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Journal ArticleDOI

Crisis in Context: The End of the Late Bronze Age in the Eastern Mediterranean

A. Bernard Knapp, +1 more
- 01 Jan 2016 - 
- Vol. 120, Iss: 1, pp 99
TLDR
The authors reviewed the current state of the archaeological and historical evidence and considered the coherence of climatic explanations and overprecise chronologies in attempting to place the "crisis" in context.
Abstract
Explanations for the Late Bronze Age crisis and collapse in the eastern Mediterranean are legion: migrations, predations by external forces, political struggles within dominant polities or system collapse among them, inequalities between centers and peripheries, climatic change and natural disasters, disease/plague. There has never been any overarching explanation to account for all the changes within and beyond the eastern Mediterranean, some of which occurred at different times from the mid to late 13th throughout the 12th centuries B.C.E. The ambiguity of the evidence—material, textual, climatic, chronological—and the differing contexts involved across the central-eastern Mediterranean make it difficult to disentangle background noise from boundary conditions and to distinguish cause from effect. Can we identify the protagonists of the crisis and related events? How useful are recent explanations that focus on climate and/or chronology in providing a better understanding of the crisis? This article reviews the current state of the archaeological and historical evidence and considers the coherence of climatic explanations and overprecise chronologies in attempting to place the “crisis” in context. There is no final solution: the human-induced Late Bronze Age “collapse” presents multiple material, social, and cultural realities that demand continuing, and collaborative, archaeological, historical, and scientific attention and interpretation. This article is available as open access on (AJA Online).

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Citations
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Journal ArticleDOI

Up the Wadi: Development of an Iron Age Industrial Landscape in Faynan, Jordan

TL;DR: In 2014, the Edom Lowlands Regional Archaeology Project renewed excavations at Khirbat al-Jariya (KAJ), an Iron Age copper smelting site in Faynan, Jordan.
Journal ArticleDOI

Severe multi-year drought coincident with Hittite collapse around 1198–1196 bc

TL;DR: This paper examined the collapse of the Hittite Empire around 1200 BC and identified an unusually severe continuous dry period from around 1198 to 1196 (±3) BC, potentially indicating a tipping point, and signals the type of episode that can overwhelm contemporary risk-buffering practices.
Journal ArticleDOI

Land use, climate change and ‘boom-bust’ sequences in agricultural landscapes: Interdisciplinary perspectives from the Peloponnese (Greece)

TL;DR: In this article, the authors studied changes in both the extent and intensity of land use in NE Peloponnese, Greece, across more than two thousand years, from the end of the Middle Bronze Age to Roman times (~1800 BCE-330 CE).

Digital Palace of Nestor: Assessing Mycenaean Palatial Complex Construction of Socio-Political Status and Navigation Through Architecture

Caleb Ward
TL;DR: In this paper, the authors combine experiential and spatial syntax techniques to gain a deeper understanding of how Mycenaeans shaped space to construct status and navigation in the Palace of Nestor at Pylos.
References
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Journal ArticleDOI

Long-Term Aridity Changes in the Western United States

TL;DR: Using gridded drought reconstructions that cover most of the western United States over the past 1200 years, it is shown that this drought pales in comparison to an earlier period of elevated aridity and epic drought in AD 900 to 1300, an interval broadly consistent with the Medieval Warm Period.
Journal ArticleDOI

Asian monsoon failure and megadrought during the last millennium.

TL;DR: The Monsoon Asia Drought Atlas (MADA), a seasonally resolved gridded spatial reconstruction of Asian monsoon drought and pluvials over the past millennium, derived from a network of tree-ring chronologies, provides a long-term context for recent monsoon variability that is critically needed for climate modeling, prediction, and attribution.
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