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Chert

Pictures of Sedimentary Rock Types

From Andrew Alden, About.com

Chert is a sedimentary rock composed mostly of the mineral chalcedony—cryptocrystalline silica, or quartz in crystals of submicroscopic size. (more below)
Silica-based rockPhoto (c) 2005 Andrew Alden licensed to About.com
Chert can form in parts of the deep sea where the tiny shells of siliceous organisms are concentrated, or elsewhere where underground fluids replace sediments with silica. Chert nodules also occur in altered limestones.

This is a piece of a chert nodule that I found in the Mojave Desert. It shows chert's typical clean conchoidal fracture and waxy luster.

Chert may have a high clay content and look at first glance like shale, but its greater hardness gives it away. Also, the waxy luster of chalcedony combines with the earthy appearance of clay to give it the look of broken chocolate. Chert grades into siliceous shale or siliceous mudstone.

Chert is a more inclusive term than flint or jasper, two other cryptocrystalline silica rocks. Flint is a dark, hard chert like the rock that prehistoric stone tools are made from, and jasper is a bright, reddish chert associated with iron-rich deposits. All of these have a similar waxy luster, and a hardness and density near that of quartz. Silica rocks of greater purity, translucency, and refined appearance tend to be classified as agate.

Three big close-up pictures of chert are available as free wallpaper images.

For more photos see the Sedimentary Rocks Gallery.

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