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Porcellanite - Wikipedia, the free encyclopedia
Porcellanite or porcelanite , is a hard, dense rock somewhat similar in appearance to unglazed porcelain. It is often an impure variety of chert containing clay and calcareous matter. At Tievebulli...
en.wikipedia.org/wiki/Porcellanite
A dense siliceous rock having the texture, dull luster, hardness, conchoidal fracture, and general appearance of unglazed porcelain; it is less hard, dense, ...
www.webref.org/geology/p/porcellanite.htm www.webref.org/geology/p/porcellanite.htm
Nov 8, 2009 ... Media in category "Porcellanite". The following 4 files are in this category, out of 4 total. MaloneHoard.JPG 2625380 bytes ...
commons.wikimedia.org/wiki/Category:Porcellanite commons.wikimedia.org/wiki/Category:Porcellanite
Y. Kolodny, Y. Nathan, and E. Sass ... The porcellanite occurs in association with chert in the lower part of the Mishash formation (Cretaceous). It is composed mostly of opal and is highly porous.
jsedres.sepmonline.org/cgi/content/abstract/35/2/454
The characteristics of reaction phases, microstructure and microhardness of thermally fused powder mixtures of porcellanite and limestone batched in various ...
linkinghub.elsevier.com/retrieve/pii/S0272884204004535
Porcellanite was the single most important raw material used in the manufacture of stone axes in Ireland, accounting for more than half of the total. ...
linkinghub.elsevier.com/retrieve/pii/S0305440396901570
The present invention provides high grade opaliform porcellanite having a purity of at least 80% active silica. The invention also provides a process for ...
www.freepatentsonline.com/5102837.html
Descriptions and examples of Tertiary porcellanite from Northern Bohemia ... Porcellanite is, like the name already suggests a material very similar to porcelain. Basically it is a natural ceramic formed by thermal metamorphism of, mostly kaolinitic, clays.
www.flintsource.net/other/CZ_porcel.html
www-odp.tamu.edu/publications/185_SR/002/002_f1.htm
Calcareous porcellanite...
www-odp.tamu.edu/publications/198_SR/107/107_t4.htm