Arikah Map

Flint

This article is about the sedimentary rock. For other uses, see Flint (disambiguation).
Flint:A flint nodule from the Onondaga limestone layer, Buffalo, New York. (3.8 cm wide)
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A flint nodule from the Onondaga limestone layer, Buffalo, New York. (3.8 cm wide)

Flint (or flintstone) is a hard, sedimentary cryptocrystalline silicate form of the mineral quartz, categorized as a variety of chalcedony. Flint is usually dark-grey, blue, black, or deep brown in color, and often has a glassy appearance. It occurs chiefly as nodules and masses in sedimentary rocks, such as chalks and limestones.

The exact mode of formation of flint is not yet clear or agreed but it is thought that it occurs as a result of chemical changes in compressed sedimentary rock formations, during the process of diagenesis. One theory is that a gelatinous material fills cavities in the sediment, such as holes bored by crustaceans or molluscs and that this becomes silicified. This could certainly explain the complex shapes of flint that are found.


Contents

Uses

In Europe, some of the best toolmaking flint has come from Belgium (Obourg, flint mines of Spiennes), the coastal chalks of the English Channel, the Paris Basin, the Sennonian deposits of Rügen, Grimes Graves in England and the Jurassic deposits of the Kraków-area in Poland. Flint mining is attested since the Palaeolithic, but became more common since the Neolithic (Michelsberg culture, Funnelbeaker culture).

Flint:Pebble beach made up of flint nodules eroded out of the nearby chalk cliffs, Cape Arkona, Rügen
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Pebble beach made up of flint nodules eroded out of the nearby chalk cliffs, Cape Arkona, Rügen

See also

Categories


Sedimentary rocks | Lithics

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