Holocene lake sediments as a source of building material in ancient Egypt; archeometric evidence from Wadi Tumilat (Nile Delta)

Journal Title: Studia Quaternaria - Year 2017, Vol 34, Issue 2

Abstract

The Tell el-Retaba archaeological site is located in the middle part of Wadi Tumilat, which extends along the north-eastern margin of the Nile Delta. It contains fragments of fortified and domestic objects of the ancient fortress and other constructions built of mud bricks. The establishment and functioning of the fortress is dated at the times of the reign of two great pharaohs, Ramesses II and Ramesses III (13th and 12th centuries BC). The grain size composition of the sediments used for mud brick production had significant influence on their physical and mechanical properties, which was used by the ancient Egyptians for the improvement of bricks. The finest fractions, clay and silt, which generally comprise clay minerals and organic matter played a significant role. These components significantly influenced the mud brick properties and resulted in a structural cohesion of the material. The second important component of mud bricks were coarse fractions – sand and gravel. The source of material used for brick production were the natural sediments located in the vicinity of the fortress, i.e. the Holocene lake clay and the Pleistocene gravel and sand of the gezira formation, deposited by a braided river. Clay sediments have a variable lithology as can be deduced from grain size composition of mud bricks and their properties. This variability was caused by a variable regime of the Nile, which supplied material to the lake basin. Geological studies were used to recognize ancient environment and morphology of the area, and to find clay, sand and gravel open-pits that existed in the area. The fortress site was selected optimally in relation to the landscape morphology and close vicinity of the source of basic material and water used for mud brick production. The area around the fortress was substantially transformed by humans due to settlement.

Authors and Affiliations

Małgorzata Zaremba, Jerzy Trzciński, Fabian Welc

Keywords

Related Articles

CHRONOSTRATIGRAPHY OF THE LATE VISTULIAN IN CENTRAL POLAND AND THE CORRELATION WITH VISTULIAN GLACIAL PHASES

The Vistulian decline was a period of rapid environmental events. The authors correlated ages of the last Scandinavian Ice Sheet limits in northern Poland with ages of prominent events adapting the conditions of periglac...

ORIGIN AND EVOLUTION OF BASINS IN THE EASTERN PART OF JASŁO-SANOK DEPRESSION (POLISH CARPATHIANS) IN THE LATE VISTULIAN AND HOLOCENE

Results of a geomorphologic study as well as radiocarbon and pollen analyses of sediments in small basins of the Jasło-Sanok Depression (Western Carpathians) are summarised. Floors of these basins, carved in soft shale-s...

Late Holocene changes in vegetation of the Mrągowo Lakeland (NE Poland) as registered in the pollen record from Lake Salęt

Pollen analysis of sediments from the upper part of bottom deposits from the Lake Salęt allowed reconstruction of main stages of the Late Holocene vegetation transformation in the Mrągowo Lake District (from ca. 3600 cal...

Late Holocene Palaeoenvironment of Tse Dura, a Later Stone Age (LSA) Rock Shelter, north-central Nigeria

Palynological and archaeobotanical analyses were conducted on excavated sediments from Tse Dura, a Later Stone Age rock shelter in north-central Nigeria with the aim of reconstructing the environment conditions at the si...

PALYNOLOGY AND ARCHAEOLOGY OF LATE VISTULIAN AND EARLY HOLOCENE SITES IN LUBUSKIE LAKE DISTRICT, WESTERN POLAND

The Lubuskie Lake District played an important part in recolonisation of the Polish Plain due to its location and the character of the terrain. Despite that, it is and especially its northern part, poorly explored regard...

Download PDF file
  • EP ID EP359576
  • DOI 10.1515/squa-2017-0009
  • Views 80
  • Downloads 0

How To Cite

Małgorzata Zaremba, Jerzy Trzciński, Fabian Welc (2017). Holocene lake sediments as a source of building material in ancient Egypt; archeometric evidence from Wadi Tumilat (Nile Delta). Studia Quaternaria, 34(2), 109-118. https://www.europub.co.uk/articles/-A-359576