Azurite (pigment)
Azurite is an inorganic pigment derived from the mineral of the same name.[1] It was likely used by artists as early as the Fourth Dynasty in Egypt, but it was less frequently employed than synthetically produced copper pigments such as Egyptian Blue.[1]: 23–26 In the Middle Ages and Renaissance, it was the most prevalent blue pigment in European paintings, appearing more commonly than the more expensive ultramarine.[1]: 26 Azurite's derivation from copper mines tends to give it a greenish hue, in contrast with the more violet tone of ultramarine.[2] Azurite is also less stable than ultramarine, and notable paintings such as Michelangelo's The Entombment have seen their azure blues turn to olive green in time.[2] Azurite pigment typically includes traces of malachite and cuprite; both minerals are found alongside azurite in nature, and they may account for some of the green discoloration of the pigment.[1]: 26 The particle size of azurite pigment has been shown to have a significant effect on its chromatic intensity, and the manner of grinding and preparing the pigment therefore has a major impact on its appearance.[3]
- Michelangelo, The Entombment, ca. 1500–1501. The azure blue in the drapery has turned green in time.
- Albrecht Altdorfer, Christ Taking Leave of His Mother, ca. 1520. The blue color of the clothing and sky is derived exclusively from azurite.
References
- Gettens, Rutherford J.; Fitzhugh, Elisabeth West (1993). "Azurite and Blue Verditer". In Roy, Ashok (ed.). Artists' Pigments: A Handbook of Their History and Characteristics. Vol. 2. Archetype. pp. 23–36.
- Finlay, Victoria (2002). Color: A Natural History of the Palette. Random House. pp. 287–88.
- Price, Michael (2000). "A Renaissance of Color: Particle Separation and Preparation of Azurite for Use in Oil Painting". Leonardo. 33 (4): 281–288. doi:10.1162/002409400552667. ISSN 0024-094X. JSTOR 1576902. S2CID 57571083.