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Shale (right) and garnet-mica-schist (left)
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Shale (right) and garnet-mica-schist (left)
Shale is sedimentary and garnet-mica-schist is metamorphoc in origin. Specimen held at the Natural History Museum, London
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Compare Comparison Contrast Dull Garnet Metamorphic Mica Mineral Natural History Museum Nesosilicate Orthosilicate Phyllosilicate Sedimentary Sedimentary Rock Shale Shiny Silicate Silicate Mineral The Natural History Museum Schist
EDITORS COMMENTS
In this photograph, the contrast between two distinct geological formations, Shale on the right and Garnet-Mica-Schist on the left, is showcased in a stunning studio setting at The Natural History Museum in London. The Shale, a sedimentary rock, is characterized by its dull, homogeneous appearance, with layers of fine-grained clay, silt, and organic matter. In contrast, the Garnet-Mica-Schist, a metamorphic rock, displays a shimmering, silky sheen, revealing its complex mineral composition. The Garnet-Mica-Schist, a phyllosilicate and orthosilicate rock, is composed primarily of mica and garnet, with quartz and feldspar also present. The garnets, with their distinctive red hue, are nestled among the mica flakes, creating a striking visual effect. The mica, a silicate mineral, adds to the schist's unique luster and sheen. The Shale, on the other hand, is a sedimentary rock formed from the accumulation and compaction of organic and inorganic sediments. Its dull appearance is a result of the absence of any prominent minerals or crystals. Despite its unassuming appearance, Shale plays a crucial role in the Earth's carbon cycle, serving as a significant reservoir for hydrocarbons, including oil and natural gas. This comparison of Shale and Garnet-Mica-Schist serves as a reminder of the diverse range of geological formations that can be found within our planet. The Natural History Museum's extensive collection of rocks and minerals provides valuable insights into the Earth's geological history and the complex processes that have shaped our world.
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