Feldspar
Feldspars make up almost 60% of the Earth's curst. It crystallizes from magma as veins and is present in metamorphic rocks. It is pink, white, gray, or brown in color with a mohs hardness of 6-6.5.
Feldspars make up almost 60% of the Earth's curst. It crystallizes from magma as veins and is present in metamorphic rocks. It is pink, white, gray, or brown in color with a mohs hardness of 6-6.5.
Objects: Feldspar Export: JSON - XML - CSV
| Object | U Number | Museum Number (UPM Date Reg Number) | Museum Number (BM Registration Number) | Museum Number (UPM B-number) | Description (Catalog Card) |
|---|---|---|---|---|---|
 | 15447 | (none) | (none) | (none) | Glazed beads; and some felspar(?) beads. Glazed rings and felspar(?) cuboids. |
| 17365 | (none) | (none) | (none) | Beads. Carnelian double conoids and quartz. Agate lentoids and quartz. Lapis ball and lentoid. Glass paste balls. Green amazonite (?) ring beads. |
| 17826 | (none) | (none) | (none) | Beads. Mixed: a long barrel of blue paste with gold caps, lentoids of carnelian, jasper, amazonite (?) and chrysoprase, crystal pendant and carnelian rings. Kassite. |
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Related Terms
Apatite - Aragonite - Calcite Group - Chlorite - Dolomite - Gypsum - Magnesite - Pigment - Serpentine - Semi-precious
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Parent Terms
Inorganic Remains > Stones and Minerals > Mineral > Feldspar