Difference between revisions of "White earth"
Jump to navigation
Jump to search
| Line 1: | Line 1: | ||
== Description == | == Description == | ||
| − | A general class of minerals that produce a fine white powder when ground, such as chalk, kaolinite, diatomite, and gypsum. White earths have been used directly as pigments, extenders and as a base for some lake pigments. | + | A general class of minerals that produce a fine white powder when ground, such as [[chalk]], [[kaolinite]], diatomite, and [[gypsum]]. White earths have been used directly as pigments, extenders and as a base for some lake pigments. |
It is not the same as [[terra alba]] (Mayer 1969). | It is not the same as [[terra alba]] (Mayer 1969). | ||
Revision as of 14:12, 28 February 2024
Description
A general class of minerals that produce a fine white powder when ground, such as Chalk, Kaolinite, diatomite, and Gypsum. White earths have been used directly as pigments, extenders and as a base for some lake pigments.
It is not the same as Terra alba (Mayer 1969).
Synonyms and Related Terms
terre blanche (Fr.);
Resources and Citations
- Ruth Siddall, 'Mineral Pigments in Archaeology: Their Analysis and the Range of Available Materials' Minerals Vol 8, p. 201 (2018). Link
- Ralph Mayer, A Dictionary of Art Terms and Techniques, Harper and Row Publishers, New York, 1969 (also 1945 printing)