This is a very large, smooth and uniform piece of “Ocean Jasper”. “Ocean Jasper” is formed through the silicification and alteration of volcanic tuffs by mineral-rich hydrothermal fluids, which deposit minerals in concentric rings to create its distinctive orbicular patterns. | Omar Nacer
0:15
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This is a very large, smooth and uniform piece of “Ocean Jasper”. “Ocean Jasper” is formed through the silicification and alteration of volcanic tuffs by mineral-rich hydrothermal
Omar Nacer. Omar Nacer · Original audio. This is a very large, smooth and uniform piece of “Ocean Jasper”. “Ocean Jasper” is formed through the silicification and alteration of volcanic tuffs by mineral-rich hydrothermal fluids, which deposit minerals in concentric rings to create its distinctive orbicular patterns.
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The Green “Jasper”, formed from silica-rich solutions depositing within pre-existing rocks, exhibits verdant hues due to iron impurities. During its formation, microscopic quartz crystals interlock, creating a dense, opaque structure. Variations in colour and pattern arise from differing concentrations and distributions of included minerals, such as iron oxides or hydroxides, which produce bands, spots, and other intriguing visual effects within the stone. | Omar Nacer
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The Green “Jasper”, formed from silica-rich solutions depositing within pre-existing rocks, exhibits verdant hues due to iron impurities. During its formation, microscopic quartz crystals interlock, creating a dense, opaque structure. Variations in colour and pattern arise from differing concentrations and distributions of included minerals, such as iron oxides or hydroxides, which produce bands, spots, and other intriguing visual effects within the stone. | Omar Nacer
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The Green “Jasper”, formed from silica-rich solutions depositing within pre-existing rocks, exhibits verdant hues due to iron impurities. During its formation, microscopic quartz crystals interlock, creating a dense, opaque structure. Variations in colour and pattern arise from differing concentrations and distributions of included minerals, such as iron oxides or hydroxides, which produce bands, spots, and other intriguing visual effects within the stone. | Omar Nacer
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The Green “Jasper”, formed from silica-rich solutions depositing within pre-existing rocks, exhibits verdant hues due to iron impurities. During its formation, microscopic quartz crystals interlock, creating a dense, opaque structure. Variations in colour and pattern arise from differing concentrations and distributions of included minerals, such as iron oxides or hydroxides, which produce bands, spots, and other intriguing visual effects within the stone. | Omar Nacer
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The creation of Brecciated Jasper begins with the fracturing of pre-existing jasper. Tectonic activity or powerful impacts shatter the stone into angular fragments, which then naturally cement together. The cement, often composed of silica or iron oxides, forms within sedimentary or hydrothermal environments. Iron oxides contribute reds and browns, while other minerals create yellows, greens, and blacks. | Omar Nacer
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The creation of Brecciated Jasper begins with the fracturing of pre-existing jasper. Tectonic activity or powerful impacts shatter the stone into angular fragments, which then naturally cement together. The cement, often composed of silica or iron oxides, forms within sedimentary or hydrothermal environments. Iron oxides contribute reds and browns, while other minerals create yellows, greens, and blacks. | Omar Nacer
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This is a “banded jasper” or “hematic jasper”. This type of rock with distinct “banding” patterns and a reddish-brown color, which aligns with descriptions of “banded jasper”, especially when formed in iron-rich environments. While other options like banded chert, mudstone, can have banding, the appearance of the rock, particularly its color and the nature of the “banding” strongly suggests a form of jasper that has undergone silicification and potentially iron oxidation. | Omar Nacer
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‎عمر ناصر | Omar Nacer‎ on Instagram: "The Green “Jasper”, formed from silica-rich solutions depositing within pre-existing rocks, exhibits verdant hues due to iron impurities. During its formation, microscopic quartz crystals interlock, creating a dense, opaque structure. Variations in colour and pattern arise from differing concentrations and distributions of included minerals, such as iron oxides or hydroxides, which produce bands, spots, and other intriguing visual effects within the stone."
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Willow Creek Jasper formed 25-30 million years ago and can be found near Eagle Idaho. I enjoyed making this Cabachon. It took a beaufltiful shine and came out great. #cabachon #jasper #willowcreek #handmadejewelry #crystals
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