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chert
(redirected from cherts)

   Also found in: Encyclopedia, Wikipedia 0.02 sec.
chert  (chûrt)
n.
1. A variety of silica that contains microcrystalline quartz.
2. A siliceous rock of chalcedonic or opaline silica occurring in limestone.

[Origin unknown.]

cherty adj.

chert [tʃɜːt]
n
(Earth Sciences / Minerals) a microcrystalline form of silica usually occurring as bands or layers of pebbles in sedimentary rock. Formula: SiO2. Varieties include flint, lyddite (Lydian stone) Also called hornstone
[of obscure origin]
cherty  adj

chert  (chûrt)
A hard, brittle sedimentary rock consisting of microcrystalline quartz. It is often reddish-brown to green but can also occur in a variety of other colors, especially white, pink, brown, or black. Chert often contains impurities such as calcium, iron-oxide, or the remains of silica-rich organisms. It usually occurs as nodules in limestone and dolomite and has curved fractures.
ThesaurusLegend:  Synonyms Related Words Antonyms
Noun1.chert - variety of silica containing microcrystalline quartz
taconite - a variety of chert containing magnetite and hematite; mined as a low-grade iron ore
silica, silicon dioxide, silicon oxide - a white or colorless vitreous insoluble solid (SiO2); various forms occur widely in the earth's crust as quartz or cristobalite or tridymite or lechatelierite
Translations
chert
n (Min) → Kieselschiefer m, → Feuerstein m, → Hornstein m; (Build) → Gneiszuschlag(stoff) &, Feingranitzuschlag m (für Sichtbeton)


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? Mentioned in ? References in periodicals archive
 
For their study of the Permian, the Canadian team collected a section of well-preserved shales and cherts from northeastern British Columbia.
Of particular interest, drilling in holes F-05-03 and two holes currently in progress in Q2-2006 (F-05-4, F-05-05) on Metco properties 1-2 km northeast of the Horne-Quemont Mines, have intersected Horne Rhyolite, cherts and exhalite-sulphide-bearing rocks typical of the Horne Mine stratigraphy.
20 m thick exhalite zone consisting of cherts, silica sinter and a 1.
 
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