The coastal landslides of Shetland

Little is known of hard-rock coastal landsliding in Scotland. We identify 128 individual coastal landslides or landslide complexes >50 m wide along the coasts of Shetland. Most are apparently translational slides characterized by headscarps, displaced blocks and/or debris runout, but 13 deep-seated failures with tension cracks up to 200 m inland from cliff crests were also identified. Thirty-one sites exhibit evidence of at least localized recent activity. Landslide distribution is primarily determined by the distribution of coastal cliffs >30 m high, and they are preferentially developed on metasedimentary rocks. Analysis of 16 landslides on Fetlar (NE Shetland) indicates that most are translational dip-slip failures; 3 represent deep-seated failures and several exhibit active frontal erosion attributable to basal sapping by storm waves. As these landslides terminate in shallow water, failure was probably initiated when rising sea level resulted in footslope erosion and upslope propagation of instability, causing downslope displacement of landslide blocks on upper slopes. ¹⁰Be exposure dating of two headscarps yielded ages of 4.8?±?0.2 ka and 4.4?±?0.2 ka, consistent with the onset of footslope erosion as sea level rose. Our results suggest that landslides have played a hitherto undocumented but important role in retreat of cliffed coastlines in Scotland.     

Local knowledge is required: a rhythmanalytical approach to the late Mesolithic and early Neolithic of the East Anglian Fenland, UK

This is a paper about blurring the boundaries between people, land and water in the past and of appreciating the importance of the wider environment in our accounts of prehistory. Maritime approaches to time/space are shown to offer new ways of looking at how people engage with the world around them. Informed by these approaches, and building on Lefebvre’s concepts of lived space and rhythm, current tensions within archaeology between cartesian and phenomenological approaches to the past will be shown to be unconstructive. These issues are all addressed in relation the late Mesolithic and early Neolithic of the East Anglian Fenland. Here a rhythmical, maritime approach will be shown to offer us a subtly different view of life during this period.     

The last outpost of Empire: Rockall and the Cold War

This paper is about what can be seen at sea. It considers the historical geography of a site at the geopolitical axis of the British Empire and the Cold War. It focuses on a hitherto unacknowledged historical reference point: the last territorial expansion of the UK, which laid claim to the tiny islet of Rockall, lying some 300 miles west of the Scottish mainland. Rockall was annexed in September 1955 because it was situated within radio-electrical range of a test site for Britain's first nuclear missile, the American-made ‘Corporal’. As a ‘tactical’ nuclear missile designed for potential deployment in Eastern Europe, the Corporal was a central part of NATO defence policy in the 1950s. Crucial to its development was a testing station in the Outer Hebrides, from which the guided missile could be fired and its ballistic trajectory tracked over the North Atlantic. Occupying an area only 83 feet across and 100 feet wide, Rockall represented a strategic vantage point for the rival gaze of Soviet intelligence. Following Paul Virilio's argument that the logic of war is less about scoring territorial or material victories than about securing ‘the “immateriality” of perceptual fields’, this paper details the ceremonial annexation of Rockall and the subsequent transformation of the Hebridean seascape into a vast topography for military surveillance. This final expansive moment of British imperialism was legitimated by symbolic and rhetorical strategies tying Rockall to both earlier geographical exploration and the science of natural history.     

Ecological livelihoods of farmers and pollinators in the Himalayas: Doing critical physical geography using citizen science

In farming communities dependent on the cultivation of pollinator-dependent crops, the livelihoods of farmers are inextricably linked with pollinator health. A global pollination crisis interlinked with a crisis of food production and farmer livelihoods, exacerbated by processes of socio-environmental change, is emblematic of the Anthropocene and of the kinds of ecosocial problems with which critical physical geography (CPG) engages. We propose examining the farmer-pollinator system in the Indian Himalayas through an ecological livelihoods approach using a range of collaborative citizen science methods including bloom observations to document pollinator visits, plant phenological observations to document year-round floral resource availability, and farm diaries to document orchard management practices. An ecological livelihoods approach draws on posthumanist theory, which has remained largely disengaged with methodological questions that are of concern to CPG. Citizen science, although widely used across a range of disciplines, has seen limited engagement in CPG. After elaborating some of the opportunities and challenges that an engagement between CPG, posthumanist theory, and citizen science opens up, we propose a methodology that would be simultaneously epistemological (understanding interdependence between livelihoods of farmers and pollinators) and ontological (imagining and building worlds where farmer and pollinator habitats are recomposed).     

The Preservation and Interpretation of δ34S Values in Charred Archaeobotanical Remains

The measurement of sulphur isotope (δ³⁴S) values in charred plant remains has the potential to inform understanding of the spatial configuration and ecology of crop production. We investigated the effects of charring, manuring, oxidation and anaerobic soil conditions on modern cereal grain/pulse seed δ³⁴S values, and assessed the effect of chemical pre‐treatment on charred modern and archaeobotanical grain/seed δ³⁴S values. We used these results to interpret δ³⁴S values in archaeobotanical material from Neolithic Çatalhöyük. Our results suggest that δ³⁴S values can be reliably preserved in charred grain/seeds but are subject to influence by anaerobic soil conditions, the effect depending on the timing of flooding in relation to S assimilation.