Results of a survey conducted in the area of the Jiyeh Marina Resort hotel complex in the 2012 season

2016 ◽  
Vol XXIV (1) ◽  
pp. 491-503
Author(s):  
Zofia Kowarska ◽  
Szymon Lenarczyk

In 2012, an initial reconnaissance was conducted of the area north of the Jiyeh (Porphyreon) site. This coastal region is heavily urbanized and progressing building investment is causing the destruction of archaeological remains, which until quite recently were relatively well preserved in places. Subsequent investments involved the expansion of the Jiyeh Marina Resort hotel complex into terrain lying to the north of the Polish excavation area. Earlier construction work connected to the hotel complex was carried out in an area originally occupied by a pottery workshop from the late Hellenistic and early Roman periods, as well as at the site of a Roman– late antique necropolis. Further construction work, conducted without archaeological supervision, revealed more ancient structures which were in all probability connected with wine production.

2018 ◽  
Vol 31 ◽  
pp. 387-405
Author(s):  
Roi Sabar

Eastern Upper Galilee in the Roman period evidently housed two ethnic groups in an often hostile relationship (cf. Jos., BJ 3.35-40): in the north, a pagan population belonging to the chora of Tyre, which would have included Qedesh, and in the south a Jewish population. The two ethnic-based territories, which exhibit clear differences in their material culture, were separated by the deep ravine of Naḥal Dishon (wadi Hindaj). Other than urban temples, pagan temples, usually dated to the 2nd and 3rd c. A.D., are limited to the area north of Naḥal Dishon, while synagogues, which continued to be erected into the late-antique period, lie to its south. Qedesh lies 35 km southeast of the large metropolis of Tyre (fig. 1) across a rough mountainous area which made communication somewhat difficult.


2020 ◽  
pp. 469-496
Author(s):  
Grzegorz Majcherek

The report offers an account of archaeological and conservation work carried out at the site. Excavations in the central part of the site (Sector F) were continued for the fourth season in a row. Exploration of remains of early Roman houses led to the discovery of a well preserved multicolored triclinium mosaic floor with a floral and geometric design. A large assemblage of fragments of polychrome marble floor tiles, recorded in the house collapse, showed the scale of importation of decorative stone material from various regions of the Mediterranean. Overlying the early Roman strata was direct evidence of intensive construction work carried out in the vicinity in the form of large-scale kilnworks, supplying lime most probably for the building of the late Roman bath and cistern. Included in the presentation is a brief review of the limited conservation work that was conducted in the complex of late antique auditoria.


Author(s):  
Brian Chadwick ◽  
Adam A. Garde ◽  
John Grocott ◽  
Ken J.W. McCaffrey ◽  
Mike A. Hamilton

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Chadwick, B., Garde, A. A., Grocott, J., McCaffrey, K. J., & Hamilton, M. A. (2000). Ketilidian structure and the rapakivi suite between Lindenow Fjord and Kap Farvel, South-East Greenland. Geology of Greenland Survey Bulletin, 186, 50-59. https://doi.org/10.34194/ggub.v186.5215 _______________ The southern tip of Greenland is underlain by the Palaeoproterozoic Ketilidian orogen (e.g. Chadwick & Garde 1996; Garde et al. 1998a). Field investigations in the summer of 1999 were focused on the structure of migmatites (metatexites) and garnetiferous granites (diatexites) of the Pelite Zone in the coastal region of South-East Greenland between Lindenow Fjord and Kap Farvel (Figs 1, 2). Here, we first address the tectonic evolution in the Pelite Zone in that region and its correlation with that in the Psammite Zone further north. Then, the structure and intrusive relationships of the rapakivi suite in the Pelite Zone are discussed, including particular reference to the interpretation of the controversial outcrop on Qernertoq (Figs 2, 8). Studies of the structure of the north-eastern part of the Julianehåb batholith around Qulleq were continued briefly from 1998 but are not addressed here (Fig. 1; Garde et al. 1999). The field study was keyed to an interpretation of the Ketilidian orogen as a whole, including controls of rates of thermal and tectonic processes in convergent settings. Earlier Survey field work (project SUPRASYD, 1992–1996) had as its principal target an evaluation of the economic potential of the orogen (Nielsen et al. 1993). Ensuing plate-tectonic studies were mainly funded in 1997–1998 by Danish research foundations and in 1999 by the Natural Environment Research Council, UK. The five-week programme in 1999 was seriously disrupted by bad weather, common in this part of Greenland, and our objectives were only just achieved. Telestation Prins Christian Sund was the base for our operations (Fig. 2), which were flown with a small helicopter (Hughes MD-500).


Author(s):  
Feiko Kalsbeek ◽  
Lilian Skjernaa

NOTE: This article was published in a former series of GEUS Bulletin. Please use the original series name when citing this article, for example: Kalsbeek, F., & Skjernaa, L. (1999). The Archaean Atâ intrusive complex (Atâ tonalite), north-east Disko Bugt, West Greenland. Geology of Greenland Survey Bulletin, 181, 103-112. https://doi.org/10.34194/ggub.v181.5118 _______________ The 2800 Ma Atâ intrusive complex (elsewhere referred to as ‘Atâ granite’ or ‘Atâ tonalite’), which occupies an area of c. 400 km2 in the area north-east of Disko Bugt, was emplaced into grey migmatitic gneisses and supracrustal rocks. At its southern border the Atâ complex is cut by younger granites. The complex is divided by a belt of supracrustal rocks into a western, mainly tonalitic part, and an eastern part consisting mainly of granodiorite and trondhjemite. The ‘eastern complex’ is a classical pluton. It is little deformed in its central part, displaying well-preserved igneous layering and local orbicular textures. Near its intrusive contact with the overlying supracrustal rocks the rocks become foliated, with foliation parallel to the contact. The Atâ intrusive complex has escaped much of the later Archaean and early Proterozoic deformation and metamorphism that characterises the gneisses to the north and to the south; it belongs to the best-preserved Archaean tonalite-trondhjemite-granodiorite intrusions in Greenland.


2015 ◽  
Vol 36 (4) ◽  
pp. 437-443 ◽  
Author(s):  
Aziza Lansari ◽  
Miguel Vences ◽  
Susanne Hauswaldt ◽  
Ralf Hendrix ◽  
David Donaire ◽  
...  

We assessed the genetic variation of 47 Moroccan populations of the North African water frog (Pelophylax saharicus) using partial sequences of the mitochondrial cytochrome oxidase subunit I gene (COI). All 239 samples belonged to the main haplotype clade previously identified from Morocco, with no haplotypes of the Algerian/Tunisian clades among our samples. Altogether 40 haplotypes were found, with a maximum of 13 mutational steps between them. Two weakly divergent haplogroups separated by a minimum of six mutational steps were distributed (i) in the Anti-Atlas and the Sahara (south of the High Atlas Mountains) versus (ii) in the Middle Atlas, the High Atlas, and in the Rif area north of the Atlas Massif. Haplotypes of the northern haplogroup were found at the southernmost locality, which might be due to human translocation, and co-occurrence of the two haplogroups was recorded at three sites within the range of the northern haplogroup.


2016 ◽  
Vol 19 (2) ◽  
pp. 265-286 ◽  
Author(s):  
GUILLAUME LETURCQ

Abstract The environmental impacts of hydroelectric dams in Brazil are investigated in local and regional scales, for the last years. In this paper, we analyze the impact than the establishment of a hydroelectric dam has for the people and their spaces, with the comparative experiences occurred for the North and South of Brazil. We will focus on aspects related to the organization of families, social fight, the compensation and resettlement of people affected by the dam's construction, as well we take a look to the similarities between the two areas, with emphasis on aspects related to migration, mobility and landscapes. For this, we rely on research carried out on the river Uruguay (South), based on interviews, questionnaires and studies of primary and secondary sources, from 2007 to 2014 and also in a survey that is currently being held in Belo Monte area (North), which also uses primary and secondary sources, with fieldwork periods.


Koedoe ◽  
1995 ◽  
Vol 38 (2) ◽  
Author(s):  
A.J. Viljoen

All observations and data related to the impact of the 1991/92 drought on the woody vegetation, excluding the riverine vegetation of major rivers, are summarised. This includes data from a visual estimate of damage from aerial photographs, surveys on selected sites, and general observations. Despite lower rainfall, the area north of the Olifants River (excluding the far-northern part) was less affected than the area south of it, suggesting that the woody vegetation in the north is more adapted to drought. A characteristic of the drought was the localised distribution pattern and variable intensity of damage to the same species in the same general area. Information on 31 species are presented briefly. Although a large number of woody species was to some extent damaged, when the woody vegetation is considered as a whole, the influence of the drought was not very severe.


1967 ◽  
Vol 16 (1) ◽  
pp. 13-22 ◽  
Author(s):  
Ellen F. Luedemann

In February-March 1963, during the Equalant Operation for the ICITA program, 476 drift-bottles were released at the equatorial waters off the northern Brazilian coast (01ºS to 09ºN and 043ºW to 053ºW). Thirty-five, bottles were recovered (7,4%). Those were classed in five groups according to their different velocity ranges and areas of recovery (Trinidad Island; Lesser Antilles; Caribbean and Florida area; north Brazil; northeastern Brazil). The recoveries of bottles released within 300 nm off the northern and northeastern coast of Brazil confirmed a strong current along the north and northeast coast in northwestern direction (South Equatorial Current and branches). In late February-early March the bottles showed maximum velocities of this current (3,6 knots). The region off the northern coast of Brazil, between 05ºN and 09ºN up to 050ºW seems to have been under the influence of an eastward component of the surface current in this same period, while at late March this influence appears to have been weaker. In the region from Trinidad Island to Yucatan Peninsula the current seems to be stronger on the northeastern side of the Caribbean Sea.


Starinar ◽  
2015 ◽  
pp. 197-220
Author(s):  
Nadezda Gavrilovic-Vitas ◽  
Bojan Popovic

During June and July 2014, at the site of Zadruzni Dom in Skelani, archaeological investigations of the late antique building were carried out, whose rooms were first discovered in the course of archaeological excavations in 2008. The building has a rectangular base, of a northeast-southwest orientation, with the discovered part measuring 20.90 x 30.90 m. What is distinguishable within the asymmetrical base is an entrance, along with eleven rooms, two of which have apses, and a peristyle, i.e. an inner courtyard with a roofed corridor surrounding it which connects all the rooms of the building. During the archaeological excavations, entrance thresholds and extremely well preserved mortar floors with mortar skirting were noted in most rooms, along with traces of fresco painting on the walls and mosaic floors, executed in the opus tesselatum technique, observed in several rooms, the peristyle and the encompassing corridor. The discovered mosaic fragments are decorated with geometric motifs in the form of a swastika, a Solomon?s knot, a square, a rhomboid, overlapping circles, etc. and floral motifs of ivy and petals, as well as a double braid motif. Small but, unfortunately, fragmented pieces of a mosaic with a figural representation were discovered in the central part of the peristyle, while the mosaic in room K was decorated with a motif portraying the winged head of Medusa. Two construction phases were noted, an older and a younger, with the walls, which were two Roman feet wide and built from dressed stone, and the older mortar floor belonging to the older construction phase, and the second, younger construction phase comprising mosaics, fresco painting, the younger mortar floor and two furnaces. Contemplating the planimetry of the building, one gets the impression of the rooms being divided between two parts - public and private, whereby the public part of the building would be located near the main entrance hall and would comprise rooms A, B, C, D and F, with mortar floors and traces of fresco painting on the walls. The other, possibly private, part of the building would include five rooms G, H, I, J and K and the inner courtyard. Rooms I, J and K had floor and wall heating, while rooms G and H had an arched apse and possibly functioned as a reception hall and/or a stibadium. The hallway with mosaics, which flanks the inner courtyard, was most likely roofed. Traces of burning in the north-western corridor testify to the destruction of the building in a fire. Based on the architectural elements and the traces of fresco painting and mosaics in the building at the site of Zadruzni Dom in Skelani, it can be deduced that this is a late antique building which can roughly be dated to the period between the end of the 3rd and the mid-4th century AD, and whose lavish decoration implies that it was owned by an affluent resident of Skelani from the aforementioned period.


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