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Indigenous peoples, rural and peasant populations, and Afro-descendants have increasingly disputed mining and other extractive ventures in the territories they inhabit in various regions of Latin America. This article introduces an open-access digital and bilingual curated repository of data that compiles legal and legal-like actions by various actors in the context of paradigmatic conflicts over mining in Central America and Mexico. It situates the relevance of this digital resource against the background of the increasing global recourse to law in socioenvironmental conflicts—a tendency that may be defined as the juridification of environmental politics. The article also places the database in relation to key debates in digital humanities and discusses potential uses as well as future developments and challenges to expanding and improving such a resource.
Ideal for researchers and practitioners looking for fresh approaches to transport problems, this book combines cutting-edge qualitative and qualitative knowledge to inform transport futures. It uses engaging case studies based in The Gambia and the US to show how and why a transdisciplinary approach can result in better planning decisions.
This chapter focuses on how urban development relates to riverine flood risk. It begins with an overview of flooding and related riverine processes (e.g., sediment transport, floodplain formation, channel migration). It then presents the urban development and flood histories of Vienna (Austria) on the Danube and Calgary (Canada) on the Bow River, including the latter’s 2013 flood disaster. The cases are assessed and compared using the Urban Risk Dynamics framework. Vienna and Calgary demonstrate several key themes, including the “levee effect.” Each city’s relationship with the river has been one of technological control, intensifying over time. During periods of major population growth, flood protection investments are made that allow the city to expand into hazard lands. Once set in motion, the reliance on technology for flood protection becomes self-reinforcing, difficult to reverse as more of the city comes to depend on it. Over time, there is a loss of collective memory about flood risk. The role of government becomes increasingly important. Disaster events lead to learning and adaptation but do not fundamentally alter processes of urban development that give rise to risk.
This chapter focuses on how urban development relates to coastal flood risk. It begins with key concepts related to coastal geomorphology and flooding in river deltas and estuaries (e.g., processes of landscape formation, protective benefit of wetlands, storm surge, human impacts on coastlines). It then presents the urban development and flood histories of New Orleans (including Hurricane Katrina) and New York City (including Hurricane Sandy). The cases are assessed and compared using the Urban Risk Dynamics framework. Both demonstrate how urbanization in coastal cities often entails extensive loss of wetlands, construction of navigational waterways that inadvertently funnel storm surge, and floodplain expansion through land subsidence or building out the waterfront. Urban expansion into more hazardous lands may be intentionally enabled through construction of flood protection structures. Generally, the least economically valuable land was occupied by the most socially vulnerable populations. Catastrophic events like Hurricanes Katrina and Sandy spur mitigation but reinforce ongoing urbanization trends. Lower density areas, however, provide opportunities for strategic retreat.
Cities are economic entities. Their location, functioning, growth, decline, and internal structure are all heavily influenced by economic forces. This chapter draws from the fields of urban economics, economic geography, and regional science in order to present some core concepts of urban growth and change organized around three questions: Why are cities where they are? What drives urban growth and change? And how does a city grow across a landscape? Foundational concepts (e.g., first and second nature, competition between cities, agglomeration economies, density gradients, transport technology and urban form, the monocentric city model, nonmarket forces) are explained narratively and illustrated through examples from cities around the world. A key message is that the economic logic of urban development is constrained by geography, enabled by technology, and shaped by human institutions, including urban planning. The chapter emphasizes that the urban built environment at risk from hazards is a tangible accumulation of the city’s economic history.
This chapter focuses on how urban development relates to earthquake risk. It draws connections between earthquakes and floods, then introduces key technical concepts (e.g., magnitude v. intensity, liquefaction, structural response to shaking). It presents the urban development and disaster histories of Kobe (Japan; including the 1995 earthquake) and Christchurch (New Zealand; including the 2010–2011 Canterbury earthquake sequence), assessing and comparing them using the Urban Risk Dynamics framework. Findings resonate with themes from the flood chapters. Urbanization often involves modifying lands (e.g., draining wetlands, expanding waterfronts, constructing islands), which are susceptible to ground failure in earthquakes. While newer structures are less prone to damage because of technological and building code advances, many older buildings are concentrated in neighborhoods that are hotspots of physical and social vulnerability. Postdisaster reconstruction and recovery accelerate prior trends. Catastrophic events trigger learning and instigate diversification in risk reduction strategies. Retreat from hazard lands is possible, as exemplified in Christchurch’s residential red zone.
In order to understand how urban disaster risk changes, it is essential to understand how cities change. This chapter argues that cities are continually evolving entities whose past and present dynamics provide insights into future trends and possibilities. The chapter first reviews global trends in disaster losses, along with well-established definitions and frameworks about disaster risk. It explains why these are inadequate for understanding how a city’s disaster risk changes over time. It then proposes a simple conceptual framework, the Urban Risk Dynamics framework, to help guide empirical study of evolving disaster risk in any city. The framework is based on several premises: that local geography, or landscape, is vital to understanding urban disaster risk; that cities must be understood as economic entities; and that technological change is a key driver of urban change. The chapter then introduces and justifies the selection of the six case studies to be analyzed using the framework in Chapters 3–5.
The concluding chapter provides a synthesis and reflection on insights from this book. It first summarizes the main findings regarding how disaster risk today is a legacy of urban history, drawing on salient examples from the six case study cities and cautioning that risk becomes very “path dependent” as future options are constrained by past decisions. After discussing limitations of the study and further research needs, the chapter suggests that the Urban Risk Dynamics framework and findings from the six cases are relevant to any city, demonstrating this for Vancouver (Canada). It then reflects on the practical significance of the book. It argues that the findings demonstrate why disaster risk and risk reduction should be viewed dynamically; why understanding risk should start with the city, not the hazard or disaster; and why interdisciplinary approaches are critical for reducing risk. Recognizing this can help analysts, planners, and policy-makers, for example, to not only identify current risk hotspots but anticipate future ones, to consider risk from a multihazard standpoint, and to develop strategies and solutions that are effective in the long term.
This book examines the specific manifestations and causes of housing precarity across a diverse range of geographic settings and housing types. Chapters offer fresh insights into how housing affects wellbeing in terms of physical and mental health, identity and participation in communities.
The prehistoric human habitation of the Tibetan Plateau (TP) is well evidenced by the archaeological record, but poorly constrained in time and space. To test the plausibility of in situ survival during the last glacial maximum (LGM) and the coldest periods of the Pleistocene, this paper gauges the effects of LGM conditions and varying local ice coverage on the climate. Three different climate model scenarios are generated, and their outputs are used to drive vegetation simulations. This allows us to evaluate 10 archaeological sites that show evidence of human activity either pre- or post-LGM as possible human refugia. The results show that the higher the level of ice coverage on the plateau, the colder and drier the climate becomes, and barren unproductive land extends farther south. However, there are sites that remain habitable in all scenarios, with the southern and northeastern plateau identified as the areas with the highest likelihood of refugia during the LGM, specifically at the locations of Baishiya Karst Cave and Siling Co. There is a high probability of the TP being habitable during the LGM, as even the scenario with the most ice yields some regions with favourable conditions that are within the habitability criteria.
Mandibular and dental material of hyaenids from the Central Asian localities of Zasukhino-3 (Russia) and Nalaikha (Mongolia), dating to the late Early Pleistocene (0.9–0.78 Ma) was identified as giant hyena Pachycrocuta brevirostris based on morphological and size similarities. Comparative analysis of Eurasian P. brevirostris from different stratigraphic levels (from 2.1 to 0.5 Ma) revealed two evolutionary stages of the lower cheek teeth of the giant hyenas. The stages are determined as morphotypes A and B, directed toward the differentiation of the function of premolar and enhancing the cutting function of m1. We traced the microprocesses that occurred during the transition from the primitive structure of the m1 talonid to its more advanced state. This event occurred during the transition from the late Villafranchian to the Epivillafranchian (ca. 1.1–0.9 Ma). The stabilized advanced morphotype B was found in samples from Zasukhino-3, Nalaikha, and other close-in-age localities such as Lakhuti-2. The new finds from Asian Russia and Mongolia suggest that P. brevirostris from these regions represent a single giant hyena population occupying the northernmost part of their Asian range.
Fields of sandy paleodunes have been identified in Brazil, Colombia, Venezuela, and Guyana north of the South American continent. In this study, geochronological data obtained by optically stimulated luminescence (OSL) for paleodunes in the Middle Rio Negro region (Brazil) allowed the identification of two stages of dune deposition: the older from 169.74 ± 1.01 ka to 124.38 ± 0.91 ka and the younger from 18.89 ± 0.88 ka to 14.75 ± 0.77 ka. The older interval is the first reported in the Amazon; no correlated sediment has been documented. In contrast, the more recent depositional interval correlates to the interval of paleodune fields of the region called “dry corridor” in the Late Pleistocene–Holocene. In this study, we associated the genesis of paleodunes with the reworking of alluvial deposits from the Negro and Demini rivers, driven by river seasonality during the Pleistocene–Holocene, as evidenced by characteristic microtextural data.
Thus far it is evident that the rural livelihoods in southern Morang are embedded within a deeply inequitable agrarian structure, with dual surplus appropriation by landlords and merchant capital. However, it is important to remember that feudalism, like capitalism itself, is not a static system, but is dynamic and subject to evolution and flux. While changes to the feudal system over the last few centuries were explored in Chapter 3, this chapter explores the contemporary trajectory of change. The last three decades in particular have marked a new era in Nepal's agrarian political economy. As noted earlier in this book, pre-capitalist inequalities have not been undermined, and these in part contributed to the 10-year civil war and waves of more recent ethnic unrest. However, at a national level, Nepal has also undergone significant economic change following neoliberal restructuring.
Within this context, capitalism is articulating with rural pre-capitalist economic formations like never before. A key argument is that there is growing ‘agrarian stress’ associated with climatic-ecological pressures, expanding capitalist markets with an associated wave of monetisation and cultural change. In its wake, farmers are becoming more dependent than ever before on off-farm labour in the capitalist sector both locally and overseas, to supplement the meagre returns gained from the land under feudal agriculture This has intensified throughout the 17 years within which this research has taken place. We explore these changes in turn below.