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Abstract

Although the recent publication of the results of excavation and restoration in the Siq at Petra by the Petra National Trust has thrown welcome light on the hydraulic engineering skills of the Nabataeans, it is suggested here that the conclusions reached by the authors regarding the chronology of those works are not necessarily correct and should not be accepted as definitive. It is shown that the interpretation of the ceramic evidence is faulty and that other, epigraphic, evidence is ignored. In particular, it is argued that the major works — the dam and the tunnel — as well as the paved road through the Siq, may be as late as, or even later than, the middle of the 1st century AD, rather than the late 1st century BC, as the authors assume. It is further suggested that this could also be the date of the Khazneh, and that this may be indicated also by the recent discovery of earlier tomb façades beneath the Khazneh.  相似文献   
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The explosive eruption at Santorini in the Aegean Sea during the second millennium BCE was the largest Holocene volcanic upheaval in the Eastern Mediterranean region. The eruption was disastrous for the Minoan settlements at Santorini, but the effect on human society in the neighbouring islands and regions is still clouded in uncertainty. Tsunami generation was suggested, but comparatively little evidence was found. The lack of firm tsunami traces is particularly puzzling in Crete with its coastal settlements of the Late Minoan IA period, during which the Santorini eruption occurred. Here, we report the discovery of extensive geoarchaeological tsunami deposits at Palaikastro in north-eastern Crete. These deposits are characterized by a mixture of geological materials, including volcanic Santorini ash, and archaeological settlement debris. Various tsunami signatures were identified: (1) erosional contact with the underlying strata, (2) volcanic ash intraclasts in the lower part of the deposit, (3) reworked building stone material in the lower part of the deposit, (4) individual marine shells, (5) marine micro-fauna, (6) imbrication of rounded beach pebbles, settlement debris, ceramic sherds and even bones, (7) multi-modal chaotic composition. Late Minoan human settlement activities at Palaikastro provided architectural and stratigraphic frameworks in space and time that recorded and preserved tsunami evidence as geoarchaeological deposits. Such stratigraphic resolution and preservation may not occur in the natural landscape. Volcanic ash transported by wind from Santorini south-east to Crete preceded the tsunami. Geological, archaeological and radiocarbon dating criteria all converge, indicating that the tsunami deposits are coeval with the Minoan Santorini eruption. Field evidence suggests that tsunami waves at Palaikastro were at least 9 m high. Inverse tsunami modeling was attempted, based on these newly discovered tsunamigenic deposits. The initial wave in the generation region at Santorini that best fits the stratigraphic data is a wave with +35 to −15 m initial amplitude and a crest length of about 15 km.  相似文献   
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Dana Hercbergs  Chaim Noy 《对极》2015,47(4):942-962
This article analyses a recent ideological shift in the visual management of Jerusalem. Through two case studies in the real estate and tourism industries we show how mobile technologies are shaping both actual settings in, and visual consumption of, Jerusalem. The analysis points at the creation of a “tunnel vision” for consumers and visitors, which promotes Jewish hegemony in the city and simultaneous detachment from Palestinian spaces and histories. This tunnel vision situates the viewers in physical and simulated enclaves within the city, creating a relationship of distance and elevation to promote their embodied identification with Israel's Judaizing mission for the area, primarily the Holy Basin. This mode of viewing Jerusalem is evocative of Israel's post‐second intifada policies and the concurrent rise of right‐wing ideologies, which relegate to the margins alternative readings of the contested urban landscape.  相似文献   
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Drawing on ethnographic fieldwork, this article explores two widespread types of informal and precarious work in eastern India's coal mining tracts. It seeks to contribute to recent attempts to disaggregate the umbrella notion of precarity and the related concept of ‘classes of labour’ in the context of the global South. It does so by illuminating the more nuanced yet significant relative distinctions between different forms of precarious coal-related work as perceived and experienced by labourers. The article illustrates how labourers evaluate such forms of work in relation to one another in terms of relative stability, autonomy, tempo and gender dynamics, which affect their livelihood decisions and activities. It thereby turns attention to differentiating dimensions of precarious work that are easily veiled in broad debates about precarity and ‘classes of labour’. Such dimensions are essential to probe — through comparative ethnographic study — to understand how people engage with different modalities of precarious work on the ground and how they configure their livelihood strategies in particular capitalist and social contexts.  相似文献   
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