petrological

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A White Stone Textur with Black Horizontal Lines Royalty Free Stock Photo
Vibrant opal gemstone in natural rock formation Royalty Free Stock Photo
Rutil Stone On Isolated Transparent Background, Png. Generative AI Royalty Free Stock Photo
Detailed image of the surface of Mammoth Hot Springs in Yellowstone National Park. Royalty Free Stock Photo
Desert Spiny Lizard displays vibrant spiny scales while perched gracefully on a rugged rock in a well lit environment Royalty Free Stock Photo
   
   
Flint ore on a white background.
   
   
   
   
   
   
   
Flint is a hard, sedimentary cryptocrystalline form of the mineral quartz, ategorized as a variety of chert. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones. Inside the nodule, flint is usually dark grey, black, green, white or brown in colour, and often has a glassy or waxy appearance. A thin layer on the outside of the nodules is usually different in colour, typically white and rough in texture. From a petrological point of view, `flint` refers specifically to the form of chert which occurs in chalk or marly limestone. Similarly, `common chert` sometimes referred to simply as `chert` occurs in limestone.


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