Flint
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![]() A sample of Miorcani flint from the Cenomanian chalky marl layer of the Moldavian Plateau. (ca. 7.5 cm wide) |
Flint is a hard, sedimentary cryptocrystalline form of the mineral quartz, categorized 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.
- Related: Agate, Chalcedony, Chert, Eolith, Jasper, Nodule (geology), Obsidian, Onyx, Opal, Whinstone, Clovis Point, Grimes Graves, Flint Ridge State Memorial, Flint mine
Flint Architecture of East Anglia Flint Architecture of East Anglia www.gilesdelamare.co.uk/page3.htm - Web |
Flintsource.net European Artefacts - detailed site Flintsource.net European Artefacts - detailed site www.flintsource.net - Web |
Flint circles and paramoudra - Beeston Bump Flint circles and paramoudra - Beeston Bump www.geulogy.com/introdis-beestonbump.html - Web |
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Paramoudras and flint circles photograph collectio... Paramoudras and flint circles photograph collection www.electricyouniverse.com/eye/index.php?level=album&id=71 - Web |
Winchester Cathedral Close Winchester Cathedral Close www.kimwilkie.com/pages/projects/uk/uk_wcath.html - Web |