Respectable Rags: Working-Class Poverty and the 1913–14 Southern Colorado Coal Strike

This article uses the events of the 1913–14 Southern Colorado Coal strike and the cooperative work of the Colorado Coalfield War Archaeology Project to explore emergent historical narratives of working-class poverty and the role they play in shaping contemporary ideologies and public policy. It uses clothing as an entrée into discussions of the deserving and undeserving poor, and asks how competing groups used dress in the context of the 1913–14 southern Colorado coal strike to fashion subjects in particular ways. In so doing, it demonstrates the ineffectiveness of either-or dichotomies of deserving and undeserving that still influence current public policy.     

Poverty in the Modern City: Retrospects and Prospects

The outcome of over fifteen years research on large urban assemblages from the Australian cities of Sydney and Melbourne is discussed in terms of approaches to the archaeology of the modern city as they have evolved over the period. To better understand the archaeology of urban poverty we require innovations in both methods and ideas, the most far-reaching being a transnational archaeology of urban poverty founded on the analysis of migration, consumption and class formation.     

Transformative Transportation: The Early Twentieth-Century Railroad on the Southwest Florida Frontier

The Venice Train Depot is a case study for an archaeology of transportation, an examination of new places and more rapid travels over the modern period. The goal of this approach is to capture the dynamics of landscapes, agency, and movement. There have been productive discussions of transportation networks and national integration; methodological discussions have noted the need to account of the movement of things in the analysis of the material record. The case study exposes the dynamics of change for the Florida frontier in the twentieth century focused on the construction of a railroad line and station in Venice, Florida.     

A Trip to the Mountains: Travel and Social Relations in the Catskill Mountains of New York

The Catskill Mountains in upstate New York have been a tourist destination since the early nineteenth century. At a superficial level, the history of Catskill tourism follows a basic trajectory from elite destination in the nineteenth century to more inclusive tourist area in the twentieth century. This trajectory incorporates a “trickle down” theory of tourism and leisure that masks the complexity of changes in social relations. Jewish tourism in the Catskills evidences how class, ethnic, and gender relations intertwined in the creation of a specific place—the Borscht Belt. Archaeology in the Borscht Belt places tourism within larger capitalist relations in America and complicates concepts of tourism as consumption and leisure.     

An Archaeology of Community Life: Appalachia, 1865–1920

Archaeology has the potential to contribute significant information about community building in the lives of former enslaved laborers. In this article, I consider the role of race and racism in the creation, maintenance and material manifestation of community in post-emancipation Appalachia.     

Creating a Diasporic Archaeology of Chinese Migration: Tentative Steps Across Four Continents

This article calls for a specific form of comparative inquiry within historical archaeology as drawn from diaspora studies. Such a project encourages archaeologists to compare research from emigrant areas alongside work at overseas sites. This diasporic approach provides new potentials for engaging with the modern world by intersecting with both traditional and new aspects of archaeological practice. In order to showcase these aspects of a diasporic approach, the author explores three case studies from Montana, Peru, and New Zealand – connecting each to its related home area. The case studies explore how data drawn from a group’s homeland can support established heritage practices, engage with modern social problems, and illuminate complexities arising within sites based on ethnolinguistic differences within populations.     

Record of the meso- and neoholocene palaeoenvironmental changes in the Jesionowa landslide peat bog (Beskid Sądecki MTS. Polish Outer Carpathians)

The paper presents an analysis of depositional sequences of landslide peat bog situated in the depressions developed within the landslide landforms Jesionowa in the Beskid Sądecki Mts. (Outer Carpathians). The peat bog, with depositional sequence 2.80 m long, started to form at the beginning of the Atlantic Phase ca. 6390–5910 cal BC. Palynological and lithological analyses as well as several (14) radiocarbon age determinations of different horizons in the sediments enabled the reconstruction of palaeoenvironmental changes during the Meso-and Neoholocene. The increase in climate humidity at the beginning of the Subboreal and Subatlantic Phases was observed as delivery of minerogenic material to the peat bog basin and formation of a mineral horizon and an illuvial level within the peat. The particularly intensive delivery of allochthonous material to the peat bog took place at the beginning of the Subboreal Phase and was the result of both significant humid climate and increased human impact (colonization of the Funnel Beaker Culture) in the landslide area. Similar influence of younger colonisations of landslide area (Przeworsk Culture and, later, Valachian colonisation) was also recorded within the deposits of peat bog (illuvial and mineral horizons) in the early Subatlantic Phase. Rejuvenation of the landslide zone and formation of the younger landslide were connected with the increase in climate humidity at the beginning of the Subboreal Phase. The peat bog deposits situated within this younger landslide, which are ca. 1.8 m thick, are significantly contaminated with mineral material.     

Stability of IRSL signals from sedimentary K-feldspar samples

Recent work has identified IR stimulated luminescence signals at elevated temperature from both potassium- and sodium-rich feldspars that have much lower anomalous fading rates than the conventional signal measured using IR stimulation at 50°C. This paper examines the stability of these signals for potassium-rich sedimentary feldspars. We show that the natural post-IR IRSL (pIRIR) signal from a 3.6 Ma old sample is in apparent saturation on a laboratory generated dose response curve, i.e. it does not show detectable fading in nature although a low fading rate is observed on laboratory time scales. We show that the pIRIR signal has a greater thermal stability than the IRSL signal and that the trend in increasing thermal stability is mirrored by a decreasing fading rate. We also investigate the effect of preheat temperature and IR stimulation power on the decay shape and conclude that the data can be explained in terms of either a single- or multiple-trap model. We present evidence that may suggest that at least part of pIRIR signal is derived from a high temperature trap (∼550°C thermoluminescence (TL) peak), although again the data can also be explained in terms of a single-trap model. Finally, we present dose response curves and characteristic curvature constants (D₀) values for various IRSL signals and conclude that the more stable signals saturate more quickly than the less stable signals and that the initial and final signals saturate at approximately the same level.     

Holocene marine ingressions in the coastal zone of the pomeranian bay based on radiocarbon assays

In recent years, a team at the Geology and Paleogeography Unit, Marine Sciences Institute, University of Szczecin, has been performing geological, geochronological and paleogeographic surveys in (i) the Szczecin Lagoon and Świna Gate Sandbar and (ii) the estuary section of the Rega river valley near Mrzeżyno. These studies have helped to examine and identify not only the distribution of fossil marine sediments but also their lithological and sedimentological characteristics. The age of marine ingressions and regressions in the coastal zone of the Pomeranian Bay were determined using approximately 170 radiocarbon assays.