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1.
Archaeological studies on olive oil produced in Crete in the Bronze Age focus primarily on aspects such as the period when olive cultivation became widespread, the number of olive trees cultivated, or the quantity of oil stored in the Minoan palaces. Olive oil is however an organic substance, a perishable product, the nutritional and storage properties of which are determined by environmental, agronomic, processing and storage conditions. In this paper archaeological, environmental and biochemical evidence is combined to present a comprehensive picture of the potential quality, nutritional and storage properties of Minoan olive oil. The comparative evidence presented suggests that Minoan olive oil was equal in quality to the cold-pressed virgin olive oils produced today, and as such, the oil was nutritionally important in the Bronze Age and a valuable trade commodity.  相似文献   

2.
Summary.   The palaces are the most distinctive feature of the Minoan civilization, although their functions and meanings remain enigmatic. This paper explores these inhabited monuments with the application of a phenomenological approach. By constructing a series of categories based on data collected from all the entrances, not just the main ones, we can highlight the myriad everyday experiences encountered upon approaching and entering them. Categories based on function, yet also sensitive to experiential qualities of the use of space, are utilized in order to draw out the varied ways in which people perceived four different Minoan palaces (Knossos, Malia, Phaistos and Zakros).  相似文献   

3.
The microstructures and chemical compositions of some 15 faience objects from Crete spanning the period from Middle Minoan IIIA through to Late Minoan IA are determined using analytical scanning electron microscopy. The Minoan faience is compared with replicate faience beads produced in the laboratory using various combinations of manganese, copper and iron as colorants. The alkali contents of the replicate beads are varied so that the colorants are present both as ions in a glass phase and as particulate oxides. These data are then used to try to infer the original colour of the Minoan faience, the great majority of which has suffered severe weathering during burial. The results suggest that instead of the present day “hallmark greys and browns” and “subtle greens and blues”, Minoan faience originally exhibited a wide range of colours, including bright turquoise blue, purple and violet, and pale yellow-green and greenish turquoise.  相似文献   

4.
This study is a step forward in understanding the palaeoenvironmental effects of the Minoan eruption of Santorini (1627–1600 BCE). We employ geostatistics to produce a prediction map for the thickness of the tephra fallout over the Eastern Mediterranean, and we reconstruct the effects by comparisons with recent eruption analogues. Based on the geostatistical map, the amount of environmental disruption over so far undocumented areas is estimated by comparison with archaeological sites where emplaced Minoan tephra has been recorded before. Nevertheless, independent field evidence suggest that the environment responded differently in places, occasionally posing challenges to the presented interpolation. A second line of evidence coming from contemporaneous fluvial archives provides clues for a widespread ‘Minoan flood’ over a large part of the Eastern Mediterranean, associated with the eruption itself. This simultaneous hydrological event may have had a counterbalancing effect on the impacts of the Minoan tephra cover, and could explain the sporadic discrepancies between the predicted effects and the palaeoenvironmental evidence. Traces of the effects of this extraordinary volcanic event are also sought in the regional Late Bronze Age literature.  相似文献   

5.
6.
Summary.  This paper uses Middle Minoan architecture to explore the degree to which the conceptualization and reconstruction of the First Palaces on Crete have been unduly influenced by the model of the Minoan palace as the centralized political, economic and religious authority. It is generally assumed that this model, first formulated on the basis of the LM II–III palace at Knossos, also serves to explain the First Palaces despite the fact that relatively little attention has hitherto been paid to their external and internal characteristics. Detailed reassessment of the available data strongly suggests that the First Palaces differed from their Late Bronze Age counterparts in several important ways. Particularly striking is the absence of so-called 'palatial' architectural features (e.g. ashlar masonry, Minoan Hall, Lustral Basin, etc.), which hitherto had been thought to form an integral part of the First Palaces. Rather, the earliest evidence for these architectural features seems to be found in elite residences in settlement contexts (e.g. Malia). This observation urges a reassessment not only of the term 'palatial' architecture but also of the nature and location of power in Middle Bronze Age Crete and the role played by architecture as a medium of elite conspicuous consumption.  相似文献   

7.
The formation of reference groups comprises an important procedure in chemical provenance studies of archaeological pottery. Material from ancient kilns is thought to be especially suitable for reference groups, as it comprises a definite unit of past production. Pottery from the Late Minoan IA kiln excavated at Kommos, Crete was analysed in order to produce a reference group in this important area of Minoan ceramic production. The samples were characterized by a combination of techniques providing information on the chemistry, mineralogy and microstructure of the ceramic body. Initially, the study was unable to establish, in a straightforward manner, a chemical reference group. Different ceramic pastes and a range of selective alterations and contaminations, affected by variable firing temperatures and burial environment, were shown to be responsible for the compositional variability. Procedures are described to compensate for such alterations and the perturbations in the data that they produce.  相似文献   

8.
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   

9.
Five deposits of Santorini tephra have been found in the excavations currently under way at the site of Mochlos which lies on the north coast of Crete about 140 km to the south of Santorini. This paper provides refractive index and trace element analyses for the largest of these deposits, examines the stratigraphy of all five deposits, and notes the chronological implication of this stratigraphy for the Late Minoan IB period, the floruit of Minoan civilization.  相似文献   

10.
Abstract

The sandstone quarry at Mochlos is one of four major quarries in eastern Crete that were worked during the New Palace Period of Minoan civilization (ca. 1700–1450 B.C.) to produce large ashlar blocks for nearby Minoan sites. At that time sandstone, or ammoudha, as it is known locally, was especially valued as a building material, partly because of its distinctive color and texture, but mainly because of the ease with which it could be cut, and the stone was used extensively for exterior façades, for walls around interior courts, and for other architectural features of the more important buildings on these sites. This article describes the quarry at Mochlos in some detail, including the quarrying techniques employed, and argues that the destination of the stone from the Mochlos quarry was the Minoan palace at Gournia. The article ends with a comparison of the four ammoudha quarries in eastern Crete.  相似文献   

11.
P. M. WARREN 《Archaeometry》1987,29(2):205-211
A recent argument for raising the absolute date of the beginning of the Aegean Late Bronze (LB) Age to about 1700 B.C. is critically examined. It is argued here that: (1) the alabaster lid from Knossos did have the strati-graphical context assigned to it by Evans, in all probability Middle Minoan IIIA, c. 1650 B.C.; (2) the attempt to date the alabastron found in an early Eighteenth Dynasty context at Aniba to Late Minoan IIIA:1 is open to objections; (3) radiocarbon dates from Aegean LB I contexts are too wide in their calibrated ranges and too inconsistent both within and between site sets to offer any reliable grounds at present for raising Aegean LB I absolute chronology to 1700 B.C. Other evidence, however, suggests this period began about 1600 B.C., i.e. some fifty years earlier than the conventional date of 1550 B.C.  相似文献   

12.
Summary.   This article publishes an Archaic Greek cup of individual form from the extramural sanctuary of the Achaian colony of Sybaris at Francavilla Marittima in south Italy. The Francavilla cup, which is Achaian or Achaian-style, is fully discussed and similar Archaic cups from the site of Incoronata, near the Achaian apoikia of Metapontion, are assembled. These vessels find no immediate parallel among contemporary Greek or indigenous pottery of the seventh and earlier sixth centuries BC, but bear a remarkable similarity to the characteristic cylindrical, so-called Vapheio cups of the Aegean Bronze Age which are known in metal, clay and stone versions from as early as the Early Minoan III period through the Late Helladic era. It is argued that these cups represent the Archaic creation or re-creation of a well-known Bronze Age shape in the Achaian apoikiai of south Italy.  相似文献   

13.
The Minoan Terracotta pipes with their conical shape were widely used in the water distribution system in the ancient Minoan civilization. They remain one of the brightest achievements of the Minoan tribe in water supply technology and raise admiration as well as many questions about the technological advancements of antiquity, that are yet to be understood. The present work aims at answering the following questions: a) what inspired the Minoans to manufacture pipes with such a peculiar shape, that differs greatly not only from later pipe designs of antiquity, but also from contemporary cylindrical pipes and b) why was the design of those pipes abandoned after the fall of the Minoan civilization? It tries to address these questions by investigating the flow physics and dynamics that take place in such pipes, adopting advanced numerical and computational methods. The time-averaged Navier–Stokes equations along with the k − ? turbulence model are solved for a variety of geometrical parameters, pipe orientations and flow rates, in order to produce a comparative picture of the hydraulic efficiency of the conical Minoan pipes. The flow field is visualized and critical flow parameters, such as the head loss, the velocity magnitude and turbulence intensity, are calculated. These calculations show clearly that the conical Minoan pipes exhibit significantly higher pressure drops along their length compared to an equivalent straight pipe. In their widest part an extended recirculation appears, which could wash out impurities that may be present in the water, which at the same time cannot be deposited on the pipe wall. This evidence proves that the Minoan pipes are energetically expensive to operate and consequently their replacing by cylindrical pipes was inevitable. Therefore, it seems that the main advantage and purpose of the particular geometry was that they could be easily connected on site, forming long straight or slowly bending lines without having to add straight or many different fittings in between.  相似文献   

14.
Summary. This paper analyses coffin use in the tombs of Late Bronze Age Crete in terms of both mortuary traditions on the island and regional variations in cultural practices. It argues that the revival of coffin use in the Final and Post-palatial periods (in ceramic terms, Late Minoan II–IIIB) constituted a recourse to an earlier burial custom within negotiations of rapidly changing mortuary practices across the island. However, this ‘re-invention’ involved significant modifications to the form and significance of the coffin. The paper then explores spatial variations in choices of coffin types, as one potential window onto the issue of intra-island regionalism in social and cultural practices.  相似文献   

15.
This paper reconsiders the ‘Temple House’, a building excavated in 1969–70 on the Temple terrace of the site of Lato in eastern Crete. While the building was dated to the Hellenistic (HL) period and identified as domestic space by the excavator, a restudy of the material from the excavation, combined with an examination of the excavation notebooks, and observations on site, reveal a more complex history of use, unusual architectural details, and a heterogeneous range of dates (from Late Minoan (LM) IIIC to HL) and functions, suggesting original funerary and post‐funerary cult contexts. It is possible to recognize the remains of a Subminoan (SM)/Protogeometric (PG) burial and evidence for an Early Iron Age (EIA) and HL tomb cult, allowing a reconsideration of the history of Lato and the process of city‐state formation in eastern Crete.  相似文献   

16.
The historic landscape of Orchha in Central India, once the capital of the Bundela Rajputs from 1531 to 1783 CE, was read as an oracle promising well-being and affording protection. Site readings and mappings of the landscape show that the built environment was visualized as a concrete embodiment of archetypal imagery of cosmic mountain and pillar, mandala and yantra, and sites of the epic Ramayana. Design strategies for envisioning, or reading this auspicious landscape, consisted of deliberate location and orientation of temples and palaces, interior surfaces as spaces of representation of narrative imagery, and spatial transposition. Today this visual structure is illegible due to abandonment, encroachment, and new development as a result of increasing number of pilgrims and tourists. Grounded speculation from site studies of the cultural landscape is proposed as the frame for reclaiming the lost heritage. Preserving view sheds and planning heritage trails will amplify the hidden visual structure of Orchha and suggest the reconciliation of myth and history.  相似文献   

17.
Climate deterioration at around the time of the Bronze Age/Iron Age transition has for long been argued to have resulted in upland abandonment in northern and western Britain, and recent research has provided evidence that a major climate downturn from 850 cal BC caused settlement abandonment in western Europe and potentially worldwide. It is, however, unclear to what extent only ‘marginal’ sites were affected, due to the lack of any systematic attempt to view the evidence for settlement and land-use change across a range of landscape types with differing sensitivities to environmental change. This paper addresses this issue by an evaluation of 75 pollen sequences spanning the late Bronze Age and early Iron Age in Britain to assess whether climatic deterioration was sufficient to cause widespread land abandonment. The results provide no evidence for wholesale land-use change at this time; the overall picture is one of continuity of land use or even increased agricultural activity. There are, however, hints of regional variability, with a greater tendency to abandonment of upland areas in Wales, and signs of woodland regeneration in agriculturally productive areas of lowland central southern England. The latter pattern may reflect a combination of rising ground-water levels affecting local land-use in the immediate vicinity of the mires which provide the source of the pollen data, against a backdrop of regional-scale social and economic changes at the Bronze Age-Iron Age transition.  相似文献   

18.
This paper reexamines the archaeological evidence for three episodes of rural abandonment and resettlement in the countrysides of Late Roman Greece (200–700 CE): an abandoned Late Hellenistic-Early Roman countryside (second century BCE to third century CE), a decline in the third to early fourth centuries CE, and the Dark Age beginning in the seventh century CE. The first and third episodes of abandonment, especially, have sharply defined Late Antiquity (250–700 CE) as a healthy period of new rural settlement and economic resurgence, and the entire pattern has been described in the terms of “boom-and-bust” demographic and economic cycles. Closer readings of the archaeological data can contribute to more sensitive pictures of continuity and change in settlement and connectivity in the late antique Corinthian countryside and other regions in Greece.  相似文献   

19.
In a series of recent studies, changes in material culture and settlement pattern in the Late Glacial of Northern Europe have been linked to the eruption of the Laacher See volcano. This eruption occurred c. 13,000 years ago towards the end of the Allerød chronozone. It is argued that the tephra fall-out from this eruption set in motion significant demographic fluctuations along the northern periphery of Late Glacial human settlement and that these led to a number of material culture transformations. In particular, the emergence of the regionally distinct techno-complexes with large tanged points – the Bromme culture in southern Scandinavia and the Perstunian culture in northeastern Europe – and the temporary abandonment of central European regions are thought to relate to this eruption. While numerous archaeological datasets are in accord with this ‘Laacher See hypothesis’, the forcing mechanism or mechanisms that brought about these archaeologically visible changes have remained largely unexplored. A particular challenge is to explain how some of the culture-historical effects of the Laacher See eruption seem to change or become more pronounced with distance from the eruptive centre. We here investigate one potential middle-range link between the Laacher See eruption and Late Glacial fauna and foragers: tephra as dental abrasive. We use instrumented nanoindentation to quantitatively investigate tephra from a number of sites covering the medial and distal fall-out zones as well as the dental enamel of Homo sapiens and key prey species of Late Glacial foragers. Our results show that the Laacher See tephra contained particles roughly twice as hard as even the hardest portions of any of the teeth investigated. We also suggest that fluoride-induced weakening of dental enamel may have further aggravated tooth wear. These mechanisms may have acted in concert to produce elevated levels of, in particular, animal mortality, which in turn may have led to an abandonment of the affected landscapes.  相似文献   

20.
During the second millennium BC , the Minoan civilization was established in the southern Aegean Sea. In Minoan art, especially on Crete, birds occupied a prominent place, and were often represented in wall-paintings and craft objects. Species still occurring on the island, such as cormorants, mallards, cuckoos, owls, hoopoes, and swallows, as well as exotic taxa such as partridges and possible domestic forms such as pigeons, were the subject of artistic inspiration, and they were depicted not only in purely cult contexts, but also in the backgrounds of naturalistic landscapes. The aim of this paper is to reconsider the identification of some of the birds depicted and to discuss them in the context of the environmental conditions and osteological finds from the southern Aegean islands in Minoan times. © 1997 John Wiley & Sons, Ltd.  相似文献   

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