Archaeological Landscapes of the Bekaa
Past Results and Future Prospects
Paul Newson*
Abstract
This exploratory paper makes an assessment of our knowledge of the archaeological landscapes of the Bekaa Valley.
As an exemplar the paper utilises as a framework the seminal fieldwork study of Leon Marfoe in assessing what
we understand about the central Bekaa in the Graeco-Roman period. Marfoe’s model of settlement development
for this region and period is comprehensive and complex, however as the paper reveals, modern techniques of
landscape archaeology can provide more detailed information and a more nuanced understanding of the settlement
history. The paper indicates that the Bekaa is a rich archaeological palimpsest for future research.
Keywords Landscape archaeology, Bekaa Valley, Graeco-Roman, settlement development, Lebanon
Introduction
The Bekaa Valley is a fascinating region
of modern Lebanon, at once spectacularly
impressive in its visual impact: it gives an illusion
of a certain separateness, a sense intensified when
approaching from the coast, as one descends down
the bordering mountain slopes of Mount Lebanon
into the plain below (Figure 1). The valley floor
is a flattish plain, 100 kilometres or so long and
only eight to ten kilometres wide, sandwiched
between two high and imposing mountain chains
– the Lebanon and the Anti-Lebanon (Horden
and Purcell 2000: 54; Rey-Coquais 1967: 21). It
is this essential physical geography of the Bekaa
Valley region which engenders these notions
of remoteness, difference and otherness. The
resultant environment provokes reactions in the
visitor and has helped shape the lives of the valley
inhabitants: the physical characteristics help create
* Associate Professor, Department of History and
Archaeology, American University of Beirut, Lebanon
mental maps and a sense of place unlike those
of the rest of Lebanon, which has, ultimately, an
outlook to the Mediterranean Sea. This has long
been noted; for example, the geographer Richard
Thoumin wrote ‘one experiences the deep
impression of being in a region separate from the
rest of the world’ (‘on ressent l’impression très
vive de se trouver en une région séparée du reste
du monde.’) (1936: 273). And Ussama Makdisi
commented on how Western travellers viewed
the wide expanse of the Bekaa as ‘a portal into
a different world’ (1998: 145). Whilst seemingly
separate from the adjacent areas, the plains’
structure is open-ended, and it lies almost parallel
to the coastline, which has allowed it to serve as a
communications corridor between the north and
the south. Also, several mountain passes over
both defining ranges have permitted reasonable
east-west links (Rey-Coquais 1967: 26-27).
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Paul Newson
Figure 1: Bekaa landscape: view west from the Upper Ferzol valley (the foothills of Mount Lebanon) to
the plain and the Anti-Lebanon beyond (photo Hassan el-Hajj)
The special position of the Bekaa as a zone of
transformation has attracted scholars who have
sought to establish theories that explain the
region’s special nature and why it has developed
in particular ways (exemplifying diverse studies
which highlight the exceptional nature of the
Bekaa: Abou Diwan and Doumit 2016; Chatty
1975, 2013; Sommer 2001). Most prominent of
these is the work of Leon Marfoe, an archaeologist
who undertook an innovative archaeological site
survey in the early 1970s across the valley floor
and whose PhD developed influential theories
on the long-term ecology and settlement history
of the region (1978, 1979). Taking Marfoe’s
seminal work as a starting point, this paper will
explore issues of the landscape archaeology of
this region. Using the Graeco-Roman period
as an example, I will discuss some of the key
findings of the long-term settlement history of
the region and its potential in the future. As it is
a large subject, I will concentrate on the region
of the central Bekaa, which can be said to extend
from the Chtaura-Anjar region at the southern
end up to the headwaters of the River Orontes
(Nahr el-Assi) in the north (Figure 2). This has
long been suspected of being the core region of
a programme of Roman settlement development
when it was part of the territory of Beirut (Newson
2015; Sommer 2001).
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Figure 2: The Bekaa region, areas and sites mentioned in
the text
How the Bekaa has been seen
In terms of how the Bekaa has been investigated
archaeologically, the initial attraction was
undoubtedly the monumental temples at Baalbek.
These had been noted by Arab travellers and
geographers throughout the early and medieval
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects
Islamic and into the Ottoman periods, along with
information on the geography, ecology and the
socio-cultural aspects of the valley (Jidejian 1975:
72-78). By the late 17th century CE, European
travellers were drawn to the region specifically
to record the remains of the temples in the town
(Jidejian 1975: 1-10). The first serious study of
these temple ruins were undertaken in 1751 CE by
James Dawkins and Robert Wood (Wood 1757).
Their huge volume of work on Baalbek and also
Palmyra proved to be highly influential both on
architectural fashions in Europe and perceptions
of the orient (Makdisi 1998; Rey-Coquais 1967:
17).
Other visitors followed and began to describe
the customs and culture of the Bekaa more
generally and also individual aspects of ancient
material culture that they encountered, especially
inscriptions, but also various ruins, particularly
of Graeco-Roman temples and structures such as
rock-cut tombs. Visitors included Volney, who
emphasized in Orientalist detail the context of
the temples at Baalbek, and Burckhardt, who
included descriptions of the Bekaa in an account
of a journey to the Lebanon from Damascus
(Burckhardt 1822: 1-50; Makdisi 1998: 141-44;
Volney 1787: 232-48).
The central Bekaa Valley has been the subject
of a variety of archaeological work over the past
sixty years. This work has been very valuable
in providing details of various aspects of the
settlement history of the Bekaa, although a high
percentage of this work has naturally focussed
on understanding the important religious site of
Baalbek. In this regard, one of the first fundamental
studies beyond Baalbek was the documentation of
many of the monumental Graeco-Roman temple
sanctuaries (Krencker and Zschietzschmann
1938). Beyond this, there has been some attempt
through archaeological excavations to determine
the development of the many prominent tells
situated on the valley floor. On this point, the
continuing study of the tell settlement at Kamid
el-Loz in the southern Bekaa Valley has been
significant (e.g., Hachmann 1989; Heinz et al.
2010). A further series of tell excavations has
been those undertaken at the central Bekaa site
of Tell el-Ghassil by the American University
of Beirut Museum (Baramki 1961, 1964, 1966;
Doumet-Serhal 1996).
Other work has concentrated on exploring the
evidence found in the valley for human activity
during earlier prehistoric periods prior to the
development of tells, particularly that of the
Neolithic (notably Copeland 1969; Copeland and
Wescombe 1965, 1966; Kuschke 1978; Kuschke
et al. 1976; Schroeder 1970, 1991). In terms of
the periods of settlement after the tell sites were
abandoned, greatest attention has been paid to
two extraordinary sites of the Classical and early
Islamic periods. The earlier of these two sites
and one which has merited continual research
has been the settlement and sanctuary site at
Baalbek. Recent work has continued to document
and excavate the main temple sanctuary complex
of Baalbek, and to begin an exploration of the
environs (van Ess 2008). An additional historic
site of international importance which has
also been the subject of research is that of the
Umayyad settlement of Anjar (located in the
eastern central Bekaa). Whilst the interior of
the Umayyad settlement has been the subject of
intense excavation and detailed assessments of
the architecture and the site purpose, the territory
and context of this settlement has been largely
ignored (e.g., Chéhab M 1963; Chéhab H 1993;
Finster 2007; Hillenbrand 1999).
Current orthodoxy
The current orthodoxy on long-term settlement
history is founded upon the pioneering survey
work of Leon Marfoe in the 1970s (Marfoe 1978),
the first half of which, dealing with the early
periods up to the Iron Age, was re-edited and
republished in the 1990s (Marfoe 1995, 1998).
Subsequent to this work using the theories of
Clifford Geertz, he developed a complex model
of socio-political organization which he termed
the ‘Integrative Transformation’ (Marfoe 1979,
1982). This model built upon Marfoe’s broad
brushstroke approach to the long-term pattern of
settlement history, which resulted from the many
site visits he made along the length of the Bekaa
(Marfoe 1978). The model essentially explained
changing settlement patterns in the Bekaa as a
consequence of political structural development
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Paul Newson
based on the agglomeration and dispersal of
centralised political units.
Important to Marfoe’s theory was the influence
played by the complex pattern of localized
environments, shaped by different combinations
of natural elements. Influencing factors include:
the mountain topography which impacts on, for
example, the degree of exposure to prevailing
winds and sunlight, and variations in precipitation
due to rain-shadow effects; the underlying
limestone geology ensures an uneven distribution
of surface water leading to a reliance on springs in
most areas, but specific geology in some regions
has led to the creation of lakes and marshy zones
(Horden and Purcell 2000: 56). Consequently,
in terms of land use and settlement types, the
multiple microenvironments thus encouraged
a range of local adaptations. So to give some
examples, in some locations, especially within
the areas with strong perennial karstic springs,
irrigation farming regimes were established,
while in progressively drier regions of the
plain, cereal dry-farming to steppe pastoralism
developed, and the mountain slope regions
experienced the growth of terraced farming and
vertical transhumance (Marfoe 1978: 787-88).
On a regional level, the Bekaa throughout many
periods was envisaged by Marfoe as a distinct no
man’s land between different political entities,
be it Egyptians and Hittites in the Bronze
Age; Seleucid and Ptolemaic kingdoms in the
Hellenistic period; or Fatimids and Hamdanids
in the Early Middle Ages (Horden and Purcell
2000: 87-88; Marfoe 1978: 18). So for a large
part of its history, the Bekaa has acted as a
narrow communications corridor between
dominant political entities situated at the northern
and southern ends, but was itself never fully
dominated by one or the other as a result of the
mountainous environs and the patchy nature of
populations across the valley.
Taking into account these two intersecting
factors – local ecosystems and regional sociopolitical processes – Marfoe envisaged a threelevel development in land use and settlement
within the Bekaa. The first lasted from the end
of the Palaeolithic until the fourth millennium
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BCE and was denoted in the plain by a gradual
specialization into early forms of agriculture and
the establishment of some permanent settlements
in areas with the maximum access to all potential
food sources, be it hunted, collected or farmed
(Marfoe 1978: 789-90). The second level (from
the fourth millennium BCE to the Hellenistic
period) was centred round the advent of urban
forms of settlement, which reflected increasing
populations as a result of specialization in
agricultural techniques and efficiency and in
human occupations (Marfoe 1978: 790-93).
During this period, the population totals in
the valley fluctuated in periods of growth and
decline, a process which continued throughout
the third level of settlement development, which
Marfoe characterized as beginning in the early
Hellenistic period and continuing until the end
of the Ottoman period (1978: 797-99). This
third level was exemplified by the exploitation
and settlement of previously little utilised zones
in the valley region, particularly those zones at
higher altitudes with the emergence of terrace
agriculture and vertical transhumant economies.
A key period within this third phase was from
the beginning of the fourth century BCE to the
eighth century CE – i.e., from the Hellenistic to
the early Islamic. This was an important period
of both political and technical developments
that introduced the basic frameworks which in
many ways governed the settlement and land use
parameters for the rest of the period and continued
until the changes of the 20th century. Many of
these innovations can be seen to stem from the
point when substantial parts of the valley were
incorporated and developed as a Roman colony at
the very end of the first century BCE. Therefore,
because of its potential part in the formation of
the modern landscape, as constituted by Marfoe,
the Graeco-Roman period will form the focus for
the rest of the paper.
In summarizing Marfoe’s survey of settlement for
the period, we can identify a number of points:
1. He saw difficulty in pinpointing Hellenistic
settlement with the result that he regarded it
as ‘ambiguous’ (Marfoe 1978: 620). Though
the evidence was unclear, Marfoe postulated
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects
increases in population and urbanization,
with an exodus from the plain and the central
Bekaa region (1978: 625).
2. For the Roman period, the evidence from
his survey pointed to settlement being at its
greatest. From this, he suggested that Roman
colonial settlement was particularly strong
in the western foothills or piedmont of the
Bekaa, the region in which Hosn Niha is
situated (Marfoe 1978: 647).
3. For the Byzantine period, Marfoe saw a
decline in settlement with a significant focus
shift from small sites to big sites, which he
interpreted as a result of depopulation due
to over-taxation, population decline, and
peasant impoverishment amongst other
reasons (1978: 675-76).
4. For the subsequent early Islamic period,
Marfoe saw a near absence of sites in light
of political uncertainty, which was not fully
overcome until the medieval period and the
resultant settlement expansion of the Mamluk
era (1978: 696-97, 720).
As a result of his survey findings, Marfoe’s
long-term settlement trajectory for the GraecoRoman period marked it as a distinct one, a
pattern which goes against the grain of the results
of many other Near Eastern surveys. This other
survey work has tended to establish the height
of settlement in the Graeco-Roman era to be
during the Byzantine period: with a density in
settlement (and population) not reached again
until very recently. This expansion and increased
density of settlement has been put forward
using as clear case studies the marginal regions
of the Hauran and limestone massif in modern
day Syria (Decker 2009; Tate 1997). Figure 3
shows the comparisons of Marfoe’s survey with
some other surveys of marginal regions of the
Near East in terms of number of sites for each
period. Consequently, the received picture of the
Bekaa is one at odds with most other regions of
the Near East over a comparable timescale (cf
Decker 2007 for other surveys on the frontiers
of Mesopotamia). Is this a true reflection of the
settlement sequence?
Figure 3: Comparison of Mafoe survey site numbers by period with the results of some other notable archaeological surveys
of marginal zones of the Near East. The information is compiled from the results of the following surveys: Birecik-Carchemish
– Algaze et al. 1994; Limes Arabicus - Parker 1992; Southern Ghors - MacDonald 1992; Upper Khabur – Lyonnet 1996; Wadi
el-Hasa - MacDonald 1988
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Paul Newson
Marfoe put forward a number of hypotheses
to explain this particular settlement trajectory
from the Hellenistic to the early Islamic. The
Bekaa region’s incorporation into the Roman
Empire linked it to regional markets and saw
the investment of capital. New, large-scale
investment led to the development of previously
neglected agricultural regions, particularly for
orchard cultivation, terrace agriculture and
increasing transhumance as sheep and goat made
use of higher altitude natural pastures (1978:
797). By the Late Roman period the success
of this expansion had resulted in a large, dense
population, which led to more and more marginal
land being cultivated. Simultaneously, empirewide social changes brought about higher taxes
and rents, and the concentration of landholdings
(Marfoe 1978: 813-14). The cumulative effect
of these processes increased the numbers of
impoverished rural dwellers and led eventually
to the abandonment of settlements and cultivated
land. Marfoe proposed that the remaining rural
population, in order to maximise profits and also
avoid the higher taxes, specialized in animal
husbandry (1978: 815).
At the same time, the development of camel
pastoralism in the semi-arid steppe regions to the
east of the Bekaa resulted in increased pressures
on the availability of pasture within the Bekaa
as sheep and goat herders could no longer utilize
winter pastures in the steppe plains to the north
and east of the Bekaa (Marfoe 1978: 815). The
cycle of increased impoverishment of sedentary
agriculturalists, subsequent farmland abandonment, and takeover by pastoralists continued
until the overall population had decreased and the
dominant settlement and land use patterns within
the Bekaa had been completely transformed in
the Byzantine period (Marfoe 1978: 816). Marfoe
suggested this general pattern of expansion and
contraction had been repeated in other periods:
often as a result of similar processes of political
and social change which, aided by the inherent
ecological constraints of the Bekaa, in turn created
cycles of land use changes and the accompanying
settlement expansion and contraction.
In formulating this rational and credible
hypothesis, Marfoe collected evidence from
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known and visible sites through what might be
called today a ground-truthing exercise. Sites were
known through previous surveys and excavations,
and also a number were found marked on the
1:20,000 topographic maps and available aerial
photographs (Marfoe 1978: 865). In making a
site visit, surface pottery was collected using a
basic systematic collection method, and site size
estimated. Where possible, the diagnostic pottery
was then broadly dated through reference to
similar stratified excavated examples (Marfoe
1978: 829-30). This methodology was very
successful in the sense that a Bekaa-wide range
of sites of different types and sizes was sampled
giving us the most complete picture of the
archaeological resource of the Bekaa as a whole
(Figure 4). Conspicuous in the archaeological
catalogue are the large prominent tell sites of
the central plain region. This is a reflection of a
number of issues beginning with the undoubted
importance of such sites as the main settlement
foci of the Bekaa for much of human history in
the last 10,000 years.
However, it is clear that given the resources and
the time available, Marfoe’s survey had to be
large in scale and broad in scope. This meant that
he relied on published work for many of the sites
prior to the Bronze Age, and areas above the 1500
m contour level were not included (1979: 866). In
completing the fieldwork over such a large region,
there was by necessity a heavy reliance on sites
which were clearly visible and published on the
1:20,000 scale maps. Since Marfoe’s survey was
completed in the 1970s, fieldwork methodologies
have developed exponentially, creating the current
discipline of landscape archaeology. Growing
numbers of fieldwork studies of areas in the Near
East have helped highlight the limitations of
Marfoe’s pioneering study.
There is now an acceptance of the importance
of scale and, in order to obtain a holistic picture
of settlement development, archaeologists
should not only take full account of intra-site
developments but also inter-site relationships
as well. For example, as has been recognized
through more recent studies, the draw of and
emphasis on tell sites has created ‘Landscapes
of Tells’ in many areas of the Near East ignoring
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects
Figure 4: A map of Marfoe’s sites for the Central Bekaa region. The 1500 m contour level (red line) is the
demarcation line for Marfoe’s survey, but note the general absence of sites above the 1250 m contour. The
following symbols represent particular site types: circles - modern villages; squares – tell sites; triangles
– other archaeological sites
other, less conspicuous occupation sites inbetween (Wilkinson 2003: 123). The poor
knowledge of the relationship of settlement
change to material culture change has also been
shown to be responsible for gaps in settlement, as
demonstrated by the transformation of settlement
types in the Early Bronze IV and Persian periods
in Jordan (Banning 1996).
Recent work
Shortly after Marfoe’s fieldwork survey had been
initiated, Lebanon descended into fifteen long
years of civil war, and it was not really possible
to undertake any archaeological work until the
dawning of the current century. The majority
of this new phase of work has been completed
at the large important sites such as Baalbek and
Kamid el-Loz. There has been some survey and
site recording work attempted in the continuing
difficult political environment which still
persists in the Bekaa Valley (Figure 5). A crucial
element of this work has been completed by the
Department of Antiquities of Lebanon as part
of CRM (Cultural Resource Management) and
development recording. Conspicuous among the
published survey work has been the preliminary
results of Bonatz and others conducted at the
beginning of this century to the east of Kamid
el-Loz in the foothills of the Anti-Lebanon (Bonatz
et al. 2002). A second survey was carried out in
the immediate environs of Baalbek by FischerGenz and Ehrig, and though this was interrupted
by the 2006 war, the results as with the earlier
survey by Bonatz reveal a very different picture
of settlement and land use for the region (FischerGenz and Ehrig 2005).
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Paul Newson
Figure 5: Map of the Bekaa valley with location of recent survey work areas: A = Baalbek Hinterland
Survey (Fischer-Genz and Ehrig 2005); B = Kamid el-Loz and Anti-Lebanon Survey (Bonatz et al. 2002);
C = Central Bekaa Region – Niha and Ferzol Valleys (Newson and Young 2014, 2015). Black dots are sites
recorded in Marfoe’s survey (1978)
Both surveys concentrated their work on small
sample areas and so were able to use more
intensive methods than Marfoe for recording
archaeological information. Bonatz’s team
walked the majority of their survey area
(c. 150 km2), with particular attention on areas
away from the mountain tops and very steep
slopes (2002: 287). The Fischer-Genz and Ehrig
survey covered a similar area (c. 120 km2) using
a combination of ‘extensive survey’ – locating
sites with information from maps and local
informants and in some test areas walking a series
of short intensive transects (2005: 138). Perhaps
the key outcome from each of these short-lived
small area surveys relates to the high density of
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archaeological remains that can be documented
within different topographical environments on
the margins of the Bekaa Valley, specifically in
these instances from among the piedmont regions
of the western slopes of the Anti-Lebanon.
Both surveys documented a range of sites with
different functions, from dwelling to agricultural
production, and dating to all the main periods
from the prehistoric to the Islamic.
As one might expect from a more intensive
approach to fieldwork, the density of sites in both
areas is far greater than one would suppose from
Marfoe’s work. Within the Baalbek region, of
the 13 substantial settlement sites recorded and
represented on the Bekaa hinterland survey map,
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects
only five were previously noted by Marfoe in
his survey (Fischer-Genz and Ehrig 2005: 137;
Fig. 21). The Bonatz survey has published more
extensive information on the types of site they
recorded in their survey. They classify a variety
of different settlement sites, from temporary
nomadic sites (e.g., Sites 35, 52 and 53) to longterm farmhouse and/or hamlet settlement sites
(e.g., Sites 19, 30 and 45) (Bonatz et al. 2002:
292-97). In addition, there were numerous other
site types, such as Roman religious sites (Sites
36 and 38) and watermills of the Islamic periods
(Sites 26-28, 34), amongst others (Bonatz et al.
2002: 292-95). Each survey also recorded what
they describe as tell sites: Tell Kabb el-Kroûm
(Site 14) (Bonatz et al. 2002: 288; Fig. 7) and
Site 33 (Fischer-Genz and Ehrig 2005: 137).
These small tell sites are important for they reveal
Bronze Age (and later) occupations away from
the plain at strategic points controlling access
along narrow valleys of the Anti-Lebanon.
Whilst only preliminary summaries of the surveys
have been published, both these surveys thus
effectively demonstrate the intensive occupation
of the land in regions which had previously been
classified as somewhat marginal. Secondly, they
also effectively provide evidence which seems
in certain ways to contradict the survey results
and subsequently some of the conclusions
reached by Marfoe. For example, Fischer-Genz
and Ehrig point out that their survey results
indicating prehistoric settlement beyond the
plain overturn Marfoe’s notion of forest cover
inhibiting settlement exploitation of the slopes of
the Anti-Lebanon (Fischer-Genz and Ehrig 2005:
138). Thirdly, on a wider scale, both surveys
have recorded sites from all periods, some of
which have previously been under-represented in
Marfoe’s seminal work. This is particularly true
for off-tell sites of the Bronze and Iron Ages, and
for both surveys, especially the Hellenistic. In
the Bonatz survey, Hellenistic sites proved to be
17 in number, second only to Islamic sites (with
24) (Bonatz et al. 2002: 300). Clearly, a more
intensive investigation of a smaller area using
modern methods and approaches to landscape
survey can provide new insights to the settlement
development and land use within the Bekaa.
These surveys also help stress the point that
Marfoe’s model of the Bekaa would benefit from
a reassessment.
New work
The prospect of investigating a vital region in
the Bekaa, the central western piedmont, has
provided an opportunity to apply more systematic
methodologies in recording archaeological
remains and surface material. An important
intention of the Central Bekaa Project (CBP),
an ongoing fieldwork project by this author,
was to document the morphology of settlements
in the Graeco-Roman period and explore the
relationships between settlements and their
environments. This project has also provided a
basis with which to explore in depth some of the
issues raised by Marfoe, who listed only a limited
number of sites for this region (on the whole just
village sites – the list of information for his sites
in this area can be seen in Table 1; Figure 6). The
initial impetus to the project was an invitation
from the Department of Antiquities to document
the surface archaeology of the remains of the
village associated with and dominated by the stillstanding remains of a Roman period monumental
temple sanctuary at Hosn Niha (Newson and
Young 2014, 2015). Since then, work has
expanded down the Niha Valley to the environs
of the village of Niha and into the parallel Ferzol
Valley (Wadi el-Habis) 2 km or so to the southeast.
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Figure 6: Map of sites from Marfoe’s survey within the western piedmont region, that is, above the 1000 m contour
line (see Table 1). Key sites include: 199 = Niha; 200 = Hosn Niha; 201 = Ferzol; 205 = Le Laure (Nabaa el-Habis)
Hosn Niha
The site at Hosn Niha was chosen for a number
of reasons. The monumental scale of the large
temple at Hosn Niha and its well-preserved and
picturesque bearing have ensured that the site
has attracted attention from visitors, both tourists
and archaeologists (Figure 7). The majority
of previous work there has been focussed on
documenting the main religious sanctuary,
which includes a later Byzantine basilica church
(Aliquot 2009: 303-06; Steinsapir 2005: 7880). Long known to be associated with this
large religious sanctuary are the remains of a
settlement. Unfortunately, a high percentage of
the settlement has been badly damaged in a long
series of illegal excavations going back at least to
the 19th century CE, if not earlier. It was known
that some of this damage was carried out during
the civil war period, so as well as recording any
archaeological features, a significant aim of the
project was to make an assessment of the extent
of the damage (Newson and Young 2015).
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Prior to our project, Jean Yasmine had completed a
series of site studies and an excellent examination
of the structures related to the religious complex
(2005, 2006, 2009, 2013). As part of this work,
Yasmine also sketched a brief outline of the visible
remains of the associated village and collected
some pottery sherds exposed in sections or brought
to the surface in the illegal excavations (2006: 1318, 47-48). Most of the pottery sherds were found
to be locally sourced coarsewares, and at the
time these pottery types were little known from
excavated contexts elsewhere. Because of this fact,
Yasmine’s pottery expert Abdallah Allamedine
could only make a preliminary analysis. In this
analysis, the majority of the diagnostic pottery was
dated to either the first century or the sixth century
CE (Yasmine 2006: 57-58).
From such analyses as were made, it was suggested
that the village was founded in the first century
CE as part of the Roman colony of Beirut. That
is, it was founded by veteran legionary soldiers
and their families who, as far as we know, were
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects 11
Figure 7: The large Graeco-Roman temple at Hosn Niha
given parcels of agricultural land in the central
Bekaa Valley. Although the pottery did not reflect
this, as little was dated to the second century CE,
it was assumed the settlement’s prosperity reached
its peak during this century, as it was during this
period that the large temple was constructed.
The building of a church and at least one large
farmstead in the Byzantine period suggests the
settlement continued to function into the later
period. From the pottery, it was assumed that the
settlement was completely abandoned with the
coming of Islam in the mid-seventh century CE
(Yasmine 2006: 48).
Therefore, to obtain a more comprehensive
assessment of the village remains, it was
necessary to employ systematic methods of
enquiry. Through the use of these approaches the
work began to achieve a number of specific aims
including:
1. A record of the range and spatial location
of different structures and the extent of their
preservation;
2. The acquisition of a more nuanced picture
of the relationship between the village and
the religious complex of temples and the
succeeding church;
3. The reconstruction of the spatial and
chronological development of the village;
4. And finally the placement of the settlement
within its regional context.
Although the work at Hosn Niha is ongoing, the
first season in late 2011 was spent assessing the
extent of the visible structural remains and their
spatial relationships. The village remains were
found to extend across some 600 metres southwest–north-east following the contour line of the
slope and some 100 metres down to the foot of
the slope (Figure 8). Within this six hectare area
a range of features was recorded by differential
GPS including various tombs, structures and
exposed wall fragments of buried structures and
terraces (Newson and Young 2014). As there
appeared to be few complete structural remains
on the surface, a series of 50-metre transects was
undertaken to record surface density distributions
of pottery and to collect a sample of diagnostic
sherds from across the village site. This sample
diagnostic pottery is currently being processed
(by Dr Hanna Hamel), and further work is
required on its assessment, particularly in light of
potential future work at the site. However, some
preliminary remarks can be made.
Berytus LVI, 2016
12 Paul Newson
A high percentage of the pottery recovered has
been storage vessels, which follows Yasmine’s
findings and reflects the intense agricultural
nature of the settlement. Nevertheless, there are
some finewares of different periods and there
is some differential spatial patterning of pottery
types and periods beginning to emerge across the
site. As a consequence, it appears that the history
of settlement at the site is perhaps more complex
than either Marfoe or Yasmine predicted. Certainly
it is amply clear settlement that extended into
the Byzantine, perhaps the Early Islamic, which
Marfoe did not envisage. Having said this, in
line with the views of Yasmine, there is as yet
no definite sign of settlement prior to the first
century CE with an absence of evidence so far for
early Hellenistic or earlier pottery, although some
Eastern Sigillata A has been collected that could
date to the first century BCE. This would seem
to confirm that large-scale sedentary occupation
at this relatively high altitude location could be
directly related to the institution of the Roman
colony. As perceived by Marfoe, this entailed the
subsequent increased exploitation of formerly
Figure 8: The key site remains at Hosn Niha
Berytus LVI, 2016
marginal areas by Roman smallholders for the
production of olive and vine (1978: 661-63).
Undoubtedly, the main focus of settlement is that
of the Roman and Byzantine period. Given such
a long period of time, over 600 years at least,
it is probably not surprising that the evidence
so far collected would seem to suggest there
were changes in the spatial morphology of the
village. The surface pottery indicates that for
the Roman period the settlement was a more
dense agglomeration at the foot of the slope in
the south-western area of the site. By the time of
the Byzantine period, this compactness had been
replaced by a more diffuse form of occupation
spread over a greater area (Newson and Young
2015: 459). The type of dwelling also seems to
have evolved between the two periods. In the
Roman period, the village form would appear
to be a concentration on many small dwellings,
densely clustered with some less dense occupation
on the margins. In the Byzantine period, there
were more dispersed, large farmhouse types,
as demonstrated by the substantial well-built
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects 13
remains of HN016 (Newson and Young 2014:
262; Yasmine 2006: 14-15). The numbers of these
large farm houses may have been relatively few.
As stated earlier, an additional problem is the
current knowledge of the local pottery types.
Particularly problematic is the extent to which
the Byzantine pottery types continued into the
early Islamic period. Whilst for the Bekaa this
is at present unclear, what is very clear is that
following a hiatus there was a reoccupation
of part of the settlement in the early medieval
period. The surface collection of diagnostics
has identified a particular concentration of
characteristic and glazed pottery sherds dating to
the 13th and 14th centuries CE in the vicinity of
the large stone construction in the south-western
part of the site (HN003) (Newson and Young
2014: 265-66). In reviewing the evidence gained,
particular questions spring to mind; notably, does
this represent a continuation of occupation from
the early Islamic period, or is this a reoccupation
of the most favourable part of the site? Was
the large stone ‘Tower construction’ (HN003)
perhaps an early medieval fortified farm that
guarded a pass over the mountain, the focus of a
renewed or rejuvenated settlement?
The interesting results from Hosn Niha in terms
of its settlement development history and size
have invited comparisons with other settlements
to see if these results were similar or different.
There was as yet no directly comparable rural site
of a similar size and function in the central Bekaa
Valley with which to make valid comparisons
in terms of settlement history. Kamid el-Loz
provides substantial evidence for occupation in
the Hellenistic and the Roman period, but there
is a shift away from this ancient tell site during
the Byzantine period (Heinz 2016: 47). Hence in
terms of the trajectory of settlement development
and occupation, there are major differences
apparent between these sites. On the other side
of Mount Sannine, in the region of the Metn,
one of the few rural sites in terms of comparable
size and geographic situation to Hosn Niha has
been investigated. This is the village site of
Ej-Jaouze, the archaeological results of which are
in the process of being published by the director
Lina Nacouzi and others (Nacouzi et al. 2004)
(Figure 2).
The site of Ej-Jaouze, which lies at an altitude
of 1320 m, seems to exhibit a similar occupation
sequence for the Graeco-Roman period onwards.
From the structural evidence at this site, it is
clear there was a contrast in settlement structure
between the small dense structures of the Roman
period and the Byzantine period, which is
characterised by the construction of a single large
rectangular farmstead: a farmstead that appears
very similar in design to the exposed rectangular
structure ‘le grande residence,’ as named by
Yasmine at Hosn Niha (HN016 - Figure 8). A
further indication is that the surface pottery
assemblage from Ej-Jaouze, which consists of
pottery from the Roman and Byzantine periods
followed by a lacuna in sherds until pottery of the
12th and 14th centuries, reveals a reoccupation of
the site, just as at Hosn Niha.
Niha
Perhaps the best location for comparisons to
Hosn Niha of village size, development history
and occupation is the adjoining site of the village
of Niha, two kilometres to the south-east, at an
altitude of 1100 m (Figure 9). This too has a
monumental Graeco-Roman temple sanctuary
whose remains date to the first and second
centuries CE and whose architecture is similar
in style to that of Hosn Niha (Freyburger 1999;
Krencker and Zschietzschmann 1938, 105-37;
Steinsapir 2005: 74-78). Often found associated
with the temple sanctuary are numerous statues,
altars and other worked stone (Fani 2009). Niha
village is also very important for the GraecoRoman period in terms of the number of Greek and
Latin inscriptions that have been recorded in its
environs. A high proportion of these inscriptions
are memorials to burials, while others are altar
and statue dedications (Figure 10). In terms of
the Bekaa region, these form the best collection
of inscriptions for this period outside Baalbek,
and have been used frequently to provide insights
into the society and governance of the Roman
colony (Ghadban 1987; Rey-Coquais 1987).
Berytus LVI, 2016
14 Paul Newson
Figure 9: The Niha valley looking south towards the village of Niha, to the right of the village is the
reconstructed large Graeco-Roman temple
As with Hosn Niha, the temple sanctuary at Niha,
and particularly the large temple, has been the
subject of continued research on different aspects
and of a protracted series of excavations and
restorations in the 1940s and 1960s (summaries:
Aliquot 2009: 300-03; Donceel 1966: 255-56;
Yasmine 2009: 141-44). Unfortunately, the
detailed evidence from the excavations, such
as the pottery finds, have not been published.
Consequently, there are gaps in the story of
the sanctuary development, and very little is
known about the village associated with it. A key
hindrance to studying Niha village development
is the occupation of the site today by the modern
village. However, within and around the village
are enclosed areas of open land or what might be
designated fields, some of which are cultivated as
vineyards or orchards or olive groves, and others
of which are used as gardens or remain waste
land. These areas have offered opportunities for
the collection of surface material with which to
compare the results from Hosn Niha.
villagers, the addition or removal of topsoil from
and to other regions around the village. Though
some of these claims may have been aimed at
dissuading archaeologists from investigating
their land, others could have some truth in
them. There has certainly been a great deal of
remodelling of the Niha village landscape, for
example, with new houses sometimes built on
large, high platforms and the construction of
roads on extended causeways; all of which has
necessitated an extensive amount of terrace
cutting into the steep-sided slopes of the narrow
valley that Niha village occupies. The open
areas were sampled in a systematic way so that
densities of surface pottery could be calculated
and could act as a check on soil changes. So
transects of 10 metres apart were walked along the
longest axis of each field, followed by a general
collection of diagnostics. As with Hosn Niha, any
archaeological feature, such as rock-cut tombs
and ancient terracing, as well as information on
the position of worked stones were recorded.
There are some potential problems in collecting
surface material from such fields, including
the levelling of areas and, as reported by some
Preliminary results have proved to be very
promising. The collection of surface pottery has
revealed interesting patterns in terms of their
Berytus LVI, 2016
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects 15
density across the village (Figure 11).
The densest areas of pottery are located
to the north and south of the temple
sanctuary (Fields NH 2, 5, 6 and 12).
The remaining dense areas of pottery
generally line the course of the stream
bed of the Nahr (river) Niha which
bisects the village (Fields NH 12-15,
21, 33). Otherwise apart from the large
fields NH 24 and 25 which abut the
edge of the village in a small side valley,
surface sherd density is very low. This
is true as one moves further away from
the present-day village core and also,
interestingly, for the steeply terraced
fields of the valley slopes which tightly
Figure 10: The reconstructed large temple at Niha
encompass the village. The lack of
sherds on the terrace fields and on fields
away from the village would suggest that higher
seem to allude to some form of earlier activity/
density areas are a sign of occupation – i.e., where
occupation of the site.
the villagers lived. This would strongly suggest
that the current village core is built more or less
Further work
on the ancient village.
The need to go beyond the known site and to
As for the periods in which this village was
try and expand knowledge of the relationship
inhabited, the post-Graeco-Roman period pottery
between core village settlement sites and the, at
has yet to be studied, but cursory analyses reveal
present, relatively unknown inter-site regions of
some patterning in sherd distribution (Figure 12).
the Bekaa has led to a recent expansion of the
The fields at the north end of the village (e.g.,
Central Bekaa Project (Figure 13). As a contrast
NH 1, 2, 5 and 6) are dense in Graeco-Roman
and comparison to the Niha Valley, the nearby
wares, particularly finewares of Eastern Sigillata
Ferzol Valley provides a good opportunity to
A forms of the very end of the first century
explore such inter-site relationships in depth. As
BCE and early first century CE. This contrasts
with Niha Valley, the Ferzol Valley is dominated
sharply with fields immediately south of the
by the site of a Graeco-Roman village which
temple and along the course of the Nahr Niha,
also has its own monumental temple sanctuary
where, although there are some early Graecocomplex (Aliquot 2009: 306; Taylor 1971: 33).
Roman sherds, the majority are from the Islamic
The Ferzol Valley (also called the Wadi el-Habis)
periods and particularly apparent are the glazed
is wider and more densely farmed than the Niha
wares of the 13th-14th centuries CE. Of more
Valley (Figure 14). A programme of intense
intriguing interest are a number of earlier sherds,
systematic fieldwalking was begun in 2016 at
occasional sherds of the third-fourth millennium
different locations within the valley to sample
Chalcolithic, Bronze and Iron Ages which were
different valley environments and to look for
located in fields on the eastern and southern edges
evidence of small sites and other occupational
of the built-up core of the village (NH14, 15,
activity outside the large long-term settlement
21 and 33). Although only very few in number,
sites as epitomised by the village sites at Niha
the consistent location of these earlier sherds,
and Ferzol. Therefore, for the first season, four
and their being from successive periods would
areas were fieldwalked:
Berytus LVI, 2016
16 Paul Newson
Figure 11: Density map of surface pottery in and around the village of Niha. There is a much higher density
of sherds within the core village area, especially along the course of the Nahr Niha, and in the environs of the
Graeco-Roman temple sanctuary
Berytus LVI, 2016
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects 17
Figure 12: Map of Niha showing pattern of sherds relating to major periods. This is based on a preliminary
assessment of the surface pottery. The distribution highlights a number of issues which require further work.
Although the numbers are very few, there is evidence for some activity in the valley in the period before the
Hellenistic. Secondly, there is a significant concentration of early Roman pottery in the regions to the north
of the present village. Thirdly, pottery numbers drop significantly as one moves away from the village centre
(see Figure 11), in this central region, medieval Islamic pottery dominates, although there are also significant
numbers of Roman ceramic sherds
Berytus LVI, 2016
18 Paul Newson
1. The upper high valley area beyond the
escarpment which divides it from the rest of
the valley.
monastery, includes the site of numerous
rock-cut tombs and a karstic spring (Newson
2015; Nordiguian 2005: 46-49).
2. The region of Nabaa el-Habis or, as
commonly called in academic publications,
‘La Laure’ (French - hermetic monastery),
immediately at the foot of the escarpment
which, besides the supposed hermetic
3. A sample of fields midway between ‘La
Laure’ and the village of Ferzol.
4. A sample of open areas closest to the
location of the Graeco-Roman temple
sanctuary.
Figure 13: Map of fieldwalked areas of the Ferzol valley. Initial results suggest areas of dense
pottery within Areas 2 and 4. Area 3 has significant coverage of pottery, while Area 1 has very little.
Further systematic fieldwalking is planned
Berytus LVI, 2016
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects 19
Figure 14: The Ferzol valley (Wadi el Habis) looking southwest towards the Bekaa valley taken from ‘La
Laure’. This valley is wider than the neighbouring Niha valley, and is unsurprisingly much more densely
cultivated with many fine vineyards
The results are at a preliminary stage, but
again the collection of surface material in
a systematic manner is already providing
valuable information. The density of sherds
varies between the different sample areas,
with very few sherds from area 1 compared to
area 3, indicating that the upper region was an area
of little activity. Within area 3, very dense areas
of surface sherds have indicated the presence of
isolated, small occupation sites, including at least
one for the Hellenistic period, which is likely
to be related to a farmstead of some sort. There
is pottery from multiple periods from both ‘La
Laure’ and the village, especially of the Islamic
and Graeco-Roman periods, suggesting as with
the Niha Valley, long-term occupation over many
periods. Furthermore, initial impressions of the
very high percentage of early medieval Islamic
pottery at the ‘Laure’ site would seem to suggest
that at this time a thriving community was
prospering in this location (Figure 15).
Conclusion
This paper has sought to highlight and discuss
just a few of the issues concerned with our
understanding of the Bekaa. It has shown that
relatively little work has so far been accomplished
beyond intra-site studies of pivotal sites within
the Bekaa plain. Although the magisterial work
of Marfoe remains the basis for any assessment
of long-term settlement, the application of
modern landscape methodologies is beginning to
clarify our views. Many of Marfoe’s hypotheses
are being confirmed whilst others will have to be
re-thought.
Systematic surface investigation in the central
Bekaa Valley is beginning to show interesting
results and is changing perceived notions of
the rural settlement history of the Bekaa. It is
hoped this work will continue in the near future
and allow us to obtain a more nuanced view
of the occupation sequence within this region,
Berytus LVI, 2016
20 Paul Newson
Figure 15: The rock-cut limestone scarp of ‘La Laure’ in the Ferzol valley. This is a rich zone of rockcut tombs; some were converted to troglodyte habitations in later periods and traditionally formed a
monastery
particularly for evidence of the cycle of population
continuity or rupture between different settlement
periods between the Late Byzantine and the early
Islamic periods.
It could be that what the archaeology at sites
such as Hosn Niha is revealing is a characteristic
settlement history for the upland regions of the
Lebanon, in which relatively high altitude areas are
only settled as a result of particular socio-cultural
conditions prevalent in the lower lying regions.
This tends to confirm Marfoe’s thesis on some
levels, but it also highlights some of the limitations
of his study in concentrating on the Bekaa plain
and regions below the 1500 m contour.
Berytus LVI, 2016
Future work will necessarily need to investigate
the relationship between the plain and the
mountain, and to use the whole raft of tools
available to current landscape archaeologists
(e.g., remote sensing technologies, geophysical
work, diatom studies and residue analyses) to
account for new concerns from levels of scale to
environment exploitation (Altaweel 2016: 1706).
By completing such studies, we will be able to
better assess the extent to which this important
region conforms or otherwise to other regions
in the Near East, and not just in settlement
trajectories but in many other ways as well.
Archaeological Landscapes of the Bekaa – Past Results and Future Prospects 21
Marfoe
Site
Number
Marfoe Site Name
(Other Name)
Site Type
Source of
Information
Marfoe
Palaeolithic
Environment
Zone
196
El Karak (Karak
Nuh)
Modern village:
Tomb
Archaeological
remains
UCAT
197
Qsarnaba
Modern village:
Temple
Archaeological
remains
198
Temnine el Faouqa
Temple
199
Niha
200
Late
Bronze
Hellenistic
Islamic
(Medieval)
Ottoman
X
X
X
PPW
X
X
X
Archaeological
remains
PPW
X
Modern village:
Temple
Archaeological
remains
PPW
X
X
X
Hosn Niha
Temple
Archaeological
remains
PPW
X
201
El Fourzol (Ferzol)
Modern village:
Temple
Archaeological
remains
PPW
X
X
202
Ain es Sefli
Roman site
Archaeological
remains
PPW
203
Bir el Joubb
Unknown
Archaeological
remains
PPW
204
Balbassane
Unknown
Archaeological
remains
PPW
205
Nebaa el Habis
Tombs
Archaeological
remains
PPW
*230
Jebel Baniya
Palaeolithic tool
scatter
Archaeological
remains
MS-MW
246
Mseidej
Roman site
Archaeological
remains
RPS
428
Zahle
Modern town
Text reference
PPW
429
Maallaqa
Modern village
Text reference
AAF
430
Nabi Ayla
Modern village
Text reference
PPW
X
443
Bednayel
Modern village
Text reference
PPW
X
444
Beit Chama
Modern village
Text reference
PPW
X
445
Kfar Dabach
Modern village
Text reference
RPS
X
X
Roman
X
Byzantine
X
X
X
X
X
X
X
Table 1: Shows a summary of Marfoe’s site catalog for the Western Piedmont of the Bekaa (See Figure 6). For each site
the known dated material information is shown, and the Marfoe environment zone of each site location (Marfoe 1978). The
Environment Zone abbreviations stand for: AAF – Active Alluvial Fan; MS-MW – Mountain Slope/Mountain Wadi; PPW
– Perennial Piedmont Wadis; RPS – Rocky Piedmont Slopes; UCAT – Upper Colluvial-Alluvial Terraces. An * for the site
number 230 (Jebel Baniya) means the site is outside Marfoe’s Survey Area
Acknowledgements
The fieldwork mentioned in this paper has been
funded by generous grants from the University
Research Board of AUB. I would also like to thank
the Directorate General of Antiquities, Lebanon,
and especially the Director General Sarkis El
Khoury and Raffi Gerjian for their continued
support, as well as the people of Ferzol and Niha.
And not least, I am grateful to the late Professor
Tony Wilkinson for interesting discussions of his
work and time with Leon Marfoe in the Bekaa
and its importance as an exceptional phenomena
of the Near East.
Berytus LVI, 2016
22 Paul Newson
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