Petrography rock was affixed to a microscope slide and then ground so thin that light could be transmitted through mineral grains that otherwise appeared opaque. The position of adjoining grains was not disturbed, thus permitting analysis of rock texture. Thin section petrography became the standard method of rock study. Since textural details contribute greatly to knowledge of the sequence of crystallization of the various mineral constituents in a rock, petrography progressed into petrogenesis and ultimately into petrology. It was in Europe, principally in Germany, that petrography advanced in the last half of the nineteenth century. The macroscopic characters of rocks, those
Ceramic petrography ceramics are "sensitive indicators of human decision making and materials interaction". By examining microstructural evidence for processes such as clay paste preparation, forming and firing, ceramic petrographers can reconstruct the steps involved in the production of ceramic artefacts. Ceramic petrography originated in the American Southwest with the work of Anna O. Shepard but has mainly been developed in the Old World in the later half of the 20th century. Other early studies include the work of David Peacock and his students in the UK Ceramic petrography continues to be applied to the interpretation of British ceramics and is used heavily