving artworks.

Sources: SRC-132 SRC-133 SRC-134

About Rock crystal →

Smoky quartz at Planggenstock

Giant Alpine-cleft quartz in which smoky and clear crystals occur together with pink fluorite, grown in Aar Massif granite.

Formula
SiO₂
Morphology
Large crystals and crystal groups grown in an Alpine cleft
Color / luster
Smoky shade varies by crystal, depending on how long it was in contact with the radioactive granite; cleft-floor crystals can carry greenish, cloudy chlorite patches while ceiling-side crystals stayed clear
Associated minerals
Rock crystalfluorite (pink, up to about 8 cm)chloriteadularia
Trace elements
Aluminium-related colour centres produced by natural irradiation (general for the variety, not locality-specific)
History
Exploratory digging began in 1994; on 21 September 2005 almost fifty large clear crystals and clusters were found, with another significant find in May 2008. The Natural History Museum Bern bought the 2005 find in 2010 for 4.5 million francs and has shown it since May 2011.

Sources: SRC-132 SRC-133 SRC-134

About Smoky quartz →

Geology of the locality

Setting
Alpine fissure (cleft) formed during the Alpine orogeny about 50 million years ago; hot mineral-rich fluid above 300 degrees C deposited quartz as the rock rose and cooled. The cleft explored by the miners lies at about 2,600 m on the peak.
Host rock
Granite of the Aar Massif
Region
Uri
Country
Switzerland

Coordinates (converted from 46 37 50 N, 8 28 24 E) are those of the peak on the Mindat locality page; the cleft sits below the summit, so the pin is approximate. Permission from landowners and mineral-rights holders is needed before visiting any such site.

Sources: SRC-132 SRC-133

Sources

  1. SRC-132 · Database
    Planggenstock, Goescheneralp, Goeschenen Valley, Uri, SwitzerlandMindat.org contributors · Mindat.org
  2. SRC-133 · Museum / collection
    Info brochure: The Planggenstock treasure (EN)Natural History Museum Bern · Naturhistorisches Museum Bern
  3. SRC-134 · Article
    Quartz crystals from alpine fissures: their formation and the historical significance of alpine quartz as raw material for objets d'artHuegi, M.F. · 2023 · 37th International Geological Congress (IGC), Tokyo

Draft data from the Provenite workbook. Check entries against the cited sources before relying on them. Photos are open-licence images from Wikimedia Commons; the author and licence are given with each photo.