Etienne Wismer Glaciers do not only consist of ice. In their porous spaces, they contain mineral particles, oxygen, and, ultimately, snow and water. Carl Ludwig Hackert’s Vue de la Source de l’Arveron (1781) shows a glacier crisscrossed by meltwater streams and numerous erratic blocks (Fig. 1). Hackert’s depiction embodies the…
Making Sense of Ice? Engaging Meltwater in the Long Eighteenth Century in Switzerland and France
