Pisolite
{{short description|Sedimentary rock made of large grains, usually of calcium carbonate}}
Image:PisolitesConococheagueUpperCambrian.jpg
Image:Calcario2EZ.jpg, Rio de Janeiro, Brazil; pisolith diameters average 1.0 cm]]
Image:Qemscan_pisoliths.png mineral map of bauxite forming pisoids]]
A pisolite ({{ety|grc|πίσον (píson)|pea}}) is a sedimentary rock made of pisoids, which are concretionary grains – typically of calcium carbonate which resemble ooids, but are more than 2 mm in diameter.[http://www.mindat.org/min-26778.html Mindat - Pisolite] These grains are approximately spherical and have concentric layers reaching 10 mm in diameter.
Bauxites, limonites, and siderites often have a pisolitic structure.
See also
References
{{Reflist}}
Further reading
- {{cite book |last1=Manutchehr-Danai |first1=Mohsen |title=Dictionary of gems and gemology |date=2009 |publisher=Springer |isbn=978-3-540-72795-8 |edition=3rd}}
{{Authority control}}
{{sedimentary-rock-stub}}