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Tell Abu en-Ni'aj

Photo 4.6

View of Tell Abu en-Ni‘aj, facing northeast, during backfilling at the end of the 1996/97 field season. Tell el-Hayyat is visible as the distant low mound to the right. The town of Meshara lies in the distance.

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Falconer et al. (2019)


Names
Transliterated Name Language Name
Tell Abu en-Niaj Arabic تل أبو النِّعاج
Introduction
Introduction

Tell Abu en-Ni'aj (تل أبو النعاج) is an Early Bronze Age settlement mound located in the northern Jordan Valley of Jordan. Situated approximately 257 m below sea level, the site occupies a strategic position overlooking the fertile agricultural lands of the Jordan Rift Valley. Excavations have demonstrated that Tell Abu en-Ni'aj was an important village community during the Early Bronze IV period, a time traditionally viewed as following the decline of the urban centers of the Early Bronze III.

Archaeological investigations directed by Steven E. Falconer and Patricia L. Fall exposed a substantial settlement covering approximately 2.5 hectares. The excavations revealed mudbrick architecture, courtyards, storage facilities, work areas, streets, and domestic structures that document long-term village occupation. These discoveries have played a major role in demonstrating that sedentary farming communities flourished in the Jordan Valley during the Early Bronze IV period.

Tell Abu en-Ni'aj is particularly important for its well-dated occupational sequence. More than twenty AMS radiocarbon determinations have been obtained from the site, allowing the construction of one of the most detailed chronologies currently available for the Early Bronze IV southern Levant. The evidence indicates that occupation began during the mid-third millennium BCE and continued through multiple architectural phases before the settlement was eventually abandoned near the end of the Early Bronze IV period.

Excavations recovered abundant evidence for agriculture, animal husbandry, food storage, and craft production. Archaeobotanical studies indicate that the inhabitants cultivated crops and managed livestock while taking advantage of the favorable environmental conditions of the Jordan Valley. The site therefore provides valuable evidence for rural economic strategies during a period of significant social and political transformation in the southern Levant.

Today Tell Abu en-Ni'aj serves as one of the key reference sites for understanding Early Bronze IV chronology, settlement organization, subsistence practices, and village life in the Jordan Valley. Its combination of extensive excavation, environmental analysis, and radiocarbon dating has made it an important benchmark for studies of the late third millennium BCE in Jordan and the wider Levant.

Maps, Aerial Views, and Plans
Maps, Aerial Views, and Plans

Maps

  • Fig. 11.1 - Location Map from Falconer et al. (2019)

Aerial Views

  • Tell Abu en-Niaj vicinity in Google Earth

Plans

Site Plans

Normal Size

  • Fig. 2.1 - Topographic Map with excavation squares from Falconer et al. (2019)

Magnified

  • Fig. 2.1 - Topographic Map with excavation squares from Falconer et al. (2019)

Archaeoseismic Chronology
Stratigraphy/Phasing

Tell Abu en-Ni‘aj Stratigraphic Phases

Phase Period Date Description
VII Early Bronze IV earliest occupation Initial settlement founded directly upon archaeologically sterile lakebed deposits. Architecture is confined primarily to Field 4 and represents the earliest village occupation identified at the site.
VI Early Bronze IV early occupation Expansion and remodelling of the village. Architectural remains include domestic structures and a broad-room temple associated with ritual activity and animal burials.
V Early Bronze IV middle occupation Substantial rebuilding and architectural reorganization. Well-preserved domestic architecture occurs in several excavation fields and reflects continued village growth.
IV Early Bronze IV middle occupation Continued occupation with extensive architectural remodelling. Multiple domestic structures, installations, and activity areas indicate an established agricultural village community.
III Early Bronze IV late occupation Village layout becomes particularly clear. Architectural remains from Fields 1 and 4 are linked by streets and shared planning elements, allowing reconstruction of broader settlement organization.
II Early Bronze IV late occupation Occupation becomes restricted to the upper portions of the tell. Domestic architecture continues, but surviving remains are less extensive because of later erosion.
I Early Bronze IV latest occupation Final village occupation preserved immediately beneath the modern surface. Includes a shrine and associated ritual features. Represents the last phase before abandonment.


The excavators identified seven continuous architectural phases (VII–I) buried within approximately 3.3 m of cultural deposits. The sequence begins with Phase VII, founded on sterile lakebed sediments, and continues without evidence for a stratigraphic hiatus through Phase I. All phases belong to the Early Bronze IV period. Architectural remains consist primarily of mudbrick and occasional rammed-earth wall foundations; no stone-founded architecture was identified. The settlement occupied approximately 2.5 ha, of which about 800 m² (roughly 3.2%) was excavated.

Traditional and revised Early and Middle Bronze Age chronologies for the Southern Levant

Table 1.1

Traditional and revised Early and Middle Bronze Age chronologies for the Southern Levant. Traditional chronology based on Levy (1995: fi g. 3); revised chronology based on Regev et al. (2012a), Falconer and Fall (2016, 2017) and Höfl mayer (2017)

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Falconer et al. (2019)


Radiocarbon Chronologies

Table 5.2

Radiocarbon chronologies for the occupations of Early Bronze IV Tell Abu en-Ni‘aj and Middle Bronze Age Tell el-Hayyat. AMS ages based on phase boundary medians produced by Bayesian modelling of calibrated 14C ages. Calibration and modelling of Tell Abu en-Ni‘aj uses OxCal 4.3.2 (Bronk Ramsey 2017) and the IntCal13 atmospheric curve (Reimer et al. 2013). Calibration and modelling of Tell el-Hayyat follows Falconer and Fall (2017) and uses OxCal 4.2.4 (Bronk Ramsey and Lee 2013) and the IntCal 13 atmospheric curve (Reimer et al. 2013). (*Estimated end date for Tell Abu en-Ni‘aj Phase 1)

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Falconer et al. (2019)


Ceramic and Radiocarbon Ages for Tell Abu en-Ni‘aj and Tell el-Hayyat - Falconer and Fall (2017)

Table 1

Chronological revision for the occupations of Middle Bronze Age Tell el-Hayyat and Early Bronze IV Tell Abu en-Ni‘aj. AMS ages based on phase boundary medians produced by Bayesian analysis of 14 radiocarbon ages from Tell el-Hayyat and 24 radiocarbon ages from Tell Abu en-Ni‘aj.

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Falconer and Fall (2017)


Chronological Divisions

The Bronze Age of the Levant

Event XA - Early Bronze IV - 2300-2000 BCE or ~2300 BCE

Discussion

Discussion

References
Ferry et al. (2011)

Archaeoseismology

...Event XA: This event is documented at Tell Abu en-Ni’aj by Savage et al. (2003) as a series of ash layers offset by a fault splay. According to our mapping of the JVF (Fig. 6; Al-Taj, 2000; Ferry et al., 2007), Tell Abu en-Ni’aj appears to be west and off the main active trace by ∼1 km. Savage et al. (2003) do not provide details about the amount or intensity of deformation along that fault, and it is presently not possible to decide whether the observed offsets are related to coseismic fault slip. At Khirbet Iskander, located ∼30 km southeast of the JVF (Fig. 6), Savage et al. (2003) describe a destruction layer in great detail (Table 2), where fire was attested by burnt stones, ash layers, and charred grain. Well-preserved wooden beams and human remains suggest a sudden possibly earthquake-related catastrophe. Proposed date: ∼2300 B.C.

... Overall, our compilation of archaeological studies on tells in the vicinity of the JVF strongly suggests the occurrence of four events: in 759 B.C., ∼1150 B.C., ∼2300 B.C., and ∼2900 B.C.
Here, the archaeological record intersects the historical record, as attested by the 759 B.C. earthquake described in written documents. Furthermore, the archaeoseismic event XA can be correlated with the paleoseismic event YT4 and compensates for the sedimentary hiatus observed in paleoseismic trenches (period ∼1500 B.C. to ∼4500 B.C.). It should be noted that indications for surface breaks affecting tells may not necessarily be considered as faulting evidence. Indeed, tells are artificial mounds made of heterogeneous material that includes rubble, dirt, and architectural remains (Fig. 8a). As such, they are very sensitive to gravitational collapse, especially under seismic shaking. Hence, for sites that are not directly located across the main active trace of the JVF, we consider surface deformation as secondary evidence in the sense of McCalpin (1998). Nonetheless, such indications may provide a relevant chronological constraint for a seismic event. Thus, the mention by Franken (1989, p. 203) of “a victim […] found completely squashed in a crack in the earth” at Tell Deir’ Alla (∼3 km east of the JVF) and Savage et al.’s (2003) previously mentioned “earthquake slip fault” at Tell Abu en-Ni’aj are not considered as strong evidence for surface rupture but may document off-fault effects of a large earthquake.

Table 2 - Archaeoseismic Evidence in the Jordan Valley

Table 2

Compilation of Archaeological Evidence for Strong Perturbations at Archaeological Sites in the Vicinity of the Jordan Valley Fault

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Ferry et al. (2011)


Savage et al. (2001)

The Jordan Valley Village Project: Excavations at Tell Abu en-Ni`aj, 2000

Tell Abu en-Ni`aj is an Early Bronze IV agricultural village site located southwest of the modern town of Meshara in the northern Jordan Valley, approximately 250 m below sea level and 500 m east of the Jordan River. This low tell, originally measuring 2.5 ha, lies at the edge of the ghor (Jordan Rift bottomlands), overlooking the zor (modern Jordan River floodplain). Deep stratified deposits (totaling 3.3 m) and a few Early Bronze III sherds found in the lowest levels indicate that Tell Abu en-Ni`aj enjoyed a long occupational history beginning very early in EB IV. The site's stratification provides a rare opportunity to study diachronic changes in village organization, animal and plant use, and craft production during this period of urban collapse (ca. 2300-2000 B.C.).

The East Jordan Valley Survey discovered Tell Abu en-Ni`aj in 1975 (site 64). Two weeks of testing were conducted in October 1985 during the final excavation season at nearby Tell el-Hayyat. The Jordan Valley Village Project resumed excavation at Tell Abu en-Ni`aj in a five-week season during December 1996 and January 1997, and continued with a 10-week season between January and March 2000.

Ten 4 x 4 m units excavated in 1985 produced abundant material culture, floral and faunal remains, and mudbrick architecture consistent with a sedentary Early Bronze IV farming village. Soundings in two units reached archaeologically sterile sediments and revealed at least three major EB strata. The 1996-1997 season demonstrated that Tell Abu en-Ni`aj contains stratified deposits spanning most or all of Early Bronze IV. Evidence from the basal level suggests that Tell Abu en-Ni`aj was founded shortly after the end of Early Bronze III, then rebuilt in a series of six successive strata lasting until approximately 2000 B.C. (phase 7 is the earliest and phase 1 the latest). Sixteen contiguous 4 x 4 m units revealed a series of domestic structures (figs. 10, 11) and sherd-paved streets located west of courtyards with hearths, pits, storage bins, and a large mudbrick installation possibly used for pressing olives or grapes.

Noncultural sediments were reached in 13 of the 14 4 x 4 m units excavated in 2000, including five started during the 1996-1997 season. In fall 1999 bulldozing on the western side of Tell Abu en-Ni`aj cleared a 26 m long stratigraphic cross-section, revealing an earthquake slip fault. Early Bronze IV deposits capped a series of offset ash layers, indicating that the earthquake occurred during the occupation of Tell Abu en-Ni`aj. A group of three articulated sheep burials allude to Early Bronze IV ritual behavior. Each burial was marked with several 20-50 cm high stones, and each sheep was buried in a 1 m deep pit on its right side, with its head pointed east.

The 2000 field season also revealed diachronic changes in village architecture and ceramic manufacture. Village houses grew denser through time and wall alignments shifted to a new orientation between phases 6 and 5. Despite these changes, Tell Abu en-Ni`aj appears to have been occupied continuously from the time it was founded. Roughly accompanying the architectural changes, local potters stopped using large calcite inclusions in favor of smaller basalt and limestone particles, commonly known as "salt and pepper" temper. These changes hint at the vitality and growing population of this village during the collapse of regional urbanism.

Raphael and Agnon (2018)

EB IV (2300-2000 BCE)

Tell Abu en-Ni'aj: village southwest of the modern town of Meshara, northern Jordan Valley. A 26 m long stratigraphic cross-section along the west revealed an earthquake slip fault (Savage et al., 2001:438-439).

Archaeoseismic Effects
Event XA - Early Bronze IV - 2300-2000 BCE or ~2300 BCE

Effect                                       Location                                       Image(s) Comments
Offset Layers western side of Tell
  • "In fall 1999 bulldozing on the western side of Tell Abu en-Ni`aj cleared a 26 m long stratigraphic cross-section, revealing an earthquake slip fault. Early Bronze IV deposits capped a series of offset ash layers, indicating that the earthquake occurred during the occupation of Tell Abu en-Ni`aj." - Savage et al. (2001:439)

  • "This event is documented at Tell Abu en-Ni’aj by Savage et al. (2001:439) as a series of ash layers offset by a fault splay. According to our mapping of the JVF (Fig. 6; Al-Taj, 2000; Ferry et al., 2007), Tell Abu en-Ni’aj appears to be west and off the main active trace by ∼1 km. Savage et al. (2003) do not provide details about the amount or intensity of deformation along that fault, and it is presently not possible to decide whether the observed offsets are related to coseismic fault slip." - Ferry et al. (2011:56)

Archaeoseismic Intensity Estimates
Event XA - Early Bronze IV - 2300-2000 BCE or ~2300 BCE

Effect                                       Location                                       Image(s) Comments Intensity
Offset Layers (fault scarp) western side of Tell
  • "In fall 1999 bulldozing on the western side of Tell Abu en-Ni`aj cleared a 26 m long stratigraphic cross-section, revealing an earthquake slip fault. Early Bronze IV deposits capped a series of offset ash layers, indicating that the earthquake occurred during the occupation of Tell Abu en-Ni`aj." - Savage et al. (2001:439)

  • "This event is documented at Tell Abu en-Ni’aj by Savage et al. (2001:439) as a series of ash layers offset by a fault splay. According to our mapping of the JVF (Fig. 6; Al-Taj, 2000; Ferry et al., 2007), Tell Abu en-Ni’aj appears to be west and off the main active trace by ∼1 km. Savage et al. (2003) do not provide details about the amount or intensity of deformation along that fault, and it is presently not possible to decide whether the observed offsets are related to coseismic fault slip." - Ferry et al. (2011:56)
VII+
This evidence requires a minimum Intensity of VII (7+) when using the Earthquake Archeological Effects chart of Rodríguez-Pascua et al (2013: 221-224.

Notes and Further Reading
References