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Shale. Compacted platy clay particles give shales their typical laminated structure
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Shale. Compacted platy clay particles give shales their typical laminated structure
Compacted platy clay particles give shales their typical laminated structure. Shale is a sedimentry rock which is composed of many fine-grained clay particles
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Media ID 8581261
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Black Background Clay Clay Mineral Mineral Phyllosilicate Sedimentary Sedimentary Rock Shale Silicate Silicate Mineral Specimen
EDITORS COMMENTS
In this studio shot, a single specimen of shale takes center stage against a stark black background, its intricate structure illuminated by the soft glow of a nearby light source. Shale, a sedimentary rock, is characterized by its fine-grained composition, primarily made up of compacted platy clay particles. These clay particles, which are themselves composed of phyllosilicate and other silicate minerals, give shale its distinctive laminated or layered appearance. The silicate minerals in shale are an essential component of the Earth's crust, making up a significant portion of the planet's geological formations. The clay minerals, in particular, are known for their unique properties, including their ability to absorb water and swell, making them an essential component of many natural systems, from soil to industrial applications. Shale's formation typically occurs in quiet, shallow water environments, where clay particles settle and compact over time, forming thin layers. These layers can be seen in the specimen, with their subtle variations in color and texture, creating a mesmerizing visual display. This photograph serves as a reminder of the beauty and complexity of the natural world, showcasing the intricate details of a seemingly ordinary rock. The shale specimen, with its silicate minerals and clay particles, is a testament to the wonders of geology and the intricacies of the Earth's formation.
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