Selling green militarization: The discursive (re)production of militarized conservation in the Virunga National Park,Democratic Republic of the Congo

In recent years, the militarization of nature conservation has intensified, especially in protected areas located in conflict zones or plagued by ‘poaching crises’. Such ‘green militarization’ is enabled by a range of discursive techniques that allow it to be seen as a ‘normal’ and ‘legitimate’ response. This article analyzes these techniques in relation to the Virunga National Park, located in the war-ridden east of the Democratic Republic of the Congo, where militarized approaches to conservation have a long lineage. It demonstrates that many of the discursive techniques that are currently at play show strong continuities with the past. These include moral boundary-drawing grounded in colonial tropes that accomplish the (racial) Othering of poachers and rebels, and the long-established practice of invoking states of emergency as part of wider mechanisms of securitization. However, the rise of neoliberal conservation, with its emphasis on marketing and marketization, has induced transformations in the employed discursive techniques. Notably, it has intensified the spectacularization of militarized conservation and anchored it in everyday consumer practices, by actively inviting individual supporters to directly fund militarized interventions, thus generating ‘militarization by consumption’. This shows that ‘green militarization’ is not only driven by the growing commodification of nature conservation, but is increasingly subject to commodification itself.     

Thick lava flows of Karisimbi Volcano, Rwanda: insights from SIR-C interferometric topography

 We use a digital elevation model (DEM) derived from interferometrically processed SIR-C radar data to estimate the thickness of massive trachyte lava flows on the east flank of Karisimbi Volcano, Rwanda. The flows are as long as 12 km and average 40–60 m (up to >140 m) in thickness. By calculating and subtracting a reference surface from the DEM, we derived a map of flow thickness, which we used to calculate the volume (up to 1 km³ for an individual flow, and 1.8 km³ for all the identified flows) and yield strength of several flows (23–124 kPa). Using the DEM we estimated apparent viscosity based on the spacing of large folds (1.2×10¹² to 5.5×10¹² Pa s for surface viscosity, and 7.5×10¹⁰ to 5.2×10¹¹ Pa s for interior viscosity, for a strain interval of 24 h). We use shaded-relief images of the DEM to map basic flow structures such as channels, shear zones, and surface folds, as well as flow boundaries. The flow thickness map also proves invaluable in mapping flows where flow boundaries are indistinct and poorly expressed in the radar backscatter and shaded-relief images. Received: 6 September 1997 / Accepted: 15 May 1998