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The Hebrew word may have designated a green jasper. [12] Flinders Petrie suggested that the odem – the first stone on the High Priest's breastplate – was a red jasper, whilst tarshish, the tenth stone, may have been a yellow jasper. [13] Male torso carved from red jasper, Bronze Age, Harappa, Indus Valley civilisation, Pakistan
Green Jasper ring of Pharaoh Tutankhamun Green Jasper - Hebrew בָּרֶקֶת‬ bareḳeth . The third stone of the priestly breastplate (Exodus 28:17, 39:10), representing the tribe of Levi ; it is the ninth stone in Ezekiel 28:13, and the fourth foundation stone of the celestial Jerusalem (Rev. 21:19).
This semiprecious stone should not be confused with other ornamental stones that contain red jasper. Setonite, also called African bloodstone, is composed of red jasper, grey chalcedony, and pyrite. Dragon's Blood, sometimes called Australian bloodstone, is composed of red jasper and green epidote.
Green diopside crystals included within a white feldspar matrix are also sold as gemstones, usually as beads or cabochons. This stone is often marketed as 'green spot jasper' or green spot stone'. Violane is a manganese-rich variety of diopside, violet to light blue in color. [11]
The relic of the Virgin Mary's wedding ring, which according to different accounts had an onyx, amethyst, or green jasper, was supposedly brought back from the Holy Land in 996 CE. It was placed in the Church of Santa Mustiola, Clusium (modern Chiusi), Italy, and in 1473 the ring was transferred to the Franciscan monastery in that city.
Orbicular jasper from Madagascar. Orbicular jasper is a variety of jasper which contains variably-colored orbs or spherical inclusions or zones. In highly silicified rhyolite or tuff, quartz and feldspar crystallize in radial aggregates of needle-like crystals which provide the basis or seed for the orbicular structure seen in this kind of jasper. [1]
The dominant green epidote in unakite rocks is the metasomatic alteration product of plagioclase feldspar, while the orthoclase and quartz crystals remain unaffected. Distribution [ edit ]
Incomplete alteration causes the physical properties of serpentines to vary widely. Antigorite is the polymorph of serpentine that most commonly forms during metamorphism of wet ultramafic rocks and is stable at the highest temperatures—to over 600 °C (1,100 °F) at depths of 60 km (37 mi) or so.
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