Silver - Ring - Ring + garnet pendant





€11 | ||
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€8 | ||
€7 | ||
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Garnet set: ring and pendant in 925 sterling silver, total weight 7.66 g, ring size EU 58, condition as new, no laboratory report.
Description from the seller
Garnet Set: ring + pendant
/ rough / new - 7.66 g - (2)
Ring: 925 sterling silver
9.6 mm x 9.6 mm
Ring size:
U 59
UK R
US 8.7
Fr 19
Inner diameter 18.8 mm
Weight: 4.12 g
Pendant: 925 sterling silver
18.6 mm x 10.9 mm x 7.4 mm
Weight: 3.54 g (weighed without leather band)
The garnet group (shortly garnets) is an important group of rock-forming minerals from the mineral class of 'silicates and germanates'. Structurally, garnets belong to the island silicate (nesosilicate).
Within the garnaloid group, to which all minerals that crystallize with the garnet structure belong, including those from other mineral classes (for example halides, hydroxides), the garnaloid group brings together all minerals with 12 positive charges per formula unit at the Z-position. At this time (2013) these are only silicates.
Garnet minerals typically crystallize in the cubic crystal system and mainly form isometric crystals with the characteristic shapes of the rhombic dodecahedron (historically also called garnethedron), icositetrahedron, and their combinations.
Garnet Set: ring + pendant
/ rough / new - 7.66 g - (2)
Ring: 925 sterling silver
9.6 mm x 9.6 mm
Ring size:
U 59
UK R
US 8.7
Fr 19
Inner diameter 18.8 mm
Weight: 4.12 g
Pendant: 925 sterling silver
18.6 mm x 10.9 mm x 7.4 mm
Weight: 3.54 g (weighed without leather band)
The garnet group (shortly garnets) is an important group of rock-forming minerals from the mineral class of 'silicates and germanates'. Structurally, garnets belong to the island silicate (nesosilicate).
Within the garnaloid group, to which all minerals that crystallize with the garnet structure belong, including those from other mineral classes (for example halides, hydroxides), the garnaloid group brings together all minerals with 12 positive charges per formula unit at the Z-position. At this time (2013) these are only silicates.
Garnet minerals typically crystallize in the cubic crystal system and mainly form isometric crystals with the characteristic shapes of the rhombic dodecahedron (historically also called garnethedron), icositetrahedron, and their combinations.

