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Ancient Egyptian pottery

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Through Clay, Pottery and Chemistry

Specialists in ancient Egyptian pottery draw a fundamental distinction between ceramics made of Nile clay and those made of marl clay, based on chemical and mineralogical composition and ceramic properties. Nile clay is the result of eroded material in the Ethiopian mountains, which was transported into Egypt by the Nile. This clay has deposited on the banks of the Nile in Egypt since the Late Pleistocene by the flooding of the Nile. Marl clay is a yellow-white stone which occurs in limestone deposits. These deposits were created in the Pleistocene, when the primordial waters of the Nile and its tributaries brought sediment into Egypt and deposited in on what was then the desert edge.

Our understanding of the nature and organisation of ancient Egyptian pottery manufacture is based on tomb paintings, models, and archaeological remains of pottery workshops. A characteristic of the development of Egyptian ceramics is that the new methods of production which were developed over time never entirely replaced older methods, but expanded the repertoire instead, so that eventually, each group of objects had its own manufacturing technique. Egyptian potters employed a wide variety of decoration techniques and motifs, most of which are associated with specific periods of time, such as the creation of unusual shapes, decoration with incisions, various different firing processes, and painting techniques.

An important classification system for Egyptian pottery is the Vienna system, which was developed by Dorothea Arnold, Manfred Bietak, Janine Bourriau, Helen and Jean Jacquet, and Hans-Åke Nordström at a meeting in Vienna in 1980.

Seriation of Egyptian pottery has proven useful for the relative chronology of ancient Egypt. This method was invented by Flinders Petrie in 1899. It is based on the changes of vessel types and the proliferation and decline of different types over time.

Material

Understanding of the raw material is essential for understanding the development, production, and typology of Egyptian ceramics. In Egyptian archaeology the distinction between Nile clay and marl clay is fundamental. Mixtures of the two types of clay can be seen as a third group.

Nile clay

Nile clay is the result of eroded material in the Ethiopian mountains, which was transported into Egypt by the Nile. This clay was deposited on the banks of the Nile in Egypt since the Late Pleistocene by the cyclic Nile floods. As a result, deposits can be found far from the modern floodplain as well as within the level covered by the flood in modern times. Chemically, the clay is characterised by high silicon content and a high level of iron oxide. Mineralogically, it is micacaeous, illite-rich sediment clay, containing many different sand and stone particles brought from the various contexts through which the Nile flows. The clay turns a red or brown colour when it is fired in an oxygen-rich oven. When unfired, it varies in colour from grey to nearly black.

Marl clay

The marl clay (or 'desert clay') is found along the Nile valley, from Esna to Cairo, in the oases and at the edges of the Nile Delta. It is a yellow-white stone, which is found in limestone deposits. The deposits were created in the Pleistocene, when the original Nile river and its tributaries deposited this clay in what had previously been desert. Marl clay includes a range of kinds of clay based on their base substance. In general, they have a lower percentage of silica and significantly higher calcium content. The most important sub-types of marl clay are:

  • Qena clay: secondary deposits like that at Wadi Qena. This clay comes from sediments which were washed down the wadi and mixed with local slate and limestone.
  • Marl clay from slate and limestone which is found along the Nile between Esna and Cairo.

Marl clay is normally cream or white in colour when it is fired in an oxygen-rich oven. Cuts can reveal pink or orange areas. It is rich in mineral salts, so the outer surface often has a thin layer of weathered salt which forms a white surface layer when fired, which can be mistaken for a 'glaze' by the unwary. At higher firing temperature (c. 1000 °C), this layer becomes olive-green and resembles a green glaze.

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