Hostname: page-component-77f85d65b8-45ctf Total loading time: 0 Render date: 2026-03-29T18:42:35.677Z Has data issue: false hasContentIssue false

The “Governor’s Residency” at Tel ‘Eton, The United Monarchy, and the Impact of the Old-House Effect on Large-Scale Archaeological Reconstructions

Published online by Cambridge University Press:  13 March 2018

Avraham Faust*
Affiliation:
The Institute of Archaeology, The Martin (Szusz) Department of Land of Israel Studies and Archaeology, Ramat-Gan 5290002, Israel
Yair Sapir
Affiliation:
The Institute of Archaeology, The Martin (Szusz) Department of Land of Israel Studies and Archaeology, Ramat-Gan 5290002, Israel
*
*Corresponding author. Email: avraham.faust@biu.ac.il.
Rights & Permissions [Opens in a new window]

Abstract

The “governor’s residency” at Tel ‘Eton was destroyed in the late 8th century BCE in an Assyrian military campaign. While the numerous finds enable a detailed reconstruction of life on the eve of the destruction, this elite house was cleaned continuously, and since no floor raisings were identified, little was known of the building’s period of use. Radiocarbon (14C) samples taken from within a foundation deposit and from the floor make-up, however, indicate that the earliest phase of the residency was built in the late 11th–10th century BCE. This has bearings on the date in which social complexity evolved in Judah, on the debate regarding the historicity of the kingdom of David and Solomon, and it also provides the earliest date for the use of ashlar stones in Judah. Finally, the long life of the “governor’s residency” exemplifies a little addressed phenomenon—the old-house effect—in which buildings and settlements existed for a few centuries, but only left significant remains from their last phase. The earlier phases are hardly represented in the finds, barely studied, and rarely published. We suggest that the old-house effect influences archaeological interpretations world-wide, and is also responsible for recent attempts to down-date social complexity in Judah.

Information

Type
Research Article
Creative Commons
Creative Common License - CCCreative Common License - BYCreative Common License - NCCreative Common License - SA
The online version of this article is published within an Open Access environment subject to the conditions of the Creative Commons Attribution-NonCommercial-ShareAlike licence <http://creativecommons.org/licenses/by-nc-sa/4.0/>. The written permission of Cambridge University Press must be obtained for commercial re-use.
Copyright
© 2018 by the Arizona Board of Regents on behalf of the University of Arizona
Figure 0

Figure 1 Location map of Tel ‘Eton and other sites mentioned in the text. (All figures courtesy of the Tel ‘Eton Archaeological Expedition.)

Figure 1

Figure 2 Plan of Tel ‘Eton, with excavation areas marked.

Figure 2

Figure 3 Composite aerial photograph of Area A, showing Building 101. (Photographs by Sky-View and Griffin Aerial Imaging; dividing lines not marked.)

Figure 3

Figure 4 Plan of Area A, with Building 101. The locations of the sections (Figures 6 and 7a) and of the 14C samples are marked.

Figure 4

Figure 5 Ashlar stones: (a) ashlar stones at the main entrance to the building, looking north; (b) ashlar stones at the corners of the entrances to the rooms at the broad space (Rooms 101B and 101C), looking west.

Figure 5

Figure 6 Section in the floor of Room 101D, revealing a loose layer of small fragments of limestone mixed with ash (looking east). Note the earth layers (below the stone foundations) to the right (south).

Figure 6

Figure 7 (a) The section in the courtyard, looking east. Note the chalk tablets (mainly in the left) and the hard, compact earth (to the right), which was subsequently excavated and in which the foundation deposit (Figure 7b) was unearthed (approximate area is marked); (b) the foundation deposit below the floor of space 101A3 in the course of the excavations (looking east).

Figure 7

Figure 8 Stratigraphic sequence of calibrated dates in Area A, calibrated and determined with the OxCal 4.2 program (Bronk Ramsey 1995, 2009), using the IntCal13 calibration curve (Reimer et al. 2013).

Figure 8

Table 1 14C results for the four samples that were taken from the floor make-up of the “governor’s residency” and below it, determined and calibrated with the OxCal 4.2 program (Bronk Ramsey 1995, 2009), using the IntCal13 calibration curve (Reimer et al. 2013).